{"meta":{"query_hash":"100143cf9cb9","filters":{"topic":"earthquake and tectonic studies"},"cohort_total":2613,"direct_labels_cover":0,"predictions_cover":2613,"exported":2613,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/100143cf9cb9","api":"https://metacan.xera.ac/api/v1/cohort?topic=earthquake+and+tectonic+studies"},"results":[{"id":"W1058075183","doi":"10.1016/j.tecto.2015.07.013","title":"Identifying low-frequency earthquakes in central Cascadia using cross-station correlation","year":2015,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Division of Earth Sciences; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Seismology; Waveform; Subduction; Autocorrelation; Geodesy; Tectonics; Telecommunications; Statistics","score_opus":0.051941324645205636,"score_gpt":0.2798684445410503,"score_spread":0.2279271198958447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1058075183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99849486,0.00004420617,0.00052103895,0.000027291051,0.000004685023,0.0000049532673,0.00031120863,0.000029120714,0.0005626687],"genre_scores_gemma":[0.9989355,0.000025905356,0.00027763745,0.00000407413,0.0000041375383,0.0000035607927,0.00047617103,0.0000043728883,0.00026870842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997135,0.000049783215,0.00003181468,0.00010033313,0.000042250584,0.0000622676],"domain_scores_gemma":[0.998456,0.0003872137,0.00027169535,0.00015143612,0.00048557427,0.0002480107],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005960492,0.00043256962,0.00029823216,0.002637854,0.0005826201,0.0007111361,0.00042482832,0.00045258668,0.0010787854],"category_scores_gemma":[0.002563197,0.0002693805,0.00031136893,0.0024852303,0.00027315726,0.00045335852,0.00070436136,0.00027713855,0.00029283966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000100562705,0.000066631765,0.978394,0.000024720051,0.00010835379,0.00017700413,0.0003810927,0.004699236,0.004086002,0.00011732409,0.00038584622,0.0114593],"study_design_scores_gemma":[0.0000041702015,0.000017973543,0.9914825,0.000003375825,0.000027815891,0.000020653577,0.0002510476,0.007789139,0.00018053471,0.000035238518,0.00018141491,0.00000611676],"about_ca_topic_score_codex":0.08448546,"about_ca_topic_score_gemma":0.15415858,"teacher_disagreement_score":0.08448546,"about_ca_system_score_codex":0.00061617733,"about_ca_system_score_gemma":0.00076409685,"threshold_uncertainty_score":0.1679874},"labels":[],"label_agreement":null},{"id":"W1093500","doi":"","title":"Vertical Anatolian Movements Project (VAMP): a collaborative research project of the TopoEurope initiative of ESF","year":2009,"lang":"en","type":"article","venue":"EGUGA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geography; Political science; Archaeology","score_opus":0.08302186866207148,"score_gpt":0.34022966361898627,"score_spread":0.2572077949569148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1093500","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.58093536,0.01199017,0.015050664,0.013253676,0.0015192529,0.0006233289,0.1376157,0.0016420634,0.23736976],"genre_scores_gemma":[0.7662053,0.0036142992,0.04800365,0.00053343613,0.00017671262,0.000542813,0.08780897,0.0008642568,0.0922505],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99964106,0.00011712381,0.00001582781,0.00007068479,0.000092262475,0.00006302702],"domain_scores_gemma":[0.9992805,0.00009493389,0.00011367929,0.00008064744,0.0002964952,0.00013379999],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010500721,0.000498558,0.00028246705,0.00093189435,0.0005032456,0.0009703079,0.0005350411,0.0004051379,0.007928477],"category_scores_gemma":[0.0012808223,0.00012608214,0.00015512858,0.000992442,0.00032185327,0.0005457581,0.0010531688,0.00029944387,0.0017063835],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014673476,0.00027154412,0.12762128,0.0006744095,0.00019943112,0.0006499274,0.001677248,0.003214088,0.006197716,0.032376554,0.18507284,0.64057755],"study_design_scores_gemma":[0.00020177747,0.00025554904,0.3056304,0.000299534,0.00008455216,0.00053791003,0.0020638644,0.004751662,0.004213868,0.0037409358,0.67819697,0.000022970939],"about_ca_topic_score_codex":0.037293445,"about_ca_topic_score_gemma":0.038629018,"teacher_disagreement_score":0.037293445,"about_ca_system_score_codex":0.0015507768,"about_ca_system_score_gemma":0.00472363,"threshold_uncertainty_score":0.07415271},"labels":[],"label_agreement":null},{"id":"W111264519","doi":"","title":"Numerical modelling concepts for tsunami warning systems","year":2006,"lang":"en","type":"article","venue":"Current Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Indian ocean; The arctic; Tsunami wave; Continental shelf; Oceanography; Amplitude; Arctic; Seismology; Climatology; Geography; Physics","score_opus":0.04454511982510061,"score_gpt":0.2876801910186692,"score_spread":0.24313507119356859,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W111264519","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0021333636,0.0065712887,0.95638514,0.0017565533,0.0008298371,0.00013343414,0.00032880955,0.00043593705,0.03142566],"genre_scores_gemma":[0.21956483,0.01743399,0.71170616,0.00095647335,0.0020648106,0.0014327548,0.0012820577,0.00043735886,0.04512154],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987337,0.0003926762,0.00011786533,0.00016475002,0.00052345614,0.000067507346],"domain_scores_gemma":[0.9988587,0.0004037963,0.00013227502,0.00012768505,0.00042343873,0.000054161654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019559313,0.0013918072,0.00074317364,0.001504253,0.0008221572,0.0028430882,0.0018572083,0.0016834385,0.008046643],"category_scores_gemma":[0.0035199898,0.0005147122,0.0011463151,0.0014737099,0.0019512223,0.0028501495,0.0021930898,0.0029644084,0.0027250266],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010902852,0.000014537074,0.00014654003,0.0002084739,0.000016885733,0.00008138901,0.00028073037,0.11198585,0.0013525798,0.850568,0.006889882,0.028444195],"study_design_scores_gemma":[0.000015432359,0.000024031795,0.00010441584,0.00020791093,0.000013227279,0.00012979192,0.00009207068,0.3399479,0.000656292,0.4799034,0.1788771,0.000028423188],"about_ca_topic_score_codex":0.0029520444,"about_ca_topic_score_gemma":0.0014567829,"teacher_disagreement_score":0.008046643,"about_ca_system_score_codex":0.0016509121,"about_ca_system_score_gemma":0.0011854476,"threshold_uncertainty_score":0.026918769},"labels":[],"label_agreement":null},{"id":"W1140552005","doi":"10.1007/s00024-015-1127-5","title":"On the Leading Negative Phase of Major 2010–2014 Tsunamis","year":2015,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Ocean Service; National Oceanic and Atmospheric Administration; Russian Science Foundation","keywords":"Geology; Seismology; Series (stratigraphy); Phase (matter); Tide gauge; Deep sea; Sampling (signal processing); Pacific ocean; Oceanography; Climatology; Paleontology; Sea level; Computer science; Physics; Detector","score_opus":0.027675006330210236,"score_gpt":0.23527300763560402,"score_spread":0.2075980013053938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1140552005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97218657,0.0002119321,0.00017406927,0.0016154442,0.00018298182,0.000005325503,0.0010746396,0.000007573493,0.024541466],"genre_scores_gemma":[0.99723583,0.000114024486,0.000026987253,0.00008918981,0.000039843362,0.0000021176022,0.00059125543,0.000004135449,0.0018965662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999232,0.0000099685085,0.0000035157566,0.0000129763785,0.000015227235,0.000035090423],"domain_scores_gemma":[0.9994411,0.00011389214,0.00012409924,0.000018119097,0.00017750917,0.0001252325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023747378,0.0001672247,0.00010772591,0.00043279876,0.00050084165,0.0007602293,0.00018292635,0.0003724635,0.00838259],"category_scores_gemma":[0.0019090327,0.0000793983,0.00010179442,0.00044449113,0.00037708625,0.00048739323,0.0007884589,0.00069773215,0.0006385259],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004044677,0.00026856072,0.82238984,0.00021145795,0.00014751646,0.00079196185,0.0029872796,0.008552487,0.005414772,0.04618603,0.0402423,0.06876315],"study_design_scores_gemma":[0.00002515925,0.00014186476,0.97339004,0.00009499693,0.000040792416,0.00009118409,0.0036975322,0.0029256695,0.00052024523,0.004044441,0.015012412,0.00001564808],"about_ca_topic_score_codex":0.022633404,"about_ca_topic_score_gemma":0.08794818,"teacher_disagreement_score":0.022633404,"about_ca_system_score_codex":0.0006151863,"about_ca_system_score_gemma":0.00061459234,"threshold_uncertainty_score":0.045003355},"labels":[],"label_agreement":null},{"id":"W129338705","doi":"10.3133/ofr20091263","title":"Sizes of the largest possible earthquakes in the central and eastern United States— Summary of a workshop, September 8–9, 2008, Golden, Colorado","year":2009,"lang":"en","type":"article","venue":"Antarctica A Keystone in a Changing World","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Estimation; Seismic hazard; Geography; Seismology; Geological survey; Commission; Geology; Political science; Engineering; Law; Geophysics","score_opus":0.01597018087356836,"score_gpt":0.23445414610556653,"score_spread":0.21848396523199817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W129338705","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.16169229,0.09540019,0.018487323,0.30225518,0.056054845,0.0034412104,0.03471462,0.001244627,0.32670978],"genre_scores_gemma":[0.320217,0.07001457,0.013419061,0.01747884,0.016504679,0.0025607038,0.039556954,0.0007262492,0.51952195],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993274,0.00008715705,0.000048940405,0.00021054738,0.00019437252,0.00013152229],"domain_scores_gemma":[0.9972156,0.00029041403,0.00014297426,0.00006740332,0.0016091786,0.0006744361],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003722904,0.0013489068,0.0005346844,0.001294976,0.0042326665,0.0026498379,0.0015515456,0.002397302,0.016864454],"category_scores_gemma":[0.0022522737,0.00089402427,0.00054728985,0.00083482894,0.00065697334,0.0019413789,0.0025772525,0.0024767006,0.0042256946],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002565254,0.00018904648,0.008785431,0.0004911809,0.000031731404,0.00056360377,0.0030678336,0.0007431362,0.0014916805,0.0009091945,0.9007056,0.08276505],"study_design_scores_gemma":[0.00007421375,0.00032791612,0.067334026,0.0016656012,0.000054914697,0.00035595856,0.018281082,0.00095273403,0.0016452163,0.001550657,0.90766245,0.000095266354],"about_ca_topic_score_codex":0.10139719,"about_ca_topic_score_gemma":0.24852648,"teacher_disagreement_score":0.10139719,"about_ca_system_score_codex":0.0036041099,"about_ca_system_score_gemma":0.003938762,"threshold_uncertainty_score":0.20161396},"labels":[],"label_agreement":null},{"id":"W133870503","doi":"10.1007/978-3-319-06874-9_9","title":"Quantitative Stratigraphy, Splining and Geologic Time Scales","year":2014,"lang":"en","type":"book-chapter","venue":"Quantitative geology and geostatistics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Stratigraphy; Geology; Geologic time scale; Physical geography; Paleontology; Geography; Sedimentary rock","score_opus":0.02793642649270288,"score_gpt":0.24949947371242812,"score_spread":0.22156304721972525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W133870503","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.060641,0.043460958,0.65250224,0.0038745324,0.000784359,0.000079165526,0.0031440214,0.0011232633,0.23439045],"genre_scores_gemma":[0.5785959,0.027830575,0.19187751,0.0006864269,0.00086281745,0.00014467289,0.0024957967,0.000886534,0.1966198],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996779,0.000056846064,0.000015469413,0.000092604205,0.00014092016,0.00001623362],"domain_scores_gemma":[0.99912363,0.0004836106,0.000108224966,0.00011358169,0.00014397809,0.000026883863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072108576,0.00053825154,0.00027900471,0.0010803867,0.00017922063,0.0023275998,0.0006966614,0.00049407315,0.007682052],"category_scores_gemma":[0.003535342,0.00041580028,0.00026365655,0.0019190557,0.0016062695,0.0027104162,0.00044588948,0.0011715061,0.0012013665],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030740124,0.000028183014,0.003976376,0.00039253134,0.000032269894,0.000042129635,0.0005247888,0.013145895,0.0059103896,0.7138017,0.0122959325,0.24981914],"study_design_scores_gemma":[0.0000070378874,0.000046413574,0.016247924,0.0001307046,0.000030505342,0.0001913402,0.00042323058,0.03343074,0.0031649228,0.8184609,0.12783241,0.000033757995],"about_ca_topic_score_codex":0.0029164874,"about_ca_topic_score_gemma":0.004325368,"teacher_disagreement_score":0.007682052,"about_ca_system_score_codex":0.0010092268,"about_ca_system_score_gemma":0.0006812305,"threshold_uncertainty_score":0.02569902},"labels":[],"label_agreement":null},{"id":"W134539922","doi":"10.21236/ada449981","title":"Evaluation of Cross-Correlation Methods on a Massive Scale for Accurate Relocation of Seismic Events in East Asia","year":2006,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Relocation; Seismology; Scale (ratio); Geology; East Asia; Geography; Computer science; Cartography; China; Archaeology","score_opus":0.10954587696161998,"score_gpt":0.4032568094564916,"score_spread":0.2937109324948716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W134539922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6870465,0.00049164577,0.30456465,0.00022566173,0.00009061854,0.00023824506,0.0010641604,0.0031585856,0.0031199493],"genre_scores_gemma":[0.71132904,0.00015619067,0.28573418,0.00006391477,0.000040244737,0.00012724104,0.0018300541,0.000214168,0.00050499325],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9976755,0.0009212098,0.00023601316,0.00049846864,0.0005057166,0.00016324739],"domain_scores_gemma":[0.98419005,0.0077814483,0.0011384614,0.002586587,0.0038633505,0.00044003667],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00788798,0.0009452052,0.0005609425,0.002310881,0.0006625121,0.0010631826,0.0013278119,0.0007508379,0.0016345482],"category_scores_gemma":[0.023019481,0.00038146263,0.0006101351,0.0023424022,0.00046815912,0.001412491,0.0019605472,0.0006353314,0.0006172927],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009526517,0.00059363246,0.10917715,0.00031508761,0.0006176964,0.00044905077,0.00054915476,0.39241564,0.018284813,0.00475013,0.0046786414,0.4672163],"study_design_scores_gemma":[0.000049468064,0.0001398162,0.01915231,0.000017322714,0.000046967016,0.000097920994,0.00021000711,0.97126657,0.007308791,0.000770805,0.0009221809,0.000017766384],"about_ca_topic_score_codex":0.009926456,"about_ca_topic_score_gemma":0.010417764,"teacher_disagreement_score":0.009926456,"about_ca_system_score_codex":0.00061010453,"about_ca_system_score_gemma":0.0014390649,"threshold_uncertainty_score":0.0417161},"labels":[],"label_agreement":null},{"id":"W138516669","doi":"10.4401/ag-3618","title":"Some preliminary results of a worldwide seismicity estimation: a case study of seismic hazard evaluation in South America","year":2000,"lang":"en","type":"article","venue":"Annals of Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Seismology; Geology; Seismic moment; Seismic hazard; Moment magnitude scale; Maximum magnitude; Magnitude (astronomy); Subduction; Hazard map; Geodesy; Fault (geology); Tectonics; Geometry; Scaling; Mathematics","score_opus":0.052017104068144596,"score_gpt":0.29478100014615055,"score_spread":0.24276389607800597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W138516669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954,0.00008248235,0.0028127825,0.00006268372,0.0000016293052,0.000024734609,0.0002966491,0.000023613185,0.0012954558],"genre_scores_gemma":[0.9959273,0.000101072634,0.0027149268,0.000008355472,0.0000032529335,0.000015992973,0.00058930495,0.000014138375,0.0006258216],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996032,0.00020446074,0.000028203245,0.000053966054,0.00006310439,0.000047021258],"domain_scores_gemma":[0.9982224,0.0010827332,0.00025091236,0.00012492544,0.0002344363,0.00008452909],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010768679,0.00050704804,0.00029356676,0.0019212535,0.00028567913,0.0005431662,0.0002813047,0.00033691636,0.0015029832],"category_scores_gemma":[0.0057530063,0.00012369687,0.00028868817,0.0028915629,0.0003773662,0.0005884778,0.00078408176,0.0002342524,0.00012463744],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038885794,0.00028253807,0.81921864,0.00021492825,0.00022369473,0.0026483475,0.0056541255,0.055211637,0.004354473,0.0016436516,0.0013551291,0.108804],"study_design_scores_gemma":[0.00004559826,0.00038919903,0.9177634,0.000052448497,0.00017375607,0.00072405714,0.012243199,0.059657466,0.002757118,0.0011121618,0.0050218184,0.000059791113],"about_ca_topic_score_codex":0.038152535,"about_ca_topic_score_gemma":0.06894918,"teacher_disagreement_score":0.038152535,"about_ca_system_score_codex":0.0006196234,"about_ca_system_score_gemma":0.00026708707,"threshold_uncertainty_score":0.07586092},"labels":[],"label_agreement":null},{"id":"W1442504365","doi":"","title":"Carbonates in thrust fault: high temperature investigations into deformation processes in calcite-dolomite systems","year":2012,"lang":"en","type":"article","venue":"The EGU General Assembly","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Dolomite; Calcite; Geology; Mineralogy; Carbonate; Carbonate minerals; Materials science; Metallurgy","score_opus":0.01732757777195728,"score_gpt":0.22732183656323973,"score_spread":0.20999425879128245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1442504365","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999213,0.00017727971,0.0001963573,0.0000069365265,0.0000011791661,0.0000049429086,0.00004052263,0.0000029036476,0.00035687184],"genre_scores_gemma":[0.99942005,0.00010618193,0.00024951124,0.0000039105175,0.0000016100472,0.000004037326,0.000055219476,0.0000025291506,0.00015686611],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99988914,0.000010495823,0.0000066188372,0.000023655815,0.000040035797,0.000030006453],"domain_scores_gemma":[0.9998963,0.000022539873,0.000028067461,0.000009685101,0.000025146483,0.000018348324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014982397,0.00019395296,0.0001613469,0.00027989058,0.000290274,0.00024277225,0.00018310381,0.00014487536,0.0010876666],"category_scores_gemma":[0.0001939317,0.00012567188,0.000113576316,0.00028862432,0.00031416886,0.0002322318,0.00018376003,0.00024645127,0.00008285098],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009644451,0.000019511583,0.0051710103,0.00004899704,0.0000070609617,0.00004577365,0.0001066592,0.0001902046,0.99316025,0.00004157762,0.000006684126,0.0011056347],"study_design_scores_gemma":[0.000018276663,0.00035255423,0.13209762,0.00000960175,0.000020529573,0.0001892443,0.00029485972,0.0021836066,0.86386603,0.000054614953,0.0009011357,0.000012083823],"about_ca_topic_score_codex":0.0035513989,"about_ca_topic_score_gemma":0.006828316,"teacher_disagreement_score":0.0035513989,"about_ca_system_score_codex":0.00027573959,"about_ca_system_score_gemma":0.00018115916,"threshold_uncertainty_score":0.007061422},"labels":[],"label_agreement":null},{"id":"W1481510234","doi":"10.1007/978-94-010-0093-2_39","title":"Characteristics of Several Tsunamigenic Submarine Landslides","year":2003,"lang":"en","type":"book-chapter","venue":"Advances in natural and technological hazards research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"","keywords":"Landslide; Submarine landslide; Geology; Submarine; Seismology; Seafloor spreading; Oceanography","score_opus":0.025860656714065813,"score_gpt":0.2887514841159527,"score_spread":0.2628908274018869,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1481510234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99328387,0.0001923684,0.0004494151,0.000012170981,0.000004923579,0.000011256253,0.0008341071,0.000022802229,0.0051890733],"genre_scores_gemma":[0.9975036,0.00009106588,0.0002145626,0.0000047792846,0.0000056471517,0.000005407097,0.0007861573,0.0000093339795,0.0013794366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996424,0.0000023408693,0.000003582129,0.00000914385,0.000012440025,0.000008251867],"domain_scores_gemma":[0.9996176,0.00009377255,0.000098463606,0.000018301167,0.000121926074,0.00005003693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009448361,0.00016332962,0.00012570653,0.0015256766,0.00023998896,0.00037091164,0.00017698563,0.00018200527,0.0016930776],"category_scores_gemma":[0.00037649824,0.00010225079,0.000113985894,0.0012466807,0.00015237715,0.00020161377,0.00012916615,0.0001037394,0.0003021821],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011555334,0.00015274738,0.7752956,0.00016262758,0.00009563756,0.0019513943,0.0013855032,0.008021661,0.13584843,0.0022576118,0.0022276677,0.07144551],"study_design_scores_gemma":[0.000010078333,0.00013413705,0.98881966,0.00000614333,0.00003224359,0.00089939113,0.00040977608,0.0018794468,0.005657632,0.00023948002,0.0019019875,0.000010123647],"about_ca_topic_score_codex":0.0030259297,"about_ca_topic_score_gemma":0.0040251478,"teacher_disagreement_score":0.0030259297,"about_ca_system_score_codex":0.00019032529,"about_ca_system_score_gemma":0.000095589494,"threshold_uncertainty_score":0.006016612},"labels":[],"label_agreement":null},{"id":"W1481671034","doi":"","title":"International Year of Planet Earth 7. Oceans: Submarine Landslides and Consequent Tsunamis in Canada","year":2009,"lang":"en","type":"article","venue":"Geoscience Canada","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Landslide; Submarine landslide; Geology; Submarine; Continental margin; Continental shelf; Seismology; Oceanography; Tectonics","score_opus":0.00721418706120384,"score_gpt":0.1741322180281806,"score_spread":0.16691803096697677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1481671034","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0046540056,0.03452921,0.0011810364,0.015142369,0.04410894,0.0003086028,0.28858122,0.0035712114,0.60792345],"genre_scores_gemma":[0.041542053,0.049162056,0.0022525338,0.0036338365,0.0053411033,0.00020797632,0.32642838,0.002232118,0.5691999],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.999161,0.000019070192,0.000032161268,0.000053876018,0.00049076264,0.00024312544],"domain_scores_gemma":[0.99631256,0.00006679235,0.00014055402,0.0001687134,0.0023213709,0.0009900983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008451065,0.0013084755,0.0008270642,0.0063930084,0.0036170478,0.008519753,0.0014968514,0.0013873581,0.09544998],"category_scores_gemma":[0.0025518613,0.00041881105,0.0006133897,0.013661082,0.0010883517,0.002547646,0.0037138879,0.0022719144,0.039469764],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023946059,0.000011163109,0.0017072399,0.0003052092,0.000008776584,0.00006091501,0.000090771486,0.00013686715,0.00011915846,0.0016356283,0.9677184,0.028181883],"study_design_scores_gemma":[0.000002949113,0.0000035590128,0.007246265,0.00012695561,0.0000043252035,0.00002456445,0.00013620906,0.000047892143,0.00003072129,0.0001779117,0.9921914,0.0000073549486],"about_ca_topic_score_codex":0.8621558,"about_ca_topic_score_gemma":0.8976424,"teacher_disagreement_score":0.1378442,"about_ca_system_score_codex":0.009552161,"about_ca_system_score_gemma":0.030470941,"threshold_uncertainty_score":0.31931204},"labels":[],"label_agreement":null},{"id":"W1484374422","doi":"10.1029/170gm08","title":"Uncertainties in earthquake source spectrum estimation using empirical Green functions","year":2006,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Seismology; Geology; Estimation; Green S; Mathematics; Economics; Mathematical analysis","score_opus":0.027038537792899938,"score_gpt":0.23082430563416353,"score_spread":0.2037857678412636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1484374422","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07667623,0.00072532543,0.92061734,0.0002191109,0.000017842485,0.000017333421,0.00020109373,0.00028876256,0.0012370438],"genre_scores_gemma":[0.787721,0.0011635694,0.20892122,0.00009535823,0.00012492691,0.00008439027,0.00085169764,0.00024659382,0.00079135766],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99788874,0.0009861757,0.000095556505,0.0002856269,0.0006610644,0.000082831604],"domain_scores_gemma":[0.97107434,0.025290033,0.0012993385,0.001387392,0.00085685716,0.00009209021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006423962,0.00083223963,0.0007092678,0.0027450258,0.00027431472,0.0013703262,0.001457916,0.000832695,0.0005261753],"category_scores_gemma":[0.03470377,0.00049452827,0.00065181963,0.0014415435,0.0012451902,0.0021116685,0.0014092858,0.0010711133,0.00016988552],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054707783,0.00002397176,0.008282725,0.0000976258,0.00011289733,0.00015202665,0.00013812672,0.8765188,0.0029076275,0.025456924,0.000675877,0.085578665],"study_design_scores_gemma":[0.000005081815,0.000014732202,0.0034612182,0.000035993202,0.0000104555875,0.00006876558,0.0000263038,0.95602316,0.0017988854,0.037931416,0.0005975805,0.000026498272],"about_ca_topic_score_codex":0.003802608,"about_ca_topic_score_gemma":0.0022535685,"teacher_disagreement_score":0.006423962,"about_ca_system_score_codex":0.000791988,"about_ca_system_score_gemma":0.00045663028,"threshold_uncertainty_score":0.033973575},"labels":[],"label_agreement":null},{"id":"W1484667928","doi":"10.1002/jgrb.50306","title":"Triggering cascades and statistical properties of aftershocks","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Alberta Innovates - Technology Futures","keywords":"Aftershock; Power law; Shock (circulatory); Exponent; Magnitude (astronomy); Geology; Seismology; Statistics; Mathematics; Physics; Astrophysics","score_opus":0.05540136032496293,"score_gpt":0.30271603183948526,"score_spread":0.24731467151452233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1484667928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9857202,0.00013199967,0.011887707,0.000053485852,0.000004125283,0.000059950922,0.0007212369,0.00019485473,0.0012264185],"genre_scores_gemma":[0.9972817,0.00006902363,0.0017557896,0.0000058360138,0.0000090303965,0.000021196769,0.0006478125,0.000017532813,0.00019206977],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995555,0.000058323454,0.000042199455,0.00017389531,0.00011005179,0.00005993841],"domain_scores_gemma":[0.9881511,0.0054656607,0.003757303,0.0013456723,0.00086180447,0.00041858104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018780796,0.000311937,0.00042798094,0.00338844,0.00050433475,0.0015505465,0.0006842747,0.0004865447,0.0021796268],"category_scores_gemma":[0.017366808,0.00033133104,0.000578283,0.0022794888,0.00069039705,0.0011903356,0.0006575499,0.0005392886,0.00025674218],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027780488,0.00008443049,0.8469131,0.00014082777,0.00026104576,0.0006639661,0.0007920479,0.08680063,0.01623914,0.0111676315,0.0010024423,0.03565701],"study_design_scores_gemma":[0.00004526469,0.00013773331,0.71715903,0.000025766876,0.00011213615,0.00047740492,0.0002611424,0.26948372,0.0046120584,0.0068377573,0.00079296675,0.000055018052],"about_ca_topic_score_codex":0.007930439,"about_ca_topic_score_gemma":0.0052840402,"teacher_disagreement_score":0.007930439,"about_ca_system_score_codex":0.0006856253,"about_ca_system_score_gemma":0.00046355618,"threshold_uncertainty_score":0.015768528},"labels":[],"label_agreement":null},{"id":"W1486970133","doi":"10.37099/mtu.dc.etds/316","title":"Numerical and granulometric approaches to geophysical granular flows","year":2003,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Oak Ridge National Laboratory; National Energy Technology Laboratory; Michigan Technological University; Natural Sciences and Engineering Research Council of Canada; Nuffield Foundation; McGill University","keywords":"Pyroclastic rock; Geology; Peléan eruption; Volcanic ash; Volcano; Pyroclastic fall; Phreatic eruption; Explosive eruption; Elutriation; Volcanology; Earth science; Petrology; Geophysics; Geomorphology; Geochemistry; Magma","score_opus":0.04278437597734314,"score_gpt":0.21815317762451725,"score_spread":0.1753688016471741,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1486970133","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01344966,0.00033159443,0.9826905,0.00026663652,0.00007540313,0.00006586393,0.00022835382,0.00037992548,0.0025121015],"genre_scores_gemma":[0.41028455,0.0008994502,0.58254236,0.00013446121,0.00037423146,0.00043725895,0.0005657561,0.00026427084,0.0044977185],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99946696,0.00017583664,0.00004716588,0.00007780203,0.0001733033,0.00005891997],"domain_scores_gemma":[0.99661785,0.0020391254,0.00039008108,0.00047189734,0.00033854358,0.00014252056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017523182,0.0006153329,0.00078756385,0.0029359886,0.00070259714,0.0027599826,0.0017281256,0.0012942842,0.0027544273],"category_scores_gemma":[0.009388731,0.00061681285,0.001112521,0.0021550346,0.0019546265,0.0017910235,0.0020017533,0.0013524417,0.00048443096],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035316585,0.00003995022,0.0016779858,0.00007070053,0.000044093136,0.00007838241,0.00006991237,0.79978406,0.00049758056,0.17333601,0.00065880816,0.023707263],"study_design_scores_gemma":[0.000005140446,0.000002825915,0.00011121691,0.000003774927,0.0000027013846,0.0000070108417,0.0000083079885,0.9532742,0.00008662722,0.04585227,0.00064259715,0.0000032231592],"about_ca_topic_score_codex":0.006527674,"about_ca_topic_score_gemma":0.004157772,"teacher_disagreement_score":0.006527674,"about_ca_system_score_codex":0.0015603958,"about_ca_system_score_gemma":0.00077379483,"threshold_uncertainty_score":0.012979329},"labels":[],"label_agreement":null},{"id":"W1487245719","doi":"10.1002/2013jb010928","title":"Understanding subsidence in the Mississippi Delta region due to sediment, ice, and ocean loading: Insights from geophysical modeling","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Canada Research Chairs; University of Ottawa","keywords":"Geology; Post-glacial rebound; Subsidence; Lithosphere; Geodetic datum; Sediment; Sea level; Glacial period; Delta; Geomorphology; Geophysics; Geodesy; Seismology; Tectonics; Oceanography","score_opus":0.13282836809698234,"score_gpt":0.3193974769949339,"score_spread":0.18656910889795159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1487245719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99600476,0.00008014815,0.0022231636,0.00019077666,0.0000022970726,0.0000062315025,0.00010152761,0.000020590227,0.0013705477],"genre_scores_gemma":[0.99921846,0.000081704144,0.00050055364,0.000013044965,0.0000017507265,0.0000034292077,0.000039220624,0.0000030131332,0.0001388009],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999641,0.000012684256,0.0000027153594,0.0000086849495,0.0000052014493,0.000006572997],"domain_scores_gemma":[0.9998822,0.000056000856,0.000025772051,0.000009528224,0.000015909487,0.000010651999],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020821557,0.00028763348,0.00021221531,0.00038622777,0.00025900782,0.0005905306,0.00034206215,0.00058656215,0.00063676387],"category_scores_gemma":[0.00054733915,0.0002038145,0.00038720676,0.00030978068,0.00033549804,0.00038606027,0.00028587913,0.0002336501,0.00006322492],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028219923,0.000048397924,0.03590992,0.000026383677,0.000040012896,0.00014286104,0.00007649296,0.9558294,0.0033809824,0.0011465581,0.000117846495,0.0032529107],"study_design_scores_gemma":[0.0000044586877,0.000023635093,0.013192684,0.0000062122926,0.000012155959,0.000023970826,0.00007359884,0.9856339,0.00030795694,0.0005142971,0.00020178425,0.0000053724266],"about_ca_topic_score_codex":0.059164047,"about_ca_topic_score_gemma":0.03310752,"teacher_disagreement_score":0.059164047,"about_ca_system_score_codex":0.00094283425,"about_ca_system_score_gemma":0.0005641416,"threshold_uncertainty_score":0.11763936},"labels":[],"label_agreement":null},{"id":"W1487292691","doi":"","title":"The Newfoundland Tsunami of November 18, 1929: An Examination of the Twenty-eight Deaths of the \"South Coast Disaster\"","year":2006,"lang":"en","type":"article","venue":"Newfoundland and Labrador Studies","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Slumping; Geology; Continental shelf; Landslide; Seismology; Oceanography; Submarine landslide; Submarine pipeline; Canyon; Archaeology; Geography; Geomorphology","score_opus":0.018421526553458637,"score_gpt":0.23384050153226596,"score_spread":0.21541897497880733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1487292691","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93017113,0.009565482,0.00011237823,0.008681419,0.00032737805,0.00007031444,0.011693184,0.00003508064,0.03934363],"genre_scores_gemma":[0.95091563,0.0133339,0.00019345725,0.003474117,0.00031168584,0.000052314193,0.008334376,0.000028117238,0.023356345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971265,0.000013454905,0.000018090708,0.000026010455,0.00006633204,0.00016335731],"domain_scores_gemma":[0.9990638,0.00004347466,0.0002386698,0.00002416775,0.000366346,0.00026357992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002474102,0.0003296008,0.0001428832,0.0018633718,0.0031951698,0.0011986484,0.0005843429,0.0005923731,0.0032359601],"category_scores_gemma":[0.00080518314,0.00018350108,0.0001805191,0.0019259105,0.00096757535,0.0006093529,0.0013144322,0.00079363416,0.000548052],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002976566,0.000078174875,0.81561816,0.00044122073,0.00012379866,0.0077164667,0.01571362,0.00041892505,0.0012924799,0.0005676378,0.09932212,0.058409736],"study_design_scores_gemma":[0.0000017969691,0.000014473955,0.97781575,0.00007217954,0.0000099574,0.00023240676,0.0061340407,0.000019762787,0.000051888466,0.000014699321,0.015625568,0.000007464023],"about_ca_topic_score_codex":0.9310039,"about_ca_topic_score_gemma":0.98513955,"teacher_disagreement_score":0.06899607,"about_ca_system_score_codex":0.012136904,"about_ca_system_score_gemma":0.0076805684,"threshold_uncertainty_score":0.13880473},"labels":[],"label_agreement":null},{"id":"W1490967276","doi":"","title":"The 1929 Newfoundland Tsunami","year":2006,"lang":"en","type":"article","venue":"Newfoundland and Labrador Studies","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geography; Seismology","score_opus":0.015728737519257106,"score_gpt":0.23666158074236213,"score_spread":0.22093284322310502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1490967276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88325447,0.003159213,0.0002478672,0.0065397266,0.00037060076,0.00005506629,0.011439512,0.000026767693,0.0949066],"genre_scores_gemma":[0.9100257,0.0034833364,0.00046469827,0.0016430487,0.00012911492,0.00004975128,0.006131921,0.000025250261,0.07804712],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99969745,0.000018443998,0.000017614095,0.000031712963,0.000054269723,0.0001805134],"domain_scores_gemma":[0.9989754,0.00010341597,0.00024528976,0.00007704654,0.00038729265,0.00021153066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034362337,0.00021137987,0.00015586757,0.0018890963,0.0024520108,0.0013629852,0.00042481473,0.0003747288,0.0066445046],"category_scores_gemma":[0.0014880798,0.00017194757,0.00018045129,0.0026501704,0.00065190723,0.00095672504,0.0013348954,0.00071514247,0.0005106922],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029530167,0.00007318457,0.7643035,0.00035987512,0.0002034138,0.002688459,0.01293334,0.0016676902,0.0027462777,0.0068740947,0.10561465,0.10224021],"study_design_scores_gemma":[0.0000054176644,0.000013332392,0.9327127,0.00008264005,0.00002401447,0.000106128726,0.0042839395,0.000070031165,0.00021012386,0.00008656416,0.06238943,0.000015665515],"about_ca_topic_score_codex":0.9716491,"about_ca_topic_score_gemma":0.9956044,"teacher_disagreement_score":0.02835089,"about_ca_system_score_codex":0.017664336,"about_ca_system_score_gemma":0.010191752,"threshold_uncertainty_score":0.12816435},"labels":[],"label_agreement":null},{"id":"W1492904818","doi":"10.1002/2015jb011920","title":"Cascadia subducting plate fluids channelled to fore‐arc mantle corner: ETS and silica deposition","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":135,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Mantle (geology); Oceanic crust; Mantle wedge; Transition zone; Crust; Convergent boundary; Seismology; Petrology; Volcanic arc; Geochemistry; Tectonics","score_opus":0.07221616726683112,"score_gpt":0.3273406265674197,"score_spread":0.2551244593005886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1492904818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99754506,0.0002554699,0.0002017769,0.00007102591,0.0000027104265,0.000001579558,0.00020625797,0.000025878084,0.001690247],"genre_scores_gemma":[0.99928695,0.00007960766,0.00006637679,0.000005457588,0.0000018360125,8.757685e-7,0.000083208324,0.0000037256864,0.00047191262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999583,0.000002124003,0.0000035470493,0.000018559474,0.00000942176,0.000008070148],"domain_scores_gemma":[0.9998851,0.00001774552,0.000040678362,0.0000063678526,0.000029281311,0.00002078004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006479233,0.0003026622,0.00017856494,0.0006000243,0.00033553562,0.00041831666,0.00017451405,0.00018317209,0.0025107325],"category_scores_gemma":[0.0002346928,0.00016017501,0.00017035496,0.00035697644,0.00030761343,0.00022702172,0.00046068142,0.00018170374,0.00021671549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030216624,0.000018762295,0.7186887,0.00019431111,0.00009873048,0.00075144647,0.0005318877,0.0036386251,0.26549715,0.00057050074,0.0002374387,0.009470373],"study_design_scores_gemma":[0.0000025245138,0.00002385401,0.9909474,0.000005083309,0.000016618596,0.000056507124,0.00020683507,0.00089341844,0.0070812376,0.00015168195,0.0006096156,0.0000051029706],"about_ca_topic_score_codex":0.020715933,"about_ca_topic_score_gemma":0.020301217,"teacher_disagreement_score":0.020715933,"about_ca_system_score_codex":0.000656406,"about_ca_system_score_gemma":0.00032960926,"threshold_uncertainty_score":0.041190684},"labels":[],"label_agreement":null},{"id":"W1493487809","doi":"10.1029/2003tc001557","title":"Tectonic processes during oblique collision: Insights from the St. Elias orogen, northern North American Cordillera","year":2004,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Geology; Subduction; Seismology; Foreland basin; Terrane; Tectonics; Sinistral and dextral; Trench; Thrust fault; Passive margin; Pacific Plate; Clockwise; Paleontology; Fold (higher-order function); Rift","score_opus":0.011918416879763137,"score_gpt":0.2043308800210847,"score_spread":0.19241246314132157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1493487809","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984427,0.00009132198,0.000024980447,0.000035812674,9.0410254e-7,0.0000023625998,0.00006249255,0.0000025716117,0.0013367769],"genre_scores_gemma":[0.9991979,0.00016547013,0.00008159998,0.00001893913,0.0000022940105,0.0000029374605,0.0001391563,0.0000033972312,0.00038843675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999509,0.000004170468,0.0000028917177,0.000014106454,0.000012449626,0.000015588857],"domain_scores_gemma":[0.99990296,0.000010399807,0.000031810483,0.000004765426,0.000026227452,0.000023756478],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001106787,0.00020495491,0.00019625336,0.00074738386,0.0010473123,0.00087245565,0.00026802145,0.00040126697,0.0017244664],"category_scores_gemma":[0.00037688034,0.00014906202,0.00014706321,0.0010817235,0.00044247104,0.00036075132,0.0008455483,0.00022899479,0.0001730811],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012764374,0.00005330755,0.96821076,0.000050649076,0.000052744763,0.0010862235,0.005339,0.0016683174,0.009917668,0.00041589452,0.00027631404,0.012801508],"study_design_scores_gemma":[0.0000029396629,0.0000074618683,0.9969277,0.0000097045295,0.00001034858,0.000057626577,0.0016147699,0.0007312754,0.00013431627,0.00006555173,0.00043473815,0.0000036776744],"about_ca_topic_score_codex":0.31980938,"about_ca_topic_score_gemma":0.5723793,"teacher_disagreement_score":0.31980938,"about_ca_system_score_codex":0.0015335884,"about_ca_system_score_gemma":0.0010720693,"threshold_uncertainty_score":0.6358957},"labels":[],"label_agreement":null},{"id":"W1496946697","doi":"10.3133/pp1661c","title":"Crustal structure and earthquake hazards of the subduction zone in southwestern British Columbia and western Washington","year":2005,"lang":"en","type":"article","venue":"USGS professional paper","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Tectonics","score_opus":0.007117874734724681,"score_gpt":0.20754786249204035,"score_spread":0.20042998775731566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1496946697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99713564,0.0002279755,0.000020235771,0.00011393499,0.000002632682,0.0000062387207,0.00069064286,0.0000037951681,0.001798973],"genre_scores_gemma":[0.99712497,0.00026368402,0.000046915775,0.000029731578,0.0000014696409,0.00000548302,0.00055330567,0.0000024392693,0.0019720218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983966,0.000017994304,0.000016496038,0.000025549856,0.00003747285,0.00006291209],"domain_scores_gemma":[0.9989305,0.000114579045,0.0001615466,0.000034803783,0.0005168732,0.00024172259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021034868,0.00019373783,0.0002528406,0.0018569919,0.0014940546,0.0010639045,0.0007503429,0.00029224055,0.0023743957],"category_scores_gemma":[0.0012976391,0.00023522104,0.00016621113,0.0034987906,0.0005112423,0.00030821492,0.0008316681,0.00039821194,0.0002089048],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000085164065,0.00003607941,0.98479295,0.0000326562,0.000057654794,0.00030983108,0.0018917598,0.00060523814,0.0007255485,0.00024897335,0.0012597078,0.009954495],"study_design_scores_gemma":[0.0000037848695,0.0000039469137,0.996488,0.000018293507,0.000011610076,0.000030875377,0.0024438659,0.00025259575,0.000054251985,0.000024902147,0.00066347077,0.000004537626],"about_ca_topic_score_codex":0.9890035,"about_ca_topic_score_gemma":0.9970559,"teacher_disagreement_score":0.0109965205,"about_ca_system_score_codex":0.009069532,"about_ca_system_score_gemma":0.0073777344,"threshold_uncertainty_score":0.06580436},"labels":[],"label_agreement":null},{"id":"W1497590817","doi":"10.1002/2014jb011108","title":"A brittle failure model for long‐period seismic events recorded at Turrialba Volcano, Costa Rica","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science Foundation Ireland","keywords":"Seismology; Volcano; Geology; Impact crater; Brittleness; Isotropy; Shear (geology); Moment tensor; Waveform; Scaling; Dipole; Magnitude (astronomy); Inversion (geology); Scaling law; Modal; Physics; Tectonics; Mathematics; Radar; Geometry; Materials science; Engineering; Astrophysics; Petrology; Optics","score_opus":0.08055019344567912,"score_gpt":0.33641923505220295,"score_spread":0.2558690416065238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1497590817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97735345,0.00021005957,0.018981064,0.00021798458,0.000009854053,0.000031909174,0.000414159,0.00013328422,0.0026481263],"genre_scores_gemma":[0.9987453,0.000054337044,0.0006118411,0.000006683917,0.000003888027,0.000010969116,0.00010648613,0.000011014643,0.0004494724],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991906,0.000024685372,0.0000054452416,0.000018403103,0.000013054024,0.000019312129],"domain_scores_gemma":[0.9998087,0.00006409425,0.000050806408,0.000020622103,0.00003529768,0.000020476338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035703616,0.00061887264,0.00032121016,0.00064610783,0.00032264407,0.0005079875,0.00095268677,0.00056690624,0.0010245558],"category_scores_gemma":[0.0008716136,0.00031849806,0.0004931199,0.00032107852,0.00037158537,0.0003129131,0.00036088921,0.00030962654,0.00016000649],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006465807,0.000043516975,0.033592723,0.00002947096,0.000058656642,0.00033755534,0.00011600555,0.95523465,0.0037454104,0.0021532958,0.0003778557,0.004246272],"study_design_scores_gemma":[0.0000030087438,0.000006992978,0.0052593993,0.0000021369133,0.0000049566265,0.00001505157,0.000015181531,0.994383,0.000058544116,0.00016986213,0.00007858042,0.000003287046],"about_ca_topic_score_codex":0.06424277,"about_ca_topic_score_gemma":0.037004624,"teacher_disagreement_score":0.06424277,"about_ca_system_score_codex":0.00086844095,"about_ca_system_score_gemma":0.000660647,"threshold_uncertainty_score":0.1277377},"labels":[],"label_agreement":null},{"id":"W1498015964","doi":"10.7202/032963ar","title":"Seismicity and Seismotectonics of the Western Lake Ontario Region","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lineament; Induced seismicity; Geology; Seismology; Seismotectonics; Seismic hazard; Range (aeronautics); Tectonics","score_opus":0.01589088991698702,"score_gpt":0.21776225656522244,"score_spread":0.2018713666482354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1498015964","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9731165,0.00090184214,0.00022360373,0.00032613613,0.000007362983,0.000036360343,0.0074246335,0.000034789515,0.017928887],"genre_scores_gemma":[0.9893958,0.0008056543,0.00028788345,0.000021621672,0.000007516305,0.000019700203,0.0028345361,0.000011236652,0.0066161123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982893,0.00000908342,0.0000112686985,0.000019924655,0.00008424462,0.000046490724],"domain_scores_gemma":[0.99956673,0.000022410077,0.0001110218,0.000017680386,0.0002146497,0.00006752462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116153584,0.00016493753,0.00011677917,0.0018726235,0.0009924406,0.000657046,0.00037496822,0.00012530944,0.0023259027],"category_scores_gemma":[0.0008800003,0.00012378536,0.000116108946,0.0044671777,0.00043178996,0.0002135102,0.00042399953,0.00013298054,0.00026703384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014799954,0.0000339772,0.9339791,0.00018755271,0.00007633418,0.0006514238,0.005284601,0.003139978,0.004334741,0.0011979289,0.008266198,0.042700037],"study_design_scores_gemma":[0.0000023406665,0.000004839264,0.99326295,0.000010952132,0.0000060931875,0.000022257409,0.0005912113,0.00035972582,0.00006521933,0.000019443813,0.005648762,0.000006252955],"about_ca_topic_score_codex":0.99002004,"about_ca_topic_score_gemma":0.9954609,"teacher_disagreement_score":0.011265453,"about_ca_system_score_codex":0.011265453,"about_ca_system_score_gemma":0.0076348116,"threshold_uncertainty_score":0.08173698},"labels":[],"label_agreement":null},{"id":"W1501218190","doi":"10.1029/2012gc004391","title":"Low frequency earthquakes below southern Vancouver Island","year":2012,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismology; Induced seismicity; Subduction; Slip (aerodynamics); Coda; Tectonics","score_opus":0.008236768171553522,"score_gpt":0.18683498519340663,"score_spread":0.1785982170218531,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1501218190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971264,0.000039378647,0.000099861834,0.00002194249,9.4935706e-7,0.000007361647,0.0006668897,0.00001275044,0.0020244108],"genre_scores_gemma":[0.9971449,0.0000620975,0.00020581455,0.0000075309317,7.481399e-7,0.0000050011095,0.0009979937,0.000002842392,0.0015731694],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998971,0.0000054294983,0.0000049953046,0.000021375456,0.000041115127,0.000029989214],"domain_scores_gemma":[0.9996513,0.00002138641,0.000062809915,0.000014604988,0.00015816212,0.00009175291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007122239,0.000177029,0.00014117046,0.0010781068,0.00083495653,0.00065389625,0.0001999145,0.00017509909,0.0014298994],"category_scores_gemma":[0.0004699306,0.00012970317,0.00006237264,0.0014447242,0.0002217745,0.00012407891,0.0004981288,0.00016729328,0.00023417466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008775842,0.000024553201,0.9460658,0.000044639262,0.000031194002,0.00040491248,0.0011219272,0.0011594722,0.011990235,0.00014971437,0.0009957162,0.03792415],"study_design_scores_gemma":[0.000001638638,0.000006881038,0.9978877,0.000006135175,0.0000037446607,0.0000402216,0.00048721078,0.0007284003,0.00027219745,0.000020177373,0.00054281036,0.0000029717353],"about_ca_topic_score_codex":0.7147492,"about_ca_topic_score_gemma":0.90384674,"teacher_disagreement_score":0.28525078,"about_ca_system_score_codex":0.001750495,"about_ca_system_score_gemma":0.0019073372,"threshold_uncertainty_score":0.57386136},"labels":[],"label_agreement":null},{"id":"W1505638149","doi":"10.3133/ofr20101083o","title":"Seismicity of the Earth 1900-2013 offshore British Columbia-southeastern Alaska and vicinity","year":2014,"lang":"en","type":"article","venue":"Antarctica A Keystone in a Changing World","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Pacific Plate; North American Plate; Plate tectonics; Seismology; Subduction; Convergent boundary; Transform fault; Intraplate earthquake; Triple junction; Slab window; Submarine pipeline; Induced seismicity; Lithosphere; Eurasian Plate; Tectonics; Oceanic crust; Oceanography","score_opus":0.010148711938067637,"score_gpt":0.19535517302077546,"score_spread":0.18520646108270783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1505638149","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9241733,0.0010047886,0.00011382537,0.000214798,0.000029321784,0.000031789605,0.032391492,0.00009107983,0.04194972],"genre_scores_gemma":[0.9429117,0.0014731047,0.00024327295,0.00006131553,0.000011817464,0.000026864262,0.021375492,0.000030086316,0.033866387],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993134,0.0000023151763,0.000004816865,0.000014248466,0.00002909993,0.000018206763],"domain_scores_gemma":[0.9996306,0.00001118911,0.000027619439,0.000008871801,0.00024931377,0.00007243374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000077961005,0.00028417638,0.00017032606,0.0026281744,0.0015005106,0.0008570681,0.0003801595,0.00021356108,0.0053728665],"category_scores_gemma":[0.00040513906,0.00015334891,0.00011968562,0.004167734,0.00020642916,0.00022855395,0.0005405835,0.00028757317,0.0014051072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013533047,0.000068192916,0.90820557,0.00023682161,0.00010218008,0.0007824943,0.0024144633,0.0027001046,0.0031195607,0.00038180684,0.02896271,0.052890863],"study_design_scores_gemma":[0.0000026114428,0.0000047985086,0.9848556,0.000060694223,0.000016076616,0.000052921278,0.0018317602,0.0004120578,0.00018335583,0.000017574694,0.012552451,0.000010129324],"about_ca_topic_score_codex":0.969972,"about_ca_topic_score_gemma":0.9921582,"teacher_disagreement_score":0.030027986,"about_ca_system_score_codex":0.004669453,"about_ca_system_score_gemma":0.0045981375,"threshold_uncertainty_score":0.060409606},"labels":[],"label_agreement":null},{"id":"W1508924242","doi":"10.1016/j.jog.2003.11.001","title":"Stress field in the Vanuatu (New Hebrides) Wadati–Benioff zone inferred by inversion of earthquake focal mechanisms","year":2004,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Council","keywords":"Geology; Slab; Seismology; Clockwise; Geodesy; Magnetic dip; Stress field; Tension (geology); Mantle (geology); Geophysics; Rotation (mathematics); Geometry; Compression (physics); Physics","score_opus":0.008966463286421597,"score_gpt":0.20894239687256413,"score_spread":0.19997593358614255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1508924242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99714845,0.00021830459,0.000062180625,0.0000403336,0.0000040979094,0.000004877237,0.0002516385,0.0000054117436,0.0022648287],"genre_scores_gemma":[0.99879825,0.000078785095,0.00011394193,0.000013440418,0.0000018804024,0.0000068143913,0.00023733683,0.0000027001645,0.0007469535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999336,0.000010461453,0.000005338506,0.000018384724,0.000009258704,0.000022883367],"domain_scores_gemma":[0.9998254,0.000039011862,0.0000410212,0.000009092107,0.000043504857,0.000042033935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014593951,0.00015192492,0.00022176966,0.0012193164,0.0006628402,0.0007875106,0.0006060188,0.0003842756,0.0024975806],"category_scores_gemma":[0.0007636979,0.00022777668,0.000076463795,0.0015127171,0.0007272124,0.00028792652,0.0006358145,0.0002590713,0.00025690158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009827339,0.00012346251,0.8965531,0.00027416757,0.00019708417,0.0034825434,0.013549874,0.006562143,0.026277646,0.0043883803,0.0026979567,0.044910964],"study_design_scores_gemma":[0.000030428973,0.000024108953,0.99414897,0.00005074604,0.000021036747,0.00014483332,0.0016970455,0.0014036844,0.0004399098,0.00009932712,0.001928296,0.000011571221],"about_ca_topic_score_codex":0.5472036,"about_ca_topic_score_gemma":0.67132485,"teacher_disagreement_score":0.5472036,"about_ca_system_score_codex":0.0022705486,"about_ca_system_score_gemma":0.00086157065,"threshold_uncertainty_score":0.910926},"labels":[],"label_agreement":null},{"id":"W1511418107","doi":"10.1002/ggge.20051","title":"In situ stress and pore pressure in the Kumano Forearc Basin, offshore SW Honshu from downhole measurements during riser drilling","year":2013,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Natural Environment Research Council; Sight Research UK; Consortium for Ocean Leadership","keywords":"Forearc; Geology; Pore water pressure; Accretionary wedge; Subduction; Drilling; Scientific drilling; Petrology; Seismology; Geomorphology; Geotechnical engineering; Tectonics","score_opus":0.01348802047510093,"score_gpt":0.19461703826222052,"score_spread":0.1811290177871196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1511418107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996026,0.000018924262,0.00006138746,0.0000040919876,9.030112e-7,0.0000029658534,0.0000821263,0.0000070485753,0.00021996403],"genre_scores_gemma":[0.9993224,0.00003068748,0.0003029933,0.000007890568,0.0000019014292,0.000009226997,0.0001658018,0.0000033755891,0.00015568762],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987257,0.000008178995,0.000010014675,0.000034401048,0.000045825323,0.000029089177],"domain_scores_gemma":[0.999814,0.000029326095,0.0000415623,0.000013380141,0.000056773126,0.000044973214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015994409,0.00035207742,0.00028370993,0.00073374936,0.00046271915,0.0003658358,0.00034181375,0.00041619604,0.00047197856],"category_scores_gemma":[0.0003174867,0.00028082772,0.00017036893,0.0005716558,0.00039923136,0.00037391772,0.0004945207,0.00021319652,0.00011961089],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021423787,0.00010642738,0.814739,0.00007784479,0.000040121802,0.0010535195,0.0025992298,0.0008985256,0.16511719,0.000055896937,0.00013997611,0.0149580445],"study_design_scores_gemma":[0.0000052283795,0.000045704553,0.9965758,0.0000054111583,0.000009807485,0.000056783054,0.00034890353,0.00080624106,0.0019757494,0.000008055116,0.0001568668,0.0000054745883],"about_ca_topic_score_codex":0.0240758,"about_ca_topic_score_gemma":0.07628268,"teacher_disagreement_score":0.0240758,"about_ca_system_score_codex":0.00029792264,"about_ca_system_score_gemma":0.00039326784,"threshold_uncertainty_score":0.04787135},"labels":[],"label_agreement":null},{"id":"W1511645316","doi":"10.1029/2003gl018106","title":"Stress change near the Kunlun fault before and after the Ms 8.1 Kunlun earthquake","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Geology; Seismology; Intraplate earthquake; Fault (geology); Principal stress; Stress field; Magnitude (astronomy); Stress (linguistics); Interplate earthquake; Tectonics; Petrology; Shear (geology)","score_opus":0.03568725444292759,"score_gpt":0.27342106029181346,"score_spread":0.23773380584888587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1511645316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996679,0.00002498993,0.000009536144,0.000012974931,0.0000025183488,0.0000010812046,0.000040805113,0.0000015113659,0.00023879998],"genre_scores_gemma":[0.9995074,0.000027964998,0.000016439366,0.000009455994,0.000003798355,0.000002532785,0.00015900163,7.602385e-7,0.0002725717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998963,0.0000074621303,0.000006270819,0.00002403566,0.000027954595,0.000037869922],"domain_scores_gemma":[0.9997228,0.000015864016,0.00009367945,0.000013953798,0.000075303135,0.00007837668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012393856,0.00019469911,0.00032584934,0.0006083168,0.00062834786,0.0004311446,0.00024433783,0.0004563422,0.0008437037],"category_scores_gemma":[0.0004110989,0.00021145165,0.00016822762,0.0005831148,0.00045613563,0.00031792375,0.00032480722,0.0002739112,0.00016829935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013410961,0.00024402988,0.7758832,0.0001281657,0.000094533396,0.0031346357,0.0055792555,0.0016356875,0.19232175,0.00027526915,0.00083364703,0.018528817],"study_design_scores_gemma":[0.0000056194326,0.00008197545,0.99817955,0.0000034867103,0.0000045953784,0.000057620415,0.0003115156,0.00015813211,0.00095552864,0.000017427783,0.00021825457,0.000006300781],"about_ca_topic_score_codex":0.01695269,"about_ca_topic_score_gemma":0.029160049,"teacher_disagreement_score":0.01695269,"about_ca_system_score_codex":0.00090725266,"about_ca_system_score_gemma":0.00036293504,"threshold_uncertainty_score":0.033708036},"labels":[],"label_agreement":null},{"id":"W1511742916","doi":"10.1029/2011gl048305","title":"Deep-sea observations and modeling of the 2004 Sumatra tsunami in Drake Passage","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Tide gauge; Geology; Amplitude; Tsunami wave; Seismology; Dispersion (optics); Indian ocean; Wind wave; Arrival time; Geodesy; Sea level; Oceanography; Physics","score_opus":0.11595570887898105,"score_gpt":0.28280554396478474,"score_spread":0.1668498350858037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1511742916","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841547,0.000030591753,0.0005870615,0.00005330572,0.000006670173,0.0000073333226,0.00031418342,0.000036041838,0.0005494377],"genre_scores_gemma":[0.99910563,0.000023144794,0.00037445524,0.0000067021615,0.000002465091,0.0000062097156,0.00024324626,0.0000066443245,0.00023136861],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992037,0.000018887,0.0000074250765,0.000027383967,0.000010336873,0.000015577178],"domain_scores_gemma":[0.99980944,0.000051736526,0.000043228556,0.000022926613,0.000036163547,0.000036497826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018605574,0.00061305834,0.00029543444,0.0003600068,0.00045103967,0.00072390697,0.00061670906,0.00076631835,0.0008771189],"category_scores_gemma":[0.0007775309,0.00041675562,0.00041360856,0.00035278217,0.00038593425,0.00051439024,0.00038799952,0.0004819106,0.00019914951],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016852254,0.00009630656,0.06606921,0.000027411294,0.000072564195,0.00032270228,0.00011329195,0.9258993,0.0039667664,0.00031136844,0.00035940125,0.002593092],"study_design_scores_gemma":[0.000039050978,0.00006819704,0.043136287,0.0000059196136,0.000025693185,0.00004060454,0.0000829607,0.95560896,0.0006040172,0.00014316071,0.00022643743,0.00001869688],"about_ca_topic_score_codex":0.07435295,"about_ca_topic_score_gemma":0.051172126,"teacher_disagreement_score":0.07435295,"about_ca_system_score_codex":0.0016268921,"about_ca_system_score_gemma":0.00052259327,"threshold_uncertainty_score":0.14784032},"labels":[],"label_agreement":null},{"id":"W1512502938","doi":"10.1002/2015jb011892","title":"High‐resolution imaging of rapid tremor migrations beneath southern Vancouver Island using cross‐station cross correlations","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Front (military); Seismology; Wavefront; Geodesy; Shear (geology); Physics; Optics","score_opus":0.06330754210976347,"score_gpt":0.34433453206376774,"score_spread":0.28102698995400427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1512502938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98815876,0.0002658856,0.004769795,0.00008793525,0.000017164873,0.00003123347,0.0012268962,0.00022822335,0.0052141175],"genre_scores_gemma":[0.9912135,0.00016190104,0.006239003,0.000037320035,0.000018748198,0.000017982296,0.00094394357,0.000041990468,0.0013255865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985576,0.000010146633,0.000004493867,0.000032190503,0.00005627219,0.00004107459],"domain_scores_gemma":[0.9995485,0.00003923698,0.00004201396,0.000029523046,0.0002760518,0.00006462475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021861089,0.0003170324,0.00017915656,0.0020507944,0.00041209316,0.0006436721,0.0003334129,0.00028243876,0.0015715342],"category_scores_gemma":[0.0005817218,0.00026895065,0.00015080262,0.0015325784,0.00013716459,0.00021523202,0.00049433456,0.00029699306,0.00035100617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026274574,0.0002587887,0.50632703,0.00017462224,0.00040055803,0.0008882828,0.0011217461,0.012024057,0.34203428,0.0005407036,0.005714599,0.13025257],"study_design_scores_gemma":[0.000012959714,0.000031721294,0.9570895,0.000022741666,0.00005583579,0.00016183793,0.00032390916,0.032297906,0.007601695,0.000085678126,0.0022899737,0.00002623998],"about_ca_topic_score_codex":0.12341447,"about_ca_topic_score_gemma":0.32842195,"teacher_disagreement_score":0.87658554,"about_ca_system_score_codex":0.00051761523,"about_ca_system_score_gemma":0.0009230442,"threshold_uncertainty_score":0.2453922},"labels":[],"label_agreement":null},{"id":"W1513300606","doi":"10.1002/2013gl057919","title":"Are scale‐invariant stress orientations related to seismicity rates near the San Andreas fault?","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"San andreas fault; Geology; Induced seismicity; Scaling; Scale invariance; Amplitude; Seismology; Slip (aerodynamics); Magnitude (astronomy); Nonlinear system; Fault (geology); Invariant (physics); Orientation (vector space); Stress (linguistics); Geodesy; Geometry; Physics; Statistics; Mathematics; Optics","score_opus":0.031127840373387713,"score_gpt":0.29293070098900315,"score_spread":0.2618028606156154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1513300606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970054,0.00014042752,0.0015332411,0.00013220572,0.000006137361,0.0000039369456,0.00007996315,0.000022752276,0.0010760204],"genre_scores_gemma":[0.99965835,0.000064055224,0.00011961113,0.000010007268,0.000005790774,0.0000015254964,0.000030244448,0.0000037733753,0.00010652535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998017,0.000034567503,0.000015272852,0.00007144986,0.000028898377,0.000048213114],"domain_scores_gemma":[0.9979425,0.0003411145,0.0012101185,0.00018296212,0.00015437577,0.00016884605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035785176,0.00018659618,0.0002449053,0.00077193585,0.00015562995,0.00066184346,0.00026366432,0.00038877947,0.0012278851],"category_scores_gemma":[0.0032030998,0.00033827196,0.00017170787,0.00087017,0.0010713362,0.00087649806,0.00025069917,0.0002804507,0.0003326693],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001394238,0.00005085178,0.9496561,0.000050661984,0.000111007386,0.00025615707,0.0004065176,0.004172907,0.024615424,0.0018063607,0.00026114777,0.018473404],"study_design_scores_gemma":[0.0000036492795,0.000015369316,0.9955089,0.0000037352925,0.000007809892,0.00008802803,0.00013571559,0.0029038172,0.0006291779,0.0005800878,0.00011038157,0.000013311529],"about_ca_topic_score_codex":0.0055131186,"about_ca_topic_score_gemma":0.005308457,"teacher_disagreement_score":0.0055131186,"about_ca_system_score_codex":0.00035008398,"about_ca_system_score_gemma":0.0001737738,"threshold_uncertainty_score":0.010962069},"labels":[],"label_agreement":null},{"id":"W1514580854","doi":"10.5772/56444","title":"Microseismic Monitoring Developments in Hydraulic Fracture Stimulation","year":2013,"lang":"en","type":"book-chapter","venue":"InTech eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Calgary; University of Alberta","funders":"Microseismic Industry Consortium","keywords":"Microseism; Hydraulic fracturing; Geology; Seismology; Petroleum engineering","score_opus":0.024284180287672836,"score_gpt":0.2288576443772921,"score_spread":0.20457346408961927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1514580854","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07706592,0.079421975,0.7744444,0.0031056427,0.0009238663,0.00014841964,0.0029376037,0.0027483194,0.059203982],"genre_scores_gemma":[0.42404878,0.06639375,0.46696845,0.00082826207,0.0021891545,0.0002643377,0.0031659536,0.00071583036,0.03542546],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99968684,0.000043834225,0.00001182869,0.000097121556,0.00014393443,0.000016465823],"domain_scores_gemma":[0.9990501,0.00047404453,0.000078144876,0.00012053486,0.00024097995,0.00003629205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048127453,0.00046185782,0.00039961384,0.0021264541,0.00011130345,0.00094196637,0.00070331595,0.00064178027,0.0039004546],"category_scores_gemma":[0.0010274579,0.00039773335,0.00023091676,0.0028638057,0.0005235917,0.0012345203,0.00082470133,0.0007967333,0.0013489543],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000085980515,0.000045567725,0.004655633,0.00076426467,0.00003270266,0.00017612586,0.0002681985,0.0059876544,0.058254167,0.009707376,0.00786737,0.91215503],"study_design_scores_gemma":[0.00005171716,0.0005153235,0.12280742,0.0010075144,0.00017790541,0.003642924,0.0011785836,0.116782,0.13563089,0.06908933,0.54885733,0.00025908556],"about_ca_topic_score_codex":0.0006287816,"about_ca_topic_score_gemma":0.0010892504,"teacher_disagreement_score":0.0039004546,"about_ca_system_score_codex":0.00032410226,"about_ca_system_score_gemma":0.0002369938,"threshold_uncertainty_score":0.013048351},"labels":[],"label_agreement":null},{"id":"W1518482876","doi":"10.1029/2010tc002802","title":"Miocene south directed low‐angle normal fault evolution on Kea Island (West Cycladic Detachment System, Greece)","year":2011,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Accelerated Innovation Research Initiative Turning Top Science and Ideas into High-Impact Values; Universität Wien; Austrian Science Fund","keywords":"Geology; Mylonite; Shear zone; Greenschist; Epidote; Cataclastic rock; Geochemistry; Dolostone; Schist; Petrology; Blueschist; Shear (geology); Fault (geology); Seismology; Chlorite; Metamorphic rock; Sedimentary rock; Subduction; Eclogite; Paleontology; Quartz; Carbonate rock; Tectonics","score_opus":0.018157453751220628,"score_gpt":0.19569102522625356,"score_spread":0.17753357147503293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1518482876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998176,0.000053044274,0.000021184396,0.000010711799,0.0000010590511,0.0000029393325,0.00014281896,0.0000070415904,0.0015852043],"genre_scores_gemma":[0.99911803,0.00004319949,0.000050637173,0.0000045160405,0.0000010131863,0.0000026777252,0.00025195914,0.0000030624944,0.00052477326],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.0000058114138,0.000005809773,0.000025369442,0.000008063841,0.000013665116],"domain_scores_gemma":[0.9999354,0.0000061060864,0.000019761375,0.000008853051,0.000015264466,0.000014553793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008077122,0.00021873452,0.00014795805,0.0009802105,0.00032977428,0.00050500483,0.00024284635,0.00030865482,0.0016421793],"category_scores_gemma":[0.00019965392,0.00016239415,0.00011695524,0.00070839806,0.00052476337,0.0002363676,0.00057064684,0.00012478478,0.00049426575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017702306,0.000041364598,0.9221637,0.00010966137,0.00011148553,0.0021361734,0.0036291506,0.0016036197,0.046607498,0.0005135323,0.00042315095,0.022483606],"study_design_scores_gemma":[0.0000034108139,0.000023014092,0.9980246,0.0000055248734,0.000006088127,0.00032077127,0.0003987809,0.00015036887,0.00019922575,0.000028045393,0.00083725684,0.0000030412184],"about_ca_topic_score_codex":0.023845436,"about_ca_topic_score_gemma":0.042369563,"teacher_disagreement_score":0.023845436,"about_ca_system_score_codex":0.0006559832,"about_ca_system_score_gemma":0.0003530106,"threshold_uncertainty_score":0.04741329},"labels":[],"label_agreement":null},{"id":"W1527967362","doi":"10.1002/9781118666647.ch1","title":"Absolute Gravimetry Applied to Postglacial Rebound Studies: Progress in Laurentia","year":2013,"lang":"en","type":"article","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Gravimetry; Laurentia; Geology; Geodesy; Geophysics; Absolute (philosophy); Paleontology; Philosophy; Epistemology","score_opus":0.014958346837995011,"score_gpt":0.2419538926085555,"score_spread":0.22699554577056047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1527967362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8366591,0.044078086,0.02238368,0.0015431212,0.00048767013,0.00019756546,0.0057682497,0.00073991553,0.08814262],"genre_scores_gemma":[0.92622155,0.011412351,0.027181992,0.00021060192,0.0001947391,0.00011484437,0.002492279,0.00025876137,0.031912886],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99909794,0.00010537591,0.000070452894,0.00028959409,0.00032739475,0.0001091333],"domain_scores_gemma":[0.9990075,0.00016784527,0.00023972025,0.00013111568,0.00039976492,0.000054049025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017059385,0.0006358739,0.00075238326,0.004106252,0.0011108717,0.0019917085,0.0011393272,0.0004174234,0.0019791978],"category_scores_gemma":[0.0019951474,0.00030878079,0.00029913086,0.003904612,0.00080455653,0.001184312,0.001477184,0.0005501825,0.0007851645],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022486936,0.00008187776,0.20333464,0.0007287191,0.00014265458,0.0006174985,0.00506504,0.0030042888,0.023037022,0.0021938307,0.0029142608,0.75865525],"study_design_scores_gemma":[0.000021837448,0.00016833887,0.88560444,0.00030617943,0.00009834432,0.000500204,0.0020398009,0.0025400866,0.00979984,0.0006393989,0.09822796,0.000053732445],"about_ca_topic_score_codex":0.20173232,"about_ca_topic_score_gemma":0.49584937,"teacher_disagreement_score":0.20173232,"about_ca_system_score_codex":0.0022664594,"about_ca_system_score_gemma":0.003167242,"threshold_uncertainty_score":0.40111625},"labels":[],"label_agreement":null},{"id":"W1531280820","doi":"10.1002/2015jb011963","title":"Frictional properties of the active San Andreas Fault at SAFOD: Implications for fault strength and slip behavior","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Geology; Borehole; Slip (aerodynamics); Seismology; Fault (geology); Creep; San andreas fault; Geotechnical engineering; Petrology; Materials science; Composite material","score_opus":0.10594517933876572,"score_gpt":0.3421397163003114,"score_spread":0.2361945369615457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1531280820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992594,0.000039158916,0.00016086941,0.000009055159,8.5408504e-7,0.0000030870096,0.00014155296,0.000013464191,0.00037247138],"genre_scores_gemma":[0.99955815,0.000023500099,0.00015250932,0.000004824356,0.0000013000862,0.000002748256,0.00012755483,0.0000027389833,0.00012663922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984896,0.0000093665585,0.000010348128,0.000046600762,0.000056191584,0.000028528886],"domain_scores_gemma":[0.99975413,0.0000281373,0.000075559576,0.00003369052,0.000069482856,0.0000389858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021414855,0.00031640643,0.0004517867,0.0008035589,0.00046738394,0.000478344,0.0003606698,0.00031839847,0.0006287196],"category_scores_gemma":[0.00047313914,0.0002155115,0.00020841161,0.0005529222,0.000440769,0.00030465279,0.00030658106,0.0002566526,0.00017369578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018047454,0.00010505424,0.79972994,0.00006576428,0.00009282993,0.0002636061,0.0004954082,0.003207008,0.18916823,0.00017532961,0.00011457479,0.0064018327],"study_design_scores_gemma":[0.0000063418865,0.00006573819,0.9857384,0.0000053055596,0.000014857773,0.00008842625,0.00018422531,0.0032831097,0.010218062,0.00003704999,0.00035041766,0.000008050161],"about_ca_topic_score_codex":0.02251592,"about_ca_topic_score_gemma":0.03159618,"teacher_disagreement_score":0.02251592,"about_ca_system_score_codex":0.0006175104,"about_ca_system_score_gemma":0.00031074614,"threshold_uncertainty_score":0.044769704},"labels":[],"label_agreement":null},{"id":"W1532952932","doi":"10.1029/2009gc002570","title":"Common depth of slab‐mantle decoupling: Reconciling diversity and uniformity of subduction zones","year":2009,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":506,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Slab; Subduction; Slab window; Mantle wedge; Volcanic arc; Mantle (geology); Geophysics; Hotspot (geology); Seismology; Petrology; Oceanic crust; Tectonics","score_opus":0.018725684069676417,"score_gpt":0.2095943327161423,"score_spread":0.19086864864646588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1532952932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98792005,0.000083684055,0.011088706,0.0000628856,0.0000030499539,0.000007070711,0.000050001832,0.000041248502,0.0007432726],"genre_scores_gemma":[0.99900645,0.000021244912,0.0008967238,0.0000041729118,0.0000015385962,0.000002534303,0.000023967508,0.0000084022495,0.000034954825],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99974984,0.00007283488,0.000020979945,0.00006988276,0.00003958676,0.00004685276],"domain_scores_gemma":[0.9992716,0.00020630051,0.00019446161,0.00017657822,0.00005323199,0.00009795092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00064250454,0.0005389667,0.0004641982,0.0005148096,0.00040223918,0.0008767232,0.0007100888,0.0005588042,0.00037249952],"category_scores_gemma":[0.0024690516,0.00044899966,0.0006208488,0.00041565683,0.00074277713,0.0011808892,0.0020367033,0.00068320474,0.00005437154],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030590902,0.000082772574,0.16816957,0.00008925336,0.00019420538,0.00041735618,0.0005671182,0.7459049,0.056609146,0.015002752,0.00014065462,0.012516358],"study_design_scores_gemma":[0.00004311562,0.00006340675,0.038201004,0.000009839842,0.000055981825,0.000088057575,0.00020230262,0.94620067,0.0067789136,0.007939401,0.000382697,0.000034676104],"about_ca_topic_score_codex":0.0036027315,"about_ca_topic_score_gemma":0.0027301384,"teacher_disagreement_score":0.0036027315,"about_ca_system_score_codex":0.0007735666,"about_ca_system_score_gemma":0.00048362775,"threshold_uncertainty_score":0.0071635246},"labels":[],"label_agreement":null},{"id":"W1540743406","doi":"10.1029/2010gc003264","title":"A seismic swarm and regional hydrothermal and hydrologic perturbations: The northern Endeavour segment, February 2005","year":2010,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Induced seismicity; Geology; Earthquake swarm; Swarm behaviour; Seismology; Dike; Seafloor spreading; Ridge; Borehole; Tectonics; Geophysics; Paleontology","score_opus":0.009511164588641732,"score_gpt":0.18958375721493795,"score_spread":0.1800725926262962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1540743406","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987564,0.000042324657,0.00003195244,0.000034140066,0.0000030174556,0.000003852603,0.00021571673,0.0000061637384,0.0009064928],"genre_scores_gemma":[0.99787414,0.0000427205,0.00007142415,0.000018232871,0.000014075921,0.0000046097807,0.0010395437,0.0000025410668,0.0009327688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999305,0.000006705763,0.0000052918863,0.000019388859,0.000016672466,0.000021430995],"domain_scores_gemma":[0.9997466,0.000012133575,0.000080071215,0.000011641336,0.000046429737,0.0001030134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014541042,0.00022512187,0.00015751133,0.0003912031,0.00033298053,0.0005087114,0.00014813183,0.00024135494,0.0008408609],"category_scores_gemma":[0.00040063323,0.0000861401,0.000104883075,0.00031333044,0.00014962595,0.00016538746,0.0003437639,0.00014649106,0.00013096172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035586237,0.00010873712,0.970334,0.00003126699,0.00008246826,0.0009802806,0.0020668586,0.000669132,0.0099014165,0.00013951595,0.0018322611,0.013498198],"study_design_scores_gemma":[0.0000032329797,0.00003881328,0.99885035,0.000002400268,0.0000042693773,0.000057779747,0.0002089466,0.00017334906,0.00009561319,0.0000087862645,0.00055476726,0.0000016878365],"about_ca_topic_score_codex":0.02923986,"about_ca_topic_score_gemma":0.09667616,"teacher_disagreement_score":0.02923986,"about_ca_system_score_codex":0.00070440664,"about_ca_system_score_gemma":0.00027199817,"threshold_uncertainty_score":0.058139324},"labels":[],"label_agreement":null},{"id":"W1542178928","doi":"10.1002/9781118670101.ch7","title":"Effect of Mantle Structure on Postglacial Induced Horizontal Displacement","year":2013,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Mantle (geology); Displacement (psychology); Geodesy; Geophysics; Seismology","score_opus":0.00591563542942928,"score_gpt":0.21165295828230035,"score_spread":0.20573732285287108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1542178928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99944586,0.000030063626,0.000047429337,0.000014948433,0.0000021650972,9.84866e-7,0.000057911922,0.0000059101653,0.0003946748],"genre_scores_gemma":[0.9997936,0.000011364783,0.000016940163,0.0000055597625,0.0000011707567,6.381717e-7,0.00003639131,0.0000023154007,0.0001320125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993956,0.000015539166,0.0000038980293,0.000010109811,0.000005372605,0.000025530047],"domain_scores_gemma":[0.99964654,0.00021165762,0.000027805887,0.000021094196,0.000028162565,0.00006476794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019644113,0.00023385827,0.00022489576,0.00020448487,0.0002643729,0.0005251329,0.00023264489,0.00041051343,0.0036964423],"category_scores_gemma":[0.0011543657,0.00017086153,0.00026140307,0.00021123321,0.0003735883,0.0002157358,0.0003742713,0.0002864507,0.00019561034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.020167101,0.0006602035,0.46576306,0.00021852253,0.0004869342,0.0016181698,0.00059047464,0.0386685,0.43906665,0.0014401163,0.0005396984,0.030780599],"study_design_scores_gemma":[0.00011990998,0.00096659973,0.97721076,0.000006237145,0.00015287944,0.000119525444,0.00018753686,0.007933237,0.012859004,0.00016556683,0.00026583663,0.000012898607],"about_ca_topic_score_codex":0.0066392543,"about_ca_topic_score_gemma":0.009108505,"teacher_disagreement_score":0.0066392543,"about_ca_system_score_codex":0.00039369456,"about_ca_system_score_gemma":0.00030019076,"threshold_uncertainty_score":0.013201177},"labels":[],"label_agreement":null},{"id":"W1544893730","doi":"10.1016/0967-0653(93)95922-s","title":"10.1016/0967-0653(93)95922-s","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Sequence (biology); Tectonics; Sequence stratigraphy; Paleontology; Seismology; Stratigraphy; Biology; Genetics; Facies","score_opus":0.0080618790293458,"score_gpt":0.15986119219143902,"score_spread":0.15179931316209322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1544893730","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00046902834,0.00024753928,0.00040954814,0.00032424307,0.00024247564,0.00010201622,0.00085783965,0.0007332081,0.99661404],"genre_scores_gemma":[0.0007012682,0.00017404955,0.00027496612,0.00022938529,0.000069281996,0.000052069914,0.0004112238,0.0001412916,0.99794644],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994562,0.00004231293,0.0000491009,0.00019368918,0.00014075944,0.000117999094],"domain_scores_gemma":[0.99809223,0.00041632963,0.00010940121,0.00022800364,0.00048486554,0.0006692108],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00090680626,0.002506288,0.0015849929,0.002651697,0.0026104082,0.003371398,0.0028002039,0.0051632347,0.9903984],"category_scores_gemma":[0.001523293,0.0010053249,0.001267958,0.002417312,0.0017906706,0.00468262,0.0030072352,0.0021031958,0.9927181],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038040074,0.00025872036,0.0012540339,0.00054472795,0.0000386631,0.00030424385,0.00013011106,0.00046894266,0.0024372921,0.005268112,0.43852335,0.5503915],"study_design_scores_gemma":[0.00005554,0.00012982028,0.0010683942,0.00031230753,0.000013338527,0.00032268587,0.0001389697,0.00014608106,0.0002865209,0.00051261403,0.99699056,0.000023249606],"about_ca_topic_score_codex":0.0058516855,"about_ca_topic_score_gemma":0.0050498615,"teacher_disagreement_score":0.009601593,"about_ca_system_score_codex":0.0010713888,"about_ca_system_score_gemma":0.000899743,"threshold_uncertainty_score":0.013695419},"labels":[],"label_agreement":null},{"id":"W1545041215","doi":"10.1306/m82813c9","title":"Gravity-driven Fold Belts on Passive Margins","year":2004,"lang":"en","type":"book-chapter","venue":"American Association of Petroleum Geologists eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":394,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Thrust; Fold and thrust belt; Thrust fault; Tectonics; Geodynamics; Fold (higher-order function); Hydrocarbon exploration; Nappe; Inversion (geology); Seismology; Foreland basin; Geomorphology; Paleontology; Engineering; Aerospace engineering","score_opus":0.01069672530964684,"score_gpt":0.21053244804314505,"score_spread":0.1998357227334982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1545041215","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9491074,0.00069221796,0.0054550692,0.00035382068,0.0000478997,0.000016641496,0.00019712921,0.00011884303,0.04401106],"genre_scores_gemma":[0.9911704,0.00019209296,0.0003518955,0.000012356158,0.000009357941,0.0000023987861,0.00006502051,0.0000066432262,0.008189845],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99996996,0.0000046286705,0.0000018145349,0.000006283661,0.000010516912,0.000006819133],"domain_scores_gemma":[0.99995494,0.000010024042,0.000011642295,0.000006647576,0.000010048526,0.0000067423634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000054285534,0.00008835742,0.00008691969,0.0003407953,0.00020142682,0.00048447074,0.00022016719,0.00016730795,0.0042832675],"category_scores_gemma":[0.00023599897,0.000071437746,0.00008125909,0.000297076,0.0005202663,0.0004093887,0.0003889018,0.0001590588,0.0002657302],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055258645,0.00008201703,0.10718542,0.00036196003,0.00003979683,0.0022265774,0.004425361,0.07799348,0.14431266,0.35088313,0.012729697,0.29920727],"study_design_scores_gemma":[0.00006768144,0.00039928532,0.66995025,0.00011477514,0.000029976227,0.0018628718,0.0038609041,0.08185715,0.020984413,0.10527885,0.11554951,0.00004432688],"about_ca_topic_score_codex":0.0031792452,"about_ca_topic_score_gemma":0.0031867872,"teacher_disagreement_score":0.0042832675,"about_ca_system_score_codex":0.00050397386,"about_ca_system_score_gemma":0.0001277241,"threshold_uncertainty_score":0.014329016},"labels":[],"label_agreement":null},{"id":"W1547529343","doi":"10.4186/ej.2015.19.2.157","title":"Coseismic and Postseismic Displacement of 2011 Mw 6.8 Tarlay Earthquake, Myanmar using InSAR Techniques and Inversion Analysis","year":2015,"lang":"en","type":"article","venue":"Engineering Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; Chulalongkorn University; Geo-Informatics and Space Technology Development Agency; University of Leeds","keywords":"Interferometric synthetic aperture radar; Seismology; Geology; Displacement (psychology); Geodesy; Inversion (geology); Remote sensing; Synthetic aperture radar; Tectonics","score_opus":0.01793163525716719,"score_gpt":0.21100147178566916,"score_spread":0.19306983652850196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1547529343","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999236,0.000025210531,0.0002522074,0.000021104383,0.0000012044982,0.0000015974548,0.00008373958,0.000009429179,0.00036959775],"genre_scores_gemma":[0.9992718,0.00002593445,0.00028946335,0.0000033461497,0.0000025025865,0.0000018256328,0.00019940281,0.0000018333619,0.00020385762],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999486,0.0000074835234,0.000003125666,0.000015030163,0.000009602732,0.000016150927],"domain_scores_gemma":[0.99993086,0.0000089553005,0.000028630358,0.000008340232,0.00001662002,0.000006627881],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011387541,0.00021326402,0.000113137896,0.0004128247,0.000121920304,0.00020157438,0.0001535624,0.00014966163,0.00045708168],"category_scores_gemma":[0.00025379268,0.00010913548,0.00016347095,0.0004167618,0.00010448259,0.000258221,0.00020587724,0.00013680382,0.00014481362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002615902,0.00017556777,0.86287177,0.00006883954,0.00012954003,0.0010805466,0.0008395311,0.02394847,0.049911115,0.0006917685,0.0008525412,0.059168663],"study_design_scores_gemma":[0.00001001828,0.00007156789,0.9523355,0.000007395573,0.00003467718,0.00014923628,0.00035222282,0.042933624,0.0032985357,0.000060115068,0.0007337076,0.000013370088],"about_ca_topic_score_codex":0.011764336,"about_ca_topic_score_gemma":0.022163618,"teacher_disagreement_score":0.011764336,"about_ca_system_score_codex":0.00021914074,"about_ca_system_score_gemma":0.00021490105,"threshold_uncertainty_score":0.023391724},"labels":[],"label_agreement":null},{"id":"W1548686908","doi":"","title":"Early Earthquakes in the Americas","year":2006,"lang":"en","type":"article","venue":"Geoscience Canada","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Seismology; Geology; Geography","score_opus":0.009225596502156362,"score_gpt":0.18607158561542048,"score_spread":0.1768459891132641,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1548686908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9586239,0.0050104978,0.00012067995,0.0027458954,0.00010659031,0.000020757805,0.002933916,0.000022477076,0.030415239],"genre_scores_gemma":[0.9929929,0.002362681,0.00009946892,0.00019575565,0.00006286938,0.000005009027,0.0011707529,0.0000061333208,0.0031044672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997781,0.00001768345,0.000013452988,0.000023680634,0.00006707737,0.00010001326],"domain_scores_gemma":[0.99769187,0.00017947442,0.0003166409,0.000052084735,0.0013946118,0.00036535412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034068082,0.00021625396,0.000191165,0.0027895789,0.0014668271,0.0012453959,0.00031361138,0.0004376426,0.0023496577],"category_scores_gemma":[0.0019508982,0.00016373707,0.00008786153,0.004793024,0.0007541314,0.0007740758,0.0008191094,0.0006849317,0.00016456789],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024155245,0.00012951535,0.8949307,0.00025239508,0.00008009691,0.0010397229,0.010653552,0.0009451481,0.0015480092,0.0058482992,0.017492149,0.06683887],"study_design_scores_gemma":[0.0000054835905,0.000007926475,0.9831351,0.000040181505,0.000007549176,0.00007685251,0.0031886369,0.000058274316,0.000052586092,0.00014704443,0.013275886,0.000004464539],"about_ca_topic_score_codex":0.78507,"about_ca_topic_score_gemma":0.9135554,"teacher_disagreement_score":0.21493,"about_ca_system_score_codex":0.005513398,"about_ca_system_score_gemma":0.00466329,"threshold_uncertainty_score":0.43239152},"labels":[],"label_agreement":null},{"id":"W154980728","doi":"10.1016/s0967-0653(97)80990-8","title":"10.1016/s0967-0653(97)80990-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Shizuoka University","keywords":"Trench; Triple junction; Geology; Seismology; Tectonics; Materials science; Geophysics; Nanotechnology","score_opus":0.009999596858633759,"score_gpt":0.1668125535474884,"score_spread":0.15681295668885464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W154980728","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00046631062,0.00037448553,0.000508646,0.00037587556,0.00029266113,0.00012396781,0.0009467195,0.00089016976,0.9960212],"genre_scores_gemma":[0.0005209028,0.00018054915,0.00026291425,0.00022490995,0.00006534799,0.00007240334,0.00040422604,0.00016625403,0.9981025],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99925524,0.00004826762,0.00006853535,0.00029039697,0.00017307024,0.00016453261],"domain_scores_gemma":[0.99748814,0.00058153144,0.00018073167,0.00032682516,0.0006252657,0.0007975685],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013131154,0.0037330554,0.0024871458,0.0033852467,0.0028461707,0.004658472,0.0042120866,0.0073431814,0.9914801],"category_scores_gemma":[0.0018280238,0.0013924051,0.0017825806,0.0031725757,0.0026585828,0.006954687,0.0039880276,0.0033726385,0.99513936],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043795843,0.00026061802,0.0009850813,0.00069864327,0.00004747834,0.000293247,0.00014317065,0.000478569,0.002172692,0.0061165476,0.4154646,0.5729014],"study_design_scores_gemma":[0.00007811194,0.00014819056,0.0008261158,0.00046868305,0.00001787941,0.0003757076,0.00014982931,0.00018315957,0.0002941912,0.00060971966,0.9968154,0.000033003435],"about_ca_topic_score_codex":0.0052146213,"about_ca_topic_score_gemma":0.0043501304,"teacher_disagreement_score":0.008519888,"about_ca_system_score_codex":0.0014253517,"about_ca_system_score_gemma":0.0011903231,"threshold_uncertainty_score":0.012152493},"labels":[],"label_agreement":null},{"id":"W1558253042","doi":"10.1029/rf004p0553","title":"ESR Dating of Times of Movement on the San Gabriel Fault in the Little Tujunga Region, Los Angeles, California","year":2011,"lang":"en","type":"book-chapter","venue":"AGU reference shelf","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Fault (geology); Movement (music); Archaeology; Cartography; Geography; Seismology; Geology; Art; Aesthetics","score_opus":0.053174889444149324,"score_gpt":0.2227448906302308,"score_spread":0.16957000118608148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1558253042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7728703,0.010282627,0.0067821923,0.00094595464,0.00034823266,0.00007490643,0.027198073,0.0015988474,0.17989886],"genre_scores_gemma":[0.83642215,0.008419605,0.018526467,0.00018351119,0.00023601783,0.000080858386,0.018889582,0.00042723576,0.11681464],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99994564,0.000003946741,0.000004168518,0.000017359385,0.000022684262,0.000006184393],"domain_scores_gemma":[0.99967706,0.000040484072,0.00004560889,0.000030236275,0.00019231017,0.000014220764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000272375,0.00016890091,0.00011031771,0.002633344,0.00062207395,0.0008278969,0.0004895455,0.00026139434,0.004002019],"category_scores_gemma":[0.00068439497,0.00023259214,0.00008885178,0.003761027,0.00023919399,0.0005305424,0.0002188979,0.0003151264,0.00068204413],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015820397,0.000061722094,0.27031523,0.00042857704,0.00008829182,0.00040937483,0.004354102,0.0087655,0.01669135,0.006811533,0.121622466,0.57029366],"study_design_scores_gemma":[0.000011241848,0.000022191205,0.79452276,0.0001795825,0.00004227826,0.00017594638,0.00055286085,0.0011168612,0.00291451,0.00037080966,0.2000679,0.000023020188],"about_ca_topic_score_codex":0.1562509,"about_ca_topic_score_gemma":0.48117727,"teacher_disagreement_score":0.1562509,"about_ca_system_score_codex":0.0013955801,"about_ca_system_score_gemma":0.00075030146,"threshold_uncertainty_score":0.31068283},"labels":[],"label_agreement":null},{"id":"W1565595715","doi":"10.1029/2008tc002334","title":"Fault displacement accumulation and slip rate variability within the Taupo Rift (New Zealand) based on trench and 3‐D ground‐penetrating radar data","year":2009,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Trench; Seismology; Ground-penetrating radar; Slip (aerodynamics); Fault (geology); Rift; Active fault; Thrust fault; Submarine pipeline; Tectonics; Radar; Geotechnical engineering","score_opus":0.043662242551695075,"score_gpt":0.27515403235645747,"score_spread":0.2314917898047624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1565595715","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994997,0.000022926373,0.0001702984,0.0000038178127,3.1952135e-7,0.0000024321944,0.00010332273,0.0000035458215,0.00019360306],"genre_scores_gemma":[0.9993923,0.000045994417,0.00022864534,0.0000012972462,7.53349e-7,0.000003145877,0.00023143036,0.0000015348368,0.00009491309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988294,0.000009742305,0.000010060247,0.00004713653,0.000028540988,0.000021681015],"domain_scores_gemma":[0.999469,0.00008246392,0.00028140398,0.000048699167,0.00007003242,0.000048409664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022751513,0.00017806694,0.00013795687,0.00090581545,0.00017216412,0.00041134056,0.00017680328,0.000153035,0.00053705595],"category_scores_gemma":[0.0010755745,0.00014297097,0.00015386374,0.0008128308,0.00040232218,0.00037738887,0.00033599307,0.00013523344,0.000113555296],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012670092,0.000025027774,0.962068,0.000031611256,0.00005002684,0.0002947686,0.0011034614,0.0029496546,0.01518057,0.000062307874,0.00008532102,0.018022455],"study_design_scores_gemma":[0.0000018854882,0.000015330366,0.99849653,0.0000022845934,0.0000056361832,0.00005753382,0.00006805161,0.0010525123,0.00021889013,0.000009340189,0.00006888925,0.0000030168055],"about_ca_topic_score_codex":0.065456346,"about_ca_topic_score_gemma":0.11368676,"teacher_disagreement_score":0.065456346,"about_ca_system_score_codex":0.00060553406,"about_ca_system_score_gemma":0.0002274403,"threshold_uncertainty_score":0.13015068},"labels":[],"label_agreement":null},{"id":"W1570914366","doi":"10.1002/2013jb010578","title":"The long‐wavelength admittance and effective elastic thickness of the Canadian Shield","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Craton; Lithosphere; Indian Shield; Crust; Mantle (geology); Shield; Seismology; Convection; Geophysics; Wavelength; Admittance; Geodesy; Tectonics; Petrology; Mechanics; Physics","score_opus":0.019611468512191116,"score_gpt":0.2834648703866294,"score_spread":0.2638534018744383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1570914366","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99556255,0.00008222641,0.0006496549,0.00003709198,0.0000022993024,0.000004665811,0.00096698914,0.000017679205,0.0026768777],"genre_scores_gemma":[0.99905306,0.000041501724,0.00024770483,0.0000050247722,8.28895e-7,0.0000012638355,0.0002586366,0.0000034495783,0.0003884838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987805,0.0000042726697,0.000004074429,0.000021802953,0.000058816906,0.000033003616],"domain_scores_gemma":[0.99958175,0.000041597687,0.000058598398,0.000013344936,0.000255109,0.000049566755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014870599,0.00035183554,0.000114436,0.001598521,0.0008713096,0.0007117694,0.00043687256,0.00020930155,0.0020409205],"category_scores_gemma":[0.0006801102,0.00012465587,0.00017233871,0.0015529527,0.00049678003,0.00026411592,0.00032870614,0.00017413772,0.00017693569],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018867034,0.000028405617,0.91040784,0.00007350227,0.00014614548,0.0005341977,0.0009429022,0.013611213,0.035877567,0.0018369908,0.0010248242,0.035327747],"study_design_scores_gemma":[0.0000023994044,0.000004053606,0.99294734,0.0000066929238,0.000008783924,0.00005350646,0.00037983325,0.004470965,0.0013981148,0.0001193956,0.0005962881,0.000012499295],"about_ca_topic_score_codex":0.92639107,"about_ca_topic_score_gemma":0.95131856,"teacher_disagreement_score":0.073608935,"about_ca_system_score_codex":0.0047250288,"about_ca_system_score_gemma":0.0025766396,"threshold_uncertainty_score":0.14808482},"labels":[],"label_agreement":null},{"id":"W1576236270","doi":"","title":"LARGE LEONID ENTRY MODELING: APPLICATION TO THE BOLIDE OF 11/17/1998","year":2001,"lang":"en","type":"paratext","venue":"University of North Texas Digital Library (University of North Texas)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Douglas College","funders":"Los Alamos National Laboratory; U.S. Department of Energy","keywords":"Aerodynamics; Aerospace engineering; Event (particle physics); Astrobiology; Physics; Geology; Engineering; Astrophysics","score_opus":0.011464453764425406,"score_gpt":0.17245284320207713,"score_spread":0.16098838943765173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1576236270","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9180175,0.00031452486,0.035787545,0.0007071062,0.00007435026,0.00009903007,0.0013342362,0.0007343211,0.04293152],"genre_scores_gemma":[0.99005085,0.00015579218,0.005732999,0.000041115723,0.000020857788,0.000050008326,0.0005397197,0.000110003995,0.0032986617],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998629,0.000042155225,0.000005763291,0.000032709795,0.000024792464,0.000031664236],"domain_scores_gemma":[0.9994843,0.00029044363,0.00006465462,0.000028571021,0.00006699674,0.00006501639],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031194626,0.00062100444,0.0007719991,0.000619175,0.0009292114,0.0014196545,0.0014778599,0.001523346,0.004111657],"category_scores_gemma":[0.0017040401,0.000380484,0.0006610054,0.0006355994,0.00061929924,0.000696771,0.00092882063,0.0010502702,0.0003405847],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040848056,0.000042582287,0.00607908,0.00001888612,0.00002010881,0.00017970966,0.00012298409,0.98598623,0.00022421952,0.0033081863,0.0011524812,0.0028247156],"study_design_scores_gemma":[0.000023699125,0.000020342006,0.0011464763,0.0000065350537,0.000007734087,0.000018678826,0.00008208492,0.99696976,0.0001012911,0.0007126407,0.0009022245,0.000008594132],"about_ca_topic_score_codex":0.111288376,"about_ca_topic_score_gemma":0.08820051,"teacher_disagreement_score":0.111288376,"about_ca_system_score_codex":0.0017354665,"about_ca_system_score_gemma":0.0012271355,"threshold_uncertainty_score":0.22128117},"labels":[],"label_agreement":null},{"id":"W1579686336","doi":"10.3133/ofr20081343","title":"Report on the Aseismic Slip, Tremor, and Earthquakes Workshop","year":2008,"lang":"en","type":"article","venue":"Antarctica A Keystone in a Changing World","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Oregon State University; University of Washington; Harvard University; Georgia Institute of Technology; University of Miami","keywords":"Outreach; Engineering; Seismic hazard; Forensic engineering; Earthquake engineering; Library science; Psychology; Seismology; Civil engineering; Political science; Geology; Computer science; Law","score_opus":0.03427930340507576,"score_gpt":0.23835972315046294,"score_spread":0.20408041974538718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1579686336","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.034585606,0.018708512,0.0071236463,0.2570763,0.19454065,0.00303229,0.0150134945,0.0008398655,0.4690796],"genre_scores_gemma":[0.08483246,0.015019485,0.005055847,0.05092261,0.021126792,0.0047779027,0.017241795,0.0009832932,0.8000399],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99607384,0.00082048326,0.00013294104,0.00039853074,0.0014506025,0.0011236462],"domain_scores_gemma":[0.9919356,0.0010442791,0.00016426151,0.00021617854,0.0026360764,0.0040035984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008433752,0.0013746468,0.0008559223,0.0008991178,0.0057350816,0.009090164,0.002620066,0.005994812,0.05882205],"category_scores_gemma":[0.008478194,0.0007021105,0.0013675276,0.0010750403,0.0010321528,0.0033515322,0.0094958125,0.007881258,0.025118234],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000105835825,0.00017604105,0.00046087336,0.00023991111,0.0000101399155,0.00039770067,0.0030274333,0.00016332907,0.00045399397,0.0021148932,0.9731476,0.01970227],"study_design_scores_gemma":[0.000021913813,0.000043645996,0.0013918054,0.00024864957,0.000006199482,0.00004624881,0.005269462,0.00005392029,0.00013546422,0.00064690557,0.99211216,0.000023686709],"about_ca_topic_score_codex":0.015789576,"about_ca_topic_score_gemma":0.031105747,"teacher_disagreement_score":0.05882205,"about_ca_system_score_codex":0.0040072147,"about_ca_system_score_gemma":0.011393708,"threshold_uncertainty_score":0.19677937},"labels":[],"label_agreement":null},{"id":"W1580920507","doi":"","title":"한반도 남부에서의 지진파 감쇠 : 분석방법과 사용한 자료에 따른 변화 비교","year":2007,"lang":"ko","type":"article","venue":"Journal of the geological society of Korea","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Coda; Physics; Mathematics; Geology; Seismology","score_opus":0.025074732324044207,"score_gpt":0.23568494030809292,"score_spread":0.21061020798404873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1580920507","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.055131774,0.010179216,0.03633084,0.03346789,0.0018628653,0.00020129606,0.0005032138,0.00024202153,0.86208093],"genre_scores_gemma":[0.86392874,0.00577382,0.02472426,0.0031790251,0.0005930705,0.00018762912,0.00027540742,0.00011357566,0.10122446],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.998618,0.00039689496,0.0001036645,0.00028352934,0.00044433668,0.00015349443],"domain_scores_gemma":[0.99821424,0.00047423915,0.0002773555,0.00014187602,0.0006618649,0.00023046044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018812813,0.00046669968,0.00028839603,0.0014089087,0.0025692838,0.008103294,0.000703849,0.0014109933,0.014977129],"category_scores_gemma":[0.0037758495,0.00035518387,0.00034977554,0.001538577,0.009689676,0.007284493,0.0016646913,0.0018754847,0.003231876],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049852806,0.00004279687,0.0041541653,0.0002897617,0.000036822734,0.00019146637,0.005794192,0.0007053589,0.00093949167,0.88934237,0.020346561,0.078107156],"study_design_scores_gemma":[0.000031731863,0.00009132517,0.009847681,0.00041778528,0.000055047898,0.0006178274,0.01098512,0.0015435357,0.0016876543,0.5180296,0.4566232,0.00006961076],"about_ca_topic_score_codex":0.006089695,"about_ca_topic_score_gemma":0.006724257,"teacher_disagreement_score":0.014977129,"about_ca_system_score_codex":0.0040635867,"about_ca_system_score_gemma":0.0047841663,"threshold_uncertainty_score":0.050103486},"labels":[],"label_agreement":null},{"id":"W1581619530","doi":"10.1002/tect.20075","title":"Thermal‐mechanical modeling of salt‐based mountain belts with pre‐existing basement faults: Application to the Zagros fold and thrust belt, southwest Iran","year":2013,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Basement; Foreland basin; Petrology; Décollement; Fold (higher-order function); Geothermal gradient; Crust; Anticline; Fold and thrust belt; Seismology; Geomorphology; Geochemistry; Geophysics; Tectonics","score_opus":0.022362414333726956,"score_gpt":0.22747502036484263,"score_spread":0.20511260603111567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1581619530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990399,0.00012972666,0.0064997794,0.00011457512,0.000017706649,0.0000338257,0.00034785553,0.00016739531,0.0022900573],"genre_scores_gemma":[0.99716467,0.00006628936,0.002109835,0.00001017029,0.0000101321,0.000019265652,0.00014191256,0.00001531966,0.00046242596],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992454,0.000015328722,0.0000062160734,0.000020078329,0.000011663856,0.000022159837],"domain_scores_gemma":[0.9998282,0.000054422628,0.000037868354,0.000020404263,0.000030568703,0.000028489334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021337038,0.0006548991,0.0005121915,0.00063770404,0.0005915234,0.0009286167,0.0012094796,0.0012459862,0.001291954],"category_scores_gemma":[0.00058151607,0.00057660486,0.0010039002,0.00070499233,0.00046418005,0.0004009943,0.00042678355,0.00040792156,0.00018711768],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033455726,0.000060294096,0.008573802,0.000011922787,0.000025413188,0.00009136397,0.000038670965,0.9878991,0.0010763198,0.00018688335,0.000092788236,0.0019099696],"study_design_scores_gemma":[0.000014778952,0.000012186945,0.003465456,0.0000017875192,0.00000571171,0.000013475318,0.00002719152,0.9962214,0.00008375266,0.00006760721,0.00008167572,0.000004928345],"about_ca_topic_score_codex":0.079393744,"about_ca_topic_score_gemma":0.03791236,"teacher_disagreement_score":0.079393744,"about_ca_system_score_codex":0.000883428,"about_ca_system_score_gemma":0.0008847282,"threshold_uncertainty_score":0.15786326},"labels":[],"label_agreement":null},{"id":"W1582289655","doi":"","title":"Plate Boundary Observatory Borehole Strainmeter Recordings Of The 29 September 2009 Tsunami","year":2009,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Epicenter; Trough (economics); Observatory; Oceanography","score_opus":0.0219535844893385,"score_gpt":0.2221833551203014,"score_spread":0.20022977063096292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1582289655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9495922,0.000059681908,0.00072354334,0.00020625349,0.0001134253,0.00010945905,0.031569816,0.00024130105,0.01738436],"genre_scores_gemma":[0.9660063,0.0001002039,0.0020308422,0.00006986459,0.00004299785,0.00007902536,0.026256302,0.000025473635,0.005389062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998017,0.000010245213,0.000016152699,0.000039278562,0.0001013898,0.000031140753],"domain_scores_gemma":[0.99949455,0.000025865676,0.00011849971,0.000043777167,0.00024974815,0.00006748202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017963465,0.00023342902,0.00013620079,0.00080153,0.00045354376,0.00035837395,0.0002672325,0.0003594233,0.003292527],"category_scores_gemma":[0.00067226024,0.00014258514,0.00006436918,0.00077353744,0.00015079355,0.00033916935,0.0004907945,0.000369068,0.0012870493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010607629,0.0006296145,0.73601544,0.00021365334,0.000050800092,0.0016698962,0.005501083,0.0016332554,0.12117834,0.00070122076,0.051159214,0.08018667],"study_design_scores_gemma":[0.00001862152,0.0000805038,0.98919535,0.000014608075,0.0000057941834,0.00007997747,0.0005071315,0.0007447454,0.0031239144,0.000041761712,0.006174024,0.000013513533],"about_ca_topic_score_codex":0.036010806,"about_ca_topic_score_gemma":0.11008116,"teacher_disagreement_score":0.036010806,"about_ca_system_score_codex":0.00036696665,"about_ca_system_score_gemma":0.00046211435,"threshold_uncertainty_score":0.071602404},"labels":[],"label_agreement":null},{"id":"W1584202978","doi":"10.1029/me004p0367","title":"Velocity Changes in the Charlevoix Region, Quebec","year":2011,"lang":"en","type":"book-chapter","venue":"Maurice Ewing series","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shot (pellet); Geology; Shore; Magnitude (astronomy); Geodesy; Seismology; Physics; Oceanography","score_opus":0.03922534180930127,"score_gpt":0.20168488785109795,"score_spread":0.1624595460417967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1584202978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906337,0.0007162161,0.00025794024,0.000214055,0.00001646945,0.000028426253,0.0016295803,0.000040642648,0.006463144],"genre_scores_gemma":[0.9934069,0.00024886843,0.00023858513,0.00004123476,0.000003891314,0.000012535097,0.0008997486,0.000006585869,0.0051417304],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99968946,0.000026230153,0.0000106290545,0.00007319758,0.0001063273,0.00009418262],"domain_scores_gemma":[0.9991886,0.000059382535,0.00014908507,0.000023901477,0.00044814099,0.00013091565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025397472,0.00025936688,0.00017730182,0.0011408883,0.0014332694,0.0010539116,0.0006918375,0.00034551712,0.0026027951],"category_scores_gemma":[0.0010874589,0.00018027966,0.0001107732,0.0017715995,0.00062467204,0.00026707383,0.00035299765,0.00034288884,0.0002578232],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003611246,0.0002046889,0.8768111,0.00018141021,0.0001884469,0.0008732564,0.003502636,0.0049995356,0.012779173,0.001291626,0.008140786,0.090666346],"study_design_scores_gemma":[0.00001121245,0.000030451258,0.99471104,0.000015804339,0.000007765949,0.000034899025,0.0005617183,0.00082137325,0.0002679012,0.000017544968,0.0035077273,0.000012650817],"about_ca_topic_score_codex":0.9912901,"about_ca_topic_score_gemma":0.9966235,"teacher_disagreement_score":0.020987786,"about_ca_system_score_codex":0.020987786,"about_ca_system_score_gemma":0.008465092,"threshold_uncertainty_score":0.15227777},"labels":[],"label_agreement":null},{"id":"W1585019985","doi":"","title":"Effects of Plate Boundary Variations on Elevation, Coast Mountains, British Columbia","year":2004,"lang":"en","type":"article","venue":"Occidental College Scholar (Occidental College)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Elevation (ballistics); Geology; Boundary (topology); Geography; Physical geography; Oceanography; Climatology; Geometry","score_opus":0.005720456433584487,"score_gpt":0.20106322710819532,"score_spread":0.19534277067461084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1585019985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99360234,0.00021288473,0.000057506044,0.0001364211,0.000006939183,0.000007847101,0.0010428742,0.000021963686,0.0049111573],"genre_scores_gemma":[0.9973569,0.00009922706,0.00005738786,0.000017211254,0.0000012911985,0.000005881804,0.00071983703,0.0000102646145,0.0017320184],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993544,0.00012008959,0.0000323144,0.000121905025,0.0002260758,0.00014515482],"domain_scores_gemma":[0.99779236,0.0004412141,0.0002616102,0.00012913755,0.0008170756,0.0005586708],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000267151,0.00021660683,0.00029434584,0.0008803986,0.0015222498,0.0016836479,0.00061741535,0.0002230037,0.004303787],"category_scores_gemma":[0.003156367,0.00016790215,0.00022159526,0.002362924,0.0006743782,0.00025808022,0.0008334098,0.0004646916,0.0003687439],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002617996,0.00006378023,0.9808092,0.000025948508,0.00010949074,0.00051399984,0.00069353025,0.0016110252,0.0015962677,0.0002775938,0.0018870671,0.012150217],"study_design_scores_gemma":[0.000002803762,0.00000998936,0.9982539,0.000008318459,0.000011885318,0.000027211705,0.000713564,0.00037296608,0.00007463516,0.00002142107,0.00049932156,0.0000039641704],"about_ca_topic_score_codex":0.95690674,"about_ca_topic_score_gemma":0.97703826,"teacher_disagreement_score":0.043093264,"about_ca_system_score_codex":0.007222004,"about_ca_system_score_gemma":0.0053596343,"threshold_uncertainty_score":0.08669406},"labels":[],"label_agreement":null},{"id":"W1586209620","doi":"10.1002/grl.50220","title":"Tremors along the Queen Charlotte Margin triggered by large teleseismic earthquakes","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Seismology; Geology; Epicenter; Rayleigh wave; Thrust fault; Amplitude; Tectonics; Fault (geology); Queen (butterfly); Geodesy; Surface wave","score_opus":0.02306543395290682,"score_gpt":0.25863779705872986,"score_spread":0.23557236310582302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1586209620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99804485,0.0001535445,0.000060249204,0.000024184812,0.0000023390892,0.000018303488,0.0005956477,0.000008124479,0.0010926636],"genre_scores_gemma":[0.99856925,0.00010137758,0.000109716224,0.000017743545,0.0000025702018,0.000007527842,0.0004391517,0.0000024733683,0.00075007585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971956,0.000018451023,0.000013582386,0.000055818255,0.00013178689,0.000060775223],"domain_scores_gemma":[0.99847883,0.00013657923,0.00048293106,0.00006283744,0.0005575284,0.0002813218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015333867,0.00019434745,0.000204875,0.0021995406,0.0010416891,0.0006182607,0.0004047023,0.00025859821,0.0009274278],"category_scores_gemma":[0.0008245776,0.00012868264,0.00013085773,0.002073797,0.00047260206,0.00012878698,0.000523907,0.00016181899,0.00016850005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014044676,0.000031804553,0.97263217,0.000063905856,0.000046369893,0.00066227716,0.0009966074,0.00031201792,0.012376701,0.000069096604,0.00067858474,0.01199002],"study_design_scores_gemma":[0.0000022591153,0.000016271062,0.9985636,0.000007001447,0.0000047721414,0.00007392847,0.00030784533,0.000101233054,0.00033783508,0.000004799732,0.00057652977,0.0000039975766],"about_ca_topic_score_codex":0.78992695,"about_ca_topic_score_gemma":0.92433673,"teacher_disagreement_score":0.78992695,"about_ca_system_score_codex":0.003215003,"about_ca_system_score_gemma":0.004217504,"threshold_uncertainty_score":0.42262042},"labels":[],"label_agreement":null},{"id":"W1589276833","doi":"10.1029/gm043p0391","title":"Lithospheric Thinning Under the Atlantis-Meteor Seamount Complex (North Atlantic)","year":2011,"lang":"en","type":"book-chapter","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Seamount; Meteor (satellite); Geology; Lithosphere; Thinning; Subduction; Oceanography; Mid-Atlantic Ridge; Seismology; Tectonics; Geography; Meteorology","score_opus":0.03481205524168205,"score_gpt":0.20717449007382147,"score_spread":0.17236243483213942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1589276833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993818,0.00007653286,0.000039936527,0.0000040688196,6.852344e-7,0.000001328947,0.000109164095,0.000004872118,0.00038152104],"genre_scores_gemma":[0.99965346,0.00003965326,0.000060450682,0.0000014456267,9.663446e-7,8.0013217e-7,0.00012264347,0.000001072456,0.00011946667],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9999403,0.000006242936,0.000006120966,0.000016935865,0.000014635343,0.000015780211],"domain_scores_gemma":[0.9999069,0.0000063267985,0.000049515213,0.000008741905,0.000015557966,0.000012988918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011493612,0.00014149836,0.00008943245,0.00054139615,0.00028321563,0.000400744,0.00013944633,0.0001571035,0.00092327956],"category_scores_gemma":[0.0002233565,0.00008238938,0.00015836372,0.0006092574,0.00022082438,0.00016660496,0.0003461422,0.0000899173,0.00012616586],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027324472,0.000013409834,0.93360895,0.000056061388,0.00006649155,0.0006755285,0.0006271944,0.0025434997,0.046964303,0.00023334866,0.000094040544,0.014844063],"study_design_scores_gemma":[0.0000013675075,0.00001854531,0.9982951,0.000002202032,0.0000063995235,0.000114464674,0.00008795927,0.0004125976,0.00079625554,0.000014353876,0.00024915388,0.00000162539],"about_ca_topic_score_codex":0.024742149,"about_ca_topic_score_gemma":0.030745687,"teacher_disagreement_score":0.024742149,"about_ca_system_score_codex":0.000483996,"about_ca_system_score_gemma":0.00027544532,"threshold_uncertainty_score":0.049196303},"labels":[],"label_agreement":null},{"id":"W1589718177","doi":"","title":"A Regional Seismic Travel Time Model for North America","year":2010,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Epicenter; Geology; Magnitude (astronomy); Tectonics; Geodesy","score_opus":0.021023866924979834,"score_gpt":0.21165928388484154,"score_spread":0.1906354169598617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1589718177","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3393622,0.00086622534,0.6008231,0.0015741864,0.00013142268,0.00025477094,0.009368452,0.0022367428,0.045382895],"genre_scores_gemma":[0.90316117,0.00074405194,0.05885793,0.00017278382,0.000051277537,0.00043643324,0.005370479,0.00043500715,0.030770846],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998431,0.000040054118,0.000008465281,0.000060535367,0.000025700385,0.000022098184],"domain_scores_gemma":[0.99968445,0.00011825746,0.000048389174,0.00002574448,0.00010377212,0.000019322866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048607812,0.0007984027,0.00051401946,0.0007022591,0.00038341843,0.0010991325,0.001890144,0.0010502953,0.007823233],"category_scores_gemma":[0.001456796,0.0005858129,0.0009747866,0.0010182895,0.00043230824,0.0008147167,0.0005784285,0.0010280601,0.001247902],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023705077,0.000010295666,0.001166514,0.000011645531,0.000019447249,0.000032794287,0.000033709483,0.9917148,0.00025430226,0.0033466811,0.000589015,0.0027971156],"study_design_scores_gemma":[0.0000054866664,0.000003730842,0.00024924928,0.000002817047,0.0000054161137,0.000011058655,0.0000067463534,0.9982431,0.000041620136,0.00065796875,0.0007696383,0.000003226811],"about_ca_topic_score_codex":0.09317621,"about_ca_topic_score_gemma":0.04210085,"teacher_disagreement_score":0.09317621,"about_ca_system_score_codex":0.0019621714,"about_ca_system_score_gemma":0.0016649354,"threshold_uncertainty_score":0.18526775},"labels":[],"label_agreement":null},{"id":"W160165940","doi":"","title":"Microstructures from the San Andreas Fault Observatory at Depth (SAFOD) Phase 3 Cores","year":2010,"lang":"en","type":"article","venue":"EGUGA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of New Brunswick","funders":"","keywords":"Geology; Phase (matter); Observatory; Seismology; Chemistry","score_opus":0.02049452332423579,"score_gpt":0.24105658690090678,"score_spread":0.220562063576671,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W160165940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931039,0.00006388948,0.00019856516,0.000027347753,0.0000061017304,0.000008762659,0.0034619877,0.000041816627,0.0030875406],"genre_scores_gemma":[0.9947908,0.00006458217,0.0005378913,0.000022245837,0.000010083659,0.00000929958,0.0032032386,0.000028110298,0.0013337381],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.0000045379284,0.000009118145,0.000029326926,0.00003214016,0.00002257107],"domain_scores_gemma":[0.9993315,0.000034743425,0.00013285203,0.00005123534,0.00036090202,0.00008895817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013406889,0.00018829676,0.0002071589,0.0014118126,0.0005041838,0.00038620547,0.00023338539,0.00034213654,0.003166557],"category_scores_gemma":[0.0006081272,0.00023597376,0.00012885676,0.0012232915,0.00023745795,0.0002770157,0.0003230747,0.00016883874,0.000638156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005821361,0.00023414579,0.8192418,0.000109971785,0.00008577313,0.000450986,0.0016783894,0.0025622004,0.1381006,0.0007235076,0.004224707,0.032005705],"study_design_scores_gemma":[0.00000462038,0.000021011985,0.9970619,0.000002681773,0.00000818752,0.000037846217,0.00010826677,0.0005577743,0.001155419,0.00002094432,0.0010178422,0.0000034873133],"about_ca_topic_score_codex":0.063176386,"about_ca_topic_score_gemma":0.17024916,"teacher_disagreement_score":0.063176386,"about_ca_system_score_codex":0.00044924286,"about_ca_system_score_gemma":0.00042022998,"threshold_uncertainty_score":0.12561733},"labels":[],"label_agreement":null},{"id":"W1602863192","doi":"","title":"The 2005 Modification of GIT Geological Map of the Ocean Floor - an Effective Tool for the Prediction of the Most Powerful Earthquakes","year":2007,"lang":"en","type":"article","venue":"RACO (Revistes Catalanes amb Accés Obert) (Consorci de Serveis Universitaris de Catalunya)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Cartography; Seismology; Geography","score_opus":0.011463980677060477,"score_gpt":0.21456884293206507,"score_spread":0.2031048622550046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1602863192","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19998498,0.0020287929,0.08284358,0.005163921,0.0021754897,0.0023402274,0.46990812,0.03079072,0.2047641],"genre_scores_gemma":[0.3548813,0.0024073124,0.22598766,0.00052156224,0.0003135725,0.0008438438,0.34251636,0.003634822,0.06889355],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9996706,0.000040524064,0.000020698575,0.000029597528,0.00019855505,0.000040010178],"domain_scores_gemma":[0.998475,0.00007822079,0.0001234253,0.00013778162,0.001033999,0.0001515848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005523254,0.0005505269,0.00030730327,0.0041951803,0.00036285358,0.0010738447,0.00045789327,0.0004022472,0.010863912],"category_scores_gemma":[0.003157345,0.0002984062,0.00036404844,0.003569244,0.00018509105,0.00038940113,0.0008900813,0.0005650123,0.006893087],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043252922,0.000066208726,0.070509315,0.0002733892,0.000079441896,0.0006881258,0.00044604644,0.025560891,0.0043353797,0.0012296714,0.61990035,0.2764787],"study_design_scores_gemma":[0.0001879737,0.00012274404,0.30254903,0.00022794372,0.00011202393,0.00031667203,0.0007861543,0.033640675,0.0046891514,0.0007114169,0.6565563,0.00009991942],"about_ca_topic_score_codex":0.16830342,"about_ca_topic_score_gemma":0.20522813,"teacher_disagreement_score":0.16830342,"about_ca_system_score_codex":0.001139654,"about_ca_system_score_gemma":0.0031997538,"threshold_uncertainty_score":0.3346476},"labels":[],"label_agreement":null},{"id":"W1602907915","doi":"10.1017/cbo9781107296916.013","title":"Applications in geological monitoring: paleoseismology and paleoclimatology","year":2014,"lang":"en","type":"book-chapter","venue":"Cambridge University Press eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Salt marsh; Flooding (psychology); Shore; Marsh; Climate change; Storm; Oceanography; Physical geography; Geography; Ecology; Wetland","score_opus":0.02296607479078365,"score_gpt":0.19715854271933322,"score_spread":0.1741924679285496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1602907915","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0035122086,0.12633844,0.080296926,0.013855398,0.0053828266,0.00014637956,0.0020587682,0.0012508364,0.7671582],"genre_scores_gemma":[0.05208471,0.124797024,0.07670453,0.0032675453,0.0050139185,0.00021784683,0.0021803067,0.00080126437,0.73493284],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997434,0.00006175908,0.000020961072,0.00006240442,0.000097324264,0.000014067983],"domain_scores_gemma":[0.99956506,0.00020327515,0.000025069681,0.00006441514,0.00010441528,0.000037794754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006123661,0.00085206237,0.00045678965,0.0017635386,0.00047914122,0.0031523006,0.0007765519,0.0013020867,0.05254395],"category_scores_gemma":[0.0013625778,0.00033830904,0.00026526797,0.004435325,0.0012699201,0.0037610412,0.0017438551,0.0012464396,0.014691371],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013715445,0.000020807025,0.0009881286,0.00043349044,0.000012111263,0.000081710925,0.0004526473,0.0012482762,0.0005579409,0.13798836,0.16566296,0.6925399],"study_design_scores_gemma":[0.0000023045613,0.0000069629036,0.0014264461,0.00025657413,0.0000049537475,0.0001626467,0.00017413803,0.0008489651,0.00018089711,0.052872505,0.9440547,0.00000888554],"about_ca_topic_score_codex":0.0030663789,"about_ca_topic_score_gemma":0.0053516533,"teacher_disagreement_score":0.05254395,"about_ca_system_score_codex":0.00083931675,"about_ca_system_score_gemma":0.000512078,"threshold_uncertainty_score":0.17577702},"labels":[],"label_agreement":null},{"id":"W1603372043","doi":"10.1002/2015gl064363","title":"Low‐frequency earthquakes at the southern Cascadia margin","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of British Columbia","funders":"","keywords":"Geology; Seismology; San andreas fault; Episodic tremor and slip; Slip (aerodynamics); Fault (geology); Subduction; Tectonics","score_opus":0.05600191853403335,"score_gpt":0.2834310451376872,"score_spread":0.22742912660365383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1603372043","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99919134,0.000017146702,0.000044269294,0.000019520823,9.675842e-7,0.0000022532672,0.00026040676,0.000015916394,0.0004482354],"genre_scores_gemma":[0.9994004,0.000010861829,0.00006402483,0.0000021968053,0.0000012373812,0.0000021893472,0.00037416458,0.0000018913316,0.00014309426],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985945,0.000021479887,0.000008749981,0.00004957022,0.000037120433,0.000023718296],"domain_scores_gemma":[0.99944276,0.00007695214,0.00015488056,0.000065015374,0.00010888129,0.00015146412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024604207,0.00021379498,0.00016706024,0.0009907405,0.00046934944,0.00048409335,0.00022170009,0.00018776002,0.001077881],"category_scores_gemma":[0.0012823843,0.000113694856,0.00012680993,0.00071840966,0.00020720156,0.00013978129,0.0003559347,0.00014290745,0.00015729415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014655356,0.000035378944,0.9829914,0.000020067471,0.000042996733,0.00020010227,0.00035295502,0.0027495036,0.005918426,0.000060251667,0.00032774967,0.007154582],"study_design_scores_gemma":[0.0000054028637,0.000010850186,0.99855775,0.000002567448,0.00000700683,0.000014498302,0.00010152754,0.0010002736,0.00013485883,0.000015263598,0.00014727804,0.0000027303977],"about_ca_topic_score_codex":0.10073173,"about_ca_topic_score_gemma":0.18486105,"teacher_disagreement_score":0.10073173,"about_ca_system_score_codex":0.00084482593,"about_ca_system_score_gemma":0.00041058232,"threshold_uncertainty_score":0.2002908},"labels":[],"label_agreement":null},{"id":"W1604312882","doi":"10.1002/2014jb011744","title":"Self‐similar rupture implied by scaling properties of volcanic earthquakes occurring during the 2004‐2008 eruption of Mount St. Helens, Washington","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Volcano; Scaling; Geology; Impact crater; Seismometer; Geodesy; Physics; Mathematics; Geometry","score_opus":0.0435549921846325,"score_gpt":0.286415734267319,"score_spread":0.2428607420826865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1604312882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99958795,0.000007621782,0.00021605226,0.0000044364747,4.626335e-7,0.000001962366,0.000033450462,0.000004710094,0.00014338999],"genre_scores_gemma":[0.9998356,0.000003966879,0.00007481939,0.0000010422912,0.0000011931352,0.0000010783058,0.00006240345,0.0000011001347,0.000018830942],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998665,0.000026506708,0.00001560624,0.000036935722,0.000028706596,0.000025753661],"domain_scores_gemma":[0.9986299,0.00032598706,0.000554331,0.00021270663,0.00014900413,0.00012809581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033176693,0.00014743555,0.00019286531,0.001434219,0.00025870523,0.0004789081,0.00018295879,0.00021735388,0.00062496145],"category_scores_gemma":[0.0023741608,0.00017902984,0.00027362094,0.000582847,0.00044164743,0.00036145683,0.0002872435,0.00015187437,0.00012519919],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083358325,0.00006670803,0.980368,0.000008578522,0.0000886783,0.0002329043,0.00020771772,0.008242663,0.0054383655,0.00033514414,0.00014913111,0.0047787516],"study_design_scores_gemma":[0.000002880775,0.000026888687,0.97430336,0.0000020041089,0.000011588749,0.00009641587,0.00011618368,0.024843777,0.00029663107,0.00022843094,0.00006479299,0.0000069835164],"about_ca_topic_score_codex":0.0035848098,"about_ca_topic_score_gemma":0.003823432,"teacher_disagreement_score":0.0035848098,"about_ca_system_score_codex":0.0002791987,"about_ca_system_score_gemma":0.00009916596,"threshold_uncertainty_score":0.007127881},"labels":[],"label_agreement":null},{"id":"W1607830411","doi":"10.1023/a:1022994411319","title":"Tsunami Hazard and Risk in Canada","year":2003,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"W.F. Baird & Associates Coastal Engineers (Canada); Simon Fraser University; Geological Survey of Canada","funders":"","keywords":"Landslide; Natural hazard; Geology; Shore; Seismology; Harbour; Oceanography; Arctic; Hazard; The arctic; Geography","score_opus":0.006230292401940123,"score_gpt":0.19117839006881615,"score_spread":0.18494809766687603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607830411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9745558,0.0022322761,0.00018366844,0.0034631654,0.000044942324,0.000034311928,0.0060635014,0.000030503581,0.0133918235],"genre_scores_gemma":[0.98799753,0.0016526129,0.00014694495,0.00018071607,0.000011949804,0.000008901699,0.0012252392,0.0000134589045,0.008762631],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993642,0.000045692253,0.000035954225,0.000050640952,0.0001926003,0.0003108561],"domain_scores_gemma":[0.9962345,0.00031559935,0.00044658684,0.00006574742,0.001629893,0.0013077924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047485152,0.00026013906,0.00032820294,0.002394488,0.003716996,0.0021417923,0.0014312875,0.0006494518,0.0069186836],"category_scores_gemma":[0.0033386536,0.00039048697,0.0005529781,0.005523324,0.0008938573,0.0005313575,0.0012016624,0.0012174521,0.00029572612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050469354,0.00012914198,0.9455731,0.00009671936,0.00018443914,0.0006802722,0.0029099556,0.0044485694,0.0002275852,0.008111067,0.012692624,0.024441823],"study_design_scores_gemma":[0.00008324855,0.00006664719,0.9668209,0.00014257514,0.00010413843,0.00030307355,0.0082405275,0.006035678,0.00023250624,0.0018796052,0.01601275,0.00007839146],"about_ca_topic_score_codex":0.99932337,"about_ca_topic_score_gemma":0.9995889,"teacher_disagreement_score":0.08580091,"about_ca_system_score_codex":0.08580091,"about_ca_system_score_gemma":0.08904333,"threshold_uncertainty_score":0.62253207},"labels":[],"label_agreement":null},{"id":"W1607838611","doi":"10.1002/9781118670101.ch14","title":"Postglacial Induced Surface Motion, Gravity and Fault Instability in Laurentia: Evidence for Power Law Rheology In the Mantle?","year":2013,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Laurentia; Geology; Instability; Rheology; Mantle (geology); Power law; Geophysics; Physics; Mechanics; Paleontology; Paleozoic; Thermodynamics","score_opus":0.04007525117722903,"score_gpt":0.26753260552028135,"score_spread":0.2274573543430523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607838611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99853766,0.0001214852,0.000024021576,0.00008458168,0.0000017621206,8.040317e-7,0.000058681286,0.0000026473535,0.0011683776],"genre_scores_gemma":[0.9995721,0.000058918584,0.00002655884,0.000013599992,0.0000024764875,6.6193354e-7,0.00005442804,0.000001688486,0.00026959117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989736,0.0000106191455,0.0000069807097,0.00002818492,0.000008432196,0.00004827566],"domain_scores_gemma":[0.99968505,0.000049763617,0.00013489703,0.000036369875,0.000049269624,0.000044759312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026991885,0.00012304139,0.00020453715,0.0007640404,0.00052088284,0.00073353125,0.00045690048,0.00023456103,0.0015553338],"category_scores_gemma":[0.0012938565,0.000099823454,0.00013004955,0.0005579878,0.0006531865,0.00068171177,0.00053063396,0.00018199053,0.0002786764],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031734694,0.000055728244,0.95319396,0.000054968896,0.000082738254,0.0009623382,0.0038578461,0.0007661534,0.01489889,0.0018500511,0.00032880105,0.023631135],"study_design_scores_gemma":[0.0000039423903,0.000013037791,0.9980349,0.0000073026094,0.000007795317,0.00007126425,0.0006413831,0.00031438403,0.00022476756,0.00010168092,0.00057546695,0.0000040135847],"about_ca_topic_score_codex":0.24377432,"about_ca_topic_score_gemma":0.4563577,"teacher_disagreement_score":0.7562257,"about_ca_system_score_codex":0.0015535465,"about_ca_system_score_gemma":0.0009285862,"threshold_uncertainty_score":0.4847108},"labels":[],"label_agreement":null},{"id":"W1607987656","doi":"10.1029/2011gl046728","title":"Observation of the 2009 Samoa tsunami by the NEPTUNE-Canada cabled observatory: Test data for an operational regional tsunami forecast model","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Fisheries and Oceans Canada","funders":"","keywords":"Geology; Observatory; Tide gauge; Oceanography; Seismology; Neptune; Seafloor spreading; Meteorology; Climatology; Sea level; Geography","score_opus":0.22859173342666525,"score_gpt":0.2978615471840376,"score_spread":0.06926981375737237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607987656","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953851,0.000033191536,0.0012172716,0.00006948071,0.000010357174,0.000032190754,0.002272437,0.00014195169,0.000838],"genre_scores_gemma":[0.9945703,0.00003107033,0.0023041503,0.000009383335,0.000004620364,0.000014679089,0.0028476615,0.0000148087165,0.0002033095],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988425,0.000015062441,0.0000061330807,0.000035081095,0.000035468292,0.000023961265],"domain_scores_gemma":[0.9996213,0.000052193373,0.00003942965,0.000051565286,0.00015399558,0.00008149477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030894275,0.00043822854,0.00015442831,0.00026362008,0.00044966102,0.000471284,0.0008891014,0.00024486703,0.0006120481],"category_scores_gemma":[0.0009878083,0.00019386293,0.00022090378,0.00046182898,0.00031409282,0.00032250906,0.0003059807,0.00031658928,0.00012918156],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006726337,0.0002770858,0.4135109,0.000046798108,0.00013042564,0.00026267767,0.00026738047,0.54799753,0.007536453,0.0005884385,0.004310048,0.024399592],"study_design_scores_gemma":[0.0001307894,0.00009420793,0.13530731,0.000011226365,0.00004299543,0.000034267865,0.00014158114,0.8603284,0.0028202243,0.000099342025,0.0009572481,0.00003246292],"about_ca_topic_score_codex":0.7417264,"about_ca_topic_score_gemma":0.6452903,"teacher_disagreement_score":0.2582736,"about_ca_system_score_codex":0.0036291853,"about_ca_system_score_gemma":0.0029200383,"threshold_uncertainty_score":0.5195892},"labels":[],"label_agreement":null},{"id":"W1608109633","doi":"10.1002/ggge.20076","title":"Laboratory observation of acoustic fluidization in granular fault gouge and implications for dynamic weakening of earthquake faults","year":2013,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China; National Science Foundation","keywords":"Fault gouge; Geology; Fluidization; Split-Hopkinson pressure bar; Geotechnical engineering; Seismology; Slip (aerodynamics); Dynamic loading; Pore water pressure; Fault (geology); Dilatant; Seismic wave; Structural engineering; Materials science; Strain rate; Engineering","score_opus":0.009961362218993429,"score_gpt":0.21271348710644447,"score_spread":0.20275212488745104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1608109633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991273,0.000018418297,0.0007047391,0.0000089620935,0.0000020655891,0.000004399695,0.000020480189,0.000013573343,0.000100107085],"genre_scores_gemma":[0.99967384,0.000009044205,0.0002476886,0.0000029103692,9.891904e-7,0.0000035258684,0.000014632197,0.0000013239218,0.000046068846],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999186,0.0000129056625,0.0000057476773,0.000016530947,0.000026233814,0.000020040523],"domain_scores_gemma":[0.9997873,0.00006450052,0.000066169545,0.000024136656,0.000021902753,0.000036008438],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116769144,0.00012718982,0.0001067635,0.00015099643,0.0001739668,0.00024641864,0.00014651075,0.0001373676,0.0007979175],"category_scores_gemma":[0.0003222334,0.00009281592,0.000077605786,0.00008624086,0.00050074834,0.00014225555,0.00029320733,0.00021708859,0.00006584021],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009294932,0.00003639201,0.002193782,0.000013149065,0.0000036455317,0.00005230873,0.000029712408,0.00022376243,0.99653155,0.000046215988,0.000017198552,0.0007592998],"study_design_scores_gemma":[0.000029206765,0.0007876594,0.023348602,0.0000033398062,0.000008359416,0.00012332197,0.00012612215,0.0056605837,0.9695277,0.00008615799,0.00029063658,0.0000083302575],"about_ca_topic_score_codex":0.00037874695,"about_ca_topic_score_gemma":0.0002780914,"teacher_disagreement_score":0.0007979175,"about_ca_system_score_codex":0.00015094086,"about_ca_system_score_gemma":0.00005906626,"threshold_uncertainty_score":0.0026693344},"labels":[],"label_agreement":null},{"id":"W1612553446","doi":"10.1029/2007gl030822","title":"Automatic detection and characterization of seismic tremors in northern Cascadia","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Seismology; Waveform; Seismogram; Geology; Event (particle physics); Notice; Chart; Algorithm; Computer science; Telecommunications; Law; Statistics","score_opus":0.02141531044344082,"score_gpt":0.26229063598191094,"score_spread":0.24087532553847013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1612553446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5959849,0.00022743377,0.38233444,0.00022126178,0.000023684943,0.00013745723,0.0014269844,0.013927548,0.0057163406],"genre_scores_gemma":[0.8616818,0.0001050099,0.1324921,0.000030019351,0.000018744739,0.000072190356,0.002910566,0.0002113847,0.0024782126],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99963343,0.00003988328,0.00003106279,0.00014080065,0.00011320471,0.00004160932],"domain_scores_gemma":[0.99901235,0.00019270259,0.0001654626,0.00012831559,0.0004173446,0.00008391692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041924906,0.0005755062,0.00040086076,0.0027970728,0.000399404,0.00072784885,0.0006132252,0.0003200907,0.0012024111],"category_scores_gemma":[0.0018889684,0.00021681677,0.00019359803,0.0009526777,0.0003107355,0.0003764821,0.0005134441,0.00024211487,0.00052602735],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038399076,0.000114586,0.11523961,0.00016617082,0.000078197736,0.00034542626,0.00047405876,0.048227835,0.08112244,0.0012941922,0.0058642915,0.74668926],"study_design_scores_gemma":[0.000093573166,0.00016608107,0.2599201,0.000020915388,0.00006682872,0.00044019928,0.0003335344,0.6807354,0.04812407,0.0023155243,0.0077072447,0.00007650698],"about_ca_topic_score_codex":0.018288102,"about_ca_topic_score_gemma":0.024344053,"teacher_disagreement_score":0.018288102,"about_ca_system_score_codex":0.0005383352,"about_ca_system_score_gemma":0.0009792281,"threshold_uncertainty_score":0.036363304},"labels":[],"label_agreement":null},{"id":"W1616547970","doi":"10.1029/2005gl023157","title":"Are some domes the ghosts of basins?","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Structural basin; Sedimentary basin; Crust; Back-stripping; Tectonic subsidence; Inversion (geology); Seismology; Sedimentary rock; Petrology; Extensional definition; Subsidence; Pull apart basin; Tectonics; Geomorphology; Geophysics; Sedimentary basin analysis; Paleontology","score_opus":0.04742984873729317,"score_gpt":0.300427536602767,"score_spread":0.25299768786547383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1616547970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87460756,0.003878298,0.015064141,0.014828238,0.00028500217,0.000054574597,0.000758606,0.0002720223,0.09025155],"genre_scores_gemma":[0.989833,0.000442087,0.0026960862,0.00067732844,0.00004851664,0.000010881138,0.000095434705,0.000042039053,0.0061547863],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99969363,0.000092287395,0.00001436494,0.0000761049,0.000042565403,0.00008101502],"domain_scores_gemma":[0.9992059,0.00012046286,0.00011994562,0.00029822293,0.000104456325,0.00015108217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005041956,0.00014321835,0.00029895292,0.0005152293,0.0016099524,0.0023068748,0.0003218241,0.0006979396,0.005284842],"category_scores_gemma":[0.0023077684,0.00028237147,0.00018822248,0.0005940167,0.0042547267,0.0036171768,0.0015249882,0.00049166894,0.0007514549],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059334026,0.000042179763,0.18747413,0.0003068441,0.00013749492,0.0022809952,0.03043667,0.0012886893,0.009900994,0.5917014,0.02081687,0.15502037],"study_design_scores_gemma":[0.000072607196,0.00009329459,0.23099898,0.0002240323,0.00008845152,0.0055211317,0.03641065,0.0027175716,0.0042917947,0.29692447,0.42256725,0.00008981333],"about_ca_topic_score_codex":0.0026737358,"about_ca_topic_score_gemma":0.006650468,"teacher_disagreement_score":0.005284842,"about_ca_system_score_codex":0.00049624685,"about_ca_system_score_gemma":0.00050592533,"threshold_uncertainty_score":0.017679572},"labels":[],"label_agreement":null},{"id":"W1616577258","doi":"10.1029/2006tc002090","title":"Tectonic evolution of the active Hikurangi subduction margin, New Zealand, since the Oligocene","year":2007,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":256,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Alberta Energy","funders":"","keywords":"Geology; Subduction; Pacific Plate; Episodic tremor and slip; Seismology; Paleomagnetism; Clockwise; Terrane; Thrust fault; Plate tectonics; Fault (geology); Tectonics; Paleontology; Rotation (mathematics); Geometry","score_opus":0.010838976557378047,"score_gpt":0.20923021215345275,"score_spread":0.1983912355960747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1616577258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960439,0.00059487694,0.00010349811,0.000069345,0.0000061461083,0.000013951273,0.00032099066,0.000008709593,0.0028385404],"genre_scores_gemma":[0.99751425,0.00062788406,0.00032054182,0.000019733618,0.0000048174907,0.000011506302,0.00029412916,0.000005451846,0.001201593],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998591,0.0000049665477,0.000015381502,0.00005671232,0.00003823098,0.000025519546],"domain_scores_gemma":[0.9996238,0.000012123433,0.000142002,0.000013908866,0.00013543323,0.00007258247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028241696,0.00036218364,0.00023719613,0.0011134169,0.00063671404,0.00081000786,0.0003309194,0.0002276056,0.001269356],"category_scores_gemma":[0.0008695414,0.00029514503,0.00021684695,0.0013536658,0.0009211141,0.0005600794,0.0007238163,0.00033495008,0.00021697723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026699287,0.000044168308,0.9072773,0.0003399787,0.0001892815,0.0011154391,0.004547466,0.0017807587,0.0430385,0.0005758324,0.00049132935,0.040333014],"study_design_scores_gemma":[0.000003424593,0.000013806388,0.99816495,0.000010323962,0.000013208605,0.00009528997,0.00020664967,0.00014341244,0.00014919919,0.000015978298,0.0011794863,0.000004230953],"about_ca_topic_score_codex":0.44565874,"about_ca_topic_score_gemma":0.54123765,"teacher_disagreement_score":0.44565874,"about_ca_system_score_codex":0.0033955937,"about_ca_system_score_gemma":0.001572421,"threshold_uncertainty_score":0.88612944},"labels":[],"label_agreement":null},{"id":"W1621319362","doi":"10.1007/978-3-7643-8364-0","title":"Tsunami and Its Hazards in the Indian and Pacific Oceans","year":2007,"lang":"en","type":"book","venue":"Birkhäuser Basel eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Environmental science; Geology; Geography; Climatology","score_opus":0.018027897429363293,"score_gpt":0.2123647785098683,"score_spread":0.194336881080505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1621319362","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008456793,0.72843015,0.0012413313,0.025991559,0.048198324,0.00015500985,0.0029677274,0.00016659021,0.18439253],"genre_scores_gemma":[0.06112215,0.7174854,0.0009360772,0.004127758,0.06476528,0.0001321307,0.004814695,0.00008360938,0.14653283],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998623,0.000026198486,0.000018622386,0.00001727713,0.000049781844,0.000025718873],"domain_scores_gemma":[0.99925023,0.00015617853,0.00006381388,0.0000198679,0.0003857877,0.00012407081],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035902916,0.0007392559,0.0003634745,0.0026025192,0.0007560199,0.002007862,0.00042694897,0.00068820553,0.021780314],"category_scores_gemma":[0.0008431146,0.00018260394,0.00028333932,0.0041744285,0.0004229586,0.0012880542,0.0007341229,0.0013169692,0.0040077134],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006812712,0.00008574116,0.012533664,0.00090090337,0.00002696653,0.00034705107,0.00054726173,0.0007777628,0.0005779616,0.005333926,0.75811213,0.22068848],"study_design_scores_gemma":[0.000004391498,0.000076368706,0.04558331,0.0010242558,0.000026655462,0.00027539773,0.0013518481,0.00020256903,0.00006781733,0.0023904343,0.94898134,0.000015555617],"about_ca_topic_score_codex":0.025403017,"about_ca_topic_score_gemma":0.033678353,"teacher_disagreement_score":0.025403017,"about_ca_system_score_codex":0.0007445939,"about_ca_system_score_gemma":0.0014015584,"threshold_uncertainty_score":0.07286239},"labels":[],"label_agreement":null},{"id":"W1623696198","doi":"10.1029/2011tc003068","title":"Kinematics of Tertiary to Quaternary intracontinental deformation of upper crust in the Eastern Cordillera, southern Central Andes, NW Argentina","year":2012,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Seismology; Crust; Kinematics; Doming; Fault (geology); Slip (aerodynamics); Paleontology; Tectonics","score_opus":0.016338637134192622,"score_gpt":0.22439779595299564,"score_spread":0.20805915881880302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1623696198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973726,0.00034999114,0.00008663727,0.000028677983,0.000003590073,0.000011290651,0.00035972137,0.000017225746,0.0017702242],"genre_scores_gemma":[0.99818003,0.000313968,0.00026543296,0.000005905591,0.0000037764034,0.000009056668,0.0004923232,0.000004129035,0.0007254302],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989295,0.000008266425,0.0000090227695,0.000038012175,0.000024191313,0.00002754884],"domain_scores_gemma":[0.9998716,0.00000986179,0.00004933746,0.000008769301,0.000040412404,0.000019992242],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016345832,0.00035802444,0.00019648254,0.0010837028,0.00037328675,0.0005843209,0.00025748054,0.00022149875,0.0011141782],"category_scores_gemma":[0.00034999353,0.00015788637,0.0001641961,0.0010163195,0.00023898562,0.00019906407,0.00033782882,0.00011790256,0.00018496138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024078028,0.00003819803,0.9512585,0.00009126219,0.000060555685,0.00041567744,0.0006431268,0.0022936072,0.014899163,0.00019872226,0.0003642177,0.02949615],"study_design_scores_gemma":[0.0000028821771,0.000008877105,0.9987717,0.00000715305,0.0000065124414,0.0000334075,0.000088593995,0.00057810824,0.0001691434,0.000014563108,0.00031701807,0.0000018455754],"about_ca_topic_score_codex":0.15851878,"about_ca_topic_score_gemma":0.24003866,"teacher_disagreement_score":0.15851878,"about_ca_system_score_codex":0.0010708511,"about_ca_system_score_gemma":0.00053626153,"threshold_uncertainty_score":0.31519222},"labels":[],"label_agreement":null},{"id":"W1630947333","doi":"10.1029/2011jb008624","title":"Stick, slip, and opening of wavy frictional faults: A numerical approach in two dimensions","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Basic Energy Sciences; Southern California Earthquake Center; McGill University; U.S. Geological Survey; U.S. Department of Energy","keywords":"Slip (aerodynamics); Amplitude; Wavelength; Geometry; Isotropy; Planar; Discontinuity (linguistics); Boundary value problem; Fault trace; Anisotropy; Geology; Mathematical analysis; Mechanics; Physics; Fault (geology); Mathematics; Optics; Computer science; Seismology","score_opus":0.04945430176759765,"score_gpt":0.32927523802268877,"score_spread":0.27982093625509113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1630947333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.59300804,0.00058184855,0.39274004,0.00043132616,0.00011436698,0.00009916297,0.00015888856,0.0003283271,0.012538045],"genre_scores_gemma":[0.9134623,0.00020476089,0.083875015,0.00006161772,0.000021167038,0.00010356667,0.00005977596,0.000054223234,0.0021577359],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998914,0.000025667649,0.0000076629485,0.000016719265,0.000037562204,0.00002098726],"domain_scores_gemma":[0.9994455,0.00030383974,0.00009714126,0.000051386374,0.00006723281,0.000034986195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033237605,0.0003468106,0.00042525618,0.00083669083,0.00061105686,0.0011022887,0.000721049,0.0010510529,0.0012526041],"category_scores_gemma":[0.0016045085,0.00048271468,0.0003848965,0.0005260559,0.0010845585,0.0005815679,0.0006783072,0.0005814318,0.00010330781],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041133957,0.000056430803,0.0025747651,0.00007799647,0.000020319369,0.0001242722,0.00015830908,0.9607081,0.010689824,0.01816705,0.00022339492,0.007158393],"study_design_scores_gemma":[0.0000066312004,0.0000051500083,0.00014843825,0.0000034640934,0.0000012997377,0.000010085957,0.000011321264,0.9982749,0.00038307326,0.0009976719,0.00015450583,0.0000033917247],"about_ca_topic_score_codex":0.0057205204,"about_ca_topic_score_gemma":0.0036378945,"teacher_disagreement_score":0.0057205204,"about_ca_system_score_codex":0.0009840393,"about_ca_system_score_gemma":0.0008229402,"threshold_uncertainty_score":0.011374474},"labels":[],"label_agreement":null},{"id":"W1635390369","doi":"","title":"Cenozoic Evolution of the West Cycladic Detachment System","year":2010,"lang":"en","type":"article","venue":"EGU General Assembly Conference Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Boulevard; Sedimentology; Geology; Structural geology; Cenozoic; Archaeology; Geography; Paleontology","score_opus":0.013114675378796096,"score_gpt":0.21105134779086562,"score_spread":0.19793667241206953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1635390369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98114955,0.000755895,0.00018465964,0.00029237903,0.000010786176,0.000010997907,0.00029147198,0.000014438124,0.017289842],"genre_scores_gemma":[0.99728084,0.0003439667,0.00012440272,0.000019850655,0.0000046985556,0.000003824991,0.00018296954,0.00000777127,0.002031581],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998586,0.000025130286,0.0000090211,0.000044417473,0.00002074045,0.00004206433],"domain_scores_gemma":[0.9998129,0.000012292717,0.00006226086,0.000014638643,0.00006436189,0.000033614448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027479927,0.0002238091,0.00014167927,0.0014335336,0.0009516983,0.0014227594,0.00021728115,0.00026824436,0.009484736],"category_scores_gemma":[0.00082396343,0.00023044783,0.000056640998,0.0015222222,0.0011787416,0.00056156033,0.00090065994,0.00033449059,0.00080099446],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008172298,0.000120347395,0.6943699,0.00043203778,0.00015888023,0.0008773484,0.03572217,0.0043108934,0.023659684,0.059545696,0.006258277,0.17372744],"study_design_scores_gemma":[0.000012186771,0.000044818033,0.9727163,0.000060981063,0.0000170521,0.0002144148,0.0031818773,0.0004945156,0.0003603185,0.00072483724,0.022164363,0.000008298253],"about_ca_topic_score_codex":0.06677348,"about_ca_topic_score_gemma":0.16935964,"teacher_disagreement_score":0.06677348,"about_ca_system_score_codex":0.0020052695,"about_ca_system_score_gemma":0.00089524407,"threshold_uncertainty_score":0.13276964},"labels":[],"label_agreement":null},{"id":"W1637942467","doi":"10.1002/jgrb.50194","title":"The role of viscous magma mush spreading in volcanic flank motion at Kīlauea Volcano, Hawai‘i","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; University of the Pacific; University of Hawai'i; U.S. Geological Survey; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Volcano; Magma; Flank; Dike; Seismology; Rift zone; Magma chamber; Geodesy; Interferometric synthetic aperture radar; Tectonics; Rift; Petrology; Synthetic aperture radar","score_opus":0.020674281772382862,"score_gpt":0.28080833577406217,"score_spread":0.2601340540016793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1637942467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972554,0.00009403092,0.0010980609,0.00009773157,0.0000067361957,0.0000063011457,0.00005457841,0.00002574313,0.001361348],"genre_scores_gemma":[0.9996897,0.000024936027,0.0001327845,0.0000056002004,0.0000021081378,0.0000020515367,0.000015684058,0.0000027689657,0.00012429857],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99997354,0.0000048307866,0.00000195241,0.000007583705,0.0000041994945,0.000007978715],"domain_scores_gemma":[0.9999006,0.000030497013,0.000023141658,0.000006953583,0.000013399472,0.000025440535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011187188,0.00043606246,0.00023777988,0.00032399013,0.00040460375,0.000658511,0.00053669827,0.0005826567,0.0011926038],"category_scores_gemma":[0.00037947338,0.00029538656,0.00045903344,0.0001677047,0.00052827015,0.000537186,0.00028457656,0.0002549449,0.00012599683],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018568277,0.00014551893,0.22359775,0.000104328494,0.00016346021,0.0011945168,0.000428325,0.71623087,0.048000216,0.0022476779,0.00044982848,0.0072518196],"study_design_scores_gemma":[0.000038508475,0.000074886004,0.09260074,0.000015588832,0.00004122599,0.00007608102,0.00016216384,0.904546,0.0016383288,0.0005006176,0.00027644832,0.000029358462],"about_ca_topic_score_codex":0.046459213,"about_ca_topic_score_gemma":0.022183416,"teacher_disagreement_score":0.046459213,"about_ca_system_score_codex":0.0011605778,"about_ca_system_score_gemma":0.00046006395,"threshold_uncertainty_score":0.09237754},"labels":[],"label_agreement":null},{"id":"W164005984","doi":"10.4401/ag-3452","title":"Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems","year":2003,"lang":"en","type":"article","venue":"Annals of Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Geology; Subduction; Seismology; Holocene; San andreas fault; Fault (geology); Tectonics; Paleontology","score_opus":0.024100628861997604,"score_gpt":0.23098212150927433,"score_spread":0.20688149264727673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W164005984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99683243,0.00026349883,0.00011220573,0.00009471883,0.0000042982338,0.0000027424587,0.00057469413,0.000017955792,0.0020975117],"genre_scores_gemma":[0.9987551,0.00014073422,0.00012703103,0.000009889021,0.000006992679,0.0000030261256,0.000640607,0.0000054819784,0.0003110645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982196,0.00003340454,0.000020576977,0.000053534364,0.000035587647,0.000034864788],"domain_scores_gemma":[0.9987895,0.00019465512,0.00042616227,0.00008844345,0.00014258288,0.00035863245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004948218,0.00037975147,0.00024090019,0.0019747221,0.00037163583,0.0011648601,0.00026423432,0.00026481744,0.0018013658],"category_scores_gemma":[0.0017781919,0.00018922007,0.00020633018,0.0022074664,0.00048845203,0.00055276835,0.0008007792,0.0003171899,0.00026819785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024029383,0.000009435464,0.99572265,0.000017153498,0.0000453818,0.000049641683,0.000564874,0.00027233237,0.00080792705,0.00008789097,0.00016060394,0.0022380447],"study_design_scores_gemma":[0.0000010553316,0.0000050091066,0.9990834,0.000004294195,0.0000063846596,0.000011163114,0.00028200907,0.00026752896,0.00003573713,0.000036828846,0.0002644308,0.000002141961],"about_ca_topic_score_codex":0.06355577,"about_ca_topic_score_gemma":0.1919493,"teacher_disagreement_score":0.06355577,"about_ca_system_score_codex":0.0008002208,"about_ca_system_score_gemma":0.0004949357,"threshold_uncertainty_score":0.12637168},"labels":[],"label_agreement":null},{"id":"W1643601001","doi":"","title":"Cascadia Great Earthquake Recurrence: Rupture lengths, Correlations and Constrained OxCal Analysis of Event Ages","year":2005,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Event (particle physics); Radiocarbon dating; Series (stratigraphy); Sedimentary depositional environment; Bayesian probability; Margin (machine learning); Subduction; Paleontology; Statistics; Tectonics","score_opus":0.01446649121510154,"score_gpt":0.23845411989182516,"score_spread":0.22398762867672362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1643601001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948966,0.000037984246,0.002811538,0.00003705925,0.000002277464,0.000010383691,0.0008982686,0.00005400349,0.0012518758],"genre_scores_gemma":[0.99538064,0.000017523224,0.0024512326,0.000011516168,0.0000044263666,0.000018201868,0.0016271919,0.000027839764,0.00046152115],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99920887,0.00030398573,0.00008102936,0.00018580964,0.00016466783,0.000055785593],"domain_scores_gemma":[0.992431,0.003238219,0.0016849801,0.0010199861,0.0013373543,0.00028861407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026303588,0.00027889246,0.0002408924,0.0018993482,0.00036985977,0.0007143779,0.00051934645,0.00019109756,0.0024691748],"category_scores_gemma":[0.0104068015,0.00015219126,0.00028293574,0.0017829523,0.00036598512,0.00058047526,0.00054854905,0.00030167177,0.00022543762],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000103399005,0.000017706396,0.9778967,0.000020448893,0.0001215301,0.00005969273,0.00020678804,0.01158637,0.0006307329,0.00043577136,0.00033785647,0.008583081],"study_design_scores_gemma":[0.000017607807,0.000052987776,0.9169135,0.000011915538,0.0000369382,0.000043988275,0.00023851405,0.0807069,0.00059715775,0.00051144464,0.0008524785,0.000016612443],"about_ca_topic_score_codex":0.0432738,"about_ca_topic_score_gemma":0.0729009,"teacher_disagreement_score":0.0432738,"about_ca_system_score_codex":0.0009703818,"about_ca_system_score_gemma":0.0007796301,"threshold_uncertainty_score":0.086043835},"labels":[],"label_agreement":null},{"id":"W1645451816","doi":"10.3319/tao.2006.17.3.503(t)","title":"From Tornadoes to Earthquakes: Forecast Verification for Binary Events Applied to the 1999 Chi-Chi, Taiwan,Earthquake","year":2006,"lang":"en","type":"article","venue":"Terrestrial Atmospheric and Oceanic Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"U.S. Geological Survey; National Science Council; Japan Society for the Promotion of Science; Southern California Earthquake Center; National Aeronautics and Space Administration; University of California, Davis; U.S. Department of Energy; National Science Foundation","keywords":"Tornado; Seismology; Earthquake prediction; Geology; Meteorology; Geography","score_opus":0.019710335066824267,"score_gpt":0.22760382831922596,"score_spread":0.2078934932524017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1645451816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9774061,0.00006463814,0.021259835,0.000090557136,0.000016199809,0.000033843506,0.0004608064,0.00019713322,0.00047091558],"genre_scores_gemma":[0.9936686,0.00001608894,0.005955936,0.000005410909,0.000006060052,0.000009958195,0.00027439022,0.000005370025,0.000058156114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982326,0.00089804595,0.0001927076,0.00024845585,0.00033981435,0.000088306755],"domain_scores_gemma":[0.9573689,0.034193162,0.0034887923,0.0020136898,0.002482431,0.00045309795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0071092406,0.00026661257,0.00029771682,0.00096321094,0.0002424854,0.0005347492,0.00038397624,0.00037553077,0.00092188944],"category_scores_gemma":[0.05114708,0.00013390076,0.00027836967,0.00064475514,0.00032752092,0.00063849153,0.00058810774,0.00044996373,0.000159992],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028024595,0.00021116876,0.6552219,0.00013306034,0.0002672299,0.0005055984,0.0006073149,0.13444485,0.0064715324,0.0020696702,0.0016080777,0.19565709],"study_design_scores_gemma":[0.00009267759,0.00051567034,0.17588292,0.000014820424,0.000062031315,0.00018362995,0.0002578931,0.8122664,0.008375234,0.0018324954,0.00046755225,0.00004871578],"about_ca_topic_score_codex":0.00849038,"about_ca_topic_score_gemma":0.0071509066,"teacher_disagreement_score":0.00849038,"about_ca_system_score_codex":0.00044872158,"about_ca_system_score_gemma":0.00087936944,"threshold_uncertainty_score":0.037597716},"labels":[],"label_agreement":null},{"id":"W1647067242","doi":"10.1029/2005gl024446","title":"Scaling of fracture energies: The rationalization of different laboratory measurements","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Wilson Centre; University of Toronto","funders":"","keywords":"Scaling; Geology; Seismology; Fracture (geology); Scaling law; Geophysics; Geotechnical engineering; Geometry; Mathematics","score_opus":0.03960597596709549,"score_gpt":0.2778945243546335,"score_spread":0.23828854838753805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1647067242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8780354,0.001946002,0.108735554,0.00056114857,0.00012182014,0.00011554485,0.00048662367,0.0004960779,0.00950185],"genre_scores_gemma":[0.9926924,0.00025816928,0.006561452,0.00008029243,0.000024700192,0.0000758295,0.00012309387,0.000023505763,0.00016047472],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993656,0.00015200867,0.00003682889,0.00023767307,0.00015199228,0.000055865905],"domain_scores_gemma":[0.99757737,0.0010917286,0.00036297957,0.00066519383,0.00021902549,0.00008371379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014687987,0.0005428536,0.00032293674,0.0008042602,0.00032781236,0.00071919226,0.0010324912,0.0008343795,0.0010631026],"category_scores_gemma":[0.005188765,0.0003413593,0.0003457247,0.00039412113,0.0018544613,0.0011821802,0.0008322495,0.0010244303,0.00021426885],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008993698,0.0008213566,0.06274951,0.00038914703,0.00018883501,0.0009631834,0.000478231,0.030876178,0.7989986,0.053853143,0.0021219845,0.04766048],"study_design_scores_gemma":[0.0001137107,0.0015309008,0.13905333,0.0000751389,0.00011581021,0.0011901202,0.00042180732,0.20632504,0.59736645,0.04842282,0.005165517,0.00021937361],"about_ca_topic_score_codex":0.00039598945,"about_ca_topic_score_gemma":0.00023665513,"teacher_disagreement_score":0.0014687987,"about_ca_system_score_codex":0.0005147284,"about_ca_system_score_gemma":0.00012902016,"threshold_uncertainty_score":0.0077677965},"labels":[],"label_agreement":null},{"id":"W1653918777","doi":"10.1029/2010gc003462","title":"Evolution of seismic layer 2B across the Juan de Fuca Ridge from hydrophone streamer 2‐D traveltime tomography","year":2011,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Ridge; Seismology; Magma chamber; Mid-ocean ridge; Seafloor spreading; Seismic tomography; Subduction; Geophysics; Crust; Oceanic crust; Lithosphere; Magma; Tectonics; Volcano; Paleontology; Mantle (geology)","score_opus":0.014516514894039347,"score_gpt":0.20013775562216685,"score_spread":0.1856212407281275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1653918777","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99499476,0.000065708766,0.0019402369,0.000085144384,0.000008916415,0.000009990132,0.0012454911,0.00020910101,0.0014406363],"genre_scores_gemma":[0.9961104,0.000058087466,0.0020766333,0.000010944058,0.000005072331,0.000007433536,0.0013101352,0.000030974632,0.0003902937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.0000061180463,0.000002885752,0.000020456111,0.000014716122,0.000017855838],"domain_scores_gemma":[0.9998672,0.000017046705,0.000032142838,0.000017422839,0.000035689965,0.000030478317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017434773,0.00053400657,0.000198133,0.00080580555,0.00023050408,0.00063161534,0.00030015784,0.00044832757,0.0015390876],"category_scores_gemma":[0.00055121706,0.00037019828,0.00046593335,0.00067479507,0.00021181951,0.00025614706,0.0003864703,0.00027546787,0.00022061204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000589274,0.00022748834,0.48109785,0.00014564572,0.00035519505,0.00088604545,0.0009221199,0.36903235,0.101857275,0.0014333486,0.002494213,0.040959198],"study_design_scores_gemma":[0.0000577355,0.000060150436,0.5235849,0.000030903822,0.00006886043,0.0001886837,0.00021241556,0.46980038,0.004211735,0.0003477184,0.001366534,0.00006989487],"about_ca_topic_score_codex":0.047077447,"about_ca_topic_score_gemma":0.048062015,"teacher_disagreement_score":0.047077447,"about_ca_system_score_codex":0.0007054405,"about_ca_system_score_gemma":0.00081955164,"threshold_uncertainty_score":0.09360683},"labels":[],"label_agreement":null},{"id":"W1660805619","doi":"10.1029/2011gl048270","title":"Forearc extension and slow rollback of the Calabrian Arc from GPS measurements","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Subduction; Forearc; Seismology; Reference frame; Geodesy; Foreland basin; Trench; Arc (geometry); Wedge (geometry); Global Positioning System; Tectonics; Geometry; Frame (networking)","score_opus":0.11975863308516788,"score_gpt":0.27659058052849655,"score_spread":0.15683194744332868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1660805619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97451615,0.0015379034,0.0044248067,0.00013467224,0.000031496467,0.000044773406,0.0071193227,0.00022332904,0.011967551],"genre_scores_gemma":[0.98889685,0.0004389573,0.0037780772,0.00001810496,0.000020142068,0.000016198612,0.0060075363,0.000020026951,0.0008042534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998227,0.000022109198,0.000010874234,0.000067311186,0.00005287141,0.000024125015],"domain_scores_gemma":[0.99967265,0.000041131665,0.00009508397,0.000045842866,0.00012156044,0.000023745886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025675955,0.0003416792,0.00014498246,0.0016406267,0.00021902399,0.0005925388,0.0003007904,0.00019038282,0.0018254165],"category_scores_gemma":[0.0014935012,0.0001306829,0.00011136834,0.001925223,0.0001636467,0.00018648253,0.00040167055,0.00028641985,0.00041113005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012965906,0.000015690655,0.87437385,0.000084063795,0.000051990723,0.000113220034,0.0007081036,0.0040052924,0.005651657,0.00028181286,0.0019871313,0.11259753],"study_design_scores_gemma":[0.00000575352,0.000013640346,0.9953151,0.0000147086985,0.00000967535,0.000035780897,0.00009688504,0.001200275,0.00022092453,0.000053904696,0.0030297185,0.0000036186188],"about_ca_topic_score_codex":0.14188479,"about_ca_topic_score_gemma":0.23149994,"teacher_disagreement_score":0.14188479,"about_ca_system_score_codex":0.0006512291,"about_ca_system_score_gemma":0.0003347107,"threshold_uncertainty_score":0.2821179},"labels":[],"label_agreement":null},{"id":"W1672760660","doi":"","title":"Revised Iranian earthquake catalog for moderate and strong earthquakes","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Seismology; Geology","score_opus":0.05533461907529172,"score_gpt":0.3140300546531785,"score_spread":0.25869543557788677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1672760660","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.114065655,0.009955366,0.011614325,0.004698964,0.00538742,0.0022561403,0.7463845,0.003525541,0.10211217],"genre_scores_gemma":[0.123498015,0.0051879114,0.020683067,0.0005654926,0.0013414691,0.0012478309,0.79434687,0.00044278384,0.052686583],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9991573,0.00006377114,0.00022202983,0.00009268494,0.00026295226,0.00020118593],"domain_scores_gemma":[0.99468994,0.00012360969,0.00043845683,0.0006341398,0.0039085196,0.00020530411],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017928974,0.001237579,0.000657377,0.011829598,0.0010292243,0.0009184022,0.0013057614,0.00042671504,0.015568731],"category_scores_gemma":[0.0039342167,0.00041601653,0.0004970045,0.008331976,0.00031570287,0.0013509548,0.0012102021,0.00062248466,0.01256986],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036951716,0.00007536974,0.06045449,0.00063081883,0.00007458279,0.00042497594,0.0006508888,0.00066643034,0.0016241375,0.002240751,0.75023097,0.18255694],"study_design_scores_gemma":[0.000054995147,0.000058461195,0.2536245,0.00013998082,0.0000838284,0.0005470387,0.00050537597,0.00024847963,0.00077126874,0.000522107,0.74341565,0.000028283737],"about_ca_topic_score_codex":0.089918256,"about_ca_topic_score_gemma":0.08699851,"teacher_disagreement_score":0.089918256,"about_ca_system_score_codex":0.0012914686,"about_ca_system_score_gemma":0.0076475777,"threshold_uncertainty_score":0.17878973},"labels":[],"label_agreement":null},{"id":"W1674104847","doi":"10.1029/2010gl044927","title":"Estimating seismic moment magnitude (<i>M</i><sub><i>w</i></sub>) of tremor bursts in northern Cascadia: Implications for the “seismic efficiency” of episodic tremor and slip","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; University of Toronto; Geological Survey of Canada","funders":"U.S. Geological Survey","keywords":"Seismogram; Seismology; Geology; Amplitude; Slip (aerodynamics); Magnitude (astronomy); Seismic moment; Moment magnitude scale; Episodic tremor and slip; Consistency (knowledge bases); Seismic wave; Geodesy; Subduction; Physics; Tectonics; Mathematics; Geometry","score_opus":0.024850585016031282,"score_gpt":0.2801703168840403,"score_spread":0.25531973186800905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1674104847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98455334,0.000080929225,0.013983584,0.000053336655,0.000002775041,0.000010137386,0.00024036347,0.0001509787,0.0009245084],"genre_scores_gemma":[0.9939744,0.000060333707,0.0055308966,0.0000032276803,0.0000049919163,0.000009032591,0.00022006733,0.000010554631,0.00018651543],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.000017614446,0.000007926184,0.000034709472,0.000026678339,0.000010697904],"domain_scores_gemma":[0.9993692,0.00015707624,0.00023560403,0.00007223174,0.000096030955,0.00006987987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030439644,0.00045711632,0.00015451682,0.0012292584,0.00018688357,0.00023883756,0.00033519542,0.00021333153,0.00042266538],"category_scores_gemma":[0.0018942353,0.0002539718,0.00014061252,0.0005921729,0.0002391577,0.00025445997,0.00033495683,0.00018684562,0.00015967271],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018456277,0.000043538854,0.8244593,0.00009286756,0.00010810348,0.0001616767,0.00053302635,0.030342456,0.04197702,0.00024129766,0.00029526578,0.10156098],"study_design_scores_gemma":[0.00001638699,0.000092207476,0.92471945,0.000009799109,0.000043049396,0.00013118892,0.0001929123,0.06559404,0.008250784,0.0003138391,0.00060372666,0.000032619275],"about_ca_topic_score_codex":0.012358866,"about_ca_topic_score_gemma":0.023761278,"teacher_disagreement_score":0.012358866,"about_ca_system_score_codex":0.00045235208,"about_ca_system_score_gemma":0.0003622786,"threshold_uncertainty_score":0.024573863},"labels":[],"label_agreement":null},{"id":"W167462748","doi":"10.5065/9bjj-7t73","title":"The effects of the 8.2 ka event on the ITCZ in the tropical Atlantic","year":2021,"lang":"en","type":"article","venue":"Open MIND","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intertropical Convergence Zone; Tropical Atlantic; Climatology; Environmental science; Tropics; Geology; Meteorology; Geography; Sea surface temperature; Precipitation; Biology; Fishery","score_opus":0.021585277518081092,"score_gpt":0.24699574295626534,"score_spread":0.22541046543818424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W167462748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977131,0.000052265277,0.00004078055,0.0001245673,0.000019128265,0.0000056802523,0.00050470384,0.000011724329,0.0015280395],"genre_scores_gemma":[0.9993981,0.00004187892,0.000035428304,0.000031649575,0.000008842786,0.0000044490494,0.00032813402,0.000004619816,0.00014685014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998342,0.000025692361,0.000013679143,0.000040441504,0.000027311478,0.00005860369],"domain_scores_gemma":[0.9995703,0.000065748805,0.00009111141,0.000026849726,0.000114694325,0.00013117379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027792735,0.00029293908,0.00022955202,0.00031508677,0.0004678852,0.00092970417,0.00034763815,0.00050176797,0.0019701743],"category_scores_gemma":[0.0011730482,0.00015417449,0.00047560944,0.00044800137,0.0003090232,0.00045450046,0.00058066065,0.0005811154,0.00014648338],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00095500884,0.0002700228,0.93221164,0.00011152982,0.00036412862,0.0014669459,0.000585672,0.038414754,0.013712733,0.001079145,0.0028763963,0.007952053],"study_design_scores_gemma":[0.000038263042,0.000051950607,0.9840845,0.00001574269,0.00007769395,0.000047506266,0.00036763304,0.013737812,0.00048757513,0.00006122183,0.0010174342,0.000012610604],"about_ca_topic_score_codex":0.14487733,"about_ca_topic_score_gemma":0.14674969,"teacher_disagreement_score":0.14487733,"about_ca_system_score_codex":0.0014992637,"about_ca_system_score_gemma":0.000983589,"threshold_uncertainty_score":0.28806806},"labels":[],"label_agreement":null},{"id":"W1677874448","doi":"10.1029/2001jb001744","title":"Irregular recurrence of paleoearthquakes along the central Garlock fault near El Paso Peaks, California","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Bureau of Land Management; McGill University; National Science Foundation","keywords":"Geology; Radiocarbon dating; Seismology; Event (particle physics); Fault scarp; Fault (geology); Paleontology; Physics","score_opus":0.02929874469164742,"score_gpt":0.2862526400180487,"score_spread":0.2569538953264012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1677874448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981818,0.00013543613,0.000044866752,0.000045181016,0.000004551664,0.0000039173824,0.00019260208,0.0000116203655,0.0013800527],"genre_scores_gemma":[0.99917185,0.0001295122,0.00008527488,0.000013007163,0.0000062603026,0.000003501211,0.00025088454,0.0000023216307,0.0003374416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988425,0.000007369951,0.000008609446,0.00004691603,0.000029437411,0.000023454424],"domain_scores_gemma":[0.9995228,0.00006551367,0.00015346013,0.000036946414,0.0001314705,0.000089845795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022740757,0.000117894466,0.00014834951,0.00083650154,0.00063419674,0.0005871251,0.00024780302,0.00024354194,0.0006635421],"category_scores_gemma":[0.00074640795,0.000111072004,0.00005255686,0.00058055937,0.00043048302,0.00025930555,0.00045093757,0.00020051107,0.00006586948],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012482495,0.00005998982,0.97432464,0.00005562981,0.000047021167,0.000548269,0.0021241673,0.0005834462,0.002939095,0.00014642072,0.0015309013,0.017515542],"study_design_scores_gemma":[0.0000037957534,0.000012127278,0.99835616,0.000009773645,0.0000069154457,0.00005159446,0.00039752855,0.00015833063,0.000097665485,0.000023566605,0.00087983365,0.0000025978864],"about_ca_topic_score_codex":0.07572115,"about_ca_topic_score_gemma":0.25979623,"teacher_disagreement_score":0.07572115,"about_ca_system_score_codex":0.0005216589,"about_ca_system_score_gemma":0.0003848543,"threshold_uncertainty_score":0.1505608},"labels":[],"label_agreement":null},{"id":"W1681273431","doi":"10.1016/j.tecto.2015.08.017","title":"Earthquake relocations, crustal rheology, and active deformation in the central–eastern Alps (N Italy)","year":2015,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"LOEWE Zentrum AdRIA","keywords":"Geology; Seismology; Crust; Induced seismicity; Tectonics; Upper crust; Fault (geology); Focal mechanism; Seismotectonics; Geophysics","score_opus":0.02595120124823223,"score_gpt":0.22490037930762968,"score_spread":0.19894917805939746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1681273431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880326,0.0001780311,0.000018348133,0.000046309946,0.0000037412256,0.0000017286183,0.00022445267,0.0000042861425,0.0007199095],"genre_scores_gemma":[0.9990933,0.00007739043,0.000030975883,0.000016057958,0.000009859378,0.0000025496172,0.00040449537,0.0000023815865,0.0003629999],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989176,0.0000293359,0.00001108735,0.000029630031,0.000008814444,0.000029343819],"domain_scores_gemma":[0.9996952,0.000054061944,0.00015625599,0.000027852704,0.000024696468,0.000042060343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031573838,0.00016198587,0.00013979727,0.0010246001,0.0002137434,0.00038470794,0.00020080054,0.0002958784,0.001963439],"category_scores_gemma":[0.00059037155,0.00012938569,0.00031719776,0.0008076025,0.00036202447,0.00024755223,0.00040271072,0.00018459138,0.00035435427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023124558,0.00005819346,0.99190676,0.000018328454,0.000055599332,0.00014439561,0.0005252873,0.00028037,0.00077012717,0.00007914128,0.0004982953,0.0054322667],"study_design_scores_gemma":[0.0000028019438,0.000009221489,0.99964833,0.000002562205,0.000005420155,0.000028418086,0.00008747337,0.000053231703,0.0000083696395,0.0000048246216,0.00014870543,6.020011e-7],"about_ca_topic_score_codex":0.0285454,"about_ca_topic_score_gemma":0.04741507,"teacher_disagreement_score":0.0285454,"about_ca_system_score_codex":0.00038052918,"about_ca_system_score_gemma":0.00018593922,"threshold_uncertainty_score":0.056758523},"labels":[],"label_agreement":null},{"id":"W1705777835","doi":"10.1029/2005gc000917","title":"On the relationships between slab dip, back‐arc stress, upper plate absolute motion, and crustal nature in subduction zones","year":2005,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":533,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Slab; Slab window; Seismology; Lithosphere; Convergent boundary; Magnetic dip; Volcanic arc; Discontinuity (linguistics); Seamount; Oceanic crust; Geophysics; Tectonics; Paleontology","score_opus":0.013813811933083755,"score_gpt":0.20045069717434272,"score_spread":0.18663688524125896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1705777835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979997,0.00015333942,0.00079558964,0.000022665221,0.0000022871006,0.000004810605,0.00037021138,0.000016623397,0.0006347622],"genre_scores_gemma":[0.99909914,0.00004834244,0.00029732077,0.0000057266525,0.000006952007,0.0000041760336,0.00044480473,0.0000054769002,0.00008818833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989519,0.0003645599,0.00012136094,0.00029511433,0.00015711624,0.000109967514],"domain_scores_gemma":[0.9747662,0.02017738,0.0026876586,0.0009678627,0.00076172955,0.00063926814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031596634,0.0003809929,0.00027247603,0.0026419116,0.00036036392,0.0007491919,0.00030477016,0.00041926786,0.001672602],"category_scores_gemma":[0.0070223142,0.00024159624,0.000800028,0.0028938693,0.0011291777,0.00081102,0.0004957105,0.0004670386,0.0004321437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000098213975,0.000010788541,0.9952289,0.000009758764,0.00012596163,0.00005066284,0.000072295756,0.00052649353,0.001150612,0.00005860979,0.00003482351,0.0026328783],"study_design_scores_gemma":[0.0000014979884,0.00008386981,0.9973029,0.000002478422,0.000032831893,0.00009985903,0.0001149741,0.0020308627,0.00019315524,0.00005836653,0.00007154519,0.000007669696],"about_ca_topic_score_codex":0.0041869115,"about_ca_topic_score_gemma":0.0050600083,"teacher_disagreement_score":0.0041869115,"about_ca_system_score_codex":0.00024590205,"about_ca_system_score_gemma":0.00040930926,"threshold_uncertainty_score":0.016710043},"labels":[],"label_agreement":null},{"id":"W1716057239","doi":"10.17491/jgsi/2006/670106","title":"Origin of Fluorite Mineralisation and Hydrothermal Alteration at the Chandidongri Deposit, Rajnandgaon District, Central India - Evidence from Oxygen and Hydrogen Isotopes","year":2006,"lang":"en","type":"article","venue":"Journal of the Geological Society of India","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Fluorite; Geology; Geochemistry; Quartz; Proterozoic; Hydrothermal circulation; Mineralization (soil science); Fluid inclusions; Meteoric water; Magmatic water; Isotopes of oxygen; Vein; Schist; Mineralogy; Metamorphic rock; Tectonics","score_opus":0.015008406393607574,"score_gpt":0.20480681157504418,"score_spread":0.18979840518143662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1716057239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994759,0.000040968866,0.000019728086,0.0000046361047,3.6445832e-7,0.0000018321283,0.00005845573,0.0000026074683,0.00039553238],"genre_scores_gemma":[0.99973077,0.000026531536,0.00003599064,0.0000025146098,4.764985e-7,0.0000013264059,0.000060441176,6.944811e-7,0.0001411673],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999223,0.000005276739,0.000006879252,0.00002290625,0.000015574755,0.000027022817],"domain_scores_gemma":[0.99985945,0.000026414767,0.000036122856,0.000010794238,0.00003596628,0.00003125293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008025321,0.00014683284,0.00013396576,0.0012888175,0.00073848024,0.0005126768,0.0003851044,0.00016542786,0.0006243658],"category_scores_gemma":[0.0002436711,0.00022427925,0.000115371935,0.00075983565,0.0005776462,0.00019456068,0.00031202953,0.00012360349,0.000092326794],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023736956,0.000028993996,0.92496324,0.00008174518,0.00004185173,0.0010112002,0.004811887,0.00023881163,0.059643146,0.00023880138,0.00006393256,0.0086390115],"study_design_scores_gemma":[0.0000037431541,0.000020231462,0.9977659,0.0000037227908,0.0000064364435,0.0002959464,0.0006811598,0.00005184591,0.00093502057,0.000017127222,0.00021529963,0.00000353203],"about_ca_topic_score_codex":0.07984253,"about_ca_topic_score_gemma":0.13244614,"teacher_disagreement_score":0.07984253,"about_ca_system_score_codex":0.0007850938,"about_ca_system_score_gemma":0.0005107029,"threshold_uncertainty_score":0.1587556},"labels":[],"label_agreement":null},{"id":"W1742644122","doi":"10.1002/grl.50625","title":"The open ocean energy decay of three recent trans‐Pacific tsunamis","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; North Pacific Marine Science Organization","funders":"Russian Foundation for Basic Research","keywords":"Seismology; Geology; Pacific ocean; Range (aeronautics); Period (music); Oceanography; Physics","score_opus":0.04956692538873289,"score_gpt":0.2825790430352771,"score_spread":0.2330121176465442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1742644122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991716,0.000040705316,0.000055426313,0.000022007402,0.0000037586046,0.0000013227418,0.00019405645,0.000003102661,0.00050787616],"genre_scores_gemma":[0.99916387,0.00007073452,0.000053047777,0.0000070809197,0.000004444716,0.0000027001793,0.00046934863,0.000002313108,0.0002265301],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999627,0.000001972519,0.000004099001,0.000010057634,0.000009324493,0.00001188667],"domain_scores_gemma":[0.9996896,0.000042160136,0.0001042467,0.000019695302,0.0000851301,0.00005928072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010320354,0.00018382628,0.000087065695,0.0004469131,0.00026691623,0.0004987096,0.00012641755,0.00020527116,0.00087004696],"category_scores_gemma":[0.0006766075,0.000119277975,0.00016797021,0.0005347583,0.00024269104,0.0003940394,0.000675191,0.00031792742,0.00011404177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048480948,0.00008264156,0.94665945,0.00006567932,0.0001521875,0.00036988384,0.0005780218,0.0020676248,0.024285775,0.0003409979,0.00044742462,0.024465488],"study_design_scores_gemma":[0.0000040542086,0.000022922964,0.99814427,0.0000036734853,0.000012965365,0.000031547555,0.00015100876,0.0006151038,0.0006073883,0.00004142093,0.0003602511,0.0000053334734],"about_ca_topic_score_codex":0.02264208,"about_ca_topic_score_gemma":0.03732503,"teacher_disagreement_score":0.02264208,"about_ca_system_score_codex":0.00048027112,"about_ca_system_score_gemma":0.00027609392,"threshold_uncertainty_score":0.04502058},"labels":[],"label_agreement":null},{"id":"W1755440556","doi":"10.18867/ris.91.178","title":"DESAGREGACIÓN DEL PELIGRO SÍSMICO PARA ALGUNOS SITIOS SELECCIONADOS DE MÉXICO","year":2014,"lang":"es","type":"article","venue":"Revista de Ingeniería Sísmica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Humanities; Art","score_opus":0.015299116944448809,"score_gpt":0.23818343726280286,"score_spread":0.22288432031835406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1755440556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.979521,0.00031131276,0.0109538045,0.0002530718,0.000018582428,0.00006746744,0.0028073057,0.00019840377,0.005869079],"genre_scores_gemma":[0.9894574,0.00033777868,0.0050200718,0.000030410634,0.000006048554,0.00008109873,0.0015295921,0.000030261757,0.0035073233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998123,0.000046297264,0.0000075485723,0.00006306446,0.000022715743,0.000048087164],"domain_scores_gemma":[0.999736,0.00007398091,0.00006923924,0.000023686098,0.00006862053,0.000028380682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038916102,0.00048755103,0.00040450325,0.00055060716,0.000385053,0.001104857,0.0006516591,0.00036913168,0.0030792814],"category_scores_gemma":[0.00063606875,0.00024211555,0.00081678556,0.000847926,0.00026908994,0.0004377325,0.0006367259,0.000376938,0.00022465893],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044989353,0.000093967144,0.55893254,0.00025450287,0.00043400846,0.0004870683,0.00046694162,0.39412194,0.007564076,0.0036080475,0.002668956,0.030917961],"study_design_scores_gemma":[0.000058265643,0.00029440047,0.4644231,0.00008941809,0.000386209,0.000139792,0.0020620483,0.51435494,0.0023409047,0.0017226397,0.014068728,0.000059530248],"about_ca_topic_score_codex":0.19174126,"about_ca_topic_score_gemma":0.17230198,"teacher_disagreement_score":0.19174126,"about_ca_system_score_codex":0.0018352607,"about_ca_system_score_gemma":0.0012563912,"threshold_uncertainty_score":0.38125038},"labels":[],"label_agreement":null},{"id":"W175796641","doi":"10.1023/a:1004781927661","title":"Morphology and tectonics of the Yap Trench","year":2000,"lang":"en","type":"article","venue":"Marine Geophysical Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Hydrographic Service","funders":"","keywords":"Trench; Geology; Subduction; Convergent boundary; Seismology; Volcanic arc; Seafloor spreading; Ridge; Bathymetry; Gravity anomaly; Back-arc basin; Plate tectonics; Arc (geometry); Tectonics; Geomorphology; Oceanic crust; Paleontology; Geometry","score_opus":0.0336795765100525,"score_gpt":0.28398637199351695,"score_spread":0.25030679548346446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W175796641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967501,0.00003425671,0.00004348892,0.00003333861,6.2468536e-7,0.000002666703,0.00019986555,0.0000043269474,0.0029313574],"genre_scores_gemma":[0.9988011,0.00003682943,0.000071213675,0.0000037509635,9.41035e-7,0.0000032931287,0.00013653409,0.000004282783,0.00094199716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999517,0.0000048941442,0.0000019412314,0.000014186414,0.000009445252,0.000017923287],"domain_scores_gemma":[0.99987745,0.0000100584275,0.000045526074,0.000007690882,0.000035612404,0.00002363894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000071051916,0.00009266576,0.0000917695,0.00071582163,0.00053508976,0.00064781273,0.0002089271,0.00013719403,0.0024768442],"category_scores_gemma":[0.00038619945,0.00015454157,0.000072472605,0.00086428,0.00064919837,0.00022049072,0.0006126098,0.000119338154,0.00023512998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029211983,0.000026514983,0.92768824,0.00006581004,0.000053067382,0.00068885705,0.004365021,0.0042961324,0.021842163,0.002952411,0.001368216,0.03636139],"study_design_scores_gemma":[0.0000018366512,0.00001311091,0.99780196,0.0000031862094,0.0000029212044,0.00007085508,0.0006041167,0.0003918094,0.000099636585,0.000050724648,0.0009571619,0.000002543448],"about_ca_topic_score_codex":0.17346817,"about_ca_topic_score_gemma":0.4155545,"teacher_disagreement_score":0.17346817,"about_ca_system_score_codex":0.0010880983,"about_ca_system_score_gemma":0.0009654904,"threshold_uncertainty_score":0.34491694},"labels":[],"label_agreement":null},{"id":"W1777568429","doi":"10.1139/cjes-2013-0160","title":"The geometry of the North Anatolian transform fault in the Sea of Marmara and its temporal evolution: implications for the development of intracontinental transform faults","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"North Anatolian Fault; Geology; Transform fault; Seismology; Fault (geology); Strike-slip tectonics; Structural basin; Echelon formation; Shear (geology); Context (archaeology); Bathymetry; Paleontology; Oceanography","score_opus":0.019524196766460424,"score_gpt":0.22855609707538482,"score_spread":0.2090319003089244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1777568429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984768,0.00022203928,0.000095604875,0.000027567283,0.0000041000517,0.0000025736426,0.00017095261,0.0000036753606,0.0009967684],"genre_scores_gemma":[0.9994553,0.0001067442,0.00013904633,0.0000034920388,0.000004855022,0.0000024650815,0.00017721097,0.0000028598336,0.000108019565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971896,0.000054435935,0.000030323397,0.00009898694,0.000035339133,0.00006192565],"domain_scores_gemma":[0.99966085,0.00003998667,0.0001436971,0.000026882366,0.00008405953,0.000044535755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030936365,0.0002778757,0.0002982785,0.0021324381,0.0007235028,0.0014011273,0.00034615377,0.00036650553,0.0011738065],"category_scores_gemma":[0.00077108195,0.0001911373,0.00022574133,0.0029158068,0.0006485695,0.0005792028,0.0006456059,0.00021953476,0.00022907821],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010345026,0.00004005905,0.96365035,0.000048399397,0.00010223605,0.00077040785,0.0019770677,0.0016505335,0.009299444,0.00041262494,0.00017296181,0.02177255],"study_design_scores_gemma":[8.4967905e-7,0.0000087733615,0.9983209,0.000006999926,0.00001049046,0.00012876032,0.00057503214,0.00039953168,0.00016527933,0.00003370465,0.0003454712,0.000004137746],"about_ca_topic_score_codex":0.01677586,"about_ca_topic_score_gemma":0.027479738,"teacher_disagreement_score":0.01677586,"about_ca_system_score_codex":0.00065828796,"about_ca_system_score_gemma":0.00040248313,"threshold_uncertainty_score":0.03335643},"labels":[],"label_agreement":null},{"id":"W178889294","doi":"","title":"GPS studies of crustal deformation in the northern Cascadia subduction zone","year":2000,"lang":"en","type":"dissertation","venue":"UVic’s Research and Learning Repository (University of Victoria)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Global Positioning System; Seismology; Geodesy; Episodic tremor and slip; Deformation (meteorology); Tectonics; Oceanography; Engineering; Telecommunications","score_opus":0.02875216355457243,"score_gpt":0.2638078412826994,"score_spread":0.23505567772812697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W178889294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958165,0.00022307834,0.00006413312,0.000053094707,0.0000017258438,0.000010255164,0.0008820879,0.000008000857,0.0029410897],"genre_scores_gemma":[0.9961158,0.0004224439,0.00017582744,0.000011715175,0.0000015295365,0.000008115105,0.0012303696,0.0000032297144,0.0020309414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987364,0.000009969955,0.0000072032294,0.000029744297,0.000050224844,0.000029261044],"domain_scores_gemma":[0.9995419,0.000023934886,0.000070393646,0.000028160208,0.00022759239,0.00010801862],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000103377875,0.00017441774,0.00014549293,0.0012644335,0.00081558083,0.0004708289,0.00023752473,0.00014295694,0.0010147695],"category_scores_gemma":[0.00071051804,0.0001636197,0.00007663811,0.003293723,0.00041180235,0.000120627206,0.00039309767,0.00017683684,0.00019398477],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008893309,0.00003156844,0.9630968,0.00007357859,0.00004139368,0.00039459008,0.0030439768,0.001765844,0.0043711686,0.00016617442,0.0009629984,0.025963008],"study_design_scores_gemma":[0.0000017944316,0.00000671384,0.9985851,0.0000062604104,0.0000024652195,0.00003223184,0.0003491845,0.000143125,0.00006195165,0.000008548011,0.00080051407,0.000002195206],"about_ca_topic_score_codex":0.91906434,"about_ca_topic_score_gemma":0.9659561,"teacher_disagreement_score":0.08093566,"about_ca_system_score_codex":0.004129655,"about_ca_system_score_gemma":0.0026411845,"threshold_uncertainty_score":0.16282457},"labels":[],"label_agreement":null},{"id":"W1789072681","doi":"10.1093/gji/ggv337","title":"Using a modified time-reverse imaging technique to locate low-frequency earthquakes on the San Andreas Fault near Cholame, California","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Amplitude; Seismology; Coherence (philosophical gambling strategy); Geology; A priori and a posteriori; Event (particle physics); Phase (matter); Geodesy; Algorithm; Computer science; Physics; Optics; Statistics; Mathematics","score_opus":0.041119541030586175,"score_gpt":0.26252225354545433,"score_spread":0.22140271251486815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1789072681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6671138,0.0008513417,0.31114677,0.00034809086,0.00018334528,0.00015236388,0.001268998,0.0031267346,0.015808722],"genre_scores_gemma":[0.55093926,0.00037209198,0.44270372,0.00006598709,0.000097231,0.000082327475,0.0011675361,0.00016237599,0.0044094096],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99979025,0.000013462572,0.000012674033,0.00007348286,0.00008600206,0.000024078583],"domain_scores_gemma":[0.9994672,0.00006182086,0.00012252033,0.00007365181,0.00024043651,0.000034399232],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023994318,0.00048946106,0.0002901907,0.0015808586,0.00030562823,0.00070831605,0.0005961597,0.00040276503,0.0011354197],"category_scores_gemma":[0.0011207659,0.0002964468,0.00029626087,0.00080023846,0.00018318537,0.00051764137,0.00036308804,0.0003741377,0.00054454926],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002803395,0.00014990075,0.06914508,0.0003375415,0.00018335685,0.0008044706,0.000983443,0.027520131,0.28594795,0.0013893511,0.0043182494,0.60894006],"study_design_scores_gemma":[0.0001909688,0.00043714108,0.2551687,0.00015156879,0.00038382228,0.0033509086,0.000754259,0.5500899,0.15617962,0.0012707915,0.031761553,0.00026070373],"about_ca_topic_score_codex":0.011052067,"about_ca_topic_score_gemma":0.028961046,"teacher_disagreement_score":0.011052067,"about_ca_system_score_codex":0.00029813606,"about_ca_system_score_gemma":0.0006863958,"threshold_uncertainty_score":0.021975458},"labels":[],"label_agreement":null},{"id":"W1819806734","doi":"10.1029/2012jb009209","title":"Nucleation and arrest of dynamic slip on a pressurized fault","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":204,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Overpressure; Slip (aerodynamics); Nucleation; Pore water pressure; Geology; Materials science; Mechanics; Fault (geology); Geotechnical engineering; Seismology; Physics; Thermodynamics","score_opus":0.03286865699257321,"score_gpt":0.3079562125059899,"score_spread":0.27508755551341674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1819806734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996914,0.00008034826,0.0016007636,0.000013746662,0.0000030153178,0.000004732424,0.000022645812,0.000016499485,0.0013443381],"genre_scores_gemma":[0.9995846,0.000029306368,0.00013258429,0.0000020356256,0.0000013097329,0.0000028862678,0.000014499598,0.0000015124397,0.00023134226],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993837,0.00000489365,0.0000034826028,0.000016673615,0.000012041563,0.00002452565],"domain_scores_gemma":[0.9999025,0.000017726648,0.00003421626,0.0000076301885,0.000009669998,0.000028267948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007275013,0.00017769921,0.0002213638,0.00023040321,0.0002825958,0.00044189507,0.00028267072,0.0003360278,0.0009101688],"category_scores_gemma":[0.00028595244,0.00015380331,0.00027488937,0.00009457672,0.0005561631,0.00033557368,0.00036711677,0.00024981349,0.00006218579],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063750555,0.0002924927,0.04722128,0.00017902072,0.000086927714,0.0027540252,0.00046123797,0.35927632,0.56115454,0.014710725,0.0003414483,0.012884536],"study_design_scores_gemma":[0.000066444816,0.0005554249,0.04691095,0.000017288938,0.000044586057,0.0005058313,0.00027778433,0.82927424,0.118891194,0.0025833007,0.000830601,0.000042288983],"about_ca_topic_score_codex":0.0042933603,"about_ca_topic_score_gemma":0.0024191525,"teacher_disagreement_score":0.0042933603,"about_ca_system_score_codex":0.0005998968,"about_ca_system_score_gemma":0.00035672926,"threshold_uncertainty_score":0.008536696},"labels":[],"label_agreement":null},{"id":"W1822460102","doi":"10.1016/j.sandf.2015.09.006","title":"Reconnaissance report on geotechnical and structural damage caused by the 2015 Gorkha Earthquake, Nepal","year":2015,"lang":"en","type":"article","venue":"SOILS AND FOUNDATIONS","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Engineering and Physical Sciences Research Council; Japan Society for the Promotion of Science; Japan Society for the Promotion of Science London","keywords":"Aftershock; Geology; Landslide; Field survey; Masonry; Moment magnitude scale; Seismology; Geotechnical engineering; Natural hazard; Geography; Archaeology","score_opus":0.043523221453612294,"score_gpt":0.27876722189321507,"score_spread":0.23524400043960278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1822460102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9759511,0.0003077508,0.00032245362,0.0004587803,0.000053864544,0.00016942986,0.008024899,0.000029895284,0.014681886],"genre_scores_gemma":[0.9841127,0.0005838561,0.0003003196,0.00019408998,0.000025789672,0.00007370859,0.0063966075,0.0000050351127,0.008307885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997074,0.000035116092,0.000045362667,0.00003439658,0.00011176602,0.00006589273],"domain_scores_gemma":[0.99938965,0.00008603551,0.00016673774,0.00004097975,0.00026106197,0.0000555183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003462399,0.00023849965,0.00016623523,0.0014154864,0.0007128457,0.00046981743,0.00038328083,0.000572042,0.0019038935],"category_scores_gemma":[0.0011475759,0.00018154772,0.00018121512,0.001154483,0.00023084717,0.0003175427,0.00073362945,0.0003283062,0.00041365606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023531949,0.00030563513,0.88591725,0.0005534179,0.00016367895,0.013697015,0.015513012,0.0021423274,0.0070298156,0.00063862785,0.018772228,0.055031758],"study_design_scores_gemma":[0.0000037056482,0.00015065359,0.98044235,0.000060193048,0.000027245062,0.0011052055,0.006933198,0.0002582983,0.0007357838,0.000059428552,0.010212657,0.000011295753],"about_ca_topic_score_codex":0.059300076,"about_ca_topic_score_gemma":0.104467936,"teacher_disagreement_score":0.059300076,"about_ca_system_score_codex":0.00076894736,"about_ca_system_score_gemma":0.0014403592,"threshold_uncertainty_score":0.11790979},"labels":[],"label_agreement":null},{"id":"W1829440091","doi":"10.1139/e10-011","title":"Great earthquakes on Canada’s west coast: a review This article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>. Geological Survey of Canada Contribution 20090196.","year":2010,"lang":"en","type":"review","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"University of Victoria","keywords":"Geology; Subduction; Seismology; Thrust fault; Slip (aerodynamics); Limiting; Continental margin; Fault (geology); Episodic tremor and slip; Tectonics","score_opus":0.02772243639399464,"score_gpt":0.2225424397122526,"score_spread":0.19482000331825797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1829440091","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00084159017,0.99164283,0.00008144748,0.0035485597,0.00090362795,0.000009204504,0.00023865278,0.000011193951,0.0027229467],"genre_scores_gemma":[0.0028004092,0.9949774,0.00010183995,0.00062845944,0.00055975374,0.0000045781303,0.00015009801,0.0000050812764,0.00077229325],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995523,0.000023961013,0.00006433168,0.00007099427,0.00021101916,0.000077399185],"domain_scores_gemma":[0.99558794,0.0009513043,0.00034281655,0.00005687129,0.002545543,0.0005156111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00093575974,0.0011739782,0.0010340008,0.007728558,0.001706101,0.003662398,0.001157315,0.0015856616,0.004286217],"category_scores_gemma":[0.0030796006,0.0005175987,0.00043450395,0.014771974,0.001956325,0.0018453179,0.0010904912,0.001750845,0.0007972038],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000082547784,0.000054175613,0.00921043,0.012890869,0.00015721133,0.0003888903,0.0016352914,0.000532587,0.0003287549,0.0044311364,0.1871221,0.78316593],"study_design_scores_gemma":[0.000007601685,0.000041132236,0.03515476,0.012403863,0.00015902454,0.0005338619,0.0016674284,0.00012504424,0.000100601865,0.00073882996,0.94900507,0.0000628189],"about_ca_topic_score_codex":0.86469644,"about_ca_topic_score_gemma":0.9055075,"teacher_disagreement_score":0.13530356,"about_ca_system_score_codex":0.014158156,"about_ca_system_score_gemma":0.052964777,"threshold_uncertainty_score":0.2722007},"labels":[],"label_agreement":null},{"id":"W1830894573","doi":"10.1360/02yd0144","title":"On deposits controlled by tectonic lenses","year":2004,"lang":"en","type":"article","venue":"Science in China Series D Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal; Geological Survey of Canada","funders":"","keywords":"Tectonics; Geology; Lens (geology); Tectonic phase; Petrology; Geochemistry; Seismology; Paleontology","score_opus":0.010836528642368571,"score_gpt":0.22470872094965513,"score_spread":0.21387219230728657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1830894573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97662145,0.00022704549,0.0014428758,0.00017947095,0.000022745042,0.000008731393,0.0001506607,0.000049588667,0.021297423],"genre_scores_gemma":[0.9977488,0.00011179978,0.00018391806,0.000008875865,0.000017792314,0.0000029324538,0.00007938815,0.0000128408665,0.001833594],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99979264,0.000025293324,0.000013205612,0.000059826976,0.000046461642,0.00006257376],"domain_scores_gemma":[0.9991061,0.00018978115,0.0002862149,0.00014404312,0.00016466314,0.00010915564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025174397,0.00033195168,0.0006074723,0.0015716262,0.0011546633,0.0020464095,0.00057620683,0.0004039133,0.0069363285],"category_scores_gemma":[0.001681747,0.0002756334,0.00028131998,0.0011300935,0.0016918861,0.0015235294,0.000925384,0.00034938645,0.00030398724],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004505464,0.00022747087,0.14156751,0.0004999887,0.000377922,0.0052317274,0.0030301781,0.05651748,0.07923845,0.64486796,0.0053295367,0.05860621],"study_design_scores_gemma":[0.001227032,0.00034609702,0.45511675,0.00014381477,0.0005384778,0.0010113843,0.0033254363,0.118478164,0.019211495,0.37916845,0.021247456,0.00018549191],"about_ca_topic_score_codex":0.023109682,"about_ca_topic_score_gemma":0.02229512,"teacher_disagreement_score":0.023109682,"about_ca_system_score_codex":0.0018179839,"about_ca_system_score_gemma":0.0008529343,"threshold_uncertainty_score":0.045950294},"labels":[],"label_agreement":null},{"id":"W1838916818","doi":"10.1111/j.1365-246x.2007.03583.x","title":"Evidence for underthrusting beneath the Queen Charlotte Margin, British Columbia, from teleseismic receiver function analysis","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Receiver function; Geology; Seismology; Crust; Oceanic crust; Subduction; Fault (geology); Margin (machine learning); Lithosphere; Tectonics; Geophysics","score_opus":0.03525684656665979,"score_gpt":0.2562751332544439,"score_spread":0.22101828668778412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1838916818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968689,0.00008527028,0.00020522375,0.000048147624,0.0000015626302,0.000003681809,0.0003172426,0.000013424015,0.0024564923],"genre_scores_gemma":[0.998417,0.00008206692,0.00015206973,0.000014897115,0.0000012775378,0.0000024091546,0.0002973309,0.000004299798,0.0010285167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997969,0.0000118318885,0.000012026387,0.00004062624,0.0000739924,0.00006456195],"domain_scores_gemma":[0.99855727,0.00018364139,0.00032854592,0.000089177694,0.00064742827,0.0001939301],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020770499,0.00022291571,0.00012949851,0.0011864268,0.0006218458,0.0010114287,0.00036493814,0.00026138985,0.0023948469],"category_scores_gemma":[0.001680796,0.00027806225,0.00006357661,0.0015477814,0.0006884319,0.00019205565,0.00041710757,0.00023196358,0.000340387],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001414567,0.000014790633,0.9580701,0.000043983604,0.0000298558,0.0006132428,0.0020859465,0.00057630177,0.023090709,0.0002868633,0.0006750523,0.014371666],"study_design_scores_gemma":[0.0000028859354,0.000005607699,0.99810934,0.000011329678,0.000007722633,0.00010571269,0.00038406425,0.0004633786,0.00039868985,0.000019900104,0.00048605257,0.000005241571],"about_ca_topic_score_codex":0.85881597,"about_ca_topic_score_gemma":0.95756376,"teacher_disagreement_score":0.14118403,"about_ca_system_score_codex":0.0023610822,"about_ca_system_score_gemma":0.0027876468,"threshold_uncertainty_score":0.28403097},"labels":[],"label_agreement":null},{"id":"W1845672550","doi":"10.1002/grl.50509","title":"Geometrical effects of a subducted seamount on stopping megathrust ruptures","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Seamount; Geology; Subduction; Seismology; Fault gouge; Fault (geology); Tectonics; Oceanography","score_opus":0.028396758658262918,"score_gpt":0.275926717459429,"score_spread":0.24752995880116607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1845672550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977375,0.00002693779,0.0008065515,0.000032288066,0.0000066563694,0.0000070255005,0.000052390864,0.000033481232,0.0012970426],"genre_scores_gemma":[0.9993993,0.000014597965,0.0003786556,0.0000067216465,0.0000010903282,0.0000033695512,0.000028456996,0.0000053396498,0.00016253704],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998739,0.000030582698,0.000008954996,0.000018860635,0.000020711115,0.000047009595],"domain_scores_gemma":[0.9996105,0.00013329466,0.00008317353,0.00004772329,0.000050190272,0.00007517306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029572414,0.00039501066,0.00038374987,0.0003893781,0.0004645198,0.0007099887,0.00084978476,0.0008501277,0.0024078658],"category_scores_gemma":[0.0015495886,0.00031764596,0.00051320577,0.00029398798,0.00083489454,0.00035108984,0.0006810192,0.00030421626,0.00012468724],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021212154,0.0000548871,0.014714208,0.000031800588,0.000050045335,0.00038941726,0.00007739289,0.97552615,0.006325262,0.0008321337,0.00007949795,0.0017071416],"study_design_scores_gemma":[0.00009749293,0.00038759934,0.01063621,0.00001646014,0.000056732402,0.0000969228,0.0001327246,0.9845195,0.0034152262,0.00029589527,0.0003200596,0.000025210866],"about_ca_topic_score_codex":0.015096374,"about_ca_topic_score_gemma":0.008406874,"teacher_disagreement_score":0.015096374,"about_ca_system_score_codex":0.0008511908,"about_ca_system_score_gemma":0.00068236823,"threshold_uncertainty_score":0.030017018},"labels":[],"label_agreement":null},{"id":"W1850611326","doi":"10.1007/s10040-014-1206-1","title":"Permeability of a fault zone crosscutting a sequence of sandstones and shales and its influence on hydraulic head distribution in the Chatsworth Formation, California, USA","year":2014,"lang":"en","type":"article","venue":"Hydrogeology Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Guelph; Boeing","keywords":"Geology; Oil shale; Outcrop; Fault (geology); Hydrogeology; Borehole; Petrology; Permeability (electromagnetism); Hydraulic head; Geotechnical engineering; Geomorphology; Seismology; Paleontology","score_opus":0.02238542758410008,"score_gpt":0.2533817535062248,"score_spread":0.23099632592212474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1850611326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997154,0.000025345527,0.0000331105,0.000005301551,2.3805968e-7,0.0000014624538,0.00003209948,0.0000022487436,0.0001847846],"genre_scores_gemma":[0.9997807,0.000024386822,0.00006436792,0.0000017929103,2.6358006e-7,9.303483e-7,0.00003999898,2.868243e-7,0.000087297674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993813,0.0000050978765,0.000004680627,0.000019785151,0.000021676009,0.00001060181],"domain_scores_gemma":[0.9998436,0.000028502056,0.000055025776,0.000006540779,0.000042650827,0.0000235994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011014795,0.0001105126,0.00009245551,0.00061867066,0.00040662562,0.00035098175,0.00018768875,0.00012524659,0.00030637273],"category_scores_gemma":[0.00030268557,0.00014609545,0.00006873586,0.00037994664,0.0003992091,0.00015351379,0.00019448758,0.000115332004,0.00002294879],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012172601,0.00005203935,0.95672876,0.00004065999,0.00003596612,0.00026990724,0.00064033247,0.00226052,0.031291004,0.0001449725,0.00015637443,0.008257767],"study_design_scores_gemma":[0.0000022267704,0.000015159119,0.99767226,0.000002823174,0.0000063168986,0.000029886836,0.00012385326,0.0011718534,0.0008816041,0.000016187027,0.00007575845,0.0000020269042],"about_ca_topic_score_codex":0.23246293,"about_ca_topic_score_gemma":0.4752774,"teacher_disagreement_score":0.23246293,"about_ca_system_score_codex":0.0013321907,"about_ca_system_score_gemma":0.0007698129,"threshold_uncertainty_score":0.46221972},"labels":[],"label_agreement":null},{"id":"W1851392737","doi":"10.1002/2013jb010351","title":"Shallow, old, and hydrologically insignificant fault zones in the Appalachian orogen","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Université du Québec à Montréal; Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Groundwater; Geology; Aquifer; Bedrock; Groundwater flow; Thrust fault; Paleozoic; Fault (geology); Hydrology (agriculture); Permeability (electromagnetism); Geochemistry; Petrology; Geomorphology; Geotechnical engineering; Seismology","score_opus":0.041507577070985145,"score_gpt":0.30242461695016987,"score_spread":0.26091703987918474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1851392737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951696,0.000028131108,0.000040263185,0.0000073280594,2.967598e-7,0.00000270564,0.00007483771,0.0000020110906,0.0003275908],"genre_scores_gemma":[0.99976593,0.000031623713,0.00006464164,0.000003884765,5.2176085e-7,0.000002139336,0.000068023655,5.5301143e-7,0.00006265725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984753,0.000023175811,0.000010022679,0.000040435985,0.000024289177,0.000054468903],"domain_scores_gemma":[0.9997949,0.000057422305,0.00006443006,0.000016040634,0.00004316959,0.000024036846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016590474,0.00017372494,0.00021930652,0.00084855,0.000736138,0.0007896737,0.0003237021,0.00020325113,0.0006047172],"category_scores_gemma":[0.0004884099,0.00014027397,0.00016997367,0.0012681349,0.00083508866,0.00021373302,0.00037488746,0.0001257269,0.000041703228],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000121325575,0.000028273667,0.9838129,0.000039085848,0.00006453122,0.00059993914,0.0007532985,0.0036510574,0.0052017192,0.00030398418,0.00006747229,0.0053563807],"study_design_scores_gemma":[0.0000061897435,0.000015430864,0.99543554,0.0000078243975,0.000027940034,0.000076628996,0.0010525876,0.0027592925,0.000269369,0.0000978359,0.00024459828,0.0000068065306],"about_ca_topic_score_codex":0.57267666,"about_ca_topic_score_gemma":0.68502384,"teacher_disagreement_score":0.57267666,"about_ca_system_score_codex":0.002252921,"about_ca_system_score_gemma":0.0014340497,"threshold_uncertainty_score":0.8596799},"labels":[],"label_agreement":null},{"id":"W1857553324","doi":"10.7202/032964ar","title":"Natural and Induced Seismicity in the Lake Erie-Lake Ontario Region: Reactivation of Ancient Faults with Little Neotectonic Displacement","year":2007,"lang":"en","type":"article","venue":"Géographie physique et Quaternaire","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Lamont-Doherty Earth Observatory, Columbia University; U.S. Geological Survey; John Carroll University; U.S. Nuclear Regulatory Commission","keywords":"Geology; Induced seismicity; Seismology; Aftershock; Fault (geology); Lineament; Paleozoic; Active fault; Tectonics; Basement; Neotectonics; Paleontology; Archaeology","score_opus":0.015437715311834866,"score_gpt":0.2250750421912111,"score_spread":0.20963732687937625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1857553324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992403,0.00005039582,0.000013894384,0.000016691893,3.4346158e-7,0.0000040513664,0.00011539185,0.0000013756425,0.0005576113],"genre_scores_gemma":[0.99925345,0.00007005085,0.000032798216,0.000007707435,9.1919634e-7,0.0000052033124,0.00018492235,8.62621e-7,0.00044396878],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981064,0.000016832795,0.000012208455,0.000030650193,0.000049397015,0.00008034538],"domain_scores_gemma":[0.99967194,0.000023192171,0.00014315854,0.000017664112,0.00007449703,0.00006958616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013296369,0.00010534767,0.00011359689,0.00053008314,0.00062497373,0.00042652205,0.0003429454,0.00021307985,0.00074383226],"category_scores_gemma":[0.000678537,0.0001440023,0.00011150253,0.0010129706,0.0007286779,0.00018190622,0.0004722596,0.000115186376,0.00006837968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018887792,0.000027385935,0.9859141,0.0000468312,0.000042190884,0.00067023473,0.0031180868,0.0004374547,0.0040721074,0.00016677273,0.00023341176,0.005082587],"study_design_scores_gemma":[0.0000027598146,0.000008542649,0.9990853,0.0000023804548,0.0000036321007,0.00003793246,0.00047376164,0.00005495259,0.00006125402,0.000004883193,0.00026275258,0.0000018243297],"about_ca_topic_score_codex":0.78436553,"about_ca_topic_score_gemma":0.95102376,"teacher_disagreement_score":0.21563447,"about_ca_system_score_codex":0.005869708,"about_ca_system_score_gemma":0.0037571536,"threshold_uncertainty_score":0.43380874},"labels":[],"label_agreement":null},{"id":"W1860926049","doi":"10.1016/j.tecto.2015.10.009","title":"Stress adjustment revealed by seismicity and earthquake focal mechanisms in northeast China before and after the 2011 Tohoku-Oki earthquake","year":2015,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Natural Science Foundation of China","keywords":"Induced seismicity; Seismology; Geology; Seismic moment; Focal mechanism; Subduction; Stress field; Intraplate earthquake; Slip (aerodynamics); Fault (geology); Tectonics","score_opus":0.009401283895241799,"score_gpt":0.1956549874176917,"score_spread":0.18625370352244988,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1860926049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99970585,0.000031633095,0.0000105468525,0.000029238394,0.0000024457765,0.000001486547,0.00006141517,9.762317e-7,0.00015641494],"genre_scores_gemma":[0.9994572,0.000046000565,0.000012277706,0.000015365822,0.000005055767,0.0000028496136,0.00018727063,0.0000011882333,0.00027287737],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999772,0.000016601494,0.000027039043,0.00006033166,0.000029613066,0.00009448062],"domain_scores_gemma":[0.9993031,0.0000451436,0.00023848463,0.00004159894,0.00012284066,0.0002488227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030634995,0.00044105214,0.00048598083,0.0017020256,0.00094899465,0.000767273,0.0005360727,0.0005421896,0.0010754209],"category_scores_gemma":[0.0005996053,0.000412661,0.00047122312,0.0023961677,0.00071260217,0.0006148659,0.00088779774,0.00034921098,0.00013624509],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014032812,0.000051616196,0.99091727,0.000024101684,0.00009700251,0.00035819056,0.0019608778,0.00032394016,0.0031869537,0.00012765388,0.0001769652,0.0026351162],"study_design_scores_gemma":[9.480984e-7,0.000007777791,0.9993149,0.0000014458097,0.000009073323,0.0000112403495,0.00047185968,0.00008615312,0.000023322486,0.000007767733,0.000062007566,0.0000033867593],"about_ca_topic_score_codex":0.09849223,"about_ca_topic_score_gemma":0.23068121,"teacher_disagreement_score":0.09849223,"about_ca_system_score_codex":0.0016418542,"about_ca_system_score_gemma":0.0015688788,"threshold_uncertainty_score":0.19583791},"labels":[],"label_agreement":null},{"id":"W1878741970","doi":"10.1002/2015gc005971","title":"Late <scp>M</scp>iocene to recent plate tectonic history of the southern <scp>C</scp>entral <scp>A</scp>merica convergent margin","year":2015,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Alfred P. Sloan Foundation; National Science Foundation","keywords":"Geology; Subduction; Seamount; Neogene; Volcanism; Convergent boundary; Seismology; Volcanic arc; Triple junction; Slab window; Plate tectonics; Oceanic crust; Tectonics; Paleontology; Geophysics; Structural basin","score_opus":0.018933085108828865,"score_gpt":0.19472498353286558,"score_spread":0.1757918984240367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1878741970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870695,0.00051818066,0.00016722505,0.00018933746,0.000011272529,0.00000558111,0.00077578466,0.0000425306,0.011220565],"genre_scores_gemma":[0.99818146,0.00015387882,0.00012031641,0.000014715566,0.0000087019625,0.000003857964,0.0007954526,0.000008916712,0.00071277365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999515,0.0000023581392,0.000002612446,0.000018613588,0.0000115053235,0.000013383615],"domain_scores_gemma":[0.99983203,0.000009700036,0.000040511786,0.000015757001,0.00007715227,0.000024798226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015795924,0.00012427986,0.00010861732,0.000803639,0.00051606714,0.0009734302,0.00017237471,0.00018659921,0.0029461822],"category_scores_gemma":[0.000450984,0.00010285437,0.00013199112,0.00075090985,0.00036406805,0.00020695478,0.00044975616,0.00026041103,0.0002919462],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019261091,0.000032219286,0.914236,0.000108150496,0.00010701575,0.00032698293,0.0011940554,0.0029845294,0.022322332,0.0022106748,0.0019299899,0.05435542],"study_design_scores_gemma":[0.0000048263,0.000005799574,0.99328387,0.000018708366,0.000009447382,0.00004104178,0.00015209164,0.00070842396,0.00043757656,0.000084974155,0.005250651,0.0000027226522],"about_ca_topic_score_codex":0.13544068,"about_ca_topic_score_gemma":0.20494086,"teacher_disagreement_score":0.13544068,"about_ca_system_score_codex":0.0016084708,"about_ca_system_score_gemma":0.00075552554,"threshold_uncertainty_score":0.26930463},"labels":[],"label_agreement":null},{"id":"W1879854322","doi":"10.1029/2011gc003623","title":"Heat flow distribution and thermal structure of the Nankai subduction zone off the Kii Peninsula","year":2011,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Japan Society for the Promotion of Science; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Geology; Subduction; Forearc; Trough (economics); Accretionary wedge; Seismology; Petrology; Geomorphology; Geophysics; Tectonics","score_opus":0.00820665210719886,"score_gpt":0.1654846138505324,"score_spread":0.15727796174333353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1879854322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996507,0.000019576286,0.000035619916,0.000005193015,2.99898e-7,0.000002181639,0.000061897044,0.0000043407185,0.00022009443],"genre_scores_gemma":[0.99959975,0.000020192783,0.00008244035,0.0000019382585,6.803226e-7,0.0000046275923,0.00011988287,0.0000011819895,0.00016930654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999685,0.0000031801362,0.0000024127924,0.000012134058,0.0000048705083,0.000008833458],"domain_scores_gemma":[0.9999341,0.000009444273,0.000019447298,0.0000050805384,0.0000147659275,0.000017177195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000656418,0.00018498994,0.00014310695,0.0005732742,0.00021025786,0.00028423162,0.00018953318,0.00014936125,0.000631631],"category_scores_gemma":[0.00012643768,0.00015417715,0.00012155453,0.0004521419,0.0003136338,0.0001462217,0.00022101986,0.00011020741,0.000110775945],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020568224,0.00005652892,0.9385585,0.000057093133,0.00004902174,0.00043043194,0.0016524567,0.0050048423,0.041222956,0.00019046878,0.000112749294,0.012459269],"study_design_scores_gemma":[0.0000024113986,0.000012596471,0.99808985,0.000002081142,0.0000033309018,0.000026332835,0.00016762523,0.0013477956,0.00024148231,0.00000981057,0.000093441915,0.0000032663393],"about_ca_topic_score_codex":0.029688554,"about_ca_topic_score_gemma":0.03451287,"teacher_disagreement_score":0.029688554,"about_ca_system_score_codex":0.0005228873,"about_ca_system_score_gemma":0.00030126737,"threshold_uncertainty_score":0.059031546},"labels":[],"label_agreement":null},{"id":"W1891800431","doi":"10.1002/2015gl063455","title":"Hydraulic fracturing and the Crooked Lake Sequences: Insights gleaned from regional seismic networks","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Western University","funders":"","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Seismology; Seismometer; Sequence (biology); Paleontology","score_opus":0.05631406258949844,"score_gpt":0.27134961307717137,"score_spread":0.21503555048767292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1891800431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980292,0.00006778967,0.00028552004,0.000028430804,0.0000013920484,0.0000071186437,0.00051817147,0.000010449797,0.0010519343],"genre_scores_gemma":[0.998727,0.00004053925,0.00030928125,0.000004825363,0.0000017224028,0.00000228827,0.00067555846,0.000003065579,0.00023568088],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999107,0.000008707673,0.000006094713,0.000019396133,0.000024146706,0.000030906056],"domain_scores_gemma":[0.99955386,0.000056149445,0.0001090054,0.000026300584,0.00019360968,0.000061020022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013525627,0.0001378819,0.00013789203,0.0018800203,0.0003836579,0.00046859868,0.00026577403,0.00018355042,0.0008619432],"category_scores_gemma":[0.0012217491,0.000067670284,0.00010254236,0.0020445727,0.00034477576,0.00017590332,0.0004381523,0.00013111504,0.00011387074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016587818,0.00003987072,0.9435165,0.000068299254,0.00007301241,0.00054471404,0.0015408621,0.0075949496,0.013553939,0.0006208683,0.0008352903,0.031445943],"study_design_scores_gemma":[0.0000030484973,0.000012573008,0.99326247,0.0000108886825,0.0000118588905,0.00006151997,0.0010195639,0.0043577747,0.00038417344,0.00006505387,0.0008045091,0.0000066690295],"about_ca_topic_score_codex":0.60510963,"about_ca_topic_score_gemma":0.8081914,"teacher_disagreement_score":0.60510963,"about_ca_system_score_codex":0.0010976682,"about_ca_system_score_gemma":0.001334284,"threshold_uncertainty_score":0.7944319},"labels":[],"label_agreement":null},{"id":"W1896307426","doi":"10.1002/jgrb.50118","title":"InSAR Evidence for an active shallow thrust fault beneath the city of Spokane Washington, USA","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Interferometric synthetic aperture radar; Fault (geology); Seismic hazard; Seismic gap; Thrust fault; Active fault; Slip (aerodynamics); Synthetic aperture radar; Remote sensing; Engineering","score_opus":0.1691329890104908,"score_gpt":0.3888724245118331,"score_spread":0.21973943550134234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1896307426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882533,0.00016970899,0.00022745488,0.0003766157,0.0000263531,0.000011746415,0.0026967255,0.000021012287,0.008217183],"genre_scores_gemma":[0.99547076,0.00021020218,0.00036289592,0.00012146302,0.000017434924,0.000009838368,0.0023867975,0.000004167039,0.0014164164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998908,0.0000070560686,0.000007521383,0.00002550116,0.000029072957,0.00003997791],"domain_scores_gemma":[0.9996088,0.000026042226,0.000105841726,0.000034459998,0.00016011234,0.000064701286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012695257,0.00019854355,0.000120469835,0.0009496504,0.00079998444,0.00064027734,0.00020664737,0.00034556867,0.0015249113],"category_scores_gemma":[0.0004650971,0.00014671571,0.00007669873,0.0012044212,0.00034908997,0.00024001936,0.0005099793,0.00034073764,0.00032851315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008343697,0.00003648729,0.96587765,0.00007518316,0.00006589979,0.00066063745,0.0012343285,0.00021279651,0.0064209583,0.00022877663,0.00788398,0.01721986],"study_design_scores_gemma":[0.000003988395,0.000009270431,0.993386,0.000019282214,0.000012872216,0.000111634305,0.0015378254,0.0001304056,0.00031013525,0.000024595762,0.004448818,0.0000052338933],"about_ca_topic_score_codex":0.19362558,"about_ca_topic_score_gemma":0.4228378,"teacher_disagreement_score":0.19362558,"about_ca_system_score_codex":0.00050025765,"about_ca_system_score_gemma":0.0008508243,"threshold_uncertainty_score":0.38499707},"labels":[],"label_agreement":null},{"id":"W1897211107","doi":"10.1139/e10-026","title":"Application of modern 2-D and 3-D seismic-reflection techniques for uranium exploration in the Athabasca BasinThis article is one of a series of papers published in this Special Issue on the theme<i>Lithoprobe — parameters, processes, and the evolution of a continent</i>.","year":2010,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; Cameco (Canada); Geological Survey of Canada","funders":"","keywords":"Geology; Unconformity; Structural basin; Borehole; Basement; Geochemistry; Drilling; Seismology; Geomorphology; Mining engineering; Paleontology","score_opus":0.01756182333700454,"score_gpt":0.21626273028116366,"score_spread":0.19870090694415912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1897211107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85561484,0.0017394924,0.116496935,0.0006235323,0.000074868694,0.000106641695,0.0024250844,0.0015416052,0.021377033],"genre_scores_gemma":[0.8828582,0.00074100855,0.11367523,0.00009758099,0.000018821922,0.00004960524,0.00077087386,0.00006577722,0.0017229309],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99985147,0.000020817584,0.00000777699,0.000041078056,0.000054894226,0.000023886536],"domain_scores_gemma":[0.9999176,0.000018613368,0.000017315679,0.000014628118,0.000023622357,0.000008188026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020685159,0.0003200895,0.00013056882,0.001098776,0.00028740073,0.00053588755,0.00037601273,0.00030041407,0.0016017114],"category_scores_gemma":[0.00028169894,0.00017337578,0.0002047184,0.0011644713,0.00020083519,0.0003058442,0.00045441272,0.00024483528,0.0002263653],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020275636,0.00014249809,0.07287424,0.00024203291,0.00009815387,0.00062374846,0.0007304093,0.03581834,0.4705933,0.0022973213,0.0019710765,0.41440612],"study_design_scores_gemma":[0.0000861709,0.00022917213,0.55370516,0.000087233806,0.00008895104,0.0016241218,0.0017689901,0.32807758,0.07742465,0.0028308174,0.033896204,0.00018093995],"about_ca_topic_score_codex":0.0137191,"about_ca_topic_score_gemma":0.04887318,"teacher_disagreement_score":0.0137191,"about_ca_system_score_codex":0.00040393684,"about_ca_system_score_gemma":0.0004395818,"threshold_uncertainty_score":0.027278543},"labels":[],"label_agreement":null},{"id":"W1900036548","doi":"10.1029/2012jb009407","title":"Juan de Fuca slab geometry and its relation to Wadati‐Benioff zone seismicity","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":275,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Forearc; Subduction; Seismology; Induced seismicity; Slab; Aftershock; Slab window; Accretionary wedge; Tectonics; Plate tectonics; Trench; Oceanic crust; Geophysics","score_opus":0.042495158966870346,"score_gpt":0.308805083072967,"score_spread":0.26630992410609666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1900036548","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924871,0.000094874886,0.003899674,0.00008677652,0.000005101034,0.000009957077,0.00030889484,0.00007104729,0.003036655],"genre_scores_gemma":[0.9988201,0.000049432583,0.00067404757,0.0000025615207,0.0000021240107,0.000006433322,0.00010706559,0.000004367261,0.00033383945],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999949,0.000006136754,0.0000019445836,0.000019669775,0.0000073197907,0.000016073305],"domain_scores_gemma":[0.99989223,0.0000149187,0.000041155374,0.000013939429,0.000019590298,0.000018218212],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000088446024,0.00045621977,0.00017872693,0.0004294442,0.00037381114,0.00069191534,0.00042000666,0.00028129452,0.0008279624],"category_scores_gemma":[0.00061254756,0.0002914423,0.00025072045,0.0003451316,0.00040057956,0.00021867614,0.0003843309,0.00022184411,0.00009912039],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013777398,0.000037212267,0.38256636,0.000026892192,0.00006362696,0.00023209253,0.00021458828,0.59452057,0.006275975,0.004479541,0.00041891192,0.011026456],"study_design_scores_gemma":[0.000027742864,0.00003244973,0.26722735,0.000013416007,0.000031097094,0.00017874777,0.00011779203,0.7276029,0.0008313848,0.0021133719,0.0017879193,0.000035851983],"about_ca_topic_score_codex":0.15335542,"about_ca_topic_score_gemma":0.08436319,"teacher_disagreement_score":0.15335542,"about_ca_system_score_codex":0.0013184149,"about_ca_system_score_gemma":0.0006648417,"threshold_uncertainty_score":0.30492556},"labels":[],"label_agreement":null},{"id":"W1903059073","doi":"10.1002/jgrb.50101","title":"Heterogeneous rupture in the great Cascadia earthquake of 1700 inferred from coastal subsidence estimates","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":153,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Ocean Networks Canada Society; University of Victoria","funders":"U.S. Geological Survey; University of Victoria; National Science Foundation","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Episodic tremor and slip; Moment magnitude scale; Plate tectonics; Subsidence; Tectonics; Paleontology; Geometry","score_opus":0.04319703663587497,"score_gpt":0.3080497416380789,"score_spread":0.2648527050022039,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1903059073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984041,0.000057875946,0.00027225495,0.000014827641,0.000001486626,0.0000017841706,0.00038008858,0.000022728898,0.00084494986],"genre_scores_gemma":[0.9993783,0.000033723656,0.00011659548,0.000002635113,0.0000013208219,9.565798e-7,0.00040232058,0.0000026559098,0.000061342726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988997,0.000016773123,0.000014326331,0.000031653344,0.000028115048,0.00001918549],"domain_scores_gemma":[0.999395,0.0001326192,0.00016926284,0.00008544283,0.00010848441,0.000109135566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004296238,0.00043025677,0.00020584719,0.0015565271,0.00025477968,0.000695649,0.00032938216,0.0003343372,0.0010192688],"category_scores_gemma":[0.001524094,0.00036399427,0.0002923696,0.001110268,0.00032231663,0.00033747457,0.00051963044,0.0001629555,0.00029989498],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042036656,0.00001132118,0.98783964,0.000024669622,0.000051552353,0.00012114025,0.00015697192,0.007093207,0.0019494898,0.00009657433,0.00015101371,0.0024623296],"study_design_scores_gemma":[0.0000031304878,0.000011106801,0.9920614,0.000007273259,0.0000124668895,0.00003953307,0.00012886347,0.007196618,0.0002342399,0.00006402645,0.00023381361,0.0000075019693],"about_ca_topic_score_codex":0.052295607,"about_ca_topic_score_gemma":0.06123678,"teacher_disagreement_score":0.052295607,"about_ca_system_score_codex":0.000862607,"about_ca_system_score_gemma":0.00034013786,"threshold_uncertainty_score":0.10398239},"labels":[],"label_agreement":null},{"id":"W1903237231","doi":"10.1029/2012gl053716","title":"Experimental craters formed by single and multiple buried explosions and implications for volcanic craters with emphasis on maars","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Istituto Nazionale di Geofisica e Vulcanologia","keywords":"Impact crater; Ejecta; Geology; Volcano; Maar; Explosive material; Explosive eruption; Seismology; Geophysics; Astrobiology; Pyroclastic rock","score_opus":0.06689322472392299,"score_gpt":0.30724980048755207,"score_spread":0.24035657576362907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1903237231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99938774,0.00005963087,0.00027622253,0.0000068505456,0.000003311463,0.00001667442,0.00004599417,0.0000049845007,0.00019845912],"genre_scores_gemma":[0.9977633,0.0000898646,0.0013799313,0.000014590617,0.000006705027,0.000049008988,0.00012737776,0.000007687262,0.0005615445],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99957293,0.000062343875,0.00005942685,0.000091626105,0.000081789185,0.00013185568],"domain_scores_gemma":[0.99892694,0.00051107304,0.00014185498,0.00020341115,0.00007329607,0.00014339782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036575313,0.00044259257,0.00030719256,0.00040814915,0.0003894384,0.0003203444,0.00036267182,0.00050935237,0.002586857],"category_scores_gemma":[0.00080119324,0.00028814838,0.0004282911,0.00021389489,0.0007488514,0.0003073736,0.00079813803,0.0008115612,0.000118534175],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027228235,0.0014365215,0.011187807,0.00009138869,0.00005191844,0.00035408625,0.0002320129,0.0025833615,0.9763188,0.00022130676,0.00004878156,0.0047512595],"study_design_scores_gemma":[0.0005412683,0.03544158,0.10094013,0.000039532548,0.0001982302,0.0017738958,0.0008591631,0.008124884,0.85056037,0.00039493377,0.0010753104,0.000050788974],"about_ca_topic_score_codex":0.0009034395,"about_ca_topic_score_gemma":0.0014507731,"teacher_disagreement_score":0.002586857,"about_ca_system_score_codex":0.00020415604,"about_ca_system_score_gemma":0.00012427926,"threshold_uncertainty_score":0.008653939},"labels":[],"label_agreement":null},{"id":"W1905593031","doi":"10.1029/2008gc002272","title":"High <sup>3</sup>He emanations from the source regions of recent large earthquakes, central Japan","year":2008,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC","funders":"","keywords":"Geology; Mantle (geology); Lithosphere; Crust; Seismology; Mantle wedge; Slab; Isotopes of helium; Helium; Subduction; Geophysics; Tectonics","score_opus":0.01647455942023878,"score_gpt":0.1937999429132872,"score_spread":0.1773253834930484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1905593031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99885225,0.00014285861,0.00017639037,0.00003253739,0.0000050811827,0.00000394598,0.00008631205,0.0000064370824,0.00069422595],"genre_scores_gemma":[0.9987704,0.00015395638,0.00027796847,0.000017467744,0.0000064971355,0.0000043841155,0.00018603123,0.0000020804903,0.0005811561],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993336,0.0000053877848,0.000009013639,0.000019330997,0.000014800528,0.000018109102],"domain_scores_gemma":[0.9997539,0.000017264041,0.0000870144,0.000014830734,0.00006889086,0.0000581229],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018815768,0.0003353367,0.00014837937,0.0006716525,0.0006802576,0.00052933313,0.00017696082,0.00022226435,0.000689812],"category_scores_gemma":[0.00023254933,0.00021255351,0.00011092203,0.0008076802,0.0003034689,0.00034061488,0.00047164597,0.0001506033,0.00016721913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021941586,0.00003446579,0.879796,0.00012961177,0.00009761698,0.001791506,0.0016068064,0.0002738906,0.098638825,0.00012536647,0.00037978322,0.016906727],"study_design_scores_gemma":[0.000003601297,0.000025427433,0.99585587,0.0000034823775,0.000031731775,0.00024356977,0.00075170235,0.00012858001,0.0023204728,0.000037402435,0.00059284124,0.000005346419],"about_ca_topic_score_codex":0.015931034,"about_ca_topic_score_gemma":0.051564083,"teacher_disagreement_score":0.015931034,"about_ca_system_score_codex":0.0003792831,"about_ca_system_score_gemma":0.00035233833,"threshold_uncertainty_score":0.03167665},"labels":[],"label_agreement":null},{"id":"W1906122928","doi":"10.1029/2008tc002341","title":"Normal faulting along the southern margin of the Puna Plateau, northwest Argentina","year":2009,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"College of Family Physicians of Canada","funders":"","keywords":"Geology; Plateau (mathematics); Lithosphere; Late Miocene; Paleontology; Tectonics; Extensional definition; Cenozoic; Seismology; Fault (geology); Geomorphology; Structural basin","score_opus":0.012214490190825548,"score_gpt":0.2008539981600891,"score_spread":0.18863950796926354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1906122928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936985,0.000286812,0.00011662078,0.000045232395,0.000007039904,0.000011941899,0.0006685922,0.00002291794,0.0051424038],"genre_scores_gemma":[0.9968477,0.00030882028,0.0003122166,0.000013301329,0.000007633694,0.000017918997,0.0011045682,0.000005053485,0.0013828187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999089,0.000011705998,0.0000073738734,0.000033654822,0.000019212055,0.000019165282],"domain_scores_gemma":[0.9997389,0.000023845907,0.00009300131,0.000019241,0.00008807858,0.0000370198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016307457,0.0002197903,0.00017962592,0.000757512,0.0004659456,0.00060738606,0.00017133793,0.0001482624,0.0015195552],"category_scores_gemma":[0.00042590674,0.00013373334,0.00008123197,0.0009560128,0.0003367447,0.00024224208,0.00037746193,0.0001350909,0.00019663884],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017002871,0.00006804902,0.9560297,0.000097270306,0.000033679193,0.0005039142,0.0011457752,0.00079737196,0.007745538,0.00034053158,0.0008268,0.032241315],"study_design_scores_gemma":[0.000006440347,0.000019354615,0.99782085,0.000010080774,0.0000041652575,0.00011723868,0.00022834048,0.00015694165,0.00007033479,0.000030217314,0.0015338368,0.0000022178972],"about_ca_topic_score_codex":0.06117603,"about_ca_topic_score_gemma":0.16264825,"teacher_disagreement_score":0.06117603,"about_ca_system_score_codex":0.00042478315,"about_ca_system_score_gemma":0.00048400916,"threshold_uncertainty_score":0.12163991},"labels":[],"label_agreement":null},{"id":"W1906986918","doi":"","title":"Neogene sedimentary history of the Cilicia Basin, eastern Mediterranean","year":2013,"lang":"en","type":"dissertation","venue":"Memorial University Research Repository (Memorial University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Structural basin; Sedimentary rock; Sedimentary depositional environment; Neogene; Fold and thrust belt; Paleontology; Late Miocene; Sedimentary basin; Tectonics; Geomorphology; Geochemistry; Foreland basin","score_opus":0.03359094118362984,"score_gpt":0.2276640763171906,"score_spread":0.19407313513356075,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1906986918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99851924,0.00022816712,0.000026035234,0.000016754044,0.000002264243,0.0000031181276,0.00012266857,0.0000059832914,0.0010757694],"genre_scores_gemma":[0.9992223,0.00015068777,0.00008214024,0.000006861736,0.0000031732413,0.000003277176,0.00018757206,0.000002408404,0.00034167396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995375,0.000004007175,0.000005404847,0.00001330501,0.000010613346,0.000012985625],"domain_scores_gemma":[0.999936,0.0000048158354,0.000025051017,0.000005097729,0.000020030782,0.000009092627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012349169,0.00016530012,0.00014761477,0.00089314266,0.0002638884,0.0004086163,0.00020531422,0.0001874391,0.0006221487],"category_scores_gemma":[0.000293372,0.00009182001,0.00016082989,0.0006297757,0.00026839555,0.00017061539,0.0003497339,0.00006310144,0.00013859766],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018311212,0.000029466764,0.9496093,0.00009232181,0.00006448574,0.00093766727,0.0019565115,0.0007398985,0.010105332,0.00029261515,0.0004007155,0.035588674],"study_design_scores_gemma":[0.0000031378434,0.000008182451,0.998869,0.000004731387,0.000004389979,0.00005502333,0.00015121802,0.00010350648,0.00008638868,0.000011475061,0.00070185197,0.0000010828512],"about_ca_topic_score_codex":0.026871888,"about_ca_topic_score_gemma":0.046743575,"teacher_disagreement_score":0.026871888,"about_ca_system_score_codex":0.0010971898,"about_ca_system_score_gemma":0.00037640423,"threshold_uncertainty_score":0.053430974},"labels":[],"label_agreement":null},{"id":"W1907162398","doi":"10.1002/2015gl064377","title":"Isolated cases of remote dynamic triggering in Canada detected using cataloged earthquakes combined with a matched‐filter approach","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Waveform; Shock (circulatory); Filter (signal processing); Statistical analysis; Statistics","score_opus":0.05271104119515374,"score_gpt":0.2657852839870638,"score_spread":0.21307424279191006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1907162398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995148,0.00010871781,0.00071419234,0.00003170925,0.0000034056175,0.000025395017,0.0018037474,0.000052265455,0.0021126065],"genre_scores_gemma":[0.99754506,0.00006327099,0.0005397587,0.000012678816,0.0000021197118,0.0000049427067,0.0012286686,0.000004609061,0.0005988055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997017,0.000011681024,0.000015447094,0.00005338151,0.00011501118,0.00010271732],"domain_scores_gemma":[0.9990115,0.000120665,0.00027212562,0.00007636272,0.00031376298,0.00020545235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024426263,0.000233838,0.00020585465,0.0021384107,0.0010178379,0.00068536727,0.00055531267,0.00020599738,0.002114381],"category_scores_gemma":[0.001320081,0.00015076781,0.00022703383,0.0026786227,0.00035007193,0.00015990568,0.00055981125,0.00017425217,0.0001677103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015345846,0.00003210798,0.97123295,0.0000294374,0.00009709447,0.00057652424,0.00028009422,0.0009913496,0.004396097,0.0001299062,0.0007387921,0.021342246],"study_design_scores_gemma":[0.000004995145,0.000019232975,0.99700576,0.0000056298077,0.0000264463,0.00013667968,0.00037427628,0.0011687159,0.00065648305,0.000020557836,0.0005753346,0.0000058704436],"about_ca_topic_score_codex":0.91168433,"about_ca_topic_score_gemma":0.96618193,"teacher_disagreement_score":0.088315666,"about_ca_system_score_codex":0.0029904323,"about_ca_system_score_gemma":0.004451026,"threshold_uncertainty_score":0.17767149},"labels":[],"label_agreement":null},{"id":"W1913679562","doi":"10.1103/physrevlett.106.108501","title":"New Approach to Gutenberg-Richter Scaling","year":2011,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"U.S. Department of Energy","keywords":"Scaling; Exponent; Statistical physics; Physics; Lattice (music); Fault (geology); Critical exponent; Mathematics; Geology; Geometry; Seismology","score_opus":0.051490212892950006,"score_gpt":0.25372466919318026,"score_spread":0.20223445630023026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1913679562","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10102628,0.0042782263,0.7315998,0.007493463,0.0017951615,0.00013162942,0.00050711166,0.0008841123,0.15228423],"genre_scores_gemma":[0.83082193,0.002538448,0.13476846,0.0026366662,0.0030055023,0.0004117145,0.0002681501,0.00039963317,0.025149416],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9994004,0.00020683598,0.000027382519,0.00010721876,0.00018298911,0.0000751929],"domain_scores_gemma":[0.99891424,0.00036479323,0.00013884401,0.0002636508,0.00017289836,0.00014558557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011043204,0.00081276346,0.001210563,0.0021082717,0.0010082672,0.0016951092,0.001442427,0.0016498569,0.004634564],"category_scores_gemma":[0.0037232328,0.0003631967,0.0012743014,0.00090941286,0.00204687,0.0039301864,0.0015224599,0.0022650883,0.0007980144],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000053168646,0.000017183782,0.0001498491,0.000020300306,0.000009634762,0.000077897435,0.000070376474,0.009574013,0.0005952562,0.9860298,0.0015344139,0.001915935],"study_design_scores_gemma":[0.000008063733,0.000015673408,0.000117772855,0.000010025261,0.000003356201,0.00006473756,0.00001878337,0.11197046,0.00013109074,0.88341665,0.004229311,0.000014086903],"about_ca_topic_score_codex":0.0013354911,"about_ca_topic_score_gemma":0.0011382641,"teacher_disagreement_score":0.004634564,"about_ca_system_score_codex":0.0012239278,"about_ca_system_score_gemma":0.00067954324,"threshold_uncertainty_score":0.015504122},"labels":[],"label_agreement":null},{"id":"W1913885649","doi":"10.1002/ggge.20276","title":"The active portion of the Campi Flegrei caldera structure imaged by 3‐D inversion of gravity data","year":2013,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saint Mary's University; St. Mary's University","funders":"","keywords":"Caldera; Geology; Volcano; Seismology; Lineament; Inversion (geology); Tectonics; Geophysics","score_opus":0.00861287177740914,"score_gpt":0.19211390177674922,"score_spread":0.1835010299993401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1913885649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9200887,0.00013177749,0.071503386,0.00019823162,0.000015390393,0.000048533373,0.0016842354,0.0009439684,0.0053857435],"genre_scores_gemma":[0.982463,0.000064043634,0.01611607,0.000015944002,0.000005901757,0.000015537496,0.00082016987,0.000028770535,0.00047069654],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999647,0.0000029142604,0.0000011634047,0.000012838518,0.000010211093,0.00000810412],"domain_scores_gemma":[0.99996245,0.000006427683,0.0000060930297,0.000008921776,0.000009296344,0.000006847168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007960884,0.000325528,0.00013850241,0.00054041605,0.000120273224,0.0004563194,0.00039569248,0.0003164339,0.000572228],"category_scores_gemma":[0.000199077,0.00021058026,0.0003206105,0.00038874257,0.00019247088,0.00018948474,0.0002829649,0.00027734315,0.00017212161],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013004502,0.00012390321,0.10812372,0.00007586848,0.00012371784,0.0007603076,0.0004643403,0.7120935,0.0927292,0.0034944243,0.0025389174,0.07934209],"study_design_scores_gemma":[0.00002505012,0.000015985404,0.055554807,0.00001248989,0.000020791871,0.0001417491,0.000050208506,0.93875957,0.0033257022,0.0004492653,0.0016259212,0.000018515966],"about_ca_topic_score_codex":0.046055347,"about_ca_topic_score_gemma":0.041510113,"teacher_disagreement_score":0.046055347,"about_ca_system_score_codex":0.00058448804,"about_ca_system_score_gemma":0.0005282409,"threshold_uncertainty_score":0.09157455},"labels":[],"label_agreement":null},{"id":"W1915783104","doi":"10.1002/2014jb011385","title":"Spatiotemporal changes, faulting regimes, and source parameters of induced seismicity: A case study from The Geysers geothermal field","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Helmholtz-Alberta Initiative; Helmholtz-Gemeinschaft","keywords":"Induced seismicity; Geothermal gradient; Hypocenter; Geology; Pore water pressure; Poromechanics; Slip (aerodynamics); Injection well; Hydraulic fracturing; Seismology; Fault (geology); Hydrogeology; Petrology; Geotechnical engineering; Geophysics; Petroleum engineering","score_opus":0.067117975632054,"score_gpt":0.32099736891729513,"score_spread":0.2538793932852411,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1915783104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994523,0.000016085327,0.00008041851,0.0000072950093,3.9365693e-7,0.000006091722,0.00015965657,0.000010055205,0.00026766653],"genre_scores_gemma":[0.9988649,0.000038493068,0.0004063308,0.0000031707425,0.000002084558,0.0000050093445,0.00041765065,0.0000029244281,0.00025936466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990916,0.000011170136,0.0000061554183,0.000025452939,0.000024707528,0.000023288356],"domain_scores_gemma":[0.9997515,0.000068748086,0.00007737158,0.000025008518,0.00004539211,0.00003192345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019789433,0.00022689623,0.00016169838,0.0011421046,0.00033374998,0.00029914483,0.00025991965,0.00024003447,0.0005389166],"category_scores_gemma":[0.00045534302,0.00011805894,0.00018620072,0.0010241542,0.00037960292,0.00018164607,0.00026952798,0.00013967202,0.000052996333],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002806868,0.00022124783,0.9217567,0.00011702709,0.00012340747,0.00774771,0.0023557267,0.02286586,0.021846522,0.00035172436,0.0010355678,0.021297844],"study_design_scores_gemma":[0.00001929647,0.00007547471,0.9877303,0.000009435,0.00003187433,0.0003245169,0.0010112986,0.00846281,0.0015962682,0.00004741975,0.00067769166,0.000013587929],"about_ca_topic_score_codex":0.10248698,"about_ca_topic_score_gemma":0.19921736,"teacher_disagreement_score":0.10248698,"about_ca_system_score_codex":0.0006800454,"about_ca_system_score_gemma":0.0004304383,"threshold_uncertainty_score":0.20378083},"labels":[],"label_agreement":null},{"id":"W1916254573","doi":"10.1002/2013gc005031","title":"Imaging slow slip fronts in Cascadia with high precision cross‐station tremor locations","year":2013,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Coda; Arrival time; Geodesy; Front (military); Slip (aerodynamics); Episodic tremor and slip; Waveform; Subduction; Tectonics; Computer science; Physics; Telecommunications","score_opus":0.006224760792897365,"score_gpt":0.1974436293297586,"score_spread":0.19121886853686124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1916254573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9707581,0.00015832284,0.02095053,0.00011750888,0.000026218302,0.000048605452,0.0011456277,0.00073822954,0.006056863],"genre_scores_gemma":[0.96927714,0.00013427003,0.027834814,0.000019021269,0.000026313917,0.000039772975,0.0009280718,0.000072503746,0.0016680951],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984515,0.000009709937,0.000006549952,0.00004561556,0.00006752385,0.00002533067],"domain_scores_gemma":[0.9994079,0.000058079513,0.00009343139,0.00007776554,0.00027889071,0.000083995794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002744654,0.00033205678,0.00019475965,0.00189803,0.00039137673,0.0005311417,0.00032650548,0.00024902113,0.0012902508],"category_scores_gemma":[0.0008980356,0.00029173362,0.00015583755,0.00095638,0.00016998696,0.00022814442,0.0006848335,0.00026575453,0.00035363308],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036632322,0.00012975432,0.4643924,0.00019912774,0.0002534969,0.00092238636,0.001835655,0.01460515,0.31768,0.00047488284,0.002145086,0.19699568],"study_design_scores_gemma":[0.00005050388,0.00011699792,0.9324848,0.000021397562,0.00007323708,0.00042052206,0.00040964616,0.04509039,0.01727584,0.00020470622,0.0038108372,0.000041172647],"about_ca_topic_score_codex":0.043466114,"about_ca_topic_score_gemma":0.1495172,"teacher_disagreement_score":0.043466114,"about_ca_system_score_codex":0.0004378859,"about_ca_system_score_gemma":0.0006237568,"threshold_uncertainty_score":0.08642626},"labels":[],"label_agreement":null},{"id":"W1916618959","doi":"10.1193/010915eqs005m","title":"Estimating Annualized Earthquake Losses for the Conterminous United States","year":2015,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hillsborough Hospital","funders":"U.S. Geological Survey","keywords":"Census; Geography; Seismic hazard; Population; Magnitude (astronomy); Environmental science; Seismology; Geology; Demography","score_opus":0.04011668683775079,"score_gpt":0.2652407644302182,"score_spread":0.22512407759246741,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1916618959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9823745,0.00020055022,0.004209532,0.00015364903,0.000013564943,0.00003299158,0.0056768074,0.0000770307,0.0072612735],"genre_scores_gemma":[0.98963964,0.00021328949,0.0025794324,0.000025260351,0.000010537344,0.000045310724,0.006220417,0.000013582112,0.0012526265],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99978477,0.000041924697,0.000023091141,0.000038027316,0.00008921028,0.000022876164],"domain_scores_gemma":[0.9990959,0.00015475035,0.00033268685,0.00006553817,0.00031559228,0.00003552577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003942859,0.00029879337,0.00011415417,0.00205424,0.00016120113,0.00046774678,0.00027862508,0.00013809506,0.0008209375],"category_scores_gemma":[0.0026805943,0.00014925504,0.00017822253,0.001278906,0.000110913774,0.0006321453,0.0005129769,0.00024332608,0.0001707757],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006542902,0.000062148734,0.8993739,0.000042550553,0.00016999473,0.00013139682,0.00033855563,0.05045096,0.00077158696,0.0017864072,0.0054655354,0.041341424],"study_design_scores_gemma":[0.0000060699795,0.00007022178,0.92631084,0.00003565304,0.000048650993,0.00015809396,0.00057620084,0.0627839,0.0010086962,0.0010336216,0.007947167,0.000020919084],"about_ca_topic_score_codex":0.031915512,"about_ca_topic_score_gemma":0.045354202,"teacher_disagreement_score":0.031915512,"about_ca_system_score_codex":0.0007695771,"about_ca_system_score_gemma":0.0003036052,"threshold_uncertainty_score":0.063459516},"labels":[],"label_agreement":null},{"id":"W1918123779","doi":"10.1029/2003tc001585","title":"Response of the tectonically erosive south Peruvian forearc to subduction of the Nazca Ridge: Analysis of three‐dimensional analogue experiments","year":2004,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Leibniz-Gemeinschaft; Deutsche Forschungsgemeinschaft","keywords":"Forearc; Geology; Subduction; Ridge; Seismology; Accretionary wedge; Wedge (geometry); Ridge push; Tectonics; Paleontology; Geometry","score_opus":0.023957659175399656,"score_gpt":0.2390452260695753,"score_spread":0.21508756689417563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1918123779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996346,0.000009054335,0.00020513943,0.0000037906814,4.9383425e-7,0.0000032199334,0.00003036349,0.0000067057354,0.00010669404],"genre_scores_gemma":[0.9995505,0.000018570421,0.0002731523,0.000003509506,6.034527e-7,0.0000075850962,0.000070897186,0.0000027084466,0.00007247852],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994946,0.000012277852,0.0000035138814,0.000013320316,0.000009131768,0.000012351758],"domain_scores_gemma":[0.99974793,0.00009207481,0.000051763054,0.000052853396,0.000024643658,0.000030718504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016080581,0.00014135784,0.00018922205,0.00021354521,0.00013887441,0.00027818477,0.00021503858,0.00026020777,0.00090144674],"category_scores_gemma":[0.0005591772,0.00015075876,0.00024342797,0.00017304083,0.00025483678,0.000099897254,0.00023210607,0.0001969387,0.000057580113],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011636851,0.00043729824,0.08625128,0.00011673315,0.0001365642,0.00037000567,0.00025358566,0.036069795,0.8670621,0.00042029604,0.00011631541,0.00760241],"study_design_scores_gemma":[0.00014067598,0.0018622088,0.6446707,0.00000993284,0.00010597525,0.00025374402,0.0002472495,0.19950934,0.15169702,0.0003466206,0.0010976486,0.000058854148],"about_ca_topic_score_codex":0.0029219838,"about_ca_topic_score_gemma":0.0024009405,"teacher_disagreement_score":0.0029219838,"about_ca_system_score_codex":0.00027503853,"about_ca_system_score_gemma":0.000101143625,"threshold_uncertainty_score":0.0058099627},"labels":[],"label_agreement":null},{"id":"W1918781448","doi":"10.1002/2015gl065402","title":"The Iquique earthquake sequence of April 2014: Bayesian modeling accounting for prediction uncertainty","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Southern California Earthquake Center","keywords":"Aftershock; Geology; Foreshock; Seismology; Subduction; Slip (aerodynamics); Geodetic datum; Seismic gap; Trench; Shock (circulatory); Geodesy; Tectonics; Induced seismicity","score_opus":0.08324452757035668,"score_gpt":0.3137374505010344,"score_spread":0.23049292293067775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1918781448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7066272,0.0005305554,0.2838349,0.0018086625,0.000053467447,0.00008850546,0.00089322584,0.00029994853,0.0058635743],"genre_scores_gemma":[0.986541,0.00017542968,0.010544977,0.000074437114,0.00005618471,0.00005656686,0.00033889338,0.000028748605,0.0021838034],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995647,0.00020684199,0.000018356413,0.000096638425,0.000053315696,0.000060136037],"domain_scores_gemma":[0.9965868,0.0025967695,0.00037739018,0.00010058158,0.00023339664,0.000104942985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002957609,0.0005879407,0.0008543664,0.0007599486,0.0005894846,0.0012838978,0.0013645646,0.0012729076,0.0014932937],"category_scores_gemma":[0.007608515,0.0007755473,0.0008236176,0.00053831673,0.0006624792,0.0012517049,0.0007578373,0.0010665541,0.00020359734],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056813904,0.00003275199,0.0055932184,0.000013471135,0.000047412697,0.000047100606,0.00005146001,0.9806029,0.00019873906,0.0068731494,0.00039139605,0.006091425],"study_design_scores_gemma":[0.0000046421824,0.0000054497555,0.0006667041,0.00000255133,0.000005594379,0.000003496786,0.000004969892,0.99744654,0.000019047491,0.0017743097,0.00006226063,0.0000044417807],"about_ca_topic_score_codex":0.062112853,"about_ca_topic_score_gemma":0.039218098,"teacher_disagreement_score":0.062112853,"about_ca_system_score_codex":0.0013590332,"about_ca_system_score_gemma":0.001094153,"threshold_uncertainty_score":0.12350267},"labels":[],"label_agreement":null},{"id":"W1919391388","doi":"10.1130/2007.2425(06)","title":"Remotely triggered earthquakes following moderate main shocks","year":2007,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Intraplate earthquake; Geology; Aftershock; Remotely triggered earthquakes; Induced seismicity; Volcano; Earthquake swarm; Tectonics; Geothermal gradient; Seismic gap; Depth of focus (tectonics); Geophysics; Subduction","score_opus":0.04205080467832955,"score_gpt":0.23609686238025174,"score_spread":0.19404605770192218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1919391388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99735034,0.00027601793,0.00036238995,0.000023250303,0.000005481174,0.000010790196,0.0002619958,0.000031047457,0.0016786788],"genre_scores_gemma":[0.9993894,0.0000984986,0.000118426244,0.000017103763,0.000010138236,0.0000025788856,0.00023335984,0.0000017977222,0.00012867017],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998764,0.000010262006,0.000011194573,0.000041098905,0.00003303108,0.000028014407],"domain_scores_gemma":[0.9991948,0.00009246258,0.0005103472,0.000055406934,0.000052517047,0.000094447416],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013503873,0.00014304392,0.0001877951,0.0004725235,0.00017560973,0.00028076908,0.00021713928,0.00029854706,0.001249193],"category_scores_gemma":[0.0008012368,0.000095511314,0.00014302947,0.00036978064,0.00023104844,0.0002521711,0.0005444208,0.00022649548,0.00020736977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007044114,0.00008898249,0.902594,0.00025817176,0.00015723555,0.0023293658,0.0015846953,0.0010330515,0.05131581,0.00027158958,0.0008723458,0.03879047],"study_design_scores_gemma":[0.0000060647017,0.00011083346,0.9981908,0.000010437783,0.000012216733,0.00031715928,0.00016801798,0.000078685836,0.00062049116,0.00004527256,0.0004346972,0.0000052959],"about_ca_topic_score_codex":0.0021130112,"about_ca_topic_score_gemma":0.0040778997,"teacher_disagreement_score":0.0021130112,"about_ca_system_score_codex":0.00022003434,"about_ca_system_score_gemma":0.00007896519,"threshold_uncertainty_score":0.0042013526},"labels":[],"label_agreement":null},{"id":"W1920914286","doi":"10.1002/jgrb.50181","title":"Annual modulation of non‐volcanic tremor in northern Cascadia","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Subduction; Seismology; Crust; Volcano; Shear (geology); Continental crust; Oceanic crust; Oceanography; Paleontology; Tectonics","score_opus":0.028777753506722164,"score_gpt":0.3020246454097679,"score_spread":0.27324689190304574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1920914286","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965642,0.00011709393,0.000051225292,0.00008281045,0.0000063308044,0.000004268764,0.0008294553,0.00004720846,0.002297437],"genre_scores_gemma":[0.99890447,0.000079014404,0.000030710857,0.000008311759,0.0000043101186,0.000004236423,0.0005984036,0.000005784134,0.00036483054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984586,0.000012107835,0.000014598388,0.00005427364,0.00003534699,0.000037760616],"domain_scores_gemma":[0.9991779,0.000053605443,0.0002061787,0.000060134553,0.00018874029,0.00031344077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018521708,0.00029686312,0.00024302305,0.001665242,0.0007389157,0.0006930573,0.00032522398,0.000268404,0.0021987183],"category_scores_gemma":[0.0010354015,0.00023010357,0.0002470347,0.0014236341,0.0004454247,0.00019960024,0.00075678725,0.0002161068,0.00032380302],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010625634,0.000026102462,0.98565036,0.00006863978,0.000100770856,0.00044825167,0.0013170748,0.0013692896,0.004023029,0.00009708467,0.0012043987,0.0055887555],"study_design_scores_gemma":[0.0000013071068,0.0000032301602,0.9992735,0.0000041270864,0.0000052609385,0.000019741328,0.000150273,0.00019798407,0.000029325114,0.000009503925,0.0003030296,0.0000027927367],"about_ca_topic_score_codex":0.3061396,"about_ca_topic_score_gemma":0.49335942,"teacher_disagreement_score":0.6938604,"about_ca_system_score_codex":0.0020280173,"about_ca_system_score_gemma":0.0010681933,"threshold_uncertainty_score":0.6087153},"labels":[],"label_agreement":null},{"id":"W1929992685","doi":"10.1002/2013jb010564","title":"Multifaulting in a tectonic syntaxis revealed by InSAR: The case of the Ziarat earthquake sequence (Pakistan)","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Safran Electronics (Canada)","funders":"","keywords":"Geology; Seismology; Sinistral and dextral; Interferometric synthetic aperture radar; Tectonics; Fault (geology); Strike-slip tectonics; Slip (aerodynamics); Shear (geology); Inversion (geology); Geodesy; Synthetic aperture radar; Petrology","score_opus":0.04142221945835021,"score_gpt":0.33755282019037486,"score_spread":0.29613060073202463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1929992685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99865973,0.00004563863,0.00015826024,0.00012187118,0.0000026699402,0.00000484462,0.00013206441,0.000005896771,0.0008690661],"genre_scores_gemma":[0.9996636,0.000025250849,0.00013901682,0.000006423434,0.0000026329433,0.0000011315651,0.00009867137,0.0000013814258,0.00006189359],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998217,0.000025431398,0.000009925693,0.000048905014,0.000032910204,0.00006122731],"domain_scores_gemma":[0.99964786,0.0000762233,0.00014326176,0.000041171337,0.000051912695,0.000039514045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002994133,0.0002844206,0.00018987649,0.0010148905,0.00069381663,0.00097539916,0.00034311676,0.00055260374,0.001105723],"category_scores_gemma":[0.0011696061,0.00024697394,0.0001842555,0.0010549471,0.0009425176,0.0005335278,0.0004961572,0.00036929798,0.000186189],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050305633,0.000110516776,0.8970483,0.000086378175,0.00018786814,0.035565093,0.0025537421,0.017274473,0.020569043,0.005346399,0.0017867974,0.018968368],"study_design_scores_gemma":[0.000041756244,0.00006457066,0.9646341,0.000027130316,0.00007934325,0.0021187812,0.0027797967,0.025956757,0.0015418357,0.00084587693,0.001878137,0.000031782838],"about_ca_topic_score_codex":0.0432609,"about_ca_topic_score_gemma":0.051088713,"teacher_disagreement_score":0.0432609,"about_ca_system_score_codex":0.0009991213,"about_ca_system_score_gemma":0.0003503302,"threshold_uncertainty_score":0.086018205},"labels":[],"label_agreement":null},{"id":"W1931715449","doi":"10.1186/s40623-015-0236-9","title":"Preface for the special issue of “New Perspective of Subduction Zone Earthquakes”","year":2015,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Project 211; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Seismology; Subduction; Geology; Borehole; Trough (economics); Drilling; Scientific drilling; Seismic zone; Plate tectonics; Christian ministry; Tectonics; Induced seismicity; Paleontology; Engineering; Law","score_opus":0.02935545932859488,"score_gpt":0.2419320028681548,"score_spread":0.21257654353955993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1931715449","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00008669137,0.004623623,0.00028459748,0.030846298,0.95564085,0.000054333534,0.00041886274,0.0001611579,0.007883615],"genre_scores_gemma":[0.00056532375,0.0043300525,0.00020203332,0.016063297,0.9390058,0.0000768093,0.0006097679,0.00021250691,0.038934436],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99810326,0.0002511855,0.00022521018,0.00040945038,0.00082913553,0.00018170403],"domain_scores_gemma":[0.9862596,0.0030120262,0.0010031353,0.00062566675,0.006099481,0.0030001404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025625825,0.0031307123,0.002583686,0.004107106,0.0029949227,0.0068561826,0.0028521642,0.0060851686,0.14622755],"category_scores_gemma":[0.013124656,0.0006064094,0.001650695,0.0024761327,0.0012008231,0.0067116437,0.0030348084,0.0078725945,0.087836295],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018408742,0.000008798084,0.000039667895,0.00008804199,0.0000028659053,0.000029601135,0.000009888113,0.000010748451,0.000051870473,0.00017556142,0.9943364,0.005228154],"study_design_scores_gemma":[0.0000115020575,0.000019057274,0.0004266291,0.00015862679,0.0000065267677,0.00009174373,0.000032126307,0.00005851207,0.00004185982,0.0005557358,0.998589,0.000008611407],"about_ca_topic_score_codex":0.0017923061,"about_ca_topic_score_gemma":0.0025143307,"teacher_disagreement_score":0.14622755,"about_ca_system_score_codex":0.0019726774,"about_ca_system_score_gemma":0.0020416714,"threshold_uncertainty_score":0.4891799},"labels":[],"label_agreement":null},{"id":"W1932852026","doi":"10.1306/m82813c23","title":"Numerical Modeling of Hinge-zone Migration in Fault-bend Folds","year":2004,"lang":"en","type":"book-chapter","venue":"American Association of Petroleum Geologists eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Thrust; Thrust fault; Fold and thrust belt; Nappe; Tectonics; Geodynamics; Hydrocarbon exploration; Inversion (geology); Fault (geology); Seismology; Foreland basin; Paleontology; Geomorphology; Engineering","score_opus":0.01409672732601968,"score_gpt":0.21688473231904745,"score_spread":0.20278800499302777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1932852026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.73739594,0.0013269929,0.2097652,0.0012905138,0.00033654377,0.00010335789,0.0007990113,0.0006962009,0.04828627],"genre_scores_gemma":[0.9810534,0.00028423526,0.0103847515,0.00004786427,0.000031338615,0.000051657753,0.0001744542,0.00006621547,0.007905992],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987066,0.00003960556,0.00001077381,0.000020075484,0.000027353557,0.000031653908],"domain_scores_gemma":[0.99953103,0.00027815925,0.00005485393,0.000026066462,0.00006564492,0.00004433509],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003741095,0.00043136746,0.0006672808,0.000494319,0.00065664813,0.0012306918,0.0010453027,0.0013445773,0.0030889385],"category_scores_gemma":[0.0014834342,0.00049446773,0.0005297394,0.00063076,0.0010094369,0.00065851636,0.0008273926,0.00078104634,0.00027188903],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013212199,0.000008707341,0.0005299405,0.0000070785923,0.000004902964,0.000023066008,0.000021302849,0.9961577,0.00022189759,0.0018477918,0.00011759553,0.0010468968],"study_design_scores_gemma":[0.0000030086335,0.000003653723,0.000115058676,0.000002014161,0.0000012646416,0.0000033758847,0.000009444727,0.9990707,0.00004922263,0.00057121995,0.00016937501,0.0000016705181],"about_ca_topic_score_codex":0.029047118,"about_ca_topic_score_gemma":0.015625251,"teacher_disagreement_score":0.029047118,"about_ca_system_score_codex":0.0014361284,"about_ca_system_score_gemma":0.00090354023,"threshold_uncertainty_score":0.057756126},"labels":[],"label_agreement":null},{"id":"W1947572410","doi":"10.1111/j.1365-246x.2011.04972.x","title":"Combining double-difference relocation with regional depth-phase modelling to improve hypocentre accuracy","year":2011,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; Western University","funders":"","keywords":"Relocation; Geology; Earthquake location; Seismology; Induced seismicity; Seismic hazard; Geodesy; Tectonics; Focal mechanism; Computer science","score_opus":0.06459993677822219,"score_gpt":0.26756642003699144,"score_spread":0.20296648325876926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1947572410","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.015050858,0.000027052854,0.98394394,0.000029401072,0.000017405426,0.000019421843,0.000025261716,0.00033389812,0.00055270834],"genre_scores_gemma":[0.31494367,0.00006655826,0.6835359,0.00003487891,0.000015936566,0.00007478161,0.00010626389,0.00023189248,0.0009901957],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997416,0.000074387,0.000023322322,0.000056878536,0.00007737849,0.000026399968],"domain_scores_gemma":[0.99918133,0.00033502176,0.00013572206,0.00016146978,0.00015411993,0.000032413922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007535097,0.00086436316,0.00062208227,0.0005583636,0.00021262809,0.00069147494,0.0013994911,0.00070040603,0.0012467798],"category_scores_gemma":[0.0030681766,0.0005662612,0.0006065663,0.0005658102,0.00036239048,0.0011327012,0.0011090962,0.0006873711,0.00037948837],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008019171,0.00005329006,0.0030079582,0.00009704475,0.000044101933,0.00013007502,0.00017830072,0.8793491,0.027384626,0.0072025135,0.0005251181,0.08194771],"study_design_scores_gemma":[0.00000949784,0.000015454214,0.00012746773,0.0000030397186,0.000004252066,0.000024050272,0.000008209072,0.9958054,0.0026384047,0.00066585565,0.0006904138,0.000007825409],"about_ca_topic_score_codex":0.0060912883,"about_ca_topic_score_gemma":0.007712587,"teacher_disagreement_score":0.0060912883,"about_ca_system_score_codex":0.0004437723,"about_ca_system_score_gemma":0.00096200086,"threshold_uncertainty_score":0.012111664},"labels":[],"label_agreement":null},{"id":"W1949250275","doi":"10.1029/2007gc001721","title":"Crustal motion in the zone of the 1960 Chile earthquake: Detangling earthquake‐cycle deformation and forearc‐sliver translation","year":2007,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":151,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Universidad de Magallanes","keywords":"Geology; Forearc; Seismology; Subduction; Earthquake rupture; Geodynamics; Pacific Plate; Interplate earthquake; Plate tectonics; Intraplate earthquake; Deformation (meteorology); Remotely triggered earthquakes; Seismic hazard; Fault (geology); Geodesy; Tectonics; Seismic gap","score_opus":0.010576720094587617,"score_gpt":0.19667892849720978,"score_spread":0.18610220840262215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1949250275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983267,0.00016265504,0.00012411583,0.000042149106,0.000001968845,0.0000033739177,0.00011756152,0.000010130054,0.0012113316],"genre_scores_gemma":[0.99964297,0.0000570467,0.00004983043,0.0000030775752,0.0000014306186,0.0000017845541,0.0000961303,0.0000021406074,0.00014564383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996006,0.00000534809,0.0000043801792,0.000010222698,0.0000065158515,0.000013428169],"domain_scores_gemma":[0.99989676,0.000013885439,0.00004302889,0.000010966607,0.000010865908,0.000024454914],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010968175,0.00018106349,0.000120712466,0.00062376243,0.00015576046,0.0003331914,0.00014719802,0.0001979721,0.0012418145],"category_scores_gemma":[0.0005682969,0.00016865709,0.00027555297,0.0005370247,0.00025230387,0.00024526517,0.00049781054,0.00014815103,0.0001675725],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036879443,0.000048119105,0.8934442,0.00011195467,0.000112047164,0.0014748429,0.0015143444,0.014686119,0.05805135,0.00080466346,0.00055838446,0.028825136],"study_design_scores_gemma":[0.00000876723,0.000019322528,0.9960925,0.000007429632,0.000008123424,0.00009265725,0.0001530931,0.00271156,0.00048306785,0.00009873128,0.00031778496,0.0000070585675],"about_ca_topic_score_codex":0.025743412,"about_ca_topic_score_gemma":0.020745294,"teacher_disagreement_score":0.025743412,"about_ca_system_score_codex":0.00056293095,"about_ca_system_score_gemma":0.0002493364,"threshold_uncertainty_score":0.051187158},"labels":[],"label_agreement":null},{"id":"W1949314878","doi":"10.1002/grl.50310","title":"Eroding dynamic topography","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institute for Advanced Research","keywords":"Subaerial; Geology; Ocean surface topography; Mantle (geology); Downwelling; Sedimentary rock; Upwelling; Geomorphology; Fluvial; Geophysics; Paleontology; Structural basin; Oceanography","score_opus":0.0306353516950081,"score_gpt":0.2825138250641117,"score_spread":0.25187847336910363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1949314878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920427,0.00009293337,0.0033101074,0.000064599255,0.0000056354224,0.0000037374687,0.000080558246,0.00005152935,0.0043482147],"genre_scores_gemma":[0.9984856,0.000062503525,0.00036431014,0.000011196309,0.000003935818,0.0000013892785,0.00004752896,0.000009686936,0.0010139268],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999399,0.0000047295625,0.000003159715,0.000017478127,0.000011929612,0.00002276104],"domain_scores_gemma":[0.9997638,0.000031925123,0.000069200505,0.00006117287,0.000054887634,0.000018921213],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000072257026,0.0001380682,0.0001283913,0.00034161226,0.00012649545,0.00048413512,0.00017385418,0.00018570924,0.0016956822],"category_scores_gemma":[0.0005541896,0.00012863333,0.00009930696,0.0003465609,0.0002814152,0.00034138077,0.00046280955,0.00020377875,0.00021842628],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021643985,0.000056628956,0.29992732,0.00008531022,0.00008241154,0.0013790634,0.0010624788,0.011937983,0.5241436,0.0075314017,0.0015172388,0.15206018],"study_design_scores_gemma":[0.000015458165,0.00008817013,0.96330285,0.00001259681,0.000031791144,0.0011553229,0.0004431805,0.0115349535,0.015107734,0.0017278116,0.00655926,0.000020979443],"about_ca_topic_score_codex":0.0025280952,"about_ca_topic_score_gemma":0.0026249853,"teacher_disagreement_score":0.0025280952,"about_ca_system_score_codex":0.00022802329,"about_ca_system_score_gemma":0.00013167082,"threshold_uncertainty_score":0.0056726336},"labels":[],"label_agreement":null},{"id":"W1958797316","doi":"10.1002/grl.50899","title":"Tomographic image of melt storage beneath Askja Volcano, Iceland using local microseismicity","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Met Office; Natural Environment Research Council; Research Councils UK; Sight Research UK","keywords":"Geology; Sill; Volcano; Seismology; Magma; Magma chamber; Anomaly (physics); Caldera; Microseism; Petrology; Geophysics","score_opus":0.030791998918483044,"score_gpt":0.2742944400470217,"score_spread":0.24350244112853864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1958797316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99138016,0.00006371195,0.00075511076,0.00004701065,0.0000046712944,0.000026761425,0.0037235597,0.00013005346,0.003868885],"genre_scores_gemma":[0.9948355,0.00007665719,0.00212975,0.000013428394,0.000011582592,0.000015714992,0.0023796847,0.000018783698,0.0005188948],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999789,0.0000013099933,0.000001270852,0.000006002075,0.0000050656427,0.000007484357],"domain_scores_gemma":[0.99993443,0.000008008698,0.0000158069,0.000005575733,0.000016717047,0.000019390267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000053152624,0.00017468154,0.00010470401,0.0010255373,0.00020994795,0.0003733117,0.00016050373,0.00016566462,0.0013514381],"category_scores_gemma":[0.000095919946,0.000119606324,0.0001857891,0.0006183715,0.00015648917,0.00013208014,0.00020618958,0.00012018528,0.00019366542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007590632,0.00025966,0.7167055,0.0002705014,0.00020376944,0.0015374146,0.0020122528,0.038331848,0.15395357,0.00096485106,0.006126157,0.07887547],"study_design_scores_gemma":[0.000016031343,0.000022448467,0.9842367,0.000015633042,0.000026542559,0.000120114055,0.0002625166,0.0125989,0.0017417907,0.000042924687,0.0009097952,0.0000066985926],"about_ca_topic_score_codex":0.038196005,"about_ca_topic_score_gemma":0.07616756,"teacher_disagreement_score":0.038196005,"about_ca_system_score_codex":0.00039300814,"about_ca_system_score_gemma":0.0004039532,"threshold_uncertainty_score":0.075947344},"labels":[],"label_agreement":null},{"id":"W1959728552","doi":"10.1002/2013gl058096","title":"Breaking the oceanic lithosphere of a subducting slab: The 2013 Khash, Iran earthquake","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Subduction; Seismology; Lithosphere; Slab; Mantle (geology); Episodic tremor and slip; Interplate earthquake; Oceanic crust; Crust; Mantle wedge; Geophysics; Tectonics","score_opus":0.045208588890498225,"score_gpt":0.2762157134620481,"score_spread":0.23100712457154987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1959728552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993406,0.00003172151,0.00004998954,0.000061335384,0.0000042176925,0.0000032381809,0.00004151648,0.0000032791554,0.0004641708],"genre_scores_gemma":[0.99976,0.00003270141,0.000043733206,0.000012846299,0.0000062823656,0.0000011055433,0.000060839728,4.6804243e-7,0.00008214175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999474,0.0000039477723,0.000003751206,0.000009447355,0.000015251249,0.000020189596],"domain_scores_gemma":[0.9998807,0.000008322763,0.00005120408,0.000009138161,0.000028023398,0.000022601102],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014261642,0.00015660365,0.0001749454,0.00033155698,0.00046124365,0.0003178574,0.00018663568,0.00024814537,0.00046065619],"category_scores_gemma":[0.0003374099,0.000111274705,0.0001374014,0.00037047488,0.00047514925,0.00025524237,0.00048213135,0.00019951919,0.000113543174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042982356,0.00009619505,0.94641316,0.000057673147,0.00008651426,0.0021157977,0.0018715358,0.0024531751,0.020266982,0.00059410016,0.0014222614,0.024192639],"study_design_scores_gemma":[0.000011272106,0.00005394387,0.99684805,0.0000059385725,0.000017342354,0.0002155994,0.00082566397,0.00077709847,0.0005816889,0.00016499317,0.00049210247,0.0000062446347],"about_ca_topic_score_codex":0.012037029,"about_ca_topic_score_gemma":0.015413223,"teacher_disagreement_score":0.012037029,"about_ca_system_score_codex":0.0006040777,"about_ca_system_score_gemma":0.0005178282,"threshold_uncertainty_score":0.023933947},"labels":[],"label_agreement":null},{"id":"W1960299961","doi":"10.1029/2009gc003019","title":"Pacific‐North America plate boundary reorganization in response to a change in relative plate motion: Offshore Canada","year":2010,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Birds Canada","funders":"","keywords":"Geology; Subduction; Seismology; Plate tectonics; North American Plate; Submarine pipeline; Fault (geology); Strike-slip tectonics; Transform fault; Convergent boundary; Episodic tremor and slip; Pacific Plate; Continental margin; Slip (aerodynamics); Oceanic crust; Tectonics; Oceanography","score_opus":0.007982111628198441,"score_gpt":0.19231611947843213,"score_spread":0.18433400785023368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1960299961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964496,0.00006164855,0.000026120048,0.00006377476,0.00000240565,0.0000065794893,0.0003376593,0.0000056744384,0.0030465887],"genre_scores_gemma":[0.9981287,0.0001150861,0.000064694956,0.000019671266,6.591742e-7,0.0000039588604,0.00030962555,0.000003988997,0.0013535747],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986064,0.000004749427,0.0000042611364,0.000038032085,0.000034616787,0.000057733036],"domain_scores_gemma":[0.99954945,0.00001687399,0.00005684776,0.000016607157,0.0002507954,0.00010943782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010600226,0.00016952597,0.00022771196,0.00080583175,0.0017542152,0.0010646234,0.0005000498,0.0002920729,0.0026641376],"category_scores_gemma":[0.0007470214,0.0002069449,0.00020094514,0.0012833739,0.0006238632,0.00025629118,0.00068281975,0.00031781467,0.00018201933],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003525881,0.00004575985,0.95128566,0.00007272948,0.00010362488,0.00076286716,0.004187435,0.0039706943,0.019396838,0.00091546244,0.0018840377,0.017022265],"study_design_scores_gemma":[0.00000490302,0.0000111829095,0.9943979,0.000009034148,0.000014501464,0.000037189835,0.0025983942,0.00062495837,0.00054123555,0.00004160125,0.0017094106,0.000009797725],"about_ca_topic_score_codex":0.9770772,"about_ca_topic_score_gemma":0.99224323,"teacher_disagreement_score":0.022922814,"about_ca_system_score_codex":0.016571779,"about_ca_system_score_gemma":0.01081927,"threshold_uncertainty_score":0.12023723},"labels":[],"label_agreement":null},{"id":"W1960489672","doi":"10.1002/2014jb011842","title":"Indentor‐corner tectonics in the Yakutat‐St. Elias collision constrained by GPS","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Victoria","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche","keywords":"Geology; Seismology; Transpression; Geodesy; Tectonics; Plate tectonics; Strain rate; Fault (geology); Shear zone; Physics","score_opus":0.0735861886388752,"score_gpt":0.34223329595287827,"score_spread":0.2686471073140031,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1960489672","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990852,0.000023010598,0.000033431945,0.000010013069,8.12809e-7,0.0000017558365,0.00022885713,0.00000404051,0.00061289605],"genre_scores_gemma":[0.9992994,0.00001912903,0.00006751178,0.0000024476797,7.3759844e-7,0.000001969309,0.0003682777,0.0000016740729,0.00023886455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998671,0.000015642383,0.000006784404,0.00003619096,0.000029344745,0.000044996756],"domain_scores_gemma":[0.9997558,0.000034028726,0.000073927295,0.000021283304,0.000068249166,0.000046717803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015110792,0.00015364017,0.00024089654,0.0010164159,0.0005864263,0.00086727296,0.00030791768,0.00020193758,0.0011696841],"category_scores_gemma":[0.00062178884,0.00015144228,0.00011640517,0.0017416915,0.00028172878,0.00021379886,0.00074421545,0.00018583288,0.00012778732],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070975235,0.000016648906,0.9924585,0.0000060256607,0.000019532787,0.00016179396,0.0005666272,0.0021142694,0.0012307942,0.00010897777,0.00014482455,0.0031010392],"study_design_scores_gemma":[0.0000031862585,0.0000059710164,0.99715143,0.0000066852385,0.000005794454,0.000025561309,0.00075948157,0.0015890212,0.00008800248,0.00002651153,0.0003343568,0.000004025907],"about_ca_topic_score_codex":0.36902905,"about_ca_topic_score_gemma":0.61272067,"teacher_disagreement_score":0.36902905,"about_ca_system_score_codex":0.0014648429,"about_ca_system_score_gemma":0.0009881463,"threshold_uncertainty_score":0.73376215},"labels":[],"label_agreement":null},{"id":"W1963613810","doi":"10.1029/2004gl022293","title":"Evidence for melt lubrication during large earthquakes","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lubrication; Slip (aerodynamics); Geology; Melting point; Materials science; Mechanics; Thermodynamics; Composite material; Physics","score_opus":0.09911029649065599,"score_gpt":0.3434663241904369,"score_spread":0.24435602769978088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963613810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996051,0.0001221515,0.00007813075,0.000009516884,0.0000011136997,0.0000011617658,0.000025824958,0.000008342017,0.00014867815],"genre_scores_gemma":[0.9998209,0.00003103335,0.000034749002,0.000003459612,0.000001047896,9.233593e-7,0.00005042737,0.0000017632934,0.000055702556],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9997366,0.000030232657,0.000025967727,0.000044022247,0.000086710206,0.000076366494],"domain_scores_gemma":[0.99889636,0.00018921148,0.0004786099,0.00013432006,0.00020557368,0.000095972435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026459456,0.00020522595,0.0003878309,0.0006505517,0.00031557947,0.0004948739,0.00027165635,0.00051479245,0.00096174784],"category_scores_gemma":[0.0016129507,0.00031350466,0.00019074278,0.00041442676,0.0008396711,0.00031011342,0.000582582,0.00021446403,0.00017842998],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002301061,0.00008671244,0.23671107,0.00023431302,0.000080256956,0.0010085317,0.0014550304,0.0011888145,0.74853826,0.0002830398,0.00014123978,0.00797164],"study_design_scores_gemma":[0.000067623034,0.001021875,0.8673529,0.000016219055,0.000055428784,0.0010979298,0.0004427365,0.0020301796,0.126416,0.0002155094,0.0012576301,0.000025956982],"about_ca_topic_score_codex":0.0023751876,"about_ca_topic_score_gemma":0.0030407754,"teacher_disagreement_score":0.0023751876,"about_ca_system_score_codex":0.00034087442,"about_ca_system_score_gemma":0.00011623979,"threshold_uncertainty_score":0.0047227144},"labels":[],"label_agreement":null},{"id":"W1964249227","doi":"10.1190/tle34010102.1","title":"SEG/SPE/ARMA Injection-induced Seismicity Workshop","year":2014,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Event (particle physics); Petroleum industry; Engineering; Library science; Seismology; Forensic engineering; Operations research; History; Geology; Computer science; Physics","score_opus":0.03444959116790185,"score_gpt":0.24613684452664214,"score_spread":0.21168725335874028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964249227","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.119014844,0.012594946,0.013841581,0.16271873,0.041907344,0.00062429754,0.01008077,0.002165462,0.637052],"genre_scores_gemma":[0.3985114,0.0133661395,0.0069837873,0.010762906,0.009550651,0.0003779414,0.011659035,0.00046115025,0.54832697],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995819,0.000070933296,0.000014011808,0.000043493594,0.00020591871,0.00008375962],"domain_scores_gemma":[0.99917644,0.000089360474,0.00005474439,0.000035656634,0.0003962113,0.00024759842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015623829,0.00054384663,0.00021164549,0.00060515077,0.0012603218,0.0017940345,0.0005592537,0.0017341247,0.0151697965],"category_scores_gemma":[0.0009301973,0.00015297781,0.00043447452,0.0005301173,0.00044162743,0.0004770363,0.0012843895,0.0015802672,0.0046590287],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043652244,0.00020770132,0.0038470675,0.00018291874,0.000037345166,0.0018864867,0.00067022163,0.0019557674,0.009794886,0.0046107234,0.8847003,0.091670096],"study_design_scores_gemma":[0.000030025642,0.00017247284,0.009147645,0.00011945237,0.00001610483,0.00012982903,0.000705847,0.00041472944,0.002696247,0.0012409025,0.98530525,0.000021627442],"about_ca_topic_score_codex":0.015784783,"about_ca_topic_score_gemma":0.04786504,"teacher_disagreement_score":0.015784783,"about_ca_system_score_codex":0.0020602734,"about_ca_system_score_gemma":0.0039778054,"threshold_uncertainty_score":0.05074805},"labels":[],"label_agreement":null},{"id":"W1964780907","doi":"10.1029/2008jb005889","title":"Determination of the pore fluid pressure ratio at seismogenic megathrusts in subduction zones: Implications for strength of asperities and Andean‐type mountain building","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Differential stress; Seismology; Tectonics; Fault (geology); Overburden pressure; Shear (geology); Petrology; Geotechnical engineering; Deformation (meteorology); Oceanography","score_opus":0.03264841920783854,"score_gpt":0.3125409794192086,"score_spread":0.27989256021137005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964780907","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995066,0.00005375723,0.00017482312,0.000008645845,3.260466e-7,0.000001799899,0.000038729337,0.0000052772625,0.0002100644],"genre_scores_gemma":[0.9997589,0.000030636274,0.00015572234,0.0000011129547,5.269237e-7,0.000001390485,0.00003061014,0.0000012220561,0.000020066236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987495,0.0000171333,0.000012151774,0.00004288506,0.000029346907,0.00002356782],"domain_scores_gemma":[0.9994242,0.0001514785,0.00019992169,0.0000514963,0.00009510323,0.000077804936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032477162,0.00023755553,0.00024577737,0.0020324423,0.000317898,0.00058224896,0.00042886002,0.00024466118,0.0006604654],"category_scores_gemma":[0.0016340503,0.00024775745,0.0002442533,0.000987702,0.000545424,0.0005263602,0.00044943814,0.00016471169,0.00011819704],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084667365,0.000043504664,0.9268322,0.000067201465,0.0000788912,0.000286414,0.00045228464,0.006741988,0.056340728,0.00030857476,0.00003446337,0.008729106],"study_design_scores_gemma":[0.000007095808,0.00002045413,0.98359686,0.000005856932,0.000012284415,0.00012409991,0.00021327438,0.011357751,0.004401835,0.00016678586,0.0000837855,0.000009834386],"about_ca_topic_score_codex":0.012608376,"about_ca_topic_score_gemma":0.010496701,"teacher_disagreement_score":0.012608376,"about_ca_system_score_codex":0.0005308656,"about_ca_system_score_gemma":0.00025737376,"threshold_uncertainty_score":0.025069952},"labels":[],"label_agreement":null},{"id":"W1965073820","doi":"10.1029/2005gl022750","title":"Observations of premonitory acoustic emission and slip nucleation during a stick slip experiment in smooth faulted Westerly granite","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Nucleation; Slip (aerodynamics); Acoustic emission; Fault plane; Instability; Geology; Amplitude; Seismology; Waveform; Fault (geology); Acoustics; Mechanics; Physics; Optics","score_opus":0.045302379854108725,"score_gpt":0.29285757180455846,"score_spread":0.24755519195044973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965073820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99962914,0.000024894409,0.00019568087,0.000002405555,8.9972394e-7,0.000003524803,0.00002511846,0.000006875517,0.0001113632],"genre_scores_gemma":[0.9994949,0.0000307293,0.00022029025,0.0000047256726,0.000002387571,0.0000065837808,0.00008409962,0.0000025837373,0.0001535308],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999157,0.000009284623,0.0000035770872,0.000020180585,0.000025780413,0.00002548604],"domain_scores_gemma":[0.99976724,0.00006273326,0.000043846238,0.000018170162,0.00003474873,0.000073176336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001315605,0.00015926064,0.00024637821,0.0002945137,0.00019593177,0.00016614853,0.00015397382,0.00021380783,0.000521931],"category_scores_gemma":[0.00029897603,0.00014447351,0.00010641375,0.00014090686,0.00027166982,0.00008972647,0.00023910619,0.00028381732,0.00011938391],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037270327,0.000044880133,0.013683302,0.000020372656,0.000010520613,0.00020305204,0.00013415955,0.00016805792,0.9831457,0.00002643361,0.00002850609,0.002162225],"study_design_scores_gemma":[0.00004161013,0.0016970416,0.6834238,0.000007532778,0.000025364861,0.00031297267,0.0002352705,0.0030343665,0.31066224,0.00006598749,0.00047484855,0.000018891566],"about_ca_topic_score_codex":0.0014316973,"about_ca_topic_score_gemma":0.0031641736,"teacher_disagreement_score":0.0014316973,"about_ca_system_score_codex":0.00020024895,"about_ca_system_score_gemma":0.0000820387,"threshold_uncertainty_score":0.0028467178},"labels":[],"label_agreement":null},{"id":"W1965075827","doi":"10.1016/j.jog.2004.08.009","title":"Lateral viscosity variations beneath Antarctica and their implications on regional rebound motions and seismotectonics","year":2004,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Ice sheet; Post-glacial rebound; Antarctic ice sheet; Ice stream; Mantle (geology); Geophysics; Induced seismicity; Glacial period; Cryosphere; Seismology; Geomorphology; Sea ice; Climatology","score_opus":0.01577559393046863,"score_gpt":0.2191110187434529,"score_spread":0.20333542481298428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965075827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99783427,0.00021776791,0.000070421505,0.00012459967,0.0000067585343,0.0000025371635,0.0002628647,0.000009925301,0.0014708589],"genre_scores_gemma":[0.9994455,0.00013275813,0.00005840915,0.000013896734,0.0000085509055,0.0000025354022,0.00011343672,0.0000041081726,0.00022077297],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999392,0.000012488424,0.0000059948807,0.000009920868,0.000009406722,0.000023016084],"domain_scores_gemma":[0.9995459,0.0001280714,0.00014198606,0.00004241972,0.00008676554,0.000054829845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017644727,0.0003649594,0.00024309907,0.0017192635,0.0007243721,0.0011537584,0.00027844027,0.0006027662,0.0027207835],"category_scores_gemma":[0.0010650256,0.0003561414,0.00032631037,0.001784682,0.00068885554,0.0008295655,0.00076166977,0.00035751882,0.00043171216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000936124,0.0000794815,0.925839,0.00012264366,0.00017619571,0.0011574117,0.0020728672,0.008544908,0.040853374,0.0010535802,0.0006618906,0.018502519],"study_design_scores_gemma":[0.000012918888,0.000030981522,0.99602604,0.000010532753,0.000035862126,0.00008307097,0.0006558961,0.0018477,0.00055596844,0.0001545927,0.0005741085,0.000012360038],"about_ca_topic_score_codex":0.021028372,"about_ca_topic_score_gemma":0.021106998,"teacher_disagreement_score":0.021028372,"about_ca_system_score_codex":0.0007542162,"about_ca_system_score_gemma":0.00032850754,"threshold_uncertainty_score":0.041811943},"labels":[],"label_agreement":null},{"id":"W1965564510","doi":"10.1016/j.jog.2009.11.005","title":"Fennoscandian strain rates from BIFROST GPS: A gravitating, thick-plate approach","year":2009,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Global Positioning System; Geodesy; Strain (injury); Seismology; Strain rate; Computer science; Anatomy; Medicine","score_opus":0.013608952376374779,"score_gpt":0.23055504477981967,"score_spread":0.2169460924034449,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965564510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9298695,0.0006299754,0.05047752,0.00009733921,0.000039669918,0.00004392115,0.0029921164,0.0003238981,0.015526092],"genre_scores_gemma":[0.9697706,0.00023359712,0.0259605,0.000020524469,0.0000221746,0.000013778965,0.002260999,0.000062870735,0.0016549334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977666,0.000031454383,0.000019287807,0.000078690384,0.00007097933,0.000022851797],"domain_scores_gemma":[0.9996737,0.000066821056,0.000064515836,0.0000617018,0.00011414387,0.000019117679],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047599038,0.000764591,0.00030914575,0.0030607674,0.00035220533,0.0008412825,0.0006383005,0.00035291302,0.0011683628],"category_scores_gemma":[0.0016279133,0.0002733357,0.00026689513,0.0018940594,0.00027523265,0.0006158122,0.00044966763,0.00045158842,0.00034436138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020281841,0.00008362096,0.42138672,0.00014671206,0.00016586314,0.0004862568,0.00032122576,0.32692125,0.018335933,0.0052216416,0.0012491473,0.2254788],"study_design_scores_gemma":[0.000011517753,0.00007226025,0.60089767,0.00005365708,0.00003411855,0.0002654376,0.00027034883,0.39063966,0.003008044,0.0017215807,0.0029605394,0.00006507198],"about_ca_topic_score_codex":0.035958745,"about_ca_topic_score_gemma":0.06430949,"teacher_disagreement_score":0.035958745,"about_ca_system_score_codex":0.0006145756,"about_ca_system_score_gemma":0.00027079214,"threshold_uncertainty_score":0.07149887},"labels":[],"label_agreement":null},{"id":"W1966400405","doi":"10.1007/s00024-014-0797-8","title":"Observed and Modeled Currents from the Tohoku-oki, Japan and other Recent Tsunamis in Northern California","year":2014,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Vancouver Island University","funders":"","keywords":"Bay; Oceanography; Tide gauge; Geology; Acoustic Doppler current profiler; Current (fluid); Amplitude; Seismology; Sea level","score_opus":0.01995938169166161,"score_gpt":0.19312943907795815,"score_spread":0.17317005738629654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966400405","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991078,0.000026694383,0.000035890534,0.000012687265,0.000003195251,0.0000031328727,0.00036814262,0.000011671881,0.0004308331],"genre_scores_gemma":[0.9991503,0.000043110496,0.00006964437,0.0000035151938,0.0000022465595,0.0000042261127,0.0005294206,0.0000018830629,0.00019552131],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992776,0.0000042237543,0.000007809074,0.000028915727,0.000009992378,0.000021210873],"domain_scores_gemma":[0.9997986,0.00003289777,0.00004378063,0.000012513991,0.000061324936,0.000050928822],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012660792,0.00034093164,0.00022038918,0.00049246626,0.00060051633,0.0005233647,0.00040522558,0.0003982651,0.0007184634],"category_scores_gemma":[0.00040244148,0.0002965935,0.0003362861,0.00072342146,0.00031262357,0.00041724238,0.0002906922,0.00029832515,0.00009938218],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006373582,0.00022573638,0.9239121,0.00009361195,0.00021395276,0.0005383729,0.0009101308,0.05801814,0.0058824783,0.00022264142,0.0015111192,0.007834463],"study_design_scores_gemma":[0.000060114035,0.000041685467,0.98138213,0.0000105440995,0.00007571658,0.000042543248,0.00039199443,0.017051073,0.00038010598,0.000033973338,0.0005149842,0.0000151119375],"about_ca_topic_score_codex":0.37129742,"about_ca_topic_score_gemma":0.52309555,"teacher_disagreement_score":0.37129742,"about_ca_system_score_codex":0.0014194971,"about_ca_system_score_gemma":0.0009645287,"threshold_uncertainty_score":0.7382724},"labels":[],"label_agreement":null},{"id":"W1967045330","doi":"10.1016/j.tecto.2014.12.003","title":"Kinematics of Neogene to Recent upper-crustal deformation in the southern Central Andes (23°–28°S) inferred from fault–slip analysis: Evidence for gravitational spreading of the Puna Plateau","year":2014,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Geology; Lithosphere; Seismology; Crust; Kinematics; Neogene; Slip (aerodynamics); Fault (geology); Clockwise; Plateau (mathematics); Geodesy; Tectonics; Geophysics; Paleontology; Geometry; Rotation (mathematics); Structural basin","score_opus":0.037245786162451916,"score_gpt":0.2636226905168882,"score_spread":0.22637690435443628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967045330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994006,0.00003763475,0.000023847548,0.000017529028,0.0000010127068,0.000001913114,0.00007109365,0.0000038364014,0.00044243023],"genre_scores_gemma":[0.9995722,0.000047285066,0.00005447899,0.0000071786158,0.0000015694895,0.0000028861107,0.00011923525,0.0000017344506,0.00019336726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.000013769325,0.000007571161,0.000025008849,0.0000116478,0.00002165909],"domain_scores_gemma":[0.99965453,0.000049622253,0.00010600618,0.000025535577,0.00007099577,0.00009318567],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031218486,0.000218474,0.00017600684,0.0011292966,0.00058799004,0.00071565347,0.0003998362,0.0002501016,0.0014144995],"category_scores_gemma":[0.00065445673,0.0003193284,0.00023240744,0.0012253989,0.00064788805,0.00041136274,0.00064334925,0.0002443686,0.00018100427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017297661,0.000072654424,0.9804174,0.000041259605,0.00006684997,0.000310405,0.002764943,0.0009070175,0.0067812237,0.00024226295,0.00013510119,0.008087953],"study_design_scores_gemma":[0.0000036823333,0.000010237613,0.999385,0.0000024012227,0.000003269795,0.00003337014,0.00019567975,0.0001832575,0.00003982883,0.000015260954,0.00012643628,0.0000016150717],"about_ca_topic_score_codex":0.06379231,"about_ca_topic_score_gemma":0.10672323,"teacher_disagreement_score":0.06379231,"about_ca_system_score_codex":0.0007460464,"about_ca_system_score_gemma":0.00056376617,"threshold_uncertainty_score":0.12684202},"labels":[],"label_agreement":null},{"id":"W1967239144","doi":"10.1103/physreve.77.066104","title":"Networks of recurrent events, a theory of records, and an application to finding causal signatures in seismicity","year":2008,"lang":"en","type":"article","venue":"Physical Review E","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Event (particle physics); Statistical physics; Computer science; Econometrics; Geology; Mathematics; Seismology; Physics; Quantum mechanics","score_opus":0.027229601061863843,"score_gpt":0.28887259803587817,"score_spread":0.26164299697401433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967239144","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.023321748,0.00028976725,0.9732869,0.00034895548,0.000022513172,0.000041133455,0.00025223332,0.00010997494,0.0023267681],"genre_scores_gemma":[0.6149466,0.0015163663,0.37740806,0.00017914329,0.00030530745,0.00045337583,0.0008225382,0.00012490351,0.0042437725],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9985538,0.0005256599,0.00010948929,0.00037845055,0.00034972077,0.00008286088],"domain_scores_gemma":[0.99196553,0.00482289,0.0013269236,0.0009790168,0.0006806267,0.0002249925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025611508,0.00044875962,0.00069369795,0.0038406898,0.00080205564,0.0019516384,0.0016879138,0.00082077755,0.0020813558],"category_scores_gemma":[0.017780624,0.00060106174,0.0011063832,0.0032533198,0.0024102929,0.005006012,0.0014000682,0.0011612666,0.00024744205],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000372112,0.000029963152,0.0035665801,0.00008941831,0.00007163521,0.00016111266,0.00034294708,0.1466605,0.0014083295,0.806591,0.0008174934,0.040223837],"study_design_scores_gemma":[0.000011844847,0.000030210265,0.0014006558,0.000029820032,0.000029312925,0.00013140049,0.00008474837,0.5290148,0.0005331929,0.46599385,0.0027131506,0.000026986698],"about_ca_topic_score_codex":0.0036027657,"about_ca_topic_score_gemma":0.0027310369,"teacher_disagreement_score":0.0038406898,"about_ca_system_score_codex":0.0012323874,"about_ca_system_score_gemma":0.0009857077,"threshold_uncertainty_score":0.0135448575},"labels":[],"label_agreement":null},{"id":"W1967292019","doi":"10.1016/j.margeo.2014.03.010","title":"Establishing a new era of submarine volcanic observatories: Cabling Axial Seamount and the Endeavour Segment of the Juan de Fuca Ridge","year":2014,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"University of Victoria; National Science Foundation","keywords":"Seafloor spreading; Seamount; Geology; Volcano; Ridge; Submarine volcano; Mid-ocean ridge; Hydrosphere; Seismology; Volcanism; Submarine; Lava; Tectonics; Marine geology; Earth science; Paleontology; Oceanography; Biosphere","score_opus":0.010256884252291485,"score_gpt":0.1904320932564723,"score_spread":0.18017520900418083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967292019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9360657,0.004368367,0.0041655675,0.020516628,0.0002846111,0.000049748924,0.00021089734,0.000096751246,0.034241676],"genre_scores_gemma":[0.98979014,0.0005536866,0.0039795125,0.0005422311,0.000097788165,0.000018021152,0.00006961413,0.000016791664,0.0049322164],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993048,0.00015906645,0.000029302299,0.00010693454,0.00014560277,0.00025428517],"domain_scores_gemma":[0.9972965,0.00045665842,0.00033567904,0.00030291447,0.0005373157,0.0010708334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0034828337,0.00012647748,0.00013163316,0.0008908924,0.0021844702,0.0028864476,0.0005814351,0.00080923334,0.0025048186],"category_scores_gemma":[0.0027667352,0.00017321846,0.000116028605,0.00085569674,0.0037292854,0.0023619146,0.0026810225,0.0009392268,0.00010994658],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004290895,0.0001871656,0.4458289,0.00023433301,0.000028553432,0.0013268591,0.05465209,0.00052773627,0.018046869,0.10159414,0.010587345,0.36655688],"study_design_scores_gemma":[0.000022600754,0.00014994916,0.6338782,0.00025605262,0.000012399792,0.00034686134,0.031643875,0.0007259086,0.0014574482,0.0069698305,0.3244914,0.000045478348],"about_ca_topic_score_codex":0.08219189,"about_ca_topic_score_gemma":0.21981278,"teacher_disagreement_score":0.08219189,"about_ca_system_score_codex":0.0031822536,"about_ca_system_score_gemma":0.0140991695,"threshold_uncertainty_score":0.16342694},"labels":[],"label_agreement":null},{"id":"W1968156133","doi":"10.1029/2002jb002188","title":"A three‐dimensional <i>P</i> wave velocity model for the Charlevoix seismic zone, Quebec, Canada","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Precambrian; Tectonics; Crust; Rift; Basement; Geophysics; Paleontology","score_opus":0.04376270343239531,"score_gpt":0.2680212697878023,"score_spread":0.22425856635540697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968156133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4951884,0.0013191421,0.38018227,0.0021253326,0.00018146551,0.00071150705,0.031644937,0.0020845025,0.08656251],"genre_scores_gemma":[0.9043039,0.0008056651,0.0496352,0.00014008481,0.000025894358,0.00038209738,0.00830472,0.00019605483,0.036206424],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990785,0.000010662396,0.0000038662884,0.000019075147,0.000024387875,0.00003420408],"domain_scores_gemma":[0.9998024,0.000023211483,0.000020891579,0.000010128768,0.00011583484,0.000027605252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017006072,0.00064100453,0.0002982566,0.00046243076,0.0011612135,0.0012075756,0.002440715,0.0007317366,0.0037088364],"category_scores_gemma":[0.0005287414,0.00043802347,0.00048035788,0.0008567884,0.00057338976,0.0004406046,0.00039774663,0.00060444983,0.00073942635],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031402105,0.00002309875,0.00560813,0.000020060159,0.000014899371,0.000081059996,0.00005233517,0.9772689,0.00078546227,0.00482151,0.004652523,0.006640574],"study_design_scores_gemma":[0.00001454666,0.0000040357036,0.001653748,0.000006076918,0.0000045462175,0.000008769944,0.000023984852,0.99389255,0.00010190593,0.00048169444,0.0037966112,0.000011401482],"about_ca_topic_score_codex":0.97999156,"about_ca_topic_score_gemma":0.95797604,"teacher_disagreement_score":0.020008445,"about_ca_system_score_codex":0.011162326,"about_ca_system_score_gemma":0.013557481,"threshold_uncertainty_score":0.080988705},"labels":[],"label_agreement":null},{"id":"W1968674045","doi":"10.1016/j.jseaes.2012.06.016","title":"Evolution of the Bababurnu Basin and shelf of the Biga Peninsula: Western extension of the middle strand of the North Anatolian Fault Zone, Northeast Aegean Sea, Turkey","year":2012,"lang":"en","type":"article","venue":"Journal of Asian Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"North Anatolian Fault; Geology; Transtension; Structural basin; Tectonics; Peninsula; Fault (geology); Seismology; Echelon formation; Paleontology; Transform fault; Extensional definition; Geography; Archaeology","score_opus":0.02075668361615385,"score_gpt":0.20858670141587535,"score_spread":0.1878300177997215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968674045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985461,0.00019424203,0.00002786086,0.0000329699,0.0000039761003,0.0000020638481,0.000087759225,0.0000030076965,0.0011021529],"genre_scores_gemma":[0.99939203,0.00009677509,0.000053680276,0.000006156284,0.00000147769,0.00000210402,0.000109596454,0.0000024347032,0.00033580585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.000010672803,0.00000601286,0.000029857776,0.000010303919,0.00002295252],"domain_scores_gemma":[0.9998642,0.000011948394,0.000036402318,0.0000062632544,0.000047171532,0.000033993165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016614204,0.00027259398,0.00019196651,0.0012043966,0.0006616997,0.001104996,0.00033203053,0.00033755935,0.0016596596],"category_scores_gemma":[0.0003020531,0.0002835228,0.00020212769,0.0011617966,0.000563082,0.0004843038,0.000668877,0.00018765155,0.0002725036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032556994,0.00007484114,0.9596808,0.00006921014,0.00018559166,0.0010562086,0.0036308405,0.0020335969,0.014168526,0.0012055904,0.0006465275,0.016922763],"study_design_scores_gemma":[0.0000035712817,0.000011502629,0.9976809,0.000009258272,0.000011927774,0.00012010272,0.0010061014,0.00034700366,0.000116216535,0.00004985932,0.00063933665,0.0000042920497],"about_ca_topic_score_codex":0.041691795,"about_ca_topic_score_gemma":0.074464016,"teacher_disagreement_score":0.041691795,"about_ca_system_score_codex":0.0009047381,"about_ca_system_score_gemma":0.00079781713,"threshold_uncertainty_score":0.0828982},"labels":[],"label_agreement":null},{"id":"W1969073114","doi":"10.1016/j.tecto.2011.11.022","title":"Present-day stress analysis of the St. Lawrence Lowlands sedimentary basin (Canada) and implications for caprock integrity during CO2 injection operations","year":2011,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Geology; Caprock; Sedimentary rock; Structural basin; Borehole; Seismology; Petrology; Geomorphology; Geotechnical engineering; Geochemistry","score_opus":0.0238199417485044,"score_gpt":0.2233455800145618,"score_spread":0.1995256382660574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969073114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996058,0.00010544273,0.00006383798,0.00014356342,0.000003828025,0.0000038423336,0.0014394687,0.000010110426,0.0021718154],"genre_scores_gemma":[0.99809545,0.000083364714,0.00007659817,0.00001762109,0.0000025294964,0.0000015298587,0.00086688565,0.0000034159714,0.00085267215],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999013,0.000004823735,0.000005027988,0.000016698013,0.000031430292,0.000040731273],"domain_scores_gemma":[0.99955314,0.000015784397,0.00003815173,0.000009921522,0.00031407565,0.00006887263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014440341,0.00020262749,0.00017125887,0.0011894148,0.0011629127,0.0009787701,0.00060762523,0.00035168376,0.0016136634],"category_scores_gemma":[0.0005230341,0.00018100583,0.00014510086,0.0020928292,0.00058652274,0.00031090796,0.00034132515,0.00027785474,0.00022868495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024171922,0.00008827789,0.96395975,0.000059527316,0.0000832416,0.00030738517,0.0014476026,0.005745303,0.005800365,0.0009650592,0.0029426217,0.018359214],"study_design_scores_gemma":[0.000005288652,0.000009394922,0.9947648,0.000010263678,0.000014395981,0.000018342198,0.00075757236,0.0023866314,0.00035106647,0.00006815662,0.0016049534,0.000009194293],"about_ca_topic_score_codex":0.9852364,"about_ca_topic_score_gemma":0.9944429,"teacher_disagreement_score":0.014763594,"about_ca_system_score_codex":0.012201383,"about_ca_system_score_gemma":0.007969173,"threshold_uncertainty_score":0.08852762},"labels":[],"label_agreement":null},{"id":"W1969148653","doi":"10.1029/2002gl015406","title":"Thermal models of the Middle America Trench at the Nicoya Peninsula, Costa Rica","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":139,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Forearc; Subduction; Trench; Induced seismicity; Accretionary wedge; Seismology; Hypocenter; Hydrothermal circulation; Seafloor spreading; Thermal; Prism; Petrology; Geophysics; Tectonics; Meteorology","score_opus":0.08314370147969984,"score_gpt":0.26145007152154826,"score_spread":0.1783063700418484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969148653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9647948,0.00036453878,0.003706665,0.00034049532,0.000017423976,0.00004651217,0.0015106109,0.0002196498,0.02899939],"genre_scores_gemma":[0.9959552,0.000152558,0.00080301194,0.00002330756,0.0000069678513,0.00005167223,0.00029219026,0.000029657755,0.0026853369],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992716,0.000024062252,0.0000030118647,0.00001846531,0.000008495383,0.000018878556],"domain_scores_gemma":[0.99987614,0.000036480425,0.000020165859,0.000013864009,0.00003259734,0.00002086003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013713399,0.000488439,0.00030385857,0.0005235932,0.00066578167,0.0009219654,0.0009910818,0.0006934091,0.0031176081],"category_scores_gemma":[0.0006953643,0.00030645804,0.00041651315,0.0006194424,0.00056586135,0.00038191964,0.0005660863,0.00025320367,0.00025395027],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033949484,0.00001318799,0.0056133983,0.000012675764,0.00002232734,0.00006239432,0.00008749806,0.99093866,0.00042826936,0.0014653769,0.00032318558,0.0009989392],"study_design_scores_gemma":[0.00003910521,0.000015251688,0.007135964,0.000009792258,0.000017464981,0.000022779475,0.00014041505,0.99020445,0.00015033007,0.0007787245,0.0014710012,0.000014771141],"about_ca_topic_score_codex":0.31973606,"about_ca_topic_score_gemma":0.21218784,"teacher_disagreement_score":0.31973606,"about_ca_system_score_codex":0.0032063595,"about_ca_system_score_gemma":0.0010539417,"threshold_uncertainty_score":0.63575},"labels":[],"label_agreement":null},{"id":"W1969257951","doi":"10.1029/2004jb003163","title":"Three‐dimensional viscoelastic finite element model for postseismic deformation of the great 1960 Chile earthquake","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":155,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Geology; Seismology; Subduction; Trench; Viscoelasticity; Mantle (geology); Interplate earthquake; Slip (aerodynamics); Plate tectonics; Geodesy; Geophysics; Tectonics","score_opus":0.03530447720167236,"score_gpt":0.2799359646805951,"score_spread":0.24463148747892277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969257951","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.21938823,0.00080569694,0.74898285,0.0011650351,0.00014586512,0.0001752705,0.0012004519,0.0006879518,0.02744871],"genre_scores_gemma":[0.9311766,0.00061847345,0.045707654,0.0002028114,0.000051613213,0.00066617713,0.0006259038,0.00016145634,0.020789344],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998981,0.000028793047,0.000007367046,0.000021814163,0.000024140045,0.000019676354],"domain_scores_gemma":[0.9998135,0.000082182654,0.000033658736,0.000012640794,0.000038054455,0.00002009953],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027193493,0.00059128104,0.00058940507,0.00050104724,0.0005096032,0.00072328944,0.0016084318,0.002052572,0.0029471559],"category_scores_gemma":[0.0006687629,0.00065193826,0.0008143543,0.00040729094,0.0006274086,0.00065750704,0.00072847167,0.00075119035,0.00061039045],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008324991,0.000011093781,0.00029954824,0.00001036913,0.000007826284,0.000041693485,0.000023134504,0.9963498,0.00073245354,0.0015666747,0.00008919984,0.0008597582],"study_design_scores_gemma":[0.0000033472215,0.0000045407614,0.00007190965,0.0000023515545,0.0000018707309,0.0000051882944,0.0000047908434,0.99930036,0.000054537875,0.000315236,0.00023301349,0.000002817762],"about_ca_topic_score_codex":0.016726092,"about_ca_topic_score_gemma":0.007408167,"teacher_disagreement_score":0.016726092,"about_ca_system_score_codex":0.00074216013,"about_ca_system_score_gemma":0.0010138279,"threshold_uncertainty_score":0.033257425},"labels":[],"label_agreement":null},{"id":"W1969364518","doi":"10.1007/s00024-008-0331-y","title":"Earthquakes: Recurrence and Interoccurrence Times","year":2008,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Weibull distribution; Seismology; San andreas fault; Geology; Sequence (biology); Fault (geology); Statistics; Exponentiated Weibull distribution; Mathematics","score_opus":0.015121614560067137,"score_gpt":0.1970962324254506,"score_spread":0.18197461786538346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969364518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96919596,0.0051582647,0.016587168,0.00044332814,0.00006442993,0.000016151045,0.0034562899,0.00026944245,0.0048088613],"genre_scores_gemma":[0.9964317,0.0005726597,0.0010136758,0.000008651067,0.000079399266,0.0000102907925,0.0011571927,0.000024547724,0.0007019371],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995944,0.00012057557,0.000071206174,0.00010121828,0.00008187078,0.000030697738],"domain_scores_gemma":[0.9860659,0.009365676,0.0026469266,0.00090441835,0.00072364917,0.00029332665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015339674,0.0002292482,0.0003259513,0.0024506592,0.00022228979,0.0009437671,0.0003765092,0.0004766001,0.0037655106],"category_scores_gemma":[0.018683061,0.00017698613,0.00030553414,0.0026381349,0.0004585222,0.0013472647,0.0003339276,0.00038837735,0.0009477988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001073508,0.0001305637,0.7772093,0.0002846095,0.00054757675,0.0006706377,0.0015153404,0.022632215,0.0044703507,0.034803484,0.004724343,0.1519382],"study_design_scores_gemma":[0.00007797606,0.0005163789,0.8434827,0.000085894324,0.0005320769,0.0050994987,0.0011884142,0.083873145,0.0013850543,0.0530898,0.010561093,0.00010799113],"about_ca_topic_score_codex":0.0006253184,"about_ca_topic_score_gemma":0.0006491684,"teacher_disagreement_score":0.0037655106,"about_ca_system_score_codex":0.00017492888,"about_ca_system_score_gemma":0.00013926202,"threshold_uncertainty_score":0.012596905},"labels":[],"label_agreement":null},{"id":"W1969820276","doi":"10.1038/ngeo1835","title":"Episodic fault creep events in California controlled by shallow frictional heterogeneity","year":2013,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Creep; Geology; Slip (aerodynamics); Fault (geology); Lithology; Seismology; Geotechnical engineering; Instability; Strike-slip tectonics; Petrology; Mechanics; Materials science","score_opus":0.0069554216326310455,"score_gpt":0.21835275094051299,"score_spread":0.21139732930788194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969820276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99937683,0.000023996981,0.000019792498,0.000017491056,0.0000016067626,0.0000024063154,0.00008924773,0.000005370293,0.0004632868],"genre_scores_gemma":[0.99981636,0.000014907087,0.000016753249,0.0000035356247,0.000001701812,0.000001633241,0.00007266794,0.0000013500639,0.000071181035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984205,0.000014435496,0.000014704273,0.000054574466,0.000022093038,0.000052208983],"domain_scores_gemma":[0.9986083,0.00026621754,0.00048633592,0.0001352006,0.00020183502,0.00030229325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002885052,0.00014274975,0.00036289368,0.000882894,0.0009422079,0.0009490846,0.00040509543,0.00043819385,0.0013878716],"category_scores_gemma":[0.0016588129,0.00027292737,0.00014394424,0.0010088163,0.00071416376,0.00042478176,0.0006858452,0.00027287847,0.00009627999],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00071728043,0.00022790843,0.9826032,0.00003453461,0.00008007148,0.00036450865,0.0011085343,0.0034993947,0.003392597,0.0003856573,0.0010309014,0.0065553803],"study_design_scores_gemma":[0.000013946321,0.000018591503,0.9985765,0.000003548809,0.000013307915,0.000017805645,0.00027602407,0.0008940094,0.00004189744,0.000042553253,0.0000973515,0.00000435587],"about_ca_topic_score_codex":0.17244998,"about_ca_topic_score_gemma":0.374193,"teacher_disagreement_score":0.17244998,"about_ca_system_score_codex":0.00154393,"about_ca_system_score_gemma":0.0009882075,"threshold_uncertainty_score":0.3428924},"labels":[],"label_agreement":null},{"id":"W1970105116","doi":"10.1007/s00024-006-0164-5","title":"The 26 December 2004 Sumatra Tsunami: Analysis of Tide Gauge Data from the World Ocean Part 1. Indian Ocean and South Africa","year":2007,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":142,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Australian Antarctic Division; Russian Foundation for Basic Research","keywords":"Tide gauge; Indian ocean; Geology; Seismology; Oceanography; Tsunami wave; Pacific ocean; Tsunami earthquake; Climatology; Sea level","score_opus":0.020523865055096447,"score_gpt":0.21746331486561488,"score_spread":0.19693944981051842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970105116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98118156,0.0001977089,0.000099270364,0.00016187191,0.000026246697,0.00002029929,0.017150851,0.00002334425,0.0011389379],"genre_scores_gemma":[0.9634727,0.00050598796,0.00036627532,0.000046218393,0.000027570142,0.00004419845,0.033487532,0.00001682408,0.002032668],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980015,0.000022996779,0.00003061733,0.000028693634,0.000056504105,0.000061007126],"domain_scores_gemma":[0.9987588,0.00014400156,0.00048355042,0.00008440168,0.00037343294,0.00015588632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035709812,0.0005502677,0.0003601278,0.0034798093,0.00057276135,0.00097015896,0.0004207286,0.0003922068,0.0017238526],"category_scores_gemma":[0.001909051,0.00030962183,0.00034442588,0.0048555876,0.00028003656,0.0005497463,0.000977207,0.00039412637,0.0006631432],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047295057,0.00012397794,0.9449771,0.00023560648,0.00040446123,0.0015945294,0.0017431232,0.0074026412,0.0026865285,0.00024489456,0.011372972,0.028741328],"study_design_scores_gemma":[0.000006787305,0.000015760774,0.9963702,0.000016565957,0.0000422239,0.000111198904,0.0005274818,0.0007406074,0.00021738057,0.000021999092,0.0019214064,0.000008336928],"about_ca_topic_score_codex":0.17432196,"about_ca_topic_score_gemma":0.26429302,"teacher_disagreement_score":0.17432196,"about_ca_system_score_codex":0.0016828489,"about_ca_system_score_gemma":0.0012850196,"threshold_uncertainty_score":0.34661454},"labels":[],"label_agreement":null},{"id":"W1970321886","doi":"10.1038/ngeo1195","title":"Sedimentary underplating at the Cascadia mantle-wedge corner revealed by seismic imaging","year":2011,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; National Nuclear Security Administration; Sandia National Laboratories; U.S. Geological Survey","keywords":"Subduction; Geology; Seismology; Underplating; Convergent boundary; Episodic tremor and slip; Oceanic crust; Plate tectonics; Seismic tomography; Mantle (geology); Crust; Mantle wedge; Eclogitization; Slip (aerodynamics); Volcanic arc; Geophysics; Tectonics","score_opus":0.012489968315956784,"score_gpt":0.20884719903097318,"score_spread":0.1963572307150164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970321886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960807,0.00003483843,0.00021445054,0.00008999421,0.000008988814,0.000006296875,0.000275557,0.000057165133,0.0032319024],"genre_scores_gemma":[0.99902654,0.00003396751,0.00025284276,0.000012151426,0.000005472294,0.0000032092585,0.00018049171,0.000009089989,0.00047614356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993646,0.0000024127726,0.0000035934884,0.000020720354,0.000017104137,0.00001975614],"domain_scores_gemma":[0.9997937,0.000011690871,0.00005042263,0.000023738845,0.000055069544,0.00006534309],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000080728336,0.0003372721,0.0002956965,0.001206022,0.000741614,0.00066090963,0.00050870073,0.0006160232,0.0020907382],"category_scores_gemma":[0.0005033946,0.00038226022,0.00016570934,0.0012016584,0.00046656912,0.00036429195,0.00076338946,0.00052399165,0.00048100873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081422925,0.00021780629,0.6809974,0.00013354862,0.00011496186,0.005141702,0.0040734964,0.005409901,0.27625057,0.00091220404,0.0022525373,0.023681661],"study_design_scores_gemma":[0.00001658211,0.000041967684,0.99383247,0.000008643112,0.00002223999,0.000218445,0.00068815384,0.0021062458,0.0020186538,0.000088718414,0.0009460365,0.00001202743],"about_ca_topic_score_codex":0.040446296,"about_ca_topic_score_gemma":0.06961093,"teacher_disagreement_score":0.040446296,"about_ca_system_score_codex":0.0004723818,"about_ca_system_score_gemma":0.00058664184,"threshold_uncertainty_score":0.080421686},"labels":[],"label_agreement":null},{"id":"W1970578725","doi":"10.1038/ngeo1610","title":"The 2011 Lorca earthquake slip distribution controlled by groundwater crustal unloading","year":2012,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":171,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Seismology; Slip (aerodynamics); Groundwater; Geodetic datum; Crust; Fault (geology); Earthquake prediction; Geotechnical engineering; Geophysics; Geodesy","score_opus":0.007037103370178883,"score_gpt":0.21197012930269332,"score_spread":0.20493302593251445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970578725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99710387,0.000017706256,0.00009959528,0.000057619614,0.0000058580567,0.0000029283233,0.00023494178,0.00002008269,0.0024574592],"genre_scores_gemma":[0.99933237,0.000009779899,0.00002619639,0.0000047221565,0.0000021657331,0.0000017991442,0.00010589534,0.00000628383,0.00051073905],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998996,0.000011539252,0.000004229544,0.000024691204,0.000011059705,0.00004889488],"domain_scores_gemma":[0.9995771,0.00009228068,0.00008915808,0.000045498076,0.00011928838,0.000076697535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015217807,0.00017941264,0.00024851094,0.00045051545,0.00047408335,0.0006456904,0.00020910447,0.0002355242,0.003035534],"category_scores_gemma":[0.0011228733,0.00023974765,0.00016250552,0.00029906438,0.0004317208,0.00028922842,0.00030307943,0.0002961976,0.00041075886],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.006419777,0.0005970466,0.6220734,0.00019264566,0.00014455391,0.0011619837,0.0016276637,0.069502175,0.21631764,0.00347325,0.013946864,0.064543046],"study_design_scores_gemma":[0.000026360609,0.00012254888,0.9755256,0.0000072595935,0.000017834454,0.000052641208,0.0003029096,0.019702835,0.0031531518,0.00015500688,0.00090968737,0.00002422393],"about_ca_topic_score_codex":0.048931953,"about_ca_topic_score_gemma":0.07309865,"teacher_disagreement_score":0.048931953,"about_ca_system_score_codex":0.0013097366,"about_ca_system_score_gemma":0.00060057675,"threshold_uncertainty_score":0.09729427},"labels":[],"label_agreement":null},{"id":"W1970864415","doi":"10.1029/2000jb900232","title":"Observation of diffusion processes in earthquake populations and implications for the predictability of seismicity systems","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology; Scaling; Caldera; Magnitude (astronomy); Predictability; Diffusion; Geophysics; Physics; Geometry; Volcano; Mathematics","score_opus":0.07848016511619697,"score_gpt":0.3241797422738715,"score_spread":0.2456995771576745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970864415","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99029434,0.00015711607,0.008026651,0.0001788989,0.00000263009,0.000006952611,0.0001250676,0.00003516968,0.0011731883],"genre_scores_gemma":[0.9993831,0.00005086175,0.00046999208,0.0000042175498,0.0000034364027,0.0000024824644,0.000040564057,0.0000019958466,0.00004341823],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998839,0.000017112945,0.00001240195,0.000045110857,0.000024995685,0.000016498467],"domain_scores_gemma":[0.99795,0.00096887286,0.00073143706,0.00017760949,0.0000921252,0.00008001877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004243442,0.00014057472,0.00018016314,0.00075199397,0.00025225262,0.000596066,0.00017227973,0.00020806058,0.00060513744],"category_scores_gemma":[0.003928145,0.00018206691,0.00023403003,0.00057236623,0.0011739597,0.000780034,0.00043792158,0.0004222162,0.000040395582],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017611826,0.000075777076,0.7175197,0.0001408938,0.0001829605,0.00066948746,0.0022318228,0.11524839,0.07354326,0.046097886,0.0006153994,0.043498304],"study_design_scores_gemma":[0.000023723751,0.000053449246,0.83487236,0.0000140598795,0.00002724191,0.00048251628,0.00035703482,0.13136363,0.004875343,0.026924247,0.00095940055,0.000047106983],"about_ca_topic_score_codex":0.004542382,"about_ca_topic_score_gemma":0.0025387227,"teacher_disagreement_score":0.004542382,"about_ca_system_score_codex":0.0005755902,"about_ca_system_score_gemma":0.00018147174,"threshold_uncertainty_score":0.009031892},"labels":[],"label_agreement":null},{"id":"W1971037209","doi":"10.1016/j.cageo.2014.05.015","title":"The ValleyMorph Tool: An automated extraction tool for transverse topographic symmetry (T-) factor and valley width to valley height (Vf-) ratio","year":2014,"lang":"en","type":"article","venue":"Computers & Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Transverse plane; Geology; Extraction (chemistry); Symmetry (geometry); Aspect ratio (aeronautics); Geometry; Remote sensing; Geodesy; Geomorphology; Physics; Mathematics; Engineering; Structural engineering","score_opus":0.017590988156139766,"score_gpt":0.24601083182855701,"score_spread":0.22841984367241724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971037209","genre_codex":"methods","genre_gemma":"software","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"software","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.018219117,0.0004779265,0.7220934,0.00014124962,0.00016617707,0.0004451056,0.055711683,0.19576752,0.0069778976],"genre_scores_gemma":[0.0915285,0.00037124165,0.8129071,0.0001682276,0.0000873941,0.00082844106,0.06396541,0.019773487,0.010370185],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994641,0.00003132996,0.000062625666,0.00015750428,0.00022126862,0.00006316574],"domain_scores_gemma":[0.9989095,0.00031903823,0.00014995175,0.00013748069,0.0004328723,0.00005126951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006775315,0.0018512214,0.0010702661,0.005759621,0.00067666906,0.0016747302,0.0015228029,0.00088489,0.030022595],"category_scores_gemma":[0.0033302468,0.0010751141,0.0010987326,0.0028797523,0.0002448642,0.0015794038,0.001643012,0.00074808,0.013684862],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031170572,0.00013555311,0.01231642,0.0010007313,0.0001957369,0.00057349284,0.0004631162,0.0031077531,0.035932306,0.0028177418,0.20928377,0.7338616],"study_design_scores_gemma":[0.00044959155,0.00025531175,0.06760527,0.00047227097,0.00038030115,0.0038418416,0.00083380175,0.21664254,0.17349878,0.013095524,0.5223321,0.0005926478],"about_ca_topic_score_codex":0.0044503715,"about_ca_topic_score_gemma":0.007540337,"teacher_disagreement_score":0.030022595,"about_ca_system_score_codex":0.00026655893,"about_ca_system_score_gemma":0.0011167187,"threshold_uncertainty_score":0.100435555},"labels":[],"label_agreement":null},{"id":"W1971296307","doi":"10.1080/01490410600939231","title":"Tsunami Travel Time Atlas for the Atlantic Ocean","year":2006,"lang":"en","type":"article","venue":"Marine Geodesy","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of Waterloo; York University","funders":"","keywords":"Atlas (anatomy); Oceanography; Geography; Atlantic hurricane; Geology; Pacific ocean; Oceanic basin; Travel time; Climatology; Structural basin; Paleontology; Engineering","score_opus":0.008602378897957709,"score_gpt":0.18675569976877945,"score_spread":0.17815332087082175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971296307","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0073954915,0.0010782272,0.0038982616,0.0010023017,0.0008723767,0.00023264988,0.8847127,0.0010773129,0.09973065],"genre_scores_gemma":[0.024729872,0.0018448203,0.011475033,0.00031890566,0.00025258292,0.0002844249,0.92740107,0.00022671268,0.03346657],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998141,0.000017349488,0.000035764253,0.000022433629,0.000081433114,0.000028942039],"domain_scores_gemma":[0.99867815,0.00006351047,0.00011871702,0.00010044883,0.00088390463,0.0001552459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031977746,0.00041606414,0.00024984064,0.0030816142,0.00046974065,0.0006471873,0.0004970827,0.00021219146,0.025334762],"category_scores_gemma":[0.0009614703,0.00013832911,0.00021604581,0.0055264994,0.0000937864,0.0006969436,0.00055934134,0.0008001251,0.012049344],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013479641,0.00004285139,0.014319798,0.00024204122,0.000029392153,0.000075031654,0.0001420613,0.00044748493,0.0012985134,0.00371283,0.92822,0.051335227],"study_design_scores_gemma":[0.000029956795,0.000023140097,0.05411022,0.000052018568,0.000015243298,0.000070584385,0.00008839615,0.00029874215,0.00022053992,0.0006957758,0.94438314,0.000012328352],"about_ca_topic_score_codex":0.096499205,"about_ca_topic_score_gemma":0.11563055,"teacher_disagreement_score":0.096499205,"about_ca_system_score_codex":0.00071746274,"about_ca_system_score_gemma":0.0022352322,"threshold_uncertainty_score":0.19187504},"labels":[],"label_agreement":null},{"id":"W1971967577","doi":"10.1029/2009gl040006","title":"Bottom pressure signals at the TAG deep‐sea hydrothermal field: Evidence for short‐period, flow‐induced ground deformation","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Woods Hole Oceanographic Institution","keywords":"Hydrothermal circulation; Geology; Seafloor spreading; Ridge; Amplitude; Seabed; Permeability (electromagnetism); Mineralogy; Geophysics; Seismology; Petrology; Oceanography; Paleontology; Optics; Physics; Chemistry","score_opus":0.07334681407200014,"score_gpt":0.32774433680996645,"score_spread":0.25439752273796634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971967577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99932075,0.000028216014,0.00016214,0.00001140589,0.0000028129593,0.000001689527,0.00016248968,0.000008715783,0.00030178652],"genre_scores_gemma":[0.9995173,0.000016933316,0.00013107868,0.0000090542835,0.0000040822606,0.0000020319776,0.00019912493,0.00000188484,0.00011858449],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000028327506,0.0000028508161,0.0000102510985,0.000011120778,0.000015764985],"domain_scores_gemma":[0.9998286,0.000023692064,0.00005316671,0.000009536048,0.00003335001,0.00005159856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000079550555,0.00013898888,0.00014392241,0.00042054456,0.00019606575,0.0002469824,0.00015403389,0.0002419261,0.0006376769],"category_scores_gemma":[0.00029006542,0.00015813074,0.00009819936,0.0004105539,0.00023529596,0.00016814054,0.00018672344,0.0001613552,0.00013882821],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046976286,0.0000757952,0.61766285,0.000047028527,0.00004820088,0.00038263667,0.00038256918,0.00032075334,0.37048194,0.00009232139,0.00030521097,0.009730994],"study_design_scores_gemma":[0.000004921938,0.000030191097,0.9972518,0.0000010355308,0.000005842912,0.000073853895,0.000042389092,0.00034493243,0.0021576995,0.000008522427,0.00007580536,0.0000028999527],"about_ca_topic_score_codex":0.0069262297,"about_ca_topic_score_gemma":0.013181622,"teacher_disagreement_score":0.0069262297,"about_ca_system_score_codex":0.00021300877,"about_ca_system_score_gemma":0.00015656723,"threshold_uncertainty_score":0.013771832},"labels":[],"label_agreement":null},{"id":"W1972253275","doi":"10.1190/1.3353726","title":"It's a matter of size: Magnitude and moment estimates for microseismic data","year":2010,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Apache (Canada)","funders":"","keywords":"Microseism; Geophone; Magnitude (astronomy); Borehole; Geology; Seismology; Hydraulic fracturing; Fracture (geology); Seismic moment; Moment (physics); Geotechnical engineering; Physics","score_opus":0.03355237745396951,"score_gpt":0.27222181578769644,"score_spread":0.23866943833372695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972253275","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36879745,0.008286755,0.58011293,0.011188673,0.00084985985,0.00023364706,0.00548212,0.0008529973,0.024195487],"genre_scores_gemma":[0.90139985,0.0014987396,0.09130817,0.00033505852,0.0017867504,0.00014670324,0.0017138144,0.00024791883,0.0015630634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9981281,0.0006450926,0.00024554378,0.00027949386,0.0006351785,0.00006654173],"domain_scores_gemma":[0.9565697,0.031402968,0.0052945563,0.0030186956,0.0029381567,0.0007760389],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004073458,0.0003763307,0.00045645598,0.0029839976,0.00035961918,0.0014458479,0.00058931357,0.000585596,0.0014776664],"category_scores_gemma":[0.047668815,0.0002504593,0.00023622657,0.0024872015,0.0006992476,0.003450394,0.0013085342,0.0009169154,0.0005143029],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003069583,0.00009316219,0.46583483,0.0006248101,0.00023135882,0.00049662887,0.0022917986,0.016061058,0.01542646,0.047224026,0.01723459,0.4341744],"study_design_scores_gemma":[0.00007753386,0.00048489502,0.7224685,0.00069891335,0.00021093986,0.002669106,0.0033015495,0.10661612,0.012803426,0.0763318,0.07412384,0.00021329592],"about_ca_topic_score_codex":0.000918709,"about_ca_topic_score_gemma":0.0013750434,"teacher_disagreement_score":0.004073458,"about_ca_system_score_codex":0.0003269902,"about_ca_system_score_gemma":0.0002945839,"threshold_uncertainty_score":0.021542728},"labels":[],"label_agreement":null},{"id":"W1972952243","doi":"10.1007/s00024-015-1036-7","title":"Discrete Element Modeling of Stick-Slip Instability and Induced Microseismicity","year":2015,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Discrete element method; Slip (aerodynamics); Geology; Shear (geology); Fault (geology); Instability; Mechanics; Seismology; Engineering; Petrology; Physics","score_opus":0.028569704301936748,"score_gpt":0.2214415050455834,"score_spread":0.19287180074364665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972952243","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3301973,0.00037831173,0.636584,0.00049767323,0.00019176677,0.00006711897,0.00041739887,0.0004847521,0.031181647],"genre_scores_gemma":[0.98020107,0.00014481705,0.012082818,0.00003516364,0.000019115369,0.000042508746,0.00009856273,0.00004793738,0.0073279357],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988973,0.000025028416,0.000006761369,0.000016838381,0.00004386629,0.000017773142],"domain_scores_gemma":[0.99975544,0.00010844522,0.00003405969,0.00002368109,0.000049038517,0.000029371986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017725618,0.00033703746,0.0005688711,0.00043104478,0.0003227022,0.0009046346,0.0009299372,0.0012798773,0.0022684722],"category_scores_gemma":[0.00076434336,0.00040984357,0.0003830673,0.00036999787,0.00063752016,0.0005379438,0.0005863,0.0006188558,0.0003313892],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013964212,0.000020429918,0.0003001648,0.0000101922915,0.0000075509797,0.000032550357,0.000023360399,0.9936493,0.0010579624,0.0030712876,0.00007730875,0.0017359521],"study_design_scores_gemma":[0.0000012953145,0.0000023095993,0.000044357796,7.584046e-7,7.637627e-7,0.0000021090577,0.0000033142187,0.99953854,0.000081726255,0.00025711072,0.00006686627,9.24621e-7],"about_ca_topic_score_codex":0.0081780795,"about_ca_topic_score_gemma":0.005846174,"teacher_disagreement_score":0.0081780795,"about_ca_system_score_codex":0.0005166368,"about_ca_system_score_gemma":0.0006345393,"threshold_uncertainty_score":0.016260982},"labels":[],"label_agreement":null},{"id":"W1973012562","doi":"10.1142/s1793431107000043","title":"SEISMIC SHAKING IN SINGAPORE DUE TO PAST SUMATRAN EARTHQUAKES","year":2007,"lang":"en","type":"article","venue":"Journal of Earthquake and Tsunami","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McMaster University","keywords":"Seismology; Seismic hazard; Peak ground acceleration; Geology; Earthquake scenario; Seismogram; Seismic microzonation; Strong ground motion; Seismotectonics; Earthquake warning system; Seismic risk; Ground motion; Fault (geology); Engineering; Warning system","score_opus":0.015663398121784296,"score_gpt":0.2364587226829146,"score_spread":0.2207953245611303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973012562","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987336,0.00005314177,0.000042470543,0.000035568777,0.0000025195438,0.0000034018824,0.00017262391,0.0000060047737,0.00095069694],"genre_scores_gemma":[0.99928707,0.00007797371,0.000041090436,0.0000088943825,0.0000030816623,0.0000021282326,0.00027503842,0.0000015761325,0.00030319707],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998122,0.00003211686,0.000023494687,0.000027547558,0.00007730768,0.000027282997],"domain_scores_gemma":[0.9996264,0.00003126762,0.00018162692,0.000029127925,0.00006303595,0.00006857781],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019684201,0.00029628404,0.00023958358,0.0007331116,0.00037359292,0.00051258487,0.00019223135,0.00023315875,0.00082813285],"category_scores_gemma":[0.00059389946,0.00016984649,0.00018636449,0.0010795838,0.00032860902,0.00029987327,0.00078118703,0.00020888947,0.00029957492],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036919955,0.00008263205,0.95077,0.00010390072,0.00012966218,0.008300916,0.0028929187,0.0047967667,0.010281705,0.00019233847,0.0009077368,0.021172157],"study_design_scores_gemma":[0.0000066468447,0.00016926427,0.9932853,0.000009066273,0.000028537424,0.001130329,0.0011944597,0.0022332203,0.00074949674,0.0000555544,0.0011209274,0.000017159307],"about_ca_topic_score_codex":0.023111029,"about_ca_topic_score_gemma":0.046227746,"teacher_disagreement_score":0.023111029,"about_ca_system_score_codex":0.001042989,"about_ca_system_score_gemma":0.00029644396,"threshold_uncertainty_score":0.045952976},"labels":[],"label_agreement":null},{"id":"W1973109447","doi":"10.1029/2010jb007626","title":"Spatiotemporal correlations of aftershock sequences","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Aftershock; Sequence (biology); Spatial distribution; Distribution (mathematics); Event (particle physics); Stochastic modelling","score_opus":0.040244236162731324,"score_gpt":0.3101676763973633,"score_spread":0.269923440234632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973109447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99158937,0.0001514774,0.00631706,0.00007743219,0.0000064520154,0.000010992625,0.0005537723,0.0000382582,0.0012550686],"genre_scores_gemma":[0.9991773,0.000056573474,0.00027746742,0.0000042526563,0.000005667762,0.0000051582724,0.00030143745,0.0000046571167,0.00016743699],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972457,0.000046851936,0.000025847166,0.00008640523,0.000060375303,0.00005583041],"domain_scores_gemma":[0.9953322,0.0014858724,0.0018873229,0.00043365243,0.0006315885,0.00022938779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006627805,0.00012397779,0.0002786017,0.0010705828,0.00020837066,0.0006382719,0.00028704395,0.00025506064,0.0012955324],"category_scores_gemma":[0.0068301694,0.00015969053,0.00021037715,0.001164647,0.00036713132,0.00064845517,0.000327643,0.00031654796,0.00012052362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024111722,0.00007947062,0.6814743,0.00010565251,0.00031101637,0.0009987799,0.00075688306,0.22590211,0.017329518,0.04772298,0.00258302,0.022495188],"study_design_scores_gemma":[0.000020832986,0.00008648425,0.6281906,0.000020568861,0.000088680084,0.00039088776,0.000357658,0.35544094,0.0023737308,0.010706107,0.0022791293,0.00004448195],"about_ca_topic_score_codex":0.0072372574,"about_ca_topic_score_gemma":0.0060792044,"teacher_disagreement_score":0.0072372574,"about_ca_system_score_codex":0.0005098303,"about_ca_system_score_gemma":0.0003670349,"threshold_uncertainty_score":0.01439029},"labels":[],"label_agreement":null},{"id":"W1973271892","doi":"10.1016/j.tecto.2012.06.018","title":"Seismic properties of the Longmen Shan complex: Implications for the moment magnitude of the great 2008 Wenchuan earthquake in China","year":2012,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Bedford Institute of Oceanography; Polytechnique Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Land and Resources of the People's Republic of China; Chinese Academy of Geological Sciences; Dalhousie University; Chinese Academy of Sciences","keywords":"Geology; Felsic; Mafic; Seismology; Geothermal gradient; Crust; Tectonics; Magnitude (astronomy); Petrology; Seismic anisotropy; Geochemistry; Geophysics; Mantle (geology)","score_opus":0.041333792715602884,"score_gpt":0.23019649417445795,"score_spread":0.18886270145885506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973271892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999476,0.000032671487,0.000037385988,0.00006318095,0.0000014606597,0.0000011953788,0.00009252768,0.0000018946577,0.00029385195],"genre_scores_gemma":[0.9997954,0.000020907897,0.00001508403,0.0000067423616,0.0000027666927,0.0000010058949,0.00007487435,0.0000010222218,0.000082195744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.00001851026,0.0000123542795,0.00002923197,0.000021318796,0.000030092346],"domain_scores_gemma":[0.99947566,0.00007504374,0.0001688853,0.000038761427,0.00012124418,0.00012039108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034452113,0.0002716408,0.00028072356,0.0014365757,0.0005960327,0.00063437695,0.00036413068,0.0003113823,0.0010719921],"category_scores_gemma":[0.0008844478,0.00027004885,0.00020943732,0.0021989765,0.000557487,0.00044320346,0.00054806506,0.0002199517,0.00010227888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008410328,0.000029512388,0.98737925,0.000018903967,0.000052392916,0.00022693383,0.00080183794,0.002387281,0.0036979835,0.0003389246,0.0002311922,0.0047517316],"study_design_scores_gemma":[0.0000032215687,0.0000078181265,0.997792,0.0000018854555,0.00000811758,0.000019143867,0.00028810918,0.0016626668,0.0000533109,0.000053923628,0.00010536441,0.000004378793],"about_ca_topic_score_codex":0.10911011,"about_ca_topic_score_gemma":0.14700255,"teacher_disagreement_score":0.10911011,"about_ca_system_score_codex":0.0013553345,"about_ca_system_score_gemma":0.0013008873,"threshold_uncertainty_score":0.21695006},"labels":[],"label_agreement":null},{"id":"W1973920228","doi":"10.1007/s00367-013-0337-z","title":"Limitation of fluid flow at the Nankai Trough megasplay fault zone","year":2013,"lang":"en","type":"article","venue":"Geo-Marine Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Seafloor spreading; Fault (geology); Borehole; Thrust fault; Fluid dynamics; Petrology; Subduction; Trough (economics); Tectonics; Geophysics; Geotechnical engineering; Mechanics","score_opus":0.010200580634477102,"score_gpt":0.18746038447784458,"score_spread":0.17725980384336748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973920228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99924964,0.000021651687,0.00004851022,0.000021547106,0.0000012971104,0.0000021890628,0.000037717375,0.0000058673386,0.0006115663],"genre_scores_gemma":[0.99978083,0.0000145625245,0.00003631669,0.0000037937673,0.0000010286554,0.0000031741492,0.00003337508,8.054436e-7,0.00012612632],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998965,0.000010576022,0.000011253994,0.000026498908,0.000018554629,0.000036534893],"domain_scores_gemma":[0.9997142,0.00004921879,0.00008309082,0.000019850453,0.00007088601,0.000062797335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012384026,0.0001820433,0.0004336493,0.0009912773,0.00071733317,0.0007158411,0.0006203398,0.00049131305,0.001059847],"category_scores_gemma":[0.000618256,0.00025691726,0.00018293907,0.0005311278,0.00073899736,0.00051654794,0.00075020426,0.00026787608,0.00012347956],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012032557,0.00024211082,0.7867029,0.00019580589,0.00011332883,0.0018986551,0.003591326,0.011826415,0.17191331,0.001973199,0.00047690433,0.01986293],"study_design_scores_gemma":[0.000026812375,0.00012019338,0.99088144,0.000011767066,0.000024631698,0.000101977814,0.000944925,0.0051202658,0.0019595057,0.00025984854,0.0005262483,0.00002240685],"about_ca_topic_score_codex":0.034642473,"about_ca_topic_score_gemma":0.032537162,"teacher_disagreement_score":0.034642473,"about_ca_system_score_codex":0.0010419779,"about_ca_system_score_gemma":0.00087294553,"threshold_uncertainty_score":0.06888163},"labels":[],"label_agreement":null},{"id":"W1974274145","doi":"10.1126/science.1239577","title":"Slow Earthquakes, Preseismic Velocity Changes, and the Origin of Slow Frictional Stick-Slip","year":2013,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":176,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Seismology; Geology; Slip (aerodynamics); Shear (geology); Tectonics; Wave speed; Slow earthquake; Subduction; Petrology; Mechanics; Interplate earthquake; Physics","score_opus":0.018204547890884295,"score_gpt":0.21705828239348596,"score_spread":0.19885373450260166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974274145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984347,0.00034652828,0.0004566393,0.000017036706,0.0000029573723,0.0000038702246,0.000050670726,0.000014122537,0.00067343994],"genre_scores_gemma":[0.9995497,0.00013932335,0.00015657228,0.0000062737704,0.0000030239355,0.0000020494113,0.000039033584,0.0000014446483,0.0001025547],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999449,0.000006971375,0.0000043393093,0.000015035668,0.000014071006,0.0000146478105],"domain_scores_gemma":[0.99960583,0.000061611056,0.00019688217,0.000030743322,0.0000382338,0.000066731445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013850162,0.00021534986,0.00015717138,0.0007015597,0.00017980464,0.00033114475,0.00018474122,0.00026077105,0.0005960867],"category_scores_gemma":[0.00054400734,0.00015008035,0.00007927483,0.00034069706,0.00047542722,0.00028736485,0.00024722697,0.00021641732,0.00011954704],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005310807,0.0001281953,0.4501488,0.00019299016,0.00005030485,0.0009838213,0.0007375329,0.0013908887,0.5070893,0.00095824216,0.00019600333,0.037592877],"study_design_scores_gemma":[0.000008231974,0.00022262894,0.983084,0.000010249724,0.0000125796205,0.00036679272,0.00029883464,0.00096681993,0.014127734,0.0005043843,0.00038899467,0.000008731533],"about_ca_topic_score_codex":0.0010842042,"about_ca_topic_score_gemma":0.0013817009,"teacher_disagreement_score":0.0010842042,"about_ca_system_score_codex":0.0001576577,"about_ca_system_score_gemma":0.00010501838,"threshold_uncertainty_score":0.0021557808},"labels":[],"label_agreement":null},{"id":"W1974393412","doi":"10.1038/nature07650","title":"Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing","year":2008,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":600,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Forearc; Subduction; Mantle wedge; Mantle (geology); Oceanic crust; Convergent boundary; Eclogitization; Crust; Seismology; Transition zone; Petrology; Geophysics; Episodic tremor and slip; Tectonics","score_opus":0.03528861548564393,"score_gpt":0.2683668971953141,"score_spread":0.23307828170967015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974393412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99764246,0.000231863,0.000106012776,0.00006636584,0.000006394303,0.0000026984778,0.00011661606,0.0000049904615,0.001822564],"genre_scores_gemma":[0.9989737,0.0002108019,0.00013309685,0.00003113746,0.000012141228,0.0000012388444,0.00018920991,0.0000012285615,0.0004475381],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998677,0.000017804881,0.000019289895,0.00003138329,0.000032711763,0.000031171152],"domain_scores_gemma":[0.9979075,0.00054728,0.0007826082,0.0002604127,0.0002494284,0.00025267637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045663465,0.0002182069,0.00016350695,0.0011397396,0.0003873498,0.0006368956,0.0004719547,0.0004885971,0.0042197895],"category_scores_gemma":[0.0016728697,0.00021097779,0.00016659129,0.0011496816,0.0013738719,0.00041666604,0.00054737466,0.00030844833,0.0002725358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035398337,0.000047682413,0.97007746,0.000071989234,0.00007196617,0.0017241624,0.0007575441,0.00013352753,0.0190341,0.0007517148,0.00014237946,0.0068335007],"study_design_scores_gemma":[0.000009197652,0.000075715536,0.9956371,0.000007578615,0.000020139396,0.0014333139,0.00047407064,0.00005748774,0.0012718989,0.00024110147,0.0007698149,0.0000026549453],"about_ca_topic_score_codex":0.004626715,"about_ca_topic_score_gemma":0.0071694483,"teacher_disagreement_score":0.004626715,"about_ca_system_score_codex":0.0002576829,"about_ca_system_score_gemma":0.0002970092,"threshold_uncertainty_score":0.014116645},"labels":[],"label_agreement":null},{"id":"W1974708490","doi":"10.1130/b25455.1","title":"Evidence for possible precursor events of megathrust earthquakes on the west coast of North America","year":2005,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Nova scotia; Library science; Archaeology; Geological survey; Oceanography; Geology; Geography; Paleontology; Computer science","score_opus":0.04256742151250408,"score_gpt":0.24875493778939564,"score_spread":0.20618751627689155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974708490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.942162,0.004344041,0.0002985026,0.0033082752,0.00016960158,0.00006511629,0.0047421637,0.000056580266,0.0448538],"genre_scores_gemma":[0.985283,0.0038782007,0.0006966923,0.00035563615,0.00008967406,0.00003941516,0.005233025,0.000020506162,0.0044038044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99961734,0.000043713455,0.000059919712,0.000060939048,0.00014808985,0.00006989874],"domain_scores_gemma":[0.99639446,0.0004793432,0.0010336183,0.00019897246,0.0014431796,0.00045039016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056312815,0.00018140495,0.00028568294,0.0023262016,0.0010468184,0.0010635093,0.0005653856,0.00049718743,0.0055532446],"category_scores_gemma":[0.003569071,0.00032249,0.00014942292,0.0035193411,0.00051929546,0.00074136455,0.0011580135,0.0004336749,0.00078714476],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013025204,0.00005172887,0.94102705,0.0003688558,0.00008013872,0.0009620092,0.0054226983,0.000119137905,0.0029874884,0.00093618204,0.01846399,0.029450348],"study_design_scores_gemma":[0.000007176188,0.0000117339305,0.9909599,0.00009256962,0.000014773784,0.00010592209,0.002136935,0.00004117299,0.00011642478,0.00007809148,0.0064286217,0.000006861333],"about_ca_topic_score_codex":0.22151005,"about_ca_topic_score_gemma":0.5221116,"teacher_disagreement_score":0.77848995,"about_ca_system_score_codex":0.001060547,"about_ca_system_score_gemma":0.0019046301,"threshold_uncertainty_score":0.44044143},"labels":[],"label_agreement":null},{"id":"W1974719076","doi":"10.1029/2010jb007502","title":"Tidal modulation of slow slip in Cascadia","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Episodic tremor and slip; Slip (aerodynamics); Geology; Seismology; Amplitude; Subduction; Borehole; Geodesy; Strain rate; Geotechnical engineering; Physics; Tectonics","score_opus":0.03137333329211195,"score_gpt":0.3011789133627336,"score_spread":0.26980558007062166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974719076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980451,0.00005573109,0.00013282117,0.00006375832,0.00000457937,0.000003328244,0.00027011998,0.00004069154,0.0013839775],"genre_scores_gemma":[0.99949014,0.000028966428,0.00003839705,0.0000051419483,0.0000027073925,0.0000023382713,0.00020400641,0.0000060929924,0.00022215313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981433,0.00002539735,0.000020081361,0.000051616626,0.000048439877,0.000040240073],"domain_scores_gemma":[0.9992625,0.000094575145,0.00022849489,0.000092024056,0.00017411844,0.00014820145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002551786,0.0002830982,0.00033310853,0.0014689909,0.0005280222,0.00064301264,0.00025516012,0.00025599985,0.0015923687],"category_scores_gemma":[0.001998322,0.00031395868,0.00024094891,0.0013073718,0.00044199257,0.00020344695,0.00079099316,0.00021427355,0.00027907707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015682961,0.000022850292,0.9786269,0.000035549296,0.0000957771,0.00035517124,0.000790895,0.003550334,0.008584819,0.00017008958,0.0005203044,0.007090447],"study_design_scores_gemma":[0.0000036979561,0.0000137291745,0.9979044,0.0000036269362,0.000011482493,0.000034717243,0.00013159956,0.0012955342,0.0001318068,0.000062612315,0.0004006181,0.0000060860007],"about_ca_topic_score_codex":0.05908871,"about_ca_topic_score_gemma":0.099636346,"teacher_disagreement_score":0.9409113,"about_ca_system_score_codex":0.0010885419,"about_ca_system_score_gemma":0.0004675288,"threshold_uncertainty_score":0.11748952},"labels":[],"label_agreement":null},{"id":"W1974829434","doi":"10.2113/gssgfbull.180.5.431","title":"The late Cretaceous-Eocene instability of the Apulian passive margin in Albania (Kruja carbonate platform) and its impacts on sedimentation","year":2009,"lang":"en","type":"article","venue":"Bulletin de la Société Géologique de France","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Cretaceous; Paleontology; Massif; Carbonate platform; Facies; Structural basin","score_opus":0.007823795822493316,"score_gpt":0.23187215380616058,"score_spread":0.22404835798366726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974829434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987841,0.00011407515,0.000022063918,0.000016377648,0.0000012182733,0.0000016778357,0.00005368278,0.0000038471403,0.0010030536],"genre_scores_gemma":[0.9997526,0.00003143671,0.000018211114,0.000001265098,0.000001225123,7.974697e-7,0.000043708867,0.0000012877795,0.00014944274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999187,0.000008586014,0.0000076270817,0.000022926537,0.000015271171,0.000026939302],"domain_scores_gemma":[0.9998975,0.000011159102,0.000034901488,0.000010662834,0.000025685436,0.00002010739],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010578263,0.00015083353,0.00011009157,0.0014622513,0.0003226939,0.0007253181,0.00022672082,0.00012473125,0.0012947731],"category_scores_gemma":[0.00027182087,0.000089584384,0.00013985462,0.00082573737,0.00036229222,0.00022469876,0.0004899998,0.00012098432,0.00018806208],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017640786,0.000041148345,0.9112782,0.00011438885,0.00011176994,0.0018042058,0.0016736027,0.001325853,0.033091865,0.00085752417,0.00034321498,0.0491819],"study_design_scores_gemma":[0.0000018814256,0.000008273498,0.9984187,0.000004614866,0.0000064420306,0.00012922024,0.00015386709,0.00021709915,0.00032759213,0.000023287152,0.00070722017,0.0000017711242],"about_ca_topic_score_codex":0.015104231,"about_ca_topic_score_gemma":0.026428828,"teacher_disagreement_score":0.015104231,"about_ca_system_score_codex":0.0006819665,"about_ca_system_score_gemma":0.00033089513,"threshold_uncertainty_score":0.030032635},"labels":[],"label_agreement":null},{"id":"W1975318531","doi":"10.1080/00288306.2012.690766","title":"Temporal and spatial evolution of hypocentres and anisotropy from the Darfield aftershock sequence: implications for fault geometry and age","year":2012,"lang":"en","type":"article","venue":"New Zealand Journal of Geology and Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"University of Auckland; Earthquake Commission; National Science Foundation","keywords":"Aftershock; Geology; Seismology; Induced seismicity; Fault (geology); Anisotropy; Stress field; Slip (aerodynamics); Fault plane; Strike-slip tectonics","score_opus":0.018453045033814192,"score_gpt":0.23877214931546414,"score_spread":0.22031910428164994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975318531","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990631,0.000090380556,0.000056636156,0.0000196943,0.0000016908158,0.0000028684444,0.0002906165,0.000004330235,0.00047063353],"genre_scores_gemma":[0.99944764,0.000052028277,0.000040097926,0.0000034098057,0.000004719302,0.000001843031,0.00028378353,0.0000015077826,0.00016499426],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999049,0.000015771258,0.000006698522,0.000020143409,0.00002400737,0.000028609144],"domain_scores_gemma":[0.9987685,0.00020735242,0.0005058107,0.00004525718,0.0002931523,0.00017996099],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035328127,0.00013400064,0.00017268794,0.0017301694,0.0001740514,0.00043481367,0.00012622097,0.00020452036,0.0018152359],"category_scores_gemma":[0.0014503256,0.00012037785,0.00009282264,0.00082444993,0.00024194157,0.00026225383,0.0002484271,0.00017670268,0.0003083557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015812341,0.000017714241,0.9866541,0.000012294145,0.000011925944,0.00010343003,0.00036740254,0.0001510598,0.006764141,0.00004940725,0.00013511037,0.005575233],"study_design_scores_gemma":[6.048617e-7,0.000007550609,0.99973124,0.0000011136555,0.0000010456517,0.000019153948,0.000036885427,0.000049807317,0.00007906638,0.0000038822673,0.00006871346,8.364041e-7],"about_ca_topic_score_codex":0.013871172,"about_ca_topic_score_gemma":0.02708305,"teacher_disagreement_score":0.013871172,"about_ca_system_score_codex":0.00026659324,"about_ca_system_score_gemma":0.00016078987,"threshold_uncertainty_score":0.027580857},"labels":[],"label_agreement":null},{"id":"W1975980346","doi":"10.1785/0120070160","title":"Identifying the Rupture Plane of the 2001 Nisqually, Washington, Earthquake","year":2008,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Seismology; Fault plane; Geology; Plane (geometry); Geometry; Mathematics; Fault (geology)","score_opus":0.028725979740466662,"score_gpt":0.21913083639161293,"score_spread":0.19040485665114626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975980346","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99544466,0.000052748648,0.0014454172,0.00003233671,0.0000059990857,0.00001382327,0.00019838053,0.000019812556,0.0027868852],"genre_scores_gemma":[0.99689496,0.00006645731,0.0018227649,0.0000039332444,0.0000024072488,0.0000038207154,0.00051986985,0.000003501738,0.00068226975],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997914,0.000002210337,0.0000016775763,0.000006191434,0.0000053299786,0.0000054291304],"domain_scores_gemma":[0.99990356,0.0000067245637,0.000028987391,0.000009866132,0.000030535255,0.000020407299],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000940593,0.00014885452,0.000060424638,0.00055622513,0.00024529392,0.00036133023,0.00010562158,0.00018845177,0.0007155014],"category_scores_gemma":[0.00046209412,0.00010318218,0.000055345663,0.00026727378,0.0001525638,0.0001990508,0.00025400185,0.00018835424,0.00015712251],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003482908,0.00007449023,0.8858886,0.00003991824,0.000033711705,0.0007986793,0.0006268099,0.0069137076,0.03883392,0.002302637,0.0015700756,0.062569365],"study_design_scores_gemma":[0.000032258886,0.0001037172,0.9538171,0.000033083586,0.000022252974,0.000321007,0.0011905459,0.03224252,0.008860478,0.0007504383,0.0026092536,0.000017232554],"about_ca_topic_score_codex":0.011215577,"about_ca_topic_score_gemma":0.04097887,"teacher_disagreement_score":0.011215577,"about_ca_system_score_codex":0.00027017505,"about_ca_system_score_gemma":0.0002831951,"threshold_uncertainty_score":0.022300601},"labels":[],"label_agreement":null},{"id":"W1976741622","doi":"10.1007/s12517-014-1483-y","title":"Historical seismicity of the Jordan Dead Sea Transform region and seismotectonic implications","year":2014,"lang":"en","type":"article","venue":"Arabian Journal of Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Induced seismicity; Dead sea; Seismology; Oceanography","score_opus":0.01907167711480918,"score_gpt":0.20807161605344485,"score_spread":0.18899993893863568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976741622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9820858,0.0034162223,0.00021332542,0.0008125936,0.000045917535,0.000005883024,0.0013842002,0.0000129361815,0.012023175],"genre_scores_gemma":[0.9966941,0.0013165686,0.000115527364,0.00005575292,0.00004201241,0.0000022522895,0.00057681603,0.0000049001433,0.0011920301],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977165,0.000038631988,0.000030204434,0.000048181973,0.00004822873,0.00006306038],"domain_scores_gemma":[0.99907374,0.000072812494,0.00029996954,0.000040829815,0.00041436282,0.000098206685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055034744,0.0001742299,0.00009404127,0.0026562586,0.0007902545,0.001125415,0.0003776635,0.0003417965,0.0039283726],"category_scores_gemma":[0.001729463,0.00013739918,0.00010424634,0.0038902708,0.00086072064,0.00095427106,0.0006960691,0.00046065505,0.00064766733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004368876,0.000113055496,0.82197577,0.00034776848,0.00009189673,0.002559935,0.015146528,0.0024751604,0.003707932,0.011022824,0.006786443,0.13533585],"study_design_scores_gemma":[0.0000071519444,0.00005276509,0.9525893,0.00011331905,0.000025355721,0.0012393601,0.008774374,0.0004575533,0.00074339594,0.0006116697,0.035368163,0.000017552393],"about_ca_topic_score_codex":0.017513782,"about_ca_topic_score_gemma":0.040004767,"teacher_disagreement_score":0.017513782,"about_ca_system_score_codex":0.0014519742,"about_ca_system_score_gemma":0.0008313717,"threshold_uncertainty_score":0.034823656},"labels":[],"label_agreement":null},{"id":"W1976863828","doi":"10.1029/2005jb004092","title":"Gravity changes from a stress evolution earthquake simulation of California","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Geodesy; Seismology; Slip (aerodynamics); Fault (geology); SIGNAL (programming language); Physics; Computer science","score_opus":0.03019203010935593,"score_gpt":0.29075971962838565,"score_spread":0.2605676895190297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976863828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910512,0.000052123512,0.00092822826,0.00013199724,0.000014744994,0.000028896096,0.0025642368,0.00013485918,0.005093749],"genre_scores_gemma":[0.996696,0.000045741373,0.0010057811,0.000013790355,0.0000032088515,0.000021366235,0.0014197815,0.000014823958,0.00077939226],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998971,0.00001380011,0.0000059487493,0.00003524032,0.000021659147,0.00002620592],"domain_scores_gemma":[0.99975437,0.00007653329,0.000029599103,0.000019075675,0.000069140944,0.000051311406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001832783,0.00049360236,0.00039985657,0.00048006585,0.0004960837,0.00066328695,0.0008658011,0.00073544146,0.0020846357],"category_scores_gemma":[0.0007000927,0.00039180525,0.0003953013,0.00071831484,0.00040142573,0.0002728821,0.00039402023,0.0005969879,0.000147191],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009049153,0.00007020855,0.014939628,0.000023180117,0.00003998242,0.0000833403,0.00004909913,0.9806675,0.0006362844,0.0006588034,0.0012050369,0.0015364514],"study_design_scores_gemma":[0.00013525742,0.00006787259,0.018995322,0.0000074498357,0.000030761905,0.00001623766,0.00005644636,0.9792351,0.00031185144,0.0002634021,0.0008598895,0.00002035597],"about_ca_topic_score_codex":0.3472597,"about_ca_topic_score_gemma":0.29424307,"teacher_disagreement_score":0.3472597,"about_ca_system_score_codex":0.0022038533,"about_ca_system_score_gemma":0.0014570631,"threshold_uncertainty_score":0.69047683},"labels":[],"label_agreement":null},{"id":"W1977237358","doi":"10.1111/j.1440-1738.2007.00589.x","title":"Oceanic crust and Moho of the Pacific Plate in the eastern Ogasawara Plateau region","year":2007,"lang":"en","type":"article","venue":"Island Arc","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of British Columbia; University of Tokyo","keywords":"Geology; Crust; Plateau (mathematics); Oceanic crust; Magmatism; Transition zone; Seismology; Fracture zone; Geophysics; Subduction; Tectonics","score_opus":0.018350684507972795,"score_gpt":0.20687022558848855,"score_spread":0.18851954108051577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977237358","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99927145,0.00013083777,0.00004528252,0.000008743301,0.0000011132643,0.0000023135094,0.00009137555,0.0000031033762,0.00044592406],"genre_scores_gemma":[0.99934727,0.00011679217,0.000105229454,0.000006073871,0.0000023981527,0.0000035967796,0.00024175104,0.0000014916506,0.00017537698],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993765,0.0000057109983,0.000007248055,0.000018017583,0.0000137785755,0.000017513494],"domain_scores_gemma":[0.99985445,0.000017730548,0.000042956384,0.000010442504,0.00004386633,0.000030628304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017666847,0.00034089977,0.00019072094,0.0015122663,0.00049174717,0.00070800324,0.00021320241,0.00025076634,0.0006656376],"category_scores_gemma":[0.00024055412,0.00019315993,0.00026015594,0.0017423574,0.00040039018,0.0003409783,0.000562026,0.0001558973,0.00009237848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012213291,0.000022358896,0.9673606,0.000080269376,0.00011245242,0.0007860547,0.0012717077,0.0005394227,0.017951244,0.000060843027,0.00006094146,0.011631986],"study_design_scores_gemma":[0.0000020485359,0.000011057121,0.99887687,0.000007414789,0.000011452521,0.000045790996,0.0005633863,0.0001690304,0.00015748231,0.000011539571,0.00014157325,0.0000024091378],"about_ca_topic_score_codex":0.043705855,"about_ca_topic_score_gemma":0.062651135,"teacher_disagreement_score":0.043705855,"about_ca_system_score_codex":0.00034273556,"about_ca_system_score_gemma":0.0003977161,"threshold_uncertainty_score":0.08690292},"labels":[],"label_agreement":null},{"id":"W1977529815","doi":"10.1016/j.marpetgeo.2014.02.021","title":"Seismic Stratigraphy and Depositional Facies Models","year":2014,"lang":"en","type":"article","venue":"Marine and Petroleum Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Stratigraphy; Sedimentary depositional environment; Facies; Paleontology; Tectonics; Structural basin","score_opus":0.009000757861012832,"score_gpt":0.17979845527534571,"score_spread":0.17079769741433287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977529815","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7496941,0.000544606,0.1705029,0.0008676915,0.00015773786,0.00014574474,0.027118959,0.006199772,0.044768482],"genre_scores_gemma":[0.96902084,0.0002967353,0.014605092,0.00004598598,0.000030145377,0.00007380714,0.005157057,0.0002206422,0.010549602],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99992406,0.000017351034,0.000006199435,0.000023508903,0.000012554701,0.000016355718],"domain_scores_gemma":[0.9997986,0.000081987135,0.000021372656,0.000037863403,0.00004016571,0.000020126869],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018836842,0.00055907614,0.0004603882,0.00089283293,0.00038679078,0.00071049837,0.0013047141,0.0009821011,0.010180473],"category_scores_gemma":[0.001239616,0.00060251635,0.0008001941,0.0011991075,0.0002605101,0.00069445703,0.0003498426,0.0003845312,0.0016973458],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027349504,0.00001381678,0.0019561849,0.000010059219,0.000022216887,0.000028891516,0.000013777227,0.99196154,0.00020627103,0.0012084838,0.00051231857,0.004039116],"study_design_scores_gemma":[0.000017369728,0.0000057393404,0.00090613833,0.0000033297886,0.000011913984,0.000011101422,0.000007720755,0.9969668,0.00010979787,0.0012516675,0.0007030492,0.000005470159],"about_ca_topic_score_codex":0.070456564,"about_ca_topic_score_gemma":0.060143724,"teacher_disagreement_score":0.070456564,"about_ca_system_score_codex":0.0009665282,"about_ca_system_score_gemma":0.0009439353,"threshold_uncertainty_score":0.14009291},"labels":[],"label_agreement":null},{"id":"W1977954145","doi":"10.1002/2014jb011492","title":"Geodetic imaging of potential seismogenic asperities on the Xianshuihe‐Anninghe‐Zemuhe fault system, southwest China, with a new 3‐D viscoelastic interseismic coupling model","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Geology; Viscoelasticity; Seismology; Geodesy; Asperity (geotechnical engineering); Slip (aerodynamics); Interferometric synthetic aperture radar; Geodetic datum; Crust; Synthetic aperture radar; Remote sensing; Geophysics; Materials science; Geotechnical engineering; Physics","score_opus":0.04316034868720262,"score_gpt":0.2867110519182586,"score_spread":0.24355070323105596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977954145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961516,0.000027998876,0.0033228758,0.000032665364,0.0000022661675,0.0000064520973,0.000099577905,0.00005114742,0.0003053463],"genre_scores_gemma":[0.9972366,0.000024795494,0.0024618085,0.0000054223583,0.0000023855546,0.00000395015,0.000108885535,0.0000029126859,0.00015318798],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999536,0.0000055567293,0.0000025530198,0.000016142492,0.000012365458,0.000009805484],"domain_scores_gemma":[0.99993885,0.0000063161074,0.000015256719,0.000013151312,0.000010458316,0.000015907426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001320241,0.00032092916,0.00017835615,0.0007130315,0.00017666325,0.00029058303,0.00031168107,0.00028960672,0.00038128573],"category_scores_gemma":[0.00015526755,0.00026748283,0.0003299677,0.00046236135,0.00018503053,0.00023665896,0.00029737328,0.00016209079,0.000062751715],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034031674,0.0002305092,0.29999408,0.00008950539,0.00021367763,0.00049571646,0.0004895988,0.47310555,0.16560982,0.0007336957,0.00048657393,0.0582109],"study_design_scores_gemma":[0.000026564234,0.00005417987,0.15408263,0.00000478244,0.000032118885,0.000042117656,0.00006796929,0.84230226,0.0030346757,0.00010446123,0.00022900292,0.000019319146],"about_ca_topic_score_codex":0.02101796,"about_ca_topic_score_gemma":0.031625792,"teacher_disagreement_score":0.02101796,"about_ca_system_score_codex":0.00053641264,"about_ca_system_score_gemma":0.00051932194,"threshold_uncertainty_score":0.04179126},"labels":[],"label_agreement":null},{"id":"W1978210661","doi":"10.1029/2005jb004108","title":"Regional <b><i>P</i></b> wave velocity structure of the Northern Cascadia Subduction Zone","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Slab; Mantle (geology); Sedimentary rock; Oceanic crust; Crust; Sedimentary basin; Volcanic arc; Geophysics; Tectonics; Paleontology","score_opus":0.028245209826667443,"score_gpt":0.25934237475629623,"score_spread":0.23109716492962878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978210661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995443,0.00007153664,0.0011708244,0.0000646088,0.0000020074046,0.0000101281485,0.00053804816,0.00012518461,0.0025745197],"genre_scores_gemma":[0.99856645,0.00003926125,0.0005133582,0.0000026166163,5.28654e-7,0.000005333094,0.0005707966,0.000008781974,0.00029295997],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992824,0.0000063466346,0.0000036835618,0.00003007475,0.000016536185,0.000015021],"domain_scores_gemma":[0.9998903,0.0000075726816,0.000024541738,0.000011759555,0.000039482413,0.000026362957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011051935,0.000269657,0.00011706726,0.0006780654,0.00036133608,0.0006680988,0.00028320373,0.00020634808,0.00072540826],"category_scores_gemma":[0.00038229793,0.00022601095,0.00031625386,0.0005965343,0.00028985532,0.00016065808,0.00027607972,0.00024935303,0.00022916995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001671975,0.00004190299,0.79653627,0.00004581177,0.00013673372,0.0002184309,0.00087547855,0.15830909,0.013092445,0.0009287728,0.0015330365,0.028114853],"study_design_scores_gemma":[0.00001905607,0.000024674808,0.9321524,0.00001501051,0.00003064025,0.00007401041,0.00037875588,0.06483318,0.00059312687,0.00023831913,0.0016164944,0.000024370758],"about_ca_topic_score_codex":0.47651672,"about_ca_topic_score_gemma":0.44423074,"teacher_disagreement_score":0.47651672,"about_ca_system_score_codex":0.0018492832,"about_ca_system_score_gemma":0.0014396543,"threshold_uncertainty_score":0.94748616},"labels":[],"label_agreement":null},{"id":"W1978227080","doi":"10.1785/0120140171","title":"Shear-Wave Velocity Structure in the Vicinity of the 2012 Mw 7.8 Haida Gwaii Earthquake from Receiver Function Inversion","year":2015,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Seismology; Geology; Receiver function; Shear (geology); Wave velocity; Inversion (geology); Petrology","score_opus":0.029303903039009774,"score_gpt":0.20396793527930013,"score_spread":0.17466403224029037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978227080","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999253,0.000011165818,0.00018831756,0.000009517107,0.0000013414586,0.0000022537606,0.00013445993,0.000013816917,0.00038612777],"genre_scores_gemma":[0.9983619,0.00002121489,0.00045129002,0.000003542569,0.0000022437957,0.0000035027997,0.00082002004,0.000005281081,0.00033103742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994314,0.000004281739,0.0000030922788,0.000014445026,0.000013992404,0.000021109068],"domain_scores_gemma":[0.9998241,0.000023737619,0.00004488536,0.000014251477,0.00006323214,0.000029650357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014006293,0.0003508553,0.00024199185,0.0006390188,0.00021395629,0.00041374422,0.00021087803,0.00022662574,0.0008269602],"category_scores_gemma":[0.00055310276,0.00022785072,0.00017637796,0.00078964926,0.00022806526,0.0002762764,0.0003816343,0.0002961304,0.00021319366],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007163544,0.0001571302,0.7660962,0.00009443563,0.00013437738,0.0010899854,0.0022565925,0.011506372,0.16300534,0.00032440573,0.0011728558,0.053445965],"study_design_scores_gemma":[0.000016152126,0.000037185884,0.98356354,0.000008605337,0.000032029588,0.00006938578,0.0002518837,0.013519354,0.0021740794,0.000022030858,0.00029181424,0.000014009543],"about_ca_topic_score_codex":0.0638571,"about_ca_topic_score_gemma":0.13962689,"teacher_disagreement_score":0.9361429,"about_ca_system_score_codex":0.00041593207,"about_ca_system_score_gemma":0.0005451568,"threshold_uncertainty_score":0.12697083},"labels":[],"label_agreement":null},{"id":"W1978334180","doi":"10.1007/s00024-012-0457-9","title":"Optimization of Seismicity-Based Forecasts","year":2012,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Institute for Catastrophic Loss Reduction","keywords":"Induced seismicity; Metric (unit); Discretization; Estimation; Magnitude (astronomy); Forecast skill; Cutoff; Computer science; Statistics; Geology; Econometrics; Seismology; Mathematics; Engineering; Physics","score_opus":0.012282919046320529,"score_gpt":0.19175581994981597,"score_spread":0.17947290090349544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978334180","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13316137,0.00089145266,0.8537294,0.0016098999,0.00017897382,0.00011501798,0.0006721437,0.0009544733,0.008687177],"genre_scores_gemma":[0.9151812,0.0002666202,0.07967922,0.00017032052,0.00013293093,0.00013603218,0.00052327174,0.00015258612,0.0037577976],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995022,0.00020767024,0.000029886764,0.00009941394,0.000080222366,0.00008067195],"domain_scores_gemma":[0.9970445,0.0022966773,0.00022578589,0.000081408674,0.00025373278,0.000097866556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016215282,0.0010277629,0.0016389248,0.0009936506,0.00035286407,0.0011807515,0.0010344555,0.0020974712,0.0032785812],"category_scores_gemma":[0.0074936594,0.0012075871,0.00069408683,0.000813491,0.00080918625,0.001239257,0.0012662822,0.0010790629,0.0004631772],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041986128,0.000010025848,0.00016410009,0.000013045032,0.000010814082,0.000011499592,0.000007504424,0.99355173,0.00022548447,0.0007417289,0.0003201961,0.004901865],"study_design_scores_gemma":[0.000006293966,0.0000070827414,0.000048358615,0.0000013995844,0.0000023176478,0.0000017493854,0.000001918325,0.9992895,0.00009265284,0.000490505,0.000056467168,0.000001730519],"about_ca_topic_score_codex":0.012235833,"about_ca_topic_score_gemma":0.0079545,"teacher_disagreement_score":0.012235833,"about_ca_system_score_codex":0.0013383465,"about_ca_system_score_gemma":0.0021869775,"threshold_uncertainty_score":0.024329185},"labels":[],"label_agreement":null},{"id":"W1978669352","doi":"10.1029/2005eo020004","title":"Seismic imaging of the ocean internal structure: A new tool in physical oceanography?","year":2005,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seafloor spreading; Reflection (computer programming); Oceanography; Seabed; Physical oceanography; Water column; Solid earth; Internal wave; Front (military); Seismology; Current (fluid); Geophysics","score_opus":0.006463508053537239,"score_gpt":0.20181247789313056,"score_spread":0.19534896983959332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978669352","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02393344,0.6843622,0.1617133,0.09506639,0.010055495,0.000058156707,0.0007365357,0.00070530735,0.023369094],"genre_scores_gemma":[0.15542401,0.6623544,0.12585248,0.013034661,0.029610004,0.00009369921,0.00053172786,0.00023820718,0.012860747],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9994252,0.00016471354,0.000047637153,0.00010440574,0.0002147022,0.00004335766],"domain_scores_gemma":[0.9978568,0.0009579861,0.00022153389,0.0003387578,0.00042548848,0.00019944222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016753409,0.0007619024,0.001162761,0.0026752073,0.0004102339,0.0027598238,0.0011039433,0.002192004,0.0035199765],"category_scores_gemma":[0.0038671717,0.0004359037,0.00044140394,0.0036141395,0.006035321,0.008338365,0.0021141616,0.002074935,0.0012162396],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019975877,0.00008142038,0.009334805,0.0019134888,0.000115431816,0.00037979527,0.0008255723,0.0011736053,0.010551866,0.10343107,0.027822081,0.84417117],"study_design_scores_gemma":[0.00009642422,0.0005212003,0.01658637,0.0017130342,0.00016108075,0.004155167,0.0028070286,0.007378297,0.0059351786,0.22852646,0.7318464,0.0002733488],"about_ca_topic_score_codex":0.0018913704,"about_ca_topic_score_gemma":0.001909686,"teacher_disagreement_score":0.0035199765,"about_ca_system_score_codex":0.0007320414,"about_ca_system_score_gemma":0.0007044872,"threshold_uncertainty_score":0.011775494},"labels":[],"label_agreement":null},{"id":"W1979136251","doi":"10.1016/j.tecto.2014.01.019","title":"Source to sink: The development of the latest Messinian to Pliocene–Quaternary Cilicia and Adana Basins and their linkages with the onland Mut Basin, eastern Mediterranean","year":2014,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland","keywords":"Geology; Structural basin; Quaternary; Subsidence; Late Miocene; Isopach map; Sedimentary rock; Paleontology; Facies","score_opus":0.013767390958777045,"score_gpt":0.19279873876241369,"score_spread":0.17903134780363664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979136251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916391,0.0005458328,0.00015031603,0.00031397791,0.000010378138,0.000005655285,0.00021051557,0.000011370925,0.0071129855],"genre_scores_gemma":[0.99882334,0.0002078786,0.00010001843,0.000026726872,0.000010726722,0.00000303838,0.00009272724,0.0000076263595,0.00072792027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994266,0.000006587553,0.000004871311,0.000023850085,0.000006708275,0.00001533441],"domain_scores_gemma":[0.9998491,0.000019889367,0.000057398534,0.000011608979,0.00004011304,0.000021731328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022632776,0.00016526892,0.00013518006,0.00074921903,0.00044333658,0.00092045387,0.00028713178,0.0002336343,0.0029068138],"category_scores_gemma":[0.0007602311,0.00011414665,0.00017533584,0.00072682684,0.00069538783,0.0007934315,0.0006604519,0.00022299882,0.00018605734],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000327331,0.00003948518,0.9125406,0.0001752685,0.00009945952,0.00044619088,0.010886391,0.00071338884,0.010328661,0.008782711,0.00100012,0.054660376],"study_design_scores_gemma":[0.0000065311856,0.000012229191,0.9938496,0.000019970279,0.000018678187,0.000056519602,0.0010940974,0.00021210796,0.00021037544,0.000404714,0.004112973,0.0000022288475],"about_ca_topic_score_codex":0.024432521,"about_ca_topic_score_gemma":0.04589123,"teacher_disagreement_score":0.024432521,"about_ca_system_score_codex":0.0010474344,"about_ca_system_score_gemma":0.0006551757,"threshold_uncertainty_score":0.048580587},"labels":[],"label_agreement":null},{"id":"W1979930790","doi":"10.1126/science.1192223","title":"Finding Fault in Fault Zones","year":2010,"lang":"en","type":"letter","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Fault (geology); Geology; Seismology; Computer science","score_opus":0.024506095670923492,"score_gpt":0.246149998938046,"score_spread":0.22164390326712252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979930790","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011418149,0.012309042,0.0023291325,0.9257011,0.037329577,0.00002786114,0.00014001827,0.000095323216,0.010649806],"genre_scores_gemma":[0.12612516,0.01395391,0.0036764874,0.71148,0.12487553,0.00006245994,0.00023808068,0.000089510875,0.01949887],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99918,0.00018288073,0.00009622783,0.0002502758,0.00016766034,0.00012281604],"domain_scores_gemma":[0.9950275,0.0027486896,0.0003580797,0.00044462725,0.0010517639,0.0003693555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015539282,0.00040862933,0.0006969124,0.0007921246,0.001303258,0.0015457981,0.0013978521,0.0145442765,0.0035537856],"category_scores_gemma":[0.0136026405,0.000390111,0.0004364875,0.00049756834,0.002512454,0.004892987,0.0011558572,0.0117099285,0.003803061],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002498315,0.00006378718,0.005721837,0.00024056439,0.000045901354,0.009957515,0.0005766922,0.0002860887,0.0018168254,0.014807025,0.84889597,0.117338],"study_design_scores_gemma":[0.00039444078,0.00021138806,0.008038589,0.0005813795,0.0001060426,0.03448141,0.0018147323,0.0015145227,0.002564559,0.11049695,0.8396826,0.00011341223],"about_ca_topic_score_codex":0.0021970146,"about_ca_topic_score_gemma":0.0024594879,"teacher_disagreement_score":0.0145442765,"about_ca_system_score_codex":0.0016705475,"about_ca_system_score_gemma":0.00077466836,"threshold_uncertainty_score":0.012120783},"labels":[],"label_agreement":null},{"id":"W1980379728","doi":"10.1029/2009eo130002","title":"Shallow Submarine Hydrothermal Systems in the Aeolian Volcanic Arc, Italy","year":2009,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Submarine volcano; Geology; Submarine; Hydrothermal circulation; Volcano; Hydrothermal vent; Volcanic arc; Seafloor spreading; Aeolian processes; Oceanography; Geochemistry; Seismology; Geomorphology; Subduction; Tectonics","score_opus":0.01492477992263216,"score_gpt":0.20737429865062643,"score_spread":0.19244951872799426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980379728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99757224,0.00043386433,0.00013292547,0.00002669785,0.0000013918662,0.000009864046,0.00012064361,0.00001394039,0.0016884089],"genre_scores_gemma":[0.998944,0.00016891108,0.00033490258,0.000008035114,0.0000034361772,0.000008946411,0.00019210574,0.0000015821986,0.0003381145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999236,0.000013719338,0.0000064898586,0.000025453595,0.000011211845,0.000019581348],"domain_scores_gemma":[0.99986315,0.000020776573,0.00006820716,0.000011993258,0.000014657777,0.00002117791],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012475254,0.00017459494,0.00021148854,0.00083541457,0.00019800346,0.00029007345,0.00017198791,0.00023383019,0.0006326932],"category_scores_gemma":[0.00023011761,0.00015399614,0.00011937071,0.00060736464,0.0003577607,0.0002061988,0.00044337564,0.00010909897,0.00017210143],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032115035,0.000079291196,0.8576843,0.00025891644,0.000065897344,0.00075968524,0.004418748,0.0027887903,0.06891177,0.0009159145,0.0005536566,0.06324186],"study_design_scores_gemma":[0.0000051087695,0.00003787599,0.9986375,0.000005441105,0.00000596761,0.0001291363,0.00010939566,0.00025396905,0.0002500486,0.00004941911,0.00051343587,0.0000027133015],"about_ca_topic_score_codex":0.010462173,"about_ca_topic_score_gemma":0.013625142,"teacher_disagreement_score":0.010462173,"about_ca_system_score_codex":0.00033520663,"about_ca_system_score_gemma":0.00024451848,"threshold_uncertainty_score":0.020802557},"labels":[],"label_agreement":null},{"id":"W1981039334","doi":"10.1016/j.ijrmms.2013.12.023","title":"Dynamic modelling of fault-slip with Barton׳s shear strength model","year":2014,"lang":"en","type":"article","venue":"International Journal of Rock Mechanics and Mining Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Slip (aerodynamics); Geology; Joint (building); Seismic moment; Surface finish; Shear (geology); Fault (geology); Seismology; Particle flow; Moment (physics); Geotechnical engineering; Structural engineering; Mechanics; Discrete element method; Engineering; Petrology","score_opus":0.02195512732597902,"score_gpt":0.23447202027860978,"score_spread":0.21251689295263076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981039334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.61417574,0.0012807961,0.30992407,0.00085257035,0.00035933356,0.00014609286,0.0017568752,0.0012727404,0.07023186],"genre_scores_gemma":[0.9845978,0.00028094783,0.0054726037,0.000030497744,0.000024732806,0.000055423614,0.0003183565,0.000090287154,0.009129277],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998524,0.00003342895,0.000011343124,0.000029960085,0.000039790037,0.000032978543],"domain_scores_gemma":[0.999721,0.0000936699,0.00005385493,0.00002342145,0.0000731615,0.00003489553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020188173,0.00069460104,0.0013261068,0.00068894745,0.0006126565,0.0011194295,0.0016301506,0.0019413022,0.0044463826],"category_scores_gemma":[0.0007365503,0.00071118324,0.0006996748,0.0007142363,0.0006057679,0.00090297137,0.00066935236,0.00080015184,0.00077009026],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022315064,0.000015842263,0.00036562115,0.000016079148,0.000012290884,0.00006481467,0.000020842657,0.995738,0.00057385955,0.0015657718,0.00017421097,0.0014304309],"study_design_scores_gemma":[0.0000033975073,0.000004726306,0.0001149835,0.0000015293537,0.0000030469641,0.0000047153926,0.0000029382456,0.9994783,0.000061026993,0.00017572194,0.00014714511,0.0000024921685],"about_ca_topic_score_codex":0.041622143,"about_ca_topic_score_gemma":0.017191647,"teacher_disagreement_score":0.041622143,"about_ca_system_score_codex":0.00071338937,"about_ca_system_score_gemma":0.0009209307,"threshold_uncertainty_score":0.08275974},"labels":[],"label_agreement":null},{"id":"W1981370501","doi":"10.1029/2008jb006026","title":"Izmit earthquake postseismic deformation and dynamics of the North Anatolian Fault Zone","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"North Anatolian Fault; Geology; Viscoelasticity; Rheology; Seismology; Deformation (meteorology); Crust; Mantle (geology); Fault (geology); Viscosity; Geophysics; Materials science","score_opus":0.017796647734816366,"score_gpt":0.26579956573560704,"score_spread":0.24800291800079066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981370501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989974,0.000030073617,0.00023054625,0.000040970932,0.0000027422411,0.0000035423502,0.00012597715,0.000011943911,0.00055678026],"genre_scores_gemma":[0.9991417,0.000042710486,0.0003100938,0.000005791282,0.0000013706159,0.000009215936,0.00019559143,0.000004374041,0.000289053],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99996305,0.0000072032417,0.0000040661885,0.000009558092,0.0000057752636,0.0000103977545],"domain_scores_gemma":[0.9999199,0.00001689047,0.00002371844,0.000010465849,0.000019328507,0.000009662405],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013250273,0.00028380947,0.00024032622,0.0003104992,0.00041264153,0.0005110986,0.00047967426,0.0006667446,0.00076338614],"category_scores_gemma":[0.00037526074,0.00026890734,0.00031335972,0.00027137782,0.0002473859,0.0004531654,0.0002832432,0.00026995566,0.0001232946],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022830963,0.00017609824,0.18775883,0.000048166643,0.00009689048,0.0004056075,0.00037951648,0.7959672,0.0050382884,0.0009078896,0.00046237063,0.008530758],"study_design_scores_gemma":[0.000067624474,0.00009333485,0.09662344,0.000020699688,0.00006165134,0.00009932251,0.0002556869,0.89947534,0.0018285373,0.0002904638,0.0011626323,0.00002118057],"about_ca_topic_score_codex":0.067921124,"about_ca_topic_score_gemma":0.057996884,"teacher_disagreement_score":0.067921124,"about_ca_system_score_codex":0.0013612754,"about_ca_system_score_gemma":0.00071563537,"threshold_uncertainty_score":0.13505155},"labels":[],"label_agreement":null},{"id":"W1981523453","doi":"10.1126/science.1243719","title":"Structure and Composition of the Plate-Boundary Slip Zone for the 2011 Tohoku-Oki Earthquake","year":2013,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":294,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Seismology; Subduction; Plate tectonics; Slip (aerodynamics); Drilling; Borehole; Earthquake rupture; Fault (geology); Convergent boundary; Pelagic zone; Geotechnical engineering; Tectonics; Oceanography; Oceanic crust","score_opus":0.011640899970387183,"score_gpt":0.20544331209566327,"score_spread":0.1938024121252761,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981523453","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996468,0.000022813727,0.000016183698,0.0000064940486,4.5726097e-7,0.0000013706133,0.00011256738,0.000001934333,0.00019139428],"genre_scores_gemma":[0.9994429,0.00003528664,0.000045799687,0.000005871619,0.000001533586,0.0000045468346,0.0003605057,0.000001597621,0.00010193668],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993384,0.0000031615104,0.000007298204,0.00002017941,0.0000106995685,0.000024798337],"domain_scores_gemma":[0.9997203,0.00001831307,0.00014193435,0.00001262085,0.0000382104,0.00006855653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007727937,0.0001670201,0.00018791153,0.0014926454,0.0005346786,0.00038461975,0.00019112015,0.0003581617,0.00074950646],"category_scores_gemma":[0.00024694522,0.00020400852,0.00014323583,0.0011523558,0.00033557575,0.00028070083,0.0004634256,0.0001503307,0.00018478528],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013226511,0.000041388743,0.97148854,0.000037519494,0.000024163122,0.00018832038,0.0009925222,0.00039281076,0.021461451,0.00005733848,0.00014350931,0.0050402223],"study_design_scores_gemma":[8.7782587e-7,0.0000058655464,0.99952185,0.0000016029181,0.0000037319112,0.00003079558,0.00017420566,0.00011198521,0.00010005421,0.000004021719,0.000043253025,0.0000018144743],"about_ca_topic_score_codex":0.022801815,"about_ca_topic_score_gemma":0.05569,"teacher_disagreement_score":0.022801815,"about_ca_system_score_codex":0.0005042624,"about_ca_system_score_gemma":0.00036678565,"threshold_uncertainty_score":0.045338213},"labels":[],"label_agreement":null},{"id":"W1981941389","doi":"10.1016/j.jog.2003.08.002","title":"Estimation of the time-dependent crustal movements of the İzmit Earthquake","year":2003,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Geology; Geodesy; Seismology; Kinematics; Global Positioning System; Fault (geology); Deformation (meteorology); Crust; Magnitude (astronomy); Geophysics","score_opus":0.00679582725827587,"score_gpt":0.19657626933606503,"score_spread":0.18978044207778916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981941389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973967,0.000068771835,0.0021227687,0.000019371404,0.000003678282,0.0000034359662,0.00012435454,0.0000163127,0.00024467404],"genre_scores_gemma":[0.9979316,0.00004854641,0.0015648179,0.0000018018834,0.0000047342373,0.0000021161657,0.00028994787,0.0000031470151,0.00015335894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992645,0.000019677025,0.000005460643,0.000017610704,0.000015809625,0.00001492059],"domain_scores_gemma":[0.9993544,0.0003090517,0.000112867325,0.000047465994,0.00011024392,0.00006609216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003226407,0.00037222513,0.000248818,0.0014932561,0.00022235466,0.0002836864,0.00028242235,0.00030473387,0.0005021306],"category_scores_gemma":[0.0020509826,0.00022962643,0.00028922345,0.00049784494,0.00012241972,0.00038488858,0.00028164982,0.0002744615,0.00011138011],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018733415,0.00028230855,0.6519319,0.00012626244,0.0004449315,0.000608762,0.00031546428,0.16190399,0.05493012,0.0010394265,0.0006020532,0.12594144],"study_design_scores_gemma":[0.0000246526,0.00016672649,0.733877,0.000008131131,0.00010999505,0.00009370838,0.00010503942,0.26137322,0.00378844,0.000150602,0.00027772132,0.000024664949],"about_ca_topic_score_codex":0.00938568,"about_ca_topic_score_gemma":0.013004421,"teacher_disagreement_score":0.00938568,"about_ca_system_score_codex":0.0002914962,"about_ca_system_score_gemma":0.0002882737,"threshold_uncertainty_score":0.018662095},"labels":[],"label_agreement":null},{"id":"W1982291797","doi":"10.1029/2007jb004948","title":"GPS constraints on 34 slow slip events within the Cascadia subduction zone, 1997–2005","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":127,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Episodic tremor and slip; Slip (aerodynamics); Geodesy; Geodetic datum; Global Positioning System; Moment magnitude scale; Tectonics; Geometry","score_opus":0.04580833488805633,"score_gpt":0.29150674274668703,"score_spread":0.2456984078586307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982291797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99473405,0.00005967313,0.0002849478,0.00003156339,0.0000024205492,0.000007704743,0.0030912831,0.00003302079,0.0017553953],"genre_scores_gemma":[0.9913278,0.000085615786,0.0005248285,0.000010317426,0.000003891938,0.000017591336,0.007481582,0.000009383476,0.00053902],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975985,0.000022434038,0.000032443393,0.00006440434,0.00006699828,0.000053905886],"domain_scores_gemma":[0.99878424,0.00016834377,0.00036332512,0.00013881455,0.00039441846,0.00015078702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003278189,0.0003546114,0.00035330586,0.0016463342,0.00078847364,0.0005182545,0.0003939031,0.00020329299,0.0020171066],"category_scores_gemma":[0.0016427392,0.00025675612,0.00025509033,0.0018434629,0.000253597,0.0001780503,0.00053902296,0.00019119344,0.00027929829],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015555538,0.000028311397,0.9765781,0.00007803435,0.000052592568,0.00026509658,0.00092173135,0.0055958456,0.0033336545,0.00022100695,0.0018284235,0.0109416405],"study_design_scores_gemma":[0.000004265551,0.000010812444,0.99663794,0.000011078252,0.000012898108,0.000028505065,0.00021363393,0.0014100182,0.00024215307,0.000023052691,0.0014008605,0.000004671804],"about_ca_topic_score_codex":0.206922,"about_ca_topic_score_gemma":0.44620165,"teacher_disagreement_score":0.206922,"about_ca_system_score_codex":0.0013384548,"about_ca_system_score_gemma":0.0012224911,"threshold_uncertainty_score":0.41143513},"labels":[],"label_agreement":null},{"id":"W1983077457","doi":"10.2118/149307-ms","title":"The Stability of Fault Systems in the South Shore of the St. Lawrence Lowlands of Québec – Implications for Shale Gas Development","year":2011,"lang":"en","type":"article","venue":"Canadian Unconventional Resources Conference","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Effigis (Canada)","funders":"","keywords":"Geology; Lineament; Shore; Oil shale; Ordovician; Fault (geology); Shale gas; Seismology; Aquifer; Lead (geology); Geochemistry; Tectonics; Paleontology; Groundwater; Oceanography; Geotechnical engineering","score_opus":0.06853641679686379,"score_gpt":0.2208071949632487,"score_spread":0.1522707781663849,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983077457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992324,0.00034874244,0.00019005097,0.00031084748,0.0000036036593,0.000017820948,0.001496119,0.000016061347,0.005292853],"genre_scores_gemma":[0.9975453,0.000091382004,0.00012340577,0.000023989327,0.0000013577237,0.000005283015,0.00054895127,0.000001941736,0.0016584286],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978,0.000025359377,0.00000984281,0.000040036084,0.000054196673,0.000090530666],"domain_scores_gemma":[0.9987097,0.00008951443,0.00022572534,0.00003332203,0.0007895193,0.00015219761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021142968,0.00014637935,0.00017469485,0.0011204308,0.0014017331,0.0014307601,0.00060547295,0.00024115967,0.0040961537],"category_scores_gemma":[0.0010161662,0.000106973326,0.00010553338,0.002135961,0.00074332696,0.00032524602,0.00037850707,0.00017540104,0.00026596338],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013282982,0.00003859814,0.9624957,0.000080024736,0.00005409862,0.00030700443,0.0021531612,0.0022245392,0.0032619203,0.0009568729,0.0023019535,0.025993261],"study_design_scores_gemma":[0.000006141388,0.000012657001,0.99441284,0.000026439931,0.000007443216,0.000036642836,0.0017209623,0.0011239339,0.00015343621,0.00005386246,0.0024374803,0.000008083819],"about_ca_topic_score_codex":0.9939825,"about_ca_topic_score_gemma":0.99810994,"teacher_disagreement_score":0.01784624,"about_ca_system_score_codex":0.01784624,"about_ca_system_score_gemma":0.008734048,"threshold_uncertainty_score":0.12948418},"labels":[],"label_agreement":null},{"id":"W1983183835","doi":"10.1002/2014jb011430","title":"Tidal modulation and triggering of low‐frequency earthquakes in northern Cascadia","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Slip (aerodynamics); Seismology; Shear (geology); Shear stress; Episodic tremor and slip; Low frequency; Tidal force; Subduction; Petrology; Mechanics; Tectonics; Physics","score_opus":0.028395886563947603,"score_gpt":0.29313937714228266,"score_spread":0.2647434905783351,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983183835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99906963,0.000037016336,0.000030629522,0.000023750696,0.0000012223787,0.0000019248166,0.00042517993,0.000010518452,0.0004001298],"genre_scores_gemma":[0.99943155,0.00002727932,0.000017557813,0.0000028222628,0.0000014527044,0.0000019291401,0.0003846594,0.000001972534,0.00013079858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998056,0.00003070484,0.000018239387,0.000056427896,0.00004668713,0.000042338303],"domain_scores_gemma":[0.9985714,0.00021341893,0.00046443765,0.00013330742,0.00027966895,0.00033774562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003537735,0.00024993523,0.000282946,0.0016421129,0.0004428099,0.0006309863,0.00023994363,0.00020370433,0.0013090159],"category_scores_gemma":[0.0018819099,0.00019421964,0.0002743644,0.0016398317,0.0004172046,0.0002206217,0.0006828705,0.00019836873,0.00020297126],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005443162,0.000010832296,0.9945846,0.000015903168,0.000057225072,0.00013579625,0.00039347776,0.0008270052,0.0015457728,0.000021829937,0.00017536992,0.0021777747],"study_design_scores_gemma":[7.2445744e-7,0.0000036531906,0.9995722,0.0000014756228,0.0000038805842,0.000010268252,0.00009536637,0.00020826253,0.0000344167,0.000005334603,0.000062928455,0.0000015627177],"about_ca_topic_score_codex":0.21871586,"about_ca_topic_score_gemma":0.34861365,"teacher_disagreement_score":0.78128415,"about_ca_system_score_codex":0.001169669,"about_ca_system_score_gemma":0.0005956946,"threshold_uncertainty_score":0.43488556},"labels":[],"label_agreement":null},{"id":"W1983335362","doi":"10.1007/s11069-004-4809-3","title":"Estimation of Tsunami Risk for the Coasts of Peru and Northern Chile","year":2005,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Russian Foundation for Basic Research","keywords":"Geology; Seismology; Natural hazard; Return period; Latitude; Tsunami wave; Estimation; Magnitude (astronomy); Earthquake magnitude; Geography; Geodesy; Oceanography","score_opus":0.007220297663546317,"score_gpt":0.22446550920709674,"score_spread":0.21724521154355042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983335362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984108,0.00010081325,0.00025915456,0.00005338519,6.407542e-7,0.000011090415,0.00025522918,0.0000075613475,0.0009013929],"genre_scores_gemma":[0.9987895,0.00009929465,0.00033599534,0.0000034616046,0.0000013329114,0.000013202986,0.00038204453,0.000002359421,0.00037276497],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987924,0.000055886143,0.000010016346,0.000018595689,0.000015425296,0.00002084069],"domain_scores_gemma":[0.9991067,0.00045253514,0.00017030354,0.00005147209,0.00013148997,0.0000874208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044428426,0.00036098334,0.00020004818,0.0017187559,0.00033192322,0.0006562018,0.00038982285,0.00034492652,0.001527322],"category_scores_gemma":[0.0027148242,0.00018878179,0.0003759176,0.0009940976,0.00024426635,0.0004885752,0.00075286266,0.00026857297,0.00013892078],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000261358,0.0000715871,0.9449067,0.00007507775,0.00020474744,0.00066563045,0.0006124454,0.036112428,0.0014936904,0.001008109,0.0004304235,0.014157827],"study_design_scores_gemma":[0.00006367355,0.00013597844,0.9418477,0.000034503675,0.0001041731,0.0002206807,0.0026372015,0.052302524,0.00058274006,0.0008062116,0.0012390729,0.000025551077],"about_ca_topic_score_codex":0.07226034,"about_ca_topic_score_gemma":0.053589124,"teacher_disagreement_score":0.07226034,"about_ca_system_score_codex":0.0012274472,"about_ca_system_score_gemma":0.0007754131,"threshold_uncertainty_score":0.1436795},"labels":[],"label_agreement":null},{"id":"W1984043114","doi":"10.1029/2008jb005806","title":"Hydrologic detection and finite element modeling of a slow slip event in the Costa Rica prism toe","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Achievement Rewards for College Scientists Foundation; National Science Foundation","keywords":"Geology; Seafloor spreading; Subduction; Seismology; Slip (aerodynamics); Episodic tremor and slip; Trench; Décollement; Geophysics; Tectonics","score_opus":0.038555776626111864,"score_gpt":0.29651364112445433,"score_spread":0.25795786449834246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984043114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995561,0.000029393996,0.002989702,0.00007410045,0.000002632059,0.000008642766,0.0001510211,0.00006206352,0.0011213879],"genre_scores_gemma":[0.9984819,0.000021406848,0.0010510837,0.000007357089,0.0000012290427,0.000009562977,0.0000813482,0.000007155347,0.00033896277],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999473,0.000012393301,0.000003382845,0.000015758005,0.000008848371,0.000012321789],"domain_scores_gemma":[0.9998223,0.00007730168,0.00003555096,0.000017219969,0.000029030072,0.000018642964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016121235,0.00040857424,0.00025309916,0.00045444065,0.00027273153,0.00046475208,0.0005859251,0.00068408274,0.00068863493],"category_scores_gemma":[0.00060856267,0.0003327283,0.00040137654,0.00022981896,0.0003884464,0.00021065497,0.00030543597,0.00027250565,0.000089984125],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003860815,0.000040566665,0.010634454,0.000013789047,0.000013070395,0.00006399066,0.00004013483,0.984446,0.003023544,0.0002357492,0.00004810698,0.0014019866],"study_design_scores_gemma":[0.0000035608505,0.0000071038303,0.0020869644,0.0000012881168,0.0000022767174,0.000003832686,0.000011548405,0.9975827,0.00023920217,0.000027491582,0.00003172571,0.000002303491],"about_ca_topic_score_codex":0.08112897,"about_ca_topic_score_gemma":0.042053368,"teacher_disagreement_score":0.08112897,"about_ca_system_score_codex":0.0009739571,"about_ca_system_score_gemma":0.00077420677,"threshold_uncertainty_score":0.16131347},"labels":[],"label_agreement":null},{"id":"W1984062498","doi":"10.4081/rg.2012.e6","title":"Anomalous statistics of aftershock sequences generated by supershear ruptures","year":2012,"lang":"en","type":"article","venue":"Research in Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Institute for Catastrophic Loss Reduction","keywords":"Aftershock; Seismology; Geology; Rayleigh wave; Fault (geology); Shear (geology); Rayleigh scattering; Physics; Surface wave; Optics; Petrology","score_opus":0.06255887343919926,"score_gpt":0.31475720485280984,"score_spread":0.2521983314136106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984062498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99904495,0.000025357222,0.0005121208,0.000009016236,0.0000015412122,0.0000023281268,0.00013093317,0.00001755174,0.00025620317],"genre_scores_gemma":[0.99944097,0.000017297574,0.0000860076,0.0000014776031,0.000005645335,0.0000022860436,0.00035631264,0.0000035182593,0.000086496206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974054,0.000024352099,0.000029392619,0.00008041633,0.00007509348,0.00005021548],"domain_scores_gemma":[0.9964792,0.0009809056,0.0013886063,0.00039861575,0.00042064348,0.00033194464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037374627,0.00010998853,0.00023344993,0.0012915973,0.00017167348,0.00039986763,0.00026825359,0.00018939967,0.001107416],"category_scores_gemma":[0.0026756083,0.00012945702,0.00015163764,0.00080770324,0.00042384677,0.00032725531,0.00028095598,0.00019019541,0.00019493689],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028088497,0.000055987985,0.9492242,0.000035335903,0.00010262795,0.0006982608,0.00050274323,0.012254287,0.020746715,0.0018796419,0.0004875167,0.013731887],"study_design_scores_gemma":[0.000005248503,0.00009063374,0.9748215,0.0000026703876,0.000024725174,0.00032288927,0.00013654142,0.021577096,0.00217227,0.00042404118,0.00040797997,0.000014410326],"about_ca_topic_score_codex":0.0018222114,"about_ca_topic_score_gemma":0.0015995982,"teacher_disagreement_score":0.0018222114,"about_ca_system_score_codex":0.00023425595,"about_ca_system_score_gemma":0.00011980631,"threshold_uncertainty_score":0.0037047267},"labels":[],"label_agreement":null},{"id":"W1984458588","doi":"10.1016/j.tecto.2013.11.018","title":"Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems","year":2013,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Induced seismicity; Seismology; Slip (aerodynamics); Geodesy","score_opus":0.01368878500524401,"score_gpt":0.18420893712417366,"score_spread":0.17052015211892965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984458588","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974406,0.00018053132,0.000033155065,0.00009756057,0.0000037277293,0.0000064137844,0.0012562054,0.000004693369,0.0009771637],"genre_scores_gemma":[0.997175,0.00020149825,0.000061948,0.000032100153,0.0000016603253,0.000005501035,0.001043955,0.0000030986498,0.0014753417],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998092,0.000015235433,0.000017501827,0.00003633657,0.000042778778,0.00007895311],"domain_scores_gemma":[0.99873406,0.00013152107,0.00019530031,0.000033934997,0.00059610937,0.00030912625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021387593,0.00023082033,0.00024694382,0.0011978648,0.002043813,0.001144559,0.0006483309,0.00034339508,0.0020223507],"category_scores_gemma":[0.0013435187,0.00022686872,0.00022461287,0.003172959,0.0006565365,0.0003710342,0.00063173514,0.00034583133,0.0002125537],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000105757885,0.00002323106,0.9920711,0.000025686695,0.00005508389,0.00017146107,0.0014812732,0.00032310045,0.00064995984,0.00022291749,0.00054269185,0.0043277526],"study_design_scores_gemma":[0.000004035817,0.000005879649,0.99694014,0.000012612053,0.000009650199,0.00003745405,0.0020484275,0.00022409383,0.000052767326,0.000021715454,0.0006379302,0.000005308655],"about_ca_topic_score_codex":0.99358165,"about_ca_topic_score_gemma":0.998106,"teacher_disagreement_score":0.012848032,"about_ca_system_score_codex":0.012848032,"about_ca_system_score_gemma":0.018604381,"threshold_uncertainty_score":0.09321946},"labels":[],"label_agreement":null},{"id":"W1984459965","doi":"10.1029/2008jb006021","title":"Seven years of postseismic deformation following the 1999, <i>M</i> = 7.4 and <i>M</i> = 7.2, Izmit‐Düzce, Turkey earthquake sequence","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismology; North Anatolian Fault; Geodesy; Crust; Global Positioning System; Logarithm; Induced seismicity; Tectonics; Sequence (biology); Geophysics","score_opus":0.027979187130292776,"score_gpt":0.2856120960994105,"score_spread":0.2576329089691177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984459965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999089,0.000032162447,0.00007199503,0.000008292193,0.000004270683,0.000009072491,0.000558624,0.0000060363823,0.0002204029],"genre_scores_gemma":[0.9941934,0.000063351894,0.0002578613,0.000016579907,0.0000112843245,0.000027972286,0.005202664,0.0000042478437,0.0002226629],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976975,0.000020581985,0.000026981103,0.000057900532,0.00006133101,0.00006350602],"domain_scores_gemma":[0.99956125,0.000041074905,0.00015599566,0.00004833718,0.00011834543,0.00007503785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029699728,0.000333038,0.00027520195,0.0006894538,0.0005155447,0.00027781635,0.00038660128,0.00049475906,0.0003510744],"category_scores_gemma":[0.0005070787,0.00016034815,0.00022484257,0.0005920812,0.0003157983,0.00029484942,0.00061177457,0.00042082503,0.00017972461],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006270792,0.00042957286,0.95838886,0.00005637737,0.00013199593,0.0007257748,0.0008299246,0.0014887827,0.019712608,0.00008345657,0.0007141173,0.01681144],"study_design_scores_gemma":[0.0000061830324,0.00011742553,0.997775,0.0000032322941,0.00001524871,0.00006877142,0.00011278539,0.0003794264,0.0011081768,0.000007745186,0.00040029903,0.0000056900553],"about_ca_topic_score_codex":0.00940634,"about_ca_topic_score_gemma":0.024900522,"teacher_disagreement_score":0.00940634,"about_ca_system_score_codex":0.00039002433,"about_ca_system_score_gemma":0.00029242007,"threshold_uncertainty_score":0.018703163},"labels":[],"label_agreement":null},{"id":"W1984542041","doi":"10.1029/2007jb005061","title":"Current deformation in the northern Canadian Cordillera inferred from GPS measurements","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Comer Science and Education Foundation","keywords":"Geology; Seismology; Clockwise; Induced seismicity; Global Positioning System; North American Plate; Geodesy; Plate tectonics; Deformation (meteorology); Fault (geology); Pacific Plate; Collision; Rotation (mathematics); Tectonics; Subduction; Geometry; Oceanography","score_opus":0.07818928728925646,"score_gpt":0.31904986325901147,"score_spread":0.24086057596975502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984542041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98077637,0.00055909675,0.0002023011,0.00013640293,0.00001455199,0.000024631503,0.004217142,0.00007476466,0.013994666],"genre_scores_gemma":[0.9953857,0.00032893443,0.0004488983,0.000030591378,0.00000431493,0.000010974429,0.0020743548,0.00000891735,0.0017072683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997831,0.0000054394563,0.000009266365,0.000054061642,0.00008102838,0.00006702016],"domain_scores_gemma":[0.9994931,0.000018826016,0.00004222549,0.000014222067,0.00036405644,0.00006761811],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015224949,0.00046018284,0.00023221363,0.0023572529,0.0018166086,0.0011524189,0.000549771,0.00028294412,0.0028760594],"category_scores_gemma":[0.00084733,0.00017625206,0.00026147036,0.0037313162,0.00039431785,0.00022177093,0.0004776735,0.00024422957,0.00040553883],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012496496,0.000025374398,0.94766647,0.00007636267,0.000081285936,0.00025951164,0.0011834876,0.001994562,0.0038097263,0.00048151228,0.0031041089,0.04119263],"study_design_scores_gemma":[0.0000060890457,0.000006323085,0.99430263,0.000018986622,0.00002023785,0.000028556848,0.00048427086,0.001183815,0.0002936481,0.00003178512,0.0036119903,0.000011645116],"about_ca_topic_score_codex":0.99495196,"about_ca_topic_score_gemma":0.9973429,"teacher_disagreement_score":0.018821899,"about_ca_system_score_codex":0.018821899,"about_ca_system_score_gemma":0.0103399735,"threshold_uncertainty_score":0.13656306},"labels":[],"label_agreement":null},{"id":"W1984834368","doi":"10.1016/j.margeo.2005.03.012","title":"The Oligocene-Recent evolution of the Mesaoria Basin (Cyprus) and its western marine extension, Eastern Mediterranean","year":2005,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Forearc; Geology; Paleontology; Imbrication; Neogene; Late Miocene; Fold and thrust belt; Evaporite; Structural basin; Fold (higher-order function); Anticline; Seismology; Subduction; Foreland basin; Tectonics","score_opus":0.014949554411179422,"score_gpt":0.2145161904249357,"score_spread":0.19956663601375627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984834368","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961671,0.00044318673,0.000042176052,0.0001188964,0.000005416677,0.000002632198,0.00009972885,0.000002837596,0.003118003],"genre_scores_gemma":[0.9988593,0.00023987883,0.000048337843,0.000024913485,0.00000971386,0.0000020103002,0.00009338116,0.0000025529223,0.0007199135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993145,0.000009460331,0.0000055078676,0.000025051095,0.0000094944135,0.000018973613],"domain_scores_gemma":[0.9997764,0.000020300453,0.000079862504,0.000012865441,0.00007237925,0.000038174556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023421398,0.0001306575,0.00011749828,0.00080981146,0.00054820377,0.0007923205,0.00022979421,0.0002548166,0.002279916],"category_scores_gemma":[0.00060903496,0.00010186609,0.00010821918,0.0009166119,0.00062399165,0.00043524455,0.0004324313,0.00017068438,0.00019277116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046530753,0.00004418653,0.9358475,0.00011470112,0.00014569094,0.0009073143,0.00342465,0.0012491662,0.012957254,0.0029691276,0.0007651669,0.041109856],"study_design_scores_gemma":[0.0000016489872,0.0000038114179,0.9987394,0.0000054633592,0.000003803952,0.000046132835,0.00012128735,0.00006682059,0.000049562692,0.00002028907,0.00094088766,8.4617716e-7],"about_ca_topic_score_codex":0.046679407,"about_ca_topic_score_gemma":0.09445203,"teacher_disagreement_score":0.046679407,"about_ca_system_score_codex":0.0014148363,"about_ca_system_score_gemma":0.0006962386,"threshold_uncertainty_score":0.0928154},"labels":[],"label_agreement":null},{"id":"W1985048042","doi":"10.1103/physrevlett.110.068501","title":"Earthquake Interevent Time Distribution for Induced Micro-, Nano-, and Picoseismicity","year":2013,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Seismology; Geology; Tectonics; Scaling; Drilling; Materials science; Geometry","score_opus":0.017199947856547777,"score_gpt":0.24214051103873108,"score_spread":0.2249405631821833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985048042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972869,0.00010508363,0.001200715,0.000028820965,0.000001778088,0.0000055413348,0.00066285627,0.000026121661,0.00068215776],"genre_scores_gemma":[0.9988612,0.000080316786,0.00016755107,0.000004296201,0.0000057429465,0.000006684208,0.0006902178,0.000005741939,0.00017823272],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998791,0.000016345506,0.000013065445,0.000042222862,0.00003255208,0.000016642953],"domain_scores_gemma":[0.99686396,0.0014186983,0.0011330841,0.00025108637,0.00020260349,0.0001305407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037942216,0.00006821335,0.00015533344,0.0010416013,0.00008591819,0.00027466385,0.00018449777,0.0001574316,0.0016480201],"category_scores_gemma":[0.00334642,0.00006729678,0.00013343236,0.0011481429,0.000246941,0.00029131895,0.0003001384,0.00018274451,0.00024449188],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030736442,0.00004132088,0.9409951,0.00008175755,0.00010683451,0.00032684702,0.0005280137,0.006847941,0.012342149,0.0030794877,0.00063866086,0.034704585],"study_design_scores_gemma":[0.0000040977793,0.00004646163,0.9922087,0.0000053034973,0.0000132541345,0.00023822827,0.00012475312,0.005838603,0.00056704617,0.0004711736,0.0004737107,0.000008552568],"about_ca_topic_score_codex":0.00085337664,"about_ca_topic_score_gemma":0.0010925632,"teacher_disagreement_score":0.0016480201,"about_ca_system_score_codex":0.00018431913,"about_ca_system_score_gemma":0.00008044055,"threshold_uncertainty_score":0.0055131316},"labels":[],"label_agreement":null},{"id":"W1985068461","doi":"10.1038/ngeo1927","title":"Hydrologic control of forearc strength and seismicity in the Costa Rican subduction zone","year":2013,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"National Science Foundation","keywords":"Geology; Subduction; Seismology; Forearc; Episodic tremor and slip; Crust; Convergent boundary; Receiver function; Continental crust; Slip (aerodynamics); Induced seismicity; Oceanic crust; Fault (geology); Tectonics; Geophysics; Lithosphere","score_opus":0.006122043214315772,"score_gpt":0.1988664846602625,"score_spread":0.1927444414459467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985068461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986607,0.00009143097,0.000035794266,0.00015459135,9.1371874e-7,0.000001975849,0.00010110608,0.000006455475,0.00094701035],"genre_scores_gemma":[0.99968946,0.0000641017,0.000023931321,0.000009401601,0.0000013615131,0.000001099396,0.000051352425,0.0000023854905,0.00015694537],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999211,0.000026661313,0.0000061274836,0.000012993847,0.000007917432,0.000025361456],"domain_scores_gemma":[0.9996635,0.00007431744,0.0001182198,0.000042090745,0.000056260345,0.000045685454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002657297,0.00012545266,0.00013036504,0.00054787105,0.00026864596,0.0006110988,0.0002772625,0.00018737173,0.00086623273],"category_scores_gemma":[0.0010192081,0.00013749526,0.00018078282,0.00059657014,0.0005260893,0.00024302305,0.0004474775,0.00016054275,0.000098745106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020417929,0.00006971147,0.9605123,0.000038185146,0.00015350754,0.00024145936,0.0011998224,0.0122958915,0.01024857,0.0023984436,0.0005690523,0.012068875],"study_design_scores_gemma":[0.000004823387,0.000004674715,0.9958001,0.0000037868513,0.000015890808,0.000015404514,0.00036688495,0.0030547956,0.00023024865,0.00009968726,0.00039976873,0.0000038152925],"about_ca_topic_score_codex":0.17688233,"about_ca_topic_score_gemma":0.20336986,"teacher_disagreement_score":0.17688233,"about_ca_system_score_codex":0.001522818,"about_ca_system_score_gemma":0.00077316526,"threshold_uncertainty_score":0.3517055},"labels":[],"label_agreement":null},{"id":"W1985267200","doi":"10.1007/s00024-014-0792-0","title":"Field Survey Following the 28 October 2012 Haida Gwaii Tsunami","year":2014,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Fisheries and Oceans Canada; Parks Canada","keywords":"Geology; Submarine pipeline; Seismology; Oceanography; Debris; Storm; Inlet; Storm surge","score_opus":0.01161224231537101,"score_gpt":0.2011401363593242,"score_spread":0.1895278940439532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985267200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93691266,0.00012722569,0.0006588841,0.00030910992,0.0000862285,0.00079495774,0.04005449,0.00012415105,0.020932358],"genre_scores_gemma":[0.84769136,0.00056922995,0.0044361404,0.0006307619,0.00009449268,0.0016016626,0.066364996,0.00003955627,0.078571826],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998977,0.00000875863,0.000007696363,0.00003176315,0.000024440296,0.000029557252],"domain_scores_gemma":[0.9992362,0.000032749052,0.00013672272,0.00004822396,0.00038298094,0.00016306956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019614057,0.0002907202,0.00019208202,0.0017886031,0.0011822523,0.00024981087,0.00053228205,0.00049789593,0.0063479473],"category_scores_gemma":[0.0003610076,0.00022321621,0.00008636036,0.0015420604,0.00025000126,0.0003211921,0.0004840322,0.00040125224,0.0029890977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009958906,0.001548657,0.74436986,0.0006876791,0.000063719854,0.004137699,0.017428797,0.0005279779,0.04378885,0.0005928512,0.08355378,0.1023042],"study_design_scores_gemma":[0.000015568365,0.00016067714,0.9758733,0.000022705606,0.00000839353,0.00024450786,0.0045866235,0.00011248663,0.00059787685,0.000030318126,0.018333679,0.00001384052],"about_ca_topic_score_codex":0.13162072,"about_ca_topic_score_gemma":0.41385698,"teacher_disagreement_score":0.8683793,"about_ca_system_score_codex":0.0009809419,"about_ca_system_score_gemma":0.0022384685,"threshold_uncertainty_score":0.26170915},"labels":[],"label_agreement":null},{"id":"W1986507913","doi":"10.1130/0091-7613(2002)030<0211:aletro>2.0.co;2","title":"Asymmetric lithospheric extension: The role of frictional plastic strain softening inferred from numerical experiments","year":2002,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":141,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Nova scotia; Citation; Geology; Lithosphere; Icon; Library science; Operations research; Computer science; Oceanography; Seismology; Tectonics; Mathematics","score_opus":0.020959329167962275,"score_gpt":0.2129335580876513,"score_spread":0.19197422891968902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986507913","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99034214,0.00054494996,0.0011721998,0.00040582434,0.00004399925,0.00001560963,0.0005268992,0.00013320903,0.0068151304],"genre_scores_gemma":[0.99924916,0.00015860378,0.00031434742,0.000017138424,0.000007141974,0.0000028583497,0.00014455989,0.0000150373635,0.000091184695],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997758,0.000056835044,0.000041312625,0.000046440175,0.000050585146,0.00002906476],"domain_scores_gemma":[0.9983374,0.00086144364,0.0002099714,0.0003019946,0.00018639551,0.00010288811],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009617602,0.0002394751,0.00043917698,0.00059211144,0.0004438294,0.0011665068,0.0005959657,0.0006390921,0.0021509738],"category_scores_gemma":[0.0076599387,0.0002613667,0.0002946019,0.0009445952,0.0010018607,0.0009605285,0.0005438314,0.00060028833,0.00021972512],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00304225,0.00032274632,0.29437277,0.0012456134,0.0005150495,0.0022736616,0.0012772093,0.5220298,0.08704702,0.007923466,0.0047769197,0.07517347],"study_design_scores_gemma":[0.0004515216,0.00040544118,0.3677836,0.00033533492,0.00020560322,0.00039789587,0.0006684429,0.59891397,0.02236314,0.0044679483,0.003815872,0.00019128248],"about_ca_topic_score_codex":0.007348845,"about_ca_topic_score_gemma":0.005789571,"teacher_disagreement_score":0.007348845,"about_ca_system_score_codex":0.000665716,"about_ca_system_score_gemma":0.0003760126,"threshold_uncertainty_score":0.014612138},"labels":[],"label_agreement":null},{"id":"W1986519218","doi":"10.1130/0091-7613(2002)030<0939:pcuiit>2.0.co;2","title":"Pronounced central uplift identified in the Bosumtwi impact structure, Ghana, using multichannel seismic reflection data","year":2002,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Economic Justice; Library science; Geological survey; History; Art history; Archaeology; Geology; Political science; Geophysics; Computer science; Law","score_opus":0.08853203375656436,"score_gpt":0.2931677649885237,"score_spread":0.20463573123195933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986519218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9528158,0.002775112,0.0005419929,0.0012622094,0.000071342176,0.00011761619,0.01403807,0.00008855599,0.028289385],"genre_scores_gemma":[0.97276425,0.004520638,0.0019235663,0.00016205215,0.000052827014,0.00008548054,0.009290438,0.000052564035,0.011148117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999212,0.000008775475,0.0000066916587,0.000011731041,0.000027641832,0.00002393671],"domain_scores_gemma":[0.99978,0.00004022929,0.00008046277,0.000010233908,0.0000630112,0.00002601295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015826605,0.00024447788,0.0002395306,0.001957328,0.00044401136,0.00045460422,0.0001892769,0.0003345668,0.0050649196],"category_scores_gemma":[0.0008209031,0.00018724725,0.00008910021,0.004296586,0.00027886027,0.00042874107,0.00058348227,0.00021363828,0.0013426961],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061291084,0.000057646674,0.65678376,0.0012127247,0.000070790345,0.00776561,0.01259546,0.0005154839,0.0216119,0.00082684,0.05026177,0.24768509],"study_design_scores_gemma":[0.000017608441,0.00003367571,0.9677232,0.00016719526,0.000026530355,0.0007673062,0.0069900346,0.000117233045,0.00064288446,0.00010430175,0.023400452,0.0000096515105],"about_ca_topic_score_codex":0.059356082,"about_ca_topic_score_gemma":0.21573286,"teacher_disagreement_score":0.059356082,"about_ca_system_score_codex":0.00056852173,"about_ca_system_score_gemma":0.0008755412,"threshold_uncertainty_score":0.11802119},"labels":[],"label_agreement":null},{"id":"W1986916880","doi":"10.1029/2010jb007472","title":"Erosional control of the kinematics and geometry of fold‐and‐thrust belts imaged in a physical and numerical sandbox","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Sandbox (software development); Thrust; Geometry; Kinematics; Bedrock; Erosion; Shear (geology); Fluvial; Mechanics; Geotechnical engineering; Geomorphology; Physics; Mathematics; Classical mechanics; Petrology","score_opus":0.017310879178264283,"score_gpt":0.282985554047845,"score_spread":0.2656746748695807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986916880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989002,0.000008362929,0.000808687,0.0000057321117,0.000001119559,0.0000031377617,0.000026630207,0.000026835078,0.00021936005],"genre_scores_gemma":[0.9988907,0.000011714806,0.0009880043,0.0000022142274,4.400673e-7,0.0000055594373,0.000031356067,0.0000049233595,0.00006504729],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989796,0.000015305262,0.000011022833,0.000034432378,0.000022314565,0.000019071484],"domain_scores_gemma":[0.99959725,0.00013585071,0.00009088389,0.00009288665,0.000033049335,0.000050116287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002238763,0.00018430225,0.00025999872,0.00017052301,0.0001830827,0.00049764,0.0003146185,0.00023158129,0.00065936166],"category_scores_gemma":[0.00085500896,0.00019029045,0.00016211318,0.00014108178,0.00047980648,0.00026365402,0.00035968487,0.00023457065,0.00006943802],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004085908,0.00022536839,0.02501512,0.00006867084,0.000039011436,0.00022363312,0.00025559706,0.13877662,0.8262347,0.0014570296,0.00009394913,0.0072017335],"study_design_scores_gemma":[0.00009919619,0.00058523106,0.09927073,0.000015687963,0.0000369136,0.00015000593,0.0002411869,0.65033996,0.24785349,0.0005736271,0.0007871631,0.000046791323],"about_ca_topic_score_codex":0.0013564082,"about_ca_topic_score_gemma":0.0015655234,"teacher_disagreement_score":0.0013564082,"about_ca_system_score_codex":0.00040524258,"about_ca_system_score_gemma":0.00023329284,"threshold_uncertainty_score":0.0029402375},"labels":[],"label_agreement":null},{"id":"W1987045710","doi":"10.1190/1.3663403","title":"Inferring in-situ stress changes by statistical analysis of microseismic event characteristics","year":2011,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Microseism; Hypocenter; Geology; Seismology; Fractal dimension; Stress field; Geomechanics; Overpressure; Fractal analysis; Induced seismicity; Stress (linguistics); Slip (aerodynamics); Fractal; Geotechnical engineering; Mathematics; Physics","score_opus":0.03331065994872925,"score_gpt":0.24683559570406718,"score_spread":0.21352493575533793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987045710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96726406,0.000050172854,0.03130106,0.000028554632,0.000004826832,0.00001739426,0.00057327864,0.00013804216,0.0006225849],"genre_scores_gemma":[0.995372,0.00002442823,0.004201214,0.0000034525117,0.000006501945,0.000010391962,0.0003419552,0.0000067757674,0.000033168006],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975103,0.00006200938,0.000032633696,0.00007235347,0.000050174498,0.000031788335],"domain_scores_gemma":[0.99660313,0.0018241935,0.0009004536,0.00025718677,0.0002907404,0.00012439361],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067405624,0.00026482702,0.00028503625,0.002870203,0.00023035976,0.00046363237,0.00026462233,0.00027459968,0.00032632906],"category_scores_gemma":[0.004447157,0.00020018898,0.00026545697,0.001575317,0.00036923256,0.0005788667,0.00028504874,0.0002195377,0.00010452076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018206524,0.0001166088,0.8490254,0.00011288247,0.00023624397,0.00019214963,0.000416705,0.058768515,0.040446535,0.0012418133,0.00040347548,0.048857693],"study_design_scores_gemma":[0.0000071439604,0.000105918785,0.76141167,0.000009892656,0.00004692196,0.0002186545,0.00023790855,0.22831747,0.0075405664,0.0015039669,0.00056093355,0.000038924863],"about_ca_topic_score_codex":0.0026233953,"about_ca_topic_score_gemma":0.0035717732,"teacher_disagreement_score":0.002870203,"about_ca_system_score_codex":0.00035393375,"about_ca_system_score_gemma":0.00019299996,"threshold_uncertainty_score":0.005216241},"labels":[],"label_agreement":null},{"id":"W1987046510","doi":"10.1002/2014gc005509","title":"Segmentation of plate coupling, fate of subduction fluids, and modes of arc magmatism in <scp>C</scp>ascadia, inferred from magnetotelluric resistivity","year":2014,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Geology; Subduction; Forearc; Magnetotellurics; Magmatism; Mantle wedge; Mantle (geology); Slab; Geophysics; Petrology; Volcanic arc; Seismology; Electrical resistivity and conductivity; Tectonics","score_opus":0.008892425798794717,"score_gpt":0.19335063615990086,"score_spread":0.18445821036110616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987046510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999113,0.000009797859,0.00011901237,0.000007895929,3.3003e-7,0.0000017463997,0.0001972936,0.00001872687,0.00053217076],"genre_scores_gemma":[0.99922895,0.000008365681,0.00012085239,0.0000024765864,3.8623426e-7,0.0000019538832,0.00035635158,0.000004803502,0.00027584247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995303,0.000003173818,0.0000027302783,0.000019969439,0.000010702334,0.000010359406],"domain_scores_gemma":[0.9998392,0.000020107655,0.00003589575,0.0000128056045,0.000049466737,0.00004250098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007200535,0.00022548296,0.00009096984,0.00091438275,0.00029468053,0.00046300128,0.00014028963,0.00019945395,0.00096059946],"category_scores_gemma":[0.00027149738,0.00015328049,0.00015147348,0.0005243696,0.0002726278,0.00013428192,0.00026783574,0.00015931106,0.00017021841],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030201458,0.000027686585,0.79580617,0.000046700112,0.00005357463,0.00034874628,0.0010888178,0.0040968116,0.1864213,0.0002540762,0.00032057284,0.011233581],"study_design_scores_gemma":[0.0000014457199,0.0000087703775,0.99696916,0.0000018914292,0.0000043002337,0.000023128738,0.00010087161,0.0013728569,0.001343405,0.000017317834,0.00015415593,0.0000027113429],"about_ca_topic_score_codex":0.043804027,"about_ca_topic_score_gemma":0.058899447,"teacher_disagreement_score":0.043804027,"about_ca_system_score_codex":0.00062009686,"about_ca_system_score_gemma":0.0002548956,"threshold_uncertainty_score":0.08709812},"labels":[],"label_agreement":null},{"id":"W1987093287","doi":"10.1007/s10291-013-0354-4","title":"EPC: Matlab software to estimate Euler pole parameters","year":2013,"lang":"en","type":"article","venue":"GPS Solutions","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"University of Twente; Université Laval","keywords":"Euler's formula; Software; Euler angles; Set (abstract data type); Geodesy; Surface (topology); Computer science; Geodynamics; Geology; Tectonics; Geometry; Algorithm; Mathematics; Mathematical analysis; Seismology","score_opus":0.0305494241290193,"score_gpt":0.24539352644174625,"score_spread":0.21484410231272694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987093287","genre_codex":"methods","genre_gemma":"software","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"software","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0035902355,0.00021332844,0.65931726,0.0001648135,0.00025979642,0.00018819203,0.018410238,0.2975567,0.020299472],"genre_scores_gemma":[0.072346054,0.00037882695,0.72446835,0.00072782306,0.00015544574,0.0018698942,0.036672857,0.10837208,0.0550087],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996637,0.000060912822,0.000046111145,0.00007519276,0.000108021384,0.000046128036],"domain_scores_gemma":[0.9982565,0.00081033807,0.000116685944,0.0002045872,0.00056156074,0.000050230385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053418346,0.0014539722,0.00062745565,0.0013420162,0.00043349058,0.00096070155,0.0019463411,0.0009932015,0.16641186],"category_scores_gemma":[0.0055665583,0.00071992533,0.0006465196,0.00083761616,0.00028142406,0.0010223249,0.00086600747,0.0013695094,0.071879864],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035975635,0.00015787347,0.001464182,0.0010939065,0.00016456403,0.0004595081,0.0002382868,0.05085212,0.007094993,0.01036376,0.6093651,0.31838596],"study_design_scores_gemma":[0.000539233,0.000116512034,0.0034657002,0.0004002713,0.000113800445,0.00081884494,0.0001074162,0.55346733,0.052742958,0.020675307,0.36734933,0.0002033453],"about_ca_topic_score_codex":0.004576996,"about_ca_topic_score_gemma":0.0069638714,"teacher_disagreement_score":0.16641186,"about_ca_system_score_codex":0.00044666883,"about_ca_system_score_gemma":0.00089966675,"threshold_uncertainty_score":0.55670315},"labels":[],"label_agreement":null},{"id":"W1987152781","doi":"10.1111/gfl.12079","title":"Hydrothermal monitoring in a quiescent volcanic arc: Cascade Range, northwestern United States","year":2014,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Brock University","funders":"U.S. Geological Survey","keywords":"Fumarole; Volcano; Hydrothermal circulation; Geology; Volcanic arc; Caldera; Summit; Impact crater; Earth science; Atmospheric sciences; Geochemistry; Physical geography; Subduction; Seismology; Geography; Astrobiology","score_opus":0.014114217638717553,"score_gpt":0.2171400900313071,"score_spread":0.20302587239258954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987152781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968232,0.000074737596,0.000050848783,0.000059803246,0.0000027507733,0.000025852181,0.0007115004,0.000014487949,0.0022368422],"genre_scores_gemma":[0.9972791,0.00014808061,0.00028613108,0.000044684388,0.0000054127163,0.000021181195,0.0012223315,0.00000270421,0.0009903985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999908,0.0000071173877,0.0000047707704,0.000028542083,0.000034571774,0.000017028],"domain_scores_gemma":[0.99969614,0.000025740952,0.00006291657,0.00001289091,0.00010491261,0.00009750026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013413321,0.00018850011,0.00008321061,0.00065097347,0.00081030733,0.00036748583,0.00037637283,0.00015129679,0.0010070916],"category_scores_gemma":[0.00026898016,0.000116307085,0.00006212379,0.00060357904,0.0002717553,0.00020995796,0.00040956686,0.00024943816,0.00010557404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074812924,0.00011844707,0.98310685,0.000016617983,0.000021949383,0.0003828342,0.000785905,0.00020681546,0.004125133,0.00005040115,0.0010433308,0.010067035],"study_design_scores_gemma":[0.000008396817,0.000039261395,0.9965533,0.000007593804,0.000008677889,0.00006780171,0.00088496413,0.00038459644,0.0005774905,0.000010649014,0.001454605,0.0000027273375],"about_ca_topic_score_codex":0.5310817,"about_ca_topic_score_gemma":0.81630445,"teacher_disagreement_score":0.5310817,"about_ca_system_score_codex":0.0019839627,"about_ca_system_score_gemma":0.0018647522,"threshold_uncertainty_score":0.94335973},"labels":[],"label_agreement":null},{"id":"W1987416063","doi":"10.1002/2013eo200008","title":"Long‐distance induced tremor observed off western Canada","year":2013,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Subduction; Magnitude (astronomy); Intraplate earthquake; Tectonics; Ridge; Moment magnitude scale; Quake (natural phenomenon); Tsunami earthquake; Paleontology","score_opus":0.031463841503743574,"score_gpt":0.19655525454965436,"score_spread":0.1650914130459108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987416063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943242,0.00014369878,0.00006935915,0.00012245752,0.0000056105177,0.000012426448,0.0011136952,0.000015363268,0.004193193],"genre_scores_gemma":[0.9971136,0.000162939,0.00009411893,0.00006661937,0.0000032535518,0.000006960213,0.0006964383,0.0000048271886,0.0018512881],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998386,0.000005618047,0.0000052593373,0.000027439944,0.000058223082,0.000064946034],"domain_scores_gemma":[0.99934584,0.000033260618,0.00009921741,0.000020932364,0.00038702655,0.0001136438],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009034912,0.00021793514,0.00019982361,0.0009825545,0.0015902837,0.0007024214,0.00042990907,0.00028266505,0.001450854],"category_scores_gemma":[0.00063039997,0.0001985994,0.000110054614,0.00197482,0.00046448415,0.00013316859,0.000566887,0.00028956225,0.00019621277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022770218,0.00005797367,0.9403742,0.00009708837,0.00007820966,0.0014401518,0.0044252626,0.00044729616,0.020756438,0.00023351138,0.0041457904,0.027716193],"study_design_scores_gemma":[0.0000045385746,0.000009766405,0.9964367,0.000012729159,0.000008877932,0.00007787635,0.001094227,0.00012693368,0.00040987926,0.000010953168,0.0017999103,0.000007509782],"about_ca_topic_score_codex":0.98586327,"about_ca_topic_score_gemma":0.99550086,"teacher_disagreement_score":0.014136732,"about_ca_system_score_codex":0.0092661,"about_ca_system_score_gemma":0.009465058,"threshold_uncertainty_score":0.06723052},"labels":[],"label_agreement":null},{"id":"W1987610226","doi":"10.1785/0220120144","title":"A Unified Seismic Catalog for the Iranian Plateau (1900-2011)","year":2013,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research","keywords":"Islam; Plateau (mathematics); Humanities; Seismology; History; Library science; Geology; Art; Archaeology; Computer science","score_opus":0.08694015763447187,"score_gpt":0.30106112453067774,"score_spread":0.21412096689620586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987610226","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.24894494,0.0038413743,0.04172429,0.00060288724,0.00057935604,0.0025011299,0.56452495,0.004998168,0.13228297],"genre_scores_gemma":[0.20239991,0.0024641922,0.061253764,0.000095009644,0.00035247614,0.0012830646,0.70657253,0.00036365385,0.025215346],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99948883,0.000035864596,0.00007808583,0.000086483684,0.00022691303,0.00008387276],"domain_scores_gemma":[0.9978022,0.000065120264,0.00032970405,0.00026881037,0.0013939457,0.00014015443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094160077,0.00081819354,0.00036973096,0.014426685,0.00057562004,0.0007103264,0.0006954465,0.00023449709,0.011757409],"category_scores_gemma":[0.001992358,0.00020886319,0.00026626684,0.011588178,0.00022695679,0.0008907897,0.0010516063,0.0004193012,0.005033789],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002262094,0.00013540895,0.15353152,0.00086213497,0.000068655296,0.00048756454,0.0017851981,0.002449302,0.009061429,0.00894617,0.25240907,0.57003736],"study_design_scores_gemma":[0.000027214957,0.00009154145,0.4463098,0.000118762175,0.000036578724,0.0004548909,0.0008803686,0.0010068921,0.0011846627,0.00081104285,0.5490406,0.00003765415],"about_ca_topic_score_codex":0.037899647,"about_ca_topic_score_gemma":0.04705528,"teacher_disagreement_score":0.037899647,"about_ca_system_score_codex":0.0008568403,"about_ca_system_score_gemma":0.0038371668,"threshold_uncertainty_score":0.07535809},"labels":[],"label_agreement":null},{"id":"W1987613981","doi":"10.1126/science.1057022","title":"Space-Geodetic Constraints on Glacial Isostatic Adjustment in Fennoscandia","year":2001,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":370,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Geology; Geodetic datum; Geodesy; Lithosphere; Global Positioning System; Tectonics; Tectonic uplift; Glacial period; Tide gauge; Deformation (meteorology); Sea level; Geophysics; Seismology; Geomorphology; Oceanography","score_opus":0.018367631151415865,"score_gpt":0.23965671801139096,"score_spread":0.2212890868599751,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987613981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872333,0.00037917847,0.0011074716,0.0002196267,0.000006700047,0.000004082826,0.0005363275,0.000031126794,0.010482186],"genre_scores_gemma":[0.99900466,0.00009397442,0.00041536996,0.000014089665,0.0000018148505,0.0000028489371,0.00027387802,0.00000432115,0.00018900655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997769,0.00004477551,0.00001383751,0.00004894113,0.000050820832,0.00006477971],"domain_scores_gemma":[0.999579,0.00008095407,0.000076220305,0.00004098419,0.00017372801,0.000049076687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038773718,0.0002506313,0.0002874372,0.0011523542,0.0010183845,0.0011307428,0.0005562198,0.00022886753,0.00143277],"category_scores_gemma":[0.0020117308,0.00016432264,0.00014220549,0.001430318,0.00087297213,0.00036629714,0.00056599436,0.00024541345,0.000117401076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028729733,0.000033220087,0.7429061,0.00007496858,0.000094303774,0.00047246594,0.001348285,0.13283888,0.003962966,0.037524004,0.0022196434,0.07823797],"study_design_scores_gemma":[0.000021592305,0.000024181843,0.9243816,0.000054228673,0.0000331806,0.000104086226,0.0009747798,0.0591935,0.0006752328,0.00812186,0.0063767843,0.00003893946],"about_ca_topic_score_codex":0.47667453,"about_ca_topic_score_gemma":0.6449568,"teacher_disagreement_score":0.47667453,"about_ca_system_score_codex":0.0031198629,"about_ca_system_score_gemma":0.002930331,"threshold_uncertainty_score":0.9477999},"labels":[],"label_agreement":null},{"id":"W1988287276","doi":"10.1144/sp282.15","title":"Overview of tectonic settings related to the rifting and opening of Mesozoic ocean basins in the Eastern Tethys: Oman, Himalayas and Eastern Mediterranean regions","year":2007,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mesozoic; Geology; Rift; Tectonics; Paleontology; Mediterranean climate; Tethys Ocean; Palaeogeography; Structural basin; Oceanography; Subduction; Geography; Archaeology; Volcanism","score_opus":0.044618592037498794,"score_gpt":0.2726845758980826,"score_spread":0.2280659838605838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988287276","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9241289,0.051664237,0.00049734453,0.00070322346,0.00006984036,0.0000624992,0.00528191,0.000074712,0.017517354],"genre_scores_gemma":[0.96415806,0.028766839,0.0012387407,0.00010228855,0.00010062073,0.00002700423,0.0032327676,0.0000121895555,0.002361589],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992967,0.000009851271,0.000014869146,0.000014294581,0.000011769004,0.000019496647],"domain_scores_gemma":[0.9997929,0.000029541978,0.000095088966,0.000007130122,0.00005042379,0.000024935056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015046078,0.00028331284,0.0001450574,0.0049329037,0.00037386068,0.0005527615,0.00020410561,0.00015165484,0.0023223115],"category_scores_gemma":[0.0002124372,0.00010143107,0.00019343843,0.005351552,0.00016442641,0.00026916177,0.00034240488,0.0001369739,0.00021339337],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000111038644,0.000026757963,0.829066,0.0014423749,0.00019825043,0.0009595623,0.0023238258,0.0011632073,0.006571473,0.0008750115,0.002765856,0.15449663],"study_design_scores_gemma":[0.0000012173966,0.000011800477,0.9914363,0.00010551296,0.000022313961,0.00018477316,0.00062249776,0.00008714176,0.00016950017,0.000050190134,0.0073062936,0.0000024737644],"about_ca_topic_score_codex":0.025925133,"about_ca_topic_score_gemma":0.064654425,"teacher_disagreement_score":0.025925133,"about_ca_system_score_codex":0.0006613434,"about_ca_system_score_gemma":0.0005191804,"threshold_uncertainty_score":0.05154848},"labels":[],"label_agreement":null},{"id":"W1988942821","doi":"10.1029/2008jb005753","title":"Premonitory acoustic emissions and stick‐slip in natural and smooth‐faulted Westerly granite","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":146,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Acoustic emission; Slip (aerodynamics); Geology; Nucleation; Seismology; Fault plane; Fault (geology); Microscale chemistry; Amplitude; Shear (geology); Materials science; Petrology; Composite material; Optics; Engineering; Physics","score_opus":0.024311208543937486,"score_gpt":0.3010952093656005,"score_spread":0.27678400082166305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988942821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99988735,0.000012636907,0.00004252877,9.4145486e-7,3.2586485e-7,0.0000011643313,0.000020443258,0.0000016473894,0.000032853095],"genre_scores_gemma":[0.9996722,0.00001675256,0.00012535468,0.0000020930365,6.2397174e-7,0.0000035957262,0.00007780191,0.000001433009,0.0001002063],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99990547,0.000008486081,0.000005765004,0.000030445639,0.000023038168,0.00002689733],"domain_scores_gemma":[0.99985766,0.000025194071,0.000048101134,0.000013425463,0.00001939514,0.000036119764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009358888,0.00018198151,0.00018202767,0.00033272858,0.00014822748,0.00026573907,0.00020208317,0.0002637415,0.0003622287],"category_scores_gemma":[0.00019222402,0.00014849968,0.00010399157,0.00020407916,0.00049903436,0.00009935054,0.00018288552,0.00017187002,0.000053740434],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000350824,0.00002551643,0.011060824,0.000018779712,0.000010380307,0.00012946084,0.000083524355,0.00025949258,0.9873465,0.000021286576,0.000007605367,0.00068582885],"study_design_scores_gemma":[0.00004068454,0.0007941344,0.69673216,0.000005238613,0.000033485532,0.0003475013,0.0004341431,0.0033101006,0.29773283,0.00003638781,0.00051269814,0.000020591668],"about_ca_topic_score_codex":0.003075662,"about_ca_topic_score_gemma":0.004957696,"teacher_disagreement_score":0.003075662,"about_ca_system_score_codex":0.00029492396,"about_ca_system_score_gemma":0.00013436325,"threshold_uncertainty_score":0.006115496},"labels":[],"label_agreement":null},{"id":"W1989066011","doi":"10.1029/2010jb008015","title":"Full waveform tomographic images of the peak ring at the Chicxulub impact crater","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Impact crater; Geology; Lithology; Breccia; Impact structure; Sedimentary rock; Meteorite; Basement; Shock (circulatory); Petrology; Geophysics; Seismology; Geochemistry; Physics","score_opus":0.04348915459580823,"score_gpt":0.29099693895409695,"score_spread":0.2475077843582887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989066011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9586691,0.0004033596,0.004635674,0.00069894665,0.00007004187,0.00018598004,0.012957698,0.00078189565,0.021597166],"genre_scores_gemma":[0.9724036,0.00032986398,0.013756515,0.00016280779,0.000052226012,0.00007007106,0.009860413,0.00012576203,0.0032386086],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99992275,0.000002890881,0.0000034889545,0.000012890365,0.000040855743,0.000017163082],"domain_scores_gemma":[0.99982435,0.000020981988,0.000022694732,0.00001547689,0.00006048472,0.000056146542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010737189,0.0003549138,0.0001750662,0.0016759424,0.00043493407,0.00040118856,0.00045419077,0.00065194455,0.0060023093],"category_scores_gemma":[0.00023069514,0.00031739438,0.0001586559,0.0010475173,0.00022862304,0.00026906273,0.00037832075,0.00057983195,0.00064793957],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016713085,0.00091204135,0.12643212,0.0009633399,0.00023782573,0.008842161,0.0014896705,0.020384902,0.7082323,0.0021844658,0.036786843,0.09186296],"study_design_scores_gemma":[0.000075370874,0.00015253879,0.9455692,0.00014188988,0.000059468694,0.0029543315,0.0005972955,0.029903911,0.0131547395,0.00017599872,0.007140706,0.00007449099],"about_ca_topic_score_codex":0.016931556,"about_ca_topic_score_gemma":0.048999578,"teacher_disagreement_score":0.016931556,"about_ca_system_score_codex":0.0003753976,"about_ca_system_score_gemma":0.0006166115,"threshold_uncertainty_score":0.033666015},"labels":[],"label_agreement":null},{"id":"W1989109638","doi":"10.1139/e05-116","title":"Structural geology of the Penobsquis salt structure: late Bashkirian inversion tectonics in the Moncton Basin, New Brunswick, eastern Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Salt tectonics; Anticline; Tectonics; Structural basin; Diapir; Thrust fault; Paleontology; Geochemistry; Inversion (geology); Seismology; Petrology; Geomorphology","score_opus":0.012487436810704518,"score_gpt":0.18479582316352056,"score_spread":0.17230838635281603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989109638","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978009,0.00020297947,0.00004739216,0.00005356604,0.000002044008,0.000009008065,0.00032150385,0.0000042462716,0.001558388],"genre_scores_gemma":[0.9985331,0.00015580043,0.000114485636,0.000013144902,8.9548035e-7,0.0000037003213,0.00028718595,0.0000021711533,0.0008893794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998611,0.000009656291,0.000006679271,0.000026705544,0.000040285384,0.000055530454],"domain_scores_gemma":[0.9997608,0.000017751812,0.00005141872,0.000008888905,0.00010664504,0.000054517808],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019813262,0.0002005826,0.00016485217,0.0012163938,0.0009882211,0.000877513,0.00048647934,0.00016055423,0.0010937237],"category_scores_gemma":[0.00040997643,0.00017668432,0.0001156526,0.0016752469,0.0006683873,0.00029524972,0.00058236136,0.0002073494,0.000087595334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011039757,0.000032254036,0.96448386,0.000058348956,0.000040079784,0.00051774556,0.003251577,0.0007881347,0.006493923,0.0005618261,0.0004710474,0.023190774],"study_design_scores_gemma":[0.0000023635198,0.000007197492,0.9976928,0.000008951676,0.0000036349684,0.00004230374,0.0010885865,0.00024456938,0.00012293826,0.000013526363,0.00076886266,0.0000042452734],"about_ca_topic_score_codex":0.971762,"about_ca_topic_score_gemma":0.99359185,"teacher_disagreement_score":0.028237998,"about_ca_system_score_codex":0.0119036995,"about_ca_system_score_gemma":0.010133487,"threshold_uncertainty_score":0.086367846},"labels":[],"label_agreement":null},{"id":"W1989235867","doi":"10.1002/2014gl062767","title":"InSAR imaging of displacement on flexural‐slip faults triggered by the 2013 <i>Mw</i> 6.6 Lake Grassmere earthquake, central New Zealand","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"New Zealand Government","keywords":"Slip (aerodynamics); Geology; Interferometric synthetic aperture radar; Seismology; Episodic tremor and slip; Epicenter; Flexural strength; Synthetic aperture radar; Subduction; Tectonics; Remote sensing","score_opus":0.04101361224465221,"score_gpt":0.2871871244287047,"score_spread":0.24617351218405248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989235867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976356,0.000043212553,0.0001339833,0.000035595163,0.0000049606383,0.0000073249535,0.00067120156,0.000019179603,0.0014489247],"genre_scores_gemma":[0.9982856,0.00007061515,0.0004337566,0.00001679435,0.000004804445,0.000004411456,0.00061874243,0.000004966673,0.0005604046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994385,0.0000027699075,0.000003120659,0.000012424262,0.000021078426,0.000016805603],"domain_scores_gemma":[0.9998325,0.00000954727,0.00006186386,0.000011123528,0.00004554648,0.00003936186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012210669,0.0002050769,0.00016861994,0.0006783712,0.0003552237,0.0004078547,0.00020800345,0.0002190002,0.0010897851],"category_scores_gemma":[0.00030167145,0.00022481901,0.000107796805,0.00056256703,0.0003292305,0.00024911185,0.00037515792,0.00020621651,0.00021012158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078985107,0.00016778988,0.72829694,0.00013305705,0.000112566755,0.001348575,0.0017635663,0.0037241015,0.2254984,0.00025793587,0.003520779,0.03438638],"study_design_scores_gemma":[0.000012117486,0.000022836331,0.99664956,0.00000556491,0.000013896767,0.000059113754,0.00019394136,0.0012537024,0.0012342108,0.000016370444,0.0005324697,0.0000062190984],"about_ca_topic_score_codex":0.13687602,"about_ca_topic_score_gemma":0.27976263,"teacher_disagreement_score":0.13687602,"about_ca_system_score_codex":0.0006145627,"about_ca_system_score_gemma":0.00037918641,"threshold_uncertainty_score":0.27215862},"labels":[],"label_agreement":null},{"id":"W1989700220","doi":"10.1038/nature09828","title":"Seismic tremors and magma wagging during explosive volcanism","year":2011,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Volcano; Magma; Explosive eruption; Silicic; Seismology; Geophysics; Electrical conduit; Magma chamber; Volcanism; Oscillation (cell signaling); Petrology; Tectonics; Chemistry","score_opus":0.014206877530195894,"score_gpt":0.1951725269557046,"score_spread":0.18096564942550872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989700220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905986,0.00014288859,0.00003846344,0.000022087612,0.0000034510624,0.0000020662162,0.00007558016,0.0000024179353,0.00065312214],"genre_scores_gemma":[0.9993581,0.00015824274,0.000044563978,0.000009793031,0.000018063023,0.000002086783,0.00011277285,0.0000016845254,0.00029457142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999255,0.000017201703,0.000009362372,0.000012372376,0.000017532915,0.000017997463],"domain_scores_gemma":[0.99928963,0.00023604855,0.00030751555,0.000037479465,0.000053838055,0.000075472846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022308493,0.00014943419,0.00014265245,0.0011928674,0.0003745549,0.0005772461,0.00017290906,0.0004480896,0.00094373076],"category_scores_gemma":[0.0020503884,0.00015671793,0.00012770876,0.00097446755,0.00038746744,0.00037359828,0.00028454914,0.00025855112,0.00015781833],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028135541,0.00019113629,0.94058484,0.00008072977,0.00014738181,0.0013160091,0.0037830935,0.0005318854,0.02350692,0.00043367606,0.00038351573,0.026227161],"study_design_scores_gemma":[0.0000057392035,0.000065383036,0.9985815,0.0000045063593,0.000011073264,0.00019489709,0.00045522864,0.00012186594,0.0002645625,0.0000750664,0.0002170946,0.0000030575154],"about_ca_topic_score_codex":0.0070172097,"about_ca_topic_score_gemma":0.018241936,"teacher_disagreement_score":0.0070172097,"about_ca_system_score_codex":0.00027122366,"about_ca_system_score_gemma":0.0001309189,"threshold_uncertainty_score":0.0139526725},"labels":[],"label_agreement":null},{"id":"W1989752319","doi":"10.1016/j.jvolgeores.2010.12.012","title":"Interpretation of Nisyros volcanic terrain using land surface parameters generated from the ASTER Global Digital Elevation Model","year":2010,"lang":"en","type":"article","venue":"Journal of Volcanology and Geothermal Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"Concordia University; National Aeronautics and Space Administration","keywords":"Geology; Caldera; Volcano; Digital elevation model; Tectonics; Advanced Spaceborne Thermal Emission and Reflection Radiometer; Lava; Seismology; Fault (geology); Geomorphology; Remote sensing","score_opus":0.046666704136811024,"score_gpt":0.30756670921453855,"score_spread":0.26090000507772754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989752319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8472878,0.0006126036,0.050208226,0.00076424645,0.00041374564,0.00019383253,0.039933257,0.012190625,0.048395813],"genre_scores_gemma":[0.9625559,0.00029244644,0.024805706,0.000026800677,0.000022391947,0.00003234987,0.009544295,0.00043039513,0.0022897737],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99996316,0.000003840524,0.000003999367,0.0000100751595,0.00001283807,0.000005988259],"domain_scores_gemma":[0.99992335,0.000010028487,0.000010990824,0.000016744434,0.000031163137,0.000007821956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008795089,0.00034655366,0.00018879186,0.00086372887,0.00019705758,0.0007136273,0.00025448084,0.00023258236,0.0043768557],"category_scores_gemma":[0.0003192529,0.00014572174,0.00021530633,0.00066450716,0.0000940254,0.00026657776,0.00026516127,0.00024131192,0.0009130886],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014552817,0.0003581335,0.15835875,0.0007379766,0.00034796767,0.003293089,0.0012757161,0.39201587,0.079280704,0.008249204,0.044633865,0.30999342],"study_design_scores_gemma":[0.0002811522,0.00004735484,0.17287138,0.00017646787,0.00014546615,0.00037343448,0.0010278933,0.7726115,0.011130411,0.0030292156,0.0382466,0.000059172835],"about_ca_topic_score_codex":0.011150016,"about_ca_topic_score_gemma":0.018242856,"teacher_disagreement_score":0.011150016,"about_ca_system_score_codex":0.00024529884,"about_ca_system_score_gemma":0.00034512236,"threshold_uncertainty_score":0.022170186},"labels":[],"label_agreement":null},{"id":"W1990115551","doi":"10.1007/s00445-015-0901-7","title":"Experiments with vertically and laterally migrating subsurface explosions with applications to the geology of phreatomagmatic and hydrothermal explosion craters and diatremes","year":2015,"lang":"en","type":"article","venue":"Bulletin of Volcanology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Diatreme; Impact crater; Phreatomagmatic eruption; Geology; Ejecta; Seismology; Volcano; Maar; Petrology; Geophysics; Magma; Kimberlite; Astrobiology","score_opus":0.019838185144393866,"score_gpt":0.21636135048280866,"score_spread":0.1965231653384148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990115551","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998879,0.00001628915,0.0006394754,0.000013358263,0.000004915332,0.00003839107,0.00006146646,0.000011599995,0.00033540977],"genre_scores_gemma":[0.9967301,0.00008317449,0.0020217397,0.000025778396,0.000006955148,0.00008677182,0.000203141,0.000015032563,0.00082725205],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998049,0.000039016344,0.000018505712,0.00005084572,0.00003192723,0.000054807457],"domain_scores_gemma":[0.99878603,0.00068438525,0.00010328756,0.00015633111,0.000110058354,0.00016005516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044476474,0.0005025218,0.00042179076,0.00026753126,0.0005992728,0.0004539231,0.0006053446,0.0006400357,0.0018701347],"category_scores_gemma":[0.0012892804,0.00034743192,0.00034411115,0.00045394085,0.00073952926,0.00041754797,0.0006865276,0.0009231911,0.00013149015],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.010851926,0.003681458,0.021207893,0.00018172603,0.00009840176,0.00037010992,0.0014087192,0.0073478906,0.9400656,0.00096955954,0.00015943906,0.013657317],"study_design_scores_gemma":[0.0038650946,0.05700186,0.16632676,0.00005335873,0.00040256296,0.00060451083,0.0027873677,0.060149487,0.703126,0.0031155841,0.0023996572,0.00016775289],"about_ca_topic_score_codex":0.0038808326,"about_ca_topic_score_gemma":0.0038700309,"teacher_disagreement_score":0.0038808326,"about_ca_system_score_codex":0.00030919292,"about_ca_system_score_gemma":0.0003892328,"threshold_uncertainty_score":0.007716477},"labels":[],"label_agreement":null},{"id":"W1990153816","doi":"10.1130/ges00899.1","title":"Simulated tsunami inundation for a range of Cascadia megathrust earthquake scenarios at Bandon, Oregon, USA","year":2013,"lang":"en","type":"article","venue":"Geosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Geology; Seismology; Slip (aerodynamics); Subduction; Submarine pipeline; Tsunami earthquake; Moment magnitude scale; Shore; Fault (geology); Geotechnical engineering; Tectonics; Oceanography","score_opus":0.014118191838045892,"score_gpt":0.21106940117721665,"score_spread":0.19695120933917076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990153816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99551696,0.000012602435,0.00037477064,0.00007753314,0.000004862524,0.000015427137,0.0015034787,0.000049358932,0.0024450962],"genre_scores_gemma":[0.9973762,0.00003197591,0.00050950114,0.00001630084,0.0000014691044,0.000022798167,0.0015425087,0.000007827482,0.0004914025],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999211,0.000021998134,0.000007648602,0.000020156149,0.000011951443,0.000017216744],"domain_scores_gemma":[0.99970007,0.00013818704,0.000036811918,0.000021926755,0.00005366779,0.00004934885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024630563,0.00050448667,0.0001924595,0.00038288912,0.00034271207,0.00051945535,0.00059552625,0.00046968533,0.0020542215],"category_scores_gemma":[0.00096760393,0.00023236094,0.00034671588,0.00056960486,0.00026095708,0.0004862086,0.0003236703,0.00036574708,0.00014031706],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021990458,0.00020253478,0.09723902,0.00003210353,0.0000882462,0.00027921956,0.00010853029,0.89486676,0.0011227198,0.00077029224,0.0016307343,0.0034399435],"study_design_scores_gemma":[0.00014743822,0.0001461719,0.028299885,0.000012656752,0.000044441902,0.00004296204,0.00032935286,0.9686357,0.0010012804,0.00052609283,0.000794517,0.000019481648],"about_ca_topic_score_codex":0.08370421,"about_ca_topic_score_gemma":0.11582802,"teacher_disagreement_score":0.08370421,"about_ca_system_score_codex":0.0011201933,"about_ca_system_score_gemma":0.0005091405,"threshold_uncertainty_score":0.16643399},"labels":[],"label_agreement":null},{"id":"W1990502229","doi":"10.5194/npg-14-5-2007","title":"An Ising model for earthquake dynamics","year":2007,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Junta de Andalucía; Universidad de Almería; Fundación Ramón Areces","keywords":"Ising model; Representation (politics); Range (aeronautics); Statistical physics; Hazard; Cellular automaton; Computer science; Geology; Seismic hazard; Dynamics (music); Seismology; Physics; Algorithm","score_opus":0.02045780133637347,"score_gpt":0.2695970276054641,"score_spread":0.24913922626909063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990502229","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04737093,0.004332473,0.8675734,0.0043519903,0.0011232961,0.00017810242,0.0061251707,0.0014526879,0.067491904],"genre_scores_gemma":[0.81184214,0.004293901,0.07995953,0.0004888146,0.00063331955,0.0005196797,0.0037463729,0.00024197494,0.098274305],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996667,0.00011683362,0.00002196424,0.000073861855,0.000078759054,0.00004187947],"domain_scores_gemma":[0.999129,0.0004572426,0.00010216896,0.00010689218,0.00015638761,0.000048302823],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000747558,0.0008884189,0.0014253794,0.001079213,0.00076362916,0.0016333184,0.0020005684,0.002180963,0.014656939],"category_scores_gemma":[0.003118278,0.00039992522,0.00093224016,0.0018030315,0.0008604714,0.0022358363,0.0007499597,0.0020903442,0.0037050643],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056148114,0.000052626787,0.0011391267,0.000110476765,0.0000677806,0.0002799038,0.000116291674,0.6493976,0.0006900895,0.32311904,0.009227969,0.01574292],"study_design_scores_gemma":[0.000010759144,0.000009607934,0.00012131577,0.000009456839,0.000010050052,0.000029406223,0.000010344757,0.9357256,0.000043113847,0.061374392,0.0026472227,0.0000086981345],"about_ca_topic_score_codex":0.015520208,"about_ca_topic_score_gemma":0.013048568,"teacher_disagreement_score":0.015520208,"about_ca_system_score_codex":0.0013702993,"about_ca_system_score_gemma":0.0011667957,"threshold_uncertainty_score":0.04903233},"labels":[],"label_agreement":null},{"id":"W1991121218","doi":"10.1029/2003gl017586","title":"Distribution of the Pacific/North America motion in the Queen Charlotte Islands‐S. Alaska plate boundary zone","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Pacific Plate; Seismology; North American Plate; Plate tectonics; Sinistral and dextral; Transform fault; Tectonics; Subduction; Oceanography","score_opus":0.020973258896008862,"score_gpt":0.24964086480731607,"score_spread":0.2286676059113072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991121218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99839145,0.00014686924,0.00003078899,0.000017315122,0.0000011884524,0.0000017752291,0.00020080045,0.0000045665565,0.0012051687],"genre_scores_gemma":[0.9992099,0.000102924816,0.00007101104,0.0000048132697,0.0000011636478,0.0000027426597,0.0002548038,0.0000012451443,0.00035142305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998903,0.000012663969,0.0000099229665,0.000034208537,0.000024962068,0.000028016562],"domain_scores_gemma":[0.9993303,0.00007852214,0.00019881445,0.000042328185,0.0002184368,0.00013158037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018974383,0.00009976208,0.00011678162,0.0012788001,0.0006566294,0.00061374943,0.0002043385,0.0001681601,0.0011049465],"category_scores_gemma":[0.00081603206,0.00013296913,0.00008921422,0.001011246,0.00045500524,0.00017438346,0.000411552,0.00011688924,0.0001704791],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013112627,0.000009366691,0.9821562,0.000027507904,0.00003483834,0.00020901648,0.0015005977,0.0011408132,0.0031394842,0.00018145436,0.00045016775,0.011019307],"study_design_scores_gemma":[0.0000031150887,0.000008879175,0.99825984,0.0000106145635,0.0000070263773,0.00005603618,0.00045746434,0.00048329134,0.00014120959,0.000015793104,0.0005510093,0.0000057991083],"about_ca_topic_score_codex":0.614911,"about_ca_topic_score_gemma":0.77607244,"teacher_disagreement_score":0.38508898,"about_ca_system_score_codex":0.0017691347,"about_ca_system_score_gemma":0.0009735711,"threshold_uncertainty_score":0.7747137},"labels":[],"label_agreement":null},{"id":"W1991276707","doi":"10.1029/2004eo360004","title":"Reply [to “Comment on ‘Coupling semantics and science in earthquake research’”]","year":2004,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Slip (aerodynamics); Meaning (existential); Semantics (computer science); Epistemology; Theoretical physics; Computer science; Philosophy; Physics; Programming language","score_opus":0.05390975008416199,"score_gpt":0.30344479739411373,"score_spread":0.24953504730995174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991276707","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00018052381,0.0004686671,0.0002598561,0.9819546,0.015265975,0.000012144085,0.00012919726,0.00006984374,0.001659247],"genre_scores_gemma":[0.0016098744,0.00018357395,0.00015550165,0.98611176,0.008845249,0.00003928399,0.000035431694,0.00003898412,0.002980302],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99508625,0.0011644197,0.0006051758,0.00093827344,0.0014576194,0.0007481331],"domain_scores_gemma":[0.98414546,0.0072659706,0.0014042036,0.0006165385,0.0053177816,0.0012500345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008324304,0.0012548974,0.0016632797,0.0013458725,0.0063219327,0.0043235365,0.0057120626,0.045614198,0.014037285],"category_scores_gemma":[0.041160237,0.0013593555,0.0021522227,0.0016548905,0.007031145,0.007407879,0.003919931,0.04392705,0.009612397],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015812637,0.0000049684268,0.00010446667,0.000027423777,0.000008574821,0.00011915698,0.00023725869,0.000027908314,0.00006189835,0.0020087636,0.9963245,0.0010592272],"study_design_scores_gemma":[0.00005524931,0.000036944257,0.00244701,0.00028179123,0.000038534392,0.00032394283,0.0013924665,0.000287876,0.00035413945,0.010189975,0.98444587,0.00014627993],"about_ca_topic_score_codex":0.027041344,"about_ca_topic_score_gemma":0.02957308,"teacher_disagreement_score":0.045614198,"about_ca_system_score_codex":0.004902604,"about_ca_system_score_gemma":0.004965196,"threshold_uncertainty_score":0.05376792},"labels":[],"label_agreement":null},{"id":"W1991455340","doi":"10.1016/j.sedgeo.2014.12.004","title":"Seismites within Ordovician–Silurian carbonates and clastics of Southern Ontario, Canada and implications for intraplate seismicity","year":2014,"lang":"en","type":"article","venue":"Sedimentary Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Centre for Global Change Science, University of Toronto; Natural Sciences and Engineering Research Council of Canada; Tel Aviv University; Nuclear Waste Management Organization","keywords":"Geology; Ordovician; Paleontology; Paleozoic; Dolostone; Basement; Sedimentary rock; Unconformity; Precambrian; Slumping; Foreland basin; Carbonate rock; Structural basin","score_opus":0.007461361062577164,"score_gpt":0.1840132575640842,"score_spread":0.17655189650150704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991455340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99441886,0.0005676389,0.00008680053,0.000119024844,0.000005265538,0.000017026423,0.0010981517,0.000006628095,0.0036806706],"genre_scores_gemma":[0.997083,0.00035033826,0.0001314451,0.000029479279,0.000003724737,0.000008386111,0.0004718241,0.0000058759615,0.0019160035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996357,0.00002195177,0.00002512967,0.00005987397,0.00008683559,0.0001704823],"domain_scores_gemma":[0.9986149,0.00009623038,0.0002438885,0.000027865837,0.0007533638,0.00026380166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032215533,0.00029634984,0.00028690576,0.004575239,0.0038113932,0.0018364814,0.00092622556,0.00029701684,0.0027284694],"category_scores_gemma":[0.0018499846,0.0003288497,0.00024751094,0.00760125,0.0014961227,0.00045473923,0.0011953566,0.00033490092,0.0002252434],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001694839,0.00002132146,0.9612139,0.00012915069,0.00007233885,0.0003137543,0.014514178,0.00046950945,0.00271404,0.00071813125,0.00088779756,0.018776331],"study_design_scores_gemma":[0.000002235877,0.0000045055435,0.9944382,0.000020458621,0.000009228003,0.00003346986,0.0041953796,0.00009772352,0.000061973304,0.00002411192,0.0011088225,0.0000039416286],"about_ca_topic_score_codex":0.9955635,"about_ca_topic_score_gemma":0.99903774,"teacher_disagreement_score":0.022953447,"about_ca_system_score_codex":0.022953447,"about_ca_system_score_gemma":0.024969839,"threshold_uncertainty_score":0.16653973},"labels":[],"label_agreement":null},{"id":"W1992363677","doi":"10.1038/nature11032","title":"Deformation cycles of subduction earthquakes in a viscoelastic Earth","year":2012,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":477,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Subduction; Geology; Geodetic datum; Seismology; Deformation (meteorology); Mantle (geology); Viscoelasticity; Plate tectonics; Lithosphere; Geodesy; Geodynamics; Crust; Geophysics; Tectonics","score_opus":0.009893383040427611,"score_gpt":0.22556080145461094,"score_spread":0.21566741841418333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992363677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984944,0.000038146918,0.0004580899,0.00005841799,0.0000020123848,0.0000026634307,0.00014086398,0.000009458706,0.00079595816],"genre_scores_gemma":[0.9994618,0.000027527482,0.00013934514,0.0000050632357,0.000001909061,0.0000017717172,0.000085132786,0.00000374275,0.00027373538],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999603,0.0000073853366,0.000006646078,0.000010924036,0.0000067004776,0.000008089644],"domain_scores_gemma":[0.99963343,0.00013444251,0.000091871145,0.00004234086,0.000052725067,0.000045214325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002138961,0.00010657074,0.00014894467,0.0008994875,0.00028026148,0.0005174325,0.00024827034,0.0003497499,0.0018075978],"category_scores_gemma":[0.0016144771,0.00021352648,0.00017786365,0.0006982257,0.00040167783,0.00064498995,0.00027573985,0.00018425428,0.00013975517],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007161449,0.00033675754,0.5442347,0.0001232791,0.00016146926,0.00095608516,0.0016302308,0.33425012,0.031446725,0.02162048,0.0030072134,0.06151677],"study_design_scores_gemma":[0.000029592551,0.0001235621,0.5645892,0.0000170677,0.000030196336,0.0003436011,0.0004119509,0.4251685,0.0016705879,0.006038977,0.001537083,0.000039556562],"about_ca_topic_score_codex":0.006831589,"about_ca_topic_score_gemma":0.006897012,"teacher_disagreement_score":0.006831589,"about_ca_system_score_codex":0.00048344632,"about_ca_system_score_gemma":0.00019516544,"threshold_uncertainty_score":0.01358366},"labels":[],"label_agreement":null},{"id":"W1992442729","doi":"10.1038/nature02755","title":"Hydrological response to a seafloor spreading episode on the Juan de Fuca ridge","year":2004,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Seafloor spreading; Ridge; Geology; Oceanography; Paleontology","score_opus":0.01467466277496626,"score_gpt":0.24254047814981122,"score_spread":0.22786581537484496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992442729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948514,0.0000063889815,0.000012747808,0.0000451993,0.0000035072958,0.0000018867647,0.00007687531,0.0000036096196,0.0003647131],"genre_scores_gemma":[0.99969494,0.000012069084,0.000020686804,0.0000117527725,0.000005598548,0.000001880101,0.0001107712,0.00000108907,0.00014124089],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999305,0.000013357704,0.0000046215455,0.000013976436,0.000009573863,0.000027927412],"domain_scores_gemma":[0.9996698,0.00006299608,0.00007741087,0.000020953972,0.000059833146,0.0001089401],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019491235,0.00012364097,0.00022155767,0.00031165316,0.00046562921,0.0004668563,0.00020957613,0.00062000676,0.0010389438],"category_scores_gemma":[0.00089032174,0.000102639315,0.000175279,0.00038540334,0.00039367165,0.00019312017,0.00042591745,0.00030167695,0.00009727687],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014985733,0.00038160992,0.94575614,0.00005573445,0.00021680882,0.0012666547,0.0017948895,0.009734061,0.028169185,0.000450658,0.0013257442,0.009350056],"study_design_scores_gemma":[0.00001308754,0.000051401545,0.9966324,0.0000034043185,0.000016232363,0.000034851444,0.00046555954,0.0022446746,0.00023143373,0.000041023508,0.00026073653,0.000005089486],"about_ca_topic_score_codex":0.049097482,"about_ca_topic_score_gemma":0.07758389,"teacher_disagreement_score":0.049097482,"about_ca_system_score_codex":0.0007526295,"about_ca_system_score_gemma":0.0004937339,"threshold_uncertainty_score":0.09762341},"labels":[],"label_agreement":null},{"id":"W1992742780","doi":"10.2495/dne-v5-n3-242-253","title":"Constructal theory of plate tectonics","year":2010,"lang":"en","type":"article","venue":"International Journal of Design & Nature and Ecodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geometry; Vorticity; Lithosphere; Toroid; Geology; Physics; Convection; Mantle convection; Geophysics; Vortex; Mechanics; Tectonics; Mathematics; Seismology; Plasma","score_opus":0.008141577566958373,"score_gpt":0.22142586777712178,"score_spread":0.2132842902101634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992742780","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021566149,0.009156762,0.6538573,0.00748174,0.001276542,0.000101172525,0.0013719368,0.00068026315,0.30450812],"genre_scores_gemma":[0.66618377,0.0103332875,0.20018138,0.0019703922,0.0025561794,0.0004238159,0.0020698728,0.0006048408,0.115676515],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9991473,0.00024614684,0.000055272783,0.000191812,0.0002808156,0.0000786239],"domain_scores_gemma":[0.9991252,0.0002636278,0.00011416287,0.00014467449,0.00028042725,0.00007192708],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009773136,0.0009506321,0.00062627776,0.0032709595,0.0016204247,0.003243596,0.0012599642,0.0010259823,0.010416087],"category_scores_gemma":[0.0020605,0.00033490092,0.0011924839,0.0019443108,0.0071932464,0.0030848342,0.0023773909,0.0023726332,0.0023878624],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000010211288,0.0000010026292,0.00004686228,0.000013911721,0.0000021400278,0.000009482157,0.000053137177,0.00083062926,0.000033404613,0.9963319,0.0007262395,0.0019503629],"study_design_scores_gemma":[0.0000035178555,0.000007050619,0.00012939604,0.000015970454,0.000003234708,0.000040505467,0.000035021243,0.0073409467,0.00005363314,0.9628232,0.029541438,0.0000060071507],"about_ca_topic_score_codex":0.0052292314,"about_ca_topic_score_gemma":0.0029588172,"teacher_disagreement_score":0.010416087,"about_ca_system_score_codex":0.0028245812,"about_ca_system_score_gemma":0.0009537157,"threshold_uncertainty_score":0.034845293},"labels":[],"label_agreement":null},{"id":"W1993339143","doi":"10.1016/j.jog.2006.06.002","title":"Role of background viscosity in the investigation of postglacial rebound induced crustal motion in a laterally heterogeneous mantle","year":2006,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Forskningsrådet om Hälsa, Arbetsliv och Välfärd","keywords":"Geology; Post-glacial rebound; Classification of discontinuities; Lithosphere; Viscosity; Discontinuity (linguistics); Viscoelasticity; Deglaciation; Mantle (geology); Geophysics; Geodesy; Seismology; Glacial period; Tectonics; Geomorphology; Thermodynamics; Physics","score_opus":0.012095687827225544,"score_gpt":0.20913478849501396,"score_spread":0.19703910066778843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993339143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972826,0.0002423906,0.0016853441,0.000032208347,0.0000045285256,0.0000054136694,0.000037062353,0.000025818184,0.00068468234],"genre_scores_gemma":[0.99942696,0.0000960793,0.00035321366,0.000005075638,0.0000037206548,0.0000025014242,0.000019277237,0.0000096142485,0.00008362892],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999509,0.000011914245,0.0000037711802,0.00001140775,0.0000074848467,0.000014482589],"domain_scores_gemma":[0.99976796,0.00011818131,0.00003767796,0.00001814711,0.00002240621,0.000035635785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003205839,0.0003478225,0.00032322656,0.00061708683,0.00027122805,0.0010468838,0.00031230928,0.0003200843,0.0007358565],"category_scores_gemma":[0.0009850336,0.00026057297,0.00021358024,0.0004247775,0.0003710402,0.0007533765,0.0005047289,0.00050835684,0.00007415709],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028739765,0.00032140402,0.14746034,0.0002977019,0.00027818658,0.0013066351,0.00072294835,0.06051254,0.74227124,0.005274724,0.00013364818,0.038546566],"study_design_scores_gemma":[0.00020851617,0.0011606321,0.4797714,0.000053360083,0.0003479634,0.0004242024,0.0006195568,0.4093992,0.10531905,0.00172537,0.0008650065,0.00010576568],"about_ca_topic_score_codex":0.0021759816,"about_ca_topic_score_gemma":0.001765057,"teacher_disagreement_score":0.0021759816,"about_ca_system_score_codex":0.00033846663,"about_ca_system_score_gemma":0.00026529227,"threshold_uncertainty_score":0.0043266416},"labels":[],"label_agreement":null},{"id":"W1993875743","doi":"10.1134/s1075701508050012","title":"The Antei uranium deposit: A natural analogue of an SNF repository and an underground geodynamic laboratory in granite","year":2008,"lang":"en","type":"article","venue":"Geology of Ore Deposits","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Massif; Geology; Uranium ore; Geochemistry; Uranium; Petrography; Stockwork; Natural (archaeology); Mining engineering; Mineralogy; Paleontology; Chemistry","score_opus":0.00760757555960342,"score_gpt":0.20439989423836982,"score_spread":0.1967923186787664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993875743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954992,0.00014987726,0.00032321818,0.00004049715,0.000004778823,0.00001431212,0.00014888731,0.000035462446,0.0037837115],"genre_scores_gemma":[0.9972174,0.00006512748,0.00079296663,0.000008028129,0.000003032656,0.000011051348,0.0001536493,0.000005819588,0.0017428404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999814,0.000017490565,0.000010964685,0.000070859285,0.000037725506,0.00004899487],"domain_scores_gemma":[0.9998103,0.000023792365,0.000080761645,0.00002973816,0.000021111518,0.000034331653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021062705,0.00023911326,0.00021624591,0.001884432,0.0011697509,0.0008323174,0.0006082849,0.0006221116,0.0018451385],"category_scores_gemma":[0.00045761093,0.00027602707,0.00016243116,0.0022988599,0.0012862331,0.0004311327,0.0012513525,0.00026498083,0.00041467295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017623279,0.0001638992,0.88676417,0.0002193086,0.00005455619,0.0071217967,0.0039027724,0.0013822601,0.04287711,0.0028952395,0.00044131596,0.052415267],"study_design_scores_gemma":[0.000042818956,0.00022825139,0.9792203,0.000039457656,0.00003231001,0.0044497736,0.0028675152,0.00093282247,0.0036980147,0.0004920094,0.007973326,0.000023438653],"about_ca_topic_score_codex":0.018088738,"about_ca_topic_score_gemma":0.0583441,"teacher_disagreement_score":0.018088738,"about_ca_system_score_codex":0.0013051622,"about_ca_system_score_gemma":0.0011106293,"threshold_uncertainty_score":0.035966873},"labels":[],"label_agreement":null},{"id":"W1994478348","doi":"10.1126/science.1161927","title":"Laboratory Simulation of Volcano Seismicity","year":2008,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":170,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Induced seismicity; Volcano; Microseism; Geology; Seismology; Basalt; Mud volcano; Shear (geology); Pore water pressure; Petrology; Geotechnical engineering","score_opus":0.02301235038267178,"score_gpt":0.23287160710791344,"score_spread":0.20985925672524167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994478348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858283,0.00007818186,0.007934355,0.00019922708,0.00003791756,0.00005339661,0.00076481386,0.00021263995,0.004891176],"genre_scores_gemma":[0.9963175,0.00004455845,0.00267275,0.000018589646,0.0000051779066,0.00009294442,0.00025653283,0.000009165127,0.00058283325],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998858,0.000020440146,0.0000064664896,0.000029015364,0.000026306307,0.00003190899],"domain_scores_gemma":[0.9990995,0.00050181657,0.00010241021,0.00007397676,0.00011919852,0.000103036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031858037,0.00031408714,0.00040311785,0.00024104404,0.00025351602,0.00049575896,0.00084224896,0.00078040507,0.0022405258],"category_scores_gemma":[0.0014910784,0.0002082378,0.00029498467,0.00025550436,0.0006099589,0.0003831495,0.00060090853,0.0006547228,0.00016625313],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036033918,0.00044187752,0.008804783,0.000090239046,0.000043458338,0.0002621138,0.00007777519,0.971989,0.011683933,0.0026798954,0.00071706506,0.002849536],"study_design_scores_gemma":[0.000080771475,0.00021884346,0.0012006096,0.000004550058,0.0000124665585,0.000014421933,0.00003283646,0.9948508,0.0026390136,0.0005894742,0.00034696207,0.000009285535],"about_ca_topic_score_codex":0.0053375848,"about_ca_topic_score_gemma":0.0029127197,"teacher_disagreement_score":0.0053375848,"about_ca_system_score_codex":0.00045956476,"about_ca_system_score_gemma":0.00048148882,"threshold_uncertainty_score":0.010613084},"labels":[],"label_agreement":null},{"id":"W1994539911","doi":"10.1130/g25101a.1","title":"San Andreas fault geometry through the San Gorgonio Pass, California","year":2009,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University","keywords":"Citation; Icon; Library science; San andreas fault; Geology; Download; Art history; History; Fault (geology); World Wide Web; Computer science; Paleontology","score_opus":0.014392382154157269,"score_gpt":0.22576140732645694,"score_spread":0.21136902517229966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994539911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7071599,0.0048754252,0.0016249921,0.0038073573,0.00032195103,0.00012136587,0.002527988,0.0006964788,0.2788646],"genre_scores_gemma":[0.9611936,0.0017422327,0.0018627793,0.000087057815,0.00006770971,0.000026785165,0.0015665933,0.000042906297,0.033410233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973685,0.000014226525,0.000008702192,0.00006399663,0.0001329873,0.00004321775],"domain_scores_gemma":[0.9998258,0.000011698373,0.00003395881,0.000012499613,0.00008876712,0.000027257023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016160282,0.0001781573,0.00024020983,0.0007806888,0.0011871844,0.00078473997,0.00034521206,0.00047336606,0.007075005],"category_scores_gemma":[0.0007410569,0.00017967833,0.00010398522,0.0010648658,0.00072948146,0.00044064323,0.0006116716,0.00048792365,0.001190652],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007689856,0.00025807903,0.47718027,0.0006212914,0.00013831296,0.003812366,0.0075297058,0.014076571,0.016232397,0.043506444,0.15324566,0.28262985],"study_design_scores_gemma":[0.00010495752,0.00016066135,0.7050845,0.0002067498,0.000051634288,0.0006955655,0.0020611668,0.0025879107,0.0010523681,0.0030735217,0.28489175,0.000029275969],"about_ca_topic_score_codex":0.17404012,"about_ca_topic_score_gemma":0.3123222,"teacher_disagreement_score":0.17404012,"about_ca_system_score_codex":0.001700601,"about_ca_system_score_gemma":0.002888592,"threshold_uncertainty_score":0.3460542},"labels":[],"label_agreement":null},{"id":"W1994701284","doi":"10.1186/bf03352818","title":"Displacement analysis of the GPS station of Sampali, Indonesia","year":2008,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Precise Point Positioning; Geodesy; Global Positioning System; Displacement (psychology); Geology; Geography; Seismology; Telecommunications; Engineering","score_opus":0.01636343281951252,"score_gpt":0.20850962572997908,"score_spread":0.19214619291046656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994701284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98430496,0.000090592825,0.0015315661,0.000060643568,0.000015065923,0.000043165357,0.0044798297,0.000082251,0.009391939],"genre_scores_gemma":[0.99302846,0.000081068705,0.0018135251,0.000013594558,0.000006026632,0.000034621025,0.0032879561,0.000011205702,0.0017234716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988294,0.000015894666,0.000008677605,0.000029384306,0.000046914985,0.000016067157],"domain_scores_gemma":[0.99982363,0.000021873428,0.000033754484,0.000017474395,0.00008201828,0.000021279451],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012771021,0.00021393018,0.00019030352,0.0011927254,0.00026131162,0.00037264926,0.00031378094,0.00016777187,0.0015178561],"category_scores_gemma":[0.0004891507,0.000109666595,0.00014362384,0.0020662232,0.00013046154,0.00016166028,0.00034297336,0.00021240904,0.00045537122],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027237786,0.00008459974,0.85100245,0.00021866147,0.00010282291,0.0014949613,0.0019343183,0.011887683,0.014578371,0.0005487925,0.004115828,0.113759145],"study_design_scores_gemma":[0.000010530697,0.000054662793,0.9739663,0.000019120145,0.0000288683,0.00030317245,0.0013686502,0.016353667,0.0025928514,0.0000806126,0.005204651,0.000016926833],"about_ca_topic_score_codex":0.035886947,"about_ca_topic_score_gemma":0.043110967,"teacher_disagreement_score":0.035886947,"about_ca_system_score_codex":0.00052461535,"about_ca_system_score_gemma":0.0005538622,"threshold_uncertainty_score":0.07135612},"labels":[],"label_agreement":null},{"id":"W1994824749","doi":"10.1029/2003jb002888","title":"Stresses in the subducting slab beneath southwest Japan and relation with plate geometry, tectonic forces, slab dehydration, and damaging earthquakes","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Slab; Geology; Seismology; Slab window; Mantle (geology); Subduction; Tectonics; Geophysics; Oceanic crust","score_opus":0.02534569658668482,"score_gpt":0.2703580672434697,"score_spread":0.2450123706567849,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994824749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99973255,0.00005079304,0.000054819382,0.0000085484035,4.552316e-7,7.118016e-7,0.000038919614,0.0000030569934,0.00011002427],"genre_scores_gemma":[0.99975497,0.00004904429,0.00009192999,0.000002698949,0.0000012230165,0.00000124082,0.00005413028,9.663377e-7,0.000043763193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994576,0.00000605449,0.000009215896,0.000013836706,0.0000110484925,0.000014028409],"domain_scores_gemma":[0.9997538,0.00001866652,0.00012036511,0.000015396949,0.000052226136,0.000039616265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012231155,0.00029907725,0.00022392861,0.00087012403,0.00028861276,0.00033833552,0.00018455037,0.00020170858,0.0006824076],"category_scores_gemma":[0.00045479453,0.00027696477,0.00020510172,0.0007621014,0.00035010735,0.00025923658,0.00041381564,0.00012969229,0.00009433533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007299043,0.000012104315,0.97122866,0.0000381683,0.000027792452,0.00016871201,0.00056300283,0.001427657,0.021603229,0.00005621736,0.000033239394,0.0047681876],"study_design_scores_gemma":[0.0000023070952,0.000015580774,0.99832815,0.0000028023346,0.000009624674,0.000054987035,0.00023013225,0.00073005044,0.0005139435,0.00004285822,0.00006619773,0.0000032740186],"about_ca_topic_score_codex":0.021802137,"about_ca_topic_score_gemma":0.027813403,"teacher_disagreement_score":0.021802137,"about_ca_system_score_codex":0.0004323934,"about_ca_system_score_gemma":0.00027363558,"threshold_uncertainty_score":0.04335046},"labels":[],"label_agreement":null},{"id":"W1995127694","doi":"10.1002/2014jc010385","title":"Hydro‐acoustic and tsunami waves generated by the 2012 <scp>H</scp>aida <scp>G</scp>waii earthquake: <scp>M</scp>odeling and in situ measurements","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Oceans","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministero dell’Istruzione, dell’Università e della Ricerca; National Oceanic and Atmospheric Administration; University of Victoria","keywords":"Compressibility; Geology; Seismology; Seabed; Gravitational wave; Acoustics; Physics; Mechanics; Oceanography","score_opus":0.07414016412423304,"score_gpt":0.2970128600149271,"score_spread":0.22287269589069408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995127694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99673754,0.000009214177,0.002489226,0.000013661247,0.000007725247,0.0000046683426,0.000099370016,0.000049258106,0.0005893408],"genre_scores_gemma":[0.99846137,0.00001427882,0.00108841,0.0000026163684,0.000003278868,0.0000042903466,0.00013289748,0.000005244705,0.00028758435],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995744,0.0000074416002,0.0000030892072,0.000010123037,0.0000114319155,0.00001042694],"domain_scores_gemma":[0.9999081,0.000017000531,0.000021661346,0.000016698476,0.000018505205,0.00001805009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000091286056,0.0003526322,0.000158329,0.00036375842,0.00018135153,0.00032822517,0.00027362566,0.000331496,0.00073719636],"category_scores_gemma":[0.00025306974,0.0002351116,0.0002991605,0.00028141815,0.000199449,0.00027884488,0.00021530673,0.00019193282,0.00012967645],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035448535,0.0004926672,0.17607711,0.00016871913,0.00015412239,0.00080151414,0.00032282664,0.653476,0.13444355,0.00097347196,0.0012297867,0.03150571],"study_design_scores_gemma":[0.000023744558,0.00006908811,0.072780855,0.000007649534,0.000028607088,0.00007238618,0.00008367328,0.9157099,0.010811498,0.00013298426,0.0002598692,0.000019726967],"about_ca_topic_score_codex":0.01145388,"about_ca_topic_score_gemma":0.0127091855,"teacher_disagreement_score":0.98854613,"about_ca_system_score_codex":0.00028229234,"about_ca_system_score_gemma":0.00032914046,"threshold_uncertainty_score":0.022774398},"labels":[],"label_agreement":null},{"id":"W1995307791","doi":"10.1038/nature13778","title":"Prevalence of viscoelastic relaxation after the 2011 Tohoku-oki earthquake","year":2014,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":310,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada; University of Victoria","funders":"","keywords":"Geology; Viscoelasticity; Seismology; Subduction; Geodetic datum; Earthquake rupture; Geodesy; Trench; Deformation (meteorology); Slip (aerodynamics); Rheology; Fault (geology); Tectonics","score_opus":0.005770468933232713,"score_gpt":0.20175788325764676,"score_spread":0.19598741432441405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995307791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995919,0.000054105094,0.000013253713,0.000034365486,0.0000032103949,0.000001261998,0.000049875904,0.0000011317981,0.00025080628],"genre_scores_gemma":[0.99955374,0.00011138019,0.000015855736,0.000020217847,0.000008341389,0.0000030374313,0.000117238844,0.0000010939352,0.00016908658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998222,0.000018183297,0.000026293297,0.0000427084,0.000022283952,0.00006831204],"domain_scores_gemma":[0.9983662,0.00018576167,0.0008888679,0.00008611953,0.00019108148,0.00028192252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000283389,0.00016683896,0.00018463715,0.0011889045,0.000646528,0.0006084275,0.0003422608,0.00064313953,0.0016419479],"category_scores_gemma":[0.0014385215,0.00018443304,0.00024241328,0.0009795107,0.00044874143,0.0006440857,0.0008911165,0.00048427982,0.00018293278],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011723733,0.000041698615,0.99215686,0.000035393343,0.000030186378,0.00026529038,0.001411508,0.000030398365,0.0017081928,0.000042015363,0.00015660733,0.004004631],"study_design_scores_gemma":[6.8948174e-7,0.000016445458,0.9985342,0.000006310002,0.0000073848614,0.000112236616,0.0011145222,0.00003165024,0.00004342709,0.0000057442867,0.00012485843,0.0000025255165],"about_ca_topic_score_codex":0.00663074,"about_ca_topic_score_gemma":0.016281584,"teacher_disagreement_score":0.00663074,"about_ca_system_score_codex":0.0003206738,"about_ca_system_score_gemma":0.00041598402,"threshold_uncertainty_score":0.013184309},"labels":[],"label_agreement":null},{"id":"W1996452030","doi":"10.1007/s11069-010-9637-z","title":"Aftershock sequences of two great Sumatran earthquakes of 2004 and 2005 and simulation of the minor tsunami generated on September 12, 2007 in the Indian Ocean and its effect","year":2010,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Aftershock; Seismology; Geology; Epicenter; Tsunami earthquake; Magnitude (astronomy); Tide gauge; Fault (geology); Amplitude; Indian ocean; Oceanography; Sea level","score_opus":0.008912542331276845,"score_gpt":0.24034112174778507,"score_spread":0.23142857941650824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996452030","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958593,0.000033236054,0.00017604406,0.00011130896,0.000033348388,0.000011245773,0.0024866757,0.00004488398,0.0012439772],"genre_scores_gemma":[0.994609,0.000047046422,0.0002968541,0.00002096153,0.0000083370305,0.00002064618,0.0041839965,0.000011776354,0.0008014506],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988925,0.000017386736,0.0000151817385,0.000022774238,0.000020476718,0.000034986515],"domain_scores_gemma":[0.99955946,0.000094703355,0.00008786924,0.000033388285,0.000119519595,0.000105150466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021746581,0.0004713561,0.00042193936,0.0009952727,0.00055091846,0.00063349,0.0006865256,0.0010723706,0.003488581],"category_scores_gemma":[0.0009280187,0.00039852882,0.00058977545,0.0012941752,0.00032448783,0.0003409248,0.00048202657,0.000771057,0.0003361566],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016723692,0.0007304229,0.21405187,0.00018847862,0.00056988397,0.002077353,0.00065369054,0.75466454,0.0049502673,0.002196651,0.008798348,0.009446076],"study_design_scores_gemma":[0.0002826763,0.00039758315,0.5709125,0.00004744993,0.00029337688,0.0002604597,0.0012796882,0.42020476,0.002238374,0.00068029686,0.003299653,0.000103174796],"about_ca_topic_score_codex":0.10178631,"about_ca_topic_score_gemma":0.124399625,"teacher_disagreement_score":0.10178631,"about_ca_system_score_codex":0.0012735211,"about_ca_system_score_gemma":0.0009782247,"threshold_uncertainty_score":0.20238769},"labels":[],"label_agreement":null},{"id":"W1996834935","doi":"10.1029/1999gl011070","title":"Can deglaciation trigger earthquakes in N. America?","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Deglaciation; Geology; Margin (machine learning); Glacial period; Seismology; Lithosphere; Instability; Magnitude (astronomy); Last Glacial Maximum; Fault (geology); Geomorphology; Tectonics","score_opus":0.030603843144565084,"score_gpt":0.27916720653163657,"score_spread":0.2485633633870715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996834935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784863,0.00013258585,0.00012845833,0.0002077744,0.0000068658496,0.0000025124045,0.00015794873,0.000013487704,0.0015016602],"genre_scores_gemma":[0.9995702,0.00009504177,0.00007046159,0.000017395203,0.0000035014948,0.0000014420255,0.00008739432,0.000002157622,0.00015235852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996805,0.000005644242,0.0000018089801,0.000010484427,0.0000027916678,0.000011323941],"domain_scores_gemma":[0.99984026,0.00003677901,0.000058130358,0.000009872859,0.000020631724,0.000034243738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012405963,0.00014756495,0.00010612282,0.0002150306,0.00022056134,0.00040966878,0.00016745686,0.0003246998,0.00086648617],"category_scores_gemma":[0.0008952445,0.0001384162,0.00014724562,0.0002666189,0.00023663887,0.00039080478,0.0003154709,0.00012141979,0.00010434141],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021964299,0.00003826857,0.9624546,0.00005371686,0.000053020456,0.0007078538,0.0006250343,0.016825274,0.0034767904,0.0010934359,0.0013124372,0.013139908],"study_design_scores_gemma":[0.000027112108,0.000048457867,0.96745515,0.000018019646,0.000038112066,0.00022658623,0.0007666892,0.027892046,0.0003935374,0.0013245023,0.001798062,0.000011709192],"about_ca_topic_score_codex":0.060443096,"about_ca_topic_score_gemma":0.10503234,"teacher_disagreement_score":0.9395569,"about_ca_system_score_codex":0.00060975086,"about_ca_system_score_gemma":0.00036839643,"threshold_uncertainty_score":0.120182574},"labels":[],"label_agreement":null},{"id":"W1997253465","doi":"10.1029/2008jb005901","title":"Can compliant fault zones be used to measure absolute stresses in the upper crust?","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Crust; Fault (geology); Slip (aerodynamics); Deformation (meteorology); Tectonics; Geophysics; Petrology","score_opus":0.08465556753930734,"score_gpt":0.3291818857254476,"score_spread":0.24452631818614026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997253465","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96996146,0.0020025114,0.023837097,0.00039702962,0.000058439357,0.000032315165,0.00036045926,0.00023472606,0.0031159841],"genre_scores_gemma":[0.9893937,0.00083207455,0.009220948,0.00012339074,0.000028030006,0.000018679491,0.00013875285,0.000020667323,0.00022359718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994246,0.00019465113,0.00005490461,0.00014191928,0.0001312261,0.000052796713],"domain_scores_gemma":[0.9981633,0.00038723825,0.00078094844,0.00035025104,0.00018534987,0.00013295261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016892136,0.00095378567,0.0006138014,0.0026413677,0.0002988666,0.0014719506,0.0009771646,0.0011036588,0.000541441],"category_scores_gemma":[0.0062381844,0.0005080066,0.00042591649,0.0022378776,0.0012994591,0.0017991448,0.00091257156,0.00046454548,0.00041496495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019167425,0.00007074067,0.7816724,0.00033380542,0.0004338921,0.00019083852,0.0009240713,0.009861353,0.06714671,0.00204922,0.00043667166,0.1366886],"study_design_scores_gemma":[0.000018223254,0.00026857344,0.9536538,0.0001034086,0.00007866896,0.00027044275,0.00089288,0.023561297,0.012252871,0.0066383807,0.002156488,0.000104895196],"about_ca_topic_score_codex":0.0042353547,"about_ca_topic_score_gemma":0.008608118,"teacher_disagreement_score":0.0042353547,"about_ca_system_score_codex":0.00035942107,"about_ca_system_score_gemma":0.00018579389,"threshold_uncertainty_score":0.008933485},"labels":[],"label_agreement":null},{"id":"W1997554288","doi":"10.1017/s0016756812000751","title":"History of faulting on the Doruneh Fault System: implications for the kinematic changes of the Central Iranian Microplate","year":2013,"lang":"en","type":"article","venue":"Geological Magazine","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Clockwise; Fault (geology); Paleontology; Seismology; Kinematics; Fold (higher-order function); Rotation (mathematics); Geometry","score_opus":0.035051918193407555,"score_gpt":0.20825782642081295,"score_spread":0.1732059082274054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997554288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994068,0.001489015,0.0005178968,0.00018224724,0.000020578802,0.0000084698895,0.00021412011,0.000022173248,0.0034774342],"genre_scores_gemma":[0.99907076,0.00041736703,0.00017277726,0.00001472713,0.000018442777,0.000002523685,0.000113839196,0.0000030779318,0.00018640334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998795,0.000014349658,0.000012126858,0.000042256313,0.000023551253,0.000028156452],"domain_scores_gemma":[0.9997271,0.000025603367,0.00011032627,0.000020563115,0.00008821633,0.00002817018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052912784,0.0003284452,0.0002482914,0.0021308265,0.000778195,0.0008793234,0.00037300857,0.00042880565,0.0023343007],"category_scores_gemma":[0.0006389889,0.00015132333,0.0002730768,0.001799089,0.00094706035,0.0007304689,0.00053727,0.00030856096,0.00028362256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002566492,0.000048604972,0.909495,0.00020426315,0.00014305387,0.0010740659,0.0028509998,0.003641968,0.0336017,0.0027032022,0.0003920981,0.04558852],"study_design_scores_gemma":[0.0000081881335,0.000054710952,0.99301636,0.000039326926,0.000037186328,0.0003780885,0.001075918,0.0011187713,0.0011764665,0.00051158667,0.002567852,0.000015520325],"about_ca_topic_score_codex":0.012293217,"about_ca_topic_score_gemma":0.0111655835,"teacher_disagreement_score":0.012293217,"about_ca_system_score_codex":0.0011146001,"about_ca_system_score_gemma":0.00051666267,"threshold_uncertainty_score":0.024443328},"labels":[],"label_agreement":null},{"id":"W1997614664","doi":"10.1016/j.jog.2015.01.002","title":"The influence of viscosity structure in the lithosphere on predictions from models of glacial isostatic adjustment","year":2015,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; University of Ottawa","keywords":"Post-glacial rebound; Geology; Lithosphere; Viscosity; Glacial period; Geophysics; Geodesy; Isostasy; Seismology; Geomorphology; Tectonics; Thermodynamics","score_opus":0.014542227597132014,"score_gpt":0.2218749548254553,"score_spread":0.2073327272283233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997614664","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98974293,0.0002538179,0.0033121055,0.0010791676,0.000090803456,0.000013107003,0.00029016013,0.00011532618,0.005102544],"genre_scores_gemma":[0.99916697,0.000073976254,0.00025876428,0.0000458018,0.000019024854,0.000004387521,0.000071642695,0.000035819074,0.0003235751],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996754,0.00015823865,0.000019209785,0.000059639617,0.00003249577,0.00005500335],"domain_scores_gemma":[0.9962991,0.0027346902,0.00023504112,0.00020082325,0.00027970766,0.00025069082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001409963,0.00093732047,0.0006778929,0.00060747523,0.0008924387,0.002533143,0.0011271171,0.0020666323,0.0014995764],"category_scores_gemma":[0.0104645025,0.00097123696,0.00082019344,0.0004962632,0.0012595268,0.0013236079,0.0008142138,0.0016365258,0.00037240918],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075648204,0.000024810157,0.0067233774,0.000008718209,0.000030119429,0.000038722897,0.000029763558,0.9909416,0.00029133915,0.00087290833,0.00020787003,0.00075511076],"study_design_scores_gemma":[0.000040260307,0.000022738963,0.0030077612,0.000004972183,0.000017029332,0.0000069760977,0.00002396213,0.9958311,0.00016196395,0.00080964295,0.000060539118,0.0000131067945],"about_ca_topic_score_codex":0.05123151,"about_ca_topic_score_gemma":0.018335683,"teacher_disagreement_score":0.05123151,"about_ca_system_score_codex":0.0016194037,"about_ca_system_score_gemma":0.00097586913,"threshold_uncertainty_score":0.1018666},"labels":[],"label_agreement":null},{"id":"W1997627183","doi":"10.1029/2004jb003590","title":"GPS crustal strain, postglacial rebound, and seismic hazard in eastern North America: The Saint Lawrence valley example","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Seismic hazard; Global Positioning System; Geodesy; Seismic moment; Deformation (meteorology); Strain rate; Magnitude (astronomy); Fault (geology); Oceanography","score_opus":0.04196263444334933,"score_gpt":0.28668254797499276,"score_spread":0.24471991353164343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997627183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979665,0.00010831437,0.000039981,0.000114083334,0.0000011941414,0.000002123544,0.0006310966,0.000007645047,0.0011289475],"genre_scores_gemma":[0.99849737,0.000074837626,0.000060884704,0.000015881815,0.0000020035172,0.0000023324515,0.00067574816,0.0000020373518,0.0006688608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999305,0.000011371717,0.00000362067,0.000014108292,0.000017201955,0.000023324483],"domain_scores_gemma":[0.9994267,0.000075156735,0.00012401961,0.000026216483,0.00023881094,0.000109140594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014617278,0.000118159856,0.00011371946,0.0005406152,0.00036458744,0.0004527349,0.00040611677,0.00021677025,0.0013456258],"category_scores_gemma":[0.0006117098,0.00008019033,0.00010249553,0.001217448,0.00025764998,0.00018506826,0.00027258022,0.00019138951,0.00014232704],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002838409,0.000020042402,0.9937075,0.0000090183585,0.000024813226,0.00010271397,0.00034511526,0.0004951295,0.00031984583,0.00009533242,0.0008397241,0.004012411],"study_design_scores_gemma":[0.000003036557,0.000006334193,0.9980794,0.0000038247845,0.0000060100037,0.000025843272,0.00034235534,0.00091835763,0.00002879511,0.000017723056,0.0005653323,0.000003135258],"about_ca_topic_score_codex":0.8918778,"about_ca_topic_score_gemma":0.9550884,"teacher_disagreement_score":0.8918778,"about_ca_system_score_codex":0.0026004086,"about_ca_system_score_gemma":0.0011030067,"threshold_uncertainty_score":0.21751791},"labels":[],"label_agreement":null},{"id":"W1997752552","doi":"10.1080/13632460601031631","title":"A Fast and Efficient Simulation of the Far-Fault and Near-Fault Earthquake Ground Motions Associated with the June 17 and 21, 2000, Earthquakes in South Iceland","year":2007,"lang":"en","type":"article","venue":"Journal of Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Windsor","keywords":"Seismology; Geology; Attenuation; Fault (geology); Seismic gap; Inversion (geology); Earthquake simulation; Physics; Tectonics","score_opus":0.008928181972976455,"score_gpt":0.197596258660078,"score_spread":0.18866807668710153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997752552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887737,0.000061898696,0.0060738567,0.00012277187,0.0000235256,0.00004780849,0.0005087651,0.00016778125,0.004219789],"genre_scores_gemma":[0.99366415,0.000050833347,0.0049773334,0.00002231308,0.00000730125,0.000041677813,0.0005401949,0.00002286663,0.0006733316],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991834,0.000024209561,0.000005194138,0.000012669868,0.000016878124,0.000022541917],"domain_scores_gemma":[0.99967206,0.00016626317,0.000037027636,0.000020800693,0.00005287227,0.000050927913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032324318,0.0005055115,0.0004407134,0.000283803,0.00038229208,0.0005186442,0.0006265793,0.0007298055,0.001192635],"category_scores_gemma":[0.000971697,0.0002688412,0.00037278642,0.0002861319,0.00041455316,0.00029079642,0.00039318763,0.0004152384,0.00011928423],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005155799,0.000040525796,0.0025922451,0.00001031625,0.000012005365,0.0000428702,0.000026977445,0.9951532,0.0004406678,0.0002707212,0.00011036485,0.0012485504],"study_design_scores_gemma":[0.000021973485,0.000026955518,0.0009620301,0.0000019709148,0.0000048451748,0.000005054138,0.000019219684,0.99859315,0.0002099359,0.000058796977,0.00009343038,0.000002508617],"about_ca_topic_score_codex":0.04788257,"about_ca_topic_score_gemma":0.037128355,"teacher_disagreement_score":0.04788257,"about_ca_system_score_codex":0.0007289786,"about_ca_system_score_gemma":0.00090598373,"threshold_uncertainty_score":0.09520769},"labels":[],"label_agreement":null},{"id":"W1998189975","doi":"10.1016/s0169-1368(00)00012-3","title":"Flat vein formation in a transitional crustal setting by self-induced fluid pressure equilibrium — an example from the Géant Dormant gold mine, Canada","year":2000,"lang":"en","type":"article","venue":"Ore Geology Reviews","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Mesothermal; Vein; Fluid dynamics; Petrology; Crust; Dike; Tectonics; Hydrothermal circulation; Geochemistry; Fluid inclusions; Seismology","score_opus":0.021327861029244548,"score_gpt":0.21043968973790556,"score_spread":0.189111828708661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998189975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9804915,0.000121742814,0.0005546519,0.00016660754,0.000005861974,0.000021638925,0.00007576332,0.000020123545,0.018542068],"genre_scores_gemma":[0.9968189,0.000074471536,0.00025041698,0.0000151764725,8.896116e-7,0.0000016596533,0.000028682736,0.000005702385,0.0028041988],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998667,0.000006504844,0.0000034435457,0.000023086208,0.000041845928,0.000058419337],"domain_scores_gemma":[0.9998801,0.0000071887816,0.00001102864,0.000013278021,0.000044199496,0.00004412083],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008411628,0.00013794437,0.00027372298,0.00067524315,0.0036400189,0.0019340679,0.00083522004,0.0006078891,0.0016043145],"category_scores_gemma":[0.00035257774,0.00019399032,0.00015065142,0.00078760664,0.0027544366,0.0002908039,0.0008510059,0.00049453345,0.00026625695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012699785,0.00041814096,0.42079145,0.0002641942,0.00016733767,0.02315365,0.018884119,0.022038242,0.3234363,0.09959126,0.0054239617,0.084561385],"study_design_scores_gemma":[0.00012655603,0.00032899625,0.9007444,0.000063549574,0.00005259263,0.0031357047,0.021182612,0.01517679,0.01573636,0.010011606,0.03332055,0.000120378274],"about_ca_topic_score_codex":0.7745937,"about_ca_topic_score_gemma":0.8806752,"teacher_disagreement_score":0.22540629,"about_ca_system_score_codex":0.0063658655,"about_ca_system_score_gemma":0.004580493,"threshold_uncertainty_score":0.4534675},"labels":[],"label_agreement":null},{"id":"W1998843681","doi":"10.1029/2008je003286","title":"Constraints on deep moonquake focal mechanisms through analyses of tidal stress","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismogram; Amplitude; Seismology; Shear (geology); Shear stress; Stress (linguistics); Geodesy; Geophysics; Mechanics; Petrology; Physics","score_opus":0.07585039786671326,"score_gpt":0.35826971123713175,"score_spread":0.2824193133704185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998843681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99730325,0.00004958364,0.002058698,0.000014427281,0.000001093141,0.000004184575,0.0001398206,0.000026667753,0.0004023346],"genre_scores_gemma":[0.9988657,0.000023950102,0.00079920137,0.0000038580365,0.0000015335645,0.000002776744,0.00021441511,0.0000084954345,0.000080106474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982125,0.000041113577,0.000017960507,0.000047101446,0.000023445658,0.00004903103],"domain_scores_gemma":[0.99794966,0.0008707263,0.0004329119,0.00024502224,0.00021211017,0.0002895461],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048980553,0.00042618916,0.0005213728,0.0011198225,0.00032659018,0.0007963045,0.0003490743,0.0003058171,0.0015296857],"category_scores_gemma":[0.0028149812,0.00023492092,0.00043725417,0.001060258,0.00027262,0.00066607044,0.000905318,0.00029120565,0.00025447962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012507975,0.00002393994,0.9688663,0.000036166544,0.000076171294,0.00013093538,0.00023799045,0.009400716,0.011841749,0.00033508593,0.00011427884,0.00881168],"study_design_scores_gemma":[0.0000078468665,0.00005333407,0.96255654,0.000010442726,0.000030768435,0.00009893016,0.00036536486,0.035104,0.00094014755,0.00054554094,0.00027257827,0.000014547597],"about_ca_topic_score_codex":0.007014758,"about_ca_topic_score_gemma":0.0149035,"teacher_disagreement_score":0.007014758,"about_ca_system_score_codex":0.00021032663,"about_ca_system_score_gemma":0.00033269753,"threshold_uncertainty_score":0.0139478445},"labels":[],"label_agreement":null},{"id":"W1999211958","doi":"10.1073/pnas.1412299111","title":"Earthquake and tsunami forecasts: Relation of slow slip events to subsequent earthquake rupture","year":2014,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Seismology; Geology; Subduction; Interplate earthquake; Slip (aerodynamics); Seismic hazard; Intraplate earthquake; Earthquake magnitude; Slow earthquake; Magnitude (astronomy); Earthquake rupture; Seismic gap; Episodic tremor and slip; Seismic microzonation; Peak ground acceleration; Submarine pipeline; Earthquake prediction; Foreshock; Aftershock; Induced seismicity; Tectonics; Ground motion; Geotechnical engineering; Fault (geology)","score_opus":0.030441078738570927,"score_gpt":0.2544213591288244,"score_spread":0.22398028039025347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999211958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99709034,0.00017405952,0.00033832932,0.00016943758,0.000008116848,0.000008655854,0.0012980469,0.000032837957,0.00088020467],"genre_scores_gemma":[0.9987531,0.00007989443,0.0000936459,0.000009491449,0.000009157168,0.0000017140627,0.00092745613,0.0000023285588,0.00012318327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997067,0.00008132581,0.000042153384,0.000064968066,0.0000667495,0.000038086986],"domain_scores_gemma":[0.9893764,0.0052807913,0.003092336,0.00046347256,0.001060921,0.0007261244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012674967,0.00024086254,0.00016865147,0.0013099948,0.00013912877,0.00062396727,0.00025232768,0.0004997165,0.0015204613],"category_scores_gemma":[0.015354272,0.00014417089,0.00018966694,0.0007114276,0.00012425106,0.0006364502,0.00046484027,0.00045057925,0.00053530966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000094216375,0.000020237294,0.9903424,0.000007592808,0.000023045994,0.000056822533,0.00003363222,0.004796821,0.00009001015,0.00004295994,0.00024615656,0.0042460347],"study_design_scores_gemma":[0.00000941928,0.00007372644,0.9635287,0.000011297791,0.000013841366,0.00008637714,0.00015831724,0.03540782,0.00015836467,0.00015379956,0.0003889628,0.000009504299],"about_ca_topic_score_codex":0.019197768,"about_ca_topic_score_gemma":0.018745592,"teacher_disagreement_score":0.019197768,"about_ca_system_score_codex":0.00032491688,"about_ca_system_score_gemma":0.00029981494,"threshold_uncertainty_score":0.038172066},"labels":[],"label_agreement":null},{"id":"W1999304749","doi":"10.1080/00288306.2004.9515060","title":"Surface rupture of the Poulter Fault in the 1929 March 9 Arthur's Pass earthquake, and redefinition of the Kakapo Fault, New Zealand","year":2004,"lang":"en","type":"article","venue":"New Zealand Journal of Geology and Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Memorial University of Newfoundland","keywords":"Sinistral and dextral; Geology; Fault (geology); Seismology; Fault scarp; Active fault; Strike-slip tectonics; Tectonics; Transform fault","score_opus":0.012955358477717345,"score_gpt":0.21745896305200554,"score_spread":0.2045036045742882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999304749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986803,0.000041746993,0.000012664226,0.000051901934,0.0000025098027,0.000004718688,0.00009102456,0.0000016347944,0.0011134989],"genre_scores_gemma":[0.999411,0.00005909156,0.000019810774,0.0000069730436,0.0000025119575,0.000002526582,0.00008919939,6.905512e-7,0.00040822686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999051,0.0000072674,0.000006829891,0.000019630834,0.000030673793,0.000030607083],"domain_scores_gemma":[0.99976546,0.000021115666,0.00010146138,0.000011389255,0.00005339989,0.000047259084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000119850076,0.000141684,0.00014245725,0.0005365658,0.00063323224,0.0005583283,0.00018537875,0.00036393027,0.0016979729],"category_scores_gemma":[0.00088119926,0.00015204883,0.00010188688,0.00053591456,0.00083613454,0.00038307134,0.00053274014,0.00029152675,0.00016651061],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004660235,0.000066132765,0.94653076,0.00009930648,0.000040324918,0.0047308616,0.0065737,0.00055070996,0.017647235,0.0003729486,0.0012829386,0.021639025],"study_design_scores_gemma":[0.0000035224905,0.000024305233,0.9986172,0.00000430194,0.00000250367,0.00011980249,0.00069731055,0.000049678758,0.00008825902,0.000015782794,0.0003750103,0.0000023364296],"about_ca_topic_score_codex":0.25275153,"about_ca_topic_score_gemma":0.4490676,"teacher_disagreement_score":0.25275153,"about_ca_system_score_codex":0.0015157263,"about_ca_system_score_gemma":0.0006169851,"threshold_uncertainty_score":0.50256073},"labels":[],"label_agreement":null},{"id":"W1999927320","doi":"10.5194/npg-20-143-2013","title":"A tri-stage cluster identification model for accurate analysis of seismic catalogs","year":2013,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Institute for Catastrophic Loss Reduction","keywords":"Aftershock; Induced seismicity; Magnitude (astronomy); Identification (biology); Seismology; Cluster (spacecraft); Geology; Event (particle physics); Data mining; Ideal (ethics); Stage (stratigraphy); Computer science; Algorithm; Physics","score_opus":0.027094380551403018,"score_gpt":0.26543645100835644,"score_spread":0.23834207045695344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999927320","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00954302,0.000059228703,0.98928225,0.000076979704,0.000015877904,0.00004864295,0.00006099256,0.00031494835,0.00059807464],"genre_scores_gemma":[0.53371,0.00025245134,0.45673093,0.00014599787,0.000059502403,0.00059987704,0.0005821365,0.00019796925,0.0077210967],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991899,0.00019993297,0.000049047107,0.00025900308,0.00021013767,0.000091951755],"domain_scores_gemma":[0.9983333,0.00059018296,0.0002069944,0.0001655712,0.00063587766,0.0000681434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022280323,0.0005965633,0.00081763585,0.001165783,0.0006588205,0.0010251275,0.0025677423,0.0010441437,0.0023938275],"category_scores_gemma":[0.0042259595,0.0007048183,0.0009054642,0.0011545572,0.00073031615,0.0018571243,0.0011746465,0.0012048044,0.0010597],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013692121,0.00007692092,0.0032953764,0.00007398344,0.00008146022,0.000053672684,0.0001873786,0.89853394,0.0025281617,0.011694886,0.0013848956,0.081952415],"study_design_scores_gemma":[0.0000023628247,0.000009804046,0.00016665854,0.0000019072213,0.0000032927157,0.0000068049185,0.000004780221,0.9983406,0.00020461205,0.0010602558,0.00019429915,0.0000046130003],"about_ca_topic_score_codex":0.018936183,"about_ca_topic_score_gemma":0.01774736,"teacher_disagreement_score":0.018936183,"about_ca_system_score_codex":0.0013712099,"about_ca_system_score_gemma":0.0017492883,"threshold_uncertainty_score":0.037651956},"labels":[],"label_agreement":null},{"id":"W1999964904","doi":"10.1016/j.epsl.2011.04.017","title":"Evidence for episodic aseismic slip across the subduction seismogenic zone off Costa Rica: CORK borehole pressure observations at the subduction prism toe","year":2011,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Episodic tremor and slip; Seismology; Slip (aerodynamics); Plate tectonics; Accretionary wedge; Tectonics","score_opus":0.07083699727498691,"score_gpt":0.2402372105562873,"score_spread":0.1694002132813004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999964904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99810386,0.00008200418,0.0000370056,0.00005527797,0.0000015995714,0.0000044754725,0.00031018708,0.000005126415,0.0014005902],"genre_scores_gemma":[0.9996215,0.000055952256,0.000050517952,0.0000150135575,0.000002675097,0.0000025545485,0.00015283962,0.0000017901664,0.00009706215],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999882,0.000017148199,0.0000123949485,0.000027961929,0.00002226623,0.00003817116],"domain_scores_gemma":[0.9993081,0.000085713116,0.0002632504,0.000086705775,0.00017392325,0.00008231465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026507812,0.00016722949,0.00015131135,0.000686141,0.00044821601,0.0005897271,0.00042290118,0.00040249366,0.0006562809],"category_scores_gemma":[0.0011366875,0.0001909189,0.00011679498,0.0011717677,0.0005191143,0.00031009509,0.00068421016,0.00022221265,0.0001554665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011302679,0.000029380522,0.98166156,0.00003706467,0.000041809464,0.00020018997,0.0015089301,0.00023773532,0.011243556,0.00011957298,0.00026406787,0.0045431554],"study_design_scores_gemma":[0.0000019281342,0.0000041154085,0.99942964,0.0000028512368,0.0000033488586,0.000025487236,0.00023497314,0.0000628812,0.00009143587,0.000005321683,0.00013680058,0.0000011631081],"about_ca_topic_score_codex":0.15266949,"about_ca_topic_score_gemma":0.21440418,"teacher_disagreement_score":0.15266949,"about_ca_system_score_codex":0.00077889685,"about_ca_system_score_gemma":0.00069336226,"threshold_uncertainty_score":0.3035617},"labels":[],"label_agreement":null},{"id":"W2000114370","doi":"10.1785/0220120102","title":"EqHaz: An Open-Source Probabilistic Seismic-Hazard Code Based on the Monte Carlo Simulation Approach","year":2013,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Citation; Computer science; Library science","score_opus":0.1347924390787833,"score_gpt":0.3245867907636173,"score_spread":0.189794351684834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000114370","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008245932,0.00046622477,0.7678956,0.000626657,0.0002993983,0.00047394354,0.016739909,0.15088816,0.054364305],"genre_scores_gemma":[0.15693045,0.001349522,0.68273264,0.0005490071,0.00021330477,0.002026866,0.029880377,0.06459569,0.0617221],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99942553,0.00011465376,0.00005230423,0.00006322453,0.00028940407,0.000054938235],"domain_scores_gemma":[0.9967849,0.002002445,0.00016331427,0.0002458875,0.00068982603,0.000113711394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014820604,0.0009473626,0.0006421767,0.001374574,0.00059314055,0.0014761954,0.003277067,0.0017678678,0.07765041],"category_scores_gemma":[0.009425438,0.0009503714,0.0011482517,0.0012272478,0.0005758829,0.0023838095,0.0021415194,0.0015751835,0.020560017],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038150314,0.00022067301,0.0054806,0.0011260598,0.00018198954,0.00041232767,0.00043240632,0.5025883,0.003382072,0.048148524,0.24710836,0.19053735],"study_design_scores_gemma":[0.00022564027,0.000041029023,0.0010272485,0.00016703314,0.000036502064,0.00018721334,0.00005063587,0.7981138,0.0032246448,0.026449677,0.17037287,0.000103725404],"about_ca_topic_score_codex":0.011397716,"about_ca_topic_score_gemma":0.013191489,"teacher_disagreement_score":0.07765041,"about_ca_system_score_codex":0.0010106296,"about_ca_system_score_gemma":0.0025490872,"threshold_uncertainty_score":0.25976652},"labels":[],"label_agreement":null},{"id":"W2000989137","doi":"10.1007/s00024-006-0169-0","title":"Numerical Simulations of Tsunami Waves and Currents for Southern Vancouver Island from a Cascadia Megathrust Earthquake","year":2007,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Fisheries and Oceans Canada","funders":"Division of Ocean Sciences; Fisheries and Oceans Canada","keywords":"Geology; Seismology; Subduction; Tsunami wave; Tsunami earthquake; West coast; Earthquake rupture; Oceanography; Tectonics","score_opus":0.01061580487471529,"score_gpt":0.21553462572267776,"score_spread":0.20491882084796248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000989137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99506277,0.000040566156,0.00020646804,0.00019969702,0.00001944313,0.000013438405,0.00036830892,0.00004005506,0.0040492676],"genre_scores_gemma":[0.99751306,0.000045915942,0.00028872993,0.000026829188,0.0000056237677,0.0000126955065,0.00037720634,0.000012584821,0.0017174397],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988544,0.000018065592,0.000008443022,0.000016382297,0.000024238703,0.000047458794],"domain_scores_gemma":[0.99915004,0.00026855117,0.00006209118,0.000040486742,0.00022848182,0.00025041634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024247292,0.00059062004,0.00054433645,0.0008098083,0.0017264213,0.0013764919,0.0014584368,0.0022844935,0.004651594],"category_scores_gemma":[0.0019187067,0.0007795298,0.0006670608,0.0010652939,0.0010809704,0.00045261285,0.0008034494,0.0012480192,0.0003114206],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028470435,0.00019413928,0.02557225,0.000032332362,0.000077901044,0.0005244546,0.00019018812,0.9679202,0.0011523381,0.00077106414,0.0012856298,0.0019949106],"study_design_scores_gemma":[0.00012445457,0.00006967706,0.017146124,0.000011019467,0.0000349713,0.000028744862,0.00041306103,0.9811866,0.00029054825,0.00023799951,0.00043117482,0.000025639949],"about_ca_topic_score_codex":0.7503012,"about_ca_topic_score_gemma":0.7071703,"teacher_disagreement_score":0.24969882,"about_ca_system_score_codex":0.0050560026,"about_ca_system_score_gemma":0.0040957415,"threshold_uncertainty_score":0.50233865},"labels":[],"label_agreement":null},{"id":"W2001293412","doi":"10.1186/bf03352816","title":"Geohazard assessment from satellite magnetic data modeling—with examples from the Arctic Margin along the Canada Basin and the Korean Peninsula along 40°N (latitude) parallel","year":2008,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Sejong University","keywords":"Geology; Peninsula; Magnetic anomaly; Anomaly (physics); Latitude; Basin and Range Province; Tectonics; Seismology; Crust; Altitude (triangle); Structural basin; Paleontology; Geodesy; Geography","score_opus":0.028965781066649442,"score_gpt":0.20513131239416577,"score_spread":0.17616553132751633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001293412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960174,0.000066582055,0.001583743,0.000103156475,0.0000033390836,0.000022626544,0.00046602986,0.00009742192,0.0016397815],"genre_scores_gemma":[0.9961391,0.0000599607,0.002658944,0.0000074384243,0.0000018391471,0.0000060777265,0.0005788429,0.000015436528,0.0005323678],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997937,0.000057609002,0.0000105536665,0.00004083396,0.00006614934,0.00003112774],"domain_scores_gemma":[0.99909985,0.00028234607,0.00009004653,0.00006632261,0.00040464694,0.00005690494],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063302345,0.00043247192,0.00024182831,0.0010500776,0.00043709605,0.0009367419,0.000406892,0.00034845158,0.00047582234],"category_scores_gemma":[0.0018421868,0.0002100657,0.0003137211,0.0010127404,0.0002541976,0.00028239354,0.00030793267,0.00018606016,0.00007452829],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026826083,0.00012961907,0.35321322,0.00006250736,0.00017797758,0.0003922739,0.00038216065,0.6065562,0.0024705995,0.00096619,0.0013659004,0.03401512],"study_design_scores_gemma":[0.000025636446,0.00003549861,0.10240795,0.000013670203,0.00004812425,0.00004514823,0.000428057,0.8938235,0.0013912034,0.00017136704,0.0015936692,0.000016119728],"about_ca_topic_score_codex":0.6703506,"about_ca_topic_score_gemma":0.7214799,"teacher_disagreement_score":0.3296494,"about_ca_system_score_codex":0.0023845194,"about_ca_system_score_gemma":0.0015399212,"threshold_uncertainty_score":0.66318154},"labels":[],"label_agreement":null},{"id":"W2001537735","doi":"10.1016/j.gexplo.2005.11.021","title":"Modeling of fluid pressure evolution related to sediment loading and thrust faulting in the Lanping basin: Implications for the formation of the Jinding Zn–Pb deposit, Yunnan, China","year":2006,"lang":"en","type":"article","venue":"Journal of Geochemical Exploration","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"Natural Sciences and Engineering Research Council of Canada; University of Illinois at Urbana-Champaign","keywords":"Geology; Structural basin; Geochemistry; Sedimentary rock; Hydrostatic pressure; Mantle (geology); Cretaceous; Cenozoic; Geomorphology; Paleontology","score_opus":0.019856175815473887,"score_gpt":0.2350400806349533,"score_spread":0.2151839048194794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001537735","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99724567,0.000055936667,0.0011390743,0.0002104828,0.000012269761,0.000013918679,0.00013292872,0.000049201735,0.0011406015],"genre_scores_gemma":[0.9991252,0.00004079101,0.00040547247,0.000013982998,0.000006219421,0.000008903957,0.00007479618,0.000010790467,0.00031394445],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989796,0.000022306353,0.000009603747,0.00003001974,0.000011538738,0.00002846039],"domain_scores_gemma":[0.9996947,0.00012221337,0.00004187122,0.000018405817,0.00005547596,0.000067360044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035940736,0.0006741597,0.00070158776,0.0006126764,0.0009924893,0.0012537953,0.0014771242,0.0019920478,0.001405733],"category_scores_gemma":[0.0011944518,0.0008470002,0.0007189051,0.0006725143,0.0010971951,0.0009133984,0.00076349557,0.0007102848,0.00010487488],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008483555,0.000070273614,0.01702357,0.00001639285,0.000032659394,0.00015050969,0.000056977082,0.97967875,0.0014180135,0.0003903299,0.000103319864,0.00097426807],"study_design_scores_gemma":[0.000025451764,0.000012162122,0.0025082945,0.0000013254205,0.000008089629,0.0000058474047,0.000031226085,0.99717194,0.0001329033,0.000056071713,0.000040673276,0.000006016749],"about_ca_topic_score_codex":0.20325992,"about_ca_topic_score_gemma":0.065742604,"teacher_disagreement_score":0.20325992,"about_ca_system_score_codex":0.0019945675,"about_ca_system_score_gemma":0.0031275726,"threshold_uncertainty_score":0.40415365},"labels":[],"label_agreement":null},{"id":"W2001787672","doi":"10.1190/segam2014-1494.1","title":"Analysis of the Crooked Lake sequence near Fox Creek, Alberta: Comparison of a waveform correlation detection method to a traditional STA/LTA picker","year":2014,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magnitude (astronomy); Geology; Waveform; Induced seismicity; Sequence (biology); Seismology; Correlation; Algorithm; Mathematics; Computer science; Geometry; Physics; Telecommunications; Biology","score_opus":0.04425509288622832,"score_gpt":0.27248771560898594,"score_spread":0.22823262272275763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001787672","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891523,0.00011281614,0.005430297,0.000040761686,0.000010134395,0.00005646865,0.0010855871,0.00020625965,0.0039052805],"genre_scores_gemma":[0.97968286,0.00012764902,0.014308438,0.000025665286,0.000012191772,0.000025065587,0.003029226,0.00006904903,0.0027198622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997002,0.000016588954,0.000016690099,0.000042746182,0.00017589409,0.00004791922],"domain_scores_gemma":[0.99911135,0.00009513785,0.00010865746,0.00004647202,0.000544458,0.00009396116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042654705,0.00026352383,0.00020048201,0.0027967189,0.0004979,0.000652393,0.000434031,0.00020100204,0.0016868856],"category_scores_gemma":[0.0013104285,0.00016868266,0.0001651229,0.0022942864,0.00022708125,0.00017908824,0.00042138144,0.0001346634,0.00044982758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005273852,0.00013796595,0.72000754,0.00016936698,0.00013514025,0.0007274502,0.00081790856,0.010828788,0.07742068,0.0003179501,0.0023306047,0.18657923],"study_design_scores_gemma":[0.000013554313,0.000039474035,0.9802949,0.000008431079,0.000024384482,0.00013501888,0.0002772596,0.014826209,0.0034034085,0.00001890082,0.0009446833,0.000013783686],"about_ca_topic_score_codex":0.42091134,"about_ca_topic_score_gemma":0.69334275,"teacher_disagreement_score":0.5790887,"about_ca_system_score_codex":0.0013062553,"about_ca_system_score_gemma":0.00179959,"threshold_uncertainty_score":0.83692276},"labels":[],"label_agreement":null},{"id":"W2002074664","doi":"10.1029/2000jb900060","title":"Full interseismic locking of the Nankai and Japan‐west Kurile subduction zones: An analysis of uniform elastic strain accumulation in Japan constrained by permanent GPS","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":201,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Geology; Seismology; Trench; Plate tectonics; Forearc; Tectonics","score_opus":0.030860951966786558,"score_gpt":0.2993813788483328,"score_spread":0.26852042688154626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002074664","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99977046,0.000033200515,0.000090588095,0.0000035369565,2.5015382e-7,9.135171e-7,0.00003772865,0.0000020831299,0.00006127896],"genre_scores_gemma":[0.9997009,0.00002168234,0.00007427636,0.0000018634274,9.2354173e-7,0.00000205539,0.00016897765,0.000002707292,0.000026544332],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998012,0.000027337808,0.000023280534,0.00007266212,0.000024692728,0.00005088133],"domain_scores_gemma":[0.9991848,0.0001911583,0.00028152094,0.000084661435,0.00010731694,0.00015065023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051513384,0.00042032334,0.0004937384,0.00122675,0.00030674014,0.00063200825,0.0004827623,0.00022776799,0.00050941866],"category_scores_gemma":[0.0016564408,0.0004278814,0.0005656551,0.0012010919,0.00046169828,0.00040209654,0.00070112926,0.00016958012,0.00010391811],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020616519,0.000035255838,0.9810688,0.000022162287,0.0001929435,0.00026640957,0.00030880896,0.0076380423,0.005695702,0.00010608963,0.000048332437,0.004411303],"study_design_scores_gemma":[0.000006738458,0.00001945326,0.98727125,0.0000027454391,0.00003946718,0.000055366047,0.00013015668,0.012200959,0.0001879906,0.000029601386,0.000049148573,0.000007085725],"about_ca_topic_score_codex":0.023451123,"about_ca_topic_score_gemma":0.02401231,"teacher_disagreement_score":0.023451123,"about_ca_system_score_codex":0.00043973836,"about_ca_system_score_gemma":0.00035762155,"threshold_uncertainty_score":0.04662925},"labels":[],"label_agreement":null},{"id":"W2002322523","doi":"10.2118/102098-ms","title":"Fault Leakage Potential Analysis in the Cantarell Field, Mexico, Using Geomechanics","year":2006,"lang":"en","type":"article","venue":"SPE Annual Technical Conference and Exhibition","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Geomechanics; Geology; Pore water pressure; Wireline; Petroleum engineering; Geotechnical engineering; Permeability (electromagnetism); Fault (geology); Oil shale; Caprock; Petrology; Stress field; Seismology; Engineering","score_opus":0.017661023785643427,"score_gpt":0.23778726417975976,"score_spread":0.22012624039411632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002322523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988588,0.000046013425,0.00024681631,0.000022527569,8.807039e-7,0.000008581264,0.00038922462,0.000020037656,0.00040705322],"genre_scores_gemma":[0.99898225,0.000041233052,0.00030324946,0.0000028046868,0.0000010649717,0.000008237092,0.0004716639,0.0000014791464,0.00018800674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993086,0.000008030848,0.0000056985173,0.00002205086,0.000014236331,0.00001911224],"domain_scores_gemma":[0.99973756,0.000040710154,0.00011435186,0.00001443955,0.0000723901,0.000020482381],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019178081,0.00025561472,0.0001651996,0.0016232244,0.00043799987,0.00048762374,0.00028618018,0.00031999368,0.00079637277],"category_scores_gemma":[0.00038493573,0.00013245788,0.00020544308,0.0011900403,0.00022715768,0.00036627866,0.00028020324,0.00013479135,0.000069123416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027380476,0.00009984487,0.93004274,0.00007438715,0.000058687376,0.0005484581,0.00031197642,0.040176384,0.0056530866,0.0002750812,0.00042548077,0.022060068],"study_design_scores_gemma":[0.000017950484,0.000051770687,0.9631199,0.000014929606,0.000021783773,0.000033572273,0.00041144082,0.035171364,0.00072816666,0.00006421967,0.00035608932,0.00000880448],"about_ca_topic_score_codex":0.20139106,"about_ca_topic_score_gemma":0.28771153,"teacher_disagreement_score":0.20139106,"about_ca_system_score_codex":0.0017336286,"about_ca_system_score_gemma":0.00074879575,"threshold_uncertainty_score":0.40043765},"labels":[],"label_agreement":null},{"id":"W2002678855","doi":"10.1029/2006gl027166","title":"Tomographic evidence for the Eurasian lithosphere subducting beneath south Taiwan","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Geology; Lithosphere; Eurasian Plate; Seismology; Plate tectonics; Collision zone; Seismic tomography; Crust; Convergent boundary; Slab window; Oceanic crust; Tectonics; Geophysics; Mantle (geology)","score_opus":0.0846416965720218,"score_gpt":0.3179592711327981,"score_spread":0.2333175745607763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002678855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998021,0.00008604863,0.00031602243,0.000055938584,0.0000015206494,0.000004159277,0.00012483544,0.000016626287,0.001373831],"genre_scores_gemma":[0.9989785,0.00007455029,0.0005380928,0.00000794467,0.0000025389954,0.0000027056735,0.00019374234,0.000002970306,0.00019906466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99998236,0.0000015477173,0.0000019989486,0.0000059118156,0.000003984554,0.000004163549],"domain_scores_gemma":[0.9998809,0.000017153627,0.000043694054,0.000015118416,0.000022720811,0.000020298916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005153369,0.00012146507,0.00007489242,0.0004981682,0.00015011655,0.0002961561,0.00016064031,0.00017847591,0.0011668119],"category_scores_gemma":[0.00021226775,0.00015267848,0.00009862598,0.00047781033,0.00018307377,0.00017546244,0.00027735558,0.00015709002,0.00013162513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030987474,0.000039591214,0.767632,0.00016379816,0.000071018854,0.0030010054,0.0016343686,0.0031495078,0.19404538,0.00069371524,0.00061238545,0.028647402],"study_design_scores_gemma":[0.000028349454,0.000036303096,0.9873338,0.000029348217,0.000052599768,0.0012601644,0.0006097274,0.00496718,0.004147435,0.00021359522,0.001312197,0.0000093783665],"about_ca_topic_score_codex":0.00758639,"about_ca_topic_score_gemma":0.010919752,"teacher_disagreement_score":0.00758639,"about_ca_system_score_codex":0.0001512068,"about_ca_system_score_gemma":0.00025372664,"threshold_uncertainty_score":0.0150844455},"labels":[],"label_agreement":null},{"id":"W2003598009","doi":"10.2113/gssgfbull.182.5.437","title":"Tectonic control of the Meteora conglomeratic formations (Mesohellenic basin, Greece)","year":2011,"lang":"en","type":"article","venue":"Bulletin de la Société Géologique de France","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Anticline; Sedimentary depositional environment; Paleontology; Structural basin; Marl; Tectonics; Stratigraphy; Subduction; Geomorphology","score_opus":0.010459194547132325,"score_gpt":0.2107733292248255,"score_spread":0.20031413467769318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003598009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99496293,0.00020223294,0.000083243394,0.000040833304,0.000001593852,0.000005177035,0.00015539165,0.00000774319,0.004540986],"genre_scores_gemma":[0.9995401,0.000050328417,0.000037679725,0.0000034282511,0.0000010440052,9.645345e-7,0.00005852548,0.0000011824984,0.00030681683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999112,0.000015813981,0.0000070151896,0.00003399781,0.000015773523,0.000016269822],"domain_scores_gemma":[0.99988556,0.000009506219,0.000053162694,0.000014665166,0.000019322828,0.000017766324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012060121,0.00010763154,0.000118168406,0.0008683235,0.00017468036,0.00058585504,0.0001351825,0.00012595969,0.0012036591],"category_scores_gemma":[0.00029258095,0.000090595,0.00009056563,0.00072221225,0.00051473407,0.00015503899,0.0005119462,0.00008914959,0.00016405073],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018141587,0.000035070905,0.9019767,0.00011863055,0.00013429187,0.0012803227,0.0023896515,0.0049861856,0.030557169,0.006055411,0.0004541978,0.05183102],"study_design_scores_gemma":[0.0000035929045,0.000013756392,0.997652,0.0000070937963,0.0000043903965,0.00015467266,0.00017294637,0.00026028394,0.00027540798,0.00010605718,0.0013478193,0.0000019495276],"about_ca_topic_score_codex":0.013479716,"about_ca_topic_score_gemma":0.019759536,"teacher_disagreement_score":0.013479716,"about_ca_system_score_codex":0.00072713307,"about_ca_system_score_gemma":0.00033900933,"threshold_uncertainty_score":0.02680248},"labels":[],"label_agreement":null},{"id":"W2003605905","doi":"10.1130/g31856.1","title":"Do subducting seamounts generate or stop large earthquakes?","year":2011,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":382,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Citation; Geological survey; Geology; Library science; Seamount; Archaeology; Geochemistry; Geography; Computer science; Paleontology","score_opus":0.05885092343159948,"score_gpt":0.2406068785052005,"score_spread":0.181755955073601,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003605905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.80521303,0.009335736,0.0006034951,0.027049461,0.0013771838,0.000051267252,0.005473025,0.00008244668,0.15081446],"genre_scores_gemma":[0.96975267,0.0074644056,0.00027102252,0.00069003465,0.0004676028,0.0000112037,0.0025995558,0.000028807295,0.01871473],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998963,0.000012723725,0.000011926531,0.000021240952,0.000031062067,0.000026703197],"domain_scores_gemma":[0.9994031,0.00012419019,0.00021150017,0.000027054519,0.00016075972,0.00007343416],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003643967,0.0001233867,0.00020870153,0.00046578393,0.00039912027,0.0011918055,0.00024748995,0.0004981616,0.009567503],"category_scores_gemma":[0.0026814193,0.00012333975,0.00014316659,0.0010018498,0.00040201625,0.0008701481,0.00040803262,0.00035491935,0.0015527561],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045534273,0.00008632539,0.591406,0.0007828226,0.00023130882,0.00074226334,0.0076918746,0.000832416,0.0018119547,0.009949219,0.18121013,0.20480035],"study_design_scores_gemma":[0.00003491043,0.00009262522,0.8793189,0.00029207356,0.000098030185,0.00019516466,0.009986338,0.00044577796,0.0005034762,0.0033455752,0.10566082,0.000026273436],"about_ca_topic_score_codex":0.021957027,"about_ca_topic_score_gemma":0.061923403,"teacher_disagreement_score":0.021957027,"about_ca_system_score_codex":0.0007065705,"about_ca_system_score_gemma":0.0007844364,"threshold_uncertainty_score":0.043658495},"labels":[],"label_agreement":null},{"id":"W2005109537","doi":"10.1007/s10706-005-1148-4","title":"Seismic Hazards Assessment for Radioactive Waste Disposal Sites in Regions of Low Seismic Activity","year":2006,"lang":"en","type":"article","venue":"Geotechnical and Geological Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Induced seismicity; Seismology; Hydrogeology; Geology; Tectonics; Radioactive waste; Seismic hazard; Magnitude (astronomy); Hazard; Term (time); Geotechnical engineering; Engineering","score_opus":0.009864367836136055,"score_gpt":0.21410713498625394,"score_spread":0.20424276715011788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005109537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99845636,0.000020797737,0.0008294644,0.000015711177,8.2172676e-7,0.0000123911195,0.00012056988,0.000013072437,0.000530716],"genre_scores_gemma":[0.9989598,0.000016496837,0.00057361973,0.0000027739086,0.000001014415,0.00000508315,0.00012321559,0.0000017339682,0.00031614598],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998103,0.00006755808,0.000013268917,0.000012317375,0.00005707339,0.000039571187],"domain_scores_gemma":[0.9990482,0.0002910554,0.00025419856,0.000032737582,0.00026296847,0.00011087006],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007508901,0.00031481622,0.00029464092,0.0020465828,0.00038531647,0.00045026556,0.00041108773,0.0004150793,0.0014892337],"category_scores_gemma":[0.0014438397,0.00020614377,0.00043267728,0.00076011306,0.00014307011,0.00034553657,0.0004407136,0.00016564944,0.0002070497],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027506626,0.0003252044,0.8890909,0.00010983338,0.00017404262,0.0007545464,0.00078072207,0.051038153,0.018145211,0.00048126944,0.00048344277,0.03586617],"study_design_scores_gemma":[0.00012696805,0.0017952858,0.8662452,0.000021612903,0.00034361306,0.00042864433,0.0033396373,0.11623677,0.010046438,0.0006222527,0.00075940666,0.000034122317],"about_ca_topic_score_codex":0.010923528,"about_ca_topic_score_gemma":0.022099493,"teacher_disagreement_score":0.010923528,"about_ca_system_score_codex":0.00061736244,"about_ca_system_score_gemma":0.0006079259,"threshold_uncertainty_score":0.021719933},"labels":[],"label_agreement":null},{"id":"W2005369613","doi":"10.1007/s00024-008-0390-0","title":"Postseismic Deformation Following the 1994 Northridge Earthquake Identified Using the Localized Hartley Transform Filter","year":2008,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Princess Margaret Cancer Centre; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministerio de Economía y Competitividad; Institute for Catastrophic Loss Reduction","keywords":"Deformation (meteorology); Superposition principle; Filter (signal processing); Relaxation (psychology); Viscoelasticity; Geodesy; Geology; Global Positioning System; Seismology; Computer science; Mathematics; Physics; Telecommunications; Mathematical analysis","score_opus":0.019227504440896902,"score_gpt":0.20540551823538672,"score_spread":0.1861780137944898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005369613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957469,0.000033316745,0.001556874,0.000029100675,0.0000076044944,0.0000060544535,0.0006819694,0.000047821806,0.0018902929],"genre_scores_gemma":[0.99585754,0.0000392112,0.0012227598,0.0000082809875,0.000006196958,0.0000038863172,0.00094057224,0.000008374407,0.0019131834],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999502,0.000003466328,0.0000023557197,0.000013302527,0.000013675903,0.000016943754],"domain_scores_gemma":[0.99984884,0.00003121418,0.00003498597,0.0000126733985,0.00005190536,0.00002032552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008805192,0.00012024993,0.00014648575,0.0005397041,0.0001856694,0.0003147745,0.00011291941,0.0002416725,0.002171626],"category_scores_gemma":[0.00033523218,0.00009501913,0.000075725824,0.00061387103,0.000121605655,0.00025579124,0.00014108702,0.00015846387,0.00043114708],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019575187,0.00035951062,0.54974294,0.000111575304,0.0001576698,0.00085685047,0.00096380746,0.04102163,0.12386346,0.0014566999,0.0110529745,0.26845548],"study_design_scores_gemma":[0.000009873402,0.000029651905,0.9875311,0.0000026624277,0.000010986513,0.000030479869,0.00007793751,0.009481536,0.0019346299,0.000038061127,0.0008465335,0.000006541966],"about_ca_topic_score_codex":0.070555635,"about_ca_topic_score_gemma":0.19676389,"teacher_disagreement_score":0.070555635,"about_ca_system_score_codex":0.00033782804,"about_ca_system_score_gemma":0.00040554343,"threshold_uncertainty_score":0.1402899},"labels":[],"label_agreement":null},{"id":"W2005751790","doi":"10.5194/nhess-12-2193-2012","title":"Effect of tidal triggering on seismicity in Taiwan revealed by the empirical mode decomposition method","year":2012,"lang":"en","type":"article","venue":"Natural hazards and earth system sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Central University; National Science Council","keywords":"Induced seismicity; Hilbert–Huang transform; Seismology; Geology; Mode (computer interface); Aftershock; Statistical analysis; Tidal force; Physics; Statistics; Mathematics; Computer science","score_opus":0.026126873341412404,"score_gpt":0.3495199755989818,"score_spread":0.3233931022575694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005751790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98907065,0.00006896453,0.010331991,0.00003155705,0.0000049834734,0.000004686128,0.00009623286,0.00003309166,0.00035788532],"genre_scores_gemma":[0.9970906,0.00003544936,0.0026254992,0.0000040134023,0.000005193471,0.0000034605382,0.00016590327,0.0000056523127,0.000064129374],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996383,0.00018527854,0.000029568584,0.000053561092,0.000062217936,0.000031088424],"domain_scores_gemma":[0.99582577,0.002675422,0.0005590672,0.00039490903,0.00042036764,0.00012459683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010961525,0.00027498035,0.00020645792,0.0010294812,0.00011575664,0.00037821996,0.00017677378,0.00013824117,0.00050340756],"category_scores_gemma":[0.007698142,0.000132693,0.00024452756,0.00084392435,0.00015957485,0.00038309125,0.000342431,0.00021239527,0.000081380065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006637595,0.00015662707,0.76354265,0.00010237362,0.00034027078,0.0006612288,0.0004011198,0.06922689,0.033685967,0.0013407888,0.0006513643,0.12922697],"study_design_scores_gemma":[0.000019651989,0.00012881852,0.5086568,0.00001688829,0.000099525016,0.00017662685,0.00014444033,0.48546436,0.004364619,0.0004609446,0.00044157365,0.000025809002],"about_ca_topic_score_codex":0.0030612068,"about_ca_topic_score_gemma":0.0029313301,"teacher_disagreement_score":0.0030612068,"about_ca_system_score_codex":0.00017370257,"about_ca_system_score_gemma":0.00027525314,"threshold_uncertainty_score":0.0060867667},"labels":[],"label_agreement":null},{"id":"W2005936010","doi":"10.1029/2003jb002521","title":"Fault slip and seismic moment of the 1700 Cascadia earthquake inferred from Japanese tsunami descriptions","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":341,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Tsunami earthquake; Moment magnitude scale; Seafloor spreading; Subduction; Seismic moment; Slip (aerodynamics); Bathymetry; Magnitude (astronomy); Submarine pipeline; Shore; Earthquake rupture; Geodesy; Fault (geology); Tectonics; Oceanography; Geometry","score_opus":0.037205432693836596,"score_gpt":0.27863110306620636,"score_spread":0.24142567037236978,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005936010","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955621,0.00008059584,0.0007428924,0.000014912727,0.0000025678876,0.000002995324,0.0015549478,0.00003959962,0.0019992704],"genre_scores_gemma":[0.9971782,0.00005260841,0.0004199117,0.0000015217812,0.000002220671,0.0000027184935,0.0021452825,0.0000050511367,0.00019241209],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999001,0.000009364313,0.000019867706,0.000018925275,0.000029904764,0.000021729968],"domain_scores_gemma":[0.99951816,0.00009585503,0.00014999119,0.000038698436,0.00012242193,0.00007486186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019549622,0.00027268706,0.00009855969,0.0021207388,0.00016546618,0.00032564532,0.00019162468,0.00014438991,0.0011711908],"category_scores_gemma":[0.0013732964,0.00018964254,0.00017567773,0.0013260735,0.00019515317,0.00030851684,0.000285775,0.000108832544,0.00015870114],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017333034,0.00002221014,0.94875723,0.0000916638,0.00006369264,0.0004054519,0.00077808124,0.02474373,0.0061578946,0.0014279966,0.0009309176,0.016447658],"study_design_scores_gemma":[0.0000055338874,0.000024478395,0.9812711,0.000012919115,0.000023029253,0.00012636036,0.00022779402,0.016379591,0.0006471881,0.00028505904,0.0009810566,0.000015820393],"about_ca_topic_score_codex":0.028149562,"about_ca_topic_score_gemma":0.030803159,"teacher_disagreement_score":0.028149562,"about_ca_system_score_codex":0.0006978961,"about_ca_system_score_gemma":0.00034984626,"threshold_uncertainty_score":0.055971444},"labels":[],"label_agreement":null},{"id":"W2006217828","doi":"10.1002/2013jb010817","title":"Modeling shear wave splitting due to stress‐induced anisotropy, with an application to Mount Asama Volcano, Japan","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"State Key Laboratory of Synthetical Automation for Process Industries; Victoria University of Wellington; University of Victoria","keywords":"Anisotropy; Volcano; Geology; Stress field; Stress (linguistics); Shear wave splitting; Shear stress; Seismology; Shear (geology); Geophysics; Mechanics; Petrology; Optics; Structural engineering; Finite element method; Engineering; Physics","score_opus":0.04384439226394852,"score_gpt":0.31229362282352646,"score_spread":0.2684492305595779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006217828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912203,0.00005315099,0.007732775,0.00007288606,0.000007709856,0.0000101524065,0.000052272695,0.000067501285,0.0007832646],"genre_scores_gemma":[0.9976629,0.000027396634,0.0021167737,0.0000042542447,0.0000034352186,0.000006216901,0.000034089455,0.000007815431,0.00013710317],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999232,0.000017334198,0.0000052661867,0.00002150286,0.000015804659,0.000016776],"domain_scores_gemma":[0.9996879,0.0001309772,0.00006003938,0.000034891516,0.000050594594,0.000035479592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023779484,0.0005687485,0.00034787753,0.00038752006,0.00047063344,0.00066041946,0.0004688301,0.0008404267,0.00037494896],"category_scores_gemma":[0.0008371789,0.0004260216,0.00063078606,0.0004223647,0.00048617268,0.0003408707,0.00032629794,0.00032309318,0.000054897122],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003364004,0.0000404061,0.00974082,0.000009702172,0.000020546004,0.000093351926,0.000037121077,0.9814767,0.006059829,0.0003508155,0.00004933141,0.002087718],"study_design_scores_gemma":[0.000003721755,0.000006599375,0.001117682,5.267508e-7,0.0000025072995,0.000004756517,0.0000060773164,0.99856,0.00024157672,0.00003238944,0.00002193371,0.0000022930421],"about_ca_topic_score_codex":0.044159155,"about_ca_topic_score_gemma":0.020537807,"teacher_disagreement_score":0.044159155,"about_ca_system_score_codex":0.00077909173,"about_ca_system_score_gemma":0.00073192385,"threshold_uncertainty_score":0.0878042},"labels":[],"label_agreement":null},{"id":"W2006292869","doi":"10.1016/j.tecto.2006.12.002","title":"Linking stress field deflection to basement structures in southern Ontario: Results from numerical modelling","year":2007,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Stress field; Seismology; Terrane; Tectonics; Crust; Slip (aerodynamics); Deflection (physics); Stress (linguistics); Deformation (meteorology); Geodesy; Geophysics; Finite element method","score_opus":0.023704247068640504,"score_gpt":0.23005256652236117,"score_spread":0.20634831945372067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006292869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975369,0.000037645583,0.00027510477,0.00006736822,0.0000019955023,0.00001105607,0.000643814,0.000024143565,0.001401987],"genre_scores_gemma":[0.9978726,0.0000638231,0.00046350158,0.000008504334,0.00000184033,0.000010350598,0.00053175853,0.000007955872,0.0010396274],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998293,0.000030681855,0.000012969257,0.000046098296,0.000031318257,0.00004961526],"domain_scores_gemma":[0.99940836,0.00026433094,0.00008731686,0.000040614632,0.00013565621,0.00006369939],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027947113,0.00038464027,0.00038334297,0.00040870256,0.0011944456,0.0012057148,0.0012372107,0.001008053,0.0025219016],"category_scores_gemma":[0.0016138079,0.0005059323,0.000556603,0.0010718656,0.0008210811,0.00047743024,0.00043053986,0.0004014066,0.00032387124],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037326574,0.0002381359,0.22464086,0.00010931359,0.00012518495,0.00038765272,0.0009635311,0.7594185,0.0025575727,0.00091405807,0.0010845716,0.009187482],"study_design_scores_gemma":[0.00023856045,0.0001077586,0.2563025,0.000036396166,0.00013833008,0.000069162954,0.0014403381,0.737757,0.0011293651,0.0005154282,0.002182727,0.00008245561],"about_ca_topic_score_codex":0.9763372,"about_ca_topic_score_gemma":0.979939,"teacher_disagreement_score":0.023662806,"about_ca_system_score_codex":0.010188722,"about_ca_system_score_gemma":0.006666657,"threshold_uncertainty_score":0.07392472},"labels":[],"label_agreement":null},{"id":"W2006305975","doi":"10.1029/2006gl026568","title":"Impact of 3‐D Earth structure on Fennoscandian glacial isostatic adjustment: Implications for space‐geodetic estimates of present‐day crustal deformations","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Geology; Geodetic datum; Lithosphere; Geodesy; Mantle (geology); Glacial period; Geophysics; Earth model; Global Positioning System; Seismology; Geomorphology; Tectonics","score_opus":0.02620846353106203,"score_gpt":0.3118804405375901,"score_spread":0.2856719770065281,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006305975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9697899,0.0003184106,0.024999904,0.00043666767,0.00003695986,0.000015482165,0.0006806078,0.00024881418,0.0034731575],"genre_scores_gemma":[0.99569833,0.00010920587,0.003687565,0.00003943792,0.0000051861252,0.000006520249,0.00018863469,0.00003220902,0.00023283256],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999747,0.00009302344,0.000019963914,0.000057244753,0.000050507573,0.000032136548],"domain_scores_gemma":[0.99923444,0.00041430225,0.000086744796,0.000097307566,0.00011900845,0.000048202586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096994184,0.0004508054,0.0003611782,0.00044911267,0.00051918754,0.0012523725,0.0007041341,0.0005502661,0.0009187379],"category_scores_gemma":[0.0039507044,0.0002943694,0.0005593405,0.0008219644,0.0007966449,0.00076997065,0.0006257938,0.0004154718,0.00013117694],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000120320554,0.000025090769,0.12466085,0.000046266206,0.000113490176,0.00012744938,0.00012930945,0.8465448,0.0033034459,0.0026224018,0.00023326727,0.022073278],"study_design_scores_gemma":[0.000021546026,0.000027945509,0.09013614,0.000024010304,0.00003652757,0.00006286199,0.0000901896,0.9055504,0.0016955411,0.0013957733,0.0009210127,0.00003807311],"about_ca_topic_score_codex":0.21950269,"about_ca_topic_score_gemma":0.19373827,"teacher_disagreement_score":0.21950269,"about_ca_system_score_codex":0.0018016077,"about_ca_system_score_gemma":0.0025164078,"threshold_uncertainty_score":0.43645006},"labels":[],"label_agreement":null},{"id":"W2006308870","doi":"10.1016/j.crte.2003.11.017","title":"Kinematics of the Corinth Gulf inferred from calcite dating and syntectonic sedimentary characteristics","year":2004,"lang":"en","type":"article","venue":"Comptes Rendus Géoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Rift; Fault (geology); Sedimentary rock; Quaternary; Geomorphology; Humanities; Paleontology; Tectonics","score_opus":0.02042640262789098,"score_gpt":0.21895795344627184,"score_spread":0.19853155081838086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006308870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970042,0.00027876813,0.00011456889,0.000024354793,0.000003586937,0.000007842844,0.00031449425,0.00000913094,0.0022430571],"genre_scores_gemma":[0.9986253,0.000225663,0.00032760334,0.000007491774,0.0000017360379,0.0000048853267,0.00033061136,0.0000047559297,0.00047184015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999033,0.000009127629,0.000009375334,0.00003373616,0.000022305789,0.000022064052],"domain_scores_gemma":[0.9997063,0.00003075624,0.0001018583,0.000027089918,0.000104409526,0.00002954376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020630207,0.0005322344,0.00015248818,0.001509875,0.00031069166,0.0004937746,0.00023102356,0.00016834412,0.0014435359],"category_scores_gemma":[0.0006347773,0.00017929343,0.00009871338,0.0016162605,0.00072162226,0.0002744335,0.0004102994,0.00019242299,0.00022665209],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013917733,0.000021728392,0.93004525,0.00008040783,0.00002832852,0.00060744287,0.0013226033,0.00078801485,0.037408996,0.00045076924,0.00022982359,0.02887753],"study_design_scores_gemma":[0.000009392933,0.000028603077,0.9965707,0.000019816305,0.00000802231,0.0001813216,0.00031041494,0.0004099997,0.001369107,0.000072960596,0.0010140392,0.0000055969513],"about_ca_topic_score_codex":0.08413062,"about_ca_topic_score_gemma":0.20964606,"teacher_disagreement_score":0.08413062,"about_ca_system_score_codex":0.00096180465,"about_ca_system_score_gemma":0.00084197737,"threshold_uncertainty_score":0.16728187},"labels":[],"label_agreement":null},{"id":"W2006395624","doi":"10.1111/j.1755-6724.2011.00593.x","title":"Deformation Stages and Ar‐Ar Age Data of the Wan‐Zhe‐Gan Tectonic Zone, Southeast China, and Their Tectonic Significance","year":2011,"lang":"en","type":"article","venue":"Acta Geologica Sinica - English Edition","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Tectonics; Fault (geology); Cretaceous; Fibrous joint; Seismology; Ophiolite; Shear zone; Strike-slip tectonics; Craton; Paleontology; Subduction; Transform fault; Basement; Geography","score_opus":0.03607088964717443,"score_gpt":0.21063662806910247,"score_spread":0.17456573842192805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006395624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974847,0.00020609447,0.00010248689,0.000011669524,0.0000028425038,0.0000058698647,0.0013259116,0.000012834603,0.0008476071],"genre_scores_gemma":[0.9973573,0.00007917874,0.00012524512,0.0000045780475,0.0000024951207,0.0000045237534,0.0020032874,0.0000028520403,0.00042038242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988794,0.0000126884315,0.000021356473,0.000031246014,0.000028825341,0.000017932318],"domain_scores_gemma":[0.99969375,0.000024174919,0.0000860511,0.00003218492,0.000116436466,0.000047454225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030652233,0.00035144063,0.00014753695,0.0016320305,0.00020778005,0.00029740843,0.00023134494,0.00016517125,0.0007077148],"category_scores_gemma":[0.00028289016,0.00012434625,0.00019498335,0.0018344476,0.00019225241,0.00024632254,0.00019994177,0.000103202845,0.00019257992],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007242352,0.00001105225,0.98720294,0.000029644905,0.000036346817,0.00009228404,0.00021730426,0.00036029884,0.0050077573,0.00004500431,0.00013110056,0.006793719],"study_design_scores_gemma":[0.000001628879,0.000008569215,0.99931574,0.0000014046597,0.00000504952,0.000020053265,0.000034504872,0.00016315984,0.00018071037,0.0000045160164,0.00026334685,0.0000011964632],"about_ca_topic_score_codex":0.047127135,"about_ca_topic_score_gemma":0.09182673,"teacher_disagreement_score":0.047127135,"about_ca_system_score_codex":0.0005698628,"about_ca_system_score_gemma":0.00041127938,"threshold_uncertainty_score":0.093705654},"labels":[],"label_agreement":null},{"id":"W2007039016","doi":"10.1029/2004gl020882","title":"Anomalous topography in the western Atlantic caused by edge‐driven convection","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Ocean surface topography; Convection; Lithosphere; Geophysics; Convection cell; Subsidence; Mantle convection; Plate tectonics; Climatology; Seismology; Geomorphology; Tectonics; Meteorology; Natural convection","score_opus":0.028833407324239682,"score_gpt":0.2732160692958878,"score_spread":0.24438266197164815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007039016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998134,0.0000045912384,0.00006133304,0.0000026010532,6.5587665e-7,5.4461174e-7,0.000009207447,0.0000042096312,0.00010339913],"genre_scores_gemma":[0.9998635,0.0000053030803,0.00007520414,0.0000025278657,6.0865057e-7,6.0171567e-7,0.0000205934,7.387076e-7,0.000030828505],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999677,0.0000051478696,0.0000020813761,0.000006170414,0.000006894079,0.000012042364],"domain_scores_gemma":[0.99985814,0.000024766161,0.000044924018,0.000024311545,0.00001895392,0.000028909824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004760191,0.00009024855,0.0000941872,0.00008927754,0.00012965259,0.00013716708,0.000071646646,0.00011421536,0.00042928028],"category_scores_gemma":[0.00030620862,0.00008751451,0.00008787075,0.00007529731,0.00022480956,0.000078799174,0.00017398204,0.00012370171,0.00004328687],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005849204,0.000106396736,0.20691295,0.000030389185,0.000041597108,0.00065189326,0.00018186137,0.0108703915,0.77360636,0.00041198742,0.00019238674,0.006408888],"study_design_scores_gemma":[0.000088700275,0.00039195488,0.8921644,0.0000055061255,0.000041824387,0.0004440545,0.00014558189,0.0645808,0.041435033,0.00031544265,0.0003677962,0.000018811033],"about_ca_topic_score_codex":0.002899115,"about_ca_topic_score_gemma":0.0043535186,"teacher_disagreement_score":0.002899115,"about_ca_system_score_codex":0.00016147019,"about_ca_system_score_gemma":0.000080398524,"threshold_uncertainty_score":0.0057644844},"labels":[],"label_agreement":null},{"id":"W2007201487","doi":"10.1093/gji/ggv123","title":"Magnetic potential, vector and gradient tensor fields of a tesseroid in a geocentric spherical coordinate system","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Cartesian tensor; Spherical coordinate system; Cartesian coordinate system; Numerical integration; Gaussian quadrature; Mathematical analysis; Coordinate system; Mathematics; Vector spherical harmonics; Quadrature (astronomy); Geometry; Spherical harmonics; Physics; Tensor density; Tensor field; Exact solutions in general relativity; Boundary value problem; Nyström method","score_opus":0.012351247437268372,"score_gpt":0.20847791359157372,"score_spread":0.19612666615430535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007201487","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3255615,0.002809178,0.49142873,0.002592961,0.0019344096,0.0002481092,0.005955779,0.001683587,0.16778569],"genre_scores_gemma":[0.8487762,0.0023715915,0.0967339,0.00017840645,0.0004370627,0.00010490535,0.0023680036,0.0003237293,0.048706215],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9998841,0.00003244662,0.0000068678723,0.0000313789,0.000034704768,0.000010460635],"domain_scores_gemma":[0.99965966,0.00003211049,0.0000609679,0.000019552333,0.00018904266,0.0000386525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018834994,0.00036848284,0.00025386407,0.00089810835,0.00032607655,0.00081828475,0.00029471453,0.00029783093,0.007978844],"category_scores_gemma":[0.00079103274,0.000119072174,0.00018811876,0.001285016,0.0006089273,0.0007963242,0.00041769785,0.00030118696,0.0019744593],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008387061,0.00006546439,0.016615946,0.00064257515,0.000095628675,0.0014448472,0.003526121,0.060423397,0.06799061,0.49381724,0.103007644,0.25153175],"study_design_scores_gemma":[0.00017176224,0.0009002178,0.06581605,0.00020047832,0.00016257579,0.003077355,0.005496939,0.19544813,0.022920838,0.1319788,0.5735205,0.0003064143],"about_ca_topic_score_codex":0.0046743006,"about_ca_topic_score_gemma":0.0034743273,"teacher_disagreement_score":0.007978844,"about_ca_system_score_codex":0.00030711523,"about_ca_system_score_gemma":0.0005213977,"threshold_uncertainty_score":0.026691914},"labels":[],"label_agreement":null},{"id":"W2007383373","doi":"10.1007/s11069-012-0455-3","title":"Modeling of coastal erosion and sediment deposition during the 2004 Indian Ocean tsunami in Lhok Nga, Sumatra, Indonesia","year":2012,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Nautical Research Society","funders":"","keywords":"Bed load; Geology; Bay; Sediment transport; Deposition (geology); Sediment; Erosion; Debris; Geomorphology; Debris flow; Oceanography; Hydrology (agriculture); Geotechnical engineering","score_opus":0.007651747588825642,"score_gpt":0.2085035767660583,"score_spread":0.20085182917723265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007383373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99777716,0.000033568787,0.0003048196,0.000111727386,0.000011726267,0.000008515751,0.00035159366,0.0000362009,0.0013646965],"genre_scores_gemma":[0.9987764,0.000038457696,0.00033750708,0.000011450605,0.0000033970678,0.000011699275,0.0002617027,0.000011516883,0.00054786436],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998925,0.000022527536,0.00001340413,0.000027439486,0.000011258157,0.000033000382],"domain_scores_gemma":[0.9997085,0.00011002655,0.000043277483,0.000023272936,0.00005520008,0.000059731352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029854136,0.00070809596,0.0007115524,0.00042503572,0.0009216136,0.0014232477,0.001135674,0.0012341664,0.0012147427],"category_scores_gemma":[0.00092671096,0.00074748957,0.0009835684,0.00064214855,0.00065359345,0.0006333997,0.0005745071,0.0009098593,0.0001909018],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002390704,0.00021992672,0.05773852,0.000036000314,0.000115269904,0.00041162042,0.000097585376,0.93758035,0.0011529238,0.00027904086,0.00037324856,0.0017563852],"study_design_scores_gemma":[0.000049761784,0.00006152752,0.029680856,0.0000061262435,0.00006165264,0.000045823774,0.0002785741,0.96908444,0.00041224275,0.00009700811,0.00020210918,0.000019882638],"about_ca_topic_score_codex":0.23358944,"about_ca_topic_score_gemma":0.15363017,"teacher_disagreement_score":0.23358944,"about_ca_system_score_codex":0.0022247476,"about_ca_system_score_gemma":0.0020589277,"threshold_uncertainty_score":0.4644596},"labels":[],"label_agreement":null},{"id":"W2007473665","doi":"10.1007/s11069-011-9959-5","title":"Tsunami risk and impacts on coastlines","year":2011,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Natural hazard; Risk assessment; Geology; Environmental science; Oceanography; Computer science; Computer security","score_opus":0.01887628400072301,"score_gpt":0.22505368839074394,"score_spread":0.20617740439002094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007473665","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933323,0.00028653414,0.00007726692,0.00014777954,0.0000036576516,0.0000026448265,0.00048182273,0.0000037142772,0.0056643803],"genre_scores_gemma":[0.9985752,0.0003650776,0.000033483273,0.00000776265,0.0000060462494,0.0000010526813,0.00022624577,0.0000015455688,0.00078346726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998708,0.000036980928,0.000013284813,0.000014286654,0.000027956416,0.000036689325],"domain_scores_gemma":[0.9987662,0.00022572628,0.0005929076,0.000050937742,0.00019551271,0.00016870009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022285154,0.0001778255,0.00010595062,0.00105616,0.0003119052,0.0008000405,0.00018192704,0.00028245008,0.0049028997],"category_scores_gemma":[0.0024822874,0.0001281902,0.00031022992,0.0017240618,0.00035391908,0.000610361,0.0004135488,0.0003303174,0.0004279891],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022903988,0.000046603243,0.9840068,0.000024376808,0.000117707066,0.00042888947,0.00038885532,0.0056434344,0.00039891567,0.0017919247,0.0004714065,0.006451932],"study_design_scores_gemma":[0.00000776245,0.000081677405,0.9939122,0.000012723225,0.000038550374,0.00022185182,0.0012360468,0.0022129111,0.00007668814,0.0011241762,0.0010686035,0.000006813389],"about_ca_topic_score_codex":0.0360153,"about_ca_topic_score_gemma":0.06645877,"teacher_disagreement_score":0.0360153,"about_ca_system_score_codex":0.0007030991,"about_ca_system_score_gemma":0.000305406,"threshold_uncertainty_score":0.071611345},"labels":[],"label_agreement":null},{"id":"W2007880480","doi":"10.1016/j.tecto.2014.05.002","title":"The Fethiye–Burdur Fault Zone: A component of upper plate extension of the subduction transform edge propagator fault linking Hellenic and Cyprus Arcs, Eastern Mediterranean","year":2014,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Evaporite; Quaternary; Structural basin; Seismology; Fault (geology); Paleontology; Nappe; Transform fault; Horst; Late Miocene; Fold and thrust belt; Extensional tectonics; Tectonics; Rift; Foreland basin","score_opus":0.01613376366700741,"score_gpt":0.21137097104441152,"score_spread":0.1952372073774041,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007880480","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950936,0.0002167421,0.00020877307,0.000041596984,0.000005075191,0.000009096987,0.0001848218,0.0000109383,0.004229316],"genre_scores_gemma":[0.9989489,0.0000703388,0.00017607327,0.000007344738,0.000003907396,0.000002349701,0.00013998548,0.0000018339113,0.00064942264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993634,0.000005227756,0.0000062935674,0.000022152997,0.0000105890285,0.000019298137],"domain_scores_gemma":[0.99990284,0.000014475224,0.000040507588,0.000008596947,0.000019831377,0.00001372857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001052834,0.00015619326,0.00014192535,0.00087365566,0.00039610406,0.0005239799,0.0001426813,0.00019009404,0.00202647],"category_scores_gemma":[0.0002993097,0.0000912362,0.00009193382,0.0009891259,0.0005071544,0.00027754286,0.00034880557,0.000101592916,0.00017607449],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038677285,0.000046822486,0.889191,0.0001832526,0.00006900408,0.0018506851,0.0032893224,0.0015303263,0.025447777,0.0045996956,0.0008402531,0.07256516],"study_design_scores_gemma":[0.0000043458367,0.0000154367,0.9971938,0.000011529755,0.000008730232,0.00020868106,0.00033888387,0.0002806108,0.00038179557,0.00008640483,0.001467841,0.0000018154174],"about_ca_topic_score_codex":0.017999789,"about_ca_topic_score_gemma":0.021871528,"teacher_disagreement_score":0.017999789,"about_ca_system_score_codex":0.0005199961,"about_ca_system_score_gemma":0.00051085674,"threshold_uncertainty_score":0.035790026},"labels":[],"label_agreement":null},{"id":"W2008293258","doi":"10.1785/0120090104","title":"Precursory Rise of P-Wave Attenuation before the 2004 Parkfield Earthquake","year":2010,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto","keywords":"Seismology; Attenuation; Geology; Physics; Optics","score_opus":0.015257671696248469,"score_gpt":0.20670606868118344,"score_spread":0.19144839698493496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008293258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986332,0.00005008581,0.00014384334,0.00007258914,0.0000060223147,0.0000058803403,0.0002112111,0.000014363874,0.00086274033],"genre_scores_gemma":[0.99935764,0.000032627824,0.00008654312,0.0000111711315,0.0000071326135,0.0000024121325,0.00020396187,0.0000013957929,0.00029712496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993515,0.0000049181876,0.0000037123505,0.000018235125,0.00002184645,0.000016214077],"domain_scores_gemma":[0.99949706,0.000050516574,0.0001691423,0.00001981762,0.00016099609,0.00010245408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012717818,0.000109853,0.00014541678,0.000452384,0.00024363672,0.00034685343,0.00013517607,0.00027478038,0.0015053864],"category_scores_gemma":[0.0011014631,0.00008688563,0.00005196708,0.0002740162,0.0001626348,0.00024240656,0.00030948195,0.000455657,0.00023110597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078727177,0.00021735394,0.92295307,0.00005267219,0.000032085427,0.0021100962,0.0008608041,0.00039247182,0.035843726,0.00019403432,0.0018788839,0.03467754],"study_design_scores_gemma":[0.0000026587138,0.0001037495,0.99766386,0.000003985132,0.0000026199293,0.00021120619,0.00014443726,0.0001717312,0.0011534492,0.000019408291,0.0005203849,0.0000024984097],"about_ca_topic_score_codex":0.009520651,"about_ca_topic_score_gemma":0.01705597,"teacher_disagreement_score":0.009520651,"about_ca_system_score_codex":0.0004023628,"about_ca_system_score_gemma":0.00021458697,"threshold_uncertainty_score":0.018930495},"labels":[],"label_agreement":null},{"id":"W2008547866","doi":"10.1029/2012jb009153","title":"Spherical‐Earth finite element model of short‐term postseismic deformation following the 2004 Sumatra earthquake","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Mantle (geology); Viscoelasticity; Rheology; Mantle wedge; Subduction; Seismology; Geophysics; Seismic tomography; Aftershock; Mantle convection; Geodesy; Physics; Tectonics","score_opus":0.047567695569248704,"score_gpt":0.29901462960866343,"score_spread":0.2514469340394147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008547866","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5277761,0.00051544537,0.42197087,0.0014182383,0.00016642002,0.00018810073,0.0018608774,0.00081301446,0.04529092],"genre_scores_gemma":[0.96415675,0.00031816756,0.018670104,0.00013701846,0.000034081782,0.00025941868,0.0007897222,0.00011562731,0.015519158],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999874,0.00003579243,0.000009400145,0.000028979843,0.000029807377,0.000022007336],"domain_scores_gemma":[0.99972564,0.00010989264,0.000049758426,0.00002299092,0.000059412243,0.00003222526],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002871378,0.00051861134,0.00063350477,0.0004169444,0.00051433215,0.0009323326,0.0017593121,0.0021884493,0.0023980753],"category_scores_gemma":[0.0007685873,0.0006070333,0.0008902305,0.00041402396,0.00074275205,0.0006023604,0.00070917787,0.0006930709,0.0005926074],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014560014,0.000010792753,0.00037849022,0.0000071986005,0.00000782188,0.0000396277,0.00002183896,0.99677074,0.00073965936,0.0012591104,0.00008224137,0.00066790264],"study_design_scores_gemma":[0.00000404831,0.0000051633206,0.00013502792,0.0000019503632,0.0000027062729,0.0000054437687,0.000008678179,0.9993999,0.00007219636,0.00021060884,0.00015160271,0.0000027492104],"about_ca_topic_score_codex":0.026400354,"about_ca_topic_score_gemma":0.012278941,"teacher_disagreement_score":0.026400354,"about_ca_system_score_codex":0.0008570897,"about_ca_system_score_gemma":0.0012077224,"threshold_uncertainty_score":0.052493393},"labels":[],"label_agreement":null},{"id":"W2008973163","doi":"10.1029/2001jb000145","title":"Mechanics of viscous wedges: Modeling by analytical and numerical approaches","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Wedge (geometry); Rheology; Asymmetry; Mechanics; Plane stress; Geology; Geometry; Physics; Mathematics; Finite element method; Thermodynamics","score_opus":0.09828241754713586,"score_gpt":0.29086147277775076,"score_spread":0.19257905523061492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008973163","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.11315938,0.002234371,0.87217855,0.00041175555,0.00005895654,0.00010633797,0.00020558828,0.00025486707,0.011390233],"genre_scores_gemma":[0.85706186,0.0045018937,0.13268812,0.00008209428,0.000093080555,0.0003837243,0.00016128374,0.00012708512,0.004900879],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999892,0.000032956395,0.000008596631,0.000015181824,0.000038259448,0.0000129702075],"domain_scores_gemma":[0.9997657,0.00009598636,0.0000590985,0.00003539212,0.000029203804,0.000014675439],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043767996,0.00057806255,0.0005076167,0.0006294585,0.00028629534,0.0007799482,0.0010403225,0.00085867516,0.0007368683],"category_scores_gemma":[0.0011683388,0.0003311053,0.00048841804,0.0005293778,0.0009897697,0.0010908163,0.0006774034,0.0004720735,0.00022499956],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000151133245,0.000060764443,0.0013163823,0.00012593759,0.00001714319,0.00014227508,0.00015949621,0.9084911,0.006473479,0.07142068,0.00032848006,0.011449156],"study_design_scores_gemma":[0.0000035911542,0.0000072626863,0.00021152863,0.000009117557,0.0000018880842,0.000024128696,0.000013809588,0.99012333,0.00037809758,0.008574867,0.0006462639,0.0000061156607],"about_ca_topic_score_codex":0.0023306669,"about_ca_topic_score_gemma":0.0009110729,"teacher_disagreement_score":0.0023306669,"about_ca_system_score_codex":0.0005420354,"about_ca_system_score_gemma":0.00040316916,"threshold_uncertainty_score":0.0046342015},"labels":[],"label_agreement":null},{"id":"W2009085684","doi":"10.1016/j.tecto.2007.11.037","title":"Three-dimensional patterns of seismic deformation in the Taiwan region with special implication from the 1999 Chi-Chi earthquake sequence","year":2007,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Council","keywords":"Seismology; Geology; Seismic moment; Subduction; Seismic hazard; Sequence (biology); Seismic gap; Tectonics; Induced seismicity; Fault (geology)","score_opus":0.02064204045551402,"score_gpt":0.21734839088021135,"score_spread":0.19670635042469733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009085684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990796,0.00002351274,0.000081260834,0.00003770002,0.0000035567514,0.0000031455345,0.000261471,0.000008058783,0.0005015898],"genre_scores_gemma":[0.9993773,0.000022342265,0.000071693394,0.000006305238,0.0000031860275,0.0000028269878,0.00034998913,0.000002117932,0.00016419812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999455,0.00000515308,0.0000067771243,0.0000125955285,0.000010648763,0.000019282621],"domain_scores_gemma":[0.9996948,0.000038408176,0.00008972047,0.000022235476,0.00005797045,0.00009694271],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007916476,0.0001434712,0.00012586605,0.0011193356,0.00032303526,0.00047098866,0.00020507806,0.00032626683,0.0010059179],"category_scores_gemma":[0.0004937325,0.00013457559,0.00021579217,0.001280329,0.00037962807,0.00019907358,0.00041556012,0.0002301729,0.00014319063],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081208884,0.00015806095,0.9329129,0.000055759807,0.00014956448,0.0018960754,0.0017214528,0.007339613,0.032458123,0.00061627815,0.0014270616,0.020453056],"study_design_scores_gemma":[0.0000045107763,0.000015760863,0.99791163,0.0000024367998,0.000009175809,0.000093083196,0.00027422747,0.0013258897,0.00016803893,0.0000444435,0.00014425615,0.0000064459223],"about_ca_topic_score_codex":0.024611704,"about_ca_topic_score_gemma":0.042625975,"teacher_disagreement_score":0.024611704,"about_ca_system_score_codex":0.00038604776,"about_ca_system_score_gemma":0.00037986334,"threshold_uncertainty_score":0.048936903},"labels":[],"label_agreement":null},{"id":"W2009527236","doi":"10.1029/2006gl028477","title":"Postseismic deformation following the 1991 Racha, Georgia, earthquake","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Aftershock; Geology; Seismology; Crust; Deformation (meteorology); Seismic moment; Tsunami earthquake; Geodesy; Moment (physics); Thrust; Geophysics; Fault (geology); Oceanography","score_opus":0.029511904896875933,"score_gpt":0.2860385575895907,"score_spread":0.25652665269271474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009527236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909425,0.000014618262,0.000020024821,0.000027675818,0.0000014810089,0.000002374803,0.00018435517,0.0000047348917,0.0006504963],"genre_scores_gemma":[0.9992836,0.000018617642,0.000029416977,0.000010442266,0.0000013889071,0.0000019809752,0.00034141383,0.0000014518661,0.00031159798],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993515,0.0000066617235,0.0000033144463,0.000016878827,0.000016609842,0.000021344733],"domain_scores_gemma":[0.9997813,0.000018432462,0.000084262945,0.000021947537,0.000056836496,0.000037168396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000083286825,0.00013925898,0.000119834425,0.00029447582,0.00030404722,0.00026447274,0.00019867896,0.0003591113,0.0007095034],"category_scores_gemma":[0.0006394159,0.000111051464,0.00007669865,0.00025297637,0.00021388795,0.00014949731,0.00029354967,0.00022271919,0.00029437896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005173267,0.00013659016,0.9292929,0.000055171357,0.00006514006,0.0008767865,0.0011285617,0.0068236482,0.03681471,0.000410047,0.002858341,0.021020833],"study_design_scores_gemma":[0.0000022688002,0.000023307077,0.9989423,0.0000018126547,0.0000025772283,0.00003376892,0.00005975272,0.0005573063,0.00014211782,0.000011851587,0.00022091513,0.0000020136333],"about_ca_topic_score_codex":0.07229655,"about_ca_topic_score_gemma":0.17837028,"teacher_disagreement_score":0.07229655,"about_ca_system_score_codex":0.000884536,"about_ca_system_score_gemma":0.00036063505,"threshold_uncertainty_score":0.1437515},"labels":[],"label_agreement":null},{"id":"W2009603042","doi":"10.1007/s00024-003-2443-8","title":"Microseismic Event Detection Kalman Filter: Derivation of the Noise Covariance Matrix and Automated First Break Determination for Accurate Source Location Estimation","year":2004,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Read Jones Christoffersen (Canada)","funders":"","keywords":"Microseism; Computer science; Kalman filter; Filter (signal processing); Algorithm; Noise (video); Covariance; Data mining; Eikonal equation; Covariance matrix; Real-time computing; Geology; Seismology; Mathematics; Statistics; Artificial intelligence","score_opus":0.007018617140738443,"score_gpt":0.21382902894303576,"score_spread":0.2068104118022973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009603042","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0036141418,0.00006212472,0.99577916,0.000038928607,0.00001937824,0.000006145248,0.000050956365,0.00016362582,0.00026562487],"genre_scores_gemma":[0.35976657,0.0004894333,0.63168216,0.00007490551,0.0001226731,0.00013004398,0.00072075607,0.0002466619,0.0067668585],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996438,0.00004708806,0.000025534328,0.00009894391,0.00015615873,0.000028502694],"domain_scores_gemma":[0.999241,0.0003023175,0.000112661706,0.00009940587,0.00022419136,0.00002043776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000600725,0.0005077285,0.0005621227,0.0005497322,0.0003675207,0.0006837509,0.0007667431,0.00063850096,0.0018439833],"category_scores_gemma":[0.004056591,0.0006813324,0.0004885368,0.00061018683,0.00034930604,0.0010481991,0.00081391743,0.0010885539,0.0008555455],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018282363,0.00006270996,0.0031229986,0.0001385503,0.00010203887,0.000108644475,0.00013966601,0.5790727,0.016482402,0.07923471,0.0038310809,0.31752163],"study_design_scores_gemma":[0.0000074084924,0.000013431138,0.0013938171,0.000008367179,0.000008675087,0.00002986568,0.0000042368156,0.98910856,0.0026291653,0.005194752,0.0015897427,0.000011855492],"about_ca_topic_score_codex":0.0115628075,"about_ca_topic_score_gemma":0.018664218,"teacher_disagreement_score":0.0115628075,"about_ca_system_score_codex":0.0006160875,"about_ca_system_score_gemma":0.0017585467,"threshold_uncertainty_score":0.022991002},"labels":[],"label_agreement":null},{"id":"W2009855334","doi":"10.1073/pnas.1113481108","title":"Results of the Regional Earthquake Likelihood Models (RELM) test of earthquake forecasts in California","year":2011,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Central University; National Science Council; National Aeronautics and Space Administration","keywords":"Seismology; Earthquake prediction; Geology; Urban seismic risk; Earthquake scenario; Period (music); Earthquake swarm; Seismic hazard; Induced seismicity","score_opus":0.07498132337826542,"score_gpt":0.2508287316999652,"score_spread":0.17584740832169982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009855334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98312587,0.0004229357,0.0023560342,0.0009669072,0.00008326446,0.00005541427,0.0045594973,0.0003858321,0.008044388],"genre_scores_gemma":[0.9938922,0.000045418976,0.001067715,0.000055064298,0.000032253287,0.000025694268,0.0041271923,0.00005172398,0.00070268405],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9918166,0.0033894703,0.00058861356,0.0019196027,0.0017925901,0.000493248],"domain_scores_gemma":[0.92664564,0.053874444,0.006345243,0.004240874,0.0062317317,0.002662112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.012264081,0.00084522204,0.0009730648,0.0011065619,0.0008250649,0.0018753695,0.0011815475,0.00106786,0.0030515797],"category_scores_gemma":[0.07219217,0.00046012757,0.0011897756,0.0011057584,0.00065792137,0.001669731,0.0014883201,0.0012721646,0.00046646752],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0037542963,0.0005319651,0.46399653,0.0002069254,0.0008141379,0.00045111272,0.0007214675,0.47113195,0.0007588644,0.0033830826,0.020832095,0.033417642],"study_design_scores_gemma":[0.0006916652,0.0014840043,0.30142975,0.00009946857,0.0002983034,0.00015011801,0.0014644586,0.68067753,0.001754547,0.0048289355,0.0069072163,0.00021399303],"about_ca_topic_score_codex":0.07947175,"about_ca_topic_score_gemma":0.05317253,"teacher_disagreement_score":0.07947175,"about_ca_system_score_codex":0.0021534069,"about_ca_system_score_gemma":0.0016792398,"threshold_uncertainty_score":0.15801835},"labels":[],"label_agreement":null},{"id":"W2010204200","doi":"10.1038/nature02335","title":"Earthquake nucleation by transient deformations caused by the M = 7.9 Denali, Alaska, earthquake","year":2004,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":205,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Institutes of Health; Skaggs Institute for Chemical Biology, Scripps Research Institute; Damon Runyon Cancer Research Foundation; University of California, San Francisco; National Aeronautics and Space Administration","keywords":"Seismology; Geology; Induced seismicity; Magnitude (astronomy); Slow earthquake; Richter magnitude scale; Dynamic stress; Earthquake rupture; Foreshock; Fault (geology); Interplate earthquake; Aftershock; Dynamic loading; Scaling","score_opus":0.0073493752916340225,"score_gpt":0.20716413894347424,"score_spread":0.19981476365184023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010204200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99874556,0.00002105415,0.00006811105,0.00000855325,0.0000025975567,0.0000031302588,0.000051197876,0.0000043845835,0.00109537],"genre_scores_gemma":[0.99963105,0.000016170206,0.00003610896,0.000002744873,0.0000014440511,0.0000015580329,0.000069551075,6.950883e-7,0.00024057181],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996483,0.0000048405395,0.0000023040293,0.000009089447,0.000006488338,0.000012575705],"domain_scores_gemma":[0.9998516,0.000030831663,0.000029476003,0.000014129259,0.0000344616,0.00003958811],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011766906,0.00009418693,0.00014803736,0.00022805962,0.00055227993,0.00026998707,0.0001383485,0.00017595534,0.0012958113],"category_scores_gemma":[0.0003531976,0.00009553756,0.000092972536,0.0001570436,0.00021112185,0.00013711203,0.00028493654,0.0001751076,0.00020037462],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004469531,0.00044431395,0.69154596,0.00013216275,0.0001670407,0.0043007643,0.0012234632,0.013819153,0.2595187,0.0016424761,0.0027413687,0.019995049],"study_design_scores_gemma":[0.000046910995,0.00051667466,0.9660127,0.000013800569,0.00007817877,0.00044364695,0.001153787,0.010673514,0.019715242,0.0003371879,0.0009929774,0.000015443602],"about_ca_topic_score_codex":0.013518852,"about_ca_topic_score_gemma":0.02268568,"teacher_disagreement_score":0.013518852,"about_ca_system_score_codex":0.0003502975,"about_ca_system_score_gemma":0.00020983486,"threshold_uncertainty_score":0.026880324},"labels":[],"label_agreement":null},{"id":"W2010243369","doi":"10.1016/j.ijrmms.2014.09.019","title":"Effect of slip-weakening distance on selected seismic source parameters of mining-induced fault-slip","year":2014,"lang":"en","type":"article","venue":"International Journal of Rock Mechanics and Mining Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Slip (aerodynamics); Geology; Seismic moment; Seismology; Moment magnitude scale; Fault (geology); Shear (geology); Geometry; Engineering; Petrology","score_opus":0.013142404306779758,"score_gpt":0.24267555207349056,"score_spread":0.2295331477667108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010243369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999694,0.00002249814,0.00010375085,0.000004453772,0.0000014745646,0.0000012986357,0.000033210454,0.0000037593397,0.00013559681],"genre_scores_gemma":[0.99979967,0.000009959628,0.000035858167,0.000002409412,9.3191284e-7,8.031936e-7,0.000043951106,0.0000029085543,0.00010344327],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998981,0.000025120306,0.000012522258,0.000027784252,0.000013122586,0.000023328264],"domain_scores_gemma":[0.9980751,0.0014490936,0.00013203154,0.00007722166,0.000100409525,0.00016611318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031060367,0.00021511017,0.0003108167,0.0002055663,0.00014645963,0.00024907457,0.00019819895,0.0002780856,0.002297315],"category_scores_gemma":[0.0018291075,0.00013570882,0.00023789961,0.00015345203,0.00021440332,0.00025540232,0.0002530287,0.00026917976,0.00017726378],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.03136984,0.0014108247,0.37683544,0.0002620385,0.0004061697,0.0018087038,0.00053455087,0.023742907,0.53347665,0.00030809763,0.0003293954,0.029515386],"study_design_scores_gemma":[0.00012907165,0.0012911229,0.94398534,0.00000778516,0.00019653598,0.00036055024,0.00023857455,0.018724008,0.03476786,0.00008464233,0.00018767337,0.000026767524],"about_ca_topic_score_codex":0.0011248711,"about_ca_topic_score_gemma":0.0013649423,"teacher_disagreement_score":0.002297315,"about_ca_system_score_codex":0.00014730207,"about_ca_system_score_gemma":0.00016737482,"threshold_uncertainty_score":0.0076853037},"labels":[],"label_agreement":null},{"id":"W2010789279","doi":"10.2118/141863-ms","title":"Identifying Stress Transfer in CSS Reservoir Operations Through Integrated Microseismic Solutions","year":2011,"lang":"en","type":"article","venue":"SPE Middle East Oil and Gas Show and Conference","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Apheresis Group","funders":"","keywords":"Microseism; Geology; Stress (linguistics); Seismology; Volume (thermodynamics); Strain (injury); Energy transfer; Petroleum engineering; Deformation (meteorology); Geotechnical engineering","score_opus":0.11812742479156714,"score_gpt":0.23384855060344115,"score_spread":0.115721125811874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010789279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919423,0.000024084708,0.0059442814,0.000030076755,0.0000024917997,0.000020030951,0.00038621054,0.00010919285,0.0015414066],"genre_scores_gemma":[0.9985979,0.000012261829,0.0010847674,0.0000024791684,0.0000014499292,0.000006316721,0.00012125039,0.000003556705,0.00016998404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988556,0.000011371737,0.000006023321,0.000023224575,0.0000473141,0.00002644414],"domain_scores_gemma":[0.9997925,0.00003593576,0.00004990109,0.000009419534,0.00008728123,0.000024959814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015214006,0.00031975552,0.00022639033,0.0013588946,0.00023641379,0.0005576151,0.00033869033,0.00020612351,0.001226903],"category_scores_gemma":[0.00076850934,0.00019054319,0.00017954817,0.001341427,0.00015675322,0.00040794373,0.00036253096,0.00019328245,0.00013900133],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051580946,0.00024969954,0.6490407,0.00013343687,0.00023474457,0.0004893663,0.00078323396,0.11795469,0.08387669,0.0013566546,0.0008705576,0.14449441],"study_design_scores_gemma":[0.000015322405,0.00010195817,0.6952812,0.000013674298,0.000040791456,0.000056406996,0.0005752087,0.2961254,0.006653938,0.0005492554,0.0005600904,0.000026697147],"about_ca_topic_score_codex":0.08676386,"about_ca_topic_score_gemma":0.14028029,"teacher_disagreement_score":0.08676386,"about_ca_system_score_codex":0.0010675875,"about_ca_system_score_gemma":0.00077084353,"threshold_uncertainty_score":0.17251766},"labels":[],"label_agreement":null},{"id":"W2011049318","doi":"10.1016/j.tecto.2014.03.025","title":"The Pliocene–Quaternary tectonic evolution of the Cilicia and Adana basins, eastern Mediterranean: Special reference to the development of the Kozan Fault zone","year":2014,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; National University of Science and Technology","keywords":"Geology; Extensional tectonics; Structural basin; Fault (geology); Detachment fault; Paleontology; Quaternary; Tectonics; Seismology; Rift; Extensional definition","score_opus":0.018936237055918414,"score_gpt":0.20790038710641334,"score_spread":0.18896415005049494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011049318","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924771,0.001420209,0.00012628516,0.00018925348,0.000016884798,0.0000078179455,0.00025766273,0.000010339676,0.005494444],"genre_scores_gemma":[0.99772197,0.0005971375,0.00014832123,0.000033122567,0.000019588777,0.000004879795,0.00022508852,0.000008761687,0.0012409579],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999459,0.0000065472523,0.000005915497,0.000018154355,0.000007976455,0.000015441323],"domain_scores_gemma":[0.9999125,0.000007411859,0.000031980733,0.000006509268,0.000028929406,0.000012645507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021358329,0.00017900698,0.0001359313,0.0009371682,0.0003809179,0.0006189263,0.00027246747,0.0003411184,0.00228358],"category_scores_gemma":[0.0005182709,0.00014169709,0.00022751164,0.00079597713,0.000572387,0.00039068153,0.00048731355,0.00014708059,0.00026910688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00086840347,0.00009329745,0.8255166,0.00051032455,0.00031281865,0.0015354663,0.009283691,0.00426809,0.03828538,0.0064436886,0.0018140263,0.11106819],"study_design_scores_gemma":[0.0000078946505,0.000012633964,0.9959794,0.00001607133,0.000009624438,0.00008003437,0.0002662137,0.00016798425,0.00013233205,0.000079138,0.0032467647,0.0000019105692],"about_ca_topic_score_codex":0.027912933,"about_ca_topic_score_gemma":0.044785272,"teacher_disagreement_score":0.027912933,"about_ca_system_score_codex":0.0012300337,"about_ca_system_score_gemma":0.0006282784,"threshold_uncertainty_score":0.055500925},"labels":[],"label_agreement":null},{"id":"W2011135429","doi":"10.1007/s11069-013-0809-5","title":"Tsunami hazard assessment of Canada","year":2013,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Subduction; Geology; Seismology; Submarine landslide; Hazard; Arctic; Hazard analysis; Tsunami earthquake; Submarine pipeline; Fault (geology); Landslide; Continental shelf; Magnitude (astronomy); Hazard map; Seismic hazard; Oceanography; Tectonics","score_opus":0.007021375782336605,"score_gpt":0.22043241182098794,"score_spread":0.21341103603865133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011135429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8868764,0.0010022094,0.0016316056,0.0014269318,0.0000549184,0.00029681672,0.04793719,0.00020734429,0.060566716],"genre_scores_gemma":[0.9577699,0.0007721483,0.0016932117,0.00012701534,0.0000064018527,0.00005016782,0.0117467875,0.000042440664,0.027792033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99938464,0.000035078283,0.000021146307,0.000035755063,0.00037847928,0.00014493483],"domain_scores_gemma":[0.9969125,0.000066682456,0.000075058735,0.000034173598,0.002631349,0.00028019125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053107773,0.0003964047,0.00030388057,0.0031283142,0.0022564223,0.0014084614,0.0010904486,0.00026884195,0.003440088],"category_scores_gemma":[0.0014539126,0.00021580677,0.0003876446,0.004429379,0.00024703355,0.00035644387,0.00055695267,0.00041085677,0.00032967306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011394343,0.0004242695,0.7182891,0.00038315228,0.00046780668,0.00065176893,0.0016534406,0.04716199,0.003221849,0.00849443,0.06372564,0.15438709],"study_design_scores_gemma":[0.00009790746,0.00017479928,0.8917486,0.00013967202,0.00017031081,0.000104745486,0.0043456247,0.037413057,0.00247265,0.000818394,0.062435985,0.000078267054],"about_ca_topic_score_codex":0.99889624,"about_ca_topic_score_gemma":0.9993943,"teacher_disagreement_score":0.04810676,"about_ca_system_score_codex":0.04810676,"about_ca_system_score_gemma":0.08172217,"threshold_uncertainty_score":0.34904063},"labels":[],"label_agreement":null},{"id":"W2011432135","doi":"10.1007/s00024-005-2670-2","title":"Tidal Stress/Strain and the b-values of Acoustic Emissions at the Underground Research Laboratory, Canada","year":2005,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"University of Liverpool","keywords":"Strain (injury); Stress (linguistics); Environmental science; Atmospheric sciences; Geology; Biology","score_opus":0.014789928374971685,"score_gpt":0.23455788909606404,"score_spread":0.21976796072109236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011432135","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.984462,0.00017705819,0.00035209607,0.00025771078,0.0000128191805,0.000019719,0.0070933457,0.00003923522,0.0075859996],"genre_scores_gemma":[0.988425,0.00011942639,0.00020928307,0.000028138636,0.0000028577679,0.0000065080376,0.0025033073,0.000018699879,0.008686885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996762,0.000022588662,0.000013594627,0.000043617587,0.00014969493,0.00009426368],"domain_scores_gemma":[0.9977633,0.00018205785,0.00009775729,0.000039372655,0.0016560336,0.0002614594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002888922,0.00023628783,0.00021939854,0.0007250427,0.0015789737,0.0006991643,0.0008491825,0.0002671469,0.003493217],"category_scores_gemma":[0.0014035011,0.00021407036,0.00017948657,0.0013485645,0.00039012457,0.00032754778,0.00029298654,0.0005274141,0.0007109105],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004669155,0.00011667546,0.9726676,0.000029356259,0.000075481126,0.0001889972,0.00091224106,0.004068191,0.0033825312,0.00097521377,0.006080578,0.011036233],"study_design_scores_gemma":[0.000009145825,0.000018353885,0.9942924,0.000010801192,0.000016183241,0.000025599418,0.0011328364,0.001858245,0.0010819208,0.000093588875,0.0014429993,0.000017998322],"about_ca_topic_score_codex":0.99327046,"about_ca_topic_score_gemma":0.995611,"teacher_disagreement_score":0.013759697,"about_ca_system_score_codex":0.013759697,"about_ca_system_score_gemma":0.014135664,"threshold_uncertainty_score":0.099834025},"labels":[],"label_agreement":null},{"id":"W2012041811","doi":"10.1029/2011jb009095","title":"Split from slip and schist: Crustal anisotropy beneath northern Cascadia from non‐volcanic tremor","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismology; Seismogram; Phyllite; Anisotropy; Crust; Shear wave splitting; Schist; Clockwise; Azimuth; North American Plate; Thrust fault; Tectonics; Geophysics; Subduction; Geometry; Petrology; Metamorphic rock; Mantle (geology)","score_opus":0.03131892125593731,"score_gpt":0.2790335543655595,"score_spread":0.24771463310962216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012041811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99933654,0.000016678256,0.00005243671,0.0000150737,6.8685733e-7,0.0000012861539,0.000089118774,0.000007183867,0.00048088309],"genre_scores_gemma":[0.99974746,0.00001577759,0.000029402383,0.0000017259657,7.060008e-7,0.0000010152013,0.00012242247,0.000001689304,0.00007974595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987817,0.000010179581,0.0000108638615,0.000039103386,0.000034939647,0.00002678696],"domain_scores_gemma":[0.9997079,0.000047036767,0.000064921456,0.000033139153,0.000065681335,0.00008128264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001484204,0.00030789332,0.00022858926,0.0010261661,0.00054827094,0.000635846,0.0003133412,0.00032975985,0.001553397],"category_scores_gemma":[0.00082168495,0.00036301048,0.0002757012,0.00096495944,0.00046434914,0.000258078,0.0007341837,0.00022177727,0.00024087954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027400293,0.000040057188,0.94378793,0.000054710927,0.000087769404,0.0008107765,0.001535118,0.0038354169,0.04030275,0.0001381444,0.00015696656,0.008976456],"study_design_scores_gemma":[0.0000030649358,0.000007562314,0.9986908,0.0000022371323,0.0000088772995,0.00003442756,0.00014863639,0.0008340156,0.00020037832,0.000018430523,0.000047985744,0.0000037186446],"about_ca_topic_score_codex":0.07347177,"about_ca_topic_score_gemma":0.11975049,"teacher_disagreement_score":0.9265282,"about_ca_system_score_codex":0.00066375744,"about_ca_system_score_gemma":0.0005436474,"threshold_uncertainty_score":0.14608824},"labels":[],"label_agreement":null},{"id":"W2012247110","doi":"10.1785/gssrl.75.2.299","title":"The 16 March 1999 mN 5.1 Cote-Nord Earthquake: The Largest Earthquake Ever Recorded in the Lower St. Lawrence Seismic Zone, Canada","year":2004,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Intraplate earthquake; Foreshock; Aftershock; Tectonics","score_opus":0.0429031343526464,"score_gpt":0.2761972957555053,"score_spread":0.23329416140285889,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012247110","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0050657843,0.007259131,0.00025895092,0.004812526,0.0018317839,0.00026630893,0.5669264,0.0010193654,0.41255975],"genre_scores_gemma":[0.017081596,0.014154249,0.000592785,0.001221942,0.00039541037,0.0000817793,0.28009236,0.0006727642,0.68570703],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99950874,0.0000067599535,0.000017491297,0.000034890985,0.0003088743,0.00012330446],"domain_scores_gemma":[0.9987557,0.000023165698,0.00007539469,0.00003630285,0.0008882624,0.00022120649],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020285229,0.0009173231,0.0007987779,0.0040921993,0.003579758,0.003472106,0.0012198664,0.00092835433,0.19607204],"category_scores_gemma":[0.0017029486,0.00038120124,0.0006024945,0.012342591,0.000510308,0.0012946202,0.0017092794,0.0007914003,0.09231276],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023468363,0.000005108435,0.0016344935,0.00033702736,0.00000740871,0.000080155136,0.00009406667,0.000030496456,0.00008709449,0.0002643285,0.98300534,0.01443098],"study_design_scores_gemma":[0.000012272283,0.000007220285,0.018237013,0.0003455229,0.000014878836,0.000048854683,0.0005320144,0.000028217115,0.00012452337,0.000087669054,0.98054916,0.000012648138],"about_ca_topic_score_codex":0.9120223,"about_ca_topic_score_gemma":0.9755411,"teacher_disagreement_score":0.19607204,"about_ca_system_score_codex":0.009745745,"about_ca_system_score_gemma":0.023523908,"threshold_uncertainty_score":0.65592635},"labels":[],"label_agreement":null},{"id":"W2012474954","doi":"10.1029/2012eo330001","title":"The 2011 Virginia earthquake: What are scientists learning?","year":2012,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Induced seismicity; Seismology; Geology; Moment magnitude scale; San andreas fault; Magnitude (astronomy); Archaeology; Fault (geology); Geography","score_opus":0.014601783810627003,"score_gpt":0.2195642562369301,"score_spread":0.2049624724263031,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012474954","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013723914,0.13428402,0.00074535044,0.80688626,0.044987384,0.00005299496,0.0012863182,0.00026634312,0.010118955],"genre_scores_gemma":[0.015303594,0.34424356,0.0029840888,0.53405964,0.08191319,0.00024035876,0.0028711334,0.0002057973,0.018178616],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99506843,0.0015031353,0.000387606,0.0007378686,0.0014787127,0.0008241161],"domain_scores_gemma":[0.961985,0.009250952,0.0021393131,0.0015360025,0.013688805,0.011399975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0095517095,0.0016604128,0.0020396314,0.0034691754,0.003987007,0.013365305,0.0034147792,0.012587165,0.015178112],"category_scores_gemma":[0.055210307,0.0007672251,0.0010288444,0.0026795838,0.0043622954,0.016301721,0.005299305,0.017361503,0.0130267115],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000651783,0.00008815588,0.0021228425,0.0006919557,0.00003958319,0.000112133384,0.0004883368,0.00007978565,0.000051565097,0.0021912723,0.8269208,0.16714838],"study_design_scores_gemma":[0.000048709844,0.00011020295,0.0033811093,0.0050133476,0.00003849208,0.00015877173,0.003634543,0.00009923597,0.00010491739,0.01980691,0.9675202,0.00008356746],"about_ca_topic_score_codex":0.0108036045,"about_ca_topic_score_gemma":0.020589974,"teacher_disagreement_score":0.015178112,"about_ca_system_score_codex":0.004467345,"about_ca_system_score_gemma":0.014590673,"threshold_uncertainty_score":0.050775826},"labels":[],"label_agreement":null},{"id":"W2012504221","doi":"10.1016/j.jog.2008.03.003","title":"Using postglacial sea level, crustal velocities and gravity-rate-of-change to constrain the influence of thermal effects on mantle lateral heterogeneities","year":2008,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Post-glacial rebound; Geology; Mantle (geology); Geophysics; Lithosphere; Glacier; Geodesy; Glacial period; Tectonics; Geomorphology; Seismology","score_opus":0.06091266301636828,"score_gpt":0.25344724219172743,"score_spread":0.19253457917535916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012504221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998367,0.00006583138,0.0010194132,0.000013050976,0.0000027437877,0.000002008434,0.00013433545,0.000021594182,0.00037408367],"genre_scores_gemma":[0.9987858,0.000042433978,0.0008249366,0.000006111043,0.0000020666757,0.0000027287458,0.00023583391,0.00001213767,0.00008796767],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999835,0.000058654627,0.000010586228,0.000052503307,0.000015587959,0.000027626616],"domain_scores_gemma":[0.9991818,0.00047581695,0.00013605182,0.000088085515,0.000057411722,0.000060862676],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010233574,0.00059478456,0.0004395183,0.00086106226,0.0004443446,0.001131294,0.00038881093,0.00042819433,0.00082042837],"category_scores_gemma":[0.0020843341,0.0004196373,0.00069706456,0.0015507806,0.00032168793,0.00077674957,0.00037204634,0.000363263,0.00018296752],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010286646,0.00011516637,0.90438765,0.000058112877,0.0007222019,0.00013179381,0.00032361486,0.038080957,0.03269293,0.0005142021,0.00014616598,0.021798493],"study_design_scores_gemma":[0.00006601749,0.0001701483,0.8860798,0.000014461707,0.00048639756,0.00009501633,0.00018101174,0.10649927,0.005175584,0.0007254705,0.00046969816,0.00003698601],"about_ca_topic_score_codex":0.016755462,"about_ca_topic_score_gemma":0.034878183,"teacher_disagreement_score":0.016755462,"about_ca_system_score_codex":0.00040632416,"about_ca_system_score_gemma":0.0004933023,"threshold_uncertainty_score":0.033315897},"labels":[],"label_agreement":null},{"id":"W2012622165","doi":"10.1029/2008gl034415","title":"Characterizing an “uncharacteristic” ETS event in northern Cascadia","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Geology; Seismology; Episodic tremor and slip; Borehole; Slip (aerodynamics); Paleontology; Tectonics","score_opus":0.05274247804368247,"score_gpt":0.29322576233397835,"score_spread":0.24048328429029586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012622165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993967,0.000010140031,0.000093641305,0.0000160045,8.105594e-7,0.0000021644807,0.00009298109,0.000007399633,0.0003801192],"genre_scores_gemma":[0.9996176,0.000016122438,0.000062614265,0.0000027692363,0.00000150318,0.0000018695821,0.00019395986,0.0000017357721,0.00010175178],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998745,0.00001488203,0.000015334095,0.00004617615,0.000025922685,0.000023169896],"domain_scores_gemma":[0.99959177,0.000052389416,0.00010753003,0.00005849011,0.000074468466,0.000115374656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020222351,0.00023642124,0.00022277738,0.0007109955,0.00059480837,0.00034182874,0.0003319533,0.00030426498,0.00066215196],"category_scores_gemma":[0.0007724378,0.00018692295,0.00029808065,0.00068477175,0.00059502356,0.00027860916,0.0005081098,0.000191666,0.00010577052],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015822731,0.00004530816,0.9675878,0.000038339535,0.00005813867,0.0012363401,0.0010017178,0.010535965,0.013906521,0.00022251937,0.00021883378,0.0049902285],"study_design_scores_gemma":[0.000003731274,0.000017179189,0.99659306,0.0000017498005,0.000010525108,0.00007799821,0.00020040375,0.002627486,0.00024857136,0.000053971387,0.00015997935,0.0000053037766],"about_ca_topic_score_codex":0.084529154,"about_ca_topic_score_gemma":0.17425437,"teacher_disagreement_score":0.084529154,"about_ca_system_score_codex":0.0011807171,"about_ca_system_score_gemma":0.00053626567,"threshold_uncertainty_score":0.16807431},"labels":[],"label_agreement":null},{"id":"W2013669710","doi":"10.1139/e02-104","title":"Seismotectonic characteristics of the Lower St. Lawrence Seismic Zone, Quebec: insights from geology, magnetics, gravity, and seismics","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Montreal Police Service; Geological Survey of Canada","funders":"Polytechnique Montréal","keywords":"Precambrian; Geology; Basement; Seismology; Lineament; Fault (geology); Nappe; Shield; Sedimentary rock; Geomorphology; Geophysics; Tectonics; Paleontology","score_opus":0.011944179379351312,"score_gpt":0.18889653261877132,"score_spread":0.17695235323942002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013669710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9804441,0.0006534952,0.00032802302,0.0004811321,0.000009030484,0.000045007844,0.0061403606,0.000050079805,0.011848809],"genre_scores_gemma":[0.9918903,0.00025021873,0.00020474326,0.000061029317,0.0000054486723,0.000012755684,0.002437348,0.000009079948,0.0051289555],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998356,0.000010971031,0.0000081090575,0.00002547921,0.00006525975,0.00005451554],"domain_scores_gemma":[0.9991961,0.00004680181,0.000105645886,0.000013752322,0.0005080238,0.00012971388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018725672,0.00023208282,0.00016774036,0.0013281849,0.0009453768,0.00078151654,0.0005761747,0.00025208577,0.0040356563],"category_scores_gemma":[0.00081875623,0.000117538635,0.00009300454,0.002462385,0.0004212955,0.0002662633,0.0002861199,0.00020628101,0.00044243142],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000105151135,0.000056829882,0.95324224,0.00009775568,0.00004097912,0.000303963,0.001434083,0.0011657756,0.004169962,0.00038335178,0.0055388045,0.033461116],"study_design_scores_gemma":[0.0000045470197,0.000009355852,0.995887,0.000020304611,0.000007085529,0.000029741173,0.0005152645,0.0008117617,0.00009960559,0.000012228763,0.0025966058,0.000006531175],"about_ca_topic_score_codex":0.9946583,"about_ca_topic_score_gemma":0.9984047,"teacher_disagreement_score":0.01325421,"about_ca_system_score_codex":0.01325421,"about_ca_system_score_gemma":0.0056856913,"threshold_uncertainty_score":0.09616649},"labels":[],"label_agreement":null},{"id":"W201401052","doi":"","title":"The Junction of Hellenic and Cyprus Arcs: the Bey Daglari Lineament, Offshore Termination of the Antalya Basin","year":2009,"lang":"en","type":"article","venue":"EGUGA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Transtension; Geology; Forearc; Transpression; Subduction; Lineament; Structural basin; Seismology; Quaternary; Paleontology; Submarine pipeline; Mediterranean climate; Tectonics; Archaeology; Geography; Oceanography; Sinistral and dextral","score_opus":0.00873163340977616,"score_gpt":0.202732663713652,"score_spread":0.19400103030387583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W201401052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98070574,0.00035472377,0.000084209125,0.000110646804,0.00000752396,0.000014607557,0.00012992027,0.000009481363,0.018583125],"genre_scores_gemma":[0.99735993,0.00017409663,0.00024681594,0.000024764196,0.0000047459775,0.0000078031835,0.00013593488,0.0000042541287,0.0020416656],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999025,0.000011181913,0.000008573077,0.000032227028,0.000022481532,0.000023028058],"domain_scores_gemma":[0.999918,0.000008169621,0.00003002206,0.0000055722926,0.000020630063,0.000017662462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009252827,0.00010498975,0.000102114864,0.0005090277,0.00070248666,0.00089241145,0.00014856241,0.00022234174,0.001674597],"category_scores_gemma":[0.00031595878,0.00010771543,0.000060657363,0.0005823602,0.0005747257,0.00028153142,0.00064617035,0.00014980926,0.00028397513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006984749,0.00012858496,0.8193033,0.00027340619,0.00009208976,0.006459131,0.007892962,0.0015964146,0.026312457,0.015631631,0.0039949664,0.117616594],"study_design_scores_gemma":[0.0000148205,0.000030919757,0.98298234,0.000034520333,0.000015811223,0.0010685686,0.001469103,0.00026339453,0.0007335242,0.00021548108,0.013165339,0.0000062508993],"about_ca_topic_score_codex":0.022461785,"about_ca_topic_score_gemma":0.04766925,"teacher_disagreement_score":0.022461785,"about_ca_system_score_codex":0.00070134015,"about_ca_system_score_gemma":0.0009901772,"threshold_uncertainty_score":0.04466206},"labels":[],"label_agreement":null},{"id":"W2014164118","doi":"10.1144/sp290.14","title":"Transpressional structures on a Late Palaeozoic intracontinental transform fault, Canadian Appalachians","year":2007,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Saint Mary's University; University of Alberta","funders":"","keywords":"Paleozoic; Geology; Paleontology; Fault (geology); Transform fault; Transpression; Sinistral and dextral","score_opus":0.01430836043909961,"score_gpt":0.22577699764437278,"score_spread":0.21146863720527317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014164118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99118876,0.00030996054,0.000079606114,0.000051698873,0.0000027857245,0.000011201125,0.00081681943,0.000015641283,0.0075234263],"genre_scores_gemma":[0.99725455,0.00017182944,0.00015007213,0.000007722159,0.0000013079901,0.0000040528207,0.00043707853,0.0000036156532,0.0019697628],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998765,0.0000027754877,0.00000503124,0.000024862224,0.00004876806,0.000042038813],"domain_scores_gemma":[0.99956983,0.00001470585,0.0000341397,0.000008800243,0.00032984337,0.000042601187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007591577,0.00028389393,0.000165502,0.002590362,0.0021673692,0.00087264105,0.00038169723,0.00020689657,0.0028572988],"category_scores_gemma":[0.000374244,0.00014042815,0.00012279314,0.0035020472,0.0006086424,0.00019491142,0.00043567896,0.00021160916,0.00026560482],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021941937,0.000036893325,0.89568466,0.00012751385,0.000050075392,0.0009934506,0.0056266766,0.0011873991,0.02231472,0.0010455083,0.0015695416,0.071144216],"study_design_scores_gemma":[0.0000011172201,0.000005720715,0.99765694,0.000006893817,0.0000041397648,0.000051387156,0.00062363775,0.00013326564,0.00020476054,0.000017347556,0.0012908563,0.000003838341],"about_ca_topic_score_codex":0.9834374,"about_ca_topic_score_gemma":0.99365836,"teacher_disagreement_score":0.016562581,"about_ca_system_score_codex":0.008704839,"about_ca_system_score_gemma":0.0053472593,"threshold_uncertainty_score":0.06315833},"labels":[],"label_agreement":null},{"id":"W2014779525","doi":"10.1029/2005jb003676","title":"Coseismic deformation of the 2002 Denali Fault earthquake: Insights from GPS measurements","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Slip (aerodynamics); Seismology; Geodesy; Thrust fault; Fault (geology); Episodic tremor and slip; Seismic moment; Tectonics; Subduction","score_opus":0.04416025606914581,"score_gpt":0.27480225181376544,"score_spread":0.23064199574461963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014779525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974172,0.000062282976,0.00017488976,0.000033473323,0.0000027072272,0.0000044487415,0.00089337776,0.00001653755,0.0013951231],"genre_scores_gemma":[0.9980008,0.000080337035,0.00028204735,0.000007230547,0.0000032466883,0.000004036894,0.0013255783,0.0000044433586,0.000292349],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998516,0.000020606158,0.000012694602,0.00004549,0.000042759828,0.000026700705],"domain_scores_gemma":[0.99968195,0.000042896827,0.00009313989,0.00003887851,0.00010806911,0.000035009594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001775942,0.0002677349,0.00020113721,0.00095470255,0.00033216982,0.000529696,0.00027846656,0.00037135463,0.00061995274],"category_scores_gemma":[0.0010276067,0.00017988353,0.00013572848,0.001483283,0.00020529405,0.00036831514,0.00031013796,0.00018559345,0.00027618845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003976417,0.000033220214,0.98513633,0.000015810247,0.000022589626,0.00011049143,0.00048126513,0.0040665306,0.0017840919,0.00011692668,0.00037870702,0.0078142565],"study_design_scores_gemma":[0.000002724345,0.000015597203,0.9924522,0.000006263911,0.000010471067,0.00003599805,0.00042948694,0.0056839855,0.000370706,0.000035341403,0.0009497045,0.000007502213],"about_ca_topic_score_codex":0.21831484,"about_ca_topic_score_gemma":0.35262194,"teacher_disagreement_score":0.21831484,"about_ca_system_score_codex":0.00082256773,"about_ca_system_score_gemma":0.00049629627,"threshold_uncertainty_score":0.43408817},"labels":[],"label_agreement":null},{"id":"W2014976630","doi":"10.2118/138806-ms","title":"Surface Microseismic Mapping Reveals Details of the Marcellus Shale","year":2010,"lang":"en","type":"article","venue":"SPE Eastern Regional Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Microsemi (Canada)","funders":"","keywords":"Microseism; Geology; Geophone; Seismology; Hydraulic fracturing; Fault (geology); Slip (aerodynamics); Fracture (geology); Petrology; Geotechnical engineering","score_opus":0.026564683477195494,"score_gpt":0.21706208362510615,"score_spread":0.19049740014791067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014976630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987808,0.000019727097,0.00028152764,0.000006014985,6.6979015e-7,0.0000024164208,0.00008114455,0.000010340662,0.0008173194],"genre_scores_gemma":[0.99946195,0.000006310638,0.00020525821,0.0000014214226,9.2838565e-7,0.0000013753717,0.00005389327,0.0000012732355,0.00026760812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995875,0.0000021348117,0.0000013798137,0.000012575604,0.000012129196,0.000012899056],"domain_scores_gemma":[0.999933,0.000006118599,0.000017531425,0.0000049087066,0.000020669167,0.000017874441],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000041304622,0.00009640273,0.000093103925,0.00056842173,0.00014784228,0.00018781032,0.00008023661,0.00013640628,0.0007190282],"category_scores_gemma":[0.00011451646,0.000067113106,0.000056243556,0.00023234655,0.00013181982,0.000090010646,0.00018670956,0.000078652556,0.000117146774],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026451595,0.00006123881,0.63183117,0.000040330346,0.000031858934,0.00057143543,0.00078310585,0.0055033597,0.31584448,0.0003457438,0.00039938072,0.044323355],"study_design_scores_gemma":[0.0000017574891,0.00003781173,0.9938751,0.0000025412057,0.0000030595725,0.000044950826,0.00011913971,0.0027291267,0.0028252176,0.000023340317,0.00033561708,0.0000023292077],"about_ca_topic_score_codex":0.009785377,"about_ca_topic_score_gemma":0.025930827,"teacher_disagreement_score":0.009785377,"about_ca_system_score_codex":0.00017249539,"about_ca_system_score_gemma":0.00013658823,"threshold_uncertainty_score":0.019456863},"labels":[],"label_agreement":null},{"id":"W2015357485","doi":"10.1139/e06-002","title":"Structural variation along the Devil's Mountain fault zone, northwestern Washington","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"U.S. Geological Survey","keywords":"Geology; Seismology; Fault (geology); Transform fault; Quaternary; Fault scarp; Subduction; Strike-slip tectonics; Paleontology; Tectonics","score_opus":0.015448176634433368,"score_gpt":0.2059066781550438,"score_spread":0.19045850152061042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015357485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99886453,0.000036127924,0.000014933414,0.000010559788,0.0000010152339,0.0000017940214,0.00012406184,0.0000024623373,0.0009444673],"genre_scores_gemma":[0.9991837,0.000046464487,0.000055396864,0.0000040993327,0.0000010422604,0.000002253813,0.0002567478,7.795769e-7,0.0004494343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994886,0.0000036969195,0.000004343765,0.000021010816,0.000011126752,0.000011056938],"domain_scores_gemma":[0.9999021,0.000009960952,0.00003089825,0.000007795279,0.000028839719,0.000020424013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008699714,0.00012031165,0.000103585786,0.000753271,0.00038758398,0.00046987704,0.00012133276,0.00012172445,0.000623865],"category_scores_gemma":[0.00021900728,0.000073263574,0.00005746733,0.0006508401,0.00026490656,0.00009456734,0.00025984854,0.00009952159,0.00008710081],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048383856,0.000023973658,0.983284,0.000015595126,0.000034518813,0.00025995765,0.0009226364,0.00025356043,0.0053421706,0.00016007236,0.0002364054,0.009418825],"study_design_scores_gemma":[0.0000016309805,0.000009159618,0.9986468,0.000005098805,0.0000034119507,0.000051844887,0.00049208367,0.00007651925,0.00010928041,0.000011558851,0.00059152645,0.0000011537633],"about_ca_topic_score_codex":0.08910413,"about_ca_topic_score_gemma":0.29502943,"teacher_disagreement_score":0.08910413,"about_ca_system_score_codex":0.0006367025,"about_ca_system_score_gemma":0.00034076054,"threshold_uncertainty_score":0.17717093},"labels":[],"label_agreement":null},{"id":"W2016454065","doi":"10.1016/s0191-8141(01)00159-6","title":"Chemical changes and the development of quartz preferred orientation in zones of crenulation cleavage, Anglesey","year":2002,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Crenulation; Cleavage (geology); Quartz; Muscovite; Geology; Mineralogy; Pressure solution; Crystallography; Chemistry; Tectonics; Seismology","score_opus":0.026153573947962604,"score_gpt":0.2309238000007822,"score_spread":0.20477022605281958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016454065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995956,0.000057420053,0.00001774563,0.0000035308176,5.96786e-7,0.0000010855629,0.000042572796,4.4352544e-7,0.00028107135],"genre_scores_gemma":[0.9996107,0.000043805143,0.000026742713,0.0000031554594,6.5317164e-7,0.0000011399275,0.000058428443,6.604067e-7,0.00025479886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994254,0.000006740827,0.000004654634,0.000018279188,0.000009327045,0.000018536186],"domain_scores_gemma":[0.99975914,0.00003848163,0.00008482974,0.0000067357023,0.00005996743,0.000050873998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012869945,0.000099770536,0.00010986462,0.0008341216,0.0003935975,0.00068817864,0.00016367556,0.00021993325,0.001331173],"category_scores_gemma":[0.000416353,0.00018803736,0.00007838928,0.0005637847,0.00049590995,0.00023646386,0.00025878567,0.00016476557,0.00011910522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015130001,0.000046510442,0.9058423,0.00003498266,0.000041646188,0.00035293313,0.001067123,0.00023989692,0.08453718,0.0002775985,0.000049485796,0.0059973546],"study_design_scores_gemma":[0.0000024330109,0.000022901919,0.998604,9.252669e-7,0.000002634008,0.000046873745,0.000236897,0.000041361756,0.00093847816,0.000014245982,0.00008837037,9.4122703e-7],"about_ca_topic_score_codex":0.03344118,"about_ca_topic_score_gemma":0.058471188,"teacher_disagreement_score":0.03344118,"about_ca_system_score_codex":0.000518777,"about_ca_system_score_gemma":0.00028275888,"threshold_uncertainty_score":0.066493094},"labels":[],"label_agreement":null},{"id":"W2016614338","doi":"10.1002/2013gc005144","title":"Relationship between the Cascadia fore-arc mantle wedge, nonvolcanic tremor, and the downdip limit of seismogenic rupture","year":2014,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Mantle (geology); North American Plate; Plate tectonics; Slip (aerodynamics); Mantle wedge; Episodic tremor and slip; Wedge (geometry); Geophysics; Tectonics","score_opus":0.013536849385261068,"score_gpt":0.1969697762308964,"score_spread":0.18343292684563534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016614338","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99833846,0.000048289556,0.00009628534,0.000017355798,4.9870965e-7,0.0000012046105,0.00013592234,0.000008135973,0.0013538526],"genre_scores_gemma":[0.9996258,0.00002458884,0.000041531417,0.000002980562,5.9225795e-7,0.0000012262944,0.0001371492,0.0000020237853,0.0001640483],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992144,0.0000075784733,0.0000055703886,0.000031777596,0.000015660236,0.000017967806],"domain_scores_gemma":[0.9993567,0.00012769805,0.00023947083,0.000048609993,0.000096655735,0.00013089945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000098969096,0.0002013026,0.0001415248,0.0007353079,0.00032523673,0.0005905998,0.00019181005,0.00020138612,0.0016038159],"category_scores_gemma":[0.00090079766,0.00017866542,0.000097121236,0.0005644573,0.00031568028,0.00021696235,0.0004306045,0.00025731415,0.00016809118],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006421078,0.000010121132,0.98851645,0.00000965976,0.000024439742,0.000103722254,0.00016657471,0.0006716262,0.0082964385,0.00012693816,0.000050147093,0.0019595653],"study_design_scores_gemma":[8.969124e-7,0.0000044295098,0.9992291,0.0000014826998,0.000003514117,0.000023826748,0.00008785662,0.00030729026,0.00022686942,0.000034582517,0.000078635065,0.0000015028165],"about_ca_topic_score_codex":0.041878536,"about_ca_topic_score_gemma":0.09025289,"teacher_disagreement_score":0.041878536,"about_ca_system_score_codex":0.0005742156,"about_ca_system_score_gemma":0.00031175063,"threshold_uncertainty_score":0.08326954},"labels":[],"label_agreement":null},{"id":"W2016909981","doi":"10.1785/0120140165","title":"Source Characteristics of the 2012 Haida Gwaii Earthquake Sequence","year":2015,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Sequence (biology); Geology; Seismology; Biology","score_opus":0.0324004553176049,"score_gpt":0.22145711396068116,"score_spread":0.18905665864307625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016909981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99175984,0.000082225255,0.0001840028,0.000024423218,0.000012508348,0.00005829064,0.005316674,0.000027085134,0.002535049],"genre_scores_gemma":[0.99014014,0.00010898584,0.00035718997,0.00001032851,0.000023767843,0.00006388838,0.008074912,0.00001187337,0.0012088533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999038,0.000005420475,0.000014273479,0.0000243623,0.000028598583,0.000023501076],"domain_scores_gemma":[0.9994234,0.00003312764,0.00024252642,0.000024970095,0.00012785243,0.00014813062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000086790234,0.00040331428,0.00027207262,0.0020594294,0.00036121297,0.0003067144,0.000195401,0.00021725029,0.002585445],"category_scores_gemma":[0.0005510684,0.00016227821,0.0001233881,0.0025043862,0.00016397971,0.00021396833,0.00042435175,0.00016811039,0.0006588538],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031236952,0.00008779785,0.9494173,0.00019249594,0.000067926885,0.0012236487,0.0009072682,0.001102548,0.019538976,0.00015964896,0.003416621,0.023573413],"study_design_scores_gemma":[0.000002152369,0.000016750962,0.99883455,0.0000038002133,0.000006051143,0.00009988438,0.00010911598,0.00023516356,0.00019095722,0.00000665448,0.0004912278,0.0000036822182],"about_ca_topic_score_codex":0.01799417,"about_ca_topic_score_gemma":0.047405574,"teacher_disagreement_score":0.98200583,"about_ca_system_score_codex":0.00030499866,"about_ca_system_score_gemma":0.00036787527,"threshold_uncertainty_score":0.03577888},"labels":[],"label_agreement":null},{"id":"W2016982547","doi":"10.1038/nature01840","title":"Reflection signature of seismic and aseismic slip on the northern Cascadia subduction interface","year":2003,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":116,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Lamont-Doherty Earth Observatory, Columbia University","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Episodic tremor and slip; Reflection (computer programming); Thrust; Thrust fault; Deformation (meteorology); Tectonics","score_opus":0.01129863837769753,"score_gpt":0.22708376012609932,"score_spread":0.21578512174840178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016982547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99707675,0.000018769993,0.000110884954,0.000033523258,0.000002880696,0.0000020288883,0.00020793428,0.000031569136,0.0025156846],"genre_scores_gemma":[0.9991186,0.00001537171,0.00006591148,0.0000058630344,0.000003134637,0.0000020908483,0.00018959123,0.000007603672,0.000591885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999946,0.000003923939,0.000002828532,0.00001901345,0.000012842869,0.00001535549],"domain_scores_gemma":[0.99980396,0.00003044429,0.000043465272,0.000017347691,0.00005925562,0.00004548792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011043128,0.00021921536,0.00019897547,0.0006044054,0.00027284908,0.00033774896,0.00031947333,0.00033670026,0.0030684597],"category_scores_gemma":[0.0005163663,0.00021293729,0.00012677861,0.00057471363,0.00028518683,0.00018458592,0.00045537017,0.00029096837,0.00045607242],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024062223,0.0001774029,0.6069732,0.00012647292,0.00007250639,0.0012769988,0.0025669087,0.004391304,0.3544469,0.0007286005,0.0017014006,0.025132153],"study_design_scores_gemma":[0.000014668034,0.000033507906,0.9969747,0.0000030354358,0.000011377681,0.0000735207,0.00019211322,0.0010050728,0.0014065522,0.000030806197,0.00025092828,0.0000038307153],"about_ca_topic_score_codex":0.01601581,"about_ca_topic_score_gemma":0.016781792,"teacher_disagreement_score":0.01601581,"about_ca_system_score_codex":0.00032174558,"about_ca_system_score_gemma":0.0002653803,"threshold_uncertainty_score":0.031845152},"labels":[],"label_agreement":null},{"id":"W2017259013","doi":"10.1029/2008gl034586","title":"Rheological stratification of the lithosphere: A direct inference based upon the geodetically observed pattern of the glacial isostatic adjustment of the North American continent","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Post-glacial rebound; Geology; Lithosphere; Glacial period; Stratification (seeds); Deglaciation; Ice sheet; Rheology; Last Glacial Maximum; Geodesy; Geophysics; Climatology; Paleontology; Geomorphology; Tectonics","score_opus":0.05862973166974873,"score_gpt":0.272594135574942,"score_spread":0.21396440390519328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017259013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9753493,0.0032851659,0.0131173935,0.0006579248,0.000025585116,0.000010106239,0.00012281886,0.00009474636,0.007336959],"genre_scores_gemma":[0.9963755,0.0012009713,0.001949603,0.00003847543,0.000020881915,0.0000025101888,0.00008590045,0.0000063978746,0.00031969993],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.000013358125,0.0000027384337,0.000014532309,0.000010014959,0.0000058888],"domain_scores_gemma":[0.99980325,0.000051092025,0.00006511491,0.000034227385,0.00002956365,0.000016771843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030300114,0.00015847823,0.00009413673,0.00060888584,0.00020742316,0.0008635004,0.0002757091,0.0001846081,0.0005770169],"category_scores_gemma":[0.00092946243,0.0000980074,0.00011700644,0.00042411918,0.0013450147,0.0007302441,0.00048685068,0.00033145174,0.00014842139],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003034321,0.00005971053,0.78037524,0.00027052723,0.000100821555,0.0006879808,0.0016624687,0.014858448,0.022900345,0.030098446,0.0015449519,0.14713758],"study_design_scores_gemma":[0.000024942756,0.00017714268,0.8733271,0.00011203552,0.00013232698,0.0007824156,0.0014608391,0.073610865,0.00742666,0.030629102,0.0122592375,0.000057361034],"about_ca_topic_score_codex":0.008335451,"about_ca_topic_score_gemma":0.014260402,"teacher_disagreement_score":0.008335451,"about_ca_system_score_codex":0.00048813623,"about_ca_system_score_gemma":0.0004289903,"threshold_uncertainty_score":0.016573846},"labels":[],"label_agreement":null},{"id":"W2017584111","doi":"10.1029/2010jb007993","title":"Seismic variability of subduction thrust faults: Insights from laboratory models","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Thrust; Thrust fault; Geophysics; Fault (geology); Tectonics; Aerospace engineering","score_opus":0.05620752323744456,"score_gpt":0.2774957474956375,"score_spread":0.22128822425819294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017584111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927469,0.00010527628,0.005349456,0.000067487555,0.0000051810694,0.000012251486,0.00059154746,0.00011614767,0.0010057339],"genre_scores_gemma":[0.99907947,0.000054033437,0.00047924556,0.00000416387,0.0000038555804,0.000011750444,0.0002885536,0.000006800817,0.000072141556],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991333,0.00002582617,0.000007660924,0.000026391966,0.000013243152,0.000013583555],"domain_scores_gemma":[0.9996511,0.00013715122,0.00008413378,0.000068451955,0.000031506508,0.000027778768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030713665,0.00036577357,0.00037792296,0.00029266687,0.00012971392,0.0005204647,0.0008236945,0.0005145349,0.000599084],"category_scores_gemma":[0.0008697133,0.00016119682,0.00041703164,0.00030250812,0.00041722786,0.00044503895,0.00037555475,0.00033578568,0.00007643551],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004897987,0.000359844,0.04945615,0.00012841565,0.00016699036,0.00025595436,0.0001247498,0.9064524,0.031238386,0.004402137,0.0007226533,0.0062024244],"study_design_scores_gemma":[0.000048994105,0.00018359785,0.01653365,0.0000070607875,0.00003673088,0.000035988098,0.000040814557,0.9787321,0.0030336,0.0010143995,0.0003098425,0.000023297123],"about_ca_topic_score_codex":0.0031831553,"about_ca_topic_score_gemma":0.0016959711,"teacher_disagreement_score":0.0031831553,"about_ca_system_score_codex":0.00044314368,"about_ca_system_score_gemma":0.00018504712,"threshold_uncertainty_score":0.0063292384},"labels":[],"label_agreement":null},{"id":"W2017662684","doi":"10.1126/science.1060152","title":"A Silent Slip Event on the Deeper Cascadia Subduction Interface","year":2001,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":973,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Seismology; Geology; Episodic tremor and slip; Slip (aerodynamics); Moment magnitude scale; Induced seismicity; Submarine pipeline; Tectonics; Geotechnical engineering; Geometry","score_opus":0.02297107146818559,"score_gpt":0.2453797626681505,"score_spread":0.22240869119996493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017662684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998973,0.000045037756,0.00006773307,0.000031792115,0.000003853314,0.0000038845433,0.00016659735,0.000010078217,0.0006981258],"genre_scores_gemma":[0.999298,0.000039034625,0.000042139367,0.000012582573,0.0000043212394,0.0000026850973,0.00031076765,0.0000011366274,0.00028950543],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983144,0.000011660435,0.000010837173,0.00004238557,0.000059835,0.000043818116],"domain_scores_gemma":[0.99919766,0.000067652945,0.00023272572,0.00006778947,0.00020697298,0.00022718076],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001680253,0.00020851119,0.00020000449,0.0007051482,0.0008441412,0.00032691506,0.00036546384,0.0002734251,0.00097010407],"category_scores_gemma":[0.0009822774,0.000110025765,0.000121805606,0.0006646433,0.00074190384,0.00023745996,0.00072008726,0.0002927774,0.00014270919],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024939846,0.000054358552,0.9667108,0.00006740719,0.000052962278,0.00091375137,0.002516038,0.00034140388,0.014019456,0.00020778408,0.00081480574,0.014051909],"study_design_scores_gemma":[0.0000033161602,0.000023874007,0.999003,0.0000026786252,0.0000061491187,0.000068630405,0.00028098616,0.000073349824,0.0002744219,0.000025510635,0.00023547008,0.0000027379997],"about_ca_topic_score_codex":0.096852764,"about_ca_topic_score_gemma":0.22687346,"teacher_disagreement_score":0.9031472,"about_ca_system_score_codex":0.001362276,"about_ca_system_score_gemma":0.00079089106,"threshold_uncertainty_score":0.19257808},"labels":[],"label_agreement":null},{"id":"W2017809288","doi":"10.1029/2000jb900414","title":"Limited syntectonic fluid flow in carbonate‐hosted thrust faults of the Front Ranges, Canadian Rockies, inferred from stable isotope data and structures","year":2001,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Fault (geology); Thrust fault; Carbonate; Carbonate rock; Petrology; Front (military); Thrust; Geochemistry; Brittleness; Fluid dynamics; Sedimentary rock; Seismology","score_opus":0.04396997620208203,"score_gpt":0.2770456992508887,"score_spread":0.23307572304880664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017809288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99777573,0.00024117713,0.00007304442,0.000019851266,0.0000010363345,0.000008286011,0.00058662216,0.0000062077875,0.0012880192],"genre_scores_gemma":[0.99844116,0.00016995556,0.0002544973,0.00001295408,9.794795e-7,0.0000040324103,0.00050551404,0.000003916906,0.00060698716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999724,0.0000044024273,0.000009679841,0.000059363603,0.00012233404,0.00008036316],"domain_scores_gemma":[0.99966574,0.000016635562,0.00006337605,0.00000899548,0.00019604462,0.000049237904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011734847,0.0003056635,0.00026426357,0.0021672496,0.0021687907,0.0009935673,0.0005163129,0.0002821422,0.0011292406],"category_scores_gemma":[0.00055900903,0.00037235412,0.00016054705,0.0021530832,0.000851424,0.00035398488,0.00045875373,0.00017046838,0.00011809079],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002789908,0.000035742025,0.8907232,0.0001804455,0.00008280596,0.00041497574,0.003921232,0.0005305718,0.07623092,0.0003655297,0.0004910236,0.026744548],"study_design_scores_gemma":[0.0000023869272,0.000007903102,0.99807703,0.000004698303,0.000009239548,0.000070465525,0.00038025953,0.00013341103,0.0007915099,0.000012221168,0.00050662045,0.0000042913466],"about_ca_topic_score_codex":0.9740625,"about_ca_topic_score_gemma":0.9935446,"teacher_disagreement_score":0.025937498,"about_ca_system_score_codex":0.008470525,"about_ca_system_score_gemma":0.0073990244,"threshold_uncertainty_score":0.06145823},"labels":[],"label_agreement":null},{"id":"W2017881067","doi":"10.1029/2001gl012959","title":"Wide‐angle reflectivity across the Torngat Orogen, NE Canada","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Transect; Reflection (computer programming); Reflectivity; Seismology; Refraction; Optics; Oceanography","score_opus":0.04834963795337511,"score_gpt":0.3119233835186255,"score_spread":0.2635737455652504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017881067","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9678518,0.0008950118,0.00042056074,0.00034591547,0.000012883402,0.00005619141,0.008535252,0.00006794027,0.021814404],"genre_scores_gemma":[0.9822253,0.0008581454,0.0009132215,0.00010788105,0.0000037339287,0.000020599358,0.003949143,0.000030025156,0.011891773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997154,0.00001074751,0.00000735118,0.000040844818,0.00010077578,0.00012472938],"domain_scores_gemma":[0.9996779,0.000010229252,0.00002617138,0.000008023674,0.00022128283,0.000056297227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013381791,0.000252891,0.00019397183,0.0009272171,0.0014331288,0.0007471186,0.00045619544,0.00016158061,0.0025609597],"category_scores_gemma":[0.00037035445,0.00021641856,0.00012810086,0.0020385678,0.00034044086,0.00017295622,0.0004341361,0.00022663458,0.00040589503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059871806,0.00006782485,0.8618299,0.00032340584,0.00023341033,0.0016472578,0.004936957,0.0028611484,0.02070908,0.0017079083,0.017480599,0.08760384],"study_design_scores_gemma":[0.00001551865,0.000017380164,0.9805024,0.000047317233,0.00003711281,0.00020326265,0.0021451213,0.00080836186,0.0011729845,0.000048967613,0.014980797,0.000020743091],"about_ca_topic_score_codex":0.99326706,"about_ca_topic_score_gemma":0.9983536,"teacher_disagreement_score":0.012288163,"about_ca_system_score_codex":0.012288163,"about_ca_system_score_gemma":0.018375287,"threshold_uncertainty_score":0.08915734},"labels":[],"label_agreement":null},{"id":"W2018251025","doi":"10.1029/2012jb009227","title":"Impact of inconsistent density scaling on physical analogue models of continental margin scale salt tectonics","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Diapir; Geology; Buoyancy; Sediment; Scaling; Tectonics; Mechanics; Geomorphology; Geometry; Physics; Paleontology","score_opus":0.0500397256718086,"score_gpt":0.32441665554645727,"score_spread":0.2743769298746487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018251025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97113657,0.00012475453,0.024271589,0.00022002759,0.000025258676,0.00006768971,0.00013983523,0.00010170746,0.003912581],"genre_scores_gemma":[0.99596316,0.000060345385,0.003605287,0.000023767745,0.0000066394327,0.00003251514,0.000031953514,0.000017767517,0.0002585858],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99965036,0.00015999535,0.00003306641,0.000055198765,0.00007197738,0.000029506684],"domain_scores_gemma":[0.998329,0.0008311128,0.00029022104,0.00036971984,0.00011893009,0.000060987637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010550568,0.00040843192,0.00038249677,0.00035675953,0.00027719245,0.0009777634,0.00079759327,0.000577221,0.0008120291],"category_scores_gemma":[0.0056612105,0.00035494356,0.00043648,0.00020377505,0.0017438194,0.0008409362,0.0008263718,0.0005567773,0.00007507254],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060211896,0.000045763434,0.008116356,0.000030188277,0.00001766213,0.000087250846,0.00007071417,0.97927916,0.0047951783,0.005295172,0.000054517455,0.0021478797],"study_design_scores_gemma":[0.000014479699,0.000030067482,0.0024683746,0.0000035492862,0.000005219805,0.000017167016,0.000014302969,0.99491775,0.0007277476,0.0016696617,0.00012412346,0.000007655813],"about_ca_topic_score_codex":0.005980996,"about_ca_topic_score_gemma":0.00266934,"teacher_disagreement_score":0.005980996,"about_ca_system_score_codex":0.0008875203,"about_ca_system_score_gemma":0.0003620621,"threshold_uncertainty_score":0.011892378},"labels":[],"label_agreement":null},{"id":"W2018330650","doi":"10.1029/2002jb001823","title":"Crustal structure beneath the Strait of Juan de Fuca and southern Vancouver Island from seismic and gravity analyses","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Geology; Seismology; Terrane; Induced seismicity; Crust; Volcano; Mantle (geology); Slab; Oceanic crust; Subduction; Geophysics; Tectonics","score_opus":0.03378717875625079,"score_gpt":0.3020188812476873,"score_spread":0.26823170249143646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018330650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949885,0.0001725911,0.00004976989,0.000021736221,0.0000016391149,0.000011012681,0.0007432713,0.000007886547,0.0040034833],"genre_scores_gemma":[0.9961361,0.0002573,0.0002835417,0.000009030645,0.0000010100016,0.000009493758,0.0013381764,0.0000032308833,0.0019619318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990654,0.0000049016776,0.0000058447827,0.000018408875,0.000034746576,0.000029496716],"domain_scores_gemma":[0.99982256,0.000010833853,0.00002670497,0.000008148643,0.0000852503,0.000046539088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011278124,0.00026638134,0.00014621166,0.0013076022,0.000773375,0.0009473988,0.0002865247,0.00020016189,0.001378268],"category_scores_gemma":[0.00043871967,0.00020565238,0.00017492787,0.0013277024,0.00024261097,0.00012811444,0.00066622114,0.00018650031,0.00020150309],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060693743,0.000019812873,0.9711774,0.00004824891,0.000070353955,0.00036402044,0.000893754,0.0020499364,0.0038214703,0.00025716992,0.0005750115,0.02066207],"study_design_scores_gemma":[0.0000035829248,0.000004588237,0.9969572,0.000018111336,0.000008765975,0.00005266838,0.00066546,0.00084824057,0.000088599845,0.000029040284,0.0013193057,0.000004496322],"about_ca_topic_score_codex":0.8971907,"about_ca_topic_score_gemma":0.96703243,"teacher_disagreement_score":0.10280931,"about_ca_system_score_codex":0.0034054061,"about_ca_system_score_gemma":0.0025079718,"threshold_uncertainty_score":0.20682949},"labels":[],"label_agreement":null},{"id":"W2018717053","doi":"10.2113/econgeo.107.1.147","title":"Tectonic Deformation and Fluid Flow: Implications for the Formation of Unconformity-Related Uranium Deposits","year":2012,"lang":"en","type":"article","venue":"Economic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Unconformity; Geology; Uranium ore; Tectonics; Uranium; Deformation (meteorology); Geochemistry; Flow (mathematics); Petrology; Geometry; Paleontology; Metallurgy; Materials science","score_opus":0.013963165885968066,"score_gpt":0.209452678357496,"score_spread":0.19548951247152793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018717053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982558,0.000028473218,0.00091963576,0.000042273397,0.000001786134,0.000006369595,0.000057466325,0.000016671376,0.00067148113],"genre_scores_gemma":[0.99946517,0.000022127593,0.0004083325,0.000004674328,5.482134e-7,0.000004386621,0.000027503931,0.0000020906964,0.00006515817],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99990404,0.000027556816,0.0000072721973,0.000021710564,0.000012138542,0.000027211623],"domain_scores_gemma":[0.9998147,0.00006647002,0.000048649894,0.000020156389,0.000017297953,0.00003278614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024011619,0.00039829224,0.0003598138,0.00051697815,0.0004880048,0.0007466659,0.00057420135,0.0006662993,0.0009736912],"category_scores_gemma":[0.001249663,0.0002631184,0.00039353076,0.00050795503,0.0010184597,0.00062854314,0.00058769004,0.0002509462,0.000059339684],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000115609386,0.000090477646,0.07219128,0.000039884137,0.00002891569,0.0002562938,0.0001266871,0.91132694,0.010756225,0.0029168716,0.000042196323,0.0021086375],"study_design_scores_gemma":[0.00005756332,0.00007898714,0.030447256,0.000010780752,0.00001728417,0.000049577462,0.00017867087,0.96521133,0.0023798998,0.0013642017,0.0001832269,0.000021227295],"about_ca_topic_score_codex":0.025111139,"about_ca_topic_score_gemma":0.011629244,"teacher_disagreement_score":0.025111139,"about_ca_system_score_codex":0.0015918579,"about_ca_system_score_gemma":0.0007965435,"threshold_uncertainty_score":0.049929976},"labels":[],"label_agreement":null},{"id":"W2019115883","doi":"10.1029/2011jb008247","title":"Thermal control of the seismogenic zone of southern central Chile","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Bundesministerium für Bildung und Forschung","keywords":"Geology; Subduction; Seismology; Seafloor spreading; Borehole; Advection; Mantle wedge; Mantle (geology); Heat flow; Thermal; Geophysics; Tectonics; Geotechnical engineering","score_opus":0.03342934781636627,"score_gpt":0.2513669558731542,"score_spread":0.21793760805678794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019115883","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99398106,0.00012518794,0.0021096405,0.000107360225,0.0000059811946,0.000021310148,0.00022613614,0.000059114864,0.0033641863],"genre_scores_gemma":[0.9989686,0.00005449264,0.00038980716,0.000007664994,0.0000025014076,0.000016611186,0.0000865034,0.000010532624,0.00046324925],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999318,0.00001904472,0.0000047551584,0.000021404512,0.0000072600365,0.000015700818],"domain_scores_gemma":[0.99981743,0.00006424536,0.000046733476,0.000020952592,0.0000289792,0.000021682592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022071347,0.0003898762,0.00022513668,0.00037048195,0.00029446793,0.00083135196,0.00075534335,0.00035195646,0.0012523476],"category_scores_gemma":[0.0009795728,0.00033522613,0.0003547827,0.00032172873,0.00053741393,0.0004186534,0.0005696103,0.00029953322,0.00014212186],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007194456,0.000032814867,0.021052128,0.000032198248,0.00003060088,0.00011399289,0.00013070324,0.972843,0.0030344985,0.0009824409,0.00015112296,0.0015246439],"study_design_scores_gemma":[0.00006269302,0.000030969073,0.012906414,0.000012523929,0.00001551572,0.000023990755,0.00015196252,0.98454076,0.00088923314,0.00075269747,0.0005954537,0.000017749611],"about_ca_topic_score_codex":0.07347435,"about_ca_topic_score_gemma":0.030577462,"teacher_disagreement_score":0.07347435,"about_ca_system_score_codex":0.0018325896,"about_ca_system_score_gemma":0.0009548086,"threshold_uncertainty_score":0.14609337},"labels":[],"label_agreement":null},{"id":"W2019490786","doi":"10.1016/j.margeo.2005.03.011","title":"The Cilicia–Adana basin complex, Eastern Mediterranean: Neogene evolution of an active fore-arc basin in an obliquely convergent margin","year":2005,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Structural basin; Paleontology; Evaporite; Nappe; Neogene; Detachment fault; Basement; Quaternary; Décollement; Thrust fault; Fold and thrust belt; Sedimentary rock; Fault (geology); Foreland basin; Tectonics; Archaeology; Extensional definition","score_opus":0.025351777274212783,"score_gpt":0.23937145957694977,"score_spread":0.214019682302737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019490786","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997162,0.00022122472,0.00005254142,0.000054563097,0.00000488909,0.0000046012833,0.000051190313,0.0000046404025,0.0024443157],"genre_scores_gemma":[0.9990798,0.00009957627,0.00013719265,0.000017679324,0.0000063604857,0.0000037237207,0.00007540643,0.0000038013168,0.0005764756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999082,0.000010989546,0.0000065363874,0.000034465582,0.000016072268,0.000023652949],"domain_scores_gemma":[0.99989665,0.000010181935,0.00003728317,0.000008343805,0.000029193345,0.000018295108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021252756,0.00016306182,0.00020720593,0.0006223239,0.00047113711,0.00070262694,0.0003275512,0.00034129,0.0011307029],"category_scores_gemma":[0.00060466095,0.00012507544,0.00017736336,0.000505182,0.000621865,0.00029532207,0.0007168193,0.00010086268,0.00015980905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006315086,0.000077822246,0.8981272,0.0001677695,0.0001949541,0.0011477243,0.007621484,0.0016376539,0.02957623,0.003971846,0.00082281296,0.056022923],"study_design_scores_gemma":[0.0000140663105,0.000017208356,0.99666226,0.000010904249,0.000013493784,0.00013239954,0.0004986957,0.00030571767,0.0001427406,0.00011169284,0.0020883612,0.000002547054],"about_ca_topic_score_codex":0.028272156,"about_ca_topic_score_gemma":0.05195753,"teacher_disagreement_score":0.028272156,"about_ca_system_score_codex":0.0011164609,"about_ca_system_score_gemma":0.0006911603,"threshold_uncertainty_score":0.056215167},"labels":[],"label_agreement":null},{"id":"W2019875617","doi":"10.1016/j.jsg.2009.10.009","title":"Active fault and shear processes and their implications for mineral deposit formation and discovery","year":2009,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":135,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Kalgoorlie Consolidated Gold Mines; Barrick Gold Corporation","keywords":"Geology; Shearing (physics); Shear (geology); Shear zone; Scaling; Shear stress; Echelon formation; Seismology; Creep; Slip (aerodynamics); Petrology; Fault (geology); Geotechnical engineering; Tectonics; Mechanics; Geometry; Engineering","score_opus":0.012706894684277303,"score_gpt":0.23458210458424114,"score_spread":0.22187520989996384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019875617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99214,0.0006124244,0.001911611,0.00041925634,0.000011714945,0.0000062174654,0.000103115366,0.00000957964,0.0047860923],"genre_scores_gemma":[0.99906605,0.00023992597,0.00024608127,0.00000668614,0.000009029427,0.0000011824823,0.000019004565,0.0000017504394,0.00041026162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990594,0.000020747484,0.000009576807,0.000023981082,0.0000209774,0.000018852159],"domain_scores_gemma":[0.9989355,0.0005366962,0.00020262896,0.00008619215,0.00015790937,0.00008099235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006368895,0.00010927388,0.00012542779,0.0011337202,0.0005342405,0.0016089564,0.000329025,0.00046077123,0.0026459377],"category_scores_gemma":[0.0033241478,0.00018718996,0.00012394907,0.0009378086,0.0014007717,0.001749294,0.0004295343,0.00026967246,0.00021261045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008494121,0.00014473188,0.7451973,0.00013197721,0.000086653454,0.0011256139,0.0024705774,0.01050099,0.03198743,0.11297573,0.00074148574,0.093788095],"study_design_scores_gemma":[0.000067718465,0.00015186172,0.8699903,0.000024471005,0.000053819298,0.00059676904,0.0029472369,0.01988185,0.0050179814,0.096739985,0.004494224,0.00003386293],"about_ca_topic_score_codex":0.0035276248,"about_ca_topic_score_gemma":0.006673662,"teacher_disagreement_score":0.0035276248,"about_ca_system_score_codex":0.0007851121,"about_ca_system_score_gemma":0.00030557724,"threshold_uncertainty_score":0.008851528},"labels":[],"label_agreement":null},{"id":"W2019923788","doi":"10.5194/npg-21-1185-2014","title":"Dependence of sandpile avalanche frequency–size distribution on coverage extent and compactness of embedded toppling threshold heterogeneity: implications for the variation of Gutenberg–Richter &amp;lt;i&amp;gt;b&amp;lt;/i&amp;gt; value","year":2014,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Scaling; Exponent; Self-organized criticality; Statistical physics; Induced seismicity; Criticality; Event (particle physics); Cellular automaton; Geology; Microscale chemistry; Fault (geology); Tectonics; Range (aeronautics); Physics; Geometry; Mathematics; Seismology; Materials science","score_opus":0.030421651986414645,"score_gpt":0.27465786316052376,"score_spread":0.24423621117410912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019923788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955291,0.000029536532,0.0038171627,0.0000113864235,0.0000014580169,0.0000031448565,0.00003360668,0.000034057055,0.00054054655],"genre_scores_gemma":[0.9997553,0.0000048781108,0.0001985825,6.873536e-7,2.5033927e-7,0.0000011935858,0.000010502047,0.0000016039241,0.000027079495],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993086,0.000011602845,0.000005003378,0.00002648153,0.000010844237,0.000015236459],"domain_scores_gemma":[0.9987638,0.0007322601,0.00017210116,0.00015472222,0.000079850426,0.00009730459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019712487,0.000110901296,0.0001463333,0.00041261181,0.000104206876,0.00039853988,0.00020814966,0.0001422763,0.0010135493],"category_scores_gemma":[0.0020797837,0.00008974273,0.00011288787,0.00016770279,0.00032090498,0.00030930171,0.00021313004,0.00016216405,0.00006655188],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006440659,0.00023892964,0.21106416,0.00020764506,0.0001664089,0.00090702466,0.00048192622,0.2753101,0.46220452,0.007335108,0.00040393716,0.041036285],"study_design_scores_gemma":[0.000012783584,0.00015118273,0.21620181,0.000012271503,0.000036309295,0.0002550345,0.00016806052,0.7419774,0.038622968,0.002259095,0.00027151895,0.0000315665],"about_ca_topic_score_codex":0.0006383814,"about_ca_topic_score_gemma":0.0006704083,"teacher_disagreement_score":0.0010135493,"about_ca_system_score_codex":0.00015712224,"about_ca_system_score_gemma":0.00010270089,"threshold_uncertainty_score":0.0033906698},"labels":[],"label_agreement":null},{"id":"W2020052583","doi":"10.1016/j.jsg.2011.02.006","title":"Structural development of a high-pressure collisional accretionary wedge: The Samaná complex, Northern Hispaniola","year":2011,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Ministerio de Ciencia e Innovación; European Commission","keywords":"Geology; Nappe; Blueschist; Metamorphism; Accretionary wedge; Seismology; Greenschist; Ophiolite; Shear zone; Subduction; Geochronology; Geochemistry; Petrology; Geomorphology; Eclogite; Tectonics","score_opus":0.03565816837214796,"score_gpt":0.2262824890017634,"score_spread":0.19062432062961543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020052583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984383,0.000023652305,0.000031697466,0.000021800955,0.0000014085739,0.0000029643236,0.000013704736,0.0000016390575,0.0014647802],"genre_scores_gemma":[0.9996973,0.000017196566,0.000047558868,0.000003614086,9.454783e-7,0.0000015444265,0.000019998937,8.092459e-7,0.00021108278],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993634,0.000009182736,0.000003734755,0.00001551199,0.000011530259,0.000023656481],"domain_scores_gemma":[0.9999223,0.000010428384,0.000019230149,0.0000056465997,0.000017475884,0.000024884761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010352762,0.00017508355,0.00014495067,0.00074958004,0.0015218968,0.000751864,0.0004163925,0.00032684216,0.0024566865],"category_scores_gemma":[0.00041292133,0.00019999058,0.00008445981,0.000925742,0.00081029895,0.00031572484,0.00086577516,0.00022919597,0.00024989783],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009449529,0.00028939365,0.84987193,0.00014900486,0.0000784339,0.011569963,0.02763175,0.0016701741,0.0554917,0.004750266,0.000539949,0.047012504],"study_design_scores_gemma":[0.00001898531,0.00015107157,0.9875717,0.000013474315,0.000012538787,0.001149608,0.00789049,0.00082962436,0.000689987,0.00020277376,0.0014628142,0.000006891004],"about_ca_topic_score_codex":0.03158354,"about_ca_topic_score_gemma":0.07642271,"teacher_disagreement_score":0.03158354,"about_ca_system_score_codex":0.00070383056,"about_ca_system_score_gemma":0.00074342196,"threshold_uncertainty_score":0.062799394},"labels":[],"label_agreement":null},{"id":"W2020359576","doi":"10.1029/2003gl017022","title":"Lithospheric thickness inferred from Australian post‐glacial sea‐level change: The influence of a ductile crustal zone","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Lithosphere; Geology; Crust; Glacial period; Post-glacial rebound; Sea level; Geophysics; Seismology; Geomorphology; Oceanography; Tectonics","score_opus":0.07378921795161288,"score_gpt":0.3029481083420827,"score_spread":0.22915889039046983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020359576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99893564,0.00003572625,0.00033612832,0.00008650343,0.000002164514,0.0000017464095,0.000062494015,0.000016293772,0.00052336405],"genre_scores_gemma":[0.9997818,0.000020280284,0.000087739376,0.0000068578106,7.6724143e-7,0.0000010356185,0.000036541853,0.0000022519532,0.0000627562],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99983835,0.000055899367,0.000011280116,0.000033320484,0.000024692092,0.000036433466],"domain_scores_gemma":[0.99943334,0.00022139671,0.00010017624,0.00006804307,0.000102239566,0.000074723845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062946934,0.00033293833,0.00025411398,0.00039224923,0.0003765718,0.0009760565,0.0007570606,0.0007070731,0.0007470335],"category_scores_gemma":[0.003228029,0.00055812445,0.00046293862,0.0003550429,0.00065251236,0.00049372355,0.0008018891,0.00042325587,0.00013943888],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023230528,0.000053360094,0.30418584,0.00006298104,0.00012905849,0.0002649653,0.00034217667,0.68143255,0.006656131,0.001321344,0.00024193183,0.0050773565],"study_design_scores_gemma":[0.00006588358,0.00011960859,0.21266854,0.000021353517,0.00007465409,0.00006194859,0.00019173883,0.78388673,0.0017398882,0.0008040191,0.00033410997,0.00003150132],"about_ca_topic_score_codex":0.080173224,"about_ca_topic_score_gemma":0.040011305,"teacher_disagreement_score":0.080173224,"about_ca_system_score_codex":0.001411393,"about_ca_system_score_gemma":0.0007414246,"threshold_uncertainty_score":0.1594131},"labels":[],"label_agreement":null},{"id":"W2020951249","doi":"10.1016/j.tecto.2013.11.024","title":"Invited review paper: Fault creep caused by subduction of rough seafloor relief","year":2013,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":351,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Geology; Seafloor spreading; Seismology; Subduction; Seamount; Trench; Fault (geology); Mid-ocean ridge; Tectonics; Geophysics; Paleontology","score_opus":0.011608591463820055,"score_gpt":0.20776215854994484,"score_spread":0.19615356708612477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020951249","genre_codex":"editorial","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000889839,0.30699536,0.00048210192,0.09442135,0.5887744,0.000099305216,0.0004479588,0.00006319066,0.00782653],"genre_scores_gemma":[0.0062905583,0.2420653,0.00040163772,0.059521187,0.66682446,0.0000932394,0.0004378833,0.00007192742,0.024293855],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989215,0.00015777077,0.00011745053,0.00035342597,0.00034008958,0.00010983001],"domain_scores_gemma":[0.99439996,0.0015348493,0.00036980736,0.00014328209,0.0029559375,0.00059606484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002113849,0.0015995008,0.0016988427,0.0017261781,0.00077583594,0.0026838623,0.0019139851,0.010058298,0.0140121225],"category_scores_gemma":[0.0067617404,0.00046492554,0.0010307138,0.0012844263,0.0011762521,0.0021297592,0.0014671966,0.0033700028,0.00945297],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093406255,0.000017084223,0.00021647755,0.0020295896,0.00004690898,0.0004584515,0.000026605148,0.00006526824,0.0003836622,0.0003142328,0.9648627,0.03148564],"study_design_scores_gemma":[0.00006524597,0.000086773354,0.0019111414,0.0009155903,0.00014061232,0.001412599,0.0001127887,0.000058672198,0.00035982407,0.0011490928,0.99375314,0.000034459586],"about_ca_topic_score_codex":0.0021021492,"about_ca_topic_score_gemma":0.0025517547,"teacher_disagreement_score":0.0140121225,"about_ca_system_score_codex":0.0012646881,"about_ca_system_score_gemma":0.0019638585,"threshold_uncertainty_score":0.04687524},"labels":[],"label_agreement":null},{"id":"W2021801577","doi":"10.1029/2007jb005414","title":"Crustal deformation and block kinematics in transition from collision to subduction: Global positioning system measurements in northern Taiwan, 1995–2005","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Trillium Health Partners Foundation","keywords":"Geology; Subduction; Tectonics; Seismology; Eurasian Plate; Continental collision; Euler's rotation theorem; Transition zone; Geodesy; Foothills; Collision zone; Plate tectonics; Continental margin; Lithosphere; Rotation (mathematics); Geometry; Geophysics; Geography","score_opus":0.043459099640400484,"score_gpt":0.2816121551428215,"score_spread":0.23815305550242102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021801577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99933773,0.000029284716,0.000040831375,0.000009208668,6.0981523e-7,0.00000219868,0.00035633496,0.000007742136,0.00021598683],"genre_scores_gemma":[0.99830174,0.000038897913,0.00011720003,0.00000612154,0.0000022239105,0.000007722237,0.0012964394,0.0000020679508,0.00022742081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989676,0.000010597934,0.0000144304495,0.000036353405,0.000021585915,0.000020225209],"domain_scores_gemma":[0.99960345,0.000026356778,0.00016719861,0.000036672765,0.00008564969,0.00008066243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020664146,0.00026843217,0.00020308935,0.00079039723,0.0003703993,0.00042639422,0.0003058381,0.00029314414,0.0005414106],"category_scores_gemma":[0.00054634054,0.00017959783,0.0002472932,0.001098639,0.00024756027,0.00032146598,0.00048714987,0.00018646155,0.00018342638],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008823489,0.000025187479,0.9881031,0.000019141937,0.000046960067,0.0002307249,0.0012567136,0.0016989168,0.0029050643,0.00003813445,0.00029148036,0.005296197],"study_design_scores_gemma":[0.000003470019,0.000023475124,0.99851876,0.0000030632507,0.0000102563245,0.000049578637,0.00022094889,0.0006746197,0.00019651002,0.0000064007863,0.00028998984,0.000003025854],"about_ca_topic_score_codex":0.08469487,"about_ca_topic_score_gemma":0.120490745,"teacher_disagreement_score":0.08469487,"about_ca_system_score_codex":0.0010386964,"about_ca_system_score_gemma":0.00053058565,"threshold_uncertainty_score":0.16840374},"labels":[],"label_agreement":null},{"id":"W2022285033","doi":"10.1029/2008jb006053","title":"Slab morphology in the Cascadia fore arc and its relation to episodic tremor and slip","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Subduction; Seismology; Slab; Episodic tremor and slip; Crust; Slip (aerodynamics); Oceanic crust; Convergent boundary; Tectonics; Geophysics","score_opus":0.03515789628254908,"score_gpt":0.3017305263132103,"score_spread":0.26657263003066123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022285033","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947196,0.000023612618,0.00005597307,0.000009172574,3.1891796e-7,0.0000012733358,0.00011626362,0.000010153307,0.0003112284],"genre_scores_gemma":[0.99965096,0.000020663003,0.00006342548,0.000001659509,5.3608886e-7,0.0000017180234,0.00013015317,0.0000032081482,0.00012769861],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990606,0.000008691687,0.000010499284,0.000040453164,0.000016678327,0.000017596629],"domain_scores_gemma":[0.9996605,0.000039739472,0.00012992536,0.00003698295,0.00007487081,0.000058022546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001239213,0.00023544049,0.00018099944,0.0017317515,0.0003535289,0.0005837826,0.00027697557,0.00025830252,0.00094410306],"category_scores_gemma":[0.0007898227,0.00034795213,0.00019424799,0.0013703671,0.00047222,0.00017319336,0.00046208483,0.00016686425,0.00016623142],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000095089476,0.0000125719325,0.9727358,0.000020247033,0.00004020724,0.00020585528,0.00075362815,0.001756115,0.01943702,0.000090480964,0.000050320636,0.0048027006],"study_design_scores_gemma":[7.8822745e-7,0.0000063485018,0.9993395,8.558144e-7,0.0000036151152,0.000028239536,0.00009325488,0.0003555815,0.00012146698,0.000014632815,0.000034044966,0.0000015781555],"about_ca_topic_score_codex":0.057422947,"about_ca_topic_score_gemma":0.08045423,"teacher_disagreement_score":0.057422947,"about_ca_system_score_codex":0.0007986508,"about_ca_system_score_gemma":0.0003411706,"threshold_uncertainty_score":0.114177406},"labels":[],"label_agreement":null},{"id":"W2022351985","doi":"10.1029/2003jb002826","title":"Upper crustal structure of southwestern British Columbia from the 1998 Seismic Hazards Investigation in Puget Sound","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Terrane; Seismology; Structural basin; Basement; Seismic refraction; Sound (geography); Ridge; North American Plate; Igneous rock; Fault (geology); Subduction; Paleontology; Geomorphology; Tectonics","score_opus":0.021420607556226916,"score_gpt":0.260202445392666,"score_spread":0.2387818378364391,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022351985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9816528,0.00039886966,0.00028153573,0.00021763654,0.000008069938,0.000024701381,0.007512447,0.00008080162,0.009823124],"genre_scores_gemma":[0.982235,0.00040420995,0.0007665891,0.000059461123,0.000002918537,0.000024366424,0.0078074276,0.000019800338,0.008680241],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999249,0.0000034871753,0.0000044257345,0.000015263813,0.000031653275,0.000020254656],"domain_scores_gemma":[0.99973184,0.00001635108,0.000025043586,0.000013351128,0.00017295209,0.00004047224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000083450745,0.00019443069,0.00011527308,0.001194664,0.0009242653,0.0007523047,0.00035419973,0.0001866898,0.0028526767],"category_scores_gemma":[0.00049877545,0.00016939185,0.000119114295,0.0017132784,0.00017009396,0.00016762318,0.00031812052,0.00022561352,0.00048303],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008341337,0.000050911825,0.8695684,0.0000789519,0.00005903983,0.00077819836,0.0011850548,0.009714812,0.0027796943,0.00061306555,0.017511552,0.097576864],"study_design_scores_gemma":[0.00000766644,0.0000055741834,0.9825659,0.000034645585,0.000019706902,0.00008913328,0.0008006809,0.0047749756,0.00032007523,0.00007694145,0.01129204,0.000012749239],"about_ca_topic_score_codex":0.9853585,"about_ca_topic_score_gemma":0.9935063,"teacher_disagreement_score":0.014641523,"about_ca_system_score_codex":0.008421159,"about_ca_system_score_gemma":0.005074981,"threshold_uncertainty_score":0.061100006},"labels":[],"label_agreement":null},{"id":"W2022585183","doi":"10.1029/2000gl011978","title":"A regional study of shear wave splitting above the Cascadia Subduction Zone: Margin‐parallel crustal stress","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Shear wave splitting; Shear (geology); Anisotropy; Borehole; Geophysics; Petrology; Tectonics; Geotechnical engineering","score_opus":0.06462835755179935,"score_gpt":0.2963087153510412,"score_spread":0.23168035779924184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022585183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99969745,0.000016985396,0.000021084046,0.000004623902,2.602487e-7,0.0000013374136,0.000059918744,0.0000014557012,0.00019683319],"genre_scores_gemma":[0.9995276,0.00003975295,0.000064456835,0.0000021971564,0.0000010774257,0.0000025849945,0.00016626864,0.0000011607154,0.00019498558],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999112,0.000008696649,0.0000043395435,0.00003119291,0.000015560094,0.000028992172],"domain_scores_gemma":[0.99964416,0.000032060358,0.00009936645,0.000035730118,0.00010493207,0.00008362668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011413511,0.00024410337,0.00016630878,0.00070661906,0.0004177329,0.0003024173,0.00014509546,0.0001500626,0.00059953897],"category_scores_gemma":[0.0004708857,0.00020461359,0.0001404674,0.0008711499,0.00028490368,0.00018747181,0.00029377308,0.00016603229,0.00016067844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022513304,0.000045831606,0.9642713,0.000022988506,0.00007315095,0.0004389528,0.001664584,0.00033979263,0.025031544,0.00005920623,0.00013895732,0.007688493],"study_design_scores_gemma":[0.0000016251007,0.000015187694,0.999246,0.0000012261195,0.0000075681846,0.00007518307,0.00023797732,0.00007276618,0.00021762248,0.0000046695695,0.000118560885,0.0000017131123],"about_ca_topic_score_codex":0.12039479,"about_ca_topic_score_gemma":0.22788145,"teacher_disagreement_score":0.12039479,"about_ca_system_score_codex":0.00069980416,"about_ca_system_score_gemma":0.00045116243,"threshold_uncertainty_score":0.23938805},"labels":[],"label_agreement":null},{"id":"W2022662209","doi":"10.1080/19475705.2014.883441","title":"Earthquake forecasting and its verification in northeast India","year":2014,"lang":"en","type":"article","venue":"Geomatics Natural Hazards and Risk","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Induced seismicity; Longitude; Seismology; Geology; Earthquake prediction; Moment magnitude scale; Indian subcontinent; Hotspot (geology); Magnitude (astronomy); Latitude; Geography; Geodesy; Mathematics; History","score_opus":0.010685803063906882,"score_gpt":0.20150315507524252,"score_spread":0.19081735201133565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022662209","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992192,0.00009791446,0.0052028773,0.000068397574,0.000007358615,0.000011074089,0.00070492196,0.00017161432,0.0015439289],"genre_scores_gemma":[0.9980385,0.000034224857,0.0012990235,0.0000025413835,0.0000031857705,0.0000028167813,0.00050785224,0.0000039616825,0.00010796781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999521,0.00013239846,0.000055911532,0.0000948635,0.00013620435,0.0000596403],"domain_scores_gemma":[0.99747074,0.00089747185,0.00062774384,0.0003149371,0.00060055545,0.000088582274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075218646,0.00020089226,0.00017285449,0.001203216,0.00018349654,0.0005730977,0.0003328476,0.00015798786,0.0005197902],"category_scores_gemma":[0.00456862,0.00010831314,0.00023286218,0.0012480583,0.00017200579,0.00035068992,0.0003172852,0.00025467962,0.00029013096],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003227901,0.00006812108,0.84439176,0.00009096815,0.00006378223,0.00031368615,0.0004543803,0.040252008,0.0074335667,0.00085606216,0.0008216497,0.10493124],"study_design_scores_gemma":[0.00001277058,0.00024607385,0.76064926,0.00002812899,0.0000721056,0.0004893618,0.0008249889,0.22773935,0.007480302,0.00058439694,0.0018390499,0.000034305092],"about_ca_topic_score_codex":0.019275635,"about_ca_topic_score_gemma":0.012271223,"teacher_disagreement_score":0.019275635,"about_ca_system_score_codex":0.00037294548,"about_ca_system_score_gemma":0.0005536669,"threshold_uncertainty_score":0.03832686},"labels":[],"label_agreement":null},{"id":"W2022727764","doi":"10.1016/j.tecto.2014.04.042","title":"Late Miocene–Recent evolution of the Finike Basin and its linkages with the Beydağlari complex and the Anaximander Mountains, eastern Mediterranean","year":2014,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Marathon","keywords":"Geology; Quaternary; Paleontology; Late Miocene; Structural basin; Sinistral and dextral; Evaporite; Fault (geology); Outcrop; Subsidence; Fold (higher-order function)","score_opus":0.017227227607870016,"score_gpt":0.19911528437309392,"score_spread":0.1818880567652239,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022727764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981073,0.00043729774,0.000033655335,0.00006329355,0.000003753996,0.0000018657056,0.000095097006,0.000002024706,0.0012556241],"genre_scores_gemma":[0.9994185,0.0001267119,0.000035569894,0.000008896147,0.0000042045103,0.000001474857,0.00008757059,0.0000011520547,0.00031596766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999316,0.000008551802,0.0000050451395,0.000025865342,0.0000071097475,0.000021814145],"domain_scores_gemma":[0.9998555,0.000014860105,0.00005248706,0.000007911011,0.00003401048,0.000035276276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023432856,0.00014959429,0.0001278412,0.0008467117,0.00043165474,0.0006933923,0.00033565238,0.0002911246,0.0022116126],"category_scores_gemma":[0.0005111682,0.00012704679,0.00011265667,0.0007465165,0.0005544651,0.0005152387,0.00044833802,0.00018588958,0.0001742324],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002629099,0.000056612385,0.9565956,0.00009709538,0.00011706745,0.0009008731,0.0068902466,0.00049840315,0.008614924,0.0016623104,0.00038498387,0.023918986],"study_design_scores_gemma":[0.0000020047803,0.000008020469,0.99834216,0.0000062230924,0.0000050774356,0.00005753255,0.00041044888,0.000045214223,0.000046204594,0.0000366061,0.0010393416,0.0000011111338],"about_ca_topic_score_codex":0.025032483,"about_ca_topic_score_gemma":0.0604625,"teacher_disagreement_score":0.025032483,"about_ca_system_score_codex":0.00083046913,"about_ca_system_score_gemma":0.00041711214,"threshold_uncertainty_score":0.049773574},"labels":[],"label_agreement":null},{"id":"W2023101377","doi":"10.1111/j.1365-3121.2009.00901.x","title":"Assessing the contribution of off‐fault deformation to slip‐rate estimates within the Taupo Rift, New Zealand, using 3‐D ground‐penetrating radar surveying and trenching","year":2009,"lang":"en","type":"article","venue":"Terra Nova","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Marsden Fund; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Eidgenössische Technische Hochschule Zürich; Royal Society Te Apārangi; Royal Society","keywords":"Geology; Trench; Seismology; Ground-penetrating radar; Rift; Geodetic datum; Slip (aerodynamics); Interferometric synthetic aperture radar; Fault (geology); Radar; Geodesy; Tectonics; Remote sensing; Synthetic aperture radar","score_opus":0.04657805529515831,"score_gpt":0.2927458710450055,"score_spread":0.2461678157498472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023101377","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99935204,0.000033328775,0.0002680351,0.000009331499,7.463259e-7,0.0000024489505,0.000044297612,0.00000270093,0.00028714834],"genre_scores_gemma":[0.99958843,0.000036033834,0.00023879604,0.000002475201,0.0000010950482,0.0000019118775,0.00007093281,0.0000013284551,0.000059124657],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976474,0.00004809556,0.00001930285,0.00006138178,0.00007339463,0.000033104432],"domain_scores_gemma":[0.99914813,0.00019750648,0.0003197987,0.00007142386,0.00019440884,0.00006872081],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006319613,0.00031825007,0.00018276821,0.0007558593,0.00031199682,0.0006674001,0.00030435348,0.0002226797,0.00039404954],"category_scores_gemma":[0.0028056055,0.00025238277,0.00018110043,0.0005000691,0.00048674535,0.00055651227,0.0005032428,0.00022546427,0.000108227956],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000913966,0.000010881261,0.97575164,0.000023805287,0.000056312594,0.00017181571,0.00054218527,0.001960337,0.008293903,0.000031067168,0.00004454829,0.013022116],"study_design_scores_gemma":[0.000003854502,0.00003054959,0.9966904,0.0000044853646,0.000012990212,0.00007064822,0.00022192184,0.002488624,0.00035724585,0.000019527697,0.00009539307,0.000004290504],"about_ca_topic_score_codex":0.1296732,"about_ca_topic_score_gemma":0.19680083,"teacher_disagreement_score":0.1296732,"about_ca_system_score_codex":0.00088586734,"about_ca_system_score_gemma":0.00033861282,"threshold_uncertainty_score":0.25783682},"labels":[],"label_agreement":null},{"id":"W2023142456","doi":"10.1016/s0040-1951(02)00279-2","title":"Spatial relationships between natural seismicity and faults, southeastern Ontario and north-central New York state","year":2002,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; University of Ottawa","funders":"Canadian Space Agency; Geological Society of America","keywords":"Geology; Seismology; Induced seismicity; Fault (geology); Structural basin; Active fault; Magnitude (astronomy); Population; Paleontology","score_opus":0.044544130498068164,"score_gpt":0.18800374274653034,"score_spread":0.14345961224846218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023142456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994676,0.00024693963,0.00006863324,0.00018786824,0.0000049865866,0.000013776169,0.002357189,0.0000061658507,0.0024385275],"genre_scores_gemma":[0.99444604,0.00035777953,0.00013659228,0.000023100587,0.00000488457,0.000018160013,0.0011393606,0.0000033250205,0.003870757],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981076,0.000019201378,0.000017798997,0.000045509405,0.000055239852,0.00005161009],"domain_scores_gemma":[0.9981029,0.00032198755,0.00047804642,0.000053992924,0.000733009,0.0003099443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020947485,0.0001267814,0.00017960535,0.0011838649,0.0014993465,0.001038408,0.00053400575,0.0001692472,0.0026834372],"category_scores_gemma":[0.0017300837,0.00025144414,0.00019087012,0.002337967,0.0008173329,0.00046573108,0.000760201,0.00025247736,0.0001833248],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075691125,0.000013267158,0.99303585,0.000031583037,0.000045157594,0.00010100405,0.002338481,0.0002352445,0.0005453647,0.0003512806,0.0010425972,0.002184519],"study_design_scores_gemma":[0.000004461342,0.0000040124196,0.99668854,0.000010651496,0.00001151921,0.000028791863,0.0017803536,0.00019371345,0.000072392046,0.00003437158,0.0011671626,0.0000041610547],"about_ca_topic_score_codex":0.9865422,"about_ca_topic_score_gemma":0.99807113,"teacher_disagreement_score":0.013457775,"about_ca_system_score_codex":0.012295475,"about_ca_system_score_gemma":0.011894902,"threshold_uncertainty_score":0.08921027},"labels":[],"label_agreement":null},{"id":"W2024379371","doi":"10.1016/j.jog.2010.11.008","title":"Anomalous bathymetry, 3D edge driven convection, and dynamic topography at the western Atlantic passive margin","year":2010,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Bathymetry; Geology; Margin (machine learning); Passive margin; Geodesy; Convection; Enhanced Data Rates for GSM Evolution; Geophysics; Seismology; Oceanography; Tectonics; Meteorology; Rift; Geography","score_opus":0.00451561653788814,"score_gpt":0.19910981417960388,"score_spread":0.19459419764171573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024379371","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996983,0.000009679575,0.000024039842,0.00001795609,0.0000010193764,4.5614598e-7,0.00004827995,0.0000020764899,0.00019816197],"genre_scores_gemma":[0.9998896,0.0000049704045,0.000014652854,0.0000026498587,8.940131e-7,3.1696348e-7,0.000035916808,8.9878836e-7,0.000050062004],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999546,0.0000055989394,0.0000037501848,0.000012837727,0.0000087085045,0.000014563069],"domain_scores_gemma":[0.9997403,0.000057228484,0.00006640906,0.000024032097,0.00005050613,0.00006146053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010092387,0.0000993619,0.00016555314,0.0003908011,0.00034341458,0.0005136017,0.0002505348,0.00036836538,0.0012163225],"category_scores_gemma":[0.0007559349,0.00021572469,0.00015000236,0.00035594846,0.0004274939,0.00032292254,0.0004986088,0.00025186306,0.00016716939],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016865853,0.00003771483,0.97951996,0.0000071281997,0.00002211051,0.00019549289,0.0003390291,0.0010912686,0.014871096,0.00018848444,0.00014813484,0.0034109203],"study_design_scores_gemma":[0.0000030415758,0.0000061673522,0.99837035,0.0000013311048,0.0000035658175,0.000022844433,0.00010424563,0.0013276731,0.00008361973,0.000030043133,0.00004456581,0.0000025781437],"about_ca_topic_score_codex":0.054155193,"about_ca_topic_score_gemma":0.10881539,"teacher_disagreement_score":0.054155193,"about_ca_system_score_codex":0.0004775401,"about_ca_system_score_gemma":0.00039689307,"threshold_uncertainty_score":0.10767996},"labels":[],"label_agreement":null},{"id":"W2024387681","doi":"10.1046/j.0956-540x.2000.01364.x","title":"Three-dimensional crustal velocity structure beneath the Strait of Georgia, British Columbia","year":2001,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; University of British Columbia","funders":"","keywords":"Geology; Structural basin; Cretaceous; Inversion (geology); Seismology; Basement; Crust; Paleontology","score_opus":0.010180758351207969,"score_gpt":0.20803314038661638,"score_spread":0.19785238203540842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024387681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933616,0.00013872278,0.00025715976,0.000083739455,0.0000026521154,0.000007617989,0.0013621172,0.000055228596,0.0047312817],"genre_scores_gemma":[0.9978288,0.00009154563,0.00020645835,0.000007689513,4.122686e-7,0.0000029034022,0.000716762,0.000004754938,0.0011406945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000021233525,0.0000018889597,0.000012060098,0.000010627299,0.000016079479],"domain_scores_gemma":[0.99989104,0.0000089524,0.000010974653,0.000004289448,0.000054096363,0.00003057517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00003433172,0.00022826887,0.00014056708,0.00082519936,0.00070453587,0.0011479236,0.00038802784,0.00023958563,0.0028896318],"category_scores_gemma":[0.000331302,0.00019952109,0.00013863071,0.0011135935,0.00028521675,0.00017373967,0.0003679891,0.00022829762,0.00030302626],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017087584,0.000060503455,0.8635322,0.000076005526,0.00009211495,0.00064151105,0.0014026102,0.05878597,0.011152429,0.0020570832,0.005802218,0.05622662],"study_design_scores_gemma":[0.000008998379,0.0000072323523,0.9648538,0.000022222657,0.000012584178,0.00004403907,0.00068786176,0.03235163,0.00020501066,0.0001533688,0.0016289416,0.000024352921],"about_ca_topic_score_codex":0.97040886,"about_ca_topic_score_gemma":0.98092973,"teacher_disagreement_score":0.029591143,"about_ca_system_score_codex":0.004597478,"about_ca_system_score_gemma":0.0032294807,"threshold_uncertainty_score":0.059530795},"labels":[],"label_agreement":null},{"id":"W2025347762","doi":"10.1144/gsl.sp.2006.253.01.01","title":"Analogue benchmarks of shortening and extension experiments","year":2006,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":146,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Extension (predicate logic); Computer science; Programming language","score_opus":0.022814953561177534,"score_gpt":0.2345764765029319,"score_spread":0.21176152294175438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025347762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95672774,0.0001721333,0.037030637,0.0000462521,0.000054638956,0.00022396866,0.0006121348,0.0005327861,0.0045996387],"genre_scores_gemma":[0.98396975,0.000082766775,0.013848823,0.000031314758,0.000015084597,0.00027067924,0.0007223216,0.000111467736,0.00094778894],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9974509,0.0005885689,0.00023666023,0.0005825343,0.0009433947,0.00019799065],"domain_scores_gemma":[0.9940485,0.0018160149,0.0005581402,0.0023249125,0.0010324098,0.00022012487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020625973,0.0005117123,0.00047975226,0.0005927289,0.0005177692,0.0007210517,0.0011692129,0.00065726764,0.0041065915],"category_scores_gemma":[0.0051877536,0.00028008464,0.00041192214,0.00081746996,0.0010194256,0.0006545968,0.0011775717,0.00064140325,0.00049331784],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021214192,0.001219442,0.020394983,0.00047674926,0.00008442817,0.00025998394,0.00063414196,0.036951203,0.8872562,0.0022594377,0.000671643,0.047670353],"study_design_scores_gemma":[0.00024379804,0.009610663,0.06560707,0.000045643683,0.00014582636,0.00030878183,0.00044249944,0.1108519,0.8037171,0.0018707376,0.007015039,0.00014087965],"about_ca_topic_score_codex":0.0013479193,"about_ca_topic_score_gemma":0.0013912508,"teacher_disagreement_score":0.0041065915,"about_ca_system_score_codex":0.00062348193,"about_ca_system_score_gemma":0.00025834437,"threshold_uncertainty_score":0.013737857},"labels":[],"label_agreement":null},{"id":"W2025360865","doi":"10.1144/gsl.sp.2007.272.01.23","title":"Structural style and hydrocarbon prospectivity in fold and thrust belts: a global review","year":2007,"lang":"en","type":"review","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Encana (Canada)","funders":"","keywords":"Prospectivity mapping; Geology; Fold (higher-order function); Thrust; Geochemistry; Petrology; Paleontology; Engineering; Aerospace engineering; Mechanical engineering","score_opus":0.0513622254521129,"score_gpt":0.3068610553757079,"score_spread":0.255498829923595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025360865","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005522767,0.998998,0.000024054592,0.00014242888,0.000029653193,0.0000018442443,0.000059140362,0.0000015372543,0.00019109395],"genre_scores_gemma":[0.0032022407,0.99647933,0.000052086918,0.000074075564,0.000056894474,0.0000029978723,0.000058396025,9.452207e-7,0.00007306761],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.999648,0.000076169315,0.00008911841,0.00008622525,0.000073703995,0.000026790345],"domain_scores_gemma":[0.9966934,0.0020697846,0.00065405923,0.00004872053,0.0004376676,0.00009637552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015519046,0.000814563,0.0019635602,0.0062102643,0.00018428486,0.0016263423,0.0008210838,0.00087149104,0.0036341923],"category_scores_gemma":[0.0028777064,0.000449245,0.001284882,0.008489493,0.0008639037,0.0016802154,0.00071698736,0.00078318536,0.00064065243],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028362792,0.000059768914,0.008868036,0.05657858,0.0008901059,0.00013278358,0.00018366982,0.00039869492,0.0002673341,0.0010873539,0.010528327,0.9207218],"study_design_scores_gemma":[0.0001375662,0.00083834206,0.16782297,0.13264838,0.008220487,0.0045585497,0.001552461,0.0005964179,0.00081280945,0.0031324257,0.67948544,0.00019410862],"about_ca_topic_score_codex":0.0047890474,"about_ca_topic_score_gemma":0.006430813,"teacher_disagreement_score":0.0062102643,"about_ca_system_score_codex":0.0006259779,"about_ca_system_score_gemma":0.0014813282,"threshold_uncertainty_score":0.012157559},"labels":[],"label_agreement":null},{"id":"W2025748429","doi":"10.1038/nature13677","title":"Continuing megathrust earthquake potential in Chile after the 2014 Iquique earthquake","year":2014,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":192,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Canadian Space Agency; U.S. Geological Survey","keywords":"Seismology; Geology; Induced seismicity; Seismic gap; Interplate earthquake; Subduction; Seismic hazard; Seismotectonics; Context (archaeology); Intraplate earthquake; Fault (geology); Aftershock; Sequence (biology); Types of earthquake; Foreshock; Tectonics; Paleontology","score_opus":0.0035433881793145616,"score_gpt":0.19395488366688216,"score_spread":0.19041149548756758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025748429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98608404,0.00048539852,0.000036445286,0.0014207606,0.000030254743,0.000020542551,0.00084562245,0.000005642304,0.011071362],"genre_scores_gemma":[0.99463516,0.00042414753,0.000041534346,0.00012626489,0.000041273543,0.000024257608,0.0008297914,0.00000605321,0.0038714379],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982196,0.000025049809,0.000010293352,0.000026088177,0.000033801523,0.000082885446],"domain_scores_gemma":[0.9988433,0.00014687743,0.00032197573,0.000048437803,0.0004256018,0.00021384789],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049339497,0.0001681213,0.00030900314,0.0012233317,0.0013307591,0.001493741,0.00058266614,0.00096642965,0.0034147205],"category_scores_gemma":[0.0028644009,0.00020067516,0.00024854505,0.0019698697,0.0006698645,0.00092967635,0.0015335104,0.0007163416,0.000420362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060883194,0.00022518514,0.943794,0.0002589654,0.00015156672,0.0038375193,0.013355478,0.0014293914,0.0023542421,0.0026582899,0.008510731,0.022815846],"study_design_scores_gemma":[0.000012930023,0.00003379465,0.9876902,0.000047142323,0.000018071527,0.000112361835,0.006925526,0.00015375922,0.00008379004,0.00015578636,0.004752811,0.000013764267],"about_ca_topic_score_codex":0.16546908,"about_ca_topic_score_gemma":0.2863754,"teacher_disagreement_score":0.16546908,"about_ca_system_score_codex":0.003987825,"about_ca_system_score_gemma":0.0030288815,"threshold_uncertainty_score":0.32901186},"labels":[],"label_agreement":null},{"id":"W2026517237","doi":"10.1007/s000240300006","title":"Numerical Modelling of Tsunamis Generated by Hypothetical Landslides in the Strait of Georgia, British Columbia","year":2003,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Geology; Submarine landslide; Landslide; Seismology; Crest; Submarine pipeline; Rockslide; Trough (economics); Bathymetry; Geomorphology; Oceanography","score_opus":0.012327242380133616,"score_gpt":0.17509830547200078,"score_spread":0.16277106309186717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026517237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946943,0.000032651034,0.00033325024,0.00013151117,0.0000117451955,0.000015030343,0.00046055682,0.000034828514,0.0042861546],"genre_scores_gemma":[0.9983746,0.00003929292,0.0002035901,0.000011341598,0.0000012430077,0.0000082190745,0.00017371139,0.0000056868703,0.0011823927],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990225,0.000021201455,0.0000068736967,0.000017596612,0.000015188468,0.00003688706],"domain_scores_gemma":[0.9994918,0.00017320433,0.00004311565,0.00002779424,0.00017295148,0.000091023314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015747605,0.00040718223,0.00037677292,0.00056539965,0.0011906979,0.0013238726,0.0011325188,0.0011328749,0.0025654887],"category_scores_gemma":[0.0013966777,0.00043208373,0.0003585076,0.0011010949,0.0009245987,0.00038058485,0.00046189065,0.0006859815,0.00022305772],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009969835,0.000051004434,0.014211731,0.000018194065,0.00002247728,0.000245357,0.00008383065,0.98196226,0.00044766,0.0009320325,0.000653155,0.0012725687],"study_design_scores_gemma":[0.000049036258,0.000035431636,0.012920363,0.000009953527,0.000019444526,0.000022250268,0.00031254042,0.98572934,0.00021023373,0.0002413525,0.0004309117,0.000019070381],"about_ca_topic_score_codex":0.8880386,"about_ca_topic_score_gemma":0.87099683,"teacher_disagreement_score":0.111961424,"about_ca_system_score_codex":0.007287387,"about_ca_system_score_gemma":0.004287046,"threshold_uncertainty_score":0.22524154},"labels":[],"label_agreement":null},{"id":"W2026547081","doi":"10.1007/s10950-011-9252-9","title":"Depth determination of small shallow earthquakes in eastern Canada from maximum power Rg/Sg spectral ratio","year":2011,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Focal mechanism; Seismology; Geology; Amplitude; Focal length; Azimuth; Geodesy; Hydrogeology; Cardinal point; Optics; Fault (geology); Physics","score_opus":0.02858099266870125,"score_gpt":0.20598169654183404,"score_spread":0.17740070387313278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026547081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99650514,0.00017879125,0.00024240406,0.00003011761,0.0000026336886,0.000008223589,0.00078728196,0.000017500424,0.002227903],"genre_scores_gemma":[0.998623,0.00007542545,0.00023363966,0.000007391402,0.000001105244,0.0000016441612,0.00024778457,0.000003883723,0.0008061253],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.0000044804938,0.000005313117,0.000016953256,0.00003035619,0.000040424675],"domain_scores_gemma":[0.99946946,0.00005333055,0.000042716874,0.000010358663,0.0003159283,0.00010816036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014649218,0.00023181214,0.00017192247,0.0016614065,0.0009624033,0.000754314,0.00047143633,0.00021456835,0.0013211714],"category_scores_gemma":[0.0007223399,0.00019032691,0.00014899709,0.0016005123,0.00029140728,0.00022648058,0.00044546186,0.00023242386,0.00017353272],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003445516,0.000041994317,0.93421966,0.00007312911,0.0000667854,0.0005503376,0.0015735612,0.0031712463,0.020925589,0.00040766658,0.0008787428,0.037746854],"study_design_scores_gemma":[0.0000047917297,0.000006776434,0.99653095,0.000007966123,0.000016284806,0.000043272896,0.00065608777,0.0016186046,0.0006048266,0.000024415564,0.00047765917,0.000008360448],"about_ca_topic_score_codex":0.9731241,"about_ca_topic_score_gemma":0.9887615,"teacher_disagreement_score":0.026875913,"about_ca_system_score_codex":0.0047316803,"about_ca_system_score_gemma":0.0043373196,"threshold_uncertainty_score":0.054068327},"labels":[],"label_agreement":null},{"id":"W2026596556","doi":"10.1111/j.1365-3121.2009.00895.x","title":"Marine palaeoseismology from very high resolution seismic imaging: the Gondola Fault Zone (Adriatic foreland)","year":2009,"lang":"en","type":"article","venue":"Terra Nova","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"AGE-WELL","keywords":"Geology; Foreland basin; Seismology; Fault (geology); Anticline; Strike-slip tectonics; Vertical displacement; Slip (aerodynamics); Tectonics; Active fault; Paleontology","score_opus":0.01600312480516708,"score_gpt":0.21627408561236297,"score_spread":0.2002709608071959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026596556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887055,0.000049657443,0.000079474376,0.000009924103,5.282787e-7,0.0000021390308,0.00015219876,0.000003679283,0.000831894],"genre_scores_gemma":[0.99931645,0.000040104933,0.00019648796,0.0000029365374,0.0000018116223,0.0000017553153,0.0002208923,0.0000011508829,0.00021833381],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994564,0.0000068670765,0.000003662119,0.000013114315,0.000013447339,0.000017207745],"domain_scores_gemma":[0.99993706,0.000007344968,0.000023864332,0.0000095847245,0.000015359306,0.0000067844776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007557901,0.00017119096,0.000094890194,0.0010990965,0.00016334302,0.00041917732,0.00011394721,0.00012160866,0.0007742023],"category_scores_gemma":[0.000214797,0.00009303763,0.00011135411,0.00082660967,0.00022311577,0.00012418498,0.0002801351,0.00009349887,0.00016584291],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011205985,0.000052565443,0.91140795,0.000043732533,0.00011056457,0.0010863115,0.00078854524,0.0039914334,0.035763,0.00027527512,0.0004203816,0.045948185],"study_design_scores_gemma":[0.0000032263597,0.000014163419,0.99768853,0.0000040580962,0.0000076197734,0.00024151163,0.00015667814,0.0006646547,0.0005881348,0.00002256147,0.00060709333,0.0000019239806],"about_ca_topic_score_codex":0.013147923,"about_ca_topic_score_gemma":0.026457822,"teacher_disagreement_score":0.013147923,"about_ca_system_score_codex":0.00034098024,"about_ca_system_score_gemma":0.00014530701,"threshold_uncertainty_score":0.026142776},"labels":[],"label_agreement":null},{"id":"W2026705638","doi":"10.1175/jtech-d-12-00201.1","title":"Combining the All-Source Green's Functions and the GPS-Derived Source Functions for Fast Tsunami Predictions—Illustrated by the March 2011 Japan Tsunami","year":2013,"lang":"en","type":"article","venue":"Journal of Atmospheric and Oceanic Technology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Global Positioning System; Geology; Submarine; Elevation (ballistics); Seismology; Source function; Field (mathematics); Arrival time; Geodesy; Source model; Function (biology); Meteorology; Computer science; Geography; Oceanography; Telecommunications","score_opus":0.008113274261045182,"score_gpt":0.18779599227686475,"score_spread":0.17968271801581956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026705638","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.26262498,0.00020747664,0.73124796,0.00040878073,0.000057907393,0.000033117114,0.00016349905,0.0013125526,0.00394365],"genre_scores_gemma":[0.9151944,0.00010765487,0.0838174,0.00003388047,0.000030632928,0.00001756484,0.00013449483,0.00010475356,0.0005592848],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998932,0.00003735992,0.0000054586912,0.000020492938,0.000032479948,0.000011035623],"domain_scores_gemma":[0.99958223,0.00017261956,0.000038917136,0.00006307893,0.00011831937,0.00002479444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006521244,0.000712128,0.00033985442,0.0004991978,0.0003237527,0.000583902,0.0005990612,0.00036189286,0.000560301],"category_scores_gemma":[0.0018285408,0.00030802898,0.00043766745,0.0003443274,0.00031605668,0.000973861,0.00047109355,0.00062670495,0.00022669036],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042619944,0.000040461804,0.0065789022,0.000014979109,0.000036092886,0.00006777964,0.00004072381,0.93349946,0.0026626927,0.002513776,0.00042569652,0.054076836],"study_design_scores_gemma":[0.000003829053,0.000010757358,0.0010905873,0.0000027042638,0.0000063499956,0.0000063517514,0.000007437815,0.9968444,0.0007125314,0.0010139308,0.00029452262,0.0000066665084],"about_ca_topic_score_codex":0.01587944,"about_ca_topic_score_gemma":0.015141042,"teacher_disagreement_score":0.01587944,"about_ca_system_score_codex":0.0004532376,"about_ca_system_score_gemma":0.0007748267,"threshold_uncertainty_score":0.03157407},"labels":[],"label_agreement":null},{"id":"W2027001882","doi":"10.1007/978-3-0346-0064-4_10","title":"Tsunamis on the Pacific Coast of Canada Recorded in 1994–2007","year":2009,"lang":"en","type":"book-chapter","venue":"Birkhäuser Basel eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; Canadian Hydrographic Service","funders":"","keywords":"Geology; Seismology; Pacific ocean; Tide gauge; Oceanography; Geography; Period (music); Arrival time; Sea level","score_opus":0.020172830721876988,"score_gpt":0.180589223726019,"score_spread":0.160416393004142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027001882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8185829,0.0026540007,0.00047097172,0.00046189138,0.00012174198,0.00022503758,0.14617184,0.00018959738,0.031122018],"genre_scores_gemma":[0.86017925,0.0039369836,0.0013399199,0.00024668823,0.000048744892,0.00011244869,0.11667129,0.00004104434,0.01742358],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993144,0.000010961652,0.00003455811,0.000064428896,0.0004030268,0.0001726894],"domain_scores_gemma":[0.99755067,0.00003327733,0.00020361909,0.00003822716,0.001926951,0.0002473453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024171005,0.0006593465,0.00037802494,0.0034883139,0.0028625517,0.0011600151,0.0008409891,0.00023508738,0.002580283],"category_scores_gemma":[0.0010622906,0.0002504913,0.00027985053,0.008806351,0.00042172824,0.00031256335,0.0008441769,0.00058958825,0.0007195844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004147545,0.00010101513,0.867334,0.00046812114,0.00026359202,0.00080402417,0.002576381,0.0009617422,0.0022594489,0.0004246517,0.058270738,0.06612149],"study_design_scores_gemma":[0.000011065148,0.00002459515,0.9758933,0.00008071603,0.00004456551,0.00012069349,0.0017602585,0.00037717188,0.00040793285,0.000028721566,0.021223973,0.000026864282],"about_ca_topic_score_codex":0.99630463,"about_ca_topic_score_gemma":0.99857247,"teacher_disagreement_score":0.019570505,"about_ca_system_score_codex":0.019570505,"about_ca_system_score_gemma":0.02986025,"threshold_uncertainty_score":0.14199466},"labels":[],"label_agreement":null},{"id":"W2027368347","doi":"10.1016/s0012-821x(02)00520-4","title":"GPS deformation in a region of high crustal seismicity: N. Cascadia forearc","year":2002,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Forearc; Geology; Subduction; Seismology; Induced seismicity; Compression (physics); Episodic tremor and slip; Global Positioning System; Fault (geology); Tectonics","score_opus":0.015455945750971168,"score_gpt":0.17566197720943422,"score_spread":0.16020603145846304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027368347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980268,0.00004837652,0.00002965328,0.00014268816,0.0000033282022,0.000002336396,0.00037679932,0.000010546897,0.0013595223],"genre_scores_gemma":[0.9991836,0.000039411825,0.000043314245,0.000017171591,0.0000026665352,0.000001635907,0.00025488142,0.0000025967636,0.00045476697],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999,0.0000113310025,0.0000069012294,0.000034624063,0.000016077485,0.000031102827],"domain_scores_gemma":[0.99971944,0.000029294111,0.000052229476,0.000020256559,0.00008652047,0.000092269176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015062887,0.00025489047,0.00021889978,0.0007533467,0.00087884726,0.0005217382,0.0004295744,0.000494533,0.0023420178],"category_scores_gemma":[0.0005500388,0.00025035642,0.0002475447,0.0013372226,0.00062303635,0.00023415817,0.0006936544,0.00027546578,0.0003066711],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058773474,0.000077992336,0.9660325,0.00006856684,0.00012460227,0.001950541,0.0029627068,0.0072702086,0.01008881,0.00068178325,0.0020703124,0.0080842525],"study_design_scores_gemma":[0.0000064125716,0.000011574971,0.9986596,0.0000032252894,0.0000109729035,0.00006426595,0.0004543603,0.0003798892,0.00008151333,0.000035556583,0.00028853986,0.0000039702886],"about_ca_topic_score_codex":0.40932772,"about_ca_topic_score_gemma":0.5516424,"teacher_disagreement_score":0.59067225,"about_ca_system_score_codex":0.002153377,"about_ca_system_score_gemma":0.001210106,"threshold_uncertainty_score":0.81389034},"labels":[],"label_agreement":null},{"id":"W2027397158","doi":"10.1029/2006gl027316","title":"Observations of non‐volcanic tremor during the northern Cascadia slow‐slip event in February 2002","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"","keywords":"Episodic tremor and slip; Subduction; Geology; Seismology; Volcano; Slip (aerodynamics); Tectonics","score_opus":0.03110222833571543,"score_gpt":0.26142540855377966,"score_spread":0.23032318021806422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027397158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99649966,0.00006835476,0.00006558079,0.00006411496,0.0000065527174,0.000008282155,0.00073519914,0.000041347048,0.002510887],"genre_scores_gemma":[0.9967699,0.00008096234,0.00011824646,0.000024997193,0.00001472656,0.0000123445925,0.0015007982,0.000008310213,0.0014696516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978787,0.000019742996,0.00001551315,0.00005482508,0.00007918745,0.000042986798],"domain_scores_gemma":[0.9992865,0.00004989439,0.00017832255,0.00007019494,0.00021155193,0.00020358259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022000227,0.00033238746,0.0002579459,0.00097400387,0.0006013027,0.00048685554,0.0003518553,0.0004074348,0.0011866022],"category_scores_gemma":[0.0009450966,0.00024407591,0.0001326385,0.0007328776,0.00028465118,0.00021870575,0.0005662107,0.00025693563,0.00036331618],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003021113,0.00008191231,0.9591712,0.00008297126,0.000074980446,0.0010508379,0.003088075,0.0004934979,0.021331985,0.000065256754,0.0028058111,0.011451361],"study_design_scores_gemma":[0.0000053767167,0.00001738921,0.99878377,0.000002967822,0.000005217176,0.000058486658,0.00014719706,0.000099598044,0.00020541098,0.0000051253396,0.0006668668,0.0000025912327],"about_ca_topic_score_codex":0.08261554,"about_ca_topic_score_gemma":0.2389088,"teacher_disagreement_score":0.08261554,"about_ca_system_score_codex":0.0009847386,"about_ca_system_score_gemma":0.00043770205,"threshold_uncertainty_score":0.16426933},"labels":[],"label_agreement":null},{"id":"W2027537110","doi":"10.1016/j.gca.2006.06.705","title":"Short-lived orogenic cycles: Evidence from untransformed “metastable” domains buried to depths ⩾40km","year":2006,"lang":"en","type":"article","venue":"Geochimica et Cosmochimica Acta","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; University of Manitoba","funders":"","keywords":"Metastability; Geology; Geophysics; Paleontology; Earth science; Geochemistry; Physics","score_opus":0.02867861142470953,"score_gpt":0.254519663932564,"score_spread":0.22584105250785444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027537110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987393,0.00004482084,0.0004480168,0.000014624862,0.0000012421615,0.0000013213704,0.000037452573,0.0000065178097,0.0007066971],"genre_scores_gemma":[0.9996717,0.000030705203,0.00013015824,0.0000049345917,0.0000019148174,9.3817613e-7,0.000047011836,0.0000029780906,0.000109609144],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999954,0.0000030357337,0.0000030429915,0.000016008416,0.0000080582095,0.000015745132],"domain_scores_gemma":[0.99948263,0.000115740484,0.0001705915,0.00011868129,0.00006862787,0.000043680604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012437209,0.00009152524,0.00016727319,0.00043207858,0.0003571153,0.0005556475,0.00043394373,0.00026934894,0.0017477309],"category_scores_gemma":[0.0010012729,0.00016275456,0.0001088282,0.0005389225,0.0010267069,0.00072116713,0.00052351464,0.0002902181,0.00016670252],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015441574,0.00010344267,0.49629885,0.00014378421,0.00015898896,0.0012140515,0.002129325,0.004068214,0.45310906,0.011590826,0.00027130515,0.029367918],"study_design_scores_gemma":[0.000058623114,0.00025415444,0.91885877,0.000017261318,0.00011130496,0.0010206259,0.0012711395,0.008030938,0.056938596,0.010892139,0.0025171132,0.000029296758],"about_ca_topic_score_codex":0.0025982426,"about_ca_topic_score_gemma":0.0029919269,"teacher_disagreement_score":0.0025982426,"about_ca_system_score_codex":0.00021931675,"about_ca_system_score_gemma":0.00013969067,"threshold_uncertainty_score":0.005846739},"labels":[],"label_agreement":null},{"id":"W2027942890","doi":"10.1007/s00024-008-0426-5","title":"Numerical Modelling of the Destructive Meteotsunami of 15 June, 2006 on the Coast of the Balearic Islands","year":2008,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Balearic islands; Bathymetry; Inlet; Harbour; Geology; Disturbance (geology); Event (particle physics); Meteorology; Climatology; Environmental science; Oceanography; Geography; Physics; Geomorphology","score_opus":0.017672998609980305,"score_gpt":0.17530236690685835,"score_spread":0.15762936829687804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027942890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948856,0.00016093484,0.00046892607,0.00038623734,0.000048241647,0.000012901414,0.00044410853,0.00004831983,0.0035447204],"genre_scores_gemma":[0.99799746,0.00010098114,0.00039019436,0.00003641751,0.000011493973,0.000011971884,0.0003135031,0.000016747605,0.0011211431],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998518,0.000033081906,0.000012230423,0.000030419307,0.000017422204,0.000054980435],"domain_scores_gemma":[0.9995834,0.00012099619,0.00006309687,0.000030977015,0.000109807035,0.00009157797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045444415,0.00075480225,0.00071873865,0.0006772833,0.0009777821,0.0016749254,0.0014619415,0.0026931982,0.003148687],"category_scores_gemma":[0.0020768384,0.0006836844,0.0007344353,0.0007500476,0.0011167757,0.00086087605,0.001000582,0.0012473952,0.00022376813],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015789384,0.000110181725,0.019437289,0.00004247678,0.00008731542,0.000335703,0.00020598777,0.97510207,0.0010870011,0.0009913377,0.00084361003,0.0015991768],"study_design_scores_gemma":[0.00015083866,0.00011071464,0.03453017,0.000023431105,0.000060858772,0.00003462959,0.0005992899,0.9628281,0.00028499967,0.00036291705,0.0009730609,0.000041057505],"about_ca_topic_score_codex":0.36199504,"about_ca_topic_score_gemma":0.2697713,"teacher_disagreement_score":0.36199504,"about_ca_system_score_codex":0.0026940831,"about_ca_system_score_gemma":0.002154077,"threshold_uncertainty_score":0.71977603},"labels":[],"label_agreement":null},{"id":"W2028092617","doi":"10.1121/1.4899490","title":"Bayesian tsunami-waveform inversion with trans-dimensional tsunami-source models","year":2014,"lang":"en","type":"article","venue":"The Journal of the Acoustical Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Discretization; Inversion (geology); Tide gauge; Tsunami earthquake; Seismology; Eikonal equation; Geodesy; Sea level; Mathematics; Mathematical analysis; Oceanography","score_opus":0.009793079222189874,"score_gpt":0.1909024854295419,"score_spread":0.18110940620735205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028092617","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.036964055,0.000043016753,0.9617474,0.00005296806,0.000008607683,0.000012367445,0.00012598853,0.00026137714,0.0007841535],"genre_scores_gemma":[0.69285053,0.00014205063,0.30433497,0.00006145648,0.000023088329,0.00007795649,0.0008070424,0.0001455608,0.0015573339],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998493,0.00004393804,0.000013108363,0.00002949542,0.000049679893,0.000014423863],"domain_scores_gemma":[0.9995415,0.00021134535,0.00006784941,0.000073910895,0.00008321984,0.000022281756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005373765,0.00032417552,0.00028892746,0.00042995415,0.00016124125,0.0005600594,0.0008647429,0.00048123093,0.0007137103],"category_scores_gemma":[0.0026566957,0.00047420518,0.00042229146,0.00045899625,0.00029764246,0.00093900575,0.000785463,0.000766845,0.00030317134],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037516344,0.000024796671,0.0013091076,0.000016793972,0.000032936678,0.00002336422,0.00002921776,0.9670922,0.0036157602,0.0066851396,0.00017220559,0.020960998],"study_design_scores_gemma":[0.0000027858134,0.0000023267464,0.00012213583,9.192054e-7,0.0000015129718,0.000003535199,0.0000015142334,0.9983317,0.0002600351,0.0011876376,0.00008316812,0.0000026168523],"about_ca_topic_score_codex":0.0071310885,"about_ca_topic_score_gemma":0.008409029,"teacher_disagreement_score":0.0071310885,"about_ca_system_score_codex":0.00033771756,"about_ca_system_score_gemma":0.00085837493,"threshold_uncertainty_score":0.01417917},"labels":[],"label_agreement":null},{"id":"W2029460169","doi":"10.1029/2003jb002952","title":"Experimental and analytical modeling of basaltic ash explosions at Mount Etna, Italy, 2001","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Istituto Nazionale di Geofisica e Vulcanologia","keywords":"Strombolian eruption; Overpressure; Geology; Ejecta; Impact crater; Pyroclastic rock; Volcano; Lateral eruption; Vulcanian eruption; Explosive eruption; Magma; Petrology; Seismology; Mineralogy; Physics","score_opus":0.07353328707851045,"score_gpt":0.33296434882602394,"score_spread":0.2594310617475135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029460169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98685324,0.00011105576,0.0016947641,0.00011113066,0.000008608999,0.000036058893,0.0016365086,0.00030156807,0.009246963],"genre_scores_gemma":[0.9967951,0.00008970149,0.0010845949,0.000013439635,0.0000057854436,0.000044139968,0.0008769508,0.00003595035,0.0010541877],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988806,0.000013234095,0.0000066195685,0.000033295742,0.000027545762,0.000031146352],"domain_scores_gemma":[0.9996158,0.0001784858,0.00006860469,0.000041872863,0.000064885506,0.000030286541],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002825586,0.0007015213,0.00043582474,0.00049734645,0.00057531236,0.00067252043,0.0011360986,0.0008725097,0.002238757],"category_scores_gemma":[0.0007366205,0.00045610152,0.0005174705,0.0005870297,0.00044969554,0.0004163462,0.0002859767,0.0005234635,0.0003680924],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023396873,0.00035652422,0.024807775,0.0001330732,0.000055911125,0.00041923072,0.00014177787,0.95412207,0.0132814,0.0007738901,0.0012219703,0.004452519],"study_design_scores_gemma":[0.000060054736,0.0001017608,0.016831141,0.0000075666744,0.000030908104,0.000054272685,0.000053836724,0.9765266,0.0054102903,0.0001991206,0.0007040921,0.000020305322],"about_ca_topic_score_codex":0.02416653,"about_ca_topic_score_gemma":0.016003784,"teacher_disagreement_score":0.02416653,"about_ca_system_score_codex":0.0015029773,"about_ca_system_score_gemma":0.0004727702,"threshold_uncertainty_score":0.048051715},"labels":[],"label_agreement":null},{"id":"W2029468491","doi":"10.1029/2010eo380007","title":"Space Geodetic Data Improve Seismic Hazard Assessment in California: Workshop on Incorporating Geodetic Surface Deformation Data Into UCERF3; Pomona, California, 1–2 April 2010","year":2010,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geodetic datum; Seismology; Seismic hazard; Geology; Slip (aerodynamics); Geodesy; Geological survey; San andreas fault; Fault (geology); Engineering; Geophysics; Aerospace engineering","score_opus":0.03091121502686521,"score_gpt":0.26845467938843953,"score_spread":0.2375434643615743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029468491","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.24249092,0.031376652,0.3847709,0.105393246,0.003723238,0.0015874901,0.060566563,0.010794631,0.15929638],"genre_scores_gemma":[0.51930666,0.012690973,0.36830673,0.002368461,0.0007498496,0.00049480586,0.036818042,0.0014079625,0.05785652],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9987243,0.0003309025,0.00008228893,0.000212732,0.0005391868,0.00011059444],"domain_scores_gemma":[0.99661666,0.0009996897,0.00018769914,0.0004165483,0.0015220947,0.00025732056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009079996,0.00060746225,0.00041197627,0.0011361013,0.0009030161,0.0024109546,0.0014249186,0.00081118813,0.007330339],"category_scores_gemma":[0.009408197,0.00055960694,0.00044815833,0.0012039492,0.0005502829,0.0024811812,0.0015686413,0.0011128624,0.0009516068],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026680046,0.00011595867,0.02771685,0.00015648504,0.00004979113,0.00008906245,0.0005415609,0.03250239,0.0014000885,0.0066522947,0.41501096,0.5154978],"study_design_scores_gemma":[0.00021008715,0.0001910681,0.100694455,0.0008696044,0.000107890904,0.00012622472,0.0012293012,0.12848176,0.0064453636,0.008542446,0.7529616,0.0001402563],"about_ca_topic_score_codex":0.3410896,"about_ca_topic_score_gemma":0.3452116,"teacher_disagreement_score":0.3410896,"about_ca_system_score_codex":0.002561793,"about_ca_system_score_gemma":0.0060192524,"threshold_uncertainty_score":0.6782085},"labels":[],"label_agreement":null},{"id":"W2029643933","doi":"10.1007/s00024-014-0850-7","title":"Spatio-Temporal Complex Markov Chain (SCMC) Model Using Directed Graphs: Earthquake Sequencing","year":2014,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Markov chain; Computer science; Graph; Directed graph; Event (particle physics); Algorithm; Theoretical computer science; Machine learning","score_opus":0.027015651623682756,"score_gpt":0.21339372288033828,"score_spread":0.18637807125665554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029643933","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.023811612,0.00019607018,0.9720176,0.00037235036,0.000038232243,0.000060226113,0.0006817176,0.0002803606,0.0025418922],"genre_scores_gemma":[0.78550327,0.00092768343,0.20419161,0.0002311099,0.00009964827,0.0004628989,0.0012880089,0.00012428992,0.007171457],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999446,0.00020212689,0.00002518168,0.00016188914,0.000101490594,0.000063337604],"domain_scores_gemma":[0.99581796,0.0030225015,0.0004261546,0.00025847487,0.00031824285,0.00015666337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012172189,0.0005828625,0.0006610511,0.0010940613,0.00040955516,0.0010159222,0.0013982528,0.0009131691,0.003066144],"category_scores_gemma":[0.0059329644,0.0003093271,0.00071677973,0.0016848223,0.0009414079,0.0014954096,0.00069996226,0.0012260701,0.00045723375],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003961082,0.000021551108,0.0015897809,0.00004505176,0.00003350789,0.00014687801,0.00008611388,0.84343755,0.00072421867,0.1428557,0.00094185246,0.010078228],"study_design_scores_gemma":[0.0000062887475,0.0000056831705,0.00013719831,0.0000046197592,0.000007879338,0.000017282522,0.0000070868773,0.9724106,0.0001374652,0.02665814,0.00060047343,0.0000073716615],"about_ca_topic_score_codex":0.018985627,"about_ca_topic_score_gemma":0.0136246225,"teacher_disagreement_score":0.018985627,"about_ca_system_score_codex":0.0015355013,"about_ca_system_score_gemma":0.001436127,"threshold_uncertainty_score":0.037750244},"labels":[],"label_agreement":null},{"id":"W2029889249","doi":"10.1103/physrevlett.114.088501","title":"Foreshock and Aftershocks in Simple Earthquake Models","year":2015,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy","keywords":"Aftershock; Foreshock; Asperity (geotechnical engineering); Seismology; Geology; Scaling; Induced seismicity; Shock (circulatory); Cellular automaton; Statistical physics; Physics; Geometry; Computer science; Mathematics","score_opus":0.042511826051122144,"score_gpt":0.26589105870412993,"score_spread":0.2233792326530078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029889249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7675815,0.0036655022,0.19853091,0.0016206271,0.0002470327,0.000073670315,0.00087782094,0.0005649935,0.026837913],"genre_scores_gemma":[0.99086297,0.00095460203,0.003689447,0.0000621545,0.00006457414,0.00003806421,0.00013216864,0.000028091423,0.004167889],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999337,0.000019835774,0.0000050598464,0.000016025859,0.000012142282,0.00001320589],"domain_scores_gemma":[0.99979454,0.00007846248,0.00005375749,0.000017480585,0.000018289124,0.00003758888],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019413205,0.00044096552,0.00055573654,0.0004740314,0.00034109646,0.0006939952,0.0007649197,0.0008937615,0.0015871065],"category_scores_gemma":[0.00086100155,0.0002909775,0.0005604599,0.00036361816,0.0005985242,0.00087325956,0.000397537,0.00042461534,0.00019217582],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039991857,0.000026169386,0.0014633584,0.000052186333,0.000037135505,0.00018845445,0.00013457268,0.93229836,0.0019825387,0.06032204,0.0006342137,0.002820965],"study_design_scores_gemma":[0.000014798025,0.000023443983,0.0007216134,0.0000070148144,0.000010941619,0.000023851699,0.00002090234,0.9718107,0.00014173091,0.026531875,0.0006836651,0.000009389491],"about_ca_topic_score_codex":0.009888638,"about_ca_topic_score_gemma":0.005416458,"teacher_disagreement_score":0.009888638,"about_ca_system_score_codex":0.0005846413,"about_ca_system_score_gemma":0.00037424435,"threshold_uncertainty_score":0.019662201},"labels":[],"label_agreement":null},{"id":"W2030043506","doi":"10.1029/2006gl026122","title":"Earthquake recurrence as a record breaking process","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Perimeter Institute","funders":"","keywords":"Scaling; Induced seismicity; Magnitude (astronomy); Point process; Observer (physics); Scaling law; Statistical physics; Geology; Computer science; Seismology; Mathematics; Physics; Statistics; Geometry","score_opus":0.03510357604512188,"score_gpt":0.304952378250072,"score_spread":0.2698488022049501,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030043506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6470691,0.0018708792,0.31138018,0.0018095997,0.00011821647,0.0000662774,0.0011738833,0.00056456774,0.035947267],"genre_scores_gemma":[0.98389727,0.0006281578,0.010986455,0.00005367558,0.0001276046,0.000040659634,0.00030606898,0.00005634957,0.003903742],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994603,0.00010347169,0.00005111192,0.00019793783,0.00013363289,0.000053516018],"domain_scores_gemma":[0.99553573,0.0017080616,0.0013394792,0.0006766385,0.00043049504,0.0003096239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014370778,0.00026385268,0.00028877324,0.0013211797,0.00052124064,0.0020253623,0.0007354737,0.00066403364,0.0038968746],"category_scores_gemma":[0.008817383,0.00025066093,0.0003750433,0.0011695008,0.0012832694,0.0045528146,0.00095230644,0.0011240591,0.0004350784],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008314947,0.000033856526,0.0123216305,0.00009943075,0.000042313597,0.00025824463,0.0008666316,0.031334307,0.00531768,0.90915346,0.0013808213,0.039108578],"study_design_scores_gemma":[0.000041771484,0.00013022708,0.025483474,0.000045915694,0.00007744081,0.000487011,0.0002677793,0.23642845,0.0012926229,0.72578317,0.009904949,0.00005711309],"about_ca_topic_score_codex":0.0017993117,"about_ca_topic_score_gemma":0.00073578145,"teacher_disagreement_score":0.0038968746,"about_ca_system_score_codex":0.00064597576,"about_ca_system_score_gemma":0.0002877498,"threshold_uncertainty_score":0.013036311},"labels":[],"label_agreement":null},{"id":"W2030087806","doi":"10.1186/bf03352385","title":"Tomographic image of low P velocity anomalies above slab in northern Cascadia subduction zone","year":2014,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"University of Washington","keywords":"Geology; Subduction; Seismology; Seismic tomography; Slab; Slab window; Oceanic crust; Tomography; Crust; Mantle (geology); Eclogite; Convergent boundary; Geophysics; Tectonics","score_opus":0.005440500805592369,"score_gpt":0.1790469508131764,"score_spread":0.17360645000758404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030087806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99006176,0.000110234054,0.0006282286,0.00016527555,0.000008644464,0.000022517219,0.0025389206,0.00034427698,0.0061201234],"genre_scores_gemma":[0.9968786,0.00009084674,0.0009472959,0.000010487759,0.0000054035086,0.000010619434,0.0010561517,0.00001826436,0.0009822716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999596,0.000003076947,0.0000024849342,0.00001167859,0.000012953666,0.000010116862],"domain_scores_gemma":[0.99987364,0.00001319714,0.00002204354,0.000012531257,0.000032773067,0.000045830835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000067566405,0.00030083943,0.00016880655,0.001231312,0.00029926005,0.0003837166,0.00031918596,0.0002870486,0.0026303802],"category_scores_gemma":[0.0002472284,0.00021645715,0.0002257366,0.0011938796,0.00027292478,0.00012757827,0.0003030881,0.00022012563,0.00028593172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011682743,0.00028407876,0.7106767,0.00058813614,0.00028392952,0.006782068,0.0047230585,0.0654731,0.13142367,0.0012134358,0.009584148,0.06779934],"study_design_scores_gemma":[0.000024368906,0.000022708624,0.9858291,0.000023431796,0.000032702133,0.0001762082,0.00040080084,0.011318431,0.00085580535,0.00007109916,0.0012328945,0.000012488141],"about_ca_topic_score_codex":0.11250748,"about_ca_topic_score_gemma":0.14825065,"teacher_disagreement_score":0.11250748,"about_ca_system_score_codex":0.0006597507,"about_ca_system_score_gemma":0.0006713716,"threshold_uncertainty_score":0.22370517},"labels":[],"label_agreement":null},{"id":"W2030194729","doi":"10.1139/e03-041","title":"A study of the tectonically active Marmara region, Turkey, using a global positioning system (GPS)","year":2003,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; North Anatolian Fault; Seismology; Sinistral and dextral; Global Positioning System; Geodesy; Active fault; Tectonics; Fault (geology); Eurasian Plate; Vertical displacement; Magnitude (astronomy); Displacement (psychology); Deformation (meteorology); Geomorphology; Subduction; Oceanography","score_opus":0.03493603550334034,"score_gpt":0.23747719157606476,"score_spread":0.2025411560727244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030194729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99915576,0.00013474592,0.00012672908,0.000017038948,0.0000026708203,0.0000124184735,0.00021004556,0.000002619889,0.00033800062],"genre_scores_gemma":[0.99838257,0.00017138176,0.0005620991,0.000012026383,0.000008689077,0.000016669232,0.0006700988,0.0000022566667,0.00017426534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996112,0.00012771241,0.00003987859,0.00010189757,0.00005681019,0.0000624329],"domain_scores_gemma":[0.9995783,0.000091179245,0.00012854325,0.00003552598,0.00010798208,0.000058481906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053249695,0.0005522225,0.00034816866,0.0011242186,0.00064034876,0.0005534371,0.00039144015,0.00054914097,0.00034690058],"category_scores_gemma":[0.0010755489,0.0002348983,0.00025910142,0.0017666295,0.0003138432,0.00052682974,0.00030055016,0.00016614758,0.00014117625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003206437,0.0004480506,0.9389911,0.00025640306,0.00019126444,0.003328412,0.005225669,0.0032765598,0.009158395,0.00025973044,0.00046773822,0.038076002],"study_design_scores_gemma":[0.000005263131,0.00020439543,0.99641377,0.000009049441,0.000030707666,0.00033698272,0.0013804332,0.00069286313,0.0003461644,0.00001959147,0.00055239315,0.000008430617],"about_ca_topic_score_codex":0.034440923,"about_ca_topic_score_gemma":0.043708596,"teacher_disagreement_score":0.034440923,"about_ca_system_score_codex":0.0007755905,"about_ca_system_score_gemma":0.00058323453,"threshold_uncertainty_score":0.06848091},"labels":[],"label_agreement":null},{"id":"W2031245129","doi":"10.1144/0016-76492009-019","title":"Fault-controlled alpine topography in Norway","year":2010,"lang":"en","type":"article","venue":"Journal of the Geological Society","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Paleontology; Fault (geology); Geomorphology","score_opus":0.00986136325499212,"score_gpt":0.21088387174055476,"score_spread":0.20102250848556263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031245129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962412,0.00021956979,0.000106039995,0.00002437039,0.000006070957,0.0000033537117,0.00048247873,0.000009018747,0.002907991],"genre_scores_gemma":[0.99913776,0.000101498204,0.00009047312,0.000007359352,0.0000020468715,0.0000025038742,0.0003076815,0.0000018276088,0.00034888196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988425,0.000014034773,0.000010566537,0.0000342345,0.000015368063,0.000041461535],"domain_scores_gemma":[0.99982065,0.000029353625,0.00006281486,0.000009983945,0.00004510198,0.00003216136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001713675,0.000099406636,0.000103491104,0.0004698038,0.00028107897,0.00067952386,0.00014951629,0.00012372177,0.0012812745],"category_scores_gemma":[0.00037434534,0.00008961292,0.00008161414,0.0004967,0.0003718242,0.0002494365,0.00041420024,0.000068392736,0.00018386835],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025326433,0.00006569995,0.9363476,0.0001890637,0.000058373025,0.0019021747,0.0029276519,0.0037018482,0.015274137,0.001690613,0.0011784087,0.03641123],"study_design_scores_gemma":[0.000011863961,0.00004254888,0.9937611,0.000037445014,0.000010234037,0.00030864574,0.0011193536,0.0005578139,0.0002280928,0.00016015231,0.0037566898,0.0000060055545],"about_ca_topic_score_codex":0.07575282,"about_ca_topic_score_gemma":0.14346148,"teacher_disagreement_score":0.07575282,"about_ca_system_score_codex":0.00076210254,"about_ca_system_score_gemma":0.00055677065,"threshold_uncertainty_score":0.1506238},"labels":[],"label_agreement":null},{"id":"W2031422476","doi":"10.1134/s0001437009020027","title":"The Kuril Earthquakes and tsunamis of November 15, 2006, and January 13, 2007: Observations, analysis, and numerical modeling","year":2009,"lang":"en","type":"article","venue":"Oceanology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Russian Foundation for Basic Research","keywords":"Seismology; Geology; Pacific ocean; Seismic zone; Tsunami wave; Oceanography; Induced seismicity","score_opus":0.016373022344068865,"score_gpt":0.21822948419790603,"score_spread":0.20185646185383715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031422476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99534696,0.000104761864,0.0025204269,0.00010164293,0.0000079905585,0.000019186093,0.0005083736,0.000073091986,0.0013176466],"genre_scores_gemma":[0.9974305,0.0001336091,0.0017374902,0.000006787715,0.000008128938,0.0000258836,0.00037017066,0.000007755052,0.00027961246],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999238,0.000019640676,0.0000066374746,0.000016008651,0.000015810003,0.000017995406],"domain_scores_gemma":[0.9998186,0.000058336354,0.0000621926,0.000013960593,0.000022764205,0.000024165927],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020165936,0.0004308948,0.00027495675,0.000349664,0.00031531093,0.00047127836,0.000583497,0.0005416958,0.0006276078],"category_scores_gemma":[0.00069743634,0.00032311134,0.00034385832,0.0005226683,0.00043006832,0.0006166815,0.00039765736,0.00035357525,0.00014765476],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008090523,0.00013690484,0.051947873,0.000041696396,0.000038238868,0.00017156867,0.00013101779,0.9399558,0.0011150764,0.0014640959,0.0005480465,0.0043688696],"study_design_scores_gemma":[0.000022256512,0.000023249495,0.01756146,0.000005123681,0.000010751764,0.000022110453,0.000047642076,0.98160845,0.00025308898,0.00018573973,0.0002490467,0.000011054989],"about_ca_topic_score_codex":0.029992227,"about_ca_topic_score_gemma":0.018448621,"teacher_disagreement_score":0.029992227,"about_ca_system_score_codex":0.0008332422,"about_ca_system_score_gemma":0.0006404604,"threshold_uncertainty_score":0.05963528},"labels":[],"label_agreement":null},{"id":"W2031578087","doi":"10.1029/2009gl037160","title":"Spatiotemporal gravity changes on volcanoes: Assessing the importance of topography","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministerio de Ciencia e Innovación","keywords":"Geology; Volcano; Deformation (meteorology); Gravity anomaly; Seismology; Mass movement; Magma; Geophysics; Geodesy; Gravity current; Landslide","score_opus":0.052555781480583263,"score_gpt":0.3283430005099931,"score_spread":0.27578721902940984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031578087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991578,0.00004071865,0.00055862754,0.000012672516,0.00000102411,0.000002562558,0.00005588807,0.000012642701,0.00015800114],"genre_scores_gemma":[0.9996805,0.000028564205,0.0002247782,0.0000011516953,0.0000019729873,0.0000010135276,0.000037775837,0.000001766358,0.000022443342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998988,0.000023812405,0.000010323271,0.00002291996,0.000025401048,0.000018715898],"domain_scores_gemma":[0.9994241,0.0002335349,0.00017111952,0.00005544333,0.00006390301,0.00005200433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033779241,0.00019681685,0.00017938578,0.0008593705,0.00012615202,0.00030189415,0.00025876393,0.00031180232,0.0004197091],"category_scores_gemma":[0.0021435583,0.00009603398,0.00024389282,0.00053513516,0.00033289264,0.0005493386,0.00041955808,0.00011331302,0.00005949998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004731838,0.0001559728,0.7946145,0.00013465407,0.0002042332,0.00074007065,0.00034187917,0.10945323,0.05728023,0.0012030222,0.00023137312,0.035167575],"study_design_scores_gemma":[0.000016914335,0.000188682,0.7838143,0.00000884238,0.00005134333,0.0002063156,0.00023730002,0.21149053,0.0034434304,0.00037566468,0.0001503984,0.000016172606],"about_ca_topic_score_codex":0.004868431,"about_ca_topic_score_gemma":0.003996985,"teacher_disagreement_score":0.004868431,"about_ca_system_score_codex":0.000299951,"about_ca_system_score_gemma":0.00012912895,"threshold_uncertainty_score":0.009680152},"labels":[],"label_agreement":null},{"id":"W2032243612","doi":"10.1144/sp291.5","title":"Distribution and chronology of submarine volcanic rocks around Santorini and their relationship to faulting","year":2007,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography; Geological Survey of Canada","funders":"","keywords":"Chronology; Geology; Submarine; Volcano; Volcanic rock; Submarine volcano; Paleontology; Geochemistry; Seismology; Oceanography","score_opus":0.025202792099087944,"score_gpt":0.24249043351442692,"score_spread":0.217287641415339,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032243612","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99664354,0.0003000509,0.000040404782,0.00003314279,0.0000036859508,0.0000064202763,0.00042291608,0.0000066057764,0.0025432808],"genre_scores_gemma":[0.9988412,0.00014614986,0.00012698154,0.000005445652,0.000005115473,0.00000423889,0.00044217924,0.0000015194585,0.0004271037],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991107,0.0000100196075,0.000015170635,0.000028044411,0.000014613715,0.000021011485],"domain_scores_gemma":[0.9994906,0.00005327566,0.0002596977,0.000042953536,0.0001017309,0.000051655654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018439419,0.00014632284,0.000102167854,0.0015578469,0.00021211863,0.00032805966,0.00021136136,0.00015499744,0.001639293],"category_scores_gemma":[0.0004716716,0.000116953015,0.00010779979,0.000979549,0.00039328248,0.0002170598,0.0003075832,0.00011371167,0.00021339033],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004903565,0.0000072879707,0.9745807,0.000049513652,0.00002582731,0.00019912522,0.0007280962,0.0002317249,0.006199654,0.00017517456,0.00029057442,0.01746334],"study_design_scores_gemma":[0.0000011017756,0.00000889705,0.9986929,0.0000052411306,0.0000026111718,0.00011676346,0.00010303563,0.00008246183,0.00014211732,0.000012474298,0.0008312009,0.0000011681424],"about_ca_topic_score_codex":0.015640462,"about_ca_topic_score_gemma":0.03356853,"teacher_disagreement_score":0.015640462,"about_ca_system_score_codex":0.00060223986,"about_ca_system_score_gemma":0.0002599769,"threshold_uncertainty_score":0.031098843},"labels":[],"label_agreement":null},{"id":"W2032344151","doi":"10.1007/978-3-0348-7897-5_12","title":"Methods for Evaluation of Geodetic Data and Seismicity Developed with Numerical Simulations: Review and Applications","year":2004,"lang":"en","type":"book-chapter","venue":"Birkhäuser Basel eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geodetic datum; Induced seismicity; Computer science; Global Positioning System; Visualization; Field (mathematics); Data mining; Geology; Seismology; Geodesy; Mathematics","score_opus":0.12016739963110173,"score_gpt":0.3553260287390381,"score_spread":0.2351586291079364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032344151","genre_codex":"methods","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.001218118,0.3134458,0.6651597,0.00063553767,0.0009662526,0.0001654287,0.00028791442,0.0011619406,0.016959354],"genre_scores_gemma":[0.020947978,0.36880583,0.5967628,0.00046455473,0.0010560006,0.00061515067,0.00067351083,0.00069831364,0.009975917],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978002,0.00069524767,0.00020478037,0.00025410214,0.0010073684,0.00003828993],"domain_scores_gemma":[0.99620926,0.0026698192,0.00016960735,0.00024150936,0.0006694163,0.000040348103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00315857,0.0019262066,0.002129134,0.0052601458,0.0003364474,0.002318619,0.00237412,0.0017780861,0.005177163],"category_scores_gemma":[0.008828734,0.001000106,0.00092495425,0.007524321,0.0018059812,0.0026240617,0.0013451953,0.0014382977,0.0037339174],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040378127,0.0000575901,0.0008079673,0.004114033,0.00013964459,0.00012267775,0.00021814933,0.024677744,0.0017687224,0.07895008,0.016821405,0.8722817],"study_design_scores_gemma":[0.000050633207,0.0001117013,0.0023409377,0.003990768,0.0001637201,0.0013920205,0.00030919467,0.14904982,0.0056381803,0.15712935,0.67957807,0.0002455729],"about_ca_topic_score_codex":0.002254952,"about_ca_topic_score_gemma":0.0014983511,"teacher_disagreement_score":0.0052601458,"about_ca_system_score_codex":0.0010262468,"about_ca_system_score_gemma":0.0010949188,"threshold_uncertainty_score":0.017319381},"labels":[],"label_agreement":null},{"id":"W2032887332","doi":"10.1680/geolett.11.00022","title":"Evaluating seismic source mechanism with phasor analysis","year":2012,"lang":"en","type":"article","venue":"Géotechnique Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada; Australian Centre for Geomechanics","keywords":"Phasor; Seismology; Geology; Population; Mechanism (biology); Seismic analysis; Geotechnical engineering; Electric power system; Power (physics); Physics","score_opus":0.027555777203204956,"score_gpt":0.25907448306585634,"score_spread":0.23151870586265139,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032887332","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.21806604,0.00028878407,0.77496487,0.000065469016,0.000025182944,0.00014068683,0.00065673725,0.001736198,0.004056024],"genre_scores_gemma":[0.87095034,0.0002935087,0.12656435,0.000016400525,0.00003770497,0.0000927027,0.0006642476,0.00009245761,0.0012882967],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99962056,0.00008967395,0.000031520995,0.00006236426,0.00015803348,0.00003780705],"domain_scores_gemma":[0.99865735,0.0006771544,0.00017312709,0.00013342993,0.0003048105,0.00005415461],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00083274976,0.0005996342,0.00049647136,0.004573506,0.00024724158,0.00081403076,0.00038969357,0.0004766156,0.0048026005],"category_scores_gemma":[0.0033346447,0.00023483246,0.00041427033,0.0021348067,0.0002551414,0.0012243965,0.00054693944,0.00024559558,0.0008270481],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008697878,0.00031758117,0.07034721,0.00059135497,0.0003251347,0.0010195437,0.0004828193,0.2338247,0.11843844,0.018173564,0.0019979314,0.55361193],"study_design_scores_gemma":[0.00006157864,0.00045886938,0.044700045,0.00003795719,0.00011148017,0.0005862886,0.00035144525,0.918308,0.020447757,0.011866313,0.0030082127,0.00006205161],"about_ca_topic_score_codex":0.0011391699,"about_ca_topic_score_gemma":0.0005964172,"teacher_disagreement_score":0.0048026005,"about_ca_system_score_codex":0.00020087618,"about_ca_system_score_gemma":0.0002447573,"threshold_uncertainty_score":0.016066372},"labels":[],"label_agreement":null},{"id":"W2033046317","doi":"10.1139/t06-065","title":"Revising the areal extent of post-earthquake inspections of dams in Quebec","year":2006,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"Magnitude (astronomy); Epicenter; Earthquake scenario; Seismology; Ground motion; Urban seismic risk; Strong ground motion; Geology; Forensic engineering; Seismic hazard; Engineering","score_opus":0.012154351474363586,"score_gpt":0.21481123468531108,"score_spread":0.2026568832109475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033046317","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9753783,0.000957695,0.004460822,0.00083781325,0.000020956357,0.00010412176,0.002915808,0.00013716654,0.01518742],"genre_scores_gemma":[0.99486864,0.00030001483,0.001915158,0.00005174434,0.0000037000134,0.000016179067,0.00058329804,0.000009505398,0.00225172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99943095,0.00009725424,0.000040298863,0.00010209151,0.0002038028,0.00012556129],"domain_scores_gemma":[0.99398863,0.0010352975,0.0010535876,0.00023706684,0.0034096711,0.00027573135],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010427863,0.00012378549,0.00014483779,0.0015600935,0.00095251296,0.0008306448,0.00073729677,0.0001934445,0.0014443363],"category_scores_gemma":[0.0045166635,0.00010619864,0.00013212145,0.0023026757,0.0006377942,0.00040917564,0.00045007246,0.0002502433,0.00010943572],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000107424596,0.000056777848,0.8025669,0.00027217055,0.000048498852,0.0005259179,0.004454488,0.012822089,0.0049240664,0.002902369,0.008653502,0.16266587],"study_design_scores_gemma":[0.0000017274251,0.000017668364,0.9871913,0.00003083484,0.000009489781,0.000057378536,0.0012361472,0.0030874948,0.000468848,0.00006475763,0.007820851,0.000013536202],"about_ca_topic_score_codex":0.9615389,"about_ca_topic_score_gemma":0.985897,"teacher_disagreement_score":0.03846109,"about_ca_system_score_codex":0.015216112,"about_ca_system_score_gemma":0.011141896,"threshold_uncertainty_score":0.11040115},"labels":[],"label_agreement":null},{"id":"W2033114859","doi":"10.1111/j.1365-246x.2007.03455.x","title":"Upper-crustal structure beneath the Strait of Georgia, Southwest British Columbia","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; McGill University; University of Victoria","funders":"","keywords":"Geology; Structural basin; Seismology; Sedimentary basin; Seismic refraction; Inversion (geology); Basement; Cretaceous; Sedimentary rock; Terrane; Basin and range topography; Thrust fault; Trough (economics); Fault (geology); Geomorphology; Paleontology; Tectonics","score_opus":0.0069262318118360165,"score_gpt":0.20886266359699937,"score_spread":0.20193643178516335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033114859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9673198,0.00037486813,0.008564773,0.00023789558,0.000012901568,0.000044376324,0.003063044,0.00038800997,0.019994259],"genre_scores_gemma":[0.99092215,0.00020705756,0.0025906086,0.000030423082,0.0000011885428,0.00001375488,0.0008774252,0.000022361362,0.005335081],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999959,0.0000028815746,0.00000200526,0.000011331368,0.000012284211,0.000012520918],"domain_scores_gemma":[0.9999398,0.000004572278,0.0000072237394,0.0000048316874,0.000031650783,0.000011835859],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000032301596,0.00030834426,0.00014493754,0.00039487836,0.0006608003,0.0012445071,0.00071383617,0.00031056994,0.0020897137],"category_scores_gemma":[0.0001900868,0.00024299526,0.00020866354,0.0005395218,0.00024939227,0.00022512939,0.00031548293,0.00023537809,0.00046717215],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000076741955,0.000070480964,0.27041292,0.00011993734,0.00010629214,0.0006757542,0.0007473696,0.6261383,0.011251008,0.004920968,0.008000841,0.07747929],"study_design_scores_gemma":[0.000024916293,0.00001958274,0.23348366,0.00006141721,0.00004492711,0.00017975402,0.0005382892,0.7490771,0.0007894355,0.0011692941,0.014555396,0.000056217512],"about_ca_topic_score_codex":0.9673913,"about_ca_topic_score_gemma":0.97719383,"teacher_disagreement_score":0.032608688,"about_ca_system_score_codex":0.0057059126,"about_ca_system_score_gemma":0.005847052,"threshold_uncertainty_score":0.06560141},"labels":[],"label_agreement":null},{"id":"W2033178207","doi":"10.1016/j.jsg.2011.11.016","title":"Paradoxical pseudotachylyte – Fault melt outside the seismogenic zone","year":2011,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Slip (aerodynamics); Seismology; Crystal plasticity; Nucleation; Climb; Tectonics; Fault (geology); Creep; Brittleness; Instability; Intraplate earthquake; Petrology; Plasticity; Mechanics; Composite material; Materials science","score_opus":0.02681194547300365,"score_gpt":0.22337591276942814,"score_spread":0.1965639672964245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033178207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940836,0.000101611644,0.0003398016,0.00041434483,0.000022396449,0.000002989578,0.00006253607,0.000024192836,0.00494858],"genre_scores_gemma":[0.9997009,0.000021241076,0.00003147024,0.000018261771,0.000010682284,5.908215e-7,0.000029645176,0.000003852589,0.00018330198],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997929,0.000025781868,0.00001990005,0.000040128034,0.000050123323,0.00007120096],"domain_scores_gemma":[0.9989987,0.00026014211,0.00028329383,0.00021446226,0.00013359282,0.00010978174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003322905,0.0000975922,0.00037221148,0.00059283455,0.0010456877,0.001403967,0.00042195828,0.0007329932,0.0047606663],"category_scores_gemma":[0.0033090226,0.00015178736,0.00017787653,0.00065093127,0.0015807247,0.0012140283,0.0014325734,0.00071200414,0.00033052024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0073728207,0.00037257173,0.53449714,0.0005158882,0.00041119131,0.009582302,0.010222491,0.012239891,0.23804906,0.123716034,0.00395373,0.059066843],"study_design_scores_gemma":[0.00027959477,0.00034909527,0.88925374,0.000051983698,0.00014502241,0.0035757686,0.006396044,0.008450333,0.018165603,0.059237175,0.014043325,0.000052365835],"about_ca_topic_score_codex":0.0032870562,"about_ca_topic_score_gemma":0.0051157307,"teacher_disagreement_score":0.0047606663,"about_ca_system_score_codex":0.00075133005,"about_ca_system_score_gemma":0.00049840874,"threshold_uncertainty_score":0.015925944},"labels":[],"label_agreement":null},{"id":"W2033195642","doi":"10.1016/j.margeo.2014.03.009","title":"Complex interactions fault fans developed in a strike-slip system: Kozan Fault Zone, Eastern Mediterranean Sea","year":2014,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"National University of Science and Technology; Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland","keywords":"Geology; Fault (geology); Strike-slip tectonics; Structural basin; Slip (aerodynamics); Quaternary; Seismology; Paleontology","score_opus":0.0357122015119372,"score_gpt":0.24986235263337184,"score_spread":0.21415015112143465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033195642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941254,0.0000181562,0.00007080423,0.00000772268,0.000001006904,0.0000030090143,0.000046220972,0.000002348349,0.0004382698],"genre_scores_gemma":[0.99966824,0.000010556398,0.000061242376,0.0000012857823,9.907795e-7,0.000001327115,0.00005966513,8.2972423e-7,0.00019592962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999819,0.000030779775,0.000019348427,0.000054570915,0.000024350617,0.000052102187],"domain_scores_gemma":[0.9998005,0.000027060298,0.000057855174,0.000013343249,0.000059139235,0.000042242456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001675535,0.00023354811,0.00024442593,0.0012464059,0.0004833065,0.00073159015,0.0003151781,0.0002945519,0.0017097506],"category_scores_gemma":[0.0006226259,0.000172401,0.00016944807,0.0011102537,0.000757921,0.00032389007,0.00044919594,0.00009756596,0.00014182931],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039399782,0.000065247805,0.964464,0.00006104216,0.00008825528,0.0016902968,0.001687315,0.010217924,0.007979301,0.0015746428,0.00029931124,0.011478627],"study_design_scores_gemma":[0.000011784675,0.00003832393,0.99350995,0.0000061016467,0.000016699954,0.00015197806,0.0010662529,0.004532887,0.00013130886,0.00020096818,0.0003286247,0.00000502574],"about_ca_topic_score_codex":0.020852296,"about_ca_topic_score_gemma":0.035601694,"teacher_disagreement_score":0.020852296,"about_ca_system_score_codex":0.00092150294,"about_ca_system_score_gemma":0.00050152314,"threshold_uncertainty_score":0.041461825},"labels":[],"label_agreement":null},{"id":"W2034174370","doi":"10.1126/science.1150558","title":"Tidal Modulation of Nonvolcanic Tremor","year":2007,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":268,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Episodic tremor and slip; Slip (aerodynamics); Tectonics","score_opus":0.01662265237647677,"score_gpt":0.23680482757413862,"score_spread":0.22018217519766184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034174370","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99445325,0.00013730652,0.00029511072,0.00005575626,0.000015717194,0.000009924932,0.00024037242,0.000038214555,0.0047543026],"genre_scores_gemma":[0.9992543,0.00004078516,0.000045077813,0.000010707612,0.000007798844,0.0000025113434,0.00012011192,0.0000049935115,0.0005137841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999913,0.00000887959,0.0000062792656,0.000016824199,0.000029474946,0.000025531242],"domain_scores_gemma":[0.999634,0.00006568431,0.00009135423,0.00003746704,0.00010813444,0.00006331279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006996505,0.000116482675,0.00015364954,0.00058855803,0.00024468405,0.00049150235,0.00020251331,0.00019855208,0.0013004954],"category_scores_gemma":[0.00088704436,0.000112729205,0.00008557109,0.0004820546,0.00020630186,0.0001414819,0.0003370815,0.00016357556,0.00021792142],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008583136,0.00022535336,0.5001823,0.000143647,0.000112813716,0.0012836495,0.0017766878,0.0027789117,0.39218825,0.0016299381,0.0031909035,0.095629245],"study_design_scores_gemma":[0.000013446541,0.00006605252,0.994865,0.0000041058197,0.000013236696,0.000086270724,0.00013555333,0.0013525569,0.0023078914,0.00013927501,0.0010083478,0.000008346257],"about_ca_topic_score_codex":0.006329558,"about_ca_topic_score_gemma":0.011728004,"teacher_disagreement_score":0.006329558,"about_ca_system_score_codex":0.00040237894,"about_ca_system_score_gemma":0.0001999656,"threshold_uncertainty_score":0.012585461},"labels":[],"label_agreement":null},{"id":"W2034213279","doi":"10.1029/2012jb009306","title":"Mantle flow uplift of western Anatolia and the Aegean: Interpretations from geophysical analyses and geodynamic modeling","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lithosphere; Mantle (geology); Geophysics; Tectonics; Crust; Geodynamics; Gravity anomaly; North Anatolian Fault; Ocean surface topography; Seismology; Geodesy; Paleontology","score_opus":0.055750278979633965,"score_gpt":0.341854041319119,"score_spread":0.28610376233948503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034213279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99739254,0.00008700232,0.00051616994,0.00009529818,0.0000028421923,0.000004330512,0.00014585663,0.000026133772,0.0017298558],"genre_scores_gemma":[0.9991486,0.000094956755,0.00044775053,0.0000061196324,0.0000019481704,0.00000383497,0.00009637974,0.000007509724,0.00019297661],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99997497,0.000006286642,0.000003116176,0.000007333186,0.0000035728158,0.000004743262],"domain_scores_gemma":[0.99995995,0.000010891327,0.000012632945,0.0000044946655,0.000007838881,0.0000042108186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009658115,0.00024053162,0.00015344558,0.00041642462,0.00021154077,0.00078517565,0.00030966432,0.0003143867,0.00086529314],"category_scores_gemma":[0.00025144964,0.0001875825,0.0002776498,0.00043952375,0.00027691826,0.00031007646,0.00032087442,0.00014963465,0.00010701188],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018478527,0.0000824318,0.25979748,0.00011476862,0.00021679663,0.00071813446,0.0005427926,0.6908724,0.018349906,0.0057220096,0.0005568502,0.022841735],"study_design_scores_gemma":[0.00004419801,0.000024924577,0.16777931,0.000032396918,0.00007566521,0.00012586772,0.00040658354,0.8267071,0.0012313969,0.0015305681,0.002017507,0.00002447963],"about_ca_topic_score_codex":0.058686677,"about_ca_topic_score_gemma":0.03885796,"teacher_disagreement_score":0.058686677,"about_ca_system_score_codex":0.0009695884,"about_ca_system_score_gemma":0.0004994379,"threshold_uncertainty_score":0.11669016},"labels":[],"label_agreement":null},{"id":"W2034430788","doi":"10.1190/1.1815676","title":"Using microseismicity to map cotton valley hydraulic fractures","year":2000,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Apheresis Group","funders":"","keywords":"Geology; Hydraulic fracturing; Hydrology (agriculture); Geotechnical engineering","score_opus":0.025164342541199956,"score_gpt":0.25555691100763117,"score_spread":0.23039256846643122,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034430788","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7872623,0.0009884981,0.100379616,0.00095596863,0.00022479173,0.00029008792,0.03017924,0.0058521987,0.073867306],"genre_scores_gemma":[0.93884665,0.00033417088,0.043933768,0.000040165625,0.00006414343,0.0000785211,0.008745118,0.0003334565,0.007623936],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99977857,0.000013773073,0.000008586939,0.000041032778,0.000120662895,0.000037457667],"domain_scores_gemma":[0.9994968,0.00006320011,0.00006848175,0.000044234203,0.0002612454,0.00006586955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025404882,0.00027476545,0.00009841816,0.0040672007,0.00035097703,0.0007990466,0.00026594792,0.00029286227,0.005513066],"category_scores_gemma":[0.0010668758,0.00015109855,0.00020914755,0.0024242557,0.000108286076,0.00049111503,0.00066154485,0.00028417364,0.002040336],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025117982,0.00009720875,0.35043338,0.00019918378,0.000106291445,0.0006060513,0.0010470089,0.019934742,0.03855666,0.0022096438,0.038149185,0.5484094],"study_design_scores_gemma":[0.000040486833,0.00009708138,0.8210859,0.0001586524,0.000056051846,0.0003748527,0.0013321659,0.08419762,0.02268725,0.0025879715,0.06727353,0.00010844473],"about_ca_topic_score_codex":0.026123695,"about_ca_topic_score_gemma":0.05787074,"teacher_disagreement_score":0.026123695,"about_ca_system_score_codex":0.00032903848,"about_ca_system_score_gemma":0.0006532114,"threshold_uncertainty_score":0.051943302},"labels":[],"label_agreement":null},{"id":"W2034502165","doi":"10.1007/s00024-008-0332-x","title":"Earthquakes: Simulations, Sources and Tsunamis","year":2008,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Death toll; Seismology; Toll; Earthquake casualty estimation; Natural hazard; Natural disaster; Geology; Geography; Urban seismic risk; Seismic hazard; Socioeconomics; Oceanography","score_opus":0.012695614282022361,"score_gpt":0.18849543372966493,"score_spread":0.17579981944764256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034502165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.903755,0.0007417092,0.053133745,0.0017631972,0.00031707674,0.00010442678,0.014435443,0.002365619,0.023383778],"genre_scores_gemma":[0.98140246,0.0002607777,0.012430804,0.0000676098,0.00004294639,0.0000781223,0.0025911455,0.00013761967,0.0029885941],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99975926,0.000113436945,0.000018963077,0.000043479664,0.00003391697,0.0000309203],"domain_scores_gemma":[0.9981615,0.0013134272,0.00011607764,0.00012999446,0.00016482499,0.00011416658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070482463,0.00046934767,0.0004975914,0.00053249823,0.0002971049,0.0007949054,0.0009944589,0.0017484208,0.0069087045],"category_scores_gemma":[0.0040373066,0.0005969569,0.00059580983,0.0010405335,0.00043637186,0.0009181376,0.00046139714,0.0008731988,0.0007517894],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000116407864,0.000074173084,0.0028035094,0.000038354963,0.000038185037,0.000034364974,0.00002522996,0.990031,0.00014042259,0.0017684513,0.0014771427,0.0034526994],"study_design_scores_gemma":[0.000091077265,0.000032731048,0.0010424961,0.0000073618426,0.000023310431,0.000022192286,0.000022115782,0.99558496,0.0003763064,0.0017058441,0.0010813533,0.0000102223685],"about_ca_topic_score_codex":0.018187258,"about_ca_topic_score_gemma":0.015343778,"teacher_disagreement_score":0.018187258,"about_ca_system_score_codex":0.0006217041,"about_ca_system_score_gemma":0.00059643254,"threshold_uncertainty_score":0.036162794},"labels":[],"label_agreement":null},{"id":"W2035142411","doi":"10.1029/2011jb008213","title":"Seismic hazard in western Canada from GPS strain rates versus earthquake catalog","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Seismic hazard; Seismic moment; Global Positioning System; Geodesy; Magnitude (astronomy); Earthquake rupture; Moment magnitude scale; Fault (geology)","score_opus":0.0610174355225578,"score_gpt":0.28969410868032985,"score_spread":0.22867667315777207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035142411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97608155,0.0002316824,0.001427554,0.00015877759,0.0000056486915,0.00004806161,0.014326679,0.00013068724,0.007589173],"genre_scores_gemma":[0.9890056,0.00016249824,0.0014399815,0.000040737887,0.000002557517,0.000016681892,0.0076655555,0.000029038049,0.001637216],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996228,0.00003416343,0.000018747456,0.000073731804,0.00014532763,0.00010521992],"domain_scores_gemma":[0.9988901,0.0001378422,0.00017363642,0.00006400862,0.00060062885,0.00013384354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044424253,0.00047244644,0.00022348264,0.0022450201,0.0010723936,0.0014964895,0.00085151364,0.00027863655,0.0027796451],"category_scores_gemma":[0.0024984716,0.00021730519,0.00030104627,0.003677941,0.00058565463,0.0004693374,0.0006695553,0.00033417597,0.00033126443],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017935703,0.000040673534,0.9397804,0.00004962416,0.00011228127,0.00014127724,0.0005013191,0.035953432,0.0009211239,0.0016029037,0.004175248,0.016542342],"study_design_scores_gemma":[0.000032579246,0.00003308668,0.92166656,0.00004143047,0.000070447655,0.000077204,0.001548281,0.070400864,0.0007446392,0.0007290616,0.004606992,0.000048881644],"about_ca_topic_score_codex":0.995421,"about_ca_topic_score_gemma":0.9965333,"teacher_disagreement_score":0.022945609,"about_ca_system_score_codex":0.022945609,"about_ca_system_score_gemma":0.014350097,"threshold_uncertainty_score":0.16648287},"labels":[],"label_agreement":null},{"id":"W2035538442","doi":"10.1029/2007gl030685","title":"Double jeopardy: Concurrent arrival of the 2004 Sumatra tsunami and storm‐generated waves on the Atlantic coast of the United States and Canada","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration; Russian Foundation for Basic Research","keywords":"Tide gauge; Nova scotia; Geology; Storm; Oceanography; Shore; Submarine pipeline; Arrival time; East coast; Seismology; Climatology; Sea level","score_opus":0.03387425765395936,"score_gpt":0.262020335632289,"score_spread":0.22814607797832964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035538442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782383,0.00016905008,0.000023404129,0.00020348148,0.000012931349,0.00000600441,0.00038748863,0.0000043846876,0.0013694251],"genre_scores_gemma":[0.99858296,0.00020835607,0.000051343257,0.00007115136,0.0000067598653,0.0000042210754,0.00040345755,0.000002456943,0.00066925446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99964964,0.000023535176,0.000021987715,0.00004722253,0.00012865335,0.00012886898],"domain_scores_gemma":[0.9981717,0.0001256648,0.00041534394,0.00008808278,0.0008314023,0.00036775926],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027641313,0.00020074063,0.0002287024,0.0013570505,0.0016610902,0.0011798441,0.00036306432,0.00033036145,0.001097836],"category_scores_gemma":[0.0019315381,0.00020563239,0.00014191169,0.0018284651,0.00064664596,0.00042134066,0.00154046,0.0006156619,0.00013573573],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119391436,0.000024850051,0.9847246,0.000018163564,0.00008068528,0.0008541277,0.0017453326,0.000169255,0.0008775887,0.000084980646,0.0014063665,0.009894784],"study_design_scores_gemma":[0.0000024015496,0.000010598216,0.9949181,0.000009120886,0.000019006711,0.0001488552,0.003317747,0.00014735562,0.00014132328,0.000022934912,0.0012538086,0.000008867919],"about_ca_topic_score_codex":0.8957279,"about_ca_topic_score_gemma":0.96438617,"teacher_disagreement_score":0.10427213,"about_ca_system_score_codex":0.005892166,"about_ca_system_score_gemma":0.0054954686,"threshold_uncertainty_score":0.20977235},"labels":[],"label_agreement":null},{"id":"W2035662210","doi":"10.1029/2006jf000499","title":"Numerical simulation of the landslide‐generated tsunami in Kitimat Arm, British Columbia, Canada, 27 April 1975","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Landslide; Submarine landslide; Seismology; Debris flow; Debris; Amplitude; Geomorphology; Oceanography","score_opus":0.02295017886450193,"score_gpt":0.2748271685455846,"score_spread":0.25187698968108263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035662210","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9806794,0.000094856536,0.00093529426,0.00017434795,0.000016478783,0.000054148124,0.0007839117,0.00011585381,0.01714568],"genre_scores_gemma":[0.9912226,0.00011161483,0.0015741903,0.00003469607,0.0000027205622,0.000059906055,0.00089712144,0.000024176272,0.0060729524],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998846,0.000008875376,0.0000038505164,0.00001382892,0.00002966536,0.00005916254],"domain_scores_gemma":[0.9996176,0.0000748973,0.000022730343,0.000011095511,0.00019140623,0.00008226817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015217632,0.0005645152,0.00034460786,0.0005127266,0.0020627524,0.0010227165,0.0012055328,0.00079964346,0.0037286086],"category_scores_gemma":[0.0011350958,0.00044089006,0.00022392775,0.0006578941,0.00090285344,0.00022852694,0.0004713952,0.00052886386,0.00034295244],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017753997,0.00010084194,0.025949396,0.000037203044,0.00003444948,0.0003679942,0.00017470597,0.96385354,0.0014677602,0.0008635959,0.002217091,0.004755931],"study_design_scores_gemma":[0.00008461288,0.000036928865,0.011927312,0.000014606449,0.000021767988,0.000021391548,0.00036484795,0.9846197,0.0007973851,0.00016741676,0.0019254156,0.000018747041],"about_ca_topic_score_codex":0.9630223,"about_ca_topic_score_gemma":0.9599353,"teacher_disagreement_score":0.03697771,"about_ca_system_score_codex":0.014950912,"about_ca_system_score_gemma":0.010492194,"threshold_uncertainty_score":0.108477},"labels":[],"label_agreement":null},{"id":"W2036310474","doi":"10.1029/2005jb003727","title":"Spatial‐temporal patterns of seismic tremors in northern Cascadia","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Subduction; Slip (aerodynamics); Episodic tremor and slip; Seismometer; Seismic array; Crust; Geodesy; Tectonics; Geophysics","score_opus":0.024521230276603266,"score_gpt":0.27466736461013075,"score_spread":0.2501461343335275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036310474","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993094,0.00004007139,0.0000493458,0.000021725169,9.377896e-7,0.0000017295768,0.00012935093,0.00001336036,0.00043412196],"genre_scores_gemma":[0.99956423,0.000034800403,0.000052626776,0.0000031423249,0.000002350319,0.0000034638142,0.00018595054,0.000001940579,0.00015142924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998572,0.0000148650615,0.000015337544,0.000045890345,0.000034670225,0.000031977288],"domain_scores_gemma":[0.9993849,0.000069497284,0.0002595967,0.000045623485,0.00009845139,0.00014203388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002057583,0.00022787029,0.0002256856,0.0015002735,0.00042362948,0.00035261555,0.00023997934,0.00027645426,0.00093861663],"category_scores_gemma":[0.0008412239,0.0001691446,0.0002769246,0.001394478,0.0004687175,0.00016414946,0.00050783256,0.00014804245,0.00015425494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015144155,0.000028838644,0.98117024,0.000042390668,0.000078435005,0.00068519125,0.0019482948,0.0018689714,0.0073642693,0.00008476925,0.0002500824,0.006327085],"study_design_scores_gemma":[0.0000011966506,0.000007785666,0.9992854,0.000001643019,0.000005983995,0.000051470102,0.00015413217,0.00029056202,0.00007028068,0.0000097507,0.00011957893,0.0000022042102],"about_ca_topic_score_codex":0.059523165,"about_ca_topic_score_gemma":0.109839424,"teacher_disagreement_score":0.94047683,"about_ca_system_score_codex":0.0010138415,"about_ca_system_score_gemma":0.00039026144,"threshold_uncertainty_score":0.11835343},"labels":[],"label_agreement":null},{"id":"W2036698959","doi":"10.1134/s0001433814050090","title":"Tsunami observations in the open ocean","year":2014,"lang":"en","type":"article","venue":"Izvestiya Atmospheric and Oceanic Physics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seafloor spreading; Observatory; Oceanography; Seismology; Tsunami wave; Pacific ocean; Climatology","score_opus":0.029812094201474633,"score_gpt":0.22546838453226956,"score_spread":0.19565629033079493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036698959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9829049,0.0026465598,0.0030132525,0.00014628403,0.000034682005,0.000015634283,0.0026509035,0.00009542715,0.008492403],"genre_scores_gemma":[0.9913155,0.0016367681,0.0028901654,0.000046203084,0.00007178684,0.000008410308,0.0023519637,0.000012098143,0.0016672511],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999056,0.000009177691,0.0000114081695,0.000024831761,0.00003101316,0.000017952156],"domain_scores_gemma":[0.9997291,0.000036356218,0.000059457678,0.000035848454,0.00009182264,0.000047472968],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012687378,0.00014898033,0.00013044836,0.0010655817,0.00033089385,0.00048496024,0.00013249944,0.00019767617,0.0005591577],"category_scores_gemma":[0.00044152705,0.00008009518,0.0000891717,0.0016686155,0.00020568671,0.0004603871,0.00065665814,0.00023285126,0.00019507244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025482976,0.00007012873,0.6085017,0.00023874336,0.00008245644,0.0007587285,0.0013846499,0.0030114306,0.08376994,0.00070402096,0.0016865135,0.2995369],"study_design_scores_gemma":[0.000008353839,0.000058055473,0.9821602,0.00003864194,0.000041999952,0.00016928402,0.0007523415,0.0012518361,0.0052062934,0.00034282208,0.009953849,0.000016225644],"about_ca_topic_score_codex":0.010698531,"about_ca_topic_score_gemma":0.02104013,"teacher_disagreement_score":0.010698531,"about_ca_system_score_codex":0.0002419194,"about_ca_system_score_gemma":0.00025497726,"threshold_uncertainty_score":0.02127248},"labels":[],"label_agreement":null},{"id":"W2036717214","doi":"10.1007/s10950-015-9489-9","title":"Modeling earthquake dynamics","year":2015,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Weibull distribution; Magnitude (astronomy); Seismology; Generalized Pareto distribution; Earthquake magnitude; Geology; Mathematics; Statistics; Extreme value theory; Physics","score_opus":0.039278274645831404,"score_gpt":0.2411544043321092,"score_spread":0.20187612968627777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036717214","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49303147,0.00079671846,0.46155322,0.0013364739,0.00036886026,0.00013353629,0.0025857647,0.002698283,0.03749564],"genre_scores_gemma":[0.95336294,0.00027756227,0.03660871,0.00007223313,0.00006783073,0.00007115423,0.0007491984,0.00013911606,0.008651206],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999082,0.000022171755,0.000006189672,0.000031565985,0.000017934715,0.000014015259],"domain_scores_gemma":[0.99958616,0.00023345386,0.000041615247,0.00005302497,0.0000499951,0.000035765956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026900787,0.0006162241,0.0006257178,0.0005398101,0.00048727993,0.0009005132,0.0011958355,0.0012344733,0.006131937],"category_scores_gemma":[0.001604475,0.0006730657,0.0006624111,0.00050185836,0.0003812901,0.001038911,0.00056074176,0.0006500565,0.0007060152],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010996401,0.00001957886,0.0008869429,0.000010074269,0.000018114566,0.00001993317,0.000011295435,0.9927751,0.000293889,0.002291744,0.00033559173,0.0033267625],"study_design_scores_gemma":[0.0000032055793,0.000002758069,0.00007419945,8.5335216e-7,0.0000035157113,0.0000030889319,0.000003091443,0.9988372,0.00007028165,0.0007162803,0.00028450473,0.0000010024575],"about_ca_topic_score_codex":0.027883617,"about_ca_topic_score_gemma":0.02245907,"teacher_disagreement_score":0.027883617,"about_ca_system_score_codex":0.0006859354,"about_ca_system_score_gemma":0.0008026039,"threshold_uncertainty_score":0.05544263},"labels":[],"label_agreement":null},{"id":"W2036936972","doi":"10.1038/ngeo2017","title":"Limit of strain partitioning in the Himalaya marked by large earthquakes in western Nepal","year":2013,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Seismology; Fault (geology); Radiocarbon dating; Front (military); Active fault; Range (aeronautics); Mountain range (options); Basin and range topography; Seismic gap; Transform fault; Tectonics; Paleontology","score_opus":0.00761119913333634,"score_gpt":0.21723326277719576,"score_spread":0.20962206364385944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036936972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99685717,0.00006353982,0.00008336728,0.000049436225,7.954969e-7,0.0000034688333,0.000093596485,0.0000036720244,0.0028449302],"genre_scores_gemma":[0.999739,0.000019450774,0.000027999715,0.000008291117,0.0000011701324,0.000002625787,0.00005155582,0.0000010475522,0.00014872217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983263,0.000039298247,0.000010859637,0.00003875649,0.000014940391,0.00006350463],"domain_scores_gemma":[0.9993424,0.00024519482,0.00011419803,0.000043348773,0.00011148851,0.0001433095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023897651,0.0001356982,0.0002546539,0.0015279701,0.0013071632,0.0020402982,0.00059546833,0.00040912844,0.0020901235],"category_scores_gemma":[0.001592452,0.00027583583,0.0001239765,0.0011055403,0.0011484463,0.0006495549,0.0014480499,0.0003463695,0.00036192112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011515295,0.00020360042,0.93453544,0.00012555749,0.00020502749,0.0025892542,0.01561559,0.003789294,0.019653134,0.005691237,0.0008394722,0.015600898],"study_design_scores_gemma":[0.000018514627,0.00005478922,0.9868412,0.000027193597,0.000025641551,0.00040191697,0.0074608587,0.0030396772,0.00046294296,0.0010522952,0.0005953854,0.000019504236],"about_ca_topic_score_codex":0.048746604,"about_ca_topic_score_gemma":0.05744501,"teacher_disagreement_score":0.048746604,"about_ca_system_score_codex":0.0006182182,"about_ca_system_score_gemma":0.0005838884,"threshold_uncertainty_score":0.096925735},"labels":[],"label_agreement":null},{"id":"W2038431340","doi":"10.5539/jgg.v6n3p1","title":"Quaternary Tectonic Deformation, Holocene Paleoseismicity, and Modern Strain in the Unusually–Wide Coupled Zone of the Central Cascadia Margin, Washington and Oregon, USA, and British Columbia, Canada","year":2014,"lang":"en","type":"article","venue":"Journal of Geography and Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; Portland State University","keywords":"Geology; Subduction; Subsidence; Seismology; Holocene; Quaternary; Trench; Oceanography; Deformation (meteorology); Tectonics; Geomorphology; Paleontology","score_opus":0.0042010492845748456,"score_gpt":0.1654076179757643,"score_spread":0.16120656869118946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038431340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985066,0.00012439788,0.000016315566,0.000022347062,0.0000015972696,0.0000021485946,0.00052751513,0.0000033293609,0.0007957201],"genre_scores_gemma":[0.99824834,0.00013273676,0.000030913758,0.000006151298,0.0000014739031,0.0000031501972,0.0009807232,0.0000017488584,0.0005948937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987483,0.000008495927,0.000013961444,0.000035259938,0.000033111835,0.00003428701],"domain_scores_gemma":[0.9993463,0.000057918744,0.00016526743,0.00002936652,0.00021776992,0.00018337925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017820673,0.00022940083,0.0001611203,0.0018841056,0.00091455446,0.0009792346,0.00038406666,0.0001977314,0.0018389839],"category_scores_gemma":[0.00066572137,0.00019801044,0.0002016928,0.0029402997,0.00053363765,0.00031486576,0.00048376608,0.00023259834,0.00022679025],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034484456,0.000009570484,0.99698406,0.0000062232684,0.000039992297,0.000054159496,0.00023992678,0.00010852709,0.0003265068,0.00004491967,0.0001882126,0.0019633023],"study_design_scores_gemma":[0.0000011876468,0.0000016600411,0.99945277,0.0000035686826,0.0000048291186,0.000011618706,0.00029598403,0.000072757924,0.00001662626,0.000006268504,0.00013158722,0.0000012135325],"about_ca_topic_score_codex":0.8780958,"about_ca_topic_score_gemma":0.9675376,"teacher_disagreement_score":0.121904194,"about_ca_system_score_codex":0.0038835227,"about_ca_system_score_gemma":0.0020789327,"threshold_uncertainty_score":0.2452442},"labels":[],"label_agreement":null},{"id":"W2038668363","doi":"10.1144/gsl.sp.2001.186.01.11","title":"The nature and origin of asymmetric arrays of shear surfaces in fault zones","year":2001,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shear (geology); Geology; Fault (geology); Seismology; Petrology","score_opus":0.020045665891252423,"score_gpt":0.24552627763694557,"score_spread":0.22548061174569314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038668363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99855655,0.000054203345,0.0005226962,0.000013286014,0.0000012052391,0.000002343891,0.00005149779,0.000009728844,0.0007884908],"genre_scores_gemma":[0.99954873,0.000017624212,0.00024950388,0.0000026193302,0.0000019005959,0.0000011565445,0.00007106744,0.0000029177857,0.00010446437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998287,0.000017816315,0.000013501405,0.00004450523,0.00004186277,0.000053607935],"domain_scores_gemma":[0.99932253,0.00007576069,0.000301129,0.0001029427,0.00012741462,0.00007014916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014609628,0.00011095419,0.0001695596,0.0013120513,0.00042200214,0.0007939334,0.00021626509,0.00019902784,0.00084802584],"category_scores_gemma":[0.00074827997,0.00021163822,0.00008970235,0.00061525515,0.0007201569,0.00033541635,0.00045410744,0.0001555193,0.00023130898],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044530514,0.000063523155,0.6442317,0.00008807928,0.000038067123,0.00063537434,0.0019025478,0.002081199,0.30107734,0.008067731,0.00043165273,0.040937386],"study_design_scores_gemma":[0.000011757874,0.000033538632,0.9829017,0.00001255562,0.000010620764,0.0007626652,0.0005529267,0.003273579,0.0091984775,0.0019265679,0.0013046924,0.000010892803],"about_ca_topic_score_codex":0.0026700685,"about_ca_topic_score_gemma":0.002850934,"teacher_disagreement_score":0.0026700685,"about_ca_system_score_codex":0.00036956108,"about_ca_system_score_gemma":0.00015730361,"threshold_uncertainty_score":0.0053090453},"labels":[],"label_agreement":null},{"id":"W2038779670","doi":"10.1029/2006gl027895","title":"Descent of the ancient Farallon slab drives localized mantle flow below the New Madrid seismic zone","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Université du Québec à Montréal","funders":"","keywords":"Geology; Intraplate earthquake; Seismology; Induced seismicity; Mantle (geology); Slab; Slab window; Seismic zone; Lithosphere; Geophysics; Plate tectonics; Seismic tomography; Subduction; Tectonics; Oceanic crust","score_opus":0.02706150407703296,"score_gpt":0.27074786822548674,"score_spread":0.2436863641484538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038779670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99867815,0.00003064559,0.00019763266,0.000050762606,0.0000022963686,8.5132655e-7,0.000017094426,0.000012138861,0.0010104096],"genre_scores_gemma":[0.99963605,0.000023557177,0.000063057734,0.000005632593,0.000002762184,7.0253316e-7,0.000019858748,0.0000019617198,0.00024641945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994874,0.00000557594,0.0000017514079,0.000019864505,0.000008895554,0.000015069864],"domain_scores_gemma":[0.9998753,0.000018983805,0.0000523722,0.000010755073,0.000015482521,0.00002710088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009644641,0.00013409152,0.00012432004,0.00024283638,0.00020380109,0.00046271976,0.00019834204,0.00016615678,0.000914754],"category_scores_gemma":[0.0005460771,0.00012886658,0.00009426861,0.00010188095,0.00044068584,0.00021832094,0.00049167004,0.0001682772,0.00014934258],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00086801586,0.00010187566,0.635704,0.000094729716,0.00006999114,0.00091863883,0.0018635793,0.017890614,0.3039341,0.006624629,0.00088124553,0.031048648],"study_design_scores_gemma":[0.00004597054,0.000091666996,0.9746074,0.000012991564,0.000024436502,0.000107001295,0.0007469737,0.012285437,0.009693723,0.000997324,0.001363884,0.000023292272],"about_ca_topic_score_codex":0.011946477,"about_ca_topic_score_gemma":0.0130742,"teacher_disagreement_score":0.011946477,"about_ca_system_score_codex":0.00055138126,"about_ca_system_score_gemma":0.00037164043,"threshold_uncertainty_score":0.023753881},"labels":[],"label_agreement":null},{"id":"W2038910342","doi":"10.1016/s0025-3227(00)00159-6","title":"The behavior of redox-sensitive metals across a laminated–massive–laminated transition in Saanich Inlet, British Columbia","year":2001,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Research Council Canada; University of Washington","keywords":"Anoxic waters; Geology; Diagenesis; Total organic carbon; Manganese; Redox; Water column; Geochemistry; Mineralogy; Oceanography; Environmental chemistry; Materials science; Chemistry","score_opus":0.008586635858404157,"score_gpt":0.22024475358284706,"score_spread":0.2116581177244429,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038910342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99778736,0.000048682734,0.0000393066,0.00007854025,0.0000037383293,0.00000686262,0.00023016403,0.000007726343,0.0017977974],"genre_scores_gemma":[0.99768436,0.000041175554,0.000066936445,0.000032748747,8.4979024e-7,0.000004248453,0.00015507395,0.000004073757,0.002010443],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980456,0.000014916396,0.00001019213,0.000050653605,0.000041270847,0.00007842108],"domain_scores_gemma":[0.99931777,0.000044032266,0.000051522446,0.000015482301,0.0004453338,0.00012599616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016094695,0.00024598834,0.00042817293,0.0009625866,0.0040042144,0.0019314755,0.0010078273,0.0006584608,0.00205735],"category_scores_gemma":[0.0007139583,0.0003392662,0.00015576565,0.0017236186,0.0011902653,0.00035928097,0.0009788204,0.00065269927,0.0003165591],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009053237,0.0001601175,0.9478403,0.00009647406,0.00010544496,0.00093207526,0.008197356,0.0016028748,0.022120774,0.00051291176,0.0013660076,0.01616039],"study_design_scores_gemma":[0.000006241681,0.000024994359,0.9909627,0.00001957632,0.000011464793,0.00004189897,0.0060613425,0.0007471191,0.00085295166,0.000050247898,0.0012119338,0.000009653605],"about_ca_topic_score_codex":0.97643936,"about_ca_topic_score_gemma":0.99287015,"teacher_disagreement_score":0.023560643,"about_ca_system_score_codex":0.011435301,"about_ca_system_score_gemma":0.006736603,"threshold_uncertainty_score":0.08296931},"labels":[],"label_agreement":null},{"id":"W2038958438","doi":"10.1029/2010jb007521","title":"Relationship between structures, stress and seismicity in the Charlevoix seismic zone revealed by 3‐D geomechanical models: Implications for the seismotectonics of continental interiors","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Rift; Impact crater; Seismology; Induced seismicity; Rift zone; Intraplate earthquake; Focal mechanism; Stress field; Geophysics; Tectonics; Petrology","score_opus":0.05493920805963029,"score_gpt":0.3136676986074165,"score_spread":0.25872849054778624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038958438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954527,0.00011491905,0.001644478,0.0001548282,0.000006475899,0.000022127631,0.000654511,0.00015556409,0.0017943813],"genre_scores_gemma":[0.99822634,0.00009742722,0.000897465,0.000014890606,0.000005005302,0.000015238145,0.00031828956,0.000018954921,0.00040641936],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992657,0.000012591711,0.0000048594657,0.000018671954,0.000016667616,0.000020561492],"domain_scores_gemma":[0.99976844,0.00008359066,0.000042071322,0.000018307492,0.000044219985,0.000043361382],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024040713,0.00056153414,0.00031592627,0.00092128833,0.00062532554,0.0016980342,0.0008534778,0.0010884171,0.0014363697],"category_scores_gemma":[0.0010067837,0.00057401886,0.0004804264,0.00075723225,0.0007528734,0.00034961937,0.0005083573,0.00041985058,0.0002093329],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077278106,0.000099439436,0.07508356,0.000021664096,0.000044920143,0.00012067095,0.00019504662,0.91826594,0.0015808287,0.00081466377,0.00037802142,0.0033180416],"study_design_scores_gemma":[0.000014298965,0.000008325731,0.027907483,0.00000573188,0.000005577001,0.000009516411,0.000057667494,0.9715595,0.00008064702,0.0001656326,0.00017397491,0.00001163618],"about_ca_topic_score_codex":0.5832689,"about_ca_topic_score_gemma":0.39214796,"teacher_disagreement_score":0.41673112,"about_ca_system_score_codex":0.0042928425,"about_ca_system_score_gemma":0.0020119846,"threshold_uncertainty_score":0.8383707},"labels":[],"label_agreement":null},{"id":"W2039015288","doi":"10.1016/j.epsl.2010.07.006","title":"Shallow flank deformation at Cumbre Vieja volcano (Canary Islands): Implications on the stability of steep-sided volcano flanks at oceanic islands","year":2010,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Volcano; Seismology; Flank; Echelon formation; Geodetic datum; Geodesy; Interferometric synthetic aperture radar; Dike; Paleontology; Tectonics; Synthetic aperture radar; Remote sensing","score_opus":0.013739164225193064,"score_gpt":0.19523427234809243,"score_spread":0.18149510812289937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039015288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985221,0.00003970683,0.00003436618,0.000055289587,0.0000047785466,0.0000024634187,0.0000833784,0.0000049668647,0.0012530705],"genre_scores_gemma":[0.9997836,0.000019112178,0.000025156143,0.000005249888,0.0000025392706,9.022724e-7,0.000049476395,0.0000017504374,0.000112270674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999325,0.0000053198337,0.000005643019,0.000015934414,0.000012566738,0.00002811823],"domain_scores_gemma":[0.99976605,0.000031002863,0.000038858943,0.000022586939,0.0000667177,0.000074750715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014306793,0.00016731402,0.00026193698,0.0007488921,0.00081502926,0.0009191734,0.00044728623,0.0005929707,0.0022943332],"category_scores_gemma":[0.0010562767,0.0001785108,0.00027165274,0.0005283386,0.00058728346,0.00035444513,0.0008830901,0.0003135519,0.00024315748],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000394061,0.00007951597,0.9485974,0.00006405101,0.00011256096,0.0013461491,0.0012464218,0.0063889837,0.027050583,0.0006119055,0.0005015543,0.013606876],"study_design_scores_gemma":[0.0000064289566,0.000015540436,0.9970483,0.000004278518,0.000010703811,0.000054717937,0.00040616313,0.0019997484,0.00022763641,0.000059405786,0.00016149197,0.0000056240056],"about_ca_topic_score_codex":0.090181276,"about_ca_topic_score_gemma":0.11366724,"teacher_disagreement_score":0.090181276,"about_ca_system_score_codex":0.00077484554,"about_ca_system_score_gemma":0.00063931145,"threshold_uncertainty_score":0.17931277},"labels":[],"label_agreement":null},{"id":"W2039045810","doi":"10.1109/waina.2014.143","title":"Parallel Infrastructures and Systems for Near-Field Tsunami Detection and Impact Assessment","year":2014,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Computer science; Leverage (statistics); Scalability; Distributed computing; Computation; Field (mathematics); Emergency response; Event (particle physics); Focus (optics); Real-time computing; Database","score_opus":0.010880020212183525,"score_gpt":0.25100103054831024,"score_spread":0.2401210103361267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039045810","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.012144055,0.0003446288,0.9772496,0.0006554845,0.0000991407,0.00016530757,0.00019881528,0.0027716872,0.0063711666],"genre_scores_gemma":[0.41638866,0.0012660455,0.5755445,0.00016556188,0.0001482462,0.00048280822,0.0007936557,0.0003137739,0.004896715],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9993005,0.00024445425,0.000047093035,0.00013005991,0.00020732381,0.000070675465],"domain_scores_gemma":[0.998428,0.00058374484,0.00013980405,0.00049307564,0.00025883762,0.00009651951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014617898,0.00068755425,0.0005547127,0.00065221824,0.00088606705,0.0016626543,0.0018195801,0.0008418626,0.0060132556],"category_scores_gemma":[0.0035932816,0.00040275021,0.00052515796,0.0010174662,0.0010296504,0.00251735,0.0017131161,0.0012927713,0.0011214606],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017233344,0.00014017547,0.0014197647,0.0001989246,0.00006871975,0.00013669684,0.00014406868,0.7800691,0.004282161,0.13248077,0.0073790536,0.07350827],"study_design_scores_gemma":[0.000035428482,0.000060289098,0.00024316467,0.00001998419,0.00001980265,0.000040650808,0.00004432625,0.9495416,0.0018402094,0.03493531,0.013206697,0.000012447151],"about_ca_topic_score_codex":0.0063649546,"about_ca_topic_score_gemma":0.006035172,"teacher_disagreement_score":0.0063649546,"about_ca_system_score_codex":0.001632116,"about_ca_system_score_gemma":0.0020209122,"threshold_uncertainty_score":0.02011633},"labels":[],"label_agreement":null},{"id":"W2039091930","doi":"10.1016/j.jsg.2014.10.009","title":"Physical analog (centrifuge) model investigation of contrasting structural styles in the Salt Range and Potwar Plateau, northern Pakistan","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Foreland basin; Fault (geology); Basement; Thrust fault; Anticline; Paleontology; Fold (higher-order function); Neogene; Monocline; Petrology; Seismology; Geomorphology; Tectonics","score_opus":0.01227234592487432,"score_gpt":0.2322137487915991,"score_spread":0.21994140286672476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039091930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923206,0.000020988948,0.002718516,0.00005421224,0.000005950431,0.000022743257,0.00060355896,0.00011402285,0.0041394127],"genre_scores_gemma":[0.9985676,0.000018158627,0.0009235604,0.000009085372,0.0000018615741,0.000013062352,0.00019391841,0.0000069569073,0.00026567304],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999162,0.000012817478,0.000006647179,0.000032131844,0.000014401104,0.000017704995],"domain_scores_gemma":[0.9998148,0.00007143581,0.000032231765,0.000025562087,0.000037150363,0.000018827444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009731862,0.0003310346,0.00024518988,0.00042149774,0.0003895004,0.00068740355,0.000733482,0.0006522854,0.0026974112],"category_scores_gemma":[0.00047693713,0.00026522245,0.00039160292,0.00063768483,0.00046665894,0.00033578076,0.0003926574,0.00025005537,0.00015227865],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056682813,0.00008814769,0.024486596,0.000025421588,0.000024358616,0.00028279662,0.00011853878,0.96672094,0.003158307,0.00078484893,0.00023862583,0.0040146955],"study_design_scores_gemma":[0.000039888942,0.000051211922,0.015268963,0.000003423144,0.000014324129,0.000060466304,0.00013240486,0.983127,0.00053969614,0.00034233762,0.00040582556,0.000014383483],"about_ca_topic_score_codex":0.058597527,"about_ca_topic_score_gemma":0.03590623,"teacher_disagreement_score":0.058597527,"about_ca_system_score_codex":0.00080988166,"about_ca_system_score_gemma":0.0006316722,"threshold_uncertainty_score":0.116512895},"labels":[],"label_agreement":null},{"id":"W2039730779","doi":"10.1029/2006gl028721","title":"Imaging slow failure in triaxially deformed Etna basalt using 3D acoustic‐emission location and X‐ray computed tomography","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":119,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Acoustic emission; Basalt; Geology; Deformation (meteorology); Volcano; Shear (geology); Fault (geology); Volume (thermodynamics); Strain rate; Seismology; Compression (physics); Mineralogy; Materials science; Petrology; Composite material; Physics","score_opus":0.027716970181402355,"score_gpt":0.2878585940900741,"score_spread":0.26014162390867174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039730779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891174,0.000034982328,0.0006020414,0.000006584214,0.0000011827111,0.0000049764903,0.00005814992,0.000011993816,0.0003683585],"genre_scores_gemma":[0.99861693,0.0000278719,0.0010028327,0.000004824992,0.0000018271301,0.0000061467013,0.000078691504,0.0000045414786,0.0002563737],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998394,0.000016937322,0.000013970593,0.00003365088,0.00007137152,0.00002460763],"domain_scores_gemma":[0.9996892,0.00005334975,0.0000892684,0.000055326185,0.00007366915,0.000039252463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021243072,0.00019533896,0.00018771882,0.00069250277,0.00019555682,0.00038788616,0.00034405815,0.00042302796,0.00078195456],"category_scores_gemma":[0.0004709539,0.0002240134,0.00012798976,0.00041213873,0.00051149627,0.0002342881,0.0003083275,0.00022710938,0.00021043334],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003152464,0.00007579722,0.07850032,0.000045827917,0.000024221672,0.0005511778,0.00039684726,0.0035897873,0.90907335,0.000084074716,0.000050069906,0.007293298],"study_design_scores_gemma":[0.00003297348,0.00036695803,0.839,0.000014009653,0.00002676234,0.0014216397,0.000336418,0.021066979,0.13690501,0.00007978962,0.0007174026,0.00003199281],"about_ca_topic_score_codex":0.0027679985,"about_ca_topic_score_gemma":0.00453278,"teacher_disagreement_score":0.0027679985,"about_ca_system_score_codex":0.00019637017,"about_ca_system_score_gemma":0.000113441885,"threshold_uncertainty_score":0.005503714},"labels":[],"label_agreement":null},{"id":"W2040131119","doi":"10.1029/2005gl023991","title":"The 1999 Chi‐Chi, Taiwan, earthquake as a typical example of seismic activation and quiescence","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Epicenter; Seismology; Geology; Foreshock; Aftershock; Seismic hazard; Shock (circulatory); Earthquake prediction; Seismic microzonation; Peak ground acceleration; Hazard; Ground motion; Medicine","score_opus":0.03426168776906671,"score_gpt":0.2810443119238127,"score_spread":0.24678262415474597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040131119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905736,0.00011936387,0.0054890807,0.00012589675,0.000017564209,0.000034212346,0.0009450666,0.00011437531,0.0025808695],"genre_scores_gemma":[0.9949064,0.000073589894,0.0034584105,0.000013081768,0.0000079816455,0.000015158207,0.0011349283,0.000005553683,0.0003849449],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996567,0.0000053461363,0.0000041924345,0.000007839748,0.000009248728,0.000007669644],"domain_scores_gemma":[0.99979323,0.00005908536,0.000051637693,0.000025203191,0.000031487376,0.000039418912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000109049244,0.00018129722,0.00011714064,0.0007353096,0.00024800678,0.00020445036,0.0001497073,0.00021607321,0.0008266455],"category_scores_gemma":[0.000541148,0.000047377333,0.00009051572,0.0012505447,0.00017120548,0.00016359989,0.00028087696,0.00016837975,0.00009557983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012428926,0.00022634736,0.71128476,0.00036815912,0.00014127883,0.013156565,0.0014761138,0.023830533,0.08615689,0.006523008,0.010671295,0.14492211],"study_design_scores_gemma":[0.00006915983,0.000532856,0.9285162,0.000027318061,0.00008488206,0.005872545,0.0009472534,0.040546052,0.011164817,0.0020391685,0.010157342,0.00004241928],"about_ca_topic_score_codex":0.0037961612,"about_ca_topic_score_gemma":0.010417193,"teacher_disagreement_score":0.0037961612,"about_ca_system_score_codex":0.00013356844,"about_ca_system_score_gemma":0.00018838476,"threshold_uncertainty_score":0.0075481534},"labels":[],"label_agreement":null},{"id":"W2040245103","doi":"10.1029/2006gl027323","title":"Critical point theory of earthquakes: Observation of correlated and cooperative behavior on earthquake fault systems","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Seismology; Geology; Induced seismicity; Foreshock; Magnitude (astronomy); Remotely triggered earthquakes; Fault (geology); Scaling law; Earthquake swarm; Scaling; Geometry; Physics","score_opus":0.04360130499371933,"score_gpt":0.29147636342607736,"score_spread":0.24787505843235802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040245103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9428719,0.00036295364,0.050964616,0.00015751507,0.000011100853,0.000032918168,0.00011873114,0.00012553933,0.0053546415],"genre_scores_gemma":[0.99799997,0.00007981439,0.0016823573,0.000007260509,0.0000139755775,0.00000880313,0.000042868043,0.0000040864907,0.00016092061],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9999087,0.000011611941,0.000003134254,0.000021441854,0.000035124096,0.000020044148],"domain_scores_gemma":[0.99900407,0.00038432586,0.00021736695,0.00013570924,0.00013474912,0.00012394105],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019788378,0.00013949382,0.00023887561,0.0011217587,0.00029400003,0.0003739979,0.00037127075,0.0002538147,0.0011068006],"category_scores_gemma":[0.0024860825,0.00014057686,0.00013773552,0.00068109744,0.0010373277,0.00071895204,0.00045607958,0.00031033996,0.000092495015],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004389474,0.00016056656,0.19914289,0.00031905065,0.00016383702,0.0025734028,0.0039098193,0.12257578,0.105902515,0.4759757,0.0058092694,0.08302827],"study_design_scores_gemma":[0.00012694926,0.00019287557,0.22319317,0.0000471889,0.000053753134,0.0023427454,0.0007414216,0.42455503,0.015297161,0.32681465,0.0065450636,0.00008992578],"about_ca_topic_score_codex":0.0012160845,"about_ca_topic_score_gemma":0.0004293247,"teacher_disagreement_score":0.0012160845,"about_ca_system_score_codex":0.00035001108,"about_ca_system_score_gemma":0.00016350056,"threshold_uncertainty_score":0.003702581},"labels":[],"label_agreement":null},{"id":"W2041225337","doi":"10.1111/j.1755-6724.2009.00103.x","title":"<i>V</i><sub>p</sub>/<i>V</i><sub>s</sub> Anisotropy and Implications for Crustal Composition Identification and Earthquake Prediction","year":2009,"lang":"en","type":"article","venue":"Acta Geologica Sinica - English Edition","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Anisotropy; Geology; Seismic anisotropy; Felsic; Plagioclase; Mineralogy; Crust; Isotropy; Continental crust; Layering; Geophysics; Seismology; Petrology; Mantle (geology); Mafic; Quartz; Physics","score_opus":0.014250185248233528,"score_gpt":0.21902470306051994,"score_spread":0.20477451781228642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041225337","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873099,0.00026998276,0.007873539,0.000075024225,0.000007464778,0.000013255032,0.00039289717,0.0001915301,0.0038665629],"genre_scores_gemma":[0.99816567,0.00006859205,0.0014399438,0.000004782876,0.0000036601703,0.000002499788,0.0001634415,0.000009466014,0.00014194085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993944,0.00000943032,0.000006708842,0.000017492326,0.000014963178,0.000011993452],"domain_scores_gemma":[0.9997763,0.000042304608,0.00008474121,0.000019502953,0.000057320674,0.000019888754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019739835,0.00031146454,0.00014596789,0.0009767825,0.00013337893,0.00045213825,0.00016659399,0.00016110201,0.0011986637],"category_scores_gemma":[0.00052062026,0.00014989857,0.00012916468,0.0005914346,0.0002379604,0.0002939042,0.00020858693,0.00016680239,0.00028743336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026762878,0.00007948465,0.7237189,0.0001511647,0.000053992193,0.00024936278,0.00007658353,0.021122184,0.13272066,0.0014859342,0.0008003402,0.11927369],"study_design_scores_gemma":[0.000013230113,0.000051975927,0.8906323,0.000024371526,0.000026935739,0.00016822544,0.00013461758,0.07586016,0.030911723,0.0012449835,0.00091477507,0.000016657512],"about_ca_topic_score_codex":0.0034461021,"about_ca_topic_score_gemma":0.0035883153,"teacher_disagreement_score":0.0034461021,"about_ca_system_score_codex":0.0001909739,"about_ca_system_score_gemma":0.0001553139,"threshold_uncertainty_score":0.0068520904},"labels":[],"label_agreement":null},{"id":"W2041476815","doi":"10.1002/2014gl061975","title":"Static stress triggering explains the empirical aftershock distance decay","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Induced seismicity; Geology; Scaling; Coulomb; Stress (linguistics); Seismology; Fractal; Range (aeronautics); Exponent; Statistical physics; Fractal dimension; Physics; Magnitude (astronomy); Fault (geology); Geometry; Mathematics; Astrophysics; Mathematical analysis; Electron; Materials science","score_opus":0.08962667359589133,"score_gpt":0.3236759746102895,"score_spread":0.2340493010143982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041476815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99333936,0.00006768096,0.0048923786,0.000058680107,0.000004032411,0.000007914421,0.000063490756,0.00005130524,0.0015151447],"genre_scores_gemma":[0.9997099,0.000017169907,0.00016873537,0.0000038568255,0.000001103149,0.0000020926723,0.000020640624,0.0000046560767,0.00007183718],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999341,0.000010088067,0.0000034505138,0.000014692673,0.000013289912,0.000024410667],"domain_scores_gemma":[0.99939835,0.00025143276,0.00012310158,0.00010122323,0.000063677006,0.00006224928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033072513,0.00021462297,0.00025377478,0.00038618155,0.00020314613,0.00039369584,0.00040715138,0.00030843125,0.0012842029],"category_scores_gemma":[0.0023399354,0.00013500603,0.00027494732,0.00026040606,0.0004687072,0.0004718528,0.00026963154,0.00030908003,0.000116933166],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021509256,0.00016046959,0.12545136,0.0001291839,0.00008819765,0.00051323336,0.000310533,0.8203509,0.019186143,0.015861787,0.0013485273,0.016384564],"study_design_scores_gemma":[0.000021640479,0.000056717712,0.033614494,0.000010638989,0.00001330447,0.00007510588,0.000055199693,0.96177584,0.0012608073,0.0028713197,0.00023436287,0.000010594086],"about_ca_topic_score_codex":0.0061305366,"about_ca_topic_score_gemma":0.004177548,"teacher_disagreement_score":0.0061305366,"about_ca_system_score_codex":0.00047722246,"about_ca_system_score_gemma":0.00025204348,"threshold_uncertainty_score":0.012189746},"labels":[],"label_agreement":null},{"id":"W2041740192","doi":"10.1038/nature13275","title":"Uplift and seismicity driven by groundwater depletion in central California","year":2014,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":260,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"National Science Foundation","keywords":"Induced seismicity; Geology; Groundwater; Earth science; Seismology; Geotechnical engineering","score_opus":0.004551061382019,"score_gpt":0.19015404775981296,"score_spread":0.18560298637779396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041740192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987311,0.00005110835,0.000015073247,0.00007388196,0.000003898631,0.0000025985398,0.00020195746,0.000004173528,0.0009161086],"genre_scores_gemma":[0.9992161,0.00008135158,0.00003035292,0.000021731781,0.0000056281656,0.0000026450728,0.00024570245,0.000002130067,0.0003944031],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989724,0.000009571463,0.0000096126105,0.000028709752,0.00002108271,0.00003365976],"domain_scores_gemma":[0.9992742,0.00011563846,0.00023114649,0.000035418405,0.00018918651,0.00015448715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002387638,0.00012610499,0.00021054855,0.0009954632,0.00083480706,0.0007174289,0.00038730737,0.00038714366,0.0015790354],"category_scores_gemma":[0.000913834,0.00021298663,0.00012198507,0.0011827158,0.0003896954,0.00030009146,0.00056728703,0.000364641,0.0000843423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028961195,0.00018455456,0.98590326,0.00003140503,0.00006214681,0.0002889,0.0013773547,0.0015308758,0.0017157239,0.00035917922,0.0017733043,0.0064838487],"study_design_scores_gemma":[0.0000074817835,0.000010868421,0.9985851,0.000004584077,0.000012803212,0.000013204817,0.0005555127,0.0003679549,0.000050461338,0.00002452787,0.00036430074,0.0000032291482],"about_ca_topic_score_codex":0.4958741,"about_ca_topic_score_gemma":0.72313654,"teacher_disagreement_score":0.4958741,"about_ca_system_score_codex":0.0021023243,"about_ca_system_score_gemma":0.0013399662,"threshold_uncertainty_score":0.9859756},"labels":[],"label_agreement":null},{"id":"W2041863160","doi":"10.1007/s11069-015-1689-7","title":"Maximum-recorded overland run-ups of major nearfield paleotsunamis during the past 3000 years along the Cascadia margin, USA, and Canada","year":2015,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Subduction; Shore; Seismology; Continental margin; Elevation (ballistics); Range (aeronautics); Magnitude (astronomy); Margin (machine learning); Oceanography; Tectonics","score_opus":0.007812388357470532,"score_gpt":0.19213359067484018,"score_spread":0.18432120231736965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041863160","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98826516,0.00027137078,0.00006474812,0.00008128502,0.000009586885,0.0000056819163,0.009269073,0.000021319554,0.002011816],"genre_scores_gemma":[0.9940023,0.00030383182,0.000080813494,0.00001497432,0.0000070902993,0.0000058509504,0.0044790283,0.000004937032,0.0011010395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998859,0.0000064441183,0.0000106229545,0.000027611244,0.00003090709,0.000038563037],"domain_scores_gemma":[0.9991518,0.000059321654,0.0002052963,0.00002513035,0.0003552368,0.00020316592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013382609,0.00026460667,0.0001789237,0.001584191,0.0008760576,0.0005914194,0.00045956104,0.00031153343,0.0018504981],"category_scores_gemma":[0.0009523165,0.0001841182,0.00022919268,0.0021978815,0.00029643436,0.0003479445,0.0006485389,0.00029776705,0.00022081322],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007498137,0.000012951882,0.99266773,0.000042205633,0.00009887607,0.000081603604,0.0007720661,0.00045962748,0.00056408584,0.00008832909,0.0017151765,0.003422517],"study_design_scores_gemma":[0.0000010970389,0.000002940631,0.99882454,0.000007860025,0.000009285828,0.000022151211,0.00043362714,0.000103739636,0.000036706235,0.0000074589248,0.0005477508,0.0000028764205],"about_ca_topic_score_codex":0.87060887,"about_ca_topic_score_gemma":0.97208947,"teacher_disagreement_score":0.12939113,"about_ca_system_score_codex":0.002935348,"about_ca_system_score_gemma":0.002845869,"threshold_uncertainty_score":0.26030624},"labels":[],"label_agreement":null},{"id":"W2041983093","doi":"10.1029/2011eo490011","title":"State of the art in radiation belt research","year":2011,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Memorial University of Newfoundland","funders":"","keywords":"Van Allen radiation belt; Van Allen Probes; Magnetosphere; Satellite; Space weather; Radiation; Physics; Meteorology; Geology; Astrobiology; Astronomy; Nuclear physics","score_opus":0.0817686057231492,"score_gpt":0.273128698165878,"score_spread":0.19136009244272878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041983093","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0014898793,0.9192123,0.005463803,0.04370411,0.0044175503,0.000030757932,0.0003082843,0.00017226122,0.02520098],"genre_scores_gemma":[0.016100658,0.94795936,0.0077094114,0.008193367,0.009349167,0.00005239908,0.0005226994,0.00015179146,0.009961166],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.995323,0.0014221063,0.00039970258,0.00076642004,0.0016334691,0.00045526045],"domain_scores_gemma":[0.97284997,0.013730744,0.0012569234,0.0031057028,0.007115865,0.0019407893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.016346682,0.00097442203,0.0015252271,0.00831607,0.0018993682,0.010634641,0.0036669506,0.003983583,0.022488322],"category_scores_gemma":[0.018407075,0.0006273333,0.0010690877,0.014088999,0.007902629,0.011756317,0.003183054,0.0038764202,0.009959943],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008241977,0.00010529361,0.003374855,0.0029361036,0.000047394828,0.00007880218,0.0008286472,0.0003944555,0.0005121869,0.041130785,0.09062731,0.8598817],"study_design_scores_gemma":[0.000010756905,0.00003520873,0.0045456192,0.0045896,0.000024959658,0.00020978237,0.0009790893,0.0002782679,0.00029250747,0.030786248,0.95820975,0.000038382976],"about_ca_topic_score_codex":0.029071497,"about_ca_topic_score_gemma":0.022054516,"teacher_disagreement_score":0.029071497,"about_ca_system_score_codex":0.005553018,"about_ca_system_score_gemma":0.009584538,"threshold_uncertainty_score":0.08645052},"labels":[],"label_agreement":null},{"id":"W2042010012","doi":"10.1016/j.epsl.2005.11.054","title":"A discrete episode of seismic and aseismic deformation of the Nankai trough subduction zone accretionary prism and incoming Philippine Sea plate","year":2006,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Research Institute for Earth Science and Disaster Prevention; Japan Agency for Marine-Earth Science and Technology; British Geological Survey; National Science Foundation","keywords":"Geology; Accretionary wedge; Seismology; Subduction; Borehole; Oceanic crust; Seafloor spreading; Thrust fault; Plate tectonics; Fault (geology); Geophysics; Tectonics; Paleontology","score_opus":0.0057654322058053944,"score_gpt":0.17503543019131482,"score_spread":0.16926999798550943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042010012","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981041,0.00005352042,0.00015584877,0.00005417408,0.0000056234303,0.0000071721747,0.00021721359,0.00001281815,0.001389638],"genre_scores_gemma":[0.9994272,0.000022063768,0.00008546433,0.000014855893,0.000005822819,0.0000035411783,0.00018102083,0.0000016269664,0.0002584146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999579,0.000003419977,0.0000030862464,0.000015114304,0.0000075114863,0.00001288745],"domain_scores_gemma":[0.9997907,0.00002313307,0.00005856539,0.000017079396,0.000034117198,0.00007643905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009499766,0.00011624589,0.0001399173,0.00045285188,0.00044572185,0.00047272534,0.00022833614,0.00036550447,0.0018594902],"category_scores_gemma":[0.0004682957,0.00013003976,0.00010759327,0.00047381184,0.00035838896,0.0002595628,0.00057648285,0.00035539086,0.00016731705],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011172246,0.00018934638,0.8977967,0.0001386033,0.00014735795,0.0032841472,0.0041922904,0.002800754,0.057828758,0.0011860293,0.0017670098,0.029551746],"study_design_scores_gemma":[0.00000450909,0.0000352047,0.99787915,0.00000553013,0.000007793721,0.00016243286,0.00037669938,0.00048319573,0.0003367106,0.000045015604,0.0006601628,0.0000035155263],"about_ca_topic_score_codex":0.016220074,"about_ca_topic_score_gemma":0.031059347,"teacher_disagreement_score":0.016220074,"about_ca_system_score_codex":0.00048655216,"about_ca_system_score_gemma":0.00030144694,"threshold_uncertainty_score":0.0322513},"labels":[],"label_agreement":null},{"id":"W2042061137","doi":"10.1080/01490419.2011.547816","title":"Tsunami Hazard Evaluation at Selected Locations Along the South Andhra Coast: Numerical Modeling and Field Observations","year":2011,"lang":"en","type":"article","venue":"Marine Geodesy","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Shore; Berm; Geography; East coast; Geology; Hazard map; Oceanography; Seismology; Archaeology; Landslide","score_opus":0.06734478007658044,"score_gpt":0.23575221673601138,"score_spread":0.16840743665943092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042061137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99895966,0.00000717293,0.00023856416,0.000015034641,0.0000014527081,0.000014980612,0.00027238307,0.000030344001,0.00046033828],"genre_scores_gemma":[0.9990201,0.000014169223,0.0005076803,0.0000039429033,0.0000013523843,0.000020472797,0.00027503868,0.00000227492,0.00015500402],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988854,0.000024773128,0.000008413149,0.000033341195,0.000022923352,0.000021996579],"domain_scores_gemma":[0.9996972,0.00012256103,0.00005309523,0.000040086255,0.000053853848,0.00003319134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002546932,0.0003110808,0.0003629544,0.0003884055,0.0003659338,0.00034056406,0.00038666176,0.00037564838,0.00077005837],"category_scores_gemma":[0.00036568881,0.00013677149,0.00040407086,0.00045687848,0.00031345952,0.00029773184,0.00020790272,0.00033965244,0.0001598127],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006956841,0.0020721066,0.40213868,0.0001434118,0.00014666606,0.0012433393,0.0009777923,0.5317256,0.036025543,0.00047112606,0.0013933121,0.022966731],"study_design_scores_gemma":[0.000117672564,0.00055771734,0.31170362,0.000014220285,0.000056735404,0.00010090739,0.0007926327,0.68117636,0.0048994506,0.00017879604,0.0003551625,0.00004671714],"about_ca_topic_score_codex":0.06325769,"about_ca_topic_score_gemma":0.05822687,"teacher_disagreement_score":0.06325769,"about_ca_system_score_codex":0.0007413155,"about_ca_system_score_gemma":0.00038498585,"threshold_uncertainty_score":0.12577897},"labels":[],"label_agreement":null},{"id":"W2042540463","doi":"10.1016/j.epsl.2008.09.038","title":"Microseismicity but no tremor accompanying slow slip in the Hikurangi subduction zone, New Zealand","year":2008,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Marsden Fund; Royal Society; U.S. Geological Survey; Earthquake Commission; California Institute of Technology","keywords":"Episodic tremor and slip; Subduction; Geology; Seismology; Slip (aerodynamics); Slow earthquake; Interplate earthquake; Tectonics","score_opus":0.017275763219658315,"score_gpt":0.18908392244633448,"score_spread":0.17180815922667617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042540463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999253,0.00003192564,0.000024810088,0.000016981941,0.0000012171805,0.000004630171,0.00008022363,0.0000011288546,0.00058602955],"genre_scores_gemma":[0.99958974,0.00003113944,0.00003182051,0.000003975715,0.0000012882698,0.0000030547617,0.00005732632,8.8999406e-7,0.00028074367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989104,0.0000061381897,0.000013232305,0.000029805411,0.000027439524,0.00003235961],"domain_scores_gemma":[0.99957937,0.000056444293,0.00019476262,0.000022471097,0.0000734107,0.00007364659],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001613806,0.00019483003,0.00021499493,0.00092199736,0.00061135547,0.0004919434,0.00033507435,0.00022468572,0.0013083527],"category_scores_gemma":[0.0009114414,0.00029071548,0.00014604919,0.0009393333,0.0010149354,0.0003085339,0.00053855946,0.00025585393,0.00015207088],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064043474,0.000067385896,0.9245148,0.000096627715,0.000050987157,0.0022937409,0.004884878,0.00024136512,0.05657985,0.0001371663,0.00018836117,0.0103044845],"study_design_scores_gemma":[0.0000047201756,0.00002343111,0.9989151,0.0000016669655,0.000005202126,0.00018988841,0.00054626353,0.000042701082,0.00016189266,0.000014072152,0.000092503185,0.0000025778288],"about_ca_topic_score_codex":0.29825687,"about_ca_topic_score_gemma":0.4054188,"teacher_disagreement_score":0.29825687,"about_ca_system_score_codex":0.0009910497,"about_ca_system_score_gemma":0.00076597923,"threshold_uncertainty_score":0.59304166},"labels":[],"label_agreement":null},{"id":"W2042799429","doi":"10.1016/j.jvolgeores.2005.12.008","title":"Tephra deposits associated with a large lava dome collapse, Soufrière Hills Volcano, Montserrat, 12–15 July 2003","year":2006,"lang":"en","type":"article","venue":"Journal of Volcanology and Geothermal Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University","keywords":"Geology; Tephra; Volcano; Lava; Lava dome; Dome (geology); Seismology; Geochemistry; Petrology; Geomorphology","score_opus":0.020759886385576264,"score_gpt":0.2597497102587921,"score_spread":0.23898982387321585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042799429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99751866,0.00011643058,0.00006177587,0.00010947137,0.000010873714,0.000007974125,0.00020896137,0.00001839038,0.001947554],"genre_scores_gemma":[0.99778026,0.000075256154,0.000106624066,0.000032158325,0.000018360448,0.0000028048144,0.0003978771,0.00000523749,0.001581536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999294,0.00000368009,0.0000033929555,0.000015199415,0.000022870247,0.000025403642],"domain_scores_gemma":[0.9997503,0.000020966934,0.00006733573,0.000012694696,0.000085647414,0.00006293426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001684088,0.000192104,0.00018288798,0.0010517887,0.0016206593,0.0005617799,0.00030156333,0.00060998567,0.0010828236],"category_scores_gemma":[0.00035358942,0.000114141105,0.00015473829,0.00043031026,0.0006017571,0.00021328984,0.0005230079,0.0003686434,0.00015334203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013288533,0.00019670922,0.83262163,0.000097952994,0.00021029965,0.020717254,0.007830865,0.0012232285,0.106157355,0.00053485547,0.005477447,0.02360363],"study_design_scores_gemma":[0.000005613239,0.000035010016,0.9949896,0.000005756346,0.0000101317055,0.0006895525,0.0005269857,0.00013950966,0.0013410144,0.00001863012,0.002234979,0.0000031685413],"about_ca_topic_score_codex":0.11380213,"about_ca_topic_score_gemma":0.29955393,"teacher_disagreement_score":0.11380213,"about_ca_system_score_codex":0.0013046955,"about_ca_system_score_gemma":0.0006281889,"threshold_uncertainty_score":0.22627944},"labels":[],"label_agreement":null},{"id":"W2043178035","doi":"10.1002/2014gl061272","title":"Bayesian confidence intervals for the magnitude of the largest aftershock","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Magnitude (astronomy); Confidence interval; Bayesian probability; Statistics; Sequence (biology); Geology; Seismology; Mathematics; Physics; Biology","score_opus":0.04009245604456699,"score_gpt":0.2969755475921919,"score_spread":0.2568830915476249,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043178035","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18613766,0.0016147397,0.8058261,0.00037027398,0.00006596005,0.00009469612,0.0011193121,0.00048880384,0.0042824433],"genre_scores_gemma":[0.91939706,0.00096216664,0.07558243,0.00009725669,0.00013727273,0.00015391437,0.0027199283,0.00008624341,0.0008638265],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9958056,0.0017783627,0.0002746396,0.0009937396,0.00088979845,0.0002577229],"domain_scores_gemma":[0.89640546,0.0910859,0.0047794147,0.002712022,0.004296752,0.00072044437],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.013989419,0.0008233854,0.0011825034,0.003033973,0.00059100863,0.0023042436,0.0020412537,0.0014482761,0.0034868377],"category_scores_gemma":[0.090074845,0.00040460526,0.0013437574,0.0019412237,0.0016740056,0.002445931,0.001436235,0.002011522,0.00058672344],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009414355,0.00019646938,0.04769694,0.00039112472,0.00063584,0.00050841423,0.0006510901,0.6393105,0.0030182502,0.14669052,0.0038259395,0.15613346],"study_design_scores_gemma":[0.00006777082,0.00014635288,0.019772852,0.0002227235,0.00013377762,0.00029180315,0.00017968404,0.89083004,0.0016912777,0.08494249,0.0016171887,0.00010407231],"about_ca_topic_score_codex":0.0030951868,"about_ca_topic_score_gemma":0.002055345,"teacher_disagreement_score":0.013989419,"about_ca_system_score_codex":0.000776489,"about_ca_system_score_gemma":0.0008168863,"threshold_uncertainty_score":0.07398403},"labels":[],"label_agreement":null},{"id":"W2043470373","doi":"10.1016/j.jsg.2004.02.012","title":"Comparisons between analogue and numerical models of thrust wedge development","year":2004,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":137,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Dalhousie University; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Thrust; Geology; Wedge (geometry); Finite element method; Mechanics; Plasticity; Geometry; Physics; Structural engineering; Mathematics; Engineering","score_opus":0.03589483541010983,"score_gpt":0.24428593814634256,"score_spread":0.20839110273623274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043470373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95785034,0.0003575678,0.025651919,0.00030824446,0.00008007985,0.000039473507,0.0005273527,0.00030294657,0.014882109],"genre_scores_gemma":[0.9969748,0.00010328902,0.0021370829,0.000013676938,0.000013638045,0.000013713847,0.000096844866,0.000026329872,0.00062060234],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996803,0.00013268918,0.00003010672,0.0000692107,0.000054350727,0.000033350374],"domain_scores_gemma":[0.9938737,0.005013906,0.00023695265,0.0003399284,0.0004306445,0.00010490261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000906212,0.00028755012,0.00046602526,0.00092928304,0.00030545986,0.0011621359,0.0013851923,0.0012975433,0.00504845],"category_scores_gemma":[0.008287161,0.00042678398,0.00048353415,0.0012281325,0.0007809604,0.001029854,0.00046711403,0.0006815802,0.00027043506],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008696265,0.00006292603,0.0033354494,0.000027825035,0.00001578522,0.000025390033,0.00003093834,0.9905049,0.0002013923,0.0021103006,0.0001493904,0.0034486856],"study_design_scores_gemma":[0.00003076649,0.000021058417,0.0011348118,0.000003724785,0.0000069592857,0.0000089369405,0.000011682118,0.9978521,0.00011625266,0.000689321,0.000118339056,0.0000061284422],"about_ca_topic_score_codex":0.016569844,"about_ca_topic_score_gemma":0.007084119,"teacher_disagreement_score":0.016569844,"about_ca_system_score_codex":0.0014941158,"about_ca_system_score_gemma":0.0005730557,"threshold_uncertainty_score":0.032946825},"labels":[],"label_agreement":null},{"id":"W2043656141","doi":"10.1029/2003jb002498","title":"Temporal changes in <i>P</i> wave attenuation in the Loma Prieta rupture zone","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Attenuation; Seismology; Compaction; Amplitude; Shock wave; Porosity; Saturation (graph theory); Mineralogy; Geotechnical engineering; Mechanics; Physics","score_opus":0.048979331570210644,"score_gpt":0.2980949945664216,"score_spread":0.24911566299621093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043656141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995352,0.000021284637,0.000036499892,0.000009623381,5.499385e-7,0.0000017213604,0.00008395276,0.0000054875163,0.0003055979],"genre_scores_gemma":[0.9995819,0.000029494395,0.00006177431,0.000005472475,0.000002655683,0.000004696721,0.00018776917,0.0000014340169,0.00012488815],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999465,0.0000040658692,0.0000034163525,0.000016286696,0.000012233238,0.000017422955],"domain_scores_gemma":[0.99962723,0.000058403224,0.00017525555,0.000021781858,0.00007764491,0.0000395827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015178302,0.00007707742,0.0001121743,0.0006013683,0.00025483605,0.00031026243,0.00018528951,0.00024363042,0.0005390412],"category_scores_gemma":[0.0006895544,0.00012578674,0.0000642852,0.00039010282,0.00025783773,0.00017659504,0.00029041962,0.00027379423,0.0001606567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043916202,0.00008997988,0.95376843,0.00004236565,0.00006715911,0.0004721335,0.00087032275,0.0012698186,0.02806612,0.000101126294,0.0005697153,0.014243636],"study_design_scores_gemma":[0.0000022062466,0.000015796857,0.9993697,0.000001599219,0.0000046681084,0.000038155133,0.00004612643,0.00014599433,0.00025604115,0.0000035748817,0.00011467163,0.0000015101156],"about_ca_topic_score_codex":0.01913799,"about_ca_topic_score_gemma":0.025721176,"teacher_disagreement_score":0.01913799,"about_ca_system_score_codex":0.00033392728,"about_ca_system_score_gemma":0.00013178714,"threshold_uncertainty_score":0.038053155},"labels":[],"label_agreement":null},{"id":"W2044123278","doi":"10.1029/2009gl040027","title":"Deep low‐frequency earthquakes in tremor localize to the plate interface in multiple subduction zones","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":195,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Episodic tremor and slip; Seismology; Geology; Plate tectonics; Induced seismicity; Slip (aerodynamics); Low frequency; Shear (geology); Pacific Plate; Tectonics; Petrology","score_opus":0.037225261122115716,"score_gpt":0.2884871284448063,"score_spread":0.25126186732269057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044123278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99962735,0.000017641001,0.00012361289,0.000004257559,2.1410301e-7,0.0000014539759,0.000022241164,0.0000033897961,0.0001998973],"genre_scores_gemma":[0.99972016,0.000017413315,0.00012582338,0.0000019189085,0.0000011444183,0.000001507456,0.000054491058,0.0000011236968,0.000076383665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998994,0.000011501302,0.000010995592,0.000035395573,0.0000177317,0.00002503811],"domain_scores_gemma":[0.99916375,0.00010579581,0.0004214038,0.000048376787,0.00013224855,0.00012842954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017782126,0.00013185904,0.00020193122,0.0013804514,0.00024481962,0.00039308795,0.00015546844,0.0001347997,0.00051949697],"category_scores_gemma":[0.000883603,0.00014257997,0.00009435657,0.0009285879,0.00030947957,0.00026778877,0.00050509826,0.00010996609,0.00012895079],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008412298,0.00002576409,0.9739769,0.000015820928,0.000025287873,0.0001389714,0.00058350584,0.00044303175,0.016663438,0.000077239034,0.000054017062,0.007911876],"study_design_scores_gemma":[0.0000023436933,0.000011532477,0.9989819,0.0000018172371,0.0000055107243,0.000057368004,0.00015829847,0.00045110608,0.00027440302,0.000021719768,0.00003235384,0.0000016938449],"about_ca_topic_score_codex":0.011988291,"about_ca_topic_score_gemma":0.026380014,"teacher_disagreement_score":0.011988291,"about_ca_system_score_codex":0.00028786776,"about_ca_system_score_gemma":0.0001940732,"threshold_uncertainty_score":0.02383703},"labels":[],"label_agreement":null},{"id":"W2045363524","doi":"10.1186/bf03352386","title":"Three-dimensional viscoelastic interseismic deformation model for the Cascadia subduction zone","year":2014,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Chinese Academy of Sciences","keywords":"Subduction; Geology; Seismology; Forearc; Lithosphere; Deformation (meteorology); Viscoelasticity; Mantle (geology); Slab; Geodesy; Geophysics; Tectonics","score_opus":0.01514565850310377,"score_gpt":0.19896524178135613,"score_spread":0.18381958327825237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045363524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6614659,0.0006632221,0.30228573,0.0017888256,0.00012782348,0.00016367936,0.0025575722,0.000973051,0.029974166],"genre_scores_gemma":[0.9781156,0.00040697522,0.010468508,0.000120431476,0.000028517657,0.00021822802,0.00056336814,0.00008233259,0.009995882],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988484,0.000025174486,0.000009885839,0.000032902957,0.000026146261,0.000021092224],"domain_scores_gemma":[0.99982375,0.000045561064,0.0000464638,0.000017034086,0.0000363632,0.00003083254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022806243,0.0006629125,0.0005218459,0.0005614504,0.0005342443,0.00085674477,0.0020014732,0.0016320677,0.0026654457],"category_scores_gemma":[0.0006713005,0.00050681,0.0009024354,0.00055605837,0.00070108817,0.00064189854,0.0008179472,0.00072804483,0.0004872109],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010432227,0.000012379543,0.0005430691,0.0000062849044,0.000007779548,0.000039083992,0.000025922254,0.9964814,0.0008532973,0.0014485277,0.00008601748,0.0004857182],"study_design_scores_gemma":[0.000007428149,0.0000064238207,0.00036015574,0.0000020930886,0.000004301921,0.000009346825,0.0000084997155,0.99868697,0.00006397217,0.0006096205,0.00023612993,0.0000050909443],"about_ca_topic_score_codex":0.03220054,"about_ca_topic_score_gemma":0.012377971,"teacher_disagreement_score":0.03220054,"about_ca_system_score_codex":0.0011688432,"about_ca_system_score_gemma":0.0012287152,"threshold_uncertainty_score":0.06402624},"labels":[],"label_agreement":null},{"id":"W2046016818","doi":"10.1029/2002jb001959","title":"Three‐dimensional structure from feathered two‐dimensional marine seismic reflection data: The eastern Nankai Trough","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Accretionary wedge; Seismology; Subduction; Oceanic crust; Classification of discontinuities; Tectonics; Ridge; Crust; Mid-ocean ridge; Seafloor spreading; Lithosphere; Geophysics; Paleontology","score_opus":0.059221093033808,"score_gpt":0.3161840237816676,"score_spread":0.2569629307478596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046016818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888548,0.00008277822,0.0045237825,0.000059825732,0.000011739687,0.000024710595,0.0038540333,0.00045657437,0.002131612],"genre_scores_gemma":[0.98347986,0.00008728591,0.007988778,0.000016800996,0.000011065391,0.00002105423,0.0073940116,0.000079134006,0.0009221262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999931,0.0000043690798,0.000006710641,0.000020879846,0.00002191271,0.0000151387085],"domain_scores_gemma":[0.9998448,0.000012647207,0.000029651508,0.000021348484,0.000060424558,0.000031043408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009057893,0.0003988116,0.00020213466,0.0013974912,0.00020669229,0.0005153521,0.00030398695,0.0002728111,0.0015149819],"category_scores_gemma":[0.0003543811,0.00020887931,0.00032224413,0.0017196636,0.00011857837,0.00014496091,0.00044307546,0.0002163678,0.00040304425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003691489,0.0002827426,0.48730382,0.0002995342,0.0002828404,0.0028844876,0.0014518106,0.03134685,0.29850328,0.00055892696,0.0034984965,0.17321813],"study_design_scores_gemma":[0.000027917364,0.000030052246,0.96292746,0.000013431982,0.000037893962,0.0002307615,0.00028297066,0.030880451,0.0036189912,0.00010122563,0.0018272644,0.00002165957],"about_ca_topic_score_codex":0.0298705,"about_ca_topic_score_gemma":0.059756324,"teacher_disagreement_score":0.0298705,"about_ca_system_score_codex":0.0002739906,"about_ca_system_score_gemma":0.00043488079,"threshold_uncertainty_score":0.059393287},"labels":[],"label_agreement":null},{"id":"W2046057301","doi":"10.1029/2000jb000040","title":"An episode of seafloor spreading and associated plate deformation inferred from crustal fluid pressure transients","year":2001,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Natural Resources Canada","funders":"","keywords":"Geology; Ridge; Seismology; Seafloor spreading; Magnitude (astronomy); Fault (geology); Paleontology","score_opus":0.03170002299588204,"score_gpt":0.2934573266095048,"score_spread":0.26175730361362276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046057301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993887,0.000022711554,0.000086036656,0.000007633078,0.00000159744,0.000003588329,0.00013435243,0.000010879875,0.0003444881],"genre_scores_gemma":[0.9996414,0.000017315782,0.00008151694,0.000003946052,0.000002413402,0.0000019372305,0.00017406838,0.0000010615895,0.00007622055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993014,0.0000038078117,0.0000066981165,0.00001924103,0.000018509267,0.000021620837],"domain_scores_gemma":[0.9997335,0.000030027515,0.00010864108,0.000019383819,0.000034730794,0.00007374383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000117995565,0.00021982948,0.00018342865,0.0006893941,0.00036539766,0.000335013,0.00017026256,0.0003253884,0.00052220817],"category_scores_gemma":[0.0005006994,0.00013723288,0.0001560429,0.0005613193,0.00030318086,0.00018930994,0.00035014687,0.00023210939,0.00008632018],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021475164,0.000046039484,0.9448168,0.000033335895,0.000053576914,0.0014636468,0.0008644934,0.00063973374,0.04318443,0.00006293788,0.00019551699,0.008424775],"study_design_scores_gemma":[0.0000020770287,0.000038460108,0.9981438,0.000001945018,0.000006533359,0.00021823822,0.00009615435,0.00033288813,0.0009769585,0.000009965698,0.00016894551,0.000004085755],"about_ca_topic_score_codex":0.010897455,"about_ca_topic_score_gemma":0.017920708,"teacher_disagreement_score":0.010897455,"about_ca_system_score_codex":0.00035325147,"about_ca_system_score_gemma":0.00020270052,"threshold_uncertainty_score":0.021668077},"labels":[],"label_agreement":null},{"id":"W2046375589","doi":"10.1029/2007jb005375","title":"Active megadetachment beneath the western United States","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Australian Centre for Advanced Photovoltaics; California Institute of Technology; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Seismology; Lithosphere; Subduction; Induced seismicity; Basin and Range Province; Crust; Slip (aerodynamics); Episodic tremor and slip; Plate tectonics; Basin and range topography; Seismic moment; Tectonics; Fault (geology); Geophysics","score_opus":0.05488312055109877,"score_gpt":0.3120310398733715,"score_spread":0.2571479193222727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046375589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9691524,0.0006359084,0.0002025388,0.00049039925,0.0000340891,0.000014841269,0.0024307447,0.00005266466,0.02698647],"genre_scores_gemma":[0.99192554,0.0003476496,0.0003342631,0.0001157762,0.000008524042,0.000013575134,0.0014761621,0.000004502271,0.0057740007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999542,0.000004725032,0.000002747065,0.000010775821,0.000013611031,0.000013995816],"domain_scores_gemma":[0.99978155,0.000016003718,0.000050647515,0.000009583271,0.00010104461,0.000041176965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007615068,0.00011633926,0.00007297741,0.0005434487,0.0006623729,0.0004142178,0.00019562955,0.00013864775,0.0034190884],"category_scores_gemma":[0.00021731679,0.00008484356,0.000042359443,0.0007836542,0.000115582036,0.00021260702,0.00043224503,0.00017444234,0.00024215663],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007354486,0.00008057565,0.9073234,0.00007549714,0.000052254814,0.0007513571,0.002126081,0.00052820856,0.0029281436,0.0016439313,0.016401019,0.06801592],"study_design_scores_gemma":[0.0000036168037,0.000016829305,0.97035867,0.000045596433,0.000017085575,0.000116366195,0.0029805358,0.00074825657,0.00044219696,0.00012589122,0.02513947,0.0000055468154],"about_ca_topic_score_codex":0.2758562,"about_ca_topic_score_gemma":0.59404653,"teacher_disagreement_score":0.2758562,"about_ca_system_score_codex":0.0008649852,"about_ca_system_score_gemma":0.00071190204,"threshold_uncertainty_score":0.5485011},"labels":[],"label_agreement":null},{"id":"W2046678650","doi":"10.1007/bf03162334","title":"ESR signals from clusters of iron ions as indicators of the thermal history of fault gouge","year":2001,"lang":"en","type":"article","venue":"Applied Magnetic Resonance","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Deutscher Akademischer Austauschdienst","keywords":"Fault gouge; Ion; Electron paramagnetic resonance; Biotite; Feldspar; Solid-state physics; Crystallographic defect; Fault (geology); Mineralogy; Thermal; Materials science; Analytical Chemistry (journal); Chemistry; Metallurgy; Nuclear magnetic resonance; Condensed matter physics; Crystallography; Geology; Physics; Thermodynamics; Seismology","score_opus":0.00903376156557542,"score_gpt":0.1875675607293957,"score_spread":0.17853379916382028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046678650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907494,0.000117542186,0.00027138664,0.000023302659,0.0000050830035,0.0000018607817,0.0000804238,0.000007865663,0.00041758135],"genre_scores_gemma":[0.998928,0.000059814356,0.00041274977,0.00001960574,0.00001035313,0.0000026291675,0.00018707725,0.0000039365214,0.00037577096],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99996185,0.0000067566934,0.00000151524,0.00001115217,0.0000071994004,0.00001150935],"domain_scores_gemma":[0.9998116,0.000049745242,0.00005352768,0.000009589776,0.000035488993,0.00004009084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001322248,0.00016685201,0.00012381983,0.00062858657,0.00018048381,0.00026894553,0.00013760122,0.00037127835,0.00091674546],"category_scores_gemma":[0.00034651085,0.0001309054,0.000057630983,0.00036844632,0.00028103287,0.00018291098,0.00017574742,0.00032588883,0.00015217009],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012774543,0.00004296908,0.039383385,0.000051137336,0.00004114133,0.00032049228,0.00025546004,0.0003089472,0.9533327,0.00014199656,0.00021056921,0.0046336935],"study_design_scores_gemma":[0.0000701278,0.00041740958,0.8537806,0.000011021813,0.000093585935,0.0007577613,0.00046240757,0.002530631,0.14035432,0.0003876396,0.0011130772,0.000021396949],"about_ca_topic_score_codex":0.00064258045,"about_ca_topic_score_gemma":0.0012253532,"teacher_disagreement_score":0.00091674546,"about_ca_system_score_codex":0.00008649824,"about_ca_system_score_gemma":0.00004510022,"threshold_uncertainty_score":0.0030668378},"labels":[],"label_agreement":null},{"id":"W2046922644","doi":"10.1029/2008jb006077","title":"Viscosity of the asthenosphere from glacial isostatic adjustment and subduction dynamics at the northern Cascadia subduction zone, British Columbia, Canada","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Asthenosphere; Geology; Subduction; Post-glacial rebound; Lithosphere; Mantle (geology); Slab; Geophysics; Mantle wedge; Seismology; Glacial period; Tectonics; Geomorphology","score_opus":0.010512374957563105,"score_gpt":0.22584113507052286,"score_spread":0.21532876011295976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046922644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950427,0.00026306915,0.00008743006,0.00006320811,0.0000028378713,0.000005443075,0.0015511019,0.000032569125,0.00295172],"genre_scores_gemma":[0.9976961,0.00020097889,0.00009092592,0.0000054132856,7.8286075e-7,0.0000025193954,0.0012622839,0.000008194054,0.0007327766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989986,0.0000034474747,0.0000059913878,0.000026470307,0.000038015663,0.00002625312],"domain_scores_gemma":[0.9997013,0.000025573818,0.000034191635,0.0000129364325,0.00017028615,0.000055618508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011793303,0.0005208061,0.0002065463,0.0015768582,0.0011914162,0.0011559773,0.00060649344,0.0002494667,0.0023086525],"category_scores_gemma":[0.0007151497,0.00032280898,0.00025070756,0.002159953,0.0004997091,0.00032883685,0.0003382863,0.00034240834,0.0002554106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014686795,0.00004118584,0.9447172,0.000096267024,0.00013678952,0.00036266135,0.0010390714,0.024329346,0.010307661,0.000526405,0.0020851993,0.016211301],"study_design_scores_gemma":[0.000008002187,0.0000035172184,0.991437,0.000011873704,0.00001845858,0.000021720545,0.00017434209,0.0070075314,0.0005131444,0.000045783694,0.0007453277,0.000013282556],"about_ca_topic_score_codex":0.98621595,"about_ca_topic_score_gemma":0.98961264,"teacher_disagreement_score":0.016793637,"about_ca_system_score_codex":0.016793637,"about_ca_system_score_gemma":0.0075227153,"threshold_uncertainty_score":0.121846974},"labels":[],"label_agreement":null},{"id":"W2047445831","doi":"10.5194/npg-17-293-2010","title":"A simple metric to quantify seismicity clustering","year":2010,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Workplace Safety and Insurance Board; Institute for Catastrophic Loss Reduction","keywords":"Cluster analysis; Induced seismicity; Metric (unit); Ergodicity; Ergodic theory; Statistical physics; Geology; Mathematics; Physics; Seismology; Mathematical analysis; Statistics","score_opus":0.018328584189087897,"score_gpt":0.2609287736288956,"score_spread":0.2426001894398077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047445831","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.24931529,0.0016869126,0.72281355,0.00034317398,0.00031340713,0.00039713358,0.0052856016,0.0014890544,0.018355956],"genre_scores_gemma":[0.8525655,0.00036345934,0.14140196,0.00008289472,0.00012857512,0.00027487465,0.003191856,0.00014518428,0.0018457178],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9983089,0.00037969425,0.0002750799,0.00029658366,0.00063589186,0.00010389474],"domain_scores_gemma":[0.9956617,0.001277445,0.0010594865,0.0005210017,0.0011600074,0.0003204785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013989314,0.0009607808,0.00066624215,0.0064877993,0.00048383037,0.0013664868,0.0006923899,0.00065146753,0.0026786204],"category_scores_gemma":[0.008458123,0.00021150145,0.00046374576,0.004607365,0.00089154206,0.0018509491,0.0016050311,0.0006638514,0.0008527312],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007046972,0.00024732502,0.12220588,0.0013542966,0.000837739,0.00062674313,0.0017030067,0.18694147,0.053546794,0.14824352,0.0191141,0.46447438],"study_design_scores_gemma":[0.00007015304,0.0008949124,0.15448676,0.00018656132,0.00020754342,0.0021928325,0.0013168976,0.6633108,0.022398807,0.092836134,0.06165991,0.0004386782],"about_ca_topic_score_codex":0.0019641903,"about_ca_topic_score_gemma":0.0014488733,"teacher_disagreement_score":0.0064877993,"about_ca_system_score_codex":0.00082603167,"about_ca_system_score_gemma":0.00057223206,"threshold_uncertainty_score":0.008960903},"labels":[],"label_agreement":null},{"id":"W2047562003","doi":"10.1007/s11069-014-1350-x","title":"Meteorological tsunamis on the US East Coast and in other regions of the World Ocean","year":2014,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration; Russian Foundation for Basic Research","keywords":"Seiche; Volcano; Landslide; Natural hazard; Geology; Oceanography; Sea level; Climatology; Atmospheric wave; Seismology; Geography; Gravitational wave; Gravity wave","score_opus":0.015924319434839154,"score_gpt":0.2190704342452222,"score_spread":0.20314611481038305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047562003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973193,0.000098466546,0.000025397085,0.000071466035,0.0000082240385,0.0000038773946,0.0012870199,0.000003145375,0.001183232],"genre_scores_gemma":[0.99770015,0.00017069683,0.000033894758,0.000020764968,0.000005264917,0.0000049462956,0.001339912,0.0000018983659,0.0007225237],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986315,0.000023814848,0.000016453438,0.000019503754,0.00002833431,0.000048723854],"domain_scores_gemma":[0.99950755,0.000055502187,0.00018357282,0.000022243694,0.00013556183,0.00009553597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014320332,0.00018943596,0.00011758998,0.0011014369,0.00037999247,0.0003802898,0.00016431717,0.00021217304,0.0014945121],"category_scores_gemma":[0.00083454297,0.00010265223,0.0001899413,0.0019985721,0.00020441976,0.00047519073,0.0005871066,0.00028367856,0.00015541508],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005347409,0.00002421477,0.9964539,0.000009348465,0.000034645625,0.00010315121,0.00018735572,0.00027330924,0.00019916297,0.000060601535,0.0006310716,0.0019697878],"study_design_scores_gemma":[0.0000013043995,0.0000069152534,0.998998,0.0000022836336,0.0000059098948,0.000024037325,0.00054612913,0.0001142919,0.000028585486,0.000012993445,0.00025829082,0.0000011570035],"about_ca_topic_score_codex":0.23146269,"about_ca_topic_score_gemma":0.5218458,"teacher_disagreement_score":0.23146269,"about_ca_system_score_codex":0.0008640964,"about_ca_system_score_gemma":0.0006041762,"threshold_uncertainty_score":0.46023083},"labels":[],"label_agreement":null},{"id":"W2047751097","doi":"10.1029/2004jb003381","title":"Upper mantle structure beneath the eastern Pacific Ocean ridges","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Lithosphere; Mantle (geology); Seafloor spreading; Seismometer; Seismology; Mid-ocean ridge; Crust; Geophysics; Geodesy; Tectonics","score_opus":0.027474513803197487,"score_gpt":0.2827879384297324,"score_spread":0.2553134246265349,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047751097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993728,0.000027177462,0.00013468717,0.000008101161,3.307416e-7,7.1593985e-7,0.00011615877,0.000013337515,0.0003266997],"genre_scores_gemma":[0.99941003,0.000028722292,0.0001346362,0.0000023569837,7.2181183e-7,9.103644e-7,0.00028570194,0.0000032773853,0.00013368366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999665,0.0000031251495,0.000002192435,0.000009500163,0.00000788775,0.000010916877],"domain_scores_gemma":[0.9999187,0.000015177626,0.00002509695,0.000009616126,0.000016313978,0.0000150779215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000084204796,0.00022340294,0.0001427021,0.00043127165,0.00017499544,0.00041210258,0.00014712352,0.00017361017,0.000713372],"category_scores_gemma":[0.00031912417,0.0001778616,0.00026233637,0.00046569135,0.00013977783,0.00021477854,0.00037055204,0.0001656346,0.00013585978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009028281,0.000026588852,0.9352381,0.000032161624,0.00011263965,0.0002631777,0.0004847813,0.015451307,0.027205534,0.0003295004,0.00021855537,0.020547442],"study_design_scores_gemma":[0.0000038153908,0.000014016435,0.98574,0.000005138362,0.000021715954,0.000053407002,0.00012324969,0.012929249,0.00076132163,0.00008361334,0.000259254,0.000005279987],"about_ca_topic_score_codex":0.023068283,"about_ca_topic_score_gemma":0.022858681,"teacher_disagreement_score":0.023068283,"about_ca_system_score_codex":0.00023871439,"about_ca_system_score_gemma":0.0002300439,"threshold_uncertainty_score":0.04586804},"labels":[],"label_agreement":null},{"id":"W2048154370","doi":"10.1007/s10950-013-9360-9","title":"Iranian earthquakes, a uniform catalog with moment magnitudes","year":2013,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; University of Tehran; Geological Survey and Mineral Exploration of Iran; International Institute of Earthquake Engineering and Seismology; University of Pretoria","keywords":"Magnitude (astronomy); Seismology; Geology; Moment magnitude scale; Aftershock; Seismic hazard; Induced seismicity; Tectonics; Structural geology; Seismic moment; Range (aeronautics); Earthquake magnitude; Fault (geology); Geometry; Mathematics; Physics","score_opus":0.010992797788016519,"score_gpt":0.1944489795164797,"score_spread":0.18345618172846317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048154370","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.70144,0.0028641997,0.008861612,0.000830939,0.00032101423,0.00054176897,0.2417218,0.0012900783,0.0421286],"genre_scores_gemma":[0.70230407,0.0018876402,0.012648218,0.00015195973,0.00028155322,0.00031784654,0.27258375,0.000108444445,0.009716434],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99939454,0.00004133351,0.00013951819,0.00012562175,0.00021965959,0.000079317106],"domain_scores_gemma":[0.99789387,0.00011327066,0.0004143674,0.00034702793,0.0011302781,0.00010130052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071024214,0.00044928375,0.00031871008,0.007941382,0.0005245319,0.0005550486,0.00048408133,0.0002077353,0.006353508],"category_scores_gemma":[0.0034159252,0.00017604882,0.0002343024,0.00850615,0.00024476735,0.0007549044,0.0007276252,0.0002200314,0.0033789144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046934537,0.00011380385,0.4818424,0.00049417786,0.000119959994,0.0004811861,0.0009389423,0.00085145136,0.006294795,0.002810946,0.10866495,0.39691815],"study_design_scores_gemma":[0.00003798048,0.000088902314,0.89439106,0.00004948716,0.00005983266,0.0008199901,0.0006114387,0.00060385925,0.001579226,0.0004175979,0.10131982,0.000020818854],"about_ca_topic_score_codex":0.016585695,"about_ca_topic_score_gemma":0.023305465,"teacher_disagreement_score":0.016585695,"about_ca_system_score_codex":0.00042704056,"about_ca_system_score_gemma":0.0025026405,"threshold_uncertainty_score":0.032978356},"labels":[],"label_agreement":null},{"id":"W2048704289","doi":"10.1007/s11434-013-6013-x","title":"Deep structure beneath the southwestern section of the Longmenshan fault zone and seimogenetic context of the 4.20 Lushan M S7.0 earthquake","year":2013,"lang":"en","type":"article","venue":"Chinese Science Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Institute of Geology, China Earthquake Administration; National Key Research and Development Program of China; China Earthquake Administration; National Natural Science Foundation of China","keywords":"Geology; Seismology; Epicenter; Magnetotellurics; Crust; Context (archaeology); Fault (geology); Section (typography); Mantle (geology); Electrical resistivity and conductivity; Geophysics; Paleontology","score_opus":0.0056728667903531696,"score_gpt":0.1845655713651159,"score_spread":0.17889270457476272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048704289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99972063,0.000014285352,0.0000148700365,0.0000061204387,5.063095e-7,0.0000010096043,0.00004494428,0.0000013086286,0.00019626511],"genre_scores_gemma":[0.9996025,0.0000142117315,0.00003854645,0.000004228582,0.0000015460216,0.0000019956833,0.00012848522,3.349733e-7,0.00020822695],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994993,0.00000493766,0.000003761572,0.00001702688,0.0000091523125,0.000015104974],"domain_scores_gemma":[0.9999114,0.000005864073,0.000035274075,0.000005538296,0.000018627385,0.000023292207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000078062774,0.00013783103,0.00016146542,0.0005219892,0.00025362967,0.00020574575,0.0001661788,0.00018151308,0.000466776],"category_scores_gemma":[0.00013607435,0.00009979538,0.000071810944,0.0004606338,0.00023291254,0.00016176853,0.00032306634,0.00008418794,0.00006908757],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007353067,0.00004409398,0.96766037,0.000026538932,0.000043909007,0.0007305062,0.0015122734,0.0004998121,0.017588973,0.00025261287,0.0001680218,0.011399302],"study_design_scores_gemma":[0.0000010052738,0.000009903395,0.9993887,0.0000017491054,0.000002245478,0.000027132133,0.00013979492,0.000150493,0.00011890043,0.000009746957,0.00014867757,0.0000016878574],"about_ca_topic_score_codex":0.024731226,"about_ca_topic_score_gemma":0.071228206,"teacher_disagreement_score":0.024731226,"about_ca_system_score_codex":0.00038286395,"about_ca_system_score_gemma":0.00042552158,"threshold_uncertainty_score":0.049174547},"labels":[],"label_agreement":null},{"id":"W2048736073","doi":"10.1007/s00126-005-0043-5","title":"3D numerical modelling of fluid flow in the Val-d’Or orogenic gold district: major crustal shear zones drain fluids from overpressured vein fields","year":2006,"lang":"en","type":"article","venue":"Mineralium Deposita","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"","keywords":"Geology; Fluid dynamics; Shear zone; Crust; Petrology; Metamorphic rock; Tectonics; Vein; Metamorphic core complex; Geochemistry; Seismology; Mechanics; Extensional definition","score_opus":0.01693222364656017,"score_gpt":0.20367867818831956,"score_spread":0.1867464545417594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048736073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884184,0.000068309455,0.0060640965,0.00017609724,0.000025689737,0.000033968423,0.0004910026,0.00020822712,0.004514222],"genre_scores_gemma":[0.99740905,0.000041964275,0.0015504048,0.0000141928585,0.000006119923,0.00001594222,0.00010408668,0.00001567074,0.0008426194],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998797,0.000029479306,0.000011090685,0.000027686538,0.000019537923,0.000032440163],"domain_scores_gemma":[0.9997507,0.00012461498,0.000029828467,0.00002027648,0.000030334828,0.000044245604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018500688,0.00039838642,0.00046674057,0.0006251125,0.0006489819,0.0014356476,0.00081128126,0.0015968273,0.0022472388],"category_scores_gemma":[0.00094408955,0.00050339603,0.0005252916,0.00060872186,0.0014201656,0.0005140006,0.0006498976,0.0005149814,0.00022739173],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007327222,0.000050093364,0.005936516,0.000019503408,0.000014634568,0.00013231934,0.00011729923,0.9892558,0.0017955719,0.0007307776,0.000119724136,0.001754466],"study_design_scores_gemma":[0.000017517794,0.000012207473,0.0024605393,0.0000033250494,0.000003827835,0.000010404717,0.000049544724,0.9967914,0.00034303905,0.00014321797,0.00015695611,0.000007987927],"about_ca_topic_score_codex":0.08674331,"about_ca_topic_score_gemma":0.048978407,"teacher_disagreement_score":0.9132567,"about_ca_system_score_codex":0.0016289413,"about_ca_system_score_gemma":0.0011811458,"threshold_uncertainty_score":0.17247677},"labels":[],"label_agreement":null},{"id":"W2048913362","doi":"10.1007/s00024-012-0555-8","title":"Japan's 2011 Tsunami: Characteristics of Wave Propagation from Observations and Numerical Modelling","year":2012,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fisheries and Oceans Canada; Russian Foundation for Basic Research","keywords":"Geology; Seismology; Equipartition theorem; Meteorology; Physics","score_opus":0.03037244291326001,"score_gpt":0.19035551776665036,"score_spread":0.15998307485339036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048913362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984131,0.000047057856,0.0002459003,0.000029425568,0.0000034476907,0.0000034596137,0.00066138804,0.000021594582,0.00057465653],"genre_scores_gemma":[0.9979633,0.00006969444,0.00016034376,0.0000041957073,0.0000039239044,0.0000045550964,0.0015740552,0.000005704001,0.00021427861],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999926,0.0000069838993,0.000008410167,0.00002067202,0.00001791582,0.000020053385],"domain_scores_gemma":[0.99935,0.00015377316,0.00015593352,0.000043264026,0.0002114264,0.00008548626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002250015,0.00031111075,0.0001777765,0.00069240044,0.0003115052,0.00045928225,0.00022171024,0.00038163448,0.0005132684],"category_scores_gemma":[0.0014152694,0.00017790012,0.0002270163,0.0011011118,0.00019452228,0.0005063352,0.00025847054,0.00021054674,0.00019204724],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038144315,0.00010271369,0.94050944,0.00010161031,0.00010615715,0.0005579783,0.0010996523,0.028006021,0.0052045393,0.00030018354,0.0022434907,0.021386843],"study_design_scores_gemma":[0.000006341688,0.000028875378,0.98014224,0.0000070432925,0.000043150132,0.00007721521,0.00025032624,0.018471278,0.0004628404,0.00003287197,0.0004622423,0.000015657331],"about_ca_topic_score_codex":0.06082233,"about_ca_topic_score_gemma":0.081706405,"teacher_disagreement_score":0.06082233,"about_ca_system_score_codex":0.00056505133,"about_ca_system_score_gemma":0.00057987747,"threshold_uncertainty_score":0.12093663},"labels":[],"label_agreement":null},{"id":"W2049014512","doi":"10.1144/gsl.sp.2006.268.01.13","title":"Locking of southward extrusion in favour of rapid crustal-scale buckling of the Greater Himalayan sequence, Nar valley, central Nepal","year":2006,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Queen's University","funders":"","keywords":"Geology; Sequence (biology); Scale (ratio); Extrusion; Geochemistry; Geomorphology; Paleontology; Geography; Cartography","score_opus":0.023390479496609825,"score_gpt":0.21425695928134167,"score_spread":0.19086647978473184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049014512","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99630225,0.000110144574,0.00008963354,0.000022386703,0.0000012372047,0.0000039730076,0.00007447596,0.000015994465,0.0033798967],"genre_scores_gemma":[0.9994406,0.000037329337,0.00005222332,0.0000075207927,0.000001278417,0.0000020192292,0.00005299551,0.000003270473,0.00040266194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999473,0.0000056642916,0.000003454319,0.000020732045,0.000009479718,0.0000133237045],"domain_scores_gemma":[0.99988616,0.000016878485,0.000028726605,0.000013899906,0.000034028428,0.000020309846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008900459,0.000114528586,0.00012903911,0.00076312537,0.0006636961,0.000707645,0.00020887551,0.00017150382,0.0021373548],"category_scores_gemma":[0.00031244804,0.00013981754,0.00008928673,0.00048749984,0.0004900593,0.00020414124,0.00044037556,0.0001872719,0.00027770564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024072551,0.000041305764,0.8252702,0.00016985489,0.00011828946,0.0017579219,0.005027825,0.0017031791,0.13810337,0.0010902502,0.00038138143,0.026095755],"study_design_scores_gemma":[0.000003539033,0.000023051549,0.9964347,0.000010796957,0.000007939879,0.00020969,0.0005429932,0.00047377578,0.0012300375,0.000073568735,0.000985301,0.0000046560594],"about_ca_topic_score_codex":0.02019862,"about_ca_topic_score_gemma":0.04171494,"teacher_disagreement_score":0.02019862,"about_ca_system_score_codex":0.00053752353,"about_ca_system_score_gemma":0.00039320168,"threshold_uncertainty_score":0.040162086},"labels":[],"label_agreement":null},{"id":"W2049931942","doi":"10.1016/s0012-821x(00)00082-0","title":"Convergence rate-dependent growth of experimental viscous orogenic wedges","year":2000,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Crust; Deformation (meteorology); Strain rate; Convergence (economics); Geometry; Rate of convergence; Viscosity; Front (military); Mineralogy; Petrology; Geophysics; Materials science; Composite material","score_opus":0.009344531673696348,"score_gpt":0.1953392939356733,"score_spread":0.18599476226197698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049931942","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978976,0.00007469845,0.00082617515,0.000006939714,0.0000047218564,0.00000699533,0.00015926627,0.000020979616,0.0010025816],"genre_scores_gemma":[0.9983285,0.000066683235,0.0007380391,0.000005095644,0.0000015745485,0.0000092364935,0.00028386537,0.000027841166,0.0005390983],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99985516,0.000024942248,0.00002111299,0.000030348996,0.000032157044,0.00003623708],"domain_scores_gemma":[0.9989159,0.00047542935,0.00017004562,0.00019315665,0.00013975623,0.000105686784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020382226,0.00020501921,0.00023641899,0.00037676736,0.00017988523,0.00041509452,0.00043755022,0.00023600098,0.0023213418],"category_scores_gemma":[0.0012926826,0.0001805475,0.0001254681,0.00035781783,0.00045013428,0.00029922527,0.00040623176,0.00039827687,0.0002368016],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011711399,0.00013499396,0.0033800914,0.00009747715,0.000018652248,0.00016600803,0.00023451463,0.007313621,0.982534,0.0014025115,0.00013360036,0.0034133904],"study_design_scores_gemma":[0.00014055852,0.0004827137,0.021649187,0.000023446422,0.00002782712,0.00019852177,0.00022287667,0.05215657,0.92362076,0.00056826713,0.0008853994,0.000023883358],"about_ca_topic_score_codex":0.0015122641,"about_ca_topic_score_gemma":0.0013651906,"teacher_disagreement_score":0.0023213418,"about_ca_system_score_codex":0.0003293539,"about_ca_system_score_gemma":0.00018624956,"threshold_uncertainty_score":0.0077656507},"labels":[],"label_agreement":null},{"id":"W2049950848","doi":"10.1029/2002jb002337","title":"Combined effects of tectonics and glacial isostatic adjustment on intraplate deformation in central and northern Europe: Applications to geodetic baseline analyses","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Ministero dell’Istruzione, dell’Università e della Ricerca","keywords":"Geology; Post-glacial rebound; Tectonics; Geodetic datum; Lithosphere; Geodesy; Baseline (sea); Satellite geodesy; Seismology; Deformation (meteorology); Sea level; Glacial period; Geomorphology","score_opus":0.026449379338598224,"score_gpt":0.30894488126905967,"score_spread":0.28249550193046147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049950848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99586606,0.000076735356,0.0026654564,0.000035440215,0.0000025238512,0.000007290598,0.00047208555,0.000104604194,0.00076989783],"genre_scores_gemma":[0.9964551,0.000053302316,0.0029164925,0.000007425224,0.000002010626,0.0000066346715,0.00039180624,0.000017956834,0.00014931466],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998111,0.00005630897,0.000016507904,0.000049116272,0.000039843984,0.000027149401],"domain_scores_gemma":[0.99970335,0.00013687446,0.00004510314,0.00004221568,0.0000532358,0.000019268928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067566993,0.0003365284,0.00035485358,0.0008848002,0.00026266923,0.00069537456,0.00048134953,0.0005209722,0.00079718634],"category_scores_gemma":[0.0016188249,0.00026585488,0.0006549147,0.0011623136,0.00018439682,0.00045732575,0.00037326344,0.00018859828,0.00009338393],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012412286,0.000073023126,0.13317199,0.000045023826,0.00011854384,0.00014583742,0.00019315862,0.8382395,0.00435184,0.0008605832,0.0002247223,0.022451678],"study_design_scores_gemma":[0.000046933044,0.000092112416,0.1407328,0.000017527967,0.00003654724,0.000075622345,0.00012125652,0.85576373,0.0017490605,0.0005952264,0.00073952775,0.00002957919],"about_ca_topic_score_codex":0.05046188,"about_ca_topic_score_gemma":0.0474787,"teacher_disagreement_score":0.05046188,"about_ca_system_score_codex":0.0008559741,"about_ca_system_score_gemma":0.0005935438,"threshold_uncertainty_score":0.10033631},"labels":[],"label_agreement":null},{"id":"W2050302112","doi":"10.1186/bf03352815","title":"Assessing intraplate earthquake hazards from satellite geopotential field observations","year":2008,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Kongju National University; National Science Foundation","keywords":"Intraplate earthquake; Lithosphere; Geology; Seismology; Geopotential; Gravity anomaly; Geophysics; Crust; Tectonics; Stress field; Satellite; Geodesy; Paleontology","score_opus":0.03526446627556386,"score_gpt":0.22828674177984057,"score_spread":0.1930222755042767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050302112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986577,0.000043503303,0.00035916935,0.000023309525,0.0000011157746,0.0000027091469,0.00035981167,0.000008621434,0.00054415216],"genre_scores_gemma":[0.99911684,0.0000356623,0.00027113906,0.0000040499663,0.0000042008974,0.0000018512449,0.00050552236,0.0000015967222,0.00005915721],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970835,0.000104535175,0.000024004024,0.00004432025,0.000083768144,0.0000350328],"domain_scores_gemma":[0.99757,0.00097429985,0.00073815166,0.00016953058,0.00034676315,0.00020121736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008020439,0.00030603644,0.00016091994,0.0021756005,0.0001379395,0.000645985,0.00019409928,0.00027628825,0.00070910994],"category_scores_gemma":[0.0036201905,0.0001347244,0.00020079498,0.0013919565,0.00017229519,0.00055981707,0.00061903667,0.0002470785,0.00014869479],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007177755,0.000021822294,0.98512566,0.00001047138,0.000059322883,0.000049846465,0.000079340556,0.0047477544,0.00077243266,0.00009859488,0.000116028335,0.008846906],"study_design_scores_gemma":[0.0000050608696,0.00005826106,0.97916436,0.000007702875,0.000028787292,0.000037446473,0.00015985491,0.019897388,0.00036486666,0.00010745444,0.00016299315,0.0000058351998],"about_ca_topic_score_codex":0.012177608,"about_ca_topic_score_gemma":0.020161558,"teacher_disagreement_score":0.012177608,"about_ca_system_score_codex":0.0002517303,"about_ca_system_score_gemma":0.00022981195,"threshold_uncertainty_score":0.024213493},"labels":[],"label_agreement":null},{"id":"W2051157173","doi":"10.1029/00eo00213","title":"Complex faulting confounds earthquake research in the Charlevoix Seismic Zone, Quebec","year":2000,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Intraplate earthquake; Seismology; Geology; Fault (geology); Precambrian; Seismic zone; Seismic gap; Interplate earthquake; Tectonics; Induced seismicity; Paleontology","score_opus":0.08431315062878811,"score_gpt":0.3081171973966832,"score_spread":0.2238040467678951,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051157173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9359855,0.00600991,0.0008087407,0.010699273,0.00011144502,0.000113035836,0.0032627594,0.00003268074,0.042976625],"genre_scores_gemma":[0.9923758,0.0017153599,0.00039217412,0.0005452769,0.000037647656,0.000026155378,0.0005060069,0.000008289089,0.004393474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.998659,0.00039887958,0.000078225064,0.00019034877,0.00028780728,0.0003856374],"domain_scores_gemma":[0.99353665,0.001586036,0.00087037665,0.00041288018,0.0027231753,0.0008708607],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018233228,0.00023002064,0.00034555272,0.0022163992,0.003461038,0.0021986857,0.0011451844,0.0005221021,0.004297763],"category_scores_gemma":[0.008985845,0.00017467703,0.00015884751,0.005097083,0.0021458871,0.0010179494,0.0011227053,0.00049429055,0.00023969555],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019386684,0.000099560726,0.8771387,0.0003040376,0.0001121721,0.000577421,0.010423482,0.0013501627,0.0010751954,0.012082778,0.015476061,0.08116655],"study_design_scores_gemma":[0.00001211371,0.000018924966,0.97771966,0.00013310343,0.000025220068,0.00009156479,0.008677709,0.0005606376,0.00015774784,0.00065507,0.0119290175,0.00001912219],"about_ca_topic_score_codex":0.99203485,"about_ca_topic_score_gemma":0.9977514,"teacher_disagreement_score":0.031227812,"about_ca_system_score_codex":0.031227812,"about_ca_system_score_gemma":0.033292707,"threshold_uncertainty_score":0.22657472},"labels":[],"label_agreement":null},{"id":"W2051338301","doi":"10.5194/nhess-10-641-2010","title":"The challenge of installing a tsunami early warning system in the vicinity of the Sunda Arc, Indonesia","year":2010,"lang":"en","type":"article","venue":"Natural hazards and earth system sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Indian ocean; Warning system; Shore; Natural disaster; Early warning system; Geography; Indonesian; Population; Quarter (Canadian coin); Geology; Seismology; Oceanography; Meteorology; Archaeology; Engineering","score_opus":0.012583018072186956,"score_gpt":0.2194458732753984,"score_spread":0.20686285520321146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051338301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6900107,0.004744631,0.15562691,0.041650835,0.0024174505,0.000364556,0.0010617399,0.0031522445,0.10097103],"genre_scores_gemma":[0.9484284,0.0013027706,0.040691227,0.0005365449,0.00014483184,0.00004675543,0.00029555272,0.00010904043,0.008444874],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99965,0.000103487386,0.0000350037,0.000060795337,0.00010050776,0.000050189963],"domain_scores_gemma":[0.99794465,0.00032153024,0.0001967112,0.00015168979,0.0010778767,0.00030745624],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009815464,0.0002565792,0.00022869783,0.00024649876,0.00062129245,0.0019013516,0.0005800425,0.000575763,0.002398111],"category_scores_gemma":[0.0025363644,0.00015344529,0.00010000849,0.00019343215,0.00028243448,0.0017766148,0.0009932157,0.0009907976,0.0017460694],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00076562294,0.0005116942,0.052295454,0.0009769074,0.000082204824,0.0024324267,0.0017466192,0.031307742,0.061417915,0.012201441,0.048805792,0.78745615],"study_design_scores_gemma":[0.00023927275,0.0016011972,0.13311182,0.0012873543,0.00042090664,0.0040829945,0.026953194,0.36097312,0.07748778,0.029490069,0.3640142,0.00033800583],"about_ca_topic_score_codex":0.0042638406,"about_ca_topic_score_gemma":0.0028180787,"teacher_disagreement_score":0.0042638406,"about_ca_system_score_codex":0.00037787703,"about_ca_system_score_gemma":0.0013021183,"threshold_uncertainty_score":0.008478045},"labels":[],"label_agreement":null},{"id":"W2051678914","doi":"10.1142/s1793431112500236","title":"A STRONG MOTION MODEL OF THE 2004 GREAT SUMATRA EARTHQUAKE: SIMULATION USING A MODIFIED SEMI EMPIRICAL METHOD","year":2012,"lang":"en","type":"article","venue":"Journal of Earthquake and Tsunami","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Indian Institute of Technology Roorkee; McMaster University","keywords":"Seismology; Geology; Magnitude (astronomy); Strong ground motion; Earthquake simulation; Earthquake rupture; Ground motion; Moment magnitude scale; Interplate earthquake; Geodesy; Peak ground acceleration; Fault (geology); Geometry","score_opus":0.08605104489501414,"score_gpt":0.31816086408609356,"score_spread":0.23210981919107943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051678914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6324221,0.00038829606,0.34451324,0.00048408363,0.00007684836,0.00018470547,0.001017755,0.00072385836,0.020189114],"genre_scores_gemma":[0.9549285,0.00022807202,0.040390756,0.000047362264,0.000016672655,0.00021799696,0.00049684156,0.00008149168,0.003592348],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999213,0.000026170615,0.000005698104,0.000011824832,0.00002090744,0.000014112979],"domain_scores_gemma":[0.9996238,0.00020194608,0.00004777789,0.000026998241,0.00007385454,0.000025580248],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022165042,0.00041318926,0.0004947466,0.00038349666,0.0003077058,0.000550151,0.0010958931,0.0010854795,0.0024607775],"category_scores_gemma":[0.000893223,0.00037613537,0.00058864214,0.00035825456,0.00033304407,0.00041853427,0.0005056158,0.00059821643,0.00030410872],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001152185,0.000010321975,0.00050622417,0.000010771856,0.0000060898087,0.000043444663,0.000018124547,0.9973049,0.00046738138,0.0006337924,0.000064738466,0.0009227463],"study_design_scores_gemma":[0.0000024376295,0.0000049199125,0.00007984889,9.614324e-7,0.0000014616874,0.0000040890995,0.0000035125404,0.999708,0.000041524418,0.00007521324,0.00007694387,0.0000010377248],"about_ca_topic_score_codex":0.015163137,"about_ca_topic_score_gemma":0.0080236485,"teacher_disagreement_score":0.015163137,"about_ca_system_score_codex":0.0004482923,"about_ca_system_score_gemma":0.0006205199,"threshold_uncertainty_score":0.030149758},"labels":[],"label_agreement":null},{"id":"W2051831349","doi":"10.1007/s11069-011-9958-6","title":"Tsunami risk for Western Canada and numerical modelling of the Cascadia fault tsunami","year":2011,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Natural hazard; Flooding (psychology); Geology; Seismology; Submarine pipeline; Numerical modeling; Fault (geology); Subduction; Hydrogeology; Oceanography; Geotechnical engineering; Tectonics; Geophysics","score_opus":0.021544749487825737,"score_gpt":0.2037238165205979,"score_spread":0.18217906703277217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051831349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98995334,0.0002825886,0.00048751466,0.0005909547,0.000021579437,0.000017265756,0.0022659344,0.000064198226,0.006316708],"genre_scores_gemma":[0.9955987,0.00021071754,0.00034763225,0.000026881069,0.000004881155,0.0000074744976,0.0009913105,0.000022707394,0.0027896245],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997763,0.000025024336,0.000013958085,0.000041370127,0.00006238368,0.00008105202],"domain_scores_gemma":[0.99892527,0.00023664463,0.00009226608,0.000041189003,0.00050580763,0.00019868535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039301673,0.0007666777,0.00049157074,0.001047947,0.0023388602,0.0024416824,0.0018640875,0.0013246919,0.0038212822],"category_scores_gemma":[0.002166101,0.0006723727,0.0008283905,0.0018588223,0.0010665389,0.00078538817,0.000633308,0.0012079696,0.00029568523],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024701306,0.000117066804,0.060249697,0.000044501612,0.0000976372,0.00026052506,0.00020791402,0.9270327,0.00072967185,0.004580388,0.0030429815,0.0033898659],"study_design_scores_gemma":[0.00007398567,0.000030018984,0.050449494,0.000022635997,0.000059096546,0.0000517869,0.0007596763,0.9454389,0.00031861092,0.0011253578,0.0015964081,0.00007405267],"about_ca_topic_score_codex":0.9947461,"about_ca_topic_score_gemma":0.99123174,"teacher_disagreement_score":0.031434752,"about_ca_system_score_codex":0.031434752,"about_ca_system_score_gemma":0.020134827,"threshold_uncertainty_score":0.22807616},"labels":[],"label_agreement":null},{"id":"W2052200485","doi":"10.1016/j.margeo.2005.03.006","title":"Neogene development of the Antalya Basin, Eastern Mediterranean: An active forearc basin adjacent to an arc junction","year":2005,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Paleontology; Neogene; Late Miocene; Structural basin; Transpression; Forearc; Magnetostratigraphy; Quaternary; Geomorphology; Tectonics; Seismology; Subduction; Sinistral and dextral","score_opus":0.02483105767584261,"score_gpt":0.23172327337160614,"score_spread":0.20689221569576352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052200485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955842,0.0002186596,0.000048715207,0.000049426282,0.000002386078,0.000005100572,0.00004729725,0.000002973912,0.004041226],"genre_scores_gemma":[0.9988456,0.00012343308,0.0001990621,0.000009514987,0.000002270507,0.000003383826,0.000059644124,0.0000027674037,0.0007543165],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999167,0.000012746988,0.0000073096967,0.00002437379,0.000018548757,0.000020366173],"domain_scores_gemma":[0.9998747,0.000011185174,0.000047652946,0.000008141028,0.000038748698,0.000019493975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014823131,0.000119212826,0.00012818689,0.0006292174,0.00041066197,0.000634062,0.00025990378,0.00022330668,0.00085972674],"category_scores_gemma":[0.00037493178,0.00011633792,0.00011597352,0.0006304152,0.00059232477,0.0002945137,0.00054227695,0.00010830291,0.00012274468],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010854137,0.00017248519,0.82521623,0.00035960198,0.00019838201,0.003847265,0.015350057,0.0023984145,0.05895686,0.018269412,0.0008959926,0.07324982],"study_design_scores_gemma":[0.000008754894,0.000025360201,0.99337995,0.000012219332,0.000015789756,0.00035953667,0.00097181933,0.0003175461,0.00039370265,0.00018866376,0.0043234113,0.0000032120342],"about_ca_topic_score_codex":0.023464581,"about_ca_topic_score_gemma":0.056835305,"teacher_disagreement_score":0.023464581,"about_ca_system_score_codex":0.0010746906,"about_ca_system_score_gemma":0.0009856184,"threshold_uncertainty_score":0.046656013},"labels":[],"label_agreement":null},{"id":"W2052201950","doi":"10.1029/2008jb005724","title":"Coseismic strengthening of the shallow portion of the subduction fault and its effects on wedge taper","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Subduction; Geology; Wedge (geometry); Slip (aerodynamics); Seismology; Trench; Geotechnical engineering; Drop (telecommunication); Materials science; Geometry; Tectonics; Composite material","score_opus":0.03286970518997845,"score_gpt":0.27444461839895207,"score_spread":0.24157491320897362,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052201950","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99845374,0.000053599502,0.00069537,0.000017010469,0.0000024276433,0.000002678917,0.00001865523,0.00001528141,0.00074129633],"genre_scores_gemma":[0.99980193,0.00002292351,0.00007125717,0.0000020980829,6.514271e-7,5.572589e-7,0.000007952363,0.000001780119,0.00009086419],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999336,0.000010045408,0.000005311302,0.000013804694,0.000014525702,0.000022639037],"domain_scores_gemma":[0.9997211,0.00005528138,0.00008810012,0.000054937867,0.000032615113,0.000047916656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000120820725,0.0004035042,0.00033622858,0.0004406313,0.00023133853,0.00032691416,0.0003215006,0.00029496217,0.0013971652],"category_scores_gemma":[0.00060067035,0.0002522341,0.00043448035,0.00022991146,0.00038871367,0.00029542486,0.0005927088,0.0003031719,0.00011041485],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007135553,0.00022387298,0.105714045,0.00016718324,0.00010982301,0.0024960183,0.00036014937,0.3736218,0.49745455,0.0026114273,0.00023949333,0.016288033],"study_design_scores_gemma":[0.000082071434,0.00073813275,0.22869597,0.000022007662,0.00011049238,0.0007296474,0.00039846287,0.68426085,0.08337559,0.0009975499,0.000555191,0.000034050787],"about_ca_topic_score_codex":0.0046592946,"about_ca_topic_score_gemma":0.003406978,"teacher_disagreement_score":0.0046592946,"about_ca_system_score_codex":0.00036510467,"about_ca_system_score_gemma":0.00022403816,"threshold_uncertainty_score":0.00926435},"labels":[],"label_agreement":null},{"id":"W2052212359","doi":"10.1029/2009jb007080","title":"Spatial variation of the crustal stress field along the Ryukyu‐Taiwan‐Luzon convergent boundary","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Subduction; Stress field; Convergent boundary; Island arc; Trench; Plate tectonics; Eurasian Plate; Rift; Slab; Accretionary wedge; Seamount; Focal mechanism; Tectonics; Collision zone; Geophysics; Oceanic crust; Paleontology","score_opus":0.020512783847101354,"score_gpt":0.27857627187374734,"score_spread":0.25806348802664597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052212359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989524,0.000017479942,0.000676126,0.0000070404444,0.0000013652182,0.000003028551,0.00018360879,0.000033065644,0.00012588548],"genre_scores_gemma":[0.99779296,0.000016434913,0.0013255714,0.000002783912,0.0000017190679,0.0000087943745,0.0007413743,0.000005942247,0.00010454375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999112,0.000009649024,0.0000058280225,0.00003320145,0.000017347022,0.000022748796],"domain_scores_gemma":[0.9998142,0.000016031125,0.00003695169,0.000021343822,0.000070568916,0.00004090164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021160796,0.00029291,0.00030099376,0.0008177197,0.00020782146,0.00031565232,0.00026736577,0.00020858417,0.0003593351],"category_scores_gemma":[0.0004372727,0.00018337567,0.00030002938,0.00084558985,0.00015819907,0.00017209405,0.00035943292,0.00019528868,0.00010545914],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000281489,0.00013599462,0.74971557,0.0000803274,0.00026804092,0.00061161985,0.0009101267,0.071384616,0.12739511,0.00034555534,0.000564032,0.048307512],"study_design_scores_gemma":[0.000019553807,0.000030054603,0.87007374,0.000008700566,0.000038543865,0.0000600658,0.00016211116,0.12582257,0.0033207142,0.000049239767,0.00039185566,0.00002285178],"about_ca_topic_score_codex":0.038110647,"about_ca_topic_score_gemma":0.0591917,"teacher_disagreement_score":0.038110647,"about_ca_system_score_codex":0.00033187354,"about_ca_system_score_gemma":0.0005348919,"threshold_uncertainty_score":0.07577765},"labels":[],"label_agreement":null},{"id":"W2052383001","doi":"10.1016/j.margeo.2008.02.007","title":"Structural architecture of the Rhodes Basin: A deep depocentre that evolved since the Pliocene at the junction of Hellenic and Cyprus Arcs, eastern Mediterranean","year":2008,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Evaporite; Paleontology; Nappe; Thrust fault; Late Miocene; Subsidence; Transpression; Fault (geology); Structural basin; Fold (higher-order function); Sinistral and dextral; Structural geology; Seismology; Tectonics; Flysch; Fold and thrust belt; Trough (economics); Foreland basin","score_opus":0.018637933298862132,"score_gpt":0.18973546513128284,"score_spread":0.1710975318324207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052383001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99489236,0.00042374912,0.000118450975,0.00010775563,0.000002299859,0.000008465853,0.00010690667,0.0000051217958,0.00433498],"genre_scores_gemma":[0.9992046,0.000118892814,0.00010264921,0.000011833068,0.0000017024973,0.0000020304005,0.0000523202,0.0000035070668,0.0005025772],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998845,0.000018108007,0.000008361148,0.000042698033,0.000019594612,0.000026834532],"domain_scores_gemma":[0.9998796,0.00000902437,0.000036832265,0.000017516199,0.00003185692,0.000025131918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017611378,0.00013345297,0.00018669675,0.00073680165,0.0005380407,0.00086860853,0.00037681672,0.00024937157,0.0014543496],"category_scores_gemma":[0.00043828032,0.0001552606,0.000113028,0.0007158796,0.001028379,0.00029785704,0.000836331,0.00019269326,0.00023145856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023795478,0.00006519414,0.8582426,0.00016350027,0.00022020929,0.0016981364,0.014415259,0.0020345522,0.04091132,0.0075584496,0.0010025563,0.073450334],"study_design_scores_gemma":[0.0000021526612,0.000013568812,0.99669003,0.000011550381,0.000007905679,0.00018853664,0.0010254747,0.00019010506,0.00013707453,0.000071930874,0.0016582477,0.000003317784],"about_ca_topic_score_codex":0.11478026,"about_ca_topic_score_gemma":0.26439688,"teacher_disagreement_score":0.11478026,"about_ca_system_score_codex":0.0010410456,"about_ca_system_score_gemma":0.0007882741,"threshold_uncertainty_score":0.22822428},"labels":[],"label_agreement":null},{"id":"W2052390428","doi":"10.1134/s0001433814050053","title":"Numerical modeling of the long surface waves scattering for the 2011 Japan tsunami: Case study","year":2014,"lang":"en","type":"article","venue":"Izvestiya Atmospheric and Oceanic Physics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization","funders":"U.S. Geological Survey","keywords":"Geology; Dissipation; Scattering; Tsunami wave; Equipartition theorem; Seismology; Rayleigh scattering; Rayleigh distribution; Meteorology; Geophysics; Physics; Optics","score_opus":0.021405782897963244,"score_gpt":0.22261386785386633,"score_spread":0.2012080849559031,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052390428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9700151,0.0004653608,0.021547308,0.00048213394,0.00005746671,0.00004550498,0.00035516915,0.00010275978,0.0069292313],"genre_scores_gemma":[0.99465644,0.00014676519,0.0034745664,0.000023881496,0.000015440139,0.000030629955,0.00016562568,0.000017623355,0.0014690516],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998516,0.0000420013,0.000010482205,0.00002280237,0.000027609452,0.000045451317],"domain_scores_gemma":[0.99920243,0.00045546933,0.000099849254,0.000028332011,0.000153544,0.000060375543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041400857,0.0006652977,0.000632242,0.0005054905,0.0007403073,0.001053357,0.00079117704,0.0016494108,0.0018732205],"category_scores_gemma":[0.001276003,0.00036290495,0.0007559396,0.0006133529,0.00071305805,0.00037196546,0.0006944514,0.0007601137,0.00012992028],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049966933,0.000053466643,0.004081468,0.000025485757,0.000018257082,0.00024128339,0.000044963057,0.9925085,0.0007972207,0.0008000296,0.0001923734,0.0011870089],"study_design_scores_gemma":[0.000004589325,0.000011027018,0.00075149845,0.0000017826483,0.0000045441147,0.000009244567,0.00003214622,0.9989411,0.00009456619,0.000091847534,0.000053994892,0.0000035388857],"about_ca_topic_score_codex":0.047896635,"about_ca_topic_score_gemma":0.022161359,"teacher_disagreement_score":0.047896635,"about_ca_system_score_codex":0.00079885666,"about_ca_system_score_gemma":0.00076421554,"threshold_uncertainty_score":0.095235646},"labels":[],"label_agreement":null},{"id":"W2054581776","doi":"10.1007/s00024-011-0279-1","title":"Energy Decay of the 2004 Sumatra Tsunami in the World Ocean","year":2011,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Tide gauge; Tsunami wave; Oceanography; Geology; Pacific ocean; Indian ocean; Mainland; Tsunami earthquake; Seismology; Submarine pipeline; Oceanic basin; Climatology; Sea level; Geography; Tectonics","score_opus":0.013337413612458986,"score_gpt":0.17991594252573714,"score_spread":0.16657852891327815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054581776","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99763405,0.00013120844,0.00005776792,0.00024067855,0.00001557034,0.0000018681103,0.0006546013,0.00000377477,0.0012605615],"genre_scores_gemma":[0.9981096,0.0001217721,0.00003953987,0.00002824133,0.00000840815,0.000004057522,0.000775957,0.000006222165,0.0009061429],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998565,0.000015139846,0.000019469135,0.000030049543,0.000031591968,0.000047247388],"domain_scores_gemma":[0.9990689,0.00013648464,0.00030641523,0.00006318257,0.00033719023,0.000087782406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003351136,0.00030960146,0.00032192998,0.0012900714,0.0007936652,0.0016028372,0.0004115883,0.0006669848,0.0023086215],"category_scores_gemma":[0.003545993,0.0002280133,0.00029146147,0.0024188026,0.0006310958,0.0011707207,0.0015661496,0.0008199395,0.0004679108],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010134281,0.0001096226,0.93674386,0.00015913468,0.00024496607,0.0014793689,0.00368191,0.017391535,0.0057352143,0.002264556,0.0029720676,0.028204305],"study_design_scores_gemma":[0.000004604938,0.000020589207,0.993869,0.00001690327,0.000032715765,0.00009563669,0.0016378034,0.0020846147,0.00033713641,0.00026263687,0.0016222575,0.000016106987],"about_ca_topic_score_codex":0.098966405,"about_ca_topic_score_gemma":0.12917309,"teacher_disagreement_score":0.098966405,"about_ca_system_score_codex":0.0027822782,"about_ca_system_score_gemma":0.0011136254,"threshold_uncertainty_score":0.19678074},"labels":[],"label_agreement":null},{"id":"W2054816855","doi":"10.1029/2011jb009025","title":"Frictional behavior of oceanic transform faults and its influence on earthquake characteristics","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Transform fault; Slow earthquake; Seismology; Slip (aerodynamics); Scaling; Earthquake rupture; Shear (geology); Intraplate earthquake; Fault (geology); Interplate earthquake; Geometry; Petrology; Tectonics; Thermodynamics; Physics","score_opus":0.037249028354949844,"score_gpt":0.30245908228578633,"score_spread":0.26521005393083646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054816855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99844545,0.000026363252,0.0010324256,0.000019875768,0.0000012945126,0.0000026530154,0.000053915628,0.000022367396,0.0003956623],"genre_scores_gemma":[0.9998029,0.000015298498,0.0001081461,0.0000013818042,4.1404937e-7,0.0000010125754,0.000022787435,0.0000039388156,0.000044261335],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995685,0.000010089317,0.0000036564927,0.000010265407,0.000005637271,0.000013459859],"domain_scores_gemma":[0.99973184,0.000088227935,0.00007895024,0.000034447974,0.000021670006,0.000044896762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001312644,0.00036184577,0.00025277433,0.0003962119,0.000197497,0.00054934534,0.0003527065,0.00038218917,0.0007357173],"category_scores_gemma":[0.0012938005,0.00021110858,0.00040523484,0.0003310933,0.0003509714,0.00035147445,0.00031706807,0.0002710572,0.00006393136],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007239329,0.0000435631,0.057804223,0.000019267382,0.00003824165,0.00015106889,0.00005543238,0.92992705,0.00886697,0.00096903736,0.00007603476,0.0019766986],"study_design_scores_gemma":[0.000009012053,0.000030275496,0.016670473,0.0000029319442,0.000010242386,0.000024881843,0.000025975822,0.9821685,0.00082208967,0.00017658052,0.000050558367,0.000008484437],"about_ca_topic_score_codex":0.020297548,"about_ca_topic_score_gemma":0.009371982,"teacher_disagreement_score":0.020297548,"about_ca_system_score_codex":0.0005115855,"about_ca_system_score_gemma":0.00026274635,"threshold_uncertainty_score":0.04035884},"labels":[],"label_agreement":null},{"id":"W2054955556","doi":"10.1016/j.margeo.2005.03.013","title":"The Neogene evolution of the Outer Latakia Basin and its extension into the Eastern Mesaoria Basin (Cyprus), Eastern Mediterranean","year":2005,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Structural basin; Fold and thrust belt; Anticline; Nappe; Foreland basin; Fold (higher-order function); Neogene; Paleontology; Thrust fault; Subduction; Seismology; Tectonics; Pull apart basin; Geomorphology; Sedimentary basin","score_opus":0.014717167004257029,"score_gpt":0.2125988580844265,"score_spread":0.19788169108016945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054955556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960157,0.00026447684,0.00004670208,0.00007796788,0.0000026320135,0.0000025728875,0.000059146736,0.000002480739,0.0035282883],"genre_scores_gemma":[0.998978,0.0001455439,0.000048889662,0.000012268732,0.000002873076,0.0000029182731,0.000050633647,0.0000023867433,0.0007564247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999404,0.000010020589,0.000004747406,0.000015382666,0.000008993114,0.000020495192],"domain_scores_gemma":[0.9998307,0.000021865011,0.00005956998,0.00001179385,0.000046227353,0.000029700448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016684295,0.00013232886,0.000113200906,0.0011006906,0.0006139933,0.0009180173,0.00022442259,0.00023817878,0.0017618824],"category_scores_gemma":[0.0005452979,0.00013064404,0.00012726395,0.00096610235,0.0008122703,0.00051465066,0.00061785366,0.0001860066,0.0002065934],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005568934,0.000068324734,0.8992398,0.00010428746,0.00010131542,0.0016813303,0.0073087867,0.0030361656,0.017807871,0.0083571235,0.0008398714,0.060898248],"study_design_scores_gemma":[0.000002913099,0.000005322598,0.9976301,0.000010642694,0.0000050932745,0.00008104875,0.000352995,0.00021219235,0.00010223707,0.00010652935,0.0014893803,0.0000014936303],"about_ca_topic_score_codex":0.036340993,"about_ca_topic_score_gemma":0.0719395,"teacher_disagreement_score":0.036340993,"about_ca_system_score_codex":0.0017291944,"about_ca_system_score_gemma":0.00090015586,"threshold_uncertainty_score":0.07225889},"labels":[],"label_agreement":null},{"id":"W2055056269","doi":"10.1029/2006je002847","title":"Temporal and spatial properties of some deep moonquake clusters","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Longitude; Geology; Cluster (spacecraft); Seismology; Induced seismicity; Geodesy; Event (particle physics); Latitude; Point source; Phase (matter); Relocation; Earthquake location; Computer science; Astrophysics; Physics","score_opus":0.041323473051663395,"score_gpt":0.28543934423903955,"score_spread":0.24411587118737615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055056269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99835014,0.00003751386,0.0005478241,0.000015838667,0.0000017472628,0.000004820553,0.00061052217,0.000025492773,0.00040606584],"genre_scores_gemma":[0.9967726,0.00002824929,0.00072006194,0.000004992534,0.000005927345,0.000008149307,0.0022007034,0.000019653497,0.00023971446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985063,0.000012306318,0.000015260788,0.000050678846,0.000029549887,0.000041550466],"domain_scores_gemma":[0.99828583,0.00041826308,0.00044444288,0.00020743057,0.000339403,0.0003045919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000419339,0.00014490314,0.00025959496,0.0018730529,0.00042692252,0.0005677595,0.0002591936,0.00018772743,0.0010902876],"category_scores_gemma":[0.0018584331,0.00019712732,0.00020727153,0.001591288,0.00023926469,0.00035460043,0.0008466605,0.00024455716,0.00020741564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037927815,0.000051228533,0.95956475,0.000045600333,0.0000654295,0.00035597276,0.0010590613,0.004766671,0.014802632,0.0005769667,0.0008027519,0.017529644],"study_design_scores_gemma":[0.000009696729,0.00002719048,0.9938129,0.0000034762609,0.000014500204,0.00018172621,0.000173227,0.0041690217,0.0007430023,0.0001727438,0.0006803129,0.000012271521],"about_ca_topic_score_codex":0.0072369967,"about_ca_topic_score_gemma":0.012605164,"teacher_disagreement_score":0.0072369967,"about_ca_system_score_codex":0.00027933076,"about_ca_system_score_gemma":0.00016520749,"threshold_uncertainty_score":0.014389753},"labels":[],"label_agreement":null},{"id":"W2055123544","doi":"10.1029/2003gl018644","title":"Effects of metamorphic crustal densification on earthquake size in warm slabs","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Crust; Geology; Slab; Seismology; Metamorphic rock; Mantle (geology); Deep-focus earthquake; Compression (physics); Petrology; Geophysics; Subduction; Tectonics; Materials science","score_opus":0.02895967934539929,"score_gpt":0.2760373169740348,"score_spread":0.2470776376286355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055123544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953043,0.00008697313,0.00003866379,0.000019418289,6.7127746e-7,8.969408e-7,0.000060905048,0.0000040078976,0.00025801302],"genre_scores_gemma":[0.9997135,0.000033038108,0.00001941314,0.0000052746514,0.0000016384394,7.971998e-7,0.000057208013,0.0000027173805,0.00016639696],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998523,0.00003461805,0.0000139285485,0.000027298485,0.000024671534,0.000047151585],"domain_scores_gemma":[0.9978161,0.00070244964,0.00057941844,0.00020437023,0.00011854782,0.0005790889],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043826527,0.00019627508,0.00026302983,0.0004177094,0.00024426193,0.0005931038,0.00021252209,0.00024574666,0.003982652],"category_scores_gemma":[0.0029586875,0.00024484086,0.0002496816,0.00021407484,0.0007176566,0.000379909,0.00096676854,0.00036255445,0.00023046718],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022980592,0.00013036556,0.84605736,0.00008320003,0.00020498979,0.000685937,0.00065827905,0.0061870483,0.13101928,0.00048788392,0.00016441979,0.012023143],"study_design_scores_gemma":[0.000007943761,0.00009465563,0.99648464,0.0000026987673,0.000020885536,0.00013157321,0.00011931624,0.0003945339,0.002552447,0.000094498784,0.00009226667,0.0000045493493],"about_ca_topic_score_codex":0.0040527787,"about_ca_topic_score_gemma":0.005498787,"teacher_disagreement_score":0.0040527787,"about_ca_system_score_codex":0.0004490262,"about_ca_system_score_gemma":0.00016224742,"threshold_uncertainty_score":0.013323307},"labels":[],"label_agreement":null},{"id":"W2055131863","doi":"10.1029/2008jb005698","title":"Thermal and structural models of the Sumatra subduction zone: Implications for the megathrust seismogenic zone","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Subduction; Trench; Geology; Seismology; Thermal; Thrust; Mantle (geology); Geophysics; Tectonics","score_opus":0.06066280158783275,"score_gpt":0.2997758152996119,"score_spread":0.23911301371177915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055131863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.936567,0.0004891084,0.042083796,0.0007839134,0.000033232227,0.000052507734,0.0006604973,0.00016632603,0.019163601],"genre_scores_gemma":[0.995175,0.00017543303,0.0027163466,0.000028573753,0.000008990564,0.000039033013,0.000118802345,0.000028721202,0.001709075],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999261,0.000022271566,0.0000054195516,0.000018442906,0.000013039695,0.000014832157],"domain_scores_gemma":[0.99984884,0.000050113507,0.000035488214,0.000019251564,0.000026857873,0.000019433406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015211626,0.0005194338,0.0003131232,0.0003967138,0.00039532108,0.0010803677,0.0011453666,0.00076917233,0.002356014],"category_scores_gemma":[0.0006181487,0.0004872126,0.00050378725,0.00029553642,0.00060513226,0.00072251615,0.0005525929,0.00042810358,0.0002883064],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011979732,0.000012265577,0.0017339544,0.000009729241,0.0000072149496,0.000028647011,0.000050451563,0.993468,0.0010058358,0.0028808187,0.00005150721,0.0007397362],"study_design_scores_gemma":[0.000010155203,0.000009410425,0.0024121865,0.0000056517156,0.000005220839,0.000017435525,0.00004164121,0.9944669,0.00017693694,0.0024876026,0.00035993697,0.0000068622776],"about_ca_topic_score_codex":0.024190377,"about_ca_topic_score_gemma":0.016485315,"teacher_disagreement_score":0.024190377,"about_ca_system_score_codex":0.0013404711,"about_ca_system_score_gemma":0.000622229,"threshold_uncertainty_score":0.0480991},"labels":[],"label_agreement":null},{"id":"W2055392736","doi":"10.1130/g25145a.1","title":"Effects of fluid circulation in subducting crust on Nankai margin seismogenic zone temperatures","year":2008,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Crust; Geological survey; Citation; Margin (machine learning); Subduction; Library science; Seismology; Geochemistry; Paleontology; Tectonics","score_opus":0.011442988459060935,"score_gpt":0.1975791641812456,"score_spread":0.18613617572218466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055392736","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911999,0.0006095991,0.00016837206,0.0005624635,0.000055421166,0.000010555084,0.00057636015,0.000043710243,0.0067735016],"genre_scores_gemma":[0.99824023,0.00037730677,0.000082533006,0.000030235233,0.000020011732,0.0000040360574,0.0002750985,0.000017301936,0.00095325615],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999063,0.000011777835,0.000013111849,0.000018575172,0.000025751911,0.000024529541],"domain_scores_gemma":[0.9997342,0.000044487148,0.00008288213,0.00000978918,0.00008541887,0.000043204207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021641795,0.00022280244,0.0003112585,0.00071443885,0.00059464935,0.0011406835,0.00025448157,0.00039914745,0.004685548],"category_scores_gemma":[0.0011453306,0.00021906597,0.0003008859,0.0006269508,0.0006380742,0.0007618277,0.0010346841,0.00045798905,0.0006672674],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012052793,0.00009903362,0.87061465,0.0004196574,0.0002981603,0.0011513332,0.002089983,0.012472012,0.065151535,0.0013569734,0.004648253,0.040493064],"study_design_scores_gemma":[0.000029567958,0.000056604214,0.9940606,0.000027663778,0.000043003118,0.000046039004,0.00046710996,0.0017554008,0.001506094,0.0002296116,0.0017618453,0.00001641078],"about_ca_topic_score_codex":0.041140445,"about_ca_topic_score_gemma":0.031902086,"teacher_disagreement_score":0.041140445,"about_ca_system_score_codex":0.0012425168,"about_ca_system_score_gemma":0.00067623233,"threshold_uncertainty_score":0.08180195},"labels":[],"label_agreement":null},{"id":"W2055672408","doi":"10.1007/s007100200010","title":"Experimental studies on three potassium-rich ultramafic rocks from Damodar Valley, East India","year":2002,"lang":"en","type":"article","venue":"Mineralogy and Petrology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Phlogopite; Ultramafic rock; Olivine; Geology; Geochemistry; Ilmenite; Apatite; Mineralogy; Mantle (geology)","score_opus":0.03530329830471205,"score_gpt":0.23493556584513633,"score_spread":0.1996322675404243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055672408","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995023,0.000008487191,0.000058939982,0.0000046396153,0.0000010549688,0.000011295903,0.000044667682,0.000001607608,0.00036702343],"genre_scores_gemma":[0.99817884,0.000046295827,0.00040938062,0.000014058242,0.0000022086776,0.000017089744,0.00020581487,0.0000038673184,0.001122451],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998185,0.000014681563,0.000016023812,0.00005359681,0.00003459751,0.00006265062],"domain_scores_gemma":[0.99961334,0.00010459345,0.00005510121,0.000052032734,0.000103310536,0.00007174336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001566168,0.00035258144,0.00041892345,0.00048424146,0.0017322758,0.00037316312,0.00080459524,0.00046995856,0.0014782056],"category_scores_gemma":[0.00034485466,0.00026307473,0.00034862536,0.0006765308,0.001013155,0.00038217055,0.00068753946,0.0004755394,0.00035925664],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0048707398,0.0018211992,0.14241694,0.0003004434,0.00008919149,0.005519569,0.0100475885,0.0012999068,0.82496136,0.0006995692,0.00017315336,0.0078003253],"study_design_scores_gemma":[0.00029668215,0.01106741,0.6758473,0.00003262273,0.00031129434,0.003984072,0.018915156,0.0013765846,0.28284466,0.00038880488,0.0048678843,0.000067452456],"about_ca_topic_score_codex":0.013304501,"about_ca_topic_score_gemma":0.02551379,"teacher_disagreement_score":0.013304501,"about_ca_system_score_codex":0.00041780755,"about_ca_system_score_gemma":0.00048460928,"threshold_uncertainty_score":0.02645415},"labels":[],"label_agreement":null},{"id":"W2056007538","doi":"10.1002/2013gc005198","title":"Maar‐diatreme geometry and deposits: Subsurface blast experiments with variable explosion depth","year":2014,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Natural Sciences and Engineering Research Council of Canada; University at Buffalo","keywords":"Diatreme; Ejecta; Impact crater; Maar; Geology; Phreatomagmatic eruption; Xenolith; Petrology; Volcano; Magma; Seismology; Geophysics; Basalt; Kimberlite; Astrobiology; Physics; Mantle (geology)","score_opus":0.009843020965610483,"score_gpt":0.18752713075222888,"score_spread":0.1776841097866184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056007538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996044,0.000017082824,0.00019747292,0.000001906782,8.9666247e-7,0.000008756462,0.000046153415,0.000005065489,0.00011827935],"genre_scores_gemma":[0.9990274,0.0000310175,0.0005999831,0.0000047577855,0.0000010778853,0.000015861327,0.000058230962,0.0000059138233,0.0002557624],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99989676,0.0000146067905,0.000009336318,0.000024669973,0.000029197916,0.000025409936],"domain_scores_gemma":[0.99972814,0.00009497831,0.000053601114,0.000038254275,0.000040216117,0.000044800658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019150616,0.0003225478,0.00021533424,0.00018644218,0.00016362766,0.00024322336,0.0002868106,0.00024427404,0.0010931268],"category_scores_gemma":[0.00031527516,0.00022793918,0.00013647732,0.00016858811,0.00029031635,0.0001891176,0.0004531423,0.00039952662,0.00008022965],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00076449855,0.00019587918,0.0028120077,0.000022320375,0.0000089420355,0.000075733224,0.000112266825,0.0008750728,0.9935939,0.00005196413,0.000015849555,0.0014716678],"study_design_scores_gemma":[0.00025301083,0.0071673985,0.12141696,0.00001158469,0.00006531884,0.00022313566,0.0004456899,0.012658536,0.85680795,0.00018728578,0.0007306596,0.00003244189],"about_ca_topic_score_codex":0.0013028416,"about_ca_topic_score_gemma":0.0016612667,"teacher_disagreement_score":0.0013028416,"about_ca_system_score_codex":0.00023238928,"about_ca_system_score_gemma":0.00009522658,"threshold_uncertainty_score":0.0036568642},"labels":[],"label_agreement":null},{"id":"W2057431298","doi":"10.1029/2003gl018014","title":"Source model for the M<sub><i>w</i></sub> 6.7, 23 October 2002, Nenana Mountain Earthquake (Alaska) from InSAR","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":209,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Hypocenter; Geology; Seismology; Interferometric synthetic aperture radar; Crust; Geodesy; Slip (aerodynamics); Source model; Synthetic aperture radar; Induced seismicity; Geophysics; Remote sensing","score_opus":0.041195945501439804,"score_gpt":0.2670367976828869,"score_spread":0.22584085218144712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057431298","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.33300042,0.0013222405,0.41785705,0.0025506692,0.0010323253,0.0005195855,0.11197131,0.009684034,0.12206236],"genre_scores_gemma":[0.85666984,0.00070227444,0.031004205,0.00024549954,0.00018148484,0.0004459705,0.032988,0.00091013685,0.07685252],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999447,0.0000069287216,0.00000388506,0.000015658941,0.000018436283,0.000010362797],"domain_scores_gemma":[0.99987996,0.000020760799,0.000016018868,0.000011209324,0.00006316986,0.000008887362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011021941,0.00071842846,0.0005522146,0.0006480455,0.0005290227,0.00070487836,0.001803466,0.0015410071,0.014461377],"category_scores_gemma":[0.00039150193,0.00047392186,0.00046917994,0.00087097596,0.00020812228,0.00070484716,0.00034519084,0.0007813884,0.0049730754],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001347923,0.000084690364,0.005189681,0.000108598455,0.000051799816,0.00040726733,0.00014823688,0.944431,0.0050847647,0.013566972,0.018271422,0.012520742],"study_design_scores_gemma":[0.00006670357,0.000026919854,0.0021439388,0.000012320894,0.00003176887,0.000106337364,0.000047172023,0.9842604,0.0006796445,0.002458645,0.010141926,0.000024297458],"about_ca_topic_score_codex":0.0777477,"about_ca_topic_score_gemma":0.05237429,"teacher_disagreement_score":0.0777477,"about_ca_system_score_codex":0.0007961551,"about_ca_system_score_gemma":0.001035504,"threshold_uncertainty_score":0.15459031},"labels":[],"label_agreement":null},{"id":"W2057447701","doi":"10.1038/nature03412","title":"Measuring the onset of locking in the Peru–Chile trench with GPS and acoustic measurements","year":2005,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":209,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences; National Science Foundation","keywords":"Geology; Subduction; Seismology; Trench; Seafloor spreading; Submarine pipeline; Plate tectonics; Pacific Plate; Slip (aerodynamics); Convergent boundary; Episodic tremor and slip; Global Positioning System; Thrust fault; Fault (geology); Fracture zone; Tectonics; Oceanography; Oceanic crust","score_opus":0.027041533039797266,"score_gpt":0.21982931801142902,"score_spread":0.19278778497163176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057447701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99316204,0.00010917573,0.00079780276,0.000054238502,0.000004574552,0.000024552115,0.00031764572,0.000032532844,0.005497528],"genre_scores_gemma":[0.9980483,0.00004317246,0.000617737,0.000014205288,0.000003938561,0.000022932021,0.00021040726,0.000005906924,0.0010332552],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985003,0.00003144901,0.0000061066426,0.00004071823,0.000031103555,0.00004060593],"domain_scores_gemma":[0.9993241,0.0001804921,0.00013991512,0.000054536,0.00020600542,0.00009501882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033761087,0.00018457837,0.00015052076,0.0010138887,0.00037667502,0.00059271394,0.00041020653,0.00045464278,0.0014417857],"category_scores_gemma":[0.0017993888,0.0002606545,0.000106711275,0.00092379167,0.00037901907,0.00048559118,0.0009697515,0.00038824408,0.00041798645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055555615,0.00012438848,0.8828141,0.00009936332,0.000068892434,0.00036644944,0.0040051234,0.0012800874,0.0785002,0.00049537036,0.0007269864,0.030963521],"study_design_scores_gemma":[0.000015627653,0.000055630382,0.9950794,0.0000142498075,0.000013013124,0.00005721948,0.00072352623,0.0008543336,0.0020804396,0.000052122337,0.0010444683,0.000009974863],"about_ca_topic_score_codex":0.028394612,"about_ca_topic_score_gemma":0.061332628,"teacher_disagreement_score":0.028394612,"about_ca_system_score_codex":0.0005426128,"about_ca_system_score_gemma":0.00049839285,"threshold_uncertainty_score":0.056458652},"labels":[],"label_agreement":null},{"id":"W2058050440","doi":"10.1029/2003gl017534","title":"The importance of the third dimension in granular shear","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Shear (geology); Granular material; Amplitude; Mechanics; Fault gouge; Shear rate; Geotechnical engineering; Materials science; Physics; Statistical physics; Geology; Thermodynamics; Fault (geology); Rheology; Optics; Composite material","score_opus":0.02833553622571882,"score_gpt":0.2734755420952547,"score_spread":0.24514000586953588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058050440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9009037,0.00048201962,0.08764198,0.00058574206,0.000117819094,0.000022867453,0.00010131594,0.00036897892,0.009775659],"genre_scores_gemma":[0.99465334,0.00012595965,0.0048909076,0.000029133382,0.000011172776,0.000012625111,0.0000151694185,0.00002370977,0.00023806324],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998745,0.000024408795,0.00000761471,0.000017650478,0.000044526623,0.000031223048],"domain_scores_gemma":[0.9988254,0.0006098605,0.00016656621,0.00016746743,0.00008221332,0.0001485398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030981968,0.0003008288,0.00043387542,0.00030812822,0.0007753108,0.001807166,0.00031912874,0.0007979585,0.0006084757],"category_scores_gemma":[0.0022721717,0.00038975113,0.0005815989,0.00032031385,0.0013761648,0.0011726421,0.001110168,0.0009757715,0.00009367646],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023812316,0.00007486656,0.007371209,0.00006058867,0.000042743482,0.0002862917,0.00018287562,0.92562395,0.017524017,0.042362723,0.00048370415,0.0057488913],"study_design_scores_gemma":[0.000015238545,0.00003471346,0.001453844,0.0000076529195,0.000011253656,0.000045563578,0.000018373867,0.9873378,0.0017884095,0.008746038,0.0005193096,0.000021785823],"about_ca_topic_score_codex":0.0046176133,"about_ca_topic_score_gemma":0.003736093,"teacher_disagreement_score":0.0046176133,"about_ca_system_score_codex":0.000634367,"about_ca_system_score_gemma":0.0009428926,"threshold_uncertainty_score":0.00918144},"labels":[],"label_agreement":null},{"id":"W2058344069","doi":"10.1029/2003eo410002","title":"Deformation of the 2002 Denali Fault Earthquakes, mapped by Radarsat‐1 interferometry","year":2003,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Geology; Seismology; Slip (aerodynamics); Thrust fault; Aftershock; Glacier; Magnitude (astronomy); Fault (geology); Seismic gap; Geodesy; Geomorphology","score_opus":0.01077251870256016,"score_gpt":0.19364317765690087,"score_spread":0.1828706589543407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058344069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967895,0.00006125406,0.00005533595,0.000027359187,0.0000047310923,0.000006073638,0.0014679877,0.000015600484,0.0015720314],"genre_scores_gemma":[0.9954802,0.00008356561,0.00017085028,0.0000137438665,0.0000043818,0.000007558388,0.0035141075,0.0000033078966,0.00072224933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992776,0.00000792708,0.0000061661494,0.000024481249,0.000019717965,0.000013979665],"domain_scores_gemma":[0.99987185,0.000009766644,0.000044916538,0.000012912396,0.00004132605,0.000019142815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013723811,0.00021586008,0.00014195783,0.000754981,0.00032814164,0.00047282377,0.00017319336,0.00026222758,0.00067185547],"category_scores_gemma":[0.00039964414,0.00013057367,0.00007275894,0.0007515402,0.00012272502,0.0002498235,0.0002657682,0.00013508265,0.0003317097],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003836007,0.00023150849,0.9354753,0.00009035825,0.00010126403,0.00042236905,0.001562911,0.002411104,0.027249517,0.00026072797,0.004876322,0.026935019],"study_design_scores_gemma":[0.0000019812492,0.000012805522,0.99788374,0.0000023399182,0.000004616116,0.00004707738,0.0001514985,0.00042865117,0.0004903927,0.000006058484,0.00096777984,0.0000029348255],"about_ca_topic_score_codex":0.039750915,"about_ca_topic_score_gemma":0.123652756,"teacher_disagreement_score":0.039750915,"about_ca_system_score_codex":0.00041244057,"about_ca_system_score_gemma":0.0002456738,"threshold_uncertainty_score":0.07903904},"labels":[],"label_agreement":null},{"id":"W2058974231","doi":"10.1142/s1793431108000293","title":"INDIAN OCEAN TSUNAMI ON 26 DECEMBER 2004: NUMERICAL MODELING OF INUNDATION IN THREE CITIES ON THE SOUTH COAST OF SRI LANKA","year":2008,"lang":"en","type":"article","venue":"Journal of Earthquake and Tsunami","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; McMaster University; National Science Foundation","keywords":"Sri lanka; Indian ocean; SAFER; Geography; Bathymetry; Geology; Warning system; Oceanography; Environmental planning; Engineering","score_opus":0.03191335019471069,"score_gpt":0.22202487771240872,"score_spread":0.19011152751769803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058974231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972777,0.000031095748,0.0004265319,0.00013586677,0.000009248195,0.000016921595,0.00023754525,0.00003587519,0.0018292089],"genre_scores_gemma":[0.9985489,0.000043674187,0.0004894243,0.000017006334,0.0000034145655,0.00001911253,0.00023463939,0.00001027118,0.00063338166],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998338,0.000038847753,0.000011812345,0.000024273515,0.000017223023,0.000073941104],"domain_scores_gemma":[0.9995964,0.00013283783,0.000057817717,0.00003232087,0.00008954035,0.0000911576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022344086,0.0006319089,0.0006393151,0.0005418737,0.0012724579,0.0014659697,0.0013054562,0.0015967936,0.0019568736],"category_scores_gemma":[0.0010436912,0.00060905534,0.0010656457,0.0009144965,0.0012490543,0.00057283643,0.0009937647,0.001135608,0.00025448567],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001972419,0.0001670841,0.04091395,0.00002535733,0.00007779504,0.0007266164,0.00032037095,0.9537087,0.0011516127,0.00075676624,0.0007420894,0.0012123956],"study_design_scores_gemma":[0.000079789366,0.00009605198,0.023120094,0.000009383959,0.00004365206,0.00005644316,0.00094124617,0.9747327,0.00035173396,0.00020332633,0.00033153564,0.00003409132],"about_ca_topic_score_codex":0.26990855,"about_ca_topic_score_gemma":0.17491601,"teacher_disagreement_score":0.26990855,"about_ca_system_score_codex":0.0025631397,"about_ca_system_score_gemma":0.0014529506,"threshold_uncertainty_score":0.536675},"labels":[],"label_agreement":null},{"id":"W2059198447","doi":"10.1785/gssrl.81.1.129","title":"Historical Earthquake Damage in the Ottawa-Gatineau Region, Canada","year":2010,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Icon; Citation; Download; Geography; Library science; History; Population; Cartography; Archaeology; Demography; Computer science; World Wide Web; Sociology","score_opus":0.055151744664310616,"score_gpt":0.27575398769588816,"score_spread":0.22060224303157755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059198447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.54073244,0.034482244,0.00023979148,0.006475553,0.00063280476,0.0004479416,0.27280802,0.0003411519,0.14384],"genre_scores_gemma":[0.83588874,0.024681184,0.00051169505,0.0006869337,0.00010213956,0.00013891654,0.04584979,0.00011205326,0.09202855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994211,0.000013782626,0.000039011335,0.00005663906,0.00018645464,0.00028309188],"domain_scores_gemma":[0.99835217,0.000047621143,0.00017392034,0.000045870285,0.00084536977,0.00053510274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017681054,0.0005872908,0.00035435898,0.0033881438,0.0042277514,0.0019716178,0.0011350985,0.00049543416,0.01384848],"category_scores_gemma":[0.0014058514,0.0004119078,0.0003786843,0.0075028683,0.00077096844,0.0005318545,0.0016175453,0.0006727243,0.0019350593],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003567332,0.00006984034,0.59294,0.0014797754,0.00023155718,0.0016784564,0.00916862,0.0012369318,0.00087214215,0.0019385946,0.26853845,0.12148899],"study_design_scores_gemma":[0.000011268636,0.000016656917,0.9374261,0.00028744794,0.00003345257,0.00023459026,0.004228702,0.000104573424,0.00010467999,0.00005969368,0.05745436,0.000038457943],"about_ca_topic_score_codex":0.99771607,"about_ca_topic_score_gemma":0.99936277,"teacher_disagreement_score":0.03680876,"about_ca_system_score_codex":0.03680876,"about_ca_system_score_gemma":0.049810786,"threshold_uncertainty_score":0.2670675},"labels":[],"label_agreement":null},{"id":"W2059504285","doi":"10.1007/s00024-014-1012-7","title":"Observations and Numerical Modeling of the 2012 Haida Gwaii Tsunami off the Coast of British Columbia","year":2014,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Geology; Storm; Oceanography; Seismology; Tide gauge; Numerical modeling; Inlet; Sea level; Geophysics","score_opus":0.013080083257557704,"score_gpt":0.17794250517287769,"score_spread":0.16486242191531997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059504285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996496,0.000047197937,0.00016206376,0.00016016436,0.000008947481,0.00000987588,0.001042441,0.000043336466,0.0020298953],"genre_scores_gemma":[0.99836665,0.000053818654,0.0001902869,0.000013206322,0.0000024128035,0.000009860281,0.0008060647,0.0000083838095,0.0005493949],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998154,0.000022290558,0.00001487295,0.000047526853,0.00003709162,0.00006288957],"domain_scores_gemma":[0.999482,0.00011016099,0.000069455,0.00004869692,0.00021330596,0.00007640991],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021179831,0.00039120123,0.0002547962,0.0007195683,0.0014105566,0.0013883811,0.001110459,0.000984731,0.0015112228],"category_scores_gemma":[0.0018318946,0.00058656547,0.00033609316,0.0013361163,0.0006495397,0.0005622628,0.0005856351,0.0007764875,0.00035294768],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000400895,0.00045808125,0.47701028,0.00011176908,0.00018899825,0.00071252213,0.0012016745,0.49139938,0.006939755,0.0012783976,0.0061978595,0.014100487],"study_design_scores_gemma":[0.000089228364,0.000032386746,0.47008753,0.000030436227,0.00005243699,0.00005043913,0.0011399677,0.525318,0.0008464734,0.00023952588,0.0020316988,0.00008183675],"about_ca_topic_score_codex":0.9485425,"about_ca_topic_score_gemma":0.9461281,"teacher_disagreement_score":0.051457524,"about_ca_system_score_codex":0.0071544955,"about_ca_system_score_gemma":0.0044913064,"threshold_uncertainty_score":0.10352111},"labels":[],"label_agreement":null},{"id":"W2059880183","doi":"10.1007/s11069-013-0622-1","title":"Recurrence intervals of major paleotsunamis as calibrated by historic tsunami deposits in three localities: Port Alberni, Cannon Beach, and Crescent City, along the Cascadia margin, Canada and USA","year":2013,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Subduction; Bay; Seismology; Margin (machine learning); Subsidence; Natural hazard; Microearthquake; Paleontology; Oceanography; Tectonics; Induced seismicity","score_opus":0.007645456142264041,"score_gpt":0.199349119321727,"score_spread":0.19170366317946297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059880183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99859625,0.000038032238,0.00004363392,0.000016867629,0.0000015915572,0.0000013446602,0.0009450727,0.0000074805043,0.00034975616],"genre_scores_gemma":[0.99849343,0.000028786237,0.00003542054,0.0000022050879,0.0000011192376,0.0000015763923,0.0012351683,0.0000019003428,0.00020037233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989915,0.000011594511,0.00001003297,0.00003171997,0.000020469952,0.000027061029],"domain_scores_gemma":[0.99906486,0.00014739936,0.00019434257,0.000061825434,0.0003612492,0.00017038154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002518873,0.00013332501,0.00012576251,0.0013086518,0.00055199204,0.0004928025,0.00049697066,0.00020500456,0.0012002633],"category_scores_gemma":[0.0014449306,0.000144886,0.0001710252,0.0017796542,0.00036683516,0.00023116106,0.00039019447,0.00024022818,0.0001535299],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000087505454,0.000009264917,0.9954725,0.000005484007,0.00004048942,0.00004512603,0.0005459211,0.0009819206,0.00030344777,0.00009724446,0.00037142605,0.0020395848],"study_design_scores_gemma":[0.0000024818805,0.0000036926838,0.99891365,0.0000023054822,0.000008371835,0.000015152873,0.00036371735,0.00046370996,0.000043675813,0.000012066438,0.00016850518,0.0000027392384],"about_ca_topic_score_codex":0.8055342,"about_ca_topic_score_gemma":0.90884435,"teacher_disagreement_score":0.19446582,"about_ca_system_score_codex":0.0022413714,"about_ca_system_score_gemma":0.0012884733,"threshold_uncertainty_score":0.39122212},"labels":[],"label_agreement":null},{"id":"W2059977250","doi":"10.1002/2014jb011004","title":"Thermo‐poro‐mechanics of chemically active creeping faults: 3. The role of serpentinite in episodic tremor and slip sequences, and transition to chaos","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"CMG Reservoir Simulation Foundation; National Science Foundation","keywords":"Geology; Subduction; Seismology; Trench; Slip (aerodynamics); Geophysics; Tectonics; Physics; Materials science; Nanotechnology","score_opus":0.020681724787690706,"score_gpt":0.28110977718006136,"score_spread":0.26042805239237066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059977250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976889,0.00009734004,0.0011229159,0.00004825345,0.0000025226902,0.0000044293297,0.000051793875,0.000020202733,0.0009637248],"genre_scores_gemma":[0.9998179,0.000024833327,0.00006039752,0.0000015954719,0.0000013373158,7.860242e-7,0.000010534002,0.0000018315723,0.00008082837],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999695,0.0000035371238,0.0000026196333,0.000009403804,0.000007289484,0.000007638687],"domain_scores_gemma":[0.9998789,0.000019118175,0.000055730656,0.000012409684,0.000015431808,0.000018396697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010993955,0.00021286582,0.0001706733,0.0005074283,0.00021322272,0.0005913363,0.00029079366,0.00032090498,0.0011093916],"category_scores_gemma":[0.00025985896,0.00017864157,0.00019567003,0.00017553222,0.0006114944,0.00038931094,0.00031665902,0.00016497639,0.00012107179],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050953054,0.0001999053,0.30314288,0.0002783069,0.00011856497,0.0022264235,0.00074983726,0.2372718,0.4276044,0.012322665,0.00040707164,0.015168618],"study_design_scores_gemma":[0.000031268683,0.00013928351,0.42090136,0.000012031835,0.000028782391,0.00041474812,0.00035330444,0.55342126,0.019263886,0.004579887,0.0008121458,0.000041989668],"about_ca_topic_score_codex":0.0026052091,"about_ca_topic_score_gemma":0.0017460572,"teacher_disagreement_score":0.0026052091,"about_ca_system_score_codex":0.00035156694,"about_ca_system_score_gemma":0.00016080904,"threshold_uncertainty_score":0.005180061},"labels":[],"label_agreement":null},{"id":"W2060238459","doi":"10.1016/j.margeo.2004.05.034","title":"Varying tectonic control on basin development at an active microplate margin: Latakia Basin, Eastern Mediterranean","year":2005,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Paleontology; Transtension; Structural basin; Late Miocene; Anticline; Tectonics; Pull apart basin; Fold (higher-order function); Lineament; Thrust fault; Trough (economics); Middle Miocene disruption; Fold and thrust belt; Foreland basin; Seismology; Sedimentary basin; Rift","score_opus":0.01823395638991668,"score_gpt":0.21796001617117577,"score_spread":0.1997260597812591,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060238459","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994179,0.00003389873,0.000015225767,0.000012538895,7.5589725e-7,0.0000010971966,0.000029422785,7.98938e-7,0.00048833847],"genre_scores_gemma":[0.9998109,0.0000231406,0.000018251054,0.0000031942996,0.0000017472629,8.527051e-7,0.00003553018,7.73103e-7,0.00010564618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998678,0.00002297628,0.000013173297,0.00003494685,0.000016976583,0.00004412887],"domain_scores_gemma":[0.99969304,0.00005361155,0.00010705743,0.000015329382,0.0000658035,0.000065293956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000280726,0.00016970419,0.00025303572,0.0008612773,0.00037729103,0.00076282764,0.00026410283,0.0002248846,0.0012095441],"category_scores_gemma":[0.00070950744,0.00015960285,0.00018541765,0.00087486015,0.0007052022,0.0003337223,0.00057319633,0.00013557299,0.00012442286],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005508448,0.000054278367,0.9709908,0.000044753375,0.0001174967,0.0006242188,0.0019636026,0.001039426,0.014516872,0.0006943269,0.00011788089,0.009285571],"study_design_scores_gemma":[0.000005473595,0.00001557705,0.9991173,0.000002087001,0.000011546268,0.000022220023,0.00035512118,0.00017426623,0.00012565579,0.00002875035,0.00014033675,0.0000015639949],"about_ca_topic_score_codex":0.02280632,"about_ca_topic_score_gemma":0.048113253,"teacher_disagreement_score":0.02280632,"about_ca_system_score_codex":0.0010123271,"about_ca_system_score_gemma":0.000506592,"threshold_uncertainty_score":0.045347154},"labels":[],"label_agreement":null},{"id":"W2060282317","doi":"10.1785/gssrl.80.2.214","title":"Anatomy of a Small Earthquake Swarm in Southern Ontario, Canada","year":2009,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; Western University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Citation; Library science; Download; Icon; History; Archaeology; Geography; World Wide Web; Computer science","score_opus":0.05029225959353674,"score_gpt":0.27984913456681565,"score_spread":0.22955687497327892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060282317","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7752191,0.002846548,0.0013362678,0.0026218004,0.000109901564,0.00017145039,0.0042486656,0.00021611564,0.21323012],"genre_scores_gemma":[0.96290547,0.0010387057,0.0010066262,0.00007427724,0.000016779382,0.000019407335,0.0011272983,0.00003549635,0.033776056],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998621,0.000004303604,0.0000038571256,0.000019324034,0.000050266142,0.00006014922],"domain_scores_gemma":[0.9996846,0.0000123797445,0.000048366015,0.000010461581,0.00012878283,0.00011533884],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006803892,0.00021605611,0.00016798254,0.0019256932,0.0043092794,0.0013088506,0.0004807553,0.000397336,0.009355859],"category_scores_gemma":[0.0006047875,0.00018935092,0.000112253256,0.003871226,0.0015831634,0.00030566377,0.0010685037,0.00029936194,0.0009908392],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006038981,0.00006226114,0.51410806,0.0005339205,0.00009190575,0.010477742,0.059806272,0.0040041134,0.01998228,0.034814794,0.101775646,0.25373906],"study_design_scores_gemma":[0.000014074307,0.00003546304,0.86028755,0.00012295377,0.000026130283,0.0009781714,0.015985977,0.0007155984,0.00039022908,0.0013069566,0.12010728,0.000029657986],"about_ca_topic_score_codex":0.973559,"about_ca_topic_score_gemma":0.9937097,"teacher_disagreement_score":0.026440978,"about_ca_system_score_codex":0.015444414,"about_ca_system_score_gemma":0.018290794,"threshold_uncertainty_score":0.11205757},"labels":[],"label_agreement":null},{"id":"W2060355763","doi":"10.1029/2002jb002182","title":"Glacial isostatic stress shadowing by the Antarctic ice sheet","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Deglaciation; Lithosphere; Ice sheet; Post-glacial rebound; Glacial period; Crust; Seismology; Geophysics; Holocene; Geomorphology; Paleontology; Tectonics","score_opus":0.03170683466082575,"score_gpt":0.2965009678673103,"score_spread":0.26479413320648454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060355763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968041,0.00018822672,0.00032302793,0.00003785758,0.0000031634918,0.0000014576443,0.00009482677,0.000017976014,0.0025294328],"genre_scores_gemma":[0.99942183,0.0001453806,0.0001236647,0.000008199576,0.000003241565,0.0000012403495,0.00006564545,0.000002798724,0.0002280169],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999583,0.000010942761,0.000002796317,0.0000052716928,0.000012694178,0.000010115827],"domain_scores_gemma":[0.9998568,0.000025508612,0.000058268197,0.000024925548,0.000019735153,0.000014649872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009329189,0.00019551803,0.00007255766,0.00043283196,0.00018250925,0.00040087162,0.00008538191,0.00011183477,0.00090321735],"category_scores_gemma":[0.00051753037,0.00011616676,0.00013437914,0.00046331366,0.00034676451,0.0001732419,0.00025170462,0.00008126211,0.00019473756],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038470427,0.00003167288,0.78733623,0.00009141223,0.00009835612,0.00096308463,0.0008310777,0.040992744,0.052082922,0.0046556275,0.0014345822,0.11109746],"study_design_scores_gemma":[0.0000110865985,0.00008176058,0.97668356,0.000013175784,0.0000223698,0.00048655688,0.00034617845,0.013003005,0.003844722,0.003263112,0.0022333362,0.000011220043],"about_ca_topic_score_codex":0.0040720035,"about_ca_topic_score_gemma":0.0071159927,"teacher_disagreement_score":0.0040720035,"about_ca_system_score_codex":0.00042693902,"about_ca_system_score_gemma":0.00021564984,"threshold_uncertainty_score":0.008096635},"labels":[],"label_agreement":null},{"id":"W2060897616","doi":"10.1002/grl.50438","title":"Stress tensor changes related to fluid injection at The Geysers geothermal field, California","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Helmholtz-Alberta Initiative","keywords":"Geothermal gradient; Geology; Cauchy stress tensor; Induced seismicity; Stress field; Principal stress; Seismology; Stress (linguistics); Focal mechanism; Orientation (vector space); Geophysics; Petrology; Viscous stress tensor; Geometry; Shear (geology); Mathematics; Physics; Finite element method","score_opus":0.0250694559058496,"score_gpt":0.2676124322029801,"score_spread":0.24254297629713048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060897616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926835,0.00001597835,0.00009606184,0.000010531506,0.0000012659441,0.000002478759,0.0002864168,0.000014879505,0.00030395135],"genre_scores_gemma":[0.9994286,0.000016126756,0.00013423587,0.0000024002195,0.0000017352055,0.0000025288684,0.00028192523,0.0000015910147,0.00013075965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999925,0.000004841866,0.000004362555,0.000026049469,0.00002360929,0.000016017177],"domain_scores_gemma":[0.99968445,0.00004343182,0.00010739898,0.000020977934,0.0001013378,0.000042489373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001696492,0.0002028962,0.00016147496,0.0006575803,0.0002935491,0.00031820455,0.00019512321,0.00016876246,0.00047726274],"category_scores_gemma":[0.0005035316,0.00013196269,0.000096596894,0.0005696396,0.00026856785,0.0001860976,0.0002449653,0.00019455882,0.00005188849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005057624,0.00012627551,0.9252852,0.000057787012,0.00011765962,0.00037294786,0.00066657446,0.018110339,0.037318606,0.00014905137,0.0010329637,0.016256807],"study_design_scores_gemma":[0.0000061973888,0.000024291125,0.9953381,0.0000033191282,0.000007494008,0.000017467732,0.00011212678,0.003048916,0.0012776249,0.000013813818,0.00014492084,0.000005723072],"about_ca_topic_score_codex":0.082410194,"about_ca_topic_score_gemma":0.13799083,"teacher_disagreement_score":0.082410194,"about_ca_system_score_codex":0.00056443905,"about_ca_system_score_gemma":0.00038295396,"threshold_uncertainty_score":0.16386104},"labels":[],"label_agreement":null},{"id":"W2060964265","doi":"10.1038/nature02372","title":"Seismic reflection imaging of two megathrust shear zones in the northern Cascadia subduction zone","year":2004,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; University of British Columbia","funders":"University of California, Davis; University of California, Santa Barbara","keywords":"Geology; Subduction; Episodic tremor and slip; Seismology; Convergent boundary; Plate tectonics; Shear zone; Pacific Plate; Slip (aerodynamics); Slab; Interplate earthquake; Shear (geology); Oceanic crust; Geophysics; Tectonics; Petrology","score_opus":0.010211489140181518,"score_gpt":0.24457937840547572,"score_spread":0.2343678892652942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060964265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981445,0.000030603875,0.00030620003,0.000045799286,0.0000026713662,0.0000051113097,0.00019927819,0.00004936251,0.0012165558],"genre_scores_gemma":[0.9984029,0.000034862816,0.00061106146,0.00001288932,0.0000037095122,0.000005418309,0.00024859092,0.000012041467,0.00066849944],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99992335,0.000004469219,0.0000035114178,0.000022557491,0.000018905437,0.000027177684],"domain_scores_gemma":[0.9998293,0.000022858992,0.000036687907,0.000017490798,0.00005016312,0.000043395547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013860031,0.00027322263,0.00023537809,0.0009008281,0.00035099863,0.0004300036,0.00039274988,0.00055126485,0.0016145733],"category_scores_gemma":[0.00034834197,0.00030461908,0.00017548018,0.00059205893,0.0002362045,0.00022495087,0.00039674251,0.000335182,0.00030917375],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018979587,0.00025555017,0.15863451,0.00013233715,0.00007930706,0.0016020786,0.0024850033,0.0042723767,0.80236256,0.00040661963,0.0010957997,0.02677601],"study_design_scores_gemma":[0.000046689205,0.000090025926,0.9867399,0.000007480524,0.000033693435,0.00031130188,0.00049927883,0.003298627,0.008316023,0.000051125855,0.0005917458,0.000014055119],"about_ca_topic_score_codex":0.01667026,"about_ca_topic_score_gemma":0.029139344,"teacher_disagreement_score":0.01667026,"about_ca_system_score_codex":0.0003012889,"about_ca_system_score_gemma":0.00039578057,"threshold_uncertainty_score":0.03314644},"labels":[],"label_agreement":null},{"id":"W2061045359","doi":"10.1029/2007jb005031","title":"Helium isotopes as geochemical indicators of a serpentinized fore‐arc mantle wedge","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC","funders":"","keywords":"Mantle wedge; Geology; Mantle (geology); Hotspot (geology); Helium; Geochemistry; Subduction; Geophysics; Seismology; Chemistry; Tectonics","score_opus":0.024643752932879372,"score_gpt":0.30873754454794283,"score_spread":0.2840937916150635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061045359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999619,0.00006768424,0.000072354196,0.0000029472842,5.052355e-7,0.0000012454334,0.000060349237,0.0000036386605,0.00017218708],"genre_scores_gemma":[0.99928147,0.00008848203,0.00028944848,0.000005655189,0.0000011515452,0.0000026311563,0.00018235816,0.0000026570478,0.00014609034],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994814,0.000005870455,0.0000065175886,0.000018119628,0.000010440356,0.000010867439],"domain_scores_gemma":[0.9998554,0.0000208421,0.000051155388,0.00001333921,0.000032684606,0.000026641035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010303343,0.00025796657,0.00019402658,0.0011823294,0.00021740238,0.00031564748,0.00021758425,0.00020584522,0.00041756727],"category_scores_gemma":[0.0002005826,0.0002480699,0.00013330493,0.00060058275,0.00027941226,0.00025137054,0.00032220728,0.00019831973,0.00011263927],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032577376,0.000025120162,0.7479782,0.000044601067,0.000065222885,0.0005590254,0.00061293994,0.0003650856,0.24360697,0.000041547402,0.00002391311,0.0063515957],"study_design_scores_gemma":[0.0000042206634,0.000031588665,0.9929892,0.0000036001202,0.000013877695,0.00021534952,0.00021222608,0.00041871736,0.005892817,0.000025455363,0.00018834347,0.000004581076],"about_ca_topic_score_codex":0.006894122,"about_ca_topic_score_gemma":0.012810374,"teacher_disagreement_score":0.006894122,"about_ca_system_score_codex":0.00018316493,"about_ca_system_score_gemma":0.00012022645,"threshold_uncertainty_score":0.013707995},"labels":[],"label_agreement":null},{"id":"W2061295101","doi":"10.4138/4215","title":"Evidence for historic coastal high-energy wave impact (tsunami?) in North Wales, United Kingdom","year":2007,"lang":"en","type":"article","venue":"Atlantic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Bath Spa University","keywords":"Geology; Storm; Peninsula; Oceanography; Humanities; Archaeology; Geography","score_opus":0.060578204759465945,"score_gpt":0.2643733718245906,"score_spread":0.20379516706512463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061295101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99162346,0.00077535835,0.00015365535,0.0003577541,0.000027567756,0.000009945645,0.0005498985,0.0000045257184,0.0064978125],"genre_scores_gemma":[0.99686265,0.00042298686,0.00009849931,0.00013007465,0.000006230646,0.000010350946,0.0002406884,0.0000026334676,0.002226026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99963796,0.000080584556,0.00004952711,0.0000620765,0.000078265395,0.00009153354],"domain_scores_gemma":[0.9981445,0.00033729887,0.0005534107,0.0001092271,0.0006533707,0.00020222536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038759044,0.0001047991,0.00013610277,0.0010369212,0.0006256206,0.00076389115,0.0003392216,0.0003821857,0.004410746],"category_scores_gemma":[0.0019106868,0.00024205136,0.00014364383,0.0010856562,0.00062510656,0.00037695686,0.0010264007,0.00026785565,0.00042588255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112392256,0.00001657476,0.9751066,0.00017423082,0.000031346317,0.0026717011,0.004640744,0.00013562667,0.0020905826,0.00036430548,0.0015903063,0.013065613],"study_design_scores_gemma":[0.0000019690451,0.000017196944,0.99513924,0.00003918247,0.000004923921,0.00029633217,0.0023159983,0.000043482283,0.0001050442,0.0000149011075,0.0020172545,0.000004310202],"about_ca_topic_score_codex":0.38490435,"about_ca_topic_score_gemma":0.6420815,"teacher_disagreement_score":0.38490435,"about_ca_system_score_codex":0.0018716806,"about_ca_system_score_gemma":0.0010472693,"threshold_uncertainty_score":0.76532793},"labels":[],"label_agreement":null},{"id":"W2061394982","doi":"10.1029/2006gl028430","title":"Migration characteristics of seismic tremors in the northern Cascadia margin","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Induced seismicity; Episodic tremor and slip; North American Plate; Plate tectonics; Slip (aerodynamics); Tectonics","score_opus":0.03176464825797792,"score_gpt":0.27900687758759707,"score_spread":0.24724222932961915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061394982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994259,0.000018411489,0.000028847873,0.0000075198072,5.785269e-7,0.0000017333153,0.00016592827,0.000008043268,0.00034298148],"genre_scores_gemma":[0.99936813,0.000019802183,0.000041103056,0.000002084008,0.0000015437809,0.0000028717977,0.00037396434,0.0000017436234,0.00018886194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998815,0.0000095954965,0.000012147463,0.00004080959,0.000029521898,0.00002636587],"domain_scores_gemma":[0.9995272,0.00005443027,0.00013959673,0.00003985965,0.000092284965,0.00014646979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013531018,0.00022203856,0.00019668048,0.001370764,0.0003607073,0.00033108634,0.00019439452,0.00018711161,0.00086297776],"category_scores_gemma":[0.0007781342,0.00016292877,0.00013861855,0.0011337899,0.00028871544,0.00013972877,0.00043749975,0.00011181195,0.00016267388],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016331673,0.0000252293,0.9809491,0.000021305623,0.000043711716,0.00043752862,0.0013638227,0.0009848507,0.008054389,0.000041146854,0.0002467618,0.007668731],"study_design_scores_gemma":[0.0000013024475,0.000010056201,0.99952745,0.0000012669923,0.000003426348,0.000042981792,0.00014641297,0.00011989158,0.000048565933,0.0000038199005,0.00009337058,0.0000014727646],"about_ca_topic_score_codex":0.058090813,"about_ca_topic_score_gemma":0.12245048,"teacher_disagreement_score":0.058090813,"about_ca_system_score_codex":0.0007148726,"about_ca_system_score_gemma":0.0002939283,"threshold_uncertainty_score":0.11550534},"labels":[],"label_agreement":null},{"id":"W2061645887","doi":"10.1007/s004450000075","title":"A model of diffuse degassing at three subduction-related volcanoes","year":2000,"lang":"en","type":"article","venue":"Bulletin of Volcanology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; McGill University; Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Fumarole; Geology; Volcano; Impact crater; Stratovolcano; Geochemistry; Subduction; Hydrothermal circulation; Soil gas; Magma; Crust; Petrology; Seismology; Lava; Tectonics; Astrobiology; Soil water","score_opus":0.020582611622962772,"score_gpt":0.20121176160648044,"score_spread":0.18062914998351767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061645887","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8786106,0.00043330915,0.06720434,0.004268335,0.00020855347,0.00011360373,0.0027840247,0.0008106193,0.04556661],"genre_scores_gemma":[0.9850129,0.00018827528,0.0024458559,0.00011288897,0.0000380087,0.00006188662,0.00041817772,0.00009749286,0.011624541],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998348,0.000037184283,0.0000089954565,0.000052742576,0.000016680653,0.000049680875],"domain_scores_gemma":[0.99937445,0.00021337048,0.00007211194,0.00004275288,0.000086165164,0.00021129189],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004251901,0.0008492177,0.001183429,0.00081908866,0.0011917021,0.002064583,0.0035719632,0.004662708,0.010808437],"category_scores_gemma":[0.0015927447,0.0010288885,0.0013118845,0.0009098415,0.0019611286,0.0020431527,0.0012438637,0.0017619863,0.0010535723],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006614612,0.000032892152,0.0011691152,0.000013148915,0.000017720682,0.000092889946,0.00004376731,0.98656297,0.0004705169,0.010532197,0.00035401032,0.0006446334],"study_design_scores_gemma":[0.00005376203,0.000018110362,0.0005402683,0.0000030599701,0.000016033266,0.000018989345,0.000030618576,0.99515295,0.00007139634,0.0038507173,0.0002323673,0.000011719833],"about_ca_topic_score_codex":0.06458606,"about_ca_topic_score_gemma":0.024096955,"teacher_disagreement_score":0.06458606,"about_ca_system_score_codex":0.0022211655,"about_ca_system_score_gemma":0.0017319601,"threshold_uncertainty_score":0.12842023},"labels":[],"label_agreement":null},{"id":"W2062217726","doi":"10.1186/bf03353174","title":"Co-seismic and post-seismic pore-fluid pressure changes in the Philippine Sea plate and Nankai decollement in response to a seismogenic strain event off Kii Peninsula, Japan","year":2009,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Japan Agency for Marine-Earth Science and Technology; National Science Foundation","keywords":"Geology; Seismology; Accretionary wedge; Aftershock; Seismic moment; Subduction; Décollement; Earthquake swarm; Borehole; Slip (aerodynamics); Induced seismicity; Fault (geology); Tectonics; Geotechnical engineering","score_opus":0.010028658285323839,"score_gpt":0.22698875716139777,"score_spread":0.21696009887607393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062217726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99976045,0.000017758917,0.00001855706,0.000012106614,0.0000012934836,0.0000014594071,0.000080133745,0.0000031500686,0.00010511635],"genre_scores_gemma":[0.99964964,0.000019204548,0.000032921205,0.000004542817,0.0000029943797,0.0000028713496,0.0002006876,0.0000012099254,0.000085926185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999232,0.0000087758945,0.000007818435,0.00001878212,0.00002106083,0.000020274083],"domain_scores_gemma":[0.9994443,0.000043717646,0.00020447795,0.000030468418,0.00012675529,0.0001502911],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002035492,0.00034791237,0.00025777554,0.0008998313,0.00031345442,0.00040521767,0.0003343621,0.00030149665,0.00085797714],"category_scores_gemma":[0.00059119205,0.00018947572,0.00025417772,0.00085087575,0.00034909896,0.00029785253,0.0004737969,0.00026327797,0.00014727187],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013066009,0.000039250437,0.98831,0.000018607532,0.000055215958,0.00047605918,0.0005633387,0.00033853148,0.0073702214,0.000016111297,0.00011059828,0.0025713465],"study_design_scores_gemma":[9.733088e-7,0.000017109127,0.9994273,6.7526986e-7,0.00000439597,0.000026534006,0.0002043661,0.00018952758,0.00009323799,0.000002670311,0.000031500927,0.0000018086208],"about_ca_topic_score_codex":0.040044773,"about_ca_topic_score_gemma":0.06400385,"teacher_disagreement_score":0.040044773,"about_ca_system_score_codex":0.00051194796,"about_ca_system_score_gemma":0.00027241942,"threshold_uncertainty_score":0.0796234},"labels":[],"label_agreement":null},{"id":"W2062283819","doi":"10.1029/2002gl015441","title":"Unbending combined with dehydration embrittlement as a cause for double and triple seismic zones","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Embrittlement; Slab; Induced seismicity; Geology; Fluid pressure; Mantle (geology); Seismology; Crust; Dehydration; Materials science; Geophysics; Composite material; Chemistry; Mechanics","score_opus":0.0643301016988033,"score_gpt":0.29469308589187004,"score_spread":0.23036298419306675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062283819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824614,0.0003268222,0.012067648,0.00030794737,0.000070475704,0.000025558833,0.00006271055,0.00014494157,0.004532443],"genre_scores_gemma":[0.99863094,0.000072899704,0.0006249623,0.000011276308,0.0000072354223,0.0000043713217,0.000016775537,0.000013219876,0.0006182565],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99986076,0.000012213154,0.000009742721,0.000026628933,0.000035192257,0.00005541759],"domain_scores_gemma":[0.9996755,0.00005181254,0.00012083747,0.000037711503,0.000028987411,0.00008520273],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024363042,0.00094679964,0.0004947744,0.00070192886,0.0005557916,0.00080067274,0.00096778787,0.0008070298,0.0021567363],"category_scores_gemma":[0.00063403696,0.0005256798,0.0008976985,0.00031465958,0.00083382684,0.0005770948,0.0017416195,0.0007074249,0.00025435397],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010841021,0.00019820481,0.13431944,0.00035767627,0.00020788037,0.015640222,0.0007997144,0.4656802,0.28528884,0.05899317,0.0016606807,0.03576988],"study_design_scores_gemma":[0.00015063118,0.0003384775,0.07355681,0.000031335352,0.00020743713,0.0044674105,0.0006770053,0.8612701,0.039662458,0.015866332,0.0036661422,0.00010592851],"about_ca_topic_score_codex":0.0050409567,"about_ca_topic_score_gemma":0.0046669166,"teacher_disagreement_score":0.0050409567,"about_ca_system_score_codex":0.00058916473,"about_ca_system_score_gemma":0.00055169826,"threshold_uncertainty_score":0.010023177},"labels":[],"label_agreement":null},{"id":"W2062717515","doi":"10.1130/l286.1","title":"Temporal variations in Holocene slip rate along the central Garlock fault, Pilot Knob Valley, California","year":2014,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"McGill University; Purdue University; National Science Foundation","keywords":"Holocene; Geology; Slip (aerodynamics); Alluvium; Alluvial fan; Quaternary; Fault (geology); Pleistocene; Geodetic datum; Seismology; Paleontology; Geodesy","score_opus":0.014761437935689865,"score_gpt":0.20968991363849296,"score_spread":0.19492847570280308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062717515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991652,0.000050010898,0.000023807192,0.000011356925,0.0000017369201,0.000001526727,0.00030818448,0.0000049041464,0.00043333712],"genre_scores_gemma":[0.99934393,0.000049260754,0.000040218914,0.0000035304238,0.0000022470933,0.0000022866807,0.00033939484,0.0000013751174,0.00021766081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999131,0.000006779063,0.0000064145675,0.000035640824,0.000016624816,0.000021526217],"domain_scores_gemma":[0.9995234,0.00007969973,0.00015485496,0.000029580218,0.00013424296,0.00007808994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017849992,0.00011622294,0.00012088722,0.00088488206,0.00046957366,0.00045062817,0.00021828075,0.00017388054,0.0010768181],"category_scores_gemma":[0.0005914543,0.00014301678,0.000064529835,0.0006191959,0.0002729222,0.00020601154,0.00022150064,0.00014790402,0.000108337925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009501816,0.00002240982,0.99301845,0.00001463423,0.000030264413,0.00005442443,0.0005555229,0.00027948595,0.0012037687,0.000035787714,0.0004027758,0.004287467],"study_design_scores_gemma":[0.0000013412483,0.000005616093,0.9996301,0.0000020278976,0.0000032165917,0.000009662222,0.00010331493,0.000074532276,0.000037861966,0.0000031056775,0.0001281774,9.488371e-7],"about_ca_topic_score_codex":0.12500384,"about_ca_topic_score_gemma":0.35492492,"teacher_disagreement_score":0.12500384,"about_ca_system_score_codex":0.00066962134,"about_ca_system_score_gemma":0.00027980734,"threshold_uncertainty_score":0.2485525},"labels":[],"label_agreement":null},{"id":"W2062738925","doi":"10.5194/npg-17-513-2010","title":"Intraplate seismicity in Canada: a graph theoretic approach to data analysis and interpretation","year":2010,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Induced seismicity; Intraplate earthquake; Geology; Seismology; Cluster analysis; Poisson distribution; Mathematics; Statistics","score_opus":0.011257223906211424,"score_gpt":0.2186840842606892,"score_spread":0.20742686035447777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062738925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7907377,0.0006130697,0.18846437,0.0010279643,0.000014680838,0.00028088485,0.011990892,0.00055241375,0.006318108],"genre_scores_gemma":[0.92771244,0.0002809515,0.06729978,0.00005322898,0.000005362572,0.00008962664,0.0035294425,0.00003288635,0.0009962305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995572,0.0001508939,0.000023043962,0.000094389005,0.00012189639,0.000052624448],"domain_scores_gemma":[0.99677545,0.0016065289,0.00037836173,0.00029025733,0.0008019663,0.00014748659],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010807342,0.0003186022,0.00031427163,0.0043597505,0.0011081136,0.0014490817,0.00091459276,0.00025262375,0.00111927],"category_scores_gemma":[0.0071344078,0.00016423571,0.00042302534,0.0063008107,0.0009583736,0.00047460472,0.00068963226,0.00061544287,0.00007936241],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000273892,0.00010356704,0.39137295,0.00033519775,0.00040390305,0.00053915434,0.0028261833,0.36136368,0.0030466304,0.069255695,0.007099548,0.16337954],"study_design_scores_gemma":[0.000024453804,0.00004441131,0.24659573,0.00005775503,0.00012257737,0.0001286283,0.0028598208,0.6987854,0.0014575962,0.03992816,0.00993581,0.00005964989],"about_ca_topic_score_codex":0.9453478,"about_ca_topic_score_gemma":0.9482907,"teacher_disagreement_score":0.054652214,"about_ca_system_score_codex":0.012258977,"about_ca_system_score_gemma":0.011631366,"threshold_uncertainty_score":0.1099481},"labels":[],"label_agreement":null},{"id":"W2062862625","doi":"10.1029/2009jb007139","title":"Tectonic block motion and glacial isostatic adjustment in southeast Alaska and adjacent Canada constrained by GPS measurements","year":2010,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":197,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Sinistral and dextral; Clockwise; Seismology; Bay; Tectonics; Slip (aerodynamics); Geodesy; Induced seismicity; Fault (geology); Strike-slip tectonics; Glacier; Block (permutation group theory); Plate tectonics; Rotation (mathematics); Geomorphology; Geometry; Oceanography","score_opus":0.025211181955328107,"score_gpt":0.2626094039358173,"score_spread":0.23739822198048915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062862625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998013,0.000069269176,0.00013445993,0.000018364626,0.0000012776567,0.0000028497707,0.0007186254,0.00001555476,0.0010266397],"genre_scores_gemma":[0.9985575,0.00009572318,0.00026238099,0.0000048701613,6.2705294e-7,0.0000025021507,0.0006863305,0.0000036722522,0.00038641525],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989796,0.000008174898,0.000006725302,0.00003308681,0.000025774645,0.000028368662],"domain_scores_gemma":[0.9997373,0.000039923656,0.000048336842,0.000015196205,0.00010154817,0.00005758807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014888433,0.00023063972,0.00020877756,0.000796832,0.0010318073,0.0007447954,0.00031236824,0.00023035976,0.0010680498],"category_scores_gemma":[0.0007396487,0.00021558817,0.0002429202,0.0010524492,0.0003402718,0.00021907223,0.00029413376,0.0001800486,0.0001374723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007729917,0.000020763562,0.96137935,0.000016454254,0.000065078704,0.00013589373,0.00037176104,0.02863314,0.0017799354,0.00042080952,0.00044127007,0.0066582854],"study_design_scores_gemma":[0.000012171028,0.000017463246,0.94346577,0.000026531894,0.000058131547,0.000050206952,0.0009170608,0.053394835,0.00030851932,0.00025028037,0.0014748429,0.000024178631],"about_ca_topic_score_codex":0.9768918,"about_ca_topic_score_gemma":0.9845926,"teacher_disagreement_score":0.023108184,"about_ca_system_score_codex":0.0071681757,"about_ca_system_score_gemma":0.0053278776,"threshold_uncertainty_score":0.052008986},"labels":[],"label_agreement":null},{"id":"W2062949763","doi":"10.1029/1999jb900403","title":"Transpression between two warm mafic plates: The Queen Charlotte Fault revisited","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Minnow Environmental (Canada); Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Transpression; Seismology; Plate tectonics; Transform fault; Pacific Plate; Subduction; Strike-slip tectonics; Transtension; Convergent boundary; Fault (geology); Oceanic crust; Mafic; North American Plate; Basement; Crust; Geophysics; Petrology; Sinistral and dextral; Tectonics","score_opus":0.03945215787230336,"score_gpt":0.31585421434594413,"score_spread":0.27640205647364074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062949763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9728597,0.003768308,0.0008855338,0.0014572158,0.00006113377,0.00000894432,0.00005066921,0.00001747496,0.020890959],"genre_scores_gemma":[0.9975043,0.00072959793,0.00014703459,0.00008083028,0.000022126194,9.878355e-7,0.000026066056,0.0000017741016,0.0014872728],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998338,0.000015698068,0.000009483271,0.000029979938,0.00003710872,0.00007389782],"domain_scores_gemma":[0.9996145,0.00006104089,0.00011771439,0.00003421068,0.00011225618,0.00006020169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022934571,0.00020016819,0.00022818532,0.0009554046,0.0008925837,0.0012054398,0.00069771585,0.0007549928,0.001525973],"category_scores_gemma":[0.00093859254,0.00014309658,0.00014339612,0.00092234625,0.0020256399,0.0006206142,0.00077764795,0.00081626506,0.00015543656],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00084086106,0.00006584749,0.6201713,0.00054007623,0.00017902121,0.036910262,0.008463201,0.0064055296,0.019913018,0.067475624,0.003925852,0.23510945],"study_design_scores_gemma":[0.00006580063,0.00025274864,0.9277494,0.000412426,0.00012013984,0.011090275,0.011181309,0.0052184854,0.004434293,0.0073189144,0.032082755,0.000073402414],"about_ca_topic_score_codex":0.16986209,"about_ca_topic_score_gemma":0.25635436,"teacher_disagreement_score":0.8301379,"about_ca_system_score_codex":0.003030822,"about_ca_system_score_gemma":0.0018950106,"threshold_uncertainty_score":0.33774674},"labels":[],"label_agreement":null},{"id":"W2063107284","doi":"10.1038/nature01352","title":"Hydrothermal recharge and discharge across 50 km guided by seamounts on a young ridge flank","year":2003,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":251,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Los Alamos National Laboratory; Division of Materials Research; Materials Research Science and Engineering Center, Harvard University; National Science Foundation","keywords":"Geology; Outcrop; Hydrothermal circulation; Ridge; Seamount; Lithosphere; Basement; Groundwater recharge; Crust; Oceanic crust; Mid-ocean ridge; Drilling; Geochemistry; Geomorphology; Petrology; Geophysics; Paleontology; Aquifer; Tectonics; Groundwater; Subduction","score_opus":0.011684446510026614,"score_gpt":0.252953750577152,"score_spread":0.2412693040671254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063107284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997274,0.0000044951207,0.000018624047,0.0000058796973,5.389062e-7,0.0000011447312,0.00006231101,0.0000040260084,0.00017555032],"genre_scores_gemma":[0.99966824,0.000004605789,0.000049350856,0.0000032168741,9.2505593e-7,0.0000011560519,0.00008014592,0.0000010977948,0.00019109328],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993193,0.000008146558,0.0000059148783,0.000022994984,0.000012619381,0.000018312581],"domain_scores_gemma":[0.99980515,0.00003532129,0.000043772485,0.000019994724,0.00003922266,0.000056559435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097335134,0.00012481668,0.0002314548,0.00042972635,0.00060338667,0.00049438875,0.00034040923,0.00042047302,0.00088510214],"category_scores_gemma":[0.00034284635,0.00017310386,0.00020594771,0.00048242806,0.00038376747,0.00025278158,0.0004215369,0.0002020541,0.000115309136],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007811134,0.00012909678,0.9568395,0.000026208396,0.00010920926,0.0011419764,0.0019340412,0.002309774,0.029164381,0.0001565022,0.0003040655,0.0071041463],"study_design_scores_gemma":[0.000005439042,0.000042471333,0.9981713,0.000002157242,0.00000921273,0.000045449342,0.000370364,0.0008642782,0.00038237395,0.00001634093,0.00008674163,0.0000037352447],"about_ca_topic_score_codex":0.054256663,"about_ca_topic_score_gemma":0.12420178,"teacher_disagreement_score":0.054256663,"about_ca_system_score_codex":0.0006393477,"about_ca_system_score_gemma":0.00048932136,"threshold_uncertainty_score":0.107881725},"labels":[],"label_agreement":null},{"id":"W2064499777","doi":"10.1111/j.1365-246x.2007.03371.x","title":"Fault locking, block rotation and crustal deformation in the Pacific Northwest","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":408,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Subduction; Clockwise; Pacific Plate; Seafloor spreading; Sinistral and dextral; North American Plate; Geodesy; Crust; Basin and Range Province; Shear (geology); Slip (aerodynamics); Shear zone; Fault (geology); Tectonics; Rotation (mathematics); Paleontology; Geometry","score_opus":0.010485757027192838,"score_gpt":0.23223967661324615,"score_spread":0.2217539195860533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064499777","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99862504,0.00013429254,0.00013927268,0.000015896212,7.5989846e-7,0.0000013141042,0.000109608256,0.000005471822,0.0009683006],"genre_scores_gemma":[0.9994518,0.00011338531,0.00010642608,0.0000045046645,0.000001022709,0.0000010398948,0.00013945434,0.0000020726463,0.00018014062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996376,0.000004010044,0.000004166105,0.000009598355,0.000010757913,0.000007780674],"domain_scores_gemma":[0.9997093,0.000040194118,0.0001465314,0.000019311374,0.000044412154,0.000040164654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001198062,0.00009757359,0.00010797788,0.0004894233,0.00016962897,0.00041897816,0.000111195885,0.0000922679,0.0011475441],"category_scores_gemma":[0.0006861495,0.00009167154,0.000083483224,0.00055497244,0.00024786164,0.0003206457,0.00022600214,0.00009141394,0.000094208575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004787841,0.000005999559,0.9870368,0.000011339955,0.000023655872,0.00009607574,0.00016643199,0.0010924364,0.002329854,0.00015083747,0.00007948804,0.008959199],"study_design_scores_gemma":[0.0000017120705,0.000009585531,0.99777395,0.0000076926035,0.000008673022,0.0000652382,0.00014124265,0.0012348576,0.00022865202,0.00013736724,0.00038888564,0.0000021676287],"about_ca_topic_score_codex":0.07683923,"about_ca_topic_score_gemma":0.09567042,"teacher_disagreement_score":0.07683923,"about_ca_system_score_codex":0.0004726417,"about_ca_system_score_gemma":0.0003356521,"threshold_uncertainty_score":0.15278399},"labels":[],"label_agreement":null},{"id":"W2064619784","doi":"10.1111/sed.12002","title":"High‐resolution seismic reflection profiling of neotectonic faults in Lake Timiskaming, Timiskaming Graben, Ontario‐Quebec, Canada","year":2012,"lang":"en","type":"article","venue":"Sedimentology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital; University of Toronto; McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Ontario Innovation Trust","keywords":"Geology; Graben; Horst and graben; Glacial period; Rift; Seismology; Half-graben; Horst; Neotectonics; Paleontology; Geomorphology; Tectonics","score_opus":0.016082008417229426,"score_gpt":0.21965642594524426,"score_spread":0.20357441752801483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064619784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96882296,0.0006036438,0.0006291094,0.000259544,0.0000086512855,0.00010655231,0.0074604754,0.00009872812,0.022010408],"genre_scores_gemma":[0.9858269,0.00025886303,0.0010222732,0.00005667392,0.0000032708747,0.00003385549,0.0025486394,0.000021676196,0.010227702],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979764,0.0000065419626,0.000006616767,0.00003349215,0.000088534915,0.00006712169],"domain_scores_gemma":[0.9995004,0.000016024473,0.000049097453,0.000010784209,0.00035250146,0.000071295966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013804884,0.00029260942,0.00019133878,0.0013176705,0.0015761639,0.00082199543,0.0006302293,0.00026089043,0.0038913426],"category_scores_gemma":[0.00053411216,0.00018609743,0.00012893432,0.0020835449,0.00030877933,0.00020018288,0.00033104498,0.00017265897,0.00055490714],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035848902,0.00008765927,0.86712426,0.00029610086,0.00012774776,0.0008163251,0.0052730995,0.003939848,0.030652748,0.0007294247,0.014329268,0.07626506],"study_design_scores_gemma":[0.000006777402,0.00001111417,0.9912021,0.000024690218,0.000010808147,0.000037297337,0.0011458888,0.0011608832,0.0004294232,0.000015176239,0.00594633,0.000009499385],"about_ca_topic_score_codex":0.9935714,"about_ca_topic_score_gemma":0.99872774,"teacher_disagreement_score":0.013276604,"about_ca_system_score_codex":0.013276604,"about_ca_system_score_gemma":0.009168626,"threshold_uncertainty_score":0.096328974},"labels":[],"label_agreement":null},{"id":"W2065297954","doi":"10.1029/2006jb004827","title":"Western Quebec seismic zone (Canada): Clustered, midcrustal seismicity along a Mesozoic hot spot track","year":2007,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Seismology; Intraplate earthquake; Hypocenter; Focal mechanism; Precambrian; Crust; Tectonics; Geophysics; Paleontology","score_opus":0.029037474000786403,"score_gpt":0.28265386204334253,"score_spread":0.25361638804255615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065297954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90356743,0.0013459012,0.0017087559,0.0007703204,0.000049081795,0.00018403542,0.044265293,0.00028723496,0.04782195],"genre_scores_gemma":[0.97716796,0.00042372098,0.0014568848,0.00009597236,0.000008578889,0.000032736265,0.008668756,0.000024684578,0.012120595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988544,0.000004390383,0.000003234087,0.000025746316,0.000042120853,0.000039145354],"domain_scores_gemma":[0.99964,0.000009814402,0.000047344813,0.000010066306,0.00022621159,0.00006669097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009932714,0.0002767198,0.00011556727,0.0012670489,0.0010975698,0.0006337545,0.0004017833,0.00020710875,0.0062964982],"category_scores_gemma":[0.00033437772,0.000106529995,0.000117042604,0.0027624748,0.00029934652,0.00018705844,0.00029189585,0.00019150195,0.0004296915],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020249265,0.000057249992,0.8555612,0.00014811105,0.00011973644,0.00056424394,0.001145982,0.0032788252,0.008176615,0.0025459707,0.050414205,0.07778548],"study_design_scores_gemma":[0.0000072754515,0.000006811762,0.98502284,0.000018140236,0.000010028764,0.000059868584,0.00040186237,0.0012627651,0.00032627978,0.00005714051,0.012817062,0.000010044136],"about_ca_topic_score_codex":0.99385804,"about_ca_topic_score_gemma":0.99737227,"teacher_disagreement_score":0.0110118985,"about_ca_system_score_codex":0.0110118985,"about_ca_system_score_gemma":0.009120448,"threshold_uncertainty_score":0.079897285},"labels":[],"label_agreement":null},{"id":"W2065347344","doi":"10.1186/bf03352398","title":"BIFROST project: 3-D crustal deformation rates derived from GPS confirm postglacial rebound in Fennoscandia","year":2014,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Post-glacial rebound; Geodesy; Tectonics; Satellite geodesy; Context (archaeology); Geodetic datum; Global Positioning System; Tectonic uplift; Deglaciation; Plate tectonics; Reference frame; Seismology; Glacial period; Geomorphology; Paleontology","score_opus":0.013088245777950598,"score_gpt":0.2147446624500925,"score_spread":0.2016564166721419,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065347344","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962136,0.000102143815,0.00041626234,0.000020102283,0.000004932505,0.000010024132,0.0019905209,0.00006225256,0.0011800642],"genre_scores_gemma":[0.99351585,0.00004219893,0.0015489323,0.000011070152,0.000002820487,0.000008288773,0.0044334615,0.000015480713,0.00042196215],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998049,0.000019830608,0.000012248642,0.000046634723,0.00006182747,0.00005453191],"domain_scores_gemma":[0.99975044,0.000024128978,0.000041824624,0.000042659463,0.00009116347,0.000049753493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054825604,0.00029799424,0.00023295122,0.0010043527,0.0005145535,0.00049392454,0.0004300183,0.00041335294,0.0010567503],"category_scores_gemma":[0.0008354437,0.00012143832,0.0001520887,0.0009720108,0.0003019503,0.00031070175,0.0003057629,0.00022782119,0.00030667812],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003724109,0.00009957544,0.9384504,0.000032219963,0.000049422488,0.000284124,0.00063014694,0.0024488163,0.007558368,0.000115780625,0.0012625911,0.048696227],"study_design_scores_gemma":[0.000007638939,0.000034977762,0.99614465,0.000004630035,0.000007657538,0.00008907055,0.00014689412,0.0020569358,0.000601003,0.00002164854,0.00087914173,0.000005762281],"about_ca_topic_score_codex":0.1891156,"about_ca_topic_score_gemma":0.34806252,"teacher_disagreement_score":0.1891156,"about_ca_system_score_codex":0.00072624075,"about_ca_system_score_gemma":0.0007375241,"threshold_uncertainty_score":0.3760296},"labels":[],"label_agreement":null},{"id":"W2065498449","doi":"10.1029/2008eo290002","title":"Open‐Source Software Framework Integrates Data Analysis","year":2008,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"University of Saskatchewan; University of Wyoming","keywords":"Reflection (computer programming); Computer science; Software; Visualization; Data science; Open source; Software engineering; Open source software; Data mining; Programming language","score_opus":0.06988544540480872,"score_gpt":0.2757435417833055,"score_spread":0.20585809637849678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065498449","genre_codex":"methods","genre_gemma":"software","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"software","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012413589,0.00010765686,0.819494,0.0002964747,0.00015751254,0.0005232989,0.0052600107,0.16717958,0.0057401364],"genre_scores_gemma":[0.026293164,0.00033569307,0.8639758,0.00051642675,0.00014359955,0.002189876,0.04395762,0.05010828,0.01247959],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9953082,0.0006263859,0.0008316344,0.00096401334,0.0018091573,0.00046054847],"domain_scores_gemma":[0.99054796,0.002491592,0.00043104234,0.0031921968,0.0025427898,0.0007944483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008404688,0.0019292257,0.0015287503,0.0045977747,0.0012257706,0.0040418017,0.0065574427,0.0021810224,0.029807847],"category_scores_gemma":[0.02018448,0.0017555895,0.0029637292,0.003452513,0.001155865,0.005598127,0.0077085802,0.0028861647,0.027011212],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008428985,0.00068592187,0.004616342,0.0014146451,0.0005932418,0.0011846581,0.0015171369,0.01634275,0.014165906,0.07232596,0.36018455,0.5261261],"study_design_scores_gemma":[0.00037750945,0.00014013702,0.0029154813,0.0003408135,0.00014019772,0.00092852785,0.00025539802,0.07804219,0.015004282,0.10334853,0.79814035,0.00036667526],"about_ca_topic_score_codex":0.0056630494,"about_ca_topic_score_gemma":0.004314977,"teacher_disagreement_score":0.029807847,"about_ca_system_score_codex":0.0011934526,"about_ca_system_score_gemma":0.0043565,"threshold_uncertainty_score":0.09971714},"labels":[],"label_agreement":null},{"id":"W2065652484","doi":"10.1111/j.1945-5100.2005.tb00140.x","title":"Structural characteristics of the Sudbury impact structure, Canada: Impact-induced versus orogenic deformation-A review","year":2005,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dike; Geology; Impact structure; Impact crater; Breccia; Igneous rock; Metamorphic rock; Petrology; Sedimentary rock; Classification of discontinuities; Geochemistry; Deformation (meteorology)","score_opus":0.016823870537389058,"score_gpt":0.23984335700493895,"score_spread":0.22301948646754988,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065652484","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0008149528,0.9979315,0.00006612582,0.00010264815,0.0000576593,0.0000054279117,0.00017783347,0.0000036731642,0.0008401553],"genre_scores_gemma":[0.0036358645,0.9956377,0.00010514363,0.000059464535,0.000044502405,0.0000030158376,0.00017565442,0.000001860974,0.00033685128],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99973744,0.000014157291,0.000045781082,0.000060873062,0.00011029313,0.00003149598],"domain_scores_gemma":[0.9988134,0.00035467275,0.00017957373,0.000018530289,0.0005652573,0.000068698704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006000872,0.0009854045,0.0014524235,0.0054614292,0.0005367356,0.0016439118,0.0010409708,0.0006734642,0.0025267582],"category_scores_gemma":[0.0012278815,0.000364494,0.0005316576,0.0076235696,0.0008826442,0.0010352919,0.00053555024,0.00062565814,0.0005935195],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013678361,0.000042936863,0.006102373,0.061045047,0.00027849514,0.00026074747,0.00044139515,0.0008889791,0.0019030728,0.001856806,0.016627882,0.9104155],"study_design_scores_gemma":[0.00001460658,0.000150279,0.05067529,0.02920215,0.0011832833,0.001645021,0.0009895074,0.00031789497,0.0014394234,0.0009023609,0.9133845,0.00009568735],"about_ca_topic_score_codex":0.28347263,"about_ca_topic_score_gemma":0.39033914,"teacher_disagreement_score":0.71652734,"about_ca_system_score_codex":0.0040585916,"about_ca_system_score_gemma":0.009649674,"threshold_uncertainty_score":0.56364524},"labels":[],"label_agreement":null},{"id":"W2066073101","doi":"10.1126/science.1084783","title":"Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip","year":2003,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1270,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Episodic tremor and slip; Subduction; Geology; Seismology; Slip (aerodynamics); Tectonics","score_opus":0.018983684008058475,"score_gpt":0.20927122025934244,"score_spread":0.19028753625128397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066073101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905664,0.00014208381,0.000111471505,0.000038025755,0.000001565428,0.000001087499,0.00004876373,0.0000042084116,0.0005961484],"genre_scores_gemma":[0.99970585,0.000073838695,0.000036429265,0.000007061266,0.000006489937,9.3408175e-7,0.000046920097,0.0000010989454,0.00012139348],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998431,0.00002582234,0.0000113824835,0.000030344203,0.000052817715,0.000036506124],"domain_scores_gemma":[0.99864906,0.000351789,0.00050305785,0.00012464542,0.00017532901,0.00019606746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027627352,0.00015078593,0.00015108053,0.0007261902,0.00026249146,0.0003069563,0.00020338275,0.00022870743,0.0007608819],"category_scores_gemma":[0.001802039,0.00009703515,0.00008601632,0.0005344226,0.0008317825,0.00026843295,0.0007012576,0.00017381292,0.00009482243],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044957738,0.000017136937,0.95103467,0.000081095015,0.000059205347,0.0012086106,0.0025275869,0.0006207826,0.023773232,0.00030596356,0.00021868483,0.019703329],"study_design_scores_gemma":[0.0000015397188,0.000022453565,0.9990282,0.00000433912,0.0000064020373,0.0001872056,0.0002079621,0.0001053123,0.00027599075,0.0000600404,0.000098350196,0.0000021739622],"about_ca_topic_score_codex":0.0047167707,"about_ca_topic_score_gemma":0.011804084,"teacher_disagreement_score":0.0047167707,"about_ca_system_score_codex":0.00027867692,"about_ca_system_score_gemma":0.00017099926,"threshold_uncertainty_score":0.009378672},"labels":[],"label_agreement":null},{"id":"W2066120430","doi":"10.1029/2007jb005456","title":"Deformation rates estimated from earthquakes in the northern Cordillera of Canada and eastern Alaska","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Sinistral and dextral; Tectonics; Seismic hazard; Fault (geology); Plate tectonics; Shear (geology); Transpression; Shear zone; Earthquake rupture; Terrane; Deformation (meteorology); Paleontology","score_opus":0.03960871205755765,"score_gpt":0.27329505687735467,"score_spread":0.23368634481979703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066120430","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99038565,0.00022070738,0.00036829142,0.00003394167,0.0000047726608,0.000010698815,0.0038139964,0.000068331996,0.0050936984],"genre_scores_gemma":[0.9950305,0.0002321531,0.0005087408,0.0000047719477,0.0000025466165,0.0000063739926,0.0033225487,0.000008282842,0.0008840687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987507,0.0000064410074,0.000016307573,0.00002807305,0.000050611354,0.000023391529],"domain_scores_gemma":[0.9993685,0.00006311761,0.000106633495,0.00003256278,0.00036899358,0.0000602211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019333184,0.0003298746,0.00011710188,0.0030131969,0.0007131008,0.00057466264,0.00022255424,0.00012315888,0.0010892911],"category_scores_gemma":[0.0014129848,0.0001051261,0.00018730671,0.0021868714,0.00017825347,0.00024417505,0.00028490773,0.00012204394,0.00022132118],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003673742,0.000009212083,0.96414346,0.000027030565,0.000050122617,0.00011837333,0.0002907565,0.014355558,0.0010675599,0.00037524465,0.0007347211,0.018791331],"study_design_scores_gemma":[0.000004195779,0.000007866914,0.9884064,0.000018967537,0.00001881139,0.000053446773,0.00030799644,0.008600823,0.00049929455,0.00012328137,0.0019451294,0.000013774524],"about_ca_topic_score_codex":0.9134753,"about_ca_topic_score_gemma":0.9270151,"teacher_disagreement_score":0.086524725,"about_ca_system_score_codex":0.004430134,"about_ca_system_score_gemma":0.0026793478,"threshold_uncertainty_score":0.17406851},"labels":[],"label_agreement":null},{"id":"W2066143729","doi":"10.1029/2006gl028448","title":"Decontaminating tide gauge records for the influence of glacial isostatic adjustment: The potential impact of 3‐D Earth structure","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Lithosphere; Mantle (geology); Tide gauge; Geology; Sea level; Geodesy; Geophysics; Seismology; Oceanography; Tectonics","score_opus":0.01609485394625142,"score_gpt":0.2877439010671822,"score_spread":0.27164904712093074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066143729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98547125,0.00009963479,0.012373149,0.0004948551,0.000044420012,0.000016866914,0.0003612343,0.00019274357,0.00094576034],"genre_scores_gemma":[0.99666256,0.000038608672,0.002861071,0.00005193141,0.000009084078,0.000009904716,0.00021056447,0.000021716158,0.00013463214],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995622,0.00025576173,0.000023891585,0.00005659176,0.00005130947,0.000050157512],"domain_scores_gemma":[0.9971886,0.0016600451,0.00044357392,0.0003347411,0.00022117644,0.00015183572],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014739331,0.00078196794,0.0007271903,0.00040757642,0.0005167639,0.0011246545,0.0010536998,0.0009667538,0.00069382257],"category_scores_gemma":[0.008070407,0.00044542452,0.0010389056,0.00056642905,0.0004808348,0.0008514203,0.000580566,0.0007371651,0.00017719771],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003238634,0.000081968865,0.08915837,0.000032838627,0.00022178225,0.0001702227,0.00010646192,0.8959892,0.0035348672,0.0010157045,0.00029029985,0.0090744505],"study_design_scores_gemma":[0.000071504815,0.000076764256,0.03337736,0.000013786522,0.00006413484,0.00004388737,0.00004466556,0.9634367,0.0017455675,0.00061816466,0.00046584572,0.000041520747],"about_ca_topic_score_codex":0.049684867,"about_ca_topic_score_gemma":0.030576048,"teacher_disagreement_score":0.049684867,"about_ca_system_score_codex":0.0009570093,"about_ca_system_score_gemma":0.0012331101,"threshold_uncertainty_score":0.09879136},"labels":[],"label_agreement":null},{"id":"W2066257011","doi":"10.1029/2000jb900220","title":"Permeability of a decollement zone: Results from a two‐well experiment in the Barbados accretionary complex","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Décollement; Borehole; Hydrogeology; Accretionary wedge; Permeability (electromagnetism); Petrology; Fault (geology); Drilling; Geotechnical engineering; Seismology; Subduction; Tectonics","score_opus":0.05663239576179203,"score_gpt":0.33251879108726795,"score_spread":0.27588639532547593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066257011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993055,0.000016517519,0.00042082256,0.00001255457,0.0000015764231,0.000009391485,0.00006783184,0.000013099059,0.00015271336],"genre_scores_gemma":[0.9985563,0.00004084332,0.00086559285,0.000012594739,0.0000021998244,0.000017641269,0.00009674785,0.0000067594656,0.000401376],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99964225,0.00003008333,0.00002229214,0.00011787111,0.000104964995,0.00008254897],"domain_scores_gemma":[0.9992816,0.00018356615,0.00016708516,0.000060730057,0.00015309891,0.0001538998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003673909,0.0003760194,0.0006292022,0.00034047462,0.0010310045,0.00051203894,0.0006765794,0.00078448834,0.0007316575],"category_scores_gemma":[0.00079328334,0.0003508369,0.00028452525,0.0002857731,0.0007675191,0.00070748595,0.0007999152,0.0008145525,0.00012581829],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013479583,0.0008074729,0.011425109,0.00006342278,0.000020312495,0.00035632457,0.00074030255,0.0020886331,0.98012084,0.00019361875,0.00007447638,0.002761573],"study_design_scores_gemma":[0.00034186043,0.0073913895,0.30863938,0.00002477352,0.00011473047,0.00036866896,0.0011147013,0.041703284,0.63875043,0.000306473,0.0011350212,0.00010925734],"about_ca_topic_score_codex":0.04065419,"about_ca_topic_score_gemma":0.058361154,"teacher_disagreement_score":0.04065419,"about_ca_system_score_codex":0.0011367763,"about_ca_system_score_gemma":0.0005544149,"threshold_uncertainty_score":0.080835104},"labels":[],"label_agreement":null},{"id":"W2066275084","doi":"10.1193/1.2201668","title":"Housing Reconstruction in Northern Sumatra after the December 2004 Great Sumatra Earthquake and Tsunami","year":2006,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Institute on Aging","keywords":"Government (linguistics); Geography; Quality (philosophy); Geology; Seismology","score_opus":0.008036768595407801,"score_gpt":0.1915167402071466,"score_spread":0.1834799716117388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066275084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976654,0.00006863054,0.000082523875,0.00013587267,0.0000057037782,0.000009168401,0.000039635586,0.0000023803882,0.0019906128],"genre_scores_gemma":[0.9974414,0.00011817738,0.0002311421,0.000025396706,0.0000017901452,0.000008520016,0.00010594937,0.0000025177244,0.0020651885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998259,0.00006355964,0.000009952151,0.000019714002,0.000032055123,0.000048899714],"domain_scores_gemma":[0.99977106,0.000024167613,0.00009695731,0.000018471868,0.0000411759,0.000048201156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003546466,0.00019829876,0.0001498294,0.00043187413,0.0014655405,0.000789568,0.0003894466,0.00026857245,0.0017942932],"category_scores_gemma":[0.00081394153,0.00016241227,0.00010255458,0.0009245895,0.00061211776,0.00042874803,0.0010651377,0.0004168623,0.00022045014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00096561504,0.00062608125,0.61411965,0.00035822115,0.00010915556,0.03614816,0.14260948,0.0073539224,0.02283111,0.0028388435,0.004733191,0.16730659],"study_design_scores_gemma":[0.000015428948,0.00014757107,0.8893589,0.000060071914,0.000018663068,0.0013710903,0.09123206,0.0014383462,0.002171401,0.00027584736,0.013893011,0.000017544306],"about_ca_topic_score_codex":0.03832393,"about_ca_topic_score_gemma":0.15888849,"teacher_disagreement_score":0.03832393,"about_ca_system_score_codex":0.002076797,"about_ca_system_score_gemma":0.0009846545,"threshold_uncertainty_score":0.07620174},"labels":[],"label_agreement":null},{"id":"W2066304589","doi":"10.1029/2002jb002247","title":"Structure, seismicity, and thermal regime of the Queen Charlotte Transform Margin","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Social Sciences and Humanities Research Council of Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Receiver function; Convergent boundary; Crust; Subduction; Plate tectonics; Induced seismicity; Continental margin; Oceanic crust; Accretionary wedge; Trench; Tectonics; Trough (economics); Fault (geology); Geophysics; Lithosphere","score_opus":0.022611727669517443,"score_gpt":0.26584210279241083,"score_spread":0.2432303751228934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066304589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99806136,0.00007389419,0.00005905393,0.000030070605,0.0000010509815,0.000001779652,0.0000882757,0.0000037826874,0.0016807208],"genre_scores_gemma":[0.9989196,0.00003048523,0.00006538466,0.0000089434725,9.126944e-7,0.0000016284524,0.000120276956,0.0000020900252,0.0008506806],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998945,0.000007834421,0.000002818601,0.00002360418,0.000034421493,0.00003678528],"domain_scores_gemma":[0.9996086,0.000036049412,0.000111115645,0.000020780319,0.00013237003,0.00009111126],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000085759726,0.000070361275,0.00010812542,0.00084805646,0.000938083,0.00070550776,0.0002299814,0.00015422699,0.00142125],"category_scores_gemma":[0.0006725903,0.00011042485,0.000072028415,0.00074455526,0.00065874704,0.00017551547,0.0005461945,0.00013525407,0.00023229778],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034355794,0.000023155346,0.9584985,0.000025930087,0.000017435168,0.00047170708,0.0030978143,0.0012903154,0.012698506,0.00078648434,0.00071738963,0.022029268],"study_design_scores_gemma":[0.000005008922,0.000014831169,0.99637944,0.000009000191,0.000002771513,0.0001285614,0.00085300294,0.0005741602,0.0002844425,0.000050622682,0.0016913008,0.000006915602],"about_ca_topic_score_codex":0.767413,"about_ca_topic_score_gemma":0.91131985,"teacher_disagreement_score":0.767413,"about_ca_system_score_codex":0.003634113,"about_ca_system_score_gemma":0.0030937525,"threshold_uncertainty_score":0.46791345},"labels":[],"label_agreement":null},{"id":"W2066815820","doi":"10.1007/s00024-006-0127-x","title":"Construction of an Intraplate Fault System Model of South Australia, and Simulation Tool for the iSERVO Institute Seed Project","year":2006,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Melbourne; Ontario Ministry of Natural Resources and Forestry","keywords":"Intraplate earthquake; Fault (geology); Software; Software deployment; Finite element method; Work (physics); Computer science; Observatory; Systems engineering; Geology; Aerospace engineering; Engineering; Mechanical engineering; Seismology; Structural engineering; Software engineering; Physics","score_opus":0.02311353855728783,"score_gpt":0.2270275178405801,"score_spread":0.20391397928329225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066815820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.70080423,0.0002001808,0.24952668,0.00062337524,0.00008118282,0.00070184714,0.006506585,0.0026935474,0.03886233],"genre_scores_gemma":[0.8985945,0.00015268965,0.08757321,0.00004344183,0.000009024413,0.00041928832,0.0025781572,0.00035057534,0.010279131],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999255,0.000016407173,0.0000047315475,0.00001702627,0.00002536909,0.00001088358],"domain_scores_gemma":[0.999801,0.00003845253,0.00001598594,0.000021374806,0.000097349366,0.000025812535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021595332,0.00041535895,0.00042115417,0.000546131,0.000550439,0.00047671466,0.0011323014,0.0006831468,0.006341772],"category_scores_gemma":[0.00095688493,0.0006221271,0.00041935418,0.00058489124,0.00022101079,0.0006378754,0.0004940543,0.00055915664,0.00064793095],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033666318,0.000047713285,0.0033405316,0.000045682864,0.000014705958,0.0001049804,0.0000967694,0.9824767,0.0015295075,0.0033654459,0.001344222,0.00760006],"study_design_scores_gemma":[0.000016739503,0.000010350045,0.00086815504,0.0000049587984,0.000006006364,0.000008853892,0.000020606582,0.9966371,0.0003799498,0.0006842913,0.0013578436,0.0000051120956],"about_ca_topic_score_codex":0.16715547,"about_ca_topic_score_gemma":0.13037544,"teacher_disagreement_score":0.16715547,"about_ca_system_score_codex":0.0016579918,"about_ca_system_score_gemma":0.0032940768,"threshold_uncertainty_score":0.33236504},"labels":[],"label_agreement":null},{"id":"W2067529326","doi":"10.1111/j.1440-1738.2003.00424.x","title":"Evidence for fluid flow in the Japan Trench forearc using isotope geochemistry (Cl, Sr, B): Results from ODP Site 1150","year":2004,"lang":"en","type":"article","venue":"Island Arc","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Waterloo","funders":"Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Forearc; Geology; Diagenesis; Seawater; Geochemistry; Radiogenic nuclide; Trace element; Mineralogy; Tectonics; Subduction; Oceanography; Mantle (geology); Paleontology","score_opus":0.059984225162605445,"score_gpt":0.26395812535444907,"score_spread":0.20397390019184364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067529326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992237,0.000074469586,0.00007503341,0.000009373807,0.0000015567801,0.0000033898107,0.00013191673,0.000008890807,0.00047168433],"genre_scores_gemma":[0.99847347,0.0000946798,0.00045142203,0.000016683935,0.0000024309209,0.000006489297,0.00028163218,0.0000051671404,0.0006679958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983835,0.0000060637317,0.000012936639,0.000049600385,0.00005276445,0.000040204366],"domain_scores_gemma":[0.99979883,0.000010777393,0.00005196532,0.0000058841392,0.0000873299,0.000045238805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015438531,0.00038268883,0.00026744584,0.0018090326,0.00067529234,0.0006540384,0.00044082012,0.00044714106,0.0008358386],"category_scores_gemma":[0.0002284193,0.00041973733,0.00022453837,0.0008223688,0.0005819974,0.00031540834,0.00057595014,0.00019961793,0.0001932782],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014732088,0.00003529731,0.8672799,0.000057614605,0.00003644636,0.0005016281,0.0012692655,0.00023905197,0.123840824,0.000049570877,0.00008014955,0.0064628976],"study_design_scores_gemma":[0.0000040688456,0.000029514984,0.9959657,0.0000052277555,0.000012112637,0.0000676508,0.00045499456,0.00018536203,0.0029452215,0.000006703321,0.00031911282,0.0000042952506],"about_ca_topic_score_codex":0.10305078,"about_ca_topic_score_gemma":0.19325481,"teacher_disagreement_score":0.10305078,"about_ca_system_score_codex":0.0007823074,"about_ca_system_score_gemma":0.0010280448,"threshold_uncertainty_score":0.20490187},"labels":[],"label_agreement":null},{"id":"W2067700100","doi":"10.3137/ao.440406","title":"The California tsunami of 15 June 2005 along the coast of North America","year":2006,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Hydrographic Service; Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Geology; Seismology; Tide gauge; Tsunami earthquake; Cove; West coast; Tsunami wave; Oceanography; Trough (economics); Geomorphology; Sea level","score_opus":0.006431832507007597,"score_gpt":0.1873486721174407,"score_spread":0.1809168396104331,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067700100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89038026,0.0028324232,0.00041013065,0.0015293437,0.00048485846,0.00010558189,0.013768295,0.00027402106,0.09021511],"genre_scores_gemma":[0.96915364,0.0016020485,0.00072646665,0.00027811035,0.00011522798,0.000046438716,0.008665483,0.000019328541,0.019393388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998599,0.0000053024996,0.00001035222,0.00003580975,0.000064602915,0.00002396475],"domain_scores_gemma":[0.9996184,0.0000122435895,0.00008747967,0.000014595818,0.00019568458,0.00007157746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015914041,0.00024133378,0.00016845234,0.0006404021,0.00094547676,0.00078288803,0.00028383898,0.00021720969,0.004387437],"category_scores_gemma":[0.00032774112,0.000109408174,0.00009861103,0.0007266675,0.00016356885,0.00025736395,0.0003793988,0.0002752484,0.00044442635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034651867,0.00016656634,0.69636995,0.00044767623,0.00018016559,0.0015321102,0.0030249387,0.0018756584,0.00404814,0.0007425277,0.19881433,0.0924515],"study_design_scores_gemma":[0.00001628817,0.00004351547,0.94152135,0.00010127042,0.000029149332,0.00008130659,0.0012669523,0.00039771217,0.00032810803,0.00007222612,0.05612919,0.000013029602],"about_ca_topic_score_codex":0.3819326,"about_ca_topic_score_gemma":0.6903777,"teacher_disagreement_score":0.3819326,"about_ca_system_score_codex":0.0018757078,"about_ca_system_score_gemma":0.0019581972,"threshold_uncertainty_score":0.75941896},"labels":[],"label_agreement":null},{"id":"W2068531147","doi":"10.1029/2000jb000039","title":"Multiparameter two‐dimensional inversion of scattered teleseismic body waves 3. Application to the Cascadia 1993 data set","year":2001,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; China Aerospace Science and Technology Corporation; Oregon State University","keywords":"Geology; Seismology; Lithosphere; Crust; Oceanic crust; Subduction; Seismometer; Eclogite; Mantle (geology); Continental crust; Inversion (geology); Geophysics; Tectonics","score_opus":0.06256595307432701,"score_gpt":0.33121086303899716,"score_spread":0.26864490996467016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068531147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98175734,0.000039265662,0.014122958,0.00014582786,0.000014618592,0.000032906453,0.002095609,0.00077572773,0.0010157016],"genre_scores_gemma":[0.9718499,0.000021838141,0.023408065,0.000015991835,0.000010848795,0.000036298265,0.0039280253,0.0000785609,0.0006503482],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998115,0.000037544232,0.000014227859,0.00006360275,0.000045491124,0.000027699885],"domain_scores_gemma":[0.99952304,0.00013432873,0.00005034974,0.0001242942,0.00012113516,0.000046720965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005847006,0.0006278486,0.00031854148,0.00066506123,0.00046647107,0.0007694114,0.0009704747,0.00048968225,0.0014011967],"category_scores_gemma":[0.0017333812,0.00039498074,0.0006682497,0.00058982125,0.00024120335,0.00038204,0.0006784839,0.0006327481,0.0002693194],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045639442,0.0005509532,0.1627304,0.00008067088,0.0003638593,0.0006213437,0.00059619243,0.6808795,0.03245034,0.0011865288,0.0034479827,0.11663595],"study_design_scores_gemma":[0.00007825009,0.00004603526,0.053078655,0.000004606774,0.000017492155,0.00004784409,0.00020644307,0.9424229,0.0025531293,0.0003345094,0.0011857804,0.000024396155],"about_ca_topic_score_codex":0.06994521,"about_ca_topic_score_gemma":0.09541954,"teacher_disagreement_score":0.06994521,"about_ca_system_score_codex":0.0007607456,"about_ca_system_score_gemma":0.0009896717,"threshold_uncertainty_score":0.13907617},"labels":[],"label_agreement":null},{"id":"W2068766263","doi":"10.1029/2006jb004833","title":"Multiscaling of shear zones and the evolution of the brittle‐to‐viscous transition in continental crust","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mylonite; Shear zone; Geology; Shear (geology); Shearing (physics); Brittleness; Crust; Continental crust; Scaling; Mineralogy; Geophysics; Seismology; Petrology; Geometry; Geotechnical engineering; Materials science; Tectonics; Composite material","score_opus":0.025093623895134826,"score_gpt":0.27139200066071095,"score_spread":0.24629837676557612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068766263","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96476126,0.00049760984,0.033737198,0.000038642534,0.000009417507,0.000010105822,0.00010426482,0.00018597994,0.0006553793],"genre_scores_gemma":[0.98904943,0.000095704556,0.010590877,0.000003449409,0.000008776411,0.000006434476,0.000056341483,0.00003210887,0.00015696524],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998956,0.000020734453,0.000008409895,0.000033487955,0.000029705036,0.000012054963],"domain_scores_gemma":[0.9993327,0.00021532887,0.00025241324,0.00007992304,0.00007339727,0.00004622601],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000462679,0.00024462945,0.00012877274,0.0021989315,0.00016732456,0.0005511054,0.00021939687,0.00013433928,0.00041918573],"category_scores_gemma":[0.001137099,0.0002001342,0.00030221985,0.00073701545,0.00045476068,0.0004126126,0.00036652983,0.00021222947,0.00006289927],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038380135,0.00010989916,0.3087331,0.00029037616,0.00029844334,0.00040286337,0.0013333871,0.08087793,0.29403493,0.010092924,0.00049150956,0.30295083],"study_design_scores_gemma":[0.000020224645,0.00012634389,0.72153556,0.00002728051,0.00004900429,0.00030156513,0.00030769382,0.24444658,0.023733715,0.008006321,0.001373642,0.000072100025],"about_ca_topic_score_codex":0.002613959,"about_ca_topic_score_gemma":0.0025178038,"teacher_disagreement_score":0.002613959,"about_ca_system_score_codex":0.00045590155,"about_ca_system_score_gemma":0.00011558071,"threshold_uncertainty_score":0.0051974654},"labels":[],"label_agreement":null},{"id":"W2069054265","doi":"10.1029/2008jb006038","title":"Correlation of tremor activity with tidal stress in the northern Cascadia subduction zone","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Episodic tremor and slip; Slip (aerodynamics); Shear stress; Amplitude; Thrust; Thrust fault; Tectonics; Geodesy; Physics","score_opus":0.026854947494620692,"score_gpt":0.2816127956773042,"score_spread":0.2547578481826835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069054265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99924785,0.00003437998,0.000058427402,0.000020797002,0.0000014752733,0.0000015314703,0.00028013933,0.000017281554,0.00033813302],"genre_scores_gemma":[0.9993061,0.000024291565,0.000042764426,0.0000030189144,0.0000022516206,0.0000026106802,0.00049465435,0.0000026332143,0.00012176214],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997323,0.00002710419,0.00003773207,0.00008159762,0.000069924,0.000051274073],"domain_scores_gemma":[0.9984633,0.0002079357,0.0005922707,0.00014749405,0.00026408327,0.00032488402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003252054,0.00036387754,0.00030820462,0.0015608356,0.00040400558,0.0005933685,0.00025218722,0.0003500751,0.0010069098],"category_scores_gemma":[0.00203934,0.00023132993,0.00031345952,0.0014297005,0.0004669095,0.00022447864,0.0005746911,0.00021650193,0.00018693792],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054161323,0.000012121026,0.99479336,0.000010701216,0.00004955082,0.00010454475,0.00026767945,0.0014284485,0.0013910416,0.000019259067,0.000114656024,0.0017544513],"study_design_scores_gemma":[0.000001310231,0.00000793587,0.9992642,0.0000015469597,0.0000047473636,0.000016387692,0.00006145083,0.0005106258,0.00004813295,0.0000075279318,0.000073814175,0.0000022150239],"about_ca_topic_score_codex":0.06879208,"about_ca_topic_score_gemma":0.106048256,"teacher_disagreement_score":0.06879208,"about_ca_system_score_codex":0.0010849744,"about_ca_system_score_gemma":0.000478731,"threshold_uncertainty_score":0.1367833},"labels":[],"label_agreement":null},{"id":"W2069146762","doi":"10.1007/978-3-0348-8179-1_7","title":"Reliability of Seismic Moment Tensor Inversions for Induced Microseismicity at Kidd Mine, Ontario","year":2002,"lang":"en","type":"book-chapter","venue":"Birkhäuser Basel eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Apheresis Group","funders":"","keywords":"Geology; Sill; Microseism; Seismology; Moment tensor; Shear (geology); Seismometer; Pillar; Geotechnical engineering; Petrology; Structural engineering; Engineering; Deformation (meteorology)","score_opus":0.042346478769718386,"score_gpt":0.20858183829954574,"score_spread":0.16623535952982735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069146762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9775693,0.00026939472,0.01333857,0.00016843619,0.000010464161,0.000020669348,0.0029288377,0.00039539856,0.00529894],"genre_scores_gemma":[0.9942009,0.00008667455,0.0020689385,0.0000064928463,0.000002543734,0.00000573405,0.0023921982,0.000043241558,0.0011933645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994734,0.000067648245,0.000039712944,0.00011934097,0.00023856667,0.00006137887],"domain_scores_gemma":[0.9975889,0.00079732505,0.0002600789,0.0002764966,0.0010155386,0.00006169961],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006035236,0.0003076838,0.00021443439,0.00043124042,0.00030432042,0.0006755061,0.0006235407,0.00024191065,0.00082721206],"category_scores_gemma":[0.007900965,0.00022574673,0.00019978208,0.0006824788,0.0004235612,0.0005591551,0.00031528354,0.00020879568,0.0005070529],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004948063,0.000027247901,0.751674,0.00017681469,0.0002319345,0.00032230027,0.001620524,0.048224606,0.03076314,0.0017161182,0.0050530005,0.15969555],"study_design_scores_gemma":[0.00003625504,0.00004429032,0.8428249,0.000041687294,0.00006689865,0.00021121185,0.0007226804,0.14057241,0.010139687,0.00090162404,0.0043861596,0.00005226026],"about_ca_topic_score_codex":0.38814607,"about_ca_topic_score_gemma":0.63540405,"teacher_disagreement_score":0.61185396,"about_ca_system_score_codex":0.0016943185,"about_ca_system_score_gemma":0.0017347587,"threshold_uncertainty_score":0.77177364},"labels":[],"label_agreement":null},{"id":"W2069272856","doi":"10.1029/2001jb001460","title":"Undrained poroelastic response of sandstones to deviatoric stress change","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Poromechanics; Pore water pressure; Stress (linguistics); Effective stress; Geology; Dilatant; Geotechnical engineering; Deformation (meteorology); Porosity; Materials science; Porous medium","score_opus":0.07995615097924261,"score_gpt":0.31197024606752444,"score_spread":0.23201409508828183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069272856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997904,0.0000084732665,0.000071829396,0.0000016721153,2.7801107e-7,0.0000018309037,0.000027295466,0.000004540043,0.0000936346],"genre_scores_gemma":[0.99981564,0.0000067676415,0.00006009483,0.000002397785,2.1387801e-7,0.0000016183275,0.000029268056,0.0000013431244,0.000082646475],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986863,0.000012709063,0.000013452744,0.00003694014,0.00003761082,0.000030611805],"domain_scores_gemma":[0.9996712,0.000049186736,0.000069245056,0.000059885922,0.000091017086,0.000059481798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010801032,0.00020723892,0.00021854985,0.0003491725,0.00017219303,0.00032332703,0.00023126906,0.00016314254,0.00050733885],"category_scores_gemma":[0.0005003061,0.00022208388,0.00012632692,0.00022092019,0.0005068873,0.00015906988,0.00039435283,0.00021008932,0.000083731335],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015849361,0.000028144317,0.050782677,0.000022671386,0.000026102569,0.0001393757,0.00021089647,0.0011771647,0.9453641,0.000041903808,0.000013248466,0.0020352136],"study_design_scores_gemma":[0.000009732548,0.0002466382,0.8076355,0.000002394478,0.000014833261,0.00021338588,0.00019435196,0.004009219,0.18736137,0.00006394749,0.00023053425,0.000018041896],"about_ca_topic_score_codex":0.006823942,"about_ca_topic_score_gemma":0.009662849,"teacher_disagreement_score":0.006823942,"about_ca_system_score_codex":0.00035866274,"about_ca_system_score_gemma":0.00018115278,"threshold_uncertainty_score":0.013568461},"labels":[],"label_agreement":null},{"id":"W2070415898","doi":"10.1186/bf03352279","title":"On the determination of a global strain rate model","year":2014,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Natural Resources Canada; National Oceanic and Atmospheric Administration","keywords":"Geodetic datum; Strain rate; Geodesy; Slip (aerodynamics); Seismic moment; Geology; Strain rate tensor; Azimuth; A priori and a posteriori; Seismology; Fault (geology); Geometry; Mathematics; Physics","score_opus":0.014737830362430128,"score_gpt":0.20894189481019948,"score_spread":0.19420406444776936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070415898","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.028480738,0.00019986884,0.9662484,0.00012070987,0.00002133203,0.000016094096,0.00030216647,0.00038147872,0.004229285],"genre_scores_gemma":[0.6944528,0.0011159774,0.29617757,0.00016570733,0.00010287334,0.00015740229,0.0018990786,0.00094252964,0.004986003],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996369,0.00007593834,0.000015553851,0.00014231812,0.00009301853,0.00003610541],"domain_scores_gemma":[0.9993476,0.00027376544,0.000103993814,0.00013546196,0.000108130575,0.00003096903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00089235196,0.0009600807,0.00096429634,0.0010180004,0.00029193118,0.0014784934,0.000878465,0.0006341647,0.001913131],"category_scores_gemma":[0.0030888868,0.00058830227,0.0007407513,0.0008725804,0.0007490669,0.0020396544,0.0011755667,0.0009957008,0.0009089131],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002066589,0.000016546372,0.0058373543,0.00004596771,0.000045045093,0.00007794184,0.00006333702,0.89152145,0.0050366316,0.047144633,0.000785233,0.049405172],"study_design_scores_gemma":[0.000003853308,0.000021847387,0.0028123213,0.000022656544,0.000010068596,0.000052725994,0.000023764109,0.96914357,0.0010141799,0.02458383,0.0022910743,0.000020054526],"about_ca_topic_score_codex":0.0038852512,"about_ca_topic_score_gemma":0.0032420303,"teacher_disagreement_score":0.0038852512,"about_ca_system_score_codex":0.00056333747,"about_ca_system_score_gemma":0.0006973542,"threshold_uncertainty_score":0.007725239},"labels":[],"label_agreement":null},{"id":"W2070519193","doi":"10.1111/j.1365-246x.2005.02840.x","title":"Experimental tests of simple models for the dynamics of diffuse oceanic plate boundaries","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Simple (philosophy); Geology; Plate tectonics; Convergent boundary; Dynamics (music); Geophysics; Inverse theory; Seismology; Oceanic crust; Subduction; Physics; Oceanography; Acoustics; Deformation (meteorology)","score_opus":0.015793037153698404,"score_gpt":0.24635611723004294,"score_spread":0.23056308007634455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070519193","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98934644,0.0001246299,0.00791548,0.00010864092,0.000041211144,0.000111873494,0.00014997424,0.00006610907,0.0021356065],"genre_scores_gemma":[0.9948525,0.00013582867,0.0039945864,0.000032078333,0.000009498656,0.00014428872,0.00017014309,0.000010847671,0.000650314],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99951494,0.00006439182,0.000053017655,0.00013720345,0.00016622625,0.00006426158],"domain_scores_gemma":[0.99812716,0.0007432174,0.00040375825,0.00044008397,0.00017101338,0.00011478865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007477044,0.00055591954,0.00024222751,0.0004143953,0.00037243313,0.0005893992,0.0010460941,0.0008137352,0.0024368474],"category_scores_gemma":[0.0041803857,0.00030647675,0.00033540497,0.00019996979,0.0009652826,0.0011176729,0.0009960737,0.00066088414,0.0003188599],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016235815,0.002189983,0.019280931,0.00054220355,0.00008356441,0.0004290144,0.00072960765,0.10928121,0.84084284,0.007301332,0.000824075,0.016871613],"study_design_scores_gemma":[0.00036874574,0.005496415,0.025354825,0.000082670136,0.00004929243,0.00024345468,0.0005837065,0.67541015,0.28557584,0.004151433,0.0025953325,0.00008819413],"about_ca_topic_score_codex":0.0016194283,"about_ca_topic_score_gemma":0.0008270032,"teacher_disagreement_score":0.0024368474,"about_ca_system_score_codex":0.0005567635,"about_ca_system_score_gemma":0.000307891,"threshold_uncertainty_score":0.008152068},"labels":[],"label_agreement":null},{"id":"W2070717051","doi":"10.1190/1.2369821","title":"Estimates of the hypocenter location errors of passive microseismic events located by using a 3‐C VSP downhole geophone array","year":2006,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Hypocenter; Geophone; Microseism; Geology; Seismology; Passive seismic; Geodesy; Range (aeronautics); Earthquake location; Azimuth; Acoustics; Induced seismicity; Engineering; Physics; Aerospace engineering; Optics","score_opus":0.009087117453738826,"score_gpt":0.2016192514283385,"score_spread":0.19253213397459967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070717051","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8903383,0.000043096785,0.10843004,0.000035776495,0.000017541932,0.000027486356,0.00017264922,0.00030437877,0.0006307906],"genre_scores_gemma":[0.97190803,0.000026269418,0.027810516,0.0000042769448,0.0000029818875,0.000016329728,0.00009625398,0.00001355786,0.00012174828],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9997081,0.00006093197,0.000021828122,0.000057872447,0.00012411251,0.000027206397],"domain_scores_gemma":[0.9960077,0.0020464656,0.00051340164,0.00046234773,0.000887493,0.000082498715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008394911,0.00038822484,0.00022994127,0.0004069341,0.00016025109,0.00020155284,0.0004177524,0.00036162228,0.0003519843],"category_scores_gemma":[0.005929318,0.00017028108,0.00013960092,0.00044437186,0.00024580362,0.00044219318,0.0003276483,0.00022855416,0.00010860116],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015061204,0.00020839638,0.06433603,0.00022179502,0.00013117262,0.00022843324,0.0005347661,0.541082,0.24392505,0.0023143056,0.00055870105,0.1449532],"study_design_scores_gemma":[0.00013072147,0.0005444578,0.061205458,0.000020174097,0.000072405484,0.00017316444,0.000097754164,0.8047645,0.13141188,0.00071853225,0.00077893434,0.000081965765],"about_ca_topic_score_codex":0.003125719,"about_ca_topic_score_gemma":0.0043959767,"teacher_disagreement_score":0.003125719,"about_ca_system_score_codex":0.00036540866,"about_ca_system_score_gemma":0.00030985687,"threshold_uncertainty_score":0.0062150955},"labels":[],"label_agreement":null},{"id":"W2071198079","doi":"10.1007/s00024-012-0521-5","title":"Geophysical Images of the North Anatolian Fault Zone in the Erzincan Basin, Eastern Turkey, and their Tectonic Implications","year":2012,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Geoscience BC","funders":"Natural Sciences and Engineering Research Council of Canada; Istanbul Teknik Üniversitesi","keywords":"North Anatolian Fault; Structural basin; Geology; Seismology; Pull apart basin; Tectonics; Fault (geology); Sedimentary rock; Collision zone; Inversion (geology); Eurasian Plate; Sedimentary basin; Geomorphology; Lithosphere; Paleontology; Subduction","score_opus":0.010028598906282389,"score_gpt":0.1970692769088831,"score_spread":0.1870406780026007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071198079","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99191236,0.00039436977,0.00014326959,0.00016611784,0.000020600257,0.0000114266795,0.003410349,0.000047935828,0.0038935519],"genre_scores_gemma":[0.9969848,0.00023012699,0.00043901807,0.000016156757,0.0000103351285,0.000007566795,0.0014535696,0.000008850986,0.0008496181],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999548,0.00000532288,0.000006151785,0.000012995053,0.000008723318,0.0000119926535],"domain_scores_gemma":[0.9998889,0.000014634479,0.000028481772,0.0000078438725,0.000042369295,0.000017752056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000067655375,0.00018511222,0.000114517214,0.0017290252,0.00024428614,0.00048717886,0.0001969156,0.00034555237,0.0019018358],"category_scores_gemma":[0.00026716065,0.00016049853,0.000086620246,0.0016900991,0.00025026334,0.0002696709,0.00028831026,0.00017332255,0.00020301231],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015018001,0.00042101956,0.678353,0.0008553879,0.00025813642,0.0035449332,0.005519021,0.023722067,0.07143774,0.0029393514,0.014725002,0.19672251],"study_design_scores_gemma":[0.000015788743,0.000011676124,0.9937835,0.000023175216,0.00002077742,0.0001983538,0.0007937978,0.0015580197,0.00031977848,0.0000795383,0.0031868203,0.0000087368435],"about_ca_topic_score_codex":0.039674915,"about_ca_topic_score_gemma":0.093084306,"teacher_disagreement_score":0.039674915,"about_ca_system_score_codex":0.00040158423,"about_ca_system_score_gemma":0.00044547798,"threshold_uncertainty_score":0.07888794},"labels":[],"label_agreement":null},{"id":"W2072457112","doi":"10.1029/2011jb008889","title":"Seismic and aseismic slip pulses driven by thermal pressurization of pore fluid","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Cabin pressurization; Geology; Slip (aerodynamics); Pore water pressure; Thermal; Seismology; Geotechnical engineering; Fluid pressure; Induced seismicity; Mechanics; Materials science; Engineering; Aerospace engineering","score_opus":0.02586990972061298,"score_gpt":0.2795600835306677,"score_spread":0.2536901738100547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072457112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99761283,0.000043589953,0.0015819728,0.000035776633,0.000003210505,0.0000026122486,0.00004869354,0.000026882612,0.0006445118],"genre_scores_gemma":[0.999602,0.00002861483,0.00021551059,0.000004276765,0.0000025164545,0.0000026563548,0.000031654854,0.0000030091085,0.00010973286],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995315,0.0000054914763,0.000003565525,0.00001271557,0.0000106056905,0.000014422486],"domain_scores_gemma":[0.9998566,0.00003483439,0.00005422373,0.0000110218825,0.000011946867,0.00003139294],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009579965,0.00024143091,0.00017071367,0.0002402197,0.00013521293,0.00029736478,0.00032482613,0.00047776208,0.00078457466],"category_scores_gemma":[0.0005757205,0.0002258944,0.0002758253,0.00017821912,0.00042170353,0.00036821753,0.00030600227,0.00039215802,0.00006974355],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006369173,0.00023183809,0.0678224,0.00018881568,0.0001245492,0.0016293136,0.0003153897,0.41766745,0.48915836,0.011684874,0.00048589832,0.01005413],"study_design_scores_gemma":[0.000043011987,0.00012968149,0.040669814,0.0000056019326,0.00001683728,0.00016875903,0.00009042656,0.93542033,0.021813862,0.0013940292,0.00022858607,0.000018999173],"about_ca_topic_score_codex":0.001977345,"about_ca_topic_score_gemma":0.0011346834,"teacher_disagreement_score":0.001977345,"about_ca_system_score_codex":0.00041853669,"about_ca_system_score_gemma":0.00020433363,"threshold_uncertainty_score":0.0039316416},"labels":[],"label_agreement":null},{"id":"W2073101393","doi":"10.1193/1.2206809","title":"The Effect of the December 2004 Great Sumatra Earthquake and Indian Ocean Tsunami on Transportation Systems in India's Andaman and Nicobar Islands","year":2006,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"TD Bank Group","funders":"Department of Science and Technology, Ministry of Science and Technology, India","keywords":"Indian ocean; Port (circuit theory); Geography; Work (physics); Geology; Oceanography; Engineering","score_opus":0.003672306160993068,"score_gpt":0.1846443011091535,"score_spread":0.18097199494816044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073101393","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981097,0.00006771359,0.0000072156363,0.000060583796,0.000002417037,0.0000042024744,0.00007659444,0.0000016946545,0.0016699033],"genre_scores_gemma":[0.9993279,0.00015956697,0.000019702697,0.000021895486,0.0000025101897,0.000007225938,0.00014614717,0.000001574286,0.000313524],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998148,0.000055512108,0.000017347978,0.000015997475,0.000026757534,0.00006952367],"domain_scores_gemma":[0.99951756,0.00007982523,0.00012431343,0.00004112979,0.00012944316,0.0001078514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017717693,0.00021629664,0.00017946122,0.0008750862,0.00077813864,0.0010699063,0.0003944391,0.00026261213,0.0015445447],"category_scores_gemma":[0.0013062037,0.00016549617,0.00023091676,0.0010621722,0.0007733112,0.00039576757,0.0011268229,0.00033766188,0.00023021262],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003236537,0.00010417527,0.9745403,0.000072757415,0.00017505072,0.002338672,0.006378735,0.0015143767,0.0034936687,0.0002546133,0.0009143343,0.00988967],"study_design_scores_gemma":[0.0000028501865,0.00002556169,0.99406815,0.000008246879,0.000018348434,0.00011889892,0.0049908194,0.00011372822,0.00016417803,0.000018716712,0.0004661236,0.000004497103],"about_ca_topic_score_codex":0.19203666,"about_ca_topic_score_gemma":0.21546185,"teacher_disagreement_score":0.19203666,"about_ca_system_score_codex":0.001912299,"about_ca_system_score_gemma":0.00084362045,"threshold_uncertainty_score":0.3818378},"labels":[],"label_agreement":null},{"id":"W2073700961","doi":"10.1029/2004gl021454","title":"Influence of lithospheric thickness variations on 3‐D crustal velocities due to glacial isostatic adjustment","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Adolph C. and Mary Sprague Miller Institute for Basic Research in Science, University of California Berkeley; National Aeronautics and Space Administration","keywords":"Lithosphere; Geology; Post-glacial rebound; Geodetic datum; Discontinuity (linguistics); Ridge; Geodesy; Plate tectonics; Tectonics; Seismology; Glacial period; Geophysics; Geomorphology; Paleontology","score_opus":0.025752782456059716,"score_gpt":0.28633295965481625,"score_spread":0.26058017719875654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073700961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980628,0.000053774726,0.0008011032,0.0000545376,0.000006734703,0.0000026554303,0.000120196135,0.000040443996,0.0008577301],"genre_scores_gemma":[0.9997552,0.000023062425,0.00009816296,0.000005867917,0.000001429778,0.0000011239754,0.000056825524,0.00000875163,0.000049610735],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998553,0.000053130778,0.000013478915,0.00002591749,0.000020653966,0.00003157642],"domain_scores_gemma":[0.99911517,0.00048783774,0.0001394748,0.00011673598,0.00006599648,0.000074853095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057064876,0.00037164876,0.00019213368,0.00041633056,0.00026275913,0.0009499766,0.00028950957,0.00032704975,0.00088718557],"category_scores_gemma":[0.0038172891,0.0003678742,0.0005623681,0.000357834,0.0006023691,0.00032680848,0.00061648985,0.00032054447,0.00013649501],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007482893,0.000054652395,0.25900865,0.00006605478,0.0002711538,0.000530113,0.00024396245,0.6805041,0.04128178,0.0017310174,0.00034464657,0.015215521],"study_design_scores_gemma":[0.00009233179,0.00016287346,0.48942164,0.000015338172,0.000111987305,0.0001637125,0.00013057055,0.49557963,0.012482491,0.0011613668,0.0006209609,0.000057169218],"about_ca_topic_score_codex":0.0121750785,"about_ca_topic_score_gemma":0.005528976,"teacher_disagreement_score":0.0121750785,"about_ca_system_score_codex":0.00070296886,"about_ca_system_score_gemma":0.00031225182,"threshold_uncertainty_score":0.024208426},"labels":[],"label_agreement":null},{"id":"W2073790964","doi":"10.1029/2012eo120014","title":"Passive margin earthquakes: Reviewing knowledge and challenges","year":2012,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Magnitude (astronomy); Seismology; Geology; Moment magnitude scale; Landslide; Margin (machine learning); Continental margin; Earthquake casualty estimation; Remotely triggered earthquakes; Earthquake swarm; Urban seismic risk; Seismic hazard; Induced seismicity; Tectonics","score_opus":0.06052798807337573,"score_gpt":0.24644402923008274,"score_spread":0.185916041156707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073790964","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005440542,0.98238087,0.00020175432,0.014822235,0.0009359565,0.000008082349,0.00014100944,0.0000081418875,0.0009579675],"genre_scores_gemma":[0.0046487916,0.9882684,0.0004797554,0.004244526,0.0019977984,0.000019074045,0.00019305722,0.000005822361,0.00014277376],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9972886,0.0008118199,0.00085668196,0.000428235,0.00044381645,0.0001708464],"domain_scores_gemma":[0.94810826,0.038287994,0.0041862363,0.00076092297,0.007294957,0.0013615815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008560532,0.0007195001,0.0024035824,0.0126603525,0.000993502,0.0044465745,0.0023272617,0.0033616787,0.0036089676],"category_scores_gemma":[0.033966836,0.000785044,0.0008885577,0.010642489,0.0028231523,0.011802488,0.00238901,0.003189692,0.0008953481],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009553122,0.00010311643,0.0044449456,0.0493686,0.00037763914,0.0005697897,0.001681077,0.00073274557,0.0002202802,0.009652255,0.12630166,0.8064524],"study_design_scores_gemma":[0.000022180322,0.000088280794,0.012450847,0.114766814,0.0006187386,0.0015626015,0.0056936275,0.0004734043,0.0001580176,0.022833016,0.84124225,0.00009018189],"about_ca_topic_score_codex":0.00846003,"about_ca_topic_score_gemma":0.020063654,"teacher_disagreement_score":0.0126603525,"about_ca_system_score_codex":0.0031197993,"about_ca_system_score_gemma":0.010059874,"threshold_uncertainty_score":0.045273006},"labels":[],"label_agreement":null},{"id":"W2073831195","doi":"10.1029/1999jb900439","title":"Further evidence for the compound nature of slow earthquakes: The Prince Edward Island earthquake of April 28, 1997","year":2000,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Slow earthquake; Seismogram; Transform fault; Foreshock; Fault (geology); Superposition principle; Earthquake swarm; Amplitude; Event (particle physics); Interplate earthquake; Aftershock; Induced seismicity; Physics","score_opus":0.0428334471483998,"score_gpt":0.31970653549797173,"score_spread":0.2768730883495719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073831195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984328,0.00005479669,0.00017658653,0.0000497248,0.0000029511768,0.0000069407943,0.0002782413,0.0000076274646,0.0009902907],"genre_scores_gemma":[0.998351,0.00009042654,0.0002985839,0.000014389905,0.000010361676,0.000006561749,0.0006191675,0.000006084046,0.000603482],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989283,0.000008804935,0.0000108726645,0.000023176506,0.000034621535,0.000029794439],"domain_scores_gemma":[0.9989034,0.0002256245,0.00031521835,0.000104957864,0.00032410916,0.00012666348],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019386144,0.00021891898,0.00020698832,0.0007375484,0.0003388045,0.00050018064,0.00020617267,0.00026004657,0.0022578847],"category_scores_gemma":[0.0017892546,0.00023363988,0.00011211131,0.0007787417,0.00033279552,0.0003784717,0.00067333295,0.00024339175,0.00028808028],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005601713,0.000039912426,0.934861,0.00010125621,0.00009953174,0.0019632261,0.00084717554,0.0003866795,0.045163818,0.0003453886,0.00091150723,0.0147203645],"study_design_scores_gemma":[0.000009967924,0.00005673616,0.9970004,0.000004090305,0.0000125004435,0.00040667094,0.00019541885,0.0002666956,0.0013215308,0.000057298512,0.0006636508,0.00000505996],"about_ca_topic_score_codex":0.0095858285,"about_ca_topic_score_gemma":0.032738477,"teacher_disagreement_score":0.99041414,"about_ca_system_score_codex":0.0002854665,"about_ca_system_score_gemma":0.000376061,"threshold_uncertainty_score":0.019060075},"labels":[],"label_agreement":null},{"id":"W2074230146","doi":"10.1007/s00024-009-0010-7","title":"Omori’s Law Applied to Mining-Induced Seismicity and Re-entry Protocol Development","year":2009,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Aftershock; Induced seismicity; Sequence (biology); Event (particle physics); Statistic; Rate function; Geology; Power law; Statistics; Interval (graph theory); Mathematics; Function (biology); Curvature; Seismology; Physics; Combinatorics; Geometry; Large deviations theory","score_opus":0.01658460114218295,"score_gpt":0.22450204667083534,"score_spread":0.20791744552865238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074230146","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0136367455,0.0024762722,0.6925117,0.035979882,0.00493203,0.00139515,0.001456324,0.0015373281,0.2460746],"genre_scores_gemma":[0.35047606,0.0021012742,0.5013326,0.026358549,0.0048708427,0.009080322,0.00076866767,0.00082744006,0.10418421],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9496509,0.010464589,0.012142379,0.009388224,0.01372039,0.0046335408],"domain_scores_gemma":[0.8894577,0.062481407,0.005447588,0.022720667,0.018784493,0.0011082058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.042021222,0.0011484305,0.00320359,0.0060205646,0.009366773,0.011060294,0.003920376,0.015699869,0.008688643],"category_scores_gemma":[0.12850517,0.002629142,0.0053992257,0.0040488965,0.018306177,0.021873793,0.008377843,0.023287168,0.0053112404],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031458716,0.00002155552,0.00043225757,0.00008490817,0.000024989346,0.00014638809,0.00069899624,0.00024139875,0.00018649385,0.9782672,0.008488436,0.011375927],"study_design_scores_gemma":[0.000101804435,0.00005914716,0.0007534194,0.0003803463,0.00017374309,0.0009318094,0.00029819863,0.005483062,0.0021352756,0.8621751,0.12738541,0.00012262755],"about_ca_topic_score_codex":0.010244569,"about_ca_topic_score_gemma":0.007424405,"teacher_disagreement_score":0.042021222,"about_ca_system_score_codex":0.006523222,"about_ca_system_score_gemma":0.015508306,"threshold_uncertainty_score":0.22223216},"labels":[],"label_agreement":null},{"id":"W2074295211","doi":"10.1029/2008jb005978","title":"Thermal and metamorphic environment of subduction zone episodic tremor and slip","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":192,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Subduction; Episodic tremor and slip; Oceanic crust; Crust; Blueschist; Seismology; Lithosphere; Convergent boundary; Underplating; Metamorphic rock; North American Plate; Petrology; Geochemistry; Tectonics; Eclogite","score_opus":0.031116937119851543,"score_gpt":0.2669926049630681,"score_spread":0.23587566784321656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074295211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991781,0.00009049144,0.000055795954,0.000008538751,9.2891185e-7,0.0000017260837,0.00012579485,0.0000067497886,0.00053172675],"genre_scores_gemma":[0.99965596,0.000042189855,0.000024997566,0.0000030772921,8.8671743e-7,0.0000014097808,0.00012752863,0.000001961684,0.00014207688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999255,0.0000073432157,0.000005587234,0.0000249236,0.000012700699,0.000023895278],"domain_scores_gemma":[0.99990356,0.000007953058,0.000028624987,0.0000059955246,0.000024429579,0.0000294957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008005189,0.00017627928,0.00016369835,0.0004544909,0.00023378582,0.0003672393,0.00016251745,0.00018915223,0.0011982848],"category_scores_gemma":[0.00021522319,0.00022094083,0.00013956885,0.0003066787,0.0003504112,0.00021373587,0.00030195806,0.0001427364,0.00019459277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047292595,0.000049540784,0.6895785,0.000072040864,0.000051106697,0.0005682043,0.00072368054,0.0025388973,0.3002547,0.00023559986,0.00020963239,0.0052451403],"study_design_scores_gemma":[0.000003067304,0.000021649319,0.9969284,0.0000020729374,0.0000043706955,0.0000474039,0.00015195149,0.0007642096,0.0019015262,0.000032193067,0.00013943935,0.0000037262416],"about_ca_topic_score_codex":0.011319794,"about_ca_topic_score_gemma":0.011100516,"teacher_disagreement_score":0.011319794,"about_ca_system_score_codex":0.0005239135,"about_ca_system_score_gemma":0.00016737147,"threshold_uncertainty_score":0.022507787},"labels":[],"label_agreement":null},{"id":"W2074449096","doi":"10.1007/s10518-013-9495-7","title":"Developing and testing the Automated Post-Event Earthquake Loss Estimation and Visualisation (APE-ELEV) technique","year":2013,"lang":"en","type":"article","venue":"Bulletin of Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Visualization; Event (particle physics); Estimation; Computer science; Real-time computing; Data visualization; Seismology; Data mining; Geology; Engineering; Systems engineering","score_opus":0.015213090687026087,"score_gpt":0.2175797433051197,"score_spread":0.2023666526180936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074449096","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32277182,0.00019771616,0.6430847,0.00018853418,0.000109429,0.00022443909,0.0005810514,0.029655928,0.0031862985],"genre_scores_gemma":[0.5609014,0.000084103835,0.4346659,0.000087860084,0.000029359975,0.00008773466,0.0008130249,0.0005579459,0.002772683],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99927324,0.00015785536,0.00003786683,0.0001621278,0.00030162573,0.000067275614],"domain_scores_gemma":[0.99823487,0.00095540204,0.00008865089,0.00027408043,0.00037988304,0.00006715265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009539438,0.0004417523,0.00037119555,0.00050159125,0.0002189361,0.0006129602,0.0012556632,0.0008772655,0.004046088],"category_scores_gemma":[0.004077526,0.00026789858,0.00031362992,0.00037244573,0.00026386123,0.00097352883,0.00095052127,0.0005672576,0.0011500606],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012230593,0.0006949747,0.013598246,0.0002911777,0.00014107813,0.00048800727,0.000422046,0.108318835,0.13227011,0.0032532574,0.0068366625,0.73246247],"study_design_scores_gemma":[0.00012650758,0.00040879814,0.005996092,0.000015632173,0.000029223997,0.00031931128,0.00008571105,0.91952807,0.06821193,0.0007323684,0.004516091,0.000030238141],"about_ca_topic_score_codex":0.0027648322,"about_ca_topic_score_gemma":0.0023703226,"teacher_disagreement_score":0.004046088,"about_ca_system_score_codex":0.00018331746,"about_ca_system_score_gemma":0.0004609496,"threshold_uncertainty_score":0.0135355},"labels":[],"label_agreement":null},{"id":"W2074501712","doi":"10.1029/2004eo180005","title":"“Coupling” Semantics and science in earthquake research","year":2004,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":117,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Slipping; Geodetic datum; Plate tectonics; Coupling (piping); Slip (aerodynamics); Geology; Computer science; Kinematics; Earthquake prediction; Seismology; Physics; Tectonics; Geometry; Geodesy; Mathematics; Engineering; Aerospace engineering; Classical mechanics; Mechanical engineering","score_opus":0.05229288625743987,"score_gpt":0.3034540191394107,"score_spread":0.25116113288197084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074501712","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.015422649,0.046855178,0.64950967,0.056863036,0.0075846557,0.00015025669,0.00079965557,0.000922418,0.2218924],"genre_scores_gemma":[0.69060314,0.022851828,0.22319175,0.023483459,0.013882321,0.0009702376,0.0017247426,0.0013100675,0.021982431],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9912538,0.005193859,0.0010108463,0.00119116,0.0010164251,0.00033396474],"domain_scores_gemma":[0.9871525,0.008614425,0.00094771635,0.0015021336,0.0012284858,0.00055483065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009028185,0.0013567848,0.0013521186,0.0056466293,0.0041506737,0.008236195,0.0018937702,0.0040855412,0.0072417264],"category_scores_gemma":[0.0145852035,0.00066650024,0.0013603689,0.009264157,0.026915072,0.03276445,0.005257048,0.0062684203,0.0018174725],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000055830255,0.0000022918875,0.000046193032,0.000036312693,0.0000037205405,0.000020567253,0.00056221255,0.00010724398,0.00004188763,0.9945245,0.002010475,0.002639026],"study_design_scores_gemma":[0.0000064436294,0.0000069594216,0.00007599815,0.00004070053,0.0000041410035,0.00008731997,0.00034597397,0.0005089734,0.000053903812,0.94419926,0.054660883,0.000009355115],"about_ca_topic_score_codex":0.0019553597,"about_ca_topic_score_gemma":0.0011470879,"teacher_disagreement_score":0.009028185,"about_ca_system_score_codex":0.0041174446,"about_ca_system_score_gemma":0.0018903535,"threshold_uncertainty_score":0.04774618},"labels":[],"label_agreement":null},{"id":"W2074979148","doi":"10.1080/00288306.2012.676556","title":"Statistical analysis of the 2010 <i>M</i> <sub>W</sub> 7.1 Darfield Earthquake aftershock sequence","year":2012,"lang":"en","type":"article","venue":"New Zealand Journal of Geology and Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Johns Hopkins University","keywords":"Aftershock; Seismology; Geology; Magnitude (astronomy); Sequence (biology); Foreshock; Physics","score_opus":0.014446707850699394,"score_gpt":0.2208663762596501,"score_spread":0.2064196684089507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074979148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986833,0.00002839983,0.0003264777,0.000025535715,0.000002374281,0.000007196205,0.00055800384,0.0000061672913,0.00036267276],"genre_scores_gemma":[0.99859923,0.000019100627,0.00011417178,0.0000031003096,0.000004179485,0.0000061771498,0.0010650844,0.0000034842994,0.00018544267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99944264,0.00009394517,0.00004584884,0.00014756637,0.00019645787,0.00007352746],"domain_scores_gemma":[0.9956345,0.0016579606,0.0015309533,0.00031461558,0.00052031665,0.0003416548],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009017444,0.00016086454,0.0003203789,0.001460502,0.00024368687,0.00053360965,0.0002829727,0.00023228185,0.0015950706],"category_scores_gemma":[0.00515978,0.00011207122,0.0002789704,0.001466566,0.00068431906,0.00027537046,0.00036153127,0.0003285357,0.00019447331],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033287128,0.000045049957,0.9677422,0.000053387957,0.0002195033,0.00039152085,0.00039344686,0.006700557,0.00824667,0.00068731804,0.0009141211,0.014273394],"study_design_scores_gemma":[0.0000022432241,0.000042687396,0.9953252,0.0000020194186,0.000010332804,0.000032538286,0.000109899804,0.0039372887,0.00022463518,0.00004879305,0.00025818023,0.0000062061445],"about_ca_topic_score_codex":0.04084365,"about_ca_topic_score_gemma":0.03980254,"teacher_disagreement_score":0.04084365,"about_ca_system_score_codex":0.0008304204,"about_ca_system_score_gemma":0.00045192818,"threshold_uncertainty_score":0.081211865},"labels":[],"label_agreement":null},{"id":"W2075104819","doi":"10.1016/j.jsg.2007.10.003","title":"Deformation, exhumation, and topography of experimental doubly-vergent orogenic wedges subjected to asymmetric erosion","year":2007,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Wedge (geometry); Erosion; Shear (geology); Kinematics; Geometry; Particle image velocimetry; Simple shear; Geotechnical engineering; Geomorphology; Mechanics; Physics; Petrology; Classical mechanics","score_opus":0.011499679775896436,"score_gpt":0.23915544989231802,"score_spread":0.22765577011642157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075104819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99990547,0.000002355601,0.000021856493,7.290946e-7,5.08744e-7,0.0000011690043,0.000017140621,6.385274e-7,0.000050149672],"genre_scores_gemma":[0.99977607,0.0000076413035,0.000044420456,0.0000028052486,4.6699864e-7,0.0000027659507,0.00005141676,0.0000017088275,0.00011277655],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998913,0.000015397864,0.000011312408,0.000022689563,0.000021656439,0.000037611957],"domain_scores_gemma":[0.99974424,0.00006175478,0.00005204878,0.0000625449,0.000027934037,0.00005152409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016143631,0.00019935108,0.0003893061,0.00024603267,0.00028398354,0.0002732234,0.00040605094,0.0003127121,0.0017337286],"category_scores_gemma":[0.0005025867,0.00021559946,0.0002465211,0.00031315006,0.0007272609,0.0002453627,0.0003889411,0.00035864994,0.00018092801],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.011507342,0.0018237679,0.045795597,0.00006530073,0.00007285407,0.00091936154,0.00081848825,0.003334835,0.9297834,0.00030530582,0.00009478349,0.0054790312],"study_design_scores_gemma":[0.0005531613,0.010208975,0.6494743,0.000016741391,0.0001573096,0.0012155649,0.0021236634,0.014881692,0.32032913,0.00030489126,0.0006876409,0.000046834914],"about_ca_topic_score_codex":0.002988957,"about_ca_topic_score_gemma":0.0025054098,"teacher_disagreement_score":0.002988957,"about_ca_system_score_codex":0.00020194257,"about_ca_system_score_gemma":0.0001847171,"threshold_uncertainty_score":0.0059431195},"labels":[],"label_agreement":null},{"id":"W2075670662","doi":"10.1130/l65.1","title":"State of stress in central and eastern North American seismic zones","year":2010,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Clockwise; Seismology; Induced seismicity; Azimuth; Borehole; Focal mechanism; Stress field; Intraplate earthquake; Stress (linguistics); Magnitude (astronomy); Geodesy; Rotation (mathematics); Tectonics; Geometry; Paleontology","score_opus":0.006495146780503489,"score_gpt":0.1957644384445398,"score_spread":0.1892692916640363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075670662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985598,0.000053941552,0.000660596,0.000020827662,4.8038464e-7,0.000004158622,0.00015665637,0.000009886155,0.00053375866],"genre_scores_gemma":[0.998845,0.00004572866,0.00058855687,0.000008026398,0.0000016528143,0.000008008163,0.00032664082,0.0000019609506,0.00017445748],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997856,0.00004511486,0.000013692417,0.00007485255,0.000040633724,0.000040146388],"domain_scores_gemma":[0.9994004,0.00013883424,0.00019277378,0.000030510342,0.00016460642,0.00007282394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005928896,0.00016833495,0.000207475,0.0012715462,0.00044195633,0.0005626158,0.00025282134,0.0002048295,0.0005943465],"category_scores_gemma":[0.0012559395,0.0002478387,0.00021304209,0.0011336397,0.0003404946,0.00022483956,0.00061946514,0.00018180322,0.0000603435],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001605581,0.000041495136,0.9707143,0.000019101555,0.00010721283,0.00008211502,0.0008451951,0.0082519865,0.0032001506,0.00045313482,0.0002643286,0.015860407],"study_design_scores_gemma":[0.000008281378,0.000012481299,0.98648864,0.000008151751,0.000022922492,0.000027998312,0.00032199456,0.012217852,0.0001796283,0.00030592372,0.00039651548,0.000009533453],"about_ca_topic_score_codex":0.12178893,"about_ca_topic_score_gemma":0.21238965,"teacher_disagreement_score":0.12178893,"about_ca_system_score_codex":0.0008344981,"about_ca_system_score_gemma":0.0007927502,"threshold_uncertainty_score":0.24216008},"labels":[],"label_agreement":null},{"id":"W2076036711","doi":"10.1007/s00024-011-0420-1","title":"Analysis of GPS Measurements in Eastern Canada Using Principal Component Analysis","year":2011,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Western University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geodesy; Geology; Global Positioning System; Principal component analysis; Post-glacial rebound; Tectonics; Empirical orthogonal functions; Seismology; Mathematics; Statistics; Climatology; Geomorphology; Computer science; Glacial period","score_opus":0.05309355539206375,"score_gpt":0.21574277697392258,"score_spread":0.16264922158185882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076036711","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98900294,0.0004242272,0.0010285699,0.000112280075,0.000016205557,0.000037493588,0.005844167,0.00007638201,0.00345784],"genre_scores_gemma":[0.99261004,0.00025786244,0.0013308257,0.000023800176,0.0000056558792,0.000012644784,0.0037209545,0.000015725182,0.0020225202],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996141,0.000034055913,0.000023627712,0.00006255973,0.00015287027,0.00011272087],"domain_scores_gemma":[0.9982607,0.00014949977,0.000096184776,0.00003966892,0.001333854,0.00012008453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002931215,0.0003158016,0.0003049899,0.002407946,0.0011852713,0.0010545303,0.0005133122,0.00022888347,0.0009738118],"category_scores_gemma":[0.0015226854,0.00019993797,0.00024925295,0.006161057,0.00037416586,0.00018740747,0.00042662313,0.0002687779,0.00024753762],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025914074,0.00006174498,0.9225967,0.0001138718,0.00014726496,0.00031687968,0.0015175531,0.004810103,0.004657204,0.00041335687,0.0030152258,0.062091004],"study_design_scores_gemma":[0.0000048647876,0.0000071081777,0.9948337,0.000012744535,0.000021880931,0.000030286732,0.0006393942,0.002686737,0.00027801513,0.000021798101,0.0014522008,0.000011258129],"about_ca_topic_score_codex":0.9935137,"about_ca_topic_score_gemma":0.99536103,"teacher_disagreement_score":0.008082972,"about_ca_system_score_codex":0.008082972,"about_ca_system_score_gemma":0.013362936,"threshold_uncertainty_score":0.05864632},"labels":[],"label_agreement":null},{"id":"W2076476316","doi":"10.1038/ncomms7157","title":"Probing failure susceptibilities of earthquake faults using small-quake tidal correlations","year":2015,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Kavli Institute for Theoretical Physics, University of California, Santa Barbara; Southern California Earthquake Center; Division of Materials Research; U.S. Geological Survey; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Quake (natural phenomenon); Seismology; Geology; Earthquake prediction; Remotely triggered earthquakes; Amplitude; Seismic gap; Earthquake magnitude; Magnitude (astronomy); Fault (geology); Earthquake simulation; Foreshock; Aftershock; Physics; Mathematics","score_opus":0.061922455068407704,"score_gpt":0.2790612647843436,"score_spread":0.2171388097159359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076476316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877093,0.0000331597,0.011186246,0.000061300714,0.000004733743,0.0000147355495,0.00031846625,0.000075478,0.00059673825],"genre_scores_gemma":[0.99930644,0.000015875052,0.00048364326,0.0000035073979,0.0000015408235,0.000003832431,0.00009929489,0.0000040885366,0.00008187116],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998373,0.000047469683,0.000013006942,0.000055785764,0.000022727038,0.000023732773],"domain_scores_gemma":[0.99827194,0.00082678423,0.00043081745,0.00025630198,0.00010571015,0.000108468485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005846772,0.0005029766,0.00044578747,0.0006468786,0.00023905444,0.00052147795,0.00066511036,0.00053863187,0.0013462835],"category_scores_gemma":[0.0042462316,0.00033478823,0.00054474024,0.00063837046,0.00045463495,0.0009201764,0.00039016028,0.00036607444,0.00017553724],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010437652,0.00008644193,0.16257603,0.000045367964,0.0001064374,0.00015188172,0.000073726325,0.82396215,0.0057768626,0.0011017658,0.00022579951,0.0057890983],"study_design_scores_gemma":[0.0000052867126,0.000047559817,0.041800767,0.0000030398755,0.000013891806,0.000036519563,0.000018869896,0.95634437,0.0007234499,0.00094015134,0.00005291906,0.000013125157],"about_ca_topic_score_codex":0.008781225,"about_ca_topic_score_gemma":0.008677278,"teacher_disagreement_score":0.008781225,"about_ca_system_score_codex":0.0005760234,"about_ca_system_score_gemma":0.0003651593,"threshold_uncertainty_score":0.017460227},"labels":[],"label_agreement":null},{"id":"W2076766035","doi":"10.1111/j.1945-5100.2007.tb01080.x","title":"Impactites as a random medium—Using variations in physical properties to assess heterogeneity within the Bosumtwi meteorite impact crater","year":2007,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Kwame Nkrumah University of Science and Technology","keywords":"Impact crater; Impact structure; Geology; Petrophysics; Borehole; Meteorite; Seismic velocity; Basement; Seismology; Scale (ratio); Geophysics; Petrology; Paleontology; Geotechnical engineering","score_opus":0.051191150400254834,"score_gpt":0.30042866633552096,"score_spread":0.2492375159352661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076766035","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985638,0.00003964273,0.0010707764,0.0000045856495,8.232506e-7,0.000008138501,0.000084188425,0.00001163059,0.00021645834],"genre_scores_gemma":[0.9994972,0.000015250998,0.0003335424,0.0000014743923,8.938327e-7,0.000004173186,0.00008323345,0.0000029334324,0.000061267696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988914,0.000016873255,0.0000064148912,0.00003743495,0.000026748758,0.000023348666],"domain_scores_gemma":[0.99965644,0.00010960214,0.00012062641,0.00003030222,0.000031258092,0.000051847634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018851181,0.00029203473,0.00022782272,0.0013108167,0.00024869465,0.0008505621,0.00015575571,0.00018674943,0.0007268123],"category_scores_gemma":[0.00068067695,0.00020434338,0.0001333503,0.00086390116,0.0004727555,0.0004278351,0.00037074462,0.0002064156,0.000107120715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006135732,0.00008351142,0.847221,0.000062024505,0.00011603173,0.00035617832,0.0003850148,0.007875975,0.12838152,0.0002213796,0.0000880243,0.014595736],"study_design_scores_gemma":[0.00000721492,0.00007905912,0.9786971,0.0000052258906,0.000021211918,0.00013265644,0.00029983334,0.015107699,0.0053424644,0.00008450077,0.00021263576,0.000010339953],"about_ca_topic_score_codex":0.008705251,"about_ca_topic_score_gemma":0.010461259,"teacher_disagreement_score":0.008705251,"about_ca_system_score_codex":0.00042831988,"about_ca_system_score_gemma":0.00013670576,"threshold_uncertainty_score":0.017309189},"labels":[],"label_agreement":null},{"id":"W2077371277","doi":"10.1144/sp290.6","title":"Extensional deformation and development of deep basins associated with the sinistral transcurrent fault zone of the Scotia–Antarctic plate boundary","year":2007,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sinistral and dextral; Extensional definition; Geology; Nova scotia; Fault (geology); Deformation (meteorology); Boundary (topology); Extensional fault; Seismology; Plate tectonics; Oceanography; Tectonics; Mathematics","score_opus":0.020445089684898006,"score_gpt":0.22093785952696945,"score_spread":0.20049276984207146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077371277","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99902594,0.000056489593,0.000021540003,0.000007909122,0.0000017188991,0.0000028724166,0.00018144601,0.0000021574347,0.0007000489],"genre_scores_gemma":[0.9996457,0.000025604117,0.000017882536,0.000002870596,9.082565e-7,0.0000012191601,0.00011442284,7.030306e-7,0.00019070154],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995637,0.0000030754147,0.000002957837,0.000012914632,0.0000087043845,0.000015922808],"domain_scores_gemma":[0.9998147,0.000012470732,0.00006203569,0.000011529055,0.000051015733,0.000048316157],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000077799334,0.00017671396,0.00008638737,0.0008933264,0.00031489154,0.00042862745,0.00011194882,0.0001524264,0.0011480855],"category_scores_gemma":[0.00018254301,0.00011169014,0.0001343817,0.0006734674,0.0003619658,0.00011672596,0.00030737536,0.000109444794,0.00015955674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013132257,0.000012960836,0.9703736,0.000026444215,0.00003710388,0.0005986138,0.0004327217,0.00053780794,0.024400083,0.0000871521,0.00012649105,0.0032356996],"study_design_scores_gemma":[7.2989553e-7,0.00000247855,0.9997131,0.0000013183818,0.0000011392183,0.000026721995,0.000055691562,0.00006689696,0.00006841953,0.0000033591211,0.000059544567,4.9380935e-7],"about_ca_topic_score_codex":0.14076646,"about_ca_topic_score_gemma":0.2054237,"teacher_disagreement_score":0.14076646,"about_ca_system_score_codex":0.00058800407,"about_ca_system_score_gemma":0.00038682026,"threshold_uncertainty_score":0.27989417},"labels":[],"label_agreement":null},{"id":"W2077697757","doi":"10.1016/j.jsg.2014.10.010","title":"Displacement transfer from fault-bend to fault-propagation fold geometry: An example from the Himalayan thrust front","year":2014,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Queen's University; Alberta Energy","funders":"Natural Sciences and Engineering Research Council of Canada; Oregon State University; National Science Foundation","keywords":"Geology; Fold (higher-order function); Fault (geology); Thrust; Geometry; Thrust fault; Seismology; Kinematics","score_opus":0.022678659540142584,"score_gpt":0.23023562136712863,"score_spread":0.20755696182698605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077697757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99540365,0.000058828133,0.0006010982,0.000061533414,0.0000049484165,0.000010248108,0.0001198599,0.00002292937,0.003716803],"genre_scores_gemma":[0.999456,0.000046883233,0.00020499092,0.0000072465677,0.0000022531246,0.0000011938386,0.000041444604,0.0000019563654,0.00023807342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995935,0.0000067896967,0.0000026508803,0.000010040639,0.000008290595,0.000012893149],"domain_scores_gemma":[0.99994135,0.000014685719,0.000011072884,0.000012550154,0.000011001623,0.0000093534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058384612,0.0001629283,0.00014044635,0.00041823176,0.0006399159,0.0005408213,0.0002329561,0.00038574924,0.0020465439],"category_scores_gemma":[0.00025304055,0.000097976364,0.00020354027,0.00060666347,0.00061006617,0.00017942769,0.0003258826,0.00022652638,0.0002576195],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001169994,0.00027943734,0.63416624,0.0004090923,0.00017602275,0.027461335,0.010852803,0.055058025,0.16122656,0.015564442,0.002086061,0.09155008],"study_design_scores_gemma":[0.00006823272,0.0002357908,0.92818373,0.000040444633,0.00005902527,0.0031917223,0.0041363263,0.048375033,0.008401053,0.0029562667,0.004290733,0.00006168488],"about_ca_topic_score_codex":0.02297046,"about_ca_topic_score_gemma":0.018188436,"teacher_disagreement_score":0.02297046,"about_ca_system_score_codex":0.0006347688,"about_ca_system_score_gemma":0.00023814812,"threshold_uncertainty_score":0.04567355},"labels":[],"label_agreement":null},{"id":"W2078029362","doi":"10.1007/s00024-008-0414-9","title":"Numerical Modeling and Observations of Tsunami Waves in Alberni Inlet and Barkley Sound, British Columbia","year":2008,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada","keywords":"Geology; Inlet; Seismology; Sound (geography); Amplification factor; Subduction; Fjord; Acoustics; Oceanography; Physics; Tectonics","score_opus":0.01962169270711501,"score_gpt":0.18888454942927096,"score_spread":0.16926285672215596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078029362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99805886,0.000027599297,0.00010984395,0.000054077318,0.000002929943,0.000009930726,0.00042719446,0.000021992455,0.0012874746],"genre_scores_gemma":[0.99873406,0.000043706706,0.00016774301,0.0000065470554,0.0000010246757,0.000009847875,0.0003325892,0.000004821312,0.0006997596],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997917,0.0000239601,0.000016973023,0.000045364937,0.00005670114,0.00006535174],"domain_scores_gemma":[0.99932814,0.00016693416,0.00006214917,0.000036998623,0.00030904892,0.000096696574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023492449,0.0003180135,0.0002658237,0.0008098616,0.0017456656,0.0012833085,0.0012434237,0.00075624435,0.0015323756],"category_scores_gemma":[0.0018974141,0.0005444156,0.0002717395,0.0013653635,0.00065879535,0.00043229634,0.0005411286,0.0006006689,0.00030565736],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058888434,0.0004525684,0.7012339,0.000083273175,0.00014262422,0.00060602924,0.0017332454,0.26313806,0.008798861,0.0011425166,0.0031814694,0.018898632],"study_design_scores_gemma":[0.00010954611,0.000041694482,0.66483337,0.000034679957,0.00005812792,0.000050966362,0.0016700292,0.32917395,0.0019122325,0.00020413609,0.0018485114,0.0000627263],"about_ca_topic_score_codex":0.97815037,"about_ca_topic_score_gemma":0.9791813,"teacher_disagreement_score":0.021849632,"about_ca_system_score_codex":0.011148933,"about_ca_system_score_gemma":0.007339987,"threshold_uncertainty_score":0.08089155},"labels":[],"label_agreement":null},{"id":"W2078102699","doi":"10.1785/0120040607","title":"The Mw 7.9 Denali Fault Earthquake of 3 November 2002: Felt Reports and Unusual Effects across Western Canada","year":2004,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Seismology; Geology; Fault (geology)","score_opus":0.007880695352921048,"score_gpt":0.20848287276287367,"score_spread":0.20060217740995262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078102699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885175,0.00068228383,0.00006517645,0.0011736454,0.000019186524,0.000030062172,0.0011743722,0.000018161782,0.008319505],"genre_scores_gemma":[0.99609935,0.0010327201,0.000079435944,0.00021254635,0.000013882873,0.000008692172,0.0005866855,0.0000067258334,0.001959838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995425,0.000022959211,0.000023994917,0.000035716606,0.00018843754,0.00018656305],"domain_scores_gemma":[0.9987888,0.000057448444,0.00019010954,0.0000287469,0.0006175554,0.0003173072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020624188,0.0002456827,0.00021123987,0.0013937186,0.004338345,0.0013979552,0.0005719289,0.00032695403,0.0013848158],"category_scores_gemma":[0.0011809095,0.00021990431,0.00012195972,0.0028612658,0.0011211642,0.00038493905,0.0014170536,0.00065213966,0.00011861502],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020317847,0.00009146485,0.903423,0.0001803806,0.000088397246,0.004519226,0.030409275,0.00028540616,0.0034929197,0.00080543046,0.012565933,0.043935403],"study_design_scores_gemma":[0.0000050431863,0.0000151649865,0.9798815,0.000030783296,0.000014528926,0.00033559592,0.013871072,0.000059932823,0.00016643261,0.000033166583,0.0055708354,0.000015905021],"about_ca_topic_score_codex":0.9866419,"about_ca_topic_score_gemma":0.9957207,"teacher_disagreement_score":0.013436382,"about_ca_system_score_codex":0.013436382,"about_ca_system_score_gemma":0.016015548,"threshold_uncertainty_score":0.097488225},"labels":[],"label_agreement":null},{"id":"W2078173986","doi":"10.1007/s11434-011-4417-z","title":"The earthquake precursor detected in a granular medium and a proposed model for the propagation of precursive stress-strain signal","year":2011,"lang":"en","type":"article","venue":"Chinese Science Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"MD Precision (Canada)","funders":"","keywords":"Lithosphere; Geology; Seismology; SIGNAL (programming language); Tectonics; Shear stress; Slip (aerodynamics); Shear (geology); Fault (geology); Deformation (meteorology); Stress (linguistics); Geotechnical engineering; Mechanics; Petrology; Physics","score_opus":0.018116810202246255,"score_gpt":0.221497693011274,"score_spread":0.20338088280902775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078173986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7817217,0.0005714206,0.20413437,0.0007413621,0.0002035418,0.000080684535,0.00041746383,0.0005432664,0.011586175],"genre_scores_gemma":[0.9928069,0.00014958717,0.005585156,0.000021874725,0.000022843637,0.000012394264,0.00006980034,0.00001083303,0.0013206032],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999496,0.000005178596,0.0000035801024,0.000017293987,0.000013757508,0.000010690791],"domain_scores_gemma":[0.9997466,0.000078096215,0.000054857494,0.000023682598,0.000052017393,0.00004478226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015275784,0.000423155,0.00031828193,0.00083935476,0.0003896215,0.0007675765,0.0008340581,0.0009143854,0.001966871],"category_scores_gemma":[0.0007499422,0.0003010724,0.0003970337,0.0005346416,0.0005535959,0.0010716654,0.0003918094,0.00055328174,0.00023937057],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00077626813,0.00028739785,0.0450333,0.00050561794,0.00014249279,0.013265173,0.0007918783,0.2903493,0.3264984,0.2857748,0.0028469544,0.033728544],"study_design_scores_gemma":[0.000046284826,0.00012437347,0.011767048,0.000017253908,0.000057420573,0.0008361432,0.00011389547,0.9629629,0.00619555,0.017337512,0.0004921957,0.000049362825],"about_ca_topic_score_codex":0.0026413817,"about_ca_topic_score_gemma":0.0013416596,"teacher_disagreement_score":0.0026413817,"about_ca_system_score_codex":0.00036556073,"about_ca_system_score_gemma":0.00030499775,"threshold_uncertainty_score":0.0065798163},"labels":[],"label_agreement":null},{"id":"W2078394908","doi":"10.1016/j.pepi.2011.04.012","title":"Temporal variations of coda Q: An attenuation-coefficient view","year":2011,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Coda; Attenuation; Geology; Volcano; Seismology; Canyon; Attenuation coefficient; Physics; Optics; Geomorphology","score_opus":0.0318366978033869,"score_gpt":0.21460745281862648,"score_spread":0.18277075501523957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078394908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.908695,0.0019404846,0.053871155,0.002353459,0.00024454357,0.00004169435,0.0024289587,0.0006027144,0.029821942],"genre_scores_gemma":[0.99452174,0.00021599085,0.0017543144,0.00007093129,0.000057273755,0.000008957763,0.0004587344,0.00012292607,0.0027890452],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998362,0.000014029628,0.000009134827,0.000063309235,0.000030985175,0.00004629824],"domain_scores_gemma":[0.99823797,0.00064109743,0.00035976028,0.00025533253,0.0004069605,0.00009891582],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006260486,0.0003465518,0.00021738104,0.0013795667,0.00031144495,0.0008984392,0.00056962087,0.00088968995,0.0044014896],"category_scores_gemma":[0.0037756376,0.00031966894,0.00029299522,0.0014044283,0.000572763,0.0012534729,0.0005707692,0.00095210964,0.0006222035],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00087329914,0.00040011044,0.4544597,0.00046496067,0.00036403068,0.0019162107,0.0022679577,0.1459615,0.13107786,0.09387124,0.015895648,0.15244745],"study_design_scores_gemma":[0.000054029326,0.0001411171,0.7153023,0.000086764616,0.00014238444,0.0010791324,0.0005842635,0.23765823,0.008546538,0.016780294,0.01949729,0.00012761043],"about_ca_topic_score_codex":0.009837731,"about_ca_topic_score_gemma":0.0054551805,"teacher_disagreement_score":0.009837731,"about_ca_system_score_codex":0.0005020136,"about_ca_system_score_gemma":0.0003147175,"threshold_uncertainty_score":0.019560933},"labels":[],"label_agreement":null},{"id":"W2078467113","doi":"10.3137/ao.460304","title":"Locally generated tsunamis recorded on the coast of British Columbia","year":2008,"lang":"en","type":"article","venue":"ATMOSPHERE-OCEAN","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadian Hydrographic Service; Geological Survey of Canada; Natural Resources Canada; Fisheries and Oceans Canada","funders":"U.S. Geological Survey; National Oceanic and Atmospheric Administration; Russian Foundation for Basic Research","keywords":"Seismology; Geology; Tide gauge; Subduction; Harbour; Shore; Oceanography; Tsunami earthquake; Tsunami wave; Bathymetry; Sea level; Tectonics","score_opus":0.015220472802823536,"score_gpt":0.1846564041025792,"score_spread":0.16943593129975565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078467113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970425,0.000036793765,0.0001841507,0.000033315802,0.000003311594,0.000008939301,0.00042153802,0.000033012435,0.0022363835],"genre_scores_gemma":[0.9987722,0.000033096203,0.00015595354,0.0000063660996,7.4180605e-7,0.000006472039,0.00036407934,0.0000044029994,0.0006565983],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999114,0.000009650406,0.000004515086,0.000021686388,0.00001926522,0.000033347176],"domain_scores_gemma":[0.9997662,0.00005670446,0.000025585867,0.000016602631,0.0000808248,0.00005409394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105307896,0.00027455177,0.00027501548,0.0005995821,0.00080750126,0.0010485372,0.0006025143,0.00046547258,0.0029502374],"category_scores_gemma":[0.0007889246,0.00021896072,0.00029108018,0.00088305253,0.0004881337,0.00031328952,0.0004037628,0.0003949211,0.00021665663],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032424452,0.00012228121,0.21098523,0.000091843474,0.00014691487,0.0009774445,0.00033219866,0.7694234,0.0030010745,0.0007535881,0.0017639337,0.012077767],"study_design_scores_gemma":[0.00014100451,0.00015319562,0.23247167,0.00003716733,0.000093996096,0.0001441446,0.0017243706,0.761386,0.0017722262,0.0003756034,0.0016306798,0.00006989695],"about_ca_topic_score_codex":0.7957231,"about_ca_topic_score_gemma":0.8276561,"teacher_disagreement_score":0.20427692,"about_ca_system_score_codex":0.0043444955,"about_ca_system_score_gemma":0.0021161414,"threshold_uncertainty_score":0.41095984},"labels":[],"label_agreement":null},{"id":"W2078591229","doi":"10.1007/s00024-010-0076-2","title":"Ergodicity and Earthquake Catalogs: Forecast Testing and Resulting Implications","year":2010,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"U.S. Geological Survey; National Science Council; Southern California Earthquake Center; Institute for Catastrophic Loss Reduction; National Science Foundation","keywords":"Ergodicity; Ergodic theory; Induced seismicity; Context (archaeology); Statistical physics; Measure (data warehouse); Computer science; Geology; Econometrics; Physics; Mathematics; Seismology; Data mining; Statistics","score_opus":0.017968466275965232,"score_gpt":0.2061465324181065,"score_spread":0.18817806614214125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078591229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97914064,0.0007048305,0.008637976,0.0023020809,0.00005501476,0.00002966471,0.0020678183,0.00013911958,0.0069229035],"genre_scores_gemma":[0.99743015,0.0002457641,0.0010301345,0.000037991485,0.00006651455,0.000005150658,0.00073135935,0.00001320971,0.00043971735],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987068,0.00063543284,0.00008759207,0.00026595625,0.00019224062,0.0001118317],"domain_scores_gemma":[0.8294278,0.15044925,0.0065319757,0.0055599147,0.005419734,0.0026112369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009341008,0.00039513328,0.0005101699,0.0033431342,0.00092893164,0.003024956,0.0012769075,0.0009422217,0.012030514],"category_scores_gemma":[0.10676851,0.00034482774,0.00058584556,0.0031374223,0.0021565075,0.0068007326,0.0016563098,0.0008743781,0.0006441864],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019133444,0.000205952,0.8339328,0.0001094739,0.00020850137,0.00046166507,0.0006655742,0.054200076,0.0004992152,0.032302994,0.0026115305,0.07288882],"study_design_scores_gemma":[0.00035560958,0.0003949754,0.49649072,0.00012014873,0.0006234593,0.00043318333,0.0051004416,0.3597851,0.0021622,0.13140042,0.0030034764,0.0001302985],"about_ca_topic_score_codex":0.02952358,"about_ca_topic_score_gemma":0.02084476,"teacher_disagreement_score":0.02952358,"about_ca_system_score_codex":0.0013632183,"about_ca_system_score_gemma":0.001639286,"threshold_uncertainty_score":0.058703482},"labels":[],"label_agreement":null},{"id":"W2079210410","doi":"10.1142/s0217979209063857","title":"MODELS OF EARTHQUAKE FAULTS: ERGODICITY AND FORECASTING","year":2009,"lang":"en","type":"article","venue":"International Journal of Modern Physics B","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Earthquake prediction; Fault (geology); Earthquake simulation; Seismology; Ergodicity; Computer science; Geology; Mathematics; Statistics","score_opus":0.03975585483151604,"score_gpt":0.24523283295469478,"score_spread":0.20547697812317875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079210410","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.37362888,0.0063947677,0.58416444,0.008653651,0.00045931348,0.000028993481,0.0015257546,0.0007220928,0.0244221],"genre_scores_gemma":[0.987975,0.002192337,0.006078928,0.00008795513,0.00027534502,0.0000145325475,0.00026791857,0.000051765954,0.0030562398],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998085,0.00007565165,0.000011281608,0.000032856486,0.00003567538,0.000036014524],"domain_scores_gemma":[0.99764013,0.0014871492,0.0003845223,0.0002087862,0.00014593138,0.00013349336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095538184,0.000561285,0.00083284016,0.00057951006,0.00039531107,0.0012539953,0.0011626895,0.0011354884,0.0023337556],"category_scores_gemma":[0.007497193,0.00032096374,0.0005183536,0.00094605476,0.0011705194,0.0031039477,0.0009269163,0.0008844673,0.00026349621],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035770772,0.000016109778,0.0028638542,0.000048187103,0.000037561025,0.000049507318,0.00006435234,0.8556922,0.00026428324,0.13182195,0.0012463724,0.007859944],"study_design_scores_gemma":[0.000004726515,0.000010495557,0.00054872397,0.000012815511,0.0000118987755,0.000028687413,0.000019747771,0.85919285,0.00012998836,0.13915744,0.000871761,0.000010895132],"about_ca_topic_score_codex":0.005552418,"about_ca_topic_score_gemma":0.0029344563,"teacher_disagreement_score":0.005552418,"about_ca_system_score_codex":0.0008906183,"about_ca_system_score_gemma":0.00038402804,"threshold_uncertainty_score":0.011040211},"labels":[],"label_agreement":null},{"id":"W2079654931","doi":"10.1190/tle31121438.1","title":"The potential for induced seismicity in energy technologies","year":2012,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dillon Consulting","funders":"","keywords":"Induced seismicity; Magnitude (astronomy); Seismology; Geology; Range (aeronautics); Earthquake magnitude; Natural (archaeology); Maximum magnitude; Seismic energy; Engineering; Physics; Paleontology","score_opus":0.029069914252926193,"score_gpt":0.23891943149553857,"score_spread":0.2098495172426124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079654931","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.33120596,0.016363652,0.04842764,0.0125654815,0.0005432853,0.00021387836,0.000598757,0.00033523035,0.5897462],"genre_scores_gemma":[0.9663911,0.006126321,0.004119019,0.0005388495,0.00020552715,0.000087692155,0.00018496852,0.000042196636,0.022304444],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9991398,0.00024190123,0.00003458253,0.00009401752,0.00036419003,0.00012549371],"domain_scores_gemma":[0.99729484,0.001496208,0.0003360279,0.0002637317,0.00046014602,0.00014913197],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014465558,0.00024205737,0.00017603673,0.0007400816,0.0006402492,0.001897806,0.000670556,0.0015037482,0.018521436],"category_scores_gemma":[0.0042673103,0.00021782544,0.00029912198,0.00086880976,0.0014159887,0.003290991,0.0015468149,0.0011857626,0.0025011743],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025369946,0.00037535603,0.021576503,0.0011843491,0.000071848546,0.002690115,0.0010021614,0.025054779,0.019447641,0.7627451,0.01008824,0.15551014],"study_design_scores_gemma":[0.00009487415,0.0014108927,0.03705742,0.000843185,0.000102201986,0.0059988815,0.0035900578,0.022496156,0.038460888,0.53120655,0.35861573,0.00012316222],"about_ca_topic_score_codex":0.00033870147,"about_ca_topic_score_gemma":0.00044874658,"teacher_disagreement_score":0.018521436,"about_ca_system_score_codex":0.0012383579,"about_ca_system_score_gemma":0.0007290304,"threshold_uncertainty_score":0.06196034},"labels":[],"label_agreement":null},{"id":"W2079799974","doi":"10.1029/2008gl036660","title":"Frictional behavior of materials in the 3D SAFOD volume","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Geology; Lithology; Siltstone; Outcrop; Borehole; Mineralogy; Talc; Fault gouge; Petrology; Mafic; Geochemistry; Quartz; Fault (geology); Geotechnical engineering; Seismology; Geomorphology; Facies","score_opus":0.04096782447316287,"score_gpt":0.29827752716952133,"score_spread":0.25730970269635844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079799974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963104,0.00008406993,0.0024766878,0.000010485821,0.0000022853317,0.0000033249823,0.00026953148,0.00008492588,0.0007583856],"genre_scores_gemma":[0.9986192,0.000032832428,0.00087939086,0.000002613191,0.0000011353247,0.000002603348,0.0003572691,0.000010887341,0.000094031646],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998957,0.000007412399,0.000007527806,0.00002750759,0.000043349784,0.000018503599],"domain_scores_gemma":[0.99978083,0.00007188476,0.000050618026,0.000035321074,0.000038592574,0.000022749324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011126738,0.00020593122,0.00024527826,0.0008553862,0.00027202076,0.00079839205,0.00029836752,0.00021521334,0.0010056865],"category_scores_gemma":[0.00073413405,0.00028190477,0.00030013896,0.00060453475,0.0003586453,0.00044569827,0.00031326473,0.00015448265,0.00013640407],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007194348,0.00012319394,0.30007634,0.00019586661,0.00026255858,0.0011431039,0.00090819714,0.4059299,0.23899116,0.001975254,0.00055718847,0.049117807],"study_design_scores_gemma":[0.000037215093,0.00017199734,0.4438368,0.000023348208,0.00006273214,0.0006821434,0.00032946494,0.4991066,0.05160133,0.0009234581,0.0031326867,0.00009226393],"about_ca_topic_score_codex":0.0039245845,"about_ca_topic_score_gemma":0.005018256,"teacher_disagreement_score":0.0039245845,"about_ca_system_score_codex":0.00039828368,"about_ca_system_score_gemma":0.00020636246,"threshold_uncertainty_score":0.00780344},"labels":[],"label_agreement":null},{"id":"W2080100222","doi":"10.1038/srep05011","title":"Faulting of Rocks in a Three-Dimensional Stress Field by Micro-Anticracks","year":2014,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"U.S. Geological Survey; University of Toronto; Universitetet i Oslo; University of Portsmouth; University of Oklahoma","keywords":"Nucleation; Coalescence (physics); Stress field; Geology; Stress (linguistics); Slip (aerodynamics); Orthorhombic crystal system; Shear (geology); Fault (geology); Shear stress; Acoustic emission; Waveform; Stress wave; Materials science; Seismology; Composite material; Petrology; Physics; Diffraction; Optics","score_opus":0.009695324921225847,"score_gpt":0.2140593597333014,"score_spread":0.20436403481207555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080100222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973719,0.00007714754,0.0021742573,0.00001339247,0.0000036464146,0.0000031202676,0.000033131226,0.000026703437,0.0002966327],"genre_scores_gemma":[0.99924445,0.000042198397,0.0005863387,0.0000047404837,0.0000029717546,0.0000025191698,0.000026569258,0.0000033335023,0.00008696699],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994314,0.000004391214,0.000004016334,0.000013596297,0.000018043873,0.000016820406],"domain_scores_gemma":[0.99984753,0.000025117408,0.00006483609,0.000015401627,0.000022744289,0.000024328632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000048235026,0.00010389028,0.00010749318,0.00025014,0.00017351155,0.00029877428,0.00009953459,0.00011191616,0.0006119699],"category_scores_gemma":[0.00018866699,0.00011620765,0.00011312731,0.00019882905,0.0003768022,0.00025062414,0.00017876954,0.00017217382,0.00005602697],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000100789584,0.000034073648,0.01806758,0.000048176535,0.000016357277,0.00039173337,0.00023289263,0.0055919667,0.9657521,0.00079155527,0.00009209304,0.008880772],"study_design_scores_gemma":[0.00003290773,0.00027275225,0.49939272,0.00001641992,0.0000411584,0.0010708609,0.00073439395,0.13696298,0.35726184,0.0022333467,0.0019157201,0.000064896594],"about_ca_topic_score_codex":0.0009258056,"about_ca_topic_score_gemma":0.001287704,"teacher_disagreement_score":0.0009258056,"about_ca_system_score_codex":0.00018294204,"about_ca_system_score_gemma":0.00012651258,"threshold_uncertainty_score":0.0020472407},"labels":[],"label_agreement":null},{"id":"W2081828689","doi":"10.1002/2014eo350002","title":"Decades‐Old Sediment Cores Complicate Cascadia Earthquake History","year":2014,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Seismology; Sediment; Hazard; Oceanography; Paleontology; Tectonics","score_opus":0.02514708571172378,"score_gpt":0.2079678564519434,"score_spread":0.18282077074021963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081828689","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8624551,0.018242743,0.011409981,0.014852298,0.0035916625,0.00008994803,0.015357147,0.00035613135,0.073644884],"genre_scores_gemma":[0.96744007,0.0073431246,0.006220468,0.0027822426,0.0014158529,0.00003872183,0.005160516,0.00028073604,0.009318311],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986518,0.0002204477,0.00032905024,0.00023363324,0.00046362955,0.00010147302],"domain_scores_gemma":[0.99047196,0.0024652302,0.0026682261,0.0015751884,0.0023539322,0.00046549956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0035650658,0.00039653608,0.00032742225,0.0038200642,0.000980669,0.0023953791,0.0007060146,0.00063972897,0.0033747356],"category_scores_gemma":[0.015350529,0.00057876547,0.00026073874,0.0041435766,0.0010629907,0.0025042146,0.0012036052,0.0013829792,0.0012142735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002074914,0.000036975038,0.79275715,0.00053628784,0.00026477675,0.002118486,0.0073035266,0.0014033954,0.006083829,0.0052609243,0.03979151,0.14423563],"study_design_scores_gemma":[0.0000057526645,0.00002068921,0.9001241,0.00033183873,0.000063385945,0.00060466136,0.003136022,0.0004570766,0.0010528198,0.0034568615,0.090712465,0.000034354478],"about_ca_topic_score_codex":0.048137434,"about_ca_topic_score_gemma":0.2009993,"teacher_disagreement_score":0.048137434,"about_ca_system_score_codex":0.0012353396,"about_ca_system_score_gemma":0.00097341667,"threshold_uncertainty_score":0.09571445},"labels":[],"label_agreement":null},{"id":"W2081856232","doi":"10.1126/science.1255487","title":"Strength of stick-slip and creeping subduction megathrusts from heat flow observations","year":2014,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":261,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Slip (aerodynamics); Subduction; Geology; Episodic tremor and slip; Heat flow; Seismology; Flow (mathematics); Mechanics; Tectonics; Thermal; Meteorology; Thermodynamics; Physics","score_opus":0.02559612414900526,"score_gpt":0.2158308863645157,"score_spread":0.19023476221551044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081856232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986223,0.00006905363,0.0004957363,0.000020151867,0.0000018794741,0.00000473081,0.0003748517,0.000026081685,0.00038522072],"genre_scores_gemma":[0.99958175,0.000027780152,0.00014898807,0.0000015942024,0.0000013735938,0.0000013075014,0.0001968444,0.0000032016974,0.000037167927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998778,0.000025883543,0.000012586223,0.000035197154,0.000029640443,0.000018790603],"domain_scores_gemma":[0.9994486,0.00018250402,0.00016000349,0.00006896013,0.00006258869,0.000077376615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003722129,0.00034986425,0.00031816482,0.00096068915,0.00014972287,0.00041995887,0.00032408498,0.00041183276,0.0007367911],"category_scores_gemma":[0.001661167,0.00028710224,0.00032722877,0.0006500788,0.00040205824,0.00054988626,0.00037836205,0.00023309185,0.00011241371],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019018177,0.00007783399,0.73547125,0.00013340937,0.00018979512,0.00030871743,0.00020849927,0.23781352,0.015251496,0.00054133276,0.0003582358,0.009455708],"study_design_scores_gemma":[0.000021016096,0.000047934223,0.6999751,0.000019908459,0.000036311936,0.000071522394,0.000089993664,0.29656944,0.0024731047,0.0004663997,0.0002006157,0.00002868842],"about_ca_topic_score_codex":0.007304175,"about_ca_topic_score_gemma":0.010657351,"teacher_disagreement_score":0.007304175,"about_ca_system_score_codex":0.0003607441,"about_ca_system_score_gemma":0.00018324511,"threshold_uncertainty_score":0.014523268},"labels":[],"label_agreement":null},{"id":"W2082074032","doi":"10.1029/2005gl023521","title":"The dual source region for the 2004 Sumatra tsunami","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Geology; Seismology; Dual (grammatical number); Oceanography; Climatology","score_opus":0.049511480265275444,"score_gpt":0.2951365846909577,"score_spread":0.24562510442568228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082074032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9603877,0.00033032394,0.0018569783,0.00033204255,0.000031215513,0.00004328913,0.01951758,0.000108478824,0.017392421],"genre_scores_gemma":[0.96391976,0.00031487833,0.0027003337,0.000057747347,0.000018621535,0.00009171315,0.026407223,0.000036550755,0.0064532505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998871,0.000012528415,0.000012203265,0.000031230913,0.000031419182,0.000025468667],"domain_scores_gemma":[0.99939513,0.000063969565,0.00025350545,0.000053920103,0.00016413874,0.00006929754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012745656,0.00021533917,0.00016702534,0.002145298,0.00049765204,0.0006545597,0.00020693583,0.0001828008,0.0060885297],"category_scores_gemma":[0.00081674976,0.0001269148,0.00015220897,0.002017773,0.0001875689,0.00030528253,0.0008558864,0.0003161966,0.0015412515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006370319,0.00016311897,0.76256025,0.00032053492,0.00016026538,0.0021786937,0.004147496,0.0044783005,0.038194247,0.004351447,0.028300444,0.15450822],"study_design_scores_gemma":[0.000014249319,0.000027741191,0.9759976,0.00002516024,0.000040454717,0.00075422437,0.001370575,0.0014933628,0.0015263609,0.0003204353,0.01841574,0.000014024953],"about_ca_topic_score_codex":0.029074006,"about_ca_topic_score_gemma":0.04429636,"teacher_disagreement_score":0.029074006,"about_ca_system_score_codex":0.0011325285,"about_ca_system_score_gemma":0.0008888058,"threshold_uncertainty_score":0.05780959},"labels":[],"label_agreement":null},{"id":"W2082336797","doi":"10.1785/gssrl.79.2.211","title":"Significant Canadian Earthquakes of the Period 1600-2006","year":2008,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Period (music); Seismology; Geology","score_opus":0.07957421453212468,"score_gpt":0.27249038467450776,"score_spread":0.19291617014238308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082336797","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20056812,0.0106461495,0.0008046779,0.010008722,0.0010107602,0.0002783939,0.58675975,0.0004233841,0.18950006],"genre_scores_gemma":[0.5635462,0.018015305,0.0024130638,0.0018906877,0.0004187106,0.00017462448,0.27374873,0.00020231908,0.13959028],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9993598,0.000009273781,0.000025686857,0.00005366416,0.00037085023,0.00018067317],"domain_scores_gemma":[0.9982663,0.000029407496,0.00018603774,0.000042006828,0.0012127355,0.00026359138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028970392,0.0008001842,0.00030433462,0.004858897,0.0042780456,0.0017593538,0.0007098483,0.00042212705,0.014768864],"category_scores_gemma":[0.001966098,0.00024904677,0.0003654074,0.011566771,0.0004132113,0.0006568663,0.0011457425,0.0007071566,0.0018957892],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021559604,0.000057288264,0.19318505,0.0015687093,0.00013893905,0.00085419364,0.0045044795,0.0009881562,0.0010196704,0.005937461,0.6689673,0.122563116],"study_design_scores_gemma":[0.000013404508,0.000012001178,0.69592535,0.00020117263,0.00003568656,0.00018245826,0.0024033051,0.00026695407,0.00021376701,0.00018743466,0.3005063,0.000052160383],"about_ca_topic_score_codex":0.9971215,"about_ca_topic_score_gemma":0.99922407,"teacher_disagreement_score":0.032647554,"about_ca_system_score_codex":0.032647554,"about_ca_system_score_gemma":0.056707703,"threshold_uncertainty_score":0.23687565},"labels":[],"label_agreement":null},{"id":"W2082597758","doi":"10.1029/2001gl013102","title":"The initiation of orogenic margin reverse faulting","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lithosphere; Crust; Brittleness; Compression (physics); Petrology; Seismology; Tectonics; Geophysics","score_opus":0.06646318903321433,"score_gpt":0.28886097474338884,"score_spread":0.22239778571017452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082597758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97901595,0.00045411944,0.0016094412,0.00009148609,0.000022160631,0.000026760257,0.00009721718,0.00010064123,0.018582186],"genre_scores_gemma":[0.9988954,0.000109174674,0.00021966653,0.000014735109,0.0000046495734,0.0000040066384,0.000059745245,0.000005715637,0.0006869622],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9997614,0.00002750883,0.000013658385,0.00004192052,0.000054053355,0.00010136086],"domain_scores_gemma":[0.9996506,0.000046249537,0.000102908845,0.000074471005,0.00007093722,0.000054782802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025052167,0.00022290742,0.00022124608,0.00024039131,0.00042990907,0.0005738657,0.00019462171,0.00032224873,0.0019645044],"category_scores_gemma":[0.0010106633,0.00018239218,0.00021018588,0.00012631307,0.0003867963,0.00038962037,0.00091920374,0.0003773779,0.00069842377],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010263049,0.00010752685,0.19852714,0.0004838524,0.00005505616,0.0042029046,0.0012877879,0.007428199,0.7140375,0.015220786,0.0013203295,0.056302663],"study_design_scores_gemma":[0.00011207871,0.00089878665,0.5501207,0.00014251228,0.00010872223,0.003647836,0.0015500144,0.008323889,0.38854858,0.004641194,0.041833982,0.00007167512],"about_ca_topic_score_codex":0.0016820279,"about_ca_topic_score_gemma":0.0019032619,"teacher_disagreement_score":0.0019645044,"about_ca_system_score_codex":0.0004719527,"about_ca_system_score_gemma":0.00038305362,"threshold_uncertainty_score":0.0065719485},"labels":[],"label_agreement":null},{"id":"W2082647032","doi":"10.1029/2009gl040230","title":"Laboratory simulation of fluid‐driven seismic sequences in shallow crustal conditions","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Induced seismicity; Geology; Seismology; Volcano; Aftershock; Slip (aerodynamics); Pore water pressure; Seismic hazard; Fluid pressure; Limiting; Geotechnical engineering; Mechanics","score_opus":0.03765208673907226,"score_gpt":0.3161034976753258,"score_spread":0.27845141093625353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082647032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933395,0.000035699526,0.003951521,0.00007972044,0.000014034691,0.000021225993,0.00017533186,0.00009833613,0.0022846074],"genre_scores_gemma":[0.99819726,0.000023401593,0.0013257754,0.000010957191,0.0000027910141,0.00002688164,0.00010813772,0.0000063972366,0.0002986023],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999918,0.0000162769,0.0000054261895,0.000017021886,0.000016175496,0.000026966605],"domain_scores_gemma":[0.99918145,0.00046668868,0.00012529218,0.000053009564,0.00007937971,0.0000941863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025590564,0.0003031797,0.0003523056,0.00025637526,0.0002496623,0.00053661695,0.000739464,0.00073781237,0.0015797106],"category_scores_gemma":[0.0013651964,0.00024567498,0.00035034926,0.00023092159,0.0007003019,0.00043326893,0.0005027427,0.0006462889,0.000094412],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016250489,0.00020452117,0.005958085,0.000029147921,0.000030096786,0.00013762432,0.000055655328,0.9870674,0.0036464208,0.0009346675,0.00018962112,0.0015843287],"study_design_scores_gemma":[0.000037350474,0.000090218804,0.00056783145,0.0000020888185,0.0000065284453,0.0000060625252,0.000020180667,0.99782026,0.0011548216,0.00019426252,0.00009482599,0.0000055674686],"about_ca_topic_score_codex":0.009187146,"about_ca_topic_score_gemma":0.0057536876,"teacher_disagreement_score":0.009187146,"about_ca_system_score_codex":0.0006421179,"about_ca_system_score_gemma":0.0006171645,"threshold_uncertainty_score":0.018267334},"labels":[],"label_agreement":null},{"id":"W2083145334","doi":"10.1007/s10950-009-9173-z","title":"Coseismic stress parameter of three California Earthquakes derived from the stochastic finite fault technique","year":2009,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Hypocenter; Geology; Fault (geology); Stress (linguistics); Stochastic modelling; Aftershock; Induced seismicity; Mathematics; Statistics","score_opus":0.019227421574896857,"score_gpt":0.22585170719758113,"score_spread":0.20662428562268428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083145334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968644,0.00003902339,0.0016339469,0.000021695818,0.000004145927,0.0000039162505,0.0003145095,0.000046107696,0.0010722928],"genre_scores_gemma":[0.99947566,0.000008530052,0.00031769322,0.0000011834048,0.0000013402178,0.0000012015743,0.00014939238,0.0000048881584,0.00004009668],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994254,0.0000074852337,0.0000054263123,0.000021450636,0.000012333475,0.000010741118],"domain_scores_gemma":[0.99937457,0.00026329077,0.000104322135,0.00007903508,0.00013677948,0.00004205852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025674782,0.00025325076,0.00025088905,0.0007937442,0.00027520276,0.0003605065,0.00043347903,0.00037657685,0.00084210944],"category_scores_gemma":[0.0014964252,0.00020645003,0.00021650587,0.00079774635,0.00027104115,0.0003447812,0.00016507253,0.00036067222,0.000086933615],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012423604,0.0003063296,0.39607507,0.0001489322,0.00021664641,0.00085511565,0.00068896293,0.48979005,0.04913153,0.0082667945,0.002365208,0.05091293],"study_design_scores_gemma":[0.000055515888,0.00009107024,0.56113017,0.000011099112,0.00006707757,0.00013629837,0.00015753439,0.43314442,0.0035617682,0.00090017176,0.00069132133,0.000053470332],"about_ca_topic_score_codex":0.021831306,"about_ca_topic_score_gemma":0.024642369,"teacher_disagreement_score":0.021831306,"about_ca_system_score_codex":0.0005206656,"about_ca_system_score_gemma":0.00031654254,"threshold_uncertainty_score":0.043408453},"labels":[],"label_agreement":null},{"id":"W2084049188","doi":"10.1029/2007jb005272","title":"Dissipation analysis as a guide to mode selection during crustal extension and implications for the styles of sedimentary basins","year":2008,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Dissipation; Geology; Simple shear; Shear zone; Crust; Shear (geology); Brittleness; Pure shear; Sedimentary basin; Mechanics; Shear rate; Strain rate; Plasticity; Shear band; Viscoelasticity; Viscosity; Petrology; Geophysics; Structural basin; Seismology; Physics; Thermodynamics; Geomorphology","score_opus":0.03932859759283491,"score_gpt":0.3463359253032808,"score_spread":0.30700732771044587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084049188","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0573729,0.0009038879,0.9239706,0.00060787244,0.0001300931,0.00009931756,0.00018020037,0.0007186129,0.016016548],"genre_scores_gemma":[0.6514416,0.0015834346,0.32012162,0.00020443354,0.00012058875,0.00037092908,0.00018163526,0.0012213183,0.02475439],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99986327,0.00005036222,0.0000113170545,0.000017463757,0.000033043343,0.000024559688],"domain_scores_gemma":[0.99965847,0.00016723,0.00004576424,0.00005205315,0.000051954852,0.000024594803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062040635,0.0007596506,0.00046407615,0.0013395203,0.0006566803,0.0011230957,0.0011636318,0.0005168905,0.007080634],"category_scores_gemma":[0.0017020085,0.00044196457,0.00088806596,0.00061324943,0.00073401065,0.00114494,0.00092350476,0.0012550498,0.000781956],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000081467304,0.00011110756,0.0063729156,0.00016764297,0.000049560887,0.0004675038,0.00095663767,0.53047955,0.026518473,0.33172792,0.0050924276,0.097974785],"study_design_scores_gemma":[0.000007786497,0.000030614927,0.0015543585,0.000040353207,0.0000058584787,0.00006999324,0.00012853976,0.9033267,0.0026825718,0.08666584,0.005452879,0.000034534398],"about_ca_topic_score_codex":0.0026945907,"about_ca_topic_score_gemma":0.0023591185,"teacher_disagreement_score":0.007080634,"about_ca_system_score_codex":0.00049337355,"about_ca_system_score_gemma":0.00031216192,"threshold_uncertainty_score":0.023687124},"labels":[],"label_agreement":null},{"id":"W2084438194","doi":"10.1190/1.1817923","title":"Assessing the effectiveness of hydraulic fractures with microseismicity","year":2003,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Schlumberger (Canada)","funders":"","keywords":"Geology; Hydraulic fracturing; Petroleum engineering","score_opus":0.012754970937894128,"score_gpt":0.24887195221268982,"score_spread":0.2361169812747957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084438194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898185,0.00024859005,0.0067332205,0.00008832605,0.000012827103,0.000047647743,0.0006638064,0.00005822683,0.0023287744],"genre_scores_gemma":[0.9984351,0.000041732284,0.00093383354,0.0000054550787,0.0000051717047,0.00001149671,0.00029910443,0.0000073798765,0.0002607639],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9961499,0.0007917559,0.000361897,0.0005735218,0.0016994106,0.00042342115],"domain_scores_gemma":[0.9797249,0.009523687,0.004968248,0.0014225596,0.0030979451,0.0012627825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030650117,0.00046260093,0.00037280397,0.002096604,0.0003859236,0.0012361701,0.0007114544,0.0010443407,0.0026164788],"category_scores_gemma":[0.02492195,0.0003367373,0.0006991922,0.0014416381,0.00085447094,0.0017617195,0.0017344534,0.00052739243,0.00059252867],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065620063,0.00014700054,0.9383368,0.00006205209,0.00015925593,0.00017332545,0.00011664854,0.030333526,0.0031017761,0.00074831804,0.0004462626,0.025718682],"study_design_scores_gemma":[0.000027188147,0.001180644,0.9052758,0.00004915781,0.0001455419,0.00046537354,0.0009672554,0.078919105,0.009542741,0.0022896498,0.0010916215,0.000045996294],"about_ca_topic_score_codex":0.0066933455,"about_ca_topic_score_gemma":0.010075994,"teacher_disagreement_score":0.0066933455,"about_ca_system_score_codex":0.00084729365,"about_ca_system_score_gemma":0.0008760794,"threshold_uncertainty_score":0.016209483},"labels":[],"label_agreement":null},{"id":"W2084548800","doi":"10.1029/2005gl023974","title":"Array measurements of deep tremor signals in the Cascadia subduction zone","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Istituto Nazionale di Geofisica e Vulcanologia","keywords":"Slowness; Seismometer; Geology; Seismology; Azimuth; Subduction; Transverse plane; Seismic wave; Seismic array; Geodesy; Geophysics; Optics; Physics; Tectonics","score_opus":0.07824455294584534,"score_gpt":0.30410472088375584,"score_spread":0.2258601679379105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084548800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998475,0.000026454123,0.000529003,0.000020520094,0.0000018397524,0.0000044386197,0.00027007973,0.000020757308,0.0006519843],"genre_scores_gemma":[0.9983553,0.000031129766,0.00079096085,0.000006312543,0.0000035469302,0.000008114027,0.00047866188,0.0000041032686,0.00032184116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998349,0.000016925813,0.0000115865605,0.00006278192,0.000049245537,0.000024631423],"domain_scores_gemma":[0.99957234,0.00005628704,0.00008847193,0.00004498834,0.00013666258,0.0001012903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016045109,0.00024433158,0.00018810872,0.0007054503,0.00028490505,0.00022797327,0.00017339297,0.00018136915,0.0004894508],"category_scores_gemma":[0.0007995847,0.00018336938,0.00011021288,0.00081970356,0.00017721459,0.00014453345,0.00041120723,0.00021254113,0.00016030014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057557767,0.00007521283,0.66639405,0.00007775747,0.00011287759,0.00030191278,0.0021478927,0.004802642,0.29016423,0.00014841017,0.0006214606,0.03457791],"study_design_scores_gemma":[0.000014060874,0.000079511585,0.99477506,0.000003422545,0.000021488826,0.000062460924,0.00015727628,0.0016222683,0.0027590084,0.000039597646,0.00045733247,0.000008366525],"about_ca_topic_score_codex":0.019705582,"about_ca_topic_score_gemma":0.04498278,"teacher_disagreement_score":0.019705582,"about_ca_system_score_codex":0.00039368795,"about_ca_system_score_gemma":0.0002559249,"threshold_uncertainty_score":0.03918177},"labels":[],"label_agreement":null},{"id":"W2085947043","doi":"10.1029/2011eo470001","title":"Seafloor seismometers monitor northern Cascadia earthquakes","year":2011,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Japan Agency for Marine-Earth Science and Technology; Woods Hole Oceanographic Institution; W. M. Keck Foundation; National Science Foundation","keywords":"Geology; Seismology; Subduction; Seafloor spreading; Seismometer; Submarine pipeline; Fault (geology); Tsunami earthquake; Induced seismicity; Earthquake rupture; Moment magnitude scale; Magnitude (astronomy); Tectonics; Oceanography","score_opus":0.03210322903931997,"score_gpt":0.20034812155572676,"score_spread":0.16824489251640679,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085947043","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98527354,0.00013865816,0.00032662187,0.00007367423,0.000013251734,0.000030976997,0.008022823,0.00021682805,0.0059035867],"genre_scores_gemma":[0.9906386,0.00016475306,0.00067275774,0.000022626331,0.000017931481,0.000023569432,0.006998026,0.00001586033,0.0014458138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999724,0.000031762473,0.000024285968,0.00009549461,0.00008200822,0.000042477397],"domain_scores_gemma":[0.9989573,0.000073876705,0.0003528614,0.00008492661,0.00034062905,0.00019042617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026063534,0.00048541278,0.0002014324,0.0018867787,0.00023091918,0.0003751538,0.000272679,0.00025017126,0.0019977058],"category_scores_gemma":[0.0010005864,0.00018935687,0.00012188333,0.0018747331,0.00016238191,0.00039650168,0.00058746315,0.00018144405,0.0009183322],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000082357816,0.0000461454,0.9705235,0.00007367947,0.000062395615,0.00012934998,0.0006857868,0.0006558105,0.006217919,0.00006114076,0.0037843105,0.017677628],"study_design_scores_gemma":[0.0000035167495,0.000019411107,0.9979608,0.000005651599,0.0000085116835,0.000034848177,0.00016563495,0.00026288445,0.00026113313,0.000012018494,0.0012624215,0.0000032093587],"about_ca_topic_score_codex":0.023048123,"about_ca_topic_score_gemma":0.090762556,"teacher_disagreement_score":0.023048123,"about_ca_system_score_codex":0.00051873986,"about_ca_system_score_gemma":0.00030361852,"threshold_uncertainty_score":0.045827985},"labels":[],"label_agreement":null},{"id":"W2085980973","doi":"10.1130/l164.1","title":"Miocene bivergent crustal extension in the Aegean: Evidence from the western Cyclades (Greece)","year":2011,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":156,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Accelerated Innovation Research Initiative Turning Top Science and Ideas into High-Impact Values; Austrian Science Fund","keywords":"CYCLADES; Geology; Crust; Blueschist; Detachment fault; Seismology; Shear zone; Shear (geology); Late Miocene; Fault (geology); Normal fault; Paleontology; Geochemistry; Tectonics; Subduction; Structural basin; Eclogite","score_opus":0.07141097716849992,"score_gpt":0.23727679951961622,"score_spread":0.1658658223511163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085980973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99689734,0.0004268186,0.000038651928,0.000033655495,0.0000028447585,0.0000040196296,0.000088603316,0.0000032517328,0.0025048014],"genre_scores_gemma":[0.99874926,0.00052136136,0.00010061466,0.000029724963,0.000006213708,0.000003134847,0.00016996407,0.0000025766294,0.00041709884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989426,0.000015462276,0.000016519294,0.000037380523,0.00001710573,0.000019193936],"domain_scores_gemma":[0.999846,0.000012698963,0.000067212626,0.000016225253,0.000034760516,0.000022983715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021720948,0.00031608655,0.00018531637,0.0015467765,0.00037749571,0.0005723763,0.00022856204,0.00030201508,0.0015979161],"category_scores_gemma":[0.00031358356,0.00013729047,0.00017393296,0.0011701589,0.0008208053,0.00045293698,0.000595116,0.00016005243,0.0003035942],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016504136,0.000027893953,0.9545162,0.00015796913,0.00012675588,0.0015777982,0.004270311,0.00027949724,0.012625798,0.00030095404,0.00023869055,0.025713045],"study_design_scores_gemma":[0.0000040174036,0.000026352267,0.9966978,0.000021018617,0.000014565948,0.00043465698,0.0012123102,0.000052409643,0.00019747508,0.00003954714,0.0012959851,0.0000038966355],"about_ca_topic_score_codex":0.019714018,"about_ca_topic_score_gemma":0.033393588,"teacher_disagreement_score":0.019714018,"about_ca_system_score_codex":0.00043189593,"about_ca_system_score_gemma":0.00034118525,"threshold_uncertainty_score":0.039198577},"labels":[],"label_agreement":null},{"id":"W2086471046","doi":"10.1038/nature03358","title":"Modes of faulting at mid-ocean ridges","year":2005,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":450,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Bank of Canada","funders":"National Science Foundation","keywords":"Geology; Intrusion; Plate tectonics; Mid-ocean ridge; Seismology; Transform fault; Oceanic crust; Ridge; Tectonics; Crust; Fault (geology); Subduction; Geophysics; Basalt; Paleontology; Geochemistry","score_opus":0.01042437819704805,"score_gpt":0.22833266130622537,"score_spread":0.21790828310917731,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086471046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99616253,0.000045581193,0.0009900115,0.00003643471,0.000002517731,0.0000035275514,0.00008998479,0.000021362703,0.0026481024],"genre_scores_gemma":[0.99939084,0.0000143051075,0.00016129292,0.0000017781995,0.0000021645567,9.712927e-7,0.000023744264,0.000002358735,0.00040251098],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995136,0.000006241356,0.000004467682,0.000008222295,0.000010075665,0.000019663934],"domain_scores_gemma":[0.99967015,0.000072399314,0.00008686078,0.00004479097,0.00007194188,0.000053813787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011092499,0.0001104437,0.00011421568,0.0008004897,0.00034027587,0.0005550835,0.00021070498,0.00020491582,0.0016297882],"category_scores_gemma":[0.00068072556,0.00014854343,0.00012682904,0.000392518,0.0002963182,0.00031855667,0.00030201825,0.00022625289,0.00014871462],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051882415,0.00009708694,0.84021276,0.00006583266,0.00007008546,0.001079411,0.0050231325,0.01864291,0.06618633,0.024762252,0.0014363594,0.041905046],"study_design_scores_gemma":[0.000021356855,0.000096844706,0.94958895,0.000024167737,0.00001860988,0.00065455114,0.0017527933,0.036315046,0.0026605881,0.0070583466,0.0017806505,0.000028087248],"about_ca_topic_score_codex":0.0026473112,"about_ca_topic_score_gemma":0.0043959124,"teacher_disagreement_score":0.0026473112,"about_ca_system_score_codex":0.00020733634,"about_ca_system_score_gemma":0.00011892398,"threshold_uncertainty_score":0.0054522157},"labels":[],"label_agreement":null},{"id":"W2086660433","doi":"10.1190/geo2014-0179.1","title":"Moment and moment magnitude of seismic events located by stacking","year":2014,"lang":"en","type":"article","venue":"Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Microsemi (Canada)","funders":"","keywords":"Magnitude (astronomy); Moment magnitude scale; Moment (physics); Seismic moment; Waveform; Displacement (psychology); Attenuation; Stack (abstract data type); Stacking; Noise (video); Amplitude; Geology; Mathematics; Physics; Geometry; Computer science; Seismology; Optics; Classical mechanics; Nuclear magnetic resonance","score_opus":0.007226527465231138,"score_gpt":0.188902739880473,"score_spread":0.18167621241524184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086660433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6853404,0.00021030793,0.3073324,0.00006207579,0.00006934241,0.00006567756,0.0012648007,0.0014843504,0.004170546],"genre_scores_gemma":[0.89863974,0.00009589278,0.099666044,0.000007016692,0.000039370458,0.000020472631,0.0007453299,0.00010991666,0.0006761944],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99975234,0.00003321106,0.000024679492,0.00005987205,0.000101732214,0.00002807774],"domain_scores_gemma":[0.9987276,0.00029423964,0.00041211952,0.0001571983,0.00033867455,0.00007000297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036208247,0.00043241028,0.00026514407,0.0025928507,0.00018517188,0.0006312052,0.0003699483,0.00020997877,0.0017530418],"category_scores_gemma":[0.002837002,0.00020038454,0.00026490985,0.0012776144,0.00021087803,0.0006907465,0.00046131597,0.0002782988,0.00047168127],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006239991,0.00008251616,0.12258308,0.000392866,0.00024811397,0.00068573793,0.0009437146,0.043261234,0.24709766,0.0063640415,0.0019985356,0.5757186],"study_design_scores_gemma":[0.000024657149,0.0002744749,0.51515985,0.00009417635,0.00021306297,0.0010984526,0.00057274045,0.32884404,0.13948274,0.0066924808,0.0073889247,0.00015445179],"about_ca_topic_score_codex":0.0013789369,"about_ca_topic_score_gemma":0.00226647,"teacher_disagreement_score":0.0025928507,"about_ca_system_score_codex":0.00021803904,"about_ca_system_score_gemma":0.00021586912,"threshold_uncertainty_score":0.005864501},"labels":[],"label_agreement":null},{"id":"W2087428322","doi":"10.1016/s0032-0633(00)00057-x","title":"Sound from a fireball — distinguishing between the hypersonic shock front and the terminal burst","year":2000,"lang":"en","type":"article","venue":"Planetary and Space Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mount Allison University; University of Victoria","funders":"","keywords":"Physics; Shock wave; Speed of sound; Aerospace engineering; Geology; Computational physics; Acoustics; Mechanics","score_opus":0.014034834153479146,"score_gpt":0.20053758216339168,"score_spread":0.18650274800991254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087428322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9868066,0.00055148825,0.0021315606,0.00022373786,0.00012380251,0.00004293215,0.00018459457,0.00001987232,0.00991543],"genre_scores_gemma":[0.99732375,0.00034634574,0.00095004187,0.00011432201,0.000109630084,0.000009766219,0.00018292436,0.000015522744,0.0009477298],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986184,0.000017061626,0.000011490718,0.000019298632,0.00004694828,0.000043339223],"domain_scores_gemma":[0.9985091,0.0005640131,0.00022623317,0.00008478601,0.00027784807,0.00033792784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047308416,0.00032217745,0.0002861226,0.0013513196,0.0003687327,0.0019167117,0.00036174417,0.0010923841,0.0037432276],"category_scores_gemma":[0.0052187294,0.0002496111,0.00018555879,0.00045119275,0.00069927354,0.0009965801,0.0009942979,0.00090431067,0.00095840136],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009835541,0.0004924362,0.7096501,0.00021991154,0.00011375095,0.004820309,0.0020140084,0.0010692978,0.10893047,0.0037155102,0.0019728343,0.1571658],"study_design_scores_gemma":[0.00010619116,0.00078748766,0.980029,0.00011267709,0.00007871411,0.003634936,0.0025495312,0.0036332845,0.0045743175,0.0024361205,0.0020201176,0.000037691556],"about_ca_topic_score_codex":0.002314111,"about_ca_topic_score_gemma":0.0036063744,"teacher_disagreement_score":0.0037432276,"about_ca_system_score_codex":0.00022201233,"about_ca_system_score_gemma":0.00024817092,"threshold_uncertainty_score":0.01252234},"labels":[],"label_agreement":null},{"id":"W2088738142","doi":"10.1002/2014jb011144","title":"Source scaling relations and along‐strike segmentation of slow slip events in a 3‐D subduction fault model","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Scaling; Slip (aerodynamics); Geology; Subduction; Seismology; Geometry; Physics; Mathematics; Tectonics","score_opus":0.038370950813599425,"score_gpt":0.3150976815281044,"score_spread":0.276726730714505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088738142","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97659,0.000113785325,0.018770441,0.00019245979,0.000010937219,0.000029021028,0.0007300427,0.00018895486,0.003374449],"genre_scores_gemma":[0.9981675,0.000045867222,0.0011805674,0.000010306607,0.0000034229952,0.000022086075,0.0001516684,0.000014475811,0.00040413634],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999329,0.000016391092,0.0000058336927,0.00001812516,0.000010455381,0.000016218835],"domain_scores_gemma":[0.99969316,0.00013220988,0.00007633996,0.000025558977,0.000039398692,0.00003321226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002049467,0.0005013181,0.000481403,0.000539042,0.0003653524,0.00072323397,0.00082725973,0.001157993,0.00096295535],"category_scores_gemma":[0.00076199067,0.00035081714,0.00078258995,0.00043055235,0.0005733223,0.00035566572,0.000398196,0.00048420086,0.000112655376],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015702786,0.000014153002,0.0017443972,0.0000044172616,0.000006913184,0.000031684463,0.000012574935,0.996949,0.00044592476,0.000390814,0.00004118945,0.00034318096],"study_design_scores_gemma":[0.0000032641528,0.0000043087266,0.00041109262,8.2407223e-7,0.0000019031881,0.0000028561276,0.00000324079,0.9993888,0.00004332756,0.000114270006,0.00002390809,0.0000022028094],"about_ca_topic_score_codex":0.0470305,"about_ca_topic_score_gemma":0.012736198,"teacher_disagreement_score":0.0470305,"about_ca_system_score_codex":0.0011322184,"about_ca_system_score_gemma":0.0005988785,"threshold_uncertainty_score":0.09351355},"labels":[],"label_agreement":null},{"id":"W2088931595","doi":"10.1029/2008jb005909","title":"Moment release rate of Cascadia tremor constrained by GPS","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Forearc; Episodic tremor and slip; Slip (aerodynamics); Seismic moment; Geodesy; Moment magnitude scale; Global Positioning System; Plate tectonics; Moment (physics); Tectonics; Fault (geology)","score_opus":0.028620562491143937,"score_gpt":0.2933006003162181,"score_spread":0.26468003782507415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088931595","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969649,0.00006843287,0.00089263293,0.000022536355,0.000001189578,0.0000046595405,0.00080883934,0.000054067266,0.0011827225],"genre_scores_gemma":[0.99905735,0.000026980448,0.00010798078,0.0000015157315,0.0000012100737,0.000003045745,0.0006903511,0.000008946812,0.00010263282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996247,0.000046769408,0.0000300627,0.00015884372,0.00008547029,0.000054180557],"domain_scores_gemma":[0.99893135,0.00028949004,0.00029401746,0.00021281325,0.00019027418,0.000082007624],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004972569,0.0004057805,0.0003697928,0.0010547357,0.0002507441,0.0006545553,0.0003684639,0.00023168666,0.0008122095],"category_scores_gemma":[0.0032686158,0.00030545317,0.00034047867,0.0010071122,0.0003257661,0.0003252209,0.0005489866,0.00023401085,0.0002144446],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037125908,0.000024428344,0.9123886,0.00007450903,0.00019500311,0.00030318947,0.00047376295,0.05660896,0.017642548,0.0003565658,0.0005052649,0.011055921],"study_design_scores_gemma":[0.000006051437,0.00001614283,0.97453135,0.000006342239,0.000021661524,0.00007914583,0.000048722166,0.024156742,0.0007945632,0.00006301269,0.00026302206,0.000013352737],"about_ca_topic_score_codex":0.037007272,"about_ca_topic_score_gemma":0.026602058,"teacher_disagreement_score":0.037007272,"about_ca_system_score_codex":0.00081921445,"about_ca_system_score_gemma":0.00030483236,"threshold_uncertainty_score":0.07358372},"labels":[],"label_agreement":null},{"id":"W2089613938","doi":"10.1126/science.1114576","title":"The Global Reach of the 26 December 2004 Sumatra Tsunami","year":2005,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":479,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Ridge; Geology; Submarine pipeline; Tide gauge; Seismology; Amplitude; Altimeter; Satellite altimetry; Geodesy; Satellite; Tsunami earthquake; Indian ocean; Oceanography; Sea level; Paleontology","score_opus":0.011553137381511782,"score_gpt":0.2336231849237944,"score_spread":0.22207004754228263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089613938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9816207,0.00020450477,0.0008378476,0.0003005134,0.000017425627,0.000006309994,0.002046386,0.0000381217,0.014928153],"genre_scores_gemma":[0.9966414,0.0001542548,0.000304864,0.000018066929,0.000003004683,0.000009413211,0.0013834591,0.000009171367,0.0014764527],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999634,0.0000050023573,0.0000024668266,0.0000121647345,0.000007899183,0.000009024308],"domain_scores_gemma":[0.99987817,0.000020787866,0.000034515993,0.000014788848,0.000030382766,0.000021240669],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007382808,0.00021359244,0.00014033767,0.00038483998,0.00037957449,0.00062355166,0.00012794766,0.00019375204,0.0028561088],"category_scores_gemma":[0.0007066712,0.00013392132,0.00017072995,0.0005355214,0.00021799,0.0006782128,0.00063537346,0.0003206897,0.00033275652],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000332832,0.0000890244,0.5557262,0.00025971586,0.00022801658,0.0013264235,0.0025313764,0.3095632,0.014342164,0.010194202,0.00809004,0.09731678],"study_design_scores_gemma":[0.000051143335,0.000085939675,0.8810221,0.000064853535,0.00015408333,0.0003636169,0.0015983201,0.08576484,0.0020764417,0.005375071,0.023395646,0.00004793561],"about_ca_topic_score_codex":0.03750892,"about_ca_topic_score_gemma":0.07685771,"teacher_disagreement_score":0.03750892,"about_ca_system_score_codex":0.0010852898,"about_ca_system_score_gemma":0.0006348136,"threshold_uncertainty_score":0.074581146},"labels":[],"label_agreement":null},{"id":"W2089920299","doi":"10.1007/s00024-012-0476-6","title":"Preface for “Earthquake Hazard Evaluation”","year":2012,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Geology; Seismic hazard; Earthquake prediction; Hazard","score_opus":0.02587559664809444,"score_gpt":0.24109542321603522,"score_spread":0.21521982656794078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089920299","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013655853,0.0072285975,0.031608503,0.08594579,0.50665873,0.0014904717,0.020756653,0.0027966716,0.34214893],"genre_scores_gemma":[0.008109304,0.0039353003,0.01269869,0.027475694,0.1019786,0.0010548326,0.020357937,0.0029328137,0.82145685],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988337,0.0002531213,0.00015517579,0.00014188004,0.00053165015,0.0000844879],"domain_scores_gemma":[0.9881714,0.0020817907,0.00031709173,0.0010026464,0.007770656,0.00065638736],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018832781,0.0012438507,0.0010828024,0.0029144872,0.002130413,0.0017026649,0.001642363,0.0020748551,0.3224267],"category_scores_gemma":[0.014642099,0.00039432308,0.0010234748,0.0016063887,0.00048140276,0.0024562564,0.0017708822,0.0030163128,0.2107948],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011670039,0.00001764365,0.000033075885,0.00004936924,0.0000020013886,0.000016179054,0.000010023725,0.000046088073,0.00015247369,0.0011370075,0.9869543,0.011570211],"study_design_scores_gemma":[0.000012314976,0.000024487052,0.000830085,0.00012782251,0.0000045960337,0.000046203037,0.00002906049,0.00019700636,0.00020999697,0.0038111333,0.9946972,0.000010080699],"about_ca_topic_score_codex":0.006375355,"about_ca_topic_score_gemma":0.007170636,"teacher_disagreement_score":0.3224267,"about_ca_system_score_codex":0.0014727112,"about_ca_system_score_gemma":0.0016238303,"threshold_uncertainty_score":0.9664761},"labels":[],"label_agreement":null},{"id":"W2090197264","doi":"10.1007/s11629-013-2504-0","title":"Tectonic mechanism of the Suining (Ms5.0) earthquake, center of Sichuan Basin, China","year":2013,"lang":"en","type":"article","venue":"Journal of Mountain Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Roads University","funders":"National Natural Science Foundation of China","keywords":"Geology; Seismology; Epicenter; Focal mechanism; Tectonics; Anticline; Fault (geology); Aftershock; Foreshock","score_opus":0.011654201571229152,"score_gpt":0.215344961265676,"score_spread":0.20369075969444686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090197264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986141,0.000075200755,0.00010123606,0.000093254755,0.0000051834263,0.00000862915,0.00007563157,0.000008849257,0.0010178477],"genre_scores_gemma":[0.9994918,0.00004683942,0.000038792004,0.000008776141,0.0000033397441,0.0000026104633,0.00006648798,8.650496e-7,0.000340367],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990463,0.000008342226,0.000009128964,0.00001963882,0.000021078082,0.00003709012],"domain_scores_gemma":[0.99982613,0.000015759791,0.000042157415,0.000009179413,0.000057570942,0.00004914222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023473219,0.00030004312,0.00024726233,0.0015675409,0.0011587086,0.0006738597,0.00047384572,0.0004235158,0.001529072],"category_scores_gemma":[0.00034974972,0.00026411292,0.0002681756,0.0013568276,0.00051604846,0.0003064183,0.0005094131,0.0001574756,0.000082904335],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030834682,0.00017044759,0.93090266,0.00013812285,0.00019859348,0.002070869,0.0022839415,0.016399367,0.02099134,0.005646947,0.0018206702,0.019068614],"study_design_scores_gemma":[0.000026369782,0.000065489236,0.9895845,0.000009067059,0.000060170158,0.000104049024,0.00067829597,0.007575932,0.0005747331,0.00056583155,0.0007414104,0.0000140514685],"about_ca_topic_score_codex":0.12884352,"about_ca_topic_score_gemma":0.1551911,"teacher_disagreement_score":0.12884352,"about_ca_system_score_codex":0.0014342928,"about_ca_system_score_gemma":0.002045249,"threshold_uncertainty_score":0.25618714},"labels":[],"label_agreement":null},{"id":"W2090246214","doi":"10.2118/167132-ms","title":"Structural Controls on Stress and Microseismic Response - A Horn River Basin Case Study","year":2013,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Encana (Canada); Microsemi (Canada)","funders":"","keywords":"Microseism; Geology; Borehole; Seismology; Hydraulic fracturing; Induced seismicity; Breakout; Fault (geology); Inversion (geology); Slip (aerodynamics); Tectonics; Geotechnical engineering","score_opus":0.015238704906150499,"score_gpt":0.22512054124595496,"score_spread":0.20988183633980445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090246214","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999746,0.0000025665738,0.000044950648,0.0000057102793,8.719476e-8,0.0000022262768,0.000028221106,0.0000020994005,0.00016801822],"genre_scores_gemma":[0.99982685,0.0000037888653,0.00005469295,0.0000012315411,2.2219564e-7,0.0000014986532,0.000024638694,6.887841e-7,0.00008645618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983966,0.00004026647,0.000010346532,0.00003050583,0.00003373031,0.00004546465],"domain_scores_gemma":[0.9996954,0.00008981196,0.000082012615,0.000031843636,0.000051458133,0.000049430717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022308239,0.00013538878,0.00018210667,0.00044939062,0.00031711825,0.00044744552,0.00025476437,0.00022281095,0.0007951766],"category_scores_gemma":[0.00086513977,0.00012610044,0.00014140164,0.0005412272,0.0005274465,0.00024346418,0.00040918836,0.00014703292,0.000055363555],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017188735,0.00017478809,0.9585878,0.000016478452,0.00004792945,0.0010277603,0.0007336514,0.01804415,0.010763506,0.000678694,0.00014340115,0.009609904],"study_design_scores_gemma":[0.000011660218,0.000103818114,0.9766,0.0000032163696,0.000012773067,0.00008281129,0.0008951226,0.020497452,0.0012056063,0.00022306334,0.00035529013,0.000009112078],"about_ca_topic_score_codex":0.053513177,"about_ca_topic_score_gemma":0.10109824,"teacher_disagreement_score":0.053513177,"about_ca_system_score_codex":0.0010191537,"about_ca_system_score_gemma":0.00042374438,"threshold_uncertainty_score":0.10640335},"labels":[],"label_agreement":null},{"id":"W2090376634","doi":"10.1785/0120140173","title":"Spatiotemporal Distribution of Events during the First Week of the 2012 Haida Gwaii Aftershock Sequence","year":2015,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Aftershock; Sequence (biology); Geology; Seismology; Biology","score_opus":0.027786891949374535,"score_gpt":0.21515506859074818,"score_spread":0.18736817664137365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090376634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886007,0.00019507259,0.00021496696,0.000044066623,0.0000144118485,0.000038445272,0.0063845376,0.00005249176,0.00445533],"genre_scores_gemma":[0.98799676,0.0002532235,0.00030727976,0.000019435964,0.000017385637,0.00004880677,0.009140168,0.0000101890555,0.0022066585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989176,0.0000035198495,0.000007768823,0.000033886354,0.000031444684,0.000031648906],"domain_scores_gemma":[0.9993759,0.000030026966,0.00022221758,0.000033501336,0.00020210058,0.00013640396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011608306,0.00020633452,0.00019765882,0.0017444164,0.00042007395,0.00044044375,0.00022990926,0.00014875008,0.0019320541],"category_scores_gemma":[0.0006233491,0.000101994774,0.00012875002,0.0016420863,0.00022148206,0.00024981872,0.0005074629,0.00023985168,0.00043482508],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021019127,0.000041668725,0.94830143,0.00011799301,0.00008736594,0.00037452765,0.001652704,0.0005680812,0.010964531,0.00030876233,0.0068001323,0.03057257],"study_design_scores_gemma":[9.647204e-7,0.000005597206,0.99880254,0.0000062471895,0.0000049931396,0.00003701392,0.00017047624,0.00013723844,0.000120422046,0.000006021573,0.00070550886,0.0000030491265],"about_ca_topic_score_codex":0.1752616,"about_ca_topic_score_gemma":0.43596774,"teacher_disagreement_score":0.8247384,"about_ca_system_score_codex":0.00077774015,"about_ca_system_score_gemma":0.0007689756,"threshold_uncertainty_score":0.34848297},"labels":[],"label_agreement":null},{"id":"W2090383935","doi":"10.1134/s1028334x09040333","title":"The Kuril tsunamis of November 15, 2006, and January 13, 2007: Two trans-pacific events","year":2009,"lang":"en","type":"article","venue":"Doklady Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Russian Foundation for Basic Research","keywords":"Geology; Oceanography; Seismology; Climatology","score_opus":0.014210514133271592,"score_gpt":0.23275755690323993,"score_spread":0.21854704276996834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090383935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99726874,0.00011453471,0.000053109445,0.000217132,0.0000411296,0.000015167661,0.0012253822,0.000008099988,0.0010566376],"genre_scores_gemma":[0.99516875,0.00016591941,0.00013345738,0.00007496818,0.000041053365,0.000019368414,0.0036255808,0.000007188566,0.0007637888],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997565,0.000021024713,0.000020171137,0.00004619492,0.000037636913,0.00011843315],"domain_scores_gemma":[0.99929535,0.000061813764,0.00019860624,0.000031462394,0.00017467602,0.0002381857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003042441,0.000653905,0.00038127683,0.0009708738,0.001132557,0.0010807136,0.00039087632,0.001027523,0.0021213626],"category_scores_gemma":[0.0010757928,0.00027644186,0.00042267164,0.0011382673,0.0005126609,0.00092621316,0.0018979143,0.0011052913,0.00031116002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014893071,0.00036174498,0.96983665,0.00013340404,0.0003108121,0.0026043144,0.0053802915,0.0011559594,0.0028156883,0.00040705418,0.0056069214,0.009897858],"study_design_scores_gemma":[0.000015165131,0.0000432514,0.9943011,0.000021829022,0.000051139723,0.00021247526,0.0037132313,0.0003733302,0.00014924828,0.00003563485,0.0010700471,0.000013533644],"about_ca_topic_score_codex":0.089444205,"about_ca_topic_score_gemma":0.24552695,"teacher_disagreement_score":0.089444205,"about_ca_system_score_codex":0.001072766,"about_ca_system_score_gemma":0.0011176325,"threshold_uncertainty_score":0.1778472},"labels":[],"label_agreement":null},{"id":"W2090564582","doi":"10.1016/s0040-1951(02)00607-8","title":"How soft is the crust?","year":2003,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Crust; Rheology; Geology; Lithosphere; Tectonics; Seismology; Geophysics; Petrology; Thermodynamics","score_opus":0.01857815889921929,"score_gpt":0.19926006591022966,"score_spread":0.18068190701101036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090564582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6683082,0.053489562,0.022808524,0.100699306,0.0020144978,0.000028586466,0.00095835986,0.00018178747,0.15151119],"genre_scores_gemma":[0.9827853,0.008788516,0.000777119,0.0023877728,0.00051199365,0.000005599588,0.000120722994,0.000045729732,0.004577169],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99949646,0.00015456189,0.000028661238,0.00009237043,0.0001208376,0.00010709743],"domain_scores_gemma":[0.99674726,0.001311505,0.00061008363,0.00032732516,0.00041984193,0.000584141],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009854584,0.0004536869,0.0005632508,0.0012402206,0.0008041242,0.0054943324,0.0007983354,0.002083965,0.0077285543],"category_scores_gemma":[0.011579388,0.00033576056,0.00029790594,0.0013421017,0.009431704,0.010473208,0.0020226373,0.0024550953,0.0017155315],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046324753,0.00012483214,0.08537432,0.001464797,0.00055982126,0.0015921046,0.0063454234,0.007431535,0.012597717,0.37658525,0.01630786,0.4911531],"study_design_scores_gemma":[0.000020395515,0.00009322626,0.096370034,0.0005138464,0.00012340349,0.0011779763,0.014338774,0.0021166045,0.0023723857,0.8434945,0.039272048,0.00010689851],"about_ca_topic_score_codex":0.0028639566,"about_ca_topic_score_gemma":0.0032734615,"teacher_disagreement_score":0.0077285543,"about_ca_system_score_codex":0.00091833394,"about_ca_system_score_gemma":0.00084250467,"threshold_uncertainty_score":0.025854588},"labels":[],"label_agreement":null},{"id":"W2090677076","doi":"10.1029/2004jb003510","title":"Rates and uncertainties on seismic moment and deformation in eastern Canada","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Intraplate earthquake; Geology; Seismology; Seismic hazard; Seismic moment; Induced seismicity; Lithosphere; Geodetic datum; Deformation (meteorology); Tectonics; Geodesy; Fault (geology)","score_opus":0.026818719769060386,"score_gpt":0.27895904326255133,"score_spread":0.25214032349349097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090677076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9846609,0.0007440187,0.0031982227,0.00037912538,0.000008999218,0.0000141491055,0.005349203,0.00017053893,0.0054747867],"genre_scores_gemma":[0.9963935,0.00018077747,0.00072429137,0.000019935089,0.0000019970187,0.0000037987902,0.0020838168,0.000016972406,0.0005748729],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99878854,0.00010238507,0.000087196575,0.00026841176,0.00046997794,0.00028362562],"domain_scores_gemma":[0.9938631,0.0017878652,0.00063393964,0.00039063877,0.0030301947,0.0002942021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022040987,0.00043636395,0.00039301597,0.0026292396,0.0014781941,0.0024117886,0.0012891662,0.00039456433,0.0014016979],"category_scores_gemma":[0.009659208,0.00028524612,0.00063774805,0.0033802185,0.0009628329,0.00063268415,0.0009446591,0.00043714602,0.00016747843],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032275455,0.000022486829,0.7151346,0.00008101588,0.00045809805,0.00026144466,0.0009119895,0.23380677,0.0013207122,0.007928873,0.0031426705,0.036608532],"study_design_scores_gemma":[0.000027504344,0.000016000055,0.711836,0.00008824335,0.00012279004,0.00012247369,0.00147373,0.2756546,0.0012653266,0.0032356265,0.006002468,0.0001553485],"about_ca_topic_score_codex":0.9880455,"about_ca_topic_score_gemma":0.9835767,"teacher_disagreement_score":0.029350793,"about_ca_system_score_codex":0.029350793,"about_ca_system_score_gemma":0.014221022,"threshold_uncertainty_score":0.21295589},"labels":[],"label_agreement":null},{"id":"W2091004324","doi":"10.1016/j.cageo.2007.05.013","title":"Application of DInSAR-GPS optimization for derivation of three-dimensional surface motion of the southern California region along the San Andreas fault","year":2007,"lang":"en","type":"article","venue":"Computers & Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; California Institute of Technology; Jet Propulsion Laboratory; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Geology; Global Positioning System; Geodesy; Motion (physics); Seismology; Surface (topology); Fault (geology); San andreas fault; Remote sensing; Computer science; Geometry; Artificial intelligence; Mathematics; Telecommunications","score_opus":0.017646730217932574,"score_gpt":0.21178341179361052,"score_spread":0.19413668157567793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091004324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49657348,0.00049042125,0.4652974,0.000477323,0.00012715757,0.00014741959,0.0016712819,0.002341237,0.03287434],"genre_scores_gemma":[0.9131378,0.00013723908,0.0829801,0.000054579006,0.00002321037,0.00007036156,0.00069339736,0.00023863876,0.0026646883],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99994016,0.000016682045,0.0000045622487,0.000013688344,0.000015600352,0.000009302771],"domain_scores_gemma":[0.9998431,0.00006439637,0.000017142856,0.000017255541,0.00004883657,0.000009199147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002912226,0.0005312959,0.00046675195,0.00043130477,0.00045047016,0.00051697594,0.0004651663,0.00048293395,0.0020193905],"category_scores_gemma":[0.0010125687,0.00047384418,0.00042446985,0.00042401187,0.00019672586,0.00022103733,0.00030665414,0.00035073757,0.00024390819],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018063276,0.000017266255,0.0013513218,0.000019803714,0.000014644655,0.00005982468,0.000025863988,0.9876961,0.0006277495,0.0009586978,0.00041304767,0.008797526],"study_design_scores_gemma":[0.000010102215,0.0000060095067,0.0006353006,0.0000028143381,0.000003694752,0.000005982916,0.000010809244,0.9984042,0.0002526792,0.0002411919,0.00042415562,0.000003083703],"about_ca_topic_score_codex":0.062271286,"about_ca_topic_score_gemma":0.055999067,"teacher_disagreement_score":0.062271286,"about_ca_system_score_codex":0.00050603435,"about_ca_system_score_gemma":0.0017319418,"threshold_uncertainty_score":0.12381768},"labels":[],"label_agreement":null},{"id":"W2091261697","doi":"10.1130/g20367.1","title":"Precise temperature estimation in the Tibetan crust from seismic detection of the α-β quartz transition","year":2004,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Ministry of Land and Resources of the People's Republic of China; National Natural Science Foundation of China; National Science Foundation","keywords":"Crust; Geology; Library science; History; Geophysics; Computer science","score_opus":0.007056850775541186,"score_gpt":0.19071615597334815,"score_spread":0.18365930519780696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091261697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946655,0.00043473148,0.0031582466,0.000016837676,0.0000054381176,0.0000054959214,0.00012169381,0.000021526024,0.0015705244],"genre_scores_gemma":[0.9982827,0.00014334361,0.0012339422,0.000003883551,0.0000042217544,0.0000022212569,0.00011607733,0.0000025948427,0.00021107636],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999317,0.000010477507,0.0000061454507,0.000020489095,0.000017956292,0.000013158017],"domain_scores_gemma":[0.99991846,0.000009697859,0.000028032237,0.0000064621263,0.000021328302,0.000015977452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024019773,0.00021411445,0.00011439913,0.0011344256,0.00019815133,0.00039734872,0.00017216807,0.00022275465,0.0005950913],"category_scores_gemma":[0.00036954822,0.00014553512,0.00011109638,0.00058198377,0.00024161374,0.00025981385,0.00027838454,0.000148143,0.00014491695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037243872,0.00003267046,0.49597502,0.00012785062,0.000050107814,0.00042969023,0.00081966503,0.0070590507,0.44109553,0.000891599,0.00016054208,0.052985854],"study_design_scores_gemma":[0.000012579257,0.00010844819,0.9779081,0.000018702682,0.000016102345,0.00025279872,0.00028232037,0.0071847388,0.013152754,0.0004032049,0.00064237835,0.000017938282],"about_ca_topic_score_codex":0.0046371846,"about_ca_topic_score_gemma":0.00811578,"teacher_disagreement_score":0.0046371846,"about_ca_system_score_codex":0.00024669743,"about_ca_system_score_gemma":0.00017290807,"threshold_uncertainty_score":0.009220362},"labels":[],"label_agreement":null},{"id":"W2091315108","doi":"10.1016/s0040-1951(02)00668-6","title":"Extensional shear zones as imaged by reflection seismic lines: the Larderello geothermal field (central Italy)","year":2003,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Geothermal gradient; Borehole; Seismology; Shear zone; Horizon; Crust; Shear (geology); Petrology; Brittleness; Extensional definition; Reflection (computer programming); Geophysics; Tectonics; Geometry; Geotechnical engineering","score_opus":0.011341226304006278,"score_gpt":0.22035276364576697,"score_spread":0.2090115373417607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091315108","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99707544,0.00018385689,0.0001613606,0.00003406178,0.000005340485,0.000009049684,0.0003231658,0.000037519127,0.0021702852],"genre_scores_gemma":[0.9987675,0.00012328885,0.00030682594,0.000008996916,0.000012347081,0.000007759155,0.00034130467,0.000009104851,0.00042276536],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998957,0.000012516233,0.0000047408234,0.000033935354,0.000015874024,0.0000372606],"domain_scores_gemma":[0.9998418,0.00002472149,0.00005495451,0.000018071869,0.00002829736,0.000032160227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001974057,0.00030629654,0.00022944981,0.0016758364,0.00027658502,0.0006278148,0.00031961346,0.0003872806,0.0013386186],"category_scores_gemma":[0.00042241105,0.0002524458,0.00015312346,0.0013280273,0.00051491,0.00025584587,0.00061520323,0.00019042476,0.0003145324],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019088414,0.00045423137,0.83109313,0.00026198616,0.00015312183,0.0019109779,0.005547102,0.007774507,0.08004701,0.0013486041,0.002940525,0.06655999],"study_design_scores_gemma":[0.000026609074,0.000050273924,0.997644,0.000012003477,0.000018030942,0.00010424393,0.00028895872,0.0007017263,0.00035404135,0.000034557044,0.0007599948,0.000005558671],"about_ca_topic_score_codex":0.028182246,"about_ca_topic_score_gemma":0.051795587,"teacher_disagreement_score":0.028182246,"about_ca_system_score_codex":0.0004562107,"about_ca_system_score_gemma":0.00047149966,"threshold_uncertainty_score":0.056036413},"labels":[],"label_agreement":null},{"id":"W2091527163","doi":"10.1029/2008eo420001","title":"Tremor Activity Monitoring in Northern Cascadia","year":2008,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; University of Washington","keywords":"Geology; Subduction; Seismology; North American Plate; Magnitude (astronomy); Plate tectonics; Convergent boundary; Moment magnitude scale; Slab; Margin (machine learning); Pacific Plate; Geodetic datum; Episodic tremor and slip; Oceanography; Oceanic crust; Paleontology; Geodesy; Tectonics","score_opus":0.03398153307530312,"score_gpt":0.2246408986010082,"score_spread":0.19065936552570506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091527163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98921007,0.0002544678,0.0002045217,0.00011290647,0.000010625073,0.000020578118,0.0024799388,0.00010567487,0.007601143],"genre_scores_gemma":[0.9962345,0.00019159346,0.00024829718,0.000013418121,0.000008211789,0.000016655129,0.0019147656,0.0000068669397,0.0013657955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999795,0.000019726162,0.00001778431,0.00008240378,0.00006251617,0.000022481518],"domain_scores_gemma":[0.99932396,0.000038035752,0.00014014212,0.00005443924,0.00028754474,0.00015587744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025895672,0.00029140088,0.00021573169,0.0015681678,0.00048224142,0.00031929978,0.00026094366,0.00021437,0.0010873957],"category_scores_gemma":[0.0008417147,0.00010820423,0.00014629312,0.00148096,0.00020965408,0.00018233375,0.00053402333,0.00016853878,0.00033061887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014279086,0.000031437576,0.97234523,0.00011387765,0.00006155014,0.0005244511,0.0016610917,0.0011020045,0.0055193794,0.000076712386,0.0018407813,0.016580546],"study_design_scores_gemma":[0.0000032494845,0.000019651921,0.99767977,0.000007943774,0.00001037434,0.000060728195,0.0002459384,0.00026559943,0.00017395095,0.00001611253,0.0015132432,0.0000033700983],"about_ca_topic_score_codex":0.19163226,"about_ca_topic_score_gemma":0.3644796,"teacher_disagreement_score":0.19163226,"about_ca_system_score_codex":0.0014627067,"about_ca_system_score_gemma":0.0010482316,"threshold_uncertainty_score":0.38103372},"labels":[],"label_agreement":null},{"id":"W2092958349","doi":"10.1007/s11069-014-1041-7","title":"Tsunami impact to Washington and northern Oregon from segment ruptures on the southern Cascadia subduction zone","year":2014,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Geology; Subduction; Seismology; Cape; Submarine pipeline; Oceanography; Tectonics; Geography; Archaeology","score_opus":0.008228991819042356,"score_gpt":0.21673877180529236,"score_spread":0.20850977998625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092958349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991549,0.000011494898,0.000007918099,0.000012830556,0.000002024789,0.0000023390994,0.00020113135,0.0000011451073,0.0006062634],"genre_scores_gemma":[0.9989274,0.000053135256,0.000022363301,0.00000797328,0.0000032016924,0.0000044855096,0.00058274216,0.000001319677,0.0003973462],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998958,0.000016498883,0.000013383865,0.000019044854,0.00002452547,0.000030696658],"domain_scores_gemma":[0.9995449,0.000086929285,0.00014782629,0.000030201963,0.000076211814,0.00011384978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020690702,0.00032101883,0.0002441504,0.0010755283,0.0010265029,0.0010847258,0.00031920723,0.00033529417,0.0022895574],"category_scores_gemma":[0.0010094162,0.00019347938,0.00029178287,0.001568312,0.00040781836,0.00050514226,0.0011692652,0.00041591484,0.00020159225],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006235581,0.00012884782,0.98918635,0.000023213575,0.00013768293,0.00075534196,0.00082987524,0.0014934463,0.0023216663,0.00015640463,0.00039814887,0.0039454647],"study_design_scores_gemma":[0.00001331517,0.000040783412,0.9964832,0.000014215239,0.00004733341,0.000077393015,0.0019406781,0.00062171475,0.00034193805,0.000050517414,0.0003633111,0.0000056861472],"about_ca_topic_score_codex":0.15681121,"about_ca_topic_score_gemma":0.3017749,"teacher_disagreement_score":0.15681121,"about_ca_system_score_codex":0.0010965666,"about_ca_system_score_gemma":0.00083930074,"threshold_uncertainty_score":0.3117969},"labels":[],"label_agreement":null},{"id":"W2093154009","doi":"10.1016/j.tecto.2015.04.002","title":"Reply to the comment by M.C. Alçiçek on “The Fethiye–Burdur Fault Zone: A component of upper plate extension of the subduction transform edge propagator fault linking Hellenic and Cyprus Arcs, Eastern Mediterranean,” Tectonophysics, 635, 80–99, by J. Hall, A.E. Aksu, İ. Elitez, C. Yaltirak and G. Çifçi","year":2015,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Istanbul Teknik Üniversitesi","keywords":"Geology; Seismology; Subduction; Fault (geology); Magnetotellurics; Extension (predicate logic); Kinematics; Tectonics; Engineering","score_opus":0.027947991530391108,"score_gpt":0.22612409266252811,"score_spread":0.19817610113213702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093154009","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00018421117,0.0013284561,0.00007635104,0.970251,0.027537873,0.000004988404,0.00013017982,0.000026337391,0.00046044475],"genre_scores_gemma":[0.0018139274,0.0008282085,0.00010737381,0.96844536,0.026620228,0.000020379826,0.000059833983,0.00003229248,0.0020723874],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99741447,0.0004950357,0.00038975972,0.00057767105,0.0007938884,0.00032913586],"domain_scores_gemma":[0.9856749,0.007923179,0.0010360155,0.0005001537,0.0036829023,0.0011829332],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005528384,0.0010951161,0.0014228148,0.0009007813,0.0033902798,0.003001626,0.0038171008,0.033543263,0.008099858],"category_scores_gemma":[0.028088868,0.0010801813,0.0011828443,0.0011418413,0.004520541,0.0050793523,0.0028738694,0.045852944,0.009520826],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026273867,0.0000059942527,0.00014774674,0.00004403642,0.00000766855,0.00008889242,0.000099326986,0.000017959183,0.000080281265,0.00054411835,0.9974744,0.0014632063],"study_design_scores_gemma":[0.0000900422,0.000045569108,0.0034594757,0.00029579815,0.000034237724,0.00056781183,0.0007291075,0.00017241828,0.0005950112,0.004302097,0.9896062,0.00010227142],"about_ca_topic_score_codex":0.0113602085,"about_ca_topic_score_gemma":0.013958842,"teacher_disagreement_score":0.033543263,"about_ca_system_score_codex":0.0030600983,"about_ca_system_score_gemma":0.003991404,"threshold_uncertainty_score":0.02923727},"labels":[],"label_agreement":null},{"id":"W2093813602","doi":"10.1029/2005eo170001","title":"Investigating Canada's Lithosphere and earthquake hazards with portable arrays","year":2005,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba; University of British Columbia; Carleton University; Geological Survey of Canada; University of Alberta; Natural Resources Canada; Western University","funders":"Natural Resources Canada","keywords":"Seismometer; Induced seismicity; Seismology; Geology; Broadband; Earth's magnetic field; Lithosphere; Private sector; Telecommunications; Engineering; Political science; Tectonics","score_opus":0.008392282408166111,"score_gpt":0.1812299677621674,"score_spread":0.1728376853540013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093813602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95863026,0.0005097618,0.0050739297,0.001067579,0.000031374515,0.00011944324,0.0050789574,0.00023625123,0.029252393],"genre_scores_gemma":[0.9820078,0.00067354663,0.007308944,0.00020654345,0.000021041167,0.000037436603,0.0017341177,0.000019587607,0.007990986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997527,0.000017062368,0.0000033067888,0.000032610045,0.00013036544,0.000063883366],"domain_scores_gemma":[0.9996086,0.00004341755,0.000044931272,0.000030266343,0.0002041571,0.00006869913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031039293,0.00023092623,0.000116362986,0.00061157456,0.0012032264,0.0006950013,0.00047695212,0.00020017238,0.0022712543],"category_scores_gemma":[0.0006555101,0.00011944927,0.00013212145,0.0019134451,0.00039005352,0.00032963944,0.00064830034,0.00031678344,0.00017355374],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000644268,0.00025576891,0.65769017,0.00020417439,0.0001901199,0.0007668528,0.003225761,0.00912388,0.06034581,0.005877901,0.021251798,0.24042352],"study_design_scores_gemma":[0.0000773826,0.00022941815,0.945982,0.000035546247,0.000115279516,0.00019059706,0.0037653523,0.008922131,0.010139795,0.0010768699,0.029405816,0.00005971799],"about_ca_topic_score_codex":0.9301206,"about_ca_topic_score_gemma":0.97606987,"teacher_disagreement_score":0.06987941,"about_ca_system_score_codex":0.0050902534,"about_ca_system_score_gemma":0.0063222293,"threshold_uncertainty_score":0.14058185},"labels":[],"label_agreement":null},{"id":"W2095395062","doi":"10.1007/s11069-009-9453-5","title":"Confidence levels for tsunami-inundation limits in northern Oregon inferred from a 10,000-year history of great earthquakes at the Cascadia subduction zone","year":2009,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Geology; Seismology; Seismic hazard; Slip (aerodynamics); Natural hazard; Tsunami earthquake; Tectonics; Oceanography","score_opus":0.02603866342218991,"score_gpt":0.238432417272773,"score_spread":0.2123937538505831,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095395062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975789,0.00007273067,0.00051089085,0.000082266386,0.0000045359147,0.000003028679,0.0004932637,0.000010228112,0.0012441119],"genre_scores_gemma":[0.9992016,0.000028112874,0.000108102504,0.000012418876,0.000003765843,0.0000021366156,0.0005198806,0.0000018915977,0.0001220787],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990369,0.00031331883,0.00018964913,0.00020608531,0.00013014706,0.00012400174],"domain_scores_gemma":[0.959306,0.03166821,0.005038956,0.0014959886,0.0013164844,0.001174352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0041170632,0.00022470497,0.00023829393,0.0011610333,0.00047730372,0.0016472688,0.00082525006,0.0005813052,0.00224489],"category_scores_gemma":[0.022414275,0.00019342551,0.000406905,0.00081068504,0.00082823855,0.0007399695,0.0010168353,0.00075215206,0.00017856204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005575231,0.000045071665,0.9898286,0.000020151281,0.0001940951,0.00013690135,0.00046416486,0.0044414685,0.00043227657,0.0007860991,0.00020312845,0.0028905806],"study_design_scores_gemma":[0.00005528044,0.00013087345,0.9651459,0.00008879272,0.00018076388,0.00021421515,0.0029983511,0.027329918,0.0009908222,0.0019265756,0.0009010568,0.000037450125],"about_ca_topic_score_codex":0.04222475,"about_ca_topic_score_gemma":0.036991846,"teacher_disagreement_score":0.04222475,"about_ca_system_score_codex":0.00043021943,"about_ca_system_score_gemma":0.00034879008,"threshold_uncertainty_score":0.08395797},"labels":[],"label_agreement":null},{"id":"W2095961558","doi":"10.1002/2015jb011941","title":"Recovery of secular deformation field of Mojave Shear Zone in Southern California from historical terrestrial and GPS measurements","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; McGill University; Massachusetts Institute of Technology; National Science Foundation","keywords":"Geology; Geodesy; North American Plate; Shear zone; Seismology; Global Positioning System; Shear (geology); Secular variation; Crust; Plate tectonics; Tectonics; Geophysics; Paleontology","score_opus":0.08517724420306692,"score_gpt":0.3044581269572219,"score_spread":0.21928088275415497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095961558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964095,0.00014949859,0.0003720883,0.000036870835,0.0000063995635,0.000007558362,0.0017665972,0.00008129051,0.0011702358],"genre_scores_gemma":[0.99624926,0.00011221422,0.00055881875,0.00000843478,0.0000056868244,0.000006789265,0.0024747998,0.000009398288,0.0005746009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998896,0.000008813257,0.000006809253,0.000047842215,0.0000313022,0.000015526777],"domain_scores_gemma":[0.9996283,0.000031239448,0.0001093172,0.000058230657,0.00013025019,0.000042664502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023541242,0.0002129247,0.00018588958,0.00090135913,0.00026489445,0.00057516625,0.00035352248,0.00023797719,0.00072247],"category_scores_gemma":[0.00075501873,0.00017273206,0.00013221169,0.00071378413,0.00014985197,0.0002086878,0.00025386384,0.00021730084,0.00019685608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014802058,0.000056197227,0.9530789,0.000043013144,0.00009226797,0.000074297226,0.00035231057,0.008434232,0.0029539338,0.00010098576,0.0018677511,0.032798063],"study_design_scores_gemma":[0.000006855772,0.000012580674,0.9932266,0.000012086399,0.000013394919,0.000010960539,0.00007239485,0.0053711003,0.00021743748,0.000011990398,0.0010401908,0.000004525368],"about_ca_topic_score_codex":0.19965424,"about_ca_topic_score_gemma":0.3311483,"teacher_disagreement_score":0.19965424,"about_ca_system_score_codex":0.0006105542,"about_ca_system_score_gemma":0.00043643193,"threshold_uncertainty_score":0.39698422},"labels":[],"label_agreement":null},{"id":"W2096095562","doi":"10.5194/npg-16-333-2009","title":"Recurrent frequency-size distribution of characteristic events","year":2009,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Institute for Catastrophic Loss Reduction","keywords":"Weibull distribution; Log-normal distribution; Statistics; Statistical physics; Ranging; Mathematics; Frequency distribution; Power law; Geology; Physics; Geodesy","score_opus":0.012172704546790548,"score_gpt":0.23726148005563996,"score_spread":0.22508877550884943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096095562","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9613893,0.00010900679,0.035938077,0.000038145437,0.0000094866145,0.000020898906,0.00032158996,0.00020422954,0.0019693351],"genre_scores_gemma":[0.9988238,0.000027068354,0.0006843495,0.000002619953,0.0000042222705,0.0000072037133,0.00021050249,0.000011546927,0.00022878655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996698,0.000044188724,0.00002501444,0.00011637339,0.00010379248,0.000040797797],"domain_scores_gemma":[0.99601436,0.0016711999,0.00095066807,0.0004712874,0.000703264,0.00018921569],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007084166,0.00019337646,0.0002058519,0.0010245919,0.00016353065,0.00039996504,0.00047871255,0.00033120692,0.0021484175],"category_scores_gemma":[0.0052370997,0.00012729854,0.00026089564,0.0005571348,0.00040473952,0.0006093479,0.00031755783,0.00027619713,0.00028327073],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00068567344,0.00021431137,0.44435352,0.00034911328,0.00021633731,0.001993108,0.0012548215,0.2954203,0.11685003,0.0368951,0.0017670945,0.10000058],"study_design_scores_gemma":[0.000023965993,0.00033948716,0.3245375,0.00003640422,0.00007599761,0.001813522,0.00028440027,0.6437152,0.018208753,0.00843521,0.0024460903,0.00008355521],"about_ca_topic_score_codex":0.0007397615,"about_ca_topic_score_gemma":0.00040923693,"teacher_disagreement_score":0.0021484175,"about_ca_system_score_codex":0.00041273085,"about_ca_system_score_gemma":0.00014967575,"threshold_uncertainty_score":0.0071871877},"labels":[],"label_agreement":null},{"id":"W2096570870","doi":"10.1144/sp347.8","title":"Variation in fluid contacts in the Azeri field, Azerbaijan: sealing faults or hydrodynamic aquifer?","year":2010,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"BP (Canada)","funders":"","keywords":"Aquifer; Geology; Field (mathematics); Variation (astronomy); Geotechnical engineering; Petroleum engineering; Petrology; Groundwater; Physics; Mathematics","score_opus":0.019744280188191556,"score_gpt":0.24457811256773782,"score_spread":0.22483383237954627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096570870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846673,0.000106825704,0.000044144806,0.00002025154,0.0000023465316,0.000003633915,0.00019523686,0.000004589123,0.001156191],"genre_scores_gemma":[0.9994649,0.000047584923,0.000076539516,0.0000049648884,0.000002638988,0.0000021902322,0.00018965622,0.0000010484964,0.0002105424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983597,0.00002028943,0.000012011143,0.000050214094,0.000032343665,0.00004919658],"domain_scores_gemma":[0.99980396,0.000027870403,0.00006766675,0.000012825295,0.000060269755,0.000027386759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022080753,0.00020171146,0.0002641217,0.0017316632,0.0005017804,0.00070690527,0.00031507292,0.00022655963,0.0015415692],"category_scores_gemma":[0.00043368357,0.000121194804,0.000120838464,0.0017688493,0.00058302144,0.0003221956,0.0004028756,0.00014098777,0.00019569503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019776876,0.00006966497,0.9666705,0.00004719332,0.000075108095,0.00050171866,0.0015052013,0.001086207,0.009676453,0.00041351785,0.00036168005,0.019394848],"study_design_scores_gemma":[0.0000025926656,0.000010101975,0.99900913,0.0000035975177,0.0000037716334,0.000032422402,0.0003725079,0.00014988694,0.000116701114,0.000013206621,0.00028402935,0.0000020574182],"about_ca_topic_score_codex":0.13559519,"about_ca_topic_score_gemma":0.16084214,"teacher_disagreement_score":0.13559519,"about_ca_system_score_codex":0.0014081696,"about_ca_system_score_gemma":0.00065169786,"threshold_uncertainty_score":0.2696119},"labels":[],"label_agreement":null},{"id":"W2097136530","doi":"10.1111/j.1365-246x.2005.02523.x","title":"Earthquake rate, slip rate, and the effective seismic thickness for oceanic transform faults of the Juan de Fuca plate system","year":2005,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Seismic moment; Geology; Seismology; Induced seismicity; Slip (aerodynamics); Magnitude (astronomy); Deformation (meteorology); Fault (geology); Transform fault; Seismic gap; Geodesy","score_opus":0.006604767171123582,"score_gpt":0.21577893904649986,"score_spread":0.2091741718753763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097136530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999108,0.000057837045,0.00011872837,0.0000084771955,6.590317e-7,0.0000014852982,0.00015229665,0.00000583894,0.0005465465],"genre_scores_gemma":[0.9996654,0.000027640084,0.00006725685,0.0000010233364,9.132565e-7,0.0000010179527,0.00015550375,0.0000023868758,0.00007885733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981314,0.000050370018,0.000018849096,0.00003165846,0.000042588847,0.00004351071],"domain_scores_gemma":[0.9985085,0.00079960085,0.00035594052,0.00011219851,0.00014346879,0.0000802947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082858896,0.00027537625,0.00022369775,0.0013518886,0.00017636569,0.00046518203,0.00015849348,0.00019361611,0.0008077429],"category_scores_gemma":[0.0033699165,0.00012395604,0.00029568071,0.00085765385,0.0003860943,0.00029772648,0.0002337281,0.0001663145,0.000102261234],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003831232,0.000026724421,0.9374301,0.000058211284,0.00013363217,0.0003734538,0.00021512098,0.04295446,0.006895465,0.0006034276,0.00014119863,0.010785061],"study_design_scores_gemma":[0.000005903764,0.000042927517,0.9829039,0.000006993117,0.000023304434,0.00012468381,0.000088841996,0.015774878,0.0006893684,0.00017145039,0.00015685499,0.000010866826],"about_ca_topic_score_codex":0.012226512,"about_ca_topic_score_gemma":0.0124842785,"teacher_disagreement_score":0.012226512,"about_ca_system_score_codex":0.0006266834,"about_ca_system_score_gemma":0.00024187076,"threshold_uncertainty_score":0.024310708},"labels":[],"label_agreement":null},{"id":"W2097199879","doi":"10.1016/j.jsg.2006.03.022","title":"Networking of shear zones at the brittle-to-viscous transition (Cap de Creus, NE Spain)","year":2006,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":127,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mylonite; Geology; Shearing (physics); Shear zone; Shear (geology); Petrology; Overprinting; Seismology; Geotechnical engineering; Metamorphic rock; Tectonics","score_opus":0.00911002815024685,"score_gpt":0.2105497210716902,"score_spread":0.20143969292144334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097199879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98810834,0.00018705205,0.0004250163,0.00015823448,0.000009696179,0.000013642063,0.00022871129,0.000022982977,0.010846363],"genre_scores_gemma":[0.9977053,0.000047690195,0.00028082705,0.0000105755535,0.0000027707422,0.0000055014366,0.00016694305,0.0000040432956,0.0017763684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987507,0.000014138002,0.0000047940102,0.000028612574,0.000015530786,0.00006187534],"domain_scores_gemma":[0.99954,0.000066266955,0.000088064,0.000024367979,0.00013896439,0.00014237846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024206175,0.00009765476,0.00012136967,0.0010838158,0.00070794043,0.0016108135,0.00040636328,0.0003708705,0.004402637],"category_scores_gemma":[0.0013621936,0.000091310525,0.00007584984,0.00081594964,0.00047028836,0.00049602176,0.0010845445,0.00016321457,0.00033221542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026573725,0.00028729622,0.7525824,0.00015923142,0.000092193695,0.0021908798,0.008722567,0.019584177,0.012224157,0.059113603,0.010190827,0.13219538],"study_design_scores_gemma":[0.0000886966,0.00014085215,0.93062717,0.000120136916,0.00005029346,0.00026399124,0.008596708,0.013050302,0.002041397,0.007212806,0.037781417,0.000026260106],"about_ca_topic_score_codex":0.03477597,"about_ca_topic_score_gemma":0.052619763,"teacher_disagreement_score":0.03477597,"about_ca_system_score_codex":0.0015316906,"about_ca_system_score_gemma":0.0009178625,"threshold_uncertainty_score":0.06914711},"labels":[],"label_agreement":null},{"id":"W2097606516","doi":"10.1111/j.1365-246x.2010.04734.x","title":"Near real-time simulations of global CMT earthquakes","year":2010,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Seismogram; Geology; Seismology; Seismometer; Slowness; Geodesy","score_opus":0.009019186803316667,"score_gpt":0.2459405822787008,"score_spread":0.23692139547538413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097606516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.723258,0.0002236826,0.23438993,0.00049097155,0.000271988,0.00021853954,0.004484113,0.012475581,0.024187177],"genre_scores_gemma":[0.9282752,0.000092985574,0.06565623,0.000071005314,0.000024046678,0.00015885239,0.0025302158,0.0004982561,0.0026931695],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997539,0.0000622646,0.000015331952,0.00005140753,0.0000855789,0.000031439453],"domain_scores_gemma":[0.9995073,0.0001783237,0.000041584077,0.00006716135,0.00013081935,0.00007484563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054804236,0.00052150775,0.000492154,0.0004546989,0.0002997009,0.0005687182,0.0011121236,0.00062152697,0.005261496],"category_scores_gemma":[0.0016766295,0.00028313897,0.00040887872,0.0004974455,0.00038215928,0.0007032489,0.00072814093,0.0005481813,0.000633047],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016402236,0.0000843489,0.0036746257,0.00006266347,0.000038273538,0.00012119605,0.00011690399,0.9729207,0.0053492696,0.0017182005,0.0028521302,0.012897642],"study_design_scores_gemma":[0.000034665325,0.000034952172,0.00074109004,0.0000027946314,0.0000042357824,0.000016338707,0.000019602616,0.99613,0.0012659286,0.0004086368,0.0013346144,0.0000072056523],"about_ca_topic_score_codex":0.0044466397,"about_ca_topic_score_gemma":0.0041308342,"teacher_disagreement_score":0.005261496,"about_ca_system_score_codex":0.0005347553,"about_ca_system_score_gemma":0.0005818107,"threshold_uncertainty_score":0.01760149},"labels":[],"label_agreement":null},{"id":"W2098465108","doi":"10.1785/gssrl.83.1.179","title":"CCSC: A Composite Seismicity Catalog for Earthquake Hazard Assessment in Major Canadian Cities","year":2012,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Induced seismicity; Seismology; Geology; Hazard; Seismic hazard; Hazard analysis; Engineering","score_opus":0.07735104644619292,"score_gpt":0.32662331310410336,"score_spread":0.24927226665791044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098465108","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04549511,0.00069643476,0.008133029,0.0006594143,0.00008411717,0.00086765416,0.9064229,0.001725013,0.035916325],"genre_scores_gemma":[0.14055079,0.0019674094,0.03495514,0.0002128336,0.000054148662,0.0007442631,0.796796,0.00049012597,0.024229283],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9988838,0.00004244344,0.00008244905,0.00011146816,0.00065614143,0.00022376694],"domain_scores_gemma":[0.99219733,0.00013320122,0.00039086933,0.00032251255,0.00635031,0.00060568587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009381728,0.0009091222,0.00041058153,0.015715536,0.0021831673,0.0014592953,0.001772632,0.00029790506,0.01534901],"category_scores_gemma":[0.004635536,0.000409248,0.000597989,0.022057986,0.0003526228,0.0010598586,0.0015741788,0.00047500207,0.0035969114],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020745603,0.0001053298,0.14100036,0.0006832414,0.00012546417,0.00018987591,0.0010839035,0.0063730795,0.001764765,0.011983039,0.6477107,0.18877284],"study_design_scores_gemma":[0.000054664863,0.000027559403,0.39612937,0.0002311658,0.00010266901,0.00012298152,0.0011303811,0.0058000744,0.0012765885,0.0015245322,0.5934586,0.00014137481],"about_ca_topic_score_codex":0.9920855,"about_ca_topic_score_gemma":0.99475795,"teacher_disagreement_score":0.02361146,"about_ca_system_score_codex":0.02361146,"about_ca_system_score_gemma":0.083123855,"threshold_uncertainty_score":0.17131388},"labels":[],"label_agreement":null},{"id":"W2099104873","doi":"10.1139/cgj-2014-0435","title":"Discrete element modeling of fluid injection–induced seismicity and activation of nearby fault","year":2015,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Korea Institute of Energy Technology Evaluation and Planning; Bundesministerium für Wirtschaft und Energie","keywords":"Induced seismicity; Geothermal gradient; Geology; Fluid pressure; Seismology; Pore water pressure; Geotechnical engineering; Slip (aerodynamics); Geomechanics; Discrete element method; Fault (geology); Fluid dynamics; Permeability (electromagnetism); Petrology; Geophysics; Mechanics; Engineering","score_opus":0.03582352668691158,"score_gpt":0.2362969038351273,"score_spread":0.20047337714821573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099104873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5771464,0.00025888137,0.39628708,0.00049843185,0.00013084483,0.00015406354,0.0007718193,0.0006474232,0.024105024],"genre_scores_gemma":[0.9749765,0.00012209282,0.01803881,0.00005004309,0.000013254461,0.00011928071,0.00021394023,0.000056652956,0.0064093717],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998915,0.000024475505,0.000006955881,0.00002010512,0.000036797876,0.00002017217],"domain_scores_gemma":[0.9996817,0.00015415887,0.000052142004,0.000022956981,0.0000564868,0.000032537217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025071637,0.00051700557,0.0006252132,0.0005467145,0.00038926382,0.0008206837,0.000962855,0.0015757701,0.0022291583],"category_scores_gemma":[0.0007820756,0.0005166065,0.0005626807,0.0003500751,0.0007902175,0.0004426031,0.0005436313,0.00066000794,0.00027837127],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018832767,0.000023805393,0.0005404706,0.000012273393,0.000007231578,0.000028166483,0.000028335598,0.9959286,0.0015210728,0.0007445922,0.000054184155,0.0010923987],"study_design_scores_gemma":[0.0000024544736,0.000003910592,0.00006583918,0.0000011043655,0.0000012078157,0.0000019556942,0.0000056068166,0.9995734,0.0001770633,0.000093722374,0.00007234655,0.0000013707256],"about_ca_topic_score_codex":0.018040534,"about_ca_topic_score_gemma":0.012607954,"teacher_disagreement_score":0.018040534,"about_ca_system_score_codex":0.00079392653,"about_ca_system_score_gemma":0.0010120093,"threshold_uncertainty_score":0.03587109},"labels":[],"label_agreement":null},{"id":"W2099196030","doi":"10.1785/gssrl.81.6.878","title":"Probabilities of Significant Earthquake Shaking in San Francisco Bay Area Communities","year":2010,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"U.S. Geological Survey","keywords":"Bay; Agency (philosophy); Citation; Icon; Geography; History; Library science; Archaeology; Sociology; Computer science; Social science","score_opus":0.08973300955816708,"score_gpt":0.302006794457152,"score_spread":0.2122737848989849,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099196030","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99781287,0.00007329271,0.00006432423,0.00012633746,0.0000041839276,0.000013109965,0.0005173771,0.000007955533,0.0013806166],"genre_scores_gemma":[0.99937975,0.00004768048,0.00003573774,0.000011215187,0.000007096864,0.000004561244,0.000278447,9.136366e-7,0.00023455774],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99961215,0.00009966173,0.00003232893,0.00010124431,0.00007126056,0.000083455656],"domain_scores_gemma":[0.988531,0.0051442105,0.0030495042,0.00047739517,0.0009847337,0.0018131208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009826832,0.0001610776,0.00021242788,0.0017040889,0.0005820218,0.00075657666,0.00046714008,0.0004610012,0.0053482354],"category_scores_gemma":[0.0083008455,0.0002625245,0.0003011588,0.00070700195,0.00035699006,0.00054210355,0.0006174339,0.0004830576,0.00019615346],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021094116,0.00005095622,0.9950293,0.000007941522,0.000045565826,0.00008964169,0.00018804487,0.0011973201,0.00004856947,0.0001320056,0.0005661835,0.0024336658],"study_design_scores_gemma":[0.00002520114,0.00007628352,0.99330753,0.000013890646,0.000036312347,0.00012512399,0.0011851062,0.0047281687,0.000052821713,0.00019624019,0.00024262258,0.00001067691],"about_ca_topic_score_codex":0.14192459,"about_ca_topic_score_gemma":0.16198213,"teacher_disagreement_score":0.14192459,"about_ca_system_score_codex":0.0008385613,"about_ca_system_score_gemma":0.000706278,"threshold_uncertainty_score":0.282197},"labels":[],"label_agreement":null},{"id":"W2099392746","doi":"10.1139/e04-063","title":"Seismicity in the vicinity of the SNORCLE corridors of the northern Canadian Cordillera","year":2005,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Induced seismicity; Geology; Seismology; Magnitude (astronomy); Epicenter; Tectonics; Lithosphere; Active fault; Moment magnitude scale; Focal mechanism; Earthquake swarm; Thrust fault; Volcano; Plate tectonics; Intraplate earthquake","score_opus":0.020474565906313275,"score_gpt":0.20088307000821898,"score_spread":0.1804085041019057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099392746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965749,0.00028027542,0.000027369839,0.00009319657,0.0000033889787,0.000007962335,0.0004885581,0.0000078159665,0.0025165486],"genre_scores_gemma":[0.99817705,0.00023311187,0.00008504995,0.000016114258,0.0000027155368,0.0000039140696,0.00034544594,0.0000018758648,0.001134682],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985397,0.000008221777,0.0000057629263,0.000033011886,0.000042349275,0.000056792294],"domain_scores_gemma":[0.9997602,0.000014981255,0.00004450031,0.000007342604,0.00011209826,0.000060853086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012166283,0.00023155149,0.00014892167,0.0013187828,0.0017274003,0.00070651865,0.00032966555,0.0002500251,0.0012866841],"category_scores_gemma":[0.00070653454,0.00009324013,0.00011136632,0.0022679835,0.00050331565,0.0001637555,0.000549573,0.00018772276,0.00010066772],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016469177,0.000023002483,0.9526795,0.00007386482,0.000055330165,0.00078063767,0.0049600834,0.0010825917,0.003454854,0.0004524525,0.0013379001,0.034935076],"study_design_scores_gemma":[0.0000023622495,0.000011363847,0.99618995,0.000009576129,0.000007632135,0.00005087845,0.0018176262,0.00021224056,0.00008405816,0.000018337932,0.0015894151,0.000006516181],"about_ca_topic_score_codex":0.98815244,"about_ca_topic_score_gemma":0.9963642,"teacher_disagreement_score":0.011847556,"about_ca_system_score_codex":0.010790862,"about_ca_system_score_gemma":0.0070015374,"threshold_uncertainty_score":0.07829362},"labels":[],"label_agreement":null},{"id":"W2099436744","doi":"10.1016/j.margeo.2008.04.008","title":"Miocene–Recent evolution of Anaximander Mountains and Finike Basin at the junction of Hellenic and Cyprus Arcs, eastern Mediterranean","year":2008,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Paleontology; Late Miocene; Sinistral and dextral; Syncline; Clockwise; Transpression; Quaternary; Neogene; Tectonics; Magnetostratigraphy; Fold (higher-order function); Seismology; Paleomagnetism; Structural basin","score_opus":0.01967823210503362,"score_gpt":0.19938779138874768,"score_spread":0.17970955928371407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099436744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99898916,0.00015997418,0.000014857655,0.000027951137,0.0000024436945,0.0000011701605,0.00008888336,0.0000014990579,0.00071405177],"genre_scores_gemma":[0.9994499,0.00007179179,0.000024946123,0.0000058592645,0.0000041507224,0.0000012711831,0.00012236688,8.815882e-7,0.0003188001],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999925,0.000008429253,0.000005639414,0.000028383667,0.000007635631,0.000024933286],"domain_scores_gemma":[0.9998406,0.000017605113,0.000056232282,0.0000088917595,0.000037876696,0.00003874043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017476582,0.00011458058,0.000103473445,0.0008642652,0.00049172377,0.00055845757,0.0003353642,0.0002826691,0.002133859],"category_scores_gemma":[0.00038190707,0.00010830022,0.00010798766,0.00063672324,0.00037585024,0.00033774495,0.00038411134,0.00014436609,0.00016844495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002258146,0.000037744856,0.9753425,0.00005855423,0.00009104934,0.0009507073,0.0044742133,0.00048790587,0.0053596017,0.0007935866,0.00054548547,0.011632817],"study_design_scores_gemma":[9.841852e-7,0.0000040780005,0.9991629,0.000003108163,0.000003736282,0.00004738052,0.00024866348,0.00003552724,0.000041404564,0.000008889971,0.00044253384,7.79192e-7],"about_ca_topic_score_codex":0.031714737,"about_ca_topic_score_gemma":0.07229647,"teacher_disagreement_score":0.031714737,"about_ca_system_score_codex":0.0006602621,"about_ca_system_score_gemma":0.00032642428,"threshold_uncertainty_score":0.06306028},"labels":[],"label_agreement":null},{"id":"W2099695915","doi":"10.1139/cjes-2014-0162","title":"Investigation of regional seismicity before and after hydraulic fracturing in the Horn River Basin, northeast British Columbia","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; British Columbia Oil and Gas Commission; U.S. Department of Energy","keywords":"Induced seismicity; Geology; Seismology; Seismogram; Seismometer; Tectonics; Hydraulic fracturing; Structural basin; Drainage basin; Magnitude (astronomy); French horn; Geomorphology; Geotechnical engineering; Geography","score_opus":0.0244524218907891,"score_gpt":0.19316413553802486,"score_spread":0.16871171364723575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099695915","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970132,0.00023948503,0.000053848406,0.000059001308,0.0000037587747,0.000014209893,0.00095818186,0.000009197497,0.00164911],"genre_scores_gemma":[0.9967841,0.00027516994,0.00013027643,0.000042703676,0.000004201546,0.000014597944,0.0011243911,0.000007898782,0.0016167777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996482,0.000022729806,0.000026820466,0.000086605025,0.00009141218,0.00012427468],"domain_scores_gemma":[0.99864644,0.000091391754,0.00024968857,0.00005629806,0.0006698973,0.00028630978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002254602,0.00028865517,0.00035707562,0.0032042207,0.0013443244,0.001208414,0.0006834268,0.00039161913,0.0014404737],"category_scores_gemma":[0.0013032816,0.0002570503,0.00016451816,0.004617374,0.0006139287,0.00028939944,0.00074552116,0.00034824453,0.00022479586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006103687,0.000024270803,0.980082,0.000059088656,0.000053527743,0.0006714521,0.002040177,0.00029510705,0.003378357,0.000059610393,0.000692299,0.012583203],"study_design_scores_gemma":[8.652183e-7,0.0000032839218,0.9985195,0.000008471167,0.0000060093403,0.000028811624,0.0008380464,0.00007091678,0.000045563338,0.00000274008,0.00047234775,0.0000034538964],"about_ca_topic_score_codex":0.9554568,"about_ca_topic_score_gemma":0.9899031,"teacher_disagreement_score":0.044543207,"about_ca_system_score_codex":0.0067892987,"about_ca_system_score_gemma":0.0059437365,"threshold_uncertainty_score":0.089610994},"labels":[],"label_agreement":null},{"id":"W2099735302","doi":"10.1029/2005jb004094","title":"Accretionary prisms in subduction earthquake cycles: The theory of dynamic Coulomb wedge","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":442,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Forearc; Accretionary wedge; Geology; Subduction; Wedge (geometry); Seismology; Coulomb; Fault (geology); Tectonics; Petrology; Geometry; Physics","score_opus":0.023685312463455187,"score_gpt":0.28847599979863897,"score_spread":0.2647906873351838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099735302","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.37628046,0.0076547884,0.5378413,0.001662924,0.00044105414,0.00005746163,0.00027367997,0.00025329107,0.07553502],"genre_scores_gemma":[0.98074806,0.0018750937,0.011074543,0.00008144624,0.00017100565,0.000028960676,0.000052545438,0.000041105202,0.0059271883],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99992,0.000018006633,0.0000048098327,0.000011381829,0.000030274214,0.000015527086],"domain_scores_gemma":[0.9997999,0.000053594333,0.000053207386,0.000020806825,0.000032126576,0.000040338393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024585682,0.00031284333,0.00030380033,0.0006040052,0.0003148564,0.00075626676,0.0010324622,0.00053761376,0.0019843264],"category_scores_gemma":[0.0010531865,0.00017347136,0.00040334155,0.0005281191,0.0011023686,0.0012978727,0.0010604267,0.00048196106,0.00032797054],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022282948,0.00003356926,0.0021645955,0.00008853335,0.000019577788,0.00079621497,0.0002710242,0.20536064,0.0022441575,0.7651906,0.0018361576,0.021972578],"study_design_scores_gemma":[0.000014031427,0.000040731786,0.0013239008,0.000031198764,0.000009974616,0.00036039916,0.00012156218,0.5366546,0.00033232124,0.45603237,0.005054743,0.000024186282],"about_ca_topic_score_codex":0.0016367814,"about_ca_topic_score_gemma":0.00089299586,"teacher_disagreement_score":0.0019843264,"about_ca_system_score_codex":0.00040881152,"about_ca_system_score_gemma":0.00030087956,"threshold_uncertainty_score":0.006638229},"labels":[],"label_agreement":null},{"id":"W2099863129","doi":"10.5194/nhess-9-847-2009","title":"The tsunami geomorphology of coastal dunes","year":2009,"lang":"en","type":"article","venue":"Natural hazards and earth system sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Pontificia Universidad Católica de Valparaíso; Simon Fraser University","keywords":"Geology; Coastal geography; Geomorphology; Bay; Tsunami wave; Oceanography; Seismology; Shore","score_opus":0.009567983869323147,"score_gpt":0.22136774227533138,"score_spread":0.21179975840600823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099863129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979,0.00011785368,0.00014810286,0.000028805092,0.00000303876,0.0000058660676,0.00025472982,0.000006494854,0.0015350963],"genre_scores_gemma":[0.99904376,0.000100772835,0.000100356025,0.0000037619031,0.0000020834527,0.000002613806,0.00017003625,0.0000021361927,0.00057457393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999479,0.000007989475,0.0000056971303,0.000008242271,0.000017009967,0.000013050279],"domain_scores_gemma":[0.999716,0.00003726442,0.00009815704,0.000018775614,0.000078198536,0.000051545634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009832707,0.00011473528,0.00008721294,0.0016907275,0.00034539576,0.00065094774,0.00008261753,0.000081224614,0.0013974207],"category_scores_gemma":[0.0005026715,0.000098321165,0.000097761535,0.0011144679,0.00035438128,0.00021067666,0.000276885,0.000088885936,0.00012824094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000100705896,0.000014095932,0.9562473,0.00005924815,0.000041792162,0.0009103731,0.0011068257,0.001041536,0.009739595,0.00046360487,0.000683297,0.029591512],"study_design_scores_gemma":[7.2589626e-7,0.000007724514,0.9986895,0.0000029248934,0.0000021826215,0.00016643338,0.0003507779,0.00017225354,0.00007493545,0.00002955111,0.0005015525,0.0000014865759],"about_ca_topic_score_codex":0.028243875,"about_ca_topic_score_gemma":0.05724245,"teacher_disagreement_score":0.028243875,"about_ca_system_score_codex":0.0004727877,"about_ca_system_score_gemma":0.00018731422,"threshold_uncertainty_score":0.05615896},"labels":[],"label_agreement":null},{"id":"W2100245639","doi":"10.1144/0016-76492009-136","title":"Tectonic significance of present-day stress relief phenomena in formerly glaciated regions","year":2010,"lang":"en","type":"article","venue":"Journal of the Geological Society","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Tectonics; Geochemistry; Paleontology; Present day; Paleozoic; Stress (linguistics); Stress relief; Earth science; Geomorphology; Physical geography; Geography","score_opus":0.01685108693479903,"score_gpt":0.22259987626748082,"score_spread":0.2057487893326818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100245639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992949,0.00006954294,0.000030016201,0.000011259029,0.0000011558362,9.15993e-7,0.00005640638,0.0000024584604,0.0005333501],"genre_scores_gemma":[0.999889,0.000016832622,0.000019294206,0.0000017457938,7.040096e-7,4.010836e-7,0.000043143813,2.8249536e-7,0.00002852225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994683,0.0000060240295,0.0000045577517,0.000010704555,0.000009881936,0.000022042612],"domain_scores_gemma":[0.99986064,0.000021002532,0.000044359233,0.000010854061,0.000037307153,0.000025865826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015759323,0.00008123895,0.00008896386,0.00049852947,0.0003888017,0.000349977,0.00013202826,0.00014632172,0.00071008515],"category_scores_gemma":[0.0004060202,0.000074174066,0.00007521879,0.00037417427,0.00054833444,0.00014595663,0.00022410911,0.00008749766,0.00006358474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008699875,0.000015328567,0.9830519,0.000027960648,0.000019296242,0.00019334604,0.00084021984,0.00091312744,0.008914549,0.00017225638,0.00008822126,0.00567676],"study_design_scores_gemma":[0.0000010414509,0.000007665068,0.99954623,0.0000019485017,0.0000017773332,0.000026969872,0.00010303666,0.00009389776,0.00010247026,0.000014859363,0.00009920853,7.333066e-7],"about_ca_topic_score_codex":0.050371274,"about_ca_topic_score_gemma":0.114692934,"teacher_disagreement_score":0.050371274,"about_ca_system_score_codex":0.0008136569,"about_ca_system_score_gemma":0.00037588555,"threshold_uncertainty_score":0.10015619},"labels":[],"label_agreement":null},{"id":"W2100408536","doi":"10.1111/j.1365-246x.2007.03511.x","title":"Simultaneous iterative time-domain sparse deconvolution to teleseismic receiver functions","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Deconvolution; Algorithm; Computer science; Time domain; Compressed sensing; Multiple; Cauchy distribution; Domain (mathematical analysis); Blind deconvolution; Iterative method; Geology; Mathematics; Statistics; Computer vision; Mathematical analysis","score_opus":0.01012381843342613,"score_gpt":0.2348924248072941,"score_spread":0.22476860637386797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100408536","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00803224,0.000022882125,0.9914948,0.000017576956,0.000006926393,0.00001043081,0.000008740014,0.00014277127,0.00026368516],"genre_scores_gemma":[0.113577686,0.00009433834,0.8851086,0.000031857675,0.00003624021,0.000047772384,0.00010351716,0.00006391024,0.00093610486],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995283,0.00010342566,0.000024795232,0.00007080439,0.00023172224,0.000041019768],"domain_scores_gemma":[0.99878937,0.00052176457,0.00013424704,0.00016892988,0.00034991838,0.000035703586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008185,0.00088287296,0.00060441723,0.0007066564,0.00031327517,0.0004963805,0.00083938875,0.0007243393,0.0011174111],"category_scores_gemma":[0.0034259488,0.0003657425,0.00075285725,0.0007061721,0.00060007954,0.0011492684,0.00106113,0.0007020968,0.00053523615],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029042197,0.00013354239,0.0016889399,0.00020484281,0.00014224462,0.0001930325,0.00031679615,0.44734773,0.12206335,0.01626989,0.0010519976,0.4102972],"study_design_scores_gemma":[0.0000134289685,0.000042299813,0.00024674498,0.0000048052816,0.000011659515,0.000075936616,0.000015605174,0.97801834,0.01809972,0.002640085,0.0008174313,0.000013891091],"about_ca_topic_score_codex":0.002280721,"about_ca_topic_score_gemma":0.0032447185,"teacher_disagreement_score":0.002280721,"about_ca_system_score_codex":0.0002982313,"about_ca_system_score_gemma":0.00085714326,"threshold_uncertainty_score":0.0045349},"labels":[],"label_agreement":null},{"id":"W2100446713","doi":"10.1111/j.1365-246x.2007.03546.x","title":"Radial resolving power of far-field differential sea-level highstands in the inference of mantle viscosity","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Post-glacial rebound; Lithosphere; Geophysics; Mantle convection; Geodesy; Seismology; Sea level; Tectonics","score_opus":0.02248855868727909,"score_gpt":0.2666520039561383,"score_spread":0.24416344526885922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100446713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9825051,0.00020050076,0.015397591,0.00009652158,0.0000055920154,0.0000063500197,0.00009901995,0.00008627461,0.0016029915],"genre_scores_gemma":[0.99565685,0.000038143564,0.00410212,0.000015045204,0.0000072049506,0.0000028025763,0.00009855671,0.000016371943,0.00006277863],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99891067,0.00056677655,0.00007064089,0.00020739518,0.00013920268,0.00010534319],"domain_scores_gemma":[0.99480826,0.0035969499,0.000600041,0.00044571195,0.0003891716,0.00015985132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0052681165,0.0005356881,0.00049386406,0.0014822198,0.00047407908,0.0016221012,0.0007536964,0.00041246004,0.00050690817],"category_scores_gemma":[0.018795623,0.00057944236,0.00046203684,0.001078842,0.0007330435,0.0012968959,0.0014175822,0.00068853254,0.00022703297],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010178947,0.00017791515,0.6438483,0.00017414032,0.0005233932,0.0005081689,0.00307566,0.1418054,0.08167713,0.014742759,0.00071069616,0.11173858],"study_design_scores_gemma":[0.000105193736,0.000093572045,0.32796893,0.000057008998,0.00017446099,0.00021434772,0.0005088229,0.63990253,0.014380576,0.015225732,0.0012063679,0.00016234917],"about_ca_topic_score_codex":0.009620077,"about_ca_topic_score_gemma":0.010713935,"teacher_disagreement_score":0.009620077,"about_ca_system_score_codex":0.0004801262,"about_ca_system_score_gemma":0.00054752105,"threshold_uncertainty_score":0.02786076},"labels":[],"label_agreement":null},{"id":"W2100649517","doi":"10.1002/2015tc003931","title":"Tectonic reversal of the western Doruneh Fault System: Implications for Central Asian tectonics","year":2015,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Geological Survey and Mineral Exploration of Iran; Tarbiat Modares University","keywords":"Sinistral and dextral; Geology; Neogene; Seismology; Strike-slip tectonics; Tectonics; Inversion (geology); Fault (geology); Paleontology; Structural basin","score_opus":0.034318311439828594,"score_gpt":0.24618868412224632,"score_spread":0.2118703726824177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100649517","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96027136,0.0066924095,0.0005583708,0.0028740999,0.00012253181,0.00002031955,0.00031219606,0.000031312506,0.029117456],"genre_scores_gemma":[0.9960628,0.0026594924,0.00023191949,0.000103115635,0.000051616877,0.0000046094115,0.00010075281,0.0000037884354,0.000781798],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999293,0.000010618939,0.0000073114834,0.00001630169,0.000010302755,0.000026197067],"domain_scores_gemma":[0.9997279,0.0000284,0.000093993316,0.000015984433,0.000097430944,0.000036238274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042340785,0.00030970183,0.00024058392,0.0009262291,0.00060556387,0.0016274241,0.00040651127,0.0002732333,0.0029141314],"category_scores_gemma":[0.0006697081,0.00008703963,0.00017519345,0.001970193,0.0012453324,0.0013552402,0.00040778532,0.00039780064,0.00022129799],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035041088,0.00009121855,0.78888154,0.00046203381,0.00012488685,0.0024436915,0.008599826,0.003846722,0.00978782,0.03472295,0.0031211297,0.14756772],"study_design_scores_gemma":[0.000039778966,0.000108479755,0.9398131,0.00027767636,0.00011305322,0.001270434,0.017848695,0.0030138225,0.0014498825,0.013611991,0.022400316,0.000052782612],"about_ca_topic_score_codex":0.052268106,"about_ca_topic_score_gemma":0.050672486,"teacher_disagreement_score":0.052268106,"about_ca_system_score_codex":0.0019865031,"about_ca_system_score_gemma":0.00221338,"threshold_uncertainty_score":0.10392779},"labels":[],"label_agreement":null},{"id":"W2100981277","doi":"10.1146/annurev.earth.31.100901.141246","title":"Holocene Earthquake Records from the Cascadia Subduction Zone and Northern San Andreas Fault Based on Precise Dating of Offshore Turbidites","year":2003,"lang":"en","type":"article","venue":"Annual Review of Earth and Planetary Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":332,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Geology; Holocene; Seismology; Subduction; Paleoseismology; Fault (geology); Paleontology; Continental margin; Turbidite; Geologic record; Submarine pipeline; Oceanography; Sediment; Tectonics","score_opus":0.018707266448230113,"score_gpt":0.23235594469141715,"score_spread":0.21364867824318703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100981277","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7486261,0.20087874,0.0012289366,0.0013753702,0.00025328973,0.000053399224,0.005504459,0.00009846924,0.0419812],"genre_scores_gemma":[0.7503528,0.23249733,0.0011780767,0.00017121088,0.00033006768,0.000050363033,0.0059151095,0.000013700795,0.0094913365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986565,0.000017512699,0.000014922088,0.000044706943,0.00004619177,0.000010968066],"domain_scores_gemma":[0.9993199,0.00008356336,0.0001940795,0.000044642416,0.00029860364,0.000059128735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000507902,0.00016597928,0.000118579745,0.0013265187,0.00018106763,0.00036184644,0.00020811096,0.00011017778,0.0012510028],"category_scores_gemma":[0.0008339734,0.00009170923,0.00007235859,0.0017901548,0.000174307,0.0002243077,0.00028703164,0.00014875166,0.00040405794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006758567,0.00003688666,0.67390543,0.0019478091,0.00021811243,0.00023554267,0.0012732758,0.00039408877,0.006545043,0.0009983678,0.009529209,0.3048487],"study_design_scores_gemma":[0.0000024134602,0.000018441086,0.9687593,0.00015361352,0.00003976989,0.000057807374,0.00019112299,0.000026779295,0.00020288806,0.000052509324,0.030492233,0.0000031197396],"about_ca_topic_score_codex":0.03022643,"about_ca_topic_score_gemma":0.0992105,"teacher_disagreement_score":0.9697736,"about_ca_system_score_codex":0.00037244803,"about_ca_system_score_gemma":0.00055126275,"threshold_uncertainty_score":0.060101032},"labels":[],"label_agreement":null},{"id":"W2101676819","doi":"10.1144/gsl.sp.2000.167.01.12","title":"NE Atlantic continental rifting and volcanic margin formation","year":2000,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":269,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Continental margin; Rift; Margin (machine learning); Volcano; Passive margin; Paleontology; Geochemistry; Petrology; Tectonics","score_opus":0.016172616432312745,"score_gpt":0.21025504694021116,"score_spread":0.19408243050789842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101676819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963726,0.0002850573,0.000019533836,0.00010222638,0.0000062792346,0.0000025245042,0.0005176692,0.0000026637847,0.0026915413],"genre_scores_gemma":[0.9989421,0.00009750247,0.0000141649825,0.000013938088,0.000004228203,0.0000012380872,0.00032393294,0.0000013270062,0.00060161913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999366,0.0000102537215,0.0000053566114,0.000013563508,0.00001190399,0.000022343984],"domain_scores_gemma":[0.999418,0.00008305345,0.00021437944,0.000033172164,0.00007460862,0.00017680413],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020105169,0.00010495521,0.000093268405,0.00029785736,0.00015119914,0.0003870342,0.00014289192,0.00013744923,0.0045974497],"category_scores_gemma":[0.0007356089,0.00006175793,0.00016094325,0.00026518758,0.00013260523,0.00014868316,0.0001738633,0.0001829075,0.00028454073],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089392895,0.000015093267,0.9956279,0.000005184582,0.000038545022,0.00009983346,0.00005084892,0.000050934974,0.0005539687,0.00008374197,0.00024333992,0.0031413543],"study_design_scores_gemma":[0.000002601682,0.0000062249305,0.9995994,0.0000026813314,0.000006936959,0.00003884587,0.000039448645,0.000051117477,0.000029328357,0.0000139491485,0.00020884321,5.832796e-7],"about_ca_topic_score_codex":0.054245118,"about_ca_topic_score_gemma":0.14612126,"teacher_disagreement_score":0.054245118,"about_ca_system_score_codex":0.00041407527,"about_ca_system_score_gemma":0.00032863126,"threshold_uncertainty_score":0.10785872},"labels":[],"label_agreement":null},{"id":"W2101802606","doi":"10.1785/0120110054","title":"The 16 May 1909 Northern Great Plains Earthquake","year":2011,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology","score_opus":0.02451586670974437,"score_gpt":0.20197699032207683,"score_spread":0.17746112361233246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101802606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9764498,0.000114827635,0.00009389447,0.0007205548,0.00007269538,0.0000137924035,0.005103993,0.00003279786,0.017397562],"genre_scores_gemma":[0.9896535,0.00015595439,0.00010307326,0.00010027831,0.00007357875,0.00000985913,0.0040514376,0.00000580252,0.00584638],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999137,0.00000773444,0.0000041279854,0.000013925471,0.000032125023,0.000028307439],"domain_scores_gemma":[0.9998197,0.000010857239,0.00005758128,0.000012335712,0.00004423828,0.00005541098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010256876,0.000109423614,0.00010355715,0.000427629,0.0005434544,0.0004234104,0.0001400098,0.00018316353,0.004446513],"category_scores_gemma":[0.0004870115,0.00006449434,0.00006781279,0.0005781168,0.00028522,0.00017377098,0.0005015573,0.0002422236,0.0006831881],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020310916,0.00008160307,0.9403392,0.000071458875,0.000044835295,0.0017646892,0.0011733122,0.0010470535,0.0039759353,0.0006819073,0.023675742,0.026941132],"study_design_scores_gemma":[0.000005413667,0.000014849491,0.989175,0.00000951727,0.0000044888493,0.00008287833,0.00027460704,0.00009169344,0.00017125116,0.00007227529,0.0100954985,0.0000025290485],"about_ca_topic_score_codex":0.066698,"about_ca_topic_score_gemma":0.12988451,"teacher_disagreement_score":0.066698,"about_ca_system_score_codex":0.0013714038,"about_ca_system_score_gemma":0.00050349656,"threshold_uncertainty_score":0.13261956},"labels":[],"label_agreement":null},{"id":"W2102338328","doi":"10.1130/g32878.1","title":"Strengthening of the Northeast Monsoon over the Flores Sea, Indonesia, at the time of Heinrich event 1","year":2012,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Lamont-Doherty Earth Observatory, Columbia University; National Oceanic and Atmospheric Administration","keywords":"Citation; Icon; Event (particle physics); History; Oceanography; Geography; Library science; Art history; Geology; Archaeology","score_opus":0.0099188348779349,"score_gpt":0.20480701623438693,"score_spread":0.19488818135645203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102338328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991891,0.00005035481,0.00001549753,0.000021415655,0.0000015795168,0.000001492997,0.00007932341,0.0000025900802,0.0006387096],"genre_scores_gemma":[0.9997104,0.000035295987,0.000024460594,0.0000059546815,0.0000019408906,8.794513e-7,0.00007404141,6.0203735e-7,0.00014636437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999542,0.0000053978647,0.0000040557197,0.000015194153,0.000009028952,0.000012097361],"domain_scores_gemma":[0.99983406,0.000015626927,0.000072214636,0.000009074366,0.000026678883,0.00004225995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011675567,0.0001323228,0.00013573054,0.00040291555,0.0003963743,0.00044248687,0.00011797172,0.00011343485,0.0007287373],"category_scores_gemma":[0.00036914754,0.00010137276,0.00008170159,0.0002916124,0.00028310466,0.00023097663,0.00038158626,0.0002139163,0.000073077696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007881197,0.000015212044,0.9870449,0.00001952615,0.000028850101,0.00041035304,0.0006018681,0.00013812595,0.004732204,0.000054557004,0.00010445432,0.006771074],"study_design_scores_gemma":[2.977304e-7,0.000006707401,0.9995931,0.0000014352041,0.0000020661578,0.00005177987,0.0001117833,0.000038401955,0.00009382912,0.000004241268,0.0000957198,7.788408e-7],"about_ca_topic_score_codex":0.029671451,"about_ca_topic_score_gemma":0.08598,"teacher_disagreement_score":0.029671451,"about_ca_system_score_codex":0.00060334924,"about_ca_system_score_gemma":0.0003135755,"threshold_uncertainty_score":0.058997512},"labels":[],"label_agreement":null},{"id":"W2102376081","doi":"10.5539/esr.v2n2p143","title":"Some Characteristics of Seismicity Before Strong Earthquake Chi-Chi (MW = 7.6), 1999, Taiwan","year":2013,"lang":"en","type":"article","venue":"Earth Science Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Seismology; Induced seismicity; Geology; Range (aeronautics)","score_opus":0.042484570105386796,"score_gpt":0.2981130706874079,"score_spread":0.2556285005820211,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102376081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99934584,0.000040426687,0.000032410386,0.00001209624,7.7131364e-7,0.0000018805149,0.00023581521,0.0000025436013,0.00032815032],"genre_scores_gemma":[0.9988564,0.000036673715,0.000020076055,0.000003455853,0.0000033958695,0.0000026069558,0.00094945193,0.0000018821858,0.00012596213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991107,0.000009888379,0.000012748376,0.000025924079,0.000014267105,0.000026069709],"domain_scores_gemma":[0.99903905,0.00016221846,0.00040991654,0.000060372695,0.00015565964,0.00017275117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017179025,0.000097190816,0.00012094659,0.0012661839,0.00017690397,0.0004009704,0.00013952481,0.0001934945,0.0007407089],"category_scores_gemma":[0.0011091453,0.00010015679,0.00011477292,0.0010659894,0.00022649417,0.00022908715,0.00028442356,0.00020149577,0.0002056767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009243827,0.00001851389,0.9934002,0.000013667532,0.000020476753,0.0002755742,0.00041000955,0.0002474614,0.0025525813,0.0000824418,0.00015334488,0.0027333514],"study_design_scores_gemma":[7.6581387e-7,0.000023743341,0.9994073,0.0000017573007,0.0000024835026,0.000094838426,0.00012357837,0.00013074964,0.00006708966,0.000010835283,0.00013517696,0.0000017111125],"about_ca_topic_score_codex":0.0075250794,"about_ca_topic_score_gemma":0.010732079,"teacher_disagreement_score":0.0075250794,"about_ca_system_score_codex":0.00029652056,"about_ca_system_score_gemma":0.000198841,"threshold_uncertainty_score":0.014962554},"labels":[],"label_agreement":null},{"id":"W2102412510","doi":"10.1002/2013jb010836","title":"An investigation of seismicity clustered near the Cordel Field, west central Alberta, and its relation to a nearby disposal well","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":108,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"University of Alberta","keywords":"Induced seismicity; Seismology; Hypocenter; Geology; Foreland basin; Structural basin; Tectonics; Paleontology","score_opus":0.02634559759588099,"score_gpt":0.29178186278990065,"score_spread":0.26543626519401964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102412510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984263,0.000055792003,0.00014117552,0.000019604642,0.0000020497296,0.000011097634,0.0003310127,0.000010160788,0.0010029029],"genre_scores_gemma":[0.9981579,0.00007671577,0.0003149675,0.000008920712,0.0000028263703,0.0000055951937,0.0005273403,0.000002215181,0.0009034906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985003,0.000006981324,0.0000052084747,0.000031766904,0.00006730341,0.000038586335],"domain_scores_gemma":[0.9995622,0.000041972886,0.00008858677,0.000016634633,0.00018313921,0.000107506756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012979831,0.00023907884,0.00017647032,0.0017609348,0.00086061604,0.0005997176,0.0004986364,0.00022639768,0.0007924802],"category_scores_gemma":[0.0005002066,0.00011592995,0.00009013485,0.0022587692,0.0004338308,0.0001293424,0.00042886066,0.0002104506,0.000085443724],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016391824,0.00007011757,0.9631197,0.00003192633,0.000033693956,0.0006523772,0.0016105538,0.0009295759,0.01198944,0.00014561211,0.0004964516,0.020756572],"study_design_scores_gemma":[0.0000024431895,0.00002110666,0.9972675,0.000004664272,0.0000072311136,0.000039234114,0.0011511473,0.0006369446,0.00036267997,0.000010068517,0.0004927903,0.000004308542],"about_ca_topic_score_codex":0.8734016,"about_ca_topic_score_gemma":0.9632982,"teacher_disagreement_score":0.12659842,"about_ca_system_score_codex":0.0036454496,"about_ca_system_score_gemma":0.0036864514,"threshold_uncertainty_score":0.2546879},"labels":[],"label_agreement":null},{"id":"W2102457532","doi":"10.1111/j.1365-246x.2010.04623.x","title":"Bias in seismic estimates of crustal properties","year":2010,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Estimator; Crust; Seismology; Least-squares function approximation; Geodesy; Seismic velocity; Grid; Seismic array; Waveform; Matching (statistics); Geophysics; Statistics; Mathematics; Physics","score_opus":0.03136437840139322,"score_gpt":0.24346526570252294,"score_spread":0.21210088730112972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102457532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5196151,0.0021343238,0.46921358,0.00055311626,0.00018677769,0.000035791687,0.0011198458,0.0023503606,0.0047911927],"genre_scores_gemma":[0.9309817,0.00069914636,0.06592519,0.00015927375,0.000072725474,0.000016485037,0.00075159257,0.00046751898,0.0009264119],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99756986,0.0007655934,0.00027564674,0.00046970186,0.00080493116,0.00011424612],"domain_scores_gemma":[0.9926076,0.0032509489,0.0010100524,0.0014727202,0.0016026854,0.000056071887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005222486,0.00064743403,0.0004902546,0.001830567,0.00018636503,0.0010657843,0.0005583179,0.00032989253,0.0008589845],"category_scores_gemma":[0.031226756,0.0005141929,0.00036257677,0.001307736,0.00037047733,0.0013842547,0.0012169112,0.00063309196,0.0005026186],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050460076,0.000055726017,0.33782938,0.0005571457,0.00075114635,0.0002517972,0.0013783032,0.07500875,0.085928045,0.015055899,0.002684569,0.47999457],"study_design_scores_gemma":[0.00008891498,0.00025201213,0.51888543,0.0004054136,0.0003522825,0.0011373631,0.0007503594,0.30334362,0.11079813,0.047166716,0.016549371,0.00027033628],"about_ca_topic_score_codex":0.0025941408,"about_ca_topic_score_gemma":0.003731442,"teacher_disagreement_score":0.005222486,"about_ca_system_score_codex":0.00038625984,"about_ca_system_score_gemma":0.00037318657,"threshold_uncertainty_score":0.027619481},"labels":[],"label_agreement":null},{"id":"W2102499426","doi":"10.1029/2003gl017585","title":"Detection of a D″ discontinuity in the south Atlantic using PKKP","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Coda; Discontinuity (linguistics); Mantle (geology); Amplitude; Jump; Seismology; Core–mantle boundary; Geodesy; Classification of discontinuities; Reflection (computer programming); Geophysics; Physics; Optics","score_opus":0.05857724332399869,"score_gpt":0.29559151099123376,"score_spread":0.23701426766723507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102499426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99573225,0.000044034576,0.0019041878,0.000042205676,0.000004898692,0.0000063439516,0.00031414814,0.00005497963,0.0018969484],"genre_scores_gemma":[0.99774337,0.000031534044,0.0017716119,0.000005893664,0.000002351893,0.000002273129,0.00031090147,0.000004205325,0.00012788852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999287,0.000007155806,0.000004821439,0.000026384772,0.000015978347,0.000017046179],"domain_scores_gemma":[0.9998035,0.00003667447,0.00005272041,0.000030778298,0.00004197297,0.00003447098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012588261,0.00012907381,0.00010419703,0.0004110397,0.00028346363,0.00037197382,0.00021950064,0.0002634505,0.0008133577],"category_scores_gemma":[0.0008020343,0.00019667222,0.00012902348,0.00042288547,0.0001611017,0.00031561105,0.00048717097,0.00028964953,0.00020336607],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005531556,0.000036082452,0.70569605,0.00011606012,0.000051852163,0.00042412014,0.00047179905,0.0048907404,0.21824598,0.0009429095,0.00046671732,0.06810457],"study_design_scores_gemma":[0.000020047946,0.000061568084,0.97004426,0.000016836642,0.000025137078,0.00035013142,0.00017448424,0.019863889,0.008245611,0.00026228657,0.00091748656,0.00001823309],"about_ca_topic_score_codex":0.01289305,"about_ca_topic_score_gemma":0.023796782,"teacher_disagreement_score":0.01289305,"about_ca_system_score_codex":0.00030366625,"about_ca_system_score_gemma":0.0002411677,"threshold_uncertainty_score":0.025636017},"labels":[],"label_agreement":null},{"id":"W2102626288","doi":"10.1002/jgrb.50390","title":"Downdip landward limit of Cascadia great earthquake rupture","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Subduction; Seismic hazard; Slip (aerodynamics); Episodic tremor and slip; Thrust; Submarine pipeline; Thrust fault; Earthquake rupture; Tectonics; Geotechnical engineering; Fault (geology)","score_opus":0.04129512463622898,"score_gpt":0.3013903984514716,"score_spread":0.2600952738152426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102626288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9724654,0.0005499778,0.0010489773,0.00021859966,0.000010775789,0.000012180747,0.00074692734,0.000071362214,0.024875863],"genre_scores_gemma":[0.9987865,0.00009744313,0.000101855556,0.00002225862,0.000008060185,0.0000056937656,0.00041424687,0.000006834838,0.0005569471],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996687,0.00005686544,0.00003075168,0.00006218252,0.000115851595,0.000065638305],"domain_scores_gemma":[0.99796236,0.00048204666,0.0005089638,0.00018589968,0.000602631,0.00025808756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005137694,0.00021129103,0.00024466723,0.0011981786,0.0004945891,0.0009881802,0.00035452744,0.0002500816,0.0054071],"category_scores_gemma":[0.0038741434,0.0001252847,0.00016455079,0.00042730485,0.00047796685,0.00046650285,0.0009525506,0.0002408304,0.0007495879],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003923343,0.000029324,0.9452806,0.00017053858,0.00007318157,0.00085221895,0.0010073811,0.009734099,0.015529708,0.0025232083,0.00199102,0.022416363],"study_design_scores_gemma":[0.000008396414,0.00006630368,0.98898447,0.000053065807,0.000016939062,0.00027105445,0.0007541558,0.002831479,0.0015551918,0.0009572122,0.004486008,0.000015669626],"about_ca_topic_score_codex":0.015070873,"about_ca_topic_score_gemma":0.019918764,"teacher_disagreement_score":0.015070873,"about_ca_system_score_codex":0.00055750506,"about_ca_system_score_gemma":0.00034230243,"threshold_uncertainty_score":0.029966354},"labels":[],"label_agreement":null},{"id":"W2103047019","doi":"10.1785/0120050162","title":"Region-Specific Key Seismic Parameters for Earthquakes in Northern Iran","year":2006,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Seismology; Geology; Key (lock); Computer science; Computer security","score_opus":0.024103972792013314,"score_gpt":0.20305877228259103,"score_spread":0.17895479949057772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103047019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997059,0.000066739274,0.0013250026,0.000012698709,0.0000015399304,0.000015451196,0.0009222122,0.00004485836,0.00055246125],"genre_scores_gemma":[0.99674857,0.000062365405,0.0013210761,0.0000017075404,0.0000035643188,0.000017556144,0.0017582852,0.000005539881,0.00008125981],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976796,0.000043352182,0.00003399482,0.00005540526,0.000069798036,0.000029485009],"domain_scores_gemma":[0.9992317,0.00014664671,0.00029407555,0.000083217696,0.00020857752,0.00003572062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049700524,0.00028924717,0.00024745337,0.0017719176,0.00018931263,0.0002252288,0.00029096505,0.00021765167,0.0005870045],"category_scores_gemma":[0.0020019428,0.00018500033,0.00031079858,0.0017711358,0.00017541426,0.00035571234,0.00025057397,0.00015805311,0.00019734095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019926911,0.000048548816,0.88704723,0.00011651043,0.00013745851,0.00037575988,0.0008192074,0.045462616,0.0099701295,0.00046449158,0.00087221264,0.054486528],"study_design_scores_gemma":[0.000009896311,0.000040038118,0.98500305,0.000005235001,0.00003010674,0.000302831,0.00034287118,0.012681518,0.0008341187,0.00014721231,0.00058606145,0.000017096554],"about_ca_topic_score_codex":0.008947434,"about_ca_topic_score_gemma":0.014655134,"teacher_disagreement_score":0.008947434,"about_ca_system_score_codex":0.0005092677,"about_ca_system_score_gemma":0.00041649883,"threshold_uncertainty_score":0.017790675},"labels":[],"label_agreement":null},{"id":"W2103977603","doi":"10.1130/b30855.1","title":"On the origin of orogens","year":2013,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":248,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Nova scotia; Citation; Library science; Download; World Wide Web; Computer science; History; Archaeology","score_opus":0.019294848663635317,"score_gpt":0.20604368733446018,"score_spread":0.18674883867082487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103977603","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10660414,0.050216638,0.0046278206,0.023529284,0.003139352,0.0002093051,0.0025664524,0.00015207141,0.808955],"genre_scores_gemma":[0.62777805,0.087977245,0.003596547,0.0051760203,0.0011944593,0.000084854466,0.0022742443,0.00034258858,0.271576],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9991653,0.0001552972,0.000036576235,0.0001172039,0.00030033913,0.00022522072],"domain_scores_gemma":[0.9989613,0.00015858836,0.00014160048,0.00017802922,0.000465311,0.0000952255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001331944,0.00040893292,0.00047749412,0.0010051036,0.0021235198,0.0026827394,0.0006190906,0.0007894626,0.023238884],"category_scores_gemma":[0.0029548977,0.00033576935,0.00031445417,0.0016479203,0.0034484053,0.0022547236,0.0026793987,0.0019746611,0.0032561107],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008072723,0.00010831578,0.028941369,0.0018703449,0.00015380922,0.0021755712,0.0057182224,0.001791151,0.0141821,0.46992412,0.10147441,0.37285328],"study_design_scores_gemma":[0.000012154326,0.000040731295,0.020479655,0.0004651915,0.00003196929,0.00018744527,0.0012147762,0.00013167961,0.0027464065,0.014022751,0.9606438,0.000023387493],"about_ca_topic_score_codex":0.044650666,"about_ca_topic_score_gemma":0.04839893,"teacher_disagreement_score":0.044650666,"about_ca_system_score_codex":0.0051688394,"about_ca_system_score_gemma":0.0043435963,"threshold_uncertainty_score":0.088781536},"labels":[],"label_agreement":null},{"id":"W2104076266","doi":"10.2113/econgeo.109.8.2129","title":"Drilling Shallow-Water Massive Sulfides at the Palinuro Volcanic Complex, Aeolian Island Arc, Italy","year":2014,"lang":"en","type":"article","venue":"Economic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University; University of Ottawa","funders":"","keywords":"Geology; Art history; History; Library science; Computer science","score_opus":0.01467898404191942,"score_gpt":0.19529304531560218,"score_spread":0.18061406127368276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104076266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962624,0.00015072964,0.00047056077,0.0000392151,0.0000046963223,0.000029476932,0.00026288244,0.000040426516,0.0027395696],"genre_scores_gemma":[0.99456525,0.00015523756,0.002545852,0.000013504333,0.000007515892,0.000031993924,0.00043893734,0.00000842384,0.002233317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994326,0.0000048491493,0.0000032647056,0.000024308236,0.000014159855,0.000010165188],"domain_scores_gemma":[0.9999472,0.000007935524,0.00001470234,0.0000045844977,0.000012109119,0.000013450593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111900474,0.00029085772,0.00009928879,0.0006485596,0.0002996546,0.00022235657,0.00020665662,0.00024415203,0.0008227011],"category_scores_gemma":[0.00015708373,0.00015216341,0.00010584541,0.0002853397,0.00021394569,0.00012477122,0.00039238986,0.00009396015,0.00028955398],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003653555,0.00010267709,0.6320567,0.0002528817,0.000058395726,0.0017895346,0.0034300706,0.0027925265,0.26824346,0.00030099804,0.001331975,0.08927539],"study_design_scores_gemma":[0.000012170134,0.00009431372,0.9936392,0.000011724683,0.000011306141,0.00025096966,0.00025260658,0.0009022001,0.002949611,0.000029551451,0.0018430271,0.0000032760158],"about_ca_topic_score_codex":0.01257231,"about_ca_topic_score_gemma":0.035489693,"teacher_disagreement_score":0.01257231,"about_ca_system_score_codex":0.00029055064,"about_ca_system_score_gemma":0.0004053465,"threshold_uncertainty_score":0.024998307},"labels":[],"label_agreement":null},{"id":"W2104634797","doi":"10.1029/2001jb000886","title":"Thermal models of the Mexico subduction zone: Implications for the megathrust seismogenic zone","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Fault (geology); Thrust fault; Thrust; Convergent boundary; Trench; Shear zone; Oceanic crust; Petrology; Tectonics","score_opus":0.07433479278969923,"score_gpt":0.2988013286221658,"score_spread":0.22446653583246656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104634797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86589813,0.0020635535,0.096374854,0.0020900774,0.0001198445,0.000101215,0.0017625135,0.0004901517,0.031099658],"genre_scores_gemma":[0.9930835,0.00054146204,0.0038266878,0.00006437162,0.000042311985,0.00006428058,0.00018584193,0.00005722186,0.0021343257],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993443,0.000019743198,0.0000036761376,0.00001358848,0.000010024277,0.000018467486],"domain_scores_gemma":[0.999772,0.00008055095,0.000054281743,0.000019010924,0.000038532475,0.000035652243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022990422,0.00044748516,0.00041182985,0.00041795595,0.00045773812,0.00079772744,0.0011975733,0.00080465735,0.002855798],"category_scores_gemma":[0.0010503698,0.00026993276,0.0005624442,0.00045054295,0.0004903507,0.0009177654,0.0006562543,0.00041698272,0.00028076212],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024753172,0.000012249818,0.002022846,0.000014354934,0.000012108142,0.00002661256,0.000034831715,0.9913119,0.00060767203,0.004780326,0.0001732921,0.0009789668],"study_design_scores_gemma":[0.000022400432,0.000012260327,0.0017654165,0.000006391433,0.000006672458,0.000013259255,0.00003559569,0.99280506,0.00014132568,0.004591752,0.0005921119,0.000007817427],"about_ca_topic_score_codex":0.022704946,"about_ca_topic_score_gemma":0.009057288,"teacher_disagreement_score":0.022704946,"about_ca_system_score_codex":0.0011640121,"about_ca_system_score_gemma":0.00057075615,"threshold_uncertainty_score":0.04514563},"labels":[],"label_agreement":null},{"id":"W2104675108","doi":"10.1046/j.1365-246x.2003.01932.x","title":"Analysis of broad-band regional waveforms of the 1996 September 29 earthquake at Bárdarbunga volcano, central Iceland: investigation of the magma injection hypothesis","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Seismology; Geology; Volcano; Seismometer; Amplitude; Seismic moment; Focal mechanism; Waveform; Geodesy; Magma chamber; Magma; Fault (geology); Radar; Physics","score_opus":0.016293229183786635,"score_gpt":0.2048470855859494,"score_spread":0.18855385640216277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104675108","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991788,0.00006136442,0.00023864926,0.000011564766,0.0000033330925,0.000005638184,0.0001940066,0.000007742958,0.0002988056],"genre_scores_gemma":[0.997971,0.000087580884,0.0006065486,0.000005869126,0.00000927309,0.000005479493,0.0010857114,0.000004217869,0.00022425473],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999951,0.0000052916866,0.000004396709,0.000014344459,0.000011477242,0.000013445245],"domain_scores_gemma":[0.9998399,0.0000310166,0.000046313824,0.000010078291,0.000045929613,0.000026781132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017327149,0.00021653292,0.00016433926,0.00059686275,0.00013738777,0.00025522994,0.00015792024,0.00013607358,0.00041041637],"category_scores_gemma":[0.00034503144,0.000062958025,0.0001270067,0.00049363746,0.0001340804,0.00013262167,0.00015128047,0.000108935856,0.000086683125],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011561261,0.00028667317,0.7288007,0.00022191548,0.00020485578,0.0018677972,0.00092195784,0.01651273,0.15714307,0.0003326655,0.00114307,0.09140835],"study_design_scores_gemma":[0.000008409723,0.00004475531,0.98949933,0.000006888341,0.000021121285,0.00012104199,0.00020763402,0.007915514,0.0018843041,0.000015686728,0.0002706264,0.000004792557],"about_ca_topic_score_codex":0.014947816,"about_ca_topic_score_gemma":0.021333195,"teacher_disagreement_score":0.014947816,"about_ca_system_score_codex":0.0003314426,"about_ca_system_score_gemma":0.00029162742,"threshold_uncertainty_score":0.029721618},"labels":[],"label_agreement":null},{"id":"W2106099674","doi":"10.1111/j.1365-246x.2008.03795.x","title":"A gravity gradient method for characterizing the post-seismic deformation field for a finite fault","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Bouguer anomaly; Geology; Gravity anomaly; Free-air gravity anomaly; Geophysics; Geodesy; Seismology; Gravitational field; Deformation (meteorology); Slip (aerodynamics); Fault (geology); Physics; Classical mechanics","score_opus":0.024496865365432358,"score_gpt":0.268294898877643,"score_spread":0.24379803351221066,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106099674","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004803767,0.00008020129,0.9936358,0.000030336787,0.000019955474,0.000027767781,0.000084119754,0.0004669869,0.000851076],"genre_scores_gemma":[0.085880555,0.00019145467,0.9104116,0.00004142243,0.000041355408,0.00008887885,0.0002556021,0.0002622256,0.0028268506],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998853,0.000030703886,0.0000071556524,0.000020763682,0.00004507583,0.000010958484],"domain_scores_gemma":[0.9998573,0.000051991854,0.0000184834,0.000020853711,0.00004167969,0.000009660786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028523552,0.00051217416,0.00026783525,0.00075959245,0.0002639785,0.00035048954,0.00048147232,0.00041506268,0.002306482],"category_scores_gemma":[0.0007184268,0.00012492467,0.0003296341,0.0007091103,0.00037275514,0.00064420816,0.0003344941,0.00056351547,0.0011118631],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014299805,0.00006176055,0.0025099823,0.00025501664,0.000067534165,0.0002347599,0.00018345419,0.121539325,0.10184627,0.12526625,0.007739039,0.64015365],"study_design_scores_gemma":[0.000017904937,0.000046728648,0.0014542132,0.000012529365,0.000017156508,0.00018669778,0.000028334629,0.9477731,0.010730169,0.023385393,0.016312959,0.00003481166],"about_ca_topic_score_codex":0.0026124066,"about_ca_topic_score_gemma":0.0029762676,"teacher_disagreement_score":0.0026124066,"about_ca_system_score_codex":0.00020977146,"about_ca_system_score_gemma":0.00057408673,"threshold_uncertainty_score":0.007716},"labels":[],"label_agreement":null},{"id":"W2106180230","doi":"10.1139/cjes-2013-0215","title":"The 5.2 magnitude earthquake near Ladysmith, Quebec, 17 May 2013: implications for the seismotectonics of the Ottawa–Bonnechere Graben","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismotectonics; Magnitude (astronomy); Seismology; Graben; Earthquake magnitude; Tectonics; Geometry","score_opus":0.02324281401113725,"score_gpt":0.22943651726530268,"score_spread":0.20619370325416542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106180230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8802242,0.0039113383,0.00040877206,0.0283023,0.00024862037,0.00014133846,0.018727869,0.0000797585,0.0679558],"genre_scores_gemma":[0.977896,0.001663103,0.00027864779,0.0013598463,0.000038654387,0.000022997829,0.0023511695,0.00001937982,0.016370123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997433,0.000017856568,0.0000067419905,0.00002906983,0.00006447825,0.00013848879],"domain_scores_gemma":[0.9992016,0.000047151694,0.0001072324,0.0000184046,0.0003782887,0.0002473783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037819688,0.00024136691,0.00022465357,0.0010065751,0.005304765,0.0023263863,0.0011381112,0.0008390181,0.010687378],"category_scores_gemma":[0.001351498,0.00021685254,0.0002022426,0.0018463922,0.0013796483,0.00059567834,0.0007341029,0.0009535222,0.00039129483],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042828682,0.00017767565,0.7155604,0.00036643722,0.00015192029,0.0031195232,0.009920587,0.004809263,0.0034721303,0.011092754,0.18043211,0.070469],"study_design_scores_gemma":[0.000027967404,0.000018696075,0.9532067,0.00016799962,0.000025111933,0.00007114692,0.008654533,0.0014030865,0.00018981268,0.0003407816,0.035857543,0.000036625108],"about_ca_topic_score_codex":0.9991603,"about_ca_topic_score_gemma":0.9997526,"teacher_disagreement_score":0.067038044,"about_ca_system_score_codex":0.067038044,"about_ca_system_score_gemma":0.06321954,"threshold_uncertainty_score":0.48639733},"labels":[],"label_agreement":null},{"id":"W2106600517","doi":"10.1111/j.1365-246x.2012.05457.x","title":"Delineating complex spatiotemporal distribution of earthquake aftershocks: an improved Source-Scanning Algorithm","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Aftershock; Seismogram; Seismology; Geology; Algorithm; Seismometer; Focal mechanism; Waveform; Geodesy; Computer science; Telecommunications; Induced seismicity","score_opus":0.025982092385529895,"score_gpt":0.2603258839431134,"score_spread":0.2343437915575835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106600517","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.045964662,0.000053492367,0.95252675,0.000058428308,0.000007634931,0.00003072365,0.00006879831,0.0009872203,0.00030225856],"genre_scores_gemma":[0.13972832,0.00005263533,0.8591438,0.000024759764,0.000018841374,0.000068129324,0.0003066617,0.00015735044,0.000499522],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99976295,0.000054962915,0.00002811491,0.000057105528,0.0000736547,0.000023236436],"domain_scores_gemma":[0.99880946,0.0005082318,0.000118835145,0.00016761638,0.0003343782,0.00006153204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011033388,0.0005757992,0.0007132242,0.0017333637,0.0002818107,0.00065278227,0.0009797921,0.0005662879,0.0013103904],"category_scores_gemma":[0.0028332358,0.000461616,0.0006016157,0.0013346119,0.00043925527,0.0008432809,0.0010094715,0.00055788114,0.0006769116],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000454195,0.00017165684,0.016747955,0.000121766825,0.00010101623,0.00025055776,0.00033047676,0.16009139,0.12245585,0.007144707,0.0018210645,0.6903093],"study_design_scores_gemma":[0.000039597613,0.000045652876,0.004061787,0.0000045432516,0.000023500535,0.00012341804,0.000020822503,0.9838329,0.008789824,0.0019153416,0.0011212853,0.000021317413],"about_ca_topic_score_codex":0.0015919798,"about_ca_topic_score_gemma":0.0024476128,"teacher_disagreement_score":0.0017333637,"about_ca_system_score_codex":0.00021716952,"about_ca_system_score_gemma":0.0009740786,"threshold_uncertainty_score":0.005835116},"labels":[],"label_agreement":null},{"id":"W2107345693","doi":"10.1785/0120140177","title":"GPS Observations of Crustal Deformation Associated with the 2012 Mw 7.8 Haida Gwaii Earthquake","year":2015,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Global Positioning System; Deformation (meteorology); Geodesy; Oceanography; Engineering; Telecommunications","score_opus":0.03574456692370988,"score_gpt":0.21008545027461636,"score_spread":0.17434088335090647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107345693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971787,0.000027493636,0.00007138376,0.000023623186,0.0000051209845,0.000013886958,0.0010644505,0.000012986244,0.0016023916],"genre_scores_gemma":[0.996021,0.00006825433,0.00031736115,0.000011917346,0.0000056054623,0.00002085588,0.0024161078,0.0000035953358,0.0011353272],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991477,0.0000058309397,0.0000046237915,0.000023056164,0.000031494597,0.000020219073],"domain_scores_gemma":[0.99972147,0.000014164344,0.00007595208,0.000024639388,0.00009662132,0.0000670991],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000110863235,0.0002444483,0.00020203677,0.0006814945,0.00038401617,0.00031516637,0.0002832491,0.00026620412,0.0007855563],"category_scores_gemma":[0.00049684796,0.00019631156,0.00009960837,0.0011630878,0.00026733827,0.00019881409,0.00042764898,0.00031581122,0.0002612643],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001260227,0.00007130075,0.9586481,0.00005427716,0.000053909804,0.00037000907,0.0016971444,0.0012309055,0.0118651595,0.0000620414,0.002379378,0.023441685],"study_design_scores_gemma":[0.000003133453,0.000016576756,0.9986279,0.000004214765,0.000007852067,0.000019239005,0.00017341017,0.00042146852,0.00017786749,0.000003812425,0.0005406625,0.0000038415524],"about_ca_topic_score_codex":0.2875858,"about_ca_topic_score_gemma":0.5904533,"teacher_disagreement_score":0.7124142,"about_ca_system_score_codex":0.0010333887,"about_ca_system_score_gemma":0.0008016324,"threshold_uncertainty_score":0.5718237},"labels":[],"label_agreement":null},{"id":"W2107660525","doi":"10.1144/sp327.7","title":"The Calabrian Orocline: buckling of a previously more linear orogen","year":2009,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Buckling; Geology; Seismology; Structural engineering; Engineering","score_opus":0.020070687340501204,"score_gpt":0.2513994124350374,"score_spread":0.23132872509453617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107660525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98072046,0.00039332875,0.00043867616,0.00029936575,0.000019547402,0.000021470383,0.00015005442,0.00004955353,0.017907616],"genre_scores_gemma":[0.99789196,0.00012453749,0.000300796,0.00010273555,0.000010633444,0.0000049147516,0.00013712182,0.000024233881,0.001403086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996051,0.000036811867,0.00001774309,0.00018693377,0.00005654035,0.00009686914],"domain_scores_gemma":[0.99966586,0.000027178174,0.000139408,0.00004898883,0.00006625648,0.000052245356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003070368,0.00030614296,0.0004099712,0.0009588485,0.0012924315,0.0019705738,0.0006330889,0.00042217833,0.00615981],"category_scores_gemma":[0.001369083,0.00022907296,0.0001648088,0.0012409892,0.0020007866,0.0005747547,0.0013737581,0.0005010035,0.0005315624],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000634979,0.00008387,0.80596113,0.0003867458,0.00031887868,0.0037196865,0.012953967,0.0060961647,0.035529852,0.012540433,0.004181209,0.11759297],"study_design_scores_gemma":[0.000021381164,0.000075824784,0.9746855,0.000065115986,0.000027503564,0.00048212777,0.0021475966,0.001934337,0.0004486525,0.0010234579,0.019070098,0.00001849048],"about_ca_topic_score_codex":0.10296229,"about_ca_topic_score_gemma":0.14253715,"teacher_disagreement_score":0.10296229,"about_ca_system_score_codex":0.0023302443,"about_ca_system_score_gemma":0.00071089255,"threshold_uncertainty_score":0.20472598},"labels":[],"label_agreement":null},{"id":"W2108197427","doi":"10.1785/gssrl.82.2.211","title":"Management of Large Seismic Datasets: I. Automated Building and Updating using BREQ_FAST and NetDC","year":2011,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"Indiana University Bloomington; National Science Foundation","keywords":"Citation; Icon; Library science; Geology; Computer science","score_opus":0.09925349897299648,"score_gpt":0.3364090118583316,"score_spread":0.23715551288533512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108197427","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009903876,0.0014794286,0.40211093,0.0025537696,0.000546058,0.0019138949,0.1793535,0.36590537,0.036233228],"genre_scores_gemma":[0.05868645,0.0027489357,0.5727368,0.00044735498,0.00042383326,0.001889658,0.3247015,0.021905545,0.016459897],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9965797,0.00053161115,0.000474203,0.00051041436,0.001694253,0.00020977193],"domain_scores_gemma":[0.9831814,0.0037299527,0.0012172264,0.0054236287,0.005692594,0.0007551422],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008537644,0.0017691591,0.0015415319,0.010736996,0.0011191869,0.0051334924,0.0041333046,0.0012877984,0.035316937],"category_scores_gemma":[0.020410204,0.0015959546,0.0012248982,0.010670985,0.00071038393,0.006813398,0.0042516105,0.0017413642,0.04432074],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003283831,0.0001116347,0.005290956,0.00071296055,0.0001334778,0.00015701258,0.0003362179,0.010517633,0.0026059,0.0031361214,0.50063163,0.47603798],"study_design_scores_gemma":[0.00046839155,0.00016832612,0.017777285,0.0006975912,0.00014644062,0.0004020582,0.0010427678,0.1882174,0.021546401,0.014035801,0.7550912,0.0004062511],"about_ca_topic_score_codex":0.016121136,"about_ca_topic_score_gemma":0.0159688,"teacher_disagreement_score":0.035316937,"about_ca_system_score_codex":0.0014311363,"about_ca_system_score_gemma":0.0029110597,"threshold_uncertainty_score":0.118146956},"labels":[],"label_agreement":null},{"id":"W2108278931","doi":"10.1785/0220150048","title":"Characterizing and Responding to Seismic Risk Associated with Earthquakes Potentially Triggered by Fluid Disposal and Hydraulic Fracturing","year":2015,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Royal Society; Royal Academy of Engineering; Canadian Association of Petroleum Producers","keywords":"Geology","score_opus":0.04267068342259056,"score_gpt":0.2752969272995214,"score_spread":0.23262624387693082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108278931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93083304,0.0040304316,0.0054732375,0.00550588,0.0002871934,0.00020881415,0.0087995995,0.00040614634,0.044455618],"genre_scores_gemma":[0.9806888,0.0034430074,0.0029867485,0.00026917766,0.00022666664,0.00005313688,0.005611423,0.00009462976,0.006626369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99946815,0.00008179972,0.0000604325,0.00005289265,0.0002637115,0.000073070354],"domain_scores_gemma":[0.9967469,0.00074554945,0.0014015388,0.000111049936,0.0006733115,0.0003216197],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008836178,0.0004071413,0.00042405713,0.0026937758,0.0003828946,0.001105326,0.00040962684,0.0007163446,0.0043088044],"category_scores_gemma":[0.008388993,0.00015598176,0.0003202021,0.0027365321,0.00027883638,0.0010696673,0.0011727298,0.00050865836,0.0017081505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003710742,0.00016205096,0.76323754,0.0005559378,0.00032952157,0.00094729196,0.0014991988,0.009735166,0.0025837945,0.002150727,0.04837542,0.1700523],"study_design_scores_gemma":[0.000030454294,0.00032658095,0.9574362,0.00031020926,0.00015918091,0.00044090513,0.004387577,0.009790316,0.0009619009,0.0035332234,0.022545747,0.00007774522],"about_ca_topic_score_codex":0.007101396,"about_ca_topic_score_gemma":0.022868196,"teacher_disagreement_score":0.007101396,"about_ca_system_score_codex":0.0005945162,"about_ca_system_score_gemma":0.0006540521,"threshold_uncertainty_score":0.01441431},"labels":[],"label_agreement":null},{"id":"W2108309279","doi":"10.1190/1.2901199","title":"Analysis of microearthquake data at Cold Lake and its applications to reservoir monitoring","year":2008,"lang":"en","type":"article","venue":"Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Microearthquake; Induced seismicity; Geology; Borehole; Seismology; Magnitude (astronomy); Microseism; Geotechnical engineering","score_opus":0.062444283366504115,"score_gpt":0.2647463075680826,"score_spread":0.20230202420157847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108309279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99528116,0.000084806685,0.0017623288,0.000070853835,0.0000046585574,0.000019487537,0.0018339027,0.00016234357,0.00078048377],"genre_scores_gemma":[0.9964103,0.000039083516,0.0015954988,0.000007821468,0.0000029331486,0.00000962928,0.0013960538,0.000010743489,0.0005279252],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985397,0.000008605623,0.000006112097,0.000022448477,0.000071843555,0.00003704808],"domain_scores_gemma":[0.99954826,0.000042749954,0.000047581856,0.000022924076,0.0002585201,0.00007987916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016891975,0.00019798777,0.00019967333,0.0010605913,0.0004769203,0.00037444974,0.0002585405,0.00016925109,0.00088210864],"category_scores_gemma":[0.0006056559,0.00010598912,0.00012584217,0.0011707258,0.00014651495,0.00019788246,0.0003475525,0.00017618517,0.00010876989],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040606273,0.00013068515,0.7796398,0.00017821041,0.00016064833,0.00093971036,0.0009225438,0.024545424,0.07315113,0.0003789119,0.003786152,0.11576087],"study_design_scores_gemma":[0.000013331841,0.000038014245,0.94773304,0.000011851796,0.000017198703,0.00010433058,0.00026921136,0.043016456,0.0063838838,0.00006188531,0.00232808,0.000022781667],"about_ca_topic_score_codex":0.5108551,"about_ca_topic_score_gemma":0.75925344,"teacher_disagreement_score":0.48914492,"about_ca_system_score_codex":0.001316993,"about_ca_system_score_gemma":0.0017595415,"threshold_uncertainty_score":0.98405117},"labels":[],"label_agreement":null},{"id":"W2108338786","doi":"10.1111/j.1365-246x.2006.03257.x","title":"Confidence intervals for earthquake source parameters","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Jackknife resampling; Multitaper; Confidence interval; Statistics; Range (aeronautics); Geodesy; Standard deviation; Mathematics; Robust confidence intervals; Geology; Seismology","score_opus":0.018384837208513798,"score_gpt":0.24105945704098378,"score_spread":0.22267461983246997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108338786","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011814294,0.00057340146,0.9846496,0.0001811633,0.000053725744,0.00005568381,0.0003510087,0.00053709274,0.0017840293],"genre_scores_gemma":[0.46302643,0.0008787769,0.5303617,0.00020941549,0.00034194993,0.0007201594,0.0026597548,0.0004212603,0.0013805536],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.98509777,0.0067185955,0.0009952639,0.0025483628,0.0041321274,0.00050796353],"domain_scores_gemma":[0.7515974,0.21470919,0.00926636,0.013256192,0.010176455,0.0009944054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.029131135,0.00122395,0.0016011099,0.006789215,0.00094788685,0.003384433,0.0038099217,0.0022122692,0.0047458597],"category_scores_gemma":[0.2111406,0.00066491764,0.0021153742,0.003448384,0.0017079585,0.0034825653,0.0023555323,0.004135093,0.0010375619],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056186854,0.0001645648,0.02812999,0.00073139946,0.0010484579,0.000698348,0.0009516122,0.33972868,0.002985907,0.26938656,0.0071555716,0.348457],"study_design_scores_gemma":[0.0001065059,0.00017383734,0.009866202,0.00047578564,0.00014370079,0.00073473796,0.0002246428,0.7402102,0.0056392876,0.23373885,0.0085072545,0.00017905133],"about_ca_topic_score_codex":0.0024556057,"about_ca_topic_score_gemma":0.0012440959,"teacher_disagreement_score":0.029131135,"about_ca_system_score_codex":0.00094383815,"about_ca_system_score_gemma":0.0007202884,"threshold_uncertainty_score":0.15406197},"labels":[],"label_agreement":null},{"id":"W2109185446","doi":"10.1002/2015jb012200","title":"Steadily propagating slip pulses driven by thermal decomposition","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Cabin pressurization; Thermal decomposition; Slip (aerodynamics); Thermal; Pore water pressure; Mechanics; Materials science; Decomposition; Thermodynamics; Geotechnical engineering; Geology; Composite material; Chemistry; Physics","score_opus":0.0633204400114171,"score_gpt":0.3476548493656741,"score_spread":0.284334409354257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109185446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9861914,0.000099445504,0.011652021,0.000058086316,0.000014893208,0.000010175035,0.000045697903,0.00012737662,0.0018008148],"genre_scores_gemma":[0.9991091,0.00002741987,0.0005373109,0.000008311218,0.0000049068376,0.0000037133432,0.000017309896,0.0000065345093,0.00028537904],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999566,0.000004691305,0.0000029802177,0.000009769931,0.00001140527,0.000014468742],"domain_scores_gemma":[0.9998198,0.000043246575,0.00005916057,0.000018933773,0.000025091667,0.00003378482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000115658215,0.00025500084,0.00020630284,0.00028343982,0.00013792068,0.000366675,0.00024196069,0.00033328068,0.0013142519],"category_scores_gemma":[0.00062730134,0.00017879186,0.0001690356,0.00014269802,0.0003239216,0.0002808877,0.0003016827,0.0003369978,0.000113331604],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009269226,0.0002974422,0.030836323,0.00023706698,0.00016159027,0.0026052601,0.0005648629,0.33907014,0.55654573,0.020825569,0.0013235719,0.046605486],"study_design_scores_gemma":[0.000028083496,0.00017059977,0.018513681,0.000015441807,0.000025155452,0.00021229297,0.00011034399,0.9429128,0.03426168,0.0031755378,0.0005514407,0.000022834376],"about_ca_topic_score_codex":0.0005307371,"about_ca_topic_score_gemma":0.0003749752,"teacher_disagreement_score":0.0013142519,"about_ca_system_score_codex":0.00027715706,"about_ca_system_score_gemma":0.00013389412,"threshold_uncertainty_score":0.0043966174},"labels":[],"label_agreement":null},{"id":"W2109716983","doi":"10.1111/j.1365-2117.2011.00531.x","title":"Compressional salt tectonics and synkinematic strata of the western <scp>K</scp>uqa foreland basin, southern <scp>T</scp>ian <scp>S</scp>han, <scp>C</scp>hina","year":2012,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"PetroChina Company Limited","keywords":"Diapir; Geology; Foreland basin; Salt tectonics; Structural basin; Sedimentary depositional environment; Geochemistry; Tectonics; Canada Basin; Anticline; Paleontology; Geomorphology","score_opus":0.05249547323962228,"score_gpt":0.29254056563635006,"score_spread":0.24004509239672778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109716983","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99969673,0.00001811409,0.000032903514,0.0000031239636,1.2064926e-7,0.0000010420757,0.000063878455,0.0000020692553,0.00018214171],"genre_scores_gemma":[0.99976164,0.000013833881,0.000055454704,0.0000015929891,2.5617172e-7,0.0000014679852,0.000099078985,0.0000011325421,0.00006557796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999052,0.000010762701,0.000011998923,0.000027423144,0.000019834904,0.000024743862],"domain_scores_gemma":[0.99979955,0.000021757955,0.00007133247,0.000019332925,0.00005731217,0.000030686504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016178335,0.0001535974,0.00020685968,0.0010019114,0.00033961504,0.00061857305,0.00022583066,0.00018870406,0.0010595042],"category_scores_gemma":[0.00034320183,0.00026799488,0.00020156246,0.0009370668,0.0005346388,0.00023643162,0.00040205475,0.00010612372,0.00014000993],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055921737,0.000015784572,0.9833545,0.000015927057,0.00006203085,0.0000882129,0.0005530203,0.0029710832,0.008653658,0.00014648066,0.00005761798,0.004025613],"study_design_scores_gemma":[0.0000017778941,0.0000059814533,0.9985581,0.0000023713114,0.000006388963,0.000013159016,0.00012285635,0.0010773308,0.00014297762,0.000013492313,0.00005364459,0.0000017979904],"about_ca_topic_score_codex":0.14410049,"about_ca_topic_score_gemma":0.24096133,"teacher_disagreement_score":0.14410049,"about_ca_system_score_codex":0.0008653401,"about_ca_system_score_gemma":0.00071530504,"threshold_uncertainty_score":0.28652346},"labels":[],"label_agreement":null},{"id":"W2109772362","doi":"10.1130/b30383.1","title":"Foreland basin subsidence driven by topographic growth versus plate subduction","year":2011,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Royal Society of Edinburgh; Scottish Government","keywords":"Foreland basin; Geology; Citation; Subduction; Subsidence; Icon; Paleontology; Structural basin; Library science; Computer science; Tectonics","score_opus":0.023692794219992017,"score_gpt":0.19650525437507774,"score_spread":0.17281246015508572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109772362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.56173515,0.004742131,0.0009478669,0.0063196733,0.0006280008,0.000088870795,0.005971239,0.00039590505,0.41917107],"genre_scores_gemma":[0.9654426,0.0024894744,0.0002385499,0.00020246087,0.00019506211,0.000010861807,0.0017732581,0.00008739055,0.029560342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998977,0.000007686147,0.0000069446696,0.000020375053,0.000040419665,0.000026866306],"domain_scores_gemma":[0.999851,0.000019622246,0.00004348962,0.000014640568,0.000044873475,0.000026430116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017582755,0.00017528703,0.00029207458,0.00070253754,0.0003280012,0.0014551801,0.00028091957,0.0004350581,0.023146473],"category_scores_gemma":[0.0007401722,0.00013689908,0.0002634922,0.0009359715,0.0004535418,0.00055048906,0.00073615625,0.00041967133,0.0025830641],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015488854,0.00024446094,0.3025479,0.0014773925,0.00029005395,0.0037922314,0.0024394651,0.012371989,0.03778441,0.06264119,0.30188808,0.27297392],"study_design_scores_gemma":[0.00010972365,0.00018065133,0.82851905,0.00023492941,0.00009652377,0.00076504005,0.0013939372,0.006776758,0.0046300823,0.007553203,0.14969324,0.00004692762],"about_ca_topic_score_codex":0.023578053,"about_ca_topic_score_gemma":0.04188575,"teacher_disagreement_score":0.023578053,"about_ca_system_score_codex":0.0011997672,"about_ca_system_score_gemma":0.000668659,"threshold_uncertainty_score":0.07743269},"labels":[],"label_agreement":null},{"id":"W2110082266","doi":"10.1029/2002gl015986","title":"Prolonged post‐seismic deformation of the 1960 great Chile earthquake and implications for mantle rheology","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Subduction; Mantle (geology); Deformation (meteorology); Slip (aerodynamics); Geophysics; Tectonics","score_opus":0.03909561833715969,"score_gpt":0.26922787059837233,"score_spread":0.23013225226121264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110082266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972964,0.0005580851,0.00006674676,0.00034293946,0.000005907091,0.0000020478083,0.00012400749,0.0000076141782,0.0015962188],"genre_scores_gemma":[0.9995478,0.0001605348,0.000016245212,0.000011936755,0.0000059675776,0.0000010677444,0.00003575084,0.0000016175946,0.00021917553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993813,0.0000123816335,0.000006021404,0.000011970812,0.0000085425,0.000022861546],"domain_scores_gemma":[0.99974793,0.000055734414,0.000083888895,0.00003495996,0.00003329787,0.00004425063],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021439372,0.00014211386,0.0001955227,0.0004225224,0.00026769456,0.0006117841,0.00023509031,0.00047829587,0.002278346],"category_scores_gemma":[0.0012333503,0.00015593358,0.0001864811,0.0005082301,0.0006508801,0.0007300242,0.00045888816,0.00021396914,0.00028057562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001005094,0.00010147285,0.8928744,0.000204963,0.000105122046,0.0043455022,0.001835654,0.016448973,0.047514774,0.0031382183,0.0012940799,0.031131713],"study_design_scores_gemma":[0.000011970447,0.000037399357,0.9953761,0.0000144374635,0.000007357385,0.00018152288,0.00055943243,0.0018744541,0.0005064007,0.0006862944,0.0007326406,0.00001196756],"about_ca_topic_score_codex":0.016288092,"about_ca_topic_score_gemma":0.013317527,"teacher_disagreement_score":0.016288092,"about_ca_system_score_codex":0.0010518167,"about_ca_system_score_gemma":0.00029078065,"threshold_uncertainty_score":0.0323866},"labels":[],"label_agreement":null},{"id":"W2110103587","doi":"10.1016/j.epsl.2013.02.019","title":"Results for aseismic creep on the Hayward fault using polarization persistent scatterer InSAR","year":2013,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Canadian Space Agency; Institute for Catastrophic Loss Reduction; Government of Canada; San Francisco State University","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Creep; San andreas fault; Polarization (electrochemistry); Fault (geology); Geodesy; Remote sensing; Synthetic aperture radar","score_opus":0.027141511232135998,"score_gpt":0.2041756281479773,"score_spread":0.1770341169158413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110103587","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98623914,0.00015002464,0.0030278368,0.0001903153,0.000044004395,0.00002429755,0.0045497366,0.00042179687,0.005352935],"genre_scores_gemma":[0.9873362,0.00009809548,0.0054596514,0.00007075349,0.000031779404,0.000018402809,0.005659179,0.00011257991,0.0012133397],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99954295,0.000078275494,0.00003222619,0.00013686072,0.00010594371,0.00010384773],"domain_scores_gemma":[0.9988888,0.00033872662,0.00009416958,0.00022001164,0.00037913263,0.000079117075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009239013,0.0007985355,0.00062373537,0.00084472686,0.0009785887,0.0012677158,0.00062232453,0.0009531552,0.0023463],"category_scores_gemma":[0.0013894519,0.00041723324,0.0011204499,0.0012540467,0.00044886614,0.0012277565,0.0005397713,0.0006177282,0.0010071525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0046875337,0.0012201178,0.56027853,0.0003691541,0.0018900798,0.0016112246,0.00087710685,0.25319877,0.089206986,0.0017315161,0.010240693,0.07468833],"study_design_scores_gemma":[0.00050320395,0.00034993578,0.7775614,0.0000479823,0.0010047868,0.00032669652,0.00080931373,0.18539672,0.027965866,0.0011098771,0.0047104703,0.00021380154],"about_ca_topic_score_codex":0.030427476,"about_ca_topic_score_gemma":0.05376998,"teacher_disagreement_score":0.030427476,"about_ca_system_score_codex":0.0003384271,"about_ca_system_score_gemma":0.00056916446,"threshold_uncertainty_score":0.06050074},"labels":[],"label_agreement":null},{"id":"W2110321124","doi":"10.1111/j.1365-3121.2004.00549.x","title":"Implications of the fault scaling law for the growth of topography: mountain ranges in the broken foreland of north‐east Tibet","year":2004,"lang":"en","type":"article","venue":"Terra Nova","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institute of Particle Physics","funders":"Core Research for Evolutional Science and Technology","keywords":"Geology; Foreland basin; Tectonics; Fault (geology); Scaling; Elevation (ballistics); Erosion; Geomorphology; Seismology; Geodesy; Geometry","score_opus":0.033295808088023175,"score_gpt":0.24465697692738816,"score_spread":0.21136116883936498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110321124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99727136,0.00009958265,0.0011996375,0.00008540646,0.000003328167,0.000003834151,0.000110146306,0.000024005554,0.0012027844],"genre_scores_gemma":[0.999691,0.000020900909,0.00018247953,0.0000032707744,0.0000018180519,9.119561e-7,0.000049771603,0.0000019738043,0.000047860136],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999174,0.000021009673,0.000006597911,0.000023157547,0.000015874914,0.000016084512],"domain_scores_gemma":[0.99960417,0.00011511869,0.00011109502,0.00004648812,0.00008474723,0.0000384417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040436102,0.0001347402,0.00011550699,0.001013724,0.0002967986,0.0008146282,0.00028323804,0.00023158925,0.0017485538],"category_scores_gemma":[0.0017078496,0.0001366716,0.00015677532,0.0008674374,0.000692615,0.0004105377,0.00024395261,0.00021385249,0.00015747981],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010451469,0.000033126806,0.91155535,0.00004047587,0.000048077833,0.00040045174,0.0004429759,0.04438301,0.008856997,0.003469126,0.0002807271,0.030385302],"study_design_scores_gemma":[0.000011622818,0.00003856718,0.9349595,0.000012267764,0.000009188025,0.00026642767,0.0002961899,0.06196643,0.00041595395,0.0016041885,0.0004059489,0.000013788703],"about_ca_topic_score_codex":0.016460624,"about_ca_topic_score_gemma":0.01289109,"teacher_disagreement_score":0.016460624,"about_ca_system_score_codex":0.00087409996,"about_ca_system_score_gemma":0.00020177262,"threshold_uncertainty_score":0.032729626},"labels":[],"label_agreement":null},{"id":"W2110420267","doi":"10.1029/2002tc001475","title":"Upward delamination of Cascadia Basin sediment infill with landward frontal accretion thrusting caused by rapid glacial age material flux","year":2004,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Bundesministerium für Bildung und Forschung; Leibniz-Gemeinschaft; U.S. Geological Survey; Deutsche Forschungsgemeinschaft","keywords":"Geology; Accretionary wedge; Subduction; Foreland basin; Accretion (finance); Passive margin; Geomorphology; Thrust fault; Paleontology; Seismology; Tectonics; Structural basin","score_opus":0.010247041707956627,"score_gpt":0.20115927330962655,"score_spread":0.19091223160166992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110420267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99896955,0.000025689636,0.00017560084,0.000021003734,0.0000017741104,0.0000015695563,0.000036172405,0.000020413217,0.00074816245],"genre_scores_gemma":[0.99966633,0.000016511622,0.000054497996,0.0000029435078,8.2770174e-7,0.0000011113933,0.000027892997,0.000002940702,0.0002270176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999105,0.000007451377,0.000008283546,0.000034363722,0.00001750203,0.000021930453],"domain_scores_gemma":[0.9998735,0.000011152132,0.000046116646,0.000022172677,0.000018246143,0.000028745095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010482079,0.00036615715,0.00019031766,0.00055308593,0.00044371435,0.00045217833,0.00027790057,0.0002468167,0.0018398874],"category_scores_gemma":[0.0003033581,0.0002931131,0.00034398882,0.00037959457,0.0004922647,0.00017149173,0.0006554742,0.0002119088,0.0001570755],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034426866,0.00008083905,0.7699577,0.00012931935,0.00014980092,0.0038241681,0.0009912021,0.028234249,0.18326092,0.0009488929,0.00041311,0.011665512],"study_design_scores_gemma":[0.000011010819,0.000059851234,0.9790319,0.0000075322723,0.000039939005,0.00037777322,0.0002740452,0.014660863,0.004761644,0.00018520308,0.0005799459,0.000010236439],"about_ca_topic_score_codex":0.023848206,"about_ca_topic_score_gemma":0.02670112,"teacher_disagreement_score":0.023848206,"about_ca_system_score_codex":0.0011024289,"about_ca_system_score_gemma":0.00044690416,"threshold_uncertainty_score":0.047418773},"labels":[],"label_agreement":null},{"id":"W2110973554","doi":"10.1111/j.1365-246x.2012.05606.x","title":"Seismic rupture and ground accelerations induced by CO2 injection in the shallow crust","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; National Energy Technology Laboratory; Dalhousie University; U.S. Department of Energy","keywords":"Geology; Crust; Seismology; Induced seismicity; Slip (aerodynamics); Acceleration; Peak ground acceleration; Fault (geology); Fluid dynamics; Geotechnical engineering; Mechanics; Ground motion; Geophysics; Engineering","score_opus":0.025887032204145663,"score_gpt":0.2527205354043987,"score_spread":0.22683350320025303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110973554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974504,0.000033816967,0.0012595835,0.00003979998,0.0000065351996,0.0000055638716,0.00007206446,0.000038212424,0.0010940706],"genre_scores_gemma":[0.99960726,0.000019655872,0.00017197452,0.0000054504108,0.0000013151407,0.0000023945436,0.00003118676,0.000004190588,0.00015656561],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999324,0.0000110720885,0.000004561743,0.000010938607,0.000011171632,0.00002982325],"domain_scores_gemma":[0.9998541,0.00003972254,0.00004738459,0.00001014412,0.000014800174,0.000033850163],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013333645,0.0004309934,0.00029433574,0.0003300234,0.00023965785,0.0005397214,0.00026935973,0.00077214517,0.001236293],"category_scores_gemma":[0.0005106525,0.00022737893,0.0005333165,0.00026413356,0.00055999,0.00038300705,0.000445674,0.00039192333,0.00008460168],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002129722,0.000092858674,0.017207224,0.000050809573,0.000048554186,0.00074517546,0.00009991559,0.94393086,0.034235623,0.00085793674,0.00014604862,0.002372012],"study_design_scores_gemma":[0.000024791998,0.00009638945,0.010459037,0.0000047855942,0.000015637012,0.00004015574,0.000059130703,0.9857248,0.003264656,0.00020786058,0.00008980681,0.0000129163855],"about_ca_topic_score_codex":0.010031824,"about_ca_topic_score_gemma":0.0038469946,"teacher_disagreement_score":0.010031824,"about_ca_system_score_codex":0.00066838856,"about_ca_system_score_gemma":0.00032000436,"threshold_uncertainty_score":0.019946873},"labels":[],"label_agreement":null},{"id":"W2111002935","doi":"10.1002/grl.50374","title":"Thermal structure and megathrust seismogenic potential of the Makran subduction zone","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Subduction; Geology; Seismology; Induced seismicity; Episodic tremor and slip; Tsunami earthquake; Tectonics","score_opus":0.01643012888993572,"score_gpt":0.23551273789956395,"score_spread":0.21908260900962823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111002935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991026,0.00002181898,0.00014463646,0.000018410485,8.1088444e-7,0.0000016701174,0.000029169662,0.000005905454,0.0006750353],"genre_scores_gemma":[0.99985504,0.000012536116,0.00004946847,0.0000018782963,7.7363285e-7,0.0000013268618,0.00002168467,9.875363e-7,0.000056367808],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995685,0.000008155771,0.0000033403485,0.000010537355,0.0000052012374,0.000015830728],"domain_scores_gemma":[0.9998529,0.000028712557,0.00005780961,0.000014772714,0.000022670458,0.00002313098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007831569,0.000244058,0.00012795217,0.00039177836,0.00028455674,0.0006431598,0.00035425596,0.00031549466,0.00094078964],"category_scores_gemma":[0.00044627962,0.00023587231,0.00023897491,0.0002458458,0.00031536323,0.00032391355,0.00045225376,0.00021116978,0.00013656818],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043065092,0.00009105709,0.58744264,0.00007395741,0.00011338303,0.001124677,0.00069550175,0.37628204,0.022259424,0.0033348128,0.0003070488,0.007844712],"study_design_scores_gemma":[0.00006205685,0.00013808797,0.5603954,0.000028661034,0.00005017433,0.00028270195,0.00064713333,0.43439877,0.001925965,0.0013978466,0.0006221539,0.000051120714],"about_ca_topic_score_codex":0.012689162,"about_ca_topic_score_gemma":0.010799314,"teacher_disagreement_score":0.012689162,"about_ca_system_score_codex":0.0007697098,"about_ca_system_score_gemma":0.00025721308,"threshold_uncertainty_score":0.025230646},"labels":[],"label_agreement":null},{"id":"W2111107436","doi":"10.1029/2003jb002653","title":"Current tectonics of northern Cascadia from a decade of GPS measurements","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Forearc; Geology; Subduction; Seismology; Global Positioning System; Geodesy; Plate tectonics; Peninsula; Tectonics; Geography","score_opus":0.07504477967052367,"score_gpt":0.3214754212593194,"score_spread":0.2464306415887957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111107436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9569166,0.0025988738,0.00088706013,0.00056551397,0.000039726434,0.000023584633,0.011212935,0.00035158245,0.02740419],"genre_scores_gemma":[0.9896702,0.0012642732,0.0005032873,0.000029749252,0.00001157021,0.000014678069,0.0061582713,0.000019453517,0.00232855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997868,0.000016210312,0.000019340203,0.00006685029,0.000085218955,0.000025685435],"domain_scores_gemma":[0.99898,0.000054215572,0.00018512263,0.00008837625,0.00052806,0.00016419907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002952576,0.00040246162,0.00019954905,0.0023217625,0.00063010893,0.00064082304,0.00031685806,0.00016511613,0.0021038754],"category_scores_gemma":[0.0011385378,0.0001839185,0.000190991,0.0031519337,0.00037589538,0.00031883986,0.00041590948,0.00029430346,0.00034205578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000978379,0.00002524209,0.9457002,0.00035975914,0.00013354745,0.00040870588,0.0016438342,0.0059559266,0.0048415223,0.00079361023,0.0044034873,0.035636313],"study_design_scores_gemma":[0.000002471999,0.000008774284,0.9930823,0.000031688425,0.000019850468,0.000048085552,0.00022028013,0.0004951956,0.0001368767,0.00007785846,0.0058707967,0.000005676071],"about_ca_topic_score_codex":0.5531244,"about_ca_topic_score_gemma":0.6853028,"teacher_disagreement_score":0.5531244,"about_ca_system_score_codex":0.0041768495,"about_ca_system_score_gemma":0.002444804,"threshold_uncertainty_score":0.8990146},"labels":[],"label_agreement":null},{"id":"W2112214252","doi":"10.1038/nature03903","title":"A wide depth distribution of seismic tremors along the northern Cascadia margin","year":2005,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":203,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Subduction; Episodic tremor and slip; Slip (aerodynamics); Submarine pipeline; Triple junction; Magnitude (astronomy); Plate tectonics; Geodesy; Geophysics; Tectonics; Oceanography","score_opus":0.007151598788305137,"score_gpt":0.20750449295940035,"score_spread":0.20035289417109522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112214252","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99796754,0.00010460384,0.00009240619,0.000040536437,0.0000016561015,0.0000014546562,0.0001867577,0.000009331324,0.0015956243],"genre_scores_gemma":[0.9994392,0.000059090075,0.00003368611,0.000008479908,0.0000027965555,0.0000011053816,0.000119755525,0.0000019428098,0.00033393616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999037,0.000009085225,0.00000737738,0.000036164678,0.000023544524,0.000020036057],"domain_scores_gemma":[0.99962556,0.000070923335,0.00008432779,0.000034621688,0.000082156854,0.00010237408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016324384,0.0001566371,0.00018280516,0.0012223125,0.0004056018,0.0004024363,0.00012138286,0.00021441968,0.0015983491],"category_scores_gemma":[0.00053405284,0.00015558145,0.000116207535,0.0010468723,0.0004366157,0.00025243452,0.000717054,0.00014518859,0.00017040597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027549118,0.00001730916,0.92487687,0.000070796465,0.00006897408,0.0003814838,0.0034563085,0.0006431336,0.04978976,0.0002935151,0.00036655713,0.01975973],"study_design_scores_gemma":[0.0000010007625,0.0000065191107,0.99945515,0.0000015496122,0.0000031389511,0.000038370814,0.00017186654,0.000028830704,0.00006029333,0.000017356811,0.00021439619,0.0000014931838],"about_ca_topic_score_codex":0.015473146,"about_ca_topic_score_gemma":0.049686454,"teacher_disagreement_score":0.015473146,"about_ca_system_score_codex":0.00027638706,"about_ca_system_score_gemma":0.0002104207,"threshold_uncertainty_score":0.03076619},"labels":[],"label_agreement":null},{"id":"W2112785012","doi":"10.1111/j.1365-246x.2011.05134.x","title":"Earthquake precursors: activation or quiescence?","year":2011,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Nucleation; Induced seismicity; Seismology; Geology; Event (particle physics); Magnitude (astronomy); Foreshock; Earthquake prediction; Fault (geology); Range (aeronautics); Statistical physics; Physics; Engineering","score_opus":0.04517624146118478,"score_gpt":0.2444906318299102,"score_spread":0.19931439036872545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112785012","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97403777,0.00047166264,0.016229315,0.0012352642,0.000022181723,0.000035406087,0.00042537152,0.00017911705,0.007363895],"genre_scores_gemma":[0.9984692,0.00018656062,0.0007155898,0.000042778804,0.000017451437,0.0000060884236,0.000110891226,0.000014672715,0.0004367324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997725,0.000052593583,0.000013761108,0.0000727062,0.000040144976,0.000048349793],"domain_scores_gemma":[0.9969506,0.0015085703,0.0008353025,0.00023303115,0.00016897722,0.00030349402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006018368,0.00033237794,0.00039199114,0.0005922935,0.00024271209,0.0013433287,0.00068611425,0.00059414003,0.0023378746],"category_scores_gemma":[0.006497023,0.000221765,0.0002896299,0.0005863293,0.00084324036,0.0017177713,0.0007306865,0.000675414,0.00025365409],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060972787,0.00014493603,0.65864724,0.00033061122,0.0001618813,0.0015793666,0.0024608395,0.17476203,0.00696722,0.09341149,0.003328517,0.057596095],"study_design_scores_gemma":[0.00014282546,0.0006943324,0.2841437,0.00008098905,0.00017466728,0.002058648,0.002679275,0.5884297,0.0048795366,0.1072435,0.009366911,0.000105937324],"about_ca_topic_score_codex":0.010571825,"about_ca_topic_score_gemma":0.009045663,"teacher_disagreement_score":0.010571825,"about_ca_system_score_codex":0.00056290085,"about_ca_system_score_gemma":0.00036144583,"threshold_uncertainty_score":0.021020591},"labels":[],"label_agreement":null},{"id":"W2112814144","doi":"10.1785/gssrl.75.3.419","title":"Historical Seismicity in the Central Highlands, Passamaquoddy Bay, and Moncton Regions of New Brunswick, Canada, 1817-1961","year":2004,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Induced seismicity; Citation; Newspaper; Icon; Bay; History; Library science; Archaeology; Geology; Media studies; Seismology; Sociology; Computer science","score_opus":0.06239628088682099,"score_gpt":0.26918213991779455,"score_spread":0.20678585903097357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112814144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7994992,0.020219434,0.00020852967,0.0052149002,0.00031829,0.00017373495,0.10570865,0.00014184717,0.06851534],"genre_scores_gemma":[0.9159168,0.013507426,0.0005764858,0.00048518248,0.00009415079,0.00009724503,0.03092316,0.000060902454,0.03833862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99953425,0.000014335227,0.00002614482,0.00006002477,0.00015711236,0.00020811823],"domain_scores_gemma":[0.9982862,0.00006440135,0.00023411792,0.000052511343,0.0010284154,0.00033436654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003293737,0.0004940519,0.00037146406,0.0037420874,0.0030764795,0.0016027786,0.001020934,0.00051224645,0.006807567],"category_scores_gemma":[0.0012928138,0.00033374745,0.0002257452,0.007847252,0.0012217206,0.00048495905,0.0014062915,0.0006096767,0.0010695384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034192097,0.000054200482,0.7794256,0.0008609178,0.00017266042,0.0016537656,0.016867625,0.0009482667,0.0032948342,0.0019282505,0.116391316,0.07806057],"study_design_scores_gemma":[0.0000101592,0.000007964297,0.9588815,0.00018529796,0.000015925609,0.00012968406,0.0043706493,0.0000579832,0.00018862372,0.000044477743,0.036090303,0.000017377632],"about_ca_topic_score_codex":0.9937449,"about_ca_topic_score_gemma":0.99876344,"teacher_disagreement_score":0.03323712,"about_ca_system_score_codex":0.03323712,"about_ca_system_score_gemma":0.03806079,"threshold_uncertainty_score":0.2411533},"labels":[],"label_agreement":null},{"id":"W2113044873","doi":"10.1007/s00024-006-0134-y","title":"Stress Shadows Determined from a Phase Dynamical Measure of Historic Seismicity","year":2006,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Basic Energy Sciences; U.S. Department of Energy; University of California, Davis; Southern California Earthquake Center; Los Alamos National Laboratory; U.S. Geological Survey; National Science Foundation","keywords":"Induced seismicity; Geology; Seismology; Proxy (statistics); Stress (linguistics); Shadow (psychology); Geophysics; Mathematics; Statistics","score_opus":0.00881678131211492,"score_gpt":0.19257432305585068,"score_spread":0.18375754174373576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113044873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929925,0.000039551916,0.0041074553,0.000014227369,0.0000066764546,0.000004419092,0.0006762294,0.000039471466,0.0021194313],"genre_scores_gemma":[0.9989322,0.000017909828,0.00056248286,0.000001102987,0.000005243586,0.0000014674192,0.00036847527,0.000007002442,0.00010404074],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999393,0.000008924505,0.0000047310937,0.0000198693,0.000014190377,0.000012939847],"domain_scores_gemma":[0.99926955,0.0002513342,0.00013410192,0.000083717554,0.00017330129,0.00008800617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020732252,0.0001162388,0.00010554847,0.0016523249,0.00021527246,0.0004193642,0.00011277931,0.00010470381,0.0016906825],"category_scores_gemma":[0.002129984,0.00009873278,0.00009584598,0.0014252253,0.00019290723,0.0003756552,0.00019108917,0.00014219072,0.00020393346],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00084473,0.000092309405,0.80336076,0.00011616262,0.00010285002,0.00028523727,0.0008407084,0.03922985,0.05658571,0.0069304365,0.0013319037,0.090279266],"study_design_scores_gemma":[0.000011491112,0.00006906736,0.9265959,0.000008193958,0.000025056706,0.00017497147,0.000182079,0.065818496,0.004722041,0.0010807111,0.0012954313,0.000016564094],"about_ca_topic_score_codex":0.0031456472,"about_ca_topic_score_gemma":0.007163429,"teacher_disagreement_score":0.0031456472,"about_ca_system_score_codex":0.0003416113,"about_ca_system_score_gemma":0.00016753832,"threshold_uncertainty_score":0.006254673},"labels":[],"label_agreement":null},{"id":"W2114371073","doi":"10.1016/j.epsl.2015.06.044","title":"Dynamic triggering of creep events in the Salton Trough, Southern California by regional<mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" altimg=\"si1.gif\" overflow=\"scroll\"><mml:mi mathvariant=\"normal\">M</mml:mi><mml:mo>≥</mml:mo><mml:mn>5.4</mml:mn></mml:math>earthquakes constrained by geodetic observations and numerical simulations","year":2015,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Creep; Geology; Seismology; Slip (aerodynamics); Trough (economics); Interferometric synthetic aperture radar; Geothermal gradient; Fault (geology); Tectonics; Amplitude; Geophysics; Synthetic aperture radar","score_opus":0.01834149845568014,"score_gpt":0.21171232710516155,"score_spread":0.1933708286494814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114371073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99564004,0.00004845258,0.00013742475,0.00008578909,0.00000617384,0.0000096133435,0.0010738368,0.000044029784,0.002954708],"genre_scores_gemma":[0.9990374,0.000026461299,0.00007693817,0.0000050724643,0.0000026713676,0.00000405311,0.00043459542,0.000004093916,0.0004088707],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999523,0.0000041372496,0.000004171871,0.000018427583,0.0000070729766,0.000013860278],"domain_scores_gemma":[0.9997253,0.00004796427,0.000063918,0.000015788935,0.000059169197,0.000087930675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012655734,0.00016654587,0.00014983026,0.0005980338,0.00041577927,0.00053570623,0.0003136885,0.00036538008,0.0035774508],"category_scores_gemma":[0.00063214713,0.00022912037,0.00015134137,0.00038461864,0.00027263767,0.00029938848,0.00048819883,0.0002502488,0.00025231924],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00096110866,0.00025563544,0.9205362,0.000100175515,0.00015174554,0.0005781479,0.00074113667,0.04061677,0.006585736,0.0012105539,0.009425943,0.018836925],"study_design_scores_gemma":[0.000067627465,0.000052316704,0.97639126,0.000019248111,0.000040889914,0.000027530736,0.00025686968,0.021911418,0.00027939212,0.00017675842,0.0007650261,0.000011518745],"about_ca_topic_score_codex":0.21752444,"about_ca_topic_score_gemma":0.3611965,"teacher_disagreement_score":0.21752444,"about_ca_system_score_codex":0.00091750093,"about_ca_system_score_gemma":0.0006310729,"threshold_uncertainty_score":0.43251663},"labels":[],"label_agreement":null},{"id":"W2114377958","doi":"10.1785/gssrl.75.5.626","title":"The 20 April 2002, Mw 5.0 Au Sable Forks, New York, Earthquake: A Supplementary Source of Knowledge on Earthquake Damage to Lifelines and Buildings in Eastern North America","year":2004,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Response Biomedical (Canada); Natural Resources Canada; Hydro-Québec","funders":"New York State Department of Transportation","keywords":"Citation; History; Art history; Library science; Archaeology; Computer science","score_opus":0.06242273321673112,"score_gpt":0.2986159671296293,"score_spread":0.23619323391289818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114377958","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0026501657,0.011001206,0.0003419083,0.006087913,0.0030039148,0.00018319438,0.79525006,0.0012051458,0.1802765],"genre_scores_gemma":[0.009402192,0.02097454,0.0010216689,0.0014102253,0.0019072196,0.00023572768,0.57062846,0.000979964,0.39344004],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9993948,0.000018404193,0.00004446958,0.000059627764,0.00040551848,0.00007718548],"domain_scores_gemma":[0.9962824,0.0002991594,0.0003043232,0.0001393224,0.0024988446,0.00047598552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044954446,0.0008369779,0.0011907921,0.009154407,0.0016363186,0.0037750192,0.0012945049,0.0016578742,0.27959102],"category_scores_gemma":[0.00397263,0.00047800326,0.000539771,0.020748978,0.00026902094,0.002150013,0.0023043477,0.0009011445,0.13610582],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014556772,0.0000051758,0.00046176102,0.00046891486,0.0000046226237,0.000063872656,0.000086060216,0.000022654036,0.000048574566,0.000058419035,0.98629874,0.012466746],"study_design_scores_gemma":[0.000012485794,0.00000507933,0.009383433,0.0006349744,0.000013276668,0.000045607372,0.00032770704,0.00002601747,0.00007969428,0.00006369531,0.98939776,0.000010406039],"about_ca_topic_score_codex":0.26383227,"about_ca_topic_score_gemma":0.45222816,"teacher_disagreement_score":0.27959102,"about_ca_system_score_codex":0.0033067665,"about_ca_system_score_gemma":0.008753283,"threshold_uncertainty_score":0.93532515},"labels":[],"label_agreement":null},{"id":"W2114405497","doi":"10.1111/1365-2478.12267","title":"Mode‐converted volcanogenic massive sulphide ore lens reflections in vertical seismic profiles from Flin Flon, Manitoba, Canada","year":2015,"lang":"en","type":"article","venue":"Geophysical Prospecting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Carleton University; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Vertical seismic profile; Gemology; Dynamite; Mode (computer interface); Petrology; Mineralogy; Volcanism; Engineering geology","score_opus":0.035491855789241626,"score_gpt":0.2359467615871193,"score_spread":0.20045490579787767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114405497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976533,0.000021857171,0.00035240647,0.000032289623,0.0000018847226,0.000012673011,0.0005463889,0.000036832324,0.0013423929],"genre_scores_gemma":[0.9977208,0.000033136745,0.0006869726,0.000009002404,5.824577e-7,0.0000051478764,0.0007122364,0.000007744388,0.0008243883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992895,0.000005096566,0.000002183264,0.000014861083,0.000024808623,0.000024103958],"domain_scores_gemma":[0.99988997,0.000012489096,0.000008043781,0.0000062998024,0.00006412533,0.000019163694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116080955,0.00028783592,0.00013719154,0.00048770092,0.000622866,0.0004879294,0.00051691436,0.00028616763,0.001281828],"category_scores_gemma":[0.0003329301,0.00025359483,0.00020934548,0.0007142795,0.00031781345,0.00013955834,0.0001938812,0.00021233413,0.00017123438],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009722189,0.00028184237,0.66538066,0.00019416517,0.00019505528,0.0017301843,0.0030177513,0.19556199,0.07483726,0.00075297424,0.0030059502,0.05407],"study_design_scores_gemma":[0.00006998356,0.00012368149,0.86330366,0.000031917505,0.00004199524,0.00015454719,0.002032185,0.12428652,0.007191798,0.00012656586,0.0025812974,0.000055829823],"about_ca_topic_score_codex":0.9492988,"about_ca_topic_score_gemma":0.9804146,"teacher_disagreement_score":0.0507012,"about_ca_system_score_codex":0.0060952273,"about_ca_system_score_gemma":0.004815421,"threshold_uncertainty_score":0.10199952},"labels":[],"label_agreement":null},{"id":"W2114606822","doi":"10.1002/2015gc005828","title":"Constraints on the evolution of crustal flow beneath <scp>N</scp>orthern <scp>T</scp>ibet","year":2015,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science Foundation Ireland","keywords":"Geology; Crust; Terrane; Plateau (mathematics); Fault (geology); Tectonics; Igneous rock; Petrology; Structural basin; Geochemistry; Geomorphology; Seismology","score_opus":0.01718296712952988,"score_gpt":0.19824483693486947,"score_spread":0.1810618698053396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114606822","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99790835,0.000024190822,0.0006835084,0.000008388012,5.678977e-7,0.000001862875,0.00012531932,0.0000122454185,0.0012356784],"genre_scores_gemma":[0.9995179,0.000007866923,0.00024610106,0.0000018273071,4.0583421e-7,0.000002216011,0.00015335024,0.000002743445,0.000067685854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999461,0.000007748926,0.0000041089643,0.000016469246,0.000010544601,0.000015066821],"domain_scores_gemma":[0.9997824,0.00007235167,0.000048333306,0.000021374999,0.000047839596,0.0000277354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015563234,0.00021195406,0.00018983158,0.00046170113,0.00036561006,0.0006152394,0.00027070646,0.00020589706,0.0014886268],"category_scores_gemma":[0.0006419035,0.00016136398,0.00018033572,0.00030188984,0.00021945774,0.00025234884,0.00028134842,0.00016198031,0.0001512065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003972708,0.0000840108,0.62418026,0.000109904795,0.0000801457,0.00060760987,0.00023737398,0.18425934,0.17153913,0.0019531057,0.00034862594,0.016203316],"study_design_scores_gemma":[0.00003383639,0.00007514294,0.7138022,0.000024114574,0.00002345104,0.00012370523,0.00018743762,0.27467653,0.009658184,0.00057076913,0.0007991792,0.000025463489],"about_ca_topic_score_codex":0.025339643,"about_ca_topic_score_gemma":0.027233856,"teacher_disagreement_score":0.025339643,"about_ca_system_score_codex":0.0005272173,"about_ca_system_score_gemma":0.0005236938,"threshold_uncertainty_score":0.050384283},"labels":[],"label_agreement":null},{"id":"W2114750030","doi":"10.1785/gssrl.79.3.457","title":"The 2006-2007 Earthquake Sequence at Bar Harbor, Maine","year":2008,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Sequence (biology); Bar (unit); Geology; Seismology; Oceanography; Biology","score_opus":0.10604377582693168,"score_gpt":0.3065538126873459,"score_spread":0.2005100368604142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114750030","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893271,0.00029198898,0.00013717313,0.0010451318,0.0000811933,0.000039534993,0.004545514,0.000048614034,0.004483854],"genre_scores_gemma":[0.9827476,0.0003768837,0.0003964799,0.00030168673,0.00011558565,0.000037739494,0.007148222,0.000012088858,0.008863553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988973,0.000007908309,0.000007384879,0.000022177626,0.000044304626,0.00002839918],"domain_scores_gemma":[0.99967134,0.000013427955,0.00010797153,0.00001110734,0.00011519253,0.00008089826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015764612,0.00019067076,0.00015664293,0.0008856446,0.00046946516,0.0003602351,0.00027858527,0.00034429703,0.0024849277],"category_scores_gemma":[0.00036691088,0.00009966329,0.00006354309,0.0005750163,0.0002331554,0.0003304623,0.00060701685,0.00029051764,0.0007342817],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013577429,0.00017913782,0.9358698,0.00012095746,0.000062309904,0.0017556538,0.002608923,0.00048390188,0.008903535,0.00020877624,0.025890455,0.023780808],"study_design_scores_gemma":[0.0000027591702,0.000021987651,0.9945973,0.000012903778,0.0000042101824,0.000066054075,0.0005389892,0.00015596168,0.00017470613,0.000014169054,0.0044087362,0.0000022395577],"about_ca_topic_score_codex":0.07168251,"about_ca_topic_score_gemma":0.30203417,"teacher_disagreement_score":0.07168251,"about_ca_system_score_codex":0.0011261377,"about_ca_system_score_gemma":0.00097121793,"threshold_uncertainty_score":0.14253056},"labels":[],"label_agreement":null},{"id":"W2115179805","doi":"10.1785/0120090167","title":"Earthquake Source Scaling: m1 versus Other Magnitude Scales","year":2010,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey","keywords":"Magnitude (astronomy); Scaling; Earthquake magnitude; Geology; Seismology; Richter magnitude scale; Geodesy; Mathematics; Physics; Geometry","score_opus":0.017137910574159327,"score_gpt":0.21949343841507224,"score_spread":0.2023555278409129,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115179805","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9554623,0.0008503451,0.018293414,0.00039377462,0.000067659166,0.000053699914,0.00076485565,0.00033073573,0.023783186],"genre_scores_gemma":[0.9969785,0.00010689174,0.0023115969,0.000019447227,0.00005748521,0.000007965256,0.00011240748,0.000026455744,0.00037918353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986434,0.00003055072,0.000010740483,0.000032401516,0.000047005116,0.000014969576],"domain_scores_gemma":[0.9974612,0.0010764841,0.0007009323,0.00023701144,0.00038455788,0.00013977502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004654575,0.00031884958,0.00017608542,0.0022448923,0.00016188489,0.0009222421,0.00022657646,0.00027408623,0.0031648234],"category_scores_gemma":[0.005486373,0.00010544958,0.00016188242,0.0010483689,0.00039482547,0.0009481036,0.0006149802,0.00038854362,0.0004625888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009424927,0.00017247802,0.5685358,0.0005156739,0.00016285224,0.0005944567,0.0028712703,0.009208341,0.05977537,0.03854517,0.008003273,0.3106729],"study_design_scores_gemma":[0.000028719147,0.00017516119,0.953532,0.00005972982,0.00004114789,0.0002764664,0.0005880871,0.020827865,0.00423623,0.015007265,0.005184028,0.00004329507],"about_ca_topic_score_codex":0.00062667986,"about_ca_topic_score_gemma":0.00041531542,"teacher_disagreement_score":0.0031648234,"about_ca_system_score_codex":0.00024742883,"about_ca_system_score_gemma":0.00009171281,"threshold_uncertainty_score":0.010587394},"labels":[],"label_agreement":null},{"id":"W2115238422","doi":"10.1046/j.1365-246x.2000.00199.x","title":"A reappraisal of postglacial decay times from Richmond Gulf and James Bay, Canada","year":2000,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Toronto","funders":"","keywords":"Bay; Geology; Sea level; Oceanography; Series (stratigraphy); Physical geography; Paleontology; Geography","score_opus":0.00583306565703886,"score_gpt":0.20649993254993373,"score_spread":0.20066686689289487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115238422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92505646,0.008657472,0.00590685,0.0012173204,0.00014776664,0.000051583906,0.035031527,0.00025302282,0.023678025],"genre_scores_gemma":[0.9545241,0.004979225,0.008473288,0.00027810474,0.000038273643,0.00004527207,0.02123052,0.00015434476,0.010276903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995491,0.000016822889,0.00003041813,0.000066008324,0.00025648478,0.00008107573],"domain_scores_gemma":[0.9958341,0.00017275754,0.0002886274,0.00017440166,0.003333724,0.00019640473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072759023,0.0004187418,0.00031328833,0.0042547,0.0019250847,0.0014246452,0.0007865577,0.00023581451,0.001364783],"category_scores_gemma":[0.0023970716,0.00020431181,0.00044824896,0.0063546402,0.00044005705,0.00047841083,0.0007613632,0.000576044,0.00024410477],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000342011,0.00002609362,0.77386254,0.00040706326,0.0003391817,0.00040824336,0.0032918788,0.0045354962,0.007782891,0.0031944315,0.018147506,0.18766254],"study_design_scores_gemma":[0.000006808024,0.000010995933,0.95497584,0.000111956106,0.000072201066,0.00007933306,0.00079832005,0.0022210034,0.002049914,0.0001383109,0.039495684,0.000039597042],"about_ca_topic_score_codex":0.98278296,"about_ca_topic_score_gemma":0.9927878,"teacher_disagreement_score":0.01721704,"about_ca_system_score_codex":0.01665529,"about_ca_system_score_gemma":0.018679878,"threshold_uncertainty_score":0.12084317},"labels":[],"label_agreement":null},{"id":"W2115729717","doi":"10.1029/2009jb006338","title":"Ultrahigh‐resolution seismic reflection imaging of the Alpine Fault, New Zealand","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Seismology; Fault (geology); Geophysical imaging; Basement; Active fault; Quaternary; Paleontology","score_opus":0.0289219555546826,"score_gpt":0.3039703679226336,"score_spread":0.275048412367951,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115729717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99504,0.0002731561,0.0008601191,0.00007894553,0.0000041302565,0.000025748875,0.00074542203,0.000047735153,0.0029247478],"genre_scores_gemma":[0.99445724,0.000421993,0.0027859614,0.000021156538,0.000007461501,0.000014714982,0.00063396245,0.000013986446,0.0016435386],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99990356,0.0000042396573,0.0000071038007,0.000023518265,0.00004435009,0.000017197472],"domain_scores_gemma":[0.9998222,0.000013285789,0.00006076384,0.000012831487,0.00006399874,0.000026937112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018631884,0.0002386937,0.00012452221,0.00088753767,0.0002579914,0.00047061127,0.00026048478,0.00018371484,0.0013176642],"category_scores_gemma":[0.00042457102,0.00021243092,0.00011492898,0.0007168869,0.00024648325,0.0004102767,0.00030904525,0.00019527882,0.00021421736],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034379988,0.000103287995,0.23066981,0.0002881405,0.00007431556,0.0017285537,0.002621541,0.0018869272,0.6703738,0.00025366485,0.0014764616,0.09017965],"study_design_scores_gemma":[0.000022039965,0.00006828968,0.990763,0.000020327494,0.000025089184,0.0005745374,0.00044929507,0.0013188142,0.00433513,0.000025937743,0.0023833942,0.000014050745],"about_ca_topic_score_codex":0.13209987,"about_ca_topic_score_gemma":0.2703971,"teacher_disagreement_score":0.13209987,"about_ca_system_score_codex":0.00051488716,"about_ca_system_score_gemma":0.000438103,"threshold_uncertainty_score":0.26266193},"labels":[],"label_agreement":null},{"id":"W2115818059","doi":"10.1785/0120000044","title":"Characterization of Active Faulting Beneath the Strait of Georgia, British Columbia","year":2000,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Active fault; Fault (geology); Archaeology; Oceanography; Geography","score_opus":0.008921654854416672,"score_gpt":0.18435569105999272,"score_spread":0.17543403620557604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115818059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959657,0.00010136197,0.00019300502,0.000038430528,0.000001927644,0.000013741997,0.0007410357,0.000023859877,0.002920978],"genre_scores_gemma":[0.9969748,0.00009991696,0.00030868888,0.000017793524,0.0000010660364,0.0000055934456,0.001035611,0.000006168042,0.0015503233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987495,0.0000050563317,0.000006789441,0.000026937814,0.000041783744,0.000044387878],"domain_scores_gemma":[0.99957234,0.00001971453,0.000052987936,0.000016787537,0.00024807666,0.00008998719],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000691362,0.00027440628,0.00013807268,0.001635022,0.0008176017,0.00071078754,0.00040221427,0.00023293123,0.0014123665],"category_scores_gemma":[0.00047034776,0.00016609153,0.00007751319,0.0019798167,0.0002579609,0.00014989599,0.0003837016,0.00014758437,0.00029110018],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008517588,0.00003097359,0.93819565,0.00005540672,0.000032776905,0.00074634724,0.0009742198,0.0017265577,0.021380354,0.00019802172,0.0013377703,0.03523677],"study_design_scores_gemma":[0.0000015990848,0.0000065993813,0.99726284,0.000008359786,0.0000049311493,0.00007353178,0.00039804773,0.0010116568,0.00037663695,0.000008754015,0.00084345054,0.0000036564343],"about_ca_topic_score_codex":0.910708,"about_ca_topic_score_gemma":0.9783659,"teacher_disagreement_score":0.08929199,"about_ca_system_score_codex":0.0026934838,"about_ca_system_score_gemma":0.002435889,"threshold_uncertainty_score":0.17963564},"labels":[],"label_agreement":null},{"id":"W2116077368","doi":"10.1785/0120130173","title":"Seismic Source Studies for Chemical Explosions in Granite","year":2013,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Citation; Suite; Library science; Geology; Download; Information retrieval; History; Computer science; Archaeology; World Wide Web","score_opus":0.028967640972703955,"score_gpt":0.23220021112000555,"score_spread":0.2032325701473016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116077368","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9110316,0.00659507,0.008875035,0.0017273457,0.00024538522,0.00033911382,0.010916105,0.0006405192,0.059629813],"genre_scores_gemma":[0.9737583,0.005653007,0.0033487815,0.00006334147,0.0001390302,0.00009782621,0.008186284,0.00021558425,0.008537862],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996594,0.000035513618,0.000025995034,0.000034661352,0.00020280093,0.00004155714],"domain_scores_gemma":[0.9993881,0.0001279328,0.00018728645,0.000052948322,0.00019117312,0.00005255206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005704233,0.0004018486,0.00030708656,0.0058237044,0.0005155536,0.00092849624,0.0005723327,0.0004282842,0.0036220313],"category_scores_gemma":[0.0022077248,0.00022158577,0.0002649841,0.0063662063,0.0003354478,0.00060310005,0.0014746421,0.0007771719,0.00072640413],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017707556,0.0004971424,0.4533472,0.0012169877,0.0006025032,0.004428515,0.012302967,0.013182379,0.018173696,0.017585957,0.057848096,0.41904384],"study_design_scores_gemma":[0.000142926,0.0002623682,0.86965674,0.0005417841,0.00027054388,0.0011261826,0.008559889,0.008778251,0.0062767225,0.0049022236,0.09939167,0.000090677306],"about_ca_topic_score_codex":0.030017596,"about_ca_topic_score_gemma":0.04219324,"teacher_disagreement_score":0.030017596,"about_ca_system_score_codex":0.0014598499,"about_ca_system_score_gemma":0.0013865947,"threshold_uncertainty_score":0.059685707},"labels":[],"label_agreement":null},{"id":"W2117705482","doi":"10.1029/2001jb001227","title":"A revised dislocation model of interseismic deformation of the Cascadia subduction zone","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":264,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Forearc; Seismology; Transition zone; Slip (aerodynamics); Geodetic datum; Deformation (meteorology); Geodesy; Plate tectonics; Tectonics; Geophysics","score_opus":0.04034635431013631,"score_gpt":0.28234717590652325,"score_spread":0.24200082159638694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117705482","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.23225465,0.0009916028,0.72391415,0.0010795349,0.00033402906,0.00021470967,0.00792171,0.0030120683,0.03027748],"genre_scores_gemma":[0.9198245,0.00074971525,0.055005137,0.0001262988,0.000064925436,0.00028205445,0.0034144733,0.00029950726,0.020233314],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998839,0.000018948154,0.000010899486,0.00003318304,0.000035429468,0.000017744247],"domain_scores_gemma":[0.99982387,0.00002810445,0.000023036771,0.00002524736,0.00007648942,0.000023228145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023161905,0.00085312536,0.0006741931,0.0005546945,0.0005003151,0.0009625036,0.0023334192,0.0009096659,0.003063105],"category_scores_gemma":[0.0006216733,0.00046578678,0.0010057593,0.0008308494,0.0003795036,0.00062483223,0.00055248284,0.0007657103,0.0006721087],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011741746,0.000008825685,0.0015948983,0.000016658843,0.000021298085,0.000064743144,0.000028224367,0.9903328,0.0009014742,0.0030604322,0.00065039773,0.0033083577],"study_design_scores_gemma":[0.00000998843,0.0000064699852,0.0004914437,0.0000029262296,0.0000082422275,0.000026579912,0.000007249696,0.99634737,0.0001495657,0.0011222602,0.0018215274,0.0000063762536],"about_ca_topic_score_codex":0.056130372,"about_ca_topic_score_gemma":0.029510036,"teacher_disagreement_score":0.056130372,"about_ca_system_score_codex":0.0012891889,"about_ca_system_score_gemma":0.0014945961,"threshold_uncertainty_score":0.11160731},"labels":[],"label_agreement":null},{"id":"W2117871563","doi":"10.1111/j.1365-246x.2008.04033.x","title":"Glacial isostatic adjustment of the British Isles: new constraints from GPS measurements of crustal motion","year":2009,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Post-glacial rebound; Geology; Geodesy; Lithosphere; Mantle (geology); Intraplate earthquake; Geophysics; Ice sheet; Seismology; Tectonics; Geomorphology","score_opus":0.024514746773035473,"score_gpt":0.23496185899186758,"score_spread":0.2104471122188321,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117871563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954385,0.00036028394,0.0011103451,0.0000948582,0.000003637854,0.00000254456,0.00027759527,0.000023140428,0.0026891117],"genre_scores_gemma":[0.99860376,0.00016100536,0.0006607279,0.000012276704,0.0000027716428,0.0000019976326,0.0003859527,0.0000076989945,0.00016394467],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972814,0.00009221307,0.000018689234,0.000056991852,0.0000728083,0.00003110967],"domain_scores_gemma":[0.9993019,0.00029565135,0.00011944971,0.00010655807,0.0001265295,0.000049857343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040056277,0.0002745324,0.00026652642,0.00076154317,0.0003084595,0.0013483642,0.0003388092,0.00023986975,0.000866657],"category_scores_gemma":[0.004420361,0.00038791873,0.0001454588,0.0012350084,0.0004423616,0.0004471108,0.00055397255,0.00038384594,0.00015027897],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024448917,0.00003320361,0.8626872,0.00013994062,0.00024156475,0.00032357938,0.0013964631,0.04923558,0.009591295,0.0020169127,0.0010665088,0.073023245],"study_design_scores_gemma":[0.000021078027,0.00002220016,0.95886934,0.00003035502,0.00003584919,0.000056740995,0.00028876995,0.037767798,0.0003460484,0.0005280195,0.0020088353,0.0000251194],"about_ca_topic_score_codex":0.3267812,"about_ca_topic_score_gemma":0.5289054,"teacher_disagreement_score":0.3267812,"about_ca_system_score_codex":0.0010315896,"about_ca_system_score_gemma":0.000805791,"threshold_uncertainty_score":0.6497583},"labels":[],"label_agreement":null},{"id":"W2118986795","doi":"10.1785/0120100336","title":"Statistical Analysis of the 2002 Mw 7.9 Denali Earthquake Aftershock Sequence","year":2011,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Seismology; Geology; Sequence (biology); Foreshock; Statistical analysis; Statistics; Mathematics","score_opus":0.037541711679480325,"score_gpt":0.22397814800363522,"score_spread":0.1864364363241549,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118986795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99843913,0.000048429752,0.0007628365,0.00003545106,0.000004408837,0.0000059852823,0.00023946966,0.000019463092,0.0004447333],"genre_scores_gemma":[0.9988391,0.000031112344,0.00022594801,0.0000047696717,0.0000082672705,0.000006230146,0.00073829864,0.000005007056,0.00014130394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997576,0.0000497087,0.000021376489,0.000073330084,0.000058619215,0.000039367616],"domain_scores_gemma":[0.9977774,0.0005529113,0.0008894028,0.00021208852,0.00038434018,0.0001839907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004395397,0.00015636403,0.00026509454,0.0014187794,0.00025539525,0.00036603553,0.00026643826,0.00024756807,0.00068658777],"category_scores_gemma":[0.0033180173,0.00010326369,0.0002081977,0.0011609951,0.00037620333,0.0002075106,0.0003167946,0.0002894331,0.00017408808],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029298448,0.00011251682,0.9015403,0.000110541936,0.0002721922,0.00085504586,0.0006757106,0.0301922,0.030135283,0.004723845,0.0016832493,0.029406153],"study_design_scores_gemma":[0.0000031485865,0.000056303463,0.962973,0.000004813913,0.000021088603,0.00014469022,0.00017152446,0.034110643,0.0012539631,0.00047180543,0.0007718913,0.000017095213],"about_ca_topic_score_codex":0.0051076123,"about_ca_topic_score_gemma":0.0051902495,"teacher_disagreement_score":0.0051076123,"about_ca_system_score_codex":0.0003219168,"about_ca_system_score_gemma":0.00018638404,"threshold_uncertainty_score":0.010155737},"labels":[],"label_agreement":null},{"id":"W2119037023","doi":"10.1306/05220605164","title":"Structurally controlled hydrothermal dolomite reservoir facies: An overview","year":2006,"lang":"en","type":"article","venue":"AAPG Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":814,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Dolomite; Facies; Geochemistry; Hydrothermal circulation; Petrology; Mining engineering; Paleontology","score_opus":0.02427421938470801,"score_gpt":0.23710440347331205,"score_spread":0.21283018408860405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119037023","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36702782,0.590438,0.009594461,0.0010881602,0.00022605581,0.00019324206,0.005719024,0.00045464557,0.02525857],"genre_scores_gemma":[0.6410167,0.32873625,0.014013049,0.00036556346,0.00059965893,0.000072760246,0.006117872,0.00012647556,0.008951618],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99974495,0.000018158846,0.000032036143,0.000067456844,0.00009392539,0.000043508328],"domain_scores_gemma":[0.99930406,0.00011886577,0.00020261655,0.00001957717,0.00026774936,0.00008705815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039138345,0.00082073535,0.0004801901,0.011219004,0.00034734764,0.0014054893,0.0006910379,0.0004042698,0.0031081364],"category_scores_gemma":[0.00059035467,0.0002919646,0.0005649428,0.0060032173,0.0005055966,0.0013787288,0.00083621853,0.00032541907,0.00071463047],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020749963,0.00010321084,0.22261283,0.0029410291,0.00025991385,0.00063358695,0.0006766193,0.0016348473,0.0073341792,0.0013349318,0.007323783,0.7549376],"study_design_scores_gemma":[0.00001436474,0.0004190197,0.6975589,0.004001743,0.0004482227,0.012022994,0.0023314853,0.0032319836,0.0062276493,0.0020232955,0.2715826,0.00013765994],"about_ca_topic_score_codex":0.0110001005,"about_ca_topic_score_gemma":0.020054448,"teacher_disagreement_score":0.011219004,"about_ca_system_score_codex":0.0006664136,"about_ca_system_score_gemma":0.00064473395,"threshold_uncertainty_score":0.021872163},"labels":[],"label_agreement":null},{"id":"W2119340201","doi":"10.1007/978-94-017-2386-2_14","title":"Earthquake Hazard for the Czech Republic, Poland and Slovakia : contribution to the ILC/IASPEI Global Seismic Hazard assessment program","year":2000,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Alberta University of the Arts","funders":"","keywords":"Seismology; Seismic hazard; Czech; Peak ground acceleration; Geology; Tectonics; Earthquake scenario; Geography; Intraplate earthquake; Structural geology; Building code; Epicenter; Hazard map; Hazard; Ground motion; Engineering; Civil engineering","score_opus":0.011000294833542822,"score_gpt":0.27574884216628787,"score_spread":0.26474854733274505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119340201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87303406,0.0036192979,0.0015370467,0.0013784576,0.00017413658,0.00030410517,0.10935116,0.00017621512,0.0104255965],"genre_scores_gemma":[0.92573565,0.003072077,0.0021950454,0.00022449733,0.000053514697,0.00020908637,0.06213112,0.00009782398,0.006281289],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996954,0.000049112936,0.0000511181,0.000033616976,0.000072018534,0.00009875991],"domain_scores_gemma":[0.999186,0.00006137528,0.00021677384,0.000043344844,0.0003205809,0.00017199895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009130312,0.0006899636,0.0005894315,0.0024026348,0.00042714155,0.0010083412,0.0006394208,0.00059502013,0.0014485589],"category_scores_gemma":[0.0011123631,0.00041297896,0.0011750651,0.002047293,0.00017798273,0.00051088765,0.0015998924,0.0004365934,0.0002771412],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019190111,0.000295771,0.84506434,0.0014926749,0.0018461542,0.00096868095,0.00062133436,0.024238365,0.0039571873,0.00132775,0.04659899,0.07166969],"study_design_scores_gemma":[0.00009572801,0.00007125193,0.9860649,0.00010242671,0.0002758028,0.00015649562,0.00048289585,0.0017850983,0.00072214694,0.000071950344,0.010150757,0.000020569265],"about_ca_topic_score_codex":0.24159504,"about_ca_topic_score_gemma":0.2795011,"teacher_disagreement_score":0.24159504,"about_ca_system_score_codex":0.00227775,"about_ca_system_score_gemma":0.006887704,"threshold_uncertainty_score":0.48037755},"labels":[],"label_agreement":null},{"id":"W2119423854","doi":"10.1002/grl.50298","title":"Numerical simulations on megathrust rupture stabilized under strong dilatancy strengthening in slow slip region","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University; Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Slip (aerodynamics); Geology; Dilatant; Episodic tremor and slip; Subduction; Seismology; Fault (geology); Geotechnical engineering; Tectonics","score_opus":0.05449481965468384,"score_gpt":0.2987603176669797,"score_spread":0.24426549801229586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119423854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9825967,0.00026688707,0.0060863486,0.00046715813,0.000059359027,0.00003308642,0.0006679439,0.0001552839,0.009667108],"genre_scores_gemma":[0.99608314,0.000104780076,0.002393648,0.000050801536,0.000009668753,0.000034600384,0.0003206533,0.000025872314,0.0009767951],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983525,0.00004128609,0.000011215827,0.00002702263,0.000022261578,0.00006290479],"domain_scores_gemma":[0.99867415,0.00074397656,0.00020064747,0.000056798195,0.00018781617,0.00013658327],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043554627,0.000616464,0.0007623753,0.0006955028,0.0006822577,0.00080329285,0.0009371074,0.0016888855,0.0032251028],"category_scores_gemma":[0.0021334023,0.0004306357,0.00079662056,0.0006755885,0.0008411418,0.00061086327,0.00068876427,0.0008931967,0.00018778292],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006823598,0.00006665288,0.0041463342,0.000031275318,0.000024705469,0.00011427561,0.000049045568,0.9923962,0.0005880629,0.0013135556,0.0002857178,0.00091587246],"study_design_scores_gemma":[0.000019918833,0.000018308921,0.0008270742,0.0000059447343,0.0000067553024,0.0000053931417,0.00003671969,0.9985354,0.00012714088,0.0003046855,0.000108069995,0.0000045735956],"about_ca_topic_score_codex":0.0329619,"about_ca_topic_score_gemma":0.022893995,"teacher_disagreement_score":0.0329619,"about_ca_system_score_codex":0.0009765732,"about_ca_system_score_gemma":0.0009940829,"threshold_uncertainty_score":0.065540075},"labels":[],"label_agreement":null},{"id":"W2121358724","doi":"10.1016/s0040-1951(01)00174-3","title":"Gravitational collapse of the continental crust: definition, regimes and modes","year":2001,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":476,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Dalhousie University","keywords":"Lithosphere; Geology; Gravitational collapse; Gravitation; Gravitational anomaly; Geophysics; Crust; Gravitational energy; Lithospheric flexure; Gravitational potential; Density contrast; Plate tectonics; Tectonics; Physics; Seismology; Classical mechanics; Astronomy","score_opus":0.01988369017942299,"score_gpt":0.20835550516949963,"score_spread":0.18847181499007665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121358724","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82494795,0.0285937,0.09849427,0.0013225687,0.0000898384,0.00008939109,0.00083132356,0.00025321497,0.045377694],"genre_scores_gemma":[0.9901276,0.003567273,0.0049284715,0.00003893064,0.00010074053,0.000020841986,0.00020516054,0.000010993623,0.0010001191],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9996495,0.000096220916,0.000045434073,0.000066948865,0.00008504716,0.000056847974],"domain_scores_gemma":[0.9991979,0.00023661758,0.00025594956,0.000089694346,0.00013257649,0.00008731022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006807723,0.0003225472,0.00027052764,0.002987136,0.00051161303,0.0015530147,0.00057509966,0.00041356284,0.0007081379],"category_scores_gemma":[0.0014153543,0.00017200792,0.00035731844,0.002170595,0.0023246384,0.0012978053,0.0013392556,0.0007086161,0.00009396804],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023614484,0.0001238321,0.21517077,0.000519173,0.00018681718,0.00042852567,0.0036806348,0.026436025,0.014506754,0.5489109,0.0031860059,0.18661444],"study_design_scores_gemma":[0.00002498825,0.00037643794,0.380288,0.00051328726,0.00014378113,0.0038463688,0.004359178,0.102507636,0.004069322,0.46617073,0.037549965,0.00015033956],"about_ca_topic_score_codex":0.0013915608,"about_ca_topic_score_gemma":0.00136811,"teacher_disagreement_score":0.002987136,"about_ca_system_score_codex":0.00046167604,"about_ca_system_score_gemma":0.00039582734,"threshold_uncertainty_score":0.0036002994},"labels":[],"label_agreement":null},{"id":"W2121628908","doi":"10.1130/0016-7606(2001)113<1010:fcovaw>2.0.co;2","title":"Fluid chemistry of veining associated with an ancient microearthquake swarm, Benmore Dam, New Zealand","year":2001,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Microearthquake; Geology; Inclusion (mineral); Library science; Archaeology; Geography; Seismology; Computer science; Mineralogy","score_opus":0.014390465109744455,"score_gpt":0.2044156849950962,"score_spread":0.19002521988535173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121628908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99181,0.000506759,0.00030265385,0.0002444283,0.000026306472,0.00002960956,0.0008304314,0.000023199045,0.006226783],"genre_scores_gemma":[0.99570054,0.00042203872,0.00039105729,0.000044139968,0.000009191749,0.00000940987,0.00049631944,0.000015585254,0.002911742],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99985087,0.000005096809,0.000005738098,0.0000309316,0.00006906866,0.000038339615],"domain_scores_gemma":[0.9998648,0.000009473297,0.00003183631,0.0000051916013,0.000055322922,0.000033391894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015479096,0.0002588767,0.00044810883,0.001233654,0.0015011922,0.00092746894,0.0002812114,0.00047776,0.0037173566],"category_scores_gemma":[0.00046526385,0.00019756047,0.00015285109,0.0013053835,0.00090975483,0.0006438813,0.00076258846,0.0005090813,0.00040064906],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011485387,0.000088114524,0.37345892,0.0007601617,0.00012736525,0.004699567,0.0068727275,0.002127722,0.5587926,0.0011710861,0.0048761526,0.04587695],"study_design_scores_gemma":[0.000041102077,0.00012334652,0.9750695,0.00004599019,0.000026578526,0.00073579815,0.0032600146,0.0012352115,0.009808537,0.00021644063,0.009399391,0.000038075465],"about_ca_topic_score_codex":0.3173221,"about_ca_topic_score_gemma":0.4221844,"teacher_disagreement_score":0.3173221,"about_ca_system_score_codex":0.0019651328,"about_ca_system_score_gemma":0.0010360256,"threshold_uncertainty_score":0.6309502},"labels":[],"label_agreement":null},{"id":"W2122171709","doi":"10.1111/j.1365-246x.2008.03856.x","title":"Wide-scale detection of earthquake waveform doublets and further evidence for inner core super-rotation","year":2008,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lamont-Doherty Earth Observatory, Columbia University; National Science Foundation","keywords":"Inner core; Geology; Seismology; Core (optical fiber); Subduction; Waveform; Geodesy; Scale (ratio); Physics; Tectonics; Geography; Cartography; Optics","score_opus":0.052695719919355524,"score_gpt":0.26982855918755855,"score_spread":0.21713283926820304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122171709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99864954,0.000103137325,0.00025313205,0.000013392844,0.0000038234157,0.000008061432,0.00019094425,0.000018176004,0.00075987977],"genre_scores_gemma":[0.9989249,0.000053916527,0.00038204787,0.000008534039,0.000007568184,0.000006681339,0.00043021378,0.0000047170133,0.000181378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986815,0.000009176788,0.000012161164,0.000035484096,0.00004133615,0.000033683118],"domain_scores_gemma":[0.9991721,0.00006730454,0.0003761967,0.000094133786,0.00010997182,0.00018035024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013001595,0.0002500916,0.00024014091,0.0011209191,0.00029935193,0.0002704624,0.00030923213,0.00020464578,0.00094674184],"category_scores_gemma":[0.00065912795,0.00016917363,0.00015484219,0.0007863479,0.00020201209,0.00017599041,0.0006766223,0.0002167936,0.0001778901],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002891722,0.000052079195,0.84624857,0.000065075474,0.00007574943,0.0010142161,0.001306081,0.00018971259,0.12484306,0.00006275879,0.0002749779,0.025578568],"study_design_scores_gemma":[0.0000025042211,0.000033425553,0.9980866,0.0000027022886,0.0000077954455,0.00031888968,0.000089711044,0.00009489835,0.00088752125,0.0000076034135,0.00046481928,0.000003498596],"about_ca_topic_score_codex":0.0051041343,"about_ca_topic_score_gemma":0.013570593,"teacher_disagreement_score":0.0051041343,"about_ca_system_score_codex":0.00017258603,"about_ca_system_score_gemma":0.00010163071,"threshold_uncertainty_score":0.010148823},"labels":[],"label_agreement":null},{"id":"W2122192876","doi":"10.1785/0120140158","title":"Coulomb Stress Changes Following the 2012 Mw 7.8 Haida Gwaii, Canada, Earthquake: Implications for Seismic Hazard","year":2015,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Resources Canada; U.S. Geological Survey","keywords":"Seismology; Seismic hazard; Geology; Hazard; Chemistry","score_opus":0.029952906366321003,"score_gpt":0.23454495066001985,"score_spread":0.20459204429369884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122192876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980579,0.000061746985,0.000073625575,0.0001444443,0.0000040739296,0.0000063112398,0.00047529195,0.000009434595,0.001167225],"genre_scores_gemma":[0.99897563,0.00012281517,0.00004891916,0.000024039859,0.0000026264483,0.000002507731,0.00035649253,0.0000037031616,0.0004633592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998505,0.000007705887,0.000005851605,0.000029658237,0.00004746524,0.000058803733],"domain_scores_gemma":[0.9994198,0.000044609424,0.0001268961,0.000023042661,0.00022153709,0.00016416598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014894751,0.00032120894,0.00027543557,0.00078258856,0.0011440701,0.0012535003,0.00073075364,0.00045234518,0.0014607281],"category_scores_gemma":[0.001611118,0.00023683454,0.00029460917,0.0013421567,0.0008312141,0.00033296912,0.0007252428,0.00050298305,0.00015196404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014051927,0.000103270104,0.9635129,0.000041205687,0.000097901815,0.0005463603,0.00072209234,0.015986744,0.0031633354,0.00040829807,0.0017670112,0.013510373],"study_design_scores_gemma":[0.000004715596,0.000014842123,0.9931276,0.0000069919865,0.000015922637,0.000025326859,0.00093548134,0.00536694,0.00017411186,0.000057353885,0.00026075344,0.000009973333],"about_ca_topic_score_codex":0.9672784,"about_ca_topic_score_gemma":0.9853212,"teacher_disagreement_score":0.03272158,"about_ca_system_score_codex":0.012688744,"about_ca_system_score_gemma":0.007440273,"threshold_uncertainty_score":0.092063665},"labels":[],"label_agreement":null},{"id":"W2122267972","doi":"10.1046/j.1365-246x.1998.00387.x","title":"Dependence of horizontal stress magnitude on load dimension in glacial rebound models","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Rijkswaterstaat","keywords":"Geology; Intraplate earthquake; Deglaciation; Lithosphere; Post-glacial rebound; Ice sheet; Mantle (geology); Viscoelasticity; Instability; Seismology; Geophysics; Inviscid flow; Mechanics; Glacial period; Tectonics; Geomorphology; Materials science","score_opus":0.02471052904139511,"score_gpt":0.23150459702148032,"score_spread":0.2067940679800852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122267972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9783157,0.00018510166,0.012997387,0.00030310833,0.000023317523,0.000019360683,0.00026819078,0.00022591834,0.0076620295],"genre_scores_gemma":[0.9981517,0.00008009763,0.00063008914,0.00001896267,0.000006459093,0.000011744415,0.00008265471,0.000035869463,0.0009823648],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991906,0.000022493401,0.0000052533087,0.000014632353,0.000014695269,0.000023922143],"domain_scores_gemma":[0.9996208,0.00019371351,0.00007020155,0.00003784057,0.00003476051,0.000042587355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035753346,0.0007411046,0.00033542336,0.00052108144,0.00032511333,0.001017315,0.00054723903,0.00068786985,0.0011000638],"category_scores_gemma":[0.0014854033,0.00039806488,0.00060257205,0.00025967293,0.00076715456,0.00058493525,0.0006630285,0.00045500373,0.00021108442],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045190307,0.00001745586,0.0044264155,0.000010500355,0.000022711005,0.00007720729,0.000033879922,0.9912744,0.0014095588,0.0013153402,0.00012558613,0.001241729],"study_design_scores_gemma":[0.000009432558,0.00002600427,0.001923144,0.0000052417745,0.000008995126,0.000013674971,0.000014436652,0.9962119,0.0003823764,0.0012721617,0.00012384618,0.000008877707],"about_ca_topic_score_codex":0.012595239,"about_ca_topic_score_gemma":0.0068651363,"teacher_disagreement_score":0.012595239,"about_ca_system_score_codex":0.00079455733,"about_ca_system_score_gemma":0.0003388562,"threshold_uncertainty_score":0.025043845},"labels":[],"label_agreement":null},{"id":"W2122589109","doi":"10.5194/se-3-121-2012","title":"The fate of fluids released from subducting slab in northern Cascadia","year":2012,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"University of Tulsa","keywords":"Forearc; Geology; Subduction; Mantle (geology); Crust; Oceanic crust; Continental crust; Seismology; Kyanite; Petrology; Geochemistry; Tectonics; Metamorphic rock","score_opus":0.01783567202409219,"score_gpt":0.22342582943353298,"score_spread":0.20559015740944078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122589109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999113,0.00006228359,0.000031193762,0.0000504031,0.00000178587,0.0000016201571,0.00013457052,0.00001256589,0.0005925396],"genre_scores_gemma":[0.99919504,0.000061557665,0.000055230794,0.000008885137,0.0000016162236,0.0000020908728,0.0001760814,0.000004649646,0.000494739],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991643,0.000008208634,0.000007086415,0.000026838052,0.00002270139,0.000018869716],"domain_scores_gemma":[0.9997156,0.000027149112,0.00007081908,0.000024730774,0.000097839904,0.00006383842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018877837,0.0005621476,0.00030130727,0.0010482775,0.0011757632,0.00062604947,0.0004352153,0.00044615992,0.0015601834],"category_scores_gemma":[0.0005786309,0.0002740593,0.00027175507,0.0007845351,0.0007100729,0.00043116126,0.0009813715,0.00033241723,0.0002710171],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075096556,0.000056941528,0.81517094,0.00022371355,0.00015367471,0.0022455286,0.0044575864,0.004966934,0.15746908,0.00047384555,0.00034572542,0.013685004],"study_design_scores_gemma":[0.000014617064,0.00011256345,0.99085814,0.000014066682,0.000035955076,0.000105769104,0.0015630146,0.0011958996,0.004627647,0.00010981467,0.001349799,0.0000128226475],"about_ca_topic_score_codex":0.14661318,"about_ca_topic_score_gemma":0.13578893,"teacher_disagreement_score":0.14661318,"about_ca_system_score_codex":0.0028658912,"about_ca_system_score_gemma":0.0010281893,"threshold_uncertainty_score":0.29151958},"labels":[],"label_agreement":null},{"id":"W2123234667","doi":"10.1029/2004jb003258","title":"Forearc structure beneath southwestern British Columbia: A three‐dimensional tomographic velocity model","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Forearc; Terrane; Subduction; Accretionary wedge; North American Plate; Seismology; Crust; Volcanic arc; Oceanic crust; Mantle (geology); Island arc; Paleontology; Tectonics","score_opus":0.027402721588570524,"score_gpt":0.26539484084475035,"score_spread":0.23799211925617983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123234667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8969392,0.00038412857,0.046778943,0.0006761731,0.000040508294,0.0001591415,0.0063692858,0.0013717632,0.047280867],"genre_scores_gemma":[0.9769504,0.00034171736,0.011833461,0.000039753875,0.000005223284,0.00009125146,0.002339098,0.00008735004,0.00831175],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995923,0.00000287837,0.0000018727768,0.000012282609,0.000011652253,0.000011994193],"domain_scores_gemma":[0.99992955,0.0000075488088,0.000008883319,0.000005466402,0.000036121495,0.000012334009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004040313,0.0004670851,0.00019563608,0.00068484753,0.0008354023,0.0016147239,0.00094585645,0.00050849305,0.002659425],"category_scores_gemma":[0.00028646982,0.00039467437,0.00034959137,0.00087773794,0.00032529532,0.00029538656,0.0002795836,0.0003815526,0.0004602118],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050616447,0.000042092328,0.024809595,0.000027056365,0.00003928266,0.00022720332,0.0001747916,0.94436103,0.0021679613,0.0031642187,0.0027345722,0.022201639],"study_design_scores_gemma":[0.000017933873,0.0000058845562,0.008154357,0.000011926227,0.000013827846,0.000036808447,0.000097547985,0.98786384,0.00020549672,0.0005087791,0.0030654846,0.00001814882],"about_ca_topic_score_codex":0.93024457,"about_ca_topic_score_gemma":0.89234143,"teacher_disagreement_score":0.069755435,"about_ca_system_score_codex":0.0051558404,"about_ca_system_score_gemma":0.0066026985,"threshold_uncertainty_score":0.1403324},"labels":[],"label_agreement":null},{"id":"W2123741020","doi":"10.5194/se-7-557-2016","title":"Numerical models for ground deformation and gravity changes during volcanic unrest: simulating the hydrothermal system dynamics of a restless caldera","year":2016,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Caldera; Geology; Poromechanics; Hydrothermal circulation; Volcano; Magma; Geophysics; Pore water pressure; Deformation (meteorology); Unrest; Fluid dynamics; Petrology; Seismology; Mechanics; Geotechnical engineering; Porous medium; Porosity","score_opus":0.02047217857717747,"score_gpt":0.2268715505006201,"score_spread":0.20639937192344263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123741020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864493,0.00010011925,0.008887861,0.00018045439,0.000029560104,0.000050762264,0.00043747269,0.00015825908,0.0037063616],"genre_scores_gemma":[0.99345833,0.000052884323,0.0051284237,0.000036455105,0.000007764561,0.000053603882,0.0002796407,0.000020488716,0.0009623689],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998778,0.000032286953,0.0000086054515,0.000028359382,0.000025226387,0.000027633752],"domain_scores_gemma":[0.99936587,0.0003386745,0.000088069144,0.000046998703,0.000079923564,0.00008054227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030329044,0.00054104405,0.00060615834,0.0006184826,0.00052803726,0.00092364475,0.0012483924,0.0017694976,0.0016650709],"category_scores_gemma":[0.0011792212,0.00032823952,0.0007786553,0.00051247695,0.0010255949,0.00033600745,0.0007150689,0.00063357543,0.000115889176],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038909413,0.000049446895,0.0022613322,0.000010886631,0.000017253142,0.000056746103,0.000024597191,0.99563473,0.0009392061,0.00025353403,0.000055467648,0.0006577756],"study_design_scores_gemma":[0.0000138062705,0.000013956231,0.00054181315,0.0000015373794,0.000003903399,0.0000033035215,0.000012442488,0.9991517,0.00013868419,0.000059437964,0.00005724057,0.0000021759818],"about_ca_topic_score_codex":0.04231803,"about_ca_topic_score_gemma":0.01873285,"teacher_disagreement_score":0.04231803,"about_ca_system_score_codex":0.0012991843,"about_ca_system_score_gemma":0.00081844704,"threshold_uncertainty_score":0.08414346},"labels":[],"label_agreement":null},{"id":"W2123949892","doi":"10.1016/j.epsl.2007.07.024","title":"Seismic and magnetic anisotropy of serpentinized ophiolite: Implications for oceanic spreading rate dependent anisotropy","year":2007,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Anisotropy; Ophiolite; Olivine; Seismic anisotropy; Shear (geology); Geophysics; Lithosphere; Peridotite; Seismology; Mineralogy; Petrology; Mantle (geology); Tectonics; Physics","score_opus":0.012833726986376361,"score_gpt":0.22229210302065713,"score_spread":0.20945837603428077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123949892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99910897,0.000032168668,0.000040378498,0.000023825973,0.0000011598487,6.16152e-7,0.000043587515,0.0000031751213,0.0007460865],"genre_scores_gemma":[0.99983,0.000027361757,0.000018371182,0.0000023941636,0.0000013641794,2.9667953e-7,0.000036639965,0.0000012701732,0.00008220337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995875,0.0000051261995,0.0000044359754,0.00001171947,0.0000068267277,0.0000131720335],"domain_scores_gemma":[0.99974185,0.0000479609,0.000076593366,0.000022304763,0.00006839892,0.000042792504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013716304,0.00019189256,0.00012453788,0.00080064835,0.0002501331,0.0005614908,0.00020401359,0.0001850958,0.0015151383],"category_scores_gemma":[0.0008481212,0.00012737977,0.000102172235,0.00045729414,0.00041374343,0.00033976857,0.00030675562,0.00020669919,0.00013967337],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011067953,0.00006120449,0.6268109,0.000058831723,0.000072121264,0.000725104,0.00067232136,0.004065976,0.35121953,0.001819672,0.00017844976,0.013209091],"study_design_scores_gemma":[0.00003194801,0.00004839594,0.9897199,0.0000034825807,0.00003089767,0.00017681158,0.00037894092,0.0031549965,0.0057760603,0.00033329474,0.00033687055,0.000008354835],"about_ca_topic_score_codex":0.016942933,"about_ca_topic_score_gemma":0.013390701,"teacher_disagreement_score":0.016942933,"about_ca_system_score_codex":0.00043183196,"about_ca_system_score_gemma":0.00030183862,"threshold_uncertainty_score":0.033688605},"labels":[],"label_agreement":null},{"id":"W2124108257","doi":"10.1002/2015gl063750","title":"Joint analysis of the 2014 Kangding, southwest China, earthquake sequence with seismicity relocation and InSAR inversion","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Seismology; Aftershock; Geology; Interferometric synthetic aperture radar; Seismic moment; Seismic gap; Hypocenter; Slip (aerodynamics); Moment magnitude scale; Induced seismicity; Geodesy; Fault (geology); Synthetic aperture radar; Scaling; Remote sensing","score_opus":0.062441935785573444,"score_gpt":0.2755993013895912,"score_spread":0.21315736560401777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124108257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982126,0.000057219502,0.00030274945,0.00001935003,0.000006993281,0.000005973057,0.0011021269,0.000023174309,0.0002699284],"genre_scores_gemma":[0.9942386,0.000041865766,0.0004247164,0.000010822601,0.000010239239,0.00000720555,0.0046957918,0.0000060726716,0.00056464534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998266,0.00001709562,0.000017606746,0.00005370131,0.0000439158,0.0000411216],"domain_scores_gemma":[0.9995901,0.000032586217,0.0001196357,0.00006207909,0.00011132955,0.000084270774],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041372763,0.0004055709,0.00033396643,0.0013261474,0.00027555824,0.00031139178,0.00021521829,0.00018384031,0.0008402157],"category_scores_gemma":[0.00052266655,0.00018841027,0.00033681662,0.0018926268,0.00020211826,0.00019403471,0.0003278902,0.00016669331,0.00025930506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025423983,0.0000926335,0.9578298,0.000055605626,0.00024382946,0.00063800946,0.00025998792,0.007341228,0.011307602,0.0001634429,0.0014739605,0.020339753],"study_design_scores_gemma":[0.000007924774,0.000027270848,0.992767,0.000003507246,0.000052954176,0.00004615949,0.00012331051,0.0056600417,0.00059142715,0.000022561137,0.00068823894,0.0000096231015],"about_ca_topic_score_codex":0.0351582,"about_ca_topic_score_gemma":0.0656142,"teacher_disagreement_score":0.0351582,"about_ca_system_score_codex":0.00044684537,"about_ca_system_score_gemma":0.0007856787,"threshold_uncertainty_score":0.06990707},"labels":[],"label_agreement":null},{"id":"W2124153265","doi":"10.1130/g34556.1","title":"The thickness of subduction plate boundary faults from the seafloor into the seismogenic zone","year":2013,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"ROWE; Geology; Subduction; Seafloor spreading; Citation; Plate tectonics; Icon; Seismology; Art history; Paleontology; Library science; History; Tectonics; Computer science","score_opus":0.009134181894333177,"score_gpt":0.19721931292225917,"score_spread":0.18808513102792598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124153265","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99082035,0.0007877205,0.0031014066,0.000054912438,0.000009153836,0.000007428954,0.0021044859,0.00012135223,0.0029933264],"genre_scores_gemma":[0.9965816,0.00038477575,0.0010146099,0.000011094711,0.0000033988154,0.0000045142815,0.0012632877,0.000018649433,0.00071798183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998933,0.000012082892,0.000016211636,0.000039918155,0.000020448682,0.000017976863],"domain_scores_gemma":[0.99968255,0.000057295023,0.00010494391,0.000045873363,0.00007026805,0.000039041417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026843318,0.00044486395,0.00020586367,0.0012992716,0.0002247322,0.0010263763,0.00046251385,0.00023354612,0.0017710811],"category_scores_gemma":[0.00086814276,0.00034704595,0.00041475397,0.00084996084,0.00040274774,0.00075922185,0.0006010317,0.00026030975,0.00031426176],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015537256,0.000023149683,0.8481908,0.00034463976,0.0002556516,0.0002062162,0.00074559636,0.09042534,0.02416464,0.0018022038,0.00057416194,0.03311233],"study_design_scores_gemma":[0.000011452597,0.00007462322,0.9412485,0.00007164628,0.00006538728,0.00018937714,0.00044525196,0.044902746,0.0057546687,0.0013115183,0.00589012,0.000034675068],"about_ca_topic_score_codex":0.014762516,"about_ca_topic_score_gemma":0.015768427,"teacher_disagreement_score":0.014762516,"about_ca_system_score_codex":0.0008339976,"about_ca_system_score_gemma":0.00038754093,"threshold_uncertainty_score":0.029353201},"labels":[],"label_agreement":null},{"id":"W2124343231","doi":"10.1029/2003gl018541","title":"Possible emplacement of crustal rocks into the forearc mantle of the Cascadia Subduction Zone","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"","keywords":"Geology; Forearc; Subduction; Mantle (geology); Mantle wedge; Oceanic crust; Crust; Transition zone; Seismology; Crustal recycling; Continental crust; Geophysics; Geochemistry; Petrology; Tectonics","score_opus":0.030598301204228504,"score_gpt":0.2792226327507885,"score_spread":0.24862433154656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124343231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99680126,0.00044453613,0.00020417501,0.00016363,0.0000039014135,0.0000037771117,0.00009012022,0.000034459234,0.0022540966],"genre_scores_gemma":[0.99825794,0.0003513338,0.00027012196,0.000023033375,0.000004609272,0.0000034634268,0.00019884083,0.0000059104973,0.000884644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998398,0.000016822758,0.000010168431,0.000037877857,0.000040797222,0.000054604745],"domain_scores_gemma":[0.9995409,0.000056892615,0.00014292971,0.000080567435,0.000105747065,0.000072917086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036236268,0.0004154215,0.00024320548,0.0012632302,0.000806648,0.0007224325,0.000493837,0.0006239741,0.0018130057],"category_scores_gemma":[0.0012096622,0.0005124296,0.00033380918,0.0011123752,0.0007126158,0.0006117092,0.0012637086,0.0004453432,0.00027152896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000587294,0.000036008903,0.8794576,0.00019975424,0.00014473373,0.0039561396,0.006222045,0.0023117303,0.07891093,0.0014480455,0.00035587503,0.02636984],"study_design_scores_gemma":[0.000010099212,0.000037349295,0.9948014,0.000019390294,0.00003331493,0.00033511844,0.00070536486,0.00033272276,0.0017026429,0.00019898349,0.0018150078,0.000008529926],"about_ca_topic_score_codex":0.032343954,"about_ca_topic_score_gemma":0.039575275,"teacher_disagreement_score":0.967656,"about_ca_system_score_codex":0.00097510184,"about_ca_system_score_gemma":0.0006348653,"threshold_uncertainty_score":0.064311385},"labels":[],"label_agreement":null},{"id":"W2124372616","doi":"10.1130/g22610.1","title":"Fault dating in the Canadian Rocky Mountains: Evidence for late Cretaceous and early Eocene orogenic pulses","year":2006,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Citation; Icon; Geology; Archaeology; Geological survey; History; Art history; Library science; Paleontology","score_opus":0.03256823169873549,"score_gpt":0.249149606692124,"score_spread":0.2165813749933885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124372616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7846666,0.043471877,0.0019239406,0.007959112,0.00037967844,0.00018101202,0.027094163,0.00044450903,0.13387905],"genre_scores_gemma":[0.947948,0.02102284,0.0027848918,0.0004439458,0.00010113984,0.00002755296,0.010350144,0.00012508925,0.017196437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99898773,0.000029646722,0.00004739458,0.00007916233,0.0007124305,0.000143625],"domain_scores_gemma":[0.9974141,0.00016330456,0.00027539243,0.00006931825,0.0019298419,0.00014795552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073973613,0.00026784136,0.0003618789,0.006277998,0.0026491901,0.0016628553,0.00071399164,0.000417712,0.004301524],"category_scores_gemma":[0.0038624243,0.0001950146,0.00023468048,0.013696974,0.0006987832,0.00068392593,0.0009500752,0.0004429513,0.00056079763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027595967,0.00004593502,0.550286,0.0015648726,0.00026885731,0.0009438275,0.008313342,0.001143309,0.0058492892,0.003459246,0.06081449,0.36703497],"study_design_scores_gemma":[0.00001656401,0.00001560991,0.9417359,0.0002606686,0.0000831048,0.00017650172,0.0017606714,0.00034645465,0.00086419645,0.00019711193,0.054507267,0.000035897505],"about_ca_topic_score_codex":0.983931,"about_ca_topic_score_gemma":0.9963128,"teacher_disagreement_score":0.016068995,"about_ca_system_score_codex":0.010288612,"about_ca_system_score_gemma":0.023293428,"threshold_uncertainty_score":0.07464945},"labels":[],"label_agreement":null},{"id":"W2124423310","doi":"10.1029/2004jb003201","title":"Modeling long‐term volcanic hazards through Bayesian inference: An example from the Tohoku volcanic arc, Japan","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mira Geoscience (Canada)","funders":"","keywords":"Geology; Volcano; Volcanism; A priori and a posteriori; Context (archaeology); Volcanic arc; Inference; Seismology; Geophysics; Subduction; Tectonics; Computer science; Paleontology; Artificial intelligence","score_opus":0.07586709174823018,"score_gpt":0.32541612223938315,"score_spread":0.24954903049115296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124423310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9371306,0.0011185593,0.054961883,0.0014747848,0.000022947066,0.000046215744,0.00036074902,0.00018603323,0.0046982686],"genre_scores_gemma":[0.98605275,0.00044915092,0.012549962,0.000040266408,0.00001774484,0.000015236136,0.0001909911,0.000022395736,0.0006614572],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99974626,0.00011657536,0.000016561027,0.000049791208,0.0000415644,0.000029171535],"domain_scores_gemma":[0.99822015,0.0011905757,0.00012701457,0.00005032402,0.00033106274,0.00008093875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016566955,0.00057019695,0.00054203277,0.0007821643,0.0007624113,0.00088750257,0.0007009355,0.0008957624,0.00060754846],"category_scores_gemma":[0.0039014216,0.00033589103,0.00056538696,0.0011431053,0.0005690421,0.00061785453,0.00061416987,0.00058364304,0.00007153066],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009929745,0.0000833731,0.05238214,0.00007785218,0.00015257085,0.0006904685,0.00048476906,0.92503625,0.00082863454,0.0049169753,0.0008019095,0.014445732],"study_design_scores_gemma":[0.000031113104,0.000024775858,0.018701037,0.0000126715995,0.00006183927,0.00006465059,0.0002265279,0.9755881,0.00017093695,0.004403182,0.0006871909,0.00002789809],"about_ca_topic_score_codex":0.24164306,"about_ca_topic_score_gemma":0.19950889,"teacher_disagreement_score":0.24164306,"about_ca_system_score_codex":0.001473383,"about_ca_system_score_gemma":0.0012405,"threshold_uncertainty_score":0.4804731},"labels":[],"label_agreement":null},{"id":"W2124649692","doi":"10.1017/s0022050709000850","title":"The Opportunity of a Disaster: The Economic Impact of the 1755 Lisbon Earthquake","year":2009,"lang":"en","type":"article","venue":"The Journal of Economic History","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Tragedy (event); Portuguese; Natural disaster; Friendship; Wage; Order (exchange); Economics; Economy; Political science; Geography; Sociology; Labour economics; Finance; Social science","score_opus":0.026304367938869568,"score_gpt":0.22619779938605053,"score_spread":0.19989343144718097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124649692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.934577,0.0057882145,0.0001671095,0.0028463867,0.00009732529,0.000015204823,0.006750791,0.00001856487,0.049739346],"genre_scores_gemma":[0.9904778,0.0037898722,0.00011140924,0.00014592953,0.00006512942,0.0000082119695,0.0026322373,0.0000098741375,0.0027594622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997075,0.00006375869,0.000019768708,0.000024401133,0.00007830623,0.000106200314],"domain_scores_gemma":[0.9993561,0.00012565561,0.00028683202,0.000025924892,0.0000984232,0.00010701409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040140122,0.0003966837,0.00020691808,0.004705754,0.0015872326,0.002798516,0.0004652698,0.000796421,0.0041162223],"category_scores_gemma":[0.0016962336,0.00017594913,0.0002449721,0.006116357,0.0010856935,0.0011598659,0.002414632,0.00075693754,0.0006993649],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013783892,0.00021547842,0.7696512,0.0011301831,0.000470369,0.010348533,0.028148726,0.011640235,0.0008203947,0.019986013,0.065005586,0.09120494],"study_design_scores_gemma":[0.0000110163855,0.00005743351,0.91788924,0.00035442982,0.00004116344,0.0005700023,0.028784098,0.00082693726,0.0002686624,0.0013217848,0.04982612,0.000049232793],"about_ca_topic_score_codex":0.07738708,"about_ca_topic_score_gemma":0.19428702,"teacher_disagreement_score":0.07738708,"about_ca_system_score_codex":0.0066705644,"about_ca_system_score_gemma":0.0008784001,"threshold_uncertainty_score":0.15387332},"labels":[],"label_agreement":null},{"id":"W2125281194","doi":"10.1007/s00024-009-0522-1","title":"Structural Properties and Deformation Patterns of Evolving Strike-slip Faults: Numerical Simulations Incorporating Damage Rheology","year":2009,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Geology; Seismology; Crust; Slip (aerodynamics); Deformation (meteorology); Brittleness; Geodetic datum; Strike-slip tectonics; Fault (geology); Tectonics; Geophysics; Geodesy; Materials science","score_opus":0.015902419763598928,"score_gpt":0.20205387120171386,"score_spread":0.18615145143811493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125281194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949993,0.0000757115,0.0018298086,0.00023568625,0.000027533013,0.00001585441,0.00027349681,0.000062182844,0.0024805046],"genre_scores_gemma":[0.99847585,0.00004359264,0.00075316016,0.000028279215,0.000009098019,0.000010797553,0.00014616482,0.000020528705,0.00051252166],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998122,0.000057730238,0.000017027458,0.000039794584,0.000027673315,0.000045587483],"domain_scores_gemma":[0.9978865,0.0012740972,0.00023446628,0.00017353792,0.00019148774,0.00023992716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007493696,0.0006270548,0.00073370495,0.0007992092,0.0007663099,0.001232328,0.0012225815,0.0028477693,0.0023727177],"category_scores_gemma":[0.005095702,0.0009928037,0.00093753525,0.0010254664,0.0016483999,0.0012402796,0.0005590442,0.0014199526,0.00025704835],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006382786,0.00007352506,0.0029278062,0.000010513618,0.000019728852,0.000070222566,0.000040026913,0.9952791,0.00042269955,0.00039946506,0.00012179373,0.00057127874],"study_design_scores_gemma":[0.000030398673,0.00002299765,0.0012688468,0.0000031012942,0.000008113562,0.000008601809,0.000021361087,0.99834585,0.00013116599,0.00011501852,0.00003842437,0.0000060959496],"about_ca_topic_score_codex":0.03925285,"about_ca_topic_score_gemma":0.022401605,"teacher_disagreement_score":0.03925285,"about_ca_system_score_codex":0.0013394296,"about_ca_system_score_gemma":0.00094319094,"threshold_uncertainty_score":0.078048766},"labels":[],"label_agreement":null},{"id":"W2125478980","doi":"10.1785/0120060242","title":"Rate Dependence of Acoustic Emissions Generated during Shear of Simulated Fault Gouge","year":2007,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Royal Society; National Science Foundation","keywords":"Shear (geology); Fault gouge; Geology; Seismology; Acoustic emission; Fault (geology); Geotechnical engineering; Acoustics; Petrology; Physics","score_opus":0.015264129449592777,"score_gpt":0.2265439914253114,"score_spread":0.21127986197571863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125478980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988218,0.000012847494,0.0008293108,0.000005124929,0.0000018510335,0.000004684815,0.0001040588,0.000027872808,0.00019239172],"genre_scores_gemma":[0.9996877,0.000009141914,0.00017932685,0.0000014142141,5.715413e-7,0.000004360155,0.00006330859,0.0000030656963,0.000051169696],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993324,0.000008992397,0.0000054432935,0.000014789619,0.000020158317,0.000017369584],"domain_scores_gemma":[0.99980134,0.00008854723,0.000035254925,0.000021271124,0.000026205984,0.000027337499],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014561228,0.0001907635,0.00015782163,0.0002459154,0.000102056074,0.00018445186,0.00018905432,0.00023319454,0.00078406354],"category_scores_gemma":[0.00042891418,0.000085619744,0.00013417657,0.0001417567,0.00015039006,0.000103513994,0.0001706198,0.00018560338,0.000092601265],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001411892,0.00046896955,0.09710907,0.00015755338,0.00013415921,0.0006571032,0.00027097028,0.14603285,0.73543704,0.00040258572,0.00040581636,0.01751201],"study_design_scores_gemma":[0.000052577576,0.0012787224,0.29980275,0.000012398862,0.000055618104,0.00016079978,0.00017005007,0.54898477,0.14882712,0.00025961187,0.00035708316,0.000038525166],"about_ca_topic_score_codex":0.0011662128,"about_ca_topic_score_gemma":0.0011312411,"teacher_disagreement_score":0.0011662128,"about_ca_system_score_codex":0.00014113507,"about_ca_system_score_gemma":0.00006843383,"threshold_uncertainty_score":0.002622962},"labels":[],"label_agreement":null},{"id":"W2125582283","doi":"10.2113/gscpgbull.58.1.36","title":"A structural study of western Anticosti Island, St. Lawrence platform, Quebec: a fracture analysis that integrates surface and subsurface structural data","year":2010,"lang":"en","type":"article","venue":"Bulletin of Canadian Petroleum Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Institut National de la Recherche Scientifique","funders":"","keywords":"Geological survey; Archaeology; Library science; Art history; Geology; Art; History; Paleontology; Computer science","score_opus":0.02009083046863769,"score_gpt":0.22644189098010442,"score_spread":0.20635106051146673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125582283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9367827,0.0014179996,0.0026519955,0.0011614978,0.000037108228,0.00026025806,0.028114656,0.00014006249,0.02943382],"genre_scores_gemma":[0.9668819,0.0007826101,0.0034852817,0.00020390289,0.000012376202,0.00009831124,0.009433672,0.00007069312,0.0190314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995981,0.00001543386,0.000010852285,0.000062229905,0.00022423638,0.00008916921],"domain_scores_gemma":[0.99869776,0.00004970774,0.00008516056,0.000041778032,0.001007524,0.0001179974],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029998907,0.00041652904,0.0003837422,0.0017025709,0.0027183727,0.001171516,0.001423458,0.00065826665,0.0050322013],"category_scores_gemma":[0.00083896494,0.00035021635,0.00044976367,0.0054458724,0.00087282574,0.000515071,0.00072596886,0.0006320869,0.0008644563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039633986,0.00022819621,0.78639156,0.0004477765,0.0003430348,0.0012429479,0.0050651347,0.009555326,0.011521977,0.0021264039,0.044465117,0.13821618],"study_design_scores_gemma":[0.00002838587,0.000038550144,0.97923195,0.000090993184,0.00005274052,0.000108773806,0.0029646351,0.0056242365,0.0005133889,0.00011903624,0.011190028,0.00003719588],"about_ca_topic_score_codex":0.99708986,"about_ca_topic_score_gemma":0.9994118,"teacher_disagreement_score":0.022793707,"about_ca_system_score_codex":0.022793707,"about_ca_system_score_gemma":0.027122501,"threshold_uncertainty_score":0.16538072},"labels":[],"label_agreement":null},{"id":"W2126834387","doi":"10.1785/012003007","title":"Seismicity of the Southern Great Lakes: Revised Earthquake Hypocenters and Possible Tectonic Controls","year":2004,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Seismology; Tectonics","score_opus":0.011873708719269686,"score_gpt":0.19449668005204085,"score_spread":0.18262297133277117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126834387","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987072,0.00009173849,0.0002149426,0.0000361708,0.0000014882293,0.0000033370586,0.00020448114,0.000014593476,0.0007260179],"genre_scores_gemma":[0.99937326,0.000038731294,0.00017500596,0.0000054424086,0.0000041248813,0.0000018013812,0.0002661,0.0000022018385,0.00013332111],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988866,0.000029480074,0.000010282058,0.000027147727,0.000027557338,0.000016929129],"domain_scores_gemma":[0.999476,0.000058562146,0.00024475358,0.000027853503,0.00013954019,0.000053397875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038275684,0.00021025023,0.00011497919,0.0013746604,0.00014882599,0.0005520602,0.00018102741,0.0000798395,0.0008021826],"category_scores_gemma":[0.0011094455,0.00010728756,0.00007194165,0.0013842487,0.0004084907,0.00022153907,0.00045498292,0.00013643723,0.00010192633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008229155,0.0000075704006,0.9749699,0.00003917807,0.0000330525,0.00016032156,0.0012388212,0.0019695822,0.0074315346,0.0003067868,0.0004019348,0.013359048],"study_design_scores_gemma":[0.0000018993909,0.0000052671617,0.9987759,0.000003179647,0.000004456213,0.000014730987,0.000116804236,0.0006647446,0.00012062204,0.000027759714,0.00026270555,0.000002086033],"about_ca_topic_score_codex":0.057214376,"about_ca_topic_score_gemma":0.088329405,"teacher_disagreement_score":0.9427856,"about_ca_system_score_codex":0.000486093,"about_ca_system_score_gemma":0.0003037717,"threshold_uncertainty_score":0.11376274},"labels":[],"label_agreement":null},{"id":"W2127048301","doi":"10.1111/1365-2478.12274","title":"Uranium mineralization indicators from seismic and well log data in the Shea Creek area at the southern margin of the Carswell impact structure, Athabasca Basin, Canada","year":2015,"lang":"en","type":"article","venue":"Geophysical Prospecting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Structural basin; Basement; Geochemistry; Seismology; Shear zone; Mineral resource classification; Tectonics; Geomorphology","score_opus":0.017003156073036103,"score_gpt":0.2111543070030778,"score_spread":0.1941511509300417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127048301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99808633,0.00003562671,0.000031765532,0.000025813917,8.000657e-7,0.000010453864,0.000930245,0.000007985476,0.00087107316],"genre_scores_gemma":[0.9980432,0.00004968895,0.00012631362,0.000008152002,8.6664926e-7,0.000008691485,0.0009799083,0.0000022070762,0.0007809766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979633,0.000012676698,0.000015163516,0.000028989036,0.00009550991,0.00005142486],"domain_scores_gemma":[0.99953115,0.000032631968,0.00007049244,0.000013229054,0.00024887043,0.00010359811],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011742291,0.00019885522,0.00013636038,0.0023932308,0.0009070643,0.00067210005,0.00038321142,0.00023517213,0.0012901188],"category_scores_gemma":[0.00054163253,0.00016409624,0.00011617906,0.002577674,0.00033853197,0.00021015764,0.00040316206,0.00014833863,0.00016587501],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006225447,0.000039650185,0.984139,0.000025831594,0.00003228158,0.00032738337,0.0011613736,0.00078947906,0.004794773,0.00011181732,0.0007506484,0.0077655176],"study_design_scores_gemma":[0.0000021757212,0.0000057210937,0.99808645,0.0000034574598,0.000003436926,0.000021180922,0.0009394873,0.00042075056,0.00014647628,0.000007680504,0.00035955285,0.0000037126392],"about_ca_topic_score_codex":0.93580025,"about_ca_topic_score_gemma":0.98398685,"teacher_disagreement_score":0.064199746,"about_ca_system_score_codex":0.004982884,"about_ca_system_score_gemma":0.0031864282,"threshold_uncertainty_score":0.12915564},"labels":[],"label_agreement":null},{"id":"W2127573006","doi":"10.1111/j.1365-246x.2006.03271.x","title":"Rapid identification of earthquake rupture plane using Source-Scanning Algorithm","year":2007,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":114,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Seismology; Geology; Waveform; Focal mechanism; Amplitude; Geodesy; Tectonics; Computer science; Telecommunications","score_opus":0.019663792663968435,"score_gpt":0.2535257267235188,"score_spread":0.23386193405955036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127573006","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05578804,0.00007292446,0.94130576,0.000025236268,0.000013066807,0.000041933825,0.00012178563,0.0015038383,0.0011274798],"genre_scores_gemma":[0.2519446,0.00010756811,0.74615365,0.000015654165,0.000017449513,0.000080912134,0.00048038067,0.00008431032,0.0011154235],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998833,0.00002174793,0.000009474655,0.000025676867,0.00004786359,0.000011989599],"domain_scores_gemma":[0.99961436,0.000098806435,0.00004874398,0.000052854906,0.000162572,0.000022615412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002908297,0.00043208906,0.0003456588,0.0011456099,0.00015586326,0.0003207921,0.00042286044,0.00031806534,0.0016219043],"category_scores_gemma":[0.0011690046,0.00019872084,0.00027111298,0.0006856936,0.00014881577,0.00046469097,0.00052197423,0.00022848161,0.0007874258],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037914544,0.000070462156,0.010396375,0.00010224424,0.000057498837,0.00029438548,0.0001969111,0.049508862,0.20399639,0.0037229627,0.0023317419,0.72894305],"study_design_scores_gemma":[0.000045774224,0.0000946708,0.009314635,0.000013520464,0.000028999188,0.00057132315,0.000051848518,0.92168915,0.061640542,0.0022803158,0.0042369985,0.00003226374],"about_ca_topic_score_codex":0.0007333195,"about_ca_topic_score_gemma":0.0010044312,"teacher_disagreement_score":0.0016219043,"about_ca_system_score_codex":0.00015538442,"about_ca_system_score_gemma":0.00036092897,"threshold_uncertainty_score":0.005425811},"labels":[],"label_agreement":null},{"id":"W2127896615","doi":"10.1785/0120060203","title":"Modeling Variable-Stress Distribution with the Stochastic Finite-Fault Technique","year":2007,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Fault (geology); Variable (mathematics); Stress (linguistics); Distribution (mathematics); Mathematics; Geology; Computer science; Applied mathematics; Mathematical analysis; Seismology","score_opus":0.01208463773341786,"score_gpt":0.2039391221209703,"score_spread":0.19185448438755243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127896615","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.290375,0.000028669338,0.70779425,0.00009231455,0.000011309002,0.00002615853,0.000090502166,0.00044825222,0.0011335982],"genre_scores_gemma":[0.9676615,0.000016035576,0.03189431,0.000011930342,0.0000058306705,0.000021809692,0.000062335144,0.000027489696,0.00029862544],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998367,0.000055999375,0.000010530071,0.000025219288,0.0000498993,0.000021632302],"domain_scores_gemma":[0.99922764,0.00044779768,0.00012356958,0.00007044349,0.00010460714,0.00002603555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049432396,0.00029150565,0.00030103655,0.0004194691,0.00025586807,0.00035002572,0.00078612764,0.00054474676,0.0007461616],"category_scores_gemma":[0.0019300937,0.00023857992,0.0003763002,0.0003364583,0.0004024647,0.00045398733,0.00031232001,0.00038235166,0.00009054923],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009533429,0.000011918377,0.0010098115,0.0000045769516,0.0000072811476,0.000020953483,0.000017619346,0.9932074,0.0017300255,0.0012354541,0.00003095487,0.0027144877],"study_design_scores_gemma":[8.103345e-7,0.0000019904753,0.000082157865,2.7044362e-7,4.6211687e-7,0.0000024468234,9.830609e-7,0.99956256,0.0002011353,0.00012748438,0.000018610926,9.894718e-7],"about_ca_topic_score_codex":0.012568344,"about_ca_topic_score_gemma":0.0084680375,"teacher_disagreement_score":0.012568344,"about_ca_system_score_codex":0.00056251796,"about_ca_system_score_gemma":0.0005318852,"threshold_uncertainty_score":0.02499038},"labels":[],"label_agreement":null},{"id":"W2127999289","doi":"10.1144/sp282.4","title":"Early Cretaceous motion of Flemish Cap with respect to North America: implications on the formation of Orphan Basin and SE Flemish Cap–Galicia Bank conjugate margins","year":2007,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Flemish; Cretaceous; Structural basin; Geography; Geology; Paleontology; Archaeology","score_opus":0.023570583901314262,"score_gpt":0.23222765194875433,"score_spread":0.20865706804744008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127999289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99523646,0.00024247993,0.000038927355,0.00007175586,0.000003929743,0.0000046158593,0.00017786476,0.0000040064706,0.0042200917],"genre_scores_gemma":[0.99950635,0.000094541494,0.000061989056,0.000011055967,0.000001940774,0.0000021542644,0.000093996336,0.0000019779955,0.0002260869],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991643,0.000013183767,0.0000055365654,0.000026065822,0.000009989997,0.000028845825],"domain_scores_gemma":[0.9997359,0.000038275408,0.00010048821,0.000018053246,0.00006130092,0.000046039026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030723622,0.00018980427,0.00015320348,0.001141041,0.00046002716,0.0008886453,0.00025184097,0.00029178342,0.0023160505],"category_scores_gemma":[0.00080354547,0.00010865524,0.00014781662,0.00093664817,0.0006326483,0.00035327976,0.000438911,0.00018344808,0.00016369509],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018802976,0.00002327492,0.97519004,0.00004203818,0.000053348107,0.0008654845,0.0013494518,0.0009998508,0.009147238,0.0005348958,0.0002123832,0.01139394],"study_design_scores_gemma":[0.0000018426721,0.0000050109425,0.99902344,0.000007769245,0.0000035526866,0.00003125752,0.00035270595,0.00013563139,0.000116686315,0.00002147757,0.00029915513,0.0000014529757],"about_ca_topic_score_codex":0.103086285,"about_ca_topic_score_gemma":0.16488308,"teacher_disagreement_score":0.8969137,"about_ca_system_score_codex":0.0013087192,"about_ca_system_score_gemma":0.0005839279,"threshold_uncertainty_score":0.2049725},"labels":[],"label_agreement":null},{"id":"W2128039424","doi":"10.1785/gssrl.83.3.505","title":"Regional Centroid-Moment-Tensor Analysis for Earthquakes in Canada and Adjacent Regions: An Update","year":2012,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geological survey; Archaeology; Library science; Geology; Geography; Paleontology","score_opus":0.09601238661060997,"score_gpt":0.3067403881171475,"score_spread":0.21072800150653753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128039424","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0053801653,0.7101413,0.053421788,0.024575789,0.015071659,0.0007652348,0.10891919,0.010126192,0.0715987],"genre_scores_gemma":[0.021538893,0.75455743,0.08727689,0.003042447,0.009272858,0.00042160184,0.06989131,0.003827247,0.05017133],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99638903,0.00017827618,0.00035885136,0.00039939792,0.0024636213,0.00021089728],"domain_scores_gemma":[0.9710517,0.0025820492,0.0011099179,0.001290619,0.022817636,0.0011480864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004160347,0.0032056174,0.002425219,0.031957295,0.0018067318,0.0049445103,0.0066871755,0.0021001026,0.017740496],"category_scores_gemma":[0.019672431,0.0014719478,0.0025091793,0.043274302,0.001695369,0.005294934,0.0022666901,0.0027651123,0.013470051],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037432976,0.000032243403,0.006190988,0.0015611934,0.0001558136,0.00014881186,0.00018329307,0.0007313601,0.00034227007,0.00083270157,0.5355103,0.45427367],"study_design_scores_gemma":[0.000020387388,0.000014760654,0.019535152,0.0014637995,0.00028164542,0.00070277153,0.00037055608,0.0011043412,0.00045002432,0.0012410181,0.97466904,0.00014648656],"about_ca_topic_score_codex":0.85772634,"about_ca_topic_score_gemma":0.91917783,"teacher_disagreement_score":0.14227366,"about_ca_system_score_codex":0.012810729,"about_ca_system_score_gemma":0.034664523,"threshold_uncertainty_score":0.28622305},"labels":[],"label_agreement":null},{"id":"W2128766429","doi":"10.1029/2003jb002892","title":"Intense <i>PP</i> reflection beneath the aseismic forearc slope of the Japan Trench subduction zone and its implication of aseismic slip subduction","year":2005,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Forearc; Seismology; Subduction; Trench; Slip (aerodynamics); Plate tectonics; Slab; Reflection (computer programming); Seismic wave; Geophysics; Tectonics; Materials science; Physics","score_opus":0.03603492623293233,"score_gpt":0.29549749145226534,"score_spread":0.25946256521933303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128766429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99919194,0.0000460958,0.000089073765,0.000015340078,0.0000012010203,0.0000019801248,0.000028879735,0.0000063402135,0.00061914267],"genre_scores_gemma":[0.99973136,0.000029728013,0.0000798704,0.0000063208095,0.000002634596,0.0000013558933,0.000040477396,0.0000014116537,0.00010678947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991155,0.0000057984535,0.000006897006,0.00002350177,0.000022506063,0.000029728295],"domain_scores_gemma":[0.99986327,0.000013488127,0.00006175777,0.000008462707,0.00002879688,0.000024219866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013264583,0.00026724752,0.00020092636,0.00059294107,0.000318143,0.00047046618,0.00037519497,0.00040827054,0.00075734744],"category_scores_gemma":[0.00022420379,0.00034863947,0.00017187955,0.0005020196,0.00043907482,0.00026527912,0.00041131253,0.00021588354,0.00014132845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029525906,0.0000431982,0.73793244,0.000114932394,0.0000794748,0.0014611318,0.0012069378,0.0006296923,0.24848837,0.00012821781,0.00014011255,0.009480183],"study_design_scores_gemma":[0.000003953212,0.000018557681,0.998042,0.0000023922992,0.000010410699,0.000117162825,0.00020748237,0.00024900472,0.0012517431,0.000012178911,0.000081961574,0.0000030761646],"about_ca_topic_score_codex":0.012055136,"about_ca_topic_score_gemma":0.012313411,"teacher_disagreement_score":0.012055136,"about_ca_system_score_codex":0.00022254554,"about_ca_system_score_gemma":0.00029753576,"threshold_uncertainty_score":0.023969948},"labels":[],"label_agreement":null},{"id":"W2128778600","doi":"10.1785/0120140036","title":"A Review Study of the Source Parameters of the 23 August 2011 Mw 5.7 Virginia Earthquake","year":2014,"lang":"en","type":"review","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geology","score_opus":0.033460103816518094,"score_gpt":0.25613160737734275,"score_spread":0.22267150356082466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128778600","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.11548664,0.86240745,0.00764687,0.001524066,0.0008056144,0.000106842,0.0034075268,0.00019350869,0.00842155],"genre_scores_gemma":[0.24163613,0.7429462,0.004758967,0.0005472922,0.00085108343,0.00006667593,0.005109852,0.00010875151,0.0039750054],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9995363,0.00006621593,0.00014154478,0.00008073859,0.0001554088,0.000019844989],"domain_scores_gemma":[0.99602723,0.0011832908,0.00074644806,0.00015877339,0.001815011,0.00006919467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010398751,0.00043239194,0.0005642916,0.009358423,0.00023258392,0.0011466307,0.0005152738,0.0004463107,0.0011372811],"category_scores_gemma":[0.0040764534,0.0002642084,0.00059767533,0.006422574,0.00030817938,0.0015955506,0.00037810064,0.00027237213,0.0004033081],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023443328,0.00005348663,0.048929773,0.0145517355,0.0005114198,0.0009001787,0.0009431336,0.0017219818,0.010249156,0.001576999,0.01649811,0.90382963],"study_design_scores_gemma":[0.000021366985,0.0004451918,0.26912048,0.010133495,0.0015406319,0.0039098575,0.0020496584,0.0026306668,0.012155928,0.0015072443,0.696309,0.00017647342],"about_ca_topic_score_codex":0.0038102653,"about_ca_topic_score_gemma":0.004798832,"teacher_disagreement_score":0.009358423,"about_ca_system_score_codex":0.000755276,"about_ca_system_score_gemma":0.0015220165,"threshold_uncertainty_score":0.0075761676},"labels":[],"label_agreement":null},{"id":"W2129019315","doi":"10.1111/gfl.12076","title":"Tectonic evolution of a Paleozoic thrust fault influences the hydrogeology of a fractured rock aquifer, northeastern Appalachian foreland","year":2014,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Aquifer; Foreland basin; Thrust fault; Hydrogeology; Ordovician; Geochemistry; Sedimentary rock; Paleozoic; Metamorphic rock; Petrology; Groundwater; Geomorphology; Tectonics; Paleontology; Geotechnical engineering","score_opus":0.007446698110937663,"score_gpt":0.19955145272679942,"score_spread":0.19210475461586174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129019315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99955624,0.000030953583,0.000009156609,0.0000127422245,4.7368033e-7,7.83353e-7,0.000079748876,0.0000013039315,0.00030863515],"genre_scores_gemma":[0.9997217,0.000033438413,0.000017397291,0.000003993649,9.353874e-7,0.0000010630527,0.000086511674,7.4593504e-7,0.00013414648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999211,0.000009459366,0.000004875612,0.00002186219,0.000013805706,0.000028878494],"domain_scores_gemma":[0.99981016,0.000027205177,0.000052512314,0.000010528255,0.000060470655,0.000039164173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010138784,0.00012505159,0.00011061582,0.0012452572,0.0007312044,0.0007896191,0.00021480107,0.00020528426,0.0013229254],"category_scores_gemma":[0.00027080532,0.00014438937,0.00010892246,0.0009886279,0.00057871686,0.0002570253,0.00031597808,0.00012994393,0.00014211115],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056465673,0.000021825852,0.9825173,0.000020172163,0.000031539694,0.0006664126,0.0013577841,0.00050244626,0.008173256,0.00014287961,0.00013483301,0.0063750227],"study_design_scores_gemma":[3.4830327e-7,0.0000027515205,0.99947697,0.0000018680022,0.0000020629332,0.000028971903,0.00028529685,0.000074377094,0.000045145942,0.000006439726,0.00007505092,7.687372e-7],"about_ca_topic_score_codex":0.17844105,"about_ca_topic_score_gemma":0.3313861,"teacher_disagreement_score":0.17844105,"about_ca_system_score_codex":0.0009978699,"about_ca_system_score_gemma":0.00054970314,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W2130070389","doi":"10.1130/0016-7606(2001)113<0320:dmapot>2.0.co;2","title":"Detrital modes and provenance of the Paleogene Khojak Formation in Pakistan: Implications for early Himalayan orogeny and unroofing","year":2001,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Citation; Orogeny; Provenance; Paleogene; Icon; Geology; Library science; Paleontology; Computer science","score_opus":0.017547384378190006,"score_gpt":0.23396254231529504,"score_spread":0.21641515793710503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130070389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9799606,0.0014286509,0.00045026533,0.000497036,0.00002417132,0.00002013326,0.0013551618,0.000023603849,0.016240275],"genre_scores_gemma":[0.9967687,0.0010442444,0.00019969248,0.000018249566,0.000013101519,0.000004389179,0.000421325,0.000010330111,0.0015200397],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998543,0.00001977923,0.00001925275,0.000025316123,0.000039858096,0.00004146504],"domain_scores_gemma":[0.999642,0.000073367286,0.0001210588,0.00003415936,0.00009473665,0.000034602057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027465884,0.00012534086,0.00018430525,0.0023012287,0.0015423826,0.0016126612,0.00018367,0.0002627732,0.004461502],"category_scores_gemma":[0.0010393377,0.00016840031,0.000100969206,0.0031413005,0.0015830044,0.00086468976,0.0010274623,0.00032024272,0.0006606908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005950169,0.000039454026,0.8657422,0.00029696646,0.00006342427,0.0026908028,0.017249217,0.0014420511,0.007503199,0.007009278,0.0026956957,0.09467274],"study_design_scores_gemma":[0.000019299134,0.00004385244,0.9782823,0.00009234741,0.000024577163,0.00042793792,0.0064014173,0.00036404515,0.0012951378,0.0015971524,0.011428488,0.000023460796],"about_ca_topic_score_codex":0.043303747,"about_ca_topic_score_gemma":0.08316973,"teacher_disagreement_score":0.043303747,"about_ca_system_score_codex":0.00089648314,"about_ca_system_score_gemma":0.0009758008,"threshold_uncertainty_score":0.08610338},"labels":[],"label_agreement":null},{"id":"W2130177045","doi":"10.1046/j.1365-246x.2002.01762.x","title":"Precursory seismicity changes associated with the 1999 August 17 Izmit (Turkey) earthquake","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Induced seismicity; Seismology; Geology; Aftershock; Epicenter; Tectonics; Seismic hazard","score_opus":0.021649769088749726,"score_gpt":0.20837539301394803,"score_spread":0.18672562392519831,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130177045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996487,0.000034830002,0.000071418355,0.000005081128,0.0000016411244,0.0000053236213,0.00010111234,0.0000074269533,0.0001244301],"genre_scores_gemma":[0.9987024,0.00005698395,0.0002746092,0.0000034755394,0.0000059151816,0.000011490427,0.0008424353,0.0000033676156,0.00009919353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998865,0.000009902878,0.000012664549,0.000027878978,0.000026454985,0.00003659384],"domain_scores_gemma":[0.9996227,0.00002804472,0.00019186338,0.000021462925,0.00007785833,0.000058055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015228576,0.00030422962,0.00029690954,0.0014957415,0.00021522319,0.00030925305,0.00022361477,0.00021084286,0.00049589557],"category_scores_gemma":[0.0007677872,0.00014530106,0.00013572277,0.0007760042,0.00020622674,0.00020377991,0.00043053922,0.00020662077,0.00014911137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033208184,0.00009365208,0.97420394,0.00003490067,0.000032999516,0.00072926364,0.00046437496,0.00092631957,0.0088714445,0.00008321982,0.0002954163,0.013932352],"study_design_scores_gemma":[0.0000037646064,0.000041555923,0.99855727,0.0000025613597,0.000012576891,0.000111977366,0.00011909601,0.0006502694,0.00034541724,0.000010870803,0.00014165988,0.0000030244128],"about_ca_topic_score_codex":0.0057162945,"about_ca_topic_score_gemma":0.009949905,"teacher_disagreement_score":0.0057162945,"about_ca_system_score_codex":0.00036318268,"about_ca_system_score_gemma":0.00026903863,"threshold_uncertainty_score":0.011366069},"labels":[],"label_agreement":null},{"id":"W2130200665","doi":"10.1029/2012jb009147","title":"Paleoearthquakes of the past 30,000 years along the North Tehran Fault (Iran)","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Geological Survey and Mineral Exploration of Iran; Centre National de la Recherche Scientifique","keywords":"Fault scarp; Geology; Seismology; Trench; Fault (geology); Seismic hazard; Slip (aerodynamics); Paleoseismology; Thrust fault; Holocene; Quaternary; Induced seismicity; Active fault; Paleontology","score_opus":0.038916812585297327,"score_gpt":0.2845049935373889,"score_spread":0.24558818095209156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130200665","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998681,0.0002601541,0.00008398091,0.00003447789,0.000009064654,0.000005301675,0.00039416392,0.0000052417727,0.0005266838],"genre_scores_gemma":[0.9982185,0.00029807206,0.00021200266,0.000013957537,0.00002230972,0.00000689268,0.0009008794,0.000002800587,0.00032460838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999199,0.000008732786,0.000008223927,0.000021854305,0.000023888011,0.000017452892],"domain_scores_gemma":[0.9998375,0.000013699554,0.00007401263,0.000013333618,0.000040408482,0.000020991134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021188777,0.00026384287,0.00013781224,0.0014854522,0.00035006562,0.00029293293,0.00021009313,0.0001921738,0.0009107843],"category_scores_gemma":[0.0004253683,0.000103256396,0.00017237947,0.0015381419,0.0003623209,0.00024320478,0.00034795512,0.00016571961,0.00014082975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000121463396,0.000041420135,0.952454,0.00008788326,0.00012638664,0.00079200685,0.0021041182,0.00063219573,0.004350137,0.00022004626,0.00071877707,0.038351562],"study_design_scores_gemma":[0.0000012823433,0.0000073662004,0.9988599,0.0000041438434,0.0000057445272,0.00009662076,0.00016132566,0.00007487415,0.00007315127,0.00001769154,0.0006962924,0.0000016496407],"about_ca_topic_score_codex":0.01792635,"about_ca_topic_score_gemma":0.049945556,"teacher_disagreement_score":0.01792635,"about_ca_system_score_codex":0.00037556855,"about_ca_system_score_gemma":0.00032025675,"threshold_uncertainty_score":0.035643995},"labels":[],"label_agreement":null},{"id":"W2131667221","doi":"10.1186/1880-5981-66-106","title":"Contributions of poroelastic rebound and a weak volcanic arc to the postseismic deformation of the 2011 Tohoku earthquake","year":2014,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Adolph C. and Mary Sprague Miller Institute for Basic Research in Science, University of California Berkeley; National Science Foundation","keywords":"Geology; Subduction; Seismology; Poromechanics; Crust; Submarine pipeline; Deformation (meteorology); Volcano; Viscoelasticity; Subsidence; Convergent boundary; Volcanic arc; Volcanology; Tectonics; Geophysics; Oceanic crust; Geotechnical engineering; Geomorphology","score_opus":0.006456635872668731,"score_gpt":0.18757609818141574,"score_spread":0.181119462308747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131667221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99837506,0.00007133308,0.00053799583,0.00007802181,0.000008462787,0.0000052243245,0.00003993288,0.000031275238,0.000852591],"genre_scores_gemma":[0.99944407,0.00005823048,0.00010558607,0.000012344444,0.0000057718476,0.000004710081,0.000049437193,0.000011166462,0.0003086426],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998455,0.00001910538,0.000013872219,0.00003606518,0.00002153431,0.00006386268],"domain_scores_gemma":[0.9996166,0.00009913068,0.00008173709,0.000046629542,0.000057694346,0.000098134835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002430752,0.0010107562,0.0005260166,0.0008478129,0.00055354525,0.00059241714,0.0005187745,0.0012273191,0.0012299751],"category_scores_gemma":[0.000996323,0.00076019124,0.0008783634,0.00053999305,0.0006549884,0.0007534623,0.0009887621,0.0006063004,0.00014801449],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007735389,0.00048507686,0.2510021,0.00023856653,0.0003028442,0.0026549606,0.0005965008,0.6291509,0.09131792,0.0017408867,0.0004497078,0.021286994],"study_design_scores_gemma":[0.000035018198,0.0002043674,0.2729425,0.00001873115,0.00018568315,0.00022764633,0.00039694164,0.71980953,0.005044589,0.00058876537,0.0004642661,0.00008189666],"about_ca_topic_score_codex":0.01976031,"about_ca_topic_score_gemma":0.011916453,"teacher_disagreement_score":0.01976031,"about_ca_system_score_codex":0.0008018161,"about_ca_system_score_gemma":0.0007644392,"threshold_uncertainty_score":0.039290607},"labels":[],"label_agreement":null},{"id":"W2131992829","doi":"10.1029/2002gl015511","title":"Evidence for both crustal and mantle earthquakes in the subducting Juan de Fuca plate","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Induced seismicity; Receiver function; Mantle (geology); Crust; Intraplate earthquake; Subduction; Oceanic crust; Geophysics; Tectonics; Lithosphere","score_opus":0.13049638660479815,"score_gpt":0.34409689491728235,"score_spread":0.2136005083124842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131992829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994011,0.000051156097,0.000025782361,0.000013200252,5.5090453e-7,5.8802476e-7,0.000027476293,0.0000021286094,0.00047801767],"genre_scores_gemma":[0.99970275,0.000039359187,0.000039639257,0.0000034478865,0.0000013638639,8.834189e-7,0.00007065263,5.156162e-7,0.00014142314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998709,0.000012672228,0.000007428591,0.000030139265,0.000033260865,0.00004557104],"domain_scores_gemma":[0.99915695,0.00014772412,0.00034508127,0.000066608605,0.0001572236,0.00012648388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018219453,0.00017478765,0.00011534092,0.000758913,0.00033997107,0.00044902557,0.0001790546,0.00027274012,0.0007337487],"category_scores_gemma":[0.0014577542,0.00017502115,0.00006526125,0.00071379024,0.0006809994,0.00018113428,0.0004391569,0.00013292705,0.00010086201],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008829999,0.000008782503,0.98035973,0.000020266956,0.000018777542,0.0001877893,0.00070840865,0.00025973612,0.012106286,0.000105506544,0.000045900528,0.0060903328],"study_design_scores_gemma":[0.0000018201739,0.000007874194,0.99931276,0.0000023388309,0.000003338633,0.00010012796,0.00021121801,0.00007473949,0.00014679,0.000018117753,0.000118901036,0.0000019942868],"about_ca_topic_score_codex":0.08522281,"about_ca_topic_score_gemma":0.1361606,"teacher_disagreement_score":0.08522281,"about_ca_system_score_codex":0.0005551266,"about_ca_system_score_gemma":0.00042763472,"threshold_uncertainty_score":0.1694535},"labels":[],"label_agreement":null},{"id":"W2132260136","doi":"10.2118/110542-pa","title":"Fluid Flow in a Fractured Reservoir Using a Geomechanically Constrained Fault-Zone-Damage Model for Reservoir Simulation","year":2009,"lang":"en","type":"article","venue":"SPE Reservoir Evaluation & Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ConocoPhillips (Canada)","funders":"ConocoPhillips; U.S. Department of Energy","keywords":"Geology; Permeability (electromagnetism); Reservoir simulation; Petrology; Seismology; Outcrop; Anisotropy; Geotechnical engineering; Fault (geology); Petroleum engineering; Geomorphology","score_opus":0.06387137769218632,"score_gpt":0.309982515334903,"score_spread":0.2461111376427167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132260136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.57114446,0.0005602991,0.4052992,0.0012380457,0.00016192079,0.00031310055,0.0023374222,0.0014922413,0.01745328],"genre_scores_gemma":[0.9521545,0.00022780431,0.04159882,0.00011051157,0.00004121136,0.0003173176,0.00074971415,0.00012428859,0.0046758973],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998128,0.000045826775,0.000015850017,0.00004246987,0.00004654973,0.000036526366],"domain_scores_gemma":[0.9991893,0.00039335448,0.000095547904,0.00006619578,0.00014784191,0.000107765816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004247384,0.00078056904,0.00094451284,0.000722948,0.0008162565,0.0014079886,0.001744433,0.0028408533,0.0029676673],"category_scores_gemma":[0.0015802146,0.00066971197,0.0013227334,0.00070808723,0.001081857,0.0008383496,0.0012915314,0.001094838,0.00031672727],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011430659,0.000020037376,0.0005644839,0.000006993734,0.0000071373415,0.000030597526,0.00001090227,0.9977671,0.0003780797,0.00066560565,0.000055858312,0.00048170696],"study_design_scores_gemma":[0.0000032028854,0.0000021165883,0.000048867594,7.8812917e-7,8.2740445e-7,0.0000018477082,0.0000017132468,0.999741,0.000037735994,0.00011630789,0.00004382151,0.0000017175279],"about_ca_topic_score_codex":0.032292765,"about_ca_topic_score_gemma":0.015321518,"teacher_disagreement_score":0.032292765,"about_ca_system_score_codex":0.0016987385,"about_ca_system_score_gemma":0.0018862472,"threshold_uncertainty_score":0.06420958},"labels":[],"label_agreement":null},{"id":"W2132816675","doi":"10.1029/2001jb001710","title":"Frequency of large crustal earthquakes in Puget Sound–Southern Georgia Strait predicted from geodetic and geological deformation rates","year":2003,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"U.S. Geological Survey","keywords":"Forearc; Geology; Seismology; Subduction; Seismic moment; Geodetic datum; Deformation (meteorology); Seismic hazard; Geodesy; Fault (geology); Tectonics","score_opus":0.027401594958766224,"score_gpt":0.283288022547717,"score_spread":0.2558864275889508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132816675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990552,0.000028299293,0.00009183569,0.00002481907,0.0000017763331,0.0000028752086,0.00039296594,0.000021574948,0.0003806772],"genre_scores_gemma":[0.998892,0.000027678028,0.00006899499,0.0000066826424,0.0000017686345,0.0000027915187,0.0008648119,0.000003032018,0.00013229772],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989367,0.000017590994,0.000009770137,0.000035638124,0.000022659775,0.000020670563],"domain_scores_gemma":[0.9996222,0.000076532364,0.00012411653,0.000043339336,0.000058307214,0.00007539184],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017269765,0.00015786,0.00009347979,0.0011042682,0.00017102536,0.0003061082,0.0001993334,0.00026244417,0.0013270362],"category_scores_gemma":[0.00088506076,0.00014811559,0.00016545024,0.0005710328,0.00018672095,0.00020582286,0.00033501143,0.00016588054,0.00036320672],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004065459,0.000013680975,0.99157906,0.000006562207,0.000017528197,0.0001056497,0.00015987703,0.000978768,0.000843209,0.000049810285,0.00045311433,0.005752043],"study_design_scores_gemma":[0.0000015253075,0.000013109814,0.99870193,0.000002430026,0.000003799332,0.00006866975,0.000060197177,0.0008667228,0.00005842712,0.000015278416,0.00020566152,0.000002269628],"about_ca_topic_score_codex":0.039159134,"about_ca_topic_score_gemma":0.069284506,"teacher_disagreement_score":0.039159134,"about_ca_system_score_codex":0.000590559,"about_ca_system_score_gemma":0.00027343316,"threshold_uncertainty_score":0.07786238},"labels":[],"label_agreement":null},{"id":"W2132896650","doi":"10.1002/jgrb.50240","title":"A double seismic zone in the subducting Juan Fernandez Ridge of the Nazca Plate (32°S), central Chile","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Slab; Seismology; Slab window; Lithosphere; Induced seismicity; Subduction; Ridge; Focal mechanism; Crust; Oceanic crust; Stress field; Mantle wedge; Volcanism; Tectonics; Geophysics; Paleontology","score_opus":0.047288889167636156,"score_gpt":0.3002259037364177,"score_spread":0.2529370145687816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132896650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99737704,0.0001495509,0.000100283054,0.00002904545,0.0000029275782,0.000011031404,0.00040916554,0.00001542882,0.0019054778],"genre_scores_gemma":[0.99886864,0.00006261886,0.00013529958,0.0000048946467,0.0000024328247,0.000012011934,0.000337658,0.0000020379807,0.0005743781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999275,0.000004245577,0.0000049539253,0.00002189363,0.000014527455,0.000026747208],"domain_scores_gemma":[0.9998524,0.00001188128,0.00005343836,0.0000113043,0.00003596095,0.000034965444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009879607,0.00023628108,0.00017386895,0.0013920082,0.00036731214,0.0005957834,0.00030424062,0.00021715874,0.0013018015],"category_scores_gemma":[0.00034702723,0.00016542042,0.0001254315,0.0010385816,0.0004067452,0.0002046536,0.0008956732,0.00014720742,0.0001723729],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034471357,0.000076372984,0.9266656,0.00017503537,0.000090058566,0.0014697578,0.002934614,0.0011445584,0.041551888,0.0005173414,0.00061731465,0.024412747],"study_design_scores_gemma":[0.000009671489,0.000016730592,0.9970626,0.0000143638,0.000007794417,0.00010173407,0.0010412494,0.00026683992,0.00038532307,0.000042758893,0.0010460641,0.000004810059],"about_ca_topic_score_codex":0.068625264,"about_ca_topic_score_gemma":0.07597287,"teacher_disagreement_score":0.068625264,"about_ca_system_score_codex":0.00074196147,"about_ca_system_score_gemma":0.0007364763,"threshold_uncertainty_score":0.13645166},"labels":[],"label_agreement":null},{"id":"W2133057110","doi":"10.1029/2012gl053892","title":"Effects of subducted seamounts on megathrust earthquake nucleation and rupture propagation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Seamount; Geology; Subduction; Seismology; Trench; Episodic tremor and slip; Nucleation; Tectonics; Oceanography; Materials science","score_opus":0.022354555514667283,"score_gpt":0.2668477002257578,"score_spread":0.24449314471109054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133057110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995528,0.00003336985,0.00016746859,0.0000057755374,0.0000012935108,0.0000014519248,0.000016675898,0.000008146848,0.00021304254],"genre_scores_gemma":[0.9998048,0.000020583375,0.00011882476,0.0000016728237,3.1905913e-7,0.000001118008,0.000012967876,0.0000011797632,0.000038545313],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999069,0.000016419484,0.000010811554,0.00002127406,0.00001656557,0.00002792875],"domain_scores_gemma":[0.9994029,0.00025301543,0.00013865557,0.00007465582,0.000033250653,0.0000975922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022131107,0.00020816295,0.0003089207,0.00026045126,0.0002975823,0.00044397305,0.00031958026,0.00028694462,0.001253495],"category_scores_gemma":[0.0013385019,0.00019670842,0.00021263013,0.00016331031,0.0004697418,0.0002999902,0.00052935584,0.0002263327,0.00006567141],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022059751,0.0004432877,0.1760039,0.00043206938,0.00020443798,0.0012778325,0.00066676043,0.29467517,0.502268,0.0030606796,0.00021676101,0.018545102],"study_design_scores_gemma":[0.00014853568,0.0024813784,0.32687017,0.000062979256,0.00020576363,0.00034866278,0.0007695241,0.5149005,0.15195288,0.0012985329,0.00088571385,0.00007531293],"about_ca_topic_score_codex":0.0038674155,"about_ca_topic_score_gemma":0.003349674,"teacher_disagreement_score":0.0038674155,"about_ca_system_score_codex":0.00037281943,"about_ca_system_score_gemma":0.00021058106,"threshold_uncertainty_score":0.0076898336},"labels":[],"label_agreement":null},{"id":"W2133646821","doi":"10.1029/2001jb000220","title":"Seismotectonics of the Explorer region","year":2002,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Plate tectonics; Seismology; Pacific Plate; Transform fault; North American Plate; Convergent boundary; Epicenter; Tectonics; Seismotectonics; Seafloor spreading; Geodesy; Subduction; Geophysics; Oceanic crust","score_opus":0.07879995389477291,"score_gpt":0.2853298257084136,"score_spread":0.2065298718136407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133646821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910177,0.00021655971,0.0003757246,0.000049398546,0.0000026332764,0.000012755151,0.002243446,0.00006738253,0.0060144006],"genre_scores_gemma":[0.99541783,0.00021233772,0.00065007294,0.000012465376,0.0000062015156,0.000008216127,0.00229208,0.000017853528,0.0013829623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992406,0.000005775578,0.0000039692736,0.000019624094,0.00003258191,0.000014017381],"domain_scores_gemma":[0.99985003,0.000017546798,0.000037572543,0.000017195602,0.000042605323,0.000035132925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011377283,0.000194572,0.00012994134,0.0010555836,0.00027054854,0.00038216947,0.00025141705,0.000118769734,0.0010099846],"category_scores_gemma":[0.00042153834,0.000088753295,0.000101356236,0.0012752241,0.00020466316,0.00014164874,0.00047096197,0.00016747955,0.00016343727],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028212246,0.000053773812,0.8566081,0.00016857503,0.00017420358,0.001963558,0.0032574108,0.012441388,0.050375685,0.0019209059,0.0032301035,0.06952412],"study_design_scores_gemma":[0.0000052898577,0.000017955088,0.9945884,0.000009165367,0.000013388324,0.00015845649,0.00031199152,0.0011940507,0.00065550144,0.00006300614,0.0029724962,0.000010352318],"about_ca_topic_score_codex":0.22342552,"about_ca_topic_score_gemma":0.34772384,"teacher_disagreement_score":0.22342552,"about_ca_system_score_codex":0.00079552864,"about_ca_system_score_gemma":0.00067284127,"threshold_uncertainty_score":0.44425005},"labels":[],"label_agreement":null},{"id":"W2134713317","doi":"10.1029/2008jb005875","title":"Seismic wave triggering of nonvolcanic tremor, episodic tremor and slip, and earthquakes on Vancouver Island","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Seismology; Geology; Aftershock; Amplitude; Induced seismicity; Episodic tremor and slip; Slip (aerodynamics); Remotely triggered earthquakes; Seismic wave; Subduction; Seismic gap; Tectonics; Physics","score_opus":0.029965481954975958,"score_gpt":0.2725669350522475,"score_spread":0.24260145309727155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134713317","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99863213,0.000029078758,0.0000150737515,0.000010399425,5.7018366e-7,0.0000044679027,0.00015532124,0.0000018579574,0.0011510022],"genre_scores_gemma":[0.9990458,0.00006581849,0.00002795003,0.0000061399237,9.4994886e-7,0.0000033473584,0.00026865248,0.0000011775124,0.00058026146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983585,0.000011206532,0.000009895985,0.000026843338,0.000052169344,0.000063954394],"domain_scores_gemma":[0.99950457,0.000045388468,0.00009596166,0.000015849833,0.0001528557,0.00018534812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010442253,0.00021085591,0.00021557913,0.00096420257,0.0009917303,0.000821784,0.00035810584,0.0002890721,0.0016768131],"category_scores_gemma":[0.0005350125,0.0002157646,0.0001329709,0.0011546479,0.00044041206,0.00013269024,0.00071624195,0.00017385038,0.0001723826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023253051,0.00006201898,0.9735357,0.000054851116,0.00007303818,0.0011146124,0.00075204426,0.0021136699,0.010950144,0.0001590623,0.00044561847,0.010506641],"study_design_scores_gemma":[0.0000034299064,0.000013267053,0.99894553,0.0000043088903,0.000005569985,0.000029867726,0.00040036102,0.00035810453,0.00010544427,0.000008899529,0.00012241249,0.000002824977],"about_ca_topic_score_codex":0.7817323,"about_ca_topic_score_gemma":0.94438094,"teacher_disagreement_score":0.7817323,"about_ca_system_score_codex":0.003075428,"about_ca_system_score_gemma":0.0019330087,"threshold_uncertainty_score":0.43910617},"labels":[],"label_agreement":null},{"id":"W2134909076","doi":"10.1002/2014jb011237","title":"Average<i>Q</i><sub>Lg</sub>,<i>Q</i><sub>Sn</sub>, and observation of Lg blockage in the Continental Margin of Nova Scotia","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Attenuation; Amplitude; Nova scotia; Continental margin; Geology; Spectral line; Physics; Phase (matter); Geodesy; Seismology; Tectonics; Optics","score_opus":0.03513808118598524,"score_gpt":0.2813312903703435,"score_spread":0.24619320918435825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134909076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99806696,0.000029834258,0.000120446224,0.000011392699,9.117441e-7,0.0000028218735,0.00041777574,0.000009481745,0.0013403299],"genre_scores_gemma":[0.9994429,0.000018833189,0.00007925742,0.0000035324742,9.312587e-7,0.000001181706,0.00023485011,0.0000023006667,0.00021619441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.000003614167,0.000003850873,0.00001154812,0.00002219533,0.000017910075],"domain_scores_gemma":[0.99966085,0.000035638695,0.00006463842,0.000021056108,0.00016158211,0.000056288805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012424965,0.000117166106,0.000081372615,0.00063081284,0.00038621892,0.0003363066,0.00017660751,0.000088744324,0.0007064342],"category_scores_gemma":[0.00039931684,0.00008387126,0.00008394031,0.0005496643,0.00026339674,0.00009689784,0.00020877716,0.00011070911,0.00013087608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010488491,0.000010781262,0.97847545,0.000014984425,0.000025245918,0.00011435367,0.00019935572,0.0007328301,0.013965057,0.000060824244,0.00027452435,0.006021627],"study_design_scores_gemma":[0.0000011446916,0.0000033909234,0.99914956,0.000001375305,0.000003088213,0.000014051838,0.000066533205,0.00031062873,0.00033576196,0.0000049234714,0.0001086234,8.119022e-7],"about_ca_topic_score_codex":0.6681258,"about_ca_topic_score_gemma":0.78448653,"teacher_disagreement_score":0.3318742,"about_ca_system_score_codex":0.001317688,"about_ca_system_score_gemma":0.0006944325,"threshold_uncertainty_score":0.6676573},"labels":[],"label_agreement":null},{"id":"W2135993575","doi":"10.1111/j.1365-246x.2006.03090.x","title":"Three-dimensional structure across the Tintina strike-slip fault, northern Canadian Cordillera, from seismic refraction and reflection tomography","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismology; Terrane; Lithosphere; Geodesy; Crust; Tectonics; Refraction; Reflection (computer programming); Fault (geology); Seismic tomography; Mantle (geology); Geophysics","score_opus":0.008171230081702945,"score_gpt":0.2228727384538443,"score_spread":0.21470150837214136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135993575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98449266,0.0005334886,0.0018690447,0.00014457515,0.000012279713,0.00008414083,0.007346457,0.0003402625,0.005177052],"genre_scores_gemma":[0.9855409,0.0005074936,0.0049129296,0.000042029445,0.0000067169817,0.000028498955,0.007240348,0.00005169952,0.0016693482],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978584,0.0000053527096,0.000009735184,0.00005393511,0.0000935368,0.000051493862],"domain_scores_gemma":[0.9997367,0.000014782555,0.000028892644,0.000014749489,0.00016419454,0.000040715287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017906689,0.0009769124,0.00024631643,0.0023449946,0.0012841125,0.0014816244,0.0008501942,0.00044729497,0.0027397706],"category_scores_gemma":[0.0010096913,0.00047557655,0.00039782096,0.004665158,0.0005257224,0.0003236632,0.0006301008,0.00032549852,0.00036792085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004902645,0.00019700715,0.6767952,0.00050668366,0.00031839538,0.0018547245,0.0023151864,0.082347594,0.06207737,0.0016023191,0.007936607,0.16355868],"study_design_scores_gemma":[0.000032371387,0.000024886203,0.94066936,0.000051389656,0.000087477216,0.00021176242,0.00085985643,0.05088324,0.0020099604,0.0001733938,0.00492226,0.00007407815],"about_ca_topic_score_codex":0.9824154,"about_ca_topic_score_gemma":0.9925997,"teacher_disagreement_score":0.017584622,"about_ca_system_score_codex":0.008642752,"about_ca_system_score_gemma":0.0132502755,"threshold_uncertainty_score":0.06270784},"labels":[],"label_agreement":null},{"id":"W2136090417","doi":"10.1785/0220150066","title":"Focal Mechanisms of Some Inferred Induced Earthquakes in Alberta, Canada","year":2015,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Citation; Library science; Download; Icon; History; Archaeology; World Wide Web; Computer science","score_opus":0.10193671526573862,"score_gpt":0.29931506305271255,"score_spread":0.19737834778697394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136090417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98634446,0.00039681877,0.00026203218,0.00026932784,0.0000096751155,0.000022716335,0.00088718935,0.000029728955,0.011778102],"genre_scores_gemma":[0.9971317,0.0001829673,0.00013450194,0.000024459117,0.000002418614,0.0000032548494,0.0002363385,0.0000028628062,0.0022815305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989414,0.0000046829214,0.000004287662,0.0000135809105,0.000035943252,0.000047266254],"domain_scores_gemma":[0.9995765,0.000031199397,0.000047072048,0.000009825746,0.00024617274,0.0000891866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014408623,0.00016793801,0.00012227483,0.0011011951,0.0014951149,0.0006800733,0.0006147426,0.00031942857,0.0029012081],"category_scores_gemma":[0.0006268854,0.00011328773,0.00009102061,0.001523164,0.0004989837,0.00012352054,0.00050360843,0.00021412526,0.00017853515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007273573,0.00012814191,0.8755822,0.00015043773,0.00009234549,0.002324039,0.0046310495,0.005905351,0.021535194,0.0045161564,0.0070355735,0.07737219],"study_design_scores_gemma":[0.000013296018,0.00002305658,0.9923396,0.000014765515,0.000021648975,0.00011036319,0.0026570174,0.0011772623,0.00075973495,0.00019172569,0.0026779445,0.000013470207],"about_ca_topic_score_codex":0.9818595,"about_ca_topic_score_gemma":0.99281305,"teacher_disagreement_score":0.018140495,"about_ca_system_score_codex":0.011764597,"about_ca_system_score_gemma":0.008518972,"threshold_uncertainty_score":0.08535856},"labels":[],"label_agreement":null},{"id":"W2136633733","doi":"10.1111/j.1365-246x.2004.02270.x","title":"Contemporary kinematics of the southern Aegean and the Mediterranean Ridge","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Nautical Research Society","funders":"","keywords":"Geology; Kinematics; Geodesy; Seismology; Ridge; Deformation (meteorology); Seamount; Strain rate; Accretionary wedge; Shear zone; Geometry; Tectonics; Subduction; Paleontology","score_opus":0.02060609875480814,"score_gpt":0.22202936686901542,"score_spread":0.20142326811420727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136633733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9336557,0.0036849452,0.0031168899,0.0005464926,0.00005815904,0.000020088151,0.0007557542,0.000088348854,0.058073573],"genre_scores_gemma":[0.9935772,0.0014127267,0.001762504,0.00003461575,0.000015951431,0.000007803284,0.0003487168,0.000014529346,0.0028258967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999474,0.000008887113,0.000004446293,0.000017100947,0.000013136132,0.000009089931],"domain_scores_gemma":[0.99995923,0.000002275858,0.00001416,0.000005123094,0.000013072301,0.000006036756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021278732,0.00020780462,0.000113396454,0.0004842378,0.00020100013,0.0006057581,0.00020725076,0.00020079096,0.0021993439],"category_scores_gemma":[0.00029291114,0.00012695536,0.00013094836,0.0004050562,0.0004896657,0.00037023306,0.00034634225,0.00014669486,0.00040282492],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024243325,0.000050748968,0.6285456,0.000186581,0.00014530652,0.0011070326,0.0023840657,0.05341713,0.01956255,0.030177176,0.0036588423,0.26052257],"study_design_scores_gemma":[0.00003370247,0.000058286598,0.92234814,0.00013919442,0.000023906927,0.00043556065,0.0012058412,0.0130429035,0.0010130653,0.003192161,0.05847798,0.000029180803],"about_ca_topic_score_codex":0.027335819,"about_ca_topic_score_gemma":0.028026583,"teacher_disagreement_score":0.027335819,"about_ca_system_score_codex":0.0010203404,"about_ca_system_score_gemma":0.0003818381,"threshold_uncertainty_score":0.054353416},"labels":[],"label_agreement":null},{"id":"W2136989388","doi":"10.3906/yer-0803-4","title":"The Relationship Between the Tectonic Setting of the Lake İznik Basin and the Middle Strand of the North Anatolian Fault","year":2009,"lang":"en","type":"article","venue":"TURKISH JOURNAL OF EARTH SCIENCES","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stantec (Canada)","funders":"","keywords":"Geology; North Anatolian Fault; Seismology; Structural basin; Tectonics; Fault (geology); Holocene; Shear (geology); Basin and range topography; Quaternary; Active fault; Geomorphology; Paleontology","score_opus":0.03616123818294137,"score_gpt":0.23737685457411603,"score_spread":0.20121561639117466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136989388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99639505,0.0005095303,0.000077614925,0.00009400269,0.0000051165503,0.000003699377,0.00010471228,0.000005428338,0.002804894],"genre_scores_gemma":[0.9994987,0.0001385084,0.00005995387,0.0000066704088,0.000003892003,0.0000021367703,0.00008011169,0.0000016377654,0.0002082973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998983,0.000015584175,0.000011633224,0.00002845972,0.000016711663,0.000029282426],"domain_scores_gemma":[0.9998542,0.000015768173,0.00006563302,0.000005788209,0.00003464331,0.000023858052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010431325,0.00012284561,0.00016072686,0.0013196107,0.00038489135,0.000797754,0.0001734004,0.00018616079,0.0020861072],"category_scores_gemma":[0.00032091967,0.00010392218,0.00010408224,0.0010603645,0.00040891985,0.00044897656,0.0005788639,0.00015190247,0.00018444887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022582876,0.00004326812,0.9682266,0.00009208454,0.00009198694,0.0007901424,0.001384941,0.000844005,0.00630483,0.0025314318,0.00051181455,0.018953081],"study_design_scores_gemma":[0.0000038856197,0.000008771925,0.99732673,0.000014777468,0.000015918966,0.00017597488,0.0005752193,0.0003508183,0.00013058164,0.00017030601,0.0012225689,0.0000044557687],"about_ca_topic_score_codex":0.016595216,"about_ca_topic_score_gemma":0.02486987,"teacher_disagreement_score":0.016595216,"about_ca_system_score_codex":0.0009602536,"about_ca_system_score_gemma":0.00067801535,"threshold_uncertainty_score":0.03299725},"labels":[],"label_agreement":null},{"id":"W2137455617","doi":"10.1785/0120040095","title":"A Revised Magnitude-Recurrence Relation for Shallow Crustal Earthquakes in Southwestern British Columbia: Considering the Relationships between Moment Magnitude and Regional Magnitudes","year":2005,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Magnitude (astronomy); Moment magnitude scale; Geology; Seismology; Moment (physics); Earthquake magnitude; Geodesy; Geometry; Mathematics; Physics","score_opus":0.03939684188599961,"score_gpt":0.22597483966868354,"score_spread":0.1865779977826839,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137455617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8181824,0.0030493627,0.11649696,0.0012976492,0.00012042476,0.00027604328,0.00989615,0.0013525524,0.04932852],"genre_scores_gemma":[0.9597182,0.0010355717,0.02778753,0.00011079721,0.00006357084,0.000061954364,0.0035808831,0.00014718968,0.0074942377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995192,0.000045074496,0.000075619166,0.00012450015,0.00017623145,0.000059286336],"domain_scores_gemma":[0.9977291,0.00031021613,0.0005042975,0.00020639678,0.0011628103,0.00008714388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070962345,0.00038089228,0.00037830326,0.0033232775,0.00048082403,0.0016324462,0.0010015048,0.00032592673,0.0024802207],"category_scores_gemma":[0.006208993,0.0001808747,0.00031155156,0.0034661253,0.00038772923,0.0007957732,0.0005078967,0.0006748501,0.00062583503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010035723,0.000075055,0.6205414,0.0003705402,0.00014594749,0.0010527939,0.0017093406,0.043859214,0.014026224,0.01156932,0.016444813,0.29010507],"study_design_scores_gemma":[0.000015973335,0.000063566906,0.89680326,0.0000889159,0.000100427984,0.00054312294,0.00064450654,0.07040593,0.002192981,0.0024750927,0.026584541,0.00008161234],"about_ca_topic_score_codex":0.6410535,"about_ca_topic_score_gemma":0.7450838,"teacher_disagreement_score":0.3589465,"about_ca_system_score_codex":0.0028764573,"about_ca_system_score_gemma":0.0025677958,"threshold_uncertainty_score":0.7221208},"labels":[],"label_agreement":null},{"id":"W2137748830","doi":"10.1002/2014jb011821","title":"Layered crustal anisotropy around the San Andreas Fault near Parkfield, California","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Crust; Anisotropy; Seismology; Seismic anisotropy; Brittleness; Deformation (meteorology); Fault (geology); Geophysics; Petrology; Mantle (geology); Materials science","score_opus":0.07337791509720246,"score_gpt":0.33172335846915146,"score_spread":0.258345443371949,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137748830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99868566,0.00005236464,0.00006428074,0.000033765005,0.0000013090379,0.0000025945587,0.00013532898,0.000020087044,0.0010045458],"genre_scores_gemma":[0.9995609,0.000031766744,0.00008933877,0.000003675809,0.000002182856,7.965203e-7,0.00009763816,0.000001380478,0.00021231084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999132,0.000005680208,0.0000044998806,0.000030153966,0.000027955388,0.000018452889],"domain_scores_gemma":[0.99983644,0.000019827394,0.000048298825,0.000012036088,0.00005755117,0.000025869393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012790972,0.0001677762,0.00015510523,0.0008561013,0.00038343013,0.00039583017,0.0002324223,0.00016677343,0.001371842],"category_scores_gemma":[0.0004207755,0.00018310083,0.000070111855,0.00041816616,0.00024068763,0.00023001124,0.00030333266,0.00015742531,0.00014846004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021407103,0.00009668991,0.9275508,0.000052219075,0.00010139541,0.00043590143,0.00095203175,0.0047648028,0.047125757,0.00036676574,0.0007072815,0.017632237],"study_design_scores_gemma":[0.000008425488,0.000010900044,0.99688333,0.0000052277937,0.000011327963,0.000037480393,0.00018303934,0.0020091536,0.00048227364,0.000026763406,0.000337633,0.000004457552],"about_ca_topic_score_codex":0.12690319,"about_ca_topic_score_gemma":0.17900752,"teacher_disagreement_score":0.12690319,"about_ca_system_score_codex":0.00063623337,"about_ca_system_score_gemma":0.00040455072,"threshold_uncertainty_score":0.25232905},"labels":[],"label_agreement":null},{"id":"W2137797182","doi":"10.1111/j.1365-246x.2006.02815.x","title":"Earthquake scaling: the effect of a viscoelastic asthenosphere","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Crust; Viscoelasticity; Scaling; Slip (aerodynamics); Seismology; Rheology; Geophysics; Creep; Geometry; Physics","score_opus":0.004948107300744713,"score_gpt":0.20820019005537463,"score_spread":0.20325208275462991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137797182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9769025,0.00088119233,0.016889334,0.00033783691,0.00003595749,0.000022514247,0.0001151608,0.00021240866,0.004603079],"genre_scores_gemma":[0.9988379,0.0001729925,0.00068744697,0.000020425132,0.000015541598,0.0000035226578,0.00001651743,0.000017452938,0.0002281185],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986076,0.00004260367,0.000011277787,0.000031907915,0.000032520427,0.000020843325],"domain_scores_gemma":[0.9989436,0.00046795947,0.00023384778,0.0002032069,0.00006139867,0.00008986877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031763504,0.00046986178,0.00028847056,0.00032745255,0.00021415426,0.00060423755,0.0003481481,0.00053577416,0.0012592479],"category_scores_gemma":[0.0035261,0.00019827057,0.00044033543,0.0002789749,0.00057598884,0.0011598323,0.0005365632,0.00030055045,0.00014594049],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033826544,0.00018525856,0.043381266,0.00026702177,0.0001789065,0.0012542313,0.0005956047,0.7278601,0.15024413,0.030455405,0.0015598318,0.04367997],"study_design_scores_gemma":[0.00006620572,0.00032706533,0.050878037,0.000034669258,0.00009595046,0.00046085267,0.00014994349,0.90620154,0.009820867,0.029716996,0.0021772156,0.00007068874],"about_ca_topic_score_codex":0.0012320417,"about_ca_topic_score_gemma":0.00055984326,"teacher_disagreement_score":0.0012592479,"about_ca_system_score_codex":0.00025235847,"about_ca_system_score_gemma":0.00017706124,"threshold_uncertainty_score":0.0042125583},"labels":[],"label_agreement":null},{"id":"W2137972163","doi":"10.1111/j.1365-246x.2004.02276.x","title":"The Source-Scanning Algorithm: mapping the distribution of seismic sources in time and space","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":447,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Seismogram; Waveform; Algorithm; Amplitude; Brightness; A priori and a posteriori; Geology; Episodic tremor and slip; Computer science; Subduction; Seismology; Optics; Telecommunications; Physics","score_opus":0.01054358402378899,"score_gpt":0.20610852878797747,"score_spread":0.19556494476418848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137972163","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0043508452,0.000047512724,0.9942636,0.000025882795,0.000010810587,0.000018420247,0.00006756449,0.00070263736,0.0005126737],"genre_scores_gemma":[0.039261926,0.000095311334,0.959159,0.000021020973,0.00002115485,0.00007870526,0.00025495156,0.00014286206,0.00096505205],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99976677,0.000046115416,0.000013727985,0.000054447366,0.00009813217,0.00002093663],"domain_scores_gemma":[0.9994142,0.00025158282,0.000067214045,0.00009600543,0.00014396764,0.000027082287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006342433,0.00078524154,0.0004584298,0.001489321,0.0003418545,0.0007473952,0.0009765774,0.00063744665,0.0030651707],"category_scores_gemma":[0.002205178,0.00038496088,0.00045688628,0.0012497767,0.0005437127,0.0013275614,0.00091492094,0.0005843285,0.0013559782],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002643647,0.000085436375,0.005691933,0.00016405403,0.000107550884,0.00022190985,0.00027337763,0.061373472,0.0712407,0.024100374,0.0053124493,0.83116436],"study_design_scores_gemma":[0.00007651233,0.00009156751,0.003524233,0.000022976981,0.000034284156,0.00075707573,0.00006970655,0.9231863,0.035445917,0.01935587,0.017385246,0.00005034271],"about_ca_topic_score_codex":0.0017275803,"about_ca_topic_score_gemma":0.0022435852,"teacher_disagreement_score":0.0030651707,"about_ca_system_score_codex":0.00022772304,"about_ca_system_score_gemma":0.00086142175,"threshold_uncertainty_score":0.010254025},"labels":[],"label_agreement":null},{"id":"W2138500572","doi":"10.1111/bre.12123","title":"Continental margin syn‐rift salt tectonics at intermediate width margins","year":2015,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Killam Trusts; Dalhousie University; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Geology; Rift; Evaporite; Graben; Salt tectonics; Clastic rock; Sedimentary rock; Passive margin; Half-graben; Lithosphere; Petrology; Progradation; Diapir; Salt pan; Geomorphology; Paleontology; Geochemistry; Tectonics; Sedimentary depositional environment","score_opus":0.09646655519021707,"score_gpt":0.32334962319133426,"score_spread":0.22688306800111718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138500572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965463,0.000037480735,0.0009825638,0.000049209266,0.0000025655308,0.0000037234781,0.00010994254,0.000023522649,0.002244651],"genre_scores_gemma":[0.9993862,0.00002177806,0.00020716588,0.0000066393486,0.0000010059733,0.0000024030032,0.00004469577,0.000005922507,0.00032433635],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993575,0.000016354288,0.0000055352416,0.000018147455,0.00000971216,0.000014583322],"domain_scores_gemma":[0.999877,0.000030462428,0.00002863433,0.000016776808,0.00002070577,0.000026382853],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017250393,0.00032043236,0.0002735495,0.00028000295,0.0002660273,0.0009445966,0.0004659016,0.0004992166,0.001531581],"category_scores_gemma":[0.0006192488,0.0002640326,0.00044058714,0.00023241655,0.00039984554,0.0003612579,0.0005594181,0.00023530134,0.00011328773],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011013841,0.000027447379,0.068494424,0.000031449043,0.00007547925,0.00023374856,0.00013151055,0.914959,0.010217578,0.0025638652,0.00015211932,0.0030031519],"study_design_scores_gemma":[0.00005626994,0.00015017758,0.07451291,0.000020488811,0.00005523418,0.00010280687,0.00014623204,0.92105156,0.0018355949,0.0012798756,0.0007611512,0.000027575285],"about_ca_topic_score_codex":0.013681161,"about_ca_topic_score_gemma":0.014470215,"teacher_disagreement_score":0.013681161,"about_ca_system_score_codex":0.00081578526,"about_ca_system_score_gemma":0.00034810213,"threshold_uncertainty_score":0.027203083},"labels":[],"label_agreement":null},{"id":"W2138660802","doi":"10.1016/j.epsl.2012.02.003","title":"An intermediate-depth tensional earthquake (MW 5.7) and its aftershocks within the Nazca slab, central Chile: A reactivated outer rise fault?","year":2012,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Seismology; Aftershock; Slab; Seafloor spreading; Fault (geology); Longitude; Induced seismicity; Seismic gap; Magnitude (astronomy); Earthquake rupture; Latitude; Geodesy; Geophysics","score_opus":0.012092336145112216,"score_gpt":0.2045430032238372,"score_spread":0.192450667078725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138660802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932721,0.0003300075,0.00006634265,0.00082042057,0.000016417122,0.000011212771,0.00011390753,0.000007799087,0.0053617912],"genre_scores_gemma":[0.99839836,0.00021522972,0.000030963285,0.00006583941,0.000020909467,0.000003832141,0.00011321223,0.000002069163,0.0011496288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999205,0.0000063654306,0.000004786699,0.0000127809635,0.000007396398,0.000048229147],"domain_scores_gemma":[0.9997315,0.000023575967,0.00011536691,0.000021530972,0.000046777703,0.000061173574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001437089,0.00016711694,0.00017677482,0.00044300727,0.0006073479,0.0011315742,0.0005586543,0.00080611743,0.004045683],"category_scores_gemma":[0.0009640796,0.00015435455,0.00019444365,0.00077812193,0.0009204693,0.0009936573,0.0008533229,0.00043198201,0.00037054942],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011819437,0.00024792278,0.9129327,0.00025358223,0.00013293393,0.010618171,0.009779817,0.0012274685,0.016301593,0.008801689,0.0028383194,0.03568392],"study_design_scores_gemma":[0.00004912362,0.000070398884,0.986642,0.000049666094,0.000034478242,0.00045209483,0.0067086234,0.00023423637,0.00038565972,0.00085381884,0.0045033772,0.000016407781],"about_ca_topic_score_codex":0.058633804,"about_ca_topic_score_gemma":0.059819907,"teacher_disagreement_score":0.058633804,"about_ca_system_score_codex":0.0013496462,"about_ca_system_score_gemma":0.0012268446,"threshold_uncertainty_score":0.116585016},"labels":[],"label_agreement":null},{"id":"W2138666411","doi":"10.1130/g34483.1","title":"Silica gel formation during fault slip: Evidence from the rock record","year":2013,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Ames Research Center; National Science Foundation","keywords":"Geology; Quartz; Fault (geology); Lubrication; Slip (aerodynamics); Impact crater; Layer (electronics); Mineralogy; Composite material; Materials science; Seismology","score_opus":0.021085570972746454,"score_gpt":0.20798909773390506,"score_spread":0.1869035267611586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138666411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99764365,0.000694274,0.00013657982,0.00003197799,0.0000052366927,0.0000040052482,0.00044633614,0.000012895213,0.0010250498],"genre_scores_gemma":[0.99887246,0.00031938832,0.00024237264,0.000015240506,0.000012094096,0.0000027264227,0.00035063614,0.0000039167444,0.00018108952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986625,0.000008543662,0.00001288681,0.00004810058,0.000041724208,0.000022500857],"domain_scores_gemma":[0.99908316,0.00012597715,0.00042423807,0.00007184803,0.00022156473,0.0000732241],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023057683,0.0001793025,0.00012473874,0.0016073075,0.0004118893,0.00039475903,0.00020108485,0.00038896,0.0006375217],"category_scores_gemma":[0.00075208175,0.0001882065,0.000105383035,0.0009163115,0.00073645945,0.00038221994,0.0003856191,0.00021086095,0.000159467],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019522395,0.000029126051,0.9371516,0.00016628578,0.00008189867,0.00040959296,0.001040784,0.0001165959,0.046104144,0.00007642098,0.00035365383,0.014274606],"study_design_scores_gemma":[0.000003262448,0.000031245858,0.9973677,0.0000058785026,0.000016045075,0.00010142831,0.00011512245,0.00007070587,0.0015780397,0.000011181501,0.0006967922,0.0000025902648],"about_ca_topic_score_codex":0.014750191,"about_ca_topic_score_gemma":0.033814173,"teacher_disagreement_score":0.014750191,"about_ca_system_score_codex":0.00035629625,"about_ca_system_score_gemma":0.0002280507,"threshold_uncertainty_score":0.029328644},"labels":[],"label_agreement":null},{"id":"W2139034619","doi":"10.1002/jgrb.50289","title":"Magma storage and migration associated with the 2011–2012 El Hierro eruption: Implications for crustal magmatic systems at oceanic island volcanoes","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Western University","funders":"","keywords":"Geology; Volcano; Magma; Seismology; Underplating; Magma chamber; Subduction; Tectonics","score_opus":0.03278165837653291,"score_gpt":0.2933098242273749,"score_spread":0.260528165850842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139034619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899954,0.00008380963,0.00037461246,0.000048085065,0.0000017856587,0.0000038307357,0.00011719273,0.0000139217655,0.00035714623],"genre_scores_gemma":[0.9994935,0.000044220895,0.00025437347,0.0000046144355,0.0000026921593,0.0000015931618,0.00013117648,0.0000042898655,0.00006353008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999461,0.000007749073,0.0000038044095,0.000020518602,0.0000064208143,0.00001533894],"domain_scores_gemma":[0.9999007,0.00002137227,0.00002973098,0.000011073839,0.000014108786,0.000023114048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020954717,0.00036143395,0.00028578946,0.0006061528,0.0003178077,0.0008257362,0.00037875993,0.0005293304,0.00078057457],"category_scores_gemma":[0.00046616455,0.00024719918,0.0004972474,0.00046791593,0.00038541327,0.00053680467,0.0004261191,0.00027849895,0.00009008226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019077807,0.00019120795,0.8005488,0.00008317517,0.00022699403,0.0004783459,0.0006205355,0.14390633,0.03701641,0.0012617522,0.00033616912,0.015139541],"study_design_scores_gemma":[0.000016645097,0.000044280845,0.72483635,0.000011428254,0.000038942257,0.00008887343,0.00039657755,0.2726088,0.0011119435,0.00046802804,0.00035405782,0.000024035047],"about_ca_topic_score_codex":0.041422248,"about_ca_topic_score_gemma":0.04098941,"teacher_disagreement_score":0.041422248,"about_ca_system_score_codex":0.00076268153,"about_ca_system_score_gemma":0.0004950351,"threshold_uncertainty_score":0.082362294},"labels":[],"label_agreement":null},{"id":"W2139098281","doi":"10.1785/0120070097","title":"Effects of Frictional Behavior and Geometry of Subduction Fault on Coseismic Seafloor Deformation","year":2008,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seafloor spreading; Subduction; Seismology; Deformation (meteorology); Geometry; Fault (geology); Geodesy; Geophysics; Tectonics; Oceanography; Mathematics","score_opus":0.011123988132513876,"score_gpt":0.19630336535607182,"score_spread":0.18517937722355793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139098281","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99908745,0.000030867035,0.00036290343,0.000020468378,0.00000233193,0.0000026057294,0.000033119668,0.000013386902,0.00044685567],"genre_scores_gemma":[0.9998254,0.0000138317555,0.00006150059,0.0000031652432,5.3576787e-7,6.158152e-7,0.000014363696,0.0000022745812,0.00007826708],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987173,0.0000391701,0.000009927601,0.000020445083,0.00001778186,0.00004093201],"domain_scores_gemma":[0.99948394,0.0002550422,0.000077894445,0.000055745102,0.000035174664,0.000092169525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002491192,0.0005432102,0.00037840367,0.000458022,0.00025406238,0.0006497456,0.00028992028,0.0005546615,0.0019023274],"category_scores_gemma":[0.0015774267,0.00034230598,0.00046186225,0.00025636304,0.0005962183,0.00036544522,0.00053110125,0.00027830093,0.0001857195],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005983516,0.00022940671,0.060367625,0.00005378646,0.00010148678,0.00039369316,0.000083535546,0.87343204,0.059046105,0.0004386887,0.00012871876,0.005126529],"study_design_scores_gemma":[0.000076762146,0.0007060464,0.07834402,0.000016512744,0.00008205985,0.00014430865,0.00015013326,0.9081207,0.011899704,0.00022592719,0.00020391968,0.000029961608],"about_ca_topic_score_codex":0.008741954,"about_ca_topic_score_gemma":0.0072472887,"teacher_disagreement_score":0.008741954,"about_ca_system_score_codex":0.00047962883,"about_ca_system_score_gemma":0.0003312723,"threshold_uncertainty_score":0.017382145},"labels":[],"label_agreement":null},{"id":"W2139644500","doi":"10.1785/0120130321","title":"Surface Ruptures of the Mw 6.8 March 2011 Tarlay Earthquake, Eastern Myanmar","year":2014,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Transportation of Ontario","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Seismology; Geology","score_opus":0.015588619551268843,"score_gpt":0.20507357112649635,"score_spread":0.18948495157522752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139644500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995321,0.000009201574,0.000017707835,0.000015190811,0.0000011703054,0.0000017003129,0.00010861214,0.0000022744648,0.0003120984],"genre_scores_gemma":[0.9994758,0.000018145682,0.000045403485,0.000004680199,0.0000024400026,0.0000032961455,0.00028807455,9.864069e-7,0.00016119667],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.000006482838,0.000004271516,0.0000121328085,0.000010613979,0.00001702119],"domain_scores_gemma":[0.9998715,0.00000878703,0.00006631993,0.000015683141,0.000021171403,0.000016558948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011647811,0.00012317122,0.000111364934,0.00025549292,0.00033084056,0.00023702138,0.00016006753,0.00022660304,0.00057087856],"category_scores_gemma":[0.0004271633,0.00009860331,0.00007313911,0.00028517868,0.00020967227,0.0002690761,0.00050001335,0.00018884048,0.00016785252],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004461136,0.00010269707,0.9312046,0.000065908396,0.00007601044,0.002199901,0.0051350375,0.0012770629,0.036607772,0.0003399477,0.0018149815,0.020729866],"study_design_scores_gemma":[0.0000036337444,0.000044966262,0.9982951,0.0000031721327,0.000004965205,0.00011113379,0.0003809332,0.0002796097,0.0004163033,0.00001203344,0.00044587007,0.0000022888428],"about_ca_topic_score_codex":0.007904965,"about_ca_topic_score_gemma":0.01988247,"teacher_disagreement_score":0.007904965,"about_ca_system_score_codex":0.00031649214,"about_ca_system_score_gemma":0.00014444596,"threshold_uncertainty_score":0.015717924},"labels":[],"label_agreement":null},{"id":"W2139680152","doi":"10.5194/adgeo-14-105-2008","title":"Near-source observations and modeling of the Kuril Islands tsunamis of 15 November 2006 and 13 January 2007","year":2008,"lang":"en","type":"article","venue":"Advances in geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Hokkaido University; Russian Foundation for Basic Research","keywords":"Geology; Tide gauge; Seismology; Source model; Tsunami wave; Tsunami earthquake; Elevation (ballistics); Waves and shallow water; Oceanography; Climatology; Sea level; Physics","score_opus":0.021781806901708667,"score_gpt":0.22556264384978825,"score_spread":0.20378083694807958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139680152","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99626607,0.00006423842,0.0019618322,0.000063030915,0.000014047396,0.00001415035,0.0004668732,0.0001036944,0.0010460351],"genre_scores_gemma":[0.99825305,0.000029660481,0.00095847494,0.0000073964397,0.000005612091,0.000010110949,0.0004969525,0.000009614483,0.00022924512],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999305,0.000014037831,0.000005785621,0.00002242762,0.000012771039,0.000014447875],"domain_scores_gemma":[0.9998022,0.00006124323,0.000039242077,0.000019510657,0.000040821884,0.000036997968],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002450695,0.00046103416,0.0003115554,0.00037398684,0.00027992288,0.00047738265,0.00074405834,0.00073485327,0.001082872],"category_scores_gemma":[0.0006545257,0.00037619183,0.000538416,0.00023986792,0.0002292141,0.0005134062,0.0003551287,0.0004449581,0.00021751042],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010030558,0.000111027526,0.03364027,0.000020886657,0.000062883584,0.00019134137,0.00007332168,0.95940375,0.0014986435,0.00044193043,0.00057084445,0.0038847753],"study_design_scores_gemma":[0.000017800154,0.000027735428,0.0115871085,0.0000031649292,0.000010990565,0.00001913468,0.0000334015,0.98781335,0.00023243949,0.00010130686,0.00014459857,0.000008909381],"about_ca_topic_score_codex":0.029657518,"about_ca_topic_score_gemma":0.02293981,"teacher_disagreement_score":0.029657518,"about_ca_system_score_codex":0.00073907553,"about_ca_system_score_gemma":0.00039222627,"threshold_uncertainty_score":0.058969796},"labels":[],"label_agreement":null},{"id":"W2139913834","doi":"10.1785/0120060113","title":"Correlation of Lg Amplitude Ratios from Peaceful Nuclear Explosions to Crustal Structure in Northern Eurasia","year":2007,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Amplitude; Geology; Tectonics; Thickening; Seismology; Sedimentary rock; Crust; Mantle (geology); Geophysics; Paleontology; Physics; Optics","score_opus":0.012941967870516755,"score_gpt":0.21208622347128117,"score_spread":0.19914425560076443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139913834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949,0.000027608472,0.000066885215,0.000008481472,7.96113e-7,9.380754e-7,0.000072853945,0.000003606967,0.00032878038],"genre_scores_gemma":[0.99968314,0.000027229336,0.000036535424,0.0000018103041,0.0000011485109,6.6949383e-7,0.00014932468,0.0000014714497,0.00009850059],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990344,0.000017001232,0.000015911037,0.00002594953,0.00001932745,0.000018412908],"domain_scores_gemma":[0.9995172,0.00007184162,0.00021966267,0.000032933705,0.00010662556,0.00005161216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019356998,0.00012886315,0.00012431506,0.00055723917,0.00009057296,0.00038175963,0.00011588553,0.00012256514,0.0007151742],"category_scores_gemma":[0.001385183,0.00010872177,0.000097996,0.00040448632,0.00019880061,0.00020425221,0.0003600466,0.0001605596,0.00011863707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000800587,0.0000068246877,0.9879061,0.000008074121,0.000029003553,0.0001379583,0.00023602098,0.00035738334,0.0038899088,0.0000329088,0.00004618971,0.007269632],"study_design_scores_gemma":[6.4053e-7,0.0000059502877,0.99964464,9.64387e-7,0.0000023973248,0.000035796096,0.000056479264,0.000105896404,0.0000985153,0.000008042758,0.000040066338,6.297323e-7],"about_ca_topic_score_codex":0.007513141,"about_ca_topic_score_gemma":0.0073681124,"teacher_disagreement_score":0.007513141,"about_ca_system_score_codex":0.00020554339,"about_ca_system_score_gemma":0.00011733169,"threshold_uncertainty_score":0.014938831},"labels":[],"label_agreement":null},{"id":"W2140282244","doi":"10.2118/110542-ms","title":"Fluid Flow in a Fractured Reservoir Using a Geomechanically-Constrained Fault Zone Damage Model for Reservoir Simulation","year":2007,"lang":"en","type":"article","venue":"SPE Annual Technical Conference and Exhibition","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ConocoPhillips (Canada)","funders":"","keywords":"Permeability (electromagnetism); Geology; Reservoir simulation; Anisotropy; Petrology; Geotechnical engineering; Seismology; Petroleum engineering","score_opus":0.049094468515453266,"score_gpt":0.297217280672682,"score_spread":0.24812281215722873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140282244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6233796,0.00036907973,0.35981867,0.00085118966,0.000113300375,0.00024200362,0.0011016227,0.001125364,0.012999099],"genre_scores_gemma":[0.9694037,0.00015007428,0.026867216,0.000058160185,0.000026789161,0.00020890468,0.00027254518,0.00006728298,0.0029453512],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998443,0.00004772799,0.000011378981,0.000028087663,0.0000417254,0.000026779948],"domain_scores_gemma":[0.99942636,0.0002866755,0.00006841778,0.00004985105,0.000095643976,0.00007309392],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003428797,0.00059554324,0.0008702563,0.00054362585,0.000639104,0.0011975927,0.0013951283,0.002142503,0.0020452547],"category_scores_gemma":[0.0013962461,0.0005582301,0.0009098311,0.0005038893,0.0009658695,0.0008125443,0.0009809639,0.00076577597,0.00022664799],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014443627,0.000019411833,0.00049257226,0.000005549424,0.0000067636097,0.00003154396,0.000012020067,0.99769455,0.00049234286,0.00065520906,0.000047035563,0.0005285424],"study_design_scores_gemma":[0.0000037336858,0.000003208372,0.00003964802,6.3340735e-7,7.6027015e-7,0.0000016839283,0.0000014883421,0.999775,0.00005380547,0.000085680906,0.000032928663,0.0000014410505],"about_ca_topic_score_codex":0.02800569,"about_ca_topic_score_gemma":0.011877921,"teacher_disagreement_score":0.02800569,"about_ca_system_score_codex":0.0014434301,"about_ca_system_score_gemma":0.0016006373,"threshold_uncertainty_score":0.05568534},"labels":[],"label_agreement":null},{"id":"W2140451609","doi":"10.1130/b26457.1","title":"Global geologic maps are tectonic speedometers--Rates of rock cycling from area-age frequencies","year":2009,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Icon; Citation; Tectonics; Geology; Geological survey; Library science; Archaeology; History; Paleontology; Computer science","score_opus":0.025915724745167477,"score_gpt":0.22927781434496314,"score_spread":0.20336208959979565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140451609","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021056997,0.013723601,0.0011785312,0.012660495,0.0014218498,0.00015898464,0.51218075,0.0025561198,0.43506274],"genre_scores_gemma":[0.11796671,0.08333494,0.0051342263,0.0015385291,0.0014189248,0.0002251782,0.46352902,0.0023058204,0.32454664],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99962735,0.000024863757,0.000029853985,0.00003687052,0.00025005994,0.000030948995],"domain_scores_gemma":[0.9992287,0.00011842933,0.00017484471,0.00006245968,0.00035252562,0.00006300697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032140684,0.0004987714,0.0005083111,0.005985781,0.00031597205,0.0020917093,0.00049965625,0.00048995425,0.13451448],"category_scores_gemma":[0.0023476912,0.0002442165,0.0002901069,0.028091071,0.00034269688,0.0024076782,0.0009628434,0.00058683363,0.057376754],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004620053,0.0000083233035,0.0077596786,0.00065664947,0.000025036832,0.00004824853,0.00023216436,0.00018652191,0.00028644747,0.0024271172,0.89806783,0.09025576],"study_design_scores_gemma":[0.000015452111,0.000015213883,0.03865925,0.00022359408,0.000024662468,0.000076042284,0.00041211664,0.00008385115,0.0002078255,0.0008167492,0.9594514,0.000013903485],"about_ca_topic_score_codex":0.027859187,"about_ca_topic_score_gemma":0.05715182,"teacher_disagreement_score":0.13451448,"about_ca_system_score_codex":0.0010253413,"about_ca_system_score_gemma":0.0013943213,"threshold_uncertainty_score":0.44999576},"labels":[],"label_agreement":null},{"id":"W2140537257","doi":"10.5194/npg-11-553-2004","title":"Earthquake statistics in a Block Slider Model and a fully dynamic Fault Model","year":2004,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"State Government of Victoria; Queensland Government; RMIT University; Australian Government; University of Queensland; Ontario Ministry of Natural Resources and Forestry","keywords":"Event (particle physics); Scaling; Induced seismicity; Block (permutation group theory); Slider; Block model; Statistics; Computer science; Geology; Statistical physics; Seismology; Mathematics; Geometry; Physics; Engineering","score_opus":0.012094708947335088,"score_gpt":0.2375878086941215,"score_spread":0.2254930997467864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140537257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98892385,0.000053118656,0.008891524,0.00010343095,0.000004244156,0.0000123620575,0.0004629097,0.00007381254,0.0014746299],"genre_scores_gemma":[0.9977319,0.00004867516,0.0010851014,0.000010715879,0.0000038799244,0.000012133469,0.00035873376,0.000018985396,0.00072977965],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999788,0.00006954429,0.000015534617,0.000047977108,0.000044236916,0.000034801284],"domain_scores_gemma":[0.9974663,0.001461995,0.0004671433,0.00022352848,0.00022188417,0.00015908483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008201591,0.000312384,0.0007997078,0.00062493165,0.00022510019,0.0007533866,0.0009556231,0.00065280526,0.002270284],"category_scores_gemma":[0.004047128,0.00027141665,0.00045859127,0.0006993195,0.00066583115,0.0014263374,0.00034028772,0.00039780955,0.00022449683],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005174363,0.000019433455,0.0032088836,0.000013928575,0.000012022089,0.000057095553,0.000030757445,0.9917971,0.00040393404,0.003537769,0.00014779902,0.00071947486],"study_design_scores_gemma":[0.0000134698375,0.000020046757,0.0011508042,0.0000013108505,0.000004698053,0.000011418628,0.000008399357,0.9975043,0.00007768777,0.001155909,0.000046204666,0.000005802583],"about_ca_topic_score_codex":0.015977068,"about_ca_topic_score_gemma":0.007583185,"teacher_disagreement_score":0.015977068,"about_ca_system_score_codex":0.0010682035,"about_ca_system_score_gemma":0.0005170861,"threshold_uncertainty_score":0.031768143},"labels":[],"label_agreement":null},{"id":"W2141628151","doi":"10.1190/segam2015-6027784.1","title":"Identifying Frac Growth in Multiple Horizons using Integrated Microseismic and Induced Seismic Monitoring Approaches","year":2015,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Apheresis Group","funders":"","keywords":"Microseism; Geology; Seismology; Computer science","score_opus":0.18009947064441129,"score_gpt":0.26509093225741365,"score_spread":0.08499146161300236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141628151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99059874,0.000079230274,0.0063644466,0.0000249527,0.000005389673,0.0000334838,0.0005201438,0.00014918458,0.0022243971],"genre_scores_gemma":[0.9928798,0.00004698676,0.006320358,0.000008217483,0.0000042755114,0.000022633572,0.00018130764,0.000010157317,0.00052629376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986243,0.0000074425393,0.000005655321,0.000042536594,0.000053651995,0.000028370468],"domain_scores_gemma":[0.9996152,0.00005136428,0.000118888034,0.000025398373,0.00013919291,0.000049926894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019455771,0.00020940077,0.0001795242,0.001189097,0.00020599503,0.00038723185,0.0003845085,0.00027069045,0.0010509118],"category_scores_gemma":[0.00042363914,0.00015867433,0.00012682455,0.0006814581,0.00015052376,0.00031656303,0.0003210479,0.00027839065,0.000163291],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036541893,0.00015040241,0.5049654,0.00021512099,0.00008928809,0.0005993419,0.0009268246,0.0147664985,0.3605185,0.00063985575,0.00062428945,0.11613892],"study_design_scores_gemma":[0.000008789637,0.00014259433,0.9381142,0.000034818135,0.000034888537,0.00018710436,0.00054831186,0.033916987,0.024830794,0.00022809491,0.0019205256,0.00003295358],"about_ca_topic_score_codex":0.009426676,"about_ca_topic_score_gemma":0.031796094,"teacher_disagreement_score":0.009426676,"about_ca_system_score_codex":0.0005037138,"about_ca_system_score_gemma":0.00034682298,"threshold_uncertainty_score":0.018743634},"labels":[],"label_agreement":null},{"id":"W2141884827","doi":"10.1785/0120020087","title":"Estimating Locations and Magnitudes of Earthquakes in Eastern North America from Modified Mercalli Intensities","year":2003,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; Boston College","keywords":"Mercalli intensity scale; Seismology; Geology; Ground motion","score_opus":0.022020715530191966,"score_gpt":0.21315862825065,"score_spread":0.19113791272045802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141884827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9862808,0.00004094631,0.0099245375,0.0000909813,0.0000025802074,0.00002808319,0.00131971,0.0002648347,0.002047554],"genre_scores_gemma":[0.98615617,0.00004467204,0.010774309,0.0000150396845,0.000004404971,0.000032946387,0.0020502396,0.000044094537,0.0008783249],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997522,0.000058570957,0.000013150788,0.00008791594,0.000058237656,0.00002992516],"domain_scores_gemma":[0.99912983,0.00020443449,0.00024652123,0.00016132217,0.00019404611,0.00006381806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050488353,0.0003702025,0.00017494573,0.00074322533,0.00025999252,0.00039722293,0.00081700896,0.00028377457,0.00093562016],"category_scores_gemma":[0.0029277047,0.00038196243,0.0002930388,0.0009497223,0.0003099337,0.00042942067,0.00059477973,0.00033216728,0.00024811437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007623887,0.00009979752,0.78272843,0.000036854406,0.00013623672,0.00010044317,0.0005640262,0.16102128,0.0029105537,0.0008991187,0.0020506815,0.049376335],"study_design_scores_gemma":[0.000027684355,0.00004839232,0.7325688,0.000012339646,0.000042091157,0.000073303825,0.00027311404,0.26253352,0.0016904413,0.0005345506,0.0021586204,0.000037172314],"about_ca_topic_score_codex":0.22583856,"about_ca_topic_score_gemma":0.35827264,"teacher_disagreement_score":0.22583856,"about_ca_system_score_codex":0.0018953661,"about_ca_system_score_gemma":0.0008333002,"threshold_uncertainty_score":0.44904804},"labels":[],"label_agreement":null},{"id":"W2142138633","doi":"10.1139/e06-057","title":"Stress in western Canada from regional moment tensor analysis","year":2007,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Thrust fault; Crust; Fault (geology); Tension (geology); Pacific Plate; Induced seismicity; Compression (physics); Subduction; Tectonics; Paleontology","score_opus":0.025433769843875777,"score_gpt":0.21828784540912874,"score_spread":0.19285407556525297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142138633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96011287,0.00093889324,0.0019660904,0.0003027764,0.000031025862,0.000052675397,0.017423471,0.00026724997,0.018904852],"genre_scores_gemma":[0.9819619,0.0009539267,0.0032011608,0.00005274395,0.00001200235,0.000024521269,0.007875786,0.00004922765,0.005868658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997975,0.0000042325423,0.000011276267,0.000035006367,0.000095392505,0.000056560133],"domain_scores_gemma":[0.9993561,0.000012990073,0.000060572856,0.000015065386,0.00048819976,0.000067135436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012005586,0.00062295265,0.000263905,0.0038333628,0.0012478681,0.0015504934,0.0005203258,0.0002382294,0.004002336],"category_scores_gemma":[0.0007952338,0.00023265065,0.00039354368,0.0063587814,0.00035956487,0.00033242072,0.0006371834,0.00027355287,0.000546188],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019017914,0.000053840165,0.7907211,0.00017522144,0.00019132903,0.00092252827,0.001983079,0.019352566,0.008734398,0.003913279,0.013392922,0.1603695],"study_design_scores_gemma":[0.000014353305,0.000017842138,0.9623962,0.00007889261,0.00007650181,0.00017684214,0.0022937339,0.018554933,0.0012005065,0.0010491664,0.014067958,0.00007300146],"about_ca_topic_score_codex":0.98944104,"about_ca_topic_score_gemma":0.99435836,"teacher_disagreement_score":0.013099196,"about_ca_system_score_codex":0.013099196,"about_ca_system_score_gemma":0.013397198,"threshold_uncertainty_score":0.09504175},"labels":[],"label_agreement":null},{"id":"W2142185003","doi":"10.1111/j.1365-246x.2006.02912.x","title":"The tsunami induced by the 2003 Zemmouri earthquake (<i>M<sub>W</sub></i>= 6.9, Algeria): modelling and results","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":119,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"University of Illinois at Urbana-Champaign","keywords":"Geology; Seismology; Balearic islands; Bathymetry; Aftershock; Mediterranean sea; Epicenter; Fault (geology); Shore; Submarine pipeline; Mediterranean climate; Tsunami earthquake; Oceanography; Geography","score_opus":0.013143103379637708,"score_gpt":0.20774732283958514,"score_spread":0.19460421945994744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142185003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9845605,0.00032217777,0.0059784185,0.00018417387,0.000039012128,0.00007512975,0.002157477,0.0003167249,0.006366388],"genre_scores_gemma":[0.9936853,0.00024248188,0.0035547074,0.000040825194,0.000016909109,0.00008906316,0.0007316933,0.000047460955,0.0015915391],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998617,0.000031742682,0.000014471411,0.000022390197,0.000024513176,0.000045178567],"domain_scores_gemma":[0.9996985,0.00013461625,0.000049291346,0.000018899098,0.000059464142,0.000039165476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030118666,0.0010462647,0.0007729885,0.0006560576,0.000529287,0.0011442471,0.0013208054,0.0020283966,0.0028763423],"category_scores_gemma":[0.0006990873,0.00040258057,0.0010323062,0.00074121973,0.0006145337,0.000395853,0.0005498208,0.00065160193,0.00039287552],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043245287,0.000046491004,0.004984307,0.000053677697,0.000028470244,0.00016352211,0.00003822488,0.9918612,0.0011954518,0.00026784974,0.00014758208,0.0011699296],"study_design_scores_gemma":[0.000041537136,0.000038728685,0.0038997764,0.0000128150195,0.000030330099,0.000037964,0.00005376925,0.99441373,0.0009089745,0.00015580327,0.0003897867,0.000016865053],"about_ca_topic_score_codex":0.08585679,"about_ca_topic_score_gemma":0.030240254,"teacher_disagreement_score":0.08585679,"about_ca_system_score_codex":0.0010263787,"about_ca_system_score_gemma":0.00083911885,"threshold_uncertainty_score":0.17071408},"labels":[],"label_agreement":null},{"id":"W214230181","doi":"10.1023/a:1014249814998","title":"Source parameters of four strong earthquakes in Bulgaria and Portugal at the beginning of the 20th century","year":2002,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Seismometer; Geology; Seismic moment; Moment magnitude scale; Magnitude (astronomy); Fault (geology); Mathematics; Physics","score_opus":0.02486526112375639,"score_gpt":0.2006049212035192,"score_spread":0.1757396600797628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W214230181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99668044,0.00035834307,0.000106945925,0.000060666844,0.000014002442,0.0000035769467,0.0010086995,0.000013063692,0.0017541548],"genre_scores_gemma":[0.9984295,0.0001239571,0.000052904747,0.00000479944,0.000006918084,0.0000026747982,0.0010731102,0.0000083070145,0.0002977472],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988055,0.000012482738,0.000016974338,0.00002444398,0.000017657268,0.00004798851],"domain_scores_gemma":[0.99959844,0.000114044204,0.00010779956,0.000032089363,0.00009685427,0.000050727223],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032129226,0.00027509598,0.00035632207,0.0018151064,0.00047558837,0.000980097,0.0003420082,0.0006466472,0.0015019057],"category_scores_gemma":[0.0013863392,0.00023008623,0.00031638352,0.0019943472,0.000445895,0.00037642126,0.0007918193,0.00031310052,0.00027581924],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013119816,0.00010095731,0.91639364,0.00027946144,0.00026454436,0.002198389,0.0055557247,0.018421248,0.005302581,0.0037475668,0.0021943036,0.044229515],"study_design_scores_gemma":[0.000020851012,0.000014063779,0.99607915,0.000026772821,0.000034865567,0.00015433943,0.0010031385,0.0011249881,0.00036473104,0.00015465579,0.0010110295,0.000011312392],"about_ca_topic_score_codex":0.050489444,"about_ca_topic_score_gemma":0.04869373,"teacher_disagreement_score":0.050489444,"about_ca_system_score_codex":0.0012109211,"about_ca_system_score_gemma":0.00048068905,"threshold_uncertainty_score":0.10039115},"labels":[],"label_agreement":null},{"id":"W2143186336","doi":"10.1111/j.1365-246x.2004.02414.x","title":"Lithospheric imaging via teleseismic scattering tomography","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Seismology; Geology; Coda; Scattering; Lithosphere; Tomography; Lineation; Seismic tomography; Induced seismicity; Seismogram; Tectonics; Geodesy; Geophysics; Mantle (geology); Physics; Optics","score_opus":0.006786795364594491,"score_gpt":0.21073887011513825,"score_spread":0.20395207475054378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143186336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8482169,0.00037087325,0.13821718,0.00017650088,0.000018567784,0.00004452876,0.00093774043,0.00062968594,0.011388056],"genre_scores_gemma":[0.9585311,0.00026473432,0.03980316,0.000010280079,0.000018416029,0.00001178001,0.0005162084,0.00002662653,0.00081772055],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999168,0.000015463169,0.0000036649205,0.000018665862,0.000033086864,0.000012188136],"domain_scores_gemma":[0.99991155,0.000015411517,0.000027177724,0.000014992643,0.000022560173,0.000008392756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013043729,0.00040106848,0.00012305922,0.0008652687,0.00015035794,0.0004521779,0.00022794136,0.00016112598,0.00080210995],"category_scores_gemma":[0.00048356687,0.0001831052,0.00017756235,0.0012072398,0.0002604031,0.00038134356,0.00043080217,0.00014768743,0.00017249704],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005027965,0.000116492076,0.087465025,0.00017155247,0.0001358389,0.00069767516,0.0005733957,0.3101049,0.33218646,0.011357227,0.0023424102,0.25434616],"study_design_scores_gemma":[0.00009473495,0.00011069546,0.08741906,0.000031052576,0.00006375489,0.00049965084,0.00027103466,0.87411135,0.028356021,0.005076584,0.0039181,0.00004792046],"about_ca_topic_score_codex":0.011266212,"about_ca_topic_score_gemma":0.016693357,"teacher_disagreement_score":0.011266212,"about_ca_system_score_codex":0.00031781226,"about_ca_system_score_gemma":0.00044364773,"threshold_uncertainty_score":0.022401273},"labels":[],"label_agreement":null},{"id":"W2143762148","doi":"10.1111/j.1365-246x.2012.05454.x","title":"Lithosphere thickness and mantle viscosity inverted from GPS-derived deformation rates in Fennoscandia","year":2012,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Geology; Mantle (geology); Geodesy; Global Positioning System; Geophysics; Deformation (meteorology); Seismology; Geodynamics; Post-glacial rebound; Tectonics; Geomorphology","score_opus":0.014878817288404539,"score_gpt":0.23330692425767902,"score_spread":0.21842810696927448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143762148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903476,0.000034089062,0.00007170984,0.000011031902,0.0000011612944,0.000001943823,0.00035702263,0.000010458471,0.0004778322],"genre_scores_gemma":[0.9984968,0.00003735296,0.00029785023,0.000006668452,6.635834e-7,0.000003614017,0.0009807526,0.000006152905,0.00017013044],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99977607,0.000019882338,0.000013632598,0.00009531616,0.000028444683,0.000066718305],"domain_scores_gemma":[0.9996886,0.00004916072,0.000048124246,0.000037384852,0.00011840658,0.000058218513],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003917552,0.000570621,0.00038836995,0.0015247246,0.0009314491,0.0011022777,0.0009023671,0.00049909006,0.0011089657],"category_scores_gemma":[0.0012932362,0.00037187844,0.00041549813,0.0021199973,0.00055561657,0.00036232764,0.00053553545,0.00040696398,0.00013770373],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043101725,0.00009372884,0.9126003,0.000050256687,0.00019635461,0.00042576442,0.0008528182,0.057784528,0.0071920757,0.0004292478,0.0005433787,0.019400597],"study_design_scores_gemma":[0.000016714612,0.000017033717,0.971034,0.000018362347,0.000037685284,0.00003404962,0.00046455036,0.027069045,0.00081857137,0.00008187529,0.00038454332,0.000023685514],"about_ca_topic_score_codex":0.76597714,"about_ca_topic_score_gemma":0.7798445,"teacher_disagreement_score":0.76597714,"about_ca_system_score_codex":0.0037865276,"about_ca_system_score_gemma":0.0026374136,"threshold_uncertainty_score":0.47080207},"labels":[],"label_agreement":null},{"id":"W2143803593","doi":"10.1785/0120060176","title":"The October 2005 Georgian Bay, Canada, Earthquake Sequence: Mafic Dykes and Their Role in the Mechanical Heterogeneity of Precambrian Crust","year":2007,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Mafic; Precambrian; Geology; Bay; Crust; Sequence (biology); Seismology; Geochemistry; Georgian; Oceanography","score_opus":0.013433260834328312,"score_gpt":0.20848303500221482,"score_spread":0.19504977416788652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143803593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9799436,0.00054103293,0.00019861793,0.00026472,0.0000128862175,0.00003319438,0.01354323,0.000052314757,0.0054106056],"genre_scores_gemma":[0.9863301,0.00038104018,0.00039043842,0.000057213456,0.000007671613,0.000012805029,0.010511395,0.000015805874,0.0022935243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998746,0.0000046183527,0.000005347133,0.000028068858,0.000046578363,0.00004077838],"domain_scores_gemma":[0.9995995,0.00001363941,0.00006700376,0.000019214667,0.00019417048,0.0001066196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015124516,0.00041024367,0.00026556052,0.0014786075,0.0013366198,0.00078007864,0.00048645635,0.00026635293,0.001506011],"category_scores_gemma":[0.0007720768,0.00018959606,0.00012448872,0.002967203,0.0005631303,0.00017054527,0.00065774703,0.00028028365,0.0002788752],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004209738,0.000044981785,0.9209338,0.00026359298,0.00011729798,0.0010229902,0.0040670866,0.0029332861,0.012418278,0.0010822389,0.020234477,0.036461],"study_design_scores_gemma":[0.0000047117937,0.0000056528315,0.99583364,0.000015069243,0.000005847983,0.00003276465,0.00037427415,0.00038734695,0.00013102885,0.000025197805,0.0031774219,0.000006953201],"about_ca_topic_score_codex":0.98024637,"about_ca_topic_score_gemma":0.9956664,"teacher_disagreement_score":0.019753635,"about_ca_system_score_codex":0.008358608,"about_ca_system_score_gemma":0.008808611,"threshold_uncertainty_score":0.060646236},"labels":[],"label_agreement":null},{"id":"W2144064310","doi":"10.1144/jgs2012-090","title":"The gigantic Seymareh (Saidmarreh) rock avalanche, Zagros Fold–Thrust Belt, Iran","year":2013,"lang":"en","type":"article","venue":"Journal of the Geological Society","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; Simon Fraser University","funders":"","keywords":"Geology; Fold (higher-order function); Fold and thrust belt; Seismology; Volcanic rock; Geochemistry; Paleontology; Geomorphology; Tectonics; Volcano; Foreland basin","score_opus":0.017356569288032368,"score_gpt":0.201769921646573,"score_spread":0.18441335235854064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144064310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944395,0.0004289777,0.00026160336,0.00012383034,0.000029640307,0.00005300379,0.00033652678,0.000028937819,0.0042979633],"genre_scores_gemma":[0.99681205,0.0003545234,0.00040777013,0.000043062882,0.000019518293,0.0000104910705,0.0007007657,0.000003348913,0.0016484715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998907,0.0000058517394,0.000009424772,0.00002933503,0.000034015666,0.000030674197],"domain_scores_gemma":[0.99994814,0.000003671637,0.000021249914,0.000005084488,0.00001118077,0.000010699792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019837194,0.00037656608,0.00018567807,0.0007781368,0.00057325483,0.0005114546,0.000248492,0.00024385145,0.0019191754],"category_scores_gemma":[0.00015425008,0.00017092752,0.00019905553,0.00057893374,0.00038023473,0.0002096311,0.00034769168,0.00022915336,0.00047648634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032232894,0.0003017858,0.8662024,0.00022479022,0.00008673264,0.002746417,0.0019205983,0.0010762638,0.012834793,0.00095256855,0.0032693015,0.110062025],"study_design_scores_gemma":[0.000025909274,0.00008013176,0.9947247,0.000019729017,0.000011697218,0.0010219571,0.0006929349,0.00027254035,0.00029064275,0.00009208704,0.002762889,0.0000046746304],"about_ca_topic_score_codex":0.0164871,"about_ca_topic_score_gemma":0.028589044,"teacher_disagreement_score":0.0164871,"about_ca_system_score_codex":0.00057659636,"about_ca_system_score_gemma":0.0007537381,"threshold_uncertainty_score":0.032782257},"labels":[],"label_agreement":null},{"id":"W2145205310","doi":"10.1029/2011jb008556","title":"Influence of dilatancy on the frictional constitutive behavior of a saturated fault zone under a variety of drainage conditions","year":2011,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Dilatant; Shearing (physics); Geology; Geotechnical engineering; Shear (geology); Nucleation; Slip (aerodynamics); Drainage; Fault gouge; Hardening (computing); Constitutive equation; Mechanics; Fault (geology); Materials science; Petrology; Composite material; Seismology; Thermodynamics","score_opus":0.05800623490456754,"score_gpt":0.3041343781112954,"score_spread":0.24612814320672785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145205310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990201,0.000028087992,0.00038645088,0.00002451797,0.0000011541263,0.000003496162,0.000049110095,0.000013506552,0.00047368236],"genre_scores_gemma":[0.99976903,0.000018615765,0.00013803219,0.000003801205,3.322983e-7,0.0000030675658,0.000021802738,0.000002853832,0.000042457483],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99989223,0.000023164252,0.00001445788,0.000018498858,0.00001979334,0.00003192517],"domain_scores_gemma":[0.99946576,0.00029303454,0.00010649955,0.00003385932,0.000042440635,0.00005846233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021839984,0.00023374638,0.00034747034,0.0005521457,0.00030717236,0.00058772106,0.00028113497,0.00038334515,0.0007040654],"category_scores_gemma":[0.0022401188,0.0001812604,0.00025661616,0.0003243777,0.00068663363,0.00036701758,0.0004565785,0.00028004166,0.000044069468],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006570976,0.00021297243,0.06799315,0.00017311613,0.00008298254,0.0009666307,0.00046660053,0.7260404,0.19469535,0.0021146273,0.00019299943,0.006404039],"study_design_scores_gemma":[0.000117125426,0.0002951207,0.040139355,0.000023312807,0.00004239761,0.00019856823,0.00037035352,0.9032525,0.054305043,0.00078032736,0.0004232169,0.00005268413],"about_ca_topic_score_codex":0.007382418,"about_ca_topic_score_gemma":0.006075244,"teacher_disagreement_score":0.007382418,"about_ca_system_score_codex":0.0008031647,"about_ca_system_score_gemma":0.00034905388,"threshold_uncertainty_score":0.0146788955},"labels":[],"label_agreement":null},{"id":"W2145729420","doi":"10.1046/j.1365-246x.2003.02043.x","title":"Neighbourhood inversion of teleseismic<i>Ps</i>conversions for anisotropy and layer dip","year":2003,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Winnipeg; University of Manitoba; Geological Survey of Canada","funders":"","keywords":"Geology; Inversion (geology); Azimuth; Receiver function; Anisotropy; Seismology; Crust; Seismogram; Prestack; Lithosphere; Geophysics; Geometry; Tectonics; Optics; Physics","score_opus":0.016884356051563017,"score_gpt":0.23252723972332598,"score_spread":0.21564288367176296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145729420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7305939,0.000035055407,0.265473,0.000037168644,0.000011809315,0.000031304895,0.00026484428,0.0006347252,0.0029180849],"genre_scores_gemma":[0.948919,0.0000154435,0.049900945,0.0000051414727,0.0000045409915,0.000024032728,0.0003140295,0.00006753658,0.0007493802],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999145,0.000019682515,0.0000064832734,0.000015672154,0.000028891636,0.000014793364],"domain_scores_gemma":[0.9996377,0.00018123431,0.00003658453,0.00006107014,0.00005998228,0.00002348006],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034275977,0.00021461397,0.00022012877,0.0004903481,0.00020879807,0.0003101415,0.00046401174,0.00020389534,0.0013154347],"category_scores_gemma":[0.0025522315,0.00020291244,0.00023757094,0.00042221375,0.00015895432,0.00021671591,0.00034620886,0.0002509175,0.00023718075],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022496605,0.00007840154,0.017488163,0.000046489848,0.000036388476,0.00023091299,0.0001968047,0.8186004,0.044013295,0.008575059,0.0007732242,0.10973577],"study_design_scores_gemma":[0.000017300888,0.000022117985,0.005401625,0.0000030533342,0.0000055691667,0.000031360385,0.000021155809,0.983537,0.009015118,0.0014192149,0.00051641045,0.000009960433],"about_ca_topic_score_codex":0.011024353,"about_ca_topic_score_gemma":0.019384965,"teacher_disagreement_score":0.011024353,"about_ca_system_score_codex":0.00039580584,"about_ca_system_score_gemma":0.0006342802,"threshold_uncertainty_score":0.021920383},"labels":[],"label_agreement":null},{"id":"W2145996801","doi":"10.1093/gji/ggt498","title":"Scaling relations and spectral characteristics of tensile microseisms: evidence for opening/closing cracks during hydraulic fracturing","year":2014,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Calgary","funders":"","keywords":"Microseism; Geology; Scaling; Ultimate tensile strength; Hydraulic fracturing; Seismology; Attenuation; Shear (geology); Seismic moment; Fracture (geology); Closing (real estate); Geotechnical engineering; Materials science; Physics; Geometry; Composite material; Mathematics; Petrology; Optics; Fault (geology)","score_opus":0.023219584048251037,"score_gpt":0.26278335645651496,"score_spread":0.23956377240826393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145996801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980804,0.000034091394,0.0012797429,0.000010906691,7.3988815e-7,0.000010015379,0.00006923423,0.000019633262,0.00049526204],"genre_scores_gemma":[0.9994388,0.000013216195,0.0004445183,0.0000013604398,0.0000012462102,0.000003838938,0.00005446419,0.0000030729993,0.00003960435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989367,0.000011773722,0.000011022943,0.000028264574,0.00003859332,0.000016729893],"domain_scores_gemma":[0.9989766,0.0002887917,0.00038014862,0.0000610414,0.00021845094,0.0000750802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023992258,0.0001888556,0.0001066834,0.0012332991,0.00022491612,0.00022353034,0.00023700623,0.00027737726,0.00073423237],"category_scores_gemma":[0.0018370522,0.00018643186,0.00015696888,0.00053916755,0.0005050595,0.00031888727,0.00023850214,0.0001633952,0.00013013477],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026153796,0.00009133763,0.76373047,0.00009852894,0.000042480315,0.0004680881,0.0016107641,0.004732631,0.1958525,0.00048303683,0.00013123211,0.032497417],"study_design_scores_gemma":[0.000002860987,0.00003461856,0.9924786,0.000004454853,0.000005170371,0.00013111478,0.00017184473,0.004923925,0.002062185,0.000116321105,0.00006141025,0.0000075499415],"about_ca_topic_score_codex":0.010275617,"about_ca_topic_score_gemma":0.013365471,"teacher_disagreement_score":0.010275617,"about_ca_system_score_codex":0.0003524781,"about_ca_system_score_gemma":0.00012834687,"threshold_uncertainty_score":0.020431578},"labels":[],"label_agreement":null},{"id":"W2146279888","doi":"10.1029/2005jb003987","title":"Bending‐like behavior of thin wedge‐shaped elastic fault blocks","year":2006,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Wedge (geometry); Geology; Accretionary wedge; Traction (geology); Bent molecular geometry; Compression (physics); Tension (geology); Geometry; Seismology; Tectonics; Subduction; Materials science","score_opus":0.031072580155860872,"score_gpt":0.2981361399929205,"score_spread":0.2670635598370596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146279888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9360687,0.00010337655,0.056157798,0.00011637247,0.000011944779,0.000012937279,0.000046840196,0.00006808446,0.007413943],"genre_scores_gemma":[0.99611664,0.000039620656,0.0026846826,0.000011422791,0.0000032178866,0.000004847131,0.000023073308,0.000008443121,0.0011080459],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999728,0.0000048767947,0.0000022202864,0.0000046885725,0.0000078734465,0.00000749579],"domain_scores_gemma":[0.9998776,0.000025112557,0.000044620196,0.000012022908,0.000020738706,0.000019922205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008610355,0.00020208088,0.00014136457,0.00023237267,0.00017162897,0.00028901699,0.00030655565,0.00035594878,0.0011105156],"category_scores_gemma":[0.0006175493,0.00017269963,0.00016859583,0.000099880584,0.00044240546,0.00024466164,0.00027652754,0.00020155727,0.00013643932],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001286374,0.000058266,0.013381725,0.00008663636,0.00004013208,0.0019613376,0.00047478903,0.76566154,0.15315343,0.048293907,0.00063845015,0.016121153],"study_design_scores_gemma":[0.000016073553,0.000039361792,0.0044128844,0.0000107360065,0.0000062466597,0.00027143426,0.000093362505,0.9836871,0.0049123806,0.006123844,0.00041293845,0.000013598181],"about_ca_topic_score_codex":0.0014683937,"about_ca_topic_score_gemma":0.001180937,"teacher_disagreement_score":0.0014683937,"about_ca_system_score_codex":0.00020566513,"about_ca_system_score_gemma":0.00015677234,"threshold_uncertainty_score":0.003715098},"labels":[],"label_agreement":null},{"id":"W2146315266","doi":"10.1016/j.epsl.2008.03.056","title":"Dynamic topography and long-term sea-level variations: There is no such thing as a stable continental platform","year":2008,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":340,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Canadian Institute for Advanced Research; National Science Foundation","keywords":"Geology; Ocean surface topography; Continental margin; Passive margin; Subduction; Paleontology; Mantle (geology); Sea level; Oceanic basin; Diachronous; Continental shelf; Tectonics; Oceanography; Rift","score_opus":0.016500407603996348,"score_gpt":0.20394697113856197,"score_spread":0.18744656353456562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146315266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896561,0.0007709282,0.0010642066,0.0034204237,0.00008654196,0.0000025315237,0.00010239857,0.000008827834,0.0048880912],"genre_scores_gemma":[0.9987243,0.0002346562,0.00015703477,0.00014859092,0.00003337334,5.824678e-7,0.000044116627,0.000007648006,0.0006496984],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999056,0.0000143112065,0.0000048729516,0.000031565094,0.000015309308,0.000028348162],"domain_scores_gemma":[0.99894387,0.00019049807,0.00030660428,0.00010836959,0.00015943432,0.00029120655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039292796,0.00019895098,0.00037859657,0.00037128598,0.0006663212,0.002573791,0.0005458458,0.0014355554,0.0034288021],"category_scores_gemma":[0.0026609444,0.00028130604,0.00028965698,0.0010095321,0.0024184976,0.0029885932,0.00082824443,0.0008638333,0.00047736787],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008888416,0.00018576202,0.88314885,0.00009938129,0.00045464654,0.0012454095,0.0012943057,0.008481147,0.008856545,0.03960151,0.004654888,0.051088702],"study_design_scores_gemma":[0.000036113634,0.00020397696,0.9431203,0.000035571822,0.00021320126,0.0005425398,0.0039184797,0.006323361,0.00048762056,0.04177295,0.0032841852,0.0000616545],"about_ca_topic_score_codex":0.013975658,"about_ca_topic_score_gemma":0.022107515,"teacher_disagreement_score":0.013975658,"about_ca_system_score_codex":0.00051619724,"about_ca_system_score_gemma":0.00040783567,"threshold_uncertainty_score":0.02778858},"labels":[],"label_agreement":null},{"id":"W2146322720","doi":"10.1144/gsl.sp.2005.243.01.07","title":"Crack-seal patterns: records of uncorrelated stress release variations in crustal rocks","year":2005,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seal (emblem); Crust; Quartz; Stress (linguistics); Deformation (meteorology); Seismology; Mineralogy; Geochemistry; Archaeology","score_opus":0.016987711809255596,"score_gpt":0.22857209846526855,"score_spread":0.21158438665601295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146322720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999241,0.0000365348,0.00024510638,0.0000027070248,3.765372e-7,0.000002373064,0.00026479707,0.0000122144575,0.00019492129],"genre_scores_gemma":[0.99951696,0.000013703379,0.00012536091,6.4332284e-7,0.0000010206135,0.0000014350154,0.00029486392,0.0000030350927,0.000042884712],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998641,0.000016211025,0.000016660202,0.00004235318,0.00003996941,0.000020659621],"domain_scores_gemma":[0.9989078,0.00018388972,0.00039448115,0.00014381032,0.00026199635,0.00010806206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002111577,0.0001313037,0.0001641205,0.0014711693,0.00019012306,0.00028300076,0.00017865383,0.00017408362,0.0005985661],"category_scores_gemma":[0.0013403925,0.0001395751,0.00012559834,0.0011117597,0.0003196744,0.00025286208,0.00033739753,0.00010584802,0.00015085367],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018244739,0.000026422718,0.94478244,0.000046961446,0.00007338616,0.00018442945,0.00045097418,0.0013457478,0.036405824,0.00015824765,0.0001415354,0.016201654],"study_design_scores_gemma":[0.0000017603178,0.00002126945,0.99782145,0.000001819983,0.0000062087943,0.00011778665,0.000038429247,0.0009924134,0.0008456338,0.000026862783,0.00012255796,0.0000039314896],"about_ca_topic_score_codex":0.0029106971,"about_ca_topic_score_gemma":0.0036868632,"teacher_disagreement_score":0.0029106971,"about_ca_system_score_codex":0.00016386343,"about_ca_system_score_gemma":0.00007375742,"threshold_uncertainty_score":0.005787492},"labels":[],"label_agreement":null},{"id":"W2146909102","doi":"10.1029/2008jb006046","title":"Northern Cascadia episodic tremor and slip: A decade of tremor observations from 1997 to 2007","year":2009,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":116,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Episodic tremor and slip; Seismology; Induced seismicity; Slip (aerodynamics); Subduction; Global Positioning System; Slow earthquake; Geodesy; Tectonics; Physics; Interplate earthquake; Telecommunications","score_opus":0.05061274467046597,"score_gpt":0.30322189457226534,"score_spread":0.2526091499017994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146909102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9796474,0.0010820675,0.0002442926,0.00014028355,0.000019274656,0.000025269794,0.014766776,0.00009094944,0.0039836853],"genre_scores_gemma":[0.9663036,0.0013955721,0.00040870643,0.000068832276,0.000053642478,0.00004062952,0.030134946,0.000024279141,0.0015698322],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99955636,0.000023651393,0.000055255878,0.00014033509,0.00015356044,0.00007070381],"domain_scores_gemma":[0.9983589,0.00011347571,0.0005451626,0.00013694522,0.00060388347,0.00024152208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004951089,0.00054065615,0.00036584787,0.002894538,0.0005612936,0.00074019236,0.00039997074,0.00033714512,0.000991145],"category_scores_gemma":[0.0011741974,0.00024007614,0.00031250736,0.0038969785,0.00040257676,0.000405452,0.00092811557,0.00028778682,0.00050738064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084707775,0.00003549604,0.97506624,0.00020228382,0.00012860086,0.0005340117,0.0014262458,0.0006101383,0.0013169212,0.000052162268,0.0045205257,0.016022567],"study_design_scores_gemma":[0.00000180283,0.0000080985,0.9972216,0.000019660964,0.000016200822,0.00006860498,0.00027249844,0.00015333404,0.000083487204,0.00000536183,0.002145205,0.000004232021],"about_ca_topic_score_codex":0.17360364,"about_ca_topic_score_gemma":0.31640598,"teacher_disagreement_score":0.17360364,"about_ca_system_score_codex":0.0015233526,"about_ca_system_score_gemma":0.0013845111,"threshold_uncertainty_score":0.34518635},"labels":[],"label_agreement":null},{"id":"W2147155627","doi":"10.1785/gssrl.79.1.119","title":"A Very Close Look at a Moderate Earthquake near Sudbury, Ontario","year":2008,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Library science; Geological survey; History; Geography; Geology","score_opus":0.0861486787866267,"score_gpt":0.28357230827556135,"score_spread":0.19742362948893466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147155627","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.025269516,0.023658015,0.000606685,0.027490975,0.008755836,0.00039586474,0.15886728,0.0009237723,0.75403196],"genre_scores_gemma":[0.055895384,0.015475567,0.0009972081,0.004202541,0.0018503227,0.00012303528,0.057526454,0.00062747544,0.863302],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99953306,0.000017080823,0.000017486784,0.000050997518,0.00023507993,0.00014631274],"domain_scores_gemma":[0.99894506,0.000046201116,0.000075565134,0.000051682626,0.00051064824,0.00037082186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030881847,0.0007076818,0.000662336,0.0025970356,0.006236198,0.0030536444,0.0009487985,0.0015087919,0.15913323],"category_scores_gemma":[0.0015475146,0.00029849613,0.00050950627,0.0053941524,0.00055148086,0.0013140792,0.0023124712,0.0011247911,0.029319715],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008168395,0.000012022834,0.004903955,0.00051636534,0.000018592866,0.0011618902,0.0011714001,0.0000679157,0.00054400874,0.0005921448,0.96683025,0.02409964],"study_design_scores_gemma":[0.000010472534,0.000011054186,0.026014589,0.00026306653,0.000011156398,0.00013566231,0.0016256368,0.00002371006,0.00008277447,0.000085565305,0.97171956,0.000016825605],"about_ca_topic_score_codex":0.8107959,"about_ca_topic_score_gemma":0.96998143,"teacher_disagreement_score":0.1892041,"about_ca_system_score_codex":0.0073216385,"about_ca_system_score_gemma":0.010695639,"threshold_uncertainty_score":0.53235364},"labels":[],"label_agreement":null},{"id":"W2147666948","doi":"10.1038/ncomms4084","title":"Helium anomalies suggest a fluid pathway from mantle to trench during the 2011 Tohoku-Oki earthquake","year":2014,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Trench; Seismology; Seafloor spreading; Mantle (geology); Plate tectonics; Subduction; Fluid pressure; Helium; Pacific Plate; Geophysics; North American Plate; Hotspot (geology); Tectonics; Mechanics; Materials science; Layer (electronics)","score_opus":0.01328505971833316,"score_gpt":0.22445623768791378,"score_spread":0.21117117796958063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147666948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992207,0.000022441405,0.000042252806,0.000071477094,0.0000040901587,0.0000018320536,0.00009078661,0.000004760658,0.0005416163],"genre_scores_gemma":[0.9995468,0.000027298422,0.00005341979,0.000016510641,0.0000032638281,0.0000019294641,0.00009673268,0.0000025626587,0.00025147872],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999472,0.0000027805193,0.000004896877,0.000014557935,0.00000616149,0.00002435985],"domain_scores_gemma":[0.99983835,0.000019147104,0.000050734412,0.000011890305,0.000043656037,0.00003623834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010634933,0.00022951984,0.00022329434,0.00073020475,0.00095292,0.0006023969,0.00030283566,0.0006545014,0.0013123313],"category_scores_gemma":[0.0003548622,0.000304,0.00015420566,0.0006253818,0.00052351214,0.0007026614,0.0009077494,0.00043327038,0.000122061756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057856995,0.00006794643,0.89573306,0.00009044817,0.00010412695,0.0015150809,0.0029047276,0.0016259019,0.08890817,0.0005560404,0.00046156402,0.0074544176],"study_design_scores_gemma":[0.0000059907075,0.000021443955,0.99606246,0.000005933185,0.000021760097,0.000057675705,0.0012709583,0.00091959984,0.0011938534,0.000073444535,0.00035783614,0.000008995733],"about_ca_topic_score_codex":0.031451453,"about_ca_topic_score_gemma":0.09314451,"teacher_disagreement_score":0.031451453,"about_ca_system_score_codex":0.0005246971,"about_ca_system_score_gemma":0.00057614065,"threshold_uncertainty_score":0.062536776},"labels":[],"label_agreement":null},{"id":"W2147846751","doi":"10.1002/2014jb010940","title":"Nontrivial decay of aftershock density with distance in Southern California","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Alberta Innovates","keywords":"Aftershock; Exponent; Seismology; Magnitude (astronomy); Geology; Crust; Shock (circulatory); Scale (ratio); Power law; Anisotropy; Geodesy; Physics; Astrophysics; Geophysics; Mathematics; Statistics; Optics","score_opus":0.02044589728389803,"score_gpt":0.27411485476135183,"score_spread":0.2536689574774538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147846751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983962,0.0000834024,0.00029442323,0.00002423605,0.0000015564525,0.000004370394,0.00048157145,0.000024076813,0.0006902114],"genre_scores_gemma":[0.998985,0.000041844363,0.00011870538,0.0000024378628,0.0000019193762,0.0000020626906,0.00065382104,0.0000021999672,0.00019195465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997979,0.00001960153,0.000012828568,0.00008034267,0.000053331998,0.000036099245],"domain_scores_gemma":[0.99808794,0.00035007202,0.00057327957,0.0002507104,0.00056909554,0.00016894154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044452611,0.00018532397,0.000316576,0.0015132913,0.00034095536,0.00097102544,0.00043810884,0.00029185574,0.0010804608],"category_scores_gemma":[0.003231566,0.00021130814,0.000116091906,0.001890511,0.00034621943,0.0005652999,0.0004726307,0.0002618251,0.00010646145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014079551,0.000054208354,0.9424104,0.00007184133,0.00010024617,0.00025988588,0.00051483477,0.031965233,0.0020121718,0.0017885288,0.0014690887,0.019212758],"study_design_scores_gemma":[0.000019684696,0.000034910947,0.9665864,0.0000161628,0.000021929773,0.000073920644,0.000280086,0.030190257,0.00049551995,0.0006318696,0.0016289272,0.000020258294],"about_ca_topic_score_codex":0.107912116,"about_ca_topic_score_gemma":0.10472821,"teacher_disagreement_score":0.107912116,"about_ca_system_score_codex":0.0011689311,"about_ca_system_score_gemma":0.0004414418,"threshold_uncertainty_score":0.21456802},"labels":[],"label_agreement":null},{"id":"W2148702592","doi":"10.1002/2014gl062401","title":"Crustal thickness variations and isostatic disequilibrium across the North Anatolian Fault, western Turkey","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Environment Research Council; Sight Research UK","keywords":"North Anatolian Fault; Geology; Lithosphere; Seismology; Crust; Mantle (geology); Fault (geology); Sedimentary rock; Subduction; Tectonics; Petrology; Geophysics; Paleontology","score_opus":0.054521033228973795,"score_gpt":0.3189080846461486,"score_spread":0.26438705141717483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148702592","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995914,0.00003898302,0.000045863057,0.000005314439,8.0893403e-7,8.716544e-7,0.0001004941,0.000003386033,0.00021291875],"genre_scores_gemma":[0.99970007,0.000021326205,0.000059274786,0.0000014914203,6.6134623e-7,0.0000011017063,0.0001494205,0.0000010858398,0.000065521344],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999144,0.0000120783425,0.0000121723315,0.000032884796,0.000013454052,0.000014967527],"domain_scores_gemma":[0.99975353,0.00003234538,0.000099355144,0.000022707605,0.00007188479,0.000020179736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016176993,0.00028135887,0.00019476206,0.0010665319,0.00020236163,0.0004225665,0.00021385062,0.00018757355,0.00056164304],"category_scores_gemma":[0.00039075006,0.00013356819,0.00010062175,0.0008706229,0.00024534584,0.00024244172,0.00028290367,0.00009814572,0.000121531346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017246595,0.000036417132,0.9737055,0.000024170038,0.00009427706,0.0004166311,0.0004980626,0.0026126234,0.008769793,0.00008603152,0.00013449402,0.013449518],"study_design_scores_gemma":[0.0000028014106,0.000008950282,0.99853396,0.0000030720887,0.000008349616,0.00006115492,0.00017585821,0.0008866862,0.00020806248,0.000015453761,0.000093611256,0.0000020539896],"about_ca_topic_score_codex":0.021563264,"about_ca_topic_score_gemma":0.027542438,"teacher_disagreement_score":0.021563264,"about_ca_system_score_codex":0.00048305202,"about_ca_system_score_gemma":0.00020153038,"threshold_uncertainty_score":0.04287553},"labels":[],"label_agreement":null},{"id":"W2148773537","doi":"10.1002/2015jb012161","title":"Precise relative locations for earthquakes in the northeast Pacific region","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Boettcher Foundation; Los Alamos National Laboratory; National Nuclear Security Administration; U.S. Geological Survey; U.S. Department of Energy; Defense Threat Reduction Agency; National Science Foundation","keywords":"Seismology; Induced seismicity; Geology; Transform fault; Submarine pipeline; Pacific Plate; Fault (geology); Rayleigh wave; Seismogram; Fracture zone; Slip (aerodynamics); Magnitude (astronomy); Subduction; Tectonics; Surface wave; Oceanography","score_opus":0.12257543922742516,"score_gpt":0.3513815990130373,"score_spread":0.22880615978561214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148773537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99730706,0.0000786008,0.0011310143,0.00001617984,0.0000032119522,0.0000043524487,0.0004918705,0.00005212039,0.00091561145],"genre_scores_gemma":[0.9983354,0.00003172695,0.0010781044,0.0000017905113,0.0000015212677,0.0000027373133,0.00040432962,0.000004830836,0.00013964172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999442,0.0000058199057,0.000003720323,0.000021471753,0.000016888045,0.000007838197],"domain_scores_gemma":[0.999752,0.000051538056,0.00006726927,0.000022512948,0.00008191063,0.000024855191],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020139648,0.00016002556,0.00010411132,0.0006413052,0.00022608662,0.00034038248,0.0002190973,0.00014512826,0.00055552466],"category_scores_gemma":[0.00085615437,0.00011569517,0.00010212149,0.0006575794,0.0001719684,0.00024033815,0.00022219591,0.00015901028,0.00007077358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018777692,0.000036598685,0.884745,0.00009144399,0.00010014253,0.00023339594,0.00042944506,0.054459777,0.019971816,0.00062200555,0.0006665062,0.038456168],"study_design_scores_gemma":[0.000013859912,0.000024866249,0.9466385,0.000016180298,0.000024702735,0.00006370326,0.0001675065,0.04929319,0.002745785,0.000080498445,0.0009142022,0.000017031065],"about_ca_topic_score_codex":0.103427984,"about_ca_topic_score_gemma":0.14805862,"teacher_disagreement_score":0.103427984,"about_ca_system_score_codex":0.0006114877,"about_ca_system_score_gemma":0.00059904234,"threshold_uncertainty_score":0.20565194},"labels":[],"label_agreement":null},{"id":"W2149532796","doi":"10.1029/2006gl027233","title":"A note on pore fluid pressure ratios in the Coulomb wedge theory","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Wedge (geometry); Coulomb; Geology; Pore water pressure; Fluid pressure; Geophysics; Mechanics; Physics; Geotechnical engineering; Nuclear physics; Optics","score_opus":0.026215877926289027,"score_gpt":0.28512644870175685,"score_spread":0.2589105707754678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149532796","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04561082,0.03985664,0.75974506,0.0153572,0.009735657,0.000075071745,0.00027437301,0.00077154394,0.12857372],"genre_scores_gemma":[0.78569144,0.027187183,0.14361185,0.0030210812,0.006411455,0.00012376666,0.00011605719,0.0006414916,0.03319568],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99868304,0.00034046912,0.00007366579,0.00018651714,0.000641153,0.00007521233],"domain_scores_gemma":[0.9978816,0.0015395734,0.000108845044,0.00023757487,0.00017949483,0.00005292738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022393782,0.000720287,0.0007865004,0.00065597665,0.00068839354,0.001534918,0.0021528783,0.0013078587,0.0035140305],"category_scores_gemma":[0.007451253,0.0003839089,0.0006380876,0.00058635,0.0041612047,0.0048073544,0.0020985233,0.0042442605,0.0011599173],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042522126,0.000028067589,0.00020148815,0.00017059487,0.000011156958,0.0005236313,0.00019011387,0.011609493,0.0044593355,0.9404036,0.0071669994,0.035193097],"study_design_scores_gemma":[0.000019395635,0.00013659286,0.00046316336,0.00009931895,0.000013899969,0.00044023016,0.000092271526,0.06348212,0.0056039323,0.87811583,0.05146914,0.000064093285],"about_ca_topic_score_codex":0.0011472119,"about_ca_topic_score_gemma":0.0004125908,"teacher_disagreement_score":0.0035140305,"about_ca_system_score_codex":0.0005105593,"about_ca_system_score_gemma":0.00040156563,"threshold_uncertainty_score":0.011843085},"labels":[],"label_agreement":null},{"id":"W2149947820","doi":"10.1029/2003jb002643","title":"Lack of continuity of the San Andreas Fault in southern California: Three‐dimensional fault models and earthquake scenarios","year":2004,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; San andreas fault; Seismology; Elastic-rebound theory; Thrust fault; Earthquake rupture; Tectonics; Transform fault; Fault (geology); Strike-slip tectonics; Echelon formation; Seismic gap; Fault scarp; Hypocenter; Slip (aerodynamics); Plate tectonics; Induced seismicity","score_opus":0.04890632754716738,"score_gpt":0.29548564317934695,"score_spread":0.24657931563217955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149947820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946338,0.00018313156,0.0014391142,0.0002706052,0.000004214378,0.0000148122745,0.00036052678,0.00003573841,0.0030580375],"genre_scores_gemma":[0.99850583,0.00022511953,0.000728021,0.000013543804,0.000004705184,0.0000103531875,0.00015512218,0.000005350906,0.00035197378],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990463,0.000025350448,0.00000782075,0.000032416418,0.000011341715,0.000018356825],"domain_scores_gemma":[0.99963784,0.00012404569,0.00009922198,0.000029488567,0.00003408681,0.00007524182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038092732,0.00046861026,0.000396301,0.0007256489,0.0007028446,0.0016677959,0.0010552855,0.0012853624,0.0010197219],"category_scores_gemma":[0.00094685686,0.00040742164,0.00058808475,0.00085164874,0.00082629896,0.00082488643,0.00062924233,0.00042843854,0.000102735474],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007769568,0.000064236905,0.051490217,0.000026804651,0.00005287704,0.00020079348,0.00019370025,0.9414378,0.0003684791,0.003619693,0.00039395157,0.0020736628],"study_design_scores_gemma":[0.000061825056,0.000044995722,0.02174613,0.000024545823,0.00004193446,0.000048168647,0.00023368074,0.97431785,0.00005918977,0.0027818573,0.00061649934,0.000023295479],"about_ca_topic_score_codex":0.13809146,"about_ca_topic_score_gemma":0.11558254,"teacher_disagreement_score":0.13809146,"about_ca_system_score_codex":0.0019060258,"about_ca_system_score_gemma":0.0008239465,"threshold_uncertainty_score":0.27457535},"labels":[],"label_agreement":null},{"id":"W2150150056","doi":"10.1785/0120140032","title":"Seismic-Wave Attenuation Determined from Tectonic Tremor in Multiple Subduction Zones","year":2014,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Subduction; Geology; Seismology; Attenuation; Tectonics","score_opus":0.02295338483293655,"score_gpt":0.2009293216387618,"score_spread":0.17797593680582524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150150056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999451,0.000016544236,0.00022144579,0.0000017943096,1.4103541e-7,0.0000021322876,0.00006229889,0.000007964848,0.00023657507],"genre_scores_gemma":[0.9997727,0.000007980833,0.00007935347,6.6208725e-7,2.3964236e-7,0.000002190769,0.00009234109,0.00000172958,0.000042753236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999168,0.000007105711,0.000012001946,0.000024791767,0.00002039996,0.000018854358],"domain_scores_gemma":[0.99922585,0.00016520827,0.0003167898,0.000067321846,0.0001556497,0.00006918108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022183478,0.00035377705,0.00023654074,0.0013285935,0.00020073986,0.0005367576,0.00033716424,0.0002027065,0.00080994883],"category_scores_gemma":[0.001311879,0.00022844569,0.00019005762,0.00088869274,0.00025762615,0.00030998868,0.00043798276,0.00015801378,0.00013142923],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010203652,0.000022049486,0.9746085,0.000018263077,0.00004205949,0.00013723956,0.00021453993,0.00646432,0.013819215,0.000052747026,0.00002886178,0.0044903033],"study_design_scores_gemma":[0.0000034810146,0.000015478165,0.99106616,0.000003054483,0.000009767376,0.00003348197,0.00010108337,0.0075113666,0.0011678413,0.000024304816,0.000060711736,0.0000032463863],"about_ca_topic_score_codex":0.031328656,"about_ca_topic_score_gemma":0.022004576,"teacher_disagreement_score":0.031328656,"about_ca_system_score_codex":0.00073554064,"about_ca_system_score_gemma":0.00019339158,"threshold_uncertainty_score":0.062292576},"labels":[],"label_agreement":null},{"id":"W2150593214","doi":"10.1111/1365-2478.12128","title":"Breakdown of the Gutenberg‐Richter relation for microearthquakes induced by hydraulic fracturing: influence of stratabound fractures","year":2014,"lang":"en","type":"article","venue":"Geophysical Prospecting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Hydraulic fracturing; Microseism; Log-normal distribution; Seismology; Fracture (geology); Attenuation; Magnitude (astronomy); Seismic hazard; Geotechnical engineering; Statistics; Mathematics","score_opus":0.0077536476699922394,"score_gpt":0.21850679105453533,"score_spread":0.2107531433845431,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150593214","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9791277,0.00009912182,0.017950574,0.00018639212,0.000005870368,0.000021601678,0.000148147,0.000098900586,0.002361674],"genre_scores_gemma":[0.9991763,0.000020654375,0.0006042324,0.000008513667,0.0000020638333,0.000006562785,0.000026142987,0.000008593519,0.00014698217],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99957734,0.00016316894,0.000025529223,0.000074690004,0.00008324568,0.00007595351],"domain_scores_gemma":[0.99096173,0.006684403,0.0013662012,0.00052788033,0.0002681469,0.00019167633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015031607,0.0002685074,0.00030918967,0.0005440427,0.00024001273,0.0005143243,0.0005189565,0.00055495946,0.001479037],"category_scores_gemma":[0.010893754,0.00018193189,0.0005551835,0.00020158994,0.00065492594,0.00063127175,0.00043682737,0.00045338925,0.00017704199],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023336605,0.00008346889,0.07802577,0.000061922125,0.00008306073,0.00065329054,0.00022276632,0.8765487,0.016099114,0.017056074,0.0005293064,0.010403159],"study_design_scores_gemma":[0.00001764756,0.0001059088,0.029688714,0.000009472698,0.000018829423,0.00016466374,0.000058914302,0.9617044,0.002777646,0.0052706744,0.00016053743,0.000022617729],"about_ca_topic_score_codex":0.006692651,"about_ca_topic_score_gemma":0.0037849413,"teacher_disagreement_score":0.006692651,"about_ca_system_score_codex":0.00052204466,"about_ca_system_score_gemma":0.00028011587,"threshold_uncertainty_score":0.013307393},"labels":[],"label_agreement":null},{"id":"W2150777094","doi":"10.1002/2014jb011084","title":"Crustal deformation and stress transfer during a propagating earthquake sequence: The 2013 Cook Strait sequence, central New Zealand","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Canadian Space Agency; Ministry of Economy, Trade and Industry; National Aeronautics and Space Administration","keywords":"Geology; Sinistral and dextral; Seismology; Foreshock; Bay; Tectonics; Geodesy; Slip (aerodynamics); Aftershock; Oceanography","score_opus":0.03960477484436853,"score_gpt":0.2931846881017314,"score_spread":0.2535799132573629,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150777094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989077,0.000034462802,0.000037686455,0.000021970494,0.0000017194283,0.000011691912,0.00036164562,0.000004225328,0.0006188567],"genre_scores_gemma":[0.99922,0.00007296852,0.00006861743,0.000005054369,0.00000170241,0.000008051619,0.00030943716,0.0000023047078,0.00031183587],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999033,0.000004697367,0.000009493577,0.000023700115,0.000033674347,0.000025038473],"domain_scores_gemma":[0.9996265,0.000020902015,0.00015476713,0.000016900094,0.00011733407,0.000063527696],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016365295,0.00033182578,0.00024141779,0.0010557717,0.0005462403,0.00073406484,0.00027990632,0.00028735143,0.0015415268],"category_scores_gemma":[0.0009508645,0.00022514162,0.00021699566,0.0014819207,0.00052027917,0.0003502365,0.00050411705,0.00027391693,0.00020928998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004728461,0.00012599498,0.93709254,0.0001596135,0.00018623623,0.0016116648,0.0066202353,0.0031933645,0.023039429,0.00018344946,0.0015876509,0.02572698],"study_design_scores_gemma":[0.0000034508244,0.000013074185,0.99903274,0.0000053102635,0.0000059280173,0.000032309606,0.00038902217,0.00026891739,0.00006968374,0.000007248668,0.00016806768,0.0000042251118],"about_ca_topic_score_codex":0.6434913,"about_ca_topic_score_gemma":0.76517963,"teacher_disagreement_score":0.6434913,"about_ca_system_score_codex":0.0023332217,"about_ca_system_score_gemma":0.001358687,"threshold_uncertainty_score":0.71721643},"labels":[],"label_agreement":null},{"id":"W2151214053","doi":"10.1002/grl.50826","title":"Scattered waves from low‐frequency earthquakes and plate boundary structure in northern Cascadia","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Geology; Subduction; Seismology; Plate tectonics; Waveform; Boundary (topology); Transect; Scattering; Geophysics; Tectonics; Physics; Optics; Oceanography","score_opus":0.01926826764238308,"score_gpt":0.2478294325732843,"score_spread":0.22856116493090123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151214053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988242,0.000011153834,0.0005977427,0.000031034568,0.0000012920898,0.000001519876,0.00010254058,0.000042319214,0.00038811783],"genre_scores_gemma":[0.99954623,0.000010219266,0.00017728862,0.0000016677483,8.465378e-7,0.0000016695449,0.0001209963,0.0000054479624,0.00013568957],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999405,0.000011273289,0.0000037195148,0.000018470331,0.000017064369,0.000008995584],"domain_scores_gemma":[0.99978846,0.000045940524,0.00003909242,0.000031325042,0.000046754234,0.0000485243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015862216,0.00029613182,0.00021141759,0.0005294813,0.0003388945,0.00050098135,0.0003934287,0.00036553878,0.0009293947],"category_scores_gemma":[0.0008011952,0.00035442115,0.0003734526,0.0004532347,0.0002828624,0.0002671334,0.0003429567,0.00029490708,0.00017922063],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019994196,0.00011062122,0.41228864,0.000051593892,0.0001615305,0.0006287932,0.000807393,0.5559755,0.018352024,0.00062597025,0.00046094725,0.010337034],"study_design_scores_gemma":[0.000032924036,0.00004673834,0.4589375,0.000009289459,0.00003081501,0.00006855967,0.0002991709,0.5383339,0.0014379417,0.0004500249,0.0003283015,0.000024924833],"about_ca_topic_score_codex":0.103647195,"about_ca_topic_score_gemma":0.08434357,"teacher_disagreement_score":0.103647195,"about_ca_system_score_codex":0.0011037877,"about_ca_system_score_gemma":0.0005413515,"threshold_uncertainty_score":0.20608783},"labels":[],"label_agreement":null},{"id":"W2151319326","doi":"10.4401/ag-6665","title":"Relations between source parameters for large Persian earthquakes","year":2015,"lang":"en","type":"article","venue":"Annals of Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"International Institute of Earthquake Engineering and Seismology; University of Tehran","keywords":"Span (engineering); Magnitude (astronomy); Earthquake magnitude; Life span; Mathematics; Physics; Geometry; Astrophysics; Medicine","score_opus":0.10438341493248446,"score_gpt":0.2906516401461784,"score_spread":0.18626822521369393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151319326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9792924,0.00069298624,0.010908735,0.00011537738,0.00001184796,0.00003123821,0.0030636203,0.00040040657,0.005483458],"genre_scores_gemma":[0.9965771,0.0001371266,0.0017578269,0.000004848068,0.000007885734,0.000008916367,0.0012345873,0.000022044154,0.00024967355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979085,0.00003962589,0.000033834047,0.00006475011,0.000052318555,0.000018598019],"domain_scores_gemma":[0.99575186,0.0025257831,0.0007716026,0.00037377904,0.00052246253,0.000054545675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006479084,0.00039705413,0.0001325678,0.0028770221,0.000099823264,0.000426856,0.00023699425,0.00019432114,0.002521549],"category_scores_gemma":[0.008378298,0.00013073103,0.0002337319,0.0022016242,0.00020916351,0.0005223827,0.0002847888,0.0002488512,0.00052184815],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012208326,0.000028683855,0.8756769,0.00011317519,0.00012275377,0.00053000223,0.0005314073,0.03745232,0.0036709001,0.0028061515,0.0015904186,0.07735516],"study_design_scores_gemma":[0.000013299362,0.00004368514,0.9516314,0.00002918426,0.000051190575,0.00047356708,0.00041568934,0.039341144,0.0026832959,0.0028830753,0.0024056807,0.000028759103],"about_ca_topic_score_codex":0.0043886243,"about_ca_topic_score_gemma":0.0036405742,"teacher_disagreement_score":0.0043886243,"about_ca_system_score_codex":0.00041329916,"about_ca_system_score_gemma":0.00024112863,"threshold_uncertainty_score":0.00872618},"labels":[],"label_agreement":null},{"id":"W2151661722","doi":"10.1142/s179343111440003x","title":"Combining Tsunami Hazard and Vulnerability on the Assessment of Tsunami Inundation Probability in Taiwan","year":2014,"lang":"en","type":"article","venue":"Journal of Earthquake and Tsunami","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McMaster University","keywords":"Vulnerability (computing); Hazard; Seismology; Tsunami wave; Seismic hazard; Geology; Probabilistic logic; Tsunami earthquake; Earthquake scenario; Conditional probability; Statistics; Computer science; Computer security; Mathematics","score_opus":0.023755262834079874,"score_gpt":0.2584173432457723,"score_spread":0.23466208041169245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151661722","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92999274,0.0002407726,0.067660354,0.00018671926,0.000008299778,0.000042522246,0.00016458961,0.000083134866,0.0016209353],"genre_scores_gemma":[0.99593997,0.000098834,0.0036887927,0.000005065411,0.0000067654055,0.000011665761,0.000071139555,0.0000036275164,0.00017411308],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996823,0.000096121985,0.000036639718,0.000062744795,0.00007503872,0.000047132376],"domain_scores_gemma":[0.9989416,0.00049055147,0.0002552565,0.000053190666,0.0001728777,0.000086399414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009237662,0.0006191417,0.0003598344,0.0020571072,0.00023916912,0.00095174374,0.00049655535,0.00050054025,0.0005196807],"category_scores_gemma":[0.0030295828,0.00025293828,0.00049966935,0.0011736277,0.00028297407,0.0008813097,0.0010354602,0.00025832,0.00005546158],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009467782,0.000047500467,0.17622443,0.00009514604,0.00015090435,0.0006745543,0.00020959746,0.77751255,0.0022539957,0.0028650505,0.00024687103,0.03962476],"study_design_scores_gemma":[0.0000038385188,0.000057717945,0.03177113,0.000012154808,0.00004790437,0.00012967196,0.00013935524,0.96527284,0.00062381703,0.0017207345,0.00020189046,0.000019079844],"about_ca_topic_score_codex":0.009435264,"about_ca_topic_score_gemma":0.00513192,"teacher_disagreement_score":0.009435264,"about_ca_system_score_codex":0.00060346577,"about_ca_system_score_gemma":0.0006639849,"threshold_uncertainty_score":0.018760681},"labels":[],"label_agreement":null},{"id":"W2152932092","doi":"10.1007/s00024-004-0190-y","title":"Some Insights into Topographic, Elastic and Self-gravitation Interaction in Modelling Ground Deformation and Gravity Changes in Active Volcanic Areas","year":2007,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy","keywords":"Volcano; Gravitation; Deformation (meteorology); Geology; Geophysics; Geodesy; Physics; Seismology; Classical mechanics","score_opus":0.009623362450029442,"score_gpt":0.2050637914952319,"score_spread":0.19544042904520245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152932092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86717474,0.00072743,0.12413493,0.0011607647,0.000043212367,0.00006462746,0.00014833295,0.0001274906,0.006418436],"genre_scores_gemma":[0.9902062,0.00021181544,0.008342387,0.000039589373,0.00002024416,0.00001955675,0.000030442588,0.000022943774,0.0011068697],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99979216,0.000103322614,0.000022089178,0.000025103323,0.000031773365,0.00002556336],"domain_scores_gemma":[0.99928313,0.0005444527,0.000041321222,0.000027476692,0.00006762396,0.000035945308],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010810426,0.0006008842,0.00058150693,0.00034901727,0.00083175837,0.0015282852,0.0009589914,0.0015069864,0.0018309873],"category_scores_gemma":[0.0038165895,0.00089372357,0.0008075724,0.00050572935,0.0011358638,0.0018246277,0.00074872223,0.0009080561,0.0001386208],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004977638,0.00006327195,0.0054865954,0.000035948302,0.00004442204,0.00021041068,0.00021534783,0.9809599,0.0032536422,0.0049557877,0.00014452105,0.0045805075],"study_design_scores_gemma":[0.000012991322,0.000033954246,0.0023791115,0.0000050952335,0.000017260903,0.00002066037,0.000092130926,0.9946883,0.00038852132,0.0021861068,0.00016608177,0.000009859759],"about_ca_topic_score_codex":0.02617735,"about_ca_topic_score_gemma":0.025245316,"teacher_disagreement_score":0.02617735,"about_ca_system_score_codex":0.0005877166,"about_ca_system_score_gemma":0.000449321,"threshold_uncertainty_score":0.052049935},"labels":[],"label_agreement":null},{"id":"W2153089272","doi":"10.1186/1880-5981-66-67","title":"A large mantle water source for the northern San Andreas fault system: a ghost of subduction past","year":2014,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Japan Society for the Promotion of Science; U.S. Geological Survey; University of Tokyo","keywords":"Geology; Subduction; Mantle wedge; Mantle (geology); Seismology; Plate tectonics; Transition zone; Volcanic arc; Tectonics; Geochemistry; Petrology","score_opus":0.00813851254881317,"score_gpt":0.18382419497334634,"score_spread":0.17568568242453317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153089272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962566,0.00012224841,0.0010541468,0.00011019732,0.000003412105,0.0000031122963,0.000058563874,0.00004638832,0.0023453897],"genre_scores_gemma":[0.9992955,0.000052473373,0.00031728053,0.0000026450684,0.0000017660515,0.00000122715,0.00003374145,0.000004288815,0.00029100335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999769,0.0000026165217,0.0000022549289,0.0000094000725,0.000004782173,0.0000040554364],"domain_scores_gemma":[0.99994946,0.0000065757345,0.000018206694,0.0000064167716,0.000007786004,0.000011526211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004425578,0.0001829757,0.00016569906,0.0003079873,0.0003720736,0.00041163238,0.00029246914,0.00026000667,0.0013385663],"category_scores_gemma":[0.00019222366,0.00019143368,0.00020903631,0.00023672619,0.00035206636,0.00044300852,0.00036400504,0.00015583102,0.00010526773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039371307,0.00015530527,0.62776375,0.00022513508,0.000154883,0.0025132431,0.0009413451,0.17800859,0.15386392,0.009589298,0.0007331169,0.025657777],"study_design_scores_gemma":[0.000077804325,0.00014511465,0.4554624,0.000031535175,0.000100837235,0.00054674014,0.00076532766,0.5290147,0.007555775,0.0032135202,0.0030419559,0.00004432497],"about_ca_topic_score_codex":0.019883715,"about_ca_topic_score_gemma":0.016992621,"teacher_disagreement_score":0.019883715,"about_ca_system_score_codex":0.0006049809,"about_ca_system_score_gemma":0.00040010977,"threshold_uncertainty_score":0.039536},"labels":[],"label_agreement":null},{"id":"W2153374388","doi":"10.1029/2011gl050064","title":"Shear wave reflectivity imaging of the Nazca‐South America subduction zone: Stagnant slab in the mantle transition zone?","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Transition zone; Subduction; Slab; Seismology; Mantle (geology); Discontinuity (linguistics); Classification of discontinuities; Slab window; Mantle wedge; Shear zone; Convergent boundary; Oceanic crust; Geophysics; Petrology; Tectonics","score_opus":0.043922225755914084,"score_gpt":0.28618831028623637,"score_spread":0.24226608453032228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153374388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984818,0.000100706544,0.0006330568,0.000021281254,0.0000010136667,0.000002992428,0.00007381253,0.000014877396,0.00067035685],"genre_scores_gemma":[0.9981541,0.00009880428,0.0013598851,0.00000947695,0.00000252359,0.0000026695986,0.00011087822,0.000005011545,0.00025662512],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997175,0.0000027422286,0.000001607811,0.0000071852323,0.000007829104,0.000008907091],"domain_scores_gemma":[0.999956,0.0000057377115,0.000010739931,0.0000047238955,0.000014072114,0.000008757387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011182473,0.0001496976,0.00010045771,0.0004740671,0.0001352996,0.00029727435,0.000175667,0.00017442972,0.00059362105],"category_scores_gemma":[0.00022183478,0.00013390381,0.00008628059,0.00039986786,0.000099187426,0.00024019749,0.00023626238,0.00011745998,0.00015615171],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025077313,0.00006355988,0.3777185,0.00006814026,0.00008497274,0.00036107213,0.0007292296,0.0015696881,0.56550264,0.00021635163,0.00026457434,0.05317049],"study_design_scores_gemma":[0.000008778522,0.00004198584,0.98015094,0.00000803625,0.000042891385,0.00026117568,0.00033649558,0.004772725,0.013448559,0.000079723926,0.0008418112,0.0000067840338],"about_ca_topic_score_codex":0.0060163005,"about_ca_topic_score_gemma":0.013828562,"teacher_disagreement_score":0.0060163005,"about_ca_system_score_codex":0.000107701875,"about_ca_system_score_gemma":0.00015563144,"threshold_uncertainty_score":0.011962593},"labels":[],"label_agreement":null},{"id":"W2154460930","doi":"10.1193/1.1542891","title":"A Methodology for Probabilistic Fault Displacement Hazard Analysis (PFDHA)","year":2003,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":194,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"","keywords":"Displacement (psychology); Fault (geology); Probabilistic logic; Seismic hazard; Seismology; Tectonics; Geology; Hazard; Attenuation; Geodesy; Statistics; Mathematics","score_opus":0.05114527396500882,"score_gpt":0.28312357412784966,"score_spread":0.23197830016284085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154460930","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000173217,0.000051853913,0.9990283,0.000026424947,0.000017447826,0.000046364312,0.000091091104,0.00017805745,0.0003871636],"genre_scores_gemma":[0.021735342,0.00018677981,0.97537804,0.00008269426,0.00009469007,0.00061482884,0.00040787418,0.00020998355,0.0012897465],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9956391,0.0020131024,0.00026603547,0.0006340243,0.0012605388,0.0001872993],"domain_scores_gemma":[0.99379855,0.0036995413,0.00036269944,0.0011069644,0.0008881473,0.00014399433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0051549627,0.001372325,0.0010701958,0.0040069045,0.0011751311,0.0017952484,0.0027637794,0.0009998179,0.009634289],"category_scores_gemma":[0.014709175,0.00090242,0.002204109,0.0027802244,0.001459157,0.0017933975,0.0033496101,0.0028751038,0.0036360316],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043483113,0.00009639701,0.0028682526,0.00044127816,0.00031990756,0.0002929061,0.00034902315,0.13688944,0.005714609,0.33098152,0.015806584,0.50619656],"study_design_scores_gemma":[0.000036496232,0.00009788774,0.0012629997,0.000086938206,0.00010462215,0.0008595546,0.00010483529,0.52093905,0.003307485,0.41046396,0.06264568,0.00009051029],"about_ca_topic_score_codex":0.002655833,"about_ca_topic_score_gemma":0.0021748305,"teacher_disagreement_score":0.009634289,"about_ca_system_score_codex":0.0009174135,"about_ca_system_score_gemma":0.0019781536,"threshold_uncertainty_score":0.0322299},"labels":[],"label_agreement":null},{"id":"W2155288505","doi":"10.1111/j.1365-246x.2010.04664.x","title":"Delineating the rupture planes of an earthquake doublet using Source-Scanning Algorithm: application to the 2005 March 3 Ilan Doublet, northeast Taiwan","year":2010,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Seismogram; Seismology; Waveform; Amplitude; Geology; Inversion (geology); Earthquake location; Geodesy; Algorithm; Magnitude (astronomy); Hypocenter; Computer science; Physics; Tectonics; Induced seismicity; Optics; Telecommunications","score_opus":0.014206349197028149,"score_gpt":0.2563789863169763,"score_spread":0.24217263711994816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155288505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98036915,0.000068290625,0.018985037,0.00004237234,0.000005128107,0.00001583248,0.00007516118,0.0001548341,0.00028421235],"genre_scores_gemma":[0.96214384,0.00006954961,0.037295185,0.0000083824425,0.000006178728,0.000010025795,0.00027432115,0.0000119119795,0.00018051449],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99992585,0.000012758222,0.000008389083,0.000023982519,0.000016000045,0.000013056901],"domain_scores_gemma":[0.9997279,0.000068142224,0.000055800414,0.000033059958,0.00007437675,0.000040742387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033168565,0.00043835054,0.00029840448,0.00075939624,0.00022175866,0.00039646027,0.00045015506,0.00044895237,0.00030195893],"category_scores_gemma":[0.000809369,0.00015849317,0.00029787325,0.0006690986,0.00014758155,0.0002287491,0.00031544414,0.00016527082,0.00007776284],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009719251,0.00053675927,0.16980547,0.00026830402,0.00020577373,0.004260526,0.0010469672,0.28082705,0.17184317,0.0013110483,0.0012575906,0.36766547],"study_design_scores_gemma":[0.000037247883,0.00013380566,0.03775297,0.000006300842,0.000035095687,0.00028728865,0.00020548383,0.95144486,0.009415872,0.00023073597,0.0004324101,0.000017878445],"about_ca_topic_score_codex":0.008050046,"about_ca_topic_score_gemma":0.008099953,"teacher_disagreement_score":0.008050046,"about_ca_system_score_codex":0.00020809371,"about_ca_system_score_gemma":0.00049781386,"threshold_uncertainty_score":0.01600641},"labels":[],"label_agreement":null},{"id":"W2155290904","doi":"10.1139/e01-100","title":"A gravity profile across southern Saganash Lake fault: implications for the origin of the Kapuskasing Structural Zone","year":2002,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Sinistral and dextral; Shear zone; Fault (geology); Seismology; Extensional definition; Shear (geology); Geodesy; Paleontology; Tectonics","score_opus":0.04497946212561604,"score_gpt":0.2609300213901272,"score_spread":0.21595055926451118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155290904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997999,0.000038463662,0.00010534174,0.00010723784,0.0000018889067,0.0000028598663,0.00005658242,0.0000090357535,0.0016795608],"genre_scores_gemma":[0.9996649,0.00002825218,0.000110846704,0.000007331549,0.0000012083536,0.0000012683367,0.00004951135,0.0000011129359,0.0001355051],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999567,0.0000029676764,0.0000035549615,0.0000074098825,0.000009960908,0.00001932811],"domain_scores_gemma":[0.9998976,0.00001140077,0.00003207476,0.000005213459,0.00003517966,0.000018588407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000717659,0.000105467385,0.000118915246,0.00063477154,0.0006230417,0.0005280262,0.00018006215,0.00018281858,0.0010718441],"category_scores_gemma":[0.0002881866,0.00012184987,0.00008853732,0.00084524904,0.0006820997,0.00035331814,0.0005608463,0.00018922007,0.00010742442],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031311202,0.000033937267,0.93185616,0.00007270048,0.000017307873,0.0013998698,0.0029980843,0.0032134717,0.024717478,0.0045254333,0.00048404443,0.030368444],"study_design_scores_gemma":[0.000013925809,0.000038193102,0.99264187,0.000014834582,0.00000907164,0.00031776106,0.0022999148,0.00231634,0.0007026868,0.0008520072,0.00078077463,0.0000125978],"about_ca_topic_score_codex":0.043201413,"about_ca_topic_score_gemma":0.07812374,"teacher_disagreement_score":0.9567986,"about_ca_system_score_codex":0.00071012025,"about_ca_system_score_gemma":0.00090176595,"threshold_uncertainty_score":0.08589989},"labels":[],"label_agreement":null},{"id":"W2155299533","doi":"10.1111/j.1365-246x.2009.04275.x","title":"Stress channelling and partitioning of seismicity in the Charlevoix seismic zone, Québec, Canada","year":2009,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Induced seismicity; Seismology; Rift; Stress field; Classification of discontinuities; Rift zone; Stress (linguistics); Tectonics; Geophysics; Finite element method","score_opus":0.01012984342548252,"score_gpt":0.2061802030277005,"score_spread":0.19605035960221798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155299533","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9812804,0.00037229553,0.0008710479,0.0002798496,0.000010182395,0.000055784098,0.006640184,0.00013740009,0.0103529105],"genre_scores_gemma":[0.9955342,0.000095064206,0.00056440977,0.000018365874,0.0000013822819,0.000011005247,0.0011794972,0.000014905926,0.002581091],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997695,0.000014143009,0.0000091301945,0.000062823085,0.000058377234,0.00008595837],"domain_scores_gemma":[0.99950945,0.00006403109,0.000056047233,0.000016142541,0.00026294187,0.0000913452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022889025,0.0003739685,0.0002658645,0.0015815572,0.0015670282,0.0017043168,0.0010684971,0.00054841413,0.0050997846],"category_scores_gemma":[0.0010666898,0.00031301755,0.00029167856,0.0021708482,0.00091507344,0.0003344322,0.0005502399,0.0003326011,0.00032010017],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002661786,0.000118509255,0.76641387,0.00015651697,0.00013827995,0.0006398654,0.0018776028,0.17000909,0.005219071,0.004663031,0.009822452,0.0406756],"study_design_scores_gemma":[0.000040739047,0.000026711461,0.8484742,0.000059736558,0.000026661579,0.000056164525,0.0014284905,0.1432831,0.0005005632,0.00036221155,0.0056642857,0.00007725083],"about_ca_topic_score_codex":0.9979036,"about_ca_topic_score_gemma":0.9986872,"teacher_disagreement_score":0.046656918,"about_ca_system_score_codex":0.046656918,"about_ca_system_score_gemma":0.018278139,"threshold_uncertainty_score":0.33852124},"labels":[],"label_agreement":null},{"id":"W2155364473","doi":"10.1029/2011jb009052","title":"The role of outcrop‐to‐outcrop fluid flow in off‐axis oceanic hydrothermal systems under abyssal sedimentation conditions","year":2012,"lang":"en","type":"article","venue":"Journal of Geophysical Research Atmospheres","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Outcrop; Geology; Geomorphology; Aquifer; Seafloor spreading; Petrology; Geochemistry; Geophysics; Groundwater; Geotechnical engineering","score_opus":0.027314502998716152,"score_gpt":0.3036584255567303,"score_spread":0.27634392255801415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155364473","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995635,0.0000073881183,0.00020372664,0.000009403151,4.6809373e-7,0.0000012118696,0.000019125438,0.000009851346,0.00018524594],"genre_scores_gemma":[0.9998549,0.0000083867835,0.000063768275,0.0000010167969,2.6706778e-7,5.733469e-7,0.000019153484,0.0000024860208,0.000049342703],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999243,0.00001357684,0.0000043755767,0.000028797593,0.000008054113,0.000020798818],"domain_scores_gemma":[0.99980825,0.000058134483,0.000046633588,0.000019646614,0.000025523872,0.000041847074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001870062,0.00033100304,0.00021846275,0.0004333563,0.00043134624,0.0006865279,0.00041918753,0.00033950937,0.0005126748],"category_scores_gemma":[0.00083840074,0.0003466987,0.0003733841,0.00024232709,0.00065014977,0.00047369287,0.00057419564,0.00019247142,0.00003806294],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027882602,0.00012247203,0.40829593,0.00004476281,0.00011027345,0.0005670077,0.0004663189,0.5351908,0.046132475,0.0011710356,0.00012040965,0.007499621],"study_design_scores_gemma":[0.000044625307,0.00013415141,0.3011083,0.000010447588,0.000041117033,0.00008422679,0.0003351389,0.6918708,0.0057385205,0.00042241788,0.00017512385,0.000035103854],"about_ca_topic_score_codex":0.06890375,"about_ca_topic_score_gemma":0.042292006,"teacher_disagreement_score":0.06890375,"about_ca_system_score_codex":0.0012365027,"about_ca_system_score_gemma":0.0007509567,"threshold_uncertainty_score":0.13700539},"labels":[],"label_agreement":null},{"id":"W2155393556","doi":"10.1130/g25247a.1","title":"Grenville Province and Monteregian carbonatite and nepheline syenite distribution related to rifting, collision, and plume passage","year":2008,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Drug Applied Research Center, Tabriz University of Medical Sciences","keywords":"Citation; Rift; Carbonatite; Geology; Library science; Archaeology; Geochemistry; Geography; Tectonics; Paleontology","score_opus":0.007778180502762587,"score_gpt":0.18833431769270184,"score_spread":0.18055613718993926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155393556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882528,0.0027710707,0.00006982983,0.00025204837,0.000010992444,0.000015433814,0.0016369037,0.000015741942,0.006975286],"genre_scores_gemma":[0.99528897,0.00094716996,0.00018745768,0.00002758098,0.000010443053,0.0000046079654,0.0018706282,0.000007098692,0.001656028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975103,0.00002332479,0.000017295664,0.000053306212,0.00010387677,0.000051170104],"domain_scores_gemma":[0.999108,0.00010273761,0.0004201912,0.00003371656,0.00024973394,0.00008557452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031057763,0.00017931104,0.00022745677,0.002677665,0.0004726106,0.00058504206,0.00044592604,0.0003484986,0.002091799],"category_scores_gemma":[0.0013118915,0.000120734454,0.00019858692,0.0027715375,0.0005669268,0.00040568595,0.00066523615,0.00020749675,0.0002763905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020697148,0.000011642818,0.97326034,0.00009006199,0.000071348666,0.00064184837,0.0008058817,0.00018623393,0.0029692075,0.0001872401,0.0015832292,0.019985868],"study_design_scores_gemma":[0.0000024829508,0.0000066960697,0.9981614,0.000012005831,0.000004466069,0.00024179852,0.00025125354,0.000043362215,0.000104784915,0.000017036897,0.0011519863,0.000002796378],"about_ca_topic_score_codex":0.26569867,"about_ca_topic_score_gemma":0.51505286,"teacher_disagreement_score":0.7343013,"about_ca_system_score_codex":0.0012295031,"about_ca_system_score_gemma":0.0010570483,"threshold_uncertainty_score":0.5283043},"labels":[],"label_agreement":null},{"id":"W2155835733","doi":"10.1193/1.4000033","title":"Factors that Exacerbated or Reduced Impacts of the 27 February 2010 Chile Tsunami","year":2012,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Stillwater (Canada)","funders":"Earthquake Engineering Research Institute","keywords":"Warning system; Vulnerability (computing); Geography; Warning signs; Natural disaster; Government (linguistics); Socioeconomics; Environmental protection; Meteorology; Engineering","score_opus":0.0409798314218374,"score_gpt":0.23751132403230604,"score_spread":0.19653149261046865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155835733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886875,0.0002943001,0.00007259272,0.000601533,0.000015980679,0.000024030142,0.00033386133,0.000006377199,0.009963762],"genre_scores_gemma":[0.9971955,0.00037736833,0.000083408944,0.000092157876,0.000018420767,0.000016004606,0.00022270421,0.000003991536,0.0019904962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970144,0.00007011796,0.000020314696,0.000048807906,0.000046672296,0.0001126428],"domain_scores_gemma":[0.9990957,0.00014325391,0.00041892906,0.000052585507,0.000160319,0.00012926801],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040154383,0.00021206887,0.0001668221,0.00048228833,0.0007110483,0.0012987148,0.00025857848,0.0003439629,0.0063943225],"category_scores_gemma":[0.0035662046,0.00010951088,0.00014630944,0.0006262837,0.00055335456,0.00065156963,0.0007662471,0.00034025026,0.0004179884],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033250547,0.00018009968,0.92993766,0.00046334372,0.0001094389,0.001560103,0.01567015,0.00051471766,0.006141707,0.0014936109,0.004630772,0.038965885],"study_design_scores_gemma":[0.0000061526525,0.000048505943,0.98224705,0.0000521186,0.000014155601,0.000096218064,0.009810159,0.00006128189,0.00035807458,0.00015952779,0.0071361745,0.000010536457],"about_ca_topic_score_codex":0.037501615,"about_ca_topic_score_gemma":0.08384179,"teacher_disagreement_score":0.037501615,"about_ca_system_score_codex":0.0014703801,"about_ca_system_score_gemma":0.0017729248,"threshold_uncertainty_score":0.07456666},"labels":[],"label_agreement":null},{"id":"W2155928202","doi":"10.1002/2014jb011596","title":"Volcanic tremor and frequency gliding during dike intrusions at Kılauea—A tale of three eruptions","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research","keywords":"Dike; Geology; Magma; Seismology; Volcano; Intrusion; Lava; Impact crater; Phase (matter); Petrology; Physics; Geochemistry","score_opus":0.07803422778911674,"score_gpt":0.3218896628652319,"score_spread":0.24385543507611518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155928202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994117,0.000032509448,0.000049756465,0.0000075816133,0.0000021992241,0.0000051515676,0.00011098861,0.000005285505,0.00037487852],"genre_scores_gemma":[0.99915063,0.000028117927,0.00012714656,0.000010535629,0.000006320687,0.000010151,0.00043162043,0.0000033488275,0.00023217987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998723,0.0000063250714,0.000010283458,0.000038772225,0.00003247763,0.000039879953],"domain_scores_gemma":[0.9996575,0.000039578088,0.000087648696,0.000023390789,0.00007403241,0.00011782954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021061541,0.00032461842,0.00040715604,0.0014155377,0.0006662469,0.0005725523,0.00033582907,0.00070780824,0.0006902529],"category_scores_gemma":[0.00032580463,0.00027573959,0.00035376896,0.00082337117,0.00041747317,0.00035378904,0.0006830378,0.000501783,0.00020051816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044631315,0.00018788756,0.9319668,0.000065933986,0.00015838597,0.0011286894,0.0018063517,0.0006202655,0.054033395,0.000047780843,0.0002593219,0.009278889],"study_design_scores_gemma":[0.0000024282006,0.000027908958,0.9989839,0.0000023684274,0.000008998059,0.00006125002,0.00025718013,0.00016864388,0.0003440607,0.0000032948847,0.00013491446,0.0000049163586],"about_ca_topic_score_codex":0.009860242,"about_ca_topic_score_gemma":0.034682233,"teacher_disagreement_score":0.009860242,"about_ca_system_score_codex":0.00050691393,"about_ca_system_score_gemma":0.00024262229,"threshold_uncertainty_score":0.019605696},"labels":[],"label_agreement":null},{"id":"W2156253249","doi":"10.1111/j.1365-246x.2006.03144.x","title":"Geophysical constraints on the crustal architecture of the Troodos ophiolite: results from the IANGASS project","year":2006,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Ophiolite; Ultramafic rock; Peridotite; Seismology; Seismic refraction; Geophysics; Petrology; Geochemistry; Tectonics; Basalt","score_opus":0.017160627156348467,"score_gpt":0.2262623514555307,"score_spread":0.20910172429918222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156253249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99799085,0.000040724033,0.000130442,0.000027640404,0.0000018040676,0.0000041048697,0.00058134773,0.000042921856,0.0011802054],"genre_scores_gemma":[0.99773335,0.00007667166,0.0004888497,0.00000808098,0.0000039790716,0.000006220484,0.0013562229,0.000031555777,0.00029504456],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998528,0.00004280178,0.0000075013977,0.000035913115,0.000019935624,0.000041111813],"domain_scores_gemma":[0.9997644,0.00008333593,0.00004484567,0.000036538357,0.000030711333,0.00004022252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042524157,0.0009454691,0.00051548553,0.00047275441,0.00040058093,0.0010860995,0.00069821504,0.000587002,0.001772837],"category_scores_gemma":[0.00074562745,0.0003426802,0.000851622,0.0006570497,0.0006940287,0.00036868488,0.00067154533,0.00033873747,0.0003320951],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055493944,0.00012038525,0.20863134,0.00010539666,0.00020452126,0.0005474309,0.00023860275,0.7769382,0.0038862673,0.00078443426,0.00069355854,0.0072948965],"study_design_scores_gemma":[0.00023998755,0.00018394447,0.231079,0.000043424745,0.00015111954,0.00015908094,0.00060508924,0.7624808,0.0018146109,0.0006609461,0.0025377572,0.00004433049],"about_ca_topic_score_codex":0.07484422,"about_ca_topic_score_gemma":0.060874715,"teacher_disagreement_score":0.07484422,"about_ca_system_score_codex":0.0009596028,"about_ca_system_score_gemma":0.00064605824,"threshold_uncertainty_score":0.14881712},"labels":[],"label_agreement":null},{"id":"W2156395869","doi":"10.1002/jgrb.50325","title":"A hydrologic model for the uppermost oceanic crust constrained by temperature estimates from carbonate minerals","year":2013,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Aquifer; Geology; Outcrop; Carbonate; Geochemistry; Crust; Petrology; Aquifer test; Carbonate rock; Geomorphology; Groundwater; Sedimentary rock; Groundwater recharge; Geotechnical engineering","score_opus":0.039133953535944135,"score_gpt":0.30049901367181253,"score_spread":0.2613650601358684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156395869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89494693,0.00020607315,0.08955703,0.00078174414,0.000030983236,0.00006638146,0.0015970584,0.00026189108,0.012551911],"genre_scores_gemma":[0.9935527,0.000108872584,0.0030636261,0.000034193974,0.00001291901,0.000046201483,0.00030053372,0.000036557234,0.0028443313],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989307,0.000023066836,0.000006905171,0.000041563406,0.000012518564,0.000022875849],"domain_scores_gemma":[0.9996599,0.00012656637,0.00008675989,0.000029237775,0.000046201294,0.00005126195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037912803,0.0005298258,0.0003210574,0.00050992245,0.00043015054,0.0013941275,0.0014669242,0.0008182988,0.00276277],"category_scores_gemma":[0.0012221204,0.0006673193,0.00071961223,0.00056218967,0.00087689364,0.0010729245,0.00068665127,0.000581211,0.00036418068],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029712834,0.000015048185,0.0047727814,0.0000068071136,0.000018341245,0.000060027127,0.000023967668,0.98981804,0.0011649721,0.0030471736,0.00012496406,0.00091813656],"study_design_scores_gemma":[0.000020708272,0.0000073657575,0.0017424067,0.000002404435,0.000008408782,0.000010653455,0.000014597434,0.9963909,0.00012746801,0.0014911983,0.00017692693,0.0000070252377],"about_ca_topic_score_codex":0.06599459,"about_ca_topic_score_gemma":0.027457071,"teacher_disagreement_score":0.06599459,"about_ca_system_score_codex":0.0014264502,"about_ca_system_score_gemma":0.0014893174,"threshold_uncertainty_score":0.13122094},"labels":[],"label_agreement":null},{"id":"W2156493223","doi":"10.1193/080512eqs254m","title":"Variation of Source‐to‐Site Distance for Megathrust Subduction Earthquakes: Effects on Ground Motion Prediction Equations","year":2013,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Subduction; Geology; Seismology; Ground motion; Fault (geology); Strong ground motion; Geodesy; Motion (physics); Tectonics; Physics; Classical mechanics","score_opus":0.01201667580750652,"score_gpt":0.20638834731412892,"score_spread":0.1943716715066224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156493223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9408817,0.0002644915,0.057148624,0.00015541834,0.000013631895,0.00002950389,0.00016434025,0.00013953482,0.0012026085],"genre_scores_gemma":[0.991521,0.00008781991,0.008106051,0.000012204949,0.0000025918441,0.000010461939,0.00009988934,0.000029414921,0.0001304787],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9993967,0.00023499363,0.00007170353,0.00012931597,0.0001313648,0.000035837355],"domain_scores_gemma":[0.9900551,0.008015075,0.00077206694,0.00041886375,0.0006459353,0.00009297459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023342695,0.00044189993,0.00043329925,0.00037845384,0.00019416778,0.00076676207,0.0010403007,0.0005957701,0.00049198326],"category_scores_gemma":[0.01377227,0.00031066826,0.0004988254,0.0003259438,0.00036868488,0.0008527897,0.00061315653,0.0006924384,0.00010799528],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086808555,0.000048379497,0.05038,0.00007750496,0.000057075693,0.00016487295,0.00013125449,0.92586315,0.0048565334,0.0015723009,0.00009929555,0.016662776],"study_design_scores_gemma":[0.000012893261,0.00003782712,0.009763893,0.000015486232,0.000016123833,0.00004202507,0.000036863006,0.9859994,0.003626941,0.00033349846,0.000100569276,0.00001442255],"about_ca_topic_score_codex":0.009344769,"about_ca_topic_score_gemma":0.0066320063,"teacher_disagreement_score":0.009344769,"about_ca_system_score_codex":0.0008437017,"about_ca_system_score_gemma":0.00073838705,"threshold_uncertainty_score":0.018580735},"labels":[],"label_agreement":null},{"id":"W2156568407","doi":"10.1002/2015jb012195","title":"Magnitudes and moment‐duration scaling of low‐frequency earthquakes beneath southern Vancouver Island","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Scaling; Moment magnitude scale; Geodesy; Attenuation; Waveform; Seismology; Magnitude (astronomy); Moment (physics); Geology; Physics; Slip (aerodynamics); Exponential decay; Geometry; Optics; Mathematics; Astrophysics; Voltage; Classical mechanics","score_opus":0.0492726265220276,"score_gpt":0.30627212708802154,"score_spread":0.25699950056599397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156568407","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99757856,0.000032507403,0.00024604975,0.000014738845,0.0000016693408,0.000004736075,0.00075999787,0.000018468168,0.0013433258],"genre_scores_gemma":[0.9985,0.000027010667,0.00019997144,0.0000028386103,0.0000012746742,0.0000029125847,0.00086104596,0.000005714781,0.00039919923],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999897,0.0000063251914,0.0000061523033,0.00002646069,0.00004188848,0.00002220604],"domain_scores_gemma":[0.99938214,0.00009016076,0.00009878076,0.000037386297,0.00027310263,0.00011844187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105535786,0.00016288683,0.00015941774,0.0011892738,0.00032985542,0.0008669304,0.00027920588,0.00021375198,0.0014935966],"category_scores_gemma":[0.0011706962,0.00019097679,0.00010606222,0.0011161668,0.00017515403,0.00013230754,0.0003326921,0.00016944032,0.00032928513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009155951,0.000032164815,0.947534,0.000044989854,0.00007056081,0.00012814814,0.00050519063,0.0038174528,0.017537698,0.00010833247,0.000526253,0.029603595],"study_design_scores_gemma":[0.0000013324192,0.0000041118815,0.99748224,0.00000308785,0.0000038576527,0.000016366988,0.00010666675,0.001963713,0.0002004921,0.000012468079,0.00020255543,0.0000031233817],"about_ca_topic_score_codex":0.41433614,"about_ca_topic_score_gemma":0.60367256,"teacher_disagreement_score":0.58566386,"about_ca_system_score_codex":0.0008954766,"about_ca_system_score_gemma":0.0006252865,"threshold_uncertainty_score":0.82384884},"labels":[],"label_agreement":null},{"id":"W2156721705","doi":"10.1002/2014jb011707","title":"Viscoelastic relaxation following subduction earthquakes and its effects on afterslip determination","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":153,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Viscoelasticity; Geology; Seismology; Subduction; Trench; Rheology; Deformation (meteorology); Geodesy; Tectonics; Physics","score_opus":0.050057334766599515,"score_gpt":0.3268103994822256,"score_spread":0.2767530647156261,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156721705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989478,0.000067877954,0.0005276833,0.00001410739,0.0000021105873,0.000003160291,0.00004558101,0.000020074638,0.00037155388],"genre_scores_gemma":[0.9997677,0.00003317969,0.00008708758,0.000002828025,0.0000011427016,0.0000014031096,0.00004152464,0.0000037569396,0.000061384075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998838,0.000022289172,0.000011905358,0.000030286341,0.000017997329,0.000033751046],"domain_scores_gemma":[0.99829453,0.0007791436,0.00044879803,0.00018097059,0.00016624272,0.00013028424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005631743,0.0004179432,0.00026012765,0.0010347777,0.00022132944,0.00057935156,0.00022910966,0.00025031273,0.0007000253],"category_scores_gemma":[0.0024804731,0.0002342593,0.00036023906,0.0005834083,0.00027586106,0.00050090416,0.0005750256,0.00032419807,0.00015434071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00097138656,0.00023455848,0.7557946,0.00014330931,0.00026652924,0.001319386,0.0007585163,0.064434886,0.12152801,0.00041113602,0.00028357445,0.053854104],"study_design_scores_gemma":[0.000008740544,0.00015467829,0.89221954,0.000020088428,0.00006407854,0.00010361807,0.00025345632,0.09879367,0.007997467,0.00014519875,0.00020968146,0.000029841287],"about_ca_topic_score_codex":0.004562883,"about_ca_topic_score_gemma":0.003946207,"teacher_disagreement_score":0.004562883,"about_ca_system_score_codex":0.00023803211,"about_ca_system_score_gemma":0.00020780085,"threshold_uncertainty_score":0.009072661},"labels":[],"label_agreement":null},{"id":"W2156755756","doi":"10.1144/gsl.sp.2006.268.01.10","title":"Interpretation of deformation fabrics of infrastructure zone rocks in the context of channel flow and other tectonic models","year":2006,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; Western University; University of New Brunswick","funders":"","keywords":"Interpretation (philosophy); Geology; Context (archaeology); Tectonics; Channel (broadcasting); Deformation (meteorology); Flow (mathematics); Petrology; Geotechnical engineering; Seismology; Mechanics; Paleontology; Computer science; Physics; Oceanography","score_opus":0.01381890824432531,"score_gpt":0.20828222836646526,"score_spread":0.19446332012213996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156755756","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97995627,0.00009140504,0.011690265,0.00016746209,0.000015624439,0.000014571443,0.0003280966,0.00023870629,0.0074976403],"genre_scores_gemma":[0.99881387,0.00003530825,0.00081454,0.0000039209995,0.0000052786063,0.0000031840248,0.00004603558,0.000022164035,0.00025574627],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993694,0.000014447112,0.000003841108,0.000013330786,0.000008617522,0.0000229058],"domain_scores_gemma":[0.9998367,0.00004850244,0.000041204414,0.000024268747,0.000019670382,0.000029639958],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022725691,0.00031247994,0.00024462014,0.001342489,0.0002705315,0.0009288835,0.00032801525,0.00037471275,0.0031127466],"category_scores_gemma":[0.0006132702,0.00016142093,0.00036218777,0.00068440125,0.0006306268,0.00044195194,0.0003997516,0.00021770979,0.00017547983],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022247402,0.00008684766,0.10227312,0.000100659956,0.00007991074,0.00052783935,0.00035510332,0.8278509,0.015359965,0.039565027,0.0006762339,0.012901917],"study_design_scores_gemma":[0.000017268969,0.000035027722,0.06554887,0.000013965178,0.000016507576,0.000098765144,0.0001455262,0.92285866,0.0007232641,0.009924829,0.00059621484,0.000021120117],"about_ca_topic_score_codex":0.005496477,"about_ca_topic_score_gemma":0.0033199734,"teacher_disagreement_score":0.005496477,"about_ca_system_score_codex":0.0005898148,"about_ca_system_score_gemma":0.0002582806,"threshold_uncertainty_score":0.010928929},"labels":[],"label_agreement":null},{"id":"W2157055914","doi":"10.1190/tle34060678.1","title":"Geomechanical modeling of induced seismicity resulting from hydraulic fracturing","year":2015,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Induced seismicity; Microseism; Hydraulic fracturing; Seismology; Seismic hazard; Geology; Magnitude (astronomy); Volume (thermodynamics); Geomechanics; Pore water pressure; Geotechnical engineering","score_opus":0.09436505451411219,"score_gpt":0.2624489993192193,"score_spread":0.16808394480510708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157055914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96473163,0.00010496447,0.020708533,0.00035282757,0.000047701087,0.00008231115,0.0009074104,0.00034138013,0.012723118],"genre_scores_gemma":[0.9973258,0.000042718162,0.0010042246,0.000018923125,0.000005774558,0.000026883643,0.00014493299,0.000020081816,0.0014105225],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987614,0.00002557063,0.000010688711,0.000023586688,0.00003096609,0.000032916294],"domain_scores_gemma":[0.99965966,0.00015265535,0.000061836654,0.000027441209,0.000057914694,0.000040462834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027731643,0.00043510244,0.00035021064,0.00065445673,0.00039276638,0.0006804185,0.00078382593,0.0013566163,0.00327961],"category_scores_gemma":[0.0010060377,0.00035165664,0.00051953335,0.00043110948,0.0007445378,0.00048535285,0.00049567176,0.00054347486,0.00026420585],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022227128,0.00004072,0.0018693627,0.000010485323,0.000008088333,0.00008220905,0.00001860014,0.994987,0.0013279237,0.00072587724,0.00009645472,0.00081099995],"study_design_scores_gemma":[0.000005223209,0.00001186644,0.0006295843,0.0000013718924,0.0000022044587,0.000005013104,0.000008403924,0.9989856,0.00014266692,0.00014830456,0.000056836394,0.0000028913876],"about_ca_topic_score_codex":0.02332013,"about_ca_topic_score_gemma":0.013594946,"teacher_disagreement_score":0.02332013,"about_ca_system_score_codex":0.00089774426,"about_ca_system_score_gemma":0.0008295595,"threshold_uncertainty_score":0.046368778},"labels":[],"label_agreement":null},{"id":"W2157778694","doi":"10.1007/s10712-006-9000-9","title":"The Sumatra tsunami of 26 December 2004 as observed in the North Pacific and North Atlantic oceans","year":2006,"lang":"en","type":"article","venue":"Surveys in Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Hydrographic Service; Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration; Russian Foundation for Basic Research","keywords":"Tide gauge; Geology; Oceanography; Pacific ocean; Seismology; Tsunami wave; Indian ocean; Tsunami earthquake; Climatology; Sea level","score_opus":0.019606103495100616,"score_gpt":0.20498380754022782,"score_spread":0.1853777040451272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157778694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99639004,0.00012698755,0.00003305542,0.00012937663,0.000031203534,0.000007415957,0.0010275458,0.000005487199,0.002248843],"genre_scores_gemma":[0.99689204,0.00030742618,0.000083753985,0.000047239842,0.000022461927,0.000013696189,0.0014390025,0.000004368619,0.0011900165],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982125,0.000019361465,0.000023939338,0.000028177321,0.000051620482,0.00005564672],"domain_scores_gemma":[0.9992974,0.00004928496,0.0003325011,0.000034031946,0.0001429336,0.00014386751],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020751753,0.00032077866,0.00030735662,0.0011903498,0.00093446963,0.0009460525,0.00022452016,0.0005025405,0.0018069046],"category_scores_gemma":[0.001488315,0.00020435701,0.00016785717,0.0018204908,0.00052223605,0.000753922,0.0016563116,0.0005678126,0.00044913773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029067486,0.000052632986,0.9765935,0.00009069385,0.000106846666,0.0016059129,0.004645186,0.00079044787,0.004454648,0.00023629626,0.0025288372,0.008604347],"study_design_scores_gemma":[0.0000020036955,0.00001173074,0.99709034,0.000009158522,0.000009585241,0.00010982195,0.0012375294,0.0000869054,0.00006654733,0.00001591498,0.0013562695,0.0000042763077],"about_ca_topic_score_codex":0.06847236,"about_ca_topic_score_gemma":0.19642954,"teacher_disagreement_score":0.06847236,"about_ca_system_score_codex":0.0014576842,"about_ca_system_score_gemma":0.0009908202,"threshold_uncertainty_score":0.13614762},"labels":[],"label_agreement":null},{"id":"W2158300980","doi":"10.5194/npg-10-573-2003","title":"Characteristic scales of earthquake rupture from numerical models","year":2003,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Asperity (geotechnical engineering); Quake (natural phenomenon); Geology; Slip (aerodynamics); Planar; Earthquake rupture; Statistical physics; Mechanics; Fault (geology); Seismology; Physics; Geotechnical engineering; Computer science","score_opus":0.017170518317324995,"score_gpt":0.22391940788855014,"score_spread":0.20674888957122514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158300980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6863199,0.00089829945,0.29245052,0.0005909428,0.000055150496,0.000076517346,0.00040246645,0.00060740835,0.01859886],"genre_scores_gemma":[0.9924696,0.00021928576,0.006494361,0.000028808672,0.000025549612,0.000043950102,0.00014879873,0.00004520003,0.0005244588],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996345,0.00011531711,0.000024659623,0.000055747332,0.00012411592,0.00004552126],"domain_scores_gemma":[0.9956852,0.0029155693,0.0004769735,0.00041913308,0.0003062054,0.00019695528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012917749,0.0004101211,0.0004621148,0.0009532864,0.0003813308,0.0012314949,0.0007429637,0.00078093953,0.0011856373],"category_scores_gemma":[0.013670086,0.00038127627,0.00047536785,0.0006509855,0.0008709062,0.0017589988,0.0009604187,0.0008313468,0.00015012886],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006521045,0.00004118965,0.005055583,0.00008087201,0.00004237283,0.00017943626,0.00017783845,0.9297915,0.0023576827,0.05362485,0.0007361634,0.007847229],"study_design_scores_gemma":[0.000005127267,0.00001186133,0.0012709615,0.000007674378,0.0000063738103,0.00003539741,0.000018127226,0.9773951,0.0003888791,0.020440187,0.0004114502,0.000008816778],"about_ca_topic_score_codex":0.0013575249,"about_ca_topic_score_gemma":0.000681487,"teacher_disagreement_score":0.0013575249,"about_ca_system_score_codex":0.0012637898,"about_ca_system_score_gemma":0.00035191316,"threshold_uncertainty_score":0.0091694},"labels":[],"label_agreement":null},{"id":"W2159243805","doi":"10.1190/1.3627502","title":"Statistical analysis of microseismic event locations and magnitudes, and their geomechanical implications","year":2011,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Microseismic Industry Consortium","keywords":"Geology; Microseism; Seismology; Hypocenter; Induced seismicity; Stress field; Fractal dimension; Slip (aerodynamics); Fractal; Rock mass classification; Geotechnical engineering; Mathematics","score_opus":0.028098155122874963,"score_gpt":0.23323694576051665,"score_spread":0.20513879063764168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159243805","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97810286,0.00023991767,0.018528499,0.00010081236,0.000018297455,0.0000450835,0.0015297262,0.00014246817,0.0012922849],"genre_scores_gemma":[0.9978275,0.00003575233,0.0013172615,0.000006588493,0.000014211317,0.000027900534,0.0006493637,0.000008148623,0.000113366645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989164,0.00027136813,0.00011107163,0.00036861058,0.00025299238,0.0000795138],"domain_scores_gemma":[0.984251,0.011100053,0.0025204138,0.0010576526,0.0007331409,0.000337769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017993624,0.00019962956,0.00031926535,0.0026976718,0.00026877687,0.00051858736,0.0003057728,0.00035956586,0.0013362411],"category_scores_gemma":[0.010871236,0.00011751723,0.00033779693,0.0020072907,0.0009456813,0.0005868554,0.00039776275,0.00040119124,0.00019943302],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043238793,0.000118096454,0.9070708,0.00015388968,0.00046526312,0.00045286087,0.0004957257,0.01589019,0.015005033,0.0034868969,0.0009550854,0.055473823],"study_design_scores_gemma":[0.000005304466,0.00018204722,0.96811163,0.000007475968,0.000034474597,0.00034013283,0.00032142273,0.026276894,0.0012307974,0.0026494754,0.000815503,0.000024902503],"about_ca_topic_score_codex":0.0012129263,"about_ca_topic_score_gemma":0.0011548931,"teacher_disagreement_score":0.0026976718,"about_ca_system_score_codex":0.0003824875,"about_ca_system_score_gemma":0.00022302709,"threshold_uncertainty_score":0.00951606},"labels":[],"label_agreement":null},{"id":"W2159331986","doi":"10.1144/gsl.sp.2004.224.01.13","title":"Geometric and kinematic analysis of a transpression terrane boundary: Minas fault system, Nova Scotia, Canada","year":2004,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Nova scotia; Transpression; Terrane; Geology; Fault (geology); Boundary (topology); Seismology; Geodesy; Oceanography; Mathematics; Tectonics; Sinistral and dextral","score_opus":0.0175051439817654,"score_gpt":0.22037656831678828,"score_spread":0.2028714243350229,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159331986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99028265,0.00009460468,0.0001488183,0.000041449443,0.000003348156,0.000033618584,0.0016066132,0.000020136218,0.007768833],"genre_scores_gemma":[0.9970674,0.00005318472,0.00028125275,0.000008121152,7.487805e-7,0.000007709269,0.0009234877,0.0000060628413,0.0016520103],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981874,0.000005328042,0.0000072218177,0.00004008383,0.000071078575,0.000057520305],"domain_scores_gemma":[0.99962556,0.000020775262,0.000042103282,0.000014214662,0.00024246424,0.00005483898],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007367237,0.00026820422,0.0002411714,0.0022115074,0.0017572824,0.0012553063,0.0005877597,0.00034693643,0.0029610263],"category_scores_gemma":[0.0005142603,0.00023642438,0.00018999456,0.0028028549,0.0008687257,0.00015914344,0.00045838824,0.00019549511,0.00043857348],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032755363,0.000085725136,0.9228755,0.00010774575,0.00006300105,0.002105563,0.0022036405,0.023358881,0.016325932,0.001870562,0.002228987,0.028446909],"study_design_scores_gemma":[0.00000832967,0.000019021454,0.988405,0.00002392843,0.000007952465,0.00013642535,0.0016332035,0.0074051544,0.00057931006,0.00008677166,0.0016800613,0.000014801553],"about_ca_topic_score_codex":0.984791,"about_ca_topic_score_gemma":0.99210393,"teacher_disagreement_score":0.015209019,"about_ca_system_score_codex":0.012327656,"about_ca_system_score_gemma":0.007665559,"threshold_uncertainty_score":0.0894438},"labels":[],"label_agreement":null},{"id":"W2159373594","doi":"10.1144/sp394.1","title":"Post-emplacement thermo-rheological history of a granite intrusion and surrounding rocks: the Monte Capanne pluton, Elba Island, Italy","year":2013,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Pluton; Geology; Intrusion; Geochemistry; Rheology; Petrology; Seismology; Tectonics","score_opus":0.01942767659789823,"score_gpt":0.2050552155158251,"score_spread":0.18562753891792685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159373594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933909,0.00031513578,0.00020561267,0.00015387271,0.0000064627693,0.000013100302,0.00046527793,0.00009128602,0.0053583714],"genre_scores_gemma":[0.99866474,0.00009176338,0.00015831085,0.000009771836,0.0000048105244,0.000004498765,0.00028929522,0.000010647079,0.0007661501],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999534,0.000005256145,0.0000021627968,0.000017450648,0.0000094804445,0.000012186175],"domain_scores_gemma":[0.9999119,0.000008712818,0.0000273741,0.000017348175,0.000015596193,0.000019011677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012888883,0.0003921025,0.00022507722,0.0008872832,0.00049502135,0.0007611513,0.00060173584,0.0007907908,0.0029925571],"category_scores_gemma":[0.0002806936,0.00025302317,0.0003120465,0.000713943,0.00085704523,0.00034116654,0.000560038,0.0003308377,0.00054275524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010829599,0.00020723758,0.82691616,0.00035518015,0.00029571768,0.004302677,0.0020971054,0.07691778,0.05307227,0.0017993227,0.0025592954,0.030394182],"study_design_scores_gemma":[0.000025893127,0.00006158618,0.98668,0.000019022224,0.000023511095,0.0002521378,0.00021010239,0.0090861665,0.0005730776,0.00013965863,0.0029141095,0.000014928991],"about_ca_topic_score_codex":0.058526058,"about_ca_topic_score_gemma":0.04741772,"teacher_disagreement_score":0.058526058,"about_ca_system_score_codex":0.0018996675,"about_ca_system_score_gemma":0.0003315709,"threshold_uncertainty_score":0.1163708},"labels":[],"label_agreement":null},{"id":"W2159736712","doi":"10.34194/geusb.v17.5002","title":"Earthquake in southern Sweden wakes up Denmark on 16 December 2008","year":2009,"lang":"en","type":"article","venue":"Geological Survey of Denmark and Greenland Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; U.S. Geological Survey; Universitetet i Bergen; Helsingin Yliopisto","keywords":"Epicenter; Induced seismicity; Seismology; Geology; Period (music)","score_opus":0.02981944839295923,"score_gpt":0.23153584136665617,"score_spread":0.20171639297369695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159736712","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99308866,0.0010459293,0.000065488326,0.00018858956,0.00007746264,0.00001031108,0.0013730968,0.000025874753,0.0041245343],"genre_scores_gemma":[0.99358976,0.0008858867,0.00016797867,0.00006682016,0.000032955293,0.000011621618,0.002237221,0.000009571615,0.0029983371],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997789,0.000022039856,0.000028420254,0.000037377315,0.00006699777,0.00006633004],"domain_scores_gemma":[0.99971837,0.000024959203,0.000090595044,0.000019802717,0.00006182229,0.00008438518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034491057,0.00028595407,0.00032522832,0.000881539,0.00083521404,0.0009566451,0.00020842154,0.0005134987,0.0008113683],"category_scores_gemma":[0.00068085955,0.00020849986,0.00022647214,0.0006201876,0.0002960446,0.00018820954,0.0015005155,0.00022731499,0.000565283],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008340046,0.000118908385,0.91260195,0.00073324546,0.00018176655,0.010476705,0.008307059,0.001835385,0.007325951,0.0007147729,0.013817353,0.043052897],"study_design_scores_gemma":[0.000026407335,0.000086293345,0.9692384,0.00024104203,0.000037951428,0.00091287086,0.0035915538,0.00018456217,0.00045825835,0.000091609814,0.025115078,0.000016084025],"about_ca_topic_score_codex":0.027555756,"about_ca_topic_score_gemma":0.062091555,"teacher_disagreement_score":0.027555756,"about_ca_system_score_codex":0.000904857,"about_ca_system_score_gemma":0.0011010666,"threshold_uncertainty_score":0.054790735},"labels":[],"label_agreement":null},{"id":"W2159738054","doi":"10.1126/science.1246518","title":"Dangers of Being Thin and Weak","year":2013,"lang":"en","type":"letter","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Trench; Geology; Seismology; Fault (geology); Drilling; Materials science; Engineering; Composite material; Mechanical engineering","score_opus":0.014810886276973894,"score_gpt":0.20687587905527077,"score_spread":0.1920649927782969,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159738054","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009974101,0.0022800982,0.00019805584,0.96787995,0.007003015,0.00001023406,0.000052920343,0.000026711823,0.012574834],"genre_scores_gemma":[0.09468082,0.0038784968,0.0004771194,0.86331886,0.030101435,0.000028951827,0.00006335745,0.0000334013,0.007417554],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990582,0.0002584037,0.00009824965,0.00013596377,0.00025515608,0.00019406866],"domain_scores_gemma":[0.9955348,0.0019282448,0.00047992638,0.00026984763,0.0006733558,0.0011138597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001804061,0.0002548545,0.0005027115,0.0003862458,0.0028264916,0.0017151608,0.00088556943,0.014180463,0.0031293049],"category_scores_gemma":[0.014792105,0.00030126967,0.0003750174,0.00036608367,0.0046847276,0.0026262328,0.0014750318,0.024291707,0.0025054216],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012758977,0.000053973406,0.021387441,0.00009048108,0.000042515872,0.02907577,0.0013802996,0.00015036874,0.0007128776,0.0130897295,0.8756692,0.058219675],"study_design_scores_gemma":[0.000098402255,0.00019955296,0.021659639,0.00061975117,0.000046339414,0.087370805,0.007669882,0.00057851814,0.00063000777,0.051798068,0.8291836,0.0001454782],"about_ca_topic_score_codex":0.004683449,"about_ca_topic_score_gemma":0.014135566,"teacher_disagreement_score":0.014180463,"about_ca_system_score_codex":0.0017790231,"about_ca_system_score_gemma":0.0014932425,"threshold_uncertainty_score":0.012907743},"labels":[],"label_agreement":null},{"id":"W2159827817","doi":"10.1190/geo2014-0382.1","title":"Regional seismicity: A potential pitfall for identification of long-period long-duration events","year":2014,"lang":"en","type":"article","venue":"Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Calgary","funders":"","keywords":"Seismology; Induced seismicity; Geology; Geophone; Stress field; Duration (music); Hydraulic fracturing; Geotechnical engineering; Engineering; Physics; Structural engineering; Acoustics","score_opus":0.013661390999692834,"score_gpt":0.2176544589518532,"score_spread":0.20399306795216038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159827817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.915981,0.0035523616,0.06136171,0.0016313846,0.00022664733,0.00023722643,0.0017311589,0.00075859996,0.01451994],"genre_scores_gemma":[0.985994,0.0003399546,0.012604873,0.00027959904,0.00006471247,0.000036842983,0.00023620932,0.00007060416,0.00037316632],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99797314,0.0009073939,0.00030184205,0.0003431069,0.0003463304,0.00012817062],"domain_scores_gemma":[0.97910196,0.009517224,0.0037388422,0.003179859,0.003693677,0.0007685006],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006023242,0.00048611476,0.00062949426,0.0018977842,0.00044210278,0.0011668924,0.0011432944,0.00077485805,0.0011185644],"category_scores_gemma":[0.029915815,0.0002269715,0.00022195201,0.001632137,0.0007870582,0.0012039175,0.0010103836,0.0006350284,0.00065847335],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008301595,0.000049329257,0.76746476,0.00087631284,0.00022277578,0.0020940895,0.002973803,0.0027540599,0.061531052,0.0016698993,0.002997257,0.1565364],"study_design_scores_gemma":[0.000021553917,0.00023013921,0.965976,0.00029133717,0.00008926134,0.0039169993,0.0025214804,0.010213953,0.007688342,0.0019635558,0.007043381,0.000044097564],"about_ca_topic_score_codex":0.0077521983,"about_ca_topic_score_gemma":0.02020384,"teacher_disagreement_score":0.0077521983,"about_ca_system_score_codex":0.00037654652,"about_ca_system_score_gemma":0.0004272146,"threshold_uncertainty_score":0.03185433},"labels":[],"label_agreement":null},{"id":"W2160196589","doi":"10.1007/s11001-006-9007-0","title":"First results from the North Iceland experiment","year":2006,"lang":"en","type":"article","venue":"Marine Geophysical Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft; McMaster University","keywords":"Geology; Lineament; Seismology; Crust; Ridge; Induced seismicity; Submarine pipeline; Fracture zone; Tectonics; Oceanic crust; Transform fault; Plate tectonics; Mid-ocean ridge; Bathymetry; Extensional definition; Subduction; Geophysics; Paleontology; Oceanography","score_opus":0.04156986967170748,"score_gpt":0.2776072523881727,"score_spread":0.2360373827164652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160196589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8762126,0.0010867132,0.0015143788,0.005465296,0.00039048409,0.00022245146,0.05379201,0.00016711846,0.06114902],"genre_scores_gemma":[0.9265287,0.0009152317,0.0019741724,0.0014102882,0.00019418287,0.00048570335,0.03863263,0.00022476896,0.029634403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9986664,0.00051090104,0.00005426196,0.00018350895,0.00041879897,0.00016603651],"domain_scores_gemma":[0.9882858,0.0049064793,0.0012389207,0.0023833474,0.0018266528,0.0013588143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005328891,0.000609804,0.00063264894,0.0005754368,0.0013333941,0.0015456959,0.00067992584,0.00076983415,0.0066234823],"category_scores_gemma":[0.00899237,0.00024805006,0.00041226583,0.0008685531,0.0009494727,0.0010363059,0.0013047403,0.0008314581,0.0015610668],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.014475477,0.0054485598,0.6767961,0.0004943036,0.0011806599,0.0006744895,0.0063561117,0.007497985,0.004546847,0.009787874,0.2045023,0.0682393],"study_design_scores_gemma":[0.00031725358,0.00029038647,0.9546753,0.000052731066,0.00019552714,0.00006636179,0.0018353411,0.00066243735,0.0018498065,0.002075567,0.0379424,0.00003683687],"about_ca_topic_score_codex":0.12354528,"about_ca_topic_score_gemma":0.2303247,"teacher_disagreement_score":0.12354528,"about_ca_system_score_codex":0.0022579536,"about_ca_system_score_gemma":0.0019715559,"threshold_uncertainty_score":0.24565238},"labels":[],"label_agreement":null},{"id":"W2160772685","doi":"10.1139/e05-108","title":"Reservoir-induced earthquakes at Sainte-Marguerite-3, Quebec, Canada","year":2006,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Collège de Maisonneuve; Hydro-Québec; Natural Resources Canada","funders":"Natural Resources Canada; Hydro-Québec","keywords":"Geology; Seismometer; Seismology; Magnitude (astronomy); Induced seismicity; Seismic zone","score_opus":0.020022620956771715,"score_gpt":0.20127193416369493,"score_spread":0.18124931320692322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160772685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847761,0.00026441578,0.0003911423,0.00033643635,0.000013926843,0.00008265499,0.0037386292,0.00006832053,0.010328418],"genre_scores_gemma":[0.9926845,0.00020413948,0.0003788268,0.000057462956,0.000004756975,0.000015252922,0.0013867525,0.000008978727,0.005259432],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998447,0.000009058373,0.0000041161834,0.000019747638,0.00006455112,0.0000577085],"domain_scores_gemma":[0.99942374,0.000033567096,0.000061820116,0.000011064566,0.00034851185,0.00012138342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001527494,0.0002519541,0.00015744241,0.00069452357,0.0018287402,0.00048737047,0.00059061695,0.00027185093,0.0023999573],"category_scores_gemma":[0.00049918925,0.00012357462,0.00012440448,0.0009347305,0.00028301452,0.00015367035,0.00037058315,0.0002734913,0.00020478458],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046993484,0.0002761315,0.8616949,0.0002019836,0.0001416841,0.003011966,0.0035642174,0.006867507,0.01908663,0.00094626425,0.02291295,0.080825776],"study_design_scores_gemma":[0.000012180201,0.00003680969,0.9937425,0.000015049437,0.00000738101,0.00008635611,0.0006913132,0.0016354957,0.00047101986,0.000022498652,0.0032651837,0.000014130412],"about_ca_topic_score_codex":0.9901007,"about_ca_topic_score_gemma":0.9981845,"teacher_disagreement_score":0.012742512,"about_ca_system_score_codex":0.012742512,"about_ca_system_score_gemma":0.0121244695,"threshold_uncertainty_score":0.09245378},"labels":[],"label_agreement":null},{"id":"W2160923948","doi":"10.1146/annurev.earth.35.031306.140302","title":"Long-Term Perspectives on Giant Earthquakes and Tsunamis at Subduction Zones","year":2007,"lang":"en","type":"article","venue":"Annual Review of Earth and Planetary Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":279,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Paleoseismology; Tsunami earthquake; Fault (geology); Remotely triggered earthquakes; San andreas fault; Natural (archaeology); Term (time); Seismic gap; Tectonics; Paleontology","score_opus":0.01641827407565303,"score_gpt":0.2523630532534379,"score_spread":0.23594477917778486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160923948","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3478792,0.48971742,0.0036993541,0.05315909,0.0016928135,0.000015582544,0.0017646427,0.00004892104,0.10202295],"genre_scores_gemma":[0.8408549,0.14568397,0.00075023226,0.001599856,0.003635771,0.0000149541665,0.00072648807,0.000010775664,0.0067231315],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996277,0.00018248748,0.000028603723,0.000040821804,0.00006757802,0.00005283374],"domain_scores_gemma":[0.9956814,0.001968395,0.0006708096,0.00018922117,0.00093250006,0.00055759196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00190666,0.00030148946,0.00023435784,0.0025078347,0.0008567464,0.0029185005,0.00044361176,0.0007968449,0.0036288681],"category_scores_gemma":[0.003995867,0.00011117479,0.00016619718,0.0021837293,0.002004061,0.004027697,0.00097029447,0.00088764133,0.0005607137],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008953244,0.00020547304,0.23542173,0.0016977638,0.00021527229,0.00269495,0.013014906,0.0025464613,0.0049810293,0.13020898,0.026658056,0.5814601],"study_design_scores_gemma":[0.000028221482,0.0006375528,0.5667332,0.0018781248,0.00022398529,0.002704221,0.021852624,0.0012096809,0.0017183665,0.11038345,0.29249474,0.00013575022],"about_ca_topic_score_codex":0.003194564,"about_ca_topic_score_gemma":0.011105772,"teacher_disagreement_score":0.0036288681,"about_ca_system_score_codex":0.0012309315,"about_ca_system_score_gemma":0.00049189647,"threshold_uncertainty_score":0.012139797},"labels":[],"label_agreement":null},{"id":"W2160991068","doi":"10.1002/2014gc005360","title":"Consolidation state of incoming sediments to the Nankai Trough subduction zone: Implications for sediment deformation and properties","year":2014,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Geology; Subduction; Pore water pressure; Consolidation (business); Tectonics; Trough (economics); Geochemistry; Seismology; Petrology; Geomorphology; Geotechnical engineering","score_opus":0.015186708782582041,"score_gpt":0.21195281397832888,"score_spread":0.19676610519574683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160991068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997743,0.000013066556,0.000039252922,0.0000026795556,2.8599868e-7,0.0000019813697,0.000028446857,0.000003906598,0.00013611393],"genre_scores_gemma":[0.99974114,0.000021212434,0.00006258128,0.0000034266654,9.172922e-7,0.0000027626959,0.00008043578,0.0000019780603,0.00008542434],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988675,0.000012199619,0.000013439701,0.000027687973,0.000031708867,0.00002820799],"domain_scores_gemma":[0.9995197,0.000042197462,0.00018189821,0.00002913426,0.00013410045,0.000092959206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002204539,0.00036290358,0.0002743419,0.0009793657,0.0003887589,0.00075747265,0.00027462168,0.00020320366,0.0010373895],"category_scores_gemma":[0.0005380443,0.00025991644,0.00017187299,0.0010332543,0.0005635593,0.0003236993,0.00045813163,0.00022707715,0.00015832538],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001222712,0.000041067502,0.91911054,0.000033658907,0.000032654334,0.000299857,0.00041624767,0.0007670112,0.07441765,0.000033359986,0.000023906148,0.0047017224],"study_design_scores_gemma":[0.0000014912124,0.000036918158,0.9976198,0.0000017750382,0.0000039625293,0.0000277384,0.00022410294,0.00031966995,0.0017162564,0.000005064847,0.000041570318,0.0000016708719],"about_ca_topic_score_codex":0.013543319,"about_ca_topic_score_gemma":0.015686478,"teacher_disagreement_score":0.013543319,"about_ca_system_score_codex":0.00046379684,"about_ca_system_score_gemma":0.00027920745,"threshold_uncertainty_score":0.026928961},"labels":[],"label_agreement":null},{"id":"W2161544177","doi":"10.1111/j.1365-246x.2005.02605.x","title":"New constraints on subduction zone structure in northern Cascadia","year":2005,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of British Columbia","funders":"","keywords":"Geology; Seismology; Subduction; Induced seismicity; Mantle (geology); Oceanic crust; Crust; North American Plate; Plate tectonics; Geophysics; Tectonics","score_opus":0.0099525793778615,"score_gpt":0.22467749658768815,"score_spread":0.21472491720982664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161544177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99741626,0.00008537757,0.00006890304,0.000031230666,8.891097e-7,0.0000028243724,0.00017782525,0.000014651233,0.0022020394],"genre_scores_gemma":[0.9992341,0.00005662554,0.00007409808,0.000006503562,8.115993e-7,0.0000045552238,0.00033414824,0.000004162954,0.00028508613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981016,0.000017769185,0.00001704897,0.00006912469,0.00003963535,0.00004626627],"domain_scores_gemma":[0.99941564,0.00010032706,0.00014082086,0.00006932275,0.00012905501,0.00014487177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021651183,0.0003738138,0.00039993474,0.0015884088,0.0011183514,0.0011718805,0.00035982014,0.00022898451,0.0025333792],"category_scores_gemma":[0.001252761,0.00035294832,0.00021390754,0.0014859658,0.0006799887,0.00027969584,0.0010910538,0.0002835371,0.00027980466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020163842,0.00002319,0.96339047,0.00006813385,0.000060822997,0.0003736396,0.0024730433,0.0015336612,0.023273017,0.0004009596,0.00019196852,0.00800938],"study_design_scores_gemma":[0.0000040087943,0.000007971642,0.99837744,0.0000086951995,0.000008158062,0.000033976467,0.00062781706,0.00025281106,0.00014919849,0.00007131869,0.00045409487,0.0000045681822],"about_ca_topic_score_codex":0.30898547,"about_ca_topic_score_gemma":0.58634245,"teacher_disagreement_score":0.30898547,"about_ca_system_score_codex":0.0019452735,"about_ca_system_score_gemma":0.0012214774,"threshold_uncertainty_score":0.6143739},"labels":[],"label_agreement":null},{"id":"W2162631429","doi":"10.1130/g32271.1","title":"Kinematics of a diffuse North America–Pacific–Bering plate boundary in Alaska and western Canada","year":2011,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"American Chemical Society Petroleum Research Fund","keywords":"Citation; Icon; Geology; Library science; Archaeology; Oceanography; Geography; Computer science","score_opus":0.01526265709499875,"score_gpt":0.18026995453200972,"score_spread":0.16500729743701098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162631429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9702359,0.000597054,0.00046487316,0.00031740437,0.000038482318,0.000033943204,0.00063272263,0.0000499235,0.027629681],"genre_scores_gemma":[0.9964372,0.00020195993,0.00034571413,0.0000183713,0.0000026732746,0.0000068771856,0.00028363388,0.000009665569,0.002693868],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998301,0.00000845286,0.0000070302112,0.000035466914,0.0000698055,0.00004910325],"domain_scores_gemma":[0.999696,0.000013940576,0.00004211701,0.000006905246,0.0001419902,0.00009920476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001661197,0.00029272158,0.0002802719,0.0011488282,0.0023944322,0.0012543466,0.00040012214,0.0006522185,0.0045325113],"category_scores_gemma":[0.00084092584,0.0002652748,0.0002065995,0.0009808742,0.0010965493,0.00045664443,0.0017393461,0.00048665976,0.00065664685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00077769754,0.00013181394,0.8696342,0.0002585657,0.00022640664,0.0019457202,0.0081024645,0.03633786,0.019693017,0.007371133,0.008817558,0.046703625],"study_design_scores_gemma":[0.000030833668,0.000044247212,0.98347604,0.00009595006,0.000035171204,0.00010242674,0.005580172,0.0052677128,0.00055570574,0.0006389678,0.0041337465,0.000039027847],"about_ca_topic_score_codex":0.9012749,"about_ca_topic_score_gemma":0.9487635,"teacher_disagreement_score":0.09872508,"about_ca_system_score_codex":0.0062669977,"about_ca_system_score_gemma":0.0077181207,"threshold_uncertainty_score":0.19861293},"labels":[],"label_agreement":null},{"id":"W2162981629","doi":"10.1002/2013jb010834","title":"Controls on spatial and temporal evolution of prism faulting and relationships to plate boundary slip offshore north‐central Sumatra","year":2014,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Bundesministerium für Bildung und Forschung; Natural Environment Research Council; University of Southampton; Sight Research UK","keywords":"Geology; Seismology; Forearc; Submarine pipeline; Slip (aerodynamics); Fault (geology); Accretionary wedge; Strike-slip tectonics; Plate tectonics; Ridge; Subduction; Tectonics; Paleontology","score_opus":0.03821904790724438,"score_gpt":0.29269940779125353,"score_spread":0.25448035988400913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162981629","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994393,0.000020517946,0.000025310297,0.000012689307,8.091875e-7,8.6407334e-7,0.00009146353,0.000002517696,0.00040650225],"genre_scores_gemma":[0.9997161,0.00002055928,0.00002290249,0.0000029889895,7.6378905e-7,0.0000018959752,0.00007693679,0.00000163617,0.00015620592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998816,0.000024157933,0.000010125746,0.000043793956,0.000013991664,0.00002634672],"domain_scores_gemma":[0.9993824,0.00014885639,0.0002405817,0.0000482288,0.00008214596,0.000097831355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021473206,0.00016895325,0.00016229988,0.00072318746,0.00022588429,0.00062512263,0.00018720762,0.00017654587,0.0023124162],"category_scores_gemma":[0.0010569688,0.00018296053,0.00011338089,0.0006236124,0.00048287827,0.00029258765,0.0004906413,0.00019867838,0.00024778294],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000333543,0.00007615528,0.93148446,0.00005721735,0.00009036886,0.000730563,0.0014314463,0.0027650697,0.05065987,0.00032078516,0.00021536405,0.011835194],"study_design_scores_gemma":[0.0000015547014,0.0000075468324,0.99913305,0.000002211527,0.0000033218844,0.00003089389,0.00023200114,0.00031620867,0.0001664149,0.000019961268,0.00008504531,0.0000017741977],"about_ca_topic_score_codex":0.015547384,"about_ca_topic_score_gemma":0.032474313,"teacher_disagreement_score":0.015547384,"about_ca_system_score_codex":0.0005634307,"about_ca_system_score_gemma":0.00020891875,"threshold_uncertainty_score":0.03091377},"labels":[],"label_agreement":null},{"id":"W2162992360","doi":"10.1111/j.1365-246x.2008.03932.x","title":"The postseismic response to the 2002<i>M</i>7.9 Denali Fault earthquake: constraints from InSAR 2003-2005","year":2009,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Crust; Seismology; Interferometric synthetic aperture radar; Mantle (geology); Viscoelasticity; Geodesy; Amplitude; North Anatolian Fault; Geophysics; Fault (geology); Synthetic aperture radar; Remote sensing; Physics","score_opus":0.010806154187622085,"score_gpt":0.23652885148758573,"score_spread":0.22572269729996364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162992360","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98152816,0.00031350958,0.0007951146,0.00027760473,0.000019951602,0.000019288687,0.009744397,0.00011170833,0.007190123],"genre_scores_gemma":[0.98157585,0.00020416881,0.0015354756,0.00009610438,0.000025905738,0.000015627742,0.015674274,0.0000461973,0.0008263186],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99957067,0.00003400614,0.0000401003,0.00011110782,0.00011619108,0.00012787114],"domain_scores_gemma":[0.9991831,0.000060161485,0.00022969385,0.00011199243,0.00030895218,0.000106098654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049078086,0.0007786623,0.00053796126,0.0011834702,0.000808632,0.001549466,0.000758853,0.0005120268,0.001450365],"category_scores_gemma":[0.0012383265,0.00047863752,0.00038137386,0.0016561033,0.0002773918,0.00039577924,0.0004999833,0.00045484412,0.0007000847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060369045,0.00034531477,0.8928977,0.00021245211,0.0003777292,0.0006320572,0.0006785759,0.018964443,0.041512746,0.0012446949,0.009110452,0.033420082],"study_design_scores_gemma":[0.000013521201,0.00001983748,0.9852175,0.000021257903,0.000048541824,0.000066515044,0.00020904644,0.0071732127,0.00222409,0.000075740565,0.004903446,0.000027291055],"about_ca_topic_score_codex":0.40629178,"about_ca_topic_score_gemma":0.64527,"teacher_disagreement_score":0.40629178,"about_ca_system_score_codex":0.002101862,"about_ca_system_score_gemma":0.0015397201,"threshold_uncertainty_score":0.8078538},"labels":[],"label_agreement":null},{"id":"W2163323499","doi":"10.5047/eps.2013.02.006","title":"Spatial distribution of seismicity parameters in the Persian Plateau","year":2013,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research","keywords":"Geology; Seismology; Induced seismicity; Crust; Tectonics; Plateau (mathematics); Attenuation; Geodynamics; Slip (aerodynamics); Stress field; Geophysics","score_opus":0.011636529920775312,"score_gpt":0.18735294823984744,"score_spread":0.17571641831907212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163323499","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983182,0.00009513244,0.00027994943,0.000020542833,0.0000012067742,0.0000026815694,0.00030154214,0.00003213331,0.00094867655],"genre_scores_gemma":[0.9994773,0.000029925095,0.00013855632,0.0000015398352,0.0000017566598,0.0000019413246,0.00025370988,0.000001769428,0.00009353719],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999256,0.000013948951,0.000004802526,0.000025677367,0.000013843687,0.000016193586],"domain_scores_gemma":[0.9996505,0.00007470387,0.00010253951,0.000028855235,0.000105872685,0.00003766944],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016518353,0.00016501965,0.0000870539,0.0017690656,0.000109313485,0.00030135238,0.00012305418,0.00011173478,0.0007137549],"category_scores_gemma":[0.0006574785,0.000068891255,0.00006216042,0.0017589444,0.00026882684,0.0001958171,0.0002034549,0.0000820157,0.00013243541],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000104727456,0.000014670595,0.9596687,0.000021902068,0.000046137662,0.00024259489,0.000667719,0.0040912363,0.0068148756,0.0005404572,0.00049844506,0.027288465],"study_design_scores_gemma":[0.0000032082912,0.000013377445,0.99588734,0.000004443571,0.0000054898146,0.000101646525,0.00050972425,0.0022228179,0.0003751912,0.00012054292,0.0007511861,0.000004970431],"about_ca_topic_score_codex":0.013051669,"about_ca_topic_score_gemma":0.010582759,"teacher_disagreement_score":0.013051669,"about_ca_system_score_codex":0.00025657602,"about_ca_system_score_gemma":0.00018698891,"threshold_uncertainty_score":0.025951385},"labels":[],"label_agreement":null},{"id":"W2163689531","doi":"10.1130/g34901.1","title":"Biomarkers heat up during earthquakes: New evidence of seismic slip in the rock record","year":2014,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Observatory; ROWE; Columbia university; Geology; Library science; Archaeology; Art history; History; Media studies; Sociology; Computer science; Management; Astronomy","score_opus":0.0243158368409191,"score_gpt":0.2313541413194242,"score_spread":0.2070383044785051,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163689531","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998044,0.0004278382,0.00041539478,0.000026390253,0.000006509,0.0000037111968,0.00038286194,0.000014743077,0.00067857525],"genre_scores_gemma":[0.99889356,0.00015586082,0.0005097447,0.0000114409,0.000012027146,0.000004503101,0.00026877585,0.00000420425,0.00013986164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982256,0.000026263235,0.000023516137,0.000051109244,0.00005474892,0.000021932183],"domain_scores_gemma":[0.9988205,0.00017169223,0.0006238235,0.00008620622,0.00020766817,0.00009015263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033920154,0.00017689705,0.00018009548,0.0016336628,0.00024060685,0.00037088429,0.00022306708,0.00040805596,0.0004904615],"category_scores_gemma":[0.0011692484,0.00016994223,0.000099259625,0.0015399021,0.00051278964,0.0004644529,0.00048782342,0.00024860573,0.00015676576],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009822341,0.0000129178925,0.9602746,0.000057939385,0.000038836275,0.0001273503,0.0007627295,0.00016555352,0.029942434,0.00007092439,0.00008965025,0.008358928],"study_design_scores_gemma":[0.0000011368098,0.000028258468,0.998024,0.000005878838,0.000012874945,0.000102143305,0.00014225759,0.00013480088,0.0011475764,0.000028903392,0.00036937714,0.0000028206168],"about_ca_topic_score_codex":0.0034563604,"about_ca_topic_score_gemma":0.007923576,"teacher_disagreement_score":0.0034563604,"about_ca_system_score_codex":0.0001929328,"about_ca_system_score_gemma":0.00014684208,"threshold_uncertainty_score":0.006872475},"labels":[],"label_agreement":null},{"id":"W2164380198","doi":"10.1016/j.jsg.2009.08.004","title":"Strain analysis and rheology contrasts in polymictic conglomerates: An example from the Seine metaconglomerates, Superior Province, Canada","year":2009,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Rheology; Strain (injury); Conglomerate; Paleontology; Thermodynamics; Biology; Physics","score_opus":0.011655482113482237,"score_gpt":0.2094180938307298,"score_spread":0.19776261171724754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164380198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961815,0.00014081631,0.000087041655,0.00005420489,0.0000013975618,0.0000072878042,0.0006400965,0.000006510107,0.0028812408],"genre_scores_gemma":[0.9987581,0.00008022414,0.00013211167,0.0000117901645,8.331384e-7,0.000001926045,0.0002626886,0.0000050774775,0.00074728427],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998066,0.000015372938,0.000010282862,0.000037152076,0.000056992896,0.00007366403],"domain_scores_gemma":[0.99955827,0.000037039386,0.000043151063,0.000018114551,0.00028344846,0.000059928057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016362299,0.00028018694,0.00034929405,0.0020362893,0.0027761871,0.0012593636,0.00060983363,0.00031395178,0.0016698843],"category_scores_gemma":[0.0008134317,0.00018490264,0.0001947004,0.0045372793,0.0010850539,0.00025890363,0.00054364535,0.00034906837,0.0002652164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030653656,0.000054135206,0.9432448,0.00006577741,0.00014943788,0.0014626198,0.010956553,0.00152927,0.009743822,0.0010820213,0.001261412,0.030143756],"study_design_scores_gemma":[0.0000036425504,0.0000076762935,0.9951042,0.000008245819,0.000019561936,0.00012338435,0.0029071525,0.0004504616,0.0003171685,0.000038715792,0.0010109453,0.0000088977895],"about_ca_topic_score_codex":0.9875537,"about_ca_topic_score_gemma":0.99602205,"teacher_disagreement_score":0.012446284,"about_ca_system_score_codex":0.008544113,"about_ca_system_score_gemma":0.005463564,"threshold_uncertainty_score":0.061992228},"labels":[],"label_agreement":null},{"id":"W2165208851","doi":"10.1130/b30187.1","title":"A record of ancient cataclysm in modern sand: Shock microstructures in detrital minerals from the Vaal River, Vredefort Dome, South Africa","year":2010,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Academy of Sciences; Geological Society of America; National Science Foundation","keywords":"Dome (geology); Citation; Icon; Geology; Archaeology; Biogeosciences; History; Paleontology; Library science; Earth science; Computer science","score_opus":0.0120626491060626,"score_gpt":0.1989046852004535,"score_spread":0.1868420360943909,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165208851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992812,0.000114682916,0.00006744098,0.000007587437,7.936992e-7,0.0000024421208,0.00013152625,0.0000038702674,0.00039045457],"genre_scores_gemma":[0.9994198,0.00007944409,0.00018166284,0.0000051278607,0.0000012881528,0.0000019528627,0.00009565439,0.0000022755892,0.00021283672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992764,0.0000042161355,0.000005783955,0.000026261336,0.000017493187,0.000018496074],"domain_scores_gemma":[0.99987125,0.000016696444,0.000044145105,0.000010196943,0.00003821814,0.00001951772],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007765465,0.0001760102,0.00015153558,0.0014211744,0.0005560205,0.00057870866,0.00023134494,0.00025832123,0.00072477706],"category_scores_gemma":[0.00028452202,0.00021217101,0.00012284116,0.001027893,0.0005209178,0.0002482611,0.00040762944,0.0001298201,0.00014166953],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001968417,0.000020538995,0.8228883,0.00009162558,0.00006365036,0.0012543454,0.0036314297,0.00022282294,0.15574972,0.00012183346,0.00009297541,0.01566595],"study_design_scores_gemma":[0.0000012613087,0.00001671174,0.9976682,0.0000054341235,0.000007018878,0.00026922757,0.00048854953,0.00006889153,0.0010058123,0.000008677141,0.00045770605,0.0000024856772],"about_ca_topic_score_codex":0.02823009,"about_ca_topic_score_gemma":0.07042657,"teacher_disagreement_score":0.02823009,"about_ca_system_score_codex":0.0004570207,"about_ca_system_score_gemma":0.00020540097,"threshold_uncertainty_score":0.05613154},"labels":[],"label_agreement":null},{"id":"W2165222578","doi":"10.1306/c9ebce73-1735-11d7-8645000102c1865d","title":"Active Normal Faulting Beneath a Salt Layer: An Experimental Study of Deformation Patterns in the Cover Sequence","year":2000,"lang":"en","type":"article","venue":"AAPG Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":285,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Cover (algebra); Deformation (meteorology); Sequence (biology); Layer (electronics); Seismology; Oceanography; Composite material; Genetics","score_opus":0.028223128542030688,"score_gpt":0.2569901892620809,"score_spread":0.2287670607200502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165222578","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995666,0.000009720433,0.00021217098,0.00000399735,0.0000021023093,0.000004454181,0.000035275905,0.000004763751,0.0001608457],"genre_scores_gemma":[0.9990841,0.000029186958,0.00035984465,0.000003547181,0.0000020004127,0.000013723844,0.00010598661,0.00000488697,0.00039669854],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99987936,0.000014236072,0.000008502028,0.000026930638,0.000028245468,0.000042772273],"domain_scores_gemma":[0.9997434,0.00007230476,0.000049384464,0.00006211775,0.000031970412,0.000040845727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017405953,0.0002681968,0.00020652937,0.00024089582,0.00035039417,0.00024800937,0.00026558354,0.00027300155,0.0012751598],"category_scores_gemma":[0.00039369942,0.00020894782,0.00022297607,0.00020013766,0.0005298869,0.00026991268,0.00031588532,0.00037401164,0.0001264431],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019595628,0.0025848264,0.018115554,0.00006782975,0.000041828727,0.00024740797,0.0004501264,0.011761088,0.95559376,0.00057393167,0.00017109833,0.00843306],"study_design_scores_gemma":[0.00043001774,0.01585341,0.11366784,0.000022487366,0.000117281204,0.00038712044,0.0005656777,0.094258904,0.7723568,0.0005843282,0.001699021,0.000057082463],"about_ca_topic_score_codex":0.0041818945,"about_ca_topic_score_gemma":0.005287184,"teacher_disagreement_score":0.0041818945,"about_ca_system_score_codex":0.00044544553,"about_ca_system_score_gemma":0.0001744603,"threshold_uncertainty_score":0.008315086},"labels":[],"label_agreement":null},{"id":"W2165746018","doi":"10.1130/0016-7606(2001)113<0855:qfhatd>2.0.co;2","title":"Quaternary faulting history along the Deep Springs fault, California","year":2001,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University; University of Arizona; Central Washington University; National Science Foundation","keywords":"Geological survey; Geology; Citation; Library science; Archaeology; History; Paleontology","score_opus":0.0175019219903224,"score_gpt":0.20232301474820744,"score_spread":0.18482109275788502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165746018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94819635,0.0025800234,0.000117340016,0.00078652427,0.000051252227,0.000011899289,0.0036713195,0.000037504302,0.044547804],"genre_scores_gemma":[0.99066293,0.0010860066,0.00012594726,0.000033674245,0.00002011103,0.000003511243,0.0015230952,0.000006044257,0.0065386896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998964,0.000005774086,0.000009477734,0.000022484377,0.000041772324,0.000024017747],"domain_scores_gemma":[0.9995078,0.000038367456,0.000127377,0.000022257875,0.0002242001,0.00007994848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015903437,0.00007288352,0.00013339304,0.0012840624,0.0011526726,0.0007741392,0.00019777249,0.00015932125,0.0033490958],"category_scores_gemma":[0.00070795097,0.000098220706,0.000068191956,0.0021368067,0.00039013755,0.00045321445,0.00043394286,0.00024040736,0.0002386871],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023645833,0.00006029472,0.803458,0.0002558944,0.000057347537,0.00060673314,0.007056263,0.0021001769,0.0017963491,0.008462862,0.04437628,0.13153338],"study_design_scores_gemma":[0.000009359178,0.000026140297,0.9620612,0.000041535557,0.000012427355,0.00006650784,0.00077872677,0.00014091408,0.00012346865,0.00025463058,0.036478218,0.0000067434135],"about_ca_topic_score_codex":0.28649577,"about_ca_topic_score_gemma":0.5371225,"teacher_disagreement_score":0.28649577,"about_ca_system_score_codex":0.0018996972,"about_ca_system_score_gemma":0.0015747149,"threshold_uncertainty_score":0.5696564},"labels":[],"label_agreement":null},{"id":"W2166058418","doi":"10.1130/b25228.1","title":"Controls on caldera structure: Results from analogue sandbox modeling","year":2004,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Université du Québec à Montréal; Natural Sciences and Engineering Research Council of Canada; McGill University; National Science Foundation","keywords":"Library science; Sandbox (software development); Art history; Computer science; History","score_opus":0.018369072317795082,"score_gpt":0.20794006980251567,"score_spread":0.1895709974847206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166058418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9095589,0.0010539725,0.041756827,0.00066154986,0.00012937006,0.00012398213,0.0016673638,0.0012385302,0.04380947],"genre_scores_gemma":[0.9933861,0.00014214622,0.004045953,0.00005391744,0.000026310961,0.000026696845,0.00038346808,0.00018474816,0.0017507385],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993025,0.00026606923,0.00003665393,0.00015853588,0.00015238588,0.00008383665],"domain_scores_gemma":[0.9899395,0.007852117,0.00051910034,0.0008495236,0.0005570963,0.0002826116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017032794,0.0008377012,0.0013573135,0.00091844384,0.0007756186,0.0017403415,0.0020478268,0.0013760731,0.007766773],"category_scores_gemma":[0.010464987,0.0005659531,0.0013134824,0.0008625613,0.0010287468,0.0019613001,0.00096632424,0.001182838,0.00050262053],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015633443,0.00007810428,0.003701917,0.000045363253,0.000047090176,0.000043302225,0.00005622658,0.98756915,0.00028969822,0.0031375466,0.0007833072,0.0040919054],"study_design_scores_gemma":[0.00004628512,0.000021382224,0.00069150585,0.000004827235,0.000022197448,0.0000066976586,0.000017703458,0.99734384,0.00014199669,0.0013728543,0.00032158988,0.000009226652],"about_ca_topic_score_codex":0.08290857,"about_ca_topic_score_gemma":0.029945964,"teacher_disagreement_score":0.08290857,"about_ca_system_score_codex":0.0017765529,"about_ca_system_score_gemma":0.00078372326,"threshold_uncertainty_score":0.16485196},"labels":[],"label_agreement":null},{"id":"W2166419762","doi":"10.1002/2015gc005794","title":"Multiscale postseismic behavior on a megathrust: The 2012 Nicoya earthquake, Costa Rica","year":2015,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Seismology; Subduction; Trench; Slip (aerodynamics); Tsunami earthquake; Interplate earthquake; Crust; Geodesy; Tectonics; Geophysics","score_opus":0.024504118813059042,"score_gpt":0.22415060661080127,"score_spread":0.19964648779774224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166419762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994159,0.000028109276,0.000097230055,0.000030300474,9.396443e-7,0.000003105462,0.000092737224,0.000010473411,0.000321288],"genre_scores_gemma":[0.99977547,0.000015025639,0.00004924082,0.0000025820134,0.0000014025478,0.000001637324,0.00008242685,0.0000016835261,0.00007042943],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999943,0.000011991894,0.0000024838268,0.000015270321,0.000007953554,0.000019205567],"domain_scores_gemma":[0.9998275,0.000027271006,0.00004089789,0.000026277445,0.000041337622,0.00003668322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001398026,0.00017389299,0.000212274,0.00051687326,0.0002479836,0.00041556885,0.00025731733,0.00026434218,0.00091801165],"category_scores_gemma":[0.0006634924,0.00010396439,0.00017197004,0.00043386986,0.00023799193,0.00021621477,0.00032946412,0.00014525451,0.00009393696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039165397,0.00022573442,0.88131535,0.000062990046,0.00028776756,0.00091737765,0.00066542573,0.0764478,0.02141204,0.00086998777,0.0014133833,0.015990434],"study_design_scores_gemma":[0.000004256861,0.000017217071,0.9451023,0.0000032062892,0.000015030378,0.000023571578,0.00020877179,0.054081287,0.0002756413,0.000058406466,0.00020386637,0.000006490517],"about_ca_topic_score_codex":0.07598607,"about_ca_topic_score_gemma":0.08239914,"teacher_disagreement_score":0.07598607,"about_ca_system_score_codex":0.00077262206,"about_ca_system_score_gemma":0.00023384222,"threshold_uncertainty_score":0.15108758},"labels":[],"label_agreement":null},{"id":"W2167520082","doi":"10.1007/s10950-005-9003-x","title":"Hybrid stochastic finite fault modeling of 2003, M6.5, Bam earthquake (Iran)","year":2006,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Fault (geology); Seismology; Calibration; Strong ground motion; Amplitude; Series (stratigraphy); Geodesy; Mathematics; Physics; Statistics; Ground motion; Optics","score_opus":0.020070233332497293,"score_gpt":0.21887043282314697,"score_spread":0.19880019949064967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167520082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847052,0.00011825546,0.0122115705,0.00027584727,0.000026902986,0.000010415887,0.00034393254,0.0000969299,0.002211023],"genre_scores_gemma":[0.99904007,0.000023140605,0.00046572523,0.000007461858,0.0000046000378,0.000004857464,0.00006999043,0.0000065570603,0.0003774728],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999292,0.000017430964,0.0000042086576,0.0000163085,0.000010006286,0.000022849856],"domain_scores_gemma":[0.9995863,0.00022494548,0.0000660589,0.000016399823,0.00006740563,0.00003886889],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031502277,0.0004453912,0.00069050887,0.00037013687,0.0005174727,0.00064984255,0.0009833464,0.001144148,0.0012285841],"category_scores_gemma":[0.0011311016,0.00042430905,0.000599693,0.00036083008,0.00045373055,0.000560434,0.00035852395,0.00068925676,0.00008714128],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003924976,0.000015914044,0.0018300104,0.0000060592547,0.000011650116,0.000043287375,0.000012642754,0.99664766,0.00017192791,0.00052661845,0.00008673056,0.00060818443],"study_design_scores_gemma":[0.0000053724816,0.000008015318,0.00054758874,6.506952e-7,0.0000037684083,0.0000033191325,0.0000074441136,0.9992483,0.000036156078,0.0001161803,0.000021223826,0.0000020227703],"about_ca_topic_score_codex":0.11025209,"about_ca_topic_score_gemma":0.05202314,"teacher_disagreement_score":0.11025209,"about_ca_system_score_codex":0.0011233189,"about_ca_system_score_gemma":0.0009351421,"threshold_uncertainty_score":0.2192207},"labels":[],"label_agreement":null},{"id":"W2168095091","doi":"10.5194/nhess-13-2863-2013","title":"A wavefront orientation method for precise numerical determination of tsunami travel time","year":2013,"lang":"en","type":"article","venue":"Natural hazards and earth system sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Wavefront; Orientation (vector space); Grid; Point (geometry); Geodesy; Computer science; Travel time; Anisotropy; Geology; Arrival time; Algorithm; Optics; Mathematics; Geometry; Physics; Engineering","score_opus":0.012107777409434726,"score_gpt":0.25624652053020974,"score_spread":0.24413874312077502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168095091","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0022460418,0.000032733584,0.99686015,0.000021912061,0.000024467154,0.000012870433,0.00001885029,0.00019300469,0.0005899855],"genre_scores_gemma":[0.046119135,0.00009892402,0.9520112,0.000025866339,0.000020868996,0.000080684404,0.00006539527,0.00009560981,0.0014823569],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998555,0.00003163665,0.00000518433,0.000016722683,0.00007872818,0.000012171127],"domain_scores_gemma":[0.99970514,0.00009032761,0.00003276286,0.00003218725,0.00012198863,0.00001750857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003208221,0.0004155003,0.0002614225,0.0003997411,0.00031896995,0.00037974172,0.0005457425,0.00038290265,0.00349548],"category_scores_gemma":[0.00086054724,0.00030168612,0.00030014757,0.00036911076,0.00029108353,0.0004964323,0.00043527214,0.00085826125,0.0010698364],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010750323,0.000108013446,0.0023486628,0.00015040742,0.000046108333,0.0001401482,0.00014834311,0.23612408,0.08080613,0.06730515,0.008635725,0.6040798],"study_design_scores_gemma":[0.000027113847,0.000029553476,0.00047867728,0.000008896745,0.0000068943596,0.0000582488,0.000011713818,0.9826193,0.0059698583,0.0033048664,0.0074660103,0.000018894933],"about_ca_topic_score_codex":0.004097796,"about_ca_topic_score_gemma":0.0059333043,"teacher_disagreement_score":0.004097796,"about_ca_system_score_codex":0.0003654038,"about_ca_system_score_gemma":0.0012904751,"threshold_uncertainty_score":0.011693537},"labels":[],"label_agreement":null},{"id":"W2168198514","doi":"10.1007/s00024-006-0099-x","title":"Virtual California: Fault Model, Frictional Parameters, Applications","year":2006,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"U.S. Department of Energy","keywords":"Data assimilation; Probability density function; Probability distribution; Computer science; Statistical physics; Gaussian; Slip (aerodynamics); Algorithm; Mathematics; Meteorology; Physics; Statistics","score_opus":0.008883563190064487,"score_gpt":0.18589644346004502,"score_spread":0.17701288026998055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168198514","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07782129,0.0023039542,0.692468,0.0011921268,0.00049529265,0.00032752458,0.06354586,0.059362583,0.102483355],"genre_scores_gemma":[0.6312561,0.0025162294,0.25130084,0.00015529408,0.00015345658,0.00050320843,0.046151325,0.003920948,0.06404253],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998816,0.00002239325,0.000008061346,0.000034343273,0.000042893527,0.000010625564],"domain_scores_gemma":[0.9997286,0.000035005593,0.00002120315,0.00007063283,0.00010997191,0.000034552293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026113976,0.00076478673,0.00044474442,0.0005944641,0.00034431706,0.0011122471,0.002017581,0.00066766725,0.019594587],"category_scores_gemma":[0.0012170792,0.00045849357,0.00027429927,0.0018687984,0.00021484493,0.0013950339,0.00057870784,0.0005285,0.004500364],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018350613,0.00008572237,0.0038972688,0.00014218183,0.00003356709,0.000067192435,0.000061567465,0.82295924,0.0013065673,0.007664373,0.07430086,0.08929804],"study_design_scores_gemma":[0.00009188517,0.000023675722,0.0013483359,0.000035873487,0.000024060513,0.00004414341,0.000036290225,0.9433217,0.0011390524,0.0041628303,0.049747624,0.000024479277],"about_ca_topic_score_codex":0.1489116,"about_ca_topic_score_gemma":0.12905611,"teacher_disagreement_score":0.1489116,"about_ca_system_score_codex":0.0008169903,"about_ca_system_score_gemma":0.0013682259,"threshold_uncertainty_score":0.29608965},"labels":[],"label_agreement":null},{"id":"W2168199593","doi":"10.1046/j.1365-246x.2002.01722.x","title":"The 1933 M<sub>s</sub>= 7.3 Baffin Bay earthquake: strike-slip faulting along the northeastern Canadian passive margin","year":2002,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Bay; Thrust fault; Moment magnitude scale; Seismogram; Slip (aerodynamics); Strike-slip tectonics; Fault (geology); Oceanography; Geometry","score_opus":0.013713306093997733,"score_gpt":0.2007268958914875,"score_spread":0.18701358979748978,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168199593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99265665,0.00018562675,0.00017243705,0.00016664788,0.0000054497737,0.000018591296,0.0015749731,0.000020671787,0.005198926],"genre_scores_gemma":[0.99609286,0.00024273696,0.00039800032,0.000039630257,0.0000035348817,0.0000057309912,0.0010754226,0.0000044751364,0.0021376046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984884,0.0000042351576,0.0000037245904,0.000013456454,0.000081018174,0.000048681726],"domain_scores_gemma":[0.99980026,0.000007864299,0.000027290114,0.0000052816486,0.00011715184,0.0000421661],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105798674,0.00017698648,0.00015288084,0.00067103445,0.0017340098,0.0004005265,0.00030802164,0.00020756878,0.0020808587],"category_scores_gemma":[0.000542761,0.00009496243,0.00010626448,0.0010626323,0.0004980457,0.00013817172,0.00033640154,0.0001761771,0.00021146456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022966246,0.00005640846,0.8927844,0.00011906009,0.0000563906,0.0009473682,0.0019835546,0.00139339,0.027768876,0.0010897809,0.007889053,0.065682076],"study_design_scores_gemma":[0.0000041414055,0.000011199843,0.9961211,0.000004556198,0.000007960289,0.00008325791,0.00032599308,0.00028877918,0.0006253578,0.00003913669,0.002482468,0.0000060712323],"about_ca_topic_score_codex":0.981604,"about_ca_topic_score_gemma":0.99244374,"teacher_disagreement_score":0.01839602,"about_ca_system_score_codex":0.007975588,"about_ca_system_score_gemma":0.0051427255,"threshold_uncertainty_score":0.05786723},"labels":[],"label_agreement":null},{"id":"W2168447320","doi":"10.1093/gji/ggu280","title":"Trans-dimensional finite-fault inversion","year":2014,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Discretization; Algorithm; Earthquake rupture; Computer science; Geology; Seismology; Fault (geology); Mathematics; Mathematical analysis","score_opus":0.013299263851473182,"score_gpt":0.2200115942164811,"score_spread":0.2067123303650079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168447320","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09846443,0.000045190343,0.8986,0.00010903275,0.000014570858,0.000016728609,0.00022650465,0.0004432437,0.0020803045],"genre_scores_gemma":[0.85996443,0.00004928545,0.13877824,0.000038794464,0.000012556245,0.000034320532,0.00027629355,0.00006287854,0.0007832943],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982435,0.00006525211,0.000013415212,0.000032288586,0.000051170737,0.000013524491],"domain_scores_gemma":[0.9993259,0.0003225057,0.00008605562,0.00014008934,0.000099096076,0.00002642823],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045811918,0.00019393816,0.00034194594,0.00035160044,0.00017528168,0.000648165,0.00073673076,0.0004624541,0.0013557632],"category_scores_gemma":[0.0030241194,0.00025124618,0.0003446067,0.00035192558,0.0005638876,0.000687101,0.00065399345,0.00064461876,0.00018606265],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003169225,0.000017151753,0.0016706656,0.00001705464,0.00001697432,0.00003133384,0.000025843281,0.9773602,0.0032696477,0.008267864,0.00011845426,0.009173037],"study_design_scores_gemma":[0.0000021531307,0.0000023390473,0.00013676465,0.0000010961933,5.824993e-7,0.0000036688214,0.0000019738216,0.9983327,0.00036238157,0.0010706868,0.00008367912,0.0000020248985],"about_ca_topic_score_codex":0.0056910533,"about_ca_topic_score_gemma":0.003983261,"teacher_disagreement_score":0.0056910533,"about_ca_system_score_codex":0.0005196847,"about_ca_system_score_gemma":0.000740465,"threshold_uncertainty_score":0.011315823},"labels":[],"label_agreement":null},{"id":"W2170289982","doi":"10.1190/1.3205028","title":"The 1998 Valhall microseismic data set: An integrated study of relocated sources, seismic multiplets, and S-wave splitting","year":2009,"lang":"en","type":"article","venue":"Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Microseism; Multiplet; Seismology; Geology; Amplitude; Shear wave splitting; Borehole; Waveform; Context (archaeology); Geophysics; Geodesy; Physics; Optics; Spectral line","score_opus":0.04382997584797643,"score_gpt":0.2433923752759308,"score_spread":0.19956239942795437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170289982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976374,0.00006475462,0.00034435175,0.000043900745,0.000007896895,0.000009266091,0.0014443565,0.00004068857,0.0004074177],"genre_scores_gemma":[0.98982424,0.00006988567,0.0014785768,0.000017676184,0.000023934355,0.000019501684,0.008110476,0.000021444901,0.00043427292],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99957055,0.000033817945,0.00004080297,0.00013920925,0.00014435218,0.000071345516],"domain_scores_gemma":[0.9990994,0.00019668862,0.0002323088,0.00016862621,0.0001745134,0.0001285356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041260888,0.00036998693,0.00038629424,0.0027477765,0.0003811878,0.00067323254,0.00048163225,0.00032527515,0.00039044712],"category_scores_gemma":[0.0009747243,0.00019917269,0.00033381107,0.0017288423,0.00029104025,0.0003503758,0.00081946264,0.0002922464,0.0001702504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063486316,0.0003170262,0.8966909,0.000095366515,0.00023518036,0.001352051,0.0008097353,0.007280981,0.015982239,0.00028768438,0.003960764,0.07235331],"study_design_scores_gemma":[0.00002780135,0.000053490265,0.9865427,0.000013673627,0.000035089844,0.00019967306,0.0006212485,0.006914772,0.0030548724,0.00008385734,0.002431993,0.000020954403],"about_ca_topic_score_codex":0.023419082,"about_ca_topic_score_gemma":0.06154609,"teacher_disagreement_score":0.023419082,"about_ca_system_score_codex":0.0005776205,"about_ca_system_score_gemma":0.00046798738,"threshold_uncertainty_score":0.046565533},"labels":[],"label_agreement":null},{"id":"W2170416040","doi":"10.1130/g30597.1","title":"Interplate earthquakes as a driver of shallow subduction erosion","year":2010,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Wedge (geometry); Erosion; Tectonics; Seismology; Basal (medicine); Plate tectonics; Mountain formation; Geomorphology; Geometry","score_opus":0.008613359144029355,"score_gpt":0.2151643784909367,"score_spread":0.20655101934690734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170416040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949078,0.00075005123,0.00028889402,0.00062295154,0.000039806193,0.0000060258244,0.0004329028,0.000011862922,0.0029396166],"genre_scores_gemma":[0.99861,0.00033810255,0.000058371403,0.000039021703,0.000033155276,0.0000011588407,0.00016519276,0.000002780532,0.0007521484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990463,0.000012575403,0.000010961059,0.000021000491,0.000033763463,0.000017057737],"domain_scores_gemma":[0.9984401,0.00042638835,0.00062620867,0.000039651837,0.00023261982,0.00023518305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024770547,0.000120609846,0.00022039843,0.00062571483,0.00017083141,0.00086022867,0.00018265723,0.00025211342,0.0048131957],"category_scores_gemma":[0.0018351943,0.00008629467,0.00014569424,0.0006622283,0.0001596094,0.0004099057,0.0003942938,0.00039748184,0.00028683193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032134305,0.00008506424,0.96249336,0.000104901366,0.00015613333,0.0010452343,0.0003417433,0.0010607705,0.0048266225,0.0011707505,0.0029200066,0.025474131],"study_design_scores_gemma":[0.000013647158,0.000047639438,0.996269,0.000012696988,0.00004644848,0.00017163802,0.00031678632,0.00138225,0.00044366426,0.00027166365,0.0010167708,0.000007801877],"about_ca_topic_score_codex":0.0032864816,"about_ca_topic_score_gemma":0.0057545854,"teacher_disagreement_score":0.0048131957,"about_ca_system_score_codex":0.00017290591,"about_ca_system_score_gemma":0.00025281386,"threshold_uncertainty_score":0.016101718},"labels":[],"label_agreement":null},{"id":"W2171164956","doi":"10.5539/jgg.v3n1p258","title":"Morphotectonic Analysis in the Ghezel Ozan River Basin, NW Iran","year":2011,"lang":"en","type":"article","venue":"Journal of Geography and Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Tectonics; Landform; Geology; Induced seismicity; Drainage basin; Digital elevation model; Geomorphology; Structural basin; Seismology; Remote sensing; Cartography; Geography","score_opus":0.019830875410955344,"score_gpt":0.20526975658268667,"score_spread":0.18543888117173132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171164956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99824035,0.000111124726,0.000217079,0.000037166927,0.0000024403403,0.000012382284,0.00040703188,0.00001218584,0.000960098],"genre_scores_gemma":[0.9982455,0.00009159619,0.0004524185,0.000006432172,0.0000023892069,0.0000109153125,0.0006587671,0.000002954585,0.0005290779],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.000009441304,0.000007341964,0.000018452118,0.000023519886,0.000018329643],"domain_scores_gemma":[0.99993086,0.0000083652685,0.00002048181,0.0000043812715,0.00002825099,0.0000075780463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010501339,0.0001442904,0.00013721312,0.0021006414,0.0002621141,0.00038506548,0.0002119393,0.00014633777,0.00078998],"category_scores_gemma":[0.00027765322,0.00011209816,0.00019002645,0.0022609301,0.00032084013,0.00020275271,0.00023646318,0.00010047975,0.000092497125],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013022669,0.0000619947,0.9244642,0.00008177326,0.00007050008,0.00068768475,0.0015309701,0.004372093,0.005875727,0.0011498214,0.0011062102,0.06046867],"study_design_scores_gemma":[0.0000021822548,0.000008403595,0.997408,0.000002897913,0.000006490946,0.000069459704,0.00054578873,0.00091998273,0.00009658333,0.00007814839,0.0008588284,0.0000033026913],"about_ca_topic_score_codex":0.07702655,"about_ca_topic_score_gemma":0.108012185,"teacher_disagreement_score":0.07702655,"about_ca_system_score_codex":0.0007981517,"about_ca_system_score_gemma":0.0006148003,"threshold_uncertainty_score":0.1531564},"labels":[],"label_agreement":null},{"id":"W2172160159","doi":"10.1111/j.1365-246x.2004.02317.x","title":"Hypocentre determination offshore of eastern Taiwan using the Maximum Intersection method","year":2004,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":178,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Residual; Geodesy; Seismology; Intersection (aeronautics); Subduction; Weighting; Magnitude (astronomy); Mathematics; Tectonics; Physics; Algorithm; Geography; Cartography","score_opus":0.024803673581092495,"score_gpt":0.2758376413610244,"score_spread":0.2510339677799319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2172160159","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.37583852,0.000200041,0.6070756,0.00013507804,0.000032299115,0.000115095936,0.0011549535,0.0031423094,0.012306105],"genre_scores_gemma":[0.71366364,0.000103657454,0.28149354,0.000015291676,0.000021159402,0.000102199694,0.0019563576,0.0003702086,0.0022738806],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997316,0.000041763727,0.000018035342,0.00007802432,0.00008063139,0.000049943752],"domain_scores_gemma":[0.99962306,0.00006436839,0.0000843415,0.000040570707,0.00015264364,0.000035007466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049185194,0.00070680963,0.00052481814,0.002290917,0.00057775545,0.001230646,0.00089624734,0.0004650949,0.002674827],"category_scores_gemma":[0.0017552611,0.0004870584,0.00056389754,0.0020390248,0.00026610747,0.0006108158,0.0013190215,0.0004491504,0.0007875706],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048769175,0.00019085556,0.099409185,0.00033406296,0.000120453544,0.0010262369,0.0019972832,0.30077392,0.07301932,0.011871238,0.0051997937,0.50556993],"study_design_scores_gemma":[0.00006295923,0.000088407374,0.03573684,0.00003353995,0.000033408418,0.00019645745,0.00038410525,0.93993294,0.013791316,0.0029412874,0.006731287,0.00006755809],"about_ca_topic_score_codex":0.009121499,"about_ca_topic_score_gemma":0.010721008,"teacher_disagreement_score":0.009121499,"about_ca_system_score_codex":0.0004792632,"about_ca_system_score_gemma":0.0016709786,"threshold_uncertainty_score":0.0181368},"labels":[],"label_agreement":null},{"id":"W2174261622","doi":"10.1130/g37206.1","title":"Constraints from fault roughness on the scale-dependent strength of rocks","year":2015,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Gordon and Betty Moore Foundation","keywords":"Surface finish; Slip (aerodynamics); Geology; Surface roughness; Asperity (geotechnical engineering); Fault (geology); Scale (ratio); Geometry; Shear (geology); Aspect ratio (aeronautics); Extant taxon; Seismology; Materials science; Geotechnical engineering; Composite material; Petrology; Mathematics; Engineering; Physics","score_opus":0.027993250893788377,"score_gpt":0.22606413416641982,"score_spread":0.19807088327263145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2174261622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920576,0.00028291126,0.003367133,0.00008498531,0.0000042460006,0.000005798084,0.00017557984,0.000025251822,0.0039965142],"genre_scores_gemma":[0.99960893,0.000046093406,0.00022809896,0.000009372574,0.0000037068169,0.0000021085607,0.00005727955,0.0000042777815,0.000040134924],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99961025,0.00007249916,0.000026764616,0.00011552664,0.000108589775,0.00006633244],"domain_scores_gemma":[0.9955804,0.0026715354,0.0007616711,0.0005497636,0.00022342373,0.00021310642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043970105,0.00026441953,0.00034435187,0.0005502289,0.00024121806,0.00086589437,0.0003561869,0.0003253521,0.0011565913],"category_scores_gemma":[0.0052381386,0.00027333153,0.00022063014,0.00030515422,0.0010335353,0.0007629149,0.0007238959,0.00029463728,0.00021195185],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008834926,0.00010834015,0.4462215,0.00031152368,0.00017989238,0.00099092,0.00049434893,0.022913035,0.4791459,0.013360935,0.0006254364,0.034764655],"study_design_scores_gemma":[0.000023253204,0.00011112362,0.9574151,0.000020418569,0.000049580773,0.00030846047,0.00015683158,0.024814025,0.009932633,0.0066970764,0.00042376382,0.000047712252],"about_ca_topic_score_codex":0.0016618354,"about_ca_topic_score_gemma":0.0027267532,"teacher_disagreement_score":0.0016618354,"about_ca_system_score_codex":0.00022774887,"about_ca_system_score_gemma":0.00015139591,"threshold_uncertainty_score":0.0038692355},"labels":[],"label_agreement":null},{"id":"W2174974575","doi":"10.1093/gji/ggv422","title":"Crustal structure from the Hecataeus Rise to the Levantine Basin, eastern Mediterranean, from seismic refraction and gravity modelling","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Memorial University of Newfoundland","funders":"","keywords":"Geology; Crust; Subduction; Oceanic crust; Seismology; Seismic refraction; Seamount; Structural basin; Geophysics; Paleontology; Tectonics","score_opus":0.03614303925174568,"score_gpt":0.24683743582849643,"score_spread":0.21069439657675076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2174974575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974452,0.00010602519,0.00014435081,0.000022128683,0.0000024092255,0.0000071776603,0.000519712,0.000024220908,0.0017287186],"genre_scores_gemma":[0.99792564,0.00010954005,0.0004435653,0.0000068068534,0.000002680566,0.00000416043,0.0010154189,0.0000065251006,0.00048554875],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995077,0.000004134463,0.000004803453,0.000016507925,0.000014039159,0.000009793214],"domain_scores_gemma":[0.9999453,0.000004410908,0.000011282527,0.0000060557113,0.000025237043,0.000007656502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000985409,0.00029301085,0.00014096963,0.0011601157,0.00027437304,0.00066438684,0.0001668757,0.00020689599,0.001012602],"category_scores_gemma":[0.00027405095,0.00015848337,0.00024618005,0.00090796046,0.00015831723,0.00018670759,0.00032111924,0.0001222993,0.00024972134],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026596524,0.00008570072,0.86556864,0.00012384658,0.00023181405,0.0017723468,0.0014599137,0.04193991,0.023820415,0.0005422083,0.0017566149,0.062432706],"study_design_scores_gemma":[0.000012456991,0.000018584842,0.9862985,0.000014057705,0.000019197003,0.0000890878,0.00023634809,0.011115667,0.00042005294,0.000051895568,0.0017182559,0.0000058845967],"about_ca_topic_score_codex":0.119817704,"about_ca_topic_score_gemma":0.14955902,"teacher_disagreement_score":0.119817704,"about_ca_system_score_codex":0.0009150705,"about_ca_system_score_gemma":0.0004366161,"threshold_uncertainty_score":0.2382406},"labels":[],"label_agreement":null},{"id":"W2175744612","doi":"10.1785/0220140204","title":"Impact of Induced Seismicity on the Evaluation of Seismic Hazard: Some Preliminary Considerations","year":2015,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"National Research Council Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Citation; Icon; Induced seismicity; Computer science; Haystack; Information retrieval; Library science; World Wide Web; Geology; Seismology","score_opus":0.3197369215488526,"score_gpt":0.4022383822463662,"score_spread":0.08250146069751363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2175744612","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.051389307,0.078142166,0.033511065,0.59060395,0.00566761,0.0014201343,0.003361152,0.00039635558,0.23550828],"genre_scores_gemma":[0.7830626,0.09248672,0.053683266,0.03235557,0.007866965,0.000624074,0.0013964344,0.00027910635,0.028245367],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9797156,0.010513919,0.0014454387,0.00050629606,0.007152599,0.00066609174],"domain_scores_gemma":[0.8473243,0.09474678,0.0042550345,0.0030257571,0.047843013,0.0028052055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.032915916,0.0011188526,0.0011906147,0.0042243763,0.0019918175,0.009385361,0.0034669735,0.0039218045,0.018170865],"category_scores_gemma":[0.12674041,0.00045659413,0.0011978472,0.0044637267,0.0037077935,0.007859711,0.003817102,0.005064819,0.0024871966],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001603005,0.00042086397,0.057462823,0.0036993779,0.00032604934,0.0023381512,0.0033715772,0.016342588,0.002389236,0.12852341,0.24221617,0.5413069],"study_design_scores_gemma":[0.00031865807,0.0033032119,0.13842906,0.023919193,0.0008505185,0.0037769384,0.029280819,0.03235442,0.0069158734,0.24175875,0.5181359,0.0009565884],"about_ca_topic_score_codex":0.042409744,"about_ca_topic_score_gemma":0.08216337,"teacher_disagreement_score":0.042409744,"about_ca_system_score_codex":0.007867433,"about_ca_system_score_gemma":0.008989017,"threshold_uncertainty_score":0.1740781},"labels":[],"label_agreement":null},{"id":"W2177737943","doi":"10.1139/cjes-2015-0129","title":"Propagation of a strike-slip plate boundary within an extensional environment: the westward propagation of the North Anatolian Fault","year":2015,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; North Anatolian Fault; Plate tectonics; Seismology; North American Plate; Eurasian Plate; African Plate; Lithosphere; Shear zone; Trough (economics); Slab; Shear (geology); Fault (geology); Structural basin; Strike-slip tectonics; Pleistocene; Tectonics; Paleontology","score_opus":0.03388487881580114,"score_gpt":0.21342184876437226,"score_spread":0.1795369699485711,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2177737943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99699306,0.00023414267,0.0002057163,0.000049519316,0.000007129873,0.0000033214906,0.00006011246,0.000013473312,0.0024334628],"genre_scores_gemma":[0.99930084,0.00010121692,0.00016797495,0.000008598869,0.0000038253547,0.000001788843,0.00007587734,0.000003901328,0.00033595873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999243,0.000007543343,0.0000094985935,0.000031785054,0.000011657026,0.000015140528],"domain_scores_gemma":[0.9998043,0.000009588015,0.00008154072,0.00002167902,0.00006347927,0.00001943028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020098864,0.00016985669,0.0001695971,0.00068308203,0.00052793813,0.00062232156,0.00023627636,0.0003360281,0.0012550689],"category_scores_gemma":[0.00040603935,0.0001368551,0.00010359606,0.000440373,0.0005307872,0.00043721017,0.00060473906,0.00025514382,0.00028476192],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002002969,0.00003180205,0.86202115,0.00010121988,0.00008637375,0.0015618646,0.0023651945,0.002246578,0.10288278,0.0015598426,0.0002919755,0.026651045],"study_design_scores_gemma":[0.000009540434,0.000039055914,0.99192315,0.000024645462,0.00002786506,0.0004811392,0.0005112411,0.001375937,0.0029472886,0.00018647539,0.0024642998,0.000009379267],"about_ca_topic_score_codex":0.011797672,"about_ca_topic_score_gemma":0.014677571,"teacher_disagreement_score":0.011797672,"about_ca_system_score_codex":0.00068551226,"about_ca_system_score_gemma":0.00037641372,"threshold_uncertainty_score":0.023458004},"labels":[],"label_agreement":null},{"id":"W2179435008","doi":"10.1190/tle34060658.1","title":"How did hydraulic-fracturing operations in the Horn River Basin change seismicity patterns in northeastern British Columbia, Canada?","year":2015,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of British Columbia; Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Hydraulic fracturing; Geology; Volume (thermodynamics); Seismology; Drainage basin; Structural basin; Magnitude (astronomy); Hydrology (agriculture); Geotechnical engineering; Geomorphology; Geography","score_opus":0.04150348848375761,"score_gpt":0.21347609099144776,"score_spread":0.17197260250769014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2179435008","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992151,0.00046158134,0.00008188114,0.00070672954,0.000010730037,0.000018381706,0.003036646,0.0000125584,0.0035204552],"genre_scores_gemma":[0.9950434,0.00043185378,0.000104527855,0.00010721596,0.0000033512194,0.000009855241,0.0011732437,0.0000073919487,0.0031191779],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99961424,0.000032953838,0.000025117222,0.00007356604,0.00008777924,0.0001662228],"domain_scores_gemma":[0.9977302,0.00013552445,0.00027394056,0.000048244172,0.0013673889,0.0004447158],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030976266,0.00026116642,0.00028868514,0.0017251808,0.0019972657,0.0017207315,0.0009138262,0.00046254226,0.0031477998],"category_scores_gemma":[0.0016041863,0.00026089538,0.00024559605,0.0044000107,0.0008168848,0.00041677727,0.00060233026,0.00056232227,0.00033349043],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007014992,0.000038235343,0.9838758,0.00004879622,0.00006449012,0.0002766517,0.0014888082,0.0004392787,0.0008070196,0.00019498562,0.0024394263,0.0102562485],"study_design_scores_gemma":[0.0000031903428,0.000005007901,0.9943427,0.000029818271,0.000015890782,0.000025672862,0.003553909,0.00040914255,0.00008168247,0.00002818115,0.0014936012,0.0000111395],"about_ca_topic_score_codex":0.99809545,"about_ca_topic_score_gemma":0.9995278,"teacher_disagreement_score":0.02783423,"about_ca_system_score_codex":0.02783423,"about_ca_system_score_gemma":0.027034916,"threshold_uncertainty_score":0.2019524},"labels":[],"label_agreement":null},{"id":"W2181709664","doi":"10.7186/bgsm47200308","title":"A dextral strike-slip model for the Miri Structure","year":2003,"lang":"en","type":"article","venue":"Bulletin of the Geological Society of Malaysia","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sinistral and dextral; Strike-slip tectonics; Geology; Seismology; Geometry; Fault (geology); Mathematics","score_opus":0.023012567173918398,"score_gpt":0.20943266430095134,"score_spread":0.18642009712703295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2181709664","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3144969,0.0016705823,0.29815227,0.0036891364,0.00046145724,0.00042944364,0.00235241,0.0021407334,0.37660697],"genre_scores_gemma":[0.9352426,0.00067526585,0.015886292,0.00016513938,0.00008323106,0.00014575514,0.00048228388,0.00017631413,0.047143064],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999037,0.0000109067005,0.000005653726,0.000027092192,0.000031668966,0.000020981133],"domain_scores_gemma":[0.9999052,0.000009174835,0.000022606917,0.000015540707,0.000022979551,0.00002440384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001482853,0.00044512632,0.00033788808,0.0006645008,0.000495862,0.0013705363,0.0018512558,0.0012425102,0.0115243085],"category_scores_gemma":[0.00037625624,0.00029768274,0.00039485257,0.0005200417,0.0010175568,0.0010002156,0.00053307845,0.0006550155,0.003490546],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006238708,0.0000864797,0.004219667,0.00013642781,0.000021206204,0.0009246141,0.00039792195,0.57896733,0.008810837,0.38191968,0.0060795173,0.018373918],"study_design_scores_gemma":[0.000024259627,0.000054210286,0.0017223082,0.000020594414,0.000006619272,0.00037374572,0.000101075704,0.9550612,0.00027131365,0.03523718,0.007106388,0.000021233041],"about_ca_topic_score_codex":0.0074239336,"about_ca_topic_score_gemma":0.0036310186,"teacher_disagreement_score":0.0115243085,"about_ca_system_score_codex":0.0009913094,"about_ca_system_score_gemma":0.0004766824,"threshold_uncertainty_score":0.0385527},"labels":[],"label_agreement":null},{"id":"W2181711980","doi":"","title":"Coulomb Stress Failures in Fracture Networks Resulting from Hydraulic Fracturing: A Tutorial","year":2011,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Poromechanics; Hydraulic fracturing; Microseism; Geology; Pore water pressure; Coulomb; Stress (linguistics); Geomechanics; Geotechnical engineering; Fluid dynamics; Mechanics; Fluid pressure; Seismology; Porous medium; Physics","score_opus":0.02126979887411821,"score_gpt":0.20668042429905117,"score_spread":0.18541062542493297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2181711980","genre_codex":"review","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.027326621,0.6269104,0.24470587,0.0026795152,0.0031090206,0.00030918643,0.0009426115,0.000712381,0.09330445],"genre_scores_gemma":[0.1068974,0.6908815,0.13835429,0.0014584716,0.009989792,0.00038834236,0.0014790619,0.0002892316,0.05026193],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99985147,0.000024090188,0.000016892614,0.00003960952,0.000051135976,0.00001681256],"domain_scores_gemma":[0.99970895,0.00017191216,0.000028510423,0.000015341811,0.000054807995,0.000020462583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039755538,0.0016147001,0.0009146943,0.0023057952,0.00049307686,0.0016030708,0.0007287723,0.0013608964,0.003008658],"category_scores_gemma":[0.000670764,0.0006894151,0.0010450861,0.0021399204,0.0009193027,0.0020663175,0.00077362446,0.0015172317,0.0015541273],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010759402,0.00036497615,0.0031458891,0.0054739667,0.00028732372,0.0023157177,0.0011639098,0.07423894,0.009004335,0.3414388,0.05944932,0.5030093],"study_design_scores_gemma":[0.000027795551,0.00043118902,0.010521723,0.0021543072,0.0001158507,0.0038993899,0.0004187386,0.0939434,0.0026072415,0.3559199,0.52973855,0.00022193424],"about_ca_topic_score_codex":0.002667236,"about_ca_topic_score_gemma":0.002379312,"teacher_disagreement_score":0.003008658,"about_ca_system_score_codex":0.00080259505,"about_ca_system_score_gemma":0.00036795455,"threshold_uncertainty_score":0.0100649595},"labels":[],"label_agreement":null},{"id":"W2183041774","doi":"10.1093/gji/ggv159","title":"Dynamic triggering of microseismicity in a mine setting","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Induced seismicity; Microseism; Geology; Seismology; Subsidence; Event (particle physics); Rock blasting; Stress (linguistics); Geotechnical engineering; Mining engineering; Structural basin; Physics; Geomorphology","score_opus":0.016662285782892073,"score_gpt":0.24990250097536623,"score_spread":0.23324021519247415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2183041774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99892503,0.00003444582,0.00043568,0.000018690896,0.0000022470515,0.000008006085,0.00015521157,0.000012339951,0.00040831935],"genre_scores_gemma":[0.99962425,0.000018400433,0.00020427715,0.0000033194692,0.0000040841032,0.000004663352,0.000090601454,0.0000015680571,0.000048693866],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998282,0.00002768234,0.000015649968,0.00005158216,0.000037886344,0.000038987608],"domain_scores_gemma":[0.9992717,0.00013732347,0.00031725058,0.0000531407,0.00009238877,0.00012819024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022762839,0.00015816679,0.0002695542,0.0010081514,0.00029711143,0.00031448234,0.00025217424,0.00043121903,0.0008038943],"category_scores_gemma":[0.0010802607,0.00014276226,0.00014781056,0.00097028894,0.00036018703,0.0002966102,0.0006215397,0.00026036362,0.00022661385],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000394032,0.00012930202,0.95325166,0.00008445324,0.000085062704,0.0014461923,0.0016904556,0.0034795064,0.025138592,0.00030162724,0.00036841672,0.013630699],"study_design_scores_gemma":[0.0000031381876,0.000090195455,0.9962529,0.000005700403,0.000007975485,0.00025973775,0.0005375526,0.0019724665,0.00052116695,0.000060848444,0.00028142126,0.000006880925],"about_ca_topic_score_codex":0.0029678533,"about_ca_topic_score_gemma":0.0070342314,"teacher_disagreement_score":0.0029678533,"about_ca_system_score_codex":0.0002290162,"about_ca_system_score_gemma":0.00013409421,"threshold_uncertainty_score":0.005901158},"labels":[],"label_agreement":null},{"id":"W2183099518","doi":"10.26443/msurj.v7i1.99","title":"Point estimates of Crustal thickness Using receiver Function Stacking","year":2012,"lang":"en","type":"article","venue":"McGill Science Undergraduate Research Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; McGill University","funders":"","keywords":"Receiver function; Seismology; Geology; Crust; Coda; Stacking; Seismic array; Broadband; Waveform; Economic shortage; Geodesy; Magnitude (astronomy); Upper crust; Function (biology); Lithosphere; Geophysics; Telecommunications; Tectonics; Computer science; Physics","score_opus":0.11897081520782601,"score_gpt":0.3541018160283366,"score_spread":0.2351310008205106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2183099518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49254993,0.000579366,0.48336032,0.00007727127,0.000025345105,0.000155453,0.0041284985,0.004757561,0.014366305],"genre_scores_gemma":[0.7540373,0.00028649202,0.23877484,0.000018824072,0.000010793747,0.00004922286,0.0025776292,0.00014597457,0.004098894],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99980265,0.000019924779,0.000010097675,0.000037407266,0.000095911215,0.00003392941],"domain_scores_gemma":[0.99956995,0.000045838504,0.0000828527,0.00005456211,0.00022981194,0.000016919037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037110498,0.00076005684,0.0001719861,0.0028670551,0.0003299076,0.00082073454,0.0005810603,0.00028677343,0.00570965],"category_scores_gemma":[0.0010822456,0.00027335968,0.00032824738,0.0015705947,0.00018597077,0.0005482341,0.0004484947,0.00026391936,0.0015663563],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024954518,0.000056154335,0.12941091,0.00020407862,0.0002552769,0.00029681457,0.0008596329,0.07908855,0.18924421,0.0032198385,0.0026307476,0.59448415],"study_design_scores_gemma":[0.000028207054,0.00017603957,0.4916875,0.00012614524,0.00015995221,0.00058773044,0.0007704139,0.3798144,0.1114221,0.0033863287,0.011612998,0.00022824117],"about_ca_topic_score_codex":0.06917084,"about_ca_topic_score_gemma":0.10295511,"teacher_disagreement_score":0.06917084,"about_ca_system_score_codex":0.0010053014,"about_ca_system_score_gemma":0.00080454384,"threshold_uncertainty_score":0.1375364},"labels":[],"label_agreement":null},{"id":"W2184268826","doi":"","title":"Earthquakes and Seismic Hazard in the Yukon-Beaufort-Mackenzie","year":2005,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Terrane; Induced seismicity; Seismic hazard; Intraplate earthquake; Tectonics; North American Plate; Subduction","score_opus":0.01673690092179157,"score_gpt":0.22042208368124075,"score_spread":0.2036851827594492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2184268826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987657,0.0000877151,0.000014199429,0.000037684906,5.2894154e-7,0.0000018169618,0.00020379285,0.000002457055,0.00088614796],"genre_scores_gemma":[0.99920386,0.00012998497,0.000030377163,0.000011605338,7.367715e-7,0.0000015400102,0.00027711302,0.0000013467364,0.00034357046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999118,0.0000054557536,0.000007679594,0.000012693865,0.000021047035,0.00004130512],"domain_scores_gemma":[0.99973744,0.000020227928,0.00010103235,0.000011050195,0.00006125964,0.00006899874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007191113,0.00011608306,0.000099779296,0.00095794717,0.00086327177,0.0005405425,0.00021349473,0.00013011195,0.0010528624],"category_scores_gemma":[0.0004837935,0.00010309839,0.000104594736,0.0013245058,0.00042732075,0.00024746588,0.00062569906,0.00015775619,0.0001053068],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041778094,0.00000717225,0.99421763,0.000009576147,0.00002139381,0.00022005696,0.00076321163,0.00021946176,0.00050518656,0.00012176365,0.00029849645,0.003574145],"study_design_scores_gemma":[0.0000013994417,0.0000046345817,0.9984303,0.000003995747,0.0000033423369,0.000061536426,0.00086064026,0.00009825263,0.00004683602,0.000010904223,0.000475477,0.0000026124203],"about_ca_topic_score_codex":0.80986917,"about_ca_topic_score_gemma":0.94356364,"teacher_disagreement_score":0.19013083,"about_ca_system_score_codex":0.0028218022,"about_ca_system_score_gemma":0.0016384878,"threshold_uncertainty_score":0.38250107},"labels":[],"label_agreement":null},{"id":"W2184907280","doi":"","title":"Fractures in the Cardium and Normal Faults in Western Alberta","year":2009,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Outcrop; Wrench; Tectonics; Fracture (geology); Kinematics; Stress (linguistics); Structural basin; Paleontology; Echelon formation; Seismology; Engineering","score_opus":0.009109668744440125,"score_gpt":0.22432663032140807,"score_spread":0.21521696157696793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2184907280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972972,0.00026854826,0.00008554936,0.000033273573,0.0000017864519,0.0000048348506,0.00031781566,0.0000065539293,0.0019843895],"genre_scores_gemma":[0.9981737,0.00014482012,0.0001765781,0.000010685574,0.0000011738173,0.0000026941484,0.00023091043,0.0000015237785,0.0012578184],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983203,0.000008633941,0.0000067953038,0.000028532759,0.00006425291,0.000059783477],"domain_scores_gemma":[0.99971193,0.000024306413,0.000068874964,0.000011256854,0.00012149718,0.000062133804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018519485,0.00013956393,0.00012576635,0.0022183456,0.0008545414,0.00063673285,0.00035405453,0.00020282212,0.0009518788],"category_scores_gemma":[0.00042862032,0.00016534569,0.000107961816,0.001907524,0.0008564967,0.00010810459,0.00049038784,0.00012828251,0.00010345667],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002873631,0.00002801459,0.94972754,0.00006159864,0.000028245437,0.0006244326,0.0019854433,0.0010514595,0.010895316,0.00067255576,0.00061458873,0.034023542],"study_design_scores_gemma":[0.000001955285,0.000007918262,0.9981945,0.0000072908265,0.000004368803,0.000078155215,0.00056869106,0.00020676262,0.00020915798,0.000040371524,0.0006778622,0.0000028887039],"about_ca_topic_score_codex":0.91973734,"about_ca_topic_score_gemma":0.9836626,"teacher_disagreement_score":0.08026266,"about_ca_system_score_codex":0.005782398,"about_ca_system_score_gemma":0.0041308873,"threshold_uncertainty_score":0.16147065},"labels":[],"label_agreement":null},{"id":"W2184994971","doi":"10.1002/2015gl066361","title":"Static stress drop in the <i>M<sub>w</sub></i> 9 Tohoku‐oki earthquake: Heterogeneous distribution and low average value","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"","keywords":"Drop (telecommunication); Geology; Slip (aerodynamics); Seismology; Fault plane; Mechanics; Fault (geology); Physics; Thermodynamics; Engineering","score_opus":0.030609092748966612,"score_gpt":0.2666330343537852,"score_spread":0.2360239416048186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2184994971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984913,0.000044256547,0.0006584055,0.000012988217,0.0000015876593,0.0000024023402,0.0002656269,0.000025020501,0.0004984378],"genre_scores_gemma":[0.9995976,0.00002257844,0.00010366786,0.0000023138298,0.0000012017794,0.000002080189,0.00021054626,0.000003833468,0.000056130113],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999261,0.0000058781907,0.000009122747,0.00002797327,0.000012408234,0.000018492026],"domain_scores_gemma":[0.99978966,0.0000386217,0.000056796223,0.0000348926,0.000046237266,0.000033798882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022200787,0.0003751713,0.000451262,0.00089677604,0.00031361796,0.00063040777,0.0006414497,0.0005468589,0.0005293097],"category_scores_gemma":[0.00039321146,0.00038176548,0.0007033015,0.0010157059,0.00031525863,0.0006816634,0.00033781308,0.00017888243,0.00017962763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032920146,0.00016658388,0.61823374,0.00022917104,0.0003641105,0.0011738598,0.00032390375,0.32861155,0.03360432,0.00054103555,0.0007265871,0.015695943],"study_design_scores_gemma":[0.000020859396,0.0001378762,0.5274472,0.000013449574,0.00013642632,0.00033117077,0.00025216557,0.46374956,0.0069876662,0.00053982105,0.00032244917,0.00006138658],"about_ca_topic_score_codex":0.010325857,"about_ca_topic_score_gemma":0.009268443,"teacher_disagreement_score":0.010325857,"about_ca_system_score_codex":0.0008435566,"about_ca_system_score_gemma":0.0002566685,"threshold_uncertainty_score":0.020531476},"labels":[],"label_agreement":null},{"id":"W2186096621","doi":"10.1002/2015jb012467","title":"Multifrequential periodogram analysis of earthquake occurrence: An alternative approach to the Schuster spectrum, with two examples in central California","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Ste. Anne's Hospital","funders":"U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Seismology; Geology; Periodogram; Series (stratigraphy); Fault (geology); Induced seismicity; Mathematics; Statistics; Paleontology","score_opus":0.08804173702369938,"score_gpt":0.3452226008246781,"score_spread":0.2571808638009787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2186096621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99236065,0.00023554999,0.0048031965,0.00007949194,0.000006730774,0.000015102617,0.0007565968,0.000089643996,0.0016529422],"genre_scores_gemma":[0.9954856,0.0000683151,0.0037525613,0.0000072806924,0.000007712285,0.000007061354,0.0004319044,0.000012532419,0.00022703526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997919,0.000061063954,0.000015357868,0.00006359507,0.000047204532,0.000020892237],"domain_scores_gemma":[0.9991442,0.0003885724,0.00012654682,0.00009440743,0.00018721235,0.000059134236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007664749,0.00023762643,0.00018890927,0.0024105085,0.0003063313,0.00059814204,0.00038899266,0.00025928256,0.00078680064],"category_scores_gemma":[0.001975776,0.000106841195,0.0002882638,0.0019320574,0.00021070919,0.00035870261,0.00033889478,0.00021723413,0.000066712644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033621665,0.00015458687,0.8173456,0.00012614318,0.0002151889,0.0008062526,0.00092082383,0.06541486,0.005685342,0.004761484,0.0030209385,0.101212464],"study_design_scores_gemma":[0.000021731255,0.00005273552,0.75877047,0.000015494576,0.000032669865,0.00014063556,0.00037509462,0.2373806,0.0004327833,0.0014039662,0.0013391764,0.000034643424],"about_ca_topic_score_codex":0.116228834,"about_ca_topic_score_gemma":0.12363223,"teacher_disagreement_score":0.116228834,"about_ca_system_score_codex":0.00069054804,"about_ca_system_score_gemma":0.0004425626,"threshold_uncertainty_score":0.23110461},"labels":[],"label_agreement":null},{"id":"W2186337726","doi":"","title":"Multiplet Relocation in a Heavy Oil Field Using the Double Difference Method","year":2011,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Multiplet; Microseism; Waveform; Event (particle physics); Relocation; Robustness (evolution); Field (mathematics); Computer science; Geology; Physics; Seismology; Mathematics; Chemistry; Spectral line; Telecommunications","score_opus":0.09987414034263638,"score_gpt":0.28223745022921576,"score_spread":0.1823633098865794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2186337726","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3089112,0.00009410178,0.6874676,0.00015230126,0.00008933558,0.000056927867,0.0002293425,0.0011853606,0.0018138397],"genre_scores_gemma":[0.6141209,0.000042740106,0.383456,0.000027962926,0.000025830224,0.000047492158,0.0003868178,0.00020508777,0.001687196],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997408,0.000038061957,0.000012891117,0.000081331375,0.00009678993,0.000030130486],"domain_scores_gemma":[0.9990609,0.00032567864,0.000111243025,0.00020826561,0.00023545274,0.000058445003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063522754,0.00040701634,0.00051080366,0.0011680439,0.0003998301,0.0006743942,0.0007068413,0.0004652257,0.0025833135],"category_scores_gemma":[0.0025814443,0.00028514632,0.00046353583,0.0007536278,0.00032742912,0.0006802622,0.00070188876,0.00064786087,0.000526836],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000997171,0.0003870711,0.018488657,0.00020068485,0.000105698724,0.001000903,0.00050465344,0.29530427,0.14157519,0.007801194,0.0024416659,0.5311928],"study_design_scores_gemma":[0.00003766841,0.00008606866,0.0051337983,0.000007938568,0.0000137550505,0.00023387054,0.00009342478,0.96981835,0.020944754,0.0019464834,0.0016552809,0.000028647217],"about_ca_topic_score_codex":0.0023135946,"about_ca_topic_score_gemma":0.0035392446,"teacher_disagreement_score":0.0025833135,"about_ca_system_score_codex":0.00036660404,"about_ca_system_score_gemma":0.0005285602,"threshold_uncertainty_score":0.008642077},"labels":[],"label_agreement":null},{"id":"W2189144241","doi":"","title":"Statistical biases in microseismicity parameters","year":2013,"lang":"ml","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Microseism; Magnitude (astronomy); Hydraulic fracturing; Event (particle physics); Geology; Threshold limit value; Computation; Fracture (geology); Seismology; Geodesy; Computer science; Algorithm; Physics; Geotechnical engineering","score_opus":0.03782670223593839,"score_gpt":0.24060631157737628,"score_spread":0.20277960934143788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2189144241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89366156,0.0010555161,0.094188415,0.00048450517,0.00018902057,0.00009439305,0.0043941247,0.0014603711,0.0044721332],"genre_scores_gemma":[0.99695504,0.000040398605,0.0018432175,0.00003865014,0.000019986805,0.000012326873,0.00087903417,0.00010467545,0.000106639854],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99243075,0.002284062,0.00064848596,0.0026013823,0.0016177995,0.0004174905],"domain_scores_gemma":[0.9134729,0.05627351,0.007576722,0.016708866,0.0052962564,0.0006716814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.012733385,0.00043209264,0.00054689776,0.001418512,0.00038552663,0.0016841984,0.0010594028,0.00068725785,0.0016291863],"category_scores_gemma":[0.064294145,0.00030083483,0.0006877905,0.0015122937,0.00094055437,0.0012431258,0.0007917733,0.0006879269,0.0005420997],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007953257,0.00007469751,0.85705024,0.00033150517,0.0014125806,0.0002593676,0.00043585777,0.073803216,0.015950695,0.0051288414,0.003151978,0.0416057],"study_design_scores_gemma":[0.000054424116,0.0001996758,0.77223295,0.00010846613,0.00038377478,0.000772614,0.00045234922,0.16930364,0.02621647,0.023762748,0.006376036,0.00013682913],"about_ca_topic_score_codex":0.002507905,"about_ca_topic_score_gemma":0.00118349,"teacher_disagreement_score":0.012733385,"about_ca_system_score_codex":0.0005543319,"about_ca_system_score_gemma":0.00034627554,"threshold_uncertainty_score":0.06734139},"labels":[],"label_agreement":null},{"id":"W2189591728","doi":"","title":"A CRUSTAL DEFORMATION STUDY OF THE CHARLEVOIX SEISMIC ZONE IN QUEBEC","year":2010,"lang":"en","type":"article","venue":"Corpus Université Laval (Université Laval)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Levelling; Geodetic datum; Geology; Geodesy; Global Positioning System; Seismology; Seismic zone; Deformation (meteorology); Crust; Geophysics; Induced seismicity; Oceanography","score_opus":0.006926868127017711,"score_gpt":0.1689386724065399,"score_spread":0.1620118042795222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2189591728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99157774,0.00034897705,0.00045018268,0.00010618188,0.00000529061,0.00003827735,0.0016741252,0.000024979148,0.00577416],"genre_scores_gemma":[0.9952803,0.00020312933,0.00043012403,0.000027210379,0.0000022043107,0.000011768163,0.0012399836,0.0000069951907,0.0027981205],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984455,0.00000970285,0.0000060912944,0.00003634565,0.000054717813,0.000048543825],"domain_scores_gemma":[0.9997322,0.000020644335,0.00003361058,0.00001416786,0.00015015255,0.000049187394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018650616,0.00024933997,0.00024725834,0.0012141365,0.0011572008,0.0008083801,0.00046360103,0.00031450484,0.0024847186],"category_scores_gemma":[0.0005059089,0.00015552375,0.00022757956,0.002501999,0.0004141491,0.0002327756,0.00036117798,0.00020825448,0.00021710513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017397324,0.00006582148,0.91667855,0.00013503926,0.00016487548,0.00083527464,0.0029897406,0.012325873,0.012471909,0.00088488683,0.0025123456,0.050761703],"study_design_scores_gemma":[0.0000052967107,0.000013670894,0.99213433,0.000020161619,0.000013700208,0.000034540735,0.0008030855,0.0039244103,0.00027773154,0.000024287383,0.0027403603,0.000008446646],"about_ca_topic_score_codex":0.9925774,"about_ca_topic_score_gemma":0.9959974,"teacher_disagreement_score":0.012838511,"about_ca_system_score_codex":0.012838511,"about_ca_system_score_gemma":0.00789824,"threshold_uncertainty_score":0.09315038},"labels":[],"label_agreement":null},{"id":"W2191915062","doi":"","title":"Field Trip B7: Transpression and Transtension along a Continental Transform Fault: Minas Fault Zone, Nova Scotia","year":2005,"lang":"en","type":"book","venue":"Atlantic Geoscience Society Special Publications eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Transtension; Transpression; Nova scotia; Geology; Fault (geology); Seismology; Geography; Sinistral and dextral; Oceanography","score_opus":0.015677680783622576,"score_gpt":0.2243244993341242,"score_spread":0.20864681855050163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2191915062","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6705079,0.004773094,0.0027304143,0.0013235178,0.0002682407,0.000260592,0.11612822,0.00037733026,0.20363057],"genre_scores_gemma":[0.74198717,0.0022379276,0.00233242,0.00012625249,0.000059388858,0.000058651294,0.0368168,0.00013021607,0.21625118],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99995375,0.0000033513018,0.0000025437462,0.0000086879,0.00002066727,0.000011142842],"domain_scores_gemma":[0.9998568,0.000020670019,0.000014267066,0.000009838958,0.00007670254,0.000021557855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000119905526,0.00025813977,0.00011665853,0.0010846293,0.00048251683,0.00039311624,0.00042118464,0.0001638539,0.008933724],"category_scores_gemma":[0.00035476446,0.00014823653,0.00008193174,0.00195642,0.00023306406,0.00025328554,0.00019338181,0.00016119113,0.0012709463],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010528374,0.00012132232,0.22911288,0.00068143493,0.000095416144,0.0021713115,0.005517455,0.012907168,0.026243737,0.0046682325,0.34310442,0.37432384],"study_design_scores_gemma":[0.000031625525,0.00007747704,0.9007883,0.000065298664,0.000013997558,0.00032773367,0.00097588653,0.0015937915,0.001472178,0.00048993056,0.09414887,0.00001489079],"about_ca_topic_score_codex":0.8745411,"about_ca_topic_score_gemma":0.960657,"teacher_disagreement_score":0.1254589,"about_ca_system_score_codex":0.0024353967,"about_ca_system_score_gemma":0.0023723105,"threshold_uncertainty_score":0.25239545},"labels":[],"label_agreement":null},{"id":"W2192062287","doi":"10.1785/0120150027","title":"The Aftershock Sequence of the 2010<i>M</i><sub>w</sub> 6.3 Rigan Earthquake in Southeast Iran: Further Evidence of a Hidden Fault in the Southern Lut Block","year":2015,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research","keywords":"Seismology; Geology; Aftershock; Sequence (biology); Fault (geology); Block (permutation group theory); Kurtosis; Seismic hazard; Algorithm; Statistics; Computer science; Mathematics","score_opus":0.04147226071900529,"score_gpt":0.23114932959119464,"score_spread":0.18967706887218935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2192062287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950578,0.00011590037,0.000118509204,0.00014357007,0.0000341384,0.000015576263,0.0008806324,0.000014997557,0.0036188988],"genre_scores_gemma":[0.9974402,0.00013085244,0.00012498681,0.000038620565,0.00003093767,0.0000043507557,0.0011153868,0.000002953201,0.0011115931],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994886,0.0000036838871,0.0000059702343,0.000007631415,0.000014589704,0.000019315356],"domain_scores_gemma":[0.99969244,0.000016780561,0.00013081139,0.000016348657,0.00010408655,0.00003960824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010458965,0.00015701335,0.00012562168,0.0008445615,0.00033557558,0.00025239168,0.00020552202,0.00030962154,0.0020257467],"category_scores_gemma":[0.00034845242,0.00008241853,0.00010539017,0.0011787949,0.00025956627,0.00020981667,0.00030965873,0.00027984096,0.00038987547],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070620235,0.00015346092,0.89847296,0.00018604596,0.000065866014,0.0048445775,0.00373195,0.0017302355,0.018127318,0.0011663568,0.008278564,0.06253659],"study_design_scores_gemma":[0.0000057750444,0.000039594725,0.99679273,0.000009141078,0.000011748688,0.00021686779,0.00048991,0.0001449242,0.00022557889,0.00004756281,0.0020134188,0.0000026652892],"about_ca_topic_score_codex":0.047776468,"about_ca_topic_score_gemma":0.11149098,"teacher_disagreement_score":0.047776468,"about_ca_system_score_codex":0.0004542304,"about_ca_system_score_gemma":0.000860783,"threshold_uncertainty_score":0.09499675},"labels":[],"label_agreement":null},{"id":"W2196442963","doi":"10.1139/cjce-2012-0247","title":"Damage to engineered structures during the 12 January 2010, Haiti (Léogâne) earthquake","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Civil Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"Induced seismicity; Interim; Building code; Earthquake engineering; Engineering; Seismic analysis; Forensic engineering; Civil engineering; Seismology; Geology; Geography; Archaeology","score_opus":0.007539182471492525,"score_gpt":0.15950525448118144,"score_spread":0.15196607200968892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2196442963","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997127,0.00006578266,0.000054695596,0.00014399351,0.000008697256,0.000010632611,0.00012464703,0.000005579956,0.0024589817],"genre_scores_gemma":[0.9982425,0.0002213612,0.00009457921,0.000048579044,0.000008109072,0.000007327068,0.00016619713,0.000002662322,0.0012087859],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998198,0.000019843845,0.000012589671,0.0000212274,0.000056992074,0.000069581336],"domain_scores_gemma":[0.999777,0.000020203548,0.00007720911,0.000023813684,0.00006388871,0.00003790008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016677138,0.00023031514,0.00015585138,0.0007284224,0.0016011015,0.00069674576,0.00036846634,0.00086100365,0.0010158858],"category_scores_gemma":[0.00081582257,0.00025540765,0.00010143001,0.0006623167,0.0012628874,0.00038117633,0.0010449806,0.0005569198,0.0002302572],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008429394,0.0006213123,0.7752948,0.0003342583,0.00016554767,0.02248304,0.039218083,0.011817672,0.033216145,0.004190166,0.0062396987,0.10557628],"study_design_scores_gemma":[0.0000089406585,0.00017792708,0.9855688,0.000042737167,0.000017155924,0.0013998293,0.0056192707,0.00066866435,0.0011203827,0.00015258964,0.005205371,0.000018352075],"about_ca_topic_score_codex":0.11583044,"about_ca_topic_score_gemma":0.34658554,"teacher_disagreement_score":0.11583044,"about_ca_system_score_codex":0.0031668292,"about_ca_system_score_gemma":0.0011626746,"threshold_uncertainty_score":0.2303124},"labels":[],"label_agreement":null},{"id":"W2206011028","doi":"10.1306/m82813c8","title":"Kinematics and Sedimentary Balance of the Sub-Himalayan Zone, Western Nepal","year":2004,"lang":"en","type":"book-chapter","venue":"American Association of Petroleum Geologists eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Kinematics; Geology; Balance (ability); Sedimentary rock; Geodesy; Physical geography; Geography; Paleontology; Physical medicine and rehabilitation; Physics","score_opus":0.007530830598065899,"score_gpt":0.19357197210987484,"score_spread":0.18604114151180895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2206011028","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9660149,0.0015116468,0.0004214999,0.0002471748,0.000011131583,0.0000121867015,0.00074837764,0.000040640705,0.030992348],"genre_scores_gemma":[0.9873585,0.0011786321,0.00037104427,0.000019213072,0.0000062409326,0.0000074143168,0.0003394729,0.000010172436,0.01070929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99998164,0.0000026642454,0.0000018583119,0.0000046604614,0.0000046798086,0.0000044751605],"domain_scores_gemma":[0.99997795,0.000005439256,0.0000047481367,0.000002011949,0.000006595423,0.0000032879973],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000037332138,0.000102309015,0.00007568439,0.00068516284,0.0003275718,0.0007557912,0.00015619176,0.00012017967,0.0023596024],"category_scores_gemma":[0.00018620199,0.0001290492,0.000057365327,0.0010291061,0.0003032757,0.00033370894,0.000291302,0.00012745765,0.00037392467],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021983904,0.00006592929,0.62511283,0.0005575406,0.00019074253,0.005923254,0.019837888,0.029083941,0.018386967,0.036192287,0.0063850004,0.25804365],"study_design_scores_gemma":[0.0000070843944,0.000028203878,0.9652303,0.000055530192,0.000024148409,0.0009753379,0.0041172863,0.006479408,0.00081504654,0.0024742053,0.019781457,0.000012093674],"about_ca_topic_score_codex":0.03826514,"about_ca_topic_score_gemma":0.08174363,"teacher_disagreement_score":0.03826514,"about_ca_system_score_codex":0.0006721699,"about_ca_system_score_gemma":0.00043135654,"threshold_uncertainty_score":0.07608479},"labels":[],"label_agreement":null},{"id":"W2210393033","doi":"10.5194/npg-22-589-2015","title":"Brief Communication: Earthquake sequencing: analysis of time series constructed from the Markov chain model","year":2015,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Markov chain; Series (stratigraphy); Computer science; Hilbert–Huang transform; Statistical physics; Time series; Mode (computer interface); State (computer science); Algorithm; Mathematics; Statistics; Physics; Geology; Machine learning","score_opus":0.026488343347766116,"score_gpt":0.23270404346427823,"score_spread":0.2062157001165121,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2210393033","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10522975,0.0009909606,0.8880845,0.0008459403,0.00035678563,0.000051695,0.0011451927,0.00039403525,0.002901156],"genre_scores_gemma":[0.88570297,0.0030815562,0.09847714,0.00025559924,0.00071222405,0.00014650714,0.0033829105,0.00013304902,0.008108006],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998344,0.00004256113,0.000010687745,0.000045780023,0.00005264803,0.0000138044825],"domain_scores_gemma":[0.9975805,0.001672769,0.0002685408,0.00013476243,0.00025881507,0.000084645784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007178297,0.0002914431,0.00031687133,0.00076609635,0.00018378247,0.00045193097,0.0002781081,0.00033318062,0.0024685583],"category_scores_gemma":[0.005880712,0.00013438823,0.0003685427,0.001053619,0.00031014238,0.00071771746,0.00021915266,0.00056731433,0.00037470614],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012416918,0.000076231285,0.014085151,0.00030773273,0.00016073284,0.00056896225,0.0002361034,0.7215411,0.009292444,0.14005314,0.010900203,0.10265404],"study_design_scores_gemma":[0.000003504455,0.000026451236,0.0026977586,0.000015964306,0.000016954804,0.000092515584,0.000011397962,0.9623515,0.0008417016,0.03139236,0.0025322596,0.000017661087],"about_ca_topic_score_codex":0.0023713568,"about_ca_topic_score_gemma":0.0019233495,"teacher_disagreement_score":0.0024685583,"about_ca_system_score_codex":0.00038308286,"about_ca_system_score_gemma":0.00034861805,"threshold_uncertainty_score":0.008258164},"labels":[],"label_agreement":null},{"id":"W2211577158","doi":"10.1002/2015jb012338","title":"Downdip variations in seismic reflection character: Implications for fault structure and seismogenic behavior in the Alaska subduction zone","year":2015,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Seismology; Subduction; Trench; Transition zone; Reflection (computer programming); Wedge (geometry); Induced seismicity; Fault (geology); Submarine pipeline; Geophysics; Tectonics; Geometry; Geotechnical engineering","score_opus":0.07882716764501506,"score_gpt":0.3629786511622943,"score_spread":0.2841514835172792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2211577158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991893,0.000050794355,0.0002580618,0.000009825144,8.562981e-7,0.0000013733714,0.00007575377,0.000009494128,0.00040445323],"genre_scores_gemma":[0.9997763,0.000020147774,0.00008607946,0.0000020282191,6.0161324e-7,7.7872517e-7,0.000052733158,0.0000017215752,0.000059588496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990594,0.000017356593,0.0000147458395,0.000029930447,0.000015761487,0.000016207265],"domain_scores_gemma":[0.99968076,0.00007185783,0.000112663256,0.000043459087,0.00004888017,0.00004243463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025626188,0.00022283728,0.0001467784,0.00085020193,0.00018961921,0.00040382246,0.00019900771,0.00017758962,0.00116456],"category_scores_gemma":[0.0009185353,0.0001768957,0.00014126526,0.000501613,0.00024865175,0.00033292058,0.0003854008,0.0001564304,0.00016382594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016116415,0.000028242048,0.94826883,0.00002879144,0.0000313037,0.00018479166,0.0005996269,0.0020590331,0.03898582,0.00007850912,0.000037713693,0.009536262],"study_design_scores_gemma":[0.0000011237229,0.000014812992,0.9976593,0.0000031863374,0.0000055611795,0.0000378699,0.00025452487,0.0013367699,0.00060067617,0.000030983472,0.000052285937,0.0000028621096],"about_ca_topic_score_codex":0.009818973,"about_ca_topic_score_gemma":0.009759523,"teacher_disagreement_score":0.009818973,"about_ca_system_score_codex":0.0002459902,"about_ca_system_score_gemma":0.00010848379,"threshold_uncertainty_score":0.01952362},"labels":[],"label_agreement":null},{"id":"W2212697146","doi":"10.1007/s00024-015-1197-4","title":"Three-Dimensional Thermal Model of the Costa Rica-Nicaragua Subduction Zone","year":2015,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Consejo Nacional de Ciencia y Tecnología; Syracuse University","keywords":"Geology; Subduction; Mantle wedge; Slab; Volcanic arc; Slab window; Mantle (geology); Seismology; Transition zone; Volcano; Geophysics; Petrology; Oceanic crust; Tectonics","score_opus":0.023145398532553565,"score_gpt":0.19556068382954797,"score_spread":0.1724152852969944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2212697146","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9177845,0.00081462535,0.00734135,0.0014026361,0.00008820961,0.000103207574,0.006422477,0.0005763836,0.0654667],"genre_scores_gemma":[0.99407464,0.00021979524,0.00110482,0.000047330002,0.000013388493,0.00009089904,0.0005890736,0.00003914623,0.0038208554],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990344,0.000039075974,0.0000053432295,0.000021570973,0.000010579727,0.000019974774],"domain_scores_gemma":[0.9998661,0.000034918074,0.000019611844,0.000017035523,0.00003854992,0.00002367529],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014163874,0.00042840236,0.0004965729,0.00047140886,0.0005824721,0.0008580797,0.001373405,0.0010534342,0.0040932586],"category_scores_gemma":[0.0006792206,0.0003113354,0.00050123426,0.00075593055,0.0006630313,0.0003802503,0.0006765443,0.0004460774,0.00037096062],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004796851,0.000023664117,0.0047341892,0.000031792024,0.000033448032,0.00010216003,0.00009041043,0.98996055,0.00055167236,0.0023367298,0.00070023956,0.0013872037],"study_design_scores_gemma":[0.00005419616,0.000014971211,0.008026033,0.000015355416,0.000026730208,0.000024488068,0.00013192426,0.98908734,0.000121974495,0.00059852214,0.0018773793,0.000021044825],"about_ca_topic_score_codex":0.37263855,"about_ca_topic_score_gemma":0.22935872,"teacher_disagreement_score":0.37263855,"about_ca_system_score_codex":0.002702123,"about_ca_system_score_gemma":0.0018689041,"threshold_uncertainty_score":0.74093914},"labels":[],"label_agreement":null},{"id":"W2215297043","doi":"10.1007/s12517-015-2027-9","title":"Effect of fault-slip source mechanism on seismic source parameters","year":2015,"lang":"en","type":"article","venue":"Arabian Journal of Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Slip (aerodynamics); Mechanism (biology); Fault (geology); Seismology; Physics; Thermodynamics","score_opus":0.019949174091086267,"score_gpt":0.2320956155365162,"score_spread":0.21214644144542993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2215297043","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998495,0.00009840416,0.0006045242,0.000033328146,0.0000124692215,0.0000036261351,0.00009411335,0.000052097592,0.0006064491],"genre_scores_gemma":[0.99939585,0.0000333092,0.00013798778,0.0000075702724,0.0000022807708,0.000001166578,0.00007113577,0.000025964868,0.00032471053],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996215,0.0001221089,0.00003521559,0.00008328415,0.00004376173,0.0000940529],"domain_scores_gemma":[0.98845416,0.008855566,0.0005543693,0.00073429366,0.00072776544,0.0006738694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011779284,0.000530166,0.00060825795,0.0005700114,0.0004217339,0.0009597427,0.0006118926,0.0008938131,0.0053139287],"category_scores_gemma":[0.008880823,0.00035588144,0.0004958216,0.00041160083,0.00049579795,0.00080474786,0.0005866264,0.000509939,0.0006016954],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.019636767,0.001104443,0.31240246,0.00040561878,0.00067816995,0.0040428066,0.00061657635,0.14676896,0.47672173,0.0014931489,0.0013102153,0.034819152],"study_design_scores_gemma":[0.00064893445,0.0027972292,0.62465185,0.000081217346,0.001580158,0.0018449287,0.001285283,0.23141806,0.13319139,0.00076151587,0.0015929674,0.00014652526],"about_ca_topic_score_codex":0.0026736557,"about_ca_topic_score_gemma":0.0023744158,"teacher_disagreement_score":0.0053139287,"about_ca_system_score_codex":0.00033981682,"about_ca_system_score_gemma":0.00050650554,"threshold_uncertainty_score":0.017776847},"labels":[],"label_agreement":null},{"id":"W2227425269","doi":"10.4138/atlgeol.2015.010","title":"Geology and Hydrogeology of Faults on Cape Breton Island, Nova Scotia, Canada: an overview","year":2015,"lang":"en","type":"article","venue":"Atlantic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Structural basin; Aquifer; Hydrogeology; Groundwater recharge; Groundwater flow; Rift; Groundwater; Geomorphology; Paleontology","score_opus":0.03746913746360408,"score_gpt":0.2405327645495119,"score_spread":0.2030636270859078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2227425269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.79569066,0.084151685,0.0013936498,0.0022507217,0.00019058664,0.0003721991,0.02904365,0.00013632205,0.08677049],"genre_scores_gemma":[0.9113071,0.055947088,0.0018118629,0.000215091,0.00003946537,0.00005173776,0.0059229364,0.000034222474,0.024670575],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997751,0.000010871488,0.00002234242,0.000030559764,0.000087220964,0.00007390609],"domain_scores_gemma":[0.99896777,0.000053989334,0.00012737012,0.000020458414,0.0006771205,0.00015325092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001805129,0.00046992584,0.00027391408,0.0062897713,0.0013181795,0.0012407287,0.0005692103,0.00021305853,0.0032410242],"category_scores_gemma":[0.000734895,0.00020265492,0.00025477918,0.010718237,0.0007348456,0.00030684308,0.000530189,0.00024682164,0.00032957314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013241763,0.00005158303,0.7836573,0.0019222026,0.00015195894,0.0018862883,0.0032562313,0.003966421,0.003160686,0.0035028805,0.016716925,0.18159516],"study_design_scores_gemma":[0.0000029979792,0.000016872456,0.95722556,0.00034534562,0.00002486345,0.00035125486,0.002011168,0.00052086887,0.00019580655,0.00010282288,0.039178997,0.000023368502],"about_ca_topic_score_codex":0.99581736,"about_ca_topic_score_gemma":0.9983701,"teacher_disagreement_score":0.023957686,"about_ca_system_score_codex":0.023957686,"about_ca_system_score_gemma":0.026299627,"threshold_uncertainty_score":0.17382598},"labels":[],"label_agreement":null},{"id":"W2227461811","doi":"10.1017/cbo9781139628921","title":"Intraplate Earthquakes","year":2014,"lang":"en","type":"book","venue":"Cambridge University Press eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Seismology; Geology; Tectonics; Tectonophysics; Plate tectonics; Geophysics","score_opus":0.016117597092382616,"score_gpt":0.17446986162492212,"score_spread":0.1583522645325395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2227461811","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.006251522,0.11434318,0.013105003,0.0040597753,0.008612032,0.000094344316,0.0012921258,0.00082605676,0.85141605],"genre_scores_gemma":[0.028067648,0.05424362,0.0039971513,0.002327643,0.0038798843,0.00005832439,0.0013644963,0.0003827762,0.9056785],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998135,0.000023772664,0.0000095613295,0.000038621965,0.0000951145,0.000019457606],"domain_scores_gemma":[0.99975127,0.000094522286,0.000027649892,0.000029822,0.00006572818,0.000030902986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015491914,0.0007264855,0.0003821746,0.00081177073,0.0005604618,0.0018161219,0.0005978876,0.0008842524,0.02999523],"category_scores_gemma":[0.0007798245,0.00024596442,0.00033905977,0.0012700345,0.00063299935,0.0016815171,0.001035768,0.0015712993,0.01596113],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000569181,0.000027587232,0.0004972272,0.0007512448,0.00001959667,0.000302956,0.001087074,0.00067580544,0.002273852,0.095804445,0.56396914,0.3345341],"study_design_scores_gemma":[0.0000036810272,0.00002569802,0.0009858563,0.00017756593,0.000006070244,0.0005240374,0.00011760099,0.00013283636,0.00029806176,0.0059113284,0.9918121,0.0000051910706],"about_ca_topic_score_codex":0.0009546021,"about_ca_topic_score_gemma":0.0021448908,"teacher_disagreement_score":0.02999523,"about_ca_system_score_codex":0.00044699683,"about_ca_system_score_gemma":0.000331453,"threshold_uncertainty_score":0.10034406},"labels":[],"label_agreement":null},{"id":"W2230994827","doi":"10.1093/gji/ggv365","title":"Seismogenic faulting of the sedimentary sequence and laterally variable material properties in the Zagros Mountains (Iran) revealed by the August 2014 Murmuri (E. Dehloran) earthquake sequence","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Seismology; Aftershock; Décollement; Sequence (biology); Fault (geology); Layering; Sedimentary rock; Thrust fault; Basement; Slip (aerodynamics); Tectonics; Paleontology","score_opus":0.03992929817099997,"score_gpt":0.2401701950100571,"score_spread":0.20024089683905713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2230994827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993031,0.00003169628,0.00012853347,0.000025064975,0.0000019013597,0.0000021005126,0.0001222521,0.000012773303,0.00037265426],"genre_scores_gemma":[0.9997025,0.000024282597,0.00008756959,0.000002082587,0.0000023752561,9.614381e-7,0.00010138806,0.0000014063938,0.00007738276],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997056,0.0000034881195,0.0000028379366,0.0000067962123,0.0000045317634,0.000011729851],"domain_scores_gemma":[0.99994326,0.00000858254,0.000023571294,0.0000063995644,0.00000957205,0.000008581461],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000088393404,0.00023052144,0.00011896843,0.0005417146,0.00019155363,0.0003126328,0.00026099093,0.00027751533,0.0008939033],"category_scores_gemma":[0.0002396263,0.00017455581,0.00024555388,0.00038140477,0.00014494307,0.00017585218,0.00022444055,0.00012535282,0.00012326827],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029120714,0.00014171163,0.8322588,0.000060411236,0.00009550477,0.0011706435,0.00047147783,0.13376674,0.010684502,0.0010086227,0.00081060076,0.019239878],"study_design_scores_gemma":[0.000046255875,0.00006622285,0.86092937,0.000013340557,0.000050009567,0.00023732308,0.00029824095,0.13695024,0.0005113429,0.0003238301,0.00056184735,0.0000120750965],"about_ca_topic_score_codex":0.030920092,"about_ca_topic_score_gemma":0.04229215,"teacher_disagreement_score":0.030920092,"about_ca_system_score_codex":0.00036005763,"about_ca_system_score_gemma":0.00028312358,"threshold_uncertainty_score":0.061480224},"labels":[],"label_agreement":null},{"id":"W2235552864","doi":"10.1016/0967-0653(93)95868-7","title":"10.1016/0967-0653(93)95868-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lineation; Geology; Seamount; Fracture (geology); Seismology; Fracture zone; Structural basin; Paleontology; Tectonics","score_opus":0.008065854314867305,"score_gpt":0.15999705494811042,"score_spread":0.1519312006332431,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2235552864","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00058650284,0.00038460348,0.00046990105,0.0004030904,0.00029512966,0.00012622881,0.00092409784,0.00086776115,0.99594265],"genre_scores_gemma":[0.0007778318,0.0002576062,0.00030446722,0.00033709037,0.000087392866,0.000075599775,0.00046104303,0.0001710198,0.997528],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99932563,0.00004519614,0.00006706966,0.0002478003,0.00014763046,0.00016670178],"domain_scores_gemma":[0.9978077,0.00055145874,0.00014187412,0.0002649496,0.0005136232,0.00072040275],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012119089,0.0035332246,0.002283734,0.0030173224,0.0032044672,0.0040778746,0.003731325,0.0066411854,0.9912174],"category_scores_gemma":[0.001670096,0.0014364539,0.0015800934,0.0028173781,0.00272298,0.006575531,0.003769424,0.0031458207,0.9944712],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049001124,0.00033380225,0.0015750426,0.0007445347,0.00005629572,0.00042162565,0.00016295846,0.00059158663,0.0028330546,0.0051178397,0.42195493,0.5657183],"study_design_scores_gemma":[0.00010065729,0.00021240854,0.0015023175,0.00060149026,0.000023949005,0.00055659906,0.00024439028,0.00022644587,0.00043016567,0.00080987235,0.99525046,0.00004122364],"about_ca_topic_score_codex":0.005582972,"about_ca_topic_score_gemma":0.005228953,"teacher_disagreement_score":0.008782625,"about_ca_system_score_codex":0.0012112223,"about_ca_system_score_gemma":0.00093051646,"threshold_uncertainty_score":0.012527287},"labels":[],"label_agreement":null},{"id":"W2237791779","doi":"","title":"Micro-Seismicity in the Southwestern Yukon, Canada","year":2012,"lang":"en","type":"dissertation","venue":"UVic’s Research and Learning Repository (University of Victoria)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Seismology; Geology; Geography; Physical geography","score_opus":0.02106259395252259,"score_gpt":0.23422219452596663,"score_spread":0.21315960057344405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2237791779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9900928,0.0007595065,0.00018764376,0.00042737197,0.0000115266375,0.000026650268,0.0033622514,0.000034971636,0.0050971652],"genre_scores_gemma":[0.99409467,0.0006423962,0.00039544667,0.000077958415,0.0000022922038,0.000013079935,0.0012918134,0.000007655595,0.0034746928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998486,0.000007435583,0.000012895655,0.000032173637,0.000043476954,0.000055435685],"domain_scores_gemma":[0.9995609,0.000022414948,0.000045838875,0.000011516767,0.00028343595,0.0000758345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009634079,0.00020148503,0.00017147292,0.0010172379,0.0018200368,0.0007171363,0.0003834769,0.0002102759,0.0018542362],"category_scores_gemma":[0.00036501698,0.00015287953,0.00015764943,0.0027672262,0.00037570158,0.00029077203,0.0004797836,0.00022053927,0.00019423832],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000085586165,0.000022918277,0.9566458,0.00013931673,0.00006855851,0.00074966514,0.0022876821,0.00094274385,0.003269033,0.0006243982,0.003313239,0.03185103],"study_design_scores_gemma":[0.0000055281466,0.000011392314,0.9899596,0.000029452971,0.000013271165,0.000117993244,0.0046767057,0.0006955825,0.00019407712,0.000059116446,0.0042246343,0.000012605934],"about_ca_topic_score_codex":0.9891803,"about_ca_topic_score_gemma":0.9977278,"teacher_disagreement_score":0.012928708,"about_ca_system_score_codex":0.012928708,"about_ca_system_score_gemma":0.01804894,"threshold_uncertainty_score":0.09380478},"labels":[],"label_agreement":null},{"id":"W2239854719","doi":"10.1130/2007.2425(09)","title":"Effects of a lithospheric weak zone on postglacial seismotectonics in eastern Canada and the northeastern United States","year":2007,"lang":"en","type":"book-chapter","venue":"Geological Society of America eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismotectonics; Geology; Lithosphere; Seismology; Paleontology; Tectonics","score_opus":0.010972149160966465,"score_gpt":0.18931644254174052,"score_spread":0.17834429338077404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2239854719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99221283,0.0010057979,0.000046770394,0.0006127357,0.000017408884,0.000005011573,0.0012989517,0.00000897281,0.004791557],"genre_scores_gemma":[0.9959407,0.00077723124,0.00006889657,0.000070841925,0.00000697348,0.0000028713039,0.0007919624,0.000005896789,0.002334662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997286,0.00002971464,0.00001545992,0.00002603221,0.00007555822,0.00012453526],"domain_scores_gemma":[0.9986784,0.00017295053,0.0001354632,0.000023625322,0.00067540153,0.00031421552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004214979,0.00023506276,0.00031845464,0.0011895088,0.002328653,0.0015827941,0.0009773159,0.00041795018,0.0023447492],"category_scores_gemma":[0.0018040936,0.00019180604,0.00031398205,0.0027929246,0.0010741261,0.0004273619,0.00096959254,0.0006653554,0.00010745916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022893495,0.00003519665,0.9773726,0.00003704921,0.000107195025,0.00027194322,0.0018700841,0.001762282,0.0006874539,0.0015986017,0.0025557545,0.0134728905],"study_design_scores_gemma":[0.0000043914138,0.000008936776,0.9957111,0.000015519592,0.000038405833,0.000017447916,0.0025139863,0.0003319916,0.00010762875,0.00009761392,0.0011470764,0.0000058787373],"about_ca_topic_score_codex":0.99539113,"about_ca_topic_score_gemma":0.99853253,"teacher_disagreement_score":0.01779747,"about_ca_system_score_codex":0.01779747,"about_ca_system_score_gemma":0.023945663,"threshold_uncertainty_score":0.1291303},"labels":[],"label_agreement":null},{"id":"W2246934854","doi":"","title":"Physical modeling of landslide generated tsunamis in various scenarios from Fjords to Conical Islands","year":2014,"lang":"en","type":"dissertation","venue":"SMARTech Repository (Georgia Institute of Technology)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Fjord; Landslide; Geology; Bathymetry; Conical surface; Oceanography; Seismology; Geomorphology; Geography; Engineering","score_opus":0.008773192761927834,"score_gpt":0.22338878207259344,"score_spread":0.2146155893106656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2246934854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99293125,0.000048728547,0.002856977,0.000077738005,0.000013308183,0.000043789223,0.00035844345,0.0001297396,0.00354015],"genre_scores_gemma":[0.9984479,0.000033099157,0.00061299093,0.000008981583,0.0000020405662,0.000021936667,0.00013670139,0.000007698688,0.0007285333],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989927,0.00001512628,0.0000069402054,0.000021657479,0.00001603873,0.000040911164],"domain_scores_gemma":[0.9997826,0.00007708006,0.000027980781,0.000018453522,0.000040842147,0.00005300424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017575061,0.00062606856,0.00039467984,0.00053858384,0.00061771617,0.0009133383,0.00091834273,0.0010407988,0.0016619492],"category_scores_gemma":[0.00042718792,0.00035633057,0.00058151025,0.00038161065,0.00061310455,0.00036580846,0.0005099159,0.0004944465,0.00014935341],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037384885,0.000046783996,0.0042489753,0.000009022473,0.000011026433,0.0001299641,0.00002397477,0.99358094,0.0010652498,0.00018300732,0.000083705396,0.0005799669],"study_design_scores_gemma":[0.000011450993,0.000029255918,0.002261957,0.0000018032842,0.0000064999167,0.000010450299,0.000033599223,0.9972579,0.00024537416,0.000061733626,0.00007577734,0.000004287416],"about_ca_topic_score_codex":0.053765092,"about_ca_topic_score_gemma":0.030121287,"teacher_disagreement_score":0.053765092,"about_ca_system_score_codex":0.0011608453,"about_ca_system_score_gemma":0.0006865384,"threshold_uncertainty_score":0.10690427},"labels":[],"label_agreement":null},{"id":"W2252967810","doi":"10.1007/s00024-015-1226-3","title":"Real-Time Assessment of the 16 September 2015 Chile Tsunami and Implications for Near-Field Forecast","year":2016,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Center for Operational Oceanographic Products and Services; National Ocean Service; National Oceanic and Atmospheric Administration; Joint Institute for the Study of the Atmosphere and Ocean","keywords":"Epicenter; Seismology; Geology; Arrival time; Quarter (Canadian coin); Geography; Archaeology","score_opus":0.010077402241426415,"score_gpt":0.23619932669591345,"score_spread":0.22612192445448703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2252967810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97588116,0.0003795738,0.0014959555,0.0024259256,0.00012714202,0.00004805844,0.009848785,0.00020107171,0.009592366],"genre_scores_gemma":[0.9946325,0.00015777304,0.00055876054,0.000037985283,0.000020747666,0.000016220642,0.0029815373,0.000011758585,0.0015827994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998266,0.000038258513,0.000016854621,0.000037131,0.00004779775,0.00003346132],"domain_scores_gemma":[0.99888796,0.00026783475,0.00023079927,0.00006029981,0.00040848023,0.0001447359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069236977,0.00024798786,0.00021118991,0.0008675395,0.00031575226,0.0011957997,0.00038901748,0.000753778,0.0030878535],"category_scores_gemma":[0.0036260101,0.00016684899,0.00020989332,0.0009042852,0.0003017848,0.0013662284,0.0006833672,0.0005727753,0.00060890237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010365485,0.00034556823,0.6334299,0.00037400099,0.00026065228,0.0012985106,0.0013260288,0.28020617,0.005992987,0.0045216437,0.02444633,0.046761673],"study_design_scores_gemma":[0.000112668735,0.00015446925,0.7064853,0.00015247641,0.000069671776,0.00010946503,0.00402192,0.27118275,0.0018304632,0.002072057,0.013699727,0.000109130546],"about_ca_topic_score_codex":0.16221315,"about_ca_topic_score_gemma":0.14717084,"teacher_disagreement_score":0.16221315,"about_ca_system_score_codex":0.0026708967,"about_ca_system_score_gemma":0.0016832897,"threshold_uncertainty_score":0.3225379},"labels":[],"label_agreement":null},{"id":"W2255897092","doi":"10.1139/cjce-2012-0553","title":"Impact and damage to structures during the 27 February 2010 Chile tsunami","year":2013,"lang":"en","type":"article","venue":"Canadian Journal of Civil Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"McMaster University; University of Ottawa","funders":"","keywords":"Masonry; Infill; Masonry veneer; Geology; Geotechnical engineering; Load bearing; Structural engineering; Punching; Engineering","score_opus":0.005019151093430986,"score_gpt":0.1704861019019032,"score_spread":0.1654669508084722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2255897092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9813829,0.00073378795,0.00010407674,0.00023710098,0.000024764164,0.000029090652,0.0010802826,0.000037394195,0.016370526],"genre_scores_gemma":[0.9898123,0.0014037156,0.00010492935,0.000063176085,0.000019206253,0.000020276406,0.00085515645,0.000007662324,0.0077134594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982786,0.000009330139,0.0000070569436,0.000015814441,0.00008127875,0.00005862233],"domain_scores_gemma":[0.99980444,0.000024681933,0.00006257684,0.0000145584245,0.000063087784,0.000030779738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012018609,0.00031141526,0.00020295694,0.0009319054,0.0008252729,0.0004765227,0.00024153154,0.0005194628,0.0024453192],"category_scores_gemma":[0.0005464014,0.0001828857,0.00014611328,0.000787134,0.0005068325,0.00020700906,0.000844086,0.0003010061,0.00048397176],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012419398,0.00035818008,0.6829915,0.00080164487,0.00023687992,0.03125108,0.0123601835,0.021806575,0.04897104,0.0015394068,0.034776714,0.1636648],"study_design_scores_gemma":[0.000009297585,0.00018614404,0.9834657,0.000058803525,0.000013487187,0.0012047311,0.002046918,0.0005411449,0.0012468495,0.00010393272,0.011105707,0.000017333985],"about_ca_topic_score_codex":0.050094914,"about_ca_topic_score_gemma":0.13353924,"teacher_disagreement_score":0.050094914,"about_ca_system_score_codex":0.0024989971,"about_ca_system_score_gemma":0.0005377592,"threshold_uncertainty_score":0.09960663},"labels":[],"label_agreement":null},{"id":"W2258143121","doi":"10.1017/s0033822200043198","title":"Recurrence and Extent of Great Earthquakes in Southern Alaska During the Late Holocene from an Analysis of the Radiocarbon Record of Land-Level Change and Village Abandonment","year":2007,"lang":"en","type":"article","venue":"Radiocarbon","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"U.S. Geological Survey","keywords":"Radiocarbon dating; Geology; Holocene; Period (music); Paleontology; Pleistocene; Chronology; Hiatus; Archaeology; Subduction; Tectonics; Geography","score_opus":0.0246757552709622,"score_gpt":0.21987525527761995,"score_spread":0.19519950000665776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2258143121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995975,0.00006739591,0.000012125877,0.0000049308765,0.0000010867748,4.5733046e-7,0.00015792013,0.000001924796,0.00015664891],"genre_scores_gemma":[0.9993759,0.00007613486,0.000028443063,0.0000029299226,0.0000023529794,0.000001726106,0.00034764208,8.1686e-7,0.0001640625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999361,0.000009809915,0.000010205912,0.000020550868,0.000009956153,0.000013248532],"domain_scores_gemma":[0.9995028,0.00007538643,0.00020564788,0.000035807476,0.00007612543,0.00010423964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022012017,0.00011756644,0.000110149536,0.0012267196,0.0003548233,0.00039569795,0.00016347218,0.0002025338,0.00064588164],"category_scores_gemma":[0.00067843776,0.00014143495,0.00012845609,0.0008550986,0.00024086093,0.00022493114,0.00032239253,0.00015693717,0.00016188936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004333926,0.0000114731965,0.9965898,0.000007773421,0.00002115979,0.00009478034,0.00050716277,0.00009558569,0.00067175046,0.000014044592,0.000049745224,0.0018933548],"study_design_scores_gemma":[4.982069e-7,0.000007692842,0.9996039,0.0000021053131,0.0000039633733,0.000036221412,0.00018432594,0.000048342332,0.00002598323,0.000004964925,0.00008103209,0.0000010387148],"about_ca_topic_score_codex":0.023629852,"about_ca_topic_score_gemma":0.052824866,"teacher_disagreement_score":0.023629852,"about_ca_system_score_codex":0.0002602661,"about_ca_system_score_gemma":0.00015334261,"threshold_uncertainty_score":0.046984613},"labels":[],"label_agreement":null},{"id":"W2261729205","doi":"10.1139/cjes-2015-0203","title":"The two-stage Aegean extension, from localized to distributed, a result of slab rollback acceleration","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Agence Nationale de la Recherche","keywords":"Geology; Seismology; Subduction; Metamorphic rock; Sedimentary rock; Neogene; Mantle (geology); Metamorphic core complex; Detachment fault; Accretionary wedge; Sedimentary basin; Paleontology; Tectonics; Structural basin","score_opus":0.03269920616654275,"score_gpt":0.24138717212855296,"score_spread":0.2086879659620102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2261729205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98491955,0.00070515356,0.0046824934,0.00011691723,0.000028084658,0.00004872943,0.00076578854,0.0001648585,0.008568422],"genre_scores_gemma":[0.99514765,0.00041202462,0.0019764076,0.000026555124,0.00000782706,0.00001621684,0.0004727572,0.000029756955,0.0019107732],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999287,0.000006005129,0.0000072382645,0.00003250729,0.00001259085,0.00001289086],"domain_scores_gemma":[0.9999528,0.00000241079,0.000017452168,0.000010242707,0.000010575932,0.00000656399],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014519897,0.00050204305,0.00014871478,0.0006778651,0.00027722813,0.000586279,0.0002571996,0.00033991275,0.0028161807],"category_scores_gemma":[0.00025299352,0.0002586384,0.0004715453,0.0005141493,0.00050117786,0.00038126393,0.00065335183,0.00025357865,0.00037543947],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064707064,0.000105022824,0.696089,0.00059063063,0.00043540713,0.0025874954,0.0014198946,0.056332782,0.13198307,0.011539073,0.0015648034,0.096705675],"study_design_scores_gemma":[0.00008125788,0.00015477891,0.9517766,0.000106267275,0.00012010281,0.0013166488,0.00038252663,0.03085983,0.0051926738,0.001831117,0.008135015,0.000043256558],"about_ca_topic_score_codex":0.011213357,"about_ca_topic_score_gemma":0.013567459,"teacher_disagreement_score":0.011213357,"about_ca_system_score_codex":0.0006584514,"about_ca_system_score_gemma":0.0004091795,"threshold_uncertainty_score":0.02229619},"labels":[],"label_agreement":null},{"id":"W2265034978","doi":"10.1093/gji/ggv353","title":"The seismic sequence of January–February 2014 at Cephalonia Island (Greece): constraints from SAR interferometry and GPS","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Geodesy; Interferometric synthetic aperture radar; Azimuth; Synthetic aperture radar; Global Positioning System; Slip (aerodynamics); Crust; Interferometry; Induced seismicity; Remote sensing; Geophysics; Geometry","score_opus":0.022817288685080858,"score_gpt":0.24319286194880632,"score_spread":0.22037557326372548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2265034978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964736,0.0000663359,0.00017394325,0.000045888835,0.0000053447743,0.000010471608,0.0017441675,0.00002064974,0.0014595917],"genre_scores_gemma":[0.99493635,0.00010593949,0.00042659754,0.0000133293615,0.000009492357,0.0000141385935,0.003962585,0.000009404906,0.0005221551],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998741,0.000017539758,0.000019338018,0.000039008104,0.00002587782,0.000024146051],"domain_scores_gemma":[0.99983835,0.000029076422,0.000049772058,0.000025881931,0.000032056312,0.000024757597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018092059,0.00030137852,0.00026172627,0.0014697174,0.00014325386,0.0005009555,0.0002552268,0.00036858756,0.0011951614],"category_scores_gemma":[0.0006884053,0.00013995146,0.0002660004,0.0014073713,0.00033382062,0.0002519793,0.0004921117,0.00014994974,0.0003305316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047412358,0.00013463153,0.84866047,0.00036409407,0.00028318504,0.0057849274,0.0018744711,0.059698388,0.022610884,0.0018403141,0.003750135,0.054524392],"study_design_scores_gemma":[0.000013011164,0.00003307128,0.98946977,0.000027834896,0.000021979438,0.00034309993,0.00044164143,0.006283264,0.0005341783,0.00014953288,0.0026685162,0.0000142243225],"about_ca_topic_score_codex":0.021520313,"about_ca_topic_score_gemma":0.0315992,"teacher_disagreement_score":0.021520313,"about_ca_system_score_codex":0.0005220534,"about_ca_system_score_gemma":0.00048397362,"threshold_uncertainty_score":0.042790115},"labels":[],"label_agreement":null},{"id":"W2267905838","doi":"10.4095/211271","title":"Regional interpretations of public domain seismic in the Liard region north of 60°: pre-Phanerozoic events, Phanerozic stratigraphy and Laramide deformation","year":2000,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Phanerozoic; Stratigraphy; Paleontology; Geology; Seismology; Tectonics; Cenozoic","score_opus":0.03926166178813205,"score_gpt":0.25129009389024703,"score_spread":0.21202843210211497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2267905838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9404167,0.0007816629,0.0009809969,0.00020400318,0.000021688322,0.000049846167,0.017949477,0.00031720687,0.03927855],"genre_scores_gemma":[0.97830236,0.00054634776,0.0018627624,0.00002613623,0.000029424958,0.00003645969,0.013889429,0.00006124979,0.0052457987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979764,0.000030114272,0.000018331735,0.000041187173,0.0000576961,0.000055044296],"domain_scores_gemma":[0.99923515,0.00010290818,0.00018975697,0.00008374534,0.00033970308,0.000048688977],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005200263,0.00037534107,0.00025235052,0.0033240612,0.0003388552,0.0008256748,0.00041454763,0.00024143183,0.004404215],"category_scores_gemma":[0.0014283552,0.000229377,0.0002604915,0.0031670253,0.00030761576,0.00034616847,0.00070310384,0.00025000743,0.0008202693],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008479396,0.00009671614,0.8786745,0.00037663567,0.00016213597,0.0013847766,0.005362717,0.0098395925,0.016233344,0.003025774,0.015471653,0.06852422],"study_design_scores_gemma":[0.000039342343,0.000025845198,0.98496073,0.000050943858,0.0000821336,0.00023106468,0.0020628595,0.0010337917,0.0017684853,0.00010446095,0.009631185,0.0000091532975],"about_ca_topic_score_codex":0.22862114,"about_ca_topic_score_gemma":0.46348155,"teacher_disagreement_score":0.7713789,"about_ca_system_score_codex":0.0014954638,"about_ca_system_score_gemma":0.0014189564,"threshold_uncertainty_score":0.45458078},"labels":[],"label_agreement":null},{"id":"W226948311","doi":"","title":"Evaluation of Cross-Correlation Methods on a Massive Scale for Accurate Relocation of Seismic Events","year":2005,"lang":"en","type":"article","venue":"Defense Technical Information Center (DTIC)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Seismology; Geology; Intraplate earthquake; Relocation; Observatory; Seismic hazard; Scale (ratio); Geodesy; Geography; Tectonics; Cartography; Physics","score_opus":0.057774036489921334,"score_gpt":0.3592201285404925,"score_spread":0.30144609205057116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W226948311","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.23937865,0.0006347854,0.7528504,0.00022395722,0.00011729208,0.0002802056,0.0004154687,0.0024097492,0.003689591],"genre_scores_gemma":[0.3486072,0.0001801984,0.6490511,0.000056739107,0.000050649276,0.00019358906,0.0006414914,0.00015775104,0.0010612687],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99643683,0.0021274704,0.00019470212,0.00034102888,0.0007544318,0.0001455981],"domain_scores_gemma":[0.9669215,0.02039934,0.0012911373,0.0033463743,0.007517235,0.0005244816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010372831,0.00087477226,0.00058026175,0.0024111324,0.0006068795,0.00089712226,0.0010462363,0.0007588081,0.0028443134],"category_scores_gemma":[0.030405667,0.00034006426,0.0004942856,0.0023292876,0.00039710046,0.0016844647,0.001259095,0.00062984927,0.0010747843],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013442519,0.000779408,0.057068273,0.00027817665,0.0005683307,0.0002441911,0.00034981713,0.14313887,0.024633951,0.010605318,0.0038868624,0.7571026],"study_design_scores_gemma":[0.000098481156,0.00041278894,0.020019157,0.000027907305,0.00007109599,0.00025079498,0.00019503567,0.9612247,0.013030377,0.002015081,0.0026068883,0.000047561833],"about_ca_topic_score_codex":0.006549685,"about_ca_topic_score_gemma":0.0099270735,"teacher_disagreement_score":0.010372831,"about_ca_system_score_codex":0.00056432607,"about_ca_system_score_gemma":0.0011271283,"threshold_uncertainty_score":0.054857433},"labels":[],"label_agreement":null},{"id":"W2275741740","doi":"10.1002/2015gl067418","title":"Rapid automated W‐phase slip inversion for the Illapel great earthquake (2015, <i>M</i><i><sub>w</sub></i> = 8.3)","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Comisión Nacional de Investigación Científica y Tecnológica; Australian Research Council","keywords":"Seismology; Geology; Trench; Inversion (geology); Slip (aerodynamics); Rake; Geodesy; Tectonics; Physics; Geomorphology","score_opus":0.04202746635573346,"score_gpt":0.2932098401865539,"score_spread":0.2511823738308204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2275741740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9338728,0.00006184359,0.053131055,0.00016272294,0.000037439517,0.00008341121,0.0018227347,0.0052412795,0.0055866763],"genre_scores_gemma":[0.9444123,0.000016086598,0.052676864,0.000032487394,0.000013132255,0.000027503098,0.0017373065,0.00014726607,0.0009369777],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9998989,0.000018050923,0.000004415392,0.000022987078,0.0000313262,0.000024294017],"domain_scores_gemma":[0.99974257,0.00007871367,0.00003759309,0.00003403782,0.00008165139,0.000025516694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000290408,0.00036408,0.00027867878,0.000630741,0.00019090761,0.00034899582,0.00041992564,0.00021502998,0.0029142143],"category_scores_gemma":[0.0011188756,0.00017645468,0.00016972102,0.00035059097,0.00013557197,0.00032535888,0.00039899015,0.00022657885,0.00060978107],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018813042,0.00055882335,0.083300605,0.00018599938,0.00024130695,0.0010326339,0.0007429496,0.25849447,0.12959403,0.001993716,0.015889678,0.5060844],"study_design_scores_gemma":[0.00022174031,0.00012945599,0.034953948,0.00001196824,0.000022545431,0.000098620825,0.00017425523,0.94316703,0.017999643,0.0006277865,0.0025550271,0.0000380004],"about_ca_topic_score_codex":0.012104228,"about_ca_topic_score_gemma":0.022585448,"teacher_disagreement_score":0.012104228,"about_ca_system_score_codex":0.00020328503,"about_ca_system_score_gemma":0.0007043855,"threshold_uncertainty_score":0.024067521},"labels":[],"label_agreement":null},{"id":"W2276946064","doi":"10.1139/cjes-2015-0119","title":"Further studies on the focal mechanism and source rupture process of the 2012 Haida Gwaii, Canada, 7.8 moment magnitude earthquake","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Seismology; Seismic moment; Slip (aerodynamics); Moment magnitude scale; Thrust fault; Focal mechanism; Tsunami earthquake; Aftershock; Subduction; Magnitude (astronomy); Thrust; Fault (geology); Tectonics; Geometry","score_opus":0.021755816192150206,"score_gpt":0.21459137861809982,"score_spread":0.19283556242594962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2276946064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961599,0.0003211576,0.00041274907,0.000060199684,0.000003903866,0.000032380998,0.0005004684,0.000009647053,0.002499552],"genre_scores_gemma":[0.995886,0.00063038094,0.00048310522,0.000016533828,0.000004450172,0.00001415541,0.0008792434,0.0000058557584,0.0020803188],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999052,0.000005019677,0.0000033705658,0.0000140844895,0.000027121885,0.000045141347],"domain_scores_gemma":[0.99966395,0.00003850175,0.00007279155,0.000014325347,0.00014675508,0.000063685795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001677151,0.00042453886,0.00036647753,0.00090796524,0.00072953216,0.0006504225,0.0005048501,0.00039498642,0.0018364385],"category_scores_gemma":[0.00056787994,0.00016545119,0.00029336638,0.0013406051,0.00025014143,0.00037067113,0.00020399918,0.0004093926,0.00027648723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045670767,0.00043692187,0.8152236,0.00050863106,0.00026865493,0.0044167736,0.0024866327,0.019384509,0.111657456,0.0023033654,0.0017000942,0.041156717],"study_design_scores_gemma":[0.000010067968,0.00007590846,0.988419,0.000018169327,0.000035764715,0.00027261206,0.0009537271,0.0058835507,0.0027451839,0.00014202343,0.0014197393,0.000024328876],"about_ca_topic_score_codex":0.576353,"about_ca_topic_score_gemma":0.71326274,"teacher_disagreement_score":0.423647,"about_ca_system_score_codex":0.0036175824,"about_ca_system_score_gemma":0.0030159557,"threshold_uncertainty_score":0.85228384},"labels":[],"label_agreement":null},{"id":"W2278470402","doi":"10.14288/1.0085017","title":"Assessment of tsunami hazards on the British Columbia coast due to a local megathrust subduction earthquake","year":2010,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Seismology; Geology; Tsunami earthquake; Forensic engineering; Tectonics; Engineering","score_opus":0.00788775113582363,"score_gpt":0.17990435556945783,"score_spread":0.1720166044336342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2278470402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976661,0.000039200644,0.0001052537,0.000045408582,0.0000012235029,0.000010088356,0.0001304778,0.000011130633,0.0019910852],"genre_scores_gemma":[0.9990596,0.00008620327,0.00013181764,0.0000071001614,6.5931977e-7,0.0000032909857,0.00013726669,0.0000016986778,0.0005723921],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998764,0.000019098628,0.000005425462,0.000012604849,0.000051099272,0.000035334822],"domain_scores_gemma":[0.9996538,0.00006852883,0.00004389812,0.000016817206,0.00013308029,0.00008384501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018761557,0.00035655944,0.00016310225,0.0006250806,0.000844545,0.0009807611,0.00048859336,0.00036458852,0.001340286],"category_scores_gemma":[0.0009771371,0.0002050851,0.00023439135,0.0008845145,0.00036497714,0.000229052,0.00037182702,0.00028887155,0.00013427154],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043104857,0.0001334953,0.74014914,0.00009419469,0.00016952911,0.0019708069,0.00036440548,0.22690257,0.0059009884,0.0010039298,0.0011770122,0.02170285],"study_design_scores_gemma":[0.000068491616,0.00026684554,0.79726523,0.000044084998,0.00013943284,0.00023120991,0.0026524963,0.1957805,0.0017242329,0.00036128447,0.0014253203,0.000040798444],"about_ca_topic_score_codex":0.8496196,"about_ca_topic_score_gemma":0.9192324,"teacher_disagreement_score":0.15038037,"about_ca_system_score_codex":0.0061939643,"about_ca_system_score_gemma":0.0033058582,"threshold_uncertainty_score":0.30253196},"labels":[],"label_agreement":null},{"id":"W2281510867","doi":"10.5539/esr.v5n1p76","title":"The Role of Surface Processes in Partitioning of Strain and Uplift, St. Elias Orogen, Southern Alaska","year":2016,"lang":"en","type":"article","venue":"Earth Science Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Tectonics; Shear (geology); Fault (geology); Seismology; Font; Geodesy; Geometry; Geomorphology; Paleontology; Mathematics","score_opus":0.04070405943278349,"score_gpt":0.3015659324928112,"score_spread":0.2608618730600277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2281510867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99853444,0.00001750163,0.00013386329,0.000011443759,0.000001371974,0.0000012218183,0.00008566367,0.00001330913,0.0012011839],"genre_scores_gemma":[0.99947065,0.000020662646,0.00008222125,0.0000020298164,5.908111e-7,0.0000012168664,0.00007767852,0.0000028220181,0.00034218072],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999641,0.000003129529,0.0000037314196,0.0000148437575,0.000007242705,0.0000069631965],"domain_scores_gemma":[0.9999355,0.0000167069,0.000018808558,0.0000047799144,0.000012120127,0.00001196683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000101644175,0.00014023426,0.00013632722,0.00038461754,0.00045724813,0.00065334555,0.00023023237,0.00021593191,0.0012956082],"category_scores_gemma":[0.00025383697,0.0001448599,0.00012328084,0.00039373094,0.00037398972,0.00025747268,0.00038388453,0.00013258487,0.00017265485],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004184061,0.000091215625,0.8336704,0.0000869153,0.000075007956,0.000978035,0.0016735902,0.10724096,0.034846563,0.0013334913,0.0004989486,0.01908651],"study_design_scores_gemma":[0.000016564863,0.000047387337,0.9582024,0.000016660302,0.000025402764,0.00011772316,0.001642285,0.036697987,0.0021948784,0.00041005024,0.00061051466,0.000018065108],"about_ca_topic_score_codex":0.06629518,"about_ca_topic_score_gemma":0.0941143,"teacher_disagreement_score":0.06629518,"about_ca_system_score_codex":0.00062192546,"about_ca_system_score_gemma":0.00035829522,"threshold_uncertainty_score":0.13181859},"labels":[],"label_agreement":null},{"id":"W2282154076","doi":"10.3846/20296991.2015.1123445","title":"ESTIMATING EULER POLE PARAMETERS FOR EASTERN CANADA USING GPS VELOCITIES","year":2015,"lang":"en","type":"article","venue":"Geodesy and Cartography","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada; Université Laval","keywords":"Intraplate earthquake; Geology; Post-glacial rebound; Seismology; Global Positioning System; Geodesy; Euler's rotation theorem; Rotation (mathematics); Current (fluid); Geomorphology; Glacial period; Geometry; Oceanography","score_opus":0.04107358040731864,"score_gpt":0.2253274169913032,"score_spread":0.18425383658398456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2282154076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97476137,0.00030434996,0.008236656,0.00009311451,0.000008236317,0.000053569267,0.011830751,0.00026823924,0.0044437493],"genre_scores_gemma":[0.9751848,0.00029585816,0.009183751,0.000012553943,0.0000045602246,0.00001870143,0.013913308,0.000033956476,0.0013524509],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997305,0.000015778105,0.000011567577,0.000066559565,0.00009276244,0.000082849496],"domain_scores_gemma":[0.9990544,0.000112789545,0.000119625875,0.00005982877,0.0005502512,0.000103239865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026392716,0.00061543286,0.00034596835,0.0034812037,0.000883311,0.0011023686,0.00047924812,0.0002761845,0.0012781754],"category_scores_gemma":[0.0024194862,0.00034785745,0.0003301735,0.0039303787,0.00034877265,0.00037072483,0.0005242667,0.00040161848,0.00040311288],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001478787,0.000046383673,0.85217184,0.000041473744,0.000120358505,0.00019110262,0.0003719787,0.0803118,0.0022470336,0.0013384626,0.0034001237,0.059611615],"study_design_scores_gemma":[0.000021853344,0.000012265526,0.87224865,0.00004337866,0.000048531736,0.000061007264,0.0005371077,0.11881466,0.0010879601,0.000679016,0.006388783,0.000056875768],"about_ca_topic_score_codex":0.97839236,"about_ca_topic_score_gemma":0.98347086,"teacher_disagreement_score":0.021607637,"about_ca_system_score_codex":0.0067373523,"about_ca_system_score_gemma":0.0110140955,"threshold_uncertainty_score":0.04888314},"labels":[],"label_agreement":null},{"id":"W2285322365","doi":"10.1002/2015gl067514","title":"Linking fossil reefs with earthquakes: Geologic insight to where induced seismicity occurs in Alberta","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Induced seismicity; Reef; Tectonics; Precambrian; Basement; Sedimentary basin; Sedimentary rock; Seismology; Devonian; Structural basin; Paleontology; Earth science; Oceanography","score_opus":0.04390893715569616,"score_gpt":0.27873332066356615,"score_spread":0.23482438350787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2285322365","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980926,0.00006588205,0.00007113643,0.00004541006,8.835603e-7,0.0000032621147,0.00036072163,0.000004690551,0.0013554194],"genre_scores_gemma":[0.9990251,0.00009577148,0.00009633447,0.0000061681435,8.1981926e-7,0.000001280909,0.00025398453,0.0000012160085,0.00051924976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998728,0.000014478931,0.000007584829,0.000020992395,0.000039168903,0.00004482441],"domain_scores_gemma":[0.9994648,0.00006676512,0.0001136298,0.000029323095,0.00021937065,0.00010607211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019555048,0.000108356006,0.00008535188,0.0013112556,0.00057279,0.00063957414,0.0004074261,0.00015835754,0.0015560508],"category_scores_gemma":[0.0009076046,0.000100858924,0.00007547753,0.0022122955,0.0004333697,0.00013073377,0.0004955565,0.00016127339,0.00010661669],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050387578,0.000019413143,0.99008876,0.000013411076,0.000015896338,0.00017935678,0.00065063155,0.0006879977,0.0014397636,0.00019067373,0.00021155574,0.0064521506],"study_design_scores_gemma":[8.911567e-7,0.000003422531,0.99860543,0.000003285044,0.0000031738905,0.000021242844,0.00074598566,0.00027862162,0.00007349138,0.000028881976,0.00023384843,0.0000017371361],"about_ca_topic_score_codex":0.92153484,"about_ca_topic_score_gemma":0.9786357,"teacher_disagreement_score":0.07846516,"about_ca_system_score_codex":0.0047546923,"about_ca_system_score_gemma":0.0039865393,"threshold_uncertainty_score":0.1578545},"labels":[],"label_agreement":null},{"id":"W2285349111","doi":"10.1785/0120140301","title":"Detection and Location of Low‐Frequency Earthquakes Using Cross‐Station Correlation","year":2015,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geology; Correlation; Geodesy; Mathematics; Geometry","score_opus":0.026055278015028962,"score_gpt":0.23595561507304,"score_spread":0.20990033705801103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2285349111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97261715,0.000079864716,0.016857281,0.0000326747,0.0000068223467,0.000045149307,0.0046094805,0.00055704627,0.005194607],"genre_scores_gemma":[0.98671246,0.0000440555,0.008364469,0.000007367414,0.0000056482863,0.000030222158,0.0040056743,0.000048785463,0.00078127644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997142,0.000022406608,0.000017816892,0.000114356175,0.00008876812,0.000042319974],"domain_scores_gemma":[0.9988117,0.00022568447,0.00026832713,0.00014611974,0.00043777164,0.00011030864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003143825,0.0002869074,0.00021470834,0.0036753437,0.0003027883,0.00056967,0.00036396255,0.00020063673,0.0022122746],"category_scores_gemma":[0.0020676167,0.00018654263,0.00019530022,0.003257959,0.00014825816,0.00026997112,0.00077030086,0.0001461272,0.0006493513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013055764,0.00006163061,0.87548935,0.00011646073,0.00016780793,0.000261313,0.00063679984,0.009081327,0.033982694,0.00055367884,0.0023690704,0.077149205],"study_design_scores_gemma":[0.0000075116427,0.00002821855,0.96061426,0.00000953099,0.000045190067,0.00012871144,0.00016490412,0.033125088,0.0044225305,0.00012461645,0.0013114039,0.000018028553],"about_ca_topic_score_codex":0.032930106,"about_ca_topic_score_gemma":0.077551946,"teacher_disagreement_score":0.032930106,"about_ca_system_score_codex":0.00042858417,"about_ca_system_score_gemma":0.00049763307,"threshold_uncertainty_score":0.065476835},"labels":[],"label_agreement":null},{"id":"W2288496799","doi":"10.1002/2015jb012416","title":"Seismic reflection imaging of the Juan de Fuca plate from ridge to trench: New constraints on the distribution of faulting and evolution of the crust prior to subduction","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Subduction; Seismology; Crust; Oceanic crust; Ridge; Trench; Receiver function; Transect; Fault (geology); Mantle (geology); Convergent boundary; Lithosphere; Paleontology; Tectonics","score_opus":0.04239652242047027,"score_gpt":0.31196079399586396,"score_spread":0.2695642715753937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2288496799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99823606,0.000045497483,0.00012489938,0.000010894867,0.0000017618488,0.0000019650217,0.00016240777,0.000014295775,0.001402143],"genre_scores_gemma":[0.9990508,0.00004692344,0.00037659824,0.0000049873656,0.0000025600875,0.000002169149,0.00022505902,0.0000041231024,0.00028674933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995756,0.0000019997765,0.000002087326,0.000014910329,0.00001179494,0.000011635733],"domain_scores_gemma":[0.999915,0.000009349203,0.0000238603,0.000008857449,0.000025072623,0.00001792321],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010156977,0.00023001208,0.00013902149,0.00067476806,0.0002354454,0.00039228235,0.00017828966,0.0002361984,0.000992904],"category_scores_gemma":[0.000248601,0.00017594326,0.00012402805,0.00044008723,0.00019525479,0.00014593366,0.00028108325,0.00016201074,0.00013915969],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020758653,0.000056810888,0.7941212,0.00006401885,0.00006252524,0.0003857872,0.0009789449,0.0014210797,0.18108372,0.000119247044,0.000255263,0.02124391],"study_design_scores_gemma":[0.0000026688988,0.000017774046,0.9972236,0.0000070192505,0.000008414599,0.00007636744,0.0002036704,0.00075918855,0.0012787969,0.0000131269,0.0004051868,0.0000042746856],"about_ca_topic_score_codex":0.03061105,"about_ca_topic_score_gemma":0.08285459,"teacher_disagreement_score":0.03061105,"about_ca_system_score_codex":0.00032688328,"about_ca_system_score_gemma":0.0002943697,"threshold_uncertainty_score":0.0608657},"labels":[],"label_agreement":null},{"id":"W2289380568","doi":"10.15530/urtec-2015-2154714","title":"Identifying the Effectiveness of Treatment Programs with Microseismicity","year":2015,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Apheresis Group","funders":"","keywords":"Computer science","score_opus":0.04877264061281174,"score_gpt":0.24826509296611346,"score_spread":0.1994924523533017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2289380568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902436,0.00060480525,0.002461081,0.0010792873,0.000059354716,0.00056081533,0.00035069263,0.000044890967,0.004595562],"genre_scores_gemma":[0.9980369,0.00015871563,0.0011391884,0.000080258615,0.000027367312,0.0001621332,0.00012382258,0.000003504419,0.00026801878],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9893216,0.00724237,0.0005687036,0.0007424317,0.00130001,0.0008248694],"domain_scores_gemma":[0.9735469,0.017856173,0.004618472,0.0013644152,0.0012534377,0.0013606678],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00712242,0.00061483897,0.0008433078,0.0012099976,0.00059016765,0.0010114845,0.0013921148,0.0014009819,0.0033759868],"category_scores_gemma":[0.053968865,0.00020921476,0.000887769,0.0010827081,0.00083515554,0.0018261394,0.0012985707,0.0011045339,0.00020634534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.017943509,0.035699062,0.45859727,0.00096622406,0.002574765,0.0001635744,0.0009162353,0.025069077,0.0023261728,0.0062631955,0.0022360987,0.44724485],"study_design_scores_gemma":[0.0025741146,0.04409317,0.8773095,0.00052726833,0.003536867,0.00025665414,0.0026896405,0.050387267,0.005846749,0.008629184,0.0040770397,0.000072440416],"about_ca_topic_score_codex":0.004982057,"about_ca_topic_score_gemma":0.009285478,"teacher_disagreement_score":0.00712242,"about_ca_system_score_codex":0.001820118,"about_ca_system_score_gemma":0.0041270168,"threshold_uncertainty_score":0.037667394},"labels":[],"label_agreement":null},{"id":"W2289948653","doi":"10.1017/cbo9781139020138.012","title":"Case histories and geological applications","year":2012,"lang":"en","type":"book-chapter","venue":"Cambridge University Press eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Geography; Archaeology","score_opus":0.03162976621963663,"score_gpt":0.1824530180056842,"score_spread":0.15082325178604755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2289948653","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03345905,0.09462375,0.01124387,0.032538228,0.004452526,0.00070969644,0.008079427,0.00059848436,0.8142948],"genre_scores_gemma":[0.37705982,0.22373922,0.02044438,0.0069581154,0.0033473952,0.00088913355,0.009677155,0.00031330695,0.35757145],"study_design_codex":"not_applicable","study_design_gemma":"case_report","domain_scores_codex":[0.99952984,0.00018317136,0.000038923376,0.00004655671,0.00013203471,0.00006940636],"domain_scores_gemma":[0.99885964,0.00062572694,0.00010790928,0.000086364314,0.00015413792,0.00016635477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007640375,0.000529174,0.00025116524,0.005841118,0.0011876435,0.0014208732,0.0010813196,0.001480057,0.066894576],"category_scores_gemma":[0.006651949,0.00020319919,0.00037991966,0.0056049633,0.0008444903,0.0013389348,0.0013080599,0.0010377023,0.005992309],"study_design_candidate":"case_report","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010891262,0.0001451337,0.008023824,0.0012913414,0.000020406254,0.037702736,0.0023365528,0.0014044059,0.00036816005,0.06226766,0.4439129,0.4424179],"study_design_scores_gemma":[0.000012777874,0.000034591783,0.0052275117,0.0015356925,0.000026267324,0.045320805,0.0022142206,0.0003642241,0.00030391646,0.022717306,0.92221117,0.000031493204],"about_ca_topic_score_codex":0.0052558687,"about_ca_topic_score_gemma":0.009957827,"teacher_disagreement_score":0.066894576,"about_ca_system_score_codex":0.0011964018,"about_ca_system_score_gemma":0.00092453306,"threshold_uncertainty_score":0.22378463},"labels":[],"label_agreement":null},{"id":"W2296457758","doi":"10.1016/j.amc.2016.01.005","title":"An analytical and numerical study of long wave run-up in U-shaped and V-shaped bays","year":2016,"lang":"en","type":"article","venue":"Applied Mathematics and Computation","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"National Oceanic and Atmospheric Administration; Russian Foundation for Basic Research; National Science Foundation","keywords":"Mathematical analysis; Nonlinear system; Mathematics; Hankel transform; Transformation (genetics); Integral equation; Inverse; Plane (geometry); Waves and shallow water; Geometry; Wave equation; Physics; Bessel function; Thermodynamics; Chemistry","score_opus":0.03099297238756523,"score_gpt":0.25690379292556076,"score_spread":0.22591082053799552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2296457758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9804349,0.0003587396,0.007603392,0.00027975623,0.00003882873,0.000018675468,0.000070755654,0.000070716254,0.011124173],"genre_scores_gemma":[0.99683255,0.00009675258,0.0010908255,0.000015866317,0.000009592319,0.0000050719145,0.000024314724,0.000012623652,0.0019123161],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999132,0.000026053536,0.0000049964187,0.000012810815,0.000013652775,0.000029210287],"domain_scores_gemma":[0.9994678,0.00024199356,0.0000809602,0.000028737268,0.000104065446,0.00007651865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028325425,0.00035008663,0.0004249239,0.0007235772,0.00074220006,0.0011467547,0.00088038057,0.00095728616,0.001988339],"category_scores_gemma":[0.002190096,0.0003428988,0.00044927388,0.0008005991,0.0013274837,0.0006911577,0.0007575134,0.00059016905,0.00015468105],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016219639,0.00015404512,0.00999794,0.00006581121,0.000037013233,0.0008303833,0.0003169234,0.96077764,0.0058154985,0.016855562,0.0005265585,0.004460458],"study_design_scores_gemma":[0.000011621149,0.00003014216,0.0022954785,0.0000052702862,0.000008272888,0.000036002133,0.00022749037,0.99595356,0.00022811604,0.0010257981,0.00016846663,0.000009860127],"about_ca_topic_score_codex":0.020487264,"about_ca_topic_score_gemma":0.0113784,"teacher_disagreement_score":0.020487264,"about_ca_system_score_codex":0.0007415617,"about_ca_system_score_gemma":0.00051082927,"threshold_uncertainty_score":0.04073602},"labels":[],"label_agreement":null},{"id":"W2296943930","doi":"10.1002/2015jb012603","title":"Discriminating induced seismicity from natural earthquakes using moment tensors and source spectra","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; University of Calgary","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium","keywords":"Seismology; Geology; Intraplate earthquake; Moment tensor; Induced seismicity; Focal mechanism; Spurious relationship; Seismic moment; Spectral line; Tectonics; Moment magnitude scale; Magnitude (astronomy); Shield; Geometry; Physics; Fault (geology); Scaling; Petrology; Mathematics","score_opus":0.06606367543509702,"score_gpt":0.32284499486352974,"score_spread":0.25678131942843274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2296943930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905054,0.00004176636,0.007613732,0.000023118606,0.000002756062,0.000014378865,0.00039650145,0.00011445418,0.0012879216],"genre_scores_gemma":[0.99664056,0.00003789937,0.002675846,0.0000029920843,0.0000015121931,0.0000031402083,0.00044316973,0.00001018107,0.00018469016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990356,0.000007429683,0.0000064704045,0.000011683717,0.000052986343,0.000017812163],"domain_scores_gemma":[0.99964094,0.000094315204,0.00008483509,0.000028114186,0.00010811395,0.000043630855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018563081,0.00030368307,0.0001107262,0.0011929146,0.00016748434,0.00039458598,0.00027753357,0.000166965,0.0009931499],"category_scores_gemma":[0.0016342867,0.00012304784,0.0001707433,0.0007908458,0.00020629242,0.00030156624,0.0002187339,0.00013196495,0.00013563792],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000268654,0.00013495065,0.72416955,0.00016089308,0.0001536899,0.00063337776,0.00040487666,0.08070235,0.08561857,0.0022090364,0.00091463176,0.10462937],"study_design_scores_gemma":[0.00001180749,0.00003868534,0.8915743,0.00000773988,0.000020865613,0.0001254291,0.00013059416,0.10019598,0.0068316483,0.00036345277,0.0006808185,0.000018575578],"about_ca_topic_score_codex":0.08397382,"about_ca_topic_score_gemma":0.21628913,"teacher_disagreement_score":0.08397382,"about_ca_system_score_codex":0.00069123646,"about_ca_system_score_gemma":0.00086560444,"threshold_uncertainty_score":0.16697007},"labels":[],"label_agreement":null},{"id":"W2297136396","doi":"10.1002/2015gl066917","title":"Source analysis of a potential hydraulic‐fracturing‐induced earthquake near Fox Creek, Alberta","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Hypocenter; Geology; Seismology; Hydraulic fracturing; Seismic moment; Focal mechanism; Fault plane; Aftershock; Moment magnitude scale; Magnitude (astronomy); Fault (geology); Oil shale; Induced seismicity; Geotechnical engineering; Paleontology","score_opus":0.04808137418258863,"score_gpt":0.2906286624480128,"score_spread":0.24254728826542415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2297136396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913557,0.000051833136,0.0015092305,0.000084071165,0.000011820647,0.000020827656,0.0028867195,0.00013462557,0.0039453055],"genre_scores_gemma":[0.99427044,0.00004374966,0.001151373,0.0000099519175,0.0000045587713,0.000004847116,0.0024065874,0.000013498965,0.002095011],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.0000013807205,0.000001415144,0.0000068190357,0.000022928349,0.000013565761],"domain_scores_gemma":[0.99988747,0.000009587532,0.000008685742,0.0000041499147,0.00007497313,0.000015048534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006295028,0.0002178857,0.00013295798,0.0007360487,0.00052543706,0.00041994522,0.00047396836,0.00017959303,0.0021189253],"category_scores_gemma":[0.00024223838,0.00009903971,0.000111221234,0.0010861601,0.00012832179,0.00009461317,0.00023518717,0.00014479527,0.00022641169],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063557224,0.00026574038,0.67184424,0.00017223551,0.00016200905,0.0044030286,0.0012456921,0.08044868,0.07520967,0.0030079698,0.013437831,0.14916734],"study_design_scores_gemma":[0.000064491614,0.000039785442,0.8699643,0.000021139544,0.00006409418,0.00021955428,0.0014333472,0.11638175,0.0055560186,0.0004595334,0.0057557467,0.000040206192],"about_ca_topic_score_codex":0.8240661,"about_ca_topic_score_gemma":0.86126655,"teacher_disagreement_score":0.1759339,"about_ca_system_score_codex":0.0019320438,"about_ca_system_score_gemma":0.0027906122,"threshold_uncertainty_score":0.35393995},"labels":[],"label_agreement":null},{"id":"W2301748736","doi":"10.1002/2015gl066446","title":"Terrane‐controlled crustal shear wave splitting in Taiwan","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Terrane; Geology; Shear wave splitting; Lithosphere; Metamorphic rock; Seismology; Shear (geology); Tectonics; Shear zone; Plate tectonics; Crust; Continental collision; Petrology; Geophysics","score_opus":0.08361527928235694,"score_gpt":0.305338154665588,"score_spread":0.22172287538323104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2301748736","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997689,0.000012517727,0.000025414321,0.0000031030888,1.5421931e-7,6.187697e-7,0.00004052515,0.0000018583596,0.00014700709],"genre_scores_gemma":[0.99978083,0.000012538462,0.000023205515,0.0000013591751,3.002126e-7,9.931939e-7,0.00011677834,9.391379e-7,0.0000629126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999961,0.0000040986506,0.0000030310277,0.000013409256,0.0000067666247,0.000011715866],"domain_scores_gemma":[0.9998996,0.00001126899,0.000031530904,0.000009194613,0.000023629324,0.000024673078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000080836566,0.000113729344,0.0001211017,0.0005524539,0.00017492472,0.00031399252,0.00011654789,0.00010485517,0.00067602517],"category_scores_gemma":[0.00019891477,0.00011184127,0.00009274426,0.0005287991,0.0001475506,0.00013744754,0.0002675282,0.00010141222,0.000091151844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033464067,0.00006372475,0.6817098,0.000038341015,0.00007749272,0.00067409757,0.00075228815,0.0028779646,0.30159926,0.00020834508,0.00021367756,0.01145033],"study_design_scores_gemma":[0.000008677298,0.00003663844,0.9941902,0.0000022604095,0.000012908377,0.00011253601,0.00023199155,0.0019285094,0.003235185,0.000053655243,0.00018147008,0.000006079173],"about_ca_topic_score_codex":0.012433436,"about_ca_topic_score_gemma":0.012321851,"teacher_disagreement_score":0.012433436,"about_ca_system_score_codex":0.0002516703,"about_ca_system_score_gemma":0.0001610753,"threshold_uncertainty_score":0.024722159},"labels":[],"label_agreement":null},{"id":"W2305722572","doi":"","title":"A Geophysical and Field Survey in Central New Hampshire to Search for the Source Region of the Magnitude 6.5 Earthquake of 1638","year":2013,"lang":"en","type":"article","venue":"PhDT","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Aftershock; Seismology; Epicenter; Terrane; Induced seismicity; Thrust fault; Magnitude (astronomy); Fault (geology); Focal mechanism; Foreshock; Basement; Seismic gap; Tectonics; Geography","score_opus":0.039606645241328356,"score_gpt":0.23680661612021064,"score_spread":0.1971999708788823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2305722572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9804417,0.0006769409,0.000511523,0.00031712605,0.0000265205,0.0002485721,0.009215175,0.00004836257,0.008514057],"genre_scores_gemma":[0.9765619,0.001272917,0.0021619177,0.0006197186,0.000034721164,0.0003871018,0.0059882933,0.000014806707,0.012958598],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979764,0.000018275876,0.000015218209,0.00006103724,0.00006357815,0.000044262033],"domain_scores_gemma":[0.9991352,0.00009044821,0.00016012794,0.00004095576,0.00035995574,0.00021338451],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015622961,0.00030420697,0.0001837723,0.001886155,0.00090559194,0.00050070946,0.0006774066,0.00031069195,0.0053524175],"category_scores_gemma":[0.0005880702,0.00029173642,0.0001132211,0.0023712262,0.0005124537,0.00037104642,0.00062056363,0.0002884821,0.0010235133],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023614535,0.00025819996,0.84837157,0.00085293676,0.00013510448,0.010390896,0.013919129,0.0008950719,0.04217225,0.0005068841,0.016192136,0.06606969],"study_design_scores_gemma":[0.0000071647705,0.000036678284,0.9902082,0.000029653422,0.0000075207404,0.0005443745,0.0024661582,0.00017846894,0.00028193957,0.000020000241,0.006209039,0.00001084601],"about_ca_topic_score_codex":0.7539808,"about_ca_topic_score_gemma":0.88688576,"teacher_disagreement_score":0.7539808,"about_ca_system_score_codex":0.004354912,"about_ca_system_score_gemma":0.0028176259,"threshold_uncertainty_score":0.49493605},"labels":[],"label_agreement":null},{"id":"W2311709859","doi":"10.14288/1.0053407","title":"Earthquake swarm on the Queen Charlotte Islands fracture zone","year":2011,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Seismometer; Seismology; Ridge; Geology; Crust; Earthquake swarm; Swarm behaviour; Magnitude (astronomy); Pacific ocean; Seismogram; Period (music); Lithosphere; Induced seismicity; Geodesy; Oceanography; Paleontology; Tectonics","score_opus":0.01422824276138064,"score_gpt":0.15601167004865743,"score_spread":0.1417834272872768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2311709859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985613,0.00003024816,0.000037643866,0.00003276863,0.0000015469424,0.000006097236,0.00013160684,0.000004169994,0.0011944859],"genre_scores_gemma":[0.99899036,0.000040886804,0.00008061587,0.000010631857,0.0000022633724,0.0000054957295,0.00027738558,0.0000012612567,0.00059118343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999874,0.00001349208,0.0000060928396,0.000017143091,0.00004815966,0.00004111618],"domain_scores_gemma":[0.99967074,0.000036866524,0.00008816947,0.000022549148,0.00008716155,0.00009455587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000081979735,0.000138562,0.00014255442,0.0007996937,0.00083160267,0.0005701228,0.00031548113,0.00022925585,0.0008370421],"category_scores_gemma":[0.00060083263,0.00009200819,0.000107914464,0.00085056777,0.00032506126,0.000106816544,0.00046298516,0.00018139837,0.000087542896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040717487,0.00011367764,0.945552,0.000059475606,0.00014810193,0.0064044744,0.0017748128,0.008276911,0.007473987,0.0006141834,0.003972868,0.025202336],"study_design_scores_gemma":[0.000013140082,0.00005479375,0.992396,0.000011611862,0.000017167147,0.00030847822,0.0009824288,0.004140965,0.0003054466,0.000048586302,0.0017101899,0.0000112368525],"about_ca_topic_score_codex":0.5672328,"about_ca_topic_score_gemma":0.7604041,"teacher_disagreement_score":0.4327672,"about_ca_system_score_codex":0.002836066,"about_ca_system_score_gemma":0.0012630661,"threshold_uncertainty_score":0.8706317},"labels":[],"label_agreement":null},{"id":"W2313538618","doi":"10.1785/0120110252","title":"Relative Source-Time Function Studies and Stress Drop of Earthquakes in Southeastern Alaska-Northwestern Canada","year":2012,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Seismology; Drop (telecommunication); Engineering; Telecommunications","score_opus":0.014334921782771461,"score_gpt":0.20099424398500668,"score_spread":0.18665932220223522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2313538618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99902165,0.000041579136,0.00022086251,0.000009247808,0.0000010769874,0.0000026712187,0.00021723026,0.0000070580354,0.00047867358],"genre_scores_gemma":[0.9993413,0.000030722265,0.00017809098,0.0000015430418,7.546494e-7,0.00000136878,0.0002040025,0.0000018658098,0.00024045576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998791,0.0000079457595,0.000009660795,0.000020446949,0.000058261438,0.000024587262],"domain_scores_gemma":[0.99913627,0.00012741894,0.00011969936,0.000026831207,0.00048635228,0.00010345422],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025419882,0.0001508895,0.00015326455,0.0019677118,0.0006179314,0.00043927436,0.0002691736,0.00014811587,0.00095051265],"category_scores_gemma":[0.0015005692,0.00008954654,0.00012596679,0.0015597935,0.00028414006,0.00022064548,0.00023924143,0.00015791165,0.00010218676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017176956,0.00003309223,0.9609697,0.00003314649,0.00005015076,0.0004978662,0.0015113185,0.0030326867,0.011890961,0.0002569805,0.00019951191,0.021352781],"study_design_scores_gemma":[0.0000016157746,0.000009999594,0.99678767,0.00000383545,0.0000069228445,0.00006296584,0.00051869894,0.0018391421,0.0005789703,0.000028434784,0.00015607264,0.00000575373],"about_ca_topic_score_codex":0.7578309,"about_ca_topic_score_gemma":0.82366264,"teacher_disagreement_score":0.24216908,"about_ca_system_score_codex":0.0022975665,"about_ca_system_score_gemma":0.0012976718,"threshold_uncertainty_score":0.48719049},"labels":[],"label_agreement":null},{"id":"W2314121611","doi":"10.1016/j.jsg.2016.04.003","title":"The spin zone: Transient mid-crust permeability caused by coseismic brecciation","year":2016,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Breccia; Mylonite; Lineation; Shear zone; Petrology; Overprinting; Seismology; Slip (aerodynamics); Crust; Shear (geology); Tectonics; Metamorphic rock; Geochemistry","score_opus":0.009558010637003718,"score_gpt":0.22076919702220993,"score_spread":0.21121118638520622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314121611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987709,0.000058842616,0.00019334476,0.000030354126,0.0000039184306,0.0000052962696,0.00004923823,0.000024799585,0.00086328154],"genre_scores_gemma":[0.99989974,0.000010632396,0.000011865876,0.0000036327917,0.0000014389863,6.232971e-7,0.000012057956,0.0000017949321,0.00005812051],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999672,0.000003738826,0.0000017392794,0.000005738186,0.0000052513024,0.000016268903],"domain_scores_gemma":[0.99988806,0.000023405268,0.00002900359,0.000016193595,0.000013669967,0.00002970351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000071828064,0.00015422243,0.00021198599,0.00022027196,0.0002613876,0.00035001757,0.00017147276,0.00032554008,0.0022502397],"category_scores_gemma":[0.00048444537,0.00013326705,0.00012139085,0.0001776909,0.00036063645,0.00029608977,0.00037580635,0.00027646322,0.0001419619],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.009787976,0.00038535698,0.18097605,0.00017213944,0.00014192033,0.013682772,0.0011564641,0.006263348,0.75685155,0.001531919,0.001299194,0.027751308],"study_design_scores_gemma":[0.00012565801,0.0006385026,0.95715564,0.000013579986,0.00007191689,0.0018173747,0.0006796232,0.008587032,0.029672213,0.00046273318,0.0007544365,0.00002130523],"about_ca_topic_score_codex":0.0032051068,"about_ca_topic_score_gemma":0.0022812658,"teacher_disagreement_score":0.0032051068,"about_ca_system_score_codex":0.00020887652,"about_ca_system_score_gemma":0.00010980052,"threshold_uncertainty_score":0.007527828},"labels":[],"label_agreement":null},{"id":"W2314161669","doi":"10.1093/gji/ggw111","title":"Receiver functions using OBS data: promises and limitations from numerical modelling and examples from the Cascadia Initiative","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Receiver function; Geology; Forearc; Subduction; Seismology; Seismometer; Oceanic crust; Lithosphere; Geophysics; Tectonics","score_opus":0.17185635606533564,"score_gpt":0.2696078049861406,"score_spread":0.09775144892080498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314161669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.70880973,0.0007197284,0.27526227,0.0017124787,0.000045860088,0.00006399312,0.0013370838,0.001701002,0.010347778],"genre_scores_gemma":[0.9596142,0.0003324883,0.037936985,0.000038714013,0.00001697134,0.000032607775,0.00061478844,0.00014252274,0.0012707202],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995803,0.00020374503,0.00002692841,0.00006153514,0.00009891309,0.00002860673],"domain_scores_gemma":[0.9979825,0.0013398152,0.00014143935,0.00026703216,0.00023365665,0.000035529392],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013168262,0.0009065013,0.00039897778,0.00046068474,0.00031118878,0.0009699686,0.001025845,0.0011889747,0.00090959057],"category_scores_gemma":[0.004162681,0.00036127996,0.0005081013,0.00081751717,0.0007203062,0.0011528537,0.00045620327,0.0007626663,0.00021264717],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000064837404,0.000045799276,0.016693186,0.000087495646,0.000037619175,0.00014253153,0.00019676161,0.9574456,0.0019901842,0.0041865623,0.0005131864,0.018596346],"study_design_scores_gemma":[0.000021513708,0.0000308334,0.0048970208,0.000020547424,0.0000140598995,0.00003240385,0.000060160924,0.9903266,0.0010492932,0.001910771,0.0016107132,0.000026099277],"about_ca_topic_score_codex":0.07340224,"about_ca_topic_score_gemma":0.05754853,"teacher_disagreement_score":0.07340224,"about_ca_system_score_codex":0.0007931261,"about_ca_system_score_gemma":0.0009924595,"threshold_uncertainty_score":0.14594996},"labels":[],"label_agreement":null},{"id":"W2314530086","doi":"10.1093/gji/ggw077","title":"Residual polar motion caused by coseismic and interseismic deformations from 1900 to present","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Polar motion; Induced seismicity; Geology; Seismology; Geodesy; Earth's rotation; Residual; Polar; Seismic moment; Plate tectonics; Magnitude (astronomy); Geophysics; Tectonics; Fault (geology); Physics","score_opus":0.011126495126505211,"score_gpt":0.22123990082377032,"score_spread":0.2101134056972651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314530086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9830755,0.00010990524,0.010575735,0.00028100476,0.00004838522,0.000017148512,0.0010809122,0.00016785997,0.0046436395],"genre_scores_gemma":[0.9975501,0.00008797899,0.0011444477,0.00002563797,0.000008224679,0.000013993759,0.00065438857,0.00003203967,0.00048314326],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998976,0.000020141593,0.00000597371,0.000029054556,0.000014047065,0.00003316302],"domain_scores_gemma":[0.999845,0.000043245025,0.000029496367,0.000036018962,0.000024138119,0.000021988699],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031040597,0.00043947974,0.00043309506,0.00038715452,0.00024681553,0.00056516443,0.00059865793,0.0005888383,0.0022244873],"category_scores_gemma":[0.0011916556,0.0002459091,0.0007645309,0.0006002111,0.0006255756,0.0007292698,0.00060621236,0.0007147684,0.00021421592],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005564446,0.0000340804,0.024544004,0.000021731683,0.000053251544,0.000052330044,0.000046212383,0.9679778,0.0012162268,0.0025240853,0.00035058463,0.003123958],"study_design_scores_gemma":[0.000046735466,0.0001056294,0.020163137,0.0000125006845,0.00004805622,0.00005586455,0.00007809002,0.97523695,0.0009578029,0.001825364,0.001442516,0.000027376489],"about_ca_topic_score_codex":0.02392807,"about_ca_topic_score_gemma":0.013915552,"teacher_disagreement_score":0.02392807,"about_ca_system_score_codex":0.0006426978,"about_ca_system_score_gemma":0.00053402234,"threshold_uncertainty_score":0.04757762},"labels":[],"label_agreement":null},{"id":"W2314646464","doi":"10.1130/g35057.1","title":"What controls the growth of the Himalayan foreland fold-and-thrust belt?","year":2014,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Royal Government of Bhutan; National Geographic Society","keywords":"Nova scotia; Library science; Foreland basin; History; Archaeology; Geology; Paleontology; Computer science","score_opus":0.00807642364300143,"score_gpt":0.18584553758601874,"score_spread":0.1777691139430173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2314646464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8751028,0.019613853,0.0015212604,0.01543568,0.000505404,0.00003067391,0.0025822364,0.00022059574,0.08498743],"genre_scores_gemma":[0.9853955,0.0068380428,0.00022700593,0.0005827569,0.00024296514,0.000011235032,0.00083618966,0.000043325337,0.005823024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996685,0.00005276268,0.000018733605,0.00007982107,0.00006699797,0.00011320673],"domain_scores_gemma":[0.9992669,0.00014306261,0.00018175981,0.000045730485,0.00017190432,0.00019064675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055371015,0.00041655704,0.00039028804,0.0012227305,0.0006889609,0.0030095908,0.0005063028,0.00052071153,0.0076544895],"category_scores_gemma":[0.0023290052,0.00021468027,0.0002971562,0.0019349231,0.001507084,0.0017066444,0.0009082512,0.0005626252,0.0017206005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005286272,0.0001032705,0.7181289,0.0011864696,0.0004210514,0.0014159714,0.0066945837,0.008097272,0.022210814,0.044604667,0.032568432,0.16404],"study_design_scores_gemma":[0.00002284307,0.000065091604,0.9378182,0.00021099055,0.00007509595,0.00016424737,0.006445646,0.0017123362,0.0014764273,0.0072366716,0.04472111,0.000051321287],"about_ca_topic_score_codex":0.051711973,"about_ca_topic_score_gemma":0.04615646,"teacher_disagreement_score":0.051711973,"about_ca_system_score_codex":0.0023002657,"about_ca_system_score_gemma":0.0012782078,"threshold_uncertainty_score":0.102821946},"labels":[],"label_agreement":null},{"id":"W2315186495","doi":"10.1061/40926(239)83","title":"Reconstructing Tsunami Run-Up from Sedimentary Characteristics: A Simple Mathematical Model","year":2007,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Nova Scotia Department of Energy","funders":"","keywords":"Geology; Sediment; Sedimentary rock; Tsunami wave; Holocene; Sedimentary structures; Geomorphology; Seismology; Oceanography; Geochemistry; Sedimentary depositional environment","score_opus":0.02388929482837889,"score_gpt":0.235241154154932,"score_spread":0.2113518593265531,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2315186495","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.110089764,0.0008735377,0.8771386,0.0014330873,0.00005792502,0.00005906084,0.001003213,0.00045838786,0.008886522],"genre_scores_gemma":[0.90222615,0.0021270788,0.07727159,0.00013837173,0.00012963872,0.00026270637,0.0007326366,0.000158508,0.016953383],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999151,0.000015271233,0.000008239109,0.000027939475,0.000019533285,0.000013875316],"domain_scores_gemma":[0.99958104,0.0002417986,0.00006854319,0.00002180238,0.00006056546,0.0000263155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005361859,0.0006026226,0.000639996,0.0009133109,0.00043676616,0.001513537,0.001564753,0.0014474909,0.0024587181],"category_scores_gemma":[0.002176463,0.00064419524,0.0007725838,0.0011798212,0.0009709709,0.0017951244,0.0008162627,0.00077629887,0.00073350087],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014977972,0.000010597055,0.0008563028,0.000029689978,0.000014323751,0.00008938645,0.00003954753,0.9672192,0.0007837272,0.026241677,0.00032924354,0.004371425],"study_design_scores_gemma":[0.0000038302564,0.000004485156,0.00013529626,0.000003452582,0.0000049150844,0.000016497885,0.0000038141557,0.9925532,0.000055245368,0.0069941864,0.00021907847,0.000005965589],"about_ca_topic_score_codex":0.015301469,"about_ca_topic_score_gemma":0.008740661,"teacher_disagreement_score":0.015301469,"about_ca_system_score_codex":0.0011235109,"about_ca_system_score_gemma":0.0010946634,"threshold_uncertainty_score":0.030424774},"labels":[],"label_agreement":null},{"id":"W2315553177","doi":"10.1093/gji/ggv061","title":"Generalized Omori–Utsu law for aftershock sequences in southern California","year":2015,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Alberta Innovates","keywords":"Aftershock; Geology; Seismology; Law","score_opus":0.03601223143801919,"score_gpt":0.25961852882551967,"score_spread":0.22360629738750049,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2315553177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94208825,0.00040005363,0.052825004,0.00020402676,0.000018176193,0.000058582336,0.00043613336,0.00029849802,0.003671265],"genre_scores_gemma":[0.99375254,0.00014135739,0.0051431293,0.000028659835,0.000024155828,0.00002739964,0.0004538032,0.000039803483,0.0003891633],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993104,0.00015387987,0.00006839627,0.00020066217,0.00017249447,0.00009424859],"domain_scores_gemma":[0.9898789,0.0039517665,0.0024179863,0.0022052894,0.0012609247,0.000285055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0032039173,0.00028558326,0.00051329605,0.0017299067,0.00044369805,0.0011109589,0.0012941043,0.0005446697,0.0015337697],"category_scores_gemma":[0.019649794,0.00019650633,0.0004175587,0.0016377689,0.0011826482,0.0012549076,0.00061368156,0.00074015075,0.00020405969],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002012948,0.00005924047,0.6082581,0.00017078519,0.00012077785,0.0007832841,0.0017659654,0.2480451,0.0045785457,0.05531363,0.0047448566,0.07595844],"study_design_scores_gemma":[0.000036572077,0.00010726981,0.35820663,0.00006530362,0.000042048945,0.0003939308,0.00046398884,0.61526257,0.0008711506,0.022318995,0.0021732787,0.000058272213],"about_ca_topic_score_codex":0.02259585,"about_ca_topic_score_gemma":0.022514818,"teacher_disagreement_score":0.02259585,"about_ca_system_score_codex":0.0011810153,"about_ca_system_score_gemma":0.0007687089,"threshold_uncertainty_score":0.04492867},"labels":[],"label_agreement":null},{"id":"W2315940070","doi":"10.17184/eac.10287736v7n1234","title":"APPORT DE LA TÉLÉDÉTECTION À L'ÉTUDE DES FAILLES ACTIVES ET DES RISQUES SISMIQUES AU NORD DU VIÊT-NAM","year":2007,"lang":"fr","type":"article","venue":"ORBi (University of Liège)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Agence Universitaire de la Francophonie; Université de Liège; Waalse Gewest","keywords":"Geology; Digital elevation model; Shuttle Radar Topography Mission; Fault (geology); Terrain; Active fault; Seismology; Remote sensing; Geomorphology; Cartography; Geography","score_opus":0.024532476945457956,"score_gpt":0.23706452870256928,"score_spread":0.21253205175711132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2315940070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99009794,0.0017582754,0.00089320436,0.0013148601,0.000090204456,0.000054118314,0.00075817964,0.000017087243,0.00501627],"genre_scores_gemma":[0.99162626,0.0011185281,0.0011574961,0.0002101101,0.00008162286,0.00008029283,0.00019333392,0.000008347331,0.005524099],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982698,0.0010710431,0.00008923666,0.00012405432,0.0002488664,0.00019700456],"domain_scores_gemma":[0.99148613,0.004193916,0.001161522,0.0002554408,0.0023137568,0.0005893186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031601905,0.00050298835,0.0002674953,0.001291243,0.00045588095,0.0012429636,0.00071806397,0.00069761445,0.0042148936],"category_scores_gemma":[0.010616158,0.00029036397,0.00033167333,0.00087054825,0.0005125707,0.00083381886,0.00064786244,0.00044565534,0.0004705534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016651722,0.00012396385,0.9377035,0.00025361413,0.00010703435,0.00056255114,0.005288909,0.0007600429,0.00086273515,0.00030117683,0.0009956706,0.052874383],"study_design_scores_gemma":[0.000024458674,0.0003700421,0.97963095,0.00025454146,0.0000901372,0.0006661387,0.0073889736,0.0019829995,0.0006378596,0.00015702151,0.008778495,0.000018517958],"about_ca_topic_score_codex":0.1456134,"about_ca_topic_score_gemma":0.11097199,"teacher_disagreement_score":0.1456134,"about_ca_system_score_codex":0.0019465929,"about_ca_system_score_gemma":0.0026936978,"threshold_uncertainty_score":0.28953165},"labels":[],"label_agreement":null},{"id":"W2316105095","doi":"10.1002/2015gc006148","title":"Modeled temperatures and fluid source distributions for the <scp>M</scp>exican subduction zone: Effects of hydrothermal circulation and implications for plate boundary seismic processes","year":2016,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Oceanic crust; Pore water pressure; Fluid dynamics; Petrology; Hydrothermal circulation; Episodic tremor and slip; Seismology; Geophysics; Overpressure; Crust; Convergent boundary; Induced seismicity; Fault (geology); Plate tectonics; Tectonics; Geotechnical engineering; Mechanics","score_opus":0.006964833423822142,"score_gpt":0.199542973450188,"score_spread":0.19257814002636586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2316105095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99689794,0.000024310151,0.0007793276,0.000064536835,0.000004126686,0.0000072172475,0.0005378027,0.000080026475,0.0016047441],"genre_scores_gemma":[0.9991304,0.000017875207,0.00031257814,0.0000059924546,0.0000014800714,0.0000076117863,0.00020734785,0.0000112528605,0.00030545928],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995077,0.00001046283,0.000002611749,0.00001577192,0.0000061784767,0.000014160366],"domain_scores_gemma":[0.9998535,0.000051192044,0.00002754402,0.000015549685,0.000022879874,0.000029286308],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016481333,0.00058026536,0.00031039913,0.000325371,0.00042847957,0.0007693861,0.00072901405,0.0008172686,0.0016714368],"category_scores_gemma":[0.00042957423,0.00035167625,0.0006361503,0.00048885983,0.0006039991,0.0003209968,0.0003300476,0.00041550884,0.00018085352],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000101864505,0.000034401815,0.020058487,0.000012519782,0.000026682263,0.0000698843,0.000028708208,0.97614485,0.002223452,0.0002920899,0.00022050142,0.00078656815],"study_design_scores_gemma":[0.000060902512,0.000035508776,0.008380807,0.0000037704262,0.000015630276,0.000008641503,0.000048653474,0.9901844,0.0009539711,0.00012773342,0.00017124978,0.000008740873],"about_ca_topic_score_codex":0.075735055,"about_ca_topic_score_gemma":0.03841892,"teacher_disagreement_score":0.075735055,"about_ca_system_score_codex":0.0014938135,"about_ca_system_score_gemma":0.00083058863,"threshold_uncertainty_score":0.15058845},"labels":[],"label_agreement":null},{"id":"W2316238748","doi":"10.1016/j.jog.2016.03.010","title":"Invited review paper: Some outstanding issues in the study of great megathrust earthquakes—The Cascadia example","year":2016,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":186,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"National Science Foundation","keywords":"Geology; Seismology; Subduction; Episodic tremor and slip; Slip (aerodynamics); Seafloor spreading; Interplate earthquake; Intraplate earthquake; Geodetic datum; Geophysics; Tectonics; Geodesy","score_opus":0.030307379915224027,"score_gpt":0.25667734076058435,"score_spread":0.22636996084536032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2316238748","genre_codex":"editorial","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00020811424,0.16741511,0.00038031855,0.3702338,0.45922828,0.00003135704,0.00013390474,0.000032023847,0.0023370893],"genre_scores_gemma":[0.002525936,0.12865882,0.00050507544,0.1711839,0.6877047,0.00005047983,0.0001531851,0.00006510311,0.009152921],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975859,0.0006352065,0.0002199144,0.0005270833,0.00078252616,0.00024944101],"domain_scores_gemma":[0.97878987,0.007207194,0.00063211954,0.0003814891,0.01028387,0.0027054145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006797825,0.0015671611,0.0018229062,0.0018920457,0.002037663,0.0065224525,0.0034523993,0.015057947,0.008331459],"category_scores_gemma":[0.02523609,0.00047062003,0.0013682467,0.0020719345,0.002096288,0.005456875,0.0029046435,0.010359285,0.0058052037],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003123845,0.000010656349,0.000096070085,0.00048449618,0.00001983078,0.000085030864,0.000045649456,0.000045445737,0.000063019506,0.0010239924,0.9866672,0.011427313],"study_design_scores_gemma":[0.00004249479,0.000032843127,0.0007555764,0.0008005121,0.000056644672,0.00019761584,0.0002145562,0.000067881425,0.0000899354,0.004974338,0.9927307,0.00003681811],"about_ca_topic_score_codex":0.0075718397,"about_ca_topic_score_gemma":0.011861065,"teacher_disagreement_score":0.015057947,"about_ca_system_score_codex":0.0032458645,"about_ca_system_score_gemma":0.00510705,"threshold_uncertainty_score":0.03595072},"labels":[],"label_agreement":null},{"id":"W2316341725","doi":"10.1002/2015jb012415","title":"In situ stress magnitudes at the toe of the Nankai Trough Accretionary Prism, offshore Shikoku Island, Japan","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Geology; Accretionary wedge; Thrust fault; Seafloor spreading; Seismology; Submarine pipeline; Thrust; Borehole; Differential stress; Slip (aerodynamics); Fault (geology); Tectonics; Subduction; Deformation (meteorology); Geotechnical engineering; Geophysics","score_opus":0.03230259012813515,"score_gpt":0.30356646764587303,"score_spread":0.2712638775177379,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2316341725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992532,0.000019761439,0.00009221525,0.0000060876973,0.0000015258075,0.0000021413814,0.00019620423,0.000008121587,0.00042071388],"genre_scores_gemma":[0.9993206,0.000025747238,0.00024610973,0.000005391883,0.0000018475197,0.0000048942843,0.00024066461,0.0000017986703,0.0001528659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998927,0.0000069155813,0.000011593154,0.00003817037,0.000028677357,0.000021938806],"domain_scores_gemma":[0.9997961,0.000014605348,0.00005064854,0.000013552178,0.000074545365,0.000050654337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018322135,0.00040852712,0.00024358444,0.00069154386,0.00044525426,0.00038573434,0.00036701828,0.00032757837,0.0007262235],"category_scores_gemma":[0.00030248245,0.00025470147,0.0002134874,0.0006689883,0.0002610004,0.00030366136,0.00045351114,0.00017431332,0.00016541223],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014270855,0.000041505133,0.9467248,0.00006654589,0.00007659618,0.00032505367,0.0006275169,0.0022072536,0.041486274,0.000037923714,0.00013977518,0.008124022],"study_design_scores_gemma":[0.000007650701,0.000031015643,0.9960984,0.000005749466,0.000018647714,0.00003510607,0.00035749024,0.0020775027,0.0012230637,0.000009095349,0.00013044807,0.0000057105362],"about_ca_topic_score_codex":0.047377095,"about_ca_topic_score_gemma":0.12666126,"teacher_disagreement_score":0.047377095,"about_ca_system_score_codex":0.00041499405,"about_ca_system_score_gemma":0.00047710608,"threshold_uncertainty_score":0.0942027},"labels":[],"label_agreement":null},{"id":"W2317079389","doi":"10.1785/0120100347","title":"Can Lateral Viscosity Contrasts Explain Asymmetric Interseismic Deformation around Strike-Slip Faults?","year":2012,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Southern California Earthquake Center","keywords":"Geology; Slip (aerodynamics); Strike-slip tectonics; Seismology; Deformation (meteorology); Viscosity; Fault (geology); Materials science; Physics; Composite material; Thermodynamics; Oceanography","score_opus":0.015521993114292839,"score_gpt":0.2108131774607503,"score_spread":0.19529118434645745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317079389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98532945,0.00039373495,0.0071923286,0.0008137421,0.00003547256,0.000023595638,0.0002358413,0.00013589673,0.0058398624],"genre_scores_gemma":[0.9995474,0.000047750098,0.00019820104,0.000021900214,0.000009265549,0.0000030671872,0.000028019456,0.000018367864,0.00012592539],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997876,0.000045981775,0.000015335188,0.00005805716,0.00003221134,0.000060831662],"domain_scores_gemma":[0.9990802,0.00027184215,0.0003244848,0.00011540296,0.00007252785,0.00013566058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005524118,0.00069355586,0.0006495406,0.0009556217,0.0003344265,0.0016198269,0.001054786,0.0012328727,0.0016807009],"category_scores_gemma":[0.0033005206,0.00054244447,0.00071953714,0.000478747,0.0008524469,0.0020113545,0.00090478844,0.00046737614,0.00043603085],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004913664,0.0003426602,0.31110606,0.00026829203,0.00042001405,0.0014344857,0.0004928675,0.60521936,0.030244173,0.028450815,0.0015513831,0.019978538],"study_design_scores_gemma":[0.000052007857,0.000078180856,0.07111923,0.000036402922,0.00005190643,0.00016198044,0.00018919146,0.90781397,0.0011290789,0.018685034,0.0006269533,0.000056079294],"about_ca_topic_score_codex":0.0046580094,"about_ca_topic_score_gemma":0.0035600064,"teacher_disagreement_score":0.0046580094,"about_ca_system_score_codex":0.00083898177,"about_ca_system_score_gemma":0.000353351,"threshold_uncertainty_score":0.009261787},"labels":[],"label_agreement":null},{"id":"W2318910466","doi":"10.1785/gssrl.73.4.534","title":"The Seismicity of the Western Lake Ontario Area: Results from the Southern Ontario Seismic Network (SOSN), 1992-2001","year":2002,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ontario Power Generation; Western University","funders":"","keywords":"Induced seismicity; Geology; Seismology; Archaeology; Geography","score_opus":0.09176900210491863,"score_gpt":0.25618847911900194,"score_spread":0.16441947701408333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2318910466","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94016224,0.0013537842,0.00020893286,0.0005143202,0.000019260182,0.00013605987,0.03954938,0.000055150387,0.018000891],"genre_scores_gemma":[0.95593035,0.0021438363,0.0005077912,0.00013096094,0.00003069706,0.00013333482,0.027995817,0.00003332509,0.013093896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995734,0.000012716246,0.000027210697,0.00004736162,0.00024359187,0.00009575772],"domain_scores_gemma":[0.9989906,0.000020587118,0.00018182135,0.000024139721,0.0006531841,0.00012960857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019881842,0.00038007635,0.00024997766,0.0014147386,0.0016615908,0.0007905459,0.000527869,0.00027443923,0.0019965228],"category_scores_gemma":[0.0010544434,0.00027302656,0.0002494158,0.004284612,0.00045707624,0.00040666456,0.00086750556,0.00020695082,0.0005749574],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020649002,0.000039209084,0.94638616,0.00035546636,0.00009371728,0.00031759238,0.003700641,0.00081881636,0.0013062255,0.00018800178,0.024484439,0.022103215],"study_design_scores_gemma":[0.000011159398,0.000010307535,0.98881567,0.000029219296,0.000019665476,0.000027961503,0.0008911897,0.00019939638,0.00008660604,0.000010771796,0.009890692,0.000007321374],"about_ca_topic_score_codex":0.9881386,"about_ca_topic_score_gemma":0.99729496,"teacher_disagreement_score":0.013335226,"about_ca_system_score_codex":0.013335226,"about_ca_system_score_gemma":0.014492754,"threshold_uncertainty_score":0.09675431},"labels":[],"label_agreement":null},{"id":"W2319378692","doi":"10.1785/0220140008","title":"Two Moderate Earthquakes near Montreal: 10 October and 6 November 2012","year":2014,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"Seismology; Geology","score_opus":0.05313396013426491,"score_gpt":0.29895593374094226,"score_spread":0.24582197360667735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319378692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9532026,0.00061644614,0.00056634884,0.0040078135,0.00045100338,0.00033004826,0.008959488,0.0002805655,0.03158566],"genre_scores_gemma":[0.9715679,0.00035662254,0.00053981825,0.0008148114,0.0002844252,0.00007219225,0.00503993,0.000044480763,0.021279706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99953806,0.000020616362,0.0000110110595,0.000065947075,0.00017153872,0.00019291269],"domain_scores_gemma":[0.9991732,0.000033598775,0.00011238172,0.000036707497,0.00023252169,0.00041154557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030968175,0.0008154786,0.0003384292,0.0009022261,0.0027264082,0.0010669408,0.0007078683,0.0015325026,0.005046594],"category_scores_gemma":[0.001223239,0.00033554138,0.00023866114,0.0009633293,0.0007389523,0.0004763442,0.0015836427,0.0012654436,0.0006192429],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00298842,0.0010498128,0.58769244,0.00060298544,0.0005108519,0.026615266,0.018993719,0.003610437,0.036110777,0.0026599208,0.22373685,0.095428504],"study_design_scores_gemma":[0.00003572393,0.00011347651,0.97565746,0.00003112612,0.000015396898,0.00035946563,0.0018035526,0.0003131604,0.00051308924,0.00006243391,0.02104371,0.000051323677],"about_ca_topic_score_codex":0.7234189,"about_ca_topic_score_gemma":0.9350838,"teacher_disagreement_score":0.2765811,"about_ca_system_score_codex":0.0069025108,"about_ca_system_score_gemma":0.00325253,"threshold_uncertainty_score":0.55641985},"labels":[],"label_agreement":null},{"id":"W2319468883","doi":"10.1785/0120120022","title":"Re-Estimated Effects of Deep Episodic Slip on the Occurrence and Probability of Great Earthquakes in Cascadia","year":2013,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Observatory; Suite; Citation; Geological survey; Icon; Geology; History; Archaeology; Library science; Computer science; Paleontology; Astronomy; Physics","score_opus":0.017650705058637802,"score_gpt":0.21179738698687262,"score_spread":0.1941466819282348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2319468883","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.73821324,0.0067805494,0.007686974,0.006117699,0.0011764951,0.00014496027,0.2038583,0.0019255658,0.034096133],"genre_scores_gemma":[0.93929857,0.0015946045,0.000926341,0.00016512215,0.0002420599,0.00005995518,0.051878206,0.00022666698,0.0056084753],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99837303,0.00041582764,0.000228967,0.00037978456,0.00043373337,0.00016866841],"domain_scores_gemma":[0.9902249,0.0028191947,0.0012219198,0.0014838724,0.0037179564,0.00053227996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002417357,0.0008649547,0.0008200649,0.0030149622,0.00041839725,0.0013206179,0.0010067314,0.0005270329,0.009812258],"category_scores_gemma":[0.024093227,0.00043366852,0.0017130141,0.0041662264,0.00029054203,0.001104254,0.0019034486,0.0013091785,0.0037062578],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003357057,0.000033195873,0.8816663,0.0005801755,0.002430467,0.00055378,0.00067079253,0.02083233,0.00037133976,0.00050965184,0.06275682,0.029259428],"study_design_scores_gemma":[0.000044400833,0.00004258165,0.9595989,0.00026835545,0.0006636245,0.00014645967,0.001137794,0.01110482,0.00024281586,0.00050359615,0.026188582,0.00005814324],"about_ca_topic_score_codex":0.28623235,"about_ca_topic_score_gemma":0.30194837,"teacher_disagreement_score":0.71376765,"about_ca_system_score_codex":0.001558898,"about_ca_system_score_gemma":0.0017174663,"threshold_uncertainty_score":0.56913257},"labels":[],"label_agreement":null},{"id":"W2321921567","doi":"10.1130/g32428.1","title":"Successive detachment faults and mantle unroofing at magma-poor rifted margins","year":2011,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Geology; Citation; Crust; Mantle (geology); Icon; Paleontology; Library science; Computer science","score_opus":0.021554219014433235,"score_gpt":0.20509843845281014,"score_spread":0.1835442194383769,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2321921567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.980395,0.005555647,0.00013420064,0.0023341335,0.00004577435,0.000011617405,0.0015231011,0.000016874137,0.009983605],"genre_scores_gemma":[0.9942128,0.0020971363,0.00006857309,0.00005646579,0.00006677616,0.0000028487016,0.0007850032,0.0000070456904,0.0027034574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997657,0.000029366403,0.000021957034,0.00003785862,0.000058129735,0.00008696972],"domain_scores_gemma":[0.9984126,0.00021639524,0.0009970213,0.000047853664,0.00013735452,0.00018873608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033334963,0.00013481756,0.00024688026,0.001404048,0.0006719073,0.0014803128,0.00029932684,0.00055131374,0.013324553],"category_scores_gemma":[0.0032940737,0.00014420762,0.00025865468,0.0020206692,0.00091038086,0.0006713952,0.0013802431,0.00048048267,0.00088358833],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024149824,0.000025222213,0.95138466,0.00015986632,0.00007077766,0.0009918666,0.0033445694,0.0006020899,0.0005225823,0.0018617089,0.009957628,0.030837577],"study_design_scores_gemma":[0.000007409495,0.000027938459,0.99126816,0.00008136509,0.000025249876,0.00031827085,0.0017581732,0.00008689887,0.000094890485,0.0007696355,0.005553427,0.00000855351],"about_ca_topic_score_codex":0.02632661,"about_ca_topic_score_gemma":0.06615482,"teacher_disagreement_score":0.02632661,"about_ca_system_score_codex":0.0006973523,"about_ca_system_score_gemma":0.0005769317,"threshold_uncertainty_score":0.052346706},"labels":[],"label_agreement":null},{"id":"W2322069610","doi":"10.1785/gssrl.73.2.125","title":"The 14 November 2001, Mw = 7.8 Kokoxili Earthquake in Northern Tibet (Qinghai Province, China)","year":2002,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; Institut de Physique du Globe de Paris; Centre National de la Recherche Scientifique","keywords":"Globe; Icon; Citation; China; Geology; Humanities; Library science; History; Cartography; Geography; Art; Archaeology; Computer science; Psychology","score_opus":0.06196564442182397,"score_gpt":0.2813876215541335,"score_spread":0.21942197713230951,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2322069610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.56661487,0.023471262,0.00062801066,0.010895768,0.0016470248,0.00035945058,0.25676808,0.0005848888,0.13903065],"genre_scores_gemma":[0.63710773,0.021333707,0.0008322484,0.00082667795,0.0010998773,0.000112556976,0.19195749,0.000122112,0.14660761],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9998971,0.0000060454604,0.000010726484,0.000011709577,0.0000487447,0.000025603767],"domain_scores_gemma":[0.9997669,0.000015752248,0.00006398884,0.000011574641,0.000084522006,0.000057329482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025369762,0.00036911236,0.00037128615,0.0027955568,0.0008154958,0.0009296316,0.0003465898,0.00048685202,0.016929945],"category_scores_gemma":[0.00062427274,0.00013829824,0.00019542764,0.007115288,0.0002067313,0.0004916258,0.0008017015,0.00021069453,0.0040134066],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041502292,0.000056838377,0.1898599,0.003982621,0.00016782456,0.0031784791,0.0032878486,0.0019824984,0.0033351511,0.0012495562,0.6266986,0.16578563],"study_design_scores_gemma":[0.0000769635,0.000073889394,0.83736616,0.00033752416,0.00008575719,0.00036945494,0.0019502951,0.00045184421,0.00036719404,0.00020749134,0.15868469,0.000028671142],"about_ca_topic_score_codex":0.10161341,"about_ca_topic_score_gemma":0.28688836,"teacher_disagreement_score":0.10161341,"about_ca_system_score_codex":0.0010404127,"about_ca_system_score_gemma":0.0021927862,"threshold_uncertainty_score":0.20204389},"labels":[],"label_agreement":null},{"id":"W2323307426","doi":"10.2208/kaigan.70.i_356","title":"Numerical Experiment on Observation Capabilities of Oceanographic Radar on Far Field and Near Field Tsunamis","year":2014,"lang":"en","type":"article","venue":"Journal of Japan Society of Civil Engineers Ser B2 (Coastal Engineering)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Radar; Peninsula; Near and far field; Field (mathematics); Tsunami wave; Geography; Engineering; Telecommunications; Physics","score_opus":0.008693594568114376,"score_gpt":0.18993746684502796,"score_spread":0.18124387227691358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2323307426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736303,0.00004809134,0.0017323892,0.000032238175,0.0000093155195,0.0000097855855,0.000054773176,0.000035734123,0.00071479566],"genre_scores_gemma":[0.9984744,0.000028992872,0.0013210552,0.0000038180565,0.0000025349639,0.000007577617,0.00006743655,0.0000029008427,0.000091350135],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99972004,0.00006623593,0.000024377785,0.00006024102,0.000050825456,0.0000782351],"domain_scores_gemma":[0.9983638,0.0008816457,0.00016987725,0.00016742581,0.00027812496,0.00013921368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009090045,0.0005606087,0.00055743015,0.0005462364,0.00038715248,0.00039127617,0.00043444164,0.00060611556,0.00070821645],"category_scores_gemma":[0.0023127869,0.00027980385,0.000529033,0.00042754482,0.0005178751,0.00074224785,0.00057973654,0.0005065386,0.00006364995],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063580414,0.00046875645,0.061125755,0.00013279115,0.00010484107,0.0003796462,0.00025904257,0.89145315,0.030839875,0.0007644952,0.00036968398,0.0134662455],"study_design_scores_gemma":[0.00008571729,0.000359696,0.019339046,0.000008861465,0.000056840156,0.000032407803,0.00010797504,0.97410303,0.005637051,0.00014619026,0.00009414014,0.000029009638],"about_ca_topic_score_codex":0.0083739525,"about_ca_topic_score_gemma":0.003221077,"teacher_disagreement_score":0.0083739525,"about_ca_system_score_codex":0.0002922347,"about_ca_system_score_gemma":0.00031155243,"threshold_uncertainty_score":0.016650379},"labels":[],"label_agreement":null},{"id":"W2324030700","doi":"10.1016/j.ijggc.2016.03.018","title":"Using microseismic data recorded at the Weyburn CCS-EOR site to assess the likelihood of induced seismic activity","year":2016,"lang":"en","type":"article","venue":"International journal of greenhouse gas control","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"British Geological Survey; Petroleum Technology Research Centre; U.S. Department of Energy","keywords":"Microseism; Induced seismicity; Geophone; Caprock; Hydraulic fracturing; Geomechanics; Geology; Seismology; Petroleum engineering; Enhanced oil recovery; Volume (thermodynamics); Wellbore; Geotechnical engineering","score_opus":0.07205803077957872,"score_gpt":0.29741149403744027,"score_spread":0.22535346325786154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2324030700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99569345,0.000014802002,0.0006920633,0.000023463863,0.0000056968925,0.000032546355,0.0020961394,0.000026150406,0.0014157202],"genre_scores_gemma":[0.99410206,0.000028237275,0.0016548807,0.0000131154575,0.00000943334,0.000029489074,0.0033675286,0.000009028739,0.0007861406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996118,0.00006818644,0.000030413716,0.00009193997,0.00012776523,0.00007003595],"domain_scores_gemma":[0.9984193,0.0003525444,0.00053616805,0.00012556705,0.0004122556,0.0001540917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005528888,0.0002975528,0.00017388187,0.0016082091,0.00034209737,0.00039400614,0.00032060652,0.00042506974,0.0014787158],"category_scores_gemma":[0.0024905459,0.00012913154,0.00018667572,0.0016512909,0.00015949711,0.0004339772,0.0003624266,0.00035169418,0.0005004365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015384294,0.00016482695,0.9785953,0.000024924122,0.00005864427,0.00017086789,0.00021540934,0.003267163,0.008048987,0.00011637674,0.000577315,0.008606289],"study_design_scores_gemma":[0.000013887992,0.00009164634,0.99024373,0.000008359544,0.000019781954,0.00004094138,0.00022758718,0.0077520604,0.0010421618,0.00003649854,0.0005158444,0.0000073923993],"about_ca_topic_score_codex":0.04724602,"about_ca_topic_score_gemma":0.15336172,"teacher_disagreement_score":0.04724602,"about_ca_system_score_codex":0.0004006493,"about_ca_system_score_gemma":0.0006282949,"threshold_uncertainty_score":0.09394199},"labels":[],"label_agreement":null},{"id":"W2324502495","doi":"10.1785/gssrl.82.6.984","title":"Moment Magnitude (Mw) Conversion Relations for Use in Hazard Assessment in Eastern Canada","year":2011,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Citation; Geological survey; Moment magnitude scale; Hazard; Library science; Observatory; Geography; Geology; Seismology; Information retrieval; Computer science; Physics; Paleontology; Mathematics; Astronomy; Chemistry","score_opus":0.15667304466622636,"score_gpt":0.3194642701478137,"score_spread":0.16279122548158734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2324502495","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.045279305,0.0037906237,0.021247085,0.0022904652,0.0006135729,0.0012446146,0.3148094,0.0059379246,0.60478705],"genre_scores_gemma":[0.42815322,0.0084033245,0.05300736,0.0006459524,0.0002641992,0.00083373743,0.18922666,0.0024684786,0.31699708],"study_design_codex":"not_applicable","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9990381,0.00003745985,0.0000539214,0.000049645838,0.00069297454,0.00012790666],"domain_scores_gemma":[0.9942629,0.0003308531,0.0002502985,0.00019278476,0.0046912082,0.00027189523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071393274,0.0006999219,0.00042062454,0.006762839,0.0017600249,0.0023957198,0.0012466208,0.0004332557,0.08721986],"category_scores_gemma":[0.0067620478,0.0003152995,0.0004757137,0.009971103,0.00045654803,0.0007448111,0.0009637094,0.0008299244,0.012959055],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022253628,0.000098584365,0.053362027,0.0005147792,0.000051562893,0.00029080172,0.0007711363,0.0044823554,0.0013145321,0.005061315,0.64696825,0.28686208],"study_design_scores_gemma":[0.00007749784,0.000055617835,0.35801962,0.00046139798,0.00008015204,0.00022520208,0.0022255485,0.007546657,0.002602564,0.003282027,0.6252603,0.00016338933],"about_ca_topic_score_codex":0.9694812,"about_ca_topic_score_gemma":0.9822578,"teacher_disagreement_score":0.08721986,"about_ca_system_score_codex":0.014534453,"about_ca_system_score_gemma":0.022406435,"threshold_uncertainty_score":0.29177952},"labels":[],"label_agreement":null},{"id":"W2325276434","doi":"10.1785/0120080316","title":"Lg Attenuation near the North Korean Border with China, Part I: Model Development from Regional Earthquake Sources","year":2009,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"China; Seismology; Geology; Attenuation; Geography; Archaeology; Physics","score_opus":0.017269664071056144,"score_gpt":0.2042188958021551,"score_spread":0.18694923173109895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325276434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994601,0.00005728963,0.0027125024,0.000079594094,0.000005166438,0.000025710775,0.0006920893,0.0000727907,0.0017537825],"genre_scores_gemma":[0.9970394,0.000069267095,0.0012512818,0.000011698614,0.000004063315,0.000028396433,0.0009777747,0.0000321786,0.00058597064],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999311,0.000020336965,0.000004311727,0.000021076428,0.0000075776506,0.00001556729],"domain_scores_gemma":[0.9997863,0.00006642422,0.000029727691,0.0000271093,0.00006165804,0.00002892766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044981384,0.0006023139,0.00039417917,0.0005375771,0.00033669703,0.0006940978,0.0013759808,0.00060375803,0.0012474521],"category_scores_gemma":[0.0008185644,0.0005007061,0.00070172525,0.00081031595,0.00037777168,0.0005509586,0.00044797765,0.00048539962,0.00023552084],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007975964,0.00004556658,0.019172257,0.00001973267,0.000041774223,0.00015640576,0.000044878787,0.97674835,0.00063691795,0.00048612806,0.00029230112,0.0022757805],"study_design_scores_gemma":[0.00005184117,0.000017376395,0.007934229,0.000004763916,0.000028250946,0.00001273342,0.000035194735,0.9913987,0.00022272795,0.00013502616,0.00014931303,0.000009925106],"about_ca_topic_score_codex":0.22863393,"about_ca_topic_score_gemma":0.09788932,"teacher_disagreement_score":0.22863393,"about_ca_system_score_codex":0.0014387231,"about_ca_system_score_gemma":0.0011530443,"threshold_uncertainty_score":0.4546063},"labels":[],"label_agreement":null},{"id":"W2325344118","doi":"10.1002/2015jb012136","title":"Laboratory observations of time‐dependent frictional strengthening and stress relaxation in natural and synthetic fault gouges","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Shearing (physics); Geology; Creep; Calcite; Slip (aerodynamics); Feldspar; Shear (geology); Quartz; Fault gouge; Geotechnical engineering; Fault (geology); Mineralogy; Seismology; Petrology; Materials science; Composite material","score_opus":0.027909595858677392,"score_gpt":0.2842998314084204,"score_spread":0.256390235549743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2325344118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99978465,0.000012894067,0.000109893575,0.0000013990699,3.707608e-7,0.0000022267259,0.000036850724,0.000003957638,0.00004783838],"genre_scores_gemma":[0.9996215,0.000012594559,0.0001971797,0.0000026219554,5.359478e-7,0.0000058750775,0.000100666235,0.0000014619902,0.000057633202],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999317,0.000010546903,0.0000064820492,0.000018246543,0.00001666864,0.00001641413],"domain_scores_gemma":[0.99979943,0.000030041698,0.00007776218,0.000021607662,0.00003626507,0.00003501368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012196622,0.00017931037,0.000118021446,0.00027598784,0.00017934934,0.00015820071,0.00015340872,0.00014362288,0.0003864707],"category_scores_gemma":[0.00023044233,0.00009901695,0.00012657266,0.00015637431,0.00038422065,0.00012182976,0.00020616953,0.00015158732,0.00005143025],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119993114,0.000027629912,0.017466608,0.000016854106,0.000010179571,0.000052767555,0.00009564733,0.00016498537,0.98138154,0.000018761597,0.00001317847,0.00063190935],"study_design_scores_gemma":[0.000031505555,0.0019625972,0.46301937,0.0000068016857,0.000032187112,0.00038170887,0.00039733973,0.0023819217,0.5312481,0.00005552987,0.00046541588,0.000017517745],"about_ca_topic_score_codex":0.0019254365,"about_ca_topic_score_gemma":0.0032352635,"teacher_disagreement_score":0.0019254365,"about_ca_system_score_codex":0.00018490071,"about_ca_system_score_gemma":0.0000900388,"threshold_uncertainty_score":0.0038284063},"labels":[],"label_agreement":null},{"id":"W2326820522","doi":"10.1190/segam2014-1647.1","title":"Estimating moment magnitude of microseismic events using true amplitude stacking","year":2014,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Microsemi (Canada)","funders":"","keywords":"Microseism; Magnitude (astronomy); Amplitude; Moment (physics); Stacking; Moment magnitude scale; Computer science; Mathematics; Physics; Geology; Optics; Seismology; Geometry; Classical mechanics; Nuclear magnetic resonance; Scaling","score_opus":0.02602471548908163,"score_gpt":0.2512091129678881,"score_spread":0.22518439747880648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2326820522","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.090358265,0.00010980722,0.90659904,0.000059231752,0.00003138523,0.00003534489,0.00044412757,0.0010314868,0.001331305],"genre_scores_gemma":[0.5833239,0.00012619203,0.41474208,0.000016504478,0.000084535444,0.00005698747,0.00075585535,0.00015191312,0.0007421016],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995838,0.00005802108,0.000034463603,0.0000894102,0.00019000465,0.00004425113],"domain_scores_gemma":[0.9985468,0.00038479967,0.00037714487,0.00023023775,0.00039670206,0.0000642924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005276408,0.00055933255,0.00037310817,0.002317233,0.00024931927,0.0008690713,0.000533033,0.00035019848,0.001388713],"category_scores_gemma":[0.004441393,0.00034899334,0.00038710007,0.0010922581,0.00025110634,0.0009890717,0.00073686556,0.0005433402,0.0007133846],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021321916,0.00007839857,0.0519046,0.00018610401,0.00019897273,0.0002694274,0.00037952038,0.08825865,0.1224489,0.009674679,0.0021678673,0.72421974],"study_design_scores_gemma":[0.000022155546,0.0002127061,0.100613676,0.000050530998,0.000105401145,0.0005523684,0.00025224185,0.7918296,0.08119662,0.016520847,0.008536073,0.000107770786],"about_ca_topic_score_codex":0.0011264945,"about_ca_topic_score_gemma":0.0014333253,"teacher_disagreement_score":0.002317233,"about_ca_system_score_codex":0.00021657915,"about_ca_system_score_gemma":0.0003405407,"threshold_uncertainty_score":0.0046456456},"labels":[],"label_agreement":null},{"id":"W2327022890","doi":"10.1103/physrevlett.108.038501","title":"No Evidence of Magnitude Clustering in an Aftershock Sequence of Nano- and Picoseismicity","year":2012,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Aftershock; Induced seismicity; Sequence (biology); Seismology; Magnitude (astronomy); Geology; Completeness (order theory); Cluster analysis; Seismic hazard; Hazard; Statistics; Mathematics; Physics","score_opus":0.05690072971655026,"score_gpt":0.30295087708311824,"score_spread":0.246050147366568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2327022890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972608,0.000072484756,0.00065774145,0.000040689276,0.0000032653634,0.0000068257323,0.00014541543,0.000012517836,0.0018001857],"genre_scores_gemma":[0.9991716,0.000030680712,0.00019823104,0.000014905134,0.00000382214,0.0000049806386,0.00024160737,0.000003315752,0.0003309159],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998882,0.000013514137,0.000015312473,0.000033463188,0.000028533517,0.0000211003],"domain_scores_gemma":[0.9982041,0.00037197847,0.0006809825,0.0003247099,0.00020798047,0.00021020825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001849321,0.000066273795,0.0002460186,0.00049181114,0.0002308879,0.00039069526,0.00018761736,0.00023029605,0.002141979],"category_scores_gemma":[0.0020550808,0.00009373266,0.000113133785,0.0006806617,0.00047376848,0.0002596009,0.00041324223,0.00023063333,0.00031735597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050832186,0.00010780921,0.9196892,0.0001450964,0.00011587647,0.0010046638,0.0015149479,0.006101922,0.04296338,0.005566802,0.00091136387,0.021370655],"study_design_scores_gemma":[0.000006681013,0.00010876291,0.9933426,0.000009495082,0.000018417091,0.00045570984,0.00038643443,0.00213325,0.0011988151,0.0010035913,0.0013278219,0.000008543142],"about_ca_topic_score_codex":0.0015292241,"about_ca_topic_score_gemma":0.002559764,"teacher_disagreement_score":0.002141979,"about_ca_system_score_codex":0.00021262646,"about_ca_system_score_gemma":0.00019841788,"threshold_uncertainty_score":0.0071656704},"labels":[],"label_agreement":null},{"id":"W2327197355","doi":"10.1190/segam2013-1106.1","title":"Hydraulic fracturing triggers postglacial rebound related strain release","year":2013,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Microsemi (Canada)","funders":"","keywords":"Hydraulic fracturing; Strain (injury); Geology; Petroleum engineering; Geotechnical engineering","score_opus":0.010446535546829786,"score_gpt":0.1971640767985385,"score_spread":0.18671754125170872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2327197355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99937904,0.000015622913,0.00005238706,0.000022108496,0.0000018401207,0.0000020108896,0.000103561506,0.000017329425,0.0004061172],"genre_scores_gemma":[0.9996753,0.000009541526,0.00003494455,0.000009496001,0.0000018965324,0.0000020756183,0.00016380643,0.0000011618848,0.00010182337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999298,0.0000059189733,0.000003389496,0.00001718012,0.000016418997,0.000027284801],"domain_scores_gemma":[0.99977845,0.000022832884,0.00007440733,0.000014179708,0.000065340784,0.000044825436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009888994,0.00013791991,0.00015233994,0.000525373,0.00027920588,0.00029298628,0.00014412307,0.0002908979,0.0010217095],"category_scores_gemma":[0.00037076266,0.00010860696,0.00007711815,0.0003796729,0.00019338069,0.00016485059,0.0002924574,0.00021536218,0.00016897696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026793696,0.00008381115,0.9339368,0.000033660566,0.000038688948,0.0009288731,0.00055092754,0.0011324827,0.04972794,0.00007013338,0.00089961925,0.012329251],"study_design_scores_gemma":[0.0000017762068,0.000022830875,0.99857175,0.0000018480199,0.0000031833747,0.000047191857,0.00019958187,0.0005295815,0.00050191587,0.000012708399,0.00010530705,0.0000022384343],"about_ca_topic_score_codex":0.01886793,"about_ca_topic_score_gemma":0.056025438,"teacher_disagreement_score":0.01886793,"about_ca_system_score_codex":0.0004690858,"about_ca_system_score_gemma":0.00024834703,"threshold_uncertainty_score":0.037516236},"labels":[],"label_agreement":null},{"id":"W2328011357","doi":"10.1190/segj082006-001.106","title":"Thin-skinned extension, salt dynamics and deformation in dynamic depositional systems at passive margins","year":2006,"lang":"en","type":"article","venue":"Proceedings of the 8th SEGJ International Symposium","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Extension (predicate logic); Dynamics (music); Sedimentary depositional environment; Deformation (meteorology); Geology; Salt (chemistry); Computer science; Geomorphology; Physics; Chemistry; Acoustics; Oceanography; Programming language","score_opus":0.0038572658791682477,"score_gpt":0.18294590498805532,"score_spread":0.1790886391088871,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2328011357","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99870086,0.00002168479,0.0009958113,0.000009588994,5.5006086e-7,0.0000013528007,0.000017016675,0.000007760458,0.00024533793],"genre_scores_gemma":[0.9995184,0.000020820973,0.00031896913,0.0000012067015,4.911083e-7,0.0000015449203,0.000018577763,0.0000018224541,0.00011824943],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999782,0.0000036648937,0.0000030845729,0.0000072414123,0.0000039679103,0.000003904345],"domain_scores_gemma":[0.99991834,0.000021298381,0.000026462667,0.0000108167205,0.000008252315,0.000014898729],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008958497,0.00015896768,0.00012006181,0.00021425333,0.00013711059,0.0003414044,0.00016884664,0.00019139407,0.0004809356],"category_scores_gemma":[0.0004408613,0.00019617534,0.00012876501,0.000185042,0.00045695732,0.00030695603,0.00027531586,0.00010015488,0.00006425744],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035298493,0.000095420655,0.26455143,0.000065778775,0.000060462593,0.000566929,0.00075766054,0.56348854,0.14485368,0.0054781474,0.00015625103,0.0195727],"study_design_scores_gemma":[0.00003437208,0.00016524045,0.33115906,0.000011656631,0.000024797047,0.00017306847,0.00021750732,0.6543748,0.009933152,0.0032711418,0.0006091655,0.000026026992],"about_ca_topic_score_codex":0.0036566188,"about_ca_topic_score_gemma":0.0045660404,"teacher_disagreement_score":0.0036566188,"about_ca_system_score_codex":0.00032588973,"about_ca_system_score_gemma":0.00014910041,"threshold_uncertainty_score":0.007270694},"labels":[],"label_agreement":null},{"id":"W2328540640","doi":"10.1785/gssrl.71.2.283","title":"Paleoseismicity: Seismicity Evidence for Past Large Earthquakes","year":2000,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Induced seismicity; Geology; Seismology","score_opus":0.15482362421536738,"score_gpt":0.35899622911854234,"score_spread":0.20417260490317496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2328540640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877702,0.00024503304,0.007343337,0.00007805793,0.000003999156,0.000023605771,0.00082331244,0.000094814255,0.0036175775],"genre_scores_gemma":[0.99796957,0.00007076271,0.0011670827,0.0000076009633,0.000004350898,0.0000051217726,0.0005714195,0.000005048102,0.00019908219],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996619,0.0001080251,0.000032656535,0.00008678869,0.000070379814,0.000040227453],"domain_scores_gemma":[0.99821126,0.0005527657,0.00070158945,0.00020889576,0.00012342517,0.00020204534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074873224,0.000317639,0.00017768463,0.003270493,0.00023113172,0.00079140667,0.00035893076,0.00043575492,0.001556742],"category_scores_gemma":[0.0035365166,0.0002505902,0.00029035402,0.0023143785,0.00060127693,0.00081912155,0.0009742995,0.00025273892,0.00036179088],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014735627,0.000028664232,0.97314125,0.000029471563,0.00009643772,0.00019000482,0.00024063568,0.009772369,0.0039360286,0.0008842085,0.00024083912,0.011292716],"study_design_scores_gemma":[0.000013419496,0.00011648141,0.9675982,0.00002730196,0.000025715073,0.0008983955,0.00031741115,0.02656246,0.0012461578,0.0016022162,0.0015656629,0.00002644489],"about_ca_topic_score_codex":0.0066856775,"about_ca_topic_score_gemma":0.009756395,"teacher_disagreement_score":0.0066856775,"about_ca_system_score_codex":0.0004399914,"about_ca_system_score_gemma":0.00027226828,"threshold_uncertainty_score":0.013293505},"labels":[],"label_agreement":null},{"id":"W2329545350","doi":"10.1785/0220150170","title":"Reply to “Comment on ‘Aftershock Statistics for Earthquakes in the St. Lawrence Valley’ by Azadeh Fereidoni and Gail M. Atkinson” by John Ebel","year":2015,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Citation; Icon; Library science; Download; History; Art history; Computer science; World Wide Web","score_opus":0.10139594364255494,"score_gpt":0.326111672295534,"score_spread":0.22471572865297906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2329545350","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00028242427,0.001113659,0.00009567469,0.95671606,0.03838036,0.000019693716,0.000766604,0.000115443785,0.0025101646],"genre_scores_gemma":[0.0019868223,0.0010284574,0.0001460283,0.9600309,0.017896514,0.000073721494,0.00043086897,0.00011793297,0.018288711],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99688715,0.0004995485,0.0004954809,0.00040235664,0.0012637082,0.00045176432],"domain_scores_gemma":[0.98964804,0.0029438706,0.0008805859,0.00028241688,0.0050114235,0.0012336222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0036074987,0.00092276774,0.0012318493,0.0015298147,0.0027105773,0.0025104734,0.002177014,0.01643839,0.029614754],"category_scores_gemma":[0.039927397,0.00084322906,0.001560401,0.0014972064,0.00226699,0.0035705802,0.0024864718,0.016679753,0.024100935],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008729938,0.0000017268908,0.00011148072,0.000013218849,0.0000018729515,0.000021074422,0.000029409332,0.0000032377288,0.000016519545,0.00009177844,0.9990239,0.00067701616],"study_design_scores_gemma":[0.000034858524,0.00002760096,0.0034165932,0.00029486345,0.000020761981,0.00023518612,0.00058947026,0.00006366794,0.00020813497,0.00091978244,0.9941215,0.00006754601],"about_ca_topic_score_codex":0.038585495,"about_ca_topic_score_gemma":0.037890695,"teacher_disagreement_score":0.038585495,"about_ca_system_score_codex":0.004100753,"about_ca_system_score_gemma":0.0053454484,"threshold_uncertainty_score":0.099071205},"labels":[],"label_agreement":null},{"id":"W2330601677","doi":"10.1139/cjes-2014-0001","title":"Fault zone migration by footwall shortcut and recumbent folding along an inverted fault: example from the Mosha Fault, Central Alborz, Northern Iran","year":2014,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Fault (geology); Seismology; Normal fault","score_opus":0.029548825917799202,"score_gpt":0.2116782938699169,"score_spread":0.1821294679521177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2330601677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992137,0.00008909201,0.0000594132,0.000018025792,0.0000028665959,0.0000056510366,0.000051055224,0.000004347266,0.0005558605],"genre_scores_gemma":[0.99934894,0.000116881725,0.00019909423,0.0000065345257,0.0000028264092,0.0000016543186,0.000088411165,8.941196e-7,0.00023480812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999422,0.0000040065866,0.0000037963923,0.00001089612,0.0000120958775,0.000027049706],"domain_scores_gemma":[0.99993575,0.0000039467395,0.000026506674,0.0000051429456,0.00001595183,0.000012725491],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006502073,0.00021025084,0.00017977979,0.0011298335,0.0005360206,0.00029347802,0.0001737574,0.00026298972,0.0006460552],"category_scores_gemma":[0.0001489052,0.00006880826,0.00020180034,0.0013704221,0.00027023506,0.00012691565,0.00021479186,0.00013911087,0.00010218519],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026966148,0.00007921171,0.93712837,0.000060679475,0.000049773447,0.008343493,0.0020297004,0.0012715653,0.01443381,0.00027979747,0.0005171354,0.035536774],"study_design_scores_gemma":[0.000005466659,0.00003706429,0.99660826,0.0000061316878,0.0000120648065,0.0006622236,0.001174369,0.00047795483,0.00027141298,0.000057368965,0.00068244577,0.0000052515825],"about_ca_topic_score_codex":0.05746808,"about_ca_topic_score_gemma":0.10410321,"teacher_disagreement_score":0.05746808,"about_ca_system_score_codex":0.00042077753,"about_ca_system_score_gemma":0.00037740273,"threshold_uncertainty_score":0.11426717},"labels":[],"label_agreement":null},{"id":"W2332225632","doi":"10.1130/g33019.1","title":"A wider seismogenic zone at Cascadia due to fluid circulation in subducting oceanic crust","year":2012,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Geology; Subduction; Crust; Icon; Citation; Oceanic crust; Seismology; Earth science; Paleontology; Library science; Tectonics; Computer science","score_opus":0.01995504176569848,"score_gpt":0.22029369271989835,"score_spread":0.20033865095419987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2332225632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8829211,0.0060602403,0.0008943216,0.006580361,0.0003525233,0.00005670419,0.0036487067,0.0006203058,0.09886575],"genre_scores_gemma":[0.98964906,0.0018314365,0.00023957099,0.000102381244,0.00017161909,0.000010938635,0.0009386053,0.000056141125,0.007000169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999777,0.00001735285,0.00001939119,0.000050754043,0.00007839245,0.000057002628],"domain_scores_gemma":[0.99959034,0.000033856693,0.00010124712,0.00002868805,0.00010303286,0.00014273204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026330483,0.00040396745,0.00036253218,0.003186487,0.0014887495,0.0016488102,0.0004149588,0.00069068465,0.018991632],"category_scores_gemma":[0.0011089774,0.0003007316,0.0004542302,0.003829979,0.0011628536,0.00073711347,0.0033101814,0.0007551256,0.0013014055],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010179436,0.000110420886,0.77705115,0.0016935513,0.0005214826,0.013137188,0.014575523,0.0059923944,0.039079607,0.0069630235,0.05281662,0.08704112],"study_design_scores_gemma":[0.000028066574,0.000030181616,0.9760464,0.00008230923,0.000054315205,0.00052868825,0.0019658855,0.00022540761,0.0003372997,0.00072931463,0.01995298,0.000019163996],"about_ca_topic_score_codex":0.07018253,"about_ca_topic_score_gemma":0.092456795,"teacher_disagreement_score":0.07018253,"about_ca_system_score_codex":0.0019779378,"about_ca_system_score_gemma":0.0009978979,"threshold_uncertainty_score":0.13954806},"labels":[],"label_agreement":null},{"id":"W2332630834","doi":"10.1190/segam2013-1416.1","title":"Detecting long-period long-duration microseismic events during hydraulic fracturing in the Cline Shale Formation, west Texas: A case study","year":2013,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Microsemi (Canada)","funders":"","keywords":"Microseism; Cline (biology); Hydraulic fracturing; Oil shale; Period (music); Geology; Duration (music); Seismology; Mining engineering; Petroleum engineering; Paleontology; Demography","score_opus":0.01679749948775856,"score_gpt":0.23604647378619373,"score_spread":0.21924897429843518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2332630834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999514,0.000010043529,0.00024353883,0.000013610334,7.047221e-7,0.0000100106245,0.000035821333,0.0000045299316,0.00016764186],"genre_scores_gemma":[0.99884963,0.00002375439,0.0009261395,0.000004789043,0.000002974033,0.000003850127,0.000047816935,0.0000015055905,0.00013938692],"study_design_codex":"observational","study_design_gemma":"case_report","domain_scores_codex":[0.99989164,0.0000150031565,0.00000841864,0.00002832912,0.00003081914,0.000025646834],"domain_scores_gemma":[0.99960047,0.00012400333,0.0001069623,0.000037189046,0.000080778584,0.00005056663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017581445,0.00023050606,0.00012915889,0.00072553067,0.00045005785,0.00027688793,0.00028631254,0.00045548042,0.00033668306],"category_scores_gemma":[0.00045404924,0.00015042606,0.00015875848,0.0005806728,0.00037364385,0.00026408926,0.0003310712,0.00020922055,0.00006140792],"study_design_candidate":"case_report","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024054358,0.00043993446,0.88492244,0.00008613142,0.0000511789,0.018279813,0.0046855537,0.0041815545,0.060450662,0.00020985788,0.0003224061,0.026129993],"study_design_scores_gemma":[0.000009778827,0.0002383759,0.9821087,0.000009747366,0.000024688145,0.0013801081,0.0029494027,0.0064662313,0.0063362513,0.00006775647,0.00039277933,0.000016159796],"about_ca_topic_score_codex":0.013508116,"about_ca_topic_score_gemma":0.04884682,"teacher_disagreement_score":0.013508116,"about_ca_system_score_codex":0.00034720942,"about_ca_system_score_gemma":0.00030328147,"threshold_uncertainty_score":0.026858985},"labels":[],"label_agreement":null},{"id":"W2333139148","doi":"10.1190/1.3627478","title":"Identifying fault activation during hydraulic stimulation in the Barnett shale: Source mechanisms, <i>b</i> values, and energy release analyses of microseismicity","year":2011,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Microsemi (Canada)","funders":"","keywords":"Microseism; Hydraulic fracturing; Geology; Oil shale; Fault (geology); Inversion (geology); Shale gas; Seismology; Source rock; Permeability (electromagnetism); Aquifer; Petroleum engineering; Energy source; Geotechnical engineering; Tectonics; Groundwater; Petroleum; Geomorphology","score_opus":0.047916093029734,"score_gpt":0.25188560090527917,"score_spread":0.2039695078755452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2333139148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99869835,0.00002451772,0.00072522607,0.000009182079,7.7998476e-7,0.0000038079222,0.00005949684,0.000015159609,0.0004635088],"genre_scores_gemma":[0.9995358,0.000008145701,0.0003183541,0.0000012918346,5.4463493e-7,0.0000016423214,0.000037653124,0.0000020307077,0.000094492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000055016153,0.0000036564734,0.000009249144,0.000014102333,0.000010300135],"domain_scores_gemma":[0.9998491,0.000031282816,0.00004934952,0.000007065808,0.000037926533,0.000025324322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011183092,0.00013519707,0.00012680207,0.00079556805,0.00017457214,0.00025711377,0.000109789115,0.0001796557,0.00060894445],"category_scores_gemma":[0.00029390503,0.00014926016,0.00009540963,0.0003600154,0.00020910328,0.00023713507,0.00019239308,0.00014113371,0.00012079065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064663275,0.00012479283,0.7654611,0.00008646851,0.00003993894,0.00040522745,0.00064663024,0.009243274,0.18526569,0.0003893878,0.00023847596,0.037452493],"study_design_scores_gemma":[0.000009139858,0.00006552342,0.9713417,0.00000676455,0.000008912795,0.000106834326,0.00020723788,0.017111711,0.010854621,0.00011277047,0.00016153778,0.000013211257],"about_ca_topic_score_codex":0.0076356884,"about_ca_topic_score_gemma":0.018569054,"teacher_disagreement_score":0.0076356884,"about_ca_system_score_codex":0.00024791528,"about_ca_system_score_gemma":0.0001941204,"threshold_uncertainty_score":0.015182495},"labels":[],"label_agreement":null},{"id":"W2334205565","doi":"10.1016/j.pepi.2016.03.009","title":"Effect of hydrothermal circulation on slab dehydration for the subduction zone of Costa Rica and Nicaragua","year":2016,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Consejo Nacional de Ciencia y Tecnología; Syracuse University","keywords":"Geology; Eclogitization; Slab; Subduction; Mantle wedge; Mantle (geology); Slab window; Hydrothermal circulation; Adakite; Geophysics; Oceanic crust; Petrology; Seismology; Tectonics","score_opus":0.009129353703295984,"score_gpt":0.20573793839697374,"score_spread":0.19660858469367776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2334205565","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99821293,0.00018841242,0.000029640769,0.00013667547,0.0000039938864,0.0000069838934,0.00034847463,0.000008093983,0.0010646852],"genre_scores_gemma":[0.999335,0.00013552938,0.000043332006,0.000018496432,0.0000028529494,0.000007580106,0.00023821788,0.000004811541,0.00021414443],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998036,0.0000595067,0.000016908278,0.00003544041,0.000015966569,0.00006856224],"domain_scores_gemma":[0.99954,0.000106004234,0.00010949775,0.000054065407,0.00010673391,0.00008373518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047371045,0.00030118035,0.00034578436,0.0010183471,0.0006264604,0.0013984918,0.0007287595,0.0005189157,0.0015318211],"category_scores_gemma":[0.0018267584,0.00021975655,0.0006909424,0.0012870224,0.0008104193,0.00053356896,0.0013181407,0.0003290733,0.00013336608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005076278,0.000063738626,0.9768528,0.00010202911,0.0004014843,0.0005383822,0.0012282508,0.009431716,0.0044127386,0.00066013273,0.0004412143,0.0053599207],"study_design_scores_gemma":[0.00001638582,0.000018625062,0.99556786,0.000014101419,0.00006479913,0.00003503621,0.00104833,0.0024056945,0.00027467698,0.00004263278,0.00050269853,0.000009213226],"about_ca_topic_score_codex":0.4602476,"about_ca_topic_score_gemma":0.4838989,"teacher_disagreement_score":0.4602476,"about_ca_system_score_codex":0.0041550477,"about_ca_system_score_gemma":0.0019752015,"threshold_uncertainty_score":0.91513735},"labels":[],"label_agreement":null},{"id":"W2335263249","doi":"10.1190/segam2013-0648.1","title":"Magnitude calibration for microseismic events from hydraulic fracture monitoring","year":2013,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Microsemi (Canada)","funders":"","keywords":"Microseism; Calibration; Hydraulic fracturing; Magnitude (astronomy); Geology; Fracture (geology); Seismology; Computer science; Geotechnical engineering; Statistics; Physics; Mathematics","score_opus":0.0157147230360063,"score_gpt":0.2212334858536739,"score_spread":0.2055187628176676,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2335263249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.73715246,0.00024266768,0.25363696,0.000084591455,0.000042902928,0.00017638091,0.0014369476,0.0015686604,0.0056584612],"genre_scores_gemma":[0.9444732,0.00006519652,0.053590238,0.000018850895,0.000015949614,0.00008787276,0.0011722248,0.0001004953,0.00047592082],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994617,0.000090152025,0.0000529698,0.000119332064,0.00023012498,0.000045699806],"domain_scores_gemma":[0.9987067,0.00031191116,0.00034190092,0.00015692839,0.00043326593,0.000049312133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080120814,0.00037713963,0.00019979828,0.0022783123,0.00016418764,0.0003661872,0.00039911742,0.00032978907,0.0010538057],"category_scores_gemma":[0.004148743,0.00021508904,0.00020816376,0.0010240712,0.00015723899,0.0006256653,0.0006150039,0.00028559606,0.00038708939],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041704852,0.00020555321,0.44314706,0.00034798382,0.00013156973,0.00035860093,0.000707865,0.078394175,0.16828407,0.0029548893,0.00256494,0.30248633],"study_design_scores_gemma":[0.000023155775,0.00015211606,0.76399106,0.000054275697,0.000033505898,0.00033029707,0.00020247867,0.18600145,0.041243907,0.002217055,0.0056887744,0.000061882376],"about_ca_topic_score_codex":0.0010484243,"about_ca_topic_score_gemma":0.0020688716,"teacher_disagreement_score":0.0022783123,"about_ca_system_score_codex":0.00030164415,"about_ca_system_score_gemma":0.0001689671,"threshold_uncertainty_score":0.0042372346},"labels":[],"label_agreement":null},{"id":"W2335832446","doi":"10.1144/sp437.4","title":"New insights into the Kawah Ijen hydrothermal system from geophysical data","year":2016,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Aquifer; Hydrothermal circulation; Geology; Hydrogeology; Impact crater; Geochemistry; Groundwater; Volcano; Silicic; Earth science; Astrobiology; Paleontology","score_opus":0.029172129010388376,"score_gpt":0.22632392734520718,"score_spread":0.1971517983348188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2335832446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994626,0.0004304061,0.0013073105,0.00009649902,0.000012535599,0.00001488361,0.00046099754,0.000024123212,0.0030271981],"genre_scores_gemma":[0.996881,0.00019096998,0.0022582554,0.000013927701,0.000012479449,0.000006486366,0.0003510687,0.00000474904,0.0002810669],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.000018085315,0.000020834323,0.000024216202,0.000028782886,0.000019731955],"domain_scores_gemma":[0.99975556,0.000048581693,0.000065058426,0.000025908776,0.00006963022,0.000035227233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017940733,0.00021196356,0.00024409198,0.0019913816,0.00019349763,0.0006181555,0.000161274,0.0002763652,0.0011469852],"category_scores_gemma":[0.000647195,0.0002053937,0.00010428381,0.0018551993,0.00030437525,0.0007163791,0.0009738531,0.00023109141,0.00015056368],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000142886,0.00006491323,0.8404949,0.00041247366,0.00008935713,0.002034301,0.0048858062,0.0025845887,0.07869737,0.0008670301,0.00080298336,0.06892334],"study_design_scores_gemma":[0.000007176954,0.00003962427,0.9836346,0.00004800608,0.000045173772,0.00035589986,0.0037095149,0.005683696,0.0014039017,0.0005707786,0.004477829,0.00002382537],"about_ca_topic_score_codex":0.0036964372,"about_ca_topic_score_gemma":0.013161071,"teacher_disagreement_score":0.0036964372,"about_ca_system_score_codex":0.00016758466,"about_ca_system_score_gemma":0.00018618866,"threshold_uncertainty_score":0.0073498487},"labels":[],"label_agreement":null},{"id":"W2339250340","doi":"10.1002/2016gl068368","title":"Tsunami data assimilation of Cascadia seafloor pressure gauge records from the 2012 Haida Gwaii earthquake","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Seafloor spreading; Geology; Tsunami earthquake; Seismology; Submarine pipeline; Tide gauge; Data assimilation; Tsunami wave; Oceanography; Meteorology; Sea level; Geography","score_opus":0.06899769150526015,"score_gpt":0.29984606076648074,"score_spread":0.2308483692612206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339250340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974132,0.0000130103,0.00074617023,0.00005779855,0.000019797362,0.0000132011755,0.00063792284,0.00013667934,0.0009621757],"genre_scores_gemma":[0.9980611,0.000013051033,0.00074088183,0.000008054745,0.0000043181594,0.000008441977,0.000893995,0.000008396668,0.00026170418],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998814,0.00001485733,0.000008177647,0.000033707987,0.000035015946,0.00002675827],"domain_scores_gemma":[0.9995115,0.000081123726,0.000049680537,0.00009034759,0.00019881655,0.00006844893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030202427,0.0006187659,0.0003291342,0.0003248125,0.000498968,0.0006247072,0.0006747391,0.00050739397,0.0010832383],"category_scores_gemma":[0.0013520187,0.00039159524,0.00048365537,0.00050779746,0.00043211482,0.0003611245,0.00033820004,0.00060986995,0.00018800651],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039553773,0.0002231682,0.08904458,0.000033148157,0.00016271917,0.00018591656,0.00015404707,0.88860226,0.005877078,0.00030033698,0.0013792022,0.013642057],"study_design_scores_gemma":[0.00014254717,0.000107518295,0.104493946,0.000008711429,0.000051296825,0.000024863642,0.00011947177,0.8910913,0.0031577933,0.00014101212,0.00061971956,0.000041711537],"about_ca_topic_score_codex":0.4283666,"about_ca_topic_score_gemma":0.40886125,"teacher_disagreement_score":0.5716334,"about_ca_system_score_codex":0.0015989192,"about_ca_system_score_gemma":0.0019295748,"threshold_uncertainty_score":0.85174644},"labels":[],"label_agreement":null},{"id":"W2341026646","doi":"","title":"Balanced cross-sections: tools for finding bypassed oil and gas in the Crowsnest Pass and Hinton areas","year":2014,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Folding (DSP implementation); Tectonics; Thrust; Fault (geology); Turtle (robot); Section (typography); Paleontology; Engineering; Structural engineering; Computer science; Aerospace engineering","score_opus":0.029848168249940802,"score_gpt":0.2574888891357334,"score_spread":0.22764072088579262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2341026646","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4311759,0.0008513333,0.4757073,0.00023605867,0.00006411892,0.0008922518,0.02735977,0.050647333,0.013065974],"genre_scores_gemma":[0.41133744,0.00033761346,0.5699334,0.000041746865,0.000021933316,0.0006358888,0.010569432,0.0031743099,0.0039482154],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997063,0.00003915055,0.000031874977,0.000101613696,0.000082709266,0.00003831821],"domain_scores_gemma":[0.9990702,0.00037337522,0.00015263374,0.00008036286,0.00021326139,0.00011009366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009934854,0.00078473997,0.00030192468,0.004748331,0.00046882342,0.0011788938,0.0006441511,0.00048996124,0.015144014],"category_scores_gemma":[0.0021503565,0.0007724642,0.00037197626,0.0016215575,0.0002779859,0.00102104,0.0013579684,0.00029532603,0.0024773993],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009277186,0.00024302819,0.1596356,0.0010502528,0.00026501168,0.0019748812,0.0061980677,0.014282225,0.10379093,0.004442165,0.028096288,0.67909384],"study_design_scores_gemma":[0.00023303887,0.0005074488,0.5088225,0.00047780667,0.00024030256,0.0039861407,0.005610586,0.28526676,0.08061554,0.0069532394,0.10702176,0.0002648933],"about_ca_topic_score_codex":0.008985964,"about_ca_topic_score_gemma":0.026380345,"teacher_disagreement_score":0.99101406,"about_ca_system_score_codex":0.00037211904,"about_ca_system_score_gemma":0.0007565107,"threshold_uncertainty_score":0.050661802},"labels":[],"label_agreement":null},{"id":"W2342149997","doi":"10.1016/j.tecto.2016.04.027","title":"Seismic reflection patterns associated with continental convergent margins through time","year":2016,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Accretionary wedge; Tectonics; Continental margin; Seismology; Metamorphism; Sedimentary rock; Foreland basin; Thrust fault; Paleontology; Subduction","score_opus":0.015460476044176375,"score_gpt":0.20927023231596845,"score_spread":0.19380975627179206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2342149997","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986644,0.000032819768,0.000119024065,0.00000775073,9.173482e-7,9.954065e-7,0.00011998917,0.000006595277,0.0010473854],"genre_scores_gemma":[0.9991887,0.000025505502,0.00010642962,0.0000023987006,0.0000016623935,0.0000010710153,0.00020338531,0.0000039952033,0.0004668592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999951,0.000005653487,0.0000046500454,0.00001705731,0.000008056986,0.000013506829],"domain_scores_gemma":[0.9995689,0.000086835425,0.0001483944,0.000033978595,0.00011230042,0.000049656628],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013349458,0.000128079,0.00009562906,0.0010543158,0.00019908516,0.00038810034,0.00015831224,0.0002328919,0.0019247743],"category_scores_gemma":[0.00086224824,0.0001115706,0.00014173305,0.00075461884,0.00024186222,0.0002070337,0.00039897035,0.0001640307,0.00025890657],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055289036,0.000031258347,0.91084665,0.000033014574,0.0000865711,0.00042431353,0.0019800123,0.002850269,0.061128847,0.0009599749,0.0002684807,0.020837791],"study_design_scores_gemma":[0.00000256373,0.000027442677,0.99801373,0.000004163981,0.000011870679,0.000071655,0.0002300488,0.00067928206,0.0006080011,0.0000485455,0.00029944733,0.000003186053],"about_ca_topic_score_codex":0.0055586216,"about_ca_topic_score_gemma":0.011804251,"teacher_disagreement_score":0.0055586216,"about_ca_system_score_codex":0.00021154743,"about_ca_system_score_gemma":0.00012001739,"threshold_uncertainty_score":0.011052489},"labels":[],"label_agreement":null},{"id":"W2345518418","doi":"10.1126/science.aaf2349","title":"Slow slip near the trench at the Hikurangi subduction zone, New Zealand","year":2016,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":332,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Engineering and Physical Sciences Research Council; Medical Research Council; Lamont-Doherty Earth Observatory, Columbia University; Natural Sciences and Engineering Research Council of Canada; University of Tokyo; European Commission; Japan Society for the Promotion of Science; Ministry of Education, Culture, Sports, Science and Technology; National Science Foundation","keywords":"Trench; Subduction; Geology; Seismology; Episodic tremor and slip; Plate tectonics; Slip (aerodynamics); Tectonics; Geodetic datum; Deformation (meteorology); Pacific Plate; Geodesy; Oceanography","score_opus":0.01489352853183729,"score_gpt":0.21010602517627017,"score_spread":0.19521249664443288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2345518418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991153,0.00002448516,0.00003400819,0.000012273285,9.62752e-7,0.000007688831,0.00016136076,0.0000033748895,0.00064052583],"genre_scores_gemma":[0.99929154,0.000056905006,0.000097884986,0.0000044217754,0.0000013223671,0.000006563241,0.00015882304,0.0000012696296,0.00038124688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998964,0.0000049886835,0.000008488157,0.00003431854,0.00002933363,0.000026508485],"domain_scores_gemma":[0.99980026,0.000015934784,0.00008628865,0.000010513784,0.000040112413,0.00004682886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001299095,0.00023860812,0.00022176605,0.00084275234,0.00065486855,0.00057725265,0.00026566358,0.00024891453,0.000843254],"category_scores_gemma":[0.00047663104,0.00021968133,0.00012390298,0.00072683935,0.0006556785,0.00036847775,0.00066337036,0.00020910568,0.00012984955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021390419,0.000058565383,0.9527376,0.00007877716,0.00005203968,0.0018137712,0.0051169163,0.001174787,0.025159473,0.00010633491,0.00035332737,0.013134493],"study_design_scores_gemma":[0.0000029219118,0.000018485816,0.99896336,0.000003829753,0.000003119681,0.00005672753,0.00049661344,0.0001704824,0.000114391856,0.000007968839,0.0001594087,0.000002701466],"about_ca_topic_score_codex":0.23591232,"about_ca_topic_score_gemma":0.4750326,"teacher_disagreement_score":0.23591232,"about_ca_system_score_codex":0.0010248608,"about_ca_system_score_gemma":0.00076518214,"threshold_uncertainty_score":0.4690783},"labels":[],"label_agreement":null},{"id":"W2346899148","doi":"10.3389/fmars.2016.00057","title":"Modern Approaches in Meteotsunami Research and Early Warning","year":2016,"lang":"en","type":"article","venue":"Frontiers in Marine Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Russian Science Foundation; Shirshov Institute of Oceanology, Russian Academy of Sciences; Division of Ocean Sciences; Hrvatska Zaklada za Znanost; Unity through Knowledge Fund","keywords":"Warning system; Natural hazard; Relevance (law); Meteorology; Environmental science; Hazard; Climatology; Early warning system; Environmental resource management; Geography; Engineering; Geology; Telecommunications; Ecology; Political science","score_opus":0.0666947649828852,"score_gpt":0.2607931529941426,"score_spread":0.1940983880112574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2346899148","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007924528,0.054317884,0.8925785,0.00898269,0.001274274,0.00008962589,0.00031211824,0.00019865003,0.034321733],"genre_scores_gemma":[0.36958203,0.103718005,0.49946442,0.00246093,0.006217369,0.0006349586,0.0006901622,0.00014829692,0.01708383],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985342,0.0007412189,0.00012898867,0.00026264924,0.00027459042,0.00005827403],"domain_scores_gemma":[0.99719185,0.0017701336,0.00033399812,0.00035846746,0.0002750521,0.000070517395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024575288,0.000860336,0.00075841235,0.0025625643,0.0008591945,0.0035024364,0.0015053828,0.0015641623,0.0037426387],"category_scores_gemma":[0.0055102617,0.0003086563,0.00062318455,0.0022148865,0.0032841736,0.002942989,0.0021917378,0.0023721613,0.0012926544],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003444376,0.000044170814,0.0016699497,0.0007213408,0.00007517149,0.00017391054,0.0008930323,0.011822308,0.0013466175,0.79135305,0.0038293009,0.18803668],"study_design_scores_gemma":[0.000012994979,0.000066279856,0.0013499059,0.00030449915,0.00003417611,0.00024152109,0.0005427512,0.019788008,0.0007250282,0.8802422,0.09665238,0.000040163133],"about_ca_topic_score_codex":0.0014028611,"about_ca_topic_score_gemma":0.0012319437,"teacher_disagreement_score":0.0037426387,"about_ca_system_score_codex":0.0013420691,"about_ca_system_score_gemma":0.0014603719,"threshold_uncertainty_score":0.012996793},"labels":[],"label_agreement":null},{"id":"W2353368334","doi":"10.1144/sp439.5","title":"Widening of normal fault zones due to the inhibition of vertical propagation","year":2016,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Normal fault; Geology; Fault (geology); Seismology; Geodesy","score_opus":0.020443790796513303,"score_gpt":0.22443830725936614,"score_spread":0.20399451646285283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2353368334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948066,0.0002829176,0.00362682,0.000018654158,0.0000041732637,0.000003766729,0.00004094984,0.000060921524,0.0011552933],"genre_scores_gemma":[0.9996909,0.000033117012,0.0001416516,0.0000016302181,0.0000013190656,0.0000011773473,0.000016581238,0.0000021664646,0.00011144849],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991333,0.000007552345,0.00000592943,0.000025013376,0.000024002651,0.000024221355],"domain_scores_gemma":[0.9995647,0.0000890776,0.00017446918,0.00007402702,0.000040484814,0.000057161113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013715767,0.00015366786,0.00021273435,0.000449139,0.00019301892,0.0004501308,0.00033184222,0.0002222349,0.0012744763],"category_scores_gemma":[0.0006547066,0.00020926005,0.00018132506,0.00020600525,0.0005104056,0.00030151533,0.00061526394,0.0003276777,0.00012982987],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060558907,0.00010473354,0.1494709,0.00022208829,0.0000766706,0.0012144989,0.00063072,0.08151583,0.72719437,0.007247358,0.0003364177,0.031380877],"study_design_scores_gemma":[0.000049742477,0.00047776964,0.6797844,0.00004234314,0.00007568636,0.0018986639,0.00040943956,0.15937804,0.1475672,0.0052117617,0.005047969,0.00005695524],"about_ca_topic_score_codex":0.0014936008,"about_ca_topic_score_gemma":0.0011346531,"teacher_disagreement_score":0.0014936008,"about_ca_system_score_codex":0.00041101233,"about_ca_system_score_gemma":0.00015117016,"threshold_uncertainty_score":0.0042635202},"labels":[],"label_agreement":null},{"id":"W2373749322","doi":"10.1007/s11631-007-0215-3","title":"Structural geochemistry of gold mineralization in the Linglong-Jiaojia district, Shandong Province, China","year":2007,"lang":"en","type":"article","venue":"Geochemistry","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Chicoutimi","funders":"","keywords":"Geology; Shear zone; Sinistral and dextral; Shear (geology); Brittleness; Quartz; Seismology; Tectonics; Geochemistry; Petrology; Paleontology; Metallurgy","score_opus":0.008677994199512075,"score_gpt":0.20966370907885298,"score_spread":0.20098571487934092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2373749322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996482,0.00003391359,0.000026879183,0.000009031579,5.491118e-7,0.000001483128,0.000095709016,0.0000013830365,0.00018275296],"genre_scores_gemma":[0.9996191,0.000023848985,0.000053615207,0.0000032951093,8.3365546e-7,0.0000018382912,0.000097470154,5.197753e-7,0.00019937496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998838,0.000012787479,0.000011078447,0.000037124664,0.000027256498,0.00002792174],"domain_scores_gemma":[0.9998293,0.00001767333,0.000053348325,0.0000075470225,0.000054105818,0.000037931575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018763867,0.00024044196,0.00026285584,0.0018372622,0.0008006827,0.00038553917,0.00041326115,0.0002350531,0.00040402287],"category_scores_gemma":[0.00020144103,0.00027220184,0.00020442386,0.0019341349,0.0004577178,0.00020684667,0.00039035783,0.0001562031,0.00004883384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012664731,0.000029796965,0.97745615,0.00005435834,0.00008331024,0.00023187858,0.0013181524,0.000645396,0.013975297,0.00015361316,0.00011168519,0.0058138017],"study_design_scores_gemma":[0.0000030938634,0.000015056538,0.9987025,0.0000018852334,0.000011654546,0.000032356795,0.00038882665,0.00037798204,0.00030757766,0.000018845692,0.00013746085,0.0000027442857],"about_ca_topic_score_codex":0.21686175,"about_ca_topic_score_gemma":0.37693515,"teacher_disagreement_score":0.21686175,"about_ca_system_score_codex":0.001826815,"about_ca_system_score_gemma":0.0019467347,"threshold_uncertainty_score":0.43119895},"labels":[],"label_agreement":null},{"id":"W2400400298","doi":"10.1002/2015tc003950","title":"Seamount, ridge, and transform subduction in southern Central America","year":2016,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Subduction; Seamount; Seismology; Seafloor spreading; Ridge; Lithosphere; Bathymetry; Plate tectonics; Deformation (meteorology); Tectonics; Geophysics; Paleontology","score_opus":0.009807384151469416,"score_gpt":0.19555626705433532,"score_spread":0.1857488829028659,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2400400298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992792,0.00021220304,0.000026511258,0.000018967929,0.0000011197425,0.0000024267974,0.000044102853,0.0000038619714,0.0004116968],"genre_scores_gemma":[0.9994867,0.00017889761,0.000070132584,0.000014399106,0.000002250915,0.0000032106448,0.00010256955,0.0000013112929,0.00014060769],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999145,0.000008238892,0.0000075295998,0.000024442454,0.000019447863,0.00002584902],"domain_scores_gemma":[0.9998005,0.000022034048,0.00008356417,0.000011062702,0.00004443472,0.00003836252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021754838,0.00022074248,0.00020259192,0.0014395673,0.000602626,0.00077570404,0.0003294192,0.0002757961,0.0006157996],"category_scores_gemma":[0.0004211953,0.00017142716,0.00020220711,0.0017984546,0.00056576106,0.0003685359,0.00066272746,0.0001395147,0.000050796447],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016298113,0.00004357043,0.9652605,0.00008675259,0.000082480925,0.0006284616,0.0026145165,0.0022942252,0.010940848,0.00029137943,0.00020918694,0.01738512],"study_design_scores_gemma":[0.0000036084873,0.000015064257,0.9980117,0.000011385367,0.0000102999775,0.000051286388,0.0008635386,0.0004884384,0.00018206723,0.00007323408,0.00028549816,0.0000038394496],"about_ca_topic_score_codex":0.14664651,"about_ca_topic_score_gemma":0.25439304,"teacher_disagreement_score":0.14664651,"about_ca_system_score_codex":0.001236432,"about_ca_system_score_gemma":0.0008694316,"threshold_uncertainty_score":0.29158586},"labels":[],"label_agreement":null},{"id":"W2401913264","doi":"10.1144/sp441.4","title":"Towards real-time earthquake impact alerting in Indonesia","year":2016,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; History; Geology","score_opus":0.022553710540884054,"score_gpt":0.25153534109953185,"score_spread":0.2289816305586478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2401913264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.668155,0.0008657888,0.27751297,0.0030166737,0.00035473274,0.00040231255,0.004434775,0.01267358,0.032584168],"genre_scores_gemma":[0.9303045,0.00020914947,0.066102855,0.00012012368,0.000030745014,0.000049516962,0.00093789544,0.00007411624,0.0021711371],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996069,0.0001052048,0.000039967435,0.000078513476,0.00013552864,0.000034046676],"domain_scores_gemma":[0.99929917,0.00010502709,0.0001185663,0.00007774121,0.00031654575,0.00008305205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008291103,0.00037618002,0.00027124665,0.0008205871,0.00016590253,0.0010395611,0.0006185598,0.00035124584,0.0015039908],"category_scores_gemma":[0.0019439379,0.0001854654,0.000121138306,0.0005005961,0.00017354976,0.00079822855,0.00080725085,0.0004481556,0.0010283152],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091803167,0.00046210096,0.1423468,0.00041436643,0.000090758345,0.0007293225,0.001258247,0.06517607,0.07012993,0.0021530718,0.020877495,0.69544387],"study_design_scores_gemma":[0.00008280246,0.00043169322,0.15690868,0.00023087116,0.000115463496,0.0005040408,0.0029396545,0.75974256,0.042548265,0.004032913,0.03237316,0.00008986665],"about_ca_topic_score_codex":0.006931735,"about_ca_topic_score_gemma":0.006354351,"teacher_disagreement_score":0.006931735,"about_ca_system_score_codex":0.00043386593,"about_ca_system_score_gemma":0.00054617785,"threshold_uncertainty_score":0.01378274},"labels":[],"label_agreement":null},{"id":"W2415257091","doi":"","title":"Regional Seismic Images Beneath the McArthur River Ore Bodies, Saskatchewan","year":2002,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Unconformity; Crust; Tectonics; Basement; Inversion (geology); Metallogeny; Paleontology; Hydrothermal circulation","score_opus":0.024671950045090277,"score_gpt":0.19901291903398827,"score_spread":0.174340968988898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2415257091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96637404,0.00013632058,0.0005943125,0.00025778622,0.000013203606,0.00010158454,0.01251648,0.00015497286,0.019851325],"genre_scores_gemma":[0.9638088,0.0005277401,0.0023791683,0.00012441259,0.0000055845444,0.0000872276,0.00922556,0.000027918568,0.023813624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999491,0.0000034409766,0.0000031756495,0.000011962292,0.000013334635,0.000018939527],"domain_scores_gemma":[0.99990773,0.0000071497348,0.00001228719,0.000007841328,0.000040182087,0.000024871062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000049117378,0.00031733417,0.00010154952,0.0014644057,0.0005694824,0.00039580432,0.00034041976,0.00022923313,0.007694616],"category_scores_gemma":[0.00013874615,0.00020705919,0.00011476975,0.002466523,0.00026641513,0.00018582844,0.00054271077,0.00021878355,0.000911742],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058613013,0.000258408,0.5856226,0.000329053,0.00022919325,0.002666742,0.0061301906,0.010859371,0.1589118,0.003127684,0.02733632,0.20394255],"study_design_scores_gemma":[0.000024838217,0.000021977065,0.9813763,0.000045658206,0.000020849,0.0001643494,0.004277656,0.0025167507,0.0020403138,0.00019126656,0.009289197,0.00003081227],"about_ca_topic_score_codex":0.8023299,"about_ca_topic_score_gemma":0.9708575,"teacher_disagreement_score":0.1976701,"about_ca_system_score_codex":0.0025367397,"about_ca_system_score_gemma":0.00396655,"threshold_uncertainty_score":0.39766842},"labels":[],"label_agreement":null},{"id":"W2426019861","doi":"10.1002/2016jb012884","title":"Modeling 3‐D crustal velocities in the United States and Canada","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Geology; Post-glacial rebound; Glacier; Geodetic datum; Geodesy; Residual; Glacial period; Longitude; Reference frame; Ice caps; Tectonics; Field (mathematics); Ice sheet; Latitude; Geophysics; Seismology; Geomorphology; Frame (networking)","score_opus":0.045821759876559696,"score_gpt":0.2947027526782399,"score_spread":0.24888099280168022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2426019861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95214504,0.0004202791,0.015935324,0.0005072537,0.000040636583,0.00010195879,0.0077093956,0.00049497234,0.022645142],"genre_scores_gemma":[0.98311156,0.00034685974,0.009917575,0.00005587951,0.0000032273276,0.000045386416,0.0029899683,0.000045312114,0.0034841895],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998783,0.00000961738,0.000005465434,0.00002815835,0.000046213416,0.000032133597],"domain_scores_gemma":[0.9996809,0.000037853744,0.00002696363,0.0000137547695,0.00019725933,0.00004335643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023366483,0.0004421051,0.00021804219,0.0010821945,0.0015355818,0.0014166867,0.0011634356,0.0004938377,0.0012576215],"category_scores_gemma":[0.0009995741,0.0002785279,0.00056575675,0.0016043993,0.0005207902,0.0004448964,0.0006474439,0.0004708451,0.00018165004],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004836297,0.000035990113,0.052295227,0.000023120778,0.00007209458,0.000115597264,0.00017362692,0.9276447,0.0006045738,0.004353191,0.0025078251,0.012125646],"study_design_scores_gemma":[0.00001636696,0.000009124661,0.018011658,0.000020688392,0.000023727956,0.000019893385,0.0001711828,0.9745224,0.00045038507,0.0007695395,0.0059554735,0.000029441735],"about_ca_topic_score_codex":0.990812,"about_ca_topic_score_gemma":0.9839363,"teacher_disagreement_score":0.021974986,"about_ca_system_score_codex":0.021974986,"about_ca_system_score_gemma":0.015447808,"threshold_uncertainty_score":0.15944046},"labels":[],"label_agreement":null},{"id":"W2433124349","doi":"10.1007/s12665-016-5663-9","title":"The North Tabriz Fault, a barrier to groundwater flow in an alluvial aquifer northwest of Tabriz, Iran","year":2016,"lang":"en","type":"article","venue":"Environmental Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Vlaamse Instelling voor Technologisch Onderzoek; Università degli Studi di Parma; McMaster University; University of California","keywords":"Geology; Aquifer; Hydrogeology; Groundwater; Groundwater flow; Alluvium; Fault (geology); Bedrock; Tectonics; Geomorphology; Geochemistry; Petrology; Geotechnical engineering; Seismology","score_opus":0.014119485655845107,"score_gpt":0.20249389193708017,"score_spread":0.18837440628123506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2433124349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99861336,0.00005355922,0.00013049436,0.00009768059,0.0000061125406,0.0000116998535,0.00007641387,0.000009153696,0.0010015541],"genre_scores_gemma":[0.9991947,0.000037716633,0.00021363383,0.000013641807,0.0000034471434,0.0000042328106,0.00008720933,9.912494e-7,0.00044440245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998609,0.000018055745,0.000013280627,0.000028093675,0.00003132794,0.000048406713],"domain_scores_gemma":[0.99983156,0.000024191166,0.00006804447,0.000010363097,0.000039183393,0.00002660394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013617534,0.00024136185,0.00023165814,0.00079293683,0.0013878437,0.0007024415,0.000470572,0.00053172454,0.0011988671],"category_scores_gemma":[0.0004232383,0.00020981107,0.00014314613,0.0014497718,0.0010179902,0.00038108806,0.00048518192,0.00016202341,0.00014199114],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051890634,0.00022386502,0.9294727,0.00021581554,0.00006699082,0.007465776,0.0076323226,0.003816449,0.011803847,0.0023584538,0.00212788,0.034296982],"study_design_scores_gemma":[0.000037645583,0.00008213867,0.9869529,0.000028844634,0.000035129247,0.00112919,0.006584327,0.0022587643,0.0005291084,0.00046895182,0.0018782348,0.0000147072],"about_ca_topic_score_codex":0.08407107,"about_ca_topic_score_gemma":0.13331632,"teacher_disagreement_score":0.08407107,"about_ca_system_score_codex":0.0012234102,"about_ca_system_score_gemma":0.003282289,"threshold_uncertainty_score":0.16716343},"labels":[],"label_agreement":null},{"id":"W2436856893","doi":"10.1103/physreve.94.022314","title":"Self-similar aftershock rates","year":2016,"lang":"en","type":"article","venue":"Physical review. E","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Università degli Studi di Padova; Alexander von Humboldt-Stiftung","keywords":"Aftershock; Foreshock; Seismology; Induced seismicity; Geology; Seismic hazard; Event (particle physics); Exponent; Hazard; Power law; Econometrics; Statistics; Mathematics; Physics","score_opus":0.017709471069163256,"score_gpt":0.27724347778308356,"score_spread":0.2595340067139203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2436856893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.77275836,0.0010863991,0.21164079,0.00046212444,0.0000718439,0.00009638819,0.0003509897,0.000443905,0.0130891],"genre_scores_gemma":[0.9938446,0.00030964732,0.0036624784,0.000060571412,0.000023088001,0.000029847195,0.00013906634,0.000019619403,0.0019111873],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998018,0.00003026102,0.000016883401,0.00007712506,0.00004907911,0.000024797098],"domain_scores_gemma":[0.9983929,0.0004942855,0.0005014889,0.00031270206,0.00021933127,0.0000791737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071593246,0.00017748923,0.0002850395,0.00068880594,0.0002018573,0.0006190697,0.00067006564,0.00067283807,0.0016482885],"category_scores_gemma":[0.0037913315,0.00017621844,0.00047837888,0.00028820417,0.00058875605,0.0013166361,0.00044781886,0.00035905192,0.0003451635],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013858323,0.00013784194,0.12971975,0.0006184039,0.00041552135,0.0012266045,0.0017519114,0.35353377,0.033822857,0.37808752,0.0032836043,0.09726367],"study_design_scores_gemma":[0.00002951887,0.00019224873,0.09991749,0.000073789124,0.00013483793,0.001993113,0.00039620383,0.62059397,0.005432394,0.2646114,0.0065245917,0.00010054487],"about_ca_topic_score_codex":0.00067632995,"about_ca_topic_score_gemma":0.0004935003,"teacher_disagreement_score":0.0016482885,"about_ca_system_score_codex":0.00039940877,"about_ca_system_score_gemma":0.00017483499,"threshold_uncertainty_score":0.0055140257},"labels":[],"label_agreement":null},{"id":"W2436874198","doi":"10.1007/s10950-012-9294-7","title":"Studies on the June 23, 2010 north Ottawa M W 5.2 earthquake and vicinity seismicity","year":2012,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Seismology; Geology; Induced seismicity; Focal mechanism; Magnitude (astronomy); Thrust fault; Structural geology; Graben; Seismic moment; Seismic zone; Fault (geology); Tectonics","score_opus":0.04326194276877374,"score_gpt":0.25437974235468713,"score_spread":0.2111177995859134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2436874198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9849775,0.00025415875,0.000024187771,0.00025154458,0.00001884209,0.000040452538,0.002999943,0.0000043760006,0.01142901],"genre_scores_gemma":[0.9825723,0.0006940994,0.000096670236,0.00021372073,0.000020603471,0.000027117723,0.002816149,0.0000058337487,0.013553444],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997073,0.000026531392,0.000018459577,0.000034610388,0.00008722186,0.00012586592],"domain_scores_gemma":[0.99882215,0.00010698865,0.00026127454,0.00005790874,0.0005045284,0.00024725846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022219232,0.00023536776,0.00021316114,0.0017386449,0.0026510493,0.00069703924,0.00047140685,0.0004764403,0.0027062641],"category_scores_gemma":[0.0012065817,0.00024672094,0.00023791617,0.0026680327,0.0006020422,0.00045736344,0.0007965151,0.0005735986,0.0005788534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033005065,0.00014158947,0.95622414,0.00014025226,0.0000746213,0.001025656,0.017467467,0.00026322898,0.00285514,0.00052726606,0.008939577,0.012010968],"study_design_scores_gemma":[0.0000017938556,0.00002791694,0.99003243,0.00001306984,0.000013929606,0.000055061777,0.005952519,0.000015261985,0.000116325464,0.0000068861523,0.0037582065,0.0000066046],"about_ca_topic_score_codex":0.9477957,"about_ca_topic_score_gemma":0.9926442,"teacher_disagreement_score":0.05220431,"about_ca_system_score_codex":0.0073427707,"about_ca_system_score_gemma":0.0075209206,"threshold_uncertainty_score":0.10502344},"labels":[],"label_agreement":null},{"id":"W2463113218","doi":"10.1002/2016gl069750","title":"Very low frequency earthquakes spatiotemporally asynchronous with strong tremor during the 2014 episodic tremor and slip event in Cascadia","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Episodic tremor and slip; Slip (aerodynamics); Moment tensor; Slow earthquake; Asynchronous communication; Inversion (geology); Foreshock; Aftershock; Subduction; Interplate earthquake; Computer science; Deformation (meteorology); Physics; Tectonics","score_opus":0.015822641693187405,"score_gpt":0.2450076607388373,"score_spread":0.22918501904564992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2463113218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989172,0.000022483962,0.00012825809,0.00004478849,0.0000028501527,0.000002607838,0.0001876871,0.000014400621,0.0006797285],"genre_scores_gemma":[0.9996456,0.000012322066,0.00004848443,0.000003811196,0.0000024793399,0.000002041442,0.00016019872,0.0000020546963,0.00012301924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998443,0.000020056508,0.00001770943,0.00004393329,0.000036832967,0.000037118312],"domain_scores_gemma":[0.9992842,0.00008599329,0.00019353474,0.000059809212,0.0002003567,0.00017612817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002785186,0.00018922584,0.0002510338,0.0012187957,0.0005636651,0.00047976803,0.00028671874,0.00028078302,0.0014188307],"category_scores_gemma":[0.0017583735,0.00018040415,0.00016516022,0.0010868288,0.0005228235,0.00024839866,0.0006304531,0.00021253424,0.00022953779],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011755315,0.000028495408,0.9845353,0.00003506366,0.00007055896,0.00035963068,0.0008723866,0.0012934651,0.0062235454,0.00010170691,0.00046948492,0.0058927867],"study_design_scores_gemma":[0.0000025326779,0.000007916071,0.9989963,0.0000032500259,0.000008080119,0.000025780791,0.00027930248,0.00045099753,0.00008620825,0.000022819702,0.00011358867,0.0000032172452],"about_ca_topic_score_codex":0.06400572,"about_ca_topic_score_gemma":0.1144733,"teacher_disagreement_score":0.06400572,"about_ca_system_score_codex":0.00061074074,"about_ca_system_score_gemma":0.0005166149,"threshold_uncertainty_score":0.12726635},"labels":[],"label_agreement":null},{"id":"W2468955254","doi":"10.1002/2016gl069800","title":"Stress drop estimates and hypocenter relocations of induced seismicity near Crooked Lake, Alberta","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; McGill University","funders":"","keywords":"Hypocenter; Geology; Seismology; Lineation; Induced seismicity; Fault plane; Tectonics; Fault (geology); Focal mechanism; Magnitude (astronomy); Drop (telecommunication)","score_opus":0.039138615529297455,"score_gpt":0.2834721154750596,"score_spread":0.24433349994576217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2468955254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972536,0.000032444383,0.0003628628,0.000011514799,0.0000014667007,0.000010539038,0.0010093128,0.00003564814,0.001282684],"genre_scores_gemma":[0.9975199,0.000037881044,0.00047225284,0.0000033564281,0.0000010984306,0.000005324132,0.0013967936,0.000005546109,0.0005578036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986994,0.000006169934,0.000007035938,0.000024885923,0.000058664,0.000033274348],"domain_scores_gemma":[0.9996861,0.000024479019,0.000076313794,0.000012383189,0.00015699845,0.000043778964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012778428,0.00021256323,0.0001290599,0.0018808981,0.00037724175,0.0005345805,0.0004434834,0.00012954434,0.0013137759],"category_scores_gemma":[0.0008224541,0.000112289556,0.00010126368,0.0017038494,0.00020595321,0.00015206392,0.00030010293,0.00015138625,0.00017863374],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013944179,0.000037050508,0.9594697,0.000033205906,0.000043404554,0.00017760482,0.0004397451,0.0069929557,0.010716965,0.00013429706,0.00060114573,0.021214351],"study_design_scores_gemma":[0.0000027451515,0.000006991523,0.99654925,0.0000026976275,0.000004245089,0.000014272626,0.00021087851,0.0024263093,0.00053568895,0.000011222162,0.00023262743,0.0000030979636],"about_ca_topic_score_codex":0.7420767,"about_ca_topic_score_gemma":0.8877424,"teacher_disagreement_score":0.2579233,"about_ca_system_score_codex":0.0022996243,"about_ca_system_score_gemma":0.001403864,"threshold_uncertainty_score":0.51888454},"labels":[],"label_agreement":null},{"id":"W2469158815","doi":"10.1002/2016gl069507","title":"Pattern of dynamic displacements in a strike‐slip earthquake","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; Strong","keywords":"Geology; Seismology; Slip (aerodynamics); Attenuation; Strike-slip tectonics; Geodesy; Directivity; Fault (geology); Trough (economics); Seismic gap","score_opus":0.03077124801852221,"score_gpt":0.29631266527972133,"score_spread":0.2655414172611991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2469158815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99902177,0.000022695596,0.00014196523,0.000009380684,0.0000012724502,0.000002065958,0.00025237154,0.00000737417,0.00054100517],"genre_scores_gemma":[0.9994542,0.00001192003,0.00006477282,0.0000020528655,0.0000014280885,0.0000014880079,0.00025742687,8.705354e-7,0.00020593934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993074,0.0000060229268,0.00000670785,0.00002449608,0.000018696675,0.0000134045795],"domain_scores_gemma":[0.9997708,0.000032648197,0.00009331835,0.000018723284,0.00005244499,0.000032093365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000057659458,0.0001422626,0.00012367695,0.0009773578,0.0001255235,0.00021294157,0.00012920484,0.00020541897,0.0010644717],"category_scores_gemma":[0.00042324193,0.000108096145,0.00005885906,0.0007766152,0.00016831988,0.0001293535,0.00019777702,0.00008307384,0.00025376608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036018732,0.000065357795,0.90343565,0.000054154123,0.00006464066,0.0007067628,0.00061324035,0.00231851,0.06527767,0.00023915825,0.00047015038,0.026394526],"study_design_scores_gemma":[0.0000024559647,0.000039736347,0.9977951,0.0000027793867,0.000004843136,0.00023284851,0.00012416692,0.00090858754,0.00063843007,0.000018345667,0.0002295192,0.0000030562003],"about_ca_topic_score_codex":0.0025004619,"about_ca_topic_score_gemma":0.0037825722,"teacher_disagreement_score":0.0025004619,"about_ca_system_score_codex":0.00017236944,"about_ca_system_score_gemma":0.000073593095,"threshold_uncertainty_score":0.004971862},"labels":[],"label_agreement":null},{"id":"W2470873809","doi":"10.2174/1874834101609010055","title":"Induced Microseismicity: Short Overview, State of the Art and Feedback on Source Rock Production","year":2016,"lang":"en","type":"article","venue":"The Open Petroleum Engineering Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Hydraulic fracturing; Geology; Fracture (geology); Seismology; Microseism; Production (economics); Mining engineering; State (computer science); Oil shale; Interpretation (philosophy); Petroleum engineering; Computer science; Geotechnical engineering; Paleontology","score_opus":0.02034384924646099,"score_gpt":0.21398238267002245,"score_spread":0.19363853342356147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2470873809","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18445772,0.5772545,0.14282872,0.0103708375,0.0018227053,0.00017358596,0.0039146002,0.0019833792,0.07719396],"genre_scores_gemma":[0.56994945,0.3822408,0.032905165,0.0010017706,0.0023654078,0.000114636285,0.0020151509,0.0005882263,0.008819458],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99887234,0.00019639429,0.00009284957,0.00032814502,0.00041873197,0.000091402486],"domain_scores_gemma":[0.9892791,0.007089226,0.0010685741,0.0006330364,0.0017011836,0.00022886854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023669333,0.0007488322,0.00060708745,0.004164057,0.0004949385,0.0029339711,0.0011290815,0.0011146474,0.004278219],"category_scores_gemma":[0.008046555,0.000615556,0.00038861734,0.0049323468,0.0014105284,0.0036780057,0.0015356964,0.0011355241,0.0011293251],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028069623,0.00012508481,0.0352598,0.0062255226,0.000111838985,0.00046690952,0.0026395402,0.0074806404,0.008443315,0.023681352,0.009884979,0.9054003],"study_design_scores_gemma":[0.00002361236,0.0009180805,0.13087958,0.009665864,0.0004238153,0.0027430472,0.0074613728,0.016534802,0.03710406,0.040927354,0.7529535,0.00036481908],"about_ca_topic_score_codex":0.002856136,"about_ca_topic_score_gemma":0.0033984757,"teacher_disagreement_score":0.004278219,"about_ca_system_score_codex":0.0013975644,"about_ca_system_score_gemma":0.0010566973,"threshold_uncertainty_score":0.014312029},"labels":[],"label_agreement":null},{"id":"W2475115223","doi":"10.1016/j.epsl.2016.06.046","title":"Shallow earthquake inhibits unrest near Chiles–Cerro Negro volcanoes, Ecuador–Colombian border","year":2016,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Geology; Seismology; Volcano; Induced seismicity; Unrest; Earthquake swarm; Tectonics; Fault (geology); Magma","score_opus":0.009333443951013995,"score_gpt":0.20130307912658277,"score_spread":0.19196963517556878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2475115223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99228597,0.00018534978,0.000035602807,0.00021156491,0.000007850866,0.000006573502,0.00018020727,0.0000060213506,0.0070809303],"genre_scores_gemma":[0.9989096,0.00007410334,0.000020917001,0.000016507638,0.0000053352014,0.0000035875257,0.00011566652,0.0000017811814,0.00085253676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988997,0.000016616457,0.0000063149005,0.000013625546,0.000013964212,0.000059459308],"domain_scores_gemma":[0.9992888,0.00013407967,0.00022564655,0.000035954185,0.0001476336,0.00016794154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015158833,0.00011060844,0.00016690229,0.0006689522,0.0007528132,0.0012231324,0.00024327134,0.00029542233,0.0058425725],"category_scores_gemma":[0.0017043338,0.00008038533,0.00007674958,0.0005540229,0.0004022848,0.00047278186,0.0011577096,0.0002848089,0.00038201505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005839529,0.00012676661,0.95855445,0.00013736208,0.000058709687,0.0011421745,0.004907271,0.0010476055,0.0037224775,0.0013292652,0.0034197413,0.024970224],"study_design_scores_gemma":[0.000014901041,0.000017444143,0.9909452,0.000024277899,0.000011536208,0.00004262802,0.006151111,0.0002161236,0.00013612649,0.00010828654,0.0023281772,0.000004073419],"about_ca_topic_score_codex":0.08085162,"about_ca_topic_score_gemma":0.13933118,"teacher_disagreement_score":0.08085162,"about_ca_system_score_codex":0.001114211,"about_ca_system_score_gemma":0.00065886753,"threshold_uncertainty_score":0.16076201},"labels":[],"label_agreement":null},{"id":"W2476463576","doi":"10.1002/2016jb013102","title":"Fluid‐assisted deformation of the subduction interface: Coupled and decoupled regimes from 2‐D hydromechanical modeling","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"European Commission","keywords":"Subduction; Geology; Slab; Cohesion (chemistry); Shear (geology); Mechanics; Deformation (meteorology); Geophysics; Petrology; Tectonics; Seismology; Physics","score_opus":0.04695211259650907,"score_gpt":0.30594772046114466,"score_spread":0.2589956078646356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2476463576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87737435,0.00045126822,0.10715157,0.0004841475,0.000049307557,0.00013226974,0.00053113984,0.00033230986,0.013493771],"genre_scores_gemma":[0.99288964,0.00015026121,0.0057355496,0.000041077798,0.000015590407,0.000076630655,0.0001173049,0.00002944078,0.00094437046],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988604,0.000033107404,0.000008005042,0.000023870762,0.000029599558,0.000019402423],"domain_scores_gemma":[0.99976164,0.00010809813,0.000046039248,0.000025804702,0.00003344415,0.000025023919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021494982,0.00065094646,0.0005856117,0.0005891524,0.00036942985,0.0009706066,0.0009786573,0.0013945365,0.0012441949],"category_scores_gemma":[0.0008517758,0.00050378195,0.0008040809,0.0004255015,0.00083455845,0.00078577903,0.0009104394,0.0006359081,0.00013884979],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017746168,0.000030426272,0.0012857795,0.000020366388,0.000015171112,0.000051454066,0.000035169694,0.99367404,0.0026058014,0.0013079502,0.000063599786,0.0008925338],"study_design_scores_gemma":[0.0000026959156,0.0000023726977,0.00020231068,0.0000010144792,0.0000010284461,0.0000019514005,0.000002351821,0.9995432,0.00007001992,0.00013758155,0.00003342409,0.000002073083],"about_ca_topic_score_codex":0.012698885,"about_ca_topic_score_gemma":0.006743389,"teacher_disagreement_score":0.012698885,"about_ca_system_score_codex":0.0007657913,"about_ca_system_score_gemma":0.0006532659,"threshold_uncertainty_score":0.025249958},"labels":[],"label_agreement":null},{"id":"W2477550485","doi":"10.1002/2016jb012857","title":"Spatiotemporal evolution of slow slip events in a nonplanar fault model for northern Cascadia subduction zone","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Geology; Slip (aerodynamics); Subduction; Episodic tremor and slip; Seismology; Fault (geology); Tectonics; Physics","score_opus":0.046797554330904156,"score_gpt":0.3135177467491904,"score_spread":0.26672019241828626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2477550485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99617505,0.00007505866,0.0018144192,0.00011643243,0.000010350042,0.00001006837,0.000306184,0.00006713313,0.0014252483],"genre_scores_gemma":[0.9989686,0.000036848818,0.00025326412,0.000007123394,0.000002541497,0.000010023834,0.00017919802,0.000008056121,0.0005342946],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999232,0.000017047547,0.0000048871025,0.00002304541,0.000008918482,0.000022830072],"domain_scores_gemma":[0.99976975,0.00006393541,0.00004343039,0.00002347201,0.000036007597,0.000063508385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019200219,0.00062256836,0.00048525597,0.00066077954,0.0005043667,0.0007533335,0.0012220482,0.0011656166,0.0022839308],"category_scores_gemma":[0.0006837959,0.00030218615,0.0007222931,0.00041863305,0.00067870674,0.00027884703,0.0005220469,0.00050902937,0.00014068294],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044711127,0.000034549095,0.011367041,0.000011926793,0.00002771545,0.00015888477,0.000029038092,0.9864807,0.00085919985,0.00043369064,0.00013314789,0.00041934356],"study_design_scores_gemma":[0.000012261436,0.000015820393,0.003599986,0.0000022628096,0.000009029399,0.000009617459,0.000022025355,0.9960634,0.00007013368,0.000112121845,0.000078028,0.0000053951167],"about_ca_topic_score_codex":0.1343171,"about_ca_topic_score_gemma":0.05793457,"teacher_disagreement_score":0.1343171,"about_ca_system_score_codex":0.0016766199,"about_ca_system_score_gemma":0.0008120411,"threshold_uncertainty_score":0.2670706},"labels":[],"label_agreement":null},{"id":"W2490421907","doi":"","title":"Marine and Petroleum Geology","year":2013,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geothermal gradient; Hydraulic fracturing; Induced seismicity; Borehole; Fault (geology); Poromechanics; Pore water pressure; Permeability (electromagnetism); Fluid dynamics; Fluid pressure; Sedimentary rock; Effective stress; Geotechnical engineering; Petroleum engineering; Seismology; Geochemistry; Geophysics; Porosity","score_opus":0.008346848133973033,"score_gpt":0.17853638421020943,"score_spread":0.17018953607623638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2490421907","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02003091,0.088977545,0.0039786114,0.0049557486,0.0040131425,0.00014884227,0.08091913,0.0008517344,0.7961243],"genre_scores_gemma":[0.17630577,0.18895037,0.011101338,0.001605723,0.0032078817,0.00014570131,0.06598489,0.00060053036,0.55209774],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99970645,0.00003722038,0.000054914228,0.00004375022,0.00013227774,0.000025343152],"domain_scores_gemma":[0.9994092,0.00012318313,0.00008227989,0.00011422342,0.00022570838,0.000045392495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028505962,0.00055767724,0.00037059444,0.0088866465,0.0006463844,0.0018265131,0.00030436393,0.0002920804,0.04374333],"category_scores_gemma":[0.0020688924,0.00013383463,0.00020041168,0.012618169,0.00057877094,0.0014378793,0.0009873445,0.00042415154,0.013236025],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007328001,0.000026034597,0.011639413,0.0021746967,0.000044200224,0.0007487939,0.0008479506,0.0011003864,0.0010688195,0.06841323,0.35233358,0.56152964],"study_design_scores_gemma":[9.622479e-7,0.000010254193,0.008643709,0.00016288146,0.0000034108664,0.000174406,0.0001413721,0.00006564408,0.00010564649,0.0018445926,0.9888425,0.0000046644054],"about_ca_topic_score_codex":0.01684932,"about_ca_topic_score_gemma":0.021779194,"teacher_disagreement_score":0.04374333,"about_ca_system_score_codex":0.0011447481,"about_ca_system_score_gemma":0.0013518906,"threshold_uncertainty_score":0.14633608},"labels":[],"label_agreement":null},{"id":"W2491285181","doi":"10.2973/odp.proc.sr.169.115.2000","title":"Permeability, electrical, and thermal properties of sulfide, sedimentary, and basaltic units from the Bent Hill area of Middle Valley, Juan de Fuca Ridge","year":2000,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ridge; Geology; Basalt; Sedimentary rock; Sulfide; Bent molecular geometry; Permeability (electromagnetism); Geochemistry; Geomorphology; Petrology; Mineralogy; Paleontology; Materials science; Chemistry; Composite material; Metallurgy","score_opus":0.044713036292227136,"score_gpt":0.18719011938311064,"score_spread":0.1424770830908835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2491285181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996798,0.000034398447,0.000049112074,0.0000018005835,2.5056016e-7,0.0000012407029,0.00008900174,0.0000016454837,0.0001427662],"genre_scores_gemma":[0.9994727,0.000028927687,0.00014835112,0.0000018316682,7.882348e-7,0.000002344639,0.00022931758,0.0000012859169,0.00011439551],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999212,0.000004493287,0.000006817409,0.00002604607,0.000023969375,0.000017440336],"domain_scores_gemma":[0.9998859,0.000020484777,0.0000361697,0.000006952699,0.000026911714,0.000023554325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011296831,0.00020387824,0.00014462347,0.0008772417,0.0003757426,0.00036917356,0.0001997396,0.00017358254,0.0003140503],"category_scores_gemma":[0.00021190335,0.0001591515,0.00013074985,0.0006226823,0.00028945794,0.0001826062,0.0002414758,0.00012867284,0.000059378573],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005075598,0.000073096926,0.5515595,0.00008399744,0.000085302796,0.00043730065,0.001280488,0.0009510894,0.43477675,0.00010229933,0.00005888012,0.010083684],"study_design_scores_gemma":[0.0000045022603,0.000035825295,0.9904304,0.0000025580448,0.000011293601,0.00015555552,0.00023460669,0.00055990403,0.008384168,0.000015490112,0.00016160937,0.0000039611164],"about_ca_topic_score_codex":0.013862123,"about_ca_topic_score_gemma":0.021734826,"teacher_disagreement_score":0.013862123,"about_ca_system_score_codex":0.00031033732,"about_ca_system_score_gemma":0.0001487759,"threshold_uncertainty_score":0.027562916},"labels":[],"label_agreement":null},{"id":"W2491653386","doi":"10.1093/gji/ggw305","title":"High-resolution reconstructions of Pacific–North America plate motion: 20 Ma to present","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Seismology; Geodesy; Motion (physics); Artificial intelligence","score_opus":0.01415188830054578,"score_gpt":0.21873823107305956,"score_spread":0.20458634277251378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2491653386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9275377,0.0035760798,0.008383832,0.0004337071,0.00016042773,0.000043608463,0.0058271047,0.0012997887,0.052737776],"genre_scores_gemma":[0.9832965,0.001029661,0.0057657408,0.00006895951,0.00008373349,0.000034480658,0.0064521586,0.00024908056,0.003019658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987876,0.000009450057,0.0000072210255,0.000055345277,0.000029634535,0.000019479301],"domain_scores_gemma":[0.99974924,0.000013825096,0.000056808825,0.000043761524,0.000094742114,0.00004161704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031203695,0.0004712397,0.0002890655,0.0017755724,0.00072380697,0.0011777427,0.00060031493,0.00064830185,0.0041532726],"category_scores_gemma":[0.00089908484,0.0005991631,0.0004178195,0.001310612,0.00047126936,0.00062944955,0.00088793266,0.000655832,0.0012339266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046533308,0.00019307312,0.670422,0.0005221403,0.001353452,0.00136225,0.0052243043,0.057103,0.09544513,0.007625569,0.01587835,0.14440535],"study_design_scores_gemma":[0.000066362285,0.000051544488,0.88085455,0.0001391356,0.00031860094,0.000692237,0.0005471546,0.02631818,0.0029635662,0.0015449255,0.086433366,0.00007025195],"about_ca_topic_score_codex":0.039805893,"about_ca_topic_score_gemma":0.08910333,"teacher_disagreement_score":0.039805893,"about_ca_system_score_codex":0.0013199402,"about_ca_system_score_gemma":0.0010855963,"threshold_uncertainty_score":0.07914841},"labels":[],"label_agreement":null},{"id":"W2496773083","doi":"10.1201/9780415601658-136","title":"Experimental study of the temperature-pressure effect on gas transport in peridotite sample from Sudbury Basin, Canada","year":2010,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Peridotite; Geology; Sample (material); Structural basin; Geochemistry; Geomorphology; Basalt; Thermodynamics; Physics","score_opus":0.00846660480286689,"score_gpt":0.19147182639659638,"score_spread":0.18300522159372948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2496773083","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99716514,0.00007013971,0.00020755884,0.000017120174,0.0000031582879,0.000016876256,0.0008496511,0.000009245353,0.001660991],"genre_scores_gemma":[0.99497473,0.00016600607,0.0007119934,0.000023207424,0.0000027136768,0.000022205413,0.0010061382,0.000014845881,0.003078062],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99978536,0.000008318501,0.0000074810746,0.00006244907,0.00007090491,0.00006541081],"domain_scores_gemma":[0.99971145,0.00005150128,0.000016808364,0.000011921552,0.00017562888,0.000032666656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015383425,0.00022999915,0.0002244078,0.00052611565,0.0030191103,0.00052248425,0.000843856,0.00031715876,0.0011656577],"category_scores_gemma":[0.00032698616,0.0002538031,0.00014502672,0.0010127424,0.0007406591,0.00021147162,0.0003063707,0.00040769688,0.00020002948],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015756236,0.0003520828,0.20031336,0.00010063953,0.00008412318,0.00070759247,0.002640323,0.0020312488,0.7787799,0.00070355413,0.0012427046,0.011468755],"study_design_scores_gemma":[0.000043253145,0.00029670168,0.8499196,0.000013945204,0.000051109266,0.00020617768,0.0020254147,0.002337165,0.14134829,0.00007457276,0.0036527556,0.00003095201],"about_ca_topic_score_codex":0.93544817,"about_ca_topic_score_gemma":0.96280277,"teacher_disagreement_score":0.06455183,"about_ca_system_score_codex":0.0052655656,"about_ca_system_score_gemma":0.0037332894,"threshold_uncertainty_score":0.12986392},"labels":[],"label_agreement":null},{"id":"W2496989734","doi":"10.1002/2016jb013228","title":"A 2‐D tomographic model of the Juan de Fuca plate from accretion at axial seamount to subduction at the Cascadia margin from an active source ocean bottom seismometer survey","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Geology; Subduction; Seismology; Crust; Oceanic crust; Mantle (geology); Seamount; Seafloor spreading; Seismic tomography; Detachment fault; Underplating; Geophysics; Petrology; Tectonics; Paleontology","score_opus":0.04900055408168715,"score_gpt":0.3017570488467472,"score_spread":0.25275649476506007,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2496989734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993331,0.00004416412,0.0018361573,0.00013707664,0.0000068207532,0.000019773448,0.0009989776,0.0002455874,0.0033802586],"genre_scores_gemma":[0.9979511,0.000038630507,0.00088741817,0.0000095179785,0.000003000594,0.000014050156,0.00046197156,0.000016347316,0.00061799056],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999552,0.000006400367,0.0000024237886,0.000017199769,0.000008185477,0.000010592299],"domain_scores_gemma":[0.99991477,0.000016134587,0.000013682554,0.000013576374,0.000016984148,0.000024920908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011756027,0.00052339217,0.00022693428,0.0006970868,0.0005074106,0.00076261,0.00087403244,0.0009177606,0.0029797237],"category_scores_gemma":[0.00031871037,0.0004906899,0.00071436935,0.0007009118,0.00047376877,0.0002512213,0.00040962957,0.000308631,0.00028384113],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015874843,0.00007104377,0.054293375,0.000032229378,0.00009018073,0.00042160237,0.00016555452,0.93401676,0.006571562,0.00067196303,0.0004409931,0.0030658976],"study_design_scores_gemma":[0.00006640388,0.000052763564,0.06678569,0.000011730957,0.000035056186,0.00007589857,0.00014238748,0.93151236,0.00043824204,0.00032748756,0.00052628154,0.000025639192],"about_ca_topic_score_codex":0.16556399,"about_ca_topic_score_gemma":0.11299958,"teacher_disagreement_score":0.16556399,"about_ca_system_score_codex":0.0017713322,"about_ca_system_score_gemma":0.0012876991,"threshold_uncertainty_score":0.32920063},"labels":[],"label_agreement":null},{"id":"W2497840897","doi":"10.1016/b978-0-444-53042-4.00007-8","title":"Crustal seismic reflection profiles of collisional orogens","year":2012,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Reflection (computer programming); Seismology; Geophysics; Earth science; Computer science","score_opus":0.025691857453792863,"score_gpt":0.23465540420930234,"score_spread":0.2089635467555095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2497840897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95397985,0.00072132755,0.00382919,0.00004216353,0.0000049816204,0.000007491761,0.0010715519,0.00015362943,0.040189832],"genre_scores_gemma":[0.98445016,0.00053204066,0.0016546282,0.000008604949,0.0000042897345,0.0000021647645,0.0009223302,0.00009776799,0.01232802],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999778,0.000002118764,0.0000016810428,0.0000056210265,0.000007449307,0.0000053260947],"domain_scores_gemma":[0.9999589,0.000008426629,0.000008479432,0.0000066505568,0.000012337053,0.0000053307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000660943,0.00015270352,0.000096615506,0.00044384337,0.00010769458,0.00034850655,0.00021427355,0.00012244716,0.0057474477],"category_scores_gemma":[0.00028767707,0.00016304813,0.000078765144,0.000967015,0.00013082568,0.00021655831,0.00022658423,0.00014229937,0.0009336455],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006659326,0.00009299469,0.21703443,0.00016479546,0.000108969485,0.0010980462,0.004147189,0.037073106,0.17183219,0.0063195606,0.0050645685,0.55639833],"study_design_scores_gemma":[0.000017886236,0.000090621725,0.96174973,0.000035267327,0.000034208424,0.0005375895,0.0009186124,0.014633329,0.006277196,0.0016513717,0.014028014,0.00002618577],"about_ca_topic_score_codex":0.006805665,"about_ca_topic_score_gemma":0.010385085,"teacher_disagreement_score":0.006805665,"about_ca_system_score_codex":0.00017138204,"about_ca_system_score_gemma":0.000113747345,"threshold_uncertainty_score":0.019227087},"labels":[],"label_agreement":null},{"id":"W2498248233","doi":"","title":"Styles of Deformation on Either Side of a Ridge-Transform Intersection, Troodos Ophiolite, Cyprus","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Ophiolite; Geology; Ridge; Intersection (aeronautics); Deformation (meteorology); Mid-ocean ridge; Geochemistry; Seismology; Paleontology; Geography; Tectonics; Cartography; Oceanography","score_opus":0.027184735259439687,"score_gpt":0.24200667086084565,"score_spread":0.21482193560140597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2498248233","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98639965,0.00003490617,0.0002782906,0.00004031612,0.000020734622,0.000011950006,0.00071285234,0.00006247625,0.012438793],"genre_scores_gemma":[0.99737215,0.000019789904,0.0002111074,0.000003964928,0.0000050209946,0.0000021857586,0.00037690194,0.0000133009435,0.0019955433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999304,0.000006649911,0.000003834151,0.000021081558,0.000015930398,0.000022125923],"domain_scores_gemma":[0.9998561,0.000019287023,0.00003271235,0.000022021113,0.00003434174,0.0000356271],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000079138495,0.00016545466,0.000108415945,0.0010423185,0.00058911194,0.0007468228,0.00015493657,0.00024407661,0.0045389617],"category_scores_gemma":[0.0003795208,0.00010734404,0.00015791015,0.00060782384,0.00041326767,0.00014402978,0.00035858087,0.00024087864,0.0004245435],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020154682,0.00019815787,0.7869236,0.00012635034,0.00015044435,0.0047268053,0.004154609,0.032952387,0.065066695,0.0054981504,0.008419276,0.089768],"study_design_scores_gemma":[0.0000075696767,0.000044564662,0.99276954,0.000011700219,0.000009661692,0.0002396158,0.0005292475,0.0034012226,0.00065665465,0.00008287987,0.0022400839,0.0000072271696],"about_ca_topic_score_codex":0.017574562,"about_ca_topic_score_gemma":0.04780642,"teacher_disagreement_score":0.017574562,"about_ca_system_score_codex":0.0004203804,"about_ca_system_score_gemma":0.00035151065,"threshold_uncertainty_score":0.034944534},"labels":[],"label_agreement":null},{"id":"W2502015534","doi":"10.1007/s40808-016-0201-z","title":"Seismicity and recent stress regime of Diyala City, Iraq–Iran border","year":2016,"lang":"en","type":"article","venue":"Modeling Earth Systems and Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research","keywords":"Seismology; Induced seismicity; Geology; Fault (geology); Magnitude (astronomy); Focal mechanism; Active fault; Seismic gap","score_opus":0.031145615103901077,"score_gpt":0.2096615520948138,"score_spread":0.17851593699091273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2502015534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99852496,0.00004264156,0.000028079694,0.00011687349,0.0000043566915,0.0000025154886,0.0003861634,0.000003285124,0.000891105],"genre_scores_gemma":[0.99916494,0.00005122875,0.000033586064,0.0000105390955,0.0000072895746,0.000002776029,0.00041287523,0.0000010909827,0.00031575887],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988604,0.00001272021,0.000009271676,0.000024401676,0.000018276638,0.000049275208],"domain_scores_gemma":[0.99960035,0.000046431403,0.0001309781,0.000018691302,0.00013717225,0.00006647599],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021479555,0.00015114076,0.00017074755,0.0008940929,0.0004899993,0.00078695774,0.00049736776,0.0003957289,0.0018638816],"category_scores_gemma":[0.0007381461,0.00016733047,0.00023258479,0.0015316082,0.0003343025,0.00045157035,0.00050458865,0.00035887258,0.00025884563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014194992,0.00009041957,0.98573816,0.000021324586,0.0000874478,0.00034350343,0.0011944675,0.0036526767,0.0006762535,0.0007991307,0.0016610748,0.0055935644],"study_design_scores_gemma":[0.000009091407,0.000019958921,0.9948068,0.0000068494064,0.000021250458,0.00006177908,0.0021217733,0.0018013518,0.00006401301,0.000065102904,0.0010160807,0.000005832679],"about_ca_topic_score_codex":0.13649178,"about_ca_topic_score_gemma":0.17650986,"teacher_disagreement_score":0.13649178,"about_ca_system_score_codex":0.0013387499,"about_ca_system_score_gemma":0.0010507766,"threshold_uncertainty_score":0.2713946},"labels":[],"label_agreement":null},{"id":"W250312994","doi":"","title":"Surface and deep water variations and their impact on the Meridional Overturning Circulation during the mid-Brunhes as revealed at IODP Sites U1313 and U1305","year":2010,"lang":"en","type":"article","venue":"Portuguese National Funding Agency for Science, Research and Technology (RCAAP Project by FCT)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Oceanography; Circulation (fluid dynamics)","score_opus":0.04272297578927841,"score_gpt":0.3199091832621489,"score_spread":0.2771862074728705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W250312994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986965,0.000032921605,0.00003362479,0.00002270286,0.0000026566452,0.0000019296897,0.00049497007,0.0000040940486,0.00071060646],"genre_scores_gemma":[0.9991147,0.00004209987,0.00007573879,0.0000058404044,0.0000027963727,0.000003663902,0.00045267126,0.0000033961192,0.00029910373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999596,0.0000048362504,0.0000021675555,0.000009513906,0.0000067390583,0.000017116543],"domain_scores_gemma":[0.9998815,0.00002365277,0.000029154593,0.000006912715,0.000022240498,0.000036412912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010685516,0.00014643632,0.00014647402,0.00033545884,0.0002356118,0.000420229,0.00016808989,0.00023959934,0.0012099134],"category_scores_gemma":[0.00030555192,0.000119807926,0.00011401797,0.00074346154,0.00024676116,0.00023875809,0.00037501595,0.00023378494,0.00018786745],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063528446,0.000061345556,0.9568751,0.00004464751,0.000051460913,0.00047641047,0.002209147,0.0009961636,0.019892052,0.00034096924,0.0009478457,0.017469535],"study_design_scores_gemma":[0.0000030141891,0.0000075932962,0.9992465,0.0000025431398,0.0000024149344,0.000018251818,0.00022807585,0.00017835622,0.000085923486,0.000011065253,0.00021481515,0.0000014673996],"about_ca_topic_score_codex":0.08580714,"about_ca_topic_score_gemma":0.18005505,"teacher_disagreement_score":0.08580714,"about_ca_system_score_codex":0.00045731486,"about_ca_system_score_gemma":0.00028169868,"threshold_uncertainty_score":0.17061538},"labels":[],"label_agreement":null},{"id":"W2507701880","doi":"10.1002/2015jb012311","title":"The damage is done: Low fault friction recorded in the damage zone of the shallow Japan Trench décollement","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Geology; Trench; Slip (aerodynamics); Seismology; Décollement; Cataclastic rock; Fault (geology); Strike-slip tectonics; Drilling; Shear zone; Shear (geology); Petrology; Materials science; Composite material; Tectonics","score_opus":0.03637898421134305,"score_gpt":0.30821931956362264,"score_spread":0.2718403353522796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2507701880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997321,0.000017682722,0.00004892764,0.0000020382045,3.4077118e-7,0.0000010566182,0.00006811827,0.0000036911479,0.00012603517],"genre_scores_gemma":[0.9997955,0.00000855372,0.000049605023,0.0000012559989,3.4870482e-7,9.665714e-7,0.00006429317,8.9482114e-7,0.00007853128],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999323,0.0000025432307,0.0000039480965,0.000020325395,0.000017071749,0.000023910714],"domain_scores_gemma":[0.9998615,0.000009892228,0.000054633485,0.000010692602,0.000028107626,0.00003519127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000060704642,0.00016063999,0.00021236045,0.00066162273,0.0004099831,0.00026223308,0.00021118266,0.00023280754,0.00052956503],"category_scores_gemma":[0.00025932136,0.000128021,0.00011239657,0.0005251394,0.00029853938,0.0001932548,0.000289307,0.00014909416,0.00008258547],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023775658,0.000035782978,0.9164612,0.00005648694,0.000043050364,0.000774491,0.0008755426,0.0015692137,0.07187832,0.00007555791,0.00017314851,0.007819453],"study_design_scores_gemma":[0.0000010615834,0.000015227953,0.9985285,0.0000015631537,0.0000039183765,0.0000620857,0.00008585437,0.00057543867,0.0006408505,0.000004380287,0.00007884566,0.0000022665067],"about_ca_topic_score_codex":0.029660895,"about_ca_topic_score_gemma":0.07533538,"teacher_disagreement_score":0.029660895,"about_ca_system_score_codex":0.0005077989,"about_ca_system_score_gemma":0.00020883509,"threshold_uncertainty_score":0.05897647},"labels":[],"label_agreement":null},{"id":"W2508154350","doi":"10.1785/0220160074","title":"The 2015 Canada Day,<i>M</i><sub>w</sub> 3.8, Earthquake in Nova Scotia","year":2016,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Citation; Nova scotia; Geological survey; Icon; Observatory; Library science; Service (business); History; Geography; Political science; Computer science; Geology; Archaeology; Business; Paleontology; Astronomy; Physics","score_opus":0.046196446015821895,"score_gpt":0.2784181576924881,"score_spread":0.23222171167666622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2508154350","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07446404,0.031358887,0.00048629867,0.03644366,0.0115744155,0.00043728895,0.22676039,0.00089969387,0.61757535],"genre_scores_gemma":[0.18756412,0.026728375,0.0010011208,0.0038824475,0.0012342399,0.00009450805,0.07468485,0.00047375335,0.7043365],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99969363,0.000007591741,0.000014480009,0.00002681442,0.00016062421,0.00009683531],"domain_scores_gemma":[0.99915934,0.000027623722,0.00007909345,0.000028721606,0.0003649652,0.0003402648],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020494434,0.00043309553,0.00042692924,0.0017276685,0.0027218536,0.0024011482,0.00049828197,0.0010083426,0.056847155],"category_scores_gemma":[0.0014581617,0.00022072734,0.0003108173,0.0035415795,0.0006713201,0.00076713524,0.0014939365,0.0009149339,0.020043334],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009617243,0.000010800265,0.012240505,0.0004960894,0.00001503852,0.00061733153,0.0006763934,0.00015418134,0.00057097914,0.0009448338,0.9539837,0.030193834],"study_design_scores_gemma":[0.000027590479,0.000027433842,0.16954951,0.00079305505,0.00002370416,0.00018474724,0.0027539206,0.00014177752,0.00036271414,0.00028951344,0.82580614,0.00003984059],"about_ca_topic_score_codex":0.9494118,"about_ca_topic_score_gemma":0.9858766,"teacher_disagreement_score":0.056847155,"about_ca_system_score_codex":0.0109155765,"about_ca_system_score_gemma":0.022342118,"threshold_uncertainty_score":0.19017267},"labels":[],"label_agreement":null},{"id":"W2509432284","doi":"10.1785/0120160048","title":"Maximum Magnitude (<i>M</i><sub>max</sub>) in the Central and Eastern United States for the 2014 U.S. Geological Survey Hazard Model","year":2016,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Craton; Geology; Seismology; Rift; Moment magnitude scale; Magnitude (astronomy); Seismic hazard; Crust; Induced seismicity; Tectonics; Continental crust; Geological survey; Paleontology; Geometry","score_opus":0.023814556865899533,"score_gpt":0.21424853862102258,"score_spread":0.19043398175512305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2509432284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.76502573,0.00087975885,0.023790646,0.0029437505,0.00033467409,0.00019126506,0.15001741,0.0015622358,0.05525452],"genre_scores_gemma":[0.9421505,0.0003069791,0.0034076069,0.00022739942,0.000042746648,0.00018654308,0.048415996,0.00006262084,0.005199608],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998857,0.000026068996,0.0000067635015,0.000030508048,0.000026478237,0.000024515448],"domain_scores_gemma":[0.99974805,0.00007091465,0.000045994213,0.000020414149,0.00008705456,0.00002762877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003520358,0.00035298485,0.00020258923,0.0007919057,0.00018137485,0.0005758272,0.00071722554,0.00042899945,0.005362622],"category_scores_gemma":[0.0012556387,0.00016984939,0.0002670071,0.0008571988,0.00015062283,0.000556407,0.00042206267,0.00041125724,0.00077069295],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035259937,0.00016289443,0.24632989,0.00017807249,0.00021824952,0.00032168618,0.00016678599,0.46729589,0.0005460184,0.023911966,0.22176994,0.038745895],"study_design_scores_gemma":[0.00012876301,0.00014000252,0.15626772,0.00012862323,0.000085766966,0.0002523126,0.00064747006,0.7762943,0.0005662656,0.022704778,0.042717006,0.00006711784],"about_ca_topic_score_codex":0.048621003,"about_ca_topic_score_gemma":0.04532401,"teacher_disagreement_score":0.048621003,"about_ca_system_score_codex":0.0012790138,"about_ca_system_score_gemma":0.0007602112,"threshold_uncertainty_score":0.09667599},"labels":[],"label_agreement":null},{"id":"W2513355907","doi":"10.1002/2016gl069755","title":"Tectonic tremor on Vancouver Island, Cascadia, modulated by the body and surface waves of the <i>M<sub>w</sub></i> 8.6 and 8.2, 2012 East Indian Ocean earthquakes","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Subduction; Tectonics; Episodic tremor and slip; Tsunami wave; Slip (aerodynamics); Plate tectonics; Seismic wave; Indian ocean; Surface wave; Modulation (music); Oceanography; Physics","score_opus":0.01349101572858114,"score_gpt":0.22360118370808893,"score_spread":0.2101101679795078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2513355907","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99835074,0.000031463274,0.000012627104,0.00003083663,0.000002649247,0.0000035519136,0.00023326941,0.0000069727844,0.0013279034],"genre_scores_gemma":[0.9991239,0.000055754044,0.00002520549,0.0000068938216,0.0000023270986,0.000003161246,0.00021403938,0.0000017990606,0.0005668713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993896,0.0000039114175,0.0000034363113,0.000015106179,0.000021603611,0.000016941205],"domain_scores_gemma":[0.9997855,0.000011515455,0.00003667836,0.000008244123,0.000073181014,0.0000849224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006274089,0.00028466093,0.00018373008,0.000604833,0.00074671605,0.00045956933,0.0002649803,0.00028130418,0.0014314892],"category_scores_gemma":[0.00040405255,0.00018538247,0.00011286366,0.00066297915,0.00031608864,0.00010919024,0.0005449605,0.0002503619,0.00026891605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000559094,0.00012938559,0.91181165,0.00012497441,0.00013025856,0.0018717169,0.0019894135,0.002721001,0.05788164,0.000108267894,0.0026496057,0.020023042],"study_design_scores_gemma":[0.0000054394063,0.000017939989,0.99891055,0.00000379902,0.0000082372235,0.000036510908,0.00023846985,0.0003079617,0.00018359917,0.000008570602,0.0002750481,0.0000038225626],"about_ca_topic_score_codex":0.486215,"about_ca_topic_score_gemma":0.7363471,"teacher_disagreement_score":0.513785,"about_ca_system_score_codex":0.0013741172,"about_ca_system_score_gemma":0.0009877689,"threshold_uncertainty_score":0.9667698},"labels":[],"label_agreement":null},{"id":"W2514354369","doi":"","title":"Possible Interactions between the 2012 M w 7.8 Haida Gwaii Subduction Earthquake and the Transform Queen Charlotte Fault","year":2014,"lang":"en","type":"article","venue":"2014 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Subduction; Seismology; Queen (butterfly); Geology; Transform fault; Fault (geology); Tectonics","score_opus":0.014187432303370018,"score_gpt":0.22372331932681658,"score_spread":0.20953588702344655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2514354369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.966694,0.0003132506,0.00061401457,0.0028132906,0.000106247324,0.000027478976,0.00038424585,0.000030014364,0.029017352],"genre_scores_gemma":[0.9972905,0.0001464717,0.00013332904,0.000119040014,0.000035107914,0.000007667794,0.00015179419,0.0000035723908,0.0021126685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998221,0.000035271092,0.000009896614,0.00003635177,0.000030182058,0.0000662588],"domain_scores_gemma":[0.9992151,0.0002456005,0.00023278595,0.00003143057,0.00015299079,0.00012211387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034994265,0.00029719018,0.00027244433,0.00114773,0.001703448,0.0019863984,0.00054701214,0.0017315774,0.007681619],"category_scores_gemma":[0.0022476912,0.00034123013,0.0002575473,0.0010314456,0.001320823,0.0010170548,0.0013256699,0.0009135842,0.0005174438],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023882212,0.0003813338,0.84655035,0.00029999847,0.0002559258,0.01558101,0.007451038,0.016422754,0.025060315,0.03630015,0.010503234,0.038805682],"study_design_scores_gemma":[0.00012721823,0.00017942066,0.9678984,0.00010990507,0.00008257787,0.0008386617,0.005257293,0.007070188,0.0010836556,0.0052369614,0.012045327,0.00007036327],"about_ca_topic_score_codex":0.05303689,"about_ca_topic_score_gemma":0.1329151,"teacher_disagreement_score":0.94696313,"about_ca_system_score_codex":0.002010632,"about_ca_system_score_gemma":0.0013887078,"threshold_uncertainty_score":0.10545635},"labels":[],"label_agreement":null},{"id":"W2514400434","doi":"","title":"GPS monitoring of crustal strain in southwest british columbia with the western canada deformation array","year":2019,"lang":"en","type":"article","venue":"GEOMATICA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Global Positioning System; Geography; Geology; Geodesy; Seismology; Deformation (meteorology); Strain (injury); Archaeology; Cartography; Remote sensing; Oceanography; Telecommunications","score_opus":0.0066379238041180495,"score_gpt":0.16915332889587398,"score_spread":0.16251540509175594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2514400434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9707375,0.0007496975,0.0003578123,0.00042306155,0.000018334731,0.000077338,0.016440863,0.00004837921,0.011147069],"genre_scores_gemma":[0.98162675,0.00071664597,0.00093458086,0.0001223447,0.0000058154205,0.00003978275,0.0058758236,0.000014348734,0.010663893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997352,0.000022321401,0.00001677334,0.00005668226,0.000108011074,0.00006104035],"domain_scores_gemma":[0.99906486,0.000029722167,0.000081456405,0.0000309982,0.0006604636,0.00013248337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021948808,0.00028246085,0.00019089233,0.0012871724,0.0013781493,0.000707164,0.0006322478,0.00024039796,0.002150191],"category_scores_gemma":[0.0006834073,0.00020381507,0.00011063871,0.0039035846,0.00034514017,0.0002321273,0.0005673184,0.0003149417,0.00048147023],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000111038324,0.00006132786,0.9455751,0.00008104616,0.00007805335,0.00023335521,0.0013634275,0.0009548389,0.0027475057,0.00020200737,0.009864912,0.03872732],"study_design_scores_gemma":[0.0000068863533,0.0000075464286,0.994749,0.000021294767,0.000012878967,0.000026262218,0.0007729367,0.00046432336,0.00023297267,0.000013380925,0.003684659,0.000007958177],"about_ca_topic_score_codex":0.9971414,"about_ca_topic_score_gemma":0.9992507,"teacher_disagreement_score":0.011216233,"about_ca_system_score_codex":0.011216233,"about_ca_system_score_gemma":0.01308113,"threshold_uncertainty_score":0.08137989},"labels":[],"label_agreement":null},{"id":"W2515185451","doi":"10.1130/g38118.1","title":"Control of lithospheric inheritance on neotectonic activity in northwestern Canada?","year":2016,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"Natural Resources Data Management System; National Science Foundation","keywords":"Citation; Geologist; Icon; Windsor; Library science; History; Archaeology; Geology; Computer science","score_opus":0.008927996292793366,"score_gpt":0.1880745688774354,"score_spread":0.17914657258464203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515185451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99726534,0.00010738848,0.00004361143,0.00007579221,0.0000016896865,0.0000026828934,0.0003675249,0.000007718782,0.002128353],"genre_scores_gemma":[0.9990683,0.00007722719,0.000048920014,0.000011947266,6.5749447e-7,0.0000011351119,0.00015547135,0.000002151834,0.00063423626],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998803,0.000006321576,0.0000033357953,0.000025138264,0.000024883479,0.000059999642],"domain_scores_gemma":[0.9996432,0.00001860478,0.000057454836,0.000011417342,0.00016464676,0.00010463717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010899613,0.00016248321,0.00014872952,0.0006534262,0.0008953153,0.0007107472,0.0003184097,0.0001484977,0.002024625],"category_scores_gemma":[0.00046829658,0.00008860751,0.00009282406,0.0009888484,0.0004590928,0.00013662914,0.00038740484,0.00012985327,0.0001373181],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030280283,0.000027953358,0.9428873,0.000038609236,0.00004509342,0.00033824838,0.0012795039,0.0010937505,0.029831378,0.00097388367,0.00078654866,0.022394925],"study_design_scores_gemma":[0.0000032936623,0.0000053972367,0.99726105,0.000006828429,0.00000677909,0.00002328219,0.00074909814,0.00045067698,0.0005379044,0.00006171735,0.0008886904,0.0000054042516],"about_ca_topic_score_codex":0.96845776,"about_ca_topic_score_gemma":0.9871186,"teacher_disagreement_score":0.03154224,"about_ca_system_score_codex":0.010112515,"about_ca_system_score_gemma":0.00690307,"threshold_uncertainty_score":0.07337171},"labels":[],"label_agreement":null},{"id":"W2515539769","doi":"","title":"Active Tectonics and the Earthquake Cycle: Approaches, Observations, Insights IIII","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Kootenay Association for Science & Technology","funders":"","keywords":"Geology; Tectonics; Seismology; Geophysics; Plate tectonics","score_opus":0.06709790393617485,"score_gpt":0.22841482428551288,"score_spread":0.16131692034933803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515539769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7695056,0.015898079,0.020731166,0.0034234442,0.00014796607,0.00017026713,0.011227509,0.00021899398,0.1786769],"genre_scores_gemma":[0.97929126,0.0057235593,0.004844261,0.0002120781,0.0001614638,0.00003810933,0.0030137906,0.000035802994,0.006679707],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998173,0.000046623914,0.000015873113,0.00003401499,0.000056342193,0.00002984155],"domain_scores_gemma":[0.9995859,0.00014994344,0.00009890006,0.000052231564,0.00007439988,0.000038606104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041758816,0.00030088646,0.00021962603,0.0021073602,0.0004886681,0.0021108496,0.00028699494,0.00028646024,0.003603115],"category_scores_gemma":[0.001144137,0.00015903317,0.0003069648,0.003599664,0.00061542814,0.0011878903,0.00087607565,0.0005725662,0.00038084036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027150146,0.00019277965,0.6314197,0.00048213048,0.00012222017,0.0002230798,0.0035219858,0.004750694,0.0052616997,0.047296368,0.010450192,0.2960076],"study_design_scores_gemma":[0.00001027355,0.000062782245,0.9475454,0.00021545112,0.000036031914,0.00013037311,0.0025763386,0.004741462,0.0010277069,0.01059044,0.03303807,0.000025654317],"about_ca_topic_score_codex":0.034427647,"about_ca_topic_score_gemma":0.045575894,"teacher_disagreement_score":0.034427647,"about_ca_system_score_codex":0.0015679327,"about_ca_system_score_gemma":0.0007325184,"threshold_uncertainty_score":0.068454504},"labels":[],"label_agreement":null},{"id":"W2515563217","doi":"10.15273/ijge.2016.03.014","title":"Dating Strong Prehistoric Earthquakes and Estimating Their Recurrence Interval Applying Radiocarbon Analysis and Dendroseismological Approach – Case Study from SE Altai (Russia)","year":2016,"lang":"en","type":"article","venue":"International journal of geohazards and environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Siberian Federal University; Siberian Branch, Russian Academy of Sciences","keywords":"Radiocarbon dating; Geology; Massif; Seismology; Holocene; Induced seismicity; Active fault; Context (archaeology); Chronology; Kola peninsula; Seismic risk; Fault (geology); Paleontology; Geochemistry","score_opus":0.029075995179521745,"score_gpt":0.24623947523748982,"score_spread":0.21716348005796807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515563217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995658,0.000032791326,0.00014168401,0.0000031340426,4.2315347e-7,0.0000024050125,0.000018707005,0.0000014091308,0.00023353017],"genre_scores_gemma":[0.9993562,0.000076941156,0.00039139655,8.4982645e-7,0.0000010209379,0.000001917149,0.00005593596,0.0000014116745,0.000114211696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998621,0.00003784357,0.000011251772,0.000030074396,0.000022715465,0.000036048135],"domain_scores_gemma":[0.9996878,0.00009106097,0.00009405662,0.000040741066,0.000060868533,0.000025490826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037936194,0.00023041134,0.00017391703,0.0010102956,0.0004976039,0.0004297829,0.000295001,0.00025395027,0.00023524885],"category_scores_gemma":[0.0006514576,0.00012768719,0.00027607734,0.0011200908,0.00037186957,0.00016762206,0.00025770254,0.00015733286,0.000076276774],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012285926,0.00011320236,0.94971174,0.000039893144,0.00006264274,0.0060553495,0.0027315107,0.004495491,0.016846133,0.00044473665,0.00008359542,0.019292884],"study_design_scores_gemma":[0.00000400432,0.00013132709,0.9906098,0.00000865666,0.000040441624,0.00088515744,0.0017071093,0.0031102633,0.0027788165,0.000082344326,0.00063359994,0.000008401724],"about_ca_topic_score_codex":0.022980865,"about_ca_topic_score_gemma":0.034735046,"teacher_disagreement_score":0.022980865,"about_ca_system_score_codex":0.00043562724,"about_ca_system_score_gemma":0.000268436,"threshold_uncertainty_score":0.045694232},"labels":[],"label_agreement":null},{"id":"W2515592211","doi":"10.1002/2016jb013085","title":"Characteristics of slow earthquakes in the very low frequency band: Application to the Cascadia subduction zone","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Seismology; Subduction; Geology; Very low frequency; Seismogram; Seismometer; Episodic tremor and slip; Frequency band; Geophysics; Geodesy; Tectonics; Bandwidth (computing); Physics","score_opus":0.02510652625031032,"score_gpt":0.29085429085960945,"score_spread":0.2657477646092991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515592211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966091,0.0001075942,0.0021084314,0.00004936518,0.000005379089,0.000009135882,0.00036914484,0.00011825805,0.0006236726],"genre_scores_gemma":[0.9985505,0.00004514842,0.0009257032,0.0000030592257,0.0000047143913,0.0000030087824,0.00033187258,0.000009414742,0.00012656488],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999899,0.000015745827,0.000010605056,0.0000319671,0.000026798863,0.00001577646],"domain_scores_gemma":[0.9995536,0.00011131816,0.00008464166,0.00007676248,0.0001034709,0.00007024412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032060652,0.00052898005,0.00027626904,0.0018635526,0.00034511712,0.00041239476,0.00033342338,0.00036905467,0.00082701305],"category_scores_gemma":[0.0010089971,0.00017484,0.00032324228,0.0017497421,0.00023516451,0.00017316444,0.00039603963,0.00019499507,0.00019146563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051966595,0.00023713821,0.7559514,0.00026252164,0.00028014794,0.0021057366,0.0012602997,0.046237797,0.10582195,0.0002890229,0.0010025243,0.08603174],"study_design_scores_gemma":[0.000024025787,0.00009408557,0.9462613,0.000012310814,0.00007606976,0.0001954534,0.00028619583,0.04843151,0.0036556933,0.0001838275,0.00075252383,0.000027049884],"about_ca_topic_score_codex":0.019864423,"about_ca_topic_score_gemma":0.02205592,"teacher_disagreement_score":0.019864423,"about_ca_system_score_codex":0.00027139697,"about_ca_system_score_gemma":0.00024596442,"threshold_uncertainty_score":0.039497554},"labels":[],"label_agreement":null},{"id":"W2516764388","doi":"10.1002/2016jb012981","title":"An efficient repeating signal detector to investigate earthquake swarms","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Seismology; Induced seismicity; Seismometer; Geology; Volcano; Earthquake swarm; Waveform; Computer science","score_opus":0.04896967192179296,"score_gpt":0.3255477969576598,"score_spread":0.2765781250358668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2516764388","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19552408,0.00017879906,0.7971569,0.00010919391,0.000060937546,0.00013458493,0.00084854016,0.003922314,0.0020646907],"genre_scores_gemma":[0.4361513,0.00007942846,0.5605903,0.00004807482,0.000022831347,0.00011522052,0.0014114091,0.00011013749,0.001471331],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997322,0.000033323904,0.000021700456,0.000064604086,0.00011564601,0.000032531818],"domain_scores_gemma":[0.99916863,0.00028290026,0.00009325182,0.000107367014,0.00027635007,0.00007153637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004973998,0.00046776189,0.0005142586,0.0022935627,0.00027772336,0.00047670555,0.0007060304,0.0003749845,0.0017192813],"category_scores_gemma":[0.0017936904,0.00025909278,0.0002835071,0.0014647781,0.0001960682,0.00042436022,0.00073318323,0.0002598203,0.0008661815],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054095447,0.00028271863,0.037197612,0.00022118528,0.00017247454,0.00045598418,0.0002494178,0.07456068,0.22571914,0.00406156,0.0063435775,0.6501947],"study_design_scores_gemma":[0.000043390628,0.00015678183,0.009571012,0.000008444797,0.000024867431,0.00022732723,0.00009641608,0.9561872,0.028729657,0.0012326778,0.0036931909,0.00002900396],"about_ca_topic_score_codex":0.0020851744,"about_ca_topic_score_gemma":0.003643675,"teacher_disagreement_score":0.0022935627,"about_ca_system_score_codex":0.00031430848,"about_ca_system_score_gemma":0.0007996087,"threshold_uncertainty_score":0.00575161},"labels":[],"label_agreement":null},{"id":"W2518078323","doi":"10.1130/g38178.1","title":"The mechanism of partial rupture of a locked megathrust: The role of fault morphology","year":2016,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":117,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Canadian Space Agency","keywords":"Geology; Mechanism (biology); Morphology (biology); Fault (geology); Seismology; Paleontology; Epistemology; Philosophy","score_opus":0.00787747943200566,"score_gpt":0.19525479012291588,"score_spread":0.18737731069091024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2518078323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911048,0.0002781218,0.0044379802,0.00026434445,0.0000113949145,0.000012575246,0.00006982601,0.00007793801,0.0037430783],"genre_scores_gemma":[0.9995757,0.00004704746,0.00014431933,0.000008204999,0.0000028998688,0.0000021069227,0.000010835104,0.0000025137786,0.00020647669],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992096,0.000013562442,0.000006789307,0.000020579151,0.000015718537,0.000022315866],"domain_scores_gemma":[0.9994709,0.00011429323,0.00017292955,0.00010514536,0.00006423051,0.00007255469],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028499306,0.00022094253,0.0003251626,0.00066370243,0.0004205754,0.0013063026,0.00082032435,0.0007113626,0.0017782544],"category_scores_gemma":[0.0010145328,0.00030628775,0.00021480682,0.00025227354,0.00091537955,0.0011214376,0.00067858613,0.00032093865,0.00031987837],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006089428,0.00031250267,0.47905913,0.00059117854,0.00041324398,0.0062708994,0.0018722545,0.103895254,0.296117,0.059189517,0.0020405396,0.049629577],"study_design_scores_gemma":[0.0000822617,0.000634293,0.555833,0.00012107506,0.00015301966,0.0045341817,0.0022772236,0.35981756,0.046512548,0.02598035,0.0039355597,0.00011893737],"about_ca_topic_score_codex":0.0013524005,"about_ca_topic_score_gemma":0.001073357,"teacher_disagreement_score":0.0017782544,"about_ca_system_score_codex":0.00056569715,"about_ca_system_score_gemma":0.00023336158,"threshold_uncertainty_score":0.0059488416},"labels":[],"label_agreement":null},{"id":"W2518496520","doi":"10.1002/2016gl070421","title":"Poroelastic stress triggering of the December 2013 Crooked Lake, Alberta, induced seismicity sequence","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":177,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Induced seismicity; Poromechanics; Geology; Pore water pressure; Hydraulic fracturing; Coulomb; Seismology; Stress (linguistics); Sequence (biology); Geotechnical engineering; Physics; Porous medium","score_opus":0.053895171252366376,"score_gpt":0.2861689851266961,"score_spread":0.23227381387432972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2518496520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976433,0.000029549166,0.00019526608,0.000044466513,0.000003557204,0.000015823409,0.00043868093,0.000038555263,0.0015907474],"genre_scores_gemma":[0.9990331,0.000024965771,0.0001043417,0.000006272747,0.0000010064796,0.0000037298444,0.00024612853,0.0000031305954,0.00057740015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992585,0.0000028561694,0.0000032133698,0.000010815027,0.000033497687,0.000023794366],"domain_scores_gemma":[0.9998679,0.000007657918,0.0000214996,0.000004397191,0.000057367655,0.000041246272],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009716645,0.0002233301,0.00013998456,0.000618482,0.0006273955,0.0005301117,0.00050454825,0.000321649,0.0013277782],"category_scores_gemma":[0.0004331919,0.00012887875,0.00011290929,0.0007434162,0.00048105046,0.000108396205,0.00032047083,0.000201673,0.00011619679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011107555,0.00026047774,0.81673956,0.00020353345,0.00013925093,0.003942966,0.001212088,0.079055406,0.059634585,0.0013129002,0.004377469,0.032011114],"study_design_scores_gemma":[0.000020549982,0.000032581298,0.9802822,0.000008561738,0.000015178379,0.000054217584,0.00047695008,0.01633611,0.0018606725,0.00006169132,0.0008384457,0.000012900705],"about_ca_topic_score_codex":0.86609805,"about_ca_topic_score_gemma":0.9402418,"teacher_disagreement_score":0.13390195,"about_ca_system_score_codex":0.005438863,"about_ca_system_score_gemma":0.0042928015,"threshold_uncertainty_score":0.269381},"labels":[],"label_agreement":null},{"id":"W2519167552","doi":"10.1002/2016gl070427","title":"Relocation of long‐period (LP) seismic events reveals en echelon fractures in the upper edifice of Turrialba volcano, Costa Rica","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"Consejo Nacional de Rectores; Science Foundation Ireland","keywords":"Geology; Volcano; Echelon formation; Seismology; Relocation; Joint (building); Shearing (physics); Fault (geology); Geotechnical engineering; Computer science","score_opus":0.024604067946953963,"score_gpt":0.30011295111814185,"score_spread":0.2755088831711879,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2519167552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992855,0.000030196257,0.00019038883,0.0000118201315,0.0000010531962,0.00000442742,0.00013579837,0.0000143385905,0.00032655933],"genre_scores_gemma":[0.9995403,0.000011426428,0.00020868455,0.0000023695952,0.0000012831729,0.0000025107618,0.00016086768,0.0000019729423,0.000070704096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999094,0.000015229871,0.000007292418,0.000029459245,0.000017172073,0.000021414606],"domain_scores_gemma":[0.99973065,0.000032774537,0.000087620836,0.000053389984,0.0000624721,0.00003314952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020675537,0.00015461321,0.0001577968,0.0006030279,0.00021294905,0.00027532846,0.00027304215,0.00024039976,0.00033923678],"category_scores_gemma":[0.0005620844,0.00010010208,0.00014389648,0.0005509605,0.00024218112,0.00012813251,0.00035331145,0.00012193368,0.00008502645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030925052,0.000113810966,0.90121156,0.00008278321,0.00012683848,0.00091968983,0.0016943899,0.008816048,0.05033785,0.0002218233,0.00056987704,0.03559605],"study_design_scores_gemma":[0.0000046260075,0.000016773163,0.9946577,0.0000054536195,0.00001150426,0.00007867578,0.00027415593,0.0040177144,0.0006271704,0.000011903134,0.00029075428,0.000003683356],"about_ca_topic_score_codex":0.029500853,"about_ca_topic_score_gemma":0.06389388,"teacher_disagreement_score":0.029500853,"about_ca_system_score_codex":0.00033251423,"about_ca_system_score_gemma":0.00022886819,"threshold_uncertainty_score":0.058658242},"labels":[],"label_agreement":null},{"id":"W2520282094","doi":"10.1111/gfl.12188","title":"The biases and trends in fault zone hydrogeology conceptual models: global compilation and categorical data analysis","year":2016,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; McGill University","funders":"Japan Atomic Energy Agency; Fonds de recherche du Québec – Nature et technologies; U.S. Geological Survey","keywords":"Electrical conduit; Geology; Lithology; Hydrogeology; Outcrop; Petrology; Fault (geology); Borehole; Sedimentary rock; Permeability (electromagnetism); Categorical variable; Seismology; Geochemistry; Geotechnical engineering","score_opus":0.07192914647151451,"score_gpt":0.2738672665460626,"score_spread":0.2019381200745481,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2520282094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.44009778,0.3571284,0.12892786,0.0068116165,0.0007595085,0.00032704597,0.04956985,0.0013121897,0.015065769],"genre_scores_gemma":[0.8887813,0.05650806,0.03770683,0.0007959164,0.00028424454,0.00037423545,0.014685701,0.0003795474,0.0004840819],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.96504307,0.01914949,0.005217122,0.0044899127,0.00573594,0.00036449282],"domain_scores_gemma":[0.6157086,0.29247734,0.030217916,0.0190848,0.04188152,0.0006298415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.06294417,0.0008218224,0.0011767722,0.021368908,0.00025516306,0.004253349,0.0019670152,0.0006004219,0.00162646],"category_scores_gemma":[0.17981519,0.0004914686,0.0028467025,0.030994257,0.0015719525,0.00398706,0.0020718114,0.0010079397,0.00040991412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037626686,0.00005734225,0.5630099,0.025180297,0.009294847,0.00016296605,0.004115047,0.02171704,0.00093695207,0.01741297,0.011259356,0.34647697],"study_design_scores_gemma":[0.00010464822,0.0005643185,0.7370132,0.041906197,0.007546441,0.0006773317,0.009185092,0.05322084,0.0040953024,0.029522903,0.115743555,0.00042017974],"about_ca_topic_score_codex":0.00731665,"about_ca_topic_score_gemma":0.0071218605,"teacher_disagreement_score":0.06294417,"about_ca_system_score_codex":0.0022376732,"about_ca_system_score_gemma":0.0020749134,"threshold_uncertainty_score":0.3328845},"labels":[],"label_agreement":null},{"id":"W2521154339","doi":"","title":"Erosion of Fluted Cliffs on the Na Pali Coast, Kauai, Hawaiian Islands","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Erosion; Archaeology; Oceanography; Geography; Geomorphology","score_opus":0.04088656184474962,"score_gpt":0.2362298664248273,"score_spread":0.19534330458007768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521154339","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999343,0.000025880976,0.000008229134,0.000007686734,6.1102867e-7,0.000002139667,0.00007693147,0.0000011746254,0.000534279],"genre_scores_gemma":[0.99953175,0.00002309699,0.000026983993,0.0000031243599,7.462124e-7,0.0000027575034,0.00009006321,6.278796e-7,0.00032098131],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993813,0.000007763162,0.0000061398136,0.0000152198545,0.000010449276,0.000022238046],"domain_scores_gemma":[0.9998023,0.000023423936,0.000047745878,0.000010701558,0.00007185115,0.00004390547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012991519,0.000188649,0.0001550236,0.00087063125,0.0007695991,0.0007224979,0.000357004,0.00028333013,0.0011954911],"category_scores_gemma":[0.00046459906,0.00014936295,0.00017659353,0.0009727899,0.0004244883,0.00032725747,0.00055160176,0.00016384125,0.00011558269],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017261322,0.000032422515,0.9845999,0.000043948858,0.000081332226,0.0007459924,0.0038680953,0.00076551957,0.0029452438,0.00009703366,0.00024339904,0.006404582],"study_design_scores_gemma":[0.0000021437904,0.00001093442,0.99777055,0.000004937002,0.000007663004,0.000040184055,0.0016983316,0.00021229386,0.000047810034,0.000007688535,0.00019463632,0.0000030598578],"about_ca_topic_score_codex":0.29126957,"about_ca_topic_score_gemma":0.48728582,"teacher_disagreement_score":0.29126957,"about_ca_system_score_codex":0.001327622,"about_ca_system_score_gemma":0.0006772533,"threshold_uncertainty_score":0.5791484},"labels":[],"label_agreement":null},{"id":"W2521339852","doi":"10.1126/science.aag0262","title":"Surface uplift and time-dependent seismic hazard due to fluid injection in eastern Texas","year":2016,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":168,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Environment Research Council; Biodesign Institute, Arizona State University; Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Sight Research UK; Canadian Space Agency; National Science Foundation","keywords":"Induced seismicity; Geology; Pore water pressure; Poromechanics; Seismology; Compressibility; Interferometric synthetic aperture radar; Seismic hazard; Fluid pressure; Petrology; Geomorphology; Geotechnical engineering; Porosity; Synthetic aperture radar; Porous medium","score_opus":0.013276826108505968,"score_gpt":0.22162206403979007,"score_spread":0.2083452379312841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521339852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998547,0.0000034421878,0.000023130646,0.0000059697854,1.9993178e-7,5.9931824e-7,0.000025080317,0.0000013383882,0.000085630956],"genre_scores_gemma":[0.9998512,0.0000075510616,0.000027157612,0.0000018181318,6.5998626e-7,7.9714306e-7,0.00003965407,4.143534e-7,0.00007053882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999391,0.000007043071,0.0000053588064,0.00001544923,0.000009884781,0.000023195204],"domain_scores_gemma":[0.9995184,0.000060353465,0.00027345994,0.000022061595,0.00005986164,0.00006596534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014436156,0.00012942,0.00010728775,0.00052148965,0.00024301356,0.00030820316,0.00016183025,0.00018270845,0.0007151858],"category_scores_gemma":[0.00045599366,0.000098907585,0.000101525126,0.0005576055,0.0003832463,0.00026824922,0.00046407565,0.00015955933,0.000076777025],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017860168,0.00005445189,0.98499286,0.000010854792,0.000022493388,0.0004299968,0.000488536,0.0030211369,0.007011617,0.00008396558,0.00007463062,0.0036307736],"study_design_scores_gemma":[0.0000030132228,0.000043059867,0.9967032,0.0000025151915,0.0000065760883,0.000046086967,0.00041811005,0.0021280868,0.0005302481,0.000024717958,0.00009122871,0.0000031983343],"about_ca_topic_score_codex":0.023907978,"about_ca_topic_score_gemma":0.04528847,"teacher_disagreement_score":0.023907978,"about_ca_system_score_codex":0.0007555042,"about_ca_system_score_gemma":0.00034076168,"threshold_uncertainty_score":0.047537684},"labels":[],"label_agreement":null},{"id":"W2521961519","doi":"10.1002/2016gl070042","title":"A preliminary statistical model for hydraulic fracture‐induced seismicity in the Western Canada Sedimentary Basin","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Seismology; Structural basin; Sedimentary rock; Geotechnical engineering; Geomorphology; Geochemistry","score_opus":0.04681803951420596,"score_gpt":0.2925469930871686,"score_spread":0.24572895357296262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521961519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8630463,0.0004066783,0.12333814,0.001593657,0.00003974901,0.00021986864,0.0038638564,0.000559721,0.006932063],"genre_scores_gemma":[0.9897983,0.00019004893,0.0032363562,0.00007136404,0.000024605666,0.00010048302,0.00076956756,0.000039322516,0.005769985],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99933654,0.00013031156,0.00002307115,0.00017126076,0.0001243292,0.00021436422],"domain_scores_gemma":[0.99698347,0.0015327017,0.0005390864,0.00018116953,0.0005490923,0.00021441841],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024298204,0.00065721065,0.00090988696,0.0015711751,0.001236273,0.0017059905,0.0028773767,0.0008486879,0.0037413],"category_scores_gemma":[0.007550574,0.0008073363,0.00085353194,0.0014844404,0.002547616,0.000867611,0.000837969,0.00094517,0.00037613342],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007964375,0.000022856082,0.0131988395,0.000015404834,0.00005790908,0.00013143689,0.000119057324,0.964267,0.0006373126,0.017489182,0.00091075373,0.0030705873],"study_design_scores_gemma":[0.0000130539165,0.00001868698,0.004975972,0.0000057500506,0.000020445646,0.000021632339,0.000043662785,0.9917303,0.00008695978,0.002745232,0.00032378017,0.000014596385],"about_ca_topic_score_codex":0.81004524,"about_ca_topic_score_gemma":0.6206012,"teacher_disagreement_score":0.18995476,"about_ca_system_score_codex":0.008012005,"about_ca_system_score_gemma":0.006855391,"threshold_uncertainty_score":0.38214684},"labels":[],"label_agreement":null},{"id":"W2522060887","doi":"10.1002/2016gc006500","title":"Experimental constraints on the relationship between clay abundance, clay fabric, and frictional behavior for the <scp>C</scp>entral <scp>D</scp>eforming <scp>Z</scp>one of the <scp>S</scp>an <scp>A</scp>ndreas <scp>F</scp>ault","year":2016,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Geology; Clastic rock; Fault gouge; Quartz; Clay minerals; Slip (aerodynamics); Borehole; Fault (geology); Mineralogy; Shear (geology); Geotechnical engineering; Petrology; Sedimentary rock; Geochemistry; Seismology","score_opus":0.032769960102919694,"score_gpt":0.24138706362356674,"score_spread":0.20861710352064705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2522060887","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979109,0.00005219648,0.0010928662,0.000010880803,0.0000013974084,0.000013111903,0.00025667736,0.000012511276,0.00064940524],"genre_scores_gemma":[0.9982298,0.00002585286,0.0010871575,0.00001118034,0.0000011104866,0.000028567265,0.00039623497,0.000007634019,0.00021255856],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996,0.000073186,0.000053637246,0.00011984083,0.00009428607,0.000059144517],"domain_scores_gemma":[0.99869555,0.0006329234,0.00021881583,0.00023392843,0.00015138509,0.00006733651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005019514,0.00022187583,0.00014588468,0.00025834315,0.00037359167,0.00027925248,0.0003040162,0.00021631128,0.0020314965],"category_scores_gemma":[0.0011421498,0.00022825299,0.00012597135,0.00016711281,0.00068680214,0.00022822275,0.00029249198,0.00020646656,0.00021960174],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024209818,0.00008919698,0.02383528,0.00003001175,0.000011525715,0.000031979653,0.000063718064,0.0002464828,0.9740451,0.0001044896,0.000030238398,0.0012698496],"study_design_scores_gemma":[0.000020097039,0.00048064103,0.35779855,0.0000082295965,0.00002227979,0.000156429,0.0001981051,0.0028938567,0.6374414,0.000087841734,0.0008793426,0.000013259221],"about_ca_topic_score_codex":0.007951979,"about_ca_topic_score_gemma":0.016447589,"teacher_disagreement_score":0.007951979,"about_ca_system_score_codex":0.000520854,"about_ca_system_score_gemma":0.0002457059,"threshold_uncertainty_score":0.015811384},"labels":[],"label_agreement":null},{"id":"W2525535596","doi":"10.1111/gfl.12200","title":"Complexity of hydrogeologic regime around an ancient low‐angle thrust fault revealed by multidisciplinary field study","year":2016,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; University of Victoria; McGill University","funders":"McGill University","keywords":"Geology; Hydrogeology; Aquifer; Thrust fault; Fault (geology); Outcrop; Karst; Groundwater flow; Groundwater; Geomorphology; Petrology; Geotechnical engineering; Seismology; Paleontology","score_opus":0.03775952191381016,"score_gpt":0.2615370125803619,"score_spread":0.22377749066655173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2525535596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99957687,0.000033132696,0.00007204249,0.000007845981,4.0192623e-7,0.0000035923192,0.0000558285,0.0000021323772,0.00024821932],"genre_scores_gemma":[0.9995504,0.000029793186,0.00013785336,0.0000062760187,0.0000016920956,0.0000035327632,0.000111318965,8.163998e-7,0.00015838855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980193,0.000037083766,0.000010683363,0.00006391766,0.000034075372,0.000052323227],"domain_scores_gemma":[0.9995895,0.000060847975,0.00013833893,0.000031738975,0.00010705042,0.00007256558],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002839862,0.00014991958,0.00020837365,0.002696588,0.00074620603,0.0005935183,0.00030722097,0.00027849496,0.0006278229],"category_scores_gemma":[0.00041801512,0.00013355073,0.00009648973,0.0012835457,0.00072724983,0.00038727355,0.0004998432,0.00013023918,0.00007882495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000051065796,0.00003830368,0.9716017,0.000019367277,0.00004125807,0.00043658176,0.0017950948,0.0003278044,0.016549582,0.00009683159,0.00011696571,0.008925462],"study_design_scores_gemma":[8.257652e-7,0.000012666625,0.9985409,0.0000041929343,0.000003704764,0.00007706865,0.0007411984,0.00023459364,0.00015967472,0.000023663648,0.00019949142,0.0000020168209],"about_ca_topic_score_codex":0.054248065,"about_ca_topic_score_gemma":0.15378791,"teacher_disagreement_score":0.054248065,"about_ca_system_score_codex":0.0011207573,"about_ca_system_score_gemma":0.00048321256,"threshold_uncertainty_score":0.10786462},"labels":[],"label_agreement":null},{"id":"W2528648791","doi":"10.1038/nature19787","title":"Asthenosphere rheology inferred from observations of the 2012 Indian Ocean earthquake","year":2016,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":117,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Asthenosphere; Seismology; Lithosphere; Plate tectonics; Crust; Mantle (geology); Convergent boundary; Earthquake rupture; Mantle convection; Interferometric synthetic aperture radar; Intraplate earthquake; Geophysics; Tectonics; Oceanic crust; Subduction; Synthetic aperture radar","score_opus":0.014012021289357286,"score_gpt":0.20871800755203745,"score_spread":0.19470598626268018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528648791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967655,0.00005142675,0.00011073665,0.000036717865,0.0000065425124,0.0000031691063,0.0014290113,0.000023107104,0.0015738701],"genre_scores_gemma":[0.9986059,0.000073455114,0.000097076874,0.0000071007958,0.0000072556254,0.0000019982774,0.0009824509,0.000005130652,0.000219597],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992204,0.000009338228,0.000010550482,0.000017393808,0.000016028482,0.000024686531],"domain_scores_gemma":[0.9995578,0.000081442835,0.0001334577,0.000050454546,0.00013042496,0.000046370307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011878831,0.0002737718,0.00016599367,0.0012617554,0.00028008304,0.00043373133,0.0002056567,0.00022171532,0.0010286674],"category_scores_gemma":[0.0011222648,0.0002118084,0.00018099064,0.0014612017,0.00015873548,0.00043095046,0.00035161237,0.00027545975,0.00033828293],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018466794,0.00003904649,0.96965605,0.00007606337,0.00006319801,0.00032753768,0.0006661869,0.0039164023,0.012692114,0.00014440819,0.0011185226,0.011115878],"study_design_scores_gemma":[0.0000019561217,0.0000059681993,0.9981553,0.0000034497505,0.00001113456,0.000024067125,0.00010333817,0.0010194522,0.00030437147,0.0000134280135,0.0003530148,0.0000044926724],"about_ca_topic_score_codex":0.0544827,"about_ca_topic_score_gemma":0.12569758,"teacher_disagreement_score":0.0544827,"about_ca_system_score_codex":0.00032740197,"about_ca_system_score_gemma":0.00035409388,"threshold_uncertainty_score":0.108331144},"labels":[],"label_agreement":null},{"id":"W2528827837","doi":"10.1002/2016gl070983","title":"Nontrivial clustering of microseismicity induced by hydraulic fracturing","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium; University of Calgary; ConocoPhillips","keywords":"Microseism; Induced seismicity; Geology; Hydraulic fracturing; Magnitude (astronomy); Seismology; Layering; Aftershock; Fault (geology); Geophysics; Geotechnical engineering; Physics","score_opus":0.03513628772004963,"score_gpt":0.2813511092821919,"score_spread":0.2462148215621423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528827837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99024045,0.000025196481,0.008916307,0.00002054748,0.0000028526465,0.000016700411,0.00015878383,0.000056515997,0.0005626244],"genre_scores_gemma":[0.99937004,0.0000072273665,0.0003817402,0.0000021691012,0.0000027978879,0.000005068529,0.0001320262,0.000004767649,0.00009424578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998048,0.000024898782,0.000017176826,0.00005474325,0.0000497311,0.00004866505],"domain_scores_gemma":[0.9973122,0.00066198705,0.0009238762,0.00042720864,0.0004188254,0.0002559684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027695735,0.00012351088,0.00023047991,0.0012175784,0.00021241189,0.00043503192,0.00029409226,0.00019138787,0.0012152363],"category_scores_gemma":[0.0027775974,0.000119825745,0.0001881315,0.0007083795,0.0004571917,0.0003937362,0.00049438974,0.00017392731,0.00013949847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073551777,0.00018607642,0.69370747,0.00023579446,0.00030736506,0.0017940257,0.0014658436,0.109625995,0.122477055,0.022480095,0.0024218955,0.04456288],"study_design_scores_gemma":[0.000020543745,0.00010759945,0.8210896,0.000011321749,0.00003921854,0.00046884918,0.00038222843,0.15937439,0.007687173,0.009907073,0.0008607849,0.00005120123],"about_ca_topic_score_codex":0.00132489,"about_ca_topic_score_gemma":0.0012819201,"teacher_disagreement_score":0.00132489,"about_ca_system_score_codex":0.0003577283,"about_ca_system_score_gemma":0.00018470705,"threshold_uncertainty_score":0.0040653944},"labels":[],"label_agreement":null},{"id":"W2528969322","doi":"10.1139/cjes-2016-0115","title":"Seismic velocity model of the crust in the northern Canadian Cordillera from Rayleigh wave dispersion data","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Crust; Seismology; Rayleigh wave; Receiver function; Upper crust; Mantle (geology); Azimuth; Shear (geology); Surface wave; Geodesy; Geophysics; Lithosphere; Tectonics; Paleontology; Geometry","score_opus":0.0582941266709383,"score_gpt":0.21351073744481233,"score_spread":0.15521661077387403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528969322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97496766,0.0004380445,0.010990059,0.00014531089,0.000011850188,0.00006246555,0.0031247912,0.00046956472,0.00979021],"genre_scores_gemma":[0.99316895,0.00021800207,0.0032853258,0.00001351652,0.0000026348785,0.000017914575,0.0017847798,0.000035284687,0.0014735608],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99987304,0.000007825361,0.0000069426173,0.000045013247,0.00003306968,0.00003419806],"domain_scores_gemma":[0.9998776,0.000010840423,0.000019671448,0.000013254405,0.000059112157,0.000019475821],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016862011,0.00071293133,0.00023844486,0.0014380396,0.0007705545,0.0010298854,0.0012594237,0.00035951036,0.0021117928],"category_scores_gemma":[0.0008655067,0.0002688704,0.00037448507,0.0014253232,0.00038351037,0.00043894013,0.00039934367,0.00027075963,0.00035438873],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015982092,0.000063499836,0.19421044,0.000083906,0.0001190848,0.0002723603,0.00058883405,0.73644257,0.012016716,0.0057307007,0.0021699078,0.048142195],"study_design_scores_gemma":[0.0000368406,0.000026667456,0.13275963,0.000023462173,0.000041091327,0.000056656187,0.00018000166,0.86186725,0.0010078814,0.00085676037,0.0030930564,0.000050761104],"about_ca_topic_score_codex":0.9545555,"about_ca_topic_score_gemma":0.93167436,"teacher_disagreement_score":0.04544449,"about_ca_system_score_codex":0.010613615,"about_ca_system_score_gemma":0.0072507886,"threshold_uncertainty_score":0.09142417},"labels":[],"label_agreement":null},{"id":"W253173647","doi":"","title":"Development of the aftershock process of the 2010 Val-des-Bois (Quebec) Mw 5.0 Earthquake","year":2011,"lang":"en","type":"article","venue":"American Geophysical Union Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Geology; Seismology; Foreshock","score_opus":0.018408289032060036,"score_gpt":0.20949147806008292,"score_spread":0.19108318902802288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W253173647","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9556495,0.00080512546,0.00041396508,0.0021045108,0.000045214747,0.00007817587,0.003571171,0.000035441568,0.03729693],"genre_scores_gemma":[0.990599,0.00022972794,0.00013745314,0.00012587116,0.000007773375,0.00000935309,0.00078341295,0.000009893407,0.008097602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998406,0.000014958845,0.000005569343,0.000025204286,0.00004083607,0.000072685856],"domain_scores_gemma":[0.99893326,0.000052952644,0.000115438925,0.000019345247,0.0007212766,0.000157766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033545293,0.0001947472,0.00014112107,0.0013489197,0.0013974566,0.0017840102,0.0004844465,0.00070257066,0.008459723],"category_scores_gemma":[0.0013411121,0.00020121451,0.00016823002,0.00090391986,0.00059497164,0.0005252483,0.0007139212,0.00054776977,0.00059772603],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007445667,0.00026802163,0.83374256,0.00018617106,0.00012027193,0.0017343995,0.007394731,0.010008717,0.02046899,0.015917215,0.024471704,0.08494274],"study_design_scores_gemma":[0.000009224014,0.00003734461,0.9855995,0.000048525646,0.000010623905,0.00004523458,0.00178931,0.0017168728,0.00047003725,0.00017759917,0.01007724,0.000018518263],"about_ca_topic_score_codex":0.9729803,"about_ca_topic_score_gemma":0.9869802,"teacher_disagreement_score":0.02701968,"about_ca_system_score_codex":0.020175122,"about_ca_system_score_gemma":0.015183073,"threshold_uncertainty_score":0.14638144},"labels":[],"label_agreement":null},{"id":"W2534273878","doi":"10.1007/978-3-319-45612-6_3","title":"From Labquakes in Porous Materials to Earthquakes","year":2016,"lang":"en","type":"book-chapter","venue":"Understanding complex systems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Acoustic emission; Compression (physics); Seismology; Porosity; Geology; Porous medium; Materials science; Geotechnical engineering; Composite material","score_opus":0.10452729074864643,"score_gpt":0.24466221422783074,"score_spread":0.14013492347918433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2534273878","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02775943,0.08475967,0.14035656,0.00573285,0.0033852875,0.000049051025,0.00070019305,0.00091647555,0.73634046],"genre_scores_gemma":[0.28279835,0.07937353,0.03922249,0.0015948864,0.0016561815,0.0001278709,0.00067469355,0.0007028223,0.5938491],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9999484,0.000007792518,0.0000026808095,0.000010703469,0.000024113073,0.000006476671],"domain_scores_gemma":[0.99990964,0.000045254303,0.000005139772,0.000017140155,0.0000136595245,0.0000091161155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000112515925,0.0004865178,0.0003209821,0.00067376305,0.0004306706,0.0014933201,0.00055970374,0.00070684234,0.01554766],"category_scores_gemma":[0.0003473612,0.00030489397,0.00021393324,0.00080002565,0.0018415388,0.0026675456,0.0011991622,0.0011558844,0.0026775608],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014616121,0.000019367664,0.00008889614,0.00029420774,0.000005458615,0.00009641067,0.0002641777,0.004399069,0.003101054,0.88353044,0.021259448,0.08692688],"study_design_scores_gemma":[0.0000055736473,0.000017685164,0.00016061829,0.00008276528,0.0000047508365,0.00018048176,0.00011992344,0.0036881275,0.0023892228,0.66478103,0.32855624,0.000013622641],"about_ca_topic_score_codex":0.0005700915,"about_ca_topic_score_gemma":0.0010565469,"teacher_disagreement_score":0.01554766,"about_ca_system_score_codex":0.0004913517,"about_ca_system_score_gemma":0.00028981554,"threshold_uncertainty_score":0.052012086},"labels":[],"label_agreement":null},{"id":"W2537607085","doi":"10.1002/2016jb013244","title":"Distinct crustal structure of the North American Midcontinent Rift from <i>P</i> wave receiver functions","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; University of Manitoba","funders":"Northwestern University; National Science Foundation","keywords":"Geology; Rift; Seismology; Bouguer anomaly; Receiver function; Terrane; Crust; Archean; Underplating; Fault (geology); Gravity anomaly; Tectonics; Geophysics; Paleontology; Lithosphere","score_opus":0.02701380788038219,"score_gpt":0.2693459747573953,"score_spread":0.24233216687701312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2537607085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984812,0.00007868411,0.00015018179,0.000020384625,0.0000011930837,0.0000014205264,0.00032527308,0.00001558395,0.0009261635],"genre_scores_gemma":[0.99898344,0.000029304667,0.00010848588,0.0000060374196,0.0000017653654,0.0000012165063,0.000580533,0.0000031205323,0.00028609627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996054,0.000004732123,0.000001814928,0.000011795988,0.000009671113,0.000011470009],"domain_scores_gemma":[0.99975175,0.000035507313,0.000053404914,0.000016711047,0.000101654856,0.000040964034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012805531,0.00014478216,0.00007177383,0.0005483269,0.00017805658,0.00036592266,0.00012858109,0.00012395073,0.0014518477],"category_scores_gemma":[0.00035221005,0.00009807096,0.000080945945,0.00037180577,0.00011265324,0.00016130292,0.00021603944,0.0001098858,0.00022362116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075611424,0.000022718888,0.942202,0.000023895382,0.000042229673,0.00024222738,0.0005540512,0.00065854273,0.029643618,0.00013226364,0.0005362346,0.025866603],"study_design_scores_gemma":[5.38628e-7,0.000003950924,0.9993591,0.000001586353,0.0000030888841,0.000020486816,0.00003397872,0.00026697494,0.00011736735,0.0000048274037,0.00018714994,9.202206e-7],"about_ca_topic_score_codex":0.032103647,"about_ca_topic_score_gemma":0.067816846,"teacher_disagreement_score":0.032103647,"about_ca_system_score_codex":0.00018783844,"about_ca_system_score_gemma":0.00018907903,"threshold_uncertainty_score":0.063833594},"labels":[],"label_agreement":null},{"id":"W2541088369","doi":"10.1007/s00024-016-1414-9","title":"Probabilistic Tsunami Hazard Assessment for a Site in Eastern Canada","year":2016,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Energie NB Power (Canada); Amec Foster Wheeler (Canada)","funders":"","keywords":"Geology; Seismology; Fault (geology); Subduction; Seismic hazard; Hazard; Drawdown (hydrology); Landslide; Hazard analysis; Return period; Tectonics; Geography; Aquifer; Geotechnical engineering; Groundwater; Archaeology","score_opus":0.010058914134422699,"score_gpt":0.2047953240919901,"score_spread":0.1947364099575674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2541088369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99558616,0.000038457565,0.0006082286,0.000062625404,0.0000020272216,0.00002580688,0.0017692724,0.00002843531,0.0018790229],"genre_scores_gemma":[0.9975793,0.00003185746,0.00057361234,0.00000561945,7.4102815e-7,0.00000397313,0.0008083173,0.0000032110306,0.0009933678],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998343,0.000016451659,0.000008035774,0.000023498678,0.00006163954,0.000056079938],"domain_scores_gemma":[0.99946266,0.00007306048,0.00004655305,0.000020912823,0.00031624598,0.00008061001],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026032687,0.0002863524,0.00018974257,0.0012349267,0.001065465,0.0007711962,0.00080624764,0.00034374095,0.0018145329],"category_scores_gemma":[0.0009002082,0.00018010147,0.00031667715,0.0016570726,0.00034894675,0.0002665391,0.0004417769,0.00027710898,0.00013334662],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047392998,0.000115279916,0.78454113,0.00006512713,0.00015134455,0.0006403671,0.00045969355,0.18021639,0.0027155296,0.0015602513,0.0022466697,0.02681436],"study_design_scores_gemma":[0.000040481616,0.00008639184,0.78557974,0.000020605656,0.00008068556,0.00012051396,0.0026738963,0.207608,0.0010798929,0.0006254189,0.0020376218,0.00004679641],"about_ca_topic_score_codex":0.9832872,"about_ca_topic_score_gemma":0.99315804,"teacher_disagreement_score":0.016712785,"about_ca_system_score_codex":0.009637575,"about_ca_system_score_gemma":0.009711567,"threshold_uncertainty_score":0.069925845},"labels":[],"label_agreement":null},{"id":"W2546285388","doi":"10.1007/s00024-016-1407-8","title":"A Comparative Analysis of Coastal and Open-Ocean Records of the Great Chilean Tsunamis of 2010, 2014 and 2015 off the Coast of Mexico","year":2016,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Tide gauge; Pacific ocean; Submarine pipeline; Oceanography; Tsunami wave; Geology; Spectral analysis; Seismology; Climatology; Sea level","score_opus":0.014350345458794536,"score_gpt":0.22440422693497067,"score_spread":0.21005388147617612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2546285388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958056,0.0003587733,0.000045525427,0.00006856058,0.000006528475,0.000004845558,0.0028719306,0.0000045148895,0.00083370775],"genre_scores_gemma":[0.99226415,0.00048412586,0.00014104998,0.000027102213,0.000019457706,0.000014963082,0.0060380152,0.0000058153414,0.0010052659],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986875,0.00001548729,0.000018243738,0.00004128389,0.000020224952,0.000035919107],"domain_scores_gemma":[0.9992211,0.00014803257,0.00028726656,0.000058342877,0.00019763302,0.00008755463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031250645,0.0001541016,0.00015810994,0.0023061298,0.00031687887,0.00068516383,0.00023567067,0.00030809623,0.0012590674],"category_scores_gemma":[0.0010167195,0.00013326235,0.00025486326,0.0028320975,0.00025064708,0.0004909126,0.0008364226,0.00017021761,0.00017644811],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016277439,0.000025288058,0.9868297,0.00008391535,0.00018117815,0.00023273633,0.0010219853,0.00027711497,0.0021464664,0.00013199043,0.0008054371,0.008101453],"study_design_scores_gemma":[0.0000010953747,0.000003834714,0.9988914,0.0000072494818,0.000012393457,0.000021255515,0.00033282753,0.000047290236,0.000032815613,0.0000034794175,0.0006445671,0.0000017505157],"about_ca_topic_score_codex":0.10204817,"about_ca_topic_score_gemma":0.19367497,"teacher_disagreement_score":0.10204817,"about_ca_system_score_codex":0.0007366949,"about_ca_system_score_gemma":0.00072144484,"threshold_uncertainty_score":0.20290834},"labels":[],"label_agreement":null},{"id":"W2548976767","doi":"10.4095/211145","title":"Neotectonics in the Strait of Georgia: first tentative correlation of seismicity with shallow geological structure in southwestern British Columbia","year":2000,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Neotectonics; Induced seismicity; Geology; Seismology; Oceanography; Geography; Tectonics","score_opus":0.016761869900900426,"score_gpt":0.21334323510601344,"score_spread":0.19658136520511302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2548976767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958502,0.00016042763,0.000041596228,0.00012406515,0.0000031174955,0.000009109939,0.0008674295,0.000010573502,0.0029335849],"genre_scores_gemma":[0.996234,0.00025199176,0.00014117324,0.000052655476,0.0000016489151,0.000006943881,0.0012180698,0.0000045100655,0.0020889775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984574,0.000010580609,0.000011896554,0.000027122524,0.000043095602,0.000061450075],"domain_scores_gemma":[0.99938,0.000028385406,0.00009908161,0.00002734999,0.0003296713,0.00013542915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012476527,0.00017536059,0.00014410588,0.001493492,0.0012338002,0.00063848094,0.0003519288,0.0002131394,0.0011034103],"category_scores_gemma":[0.00056700787,0.00018679306,0.00008032495,0.0022876717,0.00046490406,0.00016039664,0.00067960843,0.00030691185,0.00028165465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027688204,0.000016599532,0.98276097,0.000022982998,0.000014780214,0.00031173983,0.0012411868,0.00015014237,0.0016852064,0.000102898885,0.001136591,0.012529155],"study_design_scores_gemma":[0.0000013748664,0.0000036369186,0.99812907,0.000008977799,0.000003807171,0.00005205913,0.0007235854,0.0000727089,0.00006680791,0.000010678199,0.0009245425,0.000002761302],"about_ca_topic_score_codex":0.9705995,"about_ca_topic_score_gemma":0.9960968,"teacher_disagreement_score":0.029400527,"about_ca_system_score_codex":0.0066707926,"about_ca_system_score_gemma":0.0055726934,"threshold_uncertainty_score":0.0591473},"labels":[],"label_agreement":null},{"id":"W2551002772","doi":"10.5539/jgg.v8n4p1","title":"Thermal Structure of the Outer Northern Apennines along the CROP-03 Profile","year":2016,"lang":"en","type":"article","venue":"Journal of Geography and Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Submarine pipeline; Lithosphere; Peninsula; Basement; Geomorphology; Sedimentary rock; Geochemistry; Tectonics; Seismology; Oceanography; Geography","score_opus":0.00576416093333977,"score_gpt":0.1856887667395383,"score_spread":0.17992460580619854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2551002772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893351,0.00010560008,0.0028922295,0.00005241636,0.000007421002,0.000014093068,0.000496329,0.00008925801,0.007007525],"genre_scores_gemma":[0.99770254,0.00007813129,0.00085235154,0.000006012257,0.0000029508892,0.000012693002,0.00020832369,0.000012822479,0.0011242327],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999696,0.0000059398267,0.0000013799971,0.000010832987,0.0000040956807,0.000008131131],"domain_scores_gemma":[0.9999509,0.00001071473,0.000010186664,0.000007799996,0.000011281515,0.000009097585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000049962244,0.00032104237,0.0001973289,0.00032669483,0.0003083419,0.0008171214,0.00035117185,0.00046101352,0.001589464],"category_scores_gemma":[0.0002586813,0.00019463582,0.00029195455,0.00043239974,0.00028951647,0.0002315411,0.00031247578,0.00020216627,0.00027714015],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000092619965,0.00006727318,0.06559599,0.000053734842,0.000046727866,0.000441268,0.00027131007,0.9172532,0.005022316,0.0012119731,0.00037456804,0.009568963],"study_design_scores_gemma":[0.000050862403,0.000051143885,0.09785465,0.000020674799,0.000026116311,0.00015700616,0.00027278313,0.8974304,0.0006240347,0.0005449217,0.0029374477,0.000029934788],"about_ca_topic_score_codex":0.036996838,"about_ca_topic_score_gemma":0.021429274,"teacher_disagreement_score":0.036996838,"about_ca_system_score_codex":0.0005876155,"about_ca_system_score_gemma":0.00038627526,"threshold_uncertainty_score":0.07356298},"labels":[],"label_agreement":null},{"id":"W2551254733","doi":"10.1093/gji/ggw439","title":"Asperity generation and its relationship to seismicity on a planar fault: a laboratory simulation","year":2016,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Asperity (geotechnical engineering); Geology; Surface finish; Fault (geology); Nucleation; Wavelength; Seismology; Induced seismicity; Stress (linguistics); Surface roughness; Materials science; Geotechnical engineering; Composite material","score_opus":0.03703779067152956,"score_gpt":0.2681328307770848,"score_spread":0.2310950401055552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2551254733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967457,0.00001966673,0.0013653357,0.0000824758,0.0000055808446,0.000020334954,0.00027540323,0.000046617053,0.0014388784],"genre_scores_gemma":[0.9979546,0.000024440722,0.0013776565,0.000014337668,0.0000022855256,0.000033499502,0.00019024136,0.000006145062,0.00039686705],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998815,0.000020547432,0.0000065681807,0.000025138055,0.00002347356,0.00004280485],"domain_scores_gemma":[0.999091,0.0005041332,0.00010805004,0.000081113416,0.00011294977,0.00010275018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003030173,0.00029477806,0.00050221826,0.00044688393,0.0003464709,0.0005635413,0.0010384916,0.0012141394,0.0023749073],"category_scores_gemma":[0.0015192949,0.0003182713,0.0005396051,0.00041538486,0.00074742624,0.00046420083,0.0007141873,0.0007890656,0.00013081433],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022510387,0.00038834987,0.013190738,0.000043357326,0.000047160353,0.00031633186,0.000080704056,0.9778072,0.004514188,0.0011924813,0.00038596545,0.0018083291],"study_design_scores_gemma":[0.000086500906,0.00025335638,0.0023018,0.0000043091527,0.000018306173,0.000024306175,0.00007748073,0.99562424,0.0011114746,0.00029591698,0.00019111414,0.0000111544],"about_ca_topic_score_codex":0.01966897,"about_ca_topic_score_gemma":0.009610482,"teacher_disagreement_score":0.01966897,"about_ca_system_score_codex":0.0009567847,"about_ca_system_score_gemma":0.0006892114,"threshold_uncertainty_score":0.039108932},"labels":[],"label_agreement":null},{"id":"W2551400655","doi":"10.1111/gfl.12180","title":"The effects of basement faults on thermal convection and implications for the formation of unconformity‐related uranium deposits in the Athabasca Basin, Canada","year":2016,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Regina","funders":"Cameco","keywords":"Geology; Unconformity; Convection; Convection cell; Fault (geology); Geothermal gradient; Petrology; Basement; Fluid dynamics; Structural basin; Plume; Upwelling; Geophysics; Uranium ore; Thermal; Shear (geology); Geochemistry; Geomorphology; Seismology; Natural convection; Uranium; Mechanics; Combined forced and natural convection; Meteorology","score_opus":0.006683669626555591,"score_gpt":0.19438363179597393,"score_spread":0.18769996216941834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2551400655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977914,0.000074012205,0.00031802017,0.00007465574,0.000004231032,0.0000064308897,0.00016064382,0.000026285525,0.0015442624],"genre_scores_gemma":[0.99953854,0.0000402697,0.00015095227,0.0000064670303,6.769441e-7,0.0000021319333,0.000048240756,0.0000042073666,0.00020854153],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998627,0.000021663462,0.00000749821,0.000023137736,0.00002575339,0.00005929392],"domain_scores_gemma":[0.9997646,0.00006367319,0.000032293927,0.000014917933,0.000065982655,0.00005843298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001777509,0.0004802217,0.00028234132,0.0005983733,0.0011603041,0.0012965951,0.000742332,0.00074975117,0.0019213898],"category_scores_gemma":[0.00071766856,0.00023170718,0.0005847252,0.000635191,0.00090110366,0.00038308505,0.0005923895,0.0003721013,0.000106009844],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015922193,0.000089158566,0.10025205,0.000060429626,0.000071708455,0.0003992092,0.00022113284,0.8825038,0.009710411,0.0011678542,0.00032488428,0.0050401],"study_design_scores_gemma":[0.000099127144,0.00008072472,0.08157495,0.000022749873,0.000045475994,0.00007437589,0.00073120114,0.9140143,0.00213202,0.00051615876,0.00066099415,0.000047994585],"about_ca_topic_score_codex":0.7555337,"about_ca_topic_score_gemma":0.639019,"teacher_disagreement_score":0.2444663,"about_ca_system_score_codex":0.0074792253,"about_ca_system_score_gemma":0.00403668,"threshold_uncertainty_score":0.491812},"labels":[],"label_agreement":null},{"id":"W2553168182","doi":"10.1126/science.aag2583","title":"Fault activation by hydraulic fracturing in western Canada","year":2016,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":574,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; University of Calgary","keywords":"Hydraulic fracturing; Geology; Fault (geology); Petroleum engineering; Geotechnical engineering; Mining engineering; Seismology","score_opus":0.009402472416293231,"score_gpt":0.20361041264179347,"score_spread":0.19420794022550025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2553168182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91211236,0.00428751,0.0003317268,0.0084408615,0.00009774268,0.00005723889,0.0049970234,0.00008719602,0.06958832],"genre_scores_gemma":[0.9825716,0.0028736533,0.0003075933,0.0007357979,0.00001505601,0.00000911102,0.0010717795,0.00002089184,0.012394562],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974185,0.000009435023,0.000009966074,0.000027541311,0.00007353124,0.0001376354],"domain_scores_gemma":[0.9993537,0.000023213594,0.000065192726,0.000012645565,0.00037255484,0.00017277477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014380376,0.00023079965,0.00022266357,0.0014060028,0.003694292,0.0015372217,0.00051271956,0.00045574494,0.0041048676],"category_scores_gemma":[0.0005739472,0.00020408617,0.00020009682,0.0039371103,0.0010202418,0.00035595454,0.000853053,0.00051855994,0.00027837153],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043509484,0.00014681398,0.73587674,0.00053156965,0.0002020688,0.0042809225,0.01747524,0.0024160286,0.008359875,0.010658296,0.07371551,0.14590187],"study_design_scores_gemma":[0.00002640888,0.000031395943,0.9418673,0.00014726531,0.000047569996,0.00042673998,0.013942853,0.00064839015,0.0006490849,0.0007807344,0.04137865,0.000053665663],"about_ca_topic_score_codex":0.9987203,"about_ca_topic_score_gemma":0.99963164,"teacher_disagreement_score":0.043610875,"about_ca_system_score_codex":0.043610875,"about_ca_system_score_gemma":0.05154708,"threshold_uncertainty_score":0.3164205},"labels":[],"label_agreement":null},{"id":"W2557168806","doi":"10.1002/2016jb013534","title":"Advanced seismic imaging techniques characterize the Alpine Fault at Whataroa (New Zealand)","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"University of Alberta; German-Israeli Foundation for Scientific Research and Development; University of Otago","keywords":"Geology; Seismology; Fault (geology); Basement; Borehole; Reflector (photography); Reflection (computer programming); Drilling; Paleontology","score_opus":0.02895352837546385,"score_gpt":0.30713471931117325,"score_spread":0.2781811909357094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2557168806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938524,0.0001751765,0.001130253,0.000046286215,0.000004015761,0.000034560777,0.0008113639,0.000041417083,0.0039044742],"genre_scores_gemma":[0.9933295,0.0002066613,0.0035739657,0.000015832078,0.000005728674,0.00002138051,0.0007993097,0.000016505765,0.0020311696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990165,0.0000039677957,0.0000050379404,0.000024594852,0.000044084092,0.000020634447],"domain_scores_gemma":[0.99981564,0.000013581813,0.00006476518,0.000010765699,0.00006955397,0.000025741574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014594744,0.00029346094,0.00011909262,0.0014845338,0.00023903439,0.00057560555,0.00025629363,0.00027568042,0.001913385],"category_scores_gemma":[0.0004355118,0.00020029972,0.00013390332,0.0009344158,0.00023731377,0.00037801036,0.00033395115,0.00023625989,0.00033997514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032083425,0.0001547988,0.4446076,0.00024734304,0.00008227718,0.0010290678,0.002097391,0.0036330814,0.42448625,0.00039485178,0.0013737723,0.12157268],"study_design_scores_gemma":[0.00001598196,0.000043247735,0.99162793,0.000015284482,0.000014333652,0.00018725914,0.00040273648,0.0033326629,0.0025903,0.00003888362,0.0017222658,0.00000918907],"about_ca_topic_score_codex":0.14470936,"about_ca_topic_score_gemma":0.30987972,"teacher_disagreement_score":0.14470936,"about_ca_system_score_codex":0.00058195327,"about_ca_system_score_gemma":0.00037796568,"threshold_uncertainty_score":0.2877341},"labels":[],"label_agreement":null},{"id":"W2557223958","doi":"10.1038/srep36668","title":"Power-law rheology controls aftershock triggering and decay","year":2016,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Viscoelasticity; Rheology; Geology; Crust; Power law; Nonlinear system; Seismology; Geophysics; Statistical physics; Physics; Mathematics; Statistics; Thermodynamics","score_opus":0.01061365535015392,"score_gpt":0.20756710045482907,"score_spread":0.19695344510467516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2557223958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922637,0.000053582586,0.006639967,0.00002422545,0.0000028911384,0.000005519321,0.00003304009,0.00006321777,0.0009139142],"genre_scores_gemma":[0.999647,0.000027126987,0.00018171211,0.0000016426359,7.7070916e-7,0.0000012548942,0.000010016216,0.0000037784496,0.00012664661],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999583,0.0000069801167,0.0000026111088,0.000014561526,0.000005671197,0.000011796467],"domain_scores_gemma":[0.9996101,0.00012245211,0.00014152662,0.000051837815,0.000030835803,0.000043170097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011281437,0.00018034705,0.00018867347,0.0002735649,0.000096818774,0.00054975605,0.00017788468,0.00020158014,0.0010770634],"category_scores_gemma":[0.0012911969,0.00012447758,0.00013876376,0.0001334527,0.00028797812,0.0004136141,0.00021547882,0.00017689401,0.00021485148],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004843676,0.00023155259,0.15618438,0.0001704323,0.00017494668,0.0011789608,0.0006984732,0.23334962,0.55504096,0.016227046,0.0005203608,0.035739005],"study_design_scores_gemma":[0.000020589818,0.00017822154,0.10367358,0.0000103673,0.000046587425,0.00026253794,0.0001339867,0.86827207,0.020860655,0.006077586,0.0004356988,0.000028240322],"about_ca_topic_score_codex":0.001084261,"about_ca_topic_score_gemma":0.0006766191,"teacher_disagreement_score":0.001084261,"about_ca_system_score_codex":0.00019816776,"about_ca_system_score_gemma":0.00016212912,"threshold_uncertainty_score":0.0036031008},"labels":[],"label_agreement":null},{"id":"W2560145442","doi":"10.1139/cjes-2016-0111","title":"Focal depth distribution of the 1982 Miramichi earthquake sequence determined by modelling depth phases","year":2016,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Geology; Seismology; Foreshock; Magnitude (astronomy); Focal mechanism; Geodesy; Tectonics","score_opus":0.04261974297062024,"score_gpt":0.2346072955795724,"score_spread":0.19198755260895217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560145442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961241,0.000070786,0.00087870704,0.0000075473677,0.0000011053216,0.000008075319,0.000967483,0.00004002607,0.001902165],"genre_scores_gemma":[0.99702555,0.000049726837,0.0009309554,0.0000021863748,9.852714e-7,0.000008755964,0.0015521169,0.0000057935677,0.0004239581],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999946,0.0000036386846,0.0000025353322,0.000017221017,0.00001353104,0.0000170705],"domain_scores_gemma":[0.99987006,0.000014622513,0.00003167488,0.000008918264,0.000051114253,0.00002348695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000096353935,0.00027516656,0.00014249243,0.00080610014,0.00014120694,0.00026002424,0.00027334585,0.00016428316,0.0008266396],"category_scores_gemma":[0.00058454403,0.00016386514,0.00011533894,0.0007970185,0.000080092665,0.00013720253,0.00025110657,0.00007902688,0.00021999281],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005694806,0.00006253886,0.8312263,0.000094050054,0.000070833106,0.00045572332,0.00063485396,0.071163535,0.027086722,0.0005522312,0.0013269174,0.06675675],"study_design_scores_gemma":[0.000015375173,0.00004959552,0.9375476,0.000008354492,0.000024371655,0.00008523613,0.00019681292,0.058329336,0.0024184384,0.000056143163,0.001257428,0.0000112980215],"about_ca_topic_score_codex":0.15616734,"about_ca_topic_score_gemma":0.19075899,"teacher_disagreement_score":0.15616734,"about_ca_system_score_codex":0.0009243724,"about_ca_system_score_gemma":0.00031118136,"threshold_uncertainty_score":0.31051666},"labels":[],"label_agreement":null},{"id":"W2560560141","doi":"10.1002/2016jb013123","title":"3‐D velocity structure in southern Haiti from local earthquake tomography","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; U.S. Geological Survey; Institut de Physique du Globe de Paris; Centre National de la Recherche Scientifique; Institut Français de Recherche pour l'Exploitation de la Mer","keywords":"Geology; Seismology; Aftershock; Hypocenter; Fault (geology); Submarine pipeline; Structural basin; Peninsula; Seismometer; Seismic tomography; Geomorphology; Induced seismicity; Paleontology; Oceanography; Geography","score_opus":0.028215322223662815,"score_gpt":0.28475677498635843,"score_spread":0.25654145276269563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560560141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984471,0.000026843685,0.0005429759,0.000022708362,0.0000013819533,0.000007537273,0.00027261305,0.00003233702,0.00064648234],"genre_scores_gemma":[0.99860114,0.000027471768,0.0006898615,0.0000054105953,0.0000019681881,0.000005500068,0.0004560417,0.000004594659,0.00020799773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999962,0.0000035846324,0.0000023547368,0.000011168808,0.000009943003,0.000010982572],"domain_scores_gemma":[0.9998727,0.000016381104,0.000040237934,0.000010791086,0.00004221969,0.000017606686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010118916,0.0002504569,0.000118310694,0.0009693948,0.00023607704,0.00051849097,0.00022669682,0.00023915566,0.00061798265],"category_scores_gemma":[0.00040457945,0.00018699729,0.00015718292,0.0009168368,0.0002459236,0.00024284355,0.00031960098,0.00017335858,0.0001506217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028402734,0.00014004036,0.89101964,0.00009003145,0.000110749024,0.0011449546,0.0014256012,0.019244207,0.049341,0.0005036191,0.00075988716,0.035936248],"study_design_scores_gemma":[0.0000134980255,0.00003108968,0.96512026,0.00001428121,0.000036576632,0.00022886923,0.00056470756,0.030691124,0.0025950489,0.00006095417,0.0006270524,0.00001658888],"about_ca_topic_score_codex":0.054769643,"about_ca_topic_score_gemma":0.13344266,"teacher_disagreement_score":0.054769643,"about_ca_system_score_codex":0.00040533434,"about_ca_system_score_gemma":0.0005419907,"threshold_uncertainty_score":0.10890168},"labels":[],"label_agreement":null},{"id":"W2560600136","doi":"10.1002/2016jb013570","title":"A seismological overview of the induced earthquakes in the Duvernay play near Fox Creek, Alberta","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":189,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Alberta","funders":"","keywords":"Geology; Seismology; Hydraulic fracturing; Induced seismicity; Lineament; Focal mechanism; Precambrian; Stress field; Basement; Fault (geology); Paleontology; Tectonics; Geography","score_opus":0.10442221959556322,"score_gpt":0.3443423533590797,"score_spread":0.23992013376351648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2560600136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98057556,0.0018311098,0.0006139158,0.00017701383,0.000008288029,0.00004773959,0.0026666776,0.00004394719,0.014035776],"genre_scores_gemma":[0.99162185,0.001470501,0.00075014716,0.00003745774,0.0000089085825,0.000009417185,0.0013007885,0.0000066348584,0.004794442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987066,0.0000067913807,0.000006035473,0.00001916179,0.00006136294,0.00003587043],"domain_scores_gemma":[0.9996854,0.000031080996,0.00005087223,0.0000086424625,0.0001655523,0.000058468653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001630542,0.00021208102,0.00013630408,0.0034502132,0.00086883287,0.00085834344,0.00041616333,0.00016096597,0.0014983916],"category_scores_gemma":[0.00035022717,0.00010467805,0.000088994246,0.0037780113,0.00042261402,0.00012578937,0.00039630913,0.000118626434,0.00014118674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000113199676,0.000042414104,0.9101196,0.00018648757,0.00005518237,0.0010054399,0.004594866,0.002569151,0.012686815,0.0011065817,0.0019347287,0.06558559],"study_design_scores_gemma":[0.0000014430843,0.000012803778,0.99301296,0.000017378217,0.000008489465,0.000100877936,0.0015969484,0.0004324739,0.0002894837,0.000043279695,0.004478336,0.0000056662097],"about_ca_topic_score_codex":0.92652845,"about_ca_topic_score_gemma":0.9812531,"teacher_disagreement_score":0.073471546,"about_ca_system_score_codex":0.006067927,"about_ca_system_score_gemma":0.0042216014,"threshold_uncertainty_score":0.14780843},"labels":[],"label_agreement":null},{"id":"W2561816591","doi":"10.1201/9781315388502-18","title":"Tensor variate normal distribution for stress variability analysis","year":2016,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Random variate; Stress (linguistics); Tensor (intrinsic definition); Normal distribution; Cauchy stress tensor; Distribution (mathematics); Computer science; Mathematics; Statistics; Geometry; Mathematical analysis; Random variable","score_opus":0.012727303806980016,"score_gpt":0.2155721754623067,"score_spread":0.2028448716553267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2561816591","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0051092175,0.00010701972,0.99307245,0.000048932292,0.000031694337,0.000017817374,0.00037626817,0.00058255874,0.000654133],"genre_scores_gemma":[0.4444398,0.0010703376,0.5334069,0.0000996535,0.00037447037,0.00034187833,0.004052726,0.0016467115,0.014567589],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995803,0.00016077873,0.000027944961,0.00007427795,0.00012105883,0.000035595338],"domain_scores_gemma":[0.99745876,0.0011986855,0.00021496115,0.0004940225,0.00053224305,0.00010135818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013424321,0.00055296754,0.0005588495,0.0013890339,0.00033929807,0.0008685324,0.00072579103,0.00042286306,0.0037032375],"category_scores_gemma":[0.006271225,0.00028663207,0.0005691607,0.0018473011,0.00049156864,0.0012058751,0.0006667868,0.0010210712,0.0017140002],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002167822,0.00011919708,0.005484577,0.00012731626,0.00011689238,0.00023638256,0.0001358967,0.36701235,0.014878989,0.26002198,0.0130422115,0.33860752],"study_design_scores_gemma":[0.0000035074577,0.000010899499,0.0009274002,0.0000050190292,0.000006293424,0.000058406255,0.000013464913,0.9605434,0.0006603791,0.035000846,0.0027582531,0.000012178325],"about_ca_topic_score_codex":0.005611909,"about_ca_topic_score_gemma":0.0032398491,"teacher_disagreement_score":0.005611909,"about_ca_system_score_codex":0.00038497537,"about_ca_system_score_gemma":0.00080291677,"threshold_uncertainty_score":0.012388587},"labels":[],"label_agreement":null},{"id":"W2563807909","doi":"","title":"Episodic slow slip events in a non-planar subduction fault model for northern Cascadia","year":2014,"lang":"en","type":"article","venue":"2014 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Subduction; Geology; Episodic tremor and slip; Seismology; Slip (aerodynamics); Tectonics","score_opus":0.015635844098770352,"score_gpt":0.22129828100989185,"score_spread":0.2056624369111215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2563807909","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99654824,0.00005143506,0.0005029177,0.00035985123,0.000018112592,0.000009610575,0.0005667211,0.000101591635,0.0018415581],"genre_scores_gemma":[0.9986714,0.00003885584,0.00019188764,0.000018684921,0.000008024544,0.0000072696075,0.00034960386,0.000027484812,0.0006869126],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998692,0.000036088775,0.000010416122,0.00004352224,0.000011138245,0.000029666742],"domain_scores_gemma":[0.99957496,0.00011566499,0.000042462845,0.000053279644,0.000058680314,0.00015499502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041443697,0.0006392517,0.0008321203,0.00052399817,0.0008871944,0.0012519713,0.002056014,0.0020201048,0.004847866],"category_scores_gemma":[0.0014302016,0.00073591917,0.0008764134,0.00061995327,0.0010211874,0.0006521664,0.0008444441,0.0010940884,0.00038072022],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002118266,0.00009647715,0.016702475,0.000021477337,0.00006447379,0.00024069367,0.00011805035,0.9792901,0.00056390424,0.0009947695,0.00078965555,0.0009061353],"study_design_scores_gemma":[0.000100606914,0.00004205523,0.008792365,0.000005923308,0.000026990841,0.000020005087,0.00008917444,0.9902384,0.00006685638,0.0003900827,0.0002118771,0.000015672984],"about_ca_topic_score_codex":0.2182535,"about_ca_topic_score_gemma":0.14464188,"teacher_disagreement_score":0.7817465,"about_ca_system_score_codex":0.0026538544,"about_ca_system_score_gemma":0.0017843735,"threshold_uncertainty_score":0.43396622},"labels":[],"label_agreement":null},{"id":"W2565143487","doi":"10.1002/2016jc012170","title":"A new real‐time tsunami detection algorithm","year":2016,"lang":"en","type":"article","venue":"Journal of Geophysical Research Oceans","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration","keywords":"Algorithm; Warning system; Computer science; Underwater; Reliability (semiconductor); Real-time computing; Geology; Telecommunications","score_opus":0.028854404393378583,"score_gpt":0.29459675237838345,"score_spread":0.26574234798500485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2565143487","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009184299,0.00010604798,0.9885628,0.0000629764,0.000066968,0.00004491138,0.000051822248,0.0011912948,0.00072888634],"genre_scores_gemma":[0.12023209,0.00010053825,0.8756435,0.00010754379,0.000080981605,0.00014358063,0.0003240222,0.0001054074,0.0032623345],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99898857,0.00011403257,0.00009315148,0.00030526915,0.00041145072,0.00008748886],"domain_scores_gemma":[0.9978331,0.00067151076,0.00020132205,0.00024361366,0.0009653631,0.00008514576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010722787,0.00073922524,0.00090653385,0.0015874819,0.00046321916,0.0014037999,0.001785841,0.0012541136,0.003131744],"category_scores_gemma":[0.002998755,0.00050435564,0.0005790813,0.0010006222,0.00050727284,0.001729752,0.00095273176,0.0010927665,0.0014464924],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047056918,0.00021754259,0.0018907,0.00012699098,0.000105016195,0.00012239958,0.00008820147,0.2218412,0.04465737,0.0095383,0.0039712116,0.7169705],"study_design_scores_gemma":[0.000038173635,0.000040134943,0.00030891216,0.0000054585516,0.0000108509175,0.00008422916,0.0000046135488,0.9911164,0.0052827406,0.0011680342,0.0019263946,0.0000139881195],"about_ca_topic_score_codex":0.0038170153,"about_ca_topic_score_gemma":0.0024765558,"teacher_disagreement_score":0.0038170153,"about_ca_system_score_codex":0.0007510058,"about_ca_system_score_gemma":0.0012329903,"threshold_uncertainty_score":0.010476768},"labels":[],"label_agreement":null},{"id":"W2565701990","doi":"10.1002/2016gc006489","title":"Variations in slow slip moment rate associated with rapid tremor reversals in <scp>C</scp>ascadia","year":2016,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Slip (aerodynamics); Geology; Episodic tremor and slip; Seismology; Seismic moment; Borehole; Strain rate; Geodesy; Moment magnitude scale; Subduction; Geotechnical engineering; Geometry; Tectonics; Physics; Materials science; Mathematics; Composite material","score_opus":0.010223117184705244,"score_gpt":0.18397066960887937,"score_spread":0.1737475524241741,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2565701990","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99890876,0.000010083847,0.000052908694,0.000010890404,0.0000011912667,0.0000037195841,0.0004355464,0.000015123319,0.00056186115],"genre_scores_gemma":[0.99927753,0.0000073419574,0.000054619388,0.0000030869417,0.0000018320844,0.0000024500478,0.0005171953,0.000003082194,0.00013289781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987364,0.000009070824,0.000008819901,0.00002806396,0.000048985974,0.00003137217],"domain_scores_gemma":[0.9993117,0.00006327627,0.00025699235,0.000040630228,0.0001747097,0.0001527149],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015264486,0.0001594965,0.00018932257,0.0014127056,0.00035131318,0.00047753553,0.00014913411,0.00021774218,0.0010893657],"category_scores_gemma":[0.0008737414,0.00012845511,0.000104644314,0.0009853475,0.00027047787,0.00010911322,0.0002355004,0.00023257261,0.00027804263],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022318364,0.00005184552,0.9584987,0.000026091851,0.00004659487,0.00032876935,0.0004177739,0.00122601,0.031248476,0.000077941506,0.0006709543,0.007183695],"study_design_scores_gemma":[0.0000016923917,0.000011823281,0.9989229,0.0000011274427,0.0000021002563,0.000031834057,0.000050629118,0.0005044104,0.00031711202,0.0000068808886,0.0001470475,0.0000023653959],"about_ca_topic_score_codex":0.04998939,"about_ca_topic_score_gemma":0.07961543,"teacher_disagreement_score":0.04998939,"about_ca_system_score_codex":0.0007353524,"about_ca_system_score_gemma":0.00031557315,"threshold_uncertainty_score":0.099396884},"labels":[],"label_agreement":null},{"id":"W2567699116","doi":"10.1016/j.jsg.2016.12.010","title":"Significance of first-order faults in folding mechanically isotropic layers: Evidence from the Sudbury Basin, Canada","year":2016,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Fold (higher-order function); Slip (aerodynamics); Geometry; Anisotropy; Petrology; Isotropy; Crust; Brittleness; Fault (geology); Structural basin; Kinematics; Echelon formation; Seismology; Geophysics; Geomorphology; Composite material; Materials science","score_opus":0.017528589591104135,"score_gpt":0.21934685665837103,"score_spread":0.2018182670672669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2567699116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99365,0.00036413295,0.000101142025,0.00013555652,0.0000045330435,0.000016786593,0.0007238417,0.0000053690896,0.0049985107],"genre_scores_gemma":[0.9983494,0.0002502388,0.000177863,0.0000309561,0.0000020224777,0.0000057273946,0.00034050198,0.0000042809647,0.0008389524],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993765,0.000047203594,0.00003376308,0.00010735995,0.00016993772,0.00026532798],"domain_scores_gemma":[0.9969188,0.00031234967,0.00048469214,0.000117738695,0.0018383212,0.00032808504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045109214,0.00034545123,0.00048643758,0.0029870167,0.0048731114,0.002920963,0.0012160821,0.00047276515,0.0032938279],"category_scores_gemma":[0.0031172733,0.00036125068,0.0002459316,0.005586499,0.0021394335,0.00054255896,0.0011664401,0.00050902646,0.00024951712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016042581,0.00004198033,0.97086024,0.000079020436,0.000082154234,0.00034652953,0.0047495537,0.00051441335,0.0031456705,0.0009157318,0.00074995746,0.018354312],"study_design_scores_gemma":[0.0000065481495,0.0000050963204,0.9963911,0.000031397383,0.000016000911,0.00004512182,0.0023524358,0.00017265714,0.00015523049,0.00006294211,0.00075341616,0.000007999582],"about_ca_topic_score_codex":0.9941444,"about_ca_topic_score_gemma":0.99852705,"teacher_disagreement_score":0.015615142,"about_ca_system_score_codex":0.015615142,"about_ca_system_score_gemma":0.017607499,"threshold_uncertainty_score":0.11329633},"labels":[],"label_agreement":null},{"id":"W2572328258","doi":"10.1038/ncomms14044","title":"Large fault slip peaking at trench in the 2011 Tohoku-oki earthquake","year":2017,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Trench; Slip (aerodynamics); Seismology; Episodic tremor and slip; Geology; Subduction; Bathymetry; Seismic gap; Fault (geology); Tectonics; Materials science","score_opus":0.038385787775467146,"score_gpt":0.29583271911841,"score_spread":0.2574469313429429,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2572328258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992611,0.000023583063,0.000092470036,0.000029541898,0.0000034017646,0.0000023071202,0.00007861328,0.000009519799,0.00049952825],"genre_scores_gemma":[0.99961436,0.000022979855,0.0000564593,0.0000073501637,0.0000017795065,0.0000019727233,0.00009295258,0.00000331392,0.00019875227],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991727,0.0000074453255,0.0000035406922,0.000023999428,0.00001099082,0.000036780784],"domain_scores_gemma":[0.9999025,0.000015350384,0.000020660082,0.000008982777,0.000016214011,0.00003633521],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015405298,0.0003277958,0.00037793865,0.00036160625,0.00063590566,0.0006923322,0.00040234215,0.0007041962,0.0010176285],"category_scores_gemma":[0.00036806715,0.0003323862,0.00039791348,0.00046547744,0.0004769883,0.00046369425,0.000734541,0.00032369685,0.00010694761],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028688484,0.0002512237,0.35210505,0.000091735536,0.00021134024,0.0011694876,0.0005622796,0.63072443,0.005774168,0.001163583,0.0011689848,0.0064908084],"study_design_scores_gemma":[0.00004800812,0.00015796025,0.473131,0.000023439166,0.000102959464,0.00009323709,0.0008862927,0.5238979,0.000720988,0.0003569388,0.00051320373,0.000068099245],"about_ca_topic_score_codex":0.09054539,"about_ca_topic_score_gemma":0.17104568,"teacher_disagreement_score":0.09054539,"about_ca_system_score_codex":0.001411377,"about_ca_system_score_gemma":0.0009258355,"threshold_uncertainty_score":0.18003672},"labels":[],"label_agreement":null},{"id":"W2575768900","doi":"10.1002/2016jb013405","title":"On corner frequencies, attenuation, and low‐frequency earthquakes","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Attenuation; Geology; Seismology; Seismogram; Frequency band; Saturation (graph theory); Anelastic attenuation factor; Physics; Geodesy; Optics; Mathematics; Bandwidth (computing); Telecommunications","score_opus":0.05683777357723818,"score_gpt":0.3289944415736522,"score_spread":0.272156667996414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2575768900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8919513,0.0079837935,0.087865,0.0003364128,0.000023967741,0.000025402136,0.0002772915,0.00012263954,0.011414236],"genre_scores_gemma":[0.99433494,0.0014422501,0.003378693,0.00003009702,0.000033881777,0.000005578476,0.00008787468,0.000015874119,0.0006708704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999634,0.00008725599,0.000021019709,0.00007554337,0.00014976187,0.000032397573],"domain_scores_gemma":[0.99134266,0.0065121395,0.00095665856,0.00032602725,0.00075599726,0.00010657321],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013119733,0.00026971873,0.0003311157,0.002091998,0.00021681118,0.0007279536,0.00045785375,0.00039279336,0.0013935148],"category_scores_gemma":[0.009526777,0.00019314833,0.00013274237,0.0017481262,0.0012432608,0.0009195357,0.00067281816,0.0004138107,0.00021071383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063977356,0.000074185016,0.4678002,0.001189227,0.00017406775,0.0020458337,0.003196332,0.072870195,0.05419889,0.074701495,0.001693721,0.32141602],"study_design_scores_gemma":[0.0000125143015,0.00016839246,0.8297004,0.00030137302,0.00007542449,0.00094381324,0.0010563293,0.08694198,0.013886109,0.05880124,0.008005419,0.00010702156],"about_ca_topic_score_codex":0.009112414,"about_ca_topic_score_gemma":0.008831601,"teacher_disagreement_score":0.009112414,"about_ca_system_score_codex":0.00071124866,"about_ca_system_score_gemma":0.00019623783,"threshold_uncertainty_score":0.01811874},"labels":[],"label_agreement":null},{"id":"W2577471140","doi":"","title":"Algorithms for Tsunami Detection by High Frequency Radar : Development and Case Studies for Tsunami Impact in British Columbia, Canada","year":2016,"lang":"en","type":"article","venue":"Journal of Media Literacy Education","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society","funders":"","keywords":"Radar; Geology; Remote sensing; Seismology; Geography; Computer science; Telecommunications","score_opus":0.01182850691062149,"score_gpt":0.2604280209903009,"score_spread":0.2485995140796794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2577471140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.794843,0.0023662203,0.18187915,0.00079026964,0.00006642972,0.00081316725,0.0014543768,0.002139452,0.015647884],"genre_scores_gemma":[0.8151994,0.0012283841,0.17352635,0.00011186852,0.000012817395,0.00013806029,0.0015508073,0.00011389796,0.008118453],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993704,0.00007527128,0.000044220888,0.00009993683,0.00027600734,0.00013417928],"domain_scores_gemma":[0.9980205,0.0004016489,0.00005935346,0.000053264917,0.0013968798,0.0000683231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010656776,0.0007943976,0.0003833601,0.0012324532,0.000876887,0.0014992459,0.0011955787,0.000572596,0.0013911772],"category_scores_gemma":[0.003470242,0.00021516206,0.0002748375,0.0019919814,0.00043390418,0.00039584073,0.0003792497,0.00037554957,0.00028708827],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000354444,0.00021919474,0.043589044,0.00020035067,0.00009849307,0.000473383,0.00032193033,0.5244335,0.0071584303,0.0026626235,0.0057792026,0.41470948],"study_design_scores_gemma":[0.000060988445,0.000043659817,0.014158219,0.00001871262,0.000033669134,0.00008487133,0.0002853303,0.97941726,0.0028548297,0.00029451906,0.0027237146,0.000024231502],"about_ca_topic_score_codex":0.94858176,"about_ca_topic_score_gemma":0.93133986,"teacher_disagreement_score":0.051418245,"about_ca_system_score_codex":0.008783562,"about_ca_system_score_gemma":0.008678348,"threshold_uncertainty_score":0.10344207},"labels":[],"label_agreement":null},{"id":"W2578986756","doi":"10.1002/2016ja023727","title":"GPS detection of ionospheric Rayleigh wave and its source following the 2012 Haida Gwaii earthquake","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Space Physics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Ionosphere; Total electron content; Geodesy; Rayleigh wave; Seismology; Amplitude; Epicenter; Waveform; TEC; Geophysics; Surface wave; Physics; Optics","score_opus":0.05554248313358498,"score_gpt":0.3010675648786206,"score_spread":0.2455250817450356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2578986756","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949884,0.000014832325,0.000055840646,0.000007814379,0.0000021404906,0.00000232698,0.000089097804,0.0000039798565,0.00032521045],"genre_scores_gemma":[0.9995578,0.000019225687,0.00007806582,0.000002559653,0.0000015854582,0.0000017576323,0.0001947419,6.128947e-7,0.00014366613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999471,0.000004113379,0.0000026149046,0.0000123101945,0.000017215894,0.000016740505],"domain_scores_gemma":[0.9998826,0.000008082416,0.000038721188,0.000007965142,0.000035526933,0.000027147793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006282171,0.00017493771,0.00015275406,0.00040486435,0.00019040825,0.00024082052,0.00014160687,0.00017055243,0.00029304938],"category_scores_gemma":[0.00031073432,0.00009687317,0.00006894369,0.0004589151,0.00016750014,0.00009117792,0.0002470015,0.00015299635,0.00007124066],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028381162,0.0000474628,0.9461729,0.000029510316,0.00003957826,0.00058619166,0.0006508397,0.0014850067,0.033718728,0.00008172293,0.00046584688,0.016438372],"study_design_scores_gemma":[0.0000040503487,0.000023580244,0.9981065,0.00000258033,0.000008665444,0.000042266834,0.00013915099,0.00090171216,0.0005953605,0.0000064172095,0.0001669753,0.0000028544682],"about_ca_topic_score_codex":0.07240511,"about_ca_topic_score_gemma":0.13690369,"teacher_disagreement_score":0.07240511,"about_ca_system_score_codex":0.00039235957,"about_ca_system_score_gemma":0.00033063782,"threshold_uncertainty_score":0.14396733},"labels":[],"label_agreement":null},{"id":"W2581362683","doi":"","title":"A Hybrid FLAC3D-PFC3D Model to Study the Microseismic Response of Caprock","year":2015,"lang":"en","type":"article","venue":"13th ISRM International Congress of Rock Mechanics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Caprock; Geology; Microseism; Seismology; Geotechnical engineering","score_opus":0.04509666096389526,"score_gpt":0.27568338342357074,"score_spread":0.23058672245967549,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2581362683","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46524566,0.0013234793,0.38846233,0.0016251331,0.00074671436,0.00035317443,0.011381519,0.0057059755,0.12515603],"genre_scores_gemma":[0.9601674,0.00033014457,0.02596959,0.00022780766,0.00008644971,0.00024262628,0.0021140475,0.00032480736,0.010537147],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998865,0.000017489232,0.0000068250565,0.000023039795,0.0000380314,0.000028078188],"domain_scores_gemma":[0.9997348,0.0000726343,0.000024892672,0.000032163076,0.00008868526,0.000046787853],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001742201,0.00077045505,0.0007552501,0.0006241704,0.0006937089,0.0010768053,0.0023262592,0.003064423,0.010233618],"category_scores_gemma":[0.0005712177,0.00051733904,0.00087086024,0.0007113378,0.00050216366,0.00060422346,0.000771316,0.00073285593,0.0010764904],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033602846,0.000036932193,0.00085224956,0.00003913833,0.00001741005,0.00012018629,0.000028028207,0.99236155,0.0014457221,0.0011339496,0.0009353265,0.002995829],"study_design_scores_gemma":[0.000012681338,0.000008371483,0.00028811302,0.0000049862238,0.0000048609636,0.000014995473,0.000013254664,0.9985802,0.00014526481,0.00021097966,0.00070845964,0.000007782599],"about_ca_topic_score_codex":0.053657833,"about_ca_topic_score_gemma":0.032267585,"teacher_disagreement_score":0.053657833,"about_ca_system_score_codex":0.0006355791,"about_ca_system_score_gemma":0.0015846736,"threshold_uncertainty_score":0.106691},"labels":[],"label_agreement":null},{"id":"W2582378202","doi":"","title":"How fault zones impact regional permeability and groundwater systems: insights from global database of fault zone studies.","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Groundwater; Database; Permeability (electromagnetism); Computer science; Geotechnical engineering","score_opus":0.033052667376878,"score_gpt":0.25592823555161076,"score_spread":0.22287556817473275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2582378202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.956998,0.003252108,0.0011678188,0.0012210534,0.000012755261,0.000010133909,0.034838352,0.000038382288,0.0024613894],"genre_scores_gemma":[0.9871535,0.0017374312,0.0008558251,0.00007905303,0.00000668503,0.0000070506517,0.009973148,0.000017061824,0.0001703372],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99956495,0.00015164062,0.000054035983,0.00010858392,0.00006524408,0.00005550204],"domain_scores_gemma":[0.996711,0.0014950271,0.00096522155,0.00032834403,0.00034171564,0.00015867765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009445673,0.00017773277,0.0003058865,0.002066466,0.00016717959,0.0011756574,0.0003516789,0.00026508517,0.0011059796],"category_scores_gemma":[0.005815985,0.00012149124,0.0003302308,0.00635729,0.0002743788,0.0012496135,0.0008820918,0.00028109318,0.000219513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009980007,0.00002393464,0.9609468,0.00016666952,0.00051413133,0.000087311964,0.0006843637,0.0022353292,0.0010824727,0.0009537608,0.0037820854,0.02942332],"study_design_scores_gemma":[0.00000763611,0.000022580558,0.9925296,0.00005438,0.0002320646,0.000075715616,0.0011556356,0.0011032359,0.00023175718,0.0009460062,0.0036315601,0.000009809505],"about_ca_topic_score_codex":0.036088876,"about_ca_topic_score_gemma":0.06919066,"teacher_disagreement_score":0.036088876,"about_ca_system_score_codex":0.00041716147,"about_ca_system_score_gemma":0.00057898834,"threshold_uncertainty_score":0.071757674},"labels":[],"label_agreement":null},{"id":"W2584389507","doi":"10.1007/s00015-017-0262-7","title":"The 1905 Chamonix earthquakes: active tectonics in the Mont Blanc and Aiguilles Rouges massifs","year":2017,"lang":"en","type":"article","venue":"Swiss Journal of Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centre For Cold Ocean Resources Engineering","funders":"","keywords":"Seismology; Geology; Massif; Tectonics; Fault (geology); Seismic hazard; Paleontology","score_opus":0.02012615494917037,"score_gpt":0.25165246945374053,"score_spread":0.23152631450457017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2584389507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976991,0.00023169888,0.00006657025,0.00006635043,0.0000026940259,0.0000045363313,0.0001608101,0.000008791526,0.0017594049],"genre_scores_gemma":[0.99928075,0.00007428756,0.00008771423,0.000009328236,0.000007959908,0.0000024111328,0.00023232817,0.0000014230881,0.00030371346],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998989,0.000015722087,0.0000036407764,0.000025745854,0.000027694568,0.000028290262],"domain_scores_gemma":[0.99975806,0.00003557675,0.00010651912,0.000013099831,0.000040655203,0.000046024812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002527189,0.00027712033,0.0001320868,0.0013769437,0.0005249645,0.00067089923,0.00018859774,0.00036953678,0.0015609828],"category_scores_gemma":[0.0004595071,0.00007469663,0.00011852073,0.0007835141,0.00047261405,0.00027720488,0.00032083614,0.00016384953,0.00016332993],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003089412,0.000061094834,0.95256084,0.000044017383,0.000058507405,0.00087954116,0.0024246739,0.0014535133,0.012609834,0.00059131143,0.00062768057,0.028379899],"study_design_scores_gemma":[0.0000016786933,0.00001600459,0.99904114,0.000002774571,0.0000022837958,0.000046217458,0.00014822488,0.00013874225,0.00007825292,0.000010596391,0.00051215006,0.0000019355023],"about_ca_topic_score_codex":0.15204157,"about_ca_topic_score_gemma":0.19668038,"teacher_disagreement_score":0.15204157,"about_ca_system_score_codex":0.0014888835,"about_ca_system_score_gemma":0.000431784,"threshold_uncertainty_score":0.30231315},"labels":[],"label_agreement":null},{"id":"W2586342266","doi":"10.1002/2016jb013430","title":"Deformation pattern during normal faulting: A sequential limit analysis","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"China Scholarship Council","keywords":"Geology; Echelon formation; Graben; Wedge (geometry); Fault (geology); Seismology; Detachment fault; Rotation (mathematics); Half-graben; Tectonics; Geometry","score_opus":0.0621319999010266,"score_gpt":0.34304792310465804,"score_spread":0.28091592320363146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2586342266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86251575,0.00026319228,0.12596042,0.00031368315,0.000019146011,0.000040724328,0.00018200674,0.00023347806,0.010471728],"genre_scores_gemma":[0.9950617,0.000082112274,0.0029490981,0.000012485123,0.0000075227276,0.000028805487,0.000038985905,0.000025060195,0.0017943112],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987483,0.00003594091,0.000008508106,0.000030277984,0.000029529696,0.00002085716],"domain_scores_gemma":[0.99971944,0.00009239792,0.000075182616,0.000026550624,0.00004087187,0.000045463956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045663206,0.0004424268,0.00046776547,0.0007687829,0.00040372874,0.0007583068,0.0010258798,0.00069658936,0.0021018232],"category_scores_gemma":[0.001140828,0.00037437014,0.0007436135,0.00046215532,0.0011405754,0.0007224948,0.000696464,0.00038110185,0.00017393213],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021424932,0.000022229782,0.00234643,0.000011993315,0.000014262121,0.0001139197,0.000036387595,0.9841739,0.0013613089,0.010134007,0.000094933624,0.0016691827],"study_design_scores_gemma":[0.000003877283,0.000007235854,0.00026073557,0.000001116978,0.000002697369,0.000011184602,0.0000035512421,0.99796593,0.00008731898,0.0015629624,0.000090840855,0.0000025116456],"about_ca_topic_score_codex":0.014331452,"about_ca_topic_score_gemma":0.0040801642,"teacher_disagreement_score":0.014331452,"about_ca_system_score_codex":0.0011020986,"about_ca_system_score_gemma":0.00053937297,"threshold_uncertainty_score":0.028496087},"labels":[],"label_agreement":null},{"id":"W2586978777","doi":"","title":"Comparing Biases of Fault Zone Permeability Magnitudes and Inferred Conceptual Models - Global Multidisciplinary Compilation and Mapping","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Multidisciplinary approach; Geology; Computer science; Political science","score_opus":0.12349476406365768,"score_gpt":0.28992839429683326,"score_spread":0.1664336302331756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2586978777","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9868933,0.000081792125,0.0055565652,0.00013918777,0.00001516096,0.000013474629,0.004094955,0.00027153242,0.0029339658],"genre_scores_gemma":[0.9871546,0.00007736332,0.0051940465,0.000043036183,0.000009996487,0.000020998736,0.007014016,0.000108437554,0.00037756833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99894637,0.00039026493,0.00007471195,0.00036045085,0.0001544166,0.000073836796],"domain_scores_gemma":[0.9906329,0.0044794576,0.001341207,0.0020435045,0.0013085465,0.0001943972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031132912,0.00038183772,0.0002532882,0.0018026626,0.00026712654,0.0010944001,0.0005593656,0.00044349465,0.0010607197],"category_scores_gemma":[0.01322302,0.000250166,0.00043644526,0.0017638501,0.0003928259,0.0015305644,0.0013440556,0.00031232476,0.0004088076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051561964,0.00017008034,0.8466112,0.00018557298,0.0006416384,0.00011047429,0.0026999512,0.040793415,0.008960502,0.002959282,0.0059749503,0.09037734],"study_design_scores_gemma":[0.000066324974,0.00005896844,0.9479528,0.00010161244,0.00028838293,0.00010160779,0.0013574567,0.036038514,0.006607081,0.0017514102,0.0056290617,0.000046797897],"about_ca_topic_score_codex":0.019217081,"about_ca_topic_score_gemma":0.026342075,"teacher_disagreement_score":0.019217081,"about_ca_system_score_codex":0.0005701323,"about_ca_system_score_gemma":0.0005703804,"threshold_uncertainty_score":0.03821045},"labels":[],"label_agreement":null},{"id":"W2587061311","doi":"10.1130/gsatg291a.1","title":"Quaternary Rupture of a Crustal Fault beneath Victoria, British Columbia, Canada","year":2017,"lang":"en","type":"article","venue":"GSA Today","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Quaternary; Seismology; Fault (geology); Archaeology; Paleontology; Geography","score_opus":0.009558714784589573,"score_gpt":0.19776556895090816,"score_spread":0.18820685416631858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2587061311","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98953056,0.00030574124,0.0001481292,0.00015642338,0.0000052147047,0.000016688438,0.0015716288,0.000022556944,0.008242984],"genre_scores_gemma":[0.9959019,0.00018989769,0.00020840712,0.00003695017,0.0000010002743,0.000004716037,0.0006112611,0.000004254202,0.0030417317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980074,0.000008702266,0.0000076245096,0.000050016897,0.00006873954,0.00006416695],"domain_scores_gemma":[0.9994615,0.000027698772,0.000052984084,0.000015825057,0.00032606843,0.00011586526],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013771214,0.00020044264,0.00015620726,0.0011962331,0.002597856,0.0013348337,0.00049506663,0.00032211852,0.0024416603],"category_scores_gemma":[0.0007057088,0.000174817,0.0000996861,0.002310006,0.0004975603,0.00023592856,0.0006088037,0.0003116582,0.00031604164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013653532,0.000060396695,0.9116665,0.00012570477,0.00006458951,0.0017563171,0.003896697,0.0019366045,0.012843206,0.0005618534,0.0052454593,0.061706115],"study_design_scores_gemma":[0.0000046863056,0.0000107566975,0.99169534,0.000032384145,0.000012895167,0.00012324966,0.0025561098,0.0012069424,0.0005783621,0.00004985691,0.003715982,0.000013424974],"about_ca_topic_score_codex":0.9909277,"about_ca_topic_score_gemma":0.99766016,"teacher_disagreement_score":0.012160176,"about_ca_system_score_codex":0.012160176,"about_ca_system_score_gemma":0.013040525,"threshold_uncertainty_score":0.0882287},"labels":[],"label_agreement":null},{"id":"W2587866114","doi":"10.1002/2017gl072538","title":"On factors controlling precursor slip fronts in the laboratory and their relation to slow slip events in nature","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Slip (aerodynamics); Nucleation; Asperity (geotechnical engineering); Materials science; Drop (telecommunication); Stress field; Standard deviation; Mechanics; Stress (linguistics); Geology; Slip line field; Composite material; Thermodynamics; Physics; Shear (geology)","score_opus":0.029732347309283445,"score_gpt":0.29365780601295693,"score_spread":0.2639254587036735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2587866114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991059,0.00015236402,0.00041741133,0.0000104367755,0.000002199581,0.000010416303,0.000046330384,0.0000075446915,0.0002473275],"genre_scores_gemma":[0.9993948,0.00006299719,0.00030707137,0.000008386002,0.0000025487477,0.000011587284,0.00006466991,0.0000035929597,0.00014440004],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99979,0.00003939436,0.000017521548,0.000048036363,0.000057930258,0.000047129364],"domain_scores_gemma":[0.9991715,0.00021836002,0.00032857782,0.000050287264,0.00013098471,0.000100189834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027611025,0.0001725222,0.0002428748,0.00040704833,0.00015052735,0.00047830044,0.00014521809,0.00020884405,0.00093500357],"category_scores_gemma":[0.0009820168,0.00014967575,0.00016063095,0.00018235078,0.00029863275,0.00030858538,0.00025660245,0.00035924948,0.0001304302],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021880321,0.00006767783,0.024825187,0.000038875227,0.000007985161,0.000104148756,0.000074615695,0.00023022937,0.97120494,0.00008550833,0.00003695605,0.0031050628],"study_design_scores_gemma":[0.000014572296,0.000834176,0.4522779,0.000013644245,0.000023530687,0.00025285644,0.00033292457,0.004795803,0.54034543,0.00014199715,0.00094321737,0.000023920442],"about_ca_topic_score_codex":0.0011031748,"about_ca_topic_score_gemma":0.0008825887,"teacher_disagreement_score":0.0011031748,"about_ca_system_score_codex":0.0003033101,"about_ca_system_score_gemma":0.00014693227,"threshold_uncertainty_score":0.0031279325},"labels":[],"label_agreement":null},{"id":"W2588492572","doi":"10.1007/s11069-017-2778-6","title":"Quantitative analysis of earthquake fatalities: case of Iran","year":2017,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Natural hazard; Seismology; Earthquake scenario; Geology; Forensic engineering; Seismic hazard; Engineering","score_opus":0.03953254724516147,"score_gpt":0.30557374615470045,"score_spread":0.266041198909539,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2588492572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964126,0.000106864885,0.0010784111,0.00010861663,0.000004389628,0.00001189616,0.0008033983,0.000016467002,0.0014573388],"genre_scores_gemma":[0.9991079,0.000050437946,0.00025193446,0.0000023639461,0.0000066313814,0.000003945804,0.0003813743,0.0000013285512,0.00019401261],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996753,0.00007991057,0.000023430119,0.000043626867,0.00008762735,0.00009016673],"domain_scores_gemma":[0.9983437,0.000705999,0.00037907282,0.00008642662,0.00039334464,0.00009144459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006453075,0.00023284883,0.00017382734,0.0033692713,0.0002964889,0.00042606122,0.00062901893,0.0003368285,0.0015119303],"category_scores_gemma":[0.0024491397,0.00010210494,0.00041024055,0.001955532,0.00034510132,0.0004065167,0.0002770469,0.00032941357,0.00012926632],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029650435,0.00026361787,0.8924251,0.00013101893,0.00017215661,0.0024310097,0.0010905154,0.06707237,0.001774688,0.0053802743,0.0026020345,0.026360624],"study_design_scores_gemma":[0.000011448299,0.00014871986,0.89072484,0.00001540775,0.00006701106,0.0011131293,0.003948562,0.10031362,0.0007073585,0.0013962808,0.0015223324,0.00003116556],"about_ca_topic_score_codex":0.036409684,"about_ca_topic_score_gemma":0.02681831,"teacher_disagreement_score":0.036409684,"about_ca_system_score_codex":0.0011312433,"about_ca_system_score_gemma":0.000568084,"threshold_uncertainty_score":0.0723955},"labels":[],"label_agreement":null},{"id":"W2588493932","doi":"","title":"Neotectonics and Paleoseismology of a Previously Unmapped Reverse Fault in Central Philippines―Insights from the Magnitude Mw 7.2 Bohol Earthquake of 15 October 2013","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Magnitude (astronomy); Seismology; Geology; Neotectonics; Fault (geology); Paleoseismology; Geography; Physics","score_opus":0.02310395154221781,"score_gpt":0.22264963492079456,"score_spread":0.19954568337857675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2588493932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971228,0.0001987506,0.00006620469,0.00009595162,0.0000025495583,0.0000033725112,0.00021650187,0.000005493754,0.002288358],"genre_scores_gemma":[0.99932086,0.00015189823,0.00007635921,0.000010693284,0.0000030319084,0.0000015209102,0.00014339911,0.0000028792826,0.00028939915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995244,0.0000070941555,0.0000038926555,0.000018072145,0.0000067620767,0.000011679598],"domain_scores_gemma":[0.9998072,0.000017350196,0.00007354482,0.000014538555,0.000059544833,0.000027848493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012584553,0.0001611633,0.00007618242,0.00090763014,0.00036360932,0.0005780457,0.0002321678,0.00019652357,0.0022646906],"category_scores_gemma":[0.00044150982,0.0001331808,0.00009258573,0.0012565049,0.00059743586,0.00048859476,0.0005119135,0.00023682011,0.00021392142],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021122087,0.000053272335,0.9127511,0.00013326375,0.000060875653,0.0010319919,0.014205774,0.0022661265,0.01171597,0.0016220455,0.00087941077,0.0550689],"study_design_scores_gemma":[0.0000022512124,0.000015730311,0.9953334,0.00001703883,0.000008007217,0.000124154,0.0017799807,0.00052831427,0.00017509353,0.00010030096,0.00190933,0.000006317639],"about_ca_topic_score_codex":0.066406175,"about_ca_topic_score_gemma":0.12611926,"teacher_disagreement_score":0.066406175,"about_ca_system_score_codex":0.0006630569,"about_ca_system_score_gemma":0.00041227313,"threshold_uncertainty_score":0.13203931},"labels":[],"label_agreement":null},{"id":"W2588651516","doi":"10.2113/econgeo.112.2.451","title":"Structural Controls on Fluid Flow During Compressional Reactivation of Basement Faults: Insights from Numerical Modeling for the Formation of Unconformity-Related Uranium Deposits in the Athabasca Basin, Canada","year":2017,"lang":"en","type":"article","venue":"Economic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Cameco (Canada); University of Regina","funders":"Natural Resources Canada; Cameco","keywords":"Geology; Unconformity; Fault (geology); Petrology; Fluid dynamics; Deformation (meteorology); Basement; Structural basin; Fluid pressure; Overpressure; Compression (physics); Geotechnical engineering; Seismology; Geomorphology; Mechanics","score_opus":0.014418688717710806,"score_gpt":0.20463733460969682,"score_spread":0.190218645891986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2588651516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99666214,0.0000481905,0.0007893345,0.00008595172,0.000004386098,0.000016028176,0.00018873806,0.000027183476,0.0021780594],"genre_scores_gemma":[0.99887234,0.000053210722,0.00048004196,0.000008700821,0.0000015738235,0.000009907373,0.00008938202,0.0000074647683,0.0004773756],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999095,0.000013232876,0.0000062475265,0.000019110084,0.00001736717,0.000034576842],"domain_scores_gemma":[0.9997962,0.00007702665,0.00003438615,0.000010839044,0.000042608805,0.000038805083],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013656543,0.00044456127,0.00034045224,0.00060471543,0.0010445302,0.0011603539,0.0009578924,0.0010223001,0.0012266764],"category_scores_gemma":[0.0007483181,0.0004138973,0.0005176224,0.0005792519,0.0011451882,0.0003725956,0.0005367407,0.00041717457,0.00009429108],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052259948,0.000067062414,0.017193267,0.000018285265,0.000019588062,0.00011974064,0.00009222076,0.9780985,0.00241026,0.00066744955,0.00009385992,0.0011675677],"study_design_scores_gemma":[0.000020911895,0.000013141722,0.0070292517,0.0000029950122,0.000007388829,0.000008821572,0.000081624916,0.99233246,0.00030238388,0.00010147958,0.00008918041,0.0000102587055],"about_ca_topic_score_codex":0.76525366,"about_ca_topic_score_gemma":0.5898774,"teacher_disagreement_score":0.23474634,"about_ca_system_score_codex":0.006730451,"about_ca_system_score_gemma":0.0043902057,"threshold_uncertainty_score":0.47225755},"labels":[],"label_agreement":null},{"id":"W2588723440","doi":"10.4236/ojer.2017.61001","title":"Late Stage Interseismic Strain Interval, Cascadia Subduction Zone Margin, USA and Canada","year":2017,"lang":"en","type":"article","venue":"Open Journal of Earthquake Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Subsidence; Seismology; Volcano; Pacific Plate; Margin (machine learning); Geomorphology; Tectonics","score_opus":0.09471183246253742,"score_gpt":0.34223280949395485,"score_spread":0.24752097703141743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2588723440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95084375,0.0009698608,0.0001228765,0.00032172972,0.000018016111,0.000040193765,0.03813374,0.00005247387,0.009497384],"genre_scores_gemma":[0.9702969,0.0010398835,0.00035563402,0.0000692872,0.000010271042,0.000038134225,0.020776382,0.000013310273,0.0074001024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998272,0.000007440666,0.000010956165,0.000047236455,0.00006433741,0.000042872627],"domain_scores_gemma":[0.99907815,0.000029345481,0.00013240833,0.000017851668,0.0005153656,0.00022687302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018354588,0.00033014643,0.0002013886,0.0022547366,0.0014614564,0.00073069136,0.00060132844,0.00020025867,0.0024797525],"category_scores_gemma":[0.0008470309,0.00016030124,0.00020627788,0.004642192,0.0003729741,0.0003268462,0.0005196812,0.00037721446,0.00033989522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007664023,0.000021949065,0.9845412,0.000055697805,0.00007139759,0.00019793025,0.0009571614,0.00025281715,0.00043897293,0.0002797022,0.006474521,0.0066319956],"study_design_scores_gemma":[0.0000022270224,0.0000029817397,0.99798393,0.000008935239,0.0000062366726,0.000020612557,0.00055671396,0.000051786563,0.000017167076,0.0000093101435,0.0013376607,0.0000024864569],"about_ca_topic_score_codex":0.9890899,"about_ca_topic_score_gemma":0.99728405,"teacher_disagreement_score":0.010910094,"about_ca_system_score_codex":0.010008333,"about_ca_system_score_gemma":0.010349698,"threshold_uncertainty_score":0.07261592},"labels":[],"label_agreement":null},{"id":"W2589638263","doi":"10.1002/2016gc006775","title":"Tectonic structure, evolution, and the nature of oceanic core complexes and their detachment fault zones (13°20′N and 13°30′N, Mid Atlantic Ridge)","year":2017,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Environment Research Council; Institut de Physique du Globe de Paris; Centre National de la Recherche Scientifique; Agence Nationale de la Recherche; GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel; Sight Research UK; Institut Français de Recherche pour l'Exploitation de la Mer; Alfred P. Sloan Foundation","keywords":"Geology; Detachment fault; Fault scarp; Slumping; Seafloor spreading; Fault (geology); Mass wasting; Seismology; Lithology; Strike-slip tectonics; Petrology; Transform fault; Extensional fault; Tectonics; Geomorphology; Geophysics; Rift; Landslide; Extensional definition","score_opus":0.008484559753990234,"score_gpt":0.20679404258891995,"score_spread":0.19830948283492972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2589638263","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99888223,0.000047457546,0.000029153716,0.000010100336,0.0000011367418,0.0000033166637,0.00020989976,0.0000032555643,0.0008132894],"genre_scores_gemma":[0.99922323,0.000027347995,0.00006159241,0.0000071281934,0.0000012713045,0.0000031320158,0.00039052556,0.0000026703258,0.00028307957],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999838,0.0000096991325,0.000010728449,0.000045511297,0.000040648953,0.000055394667],"domain_scores_gemma":[0.99934715,0.000037256927,0.00019577237,0.00003065855,0.00020312678,0.0001860281],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017449108,0.0001600297,0.00017451937,0.0011939313,0.00049608987,0.0007551526,0.00031254432,0.0002507061,0.0011377535],"category_scores_gemma":[0.0005138715,0.00017851539,0.00015572614,0.00095179846,0.00049408706,0.00021183446,0.00051499635,0.00017287658,0.00024746658],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030741754,0.000010928703,0.99327,0.000006406231,0.000020049709,0.000032339325,0.00019717729,0.00013691915,0.0038535995,0.00005788207,0.000107408516,0.0022766301],"study_design_scores_gemma":[6.6205666e-7,0.0000036438962,0.99963975,0.0000012154554,0.0000016310071,0.000011017853,0.00009262601,0.00009453031,0.00004906956,0.0000030413623,0.00010227501,6.4829976e-7],"about_ca_topic_score_codex":0.165001,"about_ca_topic_score_gemma":0.35326207,"teacher_disagreement_score":0.165001,"about_ca_system_score_codex":0.0014804588,"about_ca_system_score_gemma":0.00067154336,"threshold_uncertainty_score":0.3280812},"labels":[],"label_agreement":null},{"id":"W2591365303","doi":"10.1038/srep42949","title":"Magma plumbing system and seismicity of an active mid-ocean ridge volcano","year":2017,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Miljøstyrelsen; Agence Nationale de la Recherche; Deutsche Forschungsgemeinschaft; Russian Science Foundation; Polar Knowledge Canada","keywords":"Geology; Volcano; Seismology; Magma; Ridge; Microearthquake; Volcanism; Induced seismicity; Mid-ocean ridge; Intrusion; Tectonics; Geophysics; Basalt; Paleontology; Geochemistry","score_opus":0.017440667294421813,"score_gpt":0.22618151600900388,"score_spread":0.20874084871458207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2591365303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953306,0.000016889764,0.00006640847,0.0000086215705,6.6503344e-7,0.0000016390655,0.00007837564,0.000009251642,0.00028498465],"genre_scores_gemma":[0.9997193,0.0000102437725,0.00009163734,0.0000018506679,0.0000014204361,8.28503e-7,0.00009972547,0.0000010825314,0.000073730196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999747,0.000002185318,0.0000019433155,0.0000072476055,0.0000048396087,0.0000089922205],"domain_scores_gemma":[0.9999113,0.0000087090575,0.00003110267,0.0000065004638,0.000012766252,0.000029664792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000041632895,0.00010214973,0.000095780466,0.00041194822,0.0001481492,0.00023715249,0.0001373676,0.00020870731,0.0009960078],"category_scores_gemma":[0.00016931063,0.00009946305,0.000104986546,0.00029663622,0.00019780964,0.000121265315,0.00021535622,0.0001252761,0.00010693466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025032475,0.0000820656,0.8469489,0.000044572877,0.000043956727,0.0011678868,0.0008802964,0.0022513785,0.13739502,0.0002062291,0.00021669833,0.010512685],"study_design_scores_gemma":[0.0000015282899,0.000022743143,0.99821174,0.0000013720042,0.0000041767717,0.00013484347,0.00011057153,0.0010044286,0.0004148626,0.000017161827,0.00007475425,0.0000018950368],"about_ca_topic_score_codex":0.0065143253,"about_ca_topic_score_gemma":0.009537794,"teacher_disagreement_score":0.0065143253,"about_ca_system_score_codex":0.00016745846,"about_ca_system_score_gemma":0.00012868902,"threshold_uncertainty_score":0.012952805},"labels":[],"label_agreement":null},{"id":"W2592737526","doi":"","title":"Coseismic brecciation at fault stepovers and transient fluid pathways in a mid-crustal San Andreas analogue: The Pofadder Shear Zone, Namibia and South Africa","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Shear zone; Seismology; Shear (geology); Fault (geology); Paleontology; Tectonics","score_opus":0.026737214964250064,"score_gpt":0.20945839122809987,"score_spread":0.18272117626384982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2592737526","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99858,0.000051694984,0.000023327413,0.000038362086,0.0000010614295,0.0000035791595,0.000095553594,0.0000016778655,0.0012046769],"genre_scores_gemma":[0.99966335,0.000039303774,0.00003986949,0.0000050227377,0.0000012607086,0.000002506759,0.00005896742,0.0000013823665,0.0001883121],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998934,0.000018065184,0.000009599272,0.000027156997,0.000011653065,0.00003998846],"domain_scores_gemma":[0.9997831,0.000050106053,0.00007355911,0.000012474334,0.000050006714,0.000030726937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016602692,0.00020593396,0.00021235457,0.0013486563,0.001117377,0.0012173216,0.00044037343,0.00046737504,0.0025720738],"category_scores_gemma":[0.0009644593,0.00026569067,0.00016433817,0.0022791082,0.00094992056,0.0007738497,0.000737202,0.00029684586,0.0002581058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064235314,0.00011161768,0.9387705,0.0000982245,0.0000730024,0.0019695447,0.017391153,0.0017797146,0.01799715,0.0016933461,0.00027346375,0.019199835],"study_design_scores_gemma":[0.000010990537,0.0000231805,0.99337703,0.000016327012,0.000011324176,0.0001402209,0.0047472212,0.00070839986,0.00030957928,0.00007942483,0.00056821166,0.00000814382],"about_ca_topic_score_codex":0.25689483,"about_ca_topic_score_gemma":0.36014432,"teacher_disagreement_score":0.25689483,"about_ca_system_score_codex":0.0019584685,"about_ca_system_score_gemma":0.00088570867,"threshold_uncertainty_score":0.51079905},"labels":[],"label_agreement":null},{"id":"W2593267156","doi":"10.1038/nature21389","title":"Rheological separation of the megathrust seismogenic zone and episodic tremor and slip","year":2017,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":250,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"","keywords":"Geology; Subduction; Episodic tremor and slip; Mantle wedge; Seismology; Transition zone; Mantle (geology); Slip (aerodynamics); Slab; Rheology; Slow earthquake; Geophysics; Discontinuity (linguistics); Shear zone; Shear (geology); Petrology; Tectonics; Interplate earthquake; Materials science","score_opus":0.013911518059640738,"score_gpt":0.2508561579174261,"score_spread":0.23694463985778536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2593267156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99690765,0.0002266897,0.0001489645,0.00003509002,0.0000035695757,0.0000019383033,0.00008854459,0.0000031258933,0.0025844437],"genre_scores_gemma":[0.9996382,0.00005470642,0.000029577604,0.0000043201185,0.000003461673,6.136611e-7,0.000059187743,0.000001942721,0.00020798948],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994504,0.00001104328,0.000006981122,0.0000118817015,0.000009384636,0.000015591473],"domain_scores_gemma":[0.9994159,0.00013938537,0.00024273054,0.000043044143,0.00007878241,0.00008022631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018835998,0.00012164358,0.000108317676,0.0018679544,0.0002410992,0.00066724676,0.00019182413,0.0002025848,0.002394069],"category_scores_gemma":[0.0013577866,0.00012718704,0.0001136034,0.0010391412,0.0005412403,0.000582456,0.0003886527,0.00027746745,0.00036165814],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011694103,0.00009382681,0.93920565,0.00004941549,0.00006777926,0.00047383914,0.0012743268,0.0007578964,0.032117106,0.0025568786,0.00020696233,0.02202691],"study_design_scores_gemma":[0.000004129597,0.00002228844,0.99851686,0.000004539751,0.0000058564196,0.0000908553,0.00020836294,0.00026418435,0.00047088362,0.00019641501,0.00021385957,0.0000017964867],"about_ca_topic_score_codex":0.0051783663,"about_ca_topic_score_gemma":0.007950779,"teacher_disagreement_score":0.0051783663,"about_ca_system_score_codex":0.00027153984,"about_ca_system_score_gemma":0.00020331568,"threshold_uncertainty_score":0.010296464},"labels":[],"label_agreement":null},{"id":"W2593504399","doi":"","title":"Surface uplift and time-dependent seismic hazard due to fluid-injection in eastern Texas","year":2015,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Induced seismicity; Pore water pressure; Poromechanics; Seismology; Compressibility; Interferometric synthetic aperture radar; Geomorphology; Petrology; Geotechnical engineering; Porosity; Synthetic aperture radar; Porous medium","score_opus":0.023376248337581566,"score_gpt":0.22719784109879254,"score_spread":0.20382159276121098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2593504399","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998653,0.0000028022766,0.000019194278,0.0000053404688,1.9098069e-7,5.340659e-7,0.000025032625,0.000001117582,0.0000804849],"genre_scores_gemma":[0.99985373,0.000005863668,0.000023455186,0.0000015835791,5.8323997e-7,7.2402935e-7,0.00003982137,3.3497892e-7,0.00007395421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.000006659933,0.0000052633686,0.000015556921,0.000009113846,0.000022531058],"domain_scores_gemma":[0.99955493,0.00005526876,0.00024520536,0.000021578742,0.00005619424,0.00006669789],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013659397,0.00012327873,0.00010071438,0.0004763315,0.00023686077,0.0002871737,0.0001628842,0.00017636654,0.0007562195],"category_scores_gemma":[0.00041957473,0.00009531606,0.00009793359,0.00049181044,0.00034743987,0.00024434555,0.00043293988,0.00015443758,0.00007868932],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017479295,0.000055512304,0.98629946,0.000009569313,0.000020754456,0.0003712226,0.00044287974,0.0025839799,0.006601309,0.00007306272,0.00007237325,0.0032950188],"study_design_scores_gemma":[0.0000024863477,0.000039181807,0.99723804,0.000002034718,0.0000052376695,0.000038066013,0.00036937214,0.00174717,0.00045855137,0.000018821182,0.000078480916,0.0000025749644],"about_ca_topic_score_codex":0.024157712,"about_ca_topic_score_gemma":0.046907783,"teacher_disagreement_score":0.024157712,"about_ca_system_score_codex":0.00067814713,"about_ca_system_score_gemma":0.00030069347,"threshold_uncertainty_score":0.04803419},"labels":[],"label_agreement":null},{"id":"W2593586464","doi":"","title":"Continental Rifts: Lithospheric Weakness and Strength Contrasts as Triggers for Necking Instabilities","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Necking; Geology; Weakness; Lithosphere; Rift; Seismology; Anatomy; Medicine; Materials science; Tectonics; Composite material","score_opus":0.011740942351636129,"score_gpt":0.2171171294899284,"score_spread":0.20537618713829225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2593586464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976221,0.000079963334,0.00016071307,0.00006462247,0.0000022099944,0.0000042932948,0.00012822979,0.000011748778,0.0019259636],"genre_scores_gemma":[0.9997732,0.0000251182,0.00005107875,0.000007844656,0.0000030623758,0.0000011350345,0.000044321816,0.0000031818204,0.000091037226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.000010888605,0.000005575731,0.000015755933,0.000011684498,0.000018153794],"domain_scores_gemma":[0.9994271,0.0001999114,0.0001876413,0.00003467346,0.000055213597,0.00009551544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027176412,0.00018323147,0.00019642578,0.000534554,0.0002672399,0.0012125641,0.00021255187,0.00041372588,0.002458131],"category_scores_gemma":[0.0017688223,0.00015674708,0.000124951,0.00035094292,0.00039692657,0.0005444208,0.000545947,0.00027885285,0.00020586721],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049961376,0.00004611641,0.9350717,0.00007147364,0.000118567885,0.0006849276,0.0009807342,0.004219761,0.04176429,0.0022904885,0.00070456567,0.013547698],"study_design_scores_gemma":[0.000010934276,0.000052345422,0.9944924,0.0000065865233,0.000028907665,0.00010119051,0.00050379167,0.0029492045,0.00080536894,0.00072199106,0.00031862865,0.000008552851],"about_ca_topic_score_codex":0.0022783743,"about_ca_topic_score_gemma":0.003927738,"teacher_disagreement_score":0.002458131,"about_ca_system_score_codex":0.00035359667,"about_ca_system_score_gemma":0.00016593655,"threshold_uncertainty_score":0.008223236},"labels":[],"label_agreement":null},{"id":"W2594231710","doi":"10.1002/2016jb013778","title":"Modeling slow‐slip segmentation in Cascadia subduction zone constrained by tremor locations and gravity anomalies","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Subduction; Seismology; Episodic tremor and slip; Slip (aerodynamics); Bouguer anomaly; Global Positioning System; Geodesy; Lithosphere; Slab; Gravity anomaly; Geophysics; Tectonics","score_opus":0.052653627948352634,"score_gpt":0.33678930101728943,"score_spread":0.2841356730689368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2594231710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941512,0.000063844964,0.0035370335,0.00016006279,0.000010178075,0.000012391283,0.00028650896,0.00019547889,0.0015832855],"genre_scores_gemma":[0.99898165,0.000025881267,0.0004733153,0.000009494355,0.0000027206013,0.000008126431,0.00013346576,0.000014680414,0.00035059455],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990094,0.000021534353,0.0000055818878,0.00003247215,0.000011089461,0.000028379029],"domain_scores_gemma":[0.9996524,0.00012464078,0.000054597585,0.000029584118,0.000045265017,0.000093583025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028445665,0.0009041107,0.00048688176,0.000560602,0.00060306303,0.0008377542,0.0010420792,0.0012487284,0.0016227684],"category_scores_gemma":[0.00090999703,0.0007241081,0.0007870717,0.00043212142,0.0007020366,0.00035014338,0.00064023,0.00062836765,0.00015729821],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025892328,0.000015807675,0.006619112,0.000005891139,0.000020631354,0.000050744347,0.000016998702,0.99235207,0.00040080707,0.000117558804,0.00006786693,0.00030660132],"study_design_scores_gemma":[0.000010534267,0.000009661856,0.002269098,0.0000015016319,0.0000069838397,0.0000038434846,0.000012761425,0.99748397,0.000057423702,0.000083862884,0.000056241104,0.000004066938],"about_ca_topic_score_codex":0.19702907,"about_ca_topic_score_gemma":0.107182845,"teacher_disagreement_score":0.19702907,"about_ca_system_score_codex":0.0020159704,"about_ca_system_score_gemma":0.0016030121,"threshold_uncertainty_score":0.39176446},"labels":[],"label_agreement":null},{"id":"W2594255904","doi":"","title":"New kinematic and geochronologic evidence for the Quaternary evolution of the Central Anatolian Fault Zone (CAFZ)","year":2014,"lang":"en","type":"article","venue":"2014 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Quaternary; Geology; Kinematics; North Anatolian Fault; Paleontology; Fault (geology); Seismology","score_opus":0.024931678870284562,"score_gpt":0.23776918660188295,"score_spread":0.2128375077315984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2594255904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9840349,0.0014828626,0.0013743336,0.00024663343,0.00006763745,0.000016347203,0.0009136479,0.0000538062,0.01180992],"genre_scores_gemma":[0.997468,0.00035390124,0.0009162052,0.000015373986,0.000018536452,0.000010021431,0.00050621084,0.000017864317,0.0006939661],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982005,0.000018603529,0.000037462723,0.00006432774,0.000033436445,0.000026081883],"domain_scores_gemma":[0.99919814,0.00006113977,0.00035211202,0.0000848615,0.00027469598,0.000029042954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000410913,0.00027888393,0.000209009,0.0033002384,0.0006556757,0.0010559497,0.0004106457,0.00039507262,0.0034846163],"category_scores_gemma":[0.0014333895,0.0002446733,0.00017349068,0.0028040442,0.00077608036,0.00090654247,0.0007693992,0.00035952975,0.0005597277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006993331,0.00009180421,0.8458386,0.00031800798,0.00013151801,0.00096797384,0.0038562817,0.0018452879,0.04699981,0.0053115105,0.0011477317,0.09279197],"study_design_scores_gemma":[0.000011765572,0.000028082055,0.9934918,0.00003794932,0.000031046613,0.0003690829,0.0004315576,0.00070486974,0.0005370645,0.00034776144,0.004002378,0.0000065955837],"about_ca_topic_score_codex":0.01989211,"about_ca_topic_score_gemma":0.036368083,"teacher_disagreement_score":0.01989211,"about_ca_system_score_codex":0.0008668656,"about_ca_system_score_gemma":0.00079139584,"threshold_uncertainty_score":0.03955263},"labels":[],"label_agreement":null},{"id":"W2594943952","doi":"10.1002/2017gl072690","title":"Subsidence at Cerro Prieto Geothermal Field and postseismic slip along the Indiviso fault from 2011 to 2016 RADARSAT‐2 DInSAR time series analysis","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Geology; Interferometric synthetic aperture radar; Seismology; Geothermal gradient; Slip (aerodynamics); Geodesy; Fault (geology); Subsidence; Synthetic aperture radar; Geomorphology; Geophysics; Remote sensing; Structural basin","score_opus":0.02597927326330838,"score_gpt":0.27471805245615205,"score_spread":0.24873877919284368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2594943952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978364,0.00006431434,0.00008467363,0.000019308587,0.0000043647333,0.00000404153,0.001072749,0.000016414324,0.0008976934],"genre_scores_gemma":[0.99703395,0.00005950234,0.00019149976,0.0000074976115,0.000011335208,0.000005056999,0.0023818319,0.000003852655,0.0003054134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998802,0.000010568661,0.0000084311905,0.00004014199,0.00003247036,0.000028255676],"domain_scores_gemma":[0.9996754,0.000034102137,0.0001289542,0.00004318016,0.00008345441,0.000034963487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024374078,0.0001889399,0.00015515418,0.0008440406,0.00009584725,0.0003563564,0.00019114003,0.00017324457,0.00042697787],"category_scores_gemma":[0.0006988855,0.00006622048,0.0001355456,0.00068949885,0.0001378698,0.00013331167,0.0002489333,0.00013224309,0.00013150381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032744705,0.00008980628,0.9614964,0.000059305246,0.00011336046,0.00035066664,0.00028715268,0.00557001,0.007103896,0.00018068709,0.0017634594,0.022657843],"study_design_scores_gemma":[0.000003006687,0.000010584871,0.99772376,0.0000047088574,0.0000059062645,0.000035041867,0.00004168462,0.0010712906,0.00029622164,0.0000067563033,0.00079848187,0.0000026643056],"about_ca_topic_score_codex":0.023605892,"about_ca_topic_score_gemma":0.032586075,"teacher_disagreement_score":0.023605892,"about_ca_system_score_codex":0.0004525162,"about_ca_system_score_gemma":0.00023095417,"threshold_uncertainty_score":0.04693699},"labels":[],"label_agreement":null},{"id":"W2597139004","doi":"10.5382/rev.14.05","title":"Vein Formation and Deformation in Greenstone Gold Deposits","year":2001,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Barrick Gold (Canada)","funders":"","keywords":"Greenstone belt; Vein; Deformation (meteorology); Geology; Geochemistry; Archean; Psychology; Oceanography","score_opus":0.018699498377108006,"score_gpt":0.19346882720196965,"score_spread":0.17476932882486163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2597139004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925095,0.000039009345,0.000058978683,0.000005609992,7.1684457e-7,0.0000019342588,0.00010410401,0.000004869283,0.0005337852],"genre_scores_gemma":[0.99957734,0.000016562399,0.00006839686,0.0000035573494,5.285662e-7,8.53588e-7,0.000106194384,0.000001394342,0.00022525582],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999118,0.000009829549,0.000006562006,0.00002931663,0.000021499332,0.000021100135],"domain_scores_gemma":[0.9998673,0.00001608334,0.000050578925,0.000009377823,0.00003444292,0.000022168291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011660748,0.00012090912,0.00010029423,0.0015535428,0.00024818582,0.0005806767,0.0001179148,0.00019234135,0.0008487623],"category_scores_gemma":[0.00030582646,0.00011145747,0.0001347718,0.0011294294,0.00044592287,0.00021715276,0.00038445074,0.00009430762,0.0001439474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017570108,0.00001121295,0.93640256,0.000033225282,0.000034223358,0.00051489804,0.0007059498,0.000875191,0.048247516,0.0002941429,0.00009035299,0.012615095],"study_design_scores_gemma":[0.0000014372166,0.000009194648,0.998733,0.0000015819171,0.0000020610928,0.000061288214,0.00009619331,0.00029661914,0.00054777815,0.00005200238,0.00019736777,0.0000014397202],"about_ca_topic_score_codex":0.015324093,"about_ca_topic_score_gemma":0.032932155,"teacher_disagreement_score":0.015324093,"about_ca_system_score_codex":0.0007560905,"about_ca_system_score_gemma":0.00019454751,"threshold_uncertainty_score":0.030469775},"labels":[],"label_agreement":null},{"id":"W2597383049","doi":"","title":"Episodic slow slip process in a non-planar fault model constrained by non-volcanic tremor locations along Cascadia subduction zone","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Subduction; Episodic tremor and slip; Seismology; Slip (aerodynamics); Volcano; Planar; Fault (geology); Geophysics; Tectonics","score_opus":0.02066631963468998,"score_gpt":0.2436843040376297,"score_spread":0.2230179844029397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2597383049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99387944,0.00013859419,0.0021670577,0.00060197234,0.00004059709,0.000010822407,0.0008129607,0.00014153881,0.0022069751],"genre_scores_gemma":[0.9984785,0.000060434362,0.0001703101,0.000021204847,0.000015220206,0.0000063034367,0.00031646108,0.000019065124,0.0009124106],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99988353,0.00002539509,0.0000081528315,0.00004201029,0.000008375809,0.000032626383],"domain_scores_gemma":[0.9993724,0.00024466965,0.000092205315,0.00006416241,0.0000624028,0.00016415301],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042262772,0.0006897328,0.0010721781,0.0006465091,0.0006492572,0.0012259592,0.00204984,0.0026581364,0.004008292],"category_scores_gemma":[0.0016493346,0.0010492451,0.0010657661,0.0006138099,0.0012956501,0.00080167246,0.00067276566,0.0012572998,0.0003921885],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011965907,0.000036703124,0.0053307633,0.000015111955,0.000042904412,0.00016971145,0.00002774781,0.9924459,0.00030352277,0.0007705723,0.00033968437,0.000397754],"study_design_scores_gemma":[0.000040745,0.000016484699,0.0027737704,0.000003741509,0.000019128622,0.000012227381,0.000020545787,0.9968177,0.000024922148,0.00020783981,0.00005473289,0.000008160946],"about_ca_topic_score_codex":0.112628855,"about_ca_topic_score_gemma":0.055817775,"teacher_disagreement_score":0.112628855,"about_ca_system_score_codex":0.0013006359,"about_ca_system_score_gemma":0.0011859874,"threshold_uncertainty_score":0.22394657},"labels":[],"label_agreement":null},{"id":"W2598873077","doi":"10.2172/838903","title":"INNOVATIVE METHODOLOGY FOR DETECTION OF FRACTURE-CONTROLLED SWEET SPOTS IN THE NORTHERN APPALACHIAN BASIN","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Lineament; Geology; Outcrop; Structural basin; Seismology; Drilling; Bedrock; Anticline; Paleontology; Tectonics; Geomorphology; Mining engineering","score_opus":0.06904954852157706,"score_gpt":0.30453918872392505,"score_spread":0.23548964020234797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2598873077","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8027811,0.00049158756,0.18810278,0.000113330585,0.000049269875,0.00042031714,0.0012758176,0.0006957303,0.006070088],"genre_scores_gemma":[0.72335106,0.00025423738,0.27268127,0.0000546067,0.000027931072,0.0004420149,0.0010804691,0.00003640464,0.0020720568],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9995394,0.00007663776,0.000041922565,0.0001790839,0.000109643144,0.000053403397],"domain_scores_gemma":[0.9993697,0.00010690549,0.00012337834,0.000058858586,0.0002922579,0.000048897124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00078343763,0.0003073713,0.00022522193,0.0034211967,0.00061064906,0.0008330358,0.0005814052,0.00039360728,0.0013535459],"category_scores_gemma":[0.0010826286,0.00026980438,0.00021563914,0.0018811739,0.0002932604,0.00036922778,0.00061844545,0.00022313856,0.00029808434],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002147596,0.00016847142,0.43652543,0.0002949885,0.0001764182,0.0010079244,0.0020421278,0.005272003,0.11794857,0.001888608,0.002150897,0.4323098],"study_design_scores_gemma":[0.00003971071,0.00017743789,0.900791,0.000062698375,0.0001042155,0.0012558884,0.0018624085,0.07109641,0.014242282,0.0015328208,0.008772181,0.00006291173],"about_ca_topic_score_codex":0.008282836,"about_ca_topic_score_gemma":0.030418681,"teacher_disagreement_score":0.008282836,"about_ca_system_score_codex":0.00033089513,"about_ca_system_score_gemma":0.0008575272,"threshold_uncertainty_score":0.01646924},"labels":[],"label_agreement":null},{"id":"W2599349705","doi":"10.1130/g38766.1","title":"Timing of initial seafloor spreading in the Newfoundland-Iberia rift","year":2017,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Citation; Geological survey; Icon; Geology; Library science; History; Paleontology; Computer science","score_opus":0.04534288974851245,"score_gpt":0.3016986830946547,"score_spread":0.2563557933461422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2599349705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9395497,0.005977639,0.00024177089,0.001445156,0.00012378799,0.00003269066,0.0058352677,0.00006980355,0.046724185],"genre_scores_gemma":[0.9897774,0.0024973394,0.00024860108,0.00007435533,0.000040125622,0.000012117402,0.0026401964,0.00002346344,0.004686503],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998266,0.000013144971,0.0000125364895,0.000028474076,0.000044106055,0.000075151176],"domain_scores_gemma":[0.9991264,0.000067454916,0.00022972681,0.000024536954,0.0004226076,0.00012933846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040900699,0.00022218977,0.00029017855,0.0023429785,0.0007583166,0.0016882673,0.000274585,0.00036054812,0.0041395095],"category_scores_gemma":[0.0015216954,0.00015509827,0.00019346407,0.0023622182,0.000692915,0.0006186335,0.0011576776,0.00039189865,0.00074541],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006552803,0.00005596313,0.85254693,0.00046260815,0.00025536615,0.0010775747,0.0046903915,0.0025231969,0.0032197877,0.00249304,0.031267893,0.10075203],"study_design_scores_gemma":[0.0000055750434,0.000012203102,0.99015874,0.00009855376,0.000014780632,0.00003664142,0.0009745356,0.00014960546,0.00012480648,0.000042169355,0.008373128,0.0000092948285],"about_ca_topic_score_codex":0.66591257,"about_ca_topic_score_gemma":0.7715678,"teacher_disagreement_score":0.33408743,"about_ca_system_score_codex":0.0045819213,"about_ca_system_score_gemma":0.0023823143,"threshold_uncertainty_score":0.67210984},"labels":[],"label_agreement":null},{"id":"W2601287886","doi":"10.1130/l609.1","title":"Geology and in situ stress of the MH-2 borehole, Idaho, USA: Insights into western Snake River Plain structure from geothermal exploration drilling","year":2017,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"U.S. Air Force; University of Alberta; Natural Sciences and Engineering Research Council of Canada; Utah State University; U.S. Department of Energy","keywords":"Geology; Borehole; Basalt; Drilling; Geothermal gradient; Lithology; Geochemistry; Sedimentary rock; Petrology; Paleontology","score_opus":0.014393439724470736,"score_gpt":0.21654029397565008,"score_spread":0.20214685425117934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2601287886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99815637,0.000020607215,0.000106217405,0.000019450363,0.0000014879731,0.000007362571,0.0004512051,0.000009953657,0.0012272198],"genre_scores_gemma":[0.9988102,0.000034996916,0.00036069108,0.000015379102,0.0000025906515,0.000012003317,0.0003918645,0.0000032347218,0.000369146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992836,0.000006867678,0.000005759915,0.000019407762,0.00002566473,0.000013990929],"domain_scores_gemma":[0.99983716,0.000016086275,0.000047905127,0.000011085307,0.00005529623,0.000032365733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014047034,0.00017423654,0.00012962577,0.0009914794,0.0003552723,0.00037827584,0.0003683127,0.00021438471,0.00064394885],"category_scores_gemma":[0.00028425007,0.00015056913,0.00008537451,0.0008300142,0.00029909177,0.00025073122,0.0005444021,0.00016027738,0.00015976393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000087412234,0.000082044964,0.9741856,0.000024704332,0.000016138487,0.00027442112,0.0012438959,0.00037603313,0.014976036,0.000105744206,0.00042061074,0.008207338],"study_design_scores_gemma":[0.0000019716256,0.0000073186625,0.9987704,0.0000029822006,0.0000026674693,0.000036697806,0.00034108767,0.00034331813,0.00033080453,0.0000103623215,0.00015078206,0.0000016112948],"about_ca_topic_score_codex":0.06508027,"about_ca_topic_score_gemma":0.24588884,"teacher_disagreement_score":0.06508027,"about_ca_system_score_codex":0.0005968812,"about_ca_system_score_gemma":0.0004513838,"threshold_uncertainty_score":0.12940294},"labels":[],"label_agreement":null},{"id":"W2601538800","doi":"10.1002/2017jb013983","title":"Continental crust anisotropy measurements from tectonic tremor in Cascadia","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Seismology; Tectonics; Crust; Anisotropy; Continental crust; Stress field; Shear wave splitting; Subduction; Continental margin; Passive margin; Aftershock; Geophysics; Shear (geology); Paleontology; Rift","score_opus":0.10644487521237204,"score_gpt":0.3560746163890352,"score_spread":0.24962974117666314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2601538800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972861,0.00004481059,0.00029825835,0.000019294735,0.0000027486278,0.0000029921669,0.00053270103,0.000061908126,0.0017512003],"genre_scores_gemma":[0.9992581,0.000029791772,0.00014212115,0.000002412081,0.0000016397793,0.0000026054015,0.00035602448,0.000005773746,0.00020139992],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987805,0.0000069861358,0.000008702026,0.000042305524,0.000045307414,0.000018671903],"domain_scores_gemma":[0.99965835,0.000027903972,0.00007664674,0.000032194737,0.00011955718,0.000085370935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013978595,0.0004184284,0.00018817365,0.0013357716,0.0004970436,0.00037929774,0.0001794128,0.00016733812,0.0012488366],"category_scores_gemma":[0.00059889193,0.00020078599,0.00022080143,0.00097550754,0.00022433893,0.00017419833,0.00044197112,0.00022771867,0.00022210505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024546622,0.000031183634,0.8779915,0.00004787292,0.0001286084,0.00033411907,0.0006762348,0.002536075,0.106331386,0.00008746617,0.00036372853,0.011226339],"study_design_scores_gemma":[0.0000031804482,0.000010562056,0.99776125,0.0000020895336,0.000011714065,0.000025838557,0.00008256677,0.00056581374,0.0012852703,0.000016851578,0.0002313373,0.0000035361218],"about_ca_topic_score_codex":0.048549652,"about_ca_topic_score_gemma":0.07572753,"teacher_disagreement_score":0.95145035,"about_ca_system_score_codex":0.0006957528,"about_ca_system_score_gemma":0.00028010842,"threshold_uncertainty_score":0.09653413},"labels":[],"label_agreement":null},{"id":"W2602332582","doi":"10.1002/2017gc006838","title":"Thermal state of the <scp>E</scp>xplorer segment of the <scp>C</scp>ascadia subduction zone: Implications for seismic and tsunami hazards","year":2017,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Ocean Networks Canada Society; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Hypocenter; Geodetic datum; Seismotectonics; Episodic tremor and slip; Earthquake rupture; Fault (geology); Submarine pipeline; Induced seismicity; Geodesy; Tectonics","score_opus":0.01261771595726405,"score_gpt":0.2138568572675324,"score_spread":0.20123914131026835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2602332582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99738103,0.000018675075,0.0010539932,0.00005085895,0.00000190811,0.0000031219213,0.00017831892,0.000030246394,0.0012817876],"genre_scores_gemma":[0.9996958,0.000007341921,0.00009207836,0.0000019128743,6.022456e-7,0.0000014153278,0.000055948032,0.0000026035316,0.00014243867],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999449,0.000014707173,0.0000033823724,0.000013471796,0.000010522577,0.000013034632],"domain_scores_gemma":[0.9998635,0.000042055988,0.000026495458,0.00001877627,0.000024499477,0.000024682591],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016539614,0.00022918262,0.00012443472,0.00040847782,0.0003323713,0.0007236521,0.00033965652,0.0003767264,0.001536932],"category_scores_gemma":[0.0005537616,0.00022650996,0.00024396238,0.0002779594,0.0004937862,0.00030713985,0.00030176612,0.00020046538,0.00017179205],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011687448,0.00007429539,0.18394431,0.00002761524,0.00006414609,0.00020016721,0.00016083826,0.7985479,0.011436073,0.0010452216,0.00040616607,0.0039763725],"study_design_scores_gemma":[0.000015652038,0.000034705434,0.14918332,0.000010392543,0.000019665087,0.000035628167,0.0002107135,0.8479257,0.0015745768,0.00065947487,0.00030820924,0.000021967344],"about_ca_topic_score_codex":0.064046875,"about_ca_topic_score_gemma":0.061437145,"teacher_disagreement_score":0.064046875,"about_ca_system_score_codex":0.0010476755,"about_ca_system_score_gemma":0.0006107233,"threshold_uncertainty_score":0.12734812},"labels":[],"label_agreement":null},{"id":"W2602836083","doi":"10.1002/2017jb014048","title":"Microgravity changes at the Laguna del Maule volcanic field: Magma‐induced stress changes facilitate mass addition","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Dike; Magma; Sill; Volcano; Rock mass classification; Fault (geology); Petrology; Rhyolite; Deformation (meteorology); Stress field; Seismology; Silicic; Intrusion; Geochemistry; Volcanic rock; Geotechnical engineering","score_opus":0.08974914259721456,"score_gpt":0.33805599192339614,"score_spread":0.24830684932618158,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2602836083","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990677,0.000034604844,0.00008512357,0.000027028964,0.0000017490039,0.0000029163425,0.00013356944,0.00001882093,0.00062843534],"genre_scores_gemma":[0.9997008,0.000018848488,0.000057148885,0.0000044912085,0.0000017482505,0.000001726896,0.00006883289,0.0000018015248,0.00014465407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996257,0.000003138374,0.0000019086501,0.000011730496,0.000006315329,0.000014308364],"domain_scores_gemma":[0.9999193,0.000010755486,0.000029956862,0.0000071001064,0.000012594298,0.00002026776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000069068,0.00026147286,0.00011737567,0.00046017824,0.00018790024,0.00049244514,0.00023391514,0.00025518227,0.001699358],"category_scores_gemma":[0.0002752804,0.000121307654,0.0001909291,0.00034888703,0.00024494034,0.00036309042,0.0002718004,0.00012498806,0.00010289204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021477562,0.000076913915,0.91541874,0.00007629725,0.00009765065,0.000680258,0.0005937173,0.012693037,0.057023298,0.0002847424,0.00048105733,0.012359531],"study_design_scores_gemma":[0.0000067858427,0.000018979257,0.99448013,0.000002847129,0.00000916944,0.00003191208,0.00016607156,0.003976886,0.0009694082,0.000046624387,0.00028570218,0.000005402118],"about_ca_topic_score_codex":0.017868528,"about_ca_topic_score_gemma":0.021422895,"teacher_disagreement_score":0.017868528,"about_ca_system_score_codex":0.0005875024,"about_ca_system_score_gemma":0.00028363662,"threshold_uncertainty_score":0.035529017},"labels":[],"label_agreement":null},{"id":"W2603252594","doi":"10.1785/0220170131","title":"Relative Location Analysis and Moment Tensor Inversion of the 2012 Gulf of Maine Earthquake Swarm","year":2017,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Boston College","keywords":"Moment tensor; Geology; Seismology; Inversion (geology); Swarm behaviour; Moment (physics); Earthquake swarm; Geodesy; Oceanography; Mathematics; Mathematical optimization; Induced seismicity; Physics; Classical mechanics; Tectonics","score_opus":0.06433198361462382,"score_gpt":0.3056678192977347,"score_spread":0.24133583568311084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2603252594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9351464,0.00097354694,0.030020606,0.0018469011,0.00042965228,0.00007915628,0.009329278,0.0019399645,0.020234559],"genre_scores_gemma":[0.96294457,0.0006716844,0.020577539,0.00008866627,0.00023241788,0.000033355645,0.010709115,0.0003911231,0.0043514716],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99985194,0.000021713946,0.00001181078,0.000023245862,0.000063534084,0.000027758895],"domain_scores_gemma":[0.999642,0.000040366303,0.00006128779,0.00003878016,0.00017268407,0.000044927885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003509732,0.00040874854,0.0002522377,0.001756513,0.00026059806,0.00071379537,0.00036703958,0.00043945003,0.0028649184],"category_scores_gemma":[0.0019677887,0.00022096233,0.00039770376,0.0015422308,0.00021126845,0.00086257653,0.00069167075,0.0005436598,0.0017705552],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008515203,0.00035647847,0.20602402,0.00064928376,0.00036253445,0.0016741696,0.0024197297,0.122262746,0.08734267,0.008339477,0.07090405,0.49881336],"study_design_scores_gemma":[0.00014861493,0.00020812427,0.56753653,0.00017560653,0.00012975956,0.0005043051,0.0019923039,0.3891094,0.008825999,0.0038496829,0.027336877,0.0001828389],"about_ca_topic_score_codex":0.01461328,"about_ca_topic_score_gemma":0.02312758,"teacher_disagreement_score":0.01461328,"about_ca_system_score_codex":0.0003984166,"about_ca_system_score_gemma":0.0007752358,"threshold_uncertainty_score":0.02905643},"labels":[],"label_agreement":null},{"id":"W2603749522","doi":"","title":"On the Possibility of Slip-to-trench Rupture in Cascadia Megathrust Earthquakes","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Trench; Geology; Seismology; Episodic tremor and slip; Slip (aerodynamics); Subduction; Tsunami earthquake; Tectonics; Engineering","score_opus":0.034247527547552566,"score_gpt":0.25056974310058017,"score_spread":0.2163222155530276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2603749522","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97818065,0.00053873454,0.0012953739,0.00096825,0.000040740208,0.000009393635,0.00014260675,0.000023247429,0.018801082],"genre_scores_gemma":[0.99955755,0.0000682976,0.000056754183,0.000018879391,0.00002921416,7.9629206e-7,0.000027338732,0.0000016593477,0.00023948516],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99960274,0.00012294663,0.000029355066,0.000075195494,0.00006408313,0.000105748055],"domain_scores_gemma":[0.9953564,0.003164142,0.00044316822,0.00046111748,0.00031518165,0.00026004534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016884418,0.00029953895,0.0002840087,0.0010685913,0.0011550686,0.0019899749,0.000995285,0.0023141934,0.005563445],"category_scores_gemma":[0.009077078,0.00027424985,0.00041224615,0.00068701355,0.0014902097,0.0013440608,0.0012220815,0.00073275366,0.0005655287],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038614068,0.00013993534,0.8817797,0.00022545455,0.0003415833,0.01369393,0.0015348464,0.022956101,0.0067532402,0.038267996,0.002296093,0.028149804],"study_design_scores_gemma":[0.00022673185,0.00062997406,0.90106386,0.00010586974,0.00034960097,0.0043984,0.0051579527,0.039483707,0.003827005,0.039926335,0.004748569,0.00008189511],"about_ca_topic_score_codex":0.0051764753,"about_ca_topic_score_gemma":0.005242849,"teacher_disagreement_score":0.9948235,"about_ca_system_score_codex":0.00061217113,"about_ca_system_score_gemma":0.00037494572,"threshold_uncertainty_score":0.01861155},"labels":[],"label_agreement":null},{"id":"W2604559072","doi":"10.36487/acg_rep/1511_04_brown","title":"Seismic hazard assessment using apparent stress ratio","year":2015,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Laurentian University; Agnico Eagle (Canada)","funders":"","keywords":"Seismic hazard; Stress (linguistics); Hazard; Seismology; Seismic risk; Geology; Rock mass classification; Hazard analysis; Term (time); Earthquake scenario; Mining engineering; Geotechnical engineering; Engineering; Reliability engineering","score_opus":0.06492770442584381,"score_gpt":0.28515965384621217,"score_spread":0.22023194942036836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2604559072","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8688589,0.0008116031,0.10381506,0.00018409462,0.00005445139,0.00019885188,0.004101688,0.0018400133,0.020135392],"genre_scores_gemma":[0.9855282,0.00022729345,0.012092614,0.000012104266,0.00002457095,0.00003431199,0.000890074,0.00003301143,0.0011578315],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99947387,0.00009676095,0.000058673322,0.000075722324,0.0002497468,0.00004534982],"domain_scores_gemma":[0.997701,0.00064829784,0.00077227,0.00010305745,0.0006305832,0.00014486257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008200931,0.0006831836,0.00041021258,0.0063558356,0.00019288903,0.0008475096,0.0005291846,0.00051566144,0.0033963814],"category_scores_gemma":[0.0037789694,0.00020802626,0.00035728916,0.0025325466,0.00025069033,0.0010003434,0.00053402083,0.00031434922,0.0012029032],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056863687,0.0002506369,0.61254394,0.00035231415,0.00023721394,0.0010427744,0.0005632776,0.091493234,0.029015385,0.003335613,0.0030243495,0.25757253],"study_design_scores_gemma":[0.000029260043,0.001021181,0.63430804,0.00007930059,0.000103425395,0.0016903663,0.001096895,0.34026858,0.007952973,0.0060414667,0.0072117993,0.00019672395],"about_ca_topic_score_codex":0.0023418153,"about_ca_topic_score_gemma":0.002221364,"teacher_disagreement_score":0.0063558356,"about_ca_system_score_codex":0.0003322696,"about_ca_system_score_gemma":0.00023046914,"threshold_uncertainty_score":0.011362076},"labels":[],"label_agreement":null},{"id":"W2604618214","doi":"10.1016/j.tecto.2017.04.006","title":"Cyclical shear fracture and viscous flow during transitional ductile-brittle deformation in the Saddlebag Lake Shear Zone, California","year":2017,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Mylonite; Shear zone; Pressure solution; Metamorphic rock; Shear (geology); Cataclastic rock; Foliation (geology); Differential stress; Quartz; Feldspar; Mineralogy; Shearing (physics); Petrology; Deformation (meteorology); Geotechnical engineering; Diagenesis; Seismology; Fault (geology); Tectonics","score_opus":0.010866346913240224,"score_gpt":0.2138692974192473,"score_spread":0.20300295050600706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2604618214","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996542,0.00001508925,0.000016357044,0.000010343222,8.838757e-7,0.000002257736,0.000083559746,0.0000029437247,0.0002144618],"genre_scores_gemma":[0.99966645,0.000014292127,0.000027773287,0.000005775731,0.0000011761334,0.0000036914091,0.00010827767,0.0000017888935,0.00017074724],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989355,0.000008570827,0.0000080488435,0.000034220164,0.000022052896,0.000033470198],"domain_scores_gemma":[0.9997185,0.00005190636,0.000068721354,0.000017587005,0.00007371812,0.00006944621],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001846294,0.00015148503,0.0002645015,0.0011943527,0.0013678917,0.000835066,0.00062775885,0.0005679498,0.0013489878],"category_scores_gemma":[0.0006296026,0.0003370479,0.00017394505,0.0009249992,0.0008180486,0.00046907485,0.0007329097,0.00032996896,0.00012357922],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005800498,0.00028105822,0.9765853,0.00004152985,0.00008750789,0.0004007521,0.003528679,0.0013298559,0.0077769062,0.00023276803,0.00058247836,0.008573174],"study_design_scores_gemma":[0.0000062072368,0.000015693462,0.99905926,0.00000306044,0.0000051496377,0.000011806483,0.00047453062,0.0002685803,0.00006851858,0.000010048826,0.000074163945,0.0000029214677],"about_ca_topic_score_codex":0.3311305,"about_ca_topic_score_gemma":0.60411537,"teacher_disagreement_score":0.3311305,"about_ca_system_score_codex":0.002066474,"about_ca_system_score_gemma":0.0014377595,"threshold_uncertainty_score":0.65840626},"labels":[],"label_agreement":null},{"id":"W2609620467","doi":"10.1007/s11069-017-2864-9","title":"New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites","year":2017,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"College of William and Mary; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Paleoseismology; Turbidite; Episodic tremor and slip; Submarine pipeline; Ridge; Holocene; Accretionary wedge; Oceanography; Paleontology; Fault (geology); Tectonics; Sediment","score_opus":0.007095329077382172,"score_gpt":0.21129854849079452,"score_spread":0.20420321941341235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2609620467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970229,0.00008638615,0.00079929305,0.00006146639,0.0000032210785,0.0000018760811,0.00059577206,0.000029815472,0.0013991294],"genre_scores_gemma":[0.99903405,0.000040876894,0.00019898803,0.0000055891032,0.0000032520772,0.000001954169,0.0006104121,0.0000063271864,0.000098592776],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998355,0.000024695413,0.00002099011,0.00006162738,0.000031549967,0.000025576832],"domain_scores_gemma":[0.99920124,0.00024104696,0.0002329224,0.00011290029,0.0001001847,0.00011176165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004586667,0.00040350787,0.00026993122,0.0007018757,0.00035866772,0.0009946257,0.000353505,0.0003114262,0.0023749818],"category_scores_gemma":[0.0030921986,0.0003873869,0.0002378284,0.0006978575,0.00029805562,0.00069743866,0.0005076985,0.000342487,0.00026847722],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015198454,0.000037613536,0.92312187,0.000039167284,0.000088695095,0.0001475904,0.00024037554,0.063972436,0.0052867164,0.0008281508,0.0003611976,0.0057241945],"study_design_scores_gemma":[0.00002474656,0.000047409358,0.88223344,0.000027323116,0.000033386626,0.000084454754,0.00022487316,0.11367283,0.001010859,0.0011530911,0.0014633383,0.000024335428],"about_ca_topic_score_codex":0.027489232,"about_ca_topic_score_gemma":0.050167654,"teacher_disagreement_score":0.027489232,"about_ca_system_score_codex":0.00063469954,"about_ca_system_score_gemma":0.00048129744,"threshold_uncertainty_score":0.054658473},"labels":[],"label_agreement":null},{"id":"W2610328821","doi":"","title":"Early warning system of tsunami by measuring tsunamigenic ionospheric hole","year":2015,"lang":"en","type":"article","venue":"Japan Geoscience Union","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Digital Payment Technologies (Canada)","funders":"","keywords":"Ionosphere; Warning system; Geology; Seismology; Meteorology; Geophysics; Remote sensing; Environmental science; Telecommunications; Physics; Computer science","score_opus":0.021962671127405423,"score_gpt":0.19842417075613653,"score_spread":0.1764614996287311,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2610328821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96863025,0.0002227899,0.017261466,0.00023373065,0.00022464606,0.00014505596,0.0036808606,0.0009714928,0.0086298445],"genre_scores_gemma":[0.98877317,0.00008137343,0.0068065273,0.000055145512,0.000040825333,0.00006069432,0.0020171034,0.000017682101,0.0021476625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983525,0.00002601161,0.00002153902,0.00004310165,0.00004362627,0.000030385865],"domain_scores_gemma":[0.99930656,0.000053981996,0.00009180125,0.000050853487,0.00039956663,0.000097257056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043645923,0.00045616235,0.00023532737,0.0012841418,0.0003843978,0.00046166568,0.00033173373,0.00039759954,0.0015761857],"category_scores_gemma":[0.0008580229,0.0001431827,0.00013930413,0.00060340884,0.00008808048,0.0005338155,0.00048806946,0.00029119954,0.00042310377],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094325934,0.00025140343,0.7742993,0.00019099515,0.00014756642,0.00032550594,0.0009790995,0.0080888495,0.055785403,0.0010352097,0.012967264,0.14498612],"study_design_scores_gemma":[0.00022407164,0.0006237844,0.85188127,0.000057910704,0.00048696942,0.00026996306,0.0010891653,0.11177611,0.022914233,0.0009725509,0.009599872,0.000104147046],"about_ca_topic_score_codex":0.0052096075,"about_ca_topic_score_gemma":0.006851444,"teacher_disagreement_score":0.0052096075,"about_ca_system_score_codex":0.00024559276,"about_ca_system_score_gemma":0.0006221727,"threshold_uncertainty_score":0.010358572},"labels":[],"label_agreement":null},{"id":"W2611160697","doi":"","title":"Modeling the Failure of Magmatic Foams and Application to Infrasonic Signals at Stromboli Volcano, Italy","year":2014,"lang":"en","type":"article","venue":"2014 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Volcano; Seismology; Geology; Infrasound; Acoustics","score_opus":0.009188375179700586,"score_gpt":0.20734570704637809,"score_spread":0.1981573318666775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2611160697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9821813,0.00029897966,0.01379983,0.00026026115,0.000030695235,0.000022951313,0.00029301268,0.00020390646,0.0029091437],"genre_scores_gemma":[0.9982856,0.0000598529,0.0010483795,0.000008638513,0.000010135086,0.000011453931,0.0000697997,0.000013849904,0.00049235276],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990726,0.000022836677,0.0000063914235,0.000022252378,0.000012204721,0.000028997729],"domain_scores_gemma":[0.9991671,0.0005429064,0.00010183024,0.00003618805,0.000080499216,0.00007144552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040119677,0.00080819137,0.0006543432,0.0008167688,0.00041070682,0.0009095026,0.0010909099,0.0022133295,0.0013642529],"category_scores_gemma":[0.0021721448,0.00046137313,0.00064243656,0.0004507678,0.0006770932,0.00051928556,0.00052283646,0.0005682538,0.00016424747],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004360093,0.00003203918,0.0043319096,0.000017854902,0.0000120885725,0.00008111005,0.000026617734,0.9923494,0.0007098486,0.00046928573,0.00013775053,0.0017885017],"study_design_scores_gemma":[0.0000031267402,0.000007399127,0.0005875109,0.0000015205821,0.000003194247,0.0000051088,0.00000647334,0.9992073,0.00007100334,0.00008277029,0.000022636901,0.0000019032364],"about_ca_topic_score_codex":0.046542987,"about_ca_topic_score_gemma":0.01584374,"teacher_disagreement_score":0.046542987,"about_ca_system_score_codex":0.0007355445,"about_ca_system_score_gemma":0.0005809518,"threshold_uncertainty_score":0.0925442},"labels":[],"label_agreement":null},{"id":"W2611252483","doi":"","title":"Foreshock activity of the large-scale interplate earthquakes around Japan","year":2014,"lang":"en","type":"article","venue":"Japan Geoscience Union","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Digital Payment Technologies (Canada)","funders":"","keywords":"Foreshock; Seismology; Intraplate earthquake; Geology; Scale (ratio); Earthquake prediction; Geophysics; Aftershock; Tectonics; Geography; Cartography","score_opus":0.010299074511325857,"score_gpt":0.2126155564439604,"score_spread":0.20231648193263455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2611252483","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994673,0.000065485794,0.000025396359,0.000021913522,0.0000047070203,0.0000018309544,0.00008255262,0.000001213791,0.00032958973],"genre_scores_gemma":[0.9996043,0.00006458325,0.000019681982,0.000006812025,0.000008361261,0.000001924343,0.00012810004,9.321519e-7,0.00016543594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999019,0.000008047361,0.000012022914,0.000023869045,0.000014855183,0.000039276056],"domain_scores_gemma":[0.9994686,0.000057488975,0.00018191998,0.000024649653,0.00012325673,0.00014398304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019365786,0.0002969214,0.00018882913,0.0012194924,0.00057720725,0.00050716306,0.00021065156,0.00029022805,0.00085464556],"category_scores_gemma":[0.00056861195,0.0002330103,0.0002282763,0.0009796087,0.0003634551,0.0005647418,0.0005246026,0.00022166163,0.00009813702],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002575372,0.000043672295,0.98659503,0.00003721639,0.000079348945,0.00058670476,0.0024052989,0.0005536529,0.0043295757,0.0000981675,0.00028423482,0.0047295513],"study_design_scores_gemma":[0.0000032257942,0.000021116886,0.99865305,0.000003045253,0.000017855544,0.000036159083,0.00085013406,0.0001837026,0.000066061904,0.000012748862,0.00014892334,0.000003960124],"about_ca_topic_score_codex":0.057922628,"about_ca_topic_score_gemma":0.11729734,"teacher_disagreement_score":0.057922628,"about_ca_system_score_codex":0.00053544564,"about_ca_system_score_gemma":0.00071615836,"threshold_uncertainty_score":0.115170956},"labels":[],"label_agreement":null},{"id":"W2611925948","doi":"10.1139/cjes-2016-0226","title":"Secondary rock structures and the regional hydrogeology of claystone-rich cretaceous strata, Williston Basin, Saskatchewan, Canada","year":2017,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Mosaic Company","keywords":"Geology; Cretaceous; Sedimentary rock; Structural basin; Fault (geology); Paleontology; Hydrogeology; Sequence stratigraphy; Denudation; Geomorphology; Facies; Tectonics; Geotechnical engineering","score_opus":0.015401641147576143,"score_gpt":0.20867810258718403,"score_spread":0.1932764614396079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2611925948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887228,0.00035796917,0.00023969603,0.00013281948,0.0000053980184,0.000055006356,0.006567753,0.000029000828,0.0038895344],"genre_scores_gemma":[0.9926184,0.00042156127,0.0006138036,0.00004186256,0.000002086179,0.000035102596,0.0035246706,0.000012459812,0.0027300373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981576,0.000011277667,0.000013642777,0.00005472031,0.00005537526,0.00004926249],"domain_scores_gemma":[0.99901736,0.000078575526,0.00011914145,0.00004568559,0.00056186435,0.00017738891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021247365,0.00032637853,0.00024895108,0.0023811439,0.0012252546,0.0012598605,0.0007249394,0.00022144342,0.0024656772],"category_scores_gemma":[0.0007439347,0.00026478787,0.00022497939,0.004818962,0.00072199956,0.00030634413,0.0006050651,0.0002555543,0.00036087254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006282209,0.000027636826,0.9721061,0.00007914335,0.00015089908,0.00027630094,0.0015414952,0.0015704772,0.0040249326,0.0003122208,0.0020709848,0.017777003],"study_design_scores_gemma":[0.0000040783525,0.000002753185,0.99688965,0.000018921959,0.0000107738115,0.000025696756,0.0009240675,0.0005341863,0.00017702258,0.00002547515,0.0013787881,0.000008581451],"about_ca_topic_score_codex":0.99141437,"about_ca_topic_score_gemma":0.9982717,"teacher_disagreement_score":0.015547734,"about_ca_system_score_codex":0.015547734,"about_ca_system_score_gemma":0.020624962,"threshold_uncertainty_score":0.112807274},"labels":[],"label_agreement":null},{"id":"W2613764486","doi":"10.1111/iar.12192","title":"Strength and deformation behavior of the Shimanto accretionary complex across the Nobeoka thrust","year":2017,"lang":"en","type":"article","venue":"Island Arc","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Japan Society for the Promotion of Science","keywords":"Geology; Subduction; Brittleness; Accretionary wedge; Petrology; Seismology; Deformation (meteorology); Cataclastic rock; Geochemistry; Tectonics; Materials science; Composite material","score_opus":0.030938149621124095,"score_gpt":0.26374059989705617,"score_spread":0.23280245027593208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2613764486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997811,0.000009378498,0.000016134798,0.0000018338153,2.7099745e-7,8.6375087e-7,0.00002348495,9.907818e-7,0.00016598059],"genre_scores_gemma":[0.99970764,0.000012491201,0.000042493197,0.0000024834317,6.5512353e-7,0.0000015280934,0.00008531328,9.584604e-7,0.00014651619],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990785,0.0000050068047,0.000009176819,0.000032031498,0.000024550056,0.000021363498],"domain_scores_gemma":[0.99984634,0.000011433185,0.000048049787,0.000013601959,0.00003605771,0.000044420525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000082298604,0.00018921663,0.0002633141,0.0012845907,0.0006705917,0.00042663308,0.00027138556,0.00027438978,0.0009789268],"category_scores_gemma":[0.00025921236,0.00022868125,0.00015932777,0.0009747419,0.0005480484,0.00015958564,0.00051664544,0.00012251128,0.00019909901],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034808356,0.00006162507,0.90406,0.00005006596,0.00007455297,0.0008685818,0.0015972701,0.000954924,0.083504446,0.000082239465,0.00007507302,0.008323151],"study_design_scores_gemma":[0.0000018523709,0.000021459118,0.99880314,0.0000018461316,0.0000066919197,0.000055861252,0.00027994442,0.00024314385,0.0005267753,0.000003972666,0.00005371873,0.0000016531833],"about_ca_topic_score_codex":0.028837604,"about_ca_topic_score_gemma":0.07150939,"teacher_disagreement_score":0.028837604,"about_ca_system_score_codex":0.0003991566,"about_ca_system_score_gemma":0.00026533045,"threshold_uncertainty_score":0.05733949},"labels":[],"label_agreement":null},{"id":"W2615453838","doi":"10.1038/nature22355","title":"Extreme hydrothermal conditions at an active plate-bounding fault","year":2017,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":135,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Alberta","funders":"Marsden Fund; Natural Environment Research Council; Victoria University; Centre National de la Recherche Scientifique; Victoria University of Wellington; Université de Montpellier; Sight Research UK; University of Otago","keywords":"Geology; Geothermal gradient; Borehole; Fault (geology); Hydrostatic pressure; Crust; Seismology; Intraplate earthquake; Hydrostatic equilibrium; Heat generation; Petrology; Hydrothermal circulation; Rock mass classification; Active fault; Fluid pressure; Geophysics; Geotechnical engineering; Tectonics; Mechanics","score_opus":0.03058966788397342,"score_gpt":0.27587743069091814,"score_spread":0.24528776280694473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2615453838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992205,0.0000074765053,0.000058847218,0.00002045206,0.0000017646328,0.0000013167211,0.000042264157,0.000002901928,0.00064437435],"genre_scores_gemma":[0.999869,0.0000070295064,0.00003300319,0.0000035702099,0.0000024356095,4.5025683e-7,0.000021566548,5.1816585e-7,0.00006249797],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999443,0.0000074220757,0.00000519733,0.000012762595,0.000008869035,0.000021426938],"domain_scores_gemma":[0.9998196,0.000029154678,0.000057713216,0.000017143499,0.000026409029,0.0000500395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000099168705,0.00009290996,0.00017355259,0.0004116454,0.0005994007,0.00049756386,0.00022882738,0.00046262407,0.0009731997],"category_scores_gemma":[0.0005284809,0.0001296003,0.00011362538,0.00033283458,0.0007704356,0.000360566,0.00041357704,0.00027475864,0.00008390606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014285905,0.00014409337,0.84547055,0.000045577308,0.00007366444,0.004630976,0.0025636174,0.0038405943,0.13095097,0.0013997244,0.0004395497,0.009012148],"study_design_scores_gemma":[0.000018877994,0.00017214488,0.99394,0.0000036113804,0.000017607923,0.00058343366,0.0008335397,0.0009912826,0.0027358658,0.00036422396,0.00033071093,0.000008719098],"about_ca_topic_score_codex":0.006049916,"about_ca_topic_score_gemma":0.011887483,"teacher_disagreement_score":0.006049916,"about_ca_system_score_codex":0.00043490567,"about_ca_system_score_gemma":0.0002520514,"threshold_uncertainty_score":0.012029409},"labels":[],"label_agreement":null},{"id":"W2615893689","doi":"","title":"An estimate of the tsunami-debris quantity washed ashore on the US and Canadian beaches, based on a webcam monitoring and a particle tracking model experiment","year":2017,"lang":"en","type":"article","venue":"Japan Geoscience Union","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Debris; Tracking (education); Particle (ecology); Environmental science; Geology; Remote sensing; Computer science; Real-time computing; Oceanography; Psychology","score_opus":0.04004973685038598,"score_gpt":0.26804379165121106,"score_spread":0.22799405480082507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2615893689","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99120927,0.000079719524,0.0016367347,0.00003755559,0.000005069758,0.000038744667,0.004547841,0.0000752445,0.002369841],"genre_scores_gemma":[0.9894142,0.000113484486,0.0053690616,0.000023446177,0.0000035619462,0.000027669457,0.0033340286,0.000010544512,0.0017040004],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998579,0.0000059059294,0.000007100795,0.000038690923,0.000064206426,0.000026141293],"domain_scores_gemma":[0.9996278,0.000037177506,0.00004648239,0.000018350991,0.00023432462,0.000035898673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016001992,0.00039213017,0.00017555515,0.0015141764,0.0009111797,0.0006739663,0.0004699046,0.00026581963,0.0012567677],"category_scores_gemma":[0.0006950837,0.00020817627,0.0002746049,0.0013649552,0.00015837942,0.00044918226,0.00026091654,0.00023189813,0.00017876699],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002593629,0.00012516232,0.9446255,0.000060620558,0.00018721391,0.00009046074,0.00023474205,0.00810479,0.0159176,0.0002621883,0.001151785,0.02898048],"study_design_scores_gemma":[0.000012602977,0.0000144798005,0.9887245,0.000005119223,0.000034501594,0.000014951312,0.00012432407,0.008844441,0.0016524148,0.000023241184,0.0005397438,0.000009663213],"about_ca_topic_score_codex":0.9356917,"about_ca_topic_score_gemma":0.9702317,"teacher_disagreement_score":0.064308286,"about_ca_system_score_codex":0.0044551697,"about_ca_system_score_gemma":0.0030101775,"threshold_uncertainty_score":0.12937397},"labels":[],"label_agreement":null},{"id":"W2618616759","doi":"10.1002/2017gl072803","title":"Strain release at the trench during shallow slow slip: The example of Nicoya Peninsula, Costa Rica","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration; National Science Foundation","keywords":"Subduction; Trench; Geology; Seismology; Slip (aerodynamics); Episodic tremor and slip; Seafloor spreading; Geophysics; Tectonics","score_opus":0.05895102504109099,"score_gpt":0.2932685783590058,"score_spread":0.23431755331791485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618616759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983102,0.000050921863,0.00007462486,0.00002897677,0.0000010162297,0.000004906778,0.0002565473,0.0000130109765,0.0012597167],"genre_scores_gemma":[0.99945325,0.000034283214,0.000104849314,0.000004219773,0.0000013988516,0.000002744851,0.00018497308,0.0000018349491,0.00021228778],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.000010687832,0.000003583432,0.000017787428,0.000011951861,0.000018159872],"domain_scores_gemma":[0.999845,0.000017802917,0.00004415426,0.000018860595,0.00005648595,0.000017655986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011243087,0.00015278217,0.00012387983,0.00068161264,0.00028822065,0.0004533043,0.00020327477,0.00018104054,0.0006412339],"category_scores_gemma":[0.00041646493,0.0000628985,0.00008972715,0.000802558,0.00022690443,0.00017846058,0.00038230632,0.00010503541,0.0000903225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009833212,0.000034636763,0.9683266,0.00004295771,0.000059054353,0.0007566292,0.0012030824,0.0035886283,0.008156736,0.00018906621,0.0004945525,0.017049795],"study_design_scores_gemma":[0.0000015696528,0.000006451332,0.99558324,0.0000059065965,0.000007667527,0.000052281783,0.0005954802,0.0028767148,0.00033704174,0.000015877655,0.00051383907,0.000003936526],"about_ca_topic_score_codex":0.20716245,"about_ca_topic_score_gemma":0.31279865,"teacher_disagreement_score":0.20716245,"about_ca_system_score_codex":0.00092922425,"about_ca_system_score_gemma":0.00040399306,"threshold_uncertainty_score":0.41191322},"labels":[],"label_agreement":null},{"id":"W2618937301","doi":"10.1785/0220170019","title":"A Slip Gap of the 2016<i>M</i><sub>w</sub> 6.6 Muji, Xinjiang, China, Earthquake Inferred from Sentinel‐1 TOPS Interferometry","year":2017,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Japan Aerospace Exploration Agency; National Natural Science Foundation of China; Canadian Space Agency; National Research Foundation; National Science Foundation; Earth Observatory of Singapore; European Space Agency","keywords":"China; Beijing; Citation; Icon; Library science; Geography; History; Archaeology; Computer science","score_opus":0.07301181943756802,"score_gpt":0.3033953698905699,"score_spread":0.2303835504530019,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618937301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998415,0.000031662403,0.00019799556,0.000023389248,0.00000607341,0.0000046657797,0.00084890873,0.000030971092,0.0004413305],"genre_scores_gemma":[0.9985885,0.000033602755,0.00020585948,0.00000660966,0.0000044332774,0.0000040247287,0.0009745076,0.0000030358585,0.00017936164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990153,0.000006574316,0.000009680361,0.000032898362,0.000016894719,0.00003237915],"domain_scores_gemma":[0.99986804,0.000008587969,0.000049796083,0.000018006434,0.000019932164,0.00003566757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019157592,0.00043335027,0.00023055817,0.0007575661,0.00033089606,0.0004351106,0.0003352357,0.00037165108,0.00086435],"category_scores_gemma":[0.0004153435,0.0002358957,0.00025679212,0.0007399314,0.0002597762,0.00032420983,0.00037682377,0.00015726192,0.0001962122],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035750843,0.00016153726,0.93040556,0.00009917308,0.00009059587,0.00080842077,0.00048585216,0.032990187,0.017611515,0.00035666628,0.0018681401,0.014764969],"study_design_scores_gemma":[0.000016215621,0.00006354033,0.96411663,0.00001590062,0.000036951682,0.00009318604,0.0002104527,0.032750044,0.0016567846,0.00006500101,0.00096187234,0.000013410212],"about_ca_topic_score_codex":0.025633797,"about_ca_topic_score_gemma":0.036302164,"teacher_disagreement_score":0.025633797,"about_ca_system_score_codex":0.0005203506,"about_ca_system_score_gemma":0.0005632602,"threshold_uncertainty_score":0.050969183},"labels":[],"label_agreement":null},{"id":"W2619303567","doi":"10.1093/gji/ggx204","title":"Source characteristics and geological implications of the January 2016 induced earthquake swarm near Crooked Lake, Alberta","year":2017,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Seismology; Geology; Focal mechanism; Intraplate earthquake; Earthquake swarm; Magnitude (astronomy); Epicenter; Moment magnitude scale; Borehole; Seismic moment; Fault (geology); Microseism; Tectonics; Induced seismicity; Paleontology","score_opus":0.02158850685043148,"score_gpt":0.2453180796605135,"score_spread":0.22372957281008202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619303567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972709,0.00005345004,0.00017804281,0.00006043713,0.00000430243,0.000011181856,0.00044436313,0.000021923515,0.0019554673],"genre_scores_gemma":[0.9985305,0.000059281712,0.00019382247,0.000008662496,0.0000036970948,0.0000026962762,0.0004191813,0.000004957026,0.0007771998],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998903,0.0000040756604,0.0000042636375,0.000016740529,0.000048245674,0.00003630733],"domain_scores_gemma":[0.99980706,0.000013579651,0.000044043576,0.0000073897777,0.00008534008,0.000042609674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000099347024,0.00021618839,0.00014520633,0.0010685099,0.0006750903,0.00072837766,0.0003903528,0.00022687392,0.0010090423],"category_scores_gemma":[0.0005401593,0.0001230705,0.000095901836,0.0012552226,0.00043226106,0.00012955088,0.00043673825,0.00016642871,0.0001472105],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023145706,0.00008777984,0.924181,0.00006902513,0.000041309144,0.0024025175,0.0017728776,0.007587415,0.021288866,0.00058137876,0.0016708528,0.040085442],"study_design_scores_gemma":[0.0000074024756,0.00001544669,0.9932327,0.0000094374045,0.000010985848,0.00012504813,0.0009542064,0.0043289894,0.0004908251,0.000054406904,0.00076032954,0.000010124413],"about_ca_topic_score_codex":0.79802346,"about_ca_topic_score_gemma":0.8897159,"teacher_disagreement_score":0.20197654,"about_ca_system_score_codex":0.0027229579,"about_ca_system_score_gemma":0.0027726342,"threshold_uncertainty_score":0.40633202},"labels":[],"label_agreement":null},{"id":"W2619414478","doi":"10.1002/2017jb014248","title":"Slip Behavior of the Queen Charlotte Plate Boundary Before and After the 2012, <i>M</i><sub><i>W</i></sub> 7.8 Haida Gwaii Earthquake: Evidence From Repeating Earthquakes","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geology; Subduction; Episodic tremor and slip; Slip (aerodynamics); Plate tectonics; Interplate earthquake; Thrust fault; Seismic hazard; Fault (geology); Tectonics; Engineering","score_opus":0.03465619226459602,"score_gpt":0.30047934055118847,"score_spread":0.2658231482865924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619414478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992392,0.000014920548,0.000015637228,0.000005745689,8.6955333e-7,0.0000031162392,0.0001938171,0.0000031277586,0.0005236337],"genre_scores_gemma":[0.9989668,0.000022504923,0.000050539395,0.0000042056777,0.0000013242338,0.0000051847132,0.0005494081,0.0000017547379,0.00039821962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999101,0.0000069959206,0.00000567246,0.000023805069,0.000031246647,0.000022156642],"domain_scores_gemma":[0.99935585,0.00004489079,0.00022793816,0.000033908233,0.00017100295,0.00016643583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013967163,0.00013940233,0.00025669593,0.001371957,0.00048299425,0.0005804913,0.0002391682,0.00024378428,0.0009864894],"category_scores_gemma":[0.0007716391,0.00017072995,0.00008198794,0.0012505852,0.0004135372,0.00018469103,0.0004142553,0.0001514108,0.00039550412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014449442,0.00003144144,0.9854079,0.000017945538,0.0000202614,0.00034640828,0.0011230846,0.0005130764,0.0056961044,0.000035876343,0.00044384977,0.006219629],"study_design_scores_gemma":[0.0000010836774,0.000008290278,0.99945575,0.0000020668633,0.0000012481642,0.000020620506,0.00015013409,0.00017432343,0.000095179,0.0000025372253,0.000087298016,0.0000015059195],"about_ca_topic_score_codex":0.12726489,"about_ca_topic_score_gemma":0.26483414,"teacher_disagreement_score":0.87273514,"about_ca_system_score_codex":0.00094021164,"about_ca_system_score_gemma":0.0005302123,"threshold_uncertainty_score":0.25304824},"labels":[],"label_agreement":null},{"id":"W2621812869","doi":"10.1002/2017gc006915","title":"Human‐induced seismicity and large‐scale hydrocarbon production in the <scp>USA</scp> and <scp>C</scp>anada","year":2017,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Microseismic Industry Consortium","keywords":"Induced seismicity; Geology; Seismology; Seismic hazard; Tectonics; Hydraulic fracturing; Fault (geology); Magnitude (astronomy); Hydrology (agriculture); Geochemistry; Geotechnical engineering","score_opus":0.014608463989504937,"score_gpt":0.21678167441355892,"score_spread":0.20217321042405398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2621812869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99729496,0.000023658928,0.00003793891,0.00004886551,0.0000027210688,0.000004030724,0.0014418889,0.0000043527775,0.0011415209],"genre_scores_gemma":[0.9985306,0.00004858496,0.00005216508,0.000015413027,0.0000023729742,0.0000049554474,0.00110064,0.0000012896962,0.00024391673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992037,0.000012353036,0.000005347684,0.000014280551,0.000021662358,0.000025891062],"domain_scores_gemma":[0.9994677,0.000059033006,0.00013388607,0.000021862657,0.00022405772,0.00009339243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014012332,0.000116000054,0.000085876,0.0006906116,0.00047237484,0.00043833614,0.00021715047,0.00014291087,0.0010735262],"category_scores_gemma":[0.00053444295,0.000079256235,0.00013800134,0.0013275228,0.00025984185,0.00014100337,0.00027066565,0.00022353101,0.00010721708],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027332044,0.000026006033,0.99624807,0.0000083091345,0.000037929236,0.00004145271,0.00014005213,0.00029084532,0.00034110085,0.00004582397,0.0007459624,0.0020471178],"study_design_scores_gemma":[0.0000014347322,0.0000063321468,0.9988071,0.0000036862452,0.000005615302,0.000011700004,0.00041331424,0.00029937146,0.00006152796,0.0000073150513,0.0003805794,0.0000021182743],"about_ca_topic_score_codex":0.76088405,"about_ca_topic_score_gemma":0.89357054,"teacher_disagreement_score":0.23911595,"about_ca_system_score_codex":0.0019885208,"about_ca_system_score_gemma":0.001979634,"threshold_uncertainty_score":0.4810483},"labels":[],"label_agreement":null},{"id":"W2622997065","doi":"10.1002/2016tc004427","title":"Kinematic evidence for the effect of changing plate boundary conditions on the tectonics of the northern U.S. Rockies","year":2017,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; National Science Foundation","keywords":"Geology; Basin and Range Province; Tectonics; Seismology; Geodesy; Kinematics; Geodetic datum; Slip (aerodynamics); Fault (geology); Crust; Vergence (optics); Plate tectonics; Basin and range topography; Sinistral and dextral; Geomorphology; Paleontology","score_opus":0.04260397432884514,"score_gpt":0.2824655537280787,"score_spread":0.23986157939923355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2622997065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99888486,0.0000348573,0.000022313821,0.000024126946,8.270255e-7,0.000001203003,0.00012456051,0.0000018506103,0.00090546533],"genre_scores_gemma":[0.9996911,0.000030328078,0.000041894113,0.0000063430357,9.287722e-7,9.308311e-7,0.00015168796,9.347568e-7,0.00007595853],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998504,0.000034763787,0.000011976442,0.000034908,0.00003770699,0.000030375633],"domain_scores_gemma":[0.999209,0.0001341736,0.0003490313,0.000059143713,0.0001577835,0.00009087199],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027755607,0.00012174255,0.00014415027,0.00065050053,0.0003919799,0.00056904374,0.0002151762,0.0001410951,0.0015962367],"category_scores_gemma":[0.0015162858,0.00014209002,0.00011818418,0.00093759596,0.0006645382,0.00022147973,0.00027463055,0.00015963527,0.0001150406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008659783,0.000018567858,0.99117273,0.000008921046,0.000029483832,0.00006610824,0.0004073259,0.00057170703,0.002213542,0.00010601225,0.00010925943,0.0052097724],"study_design_scores_gemma":[9.873543e-7,0.000005251829,0.9996383,0.0000019319348,0.0000036361428,0.0000072722755,0.0001114252,0.000081150116,0.00008042382,0.000006883282,0.00006183226,8.7891675e-7],"about_ca_topic_score_codex":0.45710787,"about_ca_topic_score_gemma":0.66455066,"teacher_disagreement_score":0.45710787,"about_ca_system_score_codex":0.0012121912,"about_ca_system_score_gemma":0.0010983183,"threshold_uncertainty_score":0.9088944},"labels":[],"label_agreement":null},{"id":"W2626219529","doi":"10.1126/science.aan3120","title":"Recurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrust","year":2017,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":338,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Geomechanica (Canada)","funders":"Japan Society for the Promotion of Science; National Science Foundation","keywords":"Episodic tremor and slip; Trench; Subduction; Seismology; Slip (aerodynamics); Geology; Tectonics; Materials science; Physics","score_opus":0.027783086501551316,"score_gpt":0.2516006640713504,"score_spread":0.2238175775697991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2626219529","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999348,0.00001748078,0.000042549345,0.0000085429,0.0000013396876,0.00000244275,0.000042886215,0.0000030413098,0.00053388235],"genre_scores_gemma":[0.9996221,0.00001740158,0.000051264316,0.0000024212673,0.0000012172899,0.0000011966132,0.00005043614,5.775202e-7,0.00025350935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994934,0.000005656357,0.0000031734553,0.000011535281,0.000012833473,0.0000174308],"domain_scores_gemma":[0.9999124,0.0000063645234,0.000035208745,0.0000051165453,0.000016181823,0.000024811574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008718442,0.00013816236,0.00010344128,0.00038805872,0.00041472903,0.00028339983,0.0002106869,0.0001996345,0.0009566365],"category_scores_gemma":[0.0002354234,0.000110037196,0.00006939745,0.00034395602,0.00024158933,0.00017421842,0.0004255867,0.00012432787,0.000098135424],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086699365,0.000044380296,0.9624482,0.00006676633,0.00004110037,0.0019742511,0.00186315,0.0020077252,0.017020991,0.0002909114,0.0003240691,0.013831696],"study_design_scores_gemma":[0.0000024909298,0.000023184086,0.9985195,0.0000027287338,0.000004333024,0.00006891679,0.00036118232,0.0005918181,0.00015536163,0.000029193672,0.00023893798,0.0000023796238],"about_ca_topic_score_codex":0.018064404,"about_ca_topic_score_gemma":0.07899174,"teacher_disagreement_score":0.018064404,"about_ca_system_score_codex":0.0003665948,"about_ca_system_score_gemma":0.0002975318,"threshold_uncertainty_score":0.035918534},"labels":[],"label_agreement":null},{"id":"W2626468894","doi":"10.1785/0120170015","title":"Multichannel Deconvolution for Earthquake Apparent Source Time Functions","year":2017,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Deconvolution; Seismogram; Seismology; Geology; Function (biology); Scaling; Toeplitz matrix; Algorithm; Mathematics; Geometry; Pure mathematics","score_opus":0.022026467293618502,"score_gpt":0.22335728711194988,"score_spread":0.20133081981833137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2626468894","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05063635,0.00014179316,0.9461601,0.00010843701,0.000035973124,0.000030349025,0.00020230377,0.0005116204,0.0021729989],"genre_scores_gemma":[0.3510749,0.0001581659,0.64351875,0.000059548387,0.000031670126,0.000057764788,0.0004343525,0.0001917953,0.0044730306],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999008,0.000019949477,0.0000055462347,0.000026202892,0.000035554764,0.000011905176],"domain_scores_gemma":[0.99959105,0.00020474293,0.000045335943,0.00004467898,0.000098087046,0.000016189217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054609973,0.00052452384,0.00030825252,0.000495548,0.00022358516,0.0003334733,0.00037196226,0.0004729371,0.0029769214],"category_scores_gemma":[0.001464923,0.00017458512,0.00040430378,0.0004080645,0.00027508655,0.0004527082,0.00041376374,0.0004478558,0.00040466487],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027161778,0.0001103998,0.0036629764,0.0001660265,0.00007030426,0.00016209127,0.00012051656,0.5697803,0.07102197,0.018411646,0.0038486782,0.3323735],"study_design_scores_gemma":[0.0000072503103,0.000014513744,0.0006940148,0.000003548313,0.0000042293955,0.000022504099,0.00000940383,0.98825896,0.007848757,0.00196933,0.0011583423,0.000009151216],"about_ca_topic_score_codex":0.0046654106,"about_ca_topic_score_gemma":0.007072071,"teacher_disagreement_score":0.0046654106,"about_ca_system_score_codex":0.00045938647,"about_ca_system_score_gemma":0.0009416936,"threshold_uncertainty_score":0.009958804},"labels":[],"label_agreement":null},{"id":"W2724561890","doi":"10.1016/0967-0653(96)83892-0","title":"10.1016/0967-0653(96)83892-0","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Volcano; Geology; Seismology; Explosive eruption; Submarine; Magma; Volcanism; Explosive material; Submarine volcano; Tectonics; Geography; Oceanography; Archaeology","score_opus":0.008540752887929742,"score_gpt":0.16296863133201872,"score_spread":0.15442787844408898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2724561890","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004692972,0.00034797532,0.00043944095,0.00038993004,0.00025921603,0.00016003041,0.0006971424,0.0007288317,0.99650806],"genre_scores_gemma":[0.00063235173,0.0002555462,0.00029222923,0.00036881445,0.00007561658,0.000074917516,0.0003746144,0.00017047075,0.9977556],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990841,0.00006980426,0.00008977981,0.00033787003,0.00019464365,0.00022380178],"domain_scores_gemma":[0.99735224,0.0005856433,0.0001376603,0.0003453141,0.0006287147,0.0009504324],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0014491293,0.003960827,0.002296643,0.003436926,0.003217862,0.004851518,0.003920797,0.007979848,0.9924597],"category_scores_gemma":[0.0017638928,0.0014641192,0.0017339381,0.0024142105,0.0030431007,0.007641595,0.0044033164,0.0034387035,0.99419975],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004507591,0.00052620884,0.0015814188,0.0008548955,0.000059908594,0.00058433117,0.00018328252,0.00047718541,0.0027969433,0.0046122815,0.4209274,0.5669453],"study_design_scores_gemma":[0.000079904916,0.00016020284,0.0012264333,0.000620248,0.000017679808,0.000504927,0.00022359616,0.00018214317,0.0003048358,0.0006443878,0.9960019,0.0000338605],"about_ca_topic_score_codex":0.0046652644,"about_ca_topic_score_gemma":0.004738107,"teacher_disagreement_score":0.007979848,"about_ca_system_score_codex":0.0012701881,"about_ca_system_score_gemma":0.0010489024,"threshold_uncertainty_score":0.0107553005},"labels":[],"label_agreement":null},{"id":"W2725585300","doi":"10.1002/2017jb014035","title":"Large and primarily updip afterslip following the 2012 <i>M</i><sub><i>w</i></sub> 7.6 Nicoya, Costa Rica, earthquake","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Earth Sciences; National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; College of Computing; National Science Foundation","keywords":"Geology; Seismology; Slip (aerodynamics); Moment magnitude scale; Geodesy; Aftershock; Geometry; Physics","score_opus":0.03253951993068241,"score_gpt":0.30651117599316546,"score_spread":0.2739716560624831,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2725585300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976647,0.000044650067,0.00013580701,0.000027736605,0.000004258827,0.0000072069874,0.00047782695,0.000031195876,0.0016064753],"genre_scores_gemma":[0.9990103,0.000030586343,0.00008682896,0.000011328966,0.0000047812478,0.000006012857,0.00048447313,0.000004025907,0.00036173157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999261,0.0000057014468,0.000004225616,0.000016293854,0.000022088429,0.000025637984],"domain_scores_gemma":[0.99983513,0.000010212447,0.000064142296,0.000020289066,0.000046956517,0.000023204166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000812113,0.00018182333,0.00019021753,0.00040087508,0.00028747364,0.00036764052,0.00020202347,0.00022533597,0.0007432742],"category_scores_gemma":[0.00028364366,0.000113861504,0.00013034404,0.0003961605,0.00018231844,0.00012657193,0.0003228219,0.00020293491,0.00015063504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000182224,0.00007432782,0.93734545,0.000056708337,0.00010189634,0.0005878794,0.00047164128,0.0025841792,0.037116386,0.00014066805,0.0016609154,0.019677801],"study_design_scores_gemma":[9.544693e-7,0.0000087064,0.9988047,0.0000023777534,0.0000036903589,0.00002174802,0.00005990527,0.00040013817,0.00038517313,0.0000035311814,0.00030743054,0.0000016985132],"about_ca_topic_score_codex":0.04642305,"about_ca_topic_score_gemma":0.11449955,"teacher_disagreement_score":0.04642305,"about_ca_system_score_codex":0.00051421917,"about_ca_system_score_gemma":0.00028643294,"threshold_uncertainty_score":0.09230566},"labels":[],"label_agreement":null},{"id":"W2727893482","doi":"10.1190/microseismic2017-011","title":"Hydraulic fracturing induced seismicity in western Canada: insights from focal mechanism and swarm analysis","year":2017,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Induced seismicity; Hydraulic fracturing; Swarm behaviour; Mechanism (biology); Focal mechanism; Geology; Seismology; Computer science; Petroleum engineering; Artificial intelligence; Physics","score_opus":0.019860277721905753,"score_gpt":0.21484173165384832,"score_spread":0.19498145393194255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2727893482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979552,0.00007026125,0.00014545176,0.00003270195,0.0000010466789,0.0000074297454,0.0007105409,0.0000120267505,0.0010653643],"genre_scores_gemma":[0.99864525,0.00008342845,0.00015746141,0.0000061316528,0.0000010347046,0.0000028394456,0.0005991659,0.0000036046608,0.0005011021],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998894,0.0000040530826,0.000005540065,0.000019422929,0.00003507568,0.000046580164],"domain_scores_gemma":[0.99965906,0.000022803719,0.00006461821,0.000013877638,0.00016277614,0.00007691919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013370797,0.00022347046,0.00017185397,0.0016623979,0.0007617024,0.0005959509,0.00041657788,0.00016562309,0.0011895008],"category_scores_gemma":[0.00059081404,0.00013100955,0.00015757083,0.0027477017,0.000362123,0.00018454967,0.00047875658,0.00015079472,0.00010362174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000778691,0.000038522092,0.96813893,0.000042170675,0.00006145243,0.00035094994,0.0015110422,0.0024265442,0.005636942,0.0004537707,0.0008324642,0.020429363],"study_design_scores_gemma":[0.0000028192285,0.000007025185,0.9954782,0.000005686163,0.000016715241,0.00002978149,0.0010018055,0.002553977,0.00028459044,0.000038200058,0.0005744673,0.000006671927],"about_ca_topic_score_codex":0.9751703,"about_ca_topic_score_gemma":0.98942953,"teacher_disagreement_score":0.024829686,"about_ca_system_score_codex":0.006293169,"about_ca_system_score_gemma":0.0059071616,"threshold_uncertainty_score":0.04995179},"labels":[],"label_agreement":null},{"id":"W2730270853","doi":"10.1007/s00024-017-1593-z","title":"The 2011 Tohoku Tsunami on the Coast of Mexico: A Case Study","year":2017,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Russian Science Foundation; Universidad Nacional Autónoma de México; Centro de Investigación Científica y de Educación Superior de Ensenada, Baja California; Instituto Politécnico Nacional","keywords":"Geology; Seismology; Tsunami earthquake; Tsunami wave; Tide gauge; Pacific ocean; Oceanography; Infragravity wave; Climatology; Sea level; Wave propagation","score_opus":0.021508289011803863,"score_gpt":0.22685565197359037,"score_spread":0.20534736296178652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2730270853","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99664307,0.0002164078,0.00006197409,0.0003219446,0.000006026775,0.000016593693,0.0001548012,0.0000025885508,0.002576509],"genre_scores_gemma":[0.9973423,0.00090363564,0.00014275154,0.00005100069,0.0000096784015,0.000017481601,0.00019731466,0.000003240217,0.001332674],"study_design_codex":"observational","study_design_gemma":"case_report","domain_scores_codex":[0.9998549,0.000026306123,0.0000072844796,0.000017807575,0.000016134436,0.00007756015],"domain_scores_gemma":[0.9996136,0.00009770395,0.00014448717,0.000019170167,0.000051647967,0.00007344837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019112727,0.0003788305,0.00022668882,0.00090213935,0.0026903169,0.00094605924,0.0005084879,0.0016265134,0.0018872521],"category_scores_gemma":[0.0010092421,0.00018480183,0.0002265903,0.0018970077,0.00074473163,0.00069256214,0.0009885691,0.0005181676,0.00012614108],"study_design_candidate":"case_report","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005260284,0.0007593096,0.7908685,0.000537991,0.00028750728,0.111252286,0.041450914,0.0073533156,0.0032728275,0.0037298703,0.0073776823,0.03258376],"study_design_scores_gemma":[0.00004806416,0.00020147495,0.7724457,0.00026895525,0.00024371242,0.009192131,0.19879681,0.002735909,0.00059305545,0.000534305,0.0148889925,0.000050876715],"about_ca_topic_score_codex":0.2205664,"about_ca_topic_score_gemma":0.41957894,"teacher_disagreement_score":0.2205664,"about_ca_system_score_codex":0.0030681037,"about_ca_system_score_gemma":0.0013492107,"threshold_uncertainty_score":0.43856514},"labels":[],"label_agreement":null},{"id":"W2732019400","doi":"10.1002/2016jb013828","title":"Grain size‐dependent strength of phyllosilicate‐rich gouges in the shallow crust: Insights from the SAFOD site","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of New Brunswick","funders":"","keywords":"Geology; Brittleness; Grain size; Creep; Quartz; Pressure solution; Deformation (meteorology); Fault gouge; Mineralogy; Slip (aerodynamics); Strain rate; Diffusion creep; Petrology; Fault (geology); Seismology; Composite material; Diagenesis; Materials science; Grain boundary; Geomorphology; Microstructure","score_opus":0.04733484949062085,"score_gpt":0.32450157419461756,"score_spread":0.2771667247039967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2732019400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943894,0.000052164152,0.000046597073,0.000012453164,7.472768e-7,0.0000017905344,0.00013989037,0.0000061667865,0.00030130395],"genre_scores_gemma":[0.9995758,0.00004071568,0.0000771433,0.000009119193,0.000001385825,0.0000014313836,0.00013805131,0.000004276918,0.00015199874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999114,0.0000056205354,0.000006632001,0.000035910638,0.0000223021,0.00001803377],"domain_scores_gemma":[0.9997961,0.000022881351,0.00006242271,0.000013697889,0.000054945136,0.000049890135],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016765163,0.00027861155,0.0003564563,0.0012957397,0.00041875898,0.0004951939,0.00031327907,0.00037095623,0.0013365512],"category_scores_gemma":[0.0003644078,0.0002922411,0.00018485454,0.00059448194,0.00050109735,0.00031008918,0.00047284135,0.00017508274,0.00029817782],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001448325,0.000044565775,0.89898556,0.00006341284,0.000070985225,0.0003401492,0.00086300704,0.0006735231,0.09408638,0.000087205226,0.00010777182,0.0045325793],"study_design_scores_gemma":[0.0000030174904,0.000018092393,0.9980386,0.0000029292742,0.0000073490546,0.000057288584,0.00020810925,0.00040351652,0.001050384,0.00001776409,0.00018921206,0.0000037946181],"about_ca_topic_score_codex":0.029673003,"about_ca_topic_score_gemma":0.071279645,"teacher_disagreement_score":0.029673003,"about_ca_system_score_codex":0.00057607394,"about_ca_system_score_gemma":0.00021323595,"threshold_uncertainty_score":0.05900061},"labels":[],"label_agreement":null},{"id":"W2734613673","doi":"10.1002/2017gl073597","title":"Thermal structure of the Kanto region, Japan","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Slab; Mantle wedge; Subduction; Forearc; Seismology; Mantle (geology); Pacific Plate; Volcanic arc; Thermal; Geophysics; Tectonics","score_opus":0.04249591997501954,"score_gpt":0.2877568427443841,"score_spread":0.2452609227693646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2734613673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99674475,0.00010969023,0.0010053519,0.000095948904,0.000005400924,0.000006893546,0.00028063403,0.000036704918,0.001714558],"genre_scores_gemma":[0.99911577,0.000057814777,0.0003396965,0.000011935215,0.000002876875,0.0000103264465,0.00020745437,0.0000057009947,0.00024841187],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993527,0.000010663827,0.0000038868166,0.000023163526,0.000007379274,0.000019572317],"domain_scores_gemma":[0.9999131,0.000011398892,0.00001761828,0.000009005328,0.00002109845,0.000027774151],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008225828,0.0004252242,0.00032098487,0.00044445304,0.00086402183,0.0008966355,0.0004389215,0.00053637044,0.0009862492],"category_scores_gemma":[0.00022870219,0.00041927022,0.00060463045,0.0006752274,0.0005881495,0.0005179205,0.00060693384,0.00024874776,0.00013150118],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028564525,0.000093899915,0.16867298,0.00010173269,0.00020247458,0.00051007775,0.00074968603,0.8145931,0.0073219314,0.0022309185,0.00066941435,0.004568097],"study_design_scores_gemma":[0.00010588935,0.00006627498,0.16212256,0.000021178232,0.00013294285,0.00011551212,0.0006914447,0.833592,0.0007585179,0.0012616166,0.0010385572,0.000093525035],"about_ca_topic_score_codex":0.10836501,"about_ca_topic_score_gemma":0.07081199,"teacher_disagreement_score":0.10836501,"about_ca_system_score_codex":0.0013473096,"about_ca_system_score_gemma":0.0012131019,"threshold_uncertainty_score":0.21546847},"labels":[],"label_agreement":null},{"id":"W2736214231","doi":"10.1785/0120170032","title":"Frequency‐Dependent Coda Amplitude Decays in the Region of Himalaya, India","year":2017,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Coda; Amplitude; Geology; Seismology; Physics; Optics","score_opus":0.026380711399513652,"score_gpt":0.23350090927625572,"score_spread":0.20712019787674207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2736214231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782276,0.000064162516,0.0001326407,0.00002518083,0.0000020791506,0.0000032240346,0.0015250439,0.000030468518,0.0003945336],"genre_scores_gemma":[0.9963727,0.00005095033,0.0001351387,0.0000064107007,0.0000040134746,0.0000030468416,0.0032647839,0.0000045488296,0.00015847998],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975866,0.00003740894,0.000023733757,0.00006611555,0.000056476176,0.00005759226],"domain_scores_gemma":[0.99870586,0.00031052722,0.00026000213,0.00025965468,0.0003408728,0.00012312413],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033347678,0.000256365,0.00026738667,0.0017891651,0.00027039924,0.0010077218,0.0003536093,0.00020818438,0.00064000674],"category_scores_gemma":[0.0015499259,0.00017176273,0.00024959707,0.002173699,0.00032040733,0.00032736265,0.0004398813,0.00020750999,0.00036467385],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016554567,0.000038820217,0.97798824,0.000059761143,0.00013553968,0.0003495666,0.0004674708,0.0036108189,0.0054437104,0.00012876428,0.0007768532,0.010834947],"study_design_scores_gemma":[0.000002325999,0.000011408586,0.99567527,0.000004353349,0.000016659882,0.00007539641,0.00025815258,0.003230151,0.0004146821,0.000016225358,0.0002892617,0.0000060684115],"about_ca_topic_score_codex":0.04882879,"about_ca_topic_score_gemma":0.04232866,"teacher_disagreement_score":0.04882879,"about_ca_system_score_codex":0.0005053677,"about_ca_system_score_gemma":0.00035068157,"threshold_uncertainty_score":0.09708911},"labels":[],"label_agreement":null},{"id":"W2736681395","doi":"10.1002/2017gl073744","title":"Links between clay transformation and earthquakes along the Costa Rican subduction margin","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada); University of Calgary","funders":"United States Science Support Program; National Science Foundation","keywords":"Geology; Subduction; Slip (aerodynamics); Lithification; Trench; Clay minerals; Seismology; Tectonics; Sediment; Geochemistry; Geomorphology","score_opus":0.054938431841057705,"score_gpt":0.30549704570654757,"score_spread":0.25055861386548983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2736681395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99950254,0.000020740497,0.000044326855,0.000016281452,1.8999164e-7,9.821641e-7,0.00006585524,0.000005708317,0.0003433017],"genre_scores_gemma":[0.9999025,0.00000774813,0.000015992258,0.0000012496752,2.9661106e-7,3.903124e-7,0.000034352208,7.302107e-7,0.000036835885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.00001325656,0.000004264113,0.000015702788,0.000012090685,0.000014634362],"domain_scores_gemma":[0.99975246,0.00004759675,0.00010234216,0.00002703622,0.000045365927,0.000025160329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014448026,0.00012215595,0.000096279626,0.0005172508,0.00015115042,0.00035017694,0.00014134408,0.00015488487,0.0006382074],"category_scores_gemma":[0.0006576615,0.00009341706,0.00011891286,0.000526301,0.00025286278,0.00013369381,0.00037435425,0.00009203504,0.00007996224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005916996,0.000010476999,0.9879006,0.000009633877,0.000037464444,0.0000843566,0.00034668564,0.0044618472,0.003157482,0.00014266075,0.00007671817,0.0037128853],"study_design_scores_gemma":[0.0000013039063,0.0000036457286,0.9968629,0.0000018043845,0.000002680545,0.000014342828,0.00010184172,0.0027284098,0.00014353891,0.000020567128,0.000117518735,0.0000015016503],"about_ca_topic_score_codex":0.043818567,"about_ca_topic_score_gemma":0.061658,"teacher_disagreement_score":0.043818567,"about_ca_system_score_codex":0.00059301674,"about_ca_system_score_gemma":0.00018360854,"threshold_uncertainty_score":0.08712703},"labels":[],"label_agreement":null},{"id":"W2738023380","doi":"10.1007/s11430-017-9063-0","title":"Induced earthquakes in the development of unconventional energy resources","year":2017,"lang":"en","type":"article","venue":"Science China Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Hazard; Energy resources; Seismic hazard; Climate change; Natural resource economics; Government (linguistics); Environmental science; Environmental planning; Geology; Business; Seismology; Environmental protection; Economics; Ecology","score_opus":0.04149525336907186,"score_gpt":0.26762022785977313,"score_spread":0.22612497449070126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2738023380","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922746,0.0007455456,0.0003140749,0.00030002207,0.000015901149,0.000005623027,0.00006795093,0.0000036862716,0.0062725577],"genre_scores_gemma":[0.9990939,0.000323904,0.000047482412,0.000014715398,0.0000045717093,0.0000013452315,0.000020155232,5.6276673e-7,0.0004934441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998894,0.000027648439,0.000010678634,0.000013156331,0.00002438059,0.00003470598],"domain_scores_gemma":[0.9997683,0.000049752245,0.00009025866,0.000009960313,0.00004618454,0.000035470643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022886535,0.00013193676,0.00008371744,0.00057272066,0.0002651787,0.0005752751,0.00017334057,0.00027501676,0.0013121264],"category_scores_gemma":[0.00050517457,0.000067772904,0.000100329045,0.00077738566,0.00033943652,0.00038327993,0.0004757427,0.0002737637,0.00006424194],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045550277,0.00037155361,0.8456144,0.0003602839,0.00017702983,0.0039664186,0.0038135073,0.013374693,0.013025246,0.04772495,0.0023206605,0.06879579],"study_design_scores_gemma":[0.000013057189,0.00011847446,0.9740316,0.00005306045,0.00005894765,0.00032625295,0.005870031,0.005454024,0.0014461823,0.005967002,0.0066449977,0.000016437409],"about_ca_topic_score_codex":0.0058628474,"about_ca_topic_score_gemma":0.011906072,"teacher_disagreement_score":0.0058628474,"about_ca_system_score_codex":0.0010458875,"about_ca_system_score_gemma":0.000712282,"threshold_uncertainty_score":0.011657476},"labels":[],"label_agreement":null},{"id":"W2738231860","doi":"10.1016/j.epsl.2017.06.048","title":"Highly variable coastal deformation in the 2016 MW7.8 Kaikōura earthquake reflects rupture complexity along a transpressional plate boundary","year":2017,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":194,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Ministry of Business, Innovation and Employment; Natural Hazards Research Platform; Genome Institute of Singapore; Serono Symposia International Foundation; Earthquake Commission; National Science Foundation","keywords":"Geology; Seismology; Submarine pipeline; Slip (aerodynamics); Earthquake rupture; Deformation (meteorology); Geodesy; Lidar; Fault (geology); Remote sensing; Oceanography","score_opus":0.023330229336718224,"score_gpt":0.22734217643350235,"score_spread":0.20401194709678414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2738231860","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991517,0.000021980997,0.00008767815,0.000017378388,0.0000021824035,0.0000017030975,0.00013696981,0.0000040319405,0.0005763791],"genre_scores_gemma":[0.9994821,0.00002278762,0.00007546932,0.0000060816815,0.0000022545353,0.0000020860393,0.00024673963,0.0000028590214,0.00015961213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998921,0.000007892665,0.000013255103,0.000033482345,0.00002260162,0.00003059764],"domain_scores_gemma":[0.99972516,0.000022135902,0.0001422326,0.000025716156,0.000038057042,0.000046782046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014308402,0.00024137036,0.00026597656,0.00082596485,0.00037956054,0.0006038038,0.00014338779,0.00029658727,0.000841596],"category_scores_gemma":[0.00046269907,0.00021806962,0.00023270215,0.001162086,0.00045977772,0.00045805826,0.00069524936,0.0002590209,0.00023808226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025548085,0.000038435974,0.95655245,0.00003710309,0.000057955225,0.0004198381,0.0009835358,0.00094058504,0.027746111,0.00019047057,0.00036333108,0.012414729],"study_design_scores_gemma":[0.0000011560962,0.000010507446,0.99906415,0.0000023838757,0.000004830925,0.000054961594,0.00018431568,0.00027149217,0.00027313683,0.000038284943,0.000090107045,0.000004497329],"about_ca_topic_score_codex":0.0048002256,"about_ca_topic_score_gemma":0.016686307,"teacher_disagreement_score":0.0048002256,"about_ca_system_score_codex":0.00036657244,"about_ca_system_score_gemma":0.0002119773,"threshold_uncertainty_score":0.009544551},"labels":[],"label_agreement":null},{"id":"W2738929223","doi":"10.1007/s00024-017-1619-6","title":"Tsunami Detection by High Frequency Radar Beyond the Continental Shelf: II. Extension of Time Correlation Algorithm and Validation on Realistic Case Studies","year":2017,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society","funders":"","keywords":"Radar; Geology; Algorithm; Remote sensing; Doppler effect; SIGNAL (programming language); Geodesy; Computer science; Seismology; Telecommunications; Physics","score_opus":0.009428165108398945,"score_gpt":0.21351649141910423,"score_spread":0.20408832631070528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2738929223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9363834,0.00030802097,0.060761373,0.0001652111,0.000027078653,0.000102159465,0.00026793146,0.00018418665,0.0018004931],"genre_scores_gemma":[0.9831849,0.00013637883,0.016105764,0.000016756887,0.000007917643,0.00002626289,0.00023152166,0.000018728973,0.0002717903],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99913603,0.0004545233,0.000058167912,0.00012973478,0.00012657813,0.000095063384],"domain_scores_gemma":[0.99476236,0.0036403947,0.0003065498,0.00044867408,0.00074643246,0.00009566735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028263773,0.00076017744,0.0005199153,0.00067143876,0.0003418418,0.0008573344,0.00084921083,0.001452147,0.0007140263],"category_scores_gemma":[0.0073843757,0.0003006043,0.000498847,0.0006889123,0.00059115567,0.00089472433,0.000675331,0.0005805248,0.00012520039],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034063446,0.00029852078,0.015976122,0.00012227526,0.000054748856,0.00036710908,0.00009167571,0.95445937,0.005078751,0.00095396186,0.0003751291,0.021881752],"study_design_scores_gemma":[0.000034677047,0.000101808815,0.0043614847,0.000012972109,0.00001712485,0.000066619206,0.000036296206,0.9926207,0.002381535,0.00022574546,0.00012914668,0.000011883188],"about_ca_topic_score_codex":0.013359548,"about_ca_topic_score_gemma":0.008065504,"teacher_disagreement_score":0.013359548,"about_ca_system_score_codex":0.0006336029,"about_ca_system_score_gemma":0.0006410272,"threshold_uncertainty_score":0.026563585},"labels":[],"label_agreement":null},{"id":"W2740912949","doi":"10.1140/epjst/e2017-70072-4","title":"Are triggering rates of labquakes universal? Inferring triggering rates from incomplete information","year":2017,"lang":"en","type":"article","venue":"The European Physical Journal Special Topics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Aftershock; Geology; Event (particle physics); Seismology; Sequence (biology); Physics; Astrophysics; Biology","score_opus":0.03976913491497003,"score_gpt":0.25228749877947293,"score_spread":0.2125183638645029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2740912949","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9627357,0.00047353577,0.03333161,0.00030722332,0.000021012991,0.000011752681,0.0019315467,0.00014388382,0.0010437034],"genre_scores_gemma":[0.99785596,0.000075531854,0.0012470968,0.00001628832,0.000022469758,0.000005146364,0.0006813776,0.000012142444,0.000083970604],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99895644,0.00031101328,0.00014892228,0.00032302167,0.00007597767,0.00018458269],"domain_scores_gemma":[0.9587169,0.028722143,0.0057892865,0.0048350734,0.0010833247,0.0008533271],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033529736,0.00040717682,0.0010547297,0.0018757794,0.00040633013,0.0016472129,0.0012941228,0.001221396,0.0019176559],"category_scores_gemma":[0.04240875,0.0007870455,0.0006742397,0.001770202,0.0010441327,0.0036808602,0.0013674874,0.0011554593,0.00031741802],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066865486,0.000078513964,0.8295798,0.00025701933,0.00055943645,0.0005703431,0.0006565604,0.103703,0.0038581006,0.011095721,0.0015562386,0.047416657],"study_design_scores_gemma":[0.00008067491,0.0000958381,0.43288055,0.00009756035,0.0004058569,0.0004023077,0.00046131184,0.49912047,0.0026220977,0.06230085,0.0014456452,0.000086738706],"about_ca_topic_score_codex":0.0059706154,"about_ca_topic_score_gemma":0.0071627307,"teacher_disagreement_score":0.0059706154,"about_ca_system_score_codex":0.0004998999,"about_ca_system_score_gemma":0.00053882675,"threshold_uncertainty_score":0.017732382},"labels":[],"label_agreement":null},{"id":"W2741410973","doi":"10.1002/2017gl074027","title":"The postearthquake stress state on the Tohoku megathrust as constrained by reanalysis of the JFAST breakout data","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Gordon and Betty Moore Foundation","keywords":"Geology; Breakout; Seismology; Borehole; Fault (geology); Stress (linguistics); Stress field; Subduction; Geotechnical engineering; Tectonics; Structural engineering","score_opus":0.059175216550201554,"score_gpt":0.3132076940645925,"score_spread":0.25403247751439095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2741410973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991892,0.00002484563,0.00019919456,0.000016410984,0.0000023811338,0.0000018558902,0.00037838376,0.000015839936,0.00017185324],"genre_scores_gemma":[0.99855274,0.00003668239,0.00031368888,0.00000643991,0.000003196779,0.0000036390143,0.0010086759,0.000006531026,0.00006829203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998642,0.000019936575,0.000014729623,0.000045783137,0.000025261337,0.000030008996],"domain_scores_gemma":[0.99953413,0.000048478887,0.00012207133,0.000090553294,0.00012593332,0.00007887473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039313405,0.00034615936,0.00032944654,0.000924641,0.0003035441,0.00053799816,0.00033266292,0.00026031793,0.00044129562],"category_scores_gemma":[0.00078712014,0.00022829324,0.0004906539,0.0010189615,0.00029277347,0.00048792156,0.00044569888,0.00028322724,0.00008375129],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026487524,0.00009214884,0.9384758,0.000053057258,0.0002978453,0.00027470032,0.0003797801,0.024419576,0.022781558,0.0002201506,0.0005604704,0.012180039],"study_design_scores_gemma":[0.000011631216,0.00002812931,0.9818733,0.0000059297763,0.000062709485,0.00002602521,0.00013270459,0.016476385,0.0010460331,0.00005814632,0.00026042378,0.00001847702],"about_ca_topic_score_codex":0.06779732,"about_ca_topic_score_gemma":0.113337524,"teacher_disagreement_score":0.06779732,"about_ca_system_score_codex":0.00060587557,"about_ca_system_score_gemma":0.0005684897,"threshold_uncertainty_score":0.13480538},"labels":[],"label_agreement":null},{"id":"W2742484830","doi":"10.1093/gji/ggx307","title":"Subduction and vertical coastal motions in the eastern Mediterranean","year":2017,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Episodic tremor and slip; Shear zone; Tectonics; Seismotectonics","score_opus":0.03515859107357765,"score_gpt":0.26944005507187185,"score_spread":0.2342814639982942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2742484830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99890494,0.00011983553,0.000033018696,0.000021570757,0.0000014338879,0.0000012554033,0.000043351625,0.0000037537225,0.00087078253],"genre_scores_gemma":[0.9996803,0.000061804734,0.00006153666,0.000005717096,0.0000013899474,0.0000013227994,0.00005664872,0.0000011354412,0.00013009495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995613,0.000010282742,0.000005048787,0.000013716357,0.0000070743054,0.000007883668],"domain_scores_gemma":[0.99990964,0.000012100538,0.00004244228,0.0000058710457,0.00001676384,0.000013181564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001356387,0.00013762695,0.00013005215,0.0005065367,0.0001998457,0.00045332848,0.00013799,0.00017996966,0.00078096415],"category_scores_gemma":[0.0004607137,0.00010022998,0.00012600138,0.00037918388,0.00019754426,0.00019973484,0.00029778012,0.00008329794,0.00013198634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010135639,0.000025478746,0.9696913,0.000022586462,0.00007502817,0.00045193994,0.0012357915,0.0016002025,0.0049787485,0.00031946885,0.00028351106,0.021214517],"study_design_scores_gemma":[0.0000061827177,0.000011522121,0.9978079,0.000007391562,0.0000058485234,0.00005835161,0.00043159755,0.0009614946,0.00006474747,0.000052389016,0.0005905445,0.000002092567],"about_ca_topic_score_codex":0.019444766,"about_ca_topic_score_gemma":0.028171284,"teacher_disagreement_score":0.019444766,"about_ca_system_score_codex":0.0005604554,"about_ca_system_score_gemma":0.00017129756,"threshold_uncertainty_score":0.03866315},"labels":[],"label_agreement":null},{"id":"W2744654333","doi":"10.1038/s41598-017-08192-7","title":"Source and dynamics of a volcanic caldera unrest: Campi Flegrei, 1983–84","year":2017,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Aberdeen; Royal Society of Edinburgh; Royal Society","keywords":"Caldera; Geology; Unrest; Seismology; Tiltmeter; Volcano; Earthquake swarm; Induced seismicity","score_opus":0.015444513515028242,"score_gpt":0.22658798207297434,"score_spread":0.2111434685579461,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2744654333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944958,0.00048489968,0.00004124675,0.0003477544,0.0000037423038,0.0000126195,0.00051388127,0.000011356949,0.004088492],"genre_scores_gemma":[0.99874854,0.00017141647,0.000049309496,0.000021423286,0.000011481657,0.000005275413,0.00051206996,0.000002268386,0.00047832303],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999069,0.000007673232,0.0000043254813,0.000026886239,0.000019873034,0.000034385037],"domain_scores_gemma":[0.99965477,0.000032237855,0.00018452333,0.000024610901,0.000054439086,0.00004941462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017982368,0.00015381534,0.00013028477,0.0010726481,0.00036163037,0.00042612295,0.00031087268,0.00043211156,0.0013215918],"category_scores_gemma":[0.00068758964,0.00011015142,0.00011184959,0.0010381542,0.00054106984,0.00022424653,0.0004169444,0.00038014466,0.00026325538],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002372926,0.00008774219,0.9521166,0.00007724546,0.000055124034,0.0013822325,0.0020212492,0.0007366372,0.004732007,0.0003439371,0.0029968075,0.03521318],"study_design_scores_gemma":[0.0000033609633,0.000010318795,0.9986563,0.0000060330026,0.000003577365,0.000091501584,0.00012573732,0.000119761266,0.00006444402,0.000011298888,0.00090622,0.0000014210408],"about_ca_topic_score_codex":0.13590875,"about_ca_topic_score_gemma":0.16671279,"teacher_disagreement_score":0.13590875,"about_ca_system_score_codex":0.0019217983,"about_ca_system_score_gemma":0.00046968245,"threshold_uncertainty_score":0.27023536},"labels":[],"label_agreement":null},{"id":"W2745230667","doi":"10.1002/2017jb014191","title":"Velocity models and hypocenter relocations for the Charlevoix Seismic Zone","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Hypocenter; Seismology; Rift; Impact structure; Devonian; Fault (geology); Basement; Shore; Tectonics; Paleontology; Induced seismicity","score_opus":0.1038744162207912,"score_gpt":0.3527415045320664,"score_spread":0.2488670883112752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2745230667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9768357,0.00007951491,0.018684609,0.000061332365,0.000008400935,0.00003865186,0.00087713916,0.0004410888,0.0029735556],"genre_scores_gemma":[0.99463236,0.000044808374,0.0033364145,0.0000035258365,0.0000022177553,0.000019703532,0.0010866987,0.000030012283,0.00084423844],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999007,0.000015138885,0.000005655974,0.000031959287,0.000026898306,0.000019598798],"domain_scores_gemma":[0.99976665,0.000040035437,0.00007535299,0.00002369342,0.00006240254,0.000031907377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002843883,0.00049376616,0.00016957561,0.001065901,0.00037733707,0.0010190124,0.00077023514,0.00034997388,0.0012347949],"category_scores_gemma":[0.0007394453,0.00023487165,0.00029631087,0.000769021,0.00022935926,0.00026744916,0.00038491996,0.0003046946,0.00032840387],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014835024,0.00005070086,0.108303204,0.000015744441,0.000018912078,0.00014221226,0.00024548417,0.86734045,0.0026764786,0.0016067319,0.0008166925,0.018634979],"study_design_scores_gemma":[0.000020286403,0.000020172158,0.024839617,0.0000063829502,0.0000043225377,0.000028062037,0.0000835436,0.97309315,0.0008122657,0.0002913726,0.00078731996,0.000013472752],"about_ca_topic_score_codex":0.13658406,"about_ca_topic_score_gemma":0.07628493,"teacher_disagreement_score":0.86341596,"about_ca_system_score_codex":0.0021210194,"about_ca_system_score_gemma":0.0010743984,"threshold_uncertainty_score":0.27157807},"labels":[],"label_agreement":null},{"id":"W2745290602","doi":"10.1103/physrevlett.119.068501","title":"Triggering Processes in Rock Fracture","year":2017,"lang":"en","type":"article","venue":"Physical Review Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Alexander von Humboldt-Stiftung","keywords":"Acoustic emission; Induced seismicity; Geology; Aftershock; Seismology; Event (particle physics); Fracture (geology); Displacement (psychology); Compression (physics); Relation (database); Physics; Geotechnical engineering; Astrophysics","score_opus":0.0245566930590273,"score_gpt":0.27848735474828845,"score_spread":0.25393066168926115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2745290602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846256,0.00010720941,0.0009544573,0.000006929816,0.0000012934537,0.000007174648,0.000031554697,0.000018540075,0.0004102563],"genre_scores_gemma":[0.99970907,0.000038595434,0.00017333703,0.000001747125,0.0000014527695,0.0000036748747,0.000020624393,0.0000010996828,0.000050317154],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999853,0.000017193257,0.000008759759,0.00004585927,0.000032773423,0.000042438867],"domain_scores_gemma":[0.9996024,0.000111039735,0.00014235503,0.0000582477,0.000040686256,0.000045271387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019739194,0.00014554788,0.0002046651,0.0004886348,0.00026177918,0.00028292954,0.00023574305,0.00024548813,0.0010313562],"category_scores_gemma":[0.00087919063,0.0001533742,0.00014949875,0.00028294546,0.00037874113,0.00030156277,0.00036994176,0.00014703894,0.00012396456],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006509701,0.00016430607,0.14159927,0.00016068033,0.000083243554,0.0010772027,0.00047943942,0.016184837,0.80752176,0.0016926685,0.00014431519,0.030241389],"study_design_scores_gemma":[0.000043489974,0.00086218695,0.75752306,0.000019039773,0.000068154724,0.000851972,0.00044435286,0.04501545,0.19268478,0.0015567266,0.0008879999,0.00004284035],"about_ca_topic_score_codex":0.0012739361,"about_ca_topic_score_gemma":0.0013722033,"teacher_disagreement_score":0.0012739361,"about_ca_system_score_codex":0.0002732612,"about_ca_system_score_gemma":0.00011169473,"threshold_uncertainty_score":0.0034502745},"labels":[],"label_agreement":null},{"id":"W2746226973","doi":"","title":"Wide angle seismic recordings from the 2002 Georgia Basin Geohazards Initiative, Northwestern Washington and British Columbia","year":2003,"lang":"en","type":"report","venue":"Helmholtz Centre for Ocean Research Kiel (GEOMAR)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Structural basin; Coast guard; Seismometer; Geological survey; Remote sensing; Geography; Paleontology","score_opus":0.05509928812835132,"score_gpt":0.27721121791009073,"score_spread":0.2221119297817394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2746226973","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9610474,0.00026738437,0.0007146642,0.00011784657,0.000018260853,0.00017734127,0.011725299,0.00017726011,0.0257545],"genre_scores_gemma":[0.9260719,0.0007559995,0.004435631,0.00019972972,0.000013967185,0.00022090004,0.026256923,0.0000908437,0.0419541],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974674,0.00001006452,0.000009633628,0.00003979631,0.00013660289,0.00005717687],"domain_scores_gemma":[0.99946696,0.000015688072,0.000025843512,0.00002130087,0.0003820857,0.00008805572],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013799989,0.00030852098,0.0001737415,0.0017428261,0.0015493657,0.00063227065,0.00039208512,0.00021467822,0.0022790376],"category_scores_gemma":[0.0003606815,0.00017400461,0.000064420215,0.003132262,0.00027381093,0.00017687884,0.00071661576,0.00031303096,0.00061106094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004729498,0.00027717877,0.5926429,0.00018376113,0.00009130715,0.0016090226,0.010600844,0.00124175,0.048913334,0.00065573154,0.046849143,0.29646212],"study_design_scores_gemma":[0.000012201639,0.000027344468,0.9657169,0.000034066292,0.00001880143,0.00010247963,0.0040215347,0.00045964684,0.0024294318,0.00003517108,0.027118511,0.00002401998],"about_ca_topic_score_codex":0.9280904,"about_ca_topic_score_gemma":0.9909066,"teacher_disagreement_score":0.07190961,"about_ca_system_score_codex":0.0030601914,"about_ca_system_score_gemma":0.005698462,"threshold_uncertainty_score":0.14466614},"labels":[],"label_agreement":null},{"id":"W2748368143","doi":"10.3133/ofr20171104","title":"Modified mercalli intensities for nine earthquakes in central and western Washington between 1989 and 1999","year":2017,"lang":"en","type":"article","venue":"Antarctica A Keystone in a Changing World","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; U.S. Geological Survey","keywords":"Mercalli intensity scale; Seismology; Geology; Geological survey; Seismic zone; Aftershock; Earthquake prediction; Induced seismicity; Peak ground acceleration; Ground motion; Geophysics","score_opus":0.03790074258265412,"score_gpt":0.26768558421899075,"score_spread":0.2297848416363366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2748368143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99453884,0.00006429594,0.00012571404,0.000031502655,0.000005764603,0.000032131404,0.001880968,0.000014213233,0.0033065013],"genre_scores_gemma":[0.9919762,0.00013711977,0.0004940025,0.000026590778,0.000021532884,0.00007754748,0.0055756364,0.000008335485,0.0016829893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980813,0.000025959012,0.00003550312,0.000040158244,0.00005600648,0.00003427528],"domain_scores_gemma":[0.99823487,0.0001370071,0.0010826592,0.000077755496,0.00033368805,0.00013401546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000298456,0.0002168484,0.00014097865,0.0020506957,0.00035649928,0.00039706298,0.00023012924,0.0002146019,0.0016823316],"category_scores_gemma":[0.0019162002,0.0001635311,0.00012716388,0.0014562766,0.00017264298,0.00037807378,0.0006032412,0.00032945597,0.0002808842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012102446,0.000042443036,0.98794633,0.00003032715,0.00003498178,0.00008688364,0.0005622551,0.00007964638,0.0007061708,0.00006364241,0.00092725665,0.009398995],"study_design_scores_gemma":[0.0000016397806,0.000015162475,0.9988444,0.0000037597824,0.000005134908,0.000046006702,0.0002581999,0.00003901575,0.00014849403,0.000008409679,0.00062753947,0.0000022622044],"about_ca_topic_score_codex":0.015550376,"about_ca_topic_score_gemma":0.051559936,"teacher_disagreement_score":0.015550376,"about_ca_system_score_codex":0.0006630152,"about_ca_system_score_gemma":0.0002006306,"threshold_uncertainty_score":0.03091973},"labels":[],"label_agreement":null},{"id":"W2749120426","doi":"10.1002/2017gl075381","title":"Mapping fluids to subduction megathrust locking and slip behavior","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Subduction; Geology; Magnetotellurics; Seismology; Episodic tremor and slip; Slip (aerodynamics); Electrical resistivity and conductivity; Thrust; Pore water pressure; Electrical conductor; Creep; Geophysics; Petrology; Geotechnical engineering; Tectonics; Materials science","score_opus":0.0751477371591958,"score_gpt":0.32332269394164453,"score_spread":0.24817495678244872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2749120426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988763,0.00013466932,0.00052296004,0.000020561885,0.0000021054786,0.0000037090877,0.00012663903,0.000021811686,0.00029124352],"genre_scores_gemma":[0.9993544,0.0000513501,0.00039431066,0.0000041334315,0.0000020376851,0.0000021503577,0.00009146205,0.0000037100317,0.00009637551],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993134,0.000012156366,0.0000051424227,0.000022502216,0.000011153968,0.000017701059],"domain_scores_gemma":[0.99966574,0.00006888124,0.00013645187,0.00002028675,0.00005457452,0.000054093096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019746498,0.0002646912,0.00019273697,0.0020696388,0.00021342676,0.0008443716,0.00018229862,0.00031319755,0.0008026697],"category_scores_gemma":[0.0009739844,0.00016325162,0.00014381131,0.0011916828,0.0003645395,0.00059802434,0.0007661953,0.00021486172,0.00022790549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004282657,0.000110032,0.8976904,0.00008151658,0.00007803345,0.00020167927,0.00090644567,0.0022143165,0.061479386,0.0003641659,0.00019539466,0.03625036],"study_design_scores_gemma":[0.000011638134,0.00008309626,0.9825173,0.000022408118,0.000034529152,0.000112024776,0.0009182151,0.00830534,0.006912331,0.00042888767,0.00064060773,0.000013560216],"about_ca_topic_score_codex":0.0026895646,"about_ca_topic_score_gemma":0.0039988784,"teacher_disagreement_score":0.0026895646,"about_ca_system_score_codex":0.00023180619,"about_ca_system_score_gemma":0.00016005212,"threshold_uncertainty_score":0.0053477883},"labels":[],"label_agreement":null},{"id":"W2749729974","doi":"10.1098/rsta.2016.0001","title":"On the effective stress law for rock-on-rock frictional sliding, and fault slip triggered by means of fluid injection","year":2017,"lang":"en","type":"article","venue":"Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Geology; Fault plane; Fault gouge; Induced seismicity; Slip (aerodynamics); Fluid pressure; Fault (geology); Geotechnical engineering; Permeability (electromagnetism); Microseism; Pore water pressure; Fluid dynamics; Hydraulic fracturing; Seismology; Mechanics; Membrane","score_opus":0.01867341773468537,"score_gpt":0.23007488133106388,"score_spread":0.2114014635963785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2749729974","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3491706,0.030866163,0.47792956,0.0073961914,0.0019973288,0.00022341976,0.0008039734,0.0005558036,0.13105704],"genre_scores_gemma":[0.94925326,0.008265781,0.01605925,0.00062592,0.00060635596,0.00015341974,0.00028905077,0.00015534268,0.024591662],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99974746,0.000043007207,0.000019120329,0.00008300147,0.00006899108,0.00003846595],"domain_scores_gemma":[0.99975973,0.00008122686,0.000050322393,0.000040334882,0.000044290795,0.000024045492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053635,0.0006268101,0.00056342664,0.0007529347,0.000323278,0.0010286572,0.00095132354,0.0009396905,0.0060956203],"category_scores_gemma":[0.0014210404,0.00027522427,0.00049993326,0.00036671976,0.0026090045,0.0014390751,0.00093580526,0.00128848,0.0011070546],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078938334,0.000070117945,0.0023016632,0.00047253323,0.00004037878,0.00073804735,0.00042591392,0.07250977,0.040258083,0.83185697,0.0059235324,0.04532397],"study_design_scores_gemma":[0.00004698993,0.00016434291,0.010277329,0.00012302707,0.00002323878,0.0006645943,0.00016223444,0.5594165,0.0054338314,0.40165478,0.021933459,0.00009967769],"about_ca_topic_score_codex":0.002827892,"about_ca_topic_score_gemma":0.0011787612,"teacher_disagreement_score":0.0060956203,"about_ca_system_score_codex":0.00085390813,"about_ca_system_score_gemma":0.00035351646,"threshold_uncertainty_score":0.020391881},"labels":[],"label_agreement":null},{"id":"W2750687209","doi":"10.1002/2017gl074095","title":"Significant lateral dip changes may have limited the scale of the 2015 <i>M</i><sub><i>w</i></sub> 7.8 Gorkha earthquake","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Japan Aerospace Exploration Agency; National Natural Science Foundation of China","keywords":"Geology; Seismology; Aftershock; Geodetic datum; Anomaly (physics); Earthquake rupture; Slip (aerodynamics); Fault (geology); Magnetic dip; Slab; Geodesy; Geophysics; Physics","score_opus":0.046186534312128075,"score_gpt":0.2847731819454449,"score_spread":0.2385866476333168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2750687209","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99546874,0.0000600973,0.0007369658,0.00009158109,0.000014282694,0.000007664379,0.0002610209,0.000054504224,0.003305144],"genre_scores_gemma":[0.9995049,0.000019491004,0.00011899129,0.000012175705,0.0000035897663,0.000002575261,0.00012037429,0.000005603049,0.00021230138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998851,0.000018709716,0.000011999367,0.000029617573,0.000014018745,0.00004048331],"domain_scores_gemma":[0.9996835,0.000050507882,0.0000980014,0.000049127524,0.00006754642,0.00005130121],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022793375,0.00019470356,0.00031352197,0.00033981522,0.00024355286,0.00065903494,0.00027838824,0.00019114897,0.0046388814],"category_scores_gemma":[0.0008585251,0.00013914362,0.0002349028,0.00038393945,0.00034153217,0.00045170292,0.00057883386,0.00029847052,0.0005811612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027653252,0.0001097554,0.8911971,0.00018199948,0.00013900062,0.0005449027,0.0004946497,0.0049802437,0.0673805,0.002029237,0.0010278716,0.031638235],"study_design_scores_gemma":[0.000011093268,0.00009585616,0.9894587,0.000016554855,0.000039556355,0.0001537152,0.00051192957,0.0047929087,0.0026922717,0.0005239005,0.0016887136,0.000014816314],"about_ca_topic_score_codex":0.0057274248,"about_ca_topic_score_gemma":0.009509079,"teacher_disagreement_score":0.0057274248,"about_ca_system_score_codex":0.00032276096,"about_ca_system_score_gemma":0.00030876254,"threshold_uncertainty_score":0.015518606},"labels":[],"label_agreement":null},{"id":"W2752064580","doi":"10.1130/b31731.1","title":"Miocene postorogenic extension of the Eocene synorogenic imbricated Hellenic subduction channel: New constraints from Milos (Cyclades, Greece)","year":2017,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geodynamics; Geology; Sedimentology; CYCLADES; Structural geology; Subduction; Paleontology; Archaeology; Geography; Geochemistry","score_opus":0.024408964105000666,"score_gpt":0.21696206663783213,"score_spread":0.19255310253283148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2752064580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93211293,0.006211375,0.00065739406,0.0030401682,0.00013843716,0.000031736257,0.0022421563,0.0000548583,0.055510968],"genre_scores_gemma":[0.99301857,0.0027342741,0.00033860424,0.00020150038,0.000080708414,0.000012466667,0.0013152177,0.000043814292,0.0022546784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998141,0.00002269584,0.000015323434,0.000051315008,0.000048974885,0.000047548278],"domain_scores_gemma":[0.9994825,0.0000808381,0.0001644072,0.00005080824,0.00014249905,0.000078851546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040205746,0.00020342309,0.00027240123,0.001836185,0.00072721037,0.0017041821,0.00034572222,0.00046841247,0.007977765],"category_scores_gemma":[0.0014959879,0.00018069026,0.00015687732,0.0028053215,0.0017142809,0.0014709311,0.0018247935,0.00050291355,0.0009570372],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010269999,0.000116711475,0.7062491,0.0013377516,0.00028754084,0.002464573,0.02027863,0.0033301385,0.009887319,0.023913855,0.020395136,0.21071228],"study_design_scores_gemma":[0.00003911474,0.000035365374,0.9391099,0.00034756341,0.00006118344,0.0002166927,0.0055012405,0.0005958456,0.0004289219,0.002503112,0.051135376,0.000025734282],"about_ca_topic_score_codex":0.028142095,"about_ca_topic_score_gemma":0.065187015,"teacher_disagreement_score":0.028142095,"about_ca_system_score_codex":0.0012152073,"about_ca_system_score_gemma":0.0010813057,"threshold_uncertainty_score":0.055956602},"labels":[],"label_agreement":null},{"id":"W2752364613","doi":"10.1016/j.epsl.2017.07.046","title":"Early Neogene foreland of the Zagros, implications for the initial closure of the Neo-Tethys and kinematics of crustal shortening","year":2017,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":172,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Foreland basin; Geology; Diachronous; Paleontology; Unconformity; Magnetostratigraphy; Molasse; Neogene; Passive margin; Mountain formation; Geomorphology; Structural basin; Tectonics; Rift","score_opus":0.02710819224346967,"score_gpt":0.24098363368089584,"score_spread":0.21387544143742618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2752364613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99617225,0.00032592216,0.00009352504,0.00013750241,0.000006672371,0.0000033802387,0.0001053959,0.0000026446262,0.0031528305],"genre_scores_gemma":[0.99881005,0.00017279181,0.000096552205,0.000014648904,0.0000027109688,0.000001139336,0.00009201871,0.0000013107287,0.0008087301],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995065,0.0000069214457,0.000005397397,0.000013111518,0.0000052083633,0.000018745484],"domain_scores_gemma":[0.9999151,0.000008331816,0.00003417052,0.000009391535,0.000017301176,0.000015610469],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017054674,0.00015524786,0.00011591061,0.0005112779,0.0006439154,0.0008606493,0.00017126149,0.00017539202,0.0022375667],"category_scores_gemma":[0.00037333302,0.00012889854,0.00009628036,0.000541026,0.0007018142,0.00048816556,0.0005833566,0.00024627324,0.00029045145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013492475,0.00009084012,0.87333125,0.00022304735,0.00006992381,0.0010820447,0.007215166,0.002984706,0.02275497,0.017382994,0.00047811738,0.07303767],"study_design_scores_gemma":[0.00001647236,0.00004541789,0.9948139,0.00003056267,0.000012847789,0.00010482165,0.0013783252,0.00038014067,0.0002915575,0.00062295666,0.0023000627,0.0000028437717],"about_ca_topic_score_codex":0.07913817,"about_ca_topic_score_gemma":0.17829229,"teacher_disagreement_score":0.07913817,"about_ca_system_score_codex":0.0014036809,"about_ca_system_score_gemma":0.00080440706,"threshold_uncertainty_score":0.15735507},"labels":[],"label_agreement":null},{"id":"W2752459840","doi":"10.1029/2017jb015394","title":"Direct Observation of Faulting by Means of Rotary Shear Tests Under X‐Ray Micro‐Computed Tomography","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Canada Foundation for Innovation; Carbon Management Canada; CMG Reservoir Simulation Foundation","keywords":"Slip (aerodynamics); Shear (geology); Surface finish; Surface roughness; Interlocking; Tomography; Contact area; Power law","score_opus":0.05064586725670303,"score_gpt":0.3174288948849649,"score_spread":0.2667830276282619,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2752459840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99727064,0.0000558792,0.0022604202,0.0000061251635,0.000002766246,0.000012891658,0.00009818279,0.000022317483,0.0002707023],"genre_scores_gemma":[0.9990073,0.000023569204,0.00083359075,0.0000028567968,0.000001449336,0.0000077683635,0.000030965155,0.0000023464077,0.00009019443],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997861,0.000028800421,0.000018701548,0.0000514312,0.000077836004,0.000037146743],"domain_scores_gemma":[0.9991929,0.0002765661,0.00021707425,0.00013059388,0.000122021054,0.00006101015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019529986,0.0002650622,0.00018427237,0.0004182062,0.00015621963,0.00024455576,0.00023081638,0.00020150404,0.0014879254],"category_scores_gemma":[0.00059520814,0.00014824898,0.00013703204,0.00025313947,0.0005663799,0.00018463575,0.00027281474,0.00022667545,0.000102076614],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012438846,0.00002792612,0.0063827774,0.000026296584,0.000006751834,0.000075992706,0.00005796545,0.00048736317,0.99061686,0.00004444734,0.000019516856,0.00212975],"study_design_scores_gemma":[0.000021933287,0.00090494496,0.1282519,0.0000072539265,0.00002368236,0.00027684117,0.00015062881,0.010077805,0.859945,0.000050863335,0.00027359056,0.000015519989],"about_ca_topic_score_codex":0.0010333428,"about_ca_topic_score_gemma":0.0012884352,"teacher_disagreement_score":0.0014879254,"about_ca_system_score_codex":0.0001318393,"about_ca_system_score_gemma":0.00010066292,"threshold_uncertainty_score":0.004977584},"labels":[],"label_agreement":null},{"id":"W2752685744","doi":"","title":"Empirical Tsunami Hazard Assessment of Near-Field Plate-Boundary and Crustal Fault Sources Demonstrated for the Pacific Coast of Canada","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Seismology; Fault (geology); Hazard; Boundary (topology); Field (mathematics)","score_opus":0.031076852729599085,"score_gpt":0.26367406249787123,"score_spread":0.23259720976827214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2752685744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99731654,0.000040913506,0.0005158482,0.000023252573,9.800253e-7,0.000010470695,0.0004532465,0.000020851523,0.0016179084],"genre_scores_gemma":[0.9987972,0.000025184876,0.00027945088,0.0000021001463,5.2613774e-7,0.0000017940903,0.0003211424,0.000002911624,0.0005697509],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998951,0.000013251805,0.000005508161,0.0000258605,0.00003460517,0.000025742122],"domain_scores_gemma":[0.9990226,0.0002184885,0.00005949884,0.000058785645,0.00056040374,0.00008016812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004281095,0.00030794324,0.00015851948,0.00089307537,0.00063054234,0.0006730462,0.0007530517,0.00024611573,0.002163351],"category_scores_gemma":[0.0020673198,0.00018807912,0.00020561022,0.0009267194,0.00040268328,0.00039152487,0.00031063627,0.00028259985,0.00014900604],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003274345,0.00016508465,0.6755532,0.00007032309,0.00010974473,0.00037416886,0.00058467174,0.28093272,0.002508021,0.0014921263,0.001584657,0.036297876],"study_design_scores_gemma":[0.00003102497,0.000045991113,0.6331885,0.000019861303,0.000048647606,0.000075649215,0.0009507971,0.3632948,0.0009797614,0.0005060613,0.00083104376,0.00002783199],"about_ca_topic_score_codex":0.93955183,"about_ca_topic_score_gemma":0.961367,"teacher_disagreement_score":0.06044817,"about_ca_system_score_codex":0.004984468,"about_ca_system_score_gemma":0.0041959393,"threshold_uncertainty_score":0.12160826},"labels":[],"label_agreement":null},{"id":"W2753057425","doi":"10.1002/2017gl074826","title":"Thermal State, Slab Metamorphism, and Interface Seismicity in the Cascadia Subduction Zone Based On 3‐D Modeling","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Subduction; Geology; Slab; Seismology; Eclogitization; Episodic tremor and slip; Metamorphism; Induced seismicity; Slab window; Geophysics; Petrology; Oceanic crust; Tectonics","score_opus":0.0629607306426964,"score_gpt":0.3067962757409377,"score_spread":0.2438355450982413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2753057425","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920568,0.00004819981,0.005433083,0.000107779604,0.000007631964,0.000012779744,0.00034442337,0.0002028984,0.0017864003],"genre_scores_gemma":[0.9983991,0.00003418802,0.0011092279,0.0000091078755,0.0000030542901,0.000012591964,0.00014749554,0.000018130715,0.0002670626],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993944,0.000015443551,0.0000050793988,0.00001772066,0.000010009224,0.000012239991],"domain_scores_gemma":[0.99977165,0.00008156971,0.000043953314,0.000025735433,0.000032162854,0.00004486469],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018426975,0.0006732556,0.00035584276,0.00072041433,0.0005012739,0.00067715964,0.00081107527,0.00087904785,0.0013519729],"category_scores_gemma":[0.0006509235,0.0006222142,0.0012479792,0.00045678354,0.00046436815,0.00030046562,0.0004792294,0.0004665876,0.00015838153],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002863813,0.00002599948,0.012532551,0.000007148487,0.000033344757,0.000052975844,0.000037795664,0.9853419,0.0010514864,0.00019792956,0.00006123204,0.00062905485],"study_design_scores_gemma":[0.0000073461024,0.0000073357833,0.004669167,0.0000016965239,0.000008270054,0.0000060701163,0.000013345276,0.9950342,0.000083349696,0.00010633487,0.00005616867,0.0000067039527],"about_ca_topic_score_codex":0.126739,"about_ca_topic_score_gemma":0.058995575,"teacher_disagreement_score":0.126739,"about_ca_system_score_codex":0.0014973312,"about_ca_system_score_gemma":0.00097418355,"threshold_uncertainty_score":0.2520026},"labels":[],"label_agreement":null},{"id":"W2753757929","doi":"","title":"The Roles of Far Field Stress and Mantle Downwelling In Intraplate Deformation: The Michigan Basin","year":2012,"lang":"en","type":"dissertation","venue":"Library and Archives Canada (Government of Canada)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Downwelling; Geology; Mantle (geology); Seismology; Stress field; Structural basin; Geophysics; Paleontology; Oceanography; Engineering; Upwelling; Tectonics","score_opus":0.002870451770923691,"score_gpt":0.13923360302121265,"score_spread":0.13636315125028897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2753757929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996424,0.000024285839,0.00006188502,0.000007750947,7.0238684e-7,0.0000020851285,0.000010290128,0.0000011980923,0.00024945327],"genre_scores_gemma":[0.99980193,0.000022235461,0.000071823444,0.00000613078,0.0000012612416,0.0000025646184,0.000012155129,6.953013e-7,0.0000811329],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999418,0.000018963317,0.000004154366,0.000016527203,0.000007262131,0.000011277702],"domain_scores_gemma":[0.9998437,0.000053068736,0.000034485158,0.000018169821,0.000011724473,0.000038909093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001510752,0.00016161188,0.00017041052,0.00026736935,0.0001870187,0.00035004577,0.00017383149,0.00027135012,0.0010069122],"category_scores_gemma":[0.0003233477,0.000092908194,0.00013994105,0.00012952505,0.0006289905,0.00025331476,0.00025575125,0.00022600881,0.00005196505],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024332486,0.0006594655,0.14118,0.00007668822,0.000089660956,0.00032811833,0.00037364181,0.0023518428,0.8370171,0.0014621207,0.000062510575,0.013965597],"study_design_scores_gemma":[0.00007620014,0.0011443098,0.95877576,0.00000681818,0.00005400153,0.00008280428,0.00030925224,0.011683186,0.0268366,0.0006372649,0.00037318384,0.000020701465],"about_ca_topic_score_codex":0.0035321938,"about_ca_topic_score_gemma":0.004422336,"teacher_disagreement_score":0.9964678,"about_ca_system_score_codex":0.0003491241,"about_ca_system_score_gemma":0.000105540224,"threshold_uncertainty_score":0.007023275},"labels":[],"label_agreement":null},{"id":"W2754165816","doi":"10.1002/2017jc013078","title":"The 2004 Sumatra tsunami in the Southeastern Pacific Ocean: New Global Insight from Observations and Modeling","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Oceans","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization","funders":"National Oceanic and Atmospheric Administration; Russell Sage Foundation","keywords":"Geology; Tide gauge; Pacific ocean; Seismology; Oceanography; Tsunami earthquake; Climatology; Sea level","score_opus":0.12178562492412105,"score_gpt":0.3307937342458439,"score_spread":0.20900810932172287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2754165816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963379,0.00019744107,0.001234012,0.00021295376,0.000008943296,0.0000094228535,0.00051657314,0.000054581473,0.0014282329],"genre_scores_gemma":[0.9978078,0.0003022137,0.0011283675,0.000016331382,0.000011890446,0.000011156402,0.00043498215,0.000012502969,0.00027471723],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999449,0.000012486055,0.0000044131025,0.000019693724,0.0000103619595,0.000008067625],"domain_scores_gemma":[0.9998673,0.000039459825,0.000040030573,0.00001936991,0.000020840043,0.0000128882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019520061,0.0005275493,0.00024295865,0.0004448468,0.00023031846,0.0008967833,0.0004284461,0.00042165347,0.0007082745],"category_scores_gemma":[0.0004820962,0.00030165276,0.0005036626,0.0008609942,0.0002854654,0.0006524866,0.00051259954,0.0003781192,0.00009049519],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009966954,0.00022132507,0.3857931,0.00012721367,0.0003048271,0.00064170925,0.00040005994,0.57977945,0.0039851605,0.0014190946,0.0015006721,0.025727727],"study_design_scores_gemma":[0.000032591088,0.000038220758,0.18706621,0.000030552994,0.00010142132,0.000048811955,0.000383208,0.8094671,0.00051124766,0.00085574365,0.0014330995,0.00003174716],"about_ca_topic_score_codex":0.0797945,"about_ca_topic_score_gemma":0.05127535,"teacher_disagreement_score":0.0797945,"about_ca_system_score_codex":0.00094932877,"about_ca_system_score_gemma":0.0005297554,"threshold_uncertainty_score":0.15866005},"labels":[],"label_agreement":null},{"id":"W2755216794","doi":"10.1016/j.epsl.2017.08.036","title":"The deep Peru 2015 doublet earthquakes","year":2017,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico; Universidad de Chile","keywords":"Geology; Seismology; Inversion (geology); Brittleness; S-wave; Shear (geology); Geodesy; Petrology; Tectonics; Physics","score_opus":0.014482643077518459,"score_gpt":0.21936209190044936,"score_spread":0.2048794488229309,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2755216794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93399405,0.002133071,0.0008195379,0.01920546,0.00038478817,0.000035751422,0.0035686735,0.0000652734,0.039793402],"genre_scores_gemma":[0.99211085,0.0005831497,0.00010854749,0.00052225566,0.00016560909,0.000012541375,0.0009876788,0.000009397805,0.0055000144],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987864,0.000017659579,0.000007190129,0.000020108371,0.000025449055,0.000050886676],"domain_scores_gemma":[0.99950755,0.000059665548,0.00016627354,0.000044667835,0.00013701597,0.0000848907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003144242,0.0002175604,0.00015973317,0.0006680638,0.00073699333,0.001027992,0.00016568248,0.0009739789,0.0038075026],"category_scores_gemma":[0.0025441586,0.00013236319,0.00014664087,0.00095045235,0.0004635206,0.0009950139,0.0021189374,0.000834613,0.0005960165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011653791,0.00021236776,0.5966039,0.0010112154,0.00038302538,0.0036237754,0.021462671,0.004774387,0.01604317,0.043313988,0.10051253,0.2108937],"study_design_scores_gemma":[0.000016490128,0.00010230486,0.9272918,0.0001380063,0.00004257143,0.00025471803,0.0071515697,0.0005098232,0.00080827426,0.0039511034,0.05970374,0.00002960034],"about_ca_topic_score_codex":0.019168954,"about_ca_topic_score_gemma":0.04669316,"teacher_disagreement_score":0.019168954,"about_ca_system_score_codex":0.0014896359,"about_ca_system_score_gemma":0.00077660044,"threshold_uncertainty_score":0.038114727},"labels":[],"label_agreement":null},{"id":"W2755256037","doi":"10.1002/2017gl075127","title":"In Situ Stress and Pore Pressure in the Deep Interior of the Nankai Accretionary Prism, Integrated Ocean Drilling Program Site C0002","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Japan Agency for Marine-Earth Science and Technology; Japan Society for the Promotion of Science; Ministry of Education, Culture, Sports, Science and Technology; National Science Foundation","keywords":"Accretionary wedge; Geology; Pore water pressure; Drilling; Seismology; Borehole; Slip (aerodynamics); Subduction; Petrology; Décollement; Differential stress; Fault (geology); Geotechnical engineering; Tectonics; Deformation (meteorology)","score_opus":0.027340922005032187,"score_gpt":0.29618032709234343,"score_spread":0.26883940508731125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2755256037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993886,0.000006031217,0.00007347814,0.0000044182807,6.367389e-7,0.0000032340895,0.00019634199,0.0000064576916,0.0003208368],"genre_scores_gemma":[0.99890435,0.000012825638,0.00042055774,0.000006446228,0.0000012108926,0.0000103913535,0.0004210319,0.000003008012,0.00022023254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989045,0.000007014482,0.000007129471,0.00004312446,0.00003131297,0.000020842554],"domain_scores_gemma":[0.99980575,0.00002099327,0.000048228667,0.000014118348,0.000056194083,0.000054741893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015932444,0.00028418476,0.00018440386,0.00066875585,0.00041204525,0.00041617578,0.00043309218,0.00031538188,0.00045308637],"category_scores_gemma":[0.00036510782,0.0002738856,0.00014699591,0.0005351872,0.00035347484,0.00029810308,0.0005710892,0.00025075322,0.00012844506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026414567,0.00015740986,0.83068085,0.000037890506,0.000038958773,0.00030882857,0.0013383876,0.0008507959,0.15812801,0.0000739577,0.00016726622,0.007953542],"study_design_scores_gemma":[0.000008052464,0.000043361586,0.996071,0.0000027381825,0.000008237294,0.000045883993,0.00022381285,0.001232023,0.0022128783,0.000011579547,0.00013551328,0.00000494194],"about_ca_topic_score_codex":0.04340556,"about_ca_topic_score_gemma":0.095994644,"teacher_disagreement_score":0.04340556,"about_ca_system_score_codex":0.00046375062,"about_ca_system_score_gemma":0.00049993757,"threshold_uncertainty_score":0.08630586},"labels":[],"label_agreement":null},{"id":"W2756298939","doi":"10.1016/j.tecto.2017.09.008","title":"Effects of lateral variations of crustal rheology on the occurrence of post-orogenic normal faults: The Alto Tiberina Fault (Northern Apennines, Central Italy)","year":2017,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Università degli Studi di Perugia; Carleton University","keywords":"Geology; Lithosphere; Crust; Mantle (geology); Brittleness; Shear zone; Seismology; Rheology; Petrology; Fault (geology); Tectonics; Shear (geology); Compression (physics); Extensional tectonics; Geophysics; Extensional definition","score_opus":0.009991398192514987,"score_gpt":0.21323982092475274,"score_spread":0.20324842273223775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2756298939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999655,0.000025158499,0.000015860413,0.000016289325,0.0000033892597,7.7460896e-7,0.00007621083,0.000003502904,0.00020380068],"genre_scores_gemma":[0.9997017,0.000019357634,0.000010910114,0.0000065222357,0.000002882328,0.0000011416327,0.000110064844,0.000003645408,0.00014378727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997987,0.00006634204,0.00001387775,0.000053003176,0.000011290873,0.000056840847],"domain_scores_gemma":[0.99885917,0.0005052651,0.00018563854,0.000090123285,0.00008551079,0.00027431385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035847782,0.00032696556,0.00027834447,0.0004361165,0.00026326193,0.00073224027,0.0002535982,0.0004993751,0.0028256155],"category_scores_gemma":[0.0015959061,0.00015237495,0.00039684313,0.0005064592,0.000639654,0.00030473093,0.00045839176,0.00028563582,0.00024558575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003463726,0.00041215552,0.94581777,0.000076757125,0.0005391047,0.0013242543,0.00072577165,0.0055490425,0.033123866,0.00017407068,0.0005285459,0.008264841],"study_design_scores_gemma":[0.000013591115,0.00011244217,0.99847776,0.0000023964226,0.00003997372,0.00003267414,0.00019064559,0.00080549775,0.0002179258,0.00001226053,0.0000910978,0.0000037788848],"about_ca_topic_score_codex":0.013766797,"about_ca_topic_score_gemma":0.020098964,"teacher_disagreement_score":0.013766797,"about_ca_system_score_codex":0.0005110021,"about_ca_system_score_gemma":0.0002346619,"threshold_uncertainty_score":0.027373314},"labels":[],"label_agreement":null},{"id":"W2757362726","doi":"10.1093/gji/ggx407","title":"Constraining the magnitude of the largest event in a foreshock–main shock–aftershock sequence","year":2017,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Aftershock; Foreshock; Magnitude (astronomy); Seismology; Shock (circulatory); Sequence (biology); Geology; Event (particle physics); Maximum magnitude; Bayesian probability; Statistics; Induced seismicity; Mathematics; Physics","score_opus":0.031300093785192266,"score_gpt":0.2776527578722951,"score_spread":0.24635266408710282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2757362726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.67965734,0.00019346237,0.31778258,0.000095842275,0.00001382995,0.000036369336,0.00046434824,0.00016208195,0.0015941892],"genre_scores_gemma":[0.97358465,0.00008843781,0.025046844,0.00001181395,0.000021428255,0.0000137003835,0.00081206235,0.000020711144,0.00040023847],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99968076,0.000094377094,0.000023907047,0.00010055035,0.000065553155,0.000034793473],"domain_scores_gemma":[0.99653244,0.0024024283,0.0005672108,0.00017896008,0.00019398052,0.0001249052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014721188,0.00032009985,0.00033285993,0.0013259761,0.00020435778,0.0005612725,0.00036542834,0.00028732733,0.0010250488],"category_scores_gemma":[0.005180226,0.00025337032,0.00026898785,0.0007687283,0.0003796628,0.0005439568,0.00051417697,0.00040097826,0.00015450474],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052114035,0.00014893065,0.19300684,0.00013310825,0.00018389006,0.0007895403,0.00032445946,0.5919467,0.019649006,0.023863666,0.00114835,0.16828439],"study_design_scores_gemma":[0.000015499805,0.00007619208,0.06688773,0.000023008706,0.00002690347,0.00020018843,0.00007122332,0.9157765,0.0036229792,0.012430832,0.00084091636,0.00002810193],"about_ca_topic_score_codex":0.002652396,"about_ca_topic_score_gemma":0.0038046027,"teacher_disagreement_score":0.002652396,"about_ca_system_score_codex":0.00029974006,"about_ca_system_score_gemma":0.00069764734,"threshold_uncertainty_score":0.00778538},"labels":[],"label_agreement":null},{"id":"W2757968317","doi":"10.1093/gji/ggx394","title":"Monitoring interseismic activity on the Ilan Plain (NE Taiwan) using Small Baseline PS-InSAR, GPS and leveling measurements: partitioning from arc-continent collision and backarc extension","year":2017,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Seismology; Eurasian Plate; Geodesy; Global Positioning System; Collision zone; Tectonics; Interferometric synthetic aperture radar; Subsidence; Collision; Baseline (sea); Inversion (geology); Crust; Deformation (meteorology); Trough (economics); Slip (aerodynamics); Structural basin; Subduction; Geomorphology; Remote sensing; Geophysics; Synthetic aperture radar","score_opus":0.10877795002761205,"score_gpt":0.2838031482129044,"score_spread":0.17502519818529239,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2757968317","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996352,0.000006172552,0.00011912058,0.0000051936076,4.1898164e-7,0.0000031365867,0.000066631655,0.000008093033,0.00015590218],"genre_scores_gemma":[0.99905545,0.000012246571,0.0004355495,0.0000034990608,0.0000014733247,0.0000072555554,0.00039886136,0.0000020275359,0.00008369603],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999294,0.000012119094,0.0000050278613,0.000023436613,0.000013239844,0.000016770522],"domain_scores_gemma":[0.99985373,0.000026286905,0.000039278995,0.000016442224,0.00003011964,0.000034042256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015956814,0.00029529195,0.0001538017,0.0005843129,0.00021736756,0.0003136,0.0002773392,0.00021230416,0.00028400897],"category_scores_gemma":[0.0003073528,0.00014696197,0.00017007631,0.0006932268,0.00015393521,0.0003274516,0.0003238419,0.00016400771,0.000056407276],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027846417,0.0002447628,0.92436117,0.000027192651,0.00008061951,0.00038889173,0.00042136546,0.014355947,0.038717,0.00009077072,0.00016679024,0.020866925],"study_design_scores_gemma":[0.000023244464,0.000081677914,0.9543519,0.000003334762,0.00003767699,0.000053939286,0.00020754267,0.04250045,0.0025181689,0.0000285046,0.0001834799,0.000010115164],"about_ca_topic_score_codex":0.017652448,"about_ca_topic_score_gemma":0.03369953,"teacher_disagreement_score":0.017652448,"about_ca_system_score_codex":0.00035000322,"about_ca_system_score_gemma":0.0003155479,"threshold_uncertainty_score":0.035099387},"labels":[],"label_agreement":null},{"id":"W2758217104","doi":"","title":"Geodynamic constraints on deep-mantle buoyancy: Implications for thermochemical structure of LLSVP and large-scale upwellings under the Pacific Ocean.","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle (geology); Upwelling; Buoyancy; Scale (ratio); Geophysics; Oceanography; Climatology; Geography; Thermodynamics","score_opus":0.017870968751210133,"score_gpt":0.23891077416141182,"score_spread":0.22103980541020168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2758217104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99513584,0.00024116148,0.0005046876,0.00039639065,0.000010977839,0.0000046038613,0.00044878264,0.00001804459,0.0032395055],"genre_scores_gemma":[0.99958414,0.0000775583,0.000099254976,0.000026064468,0.0000039030147,0.000002380567,0.00012466042,0.0000041949256,0.00007776931],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994767,0.000008468169,0.0000049593386,0.0000125235465,0.0000105499885,0.00001569969],"domain_scores_gemma":[0.99977535,0.00005869432,0.000057253255,0.000015530008,0.000041494557,0.00005170842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023463798,0.00024241352,0.0002112616,0.000444356,0.00049469236,0.0006527135,0.0004059505,0.00034241634,0.0028577214],"category_scores_gemma":[0.0010644946,0.00023087976,0.00018931572,0.0005594965,0.00066230376,0.0008340831,0.00095301814,0.00038188812,0.00020499165],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047092157,0.00011329101,0.8525769,0.00019622687,0.00014252873,0.00041660108,0.0012257656,0.0068835355,0.091403134,0.006464088,0.0014672466,0.038639892],"study_design_scores_gemma":[0.000019816536,0.00002386051,0.990537,0.000017423907,0.00002566503,0.000036428137,0.0007793802,0.004987627,0.0010795802,0.0016753244,0.0008054117,0.000012564878],"about_ca_topic_score_codex":0.04134715,"about_ca_topic_score_gemma":0.06192094,"teacher_disagreement_score":0.04134715,"about_ca_system_score_codex":0.00057264866,"about_ca_system_score_gemma":0.00067224714,"threshold_uncertainty_score":0.082212985},"labels":[],"label_agreement":null},{"id":"W2758595231","doi":"","title":"Multi-surface Earthquake Rupture Recorded in Pseudotachylyte Vein Geometries, Norumbega Shear Zone, southern Maine","year":2015,"lang":"en","type":"article","venue":"2015 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Seismology; Shear zone; Shear (geology); Intraplate earthquake; Vein; Surface rupture; Petrology; Tectonics; Fault (geology)","score_opus":0.03263752396678985,"score_gpt":0.24345604550714342,"score_spread":0.21081852154035358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2758595231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986534,0.000031972097,0.00003203381,0.000014766761,0.0000021461437,0.0000035698229,0.00062605046,0.0000037759253,0.0006323232],"genre_scores_gemma":[0.9984931,0.00003402408,0.00007052354,0.000008488232,0.0000028973056,0.0000063860616,0.0008879772,0.0000019786908,0.0004946506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999268,0.000011099853,0.0000068452005,0.00002159795,0.000011181886,0.000022549439],"domain_scores_gemma":[0.9998357,0.000025971367,0.000049021597,0.000012438354,0.0000413464,0.00003544733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013168978,0.00018129603,0.00017470184,0.0008187169,0.00035934433,0.00041183672,0.0002806096,0.00032951316,0.0007178625],"category_scores_gemma":[0.00040484022,0.00012123896,0.00010263343,0.0009882391,0.00028180453,0.0002785701,0.0005686556,0.00011953769,0.00018201691],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003165463,0.00005713055,0.9758748,0.000052203082,0.000056434008,0.00070191984,0.0030678674,0.0006370454,0.009951836,0.0001350273,0.0007505002,0.008398734],"study_design_scores_gemma":[0.000003458029,0.000011349399,0.99896026,0.000003721273,0.000004415675,0.000035036646,0.00044623564,0.0001463342,0.00009815283,0.0000066884672,0.00028346264,0.0000010070416],"about_ca_topic_score_codex":0.07288237,"about_ca_topic_score_gemma":0.25748312,"teacher_disagreement_score":0.07288237,"about_ca_system_score_codex":0.0005692334,"about_ca_system_score_gemma":0.00043586924,"threshold_uncertainty_score":0.14491624},"labels":[],"label_agreement":null},{"id":"W2759313668","doi":"","title":"Updated Rupture Model for the M7.8 October 28, 2012, Haida Gwaii Earthquake as Constrained by GPS-Observed Displacements","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Global Positioning System; Geology; Seismology; Geodesy; Computer science; Telecommunications","score_opus":0.02555074271820904,"score_gpt":0.23576860912404796,"score_spread":0.21021786640583892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2759313668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7183371,0.00062243233,0.031064175,0.003438034,0.0007278863,0.00013492885,0.19806312,0.0029032547,0.04470905],"genre_scores_gemma":[0.93746924,0.00027422464,0.005909609,0.00018946463,0.00011453876,0.00015865154,0.04392228,0.0003700185,0.011591913],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998827,0.000018523468,0.00000878026,0.000043041666,0.000017551522,0.000029398538],"domain_scores_gemma":[0.9995672,0.00009079133,0.000057637822,0.000054765016,0.00016099756,0.00006853217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042006458,0.0006100676,0.0008737086,0.00087676547,0.00056306773,0.0011180126,0.0030258289,0.0032729823,0.010418249],"category_scores_gemma":[0.0013067487,0.0010903869,0.0008673895,0.0012116012,0.0004238017,0.001162039,0.00043036728,0.0013195857,0.0029776504],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001482146,0.00005357697,0.005536556,0.000037315534,0.00006944095,0.000118355776,0.00004140088,0.9819417,0.00054853864,0.001862725,0.0073295706,0.00231261],"study_design_scores_gemma":[0.00012785477,0.00001877161,0.007151841,0.000022356046,0.00004709134,0.00004090547,0.000045793655,0.9881286,0.00020305128,0.0009784371,0.003188445,0.000046963924],"about_ca_topic_score_codex":0.15506427,"about_ca_topic_score_gemma":0.13067521,"teacher_disagreement_score":0.8449357,"about_ca_system_score_codex":0.0016270392,"about_ca_system_score_gemma":0.0019898687,"threshold_uncertainty_score":0.30832344},"labels":[],"label_agreement":null},{"id":"W2759465642","doi":"10.1007/s11200-017-0411-5","title":"Acoustic and vibration precursors from shear-slip characteristics of simulated zigzag-type gouge fault","year":2017,"lang":"en","type":"article","venue":"Studia Geophysica et Geodaetica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Foreshock; Shear (geology); Seismology; Geology; Fault gouge; Slip (aerodynamics); Zigzag; Structural geology; Vibration; Instability; Geotechnical engineering; Fault (geology); Petrology; Mechanics; Engineering; Aftershock; Physics; Geometry; Acoustics","score_opus":0.015544441627735932,"score_gpt":0.24558796373124245,"score_spread":0.2300435221035065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2759465642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988814,0.0000061398564,0.00019626367,0.00000995386,0.0000031226157,0.000005355875,0.00027264943,0.00003266488,0.00059249665],"genre_scores_gemma":[0.9992841,0.0000055285436,0.00015329843,0.0000022949655,0.0000015347614,0.000003433753,0.0003585101,0.000005263624,0.00018606568],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999366,0.000007204109,0.00000314489,0.000016625443,0.000018361912,0.000018184839],"domain_scores_gemma":[0.99976104,0.00006461358,0.000032903783,0.000014156073,0.00006599538,0.00006122593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009294816,0.00027168638,0.00015551604,0.00039337212,0.0001888756,0.00020936842,0.00024565952,0.0004936758,0.0022869187],"category_scores_gemma":[0.00046118913,0.00017889061,0.00020100686,0.0002865102,0.00025082662,0.00015038748,0.00018750489,0.00027768448,0.00030353834],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0035948923,0.0008108647,0.50131416,0.00023962244,0.0001740933,0.0047395024,0.0017145235,0.14106303,0.3102466,0.0010203965,0.0025761374,0.032506157],"study_design_scores_gemma":[0.000058340862,0.00029659623,0.91751134,0.000012222648,0.000036773054,0.00020787094,0.00033538655,0.074968815,0.005969266,0.000086151515,0.0004928777,0.000024518713],"about_ca_topic_score_codex":0.009663282,"about_ca_topic_score_gemma":0.013834571,"teacher_disagreement_score":0.009663282,"about_ca_system_score_codex":0.0002157681,"about_ca_system_score_gemma":0.00021169109,"threshold_uncertainty_score":0.019214094},"labels":[],"label_agreement":null},{"id":"W2760255177","doi":"10.1016/j.margeo.2017.09.013","title":"Messinian evaporites across the Anaximander Mountains, Sırrı Erinç Plateau and the Rhodes and Finike basins, eastern Mediterranean Sea","year":2017,"lang":"en","type":"article","venue":"Marine Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland","keywords":"Evaporite; Geology; Plateau (mathematics); Paleontology; Mediterranean climate; Structural basin; Late Miocene; Ridge; Archaeology; Geography","score_opus":0.021492700993775385,"score_gpt":0.257515771347871,"score_spread":0.23602307035409564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2760255177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998511,0.00016019768,0.000025058798,0.000023141081,0.0000011054087,0.0000038373355,0.00010042244,0.000002224203,0.0011730075],"genre_scores_gemma":[0.9992465,0.00006939793,0.00004700663,0.000005336644,0.000002201387,0.0000040441155,0.00013201199,0.0000015477735,0.0004921057],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999286,0.000008917178,0.000007199326,0.000022676306,0.000012284224,0.000020365133],"domain_scores_gemma":[0.999936,0.000009657659,0.000019747691,0.000004762608,0.000017495251,0.000012264416],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013970665,0.00014399791,0.00016458421,0.00060972205,0.0005088632,0.0004036997,0.00019896067,0.00018314729,0.0010081658],"category_scores_gemma":[0.00020016954,0.000106276035,0.00011944449,0.00054595247,0.0003910875,0.00021413261,0.00045200792,0.000093383744,0.00014883805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061797176,0.000081501865,0.92788166,0.00022615216,0.00025407653,0.0012716699,0.008654199,0.000957656,0.023447508,0.0011567341,0.0008018555,0.03464911],"study_design_scores_gemma":[0.0000032492412,0.000007143087,0.99851316,0.0000048010643,0.000005179632,0.000049088827,0.0006988163,0.000057979505,0.00008695607,0.000013665734,0.00055878086,0.0000012440673],"about_ca_topic_score_codex":0.037899684,"about_ca_topic_score_gemma":0.1359758,"teacher_disagreement_score":0.037899684,"about_ca_system_score_codex":0.0004800139,"about_ca_system_score_gemma":0.0004257125,"threshold_uncertainty_score":0.07535815},"labels":[],"label_agreement":null},{"id":"W2762851563","doi":"10.1016/j.epsl.2017.09.021","title":"Trench-breaching afterslip following deeper coseismic slip of the 2012 Mw 7.6 Costa Rica earthquake constrained by near-trench pressure and land-based geodetic observations","year":2017,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; University of Victoria; National Science Foundation","keywords":"Trench; Geology; Seismology; Subduction; Seafloor spreading; Episodic tremor and slip; Earthquake rupture; Slip (aerodynamics); Interplate earthquake; Tsunami earthquake; Submarine pipeline; Moment magnitude scale; Tectonics; Fault (geology); Geophysics; Geotechnical engineering","score_opus":0.01318654811350073,"score_gpt":0.1996201889132826,"score_spread":0.18643364079978186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2762851563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979792,0.000038326067,0.000041972173,0.00006878058,0.000004119434,0.000004695138,0.00071320304,0.000012953385,0.0011366153],"genre_scores_gemma":[0.9986773,0.00002174029,0.000035014164,0.0000142879435,0.00000252368,0.0000033943638,0.00058982533,0.000004561286,0.00065148727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998739,0.000012055965,0.0000051787424,0.00003331522,0.000012167299,0.000063399166],"domain_scores_gemma":[0.9996568,0.000025749367,0.000118690084,0.000036011705,0.00009264447,0.0000701401],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002026182,0.00019303529,0.00022635257,0.00058657164,0.0005759946,0.0007424304,0.000410913,0.0005834239,0.0028299019],"category_scores_gemma":[0.0008312759,0.00020051641,0.00020496038,0.0008479434,0.00032190728,0.0003575899,0.0010298996,0.00030463887,0.00048036198],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040268805,0.00013638443,0.9762792,0.00003222074,0.00012727191,0.0004632445,0.0012415682,0.0045544645,0.0050654416,0.00039448097,0.002472371,0.008830618],"study_design_scores_gemma":[0.0000026204991,0.000006799054,0.99810445,0.0000042764336,0.0000072672615,0.000012852306,0.00029024188,0.0010586688,0.000072074174,0.000014768274,0.00042250362,0.0000034159339],"about_ca_topic_score_codex":0.30029625,"about_ca_topic_score_gemma":0.5473158,"teacher_disagreement_score":0.30029625,"about_ca_system_score_codex":0.001131607,"about_ca_system_score_gemma":0.0008567146,"threshold_uncertainty_score":0.5970967},"labels":[],"label_agreement":null},{"id":"W2763553858","doi":"","title":"A comparison of the seismic structure of oceanic island arc crust and continental accreted arc terranes","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Terrane; Geology; Continental crust; Oceanic crust; Island arc; Crust; Subduction; Continental margin; Arc (geometry); Seismology; Earth science; Geophysics; Tectonics","score_opus":0.02801817625470792,"score_gpt":0.24715009021305442,"score_spread":0.2191319139583465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763553858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99802953,0.000055272063,0.000024466439,0.00001684454,7.230138e-7,0.0000013658574,0.00016381538,0.000002509507,0.0017054245],"genre_scores_gemma":[0.99894625,0.00007487242,0.00007859609,0.0000072636653,0.0000014750461,0.0000014419667,0.00043611432,0.0000025930858,0.00045141514],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999465,0.000008890208,0.0000057310444,0.000014363203,0.000011614218,0.000012990187],"domain_scores_gemma":[0.9998092,0.00002735031,0.000048773665,0.000013451765,0.000056150617,0.000045137953],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009648605,0.00010212889,0.00009981556,0.0011389403,0.0003208117,0.0005039313,0.00015794282,0.00014415054,0.0022956992],"category_scores_gemma":[0.0004761,0.000091715265,0.00011708938,0.0011998975,0.00019124468,0.00020703686,0.00048144962,0.00013947187,0.00021964553],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023862833,0.00002915809,0.97087586,0.000025105277,0.00006806136,0.0001691941,0.0009846028,0.0005900534,0.012087071,0.00026179917,0.00016975106,0.014500709],"study_design_scores_gemma":[0.0000014042514,0.000009651468,0.9993092,0.0000013435904,0.0000057338957,0.000029284882,0.00022481065,0.00011302982,0.00008572645,0.000008875099,0.00021013092,7.699647e-7],"about_ca_topic_score_codex":0.03912128,"about_ca_topic_score_gemma":0.06992782,"teacher_disagreement_score":0.03912128,"about_ca_system_score_codex":0.00035231968,"about_ca_system_score_gemma":0.0003401223,"threshold_uncertainty_score":0.0777871},"labels":[],"label_agreement":null},{"id":"W2765333376","doi":"10.1080/00288306.2017.1375533","title":"Bedrock geology of DFDP‐2B, central Alpine Fault, New Zealand","year":2017,"lang":"en","type":"article","venue":"New Zealand Journal of Geology and Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; McGill University","funders":"Marsden Fund; Natural Environment Research Council; Ministry for Business Innovation and Employment; Ministry of Business, Innovation and Employment; Royal Society Te Apārangi; Centre National de la Recherche Scientifique; Université de Montpellier; Sight Research UK","keywords":"Geology; Mylonite; Lithology; Bedrock; Fault (geology); Terrane; Schist; Borehole; Geomorphology; Geochemistry; Quartz; Facies; Sedimentary rock; Shear zone; Tectonics; Petrology; Metamorphic rock; Seismology; Structural basin; Geotechnical engineering; Paleontology","score_opus":0.012517307305200719,"score_gpt":0.23020354970850068,"score_spread":0.21768624240329995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765333376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967726,0.00010635752,0.000051121642,0.000023021572,0.0000014954038,0.000021512355,0.0015999437,0.000008213889,0.0014156498],"genre_scores_gemma":[0.9973437,0.00010220089,0.00018253384,0.000011262257,0.0000016899677,0.000027761895,0.001214263,0.000002653611,0.0011140765],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999838,0.000008136491,0.000014391919,0.000044771536,0.000058606493,0.000036066696],"domain_scores_gemma":[0.9996624,0.000018696812,0.00011162444,0.000016309126,0.0001131347,0.00007784115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001560667,0.00031621885,0.00020517742,0.0015928372,0.00058214384,0.00054020924,0.00029376076,0.00018478844,0.0022916475],"category_scores_gemma":[0.00047787183,0.00025779888,0.00015176667,0.0012770401,0.00043429376,0.00027089464,0.00048314303,0.00020201517,0.00032839697],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039780326,0.000079420846,0.94460624,0.00015717938,0.00007347204,0.0009820593,0.003186977,0.00034431336,0.026402015,0.00013522833,0.0009888847,0.02264636],"study_design_scores_gemma":[0.000004382653,0.000016131256,0.9991041,0.0000039423367,0.0000026263351,0.000049283837,0.00024022497,0.00004193189,0.00008403299,0.0000026703742,0.00044927766,0.000001411547],"about_ca_topic_score_codex":0.5657166,"about_ca_topic_score_gemma":0.7491934,"teacher_disagreement_score":0.5657166,"about_ca_system_score_codex":0.0020828936,"about_ca_system_score_gemma":0.0008529774,"threshold_uncertainty_score":0.8736819},"labels":[],"label_agreement":null},{"id":"W2765682674","doi":"10.1002/2017tc004502","title":"Necessary Conditions for Intraplate Seismic Zones in North America","year":2017,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; Natural Resources Canada; National Science Foundation","keywords":"Intraplate earthquake; Geology; Seismology; Basement; Crust; Rift; Geophysics; Tectonics; Archaeology","score_opus":0.02370499209605275,"score_gpt":0.25739062923421874,"score_spread":0.23368563713816598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765682674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869552,0.00025110896,0.0022938454,0.00039086177,0.000009252165,0.000028304308,0.0007610613,0.00005143782,0.009258888],"genre_scores_gemma":[0.99859196,0.0000471646,0.00068462145,0.000026843456,0.000011331709,0.000012932519,0.000347027,0.0000047463877,0.00027347708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972516,0.00003657635,0.000029725163,0.00007834354,0.000040311686,0.00008996225],"domain_scores_gemma":[0.9977315,0.0006426969,0.00071722607,0.00010702747,0.00040534794,0.00039628937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000377014,0.00024355379,0.00035616927,0.0019751347,0.0010568077,0.0011630966,0.0004926705,0.0006278977,0.012428139],"category_scores_gemma":[0.0032098424,0.00033179604,0.00023004564,0.00090280705,0.000997915,0.00080324657,0.0014389717,0.00044825918,0.00030613827],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007870762,0.00020854856,0.8911381,0.0004324665,0.00014778863,0.0028744414,0.0019892594,0.0069008605,0.02980756,0.03914871,0.0024599251,0.024105242],"study_design_scores_gemma":[0.00008040032,0.0001366606,0.95543355,0.00007702086,0.0000523143,0.0014477491,0.002986722,0.007765015,0.001765862,0.026014566,0.004213355,0.00002688711],"about_ca_topic_score_codex":0.01403607,"about_ca_topic_score_gemma":0.026860649,"teacher_disagreement_score":0.98596394,"about_ca_system_score_codex":0.0007869416,"about_ca_system_score_gemma":0.000710236,"threshold_uncertainty_score":0.041576266},"labels":[],"label_agreement":null},{"id":"W2766232693","doi":"10.1002/2017jb014074","title":"Hydromechanical Modeling of Stress, Pore Pressure, and Porosity Evolution in Fold‐and‐Thrust Belt Systems","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Total; Universiti Teknologi Petronas; Statoil; European Network and Information Security Agency; Petrobras; BG Group; ConocoPhillips; DONG Energy; Chevron; BP","keywords":"Anticline; Geology; Overpressure; Pore water pressure; Porosity; Thrust; Stress field; Fold and thrust belt; Overburden pressure; Thrust fault; Fold (higher-order function); Hydrostatic equilibrium; Compaction; Geotechnical engineering; Petrology; Stress (linguistics); Tectonics; Finite element method; Seismology; Structural engineering","score_opus":0.053527211597544665,"score_gpt":0.3202014406087605,"score_spread":0.26667422901121585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766232693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99605477,0.000021602042,0.0022774565,0.00007594527,0.000004889697,0.000011045814,0.00010406804,0.000043047366,0.0014071894],"genre_scores_gemma":[0.9990501,0.000012426897,0.00061942684,0.0000110916535,0.0000025140216,0.0000135727205,0.000047114336,0.000009847676,0.00023393315],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992955,0.000015226242,0.000003483658,0.000013361577,0.000012486495,0.000025873973],"domain_scores_gemma":[0.9997079,0.00013873188,0.00004288231,0.000020096235,0.000037297326,0.00005311798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021565538,0.00039514873,0.00042009357,0.0005014416,0.0005805331,0.00079334644,0.00092017907,0.0011170364,0.0012665928],"category_scores_gemma":[0.0009707041,0.00032371073,0.00053856586,0.00029740107,0.0011931065,0.0005832312,0.00051179325,0.00045371306,0.00008291358],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030741045,0.00004231524,0.0033942387,0.000008452933,0.000016872791,0.000064405125,0.000038209022,0.99329996,0.0019283699,0.000697677,0.000043357897,0.00043545992],"study_design_scores_gemma":[0.000016136342,0.000012614834,0.0011325154,0.0000011704321,0.0000032801734,0.0000045444117,0.000012810361,0.9983808,0.00024071403,0.0001523801,0.000039503044,0.000003417626],"about_ca_topic_score_codex":0.03569665,"about_ca_topic_score_gemma":0.012075871,"teacher_disagreement_score":0.03569665,"about_ca_system_score_codex":0.0017737488,"about_ca_system_score_gemma":0.0010036606,"threshold_uncertainty_score":0.07097775},"labels":[],"label_agreement":null},{"id":"W2766792892","doi":"10.3390/geosciences7040111","title":"Structure of Volatile Conduits beneath Gorely Volcano (Kamchatka) Revealed by Local Earthquake Tomography","year":2017,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Population and Public Health; Russian Science Foundation; King Saud University; Russian Foundation for Basic Research","keywords":"Geology; Volcano; Magma; Induced seismicity; Seismology; Anomaly (physics); Impact crater; Seismic tomography; Electrical conduit; Petrology; Geophysics; Mantle (geology)","score_opus":0.012484420211559882,"score_gpt":0.2194836381517043,"score_spread":0.20699921794014442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766792892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880457,0.00005277468,0.00026739284,0.000024197221,0.0000023800037,0.0000051001066,0.00034914268,0.000045896933,0.00044852574],"genre_scores_gemma":[0.9991591,0.000039725528,0.0002519356,0.0000041046496,0.0000021171386,0.0000037436434,0.00042588494,0.000009831464,0.000103456005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994695,0.000005225723,0.0000045391603,0.00001771848,0.0000088610595,0.00001670677],"domain_scores_gemma":[0.99987876,0.0000201503,0.000032712815,0.0000145180775,0.000024042301,0.000029793735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007326182,0.00039964757,0.00032772048,0.0010730865,0.00024355773,0.00069835514,0.00037414307,0.0004210385,0.0010426095],"category_scores_gemma":[0.0003920556,0.00031778164,0.00025006323,0.0010179292,0.0005142951,0.0004842053,0.0006996715,0.00022477913,0.00017071172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067506824,0.00026004377,0.7734952,0.00028590145,0.00039149192,0.0039596227,0.001693419,0.10363535,0.091912664,0.0012888191,0.0013816927,0.02102068],"study_design_scores_gemma":[0.00006319399,0.000082699866,0.89485663,0.00002962052,0.00010187547,0.00039495158,0.00087900914,0.1004362,0.0020075522,0.00030401,0.00080000237,0.0000442992],"about_ca_topic_score_codex":0.013854263,"about_ca_topic_score_gemma":0.013256618,"teacher_disagreement_score":0.013854263,"about_ca_system_score_codex":0.00034619682,"about_ca_system_score_gemma":0.0003753636,"threshold_uncertainty_score":0.02754724},"labels":[],"label_agreement":null},{"id":"W2767620640","doi":"10.1016/j.epsl.2017.10.051","title":"Active tectonics around the Yakutat indentor: New geomorphological constraints on the eastern Denali, Totschunda and Duke River Faults","year":2017,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"U.S. Geological Survey; Agence Nationale de la Recherche","keywords":"Geology; Seismology; Thrust fault; Tectonics; Slip (aerodynamics); Fault (geology); Active fault; Geomorphology","score_opus":0.028367777641240457,"score_gpt":0.22368092237325088,"score_spread":0.19531314473201042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767620640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962309,0.00025180337,0.000059267997,0.000042118183,0.0000042584,0.000005331241,0.00019267236,0.000004584046,0.0032091902],"genre_scores_gemma":[0.998591,0.00017729106,0.00015188359,0.00001255596,0.000004447161,0.00000704476,0.00042137536,0.0000034503214,0.0006308839],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987733,0.0000102595495,0.000011808017,0.000030749765,0.000021514345,0.000048408758],"domain_scores_gemma":[0.99982053,0.00003284557,0.00006456002,0.000012850238,0.00003759556,0.00003165347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022506759,0.00024872308,0.00030035764,0.0017025709,0.0010149204,0.0011391883,0.00039711216,0.00025597055,0.0026060047],"category_scores_gemma":[0.0004305542,0.00022636054,0.0001596007,0.0021747416,0.001104778,0.000631678,0.0011605053,0.00026226684,0.0002637654],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032223438,0.0001129697,0.92562574,0.00012528086,0.000058951475,0.0015798872,0.0072255563,0.0016496016,0.012776899,0.0023979642,0.00061608286,0.04750889],"study_design_scores_gemma":[0.000008815475,0.000015765916,0.9966972,0.00001870964,0.000009607741,0.0001606851,0.0014735608,0.0002576188,0.0001128991,0.000097646036,0.0011426681,0.000004927375],"about_ca_topic_score_codex":0.060358454,"about_ca_topic_score_gemma":0.25546584,"teacher_disagreement_score":0.060358454,"about_ca_system_score_codex":0.0008210173,"about_ca_system_score_gemma":0.0010788784,"threshold_uncertainty_score":0.12001425},"labels":[],"label_agreement":null},{"id":"W2767779763","doi":"10.1002/2017jb014946","title":"Seismicity During the Initial Stages of the Guy‐Greenbrier, Arkansas, Earthquake Sequence","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Livermore National Laboratory; Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; U.S. Geological Survey; National Science Foundation; University of Cambridge; British Columbia Oil and Gas Commission; National Science Foundation of Sri Lanka","keywords":"Induced seismicity; Seismology; Geology; Hydraulic fracturing; Seismic hazard; Waveform; Fault (geology); Geotechnical engineering; Engineering","score_opus":0.08908635233086566,"score_gpt":0.361341438118219,"score_spread":0.27225508578735336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767779763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846965,0.00003111662,0.00010353192,0.000020150015,0.0000013267759,0.0000042681736,0.00090143527,0.000050168,0.00041832734],"genre_scores_gemma":[0.9982003,0.000018574417,0.00013700209,0.000006160859,0.000003189832,0.000006348102,0.0014278219,0.0000035173955,0.00019705284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998907,0.000012425983,0.0000092042,0.000028205062,0.000024387085,0.000035063855],"domain_scores_gemma":[0.9995925,0.0000522617,0.00015944005,0.000023514582,0.000081028156,0.00009126928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012455974,0.00013483452,0.0001551002,0.00095698016,0.00033682803,0.00036604496,0.00020428981,0.00026149355,0.0008849048],"category_scores_gemma":[0.0004119121,0.00008407105,0.0001143603,0.0007947122,0.00021214108,0.00017733767,0.0003633723,0.00019049777,0.00020751514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059267937,0.00010772783,0.959955,0.00005422974,0.00005490358,0.00070208387,0.0006544497,0.00512482,0.018835125,0.000068812,0.0016571718,0.01219309],"study_design_scores_gemma":[0.0000039743522,0.000030417092,0.99811375,0.0000022487643,0.0000062625295,0.0000294672,0.00015981922,0.0010308082,0.00037061455,0.000005136307,0.00024346964,0.000004024972],"about_ca_topic_score_codex":0.050053142,"about_ca_topic_score_gemma":0.12688056,"teacher_disagreement_score":0.050053142,"about_ca_system_score_codex":0.00052773085,"about_ca_system_score_gemma":0.00038001296,"threshold_uncertainty_score":0.099523604},"labels":[],"label_agreement":null},{"id":"W2768747244","doi":"10.1130/g39551.1","title":"Monitoring and forecasting fault development at actively forming calderas: An experimental study","year":2017,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Caldera; Geology; Fault (geology); Seismology; Development (topology); Geodesy; Volcano","score_opus":0.07406250650744382,"score_gpt":0.2900895028511662,"score_spread":0.21602699634372236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768747244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99912494,0.000019658217,0.0006691686,0.000008659606,0.0000025518577,0.00002334551,0.00006486503,0.000013214274,0.000073620125],"genre_scores_gemma":[0.99600583,0.000062713014,0.003436303,0.000011549874,0.0000044749504,0.00005138069,0.0002187931,0.0000029888506,0.00020597193],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99978215,0.000029184574,0.000013561013,0.00009173614,0.000044668093,0.00003863792],"domain_scores_gemma":[0.99895585,0.00040247588,0.00021651795,0.0001708566,0.00015002681,0.000104214305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042853144,0.0004061981,0.0003085851,0.0003150636,0.00027770377,0.00028341767,0.00050760945,0.0005924756,0.00068834896],"category_scores_gemma":[0.0010443078,0.00019875342,0.00021174802,0.000199006,0.0004603344,0.00037439493,0.000401105,0.0004477478,0.00007147897],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017669455,0.008343989,0.09977121,0.0002002116,0.00012470713,0.00035123894,0.00041353548,0.04399721,0.8153388,0.00039647758,0.00031819567,0.028977504],"study_design_scores_gemma":[0.00038339695,0.013293757,0.21632747,0.0000225078,0.00013213174,0.00018364227,0.00058307097,0.42878294,0.33883503,0.0004199949,0.0009831445,0.00005293651],"about_ca_topic_score_codex":0.005403547,"about_ca_topic_score_gemma":0.009951643,"teacher_disagreement_score":0.005403547,"about_ca_system_score_codex":0.0005689833,"about_ca_system_score_gemma":0.00029686256,"threshold_uncertainty_score":0.010744214},"labels":[],"label_agreement":null},{"id":"W2770087930","doi":"10.1190/tle21050495.1","title":"Reviews","year":2002,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Calgary Construction Association; Capilano University","funders":"","keywords":"Ilya; Art history; Humanities; Philosophy; Art","score_opus":0.07732743860381933,"score_gpt":0.24547471867044074,"score_spread":0.1681472800666214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2770087930","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000771221,0.2248604,0.0032459293,0.025307322,0.054271042,0.00024730043,0.006556179,0.0017758716,0.68296474],"genre_scores_gemma":[0.0041341656,0.12487577,0.0027278275,0.011384358,0.013425039,0.00021568326,0.006202846,0.0008290119,0.83620524],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983246,0.0001986494,0.0001330502,0.00044430353,0.000727168,0.00017220962],"domain_scores_gemma":[0.9980003,0.00037239355,0.00012363987,0.00027570545,0.0008695079,0.00035843113],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009470238,0.0015555738,0.0015088315,0.0031983682,0.0013260974,0.00639718,0.002663246,0.0029494197,0.4595435],"category_scores_gemma":[0.0050704805,0.0005198276,0.0010306406,0.0033753547,0.0010688275,0.0045149224,0.0033790267,0.0028992489,0.39907646],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024510891,0.000022063981,0.00011811175,0.00084863475,0.000009725596,0.0000936155,0.00009862867,0.000063869025,0.00021435833,0.007909105,0.8249448,0.16565253],"study_design_scores_gemma":[0.0000017087685,0.0000032659061,0.00007229209,0.00016925274,0.00000196078,0.0000694802,0.000025950181,0.000006926753,0.000022343633,0.00081208244,0.99881244,0.0000024105339],"about_ca_topic_score_codex":0.0031079738,"about_ca_topic_score_gemma":0.0043585687,"teacher_disagreement_score":0.54045653,"about_ca_system_score_codex":0.002377997,"about_ca_system_score_gemma":0.004076589,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W2771374424","doi":"10.1130/abs/2017am-300236","title":"EVOLUTION OF JURA-CRETACEOUS BASINS IN SOUTHWEST YUKON, WITH IMPLICATIONS FOR MESOZOIC ACCRETIONARY PROCESSES IN THE WESTERN NORTH AMERICAN CORDILLERA","year":2017,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Cretaceous; Mesozoic; Paleontology; Earth science; Structural basin","score_opus":0.02630691164758571,"score_gpt":0.2555812964092539,"score_spread":0.22927438476166823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2771374424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99886775,0.00013760796,0.000023348315,0.0000421979,0.0000015082161,0.0000021691983,0.000102495775,0.0000037113384,0.0008191787],"genre_scores_gemma":[0.9994759,0.00007087864,0.000049886286,0.00000802392,9.137646e-7,0.000002680632,0.00012053495,0.0000022084664,0.00026900586],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999329,0.0000069205175,0.0000064781025,0.000020723008,0.000008103816,0.00002496632],"domain_scores_gemma":[0.9997906,0.000021949163,0.000063868,0.000010603845,0.00006504253,0.00004795574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012660152,0.00018410133,0.000194447,0.0015906617,0.0013354059,0.0010233378,0.00040374603,0.00033652136,0.0023497764],"category_scores_gemma":[0.00052255695,0.00017307549,0.0001811785,0.0020356392,0.00062245445,0.0003704581,0.0008028743,0.000186506,0.00016515549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000192595,0.00003564818,0.972937,0.000051999537,0.000117690106,0.0004937768,0.0036184823,0.0011074989,0.006181391,0.0015169206,0.00031918593,0.013427867],"study_design_scores_gemma":[0.0000041178555,0.0000042123283,0.99847907,0.0000059615786,0.000009123228,0.00003789939,0.0007606676,0.00027719792,0.000056595924,0.000070026545,0.00029306317,0.0000020678979],"about_ca_topic_score_codex":0.299901,"about_ca_topic_score_gemma":0.57221925,"teacher_disagreement_score":0.700099,"about_ca_system_score_codex":0.0023769508,"about_ca_system_score_gemma":0.0021562632,"threshold_uncertainty_score":0.5963108},"labels":[],"label_agreement":null},{"id":"W2773413449","doi":"10.1002/2017gc007202","title":"Petrophysical, Geochemical, and Hydrological Evidence for Extensive Fracture‐Mediated Fluid and Heat Transport in the Alpine Fault's Hanging‐Wall Damage Zone","year":2017,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Alberta","funders":"Marsden Fund; Natural Environment Research Council; Victoria University; Ministry of Business, Innovation and Employment; Royal Society Te Apārangi; Victoria University of Wellington; University of Otago; Sight Research UK; Royal Society","keywords":"Geology; Borehole; Petrophysics; Seismology; Fault (geology); Active fault; Shear zone; Crust; Petrology; Earthquake rupture; Permeability (electromagnetism); Geophysics; Geotechnical engineering; Porosity; Tectonics","score_opus":0.026111368566546774,"score_gpt":0.2504955731129001,"score_spread":0.22438420454635333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2773413449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99979323,0.0000109609455,0.000036183763,0.0000041465405,1.6627783e-7,5.570553e-7,0.000028524277,0.0000023427933,0.00012399566],"genre_scores_gemma":[0.99987435,0.000009001424,0.000037858328,0.0000017182518,0.0000012466404,6.116989e-7,0.000048242193,3.558605e-7,0.000026732143],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999905,0.000012883021,0.00000854365,0.000021487136,0.000027163529,0.000024832316],"domain_scores_gemma":[0.9997073,0.000041070565,0.0001368083,0.0000237574,0.00003738234,0.000053617638],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013683748,0.00016594635,0.00017754745,0.0009871428,0.00035960446,0.00048174502,0.0001603379,0.00025337056,0.0005744247],"category_scores_gemma":[0.00031856852,0.00013691893,0.000107837834,0.00055414945,0.0005843293,0.00024012191,0.00038494656,0.00013276136,0.000055611035],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001112914,0.000044911623,0.949853,0.000020562195,0.00003532965,0.00044804654,0.00053397997,0.001138492,0.042598326,0.00011951821,0.000043024913,0.0050534857],"study_design_scores_gemma":[0.0000024319809,0.000016284961,0.998524,0.00000155792,0.0000034407517,0.000067264875,0.00013427102,0.0006401959,0.0005315305,0.000020411977,0.00005684411,0.0000017156727],"about_ca_topic_score_codex":0.0066770255,"about_ca_topic_score_gemma":0.010221103,"teacher_disagreement_score":0.0066770255,"about_ca_system_score_codex":0.00033793433,"about_ca_system_score_gemma":0.00013783194,"threshold_uncertainty_score":0.013276339},"labels":[],"label_agreement":null},{"id":"W2774908743","doi":"10.5150/cmcm.2017.033","title":"Towards an understanding and operational early warning of the Adriatic meteotsunamis: Project MESSI","year":2017,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Warning system; Computer science; Telecommunications","score_opus":0.07813658982362966,"score_gpt":0.2778516449250356,"score_spread":0.19971505510140597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2774908743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5475652,0.002721622,0.4090432,0.006327622,0.0002357773,0.001100735,0.001820651,0.00237001,0.028815223],"genre_scores_gemma":[0.6906232,0.0011502337,0.2963768,0.00019568914,0.00006935622,0.00051224587,0.0022971064,0.00015967005,0.008615702],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99934083,0.00027531854,0.000027621732,0.00012540423,0.00015223425,0.00007856357],"domain_scores_gemma":[0.99942315,0.000110405126,0.00011169003,0.00010499525,0.00014946406,0.000100300924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020182414,0.00068635127,0.00031024558,0.000598983,0.00043109016,0.0016178617,0.000496624,0.0005976591,0.0015462325],"category_scores_gemma":[0.0019600294,0.00019895933,0.0002883144,0.00029541357,0.00067123945,0.0012903516,0.0017465134,0.00068416033,0.0005584187],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00079974014,0.0005699792,0.051366005,0.0009676648,0.00012799649,0.00080983725,0.012401504,0.073739514,0.058969703,0.043919075,0.009895747,0.7464333],"study_design_scores_gemma":[0.0003773395,0.0026775207,0.13011402,0.0011182193,0.00029984594,0.0015991394,0.014295214,0.3654321,0.09256482,0.04216688,0.3491035,0.00025132752],"about_ca_topic_score_codex":0.0037963882,"about_ca_topic_score_gemma":0.0024063943,"teacher_disagreement_score":0.0037963882,"about_ca_system_score_codex":0.00083515904,"about_ca_system_score_gemma":0.0023712453,"threshold_uncertainty_score":0.010673642},"labels":[],"label_agreement":null},{"id":"W2775005333","doi":"10.5194/sd-23-57-2017","title":"Scientific Exploration of Induced SeisMicity and Stress (SEISMS)","year":2017,"lang":"en","type":"article","venue":"Scientific Drilling","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; McGill University","funders":"U.S. Geological Survey; Southern California Earthquake Center","keywords":"Induced seismicity; Geology; Seismology; Tectonics; Fault (geology); Drilling; Earthquake prediction; Engineering","score_opus":0.07282609440347464,"score_gpt":0.26405826108956704,"score_spread":0.1912321666860924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2775005333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5608126,0.15427779,0.16180114,0.034816984,0.0024149683,0.0010617574,0.008645869,0.000644429,0.07552453],"genre_scores_gemma":[0.9093005,0.050314404,0.030614922,0.0030853825,0.0003682512,0.00044345626,0.0011976849,0.00006332714,0.0046120803],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9974969,0.0011392938,0.0002127153,0.00032146386,0.0007593286,0.000070205686],"domain_scores_gemma":[0.9858453,0.00968817,0.0018204243,0.0008341519,0.0015498438,0.0002620355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0077002766,0.00039041456,0.00042103272,0.0017498179,0.00031365085,0.0010350844,0.00063721766,0.00095936976,0.0023219825],"category_scores_gemma":[0.011707848,0.00024230398,0.00047295447,0.0016899044,0.0017962124,0.0020241241,0.0014453277,0.0010682528,0.00027583528],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010496419,0.0004674735,0.066391945,0.023486717,0.00076730485,0.00083318277,0.0053636576,0.0056680962,0.13867012,0.06745377,0.014804068,0.67504394],"study_design_scores_gemma":[0.00018280729,0.0051106163,0.225765,0.0067605553,0.000760068,0.0017349367,0.012349129,0.0050425134,0.13111009,0.14855942,0.46224192,0.0003829838],"about_ca_topic_score_codex":0.0004768146,"about_ca_topic_score_gemma":0.0008509694,"teacher_disagreement_score":0.0077002766,"about_ca_system_score_codex":0.0008978192,"about_ca_system_score_gemma":0.0016219451,"threshold_uncertainty_score":0.040723443},"labels":[],"label_agreement":null},{"id":"W2776681536","doi":"10.1016/j.sedgeo.2017.12.018","title":"The Devils Mountain Fault zone: An active Cascadia upper plate zone of deformation, Pacific Northwest of North America","year":2017,"lang":"en","type":"article","venue":"Sedimentary Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"University of Victoria","keywords":"Geology; Fault (geology); Seafloor spreading; Seismology; Quaternary; Holocene; Active fault; Fault trace; Fault scarp; Paleoseismology; Paleontology","score_opus":0.009875550911327425,"score_gpt":0.22521694835971112,"score_spread":0.2153413974483837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2776681536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929368,0.00030279346,0.00011724772,0.00017433694,0.0000074267823,0.00002251268,0.00065486616,0.000021232408,0.0057627345],"genre_scores_gemma":[0.9972205,0.00026690357,0.00035143155,0.00003073725,0.0000049358378,0.000009987445,0.00052247,0.0000028402987,0.0015901341],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999198,0.000008273523,0.000005825494,0.000021448472,0.000028489063,0.000016224407],"domain_scores_gemma":[0.9998223,0.000012489657,0.000036719925,0.0000066078755,0.00006818819,0.00005374443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012588213,0.00016545608,0.00015138366,0.0009427485,0.0011727202,0.0007869727,0.00024514477,0.00018696216,0.0011387293],"category_scores_gemma":[0.00034676745,0.00011165906,0.00007395286,0.0014019555,0.00066691585,0.00037318195,0.00075160817,0.00014344671,0.000101444224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006749392,0.000051161656,0.9649029,0.00010693616,0.00004355881,0.00071661215,0.003543822,0.00066938275,0.0036882597,0.0012689511,0.0019829914,0.022957968],"study_design_scores_gemma":[0.0000051908332,0.00000953392,0.9940157,0.0000128698775,0.0000087949775,0.00013028609,0.001954228,0.00023844145,0.000111643196,0.00013736775,0.003372714,0.000003151539],"about_ca_topic_score_codex":0.3717699,"about_ca_topic_score_gemma":0.73114145,"teacher_disagreement_score":0.3717699,"about_ca_system_score_codex":0.001239591,"about_ca_system_score_gemma":0.002766905,"threshold_uncertainty_score":0.7392119},"labels":[],"label_agreement":null},{"id":"W2779742602","doi":"10.1002/2017jb014911","title":"Segmentation of Slow Slip Events in South Central Alaska Possibly Controlled by a Subducted Oceanic Plateau","year":2017,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Research Foundation of Korea; Natural Sciences and Engineering Research Council of Canada; Korea Meteorological Administration; National Science Foundation","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Plateau (mathematics); Fault (geology); Slab; Tectonics; Geophysics","score_opus":0.03350542124215864,"score_gpt":0.31892817447306965,"score_spread":0.285422753230911,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2779742602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99967396,0.000013252894,0.00006686487,0.000004880417,5.7472766e-7,0.0000015301637,0.000024019642,0.000004360607,0.00021045233],"genre_scores_gemma":[0.9998846,0.000008016016,0.00003605393,7.383894e-7,4.999004e-7,0.0000012018057,0.000034497065,8.230803e-7,0.000033616958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999293,0.000012315788,0.000008349705,0.000024499923,0.0000090918375,0.000016416532],"domain_scores_gemma":[0.9997464,0.000055051496,0.00009670614,0.000018044657,0.000031541564,0.00005222899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016743389,0.00015342803,0.00019450707,0.0006394077,0.000347012,0.0005395966,0.00020964148,0.00026256882,0.0008178393],"category_scores_gemma":[0.0007034102,0.0001458164,0.00024408127,0.00041223576,0.00042079418,0.00028892138,0.00037478792,0.00012022506,0.0000847441],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002764776,0.000052514966,0.9628118,0.000033983615,0.000082317994,0.00088520313,0.0006037554,0.019752571,0.011643374,0.0005574976,0.00009248149,0.003208052],"study_design_scores_gemma":[0.000011325094,0.00005740634,0.96814716,0.000010952305,0.000026630212,0.00009224767,0.00061023154,0.03009809,0.0005233888,0.00028653667,0.00012431265,0.000011732753],"about_ca_topic_score_codex":0.020941885,"about_ca_topic_score_gemma":0.021715991,"teacher_disagreement_score":0.020941885,"about_ca_system_score_codex":0.0005254341,"about_ca_system_score_gemma":0.00033377067,"threshold_uncertainty_score":0.041639984},"labels":[],"label_agreement":null},{"id":"W2781104394","doi":"10.1007/s00024-017-1759-8","title":"The Central Italy Seismic Sequence (2016): Spatial Patterns and Dynamic Fingerprints","year":2017,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saint Mary's University","funders":"","keywords":"Geology; Seismology; Induced seismicity; Tectonics; Sequence (biology); Seismic gap","score_opus":0.010308934930249022,"score_gpt":0.20886286753057226,"score_spread":0.19855393260032322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2781104394","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9715263,0.0008111829,0.00086603814,0.00023827022,0.00009103156,0.00002478021,0.017443024,0.00017340151,0.008825968],"genre_scores_gemma":[0.9754098,0.00034734205,0.0011678829,0.000015260184,0.000100207995,0.000016921036,0.019633748,0.000037245798,0.0032716342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999871,0.000009929184,0.000014042432,0.00004220392,0.000031529944,0.00003122145],"domain_scores_gemma":[0.9995734,0.000028463826,0.00014879556,0.00005127737,0.000121068035,0.00007690835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002284546,0.00031161393,0.00016508071,0.0031108044,0.0002130382,0.0005491001,0.00019340873,0.0002998644,0.0020793958],"category_scores_gemma":[0.0010695858,0.000102203914,0.000198222,0.0029214157,0.00022123384,0.00030315487,0.0005992605,0.00017936644,0.0012050018],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00093341904,0.00011291619,0.77675563,0.00027467043,0.00010078013,0.0006640125,0.0014304478,0.0055122515,0.012683965,0.0018616735,0.018239448,0.18143082],"study_design_scores_gemma":[0.000006253426,0.000039078022,0.9891104,0.000024579796,0.000016712354,0.00033623603,0.00015700681,0.0011031644,0.00028538075,0.000119760436,0.008794753,0.00000663977],"about_ca_topic_score_codex":0.012744672,"about_ca_topic_score_gemma":0.02147004,"teacher_disagreement_score":0.012744672,"about_ca_system_score_codex":0.0003588035,"about_ca_system_score_gemma":0.00052128534,"threshold_uncertainty_score":0.025340974},"labels":[],"label_agreement":null},{"id":"W2782702107","doi":"10.1103/physreve.97.033002","title":"Universal avalanche statistics and triggering close to failure in a mean-field model of rheological fracture","year":2018,"lang":"en","type":"article","venue":"Physical review. E","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Statistical physics; Dissipation; Viscoelasticity; Rheology; Quasistatic process; Hardening (computing); Criticality; Dissipative system; Critical point (mathematics); Weissenberg number; Mechanics; Physics; Mathematics; Materials science; Thermodynamics; Mathematical analysis","score_opus":0.020222232546836503,"score_gpt":0.2815239472940089,"score_spread":0.2613017147471724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782702107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8473712,0.0023159804,0.14114729,0.0015689767,0.00005833151,0.00003174443,0.00018708818,0.00020133152,0.0071181026],"genre_scores_gemma":[0.9956436,0.0007128794,0.0021488767,0.00004628397,0.000045961682,0.00001851487,0.000044578912,0.000016249975,0.0013230819],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998584,0.000041822994,0.000008758053,0.000032741387,0.000021610524,0.000036749032],"domain_scores_gemma":[0.998958,0.00058260164,0.00022320892,0.00006059309,0.00007154783,0.00010403112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011540223,0.00034706248,0.00067964563,0.0010457992,0.00038334238,0.00096199714,0.0011729877,0.0011091089,0.00092924334],"category_scores_gemma":[0.0025507328,0.00038988807,0.00078530627,0.00045802398,0.0017073553,0.0017798321,0.0005329189,0.0008019231,0.000094140145],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009625052,0.0000735884,0.0061598103,0.00013281748,0.000080066464,0.0006418216,0.0004487077,0.33399984,0.003592941,0.6464039,0.0012613251,0.007108906],"study_design_scores_gemma":[0.000025540487,0.000033305674,0.0030838924,0.000017489403,0.000028178254,0.00011168591,0.000047458594,0.71194625,0.0002395065,0.28399006,0.00045247056,0.000024059835],"about_ca_topic_score_codex":0.003134599,"about_ca_topic_score_gemma":0.0013638416,"teacher_disagreement_score":0.003134599,"about_ca_system_score_codex":0.0011502813,"about_ca_system_score_gemma":0.00051947247,"threshold_uncertainty_score":0.008345902},"labels":[],"label_agreement":null},{"id":"W2783186902","doi":"","title":"Seismic Constraints on the Japan Subduction Zone from Waveform Inversions of SS precursors","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Subduction; Geology; Seismology; Waveform; Tectonics; Computer science","score_opus":0.019482383245371857,"score_gpt":0.2055015732686846,"score_spread":0.18601919002331274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783186902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99632865,0.000073652234,0.0011713422,0.000048116985,0.0000064614155,0.000003758437,0.0003628185,0.000023096536,0.0019821995],"genre_scores_gemma":[0.99836797,0.000052183448,0.00074586587,0.000009178936,0.00000798396,0.0000033120552,0.0006158017,0.000011487257,0.00018622106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993753,0.000006993511,0.000007275507,0.000018582485,0.000011242207,0.000018449571],"domain_scores_gemma":[0.9996562,0.00006731525,0.00007053435,0.000029912471,0.00010711967,0.00006891606],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018227464,0.00038969898,0.0001855303,0.0010879874,0.00032192143,0.00067890313,0.0002461643,0.00020987948,0.001729756],"category_scores_gemma":[0.0010322713,0.00022682309,0.00016508748,0.0010655021,0.0002201993,0.000476213,0.00056484377,0.00028551358,0.00026606434],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072487653,0.000110196874,0.69817126,0.000113313974,0.00011765386,0.0011100251,0.0017350502,0.013088752,0.20774886,0.0030331148,0.0017340163,0.072312936],"study_design_scores_gemma":[0.000060904855,0.000063933614,0.9594198,0.00002241881,0.00016937387,0.00017387398,0.0010233707,0.029990457,0.0058006323,0.0007343365,0.0025160587,0.000024862356],"about_ca_topic_score_codex":0.01433951,"about_ca_topic_score_gemma":0.026973475,"teacher_disagreement_score":0.01433951,"about_ca_system_score_codex":0.00015414364,"about_ca_system_score_gemma":0.00064519496,"threshold_uncertainty_score":0.02851206},"labels":[],"label_agreement":null},{"id":"W2783522532","doi":"10.1016/j.epsl.2018.01.002","title":"Stress rotation across the Cascadia megathrust requires a weak subduction plate boundary at seismogenic depths","year":2018,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University; Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Geology; Subduction; Seismology; Pacific Plate; Plate tectonics; Mantle (geology); Convergent boundary; Slip (aerodynamics); Episodic tremor and slip; Thrust fault; Geophysics; Thrust; Stress field; Fault (geology); Focal mechanism; Tectonics; Oceanic crust","score_opus":0.01314816927140433,"score_gpt":0.2220297880583445,"score_spread":0.20888161878694017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783522532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968424,0.000040176783,0.00042302263,0.00020544993,0.000009738678,0.000005010303,0.00007655411,0.00003144712,0.0023661717],"genre_scores_gemma":[0.9995716,0.0000150353035,0.0000724006,0.000019690708,0.0000036362019,0.0000027796393,0.00007139024,0.00000777769,0.00023560163],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998833,0.000012645741,0.00001394566,0.000032792203,0.000013995464,0.000043398264],"domain_scores_gemma":[0.99918383,0.00009951572,0.00020804409,0.00008100267,0.0001885928,0.00023895815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023723254,0.00029790873,0.00039508543,0.00036987162,0.0007716718,0.0012045313,0.00034495923,0.0005395303,0.0046355934],"category_scores_gemma":[0.0023050748,0.00044989405,0.0002849732,0.00027291803,0.0009266956,0.00073903747,0.001339882,0.000605273,0.0007192224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019059782,0.00015980916,0.6114932,0.00019731048,0.000103035905,0.00089609646,0.0010367497,0.013504255,0.347121,0.009609957,0.0010161687,0.012956473],"study_design_scores_gemma":[0.00004651112,0.00012558277,0.9908766,0.000010837838,0.000021893766,0.000089182824,0.00049606495,0.0029356836,0.003667329,0.001288188,0.0004280992,0.000013970045],"about_ca_topic_score_codex":0.011469176,"about_ca_topic_score_gemma":0.016962554,"teacher_disagreement_score":0.011469176,"about_ca_system_score_codex":0.0009146137,"about_ca_system_score_gemma":0.0008869223,"threshold_uncertainty_score":0.022804856},"labels":[],"label_agreement":null},{"id":"W2784050139","doi":"","title":"Tsunami Detection by High Frequency Radar Using a Time-Correlation Algorithm: Performance Analysis Based on Data From a HF Radar in British Columbia","year":2017,"lang":"en","type":"preprint","venue":"Journal of Media Literacy Education","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society","funders":"","keywords":"Geology; Bathymetry; Radar; Seafloor spreading; Seismology; Remote sensing; Drifter; Doppler effect; Geodesy; Geophysics; Computer science; Oceanography; Telecommunications; Physics","score_opus":0.01675295748555073,"score_gpt":0.25378668346122235,"score_spread":0.23703372597567163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2784050139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99603635,0.0000807352,0.0025826145,0.000036214402,0.000004140611,0.000015333306,0.00019283086,0.00011123609,0.0009405039],"genre_scores_gemma":[0.995915,0.00006638868,0.0029812008,0.000009872456,0.0000025107854,0.0000073408487,0.0005941075,0.000009495996,0.00041408176],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9996488,0.00005708883,0.00002271034,0.00006343073,0.0001294525,0.00007852529],"domain_scores_gemma":[0.9982451,0.00054252753,0.000098037686,0.00007782751,0.0009289145,0.00010756198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007558287,0.00045755965,0.00027881298,0.00083793997,0.00042378498,0.00055656635,0.00045846344,0.00038334203,0.0004717496],"category_scores_gemma":[0.0025030703,0.00013404946,0.00015255231,0.0011739038,0.00029112014,0.00025821413,0.00028507187,0.00025179438,0.00015134743],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017460762,0.00055212836,0.3518521,0.00015208145,0.00023987379,0.0004956741,0.00037010273,0.40945414,0.03970615,0.00074211136,0.0026323784,0.19205727],"study_design_scores_gemma":[0.000052290896,0.00017756545,0.1347756,0.000007555413,0.00003974479,0.00007589728,0.000104867584,0.8574248,0.0068241665,0.00006284627,0.00042561465,0.000029037174],"about_ca_topic_score_codex":0.55298525,"about_ca_topic_score_gemma":0.47817093,"teacher_disagreement_score":0.44701475,"about_ca_system_score_codex":0.0017785922,"about_ca_system_score_gemma":0.0013689513,"threshold_uncertainty_score":0.8992946},"labels":[],"label_agreement":null},{"id":"W2785638767","doi":"10.1190/tle37020135.1","title":"What controls the maximum magnitude of injection-induced earthquakes?","year":2018,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Magnitude (astronomy); Maximum magnitude; Earthquake magnitude; Fault (geology); Seismology; Geology; Probabilistic logic; Moment magnitude scale; Volume (thermodynamics); Mathematics; Statistics; Seismic hazard; Physics; Geometry","score_opus":0.032733997734213024,"score_gpt":0.2558368169166064,"score_spread":0.22310281918239339,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2785638767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8506309,0.0008677256,0.13109772,0.0015339408,0.00012299685,0.000064849846,0.00054353365,0.0005227052,0.014615497],"genre_scores_gemma":[0.99846363,0.000093859766,0.0011740273,0.000021465414,0.000017581018,0.0000058576043,0.000035696776,0.000008050436,0.0001797462],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9996656,0.000087729604,0.000029253284,0.00010556064,0.000063264095,0.000048674196],"domain_scores_gemma":[0.99239326,0.0043039005,0.0022202577,0.0002663665,0.0005207951,0.000295446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014072628,0.00027501414,0.00033767457,0.0005596104,0.00021488998,0.0013044974,0.00050464395,0.0005944513,0.0019720027],"category_scores_gemma":[0.01464417,0.00024826868,0.00026395154,0.00028283274,0.0006435365,0.0012797987,0.00030018762,0.00040123062,0.00032036088],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091009255,0.00023261567,0.29818293,0.00073532196,0.00030609427,0.001075527,0.0005301141,0.4266261,0.055842377,0.095738865,0.004097641,0.115722306],"study_design_scores_gemma":[0.000060722643,0.0006035977,0.26372832,0.00017581272,0.00013038344,0.00069451286,0.00081427355,0.6149559,0.019899555,0.09540584,0.0034129836,0.000118090145],"about_ca_topic_score_codex":0.0017107332,"about_ca_topic_score_gemma":0.0010919367,"teacher_disagreement_score":0.0019720027,"about_ca_system_score_codex":0.00065596664,"about_ca_system_score_gemma":0.0003860266,"threshold_uncertainty_score":0.0074424148},"labels":[],"label_agreement":null},{"id":"W2785962122","doi":"10.1190/tle37020117.1","title":"Performance assessment of the induced seismicity traffic light protocol for northeastern British Columbia and western Alberta","year":2018,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society; Geological Survey of Canada","funders":"University of Calgary","keywords":"Induced seismicity; Seismology; Magnitude (astronomy); Hydraulic fracturing; Geology; Geotechnical engineering; Physics","score_opus":0.02948114273030188,"score_gpt":0.26964665140591837,"score_spread":0.24016550867561648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2785962122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98929626,0.000071140756,0.0023815641,0.00014293357,0.000014035484,0.00032126118,0.0007995299,0.0004215893,0.00655171],"genre_scores_gemma":[0.9926611,0.00008644397,0.0023534417,0.00004253994,0.000004026216,0.000072120296,0.0013382463,0.000024045454,0.0034179294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99883145,0.00010850175,0.00004582386,0.000121936435,0.00065458583,0.00023771168],"domain_scores_gemma":[0.9961384,0.0004115555,0.0002991065,0.00021613554,0.0024980262,0.00043682192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017802676,0.0004616494,0.00023307429,0.0013146532,0.00079469633,0.001011154,0.0011524392,0.00034644132,0.001154258],"category_scores_gemma":[0.0030010568,0.00018040741,0.00016318749,0.0012133706,0.0006893799,0.00035868515,0.0005572336,0.0003671397,0.00026770198],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028231782,0.0013164661,0.49458182,0.00021579258,0.00020080135,0.00069126894,0.0009138352,0.24967635,0.04579413,0.0018723164,0.008634276,0.19327974],"study_design_scores_gemma":[0.00023883593,0.0020045796,0.5647826,0.00007328175,0.00017089129,0.00014910351,0.0052998806,0.3804492,0.03080563,0.0006143249,0.015215187,0.00019647177],"about_ca_topic_score_codex":0.9003333,"about_ca_topic_score_gemma":0.9292341,"teacher_disagreement_score":0.099666715,"about_ca_system_score_codex":0.011592936,"about_ca_system_score_gemma":0.013425311,"threshold_uncertainty_score":0.20050728},"labels":[],"label_agreement":null},{"id":"W2785980453","doi":"10.1190/tle37020107a1.1","title":"Five key lessons gained from induced seismicity monitoring in western Canada","year":2018,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Seismic hazard; Seismology; Key (lock); Hazard; Event (particle physics); Ground motion; Geology; Computer science; Computer security","score_opus":0.04544936664264598,"score_gpt":0.26051307443330723,"score_spread":0.21506370779066125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2785980453","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91616726,0.0022377209,0.00901458,0.015043348,0.00010544626,0.00014100932,0.014176112,0.00019895748,0.042915553],"genre_scores_gemma":[0.9835783,0.0014809538,0.007465298,0.0006329341,0.000059522798,0.00002271467,0.0031731722,0.000046292786,0.0035407546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99918765,0.000101407866,0.00005363338,0.00014278112,0.00032311986,0.00019138904],"domain_scores_gemma":[0.995421,0.0008108253,0.00040669463,0.0004402289,0.002539231,0.00038199706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011216133,0.00035815604,0.00026589163,0.0015595387,0.0014744259,0.0027306837,0.0012457068,0.00045241247,0.0014177995],"category_scores_gemma":[0.0066164555,0.00019208422,0.00016244478,0.0048170756,0.0011950675,0.00083331205,0.0012830689,0.00092910114,0.00018792406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001736344,0.00011267541,0.7536048,0.00027614128,0.00013241875,0.0015169316,0.01273367,0.009386797,0.0050698356,0.00879532,0.020494152,0.18770365],"study_design_scores_gemma":[0.000021387255,0.000049004495,0.87637013,0.00037953552,0.000114128736,0.00037039054,0.02319729,0.0145840915,0.0037516158,0.006418567,0.07463345,0.00011035174],"about_ca_topic_score_codex":0.98443615,"about_ca_topic_score_gemma":0.9934975,"teacher_disagreement_score":0.015563846,"about_ca_system_score_codex":0.012697206,"about_ca_system_score_gemma":0.025584957,"threshold_uncertainty_score":0.09212512},"labels":[],"label_agreement":null},{"id":"W2787028490","doi":"10.1002/2017jb015021","title":"Seismicity Relocation and Fault Structure Near the Leech River Fault Zone, Southern Vancouver Island","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Geology; Seismology; Induced seismicity; Fault (geology); Sinistral and dextral; Seismometer; Active fault; Fault trace; Crust; Paleontology","score_opus":0.022358002500154548,"score_gpt":0.2876856933844599,"score_spread":0.2653276908843053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2787028490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980761,0.00007435044,0.000072965864,0.000020822219,0.000001557432,0.000009760276,0.0006024615,0.000009016498,0.0011328696],"genre_scores_gemma":[0.99792176,0.00007629412,0.00021657783,0.000011870785,9.575981e-7,0.000007908892,0.0008550267,0.0000030776043,0.00090665906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998325,0.000008604372,0.0000080906475,0.00005495264,0.00005129027,0.000044492197],"domain_scores_gemma":[0.9995352,0.00002579005,0.0000876485,0.000023895109,0.00021838016,0.000109068875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012576084,0.00021091584,0.00015597254,0.0014403249,0.0009974237,0.00085027877,0.00032062578,0.00024749892,0.0012011051],"category_scores_gemma":[0.0004932487,0.00015288316,0.00009395164,0.0015940616,0.0004206546,0.00014186988,0.0005713563,0.00024232618,0.00018878467],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004356585,0.000014981947,0.97763467,0.00003639216,0.000036275043,0.00023257744,0.0011402242,0.0005506675,0.007188778,0.000061891165,0.00042155644,0.012638483],"study_design_scores_gemma":[0.0000013773309,0.0000039454253,0.9984156,0.0000068992567,0.0000036225217,0.0000316736,0.0007583204,0.0002003038,0.00015949628,0.0000062997105,0.00041000743,0.0000024894073],"about_ca_topic_score_codex":0.84553254,"about_ca_topic_score_gemma":0.96046543,"teacher_disagreement_score":0.15446746,"about_ca_system_score_codex":0.0028675813,"about_ca_system_score_gemma":0.002395795,"threshold_uncertainty_score":0.31075424},"labels":[],"label_agreement":null},{"id":"W2787691980","doi":"10.1190/tle37020100.1","title":"How faults wake up: The Guthrie-Langston, Oklahoma earthquakes","year":2018,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Alexander von Humboldt-Stiftung","keywords":"Geology; Induced seismicity; Seismology; Sedimentary rock; Basement; Stress field; Fault (geology); Slip (aerodynamics); Paleontology; Archaeology","score_opus":0.03074342179532691,"score_gpt":0.23640041345462412,"score_spread":0.2056569916592972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2787691980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978531,0.00007323214,0.000022720471,0.0003549791,0.0000062819768,0.0000036448075,0.00030724806,0.000004517068,0.0013742589],"genre_scores_gemma":[0.99933547,0.00004815985,0.00002797187,0.000036553833,0.0000044700178,0.0000018616149,0.00012963885,0.0000018405793,0.00041396476],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990714,0.0000082463375,0.000005021414,0.000018648956,0.000012471137,0.00004846466],"domain_scores_gemma":[0.9996284,0.000044389206,0.000114071336,0.000017961906,0.000060198745,0.00013504372],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012285053,0.00012540063,0.00012806935,0.0005947888,0.0012665186,0.000986919,0.00024782098,0.00054314703,0.0023623137],"category_scores_gemma":[0.00054409605,0.00010329805,0.00009895324,0.00065943674,0.00041892222,0.0004716336,0.0006350635,0.000358465,0.00022457026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011307144,0.00006419837,0.9727284,0.00003869729,0.000055942775,0.0009170241,0.0035605885,0.0010832764,0.004853221,0.0002689782,0.0026060147,0.0137105975],"study_design_scores_gemma":[0.0000021731641,0.000010283639,0.995626,0.000009117066,0.000009697923,0.000028010909,0.0028878115,0.0003199842,0.00012289941,0.000029231423,0.0009497533,0.0000050330254],"about_ca_topic_score_codex":0.21789928,"about_ca_topic_score_gemma":0.50886357,"teacher_disagreement_score":0.21789928,"about_ca_system_score_codex":0.0018485861,"about_ca_system_score_gemma":0.0010116195,"threshold_uncertainty_score":0.43326187},"labels":[],"label_agreement":null},{"id":"W2788184996","doi":"10.5194/nhess-2018-37","title":"Risk assessment and management for an extreme accident at a waste slag site","year":2018,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Fundamental Research Funds for the Central Universities; China University of Geosciences; National Natural Science Foundation of China","keywords":"Tailings; Tailings dam; Hazard; Risk management; Slag (welding); Risk analysis (engineering); Environmental science; Civil engineering; Risk assessment; Vulnerability (computing); Waste management; Engineering; Business; Computer science","score_opus":0.03979110737148694,"score_gpt":0.27280186889951424,"score_spread":0.2330107615280273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788184996","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6161121,0.000214954,0.37808365,0.00046243137,0.00005779144,0.000235658,0.00014335255,0.00048235676,0.004207628],"genre_scores_gemma":[0.98300606,0.000046012447,0.015912687,0.0000150501755,0.000008638452,0.000042878375,0.000064985485,0.000010677507,0.00089295546],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990409,0.0003252258,0.000061752304,0.0001305349,0.00030790264,0.00013362753],"domain_scores_gemma":[0.9987503,0.0003807569,0.00025568658,0.0000974593,0.00037877727,0.00013694848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018883978,0.0008382514,0.00052599655,0.0019169024,0.0010988148,0.0011324638,0.0008681841,0.001352119,0.0017140892],"category_scores_gemma":[0.002571609,0.00032121627,0.0011608369,0.00053957396,0.00060251285,0.0010629846,0.0014243094,0.00070369744,0.00016518384],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034813693,0.00021622892,0.04145062,0.00011561434,0.0001331387,0.0009714975,0.00058261113,0.8959984,0.009749879,0.006944112,0.0012251073,0.042264592],"study_design_scores_gemma":[0.000011728355,0.00022966348,0.0064708893,0.000015918999,0.0000549277,0.00016241158,0.00033853322,0.98652214,0.002403231,0.0033491624,0.00040366434,0.00003767461],"about_ca_topic_score_codex":0.005362589,"about_ca_topic_score_gemma":0.0033765147,"teacher_disagreement_score":0.005362589,"about_ca_system_score_codex":0.0010995127,"about_ca_system_score_gemma":0.0009815753,"threshold_uncertainty_score":0.010662794},"labels":[],"label_agreement":null},{"id":"W2788422104","doi":"10.1130/g39864.1","title":"Timing and mechanism of the rise of the Shillong Plateau in the Himalayan foreland","year":2018,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; European Commission; Sight Research UK","keywords":"Foreland basin; Geology; Plateau (mathematics); Lithosphere; Tectonics; Structural basin; Geomorphology; Sedimentary rock; Fault (geology); Paleontology; Seismology","score_opus":0.01609334049863476,"score_gpt":0.20650715546742288,"score_spread":0.19041381496878812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788422104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99730194,0.00019789294,0.00015045141,0.000099137316,0.0000038613566,0.000004411802,0.00009455852,0.000014367151,0.0021333897],"genre_scores_gemma":[0.9996604,0.000068318186,0.00004532689,0.000006484952,0.0000028777515,0.000001197521,0.000033978915,0.0000010627048,0.00018041514],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.000009200394,0.0000049602586,0.00001664588,0.000011930177,0.00002056735],"domain_scores_gemma":[0.99971443,0.000046062498,0.00008487022,0.000023159073,0.00007614976,0.000055302786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018115621,0.00010076626,0.00012775516,0.0011046323,0.00042907754,0.00093222247,0.00022872008,0.0002511899,0.0017149068],"category_scores_gemma":[0.00040122087,0.0001652976,0.000110965084,0.0010975219,0.00055006606,0.00034444281,0.00035932328,0.0002046577,0.000188549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024093318,0.000044523378,0.9440148,0.00010734336,0.00006298924,0.0016485613,0.0021523982,0.003549072,0.027511472,0.0029880386,0.00051772076,0.017162135],"study_design_scores_gemma":[0.000005143738,0.000020978454,0.9969092,0.000012080231,0.0000078170815,0.000119856326,0.000619079,0.00095930655,0.00059685763,0.00018439864,0.0005599894,0.000005450067],"about_ca_topic_score_codex":0.030517893,"about_ca_topic_score_gemma":0.036343943,"teacher_disagreement_score":0.030517893,"about_ca_system_score_codex":0.0008823108,"about_ca_system_score_gemma":0.00046898946,"threshold_uncertainty_score":0.06068057},"labels":[],"label_agreement":null},{"id":"W2788621558","doi":"10.1038/s41561-018-0061-4","title":"Corrugated megathrust revealed offshore from Costa Rica","year":2018,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Subduction; Trench; Seismology; Slip (aerodynamics); Submarine pipeline; Fault (geology); Episodic tremor and slip; Convergent boundary; Plate tectonics; Reflection (computer programming); Petrology; Tectonics; Geotechnical engineering; Oceanic crust; Materials science","score_opus":0.010460567823729035,"score_gpt":0.23045438787494837,"score_spread":0.21999382005121934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2788621558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930438,0.00013927816,0.0001627378,0.00006709574,0.000005722386,0.000012908441,0.00033294418,0.000014660502,0.0062209996],"genre_scores_gemma":[0.9988502,0.00006166079,0.00019287188,0.000014948133,0.0000029740715,0.0000044459066,0.00016125136,0.000003342002,0.0007082661],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.000009273168,0.0000045024053,0.000013566932,0.000011962104,0.000020662967],"domain_scores_gemma":[0.9997774,0.000019510453,0.00006138449,0.000042953812,0.0000754152,0.000023401826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011337235,0.00021649864,0.00015356386,0.0007967087,0.00064062007,0.0004154114,0.00029826572,0.00037279844,0.0013442117],"category_scores_gemma":[0.0005520412,0.00010661729,0.00009610498,0.00094780995,0.00030722594,0.00017372759,0.0006791788,0.0002378073,0.00025805563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020590742,0.00005558665,0.9160698,0.00009948186,0.000074567535,0.0057164226,0.005739595,0.001386455,0.038614955,0.0010102097,0.0013866506,0.029640434],"study_design_scores_gemma":[0.0000029971231,0.000019221316,0.9948224,0.000011670187,0.00001354442,0.0005289422,0.0015185786,0.0004665371,0.00036124242,0.000039542694,0.002211899,0.0000034731677],"about_ca_topic_score_codex":0.062064443,"about_ca_topic_score_gemma":0.18506825,"teacher_disagreement_score":0.062064443,"about_ca_system_score_codex":0.0005080095,"about_ca_system_score_gemma":0.00046642972,"threshold_uncertainty_score":0.12340635},"labels":[],"label_agreement":null},{"id":"W2789459589","doi":"10.1126/sciadv.aar2982","title":"Fluid pressure and shear zone development over the locked to slow slip region in Cascadia","year":2018,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Alfred P. Sloan Foundation","keywords":"Subduction; Episodic tremor and slip; Geology; Seismology; Slip (aerodynamics); Shear (geology); Transition zone; Fluid pressure; Petrology; Geophysics; Mechanics; Tectonics; Physics","score_opus":0.013883391238983536,"score_gpt":0.2380977452798776,"score_spread":0.22421435404089407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789459589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990196,0.000057613663,0.000041981602,0.000046643,0.000001934239,0.0000017942349,0.00012763367,0.000026033553,0.0006767841],"genre_scores_gemma":[0.99958473,0.00004093408,0.000040446837,0.000006411079,0.0000013574164,0.0000025299532,0.0001100652,0.0000043026066,0.0002092173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998745,0.000007677199,0.000010200108,0.00005778016,0.000023000945,0.000026832933],"domain_scores_gemma":[0.99969816,0.000028090306,0.00009564189,0.00002129828,0.000060247283,0.00009648409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014227563,0.00041321665,0.00028497865,0.0018215594,0.000650819,0.000749102,0.00031687584,0.000379407,0.0020904774],"category_scores_gemma":[0.00074093125,0.00039651166,0.0002709138,0.00091753766,0.0009083785,0.00032321856,0.00095830136,0.00030947427,0.00025900238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047323768,0.0000734235,0.9015361,0.00013403491,0.00014787662,0.001271427,0.004366973,0.0035695005,0.07660301,0.00031307302,0.00042677732,0.011084456],"study_design_scores_gemma":[0.0000042987126,0.000013968307,0.99898964,0.000004574961,0.000008448639,0.00003594349,0.00033668356,0.0002522371,0.00018458637,0.000023927434,0.0001413193,0.00000437212],"about_ca_topic_score_codex":0.07770529,"about_ca_topic_score_gemma":0.104327,"teacher_disagreement_score":0.07770529,"about_ca_system_score_codex":0.0013993543,"about_ca_system_score_gemma":0.0006498258,"threshold_uncertainty_score":0.15450597},"labels":[],"label_agreement":null},{"id":"W2789862492","doi":"10.1002/2017jb014966","title":"Catalog of Offshore Seismicity in Cascadia: Insights Into the Regional Distribution of Microseismicity and its Relation to Subduction Processes","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; National Science Foundation","keywords":"Induced seismicity; Geology; Seismology; Subduction; Intraplate earthquake; Submarine pipeline; Seismometer; Triple junction; Pacific Plate; Deformation (meteorology); Tectonics; Oceanography","score_opus":0.0384170504282442,"score_gpt":0.3082508591527469,"score_spread":0.2698338087245027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789862492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98387975,0.00033096672,0.00034955953,0.000045189514,0.000005035659,0.00002846704,0.012023298,0.00014177259,0.0031958423],"genre_scores_gemma":[0.97589207,0.00056816725,0.0006219193,0.0000133579615,0.000013199869,0.000053898188,0.02159057,0.000039988085,0.0012068339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966943,0.000023492788,0.00004944928,0.00008053047,0.000113633774,0.00006340084],"domain_scores_gemma":[0.99784625,0.00018195702,0.0006804196,0.00023395917,0.00063703593,0.0004204231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003729476,0.0004699254,0.00037093836,0.008716805,0.0005380215,0.0005843298,0.00034528348,0.00020475216,0.0016678991],"category_scores_gemma":[0.0012518538,0.00023711857,0.00030980105,0.008004891,0.00027163333,0.00027286573,0.0011174567,0.0001641288,0.00046170113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004484039,0.000015919397,0.98328364,0.000085085216,0.000057742986,0.00019041062,0.00065861875,0.00076361344,0.0026143973,0.00007871438,0.0011191812,0.011087821],"study_design_scores_gemma":[0.0000017721342,0.000009860163,0.99813473,0.000008140645,0.0000083501955,0.00004750265,0.00018526734,0.00020078442,0.00011293359,0.000018335364,0.0012684092,0.000003898675],"about_ca_topic_score_codex":0.062153365,"about_ca_topic_score_gemma":0.10745181,"teacher_disagreement_score":0.062153365,"about_ca_system_score_codex":0.0006312901,"about_ca_system_score_gemma":0.0008944333,"threshold_uncertainty_score":0.1235832},"labels":[],"label_agreement":null},{"id":"W2790154456","doi":"10.1144/sp477.9","title":"Tsunami modelling of the 7250 cal years BP Betsiamites submarine landslide","year":2018,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"SNC-Lavalin (Canada); Université Laval","funders":"Ministère des Transports; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Landslide; Submarine landslide; Submarine; Geology; Seismology; Oceanography","score_opus":0.033682275469551305,"score_gpt":0.22284809652779825,"score_spread":0.18916582105824695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790154456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963659,0.000030338386,0.0006880407,0.00004396643,0.000008191391,0.000013077379,0.00058937335,0.00007343238,0.002187668],"genre_scores_gemma":[0.9983437,0.000024770994,0.0003195781,0.0000071086056,0.000003040787,0.000007918116,0.00055841013,0.00001152133,0.00072398706],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994004,0.0000040312216,0.000003359874,0.000010948961,0.00001857927,0.000023052437],"domain_scores_gemma":[0.9998698,0.000016582437,0.000021163394,0.000008878868,0.000047983514,0.00003549756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011367101,0.00055418507,0.0002736778,0.00070527924,0.0006241731,0.0007718701,0.0006394793,0.000831424,0.0018637618],"category_scores_gemma":[0.00034997484,0.00025622497,0.0005006252,0.0005504188,0.0003082552,0.00023061421,0.00030333383,0.00046247066,0.00041945133],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033739686,0.00018868389,0.19298097,0.00006530393,0.00019659052,0.0021752457,0.0003346504,0.7737402,0.01701018,0.00082569424,0.0017602164,0.010384877],"study_design_scores_gemma":[0.000042642656,0.000062410734,0.20797268,0.000019049761,0.000041153213,0.00009586082,0.00022934907,0.7886885,0.001489248,0.00012327627,0.001201127,0.00003474767],"about_ca_topic_score_codex":0.50105995,"about_ca_topic_score_gemma":0.4737016,"teacher_disagreement_score":0.50105995,"about_ca_system_score_codex":0.002323461,"about_ca_system_score_gemma":0.0013589406,"threshold_uncertainty_score":0.9962869},"labels":[],"label_agreement":null},{"id":"W2790774395","doi":"10.2118/189820-ms","title":"Empirical and Numerical Investigation of the Effects of Hydraulic Fracturing Injection Rate on the Magnitude Distribution of Induced Seismicity Events","year":2018,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Induced seismicity; Geology; Slip (aerodynamics); Hydraulic fracturing; Pore water pressure; Magnitude (astronomy); Seismology; Geotechnical engineering; Physics; Thermodynamics","score_opus":0.020944634822165107,"score_gpt":0.23727842918130038,"score_spread":0.21633379435913527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790774395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925345,0.00000862791,0.0003046709,0.000008742559,3.315579e-7,0.0000037777831,0.000067886154,0.0000124897415,0.00033992872],"genre_scores_gemma":[0.9997451,0.0000060898637,0.00014217928,8.3609507e-7,2.482993e-7,0.0000015166113,0.000053001593,0.0000015267988,0.000049421156],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99969053,0.000083765844,0.000029502835,0.00006175452,0.00008162487,0.00005277728],"domain_scores_gemma":[0.9884548,0.009161248,0.0011981433,0.00039929085,0.0006151169,0.00017136721],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00084544637,0.00017431182,0.00017299612,0.0005715003,0.0001819456,0.00043557413,0.00039475865,0.0002887135,0.0010086227],"category_scores_gemma":[0.009148266,0.00018741177,0.00017431332,0.00059314794,0.000572745,0.0003005361,0.00021020013,0.00027948577,0.00009597438],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028933783,0.00023056992,0.74345005,0.00007318895,0.000084599604,0.00048223243,0.00027515664,0.23244093,0.009493896,0.00062496756,0.00022786978,0.012327203],"study_design_scores_gemma":[0.000012408884,0.00015436503,0.56145084,0.000012001472,0.000021415472,0.00015621205,0.00032699556,0.43386012,0.003656577,0.00010125301,0.00022619366,0.00002154494],"about_ca_topic_score_codex":0.046721157,"about_ca_topic_score_gemma":0.05496306,"teacher_disagreement_score":0.046721157,"about_ca_system_score_codex":0.00095425604,"about_ca_system_score_gemma":0.0005163476,"threshold_uncertainty_score":0.09289843},"labels":[],"label_agreement":null},{"id":"W2790953978","doi":"10.1002/2017jb015025","title":"Pressure and Stress Prediction in the Nankai Accretionary Prism: A Critical State Soil Mechanics Porosity‐Based Approach","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Accretionary wedge; Geology; Porosity; Wedge (geometry); Pore water pressure; Shear (geology); Overburden pressure; Effective stress; Shear stress; Shearing (physics); Décollement; Differential stress; Stress (linguistics); Prism; Geotechnical engineering; Mineralogy; Mechanics; Subduction; Petrology; Materials science; Seismology; Geometry; Composite material; Deformation (meteorology); Optics; Tectonics","score_opus":0.039191433163419324,"score_gpt":0.3129041564054361,"score_spread":0.2737127232420168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790953978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98123115,0.00006811882,0.01605215,0.00009045612,0.0000059790314,0.00001715571,0.00016424942,0.0000949597,0.0022757652],"genre_scores_gemma":[0.99893755,0.000019872976,0.00091254554,0.000004404098,0.0000014035872,0.0000042913,0.000041277668,0.0000033583722,0.000075237316],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999008,0.000016730777,0.000006825655,0.000023017437,0.000031040177,0.00002161383],"domain_scores_gemma":[0.9996662,0.00010030848,0.000062943785,0.000025663461,0.00010117826,0.000043776003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029575234,0.00039130752,0.00032118475,0.00086568936,0.00044175438,0.0008576015,0.0012374877,0.0007156132,0.0006903184],"category_scores_gemma":[0.0012110827,0.00054901827,0.0004713507,0.0005181652,0.00073944964,0.0005911227,0.00058029825,0.00042370296,0.0001259202],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045092493,0.000041192845,0.04742547,0.000029094832,0.00003206921,0.0001681108,0.000044717057,0.9425883,0.0035133867,0.0014722822,0.000101413905,0.0045389268],"study_design_scores_gemma":[0.000006951194,0.000018599258,0.0100556705,0.0000054561847,0.000004814974,0.000019915611,0.000023140594,0.9883359,0.0006844412,0.00078285893,0.00005332058,0.000008950878],"about_ca_topic_score_codex":0.032768562,"about_ca_topic_score_gemma":0.018743558,"teacher_disagreement_score":0.032768562,"about_ca_system_score_codex":0.0013292213,"about_ca_system_score_gemma":0.0014762812,"threshold_uncertainty_score":0.065155625},"labels":[],"label_agreement":null},{"id":"W2791374322","doi":"10.5194/se-9-833-2018","title":"Density structure and isostasy of the lithosphere in Egypt and their relation to seismicity","year":2018,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Population and Public Health; King Saud University","keywords":"Geology; Lithosphere; Crust; Isostasy; Mantle (geology); Gravity anomaly; Seismology; Seismic tomography; Geophysics; Asthenosphere; Tectonics; Paleontology","score_opus":0.008439607677011943,"score_gpt":0.2020307319908778,"score_spread":0.19359112431386585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791374322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990256,0.000053075448,0.00035203405,0.000010706612,4.1046198e-7,0.0000013484198,0.0001650267,0.000010363596,0.0003814467],"genre_scores_gemma":[0.99949586,0.000041801453,0.00014132149,9.0771425e-7,6.039367e-7,0.000001136796,0.00022220273,0.0000014332742,0.00009473455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994755,0.0000073431256,0.00000534811,0.000012489339,0.000013113878,0.000014164616],"domain_scores_gemma":[0.999851,0.00003283577,0.00004646121,0.000014597599,0.000036918107,0.000018123952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014860378,0.00019139095,0.00015098737,0.0013443104,0.0001230124,0.00050919387,0.00021626076,0.00014997162,0.0009787678],"category_scores_gemma":[0.00052460784,0.00019814055,0.00023370492,0.0010679532,0.00016851885,0.00027533868,0.00042333556,0.00012248827,0.00015101573],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012717639,0.000023489061,0.928674,0.00003028501,0.00011782157,0.00014548702,0.0001736961,0.051148295,0.005170823,0.00061891665,0.00011551196,0.013654567],"study_design_scores_gemma":[0.000008546668,0.000013954307,0.9266495,0.000008270358,0.000018240022,0.0000596051,0.00019899468,0.07174105,0.0007219048,0.00022135362,0.00035092756,0.000007645236],"about_ca_topic_score_codex":0.03785742,"about_ca_topic_score_gemma":0.021319296,"teacher_disagreement_score":0.03785742,"about_ca_system_score_codex":0.0006025286,"about_ca_system_score_gemma":0.00031553165,"threshold_uncertainty_score":0.07527411},"labels":[],"label_agreement":null},{"id":"W2791589553","doi":"10.1002/2017gl076100","title":"The Geological Susceptibility of Induced Earthquakes in the Duvernay Play","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology; Tectonics; Seismic hazard; Basement; Sedimentary rock; Paleontology","score_opus":0.0656186787181504,"score_gpt":0.316037116866944,"score_spread":0.2504184381487936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791589553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993081,0.000011304894,0.00010520155,0.000028224486,3.8454215e-7,0.0000014540177,0.00006627509,0.000004934651,0.00047427282],"genre_scores_gemma":[0.99979776,0.00000437029,0.000026769943,0.0000014992157,2.0056318e-7,4.085979e-7,0.0000701777,8.999984e-7,0.00009792029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997731,0.00007610413,0.000016285425,0.000047529466,0.00003322911,0.000053699412],"domain_scores_gemma":[0.9991289,0.0002879762,0.00018934111,0.000082071565,0.00017054625,0.00014114019],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003126167,0.00011788569,0.00018012863,0.0009098758,0.00046306153,0.0007598914,0.00040708308,0.00027822718,0.002079],"category_scores_gemma":[0.0028174652,0.0001256121,0.00013582585,0.00051746506,0.00069718016,0.00029627274,0.00067223137,0.0002070207,0.0002597606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012118826,0.000019385461,0.98680633,0.00001095382,0.000051343173,0.00015070003,0.0011777185,0.0045189383,0.002174095,0.0008170989,0.00018569505,0.0039664507],"study_design_scores_gemma":[0.0000033824451,0.000026040292,0.98550236,0.000004088873,0.0000066443313,0.00005643294,0.0008766785,0.012775611,0.00019347064,0.00016175765,0.00038781334,0.0000057705597],"about_ca_topic_score_codex":0.24035707,"about_ca_topic_score_gemma":0.351331,"teacher_disagreement_score":0.24035707,"about_ca_system_score_codex":0.0015755824,"about_ca_system_score_gemma":0.0005073768,"threshold_uncertainty_score":0.47791606},"labels":[],"label_agreement":null},{"id":"W2791804126","doi":"10.3103/s0747923918020081","title":"Characteristics of Seismicity in the Areas of Large Water Reservoirs and Waterfalls: The Role of Effects from Additional Load and Permanent Vibration","year":2018,"lang":"en","type":"article","venue":"Seismic Instruments","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology; Crust; Hydrology (agriculture); Geotechnical engineering; Geophysics","score_opus":0.006279869985673189,"score_gpt":0.1933033381346451,"score_spread":0.18702346814897192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791804126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99959165,0.000015783151,0.00015265298,0.0000035721034,6.6761237e-7,0.0000022523025,0.00004943742,0.0000043533337,0.00017953463],"genre_scores_gemma":[0.99982244,0.00000931365,0.00004519408,7.4708106e-7,0.000001377999,0.0000012838632,0.00007417411,8.3529426e-7,0.00004460166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990594,0.00001315823,0.000010485634,0.000019879724,0.000027599055,0.000022822343],"domain_scores_gemma":[0.9993432,0.0001636031,0.00026617548,0.00002961324,0.000074709846,0.00012271198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011396633,0.00014809807,0.0001583678,0.0007229714,0.00014907695,0.00015943963,0.00013004571,0.0001842204,0.0007135206],"category_scores_gemma":[0.00091397605,0.00009828996,0.00011163158,0.0007308188,0.00024731658,0.00018647754,0.000276298,0.00010845255,0.00009469747],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029565714,0.00005647544,0.95504457,0.000046545632,0.000039739112,0.0011602589,0.0008825677,0.0032161006,0.028434157,0.000112323934,0.00009717323,0.010614388],"study_design_scores_gemma":[0.0000020798943,0.00007670771,0.9978836,0.0000016052173,0.000006395044,0.00023454343,0.00022554789,0.0010511227,0.00041620867,0.000019102528,0.000079607984,0.0000034465525],"about_ca_topic_score_codex":0.0021836825,"about_ca_topic_score_gemma":0.0034902159,"teacher_disagreement_score":0.0021836825,"about_ca_system_score_codex":0.00014873051,"about_ca_system_score_gemma":0.00011604166,"threshold_uncertainty_score":0.00434196},"labels":[],"label_agreement":null},{"id":"W2792569489","doi":"10.1093/gji/ggx519","title":"Inference of viscosity jump at 670 km depth and lower mantle viscosity structure from GIA observations","year":2017,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Jump; Mantle (geology); Inference; Viscosity; Geophysics; Geodesy; Thermodynamics; Physics; Computer science; Astronomy; Artificial intelligence","score_opus":0.03084908236543387,"score_gpt":0.26321299274304927,"score_spread":0.2323639103776154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792569489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99756986,0.000032204873,0.0015245584,0.000019564677,9.726812e-7,0.0000058887235,0.00032482095,0.000066972316,0.00045510608],"genre_scores_gemma":[0.9980045,0.000026672407,0.00106166,0.0000050091166,0.0000018798399,0.000005561735,0.00077116594,0.000010276277,0.00011320837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985397,0.000020294769,0.0000067083192,0.00005558972,0.000023922115,0.00003955032],"domain_scores_gemma":[0.9995839,0.000082951025,0.000115318304,0.000057488036,0.000059274225,0.000101075995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042409755,0.00042280543,0.0003273511,0.0015934941,0.0003374685,0.0007452122,0.00047576067,0.00051077834,0.000471253],"category_scores_gemma":[0.0018468949,0.0005697843,0.0008101422,0.0008203857,0.0004322603,0.0006127099,0.00071005156,0.00048188207,0.00026183858],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020180081,0.000085495936,0.92264897,0.000035588175,0.00017029219,0.00012989143,0.00039679074,0.04131794,0.024580996,0.0010506761,0.0002838594,0.00909774],"study_design_scores_gemma":[0.000015299955,0.00002692177,0.8198116,0.0000081524295,0.0000515805,0.000043263033,0.00009841678,0.17707363,0.0021994703,0.00033145543,0.00031354016,0.000026772552],"about_ca_topic_score_codex":0.06392933,"about_ca_topic_score_gemma":0.045871805,"teacher_disagreement_score":0.06392933,"about_ca_system_score_codex":0.0013553287,"about_ca_system_score_gemma":0.00074088085,"threshold_uncertainty_score":0.12711442},"labels":[],"label_agreement":null},{"id":"W2792596103","doi":"10.1130/ges01531.1","title":"Learning from crustal deformation associated with the M9 2011 Tohoku-oki earthquake","year":2018,"lang":"en","type":"article","venue":"Geosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Interplate earthquake; Subduction; Slip (aerodynamics); Trench; Tsunami earthquake; Seafloor spreading; Geodetic datum; Episodic tremor and slip; Seismic gap; Submarine pipeline; Bathymetry; Earthquake rupture; Fault (geology); Geodesy; Tectonics; Geophysics; Geotechnical engineering","score_opus":0.012019136422264088,"score_gpt":0.18403668417151614,"score_spread":0.17201754774925204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792596103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963967,0.00017392501,0.0011941397,0.0002054486,0.00002131302,0.000008119375,0.00066177396,0.00006288379,0.00127575],"genre_scores_gemma":[0.9969415,0.0002297083,0.00096343504,0.000028534994,0.000031563497,0.000005801212,0.0013799373,0.000009474758,0.0004099641],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999225,0.0000098965875,0.00000808667,0.000032371707,0.000012197135,0.000014891404],"domain_scores_gemma":[0.99959856,0.00008374097,0.00012226049,0.000055559252,0.000075719785,0.000064263644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021322172,0.00043173396,0.0002312706,0.0007268809,0.0002620159,0.0005395953,0.00030455724,0.00046764818,0.0010744162],"category_scores_gemma":[0.0019724325,0.000174819,0.00028486212,0.0007117521,0.00018730902,0.00076388096,0.0006205666,0.00039853432,0.0004886595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002541022,0.00018911494,0.80838245,0.00010415124,0.00011727573,0.00095065124,0.00070818857,0.032635693,0.0058036083,0.0004155378,0.003939204,0.14650008],"study_design_scores_gemma":[0.000013698145,0.00012546034,0.901906,0.00006035944,0.00005651011,0.00016043393,0.00091940135,0.092399895,0.0013470758,0.0013016571,0.001670184,0.000039345206],"about_ca_topic_score_codex":0.005616869,"about_ca_topic_score_gemma":0.0120668,"teacher_disagreement_score":0.005616869,"about_ca_system_score_codex":0.00029035372,"about_ca_system_score_gemma":0.00021044338,"threshold_uncertainty_score":0.011168361},"labels":[],"label_agreement":null},{"id":"W2793178148","doi":"10.1155/2018/9479528","title":"Modelling Seismically Induced Mesothermal Goldfields along the Deep-Rooted Cadillac-Larder Lake Fault, Abitibi, Canada","year":2018,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ministère des Ressources naturelles et des Forêts (Québec); Université du Québec à Chicoutimi","funders":"Ministère de l'Énergie et des Ressources Naturelles; Université du Québec à Chicoutimi","keywords":"Geology; Archean; Fault (geology); Hydrogeology; Hydrothermal circulation; Induced seismicity; Seismology; Geochemistry; Geotechnical engineering","score_opus":0.0163698478053626,"score_gpt":0.20192249664136686,"score_spread":0.18555264883600425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793178148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9859428,0.00013572117,0.006114138,0.00016779239,0.000018920728,0.000040398805,0.001238352,0.00018961889,0.0061522913],"genre_scores_gemma":[0.9945634,0.00010020884,0.0028226317,0.00001878141,0.000004920598,0.000022417691,0.0004719091,0.000025256764,0.0019703342],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999349,0.000006367168,0.0000032378794,0.000018305163,0.000013103236,0.000024060535],"domain_scores_gemma":[0.9998573,0.0000471668,0.000021484368,0.000008868186,0.000040227224,0.000024990395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012501416,0.00068987085,0.0002768721,0.00048768296,0.00045582224,0.0011336387,0.0009402112,0.001069702,0.001517838],"category_scores_gemma":[0.00059394276,0.00034584504,0.00045837602,0.0005556838,0.0007071823,0.00021789192,0.0003982799,0.00037114407,0.00012120105],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027606557,0.00002214943,0.008525183,0.0000242717,0.000013823454,0.00007944537,0.000039262955,0.9878656,0.0013002979,0.0004239027,0.00015938467,0.0015191096],"study_design_scores_gemma":[0.000011834892,0.000008584626,0.003988099,0.000004172269,0.0000063439084,0.0000068493796,0.000048411614,0.9953258,0.0002777415,0.00009087113,0.00022619926,0.000005081369],"about_ca_topic_score_codex":0.7572497,"about_ca_topic_score_gemma":0.69516504,"teacher_disagreement_score":0.24275029,"about_ca_system_score_codex":0.0040509044,"about_ca_system_score_gemma":0.00510865,"threshold_uncertainty_score":0.48835975},"labels":[],"label_agreement":null},{"id":"W2793462505","doi":"10.1007/s10950-018-9734-0","title":"Fault slip and identification of the second fault plane in the Varzeghan earthquake doublet","year":2018,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Institutes of Health Research; Uppsala Universitet; Northwestern University","keywords":"Aftershock; Seismology; Geology; Slip (aerodynamics); Intraplate earthquake; Coulomb; Induced seismicity; Structural geology; Geodesy; Physics; Tectonics; Nuclear physics","score_opus":0.01607345027571372,"score_gpt":0.23342474970252822,"score_spread":0.2173512994268145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793462505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994647,0.000023641263,0.00016431321,0.000011789622,0.000002970576,0.0000019189451,0.000046708876,0.0000059242543,0.00027806067],"genre_scores_gemma":[0.99953365,0.000019112706,0.00017765739,0.000003200316,0.0000029217013,0.0000015123769,0.00018166032,0.0000018737267,0.00007822559],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989283,0.000011839615,0.0000051924353,0.000027650804,0.000024368725,0.00003811683],"domain_scores_gemma":[0.9998068,0.000029661864,0.00006934585,0.000016452746,0.000048017933,0.000029701096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016188828,0.0003087543,0.00026617927,0.0013777949,0.00028145948,0.00052672677,0.00021429847,0.00028668213,0.00047168398],"category_scores_gemma":[0.0006928259,0.00013587066,0.00016983662,0.000770157,0.00022559437,0.00023337716,0.00033003945,0.00024210608,0.00013292603],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050468184,0.000113219176,0.9278902,0.000036384965,0.00006088043,0.0012305349,0.00036792675,0.017678784,0.02213437,0.00067598914,0.0007034215,0.028603712],"study_design_scores_gemma":[0.000019800764,0.00004500197,0.9673883,0.0000075955463,0.000014083328,0.0001931046,0.00025720417,0.030465974,0.0011288323,0.00013088498,0.00034003935,0.000009234311],"about_ca_topic_score_codex":0.022759872,"about_ca_topic_score_gemma":0.028269341,"teacher_disagreement_score":0.022759872,"about_ca_system_score_codex":0.00039068112,"about_ca_system_score_gemma":0.00033827245,"threshold_uncertainty_score":0.045254827},"labels":[],"label_agreement":null},{"id":"W2793768150","doi":"10.1002/2017jb014524","title":"Migration Imaging of the Java Subduction Zones","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Slab; Subduction; Classification of discontinuities; Seismology; Discontinuity (linguistics); Trench; Transition zone; Mantle (geology); Underplating; Petrology; Geophysics; Tectonics","score_opus":0.03966884684266202,"score_gpt":0.3224649870142029,"score_spread":0.28279614017154087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793768150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99697626,0.00006188376,0.0012030083,0.00002092304,0.0000043586633,0.0000068230233,0.00033203137,0.00008417065,0.0013105634],"genre_scores_gemma":[0.9966871,0.000056538393,0.0025877177,0.000007907616,0.0000032980452,0.0000039043907,0.0002774977,0.000012524064,0.00036342893],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999615,0.0000021393055,0.0000024083201,0.000012649624,0.000008966634,0.0000124335975],"domain_scores_gemma":[0.99993014,0.000005004119,0.000020513815,0.000004900783,0.000023093819,0.000016350703],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009148039,0.00025286738,0.000116383424,0.0010446531,0.00022604717,0.00030168757,0.00024314452,0.0001569834,0.00080224796],"category_scores_gemma":[0.00014870909,0.00012883145,0.00011609855,0.0006277697,0.00011842255,0.00017387689,0.00038407344,0.00016142662,0.00016883972],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048247125,0.00012076055,0.28262207,0.00011207084,0.00006839929,0.0005505113,0.0009127402,0.003771884,0.64074564,0.0004224827,0.000554173,0.06963687],"study_design_scores_gemma":[0.000029403285,0.000083953375,0.9604389,0.00001916557,0.000046919817,0.00031391424,0.00058004895,0.012507353,0.024079643,0.0001560536,0.0017215926,0.000023015558],"about_ca_topic_score_codex":0.011893591,"about_ca_topic_score_gemma":0.022527635,"teacher_disagreement_score":0.011893591,"about_ca_system_score_codex":0.0002245435,"about_ca_system_score_gemma":0.00023324123,"threshold_uncertainty_score":0.023648739},"labels":[],"label_agreement":null},{"id":"W2793853953","doi":"10.1144/sp470.9","title":"Examining the influence of tectonic inheritance on the evolution of the North Atlantic using a palinspastic deformable plate reconstruction","year":2018,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Inheritance (genetic algorithm); Plate tectonics; Paleontology; Tectonics; Geology; Evolutionary biology; Biology; Genetics","score_opus":0.03597479312741776,"score_gpt":0.21949115343733175,"score_spread":0.18351636030991397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793853953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97345454,0.000056832225,0.024073934,0.00009525489,0.0000055686637,0.000010903414,0.0003321477,0.0001750324,0.0017958339],"genre_scores_gemma":[0.99247086,0.000019589967,0.006984522,0.000006047174,0.0000010542581,0.0000036752613,0.00021724656,0.00003069989,0.00026633145],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981266,0.000051773855,0.000014614786,0.00006305323,0.000042151543,0.000015656053],"domain_scores_gemma":[0.9993988,0.00019683839,0.00012742895,0.00012373511,0.000121226425,0.00003184764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006601898,0.00034911928,0.00020367772,0.00058144843,0.00025036596,0.0005839555,0.000594604,0.0003210491,0.0014419319],"category_scores_gemma":[0.002335598,0.0003160808,0.0005184698,0.00040542244,0.00034167807,0.00034256213,0.00042556238,0.00036534265,0.00022827106],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001221537,0.000040055194,0.10517038,0.000035164332,0.000115289404,0.00012209012,0.0001415904,0.8536305,0.0134230945,0.0014141167,0.00011331791,0.025672255],"study_design_scores_gemma":[0.000007852442,0.00004073819,0.0608105,0.0000092130185,0.000021579592,0.0000498291,0.00006099829,0.9365868,0.0018663214,0.0002704503,0.00026097105,0.000014817876],"about_ca_topic_score_codex":0.04450639,"about_ca_topic_score_gemma":0.049417987,"teacher_disagreement_score":0.04450639,"about_ca_system_score_codex":0.0008612317,"about_ca_system_score_gemma":0.0004115412,"threshold_uncertainty_score":0.08849472},"labels":[],"label_agreement":null},{"id":"W2793870849","doi":"10.1093/gji/ggy114","title":"The 2017 July 20 Mw 6.6 Bodrum–Kos earthquake illuminates active faulting in the Gulf of Gökova, SW Turkey","year":2018,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Seismology; Aftershock; Graben; Induced seismicity; Ridge; Fault (geology); Bathymetry; Fault trace; Active fault; Fault plane; Epicenter; Echelon formation; Tectonics; Paleontology; Oceanography","score_opus":0.017552637624527596,"score_gpt":0.259043655982056,"score_spread":0.24149101835752837,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793870849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925715,0.000044379576,0.000025500705,0.000014268875,0.0000029289993,0.0000026093378,0.00017271934,0.000004887789,0.00047550944],"genre_scores_gemma":[0.99903655,0.00008436358,0.00008845402,0.0000060939633,0.0000033406177,0.0000026479845,0.000593829,0.000001825156,0.0001829668],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993527,0.000003901025,0.0000064492874,0.000013443353,0.000016600197,0.0000243587],"domain_scores_gemma":[0.9999064,0.0000046205173,0.000042893487,0.0000049999267,0.000016293658,0.00002464987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000066000386,0.0002683224,0.00017416579,0.00080766366,0.0002312662,0.00025755787,0.00015128047,0.00021059533,0.0006070663],"category_scores_gemma":[0.00014587092,0.00010149202,0.00010023562,0.0005099859,0.00035488367,0.00023016191,0.0004936337,0.00012901191,0.00013675165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026582056,0.000084611005,0.9436431,0.00010115221,0.000035709618,0.002569199,0.0014539078,0.001090252,0.026912142,0.00023742601,0.0009783615,0.022628296],"study_design_scores_gemma":[0.0000050608096,0.00003485002,0.997652,0.000008236782,0.0000064165756,0.0002075107,0.00055649003,0.00023191144,0.0005658495,0.00001952785,0.00070954754,0.0000027483254],"about_ca_topic_score_codex":0.009855447,"about_ca_topic_score_gemma":0.020491458,"teacher_disagreement_score":0.009855447,"about_ca_system_score_codex":0.0003734763,"about_ca_system_score_gemma":0.00033994546,"threshold_uncertainty_score":0.01959616},"labels":[],"label_agreement":null},{"id":"W2794168182","doi":"10.1007/s10236-018-1139-7","title":"Tsunami detection by high-frequency radar in British Columbia: performance assessment of the time-correlation algorithm for synthetic and real events","year":2018,"lang":"en","type":"article","venue":"Ocean Dynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society","funders":"","keywords":"Radar; Geology; Algorithm; Seismology; SIGNAL (programming language); Subduction; Geodesy; Computer science; Meteorology; Telecommunications; Physics","score_opus":0.0031900852494602763,"score_gpt":0.18687434013783616,"score_spread":0.1836842548883759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794168182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971853,0.00005963983,0.0015039638,0.00007899803,0.00000595135,0.000008833715,0.00034687313,0.00008809155,0.00072224624],"genre_scores_gemma":[0.9963308,0.000053291602,0.002131156,0.000015178258,0.0000035626958,0.0000040429045,0.00081028114,0.000012587804,0.0006391377],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99974173,0.00006583213,0.000024354262,0.00006200732,0.000055338063,0.00005085536],"domain_scores_gemma":[0.9983015,0.0006714664,0.00009646504,0.00013045981,0.0006735157,0.00012650897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007687064,0.0002853892,0.0001775048,0.00052035006,0.0004363658,0.0006912555,0.00061847613,0.00039192106,0.0009880079],"category_scores_gemma":[0.004202525,0.00018024303,0.00013593001,0.0007238052,0.0002860105,0.0003984508,0.0003719346,0.00028534568,0.00027015674],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024143918,0.00044568814,0.522144,0.00017493509,0.0003034093,0.00057470216,0.00045676104,0.2295602,0.027818471,0.0009942371,0.003534718,0.2115784],"study_design_scores_gemma":[0.00017224025,0.00008262223,0.4061836,0.000017295222,0.00008352682,0.00012626676,0.0003184637,0.58680993,0.005198198,0.00015306572,0.0008202833,0.000034395394],"about_ca_topic_score_codex":0.71413255,"about_ca_topic_score_gemma":0.769559,"teacher_disagreement_score":0.28586745,"about_ca_system_score_codex":0.0018774585,"about_ca_system_score_gemma":0.0027123413,"threshold_uncertainty_score":0.575102},"labels":[],"label_agreement":null},{"id":"W2794206392","doi":"10.4095/306559","title":"Investigation of the Potsdam Group sandstone aquifer vulnerability with the DFN-M approach","year":2018,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Aquifer; Group (periodic table); Vulnerability (computing); Geology; Hydrology (agriculture); Geotechnical engineering; Groundwater; Computer science; Chemistry; Computer security","score_opus":0.04748325546064438,"score_gpt":0.23451340790616648,"score_spread":0.1870301524455221,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794206392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921956,0.000048987,0.0015608659,0.000044698045,0.000004723718,0.00005252847,0.00093166943,0.000020097725,0.0051408606],"genre_scores_gemma":[0.99368894,0.000042077194,0.004262712,0.000013330029,0.000002705929,0.0000392231,0.0005030322,0.000004023273,0.0014438609],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998067,0.000023563938,0.000010049355,0.00004741923,0.000074928124,0.00003733016],"domain_scores_gemma":[0.9996792,0.00006173392,0.00007413498,0.000034440705,0.00010991457,0.000040577743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029438906,0.00021072608,0.00014057364,0.0026615444,0.000496026,0.0005804232,0.0004903294,0.00024137406,0.0016067536],"category_scores_gemma":[0.0009781608,0.00013685001,0.00019317928,0.00204905,0.00035154383,0.00038510273,0.0009819176,0.00015844891,0.00016454593],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078850666,0.000060085873,0.94359845,0.000060227285,0.000055383956,0.00073711236,0.0012124184,0.003486822,0.005201065,0.0013998604,0.00090170983,0.043208096],"study_design_scores_gemma":[0.0000041402122,0.00005667509,0.98536587,0.00001570994,0.000016586455,0.00023605075,0.0021302742,0.00832217,0.0008192675,0.0004193949,0.0026048745,0.000008972075],"about_ca_topic_score_codex":0.089526385,"about_ca_topic_score_gemma":0.31477398,"teacher_disagreement_score":0.089526385,"about_ca_system_score_codex":0.0010539332,"about_ca_system_score_gemma":0.00068012904,"threshold_uncertainty_score":0.17801058},"labels":[],"label_agreement":null},{"id":"W2794372004","doi":"10.1016/j.ijrmms.2018.02.003","title":"The b-value evolution of mining-induced seismicity and mainshock occurrences at hard-rock mines","year":2018,"lang":"en","type":"article","venue":"International Journal of Rock Mechanics and Mining Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Glencore (Canada)","funders":"National Institute for Occupational Safety and Health","keywords":"Induced seismicity; Geology; Seismology; Magnitude (astronomy); Mining engineering; Completeness (order theory); Mathematics","score_opus":0.029134390902538665,"score_gpt":0.2616541306939118,"score_spread":0.23251973979137314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794372004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99916255,0.000020972962,0.000105894,0.00001586786,0.0000011870801,0.0000014233433,0.00017680512,0.0000058852306,0.000509452],"genre_scores_gemma":[0.99957937,0.000008998803,0.000039783117,0.0000028596269,0.0000016733176,9.05301e-7,0.00021489186,0.000002342004,0.00014923145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990916,0.000015366688,0.000009787924,0.00002328407,0.000018088607,0.000024265206],"domain_scores_gemma":[0.9989016,0.00038012408,0.00024438323,0.00004854705,0.00019800122,0.00022734706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019836532,0.00010872021,0.00013827399,0.0010720728,0.00020253997,0.00038214546,0.00023904395,0.0003933552,0.0019008468],"category_scores_gemma":[0.0014539555,0.00017157727,0.00017180188,0.0007273181,0.0001646332,0.00034842984,0.0003184452,0.00028396104,0.0005286731],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029295252,0.00007485618,0.9825351,0.000013613068,0.000054704455,0.0001914314,0.00020027813,0.002031064,0.009286526,0.00022491436,0.00020705009,0.004887359],"study_design_scores_gemma":[0.0000024684355,0.000017174125,0.997758,0.0000013488864,0.0000035979224,0.000049641694,0.00007676325,0.0018330795,0.00016201804,0.00003846277,0.000055009743,0.0000026053408],"about_ca_topic_score_codex":0.0050985655,"about_ca_topic_score_gemma":0.005380213,"teacher_disagreement_score":0.0050985655,"about_ca_system_score_codex":0.00022608727,"about_ca_system_score_gemma":0.00014983011,"threshold_uncertainty_score":0.010137737},"labels":[],"label_agreement":null},{"id":"W2794450887","doi":"10.1155/2018/6953165","title":"Effects of Particle Size on Fault Gouge Frictional Characteristics and Associated Acoustic Emission","year":2018,"lang":"en","type":"article","venue":"Advances in Civil Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Fundamental Research Funds for the Central Universities; Priority Academic Program Development of Jiangsu Higher Education Institutions; Government of Jiangsu Province; National Natural Science Foundation of China","keywords":"Slipping; Fault gouge; Slip (aerodynamics); Acoustic emission; Materials science; Shear (geology); Mechanics; Instability; Particle size; Drop (telecommunication); Geotechnical engineering; Fault (geology); Geology; Composite material; Structural engineering; Physics; Engineering; Seismology; Thermodynamics","score_opus":0.004443415250906141,"score_gpt":0.2028062684078255,"score_spread":0.19836285315691937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794450887","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99859375,0.000047444704,0.0010547084,0.000007796075,0.0000050428075,0.000011797077,0.000039989725,0.000013611893,0.0002259244],"genre_scores_gemma":[0.99933606,0.000032567496,0.00048832403,0.0000042766383,0.0000014316107,0.000007640484,0.000029346282,0.000006291163,0.00009417043],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997346,0.000037806603,0.000022287866,0.000073420415,0.0000793674,0.000052533993],"domain_scores_gemma":[0.9986971,0.0008336483,0.00015838076,0.00009474581,0.00014272313,0.00007347682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003621691,0.00025577855,0.00024870248,0.00022993273,0.00020231222,0.00033494242,0.00022181237,0.00027533845,0.0008783634],"category_scores_gemma":[0.0016249223,0.00014191169,0.00016318719,0.0001219468,0.00033758703,0.00029018658,0.00024143023,0.00020495061,0.000081103026],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010231489,0.00016446086,0.009019217,0.000084572544,0.00001740476,0.00016399492,0.00010254831,0.0035196396,0.9806567,0.000120452445,0.000038287868,0.005089491],"study_design_scores_gemma":[0.000061667655,0.0017682188,0.04217471,0.0000065525196,0.00004613508,0.000101474776,0.00013832838,0.015308301,0.9398929,0.000088042834,0.0003895962,0.000024104578],"about_ca_topic_score_codex":0.0010171866,"about_ca_topic_score_gemma":0.0009104043,"teacher_disagreement_score":0.0010171866,"about_ca_system_score_codex":0.00018778937,"about_ca_system_score_gemma":0.00009872741,"threshold_uncertainty_score":0.0029384494},"labels":[],"label_agreement":null},{"id":"W2794878008","doi":"10.1002/2017jb015059","title":"Along‐Trench Structural Variations of the Subducting Juan de Fuca Plate From Multichannel Seismic Reflection Imaging","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Subduction; Seismology; Trench; Convergent boundary; Crust; Oceanic crust; Seafloor spreading; Slip (aerodynamics); Slab; Episodic tremor and slip; Mantle (geology); Receiver function; Slab window; Plate tectonics; Geophysics; Lithosphere; Tectonics","score_opus":0.04747210796864953,"score_gpt":0.3405989400635845,"score_spread":0.29312683209493495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794878008","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99855334,0.000032851844,0.00015503448,0.00000647267,0.0000019973832,0.00000301679,0.00020843494,0.000027741038,0.0010111408],"genre_scores_gemma":[0.9988362,0.000025922798,0.00049552304,0.0000033840654,0.0000033624153,0.00000340182,0.00028184525,0.0000058965534,0.0003444936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992573,0.0000034281088,0.0000027194715,0.000025360147,0.000022600289,0.000020048463],"domain_scores_gemma":[0.99987113,0.000013341227,0.000043945365,0.000013610601,0.00003768149,0.000020209942],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014457824,0.00040709588,0.00015745788,0.0010799792,0.00022386776,0.0003439281,0.00022000227,0.0002632318,0.0010666547],"category_scores_gemma":[0.0002686434,0.00018689194,0.0001745222,0.0005945839,0.00018230594,0.00014490812,0.0002420673,0.00014546547,0.00018785633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000295178,0.000087896326,0.7090218,0.00008832884,0.00015098455,0.0006473823,0.001335354,0.005068145,0.2386216,0.00009776524,0.0005021576,0.044083398],"study_design_scores_gemma":[0.0000025038432,0.000019720641,0.99659413,0.0000038869744,0.000010832806,0.00009009926,0.00014107027,0.0013452877,0.0014638159,0.000007770536,0.00031520726,0.0000057021107],"about_ca_topic_score_codex":0.022481231,"about_ca_topic_score_gemma":0.05496697,"teacher_disagreement_score":0.022481231,"about_ca_system_score_codex":0.00029354435,"about_ca_system_score_gemma":0.00025902336,"threshold_uncertainty_score":0.04470074},"labels":[],"label_agreement":null},{"id":"W2794932435","doi":"10.1144/sp477.23","title":"Assessment of the effect of mass-transport deposits on fault propagation in Penobscot area, offshore Nova Scotia","year":2018,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nova scotia; Submarine pipeline; Fault (geology); Geology; Seismology; Nova (rocket); Oceanography; Engineering; Aeronautics","score_opus":0.018852556013358363,"score_gpt":0.2547920062791558,"score_spread":0.23593945026579746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794932435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99847287,0.00011577869,0.000039959727,0.00001626133,0.0000021957044,0.000010863915,0.00040528024,0.0000031346701,0.0009336009],"genre_scores_gemma":[0.99938107,0.00006744097,0.000056723493,0.00000599166,8.74876e-7,0.0000037863024,0.00015664203,9.760095e-7,0.00032659646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981123,0.000024791916,0.000016984803,0.000040538966,0.000049984617,0.00005644576],"domain_scores_gemma":[0.9986249,0.00018857901,0.00041168355,0.00006208318,0.0004905573,0.00022217452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028451983,0.0002785287,0.00015308258,0.0014105411,0.0004745959,0.00074013637,0.00024555108,0.00013883323,0.0010073272],"category_scores_gemma":[0.0013806866,0.00016523773,0.00014346094,0.0011562868,0.00051853596,0.00014830101,0.0005032739,0.000109158915,0.00011536765],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017254161,0.000011803487,0.9885194,0.000040765255,0.000034908066,0.00071744056,0.0003549277,0.0007866846,0.004909273,0.00004268953,0.00009633739,0.0043131285],"study_design_scores_gemma":[0.0000015634963,0.000007817347,0.9993838,0.0000054297498,0.0000039727242,0.00003159336,0.00018675378,0.00015121388,0.00010750069,0.000002459012,0.00011659911,0.0000011966748],"about_ca_topic_score_codex":0.8151414,"about_ca_topic_score_gemma":0.9195088,"teacher_disagreement_score":0.18485862,"about_ca_system_score_codex":0.0033750501,"about_ca_system_score_gemma":0.0021907382,"threshold_uncertainty_score":0.37189454},"labels":[],"label_agreement":null},{"id":"W2797048599","doi":"","title":"Forward stratigraphic basin modelling as a key to relief evolution at subduction margins: first results on the Meso-Hellenic piggyback basin (Greece)","year":2006,"lang":"en","type":"preprint","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"","keywords":"Geology; Structural basin; Subduction; Anticline; Paleontology; Tectonics; Subsidence; Palaeogeography; Fault (geology); Diachronous; Stratigraphy; Geomorphology; Seismology; Volcanism","score_opus":0.018614181821209982,"score_gpt":0.2001327900005861,"score_spread":0.1815186081793761,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2797048599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96578914,0.00030673397,0.029779406,0.0002277854,0.000031029856,0.00005211238,0.0005790839,0.0006377345,0.002596883],"genre_scores_gemma":[0.98978066,0.00012180476,0.0088383695,0.000015734884,0.00001038086,0.0000135094,0.00020975644,0.00010719269,0.0009025454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999884,0.000043967437,0.000010329736,0.0000312769,0.00001379577,0.00001659172],"domain_scores_gemma":[0.9993338,0.00040384952,0.000048241363,0.00007917527,0.00009514706,0.000039686733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038429795,0.0006623366,0.0008170265,0.00068171177,0.0003316803,0.0010025988,0.0009246314,0.00084567367,0.002625703],"category_scores_gemma":[0.0017735123,0.0004632633,0.0006506438,0.00073226955,0.00043287757,0.00073820795,0.0006693297,0.0005694059,0.00023709936],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014349764,0.00009439631,0.012905523,0.000083365085,0.000094370655,0.00010665517,0.00022474598,0.95182157,0.0040681614,0.0010505653,0.00029920056,0.029107923],"study_design_scores_gemma":[0.000023141518,0.00002034728,0.00307745,0.000006155991,0.000019785308,0.000011295186,0.000038647235,0.9953117,0.0006674626,0.00060993485,0.00020694417,0.0000072626462],"about_ca_topic_score_codex":0.062168643,"about_ca_topic_score_gemma":0.035969473,"teacher_disagreement_score":0.062168643,"about_ca_system_score_codex":0.00076641765,"about_ca_system_score_gemma":0.000943044,"threshold_uncertainty_score":0.123613596},"labels":[],"label_agreement":null},{"id":"W2797910845","doi":"10.4095/306961","title":"The 1929 magnitude 7.2 Grand Banks earthquake: felt reports from the dominions of Canada and Newfoundland and islands of Saint-Pierre and Miquelon, France","year":2018,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"SAINT; Magnitude (astronomy); History; Geography; Genealogy; Demography; Seismology; Geology; Art history; Sociology; Physics; Astronomy","score_opus":0.011632922499574611,"score_gpt":0.2124922406016601,"score_spread":0.2008593181020855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2797910845","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.28175044,0.00063747156,0.00040470052,0.0015768261,0.000111524314,0.0003987835,0.6475811,0.00046490497,0.067074366],"genre_scores_gemma":[0.42059168,0.0022275266,0.002048745,0.00039989833,0.00012500028,0.00042349345,0.4696479,0.000298759,0.104236886],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99886477,0.000035470264,0.00007187227,0.00006571355,0.00073736097,0.00022488282],"domain_scores_gemma":[0.993001,0.00042495193,0.00061824836,0.0001638453,0.005201784,0.0005902015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006238584,0.0004508673,0.00019815113,0.007472825,0.001543464,0.001578791,0.0007859186,0.00025468957,0.012516475],"category_scores_gemma":[0.004168975,0.00019920534,0.00015427626,0.010893574,0.0004139265,0.00050002954,0.0010028869,0.00032414123,0.002370494],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036515668,0.00013402964,0.43876752,0.00083417125,0.00008271656,0.001227701,0.011584969,0.0005575065,0.0024839393,0.0011087562,0.44119796,0.10165545],"study_design_scores_gemma":[0.000014614636,0.000019209312,0.9125478,0.00009748849,0.0000139187305,0.00009568863,0.0070896903,0.000119797,0.00058300846,0.00002670316,0.079365164,0.00002684779],"about_ca_topic_score_codex":0.981987,"about_ca_topic_score_gemma":0.99137056,"teacher_disagreement_score":0.018013,"about_ca_system_score_codex":0.013095696,"about_ca_system_score_gemma":0.01926445,"threshold_uncertainty_score":0.09501642},"labels":[],"label_agreement":null},{"id":"W2799536474","doi":"10.1002/2017gl075839","title":"Seafloor Displacement After the 2011 Tohoku‐oki Earthquake in the Northern Japan Trench Examined by Repeated Bathymetric Surveys","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Japan Agency for Marine-Earth Science and Technology; Bundesministerium für Bildung und Forschung; Ministry of Education, Culture, Sports, Science and Technology; Ministry of Education","keywords":"Trench; Geology; Bathymetry; Seafloor spreading; Seismology; Submarine pipeline; Slip (aerodynamics); Displacement (psychology); Submarine landslide; Vertical displacement; Landslide; Geomorphology; Oceanography","score_opus":0.03984361399257743,"score_gpt":0.2843468162861515,"score_spread":0.24450320229357406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2799536474","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99978656,0.000013168031,0.000010970785,0.000004785428,9.011864e-7,0.0000014465667,0.00003413385,7.894628e-7,0.00014728164],"genre_scores_gemma":[0.99954283,0.000035205027,0.000037113598,0.000008147389,0.0000020155242,0.000003762311,0.00010076868,0.0000010221498,0.00026916736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999051,0.000010421156,0.0000056935355,0.00001924699,0.000019750923,0.00003975883],"domain_scores_gemma":[0.9996675,0.00001813418,0.00012785879,0.000017759825,0.000082635015,0.000086129716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015277984,0.00023109428,0.00025624136,0.00057328155,0.0006237449,0.00040669812,0.0002045038,0.00031167277,0.0006095875],"category_scores_gemma":[0.0003584643,0.0001826461,0.00015877528,0.0006910402,0.00036201102,0.00025264325,0.0005302706,0.00021254335,0.00015782224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006990902,0.000026734146,0.98956513,0.000016871936,0.000027872245,0.0005508026,0.001614738,0.0002607925,0.004859894,0.000011469322,0.000107506545,0.0028882502],"study_design_scores_gemma":[7.738217e-7,0.000012247258,0.99924684,0.0000014027771,0.0000046364835,0.000021713164,0.00053598185,0.000054917833,0.000058720274,0.0000012895435,0.000059896876,0.000001611822],"about_ca_topic_score_codex":0.096893586,"about_ca_topic_score_gemma":0.23355068,"teacher_disagreement_score":0.096893586,"about_ca_system_score_codex":0.000739697,"about_ca_system_score_gemma":0.0005555257,"threshold_uncertainty_score":0.1926592},"labels":[],"label_agreement":null},{"id":"W2800286924","doi":"10.2118/190018-ms","title":"Parametric Probabilistic Models for Fluid Diffusivity Inversion and Forward Microseismic Generation Using Seismicity Rates","year":2018,"lang":"en","type":"article","venue":"SPE Western Regional Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Eidgenössische Technische Hochschule Zürich; Branco Weiss Fellowship – Society in Science; China National Offshore Oil Corporation; University of Calgary","keywords":"Microseism; Induced seismicity; Probabilistic logic; Geology; Statistical model; Bayesian inference; Computer science; Bayesian probability; Seismology; Machine learning; Artificial intelligence","score_opus":0.07711964739292308,"score_gpt":0.2701353459616613,"score_spread":0.19301569856873818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800286924","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03789963,0.00008863262,0.959993,0.00019299219,0.000010908265,0.00002950708,0.00011621886,0.00018843666,0.0014806222],"genre_scores_gemma":[0.95047164,0.00015618882,0.045224573,0.000044350247,0.000024942186,0.00015069661,0.00018264711,0.00006509032,0.0036798995],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992976,0.00024040489,0.000034602577,0.00018742832,0.0001640642,0.00007590626],"domain_scores_gemma":[0.9969795,0.0019315965,0.0005094435,0.0001371465,0.00036501526,0.000077405726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020789662,0.00075567747,0.00075598934,0.0010237674,0.00041142467,0.0011146994,0.001974711,0.0014129484,0.0016623012],"category_scores_gemma":[0.0061898036,0.00079543726,0.0010866543,0.000714493,0.001311669,0.0014801247,0.0011520463,0.0012986555,0.00028041864],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008661703,0.0000072570147,0.00034299382,0.0000073222586,0.0000074001964,0.000015148056,0.000017838138,0.9845077,0.00027440436,0.012068549,0.000060584716,0.0026821669],"study_design_scores_gemma":[8.5092773e-7,0.000002299833,0.00005756595,9.0969314e-7,0.0000013169966,0.0000029612452,0.000001274945,0.9971409,0.000068051435,0.0026785822,0.000042597487,0.0000027481124],"about_ca_topic_score_codex":0.011265973,"about_ca_topic_score_gemma":0.0072016893,"teacher_disagreement_score":0.011265973,"about_ca_system_score_codex":0.001457662,"about_ca_system_score_gemma":0.0009353318,"threshold_uncertainty_score":0.022400796},"labels":[],"label_agreement":null},{"id":"W2800369412","doi":"10.1144/sp477.28","title":"Modelling the 1929 Grand Banks slump and landslide tsunami","year":2018,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Norges Forskningsråd","keywords":"Geology; Slump; Landslide; Seismology; Geotechnical engineering; Archaeology; Geography","score_opus":0.030039630858888614,"score_gpt":0.22715735364520662,"score_spread":0.197117722786318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800369412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98981595,0.00008684268,0.0035781807,0.00022857208,0.0000241983,0.000032188902,0.0007543372,0.000098982324,0.0053807525],"genre_scores_gemma":[0.9962011,0.00006289771,0.0015981819,0.00002153047,0.0000073751003,0.000018379284,0.00033108797,0.000022226975,0.0017372089],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998963,0.0000209786,0.0000058522965,0.000016451568,0.0000155838,0.000044875207],"domain_scores_gemma":[0.9995216,0.00024100632,0.00006608071,0.000021652726,0.000084832165,0.00006480828],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028133366,0.00070043,0.00056790677,0.00046399227,0.0007886344,0.0011198039,0.0012887757,0.0017223541,0.003078696],"category_scores_gemma":[0.0011791943,0.0006922428,0.0006931327,0.0004595713,0.00081395544,0.0005286308,0.00048974017,0.0009740642,0.00024507722],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036174162,0.00003441199,0.0063747,0.000016368038,0.000029301744,0.00013002218,0.000030436984,0.99156135,0.00033782356,0.0005326878,0.00020239501,0.00071428495],"study_design_scores_gemma":[0.000023503324,0.000031112504,0.0028304928,0.0000049618334,0.00001830095,0.000012410388,0.00004744244,0.99645716,0.00018600136,0.00016533854,0.00021623935,0.0000070247065],"about_ca_topic_score_codex":0.38788596,"about_ca_topic_score_gemma":0.34186336,"teacher_disagreement_score":0.6121141,"about_ca_system_score_codex":0.003681663,"about_ca_system_score_gemma":0.001975948,"threshold_uncertainty_score":0.77125645},"labels":[],"label_agreement":null},{"id":"W2800463422","doi":"10.1093/gji/ggy167","title":"Increased likelihood of induced seismicity in highly overpressured shale formations","year":2018,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Overpressure; Geology; Hydraulic fracturing; Pore water pressure; Kerogen; Oil shale; Induced seismicity; Seismology; Sedimentary rock; Fluid pressure; Geomechanics; Petrology; Sedimentary basin; Geotechnical engineering; Structural basin; Source rock; Geochemistry; Geomorphology","score_opus":0.014586705036691112,"score_gpt":0.24092668527208047,"score_spread":0.22633998023538937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800463422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99961287,0.000014651774,0.00009586759,0.000014995555,8.267116e-7,0.0000013216006,0.00005644737,0.000005444145,0.00019760251],"genre_scores_gemma":[0.99986637,0.000005726772,0.000029235674,0.0000030164474,0.0000012838498,4.5895712e-7,0.0000443131,5.223809e-7,0.000049001366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997336,0.00005670596,0.000022645176,0.000067009816,0.00006125403,0.000058779817],"domain_scores_gemma":[0.9972113,0.0006878808,0.0011200632,0.00025105267,0.00025900194,0.0004706574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003164357,0.00009328922,0.00015182006,0.00070400466,0.00022620564,0.0003986896,0.00020921037,0.00021211519,0.0018577689],"category_scores_gemma":[0.0022614412,0.00008467569,0.0001209285,0.0004433752,0.00052594644,0.00017102568,0.00047268474,0.00024474284,0.000111996545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004204166,0.000008335701,0.99642307,0.0000054672905,0.000016354661,0.000100509824,0.00015047702,0.0002573633,0.0016483942,0.00005671553,0.000040650015,0.0012505538],"study_design_scores_gemma":[0.0000012472016,0.00001835907,0.9989459,0.0000011685664,0.0000042907345,0.00011110913,0.00015874479,0.00041797204,0.00021678294,0.000040405997,0.00008230294,0.0000017405912],"about_ca_topic_score_codex":0.015112455,"about_ca_topic_score_gemma":0.022384034,"teacher_disagreement_score":0.015112455,"about_ca_system_score_codex":0.0004413154,"about_ca_system_score_gemma":0.0002773442,"threshold_uncertainty_score":0.030048966},"labels":[],"label_agreement":null},{"id":"W2801116929","doi":"10.5194/se-9-1061-2018","title":"Channel flow, tectonic overpressure, and exhumation of high-pressure rocks in the Greater Himalayas","year":2018,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Fundação para a Ciência e a Tecnologia","keywords":"Geology; Subduction; Overpressure; Continental collision; Tectonics; Transpression; Seismology; Geodynamics; Petrology; Geophysics; Geomorphology; Sinistral and dextral","score_opus":0.014106416661365855,"score_gpt":0.21838495666716304,"score_spread":0.20427854000579718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801116929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986727,0.000043140473,0.00040285807,0.000052454678,0.0000023979742,0.0000029214907,0.000051227158,0.00001838802,0.0007539717],"genre_scores_gemma":[0.9996978,0.000029878363,0.00009934421,0.0000052074633,0.000001689399,0.0000016618294,0.000015652478,0.000002643311,0.00014611694],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993527,0.000018936593,0.0000044874837,0.0000141569735,0.000010016258,0.00001711201],"domain_scores_gemma":[0.9998671,0.00004945991,0.00002275923,0.000012095037,0.000015773414,0.000032905173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018696002,0.00023880182,0.00020996276,0.0005464553,0.0004716961,0.0008469792,0.00030667902,0.0005311531,0.0012112159],"category_scores_gemma":[0.00047166823,0.00022061077,0.00033235893,0.0006166574,0.00089904974,0.00043748933,0.00034605627,0.00023870938,0.0000876209],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013314513,0.000111095615,0.100033686,0.0000540403,0.00006542608,0.0005009184,0.00037268116,0.88153845,0.008881553,0.004404517,0.00020496594,0.003699469],"study_design_scores_gemma":[0.000067433895,0.00009391287,0.099066086,0.000010305024,0.000027765014,0.000079903504,0.00022807001,0.8975112,0.0014330482,0.001159165,0.00029868085,0.000024481844],"about_ca_topic_score_codex":0.0528774,"about_ca_topic_score_gemma":0.022221284,"teacher_disagreement_score":0.0528774,"about_ca_system_score_codex":0.0017078398,"about_ca_system_score_gemma":0.0008257558,"threshold_uncertainty_score":0.105139256},"labels":[],"label_agreement":null},{"id":"W2801157003","doi":"","title":"U-PB GEOCHRONOLOGY AND HF ISOTOPE SIGNATURES OF DETRITAL ZIRCON GRAINS FROM THE NEOPROTEROZOIC AMUNDSEN BASIN OF NORTHWESTERN CANADA","year":2012,"lang":"en","type":"article","venue":"2012 GSA Annual Meeting in Charlotte","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Zircon; Geochronology; Geology; Geochemistry; Structural basin; Isotope; Paleontology","score_opus":0.010162354042659433,"score_gpt":0.20060523949411854,"score_spread":0.1904428854514591,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801157003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963148,0.00030073847,0.00009829808,0.000034199948,0.000002991101,0.0000041002518,0.0013768346,0.000012180767,0.0018559245],"genre_scores_gemma":[0.99610764,0.00019772552,0.00021140714,0.000018917794,0.0000013405445,0.0000032736039,0.00094091793,0.00001302662,0.002505714],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989295,0.0000021547482,0.0000059930603,0.000028905206,0.000029691562,0.000040308187],"domain_scores_gemma":[0.99982244,0.000008024435,0.000015151076,0.000006890015,0.00012220276,0.000025425987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009739261,0.00022577748,0.00023711633,0.0016656005,0.0019247524,0.0008596854,0.00056125934,0.00023859812,0.0017089279],"category_scores_gemma":[0.00023847712,0.00024322706,0.00014290678,0.0021113337,0.00047306318,0.00020666451,0.0003901755,0.00019080316,0.0002962541],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00076734665,0.00005366098,0.8272445,0.00014778296,0.00013330353,0.0007141831,0.005671079,0.0014407777,0.11072068,0.00076840265,0.0017536687,0.05058463],"study_design_scores_gemma":[0.000004840758,0.000006699635,0.9955244,0.000006818749,0.000013890507,0.000063635875,0.0005306157,0.00023233147,0.0017469721,0.000030577412,0.001834217,0.000005069202],"about_ca_topic_score_codex":0.9756798,"about_ca_topic_score_gemma":0.9902873,"teacher_disagreement_score":0.024320185,"about_ca_system_score_codex":0.0074371006,"about_ca_system_score_gemma":0.004585755,"threshold_uncertainty_score":0.053960145},"labels":[],"label_agreement":null},{"id":"W2801838017","doi":"10.5539/jgg.v10n2p43","title":"Relationship between Seismic Activity and Variations in the Earth’s Rotation Angular Velocity","year":2018,"lang":"en","type":"article","venue":"Journal of Geography and Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Russian Academy of Sciences; Russian Foundation for Basic Research","keywords":"Angular velocity; Rotation (mathematics); Earth's rotation; Acceleration; Seismic velocity; Geodesy; Geology; Earth (classical element); Angular acceleration; Seismology; Physics; Geophysics; Classical mechanics; Geometry; Mathematics","score_opus":0.02010342275652638,"score_gpt":0.23889256800428046,"score_spread":0.21878914524775409,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801838017","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973653,0.00016699043,0.00032695138,0.000031330495,0.000006354016,0.0000043269843,0.00036057137,0.000011581013,0.0017266097],"genre_scores_gemma":[0.9993309,0.00007589988,0.0000758907,0.0000027940398,0.000006927824,0.0000021921826,0.00028752536,0.0000030436427,0.00021476652],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997632,0.000043573316,0.000029661926,0.000059753995,0.000046143407,0.000057739908],"domain_scores_gemma":[0.99754995,0.00096724526,0.00079301174,0.00012918182,0.00031748868,0.0002430793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003018441,0.0001685772,0.00018096856,0.0010430367,0.000120668046,0.0005103375,0.00014968059,0.00022643308,0.002167923],"category_scores_gemma":[0.0032999278,0.000110843466,0.00013066149,0.0011999953,0.000282857,0.00029119288,0.00028387038,0.00038492878,0.0004455203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009178553,0.00002069499,0.9921176,0.000010742718,0.000049782473,0.000085916465,0.00013000544,0.00082401227,0.0018712947,0.00016614316,0.00011779809,0.004514263],"study_design_scores_gemma":[9.884673e-7,0.000014314663,0.9989574,0.0000018115793,0.0000058762384,0.00005299,0.0000911127,0.0005020515,0.0001241907,0.00003630852,0.00021060675,0.0000022895226],"about_ca_topic_score_codex":0.003858185,"about_ca_topic_score_gemma":0.0035250594,"teacher_disagreement_score":0.003858185,"about_ca_system_score_codex":0.000205446,"about_ca_system_score_gemma":0.00014243592,"threshold_uncertainty_score":0.007671416},"labels":[],"label_agreement":null},{"id":"W2802256927","doi":"10.1144/sp481.4","title":"Influence of inherited Indian basement faults on the evolution of the Himalayan Orogen","year":2018,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Basement; Paleontology; Seismology; Geochemistry; Geography; Archaeology","score_opus":0.018419272945219344,"score_gpt":0.22193961676231969,"score_spread":0.20352034381710035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802256927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983455,0.0000606336,0.00006368033,0.000025317535,0.0000016983283,0.0000015024331,0.00012450393,0.000008243295,0.0013690316],"genre_scores_gemma":[0.9997217,0.000046141537,0.00003217385,0.0000042197676,0.0000014979413,4.7398333e-7,0.00006937964,0.0000029593323,0.000121418685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998393,0.000040183786,0.000009256753,0.000039901843,0.000029339006,0.000042016327],"domain_scores_gemma":[0.99974793,0.000067117835,0.000055720117,0.000030046913,0.00004773322,0.000051381885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019009461,0.00020657999,0.00020611015,0.0008861308,0.00045537492,0.0014098154,0.00023498006,0.00017495807,0.0019098623],"category_scores_gemma":[0.00058486057,0.00012270594,0.00020952399,0.0011784952,0.0003999069,0.00018809903,0.00041703242,0.00017753798,0.00020457651],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003147208,0.000052183063,0.9361171,0.00005342651,0.00025168408,0.0011493837,0.00078596204,0.023534646,0.021192152,0.0012397241,0.0002684565,0.015040573],"study_design_scores_gemma":[0.000007342706,0.000023761615,0.99172884,0.000006916066,0.00005051809,0.0001004222,0.00049749424,0.0062391963,0.0007332021,0.00010670301,0.00049573526,0.000009871827],"about_ca_topic_score_codex":0.037155025,"about_ca_topic_score_gemma":0.032508444,"teacher_disagreement_score":0.037155025,"about_ca_system_score_codex":0.0008532762,"about_ca_system_score_gemma":0.00043048096,"threshold_uncertainty_score":0.07387751},"labels":[],"label_agreement":null},{"id":"W2802620003","doi":"10.1029/2017gc007368","title":"The Alpine Fault Hangingwall Viewed From Within: Structural Analysis of Ultrasonic Image Logs in the DFDP‐2B Borehole, New Zealand","year":2018,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"H2020 European Research Council; Marsden Fund; Natural Environment Research Council; Georgian National Science Foundation; Victoria University; Centre National de la Recherche Scientifique; Victoria University of Wellington; Université de Montpellier; Sight Research UK; University of Otago","keywords":"Geology; Mylonite; Outcrop; Borehole; Fault (geology); Detachment fault; Petrology; Slip (aerodynamics); Foliation (geology); Seismology; Geomorphology; Metamorphic rock; Shear zone; Tectonics; Geotechnical engineering; Extensional definition","score_opus":0.008712168083677661,"score_gpt":0.2176443544374556,"score_spread":0.20893218635377794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802620003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980502,0.00003455849,0.00022494578,0.00001322255,0.0000015379476,0.000013910512,0.00068219495,0.000025040452,0.00095436577],"genre_scores_gemma":[0.9981104,0.000057277797,0.0004943163,0.0000065089052,0.0000021421517,0.00001626844,0.00071839197,0.0000072339,0.0005874807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998771,0.0000034871482,0.000007049757,0.0000316174,0.000050417555,0.000030315006],"domain_scores_gemma":[0.99981123,0.00001861966,0.000059214475,0.000011312452,0.00006634648,0.000033255674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011017778,0.00027770113,0.00021123099,0.0013249575,0.00036179935,0.000558543,0.00041679616,0.0002794096,0.0012576394],"category_scores_gemma":[0.00046490695,0.00028254272,0.00015560265,0.0011424555,0.00047177504,0.0003067486,0.00048263458,0.0002126944,0.00026343716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043440438,0.00011124999,0.7008974,0.00017279049,0.000046893663,0.0020785765,0.004711363,0.0019525468,0.23018773,0.00015571693,0.0007810254,0.05847031],"study_design_scores_gemma":[0.0000059457634,0.000021141508,0.99765635,0.000004843345,0.0000055842497,0.000089193636,0.0004214373,0.00055968104,0.00085473,0.000006374555,0.00036935732,0.0000052217133],"about_ca_topic_score_codex":0.30578402,"about_ca_topic_score_gemma":0.44157377,"teacher_disagreement_score":0.30578402,"about_ca_system_score_codex":0.00084427826,"about_ca_system_score_gemma":0.0004966962,"threshold_uncertainty_score":0.6080083},"labels":[],"label_agreement":null},{"id":"W2802696279","doi":"10.1139/cjes-2017-0231","title":"Further studies on the 1988 <i>M</i><sub>W</sub> 5.9 Saguenay, Quebec, earthquake sequence","year":2018,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Carleton University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Geology; Seismology; Graben; Seismometer; Sequence (biology); Focal mechanism; Foreshock; Hypocenter; Seismic moment; Induced seismicity; Fault (geology); Tectonics","score_opus":0.05448337184608769,"score_gpt":0.24795690265393325,"score_spread":0.19347353080784557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802696279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98330784,0.00065550563,0.0031487474,0.00020235126,0.0000132201885,0.0001561718,0.0028897175,0.000050497056,0.009575984],"genre_scores_gemma":[0.98341125,0.0007696489,0.0051677963,0.000094387826,0.00001416253,0.00004660734,0.0044148746,0.000017877233,0.006063487],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991643,0.000012731046,0.0000031320283,0.0000148478075,0.000024292913,0.00002857092],"domain_scores_gemma":[0.99953866,0.00005393227,0.00008105509,0.00002362656,0.00024928918,0.000053504195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021075863,0.00021914285,0.00015416906,0.0005657422,0.00061763875,0.00030517633,0.00023372295,0.00010360051,0.00207574],"category_scores_gemma":[0.000641838,0.00005515288,0.00017956873,0.0011907134,0.0001527159,0.00020918963,0.00011231921,0.00018098253,0.0002519087],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026643422,0.00022804413,0.6990304,0.00040306212,0.00012797082,0.0009538756,0.0022324235,0.010498256,0.06872509,0.0021628446,0.005824472,0.20954712],"study_design_scores_gemma":[0.0000054674283,0.000051212483,0.98867863,0.000016397898,0.000014542482,0.00005017465,0.0004715695,0.0023034501,0.0008538272,0.00004811771,0.0075002275,0.0000064447],"about_ca_topic_score_codex":0.90957165,"about_ca_topic_score_gemma":0.9694937,"teacher_disagreement_score":0.09042835,"about_ca_system_score_codex":0.0038838417,"about_ca_system_score_gemma":0.0039248494,"threshold_uncertainty_score":0.18192178},"labels":[],"label_agreement":null},{"id":"W2803190997","doi":"10.1029/2017gc007417","title":"Seismicity, Metamorphism, and Fluid Evolution Across the Northern Cascadia Fore Arc","year":2018,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Crust; Seismology; Subduction; Oceanic crust; Continental crust; Slab; Induced seismicity; Petrology; Mantle (geology); Tectonics; Geochemistry; Geophysics","score_opus":0.010182068923842708,"score_gpt":0.20886389236692626,"score_spread":0.19868182344308355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803190997","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99940145,0.00003942572,0.000022266824,0.000020097395,5.9264363e-7,0.0000011847872,0.00014764602,0.0000086927375,0.00035855817],"genre_scores_gemma":[0.99959177,0.00003230932,0.000034156048,0.0000029654113,8.598358e-7,0.0000013874633,0.00017679286,0.0000021471874,0.00015763576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987435,0.000011713331,0.00000926227,0.000049758328,0.000027226131,0.000027737819],"domain_scores_gemma":[0.9996464,0.000036222402,0.000092226466,0.00002735243,0.00009266949,0.00010504614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018646849,0.00031643207,0.00021244083,0.0019235526,0.0006471355,0.0005106683,0.00031778042,0.00027896214,0.0012999944],"category_scores_gemma":[0.00066769874,0.00023213883,0.00024109091,0.0012346896,0.00040480978,0.0001554763,0.00048112776,0.00017516206,0.00018481856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007493249,0.000014880255,0.98680824,0.000017062428,0.00007024088,0.00017205265,0.0004971553,0.0006975942,0.0078107514,0.00003784429,0.00007914855,0.0037201492],"study_design_scores_gemma":[7.7306254e-7,0.0000041478283,0.9996136,0.000001301539,0.00000414512,0.000012463469,0.000102177386,0.00014446498,0.000050564784,0.0000051599545,0.000060053582,0.0000012186537],"about_ca_topic_score_codex":0.23618683,"about_ca_topic_score_gemma":0.33561102,"teacher_disagreement_score":0.23618683,"about_ca_system_score_codex":0.0013268585,"about_ca_system_score_gemma":0.0006422187,"threshold_uncertainty_score":0.46962416},"labels":[],"label_agreement":null},{"id":"W2803452496","doi":"10.1016/s0967-0653(98)82111-x","title":"10.1016/s0967-0653(98)82111-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Reef; Geology; Oceanography; Tsunami wave; Atoll; Great barrier reef; Tropical cyclone; Coral reef; Fringing reef; Paleontology; Seismology","score_opus":0.008745001958806111,"score_gpt":0.16649933505249478,"score_spread":0.15775433309368866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803452496","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0006956134,0.00040938167,0.000573552,0.0004289878,0.00033472493,0.000103964056,0.0010109341,0.0007691625,0.9956737],"genre_scores_gemma":[0.0006802416,0.00015260662,0.00027563135,0.00014353097,0.000064682994,0.00004217646,0.00036852434,0.00014077027,0.9981318],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990706,0.000075904434,0.00009743228,0.00030467907,0.0002736953,0.00017769415],"domain_scores_gemma":[0.9977163,0.0005173265,0.0001515494,0.00030156155,0.0006135398,0.0006997215],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011584663,0.0021560406,0.0014979473,0.0026519622,0.0015293398,0.004080434,0.0024328318,0.0042699412,0.9872913],"category_scores_gemma":[0.0014886594,0.0008314228,0.0011252535,0.002034634,0.0014729854,0.0038742463,0.0031728954,0.0019299451,0.9883033],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028434698,0.0003038941,0.0012935641,0.00047634737,0.000030169113,0.00032738113,0.00011409552,0.0003090905,0.0019005748,0.0043803947,0.25473005,0.7358501],"study_design_scores_gemma":[0.000043011692,0.00012395869,0.0014162239,0.00039632522,0.000009596968,0.00030516222,0.0001102502,0.00021482394,0.00024494107,0.0005900525,0.9965275,0.00001807484],"about_ca_topic_score_codex":0.0028731416,"about_ca_topic_score_gemma":0.002851009,"teacher_disagreement_score":0.012708724,"about_ca_system_score_codex":0.001004825,"about_ca_system_score_gemma":0.0010088816,"threshold_uncertainty_score":0.018127441},"labels":[],"label_agreement":null},{"id":"W2803932968","doi":"10.1515/jag-2018-0010","title":"Improving TRANS4D’s model for vertical crustal velocities in Western CONUS","year":2018,"lang":"en","type":"article","venue":"Journal of Applied Geodesy","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"Geology; Geodetic datum; Longitude; Caldera; Geodesy; Seismology; Subsidence; Volcano; Fault (geology); Post-glacial rebound; Geomorphology; Glacial period; Latitude; Structural basin","score_opus":0.02339392512037288,"score_gpt":0.23335694446567173,"score_spread":0.20996301934529885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803932968","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.79928917,0.0003535298,0.1770139,0.00064685725,0.00013817206,0.00008970054,0.0025596952,0.0019915865,0.017917475],"genre_scores_gemma":[0.968072,0.00010151964,0.026482489,0.000047405196,0.000012414976,0.00004996169,0.0010255022,0.00019223381,0.004016518],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986124,0.00003131236,0.000011875721,0.000041445124,0.000031346506,0.000022736338],"domain_scores_gemma":[0.9996997,0.00007445669,0.000035578072,0.00002995254,0.00012685588,0.000033419765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005308899,0.0005447455,0.0003864169,0.00060131535,0.00081220176,0.0013018586,0.0010100193,0.00050887774,0.0021228287],"category_scores_gemma":[0.001137412,0.00042706437,0.0004719149,0.0006088345,0.0003442283,0.0005597336,0.0006968327,0.00075350393,0.00032145125],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001985566,0.000017780858,0.00941882,0.000008372101,0.000012807486,0.00005696959,0.000026334272,0.979764,0.00040611782,0.0010033355,0.00076604297,0.008499583],"study_design_scores_gemma":[0.000002864345,0.0000021809792,0.00057273445,0.0000018757803,0.000001461464,0.0000040221303,0.000006864919,0.9987663,0.00008641581,0.00009594758,0.00045650528,0.000002874122],"about_ca_topic_score_codex":0.3494438,"about_ca_topic_score_gemma":0.2645435,"teacher_disagreement_score":0.3494438,"about_ca_system_score_codex":0.0022888691,"about_ca_system_score_gemma":0.0024444703,"threshold_uncertainty_score":0.69481957},"labels":[],"label_agreement":null},{"id":"W2804276086","doi":"10.1029/2018gl077879","title":"Numerical Modeling of Dynamically Triggered Shallow Slow Slip Events in New Zealand by the 2016 <i>M</i><sub><i>w</i></sub> 7.8 Kaikoura Earthquake","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Royal Society Te Apārangi; National Science Foundation","keywords":"Subduction; Perturbation (astronomy); Slip (aerodynamics); Amplitude; Geology; Dynamic stress; Seismology; Geotechnical engineering; Physics; Dynamic loading; Tectonics; Structural engineering; Engineering","score_opus":0.025754102777399132,"score_gpt":0.2636020691499413,"score_spread":0.23784796637254213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804276086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99496955,0.000054703356,0.0010695464,0.00016713432,0.000017360064,0.000026825654,0.0002489202,0.00002810211,0.0034179755],"genre_scores_gemma":[0.998659,0.000043916916,0.00060691324,0.000016306047,0.0000035367289,0.000015853453,0.00013409184,0.00000859642,0.0005117789],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999107,0.000016231967,0.000006976577,0.000019967127,0.000014242222,0.000031861735],"domain_scores_gemma":[0.99958915,0.00014163907,0.00008983942,0.000021598791,0.00008340838,0.00007433161],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002699783,0.0006100746,0.0004718202,0.00036319724,0.0005185419,0.0009912552,0.001241665,0.0012943797,0.0023398064],"category_scores_gemma":[0.0014282056,0.0004931072,0.00059928105,0.00033443444,0.0010914251,0.00062548765,0.00068796624,0.0006874828,0.0001567278],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015563439,0.00013001633,0.021046983,0.00002529381,0.000048195863,0.00027459432,0.00007128364,0.9743367,0.0017720953,0.000540255,0.00025661266,0.0013424191],"study_design_scores_gemma":[0.000074143034,0.00005465479,0.007362136,0.0000058796486,0.00002123401,0.000015103981,0.00009397296,0.9918731,0.00018073402,0.00014253876,0.0001644408,0.000012080938],"about_ca_topic_score_codex":0.25651395,"about_ca_topic_score_gemma":0.13072814,"teacher_disagreement_score":0.25651395,"about_ca_system_score_codex":0.001789699,"about_ca_system_score_gemma":0.0012455472,"threshold_uncertainty_score":0.5100417},"labels":[],"label_agreement":null},{"id":"W2804459945","doi":"10.1016/j.tecto.2018.05.013","title":"Low-angle faulting in strike-slip dominated settings: Seismic evidence from the Maritimes Basin, Canada","year":2018,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Structural basin; Terrane; Paleozoic; Seismology; Detachment fault; Pull apart basin; Echelon formation; Transtension; Sedimentary rock; Tectonics; Sedimentary basin; Paleontology; Sinistral and dextral","score_opus":0.012090325995404723,"score_gpt":0.20795755836409097,"score_spread":0.19586723236868625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804459945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957385,0.00018743346,0.000041514802,0.00009861444,0.0000020500179,0.000012113165,0.0006853566,0.0000034358784,0.0032309634],"genre_scores_gemma":[0.9983229,0.0002777327,0.00010743625,0.000023102919,0.0000018232436,0.000004111977,0.0003721991,0.0000037422733,0.00088698126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995869,0.000023789953,0.000021869582,0.00005726201,0.00014009721,0.0001699944],"domain_scores_gemma":[0.9984285,0.0001099771,0.00024703136,0.000047866204,0.00087039085,0.00029609608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024475288,0.00029250066,0.0003492824,0.002784622,0.004477372,0.0017414553,0.0010266125,0.00036555185,0.0020981012],"category_scores_gemma":[0.0017668222,0.00031672153,0.00014316673,0.0064894897,0.0017094755,0.00043376914,0.0011128766,0.00036578384,0.00021949605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015039527,0.000064751715,0.96929854,0.00007370096,0.0000527472,0.00054547767,0.009092131,0.00037736993,0.0032806285,0.00064413797,0.0009008145,0.01551933],"study_design_scores_gemma":[0.000005102067,0.000008166986,0.99389774,0.000022271295,0.00001553281,0.00007378697,0.004740915,0.000115470735,0.00011368281,0.000038140213,0.0009623847,0.000006718774],"about_ca_topic_score_codex":0.9950918,"about_ca_topic_score_gemma":0.9990563,"teacher_disagreement_score":0.015382622,"about_ca_system_score_codex":0.015382622,"about_ca_system_score_gemma":0.020248173,"threshold_uncertainty_score":0.11160928},"labels":[],"label_agreement":null},{"id":"W2804925393","doi":"10.1190/geo2017-0273.1","title":"A regularized approach for estimation of a composite focal mechanism from a set of microearthquakes","year":2018,"lang":"en","type":"article","venue":"Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Focal mechanism; Azimuth; Amplitude; Microseism; Geology; Seismology; Hydraulic fracturing; Logarithm; Induced seismicity; Algorithm; Mathematics; Geodesy; Mathematical analysis; Geometry; Physics; Optics","score_opus":0.018692635154709814,"score_gpt":0.22332697961089762,"score_spread":0.2046343444561878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804925393","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.051179837,0.000043148066,0.94811726,0.000055851542,0.00000926044,0.00002704064,0.000060009683,0.00023226644,0.00027530605],"genre_scores_gemma":[0.51526076,0.00005806728,0.48288235,0.00006405866,0.00003795744,0.00015392042,0.0004079709,0.000112674286,0.0010222648],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99968135,0.00009974956,0.000018678844,0.000071627226,0.00008911314,0.000039422957],"domain_scores_gemma":[0.9992436,0.0003542803,0.000119857876,0.000072725554,0.00017594476,0.000033605564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010197369,0.00056895864,0.0006157027,0.00095985935,0.0002711996,0.00061206555,0.0011504928,0.00087207125,0.0008626731],"category_scores_gemma":[0.0025862395,0.0004938438,0.0010929159,0.0004278047,0.000552554,0.000511256,0.0007476072,0.00062338857,0.00019662948],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000079604746,0.000039051574,0.0016561595,0.000043052907,0.000091201255,0.00008966888,0.000052277013,0.9503939,0.01166483,0.0026575716,0.00034555173,0.032887153],"study_design_scores_gemma":[0.0000028458796,0.0000053155964,0.0001828903,0.0000014225159,0.0000020470284,0.000005309962,0.0000028522377,0.99902177,0.00038446079,0.00033215148,0.000055649176,0.0000033848619],"about_ca_topic_score_codex":0.0050951513,"about_ca_topic_score_gemma":0.004007708,"teacher_disagreement_score":0.0050951513,"about_ca_system_score_codex":0.0004272146,"about_ca_system_score_gemma":0.0009286693,"threshold_uncertainty_score":0.0101310015},"labels":[],"label_agreement":null},{"id":"W2805272166","doi":"10.4095/293320","title":"Ground deformation produced by 2013 M6.1 Minab earthquake in Iran mapped with RADARSAT-2 DInSAR","year":2013,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Deformation (meteorology); Geodesy; Oceanography","score_opus":0.028009235436159834,"score_gpt":0.22390808035630372,"score_spread":0.1958988449201439,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805272166","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99077564,0.00013325502,0.00018605922,0.000115900126,0.00003544442,0.000024299618,0.006727196,0.00005109188,0.0019510876],"genre_scores_gemma":[0.98452467,0.00032435797,0.00055657525,0.000039880637,0.00003689749,0.000019490804,0.013282978,0.000008694229,0.001206559],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985826,0.000008974794,0.000011318714,0.000025415258,0.000052557432,0.00004349272],"domain_scores_gemma":[0.9998005,0.0000100168945,0.000055037362,0.000016557047,0.00008824637,0.000029688279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023079151,0.000573474,0.00034542818,0.0010305273,0.0002883141,0.0002547559,0.00031250555,0.0003785029,0.0008114321],"category_scores_gemma":[0.00030681968,0.00018177099,0.00025592223,0.0016750346,0.00016768009,0.00024865125,0.00030985894,0.00028437775,0.0003786758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014363425,0.0004956053,0.87482715,0.00035743878,0.00024244061,0.0023584168,0.0009420456,0.015330538,0.018239208,0.00055321725,0.02785641,0.057361234],"study_design_scores_gemma":[0.00003001679,0.00004100067,0.99558276,0.000010712966,0.000028831428,0.00014306915,0.00030908504,0.0013200305,0.000897014,0.000028621987,0.0016006886,0.000008171016],"about_ca_topic_score_codex":0.058766432,"about_ca_topic_score_gemma":0.077153474,"teacher_disagreement_score":0.058766432,"about_ca_system_score_codex":0.0006603087,"about_ca_system_score_gemma":0.0010188435,"threshold_uncertainty_score":0.11684871},"labels":[],"label_agreement":null},{"id":"W2805640597","doi":"10.1029/2018gl078014","title":"The 1 May 2017 British Columbia‐Alaska Earthquake Doublet and Implication for Complexity Near Southern End of Denali Fault System","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China; Northwestern University","keywords":"Seismology; Geology; Aftershock; Focal mechanism; Fault (geology); Transpression; Geodesy; Collision; Induced seismicity; Sinistral and dextral","score_opus":0.05564822715405307,"score_gpt":0.29790047834493527,"score_spread":0.2422522511908822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805640597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99581784,0.0000591668,0.000053698255,0.00026511762,0.000003664507,0.0000048886686,0.00013037065,0.000007413833,0.003657788],"genre_scores_gemma":[0.99947613,0.000032092656,0.000034761048,0.000011945351,0.0000013754726,7.72601e-7,0.0000702013,0.0000010404725,0.00037156255],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998826,0.000013446352,0.000006602793,0.0000320353,0.000023933137,0.000041448064],"domain_scores_gemma":[0.9995732,0.000041835872,0.00011194643,0.000020990805,0.000113736445,0.00013841242],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001035221,0.00014550709,0.00019623688,0.0010490393,0.0016633581,0.0018065837,0.00030496257,0.0003937527,0.003680178],"category_scores_gemma":[0.0009673536,0.00013451939,0.00009561849,0.0010006211,0.0008947853,0.00050225103,0.00081959035,0.00034197542,0.00016622334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012528274,0.00004653121,0.9739889,0.00003743947,0.000046201298,0.0012957247,0.0016143896,0.0031598913,0.0049443278,0.0015692412,0.0012739609,0.01189815],"study_design_scores_gemma":[0.0000031806487,0.000007371465,0.9953009,0.000012380003,0.000008820755,0.00007155979,0.0019918813,0.0013993641,0.0001239772,0.00030103556,0.0007714507,0.000008124224],"about_ca_topic_score_codex":0.48231712,"about_ca_topic_score_gemma":0.67544407,"teacher_disagreement_score":0.5176829,"about_ca_system_score_codex":0.003147611,"about_ca_system_score_gemma":0.0016801873,"threshold_uncertainty_score":0.9590194},"labels":[],"label_agreement":null},{"id":"W2805829540","doi":"10.1038/s41598-018-25649-5","title":"Lateral Variation of Crustal Lg Attenuation in Eastern North America","year":2018,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Geology; Crust; Tectonics; Seismology; Attenuation; Seismogram; Volcano; Broadband; Amplitude; Geophysics","score_opus":0.017243240664324425,"score_gpt":0.22390897169545432,"score_spread":0.2066657310311299,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805829540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991709,0.000040616294,0.00012930008,0.000011748505,4.1712488e-7,0.0000013363815,0.00028085872,0.000017915032,0.00034690448],"genre_scores_gemma":[0.9992743,0.000035010777,0.0001855275,0.000004755287,8.224689e-7,0.0000017811759,0.0003844302,0.000002651503,0.0001106353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999416,0.0000062712465,0.0000034607096,0.000019689074,0.00001200869,0.0000169711],"domain_scores_gemma":[0.9997961,0.000029817478,0.000049952694,0.000018247512,0.00008004479,0.000025868054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011265227,0.00016540513,0.00010655713,0.0008570187,0.00018964615,0.00034229556,0.00012886795,0.00011564312,0.00080596074],"category_scores_gemma":[0.0003701395,0.00012875703,0.00009940636,0.0010059788,0.00021956071,0.0001912082,0.00028081806,0.00007519247,0.00009989059],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000085968146,0.000019465084,0.9555822,0.000025115116,0.00009373335,0.00022805211,0.0005194401,0.0031125506,0.01969509,0.00006785921,0.00038032836,0.020190215],"study_design_scores_gemma":[0.0000015010727,0.000003463893,0.9981515,0.0000021889564,0.000006371943,0.000021894692,0.00010601358,0.0013358433,0.00020033027,0.00001091238,0.00015813808,0.0000018152764],"about_ca_topic_score_codex":0.14213346,"about_ca_topic_score_gemma":0.22449222,"teacher_disagreement_score":0.8578665,"about_ca_system_score_codex":0.00040979087,"about_ca_system_score_gemma":0.00032936866,"threshold_uncertainty_score":0.28261232},"labels":[],"label_agreement":null},{"id":"W2806100292","doi":"10.1038/s41598-018-23303-8","title":"Groundwater oxygen isotope anomaly before the M6.6 Tottori earthquake in Southwest Japan","year":2018,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Japan Society for the Promotion of Science; Korea Polar Research Institute","keywords":"Groundwater; Epicenter; Geology; Aquifer; Isotopes of oxygen; δ18O; Seismology; Anomaly (physics); Geochemistry; Stable isotope ratio; Geotechnical engineering","score_opus":0.014586858863504694,"score_gpt":0.21523439216286716,"score_spread":0.20064753329936247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806100292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999619,0.000044239692,0.000029500865,0.000018894782,0.000004477678,0.0000012534155,0.0000844519,0.000002117812,0.00019607063],"genre_scores_gemma":[0.99951804,0.00005127927,0.00005953028,0.000009688337,0.0000063282355,0.0000017057557,0.00014328961,9.1614334e-7,0.0002092251],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994886,0.0000034911122,0.000004524609,0.000016051215,0.000010954855,0.000016080327],"domain_scores_gemma":[0.99984515,0.000007623598,0.000046539786,0.00000626996,0.000055200147,0.00003925589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001077708,0.00018718334,0.00027225688,0.0005038643,0.00044832777,0.00035123245,0.00015200171,0.00037190696,0.0004708291],"category_scores_gemma":[0.00019481964,0.0001320095,0.000115941126,0.00047190816,0.00029044482,0.00027012068,0.00036591585,0.00021017787,0.000097417214],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041889184,0.00008293097,0.9242978,0.00007457118,0.00004198971,0.0015574811,0.00225708,0.00033227037,0.06137964,0.00007680203,0.00029669932,0.009183834],"study_design_scores_gemma":[0.0000024022293,0.000055974844,0.9975999,0.000004794496,0.0000112868065,0.000078606194,0.0007074122,0.000106230094,0.0010938324,0.0000109374205,0.00032428504,0.000004327573],"about_ca_topic_score_codex":0.01882071,"about_ca_topic_score_gemma":0.040876504,"teacher_disagreement_score":0.01882071,"about_ca_system_score_codex":0.00040062825,"about_ca_system_score_gemma":0.00024709478,"threshold_uncertainty_score":0.0374223},"labels":[],"label_agreement":null},{"id":"W2806463632","doi":"10.1029/2018gl078577","title":"Geodetic Constraints of the 2017 M<sub>w</sub>7.3 Sarpol Zahab, Iran Earthquake, and Its Implications on the Structure and Mechanics of the Northwest Zagros Thrust‐Fold Belt","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Japan Aerospace Exploration Agency; Canadian Space Agency","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Slip (aerodynamics); Seismic gap; Geodetic datum; Synthetic aperture radar; Thrust fault; Interplate earthquake; Aftershock; Geodesy; Fold (higher-order function); Fault (geology); Foreshock; Remote sensing","score_opus":0.041707396895432895,"score_gpt":0.26761583204774286,"score_spread":0.22590843515230996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806463632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99930525,0.0000210491,0.00004628491,0.000028317367,0.000002209648,0.0000013107448,0.000104381266,0.000004055136,0.0004871641],"genre_scores_gemma":[0.9996817,0.000022989208,0.000047437814,0.0000049675423,0.0000041965554,0.0000010839658,0.00018779778,0.0000010255025,0.00004886833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992895,0.0000075616726,0.000004306063,0.000012382724,0.000016907721,0.000029857896],"domain_scores_gemma":[0.99977416,0.000019995057,0.00011485466,0.000016092028,0.00005085225,0.000023964158],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015620964,0.00014845295,0.00015429583,0.0006477152,0.00027503123,0.00031949038,0.00016937926,0.00019515837,0.00059599045],"category_scores_gemma":[0.00039265628,0.000100305326,0.00012768914,0.00048882933,0.00025349355,0.00020699305,0.0002447846,0.00015201607,0.00019547348],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001277998,0.000060922703,0.97362024,0.000020963462,0.000022862403,0.0003043005,0.0003749175,0.0014127132,0.008590086,0.0002856377,0.0006651034,0.014514591],"study_design_scores_gemma":[0.000003648186,0.000016091455,0.99861896,0.0000032375958,0.0000054770303,0.000031914853,0.00024263625,0.00062101224,0.00017369495,0.00003229755,0.0002492825,0.0000016871559],"about_ca_topic_score_codex":0.01791726,"about_ca_topic_score_gemma":0.034236394,"teacher_disagreement_score":0.01791726,"about_ca_system_score_codex":0.00034984478,"about_ca_system_score_gemma":0.0004999204,"threshold_uncertainty_score":0.035625994},"labels":[],"label_agreement":null},{"id":"W2806702091","doi":"10.4095/292275","title":"Strong motion data from the magnitude 7.7 \"Haida Gwaii\" earthquake on October 27, 2012 (local time)","year":2013,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Magnitude (astronomy); Seismology; Geology; History; Physics","score_opus":0.0675172148263961,"score_gpt":0.2666380777625424,"score_spread":0.19912086293614628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806702091","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13192485,0.00012827189,0.0007506995,0.0005634888,0.00034513822,0.00033589356,0.8377987,0.0003233985,0.027829492],"genre_scores_gemma":[0.13735798,0.00034267057,0.001408329,0.000104015824,0.0001788265,0.00038557572,0.826446,0.00006739448,0.033709135],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9996939,0.000017758884,0.000032964133,0.00003690829,0.00015593156,0.00006254647],"domain_scores_gemma":[0.99844724,0.000061741805,0.00023579535,0.000119691904,0.0009251451,0.00021041589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042625458,0.00068475975,0.000387068,0.0021183286,0.00058936747,0.00039551614,0.0005850964,0.00053651567,0.009625949],"category_scores_gemma":[0.0011103526,0.0003442683,0.00021696069,0.0023474176,0.0001362482,0.00042798562,0.00075167266,0.00063033897,0.0053709275],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094469235,0.00044181384,0.28405273,0.00073244376,0.00013101746,0.0006054888,0.00067271176,0.0013918814,0.005935585,0.00086767465,0.6665083,0.03771567],"study_design_scores_gemma":[0.000063235166,0.000092865055,0.9197681,0.00004425633,0.0000437507,0.00007617941,0.00032392523,0.00049423095,0.0015340836,0.000065926775,0.077468984,0.000024570629],"about_ca_topic_score_codex":0.12006028,"about_ca_topic_score_gemma":0.3236628,"teacher_disagreement_score":0.87993973,"about_ca_system_score_codex":0.00057467225,"about_ca_system_score_gemma":0.0025143474,"threshold_uncertainty_score":0.23872286},"labels":[],"label_agreement":null},{"id":"W2806792168","doi":"10.1029/2017jb015242","title":"Crustal Deformation Following Great Subduction Earthquakes Controlled by Earthquake Size and Mantle Rheology","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Mantle (geology); Viscoelasticity; Plate tectonics; Episodic tremor and slip; Interplate earthquake; Elastic-rebound theory; Geodetic datum; Earthquake rupture; Rheology; Crust; Geophysics; Geodesy; Fault (geology); Seismic gap; Tectonics","score_opus":0.0238578813710182,"score_gpt":0.3017235998731396,"score_spread":0.27786571850212144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806792168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953425,0.000010527689,0.00028771363,0.0000028846694,3.642353e-7,7.48263e-7,0.000035040062,0.000008454969,0.00011994134],"genre_scores_gemma":[0.99985695,0.0000054779243,0.0000718163,5.6081683e-7,2.0068681e-7,5.1416697e-7,0.000036582638,0.0000014866043,0.000026486696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996686,0.000006032727,0.000002781969,0.00001084379,0.0000053220765,0.000008158615],"domain_scores_gemma":[0.999788,0.000058591155,0.00007168169,0.000033601205,0.000018833547,0.000029405173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018093163,0.00017076706,0.00012621279,0.00041232814,0.00009185294,0.00029636003,0.00019097755,0.00018064083,0.0005093468],"category_scores_gemma":[0.00073474646,0.00015251902,0.00019614636,0.00023236337,0.00024569652,0.00018384293,0.00020768438,0.00012147666,0.00009936484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047764336,0.00011264178,0.66253823,0.00004749821,0.00012485062,0.00038330758,0.0003833264,0.13773303,0.18281193,0.0007330555,0.00018013996,0.014474417],"study_design_scores_gemma":[0.000009181892,0.0000869051,0.8645971,0.000005958486,0.00001902017,0.00008235003,0.00008476736,0.12755229,0.0072898725,0.00013082218,0.00012739805,0.000014427632],"about_ca_topic_score_codex":0.0036078054,"about_ca_topic_score_gemma":0.0034627537,"teacher_disagreement_score":0.0036078054,"about_ca_system_score_codex":0.00021660353,"about_ca_system_score_gemma":0.00010191292,"threshold_uncertainty_score":0.007173598},"labels":[],"label_agreement":null},{"id":"W2808110972","doi":"10.1130/abs/2018nc-312533","title":"GEOPHYSICAL ANALYSIS OF OTTAWA LAKE AND RELATIONSHIP TO GLACIAL LAKE ARKONA, MONROE COUNTY, MICHIGAN","year":2018,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Glacial period; Geology; Glacial lake; Oceanography; Physical geography; Geomorphology; Geography","score_opus":0.019139602574665557,"score_gpt":0.2395974240375402,"score_spread":0.22045782146287463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2808110972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99608105,0.000070415605,0.000038804166,0.00010987486,0.0000027328754,0.000010166925,0.0013270007,0.000006830849,0.0023532205],"genre_scores_gemma":[0.9973757,0.000068080255,0.00017766074,0.000014586563,0.0000033123786,0.000010398363,0.00070428266,0.000002482052,0.0016433471],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998772,0.00001411653,0.000014075099,0.00003073115,0.000029304241,0.00003451991],"domain_scores_gemma":[0.99953043,0.000056816596,0.00010374812,0.000020822017,0.00020259654,0.00008557756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012102424,0.0001236813,0.00012171597,0.0014403776,0.0018290152,0.00071876333,0.00052611134,0.00020681629,0.0023382106],"category_scores_gemma":[0.00085773924,0.00017323284,0.0001762507,0.002067002,0.00048172456,0.00031733993,0.00077773794,0.0002410022,0.00018604651],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053454187,0.000014644729,0.9941555,0.000018140587,0.000037445017,0.00012572289,0.00105449,0.00024743404,0.00052906683,0.00015447049,0.00078025897,0.0028293112],"study_design_scores_gemma":[0.0000014480693,0.0000057562734,0.99684805,0.0000061821092,0.000011381672,0.00002805123,0.0017383347,0.0002334015,0.00008969256,0.000016571057,0.0010180883,0.0000031318827],"about_ca_topic_score_codex":0.86546326,"about_ca_topic_score_gemma":0.9796727,"teacher_disagreement_score":0.86546326,"about_ca_system_score_codex":0.0043346104,"about_ca_system_score_gemma":0.0039273445,"threshold_uncertainty_score":0.27065808},"labels":[],"label_agreement":null},{"id":"W2809801739","doi":"10.1007/s11069-018-3397-6","title":"Defining megathrust tsunami source scenarios for northernmost Cascadia","year":2018,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Ocean Networks Canada Society; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Canada","keywords":"Geology; Seismology; Trench; Seafloor spreading; Thrust fault; Slip (aerodynamics); Tsunami earthquake; Fault (geology); Thrust; Earthquake rupture; Subduction; Geophysics; Tectonics","score_opus":0.009746397422316954,"score_gpt":0.234867397063166,"score_spread":0.22512099964084906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2809801739","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97476834,0.00007208935,0.0051522423,0.00032915655,0.000013812315,0.0000818709,0.0019228079,0.00011180408,0.017547859],"genre_scores_gemma":[0.9971962,0.000038974635,0.0014410869,0.000012293679,0.0000028468085,0.000023393957,0.0006723003,0.000016538315,0.00059641514],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997539,0.00008556363,0.000013796528,0.000036627884,0.00003949405,0.00007062687],"domain_scores_gemma":[0.99929917,0.00022412551,0.0001089155,0.00004688187,0.00014970227,0.0001712168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085549906,0.000692781,0.00031615916,0.0017723873,0.00077549554,0.001884676,0.0009092058,0.0013376271,0.00260731],"category_scores_gemma":[0.002108922,0.00033170084,0.000775039,0.0010268271,0.00035090296,0.0009094232,0.00084786507,0.00049527385,0.00021933683],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028396022,0.00009502465,0.03886471,0.000048763868,0.000072013354,0.0012542553,0.00049452373,0.9312187,0.00134448,0.01957873,0.0017444053,0.005000442],"study_design_scores_gemma":[0.000102890655,0.00011106231,0.026657676,0.000049505663,0.00006779101,0.00018686218,0.0016014883,0.95697355,0.0011027834,0.010432072,0.0026767843,0.00003758578],"about_ca_topic_score_codex":0.039019987,"about_ca_topic_score_gemma":0.06207167,"teacher_disagreement_score":0.039019987,"about_ca_system_score_codex":0.0022666685,"about_ca_system_score_gemma":0.0010840818,"threshold_uncertainty_score":0.07758576},"labels":[],"label_agreement":null},{"id":"W2810509690","doi":"10.26464/epp2018029","title":"Source complexity of the 2016 &lt;i&gt;M&lt;/i&gt;&lt;sub&gt;W&lt;/sub&gt;7.8 Kaikoura (New Zealand) earthquake revealed from teleseismic and InSAR data","year":2018,"lang":"en","type":"article","venue":"Earth and Planetary Physics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Slip (aerodynamics); Interferometric synthetic aperture radar; Geodesy; Subduction; Seismic moment; Tectonics; Synthetic aperture radar; Physics","score_opus":0.03212585787857053,"score_gpt":0.21012229264220386,"score_spread":0.17799643476363333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2810509690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986844,0.00032266765,0.0040823338,0.00021549677,0.000022090406,0.000030421388,0.0034345272,0.000100826524,0.004947573],"genre_scores_gemma":[0.995915,0.00015685895,0.001000019,0.000011528451,0.00001778251,0.000013073953,0.0019893618,0.000037257443,0.0008590818],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998492,0.000006697881,0.000011901972,0.000049398826,0.000049246424,0.000033572127],"domain_scores_gemma":[0.99969435,0.000056539902,0.00009273095,0.00003423822,0.00008593716,0.00003630818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014942221,0.0003540294,0.00033727245,0.0010213397,0.0002564777,0.0006779123,0.00031351,0.00035650335,0.0020295843],"category_scores_gemma":[0.00094757794,0.0003457649,0.00029932882,0.0013137101,0.00036151576,0.00052653125,0.0005798363,0.00042426554,0.00037502186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012042456,0.00007380796,0.65233284,0.0006255324,0.00045209023,0.0070968987,0.0036261692,0.03730415,0.17980434,0.0043070163,0.004296846,0.10887608],"study_design_scores_gemma":[0.00003753285,0.000035866495,0.9686478,0.000042011314,0.00013981434,0.00067145616,0.0007243111,0.021340745,0.004182401,0.00072048133,0.0033964405,0.000061095394],"about_ca_topic_score_codex":0.042294577,"about_ca_topic_score_gemma":0.052318502,"teacher_disagreement_score":0.042294577,"about_ca_system_score_codex":0.000636884,"about_ca_system_score_gemma":0.00062076654,"threshold_uncertainty_score":0.08409679},"labels":[],"label_agreement":null},{"id":"W2810652856","doi":"10.5194/se-2018-45","title":"To what degree the geometry and kinematics of accretionary wedges in analogue experiments is dependent on material properties","year":2018,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Natural Science Foundation of Sichuan Province; National Natural Science Foundation of China","keywords":"Quartz; Cohesion (chemistry); Grain size; Kinematics; Wedge (geometry); Sorting; Geometry; Materials science; Granular material; Geology; Shape factor; Mineralogy; Composite material; Mathematics; Physics; Classical mechanics","score_opus":0.06131310301500786,"score_gpt":0.25537389467402255,"score_spread":0.1940607916590147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2810652856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915952,0.000098817574,0.0065281237,0.000031569147,0.000023508417,0.000030112518,0.00023983937,0.00007865406,0.0013741113],"genre_scores_gemma":[0.9972186,0.000041008156,0.002204818,0.000012305381,0.0000029664225,0.00001551149,0.00015472465,0.000018359196,0.00033183413],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9993912,0.000094812116,0.00005156222,0.00019521125,0.00018316657,0.00008403133],"domain_scores_gemma":[0.9986582,0.0004421414,0.00018474646,0.0004855825,0.00014527657,0.00008402793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006306373,0.00032724405,0.0004445384,0.00030253813,0.00030918495,0.0007411566,0.00065043394,0.00063660246,0.0026695242],"category_scores_gemma":[0.0028462303,0.00035500346,0.0004507906,0.000354905,0.0008704968,0.00077754084,0.0005397039,0.0007276609,0.0003114283],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018198695,0.0007050763,0.041556362,0.0005607924,0.00015214877,0.0010375126,0.0007568044,0.057551898,0.8755705,0.0015683671,0.00049895846,0.018221641],"study_design_scores_gemma":[0.0001302277,0.0027588732,0.12866394,0.00008640646,0.00024679315,0.0011237132,0.0010690695,0.19839992,0.66078955,0.0026713847,0.0038884282,0.00017179536],"about_ca_topic_score_codex":0.0013476439,"about_ca_topic_score_gemma":0.0014345311,"teacher_disagreement_score":0.0026695242,"about_ca_system_score_codex":0.00030918937,"about_ca_system_score_gemma":0.00016154579,"threshold_uncertainty_score":0.008930385},"labels":[],"label_agreement":null},{"id":"W284572635","doi":"","title":"Preliminary Comparative Analysis of Shock Metamorphism of Crystalline Basement Clasts in the Haughton Impact Ejecta Layer, Canada","year":2009,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science Supplement","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Ejecta; Shock metamorphism; Clastic rock; Geology; Basement; Metamorphism; Impact structure; Geochemistry; Petrology; Archaeology; Impact crater; Sedimentary rock; Astrobiology; Geography","score_opus":0.024416371672511438,"score_gpt":0.2681922923521322,"score_spread":0.24377592067962078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W284572635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943809,0.00027660883,0.00005641085,0.000017118104,0.000001705222,0.000015526866,0.00134908,0.000004155167,0.0038985678],"genre_scores_gemma":[0.9946413,0.00032613458,0.00012572292,0.000011004765,0.0000010144095,0.000005687476,0.0012887059,0.000004637885,0.0035957356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978524,0.000010078441,0.000010585581,0.000028998753,0.00007749951,0.000087665416],"domain_scores_gemma":[0.99889696,0.00005239725,0.00007105803,0.0000210095,0.0008249225,0.00013357158],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022752509,0.00025208673,0.00025797664,0.003277645,0.0020189034,0.0010709658,0.00047382925,0.0001946386,0.0026718902],"category_scores_gemma":[0.0006621848,0.00020292212,0.0002269122,0.0036625704,0.00037037706,0.00023740834,0.00041833342,0.00017187561,0.00030878725],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009412683,0.000054227705,0.960276,0.00006607682,0.000111798036,0.00038550096,0.0016948187,0.00079277897,0.019301005,0.00042694944,0.0005456362,0.015404152],"study_design_scores_gemma":[0.000001496972,0.000009606308,0.9985624,0.0000029289786,0.000007729604,0.000016124262,0.00042999387,0.00006403286,0.00044460586,0.0000044921094,0.00045500224,0.0000015994746],"about_ca_topic_score_codex":0.9775685,"about_ca_topic_score_gemma":0.9946319,"teacher_disagreement_score":0.022431493,"about_ca_system_score_codex":0.009779239,"about_ca_system_score_gemma":0.006933827,"threshold_uncertainty_score":0.07095373},"labels":[],"label_agreement":null},{"id":"W2851025245","doi":"10.1029/2018jb015581","title":"The<i>M</i>7 2016 Kumamoto, Japan, Earthquake: 3‐D Deformation Along the Fault and Within the Damage Zone Constrained From Differential Lidar Topography","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Southern California Earthquake Center; National Science Foundation","keywords":"Fault trace; Geology; Seismology; Fault (geology); Geodesy; Deformation (meteorology); Slip (aerodynamics); Echelon formation; Displacement (psychology)","score_opus":0.02265004269761835,"score_gpt":0.28125703748043757,"score_spread":0.25860699478281923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2851025245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981772,0.000033238677,0.00079078734,0.000027475717,0.0000033411136,0.0000035599426,0.00023687865,0.000026460837,0.0007011357],"genre_scores_gemma":[0.9984604,0.000030846786,0.0010473717,0.0000062377167,0.0000028571615,0.0000033935391,0.00033179866,0.000006019447,0.00011101405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996686,0.0000033247834,0.0000026382795,0.000009804137,0.000009795193,0.0000076659535],"domain_scores_gemma":[0.999905,0.00000942951,0.0000326627,0.000014889042,0.000023275512,0.000014756643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011180512,0.0001633318,0.00017425665,0.000308115,0.00019528272,0.00046055648,0.00017232967,0.00026163546,0.0005575186],"category_scores_gemma":[0.00033716182,0.00016864664,0.00014508812,0.0004532654,0.00019230852,0.00022954654,0.00032654472,0.00014959456,0.0001858506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019324016,0.000112201196,0.73430747,0.00012933493,0.000112463975,0.0010036519,0.00064222753,0.0431055,0.14827947,0.0007965363,0.0022720767,0.069045775],"study_design_scores_gemma":[0.000010887724,0.000036875295,0.9320954,0.000015266705,0.000027497661,0.00014349945,0.0002757391,0.061359137,0.0048404844,0.00021309234,0.00095910893,0.000022882943],"about_ca_topic_score_codex":0.013216073,"about_ca_topic_score_gemma":0.031592693,"teacher_disagreement_score":0.013216073,"about_ca_system_score_codex":0.00026135275,"about_ca_system_score_gemma":0.00035461277,"threshold_uncertainty_score":0.026278317},"labels":[],"label_agreement":null},{"id":"W2854262204","doi":"10.1029/2018gl078304","title":"In Situ Permeability and Scale Dependence of an Active Accretionary Prism Determined From Cross‐Borehole Experiments","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Borehole; Geology; Accretionary wedge; Permeability (electromagnetism); Advection; Tectonics; Fluid dynamics; Petrology; Submarine pipeline; Drilling fluid; Drilling; Subduction; Seismology; Geotechnical engineering; Mechanics; Materials science","score_opus":0.039331178857534455,"score_gpt":0.3334711768420309,"score_spread":0.29413999798449647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2854262204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990613,0.000010576604,0.0007034044,0.0000035579753,6.0767815e-7,0.000003067611,0.000047412763,0.0000113612905,0.00015875796],"genre_scores_gemma":[0.9995827,0.000008940614,0.00034862265,0.0000017348046,4.1554782e-7,0.0000027142696,0.000027338014,0.0000010346236,0.00002657693],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99989176,0.000011655424,0.000010475231,0.00003851677,0.000025095436,0.00002247362],"domain_scores_gemma":[0.999678,0.00008544038,0.00011456772,0.000029783832,0.000055201184,0.000037133523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018926914,0.00020614061,0.00013780067,0.00022638042,0.00018567985,0.0002091689,0.00022708645,0.0001951273,0.00027581293],"category_scores_gemma":[0.0006248239,0.00016637001,0.00011821969,0.00017181956,0.00033690094,0.00030065535,0.00028100636,0.00019189822,0.000043789958],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016680369,0.0000547277,0.04287434,0.00003307676,0.000012357265,0.00012436116,0.0002132819,0.0014960245,0.95280397,0.000078592704,0.000028096658,0.002114296],"study_design_scores_gemma":[0.00003483035,0.0005534178,0.5984208,0.000008569002,0.000040796833,0.00024883074,0.0003484607,0.021367634,0.378436,0.000105537656,0.0004049341,0.000030202375],"about_ca_topic_score_codex":0.0025997185,"about_ca_topic_score_gemma":0.0030725247,"teacher_disagreement_score":0.0025997185,"about_ca_system_score_codex":0.00017588641,"about_ca_system_score_gemma":0.00009305165,"threshold_uncertainty_score":0.005169153},"labels":[],"label_agreement":null},{"id":"W2866581105","doi":"10.1029/2018gl077551","title":"Geomechanical Sensitivities of Injection‐Induced Earthquakes","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Induced seismicity; Geology; Pore water pressure; Seismology; Hydrostatic equilibrium; Slip (aerodynamics); Overburden; Fluid pressure; Hydrostatic pressure; Geotechnical engineering; Mechanics","score_opus":0.056116360086624115,"score_gpt":0.30083686376065805,"score_spread":0.24472050367403392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2866581105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991793,0.000023831675,0.00027686238,0.00001008251,0.0000010576717,0.0000033318038,0.0001247818,0.000014209184,0.00036649656],"genre_scores_gemma":[0.99986446,0.000008114327,0.000027473307,0.0000025301017,4.986096e-7,0.0000011190058,0.000059393467,0.0000015472338,0.00003483091],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985206,0.000024415558,0.000016487638,0.00003471256,0.000032892687,0.000039438077],"domain_scores_gemma":[0.99942964,0.00017279267,0.00016683046,0.00005553556,0.00010452626,0.00007076278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019764091,0.00016466662,0.00022101754,0.00048732822,0.00012338128,0.00027710976,0.0001704349,0.00026244667,0.0014024036],"category_scores_gemma":[0.0010106902,0.00014354443,0.00018432616,0.00033319203,0.00019285867,0.00022105883,0.0003430208,0.00020313333,0.00016100633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00097432005,0.00017270679,0.5436898,0.00011495123,0.0002264337,0.00058451813,0.00025913803,0.06805724,0.37064806,0.0004577883,0.00030331084,0.014511751],"study_design_scores_gemma":[0.0000096429985,0.00047064965,0.91592216,0.000005614224,0.00004308302,0.0002724427,0.00029144384,0.037002504,0.04537743,0.0002679402,0.000310041,0.000026994034],"about_ca_topic_score_codex":0.0012727809,"about_ca_topic_score_gemma":0.0013437477,"teacher_disagreement_score":0.0014024036,"about_ca_system_score_codex":0.0002718455,"about_ca_system_score_gemma":0.00008593425,"threshold_uncertainty_score":0.004691541},"labels":[],"label_agreement":null},{"id":"W2874971891","doi":"10.1038/s41598-018-29105-2","title":"Growth of mountain belts in central Asia triggers a new collision zone in central India","year":2018,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Russian Science Foundation; King Saud University; Russian Foundation for Basic Research; Institute of Population and Public Health; Department of Science and Technology, Ministry of Science and Technology, India","keywords":"Collision zone; Geology; Lithosphere; Central asia; Lineament; Continental collision; Collision; Seismology; Induced seismicity; Plate tectonics; Eurasian Plate; South asia; Tectonics; Geography; Subduction; Physical geography; Ancient history; History","score_opus":0.012120262515723032,"score_gpt":0.22020400155693454,"score_spread":0.2080837390412115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2874971891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99928856,0.000033557048,0.0001461261,0.000019525887,0.0000012264303,0.0000030936542,0.000021316697,0.00001391106,0.00047263966],"genre_scores_gemma":[0.9998042,0.000020024265,0.00008648498,0.0000025369316,7.913959e-7,0.0000015951381,0.00002740913,0.0000010471872,0.00005595175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995446,0.0000054144,0.0000036622214,0.00001072847,0.000008421049,0.000017196002],"domain_scores_gemma":[0.99989057,0.000015352016,0.000036899295,0.000010408717,0.000012967183,0.00003373679],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000092340524,0.0001332006,0.00015577085,0.00041669008,0.0003895279,0.0006992469,0.0003726185,0.00018186442,0.0005533282],"category_scores_gemma":[0.00024855573,0.00021562228,0.00025253682,0.00044306577,0.00034995686,0.00020110155,0.0004963814,0.00015770821,0.00006127619],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030478425,0.00013307217,0.9037297,0.000117884054,0.00011826668,0.0031183695,0.0023034962,0.03557654,0.04075712,0.0028608236,0.0005875217,0.010392439],"study_design_scores_gemma":[0.00004110443,0.0001345928,0.94679654,0.000017211736,0.00007403279,0.0008261795,0.002041413,0.04630215,0.0017909097,0.00078931043,0.0011607319,0.000025735695],"about_ca_topic_score_codex":0.021618394,"about_ca_topic_score_gemma":0.024677446,"teacher_disagreement_score":0.021618394,"about_ca_system_score_codex":0.0006038774,"about_ca_system_score_gemma":0.00050105224,"threshold_uncertainty_score":0.04298514},"labels":[],"label_agreement":null},{"id":"W287805110","doi":"","title":"Linking postseismic and interseismic deformation along the North Anatolian Fault Zone: The role of transient rheology and low-viscosity shear zones","year":2010,"lang":"en","type":"article","venue":"EGUGA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Crust; Rheology; Shear zone; Mantle (geology); Viscoelasticity; Seismology; Shear (geology); Upper crust; North Anatolian Fault; Petrology; Geophysics; Fault (geology); Tectonics; Materials science","score_opus":0.004822590367086582,"score_gpt":0.1858167237061662,"score_spread":0.18099413333907963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W287805110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993974,0.000095211755,0.000101665646,0.00001783933,0.0000012451691,0.0000018478114,0.000019735002,0.000004390413,0.00036069544],"genre_scores_gemma":[0.99967647,0.00008099625,0.00007271218,0.000003008856,0.0000014866309,0.0000016032701,0.00004749895,0.000001947139,0.00011434182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989045,0.00002317086,0.000013070255,0.00003644878,0.000011896291,0.000024831103],"domain_scores_gemma":[0.9996082,0.00009889464,0.00014349756,0.00003795995,0.000071590446,0.000039878396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024145901,0.00024946834,0.00020280549,0.001008494,0.00031223547,0.0007390844,0.0002737783,0.00043093195,0.00085059484],"category_scores_gemma":[0.0007876182,0.00027776125,0.00015744407,0.0006529755,0.0003306315,0.00077062426,0.0004892136,0.00018928268,0.00014534623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018534882,0.00008614812,0.9711701,0.000033551725,0.00009523958,0.0002193643,0.00039581786,0.003400628,0.010154011,0.0002724233,0.000058910504,0.0139284395],"study_design_scores_gemma":[0.00000452281,0.00002306667,0.9934701,0.000006270204,0.000022435393,0.00004478573,0.0001888618,0.00549695,0.0005108276,0.000106821775,0.000120331206,0.000005054565],"about_ca_topic_score_codex":0.017754177,"about_ca_topic_score_gemma":0.030288035,"teacher_disagreement_score":0.017754177,"about_ca_system_score_codex":0.0006685105,"about_ca_system_score_gemma":0.00039385952,"threshold_uncertainty_score":0.035301626},"labels":[],"label_agreement":null},{"id":"W2883852832","doi":"","title":"Geophysical Applications at the Site of Fort Halifax, PA (36DA0008)","year":2018,"lang":"en","type":"article","venue":"The 82nd Annual Meeting of the Society for American Archaeology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geophysics; Remote sensing","score_opus":0.009302188477939293,"score_gpt":0.2381247764796134,"score_spread":0.2288225880016741,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883852832","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.076388106,0.0019520333,0.0076003014,0.022689134,0.0051948684,0.00053798506,0.05625436,0.0067700255,0.8226131],"genre_scores_gemma":[0.19610697,0.0011783156,0.02037734,0.000927321,0.0005744574,0.0002127056,0.01458593,0.0004995625,0.7655373],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99985564,0.000015049217,0.0000035189034,0.000032815544,0.000060376766,0.000032429612],"domain_scores_gemma":[0.99949276,0.00004538283,0.000011917387,0.00003352181,0.00031681944,0.000099574594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002982674,0.00050975237,0.00021726543,0.00084554753,0.0019326509,0.0007718689,0.0006118713,0.0005473405,0.21029195],"category_scores_gemma":[0.0007131963,0.00018890298,0.0001515999,0.0008568109,0.00031192246,0.00032618814,0.0009635331,0.0004840488,0.03897515],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015901818,0.000048951228,0.009499585,0.00007508923,0.000005711782,0.00055070955,0.00038974153,0.00048633374,0.004101753,0.0013669373,0.7880716,0.19524466],"study_design_scores_gemma":[0.000059941918,0.000056352234,0.026448991,0.000053408763,0.000005540357,0.00029122108,0.00089022843,0.0013774486,0.0015335951,0.0007964256,0.96847486,0.00001193033],"about_ca_topic_score_codex":0.10562656,"about_ca_topic_score_gemma":0.28576988,"teacher_disagreement_score":0.21029195,"about_ca_system_score_codex":0.00070838997,"about_ca_system_score_gemma":0.002783685,"threshold_uncertainty_score":0.7034967},"labels":[],"label_agreement":null},{"id":"W2883867380","doi":"10.1180/clm.2018.22","title":"Fault gouge dating: history and evolution","year":2018,"lang":"en","type":"article","venue":"Clay Minerals","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ExxonMobil (Canada)","funders":"","keywords":"Geology; Fault gouge; Sedimentary rock; Radiometric dating; Thrust fault; Absolute dating; Fault (geology); Tectonics; Metamorphic rock; Igneous rock; Seismology; Illite; Geochemistry; Clay minerals; Paleontology; Quaternary","score_opus":0.02849400558957922,"score_gpt":0.23038395891530236,"score_spread":0.20188995332572313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883867380","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9687528,0.009087363,0.011148967,0.00030993787,0.000050334776,0.000020204685,0.0018233274,0.00018895633,0.008618088],"genre_scores_gemma":[0.9920682,0.0016165277,0.004171804,0.00002814636,0.000023634168,0.000005070934,0.000737011,0.00004346549,0.0013062424],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992009,0.00021703212,0.00007323958,0.0002643247,0.00019461165,0.000049850543],"domain_scores_gemma":[0.9968491,0.0006698392,0.0009872825,0.00036533913,0.0010107554,0.0001176003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024065422,0.00020919382,0.00022727101,0.004650523,0.00029684018,0.0012624658,0.00041395743,0.00039103214,0.0014841541],"category_scores_gemma":[0.005283183,0.00018232696,0.00013336519,0.0037529632,0.00053881697,0.000978542,0.00054821814,0.0002956187,0.00044291624],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015095742,0.00001820843,0.81703115,0.00017430642,0.000098718025,0.00017574707,0.00068813673,0.0016455969,0.014732381,0.0016778182,0.00061855896,0.16298844],"study_design_scores_gemma":[0.000003659681,0.00013758021,0.9596554,0.00008625048,0.0000734013,0.0012823232,0.00044406942,0.0033676308,0.012774578,0.0008973974,0.021245351,0.000032294614],"about_ca_topic_score_codex":0.0060089137,"about_ca_topic_score_gemma":0.0077088363,"teacher_disagreement_score":0.0060089137,"about_ca_system_score_codex":0.0006726146,"about_ca_system_score_gemma":0.00019600707,"threshold_uncertainty_score":0.012727141},"labels":[],"label_agreement":null},{"id":"W2883875668","doi":"10.1029/2018jb015545","title":"Controls on Mid‐ocean Ridge Normal Fault Seismicity Across Spreading Rates From Rate‐and‐State Friction Models","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Division of Earth Sciences; Division of Ocean Sciences; National Science Foundation","keywords":"Geology; Seismology; Seismic moment; Induced seismicity; Slip (aerodynamics); Ridge; Fault (geology); Tectonics; Seismic gap; Geodetic datum; Geodesy; Paleontology","score_opus":0.05216554651928905,"score_gpt":0.33673283381953956,"score_spread":0.2845672873002505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883875668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986981,0.00006942847,0.010082793,0.00011751208,0.000005305792,0.00002085766,0.00014640439,0.00004986791,0.0025268395],"genre_scores_gemma":[0.9995036,0.000021965434,0.00022475062,0.0000049741657,0.0000011188602,0.000004165249,0.00003787942,0.000006299831,0.00019530657],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998035,0.00006994851,0.000012322084,0.00003768764,0.00002917991,0.000047434096],"domain_scores_gemma":[0.99874854,0.0006680778,0.0002641708,0.00013706203,0.000081321654,0.00010081831],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009636097,0.0006074486,0.0005002231,0.00055142463,0.00024828216,0.0009447667,0.0008051574,0.0005081604,0.0014947135],"category_scores_gemma":[0.0036598449,0.00042087483,0.00077630667,0.0002821032,0.00058786874,0.0008101703,0.0006288167,0.0005466145,0.00011391124],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012984787,0.0000760517,0.020278756,0.00002946625,0.00007374994,0.00011225657,0.000062544044,0.95993346,0.009880435,0.0074119875,0.00015563522,0.001855823],"study_design_scores_gemma":[0.000010906655,0.000019974388,0.004992467,0.0000024823976,0.000012242724,0.000013938893,0.000010224312,0.9932637,0.00047714356,0.0011432997,0.00004535274,0.000008335192],"about_ca_topic_score_codex":0.013909906,"about_ca_topic_score_gemma":0.008110692,"teacher_disagreement_score":0.013909906,"about_ca_system_score_codex":0.000984088,"about_ca_system_score_gemma":0.0005479324,"threshold_uncertainty_score":0.027657866},"labels":[],"label_agreement":null},{"id":"W2883999508","doi":"10.1029/2018gl078767","title":"Spatial Variation in the Slip Zone Thickness of a Seismogenic Fault","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"University of California, Riverside; U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Slip (aerodynamics); Geology; Seismology; Crust; Geophysics","score_opus":0.03753241815705789,"score_gpt":0.2914589624862413,"score_spread":0.25392654432918343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883999508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99973625,0.000008758268,0.00008957175,0.0000023782243,2.4768363e-7,3.9128872e-7,0.000048857248,0.0000040891878,0.00010941402],"genre_scores_gemma":[0.9998536,0.000004672922,0.000049559625,0.0000011654283,5.554359e-7,6.002396e-7,0.000047322337,0.000001040154,0.00004137187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995244,0.000007778962,0.0000029890405,0.000018795894,0.0000073178544,0.000010706094],"domain_scores_gemma":[0.99966526,0.000100854,0.00011174022,0.000033876124,0.00005210615,0.000036194284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011649378,0.00008606817,0.00009328834,0.00058539625,0.00013571179,0.00023293498,0.000103111066,0.00014425477,0.0007168333],"category_scores_gemma":[0.00035088105,0.00010624686,0.00009725812,0.00034987144,0.00023323124,0.0001236201,0.0002023701,0.00010811842,0.000072276394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038250966,0.0000636065,0.685173,0.000035713543,0.00011840825,0.0004663387,0.001023565,0.0034428712,0.2989921,0.00023040987,0.00015729433,0.0099141495],"study_design_scores_gemma":[0.0000014400888,0.000017749422,0.99591994,0.000001201415,0.0000075852586,0.000084724365,0.00010031432,0.00077277975,0.00299443,0.00002063449,0.00007660365,0.0000026038642],"about_ca_topic_score_codex":0.002017844,"about_ca_topic_score_gemma":0.0019520266,"teacher_disagreement_score":0.002017844,"about_ca_system_score_codex":0.00014450864,"about_ca_system_score_gemma":0.00004892021,"threshold_uncertainty_score":0.004012227},"labels":[],"label_agreement":null},{"id":"W2884526877","doi":"10.1029/2017jb015417","title":"Structural Inheritance Control on Intraplate Present‐Day Deformation: GPS Strain Rate Variations in the Saint Lawrence Valley, Eastern Canada","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Agence Nationale de la Recherche; Université Laval","keywords":"Intraplate earthquake; Strain rate; Lithosphere; Post-glacial rebound; Geology; Tectonics; Global Positioning System; Geodesy; Strain rate tensor; Induced seismicity; Seismology; Inheritance (genetic algorithm); Paleontology; Glacial period; Genetics","score_opus":0.03731815646045556,"score_gpt":0.2945067029427489,"score_spread":0.25718854648229333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2884526877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736834,0.000059570855,0.0002418005,0.000048789523,0.000001303621,0.000004511357,0.0009737435,0.000019644962,0.0012821986],"genre_scores_gemma":[0.9991074,0.00002589045,0.0001338428,0.00000510636,6.1474185e-7,0.0000011930432,0.00041761526,0.0000029899627,0.00030535934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978024,0.0000152866,0.000008433742,0.000047506695,0.0000778334,0.00007064901],"domain_scores_gemma":[0.9992355,0.00009086314,0.000099535486,0.000041797262,0.00043730254,0.00009497443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002441064,0.00023292768,0.00024446275,0.001000452,0.0009614002,0.0010768545,0.0006227722,0.00018138748,0.0010119929],"category_scores_gemma":[0.00091056863,0.00013791358,0.00021064452,0.0018855329,0.0006039646,0.00017583442,0.00040156292,0.0002342249,0.0000939219],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000091467446,0.000020128251,0.9746249,0.000020210036,0.00008263632,0.00014201073,0.0005782492,0.008929781,0.0029374307,0.0004897221,0.00073933887,0.0113442615],"study_design_scores_gemma":[0.0000031446034,0.0000043759537,0.9925833,0.0000054860693,0.000009750381,0.000014849389,0.0003654,0.0063107526,0.00022279173,0.00004405657,0.0004262566,0.000009919996],"about_ca_topic_score_codex":0.9877456,"about_ca_topic_score_gemma":0.9919784,"teacher_disagreement_score":0.012254417,"about_ca_system_score_codex":0.008791861,"about_ca_system_score_gemma":0.007783876,"threshold_uncertainty_score":0.063789725},"labels":[],"label_agreement":null},{"id":"W2885028024","doi":"10.1007/s10950-018-9783-4","title":"Regional minimum 1-D P-wave velocity model for a new seismicity catalogue with precise and consistent earthquake locations in southern Iran","year":2018,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research","keywords":"Seismology; Hypocenter; Geology; Earthquake location; Induced seismicity; Epicenter; Geodesy; Inversion (geology); Data set; Tectonics; Statistics","score_opus":0.060823268555999524,"score_gpt":0.2439575815792628,"score_spread":0.18313431302326327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885028024","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9529267,0.0002679449,0.033140406,0.0002277257,0.00006735732,0.000053516967,0.009378898,0.00096114585,0.0029763565],"genre_scores_gemma":[0.97781277,0.0001253359,0.011032925,0.000012465612,0.000014287015,0.000051481715,0.010265166,0.00006855001,0.00061702664],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990296,0.000010265255,0.000007843294,0.00003913521,0.000016009966,0.000023784587],"domain_scores_gemma":[0.9997818,0.000028848186,0.000030324,0.000041831438,0.00010106805,0.000016147495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000362078,0.0005175901,0.00058888487,0.0008430616,0.00033481632,0.00047315066,0.0014886191,0.00066107156,0.0009973086],"category_scores_gemma":[0.0008217084,0.00041619563,0.00078505895,0.0010438114,0.00013962248,0.00058154296,0.00037934043,0.00042470824,0.0005650993],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018820114,0.00008626737,0.057132855,0.00007583338,0.00011439257,0.00020738602,0.00011460101,0.90801984,0.0020105902,0.0008555878,0.004092059,0.027102437],"study_design_scores_gemma":[0.000051699128,0.000016574568,0.031138131,0.000013716108,0.00004995116,0.000032019205,0.000063696374,0.96691585,0.0003403397,0.00030127564,0.0010549041,0.000021931157],"about_ca_topic_score_codex":0.15700102,"about_ca_topic_score_gemma":0.09878592,"teacher_disagreement_score":0.15700102,"about_ca_system_score_codex":0.00072111766,"about_ca_system_score_gemma":0.0016179427,"threshold_uncertainty_score":0.31217432},"labels":[],"label_agreement":null},{"id":"W2886428601","doi":"10.1029/2017jb015039","title":"Surface Rupture Morphology and Vertical Slip Distribution of the 1959<b><i>M</i></b><sub><b><i>w</i></b></sub>7.2 Hebgen Lake (Montana) Earthquake From Airborne Lidar Topography","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Division of Earth Sciences; Natural Sciences and Engineering Research Council of Canada; Southern California Earthquake Center; National Science Foundation","keywords":"Fault scarp; Geology; Canyon; Slip (aerodynamics); Seismology; Fault (geology); Escarpment; Geodetic datum; Surface rupture; Paleoseismology; Geodesy; Geomorphology","score_opus":0.02155665216389295,"score_gpt":0.2703957479061825,"score_spread":0.24883909574228952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886428601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999527,0.000015410453,0.00003906953,0.000004336718,2.9238237e-7,7.3795e-7,0.00013901334,0.0000043294535,0.00026991987],"genre_scores_gemma":[0.99952257,0.000008859175,0.00006225643,0.0000022192658,6.1063747e-7,7.2977457e-7,0.00028837693,0.0000010482229,0.00011333647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996865,0.0000026367222,0.0000019008323,0.000010153219,0.000008988024,0.000007654117],"domain_scores_gemma":[0.9998833,0.000012548217,0.000038584018,0.0000066117705,0.00003531836,0.000023572038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000630538,0.00006956057,0.00007729618,0.0005663877,0.00014847206,0.0002869282,0.00011483818,0.00019607416,0.0007700055],"category_scores_gemma":[0.00018267326,0.000072772404,0.00006443263,0.00042074083,0.00014491004,0.00013223337,0.00014484249,0.00006618985,0.00016773093],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011269042,0.000026802669,0.9621319,0.0000138060195,0.000026073621,0.00024709458,0.00036335914,0.0009818424,0.025528695,0.000052210118,0.0003136484,0.010201735],"study_design_scores_gemma":[6.678496e-7,0.000006915613,0.9992481,7.4412054e-7,0.0000012945577,0.000031373507,0.00006759502,0.00035529915,0.00022483528,0.0000039386805,0.000058104466,0.0000010959603],"about_ca_topic_score_codex":0.019720964,"about_ca_topic_score_gemma":0.040914938,"teacher_disagreement_score":0.019720964,"about_ca_system_score_codex":0.00032045497,"about_ca_system_score_gemma":0.00006537499,"threshold_uncertainty_score":0.039212346},"labels":[],"label_agreement":null},{"id":"W2886632892","doi":"","title":"Georgian Bay (Ontario) earthquake with magnitude m (sub N) 4.3 (October 20, 2005) and its foreshock-aftershock sequence; tectonic implications","year":2006,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Foreshock; Bay; Seismology; Geology; Magnitude (astronomy); Georgian; Tectonics; Sequence (biology); Latitude; Oceanography; Geodesy","score_opus":0.052914268655157824,"score_gpt":0.2788980357104301,"score_spread":0.22598376705527226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886632892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.72036284,0.0028718805,0.00028261793,0.0140614975,0.00034206492,0.00013479662,0.015993675,0.00010572228,0.24584489],"genre_scores_gemma":[0.92333794,0.0032374284,0.0005079477,0.00072523666,0.0000516962,0.000013827241,0.0033827124,0.00001641559,0.06872682],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999151,0.0000041265394,0.0000026068135,0.000009727913,0.000036791338,0.000031585598],"domain_scores_gemma":[0.9997198,0.000007627936,0.000062012994,0.000006913199,0.00010517205,0.00009858464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000092140865,0.00022829958,0.0001120724,0.00060279004,0.0033237594,0.000883558,0.0003490008,0.00038974633,0.01019127],"category_scores_gemma":[0.00039312485,0.00016265946,0.000081677514,0.001187466,0.0010436717,0.0002594,0.0005440901,0.00032701765,0.0009850455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006295963,0.000070438815,0.69740933,0.00057713495,0.000049751976,0.007907269,0.010335369,0.0012095612,0.01172831,0.011686276,0.19512391,0.06327313],"study_design_scores_gemma":[0.000020050757,0.000018472641,0.89972234,0.00008104843,0.000010859983,0.00026966722,0.003979703,0.00013534901,0.00023040574,0.00045645927,0.095059656,0.000015965898],"about_ca_topic_score_codex":0.9880108,"about_ca_topic_score_gemma":0.9984219,"teacher_disagreement_score":0.018005911,"about_ca_system_score_codex":0.018005911,"about_ca_system_score_gemma":0.020076802,"threshold_uncertainty_score":0.1306426},"labels":[],"label_agreement":null},{"id":"W2887175844","doi":"10.36487/acg_repo/574_40","title":"Multidisciplinary Monitoring of the Entire Life Span of an Earthquake in South African Gold Mines","year":2005,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ritsumeikan University; University of Tokyo; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Multidisciplinary approach; Life span; Span (engineering); Forensic engineering; Geology; Seismology; Engineering; Civil engineering; Medicine; Gerontology","score_opus":0.024728826105055866,"score_gpt":0.23535185683566576,"score_spread":0.2106230307306099,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887175844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993923,0.00009575763,0.00016120473,0.000022805854,0.0000018983421,0.0000069232365,0.00016650077,0.000002351235,0.00015027223],"genre_scores_gemma":[0.99892765,0.000115003146,0.0005179637,0.000010837624,0.0000053701015,0.000015451305,0.00022951142,0.0000011165956,0.00017710998],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997259,0.00004947807,0.000031013093,0.00008340547,0.00003932588,0.000070967064],"domain_scores_gemma":[0.9995683,0.000048150723,0.00013306155,0.000030270232,0.00011141654,0.00010878535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040092514,0.00030405505,0.00039737692,0.002412291,0.0005176535,0.0003496042,0.00037200164,0.00066871924,0.0002963428],"category_scores_gemma":[0.00074189715,0.00018294848,0.00021841358,0.0013928263,0.00019525182,0.0005148832,0.0011072699,0.00017937312,0.00009997502],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001127623,0.000068155874,0.97028077,0.000059442693,0.000107743836,0.0007452056,0.0019478757,0.00073530816,0.009811742,0.000042614305,0.00019043643,0.015898054],"study_design_scores_gemma":[0.0000024162275,0.000036152258,0.99680823,0.00001025707,0.000027975173,0.0001701842,0.0014602239,0.0008245498,0.00033041477,0.000022319606,0.00030283112,0.000004546818],"about_ca_topic_score_codex":0.015441028,"about_ca_topic_score_gemma":0.034549806,"teacher_disagreement_score":0.015441028,"about_ca_system_score_codex":0.0003384281,"about_ca_system_score_gemma":0.0003335251,"threshold_uncertainty_score":0.030702293},"labels":[],"label_agreement":null},{"id":"W2887308933","doi":"10.1029/2018jb015620","title":"Geodetically Inferred Locking State of the Cascadia Megathrust Based on a Viscoelastic Earth Model","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Viscoelasticity; Geodetic datum; Geodesy; Seismology; Slip (aerodynamics); Earth model; Subduction; Creep; Tectonics; Engineering","score_opus":0.04737862865242928,"score_gpt":0.3204798114179897,"score_spread":0.2731011827655604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887308933","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98777974,0.00004055262,0.009320212,0.00008299181,0.000005856473,0.000003905283,0.0002722581,0.00022366182,0.002270708],"genre_scores_gemma":[0.9989316,0.000023308272,0.0006465792,0.000004133878,9.506532e-7,0.0000018835289,0.00013767568,0.000011717263,0.00024209451],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996495,0.0000052388555,0.0000027285485,0.000013695251,0.000005926869,0.000007466238],"domain_scores_gemma":[0.9999006,0.000016025295,0.000019598534,0.000024448338,0.000020494163,0.000018908957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011850785,0.0003904196,0.00017099714,0.00054822315,0.000211201,0.00046061884,0.0004155748,0.00043827656,0.0012166568],"category_scores_gemma":[0.0005641602,0.00022681445,0.00027140472,0.0003847547,0.00026176072,0.00033078188,0.0002850224,0.00024291419,0.00020781571],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006873688,0.000035642268,0.09449623,0.000025860341,0.000057135498,0.00024083798,0.00009945753,0.88131565,0.014398606,0.001516863,0.00036836666,0.007376607],"study_design_scores_gemma":[0.000011414026,0.00002083091,0.03988153,0.0000065659224,0.000015147396,0.00003066086,0.000043334927,0.95800817,0.0011137453,0.00052398397,0.00033201382,0.000012578103],"about_ca_topic_score_codex":0.03417964,"about_ca_topic_score_gemma":0.023763495,"teacher_disagreement_score":0.03417964,"about_ca_system_score_codex":0.0006360324,"about_ca_system_score_gemma":0.0004326818,"threshold_uncertainty_score":0.067961335},"labels":[],"label_agreement":null},{"id":"W2887424155","doi":"10.1029/2018gl079027","title":"Faults and Non‐Double‐Couple Components for Induced Earthquakes","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey","keywords":"Induced seismicity; Geology; Seismology; Tectonics; Hydraulic fracturing; Thrust fault; Fault (geology); Focal mechanism; Slip (aerodynamics); Structural basin; Geomorphology; Geotechnical engineering","score_opus":0.08624623253716447,"score_gpt":0.3245176244466853,"score_spread":0.23827139190952085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887424155","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981207,0.00006211488,0.0010043165,0.000014047131,0.0000018566693,0.0000072754033,0.000070742186,0.000013659816,0.00070525386],"genre_scores_gemma":[0.9996112,0.000021624393,0.00018399535,0.0000017744187,0.0000027926044,0.000001924437,0.00007269718,0.0000020627417,0.00010200598],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999044,0.000010646315,0.000008184725,0.000017063167,0.000033656113,0.000026046971],"domain_scores_gemma":[0.9995136,0.00009183095,0.00019149604,0.00004365181,0.00008032863,0.000079112746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015542975,0.0002647707,0.00015408985,0.0013253391,0.00018274783,0.0003880495,0.00016115532,0.00014621642,0.0014974452],"category_scores_gemma":[0.000903668,0.00012373249,0.00021071383,0.0006988608,0.00026046715,0.00027446437,0.00038498806,0.00013973305,0.00010325531],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030072598,0.000090383655,0.90191406,0.00008596918,0.00011831184,0.00044929312,0.00039554312,0.005334976,0.05852473,0.0011277526,0.00023624634,0.031421993],"study_design_scores_gemma":[0.000004517062,0.000025581287,0.9905095,0.0000029703788,0.00001635111,0.00012076745,0.00010181819,0.00746404,0.0014277678,0.00015521378,0.0001664364,0.000005088618],"about_ca_topic_score_codex":0.004974064,"about_ca_topic_score_gemma":0.010958559,"teacher_disagreement_score":0.004974064,"about_ca_system_score_codex":0.000330421,"about_ca_system_score_gemma":0.00021593747,"threshold_uncertainty_score":0.009890258},"labels":[],"label_agreement":null},{"id":"W2887632907","doi":"10.1016/j.tecto.2018.07.023","title":"Structural framework and deformation history of the western Cyprus Arc","year":2018,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Paleontology; Tectonics; Structural basin; Extensional tectonics; Seafloor spreading; Quaternary; Late Miocene; Inversion (geology); Fold (higher-order function); Crust; Extensional definition","score_opus":0.01745570260084924,"score_gpt":0.20568295695610384,"score_spread":0.1882272543552546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887632907","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937349,0.00017854825,0.000088853725,0.000044933346,0.000002884962,0.00000514779,0.00054222014,0.000007741025,0.0053948746],"genre_scores_gemma":[0.99894756,0.00009107106,0.000066926994,0.0000040604245,0.000003470344,0.0000022607342,0.00028131696,0.0000028556533,0.000600531],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999145,0.000012940858,0.000008584274,0.000027027452,0.000013364295,0.000023620887],"domain_scores_gemma":[0.9998692,0.000015354457,0.00004450478,0.00001377858,0.000040482053,0.000016626132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010774225,0.00012850521,0.00010257433,0.0014625869,0.0005106817,0.00071016524,0.00022306496,0.00021322661,0.002599983],"category_scores_gemma":[0.000292463,0.000103136146,0.00013720947,0.0014992001,0.00039243794,0.00019716322,0.00034498094,0.00010980995,0.00032618226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038561018,0.00007687934,0.8986513,0.00012479808,0.00014161001,0.0010135698,0.0019325326,0.020891078,0.012902523,0.0055904808,0.001196835,0.0570928],"study_design_scores_gemma":[0.0000014590739,0.000008504606,0.997875,0.0000065849244,0.000005991835,0.000053648237,0.00014287504,0.00088281103,0.000090547335,0.000039160946,0.0008911778,0.0000022278095],"about_ca_topic_score_codex":0.08506792,"about_ca_topic_score_gemma":0.113891914,"teacher_disagreement_score":0.08506792,"about_ca_system_score_codex":0.0009636346,"about_ca_system_score_gemma":0.00053681334,"threshold_uncertainty_score":0.16914558},"labels":[],"label_agreement":null},{"id":"W2888271949","doi":"10.1029/2018jb015768","title":"Frictional Mechanics of Slow Earthquakes","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Pennsylvania State University; National Science Foundation","keywords":"Slip (aerodynamics); Mechanics; Instability; Geology; Rheology; Slip line field; Episodic tremor and slip; Seismology; Physics; Tectonics; Subduction; Shear (geology); Petrology","score_opus":0.05153245529519993,"score_gpt":0.32499826954208794,"score_spread":0.273465814246888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888271949","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969283,0.00011064198,0.0017852812,0.000017002712,0.000003691539,0.000008037766,0.000038175054,0.000022086144,0.0010867948],"genre_scores_gemma":[0.99983823,0.000020045793,0.000053253036,0.0000015586396,6.775553e-7,0.0000017483876,0.000007207496,8.8321343e-7,0.00007638744],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.0000068626796,0.0000035056119,0.000011776595,0.000014381385,0.0000108136055],"domain_scores_gemma":[0.9998282,0.00004440782,0.000055986085,0.000023948227,0.00002127957,0.000026014703],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011219151,0.00016490436,0.00020778837,0.0003102867,0.0001579213,0.00030156795,0.00013897364,0.00014550528,0.0011888326],"category_scores_gemma":[0.0003783393,0.00010258587,0.000082784485,0.00008819176,0.0003660275,0.00018712749,0.00026766036,0.00015333005,0.00011311437],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054060214,0.0001938072,0.038027808,0.00016051758,0.00005450066,0.00079634215,0.00034104715,0.057601314,0.87650675,0.005067952,0.00042586727,0.020283422],"study_design_scores_gemma":[0.00011271504,0.0024855235,0.31817642,0.00003706028,0.000051363728,0.0010571531,0.00058036146,0.4762953,0.18546465,0.012027927,0.0036069588,0.000104511644],"about_ca_topic_score_codex":0.00044765542,"about_ca_topic_score_gemma":0.00030528253,"teacher_disagreement_score":0.0011888326,"about_ca_system_score_codex":0.00018789628,"about_ca_system_score_gemma":0.00009529334,"threshold_uncertainty_score":0.0039770603},"labels":[],"label_agreement":null},{"id":"W2889384767","doi":"","title":"Geomechanical Modelling of Induced Seismicity","year":2018,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology","score_opus":0.16642149467339204,"score_gpt":0.2883777457288724,"score_spread":0.12195625105548039,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889384767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.882725,0.00037595548,0.073250234,0.0008193803,0.00013826817,0.00015101273,0.002557065,0.00079920026,0.039183907],"genre_scores_gemma":[0.99314874,0.00014302389,0.0022053495,0.000032897628,0.000015863197,0.00005862701,0.0003095096,0.000043143016,0.0040427744],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989593,0.000025484953,0.0000073476363,0.000020901427,0.00002608436,0.000024155192],"domain_scores_gemma":[0.9998276,0.00006354417,0.000032322583,0.000017918055,0.000040532475,0.00001809334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012538832,0.0004812172,0.00030240085,0.00045491874,0.00030763246,0.00071016833,0.00082546205,0.0015429828,0.0036249356],"category_scores_gemma":[0.0006490685,0.00033641467,0.0005022608,0.000413129,0.00050129613,0.00044473103,0.00049424294,0.0006176555,0.00041002687],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013654969,0.00003124235,0.0013779764,0.000014632971,0.000012994569,0.00007064395,0.00002893493,0.9938141,0.0016143312,0.0016246574,0.00019952863,0.0011973139],"study_design_scores_gemma":[0.0000043532605,0.0000085649735,0.0007347714,0.000002035318,0.0000024712706,0.0000064293467,0.000011216648,0.9985972,0.00011036734,0.00028224333,0.00023712957,0.0000031896127],"about_ca_topic_score_codex":0.019979877,"about_ca_topic_score_gemma":0.011128917,"teacher_disagreement_score":0.019979877,"about_ca_system_score_codex":0.0007352816,"about_ca_system_score_gemma":0.00060027686,"threshold_uncertainty_score":0.03972715},"labels":[],"label_agreement":null},{"id":"W2890316842","doi":"10.1029/2018jb015638","title":"Smoothing of Fault Slip Surfaces by Scale‐Invariant Wear","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Geological Society of America","keywords":"Slip (aerodynamics); Geometry; Geology; Asperity (geotechnical engineering); Slip line field; Surface finish; Scaling; Smoothing; Surface roughness; Materials science; Geotechnical engineering; Shear (geology); Composite material; Petrology; Physics; Mathematics","score_opus":0.037766970490561505,"score_gpt":0.3202534218637282,"score_spread":0.2824864513731667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890316842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819916,0.000032057524,0.0014636825,0.0000054460347,0.0000010055866,0.000003440935,0.000058773723,0.000042085885,0.00019448163],"genre_scores_gemma":[0.9995223,0.000006833543,0.00036696254,9.541391e-7,7.830165e-7,0.0000012752093,0.000045765777,0.000004671186,0.000050351435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985886,0.000014481932,0.0000054534776,0.00004244207,0.00004833806,0.000030290408],"domain_scores_gemma":[0.9992987,0.00018413825,0.00023754226,0.000113716706,0.00012274501,0.00004323079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015637581,0.00014516257,0.00031017815,0.0011664819,0.00020504482,0.00041100997,0.00016989297,0.00015797687,0.00053756934],"category_scores_gemma":[0.0010264169,0.00019413872,0.00019179653,0.0005292181,0.0003633179,0.00023500023,0.00026209035,0.00013412272,0.00006422417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048611435,0.00012414051,0.51491123,0.00013385295,0.00018846092,0.0005474918,0.0009544103,0.033317856,0.39169073,0.00076580636,0.00064705656,0.056232825],"study_design_scores_gemma":[0.000004829147,0.000052296244,0.93655807,0.0000044269045,0.000013725405,0.00013482884,0.00012247084,0.052320875,0.010164664,0.0002865733,0.00031745105,0.00001977929],"about_ca_topic_score_codex":0.0022729512,"about_ca_topic_score_gemma":0.003248584,"teacher_disagreement_score":0.0022729512,"about_ca_system_score_codex":0.00032125428,"about_ca_system_score_gemma":0.000107649306,"threshold_uncertainty_score":0.0045194626},"labels":[],"label_agreement":null},{"id":"W2890617922","doi":"10.1029/2018jb016192","title":"Geometric Complexity of Earthquake Rupture Surfaces Preserved in Pseudotachylyte Networks","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; Niagara College; McGill University","funders":"","keywords":"Seismology; Geology; Sinistral and dextral; Earthquake rupture; Fault plane; Rake; Slip (aerodynamics); Shear (geology); Fault (geology); Rake angle; Seismic gap; Perpendicular; Geometry; Petrology; Engineering","score_opus":0.08782578788538091,"score_gpt":0.33472939956115694,"score_spread":0.246903611675776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890617922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983664,0.000029655788,0.0006339348,0.00001079289,6.3706995e-7,0.0000021363307,0.000110026696,0.000010967631,0.0008354771],"genre_scores_gemma":[0.9994574,0.000018460842,0.00022433231,0.0000015632119,0.0000017407668,0.0000020144334,0.00020050516,0.0000034190446,0.00009045512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998735,0.000018367498,0.000008468259,0.00004274658,0.000031050044,0.00002583879],"domain_scores_gemma":[0.99923,0.00021567274,0.00031156075,0.00006058982,0.00011261933,0.00006953471],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011818193,0.000096252734,0.00021959841,0.002123451,0.00023342812,0.0009841955,0.0002175716,0.00018644465,0.0017612409],"category_scores_gemma":[0.0013873787,0.00014645825,0.00010982263,0.0010448522,0.0005252956,0.0006042842,0.00054949726,0.00013720777,0.00017414751],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005795664,0.00007541412,0.8396455,0.00015272867,0.00012548151,0.0009412181,0.0016884586,0.028771583,0.07572586,0.010641661,0.00076122937,0.040891286],"study_design_scores_gemma":[0.000009258939,0.00006611966,0.96038735,0.000011075995,0.000018278966,0.000705958,0.0008436112,0.030821236,0.0021185358,0.003809969,0.0011937271,0.000014797605],"about_ca_topic_score_codex":0.0009758394,"about_ca_topic_score_gemma":0.0011177735,"teacher_disagreement_score":0.002123451,"about_ca_system_score_codex":0.00029032578,"about_ca_system_score_gemma":0.00008736459,"threshold_uncertainty_score":0.005891919},"labels":[],"label_agreement":null},{"id":"W2891752115","doi":"10.1190/segam2018-2996295.1","title":"Microseismic activity after 2+ years of CO2 injection at Quest","year":2018,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Shell (Canada)","funders":"","keywords":"Microseism; Environmental science; Computer science; Geology; Seismology","score_opus":0.010683326360369517,"score_gpt":0.21354695903594922,"score_spread":0.20286363267557972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891752115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98386467,0.000078540215,0.0010284075,0.00014825523,0.00008204909,0.00004369921,0.003893858,0.0002835247,0.010577],"genre_scores_gemma":[0.9930575,0.000037916165,0.00045013914,0.000033083183,0.000024022087,0.000014098658,0.003286817,0.00004192344,0.0030544403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980503,0.000012392719,0.0000072140365,0.000038670947,0.000091864036,0.00004473289],"domain_scores_gemma":[0.9995371,0.000052177336,0.000043835014,0.0000327686,0.00023015792,0.00010396096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029522524,0.00022730502,0.00029670974,0.0007248724,0.00043346558,0.0005385112,0.00021426557,0.00047604984,0.0022753964],"category_scores_gemma":[0.0005855751,0.00010735243,0.00016104257,0.0005183215,0.00023751726,0.00035537442,0.0004037097,0.0004968617,0.00086595095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004682069,0.0005761383,0.6450971,0.0003547174,0.00017484688,0.0038496521,0.0032332751,0.0075354986,0.19824429,0.0013711115,0.02262378,0.112257645],"study_design_scores_gemma":[0.000027444761,0.00039152274,0.9677663,0.00003406483,0.000025268328,0.00032774263,0.00054910517,0.005320303,0.015454679,0.00016343743,0.00989732,0.000042817912],"about_ca_topic_score_codex":0.009577086,"about_ca_topic_score_gemma":0.021526283,"teacher_disagreement_score":0.009577086,"about_ca_system_score_codex":0.00047077797,"about_ca_system_score_gemma":0.0003238379,"threshold_uncertainty_score":0.01904273},"labels":[],"label_agreement":null},{"id":"W2891832042","doi":"10.4138/atlgeol.2018.009","title":"Investigation of the 1727 Newbury, Massachusetts, USA, earthquake using LiDAR imagery and P-wave velocity tomography","year":2018,"lang":"en","type":"article","venue":"Atlantic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lineament; Geology; Fault scarp; Seismology; Ridge; Lidar; Fault (geology); Thrust fault; Volcano; Geomorphology; Tectonics; Remote sensing; Paleontology","score_opus":0.030068470648561788,"score_gpt":0.21441365913331512,"score_spread":0.18434518848475334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891832042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99320424,0.00024000254,0.0008053013,0.00015981199,0.00001135197,0.000041556665,0.0017873275,0.00006559615,0.0036848218],"genre_scores_gemma":[0.99369967,0.00028372052,0.0021184988,0.00006122262,0.000022675866,0.000033078788,0.0020992588,0.000010270597,0.0016717401],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999188,0.0000044166927,0.000003361107,0.000022402113,0.00003633656,0.000014652933],"domain_scores_gemma":[0.9997745,0.000017198026,0.000058777732,0.000012450054,0.0000991091,0.00003794176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011780152,0.00020841716,0.00011920895,0.00093094836,0.00050785654,0.00039851098,0.00037396903,0.00026997417,0.0011448201],"category_scores_gemma":[0.00041388444,0.00015238891,0.000104451115,0.0009783431,0.00018381944,0.00040638223,0.0003898628,0.00022919224,0.00028709925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093133625,0.00017369211,0.8332752,0.00013534911,0.00010901671,0.0032252998,0.0024905137,0.0021133623,0.08516118,0.00038242052,0.007031363,0.06580956],"study_design_scores_gemma":[0.000007805259,0.000026417922,0.9928463,0.000012035059,0.000013606513,0.0001269683,0.00064494374,0.0024058793,0.00094849005,0.000016494938,0.0029443149,0.000006650487],"about_ca_topic_score_codex":0.18876256,"about_ca_topic_score_gemma":0.572576,"teacher_disagreement_score":0.18876256,"about_ca_system_score_codex":0.0006600174,"about_ca_system_score_gemma":0.00068464817,"threshold_uncertainty_score":0.37532765},"labels":[],"label_agreement":null},{"id":"W2891876926","doi":"10.1016/j.epsl.2018.08.025","title":"Three-dimensional models of hydrothermal circulation through a seamount network on fast-spreading crust","year":2018,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Science Foundation","keywords":"Geology; Seafloor spreading; Outcrop; Hydrothermal circulation; Seamount; Petrology; Crust; Groundwater recharge; Mid-ocean ridge; Oceanic crust; Advection; Ridge; Geophysics; Geomorphology; Aquifer; Tectonics; Mantle (geology); Geochemistry; Subduction; Seismology; Groundwater; Paleontology","score_opus":0.02232965860635372,"score_gpt":0.20873922851758164,"score_spread":0.18640956991122792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891876926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9893199,0.00011440162,0.0036063422,0.0004752504,0.000030136542,0.000018865729,0.0005700389,0.00015739661,0.0057076104],"genre_scores_gemma":[0.99743503,0.000086151784,0.00067490747,0.000029522382,0.000012680174,0.000015569018,0.00018037389,0.000023566448,0.0015421923],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998925,0.000030680574,0.000008123064,0.000028455486,0.000010099854,0.000030181707],"domain_scores_gemma":[0.9994844,0.00017569622,0.00006688918,0.000049726877,0.00006168141,0.00016153694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027674276,0.0005005818,0.0006444028,0.0005922836,0.0009957781,0.0016792343,0.001907054,0.002498271,0.0046799053],"category_scores_gemma":[0.0017639608,0.0007812544,0.0009820889,0.0009431281,0.0015188573,0.0011430068,0.0010917006,0.00094639417,0.0003007356],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005211995,0.000025444464,0.0028385934,0.000006412126,0.000020833084,0.000055651133,0.00004632706,0.99504906,0.000251645,0.0011803027,0.000108412045,0.000365265],"study_design_scores_gemma":[0.000039415158,0.000010993724,0.0014406216,0.0000033175684,0.000010589412,0.0000048551406,0.000035376695,0.99776447,0.00003234966,0.00055696693,0.00009197755,0.000009086406],"about_ca_topic_score_codex":0.2036306,"about_ca_topic_score_gemma":0.07585649,"teacher_disagreement_score":0.2036306,"about_ca_system_score_codex":0.0023555558,"about_ca_system_score_gemma":0.0018957423,"threshold_uncertainty_score":0.40489066},"labels":[],"label_agreement":null},{"id":"W2892595513","doi":"10.1130/b31922.1","title":"Evidence for deep crustal seismic rupture in a granulite-facies, intraplate, strike-slip shear zone, northern Saskatchewan, Canada","year":2018,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Granulite; Intraplate earthquake; Shear zone; Facies; Seismology; Geomorphology; Structural basin; Tectonics","score_opus":0.02012370338439578,"score_gpt":0.2193386424973786,"score_spread":0.19921493911298283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892595513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8597078,0.0060443035,0.0004347999,0.0032716654,0.00009812327,0.00014240084,0.03983821,0.00016130527,0.09030149],"genre_scores_gemma":[0.9483463,0.008024632,0.0007776619,0.0006606707,0.000028676393,0.000041311418,0.020716026,0.000054930206,0.021349708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996624,0.000014673531,0.000033315635,0.000048074955,0.00016736673,0.00007423469],"domain_scores_gemma":[0.997783,0.00020303934,0.0003018741,0.00013574104,0.0012283125,0.0003479596],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004135719,0.00030676878,0.00027642658,0.0033964687,0.0017206242,0.0013760319,0.00076111616,0.0005219834,0.005211815],"category_scores_gemma":[0.0014461874,0.00025706453,0.00024663017,0.009826445,0.0009925985,0.0004899748,0.0014288519,0.00044775868,0.0011944848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002890083,0.000051392846,0.85408306,0.0006053632,0.00020966813,0.0020197756,0.004893464,0.0006833396,0.005460967,0.0014468135,0.04429947,0.08595782],"study_design_scores_gemma":[0.000017313603,0.000011035928,0.9778211,0.00021421134,0.000036257818,0.0001619585,0.004242422,0.00018494671,0.00040081557,0.00015557047,0.016722912,0.00003147713],"about_ca_topic_score_codex":0.9760296,"about_ca_topic_score_gemma":0.99546343,"teacher_disagreement_score":0.023970425,"about_ca_system_score_codex":0.008614738,"about_ca_system_score_gemma":0.021444684,"threshold_uncertainty_score":0.06250459},"labels":[],"label_agreement":null},{"id":"W2893505985","doi":"10.1007/s00024-018-1996-5","title":"Source Models of the 2012 Haida Gwaii (Canada) and 2015 Illapel (Chile) Earthquakes and Numerical Simulations of Related Tsunamis","year":2018,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Seismology; Geology","score_opus":0.008045669674031487,"score_gpt":0.18514541284476085,"score_spread":0.17709974317072938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2893505985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6890161,0.0007227774,0.00921717,0.003424561,0.0005106653,0.00038008118,0.20593904,0.0028264946,0.087963104],"genre_scores_gemma":[0.9299553,0.00071850227,0.0028474964,0.00018286624,0.00004883481,0.00031266248,0.04307459,0.00037283887,0.022486772],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980146,0.000021292783,0.000014603267,0.000041516618,0.000053641714,0.00006744991],"domain_scores_gemma":[0.9989705,0.0001592822,0.00009446567,0.000050466086,0.00060449354,0.00012084372],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024147211,0.0009176523,0.0008432218,0.0018069114,0.0011577554,0.0017357286,0.003860042,0.0023378236,0.013306379],"category_scores_gemma":[0.00196062,0.00093790825,0.0007721749,0.0038732619,0.00076350913,0.001008456,0.00079603447,0.0016744375,0.0018949251],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016090952,0.00011934403,0.0078100264,0.00014052886,0.00006452203,0.00012983415,0.00018928775,0.9693225,0.00068625435,0.0043949606,0.013656762,0.0033250225],"study_design_scores_gemma":[0.00045969972,0.000038012353,0.015369068,0.000059996382,0.00007022187,0.000059463448,0.0004871043,0.9695416,0.0010620243,0.0016323755,0.011082325,0.00013813381],"about_ca_topic_score_codex":0.9356467,"about_ca_topic_score_gemma":0.8990979,"teacher_disagreement_score":0.06435329,"about_ca_system_score_codex":0.013493248,"about_ca_system_score_gemma":0.015303457,"threshold_uncertainty_score":0.1294645},"labels":[],"label_agreement":null},{"id":"W2894343555","doi":"","title":"Magnitude 3.8 earthquake in Lake Ontario, 4 August 2004 : kinematic and dynamic parameters","year":2005,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magnitude (astronomy); Geology; Earthquake magnitude; Kinematics; Seismology; Geometry; Mathematics; Physics","score_opus":0.04854600401542678,"score_gpt":0.29250261335163813,"score_spread":0.24395660933621136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2894343555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992176,0.000087953646,0.00009265857,0.0003020074,0.0000059816284,0.0000144835985,0.003355505,0.000015550968,0.003949843],"genre_scores_gemma":[0.9949214,0.00006735209,0.0000832608,0.00002613798,0.000005659234,0.0000066712414,0.0017791124,0.0000059135496,0.0031045335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998741,0.0000063691555,0.0000075055077,0.000018979075,0.000051020903,0.0000419843],"domain_scores_gemma":[0.9994216,0.000039420873,0.00014469477,0.000016458192,0.00028383732,0.000094154246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017180991,0.00022703642,0.00026315727,0.00080529973,0.0019260801,0.00095060776,0.00072471215,0.0005512809,0.002353252],"category_scores_gemma":[0.0014645731,0.00033116684,0.00020467486,0.0017983665,0.00062174053,0.00054864737,0.00061342336,0.00037056176,0.00037458757],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002787465,0.000051398107,0.97850466,0.000052702755,0.000078785444,0.00055836514,0.0019728884,0.0036398019,0.0019708236,0.00042995787,0.0056309286,0.006831011],"study_design_scores_gemma":[0.000010183791,0.000009512827,0.9966846,0.0000059244203,0.00001579916,0.000032921245,0.0007069145,0.0011652971,0.00007366913,0.000031442236,0.0012570821,0.0000066266566],"about_ca_topic_score_codex":0.9846089,"about_ca_topic_score_gemma":0.9955253,"teacher_disagreement_score":0.015391111,"about_ca_system_score_codex":0.012308105,"about_ca_system_score_gemma":0.009568763,"threshold_uncertainty_score":0.089302},"labels":[],"label_agreement":null},{"id":"W2895831433","doi":"10.1029/2018gl079288","title":"Induced Seismicity in Western Canada Linked to Tectonic Strain Rate: Implications for Regional Seismic Hazard","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; Geoscience BC; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Seismology; Seismic hazard; Tectonics; Strain rate; Foothills; Seismic moment; Fault (geology); Geography; Cartography","score_opus":0.077273001913778,"score_gpt":0.32394754289259886,"score_spread":0.24667454097882086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895831433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99769694,0.00014180061,0.00006144744,0.00009680139,0.0000016287626,0.000006505744,0.0006994044,0.000006544899,0.0012888937],"genre_scores_gemma":[0.99931526,0.0000880107,0.000045429886,0.000016391312,0.0000010784253,0.0000017705082,0.0002259874,0.0000015231922,0.00030463425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981683,0.000012528872,0.000009488384,0.0000316072,0.000043061904,0.00008652212],"domain_scores_gemma":[0.9991123,0.00007076709,0.00018727082,0.000021211752,0.0003757031,0.0002327953],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018529358,0.00020190427,0.00020530737,0.001155631,0.00071553275,0.0007417183,0.00035001923,0.00017908806,0.0016641881],"category_scores_gemma":[0.0009642315,0.00010103798,0.00015966251,0.0019744958,0.0005463072,0.00014984155,0.0004713264,0.0002327008,0.00009001373],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006124146,0.00001602601,0.9934569,0.000014962094,0.000034126046,0.00009854699,0.0002892521,0.00047679417,0.0010376761,0.00008767542,0.0002493794,0.00417752],"study_design_scores_gemma":[0.000001543745,0.0000049031632,0.9990095,0.0000050326817,0.0000068747418,0.000016334916,0.0004675161,0.00023412697,0.00006691187,0.0000129954415,0.00017127788,0.0000029089397],"about_ca_topic_score_codex":0.9859139,"about_ca_topic_score_gemma":0.99104816,"teacher_disagreement_score":0.014086127,"about_ca_system_score_codex":0.008366338,"about_ca_system_score_gemma":0.007055676,"threshold_uncertainty_score":0.060702264},"labels":[],"label_agreement":null},{"id":"W2896395469","doi":"10.1029/2018jb016240","title":"Renewed Posteruptive Uplift Following the 2011–2012 Rhyolitic Eruption of Cordón Caulle (Southern Andes, Chile): Evidence for Transient Episodes of Magma Reservoir Recharge During 2012–2018","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Sill; Magma; Volcano; Interferometric synthetic aperture radar; Seismology; Induced seismicity; Petrology; Synthetic aperture radar","score_opus":0.09905648980286537,"score_gpt":0.3632131987235892,"score_spread":0.26415670892072385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896395469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985226,0.00010312668,0.000042950007,0.000053697346,0.000005753024,0.0000048867396,0.00028737856,0.000018828501,0.0009608756],"genre_scores_gemma":[0.9994523,0.00004720114,0.000038983097,0.000011087466,0.000009933454,0.0000042765155,0.00027346064,0.000003889492,0.00015894375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999093,0.000005576752,0.000006763049,0.00003134709,0.000017614568,0.00002939388],"domain_scores_gemma":[0.99952257,0.000059841852,0.00018340845,0.000035816724,0.00011643318,0.00008198967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024481775,0.00021123099,0.00019969484,0.0008469958,0.00043844015,0.00055422995,0.00040420145,0.00043660213,0.0014279208],"category_scores_gemma":[0.0007961763,0.0001489586,0.0001814797,0.00060722284,0.00035756038,0.00030497304,0.0004675631,0.00028162537,0.00022363332],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029346207,0.000058720692,0.9714239,0.000093353665,0.000077584526,0.00093540235,0.0009332403,0.00056945015,0.015620162,0.000092691604,0.0006716713,0.009230364],"study_design_scores_gemma":[0.0000035249498,0.0000107026,0.99877125,0.000005672638,0.000009355329,0.000042273245,0.00015602063,0.00050169276,0.00021360094,0.000009727724,0.00027314818,0.0000031331408],"about_ca_topic_score_codex":0.051692057,"about_ca_topic_score_gemma":0.055878058,"teacher_disagreement_score":0.051692057,"about_ca_system_score_codex":0.0008219727,"about_ca_system_score_gemma":0.00046982645,"threshold_uncertainty_score":0.10278237},"labels":[],"label_agreement":null},{"id":"W2896536555","doi":"10.1190/geo2018-0076.1","title":"Passive seismic tomography using recorded microseismicity: Application to mining-induced seismicity","year":2018,"lang":"en","type":"article","venue":"Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Microseismic Industry Consortium","keywords":"Geology; Seismology; Microseism; Induced seismicity; Tomography; Borehole; Seismic tomography; Hypocenter; Earthquake location; Fault (geology); Geodesy; Geophysics; Geotechnical engineering; Mantle (geology)","score_opus":0.019323595203708417,"score_gpt":0.2375572390226195,"score_spread":0.21823364381891108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896536555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8590647,0.000073984265,0.13904722,0.00007026273,0.0000095111845,0.000055227323,0.0004081716,0.00043054362,0.0008403729],"genre_scores_gemma":[0.97277,0.000047329773,0.026888696,0.0000050771846,0.00000740365,0.000015021467,0.00014533038,0.000015051997,0.00010612874],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999207,0.00001989747,0.000006510806,0.000022361044,0.0000218142,0.000008635449],"domain_scores_gemma":[0.9996847,0.0001368043,0.000066120876,0.000029544924,0.000056608304,0.000026257032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019303749,0.00037174195,0.00017316909,0.00065616396,0.0001027875,0.000317408,0.0003685717,0.0002437745,0.00046119877],"category_scores_gemma":[0.0011949679,0.0002038174,0.00019765543,0.0009905499,0.00017218202,0.00031223515,0.00035106222,0.00015608649,0.00007687138],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006377614,0.00038176883,0.20350921,0.00025869664,0.000118953416,0.0013384685,0.00053321593,0.33721447,0.25107074,0.0019164727,0.0005642114,0.202456],"study_design_scores_gemma":[0.00003165114,0.00012876348,0.0664131,0.000008822493,0.000023652901,0.00026387512,0.00010104284,0.9162949,0.015568425,0.00071720727,0.00042898732,0.0000196044],"about_ca_topic_score_codex":0.0026054918,"about_ca_topic_score_gemma":0.0025651995,"teacher_disagreement_score":0.0026054918,"about_ca_system_score_codex":0.00018447771,"about_ca_system_score_gemma":0.0002894237,"threshold_uncertainty_score":0.005180657},"labels":[],"label_agreement":null},{"id":"W2897046153","doi":"10.1073/pnas.1807549115","title":"Faults and associated karst collapse suggest conduits for fluid flow that influence hydraulic fracturing-induced seismicity","year":2018,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"MacEwan University; Alberta Energy","funders":"","keywords":"Geology; Induced seismicity; Seismology; Hydraulic fracturing; Karst; Fault (geology); Tectonics; Geotechnical engineering; Paleontology","score_opus":0.04291045379401412,"score_gpt":0.27631172930957204,"score_spread":0.23340127551555792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897046153","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880683,0.00002884422,0.00023727686,0.000021677994,9.220745e-7,0.000003841754,0.000046347137,0.000015592079,0.00083864544],"genre_scores_gemma":[0.9998288,0.000014804218,0.00006447903,0.000002493228,5.038147e-7,4.5419475e-7,0.000021685404,6.6159794e-7,0.00006614019],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992704,0.000008069866,0.000004697523,0.000012789411,0.000015554806,0.000031904063],"domain_scores_gemma":[0.9997465,0.00003883384,0.00011432835,0.000012029762,0.000042760636,0.000045586927],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009789895,0.00015748551,0.00013231473,0.0008268688,0.00035337964,0.0008012006,0.00022265803,0.00025622107,0.0011973076],"category_scores_gemma":[0.00066714914,0.00015613057,0.0000799958,0.00062513154,0.0008148615,0.00028738458,0.00038464172,0.00013661454,0.000092268085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017745188,0.000045447716,0.9466945,0.0000394665,0.000024514657,0.00067276065,0.0007922829,0.0024922267,0.038273692,0.0006844959,0.00014979545,0.0099534225],"study_design_scores_gemma":[0.0000031890793,0.000018088398,0.9974595,0.000003194595,0.000006131806,0.000056676607,0.0004654567,0.0012502217,0.00052070443,0.00009965892,0.0001141419,0.0000031497948],"about_ca_topic_score_codex":0.065268144,"about_ca_topic_score_gemma":0.12992784,"teacher_disagreement_score":0.065268144,"about_ca_system_score_codex":0.0007909513,"about_ca_system_score_gemma":0.0007668414,"threshold_uncertainty_score":0.12977654},"labels":[],"label_agreement":null},{"id":"W2897215218","doi":"10.1029/2018gl079519","title":"A Lack of Dynamic Triggering of Slow Slip and Tremor Indicates That the Shallow Cascadia Megathrust Offshore Vancouver Island Is Likely Locked","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada","funders":"W. M. Keck Foundation; National Science Foundation","keywords":"Geology; Subduction; Seismology; Episodic tremor and slip; Trench; Submarine pipeline; Seafloor spreading; Slip (aerodynamics); Borehole; Tectonics; Geotechnical engineering; Geophysics","score_opus":0.05126037502936796,"score_gpt":0.2986008548861235,"score_spread":0.2473404798567555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897215218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99686474,0.000019698831,0.000126103,0.000025024689,0.0000021581427,0.0000059024737,0.00019017648,0.000013027648,0.002753173],"genre_scores_gemma":[0.9990833,0.000020407617,0.000069593494,0.000008238436,7.5171107e-7,0.0000027271335,0.00018124231,0.0000017772861,0.00063211686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.000005306793,0.000006086856,0.00002099636,0.000032394342,0.000032812444],"domain_scores_gemma":[0.99943155,0.000044442557,0.00016130072,0.00006212497,0.00012244553,0.00017800689],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007618191,0.00017097383,0.00014947666,0.00039073385,0.0005364944,0.0005139092,0.0002644309,0.00021030997,0.0026237036],"category_scores_gemma":[0.0004889493,0.00019241252,0.00008741526,0.0004724595,0.00037626878,0.00019930149,0.00042197376,0.00021300714,0.00025189188],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001906842,0.000046553472,0.88333976,0.000056717825,0.00003853876,0.0008404039,0.0005121842,0.0005822354,0.105891205,0.00015733301,0.0003037637,0.008040632],"study_design_scores_gemma":[0.0000027971064,0.000035752528,0.9975809,0.0000031185323,0.0000037982788,0.00009682245,0.00020741261,0.00020949081,0.0015047584,0.000023282062,0.0003302215,0.0000016155914],"about_ca_topic_score_codex":0.11007683,"about_ca_topic_score_gemma":0.33032924,"teacher_disagreement_score":0.88992316,"about_ca_system_score_codex":0.0009763365,"about_ca_system_score_gemma":0.00065279286,"threshold_uncertainty_score":0.21887225},"labels":[],"label_agreement":null},{"id":"W2897529245","doi":"10.1029/2018gl078711","title":"Holocene Surface Rupture History of an Active Forearc Fault Redefines Seismic Hazard in Southwestern British Columbia, Canada","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Shared Services Canada; University of Victoria","funders":"Washington State University; Northwestern University; National Science Foundation","keywords":"Forearc; Geology; Seismology; Quaternary; Seismic hazard; Holocene; Induced seismicity; Active fault; Subduction; Fault scarp; Fault (geology); Tectonics; Paleontology","score_opus":0.02517472811469667,"score_gpt":0.24661081151124342,"score_spread":0.22143608339654675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897529245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99120164,0.00041226298,0.00011656774,0.00022145429,0.0000068363943,0.00001277477,0.0031290567,0.000019438983,0.004879958],"genre_scores_gemma":[0.996033,0.00029233017,0.00015665253,0.0000411498,0.0000019806,0.0000058686323,0.0013220275,0.0000060143266,0.002140985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998318,0.000008781304,0.0000089395835,0.00003637702,0.00004540727,0.00006867542],"domain_scores_gemma":[0.99885535,0.00006367046,0.00012007783,0.000032344007,0.0007228079,0.00020581987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017731839,0.0002213039,0.00019052974,0.001853819,0.0021306968,0.001162741,0.00065974635,0.00032355243,0.0033264],"category_scores_gemma":[0.00083634217,0.0002013959,0.00011704093,0.0029805126,0.00051586324,0.000278306,0.00049787696,0.0004076421,0.00033693627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005807015,0.000027117132,0.96791774,0.000040740142,0.000040964358,0.00029798696,0.0020063668,0.00084550254,0.0014495285,0.00013166164,0.0033313842,0.023852982],"study_design_scores_gemma":[0.000001923328,0.0000038645135,0.9962437,0.000020997824,0.000008147438,0.000032679105,0.0015989995,0.0003070707,0.00011082909,0.000015508316,0.0016503135,0.0000059729364],"about_ca_topic_score_codex":0.9952571,"about_ca_topic_score_gemma":0.9990833,"teacher_disagreement_score":0.016380368,"about_ca_system_score_codex":0.016380368,"about_ca_system_score_gemma":0.010508753,"threshold_uncertainty_score":0.11884844},"labels":[],"label_agreement":null},{"id":"W2898952250","doi":"10.22059/geope.2018.255122.648378","title":"Coastal foraminifera from the Iranian coast of Makran, Oman Sea (Chabahar Bay to Gawater Bay) as an indicator of tsunamis","year":2019,"lang":"en","type":"article","venue":"Geopersia","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Foraminifera; Oceanography; Geology; Bay; Intertidal zone; Overwash; Provenance; Supralittoral zone; Paleontology; Barrier island; Shore","score_opus":0.010524267450133852,"score_gpt":0.20753696255827578,"score_spread":0.19701269510814193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898952250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995472,0.000053041917,0.00002269608,0.000008365888,0.0000016470487,0.0000032535677,0.00009081159,0.000002242455,0.0002707294],"genre_scores_gemma":[0.99935704,0.00007566503,0.00018420117,0.000004741307,0.0000028557372,0.0000076473425,0.00018888255,6.3480405e-7,0.0001783649],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999905,0.000009261282,0.0000140870925,0.000018398106,0.00002720916,0.000026098432],"domain_scores_gemma":[0.99979156,0.000017109047,0.00010340535,0.000012786495,0.000051767136,0.000023374436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001547616,0.0004567898,0.000119701035,0.0016512241,0.0006684204,0.00039088994,0.0001669623,0.00019156588,0.0007525234],"category_scores_gemma":[0.00034777093,0.00011667788,0.00011472325,0.0012407433,0.00027484717,0.00021730913,0.00046729328,0.0001494403,0.00011883568],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040657324,0.000017134153,0.9878144,0.000023368942,0.000014505403,0.00016376466,0.0009345866,0.000055538378,0.0033504474,0.000042746404,0.00015105408,0.007391666],"study_design_scores_gemma":[0.0000011579407,0.000013327364,0.99900466,0.0000021914418,0.0000034184052,0.00005773171,0.0005618021,0.00003341953,0.00014176783,0.000008947253,0.00017054717,0.0000010506834],"about_ca_topic_score_codex":0.017536337,"about_ca_topic_score_gemma":0.054712374,"teacher_disagreement_score":0.017536337,"about_ca_system_score_codex":0.0003352146,"about_ca_system_score_gemma":0.00035542302,"threshold_uncertainty_score":0.03486854},"labels":[],"label_agreement":null},{"id":"W2899331492","doi":"10.1785/0220180041","title":"Monitoring for Potentially Induced Seismicity in the St. Lawrence Valley of Quebec, Canada, during the Hydraulic Fracturing Operations of 2006–2010","year":2018,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Induced seismicity; Citation; Icon; Library science; Download; History; Hydraulic fracturing; Archaeology; Geology; Seismology; Computer science; World Wide Web; Paleontology","score_opus":0.06453049528397166,"score_gpt":0.3002220385790119,"score_spread":0.23569154329504027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899331492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81481534,0.006071945,0.0010657789,0.0060376283,0.00019691966,0.00040801906,0.10574114,0.00028839658,0.06537491],"genre_scores_gemma":[0.94898427,0.0032916714,0.0012137374,0.00066304347,0.000048257334,0.00012040891,0.022190735,0.000052934494,0.023434952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933004,0.000031483414,0.000027478165,0.00007169102,0.00033212567,0.00020710882],"domain_scores_gemma":[0.9959765,0.00016559911,0.0003870587,0.00005159695,0.0028382551,0.0005809686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041101917,0.00042939713,0.00028338336,0.001842055,0.0026620608,0.0011850726,0.0014041188,0.00052802096,0.0043130578],"category_scores_gemma":[0.00197682,0.00021569322,0.0002321614,0.004042226,0.0006617511,0.00042294047,0.0008341109,0.00061217404,0.0007277116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002336781,0.00008204712,0.7703206,0.0005693526,0.00018290966,0.00068195956,0.0059861112,0.0017612972,0.0027883425,0.0007513588,0.13506778,0.08157459],"study_design_scores_gemma":[0.0000102992,0.000022383383,0.977038,0.00015191494,0.000022183624,0.000051438914,0.0036393704,0.0004949614,0.00023123738,0.000031066324,0.018277375,0.000029784105],"about_ca_topic_score_codex":0.9981949,"about_ca_topic_score_gemma":0.9995425,"teacher_disagreement_score":0.037012804,"about_ca_system_score_codex":0.037012804,"about_ca_system_score_gemma":0.05857284,"threshold_uncertainty_score":0.2685479},"labels":[],"label_agreement":null},{"id":"W2899333328","doi":"10.1093/gji/ggy450","title":"Thermal Regime of the Northern Hikurangi Margin, New Zealand","year":2018,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Subduction; Seafloor spreading; Oceanic crust; Seismology; Bathymetry; Crust; Geophysics; Geomorphology; Tectonics; Oceanography","score_opus":0.011481696847831364,"score_gpt":0.21644771605058027,"score_spread":0.2049660192027489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899333328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992551,0.000026880864,0.000060658007,0.0000064373758,6.991061e-7,0.0000029071116,0.00009689758,0.0000039130696,0.0005464145],"genre_scores_gemma":[0.99945825,0.00004331367,0.00012482936,0.0000040093855,9.3450967e-7,0.0000056912736,0.00013219749,0.0000019758627,0.0002287492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992716,0.0000035578205,0.0000060434804,0.000029641962,0.000017850045,0.000015638072],"domain_scores_gemma":[0.99989486,0.000009761766,0.00003880928,0.000009865246,0.000024568826,0.000022106324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010597962,0.00022939338,0.00020102333,0.0004543255,0.0005174983,0.00057589414,0.0002755782,0.00020996417,0.00086798676],"category_scores_gemma":[0.00033704308,0.00021971924,0.00020523454,0.0004027821,0.00066721847,0.00032368727,0.0004482795,0.00017087377,0.00016259355],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035040674,0.000048203972,0.8942598,0.00012284666,0.00008667362,0.0006433716,0.003741188,0.0043916893,0.07748984,0.0001918381,0.00021116908,0.01846293],"study_design_scores_gemma":[0.0000062178747,0.0000232034,0.99784946,0.0000049525775,0.000010960939,0.00007640669,0.00030045924,0.0009424873,0.00041535147,0.00001578521,0.00034805815,0.0000066702078],"about_ca_topic_score_codex":0.21658218,"about_ca_topic_score_gemma":0.2999223,"teacher_disagreement_score":0.21658218,"about_ca_system_score_codex":0.0010455413,"about_ca_system_score_gemma":0.00048865646,"threshold_uncertainty_score":0.43064308},"labels":[],"label_agreement":null},{"id":"W2899534590","doi":"10.1029/2018gc007851","title":"Initiation of Strike‐Slip Faults, Serpentinization, and Methane: The Nootka Fault Zone, the Juan de Fuca‐Explorer Plate Boundary","year":2018,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seafloor spreading; Transform fault; Seismology; Shear zone; Fault (geology); Trench; Echelon formation; Shear (geology); Strike-slip tectonics; Ridge; Detachment fault; Petrology; Tectonics; Extensional definition; Geophysics; Paleontology","score_opus":0.012926097495438884,"score_gpt":0.2175080505121144,"score_spread":0.2045819530166755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899534590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99942625,0.00009462655,0.00001449802,0.000009352595,5.975824e-7,7.548726e-7,0.000053959895,0.0000017358122,0.0003981268],"genre_scores_gemma":[0.999783,0.000032379634,0.000024114763,0.0000017281038,6.253492e-7,7.3039223e-7,0.000054199987,6.4555815e-7,0.00010259791],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993074,0.000006141385,0.000004409389,0.000019916997,0.000010829488,0.000027907638],"domain_scores_gemma":[0.99977,0.000030495676,0.00010339089,0.000014404189,0.0000308064,0.00005090978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014993787,0.000109355606,0.00015553011,0.0006082142,0.00039754648,0.00046239945,0.00016443174,0.00028107924,0.0009103692],"category_scores_gemma":[0.00043746782,0.00011848851,0.00010187629,0.0003341362,0.00042822273,0.00019897736,0.00040518618,0.00010205179,0.00011468902],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021127325,0.000013649786,0.97478527,0.00004655824,0.000040318475,0.00030124187,0.0007574296,0.00060979143,0.018370407,0.00018669905,0.00006421993,0.004613143],"study_design_scores_gemma":[0.0000013059913,0.0000074011177,0.99933225,0.0000040896757,0.0000032383327,0.000031543954,0.00012449254,0.00013445443,0.00020131962,0.000014356885,0.00014390491,0.0000016054992],"about_ca_topic_score_codex":0.04231262,"about_ca_topic_score_gemma":0.072034135,"teacher_disagreement_score":0.04231262,"about_ca_system_score_codex":0.00072758226,"about_ca_system_score_gemma":0.00033830747,"threshold_uncertainty_score":0.08413267},"labels":[],"label_agreement":null},{"id":"W2899619037","doi":"10.1029/2018gl079382","title":"Earthquake Stress Drop in the Charlevoix Seismic Zone, Eastern Canada","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Intraplate earthquake; Geology; Seismology; Induced seismicity; Crust; Scaling; Drop (telecommunication); Geophysics; Tectonics; Geometry","score_opus":0.031706644885183675,"score_gpt":0.2686663522198223,"score_spread":0.23695970733463864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899619037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970282,0.000103878374,0.000071913906,0.000028127775,0.0000016010675,0.000008199854,0.0014301435,0.000013838157,0.0013142144],"genre_scores_gemma":[0.99765885,0.00007998841,0.00012319004,0.000011380397,0.000001331169,0.0000055626515,0.0012712325,0.0000031479647,0.0008453461],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997701,0.0000074772797,0.00001138732,0.000042707037,0.000088083514,0.00008025329],"domain_scores_gemma":[0.9992957,0.000036373538,0.00010816023,0.000024781473,0.0003849008,0.00015007755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019725045,0.0003036304,0.00021925948,0.0022648845,0.0010216249,0.00084747165,0.00052842195,0.00021295677,0.0010444028],"category_scores_gemma":[0.000657586,0.00014918005,0.00015413643,0.0027608566,0.0005166592,0.00018770595,0.0006952977,0.00022355316,0.0001371034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000120888915,0.000021106747,0.9823647,0.000038463342,0.000049567218,0.00020312578,0.00076670636,0.0014756556,0.0026367814,0.00013845452,0.00076159864,0.011422912],"study_design_scores_gemma":[0.0000018720742,0.000004377071,0.99863213,0.000004631427,0.0000031314528,0.000015262012,0.00033724855,0.00043669538,0.00016664887,0.000006549878,0.00038823977,0.0000032010907],"about_ca_topic_score_codex":0.9821618,"about_ca_topic_score_gemma":0.99207664,"teacher_disagreement_score":0.01783818,"about_ca_system_score_codex":0.0109593235,"about_ca_system_score_gemma":0.007005779,"threshold_uncertainty_score":0.079515874},"labels":[],"label_agreement":null},{"id":"W2900221079","doi":"10.1785/0220180264","title":"Accurate Determination of Local Magnitude for Earthquakes in the Western Canada Sedimentary Basin","year":2018,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Geoscience BC","funders":"","keywords":"Icon; Citation; Magnitude (astronomy); Geology; Download; Geological survey; Sedimentary rock; Structural basin; Library science; History; Archaeology; Geography; Paleontology; Computer science; World Wide Web; Physics","score_opus":0.07242349946980217,"score_gpt":0.3231870827005821,"score_spread":0.25076358323077996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900221079","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.31128973,0.017717527,0.026425423,0.011043161,0.001396479,0.0008017095,0.20581922,0.005256583,0.4202501],"genre_scores_gemma":[0.7733015,0.012032837,0.029313968,0.0006328417,0.0002877269,0.00027145055,0.074416816,0.0011717849,0.1085712],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9993981,0.000027166283,0.000049462695,0.000043476808,0.00038762472,0.00009415535],"domain_scores_gemma":[0.99684024,0.00013998913,0.00023676339,0.00011840072,0.0024198266,0.00024482317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053163024,0.00039769997,0.0003648585,0.0062065953,0.001017265,0.001561822,0.0006324997,0.00029121258,0.015395078],"category_scores_gemma":[0.0054722554,0.00022265421,0.00016802388,0.0062175407,0.00028939915,0.00079058175,0.001032026,0.000517269,0.00707787],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014210773,0.000033789423,0.2082595,0.0007001459,0.00007229835,0.0005398039,0.0019177393,0.0029896402,0.003899925,0.0024915403,0.35796177,0.42099178],"study_design_scores_gemma":[0.000022052343,0.000022422955,0.79701716,0.0005414012,0.000046408833,0.00013647719,0.00303548,0.0028928518,0.0017898234,0.0011576711,0.19326724,0.00007111364],"about_ca_topic_score_codex":0.8943313,"about_ca_topic_score_gemma":0.96574134,"teacher_disagreement_score":0.10566872,"about_ca_system_score_codex":0.0061354833,"about_ca_system_score_gemma":0.009645839,"threshold_uncertainty_score":0.21258199},"labels":[],"label_agreement":null},{"id":"W2900463962","doi":"10.4095/297444","title":"Ground deformation produced by 2014 Iquique earthquake mapped with RADARSAT-2 DInSAR","year":2015,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Deformation (meteorology); Geodesy; Geography; Oceanography","score_opus":0.03054856118620768,"score_gpt":0.23614414693219235,"score_spread":0.20559558574598466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900463962","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90862256,0.00012767191,0.000783305,0.00021701265,0.00018539891,0.00010668822,0.07377561,0.00024562838,0.015936034],"genre_scores_gemma":[0.81656766,0.0003171413,0.003648471,0.00010422148,0.00013468893,0.00012859637,0.1628813,0.00007244446,0.016145457],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99965596,0.000028467995,0.000022607728,0.00007261402,0.00014041949,0.00007998161],"domain_scores_gemma":[0.9991091,0.000053231357,0.00011356488,0.000093480616,0.00054749916,0.00008307459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004909077,0.00060945214,0.00038864755,0.0017837937,0.0005995427,0.00047507745,0.0005974205,0.0006712612,0.0023156428],"category_scores_gemma":[0.0009270245,0.00027449863,0.00033001963,0.0021703257,0.0001660521,0.00049922965,0.0004963289,0.00042588255,0.0011378808],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017765978,0.0011349901,0.7790456,0.0004453791,0.00054411223,0.0013234057,0.00097638136,0.020763583,0.021743162,0.0010562214,0.10502944,0.06616117],"study_design_scores_gemma":[0.000042622774,0.00007213727,0.98521775,0.000019560559,0.000036918605,0.00007547343,0.00032662612,0.0031668576,0.0013399457,0.00003893667,0.009644692,0.000018544024],"about_ca_topic_score_codex":0.20904185,"about_ca_topic_score_gemma":0.32786652,"teacher_disagreement_score":0.20904185,"about_ca_system_score_codex":0.0012770747,"about_ca_system_score_gemma":0.0015924915,"threshold_uncertainty_score":0.41565013},"labels":[],"label_agreement":null},{"id":"W2900518277","doi":"10.1093/gji/ggy497","title":"Source parameters of the 2017<i>M</i>w 6.2 Yukon earthquake doublet inferred from coseismic GPS and ALOS-2 deformation measurements","year":2018,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Geodesy; Global Positioning System; Interferometry; Thrust fault; Inversion (geology); Subpixel rendering; Fault (geology); Slip (aerodynamics); Synthetic aperture radar; Remote sensing; Tectonics; Pixel","score_opus":0.03508760470564516,"score_gpt":0.23681764515887255,"score_spread":0.2017300404532274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900518277","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99823076,0.00003551221,0.00020074993,0.00002378935,0.0000035886792,0.000006132183,0.0010813589,0.000031747688,0.0003863553],"genre_scores_gemma":[0.99811316,0.000034266675,0.00026552557,0.000004816399,0.000002684227,0.0000044495964,0.0014499313,0.000006294416,0.00011882945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999263,0.0000033574222,0.000006971013,0.000016710217,0.000020485408,0.000026122794],"domain_scores_gemma":[0.99982977,0.000013096486,0.000048712605,0.000018984607,0.000062210325,0.000027159309],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000103763734,0.00037621302,0.00026527734,0.00077720266,0.00026859753,0.00037053513,0.00037309676,0.00038912316,0.00057941757],"category_scores_gemma":[0.00043850995,0.00021699545,0.00020476466,0.0014541737,0.00017587314,0.0002411038,0.00033517627,0.00019185066,0.00018003778],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025157127,0.00008616726,0.92544913,0.00009852705,0.000079191064,0.0011220308,0.0003829216,0.018064478,0.030298298,0.0004522336,0.0017242816,0.021991123],"study_design_scores_gemma":[0.000024843977,0.000022608363,0.9774619,0.000009597115,0.00004041947,0.00013292438,0.0002883086,0.018603282,0.0021464606,0.00011181758,0.0011382569,0.000019586836],"about_ca_topic_score_codex":0.09378807,"about_ca_topic_score_gemma":0.111348435,"teacher_disagreement_score":0.9062119,"about_ca_system_score_codex":0.0006869615,"about_ca_system_score_gemma":0.0007283041,"threshold_uncertainty_score":0.18648434},"labels":[],"label_agreement":null},{"id":"W2900522121","doi":"10.5382/econgeo.2018.4606","title":"Mineralization of the Northwest Quartz-Pyrite-Gold Veins: Implications for Multiple Mineralization Events at Lepanto, Mankayan Mineral District, Northern Luzon, Philippines","year":2018,"lang":"en","type":"article","venue":"Economic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Universidad de La Frontera","keywords":"Geology; Pyrite; Geochemistry; Sphalerite; Alunite; Arsenopyrite; Fluid inclusions; Quartz; Sericite; Chalcopyrite; Mineralogy; Bornite; Hydrothermal circulation; Chemistry","score_opus":0.01687386613678543,"score_gpt":0.22119003344947466,"score_spread":0.20431616731268923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900522121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995726,0.000037629234,0.000026395985,0.000014875862,5.019627e-7,0.0000036107137,0.00007107002,0.000003020843,0.00027038224],"genre_scores_gemma":[0.999684,0.000032028478,0.00008035642,0.000003368088,0.0000012129013,0.0000028327627,0.00005965298,0.0000012994303,0.00013525062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999018,0.000014914233,0.0000051846832,0.00003708344,0.000017718286,0.000023382965],"domain_scores_gemma":[0.99977916,0.000018579294,0.00007086548,0.0000061191395,0.000060832306,0.00006441381],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018337619,0.000259402,0.000120015,0.000992294,0.0008064824,0.00070015807,0.00032985228,0.00026123764,0.0009967131],"category_scores_gemma":[0.00028627488,0.0001706987,0.00012731954,0.0008449137,0.00051087816,0.00031134282,0.00037904075,0.00017789062,0.00008986896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048997746,0.000026386664,0.9815316,0.00003435957,0.000015749392,0.00070700294,0.001745702,0.00018483077,0.011203756,0.000048027916,0.000052757507,0.004400658],"study_design_scores_gemma":[8.6578956e-7,0.00001097083,0.9985728,0.0000027184662,0.0000024726367,0.000055899098,0.0008079927,0.00018131942,0.00024035474,0.000007924724,0.000115228475,0.0000014182579],"about_ca_topic_score_codex":0.08284514,"about_ca_topic_score_gemma":0.18460369,"teacher_disagreement_score":0.08284514,"about_ca_system_score_codex":0.0012082614,"about_ca_system_score_gemma":0.0005918598,"threshold_uncertainty_score":0.1647259},"labels":[],"label_agreement":null},{"id":"W2900836359","doi":"10.4095/296208","title":"Ground deformation produced by 2014 M5.1 La Habra earthquake mapped with RADARSAT-2 DInSAR","year":2015,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Deformation (meteorology)","score_opus":0.026554648384220732,"score_gpt":0.23416216700053696,"score_spread":0.20760751861631624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900836359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8879675,0.00017702692,0.00087478245,0.00024924378,0.00011740871,0.00007984183,0.10110599,0.00036201178,0.009066211],"genre_scores_gemma":[0.8478592,0.00028563468,0.0019638715,0.00008641554,0.00007329978,0.00007079386,0.14403944,0.000043994023,0.005577308],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996872,0.000051782812,0.000030117839,0.000060077367,0.00009724151,0.000073584604],"domain_scores_gemma":[0.9994024,0.00005054909,0.00013879719,0.000072053605,0.00026837215,0.000067825094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044311854,0.0005201215,0.00029084994,0.0015231501,0.00022561352,0.0003718196,0.00037819633,0.0003973237,0.0017508616],"category_scores_gemma":[0.00066003,0.00022370265,0.00023341276,0.0017649829,0.00016570475,0.00046049771,0.00044341266,0.00029498382,0.00088802486],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023600429,0.00074524333,0.7779803,0.0005962453,0.00050819974,0.0008467967,0.00041539728,0.026353994,0.017872104,0.001057879,0.11005546,0.061208237],"study_design_scores_gemma":[0.0000403463,0.00007453219,0.98973876,0.00002651575,0.000031511398,0.00007107652,0.00012449315,0.0034343826,0.0014413211,0.000044035933,0.0049593183,0.000013695493],"about_ca_topic_score_codex":0.055828426,"about_ca_topic_score_gemma":0.09509129,"teacher_disagreement_score":0.055828426,"about_ca_system_score_codex":0.0008076044,"about_ca_system_score_gemma":0.0008603664,"threshold_uncertainty_score":0.111006916},"labels":[],"label_agreement":null},{"id":"W2900858623","doi":"10.1029/2018jb016472","title":"Modeling High Stress Drops, Scaling, Interaction, and Irregularity of Repeating Earthquake Sequences Near Parkfield","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Scaling; Seismic moment; Slip (aerodynamics); Seismology; Moment (physics); Geology; Stress (linguistics); Scaling law; Induced seismicity; Fault (geology); Physics; Mathematics; Geometry; Classical mechanics; Thermodynamics","score_opus":0.051730927662836206,"score_gpt":0.33612787483698364,"score_spread":0.28439694717414743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900858623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99106276,0.000031197153,0.008145187,0.000053719257,0.000004506398,0.000008571008,0.000055005443,0.00004630041,0.0005927575],"genre_scores_gemma":[0.9989492,0.000016526927,0.00080339843,0.0000032796254,0.0000034232296,0.000004258194,0.000026549047,0.00000538545,0.00018799155],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999337,0.0000117029385,0.0000038134583,0.000026934773,0.000006981809,0.000016765653],"domain_scores_gemma":[0.9996891,0.000113954084,0.00008697424,0.000029653733,0.000029360739,0.000050958755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018422652,0.0003869145,0.00033145712,0.0005296976,0.00025618883,0.00069043686,0.0009070565,0.00088299706,0.0006832917],"category_scores_gemma":[0.0009940616,0.0003905549,0.00044946364,0.0003359011,0.00045908793,0.00054902554,0.00038609502,0.00036820452,0.00007571283],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022654307,0.00005451293,0.013716175,0.000009420621,0.000024124285,0.00011140912,0.00003434417,0.9815409,0.0018652048,0.0009372897,0.000073884825,0.0016101175],"study_design_scores_gemma":[0.000002717969,0.000007375028,0.001335214,4.8166726e-7,0.000002957088,0.000005397739,0.000006097459,0.9984131,0.00008346826,0.00012160798,0.00001980591,0.0000017304561],"about_ca_topic_score_codex":0.027956856,"about_ca_topic_score_gemma":0.01560626,"teacher_disagreement_score":0.027956856,"about_ca_system_score_codex":0.00068404,"about_ca_system_score_gemma":0.00041517644,"threshold_uncertainty_score":0.055588245},"labels":[],"label_agreement":null},{"id":"W2900877453","doi":"10.4095/296205","title":"Ground deformation produced by 2012 M6.4 and M6.3 Ahar double earthquakes mapped with RADARSAT-2 DInSAR","year":2015,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Microseism","score_opus":0.040841819087304325,"score_gpt":0.2410495839145813,"score_spread":0.20020776482727698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900877453","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9043731,0.00009279082,0.0006227053,0.00019389148,0.00007858692,0.00005504883,0.085956976,0.00027539174,0.008351434],"genre_scores_gemma":[0.85134405,0.00019135336,0.0012067256,0.00005143962,0.0000605114,0.000044403056,0.1420691,0.000050753613,0.0049816407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996594,0.000036829388,0.000028173808,0.000052950523,0.00014426427,0.0000783753],"domain_scores_gemma":[0.9993118,0.00005871866,0.0001372007,0.000082702485,0.00028804844,0.00012151807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033154248,0.0006389255,0.00036280116,0.0016560387,0.00032970705,0.00037570766,0.00034835775,0.0005251742,0.0020962788],"category_scores_gemma":[0.00072981376,0.00025352932,0.000236728,0.0020135783,0.00014815372,0.0005186628,0.0006749292,0.00038776585,0.0013045085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0030048345,0.00089979393,0.8020757,0.00044330128,0.00025118116,0.001055942,0.0005675357,0.019825604,0.025899004,0.00082872045,0.07850095,0.06664747],"study_design_scores_gemma":[0.00002446895,0.00006354842,0.9918304,0.000014103896,0.000016949954,0.00009909084,0.00009989326,0.0029374768,0.0016391611,0.000027867265,0.003236327,0.0000106571715],"about_ca_topic_score_codex":0.054172274,"about_ca_topic_score_gemma":0.11708934,"teacher_disagreement_score":0.054172274,"about_ca_system_score_codex":0.0006411918,"about_ca_system_score_gemma":0.0006533777,"threshold_uncertainty_score":0.10771394},"labels":[],"label_agreement":null},{"id":"W2901604451","doi":"10.1029/2018jb016559","title":"Weak and Slow, Strong and Fast: How Shear Zones Evolve in a Dry Continental Crust (Musgrave Ranges, Central Australia)","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Università degli Studi di Padova; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Shear zone; Mylonite; Mafic; Crust; Continental crust; Gneiss; Geochemistry; Shear (geology); Quartz; Petrology; Metamorphic rock; Seismology; Tectonics; Paleontology","score_opus":0.056614086045254704,"score_gpt":0.3216680148280227,"score_spread":0.265053928782768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901604451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993954,0.00008931121,0.0000299342,0.000010371773,4.3291044e-7,0.00000225319,0.000042381347,0.0000018703006,0.00042807075],"genre_scores_gemma":[0.9994174,0.000059970607,0.000071918075,0.000008988924,6.2222034e-7,0.0000019377846,0.000062550396,0.000003153282,0.00037334455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984884,0.000020476888,0.000008021037,0.00005506512,0.000027349724,0.00004033925],"domain_scores_gemma":[0.9997799,0.000022135511,0.000063312604,0.000011096285,0.00006471644,0.00005890768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000237544,0.00018392305,0.00018017947,0.0014789947,0.0006426797,0.0010526318,0.000372591,0.00034934186,0.0011768367],"category_scores_gemma":[0.0006880406,0.00026976655,0.00013869126,0.0010557375,0.0010857007,0.00039142653,0.0009787999,0.00022601227,0.00018098892],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016348781,0.000029022856,0.91349447,0.00010243752,0.00012232533,0.00040565513,0.011662346,0.0007784082,0.05397152,0.0005779554,0.00022170377,0.018470723],"study_design_scores_gemma":[6.267203e-7,0.000011311652,0.99853146,0.0000043667155,0.0000036874571,0.000032881748,0.00079852797,0.00017220245,0.00012552894,0.00003390101,0.00028305655,0.0000024950011],"about_ca_topic_score_codex":0.0773406,"about_ca_topic_score_gemma":0.13913165,"teacher_disagreement_score":0.0773406,"about_ca_system_score_codex":0.0012431572,"about_ca_system_score_gemma":0.000383355,"threshold_uncertainty_score":0.15378088},"labels":[],"label_agreement":null},{"id":"W2901718220","doi":"10.1017/s0016756818000651","title":"Pooled subsidence records from numerous wells reveal variations in pre-break-up rifting along the proximal domains of the Iberia–Newfoundland continental margins","year":2018,"lang":"en","type":"article","venue":"Geological Magazine","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Rift; Geology; Subsidence; Passive margin; Margin (machine learning); Tectonics; Continental margin; Paleontology; Seismology; Tectonic subsidence; Structural basin","score_opus":0.013531611010772817,"score_gpt":0.2216604344084095,"score_spread":0.20812882339763666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901718220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99534297,0.00024801772,0.0002128444,0.000032456366,0.0000034667069,0.0000047360727,0.0028676495,0.000032602104,0.001255399],"genre_scores_gemma":[0.99501014,0.000105684674,0.0003974373,0.000016126709,0.0000036153685,0.0000069633043,0.0036871906,0.000010019865,0.0007629467],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998227,0.000010045587,0.000010813519,0.000057039055,0.000026874875,0.00007262517],"domain_scores_gemma":[0.9994103,0.000044385364,0.0001451927,0.000075532866,0.00025201862,0.000072629555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030935332,0.00023838301,0.00022875561,0.0015010757,0.00036335894,0.0008485342,0.0002693276,0.00019016638,0.0015529654],"category_scores_gemma":[0.0005964749,0.00014245413,0.00018522576,0.0015840832,0.00034310255,0.0003033555,0.0005226317,0.0001903832,0.0002455869],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010157977,0.000022987053,0.973343,0.000027003889,0.00011970951,0.00011071182,0.00046354774,0.0012993279,0.0045809243,0.00009254432,0.0016158612,0.018222747],"study_design_scores_gemma":[8.311914e-7,0.0000021457029,0.9990513,0.0000047949416,0.000007320986,0.000008300924,0.00012959134,0.00022141551,0.00011859183,0.0000033619335,0.0004502159,0.0000021900462],"about_ca_topic_score_codex":0.76107085,"about_ca_topic_score_gemma":0.88447326,"teacher_disagreement_score":0.23892915,"about_ca_system_score_codex":0.002371752,"about_ca_system_score_gemma":0.0009796508,"threshold_uncertainty_score":0.48067248},"labels":[],"label_agreement":null},{"id":"W2902108975","doi":"10.1029/2018gl079746","title":"Bilinear Magnitude‐Frequency Distributions and Characteristic Earthquakes During Hydraulic Fracturing","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Magnitude (astronomy); Geology; Hydraulic fracturing; Seismology; Bilinear interpolation; Superposition principle; Fault (geology); Range (aeronautics); Earthquake magnitude; Geotechnical engineering; Statistics; Mathematics; Geometry; Physics","score_opus":0.029525458107763178,"score_gpt":0.2822454876317737,"score_spread":0.2527200295240105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902108975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99843067,0.000016203381,0.0004409355,0.000008519516,5.7884165e-7,0.0000037227,0.00034806115,0.000014015773,0.00073718146],"genre_scores_gemma":[0.9995005,0.000005065527,0.00009567543,0.0000010260042,5.5245937e-7,0.0000011080226,0.00031199807,0.0000015772406,0.00008237903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997805,0.000035756606,0.000018226949,0.000037782138,0.00006829812,0.000059520764],"domain_scores_gemma":[0.99757487,0.000589607,0.00079886796,0.00027400453,0.00047674755,0.00028587985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004372948,0.00012366244,0.00015036209,0.0017271906,0.00025705007,0.0005029332,0.00019971713,0.00014708059,0.0013437144],"category_scores_gemma":[0.0026438762,0.00012112376,0.000091695154,0.0015282902,0.00043716916,0.00025646228,0.00047999996,0.0001914554,0.00020698358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013592871,0.000022725872,0.9856252,0.000013243714,0.000022782464,0.00008490997,0.0006607894,0.0012612343,0.005619378,0.0002246675,0.00018530573,0.0061438144],"study_design_scores_gemma":[0.0000012617866,0.000010679948,0.9982926,0.0000014399188,0.0000023040227,0.000048723232,0.0002016939,0.0009804057,0.00025992104,0.000070544964,0.0001271432,0.0000033423157],"about_ca_topic_score_codex":0.0677102,"about_ca_topic_score_gemma":0.07628631,"teacher_disagreement_score":0.0677102,"about_ca_system_score_codex":0.0005279326,"about_ca_system_score_gemma":0.00031856424,"threshold_uncertainty_score":0.13463217},"labels":[],"label_agreement":null},{"id":"W2902332342","doi":"10.1007/s00477-018-1634-x","title":"Time-dependent probabilistic tsunami hazard analysis using stochastic rupture sources","year":2018,"lang":"en","type":"article","venue":"Stochastic Environmental Research and Risk Assessment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Leverhulme Trust","keywords":"Seismology; Hazard; Computation tree logic; Geology; Probabilistic logic; Seismic hazard; Tsunami earthquake; Thrust; Hazard analysis; Magnitude (astronomy); Stochastic modelling; Computer science; Statistics; Model checking; Reliability engineering; Mathematics; Engineering; Algorithm","score_opus":0.025562068054152384,"score_gpt":0.30173969690820046,"score_spread":0.27617762885404806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902332342","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.100995675,0.00026929556,0.89654714,0.00020178963,0.00002431346,0.00003881454,0.00020446717,0.00022886161,0.0014897167],"genre_scores_gemma":[0.9729783,0.0003786483,0.023349142,0.000030121688,0.00006643486,0.000075429525,0.00027187113,0.00005747139,0.0027925954],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999483,0.00020755082,0.000033360622,0.00008528533,0.00013038822,0.000060417955],"domain_scores_gemma":[0.994399,0.0043902076,0.0005941676,0.00020359673,0.00032209363,0.000090935115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001950578,0.0008472932,0.00081478275,0.0013599278,0.0003099727,0.0009260022,0.0013289364,0.0010901096,0.0018196434],"category_scores_gemma":[0.008062716,0.0008853298,0.0011215252,0.0010409635,0.0007728058,0.0015544951,0.0012169112,0.00082501885,0.00018640359],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018629986,0.000009741388,0.0004498978,0.000011102999,0.000024479923,0.00003098811,0.000010450395,0.98964417,0.0002308255,0.0071839523,0.00006185243,0.0023239322],"study_design_scores_gemma":[0.000001747404,0.0000040326026,0.00009207119,0.0000011381944,0.0000049458267,0.0000064685873,0.0000016292179,0.9979977,0.000044923723,0.0018207362,0.000022000297,0.0000026424925],"about_ca_topic_score_codex":0.0046528834,"about_ca_topic_score_gemma":0.0033481377,"teacher_disagreement_score":0.0046528834,"about_ca_system_score_codex":0.0007365889,"about_ca_system_score_gemma":0.00082742603,"threshold_uncertainty_score":0.010315776},"labels":[],"label_agreement":null},{"id":"W2903353978","doi":"10.4095/292067","title":"A preliminary tsunami hazard assessment of the Canadian Coastline","year":2012,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Hazard; Hazard analysis; Geography; Geology; Environmental science; Engineering; Reliability engineering; Biology; Ecology","score_opus":0.0307006676626075,"score_gpt":0.2582417709273443,"score_spread":0.22754110326473678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903353978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86357456,0.0020732803,0.02742788,0.0012049854,0.000042374973,0.00066506985,0.022516636,0.00036085944,0.08213437],"genre_scores_gemma":[0.96428585,0.0012780639,0.017286561,0.00013203546,0.000011922263,0.000083567524,0.0054007275,0.00003284655,0.011488438],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99936765,0.000030152349,0.000018019047,0.00004558043,0.0004417889,0.00009689841],"domain_scores_gemma":[0.99884135,0.000057766938,0.000064814965,0.000029979781,0.00092118577,0.00008498246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005102387,0.0009390008,0.00022808962,0.0018862276,0.0018461611,0.0012798102,0.0007878762,0.00040714827,0.0029277687],"category_scores_gemma":[0.0014899416,0.00023112888,0.0007948811,0.0018010365,0.000281573,0.00041825927,0.00065874826,0.00035625347,0.0002838325],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037609646,0.00014090173,0.413037,0.0004347138,0.00040861964,0.00083518267,0.0010102522,0.35454983,0.017729266,0.01229565,0.02108185,0.17810068],"study_design_scores_gemma":[0.00003720313,0.000368223,0.719205,0.00015824869,0.00019658076,0.00033435767,0.001611312,0.23190224,0.0049651815,0.0036691835,0.037383534,0.00016896827],"about_ca_topic_score_codex":0.96606296,"about_ca_topic_score_gemma":0.9838643,"teacher_disagreement_score":0.033937037,"about_ca_system_score_codex":0.010313579,"about_ca_system_score_gemma":0.0144234495,"threshold_uncertainty_score":0.07483065},"labels":[],"label_agreement":null},{"id":"W2904143663","doi":"10.1016/0967-0653(96)87213-9","title":"10.1016/0967-0653(96)87213-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Seismometer; Ocean bottom; Geology; Seismology; Indian ocean; Oceanography","score_opus":0.008535813829888998,"score_gpt":0.1629535887325498,"score_spread":0.15441777490266081,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904143663","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005572464,0.00039144972,0.0005039278,0.00037925,0.00028394558,0.00014093991,0.00096834626,0.0009174354,0.9958574],"genre_scores_gemma":[0.00072290533,0.00028459396,0.00033741092,0.00032980344,0.000091382186,0.00008760942,0.0004898492,0.0001852466,0.9974711],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992423,0.00005203004,0.00008018071,0.00028197726,0.00016184733,0.00018171147],"domain_scores_gemma":[0.9973328,0.0007005527,0.00016734704,0.00034173467,0.00058657146,0.0008708573],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0014286014,0.0039827204,0.0027190023,0.003322046,0.0036113672,0.0046211565,0.0042672087,0.0073439525,0.991441],"category_scores_gemma":[0.001903282,0.0016965558,0.0018811461,0.0032766464,0.0032521791,0.0074349325,0.0043385387,0.0036094908,0.9951422],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055063405,0.00035602401,0.0014544028,0.0008637756,0.00006419396,0.00042225304,0.00017789721,0.0006525041,0.0028849072,0.0054670162,0.43174025,0.5553661],"study_design_scores_gemma":[0.00012168473,0.00023148791,0.001457132,0.00068409427,0.00002701145,0.00055064505,0.00026015122,0.0002527132,0.00043807068,0.0008538666,0.9950734,0.000049719525],"about_ca_topic_score_codex":0.0060783518,"about_ca_topic_score_gemma":0.005593369,"teacher_disagreement_score":0.008558989,"about_ca_system_score_codex":0.001391637,"about_ca_system_score_gemma":0.0009949555,"threshold_uncertainty_score":0.012208283},"labels":[],"label_agreement":null},{"id":"W2905684214","doi":"","title":"A Method to Assess Potential Induced Seismicity Hazard With Application to the Duvernay","year":2018,"lang":"en","type":"article","venue":"52nd U.S. Rock Mechanics/Geomechanics Symposium","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Apache (Canada)","funders":"","keywords":"Induced seismicity; Geology; Hazard; Seismology","score_opus":0.018866912036549437,"score_gpt":0.24516313998782516,"score_spread":0.2262962279512757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905684214","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10000961,0.00021362786,0.8837105,0.0001502614,0.000060393315,0.0005053749,0.0011751798,0.0026957272,0.011479304],"genre_scores_gemma":[0.45317194,0.00014362327,0.54004496,0.000041947456,0.000017709608,0.00035149686,0.00070713536,0.00014114438,0.0053800256],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995708,0.000111177265,0.000030344821,0.0000883251,0.00016996087,0.000029417324],"domain_scores_gemma":[0.99883,0.0004398168,0.00013721408,0.00008356048,0.00045205248,0.000057329038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007839712,0.0005843992,0.00041614546,0.0034044064,0.0006973167,0.0007734114,0.00058306364,0.00052150607,0.005628725],"category_scores_gemma":[0.0033318393,0.00028453287,0.00043564822,0.0017152391,0.00027723104,0.00046418735,0.000890365,0.0004346808,0.0009180165],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050225534,0.000322476,0.09822953,0.00044188692,0.00021317694,0.00034855236,0.00093962107,0.08021037,0.047116987,0.010624987,0.0070730336,0.75397724],"study_design_scores_gemma":[0.00008839733,0.0003860882,0.041078992,0.000056275636,0.00009109149,0.00056188524,0.00061357743,0.9294493,0.012612698,0.003371797,0.0115837185,0.000106214466],"about_ca_topic_score_codex":0.016717458,"about_ca_topic_score_gemma":0.026721297,"teacher_disagreement_score":0.98328257,"about_ca_system_score_codex":0.0005837818,"about_ca_system_score_gemma":0.0010549402,"threshold_uncertainty_score":0.03324032},"labels":[],"label_agreement":null},{"id":"W2906161517","doi":"10.1029/2018jb016226","title":"Quartz Flow Law Revisited: The Significance of Pressure Dependence of the Activation Enthalpy","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Northwest University; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Mylonite; Creep; Dislocation creep; Strain rate; Geology; Quartz; Rheology; Mechanics; Thermodynamics; Law; Materials science; Shear zone; Physics","score_opus":0.040913919148463436,"score_gpt":0.3160859965273456,"score_spread":0.27517207737888216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906161517","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95654273,0.0013269574,0.034693997,0.00072485907,0.000075122145,0.00007836104,0.0004097534,0.0003555639,0.005792638],"genre_scores_gemma":[0.9985115,0.00012968498,0.0010711058,0.00003106111,0.000015306534,0.0000130497665,0.000042501164,0.000013529783,0.00017217439],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99959093,0.000056923902,0.000027480359,0.000179433,0.00010784481,0.000037304915],"domain_scores_gemma":[0.99841475,0.0009625776,0.00027214107,0.00015112171,0.0001668901,0.000032431028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011863721,0.00027924898,0.00032566924,0.0008658176,0.0002218003,0.0005721857,0.00075198826,0.00042959466,0.0016185782],"category_scores_gemma":[0.0037258305,0.00019584622,0.00023530201,0.0003067919,0.0013673707,0.001204416,0.00037126648,0.00077219453,0.00016969918],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047516145,0.00039362075,0.09179732,0.0006301849,0.000105724896,0.00087805087,0.00060486846,0.123632714,0.67494184,0.041896116,0.0018085449,0.06283584],"study_design_scores_gemma":[0.00007384982,0.00082813436,0.15614101,0.000088593246,0.000047043755,0.0004329006,0.000181238,0.542364,0.26826996,0.027153494,0.0043172645,0.00010255046],"about_ca_topic_score_codex":0.0015564797,"about_ca_topic_score_gemma":0.0009425792,"teacher_disagreement_score":0.0016185782,"about_ca_system_score_codex":0.00048110733,"about_ca_system_score_gemma":0.0002750918,"threshold_uncertainty_score":0.0062742233},"labels":[],"label_agreement":null},{"id":"W2906472891","doi":"10.1029/2018jb016828","title":"Extent of Low‐Angle Normal Slip in the 2010 El Mayor‐Cucapah (Mexico) Earthquake From Differential Lidar","year":2018,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"U.S. Geological Survey","keywords":"Geology; Slip (aerodynamics); Seismology; Geodetic datum; Geodesy; Fault (geology); Magnetic dip; Fault trace; Fault plane; Surface rupture; Earthquake rupture; Strike-slip tectonics; Geometry; Physics; Geophysics","score_opus":0.03790430668542853,"score_gpt":0.3107501089246101,"score_spread":0.27284580223918153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906472891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99930537,0.000016702868,0.000039674356,0.000015025723,8.346346e-7,0.0000020011228,0.0002689764,0.0000056749354,0.0003456841],"genre_scores_gemma":[0.99944943,0.0000151449885,0.00009194835,0.000004342581,0.000001984161,0.0000033781698,0.00034421662,9.870132e-7,0.0000885685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999385,0.00000554756,0.0000031951702,0.000019158337,0.000013753328,0.000019862047],"domain_scores_gemma":[0.99983454,0.000022063963,0.000060325532,0.000012380917,0.000049370552,0.000021329075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001321575,0.00013190645,0.00013243717,0.00075530156,0.00028800915,0.0003508098,0.0002601604,0.00031926844,0.00058297144],"category_scores_gemma":[0.00038396727,0.00012219009,0.00007939716,0.0007639134,0.00019248133,0.00023628694,0.00036737934,0.00018002611,0.00010587023],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011101682,0.000068101544,0.9813286,0.000022756101,0.000026496105,0.0002364813,0.00033948896,0.0021624956,0.006159449,0.000062400475,0.00035262556,0.009130131],"study_design_scores_gemma":[0.0000039084293,0.000012065544,0.9970457,0.0000036204265,0.0000041153844,0.000030563217,0.00021432363,0.0022966505,0.0002053175,0.000009130362,0.00017138929,0.0000031845113],"about_ca_topic_score_codex":0.060461838,"about_ca_topic_score_gemma":0.09582712,"teacher_disagreement_score":0.060461838,"about_ca_system_score_codex":0.0005265335,"about_ca_system_score_gemma":0.00023625742,"threshold_uncertainty_score":0.12021983},"labels":[],"label_agreement":null},{"id":"W2906674142","doi":"10.1134/s0001433818070046","title":"Ring-Shaped Seismicity Structures in the Cascadia Subduction Zone: Possible Upcoming Large Earthquakes","year":2018,"lang":"en","type":"article","venue":"Izvestiya Atmospheric and Oceanic Physics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Subduction; Geology; Seismology; Pacific Plate; Tectonics","score_opus":0.013549651118799685,"score_gpt":0.22126629728841407,"score_spread":0.20771664616961438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906674142","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991431,0.00010030391,0.00012330535,0.000015784663,0.0000011373925,0.0000032278358,0.00007183076,0.0000064049723,0.0005347565],"genre_scores_gemma":[0.9996007,0.00006391612,0.000080574944,0.0000018655111,0.0000021331439,0.0000016844715,0.00014071415,0.0000014135032,0.00010706172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999864,0.000016611559,0.000012393355,0.000029319646,0.00003528687,0.000042440224],"domain_scores_gemma":[0.99900585,0.00012537892,0.00044148832,0.00007715191,0.00013171391,0.00021840817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026087125,0.0002770519,0.00020891755,0.0016366701,0.00037926415,0.00037512448,0.00035473486,0.0002739449,0.0010840528],"category_scores_gemma":[0.0010354429,0.00019981447,0.00032445535,0.001144633,0.00048855145,0.0003311192,0.00056278956,0.00016729553,0.00015053611],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019162838,0.000031332904,0.98148376,0.000040393945,0.00005130959,0.0011544955,0.0005850194,0.004623892,0.006509058,0.00030291502,0.00012747089,0.0048988257],"study_design_scores_gemma":[0.00000321856,0.00004115567,0.9976163,0.0000023938753,0.000014679908,0.00013682012,0.00016736172,0.0016088621,0.00017908246,0.0000851599,0.00013936227,0.000005663793],"about_ca_topic_score_codex":0.008219739,"about_ca_topic_score_gemma":0.013480871,"teacher_disagreement_score":0.008219739,"about_ca_system_score_codex":0.0006303957,"about_ca_system_score_gemma":0.00027363922,"threshold_uncertainty_score":0.016343832},"labels":[],"label_agreement":null},{"id":"W2907822770","doi":"10.1139/cjes-2018-0128","title":"A new approach to the opening of the eastern Mediterranean Sea and the origin of the Hellenic Subduction Zone. Part 1: The eastern Mediterranean Sea","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Transform fault; Subduction; Mediterranean sea; Mediterranean climate; Fault (geology); Seismology; Paleontology; Tectonics; Geography; Archaeology","score_opus":0.049107408149788805,"score_gpt":0.2275456644606543,"score_spread":0.1784382563108655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2907822770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.71063805,0.08404649,0.057663653,0.012326839,0.0013089987,0.00017879275,0.00035301846,0.00014771511,0.13333647],"genre_scores_gemma":[0.918805,0.023479717,0.030418102,0.0012436076,0.0008313152,0.0000957543,0.00023294687,0.00002483321,0.024868656],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999304,0.000014788746,0.0000068832715,0.000019670422,0.000014838276,0.000013505509],"domain_scores_gemma":[0.99981374,0.000043005217,0.00006378518,0.000018850924,0.000036376292,0.000024263329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002610763,0.00044915828,0.00020336782,0.0020202652,0.00084117986,0.0013082474,0.0005148165,0.0006035894,0.002971941],"category_scores_gemma":[0.00053783384,0.00013171026,0.00032483324,0.0011723037,0.0025763933,0.0022234607,0.001553679,0.00072812155,0.00025164633],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024629637,0.00010752325,0.13191953,0.0008613069,0.00013784893,0.005944449,0.020559818,0.00617554,0.03235276,0.36309478,0.0055144937,0.4330856],"study_design_scores_gemma":[0.00006797648,0.00017951817,0.29830596,0.0005303373,0.00011396519,0.004373785,0.011818945,0.008194088,0.0037677262,0.19022548,0.48233548,0.00008674414],"about_ca_topic_score_codex":0.019172357,"about_ca_topic_score_gemma":0.041607235,"teacher_disagreement_score":0.019172357,"about_ca_system_score_codex":0.0025760734,"about_ca_system_score_gemma":0.0009111688,"threshold_uncertainty_score":0.03812152},"labels":[],"label_agreement":null},{"id":"W2908410126","doi":"","title":"Modeling of Tsunami Propagation and Impact on West Vancouver Island, Canada","year":2019,"lang":"en","type":"article","venue":"World Academy of Science, Engineering and Technology, International Journal of Economics and Management Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Geography; Oceanography","score_opus":0.0047240005526123655,"score_gpt":0.18487689478837527,"score_spread":0.1801528942357629,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908410126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9685222,0.0003589704,0.0023881488,0.0008338093,0.000062437364,0.000073048635,0.0044627236,0.00017233298,0.023126382],"genre_scores_gemma":[0.98368394,0.00029964873,0.0016100949,0.000077174,0.0000089746645,0.00004015604,0.001590161,0.000047672835,0.01264209],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981505,0.000020544345,0.000009563661,0.000033898294,0.000042935197,0.00007809583],"domain_scores_gemma":[0.9991486,0.00021117284,0.000040999454,0.000024614703,0.0004159277,0.00015873172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027776946,0.00085319736,0.0007439857,0.0011026259,0.0029280805,0.0024890571,0.0027884527,0.0019609998,0.0072491174],"category_scores_gemma":[0.0017354566,0.00094607327,0.00083416415,0.0017879639,0.0009433105,0.00068415084,0.00076195976,0.0013319117,0.0005107501],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008855098,0.00008085704,0.011597436,0.000024830697,0.000041307507,0.00010720699,0.0000640872,0.9824256,0.00027978022,0.0009935605,0.0020820727,0.002214634],"study_design_scores_gemma":[0.000036955065,0.000013130935,0.004332963,0.000008513935,0.000019039173,0.000008661803,0.0001817026,0.9941549,0.00012021095,0.00019660135,0.0009100852,0.000017350052],"about_ca_topic_score_codex":0.9948384,"about_ca_topic_score_gemma":0.9918894,"teacher_disagreement_score":0.023117438,"about_ca_system_score_codex":0.023117438,"about_ca_system_score_gemma":0.023569673,"threshold_uncertainty_score":0.16772956},"labels":[],"label_agreement":null},{"id":"W2908701651","doi":"10.4095/212010","title":"Ground-magnetic investigations of Cenozoic structures in the northern Cascadia forearc, British Columbia","year":2001,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Forearc; Cenozoic; Geology; Seismology; Subduction; Paleontology; Tectonics","score_opus":0.029454144508182907,"score_gpt":0.23021845403145358,"score_spread":0.20076430952327068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908701651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971802,0.000058163998,0.000051012343,0.000036781377,5.3759817e-7,0.000011221453,0.00030927468,0.0000066734433,0.0023461191],"genre_scores_gemma":[0.99757963,0.00013156011,0.00017728235,0.000015558491,9.236903e-7,0.000009467053,0.00052802084,0.00000265353,0.0015548646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999871,0.000010103683,0.0000048787774,0.000022132861,0.00004742685,0.00004442472],"domain_scores_gemma":[0.9995654,0.000024008836,0.000058528745,0.000019358245,0.0002581252,0.00007464091],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009998264,0.0001745941,0.00012629152,0.0016473988,0.0013132929,0.00048410697,0.00035001407,0.00017748466,0.0016368772],"category_scores_gemma":[0.0005058231,0.00019299921,0.0000570691,0.002035124,0.0005198712,0.00016363765,0.00041110517,0.0002140275,0.00016836579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007113999,0.0000655158,0.9547479,0.00007308753,0.000023863344,0.0006546162,0.00448838,0.00087332405,0.010313138,0.00022757785,0.00096245157,0.027498964],"study_design_scores_gemma":[0.0000022625059,0.0000071529544,0.9982994,0.0000047098047,0.000002061222,0.00002843731,0.0008831886,0.00008860667,0.00015113568,0.000010630028,0.0005210247,0.0000014488697],"about_ca_topic_score_codex":0.93250644,"about_ca_topic_score_gemma":0.9842015,"teacher_disagreement_score":0.06749356,"about_ca_system_score_codex":0.0045190416,"about_ca_system_score_gemma":0.0034365356,"threshold_uncertainty_score":0.135782},"labels":[],"label_agreement":null},{"id":"W2909425419","doi":"10.4095/247644","title":"The November 1, 1935, M 6.2 Timiskaming earthquake, its aftershocks, and subsequent seismicity","year":2009,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Aftershock; Induced seismicity; Seismology; Geology; Foreshock","score_opus":0.03584142721098161,"score_gpt":0.2490645734614167,"score_spread":0.2132231462504351,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909425419","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97066814,0.0011059041,0.00022419463,0.00041248175,0.000065502594,0.00005311552,0.0064290515,0.000022999471,0.02101862],"genre_scores_gemma":[0.9721281,0.0022258034,0.00032681235,0.00008289943,0.00010023917,0.000029504206,0.008666213,0.000007232075,0.016433157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998375,0.000009850776,0.000013922034,0.000017421922,0.00007017239,0.00005106864],"domain_scores_gemma":[0.99978834,0.000017279988,0.00009986789,0.000011956994,0.0000429819,0.00003957247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016642347,0.00019037665,0.00012286294,0.0008194876,0.0005843195,0.0004150108,0.00023091413,0.00020736859,0.003433929],"category_scores_gemma":[0.0009268342,0.000112969494,0.00009756187,0.0007438031,0.00031977412,0.00029323163,0.000585365,0.00030717763,0.0005417981],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023968624,0.00011488279,0.86397153,0.00030422205,0.00005063042,0.0035519216,0.00561424,0.0009975086,0.0069217873,0.0012246956,0.023037123,0.09397174],"study_design_scores_gemma":[0.000002660174,0.000041895637,0.98226744,0.000026407706,0.000008567662,0.00029536823,0.00033808826,0.000054882137,0.00030026006,0.000027230857,0.01663184,0.0000053327863],"about_ca_topic_score_codex":0.091221854,"about_ca_topic_score_gemma":0.18677796,"teacher_disagreement_score":0.90877813,"about_ca_system_score_codex":0.0011619189,"about_ca_system_score_gemma":0.00080970925,"threshold_uncertainty_score":0.18138182},"labels":[],"label_agreement":null},{"id":"W2909468394","doi":"10.4095/220412","title":"Seismic Transects - Eglinton and Eastern Prince Patrick","year":2005,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Transect; Geology; Geography; Oceanography","score_opus":0.029581233532439164,"score_gpt":0.24078610966158828,"score_spread":0.21120487612914912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909468394","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94609576,0.0002556003,0.00031921105,0.00029139017,0.00003033961,0.00015339696,0.01874931,0.000047258764,0.03405782],"genre_scores_gemma":[0.8577254,0.00088839687,0.0025011173,0.0001847397,0.00004253233,0.00021555684,0.022661014,0.000058294474,0.11572293],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984264,0.000021582071,0.00001688757,0.000033882523,0.00004576726,0.00003917527],"domain_scores_gemma":[0.9992843,0.000075717784,0.00012393066,0.00007367542,0.0003244951,0.00011793549],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002281664,0.0003678863,0.0001467942,0.0018904004,0.00076111255,0.00049874524,0.00037544646,0.00043775258,0.010863087],"category_scores_gemma":[0.000874481,0.00027588708,0.0001321745,0.0030008515,0.00022303432,0.00052922644,0.0012334982,0.00029799226,0.002221381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010184103,0.0001639648,0.76005626,0.0005962373,0.00015048838,0.0081343055,0.02650762,0.0021210823,0.009088725,0.0016254901,0.066668354,0.12386901],"study_design_scores_gemma":[0.000013141823,0.00005546576,0.9766283,0.000034248198,0.00000967143,0.0003721555,0.0033579841,0.00016121958,0.0004894855,0.000047864658,0.018824777,0.000005751392],"about_ca_topic_score_codex":0.15970892,"about_ca_topic_score_gemma":0.4316615,"teacher_disagreement_score":0.15970892,"about_ca_system_score_codex":0.0005363454,"about_ca_system_score_gemma":0.0011645284,"threshold_uncertainty_score":0.3175586},"labels":[],"label_agreement":null},{"id":"W2909527837","doi":"10.4095/216210","title":"Seismic transects G, H, I and J","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Transect; Geology; Seismology; Oceanography","score_opus":0.03151976173623684,"score_gpt":0.2360811550276401,"score_spread":0.20456139329140327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909527837","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1272152,0.0003651845,0.004368851,0.00047648206,0.00068028586,0.0013097106,0.76185834,0.0011410529,0.1025849],"genre_scores_gemma":[0.16240737,0.001077771,0.01734015,0.00020758716,0.00021645326,0.001018986,0.60645217,0.00051658065,0.21076293],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99956506,0.000044711487,0.000037204183,0.00009311329,0.00014701804,0.00011293451],"domain_scores_gemma":[0.99771106,0.00017620497,0.00031937892,0.0002643808,0.0011738695,0.00035512244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050477555,0.0012864541,0.0004538,0.0045993924,0.0010490847,0.0005345731,0.0012293309,0.00057919644,0.022509085],"category_scores_gemma":[0.0016607281,0.0005205024,0.00030903527,0.0041047293,0.0003739494,0.0008162659,0.00056997687,0.00078856223,0.013347076],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017721569,0.0004508823,0.11601171,0.0004657877,0.00013056258,0.0005779304,0.0010989006,0.0018022261,0.012812395,0.0019952,0.7968667,0.06601555],"study_design_scores_gemma":[0.00025007105,0.0004534295,0.5654974,0.000088863286,0.00015187102,0.00044698507,0.0015193397,0.0018557119,0.019142045,0.00049027114,0.41005006,0.000053991578],"about_ca_topic_score_codex":0.14484455,"about_ca_topic_score_gemma":0.26675937,"teacher_disagreement_score":0.14484455,"about_ca_system_score_codex":0.0012094992,"about_ca_system_score_gemma":0.0033069802,"threshold_uncertainty_score":0.2880029},"labels":[],"label_agreement":null},{"id":"W2909672800","doi":"10.1016/j.jsg.2018.12.011","title":"‘Strain probe’: Best-fitting a homogeneous strain to the motions of scattered points","year":2019,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Geodetic datum; Geology; Strain (injury); Geodesy; Cartesian coordinate system; Geometry; Deformation (meteorology); Reference frame; Finite strain theory; Homogeneous; Mathematical analysis; Mathematics; Frame (networking); Finite element method; Physics; Combinatorics; Computer science","score_opus":0.01564803777806045,"score_gpt":0.23144314315770115,"score_spread":0.2157951053796407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909672800","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.23160306,0.0003888264,0.74807054,0.0003337762,0.00020439007,0.00015377627,0.0019355519,0.015376125,0.0019339465],"genre_scores_gemma":[0.4928203,0.00013975678,0.4981244,0.00016250179,0.000044471384,0.00017338103,0.00459257,0.002033999,0.0019086454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993049,0.00017131219,0.00005314424,0.00023187425,0.0001493804,0.000089459114],"domain_scores_gemma":[0.9987857,0.0005975575,0.000100349054,0.00018974162,0.0002782746,0.00004842605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023146106,0.002133441,0.0010997342,0.0018563557,0.00052512216,0.0010314971,0.0021907527,0.003298286,0.005124643],"category_scores_gemma":[0.008529825,0.0010257361,0.0014338461,0.0018988965,0.00059565343,0.0014040826,0.00091495056,0.0014835995,0.0019736146],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001187244,0.000715867,0.009021268,0.00029067346,0.00031219405,0.0003052202,0.00034280567,0.5358282,0.030694462,0.001645181,0.011635566,0.4080213],"study_design_scores_gemma":[0.000049114355,0.00010764137,0.002790309,0.000014143827,0.000026715747,0.0000799129,0.000057297853,0.9886126,0.0063380017,0.0005353039,0.0013554276,0.00003343595],"about_ca_topic_score_codex":0.010649807,"about_ca_topic_score_gemma":0.014504473,"teacher_disagreement_score":0.010649807,"about_ca_system_score_codex":0.00047792785,"about_ca_system_score_gemma":0.0011137181,"threshold_uncertainty_score":0.021175623},"labels":[],"label_agreement":null},{"id":"W2909683740","doi":"10.4095/220413","title":"Seismic Transects - Western Prince Patrick","year":2005,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Transect; Geology; Archaeology; Seismology; Geography; Paleontology; Physical geography; Oceanography","score_opus":0.034610352743443575,"score_gpt":0.2504295316190997,"score_spread":0.21581917887565613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909683740","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.79855055,0.0006341578,0.0012907753,0.0008637843,0.00012997835,0.00044982272,0.073634915,0.00024326614,0.12420281],"genre_scores_gemma":[0.7149051,0.0014299176,0.005580268,0.00027171284,0.000106470034,0.00033959764,0.047726657,0.00013492425,0.22950538],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998312,0.00001710749,0.000015050528,0.000034834437,0.000064905435,0.000036808397],"domain_scores_gemma":[0.99926597,0.000054924803,0.00010534218,0.000063549305,0.00040118193,0.0001090732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020349234,0.00048427633,0.00017073599,0.0017644857,0.0010330171,0.0005328036,0.00035951484,0.00043577072,0.01400208],"category_scores_gemma":[0.0009178262,0.00029961206,0.00016442673,0.003160231,0.00015586178,0.0004526137,0.0010090292,0.00040474895,0.0040056584],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008063281,0.000180073,0.4612708,0.00082463917,0.00015311365,0.008390304,0.020472968,0.003045669,0.00967842,0.0021498883,0.2770546,0.21597306],"study_design_scores_gemma":[0.000019998935,0.00011799198,0.90659094,0.00006515658,0.00001692145,0.000918626,0.0036795698,0.00045929023,0.0009169079,0.000097569944,0.08710273,0.0000142386125],"about_ca_topic_score_codex":0.24193779,"about_ca_topic_score_gemma":0.47292653,"teacher_disagreement_score":0.75806224,"about_ca_system_score_codex":0.00046907802,"about_ca_system_score_gemma":0.0015175157,"threshold_uncertainty_score":0.48105907},"labels":[],"label_agreement":null},{"id":"W2909721614","doi":"10.4095/216199","title":"Seismic transects A, B and C","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Transect; Geology; Seismology; Geography; Oceanography","score_opus":0.031385545495817145,"score_gpt":0.2351996364624219,"score_spread":0.20381409096660474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909721614","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14123681,0.00054306904,0.005461985,0.00050407543,0.00068427925,0.0022604757,0.6910535,0.0016408933,0.15661494],"genre_scores_gemma":[0.21807273,0.0012666006,0.023913175,0.0003553452,0.00022940598,0.0015495091,0.52286816,0.00054774445,0.23119727],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.999488,0.00004060578,0.000045970934,0.00013365444,0.00017343045,0.000118308206],"domain_scores_gemma":[0.99725986,0.00018487577,0.00032638165,0.0002925351,0.0014701888,0.00046611018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044368618,0.0013676683,0.00044059512,0.0059564873,0.0015809053,0.0007070171,0.0010649525,0.00078230107,0.026238812],"category_scores_gemma":[0.0014070437,0.00052392,0.0003107041,0.0049294736,0.0003985463,0.0008937615,0.0006337738,0.0010376904,0.014508665],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026736187,0.00066270394,0.098927625,0.0005700875,0.00015212884,0.00074719725,0.0010885007,0.0018928688,0.019963685,0.0023994874,0.7762709,0.09465123],"study_design_scores_gemma":[0.00027026536,0.0005068421,0.56802106,0.000119216194,0.000108752436,0.0005189595,0.0013609601,0.0012573595,0.016547922,0.00039639015,0.4108363,0.00005599291],"about_ca_topic_score_codex":0.2076009,"about_ca_topic_score_gemma":0.36780202,"teacher_disagreement_score":0.2076009,"about_ca_system_score_codex":0.0014492224,"about_ca_system_score_gemma":0.0037246551,"threshold_uncertainty_score":0.41278505},"labels":[],"label_agreement":null},{"id":"W2909893188","doi":"10.4095/216209","title":"Seismic transects D, E and F","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Transect; Geology; Seismology; Geography; Geodesy; Oceanography","score_opus":0.03177953946867126,"score_gpt":0.2360187008683132,"score_spread":0.20423916139964193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909893188","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.118196905,0.0005197283,0.006348755,0.0005861112,0.0009492463,0.0020923517,0.7103655,0.0014282622,0.15951316],"genre_scores_gemma":[0.19073488,0.0011460235,0.019760104,0.00041167747,0.00023783089,0.0013358112,0.52224225,0.0004837854,0.2636477],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99952614,0.000037032543,0.000038573395,0.00011398127,0.00015654873,0.00012764164],"domain_scores_gemma":[0.99779737,0.0001587941,0.0002458513,0.00026251026,0.001197978,0.0003374505],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046905986,0.0012388173,0.0004246182,0.0054370007,0.0012244087,0.0005879026,0.0011200048,0.0007407396,0.024312945],"category_scores_gemma":[0.0016037731,0.0004857178,0.000337795,0.0034974108,0.00036036014,0.00075567054,0.00062099734,0.0008044235,0.013162637],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018421537,0.00047995156,0.09161943,0.0004480628,0.0001279252,0.0006833014,0.00090221467,0.0017938481,0.013918328,0.0020605512,0.8023088,0.08381537],"study_design_scores_gemma":[0.00025374207,0.00043569683,0.48091966,0.00012959505,0.00010875875,0.00055987656,0.0012842875,0.0015012408,0.016415786,0.00042690008,0.49790972,0.000054653756],"about_ca_topic_score_codex":0.1779957,"about_ca_topic_score_gemma":0.30750966,"teacher_disagreement_score":0.1779957,"about_ca_system_score_codex":0.0013801877,"about_ca_system_score_gemma":0.0031121592,"threshold_uncertainty_score":0.35391927},"labels":[],"label_agreement":null},{"id":"W2910029199","doi":"10.4095/212164","title":"Supracrustal faults of the St. Lawrence rift system between Cap-Tourmente and Baie-Saint-Paul, Quebec","year":2001,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Rift; SAINT; Geology; Seismology; History; Art history; Tectonics","score_opus":0.028702123553560683,"score_gpt":0.24004962376600272,"score_spread":0.21134750021244203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2910029199","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88122386,0.0014503984,0.0007797004,0.00158211,0.000047764854,0.0004211776,0.03519721,0.00016009549,0.07913762],"genre_scores_gemma":[0.87385684,0.0010062006,0.0010488966,0.00016782296,0.000018169234,0.00009200027,0.015183252,0.000021581585,0.10860528],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979407,0.000008570512,0.000006129651,0.0000329183,0.000084629406,0.00007370506],"domain_scores_gemma":[0.99955696,0.000023236435,0.00006646816,0.000017787845,0.00025963667,0.000075862634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011672941,0.00026951512,0.0001276726,0.0010732623,0.0013843053,0.0006782551,0.00048382807,0.00024025084,0.011237099],"category_scores_gemma":[0.0005038843,0.00018591138,0.00007810537,0.0013464405,0.00042055637,0.00024832762,0.00027232358,0.00029156957,0.00085474865],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018582023,0.00015485077,0.8055473,0.0002727861,0.000055915167,0.0007917287,0.0027173413,0.0015315163,0.006592428,0.0041474123,0.06503095,0.11297197],"study_design_scores_gemma":[0.000015792426,0.000025182206,0.96172523,0.00003140579,0.000005220395,0.00013059829,0.00062571693,0.0004130809,0.0004940436,0.00005309246,0.036472443,0.000008154658],"about_ca_topic_score_codex":0.99040526,"about_ca_topic_score_gemma":0.9979044,"teacher_disagreement_score":0.01464029,"about_ca_system_score_codex":0.01464029,"about_ca_system_score_gemma":0.01527021,"threshold_uncertainty_score":0.106223226},"labels":[],"label_agreement":null},{"id":"W2910207761","doi":"10.1016/j.jsg.2018.12.012","title":"Hot on the trail: Coseismic heating on a localized structure along the Muddy Mountain fault, Nevada","year":2019,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Slip (aerodynamics); Geology; Slipping; Seismology; Episodic tremor and slip; Thermal; Earthquake rupture; Thrust fault; Subduction; Fault (geology); Tectonics; Geometry; Meteorology","score_opus":0.012781479824464268,"score_gpt":0.22452218059202098,"score_spread":0.21174070076755672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2910207761","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992379,0.000013577383,0.000016902193,0.000028164372,0.0000018175434,0.0000016103587,0.00007006934,0.0000018887894,0.00062816817],"genre_scores_gemma":[0.9994456,0.000015813417,0.000030867006,0.0000090590665,0.0000024403853,0.0000020715704,0.00010253091,0.0000010958069,0.00039058938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996555,0.0000045419474,0.000001507126,0.000009207031,0.0000065678305,0.000012641125],"domain_scores_gemma":[0.99988115,0.000016873715,0.000026432326,0.000008698262,0.000030947675,0.000035813857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007191977,0.00008463314,0.00013833861,0.00038892034,0.00092691684,0.00036169004,0.00030087354,0.00030320225,0.0012738724],"category_scores_gemma":[0.00023939155,0.000093466326,0.000073167364,0.00039804247,0.00035261305,0.00019887096,0.0005026605,0.00019184517,0.00010426622],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022630983,0.00014019864,0.9770602,0.000022185355,0.000037571644,0.00094837596,0.002501028,0.0009877641,0.009497137,0.00023705848,0.00082374254,0.007518405],"study_design_scores_gemma":[0.0000055315677,0.000021210673,0.9965132,0.00000446397,0.000006141514,0.000067649846,0.002276473,0.00039236722,0.00014541108,0.000034034,0.00053113385,0.0000024982783],"about_ca_topic_score_codex":0.13544545,"about_ca_topic_score_gemma":0.45714828,"teacher_disagreement_score":0.13544545,"about_ca_system_score_codex":0.00056282955,"about_ca_system_score_gemma":0.0006561161,"threshold_uncertainty_score":0.2693141},"labels":[],"label_agreement":null},{"id":"W2910564880","doi":"10.1785/0120180233","title":"Do Injection‐Induced Earthquakes Rupture Away from Injection Wells due to Fluid Pressure Change?","year":2019,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Citation; Icon; History; Engineering; Library science; Art history; Geography; Cartography; Computer science","score_opus":0.019231000202181475,"score_gpt":0.21509401895376182,"score_spread":0.19586301875158035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2910564880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6471152,0.027922897,0.0031680758,0.06745495,0.0066440213,0.00015892352,0.020560775,0.0005996488,0.22637552],"genre_scores_gemma":[0.95154744,0.0147465905,0.0006783062,0.00227244,0.0017167827,0.000039831553,0.0066902293,0.00013215083,0.02217618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997509,0.000023203913,0.000026486865,0.000041466876,0.000094791896,0.0000632491],"domain_scores_gemma":[0.99866307,0.00022466079,0.0005453333,0.000060284394,0.0003687145,0.00013789408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000476681,0.0002139153,0.0004456955,0.0011877443,0.0007323208,0.0019706339,0.0004594769,0.0011653306,0.017548129],"category_scores_gemma":[0.0040609688,0.00017577574,0.0003152021,0.002618874,0.00061833614,0.0018718301,0.0010513269,0.0008848896,0.0046028974],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009012772,0.00016944027,0.36903837,0.002769551,0.00047456298,0.0046336777,0.007510232,0.0018784999,0.004352726,0.015864003,0.30894774,0.28345996],"study_design_scores_gemma":[0.00010300528,0.00022783174,0.6602998,0.0011544976,0.00026584027,0.0010031138,0.015711527,0.0018669884,0.0015037454,0.007581315,0.3101641,0.00011822155],"about_ca_topic_score_codex":0.014054823,"about_ca_topic_score_gemma":0.032063637,"teacher_disagreement_score":0.017548129,"about_ca_system_score_codex":0.0010393526,"about_ca_system_score_gemma":0.00081234303,"threshold_uncertainty_score":0.058704317},"labels":[],"label_agreement":null},{"id":"W2910671667","doi":"10.4095/216211","title":"Seismic transects K, L and M","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Transect; Geology; Seismology; Geography; Oceanography","score_opus":0.032953556381760785,"score_gpt":0.2364850594841428,"score_spread":0.20353150310238202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2910671667","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.122075774,0.0004083038,0.0052528167,0.00039763786,0.00051268504,0.0013546307,0.74665743,0.0013105143,0.12203026],"genre_scores_gemma":[0.15486167,0.0010261099,0.016464535,0.00018455197,0.00016443973,0.0011943439,0.6149789,0.00047254268,0.21065296],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9993862,0.000054455402,0.00005832336,0.00013064442,0.00021454647,0.00015578711],"domain_scores_gemma":[0.9973072,0.00018320486,0.00034419989,0.00030594377,0.0015181735,0.00034125627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005219183,0.0013080119,0.00050664874,0.0050344127,0.0012441545,0.00068985904,0.0014403475,0.00063930015,0.021012094],"category_scores_gemma":[0.0019558996,0.0005898302,0.0003265363,0.0041655796,0.00037820553,0.00096890045,0.0007035952,0.0008942684,0.017231025],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021809514,0.0004749576,0.14079592,0.0005495808,0.00013161352,0.00071286183,0.0014390128,0.0023927975,0.012726341,0.0023894145,0.7557224,0.080484174],"study_design_scores_gemma":[0.00022005304,0.00041052088,0.5871724,0.00010901709,0.00012908474,0.00050944136,0.001658356,0.0018566696,0.015672917,0.00043198548,0.39177316,0.00005639031],"about_ca_topic_score_codex":0.1730152,"about_ca_topic_score_gemma":0.3374921,"teacher_disagreement_score":0.1730152,"about_ca_system_score_codex":0.0015598045,"about_ca_system_score_gemma":0.0041146902,"threshold_uncertainty_score":0.3440163},"labels":[],"label_agreement":null},{"id":"W2912591361","doi":"10.1029/2018jb016556","title":"The Thermal Effects of Plate‐Bending‐Related Thickening of the Oceanic Crustal Aquifer in the Nankai Trough and Japan Trench Subduction Zones","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Aquifer; Subduction; Trench; Oceanic crust; Thickening; Petrology; Crust; Trough (economics); Seismology; Geophysics; Geomorphology; Groundwater; Tectonics; Geotechnical engineering","score_opus":0.01671030225566293,"score_gpt":0.2745217362989993,"score_spread":0.25781143404333634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2912591361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905294,0.000021130098,0.00025314066,0.000020973683,0.0000020930731,0.0000026629848,0.00008290451,0.000015302994,0.00054875476],"genre_scores_gemma":[0.999678,0.000014676812,0.00012138513,0.000005166984,8.84202e-7,0.000002959265,0.000055025583,0.0000046197088,0.00011737951],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999087,0.000020805495,0.000005621737,0.00002560482,0.000008758928,0.000030582712],"domain_scores_gemma":[0.99983394,0.000051012674,0.000034052002,0.000018498204,0.000024426014,0.000037962658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018008912,0.0005461603,0.00030549016,0.00034836406,0.0004747554,0.0008101847,0.00060163403,0.0005233315,0.0012881659],"category_scores_gemma":[0.00046654776,0.00040309076,0.00077968434,0.00031303783,0.00062527513,0.00044281685,0.00058014784,0.00032455588,0.00007840409],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093699324,0.000032419623,0.049723573,0.000019319506,0.000077236844,0.000092765025,0.00006405186,0.9420109,0.0064251437,0.00036546102,0.00009201486,0.0010034951],"study_design_scores_gemma":[0.000051732095,0.00007490619,0.058396425,0.000009048177,0.000050538732,0.000030933566,0.00015095217,0.9392342,0.0015203067,0.0002754448,0.00017946643,0.000026085043],"about_ca_topic_score_codex":0.081186205,"about_ca_topic_score_gemma":0.047859065,"teacher_disagreement_score":0.081186205,"about_ca_system_score_codex":0.0018163311,"about_ca_system_score_gemma":0.00067436526,"threshold_uncertainty_score":0.16142732},"labels":[],"label_agreement":null},{"id":"W2913215586","doi":"10.1029/2018jb016499","title":"Beyond Receiver Functions: Green's Function Estimation by Transdimensional Inversion and Its Application to OBS Data","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Japan Society for the Promotion of Science","keywords":"Receiver function; Deconvolution; Algorithm; Computer science; Seismometer; Markov chain Monte Carlo; Geology; Applied mathematics; Bayesian probability; Mathematics; Seismology","score_opus":0.037366614612740094,"score_gpt":0.3019409749755807,"score_spread":0.2645743603628406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2913215586","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.051415626,0.0001570117,0.94754195,0.00011570749,0.000016861974,0.000017734135,0.00007567736,0.00026821974,0.00039115502],"genre_scores_gemma":[0.3812358,0.00038343293,0.6170822,0.00007022555,0.000035159403,0.000068977366,0.00031434154,0.00008216168,0.0007277445],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999665,0.00015708679,0.000022056647,0.000064865075,0.000069306996,0.00002161292],"domain_scores_gemma":[0.9986468,0.00070834334,0.00017282405,0.00018218516,0.00025000153,0.000039839357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013175017,0.0005347377,0.00028379948,0.0010572729,0.00027532165,0.0006154405,0.00056467444,0.0006590824,0.00056894694],"category_scores_gemma":[0.004633774,0.00025483774,0.000494003,0.0010295729,0.0005457891,0.0008553532,0.0008370943,0.0005986608,0.00017195691],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012652138,0.00010203615,0.017799843,0.00016216782,0.00015663511,0.00026597525,0.00033078008,0.6054075,0.04065188,0.024155973,0.0010319798,0.3098087],"study_design_scores_gemma":[0.000005760121,0.000008084022,0.0013808084,0.0000051349657,0.000006177527,0.00003440813,0.000011976604,0.99398744,0.0019930697,0.0021305836,0.00042390305,0.000012631514],"about_ca_topic_score_codex":0.007013403,"about_ca_topic_score_gemma":0.005660094,"teacher_disagreement_score":0.007013403,"about_ca_system_score_codex":0.00036983812,"about_ca_system_score_gemma":0.0007691592,"threshold_uncertainty_score":0.013945162},"labels":[],"label_agreement":null},{"id":"W2914154071","doi":"10.1139/cjes-2018-0260","title":"Evolution of migrating transform faults in anisotropic oceanic crust: examples from Iceland","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"National Science Foundation","keywords":"Transform fault; Geology; Seismology; Plate tectonics; Hotspot (geology); Fault (geology); Rift; Strike-slip tectonics; Mid-ocean ridge; Ridge; Tectonics; Rift zone; Seafloor spreading; Extensional definition; Paleontology; Basalt","score_opus":0.017753102009896816,"score_gpt":0.2028390283221711,"score_spread":0.18508592631227427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914154071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99157226,0.00035426993,0.0003618759,0.00003684216,0.0000029539617,0.000007590139,0.00029933604,0.000016083746,0.007348772],"genre_scores_gemma":[0.9980964,0.00028926352,0.000709336,0.000011266844,0.0000022661225,0.0000020079108,0.00030810444,0.000011942908,0.00056942063],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.0000057826437,0.0000045947263,0.000013179266,0.000008672006,0.000015066201],"domain_scores_gemma":[0.99988043,0.000016625747,0.000040415653,0.0000132369605,0.000030525818,0.000018814015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105449486,0.00023615133,0.00013167107,0.00096546154,0.000569002,0.00060278457,0.00015694718,0.00021338748,0.00096824893],"category_scores_gemma":[0.00030292865,0.00009377692,0.00016155998,0.00094006833,0.0005349832,0.00019371437,0.00035840058,0.0001764407,0.00015880012],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024493787,0.000040933533,0.8939702,0.00013734055,0.000089930065,0.002852123,0.0032009701,0.0093730735,0.04207297,0.0026008643,0.0010449352,0.044371724],"study_design_scores_gemma":[0.0000053483523,0.000021715494,0.9908048,0.000023354227,0.000017855218,0.00069802813,0.0008706605,0.0025184627,0.0016883619,0.00032074586,0.0030210877,0.000009610807],"about_ca_topic_score_codex":0.03844238,"about_ca_topic_score_gemma":0.07062372,"teacher_disagreement_score":0.03844238,"about_ca_system_score_codex":0.0007370762,"about_ca_system_score_gemma":0.00024134554,"threshold_uncertainty_score":0.076437235},"labels":[],"label_agreement":null},{"id":"W2914342647","doi":"10.1029/2019eo114003","title":"Ancient Faults Amplify Intraplate Earthquakes","year":2019,"lang":"en","type":"article","venue":"Eos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Seismology; Geology; Tectonics","score_opus":0.011538261308051889,"score_gpt":0.2053141708631046,"score_spread":0.19377590955505272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914342647","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99042577,0.00013872879,0.0003458112,0.000100074045,0.000006084248,0.000004297267,0.0003463328,0.000032917178,0.008599978],"genre_scores_gemma":[0.9980708,0.000099325924,0.00010456039,0.000013587026,0.0000044695153,8.0227284e-7,0.00014987044,0.0000060992184,0.0015505393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972934,0.00001547542,0.000009799332,0.000035638757,0.0001086112,0.00010114991],"domain_scores_gemma":[0.9986274,0.00019149072,0.00023953445,0.00009753117,0.0007002884,0.00014367675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021161664,0.00019732983,0.00022371992,0.0013833625,0.0007136372,0.0012520457,0.00025379076,0.00027070413,0.0038338837],"category_scores_gemma":[0.0021440673,0.00018295721,0.00009986897,0.001732778,0.0005196633,0.00031446494,0.0007127839,0.0002991762,0.0005486405],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017644922,0.00004031826,0.9196067,0.000066968096,0.000070431255,0.0003733058,0.001584022,0.002791727,0.014324264,0.0017246939,0.0017580095,0.05748328],"study_design_scores_gemma":[0.000004721681,0.00001571852,0.9953987,0.000011404961,0.000018326198,0.0000871585,0.00078918796,0.0008628331,0.0006902003,0.00022158373,0.0018945488,0.000005616425],"about_ca_topic_score_codex":0.49014258,"about_ca_topic_score_gemma":0.80366355,"teacher_disagreement_score":0.49014258,"about_ca_system_score_codex":0.0022458408,"about_ca_system_score_gemma":0.001891196,"threshold_uncertainty_score":0.9745793},"labels":[],"label_agreement":null},{"id":"W2914411227","doi":"10.1007/s00024-019-02116-4","title":"Including Non-Stationary Magnitude–Frequency Distributions in Probabilistic Seismic Hazard Analysis","year":2019,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Microseismic Industry Consortium","keywords":"Induced seismicity; Seismology; Monte Carlo method; Seismic hazard; Geology; Magnitude (astronomy); Probabilistic logic; Statistics; Mathematics; Physics","score_opus":0.010840838908576936,"score_gpt":0.21417468398234543,"score_spread":0.2033338450737685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914411227","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.022989113,0.00030531612,0.9752054,0.00020626537,0.00004416385,0.00002904629,0.0001090727,0.00015610107,0.0009555358],"genre_scores_gemma":[0.9090688,0.0013702717,0.081619225,0.00018172819,0.0003475845,0.00016581165,0.00051465817,0.00029692025,0.0064351046],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9983094,0.00083749456,0.00010214709,0.00020312765,0.00039309074,0.0001548354],"domain_scores_gemma":[0.9750234,0.021638108,0.0010919283,0.0012362148,0.00076830277,0.00024207291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006667829,0.0010198462,0.0013003269,0.0015448594,0.0005869474,0.0013923084,0.0021831712,0.0017647503,0.0021766475],"category_scores_gemma":[0.028723793,0.0015243647,0.0015850238,0.0016394289,0.0016241611,0.0038665175,0.0021392892,0.0021135502,0.0005363855],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027631844,0.000026260117,0.0009606321,0.00003854653,0.000047171794,0.000070971924,0.000027683991,0.9689989,0.00026996864,0.01988978,0.00022540984,0.00941702],"study_design_scores_gemma":[0.000002178125,0.0000060878,0.00020432362,0.0000039086526,0.0000073065526,0.000013929373,0.0000030622507,0.98841596,0.00006831183,0.011176265,0.00009428318,0.0000044093426],"about_ca_topic_score_codex":0.0059364922,"about_ca_topic_score_gemma":0.005522486,"teacher_disagreement_score":0.006667829,"about_ca_system_score_codex":0.00075046485,"about_ca_system_score_gemma":0.0012838,"threshold_uncertainty_score":0.03526324},"labels":[],"label_agreement":null},{"id":"W2914568489","doi":"10.1029/2018jb016221","title":"The 12 November 2017 <i>M</i><sub><i>w</i></sub> 7.3 Ezgeleh‐Sarpolzahab (Iran) Earthquake and Active Tectonics of the Lurestan Arc","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; Canada Research Chairs; Royal Society; Canada Foundation for Innovation; National Science Foundation","keywords":"Geology; Seismology; Aftershock; Basement; Escarpment; Tectonics; Fault (geology); Thrust fault; Induced seismicity; Geomorphology","score_opus":0.02879129617149324,"score_gpt":0.2812676163740509,"score_spread":0.25247632020255767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914568489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99028766,0.00024535484,0.0002391944,0.00026148712,0.00005826176,0.000019444244,0.0015116781,0.000042778007,0.0073342077],"genre_scores_gemma":[0.9932106,0.00022402886,0.0002106006,0.00004629212,0.00009273662,0.0000070982455,0.0032582534,0.000011440796,0.0029389795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999244,0.00000416051,0.000003155628,0.000012732775,0.00002644832,0.000029083363],"domain_scores_gemma":[0.99987245,0.0000036975537,0.000056352823,0.000009445763,0.000034804958,0.000023161077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009225067,0.00018113153,0.00017996055,0.0006512136,0.00026220983,0.0003615144,0.00014090579,0.00017955535,0.0019379457],"category_scores_gemma":[0.00015775845,0.000063401516,0.0001457701,0.0006383367,0.0002861139,0.00015612908,0.00042789325,0.00020446829,0.00053771754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000330306,0.00013737043,0.8855274,0.0001305217,0.000130722,0.0018506467,0.00064020196,0.0013955213,0.017631916,0.00080841326,0.018645747,0.07277117],"study_design_scores_gemma":[0.0000051271436,0.000019634022,0.99504447,0.000007784979,0.000007917732,0.00014844991,0.00017279845,0.00028314858,0.0005169279,0.000046933535,0.0037439545,0.0000027864817],"about_ca_topic_score_codex":0.010305854,"about_ca_topic_score_gemma":0.02239515,"teacher_disagreement_score":0.010305854,"about_ca_system_score_codex":0.0004211058,"about_ca_system_score_gemma":0.00046646732,"threshold_uncertainty_score":0.02049172},"labels":[],"label_agreement":null},{"id":"W2914707416","doi":"10.1016/j.euroneuro.2018.11.451","title":"Admixture analysis for clozapine plasma level monitoring to optimize treatment response","year":2019,"lang":"en","type":"article","venue":"European Neuropsychopharmacology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Schizophrenia Society of Ontario","funders":"","keywords":"Geology; Seismology; Seafloor spreading; Tsunami earthquake; Trench; Fault (geology); Kinematics; Continental shelf; Submarine pipeline; Amplitude; Geodesy; Geotechnical engineering; Oceanography","score_opus":0.04933732204439063,"score_gpt":0.2981018460264366,"score_spread":0.24876452398204596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914707416","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91519153,0.0075288266,0.06486437,0.0008475999,0.0003325884,0.0002453588,0.0050035417,0.000879118,0.005107174],"genre_scores_gemma":[0.9635049,0.00083369715,0.02967914,0.0004425292,0.00013722361,0.000117380856,0.0030162476,0.00014049935,0.0021285],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985562,0.0004249954,0.00011319611,0.00043956246,0.00035716585,0.000108887885],"domain_scores_gemma":[0.99792516,0.00074255664,0.0005917962,0.00026332572,0.0003526636,0.00012442032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022830246,0.00058789336,0.0011891281,0.0018657944,0.0005496159,0.0011790544,0.00083940354,0.0010957344,0.0037718373],"category_scores_gemma":[0.004968064,0.00029726527,0.00080667995,0.0017070563,0.00030893303,0.00045609847,0.0005939832,0.0010869001,0.00074190594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.010572808,0.0009262527,0.5314528,0.0004971211,0.005005814,0.0011232225,0.0004539857,0.009049436,0.115361504,0.0027530545,0.0058075767,0.3169964],"study_design_scores_gemma":[0.0008471877,0.0044705607,0.65447944,0.00025966763,0.006003407,0.0068624048,0.00057472923,0.16453518,0.11338563,0.008879198,0.039394334,0.00030832662],"about_ca_topic_score_codex":0.0015863397,"about_ca_topic_score_gemma":0.0026763424,"teacher_disagreement_score":0.0037718373,"about_ca_system_score_codex":0.00045143906,"about_ca_system_score_gemma":0.0005916683,"threshold_uncertainty_score":0.012618065},"labels":[],"label_agreement":null},{"id":"W2916265432","doi":"10.1029/2018tc005321","title":"Late Quaternary Activity of the La Rinconada Fault Zone, San Juan, Argentina","year":2019,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Quaternary; Seismology; Active fault; Fault (geology); Thrust fault; Latitude; Slip (aerodynamics); Strain partitioning; Main Central Thrust; Tectonics; Paleontology; Geodesy","score_opus":0.011906080458436876,"score_gpt":0.21218083068509014,"score_spread":0.20027475022665325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2916265432","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854887,0.0009555623,0.00011730531,0.00011151957,0.000015615997,0.000016351165,0.0011846881,0.000033187127,0.012076968],"genre_scores_gemma":[0.9948756,0.00075389945,0.0002760614,0.000015539437,0.00001704032,0.000016199547,0.001296454,0.000006106923,0.0027430411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999043,0.000013872361,0.000007956447,0.00003115155,0.000025423773,0.000017260547],"domain_scores_gemma":[0.9997682,0.000021184665,0.00008486337,0.000008325836,0.00009057131,0.000026821433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020232843,0.00021018971,0.00013435095,0.00074580905,0.000345322,0.00058367086,0.00016397345,0.00016091579,0.0010942875],"category_scores_gemma":[0.00035108297,0.00007337985,0.000058710397,0.00085977465,0.00019102634,0.00010786549,0.00019182797,0.0001014688,0.0001693363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017376721,0.00005195343,0.9517656,0.00016991665,0.00004993554,0.0005613737,0.000987149,0.0013545271,0.006505312,0.00045646762,0.002182771,0.035741284],"study_design_scores_gemma":[0.00000633658,0.000018456643,0.994989,0.0000181013,0.0000075139974,0.000076324824,0.00029655232,0.00038335368,0.00015616512,0.00002157648,0.004024629,0.0000020541008],"about_ca_topic_score_codex":0.12235763,"about_ca_topic_score_gemma":0.23330338,"teacher_disagreement_score":0.12235763,"about_ca_system_score_codex":0.0008096856,"about_ca_system_score_gemma":0.00049728504,"threshold_uncertainty_score":0.2432909},"labels":[],"label_agreement":null},{"id":"W2917235444","doi":"10.1016/j.lithos.2019.02.019","title":"Seismicity in Cascadia","year":2019,"lang":"en","type":"article","venue":"Lithos","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior","keywords":"Geology; Induced seismicity; Forearc; Subduction; Seismology; Slab; Convergent boundary; North American Plate; Plate tectonics; Oceanic crust; Volcanic arc; Volcano; Mantle (geology); Mantle wedge; Crust; Slab window; Pacific Plate; Tectonics; Geophysics","score_opus":0.009279969812915968,"score_gpt":0.19706124453809082,"score_spread":0.18778127472517486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2917235444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99614596,0.00011975349,0.0000219229,0.00010914718,0.000004551578,0.000002726298,0.00052270794,0.000015332993,0.0030578943],"genre_scores_gemma":[0.9985507,0.00009675321,0.000029298344,0.0000104087185,0.000004027487,0.000003160813,0.00038082947,0.0000035405064,0.00092123484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988174,0.000019218587,0.000014315997,0.000025807089,0.000018834595,0.000040064224],"domain_scores_gemma":[0.9995254,0.000033090102,0.00013672396,0.000034345674,0.00010701324,0.00016349302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018423442,0.000342385,0.00021319166,0.0028381974,0.00092416845,0.0006620289,0.00027966383,0.00024601768,0.003557727],"category_scores_gemma":[0.0006848481,0.00017289256,0.00021885907,0.0045993705,0.00075134606,0.00025713217,0.0013943984,0.00023868025,0.0004037237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020827896,0.000030294455,0.98082,0.00008098824,0.00009360779,0.0010435014,0.0055477,0.0012692849,0.0017382677,0.00078096084,0.0009859557,0.007401001],"study_design_scores_gemma":[0.000003513326,0.000010541672,0.9977169,0.000005468942,0.000008209056,0.00005006439,0.0011633151,0.00007288148,0.000032487704,0.00003784923,0.00089590537,0.000002774127],"about_ca_topic_score_codex":0.22980443,"about_ca_topic_score_gemma":0.38377425,"teacher_disagreement_score":0.22980443,"about_ca_system_score_codex":0.0020085147,"about_ca_system_score_gemma":0.0014000969,"threshold_uncertainty_score":0.45693362},"labels":[],"label_agreement":null},{"id":"W2917369889","doi":"10.1139/cjes-2018-0289","title":"Continental collisions and the origin of subcrustal continental earthquakes","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Subduction; Mantle (geology); Continental crust; Oceanic crust; Continental shelf; Crust; Seismology; Seafloor spreading; Plate tectonics; Continental collision; Geophysics; Tectonics; Oceanography","score_opus":0.016578233207938702,"score_gpt":0.21634411420927874,"score_spread":0.19976588100134005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2917369889","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99165475,0.0008086057,0.00023746987,0.00019926681,0.000012636796,0.0000043908844,0.00016319803,0.0000050952494,0.006914637],"genre_scores_gemma":[0.99888605,0.00028239875,0.000033058022,0.000020643272,0.000006966676,0.0000010049494,0.00012993481,0.0000018491659,0.0006380082],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998411,0.000020109956,0.000010649286,0.000032691027,0.000027348677,0.0000682151],"domain_scores_gemma":[0.9987764,0.0003010261,0.00043587407,0.00008620637,0.00011566024,0.0002849145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017040646,0.00013568603,0.0001921377,0.00072362,0.00080621114,0.0009812481,0.00032944497,0.000319743,0.004070267],"category_scores_gemma":[0.0018907621,0.00014305564,0.00011108916,0.0009445732,0.0005477481,0.00033883017,0.00091142673,0.00044582953,0.00048353552],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016217408,0.000043033655,0.9764921,0.000023538236,0.000040209907,0.0006997253,0.0011931584,0.0009763975,0.0010170991,0.0070695397,0.0007211518,0.011561897],"study_design_scores_gemma":[0.0000072792845,0.000022291993,0.99314743,0.000008689866,0.000014031161,0.00033601775,0.0013078531,0.0008027322,0.00017964409,0.0022233122,0.0019430522,0.00000760287],"about_ca_topic_score_codex":0.025891077,"about_ca_topic_score_gemma":0.039393924,"teacher_disagreement_score":0.025891077,"about_ca_system_score_codex":0.0007923458,"about_ca_system_score_gemma":0.00043987588,"threshold_uncertainty_score":0.05148071},"labels":[],"label_agreement":null},{"id":"W2918996510","doi":"10.1007/s00024-019-02133-3","title":"Five Great Tsunamis of the 20th Century as Recorded on the Coast of British Columbia","year":2019,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Tide gauge; Bay; Geology; Seismology; Trough (economics); Tsunami wave; Oceanography; Wave height; Crest; Sea level","score_opus":0.005038922346390808,"score_gpt":0.16363813511868583,"score_spread":0.15859921277229502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2918996510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98537123,0.0016553156,0.000048516576,0.00013815064,0.000019532734,0.00001065844,0.0027899416,0.000010091189,0.00995658],"genre_scores_gemma":[0.99175656,0.0019103172,0.00008206595,0.000045609762,0.000009813052,0.000009224253,0.0023568436,0.000004489419,0.0038250952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997937,0.000009284677,0.000027199672,0.000026475094,0.000049814662,0.000093500435],"domain_scores_gemma":[0.99897313,0.000060032395,0.00021495065,0.000023468836,0.00050824817,0.0002201488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001974149,0.00023751025,0.00020497094,0.0042408905,0.0020022371,0.0011033677,0.00035518527,0.00038126428,0.0026821627],"category_scores_gemma":[0.0010498096,0.00016708668,0.0001361225,0.0059946217,0.00068562204,0.0005091359,0.0012598855,0.00045755817,0.00029532236],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021895238,0.000035238554,0.93539965,0.0003055405,0.00012954586,0.0017451721,0.012457753,0.0005369168,0.0020885132,0.00078001374,0.0039854525,0.042317294],"study_design_scores_gemma":[0.0000014131849,0.0000072018797,0.9902942,0.00005942645,0.000011989857,0.00011377319,0.0032838772,0.00004386477,0.00006978741,0.000022273956,0.006084662,0.000007461659],"about_ca_topic_score_codex":0.8892811,"about_ca_topic_score_gemma":0.9782792,"teacher_disagreement_score":0.110718906,"about_ca_system_score_codex":0.005717801,"about_ca_system_score_gemma":0.004631538,"threshold_uncertainty_score":0.22274184},"labels":[],"label_agreement":null},{"id":"W2919567880","doi":"10.1111/1755-6724.13757","title":"Pseudotachylyte‐Induced Weakness of Plate‐Boundary Fault: Insight from the Indus‐Tsangpo Suture between India and Asia","year":2019,"lang":"en","type":"article","venue":"Acta Geologica Sinica - English Edition","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Chinese Academy of Sciences; National Science Foundation","keywords":"Fibrous joint; Geology; Indus; Brittleness; Felsic; Fault (geology); Shear (geology); Shear zone; Geochemistry; Petrology; Seismology; Mafic; Materials science; Tectonics; Composite material; Paleontology; Anatomy; Structural basin","score_opus":0.01778063396517377,"score_gpt":0.21456976355227167,"score_spread":0.1967891295870979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2919567880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990402,0.00014236971,0.000101958794,0.0000133102085,0.0000019548224,0.0000014769529,0.00004325325,0.0000041216786,0.00065142824],"genre_scores_gemma":[0.99974114,0.00005860886,0.000050139373,0.000004104688,0.0000017735379,7.5406916e-7,0.000042559917,0.0000012352231,0.000099676494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999591,0.0000032656947,0.000003839062,0.000010609638,0.000008961979,0.000014261343],"domain_scores_gemma":[0.9998739,0.000017268434,0.000048509428,0.000009512946,0.000028934717,0.000021794545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009378032,0.00014291918,0.00013306554,0.0012768522,0.0003678456,0.00040908888,0.00019652619,0.00020775825,0.0012344809],"category_scores_gemma":[0.00020287666,0.000112639915,0.00012965927,0.00082926,0.00045108373,0.00024544037,0.00044621775,0.00016381423,0.00011736391],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031470723,0.000032985987,0.63197565,0.00019447903,0.00005421381,0.001403918,0.0020947254,0.0003645828,0.34997824,0.00038528926,0.00008413729,0.01311706],"study_design_scores_gemma":[0.0000028431655,0.000042270243,0.99212074,0.000010599011,0.000019556926,0.00053915894,0.0009988996,0.00040110134,0.0052985204,0.00009869849,0.0004625003,0.0000050060307],"about_ca_topic_score_codex":0.0053470335,"about_ca_topic_score_gemma":0.007904142,"teacher_disagreement_score":0.0053470335,"about_ca_system_score_codex":0.00022513173,"about_ca_system_score_gemma":0.00021313573,"threshold_uncertainty_score":0.010631859},"labels":[],"label_agreement":null},{"id":"W2919839500","doi":"10.4095/313636","title":"Superimposed auriferous structural events along the Llewellyn-Tally Ho deformation corridor in southern Yukon and northwest British Columbia","year":2019,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Geography; Seismology; Archaeology; Physical geography","score_opus":0.013867525955651359,"score_gpt":0.20807224053431542,"score_spread":0.19420471457866406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2919839500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99608177,0.00015582443,0.000031512496,0.00008329148,0.000004336633,0.000008293064,0.0004203883,0.0000138915,0.0032005925],"genre_scores_gemma":[0.9968946,0.00013118959,0.00006340817,0.00003258409,0.000001237225,0.000007883734,0.00039359467,0.000005953503,0.0024695077],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997811,0.0000111401105,0.000011612929,0.00004854579,0.000044437544,0.000103213824],"domain_scores_gemma":[0.9995223,0.000025680894,0.00006474396,0.000016727186,0.0002405865,0.00013001164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001090007,0.00020300457,0.00024871007,0.0015165457,0.0027592673,0.0014820632,0.0004743055,0.00040940664,0.0040006125],"category_scores_gemma":[0.00047235572,0.00023366974,0.00014575565,0.0023580615,0.0009196032,0.00026945322,0.0010000989,0.00033946132,0.00027724242],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014750249,0.00003562337,0.9574147,0.00007563363,0.000076835975,0.0012047628,0.004647968,0.0007749705,0.008401253,0.00047499733,0.0022957448,0.024450058],"study_design_scores_gemma":[0.0000028137772,0.0000037206667,0.99560875,0.000016048169,0.000007070483,0.00005496972,0.0026957884,0.00014484527,0.00010659554,0.000016752176,0.0013360948,0.000006592351],"about_ca_topic_score_codex":0.9726662,"about_ca_topic_score_gemma":0.99541,"teacher_disagreement_score":0.027333796,"about_ca_system_score_codex":0.010806112,"about_ca_system_score_gemma":0.009240911,"threshold_uncertainty_score":0.07840419},"labels":[],"label_agreement":null},{"id":"W2920096496","doi":"10.5382/econgeo.2019.4621","title":"3-D Modeling of the Lisheen and Silvermines Deposits, County Tipperary, Ireland:Insights into Structural Controls on the Formation of Irish Zn-Pb Deposits","year":2019,"lang":"en","type":"article","venue":"Economic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Teck (Canada)","funders":"","keywords":"Geology; Dolomitization; Ordovician; Fault (geology); Petrology; Geochemistry; Mineralization (soil science); Shear zone; Facies; Paleontology; Tectonics; Structural basin","score_opus":0.008609891237414702,"score_gpt":0.18655718377545358,"score_spread":0.17794729253803887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2920096496","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9718416,0.00014989774,0.011174301,0.00029415466,0.000034283785,0.00008996622,0.005324121,0.00069322524,0.010398443],"genre_scores_gemma":[0.99268204,0.00009015863,0.0045264238,0.000032407344,0.000006257921,0.000035772893,0.0013504894,0.00009310649,0.0011832844],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999795,0.000024489485,0.000015290181,0.000055182747,0.00004912991,0.000060941973],"domain_scores_gemma":[0.99971825,0.00008892626,0.000043141958,0.000033958462,0.00006506878,0.000050587543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028431026,0.0005053578,0.00050018425,0.0010004891,0.0004934535,0.0019993056,0.0011668308,0.0015636889,0.0022806916],"category_scores_gemma":[0.0010216619,0.0007835963,0.001136505,0.0008993144,0.00092952704,0.00043060823,0.00072901236,0.0004984879,0.000730323],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077095974,0.00007033116,0.021001546,0.000047343918,0.00004404777,0.00025954956,0.00019407061,0.970425,0.0030265292,0.000570073,0.0009035107,0.0033809755],"study_design_scores_gemma":[0.000025208048,0.000012950858,0.011496043,0.0000138168625,0.00001109944,0.000051833675,0.00016056794,0.9869305,0.00038057554,0.00019437044,0.00070048944,0.000022527838],"about_ca_topic_score_codex":0.10707133,"about_ca_topic_score_gemma":0.107896805,"teacher_disagreement_score":0.10707133,"about_ca_system_score_codex":0.0013559742,"about_ca_system_score_gemma":0.0016882931,"threshold_uncertainty_score":0.21289623},"labels":[],"label_agreement":null},{"id":"W2922383903","doi":"10.1029/2018jb016894","title":"Along‐Strike Variations in Structure of the Continent‐Ocean Transition at the Northeastern Nova Scotia Margin From Wide‐Angle Seismic Observations","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Offshore Energy Research Association","keywords":"Geology; Crust; Oceanic crust; Mantle (geology); Transition zone; Continental crust; Continental margin; Nova scotia; Seismology; Petrology; Geophysics; Subduction; Tectonics; Oceanography","score_opus":0.03158199170843658,"score_gpt":0.2691691222688853,"score_spread":0.23758713056044872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2922383903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967289,0.00006314788,0.000115684314,0.000026622492,0.0000034158977,0.000006621158,0.0011055305,0.000015140076,0.001934856],"genre_scores_gemma":[0.99890494,0.000038026836,0.00007584076,0.000007271391,7.0265435e-7,0.0000023503953,0.0005270429,0.0000030690564,0.0004406809],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999453,0.000004708728,0.0000034799907,0.000016235455,0.000012547295,0.00001778895],"domain_scores_gemma":[0.99978286,0.00001899777,0.00004324237,0.00001444351,0.00008884096,0.000051647203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011375613,0.0002112002,0.00009576293,0.0005723971,0.00033224962,0.000700403,0.00018525313,0.00015795186,0.0014163535],"category_scores_gemma":[0.0004595111,0.00015935831,0.00019074624,0.00045754178,0.00021326198,0.00011472379,0.0003279721,0.00010874209,0.00024457395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008438862,0.000012585991,0.97803885,0.0000229968,0.000060664188,0.00017965568,0.00024922675,0.009791881,0.0058421637,0.00017681303,0.0006131571,0.0049276077],"study_design_scores_gemma":[0.0000042810066,0.0000045275688,0.99603975,0.000008536245,0.000005696026,0.000016703612,0.000103105085,0.0033445498,0.00011462934,0.000015461685,0.00033969383,0.0000031529069],"about_ca_topic_score_codex":0.8311496,"about_ca_topic_score_gemma":0.88658524,"teacher_disagreement_score":0.16885042,"about_ca_system_score_codex":0.0021802462,"about_ca_system_score_gemma":0.0016290147,"threshold_uncertainty_score":0.3396896},"labels":[],"label_agreement":null},{"id":"W2923321653","doi":"10.1029/2018jb017150","title":"Delayed Dynamic Triggering of Disposal‐Induced Earthquakes Observed by a Dense Array in Northern Oklahoma","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Induced seismicity; Geology; Fault (geology); Slip (aerodynamics)","score_opus":0.036051078539376086,"score_gpt":0.2992183321221412,"score_spread":0.26316725358276516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2923321653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99936515,0.000014591578,0.000020643585,0.000023638888,7.5846623e-7,0.0000034398265,0.00022582764,0.0000037096258,0.0003422368],"genre_scores_gemma":[0.9996082,0.000016969909,0.000036096975,0.000008697786,0.0000018637363,0.0000061685364,0.00018448624,8.050964e-7,0.00013673228],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990773,0.000009196986,0.000007195531,0.000022956741,0.000012910692,0.000040101542],"domain_scores_gemma":[0.9994943,0.00006634955,0.00018975008,0.000038185735,0.00007642492,0.00013490026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011876486,0.00014424171,0.00019028211,0.0008874688,0.000856599,0.00053434103,0.0002855533,0.00028497755,0.0014294813],"category_scores_gemma":[0.00044122394,0.00015478727,0.000097967684,0.0010311415,0.0003235688,0.00030129208,0.00078495726,0.0002320397,0.00013629251],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014037674,0.000091469985,0.98396033,0.000029246603,0.000044912522,0.00047630531,0.0012475987,0.0005677886,0.006901916,0.0000527989,0.00036167348,0.0061256383],"study_design_scores_gemma":[0.000003064077,0.000011391193,0.99847096,0.0000043873924,0.000006713943,0.0000320731,0.0008155528,0.00025339666,0.00017992075,0.0000062246313,0.00021322619,0.0000030587778],"about_ca_topic_score_codex":0.16206475,"about_ca_topic_score_gemma":0.32148325,"teacher_disagreement_score":0.16206475,"about_ca_system_score_codex":0.0013947284,"about_ca_system_score_gemma":0.00083542377,"threshold_uncertainty_score":0.3222428},"labels":[],"label_agreement":null},{"id":"W2923621790","doi":"10.1139/cjes-2018-0315","title":"A new approach to the opening of the eastern Mediterranean Sea and the origin of the Hellenic subduction zone. Part 2: The Hellenic subduction zone","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Lithosphere; Seismology; Accretionary wedge; Transform fault; Trough (economics); Paleontology; Fault (geology); Tectonics","score_opus":0.03807487843882709,"score_gpt":0.2164341174955975,"score_spread":0.1783592390567704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2923621790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84440786,0.031194976,0.06935311,0.0037733396,0.0010495997,0.00013380419,0.0007397633,0.00045613607,0.04889136],"genre_scores_gemma":[0.95871097,0.0067095915,0.026959116,0.0006634987,0.00033242727,0.000048259168,0.0004904708,0.000117557385,0.0059679337],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999174,0.000014080499,0.000007236513,0.0000327353,0.000015505826,0.000013059581],"domain_scores_gemma":[0.999881,0.000022458187,0.000036666934,0.00002886924,0.000013447446,0.00001745854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002759797,0.00047302057,0.00029369353,0.0013866805,0.0005482741,0.0018403077,0.0006680724,0.00093897444,0.0041581327],"category_scores_gemma":[0.0010308258,0.00022895179,0.00045426135,0.00076559465,0.0016070909,0.0019844992,0.0018109583,0.0011236046,0.0005325746],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006469137,0.00016740912,0.24524339,0.001200904,0.00054494716,0.00660387,0.022273976,0.031133415,0.10748829,0.21002437,0.0062228004,0.36844978],"study_design_scores_gemma":[0.00018868521,0.00025828535,0.5049087,0.00088273326,0.00029574177,0.005196441,0.0075851292,0.05335846,0.007647274,0.14367466,0.27579075,0.00021312495],"about_ca_topic_score_codex":0.0048233154,"about_ca_topic_score_gemma":0.005268044,"teacher_disagreement_score":0.0048233154,"about_ca_system_score_codex":0.0011289427,"about_ca_system_score_gemma":0.00041342308,"threshold_uncertainty_score":0.013910353},"labels":[],"label_agreement":null},{"id":"W2924090640","doi":"10.1139/cjes-2018-0118","title":"Research on the fracture structure and activity of the Qinling Mountains thrust nappe system in western Hubei","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Nappe; Outcrop; Fault (geology); Active fault; Quaternary; Pleistocene; Thrust fault; Paleontology; Tectonics","score_opus":0.04078378779502766,"score_gpt":0.2678025888430302,"score_spread":0.22701880104800254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2924090640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989103,0.00016930744,0.00037288052,0.000026156149,0.0000011286139,0.0000057938237,0.00007440152,0.0000051287766,0.00043502732],"genre_scores_gemma":[0.99909973,0.000117772106,0.00029637734,0.000009583825,0.0000013993906,0.0000045275056,0.00010484802,0.0000011210457,0.0003645921],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991655,0.000007724658,0.0000044454773,0.00002718701,0.000022586291,0.000021596019],"domain_scores_gemma":[0.9998795,0.00001650025,0.000032602802,0.000006465536,0.00004349634,0.000021382906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026199067,0.00019872045,0.00013174517,0.0012806783,0.00048477997,0.00023577543,0.00026102527,0.00016525741,0.00056436856],"category_scores_gemma":[0.00019600784,0.00011106152,0.00014812294,0.0011289604,0.00031443196,0.0002963476,0.00019048904,0.00010274527,0.000034322977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000544149,0.000039008144,0.9232802,0.00014137322,0.00010172035,0.0009070742,0.0028395192,0.0024756857,0.034620795,0.0008076314,0.00023258699,0.034500096],"study_design_scores_gemma":[0.0000015581811,0.00002634579,0.9976756,0.0000037546347,0.000014558284,0.000080596124,0.00045463914,0.00080547296,0.0004008633,0.00003806634,0.00049355865,0.000005006644],"about_ca_topic_score_codex":0.099850684,"about_ca_topic_score_gemma":0.25513968,"teacher_disagreement_score":0.099850684,"about_ca_system_score_codex":0.00086092897,"about_ca_system_score_gemma":0.0010842765,"threshold_uncertainty_score":0.19853896},"labels":[],"label_agreement":null},{"id":"W2925748543","doi":"10.1029/2019gl081991","title":"Induced Seismicity Reduces Seismic Hazard?","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismic hazard; Seismology; Crust; Hazard; Earthquake prediction; Geophysics","score_opus":0.04515377888619912,"score_gpt":0.29191313938782837,"score_spread":0.24675936050162925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2925748543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9534287,0.0007917248,0.0047700396,0.008515688,0.00013306353,0.000021920385,0.0004817679,0.00011375765,0.03174327],"genre_scores_gemma":[0.9988127,0.00013591844,0.0001509084,0.00024206477,0.000041220035,0.0000027788428,0.000054316562,0.0000067807728,0.0005532928],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99974495,0.000065295986,0.000016056852,0.00007435128,0.000040236857,0.000059018646],"domain_scores_gemma":[0.9954869,0.0015737314,0.001854575,0.00031160522,0.000259895,0.0005132443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007942284,0.00018151413,0.00024609882,0.00028680213,0.00019279083,0.0007514324,0.00049106963,0.00073218305,0.013949996],"category_scores_gemma":[0.009340836,0.00015344031,0.00016859456,0.00031256964,0.0009881053,0.0010163921,0.00071290886,0.0007672098,0.0007204936],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027244862,0.0019327255,0.5321278,0.0018944489,0.0006613477,0.0021770024,0.0018187298,0.04836102,0.056290068,0.15440096,0.024860535,0.17275093],"study_design_scores_gemma":[0.0001619743,0.0012730605,0.75194365,0.00014437128,0.00023794833,0.0011426009,0.0026185291,0.019458594,0.007079799,0.19461296,0.021253677,0.00007287996],"about_ca_topic_score_codex":0.001462644,"about_ca_topic_score_gemma":0.0016206778,"teacher_disagreement_score":0.013949996,"about_ca_system_score_codex":0.0006729821,"about_ca_system_score_gemma":0.00034744415,"threshold_uncertainty_score":0.046667337},"labels":[],"label_agreement":null},{"id":"W2928771298","doi":"10.7185/geochemlet.1907","title":"Onset of new, progressive crustal growth in the central Slave craton at 3.55 Ga","year":2019,"lang":"en","type":"article","venue":"Geochemical Perspectives Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Government of Northwest Territories; University of Alberta","funders":"","keywords":"Craton; Geology; Seismology; Tectonics","score_opus":0.007782134645520965,"score_gpt":0.20541636109035996,"score_spread":0.197634226444839,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2928771298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866474,0.00019003535,0.000100373654,0.000015201168,0.0000017704156,0.0000024685921,0.00010560188,0.0000076054816,0.0009121293],"genre_scores_gemma":[0.9992362,0.00010834457,0.00012727441,0.000008568166,0.0000016280428,0.0000014864836,0.00013722092,0.0000038438966,0.0003754989],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996877,0.0000015991693,0.000002016814,0.000012784542,0.000006136858,0.000008711619],"domain_scores_gemma":[0.99992454,0.000009156986,0.000023829714,0.000010115543,0.000018536224,0.000013797369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011652322,0.00015879012,0.00017667201,0.0008542626,0.00029741524,0.0003887724,0.00014239397,0.00017949495,0.0013265149],"category_scores_gemma":[0.00022337397,0.00013922167,0.00018461164,0.00054102653,0.0006229099,0.00016602041,0.00040415215,0.00018878431,0.00015193057],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000340086,0.000020254127,0.7586978,0.0001637512,0.00010428194,0.0021687811,0.0036089227,0.0011866736,0.20555137,0.000906854,0.000281383,0.026969858],"study_design_scores_gemma":[0.0000020628904,0.0000137266,0.998256,0.0000067325773,0.000006441454,0.00017804577,0.00013994912,0.00012754717,0.00068475574,0.000026175436,0.00055648404,0.0000020210082],"about_ca_topic_score_codex":0.027103288,"about_ca_topic_score_gemma":0.05445112,"teacher_disagreement_score":0.027103288,"about_ca_system_score_codex":0.00042427648,"about_ca_system_score_gemma":0.00029239358,"threshold_uncertainty_score":0.053891003},"labels":[],"label_agreement":null},{"id":"W2930585901","doi":"10.4095/296795","title":"Regional centroid moment tensor solutions for eastern Canadian earthquakes: 2011-2013","year":2015,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Centroid; Moment tensor; Moment (physics); Seismology; Geology; Tensor (intrinsic definition); Geodesy; Geography; Mathematics; Physics; Geometry; Classical mechanics","score_opus":0.1112213293128314,"score_gpt":0.26573107391492784,"score_spread":0.15450974460209643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2930585901","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9312399,0.00076545094,0.002951759,0.00025660812,0.000030785995,0.00007678381,0.056308117,0.00035690205,0.008013814],"genre_scores_gemma":[0.9495298,0.0007303422,0.006836053,0.000021400094,0.000011617265,0.00002809083,0.039132744,0.00008333427,0.0036264323],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997093,0.000008231609,0.000022732733,0.000040557643,0.00012953766,0.00008958771],"domain_scores_gemma":[0.9985638,0.000037051937,0.00017136743,0.00005189811,0.0010672901,0.00010847868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036645553,0.0006557029,0.00029092425,0.003365005,0.001293981,0.00072611833,0.0008268759,0.00038140206,0.0020000127],"category_scores_gemma":[0.0019542389,0.0002673069,0.0004585836,0.005840066,0.0003348214,0.00047329205,0.00062777055,0.0004358524,0.00053566566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052041124,0.00011514192,0.74195963,0.00053085235,0.00042383946,0.00091676187,0.0016900228,0.05214839,0.015594501,0.0017742579,0.024879856,0.1594464],"study_design_scores_gemma":[0.000025045367,0.000021996331,0.9782879,0.000026836926,0.00007323417,0.00013630268,0.0007494489,0.012392299,0.0026785762,0.0001279454,0.0054073525,0.00007319004],"about_ca_topic_score_codex":0.9669175,"about_ca_topic_score_gemma":0.9899047,"teacher_disagreement_score":0.033082485,"about_ca_system_score_codex":0.009428373,"about_ca_system_score_gemma":0.0096378345,"threshold_uncertainty_score":0.06840789},"labels":[],"label_agreement":null},{"id":"W2932579196","doi":"10.1016/j.jseaes.2019.03.023","title":"Differential crustal deformation across the Cona-Oiga rift, southern Tibetan Plateau","year":2019,"lang":"en","type":"article","venue":"Journal of Asian Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Geology; Rift; Plateau (mathematics); Tributary; Tectonics; Geomorphology; Cenozoic; Fluvial; Tectonic uplift; Mountain formation; Seismology; Paleontology; Structural basin; Geography","score_opus":0.013290254974418204,"score_gpt":0.22982281488752418,"score_spread":0.21653255991310597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2932579196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989454,0.00006621921,0.000015313186,0.000017173983,0.0000015131252,0.0000017455006,0.000112613234,0.0000027984547,0.00083724014],"genre_scores_gemma":[0.99957913,0.000025955938,0.000014698136,0.000005323489,0.000001688517,0.0000017400973,0.00012796202,7.1193676e-7,0.00024290383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993026,0.000010087682,0.0000049495948,0.000020020201,0.000009969863,0.000024588424],"domain_scores_gemma":[0.9998423,0.000022478636,0.00003628534,0.000009331661,0.000044480712,0.000045203637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023549347,0.00028928136,0.0002070878,0.0012781175,0.00066878233,0.0008414504,0.00026492853,0.000293714,0.001590034],"category_scores_gemma":[0.00038426768,0.00014712744,0.00017328355,0.001951982,0.0005024725,0.0002852592,0.0004418207,0.00015629143,0.000156962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036968605,0.000059537495,0.9734727,0.000058354985,0.00010862212,0.00051830936,0.001647847,0.0011899899,0.010785331,0.00022360965,0.00024583156,0.011320174],"study_design_scores_gemma":[0.0000038570083,0.0000123377795,0.99921215,0.000002893961,0.0000056662298,0.000024740464,0.00035657317,0.00024134589,0.000033460536,0.0000137490015,0.00009176054,0.0000014244866],"about_ca_topic_score_codex":0.10916982,"about_ca_topic_score_gemma":0.19306235,"teacher_disagreement_score":0.10916982,"about_ca_system_score_codex":0.00085674925,"about_ca_system_score_gemma":0.00077799446,"threshold_uncertainty_score":0.21706873},"labels":[],"label_agreement":null},{"id":"W2934560943","doi":"10.1029/2018gc008167","title":"Fluid and Melt Pathways in the Central Chilean Subduction Zone Near the 2010 Maule Earthquake (35–36°S) as Inferred From Magnetotelluric Data","year":2019,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Fondo de Financiamiento de Centros de Investigación en Áreas Prioritarias; Centro de Excelencia en Geotermia de Los Andes; National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Subduction; Magnetotellurics; Seismology; Forearc; Volcano; Volcanic arc; Slab; Crust; Induced seismicity; Mantle (geology); Tectonics; Petrology; Geophysics","score_opus":0.01589969915590891,"score_gpt":0.19251203917196671,"score_spread":0.1766123400160578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2934560943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99858284,0.00010842189,0.000058042362,0.00004132957,0.000001225833,0.000005348349,0.00052564725,0.000015498204,0.0006617987],"genre_scores_gemma":[0.99914193,0.00007061258,0.00011909484,0.000005078412,0.0000018624654,0.000005615037,0.00046253036,0.0000032851106,0.00018994983],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999409,0.000006032312,0.000006153172,0.000016100084,0.000012496452,0.000018263283],"domain_scores_gemma":[0.9997615,0.000039677972,0.00008012825,0.00001408029,0.000065942324,0.00003874937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001405778,0.00023811564,0.00018709057,0.0018611327,0.00032112902,0.0007469833,0.00026736018,0.0002916463,0.0011031716],"category_scores_gemma":[0.0006411692,0.0002377105,0.00020157803,0.0013088208,0.00031266708,0.00031098028,0.0005412403,0.00016264597,0.00016261124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028969935,0.00006277886,0.95393896,0.0001292152,0.00008936701,0.0006061592,0.0019582973,0.0062349006,0.02275879,0.00037062232,0.0006317872,0.012929348],"study_design_scores_gemma":[0.000016108272,0.000012575284,0.9940403,0.0000229036,0.000012667921,0.000041379943,0.00071954896,0.003646862,0.0005936842,0.00006471378,0.0008185189,0.000010717004],"about_ca_topic_score_codex":0.101822235,"about_ca_topic_score_gemma":0.091681875,"teacher_disagreement_score":0.101822235,"about_ca_system_score_codex":0.0010713051,"about_ca_system_score_gemma":0.0006189413,"threshold_uncertainty_score":0.2024591},"labels":[],"label_agreement":null},{"id":"W2935865199","doi":"10.1139/cjes-2018-0306","title":"Quaternary evolution of the Suluova Basin: implications on tectonics and palaeonvironments of the Central North Anatolian Shear Zone","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Structural basin; Quaternary; Sinistral and dextral; Paleontology; Transtension; Pull apart basin; Graben; Shear zone; Tectonics; Early Pleistocene; Fault (geology); Geomorphology; Pleistocene; Sedimentary basin","score_opus":0.01215424588129474,"score_gpt":0.18797478377612498,"score_spread":0.17582053789483024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2935865199","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973648,0.00045281564,0.000057159406,0.000090667694,0.000005719684,0.000002454688,0.00011322485,0.0000071426193,0.0019059732],"genre_scores_gemma":[0.9993142,0.00020174227,0.00007875486,0.0000112314265,0.0000028948803,0.000002260628,0.00012360304,0.0000042249158,0.00026117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999465,0.000007768715,0.000006579548,0.000018381437,0.000006678924,0.000014083459],"domain_scores_gemma":[0.9999443,0.000005176806,0.00001959573,0.000004074326,0.000017313912,0.000009531479],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014900448,0.00016720669,0.0001417809,0.00086907047,0.00052856683,0.0007840176,0.00020028255,0.00019654007,0.001671717],"category_scores_gemma":[0.00021479638,0.00013039737,0.0001459274,0.0007676424,0.0004032339,0.00031128997,0.00044162554,0.00011922054,0.00018833556],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001964051,0.00006184052,0.9095129,0.00015362562,0.00013653871,0.0012445075,0.004193377,0.0018900463,0.02297389,0.0028405134,0.0008085367,0.055987988],"study_design_scores_gemma":[0.00000591032,0.000013948009,0.9952128,0.000027247013,0.000017982455,0.00021945863,0.0007487287,0.00067369,0.00035836417,0.00017458714,0.00254287,0.0000043645223],"about_ca_topic_score_codex":0.019461192,"about_ca_topic_score_gemma":0.03601153,"teacher_disagreement_score":0.019461192,"about_ca_system_score_codex":0.00086808525,"about_ca_system_score_gemma":0.00061503967,"threshold_uncertainty_score":0.038695812},"labels":[],"label_agreement":null},{"id":"W2937651902","doi":"10.1029/2018jb017039","title":"Induced Seismicity Driven by Fluid Diffusion Revealed by a Near‐Field Hydraulic Stimulation Monitoring Array in the Montney Basin, British Columbia","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Research School, Ruhr University Bochum","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Seismology; Seismometer; Poromechanics; Geotechnical engineering","score_opus":0.024480550376738904,"score_gpt":0.2877279363336582,"score_spread":0.26324738595691927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937651902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866056,0.000022499567,0.000087163375,0.000026191365,7.475947e-7,0.000005305198,0.00031145537,0.00001244451,0.0008736719],"genre_scores_gemma":[0.99912506,0.000022130846,0.00012040546,0.000008852696,8.020656e-7,0.0000042739944,0.00020484197,0.0000018028619,0.0005118357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998603,0.000010132986,0.0000053101635,0.000032479777,0.000050025985,0.00004164767],"domain_scores_gemma":[0.99960095,0.000031619547,0.00006702342,0.00001873189,0.00019226818,0.00008940798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010254275,0.00014751262,0.0001771423,0.00106869,0.00070154865,0.00051631016,0.0003597015,0.00022223893,0.00078399846],"category_scores_gemma":[0.00042562748,0.00014915843,0.00006354994,0.0013434816,0.00037633642,0.00016034128,0.00049072894,0.00018282747,0.00009995738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001403898,0.00007410097,0.93909734,0.000030880514,0.00004745833,0.0003961635,0.00133565,0.0021669467,0.033187293,0.00013885483,0.0010606643,0.022324136],"study_design_scores_gemma":[0.0000033304982,0.00001068606,0.9973029,0.000003899239,0.0000049924847,0.000029224168,0.00051426,0.0011529005,0.00042237152,0.000011883975,0.00053729303,0.000006258701],"about_ca_topic_score_codex":0.9017951,"about_ca_topic_score_gemma":0.9676001,"teacher_disagreement_score":0.09820491,"about_ca_system_score_codex":0.0033198723,"about_ca_system_score_gemma":0.0030342282,"threshold_uncertainty_score":0.19756645},"labels":[],"label_agreement":null},{"id":"W2938190979","doi":"10.1139/cjes-2018-0308","title":"Spatio-temporal behaviour of continental transform faults: implications from the late Quaternary slip history of the North Anatolian Fault, Turkey","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"North Anatolian Fault; Geology; Quaternary; Seismology; Slip (aerodynamics); Geodetic datum; Shear (geology); Shear zone; Fault (geology); Tectonics; Geodesy; Paleontology","score_opus":0.019209395409923533,"score_gpt":0.20616830059460775,"score_spread":0.18695890518468422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2938190979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99895597,0.00013987478,0.000090140784,0.00003939529,0.0000032101002,0.0000013434023,0.00027125468,0.0000057536668,0.00049297855],"genre_scores_gemma":[0.9996216,0.00004899446,0.000043157997,0.000002606732,0.0000016641959,9.769709e-7,0.0002071167,0.0000019244642,0.00007193098],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999871,0.00001866401,0.000019115709,0.000051905667,0.000013810651,0.000025540277],"domain_scores_gemma":[0.9996025,0.00006364205,0.00013238726,0.00003503357,0.00012641243,0.00003998502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034599655,0.00016815656,0.0001790056,0.0010917,0.00027750633,0.00072737946,0.00027882386,0.0003393301,0.00091288815],"category_scores_gemma":[0.0009615916,0.00014130837,0.00021807171,0.0009358382,0.00030181732,0.0004034979,0.00025594223,0.00014905407,0.00019315405],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010108253,0.000019687322,0.9849899,0.000024233863,0.000063962245,0.00026167705,0.00033811879,0.005247375,0.002199238,0.00027688098,0.00025496844,0.0062229494],"study_design_scores_gemma":[0.0000021334542,0.000010324718,0.9946241,0.000007835463,0.000013533264,0.00007284169,0.0002488784,0.004530554,0.0001432242,0.000055572433,0.00028711476,0.0000038768344],"about_ca_topic_score_codex":0.03136913,"about_ca_topic_score_gemma":0.045103192,"teacher_disagreement_score":0.03136913,"about_ca_system_score_codex":0.0008366008,"about_ca_system_score_gemma":0.0003104903,"threshold_uncertainty_score":0.062373042},"labels":[],"label_agreement":null},{"id":"W2938293596","doi":"","title":"Analyse du potentiel tsunamigénique des glissements de terrain possibles dans une ancienne mine à ciel ouvert à Black Lake, Québec","year":2016,"lang":"fr","type":"article","venue":"Corpus Université Laval (Université Laval)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Humanities; Art","score_opus":0.010175433801958018,"score_gpt":0.17960659129788006,"score_spread":0.16943115749592205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2938293596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9810575,0.00020750295,0.005999114,0.0004169243,0.000018328694,0.000054254415,0.0012917579,0.000105591906,0.010848948],"genre_scores_gemma":[0.9892313,0.00016278894,0.0022353532,0.000039941722,0.000003134612,0.000034278975,0.00065346534,0.00003386036,0.0076058526],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980384,0.000018517521,0.000007923559,0.000047629666,0.00006181567,0.000060312923],"domain_scores_gemma":[0.9994747,0.00017407704,0.000039335388,0.000021633463,0.00024080755,0.000049491544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040498827,0.0005393701,0.00047385728,0.000832244,0.0011354068,0.0017539322,0.0007467353,0.0009164364,0.0041969176],"category_scores_gemma":[0.0014257337,0.00044730862,0.0007118037,0.0010667264,0.00072277954,0.0006654296,0.0005885257,0.0008316047,0.00032927416],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023645737,0.00006552522,0.08672997,0.00017878176,0.00012592167,0.0008530169,0.00067976274,0.885713,0.008432631,0.002842083,0.0019698495,0.0121730305],"study_design_scores_gemma":[0.000047389643,0.00009102313,0.10985708,0.00006732806,0.00009432433,0.00008055564,0.0015262185,0.8801308,0.0027648676,0.0010075175,0.004240703,0.00009210663],"about_ca_topic_score_codex":0.9279125,"about_ca_topic_score_gemma":0.93473905,"teacher_disagreement_score":0.07208753,"about_ca_system_score_codex":0.00880645,"about_ca_system_score_gemma":0.0072429194,"threshold_uncertainty_score":0.14502406},"labels":[],"label_agreement":null},{"id":"W2939712114","doi":"10.1029/2019gl082202","title":"The 2016 M7 Kumamoto, Japan, Earthquake Slip Field Derived From a Joint Inversion of Differential Lidar Topography, Optical Correlation, and InSAR Surface Displacements","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Centre National d’Etudes Spatiales; Canada Excellence Research Chairs, Government of Canada; European Space Agency; Institut de Radioprotection et de SÛreté Nucléaire; Arizona State University; National Science Foundation","keywords":"Geology; Interferometric synthetic aperture radar; Seismology; Slip (aerodynamics); Geodesy; Lidar; Synthetic aperture radar; Crust; Remote sensing; Geophysics","score_opus":0.01997087330812671,"score_gpt":0.247361497002225,"score_spread":0.2273906236940983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2939712114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987141,0.000024014138,0.0006387439,0.000034917615,0.0000045914335,0.000004049932,0.00019355828,0.000023180997,0.0003627405],"genre_scores_gemma":[0.9981078,0.000023351098,0.001190637,0.000008411223,0.0000042427237,0.0000039054316,0.0005017125,0.0000067505875,0.00015310572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999279,0.000010924506,0.000005072978,0.000021723861,0.000017282893,0.000017103059],"domain_scores_gemma":[0.9998461,0.000019068257,0.00004203112,0.000020244466,0.0000424444,0.00003002471],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022338802,0.00035173693,0.00034742447,0.0005284167,0.000244853,0.00035910463,0.00033714288,0.00039989644,0.0005181182],"category_scores_gemma":[0.00058981136,0.000321291,0.00030158923,0.0007027665,0.0002533056,0.00028683356,0.00045242193,0.00026125458,0.00020366376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004497074,0.0003465049,0.7070282,0.00016368186,0.00037231357,0.0014928433,0.00057950953,0.12445875,0.09455584,0.0011037485,0.00283967,0.066609204],"study_design_scores_gemma":[0.000067490815,0.000108501496,0.64134324,0.000033738892,0.000099314406,0.00017672605,0.00042427034,0.3509576,0.005525524,0.0002757346,0.0009404496,0.000047487712],"about_ca_topic_score_codex":0.019048912,"about_ca_topic_score_gemma":0.039543316,"teacher_disagreement_score":0.019048912,"about_ca_system_score_codex":0.00039552257,"about_ca_system_score_gemma":0.0008549323,"threshold_uncertainty_score":0.03787607},"labels":[],"label_agreement":null},{"id":"W2943107310","doi":"10.1007/s11069-019-03614-3","title":"Numerical modelling of coastal inundation from Cascadia Subduction Zone tsunamis and implications for coastal communities on western Vancouver Island, Canada","year":2019,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; BC Hydro (Canada)","funders":"U.S. Geological Survey; U.S. Department of Agriculture","keywords":"Bathymetry; Subduction; Geology; Hydrogeology; Natural hazard; Seismology; Tsunami earthquake; Magnitude (astronomy); Geotechnical engineering; Oceanography; Tectonics","score_opus":0.016554915936373354,"score_gpt":0.21785747215302956,"score_spread":0.20130255621665621,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2943107310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923968,0.00007679126,0.0005360222,0.00020224202,0.000019138715,0.000023787507,0.00070894003,0.000042228006,0.0059939167],"genre_scores_gemma":[0.9964568,0.00009829746,0.00038241223,0.00001798062,0.0000036261745,0.000016408021,0.00030539936,0.000016358275,0.0027026236],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998097,0.000027553482,0.000011899959,0.000033486358,0.00003501925,0.00008230556],"domain_scores_gemma":[0.99925345,0.00016605429,0.000055143762,0.0000262719,0.00032410683,0.00017493908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002704142,0.00072373275,0.000579667,0.0009520783,0.002968611,0.0028567214,0.0019024668,0.0015536672,0.0036120212],"category_scores_gemma":[0.0018784344,0.00069375546,0.0006639573,0.0018624692,0.0013220948,0.0005624863,0.0009387629,0.0010183312,0.0002789491],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012704736,0.0001168487,0.04618558,0.000038910373,0.000054650733,0.00036876372,0.00032807037,0.94657755,0.0007278291,0.0011263737,0.0014488649,0.002899618],"study_design_scores_gemma":[0.000054345943,0.000028465829,0.03134373,0.00002295554,0.000031365253,0.000028385804,0.0016043474,0.96522474,0.0002181316,0.00039630855,0.0010073686,0.000039818857],"about_ca_topic_score_codex":0.9813851,"about_ca_topic_score_gemma":0.9784153,"teacher_disagreement_score":0.018614888,"about_ca_system_score_codex":0.017470652,"about_ca_system_score_gemma":0.012914094,"threshold_uncertainty_score":0.12675905},"labels":[],"label_agreement":null},{"id":"W2943587111","doi":"10.1029/2018gl081766","title":"Spatiotemporal Variations in Crustal Seismic Anisotropy Surrounding Induced Earthquakes Near Fox Creek, Alberta","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Alberta","funders":"National Natural Science Foundation of China; Natural Environment Research Council; Sight Research UK; University of Alberta","keywords":"Geology; Seismology; Induced seismicity; Anisotropy; Shear wave splitting; Focal mechanism; Shear (geology); Seismic anisotropy; Hydraulic fracturing; Sedimentary rock; Fault (geology); Slip (aerodynamics); Geophysics; Petrology; Geotechnical engineering; Geochemistry","score_opus":0.04029212198769172,"score_gpt":0.2879887591184396,"score_spread":0.24769663713074785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2943587111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982273,0.00004234978,0.00010981524,0.000015658456,0.0000013445391,0.0000047492535,0.00054278254,0.0000068930894,0.001049234],"genre_scores_gemma":[0.9983663,0.000046581652,0.000109113935,0.000005671204,0.000001621751,0.0000027043818,0.0006452739,0.0000017728969,0.00082081585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998714,0.000007478629,0.000004096415,0.000028219232,0.00004867688,0.000040280574],"domain_scores_gemma":[0.9995628,0.0000434528,0.00008499738,0.000016664748,0.00022090354,0.00007121805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012179852,0.00012789277,0.00015649693,0.00106278,0.00051016675,0.0005588937,0.0003122176,0.00015064653,0.0010116956],"category_scores_gemma":[0.00057691766,0.00010510454,0.00006821615,0.0015129087,0.00033262296,0.00012785108,0.00031534367,0.00011551152,0.00012892485],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019380564,0.000035276924,0.959339,0.000026057633,0.00005497735,0.00038614855,0.0017930886,0.0012922317,0.018977763,0.00013918009,0.00078283314,0.016979594],"study_design_scores_gemma":[0.0000011948367,0.000004393013,0.9988943,0.000002089191,0.0000033394158,0.000020714715,0.00039986084,0.00022663969,0.00017942648,0.000006737569,0.00025890645,0.0000025115953],"about_ca_topic_score_codex":0.8185466,"about_ca_topic_score_gemma":0.93211704,"teacher_disagreement_score":0.1814534,"about_ca_system_score_codex":0.002431211,"about_ca_system_score_gemma":0.0015743056,"threshold_uncertainty_score":0.365044},"labels":[],"label_agreement":null},{"id":"W2943981462","doi":"10.3390/min9050282","title":"Mathematical Modelling of Fault Reactivation Induced by Water Injection","year":2019,"lang":"en","type":"article","venue":"Minerals","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Nuclear Safety Commission","funders":"Lawrence Berkeley National Laboratory; Canadian Nuclear Safety Commission; Office of Science; Eidgenössisches Nuklearsicherheitsinspektorat; Institut de Radioprotection et de SÛreté Nucléaire; Korea Atomic Energy Research Institute; Japan Atomic Energy Agency; Office of Nuclear Energy; Nuclear Waste Management Organization; U.S. Department of Energy","keywords":"Fault (geology); Permeability (electromagnetism); Pore water pressure; Radioactive waste; Geology; Induced seismicity; Shear (geology); Geotechnical engineering; Petrology; Seismology; Engineering; Chemistry; Waste management","score_opus":0.03429959870662383,"score_gpt":0.22205534549092956,"score_spread":0.18775574678430573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2943981462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5365162,0.0012581272,0.4127399,0.0016456142,0.00020975957,0.00016703781,0.0011022672,0.0004489678,0.045912094],"genre_scores_gemma":[0.9846006,0.00030911426,0.0062711257,0.00006608876,0.00002768889,0.00013455992,0.00017134585,0.00004727265,0.008372164],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981946,0.00005518515,0.000012448559,0.000038763817,0.00003291584,0.00004131616],"domain_scores_gemma":[0.99907994,0.00052244146,0.00018903143,0.00003557552,0.00012061929,0.000052366082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005015633,0.00065512914,0.00076391257,0.00060364837,0.00051387737,0.0010779965,0.0010910928,0.0022127419,0.0019801294],"category_scores_gemma":[0.002306527,0.00043733045,0.00081759423,0.00044085731,0.0012363596,0.00080664497,0.00094450207,0.00093553105,0.00022197464],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013206302,0.000012945152,0.00037109217,0.000020431784,0.00000754506,0.000049364375,0.000031795742,0.9927643,0.0008572358,0.0052979086,0.000097911914,0.00047632866],"study_design_scores_gemma":[0.000003843501,0.0000059097883,0.000097369746,0.0000019358986,0.0000027611977,0.0000045832835,0.000007340338,0.9990609,0.000087090855,0.0006208624,0.000104962295,0.000002497453],"about_ca_topic_score_codex":0.014768801,"about_ca_topic_score_gemma":0.0053368276,"teacher_disagreement_score":0.014768801,"about_ca_system_score_codex":0.0011754312,"about_ca_system_score_gemma":0.0008790411,"threshold_uncertainty_score":0.029365718},"labels":[],"label_agreement":null},{"id":"W2944230280","doi":"10.1016/j.tecto.2019.04.031","title":"Dramatic Pliocene–Quaternary subsidence of the southern Rhodes Basin and concomitant north-tilting and uplift of the Anaximander Mountains, the junction of Hellenic and Cyprus arcs, eastern Mediterranean Sea","year":2019,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Quaternary; Paleontology; Structural basin; Subsidence; Clockwise; Neogene; Geomorphology; Fold (higher-order function)","score_opus":0.012997960369659934,"score_gpt":0.19111050562625273,"score_spread":0.17811254525659279,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2944230280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99221295,0.00048146961,0.00009032718,0.0005437756,0.00002463015,0.000008074063,0.0003793419,0.000012126801,0.006247304],"genre_scores_gemma":[0.99727386,0.0003515006,0.00007163753,0.000101934726,0.00001909803,0.0000047164262,0.0002943372,0.0000048231786,0.0018781191],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999471,0.0000065489085,0.0000064711057,0.000016699796,0.000011236653,0.0000120674895],"domain_scores_gemma":[0.99988055,0.000007631157,0.000044257347,0.000015011921,0.000032692195,0.000019897978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017600719,0.000102574726,0.00009344289,0.0003848372,0.0004029436,0.0005866787,0.00013878309,0.00025558524,0.0034206924],"category_scores_gemma":[0.0004388928,0.00008876693,0.00011850908,0.00043192419,0.0004891204,0.0002446836,0.00046833433,0.00032219314,0.00031347832],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044799168,0.000101006604,0.8061518,0.00041332887,0.00034332406,0.0045024054,0.0059968554,0.0018352302,0.10195294,0.0048139193,0.005419265,0.068021975],"study_design_scores_gemma":[0.0000026295804,0.000007869052,0.9951197,0.000007043964,0.0000049305863,0.00020329923,0.00029791484,0.00005204433,0.0002482169,0.00002623355,0.004028641,0.0000016021717],"about_ca_topic_score_codex":0.034088757,"about_ca_topic_score_gemma":0.07794249,"teacher_disagreement_score":0.034088757,"about_ca_system_score_codex":0.00057871826,"about_ca_system_score_gemma":0.0006568622,"threshold_uncertainty_score":0.06778067},"labels":[],"label_agreement":null},{"id":"W2944407712","doi":"10.1193/041618eqs095m","title":"Increases in Life‐Safety Risks to Building Occupants from Induced Earthquakes in the Central United States","year":2019,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Federal Emergency Management Agency; National Science Foundation","keywords":"Induced seismicity; Fragility; Seismic hazard; Seismic risk; Seismology; Hazard; Natural hazard; Earthquake scenario; Ground motion; Building code; Risk assessment; Geology; Magnitude (astronomy); Environmental science; Forensic engineering; Engineering; Geography; Civil engineering; Meteorology; Computer science","score_opus":0.029603778030738218,"score_gpt":0.25589108483374495,"score_spread":0.22628730680300674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2944407712","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99876535,0.00004133902,0.00022254296,0.000048100894,0.000002595731,0.0000052405912,0.00026567673,0.0000106174575,0.00063851883],"genre_scores_gemma":[0.9994178,0.000041330375,0.000094680814,0.000012092279,0.0000013719573,0.0000030644594,0.000310081,0.0000010708706,0.00011851242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984694,0.000035972964,0.0000085048905,0.000024307772,0.00005738872,0.000027017302],"domain_scores_gemma":[0.9993119,0.00014902017,0.00024603834,0.000050313043,0.00017985312,0.000062897365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004198978,0.00029455218,0.000116122246,0.00047069223,0.0001771874,0.00044169184,0.00025579074,0.00028854894,0.0006455816],"category_scores_gemma":[0.0014914492,0.00014775532,0.00022479048,0.00039545848,0.00018780153,0.00031289342,0.000451216,0.0003090049,0.00008508257],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018042572,0.00013004542,0.9441493,0.00003301335,0.0001142451,0.00031472387,0.00054570904,0.039098468,0.0015742739,0.00043550224,0.0014700221,0.011954171],"study_design_scores_gemma":[0.0000062853096,0.00013486769,0.9749527,0.000020225205,0.000028056947,0.000086975706,0.0008072638,0.022295507,0.0006932764,0.00029018513,0.00066825404,0.00001625189],"about_ca_topic_score_codex":0.05535473,"about_ca_topic_score_gemma":0.09343055,"teacher_disagreement_score":0.05535473,"about_ca_system_score_codex":0.0009082205,"about_ca_system_score_gemma":0.00037383448,"threshold_uncertainty_score":0.11006504},"labels":[],"label_agreement":null},{"id":"W2944704635","doi":"10.4138/atlgeol.2019.002","title":"Sonar and LiDAR investigation of lineaments offshore between central New England and the New England seamounts, USA","year":2019,"lang":"en","type":"article","venue":"Atlantic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lineament; Geology; Seamount; Seismology; Fault scarp; Canyon; Terrane; Bathymetry; Submarine pipeline; Magnetic anomaly; Bathymetric chart; Geomorphology; Oceanography; Fault (geology); Paleontology; Tectonics","score_opus":0.012335776746754819,"score_gpt":0.2002089018914511,"score_spread":0.18787312514469628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2944704635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961533,0.00014508366,0.00015974141,0.000052065356,0.0000055637734,0.00001582493,0.0010034943,0.000014946607,0.0024499884],"genre_scores_gemma":[0.99350476,0.00018411272,0.00069852563,0.00006762938,0.000006223246,0.00004026467,0.0012233148,0.000005968872,0.004269086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999058,0.00000585252,0.0000096886215,0.00002935554,0.00003175214,0.000017631819],"domain_scores_gemma":[0.9995597,0.000034963778,0.00010912441,0.000019266268,0.00022026757,0.00005652894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012227039,0.00014033726,0.00012726152,0.0009937604,0.00047653494,0.00047492763,0.000319832,0.00017992179,0.0012723792],"category_scores_gemma":[0.00038982957,0.00018199156,0.00007355843,0.0012963512,0.0002487492,0.0003294569,0.0005129373,0.00012910175,0.00026004383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007176914,0.000039211685,0.96668106,0.0000439554,0.000039388928,0.00079847523,0.0021777623,0.00037114936,0.008146594,0.00008307323,0.0016099123,0.019937644],"study_design_scores_gemma":[0.0000023810644,0.000010841924,0.9965184,0.000009441581,0.000006679771,0.00008735463,0.0013056605,0.00018563725,0.00019845119,0.00000672273,0.0016656445,0.0000027731367],"about_ca_topic_score_codex":0.3562785,"about_ca_topic_score_gemma":0.7519118,"teacher_disagreement_score":0.3562785,"about_ca_system_score_codex":0.0007152863,"about_ca_system_score_gemma":0.00072372454,"threshold_uncertainty_score":0.7084095},"labels":[],"label_agreement":null},{"id":"W2945666249","doi":"10.2172/1511856","title":"Probabilistic Seismic Hazard Assessment for Georgia","year":2019,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic hazard; Hazard; Building code; Scope (computer science); Eurocode; Seismic risk; Christian ministry; Seismology; Civil engineering; Engineering; Forensic engineering; Geology; Computer science; Political science; Law","score_opus":0.04325037294680099,"score_gpt":0.29114998587153057,"score_spread":0.2478996129247296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2945666249","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.086070396,0.0044741333,0.41737425,0.005367058,0.000672315,0.0017148021,0.039715845,0.0075952867,0.43701592],"genre_scores_gemma":[0.73837805,0.006792915,0.16542467,0.0009719193,0.0002215927,0.0012082922,0.037351225,0.00073291163,0.048918445],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99929833,0.00020668434,0.000041294785,0.00009848953,0.00028666915,0.00006854144],"domain_scores_gemma":[0.99889827,0.00018672679,0.00012826275,0.00013195944,0.0005798127,0.00007496442],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012435106,0.0010053992,0.00033844245,0.0036238732,0.00057073415,0.0016723322,0.001038354,0.0007118481,0.009024764],"category_scores_gemma":[0.003623114,0.00036573346,0.00087426393,0.0031947598,0.00049696426,0.0010645807,0.0020925046,0.0010635422,0.0041761776],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022027029,0.000082620354,0.03133717,0.0007940318,0.00014565157,0.0008108939,0.0009861517,0.2156054,0.0039262036,0.12898721,0.1907164,0.42638808],"study_design_scores_gemma":[0.00005533716,0.00027894118,0.069567434,0.0008723893,0.00012608615,0.0010047054,0.0011315658,0.24349359,0.0018378305,0.12481753,0.5565844,0.00023019001],"about_ca_topic_score_codex":0.049270637,"about_ca_topic_score_gemma":0.054494604,"teacher_disagreement_score":0.049270637,"about_ca_system_score_codex":0.0031693953,"about_ca_system_score_gemma":0.0041006655,"threshold_uncertainty_score":0.097967684},"labels":[],"label_agreement":null},{"id":"W2946120984","doi":"10.1002/essoar.10500976.1","title":"The importance of pre-existing fracture networks for fault reactivation during hydraulic fracturing","year":2019,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Hydraulic fracturing; Induced seismicity; Geology; Seismology; Fracture (geology); Microseism; Pore water pressure; Fault (geology); Seismometer; Geotechnical engineering; Petrology; Petroleum engineering","score_opus":0.020498728410244492,"score_gpt":0.25151827743673066,"score_spread":0.23101954902648617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946120984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936027,0.0001399089,0.0021248837,0.00003703909,0.0000030741571,0.000012692762,0.0024932434,0.00008824533,0.0014982031],"genre_scores_gemma":[0.9960765,0.00007469771,0.0010698133,0.000004055185,0.0000025297782,0.0000051896,0.0024688877,0.0000071055897,0.00029119986],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998834,0.0000077936475,0.000005409159,0.000030501578,0.000031092575,0.000041776482],"domain_scores_gemma":[0.9996232,0.000084879954,0.00010386834,0.000042690655,0.00008804899,0.000057223147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013477901,0.00017130982,0.00016954051,0.001165978,0.00029096947,0.00063002843,0.0003188,0.00030498175,0.0013041085],"category_scores_gemma":[0.0008521906,0.00012847153,0.00012484095,0.0010501721,0.00043000584,0.00033605407,0.00041756645,0.00024021215,0.00014754175],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031101942,0.00008007336,0.89289296,0.00015563611,0.00008099244,0.00086152507,0.0009788948,0.023593653,0.047655277,0.001496227,0.0011893344,0.030704262],"study_design_scores_gemma":[0.000004231271,0.000013668405,0.985756,0.0000126632285,0.000012141567,0.000095499454,0.0003341529,0.010684963,0.001699444,0.00032870154,0.0010494617,0.0000090417025],"about_ca_topic_score_codex":0.099539116,"about_ca_topic_score_gemma":0.2417533,"teacher_disagreement_score":0.099539116,"about_ca_system_score_codex":0.000709187,"about_ca_system_score_gemma":0.0007948478,"threshold_uncertainty_score":0.19791943},"labels":[],"label_agreement":null},{"id":"W2946789848","doi":"10.1029/2018jb016885","title":"Frictional State Evolution During Normal Stress Perturbations Probed With Ultrasonic Waves","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation of Sri Lanka; Pennsylvania State University; University of Pennsylvania; National Science Foundation","keywords":"Amplitude; Shearing (physics); Slip (aerodynamics); Mechanics; Shear (geology); Geology; Ultrasonic sensor; Materials science; Stress (linguistics); Shear stress; Seismology; Geotechnical engineering; Composite material; Physics; Optics; Acoustics; Thermodynamics","score_opus":0.017218088273376293,"score_gpt":0.2646196022364902,"score_spread":0.24740151396311394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946789848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994993,0.000014983645,0.00035930652,0.000003550334,7.940927e-7,0.00000147216,0.00001565976,0.0000072688586,0.000097602635],"genre_scores_gemma":[0.9998325,0.000009460063,0.0000868782,0.0000012649591,4.5869652e-7,0.0000013261614,0.000015630181,0.0000011655983,0.00005129447],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999212,0.000009479434,0.0000037468778,0.000014873785,0.000025161504,0.000025574782],"domain_scores_gemma":[0.99988234,0.00003629818,0.00003094998,0.0000135414475,0.000018937451,0.000017902912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000118285316,0.00013076344,0.00016755702,0.00021385451,0.00010898885,0.00030058943,0.00018043787,0.0001774603,0.00047640482],"category_scores_gemma":[0.00043099525,0.00012080448,0.00008393215,0.00016725836,0.0003207817,0.00021459431,0.0002676818,0.00018541908,0.00007601233],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003556076,0.00008841092,0.019920213,0.000028402588,0.000016841142,0.0001735766,0.00026323082,0.0054437574,0.96847576,0.0001688486,0.000056438123,0.0050088554],"study_design_scores_gemma":[0.00004988359,0.0015134292,0.3193924,0.000012027472,0.000041523457,0.00035619488,0.00096855994,0.1306463,0.5456502,0.00044832597,0.0008687922,0.000052280546],"about_ca_topic_score_codex":0.00092793914,"about_ca_topic_score_gemma":0.0005843883,"teacher_disagreement_score":0.00092793914,"about_ca_system_score_codex":0.00019128917,"about_ca_system_score_gemma":0.00008993454,"threshold_uncertainty_score":0.0018450618},"labels":[],"label_agreement":null},{"id":"W2946928834","doi":"10.1029/2018jb017043","title":"Stable Forearc Stressed by a Weak Megathrust: Mechanical and Geodynamic Implications of Stress Changes Caused by the M = 9 Tohoku‐Oki Earthquake","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Forearc; Geology; Differential stress; Seismology; Wedge (geometry); Subduction; Submarine pipeline; Tectonics; Deformation (meteorology); Geotechnical engineering; Geometry","score_opus":0.02721908828681515,"score_gpt":0.29467757197549105,"score_spread":0.2674584836886759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946928834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999681,0.000012398109,0.00008586367,0.000009628512,9.897609e-7,0.0000013608759,0.000027925822,0.0000035961214,0.00017726823],"genre_scores_gemma":[0.9998766,0.0000105277,0.000033399167,0.0000032157839,6.962717e-7,0.0000010612097,0.000029236226,0.0000010194193,0.000044170396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995077,0.0000034521543,0.000004687092,0.000011805461,0.000008404299,0.000020803815],"domain_scores_gemma":[0.99987805,0.000012434895,0.000039402446,0.000012249841,0.000022903076,0.000034930614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001137558,0.00023512081,0.00027250487,0.00046880625,0.00044754302,0.00047105562,0.00035700263,0.0004315328,0.0008465863],"category_scores_gemma":[0.00023046827,0.00028929877,0.00031190252,0.0003741509,0.000487158,0.00025256138,0.0004218529,0.00022930831,0.00011129613],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072420173,0.000269393,0.77821845,0.00010023234,0.0001751372,0.0037224304,0.0005609518,0.046054494,0.15612641,0.00064218475,0.00027443006,0.013131689],"study_design_scores_gemma":[0.000011303655,0.0001099849,0.96841484,0.000006210725,0.00003931548,0.00018408503,0.0005417207,0.027260423,0.003113381,0.00015320974,0.00014646756,0.000019049005],"about_ca_topic_score_codex":0.0097235795,"about_ca_topic_score_gemma":0.014711264,"teacher_disagreement_score":0.0097235795,"about_ca_system_score_codex":0.0005045088,"about_ca_system_score_gemma":0.00024765046,"threshold_uncertainty_score":0.019333959},"labels":[],"label_agreement":null},{"id":"W2947131279","doi":"10.1139/cjes-2018-0283","title":"Reconstructing the deformation of the North Anatolian Fault Zone through restoring the Oligo–Miocene exhumation pattern of the Almacık Block (northwestern Turkey) based on the apatite (U–Th)/He ages","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Block (permutation group theory); Fault (geology); Tectonics; Seismology; North Anatolian Fault; Neogene; Paleontology; Structural basin","score_opus":0.024015422171736307,"score_gpt":0.20470261234638573,"score_spread":0.18068719017464943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947131279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965653,0.00044617587,0.0008263348,0.00008796317,0.000019799028,0.000007859543,0.0006896395,0.00009764075,0.0012592406],"genre_scores_gemma":[0.99853635,0.000115634866,0.00063190545,0.000006269024,0.0000059786653,0.0000030813064,0.0004844789,0.000019290499,0.00019703648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998914,0.000013845537,0.000009268508,0.000047788035,0.000012163928,0.000025445763],"domain_scores_gemma":[0.9998585,0.00001449674,0.000035071793,0.000020309479,0.000048179358,0.000023437722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024302005,0.00058847026,0.00025425068,0.0018011917,0.0003674273,0.0008627853,0.00048488952,0.00084777334,0.001643296],"category_scores_gemma":[0.00058857346,0.00037657827,0.00037785704,0.0011187365,0.00029981666,0.00039820094,0.00046714323,0.00022788442,0.0005146737],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011289857,0.00020304529,0.6490647,0.0003168164,0.0005843281,0.0029796357,0.0009379219,0.24749,0.043366726,0.0014831959,0.0022888323,0.05015578],"study_design_scores_gemma":[0.00017096954,0.00009632503,0.63400495,0.000091092224,0.00024593013,0.0005613627,0.0007825093,0.35586727,0.0029295308,0.00056022673,0.004627949,0.00006192201],"about_ca_topic_score_codex":0.04499765,"about_ca_topic_score_gemma":0.056686733,"teacher_disagreement_score":0.04499765,"about_ca_system_score_codex":0.000737568,"about_ca_system_score_gemma":0.00078784686,"threshold_uncertainty_score":0.08947152},"labels":[],"label_agreement":null},{"id":"W2947534168","doi":"10.1139/cjes-2018-0321","title":"Active transform faults in the Gulf of Guinea: insights from geophysical data and implications for seismic hazard assessment","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Transform fault; Seismic hazard; Tectonics; Transtension; Seismotectonics; Active fault; Fault (geology); Strain partitioning; Induced seismicity; Plate tectonics; Rift","score_opus":0.036828523129992935,"score_gpt":0.27119562085918136,"score_spread":0.23436709772918843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947534168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99661046,0.0003739761,0.0003439081,0.00025928367,0.000004983778,0.000012302849,0.0005011078,0.000009591763,0.0018842921],"genre_scores_gemma":[0.99782526,0.0007582801,0.0008562606,0.000022502712,0.000011465717,0.0000068872187,0.00038316133,0.0000029774526,0.00013318063],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998921,0.00003445011,0.000012102506,0.00001292567,0.000021210986,0.000027162454],"domain_scores_gemma":[0.99922276,0.0002648104,0.0003166127,0.000037983256,0.00009469683,0.00006312712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005652328,0.0002652986,0.00018013772,0.0031191972,0.00017403747,0.0009316719,0.00027460884,0.0003866402,0.0013453189],"category_scores_gemma":[0.0020978076,0.00015083814,0.00016704574,0.0026429924,0.0004902841,0.0007293146,0.00057944073,0.00026641032,0.00014029138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000071173876,0.000078131794,0.9495524,0.000089898625,0.000038350012,0.0007116679,0.001122409,0.0029898614,0.0020813432,0.0009616679,0.0002516117,0.042051386],"study_design_scores_gemma":[0.000009400633,0.000032558757,0.99022174,0.00009651674,0.000021920461,0.000246772,0.0019713228,0.00497083,0.00022518872,0.00073835836,0.0014535816,0.000011839374],"about_ca_topic_score_codex":0.021283796,"about_ca_topic_score_gemma":0.032988593,"teacher_disagreement_score":0.021283796,"about_ca_system_score_codex":0.00065534277,"about_ca_system_score_gemma":0.0004894014,"threshold_uncertainty_score":0.042319834},"labels":[],"label_agreement":null},{"id":"W2948502197","doi":"10.1016/j.epsl.2019.05.016","title":"Enigmatic upper-plate sliver transport paused by megathrust earthquake and afterslip","year":2019,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Seismology; Trench; Subduction; Slip (aerodynamics); Oblique case; Geodesy; Tectonics; Physics","score_opus":0.005489328217360942,"score_gpt":0.16792249285294142,"score_spread":0.16243316463558047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2948502197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9435154,0.0044217706,0.001904644,0.012147179,0.00067269197,0.000012366705,0.0014130888,0.0001558091,0.035757095],"genre_scores_gemma":[0.99391407,0.0015530661,0.0002555638,0.00041597415,0.00035016844,0.000003559902,0.00041771613,0.000041468385,0.0030484428],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999064,0.000008242559,0.0000058030373,0.000034077697,0.000012783477,0.00003265549],"domain_scores_gemma":[0.99965143,0.00006454498,0.000090661924,0.00007202429,0.000062909916,0.00005834307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004579969,0.00025029937,0.0002577394,0.0008783826,0.00070669886,0.0015517126,0.00056506693,0.0010873439,0.0050044116],"category_scores_gemma":[0.0013848183,0.0002003471,0.00024007913,0.0012365192,0.0012048044,0.0020197683,0.0011318065,0.0013024036,0.0007279027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012422452,0.00014282123,0.70990276,0.000572348,0.00037966095,0.00361022,0.013602679,0.0068655633,0.022070365,0.07235663,0.029544136,0.13971056],"study_design_scores_gemma":[0.000027652128,0.00010146766,0.92602605,0.00020875003,0.00009604364,0.00050479296,0.011626991,0.0027643573,0.0009469048,0.016075345,0.04156868,0.000052896317],"about_ca_topic_score_codex":0.015381597,"about_ca_topic_score_gemma":0.019659938,"teacher_disagreement_score":0.015381597,"about_ca_system_score_codex":0.00075992546,"about_ca_system_score_gemma":0.0006495211,"threshold_uncertainty_score":0.030584157},"labels":[],"label_agreement":null},{"id":"W2949589824","doi":"10.5194/se-11-95-2020","title":"Fault zone architecture of a large plate-bounding strike-slip fault: a case study from the Alpine Fault, New Zealand","year":2020,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"RWTH Aachen University; Deutsche Forschungsgemeinschaft; Royal Society Te Apārangi; Royal Society","keywords":"Geology; Seismology; Fault (geology); Strike-slip tectonics; Slip (aerodynamics); Fault scarp; Fault gouge; Engineering","score_opus":0.026125662761126225,"score_gpt":0.25561759674507045,"score_spread":0.22949193398394424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2949589824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978682,0.00008098139,0.00017059228,0.000051477356,0.0000010431808,0.000027425436,0.000092350565,0.0000030749952,0.0017048585],"genre_scores_gemma":[0.9987552,0.00015868315,0.0003895704,0.0000073951587,0.0000017189906,0.000007256876,0.000070914386,0.0000023639795,0.00060689007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983144,0.0000287178,0.000012696405,0.000028823768,0.000053036965,0.000045247052],"domain_scores_gemma":[0.99965835,0.00007678882,0.00012155105,0.000025760903,0.000056622146,0.000061002833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023165041,0.0004180263,0.0002785186,0.0011756765,0.0013241784,0.0009599439,0.0005581111,0.0005357563,0.0012768377],"category_scores_gemma":[0.0011127467,0.00023098369,0.0002856873,0.0016118791,0.0012850894,0.0004519646,0.0005649011,0.0003089207,0.000119035954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000572011,0.00045733285,0.76904124,0.00055864506,0.00015292005,0.10461275,0.026293084,0.009254546,0.03426987,0.0020311128,0.0013822563,0.051374223],"study_design_scores_gemma":[0.00005090439,0.00025132144,0.9634611,0.00007668089,0.00006360246,0.009362319,0.017208619,0.0038974776,0.0011677545,0.00023690029,0.0041900296,0.00003327105],"about_ca_topic_score_codex":0.461767,"about_ca_topic_score_gemma":0.6565355,"teacher_disagreement_score":0.461767,"about_ca_system_score_codex":0.0032436685,"about_ca_system_score_gemma":0.000999079,"threshold_uncertainty_score":0.9181584},"labels":[],"label_agreement":null},{"id":"W2950677086","doi":"10.3389/fbuil.2019.00073","title":"Lessons Learnt From the 2009 Padang Indonesia, 2011 Tōhoku Japan and 2016 Muisne Ecuador Earthquakes","year":2019,"lang":"en","type":"article","venue":"Frontiers in Built Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Engineering and Physical Sciences Research Council; University College London; Great Britain Sasakawa Foundation; Institution of Structural Engineers","keywords":"Landslide; Seismic hazard; Settlement (finance); Liquefaction; Geotechnical engineering; Engineering; Civil engineering; Forensic engineering; Geology; Seismology","score_opus":0.010062874812994758,"score_gpt":0.18520058899065187,"score_spread":0.1751377141776571,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2950677086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88428336,0.024768285,0.001467657,0.053149596,0.0024526494,0.000057019173,0.0015778409,0.00011582287,0.032127686],"genre_scores_gemma":[0.95336866,0.025720818,0.0018560669,0.0049590515,0.0012741679,0.00002818848,0.0009349701,0.00008437303,0.011773754],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9994985,0.00014241463,0.000043165066,0.00008496476,0.0001092609,0.00012167356],"domain_scores_gemma":[0.9993761,0.00016741538,0.00010900089,0.000058693717,0.00017748715,0.000111226334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009933425,0.00056435703,0.00037689,0.0006718196,0.0011048492,0.0024552424,0.0006846556,0.0012275039,0.0022165077],"category_scores_gemma":[0.0024638025,0.00024101164,0.0002794032,0.00084111217,0.0010847482,0.0021447367,0.0015034361,0.0015155431,0.00059457147],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035359233,0.0004033656,0.16379663,0.0025910218,0.000184922,0.019067358,0.22382751,0.0017903815,0.004703784,0.0035751567,0.078237094,0.50146914],"study_design_scores_gemma":[0.000027828422,0.00028717163,0.30195132,0.0037124797,0.00010652862,0.0033090974,0.40916964,0.00082714733,0.0030491767,0.0043238215,0.27309906,0.00013670343],"about_ca_topic_score_codex":0.0123812305,"about_ca_topic_score_gemma":0.045236688,"teacher_disagreement_score":0.0123812305,"about_ca_system_score_codex":0.0013515082,"about_ca_system_score_gemma":0.0008383237,"threshold_uncertainty_score":0.024618328},"labels":[],"label_agreement":null},{"id":"W2951189010","doi":"10.1016/j.tecto.2019.06.017","title":"Contemporary tectonic stress pattern of the Persian Gulf Basin, Iran","year":2019,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Borehole; Seismology; Tectonics; Persian; Structural basin; Paleontology","score_opus":0.018746377488970584,"score_gpt":0.19989834928698538,"score_spread":0.1811519717980148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2951189010","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99587303,0.0007741843,0.00006637443,0.00036216006,0.00001742355,0.0000043703344,0.00030733252,0.000005756476,0.0025893068],"genre_scores_gemma":[0.99873537,0.0005346268,0.00007584149,0.000032302116,0.000014987322,0.000002282731,0.00022192653,0.0000011170006,0.00038161874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999218,0.0000063463035,0.000010454926,0.000016836175,0.000021437269,0.000023035886],"domain_scores_gemma":[0.9998617,0.000011386236,0.000046620786,0.000006332718,0.000055055643,0.00001884897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017301427,0.00026811834,0.00014434931,0.0016133101,0.00044993972,0.0006079809,0.000297371,0.00024337204,0.0011338254],"category_scores_gemma":[0.00030481955,0.00011116409,0.0001145347,0.002750311,0.00067462784,0.00036417338,0.00036273978,0.0001743848,0.00014427266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016232647,0.000064464475,0.93812805,0.00012997788,0.00009788386,0.0012131175,0.0029982482,0.0025163959,0.0024771972,0.0027855572,0.0024139276,0.047012758],"study_design_scores_gemma":[0.000008340456,0.000017704731,0.9931235,0.000013395061,0.000015973155,0.00023308136,0.0022355495,0.00033406253,0.000120844124,0.00022217863,0.0036695085,0.000005877877],"about_ca_topic_score_codex":0.058776703,"about_ca_topic_score_gemma":0.08362101,"teacher_disagreement_score":0.058776703,"about_ca_system_score_codex":0.0015039522,"about_ca_system_score_gemma":0.0017063397,"threshold_uncertainty_score":0.11686915},"labels":[],"label_agreement":null},{"id":"W2951877031","doi":"10.3390/min9060360","title":"Structural Diagenesis in Carbonate Rocks as Identified in Fault Damage Zones in the Northern Tarim Basin, NW China","year":2019,"lang":"en","type":"article","venue":"Minerals","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"National Science and Technology Major Project; National Natural Science Foundation of China","keywords":"Diagenesis; Geology; Cementation (geology); Carbonate; Carbonate rock; Calcite; Geochemistry; Fault (geology); Geomorphology; Petrology; Ordovician; Sedimentary rock; Paleontology; Cement","score_opus":0.011859692745488135,"score_gpt":0.22054785232248797,"score_spread":0.20868815957699982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2951877031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997739,0.000031177267,0.000016311988,0.000005118829,2.6789172e-7,0.0000023725936,0.000022748538,0.000001269528,0.00014679068],"genre_scores_gemma":[0.99980336,0.000026208883,0.00003836629,0.000002280126,5.353786e-7,0.0000017619078,0.000043930904,4.0919332e-7,0.00008335079],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998567,0.000010787364,0.000020434423,0.000043979617,0.000029808369,0.000038364604],"domain_scores_gemma":[0.99980384,0.000013704816,0.00008719029,0.000013077539,0.00004492642,0.0000371625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016411408,0.00021977563,0.00016572277,0.0018109393,0.0005937093,0.00038681456,0.00023894553,0.00016626646,0.00046249846],"category_scores_gemma":[0.00028533806,0.00017037771,0.0001556926,0.0010798799,0.00052749476,0.0002306197,0.0003984398,0.00008833921,0.000045609544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000062801955,0.000023068564,0.9658224,0.000049394337,0.000026741403,0.00044664278,0.0015575953,0.00024327124,0.022732563,0.0001508119,0.000031933196,0.008852872],"study_design_scores_gemma":[0.0000013737891,0.000013626714,0.99909294,0.0000023345954,0.0000050026765,0.000058025504,0.00027856333,0.00015485649,0.000302581,0.000012779925,0.00007592996,0.000001882644],"about_ca_topic_score_codex":0.0511897,"about_ca_topic_score_gemma":0.14719544,"teacher_disagreement_score":0.0511897,"about_ca_system_score_codex":0.0008196044,"about_ca_system_score_gemma":0.0007611862,"threshold_uncertainty_score":0.101783454},"labels":[],"label_agreement":null},{"id":"W2954154877","doi":"10.3390/rs11111357","title":"Global Earthquake Response with Imaging Geodesy: Recent Examples from the USGS NEIC","year":2019,"lang":"en","type":"article","venue":"Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Nevada, Reno; Japan Aerospace Exploration Agency; Natural Resources Canada; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Geodetic datum; Geology; Seismology; Interferometric synthetic aperture radar; Satellite; Geodesy; Synthetic aperture radar; Remote sensing","score_opus":0.016341084615538175,"score_gpt":0.21622244690727388,"score_spread":0.1998813622917357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954154877","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2620167,0.24637915,0.024862248,0.05654821,0.0049207285,0.0006034406,0.03285907,0.0015741893,0.37023634],"genre_scores_gemma":[0.5990019,0.24993642,0.07518744,0.010899411,0.004846245,0.0002714066,0.042306885,0.00073186547,0.016818453],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9993544,0.00010094367,0.00006106466,0.000080529666,0.00034045882,0.00006245944],"domain_scores_gemma":[0.9973131,0.00053899596,0.0003300863,0.00024282096,0.0014637583,0.000111236215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015862318,0.00068166794,0.00019996961,0.0037690466,0.0004299679,0.0015090902,0.0005103569,0.000656148,0.0011297937],"category_scores_gemma":[0.003964548,0.00024401005,0.00025723196,0.010581087,0.00071230915,0.0013738098,0.0014140778,0.0010183103,0.0003704546],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010990188,0.00007977739,0.104410596,0.0015924156,0.00010693439,0.0006419541,0.0025052167,0.004629869,0.002766677,0.012860208,0.20617096,0.66412544],"study_design_scores_gemma":[0.000010675342,0.000059813243,0.135244,0.00082387694,0.00006335765,0.000450485,0.0018449797,0.0020625005,0.001487326,0.0017619843,0.85614246,0.00004865101],"about_ca_topic_score_codex":0.048072558,"about_ca_topic_score_gemma":0.090942964,"teacher_disagreement_score":0.048072558,"about_ca_system_score_codex":0.0011505109,"about_ca_system_score_gemma":0.0009198166,"threshold_uncertainty_score":0.095585465},"labels":[],"label_agreement":null},{"id":"W2954527593","doi":"10.1029/2019jb018115","title":"Seismic and Microseismic Signatures of Fluids in Rocks: Bridging the Scale Gap","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Microseism; Geology; Seismology; Induced seismicity; Suite; Archaeology; Geography","score_opus":0.023937539214572062,"score_gpt":0.2923716165613959,"score_spread":0.2684340773468238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954527593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6838476,0.22201361,0.02391124,0.013236782,0.0030227243,0.00013327018,0.0040499046,0.00025707466,0.049527843],"genre_scores_gemma":[0.8236624,0.1509589,0.012443644,0.0009329165,0.005615751,0.000073194904,0.00129036,0.00015659592,0.0048661698],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995443,0.00008435945,0.000077011806,0.00006905676,0.00019030852,0.000034965306],"domain_scores_gemma":[0.995073,0.002891383,0.0007116034,0.00021446458,0.0009990113,0.00011042671],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011679718,0.00021473598,0.00035315633,0.0059930193,0.00033141603,0.002086952,0.00036729005,0.00057868904,0.0021670968],"category_scores_gemma":[0.0044030654,0.00014796483,0.00024644777,0.0055843717,0.0009826532,0.0024320937,0.0013593833,0.0004371102,0.00034277234],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036261196,0.000097697746,0.08096909,0.006880612,0.0002849498,0.0012394233,0.0076558525,0.0015688272,0.020923173,0.010613216,0.011622416,0.8577822],"study_design_scores_gemma":[0.000027866025,0.0006435158,0.5292574,0.0068742465,0.00041382472,0.0023214605,0.0336943,0.0026005148,0.013508472,0.020099932,0.39043993,0.00011846771],"about_ca_topic_score_codex":0.0010367547,"about_ca_topic_score_gemma":0.0029033083,"teacher_disagreement_score":0.0059930193,"about_ca_system_score_codex":0.00029076842,"about_ca_system_score_gemma":0.0006397317,"threshold_uncertainty_score":0.007249713},"labels":[],"label_agreement":null},{"id":"W2955377171","doi":"10.1007/s00024-020-02451-x","title":"Introduction to “Twenty Five Years of Modern Tsunami Science Following the 1992 Nicaragua and Flores Island Tsunamis, Volume II”","year":2020,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Seismology; Geology; Landslide; Tsunami earthquake; Tsunami wave; Warning system; Submarine pipeline; Oceanography; Geography; Engineering","score_opus":0.006714908394256554,"score_gpt":0.18915779629473647,"score_spread":0.1824428879004799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2955377171","genre_codex":"review","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004959461,0.5862083,0.008670381,0.065509096,0.19029008,0.00014886934,0.004317332,0.00057897734,0.13931753],"genre_scores_gemma":[0.045084476,0.39335746,0.014596403,0.044418875,0.12656683,0.0005260206,0.007721063,0.00096389523,0.36676493],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997305,0.000073288036,0.000034154662,0.00006233855,0.00006247115,0.000037237467],"domain_scores_gemma":[0.9992155,0.00028935817,0.000068758614,0.00005384171,0.00029151194,0.00008107016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068559364,0.0010572779,0.00043969078,0.0024878902,0.0012512864,0.0021915503,0.0008020756,0.0009062457,0.020058298],"category_scores_gemma":[0.0020436535,0.00020465965,0.00035455244,0.0030394313,0.0014050123,0.0018863452,0.0014017292,0.0016113558,0.004739193],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005689039,0.000015221455,0.0009674507,0.00088540174,0.000011969047,0.00014225507,0.0010371888,0.0002877959,0.00073305494,0.020160591,0.8924019,0.083300285],"study_design_scores_gemma":[0.0000010310725,0.0000051954703,0.0010809115,0.0001969931,0.0000016650866,0.000056568588,0.00019063863,0.000018162322,0.00006005831,0.0010366235,0.99734783,0.0000044013896],"about_ca_topic_score_codex":0.019747827,"about_ca_topic_score_gemma":0.04810092,"teacher_disagreement_score":0.020058298,"about_ca_system_score_codex":0.0021134003,"about_ca_system_score_gemma":0.002378161,"threshold_uncertainty_score":0.06710172},"labels":[],"label_agreement":null},{"id":"W2955677072","doi":"10.1155/2019/9809458","title":"Seismological and Hydrogeological Controls on New Zealand-Wide Groundwater Level Changes Induced by the 2016 M<sub>w</sub>7.8 Kaikōura Earthquake","year":2019,"lang":"en","type":"article","venue":"Geofluids","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Marsden Fund; Victoria University; Royal Society; Waikato Regional Council; Victoria University of Wellington; Royal Society Te Apārangi; Aqualinc Research; Greater Wellington Regional Council; McGill University; National Institute of Water and Atmospheric Research","keywords":"Epicenter; Groundwater; Hydrogeology; Aquifer; Geology; Water level; Consolidation (business); Seismology; Ground level; Geotechnical engineering; Geography; Ground floor","score_opus":0.02797721249477201,"score_gpt":0.21105104666562347,"score_spread":0.18307383417085146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2955677072","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993709,0.000029323415,0.00001784294,0.000013687049,9.677451e-7,0.000004438973,0.000107771426,0.0000012176829,0.00045386446],"genre_scores_gemma":[0.99956113,0.000056432928,0.000030951724,0.000006086032,0.0000013701494,0.0000040166265,0.00010780304,9.792305e-7,0.00023124904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981505,0.000022099375,0.000017708675,0.00004451014,0.00004661728,0.000053971366],"domain_scores_gemma":[0.9991973,0.00006345131,0.0003863744,0.000034535475,0.00015645455,0.00016187619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025507112,0.00018671773,0.00021594284,0.0007950743,0.00028823054,0.0005229481,0.00021486764,0.00021529071,0.0011463762],"category_scores_gemma":[0.0011247697,0.00019070349,0.00016488296,0.0008635536,0.0009007011,0.00034193043,0.00068106595,0.00023643972,0.00014824416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008863689,0.00010670325,0.9124769,0.00009495679,0.000107726744,0.00081893516,0.0035241453,0.00066487404,0.066424266,0.00018551575,0.00028114195,0.014428507],"study_design_scores_gemma":[0.0000017438039,0.000018801893,0.9993839,0.0000013612787,0.000004418079,0.000020575946,0.00033811503,0.000041280564,0.00009564293,0.000006946273,0.00008443647,0.0000026386735],"about_ca_topic_score_codex":0.15317884,"about_ca_topic_score_gemma":0.32239765,"teacher_disagreement_score":0.15317884,"about_ca_system_score_codex":0.001368671,"about_ca_system_score_gemma":0.0005725651,"threshold_uncertainty_score":0.3045745},"labels":[],"label_agreement":null},{"id":"W2957524536","doi":"10.1029/2019tc005503","title":"Coseismic Ground Rupture of the 15 October 2013 Magnitude (<i>M</i><sub><i>W</i></sub>) 7.2 Bohol Earthquake, Bohol Island, Central Philippines","year":2019,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of the Philippines","keywords":"Geology; Seismology; Fault scarp; Submarine pipeline; Fault (geology); Magnitude (astronomy); Thrust fault; Fault plane; Caliphate; Anticline; Oceanography; Tectonics; Geography; Archaeology; Islam","score_opus":0.008274026507019638,"score_gpt":0.18775930928902335,"score_spread":0.1794852827820037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2957524536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974304,0.00003496584,0.000080514634,0.000033687593,0.000006155438,0.0000096955155,0.00066983013,0.000016833736,0.0017177651],"genre_scores_gemma":[0.99860257,0.000036443897,0.000101522906,0.000008337768,0.0000045001752,0.0000062137783,0.00061312685,0.000002897427,0.00062440836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994373,0.0000058757723,0.0000034854522,0.000013990117,0.000017990753,0.000014994697],"domain_scores_gemma":[0.9998286,0.000008102786,0.0000530525,0.000008248789,0.000050909854,0.00005116578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105834,0.00018903575,0.00009415612,0.0006120055,0.00042299228,0.00027025698,0.00016156999,0.00018140272,0.0017117425],"category_scores_gemma":[0.000271516,0.000096646094,0.00009020509,0.00056315603,0.00027020002,0.00017731704,0.0004837935,0.00017758369,0.00025801332],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002520861,0.00008224284,0.93993473,0.000098832694,0.000070087684,0.00195804,0.003862035,0.0013317866,0.021847527,0.00020295287,0.0027070527,0.027652692],"study_design_scores_gemma":[0.000002015952,0.000028477034,0.9973476,0.0000068742384,0.0000057359994,0.000102616556,0.00082882075,0.00029078117,0.0005325643,0.000016505026,0.0008340369,0.0000038895046],"about_ca_topic_score_codex":0.043576337,"about_ca_topic_score_gemma":0.096164845,"teacher_disagreement_score":0.043576337,"about_ca_system_score_codex":0.000476137,"about_ca_system_score_gemma":0.0005237924,"threshold_uncertainty_score":0.086645365},"labels":[],"label_agreement":null},{"id":"W2957895140","doi":"10.1017/s0016756819000645","title":"Deformation partitioning in mountain belts: insights from analogue modelling experiments and the Taiwan collisional orogen","year":2019,"lang":"en","type":"article","venue":"Geological Magazine","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Centre National de la Recherche Scientifique","keywords":"Geology; Lithosphere; Subduction; Strain partitioning; Tectonics; Continental margin; Crust; Plate tectonics; Convergent boundary; Seismology; Passive margin; Mantle (geology); Continental crust; Mountain formation; Crustal recycling; Obduction; Underplating; Geophysics; Oceanic crust; Rift","score_opus":0.018627756194953535,"score_gpt":0.21194706570373242,"score_spread":0.1933193095087789,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2957895140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99807066,0.000028497734,0.0009073177,0.000033110136,0.0000014482283,0.00000981611,0.00014781689,0.000019132018,0.00078233547],"genre_scores_gemma":[0.99920756,0.000030039091,0.0005616547,0.0000048388442,0.0000012888142,0.000006921462,0.00010645133,0.0000047374524,0.00007642566],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984527,0.0000768341,0.000013227383,0.00003171499,0.000014154337,0.000018692368],"domain_scores_gemma":[0.99959415,0.00022733682,0.000057445992,0.00007681451,0.000022341765,0.000021995407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004748113,0.00021521313,0.00033362847,0.00044797428,0.00022289826,0.00064470386,0.0008245929,0.000552307,0.0011041148],"category_scores_gemma":[0.0012304655,0.00017951839,0.0004115365,0.0006372268,0.00063701486,0.00048080913,0.00034159125,0.00032560405,0.00006122327],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048628016,0.00051435636,0.07445288,0.00012402397,0.00017373115,0.00043653476,0.00078281306,0.8976787,0.014395088,0.0037021528,0.0003082248,0.0069451253],"study_design_scores_gemma":[0.00012980234,0.0003044811,0.046187557,0.000011627791,0.000054868022,0.00007200802,0.0003373796,0.94893014,0.0019435346,0.0014136595,0.0005838067,0.000031163672],"about_ca_topic_score_codex":0.01736558,"about_ca_topic_score_gemma":0.008303236,"teacher_disagreement_score":0.01736558,"about_ca_system_score_codex":0.00058562367,"about_ca_system_score_gemma":0.00018774891,"threshold_uncertainty_score":0.03452897},"labels":[],"label_agreement":null},{"id":"W2961064253","doi":"10.1029/2019jb017831","title":"Effects of Preexisting Structures on the Seismicity of the Charlevoix Seismic Zone","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Rift; Hypocenter; Tectonics","score_opus":0.027060179018607092,"score_gpt":0.28552469232827726,"score_spread":0.2584645133096702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2961064253","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99914634,0.00003096137,0.00012619962,0.000020746913,0.0000022141776,0.0000028411034,0.00008167246,0.000016092139,0.00057284854],"genre_scores_gemma":[0.9996946,0.000017451173,0.000043568747,0.000003913633,7.508558e-7,0.0000012437399,0.00010493907,0.000003162895,0.00013053279],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997428,0.000047694433,0.000020685426,0.00005898071,0.00006171159,0.00006800775],"domain_scores_gemma":[0.9990356,0.00035565422,0.00018144792,0.000105668005,0.00012899832,0.00019263082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037869657,0.00034001563,0.00023974765,0.000516594,0.00044589714,0.0015081378,0.0005541283,0.00042965898,0.0016646548],"category_scores_gemma":[0.0023106963,0.0002815435,0.00024329431,0.00045945347,0.0006773553,0.00034017596,0.0008070809,0.0003033584,0.00013768338],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057208457,0.00017655415,0.688721,0.00005378849,0.00014356188,0.0005401346,0.00034189655,0.2715038,0.024522137,0.00082598825,0.000395284,0.012203708],"study_design_scores_gemma":[0.000046488793,0.00023348148,0.8457415,0.000016572107,0.00004616446,0.00008960291,0.0002986577,0.14928675,0.003515965,0.00009331367,0.0006114153,0.000020075591],"about_ca_topic_score_codex":0.10555108,"about_ca_topic_score_gemma":0.105581,"teacher_disagreement_score":0.89444894,"about_ca_system_score_codex":0.0024306262,"about_ca_system_score_gemma":0.0008766188,"threshold_uncertainty_score":0.20987338},"labels":[],"label_agreement":null},{"id":"W2961822722","doi":"10.5194/npg-27-1-2020","title":"Magnitude correlations in a self-similar aftershock rates model of seismicity","year":2020,"lang":"en","type":"article","venue":"Nonlinear processes in geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Society for the Study of Amphibians and Reptiles","keywords":"Magnitude (astronomy); Aftershock; Induced seismicity; Geology; Distribution (mathematics); Seismology; Statistical physics; Mathematics; Physics; Mathematical analysis","score_opus":0.026737470737239078,"score_gpt":0.23427353533655115,"score_spread":0.20753606459931206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2961822722","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81043684,0.00014124738,0.1843489,0.0009427325,0.000053227748,0.000044468274,0.00044393682,0.0002462931,0.0033422308],"genre_scores_gemma":[0.9948514,0.00006482758,0.0028437926,0.000056893205,0.000022097593,0.000022121545,0.00014875211,0.000026283366,0.0019638622],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999482,0.00019281101,0.00002605641,0.00013879791,0.000066102424,0.00009427017],"domain_scores_gemma":[0.9940268,0.0030713324,0.0015236654,0.0005021332,0.00051751087,0.00035863894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002766967,0.0004074024,0.000904386,0.0007960098,0.0003342295,0.00104956,0.001968954,0.0011327135,0.002124857],"category_scores_gemma":[0.00912302,0.0004982392,0.00097235636,0.0005865468,0.001612477,0.0016012662,0.0007916748,0.0011409878,0.00020774757],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014085,0.00008332655,0.011597827,0.00004059548,0.00010278835,0.00022117222,0.00014345018,0.8597607,0.0022509738,0.12132068,0.0007859473,0.0035516627],"study_design_scores_gemma":[0.000010481218,0.000018753359,0.0012740694,0.00000241531,0.000008603077,0.000014072916,0.000008786221,0.9903014,0.000106078376,0.008185438,0.00006217054,0.0000077308505],"about_ca_topic_score_codex":0.01120991,"about_ca_topic_score_gemma":0.0058962563,"teacher_disagreement_score":0.01120991,"about_ca_system_score_codex":0.0011113706,"about_ca_system_score_gemma":0.0008520855,"threshold_uncertainty_score":0.022289336},"labels":[],"label_agreement":null},{"id":"W2962948702","doi":"10.1029/2018jb016461","title":"The Effects of Earthquakes and Fluids on the Metamorphism of the Lower Continental Crust","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"European Research Council; Natural Environment Research Council; European Commission; Natural Sciences and Engineering Research Council of Canada; Norges Forskningsråd; Sight Research UK; Alexander von Humboldt-Stiftung","keywords":"Geology; Metamorphism; Crust; Continental crust; Metamorphic rock; Mylonite; Petrology; Shear zone; Continental collision; Lithology; Brittleness; Lithosphere; Slip (aerodynamics); Creep; Seismology; Tectonics; Geochemistry","score_opus":0.018498678158567053,"score_gpt":0.27102223589361657,"score_spread":0.25252355773504953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2962948702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943167,0.00018894889,0.00002565624,0.000016849635,0.0000016864111,0.0000014086838,0.000045169436,0.00000267207,0.00028598672],"genre_scores_gemma":[0.9996824,0.00007676871,0.000016016329,0.0000072358057,0.0000020337754,8.1899145e-7,0.000041002782,9.67303e-7,0.0001727815],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999021,0.000032866395,0.000007545356,0.000013088132,0.000014730224,0.000029614208],"domain_scores_gemma":[0.99956757,0.00014582508,0.0001067568,0.000020371997,0.000049714938,0.00010980382],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018099013,0.00023756165,0.00020932111,0.00045153033,0.00018653214,0.00047489366,0.00012905116,0.00020498676,0.0017464603],"category_scores_gemma":[0.0007070545,0.0000986113,0.00022641581,0.00026034226,0.00033553896,0.00017900972,0.00036991743,0.00020080572,0.00017765583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008318412,0.00067018747,0.5736014,0.0002924439,0.00070125354,0.0014483031,0.0005771953,0.012701707,0.3461253,0.00059384125,0.00041875636,0.054551154],"study_design_scores_gemma":[0.00002366079,0.000580619,0.98924005,0.000010161328,0.00006788508,0.00011414381,0.00019006658,0.0022501696,0.00688199,0.00013574952,0.00049539836,0.0000100409725],"about_ca_topic_score_codex":0.0036242262,"about_ca_topic_score_gemma":0.0030927309,"teacher_disagreement_score":0.0036242262,"about_ca_system_score_codex":0.00031077993,"about_ca_system_score_gemma":0.00013418835,"threshold_uncertainty_score":0.007206261},"labels":[],"label_agreement":null},{"id":"W2963111335","doi":"10.1029/2019gl083566","title":"Frictional Stabilities on Induced Earthquake Fault Planes at Fox Creek, Alberta: A Pore Fluid Pressure Dilemma","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Alberta; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Helmholtz-Alberta Initiative","keywords":"Pore water pressure; Hydraulic fracturing; Slip (aerodynamics); Fluid pressure; Hydrostatic equilibrium; Fault (geology); Induced seismicity; Hydrostatic pressure","score_opus":0.03748806663023269,"score_gpt":0.2691873581612527,"score_spread":0.23169929153102004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963111335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977736,0.000011355826,0.0011990324,0.00007651668,4.7216187e-7,0.0000017880553,0.000033760756,0.000009138483,0.0008943309],"genre_scores_gemma":[0.99987173,0.00000496753,0.00005863955,0.000001285393,2.6310323e-7,4.3102597e-7,0.0000065830413,7.691281e-7,0.000055348686],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999404,0.000009476669,0.000002799383,0.0000086654345,0.000019247265,0.000019509282],"domain_scores_gemma":[0.99945456,0.00028950965,0.00008616837,0.00003218765,0.0000914453,0.000046059966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002466198,0.00012943518,0.00015465067,0.0004204277,0.00042868752,0.0007975572,0.00050600513,0.0004530792,0.0010868479],"category_scores_gemma":[0.002206559,0.00013812588,0.00012608191,0.00026801508,0.0012955762,0.00059598277,0.00040686427,0.00027195437,0.00004266142],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011064013,0.000052253978,0.08712937,0.000031202097,0.00003499822,0.00063496066,0.00029530015,0.8816848,0.0046468717,0.019041792,0.0003395693,0.005998289],"study_design_scores_gemma":[0.000023787594,0.000051490835,0.08177351,0.000007989981,0.000017271861,0.000101409314,0.00053102284,0.9051812,0.0015544306,0.0104555385,0.0002829742,0.00001928834],"about_ca_topic_score_codex":0.07889742,"about_ca_topic_score_gemma":0.05086358,"teacher_disagreement_score":0.9211026,"about_ca_system_score_codex":0.0019328541,"about_ca_system_score_gemma":0.0009267062,"threshold_uncertainty_score":0.15687639},"labels":[],"label_agreement":null},{"id":"W2963645582","doi":"","title":"Investigating the Response of Zircon to Shock Metamorphism","year":2019,"lang":"en","type":"article","venue":"MacEwan University Student Research Proceedings","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"MacEwan University","funders":"","keywords":"Zircon; Metamorphism; Geology; Shock metamorphism; Geochemistry; Petrology; Impact crater; Astrobiology","score_opus":0.07406055746673425,"score_gpt":0.31052763489173896,"score_spread":0.23646707742500472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963645582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970366,0.0001572589,0.0005871773,0.000051038765,0.000010420028,0.000008226335,0.00054238207,0.000024385101,0.0015823932],"genre_scores_gemma":[0.99820447,0.0000858876,0.00029782407,0.000024384344,0.0000046744326,0.0000039919105,0.0004912607,0.000008757685,0.0008787541],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999136,0.00000858402,0.0000078613275,0.00002430494,0.000016828428,0.000028810002],"domain_scores_gemma":[0.99984574,0.000027321328,0.000030266307,0.000022470891,0.000061429855,0.000012734529],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026672852,0.00016657176,0.00027404755,0.00054886076,0.00031995066,0.0007330435,0.0002559825,0.0005270869,0.001712128],"category_scores_gemma":[0.0007109183,0.00022680147,0.00022253748,0.00054485165,0.00026261664,0.00032762898,0.00034285223,0.00030485503,0.00029921386],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021227603,0.00009252976,0.24125268,0.00014237741,0.00013946788,0.00045475995,0.00063624774,0.0017051002,0.73666626,0.00083485787,0.00056216307,0.015390809],"study_design_scores_gemma":[0.00005730356,0.000348003,0.8766188,0.0000118625885,0.00009924943,0.00025163314,0.0005486704,0.0023300322,0.11439863,0.00014844119,0.0051755784,0.000011873228],"about_ca_topic_score_codex":0.010424303,"about_ca_topic_score_gemma":0.010602138,"teacher_disagreement_score":0.010424303,"about_ca_system_score_codex":0.0003192264,"about_ca_system_score_gemma":0.00023161639,"threshold_uncertainty_score":0.020727277},"labels":[],"label_agreement":null},{"id":"W2963760717","doi":"10.1029/2019jb017336","title":"Seismotectonics of the Zagros (Iran) From Orogen‐Wide, Calibrated Earthquake Relocations","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Seismotectonics; Active fault; Fault (geology); Crust; Sinistral and dextral; Geophysics","score_opus":0.0400281737295255,"score_gpt":0.2913132705724643,"score_spread":0.2512850968429388,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963760717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977708,0.000119791395,0.0001381875,0.000017752604,0.0000064089118,0.000008262651,0.0012169979,0.000016532435,0.0007052557],"genre_scores_gemma":[0.9951623,0.0001291354,0.00057839823,0.0000137651705,0.000012766703,0.00000644035,0.0038168624,0.000006697556,0.00027365616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998375,0.000015532232,0.000017915037,0.00005480653,0.000037249265,0.000036899553],"domain_scores_gemma":[0.99975413,0.000015017783,0.00012122719,0.000040813615,0.000051059902,0.000017874208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031990613,0.00027058492,0.00017771278,0.0015957018,0.00020864244,0.00036561093,0.0002613328,0.00020555593,0.0006740858],"category_scores_gemma":[0.0005297947,0.00010555653,0.00022079532,0.0018134406,0.00021317965,0.00019937275,0.0003774396,0.00017817937,0.0002668259],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021778757,0.00007363216,0.9451827,0.00008014533,0.00011803261,0.00034379287,0.0008134725,0.0033823987,0.0040479195,0.00020451116,0.0008895479,0.04464604],"study_design_scores_gemma":[0.000007949308,0.000013189465,0.99849,0.0000056630474,0.0000141524415,0.000047118112,0.00013734827,0.00034475306,0.00012606838,0.000012426115,0.00079834514,0.0000029705216],"about_ca_topic_score_codex":0.036102347,"about_ca_topic_score_gemma":0.059508543,"teacher_disagreement_score":0.036102347,"about_ca_system_score_codex":0.0005519363,"about_ca_system_score_gemma":0.00039508357,"threshold_uncertainty_score":0.07178444},"labels":[],"label_agreement":null},{"id":"W2964571751","doi":"10.1029/2019jb017643","title":"Detection of Low‐Frequency Earthquakes in Broadband Random Time Sequences: Are They Independent Events?","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Natural Resources Canada; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Seismogram; Waveform; Matched filter; Impulse (physics); Filter (signal processing); Acoustics; Broadband; Seismology; Physics; Sequence (biology); Geology; Algorithm; Computer science; Telecommunications; Optics","score_opus":0.022464943443949576,"score_gpt":0.2836457150635788,"score_spread":0.2611807716196292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964571751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9373748,0.00021780896,0.060864825,0.00014693318,0.00003622023,0.000020368032,0.0000753545,0.000114055576,0.0011497742],"genre_scores_gemma":[0.99442554,0.000056079734,0.005242188,0.000015155462,0.0000138018895,0.0000046266355,0.000052122323,0.000010199757,0.00018028608],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997389,0.000053922806,0.000015650523,0.000070249094,0.0000842797,0.00003706127],"domain_scores_gemma":[0.9982968,0.0007324107,0.00050107465,0.00013774456,0.0002007435,0.00013127417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008269319,0.00024779336,0.00034803708,0.0005749774,0.00013721417,0.0005320112,0.00039713073,0.0005963501,0.00093200355],"category_scores_gemma":[0.0047570644,0.00028093724,0.00026655183,0.00036747954,0.00037899017,0.00089826324,0.00026605697,0.00026362133,0.00022899087],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012953976,0.00042117215,0.33207187,0.00071313354,0.0005485216,0.0024648963,0.00052801316,0.19063659,0.291328,0.016816838,0.0011842367,0.16199125],"study_design_scores_gemma":[0.000068803834,0.00031142382,0.20649524,0.000057216246,0.00014957505,0.00080763025,0.00022588196,0.7546556,0.028883703,0.0070390785,0.0012364539,0.00006943108],"about_ca_topic_score_codex":0.00092817296,"about_ca_topic_score_gemma":0.0008583316,"teacher_disagreement_score":0.00093200355,"about_ca_system_score_codex":0.0002401517,"about_ca_system_score_gemma":0.00016237354,"threshold_uncertainty_score":0.0043732524},"labels":[],"label_agreement":null},{"id":"W2964581642","doi":"10.1785/0120180195","title":"Spatiotemporal Variation of Crustal Anisotropy in the Source Area of the 2004 Niigata, Japan Earthquake","year":2019,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Chinese Academy of Sciences; Canadian Natural Resources Limited","keywords":"Geology; Seismology; Aftershock; Crust; Stress field; Tectonics; Subduction; Compression (physics); Focal mechanism; Geodesy; Geophysics","score_opus":0.011627757300760317,"score_gpt":0.1927003445154197,"score_spread":0.18107258721465938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964581642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99960476,0.000033704095,0.00005277366,0.000007943451,0.0000014955152,0.0000019318848,0.00014938561,0.0000033783142,0.00014458514],"genre_scores_gemma":[0.9993856,0.00004489204,0.0000815712,0.0000032380794,0.000004171498,0.0000046592604,0.0003683616,0.0000014571414,0.000106073305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999188,0.000009366704,0.000008909773,0.000023449309,0.000017847886,0.000021592814],"domain_scores_gemma":[0.99945015,0.000037479982,0.000232676,0.000044447792,0.00014798604,0.000087205415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011723561,0.00022986124,0.00026449192,0.00086924154,0.0002626532,0.00038610096,0.00016908105,0.0002019083,0.00034282968],"category_scores_gemma":[0.00055084366,0.00015363503,0.00014678511,0.0009429682,0.00018785131,0.00019804762,0.00029662516,0.00015509664,0.00011879523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016535436,0.000034288907,0.97407836,0.00002581193,0.00009427117,0.00026195924,0.0005570854,0.0006186515,0.019382438,0.00002630632,0.0002271713,0.004528334],"study_design_scores_gemma":[0.0000012942988,0.0000084979265,0.9992198,0.0000014460045,0.000010558125,0.000034493398,0.000140822,0.0002742996,0.00023260796,0.0000029199675,0.00007092809,0.000002434372],"about_ca_topic_score_codex":0.030469226,"about_ca_topic_score_gemma":0.057938017,"teacher_disagreement_score":0.030469226,"about_ca_system_score_codex":0.00033833404,"about_ca_system_score_gemma":0.00021717677,"threshold_uncertainty_score":0.06058377},"labels":[],"label_agreement":null},{"id":"W2964649173","doi":"10.1029/2019jb017926","title":"Stability of Pulse‐Like Earthquake Ruptures","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Sight Research UK","keywords":"Slip (aerodynamics); Perturbation (astronomy); Thermal; Cabin pressurization; Infinitesimal; Stress (linguistics); Steady state (chemistry)","score_opus":0.0448825337711925,"score_gpt":0.31570847695036763,"score_spread":0.27082594317917513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964649173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99057686,0.000042927386,0.007077378,0.000086126835,0.0000067409583,0.00001077348,0.00008554433,0.0000619249,0.002051601],"genre_scores_gemma":[0.9992619,0.000014539581,0.00043463358,0.000008516996,0.0000013757536,0.000007791596,0.000045914843,0.000007030104,0.00021824133],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993026,0.000012567189,0.0000038287358,0.000017691269,0.000016004786,0.000019705607],"domain_scores_gemma":[0.99970067,0.00011426218,0.000060772563,0.000025840534,0.000052241394,0.000046333967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021356373,0.00017357459,0.00030397737,0.00031858947,0.00032544235,0.0005906274,0.00041189793,0.0006053039,0.0012802478],"category_scores_gemma":[0.0013094312,0.00017732481,0.0003044133,0.00017352826,0.0005667039,0.00050597644,0.0004568567,0.00039905502,0.00009823018],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110271474,0.00008366601,0.012235099,0.000036097175,0.00007091702,0.00024567483,0.0001257211,0.9566622,0.02017999,0.0063652326,0.00038817522,0.0034969854],"study_design_scores_gemma":[0.000009185951,0.000036195088,0.002596284,0.0000031850843,0.000005364325,0.000026910093,0.000029637573,0.99426997,0.0019817033,0.0009059001,0.00012889515,0.0000067624974],"about_ca_topic_score_codex":0.0024373666,"about_ca_topic_score_gemma":0.00080058386,"teacher_disagreement_score":0.0024373666,"about_ca_system_score_codex":0.0005562055,"about_ca_system_score_gemma":0.0003470284,"threshold_uncertainty_score":0.0048463345},"labels":[],"label_agreement":null},{"id":"W2964711780","doi":"10.1130/abs/2019am-336125","title":"COMPARING THE PHANEROZOIC THERMAL EVOLUTION OF THE PROTEROZOIC TRANS-HUDSON OROGEN WITH THAT OF THE ARCHEAN SUPERIOR AND SLAVE CRATONS, CANADA","year":2019,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Archean; Proterozoic; Phanerozoic; Geology; Craton; Paleontology; Earth science; Tectonics; Cenozoic","score_opus":0.017160035764974706,"score_gpt":0.192972690476057,"score_spread":0.1758126547110823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964711780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957488,0.0002876182,0.000060569342,0.000080110745,0.0000056270337,0.0000041364715,0.00052534026,0.000004300106,0.0032835477],"genre_scores_gemma":[0.99851304,0.00020250038,0.000039318686,0.000016091024,0.0000024057722,0.0000022006734,0.00025306974,0.0000041604703,0.00096729404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.0000035190587,0.0000019701558,0.000013402821,0.000011105291,0.000032060852],"domain_scores_gemma":[0.999826,0.00001100453,0.000017576456,0.0000052079777,0.000099094825,0.000041242736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012208469,0.00013343731,0.00013969335,0.0010087582,0.00091811485,0.00085285224,0.0002588661,0.00019490121,0.0028855833],"category_scores_gemma":[0.00045161342,0.0001387127,0.00014483476,0.0014957294,0.00056426076,0.00018866142,0.000326811,0.00020612018,0.00022397815],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055984437,0.000029737233,0.95078975,0.00008074627,0.00014958704,0.00030967058,0.0025050493,0.0036457605,0.01737618,0.0020284294,0.0012603876,0.021264926],"study_design_scores_gemma":[0.0000043545974,0.0000040298914,0.99839824,0.000006433647,0.000006172556,0.000017509894,0.0004392654,0.00018474681,0.0001259465,0.000022267861,0.0007892057,0.0000017218242],"about_ca_topic_score_codex":0.93901205,"about_ca_topic_score_gemma":0.9702383,"teacher_disagreement_score":0.06098795,"about_ca_system_score_codex":0.0068704477,"about_ca_system_score_gemma":0.004548324,"threshold_uncertainty_score":0.122694194},"labels":[],"label_agreement":null},{"id":"W2964844561","doi":"10.1093/gji/ggz364","title":"A reappraisal of the H–κ stacking technique: implications for global crustal structure","year":2019,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Norges Forskningsråd; European Commission; Sight Research UK","keywords":"Receiver function; Crust; Seismogram; Stacking; Mantle (geology); Geology; Seismology; Seismometer; Perturbation (astronomy); Geophysics; Lithosphere; Physics; Tectonics","score_opus":0.012473471823795596,"score_gpt":0.2718269075196732,"score_spread":0.2593534356958776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964844561","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6514472,0.0019560438,0.32810965,0.0059907874,0.00036973678,0.00010204024,0.00044330643,0.0010959646,0.010485235],"genre_scores_gemma":[0.9191321,0.0003707169,0.07917653,0.0001932209,0.00013158802,0.000014091446,0.0000825646,0.00007933075,0.0008198441],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.998995,0.00050191645,0.0000719267,0.00014308329,0.00023933646,0.000048755235],"domain_scores_gemma":[0.99449736,0.0019516661,0.00077748124,0.0013057778,0.0012890815,0.00017867434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0052000037,0.00062180904,0.00031093345,0.0012053485,0.00063102425,0.0015639933,0.0010386786,0.0005282827,0.0011900121],"category_scores_gemma":[0.010752678,0.0002529853,0.00046555066,0.0010613161,0.000999476,0.0012082176,0.0009233605,0.0010919403,0.00027218627],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042102073,0.000105859785,0.19854562,0.0002983224,0.0004978857,0.00057163165,0.0012729424,0.1801119,0.046234746,0.028746314,0.0066327355,0.53656095],"study_design_scores_gemma":[0.000046762252,0.0002800931,0.30848086,0.00026166273,0.00024626506,0.00028704148,0.0016677048,0.599724,0.031897873,0.042110868,0.014774809,0.00022202285],"about_ca_topic_score_codex":0.010866305,"about_ca_topic_score_gemma":0.013601918,"teacher_disagreement_score":0.010866305,"about_ca_system_score_codex":0.0006780793,"about_ca_system_score_gemma":0.00075854425,"threshold_uncertainty_score":0.02750057},"labels":[],"label_agreement":null},{"id":"W2966239072","doi":"10.1126/sciadv.aaw0913","title":"Dynamic earthquake rupture in the lower crust","year":2019,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"European Research Council; Natural Sciences and Engineering Research Council of Canada; Norges Forskningsråd","keywords":"Crust; Geology; Fragmentation (computing); Seismology; Geophysics; Computer science","score_opus":0.007898092466684934,"score_gpt":0.23611086125813513,"score_spread":0.2282127687914502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2966239072","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976902,0.0005768669,0.00018679928,0.000021994041,0.0000036556053,0.00000274672,0.00008315344,0.000009223829,0.0014253601],"genre_scores_gemma":[0.99957055,0.00013820207,0.00005355123,0.0000065899517,0.0000021779385,0.0000011967603,0.00007005624,7.7335665e-7,0.00015696652],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999429,0.0000050077256,0.000005587448,0.00001745366,0.000011999283,0.000016986603],"domain_scores_gemma":[0.9998054,0.000012605071,0.00011444756,0.000014058379,0.000017127355,0.000036429174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012308516,0.00012510431,0.00017915075,0.00051654916,0.00019792737,0.00041788683,0.00016496082,0.0002488296,0.00074991974],"category_scores_gemma":[0.00034908115,0.00010096661,0.000088852204,0.00037134296,0.0003447845,0.00030430648,0.00040226447,0.00018138472,0.00015948403],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027813273,0.00011251331,0.77713203,0.00019524482,0.0000781496,0.0036071294,0.0011913608,0.0037831622,0.17292881,0.0012024848,0.0005292006,0.038961746],"study_design_scores_gemma":[0.000005720023,0.00008269596,0.99390125,0.000015399646,0.000010042822,0.0010677533,0.00017838752,0.0006055948,0.0027014753,0.00022190862,0.0012036306,0.000006031411],"about_ca_topic_score_codex":0.0054608593,"about_ca_topic_score_gemma":0.00449265,"teacher_disagreement_score":0.0054608593,"about_ca_system_score_codex":0.0005219439,"about_ca_system_score_gemma":0.00022961615,"threshold_uncertainty_score":0.0108581185},"labels":[],"label_agreement":null},{"id":"W2966372724","doi":"10.1130/abs/2019am-341094","title":"CONSIDERATIONS FOR THE CALCULATION OF U-PB DETRITAL ZIRCON MAXIMUM DEPOSITIONAL AGES: INSIGHTS FROM CRETACEOUS FOREARC AND FORELAND BASINS IN NORTH AND SOUTH AMERICA","year":2019,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Forearc; Foreland basin; Geology; Zircon; Cretaceous; Sedimentary depositional environment; Paleontology; Geochemistry; Petrology; Structural basin; Subduction; Tectonics","score_opus":0.019588598020703115,"score_gpt":0.21338816294912913,"score_spread":0.193799564928426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2966372724","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.54291356,0.016339405,0.37549502,0.011302686,0.0016170198,0.0007672032,0.0071629905,0.0020923316,0.042309735],"genre_scores_gemma":[0.6920566,0.0032750363,0.29544547,0.0013697408,0.00026930645,0.0004761179,0.0014823896,0.0009045675,0.0047208983],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99782217,0.001218363,0.00038089603,0.0002265487,0.00026086913,0.00009115066],"domain_scores_gemma":[0.99259865,0.004089033,0.00048550716,0.00051908795,0.0021128764,0.00019494387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0117564015,0.0009012497,0.0009007637,0.0029547235,0.0016589146,0.0025578728,0.002648957,0.0007272779,0.002221714],"category_scores_gemma":[0.029914992,0.0005846552,0.000979577,0.0033291946,0.0005726975,0.0014778444,0.00164417,0.0015665464,0.00057894114],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015238615,0.00022551636,0.4317536,0.002339668,0.0016069602,0.0019411981,0.008304809,0.05963865,0.028186267,0.048176672,0.028511353,0.3877915],"study_design_scores_gemma":[0.0004086462,0.00058491563,0.6309811,0.0025302635,0.0019136396,0.001983493,0.010278094,0.10782525,0.03949511,0.033106823,0.17061263,0.00028006674],"about_ca_topic_score_codex":0.09384951,"about_ca_topic_score_gemma":0.21013951,"teacher_disagreement_score":0.09384951,"about_ca_system_score_codex":0.0015078901,"about_ca_system_score_gemma":0.003130593,"threshold_uncertainty_score":0.18660647},"labels":[],"label_agreement":null},{"id":"W2967600804","doi":"10.3390/rs11161848","title":"On the Segmentation of the Cephalonia–Lefkada Transform Fault Zone (Greece) from an InSAR Multi-Mode Dataset of the Lefkada 2015 Sequence","year":2019,"lang":"en","type":"article","venue":"Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Seventh Framework Programme; Japan Aerospace Exploration Agency; FP7 Research Potential of Convergence Regions; European Regional Development Fund; Canadian Space Agency; European Commission; European Space Agency","keywords":"Geology; Seismology; Subduction; Interferometric synthetic aperture radar; Fault (geology); Tectonics; Synthetic aperture radar; Geodesy; Remote sensing","score_opus":0.030667757064482087,"score_gpt":0.27077592812868273,"score_spread":0.24010817106420065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2967600804","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98217785,0.00041655637,0.002612055,0.00011853834,0.00004365209,0.000046945792,0.01249208,0.0002970667,0.0017952331],"genre_scores_gemma":[0.93142176,0.00026354176,0.0075506694,0.000041729945,0.000036455414,0.000046281228,0.059691884,0.00006286118,0.00088477915],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99978966,0.000024675732,0.000018626433,0.000089707086,0.00003180682,0.000045603767],"domain_scores_gemma":[0.9998293,0.000042791104,0.0000378319,0.000038423597,0.000028369692,0.00002333498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028754055,0.000591562,0.00036606204,0.0022054394,0.00019916946,0.00064263836,0.00044131035,0.0006875349,0.0009749081],"category_scores_gemma":[0.0007381735,0.00017493672,0.0006153071,0.0012630232,0.00035448078,0.00033669302,0.0006227202,0.00033834984,0.000703437],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015158392,0.0010730207,0.30307782,0.00100081,0.0009648161,0.0051395283,0.0014273751,0.42056087,0.06167028,0.0025445665,0.021700095,0.17932491],"study_design_scores_gemma":[0.00021043194,0.00022919178,0.7087137,0.00024154563,0.00013425441,0.00092621136,0.0011431967,0.2559197,0.008777134,0.0014875603,0.02212535,0.00009184546],"about_ca_topic_score_codex":0.013864678,"about_ca_topic_score_gemma":0.02784079,"teacher_disagreement_score":0.013864678,"about_ca_system_score_codex":0.00039529285,"about_ca_system_score_gemma":0.0005230533,"threshold_uncertainty_score":0.027567923},"labels":[],"label_agreement":null},{"id":"W2967808288","doi":"10.1007/s00024-019-02296-z","title":"Eigenoscillations and Stability of Rocking Stones: The Case Study of “The Hus Pulpit” in The Central Bohemian Pluton","year":2019,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Human Resources Research Institute","keywords":"Geology; Pluton; Seismology; Bedrock; Multiphysics; Geometry; Physics; Finite element method; Geomorphology; Mathematics","score_opus":0.013617586828253845,"score_gpt":0.20274279557728558,"score_spread":0.18912520874903174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2967808288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99917644,0.000017100674,0.00011511618,0.00002068846,4.4673183e-7,0.000001618413,0.000013286683,0.0000010408531,0.0006541788],"genre_scores_gemma":[0.999703,0.0000084601315,0.00005015214,9.573359e-7,2.657017e-7,7.90833e-7,0.000010619309,6.512564e-7,0.00022506402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998628,0.000036941474,0.00000641411,0.000026607055,0.000019810961,0.000047465783],"domain_scores_gemma":[0.99981195,0.00009121561,0.00002836038,0.000013684031,0.000019288744,0.000035499837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025442647,0.00013303864,0.00024215154,0.0006504689,0.0014351973,0.000987242,0.000624506,0.00044543153,0.0021924046],"category_scores_gemma":[0.00066747254,0.00010745741,0.00016358399,0.000988392,0.0019640976,0.0006655155,0.0010458819,0.00024375964,0.00008017481],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009032893,0.00040995018,0.7257027,0.0001877664,0.00020688352,0.020227069,0.070298314,0.054064788,0.008418631,0.06624267,0.0011857575,0.052152116],"study_design_scores_gemma":[0.00003599521,0.00025532354,0.8174583,0.000043169963,0.0000777123,0.0009934177,0.11325248,0.04652856,0.0026978177,0.013362015,0.005227747,0.00006759982],"about_ca_topic_score_codex":0.06906871,"about_ca_topic_score_gemma":0.13724755,"teacher_disagreement_score":0.06906871,"about_ca_system_score_codex":0.0015012738,"about_ca_system_score_gemma":0.00075007015,"threshold_uncertainty_score":0.13733333},"labels":[],"label_agreement":null},{"id":"W2968211911","doi":"10.1093/gji/ggz375","title":"Relative moment tensors and deep Yakutat seismicity","year":2019,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Induced seismicity; Seismology; Geology; Scaling; Amplitude; Microseism; Principal component analysis; Geometry; Physics; Mathematics; Statistics","score_opus":0.008034155846012216,"score_gpt":0.21087424935173002,"score_spread":0.2028400935057178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2968211911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8901585,0.0002017133,0.10422085,0.00017304289,0.000031891006,0.000012780677,0.00055604667,0.0005230279,0.0041220267],"genre_scores_gemma":[0.98269457,0.000047073092,0.01626365,0.000007699274,0.000012577575,0.0000058125042,0.00037786417,0.000044902896,0.0005458646],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999012,0.000013964928,0.0000074216064,0.000029282399,0.000032237003,0.000016021362],"domain_scores_gemma":[0.99978215,0.00004004526,0.00008207481,0.00002235801,0.000051627077,0.000021755253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020159014,0.00036930927,0.0002420606,0.0006259323,0.00026492577,0.000535089,0.0002705315,0.00020633983,0.0011486269],"category_scores_gemma":[0.0010758097,0.00024538374,0.00019824013,0.00053318613,0.0002563149,0.00044592898,0.00041821203,0.00039707852,0.00019430002],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044576192,0.00011681647,0.12533677,0.00017498533,0.00019867987,0.00050369755,0.0005988791,0.47135696,0.18702456,0.02050814,0.0017847302,0.19194996],"study_design_scores_gemma":[0.000018867773,0.000044940396,0.105463885,0.000025936855,0.000024705094,0.00012457755,0.00018771134,0.8767577,0.01037087,0.0046175974,0.0023138232,0.000049467828],"about_ca_topic_score_codex":0.009743886,"about_ca_topic_score_gemma":0.014912317,"teacher_disagreement_score":0.009743886,"about_ca_system_score_codex":0.0003211085,"about_ca_system_score_gemma":0.00046530354,"threshold_uncertainty_score":0.01937437},"labels":[],"label_agreement":null},{"id":"W2968268494","doi":"10.1029/2019jb017419","title":"Interseismic Quiescence and Triggered Slip of Active Normal Faults of Kīlauea Volcano's South Flank During 2001–2018","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"University of California Berkeley; National Aeronautics and Space Administration","keywords":"Geology; Seismology; Flank; Interferometric synthetic aperture radar; Volcano; Slip (aerodynamics); Rift zone; Geodesy; Fault (geology); Rift; Tectonics; Synthetic aperture radar; Remote sensing; Anatomy","score_opus":0.029393306890855595,"score_gpt":0.2894609964926335,"score_spread":0.2600676896017779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2968268494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992273,0.000038743776,0.000017646711,0.000015802772,0.00000276693,0.000001909893,0.00036052626,0.0000045580264,0.00033081573],"genre_scores_gemma":[0.9988844,0.000038244012,0.00005081339,0.000006935925,0.000007018339,0.0000040856175,0.0007256874,0.0000017628754,0.00028105197],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999186,0.000005576527,0.0000062671684,0.00002405523,0.000022902454,0.00002257925],"domain_scores_gemma":[0.9997048,0.000022407401,0.00012841383,0.000015679256,0.00006833197,0.000060333467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015329657,0.00021895341,0.00016112799,0.0007593369,0.00029131921,0.0003884499,0.0002217335,0.0001671501,0.00087027374],"category_scores_gemma":[0.0005170526,0.00010375622,0.00012168208,0.00057459145,0.00026101258,0.00026154393,0.0003346032,0.00016565625,0.00014463105],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001296058,0.000043660293,0.9822397,0.0000418907,0.000045161454,0.00042118778,0.0013954934,0.0003642293,0.0066369846,0.00006140827,0.000569054,0.008051587],"study_design_scores_gemma":[0.0000012109356,0.0000100211455,0.9991999,0.0000033735985,0.000003763155,0.000026702728,0.0001822859,0.00015667998,0.00012313583,0.0000043544755,0.0002873424,0.0000012753976],"about_ca_topic_score_codex":0.037006237,"about_ca_topic_score_gemma":0.088997856,"teacher_disagreement_score":0.037006237,"about_ca_system_score_codex":0.0006136134,"about_ca_system_score_gemma":0.00032868987,"threshold_uncertainty_score":0.073581636},"labels":[],"label_agreement":null},{"id":"W2969531188","doi":"10.1785/0120190035","title":"Stress Drops and Directivity of Induced Earthquakes in the Western Canada Sedimentary Basin","year":2019,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Geology; Seismic moment; Directivity; Induced seismicity; Seismic hazard; Moment magnitude scale; Attenuation; Drop (telecommunication); Mathematics; Geometry; Physics; Scaling; Engineering; Optics","score_opus":0.010415607219279283,"score_gpt":0.19147420564322593,"score_spread":0.18105859842394664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969531188","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99897206,0.00002234601,0.000057933285,0.000010390531,5.122892e-7,0.0000030434032,0.00023587924,0.0000061536507,0.0006918336],"genre_scores_gemma":[0.9995596,0.00001996225,0.00003501302,0.0000021622193,3.8837538e-7,0.0000012742527,0.00021942554,0.0000014748008,0.00016074166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998085,0.000006557237,0.000008972917,0.000027156088,0.000103236445,0.000045632423],"domain_scores_gemma":[0.99935013,0.000063512794,0.00011754217,0.000025784562,0.00032937923,0.00011357906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012921174,0.00024626573,0.00020554516,0.0016748953,0.00074142497,0.0008211155,0.00047893482,0.00021524186,0.0012743135],"category_scores_gemma":[0.0014371203,0.00018760824,0.00015503069,0.0017466847,0.0006408109,0.0002115301,0.0005615558,0.00018964199,0.0001266614],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013665995,0.00004593331,0.9747574,0.00002887792,0.0000821466,0.0003581268,0.0009519722,0.006297039,0.0053918706,0.00026913447,0.00040342132,0.01127732],"study_design_scores_gemma":[0.0000018273828,0.0000049437967,0.99721897,0.0000033499798,0.000003873509,0.000016668137,0.0002642363,0.0021050517,0.00021634193,0.000025702868,0.0001350662,0.000003992757],"about_ca_topic_score_codex":0.9290504,"about_ca_topic_score_gemma":0.9473541,"teacher_disagreement_score":0.070949614,"about_ca_system_score_codex":0.005784685,"about_ca_system_score_gemma":0.0025559124,"threshold_uncertainty_score":0.14273483},"labels":[],"label_agreement":null},{"id":"W2969795225","doi":"","title":"Inter-seismic and post-seismic tectonic movements detected during the 17th century earthquake and inferred from diatom analysis in Tokachi area, Hokkaido, Japan","year":2019,"lang":"en","type":"article","venue":"Japan Geoscience Union","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Nutrasource","funders":"","keywords":"Geology; Seismology; Tectonics; Subduction","score_opus":0.005727059832507939,"score_gpt":0.18777250350403069,"score_spread":0.18204544367152276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969795225","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956137,0.000050267663,0.000020661191,0.000008579687,0.0000020037287,0.0000012857417,0.00013642461,7.7936e-7,0.00021865449],"genre_scores_gemma":[0.9991047,0.0001183689,0.0000776354,0.000009233973,0.0000051111547,0.0000045433203,0.00036900913,9.579226e-7,0.00031042227],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990094,0.0000061889546,0.000014456682,0.000028299897,0.000014678027,0.000035530127],"domain_scores_gemma":[0.99971515,0.000023924382,0.0000998223,0.000010635025,0.000072174524,0.000078185345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019314115,0.00021218458,0.00019751677,0.0014508277,0.00053538027,0.0004172959,0.00027346006,0.00027155536,0.0007853459],"category_scores_gemma":[0.00025542398,0.00022692564,0.00018531443,0.001814487,0.0004443562,0.0003177777,0.0005449158,0.00020518016,0.00013553473],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000836269,0.000022951826,0.99021834,0.000025564304,0.000047545043,0.0003200795,0.0014535949,0.00014707622,0.0042220647,0.00004615313,0.00011422367,0.003298751],"study_design_scores_gemma":[0.0000015532287,0.000007456685,0.9990971,0.0000020507644,0.000012412511,0.000028640361,0.000574016,0.00005080459,0.00006688252,0.0000041493286,0.00015329695,0.0000015549301],"about_ca_topic_score_codex":0.072080605,"about_ca_topic_score_gemma":0.1674693,"teacher_disagreement_score":0.072080605,"about_ca_system_score_codex":0.00075236236,"about_ca_system_score_gemma":0.0008820464,"threshold_uncertainty_score":0.14332211},"labels":[],"label_agreement":null},{"id":"W2970219811","doi":"10.1785/0120190055","title":"An Earthquake Nest in Cascadia","year":2019,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismology; Subduction; Slab; Mantle (geology); Crust; Geophysics; Tectonics","score_opus":0.01095016980269941,"score_gpt":0.20766183639917907,"score_spread":0.19671166659647965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970219811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990619,0.000014113577,0.000042338612,0.000021152446,0.0000013888532,0.0000039172405,0.00016552588,0.0000096553285,0.0006800659],"genre_scores_gemma":[0.9993352,0.00001124963,0.00004643131,0.0000056581684,0.0000012105835,0.0000033248991,0.00032083192,0.0000020939522,0.00027398826],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998584,0.00001555718,0.000007331485,0.000038619717,0.00003336688,0.000046617693],"domain_scores_gemma":[0.9992823,0.000049422026,0.00016405385,0.00005928364,0.00011156221,0.00033339878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013544185,0.00019587703,0.00027361469,0.0009245261,0.0011646065,0.00052978814,0.0002393676,0.00031936492,0.0016239586],"category_scores_gemma":[0.0006701812,0.00014944203,0.00017255972,0.0007894506,0.00054759433,0.00019019576,0.0010031951,0.00023843734,0.00019265946],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018034072,0.000054178734,0.9831277,0.000033042263,0.000045537825,0.0013136399,0.0019625344,0.0011543225,0.00589317,0.00023158347,0.00075771264,0.005246348],"study_design_scores_gemma":[0.0000058038418,0.000050874132,0.9974733,0.000003390126,0.000009209563,0.00016605038,0.0010873977,0.00035721392,0.00013620415,0.00004629559,0.00065933604,0.0000048874736],"about_ca_topic_score_codex":0.064965665,"about_ca_topic_score_gemma":0.16033633,"teacher_disagreement_score":0.93503433,"about_ca_system_score_codex":0.0011247762,"about_ca_system_score_gemma":0.0008735021,"threshold_uncertainty_score":0.12917507},"labels":[],"label_agreement":null},{"id":"W2970233615","doi":"10.1029/2019tc005680","title":"Cumulative and Coseismic (During the 2016 M<sub>w</sub>6.6 Aketao Earthquake) Deformation of the Dextral‐Slip Muji Fault, Northeastern Pamir Orogen","year":2019,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Deutsche Forschungsgemeinschaft; Innovative Research Group Project of the National Natural Science Foundation of China","keywords":"Geology; Seismology; Slip (aerodynamics); Fault (geology); Aftershock; Seismic gap; Seismic hazard; Sinistral and dextral; Tectonics; Active fault; Elastic-rebound theory","score_opus":0.008614871583777554,"score_gpt":0.19117428479850332,"score_spread":0.18255941321472577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970233615","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99959916,0.00001505582,0.000032208496,0.0000050851763,0.0000013444635,0.0000012956104,0.00006594388,0.0000021032763,0.00027775325],"genre_scores_gemma":[0.9996246,0.000028760229,0.00005617597,0.0000027450963,0.0000030223284,0.000002216273,0.00014758775,6.572943e-7,0.00013427704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999349,0.000007031626,0.0000071093646,0.000020262278,0.000012563078,0.00001815393],"domain_scores_gemma":[0.999871,0.000010644923,0.00006202657,0.0000120973355,0.000019456293,0.00002477064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116037125,0.00021526446,0.00012740005,0.0007935593,0.00029581352,0.00032455125,0.00016545608,0.00017450572,0.0007163201],"category_scores_gemma":[0.00029311955,0.000109480396,0.00013557586,0.0008403727,0.0002207067,0.0002228309,0.0004558744,0.00013710915,0.00015607594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014953424,0.000036270594,0.97363317,0.000033203556,0.000039428545,0.00037626084,0.00079547573,0.0006694113,0.009453633,0.00009134014,0.00015580794,0.014566507],"study_design_scores_gemma":[9.203792e-7,0.000017302586,0.999253,0.0000025327345,0.0000056036083,0.000053190455,0.00015622708,0.00025992905,0.00013405469,0.000007160579,0.00010868261,0.0000013798553],"about_ca_topic_score_codex":0.006694084,"about_ca_topic_score_gemma":0.019584028,"teacher_disagreement_score":0.006694084,"about_ca_system_score_codex":0.00022145377,"about_ca_system_score_gemma":0.00020129453,"threshold_uncertainty_score":0.013310254},"labels":[],"label_agreement":null},{"id":"W2970330873","doi":"10.1126/sciadv.aav7172","title":"The role of aseismic slip in hydraulic fracturing–induced seismicity","year":2019,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":295,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; University of Calgary","funders":"Canada First Research Excellence Fund; Microseismic Industry Consortium","keywords":"Hydraulic fracturing; Induced seismicity; Geology; Creep; Slip (aerodynamics); Geotechnical engineering; Fault (geology); Seismology; Materials science; Engineering; Composite material","score_opus":0.007308228647912735,"score_gpt":0.22363586788454162,"score_spread":0.2163276392366289,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970330873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972365,0.00012351957,0.0012624577,0.00004964959,0.0000019625597,0.0000039166293,0.00003549044,0.000021767095,0.0012646262],"genre_scores_gemma":[0.9998388,0.000027975844,0.00007508376,0.0000030012939,0.0000014029738,9.4315425e-7,0.0000087073795,9.599108e-7,0.000043059317],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989426,0.000027324635,0.000011314028,0.000026223319,0.000019232159,0.000021690319],"domain_scores_gemma":[0.9994043,0.0002157799,0.00019471569,0.000053298147,0.000052078445,0.00007993594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003454109,0.00021582242,0.00021756289,0.00036007923,0.00023660097,0.0004635725,0.00024506342,0.00034536826,0.0010172699],"category_scores_gemma":[0.0012300723,0.00015885448,0.00013407669,0.00015470818,0.000598983,0.0005922906,0.00041892866,0.00021598773,0.00013221244],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009577758,0.00038155174,0.2807635,0.00023612626,0.00007541498,0.0008634228,0.00076366076,0.027961323,0.652978,0.0054831565,0.00017724845,0.029358726],"study_design_scores_gemma":[0.00004822769,0.0008080333,0.844204,0.000021275759,0.00005166606,0.000662931,0.00049783546,0.08665264,0.06017553,0.006105201,0.00073063275,0.00004204497],"about_ca_topic_score_codex":0.0011587649,"about_ca_topic_score_gemma":0.0012005359,"teacher_disagreement_score":0.0011587649,"about_ca_system_score_codex":0.0003738653,"about_ca_system_score_gemma":0.00018497513,"threshold_uncertainty_score":0.0034031272},"labels":[],"label_agreement":null},{"id":"W2970553439","doi":"10.1093/gji/ggz396","title":"3-D attenuation tomography from microseismicity in a mine","year":2019,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Microseismic Industry Consortium","keywords":"Geology; Microseism; Seismology; Attenuation; Geophone; Inversion (geology); Tomography; Seismic wave; Amplitude; Moment magnitude scale; Seismic tomography; Geodesy; Mineralogy; Mantle (geology); Geophysics; Tectonics; Geometry; Optics; Physics","score_opus":0.009169397250667486,"score_gpt":0.21520773307283725,"score_spread":0.20603833582216977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970553439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98285335,0.00003358038,0.0150674265,0.000026743675,0.0000025045024,0.000016755215,0.00045286026,0.00024330396,0.0013035394],"genre_scores_gemma":[0.9942846,0.000024416742,0.0051668216,0.0000036153237,0.0000021831418,0.0000060505167,0.0002778982,0.000016072252,0.0002184656],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991584,0.000008707602,0.0000044386447,0.000016215836,0.00003706656,0.000017767725],"domain_scores_gemma":[0.9998091,0.00004937843,0.000042468582,0.000020505015,0.000060973063,0.000017611545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011801155,0.00027941386,0.00017636738,0.00090564106,0.00012389933,0.00032998784,0.0002088355,0.00024524177,0.0012413185],"category_scores_gemma":[0.0005140604,0.00021891564,0.00026033208,0.0008029868,0.00017447145,0.00027274713,0.0002571643,0.00020154171,0.0002705973],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00068749854,0.00028412577,0.19990844,0.00017428458,0.00013992678,0.0023039135,0.0010269351,0.182239,0.52987546,0.00083882763,0.00082756445,0.08169399],"study_design_scores_gemma":[0.000046989822,0.00022316034,0.54814637,0.000021692023,0.00004748599,0.0009149438,0.00045037305,0.4037152,0.04445437,0.0005442285,0.0013727535,0.00006254954],"about_ca_topic_score_codex":0.004853853,"about_ca_topic_score_gemma":0.0078663435,"teacher_disagreement_score":0.004853853,"about_ca_system_score_codex":0.00019837572,"about_ca_system_score_gemma":0.0002219922,"threshold_uncertainty_score":0.009651184},"labels":[],"label_agreement":null},{"id":"W2971314008","doi":"10.3390/rs11171999","title":"Source Characteristics of the 28 September 2018 Mw 7.4 Palu, Indonesia, Earthquake Derived from the Advanced Land Observation Satellite 2 Data","year":2019,"lang":"en","type":"article","venue":"Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Geodesy; Sinistral and dextral; Synthetic aperture radar; Fault (geology); Slip (aerodynamics); Radar; Satellite; Epicenter; Remote sensing; Computer science","score_opus":0.03053459226885919,"score_gpt":0.22030505412856524,"score_spread":0.18977046185970606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971314008","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89308727,0.00028036715,0.0018392926,0.00025245044,0.00014044257,0.00012351677,0.09652197,0.00044509416,0.007309481],"genre_scores_gemma":[0.90789866,0.00032542564,0.0021615645,0.00004939968,0.00011214098,0.0001852081,0.08744712,0.00009658761,0.0017238508],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999864,0.000007090735,0.000022140814,0.000031851498,0.00005139848,0.00002349559],"domain_scores_gemma":[0.9995314,0.00005702951,0.00011823631,0.000042542546,0.00021647479,0.00003437206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015352183,0.00062790577,0.0003779291,0.0013814463,0.00023829415,0.00038112927,0.00041574202,0.000356614,0.0020312683],"category_scores_gemma":[0.0007081955,0.00021290156,0.0001819888,0.0025389497,0.00012775333,0.00032926255,0.00032045468,0.00038316468,0.0011563991],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009234527,0.0006893689,0.7402381,0.0011792165,0.0002643899,0.007023821,0.00092676876,0.032290567,0.03356683,0.00088924123,0.06314675,0.118861526],"study_design_scores_gemma":[0.000071753435,0.00005084588,0.9617719,0.00006886142,0.00006647173,0.00058765156,0.00048683383,0.021561872,0.0044087237,0.00020101498,0.010673825,0.000050327984],"about_ca_topic_score_codex":0.014964535,"about_ca_topic_score_gemma":0.01306356,"teacher_disagreement_score":0.014964535,"about_ca_system_score_codex":0.00031068097,"about_ca_system_score_gemma":0.0004094564,"threshold_uncertainty_score":0.029754817},"labels":[],"label_agreement":null},{"id":"W2971547384","doi":"10.5459/bnzsee.44.3.123-166","title":"The M8.8 Chile earthquake, 27 February 2010","year":2011,"lang":"en","type":"article","venue":"Bulletin of the New Zealand Society for Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Plate tectonics; Margin (machine learning); Tectonics; Geography","score_opus":0.013225351768963136,"score_gpt":0.18001542084826197,"score_spread":0.16679006907929883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971547384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.58176875,0.006885252,0.0005827201,0.009318099,0.0012025792,0.0004746729,0.038621377,0.0004474091,0.36069912],"genre_scores_gemma":[0.7312382,0.018010775,0.0014780582,0.0014421049,0.0009360275,0.0004040536,0.04588121,0.00014481883,0.20046477],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9998857,0.000007654651,0.000007969056,0.00001062666,0.00006302381,0.000024963332],"domain_scores_gemma":[0.99983966,0.00001195095,0.000047252317,0.000010387947,0.00006535668,0.000025419367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018544028,0.00029233837,0.00017114296,0.0008358892,0.00075436395,0.0009390568,0.00024924133,0.0004138716,0.0052444083],"category_scores_gemma":[0.00094145414,0.000120875564,0.00010357088,0.0013984864,0.00026527152,0.00040081984,0.0010741098,0.00045163019,0.0015447955],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044051136,0.00016040784,0.11758194,0.0018885266,0.000056003184,0.0049816635,0.019666398,0.000744529,0.010660453,0.004677727,0.60018635,0.23895556],"study_design_scores_gemma":[0.000025441104,0.000055972116,0.36180925,0.00030657483,0.000010977506,0.0003792594,0.005155162,0.00009456999,0.0012586655,0.0002965025,0.63058156,0.000026121808],"about_ca_topic_score_codex":0.068211526,"about_ca_topic_score_gemma":0.16676983,"teacher_disagreement_score":0.068211526,"about_ca_system_score_codex":0.0019290863,"about_ca_system_score_gemma":0.002031744,"threshold_uncertainty_score":0.135629},"labels":[],"label_agreement":null},{"id":"W2971636029","doi":"10.1029/2019gl084536","title":"A Model of Shallow Viscoelastic Relaxation for Seismically Induced Tension Cracks in the Chile‐Peru Forearc","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Forearc; Geology; Tension (geology); Seismology; Crust; Submarine pipeline; Deformation (meteorology); Relaxation (psychology); Viscoelasticity; Subduction; Geotechnical engineering; Geophysics; Tectonics; Materials science; Compression (physics); Composite material","score_opus":0.06215352900652295,"score_gpt":0.2953673109117366,"score_spread":0.2332137819052137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971636029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93483573,0.00045255604,0.03382152,0.0018594094,0.000047006393,0.000079941965,0.0005335686,0.00026192618,0.02810838],"genre_scores_gemma":[0.9944305,0.0001267979,0.0007878153,0.0000408398,0.000009782566,0.000048951937,0.000050005383,0.000019489198,0.004485738],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999372,0.00001835921,0.000002740968,0.000014434433,0.0000072836406,0.000020054506],"domain_scores_gemma":[0.9997594,0.00008024677,0.000056113935,0.0000149763855,0.000038331465,0.000050895702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002385517,0.00040699285,0.00040776623,0.00046864757,0.00072372175,0.00089386763,0.0014632208,0.002387583,0.005310691],"category_scores_gemma":[0.0007568629,0.00045229128,0.00058375316,0.00032838574,0.000982995,0.0008678094,0.0006986434,0.00064712064,0.00034378355],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010004123,0.000096205775,0.0033294917,0.000049981772,0.000027403901,0.00068315456,0.00016203396,0.9715973,0.005382587,0.016350584,0.0008593311,0.0013618765],"study_design_scores_gemma":[0.000038605045,0.000028757948,0.0007779526,0.0000055942196,0.0000066580214,0.00003303737,0.000044802542,0.99729246,0.000085428546,0.0014188765,0.00025813282,0.000009778643],"about_ca_topic_score_codex":0.031098662,"about_ca_topic_score_gemma":0.011167585,"teacher_disagreement_score":0.031098662,"about_ca_system_score_codex":0.0013405528,"about_ca_system_score_gemma":0.00082681054,"threshold_uncertainty_score":0.06183529},"labels":[],"label_agreement":null},{"id":"W2972019283","doi":"10.1038/s41467-019-11958-4","title":"Forecasting the magnitude of the largest expected earthquake","year":2019,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Aftershock; Seismology; Sequence (biology); Magnitude (astronomy); Induced seismicity; Geology; Maximum magnitude; Remotely triggered earthquakes; Seismic hazard; Bayesian probability; Foreshock; Earthquake prediction; Earthquake swarm; Statistics; Mathematics; Physics","score_opus":0.028704916277289785,"score_gpt":0.24481461626981021,"score_spread":0.21610969999252044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972019283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9704333,0.00009865945,0.027427997,0.00026416467,0.000013117123,0.000011275093,0.0002972469,0.000078280784,0.0013760662],"genre_scores_gemma":[0.99473685,0.000043147276,0.004801391,0.0000074082577,0.00001090106,0.0000045608485,0.00021249015,0.0000036813346,0.00017948377],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991894,0.00002538594,0.000004992494,0.000024916071,0.000012164241,0.0000136279805],"domain_scores_gemma":[0.9987326,0.0006414732,0.00032067054,0.000047314203,0.00015225512,0.000105707506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053629786,0.00021250609,0.00020903311,0.00060455693,0.000121321886,0.00035738622,0.000253693,0.00048813462,0.0006946973],"category_scores_gemma":[0.0042674583,0.00020877637,0.00014105595,0.00035255757,0.00016941286,0.00041286522,0.000326125,0.00036095324,0.00017005505],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025679567,0.0001036633,0.41008797,0.000057141617,0.00008430982,0.0003261716,0.00019157778,0.5253762,0.0067084,0.0065093376,0.0024266734,0.047871843],"study_design_scores_gemma":[0.000011062916,0.000044078304,0.08872379,0.000011201598,0.000016134625,0.00005050615,0.00009116397,0.9071164,0.00087625283,0.002648286,0.00039833735,0.000012802879],"about_ca_topic_score_codex":0.0055346424,"about_ca_topic_score_gemma":0.00798852,"teacher_disagreement_score":0.0055346424,"about_ca_system_score_codex":0.0002661676,"about_ca_system_score_gemma":0.00032286224,"threshold_uncertainty_score":0.011004865},"labels":[],"label_agreement":null},{"id":"W2972561650","doi":"","title":"DOWNDIP LANDWARD LIMIT OF CASCADIA GREAT EARTHQUAKE RUPTURE","year":2014,"lang":"en","type":"article","venue":"2014 GSA Annual Meeting in Vancouver, British Columbia (19–22 October 2014)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Subduction; Seismic hazard; Slip (aerodynamics); Episodic tremor and slip; Submarine pipeline; Thrust; Thrust fault; Earthquake rupture; Tectonics; Geotechnical engineering; Fault (geology)","score_opus":0.006612065818914438,"score_gpt":0.19751647322145455,"score_spread":0.1909044074025401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972561650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.937384,0.0015449262,0.003165477,0.0004386143,0.00003283004,0.000032204323,0.0017383496,0.000130729,0.055532876],"genre_scores_gemma":[0.99743915,0.0003140334,0.00028824306,0.00003902445,0.000019902262,0.000010665802,0.0008044688,0.000013675088,0.0010708598],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966526,0.000051371953,0.000034997665,0.00006627192,0.00012164676,0.00006044056],"domain_scores_gemma":[0.99854636,0.00026831776,0.00044279022,0.00013378548,0.00041555095,0.00019316493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047980255,0.0002774246,0.00022404222,0.0013969842,0.0005784017,0.0009883473,0.0004593841,0.0002669539,0.0058209724],"category_scores_gemma":[0.0033169219,0.00013469266,0.00017071531,0.00058324233,0.00050607993,0.00056573923,0.0010597894,0.00028157947,0.00083574106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033333348,0.000032437223,0.92236024,0.00027151688,0.00007558975,0.0011749456,0.0010510498,0.013041719,0.016475419,0.0052706045,0.0040192343,0.035893977],"study_design_scores_gemma":[0.000009082833,0.00007710475,0.9812222,0.00008471757,0.00002436671,0.00052922685,0.00071323465,0.004003369,0.0018476158,0.0022339444,0.009233261,0.000021879661],"about_ca_topic_score_codex":0.013188999,"about_ca_topic_score_gemma":0.021313127,"teacher_disagreement_score":0.986811,"about_ca_system_score_codex":0.0006299897,"about_ca_system_score_gemma":0.00042072096,"threshold_uncertainty_score":0.026224434},"labels":[],"label_agreement":null},{"id":"W2972636138","doi":"10.3390/rs11182112","title":"Fractal Study of the 1997–2017 Italian Seismic Sequences: A Joint Analysis of Seismological Data and DInSAR Measurements","year":2019,"lang":"en","type":"article","venue":"Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Japan Aerospace Exploration Agency; Canadian Space Agency; European Commission; European Space Agency","keywords":"Geology; Seismology; Fractal dimension; Joint (building); Fractal; Epicenter; Fractal analysis; Geodesy","score_opus":0.10652198037420735,"score_gpt":0.2735944797164407,"score_spread":0.16707249934223334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972636138","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99609864,0.0001823964,0.0017310751,0.000041067124,0.000010599868,0.0000079991405,0.0011226534,0.000049820716,0.0007556859],"genre_scores_gemma":[0.99551207,0.0001127768,0.0011285658,0.0000060448165,0.000026388427,0.000007682041,0.0030510125,0.000009040476,0.00014649917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998043,0.00002061753,0.00002094844,0.000049816706,0.000052345913,0.000051917854],"domain_scores_gemma":[0.99925584,0.00015703654,0.00025504918,0.000100547775,0.00014007484,0.00009146245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057077385,0.00033294436,0.00027636124,0.0043506464,0.00016576465,0.0004467308,0.00016895389,0.00025080988,0.00037823274],"category_scores_gemma":[0.0012063375,0.00010910396,0.0004428291,0.0020094851,0.0002726356,0.0003170091,0.000357641,0.0001937007,0.0001412534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031386758,0.00014070078,0.858845,0.00020708358,0.00038802816,0.0013959305,0.00080516783,0.03353841,0.02047471,0.0015089528,0.0024596357,0.07992256],"study_design_scores_gemma":[0.0000048382917,0.00003467812,0.96516,0.000015454269,0.00006902417,0.00033928262,0.00018565553,0.03148051,0.0010834995,0.0001789028,0.0014276203,0.000020492136],"about_ca_topic_score_codex":0.006100788,"about_ca_topic_score_gemma":0.0063312645,"teacher_disagreement_score":0.006100788,"about_ca_system_score_codex":0.00031704237,"about_ca_system_score_gemma":0.00025435493,"threshold_uncertainty_score":0.012130499},"labels":[],"label_agreement":null},{"id":"W2972809293","doi":"10.1061/9780784482612.009","title":"Design Challenges—B Jetty Reconstruction, Canadian Forces Base in Esquimalt, British Columbia, Canada","year":2019,"lang":"en","type":"article","venue":"Ports 2019","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Golder Associates (Canada)","funders":"","keywords":"Jetty; Foundation (evidence); Engineering; Rock blasting; Civil engineering; Submarine pipeline; Base (topology); Construction engineering; Marine engineering; Mining engineering; Geology; Geotechnical engineering; Archaeology; Geography; Oceanography","score_opus":0.012429743066291478,"score_gpt":0.16486008945004751,"score_spread":0.15243034638375605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972809293","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.55449903,0.0046909004,0.029825198,0.017334431,0.00074085075,0.0011428942,0.0035084956,0.0011036823,0.38715455],"genre_scores_gemma":[0.72164184,0.0037742185,0.035891753,0.0012167506,0.000039796625,0.00021338412,0.0028305429,0.0003185299,0.23407315],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99849606,0.00008187391,0.00002481812,0.000097932425,0.0009651564,0.000334083],"domain_scores_gemma":[0.9981217,0.00008010783,0.000037889477,0.00005761202,0.0013890147,0.00031366592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014893025,0.00041466622,0.0001948646,0.0007914644,0.0058933143,0.0031575824,0.0011773054,0.00074101315,0.008524261],"category_scores_gemma":[0.0014909364,0.0003794446,0.00024126064,0.001224897,0.0010602423,0.0005719521,0.0009489245,0.0011003992,0.0011898209],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060444605,0.00043886452,0.07531901,0.0008019279,0.00008082927,0.0057437955,0.006900816,0.030399764,0.036915757,0.027469,0.13905537,0.6762704],"study_design_scores_gemma":[0.000103440674,0.0004589638,0.12688784,0.0004678581,0.000056219185,0.0012614869,0.022115063,0.012255206,0.009699974,0.0014819561,0.8250591,0.00015288519],"about_ca_topic_score_codex":0.9697211,"about_ca_topic_score_gemma":0.99233043,"teacher_disagreement_score":0.030278921,"about_ca_system_score_codex":0.028785827,"about_ca_system_score_gemma":0.09043288,"threshold_uncertainty_score":0.20885676},"labels":[],"label_agreement":null},{"id":"W2973357131","doi":"10.62879/c80148501","title":"Earthquake-Rotated Headstones as a Means of Re-evaluating Epicentral Location of the 1944 Massena-Cornwall Earthquake: New York, United States and Ontario, Canada","year":2019,"lang":"en","type":"article","venue":"The Compass Earth Science Journal of Sigma Gamma Epsilon","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"St. Lawrence University; State University of New York","keywords":"Epicenter; Seismology; Geology; Graben; Clockwise; Geodesy; Geological survey; Rotation (mathematics); Geometry; Tectonics; Paleontology; Mathematics","score_opus":0.030087191714039868,"score_gpt":0.23889399520865917,"score_spread":0.2088068034946193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2973357131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9759459,0.00066100725,0.0010851155,0.00009498767,0.000023171744,0.0001545752,0.008724371,0.00007731145,0.013233616],"genre_scores_gemma":[0.98554915,0.00062107993,0.0025256088,0.000020557309,0.000009644348,0.00010780087,0.0067723067,0.000048154005,0.004345683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995171,0.000037203925,0.00004335077,0.00009332591,0.00019682228,0.00011223197],"domain_scores_gemma":[0.99842864,0.00007484204,0.00017559684,0.00008263105,0.0010854341,0.00015286513],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004967033,0.0005577049,0.0003728006,0.0036193202,0.0012644033,0.0013366421,0.0008493387,0.00022237119,0.0033900153],"category_scores_gemma":[0.0030047714,0.0002461129,0.00025630757,0.007695687,0.000635428,0.00037707423,0.0010494591,0.00029496837,0.0004566233],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003107199,0.000049801976,0.93809754,0.00014366454,0.00014928776,0.00045694935,0.004003891,0.003629214,0.004236867,0.0009993963,0.004899094,0.04302365],"study_design_scores_gemma":[0.000012856586,0.000012155065,0.99041194,0.000022097302,0.000027697439,0.00002855276,0.0021256171,0.00144531,0.00036094812,0.000043691034,0.0054926146,0.000016441378],"about_ca_topic_score_codex":0.9907402,"about_ca_topic_score_gemma":0.9969146,"teacher_disagreement_score":0.013111001,"about_ca_system_score_codex":0.013111001,"about_ca_system_score_gemma":0.01364458,"threshold_uncertainty_score":0.095127404},"labels":[],"label_agreement":null},{"id":"W2973786500","doi":"10.1785/0120190008","title":"Seismic Characteristics of the Nootka Fault Zone: Results from the Seafloor Earthquake Array Japan–Canada Cascadia Experiment (SeaJade)","year":2019,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"","keywords":"Geology; Seismology; Subduction; Seafloor spreading; Oceanic crust; Fault (geology); Seismometer; Plate tectonics; Transform fault; Crust; Thrust fault; Tectonics; Paleontology","score_opus":0.010258514387896297,"score_gpt":0.1904046083631189,"score_spread":0.1801460939752226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2973786500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99812716,0.00005904538,0.00003550903,0.000013913017,0.00000301079,0.000008454461,0.0012400852,0.00000467019,0.00050813577],"genre_scores_gemma":[0.99674183,0.00007116967,0.00011826456,0.00001316351,0.000003367836,0.000010084461,0.002506449,0.0000059560825,0.0005297087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997013,0.000023616976,0.000023454204,0.00007984927,0.00009450647,0.0000771811],"domain_scores_gemma":[0.9992174,0.000043517477,0.0001121735,0.000061410574,0.0003334468,0.00023203267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024305134,0.00038333162,0.0003188459,0.0010194723,0.0008676626,0.0005797175,0.0003112508,0.00037798926,0.0006926176],"category_scores_gemma":[0.0006021458,0.00020885024,0.0002592754,0.0012023923,0.00050939777,0.00020144161,0.00048461158,0.0002357925,0.00019644077],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018985193,0.000044058725,0.9913225,0.00002371917,0.000054800395,0.00017904179,0.00053164916,0.0004767509,0.004042904,0.000026646088,0.00039028082,0.0027177846],"study_design_scores_gemma":[0.00000368477,0.0000070868296,0.99944574,0.0000019552335,0.0000066823372,0.00001618532,0.00013857757,0.0001021844,0.000095553565,0.0000022143258,0.00017766852,0.000002508595],"about_ca_topic_score_codex":0.6830863,"about_ca_topic_score_gemma":0.88345385,"teacher_disagreement_score":0.31691372,"about_ca_system_score_codex":0.0022478139,"about_ca_system_score_gemma":0.0013774688,"threshold_uncertainty_score":0.6375601},"labels":[],"label_agreement":null},{"id":"W2974713752","doi":"10.22215/etd/2017-11973","title":"Analyses of earthquakes in the Western Quebec Seismic Zone using data from the United States Transportable Array","year":2017,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Resources Canada; National Science Foundation","keywords":"Seismology; Aftershock; Geology; Induced seismicity; Focal mechanism; Relocation; Seismic zone; Earthquake location; Geodesy","score_opus":0.11724766372094238,"score_gpt":0.3288190322026408,"score_spread":0.21157136848169844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2974713752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9768025,0.00047851406,0.0014804087,0.00013816103,0.000015326941,0.000083404564,0.014832188,0.000101661295,0.0060677854],"genre_scores_gemma":[0.98091424,0.00032347065,0.0019146708,0.000045759218,0.000008197355,0.000033806566,0.01410372,0.000015055735,0.0026412087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99969757,0.000031322823,0.000016387765,0.00004982631,0.00013123378,0.00007364623],"domain_scores_gemma":[0.99854016,0.00011490341,0.00017622646,0.000063542764,0.00096938113,0.00013582112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003503716,0.0004067268,0.00019108373,0.0024807989,0.0006667296,0.0006451467,0.00040344676,0.00017666376,0.001275817],"category_scores_gemma":[0.0016096345,0.00011039854,0.00020106665,0.004526227,0.00018358404,0.00020739133,0.000383262,0.00021918023,0.00022645186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015440032,0.000059414324,0.9278056,0.000071235474,0.00017542561,0.00031079442,0.0005137987,0.0066587357,0.004606558,0.00031582016,0.005847367,0.053480785],"study_design_scores_gemma":[0.0000048463676,0.000014223158,0.990756,0.000012805574,0.000019525702,0.000027878947,0.00044005565,0.00478362,0.0004373861,0.000013012518,0.0034780358,0.0000125867755],"about_ca_topic_score_codex":0.9871607,"about_ca_topic_score_gemma":0.99419314,"teacher_disagreement_score":0.012839317,"about_ca_system_score_codex":0.0059408583,"about_ca_system_score_gemma":0.005764407,"threshold_uncertainty_score":0.043104112},"labels":[],"label_agreement":null},{"id":"W2977733879","doi":"10.1144/sp477.33","title":"Slope failures along the deformation front of the Cascadia margin: linking slide morphology to subduction zone parameters","year":2018,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Subduction; Margin (machine learning); Seismology; Deformation (meteorology); Front (military); Oceanography; Tectonics","score_opus":0.02225957911878712,"score_gpt":0.22414523102657616,"score_spread":0.20188565190778904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2977733879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99922526,0.000020489737,0.00006844839,0.000013342174,8.4598514e-7,0.0000019828667,0.00022663435,0.000012920917,0.0004300959],"genre_scores_gemma":[0.99967027,0.000012724101,0.000030948435,0.0000013652262,6.450693e-7,0.0000012855924,0.00018177491,0.0000021967428,0.00009886852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998294,0.000027054703,0.00001682719,0.000059391386,0.000035936195,0.00003129458],"domain_scores_gemma":[0.9990269,0.00016359048,0.00028330396,0.0000940843,0.00020428363,0.0002278642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031466378,0.00047216465,0.00023065005,0.0016544391,0.00034992545,0.0007424951,0.00018658675,0.00032972303,0.0016922203],"category_scores_gemma":[0.0015865285,0.0002489525,0.00025638432,0.0012787496,0.0004063429,0.00028714468,0.00054006925,0.00021594779,0.00036528934],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003383741,0.000005878316,0.9962884,0.000005495201,0.000025289788,0.000049494178,0.00016332293,0.0009571187,0.0011997913,0.000012339383,0.00006706309,0.0011919462],"study_design_scores_gemma":[5.3740376e-7,0.000006779677,0.9993191,0.0000014175808,0.000003035586,0.0000101011965,0.00009038018,0.000481674,0.000042278407,0.000007133406,0.000036179023,0.0000013099107],"about_ca_topic_score_codex":0.06547469,"about_ca_topic_score_gemma":0.07247672,"teacher_disagreement_score":0.06547469,"about_ca_system_score_codex":0.0006110304,"about_ca_system_score_gemma":0.0002860735,"threshold_uncertainty_score":0.13018715},"labels":[],"label_agreement":null},{"id":"W2978713238","doi":"10.1126/sciadv.aax5703","title":"Unusual kinematics of the Papatea fault (2016 Kaikōura earthquake) suggest anelastic rupture","year":2019,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Natural Hazards Research Platform; Canada Foundation for Innovation; University of Victoria","keywords":"Seismology; Kinematics; Geology; Fault (geology); Earthquake prediction; Differential (mechanical device); Earthquake rupture; Physics; Engineering; Aerospace engineering","score_opus":0.008492083616202668,"score_gpt":0.2231694990101868,"score_spread":0.21467741539398413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2978713238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908132,0.00011103682,0.0017428383,0.00014033304,0.000019175299,0.000016917833,0.00029326853,0.000090652145,0.0067727156],"genre_scores_gemma":[0.9989536,0.00004026475,0.00048621744,0.0000057238635,0.0000040400623,0.0000037943141,0.00010864674,0.0000043150194,0.00039347232],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999714,0.0000024210233,0.0000019513186,0.000011339626,0.000004855005,0.00000808005],"domain_scores_gemma":[0.9999213,0.000009927941,0.000032241038,0.000011661595,0.000010735247,0.000014214001],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000060935472,0.00022589463,0.00015996241,0.0003339467,0.0003997811,0.00043858166,0.00021261937,0.0003667764,0.00254457],"category_scores_gemma":[0.00032875375,0.00017898546,0.000176507,0.000373461,0.00030184205,0.00034657147,0.0004892041,0.00024544107,0.00038059917],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039076904,0.000120483106,0.77413577,0.0005251045,0.0001964852,0.011784273,0.0021470212,0.015716271,0.09239893,0.005125601,0.0023232244,0.09513606],"study_design_scores_gemma":[0.0000128035745,0.000097879594,0.9778464,0.000024195751,0.000056043416,0.002537476,0.0006777727,0.010824493,0.0024801118,0.0016861125,0.0037363525,0.00002033288],"about_ca_topic_score_codex":0.0018409684,"about_ca_topic_score_gemma":0.003846649,"teacher_disagreement_score":0.00254457,"about_ca_system_score_codex":0.00014168481,"about_ca_system_score_gemma":0.00018078815,"threshold_uncertainty_score":0.008512497},"labels":[],"label_agreement":null},{"id":"W2978851053","doi":"10.1144/sp477.25","title":"Surficial sediment failures due to the 1929 Grand Banks Earthquake, St Pierre Slope","year":2018,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Natural Resources Canada; Dalhousie University","funders":"","keywords":"Geology; Sediment; Seismology; Slope failure; Geotechnical engineering; Geomorphology; Slope stability","score_opus":0.023522287625215906,"score_gpt":0.23602672597937302,"score_spread":0.2125044383541571,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2978851053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991709,0.000019026327,0.000024443709,0.000015190955,0.0000014691452,0.0000031791542,0.00013691865,0.0000047640588,0.0006241206],"genre_scores_gemma":[0.99948466,0.000024061126,0.000030513615,0.000004272993,0.0000023231705,0.0000014359191,0.0001518552,7.4166155e-7,0.0003000921],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987066,0.000010521365,0.0000069277726,0.000018366743,0.000052585056,0.00004096633],"domain_scores_gemma":[0.9996929,0.00003692065,0.00011454442,0.000018340936,0.00007373043,0.000063560095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011176994,0.00021888976,0.00012579047,0.0009364808,0.0005222047,0.00048326643,0.0002101356,0.0002918591,0.0009629394],"category_scores_gemma":[0.00037762118,0.00015220825,0.00016729855,0.0006986567,0.00056096306,0.00012474254,0.00044015393,0.00020328563,0.00022619916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022691283,0.000030786665,0.9769495,0.000018753599,0.000044414388,0.005258835,0.0007573862,0.0023967924,0.0054736654,0.000055630608,0.00064744765,0.008139967],"study_design_scores_gemma":[0.000001107639,0.00002814551,0.9989497,0.0000017985,0.0000035046346,0.00016218866,0.00023508909,0.00029801688,0.00016739486,0.000008040264,0.00014294042,0.0000022599716],"about_ca_topic_score_codex":0.20148379,"about_ca_topic_score_gemma":0.34011635,"teacher_disagreement_score":0.20148379,"about_ca_system_score_codex":0.0015386905,"about_ca_system_score_gemma":0.00059827266,"threshold_uncertainty_score":0.400622},"labels":[],"label_agreement":null},{"id":"W2978992173","doi":"10.5459/bnzsee.42.2.129-141","title":"The Mw 6.7 George Sound earthquake of October 15, 2007","year":2009,"lang":"en","type":"article","venue":"Bulletin of the New Zealand Society for Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Seismology; Aftershock; Seismometer; Subduction; Epicenter; Fault plane; Fault (geology); Earthquake rupture; Moment tensor; North American Plate; Submarine pipeline; Tectonics; Oceanography","score_opus":0.00755470961176018,"score_gpt":0.19415406461975265,"score_spread":0.18659935500799246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2978992173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9731472,0.00032773343,0.0002470542,0.0010153585,0.0002181939,0.000078029334,0.0030072462,0.000077474106,0.021881701],"genre_scores_gemma":[0.97494656,0.0006367439,0.00067501626,0.0005202742,0.0001115159,0.000023938912,0.0058537074,0.000016583755,0.01721563],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998549,0.0000061183023,0.000007191851,0.000016314523,0.00008046334,0.00003501712],"domain_scores_gemma":[0.99972993,0.00001099526,0.00006391543,0.000020218788,0.00008201247,0.00009301937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018171551,0.00019970628,0.00019382614,0.00047741816,0.0005992539,0.00042660537,0.00021098684,0.0005291008,0.001912299],"category_scores_gemma":[0.00061861874,0.0000916185,0.000095608455,0.0004402576,0.00048012397,0.0002155074,0.0008760977,0.00049964193,0.00064741244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047624356,0.00021167348,0.67770773,0.00042087067,0.00020851406,0.005609009,0.008018314,0.001478412,0.03544106,0.0036001604,0.11719304,0.14963506],"study_design_scores_gemma":[0.00000837455,0.00009637986,0.9654142,0.000045194007,0.0000123144055,0.00027842916,0.00068704184,0.00012594015,0.00090548664,0.000102051905,0.032313846,0.000010601235],"about_ca_topic_score_codex":0.07387516,"about_ca_topic_score_gemma":0.24659976,"teacher_disagreement_score":0.07387516,"about_ca_system_score_codex":0.001200719,"about_ca_system_score_gemma":0.0011420426,"threshold_uncertainty_score":0.14689034},"labels":[],"label_agreement":null},{"id":"W2980322620","doi":"10.1130/g46317.1","title":"Nanoscale evidence for temperature-induced transient rheology and postseismic fault healing","year":2019,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Materials Research; Southern California Earthquake Center; McGill University; Utah Science Technology and Research; National Science Foundation","keywords":"Hematite; Materials science; Mineralogy; Amorphous solid; Geology; Composite material; Quartz; Magnetite; Nanoscopic scale; Transmission electron microscopy; Nanotechnology; Crystallography; Metallurgy","score_opus":0.028794834843186387,"score_gpt":0.25877605513408053,"score_spread":0.22998122029089413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980322620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887675,0.00006948083,0.000319907,0.000011631894,0.0000015828135,0.000002171165,0.000064342355,0.000014817426,0.0006392782],"genre_scores_gemma":[0.9996138,0.000011663569,0.00008620685,0.000003170083,7.5155026e-7,0.0000015239931,0.00003604128,0.000002173443,0.0002446403],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999509,0.000002232706,0.0000021374676,0.00001261079,0.000017230233,0.000014786919],"domain_scores_gemma":[0.99987066,0.00001831614,0.00004600226,0.000017132035,0.000031788473,0.000016065733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004669305,0.000053368127,0.00006421701,0.00016394658,0.0001239369,0.00017451902,0.00014655896,0.000145964,0.0012682122],"category_scores_gemma":[0.00018739692,0.00008073903,0.00004922368,0.00008892383,0.00024653025,0.00013066124,0.00015094044,0.0001414997,0.0001117676],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075737924,0.000011757562,0.0124070905,0.000022459022,0.000004419168,0.00013643701,0.000066051354,0.00013889279,0.9854388,0.00009640102,0.000059867423,0.0015419609],"study_design_scores_gemma":[0.000010737292,0.00010465737,0.512642,0.0000065710715,0.000009581097,0.00038189234,0.0003232087,0.0028345953,0.4821593,0.000118027514,0.0014021576,0.000007222322],"about_ca_topic_score_codex":0.0019704818,"about_ca_topic_score_gemma":0.0030825313,"teacher_disagreement_score":0.0019704818,"about_ca_system_score_codex":0.00031007675,"about_ca_system_score_gemma":0.00008566401,"threshold_uncertainty_score":0.004242599},"labels":[],"label_agreement":null},{"id":"W2980364451","doi":"10.1029/2019jb017944","title":"The Effects of Shear Strain, Fabric, and Porosity Evolution on Elastic and Mechanical Properties of Clay‐Rich Fault Gouge","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Stroke Foundation; U.S. Department of Energy; Office of Energy Efficiency and Renewable Energy; National Science Foundation","keywords":"Porosity; Shear (geology); Materials science; Fault gouge; Shearing (physics); Composite material; Elastic modulus; Stiffness; Shear modulus; Shear zone; Shear stress; Geotechnical engineering; Geology; Fault (geology)","score_opus":0.02119352155678692,"score_gpt":0.26884891755047097,"score_spread":0.24765539599368405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980364451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99980646,0.000024118779,0.000066968125,0.0000022491156,5.4920974e-7,0.0000012734472,0.000030621813,0.0000030668764,0.00006457273],"genre_scores_gemma":[0.99981624,0.000014917281,0.00007397365,0.0000020437524,3.043093e-7,0.0000018084896,0.000031855932,0.0000015725369,0.000057233214],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998925,0.000011767815,0.000009480255,0.000024551226,0.000031199022,0.00003043694],"domain_scores_gemma":[0.99970514,0.00007542111,0.00010089255,0.00002032227,0.000045695593,0.000052550335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001998779,0.00022896793,0.00015273527,0.00033410496,0.0001657931,0.00034161634,0.00013007411,0.00016863072,0.0007157288],"category_scores_gemma":[0.00041564312,0.00014420871,0.00010717242,0.00017503682,0.00039153104,0.00019884706,0.00019836475,0.00023140517,0.00006103498],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013989277,0.000017549251,0.0051017916,0.000022969054,0.000010276531,0.000058168403,0.00004926158,0.000586128,0.99304295,0.00003350163,0.000014069332,0.00092338613],"study_design_scores_gemma":[0.00001199252,0.0003627181,0.12511131,0.000008762577,0.000016161588,0.000102886814,0.00023522071,0.006141825,0.867631,0.000043470478,0.0003154982,0.000019210636],"about_ca_topic_score_codex":0.0016267124,"about_ca_topic_score_gemma":0.0022287988,"teacher_disagreement_score":0.0016267124,"about_ca_system_score_codex":0.00023556486,"about_ca_system_score_gemma":0.000108239095,"threshold_uncertainty_score":0.0032345057},"labels":[],"label_agreement":null},{"id":"W2980384556","doi":"10.1029/2019gl084656","title":"Compliant Volcanic Arc and Backarc Crust in Southern Kurile Suggested by Interseismic Geodetic Deformation","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Japan Society for the Promotion of Science London","keywords":"Geology; Lithosphere; Volcano; Volcanic arc; Seismology; Geodetic datum; Crust; Forearc; Rigidity (electromagnetism); Back-arc basin; Subduction; Geodesy; Geophysics; Tectonics","score_opus":0.02326455681671819,"score_gpt":0.25588014383542246,"score_spread":0.23261558701870427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980384556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992199,0.000019637728,0.00042532396,0.0000120168,6.9702713e-7,0.0000014910993,0.000017737233,0.000008339089,0.00029481426],"genre_scores_gemma":[0.99981743,0.000010022406,0.00011874017,0.0000018792487,4.4883646e-7,7.053099e-7,0.000015813494,0.0000012962715,0.00003357718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998913,0.000030178247,0.000011853211,0.000025811001,0.000015232646,0.000025644746],"domain_scores_gemma":[0.99967897,0.000087492226,0.000112795824,0.000036624086,0.000029758592,0.00005430196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033103616,0.00041094277,0.00023772978,0.0011115591,0.0002511978,0.0010806158,0.0003471543,0.0005012937,0.001515028],"category_scores_gemma":[0.001178315,0.0004094431,0.0003246286,0.0004793557,0.0006162881,0.0006177073,0.00086195994,0.00023299565,0.00017787043],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036581443,0.00007215331,0.8753347,0.00006708357,0.0001554034,0.00081893464,0.00044879827,0.08654424,0.024538264,0.0025235373,0.00012390738,0.009007243],"study_design_scores_gemma":[0.000028923136,0.000087310495,0.8154799,0.000023996126,0.000058242087,0.00029298366,0.00049811136,0.1810666,0.0012550555,0.00091602944,0.00025768564,0.000035203837],"about_ca_topic_score_codex":0.0042656856,"about_ca_topic_score_gemma":0.0046774116,"teacher_disagreement_score":0.0042656856,"about_ca_system_score_codex":0.00022404757,"about_ca_system_score_gemma":0.00019517886,"threshold_uncertainty_score":0.008481741},"labels":[],"label_agreement":null},{"id":"W2981202292","doi":"10.1130/abs/2019am-338830","title":"THE P-T-T-D EVOLUTION OF THE MAHABHARAT KLIPPE, EAST-CENTRAL NEPAL: IMPLICATIONS FOR THE OUT-OF-SEQUENCE EVOLUTION OF THE HIMALAYA","year":2019,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Sequence (biology); Geology; Evolutionary biology; Biology; Genetics","score_opus":0.026289725330876704,"score_gpt":0.24178725654993946,"score_spread":0.21549753121906276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981202292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99435127,0.000099338715,0.00013660116,0.00015029195,0.0000042260253,0.0000058653427,0.00045599858,0.0000070321444,0.0047893045],"genre_scores_gemma":[0.9988863,0.000053873224,0.00008368449,0.000021840671,0.0000022328677,0.0000036950275,0.00018706871,0.0000032762769,0.00075809675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999502,0.000010009638,0.000004193965,0.0000138118885,0.0000056598424,0.000016272845],"domain_scores_gemma":[0.9998197,0.000047502042,0.00003504753,0.000009564062,0.000053844116,0.000034335837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007975291,0.00012665355,0.00009747464,0.001063973,0.0008202595,0.00087155215,0.00031908278,0.000304178,0.0041535115],"category_scores_gemma":[0.0006150675,0.00012622867,0.0001122993,0.0013771121,0.0004251737,0.00032234614,0.0005319828,0.00032167597,0.0004509004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006926638,0.00014125052,0.8815241,0.00024099536,0.00017018901,0.004541952,0.013307365,0.003934742,0.039354183,0.005940404,0.0019146255,0.048237607],"study_design_scores_gemma":[0.000010113558,0.00003130002,0.99233353,0.000019375662,0.000020792184,0.00045903499,0.002668231,0.0009938648,0.0006860087,0.00030949837,0.0024583484,0.000009986204],"about_ca_topic_score_codex":0.049192578,"about_ca_topic_score_gemma":0.075817555,"teacher_disagreement_score":0.049192578,"about_ca_system_score_codex":0.0006664254,"about_ca_system_score_gemma":0.00053515914,"threshold_uncertainty_score":0.097812474},"labels":[],"label_agreement":null},{"id":"W2981325006","doi":"10.4095/219970","title":"SAR incidence angles for mapping areas affected by geological hazards, tropical case studies","year":2002,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geologic map; Tropical cyclone; Geography; Cartography; Geologic hazards; Incidence (geometry); Geology; Seismology; Meteorology; Landslide; Mathematics; Geometry","score_opus":0.07952128827054235,"score_gpt":0.29205580514862284,"score_spread":0.2125345168780805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981325006","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8642609,0.0027188351,0.06692506,0.00048553344,0.000108536224,0.0012396309,0.0028094426,0.0002557101,0.061196465],"genre_scores_gemma":[0.89631397,0.0033139207,0.09273662,0.00003722006,0.000051994815,0.00022419592,0.0020641903,0.00006224009,0.005195611],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996159,0.00015692557,0.00003743607,0.000029071422,0.0001307136,0.000029878054],"domain_scores_gemma":[0.9991837,0.00031410152,0.00011000792,0.000089183784,0.0002531994,0.000049678645],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008598501,0.000534936,0.00014746987,0.0016315348,0.00031078438,0.00041412577,0.0002339321,0.00020469731,0.002064915],"category_scores_gemma":[0.0020390898,0.00021040044,0.00018990709,0.0017621819,0.00017638755,0.000359169,0.00033733656,0.00018955016,0.00047109468],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010920768,0.00091170316,0.3878765,0.00096333574,0.00008873459,0.0038575623,0.0026462232,0.04246102,0.051852997,0.0032735504,0.01715392,0.48782235],"study_design_scores_gemma":[0.00017621458,0.0024964863,0.818319,0.0002725792,0.00030761177,0.013947879,0.0058950717,0.04568729,0.054416973,0.0018319705,0.05653359,0.00011528156],"about_ca_topic_score_codex":0.0042001074,"about_ca_topic_score_gemma":0.011318641,"teacher_disagreement_score":0.0042001074,"about_ca_system_score_codex":0.00014679435,"about_ca_system_score_gemma":0.00021186151,"threshold_uncertainty_score":0.008351326},"labels":[],"label_agreement":null},{"id":"W2981426491","doi":"10.4095/215330","title":"Effect of earthquake probability level on loss estimations","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Statistics; Seismology; Geology; Environmental science; Geodesy; Mathematics","score_opus":0.06034783073097329,"score_gpt":0.2920663862291178,"score_spread":0.23171855549814452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981426491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93914074,0.00065435184,0.04456829,0.0008945187,0.00005907966,0.00038205824,0.0015693238,0.0007152653,0.0120163625],"genre_scores_gemma":[0.9914522,0.00011521441,0.0073446007,0.00005976926,0.000010846906,0.00004010415,0.00038822135,0.000032108514,0.0005567435],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9817786,0.01151715,0.000630909,0.0011813592,0.004121501,0.00077050936],"domain_scores_gemma":[0.5971196,0.37198412,0.009842931,0.0072588744,0.012628851,0.0011655375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.023244457,0.0007455475,0.00072078756,0.001928173,0.00045297624,0.0017977426,0.00089305796,0.00086666323,0.0018000621],"category_scores_gemma":[0.1629582,0.0003647046,0.00085094385,0.0016431123,0.00073603424,0.0016156789,0.0012542618,0.0010489009,0.00029462323],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004979653,0.00027976523,0.26366466,0.00022049394,0.00058672496,0.0005339209,0.0005196266,0.63519317,0.0020048977,0.0039579314,0.0020473197,0.08601184],"study_design_scores_gemma":[0.0002230347,0.0036735125,0.32905394,0.00020186762,0.0010235067,0.0006959255,0.0013951721,0.63573873,0.01792019,0.0053138575,0.004500373,0.00025985707],"about_ca_topic_score_codex":0.018155444,"about_ca_topic_score_gemma":0.011172988,"teacher_disagreement_score":0.023244457,"about_ca_system_score_codex":0.0014482464,"about_ca_system_score_gemma":0.0010229674,"threshold_uncertainty_score":0.12292987},"labels":[],"label_agreement":null},{"id":"W2981462418","doi":"10.4095/220906","title":"Residual total magnetic field, 22B/09 - Monts Berry, Quebec","year":2005,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Berry; Residual; Field (mathematics); Geography; Biology; Mathematics; Botany","score_opus":0.02379538202694279,"score_gpt":0.2439451655969471,"score_spread":0.2201497835700043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981462418","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3437835,0.0015468077,0.0025682573,0.0020254545,0.00035690656,0.00088876527,0.40845954,0.0014155899,0.23895516],"genre_scores_gemma":[0.3169299,0.00085486774,0.0026522186,0.00031080184,0.00006780231,0.00020185357,0.07579341,0.0003059219,0.6028831],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99953485,0.000027143531,0.000012906641,0.000089110355,0.00020965486,0.00012638845],"domain_scores_gemma":[0.9987337,0.00007859473,0.0000610983,0.000058062535,0.00091800536,0.00015050813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003683134,0.00075920054,0.0005091546,0.001802087,0.003285957,0.0011752958,0.0015886908,0.0005397031,0.045542624],"category_scores_gemma":[0.0009364273,0.0003239398,0.00032356018,0.0024768857,0.0003621215,0.00068296026,0.00048788803,0.000889999,0.005323846],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016234125,0.00070147,0.29660445,0.00044698713,0.0002582844,0.0014820565,0.001533641,0.005898751,0.007564996,0.0032304046,0.48976976,0.1908858],"study_design_scores_gemma":[0.00016322678,0.0001503013,0.8140419,0.00008102211,0.000046160738,0.00014525237,0.0011449958,0.003883752,0.002571388,0.00022606405,0.17748514,0.00006081972],"about_ca_topic_score_codex":0.99203616,"about_ca_topic_score_gemma":0.9968149,"teacher_disagreement_score":0.045542624,"about_ca_system_score_codex":0.015278551,"about_ca_system_score_gemma":0.015340386,"threshold_uncertainty_score":0.15235525},"labels":[],"label_agreement":null},{"id":"W2981555053","doi":"10.4095/215720","title":"Shaded magnetic first vertical derivative, Sussex, 21 H/12, New Brunswick","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Derivative (finance); Geology; Business","score_opus":0.038382724529091104,"score_gpt":0.24383764971721247,"score_spread":0.20545492518812136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981555053","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.133554,0.0034259872,0.0014876851,0.0021641967,0.00055643317,0.0004622188,0.28072602,0.0011699029,0.57645357],"genre_scores_gemma":[0.06650603,0.0013481069,0.0012991754,0.00015151326,0.00004672301,0.00011412264,0.029776609,0.00029992734,0.9004578],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99973816,0.000014229013,0.000012123363,0.00005932404,0.000087257926,0.00008887581],"domain_scores_gemma":[0.9992823,0.000076743105,0.000047356723,0.00007577932,0.00038235847,0.00013542545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002605901,0.00089170935,0.00038447016,0.0019306394,0.0021734494,0.0011676563,0.0014022953,0.00049172447,0.20267034],"category_scores_gemma":[0.00065082643,0.00043667768,0.00020194046,0.0031076104,0.0003470691,0.0008341765,0.0005748377,0.0012200605,0.031786192],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009234118,0.0003041525,0.054453775,0.00048524397,0.00004424108,0.0014678114,0.0015825151,0.0018040999,0.009096144,0.002659288,0.70648396,0.22069545],"study_design_scores_gemma":[0.00009025502,0.000090411115,0.33931375,0.00011822663,0.000032772572,0.00038279264,0.0016986077,0.000521518,0.0050621117,0.00045069205,0.6521964,0.000042372896],"about_ca_topic_score_codex":0.75302154,"about_ca_topic_score_gemma":0.93945134,"teacher_disagreement_score":0.24697846,"about_ca_system_score_codex":0.0033483657,"about_ca_system_score_gemma":0.0057384,"threshold_uncertainty_score":0.67799985},"labels":[],"label_agreement":null},{"id":"W2981569833","doi":"10.4095/225934","title":"Estimated seismic design values for Canadian missions abroad","year":2008,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Computer science; Seismology","score_opus":0.10351768310935594,"score_gpt":0.3057098720808488,"score_spread":0.20219218897149288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981569833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.71288455,0.0014893573,0.022693397,0.0004193672,0.00005156802,0.00025389832,0.09598835,0.0006375964,0.16558191],"genre_scores_gemma":[0.8593941,0.0017324748,0.013386221,0.00007519638,0.000015403059,0.00021305935,0.08295579,0.00018216042,0.04204567],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989299,0.000059742182,0.00003209317,0.000085985106,0.00065322284,0.00023885755],"domain_scores_gemma":[0.9984499,0.000103190396,0.00014586178,0.00008014005,0.0011155324,0.000105466956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052000995,0.0008602545,0.000259967,0.0031959037,0.0010633938,0.00063766056,0.00058225315,0.00017310058,0.005602051],"category_scores_gemma":[0.0022152457,0.00030456306,0.00053762086,0.0035282131,0.00026888246,0.00030735484,0.0006253523,0.00045042465,0.0012697019],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039277392,0.0000849833,0.4302279,0.0006227297,0.00024244841,0.0006744152,0.0017724261,0.14202093,0.0058836197,0.013217732,0.08223818,0.32262176],"study_design_scores_gemma":[0.00003968819,0.00010941522,0.7997619,0.00013887964,0.00010675868,0.000436217,0.0021218979,0.022622522,0.006574819,0.0012237416,0.16668941,0.000174728],"about_ca_topic_score_codex":0.92803556,"about_ca_topic_score_gemma":0.95442754,"teacher_disagreement_score":0.07196444,"about_ca_system_score_codex":0.018115126,"about_ca_system_score_gemma":0.015265236,"threshold_uncertainty_score":0.14477646},"labels":[],"label_agreement":null},{"id":"W2981618955","doi":"10.4095/299138","title":"Focal depth of earthquakes of the St. Lawrence Valley based on crustal phases recorded within 100 km epicentral distance","year":2016,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Geodesy","score_opus":0.03903515776550335,"score_gpt":0.26045818394564063,"score_spread":0.2214230261801373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981618955","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99021155,0.00013152392,0.0003852463,0.00001468894,0.0000022125923,0.000019424715,0.0062512,0.000052935968,0.0029311192],"genre_scores_gemma":[0.9941981,0.0001004897,0.00065452256,0.0000044382045,0.0000019153322,0.000011424909,0.004226919,0.000008963496,0.00079339085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999884,0.0000082022725,0.000011760321,0.00002680094,0.000035051922,0.000034154044],"domain_scores_gemma":[0.99963975,0.000047558216,0.00011011272,0.000015940264,0.00013771509,0.0000489206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015876893,0.00032048675,0.00016902045,0.0019256676,0.0001915489,0.00052202103,0.00026446997,0.00012438858,0.0018982782],"category_scores_gemma":[0.0008638144,0.00013078265,0.00018247393,0.0023175208,0.000118419055,0.00018686362,0.00036509125,0.00012069831,0.00025187555],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000920396,0.000017197319,0.9775587,0.000061858205,0.00007749528,0.00012247633,0.00024194064,0.0054861302,0.0026696727,0.000152805,0.000833009,0.01268666],"study_design_scores_gemma":[0.0000051560414,0.000012820327,0.9969331,0.000007876463,0.000011097026,0.0000453378,0.0001380366,0.0018619148,0.00035638438,0.000015344815,0.0006073702,0.0000054755697],"about_ca_topic_score_codex":0.4719733,"about_ca_topic_score_gemma":0.69124275,"teacher_disagreement_score":0.5280267,"about_ca_system_score_codex":0.0013322225,"about_ca_system_score_gemma":0.0007699508,"threshold_uncertainty_score":0.93845224},"labels":[],"label_agreement":null},{"id":"W2981631412","doi":"10.1029/2019jb017875","title":"The Significance of Tomographic Edge Zones for Large Earthquakes in Taiwan","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"National Natural Science Foundation of China-Yunnan Joint Fund; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Tectonics; Seismotectonics; Seismic tomography; Crust; Geophysics; Mantle (geology)","score_opus":0.03307738090649209,"score_gpt":0.3163455562020572,"score_spread":0.2832681752955651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981631412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994006,0.000035975394,0.00017237356,0.0000135126365,0.0000011095647,0.0000018734792,0.00010108908,0.000013309653,0.0002602058],"genre_scores_gemma":[0.9997582,0.000011172646,0.000072827715,0.0000024145518,0.0000015233094,8.995861e-7,0.00012033316,0.0000016753864,0.00003090538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998877,0.000013449896,0.0000122364745,0.000035165052,0.000018183135,0.000033170923],"domain_scores_gemma":[0.99928916,0.00010971149,0.0003274487,0.0000643858,0.000110450244,0.00009880256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021974587,0.00018466038,0.00014864815,0.0015047817,0.00022251181,0.00055943493,0.00022653672,0.00025978588,0.0007878997],"category_scores_gemma":[0.0010376805,0.00016373052,0.00019645557,0.0010846737,0.00024170177,0.00031872344,0.0006037612,0.00018363954,0.00014408074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000067087705,0.00001739148,0.9864624,0.000014224013,0.000019375526,0.00020487161,0.00016762741,0.001062376,0.005372714,0.0000527849,0.00008614569,0.0064730155],"study_design_scores_gemma":[0.000003421336,0.000011670883,0.99621767,0.0000048259526,0.000011622945,0.000116557625,0.00019890678,0.0028420018,0.00041728132,0.000035371308,0.00013533795,0.0000053117888],"about_ca_topic_score_codex":0.0066462546,"about_ca_topic_score_gemma":0.008992263,"teacher_disagreement_score":0.0066462546,"about_ca_system_score_codex":0.00018387275,"about_ca_system_score_gemma":0.0002012642,"threshold_uncertainty_score":0.013215125},"labels":[],"label_agreement":null},{"id":"W2981691443","doi":"10.1016/j.epsl.2019.115882","title":"Plate boundary localization, slip-rates and rupture segmentation of the Queen Charlotte Fault based on submarine tectonic geomorphology","year":2019,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada; National Oceanic and Atmospheric Administration; Alaska Department of Fish and Game; King Abdullah University of Science and Technology; U.S. Geological Survey; Massachusetts Department of Fish and Game","keywords":"Geology; Seismology; Slip (aerodynamics); Earthquake rupture; Plate tectonics; Fault trace; North American Plate; Seafloor spreading; Tectonics; Forearc; Fault (geology); Pacific Plate; Bathymetry; Submarine pipeline; Strike-slip tectonics; Geodesy; Subduction; Paleontology; Oceanography","score_opus":0.0058865302035598,"score_gpt":0.18874471241031632,"score_spread":0.1828581822067565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981691443","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887127,0.000023485294,0.00033927508,0.000013230879,0.0000015093553,0.0000030705573,0.00020005628,0.000020730798,0.00052740565],"genre_scores_gemma":[0.9988337,0.00000871648,0.00037872256,0.0000025489787,8.532174e-7,0.0000015737986,0.0004214257,0.000009800334,0.00034269298],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999882,0.000019074763,0.000007614396,0.000042275402,0.000016593822,0.000032430777],"domain_scores_gemma":[0.99896204,0.00034100807,0.0001858176,0.000056269844,0.0002581173,0.00019681393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003631077,0.00021140407,0.0002761258,0.0022851045,0.00043977314,0.0011148247,0.0002766317,0.0004849152,0.0020191849],"category_scores_gemma":[0.0013844854,0.00018715103,0.00017485234,0.0005776773,0.0003217925,0.00031862714,0.00034922562,0.00021070719,0.00048978685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0030163452,0.00015188941,0.8826911,0.000049637776,0.00007147362,0.00057662296,0.00080305676,0.029371383,0.038784854,0.00067854143,0.001212161,0.042592827],"study_design_scores_gemma":[0.000017735141,0.000036801444,0.9267382,0.000016146289,0.000015139955,0.00006068696,0.00026123412,0.070625074,0.0019241879,0.00011775519,0.00017134243,0.000015678008],"about_ca_topic_score_codex":0.06283576,"about_ca_topic_score_gemma":0.10442507,"teacher_disagreement_score":0.93716425,"about_ca_system_score_codex":0.0008022453,"about_ca_system_score_gemma":0.00064371654,"threshold_uncertainty_score":0.12494004},"labels":[],"label_agreement":null},{"id":"W2981771265","doi":"10.4095/215721","title":"Shaded magnetic first vertical derivative, Codys, 21 H/13, New Brunswick","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Derivative (finance); Geology; Geodesy; Geometry; Physics; Mathematics; Economics","score_opus":0.0361753829507557,"score_gpt":0.24345847041651994,"score_spread":0.20728308746576424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981771265","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12856185,0.0016293278,0.0039813826,0.0017730813,0.00040955844,0.0005250453,0.44060883,0.002709506,0.41980153],"genre_scores_gemma":[0.14357659,0.0012363949,0.0051082266,0.00018203653,0.00008075966,0.0002167288,0.10369137,0.000936518,0.7449714],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99979526,0.000013167104,0.000008603132,0.00004545045,0.00008572301,0.000051883373],"domain_scores_gemma":[0.9992586,0.00008295393,0.00004880681,0.00010797071,0.00038573978,0.000115984665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032274527,0.0007862546,0.0003529598,0.001766474,0.0013479667,0.0009255008,0.0013151485,0.00038539307,0.09414681],"category_scores_gemma":[0.0007828593,0.00038874353,0.00015736363,0.0027068537,0.00028790155,0.00065378187,0.00046433808,0.000911362,0.016702332],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000948987,0.0003113569,0.051563855,0.00029126965,0.0000406519,0.0006931681,0.00077451405,0.0041619586,0.01111914,0.0032171968,0.72077537,0.20610254],"study_design_scores_gemma":[0.00019238988,0.00009368101,0.37107047,0.00009639031,0.000044531407,0.00026364275,0.00085655646,0.0035064647,0.012552251,0.0011570825,0.6101112,0.00005544116],"about_ca_topic_score_codex":0.70380205,"about_ca_topic_score_gemma":0.8873077,"teacher_disagreement_score":0.29619795,"about_ca_system_score_codex":0.0029604265,"about_ca_system_score_gemma":0.004633721,"threshold_uncertainty_score":0.5958846},"labels":[],"label_agreement":null},{"id":"W2981789785","doi":"10.4095/220907","title":"Residual total magnetic field, 22B/10 - Rivière Bonjour, Quebec","year":2005,"lang":"fr","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Residual; Field (mathematics); Geography; Mathematics","score_opus":0.029692003753573223,"score_gpt":0.23464293996805782,"score_spread":0.2049509362144846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981789785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.44714737,0.0030395025,0.0034837087,0.0016643708,0.0004660144,0.0008010685,0.35051367,0.0014959986,0.19138826],"genre_scores_gemma":[0.44912422,0.0013815244,0.0033283453,0.00027299326,0.000095739124,0.00023443539,0.069027305,0.00030161272,0.47623387],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99954456,0.0000325072,0.000014528181,0.00008446365,0.00019488292,0.00012891469],"domain_scores_gemma":[0.99901664,0.00007958096,0.000065785374,0.000046614445,0.0006700667,0.00012144557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003654968,0.00094780687,0.00067203894,0.0018058633,0.0026878538,0.0011509845,0.0015551362,0.00056661584,0.034151096],"category_scores_gemma":[0.0009665595,0.0003182428,0.00041271726,0.002381852,0.00038291395,0.00065133715,0.000490823,0.0009447828,0.0036344926],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001944499,0.0007273186,0.369297,0.00072367303,0.00054460653,0.0019801552,0.0015279492,0.009859421,0.008916364,0.0044496893,0.3834574,0.21657193],"study_design_scores_gemma":[0.00020682985,0.0001472573,0.8569644,0.000097908895,0.000057315836,0.00016443116,0.00077849766,0.0039659007,0.0023902277,0.00019971128,0.13496998,0.00005744657],"about_ca_topic_score_codex":0.9912213,"about_ca_topic_score_gemma":0.9950997,"teacher_disagreement_score":0.034151096,"about_ca_system_score_codex":0.016790496,"about_ca_system_score_gemma":0.015937615,"threshold_uncertainty_score":0.121824145},"labels":[],"label_agreement":null},{"id":"W2981897677","doi":"10.4095/211402","title":"Focal mechanisms for eastern Canadian earthquakes: 1 July-31 December 1998","year":2000,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Focal mechanism; Physical geography; Geography; Tectonics","score_opus":0.0399841200056523,"score_gpt":0.25126261202895184,"score_spread":0.21127849202329954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981897677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6200092,0.0036353818,0.0009402556,0.0023901542,0.00023037492,0.00044017629,0.31317824,0.00037053286,0.05880567],"genre_scores_gemma":[0.85017735,0.0033282945,0.00091121893,0.0002839329,0.00009025723,0.00015951149,0.08827163,0.00006497959,0.056712788],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994293,0.000008891874,0.000021977083,0.000034394387,0.00026142687,0.00024404594],"domain_scores_gemma":[0.99681574,0.0000631732,0.0003646972,0.00006670956,0.0023831336,0.00030654488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045387505,0.0007145794,0.0003076665,0.0046653375,0.00283252,0.0009628879,0.0013832821,0.0008292007,0.008856969],"category_scores_gemma":[0.001962317,0.00029964006,0.0003821877,0.0041877464,0.0002870735,0.0005419842,0.0013478005,0.00050396065,0.0012309767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056564267,0.00013823873,0.74160033,0.0005079608,0.00019379487,0.00065789104,0.0019363869,0.0017181158,0.0014338779,0.0015713045,0.16683969,0.08283681],"study_design_scores_gemma":[0.000013414166,0.000011379873,0.98681915,0.000042729116,0.000032207096,0.000075546304,0.000719471,0.000274684,0.00028189548,0.000044623488,0.011672422,0.000012485372],"about_ca_topic_score_codex":0.9882129,"about_ca_topic_score_gemma":0.99730057,"teacher_disagreement_score":0.013325624,"about_ca_system_score_codex":0.013325624,"about_ca_system_score_gemma":0.018715663,"threshold_uncertainty_score":0.096684635},"labels":[],"label_agreement":null},{"id":"W2981939260","doi":"10.4095/299244","title":"Fifth generation seismic hazard model for Canada: crustal, in-slab, and interface hazard values for southwestern Canada","year":2016,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Slab; Geology; Seismology; Hazard; Seismic hazard; Interface (matter); Geography; Geophysics; Meteorology","score_opus":0.05062978163926629,"score_gpt":0.2559744170818811,"score_spread":0.20534463544261483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981939260","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36730692,0.0014031122,0.14151458,0.0029671441,0.00023104042,0.0010535301,0.2811915,0.0031000075,0.20123222],"genre_scores_gemma":[0.79609907,0.0012156506,0.0423926,0.0002543421,0.00003186007,0.00043825462,0.099372536,0.00035679867,0.059838932],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996482,0.00003456062,0.000013147075,0.000037809397,0.00015438235,0.00011181005],"domain_scores_gemma":[0.99891984,0.00008864956,0.000050629882,0.000043120377,0.0008319478,0.00006592728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054856576,0.0007618295,0.00036759235,0.0015093999,0.0011336348,0.0012278722,0.002234962,0.00057167467,0.009586928],"category_scores_gemma":[0.0019308652,0.00039138176,0.00071514555,0.0021689062,0.00032045803,0.0005461263,0.00054917444,0.0007156708,0.0012842739],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013278004,0.00005848903,0.030398164,0.000088755616,0.00007305985,0.0001675973,0.0001714015,0.86851305,0.0005666851,0.021090308,0.052662805,0.026076928],"study_design_scores_gemma":[0.000053562148,0.000022297767,0.020740455,0.00007744872,0.000043311014,0.00006956662,0.0002717792,0.9372219,0.00040447415,0.0051946086,0.035837077,0.000063557745],"about_ca_topic_score_codex":0.9831404,"about_ca_topic_score_gemma":0.9789916,"teacher_disagreement_score":0.025630057,"about_ca_system_score_codex":0.025630057,"about_ca_system_score_gemma":0.029034533,"threshold_uncertainty_score":0.18595994},"labels":[],"label_agreement":null},{"id":"W2981952032","doi":"10.4095/212742","title":"Focal mechanisms for eastern Canadian earthquakes of 1999","year":2001,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Focal mechanism; Geography; History; Induced seismicity","score_opus":0.04769945481802505,"score_gpt":0.2536683957855019,"score_spread":0.2059689409674768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981952032","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92419976,0.0013372677,0.00091972295,0.00034217097,0.000020346395,0.00015703781,0.053083014,0.000112841175,0.019827839],"genre_scores_gemma":[0.9708435,0.0010400199,0.0011376989,0.000039904473,0.000008598664,0.000047813908,0.02000722,0.000021226806,0.0068541295],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99952734,0.000010958469,0.000027617561,0.00005345014,0.00019966469,0.00018093902],"domain_scores_gemma":[0.99803954,0.000067808025,0.0003400326,0.00009062984,0.0013028779,0.00015906214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042539058,0.00053341594,0.0002885883,0.004669624,0.0019485683,0.0007616719,0.0010595038,0.0003070728,0.004459065],"category_scores_gemma":[0.002442082,0.0002558444,0.00034157906,0.004216975,0.00033163727,0.00041358,0.00092409726,0.0002001409,0.000374178],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022505118,0.00005352397,0.90562063,0.00025573777,0.00015361332,0.0006887189,0.0017188992,0.0018159247,0.0034490952,0.002761975,0.016220707,0.06703604],"study_design_scores_gemma":[0.0000043348896,0.000007037985,0.9938114,0.000013499889,0.0000274787,0.00012754438,0.000507031,0.0004234323,0.00047618896,0.0000852606,0.0045033405,0.000013432647],"about_ca_topic_score_codex":0.97208786,"about_ca_topic_score_gemma":0.9895558,"teacher_disagreement_score":0.02791214,"about_ca_system_score_codex":0.012967956,"about_ca_system_score_gemma":0.012621948,"threshold_uncertainty_score":0.09408957},"labels":[],"label_agreement":null},{"id":"W2981968645","doi":"10.1785/0220190202","title":"The Canadian National Seismograph Network: Upgrade and Status","year":2019,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismometer; Upgrade; Broadband; Instrumentation (computer programming); Seismology; Telecommunications; Geography; Computer science; Engineering; Environmental science; Geology","score_opus":0.05550515507443374,"score_gpt":0.2935098830420201,"score_spread":0.23800472796758634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981968645","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.030279446,0.01967743,0.00860518,0.043950908,0.0049372856,0.0022110008,0.5258351,0.008439022,0.35606453],"genre_scores_gemma":[0.15677297,0.022052823,0.026824242,0.0060481043,0.0014208927,0.0009965112,0.57760704,0.001607103,0.20667034],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9908279,0.00038745906,0.00033704948,0.000551066,0.0064033987,0.0014930365],"domain_scores_gemma":[0.94493866,0.0006000225,0.0007974447,0.0015097403,0.04714905,0.0050051664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009383747,0.0011991468,0.00067312474,0.011910004,0.0041371826,0.0046846876,0.0047519966,0.0012933366,0.029909732],"category_scores_gemma":[0.0177179,0.0006635038,0.0005210561,0.016537208,0.0014779648,0.0028344374,0.0033065544,0.0016465349,0.011007838],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019487152,0.00005457903,0.017186886,0.0004426029,0.000035519046,0.00007102018,0.0002098779,0.00061055523,0.00040676116,0.0067338487,0.80593854,0.16811483],"study_design_scores_gemma":[0.000034198754,0.000017326605,0.044552814,0.00026156945,0.0000273244,0.000055824497,0.00016864903,0.0007982999,0.0003718006,0.00037507596,0.95329535,0.000041823896],"about_ca_topic_score_codex":0.9853424,"about_ca_topic_score_gemma":0.97704077,"teacher_disagreement_score":0.94878423,"about_ca_system_score_codex":0.05121576,"about_ca_system_score_gemma":0.19067526,"threshold_uncertainty_score":0.37159806},"labels":[],"label_agreement":null},{"id":"W2982032143","doi":"10.4095/298808","title":"Photographic record of the tsunami impacts on western Haida Gwaii following the Mw 7.8 Haida Gwaii earthquake on October 28, 2012","year":2016,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Archaeology; Seismology; History","score_opus":0.03251641062258073,"score_gpt":0.2570796931582911,"score_spread":0.22456328253571037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982032143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92719173,0.00048277713,0.00024983348,0.0001838308,0.00006391453,0.00017099945,0.021007605,0.00007845608,0.050570853],"genre_scores_gemma":[0.94785506,0.0014480302,0.0015936325,0.000084469575,0.000050718518,0.00010136775,0.020523472,0.000026978898,0.028316306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999347,0.0000035060937,0.000004056963,0.000012193515,0.000030627933,0.000014952736],"domain_scores_gemma":[0.9996747,0.000019166879,0.0000716316,0.000025085561,0.00014802805,0.00006148616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000076829245,0.00022886689,0.00013502933,0.0019986045,0.0007897452,0.00033166163,0.00032035323,0.0002408049,0.0046375343],"category_scores_gemma":[0.0002715572,0.00019874207,0.000079477235,0.002679929,0.0002927693,0.00020900281,0.00044916084,0.0004117994,0.0011527021],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032331375,0.00014259906,0.78492695,0.0007415099,0.000085615146,0.005220825,0.018620366,0.0009086504,0.035726972,0.00044919038,0.05550194,0.097352035],"study_design_scores_gemma":[0.000001204385,0.000011007483,0.9908202,0.0000269657,0.0000047735393,0.00017032644,0.0019129573,0.000046488294,0.0002525998,0.0000047599606,0.006744709,0.000003971217],"about_ca_topic_score_codex":0.33921027,"about_ca_topic_score_gemma":0.7758389,"teacher_disagreement_score":0.6607897,"about_ca_system_score_codex":0.0009122082,"about_ca_system_score_gemma":0.00088333077,"threshold_uncertainty_score":0.67447174},"labels":[],"label_agreement":null},{"id":"W2982037774","doi":"10.4095/215329","title":"Probabilities of significant earthquake shaking in communities across British Columbia: implications for emergency management","year":2004,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Emergency management; Seismology; Geography; Forensic engineering; Environmental science; Geology; Engineering; Political science; Law","score_opus":0.06455875610228987,"score_gpt":0.2970773616005329,"score_spread":0.23251860549824302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982037774","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993584,0.00024888266,0.00020643447,0.0008686092,0.0000050615126,0.000033323508,0.0013736566,0.000014682836,0.003665352],"genre_scores_gemma":[0.99868137,0.00020994943,0.000095724376,0.000031231655,0.0000029693804,0.000009009035,0.0003491772,0.0000029274956,0.00061760726],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993679,0.00015501391,0.000045068835,0.00008384206,0.00015550017,0.00019276916],"domain_scores_gemma":[0.9955994,0.001504499,0.0008500172,0.00013071338,0.0011366283,0.0007787289],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005712601,0.00023541713,0.00019803441,0.0017720043,0.0010136304,0.0016030952,0.0006920864,0.00045178542,0.003622916],"category_scores_gemma":[0.0076633506,0.0002744939,0.00022807918,0.0026535504,0.0006789445,0.000550608,0.0010000141,0.0006673348,0.00018381752],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011371741,0.000040365856,0.9755436,0.000038426522,0.00006334997,0.0003944248,0.0004902796,0.0074698743,0.00009508262,0.00040454938,0.0020478154,0.013298513],"study_design_scores_gemma":[0.000010489546,0.000025059178,0.9822667,0.000031412073,0.00002518592,0.00014101483,0.0049313027,0.011145617,0.000047507507,0.0006459649,0.0007130664,0.000016605969],"about_ca_topic_score_codex":0.92134243,"about_ca_topic_score_gemma":0.9513468,"teacher_disagreement_score":0.07865757,"about_ca_system_score_codex":0.00861778,"about_ca_system_score_gemma":0.00558348,"threshold_uncertainty_score":0.15824157},"labels":[],"label_agreement":null},{"id":"W2982117124","doi":"10.4095/299098","title":"A comparison of seismicity to the crustal deformation predicted by a glacial isostatic adjustment model in northern Canada and western Greenland","year":2016,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Post-glacial rebound; Geology; Induced seismicity; Glacial period; Deformation (meteorology); Seismology; Geomorphology; Oceanography","score_opus":0.025126407756691886,"score_gpt":0.25389692365902283,"score_spread":0.22877051590233094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982117124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99505013,0.00012594179,0.0003418215,0.0001156848,0.0000073248134,0.000015619667,0.0017781637,0.00007433712,0.0024910448],"genre_scores_gemma":[0.9957211,0.00012537994,0.00053630373,0.000028905919,0.0000015460726,0.0000073762026,0.002527487,0.000023281202,0.0010287034],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99979645,0.000020672218,0.000010270927,0.000058999623,0.00004246772,0.00007118403],"domain_scores_gemma":[0.9996178,0.00003759342,0.000025989786,0.000018718814,0.0002101453,0.000089629066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004005498,0.00058841245,0.00032004522,0.00085454545,0.0010327337,0.0013216076,0.0009622621,0.00038857938,0.001360897],"category_scores_gemma":[0.0010694049,0.00025094693,0.00049738603,0.0015390929,0.00049691263,0.00030116254,0.0004002025,0.00033491242,0.00021535068],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007648076,0.00014447191,0.51095563,0.00010526324,0.00034109634,0.0005852117,0.00064145384,0.44796,0.0038998548,0.001692317,0.0044526234,0.028457299],"study_design_scores_gemma":[0.00016943557,0.00006467719,0.6319354,0.00006805211,0.00010952172,0.00008152433,0.0014075594,0.36054605,0.0012506099,0.00037735928,0.0038955545,0.000094228686],"about_ca_topic_score_codex":0.99476457,"about_ca_topic_score_gemma":0.9946219,"teacher_disagreement_score":0.020057663,"about_ca_system_score_codex":0.020057663,"about_ca_system_score_gemma":0.018288683,"threshold_uncertainty_score":0.14552921},"labels":[],"label_agreement":null},{"id":"W2982160834","doi":"10.4095/220622","title":"Effects of the 26 December 2004 Indian Ocean tsunami in the Republic of Seychelles: Report of the Canada-UNESCO Indian Ocean Tsunami Expedition, 19 January - 5 February 2005","year":2005,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Indian ocean; Geography; Ancient history; Oceanography; Geology; History","score_opus":0.010548087616752536,"score_gpt":0.2196013893543975,"score_spread":0.20905330173764497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982160834","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9587515,0.0008814688,0.000076246986,0.0010097935,0.00012105844,0.000073993484,0.023588886,0.000040033457,0.015457069],"genre_scores_gemma":[0.96674925,0.0021820231,0.00024092174,0.0002808228,0.000043238164,0.00004001085,0.019054133,0.000026359421,0.011383285],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994266,0.000082107224,0.000055617013,0.00003137789,0.0001506423,0.00025365688],"domain_scores_gemma":[0.99893075,0.000065672415,0.00025381817,0.000040762738,0.00054613693,0.00016293142],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000447431,0.0005180143,0.0003810679,0.0015366904,0.0008969141,0.0009881961,0.0005894953,0.0005193935,0.002633135],"category_scores_gemma":[0.0014552431,0.00021192031,0.00039018109,0.0020022783,0.00031858822,0.00040565495,0.0013789029,0.00049796974,0.00052012946],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015012583,0.00033747163,0.9126516,0.0004013993,0.00041074777,0.003757517,0.0026349125,0.005209699,0.0027373356,0.0004135755,0.035896394,0.034048002],"study_design_scores_gemma":[0.000010120266,0.00004448537,0.99143314,0.000057964164,0.000049396775,0.00013165038,0.0017132484,0.00016120379,0.00039285858,0.000021457277,0.0059721475,0.000012320163],"about_ca_topic_score_codex":0.7654944,"about_ca_topic_score_gemma":0.8905447,"teacher_disagreement_score":0.2345056,"about_ca_system_score_codex":0.004432976,"about_ca_system_score_gemma":0.0053027524,"threshold_uncertainty_score":0.47177327},"labels":[],"label_agreement":null},{"id":"W2982162889","doi":"10.4095/296266","title":"Regional earthquake hazards","year":2015,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Geography","score_opus":0.08112009043869316,"score_gpt":0.2809242897905466,"score_spread":0.19980419935185345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982162889","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.034642525,0.0036995176,0.001606925,0.00355997,0.0018521505,0.0005685535,0.7050978,0.0012326293,0.24773982],"genre_scores_gemma":[0.109515704,0.006830826,0.0032367918,0.0006817325,0.0005759424,0.0008089082,0.53099567,0.0003662631,0.34698814],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99930835,0.000059096594,0.000040728708,0.000070883456,0.00033805385,0.0001828533],"domain_scores_gemma":[0.99904627,0.00005597117,0.00009328612,0.00009185913,0.000559379,0.00015321212],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006400537,0.00093516614,0.0005037774,0.0018765803,0.0004850203,0.0011475157,0.00084605603,0.0008043775,0.019396316],"category_scores_gemma":[0.0017261665,0.0003745024,0.00053842063,0.0023773354,0.00015205608,0.0007437961,0.0013703561,0.0008467457,0.015896631],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027876414,0.00012362796,0.015426734,0.00026444608,0.0000492032,0.00013360818,0.00013643828,0.0017523592,0.00070837035,0.003598309,0.9342099,0.043318275],"study_design_scores_gemma":[0.00007818485,0.00011180596,0.23395737,0.00016484564,0.00006174782,0.00021223802,0.00038741776,0.0015043537,0.0022837678,0.0007015029,0.7605058,0.000031054973],"about_ca_topic_score_codex":0.13015758,"about_ca_topic_score_gemma":0.13350624,"teacher_disagreement_score":0.13015758,"about_ca_system_score_codex":0.0019936382,"about_ca_system_score_gemma":0.008872726,"threshold_uncertainty_score":0.25879997},"labels":[],"label_agreement":null},{"id":"W2982175182","doi":"10.4095/224164","title":"Significant Canadian earthquakes 1600-2006","year":2007,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; History; Geography","score_opus":0.043173992092773755,"score_gpt":0.25378475774843207,"score_spread":0.2106107656556583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982175182","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010480433,0.0004309031,0.00013550198,0.0002836371,0.00010076674,0.0001472363,0.9417106,0.00019581031,0.04651513],"genre_scores_gemma":[0.031861756,0.0025516474,0.0012896907,0.0001451475,0.0000892123,0.00016417513,0.88835704,0.0001254508,0.075415954],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.999153,0.000010487285,0.00004065284,0.000048552043,0.000588772,0.00015857327],"domain_scores_gemma":[0.9968977,0.00004612116,0.00019709734,0.000069410264,0.0024381916,0.00035137674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003518048,0.0012949827,0.00039401313,0.0066730673,0.002487579,0.0012707888,0.00090459804,0.00031495793,0.048056126],"category_scores_gemma":[0.0023662252,0.00037289088,0.0004029171,0.011627764,0.00017319534,0.00049113354,0.0009997007,0.0005374613,0.0096184015],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000121846424,0.000048791702,0.025418557,0.00064524164,0.000031171316,0.00019290867,0.00054878916,0.00032409857,0.00034924404,0.0015055836,0.92014354,0.05067021],"study_design_scores_gemma":[0.000032727465,0.000026831472,0.36418113,0.00029573173,0.000033758002,0.00016882687,0.0006617194,0.00023301743,0.0004927069,0.00016422418,0.6336603,0.000049009657],"about_ca_topic_score_codex":0.9845585,"about_ca_topic_score_gemma":0.9932682,"teacher_disagreement_score":0.048056126,"about_ca_system_score_codex":0.013345909,"about_ca_system_score_gemma":0.038599674,"threshold_uncertainty_score":0.16076374},"labels":[],"label_agreement":null},{"id":"W2982180467","doi":"10.4095/288018","title":"Focal mechanisms and depths of aftershocks of the 2010 Haiti earthquake","year":2011,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Aftershock; Seismology; Geology; Focal mechanism; Tectonics","score_opus":0.039235624579078344,"score_gpt":0.22219012442664218,"score_spread":0.18295449984756385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982180467","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997855,0.00016029993,0.00023192943,0.00003102971,0.0000020560726,0.00000932867,0.00013665423,0.000014013958,0.0015596426],"genre_scores_gemma":[0.9994795,0.000099809615,0.00011356494,0.0000042160304,0.000002945541,0.000002776617,0.00012316747,0.0000019669533,0.00017206835],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999318,0.000005240061,0.0000046795617,0.000013231228,0.00001302406,0.00003212453],"domain_scores_gemma":[0.99974185,0.000027057084,0.00011456684,0.00001399989,0.00006173343,0.000040776154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001756521,0.0003897491,0.00020939556,0.0009960865,0.00030689838,0.00045246724,0.00026909917,0.00035002572,0.0011227519],"category_scores_gemma":[0.0006593368,0.0002667852,0.00022820816,0.00049213425,0.00026433586,0.00045867765,0.0005361622,0.00028532936,0.0002115787],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006288225,0.0001542597,0.8588296,0.00014266813,0.0001717758,0.0013915387,0.0018383601,0.0061315293,0.06619065,0.0010591235,0.0006546781,0.06280698],"study_design_scores_gemma":[0.00000814631,0.00006445513,0.9950814,0.000009343355,0.00003434949,0.0002170466,0.00034379348,0.0019371554,0.0019543672,0.0000722253,0.00026758367,0.000010092445],"about_ca_topic_score_codex":0.020218391,"about_ca_topic_score_gemma":0.030824557,"teacher_disagreement_score":0.020218391,"about_ca_system_score_codex":0.0005385667,"about_ca_system_score_gemma":0.00027267562,"threshold_uncertainty_score":0.040201426},"labels":[],"label_agreement":null},{"id":"W2982203991","doi":"10.4095/304228","title":"Earthquakes of the St. Lawrence Valley between Montreal and Québec: focal depth determination from Regional Depth Phases for the magnitude 2.8 and larger earthquakes for the time period 1980-2014","year":2017,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Magnitude (astronomy); Period (music); Seismology; Geology; History; Climatology; Geography; Physics; Astronomy","score_opus":0.04447878320042015,"score_gpt":0.2746926467498636,"score_spread":0.23021386354944345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982203991","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02045596,0.000106903644,0.0001940564,0.00017499796,0.000030498784,0.000117472504,0.9656016,0.0002025966,0.013115864],"genre_scores_gemma":[0.07983529,0.000503499,0.00096838485,0.00006872501,0.000040620325,0.00023655528,0.87815183,0.00018563683,0.040009398],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9996371,0.0000104263845,0.000023205832,0.00003791568,0.00019927323,0.00009200914],"domain_scores_gemma":[0.9970727,0.00015227424,0.00030311174,0.00010797778,0.002103533,0.00026041377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029135257,0.00054635305,0.00031626018,0.0032863705,0.0008357979,0.00077830214,0.0010647831,0.00029339577,0.037399415],"category_scores_gemma":[0.0022451892,0.0003191394,0.00024632702,0.0066319713,0.00014354537,0.0005018177,0.00053096784,0.000309425,0.0061156475],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012306559,0.00005990569,0.19011216,0.00046231467,0.00007401621,0.00020703537,0.0005572162,0.0011265838,0.00054657884,0.00071782054,0.7639263,0.04208696],"study_design_scores_gemma":[0.00005023552,0.000018011653,0.89606804,0.00017153002,0.000021819142,0.000070806695,0.00060473307,0.00074931985,0.00051475456,0.000057013247,0.101642534,0.0000313509],"about_ca_topic_score_codex":0.98487574,"about_ca_topic_score_gemma":0.9924899,"teacher_disagreement_score":0.037399415,"about_ca_system_score_codex":0.009374824,"about_ca_system_score_gemma":0.015620579,"threshold_uncertainty_score":0.12511349},"labels":[],"label_agreement":null},{"id":"W2982209084","doi":"10.4095/222496","title":"Geometry and membrane deformation rate of the subducting Cascadia slab","year":2002,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Slab; Deformation (meteorology); Seismology; Geometry; Geodesy; Geophysics; Oceanography; Mathematics","score_opus":0.03430832372594655,"score_gpt":0.22631035261391141,"score_spread":0.19200202888796486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982209084","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891734,0.000006370942,0.00014913133,0.000018402367,5.600708e-7,0.0000010313223,0.00006786203,0.000014227381,0.0008251432],"genre_scores_gemma":[0.9996692,0.000008018838,0.00009346249,0.0000012467792,3.0184006e-7,9.674341e-7,0.000079114645,0.0000026435177,0.00014508884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996614,0.0000034350874,0.000002738659,0.000013972297,0.0000064471187,0.0000072921503],"domain_scores_gemma":[0.99991345,0.000011604058,0.00002473963,0.000013479725,0.00001569261,0.000020919222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006240684,0.00018047882,0.000120594545,0.00050392584,0.00027811766,0.00041944793,0.00022935073,0.00021298377,0.0015433157],"category_scores_gemma":[0.00046908247,0.0002329854,0.00017409772,0.00031989207,0.00046159263,0.0001859949,0.00027936723,0.00019675137,0.00020480703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054816564,0.000110181616,0.47066322,0.00006732911,0.000082852945,0.0013337503,0.0007999869,0.2600115,0.2459315,0.006781454,0.00058391225,0.013086214],"study_design_scores_gemma":[0.000038352435,0.00013800395,0.7286585,0.000012234082,0.00002552334,0.0003905641,0.0005636306,0.25641054,0.011894409,0.0012477995,0.0005791346,0.000041289004],"about_ca_topic_score_codex":0.014332825,"about_ca_topic_score_gemma":0.008683979,"teacher_disagreement_score":0.014332825,"about_ca_system_score_codex":0.0007613099,"about_ca_system_score_gemma":0.0003001175,"threshold_uncertainty_score":0.028498828},"labels":[],"label_agreement":null},{"id":"W2982252195","doi":"10.4095/222536","title":"Thermal structure and metamorphism of subducting oceanic crust: insight into Cascadia intraslab earthquakes","year":2002,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Metamorphism; Subduction; Seismology; Oceanic crust; Crust; Geochemistry; Earth science; Tectonics","score_opus":0.026663250278783985,"score_gpt":0.22693980429796126,"score_spread":0.20027655401917727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982252195","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99809295,0.00009133265,0.00010788334,0.000022554412,9.383879e-7,0.0000033176668,0.00040490317,0.0000055406485,0.0012704426],"genre_scores_gemma":[0.998928,0.00019487232,0.00010870956,0.0000043676205,0.000002838484,0.0000023928183,0.0003958241,0.0000029039822,0.00035993944],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99997294,0.000003134279,0.0000024796482,0.0000075334724,0.0000064147066,0.0000074176533],"domain_scores_gemma":[0.99985445,0.000018343586,0.000044064487,0.000015383162,0.000038586764,0.000029095669],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000070933784,0.00021121731,0.00011324085,0.00081728847,0.00022001106,0.00021686287,0.00013783798,0.00012586617,0.0012678046],"category_scores_gemma":[0.000319046,0.00016679506,0.00015596004,0.0010109778,0.0001738968,0.0002699801,0.00028949298,0.00013152977,0.00014230126],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033456346,0.00004181018,0.95148075,0.000057254772,0.000051455172,0.00026307875,0.0006439344,0.0017065608,0.030181233,0.00017903664,0.00028389957,0.014776491],"study_design_scores_gemma":[0.0000015403128,0.000010315046,0.9993555,9.899483e-7,0.0000052812975,0.000027014301,0.0000625538,0.00014801056,0.00027472826,0.000020682244,0.000092477974,9.439327e-7],"about_ca_topic_score_codex":0.024664747,"about_ca_topic_score_gemma":0.04590294,"teacher_disagreement_score":0.97533524,"about_ca_system_score_codex":0.0002478484,"about_ca_system_score_gemma":0.00022204618,"threshold_uncertainty_score":0.049042404},"labels":[],"label_agreement":null},{"id":"W2982629646","doi":"10.3390/rs11212521","title":"Co-Seismic Deformation and Fault Slip Model of the 2017 Mw 7.3 Darbandikhan, Iran–Iraq Earthquake Inferred from D-InSAR Measurements","year":2019,"lang":"en","type":"article","venue":"Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Geology, China Earthquake Administration; Canadian Institutes of Health Research; U.S. Geological Survey; Consortium of International Agricultural Research Centers; China Earthquake Administration; National Natural Science Foundation of China; European Space Agency; National Science Foundation","keywords":"Geology; Seismology; Aftershock; Interferometric synthetic aperture radar; Thrust fault; Fault (geology); Anticline; Slip (aerodynamics); Tectonics; Synthetic aperture radar","score_opus":0.05262467608854103,"score_gpt":0.23687460861932952,"score_spread":0.18424993253078847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982629646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964026,0.0000928271,0.0012053429,0.00009937699,0.000017269198,0.000009584259,0.0011859764,0.00010606497,0.00088104286],"genre_scores_gemma":[0.99839276,0.0000394326,0.00040064065,0.000008913039,0.0000061883597,0.0000055733303,0.00093499117,0.00000889524,0.00020260483],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999039,0.000010344907,0.0000058162977,0.00003082584,0.000016099306,0.000033015865],"domain_scores_gemma":[0.9998715,0.000022557591,0.0000329244,0.000019515677,0.00003339208,0.000020119678],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024246598,0.00056026655,0.00025762,0.0010938101,0.00023973508,0.00041617875,0.00049484894,0.00058159453,0.0011564784],"category_scores_gemma":[0.00052038237,0.0002759279,0.00057307153,0.00084710674,0.00024608686,0.00037264515,0.0002504192,0.00034658253,0.00037235627],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031864177,0.00032185283,0.4717301,0.00008850041,0.0002580154,0.0009764199,0.00029098382,0.48648113,0.009316045,0.00089119666,0.00492895,0.024398236],"study_design_scores_gemma":[0.000028678956,0.000033797576,0.24246727,0.0000109025905,0.000041553772,0.00011253639,0.00011383428,0.7557427,0.0005698699,0.00019725887,0.00065828336,0.000023233475],"about_ca_topic_score_codex":0.037538905,"about_ca_topic_score_gemma":0.026730133,"teacher_disagreement_score":0.037538905,"about_ca_system_score_codex":0.0005017565,"about_ca_system_score_gemma":0.0004971879,"threshold_uncertainty_score":0.07464081},"labels":[],"label_agreement":null},{"id":"W2982692104","doi":"","title":"Shatter Cones, Shock Attenuation and Feldspars: Manicouagan Impact Structure, Canada","year":2016,"lang":"en","type":"article","venue":"79th Annual Meeting of the Meteoritical Society","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Impact structure; Attenuation; Geology; Shock (circulatory); Seismology; Mineralogy; Impact crater; Physics; Astrobiology; Optics","score_opus":0.009076045967062754,"score_gpt":0.21300129175101884,"score_spread":0.2039252457839561,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982692104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94599426,0.003698632,0.00039307692,0.001494458,0.00002557466,0.00005900445,0.0043035196,0.000044014883,0.04398744],"genre_scores_gemma":[0.96757954,0.0022665514,0.0002562724,0.00005596631,0.000005604891,0.000010462301,0.0011911377,0.000020174404,0.028614199],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982065,0.000008837578,0.000005240778,0.000021685411,0.000071733324,0.00007185295],"domain_scores_gemma":[0.9987658,0.0000572818,0.00006521822,0.000016272432,0.00095928466,0.0001360704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002543508,0.00031313277,0.00025729305,0.0018996638,0.0031728926,0.0013378373,0.0009075276,0.0002566093,0.0078076394],"category_scores_gemma":[0.00079957064,0.00025057755,0.00020364337,0.0038671512,0.0010820548,0.0004274841,0.00060365384,0.00043937692,0.0004191084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005034299,0.00009873326,0.89994437,0.000115031864,0.000083429026,0.0003380384,0.0028432456,0.003593728,0.0024160268,0.0064137564,0.011471553,0.07217865],"study_design_scores_gemma":[0.00000901734,0.000021170035,0.98780173,0.000040038343,0.000017228904,0.000049298993,0.0034806214,0.0007401619,0.00030048387,0.00028914504,0.007235155,0.00001598126],"about_ca_topic_score_codex":0.9977355,"about_ca_topic_score_gemma":0.9994073,"teacher_disagreement_score":0.027912525,"about_ca_system_score_codex":0.027912525,"about_ca_system_score_gemma":0.033051535,"threshold_uncertainty_score":0.20252049},"labels":[],"label_agreement":null},{"id":"W2983394461","doi":"10.1029/2019gl084848","title":"Lateral Variations in Lithospheric Mantle Structure Control the Location of Intracontinental Seismicity in Australia","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"University of Minnesota","keywords":"Intraplate earthquake; Induced seismicity; Geology; Lithosphere; Seismology; Mantle (geology); Attenuation; Geophysics; Tectonics; Physics","score_opus":0.01886868416152347,"score_gpt":0.27301027453107274,"score_spread":0.25414159036954925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983394461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999337,0.000045728368,0.00008884099,0.000015592503,3.3772793e-7,8.528897e-7,0.000018964503,0.0000021958579,0.0004904937],"genre_scores_gemma":[0.9998461,0.000019354136,0.00003316211,0.0000024700892,4.318856e-7,5.5174985e-7,0.000013685086,7.490678e-7,0.00008343523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999343,0.000013860849,0.000004268015,0.000017241355,0.000012765766,0.000017548644],"domain_scores_gemma":[0.99954766,0.000075042706,0.00017573968,0.000027222999,0.00012454692,0.000049740225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018193241,0.00009649084,0.000131592,0.00054672785,0.00019105784,0.00036666123,0.00020414143,0.00013979142,0.000909575],"category_scores_gemma":[0.0007711429,0.00013825712,0.00008228502,0.00044851055,0.00038866882,0.00026844573,0.00051716523,0.00013317382,0.000139561],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000113593436,0.000024317545,0.9261419,0.000034556433,0.000053817326,0.00014868798,0.0016514191,0.00086491206,0.057976086,0.00036064684,0.00009878284,0.012531182],"study_design_scores_gemma":[6.42719e-7,0.000008419012,0.99897504,0.0000023280993,0.0000038534026,0.000015403954,0.00018567865,0.00036428074,0.0003231888,0.00003942668,0.00008056215,0.0000012742754],"about_ca_topic_score_codex":0.017990785,"about_ca_topic_score_gemma":0.020280411,"teacher_disagreement_score":0.017990785,"about_ca_system_score_codex":0.0002879987,"about_ca_system_score_gemma":0.00023506208,"threshold_uncertainty_score":0.035772145},"labels":[],"label_agreement":null},{"id":"W2983876567","doi":"10.1038/s41561-019-0472-x","title":"Role of dynamic topography in sustaining the Nile River over 30 million years","year":2019,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle (geology); Mantle convection; Subsidence; Paleontology; Ocean surface topography; Nile delta; Drainage; Tectonics; Earth science; Oceanography; Subduction; Structural basin","score_opus":0.002534397831245332,"score_gpt":0.20012553069345465,"score_spread":0.1975911328622093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983876567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993739,0.0009146448,0.0003397846,0.0009859983,0.000020778907,0.0000050934987,0.0002783779,0.000009712368,0.0037066897],"genre_scores_gemma":[0.9995384,0.00020271567,0.00003926541,0.00002302848,0.0000047815306,0.0000011477742,0.000046200923,0.0000015328231,0.00014297407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978834,0.000052458312,0.000018905663,0.000039237268,0.000027196102,0.00007379636],"domain_scores_gemma":[0.999042,0.00014132564,0.00037888298,0.00006643359,0.0001436232,0.00022778464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006069804,0.00016474121,0.00015391452,0.00064146373,0.0005667601,0.0014438102,0.00044526387,0.00048112133,0.00216168],"category_scores_gemma":[0.0027121736,0.00015285911,0.00021576932,0.0005743976,0.001028912,0.00082020793,0.0012986091,0.0005108205,0.00019495212],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000099409546,0.000054176424,0.9631614,0.000087768276,0.00017409935,0.0005480101,0.00079225557,0.0042324183,0.0018768683,0.0030136474,0.000739815,0.025220143],"study_design_scores_gemma":[0.0000069541084,0.00008420401,0.98796797,0.00004540897,0.000089361485,0.00024268511,0.002688095,0.004209829,0.00017653158,0.0015547815,0.0029153626,0.000018734383],"about_ca_topic_score_codex":0.027426718,"about_ca_topic_score_gemma":0.052943323,"teacher_disagreement_score":0.027426718,"about_ca_system_score_codex":0.0010398033,"about_ca_system_score_gemma":0.0010092609,"threshold_uncertainty_score":0.054534137},"labels":[],"label_agreement":null},{"id":"W2984172238","doi":"10.1146/annurev-earth-053018-060507","title":"The State of Stress on the Fault Before, During, and After a Major Earthquake","year":2019,"lang":"en","type":"article","venue":"Annual Review of Earth and Planetary Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Seismology; Trench; Fault (geology); Earthquake rupture; Drilling; Remotely triggered earthquakes; Slip (aerodynamics); Dissipation; Slow earthquake; Shear (geology); Elastic-rebound theory; Seismic gap; Intraplate earthquake; Interplate earthquake; Petrology; Tectonics; Engineering; Materials science","score_opus":0.007618474120845492,"score_gpt":0.21454252765561985,"score_spread":0.20692405353477436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2984172238","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.018092083,0.97364604,0.00047863188,0.0013224016,0.00038074944,0.000005677225,0.00014650599,0.000018752173,0.0059091225],"genre_scores_gemma":[0.07245555,0.92432785,0.00031022177,0.00029134355,0.00044456715,0.000007784462,0.00011695377,0.000005594759,0.0020401177],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997929,0.000031463835,0.000022299115,0.00007789111,0.000047985992,0.000027512162],"domain_scores_gemma":[0.99967563,0.00009182596,0.00008942695,0.0000147863175,0.00009261141,0.000035839053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005333529,0.00031024707,0.00051226205,0.0013936729,0.0002466673,0.0012294258,0.000476201,0.00088922464,0.0006395506],"category_scores_gemma":[0.00080897193,0.00015951978,0.00016486678,0.001563729,0.00097067317,0.0009347916,0.0003458391,0.0004235019,0.0004672572],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011770934,0.00006960991,0.016056504,0.006370168,0.00022926372,0.00024745954,0.0008800554,0.0010272585,0.0114009725,0.017966848,0.015229164,0.930405],"study_design_scores_gemma":[0.000021889267,0.00048996217,0.18671906,0.0040219254,0.0003731362,0.0012560171,0.0033835773,0.0005240267,0.005104065,0.014539656,0.7834366,0.00013014575],"about_ca_topic_score_codex":0.003780875,"about_ca_topic_score_gemma":0.005406492,"teacher_disagreement_score":0.003780875,"about_ca_system_score_codex":0.00079513795,"about_ca_system_score_gemma":0.0007803117,"threshold_uncertainty_score":0.007517755},"labels":[],"label_agreement":null},{"id":"W2984243112","doi":"10.1002/essoar.10501094.1","title":"Lateral migration patterns toward or away from injection wells for earthquake clusters in Oklahoma","year":2019,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Kootenay Association for Science & Technology","funders":"","keywords":"World Wide Web; Preprint; Electronic mail; Computer science","score_opus":0.021371426070169834,"score_gpt":0.2257436611515061,"score_spread":0.20437223508133626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2984243112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993736,0.000013678084,0.000071718976,0.000015076775,9.876427e-7,0.000002922348,0.00020727848,0.0000054365023,0.00030926376],"genre_scores_gemma":[0.9991924,0.000016328922,0.00020112412,0.0000044173034,8.577956e-7,0.0000061811015,0.00025474132,0.000001885356,0.00032207568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999249,0.000007350225,0.0000066212706,0.000022591952,0.000011137442,0.000027431375],"domain_scores_gemma":[0.9996253,0.00005097368,0.00014040663,0.000019934052,0.000083624145,0.00007976915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010700708,0.00016162453,0.00017039916,0.0010282584,0.0006098665,0.00045105,0.00020374396,0.00029098446,0.0012365239],"category_scores_gemma":[0.00043223164,0.00011247934,0.00014754933,0.0010095489,0.00024563866,0.00028114705,0.00048508483,0.00017221896,0.0002047141],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021761494,0.000060353348,0.9700431,0.000037868205,0.000056162877,0.00023212048,0.0013493045,0.0030045672,0.010430018,0.00013232489,0.00041746837,0.014019065],"study_design_scores_gemma":[0.0000034869474,0.00002274758,0.9951611,0.00000943393,0.000014724696,0.00003004852,0.0014311376,0.0025242595,0.00045314032,0.00002558894,0.0003133876,0.000010839267],"about_ca_topic_score_codex":0.09452072,"about_ca_topic_score_gemma":0.22067145,"teacher_disagreement_score":0.09452072,"about_ca_system_score_codex":0.00095943967,"about_ca_system_score_gemma":0.0007267836,"threshold_uncertainty_score":0.18794107},"labels":[],"label_agreement":null},{"id":"W2986527015","doi":"10.3390/geosciences9110480","title":"Spatio-Temporal Relationships between Fumarolic Activity, Hydrothermal Fluid Circulation and Geophysical Signals at an Arc Volcano in Degassing Unrest: La Soufrière of Guadeloupe (French West Indies)","year":2019,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Institut de Physique du Globe de Paris; Università degli Studi di Palermo; Centre National de la Recherche Scientifique; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Agence Nationale de la Recherche; National Science Foundation","keywords":"Unrest; Geology; Volcano; West indies; Hydrothermal circulation; Seismology; Geophysics; History","score_opus":0.03005370757535106,"score_gpt":0.23822441162635474,"score_spread":0.20817070405100369,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2986527015","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99919707,0.00017574489,0.000041161406,0.000032483193,0.0000023211403,0.0000024944343,0.00032462337,0.000008346386,0.00021582426],"genre_scores_gemma":[0.99917245,0.00009215073,0.0001064819,0.0000098405635,0.000005127354,0.0000067651717,0.0004085533,0.0000032399957,0.0001954028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998522,0.000016085136,0.0000073684005,0.000053702483,0.000022712922,0.00004788968],"domain_scores_gemma":[0.9997062,0.00003721029,0.000116087205,0.00001474288,0.00006307671,0.000062695704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016693174,0.00026188427,0.00023854648,0.0011101707,0.00035004877,0.0007250493,0.00025410793,0.0004667295,0.00072242075],"category_scores_gemma":[0.0004797436,0.00011692091,0.00022535982,0.00090366334,0.0004044734,0.00020522535,0.00051313534,0.00020795505,0.00013457905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014877915,0.000033389177,0.97888285,0.000044253004,0.00014128748,0.00044549946,0.001816818,0.0005493388,0.010201466,0.00004617348,0.00036197668,0.0073282],"study_design_scores_gemma":[6.3073895e-7,0.000003929293,0.99937373,0.0000023322245,0.0000043531486,0.000029644209,0.00022760229,0.00007149751,0.000055402485,0.0000015123974,0.00022730314,0.0000021712306],"about_ca_topic_score_codex":0.24278432,"about_ca_topic_score_gemma":0.31560093,"teacher_disagreement_score":0.24278432,"about_ca_system_score_codex":0.0013573004,"about_ca_system_score_gemma":0.0004963422,"threshold_uncertainty_score":0.4827423},"labels":[],"label_agreement":null},{"id":"W2990757039","doi":"10.1029/2020jb020606","title":"Statistical Modeling and Characterization of Induced Seismicity Within the Western Canada Sedimentary Basin","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Aftershock; Seismology; Geology; Tectonics; Magnitude (astronomy); Structural basin; Maximum magnitude; Sedimentary rock; Paleontology","score_opus":0.057131941164127065,"score_gpt":0.2925628592753173,"score_spread":0.2354309181111902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2990757039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962961,0.00003123584,0.0023710197,0.000039806724,0.0000019240586,0.000015836076,0.0007133388,0.000029697458,0.00050097785],"genre_scores_gemma":[0.99819237,0.000028301347,0.0005577588,0.000004122287,0.0000013755897,0.000005735851,0.0008248397,0.0000037598336,0.00038167852],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997031,0.00003664803,0.00002108485,0.000074749216,0.0000922032,0.0000720878],"domain_scores_gemma":[0.9988932,0.00033941574,0.00017746096,0.00009033322,0.00039791997,0.00010165177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004972803,0.00021480396,0.00019956009,0.0013540031,0.0005572073,0.0006812857,0.0006223989,0.00018353503,0.000842371],"category_scores_gemma":[0.0028607666,0.00014034167,0.00037574777,0.0014713941,0.0005324198,0.0001957891,0.00035792938,0.00026918258,0.00007672396],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000104353676,0.000051970568,0.80300856,0.00002645456,0.00020189266,0.00026467466,0.00029583613,0.17406294,0.0018674253,0.0016278842,0.00083134155,0.017656662],"study_design_scores_gemma":[0.000005251126,0.000029498107,0.6381572,0.0000073853093,0.000038830407,0.000037443762,0.00049427745,0.35945603,0.00048834406,0.00042723498,0.00084141793,0.000017110238],"about_ca_topic_score_codex":0.92724866,"about_ca_topic_score_gemma":0.90603936,"teacher_disagreement_score":0.07275134,"about_ca_system_score_codex":0.0048495177,"about_ca_system_score_gemma":0.0045939963,"threshold_uncertainty_score":0.1463595},"labels":[],"label_agreement":null},{"id":"W2990768800","doi":"","title":"Cataclastic production of volcanic ash at Mount Saint Helens","year":2011,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Cataclastic rock; Geology; Fault gouge; Shear (geology); Compaction; Fault (geology); Seismology; Comminution; Petrology; Volcano; Dacite; Geochemistry; Geotechnical engineering; Volcanic rock; Rhyolite","score_opus":0.030436912756045983,"score_gpt":0.19428818429641678,"score_spread":0.1638512715403708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2990768800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996933,0.000014829212,0.00002253179,0.0000085826205,7.253305e-7,0.0000028115724,0.000026081687,0.0000043611485,0.00022679112],"genre_scores_gemma":[0.9996549,0.000014943777,0.000053156364,0.0000061890246,0.0000016757309,0.0000022809095,0.000046530575,0.0000015076063,0.00021874253],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998566,0.000014563197,0.0000058907904,0.00003510676,0.00006666949,0.00002120004],"domain_scores_gemma":[0.99985623,0.000023301875,0.000038364622,0.000014713346,0.000028625136,0.000038734866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017674985,0.00017444567,0.00014804796,0.0003017235,0.00037728672,0.000433467,0.00023870825,0.0003903373,0.0008563518],"category_scores_gemma":[0.00021578085,0.00019429522,0.00010427556,0.0001589892,0.0004902369,0.00017629979,0.0003221197,0.00027600996,0.00013910768],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015854939,0.000030881965,0.026477756,0.000028606835,0.000016155882,0.00033046785,0.0002948193,0.0002893865,0.9700097,0.0000519275,0.0000544587,0.0022572794],"study_design_scores_gemma":[0.000035353256,0.0007970354,0.77355653,0.0000065334616,0.0000143517345,0.000336094,0.0004500756,0.0018067186,0.22181481,0.00004898479,0.0011178544,0.000015679672],"about_ca_topic_score_codex":0.004651565,"about_ca_topic_score_gemma":0.011205926,"teacher_disagreement_score":0.004651565,"about_ca_system_score_codex":0.0005365522,"about_ca_system_score_gemma":0.00017097041,"threshold_uncertainty_score":0.009249032},"labels":[],"label_agreement":null},{"id":"W2991571263","doi":"","title":"Extreme Wave Deposits On The Pacific Coast Of Mexico: Tsunamis Or Storms? - A Multi-Proxy Approach","year":2011,"lang":"en","type":"article","venue":"The Australian Nuclear Science and Technology Organisation Institutional Repository (The Australian Nuclear Science and Technology Organisation)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Storm; Oceanography; Proxy (statistics); Geology; Geography","score_opus":0.05056564486458669,"score_gpt":0.22382671133912116,"score_spread":0.1732610664745345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2991571263","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99649006,0.00041852883,0.0005736465,0.0001412642,0.00000519216,0.000012893193,0.00096289226,0.000012826172,0.0013825804],"genre_scores_gemma":[0.997224,0.00036077754,0.0013262384,0.000016994865,0.000011017767,0.000012794334,0.00072349963,0.000004795099,0.00031989894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998129,0.000040875184,0.000024128414,0.000061346465,0.000028635717,0.00003221781],"domain_scores_gemma":[0.9992392,0.00017071431,0.00035009833,0.00006778026,0.00009630789,0.0000758174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051589275,0.00022452723,0.00031577813,0.0029267247,0.00047546145,0.0017028166,0.0004478511,0.0004103344,0.0011803376],"category_scores_gemma":[0.0015308369,0.00017777039,0.00020872043,0.0027570913,0.00031462716,0.00090179296,0.00096461276,0.0003219527,0.00012189379],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003057843,0.00001750277,0.98855364,0.000022294473,0.000090905894,0.00011979489,0.0003892432,0.0005641486,0.00044575275,0.00012858576,0.00016560777,0.009472026],"study_design_scores_gemma":[0.0000024889707,0.000015451755,0.9947737,0.000027233538,0.000046654786,0.00005560969,0.0013826217,0.0028399322,0.00010205261,0.00009025053,0.0006579815,0.000006059645],"about_ca_topic_score_codex":0.057406172,"about_ca_topic_score_gemma":0.087111555,"teacher_disagreement_score":0.057406172,"about_ca_system_score_codex":0.00063246983,"about_ca_system_score_gemma":0.0003001753,"threshold_uncertainty_score":0.11414409},"labels":[],"label_agreement":null},{"id":"W2991722808","doi":"10.1002/essoar.10501237.1","title":"Correlating earthquake static stress drop values with fault complexity in the 2016 Amatrice-Norcia earthquake sequence, Central Italy","year":2019,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Seismic moment; Aftershock; Sequence (biology); Earthquake simulation; Fault (geology); Earthquake magnitude; Seismic gap; Earthquake swarm; Induced seismicity; Scaling; Mathematics; Geometry","score_opus":0.03293863248735291,"score_gpt":0.2403569004003908,"score_spread":0.20741826791303788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2991722808","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99803275,0.00010323438,0.00013793736,0.000032985274,0.000008168103,0.000009329361,0.00082099834,0.000021987016,0.00083256],"genre_scores_gemma":[0.9965867,0.000095570984,0.00023114607,0.000010458045,0.000029700965,0.000013018797,0.0027870573,0.000011212656,0.0002352267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977297,0.000024761597,0.000025085681,0.00007443652,0.000050418796,0.000052361946],"domain_scores_gemma":[0.9990707,0.00011365261,0.0004346118,0.00011113468,0.00015404087,0.00011600898],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034853234,0.00037717,0.0003077026,0.00174507,0.00018788286,0.0006716788,0.00028593309,0.00031825888,0.0006438813],"category_scores_gemma":[0.002469991,0.00016380407,0.00023634845,0.0012924802,0.00045304923,0.0002532341,0.0006752096,0.00021150507,0.0003413818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022468397,0.000045731587,0.980135,0.00005455636,0.00006497031,0.00034712875,0.0005257784,0.0028894546,0.0037902482,0.0001016558,0.0011932495,0.010627526],"study_design_scores_gemma":[0.0000050058657,0.000010196123,0.9989303,0.0000045377815,0.0000057585685,0.000042755117,0.000052108968,0.0006154948,0.00005798044,0.0000135635755,0.00025933734,0.000002921124],"about_ca_topic_score_codex":0.026859825,"about_ca_topic_score_gemma":0.03266464,"teacher_disagreement_score":0.026859825,"about_ca_system_score_codex":0.0005751909,"about_ca_system_score_gemma":0.00031809747,"threshold_uncertainty_score":0.053406954},"labels":[],"label_agreement":null},{"id":"W2991773946","doi":"10.5539/mas.v13n12p80","title":"Late Miocene to Pliocene Tsunami Deposits in Tegal Buleud, South Sukabumi, West Java, Indonesia","year":2019,"lang":"en","type":"article","venue":"Modern Applied Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Sedimentary rock; Subduction; Siltstone; Java; Late Miocene; Paleontology; Neogene; Tectonics; Clastic rock; Bedding; Geochemistry; Structural basin","score_opus":0.010601859072324032,"score_gpt":0.20105925443057962,"score_spread":0.1904573953582556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2991773946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991779,0.00015984838,0.000020394413,0.0000107260985,0.0000013475635,0.0000025033921,0.000089923284,0.0000026008952,0.0005348093],"genre_scores_gemma":[0.9991793,0.00018419599,0.00007866661,0.000008056213,0.0000014021313,0.000003131421,0.00015092579,0.0000013296424,0.00039278623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996555,0.00000249721,0.0000062484723,0.000009172256,0.000006309298,0.000010237446],"domain_scores_gemma":[0.99993324,0.0000055105465,0.000026480278,0.0000026155544,0.000012504486,0.000019703035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006221242,0.0001935901,0.00012682505,0.00087992096,0.00035560742,0.00041170442,0.00017408327,0.00012685721,0.0010162286],"category_scores_gemma":[0.0001324335,0.00013535006,0.00006813495,0.000914209,0.00021057866,0.00021012776,0.00028754713,0.00008874238,0.00012920151],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001181421,0.00002795101,0.96012056,0.00010706106,0.000024881583,0.0014633395,0.0035192955,0.00011255345,0.011324393,0.000080079415,0.00016410949,0.02293767],"study_design_scores_gemma":[0.0000012873185,0.000008388801,0.99825543,0.000008668737,0.000004230651,0.00013685478,0.0010700874,0.00003320966,0.00014396495,0.000007449878,0.00032945108,0.0000010642993],"about_ca_topic_score_codex":0.031639062,"about_ca_topic_score_gemma":0.1210101,"teacher_disagreement_score":0.031639062,"about_ca_system_score_codex":0.0003864587,"about_ca_system_score_gemma":0.00027384277,"threshold_uncertainty_score":0.06290984},"labels":[],"label_agreement":null},{"id":"W2991969965","doi":"","title":"Lithospheric density structure beneath the Canadian shield by inversion of isostatic response function","year":2003,"lang":"en","type":"article","venue":"EGS - AGU - EUG Joint Assembly","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Shield; Lithosphere; Inversion (geology); Seismology; Petrology; Tectonics","score_opus":0.01425852954995355,"score_gpt":0.19648443130349313,"score_spread":0.1822259017535396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2991969965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926279,0.00012417982,0.0006057832,0.000116191135,0.000009412069,0.0000086703085,0.0014914002,0.000114570874,0.004901821],"genre_scores_gemma":[0.9981818,0.000052483323,0.00044235005,0.000011120329,0.0000020547834,0.000001994457,0.0006946462,0.000012136833,0.0006015192],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985886,0.000007894261,0.0000030579279,0.000026517479,0.000043472053,0.000060124425],"domain_scores_gemma":[0.9997763,0.000017561675,0.000019549283,0.0000121412395,0.00014277875,0.000031639967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015383323,0.00035004775,0.00026082204,0.0010400881,0.0010863867,0.0007125855,0.00073681504,0.00030290495,0.0021271908],"category_scores_gemma":[0.0006355431,0.00022309365,0.0002668763,0.0018776623,0.00043626866,0.00022934178,0.00031411738,0.00035098827,0.0002628799],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012880658,0.00022201936,0.6654779,0.00015229131,0.00027577998,0.000547822,0.0019425995,0.16072224,0.061851166,0.004025273,0.0099496525,0.093545236],"study_design_scores_gemma":[0.00004365226,0.000016176695,0.9325273,0.000017748589,0.00004071074,0.000058449627,0.00038447895,0.06173563,0.0021211896,0.0002086288,0.0027873034,0.00005880713],"about_ca_topic_score_codex":0.9843768,"about_ca_topic_score_gemma":0.9865975,"teacher_disagreement_score":0.015623212,"about_ca_system_score_codex":0.006535883,"about_ca_system_score_gemma":0.009676945,"threshold_uncertainty_score":0.047421396},"labels":[],"label_agreement":null},{"id":"W2992197908","doi":"10.1785/0220190230","title":"A Systematic Study of Earthquake Source Mechanism and Regional Stress Field in the Southern Montney Unconventional Play of Northeast British Columbia, Canada","year":2019,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria; Geoscience BC","funders":"","keywords":"Focal mechanism; Geology; Seismology; Fault plane; Stress field; Fault (geology); Principal stress; Slip (aerodynamics); Inversion (geology); Geodesy; Stress (linguistics); Tectonics; Paleontology; Physics","score_opus":0.027606223703684988,"score_gpt":0.2395012344054673,"score_spread":0.21189501070178232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2992197908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931906,0.00062399596,0.00020076126,0.000113595204,0.0000072660623,0.000031809217,0.0024381552,0.000021862861,0.003371938],"genre_scores_gemma":[0.99611926,0.00041862714,0.0002837019,0.00005030189,0.000002562268,0.000015984026,0.0013342837,0.0000108986505,0.0017642924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996356,0.00001995522,0.000016996546,0.00007914429,0.00011173412,0.00013643748],"domain_scores_gemma":[0.9985459,0.00007243647,0.0001651116,0.000051657345,0.0008962519,0.00026877428],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025738555,0.0004644731,0.00039566343,0.0031991012,0.0027399892,0.0013667308,0.00081840606,0.00031472318,0.0021521214],"category_scores_gemma":[0.00089501514,0.0002711696,0.00022312834,0.0061007966,0.00089676585,0.00028843313,0.0007981179,0.00035086932,0.0002957464],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000069346344,0.000028137345,0.9717691,0.00010489986,0.00007396833,0.00041588268,0.0028418186,0.00039224146,0.0048112404,0.00018002157,0.0018067851,0.017506644],"study_design_scores_gemma":[0.0000021711228,0.0000065963245,0.9947848,0.00003741166,0.0000149109355,0.00005286386,0.0025570316,0.0002548808,0.00019729033,0.00001353274,0.0020682102,0.000010347669],"about_ca_topic_score_codex":0.9933334,"about_ca_topic_score_gemma":0.9985505,"teacher_disagreement_score":0.013415172,"about_ca_system_score_codex":0.013415172,"about_ca_system_score_gemma":0.01490927,"threshold_uncertainty_score":0.097334325},"labels":[],"label_agreement":null},{"id":"W2993447891","doi":"10.1029/2019gl085651","title":"The August 2018 Kaktovik Earthquakes: Active Tectonics in Northeastern Alaska Revealed With InSAR and Seismology","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Canada Foundation for Innovation","keywords":"Seismology; Geology; Interferometric synthetic aperture radar; Tectonics; Seismic hazard; Fault (geology); Sinistral and dextral; Active fault; Synthetic aperture radar; Remote sensing","score_opus":0.020494431141001378,"score_gpt":0.2563172188177325,"score_spread":0.23582278767673112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2993447891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990128,0.00006284221,0.00009315481,0.000024285802,0.0000033694303,0.0000012287431,0.00014759297,0.000006819457,0.00064782245],"genre_scores_gemma":[0.9994844,0.00005437362,0.00011732679,0.0000027983815,0.0000023870377,6.4070656e-7,0.00014147251,8.813118e-7,0.0001956339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995375,0.000008414011,0.0000061245523,0.000014415647,0.000010041137,0.000007321927],"domain_scores_gemma":[0.9998779,0.00001267106,0.00004728884,0.000014236907,0.000026099791,0.000021675487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018636361,0.00013210798,0.000112336784,0.00046605486,0.00036837888,0.00038273406,0.0001114631,0.00018289947,0.0005430748],"category_scores_gemma":[0.00040283377,0.00008356319,0.000096526725,0.00037121575,0.0002274841,0.00038491812,0.0003728102,0.00013359378,0.00013522904],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011250374,0.000046210513,0.9767526,0.00002085097,0.00003611438,0.000544756,0.0009858925,0.0033101789,0.0049341726,0.00014305228,0.00029306443,0.012820631],"study_design_scores_gemma":[0.0000022325685,0.000023677827,0.99558663,0.00001249321,0.0000154929,0.000099502264,0.000910551,0.0023316261,0.00035796803,0.00008053053,0.0005736985,0.000005508293],"about_ca_topic_score_codex":0.041369822,"about_ca_topic_score_gemma":0.08006749,"teacher_disagreement_score":0.041369822,"about_ca_system_score_codex":0.00031484442,"about_ca_system_score_gemma":0.00028064463,"threshold_uncertainty_score":0.082258046},"labels":[],"label_agreement":null},{"id":"W2994772960","doi":"10.1029/2019jb018132","title":"Support Vector Machine Classification of Seismic Events in the Tianshan Orogenic Belt","year":2019,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Natural Science Foundation of China","keywords":"Geology; Seismology; Support vector machine; Tectonics; Aftershock; Linear discriminant analysis; Event (particle physics); Machine learning; Artificial intelligence","score_opus":0.04838211000766522,"score_gpt":0.32810722610715076,"score_spread":0.2797251160994855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2994772960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996609,0.000052533822,0.002674729,0.000037147085,0.00001073975,0.000009509702,0.00025085057,0.000038525683,0.00031705675],"genre_scores_gemma":[0.99818784,0.000017865039,0.0011695332,0.0000054043244,0.000006238381,0.000004807072,0.00045613648,0.0000010553756,0.0001511616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997925,0.00003923107,0.00003092115,0.000047139773,0.000050936767,0.000039376202],"domain_scores_gemma":[0.99954706,0.0001249361,0.00012560654,0.000030085486,0.000118864176,0.000053344964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041280617,0.00030266913,0.0002447587,0.0015548206,0.00012547444,0.00029341815,0.00028670835,0.00021722462,0.0005394254],"category_scores_gemma":[0.00095256965,0.000060744773,0.00020809866,0.00090912957,0.00012455141,0.00024158564,0.00019240483,0.00014549377,0.00015583161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005969606,0.00029748396,0.6780507,0.00010622656,0.00010649048,0.0006173182,0.00021413298,0.04336879,0.023001736,0.00040309923,0.0023118097,0.2509253],"study_design_scores_gemma":[0.000028162212,0.0001837726,0.4682947,0.000016056905,0.000042440937,0.000104706385,0.0002949915,0.52504677,0.0049710777,0.0003109154,0.0006868859,0.000019557241],"about_ca_topic_score_codex":0.005704698,"about_ca_topic_score_gemma":0.004021206,"teacher_disagreement_score":0.005704698,"about_ca_system_score_codex":0.000291683,"about_ca_system_score_gemma":0.00023461583,"threshold_uncertainty_score":0.011343002},"labels":[],"label_agreement":null},{"id":"W2995493034","doi":"","title":"Realistic simulations of tsunami detection by High-Frequency Radar in British Columbia, Canada","year":2016,"lang":"en","type":"article","venue":"EGU General Assembly Conference Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Radar; Geology; Remote sensing; Geography; Seismology; Meteorology; Computer science; Telecommunications","score_opus":0.011464500043354774,"score_gpt":0.19633286898078797,"score_spread":0.1848683689374332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995493034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9776654,0.00028100007,0.0010495135,0.0014699487,0.00005292206,0.000060336606,0.0037509867,0.0001472899,0.015522643],"genre_scores_gemma":[0.9922327,0.00016179138,0.00072724937,0.00013357768,0.000007796478,0.000032583903,0.0013229186,0.000035757894,0.005345564],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996137,0.00006594955,0.000019021601,0.0000689201,0.00006220798,0.0001702045],"domain_scores_gemma":[0.9975943,0.0008711454,0.00012264182,0.00008674823,0.00082723296,0.0004979088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005561692,0.000956267,0.0010640672,0.001116068,0.002836387,0.0024416961,0.0037909064,0.0037554868,0.008647504],"category_scores_gemma":[0.003975386,0.0013521886,0.0008902136,0.0025419595,0.002080507,0.0012601046,0.0010617822,0.0020471301,0.0006360581],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013692043,0.00010656196,0.006334467,0.000023069697,0.00003331141,0.00013486814,0.00007180958,0.9891115,0.00020134619,0.0011108677,0.0017902919,0.0009449694],"study_design_scores_gemma":[0.00020170595,0.000039229366,0.0055600884,0.000013522608,0.000030423113,0.00001729352,0.00033219936,0.9925178,0.0001296941,0.00044969763,0.0006583126,0.000050037263],"about_ca_topic_score_codex":0.9887918,"about_ca_topic_score_gemma":0.9785774,"teacher_disagreement_score":0.026906203,"about_ca_system_score_codex":0.026906203,"about_ca_system_score_gemma":0.018277925,"threshold_uncertainty_score":0.1952191},"labels":[],"label_agreement":null},{"id":"W2995539746","doi":"10.1016/j.tecto.2019.228313","title":"Fault development in transtension, McCully gas field, New Brunswick, Canada","year":2019,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Transtension; Geology; Sinistral and dextral; Seismology; Transpression; Pull apart basin; Basin and range topography; Strike-slip tectonics; Fault (geology); Echelon formation; Outcrop; Shear (geology); Strain partitioning; Structural basin; Slip (aerodynamics); Petrology; Tectonics; Paleontology; Sedimentary basin","score_opus":0.0086854458204075,"score_gpt":0.18079767918930634,"score_spread":0.17211223336889883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995539746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9067551,0.0053181327,0.00052215235,0.0021929997,0.000087052955,0.00023452594,0.025247738,0.00010530977,0.059537087],"genre_scores_gemma":[0.8812868,0.003522989,0.0014051066,0.00017550126,0.000010525719,0.0000816472,0.007666466,0.000041479074,0.10580948],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996451,0.000024888895,0.000023638835,0.000054038617,0.00011424145,0.00013811764],"domain_scores_gemma":[0.99784935,0.000115503855,0.00013936292,0.000037792826,0.0015587551,0.00029915397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033142965,0.00037473039,0.0002598037,0.0034838812,0.003162643,0.001340556,0.0010191066,0.00027615973,0.0076167504],"category_scores_gemma":[0.0016028457,0.0002824528,0.00019098664,0.0065091583,0.00066858286,0.00064554036,0.00082588213,0.0007059349,0.00062352675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005175804,0.00014110393,0.8060851,0.0002712102,0.00008913481,0.0010588045,0.006944213,0.0027425021,0.00207581,0.0039995424,0.030158622,0.14591628],"study_design_scores_gemma":[0.000017532657,0.000028874423,0.972553,0.00009639983,0.000019495514,0.00013767573,0.008459308,0.00042847393,0.00037746594,0.00014113188,0.017722141,0.000018582165],"about_ca_topic_score_codex":0.99682164,"about_ca_topic_score_gemma":0.9995123,"teacher_disagreement_score":0.040281866,"about_ca_system_score_codex":0.040281866,"about_ca_system_score_gemma":0.048245125,"threshold_uncertainty_score":0.29226673},"labels":[],"label_agreement":null},{"id":"W2995842539","doi":"10.22215/etd/2008-06355","title":"Stress parameter distribution on an earthquake fault based on a stochastic modeling approach","year":2008,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Fault (geology); Humanities; Seismology; Geology; Philosophy","score_opus":0.029638893017435566,"score_gpt":0.24317781719173248,"score_spread":0.21353892417429693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995842539","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.41113982,0.00017539453,0.58248836,0.0004585677,0.00003659926,0.000037796566,0.00036202424,0.00030103474,0.005000346],"genre_scores_gemma":[0.9916351,0.00011645723,0.0062028156,0.000018329218,0.00001894282,0.000015871832,0.00019179925,0.000025995505,0.0017748228],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998355,0.000053884625,0.000009170591,0.000038205584,0.000035783476,0.000027432534],"domain_scores_gemma":[0.99914765,0.0004888498,0.00014666529,0.00005478041,0.000117630814,0.000044381108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060722424,0.00034447483,0.000465613,0.00067313696,0.000228087,0.00072595634,0.00061536545,0.0005570217,0.0017908349],"category_scores_gemma":[0.002059547,0.00032681256,0.0006071013,0.0005630825,0.0003548549,0.00056456146,0.00030158635,0.00042413556,0.00023402425],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017953078,0.000007719151,0.001119418,0.0000045808665,0.000009211975,0.000025816462,0.0000132721025,0.991029,0.00040984363,0.0049891407,0.00012935071,0.0022446048],"study_design_scores_gemma":[0.0000010319527,0.0000028788224,0.00022466182,7.900968e-7,0.0000015010671,0.0000038456315,0.0000019118986,0.9991935,0.000031218213,0.00051059993,0.000026338183,0.0000017187873],"about_ca_topic_score_codex":0.012068933,"about_ca_topic_score_gemma":0.008463355,"teacher_disagreement_score":0.012068933,"about_ca_system_score_codex":0.00080758746,"about_ca_system_score_gemma":0.00044258113,"threshold_uncertainty_score":0.023997366},"labels":[],"label_agreement":null},{"id":"W2996338418","doi":"","title":"Seismic Anisotropy and Mantle Flow, Comparing Global Geodynamic Models and Shear Wave Splitting Observations in Eastern Canada","year":2013,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Shear wave splitting; Seismology; Seismic anisotropy; Geophysics; Mantle (geology); Shear (geology); Geodynamics; Anisotropy; Geodesy; Paleontology; Physics; Tectonics","score_opus":0.034160955324117684,"score_gpt":0.20072419473860423,"score_spread":0.16656323941448653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996338418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978537,0.00011515252,0.00006413691,0.00012774917,0.0000023322466,0.0000041065728,0.0006266941,0.000012091053,0.0011939674],"genre_scores_gemma":[0.99849296,0.00011770215,0.00009851524,0.000012999949,9.793006e-7,0.000001869535,0.00044433417,0.000004893627,0.0008257312],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983144,0.000013130011,0.000009980644,0.000039027575,0.000042102554,0.000064246255],"domain_scores_gemma":[0.99949193,0.00006923521,0.00004732291,0.000022420476,0.00027995426,0.00008905276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032087715,0.0003027346,0.00021605301,0.0008966146,0.0019343145,0.0015621426,0.0008457039,0.00035215818,0.0016970073],"category_scores_gemma":[0.0013306685,0.00027601392,0.00032394135,0.0016600736,0.0005672259,0.00042833746,0.0005236564,0.00042178395,0.0001826501],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027624585,0.00007386157,0.96303546,0.000032829998,0.00012090013,0.00018887818,0.0015888355,0.013301952,0.0022979854,0.0010613173,0.001345938,0.016675828],"study_design_scores_gemma":[0.000027466123,0.000012749214,0.9794663,0.000025850704,0.00007020152,0.00003605331,0.0030572452,0.014736968,0.0006005782,0.00012891328,0.0018112799,0.000026348125],"about_ca_topic_score_codex":0.9984517,"about_ca_topic_score_gemma":0.998749,"teacher_disagreement_score":0.029894782,"about_ca_system_score_codex":0.029894782,"about_ca_system_score_gemma":0.02461671,"threshold_uncertainty_score":0.21690285},"labels":[],"label_agreement":null},{"id":"W2996727270","doi":"","title":"Deformation and Uranium Mineralisation of the Otish Basin: A 2,1Ga Shocked Rocks Potentially Owning to a D>500 kms Impact Structure, Québec, Canada","year":2012,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science Supplement","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Deformation (meteorology); Geochemistry; Structural basin; Uranium; Mining engineering; Earth science; Paleontology; Oceanography; Metallurgy; Materials science","score_opus":0.008800693332058535,"score_gpt":0.20353417218131548,"score_spread":0.19473347884925693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996727270","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938406,0.00014777904,0.00005707031,0.00015183377,0.0000034944067,0.000016480903,0.0012628312,0.000008602025,0.004511319],"genre_scores_gemma":[0.9961085,0.000107850006,0.00010432199,0.000032797765,0.0000016204939,0.000004666357,0.00040855748,0.0000046030027,0.0032270553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986875,0.000007297395,0.0000049296564,0.000022595164,0.00003402322,0.00006246929],"domain_scores_gemma":[0.99970907,0.000017966235,0.00003193586,0.000010797102,0.0001632952,0.00006687895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013340003,0.0002440978,0.0002893945,0.00090772397,0.0026060867,0.0010636516,0.00076161465,0.0004698891,0.0036507484],"category_scores_gemma":[0.00038889953,0.00021302298,0.00024380471,0.0022488153,0.0008875821,0.0003646335,0.0005324637,0.00036971015,0.00032908365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053914916,0.00013121887,0.9528279,0.00007858808,0.000121264035,0.0011339989,0.0032457819,0.003311553,0.009584951,0.0009372427,0.0029840695,0.025104392],"study_design_scores_gemma":[0.000008734587,0.000015279526,0.9958955,0.000009100811,0.000011330539,0.00005487361,0.0012034571,0.0007320878,0.0002371147,0.000030227913,0.0017931374,0.00000916113],"about_ca_topic_score_codex":0.9943857,"about_ca_topic_score_gemma":0.99822694,"teacher_disagreement_score":0.017652705,"about_ca_system_score_codex":0.017652705,"about_ca_system_score_gemma":0.008492825,"threshold_uncertainty_score":0.12807995},"labels":[],"label_agreement":null},{"id":"W2997187031","doi":"","title":"Source Rupture Models and Tsunami Simulations of Destructive October 28, 2012 Queen Charlotte Islands, British Columbia (Mw: 7.8) and September 16, 2015 Illapel, Chile (Mw: 8.3) Earthquakes","year":2016,"lang":"en","type":"article","venue":"EGUGA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Queen (butterfly); Seismology; Geology; Geography; Oceanography","score_opus":0.00914114655942844,"score_gpt":0.20064193784728893,"score_spread":0.1915007912878605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997187031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98348284,0.00020130374,0.0010608736,0.00055948197,0.000056843553,0.000027061486,0.0050226995,0.00037275074,0.009216133],"genre_scores_gemma":[0.9946786,0.00011114073,0.0005748763,0.000047345395,0.000014720616,0.000029622395,0.0026203461,0.0000730296,0.0018503823],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998647,0.00003165203,0.000012295817,0.000029693356,0.000021625567,0.000040104747],"domain_scores_gemma":[0.99879265,0.0005813154,0.00011488227,0.000074476666,0.00027957972,0.00015709974],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004285966,0.00074879464,0.0006766598,0.0012180071,0.0007364373,0.001245323,0.0020774098,0.0020840366,0.005148716],"category_scores_gemma":[0.002562913,0.00079595664,0.00057339115,0.0015167991,0.00060768897,0.0008238103,0.00054554775,0.0013446957,0.00056323817],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002536921,0.00015197165,0.010436769,0.000039705203,0.000080223086,0.00015429097,0.000104304054,0.98259914,0.0003746304,0.0012858979,0.0024600832,0.0020592122],"study_design_scores_gemma":[0.00009699361,0.000025989293,0.00514359,0.000010788945,0.000021204643,0.000015023959,0.00010401647,0.99365944,0.00014340469,0.00036666443,0.00039638337,0.000016400452],"about_ca_topic_score_codex":0.43899077,"about_ca_topic_score_gemma":0.36166325,"teacher_disagreement_score":0.5610092,"about_ca_system_score_codex":0.0038123818,"about_ca_system_score_gemma":0.0021449,"threshold_uncertainty_score":0.8728711},"labels":[],"label_agreement":null},{"id":"W2997229921","doi":"","title":"Geosphere - Cryosphere Interactions in the Saint Elias orogen, Alaska and Yukon (Invited)","year":2009,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cryosphere; SAINT; Geology; Earth science; Physical geography; Climatology; Geography; History; Sea ice","score_opus":0.017963732111293127,"score_gpt":0.23413134939080174,"score_spread":0.21616761727950862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997229921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.65461826,0.081791446,0.0011166264,0.11937667,0.035175838,0.00010874076,0.005582008,0.00013991861,0.102090426],"genre_scores_gemma":[0.81339264,0.03741435,0.00063785276,0.0071304515,0.007908656,0.00008028106,0.0013143648,0.000062856736,0.13205846],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99996257,0.000006095436,0.0000032336147,0.000008602898,0.0000055773526,0.000013880051],"domain_scores_gemma":[0.99986696,0.000043953394,0.000013140337,0.0000029924813,0.000036201378,0.000036682326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019706623,0.000146918,0.00013301529,0.00025628117,0.0009479355,0.00078614743,0.00019435801,0.00047394895,0.0058216513],"category_scores_gemma":[0.00050466147,0.00008513249,0.00014632757,0.0006644299,0.00022917653,0.00070258137,0.00075214915,0.00046490564,0.0005522836],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007534524,0.00007240164,0.23243071,0.0011911701,0.00021202615,0.002301272,0.02277781,0.0017349903,0.0058175204,0.0047137393,0.5428647,0.18513027],"study_design_scores_gemma":[0.000018259423,0.000051220515,0.52425086,0.00033720362,0.0001608032,0.00022346996,0.041225296,0.0004474818,0.0009088704,0.0014930484,0.43086207,0.00002146872],"about_ca_topic_score_codex":0.088389054,"about_ca_topic_score_gemma":0.30794898,"teacher_disagreement_score":0.91161096,"about_ca_system_score_codex":0.00063076953,"about_ca_system_score_gemma":0.0008424942,"threshold_uncertainty_score":0.17574912},"labels":[],"label_agreement":null},{"id":"W2997237258","doi":"10.1029/2019jb018739","title":"Three‐Dimensional Surface Displacements During the 2016 <i>M</i><sub><i>W</i></sub> 7.8 Kaikōura Earthquake (New Zealand) From Photogrammetry‐Derived Point Clouds","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Slip (aerodynamics); Seismology; Fault (geology); Geodesy; Surface rupture; Lidar; Earthquake rupture; Geometry; Remote sensing; Engineering","score_opus":0.031706971082110666,"score_gpt":0.27289218701218165,"score_spread":0.24118521593007097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997237258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9869942,0.000050372375,0.0008033772,0.000044188317,0.000016961156,0.00003991861,0.00986302,0.00016809425,0.0020198904],"genre_scores_gemma":[0.9804388,0.000111492554,0.0022639956,0.000015485137,0.000011542539,0.00006290625,0.01604742,0.00002769508,0.0010206058],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982953,0.00000451836,0.000011277758,0.00004667222,0.00007561855,0.00003237154],"domain_scores_gemma":[0.9997255,0.00001593429,0.00008065612,0.00002767791,0.00009910073,0.00005096664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013028985,0.0004976559,0.00035031402,0.0009967824,0.0003209974,0.00068705285,0.00036916442,0.0003921655,0.0018635261],"category_scores_gemma":[0.0005803284,0.0002858865,0.00049591565,0.00166488,0.0003217999,0.00051612686,0.0007274218,0.0003459436,0.0008120698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075266307,0.00029874837,0.77217054,0.00039903022,0.00031635835,0.0009810105,0.0022717395,0.04951611,0.060133256,0.00035409682,0.010240744,0.10256582],"study_design_scores_gemma":[0.000022284441,0.000043779408,0.9794194,0.00002483573,0.000029716597,0.00006903691,0.0004155408,0.016571032,0.0016338589,0.00004292003,0.0016890963,0.000038477705],"about_ca_topic_score_codex":0.1676022,"about_ca_topic_score_gemma":0.26914352,"teacher_disagreement_score":0.1676022,"about_ca_system_score_codex":0.0007723041,"about_ca_system_score_gemma":0.000719341,"threshold_uncertainty_score":0.33325326},"labels":[],"label_agreement":null},{"id":"W2997516851","doi":"10.1029/2019gl084787","title":"Assessing Energy Budget of Laboratory Fault Slip Using Rotary Shear Experiments and Micro‐Computed Tomography","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Science Foundation","keywords":"Energy budget; Shear (geology); Energy (signal processing); Tomography; Slip (aerodynamics); Seismology; Computed tomography; Geology; Fault (geology); Physics; Engineering; Aerospace engineering; Statistics; Optics; Petrology; Mathematics; Radiology; Medicine","score_opus":0.056453853587233344,"score_gpt":0.31053803959683957,"score_spread":0.25408418600960625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997516851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99801505,0.00006514385,0.0015399804,0.0000080948785,0.0000021244455,0.000008959103,0.00011714704,0.0000104767105,0.0002329136],"genre_scores_gemma":[0.99875486,0.000046832567,0.0009850273,0.0000055253313,0.0000015812384,0.000013873311,0.000084556435,0.0000034291927,0.0001043201],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99982435,0.000023708892,0.000017201328,0.00003600565,0.00006653681,0.00003229656],"domain_scores_gemma":[0.9997032,0.000085244996,0.00009847768,0.00003924186,0.000048150425,0.000025664753],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030981522,0.0002901379,0.00021209274,0.0003401588,0.00020021877,0.00024362787,0.00023078028,0.0002250577,0.0011055871],"category_scores_gemma":[0.00043721,0.00014622422,0.00015112665,0.0002773458,0.0004335879,0.00025799658,0.00023160405,0.00023011542,0.000083744024],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023104897,0.000067334884,0.012561735,0.000037836773,0.000019626352,0.00005901209,0.00003707601,0.0021859072,0.98247623,0.00010897714,0.000028935941,0.0021861189],"study_design_scores_gemma":[0.000030573443,0.0013703466,0.12219449,0.000009652636,0.000041781135,0.0001855807,0.00021514602,0.02534305,0.8499569,0.00013661123,0.0004927852,0.00002299737],"about_ca_topic_score_codex":0.0012485529,"about_ca_topic_score_gemma":0.0016727161,"teacher_disagreement_score":0.0012485529,"about_ca_system_score_codex":0.00020806295,"about_ca_system_score_gemma":0.00013811151,"threshold_uncertainty_score":0.0036985278},"labels":[],"label_agreement":null},{"id":"W2998315762","doi":"","title":"Deep Focus Earthquakes, Deep Slab Fluids, and Superdeep Diamonds","year":2019,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Deep-focus earthquake; Focus (optics); Slab; Seismology; Geophysics; Subduction; Tectonics; Physics","score_opus":0.010709407741638371,"score_gpt":0.2021786956736012,"score_spread":0.19146928793196283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998315762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935322,0.0003674607,0.00023496042,0.0003829472,0.000011661021,0.0000060566663,0.00039639306,0.000009239437,0.0050591235],"genre_scores_gemma":[0.99854773,0.00021340289,0.000091584254,0.000038845654,0.000018787792,0.0000019536426,0.00016892928,0.0000020583184,0.0009165551],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999298,0.000010838529,0.0000034951531,0.00001122911,0.000020059371,0.000024635476],"domain_scores_gemma":[0.99897987,0.00033738723,0.00033143067,0.000059821225,0.00012134524,0.0001701527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002386177,0.0001550684,0.00020162223,0.0007771798,0.00025623792,0.0005088756,0.00021176315,0.0002868467,0.003769424],"category_scores_gemma":[0.0015595186,0.00007367068,0.000079677644,0.0009767816,0.00039789567,0.00044701132,0.00075689895,0.00037060803,0.00013734285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008530764,0.00014191362,0.92791843,0.00008307048,0.00006937695,0.0009905245,0.0011530395,0.0014971143,0.0032104396,0.0047724,0.0030282834,0.056282446],"study_design_scores_gemma":[0.000012146689,0.00008398546,0.99479127,0.000011880427,0.000015014516,0.00015593396,0.0011207554,0.00043209447,0.00013049634,0.0021119018,0.0011297578,0.000004740513],"about_ca_topic_score_codex":0.006703381,"about_ca_topic_score_gemma":0.011304994,"teacher_disagreement_score":0.006703381,"about_ca_system_score_codex":0.00027170582,"about_ca_system_score_gemma":0.0002348123,"threshold_uncertainty_score":0.013328731},"labels":[],"label_agreement":null},{"id":"W2998401711","doi":"10.1130/ges02158.1","title":"Unusually deep earthquakes in the central Sierra Nevada (California, USA): Foundering ultramafic lithosphere?","year":2019,"lang":"en","type":"article","venue":"Geosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"U.S. Department of Energy; National Nuclear Security Administration; National Science Foundation","keywords":"Geology; Seismology; Lithosphere; Seismometer; Crust; Ultramafic rock; Induced seismicity; Stress field; Mafic; Paleontology; Tectonics","score_opus":0.011016951641005428,"score_gpt":0.20168086628251905,"score_spread":0.1906639146415136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998401711","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899584,0.00015120966,0.00008199493,0.000028797042,0.0000027464062,0.0000019725146,0.00018843006,0.000009882778,0.0005390655],"genre_scores_gemma":[0.9994795,0.00006485699,0.00011492729,0.0000066353473,0.000003417526,9.2265066e-7,0.00022654895,9.4900184e-7,0.00010226905],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995947,0.000004286401,0.0000026696443,0.000014482229,0.000011408437,0.000007741687],"domain_scores_gemma":[0.9998118,0.000016629188,0.00007861768,0.000013133374,0.00003318017,0.000046622816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009827683,0.000103801445,0.00010350039,0.0004065322,0.00020709216,0.00039267523,0.00021208747,0.00015331821,0.0004972687],"category_scores_gemma":[0.0003310794,0.00007158129,0.000053456963,0.00036193992,0.00014551153,0.00015886767,0.00022636054,0.000100196725,0.000057670346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025831148,0.000022440396,0.98847336,0.000013605739,0.000024166999,0.00014460014,0.00015925139,0.00094610633,0.0017712666,0.0000685431,0.00045693043,0.007893911],"study_design_scores_gemma":[0.000003899242,0.000011004387,0.9973207,0.000008475598,0.000007452384,0.00007134479,0.0003003218,0.0013247362,0.00013228311,0.000044653196,0.00077190564,0.0000032197554],"about_ca_topic_score_codex":0.079125315,"about_ca_topic_score_gemma":0.22839488,"teacher_disagreement_score":0.079125315,"about_ca_system_score_codex":0.00036933005,"about_ca_system_score_gemma":0.00022149726,"threshold_uncertainty_score":0.1573295},"labels":[],"label_agreement":null},{"id":"W2998474489","doi":"10.1029/2019jb018378","title":"A Block Model of Present‐Day Kinematics of Alaska and Western Canada","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; U.S. Geological Survey","keywords":"Geology; Seismology; Subduction; North American Plate; Forearc; Slab; Clockwise; Plate tectonics; Tectonics; Euler's rotation theorem; Pacific Plate; Block (permutation group theory); Geodesy; Paleontology; Rotation (mathematics); Geometry","score_opus":0.06236617944763835,"score_gpt":0.298615024653556,"score_spread":0.23624884520591766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998474489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7839274,0.00080731325,0.1304899,0.0010722524,0.00012518499,0.0001275798,0.0054736915,0.0005964922,0.07738014],"genre_scores_gemma":[0.96329135,0.00049465237,0.0065917424,0.00004185653,0.00001735134,0.000105476065,0.0010479331,0.0000693486,0.028340338],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992967,0.0000089997,0.0000029606367,0.000017424956,0.000018261824,0.000022677086],"domain_scores_gemma":[0.99986124,0.000022144828,0.000021913484,0.00000948165,0.000053693442,0.000031569445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016139077,0.00045216092,0.00039370806,0.0006096494,0.0011074644,0.0010356328,0.0014928529,0.0007036411,0.0054036314],"category_scores_gemma":[0.00054702885,0.00043377993,0.00045519546,0.0007311225,0.000793066,0.0006856975,0.00046301383,0.00046940765,0.00076843385],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023993882,0.000006700654,0.0029828853,0.000007210573,0.00001137063,0.000054844346,0.000066926295,0.98124665,0.00032879913,0.01254739,0.00067015464,0.0020530114],"study_design_scores_gemma":[0.000012748632,0.000006719415,0.0012639606,0.0000048453644,0.000008654692,0.0000118955495,0.000029275177,0.99475694,0.00004164331,0.0020593642,0.0017941312,0.00000985106],"about_ca_topic_score_codex":0.88267106,"about_ca_topic_score_gemma":0.6744054,"teacher_disagreement_score":0.11732894,"about_ca_system_score_codex":0.005317595,"about_ca_system_score_gemma":0.0059933686,"threshold_uncertainty_score":0.23603976},"labels":[],"label_agreement":null},{"id":"W2999110294","doi":"10.1785/0220190281","title":"Analog Seismogram Archives at the Earthquake Research Institute, the University of Tokyo","year":2020,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismogram; Seismometer; Seismology; Geology; Epicenter; Observatory","score_opus":0.14435805937036036,"score_gpt":0.3081838877183499,"score_spread":0.16382582834798956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999110294","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07811441,0.0052372133,0.008505435,0.00066747126,0.0010482041,0.00059818925,0.7748861,0.009565475,0.12137753],"genre_scores_gemma":[0.13453183,0.0076317163,0.019790335,0.00025659098,0.0010429743,0.0006889134,0.7242647,0.0014710356,0.11032196],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993986,0.0000477449,0.00012438567,0.000108380256,0.00028235026,0.000038511065],"domain_scores_gemma":[0.9961778,0.00020237891,0.0003829083,0.0008034879,0.0021782157,0.00025529327],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080273807,0.0005792825,0.0005249427,0.009530805,0.0004279526,0.0013966004,0.0009026586,0.00024618776,0.07767298],"category_scores_gemma":[0.0029371546,0.00028382032,0.00018660097,0.018749334,0.00019030787,0.00091421074,0.0011138746,0.0004973889,0.029905913],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061043596,0.00012681265,0.030975275,0.0014692221,0.000073439456,0.0007354361,0.0009929278,0.00075968204,0.0099511705,0.0023816442,0.5326713,0.41925266],"study_design_scores_gemma":[0.00010944553,0.00010376632,0.24446933,0.00014752668,0.000106522064,0.0005272393,0.0005719445,0.00095515413,0.0034117748,0.00071234175,0.7488135,0.000071453156],"about_ca_topic_score_codex":0.012830789,"about_ca_topic_score_gemma":0.014335878,"teacher_disagreement_score":0.07767298,"about_ca_system_score_codex":0.0005801846,"about_ca_system_score_gemma":0.0013974899,"threshold_uncertainty_score":0.25984204},"labels":[],"label_agreement":null},{"id":"W2999458141","doi":"10.1108/ijdrbe-08-2019-0052","title":"An update of proposed Sri Lanka warning system for east and west coast tsunamis","year":2019,"lang":"en","type":"article","venue":"International Journal of Disaster Resilience in the Built Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Seismology; Tide gauge; Subduction; Warning system; Geology; Tsunami earthquake; Indian ocean; Archipelago; Ridge; Buoy; Oceanography; Computer science; Telecommunications; Tectonics; Sea level","score_opus":0.01285151180759213,"score_gpt":0.23394142796890532,"score_spread":0.22108991616131318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999458141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47161582,0.018197743,0.24991415,0.03105727,0.004428882,0.006218261,0.04885797,0.022558216,0.14715175],"genre_scores_gemma":[0.802947,0.008074872,0.14397898,0.0013488095,0.00040670164,0.0014172678,0.025069792,0.0002744812,0.016482089],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99764806,0.00066760136,0.0006781825,0.00021562145,0.000582186,0.00020838027],"domain_scores_gemma":[0.99227774,0.00086222694,0.00073301484,0.000559864,0.0052150087,0.00035214034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00497199,0.00057069986,0.00050929317,0.0036392792,0.0006129182,0.003092197,0.0018674486,0.0007941933,0.0047470536],"category_scores_gemma":[0.010054537,0.0003673002,0.00052208547,0.0018558211,0.00033638263,0.0016463695,0.0015429761,0.0009997102,0.002049685],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006931942,0.00027198062,0.14522621,0.003267075,0.0003561543,0.0021140655,0.0036015108,0.02750709,0.010422391,0.012431884,0.10683887,0.6872697],"study_design_scores_gemma":[0.00025328522,0.0013311479,0.20076634,0.0030357956,0.0011525004,0.0027794987,0.009557945,0.1346995,0.01993979,0.0072199088,0.61856544,0.00069879857],"about_ca_topic_score_codex":0.02552377,"about_ca_topic_score_gemma":0.019629354,"teacher_disagreement_score":0.02552377,"about_ca_system_score_codex":0.0014702596,"about_ca_system_score_gemma":0.0040485216,"threshold_uncertainty_score":0.050750434},"labels":[],"label_agreement":null},{"id":"W2999735632","doi":"10.1785/0120190121","title":"Variability of ETAS Parameters in Global Subduction Zones and Applications to Mainshock–Aftershock Hazard Assessment","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Geology; Subduction; Seismology; Sequence (biology); Hazard; Seismic hazard; Tectonics","score_opus":0.02084056983113353,"score_gpt":0.24198396478778833,"score_spread":0.2211433949566548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999735632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98407584,0.00016303116,0.014184474,0.00003676142,0.0000056640815,0.000013115615,0.0008431517,0.00018420965,0.00049375446],"genre_scores_gemma":[0.9966539,0.000026600392,0.0025629674,0.000004089301,0.0000028830823,0.0000058144637,0.0006885101,0.000014283125,0.000040978568],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99976164,0.00006844791,0.00003412356,0.00007521018,0.000038880233,0.000021724103],"domain_scores_gemma":[0.9965724,0.0016299592,0.0008884011,0.00048801338,0.00031152938,0.000109783425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017071342,0.00047616218,0.00029422744,0.0016097226,0.00011602374,0.00070896704,0.00045104633,0.00046228533,0.0006127023],"category_scores_gemma":[0.005964763,0.00019410078,0.00048765325,0.001129089,0.00022820078,0.00094891695,0.0006293098,0.00033667602,0.00015627744],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029791406,0.00006746812,0.57197356,0.00008878316,0.00028631775,0.00013139183,0.00017604452,0.3876195,0.010284159,0.00068254076,0.00030809443,0.028084125],"study_design_scores_gemma":[0.000019553137,0.00007929587,0.35807383,0.000027212734,0.000051242245,0.00013684499,0.000195814,0.63324034,0.0056623984,0.0019514726,0.0005124667,0.00004954269],"about_ca_topic_score_codex":0.0034032965,"about_ca_topic_score_gemma":0.0020343242,"teacher_disagreement_score":0.0034032965,"about_ca_system_score_codex":0.00033091372,"about_ca_system_score_gemma":0.00020120971,"threshold_uncertainty_score":0.009028316},"labels":[],"label_agreement":null},{"id":"W3000153556","doi":"10.1029/2022jb024704","title":"Investigating the Effect of Mantle Flow and Viscosity Structure on Surface Velocities in Alaska Using 3‐D Geodynamic Models","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Plate tectonics; Subduction; Mantle (geology); Slab; Seismology; North American Plate; Tectonics; Geodesy; Geodynamics; Ocean surface topography; Lithosphere; Geophysics","score_opus":0.036832949049705216,"score_gpt":0.3026939215059327,"score_spread":0.26586097245622753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000153556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99090356,0.00006687444,0.0069278404,0.00007686827,0.000009666498,0.000009611838,0.00026299644,0.0001442013,0.0015982992],"genre_scores_gemma":[0.99783945,0.0000538298,0.0016709873,0.00000735704,0.0000020724763,0.000008544936,0.00012315749,0.000008278419,0.00028626894],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999378,0.00001532337,0.0000061983146,0.00001719555,0.000013514653,0.00001004613],"domain_scores_gemma":[0.9996766,0.00017315758,0.000047658767,0.000029287326,0.00004640639,0.00002697941],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028278015,0.0004150807,0.00025796657,0.00048053538,0.0004888123,0.00077886716,0.00042874145,0.00085528265,0.00087541225],"category_scores_gemma":[0.0011512822,0.0005037102,0.0006353153,0.00030870104,0.00041427842,0.0005600415,0.00044363207,0.000431505,0.00013594194],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003220621,0.000031535103,0.015161186,0.00000934187,0.00002335618,0.000038102276,0.00004947527,0.9807342,0.0018784115,0.00032219623,0.000047230846,0.0016726778],"study_design_scores_gemma":[0.000007482952,0.000016591319,0.0065265265,0.00000485638,0.000011166761,0.0000074786713,0.000024900392,0.99243563,0.000650712,0.0001747642,0.00012938319,0.000010348715],"about_ca_topic_score_codex":0.10713088,"about_ca_topic_score_gemma":0.051674563,"teacher_disagreement_score":0.10713088,"about_ca_system_score_codex":0.00093768706,"about_ca_system_score_gemma":0.00078841345,"threshold_uncertainty_score":0.2130146},"labels":[],"label_agreement":null},{"id":"W3000382179","doi":"10.1093/gji/ggz574","title":"The upper mantle beneath the South Atlantic Ocean, South America and Africa from waveform tomography with massive data sets","year":2020,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"European Regional Development Fund; Geological Survey of Ireland; Science Foundation Ireland; Centre of Excellence for Environmental Decisions, Australian Research Council","keywords":"Craton; Geology; Lithosphere; Crust; Mantle (geology); Seismology; Seismogram; Geophysics; Tectonics","score_opus":0.023001866735559505,"score_gpt":0.21037596527657249,"score_spread":0.18737409854101297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000382179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98398966,0.00011486001,0.011573152,0.00018209901,0.0000050362983,0.000014599526,0.002294839,0.00029619978,0.0015295964],"genre_scores_gemma":[0.9867649,0.00012248191,0.0102464575,0.000016261514,0.0000053440585,0.0000148710615,0.0024883454,0.000038202885,0.0003030818],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999639,0.0000053902513,0.0000030889855,0.000010655816,0.0000097714565,0.000007224657],"domain_scores_gemma":[0.99987614,0.000027844255,0.000022857535,0.000028070133,0.000033480534,0.0000115981165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010313978,0.00030851684,0.00013214022,0.00085327536,0.00015654588,0.00054027466,0.00031837053,0.0002658313,0.0011772813],"category_scores_gemma":[0.0006649113,0.0002144348,0.00037867491,0.0010911714,0.00011528242,0.0003818583,0.00041735973,0.00019095713,0.00017186561],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020581491,0.00005943219,0.23990479,0.00013456242,0.00024538787,0.00080584985,0.00041852775,0.53345454,0.05225018,0.0023092995,0.0023555718,0.16785607],"study_design_scores_gemma":[0.000029277635,0.000024590088,0.13691977,0.000025446288,0.000058293535,0.00017935512,0.00030390202,0.85341895,0.003622142,0.0021815624,0.003214388,0.000022369382],"about_ca_topic_score_codex":0.028523788,"about_ca_topic_score_gemma":0.040534608,"teacher_disagreement_score":0.028523788,"about_ca_system_score_codex":0.00031474538,"about_ca_system_score_gemma":0.00041776572,"threshold_uncertainty_score":0.056715548},"labels":[],"label_agreement":null},{"id":"W3000465781","doi":"","title":"Observations of the 2011 Tohoku Tsunami on the Coast of British Columbia","year":2014,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Geography; Oceanography; Meteorology; Climatology","score_opus":0.024565953035563935,"score_gpt":0.1824978872716239,"score_spread":0.15793193423605995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000465781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924298,0.00014060049,0.00005641943,0.00014596745,0.0000104811215,0.000018769451,0.0022850381,0.000015930398,0.0048969365],"genre_scores_gemma":[0.9929584,0.00028805865,0.00016084258,0.000072850075,0.0000064726596,0.000020062143,0.0022237245,0.00000814153,0.0042614434],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998342,0.000009526494,0.000009268278,0.0000253089,0.00005073638,0.00007088343],"domain_scores_gemma":[0.99920976,0.000050426977,0.000099625504,0.00003406305,0.00046905875,0.00013703734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011884835,0.0002898158,0.00022479413,0.0015305016,0.0018939576,0.00079479173,0.0004813734,0.000561925,0.0018373942],"category_scores_gemma":[0.0010068633,0.00020463858,0.00010770433,0.0028910749,0.00040231508,0.0002838279,0.00078664994,0.00050663255,0.00042420367],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000281696,0.00011984346,0.9442711,0.00012796129,0.00007927223,0.00083501614,0.004049113,0.002007926,0.0112286,0.00024190123,0.009504294,0.027253317],"study_design_scores_gemma":[0.0000069793564,0.0000075160665,0.99423367,0.000021129768,0.0000108004315,0.000033921486,0.0016840828,0.00055800413,0.00023567924,0.000015515552,0.003182028,0.000010640147],"about_ca_topic_score_codex":0.98484147,"about_ca_topic_score_gemma":0.9954425,"teacher_disagreement_score":0.015158534,"about_ca_system_score_codex":0.0069469856,"about_ca_system_score_gemma":0.0062364787,"threshold_uncertainty_score":0.05040413},"labels":[],"label_agreement":null},{"id":"W3000587487","doi":"","title":"Seismic Constraints on the Structure and Evolution of the Coast Plutonic Complex in Western British Columbia","year":2007,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pluton; Geology; Seismology","score_opus":0.013450774172492436,"score_gpt":0.2006597880755462,"score_spread":0.18720901390305378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000587487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947566,0.00014143207,0.00005568616,0.00014197899,0.000001710287,0.0000056023846,0.00033350193,0.0000071902705,0.0045563686],"genre_scores_gemma":[0.9984504,0.000091841735,0.000086229535,0.000027172193,8.932765e-7,0.0000043563496,0.00027171042,0.000005597591,0.0010616959],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970835,0.000029989784,0.0000189709,0.000053374035,0.00005371775,0.00013557238],"domain_scores_gemma":[0.9981445,0.000274213,0.00035589165,0.00008452798,0.00079717743,0.00034363495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031739165,0.00022195687,0.00032839325,0.003172879,0.0029860327,0.0020797579,0.0009121274,0.0004489995,0.004968806],"category_scores_gemma":[0.0029816336,0.00034008018,0.0001045721,0.004936231,0.001320479,0.00042906753,0.0012489199,0.0006020812,0.00037808655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017089667,0.000043576176,0.9579774,0.00005264277,0.000061184786,0.00051462866,0.0053162067,0.0025715278,0.0057459534,0.0017749262,0.0015808909,0.024190186],"study_design_scores_gemma":[0.0000056760555,0.0000043667123,0.99506193,0.000022626322,0.000008788019,0.00003577872,0.0022624335,0.0007877305,0.000114075796,0.00009779191,0.0015915454,0.000007182347],"about_ca_topic_score_codex":0.98203605,"about_ca_topic_score_gemma":0.9954614,"teacher_disagreement_score":0.017963946,"about_ca_system_score_codex":0.013532353,"about_ca_system_score_gemma":0.009691089,"threshold_uncertainty_score":0.098184586},"labels":[],"label_agreement":null},{"id":"W3000709539","doi":"10.1016/j.enggeo.2020.105476","title":"Anomalous co-seismic surface effects produced by the 2014 Mw 6.2 Ludian earthquake, Yunnan, China: An example of complex faulting related to Riedel shear structures","year":2020,"lang":"en","type":"article","venue":"Engineering Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"State Key Laboratory of Geohazard Prevention and Geoenvironment Protection; Chengdu University of Technology; Ministry of Science and Technology of the People's Republic of China","keywords":"Sinistral and dextral; Geology; Seismology; Echelon formation; Aftershock; Shear (geology); Shear zone; Epicenter; Strike-slip tectonics; Intraplate earthquake; Fault (geology); Tectonics; Petrology","score_opus":0.016066798039828255,"score_gpt":0.21398121234732015,"score_spread":0.1979144143074919,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000709539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926347,0.000025660658,0.00006118343,0.000028480088,0.000004695395,0.0000021264477,0.00015309088,0.000009727637,0.00045153307],"genre_scores_gemma":[0.9994956,0.000026148247,0.00007439707,0.000006855913,0.000005711861,0.0000012040622,0.00022143478,0.0000019431532,0.00016663874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991155,0.0000064767905,0.000007662752,0.000021394364,0.000021167063,0.00003168583],"domain_scores_gemma":[0.9997992,0.000016350465,0.0000710984,0.000023713135,0.000045218978,0.000044384095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015466113,0.00024179142,0.00020006039,0.0010303805,0.0004391621,0.000371843,0.00032055427,0.00036153785,0.00062370417],"category_scores_gemma":[0.00035809918,0.00012678115,0.0001834801,0.0013083458,0.00036144996,0.00021881108,0.0004959962,0.00021131599,0.00008515514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027297353,0.00012148249,0.94478136,0.000052977106,0.00015311243,0.0026478996,0.00088895485,0.0033463696,0.033115923,0.00055070774,0.0012737747,0.012794372],"study_design_scores_gemma":[0.000003853587,0.000017285558,0.99736845,0.0000019500853,0.000019311348,0.00011010189,0.00026178954,0.0014322601,0.00039071805,0.000047534948,0.00034177018,0.0000049086425],"about_ca_topic_score_codex":0.039570797,"about_ca_topic_score_gemma":0.087236375,"teacher_disagreement_score":0.039570797,"about_ca_system_score_codex":0.0005515731,"about_ca_system_score_gemma":0.00068827113,"threshold_uncertainty_score":0.07868093},"labels":[],"label_agreement":null},{"id":"W3000795619","doi":"10.1038/s41467-020-14447-1","title":"Earthquake slip surfaces identified by biomarker thermal maturity within the 2011 Tohoku-Oki earthquake fault zone","year":2020,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Consortium for Ocean Leadership; National Science Foundation","keywords":"Seismology; Geology; Subduction; Trench; Slip (aerodynamics); Seismic hazard; Induced seismicity; Episodic tremor and slip; Seismic gap; Tectonics","score_opus":0.03201803915526785,"score_gpt":0.2560518997241963,"score_spread":0.22403386056892843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000795619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99957603,0.000020351645,0.00006492718,0.0000051642105,8.153251e-7,0.0000019705399,0.00012957548,0.0000037249486,0.0001974208],"genre_scores_gemma":[0.99967587,0.000013745023,0.00009833553,0.0000029556006,8.88584e-7,0.0000026894245,0.00013912105,6.936507e-7,0.00006563546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993396,0.0000042023407,0.000008372159,0.000017260465,0.000012260941,0.000023965635],"domain_scores_gemma":[0.9995902,0.000026487885,0.0002108264,0.000018979534,0.00006752736,0.00008595902],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001101405,0.00023603474,0.00020262883,0.0014606022,0.00025560425,0.0005067649,0.000121155404,0.00024458376,0.000745518],"category_scores_gemma":[0.0004940467,0.00012209167,0.00010140399,0.0010675412,0.00021279116,0.00038246013,0.0005485305,0.00012853315,0.00014186339],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007543448,0.000019005227,0.98278886,0.000019757521,0.000017354449,0.00007368908,0.00030958268,0.00027015802,0.012320298,0.000029453393,0.00008024432,0.0039962213],"study_design_scores_gemma":[0.0000010291211,0.000016975488,0.99878937,0.0000020799387,0.000005723572,0.000028719296,0.0003233137,0.00031992083,0.00044046965,0.000009576071,0.000060351675,0.0000024948506],"about_ca_topic_score_codex":0.0055817617,"about_ca_topic_score_gemma":0.013793457,"teacher_disagreement_score":0.0055817617,"about_ca_system_score_codex":0.00018591226,"about_ca_system_score_gemma":0.00014350993,"threshold_uncertainty_score":0.011098564},"labels":[],"label_agreement":null},{"id":"W3001031603","doi":"","title":"Numerical modeling of dynamically triggered shallow slow slip events in New Zealand by the 2016 M w 7.8 Kaikoura earthquake","year":2018,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Slip (aerodynamics); Seismology; Geology; Geodesy; Engineering; Aerospace engineering","score_opus":0.016005995895797546,"score_gpt":0.22387527855939804,"score_spread":0.2078692826636005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3001031603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652773,0.000045511933,0.00035459944,0.00020168303,0.000023054932,0.000012207236,0.0003097129,0.0000203219,0.0025051148],"genre_scores_gemma":[0.99903166,0.000041843843,0.00015909321,0.0000115215635,0.000004368478,0.000008065086,0.00014446299,0.00000836119,0.0005906359],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999045,0.000012714369,0.000008565821,0.00002509231,0.000014205414,0.000034869132],"domain_scores_gemma":[0.9996057,0.0001091465,0.00008071409,0.00001984722,0.000094933814,0.000089722664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024327693,0.00054419844,0.0004549016,0.0004682553,0.0007237735,0.0011927793,0.0012711418,0.001377406,0.0028646977],"category_scores_gemma":[0.0018749278,0.000667063,0.00059116184,0.00046386028,0.0011505362,0.0010227828,0.0007840826,0.0009850721,0.00022245261],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040191464,0.00020862493,0.051472496,0.000045185996,0.00008087165,0.000520336,0.00025960823,0.93945193,0.0024180545,0.0013016192,0.00096067006,0.0028785835],"study_design_scores_gemma":[0.000111085785,0.000085560925,0.03404933,0.000013988924,0.000045876408,0.00003364228,0.00031729828,0.9643408,0.0002528748,0.00030255943,0.00041262788,0.000034294822],"about_ca_topic_score_codex":0.489033,"about_ca_topic_score_gemma":0.35539317,"teacher_disagreement_score":0.489033,"about_ca_system_score_codex":0.0030933393,"about_ca_system_score_gemma":0.0020066127,"threshold_uncertainty_score":0.97237307},"labels":[],"label_agreement":null},{"id":"W3001985681","doi":"","title":"A tsunami deposit from Vancouver Island, Canada ― Geological evidence for the penultimate great Cascadia earthquake?","year":2017,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Archaeology; History","score_opus":0.046176505315032625,"score_gpt":0.25369978407945804,"score_spread":0.20752327876442542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3001985681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9828418,0.00069115905,0.000048192618,0.00070738414,0.000025951027,0.000018403753,0.0022791072,0.000009693307,0.013378327],"genre_scores_gemma":[0.9909242,0.00060357695,0.0001104585,0.00010386022,0.000008768594,0.0000041304133,0.0012357773,0.0000058109567,0.007003479],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984455,0.000006422011,0.000008648622,0.0000257923,0.000045198998,0.00006932744],"domain_scores_gemma":[0.9992605,0.000032267206,0.00007614451,0.000029657731,0.00043003255,0.0001714744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017236845,0.00022136468,0.00020174301,0.0015022347,0.0035837777,0.0016867797,0.0007539137,0.000511449,0.0050421953],"category_scores_gemma":[0.00081419904,0.0002549651,0.00010475294,0.0042795087,0.00095443515,0.00041488683,0.0007008597,0.00055481034,0.00057584204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024267532,0.00006304037,0.92718,0.00014769482,0.00006443049,0.0023699554,0.007837006,0.00030840276,0.0061678113,0.001536323,0.008763469,0.045319233],"study_design_scores_gemma":[0.000006821269,0.000010175726,0.97959167,0.000049819995,0.00001558176,0.00019123107,0.007160197,0.00011429747,0.00022093211,0.000074799085,0.012553685,0.000010778358],"about_ca_topic_score_codex":0.9918104,"about_ca_topic_score_gemma":0.99804914,"teacher_disagreement_score":0.011364001,"about_ca_system_score_codex":0.011364001,"about_ca_system_score_gemma":0.017176628,"threshold_uncertainty_score":0.08245194},"labels":[],"label_agreement":null},{"id":"W3002224910","doi":"10.23919/oceans40490.2019.8962553","title":"Northern Cascadia Subduction Zone Observatory (NCSZO): an interdisciplinary research initiative to assess tsunami and earthquake hazard from the Cascadia megathrust","year":2019,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society; Geoscience BC; Natural Resources Canada; North Pacific Marine Science Organization; University of Calgary; University of Victoria","funders":"","keywords":"Subduction; Geology; Seismology; Seafloor spreading; Observatory; Plate tectonics; Submarine pipeline; Trench; Oceanography; Tectonics","score_opus":0.10731396276491031,"score_gpt":0.32918918546074527,"score_spread":0.22187522269583496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002224910","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9062833,0.00067765283,0.0049847406,0.0010878049,0.00008758718,0.0004394714,0.05075387,0.0009793479,0.0347061],"genre_scores_gemma":[0.95117724,0.00048472872,0.011512059,0.00015359516,0.000020299121,0.00015846187,0.026096687,0.000078214085,0.010318748],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99965537,0.000036934263,0.000013665313,0.00006821387,0.00016412935,0.000061692605],"domain_scores_gemma":[0.9981852,0.00007616616,0.0002157719,0.00012528477,0.0009238691,0.00047377378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006832852,0.00044182723,0.00023755193,0.0013853506,0.0008949937,0.0005449875,0.00043809295,0.00020270575,0.0019087847],"category_scores_gemma":[0.0010321308,0.00015034417,0.00017171705,0.0014993558,0.0002699348,0.0003717324,0.0010156522,0.000399223,0.00033945433],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000168941,0.00006649938,0.948119,0.00011349574,0.00010014082,0.0001216747,0.00080346904,0.0015936925,0.008434178,0.00034842108,0.0115867825,0.028543625],"study_design_scores_gemma":[0.000030065188,0.00004590589,0.9837018,0.000022146598,0.000023084473,0.000031432715,0.0007427484,0.0016016924,0.0010814425,0.000119633216,0.012587755,0.000012296605],"about_ca_topic_score_codex":0.74726486,"about_ca_topic_score_gemma":0.90204304,"teacher_disagreement_score":0.74726486,"about_ca_system_score_codex":0.0034294834,"about_ca_system_score_gemma":0.009044325,"threshold_uncertainty_score":0.50844705},"labels":[],"label_agreement":null},{"id":"W3002239596","doi":"10.1093/gji/ggaa038","title":"Clustering characteristics of gas-extraction induced seismicity in the Groningen gas field","year":2020,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"DSM (Canada)","funders":"","keywords":"Induced seismicity; Aftershock; Seismology; Geology; Magnitude (astronomy); Seismic hazard; Physics","score_opus":0.030086127826546644,"score_gpt":0.25462436461644844,"score_spread":0.22453823678990179,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002239596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962276,0.00009206422,0.0006467114,0.000013296859,0.000003852488,0.000017034326,0.0015373381,0.000028831124,0.001433364],"genre_scores_gemma":[0.9964736,0.00007851393,0.0003952756,0.0000025346706,0.000004502889,0.000011374501,0.0025610207,0.000008233381,0.00046492217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998797,0.000013804924,0.000011829235,0.00003674417,0.000033146942,0.000024811661],"domain_scores_gemma":[0.99945515,0.00012311657,0.00022876529,0.000036158595,0.00010435611,0.00005246029],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000117345444,0.00014526893,0.00019560025,0.0016925709,0.00013348021,0.0004679793,0.00019284121,0.00015085841,0.0017343434],"category_scores_gemma":[0.0008853931,0.000075914104,0.00013164847,0.00243979,0.00022494594,0.00018831437,0.00028369718,0.00009424452,0.0003029012],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000442793,0.000047145615,0.9281067,0.0001255637,0.00018184983,0.0010915342,0.0013207525,0.016520763,0.014830572,0.0010037612,0.0021124715,0.034216035],"study_design_scores_gemma":[0.0000036831932,0.000029094348,0.99168515,0.0000076571605,0.000013186412,0.00015841582,0.00050042913,0.0057354,0.00057423336,0.0001343491,0.001148968,0.00000947238],"about_ca_topic_score_codex":0.024760082,"about_ca_topic_score_gemma":0.028656896,"teacher_disagreement_score":0.024760082,"about_ca_system_score_codex":0.0003581731,"about_ca_system_score_gemma":0.00026000568,"threshold_uncertainty_score":0.049231887},"labels":[],"label_agreement":null},{"id":"W3002289940","doi":"10.1126/sciadv.aay5174","title":"Seismic evidence for megathrust fault-valve behavior during episodic tremor and slip","year":2020,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Ottawa","funders":"","keywords":"Slip (aerodynamics); Seismology; Geology; Fault (geology); Physical medicine and rehabilitation; Medicine; Forensic engineering; Engineering; Aerospace engineering","score_opus":0.04874359349128289,"score_gpt":0.2940986350557253,"score_spread":0.24535504156444243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002289940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99940634,0.000027896192,0.00009786814,0.0000072399293,8.43388e-7,0.0000013067908,0.00007740707,0.0000097020375,0.00037145813],"genre_scores_gemma":[0.99969316,0.000021497155,0.00006364029,0.000004137716,0.0000015927099,0.0000014469309,0.00013276924,0.0000016003454,0.000080256985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999013,0.000010356686,0.000010321821,0.000023106191,0.000030572628,0.000024296947],"domain_scores_gemma":[0.99939823,0.00008135004,0.00025912575,0.000051901025,0.00008729899,0.00012204776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001764688,0.00013672689,0.00015595916,0.0007956283,0.00017155192,0.0002503051,0.00021431441,0.0002701902,0.00089189934],"category_scores_gemma":[0.0007940128,0.00016237634,0.00010296948,0.00055419933,0.00042434566,0.00019686247,0.00035093725,0.00014001166,0.0001539286],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036534443,0.000059116093,0.79449797,0.00006923272,0.000034355508,0.0005482788,0.0014869059,0.0004161063,0.19236644,0.0001904384,0.000140298,0.009825636],"study_design_scores_gemma":[0.0000035383173,0.00003431488,0.9983188,0.0000021592612,0.000003822011,0.00008409187,0.00008263378,0.00022900042,0.0011636278,0.000017075212,0.000058962956,0.0000019962401],"about_ca_topic_score_codex":0.0037778786,"about_ca_topic_score_gemma":0.006443305,"teacher_disagreement_score":0.0037778786,"about_ca_system_score_codex":0.00019247069,"about_ca_system_score_gemma":0.00011891751,"threshold_uncertainty_score":0.0075117946},"labels":[],"label_agreement":null},{"id":"W3002389389","doi":"10.1785/0220190241","title":"Graphics Processing Unit-Based Match and Locate (GPU-M&amp;L): An Improved Match and Locate Method and Its Application","year":2020,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Graphics processing unit; Microearthquake; General-purpose computing on graphics processing units; Computer science; Graphics; Computation; Seismology; Geology; Parallel computing; Computational science; Computer graphics (images); Algorithm; Induced seismicity","score_opus":0.14128117169065263,"score_gpt":0.349584627853702,"score_spread":0.20830345616304935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002389389","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.037809245,0.0006881275,0.934248,0.00039078528,0.00027671584,0.0001332436,0.00038713415,0.022693446,0.0033733177],"genre_scores_gemma":[0.22609173,0.00037567364,0.7639545,0.00033066593,0.00008909183,0.00020213617,0.0011672282,0.0014616466,0.0063273096],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992322,0.00008869876,0.00005806144,0.00017130167,0.00036354183,0.000086267915],"domain_scores_gemma":[0.99923015,0.000122001504,0.00006392559,0.00018742157,0.00030641851,0.00009004453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005342771,0.0012647797,0.0010918067,0.0017099947,0.0006668803,0.0011427021,0.0023304217,0.0009890721,0.0067394082],"category_scores_gemma":[0.0021809381,0.00060830027,0.0010747158,0.0020291787,0.00045995062,0.0014770229,0.0018469723,0.00110165,0.0021643036],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067089987,0.0001919204,0.0077698673,0.00028404332,0.00016388291,0.0005839233,0.00024570178,0.061278246,0.04694494,0.007586781,0.034333717,0.8399461],"study_design_scores_gemma":[0.00011878923,0.00009419396,0.0016475249,0.00001454543,0.000039253457,0.00024005077,0.00006886265,0.9568608,0.019690232,0.0024735888,0.01870109,0.00005106664],"about_ca_topic_score_codex":0.00683366,"about_ca_topic_score_gemma":0.0062614675,"teacher_disagreement_score":0.00683366,"about_ca_system_score_codex":0.0005596029,"about_ca_system_score_gemma":0.0013944574,"threshold_uncertainty_score":0.022545576},"labels":[],"label_agreement":null},{"id":"W3002396671","doi":"10.5194/se-2019-191","title":"An MCMC Bayesian full moment tensor inversion constrained by first-motion polarities and double couple percent","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; University of Tehran; International Institute of Earthquake Engineering and Seismology; Eidgenössische Technische Hochschule Zürich","keywords":"Markov chain Monte Carlo; Bayesian probability; Algorithm; Monte Carlo method; Moment (physics); Moment tensor; Mathematics; Covariance matrix; Covariance; Second moment of area; Computer science; Statistics; Physics; Geometry; Magnitude (astronomy)","score_opus":0.017246393918763366,"score_gpt":0.20274113703655033,"score_spread":0.18549474311778696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3002396671","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.029619452,0.000113770366,0.9659205,0.00018584965,0.000046189074,0.00008505564,0.0005086071,0.0012693448,0.0022513517],"genre_scores_gemma":[0.38665226,0.00009759513,0.6069804,0.00020406945,0.00006638111,0.00027085986,0.0018936162,0.0004266809,0.0034082425],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99952054,0.00016671601,0.00002512692,0.00009570893,0.00013668912,0.00005521929],"domain_scores_gemma":[0.9985921,0.0006635016,0.0001454469,0.00022002349,0.0003000658,0.000078785284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011599223,0.00063846994,0.00082150754,0.0009750206,0.00085793866,0.00087193627,0.0013665986,0.00091744895,0.0049299155],"category_scores_gemma":[0.005960662,0.00089415035,0.0006017513,0.0011263309,0.0006162634,0.00086398236,0.0010900305,0.0011475912,0.0010746799],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004313927,0.00015452965,0.008144247,0.00016106528,0.00023131087,0.00022164968,0.00018467424,0.701966,0.014872545,0.03914766,0.007386064,0.22709899],"study_design_scores_gemma":[0.000022970895,0.0000073951765,0.0004300915,0.000006505807,0.000007959346,0.000020176041,0.0000047723406,0.9944342,0.000832482,0.0036264702,0.0005944371,0.000012552943],"about_ca_topic_score_codex":0.019676851,"about_ca_topic_score_gemma":0.020387787,"teacher_disagreement_score":0.019676851,"about_ca_system_score_codex":0.0006943961,"about_ca_system_score_gemma":0.003156046,"threshold_uncertainty_score":0.039124668},"labels":[],"label_agreement":null},{"id":"W3003365364","doi":"10.1785/0220190248","title":"The Community Code Verification Exercise for Simulating Sequences of Earthquakes and Aseismic Slip (SEAS)","year":2020,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Slip (aerodynamics); Geology; Seismology; Earthquake rupture; Homogeneous; Nucleation; Induced seismicity; Fault (geology); Statistical physics; Physics","score_opus":0.17028437022169568,"score_gpt":0.3411045388718586,"score_spread":0.17082016865016292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3003365364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9009359,0.0001247905,0.06977315,0.00048864254,0.00014812611,0.00027479412,0.003116126,0.007921077,0.017217377],"genre_scores_gemma":[0.93115914,0.000035208006,0.06396409,0.000100591016,0.000016566593,0.00020154488,0.0023505709,0.00081623584,0.0013560893],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991972,0.00030330717,0.00005574112,0.000102783924,0.0002416836,0.00009925147],"domain_scores_gemma":[0.9954739,0.0022894412,0.00024837657,0.00064707646,0.0011284031,0.00021271229],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019747692,0.00076304836,0.0004896937,0.00043494615,0.00047379604,0.00044460007,0.0021551833,0.0009852655,0.0041201515],"category_scores_gemma":[0.007166988,0.00028104146,0.0005196864,0.00035541406,0.0005686946,0.00061419146,0.0011299736,0.001030541,0.00046973754],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008632403,0.0008062238,0.01721629,0.00031297005,0.000096698655,0.0004534827,0.00030457557,0.9104068,0.012457867,0.00853021,0.010358444,0.03819307],"study_design_scores_gemma":[0.00012947641,0.000114992545,0.0010582724,0.000015502468,0.000006318369,0.000019214836,0.00003632584,0.99179345,0.0044624405,0.00066302164,0.0016900231,0.000011020923],"about_ca_topic_score_codex":0.011678988,"about_ca_topic_score_gemma":0.011256437,"teacher_disagreement_score":0.011678988,"about_ca_system_score_codex":0.00065420073,"about_ca_system_score_gemma":0.0014208381,"threshold_uncertainty_score":0.02322203},"labels":[],"label_agreement":null},{"id":"W3004416985","doi":"10.1016/j.gete.2020.100183","title":"Pore pressure pulse migration in microcracked andesite recorded with fibre optic sensors","year":2020,"lang":"en","type":"article","venue":"Geomechanics for Energy and the Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministère de l’Europe et des Affaires étrangères; Ministère de l'Enseignement supérieur, de la Recherche et de l'Innovation; Agence de l'Environnement et de la Maîtrise de l'Energie; Deutscher Akademischer Austauschdienst; Ministère de l'Europe et des Affaires Étrangères; Providence Health Care","keywords":"Pore water pressure; Permeability (electromagnetism); Porosity; Materials science; Composite material; Hydrostatic pressure; Andesite; Overburden pressure; Stress (linguistics); Hydrostatic equilibrium; Geotechnical engineering; Geology; Chemistry; Mechanics","score_opus":0.007854045674373672,"score_gpt":0.15933286793375487,"score_spread":0.1514788222593812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3004416985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99828917,0.00004724622,0.00087530224,0.00001956986,0.000010135161,0.0000046292043,0.00019322756,0.000041621897,0.00051911577],"genre_scores_gemma":[0.9981768,0.00004998869,0.000964782,0.000009301115,0.0000078406565,0.0000054517436,0.00010004773,0.000009008847,0.00067674764],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99987125,0.0000056791787,0.0000041082612,0.000032984546,0.000059904534,0.000026039923],"domain_scores_gemma":[0.9997241,0.000071054434,0.00006793031,0.00001714546,0.000081113125,0.000038628787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009160723,0.00013103492,0.00015314113,0.0004826484,0.00023547259,0.00033673042,0.00028184563,0.00037319836,0.0016717758],"category_scores_gemma":[0.00043439315,0.00014099047,0.000099272875,0.00049227715,0.00045368925,0.00047019895,0.00019451152,0.00037939014,0.00015535759],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004043178,0.000048269354,0.008006991,0.00004372483,0.000009753388,0.00016988415,0.00027305304,0.0005428519,0.9828205,0.000090550886,0.00014141778,0.007448741],"study_design_scores_gemma":[0.000028345787,0.00043601252,0.4170202,0.000019106768,0.000039692783,0.00050035346,0.0005545495,0.01651359,0.56302714,0.000100523306,0.0017094479,0.000051084015],"about_ca_topic_score_codex":0.0042355596,"about_ca_topic_score_gemma":0.0063610384,"teacher_disagreement_score":0.0042355596,"about_ca_system_score_codex":0.0002840469,"about_ca_system_score_gemma":0.00020513986,"threshold_uncertainty_score":0.008421838},"labels":[],"label_agreement":null},{"id":"W3005438168","doi":"10.1029/2019jb018888","title":"Frictional Strengths of Subduction Thrust Rocks in the Region of Shallow Slow Earthquakes","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Japan Society for the Promotion of Science; European GNSS Agency; Natural Sciences and Engineering Research Council of Canada; National Stroke Foundation; McGill University","keywords":"Geology; Subduction; Basalt; Lithology; Seismology; Matrix (chemical analysis); Petrology; Tectonics; Materials science; Composite material","score_opus":0.06670261828134365,"score_gpt":0.31582380928264636,"score_spread":0.2491211910013027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005438168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998535,0.000018767329,0.000020865926,0.0000010877333,1.4978696e-7,6.644997e-7,0.00002581133,0.0000014313401,0.00007773006],"genre_scores_gemma":[0.9999335,0.000008286358,0.000012531014,3.482099e-7,2.3585567e-7,4.0667993e-7,0.000026801372,4.3226575e-7,0.000017564134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993086,0.000006501174,0.000009043364,0.000022551016,0.000012261242,0.000018690671],"domain_scores_gemma":[0.9997788,0.000043957403,0.00008054589,0.000016899381,0.00003474492,0.000044920453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012470271,0.00017559885,0.00023526185,0.0014607148,0.00018781533,0.00045640706,0.00014981712,0.0001856301,0.00055617845],"category_scores_gemma":[0.0005252503,0.00019203112,0.00013677565,0.0004569534,0.0002502292,0.00022873358,0.00029125033,0.00007819816,0.000097157455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041492056,0.00004685511,0.7693328,0.00006255036,0.00012249967,0.0004922452,0.0005197953,0.004366684,0.21917823,0.00015389507,0.000059594393,0.0052498765],"study_design_scores_gemma":[0.0000029875468,0.000029724806,0.9945523,0.0000022016525,0.000012351594,0.00007279769,0.000104390914,0.001875303,0.003266067,0.000020230193,0.00005838903,0.0000033956585],"about_ca_topic_score_codex":0.0038255232,"about_ca_topic_score_gemma":0.0036269356,"teacher_disagreement_score":0.0038255232,"about_ca_system_score_codex":0.00028656842,"about_ca_system_score_gemma":0.000089764464,"threshold_uncertainty_score":0.0076065063},"labels":[],"label_agreement":null},{"id":"W3005560164","doi":"10.1029/2019jb018853","title":"Three dimensional Gravity Local Inversion Across the Area Struck by the 2016–2017 Seismic Events in Central Italy","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Density contrast; Inversion (geology); Seismology; Basement; Residual; Sequence (biology); Evaporite; Geophysics; Paleontology; Tectonics; Sedimentary rock","score_opus":0.04908998779821804,"score_gpt":0.3075318829168888,"score_spread":0.2584418951186708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005560164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968227,0.00004420851,0.0010828226,0.000051667346,0.000008038639,0.0000045759425,0.0010388981,0.00018014904,0.00076693343],"genre_scores_gemma":[0.99771464,0.000020813308,0.0008987539,0.0000055644273,0.0000067814044,0.000003203003,0.0011767372,0.000012960922,0.0001605783],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999325,0.000008361455,0.0000044929006,0.000023524464,0.000010202782,0.000020745741],"domain_scores_gemma":[0.9998721,0.000024576915,0.000028745053,0.000020512896,0.00003440598,0.000019608482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015045244,0.00036458034,0.0002226249,0.00089199364,0.00016862091,0.0004293351,0.00040692673,0.00031035033,0.0012047879],"category_scores_gemma":[0.0005238164,0.00020543308,0.0005065316,0.00085328025,0.00022843131,0.00019181409,0.00036931562,0.0002289101,0.00029544174],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075015606,0.0002911303,0.41464278,0.000131329,0.0002990487,0.00069518207,0.00045014793,0.50501454,0.022405347,0.00084057736,0.0022342694,0.052245475],"study_design_scores_gemma":[0.00007378583,0.00006238588,0.49851775,0.000017344879,0.000059985447,0.00009359265,0.00021758102,0.497648,0.001860378,0.00023253229,0.0011854402,0.00003126655],"about_ca_topic_score_codex":0.07362639,"about_ca_topic_score_gemma":0.080100276,"teacher_disagreement_score":0.07362639,"about_ca_system_score_codex":0.00051634636,"about_ca_system_score_gemma":0.0007645167,"threshold_uncertainty_score":0.14639568},"labels":[],"label_agreement":null},{"id":"W3005929284","doi":"10.1306/11111918076","title":"Development and growth of basement-involved structural wedges in the northwestern Qaidam Basin, China","year":2020,"lang":"en","type":"article","venue":"AAPG Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Petro-Canada","funders":"","keywords":"Geology; Wedge (geometry); Structural basin; Echelon formation; Thrust fault; Seismology; Tectonics; Thrust; Kinematics; Décollement; Fault (geology); Petrology; Geometry; Geomorphology","score_opus":0.017584359840171575,"score_gpt":0.1955465488338395,"score_spread":0.17796218899366795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005929284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995857,0.000028955717,0.0001672703,0.000009942732,4.5086352e-7,0.0000031605666,0.000042305543,0.0000039174893,0.00015822504],"genre_scores_gemma":[0.99965954,0.00002132813,0.00014656813,0.00000322064,4.5911514e-7,0.0000021242636,0.000072511866,7.2716904e-7,0.00009351625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999225,0.0000070074593,0.000007076902,0.000025771984,0.000017075408,0.000020672616],"domain_scores_gemma":[0.9998996,0.000012588635,0.000030885472,0.000009928426,0.000022874865,0.00002409114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017838523,0.0002358831,0.00016120513,0.0010227857,0.0003827939,0.00043630277,0.00028481949,0.00021447548,0.0006015819],"category_scores_gemma":[0.00025384084,0.00027574616,0.00017966359,0.001036453,0.00034916404,0.00030623112,0.0003888727,0.000118414086,0.00006228259],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003777176,0.00004059416,0.93806547,0.000070115006,0.000041796888,0.00078412046,0.0011053259,0.00835654,0.032722976,0.0007445521,0.00012116207,0.017909758],"study_design_scores_gemma":[0.0000048532816,0.00002472063,0.9837659,0.000009651552,0.000011075631,0.00009342289,0.00036170808,0.014508643,0.0008079327,0.0001373576,0.0002690465,0.000005782143],"about_ca_topic_score_codex":0.028742652,"about_ca_topic_score_gemma":0.046482086,"teacher_disagreement_score":0.028742652,"about_ca_system_score_codex":0.0007638708,"about_ca_system_score_gemma":0.00062692905,"threshold_uncertainty_score":0.057150662},"labels":[],"label_agreement":null},{"id":"W3007523049","doi":"10.1029/2019gl086888","title":"Orthogonal Fault Rupture and Rapid Postseismic Deformation Following 2019 Ridgecrest, California, Earthquake Sequence Revealed From Geodetic Observations","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Fundamental Research Funds for the Central Universities","keywords":"Geology; Seismology; Sinistral and dextral; Aftershock; Geodetic datum; Geodesy; Interferometric synthetic aperture radar; Fault (geology); Slip (aerodynamics); Seismic moment; Synthetic aperture radar; Remote sensing","score_opus":0.06422997871925579,"score_gpt":0.2773728286163893,"score_spread":0.2131428498971335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007523049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943024,0.000016546132,0.000033961536,0.0000090441235,0.0000013350085,0.0000017769676,0.00020779335,0.0000041666312,0.00029511712],"genre_scores_gemma":[0.9993518,0.000021019949,0.000056358193,0.0000036835947,0.0000028997392,0.000001974128,0.00042184902,9.645985e-7,0.0001394638],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.000004147021,0.0000042796737,0.00001678703,0.000019518122,0.000018484268],"domain_scores_gemma":[0.99967456,0.00002155454,0.00016943875,0.00002199225,0.00007294026,0.000039541188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011717069,0.00012161318,0.00009953906,0.00047930292,0.00021004546,0.00027308328,0.00014399627,0.00016148019,0.0005276431],"category_scores_gemma":[0.00038844845,0.00009561866,0.0000701481,0.0005059738,0.00016701802,0.00013890276,0.00022268436,0.00013790451,0.00011399665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015896746,0.00005351561,0.9848363,0.000015202734,0.0000228418,0.00033400385,0.00018057472,0.0011355778,0.0070507852,0.00006173953,0.000600262,0.005550134],"study_design_scores_gemma":[0.0000022102101,0.000009264628,0.99930024,0.0000010571664,0.0000027189913,0.000018914356,0.00004069569,0.00036024326,0.00015289048,0.000004271801,0.0001063444,0.0000010765266],"about_ca_topic_score_codex":0.04175561,"about_ca_topic_score_gemma":0.09465837,"teacher_disagreement_score":0.04175561,"about_ca_system_score_codex":0.00038769818,"about_ca_system_score_gemma":0.00028520072,"threshold_uncertainty_score":0.08302516},"labels":[],"label_agreement":null},{"id":"W3008481320","doi":"10.1093/gji/ggaa085","title":"Transfer functions between teleseismic data components","year":2020,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Transfer function; Receiver function; Geology; Deconvolution; Convolution (computer science); Observable; Seismology; TRACE (psycholinguistics); Waveform; Sensitivity (control systems); Physics; Optics; Computer science; Lithosphere","score_opus":0.09480817802183653,"score_gpt":0.2616773313185157,"score_spread":0.1668691532966792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3008481320","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.31664675,0.00019956233,0.6586042,0.00039964702,0.00013897856,0.00022073637,0.002027743,0.0054065613,0.016355809],"genre_scores_gemma":[0.9215664,0.00018277578,0.0700587,0.000099714176,0.000045856206,0.00013632057,0.0014066688,0.0005002159,0.006003533],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9996408,0.000038333754,0.000019030937,0.00007346592,0.00017400224,0.00005437627],"domain_scores_gemma":[0.99887663,0.00035897925,0.00009836886,0.0001778894,0.00045598697,0.000032210057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006535387,0.0008044538,0.0001968514,0.0016104248,0.00028433977,0.0009231415,0.00052477437,0.00049958884,0.009163398],"category_scores_gemma":[0.0048490483,0.0002977699,0.00039722747,0.0012322894,0.00033006084,0.0011937643,0.00073093374,0.0005686835,0.0027581917],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006212617,0.00016407645,0.018204968,0.00032940446,0.00013121085,0.00060654496,0.00059325155,0.17455284,0.17594531,0.012708357,0.004128524,0.6120143],"study_design_scores_gemma":[0.00006983788,0.0003180461,0.05600698,0.000089201414,0.0001355557,0.0009933858,0.0005045168,0.73268956,0.16577932,0.027439727,0.015814401,0.00015943935],"about_ca_topic_score_codex":0.0017788995,"about_ca_topic_score_gemma":0.0006749851,"teacher_disagreement_score":0.009163398,"about_ca_system_score_codex":0.00065940566,"about_ca_system_score_gemma":0.00051969633,"threshold_uncertainty_score":0.030654669},"labels":[],"label_agreement":null},{"id":"W3008668289","doi":"10.1139/cjes-2019-0199","title":"A discussion of “hidden subduction” in orogenic belts","year":2020,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Lithosphere; Basement; Paleontology; Paleozoic; Cretaceous; Oceanic crust; Seismology; Sedimentary rock; Tectonics","score_opus":0.03148452506038726,"score_gpt":0.21938110184585516,"score_spread":0.1878965767854679,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3008668289","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12026339,0.08762296,0.07597777,0.120892406,0.0048687225,0.00016373342,0.00092393445,0.00018268204,0.58910435],"genre_scores_gemma":[0.9259664,0.026661107,0.00979279,0.009044584,0.004810077,0.00016222813,0.00035351052,0.00006153981,0.023147859],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99957055,0.00015534714,0.000031826545,0.000072960014,0.000056284043,0.000113028014],"domain_scores_gemma":[0.999554,0.00021680674,0.00008888393,0.000045786826,0.0000418777,0.000052680614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011744457,0.00059330964,0.00041180255,0.0016871386,0.00332004,0.0035316583,0.0018333016,0.002575532,0.0064767157],"category_scores_gemma":[0.0018887825,0.00021648337,0.00090744713,0.00216954,0.008540353,0.005444917,0.0018669359,0.002907549,0.0006885565],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000006888745,0.0000048699117,0.00089956523,0.000029154946,0.0000040180084,0.000116747426,0.0010484087,0.0006377528,0.00007303108,0.9924777,0.0016929562,0.0030089088],"study_design_scores_gemma":[0.0000154572,0.00004514334,0.0050327885,0.00033937275,0.000019990328,0.00063620775,0.0029324477,0.004495641,0.00024086748,0.7214561,0.26475555,0.000030390844],"about_ca_topic_score_codex":0.011508605,"about_ca_topic_score_gemma":0.0087565435,"teacher_disagreement_score":0.011508605,"about_ca_system_score_codex":0.0037606554,"about_ca_system_score_gemma":0.000768554,"threshold_uncertainty_score":0.027285576},"labels":[],"label_agreement":null},{"id":"W3008990966","doi":"10.3390/geosciences10020083","title":"Morphotectonic Kinematic Indicators along the Vigan-Aggao Fault: The Western Deformation Front of the Philippine Fault Zone in Northern Luzon, the Philippines","year":2020,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Seismology; Fault (geology); Kinematics; Active fault; Tectonics; Transform fault; Geodesy; Oblique case","score_opus":0.014297884724183106,"score_gpt":0.20649637837128754,"score_spread":0.19219849364710442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3008990966","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99764687,0.00011802397,0.00027206301,0.000026897991,0.0000028484858,0.000011439979,0.0007862418,0.000046653637,0.0010889181],"genre_scores_gemma":[0.9985985,0.00008798776,0.00047249367,0.000004303136,0.000003426603,0.000008005629,0.0005305451,0.0000057686702,0.00028895374],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992144,0.000008392886,0.0000055435835,0.000021114689,0.000026625243,0.000016889095],"domain_scores_gemma":[0.99980265,0.000015509355,0.000063989915,0.000011765164,0.00007100866,0.000035040848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012930798,0.00040858614,0.00014267734,0.0019892694,0.0002985835,0.00063649233,0.00019974836,0.00023103766,0.00078876445],"category_scores_gemma":[0.00041066844,0.0001140171,0.00012796852,0.0019427533,0.00045508638,0.00035006928,0.00046477382,0.00013429907,0.0001693757],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014767636,0.00003829949,0.9416201,0.0001447158,0.00004299779,0.0009832658,0.0028073923,0.0038853423,0.014746449,0.0002091539,0.00073718675,0.03463751],"study_design_scores_gemma":[0.0000022893207,0.00001672455,0.99613154,0.0000102959175,0.000008257341,0.00012430534,0.0009292597,0.0017520046,0.00038011145,0.000018751502,0.00061942876,0.000007123413],"about_ca_topic_score_codex":0.06643632,"about_ca_topic_score_gemma":0.12103488,"teacher_disagreement_score":0.06643632,"about_ca_system_score_codex":0.00045597696,"about_ca_system_score_gemma":0.00035031952,"threshold_uncertainty_score":0.13209921},"labels":[],"label_agreement":null},{"id":"W3009018953","doi":"10.1016/j.tecto.2020.228393","title":"Newly emerging cases of hydraulic fracturing induced seismicity in the Duvernay East Shale Basin","year":2020,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; Alberta Energy","funders":"","keywords":"Geology; Induced seismicity; Hydraulic fracturing; Seismology; Structural basin; Oil shale; Thrust fault; Fault (geology); Paleontology","score_opus":0.040903705103316146,"score_gpt":0.22892259507831872,"score_spread":0.18801888997500257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009018953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99440503,0.00016784974,0.00023415106,0.00024702025,0.000006263082,0.000006722203,0.000059116846,0.000005890156,0.0048679416],"genre_scores_gemma":[0.9990049,0.0001474213,0.00010512661,0.000019757226,0.000007507097,0.0000016101152,0.000047394667,9.844362e-7,0.0006651894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998248,0.000033011805,0.000016864045,0.000020274427,0.000048256734,0.00005682753],"domain_scores_gemma":[0.99916136,0.00027712714,0.00025874458,0.000083388506,0.000115677685,0.00010382342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003225724,0.00013566663,0.000108535314,0.0010480569,0.0011630933,0.0009935441,0.0003919416,0.0009083326,0.002405306],"category_scores_gemma":[0.0010422936,0.00012224614,0.00014982554,0.0011551748,0.0017967091,0.0005620013,0.0011231819,0.00068180304,0.00014709096],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004454861,0.00013593065,0.7985254,0.00019281097,0.00006368633,0.0909541,0.038222514,0.0023650306,0.012572526,0.01708959,0.002126013,0.03730698],"study_design_scores_gemma":[0.00002088175,0.00017280148,0.90013885,0.00013307552,0.00003592705,0.0317653,0.036102284,0.0026446946,0.0026510635,0.0024979268,0.023802415,0.000034883942],"about_ca_topic_score_codex":0.014849997,"about_ca_topic_score_gemma":0.058234584,"teacher_disagreement_score":0.98515,"about_ca_system_score_codex":0.0009078649,"about_ca_system_score_gemma":0.00045947192,"threshold_uncertainty_score":0.029527128},"labels":[],"label_agreement":null},{"id":"W3009020059","doi":"10.1002/essoar.10502324.1","title":"Stress chatter on a fracture network reactivated by hydraulic fracturing","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; McGill University","funders":"","keywords":"Geology; Aftershock; Seismology; Hydraulic fracturing; Differential stress; Fluid pressure; Seismometer; Slip (aerodynamics); Acoustic emission; Fault (geology); Shear (geology); Structural basin; Permeability (electromagnetism); Petrology; Geotechnical engineering; Deformation (meteorology); Geomorphology","score_opus":0.014114267993868921,"score_gpt":0.19768013277446428,"score_spread":0.18356586478059536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009020059","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993793,0.000009031337,0.00022675382,0.00000989961,5.487694e-7,0.0000013108544,0.000058392416,0.00001598709,0.00029879884],"genre_scores_gemma":[0.9997613,0.0000060012153,0.00008827515,0.0000016551589,3.4976398e-7,8.1446746e-7,0.00004415726,9.950592e-7,0.000096542826],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999436,0.000004362898,0.0000031161794,0.00001910618,0.000011542819,0.00001830101],"domain_scores_gemma":[0.99981946,0.000023167957,0.000071475944,0.00001477177,0.000043072367,0.00002808836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006659696,0.00012042126,0.00015269814,0.0006390382,0.00024906837,0.00040833885,0.00023586872,0.00018237843,0.0010836843],"category_scores_gemma":[0.00038220026,0.00013205696,0.0001344963,0.00047721385,0.00031033048,0.0001766828,0.00028254732,0.00013743572,0.000085577456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023704277,0.000061186285,0.8927439,0.000038574766,0.00007707389,0.0009276132,0.0005779914,0.022845382,0.0641399,0.00047118845,0.00035045284,0.017529739],"study_design_scores_gemma":[0.0000025932593,0.0000279065,0.9744955,0.000004319653,0.000013983669,0.000091709815,0.00024257487,0.023288138,0.0015344397,0.00012292393,0.00016967513,0.0000063098373],"about_ca_topic_score_codex":0.06937114,"about_ca_topic_score_gemma":0.11688015,"teacher_disagreement_score":0.06937114,"about_ca_system_score_codex":0.00079762895,"about_ca_system_score_gemma":0.00038908032,"threshold_uncertainty_score":0.13793468},"labels":[],"label_agreement":null},{"id":"W3009316862","doi":"","title":"On Corner Frequencies, Attenuation and Low-Frequency Earthquakes","year":2016,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Attenuation; Seismology; Geology; Seismogram; Frequency band; Anelastic attenuation factor; Saturation (graph theory); Seismic wave; Geodesy; Physics; Optics; Mathematics; Bandwidth (computing); Telecommunications","score_opus":0.019156887503682614,"score_gpt":0.21442751569915133,"score_spread":0.19527062819546873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009316862","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7569383,0.04376379,0.16590649,0.0014770582,0.00009588124,0.00003474215,0.00032620848,0.0001985925,0.031258896],"genre_scores_gemma":[0.98145884,0.009836006,0.006242831,0.00012668502,0.00014043416,0.000010033472,0.000109630986,0.000037137324,0.002038478],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9996284,0.0000742845,0.000024680647,0.00009563422,0.00013264258,0.000044345587],"domain_scores_gemma":[0.9941309,0.0041934596,0.00078969705,0.00025476186,0.00053307955,0.00009804156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011575839,0.00036351572,0.00041058759,0.00185808,0.0003613447,0.00097007444,0.0005999148,0.00052165816,0.0012810974],"category_scores_gemma":[0.007902872,0.00023168883,0.00014318079,0.0019233164,0.002204148,0.0013039731,0.000776774,0.0006438887,0.0002555704],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047184678,0.0000799327,0.17175184,0.0017530852,0.00014319128,0.0031149765,0.004466998,0.08977035,0.05209602,0.29287627,0.0026508095,0.38082469],"study_design_scores_gemma":[0.000017792072,0.00025849024,0.5278374,0.00065681705,0.00010722484,0.0020070244,0.0015500897,0.07856612,0.016540878,0.33552146,0.036750805,0.00018595204],"about_ca_topic_score_codex":0.011293035,"about_ca_topic_score_gemma":0.009231747,"teacher_disagreement_score":0.011293035,"about_ca_system_score_codex":0.00089107413,"about_ca_system_score_gemma":0.0002606162,"threshold_uncertainty_score":0.02245456},"labels":[],"label_agreement":null},{"id":"W3009364192","doi":"10.1029/2019jb018612","title":"Evolution of Elastic and Mechanical Properties During Fault Shear: The Roles of Clay Content, Fabric Development, and Porosity","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Geothermal Technologies Office; National Science Foundation","keywords":"Porosity; Clay minerals; Shearing (physics); Geology; Shear (geology); Stiffness; Elastic modulus; Composite material; Geotechnical engineering; Mineralogy; Materials science","score_opus":0.07818661726346422,"score_gpt":0.27580483862718297,"score_spread":0.19761822136371876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009364192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99975413,0.0000205465,0.00007568471,0.0000038500575,3.7344967e-7,9.707085e-7,0.000049142523,0.0000027702433,0.00009262796],"genre_scores_gemma":[0.99981564,0.000009986561,0.00005248347,0.000002187297,1.7449456e-7,0.0000010895349,0.00003774554,0.0000017273035,0.00007901253],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999201,0.000009306472,0.000007634909,0.000020909669,0.000020396565,0.000021580408],"domain_scores_gemma":[0.9997259,0.000052452237,0.000096747885,0.000023221264,0.000056636018,0.000045000485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017881472,0.00020477206,0.0001849261,0.0003151868,0.0001790061,0.0004842588,0.00014095579,0.00021234245,0.0008262584],"category_scores_gemma":[0.00037104252,0.00018589046,0.00011680768,0.00024535193,0.00041121512,0.00025820994,0.0002352522,0.00029422072,0.00010609843],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018808468,0.000028850296,0.033475608,0.000023339273,0.000016218544,0.00007437521,0.00008156266,0.0012143805,0.9633703,0.000050805513,0.000020620617,0.0014557363],"study_design_scores_gemma":[0.000010601886,0.00025937194,0.6033706,0.000008338945,0.00002109589,0.00012505,0.0004580198,0.012006095,0.38325182,0.000105306375,0.00036285393,0.000020740625],"about_ca_topic_score_codex":0.0023343917,"about_ca_topic_score_gemma":0.0027965447,"teacher_disagreement_score":0.0023343917,"about_ca_system_score_codex":0.00030738444,"about_ca_system_score_gemma":0.00012262721,"threshold_uncertainty_score":0.004641652},"labels":[],"label_agreement":null},{"id":"W3009768831","doi":"","title":"Impact Induced Crustal Differentiation: New Insights from the Sudbury Structure","year":2012,"lang":"en","type":"article","venue":"LPI","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Astrobiology","score_opus":0.02278450312495563,"score_gpt":0.23246516812201126,"score_spread":0.20968066499705562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009768831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98448074,0.00029060213,0.0012534327,0.00011496513,0.000004999027,0.0000057206394,0.00026828801,0.000014509682,0.013566695],"genre_scores_gemma":[0.9986009,0.00022100816,0.0003884211,0.000014489833,0.000004045409,0.000001379985,0.00009647033,0.000005049253,0.0006683531],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999653,0.000003420658,0.0000018726776,0.000009662511,0.000008068066,0.000011544017],"domain_scores_gemma":[0.99989593,0.000020540912,0.000026906617,0.000017301338,0.000020676898,0.000018617187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009467914,0.00015301078,0.00019461762,0.0005594888,0.00044053275,0.000895774,0.0002485607,0.0001487796,0.0029482825],"category_scores_gemma":[0.0004868931,0.00012711016,0.00010902637,0.00090572087,0.0007013468,0.00042942312,0.0006088768,0.00038148096,0.00015394269],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042977417,0.00010325121,0.56810194,0.00021378582,0.00013101223,0.0023340215,0.0047675874,0.0126253655,0.19867635,0.023945987,0.001258361,0.18741255],"study_design_scores_gemma":[0.0000069647867,0.000034291952,0.98950666,0.0000126429095,0.000018576502,0.00020316623,0.00067023985,0.0032651287,0.0024024802,0.0018571002,0.0020101722,0.000012606729],"about_ca_topic_score_codex":0.043234464,"about_ca_topic_score_gemma":0.086093836,"teacher_disagreement_score":0.043234464,"about_ca_system_score_codex":0.00076873053,"about_ca_system_score_gemma":0.00046559723,"threshold_uncertainty_score":0.08596563},"labels":[],"label_agreement":null},{"id":"W3010133896","doi":"","title":"Seismic velocity structure across the Eastern Newfoundland (Grand Banks) and Iberia Abyssal Plain Continental Margin Conjugates","year":2003,"lang":"en","type":"article","venue":"EGS - AGU - EUG Joint Assembly","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Abyssal plain; Continental margin; Seismology; Margin (machine learning); Oceanography; Paleontology; Structural basin; Tectonics","score_opus":0.01482042359153452,"score_gpt":0.22661373798794546,"score_spread":0.21179331439641094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010133896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98917764,0.0004620576,0.000085301785,0.00024696262,0.0000138757805,0.000007492735,0.004297123,0.000016934648,0.0056925323],"genre_scores_gemma":[0.9917779,0.00024843475,0.00019749641,0.00004681378,0.0000068715826,0.000008876889,0.003634648,0.0000065608756,0.004072434],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981445,0.000013966101,0.000011003302,0.000039370647,0.0000191674,0.000102029546],"domain_scores_gemma":[0.99947363,0.000029524663,0.00012597002,0.000026308959,0.00023239406,0.00011228265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002633066,0.00021159908,0.0001838077,0.0017664018,0.00063408463,0.00079450395,0.00035543623,0.00022879118,0.0029433388],"category_scores_gemma":[0.00059148733,0.00013869206,0.00019044691,0.0025727677,0.0003335305,0.000296798,0.00074515573,0.0002597284,0.00047997295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014349718,0.000039772556,0.969695,0.000035112178,0.00013317939,0.00017788363,0.0012065544,0.00078877254,0.00097561,0.00053863815,0.0053217094,0.02094429],"study_design_scores_gemma":[0.0000014699389,0.0000024463363,0.9983216,0.000007501376,0.0000057138145,0.00001365398,0.00034577766,0.000093006405,0.000022578972,0.0000058086666,0.0011790337,0.0000015120535],"about_ca_topic_score_codex":0.8668367,"about_ca_topic_score_gemma":0.948147,"teacher_disagreement_score":0.13316327,"about_ca_system_score_codex":0.004170025,"about_ca_system_score_gemma":0.0028455604,"threshold_uncertainty_score":0.26789498},"labels":[],"label_agreement":null},{"id":"W3010488991","doi":"10.1029/2019jb019101","title":"Coupled Evolution of Deformation, Pore Fluid Pressure, and Fluid Flow in Shallow Subduction Forearcs","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"United States Science Support Program; Marsden Fund; Center for Hierarchical Manufacturing, National Science Foundation","keywords":"Geology; Subduction; Pore water pressure; Forearc; Fluid dynamics; Geotechnical engineering; Permeability (electromagnetism); Petrology; Tectonics; Seismology; Mechanics","score_opus":0.03688458353640006,"score_gpt":0.28625784872993937,"score_spread":0.2493732651935393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010488991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992015,0.00001283425,0.0005878776,0.000012162075,4.8228304e-7,0.0000014453066,0.00003061394,0.000025289846,0.00012797932],"genre_scores_gemma":[0.9996275,0.000009367699,0.00024158301,0.0000030357958,5.039944e-7,0.0000019420756,0.000037560418,0.0000033643153,0.000075149466],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994195,0.000009275679,0.00000499149,0.000016067675,0.000011689651,0.00001606881],"domain_scores_gemma":[0.99985826,0.000039843355,0.000040829702,0.000017397677,0.000021554228,0.00002199134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012624926,0.00026242915,0.0002977046,0.0004569837,0.00023322146,0.00047617874,0.00044134274,0.000708989,0.0006542575],"category_scores_gemma":[0.00054397574,0.00037992836,0.00045490463,0.00028899248,0.0005324706,0.00030795851,0.00041199377,0.00028064303,0.000080312006],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002541712,0.00023457235,0.124932654,0.000048910784,0.00014463897,0.00062930846,0.0003089282,0.7363522,0.12881024,0.0012632617,0.00012397184,0.0068971487],"study_design_scores_gemma":[0.000033919318,0.00011727675,0.11403115,0.000007305553,0.000025832278,0.00009446622,0.000102029204,0.87876886,0.0061664046,0.00049071125,0.00013571983,0.000026361198],"about_ca_topic_score_codex":0.010953454,"about_ca_topic_score_gemma":0.006403433,"teacher_disagreement_score":0.010953454,"about_ca_system_score_codex":0.00085459807,"about_ca_system_score_gemma":0.000438796,"threshold_uncertainty_score":0.021779418},"labels":[],"label_agreement":null},{"id":"W3010506178","doi":"10.1029/2019rg000653","title":"Probabilistic Seismic Hazard Analysis at Regional and National Scales: State of the Art and Future Challenges","year":2020,"lang":"en","type":"article","venue":"Reviews of Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":223,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Hazard; Computer science; Multidisciplinary approach; Probabilistic logic; Seismic risk; Seismic hazard; Risk analysis (engineering); Seismology; Geology; Artificial intelligence; Business","score_opus":0.037483583823992014,"score_gpt":0.23121361618576264,"score_spread":0.1937300323617706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010506178","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012482473,0.97094554,0.016494393,0.006079417,0.0004983192,0.000013341265,0.00014566667,0.000070293034,0.0045049023],"genre_scores_gemma":[0.016118294,0.9723743,0.008657033,0.0007224862,0.001290012,0.0000268752,0.00016181811,0.000030043333,0.0006191432],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99902713,0.0003408833,0.00008862341,0.00020897221,0.00028795155,0.000046438778],"domain_scores_gemma":[0.99388486,0.0042584226,0.00045023672,0.00019610087,0.0010918161,0.00011860489],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0040397192,0.00064929586,0.0011199558,0.0018132637,0.00023632795,0.0024529614,0.0014960928,0.001656153,0.0023660262],"category_scores_gemma":[0.006837746,0.00030837365,0.0007504778,0.0032157565,0.0009900192,0.0034201466,0.0011331749,0.0018267445,0.0009606782],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044543456,0.00005724251,0.0021456897,0.011229253,0.00020448194,0.00017703476,0.00021389282,0.01556369,0.00083833444,0.0892137,0.027701039,0.852611],"study_design_scores_gemma":[0.000013480294,0.000110574096,0.0038818899,0.010907102,0.00033729227,0.00061079464,0.00062414136,0.02175277,0.0009272897,0.18839642,0.77231246,0.00012571135],"about_ca_topic_score_codex":0.0033787892,"about_ca_topic_score_gemma":0.0024599405,"teacher_disagreement_score":0.0040397192,"about_ca_system_score_codex":0.00089093874,"about_ca_system_score_gemma":0.0023210228,"threshold_uncertainty_score":0.021364331},"labels":[],"label_agreement":null},{"id":"W3010634588","doi":"","title":"Regional variations in crustal seismic attenuation across Canada from Lg waveform analysis","year":2018,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Attenuation; Waveform; Geodesy; Remote sensing; Telecommunications; Computer science","score_opus":0.018224613010736364,"score_gpt":0.2312900813838016,"score_spread":0.21306546837306525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010634588","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98917913,0.00017865979,0.0003143649,0.000099295394,0.0000058622986,0.000010095351,0.0060113147,0.000052508247,0.0041487347],"genre_scores_gemma":[0.9922374,0.00016429755,0.0004831779,0.000020487338,0.000002914445,0.000005378351,0.0046613254,0.000021374159,0.002403613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997867,0.000010744115,0.000009742166,0.000037264213,0.0000766402,0.000078959616],"domain_scores_gemma":[0.99907744,0.000051938227,0.000075442505,0.000025015644,0.00066903373,0.00010125387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002855416,0.0002490717,0.00019048832,0.0019284977,0.00084483484,0.0010024599,0.00050694897,0.00020604297,0.002231288],"category_scores_gemma":[0.0012391767,0.00013867223,0.00022502037,0.004330587,0.0002916377,0.00023303517,0.00042115213,0.0002550244,0.00036931646],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040973022,0.000045325305,0.92837745,0.00006247213,0.0001482226,0.00029732275,0.0013250196,0.003849678,0.007472111,0.0005738834,0.005056601,0.052382126],"study_design_scores_gemma":[0.000002948935,0.000005009514,0.9971208,0.000009711428,0.000021731965,0.000023427174,0.00040797988,0.0009295666,0.0002761366,0.000018950945,0.0011783451,0.0000054309553],"about_ca_topic_score_codex":0.99067163,"about_ca_topic_score_gemma":0.9939791,"teacher_disagreement_score":0.009328365,"about_ca_system_score_codex":0.0070316102,"about_ca_system_score_gemma":0.009481628,"threshold_uncertainty_score":0.05101812},"labels":[],"label_agreement":null},{"id":"W3010914975","doi":"10.1007/s00603-020-02076-5","title":"Passive Seismic Imaging of Stress Evolution with Mining-Induced Seismicity at Hard-Rock Deep Mines","year":2020,"lang":"en","type":"article","venue":"Rock Mechanics and Rock Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Vale (Canada); Glencore (Canada)","funders":"Vale Canada Limited; National Institute for Occupational Safety and Health; University of Oklahoma","keywords":"Induced seismicity; Geology; Seismology; Passive seismic","score_opus":0.009480728839804333,"score_gpt":0.17084598184657301,"score_spread":0.16136525300676868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010914975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99239916,0.00002818428,0.0066553517,0.000020304984,0.00000399727,0.00000805455,0.00026046333,0.00010249102,0.0005220775],"genre_scores_gemma":[0.9962381,0.000022685364,0.0033150043,0.000004743054,0.000005798015,0.000004921209,0.00022841245,0.0000133140275,0.00016688397],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991584,0.000011427036,0.000005552335,0.00002879691,0.000024530033,0.000013731786],"domain_scores_gemma":[0.9997396,0.00005016747,0.00007544406,0.000026733127,0.0000740063,0.000034071138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016944048,0.00027017118,0.00021148028,0.001127043,0.0001416197,0.00038398756,0.0003207536,0.00023209058,0.000678378],"category_scores_gemma":[0.0007081719,0.00020694392,0.00016226675,0.0008338486,0.0001761247,0.0004190355,0.0003618656,0.000177507,0.00013326235],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053823664,0.00022131136,0.5327103,0.00016646473,0.0001352483,0.0005732693,0.000748323,0.039143603,0.35857472,0.0005663588,0.0005614082,0.06606068],"study_design_scores_gemma":[0.000032140582,0.00014771364,0.80981326,0.000017482933,0.000060438444,0.0003241394,0.00046211667,0.16631962,0.021486213,0.0004796081,0.00082691415,0.000030290128],"about_ca_topic_score_codex":0.0021786843,"about_ca_topic_score_gemma":0.0034108544,"teacher_disagreement_score":0.0021786843,"about_ca_system_score_codex":0.00014466747,"about_ca_system_score_gemma":0.00015341165,"threshold_uncertainty_score":0.0043319464},"labels":[],"label_agreement":null},{"id":"W3011066228","doi":"10.2118/199996-ms","title":"Insights on Trigger Mechanisms of Two Large Hydraulic Fracturing-Induced Earthquakes and Sensitivity Analysis","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geomechanics; Hydraulic fracturing; Geology; Induced seismicity; Seismology; Pore water pressure; Permeability (electromagnetism); Fault (geology); Geotechnical engineering; Petrology","score_opus":0.022578077208265025,"score_gpt":0.22905374392366284,"score_spread":0.20647566671539783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3011066228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936103,0.00008373174,0.0047688507,0.00010509808,0.000008616689,0.000036301466,0.00024228722,0.000056149092,0.0010884812],"genre_scores_gemma":[0.999493,0.000015534892,0.00033785505,0.000007074604,0.000001247774,0.0000072078387,0.00005799186,0.00000228205,0.0000779248],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9996604,0.000102523125,0.000022856766,0.00006500783,0.00005259506,0.00009666417],"domain_scores_gemma":[0.9983771,0.0012196283,0.0001439346,0.00007891862,0.000115386654,0.00006497442],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010360552,0.0006844707,0.0005729432,0.0009382206,0.00042742424,0.0007243117,0.00066845387,0.0007845213,0.0016796843],"category_scores_gemma":[0.0028916646,0.00044479995,0.0010466843,0.00046516783,0.0004997189,0.00062348665,0.00063734065,0.0007489606,0.000050831768],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014045279,0.0001483037,0.047450572,0.00011456973,0.00031837646,0.0006441313,0.00010768734,0.9359244,0.009165326,0.0025316207,0.0002927142,0.0031619575],"study_design_scores_gemma":[0.000012099241,0.000060798753,0.019112736,0.000006340259,0.00005258608,0.000040381026,0.00012373645,0.9780644,0.001451621,0.0009352293,0.00011610259,0.000024016268],"about_ca_topic_score_codex":0.01753071,"about_ca_topic_score_gemma":0.008212485,"teacher_disagreement_score":0.01753071,"about_ca_system_score_codex":0.0010264349,"about_ca_system_score_gemma":0.0005775146,"threshold_uncertainty_score":0.034857333},"labels":[],"label_agreement":null},{"id":"W3011624883","doi":"10.1007/s12517-020-5250-y","title":"Probabilistic estimation of seismic parameters for Bangladesh","year":2020,"lang":"en","type":"article","venue":"Arabian Journal of Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Estimation; Probabilistic logic; Geology; Seismology; Statistics; Mathematics; Economics","score_opus":0.033565429750651056,"score_gpt":0.23514699796913754,"score_spread":0.2015815682184865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3011624883","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.849314,0.0007155146,0.1427484,0.0004989079,0.000021108937,0.000058230977,0.0025909292,0.00033361613,0.0037193883],"genre_scores_gemma":[0.99126184,0.00022330908,0.00630077,0.000012695023,0.000009768605,0.000017523493,0.001436581,0.000020040456,0.0007174474],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99972516,0.00010420339,0.000022454191,0.000070019916,0.000047485053,0.000030794505],"domain_scores_gemma":[0.9977875,0.0015793523,0.00021610306,0.0001596809,0.00020371561,0.00005354709],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009863413,0.00056503946,0.00042111037,0.0010290615,0.00025006846,0.0007172983,0.0006856253,0.0007231626,0.0015420801],"category_scores_gemma":[0.005068335,0.00051905616,0.00042328454,0.00092833047,0.0004573303,0.00065031555,0.0006491548,0.000580693,0.0004594101],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002594839,0.000021359134,0.02265615,0.000053318934,0.00006154056,0.000116288014,0.00007355725,0.9505202,0.0024074684,0.0038767457,0.0006606622,0.019293223],"study_design_scores_gemma":[0.000016800088,0.000026072452,0.012758877,0.000011346378,0.00001661412,0.00005921476,0.00005508411,0.98270386,0.0008518468,0.0029601224,0.0005108008,0.00002943995],"about_ca_topic_score_codex":0.029165808,"about_ca_topic_score_gemma":0.022466278,"teacher_disagreement_score":0.029165808,"about_ca_system_score_codex":0.00089186523,"about_ca_system_score_gemma":0.0008163922,"threshold_uncertainty_score":0.0579921},"labels":[],"label_agreement":null},{"id":"W3012148388","doi":"","title":"An Earthquake Nest in Cascadia","year":2018,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismology; Nest (protein structural motif)","score_opus":0.020918829092856486,"score_gpt":0.2416492238749599,"score_spread":0.22073039478210343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3012148388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98058355,0.000052800424,0.00019362482,0.00049554644,0.000043901306,0.000024992893,0.00084816746,0.00011532739,0.017642112],"genre_scores_gemma":[0.990316,0.000032095122,0.0002682828,0.00002900966,0.0000054276697,0.0000109768125,0.00072461064,0.000029778315,0.008583847],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990785,0.000022954422,0.0000040441605,0.000018579594,0.000015855137,0.00003067818],"domain_scores_gemma":[0.9992188,0.00007344955,0.00007146544,0.000097434466,0.00014447156,0.00039435943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018901144,0.00016328259,0.00019011907,0.00054826547,0.0031534876,0.0006333928,0.0004255857,0.00049941224,0.0086403135],"category_scores_gemma":[0.00096462347,0.00017412925,0.00011073582,0.00070564833,0.00056738436,0.00041562173,0.0011327956,0.00045617236,0.00093684],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014182327,0.0003849489,0.7380905,0.00028700757,0.00011359801,0.014370004,0.08490295,0.004107005,0.011504943,0.009246076,0.06782701,0.067747734],"study_design_scores_gemma":[0.000053783962,0.0002845755,0.87847877,0.00005945852,0.00004026297,0.0006575169,0.04443752,0.0016279335,0.0005519077,0.0010088207,0.072766535,0.000032836335],"about_ca_topic_score_codex":0.06789743,"about_ca_topic_score_gemma":0.3803455,"teacher_disagreement_score":0.93210256,"about_ca_system_score_codex":0.00095582526,"about_ca_system_score_gemma":0.0010715986,"threshold_uncertainty_score":0.13500446},"labels":[],"label_agreement":null},{"id":"W3012512506","doi":"10.1016/j.epsl.2020.116200","title":"A recent increase in megathrust locking in the southernmost rupture area of the giant 1960 Chile earthquake","year":2020,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Fundação para a Ciência e a Tecnologia; Natural Sciences and Engineering Research Council of Canada; Universidad de Chile; Technische Universiteit Delft; National Science Foundation","keywords":"Geology; Seismology; Subduction; Trench; Slip (aerodynamics); Geodesy; Viscoelasticity; Tectonics","score_opus":0.016988760381260837,"score_gpt":0.18523722883741656,"score_spread":0.1682484684561557,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3012512506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99381435,0.0009019264,0.00010809108,0.0007446828,0.000030125646,0.000004568097,0.0005540339,0.000012654827,0.0038296538],"genre_scores_gemma":[0.99798274,0.00035891158,0.000052608993,0.00009458355,0.00004216787,0.0000031555885,0.0003167459,0.0000043973587,0.0011447374],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999006,0.000010244409,0.000012210624,0.00003072955,0.000016602471,0.000029762577],"domain_scores_gemma":[0.9990889,0.00010951724,0.00035363273,0.00007691375,0.0002464279,0.00012471362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027399088,0.00009209246,0.00016211119,0.00074660365,0.00036405088,0.00077456795,0.00025941312,0.0005361282,0.0033389628],"category_scores_gemma":[0.0019513478,0.000119253404,0.00015772971,0.0011156634,0.0005322473,0.0005709379,0.000687041,0.00035607844,0.00040849787],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038120555,0.000029223567,0.9499135,0.0002141014,0.00007537522,0.0008944506,0.0016796943,0.0006280061,0.017982181,0.00085747364,0.001390041,0.02595489],"study_design_scores_gemma":[0.0000030211459,0.0000070729147,0.9979097,0.0000063521275,0.00000404664,0.000059472648,0.00023246922,0.000047742156,0.00016629708,0.000031042513,0.0015303562,0.0000024978747],"about_ca_topic_score_codex":0.023154376,"about_ca_topic_score_gemma":0.02972159,"teacher_disagreement_score":0.023154376,"about_ca_system_score_codex":0.0011743853,"about_ca_system_score_gemma":0.0005824832,"threshold_uncertainty_score":0.046039224},"labels":[],"label_agreement":null},{"id":"W3013085514","doi":"10.1126/sciadv.aay3314","title":"Slow slip source characterized by lithological and geometric heterogeneity","year":2020,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":155,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"U.S. Science Support Program, Lamont-Doherty Earth Observatory; Deutsche Forschungsgemeinschaft; Natural Environment Research Council; Sight Research UK","keywords":"Slip (aerodynamics); Biological system; Geology; Materials science; Biology; Physics; Thermodynamics","score_opus":0.023613553716748177,"score_gpt":0.2415235408941865,"score_spread":0.21790998717743834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013085514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988971,0.000058335638,0.0003557082,0.0000069365287,9.051155e-7,0.000007007206,0.00013538373,0.000010223251,0.0005283363],"genre_scores_gemma":[0.99943215,0.00004842524,0.00012732243,0.0000031760878,0.0000022555585,0.0000030587514,0.00021243903,0.0000022590111,0.00016884318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.000004773756,0.000009785428,0.000017758775,0.000024827674,0.000022588702],"domain_scores_gemma":[0.99968827,0.0000315164,0.00015757205,0.000031424857,0.000046883175,0.00004444414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097012206,0.00020818897,0.00027992445,0.0012814306,0.00018278127,0.00045895073,0.00014909786,0.00012501846,0.0017083089],"category_scores_gemma":[0.0006150948,0.00013404345,0.000106757485,0.0009177969,0.0003542796,0.0002563193,0.0005163897,0.00010396886,0.0002999127],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029127995,0.000038502654,0.9382681,0.00006251058,0.000058861748,0.0013823374,0.0004893479,0.0008219726,0.036297124,0.00035530503,0.0002277126,0.021706868],"study_design_scores_gemma":[0.0000051614397,0.000038251343,0.9969078,0.0000048392812,0.000012488499,0.00066119345,0.00021760784,0.00080027146,0.00089204905,0.00017115536,0.000284772,0.000004449711],"about_ca_topic_score_codex":0.003358327,"about_ca_topic_score_gemma":0.003915361,"teacher_disagreement_score":0.003358327,"about_ca_system_score_codex":0.00019521998,"about_ca_system_score_gemma":0.00014664199,"threshold_uncertainty_score":0.006677568},"labels":[],"label_agreement":null},{"id":"W3013290680","doi":"10.1785/0120190145","title":"Earthquake Magnitude and Lg Q Variations between the Grenville and Northern Appalachian Geologic Provinces of Eastern Canada","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Magnitude (astronomy); Seismology; Geology; Attenuation; Amplitude; Seismic hazard; Earthquake magnitude; Geodesy; Physics; Geometry","score_opus":0.01323788537044881,"score_gpt":0.17803324122426167,"score_spread":0.16479535585381286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013290680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99618053,0.00016318909,0.00010477803,0.000054240885,0.0000026811024,0.000009341409,0.0014904272,0.000013144483,0.0019816996],"genre_scores_gemma":[0.9979894,0.00008930574,0.0001465643,0.0000131417555,0.0000011762136,0.000005739992,0.0011453613,0.0000044363724,0.0006048757],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995888,0.00003788471,0.00002703927,0.00009049497,0.00013069608,0.0001251136],"domain_scores_gemma":[0.998362,0.00017277179,0.00022193773,0.00006608202,0.0010187442,0.0001584403],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037526002,0.0002365606,0.00020002738,0.0015963742,0.00090206624,0.0010252377,0.00053961255,0.00015982473,0.0011262423],"category_scores_gemma":[0.0018442473,0.00012633778,0.00018194437,0.0023390995,0.00059953413,0.00016120251,0.00052527257,0.00018564727,0.00014680708],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015075781,0.000012909328,0.97750914,0.00004145864,0.00008332158,0.000218296,0.0014131647,0.0010505579,0.0023947887,0.00015565704,0.0007483362,0.016221663],"study_design_scores_gemma":[0.0000018755628,0.0000031515021,0.99843234,0.0000069358675,0.0000059795134,0.000024717689,0.00074774516,0.00023482062,0.00009209143,0.000005926579,0.0004408296,0.0000035861328],"about_ca_topic_score_codex":0.98760915,"about_ca_topic_score_gemma":0.99260944,"teacher_disagreement_score":0.012390852,"about_ca_system_score_codex":0.007725169,"about_ca_system_score_gemma":0.0076354546,"threshold_uncertainty_score":0.05605024},"labels":[],"label_agreement":null},{"id":"W3013364492","doi":"10.1785/0120190170","title":"Method for Determination of Focal Mechanisms of Magnitude 2.5–4.0 Earthquakes Recorded by a Sparse Regional Seismic Network","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Focal mechanism; Seismogram; Seismology; Geology; Aftershock; Waveform; Rake; Seismic moment; Induced seismicity; Fault (geology); Computer science; Telecommunications","score_opus":0.027815811413913972,"score_gpt":0.23632260279176556,"score_spread":0.20850679137785158,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013364492","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15213585,0.00009199895,0.84454644,0.0000651188,0.000013427635,0.00011037968,0.000620018,0.0012070037,0.001209756],"genre_scores_gemma":[0.4897661,0.000077936216,0.50770885,0.000028518283,0.000018591938,0.000121755365,0.0010065224,0.00008762989,0.0011841418],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99981564,0.00003271377,0.000011620199,0.0000475782,0.00007349811,0.000019024572],"domain_scores_gemma":[0.9993411,0.00020822074,0.00011125607,0.000088169916,0.00021846146,0.00003280419],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004438647,0.00040512747,0.00028758662,0.0013438624,0.00023276359,0.00030172383,0.0004830829,0.00030307655,0.0019639211],"category_scores_gemma":[0.0019269071,0.0002353453,0.00040758692,0.000516413,0.00015847068,0.00028247404,0.0005394876,0.00027410765,0.00047404834],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041419367,0.00012243968,0.048965063,0.00016670497,0.00024782793,0.00021503984,0.0001873308,0.1078804,0.13210255,0.0025330842,0.0027559455,0.7044094],"study_design_scores_gemma":[0.00005609994,0.00005445748,0.039788984,0.000015576668,0.000054533924,0.00022788573,0.00004994493,0.9423231,0.014553995,0.00085371337,0.0019816586,0.00004014443],"about_ca_topic_score_codex":0.011162351,"about_ca_topic_score_gemma":0.016701953,"teacher_disagreement_score":0.011162351,"about_ca_system_score_codex":0.00035061754,"about_ca_system_score_gemma":0.0009553755,"threshold_uncertainty_score":0.022194743},"labels":[],"label_agreement":null},{"id":"W3013767667","doi":"10.1029/2019jb018519","title":"Seismic <i>P</i>  Wave Velocity Model From 3‐D Surface and Borehole Seismic Data at the Alpine Fault DFDP‐2 Drill Site (Whataroa, New Zealand)","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Penn West Exploration (Canada); University of Calgary","funders":"","keywords":"Geology; Seismology; Borehole; Vertical seismic profile; Seismic velocity; Fault (geology); Drill hole; Basement; Surface wave; Geophysical imaging; Seismic tomography; Geodesy; Geophysics; Drill; Paleontology","score_opus":0.09256110426533741,"score_gpt":0.3089365733585767,"score_spread":0.2163754690932393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013767667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99038637,0.000029678224,0.005825982,0.00008786124,0.00000969884,0.00003220954,0.0016842451,0.00035960675,0.0015843526],"genre_scores_gemma":[0.99581015,0.000030359224,0.0025405097,0.000008398698,0.0000033309345,0.000017638364,0.0013048508,0.000030005842,0.00025477447],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993026,0.0000067368364,0.0000042815323,0.000020937017,0.000019434061,0.000018286217],"domain_scores_gemma":[0.99986684,0.000027086544,0.000031064206,0.000016531118,0.000037807822,0.000020674383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015124386,0.00048317848,0.00021444891,0.0004752292,0.0002657107,0.0006622962,0.00071879313,0.00066880597,0.0008776079],"category_scores_gemma":[0.00067126856,0.00034025006,0.00052445434,0.0004740574,0.00030249084,0.0003770801,0.00021614203,0.00044387125,0.00029480897],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002734793,0.00014576675,0.12245734,0.000059865357,0.00008193509,0.00065082376,0.00030731977,0.83516884,0.0185789,0.0005392365,0.0018788527,0.019857703],"study_design_scores_gemma":[0.00007440297,0.000054735043,0.12535852,0.000013678072,0.000019923431,0.00009691879,0.00009097586,0.8721158,0.0013448574,0.00020433428,0.00057759706,0.00004829084],"about_ca_topic_score_codex":0.2207872,"about_ca_topic_score_gemma":0.1475253,"teacher_disagreement_score":0.2207872,"about_ca_system_score_codex":0.0011684969,"about_ca_system_score_gemma":0.0009767895,"threshold_uncertainty_score":0.43900412},"labels":[],"label_agreement":null},{"id":"W3013914478","doi":"","title":"The Queen Charlotte-Fairweather Fault Zone - Geomorphology of a submarine transform fault, offshore British Columbia and southeastern Alaska","year":2017,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Submarine pipeline; Geology; Fault (geology); Queen (butterfly); Submarine; Seismology; Transform fault; Geomorphology; Oceanography; Archaeology; Geography","score_opus":0.010890334441252411,"score_gpt":0.20668041858090183,"score_spread":0.19579008413964943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013914478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956321,0.00011922724,0.00005642718,0.00005479003,0.0000020599812,0.000009128362,0.00036360312,0.000006409877,0.003756304],"genre_scores_gemma":[0.99745756,0.000063313244,0.00010470364,0.000009296389,6.300953e-7,0.0000041788894,0.00016327946,0.0000021699898,0.0021949357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998913,0.000009446113,0.000007202491,0.000026251917,0.000029454242,0.000036464942],"domain_scores_gemma":[0.9996946,0.000033387354,0.00005049472,0.000018133216,0.00012771491,0.000075665404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013120822,0.00012770109,0.0001639575,0.001184109,0.0023343407,0.0011677208,0.00042975094,0.00036633434,0.0021695679],"category_scores_gemma":[0.00060266163,0.00018909886,0.00009684371,0.0018698181,0.0008509666,0.00034765308,0.0006159542,0.0002500494,0.00023344014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018292715,0.000036477948,0.9544068,0.000057892656,0.0000317346,0.0010279889,0.0066661756,0.0014188546,0.005911801,0.0010140261,0.001547955,0.027697282],"study_design_scores_gemma":[0.0000026164805,0.000007253993,0.9938461,0.000016649843,0.000004978408,0.00012432438,0.0037350066,0.00039038912,0.0001671586,0.000060073144,0.0016404645,0.0000049162704],"about_ca_topic_score_codex":0.9546875,"about_ca_topic_score_gemma":0.98986596,"teacher_disagreement_score":0.045312524,"about_ca_system_score_codex":0.005994565,"about_ca_system_score_gemma":0.005938414,"threshold_uncertainty_score":0.09115869},"labels":[],"label_agreement":null},{"id":"W3013981126","doi":"10.1029/2020gl088136","title":"The 2020 <i>M</i><sub><i>w</i></sub> 6.8 Elazığ (Turkey) Earthquake Reveals Rupture Behavior of the East Anatolian Fault","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Canada Foundation for Innovation","keywords":"Aftershock; Seismology; Geology; Slip (aerodynamics); North Anatolian Fault; Earthquake rupture; Fault (geology); Subduction; Plate tectonics; Geodesy; Tectonics","score_opus":0.029512691795815067,"score_gpt":0.26140195716969244,"score_spread":0.23188926537387738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013981126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982969,0.00004167088,0.000055290457,0.00001810557,0.000003038476,0.0000014151049,0.0004835488,0.0000148628715,0.0010850684],"genre_scores_gemma":[0.99842876,0.000040428935,0.00008677708,0.0000075785206,0.0000041115227,0.0000018572141,0.0011128597,0.0000035528178,0.00031401418],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999778,0.0000014149078,0.0000014573307,0.0000065079685,0.0000041075,0.0000087513345],"domain_scores_gemma":[0.99994755,0.0000025129923,0.000021184627,0.0000034554996,0.000011490366,0.000013816661],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000034039553,0.0001435518,0.00010435116,0.00056082464,0.00013572848,0.00022283962,0.00009197969,0.00020807942,0.0011379409],"category_scores_gemma":[0.00010591193,0.00007712625,0.00007072191,0.00043715123,0.000099697216,0.00016192425,0.00018275688,0.00011609014,0.00046088523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031220634,0.00012548118,0.8770767,0.000049207883,0.0000343609,0.0007032324,0.00030905966,0.0015944558,0.09188377,0.00019497001,0.0026621316,0.025054425],"study_design_scores_gemma":[0.0000016003659,0.000016537995,0.9979504,0.000002314661,0.0000026476139,0.00010608616,0.00008060249,0.0007058157,0.0007742257,0.000016067175,0.0003418439,0.0000018786932],"about_ca_topic_score_codex":0.00489701,"about_ca_topic_score_gemma":0.007320658,"teacher_disagreement_score":0.00489701,"about_ca_system_score_codex":0.00017749635,"about_ca_system_score_gemma":0.00008188816,"threshold_uncertainty_score":0.009737015},"labels":[],"label_agreement":null},{"id":"W3014044319","doi":"10.1029/2020gc008924","title":"Shallow Seismicity and the Classification of Structures in the Lau Back‐Arc Basin","year":2020,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Mount Royal University; University of Ottawa","funders":"Canada First Research Excellence Fund; Helmholtz Association; Natural Sciences and Engineering Research Council of Canada; GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel; Bundesministerium für Bildung und Forschung","keywords":"Geology; Lineament; Seismology; Subduction; Seafloor spreading; Structural basin; Echelon formation; Fault (geology); Induced seismicity; Tectonics; Forearc; Pull apart basin; Active fault; Slip (aerodynamics); Geodesy; Geophysics; Sedimentary basin; Geomorphology","score_opus":0.020465439040803363,"score_gpt":0.20119088441082733,"score_spread":0.18072544537002397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014044319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994764,0.000037801707,0.0000819772,0.0000106720445,5.566759e-7,0.000001717206,0.00005149496,0.0000043822047,0.000335083],"genre_scores_gemma":[0.9997124,0.000023771756,0.000101957856,0.0000024920153,7.629695e-7,0.000001935606,0.0000845145,9.889117e-7,0.00007116515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990904,0.000015682115,0.000011911088,0.000020418818,0.000021090702,0.000021770176],"domain_scores_gemma":[0.99968684,0.00005563473,0.00011774964,0.000028167487,0.00005808232,0.00005354837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015589611,0.00021151073,0.00018636201,0.0020019924,0.00026245293,0.0005864688,0.00011560606,0.00018594861,0.00063517434],"category_scores_gemma":[0.0007237535,0.00014565201,0.00013481344,0.00093879335,0.0004094853,0.00027096286,0.0004996074,0.00011569804,0.00012528518],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052524472,0.000013780428,0.97553873,0.00002029666,0.000024106077,0.00022394172,0.00081559445,0.0014624421,0.010694912,0.0001678582,0.000100762234,0.010885093],"study_design_scores_gemma":[0.0000011909137,0.000009255615,0.99753916,0.000005171461,0.0000041042017,0.0000367471,0.00024425666,0.0017409918,0.0002548843,0.00004994932,0.000112040754,0.0000023298446],"about_ca_topic_score_codex":0.016000833,"about_ca_topic_score_gemma":0.0358362,"teacher_disagreement_score":0.016000833,"about_ca_system_score_codex":0.00044694994,"about_ca_system_score_gemma":0.00020752386,"threshold_uncertainty_score":0.03181541},"labels":[],"label_agreement":null},{"id":"W3014746353","doi":"10.4095/321900","title":"Faults and lineaments of the Western Quebec Seismic Zone, Quebec and Ontario","year":2020,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Lineament; Seismology; Geology; Geography; Seismic zone; Tectonics; Induced seismicity","score_opus":0.02713306915061803,"score_gpt":0.22995282544120946,"score_spread":0.20281975629059143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014746353","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12786047,0.00091858994,0.0009258095,0.00044298716,0.000052949643,0.00028159103,0.8063209,0.00046176172,0.06273491],"genre_scores_gemma":[0.45661548,0.0016748802,0.004427133,0.00016135753,0.000029020004,0.00044038612,0.4170464,0.00026049,0.119344786],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.999723,0.0000129555165,0.0000203692,0.0000537188,0.00010674133,0.000083096544],"domain_scores_gemma":[0.9983133,0.0001341201,0.000173202,0.000063557054,0.0011220071,0.00019384077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018178277,0.0005053817,0.00029397287,0.0037529524,0.0014955556,0.0014040124,0.00093129074,0.0003010632,0.045890965],"category_scores_gemma":[0.0016070864,0.00023812018,0.00023670091,0.010358044,0.00031622458,0.00045695927,0.00038318272,0.00025879504,0.0036264516],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004313497,0.000103474085,0.34711754,0.0009147206,0.00012644558,0.0006473023,0.0029355285,0.004146766,0.0015901676,0.004286275,0.4869495,0.15075096],"study_design_scores_gemma":[0.00005356068,0.000017232373,0.8240951,0.00015019489,0.000029326504,0.00010521654,0.0017276893,0.002228825,0.00033492033,0.00014386444,0.17106993,0.0000441816],"about_ca_topic_score_codex":0.99724054,"about_ca_topic_score_gemma":0.99881387,"teacher_disagreement_score":0.045890965,"about_ca_system_score_codex":0.021561775,"about_ca_system_score_gemma":0.016203783,"threshold_uncertainty_score":0.15644234},"labels":[],"label_agreement":null},{"id":"W3014885183","doi":"","title":"Seismicity, Metamorphism, and Fluid Evolution Across the Northern Cascadia Fore Arc","year":2018,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Metamorphism; Geology; Induced seismicity; Seismology; Subduction; Arc (geometry); Island arc; Oceanography; Petrology; Tectonics","score_opus":0.015904813927892145,"score_gpt":0.22642459844490379,"score_spread":0.21051978451701164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014885183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946254,0.000040186078,0.000014131751,0.000052894575,0.0000010801169,6.852467e-7,0.00010274839,0.000004828083,0.00032087462],"genre_scores_gemma":[0.9995906,0.000029937677,0.000016459198,0.0000052289197,0.0000017772697,0.0000013668683,0.0001298146,0.0000018342862,0.00022289321],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998399,0.000022625089,0.000012517445,0.00005688261,0.000025328363,0.000042670647],"domain_scores_gemma":[0.9996227,0.000054751814,0.00009938412,0.000033854823,0.000086639084,0.00010265202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023217135,0.00031330713,0.000301641,0.0015317745,0.000851448,0.00058119354,0.00040200763,0.00049135496,0.001887944],"category_scores_gemma":[0.0010507947,0.00029655674,0.0003349894,0.0018157173,0.0006983967,0.00044022757,0.0008104503,0.0003298545,0.00019690958],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025428282,0.000041458585,0.98530895,0.000023201088,0.00010194732,0.00024019607,0.0016555245,0.0011509708,0.0052408217,0.000146491,0.00019324035,0.0056427997],"study_design_scores_gemma":[0.0000014893724,0.000004897115,0.9995029,0.000001227063,0.0000054382635,0.000011914429,0.00023365892,0.00012811672,0.000026189467,0.000010555226,0.00007209522,0.0000015362048],"about_ca_topic_score_codex":0.23905091,"about_ca_topic_score_gemma":0.33516556,"teacher_disagreement_score":0.23905091,"about_ca_system_score_codex":0.0016310697,"about_ca_system_score_gemma":0.0010477768,"threshold_uncertainty_score":0.47531897},"labels":[],"label_agreement":null},{"id":"W3015059147","doi":"","title":"Analysis of Local Earthquakes Recorded by the Batholiths Array in Western British Columbia: Pn Velocity and the State of Stress of the Coast Mountains Batholith","year":2007,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Batholith; Seismology; Geology; State (computer science); Stress (linguistics); Geography; Tectonics","score_opus":0.00714109114776152,"score_gpt":0.20312399958264651,"score_spread":0.195982908434885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3015059147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986834,0.000048962345,0.000027955935,0.0000176622,8.0497466e-7,0.0000038271646,0.0005316678,0.000002728635,0.0006829166],"genre_scores_gemma":[0.9982609,0.00007425026,0.000050126433,0.000008484479,9.673278e-7,0.00000422646,0.0006339836,0.0000026619953,0.00096436794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987996,0.000013851506,0.000011508781,0.000026161646,0.000023456918,0.000044932367],"domain_scores_gemma":[0.99928576,0.00008086182,0.00008830244,0.000028006913,0.00038421046,0.0001329637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016591519,0.00017134153,0.00020534771,0.0018975196,0.0010700974,0.00073766505,0.0005412612,0.00023913037,0.0018659668],"category_scores_gemma":[0.0012506918,0.00020894565,0.00014901656,0.004180634,0.0004230939,0.00021990201,0.00062164513,0.00028711703,0.0002681904],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007758409,0.000022036818,0.9893828,0.00002271952,0.00004528436,0.00014692509,0.0010696849,0.00045226316,0.001502132,0.000075123324,0.00040945772,0.0067939186],"study_design_scores_gemma":[8.852683e-7,0.0000027328892,0.9986039,0.0000038196076,0.000008256334,0.000013966442,0.0010120182,0.00016373077,0.000056191657,0.000004117298,0.00012869318,0.0000017186482],"about_ca_topic_score_codex":0.9692537,"about_ca_topic_score_gemma":0.9913407,"teacher_disagreement_score":0.030746281,"about_ca_system_score_codex":0.0038009754,"about_ca_system_score_gemma":0.0032900197,"threshold_uncertainty_score":0.06185466},"labels":[],"label_agreement":null},{"id":"W3015491438","doi":"10.1029/2019gl086236","title":"Insight Into Major Active Faults in Central Myanmar and the Related Geodynamic Sources","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Natural Science Foundation of China-Yunnan Joint Fund; CAS-SAFEA International Partnership Program for Creative Research Teams","keywords":"Seismology; Geology; Sinistral and dextral; Tectonics; Crust; Fault (geology); Seismotectonics; Focal mechanism; Active fault; Geophysics","score_opus":0.018692131466698438,"score_gpt":0.2510964730029014,"score_spread":0.23240434153620296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3015491438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978884,0.00025859836,0.0001510393,0.00012363779,0.0000015942071,0.0000037485938,0.00032295368,0.0000057918837,0.0012442843],"genre_scores_gemma":[0.999268,0.00010214527,0.00011197695,0.000010003581,0.0000031286393,0.000002518554,0.00021160148,9.753538e-7,0.00028974007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999658,0.0000050724884,0.0000030360065,0.0000097467555,0.000004320422,0.00001214471],"domain_scores_gemma":[0.99984384,0.000017351842,0.00007950236,0.00000937755,0.00003139739,0.000018597904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000087857756,0.00012571899,0.00008597261,0.0011577411,0.00021483898,0.00026503616,0.00016656698,0.000146596,0.0018180341],"category_scores_gemma":[0.00027136668,0.00007433736,0.00007708309,0.0010367897,0.00014000524,0.00028282977,0.00041558588,0.00009265091,0.00016576322],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036875677,0.000016719005,0.9628615,0.00005712408,0.000025176134,0.0004933949,0.0017037682,0.00054518785,0.007885401,0.0007255527,0.0005380937,0.02511113],"study_design_scores_gemma":[0.0000010222038,0.000006738719,0.9978212,0.000009374478,0.000005262549,0.00009099389,0.0007148134,0.0003752444,0.00008651841,0.00006194052,0.00082539604,0.0000015733372],"about_ca_topic_score_codex":0.015723746,"about_ca_topic_score_gemma":0.03197212,"teacher_disagreement_score":0.015723746,"about_ca_system_score_codex":0.00027942104,"about_ca_system_score_gemma":0.00026993995,"threshold_uncertainty_score":0.031264424},"labels":[],"label_agreement":null},{"id":"W3015541951","doi":"","title":"Possible seismic precursory activities to eastern Canadian earthquakes - some anecdotes","year":2003,"lang":"en","type":"article","venue":"EAEJA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology","score_opus":0.015894778349972723,"score_gpt":0.20655856057800184,"score_spread":0.19066378222802913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3015541951","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3855471,0.032917906,0.0052223364,0.117653064,0.0017297599,0.00013165941,0.0020408237,0.00016230966,0.45459512],"genre_scores_gemma":[0.924142,0.033877015,0.0018340488,0.0077288286,0.0011393778,0.000026059186,0.00044042533,0.00004008243,0.030772226],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9995517,0.000053479896,0.00002436808,0.000043043015,0.00019914772,0.00012820245],"domain_scores_gemma":[0.99464875,0.0023595635,0.00052413065,0.00019463133,0.0020114512,0.00026156512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011330815,0.00036484943,0.00018165766,0.0027328364,0.0071059465,0.003523179,0.0010493116,0.0020148915,0.0062554204],"category_scores_gemma":[0.009664592,0.00025821707,0.00019923574,0.003231025,0.0041097887,0.0020920946,0.0017474231,0.0023450502,0.0003987234],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00085762783,0.00011421544,0.17769322,0.001699892,0.000176328,0.035262678,0.14123988,0.0020242054,0.0054088775,0.22013481,0.13787481,0.2775134],"study_design_scores_gemma":[0.000052543946,0.000058555772,0.13731523,0.00094899983,0.00022202967,0.011505454,0.2590568,0.0007226209,0.0018118034,0.02205652,0.56610745,0.00014198628],"about_ca_topic_score_codex":0.7714698,"about_ca_topic_score_gemma":0.91116005,"teacher_disagreement_score":0.22853023,"about_ca_system_score_codex":0.011101024,"about_ca_system_score_gemma":0.007937904,"threshold_uncertainty_score":0.45975214},"labels":[],"label_agreement":null},{"id":"W3015666821","doi":"10.1007/s10950-020-09913-8","title":"Directivity analysis of the 2017 December Kerman earthquakes in Eastern Iran","year":2020,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; Uppsala Universitet; National Aeronautics and Space Administration","keywords":"Aftershock; Seismology; Geology; Directivity; Azimuth; Tectonics; Geometry","score_opus":0.04315678424930204,"score_gpt":0.2524781770234069,"score_spread":0.2093213927741049,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3015666821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985172,0.000040436604,0.0007726018,0.000012056198,0.0000020710045,0.000005794809,0.00014389811,0.000011848939,0.0004940572],"genre_scores_gemma":[0.99902606,0.000035426296,0.000511781,0.000003069089,0.0000048925335,0.000003662913,0.000250692,0.000003993162,0.0001603826],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990094,0.000012774437,0.000008404809,0.000022273469,0.000030845655,0.000024666337],"domain_scores_gemma":[0.99970406,0.000048777652,0.000078555255,0.000028283263,0.00011426736,0.000026075004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027713698,0.00030245565,0.00024137451,0.0016023247,0.00014362506,0.0002983223,0.00020105497,0.00015199534,0.0005256785],"category_scores_gemma":[0.00080751517,0.0001571904,0.00023299165,0.0010157063,0.0002049844,0.00020473028,0.0003571313,0.00015629262,0.00016603689],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003742656,0.000115678326,0.8832758,0.000109049804,0.0001945028,0.000993916,0.0009844902,0.015716318,0.022456579,0.00057658245,0.0006532302,0.07454957],"study_design_scores_gemma":[0.000008080296,0.000027724163,0.9906804,0.00000567496,0.000020031794,0.00017970613,0.0002568683,0.0075546703,0.00086808926,0.00009844736,0.0002920598,0.000008186264],"about_ca_topic_score_codex":0.0074230274,"about_ca_topic_score_gemma":0.010911077,"teacher_disagreement_score":0.0074230274,"about_ca_system_score_codex":0.00023801214,"about_ca_system_score_gemma":0.00023950182,"threshold_uncertainty_score":0.0147596},"labels":[],"label_agreement":null},{"id":"W3016344222","doi":"10.1785/0220200112","title":"Preface to the Focus Section on Historical Seismograms","year":2020,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Section (typography); Seismogram; Geology; Seismology; Focus (optics); Computer science; Optics; Physics","score_opus":0.129166146981814,"score_gpt":0.30354549193697633,"score_spread":0.17437934495516233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016344222","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000521665,0.026313672,0.002900929,0.07066339,0.4431232,0.0007370771,0.011183827,0.0018240346,0.44273224],"genre_scores_gemma":[0.0030559336,0.01840819,0.0017979038,0.01622681,0.14967494,0.0004816389,0.009526702,0.0012242494,0.79960364],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988104,0.00012660278,0.00009837941,0.0001408649,0.0007243148,0.00009946904],"domain_scores_gemma":[0.9919646,0.0014389505,0.00039691007,0.00046280827,0.004594329,0.0011425484],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0018287392,0.0013287214,0.00087682134,0.005056188,0.0018544075,0.003968404,0.001368134,0.00300496,0.4024541],"category_scores_gemma":[0.009732206,0.0005467343,0.00069287507,0.0036972223,0.00068365317,0.0039598695,0.0024182736,0.0040594204,0.27380314],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005758907,0.0000031228653,0.000018743915,0.000038794053,3.7584638e-7,0.000011563549,0.000010398042,0.00000989881,0.00003668862,0.00037656163,0.9921103,0.0073779137],"study_design_scores_gemma":[0.000002263359,0.0000046248015,0.00024004026,0.00010256945,5.574004e-7,0.0000206309,0.000024289257,0.0000064890705,0.000015705135,0.00039595633,0.99918455,0.0000022906174],"about_ca_topic_score_codex":0.0050506713,"about_ca_topic_score_gemma":0.007516946,"teacher_disagreement_score":0.4024541,"about_ca_system_score_codex":0.0025930875,"about_ca_system_score_gemma":0.0024556196,"threshold_uncertainty_score":0.8523267},"labels":[],"label_agreement":null},{"id":"W3016583051","doi":"10.1002/cpe.1531","title":"Pattern informatics approach to earthquake forecasting in 3D","year":2009,"lang":"en","type":"article","venue":"Concurrency and Computation Practice and Experience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"U.S. Geological Survey; Natural Sciences and Engineering Research Council of Canada; Southern California Earthquake Center; Institute for Catastrophic Loss Reduction; National Science Foundation","keywords":"Induced seismicity; Seismology; Geology; Unobservable; Tectonics; Microseism; Scale (ratio); Geography; Cartography; Econometrics; Mathematics","score_opus":0.040343145715003234,"score_gpt":0.28039744706104325,"score_spread":0.24005430134604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016583051","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.017063498,0.000121765624,0.9796479,0.0002331244,0.000023445087,0.000027899832,0.00015888002,0.000797598,0.0019259684],"genre_scores_gemma":[0.4751296,0.00039364793,0.5219135,0.00008433773,0.000069137874,0.00015520414,0.00046975925,0.00012806058,0.0016567135],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99971575,0.000078373734,0.00002633951,0.000056989895,0.00010051149,0.000022122125],"domain_scores_gemma":[0.99911946,0.00046827333,0.000096698976,0.000151832,0.0001283957,0.000035374032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005756892,0.0004381978,0.00058674806,0.0013923012,0.00035394184,0.001473482,0.001035295,0.00055433594,0.0026605153],"category_scores_gemma":[0.002667765,0.00035343354,0.0007191086,0.0015185862,0.00072561536,0.0013422302,0.0011291525,0.00078245805,0.00044654007],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010460106,0.00006507972,0.0034237711,0.000089419875,0.000048008293,0.00017413795,0.00022407038,0.7603674,0.0027069384,0.05389624,0.0017945565,0.1771058],"study_design_scores_gemma":[0.000006003002,0.0000070202623,0.00017822025,0.0000036152346,0.0000034470006,0.000014126975,0.000014635823,0.9849123,0.0003562821,0.013632471,0.00086912385,0.000002866267],"about_ca_topic_score_codex":0.0086105885,"about_ca_topic_score_gemma":0.0062072896,"teacher_disagreement_score":0.0086105885,"about_ca_system_score_codex":0.00072319055,"about_ca_system_score_gemma":0.000794607,"threshold_uncertainty_score":0.017120898},"labels":[],"label_agreement":null},{"id":"W3016675885","doi":"10.1029/2020gl087372","title":"Toward a Universal Frequency of Occurrence Distribution for Tsunamis: Statistical Analysis of a 32‐Year Bottom Pressure Record at Axial Seamount","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Amplitude; Geology; Seamount; Seismology; Geodesy; Power law; Series (stratigraphy); Standard deviation; Noise (video); Oceanography; Statistics; Physics; Mathematics; Paleontology","score_opus":0.050880409151253435,"score_gpt":0.2947564267229534,"score_spread":0.24387601757169994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016675885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987948,0.000029929395,0.0006859033,0.000023638988,0.0000018158576,0.000004556175,0.00019051341,0.000018941748,0.00024992655],"genre_scores_gemma":[0.9992661,0.000016799242,0.00029883653,0.000004799615,0.0000045478996,0.0000038213207,0.00033313723,0.000005253229,0.00006680629],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99935454,0.00014311036,0.00007822821,0.00020805046,0.00014279583,0.00007321424],"domain_scores_gemma":[0.99403906,0.0022921304,0.0016960489,0.0009771109,0.0006301394,0.00036547918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019263129,0.0001667674,0.00027037683,0.0023060443,0.0003164565,0.0007707091,0.00035895026,0.0004247939,0.0008983826],"category_scores_gemma":[0.0074808253,0.0002007123,0.0003997693,0.0013699249,0.0006159146,0.0005390196,0.0007690441,0.00036511407,0.00023769283],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053960157,0.000015214357,0.99047863,0.000012005237,0.00007143339,0.000098595374,0.00026670663,0.0007575191,0.002821055,0.000091154,0.000110310546,0.005223511],"study_design_scores_gemma":[0.0000010204047,0.000022077804,0.99737227,0.0000026335329,0.00000770573,0.00006699776,0.00011479945,0.0021572916,0.00014544417,0.000025478152,0.000079559606,0.00000462438],"about_ca_topic_score_codex":0.008806358,"about_ca_topic_score_gemma":0.0056155478,"teacher_disagreement_score":0.008806358,"about_ca_system_score_codex":0.000263152,"about_ca_system_score_gemma":0.00030372824,"threshold_uncertainty_score":0.017510176},"labels":[],"label_agreement":null},{"id":"W3016714505","doi":"","title":"Lithospheric deformation in the Canadian Appalachians: evidence from shear wave splitting","year":2016,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Shear wave splitting; Shear (geology); Seismology; Deformation (meteorology); Geophysics; Petrology; Tectonics; Oceanography","score_opus":0.0343384612855859,"score_gpt":0.21265094438660717,"score_spread":0.17831248310102127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016714505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967759,0.00019085027,0.000024528024,0.00007980056,0.0000029355708,0.0000068718123,0.00041710067,0.0000022178303,0.0024997392],"genre_scores_gemma":[0.9984353,0.0002825258,0.0000887792,0.000024588968,0.0000027440958,0.0000060678713,0.00041325795,0.0000021377377,0.0007445932],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996505,0.000024143183,0.000017311879,0.00004966783,0.00010171855,0.0001567167],"domain_scores_gemma":[0.9990903,0.00006898446,0.0001218067,0.000034348504,0.0005556833,0.00012882563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030326183,0.0003641746,0.00029678838,0.0026032324,0.003932188,0.0013228359,0.00085079105,0.00043432132,0.0022132148],"category_scores_gemma":[0.0014870005,0.0002503175,0.0001875993,0.0070401058,0.0012730561,0.00040631913,0.0009869514,0.00033961216,0.00020938859],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015495128,0.000029113622,0.966222,0.000058550406,0.000055630837,0.00041397096,0.008243987,0.00026518232,0.0017831076,0.0004154553,0.00071072124,0.021647343],"study_design_scores_gemma":[0.0000020754653,0.00000422377,0.9968047,0.0000106464,0.000006989795,0.000034655408,0.0023787399,0.00006605978,0.000048853744,0.000016754619,0.0006221336,0.0000042131005],"about_ca_topic_score_codex":0.99384296,"about_ca_topic_score_gemma":0.997493,"teacher_disagreement_score":0.008709606,"about_ca_system_score_codex":0.008709606,"about_ca_system_score_gemma":0.012659757,"threshold_uncertainty_score":0.06319296},"labels":[],"label_agreement":null},{"id":"W3016990501","doi":"10.1038/s41561-020-0562-9","title":"Subduction megathrust heterogeneity characterized from 3D seismic data","year":2020,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Subduction; Seismology; Episodic tremor and slip; Slip (aerodynamics); Surface finish; Materials science; Tectonics","score_opus":0.04079146006346175,"score_gpt":0.2501513384361789,"score_spread":0.2093598783727172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016990501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959319,0.000034888748,0.0011376983,0.00001396324,0.0000025590607,0.0000066023945,0.0021181682,0.00008124218,0.00067287835],"genre_scores_gemma":[0.99714065,0.000023471986,0.0004250613,0.0000025357094,0.0000036143715,0.000004479079,0.0022795892,0.000009964897,0.0001107648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998827,0.0000084575295,0.000013734263,0.000038648624,0.000023912744,0.000032489614],"domain_scores_gemma":[0.999488,0.00011331936,0.00014859029,0.00009031506,0.00008918177,0.00007069863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019909824,0.00027121173,0.00023482888,0.0033278782,0.00018464788,0.00062048767,0.00021883612,0.00023077939,0.0014922048],"category_scores_gemma":[0.00089489436,0.00016933146,0.00031589463,0.0018090929,0.00020041053,0.0003554686,0.0004201028,0.0001539063,0.0003710473],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004289749,0.00011601634,0.8615251,0.000062030114,0.0001337809,0.0007667053,0.0003183004,0.0675066,0.034472145,0.0006379044,0.001302933,0.03272949],"study_design_scores_gemma":[0.00000966906,0.000025008483,0.92342633,0.000008155267,0.000041418,0.00018441638,0.00019738609,0.074032426,0.0013620959,0.0001695657,0.00052992185,0.000013555846],"about_ca_topic_score_codex":0.0069762417,"about_ca_topic_score_gemma":0.008503825,"teacher_disagreement_score":0.0069762417,"about_ca_system_score_codex":0.0002229614,"about_ca_system_score_gemma":0.00026338745,"threshold_uncertainty_score":0.013871253},"labels":[],"label_agreement":null},{"id":"W3017235288","doi":"10.3319/tao.2006.17.3.503(t","title":"From Tornadoes to Earthquakes: Forecast Verification for Binary Events Applied to the 1999 Chi-Chi, Taiwan, Earthquake","year":2005,"lang":"en","type":"article","venue":"DOAJ (DOAJ: Directory of Open Access Journals)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Tornado; Earthquake prediction; Seismology; Geology; Induced seismicity; Magnitude (astronomy)","score_opus":0.1522678716871625,"score_gpt":0.44666667902233215,"score_spread":0.29439880733516965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3017235288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99646145,0.000033408734,0.0019191374,0.00008852978,0.000014740196,0.000015090671,0.0009793026,0.00007604499,0.00041230957],"genre_scores_gemma":[0.9979457,0.000017885626,0.0008561259,0.000004099497,0.0000074606323,0.0000032690461,0.0010718417,0.0000039988495,0.00008961108],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99967635,0.00008147191,0.000050939012,0.00008272114,0.0000619708,0.000046628855],"domain_scores_gemma":[0.99335504,0.0036545543,0.0008736093,0.0005174414,0.0012669739,0.00033243612],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001224754,0.00029523874,0.00026272633,0.0012121894,0.00043916798,0.0006691049,0.00048505966,0.00048155675,0.0013659117],"category_scores_gemma":[0.013973202,0.00016803204,0.00023363651,0.000785508,0.00022589936,0.0007185185,0.00053403043,0.00043271997,0.00026918977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023111308,0.00027995772,0.7481145,0.00010080361,0.00011588846,0.00071614754,0.00043723834,0.14912952,0.0033001525,0.0012544453,0.0029053474,0.091334835],"study_design_scores_gemma":[0.00008650649,0.00018851522,0.20581087,0.000021152213,0.000048385496,0.00008413861,0.0006644237,0.7899195,0.0019191224,0.0008162075,0.00041995433,0.00002123089],"about_ca_topic_score_codex":0.054787144,"about_ca_topic_score_gemma":0.04635071,"teacher_disagreement_score":0.054787144,"about_ca_system_score_codex":0.0005604116,"about_ca_system_score_gemma":0.0012574939,"threshold_uncertainty_score":0.10893655},"labels":[],"label_agreement":null},{"id":"W3017979854","doi":"10.1029/2019gc008839","title":"Evidence of Localized Failure Along Altered Basaltic Blocks in Tectonic Mélange at the Updip Limit of the Seismogenic Zone: Implications for the Shallow Slow Earthquake Source","year":2020,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Japan Society for the Promotion of Science; University of Maine; Geological Society of America","keywords":"Geology; Subduction; Seismology; Shear (geology); Shear zone; Echelon formation; Pore water pressure; Intraplate earthquake; Basalt; Petrology; Tectonics; Geotechnical engineering","score_opus":0.03132652670502445,"score_gpt":0.22566782228909857,"score_spread":0.19434129558407412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3017979854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99965525,0.000013794337,0.000047245223,0.000003550055,2.3252795e-7,0.0000017587528,0.000030315045,0.0000036316335,0.00024417145],"genre_scores_gemma":[0.9998795,0.000012092489,0.000033577435,0.0000010740968,3.97987e-7,0.0000010285655,0.00001822305,7.372591e-7,0.00005341591],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999696,0.000003296054,0.000003393069,0.000009417393,0.0000061733567,0.000008104468],"domain_scores_gemma":[0.9998331,0.000028013194,0.00006283943,0.000018557186,0.00002403238,0.00003336556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000077897246,0.00016869168,0.00021948264,0.00067511835,0.00026802556,0.00039061543,0.00019221815,0.00027496592,0.0015308799],"category_scores_gemma":[0.00030005828,0.00020317479,0.00015368807,0.00025038386,0.00039212307,0.00017198347,0.0004449469,0.00011255445,0.00014595788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028269514,0.000051454237,0.88166845,0.00005230935,0.000064708656,0.0013589853,0.0005691466,0.0044809408,0.10627012,0.0003375322,0.00006940452,0.004794343],"study_design_scores_gemma":[0.0000053211284,0.000049435715,0.9959622,0.0000040449368,0.000009458215,0.00010532454,0.00014471108,0.0022013166,0.0013811834,0.000048179354,0.000085850086,0.0000028970755],"about_ca_topic_score_codex":0.0071091903,"about_ca_topic_score_gemma":0.010379684,"teacher_disagreement_score":0.0071091903,"about_ca_system_score_codex":0.00034585575,"about_ca_system_score_gemma":0.000103366736,"threshold_uncertainty_score":0.014135659},"labels":[],"label_agreement":null},{"id":"W3018927679","doi":"","title":"Improved Modeling of Vertical Crustal Motion in Canada for a New North American Reference Frame","year":2016,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Reference frame; Geodesy; Frame (networking); Motion (physics); Seismology; Computer science; Artificial intelligence; Telecommunications","score_opus":0.02597866076769547,"score_gpt":0.21309547216108235,"score_spread":0.18711681139338687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3018927679","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9152126,0.00065998343,0.029967142,0.0009083903,0.00021809788,0.00008523415,0.006650221,0.0007835127,0.045514803],"genre_scores_gemma":[0.9813058,0.0002069834,0.009687429,0.00005070586,0.000010801358,0.00002540762,0.0015127821,0.00009754144,0.007102571],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981517,0.000020974536,0.000008396717,0.000036225887,0.00005903692,0.000060261922],"domain_scores_gemma":[0.9995635,0.000030450556,0.000019329063,0.000017843893,0.00032936127,0.00003949899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036206798,0.0005208349,0.00047984027,0.0006148925,0.001677784,0.0013058311,0.0017519805,0.00075597124,0.0028570204],"category_scores_gemma":[0.0011568867,0.0003460109,0.00052877696,0.0014757947,0.00032892247,0.00059647375,0.0003651031,0.00071610406,0.00040828768],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000081100785,0.000034178407,0.011456634,0.0000224642,0.000026243459,0.0000770082,0.00008261214,0.9715469,0.000699585,0.003536111,0.0029429581,0.009494166],"study_design_scores_gemma":[0.000027441698,0.000011280721,0.0072366297,0.000011051756,0.000023933773,0.000008437541,0.000077010314,0.988735,0.00042161503,0.00029985042,0.003125209,0.000022594957],"about_ca_topic_score_codex":0.9915799,"about_ca_topic_score_gemma":0.9885759,"teacher_disagreement_score":0.014540183,"about_ca_system_score_codex":0.014540183,"about_ca_system_score_gemma":0.018828522,"threshold_uncertainty_score":0.10549688},"labels":[],"label_agreement":null},{"id":"W3019336886","doi":"10.1029/2020jb020354","title":"Creep Burst Coincident With Faulting in Marble Observed in 4‐D Synchrotron X‐Ray Imaging Triaxial Compression Experiments","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Environmental Studies Research Funds; Norges Forskningsråd; European Synchrotron Radiation Facility","keywords":"Creep; Geology; Slip (aerodynamics); Shearing (physics); Strain rate; Nucleation; Deformation (meteorology); Materials science; Mineralogy; Geotechnical engineering; Composite material; Thermodynamics","score_opus":0.09272857214629587,"score_gpt":0.34162070210050166,"score_spread":0.2488921299542058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3019336886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992601,0.00004704167,0.00034927193,0.000010463144,0.0000015858692,0.0000050973067,0.00006401988,0.00001867646,0.00024366326],"genre_scores_gemma":[0.99884737,0.000042051608,0.0005210786,0.000007799208,0.0000020875434,0.000009774667,0.00014349201,0.000008045438,0.0004182464],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999045,0.0000072551384,0.0000070564215,0.000018611916,0.00003740776,0.000025135756],"domain_scores_gemma":[0.99952507,0.00007055268,0.00015798719,0.00006477823,0.00009891075,0.00008274996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013198823,0.00022755614,0.0001627437,0.00047263768,0.00023408336,0.00033028872,0.00031256455,0.00035539203,0.0009816011],"category_scores_gemma":[0.0003274157,0.00022266059,0.00015222552,0.00036091523,0.00028485287,0.00018024407,0.00021574032,0.00031434774,0.00012994927],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010911856,0.000035290257,0.0067569804,0.00001541307,0.000007906143,0.00018158324,0.00009496672,0.00036398912,0.9910188,0.00003210574,0.000023386487,0.001360525],"study_design_scores_gemma":[0.000018210087,0.0003483782,0.35984305,0.000008909851,0.000017978136,0.0004415345,0.0001889798,0.008033115,0.6302443,0.00004649403,0.0007901664,0.000018919862],"about_ca_topic_score_codex":0.002720816,"about_ca_topic_score_gemma":0.00527518,"teacher_disagreement_score":0.002720816,"about_ca_system_score_codex":0.00045118312,"about_ca_system_score_gemma":0.00013709084,"threshold_uncertainty_score":0.0054100156},"labels":[],"label_agreement":null},{"id":"W3019364115","doi":"10.1073/pnas.1913625117","title":"Aseismic transient slip on the Gofar transform fault, East Pacific Rise","year":2020,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Canada; National Science Foundation","keywords":"Transient (computer programming); Seismology; Geology; Slip (aerodynamics); Transform fault; Fault (geology); Engineering; Computer science; Aerospace engineering","score_opus":0.05195235222755454,"score_gpt":0.24624656579911514,"score_spread":0.1942942135715606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3019364115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968406,0.000025471347,0.00072540913,0.000037686525,0.0000015621076,0.00000424701,0.00009429636,0.00002002408,0.0022506765],"genre_scores_gemma":[0.9995067,0.000027934726,0.00019310451,0.0000027449403,0.0000010546538,0.0000027769574,0.00006433899,0.0000027065364,0.000198528],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99997413,0.0000036336132,0.0000015508014,0.000008861233,0.0000048264747,0.0000070074466],"domain_scores_gemma":[0.9999548,0.000007532747,0.000019677,0.000004070435,0.000004156825,0.000009777725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000035402743,0.00021977122,0.00015673616,0.0002155631,0.0002402181,0.00040288732,0.00034139885,0.00039869227,0.0009299638],"category_scores_gemma":[0.00025673019,0.00013301834,0.00020100379,0.00024600147,0.00046576106,0.00030007772,0.00021314672,0.0001427021,0.00007417096],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018993719,0.0001557091,0.15313612,0.000083602536,0.00007544458,0.0011313402,0.00022174734,0.80527323,0.025001299,0.004674641,0.0005955987,0.009461386],"study_design_scores_gemma":[0.000043318956,0.00008836191,0.10214468,0.000007892987,0.000035565947,0.00017937804,0.00015812615,0.8948019,0.0012030961,0.0008197134,0.00050278817,0.000015162999],"about_ca_topic_score_codex":0.040783245,"about_ca_topic_score_gemma":0.034511082,"teacher_disagreement_score":0.040783245,"about_ca_system_score_codex":0.0006065056,"about_ca_system_score_gemma":0.00044318318,"threshold_uncertainty_score":0.08109176},"labels":[],"label_agreement":null},{"id":"W3019779094","doi":"10.1002/eqe.3286","title":"Spatiotemporal seismic hazard and risk assessment of M9.0 megathrust earthquake sequences of wood‐frame houses in Victoria, British Columbia, Canada","year":2020,"lang":"en","type":"article","venue":"Earthquake Engineering & Structural Dynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia; Western University","funders":"Natural Environment Research Council; Sight Research UK; Natural Sciences and Engineering Research Council of Canada; Horizon 2020 Framework Programme; Canada Research Chairs; Southern California Earthquake Center","keywords":"Aftershock; Seismology; Geology; Seismic hazard; Fragility; Subduction; Seismic risk; Hazard; Crust; Urban seismic risk; Geophysics; Tectonics","score_opus":0.005465782549438126,"score_gpt":0.18201669076509525,"score_spread":0.1765509082156571,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3019779094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966113,0.000043106393,0.000775641,0.000111626214,0.0000033811384,0.0000256838,0.00080507924,0.000025546173,0.001598628],"genre_scores_gemma":[0.99846977,0.00003605284,0.0003105376,0.000007726365,5.760068e-7,0.000007028203,0.00053186284,0.0000024308633,0.00063401647],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981993,0.000034127177,0.000011079483,0.00003163716,0.000042750973,0.000060513416],"domain_scores_gemma":[0.999514,0.00009572993,0.00006711998,0.000027121385,0.00019210798,0.00010406728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042064782,0.00040980356,0.00023703267,0.0006916388,0.0005905939,0.0006739316,0.0010313886,0.0005181447,0.0011382782],"category_scores_gemma":[0.0015974408,0.000251684,0.00031812873,0.0008589444,0.00040239372,0.0002993277,0.00060958083,0.0003588548,0.000106311214],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018239507,0.00009472031,0.20950422,0.000037986803,0.000081435326,0.00044984417,0.00020275138,0.77867866,0.0008635139,0.0014363392,0.0014676802,0.007000472],"study_design_scores_gemma":[0.000021346556,0.000036922887,0.08876027,0.000013639026,0.000019696152,0.000034116772,0.0004386086,0.90952754,0.00031669438,0.00033590806,0.0004736173,0.00002173151],"about_ca_topic_score_codex":0.9606437,"about_ca_topic_score_gemma":0.9496299,"teacher_disagreement_score":0.03935629,"about_ca_system_score_codex":0.011551488,"about_ca_system_score_gemma":0.0060672103,"threshold_uncertainty_score":0.0838123},"labels":[],"label_agreement":null},{"id":"W3020529843","doi":"","title":"Prolonged post-seismic deformation of the 1960 great Chile earthquake and implications for mantle rheology","year":2002,"lang":"en","type":"article","venue":"Dipòsit Digital de la Universitat de Barcelona (Universitat de Barcelona)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Tectonophysics; Mantle (geology); Subduction; Geodetic datum; Earthquake rupture; Geodynamics; Plate tectonics; Geodesy; Geophysics; Fault (geology); Tectonics","score_opus":0.0087260135432692,"score_gpt":0.18365444841039277,"score_spread":0.17492843486712356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3020529843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977023,0.00055611995,0.00006943728,0.0002540821,0.000005672363,0.0000019810723,0.00013658407,0.0000073768583,0.0012664535],"genre_scores_gemma":[0.9995503,0.00015763237,0.000020823523,0.00001003011,0.0000064198703,0.0000012473255,0.000045135952,0.0000019425295,0.00020643127],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999237,0.000016863061,0.000008047789,0.000014992852,0.000011358741,0.000024995465],"domain_scores_gemma":[0.99970764,0.000067370485,0.00009891428,0.000038302296,0.000040897117,0.00004687112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002355763,0.00013728929,0.00021646355,0.00045103798,0.00023141863,0.0005778389,0.00025188853,0.00047518802,0.0020917621],"category_scores_gemma":[0.0014824169,0.00014665961,0.00018830305,0.0005348756,0.0006161683,0.0007042694,0.00045465192,0.00021218092,0.00027866522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081451726,0.000089637964,0.91845465,0.00016278635,0.00008539654,0.003238139,0.0012368712,0.012906446,0.032904077,0.0019750562,0.00079036877,0.02734208],"study_design_scores_gemma":[0.000008974488,0.000034372,0.9968119,0.000011264176,0.0000053693784,0.00013977599,0.00036216548,0.0015086049,0.00035557014,0.00035811038,0.00039587918,0.000008052823],"about_ca_topic_score_codex":0.015258069,"about_ca_topic_score_gemma":0.015105984,"teacher_disagreement_score":0.015258069,"about_ca_system_score_codex":0.000980585,"about_ca_system_score_gemma":0.00025200646,"threshold_uncertainty_score":0.030338526},"labels":[],"label_agreement":null},{"id":"W3021543736","doi":"10.1016/j.quascirev.2020.106309","title":"Palaeotsunamis along Canada’s Pacific coast","year":2020,"lang":"en","type":"article","venue":"Quaternary Science Reviews","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Volcano; Seismology; Prehistory; Oceanography; Margin (machine learning); Geologic record; Pacific Rim; Paleontology; Tectonics","score_opus":0.039786962480107296,"score_gpt":0.23550588928621527,"score_spread":0.19571892680610797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021543736","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.28046456,0.46613166,0.00056272815,0.043916296,0.0021247785,0.00007028316,0.004283438,0.00010933203,0.20233701],"genre_scores_gemma":[0.5139361,0.44476178,0.00064920186,0.0016081758,0.00038144377,0.000022014492,0.0014345419,0.000033187454,0.037173588],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997439,0.0000150282885,0.000015234961,0.000026493904,0.00011859112,0.00008081391],"domain_scores_gemma":[0.9983699,0.00009677748,0.00010421476,0.00002053473,0.0012229925,0.00018555166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043461728,0.00039547659,0.00019694037,0.0028169092,0.0025239056,0.0023527013,0.0006354089,0.0004722828,0.0036213966],"category_scores_gemma":[0.0016443604,0.00018271628,0.00018045232,0.006779107,0.0014744027,0.0007220835,0.00083125924,0.0010453261,0.00021412446],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002875481,0.000054524142,0.10277692,0.0028728289,0.00026219006,0.0006752578,0.015491256,0.0044895466,0.0015308564,0.031312123,0.12372294,0.71652406],"study_design_scores_gemma":[0.000020827623,0.00004495983,0.51085514,0.002166755,0.00011398092,0.00015136697,0.014881274,0.0004798524,0.00041099495,0.0026466958,0.4681751,0.000052998013],"about_ca_topic_score_codex":0.99508935,"about_ca_topic_score_gemma":0.9979943,"teacher_disagreement_score":0.030924287,"about_ca_system_score_codex":0.030924287,"about_ca_system_score_gemma":0.07081088,"threshold_uncertainty_score":0.2243725},"labels":[],"label_agreement":null},{"id":"W3021805678","doi":"10.1038/s43017-020-0049-7","title":"Developments in understanding seismicity triggered by hydraulic fracturing","year":2020,"lang":"en","type":"review","venue":"Nature Reviews Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":241,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Western University","funders":"","keywords":"Induced seismicity; Hydraulic fracturing; Seismology; Natural hazard; Seismic hazard; Microseism; Geology; Hazard; Natural (archaeology); Tectonics; Geotechnical engineering","score_opus":0.057563051496845846,"score_gpt":0.2685007784608745,"score_spread":0.21093772696402865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021805678","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00009325336,0.99788994,0.00029911823,0.0003450108,0.00031558578,0.0000034388063,0.000045296525,0.00000857223,0.0009998026],"genre_scores_gemma":[0.00048080244,0.99871266,0.00016835242,0.00015124468,0.00023815603,0.0000034251843,0.00004507766,0.0000013414187,0.00019893351],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99972266,0.000047044283,0.000040484956,0.00006223279,0.0000922869,0.000035234676],"domain_scores_gemma":[0.9986519,0.00086607994,0.00019239532,0.00003372091,0.00019939624,0.000056535213],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011468967,0.0014664619,0.0020066109,0.0025222076,0.00023253202,0.0017430327,0.0010824462,0.0016244032,0.006281413],"category_scores_gemma":[0.0026605634,0.0004070596,0.00075539085,0.0034167382,0.00085770735,0.0022419868,0.0011961226,0.00186556,0.0021178578],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000051974774,0.000037397094,0.00034019607,0.03304741,0.00015144712,0.000098966404,0.000056506822,0.00063390075,0.0011413364,0.006537763,0.017236965,0.9406662],"study_design_scores_gemma":[0.000018444798,0.00009475984,0.0018925987,0.009266758,0.0004089214,0.00036851884,0.00012362242,0.00018455733,0.00040174153,0.006183501,0.98102504,0.000031534073],"about_ca_topic_score_codex":0.0036143248,"about_ca_topic_score_gemma":0.0060050385,"teacher_disagreement_score":0.006281413,"about_ca_system_score_codex":0.0010463274,"about_ca_system_score_gemma":0.0031783385,"threshold_uncertainty_score":0.02101338},"labels":[],"label_agreement":null},{"id":"W3022384502","doi":"","title":"Characteristics of a Well Recorded, Bright, Meteorite-Dropping Fireball, British Columbia, Canada, September 4, 2017","year":2018,"lang":"en","type":"article","venue":"LPI","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Meteorite; Geology; Meteorology; History; Archaeology; Physical geography; Geography; Astrobiology; Physics","score_opus":0.011326604867968175,"score_gpt":0.19274669441442405,"score_spread":0.18142008954645586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022384502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94921374,0.0003928474,0.00027084968,0.00047132088,0.0000875002,0.00013094489,0.021793261,0.00009327041,0.027546283],"genre_scores_gemma":[0.96645665,0.00036762256,0.00028825225,0.00014743126,0.00004511712,0.000029444014,0.012548267,0.000027953918,0.02008914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974126,0.000006612994,0.0000144663845,0.000037530102,0.00012462227,0.0000755313],"domain_scores_gemma":[0.9984763,0.00003880844,0.00015170143,0.000027765736,0.00095349655,0.00035176234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017023903,0.00030059114,0.00020978144,0.00206994,0.0023414877,0.00089116197,0.00072790537,0.0004981689,0.0025463207],"category_scores_gemma":[0.000943239,0.00015408485,0.000096093434,0.0020576252,0.00055222755,0.00020920299,0.00053759885,0.0006062493,0.00076783693],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041663728,0.00013207643,0.9211608,0.0001295814,0.000061647595,0.0031280164,0.0047096433,0.0004922586,0.006719714,0.0002699287,0.03471525,0.028064385],"study_design_scores_gemma":[0.0000034036168,0.000020094221,0.99067265,0.00002273513,0.000008046521,0.0002995297,0.002483435,0.0001349368,0.0002220647,0.000013969461,0.0061107907,0.000008331251],"about_ca_topic_score_codex":0.9254797,"about_ca_topic_score_gemma":0.98370516,"teacher_disagreement_score":0.07452029,"about_ca_system_score_codex":0.005471568,"about_ca_system_score_gemma":0.0053595225,"threshold_uncertainty_score":0.14991826},"labels":[],"label_agreement":null},{"id":"W3022581998","doi":"10.5194/se-11-1571-2020","title":"On the morphology and amplitude of 2D and 3D thermal anomalies induced by buoyancy-driven flow within and around fault zones","year":2020,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University; University of Sudbury","funders":"Bureau de Recherches Géologiques et Minières; Agence Nationale de la Recherche","keywords":"Geology; Buoyancy; Geothermal gradient; Petrology; Fault (geology); Thermal; Amplitude; Convection; Geophysics; Fluid dynamics; Permeability (electromagnetism); Hydrothermal circulation; Mechanics; Seismology; Meteorology","score_opus":0.023064931682038953,"score_gpt":0.21945612554088978,"score_spread":0.19639119385885082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022581998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914829,0.000116513336,0.0062723453,0.0000696019,0.000016915454,0.000011669398,0.00040626584,0.00020458909,0.0014191774],"genre_scores_gemma":[0.99873286,0.000047129168,0.00083770807,0.0000065794634,0.0000035727976,0.000004800596,0.00018792988,0.000014048188,0.00016535274],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999213,0.000014457046,0.000005589705,0.000020621024,0.000019029416,0.000018923383],"domain_scores_gemma":[0.9997441,0.000085523316,0.0000617735,0.000027617547,0.000035819263,0.000045116773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009961901,0.00037752776,0.0003138785,0.00055842724,0.00020452953,0.00075921864,0.00026702086,0.00041732294,0.0014929887],"category_scores_gemma":[0.0005946853,0.00022351608,0.00048021623,0.0003719825,0.0005455857,0.0003665679,0.00034930586,0.00032868359,0.000121702156],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015520655,0.000097730095,0.022036234,0.0000974507,0.00007176846,0.0004106202,0.0001502739,0.9369081,0.031593926,0.0014932498,0.00046790813,0.0065175244],"study_design_scores_gemma":[0.000016804415,0.00003796621,0.020139946,0.000007778145,0.000017063529,0.000062794024,0.00005207843,0.9766739,0.0023617514,0.00033935398,0.00026724098,0.000023302515],"about_ca_topic_score_codex":0.0042122863,"about_ca_topic_score_gemma":0.0022683297,"teacher_disagreement_score":0.0042122863,"about_ca_system_score_codex":0.00037104767,"about_ca_system_score_gemma":0.00028691755,"threshold_uncertainty_score":0.0083755255},"labels":[],"label_agreement":null},{"id":"W3022912815","doi":"10.1038/s41467-020-15494-4","title":"Slip bursts during coalescence of slow slip events in Cascadia","year":2020,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Agence Nationale de la Recherche","keywords":"Slip (aerodynamics); Coalescence (physics); Episodic tremor and slip; Geology; Seismology; Subduction; Moment magnitude scale; Geodesy; Physics; Tectonics; Geometry","score_opus":0.026794390457099283,"score_gpt":0.25597817010109913,"score_spread":0.22918377964399986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022912815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999049,0.000042416144,0.00019196734,0.000017334229,0.0000021646294,0.0000035938274,0.00006894347,0.000027189832,0.00059741497],"genre_scores_gemma":[0.9995272,0.000030535994,0.00015644173,0.00000425598,0.0000027214696,0.000003845977,0.00012259267,0.0000053536014,0.00014707081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999249,0.0000047833796,0.0000029735882,0.000019536568,0.000026706355,0.000021081323],"domain_scores_gemma":[0.9996667,0.000039269737,0.000096809716,0.0000196846,0.000049978153,0.00012768332],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001092915,0.00016473635,0.00024569838,0.00092848396,0.00037768958,0.0004920189,0.00018564479,0.00022920143,0.00086141186],"category_scores_gemma":[0.00066358224,0.00019094476,0.000114343726,0.00046343912,0.0002604612,0.00016835102,0.0005324322,0.00029164046,0.0001277688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001317382,0.00013018664,0.68494445,0.00016919909,0.00018510665,0.0029832532,0.004806045,0.009246868,0.25001913,0.00087503804,0.0014976427,0.043825634],"study_design_scores_gemma":[0.000010040626,0.000040365365,0.99469274,0.000006494318,0.000009944643,0.00010810618,0.0003161877,0.0027662963,0.0015933,0.000076672804,0.00037138595,0.000008403943],"about_ca_topic_score_codex":0.016273063,"about_ca_topic_score_gemma":0.025101082,"teacher_disagreement_score":0.016273063,"about_ca_system_score_codex":0.0005897988,"about_ca_system_score_gemma":0.00023145106,"threshold_uncertainty_score":0.03235668},"labels":[],"label_agreement":null},{"id":"W3023973517","doi":"10.2138/am-2020-7298","title":"Oxygen isotope fractionation between gypsum and its formation waters: Implications for past chemistry of the Kawah Ijen volcanic lake, Indonesia","year":2020,"lang":"en","type":"article","venue":"American Mineralogist","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; McGill University","funders":"","keywords":"Gypsum; Geology; Geochemistry; Isotopes of oxygen; Sulfate; Fractionation; Meteoric water; Volcano; δ18O; Isotope geochemistry; Equilibrium fractionation; Crater lake; δ34S; Impact crater; Tephra; Isotope fractionation; Breccia; Mineralogy; Stable isotope ratio; Hydrothermal circulation; Chemistry; Fluid inclusions; Isotope; Paleontology","score_opus":0.0304281131803953,"score_gpt":0.2377340969585369,"score_spread":0.2073059837781416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3023973517","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986343,0.00020767402,0.00013761436,0.000047730096,0.000004510639,0.000002573278,0.00011325745,0.000008179864,0.00084416394],"genre_scores_gemma":[0.999448,0.00010940699,0.00018278851,0.000012711134,0.0000029337298,0.0000019779218,0.00007022584,0.000004305536,0.0001675429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996054,0.000003862468,0.0000046409104,0.000016932525,0.0000072959633,0.0000067485894],"domain_scores_gemma":[0.9999442,0.00000824026,0.000014629163,0.000004619449,0.000016296695,0.000011952016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015135651,0.0002323607,0.00025419737,0.0005508423,0.0005177542,0.0006331004,0.00022608532,0.00018160277,0.0006471154],"category_scores_gemma":[0.0002238998,0.00015054515,0.0001555362,0.00048264174,0.0003680447,0.00042639172,0.0002868062,0.00017980995,0.00008761697],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019744303,0.000044736935,0.8530427,0.000113125374,0.000067127105,0.00046676927,0.00076537154,0.0005750824,0.12837237,0.00024992676,0.00011996934,0.01598544],"study_design_scores_gemma":[0.000003033764,0.000022946957,0.9927349,0.000008557128,0.000018008765,0.00010900874,0.0004727309,0.0008911985,0.0049769697,0.000085265114,0.0006713635,0.000005924394],"about_ca_topic_score_codex":0.017660024,"about_ca_topic_score_gemma":0.025600713,"teacher_disagreement_score":0.017660024,"about_ca_system_score_codex":0.00067761575,"about_ca_system_score_gemma":0.00030622614,"threshold_uncertainty_score":0.035114467},"labels":[],"label_agreement":null},{"id":"W3024787920","doi":"","title":"Crustal Thickness Variations Across Eastern Canada and Maine From Receiver Function Analysis","year":2010,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Receiver function; Function (biology); Geology; Remote sensing; Geodesy; Seismology","score_opus":0.011307946818281374,"score_gpt":0.21068945598347608,"score_spread":0.1993815091651947,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3024787920","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990936,0.0003653407,0.0003048675,0.00006827985,0.000008025435,0.000014127843,0.0048808837,0.00005365402,0.0033687542],"genre_scores_gemma":[0.99389476,0.00022100135,0.00049267954,0.000021820206,0.0000036210513,0.000008048185,0.0034351991,0.00002131724,0.0019015414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977964,0.000012365617,0.0000100675,0.000047340818,0.00007668792,0.00007407189],"domain_scores_gemma":[0.999188,0.000082303035,0.00006665287,0.000029118482,0.0005321635,0.000101707665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030799548,0.00039449267,0.00035311223,0.0018920368,0.0010971199,0.0013138752,0.00071217713,0.00030173358,0.0019126084],"category_scores_gemma":[0.0011612666,0.00024563586,0.00035879682,0.003896005,0.00038003232,0.00031307575,0.00048036934,0.0003084136,0.00036839608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005741457,0.000061174636,0.9298852,0.00009275645,0.00036289514,0.0005488025,0.0017355648,0.009879714,0.01169714,0.00048989046,0.0036596274,0.04101308],"study_design_scores_gemma":[0.000010734771,0.000005390488,0.9965879,0.000017511778,0.00004215506,0.000032420037,0.00035744562,0.0015615018,0.00037358515,0.00003282366,0.00096621615,0.000012239821],"about_ca_topic_score_codex":0.9895083,"about_ca_topic_score_gemma":0.9935934,"teacher_disagreement_score":0.010491729,"about_ca_system_score_codex":0.007685789,"about_ca_system_score_gemma":0.0082200505,"threshold_uncertainty_score":0.055764616},"labels":[],"label_agreement":null},{"id":"W3025012589","doi":"10.1130/g47257.1","title":"A 1000-yr-old tsunami in the Indian Ocean points to greater risk for East Africa","year":2020,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Ocean Frontier Institute; University of Dar es Salaam; Canada First Research Excellence Fund; National Geographic Society","keywords":"Geology; Swahili; Tsunami wave; Oceanography; Indian ocean; Tanzania; Subduction; Human settlement; Seismology; Geography; Archaeology; Tectonics","score_opus":0.02557056517150982,"score_gpt":0.20937626335884774,"score_spread":0.1838056981873379,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025012589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989291,0.00013188251,0.000056684326,0.000026883907,0.000002037183,0.0000023472244,0.00004543815,0.000002338446,0.00080317765],"genre_scores_gemma":[0.9994112,0.0001723601,0.00017398715,0.0000063061007,0.000002234917,9.241577e-7,0.000026811245,8.9760306e-7,0.00020524701],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999678,0.0000060245807,0.000002962371,0.0000058743785,0.0000043902005,0.000012867167],"domain_scores_gemma":[0.99985826,0.000019702442,0.00006581079,0.000011852164,0.00002334387,0.000020954245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010277417,0.00017702344,0.00007341155,0.00080974854,0.0005621119,0.0004695014,0.00012377556,0.00012527718,0.0016341684],"category_scores_gemma":[0.00037625444,0.0001161794,0.000071730254,0.0008303809,0.0004182485,0.00025124234,0.0004401783,0.00017236962,0.00015986513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089815985,0.000015410184,0.9517234,0.000060732553,0.000022065082,0.0028118535,0.009563552,0.00013608333,0.012492622,0.00038901044,0.00029641524,0.022399016],"study_design_scores_gemma":[0.000001287344,0.000028129729,0.98994946,0.000026571119,0.000014275805,0.0010119573,0.006522823,0.00010906872,0.0006529585,0.00008523241,0.0015934714,0.000004748404],"about_ca_topic_score_codex":0.01527528,"about_ca_topic_score_gemma":0.03392059,"teacher_disagreement_score":0.01527528,"about_ca_system_score_codex":0.00028489062,"about_ca_system_score_gemma":0.00021109267,"threshold_uncertainty_score":0.030372739},"labels":[],"label_agreement":null},{"id":"W3025314972","doi":"","title":"Seismic Evidence for Compositional Asymmetry on the Newfoundland-Iberia Nonvolcanic Rifted Margin Pair: New Results From SCREECH Transect 2","year":2002,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Transect; Margin (machine learning); Geology; Paleontology; Seismology; Oceanography","score_opus":0.09424263588431163,"score_gpt":0.251398104289987,"score_spread":0.15715546840567535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025314972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99615663,0.00023269063,0.0000710967,0.00004828145,0.000004985406,0.0000065260315,0.00064369006,0.000004673023,0.002831518],"genre_scores_gemma":[0.99795675,0.00012494696,0.0002129313,0.00005421363,0.0000059261683,0.00000816608,0.00089315174,0.0000071614186,0.00073673355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99962115,0.000039065904,0.000023870129,0.000089962574,0.000048596892,0.00017731662],"domain_scores_gemma":[0.99922943,0.00005664224,0.0002447072,0.00008028955,0.0002481593,0.00014088111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037097497,0.0003274182,0.00043593798,0.0019932494,0.0011757542,0.000909214,0.00053472497,0.0003951478,0.0022453065],"category_scores_gemma":[0.00083070534,0.00024281324,0.00020523592,0.0021201195,0.0008969817,0.00037180947,0.0010323137,0.00034125146,0.00035914913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003700361,0.00006314882,0.95955056,0.00004198262,0.00013244092,0.00048558667,0.0016855755,0.0002891339,0.02318838,0.00014709015,0.00069471024,0.013351273],"study_design_scores_gemma":[0.000002898706,0.000009348655,0.99893194,0.000006278617,0.000011047538,0.000047300902,0.0003880668,0.000035858426,0.00015208898,0.000006800604,0.0004059928,0.0000023954876],"about_ca_topic_score_codex":0.5958626,"about_ca_topic_score_gemma":0.83905816,"teacher_disagreement_score":0.40413737,"about_ca_system_score_codex":0.0021367415,"about_ca_system_score_gemma":0.0015893537,"threshold_uncertainty_score":0.81303483},"labels":[],"label_agreement":null},{"id":"W3025517681","doi":"10.1029/2019jb018453","title":"The Northern Terminus of Cascadia Subduction","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Geoscience BC; University of Victoria; University of Calgary; University of British Columbia","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Plate tectonics; Submarine pipeline; North American Plate; Lithosphere; Induced seismicity; Peninsula; Ridge; Triple junction; Oceanic crust; Convergent boundary; Tectonics; Paleontology; Oceanography","score_opus":0.05665269629307689,"score_gpt":0.3131148268378913,"score_spread":0.2564621305448144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025517681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983712,0.00013358578,0.00011934216,0.00014430792,0.000011956015,0.000007983434,0.000570982,0.00006262867,0.015237139],"genre_scores_gemma":[0.99793124,0.000058665002,0.00008604623,0.000010026898,0.0000037157383,0.0000034165043,0.00039509233,0.0000051555066,0.001506838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.0000032522316,0.0000032657329,0.000022501537,0.000013997822,0.000015836898],"domain_scores_gemma":[0.999785,0.000011182135,0.000051536957,0.000015628068,0.00007732557,0.000059300743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007333704,0.00024244103,0.00018042186,0.0006353677,0.0009736518,0.00044207854,0.00015716178,0.00018093699,0.0029850178],"category_scores_gemma":[0.00035339885,0.0001224823,0.00013502328,0.00055997877,0.00033256592,0.00011519869,0.00058764435,0.00019577266,0.0004083065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028515706,0.000020816813,0.9513857,0.0001439933,0.00006913237,0.0017752564,0.0018938532,0.0031637314,0.018108636,0.0008903619,0.002357489,0.019905914],"study_design_scores_gemma":[0.0000046046907,0.0000098245655,0.99625045,0.000014986175,0.000008957004,0.00011292569,0.0004112918,0.000410143,0.00024193061,0.000083958235,0.002446845,0.000004164512],"about_ca_topic_score_codex":0.220154,"about_ca_topic_score_gemma":0.34698665,"teacher_disagreement_score":0.220154,"about_ca_system_score_codex":0.0015281818,"about_ca_system_score_gemma":0.0013771784,"threshold_uncertainty_score":0.4377451},"labels":[],"label_agreement":null},{"id":"W3025703880","doi":"","title":"Seismic evidence for mantle suture and a collisional origin for the Canadian Cordillera","year":2017,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mantle (geology); Fibrous joint; Seismology; Paleontology; Medicine","score_opus":0.08776627860921127,"score_gpt":0.30262774718127483,"score_spread":0.21486146857206356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3025703880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854093,0.00057822274,0.00009906093,0.000588043,0.000012298815,0.000011694006,0.00032022028,0.000011809193,0.012969442],"genre_scores_gemma":[0.99812835,0.0002153037,0.00020305073,0.00006626835,0.000007292241,0.000003315169,0.0002007035,0.0000030450667,0.0011727007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971324,0.000016097907,0.000013240161,0.00005661775,0.00008850246,0.0001122889],"domain_scores_gemma":[0.9985227,0.0001240053,0.0002866792,0.00006872904,0.00079210923,0.00020582552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004849665,0.0002743163,0.00022320387,0.0027303773,0.0034152593,0.0012933121,0.0009206675,0.0005979833,0.0066283694],"category_scores_gemma":[0.0028603354,0.00017888889,0.00014039896,0.0037216786,0.0014315813,0.00041723682,0.0010680808,0.0004826861,0.0002708696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042708474,0.000049349903,0.9272092,0.00008958178,0.000086315835,0.0006273143,0.0037753864,0.00053328654,0.011504465,0.0053879865,0.0015957234,0.048714165],"study_design_scores_gemma":[0.000010776303,0.000009918662,0.9950636,0.000023199007,0.000019516343,0.00007514801,0.0014994584,0.00032805715,0.00029231733,0.00018074721,0.0024909123,0.000006248276],"about_ca_topic_score_codex":0.97302806,"about_ca_topic_score_gemma":0.9877364,"teacher_disagreement_score":0.026971936,"about_ca_system_score_codex":0.012880488,"about_ca_system_score_gemma":0.012392034,"threshold_uncertainty_score":0.09345496},"labels":[],"label_agreement":null},{"id":"W3026022940","doi":"10.1007/s11069-020-04050-4","title":"Semi-empirical predictive equations for the initial amplitude of submarine landslide-generated waves: applications to 1994 Skagway and 1998 Papua New Guinea tsunamis","year":2020,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Ocean Sciences; Fisheries and Oceans Canada; Royal Society","keywords":"Landslide; Algorithm; Amplitude; Geology; Computer science; Artificial intelligence; Mathematics; Physics; Seismology; Optics","score_opus":0.047778004560985514,"score_gpt":0.30243844705762224,"score_spread":0.2546604424966367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3026022940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7699782,0.00035404772,0.22034103,0.0005836876,0.00005439713,0.00022300545,0.0013468293,0.0012339145,0.0058848183],"genre_scores_gemma":[0.9855097,0.00010542465,0.0128521435,0.000034430297,0.000011865512,0.000112047506,0.00033348196,0.00005711682,0.0009838722],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99963915,0.00012689103,0.000030783984,0.000075342374,0.000088677625,0.000039210237],"domain_scores_gemma":[0.9925252,0.0057554226,0.0006498479,0.00020111527,0.0008178807,0.000050499722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00250275,0.00079864316,0.0005373926,0.00071815774,0.00037113132,0.00093211234,0.0014713851,0.0011303917,0.001953297],"category_scores_gemma":[0.011483754,0.0005551581,0.0007709196,0.00061722536,0.00064418913,0.0008286625,0.0005658441,0.0011379789,0.0002864387],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019439147,0.000027917697,0.004602549,0.00002055428,0.000016684207,0.00006267546,0.00005025272,0.98916173,0.00040398605,0.0008985519,0.00016735912,0.004568353],"study_design_scores_gemma":[0.000002941971,0.0000034151326,0.00054783083,0.0000033310648,0.0000020533018,0.000003899166,0.0000075311223,0.999091,0.00013585793,0.00016383549,0.00003504711,0.0000031918687],"about_ca_topic_score_codex":0.06376721,"about_ca_topic_score_gemma":0.024785824,"teacher_disagreement_score":0.06376721,"about_ca_system_score_codex":0.0013837406,"about_ca_system_score_gemma":0.0012441148,"threshold_uncertainty_score":0.12679207},"labels":[],"label_agreement":null},{"id":"W3027943562","doi":"","title":"Fault gouge dating in the Canadian Rocky Mountains and implications for thrust belt kinematics","year":2003,"lang":"en","type":"article","venue":"EAEJA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Fault gouge; Kinematics; Thrust fault; Thrust; Fault (geology); Seismology; Mining engineering; Engineering","score_opus":0.03443101435678194,"score_gpt":0.25833429178099493,"score_spread":0.22390327742421298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3027943562","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97066116,0.004146943,0.0007388474,0.00100442,0.00007106534,0.000039539977,0.0039790645,0.000052244264,0.019306775],"genre_scores_gemma":[0.98883957,0.002013782,0.0013405338,0.00012684193,0.000017882963,0.000014563768,0.0014340925,0.000036270365,0.0061763935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99901783,0.000068991445,0.00005536506,0.00018076868,0.00035300932,0.00032399732],"domain_scores_gemma":[0.994713,0.00035234838,0.00036927697,0.0001619706,0.0041348715,0.0002684928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015984381,0.0003175442,0.0004343553,0.0066803596,0.005041636,0.0021923345,0.0018007425,0.00040881772,0.0032721283],"category_scores_gemma":[0.007977629,0.00022571698,0.00022983846,0.010588887,0.0011284153,0.0010338854,0.0010269847,0.0006396235,0.0002656248],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002462875,0.000060770617,0.86675316,0.00021532073,0.00014393633,0.00030700004,0.005836848,0.0020769276,0.004012877,0.00401251,0.0040914956,0.11224292],"study_design_scores_gemma":[0.000008729918,0.000010257673,0.9863473,0.00006252544,0.00004828496,0.00007966754,0.0023553711,0.00046400513,0.0007062304,0.00021388034,0.009686016,0.000017614579],"about_ca_topic_score_codex":0.994799,"about_ca_topic_score_gemma":0.9987459,"teacher_disagreement_score":0.023611844,"about_ca_system_score_codex":0.023611844,"about_ca_system_score_gemma":0.032470815,"threshold_uncertainty_score":0.17131674},"labels":[],"label_agreement":null},{"id":"W3027971977","doi":"","title":"Seismic variability of subduction thrust faults: insights from laboratory models","year":2010,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Slip (aerodynamics); Geology; Surface finish; Surface roughness; Amplitude; Thrust; Subduction; Mechanics; Overburden pressure; Thrust fault; Fault (geology); Geotechnical engineering; Seismology; Materials science; Optics; Tectonics; Composite material; Engineering; Physics","score_opus":0.011294787958755024,"score_gpt":0.19653268063015172,"score_spread":0.1852378926713967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3027971977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927469,0.00010527628,0.005349456,0.000067487555,0.0000051810694,0.000012251486,0.00059154746,0.00011614767,0.0010057339],"genre_scores_gemma":[0.99907947,0.000054033437,0.00047924556,0.00000416387,0.0000038555804,0.000011750444,0.0002885536,0.000006800817,0.000072141556],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991333,0.00002582617,0.000007660924,0.000026391966,0.000013243152,0.000013583555],"domain_scores_gemma":[0.9996511,0.00013715122,0.00008413378,0.000068451955,0.000031506508,0.000027778768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030713665,0.00036577357,0.00037792296,0.00029266687,0.00012971392,0.0005204647,0.0008236945,0.0005145349,0.000599084],"category_scores_gemma":[0.0008697133,0.00016119682,0.00041703164,0.00030250812,0.00041722786,0.00044503895,0.00037555475,0.00033578568,0.00007643551],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004897987,0.000359844,0.04945615,0.00012841565,0.00016699036,0.00025595436,0.0001247498,0.9064524,0.031238386,0.004402137,0.0007226533,0.0062024244],"study_design_scores_gemma":[0.000048994105,0.00018359785,0.01653365,0.0000070607875,0.00003673088,0.000035988098,0.000040814557,0.9787321,0.0030336,0.0010143995,0.0003098425,0.000023297123],"about_ca_topic_score_codex":0.0031831553,"about_ca_topic_score_gemma":0.0016959711,"teacher_disagreement_score":0.0031831553,"about_ca_system_score_codex":0.00044314368,"about_ca_system_score_gemma":0.00018504712,"threshold_uncertainty_score":0.0063292384},"labels":[],"label_agreement":null},{"id":"W3028008725","doi":"10.1029/2020jb019933","title":"Reactivation of an Intraplate Fault by Mine‐Blasting Events: Implications to Regional Seismic Hazard in Western Canada","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Seismology; Induced seismicity; Geology; Intraplate earthquake; Seismic hazard; Trench; Fault (geology); Peak ground acceleration; Spectral acceleration; Seismic risk; Event (particle physics); Tectonics","score_opus":0.05613225326905229,"score_gpt":0.32066201325575566,"score_spread":0.26452975998670336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3028008725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964288,0.0001950492,0.00011611519,0.00015986849,0.0000029823334,0.00001123209,0.0009676894,0.000008420425,0.0021100068],"genre_scores_gemma":[0.9988984,0.00011663355,0.00008874426,0.000015036788,0.0000010605091,0.0000023123964,0.00028728665,0.000002240403,0.00058827514],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975723,0.000015817728,0.000013732645,0.00004045575,0.000061267216,0.000111529254],"domain_scores_gemma":[0.99889576,0.00008002245,0.00017732385,0.000024683733,0.0005706904,0.0002515132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020522182,0.00019804592,0.00022423925,0.0014737732,0.0015776302,0.0014117176,0.0005357152,0.00026397168,0.0015483319],"category_scores_gemma":[0.0011773973,0.00012185091,0.00017344355,0.0029040372,0.0006561442,0.00025436076,0.00063138996,0.00037071688,0.000121661324],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008502084,0.000025851248,0.981108,0.000038356593,0.000043226893,0.00036280972,0.0011070971,0.0015854329,0.0016824184,0.00032250074,0.00082156,0.01281775],"study_design_scores_gemma":[0.0000028669108,0.0000090559815,0.99395704,0.000021226555,0.000014126671,0.000058048136,0.0031093871,0.0016476354,0.00016369254,0.0000648721,0.00094362657,0.000008409846],"about_ca_topic_score_codex":0.99414295,"about_ca_topic_score_gemma":0.99778205,"teacher_disagreement_score":0.016508192,"about_ca_system_score_codex":0.016508192,"about_ca_system_score_gemma":0.017266922,"threshold_uncertainty_score":0.11977589},"labels":[],"label_agreement":null},{"id":"W3028785539","doi":"10.1186/s40623-020-01152-y","title":"Coseismic changes in groundwater level during the 2018 Hokkaido Eastern Iburi earthquake","year":2020,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Japan Society for the Promotion of Science; Université de Nantes; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Groundwater; Epicenter; Geology; Seismology; Water level; Amplitude; Geotechnical engineering; Geography","score_opus":0.03391854587825601,"score_gpt":0.20132981960882382,"score_spread":0.1674112737305678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3028785539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996873,0.000018941015,0.00004921625,0.0000075747844,0.0000015171009,0.000002176542,0.000107253734,0.0000022301194,0.00012381592],"genre_scores_gemma":[0.9997069,0.00001622524,0.00007102556,0.0000035820647,0.0000016991982,0.0000050044337,0.000108697976,5.9518703e-7,0.00008633229],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998907,0.000014353378,0.000011321208,0.000027617774,0.000026018211,0.000030075915],"domain_scores_gemma":[0.999729,0.000027041411,0.00010204904,0.000014100849,0.000074246505,0.000053563806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016851017,0.00023613492,0.00029145842,0.0006805573,0.00041697102,0.000363497,0.00020176456,0.00034980406,0.00045608933],"category_scores_gemma":[0.00044328097,0.00014550237,0.00010473037,0.00087343674,0.000307575,0.0002910469,0.0004480964,0.00016171935,0.00009019554],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027744452,0.000064039086,0.9602366,0.000038687027,0.000068008216,0.00051982014,0.0016194088,0.0008456373,0.0290036,0.00003402307,0.00017368211,0.0071190717],"study_design_scores_gemma":[0.000002233481,0.000027198603,0.99844235,0.000002392419,0.000010150948,0.000028597937,0.00053893,0.00039232697,0.00043466184,0.0000076251376,0.00010958832,0.0000039048186],"about_ca_topic_score_codex":0.029252533,"about_ca_topic_score_gemma":0.06409872,"teacher_disagreement_score":0.029252533,"about_ca_system_score_codex":0.0005716741,"about_ca_system_score_gemma":0.00023372096,"threshold_uncertainty_score":0.058164537},"labels":[],"label_agreement":null},{"id":"W3029374297","doi":"","title":"Directional Wave Spectra of Open Ocean Tsunamis: Analysis of Recent Tsunamis Based on Records from DART Buoys and Cabled Arrays off the West Coast of Canada and the USA.","year":2018,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"West coast; Geology; Pacific ocean; Dart; Meteorology; Seismology; Remote sensing; Oceanography; Geography; Computer science","score_opus":0.019596382057202225,"score_gpt":0.2183587663214222,"score_spread":0.19876238426422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3029374297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883259,0.00016124999,0.00029011216,0.000052271782,0.000006842221,0.000009926666,0.009911315,0.0000257268,0.0012165821],"genre_scores_gemma":[0.9867273,0.0002036111,0.0007462423,0.000013522164,0.000006306107,0.000009472873,0.011558491,0.000008757083,0.00072627165],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995434,0.0000029211083,0.0000032478977,0.000008927236,0.000018285435,0.0000123367145],"domain_scores_gemma":[0.99943346,0.000045564913,0.00010464036,0.000021213797,0.0002998218,0.00009526715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011456604,0.00019452858,0.0000943008,0.0013802312,0.00025494953,0.0002634957,0.00024321431,0.00013194783,0.00060175336],"category_scores_gemma":[0.0006930838,0.00008924724,0.00010169799,0.0021465826,0.00015156709,0.00016582297,0.00023041223,0.00018315148,0.00019365859],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012376792,0.000028669676,0.975388,0.000029053888,0.000057266207,0.000092293616,0.00035002874,0.0008622322,0.002548893,0.000089064015,0.002448665,0.017982142],"study_design_scores_gemma":[0.0000023437972,0.000005184462,0.998648,0.000003385448,0.000008882813,0.000024038141,0.00013993224,0.0005160753,0.000105689476,0.000008818487,0.0005351191,0.0000025713753],"about_ca_topic_score_codex":0.7753373,"about_ca_topic_score_gemma":0.9130743,"teacher_disagreement_score":0.22466272,"about_ca_system_score_codex":0.0011180083,"about_ca_system_score_gemma":0.0016846322,"threshold_uncertainty_score":0.4519716},"labels":[],"label_agreement":null},{"id":"W3029970191","doi":"10.1029/2019jb019239","title":"<i>Vp</i>/<i>Vs</i> Ratio of Incoming Sediments Off Cascadia Subduction Zone From Analysis of Controlled‐Source Multicomponent OBS Records","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Accretionary wedge; Subduction; Submarine pipeline; Overpressure; Pore water pressure; Sedimentary rock; Sediment; Hydrostatic pressure; Seismology; Turbidite; Structural basin; Basement; Petrology; Geomorphology; Geochemistry; Tectonics; Oceanography; Geotechnical engineering","score_opus":0.043327755797265805,"score_gpt":0.3013103737667683,"score_spread":0.2579826179695025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3029970191","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99876165,0.000019834111,0.000119520024,0.000003742083,6.6427685e-7,0.000002883952,0.0005154483,0.000025373249,0.0005509221],"genre_scores_gemma":[0.99846834,0.000027315662,0.00021526226,0.0000020744058,0.0000015923629,0.0000053694653,0.001111577,0.000012895968,0.00015570625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998847,0.000006400502,0.000017377675,0.000040554627,0.00003330408,0.000017686381],"domain_scores_gemma":[0.9996567,0.000054496224,0.00010036523,0.000038818096,0.00009490497,0.000054772634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015200373,0.00039680133,0.00015455161,0.00248903,0.00028521975,0.0005258003,0.00028358743,0.00024127973,0.0009999202],"category_scores_gemma":[0.0006751917,0.00024149443,0.0003313478,0.0015663853,0.00022611895,0.0002173081,0.00039455172,0.0001590632,0.00016971941],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013243867,0.000030494753,0.94944215,0.00005110794,0.00014936362,0.0002426215,0.00030995917,0.0025747048,0.035334628,0.000082562925,0.00019689993,0.011453042],"study_design_scores_gemma":[0.0000017860021,0.0000074696404,0.99848205,0.0000022480822,0.000014054187,0.000020817224,0.000056196,0.0006033481,0.00070459436,0.000006350693,0.00009876137,0.000002327554],"about_ca_topic_score_codex":0.033602502,"about_ca_topic_score_gemma":0.039916996,"teacher_disagreement_score":0.033602502,"about_ca_system_score_codex":0.0005803129,"about_ca_system_score_gemma":0.00024459773,"threshold_uncertainty_score":0.06681383},"labels":[],"label_agreement":null},{"id":"W3030162292","doi":"10.1785/0120200101","title":"Minimal Clustering of Injection-Induced Earthquakes Observed with a Large-n Seismic Array","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Induced seismicity; Magnitude (astronomy); Seismic hazard; Slip (aerodynamics); Geothermal gradient; Earthquake magnitude; Geophysics; Geometry; Physics","score_opus":0.0327779003295028,"score_gpt":0.20725012342148472,"score_spread":0.1744722230919819,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3030162292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983663,0.000014105768,0.00081591535,0.000016756925,0.0000020062023,0.0000056397494,0.0002742771,0.000023188048,0.0004817768],"genre_scores_gemma":[0.9992299,0.000006113667,0.00035747243,0.0000025111624,0.0000024891267,0.000002205818,0.000318434,0.0000032558369,0.00007763047],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998381,0.000019016512,0.000012817932,0.000062062645,0.000031222087,0.000036663572],"domain_scores_gemma":[0.9991967,0.00015330987,0.00026079436,0.00008205085,0.00017723271,0.00013000425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022152302,0.00014216061,0.00019883152,0.0007718965,0.00028620337,0.00033444978,0.0002709024,0.00020654197,0.00076890783],"category_scores_gemma":[0.0015742907,0.00013975584,0.00014880043,0.0007065113,0.00020703017,0.00026825588,0.0003121524,0.0001516774,0.00016277381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015372357,0.000085142965,0.94464976,0.00002764074,0.000088615096,0.00028950965,0.00021676038,0.03427634,0.009407259,0.00030298455,0.0009339687,0.009568209],"study_design_scores_gemma":[0.000009672928,0.00005591115,0.92790157,0.0000067787696,0.000016782928,0.00010827068,0.0002901342,0.06983695,0.0011755804,0.0001264928,0.00045859514,0.00001325463],"about_ca_topic_score_codex":0.011129279,"about_ca_topic_score_gemma":0.0216059,"teacher_disagreement_score":0.011129279,"about_ca_system_score_codex":0.00047835222,"about_ca_system_score_gemma":0.00030784283,"threshold_uncertainty_score":0.022129},"labels":[],"label_agreement":null},{"id":"W3030386568","doi":"10.1186/s40623-020-01190-6","title":"Determination of the dipping direction of a blind reverse fault from InSAR: case study on the 2017 Sefid Sang earthquake, northeastern Iran","year":2020,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"European Space Agency; Ministry of Education, Culture, Sports, Science and Technology; Japan Society for the Promotion of Science; Canadian Institutes of Health Research; Japan Aerospace Exploration Agency; Japan International Cooperation Agency","keywords":"Seismology; Geology; Interferometric synthetic aperture radar; Aftershock; Fault (geology); Seismic gap; Active fault; Geodesy; Sinistral and dextral; Fault trace; Inversion (geology); Tectonics; Synthetic aperture radar; Remote sensing","score_opus":0.054938011297766716,"score_gpt":0.24094802647462396,"score_spread":0.18601001517685725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3030386568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99799514,0.00008962091,0.0010992811,0.00008009179,0.00001234457,0.000014716271,0.00020479909,0.000038498558,0.00046556146],"genre_scores_gemma":[0.9976198,0.0000686494,0.0018717494,0.000011192255,0.0000097215525,0.0000032063474,0.00028683955,0.0000048969728,0.00012395489],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972445,0.00004093929,0.000021724472,0.000055262273,0.00008790939,0.000069662594],"domain_scores_gemma":[0.99950135,0.00013145288,0.00010455759,0.0000702722,0.00013971831,0.000052566735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006019969,0.00058939867,0.00039835926,0.0010106411,0.0005557924,0.000547687,0.0006166333,0.0008426833,0.0003441333],"category_scores_gemma":[0.0009784591,0.00024018947,0.00054323016,0.0011453055,0.00053856976,0.000399751,0.00033123567,0.00045388346,0.00013494103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000597501,0.00054594007,0.7658363,0.00026212548,0.00029821004,0.036139596,0.0015874457,0.12475055,0.019862125,0.001059892,0.003337725,0.04572257],"study_design_scores_gemma":[0.00013104334,0.00042473516,0.62039155,0.000071048096,0.00034090728,0.0039698593,0.005132135,0.3512579,0.013017587,0.0010222835,0.0041131214,0.00012787535],"about_ca_topic_score_codex":0.040445473,"about_ca_topic_score_gemma":0.07177041,"teacher_disagreement_score":0.040445473,"about_ca_system_score_codex":0.0007866672,"about_ca_system_score_gemma":0.00076171913,"threshold_uncertainty_score":0.08042014},"labels":[],"label_agreement":null},{"id":"W3032924257","doi":"10.1111/maps.13490","title":"Preferred orientation distribution of shock‐induced planar microstructures in quartz and feldspar","year":2020,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Austrian Science Fund","keywords":"Geology; Orientation (vector space); Planar; Petrography; Shock (circulatory); Microstructure; Thin section; Quartz; Deformation (meteorology); Core (optical fiber); Mineralogy; Drill; Seismology; Materials science; Geometry; Composite material; Paleontology","score_opus":0.022016785722713882,"score_gpt":0.22323069587542518,"score_spread":0.2012139101527113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3032924257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987907,0.00007245817,0.0006649808,0.0000029879775,0.0000014166475,0.0000046728173,0.00014540384,0.0000101065025,0.00030736084],"genre_scores_gemma":[0.9989064,0.00005722461,0.000576792,0.0000034804787,0.0000013849062,0.000005068487,0.00017809449,0.0000057229004,0.0002659186],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999188,0.000003997226,0.000004592047,0.000032101056,0.000020547319,0.000019962168],"domain_scores_gemma":[0.99984086,0.000018815928,0.000048381837,0.000011382393,0.000058633494,0.000021925076],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000091205664,0.00008992734,0.00010432191,0.0006517581,0.00019946326,0.00036010277,0.00010341514,0.00016865775,0.00076438923],"category_scores_gemma":[0.00019546977,0.00019341592,0.000090091016,0.0003212258,0.0003093209,0.0001287413,0.00016236225,0.00011267612,0.0000879264],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025099522,0.000021956957,0.06835041,0.000055122873,0.000027739312,0.00015659542,0.00025727772,0.0007574554,0.92525524,0.0001452962,0.00006681009,0.004655195],"study_design_scores_gemma":[0.0000116297715,0.00014662156,0.899853,0.000007824631,0.000027242857,0.00031047867,0.0004750829,0.002066038,0.09618906,0.00006683791,0.0008292541,0.000016946153],"about_ca_topic_score_codex":0.0034480107,"about_ca_topic_score_gemma":0.006011691,"teacher_disagreement_score":0.0034480107,"about_ca_system_score_codex":0.00021390161,"about_ca_system_score_gemma":0.00014411412,"threshold_uncertainty_score":0.006855905},"labels":[],"label_agreement":null},{"id":"W3033291755","doi":"10.5194/nhess-2020-169","title":"Probabilistic tsunami inundation assessment of Kuroshio Town,Kochi Prefecture, Japan considering the Nankai-Tonankai megathrust rupture scenarios","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Leverhulme Trust","keywords":"Seismology; Geology; Probabilistic logic; Hazard analysis; Hazard; Computer science; Engineering","score_opus":0.02992431388421503,"score_gpt":0.24269228279936247,"score_spread":0.21276796891514743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033291755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947643,0.000092176284,0.003971147,0.00010508186,0.0000061750907,0.000013834363,0.00017609014,0.00002283822,0.00084828597],"genre_scores_gemma":[0.999169,0.000057100187,0.00051387283,0.000004333739,0.0000016744468,0.000006337523,0.000112159825,0.0000022213642,0.00013333937],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997881,0.00008465021,0.000012965829,0.00003971829,0.000034126417,0.000040433853],"domain_scores_gemma":[0.99966204,0.00010538875,0.000069944894,0.000019096282,0.000087200366,0.000056312816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005972582,0.00071409164,0.00042392252,0.00072719686,0.0004689922,0.00084903085,0.00055754464,0.00054367975,0.00058176334],"category_scores_gemma":[0.0011247938,0.00040602213,0.0005802535,0.0006575484,0.00036587784,0.00067630643,0.0005482276,0.00027804475,0.00005283632],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074543415,0.000035697794,0.030479673,0.00003069993,0.00007459675,0.00034588057,0.00007065656,0.9639831,0.0011353194,0.0006859155,0.00021970247,0.002864201],"study_design_scores_gemma":[0.000013779165,0.000059638696,0.018169783,0.0000058343207,0.000045848406,0.000038546787,0.00020363285,0.98035103,0.00032336882,0.0005848513,0.00018940328,0.000014264938],"about_ca_topic_score_codex":0.03575877,"about_ca_topic_score_gemma":0.029685935,"teacher_disagreement_score":0.03575877,"about_ca_system_score_codex":0.0011572614,"about_ca_system_score_gemma":0.00085291726,"threshold_uncertainty_score":0.07110125},"labels":[],"label_agreement":null},{"id":"W3033995723","doi":"10.1186/s40623-020-01209-y","title":"Realization approach of non-linear postseismic deformation model for Taiwan semi-kinematic reference frame","year":2020,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Future Earth","funders":"Ministry of Science and Technology, Taiwan; National Taiwan University; Central Geological Survey, Ministry of Economic Affairs","keywords":"Geodetic datum; Geodesy; Deformation (meteorology); Kinematics; Reference frame; Geology; Global Positioning System; Grid; Frame (networking); Function (biology); Logarithm; Convergence (economics); Linear model; Series (stratigraphy); Computer science; Mathematics; Mathematical analysis; Physics","score_opus":0.03521183626766064,"score_gpt":0.2304178857436357,"score_spread":0.19520604947597506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033995723","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.112138934,0.000076877346,0.8845063,0.00010371422,0.000022456057,0.000028946946,0.00016532851,0.00018160626,0.0027758582],"genre_scores_gemma":[0.96151537,0.00011968589,0.03336648,0.000022167065,0.000015283966,0.000087270535,0.0003520815,0.00004185074,0.004479889],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980956,0.00004089536,0.000012167759,0.00007075148,0.00003651036,0.000030130173],"domain_scores_gemma":[0.9997861,0.000060818573,0.000056852597,0.000023306018,0.000059858427,0.000013117689],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043104007,0.00040982736,0.00041442632,0.00040294186,0.00029284245,0.0005428513,0.0010540396,0.0005429312,0.0027608238],"category_scores_gemma":[0.00093090266,0.00032047115,0.0007043308,0.00050515146,0.0003313718,0.00047902248,0.00039825236,0.0005512249,0.00035768072],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025622088,0.000011819449,0.002200088,0.000024116252,0.000016718403,0.00009638059,0.00006826044,0.97057086,0.0013690994,0.015912266,0.00026449733,0.009440391],"study_design_scores_gemma":[0.0000016953264,0.000006023141,0.00022843527,0.0000010559781,0.0000026398259,0.0000050524022,0.0000039929428,0.99877304,0.000082474035,0.0007637607,0.0001293925,0.000002423067],"about_ca_topic_score_codex":0.032636162,"about_ca_topic_score_gemma":0.017847076,"teacher_disagreement_score":0.032636162,"about_ca_system_score_codex":0.0007117328,"about_ca_system_score_gemma":0.00077445136,"threshold_uncertainty_score":0.06489241},"labels":[],"label_agreement":null},{"id":"W3034110144","doi":"10.4138/atlgeol.2020.003","title":"Interpretation of lineaments and faults near Summerville, South Carolina, USA, using LiDAR data: implications for the cause of the 1886 Charleston, South Carolina, earthquake","year":2020,"lang":"en","type":"article","venue":"Atlantic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lineament; Fault scarp; Geology; Seismology; Epicenter; Quaternary; Fault (geology); Sinistral and dextral; Geomorphology; Tectonics; Paleontology","score_opus":0.06721460481029157,"score_gpt":0.2746103275643533,"score_spread":0.2073957227540617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034110144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913487,0.00012929499,0.0006336754,0.00060214836,0.000010873237,0.00002919394,0.001353931,0.000048769525,0.005843376],"genre_scores_gemma":[0.9954665,0.00016628449,0.0018819793,0.000097383265,0.0000087010085,0.000024122975,0.0011501116,0.000007842234,0.0011971021],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999064,0.000008823076,0.0000073134925,0.000021255271,0.00003363985,0.000022619388],"domain_scores_gemma":[0.99921286,0.000101813166,0.00016304971,0.000035833567,0.00039301036,0.000093396935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001793425,0.0001812834,0.00007655741,0.0019484598,0.00080701936,0.0007418267,0.0005581833,0.00026268925,0.0011909645],"category_scores_gemma":[0.0009775478,0.00010941715,0.000096726486,0.0023290287,0.00029192783,0.0002064786,0.00047589853,0.0002804272,0.00023062543],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061003557,0.00004787832,0.9002323,0.00009225943,0.000027638902,0.0015011526,0.0032294204,0.0022244398,0.027460568,0.00036774823,0.004325681,0.060429826],"study_design_scores_gemma":[0.000005352386,0.000013217953,0.9832972,0.00006271688,0.000015264288,0.0001317238,0.0068705585,0.0040771184,0.001265083,0.00010643146,0.004143583,0.0000118236185],"about_ca_topic_score_codex":0.37273657,"about_ca_topic_score_gemma":0.7080518,"teacher_disagreement_score":0.37273657,"about_ca_system_score_codex":0.0015043505,"about_ca_system_score_gemma":0.0019657959,"threshold_uncertainty_score":0.74113405},"labels":[],"label_agreement":null},{"id":"W3034286121","doi":"","title":"Geochemical and mineralogical signature of fault zones in Archean basement rocks: characterizing a multi-episodic history of fluid-rock interactions","year":2018,"lang":"en","type":"preprint","venue":"Dipòsit Digital de la Universitat de Barcelona (Universitat de Barcelona)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Archean; Basement; Geochemistry; Fault (geology); Signature (topology); Petrology; Intrusion; Seismology; Archaeology","score_opus":0.016826425759887378,"score_gpt":0.21685893330746298,"score_spread":0.2000325075475756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034286121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99875844,0.0002816105,0.00006836508,0.000006614834,9.232212e-7,0.000004391876,0.00039568727,0.0000062337317,0.0004776308],"genre_scores_gemma":[0.9985862,0.00019091774,0.00017308323,0.0000058354335,0.0000017669367,0.0000043837745,0.0006260211,0.0000048136153,0.00040697958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998485,0.000007285662,0.000009610693,0.00006455653,0.00003159434,0.000038396094],"domain_scores_gemma":[0.99985945,0.000010114884,0.000044015313,0.000010117355,0.000053532953,0.000022813469],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013975595,0.0002773315,0.00025476122,0.0024435204,0.0006975214,0.0007424311,0.0003494812,0.00030613213,0.0005810706],"category_scores_gemma":[0.00025923213,0.000187188,0.00017854893,0.0017806175,0.0006619125,0.00023498834,0.00060514524,0.00018283234,0.00014973128],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089370704,0.000024598425,0.95055467,0.00006210378,0.00006857061,0.00035719143,0.0014347244,0.00047818836,0.0364341,0.00013436157,0.00010233921,0.010259891],"study_design_scores_gemma":[0.0000011519151,0.000010409867,0.99824595,0.0000063317343,0.000008657766,0.00011089815,0.00035509196,0.00016237421,0.00065787724,0.000011804366,0.0004262276,0.000003167986],"about_ca_topic_score_codex":0.31725645,"about_ca_topic_score_gemma":0.54669,"teacher_disagreement_score":0.31725645,"about_ca_system_score_codex":0.0015001663,"about_ca_system_score_gemma":0.0011945376,"threshold_uncertainty_score":0.6308196},"labels":[],"label_agreement":null},{"id":"W3034557646","doi":"10.1029/2019rg000695","title":"Hydraulic Fracturing‐Induced Seismicity","year":2020,"lang":"en","type":"article","venue":"Reviews of Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":394,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Induced seismicity; Hydraulic fracturing; Geology; Seismology; Earth science; Petroleum engineering","score_opus":0.052935733191503034,"score_gpt":0.24300900607457981,"score_spread":0.1900732728830768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034557646","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.102032244,0.79724205,0.014844057,0.0072960733,0.0020347503,0.00027816393,0.0036151852,0.00046854987,0.07218883],"genre_scores_gemma":[0.3831957,0.59916145,0.0032804543,0.0024209714,0.001328677,0.00012095533,0.002414399,0.00005450735,0.008022924],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995185,0.00011411396,0.00010533464,0.000063622254,0.00014811971,0.000050296243],"domain_scores_gemma":[0.9985171,0.00075355987,0.0004950013,0.000052086027,0.00014778489,0.0000343666],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005083714,0.00033799073,0.00032088938,0.0014214308,0.0002140283,0.00066128856,0.00037007354,0.0006746976,0.004313308],"category_scores_gemma":[0.0025116128,0.000117856696,0.0003043886,0.0017755056,0.0005655276,0.0006217103,0.00062432175,0.00049485505,0.0007899902],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023464194,0.000060045168,0.02684716,0.029469114,0.00029244524,0.0065420754,0.0021303955,0.0014192238,0.006688679,0.021062495,0.038611893,0.86664176],"study_design_scores_gemma":[0.0000439873,0.000410606,0.07459598,0.01984043,0.00041426788,0.027229674,0.0028819996,0.00067569385,0.0072311154,0.017441254,0.8491383,0.00009665968],"about_ca_topic_score_codex":0.0015256875,"about_ca_topic_score_gemma":0.002211098,"teacher_disagreement_score":0.004313308,"about_ca_system_score_codex":0.0005543906,"about_ca_system_score_gemma":0.00055296125,"threshold_uncertainty_score":0.01442951},"labels":[],"label_agreement":null},{"id":"W3034697622","doi":"","title":"Lithospheric structure at the leading edge of the North American craton: Imaging the Shield-Cordillera transition in western Canada by teleseismic Rayleigh-wave analysis","year":2013,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Craton; Shield; Lithosphere; Seismology; Baltic Shield; Indian Shield; Enhanced Data Rates for GSM Evolution; Paleontology; Tectonics","score_opus":0.005272225372988024,"score_gpt":0.17176793304782903,"score_spread":0.166495707674841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3034697622","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99722195,0.00018772826,0.00008926251,0.000053154225,0.0000037698371,0.000009262648,0.0005337682,0.000018649282,0.0018824289],"genre_scores_gemma":[0.99830985,0.00015399256,0.00031123377,0.000018815193,0.0000033149245,0.000004282567,0.00037512326,0.000008381182,0.00081510906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998983,0.000003442003,0.0000037646325,0.000021932654,0.000027093854,0.000045449546],"domain_scores_gemma":[0.9997689,0.000012512116,0.000027147764,0.0000072277276,0.000120592595,0.00006360458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012506901,0.00039349924,0.00025139764,0.0017307049,0.0017171475,0.0010681968,0.0006233387,0.00045718867,0.0016001642],"category_scores_gemma":[0.00044614755,0.00019423685,0.00016930047,0.002417013,0.00047792992,0.00029595825,0.00063667586,0.0003238833,0.0002774955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004636341,0.00012871006,0.91857934,0.00008679218,0.00009360107,0.000784412,0.004131399,0.0022922056,0.02921871,0.0006581338,0.0021426766,0.041420303],"study_design_scores_gemma":[0.000008055911,0.000008246464,0.99636996,0.000014009018,0.00001479396,0.00005261537,0.0010519353,0.0011841119,0.00040843326,0.000027217888,0.00085256866,0.000008145315],"about_ca_topic_score_codex":0.965009,"about_ca_topic_score_gemma":0.9867193,"teacher_disagreement_score":0.034991026,"about_ca_system_score_codex":0.004827515,"about_ca_system_score_gemma":0.0064994395,"threshold_uncertainty_score":0.07039416},"labels":[],"label_agreement":null},{"id":"W3035173801","doi":"10.1144/sp505-2019-125","title":"Faulting within the San Juan–southern Gulf Islands Archipelagos, upper plate deformation of the Cascadia subduction complex","year":2020,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Commission Géologique du Canada","keywords":"Geology; Subduction; Forearc; Seismology; Archipelago; North American Plate; Bathymetry; Terrane; Fault (geology); Island arc; Plate tectonics; Paleontology; Tectonics; Oceanography","score_opus":0.038207189102792825,"score_gpt":0.22711859642156837,"score_spread":0.18891140731877554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035173801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99651885,0.00022094947,0.000021828986,0.00003796126,0.0000013763896,0.0000033530052,0.0001655037,0.0000048747524,0.0030251695],"genre_scores_gemma":[0.9982652,0.00018181864,0.00006128872,0.000006218543,0.0000015145773,0.0000034973802,0.0002745225,0.0000017917878,0.001204111],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999516,0.000005852643,0.000003557555,0.000016559121,0.000012732393,0.0000096690255],"domain_scores_gemma":[0.9998574,0.0000145702115,0.00003778155,0.000009423056,0.000047819238,0.000032944947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010223783,0.0001491179,0.00011262338,0.0010666003,0.00048954994,0.0005303114,0.00013233934,0.00010697434,0.001229222],"category_scores_gemma":[0.0004307402,0.0000997189,0.00005666401,0.0010809848,0.00046158562,0.00014224292,0.00049327174,0.00010821103,0.00012008792],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000064059175,0.000009631597,0.9788319,0.00005060008,0.00003171543,0.00046375487,0.0036309701,0.00092950213,0.0037850842,0.0002829905,0.0005625972,0.011357256],"study_design_scores_gemma":[0.0000010047214,0.0000028369282,0.99848515,0.000007379085,0.0000021097223,0.00003216352,0.000685572,0.000067124856,0.00003630762,0.000016226642,0.00066324114,9.721836e-7],"about_ca_topic_score_codex":0.43864435,"about_ca_topic_score_gemma":0.68996096,"teacher_disagreement_score":0.43864435,"about_ca_system_score_codex":0.0012251777,"about_ca_system_score_gemma":0.0008051774,"threshold_uncertainty_score":0.8721823},"labels":[],"label_agreement":null},{"id":"W3035271628","doi":"","title":"Probabilistic Seismic Hazard Analysis of Victoria, British Columbia, Canada: Considering an Active Leech River Fault","year":2017,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Leech; Fault (geology); Hazard; Seismic hazard; Seismology; Probabilistic logic; Geology; Geography; Computer science; Artificial intelligence","score_opus":0.016878027261212677,"score_gpt":0.21733470232413307,"score_spread":0.2004566750629204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035271628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896808,0.00020930149,0.0015483041,0.0006066305,0.000014084244,0.000050102703,0.0018786866,0.00004803213,0.0059640314],"genre_scores_gemma":[0.99535537,0.0001352225,0.0007500953,0.00003628246,0.000004766609,0.000012291435,0.0006783552,0.000012889743,0.0030147093],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99962676,0.00006220742,0.000017482253,0.000052075924,0.00007629929,0.00016519088],"domain_scores_gemma":[0.99890995,0.0003830772,0.00010983817,0.000045791203,0.0003817515,0.0001696172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007337798,0.0006104378,0.00067448744,0.0012727943,0.0017282292,0.002165897,0.0023138896,0.0014570049,0.0031854908],"category_scores_gemma":[0.0033692135,0.00071138045,0.0006793659,0.001966567,0.0010090811,0.0005981922,0.0008338264,0.00093920797,0.00019171278],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002334279,0.00008122922,0.04846367,0.00005909095,0.00009446832,0.0005846767,0.00012302816,0.93721026,0.00050349836,0.003208324,0.001989393,0.007448931],"study_design_scores_gemma":[0.00004045054,0.00003284096,0.037782848,0.000020770014,0.00007228984,0.000046151228,0.0005479834,0.9593359,0.00016666375,0.00110283,0.0008101953,0.000041050534],"about_ca_topic_score_codex":0.98962164,"about_ca_topic_score_gemma":0.9908601,"teacher_disagreement_score":0.025494,"about_ca_system_score_codex":0.025494,"about_ca_system_score_gemma":0.025760062,"threshold_uncertainty_score":0.18497282},"labels":[],"label_agreement":null},{"id":"W3035304857","doi":"","title":"Detection and Location of Low Frequency Earthquakes Using Cross-station Correlation","year":2013,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Seismology; Geology; Waveform; Seismogram; Epicenter; Coherence (philosophical gambling strategy); Geodesy; Subduction; Slip (aerodynamics); Pacific Plate; Tectonics; Physics; Telecommunications; Computer science","score_opus":0.018320375243951158,"score_gpt":0.23384044222703007,"score_spread":0.2155200669830789,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035304857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9693449,0.00009309428,0.01996034,0.00003629393,0.000008123386,0.000047453545,0.004572433,0.0006193541,0.005318125],"genre_scores_gemma":[0.98557264,0.000046840167,0.009435621,0.000008673173,0.0000068052245,0.00003239638,0.004041475,0.000054003933,0.0008015303],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99969256,0.000024715771,0.00001897773,0.0001235639,0.00009444645,0.000045791254],"domain_scores_gemma":[0.9987903,0.00022828937,0.0002790197,0.00015023616,0.00044104634,0.00011118744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033076108,0.00030841923,0.00023370872,0.0039369646,0.0003091434,0.00060237106,0.00036392332,0.00021260396,0.0021354193],"category_scores_gemma":[0.0020308914,0.00019458165,0.00020842034,0.003537298,0.00016198787,0.00028793912,0.000794062,0.00015700032,0.00063047657],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014486072,0.000067791334,0.86207956,0.00012923781,0.00018654525,0.00031375737,0.0006819983,0.010729709,0.037458684,0.0006178682,0.0025172506,0.08507277],"study_design_scores_gemma":[0.000007684571,0.000030197816,0.95640475,0.000009979192,0.000046150624,0.00013411867,0.00016785823,0.037286937,0.0043078326,0.00014308083,0.0014415815,0.000019862751],"about_ca_topic_score_codex":0.029010024,"about_ca_topic_score_gemma":0.0699346,"teacher_disagreement_score":0.029010024,"about_ca_system_score_codex":0.00042553456,"about_ca_system_score_gemma":0.0005077805,"threshold_uncertainty_score":0.057682335},"labels":[],"label_agreement":null},{"id":"W3035402776","doi":"10.1093/gji/ggaa285","title":"Uncovering the physical controls of deep subduction zone slow slip using supervised classification of subducting plate features","year":2020,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Subduction; Slip (aerodynamics); Seismology; Trench; Slab; Random forest; Tectonics; Geophysics; Machine learning; Computer science","score_opus":0.03156453283981898,"score_gpt":0.2501721459494933,"score_spread":0.2186076131096743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035402776","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99146616,0.00004995384,0.007788023,0.000040993014,0.00000404666,0.000013880136,0.00017426642,0.00008902025,0.00037375273],"genre_scores_gemma":[0.99747086,0.000012646488,0.0020950479,0.0000051488346,0.000003898178,0.0000064677743,0.00026904905,0.0000043889127,0.00013241537],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979967,0.000050947237,0.000015659252,0.00007196459,0.000025606692,0.00003614247],"domain_scores_gemma":[0.9990513,0.0003506954,0.00026466197,0.00010460405,0.00014942526,0.00007926605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006931872,0.00042820518,0.000384696,0.00082385936,0.00018735048,0.0006624594,0.00033635553,0.0002793816,0.0004773699],"category_scores_gemma":[0.0013267702,0.00013275148,0.00045135713,0.00035086682,0.00030596263,0.00037878918,0.0003638,0.0003402392,0.00018663747],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033653568,0.00034808266,0.73376137,0.00007771927,0.0002301264,0.0001559259,0.00023249845,0.15467162,0.018298756,0.0006359932,0.00079214736,0.09045918],"study_design_scores_gemma":[0.000007733153,0.000046899902,0.14126575,0.000011273207,0.0000188358,0.000026357757,0.00010392979,0.855959,0.0017232454,0.0007054556,0.000121229714,0.00001030769],"about_ca_topic_score_codex":0.0057869502,"about_ca_topic_score_gemma":0.0065221502,"teacher_disagreement_score":0.0057869502,"about_ca_system_score_codex":0.00036963527,"about_ca_system_score_gemma":0.00039531977,"threshold_uncertainty_score":0.011506557},"labels":[],"label_agreement":null},{"id":"W3035681603","doi":"10.1029/2019jb019095","title":"Are Aftershock Sequences Pertinent to Long‐Term Seismic Hazard Assessments? Insights From the Temporal ETAS Model","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Aftershock; Induced seismicity; Seismology; Magnitude (astronomy); Geology; Poisson distribution; Term (time); Hazard; Seismic hazard; Sequence (biology); Statistics; Mathematics; Physics","score_opus":0.11039703419095823,"score_gpt":0.354051205181799,"score_spread":0.24365417099084077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035681603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7147816,0.0006133583,0.26789728,0.0027974576,0.00008078498,0.00007326977,0.0010652528,0.0002645687,0.012426489],"genre_scores_gemma":[0.99366003,0.00022617284,0.0041796737,0.00005749052,0.00005050311,0.000024490044,0.00024028563,0.000025165955,0.0015362807],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995813,0.00014087027,0.00003298322,0.00011309521,0.00007228181,0.000059367416],"domain_scores_gemma":[0.9933269,0.0038564764,0.0016364177,0.00031517862,0.0005650364,0.00030002964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027906226,0.00040993287,0.000479225,0.0010864037,0.00027812747,0.0016264266,0.0011068654,0.00083334104,0.002404647],"category_scores_gemma":[0.015476603,0.00030559386,0.00051319844,0.0010357975,0.0007925614,0.0024530722,0.00087415864,0.00075191405,0.00031311155],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001460829,0.00008429839,0.04359633,0.00007557231,0.00009179409,0.00025797103,0.00022236099,0.8550491,0.0017945232,0.08060927,0.0013884393,0.016684199],"study_design_scores_gemma":[0.000004623205,0.000011429891,0.003424613,0.000007630203,0.000009216745,0.000036934092,0.000056434543,0.9776642,0.000086484986,0.018430375,0.00025947264,0.000008675299],"about_ca_topic_score_codex":0.012282706,"about_ca_topic_score_gemma":0.0074730054,"teacher_disagreement_score":0.012282706,"about_ca_system_score_codex":0.0009463581,"about_ca_system_score_gemma":0.0009601013,"threshold_uncertainty_score":0.024422407},"labels":[],"label_agreement":null},{"id":"W3035894658","doi":"10.1080/21664250.2020.1780719","title":"The 2018 Sulawesi tsunami in Palu city as a result of several landslides and coseismic tsunamis","year":2020,"lang":"en","type":"article","venue":"Coastal Engineering Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Institut National de la Recherche Scientifique","funders":"Japan Society for the Promotion of Science","keywords":"Geology; Seismology; Landslide; Shore; Bathymetry; Submarine landslide; Seafloor spreading; Tsunami earthquake; Bay; Submarine pipeline; Submarine; Oceanography","score_opus":0.012616209159544391,"score_gpt":0.19025856946859446,"score_spread":0.17764236030905006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035894658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984669,0.000041706917,0.00014740627,0.00013568233,0.000008229334,0.000008971737,0.00006859619,0.000008666085,0.0011137608],"genre_scores_gemma":[0.99850583,0.000117881376,0.00024016309,0.00002049675,0.0000028627571,0.000006565052,0.00014319133,0.0000022994348,0.0009607083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999597,0.0000057136795,0.0000034477534,0.000009177819,0.000010241547,0.000011696103],"domain_scores_gemma":[0.9999294,0.000010421994,0.000018471093,0.0000062439576,0.000023113213,0.000012318632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011202154,0.00021567308,0.0001181745,0.00030315976,0.00057797524,0.00061239407,0.0002047836,0.00025110034,0.0009591696],"category_scores_gemma":[0.00026153494,0.00018244957,0.00014541416,0.00061484595,0.0003949224,0.00037803018,0.0004518862,0.00031215153,0.00013936445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003044547,0.00022312757,0.90897435,0.00017565975,0.000081344355,0.010139335,0.006416879,0.019185554,0.008368586,0.0016274217,0.0033693074,0.041134056],"study_design_scores_gemma":[0.000052408832,0.00024813178,0.9362902,0.00006966156,0.0000990352,0.00121069,0.013650121,0.037718162,0.0023658518,0.001143389,0.0071134833,0.00003879584],"about_ca_topic_score_codex":0.064512,"about_ca_topic_score_gemma":0.13960828,"teacher_disagreement_score":0.064512,"about_ca_system_score_codex":0.0012951783,"about_ca_system_score_gemma":0.00092704355,"threshold_uncertainty_score":0.12827301},"labels":[],"label_agreement":null},{"id":"W3035902353","doi":"","title":"Lithospheric thickness inferred from Australian post-glacial sea-level change: the influence of a ductile crustal zone","year":2003,"lang":"en","type":"article","venue":"EAEJA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Lithosphere; Geology; Crust; Post-glacial rebound; Glacial period; Geophysics; Seismology; Geomorphology; Tectonics","score_opus":0.04058237318347609,"score_gpt":0.24142897857548865,"score_spread":0.20084660539201254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035902353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99877447,0.000036315163,0.00046242573,0.00006828362,0.000002068573,0.0000019195027,0.00008163708,0.000017841305,0.00055508845],"genre_scores_gemma":[0.9997482,0.000017349468,0.00013260433,0.0000054738293,8.253244e-7,7.9511204e-7,0.00003454826,0.0000021539556,0.0000580932],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999835,0.00006419211,0.000012188905,0.0000314953,0.000025303614,0.000031791613],"domain_scores_gemma":[0.9994487,0.00021584485,0.000105570456,0.00006367001,0.00010350938,0.00006271483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065079884,0.0003067524,0.0002203978,0.0004390441,0.0003233739,0.00082030677,0.000882162,0.0006794695,0.0008107005],"category_scores_gemma":[0.0031184442,0.00042610307,0.00036204603,0.0003596283,0.00054809486,0.0004743797,0.00060338323,0.00034589812,0.00014132388],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020349235,0.000054028405,0.35886294,0.00007447094,0.00010602862,0.00024502055,0.00024404484,0.6264454,0.007719722,0.0010908768,0.00021503573,0.0047388286],"study_design_scores_gemma":[0.00005064321,0.00011904202,0.24825767,0.00002176912,0.00006245805,0.000066422304,0.00016745499,0.7483355,0.0020068237,0.0006246908,0.0002591974,0.000028331588],"about_ca_topic_score_codex":0.068517454,"about_ca_topic_score_gemma":0.042465746,"teacher_disagreement_score":0.068517454,"about_ca_system_score_codex":0.0011805923,"about_ca_system_score_gemma":0.0005761014,"threshold_uncertainty_score":0.13623726},"labels":[],"label_agreement":null},{"id":"W3036735605","doi":"10.1029/2020gl088168","title":"Injection‐Induced Earthquakes on Complex Fault Zones of the Raton Basin Illuminated by Machine‐Learning Phase Picker and Dense Nodal Array","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Seismology; Induced seismicity; Geology; Hypocenter; Tectonics; Structural basin; Daytime; Basement; Focal mechanism; Fault (geology); Magnitude (astronomy); Geomorphology","score_opus":0.05314672318528116,"score_gpt":0.29197023750309015,"score_spread":0.238823514317809,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036735605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995505,0.000011711046,0.00011608474,0.000006691622,0.0000012677419,0.0000017591086,0.000103809296,0.000010589789,0.0001975148],"genre_scores_gemma":[0.99962986,0.000007273677,0.00012712313,0.000001346775,0.0000013545757,9.932247e-7,0.00014905863,0.0000013531129,0.00008157028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993753,0.000010227071,0.000004245474,0.000018316088,0.00001150805,0.000018026261],"domain_scores_gemma":[0.999811,0.000027262755,0.000049997238,0.00001890344,0.0000549261,0.000038008806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011943287,0.00020692243,0.00013552647,0.0011095433,0.00017172981,0.00024542774,0.00017760132,0.00013666757,0.00074679573],"category_scores_gemma":[0.00030854245,0.0001063322,0.000106799846,0.0007795403,0.00021255593,0.00015059885,0.00024529183,0.000084557796,0.000086198605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003573312,0.00009201949,0.9352406,0.000038004113,0.00006549986,0.00080746,0.0005272792,0.009839935,0.02320883,0.00027258962,0.00064792164,0.02890258],"study_design_scores_gemma":[0.0000035214168,0.000024453037,0.9834222,0.000004378572,0.000013786944,0.000061169885,0.00016039684,0.015398625,0.0006623498,0.000039099254,0.00020484472,0.000005329837],"about_ca_topic_score_codex":0.021169467,"about_ca_topic_score_gemma":0.044702053,"teacher_disagreement_score":0.021169467,"about_ca_system_score_codex":0.0002586236,"about_ca_system_score_gemma":0.0002141706,"threshold_uncertainty_score":0.042092443},"labels":[],"label_agreement":null},{"id":"W3039592234","doi":"10.1016/j.epsl.2020.116413","title":"Rupture to the trench? Frictional properties and fracture energy of incoming sediments at the Cascadia subduction zone","year":2020,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Japan Society for the Promotion of Science; Natural Environment Research Council; Sight Research UK; Geological Society of America","keywords":"Geology; Subduction; Lithology; Trench; Fracture (geology); Seismology; Shear (geology); Petrology; Geotechnical engineering; Tectonics","score_opus":0.015889899811016565,"score_gpt":0.17297689668636354,"score_spread":0.15708699687534697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3039592234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991487,0.000038516566,0.000035332752,0.00002551628,0.0000012540534,0.0000010117072,0.00007445115,0.0000048824227,0.0006701984],"genre_scores_gemma":[0.99968946,0.000023789511,0.0000119316865,0.0000047012068,0.0000012158579,6.364485e-7,0.00004187483,0.0000028281486,0.00022356333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989676,0.000007932726,0.0000062670015,0.000032822994,0.00001689409,0.000039279148],"domain_scores_gemma":[0.9997211,0.00005347406,0.000060247286,0.000034538953,0.000059580376,0.00007097701],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020465087,0.00023821623,0.0004761356,0.0010285944,0.0008134154,0.0012125641,0.0004893046,0.0007081804,0.0041893474],"category_scores_gemma":[0.0013456745,0.0004980531,0.0002587104,0.0010314106,0.00052296155,0.0007847945,0.0008452845,0.00036258972,0.00057459367],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024505382,0.00006033079,0.9788735,0.000025762332,0.00010286581,0.0005153272,0.00065533165,0.0063190446,0.0063043307,0.0003410267,0.00022593097,0.0063315555],"study_design_scores_gemma":[0.0000021765152,0.000015495074,0.998384,0.0000028332747,0.000005299411,0.000032449272,0.0002408287,0.0010617464,0.00009115407,0.00004869471,0.00011129175,0.0000040970986],"about_ca_topic_score_codex":0.053304866,"about_ca_topic_score_gemma":0.092532486,"teacher_disagreement_score":0.053304866,"about_ca_system_score_codex":0.0008570927,"about_ca_system_score_gemma":0.00041985538,"threshold_uncertainty_score":0.10598916},"labels":[],"label_agreement":null},{"id":"W3039720686","doi":"10.1029/2020jb019817","title":"Effects of Earthquake Recurrence on Localization of Interseismic Deformation Around Locked Strike‐Slip Faults","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Viscoelasticity; Seismology; Geodetic datum; Slip (aerodynamics); Deformation (meteorology); Fault (geology); Shear zone; Rheology; Geodesy; Materials science; Physics","score_opus":0.038905745073269236,"score_gpt":0.3025583879846737,"score_spread":0.2636526429114045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3039720686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999218,0.000045869496,0.00036171655,0.000012418204,0.0000016307542,0.000001168809,0.000030565465,0.00001592113,0.00031268215],"genre_scores_gemma":[0.9998733,0.000009991557,0.000028224507,0.000001962305,5.447731e-7,5.8615376e-7,0.000015541114,0.00000302366,0.000066729124],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998758,0.000047296904,0.00001008443,0.000025679909,0.0000144337255,0.000026625221],"domain_scores_gemma":[0.9980015,0.0011362268,0.0004465222,0.00013939042,0.00009981089,0.00017657103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033961263,0.00025381084,0.00025173678,0.00031801776,0.00012369841,0.0004354701,0.00021918924,0.00027310857,0.0015833774],"category_scores_gemma":[0.0027417683,0.00012164799,0.00027604078,0.00019835019,0.00024235944,0.00029864383,0.00039530473,0.00018040554,0.00018798858],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025399853,0.00042590353,0.48461667,0.00015483095,0.00034680802,0.0014102279,0.0003203378,0.37182936,0.11539544,0.00059997273,0.0003631454,0.021997314],"study_design_scores_gemma":[0.00006516416,0.0023804896,0.5793368,0.000034850338,0.00022487415,0.00038982483,0.00036740498,0.40242186,0.013958108,0.00045337903,0.00033333898,0.00003381401],"about_ca_topic_score_codex":0.0021287238,"about_ca_topic_score_gemma":0.0017475154,"teacher_disagreement_score":0.0021287238,"about_ca_system_score_codex":0.00020971146,"about_ca_system_score_gemma":0.00011118095,"threshold_uncertainty_score":0.005296886},"labels":[],"label_agreement":null},{"id":"W3040122085","doi":"10.1029/2020jb019430","title":"Depth‐Scanning Algorithm: Accurate, Automatic, and Efficient Determination of Focal Depths for Local and Regional Earthquakes","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Waveform; Geology; Algorithm; Phase (matter); Seismology; Focal mechanism; Tectonics; Constraint (computer-aided design); Computer science; Mathematics; Geometry; Physics; Telecommunications","score_opus":0.06468570908977624,"score_gpt":0.3342686452445277,"score_spread":0.2695829361547515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040122085","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.037640594,0.000085078434,0.9598378,0.000048365033,0.000018442472,0.00005890469,0.00009926302,0.0015552662,0.00065630104],"genre_scores_gemma":[0.15675509,0.00008480427,0.8421001,0.000026958493,0.000013029005,0.000067563,0.00020273976,0.000104969375,0.00064475194],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998148,0.000030028066,0.000013924041,0.000045080218,0.00007504808,0.000021049973],"domain_scores_gemma":[0.99960023,0.00010913009,0.000059863112,0.00005892075,0.00014523041,0.000026642057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038617456,0.00060193316,0.000340485,0.0010524873,0.00024250137,0.00043822685,0.0007862441,0.00046914618,0.0016891089],"category_scores_gemma":[0.0015776256,0.00032493082,0.00024303718,0.0007708002,0.00021058448,0.0007100431,0.00058943377,0.00038412065,0.00071105413],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026173267,0.00007550642,0.0052935,0.00008594845,0.00003649407,0.000104444305,0.00014580543,0.039977234,0.17041437,0.0030997545,0.0027492214,0.7777559],"study_design_scores_gemma":[0.000073624746,0.00010677637,0.0056078364,0.000011691686,0.00002460876,0.00029548502,0.000062319064,0.92837626,0.05921815,0.0017739536,0.0044104587,0.000038906855],"about_ca_topic_score_codex":0.0025121933,"about_ca_topic_score_gemma":0.0040263925,"teacher_disagreement_score":0.0025121933,"about_ca_system_score_codex":0.0002473069,"about_ca_system_score_gemma":0.00085209764,"threshold_uncertainty_score":0.0056506395},"labels":[],"label_agreement":null},{"id":"W3040174305","doi":"10.1785/0120200002","title":"Activation Rate of Seismicity for Hydraulic Fracture Wells in the Western Canada Sedimentary Basin","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Geology; Induced seismicity; Structural basin; Seismology; Sedimentary rock; Magnitude (astronomy); Hydraulic fracturing; Monte Carlo method; Fracture (geology); Maximum magnitude; Geomorphology; Geochemistry; Geotechnical engineering; Statistics","score_opus":0.016647166520238028,"score_gpt":0.20200199597092997,"score_spread":0.18535482945069193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040174305","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99830353,0.000041188297,0.00013632677,0.000027319307,8.722773e-7,0.0000056738977,0.0010552811,0.000009367433,0.00042045815],"genre_scores_gemma":[0.9993253,0.000026358593,0.00007337783,0.0000030807926,3.293269e-7,0.0000018337347,0.0003889205,8.835302e-7,0.00017985793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997403,0.000026197238,0.000018125955,0.000050723054,0.00010326356,0.000061433406],"domain_scores_gemma":[0.99890935,0.00014952062,0.00038034894,0.00004330223,0.00035243382,0.00016503628],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033883582,0.00013990837,0.00014585185,0.0013249756,0.00046005016,0.00055441674,0.00037121272,0.00020926206,0.0011576572],"category_scores_gemma":[0.0018147548,0.00011898783,0.00023897857,0.0013851469,0.00040209232,0.0001800924,0.0004445787,0.00020000507,0.00009746655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000374558,0.0000063086877,0.99489236,0.00001058473,0.000032037704,0.00006289444,0.00013704356,0.0015368048,0.00046838753,0.00009081224,0.00020640453,0.002518972],"study_design_scores_gemma":[0.0000015735326,0.000007885511,0.9957633,0.000004479368,0.00000862073,0.000031932726,0.00021021183,0.0035990572,0.00017391227,0.00003137036,0.00016118836,0.0000064479773],"about_ca_topic_score_codex":0.9193896,"about_ca_topic_score_gemma":0.9592085,"teacher_disagreement_score":0.080610394,"about_ca_system_score_codex":0.004812072,"about_ca_system_score_gemma":0.0033503533,"threshold_uncertainty_score":0.16217017},"labels":[],"label_agreement":null},{"id":"W3040695789","doi":"","title":"Crustal strain rates and seismic hazard from seismicity and GPS measurements along the St Lawrence Valley, Quebec","year":2004,"lang":"en","type":"article","venue":"AGUSM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Seismology; Geology; Seismic hazard; Global Positioning System","score_opus":0.031450447008024414,"score_gpt":0.2263753568388681,"score_spread":0.1949249098308437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040695789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9797958,0.0003762919,0.000335259,0.00048501528,0.000015090992,0.000032835604,0.012325331,0.000052168623,0.0065822164],"genre_scores_gemma":[0.9880342,0.00020573159,0.0003390574,0.000067232366,0.0000059341087,0.000016336247,0.004747097,0.000014055623,0.0065703834],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996754,0.000051807987,0.000020236743,0.000061562074,0.00010705186,0.0000839767],"domain_scores_gemma":[0.99818003,0.00022664918,0.00021739135,0.00004891289,0.0011060794,0.00022094979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045746288,0.00025688054,0.00025622034,0.0011909776,0.0012906257,0.0009197237,0.0009412272,0.00040389196,0.0040397733],"category_scores_gemma":[0.0022557438,0.00023658812,0.0002463432,0.0023302676,0.00043571633,0.00038019737,0.0004536194,0.0005116206,0.00046163733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012829715,0.000049136106,0.97569287,0.00003832966,0.00010684131,0.00013316527,0.0006559045,0.002634717,0.0005489557,0.00033083934,0.0058551584,0.013825952],"study_design_scores_gemma":[0.000011647486,0.000008472021,0.99590766,0.000022388982,0.000017084925,0.000016047108,0.00044367448,0.0018045331,0.00007287438,0.00002563949,0.001658323,0.000011657553],"about_ca_topic_score_codex":0.9971379,"about_ca_topic_score_gemma":0.9992072,"teacher_disagreement_score":0.015211261,"about_ca_system_score_codex":0.015211261,"about_ca_system_score_gemma":0.011252368,"threshold_uncertainty_score":0.11036593},"labels":[],"label_agreement":null},{"id":"W3040748029","doi":"10.1029/2020gl087254","title":"Stress Chatter via Fluid Flow and Fault Slip in a Hydraulic Fracturing‐Induced Earthquake Sequence in the Montney Formation, British Columbia","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; McGill University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Deutsche Forschungsgemeinschaft","keywords":"Geology; Aftershock; Seismology; Hydraulic fracturing; Seismometer; Slip (aerodynamics); Fluid pressure; Differential stress; Shear stress; Fluid dynamics; Geotechnical engineering; Deformation (meteorology)","score_opus":0.044634847299519886,"score_gpt":0.26609342637842703,"score_spread":0.22145857907890715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040748029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99955684,0.00000915465,0.000034829096,0.000021042675,2.9921992e-7,0.0000017192484,0.00009217942,0.0000045895003,0.0002792586],"genre_scores_gemma":[0.99970204,0.000009778302,0.000033758784,0.0000034494528,3.3416046e-7,0.0000012385175,0.00006972404,8.7294796e-7,0.00017872383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999031,0.000010461552,0.0000062376625,0.000022217595,0.00002375641,0.00003430486],"domain_scores_gemma":[0.9996934,0.000045246932,0.00008633853,0.000015609448,0.00009103326,0.00006844937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010414191,0.00016527476,0.00014964507,0.000942884,0.0005600311,0.00071859243,0.00039346263,0.00027767225,0.0012301848],"category_scores_gemma":[0.0006555626,0.0001819017,0.00011288088,0.0009923478,0.0005153239,0.00019579826,0.0004657966,0.00024289267,0.00011900474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007912083,0.0000487308,0.98465794,0.000010513297,0.000036961377,0.00027834496,0.00065838953,0.0018618399,0.005825854,0.000083859006,0.00024065831,0.0062179016],"study_design_scores_gemma":[0.000001439053,0.000005233574,0.9979151,0.0000021038138,0.0000037134253,0.000012951034,0.0003459602,0.0015066233,0.00012103201,0.000013199531,0.000069591246,0.000003037598],"about_ca_topic_score_codex":0.8658914,"about_ca_topic_score_gemma":0.9428075,"teacher_disagreement_score":0.1341086,"about_ca_system_score_codex":0.004253775,"about_ca_system_score_gemma":0.0021583603,"threshold_uncertainty_score":0.26979673},"labels":[],"label_agreement":null},{"id":"W3040828023","doi":"","title":"Post Earthquake Investigation Of The Mw7.8 Haida Gwaii, Canada, Rupture Area And Constraints On Earthquake Source Models","year":2013,"lang":"en","type":"article","venue":"AGUFM","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Earthquake prediction","score_opus":0.01508609587864024,"score_gpt":0.17441924981847734,"score_spread":0.1593331539398371,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040828023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9777272,0.00018858371,0.00071945845,0.000273246,0.0000069460107,0.000045259225,0.0068182442,0.00008757019,0.014133505],"genre_scores_gemma":[0.98689747,0.0001861944,0.0013792231,0.000031368778,0.0000024869696,0.000020631995,0.0040084547,0.0000267627,0.0074474565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985015,0.000008123588,0.0000064410983,0.000022563994,0.0000662721,0.00004644651],"domain_scores_gemma":[0.99940455,0.000042188174,0.000055057768,0.000023224584,0.00040063437,0.00007432398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026182085,0.0002753088,0.00026335457,0.001305225,0.001981454,0.0011377204,0.0011883582,0.00038133442,0.0033806893],"category_scores_gemma":[0.0013842777,0.000317075,0.00022982291,0.0025878586,0.00042253206,0.00034992598,0.00050548546,0.0004715365,0.00046008898],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078558427,0.00018164176,0.7765209,0.00032316873,0.00018937464,0.0013775572,0.005483083,0.06251055,0.013120702,0.016559279,0.015981155,0.106966935],"study_design_scores_gemma":[0.000040289382,0.000040096726,0.94024515,0.000044571232,0.000059839746,0.0001417648,0.0032895627,0.042030837,0.0016036726,0.00055256597,0.01191057,0.0000410195],"about_ca_topic_score_codex":0.99577713,"about_ca_topic_score_gemma":0.99816895,"teacher_disagreement_score":0.021789921,"about_ca_system_score_codex":0.021789921,"about_ca_system_score_gemma":0.02809982,"threshold_uncertainty_score":0.15809768},"labels":[],"label_agreement":null},{"id":"W3040996902","doi":"10.5194/egusphere-egu2020-21355","title":"The basin effect and liquefaction in the catastrophe models: Case study &amp;#8211; Vancouver region, Canada","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Structural basin; Liquefaction; Geology; Sedimentary basin; Seismology; Alluvium; Underwriting; Geotechnical engineering; Geomorphology","score_opus":0.027365851610354104,"score_gpt":0.2120750238442097,"score_spread":0.1847091722338556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040996902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96770656,0.00065120246,0.0021388424,0.0007543883,0.000038112445,0.00013651831,0.0024917831,0.00008593917,0.025996592],"genre_scores_gemma":[0.9926267,0.00035783235,0.0011269825,0.00004699006,0.000009564982,0.000029309542,0.000675498,0.00001679344,0.0051101786],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997508,0.00006356977,0.000009639107,0.000026276128,0.000049506823,0.000100214755],"domain_scores_gemma":[0.99902415,0.00044636993,0.000071304275,0.000038427308,0.00026639213,0.00015326937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049742585,0.00088591373,0.0005314035,0.0008812094,0.0015148945,0.0016945848,0.0017265527,0.0013053593,0.002337363],"category_scores_gemma":[0.0014080917,0.00036245582,0.0007226748,0.0011025071,0.0010521159,0.000361067,0.0008465806,0.0013249012,0.00016081608],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001115783,0.00018628768,0.026064647,0.000080422804,0.00006328823,0.001368402,0.00017788413,0.9582798,0.00051329494,0.0049553127,0.0047690766,0.0034299938],"study_design_scores_gemma":[0.000048541497,0.00006206906,0.014357348,0.0000346019,0.000045612393,0.00012548834,0.00091526425,0.98047847,0.00036956064,0.00095912244,0.0025692915,0.00003462963],"about_ca_topic_score_codex":0.9418232,"about_ca_topic_score_gemma":0.9359456,"teacher_disagreement_score":0.058176816,"about_ca_system_score_codex":0.008872878,"about_ca_system_score_gemma":0.006240345,"threshold_uncertainty_score":0.11703879},"labels":[],"label_agreement":null},{"id":"W3041529900","doi":"","title":"Remote Dynamic Earthquake Triggering in Shale Gas Basins in Canada and Implications for Triggering Mechanisms","year":2017,"lang":"en","type":"article","venue":"EGUGA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Shale gas; Oil shale; Seismology; Earth science; Paleontology","score_opus":0.019907185484786063,"score_gpt":0.23586267952930012,"score_spread":0.21595549404451406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041529900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973653,0.00013419938,0.00003479518,0.000117215444,0.0000015854122,0.0000043412856,0.00024139954,0.0000034010113,0.0020977727],"genre_scores_gemma":[0.99915826,0.00011668136,0.00003769368,0.000013392385,0.0000013348832,0.0000013863907,0.00014373915,0.0000017350092,0.0005258953],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981874,0.000013471355,0.000009153398,0.000027367372,0.000035234938,0.00009593398],"domain_scores_gemma":[0.9993255,0.0000988644,0.00011241225,0.000024772926,0.0002838122,0.00015464485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022580699,0.00016786598,0.00018867869,0.0013908234,0.002298229,0.0012160399,0.00061436155,0.00037569762,0.0024090735],"category_scores_gemma":[0.0014054967,0.00019413243,0.00014333913,0.001978577,0.0013211985,0.0005707121,0.0010107014,0.00035992375,0.00013564037],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001524964,0.0000555992,0.9715678,0.00005130251,0.00004652767,0.000593547,0.005951971,0.0020253197,0.002208519,0.00170536,0.0006736868,0.014967813],"study_design_scores_gemma":[0.0000056468502,0.000008663908,0.99137515,0.000022112212,0.000011348076,0.00005113552,0.006459748,0.0008184774,0.00013388113,0.00017768043,0.0009276448,0.000008488981],"about_ca_topic_score_codex":0.98673093,"about_ca_topic_score_gemma":0.9956892,"teacher_disagreement_score":0.016096635,"about_ca_system_score_codex":0.016096635,"about_ca_system_score_gemma":0.015393545,"threshold_uncertainty_score":0.11678982},"labels":[],"label_agreement":null},{"id":"W3041824822","doi":"10.1073/pnas.2001979117","title":"Active strike-slip faults and an outer frontal thrust in the Himalayan foreland basin","year":2020,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; University of Alberta","funders":"Cairn Energy; Natural Sciences and Engineering Research Council of Canada; Government of Canada","keywords":"Foreland basin; Geology; Thrust; Structural basin; Thrust fault; Seismology; Fold and thrust belt; Slip (aerodynamics); Geomorphology; Paleontology; Tectonics","score_opus":0.05144779377951659,"score_gpt":0.27515301771856154,"score_spread":0.22370522393904496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041824822","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968836,0.000356066,0.00004735785,0.00006704455,9.899645e-7,0.0000015297451,0.00007741821,0.000006808116,0.002559128],"genre_scores_gemma":[0.9996661,0.000124002,0.000032838998,0.0000070487404,0.0000014325767,5.960534e-7,0.000038397033,5.9476554e-7,0.00012891869],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994576,0.000010358786,0.0000041865937,0.000013127444,0.000009969123,0.000016615704],"domain_scores_gemma":[0.9998734,0.000025627294,0.000034835342,0.000009475601,0.00002442409,0.00003220566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007447977,0.000097166914,0.00011491496,0.0011246416,0.00067179144,0.0009434488,0.00013359352,0.0001785028,0.0013905632],"category_scores_gemma":[0.00029613916,0.00010348449,0.00006506737,0.0011062309,0.0005751372,0.00027929986,0.00035222532,0.00014306452,0.0001436978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011323207,0.00004118215,0.9523066,0.000077582496,0.00007174702,0.0020078206,0.0042965673,0.0018004528,0.013969939,0.0014387266,0.0003408141,0.023535334],"study_design_scores_gemma":[0.0000018899196,0.000007060091,0.9977442,0.000009583271,0.000007771783,0.00027871574,0.00081715075,0.00028519036,0.0001770566,0.00023065507,0.00043784062,0.0000029730938],"about_ca_topic_score_codex":0.032901887,"about_ca_topic_score_gemma":0.042620316,"teacher_disagreement_score":0.032901887,"about_ca_system_score_codex":0.00065553514,"about_ca_system_score_gemma":0.0003793151,"threshold_uncertainty_score":0.06542075},"labels":[],"label_agreement":null},{"id":"W3042146598","doi":"10.1785/0120190261","title":"A Study on the Largest Hydraulic-Fracturing-Induced Earthquake in Canada: Observations and Static Stress-Drop Estimation","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Seismology; Hypocenter; Geology; Seismometer; Hydraulic fracturing; Moment magnitude scale; Magnitude (astronomy); Microseism; Seismic moment; Maximum magnitude; Seismic hazard; Tectonics; Fault (geology); Geotechnical engineering; Induced seismicity","score_opus":0.04503977144415928,"score_gpt":0.2181974476064351,"score_spread":0.17315767616227584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042146598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980215,0.000039625655,0.00011361622,0.00002318278,0.0000012057864,0.0000125150955,0.0009996531,0.0000107328,0.0007781164],"genre_scores_gemma":[0.997741,0.00006876875,0.00022987585,0.000009017693,0.0000018444621,0.000004511769,0.001364917,0.0000032487292,0.00057687314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997861,0.000009498476,0.000008829304,0.00003525687,0.000087823966,0.000072561095],"domain_scores_gemma":[0.999153,0.000063894695,0.000098977886,0.000031399348,0.00048462691,0.000168094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020791878,0.00042010998,0.00029067666,0.0014678681,0.001205477,0.0005573972,0.0006450041,0.00029422325,0.00075171527],"category_scores_gemma":[0.00089044136,0.0002216667,0.00019753823,0.002579142,0.00038288021,0.00020337112,0.0003906491,0.00034548892,0.00018739566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011614658,0.00011935604,0.9738437,0.000044200544,0.00005413932,0.0005136382,0.0011578804,0.0017311815,0.006556771,0.00014502229,0.0007048427,0.015013179],"study_design_scores_gemma":[0.000003839614,0.000014726017,0.99620384,0.0000057373827,0.000009199097,0.000035938996,0.00065519504,0.002066863,0.00044874998,0.000010576146,0.0005377056,0.0000075590656],"about_ca_topic_score_codex":0.97785735,"about_ca_topic_score_gemma":0.9873145,"teacher_disagreement_score":0.022142649,"about_ca_system_score_codex":0.0068154675,"about_ca_system_score_gemma":0.0071523753,"threshold_uncertainty_score":0.04944986},"labels":[],"label_agreement":null},{"id":"W3042190424","doi":"10.1016/j.epsl.2020.116443","title":"Early Holocene Greenland-ice mass loss likely triggered earthquakes and tsunami","year":2020,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; Memorial University of Newfoundland","funders":"Nationale Geologiske Undersøgelser for Danmark og Grønland; Crafoordska Stiftelsen; AXA Research Fund; Royal Swedish Academy of Sciences; Durham University","keywords":"Deglaciation; Geology; Holocene; Greenland ice sheet; Ice sheet; Magnitude (astronomy); Intraplate earthquake; Surface exposure dating; Post-glacial rebound; Crust; Oceanography; Seismology; Physical geography; Climatology; Glacier; Paleontology; Moraine; Tectonics; Geography","score_opus":0.014851089973020964,"score_gpt":0.18813229652221825,"score_spread":0.1732812065491973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042190424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970265,0.00024067746,0.00034118418,0.00013265613,0.0000071085897,0.0000054472994,0.0007355829,0.000023597067,0.001487239],"genre_scores_gemma":[0.9982389,0.00019236363,0.00015922476,0.00004693282,0.0000046879695,0.0000040940467,0.00075304427,0.000006165876,0.0005946456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994063,0.0000043024274,0.000003000578,0.000014974331,0.000010146159,0.000026997168],"domain_scores_gemma":[0.9998884,0.000009037282,0.00004701759,0.00000744137,0.000020516245,0.000027584625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020165165,0.0003569426,0.00021795552,0.0007284807,0.0005187038,0.00083587767,0.00020298871,0.0002434788,0.002043457],"category_scores_gemma":[0.00034035064,0.00010215168,0.00030702274,0.0011640958,0.0003964595,0.00041690323,0.0005102485,0.00017426512,0.00021299944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006743388,0.000052270123,0.96264267,0.000057101293,0.00013120146,0.0005849821,0.00028224484,0.00846155,0.007260796,0.0013878983,0.0011751775,0.017896501],"study_design_scores_gemma":[0.0000023530347,0.000015021534,0.99504554,0.000009181866,0.00001690802,0.000072903145,0.00023729402,0.0023183227,0.00041554496,0.00034719665,0.0015157098,0.000004031386],"about_ca_topic_score_codex":0.06974141,"about_ca_topic_score_gemma":0.17295572,"teacher_disagreement_score":0.06974141,"about_ca_system_score_codex":0.0024842185,"about_ca_system_score_gemma":0.0010798187,"threshold_uncertainty_score":0.13867098},"labels":[],"label_agreement":null},{"id":"W3042360538","doi":"10.5194/egusphere-egu2020-3167","title":"Bivergent extension in the overriding plate above a slab tear (Dodecanese, Greece)","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Subduction; Shear zone; Lithosphere; Paleontology; Plate tectonics; Sinistral and dextral; Seismology; Tectonics","score_opus":0.04307202946056451,"score_gpt":0.22595275238961662,"score_spread":0.1828807229290521,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042360538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969578,0.00006137311,0.000037599693,0.000020739131,0.0000019006511,0.0000032156627,0.00015572057,0.0000027646768,0.002758905],"genre_scores_gemma":[0.9983621,0.00006478127,0.00007316511,0.00000676051,0.0000010656005,0.0000020476791,0.00021703448,0.0000012195318,0.0012717247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996614,0.000003406646,0.0000031493707,0.000013439923,0.000005130116,0.000008824193],"domain_scores_gemma":[0.99996865,0.0000028283343,0.000012501829,0.0000023671496,0.0000069716534,0.0000067368705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000047221583,0.00014565312,0.00007783562,0.0006573494,0.00029978662,0.00034193535,0.00012765129,0.00013498517,0.0024588036],"category_scores_gemma":[0.00012874242,0.000055542772,0.0000900364,0.0006951722,0.00026470912,0.000097644705,0.00040940996,0.00010000095,0.00024200082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012194649,0.000043376076,0.94556135,0.0000877964,0.000030754545,0.0027448363,0.0042432416,0.00081515574,0.010258167,0.00073808874,0.0005682998,0.034786977],"study_design_scores_gemma":[0.0000023088703,0.000019561214,0.99301225,0.000013344258,0.0000060705747,0.0005256275,0.0038833322,0.00014444576,0.00038675935,0.00006854289,0.0019356103,0.0000021285268],"about_ca_topic_score_codex":0.060330447,"about_ca_topic_score_gemma":0.14708133,"teacher_disagreement_score":0.060330447,"about_ca_system_score_codex":0.00046963926,"about_ca_system_score_gemma":0.00035104016,"threshold_uncertainty_score":0.11995858},"labels":[],"label_agreement":null},{"id":"W3042402379","doi":"10.5194/egusphere-egu2020-9531","title":"Ad-hoc estimation of landslide-generated impulse waves &amp;#8211; from the lab to the field","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shore; Landslide; Impulse (physics); Subaerial; Computer science; Marine engineering; Geology; Engineering; Geotechnical engineering; Seismology; Physics","score_opus":0.026289497991721825,"score_gpt":0.23759786082911466,"score_spread":0.21130836283739285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042402379","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.30357373,0.00027800427,0.6635205,0.00026113394,0.00026456662,0.0002634819,0.0020899514,0.009792071,0.019956583],"genre_scores_gemma":[0.7155448,0.00035519028,0.27138582,0.00014642508,0.000058618785,0.00037550653,0.0025236644,0.0003413448,0.009268672],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99970835,0.00004225875,0.000011000707,0.00008830314,0.00011475381,0.000035330402],"domain_scores_gemma":[0.99910825,0.00021466176,0.000063710024,0.0001772716,0.00035537072,0.000080627775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043090878,0.0005842458,0.0004703287,0.0009595946,0.00032315045,0.0007722397,0.0008170779,0.0006349867,0.0068353917],"category_scores_gemma":[0.001322986,0.00027853082,0.00021850815,0.0006788507,0.00033230952,0.00068672094,0.0006074688,0.00051705504,0.003764219],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006884164,0.0003825289,0.019229006,0.00044939687,0.000059579175,0.00036647377,0.000394762,0.033470403,0.3703298,0.0021644803,0.015893836,0.5565713],"study_design_scores_gemma":[0.00009877735,0.00090962905,0.035923988,0.00007212054,0.000096104755,0.00040919593,0.0006742869,0.6322897,0.30145246,0.003271665,0.024674179,0.00012790799],"about_ca_topic_score_codex":0.0016262368,"about_ca_topic_score_gemma":0.0028034,"teacher_disagreement_score":0.0068353917,"about_ca_system_score_codex":0.00034752054,"about_ca_system_score_gemma":0.0006301461,"threshold_uncertainty_score":0.022866666},"labels":[],"label_agreement":null},{"id":"W3042568462","doi":"10.1785/0220200086","title":"High-Resolution Imaging of Hydraulic-Fracturing-Induced Earthquake Clusters in the Dawson-Septimus Area, Northeast British Columbia, Canada","year":2020,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Lineation; Induced seismicity; Hydraulic fracturing; Fault (geology); Thrust fault; Azimuth; Structural basin; Tectonics; Geomorphology; Geometry; Geotechnical engineering","score_opus":0.045078639523124645,"score_gpt":0.24878310854672558,"score_spread":0.20370446902360095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042568462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.981962,0.00025685932,0.00075913314,0.00013441962,0.000011297714,0.00005442524,0.00969813,0.00014558171,0.0069781397],"genre_scores_gemma":[0.9889326,0.00023126636,0.002192412,0.000054320553,0.000006840665,0.000034031433,0.0048036203,0.000036470934,0.0037083463],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998381,0.0000044304516,0.000005015095,0.00003211518,0.000057907586,0.0000624214],"domain_scores_gemma":[0.99946684,0.000022563305,0.00003718187,0.000016805534,0.0003401156,0.000116526986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011881935,0.000344142,0.0002133165,0.0026136916,0.0012747743,0.00084127806,0.0005558356,0.0002722753,0.0021275573],"category_scores_gemma":[0.00041147353,0.00021313594,0.00012709465,0.0037947781,0.0003106354,0.00014951755,0.00048077613,0.00026112408,0.00043920422],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003073079,0.00014611003,0.84575564,0.00018069835,0.00011510624,0.0012070562,0.0024413595,0.0037787212,0.061959468,0.00032345272,0.01243923,0.07134587],"study_design_scores_gemma":[0.000009205356,0.000007707753,0.993628,0.000017679333,0.000012695726,0.000055085482,0.0009283729,0.0020639363,0.0008906457,0.000018130979,0.0023559206,0.000012569925],"about_ca_topic_score_codex":0.9683544,"about_ca_topic_score_gemma":0.99194616,"teacher_disagreement_score":0.031645596,"about_ca_system_score_codex":0.0045734798,"about_ca_system_score_gemma":0.00700294,"threshold_uncertainty_score":0.0636639},"labels":[],"label_agreement":null},{"id":"W3043150798","doi":"10.1080/21664250.2020.1780676","title":"Uncertainty of probabilistic tsunami hazard assessment of Zihuatanejo (Mexico) due to the representation of tsunami variability","year":2020,"lang":"en","type":"article","venue":"Coastal Engineering Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Weighting; Probabilistic logic; Seismology; Fault tree analysis; Seismic hazard; Monte Carlo method; Geology; Slip (aerodynamics); Hazard; Return period; Hazard analysis; Fault (geology); Moment magnitude scale; Statistics; Geography; Mathematics; Engineering; Reliability engineering","score_opus":0.01987263591542469,"score_gpt":0.24327982105399437,"score_spread":0.2234071851385697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043150798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9808915,0.00018654298,0.015594963,0.00019045254,0.000005833275,0.00002353194,0.00043646566,0.000039465715,0.002631181],"genre_scores_gemma":[0.99807644,0.00009733792,0.0014476777,0.000007220049,0.0000026594635,0.0000094055185,0.00017171392,0.0000026970529,0.0001848053],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998073,0.000061660336,0.000009297421,0.00004594209,0.00004752719,0.000028295197],"domain_scores_gemma":[0.99953616,0.00027181968,0.000099005454,0.00002243854,0.000057813566,0.000012816798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006063623,0.0003789248,0.00020732885,0.00087364233,0.0002699665,0.0009332236,0.000346385,0.00028160014,0.0006971798],"category_scores_gemma":[0.0019993712,0.00018480836,0.00028360498,0.0006223782,0.00025443474,0.0005702991,0.00053299894,0.00024102979,0.000034673743],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002529919,0.000043117387,0.16485928,0.000081895654,0.00018375876,0.000533958,0.00025659977,0.7885773,0.0028644498,0.009147647,0.00046139405,0.032737583],"study_design_scores_gemma":[0.000032908523,0.000066023655,0.10406092,0.000029634046,0.000095974116,0.00011297089,0.00039305765,0.8870758,0.0011563256,0.005504617,0.0014447729,0.000027004733],"about_ca_topic_score_codex":0.036830455,"about_ca_topic_score_gemma":0.031623606,"teacher_disagreement_score":0.036830455,"about_ca_system_score_codex":0.0013676637,"about_ca_system_score_gemma":0.0005498346,"threshold_uncertainty_score":0.073232174},"labels":[],"label_agreement":null},{"id":"W3043232900","doi":"10.1785/0120200048","title":"Nonlinear Multiple Earthquake Location and Velocity Estimation in the Canadian Rocky Mountain Trench","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Hypocenter; Seismology; Geology; Trench; Markov chain Monte Carlo; Nonlinear system; Probabilistic logic; Bayesian probability; Earthquake location; Geodesy; Statistics; Mathematics; Induced seismicity; Physics","score_opus":0.019540011363081575,"score_gpt":0.20974908733563538,"score_spread":0.19020907597255382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043232900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95064515,0.00027103885,0.043777257,0.00033720408,0.000012225063,0.00006524627,0.0013105763,0.00041980637,0.0031614169],"genre_scores_gemma":[0.9757639,0.000072712246,0.02210586,0.000022825263,0.000004653732,0.000010277768,0.00076593214,0.000025668689,0.0012282421],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9996766,0.000027294,0.000008912644,0.000098972545,0.00012149428,0.000066808505],"domain_scores_gemma":[0.99956244,0.00009557648,0.00006172724,0.000024510233,0.00021017254,0.000045593664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053919095,0.00066997844,0.00044558078,0.0012229343,0.0010144574,0.0009304765,0.0013991732,0.000576111,0.0014133736],"category_scores_gemma":[0.0021992268,0.00040274643,0.00032103475,0.0014703408,0.0004914334,0.0003493848,0.000671235,0.00045059598,0.00011976372],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013702209,0.00007089202,0.12282392,0.00012112575,0.00015950219,0.0003970331,0.00036123983,0.7793158,0.006107948,0.0025261343,0.0017021048,0.086277254],"study_design_scores_gemma":[0.000029044319,0.000012858444,0.066287674,0.000016060092,0.000018067889,0.00002623868,0.00014017877,0.9308705,0.0009864795,0.00068498036,0.00089062663,0.000037279457],"about_ca_topic_score_codex":0.9589839,"about_ca_topic_score_gemma":0.9751475,"teacher_disagreement_score":0.0410161,"about_ca_system_score_codex":0.0062891333,"about_ca_system_score_gemma":0.012316311,"threshold_uncertainty_score":0.08251524},"labels":[],"label_agreement":null},{"id":"W3043422075","doi":"","title":"Effects of lateral variations in lithospheric thickness and mantle viscosity on glacially induced surface motion and seismotectonics in Eastern Canada","year":2004,"lang":"en","type":"article","venue":"AGU Spring Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Mantle (geology); Seismotectonics; Geophysics; Seismology; Geodesy; Tectonics","score_opus":0.00870427481201524,"score_gpt":0.1934786346328779,"score_spread":0.18477435982086265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043422075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980526,0.00012258635,0.000028248283,0.00012853385,0.000003605213,0.000003259061,0.00054979225,0.000009633715,0.0011018903],"genre_scores_gemma":[0.9986355,0.00009762743,0.000044643333,0.000022684657,0.0000013995063,0.000002254986,0.00031573875,0.000008005131,0.0008721028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99964356,0.00003597347,0.000025029078,0.00006525219,0.00006412047,0.00016611231],"domain_scores_gemma":[0.99811244,0.0003881621,0.00014831236,0.00007185795,0.0007943879,0.00048500067],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005048975,0.00030259005,0.00043634415,0.0010050865,0.0027945973,0.0019048044,0.0009053503,0.00058487785,0.003379738],"category_scores_gemma":[0.002373996,0.00045836053,0.0006154437,0.0016623227,0.0012302229,0.00046104979,0.0010784037,0.00066599355,0.00027445203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00086718064,0.00007623995,0.9749288,0.000052843225,0.00026280055,0.00031367346,0.0021245047,0.006216489,0.005720776,0.00067218835,0.001141288,0.0076232357],"study_design_scores_gemma":[0.000011305547,0.000010538793,0.99675685,0.00000920271,0.000036873735,0.000020974847,0.0013266978,0.0011658529,0.00021583517,0.00003472577,0.00039536456,0.000015811038],"about_ca_topic_score_codex":0.993804,"about_ca_topic_score_gemma":0.99705565,"teacher_disagreement_score":0.026699305,"about_ca_system_score_codex":0.026699305,"about_ca_system_score_gemma":0.021015665,"threshold_uncertainty_score":0.1937179},"labels":[],"label_agreement":null},{"id":"W3043462226","doi":"10.1785/0120200107","title":"A Long-Lived Swarm of Hydraulic Fracturing-Induced Seismicity Provides Evidence for Aseismic Slip","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Geology; Hypocenter; Hydraulic fracturing; Aftershock; Seismology; Slip (aerodynamics); Pore water pressure; Fluid pressure; Overpressure; Fluid dynamics; Geotechnical engineering; Mechanics; Engineering","score_opus":0.07089034626347021,"score_gpt":0.26217329997622785,"score_spread":0.19128295371275764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043462226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903417,0.000035555127,0.00042612175,0.000005647425,0.0000012618967,0.0000026760763,0.00009860201,0.000012116605,0.00038381692],"genre_scores_gemma":[0.99964714,0.000013656668,0.00016833375,0.0000022838824,0.000002359032,0.0000013838451,0.00012121687,0.0000015903158,0.000041910695],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993193,0.00001015952,0.000008564235,0.00001801372,0.000013078927,0.00001820445],"domain_scores_gemma":[0.99953985,0.0000890646,0.00020725011,0.000037819827,0.000033569617,0.000092522736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014369411,0.00012980164,0.00018082815,0.00064209924,0.0001904896,0.00025594077,0.0001301313,0.00019122736,0.00090918806],"category_scores_gemma":[0.0004882889,0.00008615374,0.00014107882,0.00046840444,0.00026886913,0.00018881023,0.0003425533,0.00014231278,0.00012333834],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003460871,0.00013881142,0.77174634,0.000079109865,0.000104998115,0.0021148066,0.0005590687,0.0017225037,0.21246177,0.0003686422,0.00022573407,0.010132119],"study_design_scores_gemma":[0.000003917877,0.00013135491,0.99247277,0.0000040161226,0.000017113156,0.0007252001,0.00018578238,0.0026450292,0.0034247309,0.0000807917,0.00030416818,0.0000051882507],"about_ca_topic_score_codex":0.0008202192,"about_ca_topic_score_gemma":0.0013737692,"teacher_disagreement_score":0.00090918806,"about_ca_system_score_codex":0.00015285474,"about_ca_system_score_gemma":0.000082287545,"threshold_uncertainty_score":0.0030415058},"labels":[],"label_agreement":null},{"id":"W3043824897","doi":"10.1785/0120200105","title":"Factors Influencing the Probability of Hydraulic Fracturing-Induced Seismicity in Oklahoma","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Hydraulic fracturing; Geology; Seismology; Mining engineering; Geotechnical engineering","score_opus":0.04096788557743589,"score_gpt":0.2180063737960376,"score_spread":0.17703848821860171,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043824897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927215,0.00006871535,0.00014970943,0.00033410295,0.0000072098446,0.0000133513095,0.005392177,0.000016333113,0.0012967335],"genre_scores_gemma":[0.9964669,0.000061157254,0.00016610794,0.000068263595,0.0000062624667,0.000022630518,0.002724687,0.0000057156676,0.00047818813],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99957925,0.00005989458,0.000047234247,0.000091325885,0.000070851565,0.00015147585],"domain_scores_gemma":[0.997332,0.0006454823,0.00091364514,0.00017165918,0.0005241227,0.00041317582],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042005593,0.00020003883,0.00018093853,0.0011461732,0.0011312864,0.00085116527,0.0005725362,0.00034205156,0.0037855762],"category_scores_gemma":[0.0024157243,0.00016557967,0.0002478184,0.002198897,0.00036757378,0.00048415887,0.00093487126,0.00062125636,0.0003759805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024637344,0.000030980256,0.9957983,0.00001693127,0.00002678759,0.000058994017,0.00026346758,0.0002858913,0.00020215755,0.000049723923,0.00086264743,0.002379502],"study_design_scores_gemma":[0.0000023867033,0.000007768035,0.99641514,0.000024369438,0.000011053162,0.00001558841,0.0016404645,0.0006219447,0.000091268375,0.000028933682,0.0011335312,0.000007479015],"about_ca_topic_score_codex":0.52447677,"about_ca_topic_score_gemma":0.63706225,"teacher_disagreement_score":0.52447677,"about_ca_system_score_codex":0.0029281224,"about_ca_system_score_gemma":0.002702127,"threshold_uncertainty_score":0.9566474},"labels":[],"label_agreement":null},{"id":"W3043940899","doi":"10.1029/2020gl088947","title":"Coseismic Uplift of the 1999 <i>M</i><sub>w</sub>7.6 Chi‐Chi Earthquake and Implication to Topographic Change in Frontal Mountain Belts","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Future Earth","funders":"Ministry of Science and Technology, Taiwan","keywords":"Geology; Landslide; Seismology; Interferometric synthetic aperture radar; Slip (aerodynamics); Earthquake rupture; Geomorphology; Synthetic aperture radar; Remote sensing; Fault (geology)","score_opus":0.035003523956662036,"score_gpt":0.26815399482679003,"score_spread":0.233150470870128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043940899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993235,0.000025224355,0.000083239145,0.000023177585,0.0000018051298,0.0000015475711,0.000081753955,0.0000055750747,0.0004542764],"genre_scores_gemma":[0.99976295,0.000020143336,0.00004272816,0.0000045306583,0.0000034728787,8.9545955e-7,0.00010844531,9.966031e-7,0.000055913384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994993,0.0000069844996,0.0000043128607,0.00001257559,0.000008576134,0.000017687704],"domain_scores_gemma":[0.99972826,0.0000329011,0.00011880128,0.000016059768,0.000056670084,0.000047273104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013922724,0.0001354673,0.00013218282,0.0009102195,0.00017107592,0.00035048605,0.000121941,0.00018186061,0.0008575741],"category_scores_gemma":[0.00042290764,0.000082616905,0.00013053982,0.0006252216,0.00022191223,0.00021745545,0.00025650117,0.00012929935,0.00011813754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049621776,0.000018609393,0.98115563,0.000018576375,0.000033354034,0.0002776328,0.00015714567,0.0012603292,0.009615976,0.00010183544,0.0002141592,0.007097103],"study_design_scores_gemma":[0.0000010813504,0.000008851607,0.9986935,0.0000013307093,0.000006247937,0.000032470787,0.00007655605,0.00087425706,0.0001750416,0.000017382381,0.00011187256,0.0000013445181],"about_ca_topic_score_codex":0.016196337,"about_ca_topic_score_gemma":0.020466456,"teacher_disagreement_score":0.016196337,"about_ca_system_score_codex":0.0002637571,"about_ca_system_score_gemma":0.00016507316,"threshold_uncertainty_score":0.03220415},"labels":[],"label_agreement":null},{"id":"W3044548060","doi":"10.1785/0220200142","title":"Resolving Northern Alaska Earthquake Sequences Using the Transportable Array and Probabilistic Location Methods","year":2020,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Aftershock; Geology; Sequence (biology); Range (aeronautics); Tectonics; Probabilistic logic; Event (particle physics); Geodesy","score_opus":0.14758742600081967,"score_gpt":0.35068316391521087,"score_spread":0.2030957379143912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3044548060","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32182613,0.00068653264,0.67070764,0.00031556402,0.00013587016,0.000064604676,0.0010605463,0.0015611381,0.0036420487],"genre_scores_gemma":[0.7939519,0.00014014008,0.2029431,0.000049299088,0.00007480983,0.000046373378,0.0011965967,0.00006782537,0.0015299341],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9996561,0.00009990573,0.000026583852,0.00009937398,0.00009045274,0.000027645205],"domain_scores_gemma":[0.9992756,0.00024791484,0.0001543666,0.00008318469,0.00019782089,0.00004107872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00064530014,0.0005221442,0.00029033242,0.0011930969,0.00028808138,0.0007198591,0.00065766054,0.00044585782,0.0013577472],"category_scores_gemma":[0.0032824385,0.0003450051,0.00036902458,0.0008690821,0.00021795966,0.0007709313,0.0008820792,0.0004479589,0.0005410105],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038371567,0.00009796253,0.049925648,0.00012701993,0.00021275386,0.00037380154,0.00026853706,0.54115385,0.0103822425,0.004836272,0.002334792,0.38990337],"study_design_scores_gemma":[0.000022023112,0.000047012396,0.0068864217,0.000016705015,0.000024221124,0.00006924116,0.00009355195,0.98666126,0.0014569875,0.0032075588,0.0014861008,0.000028961702],"about_ca_topic_score_codex":0.011092719,"about_ca_topic_score_gemma":0.017799063,"teacher_disagreement_score":0.011092719,"about_ca_system_score_codex":0.00033103424,"about_ca_system_score_gemma":0.00069765566,"threshold_uncertainty_score":0.022056282},"labels":[],"label_agreement":null},{"id":"W3044947544","doi":"10.1130/ges02175.1","title":"Tectonic geomorphology and Plio-Quaternary structural evolution of the Tuzgölü fault zone, Turkey: Implications for deformation in the interior of the Central Anatolian Plateau","year":2020,"lang":"en","type":"article","venue":"Geosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Minnesota; National Science Foundation","keywords":"Geology; Fault (geology); Extensional fault; Plateau (mathematics); Basin and range topography; Sinuosity; Structural basin; Tectonics; Seismology; Geomorphology; Basin and Range Province; Shear zone; Extensional tectonics; Neotectonics; Fault scarp; Rift","score_opus":0.012480738395955291,"score_gpt":0.2141089495731199,"score_spread":0.20162821117716462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3044947544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99933916,0.00011901196,0.000046806057,0.000020349693,0.0000014295756,0.0000019225083,0.00008154205,0.0000056487347,0.00038422624],"genre_scores_gemma":[0.99974483,0.00004805426,0.00004005526,0.000003324153,0.0000014256974,0.0000017007152,0.000094065035,0.0000018827571,0.00006465908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999207,0.000011771862,0.000007570269,0.00002497859,0.000012423644,0.000022543862],"domain_scores_gemma":[0.99987674,0.000014222017,0.000049800794,0.000009784722,0.000033061126,0.00001639605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022778471,0.0002517166,0.00019897205,0.0015881291,0.00035268647,0.00076199323,0.00026636713,0.00035474278,0.00080276025],"category_scores_gemma":[0.00027554302,0.00013689777,0.00019212652,0.0014614821,0.00064235204,0.0004042656,0.0003696696,0.00014651466,0.0001334209],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012750161,0.00004143787,0.96893847,0.000046844514,0.00007140668,0.00063593785,0.0009944886,0.0034904124,0.0073347385,0.00035509226,0.00018977514,0.017773813],"study_design_scores_gemma":[0.0000023475986,0.000011827394,0.9984112,0.0000067012593,0.0000061928954,0.000075923956,0.000394911,0.0007696798,0.000090743335,0.000028983073,0.00019908561,0.0000023482503],"about_ca_topic_score_codex":0.02420158,"about_ca_topic_score_gemma":0.028962864,"teacher_disagreement_score":0.02420158,"about_ca_system_score_codex":0.0011855835,"about_ca_system_score_gemma":0.0005170287,"threshold_uncertainty_score":0.048121393},"labels":[],"label_agreement":null},{"id":"W3045188720","doi":"10.1007/1345_2020_115","title":"Progress in GTEWS Ground Displacement Measurements and Tsunami Warning","year":2020,"lang":"en","type":"book-chapter","venue":"International Association of Geodesy symposia","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"GNSS applications; Warning system; Geodetic datum; Global Positioning System; Early warning system; Satellite system; Computer science; Telecommunications; Remote sensing; Systems engineering; Real-time computing; Geography; Geodesy; Engineering","score_opus":0.02209025351899047,"score_gpt":0.2327423975225855,"score_spread":0.21065214400359503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3045188720","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.027897399,0.34675503,0.08694998,0.018378487,0.011330064,0.00011645228,0.0023370758,0.002699873,0.5035357],"genre_scores_gemma":[0.18931822,0.24917924,0.0773877,0.0034519865,0.006641747,0.00009198535,0.0063889567,0.0006713302,0.4668688],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9994357,0.00010088075,0.00002947504,0.00008619576,0.0003239292,0.000023806371],"domain_scores_gemma":[0.9992617,0.00033563172,0.00004216284,0.000048281232,0.00028215116,0.000030031324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013658096,0.0004949126,0.00026005946,0.0016348532,0.0001210494,0.0018342835,0.00089166395,0.0006298003,0.009259033],"category_scores_gemma":[0.0015747487,0.00020822111,0.00020880703,0.0025210045,0.00061827013,0.002302844,0.0010610971,0.0009623473,0.004259145],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029322775,0.000015954332,0.0009869128,0.0005993498,0.000009947652,0.00004185674,0.00014608909,0.0021278786,0.0023801425,0.026313486,0.049225505,0.9181236],"study_design_scores_gemma":[0.0000072991525,0.00006424807,0.0048003034,0.00043488637,0.000009177445,0.00017503671,0.00012936242,0.004508126,0.00297441,0.010519992,0.9763534,0.000023842924],"about_ca_topic_score_codex":0.0041420404,"about_ca_topic_score_gemma":0.0037771137,"teacher_disagreement_score":0.009259033,"about_ca_system_score_codex":0.0006274493,"about_ca_system_score_gemma":0.00066613767,"threshold_uncertainty_score":0.030974567},"labels":[],"label_agreement":null},{"id":"W3045973064","doi":"10.4236/eng.2020.127036","title":"Maximum Magnitude of Seismicity Induced by a Hydraulic Fracturing Stage in a Shale Reservoir: Insights from Numerical Simulations","year":2020,"lang":"en","type":"article","venue":"Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Magnitude (astronomy); Hydraulic fracturing; Induced seismicity; Maximum magnitude; Geology; Oil shale; Fault (geology); Modulus; Geotechnical engineering; Seismology; Geometry; Mathematics","score_opus":0.020156375341196145,"score_gpt":0.2087217458927745,"score_spread":0.18856537055157835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3045973064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946883,0.000044829743,0.0021893063,0.00017251451,0.0000074781105,0.000014634017,0.0002758281,0.00004717539,0.0025601077],"genre_scores_gemma":[0.9991097,0.000024406436,0.0005920242,0.00001400229,0.0000028265085,0.000011429143,0.0000777588,0.0000078267485,0.00015998127],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998267,0.00006070266,0.000016289032,0.000027180033,0.00002888428,0.000040283612],"domain_scores_gemma":[0.99814236,0.0013221679,0.00022000518,0.00009343685,0.00010074473,0.00012120212],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007290332,0.0003979275,0.00054436864,0.0007741016,0.00044236876,0.0007891039,0.0005947361,0.0015627369,0.0014167764],"category_scores_gemma":[0.0039682253,0.00038781852,0.00062937697,0.0005122005,0.0010182584,0.0006210122,0.00061972823,0.00064476934,0.00007649997],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003921418,0.000029495252,0.004466398,0.00001553265,0.000013138337,0.00006917659,0.000022771304,0.99384767,0.0005825891,0.00046284098,0.00006643916,0.0003848284],"study_design_scores_gemma":[0.000012550636,0.000032271964,0.001570117,0.000005911575,0.0000067224414,0.000011700912,0.000030647985,0.9977584,0.00021303317,0.0003017417,0.00005042129,0.0000064230394],"about_ca_topic_score_codex":0.013766499,"about_ca_topic_score_gemma":0.0094601605,"teacher_disagreement_score":0.013766499,"about_ca_system_score_codex":0.0009771163,"about_ca_system_score_gemma":0.00059558725,"threshold_uncertainty_score":0.027372718},"labels":[],"label_agreement":null},{"id":"W3046223610","doi":"10.1029/2020jb020103","title":"Well Proximity Governing Stress Drop Variation and Seismic Attenuation Associated With Hydraulic Fracturing Induced Earthquakes","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Hydraulic fracturing; Geology; Attenuation; Drop (telecommunication); Seismology; Geotechnical engineering; Optics","score_opus":0.04560944561614095,"score_gpt":0.28211793520634837,"score_spread":0.23650848959020743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046223610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991304,0.0000133846825,0.00044086616,0.0000051912975,3.390191e-7,0.0000025578754,0.00012682416,0.000013369756,0.0002669813],"genre_scores_gemma":[0.99978226,0.000006135544,0.00008553913,0.0000010422284,2.3197758e-7,8.064439e-7,0.000078401004,0.0000015289451,0.000043962078],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983466,0.000017062106,0.000009210744,0.000042107025,0.00004948086,0.00004746191],"domain_scores_gemma":[0.9991093,0.00021212368,0.00023577649,0.000054214834,0.0002953909,0.000093088136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020475274,0.00014562896,0.00022530806,0.0011983801,0.00026974417,0.0005211415,0.00020594102,0.00020075306,0.00091393985],"category_scores_gemma":[0.0016660667,0.00018489947,0.000096035175,0.0012842922,0.0003593531,0.000288277,0.00025603597,0.00015862487,0.00013582339],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007807187,0.000037212685,0.96803546,0.000014420292,0.0000483261,0.00014694958,0.0003025888,0.004689435,0.01951596,0.00008703129,0.00010686905,0.006937651],"study_design_scores_gemma":[8.0561364e-7,0.0000056495355,0.9970932,0.0000010691973,0.0000033598078,0.000013913472,0.000110338144,0.0022753295,0.0004330611,0.000018745992,0.000041543026,0.0000030149367],"about_ca_topic_score_codex":0.17637199,"about_ca_topic_score_gemma":0.2620232,"teacher_disagreement_score":0.17637199,"about_ca_system_score_codex":0.00086933933,"about_ca_system_score_gemma":0.0004551245,"threshold_uncertainty_score":0.35069078},"labels":[],"label_agreement":null},{"id":"W3046370269","doi":"10.5539/esr.v9n2p85","title":"Correlating DYFI Data With Seismic Microzonation in the Region of Montreal","year":2020,"lang":"en","type":"article","venue":"Earth Science Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismic microzonation; Seismology; Mercalli intensity scale; Geology; Earthquake scenario; Urban seismic risk; Metropolitan area; Population; Seismic hazard; Geography; Peak ground acceleration; Ground motion","score_opus":0.15195165113120826,"score_gpt":0.3322849541460774,"score_spread":0.18033330301486913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046370269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97477686,0.0003489245,0.0006790662,0.00021947875,0.000017198645,0.00006295852,0.013784501,0.00010600371,0.010004925],"genre_scores_gemma":[0.9918,0.00019658022,0.0006316351,0.000016566673,0.0000063690773,0.000023566028,0.0047211912,0.00001092566,0.0025930845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997471,0.000025579086,0.000011486934,0.00005290686,0.000080726815,0.0000822596],"domain_scores_gemma":[0.9987998,0.00012531996,0.0002476158,0.00004818079,0.0006180751,0.00016100473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034567757,0.00027426242,0.00013757957,0.0023355093,0.000504509,0.0008675696,0.00039201765,0.00016763229,0.0029353942],"category_scores_gemma":[0.0020483737,0.0001016532,0.00012335493,0.0032584346,0.00028208786,0.00022987551,0.00037966965,0.00023249921,0.00028802315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010460224,0.000029015982,0.9625647,0.00005491734,0.00007608821,0.00014975636,0.0010651546,0.0020707995,0.0026160602,0.00049234275,0.005343064,0.025433503],"study_design_scores_gemma":[0.000001811031,0.0000063566226,0.9961248,0.000007870272,0.0000059556214,0.000010912835,0.00059016095,0.000960124,0.00018687492,0.000011901608,0.002086825,0.0000063862076],"about_ca_topic_score_codex":0.9811613,"about_ca_topic_score_gemma":0.9910534,"teacher_disagreement_score":0.018838704,"about_ca_system_score_codex":0.007620838,"about_ca_system_score_gemma":0.003514463,"threshold_uncertainty_score":0.05529332},"labels":[],"label_agreement":null},{"id":"W3047238778","doi":"10.1038/s41467-020-17609-3","title":"Cascadia low frequency earthquakes at the base of an overpressured subduction shear zone","year":2020,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Alberta; University of Calgary; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Washington State University","keywords":"Geology; Subduction; Seismology; Crust; Shear (geology); Slab; Plate tectonics; Slip (aerodynamics); Shear zone; Oceanic crust; Episodic tremor and slip; Petrology; Geophysics; Tectonics","score_opus":0.023494705877545746,"score_gpt":0.24889924827317078,"score_spread":0.22540454239562505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047238778","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983273,0.000026402126,0.00008602769,0.000020822456,0.0000017889896,0.0000021204598,0.00008134739,0.000018810588,0.0014353916],"genre_scores_gemma":[0.9995024,0.000016707498,0.000047027235,0.0000043050554,8.1821406e-7,0.0000012688456,0.000088636916,0.0000013217142,0.00033747437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999373,0.0000038661183,0.0000032300134,0.000017870494,0.000019811703,0.000017952281],"domain_scores_gemma":[0.9997943,0.000013990161,0.00007314434,0.000014945976,0.00004223821,0.000061427694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000059665956,0.0001846007,0.00014072921,0.0004711272,0.0005720085,0.00033039862,0.00015184078,0.00017422841,0.0014401431],"category_scores_gemma":[0.00038220518,0.00012010337,0.00007906495,0.0003217821,0.0004154631,0.00008802691,0.0004339032,0.00019737745,0.00024679457],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028940634,0.00002751819,0.83109725,0.00007965402,0.00003540864,0.0017459895,0.0023331991,0.00061924965,0.15508556,0.00033972735,0.00049003056,0.007856971],"study_design_scores_gemma":[0.0000018720277,0.000016971697,0.9982522,0.0000029142677,0.000003865235,0.00015342022,0.00032490614,0.00011750298,0.0007804741,0.000042054577,0.00030126408,0.0000024654792],"about_ca_topic_score_codex":0.034049302,"about_ca_topic_score_gemma":0.07187914,"teacher_disagreement_score":0.034049302,"about_ca_system_score_codex":0.0005945788,"about_ca_system_score_gemma":0.00034153313,"threshold_uncertainty_score":0.067702234},"labels":[],"label_agreement":null},{"id":"W3047239985","doi":"","title":"Static stress drop of the largest recorded M 4.6 hydraulic fracturing induced earthquake and its aftershock pattern in the northern Montney Play, British Columbia, Canada","year":2016,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Hydraulic fracturing; Geology; Seismology; Foreshock; Drop (telecommunication); Geotechnical engineering; Engineering; Telecommunications","score_opus":0.012023380907186567,"score_gpt":0.1870938501439383,"score_spread":0.17507046923675174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047239985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937304,0.00007517705,0.000036902526,0.000058382124,0.000004274891,0.000009842537,0.0026779757,0.000008538606,0.0033984552],"genre_scores_gemma":[0.9961791,0.000069761576,0.000035364574,0.00001891664,0.0000022704614,0.000005847424,0.0013578229,0.0000035008925,0.0023274391],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998473,0.000007102155,0.000009607878,0.000024566556,0.000041934996,0.00006942416],"domain_scores_gemma":[0.99905616,0.00004534548,0.00010240791,0.000018492243,0.00055264187,0.00022497075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011921055,0.00022003223,0.0002453269,0.0015362252,0.0016329117,0.0007760922,0.0007747927,0.00037311172,0.0029664948],"category_scores_gemma":[0.00073425303,0.00019657848,0.00016551258,0.0026658322,0.00052365713,0.0002027993,0.00050934945,0.00043606223,0.0004443092],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018973573,0.000055258603,0.9848621,0.000030914132,0.00004219642,0.00032834054,0.0017121338,0.00030456792,0.0021152315,0.00010959155,0.0022152683,0.008034649],"study_design_scores_gemma":[0.0000013877387,0.0000056498397,0.9987772,0.0000038832072,0.0000037242548,0.000019707977,0.00082129467,0.000061109466,0.000042918866,0.000003764678,0.0002568321,0.0000025746922],"about_ca_topic_score_codex":0.9850942,"about_ca_topic_score_gemma":0.99566275,"teacher_disagreement_score":0.01490581,"about_ca_system_score_codex":0.0072209197,"about_ca_system_score_gemma":0.007066405,"threshold_uncertainty_score":0.052391708},"labels":[],"label_agreement":null},{"id":"W3048488478","doi":"","title":"Seafloor P- to T-wave Conversion at the Scotia Volcanic-Arc, South Atlantic Ocean","year":2009,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seafloor spreading; Volcano; Nova scotia; Oceanography; Arc (geometry); Seismology; Engineering","score_opus":0.019035849759525585,"score_gpt":0.209867491639983,"score_spread":0.19083164188045743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048488478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974847,0.000041436375,0.00002634306,0.000034270644,0.0000050782346,0.000005658852,0.0005731877,0.0000053769595,0.0018239972],"genre_scores_gemma":[0.9990275,0.000026531257,0.000036391666,0.00000866057,0.0000014759019,0.0000020721852,0.00024285521,0.0000023242148,0.0006523096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.000009456984,0.000006140797,0.000019760224,0.000015493155,0.00002625833],"domain_scores_gemma":[0.99955505,0.000044858818,0.00006610385,0.000017701437,0.00022840468,0.000087850916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011202582,0.00011890357,0.00011391374,0.00068571937,0.0006005553,0.00063659425,0.00022901727,0.00023164334,0.0020803737],"category_scores_gemma":[0.00067759445,0.00012274865,0.00020299024,0.00095869903,0.00030042697,0.00019529836,0.00052267173,0.00019613364,0.00030525404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039379913,0.000027443397,0.9755435,0.00004094283,0.000053247466,0.00059392524,0.0010239438,0.0013376975,0.011616683,0.00019191578,0.0009230135,0.00825383],"study_design_scores_gemma":[0.0000036034676,0.000005142238,0.9993463,0.0000032106564,0.0000028334184,0.000019028086,0.00017189617,0.000244776,0.00006446212,0.000005022687,0.00013240283,0.0000013824185],"about_ca_topic_score_codex":0.78037775,"about_ca_topic_score_gemma":0.88097084,"teacher_disagreement_score":0.78037775,"about_ca_system_score_codex":0.001365794,"about_ca_system_score_gemma":0.0015173561,"threshold_uncertainty_score":0.4418313},"labels":[],"label_agreement":null},{"id":"W3048496510","doi":"10.1029/2020gl089627","title":"Isostatic Control of Axial Rivers and Large Drainage Basins on Passive Margins","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Passive margin; Geology; Lithosphere; Margin (machine learning); Drainage system (geomorphology); Continental margin; Drainage basin; Flow (mathematics); Routing (electronic design automation); Geomorphology; Drainage; Structural basin; Paleontology; Tectonics; Geometry; Rift","score_opus":0.028325968176656446,"score_gpt":0.26591428491520985,"score_spread":0.2375883167385534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048496510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99684286,0.000021741867,0.0020853044,0.000013751475,0.0000010167847,8.56435e-7,0.000022801041,0.00001453956,0.0009970808],"genre_scores_gemma":[0.99981517,0.0000058263067,0.00010051602,0.0000010318977,5.7295136e-7,4.811459e-7,0.00000620896,0.0000013183719,0.00006892295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999621,0.000009219907,0.0000028666318,0.000015164714,0.000005126403,0.0000054799475],"domain_scores_gemma":[0.9998541,0.00003327652,0.000059773847,0.000020282214,0.000016015414,0.000016595115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000629525,0.00007846437,0.00011345833,0.00025035307,0.00013321242,0.00037226576,0.00016362002,0.00007895653,0.0011129482],"category_scores_gemma":[0.0004299837,0.00009014499,0.00009245842,0.00015949422,0.00046076003,0.00027298543,0.000338182,0.00007358004,0.00004893593],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003442534,0.00010573181,0.52363765,0.00010040144,0.000088715824,0.00089523656,0.00088100974,0.15304495,0.23341697,0.046185642,0.0005510548,0.0407483],"study_design_scores_gemma":[0.000037675334,0.00011675644,0.7180717,0.000013919575,0.000053744057,0.00041782073,0.00053580425,0.24584861,0.0135509195,0.01889957,0.0024184457,0.00003495345],"about_ca_topic_score_codex":0.0016247071,"about_ca_topic_score_gemma":0.001834521,"teacher_disagreement_score":0.0016247071,"about_ca_system_score_codex":0.00020203639,"about_ca_system_score_gemma":0.00013783116,"threshold_uncertainty_score":0.0037231445},"labels":[],"label_agreement":null},{"id":"W3048542470","doi":"","title":"Lithospheric Inventory: An Exploration of Quebec, Canada with P-to-S Receiver Functions.","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Lithosphere; Receiver function; Remote sensing; Seismology; Tectonics","score_opus":0.023541101118870023,"score_gpt":0.20612664992671811,"score_spread":0.18258554880784808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048542470","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6918614,0.0057792203,0.010706656,0.002272097,0.00011970056,0.0002894847,0.21471228,0.0011725562,0.073086604],"genre_scores_gemma":[0.91954327,0.0016913221,0.010069272,0.00040107494,0.000020400475,0.00007102805,0.032628845,0.00015061985,0.035424173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998248,0.000010380634,0.0000051001193,0.000024172785,0.00008610548,0.00004944806],"domain_scores_gemma":[0.9991867,0.000026388689,0.000041832624,0.000020145302,0.0006481626,0.000076757424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022781664,0.0005134402,0.00024147535,0.0017105369,0.0017027882,0.001015702,0.0007594592,0.00032137218,0.0073262975],"category_scores_gemma":[0.00065756374,0.00018043116,0.00020710577,0.0045143655,0.00026332567,0.00040106635,0.0004179416,0.0003579872,0.0009602664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00084244274,0.0001963716,0.42940888,0.0005564873,0.0004580094,0.0008034108,0.0020245397,0.021992614,0.024306,0.006354178,0.137998,0.37505913],"study_design_scores_gemma":[0.00008866156,0.000058788166,0.8409349,0.00021021593,0.000143338,0.00021893713,0.0021836152,0.022337075,0.0030436777,0.00038194313,0.13031195,0.00008686116],"about_ca_topic_score_codex":0.99792564,"about_ca_topic_score_gemma":0.9988219,"teacher_disagreement_score":0.014769593,"about_ca_system_score_codex":0.014769593,"about_ca_system_score_gemma":0.031610057,"threshold_uncertainty_score":0.1071614},"labels":[],"label_agreement":null},{"id":"W3048700988","doi":"","title":"Tsunami Research and Monitoring Enabled through Ocean Network Canada's NEPTUNE Cabled Observatory","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Observatory; Neptune; Meteorology; Oceanography; Remote sensing; Astrobiology; Environmental science; Geology; Geography; Astronomy; Planet; Physics","score_opus":0.04905566160142971,"score_gpt":0.25712330112012083,"score_spread":0.20806763951869112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048700988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.41427505,0.0010316905,0.010136203,0.0064889714,0.0005914339,0.00085159653,0.35879862,0.0042713336,0.2035552],"genre_scores_gemma":[0.6703138,0.0016867303,0.039831143,0.0009502401,0.00022753602,0.00033776357,0.16537797,0.0007132631,0.1205617],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9991773,0.000046544104,0.000018316534,0.000092357586,0.00050730305,0.00015821667],"domain_scores_gemma":[0.9959103,0.00015555309,0.00015092532,0.00027025572,0.002862103,0.00065084285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010027465,0.00046933585,0.0002981136,0.0018412005,0.0015184792,0.0012899075,0.00062700966,0.00032012304,0.008977157],"category_scores_gemma":[0.0019522002,0.00030959703,0.00020620963,0.00266458,0.0003598764,0.0008982667,0.0014404168,0.0006860076,0.002132633],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008298424,0.00032261,0.34774554,0.00029120795,0.00011783488,0.0003491677,0.0017110956,0.004858632,0.024261389,0.004865079,0.3913325,0.22331512],"study_design_scores_gemma":[0.0001859358,0.00010269367,0.62594146,0.00012553456,0.00005581027,0.000088660476,0.0013275312,0.011498419,0.0069656842,0.0008035449,0.35283408,0.0000706747],"about_ca_topic_score_codex":0.94585294,"about_ca_topic_score_gemma":0.97832173,"teacher_disagreement_score":0.054147065,"about_ca_system_score_codex":0.005094866,"about_ca_system_score_gemma":0.027912825,"threshold_uncertainty_score":0.10893184},"labels":[],"label_agreement":null},{"id":"W3049517812","doi":"10.1007/s00126-020-01011-6","title":"Interplay between thermal convection and compressional fault reactivation in the formation of unconformity-related uranium deposits","year":2020,"lang":"en","type":"article","venue":"Mineralium Deposita","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"iNano Medical (Canada); University of Regina","funders":"Cameco","keywords":"Geology; Unconformity; Archean; Geothermal gradient; Tectonics; Sedimentary basin; Petrology; Basement; Overpressure; Proterozoic; Structural basin; Sedimentary rock; Geochemistry; Magmatism; Convection; Geomorphology; Geophysics; Seismology; Mechanics","score_opus":0.02002768883092726,"score_gpt":0.2337319204041286,"score_spread":0.21370423157320134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3049517812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99940753,0.000059826518,0.000036593545,0.00001455438,6.9403086e-7,0.0000012152993,0.0000060288703,0.0000022504107,0.00047129107],"genre_scores_gemma":[0.9998987,0.000019027333,0.000018405924,0.0000024363046,6.804495e-7,4.8715594e-7,0.0000045168194,6.9324375e-7,0.000055105793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998423,0.000037069276,0.000015649457,0.00003118279,0.000016321179,0.00005754053],"domain_scores_gemma":[0.99974996,0.000078917794,0.00007123961,0.00002037867,0.000030622625,0.00004889656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039002378,0.00018399359,0.00025837173,0.0007651297,0.0006150702,0.0011469049,0.00035853675,0.0004209655,0.0015299902],"category_scores_gemma":[0.0009798608,0.00024579727,0.00012510849,0.00037477078,0.0012179526,0.0005146195,0.0008326137,0.00019884783,0.00014655197],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010390045,0.00015008918,0.77427626,0.0001531338,0.00013765997,0.0015338499,0.0024935193,0.0062811095,0.19198027,0.0062559834,0.00011547202,0.015583701],"study_design_scores_gemma":[0.00002937602,0.000110442255,0.98549926,0.000015253426,0.000039409042,0.0002543373,0.0014944113,0.0045450055,0.0067011085,0.000771915,0.00052151346,0.000018045836],"about_ca_topic_score_codex":0.007336979,"about_ca_topic_score_gemma":0.012526852,"teacher_disagreement_score":0.007336979,"about_ca_system_score_codex":0.0010044355,"about_ca_system_score_gemma":0.0007049375,"threshold_uncertainty_score":0.014588535},"labels":[],"label_agreement":null},{"id":"W3056175676","doi":"10.1029/2020tc006128","title":"Lateral Termination of a Cycladic‐Style Detachment System (Hymittos, Greece)","year":2020,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Greenschist; Blueschist; Detachment fault; Metamorphic core complex; Schist; CYCLADES; Massif; Metamorphic rock; Shear zone; Geochemistry; Metamorphic facies; Mylonite; Petrology; Seismology; Facies; Paleontology; Tectonics; Subduction; Eclogite","score_opus":0.01693114178993932,"score_gpt":0.2075857241175012,"score_spread":0.19065458232756188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3056175676","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9859977,0.00011768039,0.0002071332,0.00003091196,0.0000045888505,0.000025613112,0.0003660868,0.000053676147,0.01319661],"genre_scores_gemma":[0.9955474,0.000050254894,0.00017686399,0.000010062861,0.0000017177038,0.000008595426,0.00031563983,0.000005244302,0.0038842086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991524,0.0000075080497,0.0000052176442,0.00003777422,0.000014237669,0.000020024445],"domain_scores_gemma":[0.9999504,0.000004064447,0.000016337428,0.000009284679,0.000008103973,0.000011804466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006447872,0.00025350903,0.00012771715,0.000597437,0.00035252178,0.00042048222,0.00025444443,0.00028818438,0.006580277],"category_scores_gemma":[0.00012310792,0.00012625974,0.00012633078,0.00067821436,0.0004887219,0.00016299543,0.00062634755,0.00010510855,0.00079899526],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050702685,0.00012323479,0.7387241,0.00047290215,0.00021774431,0.008695406,0.004787655,0.0048924657,0.08223613,0.0075249486,0.0034280217,0.14839047],"study_design_scores_gemma":[0.00004047785,0.000176555,0.9747692,0.00004485466,0.00002057646,0.0027798896,0.0018028044,0.0006461446,0.0017013272,0.00038140934,0.01762552,0.000011264696],"about_ca_topic_score_codex":0.014832547,"about_ca_topic_score_gemma":0.01975984,"teacher_disagreement_score":0.014832547,"about_ca_system_score_codex":0.0006093845,"about_ca_system_score_gemma":0.0006481904,"threshold_uncertainty_score":0.029492438},"labels":[],"label_agreement":null},{"id":"W3077652626","doi":"","title":"Analysis of GPS Measurements in Eastern Canada Using Principal Component Analysis","year":2009,"lang":"en","type":"article","venue":"AGU Spring Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Western University","funders":"","keywords":"Geodesy; Geology; Global Positioning System; Post-glacial rebound; Principal component analysis; Time series; Mathematics; Statistics; Geomorphology; Glacial period","score_opus":0.04763466561820456,"score_gpt":0.24624245687992516,"score_spread":0.1986077912617206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3077652626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9770041,0.00041914993,0.0025628966,0.00013847106,0.000024775145,0.00005701825,0.014261314,0.00018276175,0.00534935],"genre_scores_gemma":[0.9855921,0.00032601005,0.0034915188,0.000026788828,0.000007628753,0.00002094935,0.00828934,0.00001749269,0.002228068],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997352,0.000014413017,0.000011392222,0.00004836132,0.00013190438,0.0000587157],"domain_scores_gemma":[0.99917275,0.00006391009,0.000047855174,0.000026362864,0.0006287832,0.000060302507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015238397,0.00033864254,0.00019742826,0.0020548403,0.00080623035,0.00071216805,0.00042091854,0.00017876783,0.0010637561],"category_scores_gemma":[0.0009207719,0.00014966834,0.0002220102,0.0053051775,0.00028435877,0.000118124255,0.00027643028,0.00022461887,0.00023139635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001803234,0.0000528954,0.8373121,0.00013130235,0.00015113298,0.00033743895,0.0009821547,0.0118464595,0.005513417,0.0008588068,0.006961791,0.13567214],"study_design_scores_gemma":[0.000008524117,0.000011191893,0.98148835,0.000020125475,0.000021774238,0.00004048527,0.0005908708,0.013393333,0.00056785624,0.0000663346,0.0037739011,0.000017356624],"about_ca_topic_score_codex":0.9882592,"about_ca_topic_score_gemma":0.992434,"teacher_disagreement_score":0.011740804,"about_ca_system_score_codex":0.006677092,"about_ca_system_score_gemma":0.010986616,"threshold_uncertainty_score":0.04844594},"labels":[],"label_agreement":null},{"id":"W3080411573","doi":"","title":"Seismic Attenuation Characteristics in the Canadian Cordillera","year":2002,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Attenuation; Geodesy","score_opus":0.029259901260601455,"score_gpt":0.21199460687507524,"score_spread":0.18273470561447377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080411573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927384,0.00035060017,0.00006975294,0.0001295128,0.000004111447,0.000010313205,0.0013282463,0.00002243322,0.0053464957],"genre_scores_gemma":[0.9963415,0.00015529696,0.00012332624,0.000024904708,0.000002976969,0.0000061055716,0.00087200466,0.000010671525,0.0024632926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997111,0.000014044712,0.000012558313,0.00006300091,0.000094767056,0.00010461584],"domain_scores_gemma":[0.9991279,0.000044713852,0.000091701375,0.000020379239,0.00060442905,0.00011080112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002749866,0.00044696787,0.0003459057,0.002020942,0.0019567125,0.0011340961,0.00075658894,0.00042209285,0.003478307],"category_scores_gemma":[0.0012979519,0.00020551773,0.00018753385,0.003897465,0.00042360625,0.00025556868,0.00066811533,0.00023920469,0.0005020282],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046529408,0.000052951505,0.94197905,0.000054085864,0.000069877125,0.00040487145,0.002501747,0.00183792,0.004454221,0.00051241444,0.002530092,0.04513747],"study_design_scores_gemma":[0.000005497413,0.0000066808734,0.9972657,0.000007822242,0.000010934883,0.00003487881,0.000497271,0.0005432061,0.00011945862,0.00001694109,0.0014858263,0.0000058452724],"about_ca_topic_score_codex":0.9926207,"about_ca_topic_score_gemma":0.9965463,"teacher_disagreement_score":0.01485909,"about_ca_system_score_codex":0.01485909,"about_ca_system_score_gemma":0.0070856013,"threshold_uncertainty_score":0.107810736},"labels":[],"label_agreement":null},{"id":"W3080874335","doi":"","title":"Possible Biases in Characteristic Earthquake and Seismic Hazard Studies: Illustrations for the Wasatch, New Madrid, North Africa, and Eastern Canadian Seismic Zones","year":2005,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Seismic hazard; Geology; Earthquake scenario; Urban seismic risk; Seismic risk; Hazard; Geography","score_opus":0.05499625601672793,"score_gpt":0.246554510578494,"score_spread":0.19155825456176606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080874335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93856937,0.004912288,0.0102227405,0.008593842,0.0001518182,0.00019723384,0.0016887472,0.00005935977,0.0356047],"genre_scores_gemma":[0.99155515,0.001004082,0.004444691,0.00029305348,0.00003022189,0.000037350386,0.00019097562,0.000027568225,0.0024169032],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99591714,0.0023369594,0.00024738433,0.0002908674,0.00078144815,0.00042620723],"domain_scores_gemma":[0.957723,0.025621677,0.0046397815,0.002615658,0.008699922,0.00069998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0135784075,0.000336348,0.0003379448,0.004510512,0.002484612,0.0022173242,0.0024651357,0.00085207535,0.001969192],"category_scores_gemma":[0.06451406,0.0002439647,0.00047569696,0.0081491005,0.004906055,0.0012471289,0.0013713104,0.00062488345,0.00012215455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062926376,0.00007926899,0.7849597,0.0004955224,0.0002370994,0.0014268984,0.04064288,0.004459689,0.002255473,0.08420965,0.0064883633,0.0741163],"study_design_scores_gemma":[0.00011108163,0.00006949401,0.8659847,0.0005636125,0.00033752248,0.0008561066,0.06400059,0.0069418303,0.0029382533,0.033421673,0.024682965,0.00009216361],"about_ca_topic_score_codex":0.71549183,"about_ca_topic_score_gemma":0.868494,"teacher_disagreement_score":0.28450817,"about_ca_system_score_codex":0.005648453,"about_ca_system_score_gemma":0.0067507587,"threshold_uncertainty_score":0.57236737},"labels":[],"label_agreement":null},{"id":"W3080924699","doi":"10.1029/2020jb019383","title":"Diffuse Deformation in the SE Tibetan Plateau: New Insights From Geodetic Observations","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Key Research and Development Program of China Stem Cell and Translational Research; National Natural Science Foundation of China","keywords":"Sinistral and dextral; Geology; Seismology; Geodetic datum; Slip (aerodynamics); Crust; Plateau (mathematics); Strike-slip tectonics; Fault (geology); Induced seismicity; Kinematics; Geodesy; Geophysics","score_opus":0.1264117783498151,"score_gpt":0.3189259727181349,"score_spread":0.1925141943683198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080924699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979832,0.00017066387,0.00032825212,0.000028059321,0.0000026649172,0.000004670652,0.00048621275,0.000017742095,0.0009784633],"genre_scores_gemma":[0.9990926,0.000078311445,0.000185833,0.0000073904566,0.000009257324,0.0000028897484,0.0005348256,0.0000030076553,0.00008588142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992216,0.000009785857,0.000006902159,0.000024052428,0.000022710115,0.00001435524],"domain_scores_gemma":[0.99979585,0.000025406063,0.000058733935,0.000025006288,0.000056946596,0.00003802716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024955708,0.00027310438,0.00021286582,0.0014822291,0.00025805685,0.00057752314,0.0002695565,0.00033039736,0.0006501647],"category_scores_gemma":[0.00037550283,0.00012507677,0.00019901017,0.0022541187,0.00026679158,0.00029166855,0.00033435063,0.00017242746,0.00013219063],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000065866996,0.00005801931,0.9619102,0.000057669786,0.00006900537,0.0004790895,0.0005576308,0.0036687418,0.014850755,0.00017744514,0.00027944433,0.017826179],"study_design_scores_gemma":[0.0000054044604,0.000016569144,0.9939611,0.0000093460885,0.000009028423,0.000067350964,0.00023465756,0.005105296,0.00013879089,0.00005308931,0.00039512626,0.0000043534533],"about_ca_topic_score_codex":0.017430672,"about_ca_topic_score_gemma":0.035385836,"teacher_disagreement_score":0.017430672,"about_ca_system_score_codex":0.0002748459,"about_ca_system_score_gemma":0.00019880764,"threshold_uncertainty_score":0.034658432},"labels":[],"label_agreement":null},{"id":"W3081287100","doi":"10.1007/s10712-020-09606-4","title":"Earth Observation for the Assessment of Earthquake Hazard, Risk and Disaster Management","year":2020,"lang":"en","type":"article","venue":"Surveys in Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; Natural Environment Research Council; Indian Space Research Organisation; U.S. Geological Survey; Instituto Nacional de Técnica Aeroespacial; Korea Aerospace Research Institute; National Aeronautics and Space Administration; Royal Society; European Space Agency; Sight Research UK; Japan Aerospace Exploration Agency; Nancy and Stephen Grand Technion Energy Program","keywords":"Interferometric synthetic aperture radar; Seismic hazard; Hazard; Earthquake scenario; Earth observation; Geology; Seismic risk; Seismology; Synthetic aperture radar; Risk management; Emergency management; GNSS applications; Risk analysis (engineering); Satellite; Remote sensing; Global Positioning System; Computer science; Engineering; Business","score_opus":0.035263461868604004,"score_gpt":0.2489325744832327,"score_spread":0.21366911261462868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3081287100","genre_codex":"other","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.11760784,0.2886748,0.13865606,0.09083545,0.0051968214,0.0019812726,0.054254875,0.0019473888,0.30084544],"genre_scores_gemma":[0.6424306,0.16823384,0.11054469,0.0044601723,0.0021709912,0.0004886044,0.021093749,0.00015074752,0.05042662],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99965477,0.00015242156,0.000032595166,0.000021892522,0.00011593818,0.000022283111],"domain_scores_gemma":[0.9991353,0.00023373455,0.00017551059,0.00007255274,0.00031737823,0.00006546311],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015036775,0.0002644594,0.00027755607,0.0014115409,0.00017780378,0.0011717421,0.0001483464,0.00038541178,0.0049090777],"category_scores_gemma":[0.0021469626,0.00007946724,0.0002558788,0.0017037644,0.00016173553,0.00084094267,0.000726102,0.0004750141,0.0011836027],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015806474,0.000110613946,0.08303721,0.0009359119,0.00018493585,0.00018279225,0.00016510535,0.0032173924,0.003733846,0.022030108,0.100100115,0.7861439],"study_design_scores_gemma":[0.000072738265,0.00034712112,0.22260736,0.0023403086,0.00025558288,0.00046048572,0.0015152845,0.014527504,0.0022180746,0.025884919,0.729716,0.000054630316],"about_ca_topic_score_codex":0.01012936,"about_ca_topic_score_gemma":0.011734383,"teacher_disagreement_score":0.01012936,"about_ca_system_score_codex":0.0005064247,"about_ca_system_score_gemma":0.0014014996,"threshold_uncertainty_score":0.020140827},"labels":[],"label_agreement":null},{"id":"W3082102973","doi":"10.1007/s11069-020-04203-5","title":"The meteorological tsunami of 1 November 2010 in the southern Strait of Georgia: a case study","year":2020,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Tide gauge; Hydrography; Sea level; Oceanography; Climatology; Natural hazard; Geology; Low-pressure area; Seiche; Environmental science; Meteorology; Atmospheric pressure; Geography","score_opus":0.026286739705321673,"score_gpt":0.24847702885158734,"score_spread":0.22219028914626568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082102973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970293,0.00012412513,0.000057088488,0.0003955047,0.000008880552,0.000021842168,0.00017579463,0.0000043500536,0.0021831132],"genre_scores_gemma":[0.99872655,0.00037891528,0.00011386261,0.00009202717,0.0000073164983,0.0000079063,0.00014803073,0.0000028747534,0.000522518],"study_design_codex":"observational","study_design_gemma":"case_report","domain_scores_codex":[0.99979836,0.00005786189,0.00001095659,0.000018316947,0.000025053254,0.00008954461],"domain_scores_gemma":[0.9996057,0.00008931586,0.00011581127,0.000019074057,0.000047411508,0.0001226071],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026221358,0.00040815398,0.0002003492,0.0010346544,0.0019197033,0.00076070323,0.00083950075,0.001756962,0.0009431384],"category_scores_gemma":[0.0010334797,0.00026645706,0.0003324423,0.0017897084,0.000856207,0.0005793138,0.001280276,0.0005968044,0.00019743372],"study_design_candidate":"case_report","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030990917,0.00047780786,0.80382645,0.0003026321,0.00017923776,0.12614875,0.030911077,0.006054958,0.0032230078,0.0022625248,0.006010528,0.020293204],"study_design_scores_gemma":[0.00002221144,0.000256575,0.8736972,0.00016567686,0.00008664615,0.012374453,0.104243755,0.0024702419,0.00028010027,0.00039429596,0.005961717,0.000047142486],"about_ca_topic_score_codex":0.33169332,"about_ca_topic_score_gemma":0.6922909,"teacher_disagreement_score":0.6683067,"about_ca_system_score_codex":0.003861914,"about_ca_system_score_gemma":0.0025707274,"threshold_uncertainty_score":0.6595253},"labels":[],"label_agreement":null},{"id":"W3082814151","doi":"10.1177/0959683620950389","title":"Earthquake-triggered landslides and mudflows: Was this the wave that engulfed Ancient Helike?","year":2020,"lang":"en","type":"article","venue":"The Holocene","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Mudflow; Geology; Landslide; Context (archaeology); Archaeology; Seismology; Paleontology; Geography","score_opus":0.043969958329249076,"score_gpt":0.21032029278489184,"score_spread":0.16635033445564276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082814151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91823447,0.015940983,0.00046986854,0.0031470093,0.00019715409,0.000015715834,0.00041504923,0.000019618115,0.061560187],"genre_scores_gemma":[0.98608893,0.0067778607,0.00018104147,0.00024143363,0.00012770541,0.0000043409673,0.0001531619,0.0000057387397,0.0064197574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986136,0.000021665002,0.000011984902,0.000030792322,0.000036378093,0.00003773316],"domain_scores_gemma":[0.9998267,0.00002336935,0.000066043234,0.000014875784,0.00004063237,0.000028330955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002454577,0.00013645506,0.00013541874,0.00071646756,0.00077227363,0.0010170407,0.00022561372,0.00036320763,0.0032017892],"category_scores_gemma":[0.000784737,0.00013474571,0.00006320533,0.0010329669,0.0023321141,0.0007335886,0.0005963515,0.00027831554,0.00027822083],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005921884,0.00010758942,0.42689362,0.0014470574,0.00013137764,0.011317588,0.11359542,0.0007579685,0.013931718,0.11395563,0.012127848,0.30514202],"study_design_scores_gemma":[0.000015972673,0.000078181954,0.7622682,0.00043657704,0.00003675143,0.0034399112,0.029315552,0.00012804664,0.0013333494,0.006289093,0.19661547,0.000042913292],"about_ca_topic_score_codex":0.013678666,"about_ca_topic_score_gemma":0.032871872,"teacher_disagreement_score":0.013678666,"about_ca_system_score_codex":0.0019696513,"about_ca_system_score_gemma":0.0006255839,"threshold_uncertainty_score":0.027198076},"labels":[],"label_agreement":null},{"id":"W3082873047","doi":"10.1785/0120190265","title":"Ground-Motion Evaluation of Moderate and Large Interface Earthquakes along the Chilean Subduction Zone","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"","keywords":"Seismology; Subduction; Geology; Aftershock; Slip (aerodynamics); Induced seismicity; Ground motion; Tectonics","score_opus":0.030801825480396814,"score_gpt":0.23464990070005798,"score_spread":0.20384807521966117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082873047","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975485,0.00007339351,0.00094718114,0.00004066303,0.000003734666,0.000013200196,0.00074305513,0.000090494155,0.00053973054],"genre_scores_gemma":[0.9982804,0.000037390444,0.00048486353,0.0000043911177,0.0000020376824,0.000008051783,0.0008790146,0.000006863255,0.00029698474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986184,0.00004406548,0.000010714695,0.000039745926,0.00002111587,0.000022532562],"domain_scores_gemma":[0.9995116,0.00014490419,0.00009253583,0.000053968364,0.00010486824,0.00009212752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006414702,0.0006429483,0.00031578232,0.0009030126,0.00014968461,0.0005516394,0.00040035718,0.0003011749,0.0010553669],"category_scores_gemma":[0.0013128051,0.00018350074,0.00035293,0.00053966837,0.00017287426,0.00031292834,0.0005167427,0.00018911294,0.00026752567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005334403,0.00023038215,0.74904865,0.0001598374,0.00026204844,0.00055683276,0.00039681973,0.19923936,0.00900686,0.00025361645,0.0013031092,0.039008986],"study_design_scores_gemma":[0.000056946446,0.00018009666,0.63243467,0.000036159858,0.000049544065,0.000049223385,0.0006117528,0.3635166,0.0020319566,0.00012467605,0.0008770755,0.00003129184],"about_ca_topic_score_codex":0.057263862,"about_ca_topic_score_gemma":0.0534744,"teacher_disagreement_score":0.057263862,"about_ca_system_score_codex":0.000780774,"about_ca_system_score_gemma":0.00065819477,"threshold_uncertainty_score":0.113861084},"labels":[],"label_agreement":null},{"id":"W3083315441","doi":"","title":"The 2011 Tohoku Tsunami Generated Major Environmental Changes in a Distal Canadian Fjord","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Fjord; Oceanography; Geology; Geography","score_opus":0.010848650252796172,"score_gpt":0.18408197834386786,"score_spread":0.1732333280910717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3083315441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99682295,0.000075333235,0.000051870316,0.00023596066,0.000009367707,0.000009943498,0.00039464355,0.0000075244807,0.0023922536],"genre_scores_gemma":[0.9978047,0.000083796054,0.00011366815,0.00008307531,0.000003166027,0.000004749969,0.00025834914,0.0000055100395,0.0016429097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99967086,0.0000078239345,0.000010820294,0.000054425735,0.00007385238,0.00018218791],"domain_scores_gemma":[0.9995654,0.000015887468,0.000044632096,0.000011391625,0.00022843559,0.00013415352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016603166,0.000348516,0.00038511943,0.0010498456,0.0068140407,0.0016845586,0.0011800617,0.0011962747,0.00231116],"category_scores_gemma":[0.00073014596,0.00029257845,0.00033572697,0.0025788539,0.0016492804,0.00044626664,0.001635947,0.00086475076,0.00027282853],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036018694,0.00014822486,0.94921845,0.00010979876,0.000119677235,0.0031621107,0.01016948,0.0029523033,0.007891515,0.0009164376,0.004334009,0.020617858],"study_design_scores_gemma":[0.000007896355,0.000014747986,0.9865839,0.000024267827,0.000031910407,0.00012968671,0.009504651,0.0008446028,0.00017004421,0.000077985744,0.0025892744,0.000021054735],"about_ca_topic_score_codex":0.9955314,"about_ca_topic_score_gemma":0.9986759,"teacher_disagreement_score":0.021139693,"about_ca_system_score_codex":0.021139693,"about_ca_system_score_gemma":0.023177808,"threshold_uncertainty_score":0.15337998},"labels":[],"label_agreement":null},{"id":"W3084202746","doi":"10.1029/2020jb019750","title":"A Double Difference Tomography Study of the Washington Forearc: Does Siletzia Control Crustal Seismicity?","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Forearc; Geology; Seismology; Induced seismicity; Crust; Seismic tomography; Ridge; Subduction; Tectonics; Geophysics; Paleontology; Mantle (geology)","score_opus":0.04383792682498397,"score_gpt":0.2975117801784116,"score_spread":0.2536738533534276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084202746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983449,0.000038993232,0.0010329257,0.000028800709,9.1062645e-7,0.0000026804291,0.000044616,0.000013497938,0.0004926093],"genre_scores_gemma":[0.9995202,0.000022062664,0.00031357596,0.0000035459518,7.0662156e-7,9.2825206e-7,0.00003410263,0.0000015574203,0.00010325648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999702,0.000004039502,0.000001345346,0.000010672206,0.0000051903567,0.000008496689],"domain_scores_gemma":[0.9998994,0.000021569467,0.00003493439,0.0000099245335,0.000020811436,0.000013324019],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009228921,0.00016433002,0.000116555115,0.00041849157,0.00014637237,0.00037725148,0.00023655043,0.00020123678,0.0005857937],"category_scores_gemma":[0.0003957249,0.00016000618,0.000098078446,0.0003439811,0.00026101407,0.00028863837,0.00021132105,0.00017553875,0.000062831474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059409393,0.00020862614,0.7498197,0.000050742055,0.00014958646,0.0014636515,0.00054173556,0.030434031,0.1730326,0.0020571486,0.00032860617,0.041319504],"study_design_scores_gemma":[0.000020393554,0.00008984031,0.8921772,0.000009696333,0.000040866867,0.00024478417,0.0005405752,0.09718014,0.008534772,0.00050733855,0.0006350005,0.000019350922],"about_ca_topic_score_codex":0.035591938,"about_ca_topic_score_gemma":0.05597429,"teacher_disagreement_score":0.035591938,"about_ca_system_score_codex":0.00038627032,"about_ca_system_score_gemma":0.00034538703,"threshold_uncertainty_score":0.07076955},"labels":[],"label_agreement":null},{"id":"W3084416941","doi":"10.5194/egusphere-egu2020-15909","title":"Sediment failure of St. Pierre Slope: new insights of failure mechanisms and slope instability due to the 1929 Grand Banks Earthquake","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Natural Resources Canada; Dalhousie University","funders":"","keywords":"Geology; Landslide; Seafloor spreading; Bathymetry; Seismology; Instability; Submarine pipeline; Submarine landslide; Slip (aerodynamics); Escarpment; Sediment; Holocene; Geomorphology; Geotechnical engineering; Oceanography","score_opus":0.016092354861078382,"score_gpt":0.2010972622665341,"score_spread":0.18500490740545572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084416941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989586,0.0001223745,0.00013250466,0.000027378168,9.335794e-7,0.0000030217009,0.000139454,0.000006664923,0.0006089436],"genre_scores_gemma":[0.9992843,0.00014837028,0.00016898071,0.000011341198,0.0000041211492,0.0000018240006,0.00019050375,0.0000015337084,0.00018888844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999267,0.0000069668745,0.000004889352,0.000015428219,0.000019927935,0.00002614541],"domain_scores_gemma":[0.99980944,0.000026265043,0.00007717517,0.00001299376,0.00004121917,0.00003283672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001437522,0.00025279095,0.00023675238,0.0014601557,0.00030093122,0.0005677041,0.00023164468,0.000296602,0.0005737172],"category_scores_gemma":[0.00029430012,0.00018726403,0.00021841089,0.00084872794,0.0005083232,0.0002459473,0.00039103976,0.00023552624,0.00013707843],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007036326,0.000032806383,0.9641048,0.000034498145,0.000051965413,0.0012435156,0.0005756275,0.0019956366,0.021179045,0.00010603189,0.00019492468,0.010410895],"study_design_scores_gemma":[5.895759e-7,0.000010471634,0.9983461,0.00000280908,0.0000064386386,0.00010942194,0.00019396289,0.0009844097,0.00022449356,0.000018708039,0.00009922833,0.0000033144788],"about_ca_topic_score_codex":0.122823454,"about_ca_topic_score_gemma":0.20904367,"teacher_disagreement_score":0.8771765,"about_ca_system_score_codex":0.0008628754,"about_ca_system_score_gemma":0.0005630766,"threshold_uncertainty_score":0.2442171},"labels":[],"label_agreement":null},{"id":"W3084419509","doi":"10.5194/egusphere-egu2020-21838","title":"Fluvial incised networks on top of late Ordovician interglacial valley buried hills as the result of post glacial isostatic rebound; 3D seismic input","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Glacial period; Fluvial; Paleontology; Interglacial; Tributary; Glacier; Subaerial; Post-glacial rebound; Geomorphology; Ice sheet; Structural basin","score_opus":0.013365820163618418,"score_gpt":0.2176475269303868,"score_spread":0.20428170676676838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084419509","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9822942,0.00014312932,0.004642317,0.000060241153,0.00001615892,0.000018358522,0.0042113303,0.0008117106,0.0078026652],"genre_scores_gemma":[0.9909705,0.00011751107,0.002288317,0.000008237426,0.0000053119024,0.00001055067,0.0028106342,0.00003898939,0.0037499205],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999467,0.0000025898944,0.0000035445703,0.0000161703,0.000016133687,0.000014902705],"domain_scores_gemma":[0.99994326,0.00000775535,0.000012240737,0.0000083533505,0.000018808487,0.000009477374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000053523832,0.00021181467,0.000102631384,0.0011646338,0.00015604276,0.00078485475,0.00025666214,0.0001291004,0.0066144904],"category_scores_gemma":[0.00021668202,0.00020012983,0.00013536013,0.0013214968,0.00015645097,0.00013488301,0.00035774588,0.00008214579,0.0005806714],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029244227,0.00009680618,0.5075594,0.0003170561,0.00012388939,0.0022232893,0.0016609385,0.1398199,0.044630703,0.004681978,0.008154014,0.29043964],"study_design_scores_gemma":[0.000021222088,0.000041172156,0.81044084,0.000059013073,0.000057672434,0.0005269973,0.0010712488,0.15869789,0.0067708595,0.0015106143,0.02077038,0.000032148928],"about_ca_topic_score_codex":0.017859174,"about_ca_topic_score_gemma":0.039872497,"teacher_disagreement_score":0.017859174,"about_ca_system_score_codex":0.00052213843,"about_ca_system_score_gemma":0.00033240046,"threshold_uncertainty_score":0.03551042},"labels":[],"label_agreement":null},{"id":"W3084544790","doi":"","title":"New perspectives on the 2007 seismic swarm in the Anahim Volcanic Belt, British Columbia, from earthquake cross-correlation and high-resolution relocations","year":2010,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Volcano; Earthquake swarm; High resolution; Seismic microzonation; Remote sensing; Induced seismicity","score_opus":0.011066001478956703,"score_gpt":0.21544718853496514,"score_spread":0.20438118705600844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084544790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8532194,0.043991227,0.004597837,0.025572466,0.0004218784,0.00004914254,0.008250849,0.00014464169,0.06375258],"genre_scores_gemma":[0.9684521,0.014208921,0.003398672,0.0010774995,0.00029112565,0.000016572081,0.0026646731,0.000046726167,0.009843673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999749,0.000045953788,0.000021182035,0.00004672546,0.00006569318,0.0000714149],"domain_scores_gemma":[0.9977272,0.00051171385,0.00022398411,0.00020162483,0.0010576685,0.00027777324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009020908,0.00044783615,0.00049659587,0.003684403,0.0023383764,0.00448097,0.0009135559,0.0007609958,0.0047473307],"category_scores_gemma":[0.0036459211,0.000326019,0.00023764366,0.009311117,0.0020824347,0.0019520834,0.0015674132,0.0011967836,0.00032245743],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004614623,0.00014327714,0.61402696,0.00093847694,0.00039717078,0.0026431077,0.021505073,0.0114890495,0.012150171,0.024099456,0.03690938,0.27523646],"study_design_scores_gemma":[0.000012807668,0.00001891167,0.89663213,0.00038824163,0.00015337992,0.00025447187,0.025380393,0.0033170278,0.00044405027,0.006362416,0.06695644,0.000079722544],"about_ca_topic_score_codex":0.93242097,"about_ca_topic_score_gemma":0.9819394,"teacher_disagreement_score":0.06757903,"about_ca_system_score_codex":0.00983031,"about_ca_system_score_gemma":0.009060028,"threshold_uncertainty_score":0.13595396},"labels":[],"label_agreement":null},{"id":"W3085623945","doi":"","title":"Eastern Canadian crustal deformation rates implied by Canada's fourth-generation seismic hazard model","year":2003,"lang":"en","type":"article","venue":"EGS - AGU - EUG Joint Assembly","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Seismic hazard; Deformation (meteorology); Hazard; Oceanography","score_opus":0.025315924937011482,"score_gpt":0.20847740800771677,"score_spread":0.1831614830707053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3085623945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9109173,0.0005077205,0.0023517923,0.0031075324,0.00009539722,0.000047639034,0.046001222,0.00042565516,0.036545794],"genre_scores_gemma":[0.97884274,0.00038660955,0.0013140237,0.00012024156,0.000007764648,0.000018893892,0.008915409,0.000049847797,0.0103444625],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9997347,0.000022787706,0.00001413831,0.00004175864,0.00006324753,0.0001232276],"domain_scores_gemma":[0.9989171,0.000120054334,0.00006825462,0.00005843854,0.0006984436,0.00013774789],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048337952,0.0005951214,0.00042558936,0.0013422129,0.0017441788,0.0018619684,0.0018002866,0.0009216874,0.0072308024],"category_scores_gemma":[0.0019621705,0.0005093198,0.0007800277,0.002244701,0.00057287986,0.000646666,0.00046584453,0.00095550064,0.0005569421],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031291498,0.00005951721,0.073333144,0.00007677839,0.0001635596,0.00022440661,0.00022251085,0.87370175,0.00057124643,0.015654078,0.02436551,0.01131463],"study_design_scores_gemma":[0.00020791625,0.000029691098,0.11621134,0.000070277645,0.00016982177,0.00008496187,0.00071277865,0.849755,0.00078633294,0.0044631227,0.027316943,0.00019181908],"about_ca_topic_score_codex":0.9977151,"about_ca_topic_score_gemma":0.99734604,"teacher_disagreement_score":0.038875833,"about_ca_system_score_codex":0.038875833,"about_ca_system_score_gemma":0.0374845,"threshold_uncertainty_score":0.2820652},"labels":[],"label_agreement":null},{"id":"W3085784190","doi":"","title":"The Seismicity and Tsunamis of Canada: 1663-2005","year":2005,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Seismology; Geology; Geography","score_opus":0.010939704174827342,"score_gpt":0.19433535073038594,"score_spread":0.1833956465555586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3085784190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5851514,0.005748045,0.0006567805,0.008423973,0.00070367,0.00014129453,0.33656952,0.0003325855,0.062272817],"genre_scores_gemma":[0.74304074,0.0039780904,0.0009892461,0.0008605546,0.00010100745,0.00004672669,0.09916945,0.00012826119,0.15168601],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99956805,0.000006233635,0.00002381529,0.000037304988,0.00021133765,0.00015321276],"domain_scores_gemma":[0.9977576,0.000025581923,0.0001091906,0.000026383535,0.0017383866,0.00034287694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030485998,0.0005773379,0.00039952146,0.0023171457,0.0023727992,0.002269352,0.00084819435,0.0007605383,0.011669784],"category_scores_gemma":[0.0012725386,0.0003552157,0.00041391936,0.0057484475,0.00037659408,0.000588781,0.00095267047,0.001320818,0.0022901162],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00087480975,0.00016295165,0.59770066,0.00052634405,0.00041850843,0.00054714654,0.0031385305,0.004913223,0.0014838141,0.0032482953,0.30743447,0.0795513],"study_design_scores_gemma":[0.000030837422,0.000021338405,0.8981399,0.00011892927,0.000048679987,0.00008709303,0.0021794562,0.0012146935,0.000477441,0.00024646078,0.09739504,0.000040086317],"about_ca_topic_score_codex":0.99807835,"about_ca_topic_score_gemma":0.99950576,"teacher_disagreement_score":0.03729556,"about_ca_system_score_codex":0.03729556,"about_ca_system_score_gemma":0.06338825,"threshold_uncertainty_score":0.27059954},"labels":[],"label_agreement":null},{"id":"W3086657693","doi":"10.1029/2020jb020918","title":"Crustal Velocity Variations and Constraints on Material Properties in the Charlevoix Seismic Zone, Eastern Canada","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Geology; Bouguer anomaly; Seismology; Seismic velocity; Seismic tomography; Impact structure; Tectonics; Gravity anomaly; Fault (geology); Geophysics; Petrology; Mantle (geology); Paleontology; Impact crater","score_opus":0.0445795046145749,"score_gpt":0.27636742034183664,"score_spread":0.23178791572726176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3086657693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99786264,0.00009850272,0.00008030018,0.000033746546,9.529882e-7,0.0000050970903,0.0004334938,0.00001261542,0.001472644],"genre_scores_gemma":[0.9991198,0.00005608718,0.00009125301,0.0000059577114,4.6652835e-7,0.0000019442166,0.0002847123,0.0000030459787,0.0004366754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997489,0.000009657049,0.000008866692,0.00004846323,0.00008737119,0.00009678177],"domain_scores_gemma":[0.99942005,0.000048387727,0.00008638953,0.000019568912,0.0002966995,0.00012892851],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022156253,0.0003409318,0.00025303644,0.0021630216,0.0015599137,0.0014060703,0.0006257697,0.00024735124,0.0014562593],"category_scores_gemma":[0.0007276762,0.0002333509,0.00021680228,0.0022508488,0.00081497454,0.00021773452,0.0007861977,0.0002203438,0.000112208305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006473538,0.00001964107,0.9848562,0.000020508383,0.000046225658,0.00015046333,0.00061401445,0.002085515,0.003409606,0.00036628256,0.00033345,0.0080333175],"study_design_scores_gemma":[0.0000023797857,0.0000037636821,0.9973214,0.0000069052217,0.0000063150687,0.000015792048,0.0006414153,0.0013928029,0.00017909458,0.000028301445,0.00039620828,0.0000055664796],"about_ca_topic_score_codex":0.9909219,"about_ca_topic_score_gemma":0.9949085,"teacher_disagreement_score":0.015853953,"about_ca_system_score_codex":0.015853953,"about_ca_system_score_gemma":0.010580892,"threshold_uncertainty_score":0.11502904},"labels":[],"label_agreement":null},{"id":"W3087202451","doi":"","title":"The Betsiamites-Outardes (Quebec) Submarine Mass Movements and Their Potential for Tsunami Generation","year":2003,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Submarine; Geology; Mass movement; Seismology; Oceanography; Landslide","score_opus":0.01722715833614897,"score_gpt":0.21020313854299996,"score_spread":0.192975980206851,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087202451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978455,0.0007474415,0.00026601192,0.000991358,0.000019018875,0.0000304102,0.0023453082,0.000014146371,0.01713127],"genre_scores_gemma":[0.98406065,0.00035084895,0.00019044043,0.00011191051,0.0000074126683,0.000012644138,0.0005015313,0.0000072345274,0.014757382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988925,0.000011791593,0.0000028909137,0.00001851084,0.000032486292,0.000045078763],"domain_scores_gemma":[0.99960405,0.00004763636,0.00007678422,0.000011369891,0.0001886131,0.00007159117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019236593,0.00022340401,0.00014038866,0.0007167609,0.0018074294,0.0012844151,0.00044042614,0.00036962944,0.0070774974],"category_scores_gemma":[0.000995559,0.0001286667,0.00013130835,0.0013427115,0.00059216446,0.00047712174,0.00043539747,0.00047553625,0.0003815128],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007784549,0.00011391925,0.8699877,0.00009740165,0.00017824465,0.0010009509,0.0060715205,0.005005941,0.0046991385,0.009792188,0.013716526,0.08855789],"study_design_scores_gemma":[0.000021746702,0.000028632701,0.97932863,0.00002816407,0.000018786955,0.000054055035,0.002407577,0.001954523,0.00019972546,0.00022623334,0.015718922,0.0000129623495],"about_ca_topic_score_codex":0.99381036,"about_ca_topic_score_gemma":0.9980393,"teacher_disagreement_score":0.021208793,"about_ca_system_score_codex":0.021208793,"about_ca_system_score_gemma":0.008080427,"threshold_uncertainty_score":0.15388131},"labels":[],"label_agreement":null},{"id":"W3087485137","doi":"","title":"Fault Segmentation and Earthquake Generation in the Transition from Strike-slip to Subduction Plate Motion, Saint Elias Orogen, Alaska and Yukon (Invited)","year":2010,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Subduction; Geology; Slip (aerodynamics); Plate tectonics; Fault (geology); Triple junction; Ground motion; Geophysics; Tectonics; Engineering","score_opus":0.01956253784326344,"score_gpt":0.22287857247354917,"score_spread":0.20331603463028572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087485137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99870944,0.00013758235,0.000054827608,0.00008677623,0.0000054069005,0.0000021456685,0.00009666445,0.000002453173,0.0009048588],"genre_scores_gemma":[0.9980039,0.00020136517,0.000054203007,0.000012676135,0.0000061507535,0.0000019723343,0.00012947983,0.0000032221144,0.0015869715],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999685,0.0000057199995,0.0000024474996,0.000009024278,0.0000025266754,0.00001166319],"domain_scores_gemma":[0.9997969,0.00006626225,0.000035003577,0.000003382201,0.000053906704,0.000044585082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016643172,0.000075333,0.000107155865,0.00022602259,0.0003518865,0.0007710918,0.00011558325,0.00017575882,0.0019694695],"category_scores_gemma":[0.00076672516,0.0000880301,0.00009833083,0.0005022465,0.00026837204,0.00027125547,0.00023953037,0.00015435602,0.00017124842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028212513,0.00010192421,0.9341959,0.00012357024,0.000086644046,0.00083488185,0.0053235977,0.005648735,0.013727461,0.0013746141,0.002052731,0.03370882],"study_design_scores_gemma":[0.000006038897,0.000046979316,0.99568164,0.0000094072675,0.000014752109,0.00003514135,0.0022127647,0.00076903845,0.0004919574,0.00025882176,0.00046946062,0.0000039166734],"about_ca_topic_score_codex":0.07863853,"about_ca_topic_score_gemma":0.16378048,"teacher_disagreement_score":0.92136145,"about_ca_system_score_codex":0.00068958855,"about_ca_system_score_gemma":0.0004664066,"threshold_uncertainty_score":0.15636158},"labels":[],"label_agreement":null},{"id":"W3087701769","doi":"10.5194/egusphere-egu2020-11523","title":"Geomorphic evidence for active, co-seismic slip along a low-angle normal fault: Panamint Valley, California","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Fault scarp; Detachment fault; Fault (geology); Seismology; Tectonics; Alluvial fan; Slip (aerodynamics); Basin and range topography; Normal fault; Structural basin; Paleontology; Extensional definition","score_opus":0.05767891002197934,"score_gpt":0.26233459245358326,"score_spread":0.20465568243160392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087701769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973214,0.00010975264,0.000037169528,0.000021393083,0.000002891434,0.0000042931065,0.00028127048,0.0000095308515,0.0022123775],"genre_scores_gemma":[0.99895966,0.000116009476,0.000114612776,0.000007115787,0.0000033248762,0.000003409074,0.0003805401,0.0000016878136,0.0004136337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998969,0.000006132655,0.000008113623,0.000043664255,0.000027817812,0.00001745146],"domain_scores_gemma":[0.99963653,0.000042209234,0.00010922015,0.000024933252,0.00011866039,0.000068374495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016341484,0.00012418439,0.000105014275,0.0008435196,0.0006184272,0.0006019125,0.00028918404,0.00015183166,0.0009133144],"category_scores_gemma":[0.00040485646,0.00014249951,0.000052658554,0.00089362316,0.00045936982,0.00015887464,0.0003875358,0.0001541648,0.00009213137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010702183,0.000053208667,0.9769695,0.00006210653,0.000029717272,0.00032346993,0.0014241278,0.00028762716,0.0049724584,0.00012646973,0.0010316476,0.014612701],"study_design_scores_gemma":[0.0000046254463,0.000009942043,0.99879897,0.0000078335215,0.000006903315,0.00006080409,0.00027334443,0.00008794133,0.000087217864,0.000009983126,0.0006506049,0.0000018938547],"about_ca_topic_score_codex":0.19573227,"about_ca_topic_score_gemma":0.4856045,"teacher_disagreement_score":0.19573227,"about_ca_system_score_codex":0.00087455765,"about_ca_system_score_gemma":0.0005416271,"threshold_uncertainty_score":0.38918597},"labels":[],"label_agreement":null},{"id":"W3087735662","doi":"10.1029/2020gc009214","title":"A Global Data Set of Present‐Day Oceanic Crustal Age and Seafloor Spreading Parameters","year":2020,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":355,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ARC Resources (Canada); University of Calgary","funders":"Australian Research Council; Alfred P. Sloan Foundation","keywords":"Geology; Crust; Seafloor spreading; Oceanic crust; Tectonics; Subduction; Seismology; Paleontology","score_opus":0.041126538426363275,"score_gpt":0.23835746815030046,"score_spread":0.1972309297239372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087735662","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.31046054,0.00028924152,0.0071082334,0.00010376284,0.0000374931,0.00006981971,0.67637855,0.0018159873,0.0037363835],"genre_scores_gemma":[0.2308852,0.00013150861,0.009373909,0.000028792838,0.000013998813,0.00012286403,0.7586223,0.00013895419,0.000682411],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997458,0.000024865518,0.000034461762,0.00009141491,0.00007683495,0.00002663039],"domain_scores_gemma":[0.9983741,0.00016827046,0.00020967716,0.0005559441,0.0005499605,0.00014197496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005064066,0.00068091083,0.0005114514,0.0029458222,0.0002354115,0.000618025,0.0006095384,0.00043474676,0.0032214841],"category_scores_gemma":[0.001790294,0.00026782477,0.0006012511,0.0037511988,0.00019022713,0.0006596354,0.00080163655,0.00046770016,0.002525225],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044945086,0.00028373365,0.6670809,0.0006877902,0.0007011909,0.00036733557,0.00042353634,0.07609721,0.015717972,0.0015776089,0.07512176,0.16149153],"study_design_scores_gemma":[0.000104287,0.00011146932,0.8573166,0.00011570147,0.00013405104,0.0002462446,0.0002980678,0.03535912,0.0068015023,0.0011279325,0.0982678,0.00011714461],"about_ca_topic_score_codex":0.021695174,"about_ca_topic_score_gemma":0.015473342,"teacher_disagreement_score":0.021695174,"about_ca_system_score_codex":0.0002921294,"about_ca_system_score_gemma":0.0005397754,"threshold_uncertainty_score":0.04313779},"labels":[],"label_agreement":null},{"id":"W3087814553","doi":"10.5194/egusphere-egu2020-15268","title":"Untangling the dynamics of the 2019 Ridgecrest sequence by integrated dynamic rupture and Coulomb stress modeling across an immature 3D conjugate fault network","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Fault (geology); Aftershock; Stress (linguistics); Geology; Geometry; Seismology; Mathematics","score_opus":0.01466725429784054,"score_gpt":0.23674231151919503,"score_spread":0.22207505722135448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087814553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9795864,0.00011604729,0.01234946,0.0003406376,0.000029451921,0.000024665213,0.0016979966,0.00034310663,0.005512281],"genre_scores_gemma":[0.99628663,0.000061245235,0.0023524305,0.00002325363,0.000009744645,0.000014572455,0.0006721452,0.00003384729,0.00054612954],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993885,0.000011126812,0.00000530652,0.000017906536,0.000011627572,0.000015097924],"domain_scores_gemma":[0.9998704,0.000030354928,0.000028650176,0.000022760323,0.000022212862,0.000025637486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014725585,0.00032105463,0.00031283198,0.0004815774,0.00019750038,0.0007795313,0.0006006795,0.0009049618,0.0018350483],"category_scores_gemma":[0.0006868803,0.0002510982,0.0006077077,0.0005531294,0.0003841919,0.00043271933,0.00046519842,0.0004054269,0.00024702481],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004025524,0.000033207325,0.008045483,0.000014415191,0.000022733713,0.00010753265,0.000037490638,0.98678094,0.0010516044,0.001133494,0.00029010652,0.0024427436],"study_design_scores_gemma":[0.000008663251,0.000010308667,0.0036608847,0.0000030728174,0.000003941995,0.0000149099715,0.000020997455,0.9955746,0.0001287066,0.00036823275,0.00020035634,0.000005397954],"about_ca_topic_score_codex":0.024444008,"about_ca_topic_score_gemma":0.018397138,"teacher_disagreement_score":0.024444008,"about_ca_system_score_codex":0.00062842213,"about_ca_system_score_gemma":0.000543977,"threshold_uncertainty_score":0.048603475},"labels":[],"label_agreement":null},{"id":"W3087879197","doi":"10.1139/cgj-2020-0248","title":"Quantifying discrete seismic responses to mining","year":2020,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"Natural Sciences and Engineering Research Council of Canada; Australian Centre for Geomechanics","keywords":"Induced seismicity; Rock mass classification; Underground mining (soft rock); Geology; Seismology; Rock blasting; Centroid; Mining engineering; Seismic wave; Excavation; Geotechnical engineering; Engineering; Coal mining; Computer science; Artificial intelligence","score_opus":0.05711201084092594,"score_gpt":0.25794188833628257,"score_spread":0.20082987749535663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087879197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8966881,0.000053182353,0.100426465,0.000038628827,0.00001008117,0.00004786944,0.00046421614,0.00017662061,0.0020947522],"genre_scores_gemma":[0.99138325,0.000040390838,0.008009552,0.0000056789213,0.000007075409,0.000024039911,0.00025403063,0.00001443353,0.0002616152],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999736,0.00004000597,0.000016608703,0.00007878224,0.00010155374,0.000027123373],"domain_scores_gemma":[0.9990663,0.0004130215,0.00022203775,0.00010924689,0.00012381586,0.00006555286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003789598,0.00032147148,0.00019860377,0.0011237925,0.00012625528,0.00034459308,0.00026567167,0.00029309158,0.00079407444],"category_scores_gemma":[0.0023663244,0.00011924761,0.00015306988,0.0007366461,0.00028134708,0.00040649305,0.00048563143,0.0003027863,0.00017476766],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046786357,0.00022297501,0.18183596,0.00036989356,0.00018782263,0.00035368558,0.000986212,0.3956606,0.16994618,0.0057547768,0.0010137602,0.24320023],"study_design_scores_gemma":[0.000015735493,0.00038643877,0.34895676,0.000035277022,0.000049879596,0.00032134601,0.0008856164,0.61798793,0.024455352,0.0042051952,0.0026435072,0.00005701576],"about_ca_topic_score_codex":0.0014606426,"about_ca_topic_score_gemma":0.0020053468,"teacher_disagreement_score":0.0014606426,"about_ca_system_score_codex":0.00026236285,"about_ca_system_score_gemma":0.00019513698,"threshold_uncertainty_score":0.0029043555},"labels":[],"label_agreement":null},{"id":"W3087956755","doi":"10.3390/geosciences11060254","title":"Seismicity and the State of Stress in the Dezful Embayment, Zagros Fold and Thrust Belt","year":2021,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Seismology; Induced seismicity; Thrust fault; Borehole; Stress field; Fault (geology); Cauchy stress tensor; Strike-slip tectonics; Fold (higher-order function); Focal mechanism; Geotechnical engineering","score_opus":0.013476669397381865,"score_gpt":0.21151305151180325,"score_spread":0.19803638211442137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087956755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997714,0.000025136966,0.000016421862,0.000008685612,4.0658026e-7,5.5739014e-7,0.000057999,8.7586227e-7,0.00011859076],"genre_scores_gemma":[0.99966085,0.000033673245,0.000042682135,0.0000029972507,0.0000017157581,9.212054e-7,0.00018241208,3.328135e-7,0.00007447752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998863,0.000011040126,0.000013580079,0.000027865442,0.000022373286,0.000038833456],"domain_scores_gemma":[0.9997837,0.0000212304,0.00012725139,0.00001288888,0.000029861785,0.000025015357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022774952,0.00024452593,0.00018188333,0.0012997177,0.00023481343,0.00049164286,0.00016864295,0.00020775014,0.00041712885],"category_scores_gemma":[0.00049207493,0.000130738,0.00013637402,0.0011027897,0.00032446094,0.00031979787,0.00024883245,0.0001459089,0.00012097681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007513592,0.000020572112,0.9923848,0.00000829929,0.000026350499,0.00012002862,0.00035122645,0.0003461748,0.0015936262,0.00007338546,0.000051859188,0.0049484908],"study_design_scores_gemma":[0.0000014022143,0.000010364915,0.9995702,0.0000016312295,0.0000025755546,0.000022583765,0.00015367127,0.000121647834,0.000042972566,0.000008553163,0.00006331309,0.0000010734954],"about_ca_topic_score_codex":0.029666048,"about_ca_topic_score_gemma":0.056239545,"teacher_disagreement_score":0.029666048,"about_ca_system_score_codex":0.0008042189,"about_ca_system_score_gemma":0.0002578382,"threshold_uncertainty_score":0.058986723},"labels":[],"label_agreement":null},{"id":"W3088608286","doi":"10.1080/00288306.2020.1823433","title":"Shallow seismic reflection imaging of the Alpine Fault through late Quaternary sedimentary units at Whataroa, New Zealand","year":2020,"lang":"en","type":"article","venue":"New Zealand Journal of Geology and Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Marsden Fund; University of Otago","keywords":"Geology; Quaternary; Reflection (computer programming); Seismology; Sedimentary rock; Fault (geology); Geophysical imaging; Paleontology","score_opus":0.01960610152609053,"score_gpt":0.2262458109445053,"score_spread":0.20663970941841478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088608286","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955922,0.00010342157,0.00016325472,0.00004876929,0.000004423644,0.000026966318,0.0007786334,0.000022666982,0.003259661],"genre_scores_gemma":[0.99725133,0.00017317079,0.0005156841,0.000017801836,0.000005318122,0.000015362411,0.0005384162,0.000008632362,0.001474217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992085,0.000002648423,0.0000053021754,0.000021818008,0.000029417048,0.000019975252],"domain_scores_gemma":[0.99980956,0.000008173567,0.0000593906,0.0000083139685,0.000074799114,0.000039794217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001236141,0.00027056944,0.00016405745,0.001650399,0.0005772925,0.0005993622,0.00025299375,0.00023448076,0.0017223172],"category_scores_gemma":[0.00037109648,0.00021799315,0.00012944185,0.001309057,0.00025714785,0.0002537397,0.00037983005,0.00019930319,0.00031076305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003440733,0.00013821734,0.7426561,0.00019949056,0.00008682577,0.001259242,0.008182074,0.0008112018,0.18408705,0.00015579694,0.0021821763,0.059897646],"study_design_scores_gemma":[0.000007515637,0.00002415748,0.9976712,0.000014252343,0.000009065122,0.00009638703,0.00073656347,0.00027494956,0.00044370946,0.000006113766,0.00071232836,0.000003861295],"about_ca_topic_score_codex":0.29979753,"about_ca_topic_score_gemma":0.5742384,"teacher_disagreement_score":0.29979753,"about_ca_system_score_codex":0.00074649125,"about_ca_system_score_gemma":0.00063191913,"threshold_uncertainty_score":0.59610504},"labels":[],"label_agreement":null},{"id":"W3088835964","doi":"10.1093/gji/ggaa450","title":"Local and regional P-wave spectral attenuation model for Iran","year":2020,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; International Institute of Earthquake Engineering and Seismology","keywords":"Attenuation; Amplitude; Geology; Geodesy; Coda; Range (aeronautics); Seismology; Physics; Optics; Materials science","score_opus":0.0714614262605182,"score_gpt":0.2512755527111178,"score_spread":0.17981412645059958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088835964","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47675905,0.00031161826,0.5140327,0.00016966887,0.00001752668,0.00007195471,0.0010149945,0.0008502056,0.006772295],"genre_scores_gemma":[0.98758775,0.00011880824,0.010002415,0.000014851192,0.000010482135,0.000045039847,0.0005751638,0.0000566217,0.0015888227],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998159,0.000028563632,0.0000075892594,0.00006601758,0.000048156493,0.000033782402],"domain_scores_gemma":[0.9997334,0.000052516498,0.00008011248,0.000030350422,0.00009045594,0.0000132468585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038669142,0.0005741819,0.0003824824,0.0006040599,0.00021325627,0.00045464607,0.001507084,0.0004485787,0.0013977775],"category_scores_gemma":[0.000849416,0.0002776146,0.00087343133,0.0005371773,0.00029141616,0.000609068,0.00036860126,0.0004960924,0.0005718128],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035775694,0.00002038638,0.00826123,0.000017135468,0.00003957906,0.00009261298,0.000049444723,0.9766092,0.0021550595,0.0014248706,0.00040548324,0.0108892],"study_design_scores_gemma":[0.0000032528342,0.000011485191,0.0023742288,0.000001692133,0.0000117809,0.00004088383,0.000011540164,0.9965533,0.00018574488,0.0005910046,0.00021006905,0.0000049605424],"about_ca_topic_score_codex":0.021726575,"about_ca_topic_score_gemma":0.01005967,"teacher_disagreement_score":0.021726575,"about_ca_system_score_codex":0.00075140514,"about_ca_system_score_gemma":0.0006258988,"threshold_uncertainty_score":0.043200254},"labels":[],"label_agreement":null},{"id":"W3089501435","doi":"10.5194/egusphere-egu2020-6369","title":"Coupling poroelastic stress change and rate-state fault slip models to simulate fluid injection induced seismic and aseismic slip","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Poromechanics; Induced seismicity; Geology; Hydraulic fracturing; Pore water pressure; Seismology; Slip (aerodynamics); Seismic hazard; Fluid pressure; Fault (geology); Fluid dynamics; Geotechnical engineering; Microseism; Stress (linguistics); Shear stress; Mechanics; Porosity; Engineering; Porous medium","score_opus":0.07033601586712872,"score_gpt":0.23419721732302273,"score_spread":0.163861201455894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3089501435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9716114,0.00013580537,0.01747449,0.00038574432,0.00008102723,0.000092077185,0.00065063173,0.0003041387,0.00926467],"genre_scores_gemma":[0.9949787,0.00005358781,0.003090257,0.000051653376,0.000012636204,0.00005578051,0.00019225685,0.00003239987,0.0015325611],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998116,0.000041522344,0.000015774254,0.0000389809,0.000029957147,0.000062318744],"domain_scores_gemma":[0.99910754,0.00044443682,0.0001392689,0.00005440856,0.00014505947,0.00010930705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048709483,0.00074757833,0.0008068294,0.00083847425,0.0005357287,0.001057825,0.0016012287,0.002327551,0.0030823364],"category_scores_gemma":[0.0017206471,0.0006252668,0.00096639834,0.00056497107,0.0008160818,0.00064417167,0.000808253,0.0013138646,0.00022512488],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019062934,0.00003706423,0.0019185222,0.0000074182562,0.000010658467,0.000034683802,0.000015519472,0.9969261,0.0002789782,0.00026912073,0.000071061084,0.00041189216],"study_design_scores_gemma":[0.000005075122,0.0000062932677,0.00026761417,0.0000012275402,0.000002421488,0.000001962487,0.000009015205,0.999556,0.00004709973,0.00005967647,0.000041113213,0.000002477338],"about_ca_topic_score_codex":0.08522653,"about_ca_topic_score_gemma":0.05342286,"teacher_disagreement_score":0.08522653,"about_ca_system_score_codex":0.0016514371,"about_ca_system_score_gemma":0.0015550999,"threshold_uncertainty_score":0.16946095},"labels":[],"label_agreement":null},{"id":"W3090044403","doi":"10.1029/2018tc005365","title":"Seismic Hazard Analyses From Geologic and Geomorphic Data: Current and Future Challenges","year":2020,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation","keywords":"Seismology; Seismic hazard; Geology; Earthquake scenario; Hazard; Earthquake rupture; Active fault; Fault (geology)","score_opus":0.1498747467155254,"score_gpt":0.2937427422020963,"score_spread":0.1438679954865709,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3090044403","genre_codex":"commentary","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.074667774,0.32009214,0.1673651,0.4022414,0.0034220428,0.0004241271,0.013662138,0.0025842304,0.015541052],"genre_scores_gemma":[0.30626354,0.19193906,0.45459184,0.015904572,0.012364413,0.0011267215,0.0122855315,0.00071878516,0.0048055253],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9901086,0.0046489257,0.00087915093,0.0011941392,0.0028228976,0.00034615272],"domain_scores_gemma":[0.85510457,0.102794565,0.006210104,0.0070097996,0.025348969,0.0035321396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.034515746,0.0014554628,0.0025327504,0.007224975,0.0012510659,0.0077019744,0.007944786,0.00763493,0.0043552285],"category_scores_gemma":[0.07063435,0.0018409297,0.001756345,0.009175533,0.0048658033,0.018984975,0.005629699,0.005821649,0.0028460908],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021131035,0.0007438837,0.07840931,0.0060738465,0.00059743505,0.00034304505,0.001762399,0.03874031,0.0029382042,0.06563863,0.089797266,0.71474445],"study_design_scores_gemma":[0.00008312968,0.00029197283,0.069022134,0.0064642653,0.00023293048,0.0009726494,0.011132656,0.24108951,0.0020078025,0.4116066,0.2563465,0.00074982253],"about_ca_topic_score_codex":0.019119687,"about_ca_topic_score_gemma":0.01887136,"teacher_disagreement_score":0.034515746,"about_ca_system_score_codex":0.0024743055,"about_ca_system_score_gemma":0.005361671,"threshold_uncertainty_score":0.18253893},"labels":[],"label_agreement":null},{"id":"W3090605187","doi":"10.5194/egusphere-egu2020-1999","title":"Coordinated efforts in tsunami hazard and risk analyses in Europe and link to the Global Tsunami Model network initiative","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Preparedness; Vulnerability (computing); Hazard; Disaster risk reduction; Natural hazard; Emergency management; Environmental planning; Risk assessment; Population; Risk analysis (engineering); Geography; Environmental resource management; Environmental science; Computer science; Business; Meteorology; Computer security; Economic growth; Political science; Environmental health","score_opus":0.04713951875264473,"score_gpt":0.26831846361711575,"score_spread":0.22117894486447104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3090605187","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0866707,0.049403567,0.46806413,0.2119494,0.009800023,0.0010692724,0.011956524,0.0062793368,0.15480712],"genre_scores_gemma":[0.39279577,0.033965383,0.49699348,0.018558213,0.0019742677,0.00086718233,0.023943495,0.0027256869,0.028176444],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99039286,0.005800797,0.00068603834,0.00068018533,0.0017645719,0.0006755144],"domain_scores_gemma":[0.9766301,0.0051848446,0.0017234943,0.0034745224,0.009519483,0.0034675805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.043807622,0.001347014,0.0009845884,0.0042882734,0.0010564126,0.004853595,0.0027118088,0.002534082,0.004892523],"category_scores_gemma":[0.026258435,0.00041922147,0.0016713502,0.0046015084,0.0013910335,0.0055633336,0.0089138765,0.0026762623,0.0015431929],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003294403,0.00046151044,0.040932722,0.0011885593,0.00071327336,0.000737881,0.0026564957,0.06814959,0.0025474913,0.109060615,0.20769158,0.56553084],"study_design_scores_gemma":[0.00007871378,0.00020387053,0.030884828,0.0032556427,0.00021426704,0.00038920934,0.0035143674,0.044180054,0.0025740087,0.09281146,0.8217273,0.00016631543],"about_ca_topic_score_codex":0.01774676,"about_ca_topic_score_gemma":0.011990115,"teacher_disagreement_score":0.043807622,"about_ca_system_score_codex":0.0033046862,"about_ca_system_score_gemma":0.015722757,"threshold_uncertainty_score":0.23167962},"labels":[],"label_agreement":null},{"id":"W3091100633","doi":"10.5194/se-12-959-2021","title":"Nanoscale earthquake records preserved in plagioclase microfractures from the lower continental crust","year":2021,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"European Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Plagioclase; Geology; Feldspar; Geochemistry; Wall rock; Crust; Continental crust; Petrology; Mineralogy; Quartz","score_opus":0.015494440336938505,"score_gpt":0.22470223921307864,"score_spread":0.20920779887614013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3091100633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990646,0.00011465773,0.000093051756,0.0000070044925,0.0000016903138,0.0000031410268,0.0002861755,0.000008654047,0.0004210065],"genre_scores_gemma":[0.9990853,0.000057461228,0.00016105396,0.000004398734,0.0000018028726,0.0000030704741,0.00040987297,0.0000029762357,0.00027405063],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999547,0.0000016011749,0.0000036269853,0.000016487224,0.000012289279,0.000011352801],"domain_scores_gemma":[0.999894,0.000005915015,0.000038966497,0.000008870263,0.000036226986,0.000015968106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058728987,0.00012825413,0.00010757245,0.00061037735,0.00024910137,0.0002529209,0.00013316238,0.00016068948,0.00071600924],"category_scores_gemma":[0.00013678282,0.00010185366,0.00011159454,0.00034778766,0.00018431385,0.00011082539,0.0001935528,0.00009987105,0.00016670188],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013134777,0.000016231299,0.33738774,0.00008827705,0.000041659856,0.0005041061,0.0009396061,0.00021789764,0.653108,0.00007372511,0.0001455813,0.007345849],"study_design_scores_gemma":[7.6405735e-7,0.000015160956,0.9969001,0.0000017721851,0.0000054221105,0.00009448274,0.00010554364,0.000060783364,0.002519642,0.0000049551936,0.0002905337,8.954314e-7],"about_ca_topic_score_codex":0.013261365,"about_ca_topic_score_gemma":0.034857336,"teacher_disagreement_score":0.013261365,"about_ca_system_score_codex":0.00037774845,"about_ca_system_score_gemma":0.00012267282,"threshold_uncertainty_score":0.02636838},"labels":[],"label_agreement":null},{"id":"W3091631347","doi":"10.1190/segam2020-3419416.1","title":"The influence of competing regional stress regimes on the generation of hydraulic fracturing-induced microseismicity","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Hydraulic fracturing; Stress (linguistics); Geology; Petroleum engineering; Geotechnical engineering","score_opus":0.04995950793254027,"score_gpt":0.2277042303332493,"score_spread":0.17774472240070904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3091631347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986706,0.00002781551,0.0001250911,0.000017761464,0.0000016849115,0.0000056287313,0.000061391016,0.0000091837055,0.001080986],"genre_scores_gemma":[0.9997789,0.00001538068,0.000034702374,0.0000030527706,0.0000010430234,0.0000018822001,0.000045172503,0.0000024658798,0.00011740557],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998828,0.000017784581,0.000005968889,0.00002563817,0.000019156085,0.000048607384],"domain_scores_gemma":[0.9996555,0.00008636078,0.000068836205,0.000018340652,0.0000724115,0.000098485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019615609,0.00017402302,0.00023242984,0.00038821762,0.0002242555,0.0005662183,0.00021642703,0.00020856965,0.0013536793],"category_scores_gemma":[0.0010750403,0.00014829873,0.00015429422,0.00024187649,0.00028727966,0.00015572377,0.00038789946,0.0001641958,0.00026188826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013165327,0.00019228998,0.7513493,0.000114195296,0.00015235417,0.00081662816,0.0006490883,0.018477468,0.20130718,0.0006490103,0.00070189097,0.024274154],"study_design_scores_gemma":[0.000009734348,0.00008791253,0.9917964,0.00000441627,0.000013675103,0.00004834412,0.00025488235,0.0059036654,0.0016621297,0.00008314497,0.00012683378,0.000008883059],"about_ca_topic_score_codex":0.013150324,"about_ca_topic_score_gemma":0.026727939,"teacher_disagreement_score":0.013150324,"about_ca_system_score_codex":0.0006516327,"about_ca_system_score_gemma":0.0003352044,"threshold_uncertainty_score":0.026147604},"labels":[],"label_agreement":null},{"id":"W3091835895","doi":"10.1029/2020gl091188","title":"Constraining Fault Friction and Stability With Fluid‐Injection Field Experiments","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche; National Science Foundation","keywords":"Cabin pressurization; Slip (aerodynamics); Geology; Residual; Observable; Fault (geology); Mechanics; Geotechnical engineering; Seismology; Materials science; Computer science; Physics; Thermodynamics","score_opus":0.055627735141188746,"score_gpt":0.3023509885213441,"score_spread":0.24672325338015538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3091835895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99563414,0.000059870214,0.0037702008,0.000027802062,0.000004881599,0.000009258313,0.00005899105,0.000041370942,0.00039360626],"genre_scores_gemma":[0.9994299,0.000020081872,0.00048931723,0.000002503842,0.0000011545777,0.0000043025843,0.000012934192,0.0000023417342,0.000037457317],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993503,0.000014837326,0.0000064302412,0.0000170859,0.000010823164,0.000015767853],"domain_scores_gemma":[0.9994766,0.0002622263,0.00013731312,0.000058853595,0.00003293579,0.000032146494],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021796506,0.00029916334,0.00031447544,0.0003179495,0.0001473119,0.00035799594,0.0004598051,0.0003553683,0.00087933143],"category_scores_gemma":[0.0009417457,0.00014775193,0.00022707843,0.00016080534,0.0005289183,0.0004273305,0.00028209348,0.000319647,0.000039567134],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005181653,0.0005992564,0.02666768,0.00019116321,0.0000971578,0.0002719279,0.00015837004,0.71468675,0.24292724,0.004825759,0.0002653254,0.008791211],"study_design_scores_gemma":[0.00006222687,0.0004751917,0.0051944307,0.000007733937,0.000028130597,0.000029056628,0.00003478638,0.94567496,0.047293473,0.000898385,0.00027779717,0.000023778512],"about_ca_topic_score_codex":0.0016901111,"about_ca_topic_score_gemma":0.0012190099,"teacher_disagreement_score":0.0016901111,"about_ca_system_score_codex":0.00043185975,"about_ca_system_score_gemma":0.00017259114,"threshold_uncertainty_score":0.0033605099},"labels":[],"label_agreement":null},{"id":"W3092131037","doi":"10.1016/j.jog.2020.101784","title":"Fault inversion in central Iran: Evidence of post Pliocene intracontinental left lateral kinematics at the northern Iranian Plateau margin","year":2020,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Tarbiat Modares University","keywords":"Sinistral and dextral; Geology; Kinematics; Transpression; Clockwise; Seismology; Inversion (geology); Fault (geology); Paleontology; Geodesy; Tectonics; Rotation (mathematics); Geometry","score_opus":0.0170394595511127,"score_gpt":0.2152623822946104,"score_spread":0.1982229227434977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092131037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99873453,0.00010310401,0.000045183882,0.000054301174,0.0000034927834,0.0000021759654,0.00005244247,0.000003710426,0.0010010931],"genre_scores_gemma":[0.99964654,0.000060916886,0.00005215723,0.000008745398,0.0000043685786,0.0000018505737,0.00009303797,0.0000011104632,0.00013128153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990714,0.000008446106,0.0000071519676,0.000022945957,0.000015993812,0.000038361562],"domain_scores_gemma":[0.9997267,0.00003146847,0.00009969312,0.00001886556,0.00009739813,0.000025777925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021994436,0.00017541207,0.00013850506,0.0010477713,0.0005741926,0.0004472451,0.00039502952,0.00025130273,0.0015994787],"category_scores_gemma":[0.00067151815,0.00012828007,0.000139833,0.0015248045,0.0006414213,0.000425582,0.00047092699,0.00021885928,0.00018999075],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001859753,0.000044255776,0.96561253,0.00004778742,0.000038975435,0.00084857235,0.0044224835,0.0003348044,0.0068349056,0.00045538082,0.0003063382,0.020868085],"study_design_scores_gemma":[0.0000034963273,0.000010771871,0.9983911,0.0000057140487,0.0000062060853,0.000070880276,0.0009165364,0.00009593532,0.000086128006,0.000034939756,0.00037666573,0.000001599371],"about_ca_topic_score_codex":0.07417069,"about_ca_topic_score_gemma":0.09784288,"teacher_disagreement_score":0.07417069,"about_ca_system_score_codex":0.0006545419,"about_ca_system_score_gemma":0.0011420023,"threshold_uncertainty_score":0.14747792},"labels":[],"label_agreement":null},{"id":"W3092921863","doi":"10.5194/egusphere-egu2020-6334","title":"Seismic hazard due to fluid injections","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; AXA Research Fund","keywords":"Superposition principle; Homogeneous; Pore water pressure; Geology; Fluid pressure; Hazard; Seismic hazard; Seismology; Geotechnical engineering; Mechanics; Physics; Biology; Ecology; Thermodynamics","score_opus":0.025072807802759407,"score_gpt":0.2175063266705052,"score_spread":0.1924335188677458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092921863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99747866,0.000060904018,0.0014623073,0.000036176265,0.000004966139,0.000008788066,0.00005648581,0.000031573516,0.00086009386],"genre_scores_gemma":[0.99983954,0.000026141037,0.00007128425,0.00000442234,0.000004986545,0.0000014141107,0.000022745799,0.0000011863629,0.000028199369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997273,0.0000743623,0.000019174617,0.000043971275,0.000087790264,0.000047292808],"domain_scores_gemma":[0.9979633,0.0008507298,0.0008182161,0.00010748126,0.00012936791,0.00013094205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041754855,0.00021155833,0.0002252041,0.0009925294,0.00013689241,0.00038480936,0.0001892058,0.0003886353,0.0006202807],"category_scores_gemma":[0.0033702257,0.00010455255,0.0001720934,0.00048151272,0.00048661686,0.000379121,0.00069317233,0.00029874608,0.00007549942],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002782651,0.0003030544,0.74549186,0.00023129291,0.00023547694,0.00406748,0.0011159786,0.089938864,0.08060596,0.0055202288,0.00094386714,0.06876325],"study_design_scores_gemma":[0.000055470675,0.0010672709,0.8396026,0.00003781051,0.00010266227,0.0014403829,0.0006674048,0.13302329,0.018193522,0.0048189997,0.00092856004,0.00006217168],"about_ca_topic_score_codex":0.0009271111,"about_ca_topic_score_gemma":0.0005525503,"teacher_disagreement_score":0.0009925294,"about_ca_system_score_codex":0.0004331079,"about_ca_system_score_gemma":0.00013545684,"threshold_uncertainty_score":0.0031424165},"labels":[],"label_agreement":null},{"id":"W3093010404","doi":"10.1029/2020gl089366","title":"Correlation Between Poroelastic Stress Perturbation and Multidisposal Wells Induced Earthquake Sequence in Cushing, Oklahoma","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Natural Science Foundation of China","keywords":"Poromechanics; Geology; Seismology; Pore water pressure; Seismic hazard; Shear (geology); Perturbation (astronomy); Fault (geology); Induced seismicity; Shear stress; Geotechnical engineering; Petrology; Mechanics","score_opus":0.07250017230694451,"score_gpt":0.29727713367385067,"score_spread":0.22477696136690617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093010404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994135,0.00001332185,0.000026253716,0.000025961292,0.000001464369,0.0000037785828,0.0002587151,0.0000036624156,0.00025341994],"genre_scores_gemma":[0.999526,0.0000146090215,0.000048079815,0.000010473586,0.0000016062331,0.00000636661,0.00023178957,7.0452427e-7,0.00016038989],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983907,0.000018705574,0.000016984806,0.000040780662,0.000030731702,0.00005368017],"domain_scores_gemma":[0.99914014,0.00013946216,0.00033220823,0.00004971212,0.0001538296,0.00018463284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001324152,0.00016109264,0.00013782774,0.0007800251,0.0007692611,0.0004196933,0.0002721471,0.00037125463,0.0016182769],"category_scores_gemma":[0.00068757136,0.00013359111,0.00008926111,0.000881588,0.000341898,0.00022512038,0.0004642909,0.0002773585,0.00014031678],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061963874,0.00003731869,0.99368393,0.000013736924,0.000032282034,0.0002147063,0.00033060054,0.00057423854,0.0016492023,0.000031461623,0.0002874834,0.003083044],"study_design_scores_gemma":[0.0000019047206,0.00001538053,0.9984285,0.0000044147096,0.0000051146903,0.000021595903,0.0008149086,0.00036354022,0.000119856195,0.0000058246333,0.00021541795,0.0000034242753],"about_ca_topic_score_codex":0.34015056,"about_ca_topic_score_gemma":0.6155665,"teacher_disagreement_score":0.34015056,"about_ca_system_score_codex":0.002095119,"about_ca_system_score_gemma":0.0013159404,"threshold_uncertainty_score":0.6763413},"labels":[],"label_agreement":null},{"id":"W3093319193","doi":"10.1029/2020tc006061","title":"Oblique Right‐Lateral Faulting Along the Northern Margin of the Ili Basin in the Northern Tian Shan, Northwest China","year":2020,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Natural Science Foundation of China","keywords":"Geology; Sinistral and dextral; Seismology; Active fault; Clockwise; Quaternary; Fault (geology); Tectonics; Structural basin; Fault scarp; Slip (aerodynamics); Strike-slip tectonics; Geomorphology; Paleontology; Geometry; Rotation (mathematics)","score_opus":0.013409353263792688,"score_gpt":0.20268551019264358,"score_spread":0.18927615692885089,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093319193","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943846,0.00006223557,0.00008497749,0.0000150018495,9.349048e-7,0.0000029018247,0.00007595969,0.0000063872694,0.00031307194],"genre_scores_gemma":[0.9996012,0.00003641048,0.000092386275,0.000005103201,0.0000012548006,0.000002497064,0.0001265424,8.241586e-7,0.0001338581],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999908,0.00000986578,0.000012294637,0.0000271119,0.000022559836,0.000020259857],"domain_scores_gemma":[0.9997812,0.000019822612,0.000086272856,0.000015333586,0.00005519504,0.00004217446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022697085,0.00022180857,0.00019341943,0.0011364174,0.00034867108,0.00035199034,0.00025413797,0.00018586105,0.00054213614],"category_scores_gemma":[0.00024837806,0.00015612386,0.0001500131,0.0010656432,0.00038323153,0.0001935303,0.00032053227,0.0000842052,0.00006137637],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000079011916,0.000031248284,0.9615215,0.00010322181,0.00006040516,0.00038688106,0.0009856349,0.0016755282,0.018308204,0.00018422367,0.00016384348,0.01650026],"study_design_scores_gemma":[0.0000024132319,0.000011779018,0.99831724,0.000007874179,0.00001096956,0.0000376898,0.00019951047,0.0010330217,0.00021019777,0.000012650993,0.00015355565,0.0000031468533],"about_ca_topic_score_codex":0.07166838,"about_ca_topic_score_gemma":0.12802325,"teacher_disagreement_score":0.07166838,"about_ca_system_score_codex":0.0005796418,"about_ca_system_score_gemma":0.00091127,"threshold_uncertainty_score":0.14250249},"labels":[],"label_agreement":null},{"id":"W3093807320","doi":"10.1029/2020jb020059","title":"Earthquake Rupture Through a Step‐Over Fault System: An Exploratory Numerical Study of the Leech River Fault, Southern Vancouver Island","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Fault (geology); Offset (computer science); Shear stress; Jump; Slip (aerodynamics); Shear (geology); Engineering; Mechanics; Computer science; Petrology","score_opus":0.04836871349214682,"score_gpt":0.3019546011187073,"score_spread":0.2535858876265605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093807320","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866354,0.000028972794,0.00015599532,0.00005248372,0.0000023484024,0.000008188254,0.000114429415,0.000012037835,0.0009618942],"genre_scores_gemma":[0.99906355,0.00002500604,0.0003343915,0.000014499339,0.0000019234267,0.000007613948,0.00012919497,0.0000045726824,0.00041934446],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998956,0.000019668258,0.0000056943554,0.00002086557,0.00001796578,0.000040129635],"domain_scores_gemma":[0.9994987,0.00021054833,0.00005504778,0.000029053215,0.000074441654,0.00013216551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019569148,0.00045538013,0.0004969432,0.0005805254,0.0010546036,0.0010126516,0.0011746471,0.0015365346,0.0016979463],"category_scores_gemma":[0.001013263,0.00040221695,0.00050421746,0.0007147272,0.00077957293,0.00035266398,0.00061174715,0.00067968934,0.0001221075],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034069127,0.0005475507,0.10256642,0.00007703115,0.00017433132,0.0015882548,0.00024526907,0.88519716,0.0039427355,0.0010104756,0.00084965175,0.0034604284],"study_design_scores_gemma":[0.00010953091,0.00013563782,0.027422678,0.000013823568,0.00003930948,0.00006787633,0.000551122,0.9707134,0.00043681468,0.00021409882,0.00026985942,0.000025865385],"about_ca_topic_score_codex":0.3133056,"about_ca_topic_score_gemma":0.29515862,"teacher_disagreement_score":0.6866944,"about_ca_system_score_codex":0.0018760016,"about_ca_system_score_gemma":0.0016745795,"threshold_uncertainty_score":0.6229639},"labels":[],"label_agreement":null},{"id":"W3093808080","doi":"10.1002/essoar.10503605.1","title":"Detailed nucleation process and mechanism of the July 2019 Mw 6.4 Ridgecrest, California earthquake","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Preprint; Beijing; Space Science; World Wide Web; Library science; Computer science; Physics; History; China; Archaeology; Astronomy","score_opus":0.01349402063948638,"score_gpt":0.19930362614433433,"score_spread":0.18580960550484796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093808080","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99703157,0.00015535367,0.00043931595,0.000031735533,0.0000058690057,0.000018406485,0.00056804286,0.00005296795,0.0016967905],"genre_scores_gemma":[0.9984327,0.000106190084,0.00032658322,0.000005618328,0.0000053697345,0.000013203683,0.0006470873,0.0000038459443,0.0004592842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999567,0.0000019994466,0.0000024036212,0.0000132184405,0.000011308725,0.000014365664],"domain_scores_gemma":[0.99989986,0.000009368876,0.00004450564,0.000006898018,0.000016652728,0.000022669426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010246671,0.00018791725,0.00020696483,0.0007302218,0.00038995297,0.00029802692,0.00027357164,0.0002569856,0.0011190482],"category_scores_gemma":[0.00023130346,0.00024319738,0.00019179433,0.00031338062,0.00016527444,0.00022664043,0.00024356935,0.00023896078,0.0001911433],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059529283,0.00024570155,0.82610255,0.00015352899,0.00012412459,0.001213978,0.0004679626,0.028365895,0.11701917,0.0016634809,0.0029786322,0.021069705],"study_design_scores_gemma":[0.000018557324,0.00008111639,0.97853273,0.000010691807,0.000025302403,0.000081287224,0.000083454266,0.016204815,0.003978253,0.000107934415,0.00085901096,0.0000169397],"about_ca_topic_score_codex":0.037482083,"about_ca_topic_score_gemma":0.047266435,"teacher_disagreement_score":0.037482083,"about_ca_system_score_codex":0.0007362931,"about_ca_system_score_gemma":0.0003776703,"threshold_uncertainty_score":0.0745278},"labels":[],"label_agreement":null},{"id":"W3094093430","doi":"10.1016/j.ijrmms.2020.104505","title":"An international model comparison study of controlled fault activation experiments in argillaceous claystone at the Mont Terri Laboratory","year":2020,"lang":"en","type":"article","venue":"International Journal of Rock Mechanics and Mining Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Nuclear Safety Commission","funders":"Lawrence Berkeley National Laboratory; Canadian Nuclear Safety Commission; Eidgenössisches Nuklearsicherheitsinspektorat; Institut de Radioprotection et de SÛreté Nucléaire; Korea Atomic Energy Research Institute; Japan Atomic Energy Agency; Office of Nuclear Energy; Nuclear Waste Management Organization; U.S. Department of Energy","keywords":"Borehole; Geology; Fault (geology); Classification of discontinuities; Discontinuity (linguistics); Fracture (geology); Shear (geology); Geotechnical engineering; Pore water pressure; Flow (mathematics); Hydraulic fracturing; Petrology; Seismology; Mechanics","score_opus":0.04308689046521139,"score_gpt":0.30808649997336646,"score_spread":0.26499960950815504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094093430","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99483585,0.000042410913,0.0019003483,0.00005992756,0.00000766047,0.000043098058,0.00056085084,0.00012228847,0.0024276623],"genre_scores_gemma":[0.9976927,0.000030284975,0.0013086611,0.000011200506,0.0000028574295,0.000054711185,0.0005331755,0.000020292484,0.0003462126],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997348,0.00007129936,0.00001739387,0.0000751946,0.000041372514,0.000059972375],"domain_scores_gemma":[0.9992367,0.00039480507,0.00008521919,0.0000952304,0.0001292954,0.00005890432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066745793,0.000955198,0.00074694137,0.00049150136,0.0005162937,0.000715794,0.0013704606,0.0011307957,0.0014626245],"category_scores_gemma":[0.0008914983,0.0002415253,0.00081370265,0.00053991383,0.0005395691,0.0006125727,0.0004920339,0.00071240193,0.00016782085],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049647666,0.0005816267,0.012266092,0.0000837572,0.000059495076,0.00020982049,0.00008258852,0.9720076,0.009646474,0.0005476643,0.00043318624,0.0035852261],"study_design_scores_gemma":[0.00026105883,0.000863544,0.010970132,0.000007618093,0.00005293489,0.00003467194,0.00013392803,0.9768976,0.009835125,0.00028242404,0.00061674725,0.00004415736],"about_ca_topic_score_codex":0.03086094,"about_ca_topic_score_gemma":0.024164472,"teacher_disagreement_score":0.03086094,"about_ca_system_score_codex":0.0016153927,"about_ca_system_score_gemma":0.0007134315,"threshold_uncertainty_score":0.061362624},"labels":[],"label_agreement":null},{"id":"W3094110234","doi":"10.1029/2020gl089342","title":"Using a Large‐<i>n</i> Seismic Array to Explore the Robustness of Spectral Estimations","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Deutsche Forschungsgemeinschaft","keywords":"Seismic moment; Geology; Seismology; Scaling; Spectral line; Physics; Mathematics; Geometry","score_opus":0.15385392303192055,"score_gpt":0.3362844622801319,"score_spread":0.18243053924821137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094110234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88950276,0.000113870265,0.10764664,0.00015607862,0.00003315534,0.000025199399,0.0004055025,0.00023546006,0.0018812998],"genre_scores_gemma":[0.9798543,0.000026602156,0.01966622,0.000029324614,0.000010031284,0.000011748356,0.00021560748,0.000018740584,0.0001674156],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99914277,0.00036056695,0.000052252937,0.0002695818,0.00012239556,0.000052323398],"domain_scores_gemma":[0.9928155,0.004661549,0.00062391325,0.0012809256,0.0005467452,0.00007125561],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017573576,0.00023185082,0.00020210304,0.0003748971,0.00024141156,0.0005025999,0.00030708627,0.00034012768,0.00062657415],"category_scores_gemma":[0.01049628,0.00016049041,0.00019791491,0.0004277799,0.00024894637,0.00049429195,0.0003962315,0.0002445469,0.00015029516],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001249666,0.00019440847,0.40965286,0.0001813758,0.0007700893,0.00029257877,0.000507996,0.26089978,0.14578235,0.0028185626,0.001138383,0.17651203],"study_design_scores_gemma":[0.00006976249,0.0005064376,0.335708,0.000046390895,0.0002177513,0.000421422,0.00034673628,0.6052483,0.052680697,0.0018378174,0.0028206927,0.00009599198],"about_ca_topic_score_codex":0.0051661674,"about_ca_topic_score_gemma":0.00574587,"teacher_disagreement_score":0.0051661674,"about_ca_system_score_codex":0.0002269715,"about_ca_system_score_gemma":0.00021535272,"threshold_uncertainty_score":0.010272205},"labels":[],"label_agreement":null},{"id":"W3094253074","doi":"10.5194/egusphere-egu2020-4174","title":"A unified numerical model for the simulation of the seismic cycle for normal and reverse fault earthquakes in Italy","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Crust; Slip (aerodynamics); Geodesy; Geophysics","score_opus":0.033673654128144756,"score_gpt":0.2399676323300905,"score_spread":0.20629397820194573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094253074","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.17086802,0.0014366242,0.7533051,0.0012589865,0.00044499856,0.00044463202,0.0028330656,0.002031263,0.06737736],"genre_scores_gemma":[0.86495227,0.0008185786,0.11249214,0.00020200312,0.00012207741,0.0010128871,0.0016348504,0.000259098,0.018506167],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99973875,0.000079257145,0.000023461393,0.000058119913,0.000056271077,0.000044164644],"domain_scores_gemma":[0.99965405,0.00012650037,0.00005849454,0.000029976776,0.00009597308,0.000035068268],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043457517,0.0008888999,0.00085677294,0.000722247,0.00067066395,0.001450102,0.0019754348,0.0020257882,0.005304916],"category_scores_gemma":[0.0014993951,0.00054727634,0.0010766115,0.00070157374,0.0008182041,0.00060054584,0.0010447179,0.0008980228,0.0009771711],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001490175,0.000011539298,0.0004229785,0.000014577971,0.000008034966,0.00004328436,0.000022381611,0.9943084,0.00031183826,0.0030804349,0.00026436814,0.0014973091],"study_design_scores_gemma":[0.00000791481,0.0000056646163,0.00008980968,0.0000033214042,0.0000034164013,0.0000064098354,0.0000035534983,0.9987495,0.0000477642,0.0004639279,0.0006154929,0.0000031995196],"about_ca_topic_score_codex":0.025135655,"about_ca_topic_score_gemma":0.012366504,"teacher_disagreement_score":0.025135655,"about_ca_system_score_codex":0.0014590806,"about_ca_system_score_gemma":0.0013539413,"threshold_uncertainty_score":0.049978733},"labels":[],"label_agreement":null},{"id":"W3094378591","doi":"10.1007/s00024-020-02600-2","title":"Elastic Character of Seismic Coda Envelopes Within East Indian Shield","year":2020,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Coda; Attenuation; Geology; Seismology; Tectonics; Shield; Scattering; Geophysics; Physics; Optics","score_opus":0.013276297088417563,"score_gpt":0.17773461591420717,"score_spread":0.1644583188257896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094378591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963517,0.000032433352,0.00028123858,0.00004014249,0.0000035491514,0.0000024308038,0.00014122263,0.000015579139,0.0031315675],"genre_scores_gemma":[0.999474,0.000015023858,0.000036184494,0.000003342849,0.0000018031785,8.064344e-7,0.000103657614,0.000005162029,0.00036000364],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990726,0.0000071008203,0.0000062956715,0.000019982926,0.000023253888,0.00003604653],"domain_scores_gemma":[0.9995665,0.0000974772,0.00009536027,0.00005342349,0.0001150067,0.000072224095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012483523,0.00021872995,0.00021220722,0.0013601688,0.0007300485,0.0011981837,0.00030349262,0.00032965202,0.002172705],"category_scores_gemma":[0.0008814297,0.0003138342,0.00018466038,0.0010654138,0.00058312644,0.0004385518,0.00070049544,0.00038569022,0.00040458213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001074822,0.00021916094,0.79913056,0.00009422974,0.00016074636,0.004118238,0.0026340592,0.04534127,0.10601858,0.007163243,0.001141356,0.032903742],"study_design_scores_gemma":[0.0000033176304,0.000018541496,0.9805048,0.000008481834,0.000012787404,0.00027543472,0.000991159,0.016336422,0.000989879,0.00028331878,0.0005571288,0.000018700235],"about_ca_topic_score_codex":0.014128582,"about_ca_topic_score_gemma":0.013076674,"teacher_disagreement_score":0.014128582,"about_ca_system_score_codex":0.0003991697,"about_ca_system_score_gemma":0.0002847337,"threshold_uncertainty_score":0.028092742},"labels":[],"label_agreement":null},{"id":"W3094457323","doi":"10.1029/2020jb020503","title":"Slow Slip and Inter‐transient Locking on the Nicoya Megathrust in the Late and Early Stages of an Earthquake Cycle","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"National Science Foundation","keywords":"Seismology; Slip (aerodynamics); Geology; Subduction; Episodic tremor and slip; Geodesy; Global Positioning System; Slow earthquake; Interplate earthquake; Tectonics; Physics","score_opus":0.05221594364126781,"score_gpt":0.30304174710697895,"score_spread":0.25082580346571115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094457323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993205,0.000073971954,0.00007245188,0.000010939016,0.0000011633327,0.0000025961237,0.00019078283,0.0000035248775,0.00032405998],"genre_scores_gemma":[0.9995277,0.00003199075,0.000042808395,0.0000029042767,0.0000019937781,0.0000031187833,0.00027525582,0.0000010851662,0.00011317319],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998932,0.000021672926,0.000013287835,0.000026334865,0.000020758778,0.000024806317],"domain_scores_gemma":[0.9995018,0.00007120067,0.0002152035,0.000048610324,0.000107559434,0.000055587472],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021560481,0.00016095446,0.00015710187,0.0009965189,0.00018009634,0.00043129156,0.0001746279,0.0001480615,0.00060062396],"category_scores_gemma":[0.0011645989,0.00007621178,0.00013732308,0.0006946017,0.00022352673,0.0001990358,0.00035103076,0.00010234942,0.000096334916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009109428,0.000017374312,0.9904294,0.000016084172,0.00004381114,0.00011836139,0.00022384191,0.0009163223,0.0024381557,0.00008099366,0.00012095547,0.005503639],"study_design_scores_gemma":[6.822126e-7,0.000007636955,0.99855644,0.0000031497275,0.000005427469,0.000017534743,0.00009686335,0.0010644239,0.000085582105,0.000010763159,0.00014990963,0.0000016443826],"about_ca_topic_score_codex":0.04067013,"about_ca_topic_score_gemma":0.07479924,"teacher_disagreement_score":0.04067013,"about_ca_system_score_codex":0.0004711937,"about_ca_system_score_gemma":0.00020914078,"threshold_uncertainty_score":0.08086681},"labels":[],"label_agreement":null},{"id":"W3094841974","doi":"10.1029/2020gl090482","title":"Role of Serpentinized Mantle Wedge in Affecting Megathrust Seismogenic Behavior in the Area of the 2010 <i>M</i> = 8.8 Maule Earthquake","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Aftershock; Seismology; Subduction; Intraplate earthquake; Mantle wedge; Wedge (geometry); Mantle (geology); Crust; Slip (aerodynamics); Seismic velocity; Geophysics; Tectonics","score_opus":0.04453511853104641,"score_gpt":0.27152782332204345,"score_spread":0.22699270479099704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094841974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953675,0.000042131072,0.00003284358,0.000018939716,5.2494e-7,0.0000013358055,0.00003288153,0.0000033813496,0.00033124464],"genre_scores_gemma":[0.99989235,0.000015800642,0.000012903749,0.0000029172695,5.507292e-7,4.4184696e-7,0.000013124326,7.9851884e-7,0.000061137565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999603,0.0000068650556,0.0000032697278,0.000010916528,0.0000042531487,0.000014352215],"domain_scores_gemma":[0.99978334,0.00002864301,0.00009762712,0.000012794952,0.000024436102,0.000053201788],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011005587,0.00015912433,0.00017497758,0.00038296837,0.00017742712,0.0004377901,0.00019511709,0.00021160573,0.0013697552],"category_scores_gemma":[0.0004455254,0.00012986355,0.00010840127,0.00019822577,0.00030314387,0.00022796917,0.00028515395,0.00013001545,0.00015886677],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038364355,0.00007661215,0.8920947,0.00006672176,0.00006231875,0.00086451776,0.000407974,0.0023711713,0.09585463,0.00029509235,0.000096172196,0.007426504],"study_design_scores_gemma":[0.0000029470204,0.000027403457,0.9977762,0.0000028816148,0.000007563491,0.00006298142,0.00020256914,0.0008523739,0.00091051246,0.00004588349,0.000105711784,0.000002998066],"about_ca_topic_score_codex":0.0066734464,"about_ca_topic_score_gemma":0.008053877,"teacher_disagreement_score":0.0066734464,"about_ca_system_score_codex":0.00032366722,"about_ca_system_score_gemma":0.00018225274,"threshold_uncertainty_score":0.013269246},"labels":[],"label_agreement":null},{"id":"W3094904988","doi":"10.5194/egusphere-egu2020-4544","title":"Hydraulic fracturing induced hybrid earthquakes in the Montney Basin, British Columbia, Canada may mark the transition from aseismic slip near the wellbore to seismic slip at greater distances","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; McGill University; Natural Resources Canada","funders":"","keywords":"Induced seismicity; Seismology; Geology; Seismic hazard; Microseism; Hydraulic fracturing; Slip (aerodynamics); Structural basin; Geotechnical engineering; Engineering; Geomorphology","score_opus":0.012971291927946237,"score_gpt":0.17746882341879533,"score_spread":0.16449753149084909,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094904988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927699,0.00009485071,0.00020202345,0.000116523144,0.000007212823,0.000033734468,0.0014919748,0.0000423161,0.0052413493],"genre_scores_gemma":[0.9954234,0.0001122863,0.00032007438,0.0000346341,0.0000021874625,0.000012892714,0.0007725893,0.0000071121267,0.003314897],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984694,0.0000051002903,0.000004574291,0.000031947697,0.00004828538,0.00006321736],"domain_scores_gemma":[0.99973506,0.0000113043,0.000036230587,0.0000090195035,0.0001358829,0.00007255808],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000112255504,0.0003272759,0.00018805402,0.0010768581,0.0017510509,0.0009462788,0.00040728317,0.00025876492,0.0024905128],"category_scores_gemma":[0.00033309104,0.0001921619,0.00012775004,0.0019732972,0.0006652169,0.00024455623,0.00058520044,0.0003904034,0.00017595265],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026088074,0.00009629427,0.91134924,0.00010597938,0.00007590434,0.0012517524,0.004353195,0.0022473484,0.025501592,0.00065306295,0.0049816538,0.049123187],"study_design_scores_gemma":[0.000003127187,0.000010873647,0.9952983,0.000010865457,0.00000901108,0.000034027085,0.0019391249,0.00040749568,0.00048595373,0.000025004438,0.0017674002,0.000008920853],"about_ca_topic_score_codex":0.9816695,"about_ca_topic_score_gemma":0.99719644,"teacher_disagreement_score":0.018330514,"about_ca_system_score_codex":0.0101919295,"about_ca_system_score_gemma":0.010474818,"threshold_uncertainty_score":0.073947966},"labels":[],"label_agreement":null},{"id":"W3095159451","doi":"10.1029/2020gl090219","title":"Sequential Fault Reactivation and Secondary Triggering in the March 2019 Red Deer Induced Earthquake Swarm","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Alberta Energy; Geological Survey of Canada; University of Alberta","funders":"","keywords":"Seismology; Seismometer; Geology; Induced seismicity; Fault (geology); Slip (aerodynamics); Stress field; Hypocenter; Geophone; Microseism; Earthquake swarm; Swarm behaviour; Strike-slip tectonics","score_opus":0.06894953226310341,"score_gpt":0.2966689986295678,"score_spread":0.2277194663664644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3095159451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956316,0.000018414317,0.00004682606,0.000005944415,8.574333e-7,0.0000025594277,0.00006588424,0.0000032774747,0.00029313244],"genre_scores_gemma":[0.99965465,0.000010228956,0.000038052654,0.0000029573932,0.0000012540999,0.0000017646136,0.00011040722,4.2741866e-7,0.00018024041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999155,0.00000962954,0.0000045710503,0.00002321805,0.000020650461,0.000026540689],"domain_scores_gemma":[0.9997093,0.000030849216,0.0001030696,0.00001777224,0.00006673186,0.00007226211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011620432,0.0000921124,0.0001298633,0.0006065276,0.00020054205,0.00036071797,0.00015362639,0.00015266349,0.00085248216],"category_scores_gemma":[0.00038619188,0.00006892306,0.00007511142,0.0003496202,0.00022265739,0.00007911533,0.0002899952,0.00010371991,0.00013068404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028468636,0.000050184226,0.97571325,0.0000138651585,0.000029520135,0.0006719341,0.0005995667,0.00037433326,0.01460764,0.00007257096,0.00023914127,0.0073432713],"study_design_scores_gemma":[0.0000013933724,0.0000294918,0.99907374,0.0000016681003,0.0000038358166,0.00007435226,0.00021094829,0.00019913528,0.00027392674,0.000009854776,0.000120112214,0.0000014162748],"about_ca_topic_score_codex":0.041295268,"about_ca_topic_score_gemma":0.10507919,"teacher_disagreement_score":0.9587047,"about_ca_system_score_codex":0.0006242579,"about_ca_system_score_gemma":0.00035434242,"threshold_uncertainty_score":0.08210981},"labels":[],"label_agreement":null},{"id":"W3095211316","doi":"10.1130/abs/2020am-359063","title":"TECTONIC EVOLUTION OF THE CHORTIS COMPOSITE BLOCK, NORTH-WESTERN NICARAGUA","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Tectonics; Geology; Block (permutation group theory); Seismology; Paleontology; Geometry","score_opus":0.01935549675025879,"score_gpt":0.21433655824530684,"score_spread":0.19498106149504804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3095211316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9841576,0.0006855394,0.00011389142,0.00014586409,0.000009665788,0.000028563638,0.00086326065,0.000027164893,0.013968409],"genre_scores_gemma":[0.99466246,0.00051728066,0.00041784454,0.00002549155,0.000004303652,0.00005781543,0.0007688108,0.000014581592,0.0035314928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998603,0.000031873504,0.000010172161,0.000028194738,0.00002056115,0.000048918657],"domain_scores_gemma":[0.9996532,0.00004360298,0.00007201988,0.000032677563,0.00015715776,0.00004129779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002940931,0.00032097814,0.00027478798,0.0021137865,0.0008993727,0.00087220466,0.0004996234,0.00026556736,0.0023032178],"category_scores_gemma":[0.001140035,0.0002302012,0.00021112026,0.0027230706,0.00068532967,0.00029184658,0.0012691632,0.0001585293,0.00032654472],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010296775,0.000059606227,0.8940407,0.00050136447,0.0003583743,0.0026614878,0.017339347,0.007673451,0.014604836,0.0051593375,0.0038958264,0.05267596],"study_design_scores_gemma":[0.000012145427,0.000033277087,0.9854592,0.00007935031,0.000047846854,0.0002414217,0.004421059,0.0011569674,0.00041964548,0.00011156037,0.008003959,0.000013518201],"about_ca_topic_score_codex":0.5317309,"about_ca_topic_score_gemma":0.70981926,"teacher_disagreement_score":0.5317309,"about_ca_system_score_codex":0.0033923844,"about_ca_system_score_gemma":0.0018818392,"threshold_uncertainty_score":0.9420537},"labels":[],"label_agreement":null},{"id":"W3095539344","doi":"10.1785/0220200300","title":"Juan Antonio Madrid González (1943–2019)","year":2020,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Medicine; Geology","score_opus":0.11552844531163194,"score_gpt":0.31475929626047455,"score_spread":0.19923085094884263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3095539344","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00088127994,0.01635577,0.000395446,0.022907646,0.060563423,0.00017640345,0.0116399815,0.0011901944,0.8858898],"genre_scores_gemma":[0.0019543224,0.005319837,0.00018213528,0.0025577662,0.0036525691,0.00007456604,0.0030914932,0.00030611458,0.98286116],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995427,0.000034112116,0.00002510525,0.00010073744,0.00019885102,0.00009840019],"domain_scores_gemma":[0.99887365,0.00007187113,0.00007554777,0.000052893465,0.00048033067,0.0004457559],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005383855,0.00078266906,0.00061741215,0.0013981075,0.001500102,0.0031341207,0.00094449177,0.0019463634,0.6799115],"category_scores_gemma":[0.0023346494,0.000294115,0.0003925992,0.0014568848,0.0003759312,0.0018633523,0.0025331227,0.0017228606,0.5459216],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021244594,0.0000055800883,0.00013791208,0.0000595147,0.0000010546339,0.000051426465,0.0000120732275,0.000011222405,0.000037799302,0.00036359119,0.9786673,0.020631352],"study_design_scores_gemma":[0.0000026256457,0.0000032900734,0.00024698308,0.00006946111,6.7067236e-7,0.000031705073,0.000023473629,0.0000037369769,0.000014712835,0.000048861602,0.99955267,0.0000017990365],"about_ca_topic_score_codex":0.008900617,"about_ca_topic_score_gemma":0.018514393,"teacher_disagreement_score":0.6799115,"about_ca_system_score_codex":0.0013384937,"about_ca_system_score_gemma":0.001941705,"threshold_uncertainty_score":0.4565674},"labels":[],"label_agreement":null},{"id":"W3095668307","doi":"","title":"The earthquakes of the Western Quebec Seismic Zone and their Relationship with the Great Meteor Hot Spot Track","year":2018,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Meteor (satellite); Geology; Seismology; Hot spot (computer programming); Track (disk drive); Meteorology; Geography; Engineering","score_opus":0.020942772213889092,"score_gpt":0.21158219721612403,"score_spread":0.19063942500223494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3095668307","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98403835,0.00074921135,0.00008531244,0.0010763936,0.000025870786,0.000018483288,0.0029738415,0.000010397237,0.0110220825],"genre_scores_gemma":[0.9944906,0.00030960783,0.000052067753,0.00007091919,0.000012026811,0.0000066001626,0.0008889328,0.0000057384455,0.00416354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971837,0.000034764034,0.000010825267,0.00003547411,0.00007683666,0.00012371814],"domain_scores_gemma":[0.9974335,0.0003136075,0.00057836366,0.00007292521,0.0010617161,0.0005399154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035758902,0.00017302319,0.00018233097,0.0019191268,0.002023265,0.0014799449,0.0007029474,0.0005830628,0.006954888],"category_scores_gemma":[0.0030325095,0.00016813476,0.00016737194,0.0045663156,0.0007959529,0.00049622013,0.0006436534,0.000710058,0.00037281058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015397316,0.000049987004,0.982509,0.000018163737,0.00005447581,0.00017839254,0.0014671799,0.00056519103,0.0003476758,0.00075714843,0.0039234967,0.009975277],"study_design_scores_gemma":[0.0000028175775,0.000004839974,0.997818,0.0000071657714,0.000004453502,0.000013488782,0.00074956333,0.00016922796,0.000011155825,0.00001977403,0.0011958801,0.0000035343844],"about_ca_topic_score_codex":0.9903556,"about_ca_topic_score_gemma":0.99628747,"teacher_disagreement_score":0.0130645,"about_ca_system_score_codex":0.0130645,"about_ca_system_score_gemma":0.0104060555,"threshold_uncertainty_score":0.09479004},"labels":[],"label_agreement":null},{"id":"W3096071826","doi":"10.1130/abs/2020am-358209","title":"AFTERSHOCKS AND FAULT ASEISMIC DEFORMATION IN SOUTHERN-CENTRAL ALBERTA ASSOCIATED WITH A HYDRAULIC-FRACTURING INDUCED EARTHQUAKE","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Aftershock; Seismology; Geology; Hydraulic fracturing; Foreshock; Fault (geology); Geotechnical engineering","score_opus":0.01914598543963558,"score_gpt":0.20548867732412918,"score_spread":0.1863426918844936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3096071826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988612,0.000024497804,0.000018433386,0.000035178236,0.0000025079646,0.0000036164633,0.00027437825,0.0000018299436,0.0007784195],"genre_scores_gemma":[0.9984534,0.000053255808,0.00002563961,0.000015989883,0.0000034008435,0.000002328575,0.00044473415,9.436311e-7,0.0010002932],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999378,0.000005245422,0.000004325536,0.000007914062,0.000016093203,0.000028652079],"domain_scores_gemma":[0.9995704,0.00005908093,0.00008768938,0.000011218375,0.00014043307,0.00013108802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013940803,0.00016327933,0.00011120331,0.00070715597,0.0007081456,0.00048374716,0.0003557912,0.00039130752,0.0017551557],"category_scores_gemma":[0.0006442478,0.00011326331,0.00012364557,0.0011385477,0.00036177348,0.00016138169,0.00034839992,0.0003130017,0.0001305112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051290327,0.00012056723,0.9892814,0.000014742235,0.000039076876,0.0008986401,0.0009125252,0.0012169945,0.0017813041,0.00012694678,0.00062147866,0.004473368],"study_design_scores_gemma":[0.0000034361226,0.000013166906,0.9986777,0.0000032033136,0.0000049949062,0.00003953507,0.0007682514,0.00023836468,0.000052468793,0.000015599077,0.00018120087,0.0000020557002],"about_ca_topic_score_codex":0.86527044,"about_ca_topic_score_gemma":0.941054,"teacher_disagreement_score":0.13472956,"about_ca_system_score_codex":0.002940052,"about_ca_system_score_gemma":0.002864725,"threshold_uncertainty_score":0.27104598},"labels":[],"label_agreement":null},{"id":"W3096338541","doi":"10.1029/2019jb019065","title":"Localized Afterslip at Geometrical Complexities Revealed by InSAR After the 2016 Central Italy Seismic Sequence","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Institut national des sciences de l'Univers; Agence Nationale de la Recherche; Agence Nationale pour le Développement de la Recherche en Santé; European Space Agency; Université Grenoble Alpes","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Geodesy; Fault (geology); Sequence (biology); Slip (aerodynamics); Synthetic aperture radar; Remote sensing","score_opus":0.071051130915617,"score_gpt":0.309208079454846,"score_spread":0.23815694853922903,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3096338541","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99314183,0.00016371404,0.00096923485,0.00010028142,0.00003282319,0.000011435215,0.0017705677,0.00011973178,0.003690363],"genre_scores_gemma":[0.9973043,0.000079975696,0.00047942053,0.00001820127,0.00002361087,0.000007249776,0.0016887081,0.000021384987,0.0003770064],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983203,0.000015142553,0.0000080828,0.00004325898,0.000040548082,0.00006092151],"domain_scores_gemma":[0.9996699,0.000035313584,0.00011952049,0.00006402195,0.00007493138,0.000036221936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020219114,0.00048370907,0.0003270616,0.0013135492,0.0002689799,0.00070599234,0.00027426163,0.00033434457,0.0013223492],"category_scores_gemma":[0.00063419587,0.00019747534,0.00026644714,0.0012740192,0.00036808537,0.0003194024,0.00044363632,0.00027962276,0.0006696484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007813873,0.00017719208,0.8502736,0.00014682933,0.00020595161,0.0022851715,0.0010027546,0.035700954,0.044557113,0.0009365259,0.009173732,0.05475885],"study_design_scores_gemma":[0.0000070064148,0.000022340979,0.98528117,0.000014250145,0.00002312987,0.000085663945,0.00021793802,0.01160595,0.0007059596,0.00007918058,0.0019426403,0.00001472604],"about_ca_topic_score_codex":0.016749926,"about_ca_topic_score_gemma":0.02419895,"teacher_disagreement_score":0.016749926,"about_ca_system_score_codex":0.00035185297,"about_ca_system_score_gemma":0.0003380648,"threshold_uncertainty_score":0.03330487},"labels":[],"label_agreement":null},{"id":"W3096505003","doi":"10.5194/egusphere-egu2020-8240","title":"Earthquake source parameter analysis shows hydraulic fracturing induced events are consistent with fault reactivation under regional stress in northeastern British Columbia, Canada","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Structural basin; Fault (geology); Geomorphology","score_opus":0.024824729007121925,"score_gpt":0.194716461922944,"score_spread":0.16989173291582207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3096505003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9627861,0.00028416354,0.0005160801,0.00039204996,0.000017141194,0.00003629843,0.020061187,0.00019407066,0.015712919],"genre_scores_gemma":[0.98603034,0.00023104022,0.00038062097,0.00007176252,0.000004242875,0.000014280905,0.0068492545,0.0000389883,0.006379423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977654,0.000007940998,0.000015010273,0.000047184134,0.00006900263,0.00008432492],"domain_scores_gemma":[0.9987857,0.00006885408,0.0000848951,0.00004104781,0.0008711741,0.00014839444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001287186,0.00034485894,0.00027480474,0.0019103214,0.0017175268,0.0014849154,0.00081963366,0.00033135066,0.006740624],"category_scores_gemma":[0.0010009601,0.00023228939,0.00020910529,0.003870968,0.00045860177,0.00024263456,0.00048951333,0.00035056425,0.00076309516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016022036,0.00006174636,0.9253666,0.00008703631,0.00010861137,0.0006862889,0.0013030849,0.005675226,0.005755814,0.00057723955,0.020191222,0.04002693],"study_design_scores_gemma":[0.000010793089,0.0000045544357,0.99119556,0.000025884112,0.00002812278,0.000058355618,0.001697211,0.0028873999,0.0003336901,0.00004562628,0.003691141,0.000021622654],"about_ca_topic_score_codex":0.997364,"about_ca_topic_score_gemma":0.99889094,"teacher_disagreement_score":0.012550367,"about_ca_system_score_codex":0.012550367,"about_ca_system_score_gemma":0.014698591,"threshold_uncertainty_score":0.091059744},"labels":[],"label_agreement":null},{"id":"W3097459854","doi":"10.1007/s10950-020-09966-9","title":"Green, yellow, red, or out of the blue? An assessment of Traffic Light Schemes to mitigate the impact of hydraulic fracturing-induced seismicity","year":2020,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Magnitude (astronomy); Induced seismicity; Seismology; Hydraulic fracturing; Hydrogeology; Geology; Natural hazard; Environmental science; Physics; Astrophysics; Meteorology; Geotechnical engineering","score_opus":0.03941018326611693,"score_gpt":0.3085121892559562,"score_spread":0.26910200598983924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3097459854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9817747,0.0005827541,0.002436236,0.00086659926,0.00004137169,0.00008013621,0.008207674,0.00019794032,0.005812599],"genre_scores_gemma":[0.9935861,0.00023397274,0.0022528775,0.000059042763,0.00001593175,0.000014109419,0.0034101435,0.000013785769,0.00041391616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997857,0.00006549972,0.000010349822,0.000030612424,0.00006361506,0.000044154844],"domain_scores_gemma":[0.9990096,0.00024809287,0.00021132677,0.000056434932,0.00037893414,0.00009561878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007157878,0.00030384352,0.00020949522,0.0015632088,0.00017822815,0.00066375994,0.00035906318,0.00037454895,0.0008444593],"category_scores_gemma":[0.0020601018,0.00007874967,0.00023175335,0.000983158,0.00031221224,0.00054700515,0.00033706528,0.00031065047,0.00015833443],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009078938,0.00038116658,0.71704525,0.0006004186,0.00026347904,0.00044152935,0.0005720976,0.1392512,0.0065266103,0.006129224,0.018940298,0.10894073],"study_design_scores_gemma":[0.00008134808,0.0004241076,0.69091994,0.00026063976,0.00011898299,0.00012783249,0.002722261,0.27569765,0.0046266676,0.0018949899,0.023053741,0.00007186437],"about_ca_topic_score_codex":0.07346117,"about_ca_topic_score_gemma":0.12148279,"teacher_disagreement_score":0.07346117,"about_ca_system_score_codex":0.0010139665,"about_ca_system_score_gemma":0.0006033852,"threshold_uncertainty_score":0.14606714},"labels":[],"label_agreement":null},{"id":"W3097621006","doi":"10.1029/2021gc010092","title":"How Fault Rocks Form and Evolve in the Shallow San Andreas Fault","year":2021,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Southern California Earthquake Center","keywords":"Geology; Cataclastic rock; Authigenic; Protolith; Fault (geology); Fault gouge; Seismology; Slip (aerodynamics); Fault scarp; Petrology; Geochemistry; Tectonics; Sedimentary rock","score_opus":0.01144228880887945,"score_gpt":0.19678457929860974,"score_spread":0.18534229048973028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3097621006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99959034,0.000029258754,0.000056143945,0.000010197792,2.6356406e-7,9.0518233e-7,0.000023986044,0.0000033073177,0.0002858017],"genre_scores_gemma":[0.9996069,0.000028259272,0.00008771433,0.0000031442098,3.3083424e-7,7.782361e-7,0.000036884463,0.0000014912002,0.00023441916],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999361,0.000007840226,0.0000039959,0.000021440192,0.000011400458,0.000019107238],"domain_scores_gemma":[0.99989915,0.000011371707,0.000042213724,0.000008962108,0.000019597084,0.000018736047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009800553,0.00008749057,0.0001091916,0.00046963053,0.00024850006,0.00049388147,0.00014362329,0.00024646256,0.00060837535],"category_scores_gemma":[0.0003122533,0.00016268909,0.0000703042,0.00027783116,0.00042974867,0.000362828,0.00024066695,0.0001463146,0.00012952543],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001323915,0.000038068876,0.81101,0.000044930504,0.00003217,0.00033535724,0.0012446126,0.00364168,0.16983196,0.0007200398,0.00012799523,0.012840701],"study_design_scores_gemma":[0.0000027341946,0.000031568907,0.99295133,0.0000047763897,0.0000065201507,0.0001172093,0.00046873486,0.002074133,0.0036366135,0.00009634012,0.0006051192,0.0000048598354],"about_ca_topic_score_codex":0.015108362,"about_ca_topic_score_gemma":0.03675107,"teacher_disagreement_score":0.015108362,"about_ca_system_score_codex":0.0006155229,"about_ca_system_score_gemma":0.00023961056,"threshold_uncertainty_score":0.0300408},"labels":[],"label_agreement":null},{"id":"W3097687931","doi":"10.1130/abs/2020am-350542","title":"THE ACCRETIONARY GROWTH AND REWORKING OF SOUTHEASTERN LAURENTIA THROUGH THE U-PB-HF DETRITAL ZIRCON RECORD: INSIGHTS FROM THE LAC-SAINT-JEAN REGION (CENTRAL GRENVILLE PROVINCE, QUEBEC, CA)","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Laurentia; Zircon; Geology; Geochemistry; SAINT; Paleozoic; History","score_opus":0.02067092957810068,"score_gpt":0.20159836849785331,"score_spread":0.18092743891975263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3097687931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98787886,0.0011998034,0.00016524743,0.00021963914,0.000008153124,0.00001444139,0.002924015,0.000023236013,0.0075665824],"genre_scores_gemma":[0.99420035,0.0004481803,0.00027497465,0.00006951327,0.0000061914443,0.000007549981,0.0011569354,0.00001728142,0.0038189867],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998419,0.000009593688,0.000012828497,0.00005186151,0.000030176929,0.0000535043],"domain_scores_gemma":[0.99948174,0.000028755736,0.00011575551,0.000025166855,0.0002866851,0.00006191333],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033348537,0.0002370763,0.0003126173,0.002004924,0.0018852521,0.0014653787,0.00086972205,0.0003224577,0.0024582036],"category_scores_gemma":[0.0007303213,0.00017611614,0.00019659253,0.0024413026,0.000672258,0.0004993313,0.000703856,0.00028374835,0.00043710807],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026429392,0.0000381533,0.9210907,0.00015182872,0.00018725524,0.00051428325,0.0079735145,0.00072505506,0.014031459,0.0008494831,0.0038368965,0.050337076],"study_design_scores_gemma":[0.0000029655457,0.0000041503436,0.99591845,0.000027921642,0.000010558366,0.000044702392,0.0005739888,0.00012182619,0.00018195636,0.000011384622,0.0030975281,0.0000045201577],"about_ca_topic_score_codex":0.9798814,"about_ca_topic_score_gemma":0.9938624,"teacher_disagreement_score":0.020118594,"about_ca_system_score_codex":0.010432575,"about_ca_system_score_gemma":0.0062938672,"threshold_uncertainty_score":0.075693965},"labels":[],"label_agreement":null},{"id":"W3097866668","doi":"10.1029/2020jc016465","title":"Wave Generation Across a Continuum of Landslide Conditions From the Collapse of Partially Submerged to Fully Submerged Granular Columns","year":2020,"lang":"en","type":"article","venue":"Journal of Geophysical Research Oceans","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Subaerial; Dimensionless quantity; Amplitude; Geology; Water column; Landslide; Momentum (technical analysis); Range (aeronautics); Mechanics; Mesoscopic physics; Froude number; Geotechnical engineering; Physics; Seismology; Materials science; Oceanography; Optics","score_opus":0.08554355801832918,"score_gpt":0.31892444476577286,"score_spread":0.23338088674744367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3097866668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99929845,0.000014861205,0.00045148187,0.000004749247,0.0000010915239,0.0000038651115,0.000033378168,0.00001026769,0.00018185067],"genre_scores_gemma":[0.99979395,0.000010303709,0.00012042667,0.0000031726292,4.1495127e-7,0.000003241501,0.000025515037,0.0000012965972,0.000041783183],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993205,0.000006302856,0.0000048084135,0.000014256225,0.000018033625,0.000024668798],"domain_scores_gemma":[0.99978334,0.00007333429,0.00004124892,0.000026062255,0.000031566924,0.000044448956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012956891,0.00016265186,0.000217024,0.00019112273,0.00020606654,0.000356766,0.00016347437,0.00014379443,0.0008411025],"category_scores_gemma":[0.00039589658,0.00011670259,0.00011768958,0.00013106491,0.00037061214,0.00018322415,0.00039702494,0.00029484916,0.000058678997],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000795404,0.00019541258,0.022650085,0.00006742621,0.000036398527,0.00034464963,0.00021993677,0.008256231,0.9580339,0.00033478183,0.00011274915,0.00895294],"study_design_scores_gemma":[0.000099319106,0.0024381918,0.38898006,0.000031303927,0.00006683791,0.00044078156,0.001261976,0.12651248,0.4784076,0.0011089626,0.0005793558,0.00007318151],"about_ca_topic_score_codex":0.0009866774,"about_ca_topic_score_gemma":0.0009219408,"teacher_disagreement_score":0.0009866774,"about_ca_system_score_codex":0.00016115072,"about_ca_system_score_gemma":0.0001013514,"threshold_uncertainty_score":0.002813816},"labels":[],"label_agreement":null},{"id":"W3097932134","doi":"10.1130/abs/2020am-357529","title":"A NEW GARNET FRACTIONATION MODELLING TECHNIQUE AND ITS APPLICATION TO THE YUKON-TANANA TERRANE OF NORTH-WESTERN BRITISH COLUMBIA","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Terrane; Geology; Fractionation; Geochemistry; Archaeology; Seismology; Geography; Chemistry","score_opus":0.02352033635221013,"score_gpt":0.21717999017794637,"score_spread":0.19365965382573624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3097932134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7846953,0.00024262967,0.20401622,0.00022399383,0.0000216382,0.00007903158,0.0008862563,0.0024653482,0.007369551],"genre_scores_gemma":[0.8995296,0.0001995246,0.09677475,0.000018545019,0.00000577262,0.0000321059,0.00039906346,0.00044344066,0.0025972237],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999459,0.0000073811043,0.0000053541944,0.000019913803,0.000013760305,0.000007809685],"domain_scores_gemma":[0.9998323,0.000043604094,0.000018506447,0.000016704918,0.000076650496,0.000012299357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000265657,0.00047028394,0.00022994257,0.0012861358,0.0009275494,0.0010233028,0.0006650786,0.0003670139,0.0017851959],"category_scores_gemma":[0.00076209597,0.00024568904,0.00032629297,0.0015376221,0.0002098887,0.00046893628,0.00040577954,0.0002876768,0.00028706802],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003100064,0.00011696222,0.114129946,0.00028768356,0.00015860418,0.0006393437,0.0024820825,0.42826587,0.09773315,0.0059427153,0.0018743586,0.34805933],"study_design_scores_gemma":[0.000022877015,0.00002718991,0.036931884,0.000024079602,0.00005032528,0.00011769168,0.00054144266,0.9494613,0.0067338916,0.001129735,0.0049297954,0.000029938865],"about_ca_topic_score_codex":0.40797907,"about_ca_topic_score_gemma":0.5545598,"teacher_disagreement_score":0.5920209,"about_ca_system_score_codex":0.0013118627,"about_ca_system_score_gemma":0.0015918313,"threshold_uncertainty_score":0.8112087},"labels":[],"label_agreement":null},{"id":"W3098143493","doi":"10.1029/2020gl089651","title":"Machine Learning‐Based Analysis of Geological Susceptibility to Induced Seismicity in the Montney Formation, Canada","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Tectonics; Seismology; Thrust; Geotechnical engineering","score_opus":0.06437693706879997,"score_gpt":0.28536853564272036,"score_spread":0.22099159857392037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3098143493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99827516,0.000055179687,0.00037296728,0.00004525014,0.0000010775865,0.0000051791676,0.00077282346,0.00002179411,0.00045053594],"genre_scores_gemma":[0.9981281,0.000028685397,0.00029238488,0.0000054881907,0.0000010915,0.0000021843198,0.0012512723,0.000002982546,0.00028785822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975044,0.00003223359,0.000014016122,0.000057559282,0.00007232825,0.000073354946],"domain_scores_gemma":[0.9987914,0.00027353247,0.0001932645,0.000055206485,0.0005386422,0.00014794296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004238407,0.00028969647,0.00019355834,0.0012786497,0.00063975825,0.00061393075,0.0005747062,0.00018815177,0.00082792214],"category_scores_gemma":[0.0021654333,0.00010120248,0.00026767238,0.0017011265,0.0004969692,0.00019395999,0.00035332388,0.00023915681,0.00014290758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016146468,0.000038969098,0.95334345,0.000020336814,0.00010244289,0.00011584115,0.00018636134,0.026823934,0.002306586,0.00024021188,0.0007175958,0.015942907],"study_design_scores_gemma":[0.0000079575775,0.000014549191,0.9388208,0.0000080892305,0.00001647602,0.000023914014,0.00037530393,0.059494246,0.00058110163,0.00008832525,0.00055562815,0.000013545543],"about_ca_topic_score_codex":0.97549075,"about_ca_topic_score_gemma":0.98131573,"teacher_disagreement_score":0.024509251,"about_ca_system_score_codex":0.0068760985,"about_ca_system_score_gemma":0.005459199,"threshold_uncertainty_score":0.049889803},"labels":[],"label_agreement":null},{"id":"W3100067678","doi":"10.1029/2020gl090930","title":"Aseismic Deformation During the 2014 <i>M</i><sub><i>w</i></sub> 5.2 Karonga Earthquake, Malawi, From Satellite Interferometry and Earthquake Source Mechanisms","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Tulane University; National Science Foundation","keywords":"Geology; Seismology; Aftershock; Rift; Slip (aerodynamics); Deformation (meteorology); Paleoseismology; Tectonics; Crust; Interferometric synthetic aperture radar; Geophysics; Synthetic aperture radar","score_opus":0.02273814373486951,"score_gpt":0.23004378349462629,"score_spread":0.20730563975975677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3100067678","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991849,0.00006190792,0.00009985579,0.00002954838,0.0000016929729,0.0000030717088,0.00026802145,0.0000036941412,0.00034738047],"genre_scores_gemma":[0.99928814,0.00007835449,0.00010800532,0.000007574822,0.0000040047407,0.0000020336363,0.0003768478,0.0000012083833,0.00013378609],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999349,0.000009669398,0.0000064704345,0.000014614524,0.000010916032,0.000023370765],"domain_scores_gemma":[0.99981385,0.000023233806,0.00008340024,0.000011198743,0.000036395482,0.000031963278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019046488,0.0002690089,0.0001342375,0.00072877685,0.00020698023,0.00051589526,0.00018615297,0.00020740872,0.00058548356],"category_scores_gemma":[0.00044061278,0.0001635751,0.00019060187,0.000829215,0.00031644627,0.00033077778,0.00044165188,0.00017441224,0.00010822971],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001307068,0.000036449983,0.9698108,0.00007731672,0.00008892805,0.00045348395,0.0010965117,0.0022009036,0.012476556,0.00022637585,0.0004615309,0.012940455],"study_design_scores_gemma":[0.0000028059196,0.000010042417,0.99699664,0.000011473689,0.000017865703,0.000045745484,0.00027515093,0.0019723913,0.0003687044,0.000022258519,0.00027340362,0.000003574422],"about_ca_topic_score_codex":0.04664582,"about_ca_topic_score_gemma":0.10808136,"teacher_disagreement_score":0.04664582,"about_ca_system_score_codex":0.00054765254,"about_ca_system_score_gemma":0.00047052067,"threshold_uncertainty_score":0.09274864},"labels":[],"label_agreement":null},{"id":"W3101123119","doi":"10.3390/geosciences10110452","title":"Stochastic Analysis of Tsunami Hazard of the 1945 Makran Subduction Zone Mw 8.1–8.3 Earthquakes","year":2020,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Subduction; Geology; Seismic hazard; Slip (aerodynamics); Shore; Tsunami earthquake; Tectonics; Oceanography","score_opus":0.02139358680696379,"score_gpt":0.21299529356694483,"score_spread":0.19160170675998103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3101123119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708956,0.000021041362,0.0022894705,0.000039992985,0.0000018889896,0.0000067978303,0.000095508745,0.000017169954,0.0004385537],"genre_scores_gemma":[0.99965334,0.000012178894,0.00019927988,0.0000027958265,0.000001533112,0.0000042602287,0.000046949768,0.0000014059037,0.00007830848],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983263,0.000054885084,0.000011231768,0.000035308516,0.000029308441,0.000036648307],"domain_scores_gemma":[0.99890876,0.00061963307,0.0002491295,0.00006286605,0.00010298313,0.000056651497],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055912655,0.00047116654,0.0002552509,0.00043159202,0.0002650124,0.00040377997,0.0005691769,0.00049448444,0.00058087736],"category_scores_gemma":[0.0021453744,0.00027876886,0.00049689534,0.00023685556,0.00040972463,0.0003565253,0.00034131767,0.00031299636,0.000046052282],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020117874,0.000011653975,0.0064608515,0.000004351061,0.000015825874,0.000044093522,0.000014152722,0.9921234,0.0003381566,0.0005542423,0.000026860629,0.00038615786],"study_design_scores_gemma":[0.0000052320543,0.000026965243,0.004834249,0.0000019277043,0.0000073826163,0.000010478254,0.000015716229,0.9946898,0.00017558981,0.00019571335,0.000031689935,0.000005247946],"about_ca_topic_score_codex":0.033884294,"about_ca_topic_score_gemma":0.012900256,"teacher_disagreement_score":0.033884294,"about_ca_system_score_codex":0.0013891754,"about_ca_system_score_gemma":0.00050245144,"threshold_uncertainty_score":0.06737411},"labels":[],"label_agreement":null},{"id":"W3101974018","doi":"10.5194/egusphere-egu2020-12490","title":"Spontaneous dynamic rupture modeling of 2017 M 5.4 Pohang, South Korea, earthquake, using the slip-weakening friction law","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Nexen (Canada)","funders":"","keywords":"Geology; Earthquake rupture; Slip (aerodynamics); Seismology; Stress field; Interferometric synthetic aperture radar; Thrust fault; Nucleation; Geodesy; Fault (geology); Finite element method; Structural engineering; Physics; Synthetic aperture radar; Engineering","score_opus":0.03795944739558006,"score_gpt":0.228641241500049,"score_spread":0.19068179410446895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3101974018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9707714,0.0002181063,0.025176235,0.00014296491,0.000027011203,0.000033076267,0.00054906984,0.00018594677,0.0028962244],"genre_scores_gemma":[0.99647635,0.0000770001,0.0027496722,0.000010868922,0.0000052268456,0.000018747176,0.00022525087,0.000015562184,0.00042116892],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994004,0.000008734627,0.000007246953,0.000018525006,0.000011115296,0.000014372935],"domain_scores_gemma":[0.9998915,0.000033270404,0.000026008585,0.0000129771415,0.000020225798,0.00001591874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015330387,0.0004479256,0.0002898976,0.00033052277,0.00024140351,0.00043923978,0.00066897296,0.0005906209,0.0006412908],"category_scores_gemma":[0.00041483383,0.00020867724,0.0005473911,0.00022572238,0.00021048954,0.0004420602,0.0003195193,0.00030950908,0.00007776462],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045400382,0.00005560094,0.0060690697,0.00003920209,0.00003896689,0.00024364387,0.000045307428,0.98325366,0.00531607,0.0009981195,0.00029042485,0.0036046028],"study_design_scores_gemma":[0.0000033437625,0.000011238501,0.00076842244,0.0000010955742,0.0000035562882,0.000015838703,0.000009205662,0.998599,0.0003983973,0.00009748896,0.000090137444,0.0000024141223],"about_ca_topic_score_codex":0.008487535,"about_ca_topic_score_gemma":0.0048052124,"teacher_disagreement_score":0.008487535,"about_ca_system_score_codex":0.0003275284,"about_ca_system_score_gemma":0.00037121234,"threshold_uncertainty_score":0.01687622},"labels":[],"label_agreement":null},{"id":"W3103312549","doi":"10.5194/nhess-20-3039-2020","title":"Uncertainty quantification of tsunami inundation in Kuroshio, Kochi Prefecture, Japan, using the Nankai–Tonankai megathrust rupture scenarios","year":2020,"lang":"en","type":"article","venue":"Natural hazards and earth system sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; University of Bristol; Japan Society for the Promotion of Science; Leverhulme Trust","keywords":"Seismology; Geology; Hazard analysis; Hazard; Seismic hazard; Tsunami earthquake; Engineering","score_opus":0.033162723257063986,"score_gpt":0.2520722753244658,"score_spread":0.2189095520674018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3103312549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956232,0.000092038455,0.0034684786,0.00008671514,0.0000035734656,0.000010316143,0.00016945343,0.000014353791,0.00053194346],"genre_scores_gemma":[0.99931633,0.000034958633,0.000501986,0.0000036350584,0.0000012952871,0.0000048923876,0.00010295659,0.0000012990789,0.000032638305],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996972,0.00014524422,0.000023474246,0.000050578565,0.000039048173,0.000044436652],"domain_scores_gemma":[0.9990239,0.0005401222,0.00019162304,0.000047121375,0.00013046735,0.00006673376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010270963,0.000780327,0.00035257573,0.00092906354,0.0004050601,0.00089179614,0.00051142386,0.0005492535,0.0002252683],"category_scores_gemma":[0.0029107996,0.0003536607,0.0005467315,0.0007170099,0.00042067547,0.00081436895,0.0006132167,0.00033674506,0.000021067432],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056626413,0.00003487734,0.025768736,0.000025479601,0.00007955549,0.00014993356,0.000061008013,0.96985525,0.00065758213,0.00078630255,0.0001186948,0.0024060041],"study_design_scores_gemma":[0.00000916744,0.00003818576,0.014270904,0.0000067122196,0.00003421171,0.000016241906,0.00013913208,0.98435205,0.000357169,0.0006793401,0.00008234119,0.000014513486],"about_ca_topic_score_codex":0.04400542,"about_ca_topic_score_gemma":0.025420196,"teacher_disagreement_score":0.04400542,"about_ca_system_score_codex":0.001428401,"about_ca_system_score_gemma":0.00073490513,"threshold_uncertainty_score":0.087498546},"labels":[],"label_agreement":null},{"id":"W3104700490","doi":"10.1186/s40562-020-00164-6","title":"Rebuild of the Bulletin of the International Seismological Centre (ISC)—part 2: 1980–2010","year":2020,"lang":"en","type":"article","venue":"Geoscience Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"U.S. Geological Survey; Directorate for Geosciences; Syracuse University; Universitetet i Bergen; Academia Sinica; Pennsylvania State University; University of Pennsylvania","keywords":"Epicenter; Seismology; Geology; Earthquake prediction; Biogeosciences; Magnitude (astronomy); Geodesy; Physics","score_opus":0.018594644035367886,"score_gpt":0.1821270135767366,"score_spread":0.1635323695413687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3104700490","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.16401735,0.0089319525,0.012572381,0.014034596,0.014852472,0.003981419,0.4713369,0.008570181,0.30170274],"genre_scores_gemma":[0.27747798,0.005890425,0.028420625,0.002825343,0.005276194,0.003511043,0.52277637,0.0043297913,0.14949219],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.995854,0.00036729465,0.0005718789,0.0003804376,0.0023435343,0.00048284946],"domain_scores_gemma":[0.9688996,0.0014633846,0.002468872,0.002414069,0.022861863,0.0018922059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004390381,0.0010303034,0.0006579477,0.019650443,0.0010872973,0.0033448632,0.001450224,0.00089035096,0.013194457],"category_scores_gemma":[0.017910918,0.0005565459,0.0004839607,0.01444097,0.00084544683,0.0017582538,0.0022620384,0.0015379186,0.007731711],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003247428,0.00016716153,0.035832446,0.0010451528,0.00006904613,0.00031777972,0.0016510678,0.0019912974,0.0033908156,0.004676018,0.78293717,0.16759732],"study_design_scores_gemma":[0.000017405118,0.00004650878,0.113045834,0.00020554088,0.00002750492,0.00009506648,0.00038702376,0.00032852308,0.0013760957,0.00021382413,0.8842077,0.00004895596],"about_ca_topic_score_codex":0.17997545,"about_ca_topic_score_gemma":0.11547868,"teacher_disagreement_score":0.17997545,"about_ca_system_score_codex":0.007562099,"about_ca_system_score_gemma":0.013424776,"threshold_uncertainty_score":0.35785574},"labels":[],"label_agreement":null},{"id":"W3105109430","doi":"","title":"Seismic imaging of lower crustal sutures and a shallow-dipping, lower crustal mafic slab: direct evidence for tectonic accretion of archean continental lithosphere from the western superior lithoprobe transect, superior province, canadian shield","year":2003,"lang":"en","type":"article","venue":"EGS - AGU - EUG Joint Assembly","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mafic; Archean; Lithosphere; Accretion (finance); Slab; Tectonics; Transect; Geochemistry; Seismology; Paleontology; Oceanography","score_opus":0.024620375642804043,"score_gpt":0.23834096898387025,"score_spread":0.21372059334106622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3105109430","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995331,0.00032166642,0.00023909238,0.00008142656,0.0000039428196,0.0000133242,0.00087197556,0.000011573329,0.003126021],"genre_scores_gemma":[0.9965005,0.00040012356,0.0007523611,0.000032991276,0.000005844805,0.000005629241,0.0006746318,0.0000058822147,0.001622035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992347,0.0000021598999,0.000002678361,0.0000114237455,0.00002957104,0.000030772397],"domain_scores_gemma":[0.9997662,0.000013676803,0.000042156455,0.000010125387,0.000116835996,0.000050986648],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012379717,0.00020465339,0.00014850307,0.0014404175,0.0006121478,0.0006525317,0.0003682298,0.0003328355,0.0015078282],"category_scores_gemma":[0.0004229931,0.00028589246,0.000079679085,0.001812915,0.0005066526,0.00017924524,0.00036676417,0.0002765291,0.0002026868],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072009186,0.00008524789,0.5511662,0.00021413095,0.00010551878,0.0011612332,0.003181612,0.0007532207,0.3996013,0.00069917366,0.0019123435,0.04040008],"study_design_scores_gemma":[0.0000080633,0.000010429603,0.99610716,0.000009773088,0.000017742146,0.00043185908,0.00042976148,0.0002045189,0.0018803935,0.000030571922,0.0008654881,0.0000042281627],"about_ca_topic_score_codex":0.7045237,"about_ca_topic_score_gemma":0.9014104,"teacher_disagreement_score":0.29547632,"about_ca_system_score_codex":0.0011594152,"about_ca_system_score_gemma":0.002473235,"threshold_uncertainty_score":0.59443283},"labels":[],"label_agreement":null},{"id":"W3105354007","doi":"10.22215/etd/2017-11777","title":"Numerical modelling of seismic wave propagation through a soft-sediment filled basin near Kinburn, ON.","year":2017,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Center for Spintronics Research Network, Tohoku University; Government of Ontario; Compute Canada","keywords":"Structural basin; Geology; Bedrock; Outcrop; Seismometer; Back-stripping; Pull apart basin; Sedimentary basin analysis; Sediment; Seismic refraction; Geomorphology; Seismology; Sedimentary basin","score_opus":0.04303957664972434,"score_gpt":0.24854806326093,"score_spread":0.2055084866112057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3105354007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9608311,0.00024036618,0.012871006,0.00055443065,0.000080632766,0.000058193422,0.0013993554,0.00021954533,0.023745442],"genre_scores_gemma":[0.9913913,0.00008666534,0.0036841552,0.000024004528,0.000007288073,0.000026537162,0.00039941957,0.000035308232,0.0043452308],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999435,0.000010411115,0.0000037420975,0.00001282322,0.000013603644,0.000015952804],"domain_scores_gemma":[0.9996667,0.00014351607,0.00004156014,0.000018816489,0.00007716901,0.000052122625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013536967,0.00036194545,0.00026873843,0.00033601018,0.00057119865,0.00096342433,0.0008258845,0.0011289803,0.002833866],"category_scores_gemma":[0.0011556008,0.00035150108,0.00031978384,0.00039885342,0.00053923955,0.00041433467,0.00051404175,0.0006240657,0.00027059318],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006484489,0.000059181748,0.008339126,0.00003271133,0.00002177403,0.00014648685,0.000103508646,0.98531765,0.0013983713,0.0011088279,0.00069102045,0.0027164968],"study_design_scores_gemma":[0.000014038963,0.000008870355,0.0024616367,0.0000050662884,0.000005366368,0.00001009901,0.00007141032,0.99682707,0.000101126425,0.000189498,0.00030073646,0.000005186274],"about_ca_topic_score_codex":0.2441205,"about_ca_topic_score_gemma":0.2257552,"teacher_disagreement_score":0.7558795,"about_ca_system_score_codex":0.0012935207,"about_ca_system_score_gemma":0.0015268371,"threshold_uncertainty_score":0.48539907},"labels":[],"label_agreement":null},{"id":"W3106058787","doi":"10.3390/geosciences10110460","title":"Complex Shear Partitioning Involving the 6 February 2012 MW 6.7 Negros Earthquake Ground Rupture in Central Philippines","year":2020,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Fault scarp; Seismology; Aftershock; Focal mechanism; Thrust fault; Fault (geology); Earthquake rupture; Landslide; Interplate earthquake; Foreshock","score_opus":0.04552516379968043,"score_gpt":0.23021626905974554,"score_spread":0.1846911052600651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106058787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993148,0.00003045108,0.00007327936,0.00002066687,0.0000010134776,0.0000053078843,0.0001226459,0.00000911064,0.00042263957],"genre_scores_gemma":[0.9995596,0.00002408899,0.00010994304,0.0000039165993,0.0000021787748,0.0000030146334,0.00016768869,0.0000021307546,0.00012749665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998934,0.000015702373,0.000008052351,0.000033726854,0.00001908528,0.000029905166],"domain_scores_gemma":[0.99972314,0.00002296161,0.00011380635,0.00002463976,0.00006331445,0.00005216854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012761417,0.0003934169,0.00021735908,0.0014994058,0.0005178018,0.0006618955,0.00033605166,0.00035446964,0.0010780478],"category_scores_gemma":[0.0005355947,0.00022349329,0.00017559149,0.0011117794,0.00040883606,0.0003807868,0.00063524727,0.00015476765,0.00016604149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034324304,0.00012224517,0.92379856,0.00011697769,0.00013165394,0.0062204134,0.0033108802,0.010036798,0.02593225,0.0002899843,0.0009964072,0.028700564],"study_design_scores_gemma":[0.0000065458644,0.000050222527,0.9915426,0.000009791063,0.0000150744745,0.00038644794,0.0014218707,0.005525938,0.0004985465,0.000064772,0.000464503,0.000013654664],"about_ca_topic_score_codex":0.03463046,"about_ca_topic_score_gemma":0.05553303,"teacher_disagreement_score":0.03463046,"about_ca_system_score_codex":0.00056203053,"about_ca_system_score_gemma":0.00027789528,"threshold_uncertainty_score":0.06885773},"labels":[],"label_agreement":null},{"id":"W3106362586","doi":"10.5194/egusphere-egu2020-19863","title":"A new Miocene detachment from Antiparos Island (Cyclades, Greece)","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Blueschist; Geology; Metamorphic core complex; CYCLADES; Metamorphism; Detachment fault; Metamorphic rock; Basement; Schist; Gneiss; Geochemistry; Orogeny; Rift; Shear zone; Paleontology; Metamorphic facies; Petrology; Facies; Subduction; Tectonics; Extensional definition; Eclogite; Structural basin; Archaeology","score_opus":0.02419716590104403,"score_gpt":0.20891349955003563,"score_spread":0.1847163336489916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106362586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9683975,0.00032815212,0.00029131808,0.00020935822,0.00005077212,0.000052757754,0.00039696714,0.000052585914,0.030220486],"genre_scores_gemma":[0.9900101,0.0001921794,0.00058055104,0.000064831824,0.000019926983,0.0000209192,0.00072141615,0.000013265337,0.008376858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994457,0.000003613625,0.0000029541939,0.00002820252,0.000011699406,0.00000891823],"domain_scores_gemma":[0.9999603,0.0000035786047,0.000011340821,0.000005914471,0.000008040435,0.000010918839],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000048276674,0.00033098977,0.00014489195,0.000759426,0.000680036,0.00039099687,0.0003446404,0.0005120453,0.0061428268],"category_scores_gemma":[0.00013119508,0.00020465223,0.00016393125,0.00058982405,0.00067750865,0.0002663524,0.00080703857,0.0003157188,0.0008849853],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070838147,0.00020028054,0.6008721,0.0008059141,0.000161484,0.08701504,0.014207396,0.001834399,0.11834715,0.0043941205,0.0078362655,0.16361746],"study_design_scores_gemma":[0.00003123511,0.00022104096,0.92841053,0.00006608186,0.000027100034,0.019931564,0.0032802569,0.0005141999,0.0015514777,0.00040875544,0.04553833,0.000019399335],"about_ca_topic_score_codex":0.010914567,"about_ca_topic_score_gemma":0.022424819,"teacher_disagreement_score":0.010914567,"about_ca_system_score_codex":0.000368845,"about_ca_system_score_gemma":0.00040046428,"threshold_uncertainty_score":0.021702051},"labels":[],"label_agreement":null},{"id":"W3106468226","doi":"10.1029/2020jb020529","title":"Strain Accumulation and Release Rate in Canada: Implications for Long‐Term Crustal Deformation and Earthquake Hazards","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Geology; Post-glacial rebound; Geodetic datum; Seismology; Seismic hazard; Crust; Deformation (meteorology); Strain rate; Continental crust; Seismic moment; Geodesy; Glacial period; Geophysics; Tectonics; Geomorphology; Fault (geology); Oceanography","score_opus":0.06541004199429959,"score_gpt":0.34333209228399403,"score_spread":0.2779220502896944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106468226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916814,0.00041693522,0.00036008828,0.00060857984,0.0000052299083,0.0000138211535,0.0039022292,0.000027243133,0.0029845566],"genre_scores_gemma":[0.9980185,0.0001835929,0.00020697512,0.00004099923,0.0000015910368,0.0000032091345,0.00089510425,0.000005478155,0.0006445934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996712,0.000018977216,0.000023110088,0.00005155621,0.00012374617,0.00011149786],"domain_scores_gemma":[0.9980696,0.0001985803,0.00037599166,0.00006819119,0.0009773542,0.00031044247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005613222,0.00026236888,0.00028048203,0.0014661736,0.0011263518,0.0014711749,0.0009661885,0.00028971166,0.0018508919],"category_scores_gemma":[0.0023147715,0.00017490837,0.00039297648,0.0036038358,0.00070121145,0.00046063666,0.0006506584,0.0004376768,0.000114167015],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009897487,0.000026449829,0.9828318,0.00003135153,0.00008878288,0.00014110914,0.00036251303,0.004027863,0.0009809963,0.0007444106,0.0007152516,0.009950534],"study_design_scores_gemma":[0.0000025853685,0.000005931415,0.9948009,0.000013530934,0.000015985463,0.000027208169,0.0006245647,0.003644555,0.00018443612,0.00011881704,0.00055158633,0.000009803977],"about_ca_topic_score_codex":0.9950964,"about_ca_topic_score_gemma":0.99537045,"teacher_disagreement_score":0.02379708,"about_ca_system_score_codex":0.02379708,"about_ca_system_score_gemma":0.018270543,"threshold_uncertainty_score":0.17266071},"labels":[],"label_agreement":null},{"id":"W3106682895","doi":"10.1029/2020jb020887","title":"Statistics and Forecasting of Aftershocks During the 2019 Ridgecrest, California, Earthquake Sequence","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Foreshock; Sequence (biology); Seismology; Geology; Extreme value theory; Induced seismicity; Statistics; Mathematics","score_opus":0.058773026645371755,"score_gpt":0.31158267569495046,"score_spread":0.2528096490495787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3106682895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950813,0.000052540454,0.003771415,0.000053553482,0.0000052222567,0.0000113417655,0.0005867835,0.000043572898,0.00039435306],"genre_scores_gemma":[0.99796474,0.00003607807,0.0008726968,0.0000028864863,0.000005511533,0.000004517108,0.00094226096,0.0000025295608,0.00016884563],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997713,0.000052644657,0.000018572982,0.000060708793,0.00006971118,0.000027097389],"domain_scores_gemma":[0.9958658,0.0023300925,0.0008145913,0.00016329493,0.00064280105,0.00018337186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013391785,0.00026329406,0.0002748912,0.0013118951,0.00018207419,0.0004502184,0.00031310858,0.00031524632,0.0004890272],"category_scores_gemma":[0.0047951215,0.00013926163,0.0002074206,0.00082511955,0.00027732068,0.0003175227,0.00022368728,0.00029204867,0.00010296094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028851366,0.00008472358,0.4883736,0.000044271717,0.000078418096,0.0002411813,0.00008032751,0.48637727,0.0017619566,0.0015625128,0.0012216961,0.019885404],"study_design_scores_gemma":[0.000010779674,0.00010738883,0.29565606,0.0000106521875,0.000024923675,0.000034732202,0.000121954705,0.70250505,0.00071825105,0.0005183069,0.00027473585,0.000017127977],"about_ca_topic_score_codex":0.033293556,"about_ca_topic_score_gemma":0.030318342,"teacher_disagreement_score":0.033293556,"about_ca_system_score_codex":0.0005314228,"about_ca_system_score_gemma":0.0006895081,"threshold_uncertainty_score":0.06619948},"labels":[],"label_agreement":null},{"id":"W3108815417","doi":"10.4095/327592","title":"NAD83v70VG: a new national crustal velocity model for Canada","year":2020,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Geodesy; Seismology; Geography","score_opus":0.07978629324077739,"score_gpt":0.2626191137081942,"score_spread":0.18283282046741678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3108815417","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06788715,0.0012540309,0.23718536,0.0020502633,0.00071725034,0.000628984,0.5863294,0.017189711,0.08675791],"genre_scores_gemma":[0.2562722,0.0016233581,0.21214844,0.00042053545,0.000086737804,0.0008480031,0.47782093,0.003183433,0.04759638],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99955636,0.000028954952,0.000019761044,0.00006941627,0.000217904,0.00010749475],"domain_scores_gemma":[0.9988525,0.00004426331,0.000045054785,0.00006674521,0.0009078791,0.00008357909],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048195486,0.0012548078,0.0006770807,0.0012710559,0.0012950061,0.0020797767,0.0036283557,0.00067979627,0.009013496],"category_scores_gemma":[0.0017327127,0.0006680096,0.0010045527,0.0032700081,0.0003791416,0.0010343106,0.0009880404,0.0013784945,0.002986297],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016299046,0.000058717036,0.018979723,0.00012750796,0.0001447443,0.00009439967,0.00015740926,0.6905942,0.00089257373,0.01817746,0.21762483,0.05298555],"study_design_scores_gemma":[0.000094938325,0.000010534106,0.005507996,0.00005984397,0.00003765683,0.000031009356,0.00007904484,0.8367229,0.0006368208,0.0032539926,0.15347964,0.0000856209],"about_ca_topic_score_codex":0.98162293,"about_ca_topic_score_gemma":0.967046,"teacher_disagreement_score":0.018377066,"about_ca_system_score_codex":0.015830362,"about_ca_system_score_gemma":0.030082567,"threshold_uncertainty_score":0.11485785},"labels":[],"label_agreement":null},{"id":"W3109470023","doi":"","title":"Large Historic Earthquakes of the Northern Canadian Cordillera: The 1953-1957 MacKenzie Mountains Earthquake Sequence","year":2002,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Sequence (biology); Seismology; Geography","score_opus":0.026814236170592063,"score_gpt":0.21036916775085815,"score_spread":0.1835549315802661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3109470023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98336965,0.001003943,0.000078956444,0.0005389065,0.000041407537,0.00002664517,0.007878139,0.000022815766,0.0070395935],"genre_scores_gemma":[0.9948324,0.00034589463,0.00009690605,0.00006412837,0.000016095284,0.000010161068,0.002863677,0.00000723995,0.0017634294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996381,0.000012657068,0.000019498342,0.00005405942,0.0001113607,0.00016435786],"domain_scores_gemma":[0.9986979,0.00005641539,0.00025766293,0.000052476214,0.00068968977,0.0002459214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032482212,0.00028351092,0.0002798807,0.0030691728,0.0030477205,0.0011936289,0.00084449275,0.0007609069,0.0033262828],"category_scores_gemma":[0.0020875153,0.00024655327,0.00018856158,0.005701183,0.00095587893,0.0004184152,0.001224133,0.00050747907,0.00040517576],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024319704,0.00006004241,0.944191,0.00016885527,0.00016884915,0.00092831044,0.0063039595,0.0017055543,0.002693907,0.0010715753,0.015855988,0.026608752],"study_design_scores_gemma":[0.0000018471318,0.0000023409377,0.996494,0.000011257932,0.000007943752,0.000027225871,0.00066142465,0.00008237622,0.000042351672,0.000017020155,0.0026464812,0.0000057645934],"about_ca_topic_score_codex":0.98718834,"about_ca_topic_score_gemma":0.9972736,"teacher_disagreement_score":0.017314352,"about_ca_system_score_codex":0.017314352,"about_ca_system_score_gemma":0.012522753,"threshold_uncertainty_score":0.12562501},"labels":[],"label_agreement":null},{"id":"W3109699331","doi":"10.1785/0120200180","title":"Robust Empirical Time–Frequency Relations for Seismic Spectral Amplitudes, Part 2: Model Uncertainty and Optimal Parameterization","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Amplitude; Inversion (geology); Parametric statistics; Range (aeronautics); Bootstrapping (finance); Parametric model; Nonparametric statistics; Algorithm; Computer science; Mathematics; Geology; Seismology; Statistics; Econometrics; Physics","score_opus":0.05075706477898157,"score_gpt":0.23367297411135465,"score_spread":0.1829159093323731,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3109699331","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04363008,0.00049031194,0.9542061,0.0005049165,0.000015357027,0.000033528377,0.00015348397,0.00011457746,0.0008517025],"genre_scores_gemma":[0.87346643,0.0005150845,0.12408216,0.00016366532,0.00009316284,0.00023590922,0.00043803622,0.00017666072,0.00082881615],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9959661,0.0021921596,0.00023393673,0.00090333325,0.0005143414,0.00019025362],"domain_scores_gemma":[0.96984273,0.024533134,0.0023133415,0.0022481522,0.00091319357,0.00014943544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.011331182,0.0010654416,0.0011748967,0.0015989967,0.0003834738,0.0019844198,0.0015681022,0.0011810872,0.0009397724],"category_scores_gemma":[0.048305754,0.0009612898,0.0013495011,0.0009399837,0.002126018,0.0037577834,0.0022641595,0.0026027346,0.00017437716],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028304215,0.000022974347,0.0019026351,0.000067768124,0.00010108772,0.000049721322,0.00009040719,0.94941765,0.0009300974,0.03483414,0.00026163954,0.012293719],"study_design_scores_gemma":[0.000003570189,0.0000123908285,0.00081575586,0.000019078496,0.000009885672,0.000021453907,0.000017481918,0.96429926,0.00042766056,0.03409431,0.00026298876,0.000016075084],"about_ca_topic_score_codex":0.0040325276,"about_ca_topic_score_gemma":0.001969087,"teacher_disagreement_score":0.011331182,"about_ca_system_score_codex":0.0012622945,"about_ca_system_score_gemma":0.0010577121,"threshold_uncertainty_score":0.059925735},"labels":[],"label_agreement":null},{"id":"W3110042063","doi":"10.1130/ges02178.1","title":"Systematic characterization of morphotectonic variability along the Cascadia convergent margin: Implications for shallow megathrust behavior and tsunami hazards","year":2020,"lang":"en","type":"article","venue":"Geosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Forearc; Wedge (geometry); Seismology; Subduction; Geomorphology; Tectonics; Geometry","score_opus":0.017828010384245266,"score_gpt":0.21666211785918596,"score_spread":0.19883410747494068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3110042063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994461,0.000026862088,0.00005086515,0.0000049730634,3.4698033e-7,0.0000016281799,0.0001775275,0.0000037134837,0.0002879394],"genre_scores_gemma":[0.99960357,0.00001809674,0.000040708972,0.0000023442105,4.468955e-7,0.000002418444,0.00024175238,0.0000016530082,0.000089049885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998535,0.00002097018,0.000010852679,0.00005612981,0.00003361511,0.000024882454],"domain_scores_gemma":[0.99931896,0.00006898814,0.00022040865,0.00008550724,0.00016217203,0.00014409499],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020014262,0.00018900711,0.0001811291,0.0015719442,0.00038841588,0.00041669226,0.0002100861,0.00015765544,0.00071081734],"category_scores_gemma":[0.00066377106,0.00012963034,0.00017623995,0.0016454479,0.00041762917,0.00014987584,0.00043871923,0.00014956106,0.00013154557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029951487,0.0000067119568,0.99158055,0.0000070595474,0.000037079837,0.00003877356,0.00027958688,0.000119379045,0.006350773,0.000023448354,0.000035306624,0.0014912899],"study_design_scores_gemma":[1.5608819e-7,0.000001962427,0.9998373,5.5848733e-7,0.0000011893121,0.000007383745,0.00006617657,0.00003291301,0.00003004679,0.000002284827,0.000019671857,4.2477268e-7],"about_ca_topic_score_codex":0.071116254,"about_ca_topic_score_gemma":0.1907589,"teacher_disagreement_score":0.071116254,"about_ca_system_score_codex":0.0005060121,"about_ca_system_score_gemma":0.00033932153,"threshold_uncertainty_score":0.14140463},"labels":[],"label_agreement":null},{"id":"W3110247118","doi":"10.5194/egusphere-egu2020-21286","title":"How fault creep makes its way!","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Creep; Slip (aerodynamics); Penetration (warfare); Materials science; Mechanics; Fault (geology); Geology; Thermodynamics; Composite material; Engineering; Physics; Seismology","score_opus":0.03888313483184643,"score_gpt":0.2065895444006085,"score_spread":0.16770640956876207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3110247118","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.35791752,0.0047481502,0.390646,0.014293702,0.00129938,0.00007544734,0.0008320434,0.0014220224,0.22876576],"genre_scores_gemma":[0.97303253,0.000831106,0.0059996746,0.00034998794,0.000082555845,0.000028030254,0.00009721845,0.0001203165,0.019458534],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99987125,0.000025724721,0.000008421666,0.000039192426,0.00002924212,0.00002611087],"domain_scores_gemma":[0.9998393,0.000023770466,0.000038011913,0.00003597564,0.0000356264,0.000027231981],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019146397,0.00035543795,0.00030050517,0.00036033522,0.0005616324,0.0018543625,0.0006568716,0.0014695255,0.0054441732],"category_scores_gemma":[0.0008354636,0.00019295156,0.0004039607,0.00028451523,0.0013292182,0.0025817107,0.0008273334,0.00061471446,0.00094807055],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006997452,0.000047813497,0.007781396,0.00016246909,0.000057736936,0.0008143662,0.00092136266,0.26064408,0.013735947,0.66379064,0.008102515,0.043871764],"study_design_scores_gemma":[0.000022893644,0.00009461537,0.003987312,0.000102528444,0.000043404005,0.0007832636,0.0007866577,0.50793767,0.0036725183,0.4227021,0.059774738,0.00009233093],"about_ca_topic_score_codex":0.0044459305,"about_ca_topic_score_gemma":0.0028137579,"teacher_disagreement_score":0.0054441732,"about_ca_system_score_codex":0.00058542413,"about_ca_system_score_gemma":0.00046554624,"threshold_uncertainty_score":0.018212557},"labels":[],"label_agreement":null},{"id":"W3111049417","doi":"10.1098/rsta.2020.0135","title":"Cascadia megathrust earthquake rupture model constrained by geodetic fault locking","year":2021,"lang":"en","type":"article","venue":"Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; H2020 European Research Council; Deutsche Forschungsgemeinschaft","keywords":"Geology; Subduction; Seismology; Earthquake rupture; Episodic tremor and slip; Fault (geology); Tsunami earthquake; Tide gauge; Interplate earthquake; Slip (aerodynamics); Tectonics; Sea level; Oceanography","score_opus":0.01623806086597544,"score_gpt":0.21165555484366214,"score_spread":0.1954174939776867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111049417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97293067,0.00026685727,0.01804878,0.0003918239,0.0000356387,0.00003443246,0.0007879666,0.00016944583,0.0073345043],"genre_scores_gemma":[0.99790704,0.00007481943,0.00061320723,0.000017370285,0.0000061294,0.000025842233,0.00019668633,0.000012587342,0.0011462645],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988246,0.000026046797,0.000009623768,0.00003623883,0.000013574692,0.000032046722],"domain_scores_gemma":[0.9996499,0.00007834063,0.000100749574,0.000032022042,0.000056135887,0.00008289316],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029516837,0.0006598253,0.0006785784,0.00050516106,0.00047746074,0.00091196346,0.0016554089,0.0013525332,0.0024077194],"category_scores_gemma":[0.0009992651,0.00047339537,0.00081087364,0.0004214371,0.0006536878,0.00058115256,0.00071054953,0.00055947545,0.00023411395],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031061823,0.000014746367,0.0036452287,0.00001038577,0.0000156376,0.000104270504,0.000020294925,0.99435115,0.0004353877,0.00097434234,0.00009727853,0.00030019952],"study_design_scores_gemma":[0.000013200293,0.000009921074,0.0006972454,0.000002203959,0.000006986588,0.00000953,0.000011131482,0.9988267,0.000038281793,0.00032307368,0.000058209047,0.0000035055134],"about_ca_topic_score_codex":0.0439307,"about_ca_topic_score_gemma":0.016242467,"teacher_disagreement_score":0.0439307,"about_ca_system_score_codex":0.0011093525,"about_ca_system_score_gemma":0.0010282467,"threshold_uncertainty_score":0.08735001},"labels":[],"label_agreement":null},{"id":"W3111986999","doi":"10.1002/essoar.10505267.1","title":"The spatial footprint of seismic activity and aftershock triggering in a conceptual model of fluid-induced seismicity","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Aftershock; Library science; Physics; Geography; Geology; Seismology; Computer science","score_opus":0.053464924368287266,"score_gpt":0.23871233920965215,"score_spread":0.1852474148413649,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111986999","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5678002,0.0010700215,0.40075877,0.0036563424,0.00015346357,0.000093850766,0.0010664976,0.00032856755,0.025072366],"genre_scores_gemma":[0.9855677,0.00048776265,0.0069079315,0.00012246976,0.00006483005,0.00009741503,0.00017595664,0.000051440948,0.0065244557],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998154,0.000057987116,0.000008436034,0.000047508725,0.000026546715,0.00004411166],"domain_scores_gemma":[0.99904937,0.00036936032,0.00026373978,0.000046394216,0.000115238174,0.00015574024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006067875,0.00070968363,0.00064580096,0.00092132523,0.00057223695,0.0017158713,0.0022190856,0.0023562182,0.0027854987],"category_scores_gemma":[0.0017528756,0.000563381,0.00084233854,0.0008678888,0.0022784404,0.0023881963,0.0015323792,0.0012043196,0.00031454198],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030543,0.000040120387,0.0014871268,0.000024543257,0.000014766618,0.000113574344,0.00006916425,0.9447289,0.0011345651,0.051257264,0.0002771265,0.00082238554],"study_design_scores_gemma":[0.0000068414497,0.000013286106,0.00028574537,0.0000034106579,0.0000065496088,0.000013373657,0.000024591423,0.9922753,0.00005189745,0.0071386327,0.0001734241,0.000006926169],"about_ca_topic_score_codex":0.01831006,"about_ca_topic_score_gemma":0.008838637,"teacher_disagreement_score":0.01831006,"about_ca_system_score_codex":0.0016146039,"about_ca_system_score_gemma":0.0010445615,"threshold_uncertainty_score":0.036406994},"labels":[],"label_agreement":null},{"id":"W3112152057","doi":"","title":"Predicted Tsunami Heights and Currents in Vancouver Island Harbours Caused by a Future Cascadia Subduction Zone Earthquake","year":2004,"lang":"en","type":"article","venue":"AGU Spring Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Tsunami earthquake; Episodic tremor and slip; Tectonics","score_opus":0.007285985741292125,"score_gpt":0.19463955819889378,"score_spread":0.18735357245760165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3112152057","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997054,0.000023538405,0.0001225103,0.00011431256,0.000009627124,0.000008339769,0.0010933167,0.000027325552,0.0015470051],"genre_scores_gemma":[0.99791116,0.000032280386,0.00007523818,0.000011310707,0.0000022746171,0.0000042090096,0.0008944559,0.000003012565,0.0010661014],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991,0.0000075914936,0.0000056096997,0.000016312231,0.00002312372,0.000037372844],"domain_scores_gemma":[0.9995579,0.000058181155,0.00003863839,0.000015461439,0.00018923229,0.00014064185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019267084,0.00039823848,0.00019050085,0.0005832251,0.00095657277,0.0010068235,0.0005032689,0.00075488753,0.0034540487],"category_scores_gemma":[0.0008571437,0.0004786918,0.00047508947,0.0005121659,0.00035952884,0.00032444854,0.0004148008,0.0006754704,0.0005099081],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003750355,0.00012073331,0.8419563,0.000029291561,0.00009810719,0.0007420249,0.000232835,0.14713627,0.00201025,0.00048808657,0.002348258,0.0044627576],"study_design_scores_gemma":[0.00007293856,0.00007884396,0.84079343,0.00001831369,0.00005250502,0.0000875929,0.00083237624,0.15599337,0.0007889838,0.0002726062,0.0009717854,0.000037138758],"about_ca_topic_score_codex":0.74551946,"about_ca_topic_score_gemma":0.8240684,"teacher_disagreement_score":0.25448054,"about_ca_system_score_codex":0.0050673424,"about_ca_system_score_gemma":0.0032332728,"threshold_uncertainty_score":0.5119584},"labels":[],"label_agreement":null},{"id":"W3113436741","doi":"10.4401/ag-8338","title":"Temporal properties of aftershock sequences of large earthquakes in Iran - Analysis of primary and secondary aftershocks of the Ezgeleh sequence","year":2020,"lang":"en","type":"article","venue":"Annals of Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; University of Tehran","keywords":"Aftershock; Sequence (biology); Geology; Seismology; Magnitude (astronomy); Plateau (mathematics); Inverse; Event (particle physics); Mathematics; Geometry; Physics; Mathematical analysis","score_opus":0.07491798715625606,"score_gpt":0.25030371714348204,"score_spread":0.17538572998722599,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113436741","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998038,0.00009993493,0.0011073938,0.0000181276,0.0000050506874,0.000006498367,0.00019371044,0.000022107104,0.0005091908],"genre_scores_gemma":[0.99898845,0.000051568826,0.00040003454,0.0000035792443,0.0000062833333,0.000004332274,0.0004048838,0.000005501807,0.0001352273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983966,0.000021276688,0.000017665661,0.000033002347,0.000055613105,0.00003271437],"domain_scores_gemma":[0.998899,0.00026238034,0.00038471573,0.000081886414,0.00028427117,0.000087801964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005471851,0.00022990245,0.00023372275,0.0019104396,0.00014851482,0.0003329044,0.0002451326,0.00021338768,0.0008043219],"category_scores_gemma":[0.00219222,0.00009376324,0.00032788957,0.001516192,0.0001799729,0.00032494104,0.00021701676,0.00027182995,0.0002299178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003447226,0.00006380316,0.92740506,0.00009994527,0.00016445975,0.0005707381,0.0008868719,0.0144969085,0.010546086,0.00087940105,0.0006406751,0.043901317],"study_design_scores_gemma":[0.000005531547,0.00007732888,0.9837685,0.000007524862,0.000038802493,0.00024226203,0.00038272465,0.013782891,0.0008598917,0.00021004336,0.00061437633,0.000010165168],"about_ca_topic_score_codex":0.005670258,"about_ca_topic_score_gemma":0.005529561,"teacher_disagreement_score":0.005670258,"about_ca_system_score_codex":0.0002601346,"about_ca_system_score_gemma":0.000265459,"threshold_uncertainty_score":0.011274517},"labels":[],"label_agreement":null},{"id":"W3113538668","doi":"10.1093/gji/ggaa608","title":"Numerical analysis of interseismic, coseismic and post-seismic phases for normal and reverse faulting earthquakes in Italy","year":2020,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Japan Aerospace Exploration Agency; Communal Studies Association; Entomological Society of America","keywords":"Geology; Seismology; Crust; Fault (geology); Subsidence; Tectonics; Seismic hazard; Earthquake rupture; Geophysics; Geomorphology; Structural basin","score_opus":0.016685377625685647,"score_gpt":0.2448710264985613,"score_spread":0.22818564887287565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113538668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9901412,0.00013153389,0.0041061365,0.00026732992,0.000028397519,0.000021636703,0.00032088434,0.00016079884,0.00482202],"genre_scores_gemma":[0.99775994,0.000041541243,0.0013781493,0.00002488476,0.000007611545,0.000018701778,0.00016737226,0.00001827359,0.00058354397],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987006,0.000028366438,0.000010177161,0.000027382825,0.000018258193,0.00004578576],"domain_scores_gemma":[0.99945337,0.00022457093,0.0001361815,0.00004021273,0.00007113918,0.00007449523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035848192,0.00049039954,0.00048247477,0.000822665,0.00050610234,0.0007354901,0.0008335281,0.0012652031,0.001835369],"category_scores_gemma":[0.001434469,0.00035544726,0.00073994236,0.00058608095,0.0008245474,0.00038839143,0.00054138066,0.00047605415,0.00017138221],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005537481,0.00005349675,0.0121796075,0.000022698203,0.000021842518,0.00013572157,0.00004391224,0.98413056,0.000862072,0.0006773318,0.000280056,0.0015373438],"study_design_scores_gemma":[0.00001130378,0.000017601222,0.0036686056,0.0000031837442,0.0000069737803,0.0000120360255,0.000019631967,0.99593323,0.000095836964,0.00013147056,0.00009438337,0.0000057176103],"about_ca_topic_score_codex":0.03567527,"about_ca_topic_score_gemma":0.017273162,"teacher_disagreement_score":0.03567527,"about_ca_system_score_codex":0.0011347315,"about_ca_system_score_gemma":0.0007963683,"threshold_uncertainty_score":0.07093519},"labels":[],"label_agreement":null},{"id":"W3113728275","doi":"10.1029/2020gc009190","title":"In‐situ Mass Balance Estimates Offshore Costa Rica","year":2020,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Forearc; Underplating; Subduction; Sedimentary budget; Pelagic sediment; Geomorphology; Continental margin; Convergent boundary; Accretion (finance); Submarine pipeline; Seismology; Sediment transport; Sediment; Tectonics; Oceanography; Oceanic crust","score_opus":0.012404355784940299,"score_gpt":0.204603129583482,"score_spread":0.19219877379854172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113728275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877567,0.00029028344,0.0010223124,0.00006448477,0.0000034037794,0.000018439252,0.0034193608,0.000102307175,0.0073227007],"genre_scores_gemma":[0.99639577,0.00021434802,0.00085149816,0.000013674599,0.0000041212143,0.000016169355,0.0014512362,0.000021159385,0.001031997],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995494,0.0000057410657,0.0000040986138,0.000012774701,0.000014305062,0.000008194972],"domain_scores_gemma":[0.9998696,0.000009648658,0.000039420796,0.000016406631,0.000057885663,0.000006998113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012707186,0.0004392379,0.00015811039,0.0014185059,0.00022910727,0.0005032411,0.0003680147,0.00016953534,0.0015133619],"category_scores_gemma":[0.00028438913,0.00013868623,0.00018777809,0.0011184771,0.00012016363,0.00025309267,0.00038237355,0.00008297258,0.00032033093],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014829714,0.0000377492,0.8825477,0.00019394347,0.00030376727,0.000277803,0.0005403525,0.023412574,0.048687976,0.0006056547,0.0014434238,0.041800644],"study_design_scores_gemma":[0.000012320396,0.000014208793,0.972029,0.00001801361,0.000045202672,0.000044045617,0.00018693402,0.017571298,0.0050758068,0.00010881421,0.004886095,0.000008278153],"about_ca_topic_score_codex":0.082178876,"about_ca_topic_score_gemma":0.13814391,"teacher_disagreement_score":0.082178876,"about_ca_system_score_codex":0.001217197,"about_ca_system_score_gemma":0.00033086233,"threshold_uncertainty_score":0.16340113},"labels":[],"label_agreement":null},{"id":"W3114311053","doi":"10.1130/ges02258.1","title":"Seismic velocity structure of the Queen Charlotte terrace off western Canada in the region of the 2012 Haida Gwaii Mw 7.8 thrust earthquake","year":2020,"lang":"en","type":"article","venue":"Geosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Terrace (agriculture); Seismic refraction; Seafloor spreading; Subduction; Seismometer; Tectonics; Paleontology","score_opus":0.012576322342109628,"score_gpt":0.18262091814776152,"score_spread":0.1700445958056519,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3114311053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99485946,0.0002135201,0.00006979538,0.00009782853,0.000007048969,0.00002415936,0.0014140677,0.000013499751,0.0033006836],"genre_scores_gemma":[0.99550545,0.00021958012,0.00023552879,0.000033472115,0.0000031512454,0.000013695909,0.001400362,0.000007081997,0.002581621],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977475,0.000008455391,0.000009362032,0.000037503418,0.00009385011,0.00007603302],"domain_scores_gemma":[0.99914885,0.000032023425,0.00011957628,0.000021215563,0.00047808164,0.00020017066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018306314,0.0003844612,0.00027387857,0.001911753,0.0018265288,0.0012665349,0.00070068106,0.00029474375,0.001744732],"category_scores_gemma":[0.0006363489,0.00030027062,0.00017746113,0.0028715339,0.0007455738,0.00020675182,0.0008433396,0.00035489668,0.00029656128],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013868637,0.000037556278,0.96993655,0.00008317457,0.00006695871,0.00072887103,0.0036387811,0.00081146084,0.0060743913,0.00025258024,0.002454715,0.01577619],"study_design_scores_gemma":[0.000003163449,0.0000076192414,0.99680966,0.00001607056,0.0000058172855,0.00003975545,0.0015556214,0.0002663716,0.00012906257,0.000008324839,0.0011494942,0.000008987469],"about_ca_topic_score_codex":0.9918665,"about_ca_topic_score_gemma":0.99746394,"teacher_disagreement_score":0.01217743,"about_ca_system_score_codex":0.01217743,"about_ca_system_score_gemma":0.015992276,"threshold_uncertainty_score":0.08835381},"labels":[],"label_agreement":null},{"id":"W3114341992","doi":"10.1785/0120200233","title":"Testing an Empirical Green’s Function Method for Determining the Rupture Parameters of the 24 April 2014 Vancouver Island Earthquake","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Seismology; Deconvolution; Aftershock; Geology; Epicenter; Seismometer; Submarine pipeline; Geodesy; Statistics; Geotechnical engineering; Mathematics","score_opus":0.046198325325724404,"score_gpt":0.25336029418899286,"score_spread":0.20716196886326846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3114341992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9679098,0.000046579644,0.03083154,0.00006555377,0.0000076148167,0.000016695541,0.00010826384,0.00022350809,0.0007903371],"genre_scores_gemma":[0.97926337,0.000023333077,0.020223288,0.000013261559,0.0000036440608,0.000007133323,0.00024773576,0.0000366994,0.00018146871],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99951005,0.00018471477,0.00002887926,0.000090803536,0.00012492003,0.000060744114],"domain_scores_gemma":[0.9966041,0.0017950926,0.00029823493,0.00040580644,0.0007622438,0.00013456879],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023797872,0.0005091941,0.00021980223,0.0008408793,0.00032772456,0.0006714973,0.0005370434,0.00059133145,0.00058686384],"category_scores_gemma":[0.012668128,0.00022229359,0.000367261,0.00034948642,0.0004736107,0.0006732393,0.0005100143,0.00054950954,0.00024892736],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001224135,0.00046387615,0.3097426,0.000113553026,0.00035539138,0.00034519442,0.00044002806,0.4406637,0.032173146,0.0028122168,0.0013192666,0.21034689],"study_design_scores_gemma":[0.000020821719,0.00007351198,0.042089835,0.000011660193,0.000013957941,0.00007537831,0.00010586179,0.95069194,0.006217406,0.00036149615,0.0003164711,0.000021776756],"about_ca_topic_score_codex":0.020207493,"about_ca_topic_score_gemma":0.019527262,"teacher_disagreement_score":0.97979254,"about_ca_system_score_codex":0.0006308591,"about_ca_system_score_gemma":0.0013772177,"threshold_uncertainty_score":0.04017973},"labels":[],"label_agreement":null},{"id":"W3114681218","doi":"","title":"Source Scaling Relations and Along-Strike Segmentation of Slow Slip Events in a 3-D Subduction Fault Model","year":2014,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Scaling; Slip (aerodynamics); Geology; Subduction; Seismology; Moment magnitude scale; Geometry; Geodesy; Physics; Mathematics; Tectonics","score_opus":0.017401759864523803,"score_gpt":0.2260082463198979,"score_spread":0.2086064864553741,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3114681218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9564778,0.00018436764,0.036123246,0.00027973374,0.000013544124,0.000043253163,0.0013483937,0.0003016505,0.005227981],"genre_scores_gemma":[0.99655825,0.000085533036,0.0024488023,0.000015595348,0.0000049026394,0.00003114416,0.0002457123,0.000022590993,0.00058747234],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993837,0.000012821344,0.0000061496835,0.000017772263,0.000010394593,0.000014514553],"domain_scores_gemma":[0.9997589,0.000088980014,0.00007006677,0.000021077682,0.000032989206,0.000027912849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015948935,0.00043962308,0.0004474822,0.00052589306,0.00030208245,0.00063602143,0.0008512082,0.0011173408,0.0010192042],"category_scores_gemma":[0.00070821244,0.0003258969,0.0007470061,0.0004186895,0.00051478186,0.00036813752,0.00039342348,0.0004288739,0.00014870684],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017321305,0.000013406533,0.0016424815,0.000005867615,0.000005853184,0.000035468413,0.000018152816,0.9964569,0.00063656294,0.0006265941,0.00004824652,0.0004931753],"study_design_scores_gemma":[0.0000033681727,0.0000041373714,0.00042327028,8.982414e-7,0.0000020786856,0.000004305958,0.0000035351002,0.9992963,0.00004356418,0.00018316857,0.000032961336,0.0000024747515],"about_ca_topic_score_codex":0.0360257,"about_ca_topic_score_gemma":0.011691405,"teacher_disagreement_score":0.0360257,"about_ca_system_score_codex":0.0010017554,"about_ca_system_score_gemma":0.00053109083,"threshold_uncertainty_score":0.07163203},"labels":[],"label_agreement":null},{"id":"W3115195754","doi":"10.5194/egusphere-egu2020-10497","title":"Earthquake-earthquake triggering in natural swarms and fluid-induced seismicity","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Aftershock; Seismology; Geology; Tectonics; Earthquake swarm; Remotely triggered earthquakes; Seismic hazard; Microseism; Intraplate earthquake","score_opus":0.026438069808939157,"score_gpt":0.21832170720660468,"score_spread":0.19188363739766554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3115195754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926513,0.000018371278,0.00009086236,0.0000037637667,4.6115932e-7,0.0000024262035,0.0000716757,0.000004724789,0.0005425738],"genre_scores_gemma":[0.999746,0.000013622727,0.00007758914,0.0000017280138,6.349894e-7,0.000001975623,0.000094437004,6.615602e-7,0.00006343981],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992406,0.000007997518,0.000007740121,0.000023863886,0.000015217231,0.000021084643],"domain_scores_gemma":[0.99964225,0.00006709731,0.00019346585,0.0000201926,0.00003526115,0.000041743435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008020486,0.00010074791,0.00010750651,0.00047208657,0.00013987874,0.00026378225,0.00012159637,0.00016667471,0.001101895],"category_scores_gemma":[0.0004714246,0.00008978005,0.00008855387,0.00039491826,0.00027632987,0.00018238297,0.00026627825,0.00010222457,0.00008448856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017336766,0.00014274401,0.9494142,0.000071542745,0.000043571552,0.00045544608,0.00057348254,0.0035553474,0.03681989,0.00033122324,0.00023354928,0.008185572],"study_design_scores_gemma":[0.0000022589195,0.00004519946,0.99687374,0.0000024720173,0.000004684126,0.00007078477,0.00020910008,0.0015125226,0.0011180959,0.000033157685,0.00012487151,0.0000030687158],"about_ca_topic_score_codex":0.0055285306,"about_ca_topic_score_gemma":0.009991301,"teacher_disagreement_score":0.0055285306,"about_ca_system_score_codex":0.0003354998,"about_ca_system_score_gemma":0.0001424669,"threshold_uncertainty_score":0.010992706},"labels":[],"label_agreement":null},{"id":"W3118027110","doi":"10.1785/0220200322","title":"Hunting for Quaternary Faults in Eastern Canada: A Critical Appraisal of Two Potential Candidates","year":2020,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Escarpment; Fault scarp; Geology; Bathymetry; Quaternary; Neotectonics; Graben; Seismology; Bedrock; Fault (geology); Active fault; Echelon formation; Paleontology; Geomorphology; Tectonics; Oceanography","score_opus":0.0799776291362085,"score_gpt":0.34802232699882246,"score_spread":0.268044697862614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3118027110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96170306,0.015910521,0.00024563377,0.0028552664,0.00008988676,0.0003079325,0.0021218935,0.000010576608,0.016755193],"genre_scores_gemma":[0.98460555,0.010250074,0.0005408295,0.00056582637,0.000042119063,0.00003624711,0.0008548875,0.000004891624,0.0030996124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9989568,0.00008723564,0.00005497865,0.00007299913,0.0003935907,0.00043440436],"domain_scores_gemma":[0.9950956,0.00054496137,0.00042681277,0.00007254803,0.0031326164,0.00072747876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011928941,0.0005869013,0.000491976,0.005607194,0.0058566476,0.0024314125,0.0018957901,0.0007697957,0.0021167265],"category_scores_gemma":[0.002886751,0.00022985315,0.0003480686,0.009836165,0.0017768735,0.00055833225,0.0009378216,0.000616244,0.00014694013],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015947741,0.000074501455,0.9594484,0.00031058147,0.000071944516,0.0024321242,0.0035264418,0.00022849467,0.0003475075,0.00095023925,0.0020288646,0.03042133],"study_design_scores_gemma":[0.000011115241,0.000106369145,0.9521168,0.0004258074,0.00016935883,0.0005905619,0.03550601,0.000712229,0.00020966883,0.00018373523,0.009929684,0.000038773884],"about_ca_topic_score_codex":0.98754066,"about_ca_topic_score_gemma":0.99788886,"teacher_disagreement_score":0.044025045,"about_ca_system_score_codex":0.044025045,"about_ca_system_score_gemma":0.058058746,"threshold_uncertainty_score":0.31942558},"labels":[],"label_agreement":null},{"id":"W3118798776","doi":"10.1146/annurev-earth-071620-065605","title":"Toward an Integrative Geological and Geophysical View of Cascadia Subduction Zone Earthquakes","year":2021,"lang":"en","type":"article","venue":"Annual Review of Earth and Planetary Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"U.S. Geological Survey; Washington State University","keywords":"Subduction; Geology; Seismology; Natural (archaeology); Natural hazard; Geologic record; Earth science; Earthquake casualty estimation; Urban seismic risk; Tectonics; Paleontology; Oceanography; Seismic hazard","score_opus":0.024358771324312047,"score_gpt":0.2544146006857873,"score_spread":0.23005582936147526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3118798776","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0075088604,0.9645211,0.008073064,0.0096038915,0.00075254455,0.00002433062,0.00036511687,0.00008977437,0.009061225],"genre_scores_gemma":[0.028943008,0.9609764,0.005635647,0.0016568337,0.001298879,0.000027954697,0.00039603488,0.000024136934,0.0010410975],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99966407,0.00008015927,0.000059905713,0.00009604894,0.00007447527,0.000025305128],"domain_scores_gemma":[0.9990175,0.00038294037,0.00014694913,0.0000726901,0.00029211259,0.00008781858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016588436,0.0010262076,0.00096054,0.0051289015,0.00051932613,0.0031408975,0.0013445241,0.0010331691,0.0013116866],"category_scores_gemma":[0.0021857366,0.00043152395,0.0005199711,0.0034988553,0.0019934173,0.0055109905,0.0020326888,0.0028214818,0.0005343971],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000114894894,0.000079729405,0.013831882,0.016825693,0.00073384354,0.0009661484,0.009020122,0.0055507063,0.00829187,0.17705472,0.028774885,0.73875546],"study_design_scores_gemma":[0.000014291456,0.00012048709,0.041913453,0.0077489805,0.0007863912,0.0012247667,0.00477055,0.0014805481,0.00079535134,0.11514609,0.8258962,0.00010288093],"about_ca_topic_score_codex":0.006992453,"about_ca_topic_score_gemma":0.011079696,"teacher_disagreement_score":0.006992453,"about_ca_system_score_codex":0.0011887792,"about_ca_system_score_gemma":0.0026233143,"threshold_uncertainty_score":0.013903499},"labels":[],"label_agreement":null},{"id":"W3118985795","doi":"10.1029/2020gl089673","title":"Periodicity Analysis of Earthquake Occurrence and Hypocenter Depth Near Parkfield, California, 1994–2002 Versus 2006–2014","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Geological Survey; Southern California Earthquake Center","keywords":"Hypocenter; Seismology; Geology; Trough (economics); Foreshock; Induced seismicity; Aftershock","score_opus":0.04489871911694645,"score_gpt":0.2925265264584575,"score_spread":0.24762780734151105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3118985795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99661106,0.00004903991,0.00010144991,0.000024909214,0.0000056371778,0.000005195892,0.0023476945,0.00001658998,0.0008384082],"genre_scores_gemma":[0.99633396,0.000034013443,0.00011318627,0.00000729337,0.000009555007,0.000007545791,0.0031483974,0.0000054007214,0.00034062963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997868,0.000019376314,0.00002519505,0.00007517055,0.000054105065,0.000039409715],"domain_scores_gemma":[0.9983083,0.00020568144,0.00077796116,0.00010377277,0.00039650564,0.00020780391],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004429209,0.00015281174,0.00018386486,0.0014897855,0.0003084595,0.00059395324,0.00029776478,0.0001889644,0.0014323919],"category_scores_gemma":[0.0015852336,0.00015217415,0.0002450964,0.0013732754,0.0001664995,0.000313915,0.00031821092,0.00024997647,0.00020882675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010581192,0.00002372612,0.9953127,0.000013096562,0.000051980605,0.00002857204,0.00009954624,0.000619153,0.0005015668,0.00004026791,0.0006828771,0.002520755],"study_design_scores_gemma":[0.0000015450206,0.000008948168,0.99940026,0.0000017073497,0.0000057075476,0.0000089816485,0.00006297603,0.0003190361,0.00005051833,0.0000037306672,0.00013546109,0.0000010993452],"about_ca_topic_score_codex":0.057957698,"about_ca_topic_score_gemma":0.098030426,"teacher_disagreement_score":0.057957698,"about_ca_system_score_codex":0.0005513962,"about_ca_system_score_gemma":0.0004869184,"threshold_uncertainty_score":0.11524069},"labels":[],"label_agreement":null},{"id":"W3119143243","doi":"","title":"The Junction of Hellenic and Cyprus Arcs: a Detailed Study of the Morphology and Neogene Tectonic Evolution of the Anaximander Mountains","year":2009,"lang":"en","type":"article","venue":"AGU Spring Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Geology; Neogene; Paleontology; Tectonics; Transpression; Rift; Outcrop; Seismology; Sinistral and dextral; Structural basin","score_opus":0.010821749806043827,"score_gpt":0.20297634161369055,"score_spread":0.1921545918076467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3119143243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99914587,0.000089884736,0.00001373898,0.0000049743676,5.9268314e-7,0.0000017916179,0.000037116195,8.612344e-7,0.00070517074],"genre_scores_gemma":[0.9993693,0.00013897166,0.000084617095,0.000004374796,0.0000019357317,0.000002141761,0.00013307555,0.0000013366954,0.00026438516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992096,0.000012981881,0.0000069020193,0.000024172989,0.000011301249,0.0000236459],"domain_scores_gemma":[0.99990916,0.00001314514,0.00003717861,0.0000066934804,0.000016755857,0.000016973592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012137372,0.00013225115,0.00013383757,0.0012148272,0.0004140934,0.00057864736,0.00017659471,0.000189061,0.00075915386],"category_scores_gemma":[0.00020382012,0.00010867243,0.00011841251,0.0009427996,0.0002958316,0.0002679011,0.0003252116,0.00010722578,0.00010690071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017825782,0.000041572366,0.9507902,0.00005502163,0.00006839505,0.002407709,0.00478779,0.00055518624,0.01566883,0.00037675406,0.00024612626,0.024824062],"study_design_scores_gemma":[6.71131e-7,0.000007087545,0.9991998,0.0000031658913,0.000003255267,0.00012344966,0.00024963403,0.000038663173,0.00007821243,0.000004122577,0.00029096217,8.4869004e-7],"about_ca_topic_score_codex":0.01817105,"about_ca_topic_score_gemma":0.03307089,"teacher_disagreement_score":0.01817105,"about_ca_system_score_codex":0.00040097345,"about_ca_system_score_gemma":0.00024893234,"threshold_uncertainty_score":0.036130548},"labels":[],"label_agreement":null},{"id":"W3119843760","doi":"10.1029/2020gl090853","title":"Crustal Rotation and Fluids: Factors for the 2019 Ridgecrest Earthquake Sequence?","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Sinistral and dextral; Geology; Seismology; Clockwise; Shear (geology); Rotation (mathematics); Anisotropy; Fault (geology); Shear zone; Foreshock; Geodesy; Tectonics; Geometry; Petrology; Aftershock; Physics","score_opus":0.06959101381479219,"score_gpt":0.31140106436842596,"score_spread":0.24181005055363378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3119843760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99644876,0.0011251705,0.00008669506,0.0007751799,0.000017448176,0.0000082615215,0.00026897877,0.000010822016,0.0012586006],"genre_scores_gemma":[0.9994879,0.00016976468,0.000029492945,0.000030147032,0.000021953632,0.0000012026356,0.000085530344,0.0000014735493,0.00017259028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976844,0.000037653484,0.000028668599,0.000043274136,0.000033567147,0.00008830584],"domain_scores_gemma":[0.9978951,0.00024937466,0.0012336096,0.00008523084,0.0001355586,0.00040108917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003980394,0.0003064116,0.00026014404,0.0008840999,0.0002870891,0.0009183742,0.00022575833,0.0005042023,0.0038374327],"category_scores_gemma":[0.0026978422,0.00015482845,0.00032570434,0.0008265049,0.00061053183,0.00053814973,0.00043644838,0.00034119925,0.00030852156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018550476,0.000023758696,0.991764,0.000017636678,0.000024097193,0.0005087653,0.00008814488,0.000088097484,0.0014144087,0.000086140135,0.00012926813,0.005670167],"study_design_scores_gemma":[0.0000018065664,0.000031313404,0.999113,0.0000060660573,0.000009821668,0.00015906247,0.00018754619,0.0001176999,0.00012141004,0.00003764251,0.00021177458,0.0000027389517],"about_ca_topic_score_codex":0.009868452,"about_ca_topic_score_gemma":0.013399953,"teacher_disagreement_score":0.009868452,"about_ca_system_score_codex":0.00048234325,"about_ca_system_score_gemma":0.0006618453,"threshold_uncertainty_score":0.019622028},"labels":[],"label_agreement":null},{"id":"W3121956060","doi":"10.1007/s00024-021-02661-x","title":"Forecasting of Induced Seismicity Rates from Hydraulic Fracturing Activities Using Physics-Based Models for Probabilistic Seismic Hazard Analysis: A Case Study","year":2021,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Induced seismicity; Magnitude (astronomy); Seismology; Geology; Seismic hazard; Maximum magnitude; Hazard analysis; Physics; Engineering","score_opus":0.057433819926840116,"score_gpt":0.2532904957240024,"score_spread":0.19585667579716232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3121956060","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9746097,0.00010875676,0.022133365,0.00031862606,0.00001649482,0.00004082554,0.0005474644,0.00025853424,0.0019663186],"genre_scores_gemma":[0.997068,0.000050666025,0.002429606,0.0000034982331,0.000004497916,0.000009470241,0.0001329143,0.000007310244,0.00029407328],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998118,0.00006390421,0.000014172449,0.000042579817,0.00003826036,0.00002932852],"domain_scores_gemma":[0.9977945,0.0016735212,0.00017678645,0.0001036458,0.000169437,0.00008217532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00084704946,0.00077289564,0.0005042862,0.0008688159,0.0003624826,0.0006890548,0.00087440474,0.0014509313,0.00091966277],"category_scores_gemma":[0.0023691424,0.00050696876,0.0007276845,0.0008126751,0.00037761359,0.00094026816,0.00036389698,0.00070977694,0.00016261154],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075813456,0.00008034438,0.0049938606,0.000016935848,0.000017457727,0.00025932465,0.000028089959,0.988269,0.00070367794,0.0006239371,0.0001713956,0.0047601564],"study_design_scores_gemma":[0.0000062163203,0.000019902873,0.0011794114,0.0000013124926,0.0000051772545,0.000015425298,0.000010303135,0.99822634,0.00021755387,0.0002737179,0.00003952531,0.000005105897],"about_ca_topic_score_codex":0.01880291,"about_ca_topic_score_gemma":0.013866915,"teacher_disagreement_score":0.01880291,"about_ca_system_score_codex":0.0010797895,"about_ca_system_score_gemma":0.00072114205,"threshold_uncertainty_score":0.037386954},"labels":[],"label_agreement":null},{"id":"W3122039106","doi":"10.1029/2020gc009563","title":"Insights on Controlling Factors of Hydraulically Induced Seismicity in the Duvernay East Shale Basin","year":2021,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Canada First Research Excellence Fund","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Seismology; Poromechanics; Fault (geology); Shear (geology); Structural basin; Slip (aerodynamics); Petrology; Geotechnical engineering; Porosity; Geomorphology; Porous medium","score_opus":0.019892649707686026,"score_gpt":0.20288016074089948,"score_spread":0.18298751103321345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3122039106","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984059,0.000048008667,0.0005037305,0.00010812484,0.0000026052955,0.0000043429272,0.000042286323,0.000017454924,0.00086754165],"genre_scores_gemma":[0.99983835,0.000019173545,0.000058825175,0.000004640206,9.3799787e-7,0.0000013126302,0.000014610243,0.0000019197778,0.000060249524],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989545,0.000029287567,0.00001051647,0.00002069938,0.000014994975,0.000029064939],"domain_scores_gemma":[0.99981946,0.0000557249,0.000048488426,0.000015025269,0.00003354575,0.00002784055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021382984,0.00030375837,0.00028785705,0.00062548707,0.00046233358,0.00067953166,0.00037763108,0.0005952411,0.0012187643],"category_scores_gemma":[0.0006405358,0.0003586573,0.0003316961,0.0003224688,0.000549248,0.00051488914,0.0006228562,0.00030309072,0.00007937635],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018270935,0.00027691753,0.32795575,0.00013489088,0.00020092778,0.0020482675,0.00051411986,0.5976433,0.05688973,0.0044893767,0.0005750162,0.009089015],"study_design_scores_gemma":[0.00005199381,0.00009781509,0.201117,0.000019620004,0.00007180286,0.00011647556,0.0006938338,0.79330724,0.0026611465,0.0009993633,0.0008226103,0.000041076786],"about_ca_topic_score_codex":0.03403424,"about_ca_topic_score_gemma":0.027551798,"teacher_disagreement_score":0.96596575,"about_ca_system_score_codex":0.0011114267,"about_ca_system_score_gemma":0.0008423401,"threshold_uncertainty_score":0.06767231},"labels":[],"label_agreement":null},{"id":"W3122294221","doi":"","title":"Otish Basin: Discovery of Nearly 2,1GA Shocked Rocks Potentially Owning to a D>500 kms Impact Structure, Québec, Canada","year":2011,"lang":"en","type":"article","venue":"Meteoritics and Planetary Science Supplement","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Structural basin; Impact structure; Seismology; Paleontology; Physics; Impact crater; Astrobiology","score_opus":0.013237637965679614,"score_gpt":0.2047203232842057,"score_spread":0.19148268531852608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3122294221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8925093,0.0035242308,0.0015008978,0.0027381622,0.0001714666,0.00020461246,0.01440829,0.00025614418,0.084686905],"genre_scores_gemma":[0.9746054,0.0009322351,0.0013162943,0.00056982803,0.000028434748,0.000026528556,0.00194403,0.0000339012,0.020543339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999814,0.0000045396523,0.0000041675635,0.00002871927,0.000074406635,0.00007424715],"domain_scores_gemma":[0.99960285,0.000020760866,0.000033652992,0.000026916257,0.00021400173,0.00010189594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019325408,0.0003440777,0.00027902308,0.0012658553,0.003988276,0.0012498981,0.0006407025,0.000828022,0.0053202235],"category_scores_gemma":[0.00057206216,0.0002337816,0.0002219852,0.0019055869,0.0007043217,0.0002723088,0.00089167536,0.0005774403,0.000570522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00084643037,0.0001537308,0.7039492,0.000433055,0.0003730959,0.007000434,0.0037081577,0.0028534883,0.06945503,0.0062313285,0.06371976,0.14127636],"study_design_scores_gemma":[0.000025109171,0.000036715603,0.9379031,0.000054447042,0.000045557856,0.00053615216,0.0014519931,0.00075394753,0.0016008166,0.00032507864,0.05723981,0.000027212658],"about_ca_topic_score_codex":0.97969717,"about_ca_topic_score_gemma":0.99421185,"teacher_disagreement_score":0.020302832,"about_ca_system_score_codex":0.010971626,"about_ca_system_score_gemma":0.012694439,"threshold_uncertainty_score":0.07960504},"labels":[],"label_agreement":null},{"id":"W3122400549","doi":"10.1029/2020tc006076","title":"Fault Throw and Regional Uplift Histories From Drainage Analysis: Evolution of Southern Italy","year":2021,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mining Association of Canada; University of Ottawa","funders":"Natural Environment Research Council","keywords":"Geology; Fluvial; Tectonic uplift; Fault (geology); Tectonics; Inversion (geology); Paleontology; Stream power; Geomorphology; Seismology; Structural basin; Erosion","score_opus":0.013072953011955046,"score_gpt":0.20136888227941316,"score_spread":0.1882959292674581,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3122400549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99931014,0.000038883838,0.00010495014,0.000016452477,7.219262e-7,0.0000010318802,0.00016948362,0.000021016305,0.00033730315],"genre_scores_gemma":[0.99932516,0.00002196922,0.00011562363,0.000002621433,0.0000019344743,0.0000018707864,0.00041854542,0.0000065647764,0.00010578435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985003,0.000031520714,0.000009186025,0.00006500639,0.000013929247,0.000030257086],"domain_scores_gemma":[0.9995859,0.00012304592,0.00015148596,0.000055034998,0.00003929256,0.00004526719],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034703815,0.0002313125,0.00021814054,0.001471374,0.0001656248,0.00080338935,0.00026116168,0.00028310335,0.0010842805],"category_scores_gemma":[0.0010531096,0.00017112697,0.00047997432,0.0013447906,0.0003929576,0.00021641112,0.000438938,0.00016316213,0.00021533218],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009145791,0.00002017758,0.9809982,0.0000207779,0.00006851109,0.00015787988,0.00045253625,0.004479618,0.002801134,0.0001362212,0.00023675094,0.010536645],"study_design_scores_gemma":[0.0000027004291,0.000007706355,0.9965251,0.0000036874255,0.000010256249,0.00003654585,0.000049914204,0.0030801205,0.00007177015,0.000030120596,0.0001785098,0.000003535134],"about_ca_topic_score_codex":0.014219577,"about_ca_topic_score_gemma":0.02270391,"teacher_disagreement_score":0.014219577,"about_ca_system_score_codex":0.0005322828,"about_ca_system_score_gemma":0.00022228238,"threshold_uncertainty_score":0.028273642},"labels":[],"label_agreement":null},{"id":"W3123036762","doi":"","title":"Orbit Estimation for Late Warning Asteroid Impacts: The Case of 2014 AA","year":2014,"lang":"en","type":"article","venue":"AAS/Division for Planetary Sciences Meeting Abstracts #46","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Asteroid; Sky; Range (aeronautics); Orbit (dynamics); Near-Earth object; Geodesy; Geology; Geography; Astronomy; Computer science; Remote sensing; Physics; Aerospace engineering","score_opus":0.02146531335779826,"score_gpt":0.25492866391710545,"score_spread":0.2334633505593072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3123036762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8203815,0.0002713831,0.17088641,0.0010732078,0.000052043964,0.000056742916,0.00078687124,0.0002734015,0.006218313],"genre_scores_gemma":[0.96020913,0.000086282394,0.03860315,0.000024350555,0.000023073426,0.000016596738,0.00038283307,0.000020672947,0.00063374697],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99965525,0.000112974536,0.000020827796,0.000052708972,0.00009126274,0.000066881665],"domain_scores_gemma":[0.99801826,0.0011993619,0.00027105358,0.00020404896,0.00022535534,0.00008199801],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000976636,0.0003295307,0.0003625256,0.0006250401,0.00054082106,0.0007856427,0.00068606844,0.0007350179,0.0010618536],"category_scores_gemma":[0.008466537,0.00023574394,0.0003193062,0.00074880855,0.00050039164,0.0007232922,0.001169552,0.0007049409,0.00010712786],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019409518,0.00006511848,0.05072733,0.00006517328,0.000041324776,0.0009743059,0.0002887501,0.90080523,0.0013633016,0.014190275,0.0015208126,0.02976429],"study_design_scores_gemma":[0.000011787596,0.000025341318,0.006767195,0.00001021806,0.000008327848,0.00011160628,0.00016091962,0.9866868,0.0005529785,0.004948014,0.00070790836,0.000008977147],"about_ca_topic_score_codex":0.041130476,"about_ca_topic_score_gemma":0.03658857,"teacher_disagreement_score":0.041130476,"about_ca_system_score_codex":0.0006996438,"about_ca_system_score_gemma":0.00132502,"threshold_uncertainty_score":0.08178216},"labels":[],"label_agreement":null},{"id":"W3124276329","doi":"10.1029/2020jb020311","title":"Large‐Scale Fracture Systems Are Permeable Pathways for Fault Activation During Hydraulic Fracturing","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Hydraulic fracturing; Induced seismicity; Geology; Seismology; Microseism; Fracture (geology); Fault (geology); Pore water pressure; Seismometer; Petrology; Geotechnical engineering","score_opus":0.04106879206607408,"score_gpt":0.3010435762335246,"score_spread":0.25997478416745057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3124276329","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990326,0.000021625856,0.0005779208,0.000008343634,3.9321174e-7,0.0000028506204,0.000047228725,0.000010322517,0.0002988602],"genre_scores_gemma":[0.99978095,0.000006521049,0.00015489191,7.537081e-7,2.7085275e-7,0.000001003044,0.000018419521,4.3046398e-7,0.000036803423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994195,0.000005322223,0.00000302458,0.000014342141,0.000014130752,0.000021261116],"domain_scores_gemma":[0.9996753,0.00007945,0.00013286123,0.000021402428,0.000047282545,0.00004364359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008420223,0.000091580674,0.000094343064,0.00048767927,0.00023017246,0.0003754225,0.00020583953,0.00018451009,0.0008010917],"category_scores_gemma":[0.000459117,0.00012024535,0.000080788865,0.0003867143,0.0005065768,0.00021068005,0.00029102774,0.000121063604,0.000052026488],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032666733,0.00008828244,0.79962796,0.000075827615,0.000063747444,0.000972186,0.00088937144,0.014587708,0.1609474,0.001864959,0.00022861104,0.020327302],"study_design_scores_gemma":[0.000005231538,0.00003657677,0.9865807,0.0000057055327,0.000010827859,0.00016421141,0.00046460162,0.008789607,0.0032455665,0.0004526712,0.00023629286,0.0000079288375],"about_ca_topic_score_codex":0.017501798,"about_ca_topic_score_gemma":0.04028007,"teacher_disagreement_score":0.017501798,"about_ca_system_score_codex":0.0005141167,"about_ca_system_score_gemma":0.00035893693,"threshold_uncertainty_score":0.034799874},"labels":[],"label_agreement":null},{"id":"W3124914662","doi":"10.1038/s41598-021-82292-3","title":"Detection of volcanic unrest onset in La Palma, Canary Islands, evolution and implications","year":2021,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Ministerio de Asuntos Económicos y Transformación Digital, Gobierno de España; Consejo Superior de Investigaciones Científicas; Ministerio de Ciencia e Innovación; Ministerio de Ciencia, Innovación y Universidades","keywords":"Volcano; Unrest; Archipelago; Geology; Seismology; Volcanic hazards; Submarine volcano; Geodetic datum; Oceanography; Geodesy","score_opus":0.01160907117806671,"score_gpt":0.2174653363930324,"score_spread":0.2058562652149657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3124914662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961738,0.0002547477,0.00016996336,0.00009291072,0.00000426955,0.000007998096,0.00039695532,0.000025710844,0.002873705],"genre_scores_gemma":[0.9990196,0.00011806222,0.00027698136,0.0000065390795,0.000003987953,0.0000039869988,0.00019052632,0.0000036383587,0.00037664612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998863,0.000009849979,0.0000061281817,0.00004085137,0.000022402644,0.00003455293],"domain_scores_gemma":[0.99940217,0.00009228697,0.00021809053,0.000041249477,0.00013592708,0.00011027454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002152035,0.00013031185,0.00015733181,0.0012337398,0.00035993062,0.00073192,0.00029789712,0.0002886656,0.000987632],"category_scores_gemma":[0.0010825976,0.00008339713,0.00012312812,0.0009000332,0.0003291822,0.00044359296,0.00046560814,0.00027195332,0.00017328851],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012894897,0.000044859455,0.9697216,0.000050569823,0.000036235844,0.00045148324,0.00078604126,0.00052791816,0.007570348,0.00008634007,0.0002402481,0.020355418],"study_design_scores_gemma":[0.0000010168743,0.0000095192345,0.9984226,0.0000047752596,0.000006794259,0.0001091229,0.00044192266,0.00027356294,0.0003047275,0.000023711897,0.0003993086,0.0000028451059],"about_ca_topic_score_codex":0.049127437,"about_ca_topic_score_gemma":0.071206935,"teacher_disagreement_score":0.049127437,"about_ca_system_score_codex":0.0006187125,"about_ca_system_score_gemma":0.00032070986,"threshold_uncertainty_score":0.09768295},"labels":[],"label_agreement":null},{"id":"W3124922997","doi":"10.1785/0220200242","title":"If Not Brittle: Ductile, Plastic, or Viscous?","year":2021,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Brittleness; Terminology; Geology; Confusion; Deformation (meteorology); Unification; Geotechnical engineering; Computer science; Materials science; Linguistics; Composite material; Psychology","score_opus":0.09536325187946315,"score_gpt":0.3253304229431653,"score_spread":0.22996717106370212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3124922997","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14302042,0.0968038,0.041784465,0.42604977,0.026084738,0.00011093885,0.0005219928,0.0002479058,0.26537594],"genre_scores_gemma":[0.899461,0.025609165,0.0050018844,0.029159615,0.008204799,0.000068179645,0.00017147373,0.00013217914,0.03219181],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9984871,0.00052535813,0.00016020944,0.00020190621,0.00044946978,0.00017595867],"domain_scores_gemma":[0.99644524,0.0015294116,0.00060987496,0.00022886378,0.00082996715,0.00035673007],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00195901,0.0003911546,0.00075549557,0.0018068934,0.0016180867,0.007900602,0.0014101745,0.0027707033,0.005557504],"category_scores_gemma":[0.0068298327,0.00022367299,0.00023953449,0.0015943554,0.013127922,0.0065465984,0.0014878439,0.002580266,0.0015864907],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029973884,0.000093241215,0.010653804,0.0007851267,0.00004247801,0.0011658855,0.008147557,0.0005333708,0.0026288636,0.7947723,0.0968231,0.08405446],"study_design_scores_gemma":[0.000025906953,0.00014630557,0.008774032,0.0011012214,0.000035929297,0.0023172458,0.025923539,0.0019072029,0.0019325204,0.7106476,0.24708866,0.00009979495],"about_ca_topic_score_codex":0.0013344543,"about_ca_topic_score_gemma":0.0016754685,"teacher_disagreement_score":0.007900602,"about_ca_system_score_codex":0.001382856,"about_ca_system_score_gemma":0.0007229339,"threshold_uncertainty_score":0.018591702},"labels":[],"label_agreement":null},{"id":"W3125376014","doi":"10.1785/0120200204","title":"Paleoseismic Trenching Reveals Late Quaternary Kinematics of the Leech River Fault: Implications for Forearc Strain Accumulation in Northern Cascadia","year":2021,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Forearc; Fault scarp; Quaternary; Seismology; Colluvium; Slip (aerodynamics); Fault (geology); Trench; Imbrication; Geomorphology; Subduction; Tectonics; Paleontology; Alluvium","score_opus":0.037447903330326736,"score_gpt":0.26394116377218074,"score_spread":0.226493260441854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3125376014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989342,0.000045802095,0.00005221822,0.000013221192,9.942929e-7,0.000002356003,0.00017334412,0.000008251287,0.00076961785],"genre_scores_gemma":[0.99952495,0.000023215158,0.000061501465,0.0000041961694,8.8813044e-7,0.0000024537883,0.00011840119,0.0000024316737,0.00026196428],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986243,0.000009559536,0.0000066721045,0.0000559261,0.00002967053,0.000035680063],"domain_scores_gemma":[0.99961025,0.00003834761,0.00009535326,0.000039732782,0.000107887834,0.00010854473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018758803,0.00027401515,0.00025509179,0.0013486242,0.0008555097,0.00066563505,0.00030971068,0.00035033154,0.0018620825],"category_scores_gemma":[0.0005172949,0.00023772275,0.00022278099,0.0010047704,0.00061281066,0.00019958845,0.0006049405,0.00024657257,0.0002477761],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000073563,0.000015264346,0.9806919,0.000019973026,0.000035137862,0.00030210314,0.0011897356,0.00041150604,0.013780684,0.00003816027,0.000068589965,0.0033732827],"study_design_scores_gemma":[6.856742e-7,0.0000040029004,0.9995827,0.0000015594795,0.000002164227,0.000021296104,0.00018172537,0.00005410609,0.00007458712,0.0000046554087,0.00007136177,0.0000011406362],"about_ca_topic_score_codex":0.1798515,"about_ca_topic_score_gemma":0.4419926,"teacher_disagreement_score":0.82014847,"about_ca_system_score_codex":0.0012081088,"about_ca_system_score_gemma":0.0006214295,"threshold_uncertainty_score":0.35760927},"labels":[],"label_agreement":null},{"id":"W3126968637","doi":"10.5194/se-12-765-2021","title":"Unprecedented quiescence in resource development area allows detection of long-lived latent seismicity","year":2021,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Eidgenössische Technische Hochschule Zürich; Microseismic Industry Consortium; Seoul National University; Pukyong National University; Natural Sciences and Engineering Research Council of Canada; Chungnam National University; Canadian Natural Resources Limited","keywords":"Induced seismicity; Geology; Seismology; Hydraulic fracturing; Geothermal gradient; Period (music); Stock (firearms); Geography; Paleontology; Archaeology","score_opus":0.025876033241253055,"score_gpt":0.2235226014589877,"score_spread":0.19764656821773463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3126968637","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929432,0.00009323621,0.0009632634,0.00004987891,0.0000070012434,0.000010379545,0.0012343883,0.00008526195,0.00461338],"genre_scores_gemma":[0.99799985,0.000038407536,0.00046913995,0.0000104692,0.0000042076495,0.000005699501,0.0009358603,0.00000788981,0.0005284745],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986756,0.0000069473813,0.0000048565153,0.000029840776,0.000045644694,0.00004505045],"domain_scores_gemma":[0.99967337,0.000025186186,0.00008661951,0.000019959476,0.000097367585,0.000097508266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013380643,0.00018780584,0.00013463899,0.0012192468,0.00046154318,0.00068322656,0.00024756027,0.00018253397,0.0019055197],"category_scores_gemma":[0.00046705792,0.00010748314,0.000071380746,0.0014621873,0.00034027718,0.00023130103,0.00056063297,0.0003298897,0.0003243301],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018431213,0.000049688748,0.92611706,0.000068258145,0.00004057021,0.000545657,0.0009938106,0.0011100094,0.039630953,0.00038732734,0.0018943753,0.028978026],"study_design_scores_gemma":[0.000002191198,0.000010817482,0.9964987,0.00000712888,0.000005103252,0.00006540003,0.00039691443,0.00093024294,0.00070439355,0.000049862643,0.0013244052,0.0000048432917],"about_ca_topic_score_codex":0.14897168,"about_ca_topic_score_gemma":0.3720734,"teacher_disagreement_score":0.14897168,"about_ca_system_score_codex":0.0007575365,"about_ca_system_score_gemma":0.0007975598,"threshold_uncertainty_score":0.29620916},"labels":[],"label_agreement":null},{"id":"W3127335656","doi":"10.1093/gji/ggab053","title":"Glacial isostatic adjustment of the Pacific Coast of North America: the influence of lateral Earth structure","year":2021,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; University of Ottawa","keywords":"Geology; Post-glacial rebound; Lithosphere; Subduction; Mantle (geology); Deglaciation; Seismology; Geophysics; Earth model; Earth structure; Geodesy; Glacial period; Tectonics; Geomorphology","score_opus":0.007040667970306336,"score_gpt":0.2076144185437877,"score_spread":0.20057375057348137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127335656","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99755585,0.0001180096,0.00055521564,0.0001235127,0.0000075961243,0.0000041751023,0.00017364098,0.000048882397,0.0014131506],"genre_scores_gemma":[0.99932885,0.00006271527,0.00023427732,0.000015205287,0.000002681122,0.0000024958983,0.00015452683,0.000012271987,0.00018689175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999838,0.00004936493,0.00001053355,0.000057550493,0.00002654901,0.00001800483],"domain_scores_gemma":[0.99949646,0.00019583412,0.00009665219,0.000056132463,0.0001005156,0.00005433566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033086704,0.0003363374,0.00022408091,0.0004690525,0.00028987523,0.0011165794,0.00045718928,0.00032949587,0.001016336],"category_scores_gemma":[0.0018459504,0.00024400612,0.00040693916,0.00052405434,0.000453208,0.0006288769,0.00044708542,0.00033758816,0.0001183862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012670382,0.00005539066,0.5755359,0.000067691275,0.0002618941,0.00039181788,0.00023664697,0.39890325,0.006304517,0.00066365703,0.00092273846,0.016529774],"study_design_scores_gemma":[0.000020900436,0.000041996802,0.49382505,0.00002773046,0.000077103,0.00009244457,0.0005124594,0.50176483,0.0012816329,0.0006926916,0.0016232552,0.000039957806],"about_ca_topic_score_codex":0.13625996,"about_ca_topic_score_gemma":0.099651575,"teacher_disagreement_score":0.13625996,"about_ca_system_score_codex":0.0008808081,"about_ca_system_score_gemma":0.000702228,"threshold_uncertainty_score":0.2709337},"labels":[],"label_agreement":null},{"id":"W3127359814","doi":"10.21203/rs.3.rs-66196/v1","title":"Scaling relations of seismic moment and rupture area for outer-rise earthquakes","year":2020,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"","keywords":"Seismology; Seismic moment; Scaling; Moment (physics); Geology; Scaling law; Physics; Geometry; Mathematics; Classical mechanics; Fault (geology)","score_opus":0.08927640148670456,"score_gpt":0.33568895883154426,"score_spread":0.2464125573448397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127359814","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9455757,0.00063816825,0.04636223,0.000095512994,0.00003127788,0.000050747276,0.0010334733,0.0009357627,0.0052771037],"genre_scores_gemma":[0.9917163,0.00012207661,0.00687851,0.000015300882,0.000022793009,0.000037048572,0.0006904733,0.00011743991,0.0003999865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993166,0.00016370534,0.000052218238,0.00024527177,0.00018499153,0.00003726744],"domain_scores_gemma":[0.9929422,0.003562629,0.0012998396,0.0011323722,0.00088959566,0.00017332021],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081517024,0.00047910126,0.000343254,0.0022285467,0.00017488285,0.00042486333,0.00037422992,0.00028476544,0.0015464879],"category_scores_gemma":[0.012141713,0.00021867364,0.00036726028,0.00089930627,0.00044119108,0.0007521936,0.00050476665,0.0005047712,0.00073259516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034279012,0.00011403884,0.65771353,0.00029562422,0.000299782,0.00041585104,0.0014619867,0.047920525,0.12396103,0.0044644778,0.002319508,0.16069093],"study_design_scores_gemma":[0.0000149376265,0.00024126047,0.88248205,0.000036099806,0.000048323654,0.000614299,0.00025240995,0.09164849,0.016061729,0.0043784915,0.0041497545,0.000072267576],"about_ca_topic_score_codex":0.0008169537,"about_ca_topic_score_gemma":0.00067093177,"teacher_disagreement_score":0.0022285467,"about_ca_system_score_codex":0.00028546568,"about_ca_system_score_gemma":0.000090856614,"threshold_uncertainty_score":0.005173564},"labels":[],"label_agreement":null},{"id":"W3127960535","doi":"10.1130/g48461.1","title":"Is the Eastern Denali fault still active?","year":2021,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Aftershock; Induced seismicity; Transform fault; Fault (geology); Active fault; Strike-slip tectonics; Relocation; Slip (aerodynamics)","score_opus":0.02398145653522625,"score_gpt":0.23423663045350412,"score_spread":0.21025517391827786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127960535","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97058713,0.0020438281,0.0005675404,0.0018356838,0.000076914155,0.000010083046,0.00042594864,0.00003146086,0.024421273],"genre_scores_gemma":[0.99852043,0.00035933306,0.00010296549,0.000039915274,0.000014625297,0.0000010061856,0.00015281767,0.0000023404425,0.00080655265],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997435,0.000024065313,0.00002132449,0.00008491082,0.000032946788,0.00009323841],"domain_scores_gemma":[0.9995566,0.0000626053,0.00014661076,0.000042127926,0.00012565542,0.000066387365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039748734,0.00022472169,0.0005051459,0.0006057434,0.0009242914,0.0021475255,0.0007917612,0.0008118377,0.003291998],"category_scores_gemma":[0.0010779286,0.00009888382,0.0001688948,0.0011276675,0.0011436489,0.0013146269,0.0004980915,0.00028008863,0.00046829862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045431958,0.000051881976,0.92027634,0.00029084715,0.00009449198,0.0024710717,0.0019876305,0.0040325965,0.006359902,0.024646161,0.0015521577,0.037782572],"study_design_scores_gemma":[0.000026209489,0.0001052285,0.90632325,0.0004004262,0.00018638054,0.0016286231,0.0186175,0.011813515,0.0040458506,0.010748447,0.04603434,0.000070152666],"about_ca_topic_score_codex":0.14118952,"about_ca_topic_score_gemma":0.18085898,"teacher_disagreement_score":0.14118952,"about_ca_system_score_codex":0.0022474162,"about_ca_system_score_gemma":0.0010410834,"threshold_uncertainty_score":0.28073537},"labels":[],"label_agreement":null},{"id":"W3127968807","doi":"10.22215/etd/2009-06550","title":"Stochastic finite-fault modeling of the September 26, 2003 M 8.1 Tokachi-Oki earthquake. Implications for expected ground motions for megathrust events in the Cascadia subduction zone","year":2009,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Research Institute for Earth Science and Disaster Prevention; Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Episodic tremor and slip; Fault (geology); Geodesy; Tectonics","score_opus":0.03528325077066435,"score_gpt":0.27259737413713053,"score_spread":0.23731412336646618,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127968807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97517234,0.00024526677,0.016982902,0.0009446389,0.000051392766,0.000012610901,0.00086581585,0.0001481971,0.005576794],"genre_scores_gemma":[0.998401,0.000043794964,0.00054430624,0.000016292679,0.000009059165,0.000004521712,0.00017090458,0.000011382099,0.0007988025],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999237,0.000026328336,0.0000051753273,0.000016394037,0.00000861533,0.00001981661],"domain_scores_gemma":[0.9993699,0.00036978637,0.00009880141,0.000027443511,0.00006881504,0.000065267195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003628584,0.00029951637,0.0004373319,0.0002698782,0.00038688423,0.000689105,0.0009533859,0.0009959376,0.0019334843],"category_scores_gemma":[0.0018822952,0.00035328045,0.00048324847,0.0003075879,0.0005506009,0.0006342611,0.00035769574,0.00067672745,0.000149301],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021033913,0.000010458131,0.0017887191,0.0000051894785,0.000008906548,0.000019209801,0.000011439714,0.99637824,0.00008829356,0.0011242405,0.00012713327,0.00041713534],"study_design_scores_gemma":[0.0000037165596,0.0000032378684,0.00051930425,0.0000011434853,0.0000027720484,0.000001952978,0.000006346141,0.99914706,0.000019266434,0.00026367354,0.000029916318,0.0000015800982],"about_ca_topic_score_codex":0.104235314,"about_ca_topic_score_gemma":0.07847542,"teacher_disagreement_score":0.104235314,"about_ca_system_score_codex":0.0014739836,"about_ca_system_score_gemma":0.0010278529,"threshold_uncertainty_score":0.20725721},"labels":[],"label_agreement":null},{"id":"W3128036002","doi":"10.1098/rsta.2019.0416","title":"The earthquake cycle in the dry lower continental crust: insights from two deeply exhumed terranes (Musgrave Ranges, Australia and Lofoten, Norway)","year":2021,"lang":"en","type":"article","venue":"Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Università degli Studi di Padova; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Sight Research UK; Natural Environment Research Council; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; FP7 People: Marie-Curie Actions; National Science Foundation","keywords":"Geology; Continental crust; Shear zone; Crust; Terrane; Slip (aerodynamics); Seismology; Creep; Shear (geology); Petrology; Tectonics; Geophysics","score_opus":0.020194820054611085,"score_gpt":0.22664129394127933,"score_spread":0.20644647388666823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128036002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994598,0.000072849034,0.000024805167,0.000008727735,4.4853044e-7,0.0000015695001,0.000055315704,9.05951e-7,0.00037568947],"genre_scores_gemma":[0.99931467,0.000107784894,0.00009170557,0.000015849404,0.0000021513222,0.0000028344423,0.00019569152,0.0000020301366,0.00026722034],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999496,0.00000714375,0.0000044667286,0.000013999154,0.000010133891,0.000014692591],"domain_scores_gemma":[0.9999031,0.000013058185,0.000032660333,0.0000070637234,0.000015629108,0.000028489023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010718274,0.00016917153,0.00018028395,0.0010143651,0.00034924343,0.00034582295,0.00021441822,0.00024492305,0.0007358726],"category_scores_gemma":[0.00025555503,0.00014703209,0.00013507724,0.00082400226,0.00045576427,0.00024409361,0.00060634204,0.00013421278,0.00014402978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015517454,0.00007043181,0.94787943,0.00009233662,0.00005803488,0.0010898528,0.006307241,0.00053482526,0.030777626,0.00010415263,0.00013080222,0.012800069],"study_design_scores_gemma":[0.0000010479826,0.000015083919,0.9989827,0.0000026195953,0.0000034811164,0.000104044106,0.00051105116,0.0000742339,0.00010207542,0.000008636931,0.00019360906,0.0000013742089],"about_ca_topic_score_codex":0.029962126,"about_ca_topic_score_gemma":0.06245686,"teacher_disagreement_score":0.029962126,"about_ca_system_score_codex":0.0003562966,"about_ca_system_score_gemma":0.00017929908,"threshold_uncertainty_score":0.05957544},"labels":[],"label_agreement":null},{"id":"W3128179381","doi":"10.1029/2020jb020384","title":"Fluid‐Earthquake and Earthquake‐Earthquake Interactions in Southern Kansas, USA","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Induced seismicity; Geology; Seismology; Pore water pressure; Intraplate earthquake; Fault (geology); Poromechanics; Tectonics; Geotechnical engineering; Porosity","score_opus":0.05371020253437864,"score_gpt":0.3304158486741582,"score_spread":0.27670564613977955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128179381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987431,0.000039311246,0.00006512563,0.000032220494,0.0000013251384,0.000003314861,0.0007980782,0.000010927515,0.00030673016],"genre_scores_gemma":[0.99897456,0.000025599618,0.000059206464,0.0000061617225,0.0000012536913,0.000002851733,0.00062421255,0.0000014587523,0.0003046733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999356,0.0000073519514,0.0000046411974,0.000018006675,0.000013545385,0.000020820806],"domain_scores_gemma":[0.9994229,0.00005661486,0.00026699097,0.000016598246,0.00015484987,0.000082002916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009250763,0.00013841936,0.000117666474,0.0010649876,0.00038820156,0.00045857838,0.00024530655,0.0002380364,0.0015176494],"category_scores_gemma":[0.0004694287,0.00012768866,0.00011308212,0.0016914498,0.00024345604,0.00024627557,0.00043990734,0.00019056391,0.00021832739],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040084888,0.000031683638,0.9948185,0.000022589355,0.000030788568,0.000118201824,0.00048394856,0.00063901226,0.0008783407,0.000041550004,0.00044315524,0.0024520678],"study_design_scores_gemma":[0.0000015400738,0.000009158307,0.9984049,0.0000041559233,0.000005566647,0.000015916356,0.000485311,0.000718764,0.00004845239,0.00000963754,0.00029415157,0.000002469869],"about_ca_topic_score_codex":0.2816116,"about_ca_topic_score_gemma":0.5007689,"teacher_disagreement_score":0.2816116,"about_ca_system_score_codex":0.00096926145,"about_ca_system_score_gemma":0.0007131575,"threshold_uncertainty_score":0.55994487},"labels":[],"label_agreement":null},{"id":"W3128202658","doi":"10.3389/feart.2021.665185","title":"Geologic and Structural Evolution of the NE Lau Basin, Tonga: Morphotectonic Analysis and Classification of Structures Using Shallow Seismicity","year":2021,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Mount Royal University; University of Toronto","funders":"University of Toronto; Bundesministerium für Bildung und Forschung; Natural Sciences and Engineering Research Council of Canada; Schmidt Ocean Institute","keywords":"Geology; Seismology; Transform fault; Subduction; Geodynamics; Transtension; Slab window; Sinistral and dextral; Forearc; Plate tectonics; Inversion (geology); Clockwise; Fault (geology); Strike-slip tectonics; Tectonics; Oceanic crust; Rotation (mathematics); Geometry","score_opus":0.01405443521864361,"score_gpt":0.21824151086415136,"score_spread":0.20418707564550775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128202658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941504,0.00005980632,0.000098600096,0.000014479701,5.751429e-7,0.0000031262987,0.00011358254,0.0000056474937,0.0002891991],"genre_scores_gemma":[0.99944645,0.000066623266,0.00013878981,0.0000056233407,8.991658e-7,0.0000039420784,0.00014580906,0.0000026421021,0.00018905697],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994683,0.000007796178,0.0000047006947,0.000017332079,0.000008126559,0.000015251109],"domain_scores_gemma":[0.9998729,0.000015125477,0.000041559833,0.000013473446,0.000021045436,0.000035747227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012989451,0.00018771882,0.00019057898,0.0009606252,0.00027721017,0.0003976674,0.00017906449,0.00017212277,0.00081787666],"category_scores_gemma":[0.00035964543,0.00017029828,0.00022259777,0.0009915375,0.00047117597,0.00027211284,0.0005980452,0.000103007784,0.0001321076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042565745,0.0000142318195,0.9603307,0.0000509909,0.000051569634,0.00034150784,0.0016592146,0.0010239991,0.026364282,0.00016431864,0.00010780648,0.009848693],"study_design_scores_gemma":[7.017376e-7,0.000005669001,0.9988354,0.0000022781292,0.000008480355,0.000032789903,0.00021138304,0.00059836113,0.0001242254,0.000012820681,0.00016574928,0.0000023091961],"about_ca_topic_score_codex":0.06599106,"about_ca_topic_score_gemma":0.10947984,"teacher_disagreement_score":0.06599106,"about_ca_system_score_codex":0.000630193,"about_ca_system_score_gemma":0.00054943154,"threshold_uncertainty_score":0.13121384},"labels":[],"label_agreement":null},{"id":"W3128214727","doi":"10.1029/2020jb021074","title":"What Controls Effective Elastic Thickness of the Lithosphere in the Pacific Ocean?","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Lithosphere; Seamount; Subduction; Bathymetry; Seismology; Seafloor spreading; Oceanic crust; Mantle (geology); Pacific Plate; Ridge push; Mid-ocean ridge; Geophysics; Tectonics; Oceanography","score_opus":0.024284041419390816,"score_gpt":0.30271724833223573,"score_spread":0.2784332069128449,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128214727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982973,0.0001357939,0.0006087451,0.0000422958,0.0000028605002,0.0000019198155,0.00014204095,0.000015419833,0.000753671],"genre_scores_gemma":[0.9996774,0.000057579015,0.00009562294,0.0000060393613,0.000002136123,0.0000011103843,0.0000638637,0.0000053346907,0.00009091243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992096,0.000013575836,0.000006779563,0.000023824767,0.000012493532,0.000022307631],"domain_scores_gemma":[0.9995921,0.00011148553,0.00013918796,0.00003296587,0.000057570975,0.000066708955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022025286,0.00019323823,0.0001350757,0.0005728391,0.00018604686,0.0007479827,0.00023292235,0.00024558292,0.0013619304],"category_scores_gemma":[0.0012936963,0.00023102202,0.00014009565,0.00042295843,0.0004375936,0.00050550065,0.00035054135,0.00016086102,0.00016105027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018476216,0.000030976338,0.8679631,0.00012132644,0.00019648821,0.0004088142,0.00033520843,0.01175879,0.102927364,0.00093194743,0.00027788297,0.014863369],"study_design_scores_gemma":[0.0000032082946,0.000013913382,0.9886115,0.000013007008,0.000022067863,0.000072611845,0.000282876,0.0074691297,0.0027804708,0.00048273813,0.00023678264,0.0000117575455],"about_ca_topic_score_codex":0.005573716,"about_ca_topic_score_gemma":0.004254326,"teacher_disagreement_score":0.005573716,"about_ca_system_score_codex":0.00021293058,"about_ca_system_score_gemma":0.0002183607,"threshold_uncertainty_score":0.01108253},"labels":[],"label_agreement":null},{"id":"W3128938066","doi":"10.5194/egusphere-egu2020-12637","title":"Structural inheritance and evolving rift kinematics in transform and oblique rift systems: A comparison of global examples","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Rift; Mantle (geology); Geology; Oblique case; Tectonics; Crust; Kinematics; Seismology; Potential field; Geophysics; Physics","score_opus":0.03612783517203147,"score_gpt":0.2530331266125686,"score_spread":0.21690529144053713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128938066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.960923,0.0071363733,0.0030522065,0.00017819916,0.000009375541,0.000021696475,0.00059942756,0.00007433229,0.028005257],"genre_scores_gemma":[0.9944037,0.002809383,0.0013373591,0.000013424767,0.000013500183,0.0000064440137,0.00048413628,0.000022273454,0.00090965565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985075,0.000030806154,0.00001413042,0.00004429183,0.000028668006,0.000031201558],"domain_scores_gemma":[0.99963963,0.00009707381,0.000147477,0.00003139643,0.000056978384,0.000027453692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031408173,0.00026033953,0.00026556558,0.0029852833,0.00030508006,0.0010190522,0.00019046091,0.00023928544,0.0025924006],"category_scores_gemma":[0.0005239647,0.0001100118,0.00027018637,0.0042047068,0.0009894934,0.0008251215,0.0006959434,0.0002552358,0.0003080604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003796932,0.00003690412,0.72320265,0.001186981,0.0002956271,0.0021568148,0.01775783,0.0058975234,0.009503721,0.023217265,0.0017311539,0.21463391],"study_design_scores_gemma":[0.0000064538494,0.000058547637,0.98460025,0.00007851892,0.000078075536,0.0010355907,0.0022654084,0.0016143236,0.00052934885,0.0023664308,0.007352566,0.000014564766],"about_ca_topic_score_codex":0.0043173763,"about_ca_topic_score_gemma":0.009749778,"teacher_disagreement_score":0.0043173763,"about_ca_system_score_codex":0.00039009948,"about_ca_system_score_gemma":0.000163795,"threshold_uncertainty_score":0.008672476},"labels":[],"label_agreement":null},{"id":"W3129108663","doi":"10.1785/0120200172","title":"Robust Empirical Time–Frequency Relations for Seismic Spectral Amplitudes, Part 1: Application to Regional<i>S</i>Waves in Southeastern Iran","year":2020,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Amplitude; Spurious relationship; Parametric statistics; Attenuation; Physics; Geology; Geodesy; Computational physics; Seismology; Mathematics; Statistics; Optics","score_opus":0.05422873922838519,"score_gpt":0.24064442485020576,"score_spread":0.18641568562182056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129108663","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8978336,0.0002384822,0.10026958,0.000085792046,0.000010084196,0.000046578538,0.00022088857,0.00039871543,0.00089638797],"genre_scores_gemma":[0.9780206,0.00010634175,0.02139071,0.000007815544,0.000013441722,0.000017818447,0.00026244394,0.00003277733,0.00014810855],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99965227,0.00010210468,0.000022771967,0.000110728666,0.0000795029,0.000032623724],"domain_scores_gemma":[0.99863416,0.0006444005,0.0002711148,0.00019074618,0.00023672823,0.00002279164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015173481,0.00048070258,0.00036932755,0.0010210022,0.00024345327,0.0004410698,0.000996003,0.00042961823,0.00043607183],"category_scores_gemma":[0.004598711,0.00027110887,0.00067284703,0.0010640748,0.00033882033,0.00046948416,0.000467365,0.00050877273,0.00012979942],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014335391,0.00015227919,0.08246311,0.000113284346,0.00014939353,0.0003599239,0.00036929687,0.7790378,0.007616927,0.001994844,0.00066495786,0.12693477],"study_design_scores_gemma":[0.000014489223,0.000029492885,0.030382501,0.000006475947,0.000019499017,0.00005059465,0.00009710221,0.9673474,0.000969714,0.0007985335,0.00026987577,0.000014442401],"about_ca_topic_score_codex":0.030010326,"about_ca_topic_score_gemma":0.018611325,"teacher_disagreement_score":0.030010326,"about_ca_system_score_codex":0.0005121915,"about_ca_system_score_gemma":0.00076900085,"threshold_uncertainty_score":0.059671283},"labels":[],"label_agreement":null},{"id":"W3131239598","doi":"10.5194/egusphere-egu21-546","title":"A record of plume-induced plate rotation triggering seafloor spreading and subduction initiation","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"","keywords":"Plate tectonics; Subduction; Convergent boundary; Geology; Mantle plume; Seafloor spreading; Lithosphere; Mid-ocean ridge; Tectonics; Ridge; Plume; Pacific Plate; Transform fault; North American Plate; Mantle (geology); Paleontology; Seismology; Oceanic crust; Geophysics; Geography","score_opus":0.0316045302670321,"score_gpt":0.2322158001389017,"score_spread":0.2006112698718696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3131239598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954099,0.00016604415,0.00061411265,0.00009652186,0.000010973336,0.000004235684,0.00044412544,0.00011812939,0.003135978],"genre_scores_gemma":[0.99912816,0.000055622837,0.00029071167,0.00001260646,0.0000060476586,0.0000017213141,0.0003041015,0.000006378507,0.00019456427],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999678,0.0000025888032,0.0000019680945,0.000009874645,0.000010211046,0.0000074285877],"domain_scores_gemma":[0.9998456,0.000020259771,0.00004493061,0.000018357476,0.000041778614,0.000028935778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009152297,0.00013902334,0.00012269014,0.00055084156,0.00019757835,0.0003382276,0.00019285774,0.00028122077,0.0013127194],"category_scores_gemma":[0.00042712953,0.0001167195,0.00009503535,0.00045927486,0.00030011407,0.00024677036,0.0004233366,0.0003449518,0.00023192754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030638615,0.0000722698,0.81181943,0.00019012814,0.00010667683,0.0016663186,0.0013688677,0.0045157024,0.13508186,0.002442692,0.002585228,0.03984449],"study_design_scores_gemma":[0.000010337849,0.00006616732,0.9867444,0.00002272676,0.000027928969,0.00026334467,0.00023880179,0.0048249317,0.0046261246,0.0003303945,0.0028311505,0.000013835089],"about_ca_topic_score_codex":0.005645034,"about_ca_topic_score_gemma":0.007671317,"teacher_disagreement_score":0.005645034,"about_ca_system_score_codex":0.00028125884,"about_ca_system_score_gemma":0.00019484936,"threshold_uncertainty_score":0.0112243295},"labels":[],"label_agreement":null},{"id":"W3131359423","doi":"","title":"Along Strike Variation in Response to Tectonic Processes Within a Long Lived Accretionary Orogen, Coast Mountains, British Columbia","year":2007,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Tectonics; Variation (astronomy); Seismology","score_opus":0.01539586384212069,"score_gpt":0.22997817963593215,"score_spread":0.21458231579381146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3131359423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998814,0.000028842147,0.00001920107,0.000021735821,0.0000015010652,0.000003247351,0.0003012767,0.0000020430068,0.0008080738],"genre_scores_gemma":[0.9979358,0.00003731624,0.000038593935,0.000013516413,7.9971545e-7,0.0000034054403,0.00040290164,0.0000037618834,0.001563933],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997774,0.000030393003,0.000013113597,0.000057076024,0.00004252531,0.0000795224],"domain_scores_gemma":[0.9989907,0.0000993878,0.00014327274,0.000043530013,0.00052031403,0.00020280138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018294796,0.00016532393,0.00028541344,0.00093010865,0.0015705072,0.0011122089,0.0006377745,0.00031195398,0.0024693063],"category_scores_gemma":[0.0012719228,0.00019372471,0.0001225219,0.0022685425,0.00062603876,0.00024047335,0.00066078774,0.00036621004,0.0003473935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021915702,0.00005413137,0.9856295,0.000015570637,0.0000773186,0.00025077307,0.0030887825,0.0004889054,0.0024819481,0.00010182441,0.0008011146,0.0067910235],"study_design_scores_gemma":[0.0000014519471,0.0000047417566,0.9982268,0.0000032235625,0.000004590524,0.000017468014,0.0013641356,0.00011276223,0.000032086245,0.000008608407,0.00022165389,0.0000024712],"about_ca_topic_score_codex":0.95138586,"about_ca_topic_score_gemma":0.989892,"teacher_disagreement_score":0.048614144,"about_ca_system_score_codex":0.0050016227,"about_ca_system_score_gemma":0.00293324,"threshold_uncertainty_score":0.09780085},"labels":[],"label_agreement":null},{"id":"W3132228739","doi":"10.1785/0120200251","title":"A Study on the Largest Hydraulic Fracturing Induced Earthquake in Canada: Numerical Modeling and Triggering Mechanism","year":2021,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Poromechanics; Induced seismicity; Hydraulic fracturing; Geology; Fluid pressure; Pore water pressure; Seismology; Stress field; Permeability (electromagnetism); Geotechnical engineering; Stress (linguistics); Finite element method; Mechanics; Porosity; Structural engineering; Engineering; Porous medium","score_opus":0.029451365695022002,"score_gpt":0.21063859566012708,"score_spread":0.18118722996510508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3132228739","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946681,0.00007100589,0.0014778683,0.00010880663,0.000008886633,0.000024797688,0.00030577157,0.00006326921,0.0032715257],"genre_scores_gemma":[0.9979766,0.0000691398,0.0010503402,0.000010708005,0.000002821747,0.000009304484,0.00015517871,0.000007179244,0.00071870576],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999149,0.000008734216,0.000004029068,0.000015821763,0.00002166703,0.00003476162],"domain_scores_gemma":[0.99968123,0.00009960229,0.000049251397,0.000017327608,0.000093403476,0.000059250946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017688826,0.0005760023,0.00036832725,0.0006477911,0.0010448248,0.00085088634,0.0012814434,0.00090031844,0.0014608928],"category_scores_gemma":[0.00066960603,0.00029858662,0.0004909851,0.00071430404,0.00066701276,0.00026548078,0.00042905242,0.00051998714,0.00010233605],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008231399,0.0001556972,0.03531139,0.000051170002,0.000037132406,0.00050026976,0.00012338083,0.9544532,0.0036183947,0.0016909454,0.00052312156,0.0034529993],"study_design_scores_gemma":[0.0000143433745,0.000017009901,0.005458001,0.0000036626373,0.0000124562375,0.000013732108,0.000084604326,0.9937495,0.00038946245,0.00007275128,0.0001753263,0.000009072967],"about_ca_topic_score_codex":0.8556896,"about_ca_topic_score_gemma":0.7494412,"teacher_disagreement_score":0.14431041,"about_ca_system_score_codex":0.005207695,"about_ca_system_score_gemma":0.004870197,"threshold_uncertainty_score":0.29032052},"labels":[],"label_agreement":null},{"id":"W3134421644","doi":"10.1038/s41467-021-21596-4","title":"Caldera resurgence during the 2018 eruption of Sierra Negra volcano, Galápagos Islands","year":2021,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council; Jet Propulsion Laboratory; California Institute of Technology; Institut de Recherche pour le Développement; National Aeronautics and Space Administration; Sight Research UK; Tulane University; National Science Foundation","keywords":"Geology; Caldera; Volcano; Induced seismicity; Seismology; Magma; Subsidence; Geomorphology","score_opus":0.023370037777556356,"score_gpt":0.2638514232877663,"score_spread":0.24048138551020992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134421644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948933,0.00009277015,0.00008297579,0.00008599209,0.0000072523626,0.00000314702,0.0041584927,0.00003966366,0.0006364177],"genre_scores_gemma":[0.9916557,0.000085228,0.00015480704,0.000031663854,0.000022280725,0.000007681822,0.007743531,0.0000105529625,0.00028857045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998939,0.000017252074,0.0000062078034,0.00004295259,0.000016965485,0.00002275574],"domain_scores_gemma":[0.999747,0.000047213525,0.00007394116,0.000041343123,0.000041397172,0.00004917569],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023096058,0.00024438516,0.00020961511,0.00070144574,0.00021346989,0.00037676268,0.00026550406,0.00026392663,0.0007555543],"category_scores_gemma":[0.00076561247,0.00008162901,0.00015131496,0.00055029395,0.0002654866,0.00022203052,0.00062896323,0.00028060182,0.00015231554],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020459919,0.00004305294,0.97716457,0.000063375286,0.00012252566,0.00045456213,0.0006289604,0.0025532728,0.0032594877,0.00013038896,0.00426173,0.011113586],"study_design_scores_gemma":[0.000007625782,0.000009248031,0.9962752,0.000008031144,0.000013769097,0.00007698682,0.00019900537,0.0013384979,0.00014558448,0.000046092708,0.0018763251,0.0000035494204],"about_ca_topic_score_codex":0.025396781,"about_ca_topic_score_gemma":0.042915847,"teacher_disagreement_score":0.025396781,"about_ca_system_score_codex":0.00034365186,"about_ca_system_score_gemma":0.00019388842,"threshold_uncertainty_score":0.05049795},"labels":[],"label_agreement":null},{"id":"W3134730490","doi":"10.5194/egusphere-egu21-3600","title":"Deformation mechanisms in natural dolomite mylonites from a detachment system (Mt. Hymittos, Greece)","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of Ottawa","funders":"","keywords":"Geology; Mylonite; Cataclastic rock; Greenschist; Metamorphic rock; Dolomite; Metamorphic facies; Petrography; Deformation mechanism; Geochemistry; Detachment fault; Mineralogy; Petrology; Shear zone; Facies; Tectonics; Seismology; Geomorphology; Microstructure","score_opus":0.009864731636263023,"score_gpt":0.19428300288358136,"score_spread":0.18441827124731833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134730490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99954283,0.000031904186,0.000029903546,0.0000034653588,3.5053162e-7,0.000003191333,0.00008240186,0.0000032715343,0.0003026584],"genre_scores_gemma":[0.9994079,0.00003225332,0.00010472723,0.00000404913,6.9950244e-7,0.000005002755,0.00018074375,0.0000025673703,0.0002621005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998988,0.000005966156,0.000009585053,0.0000472905,0.000022863636,0.000015521206],"domain_scores_gemma":[0.999928,0.0000064461165,0.000034293807,0.000007681917,0.000014706322,0.000008927971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010132057,0.0002376176,0.00017118426,0.0011594396,0.00031749185,0.0003153551,0.00037045474,0.0002656213,0.0006266234],"category_scores_gemma":[0.0001805709,0.0002340653,0.00014721486,0.00078012806,0.00062422396,0.00015953118,0.00044512082,0.00010359725,0.00020173243],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021918592,0.000056350626,0.7333686,0.00012306325,0.00006375384,0.0008215464,0.00201758,0.0012801692,0.24968739,0.00017609817,0.00012395158,0.01206227],"study_design_scores_gemma":[0.0000056641275,0.00004610864,0.9971396,0.0000037882728,0.000006118999,0.00029393012,0.00031334293,0.00027860477,0.0015054834,0.000015743773,0.00038906172,0.0000026646862],"about_ca_topic_score_codex":0.013421056,"about_ca_topic_score_gemma":0.02917164,"teacher_disagreement_score":0.013421056,"about_ca_system_score_codex":0.0006415454,"about_ca_system_score_gemma":0.00024524037,"threshold_uncertainty_score":0.026685894},"labels":[],"label_agreement":null},{"id":"W3134982339","doi":"10.1029/2020jb020704","title":"Subducted Lithosphere Under South America From Multifrequency <i>P</i> Wave Tomography","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Engineering and Physical Sciences Research Council; Deutsche Forschungsgemeinschaft","keywords":"Geology; Subduction; Lithosphere; Seismology; Slab; Mantle (geology); Seismic tomography; Oceanic crust; Transition zone; Cretaceous; Paleontology; Geophysics; Tectonics","score_opus":0.05095324108111181,"score_gpt":0.29956878390270947,"score_spread":0.24861554282159765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3134982339","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953908,0.000059440492,0.0020824089,0.00012648848,0.0000030725341,0.000005759942,0.0009946163,0.00008853727,0.0012489222],"genre_scores_gemma":[0.9971111,0.00006433885,0.0014040881,0.000012226688,0.000003828986,0.000004656048,0.0011498636,0.000016610717,0.00023338496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995756,0.0000064839423,0.0000023307311,0.0000142612935,0.0000093208,0.0000100591],"domain_scores_gemma":[0.99990606,0.000014460547,0.000029925513,0.000013642227,0.00002533381,0.0000105281415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001148061,0.0003245528,0.00011010237,0.00055530126,0.00014605268,0.0005147093,0.00028020216,0.00022376195,0.0013705193],"category_scores_gemma":[0.00046105374,0.00016386328,0.00031400062,0.000947438,0.00019455417,0.00036435865,0.00047850836,0.00021023481,0.00012580353],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021449031,0.000059887843,0.6962168,0.00008928199,0.00024364861,0.0005123331,0.00041721063,0.18831706,0.039500684,0.0022216735,0.0018898791,0.07031693],"study_design_scores_gemma":[0.00007245451,0.000045990502,0.648227,0.000032416396,0.000109109744,0.00024244319,0.0004636483,0.3417137,0.004249534,0.0013050877,0.0035037936,0.000034845176],"about_ca_topic_score_codex":0.051347356,"about_ca_topic_score_gemma":0.05846525,"teacher_disagreement_score":0.051347356,"about_ca_system_score_codex":0.00040685904,"about_ca_system_score_gemma":0.00072683825,"threshold_uncertainty_score":0.102096915},"labels":[],"label_agreement":null},{"id":"W3135173011","doi":"10.82308/25049","title":"The mechanics of slip at the updip limit of the seismogenic zone","year":2020,"lang":"en","type":"article","venue":"eScholarship@McGill (McGill)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Geology; Slip (aerodynamics); Geotechnical engineering; Rock mechanics; Seismology; Engineering","score_opus":0.022927008807116383,"score_gpt":0.19338721845251244,"score_spread":0.17046020964539607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3135173011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99799985,0.00014413949,0.00041396994,0.000021533378,0.0000011710861,0.0000036593424,0.000037637845,0.000009263794,0.0013688055],"genre_scores_gemma":[0.9995297,0.000106807645,0.00010280901,0.0000025385727,0.0000015501151,0.0000022903996,0.000023396566,0.0000016529302,0.00022927097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999428,0.000005307675,0.000005725135,0.00001627451,0.00001467608,0.00001525304],"domain_scores_gemma":[0.999869,0.000020360152,0.00005515158,0.000016616743,0.00001955203,0.00001930087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010621414,0.00014017263,0.00016866336,0.0007334439,0.00029743425,0.000527676,0.00022751816,0.00017840137,0.0007873706],"category_scores_gemma":[0.00051600713,0.00018460935,0.00010496732,0.00033401194,0.00063531083,0.00042883406,0.00043648665,0.00013906113,0.00015422612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004776741,0.00008869676,0.72671103,0.00017703229,0.000084960455,0.0013658218,0.0016162097,0.03861556,0.16721918,0.008277349,0.00058066193,0.054785825],"study_design_scores_gemma":[0.000012814836,0.00010707324,0.9573431,0.000025325533,0.000021431115,0.00033818296,0.0006800572,0.032028478,0.00596972,0.002149371,0.001308635,0.000015732721],"about_ca_topic_score_codex":0.004169967,"about_ca_topic_score_gemma":0.004652181,"teacher_disagreement_score":0.004169967,"about_ca_system_score_codex":0.00051388354,"about_ca_system_score_gemma":0.0001703634,"threshold_uncertainty_score":0.008291423},"labels":[],"label_agreement":null},{"id":"W3135247652","doi":"","title":"Induced Seismicity in the United States and Canada III","year":2017,"lang":"en","type":"article","venue":"2017 AGU Fall Meeting","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology","score_opus":0.0313297634422144,"score_gpt":0.23398927558214322,"score_spread":0.20265951213992883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3135247652","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97968674,0.0004284771,0.000064077285,0.00096950686,0.000029848276,0.00003525953,0.007765073,0.00002403368,0.010997011],"genre_scores_gemma":[0.98962057,0.00046742902,0.00007684478,0.00021768399,0.000008251835,0.000014815686,0.0047312723,0.000010025732,0.0048531704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99954283,0.000025835026,0.000021151633,0.000041726147,0.00018860912,0.00017979744],"domain_scores_gemma":[0.9981495,0.00007434174,0.00014762837,0.000028265284,0.0011921786,0.00040808797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003391123,0.00025410892,0.00031563875,0.0016615142,0.0020107268,0.0017307164,0.00082623714,0.0005290966,0.0021089753],"category_scores_gemma":[0.0015232518,0.00020718478,0.00029429814,0.0039829225,0.0004834314,0.0003137989,0.0010530795,0.0007235304,0.0002446726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003127568,0.00011686066,0.9731372,0.000050284158,0.0001356673,0.00031656484,0.0013253483,0.0013940083,0.00059363665,0.0011582962,0.010094821,0.011364513],"study_design_scores_gemma":[0.0000133455205,0.000015055229,0.9936434,0.000019239831,0.000017223643,0.000026248896,0.00268485,0.00048304832,0.00011523913,0.00004279928,0.002929071,0.00001053921],"about_ca_topic_score_codex":0.99625176,"about_ca_topic_score_gemma":0.9984654,"teacher_disagreement_score":0.029703936,"about_ca_system_score_codex":0.029703936,"about_ca_system_score_gemma":0.040617708,"threshold_uncertainty_score":0.21551818},"labels":[],"label_agreement":null},{"id":"W3135830361","doi":"10.1038/s41467-020-20700-4","title":"Constraining maximum event magnitude during injection-triggered seismicity","year":2021,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Geothermal Technologies Office; U.S. Department of Energy","keywords":"Induced seismicity; Mechanics; Maximum magnitude; Geology; Slip (aerodynamics); Shear (geology); Magnitude (astronomy); Event (particle physics); Seismology; Physics; Petrology; Thermodynamics","score_opus":0.022102038612746018,"score_gpt":0.26460988953585246,"score_spread":0.24250785092310645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3135830361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9577121,0.00016478234,0.038950767,0.000031094016,0.00000770978,0.000022773005,0.0005807689,0.0002072779,0.0023226328],"genre_scores_gemma":[0.9957339,0.00002647975,0.0038536817,0.0000048877064,0.0000036984172,0.000014522872,0.0002912688,0.000014720025,0.00005682487],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981457,0.000034033128,0.000015876838,0.00007936777,0.000030492323,0.000025678288],"domain_scores_gemma":[0.9980647,0.0009844406,0.0005302908,0.00017953942,0.00014995875,0.0000910992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079125323,0.00019382317,0.00022981633,0.00081934634,0.00022277527,0.00048262498,0.00046773182,0.0003178195,0.00071906106],"category_scores_gemma":[0.003839327,0.00017275992,0.00016620067,0.00041242898,0.00028036034,0.0006142468,0.00046062656,0.00029538263,0.00012319165],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051897106,0.00013048691,0.64563566,0.0002106646,0.000115598705,0.0004763009,0.0005908347,0.12402962,0.14449105,0.006204287,0.0007916458,0.07680479],"study_design_scores_gemma":[0.000027372078,0.00031053196,0.7203913,0.00006512811,0.000052859526,0.00039955662,0.00021449348,0.21355648,0.056579888,0.0046073343,0.0037292705,0.000065711945],"about_ca_topic_score_codex":0.0014924798,"about_ca_topic_score_gemma":0.002560787,"teacher_disagreement_score":0.0014924798,"about_ca_system_score_codex":0.0003664697,"about_ca_system_score_gemma":0.00023578595,"threshold_uncertainty_score":0.0041846037},"labels":[],"label_agreement":null},{"id":"W3136095488","doi":"10.1002/essoar.10506521.1","title":"Comment on “Pressure-to-Depth Conversion Models for Metamorphic Rocks: Derivation and Applications”","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Preprint; Metamorphic rock; Geology; Space (punctuation); Geochemistry; Computer science; World Wide Web; Operating system","score_opus":0.03377666198137553,"score_gpt":0.2345735318277552,"score_spread":0.20079686984637968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3136095488","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0011899255,0.0018779711,0.0071219946,0.9611289,0.020415587,0.000027224472,0.0007058263,0.0003457113,0.0071869357],"genre_scores_gemma":[0.021322878,0.0010917311,0.006706595,0.94272083,0.0177558,0.00016790097,0.00028206914,0.00022242394,0.009729701],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99650735,0.00072559447,0.00040706625,0.0007431533,0.0013593393,0.00025741896],"domain_scores_gemma":[0.9831466,0.0076549742,0.0009793807,0.0010457394,0.006600647,0.0005727283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006510638,0.0011728727,0.00093926484,0.0009529341,0.0032507002,0.0029533976,0.0050661187,0.017767662,0.0069436477],"category_scores_gemma":[0.041876003,0.00089649286,0.0018491686,0.0012546452,0.005163994,0.006034749,0.0033858533,0.030474411,0.007296455],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066259585,0.000017967894,0.00052695326,0.00007330617,0.000018299439,0.0001412224,0.0003301423,0.00053452357,0.0003609196,0.042934217,0.94762266,0.0073734857],"study_design_scores_gemma":[0.00009307079,0.000051765004,0.0021582302,0.0002557062,0.000038877126,0.00041026555,0.0003591629,0.003414396,0.0014728474,0.1056095,0.8859739,0.00016213917],"about_ca_topic_score_codex":0.026342163,"about_ca_topic_score_gemma":0.014948091,"teacher_disagreement_score":0.026342163,"about_ca_system_score_codex":0.0027068085,"about_ca_system_score_gemma":0.0030056415,"threshold_uncertainty_score":0.05237764},"labels":[],"label_agreement":null},{"id":"W3136105354","doi":"10.1785/0120200360","title":"Earthquake Magnitudes from Dynamic Strain","year":2021,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Magnitude (astronomy); Seismology; Geodesy; Moment magnitude scale; Attenuation; Epicenter; Richter magnitude scale; Waveform; Seismic moment; Range (aeronautics); Fault (geology); Physics; Mathematics; Geometry; Scaling; Optics","score_opus":0.01356156782823233,"score_gpt":0.21029285594922145,"score_spread":0.1967312881209891,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3136105354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8481143,0.0006250379,0.018840957,0.00032521616,0.00020017594,0.00014038569,0.04011261,0.001971301,0.08967004],"genre_scores_gemma":[0.97829187,0.00020261572,0.0055718315,0.000071758775,0.000094517105,0.0000592153,0.011626718,0.00012714215,0.003954343],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999624,0.000037623315,0.00004610272,0.00008253588,0.0001786373,0.000031001],"domain_scores_gemma":[0.998257,0.00026168735,0.0005485969,0.0001994539,0.00054677867,0.00018645552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021627972,0.00047308055,0.0001612397,0.0031906278,0.00012397366,0.0008800971,0.00024931738,0.00025481344,0.011897957],"category_scores_gemma":[0.0029102918,0.00014737879,0.00015103242,0.0019851038,0.00027815346,0.00086339883,0.00096545595,0.000517233,0.0026366299],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036978882,0.00011385623,0.6489821,0.0005158957,0.0001643042,0.00020906306,0.0006917574,0.00935469,0.036827855,0.009202218,0.029368516,0.2641999],"study_design_scores_gemma":[0.000010822964,0.00012229788,0.9700816,0.00003938135,0.000013518452,0.00027901988,0.0004180704,0.0037876396,0.003367611,0.002176126,0.019669134,0.00003490911],"about_ca_topic_score_codex":0.001008826,"about_ca_topic_score_gemma":0.0022431135,"teacher_disagreement_score":0.011897957,"about_ca_system_score_codex":0.00027040413,"about_ca_system_score_gemma":0.00011456921,"threshold_uncertainty_score":0.03980261},"labels":[],"label_agreement":null},{"id":"W3136151827","doi":"10.1029/2020tc006509","title":"Late Quaternary Intraplate Deformation Defined by the Las Chacras Fault Zone, West‐Central Argentina","year":2021,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Intraplate earthquake; Seismology; Quaternary; Slip (aerodynamics); Subduction; Fault (geology); Geodetic datum; Geodesy; Tectonics; Paleontology","score_opus":0.01309617828171194,"score_gpt":0.2070899929530599,"score_spread":0.19399381467134796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3136151827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9904654,0.0003696246,0.00015837797,0.000055270455,0.000009060784,0.000016457781,0.0011384843,0.000040022456,0.0077472143],"genre_scores_gemma":[0.9979551,0.00013281513,0.00026130053,0.0000068196987,0.000007958754,0.000015712847,0.00087075547,0.0000037470427,0.0007458031],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990475,0.00001081152,0.0000065322956,0.000033217264,0.000023231842,0.000021447127],"domain_scores_gemma":[0.99974555,0.000024380895,0.00010819643,0.0000129773625,0.00007613223,0.000032677992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016338663,0.0002481889,0.00018259366,0.0009467969,0.00031500775,0.00052418973,0.00016341858,0.00019373655,0.0012183975],"category_scores_gemma":[0.00034289146,0.00008036296,0.00008340493,0.00076718495,0.00022521504,0.00012481917,0.00019235235,0.0001139771,0.00022763252],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030066777,0.00006969264,0.9571845,0.00007630371,0.000040665087,0.00020867983,0.0004976267,0.0010456544,0.012348,0.0005053962,0.0017619028,0.025961006],"study_design_scores_gemma":[0.000007351316,0.000015961466,0.99795735,0.0000074998547,0.0000047463036,0.000038906153,0.0000886265,0.0004088827,0.00020368093,0.00001999698,0.0012455195,0.0000014335321],"about_ca_topic_score_codex":0.08774652,"about_ca_topic_score_gemma":0.13223287,"teacher_disagreement_score":0.08774652,"about_ca_system_score_codex":0.00092156266,"about_ca_system_score_gemma":0.0003041629,"threshold_uncertainty_score":0.17447156},"labels":[],"label_agreement":null},{"id":"W3136774598","doi":"","title":"Characterizing the Dynamic Upper Mantle Using Multidisciplinary Approaches I","year":2020,"lang":"en","type":"article","venue":"AGU Fall Meeting 2020","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Multidisciplinary approach","score_opus":0.05253427562235849,"score_gpt":0.23651070894948162,"score_spread":0.18397643332712313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3136774598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.83544326,0.0021042193,0.14463566,0.00087759615,0.000066013585,0.00006635081,0.0011936184,0.00027700645,0.0153363],"genre_scores_gemma":[0.96722835,0.00038059676,0.03106227,0.000059599603,0.000030466721,0.00003121097,0.00049428485,0.000046142526,0.0006670693],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99984133,0.00003660559,0.000009814328,0.000056071618,0.000028152048,0.00002806605],"domain_scores_gemma":[0.9997981,0.00007606612,0.000039620136,0.00003107472,0.000032432385,0.000022734752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047202915,0.00050007674,0.00031852568,0.001426474,0.00047589128,0.0024203171,0.000602,0.0007925184,0.0013063095],"category_scores_gemma":[0.0012777561,0.0003451892,0.00086671865,0.001122954,0.00042295095,0.0015992732,0.0015619886,0.00065171125,0.00021133352],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024743282,0.0002250784,0.14940654,0.00029000916,0.0009076786,0.0002837221,0.00058655214,0.5744278,0.10014019,0.019093223,0.001543582,0.15284818],"study_design_scores_gemma":[0.000018266184,0.00004686711,0.06919629,0.000052410836,0.00014613845,0.000094673705,0.00068923866,0.90256405,0.0069649117,0.016326683,0.0038529027,0.000047554473],"about_ca_topic_score_codex":0.006928165,"about_ca_topic_score_gemma":0.0072461804,"teacher_disagreement_score":0.006928165,"about_ca_system_score_codex":0.00068703125,"about_ca_system_score_gemma":0.00043845977,"threshold_uncertainty_score":0.013775706},"labels":[],"label_agreement":null},{"id":"W3137159392","doi":"","title":"Canada-United States Elevation Model Collaboration to Improve Tsunami Inundation Mapping","year":2020,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Ocean Networks Canada Society; University of Victoria; Memorial University of Newfoundland","funders":"","keywords":"Elevation (ballistics); Digital elevation model; Geology; Geography; Remote sensing; Engineering","score_opus":0.020703746730646126,"score_gpt":0.2156071759556022,"score_spread":0.19490342922495607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137159392","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15733388,0.0015161271,0.0901058,0.019674955,0.0023579372,0.0011143604,0.481186,0.020383168,0.22632782],"genre_scores_gemma":[0.4560429,0.0017689404,0.24043754,0.0022260456,0.00017348773,0.00070103706,0.23554821,0.0061293426,0.05697249],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984017,0.00015749675,0.000083080085,0.0001615227,0.0008444947,0.0003517569],"domain_scores_gemma":[0.988536,0.00034908057,0.00013751778,0.0006881091,0.009734138,0.0005550625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001732741,0.00081119273,0.00078714895,0.003503873,0.0031399347,0.0026560149,0.0018419395,0.0005871195,0.015704593],"category_scores_gemma":[0.007898517,0.00043634605,0.0007351044,0.008789484,0.00029354042,0.0014414438,0.0022537755,0.0012115164,0.003451868],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002887831,0.00025038928,0.0675855,0.00016881253,0.0002900287,0.00021958591,0.0006875455,0.031690355,0.0035663103,0.0130027,0.68998986,0.19226009],"study_design_scores_gemma":[0.00035654192,0.000036286674,0.13949634,0.00028563273,0.0004314522,0.000115506366,0.0027449187,0.17287757,0.008783998,0.005183281,0.6694982,0.00019032233],"about_ca_topic_score_codex":0.9900686,"about_ca_topic_score_gemma":0.9951994,"teacher_disagreement_score":0.015889883,"about_ca_system_score_codex":0.015889883,"about_ca_system_score_gemma":0.069601804,"threshold_uncertainty_score":0.11528969},"labels":[],"label_agreement":null},{"id":"W3137245372","doi":"10.1139/cjes-2020-0129","title":"Geological correlation between northern Cyprus and southern Anatolia","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Nappe; Transtension; Flysch; Subduction; Paleontology; Cenozoic; Andesites; Seismology; Cretaceous; Structural basin; Tectonics; Andesite; Volcanic rock; Volcano; Rift","score_opus":0.02745108023917584,"score_gpt":0.21314802915670758,"score_spread":0.18569694891753175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137245372","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98978126,0.00044654324,0.00010422883,0.000087086366,0.000006755062,0.0000050930976,0.0003556746,0.000012804242,0.00920054],"genre_scores_gemma":[0.99831414,0.00020283362,0.00014177054,0.000010905419,0.0000071064765,0.000004285286,0.00035044452,0.0000035252187,0.0009648936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989414,0.0000139879285,0.000012233414,0.00004035493,0.000017200231,0.000022092125],"domain_scores_gemma":[0.99971086,0.000030693172,0.00016221614,0.000017690996,0.000054531673,0.000023897144],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007133026,0.00009176845,0.00008877362,0.00126029,0.00037692452,0.00047824276,0.00011854017,0.00007640555,0.0027118614],"category_scores_gemma":[0.00023176198,0.00006995024,0.00008011527,0.0014247891,0.0003329434,0.00016378424,0.00027727996,0.00009291971,0.00026846904],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053137974,0.000013455451,0.9710099,0.000040206818,0.000042537227,0.00046588044,0.0008507235,0.00021869356,0.003942276,0.0014354277,0.0007672625,0.021160647],"study_design_scores_gemma":[5.361323e-7,0.0000019306347,0.99807054,0.0000058100973,0.00000406886,0.000118520395,0.00020784399,0.00005092465,0.0000656655,0.00002336308,0.0014497947,9.4800936e-7],"about_ca_topic_score_codex":0.03450464,"about_ca_topic_score_gemma":0.07615019,"teacher_disagreement_score":0.03450464,"about_ca_system_score_codex":0.0005955813,"about_ca_system_score_gemma":0.0004716237,"threshold_uncertainty_score":0.06860763},"labels":[],"label_agreement":null},{"id":"W3137298505","doi":"10.1029/2021jb022797","title":"The 2019–2020 Khalili (Iran) Earthquake Sequence—Anthropogenic Seismicity in the Zagros Simply Folded Belt?","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft; Iran National Science Foundation; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Universidad de Granada; Canada Foundation for Innovation","keywords":"Geology; Induced seismicity; Seismology; Aftershock; Hypocenter; Sequence (biology); Interferometric synthetic aperture radar; Seismic hazard; Synthetic aperture radar","score_opus":0.07053006481328974,"score_gpt":0.3498190958265939,"score_spread":0.27928903101330416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137298505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956816,0.000027959602,0.00003762577,0.00003744507,0.0000023011853,0.0000014919235,0.000058495367,0.0000024467624,0.0002640298],"genre_scores_gemma":[0.9996674,0.000025296742,0.000052679563,0.000009623075,0.000006028459,0.0000010804723,0.0001580047,7.7023117e-7,0.000079001795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999298,0.0000064222527,0.0000050064564,0.00001934771,0.000014445425,0.000024972314],"domain_scores_gemma":[0.9998178,0.000011415505,0.0001047538,0.0000120786735,0.000026241352,0.00002771491],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014564104,0.00011860484,0.00011434863,0.0004804465,0.00023858219,0.00038720158,0.00019853524,0.00023627453,0.0008070259],"category_scores_gemma":[0.0002710652,0.000082599334,0.00012254633,0.00057301746,0.00027128236,0.00023944314,0.00020693622,0.00016102692,0.00017651575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060195216,0.000026670863,0.9917902,0.0000097425145,0.000019350338,0.0002493966,0.0001736663,0.0004591016,0.001717126,0.0001327844,0.00016845738,0.0051933583],"study_design_scores_gemma":[0.0000021796827,0.000015252241,0.9988287,0.000002409849,0.0000050119156,0.00006299538,0.00022817386,0.00056124397,0.00007999068,0.000023755952,0.00018876558,0.0000015961232],"about_ca_topic_score_codex":0.017201021,"about_ca_topic_score_gemma":0.027414104,"teacher_disagreement_score":0.017201021,"about_ca_system_score_codex":0.0004670034,"about_ca_system_score_gemma":0.0003524218,"threshold_uncertainty_score":0.03420174},"labels":[],"label_agreement":null},{"id":"W3137331275","doi":"","title":"A Comparison of the Crustal Deformation Predicted by Glacial Isostatic Adjustment to Seismicity in the Baffin Region of Northern Canada","year":2016,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Post-glacial rebound; Geology; Induced seismicity; Glacial period; Deformation (meteorology); Seismology; Geomorphology; Oceanography","score_opus":0.016704876650260356,"score_gpt":0.2213244614988612,"score_spread":0.20461958484860085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137331275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99529296,0.00029702054,0.00008636605,0.00018876245,0.0000062679574,0.00000613727,0.00087300106,0.00001608737,0.003233271],"genre_scores_gemma":[0.99853444,0.00014400492,0.000070631795,0.000019282608,0.0000014523074,0.0000021671988,0.00050734956,0.0000061759238,0.0007144582],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996278,0.000033501092,0.000020638145,0.00008104083,0.00009222923,0.00014478884],"domain_scores_gemma":[0.9992066,0.00008516382,0.00005910106,0.000032402626,0.0004746624,0.00014209608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044954228,0.0002879468,0.00030494542,0.0015021624,0.0018643333,0.001903385,0.0009345582,0.0005704943,0.0025067972],"category_scores_gemma":[0.002282852,0.00033586958,0.00046871864,0.0022633323,0.0009007328,0.0003372398,0.00060240924,0.0003915734,0.00026993532],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043239808,0.00004513884,0.95011455,0.000080108126,0.0002499201,0.00032304347,0.0021606113,0.023235109,0.0028898641,0.001743117,0.0018068862,0.016919281],"study_design_scores_gemma":[0.0000130134395,0.000008316283,0.99347645,0.000016144782,0.000022099777,0.00002756559,0.0009413044,0.0038999,0.00012890926,0.00007980462,0.0013695343,0.00001695991],"about_ca_topic_score_codex":0.9962655,"about_ca_topic_score_gemma":0.997207,"teacher_disagreement_score":0.028769234,"about_ca_system_score_codex":0.028769234,"about_ca_system_score_gemma":0.021516934,"threshold_uncertainty_score":0.20873636},"labels":[],"label_agreement":null},{"id":"W3137982435","doi":"10.1029/2020jb021362","title":"Spatiotemporal Analysis of Seismotectonic State of Injection‐Induced Seismicity Clusters in the Western Canada Sedimentary Basin","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Induced seismicity; Seismology; Geology; Hydraulic fracturing; Magnitude (astronomy); Structural basin; Geotechnical engineering; Geomorphology","score_opus":0.03942951640531647,"score_gpt":0.30536418143706945,"score_spread":0.265934665031753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137982435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99875796,0.000028504743,0.00016070591,0.000018068624,8.11177e-7,0.000006587496,0.0005507039,0.000007971692,0.00046869868],"genre_scores_gemma":[0.9991616,0.000024450152,0.0000942805,0.000002221013,6.357558e-7,0.0000030227761,0.0005130006,0.0000013256697,0.00019956307],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985814,0.000009827465,0.000007018444,0.000028193683,0.000050065868,0.000046777383],"domain_scores_gemma":[0.9993155,0.000060880455,0.00015285535,0.000025949514,0.00031191533,0.00013299265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014933532,0.00014738848,0.0002015269,0.0016685994,0.0005822473,0.0006174063,0.00034467602,0.00014571994,0.0008310984],"category_scores_gemma":[0.00092522346,0.00012907677,0.00015819875,0.0023527348,0.00045214384,0.00012330213,0.00041484134,0.00017345481,0.00008307788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019006088,0.000049257036,0.9712436,0.000036141537,0.0001223414,0.00023712566,0.0011019908,0.0063805073,0.0070967753,0.00036187063,0.0007465301,0.012433676],"study_design_scores_gemma":[0.0000018071468,0.0000066492285,0.9959241,0.000003867941,0.000008552945,0.000012486485,0.00035798099,0.0032537102,0.00018254435,0.000017497796,0.0002256617,0.0000051300563],"about_ca_topic_score_codex":0.9307181,"about_ca_topic_score_gemma":0.9481422,"teacher_disagreement_score":0.069281876,"about_ca_system_score_codex":0.0038778032,"about_ca_system_score_gemma":0.0031828862,"threshold_uncertainty_score":0.13937974},"labels":[],"label_agreement":null},{"id":"W3138307258","doi":"10.4133/sageep.32-058","title":"UPPER CRUSTAL STRUCTURE OF THE BELLINGHAM BASIN FROM GRAVITY AND AEROMAGNETIC DATA","year":2019,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Structural basin; Geodesy; Paleontology","score_opus":0.012945117660995598,"score_gpt":0.1974306041916677,"score_spread":0.1844854865306721,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138307258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967141,0.00015573329,0.0003132875,0.00006302319,0.0000025204563,0.000009390476,0.00068486715,0.000026395634,0.0020307442],"genre_scores_gemma":[0.99750715,0.00012663659,0.0010417175,0.000015522963,0.000002249557,0.0000067953806,0.000911487,0.000005070016,0.00038340612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999118,0.000010001943,0.0000051243755,0.000026041973,0.000024043326,0.000022943615],"domain_scores_gemma":[0.999845,0.00002385285,0.000027907694,0.000015306878,0.00005792251,0.000029983246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011525923,0.00020511678,0.00013118082,0.0012159118,0.00045642685,0.00096687954,0.00030200413,0.00019399569,0.0014210065],"category_scores_gemma":[0.0007983266,0.00019183694,0.00013613133,0.0011966827,0.00017506888,0.00045871284,0.00059509533,0.00019172924,0.0001383096],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059160317,0.0000540501,0.9095631,0.000065048545,0.00008554647,0.0003640353,0.0010884377,0.016737752,0.003774945,0.0010024643,0.001965879,0.06523955],"study_design_scores_gemma":[0.000007456706,0.0000105758945,0.96119165,0.000040667903,0.000028861083,0.000047583155,0.00091750425,0.03317056,0.00068978133,0.0003054185,0.0035691436,0.000020811303],"about_ca_topic_score_codex":0.6240055,"about_ca_topic_score_gemma":0.8045346,"teacher_disagreement_score":0.6240055,"about_ca_system_score_codex":0.0017259537,"about_ca_system_score_gemma":0.0013458034,"threshold_uncertainty_score":0.75641763},"labels":[],"label_agreement":null},{"id":"W3138313841","doi":"10.1098/rsta.2020.0129","title":"Fracture mechanics of rate-and-state faults and fluid injection induced slip","year":2021,"lang":"en","type":"article","venue":"Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slip (aerodynamics); Fracture mechanics; Mechanics; Slip ratio; Physics; Materials science; Thermodynamics; Shear stress","score_opus":0.017407531268551327,"score_gpt":0.21482745885357873,"score_spread":0.1974199275850274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138313841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92156863,0.00062293705,0.07071216,0.00033276962,0.000028086153,0.00002006641,0.000088903354,0.000104059254,0.0065223533],"genre_scores_gemma":[0.99781066,0.00009322524,0.0011918084,0.00001076686,0.000005742999,0.0000062572253,0.000014129414,0.00000752127,0.00085993716],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99990976,0.000012962251,0.000005655087,0.000016751826,0.000032395907,0.000022537295],"domain_scores_gemma":[0.9997842,0.000058463444,0.00008042029,0.000020614301,0.00002680074,0.000029468085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001725217,0.0002202432,0.0002482353,0.0004783937,0.00023908907,0.00066072855,0.00045971,0.00077138434,0.00084249617],"category_scores_gemma":[0.0008257153,0.0001698865,0.00029082858,0.00019855227,0.0008145102,0.0006976876,0.0005244871,0.00045902995,0.000104066254],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016438786,0.00012126798,0.01284065,0.00010158849,0.000038602317,0.0011865278,0.0004894072,0.6402331,0.09883897,0.22449258,0.00074994867,0.020743057],"study_design_scores_gemma":[0.000011222328,0.00005856518,0.005367564,0.000010973387,0.0000070642786,0.00033444894,0.00007279427,0.962462,0.006415779,0.024661249,0.00057649985,0.000021822021],"about_ca_topic_score_codex":0.0019453486,"about_ca_topic_score_gemma":0.00080752163,"teacher_disagreement_score":0.0019453486,"about_ca_system_score_codex":0.00084142835,"about_ca_system_score_gemma":0.0002687561,"threshold_uncertainty_score":0.0061050057},"labels":[],"label_agreement":null},{"id":"W3138758102","doi":"10.1002/essoar.10504862.2","title":"Benchmarking Scenario Performance in the First Generation Canadian Seismic Risk Assessment","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; Geological Survey of Canada","funders":"","keywords":"Benchmarking; Computer science; World Wide Web; Business","score_opus":0.02665157626909525,"score_gpt":0.2064773236837278,"score_spread":0.17982574741463253,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138758102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91660595,0.00085810554,0.023363318,0.001798181,0.00015714818,0.00041251606,0.02116496,0.0022779098,0.033361927],"genre_scores_gemma":[0.9667099,0.000309683,0.015361471,0.00014017563,0.000012004508,0.000063611435,0.015607865,0.00014085961,0.0016544148],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99840075,0.0003857083,0.00007262971,0.00036176245,0.0004924482,0.00028666822],"domain_scores_gemma":[0.996876,0.0006899216,0.00013951035,0.00039607572,0.0016465567,0.00025191598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0034829692,0.0015880028,0.0005475659,0.0016509214,0.0013110889,0.0019459903,0.002806345,0.000973343,0.0018578157],"category_scores_gemma":[0.007933789,0.00046066407,0.0011027172,0.0022360606,0.00090888835,0.0014220855,0.001316991,0.0011060891,0.0003006261],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020502802,0.00008473568,0.017609827,0.00007022363,0.00014060439,0.000077513214,0.000072619,0.9633512,0.0005356982,0.0021149607,0.004117579,0.011620021],"study_design_scores_gemma":[0.00008513456,0.000109304834,0.024364963,0.00003416372,0.0000633928,0.000038711383,0.00028300783,0.9657478,0.0018288877,0.0016554311,0.005692754,0.00009653469],"about_ca_topic_score_codex":0.9524038,"about_ca_topic_score_gemma":0.95360744,"teacher_disagreement_score":0.047596216,"about_ca_system_score_codex":0.0223618,"about_ca_system_score_gemma":0.016091486,"threshold_uncertainty_score":0.162247},"labels":[],"label_agreement":null},{"id":"W3138835398","doi":"10.2139/ssrn.3498662","title":"The Riddle of the Great Chilean Earthquake","year":2019,"lang":"en","type":"article","venue":"SSRN Electronic Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Seismology; Geography; History; Geology","score_opus":0.006320104104601003,"score_gpt":0.18533790282399001,"score_spread":0.179017798719389,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138835398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47485656,0.012557714,0.0006923398,0.17422102,0.0011916364,0.000034087123,0.0012574305,0.000091403526,0.3350978],"genre_scores_gemma":[0.95801586,0.0028714882,0.00009250088,0.0029291343,0.0005775233,0.000008945861,0.00016650841,0.000050274688,0.03528779],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9997385,0.000081026075,0.000009747682,0.00003673625,0.000051720326,0.0000821786],"domain_scores_gemma":[0.9991804,0.0001781204,0.00012077382,0.00010974852,0.00020779096,0.00020315468],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075187394,0.00015454777,0.00024025771,0.00063435186,0.0017624662,0.0037596212,0.0004902593,0.0011540414,0.012784812],"category_scores_gemma":[0.005879792,0.00016968139,0.000117730444,0.0008724158,0.0025799077,0.0023099938,0.0028288055,0.0014223448,0.0014163244],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010899365,0.00011251993,0.11360546,0.0014151317,0.00022855484,0.006533097,0.042225935,0.004107854,0.005792207,0.348806,0.2516275,0.22445588],"study_design_scores_gemma":[0.000071543975,0.0000765903,0.24812569,0.0007434868,0.00005480703,0.000985565,0.037139907,0.0009533231,0.0006349605,0.08224565,0.62885624,0.000112211936],"about_ca_topic_score_codex":0.049745616,"about_ca_topic_score_gemma":0.057794213,"teacher_disagreement_score":0.049745616,"about_ca_system_score_codex":0.0028085343,"about_ca_system_score_gemma":0.0027452724,"threshold_uncertainty_score":0.09891212},"labels":[],"label_agreement":null},{"id":"W3139198649","doi":"10.1139/cjes-2020-0157","title":"Seismic <i>b</i> value within the Montney play of northeastern British Columbia, Canada","year":2021,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Stantec (Canada); Geoscience BC","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Canadian Association of Petroleum Producers; BC Oil and Gas Research and Innovation Society","keywords":"Geology; Induced seismicity; Seismology; Magnitude (astronomy)","score_opus":0.01163446508151713,"score_gpt":0.17667000219846374,"score_spread":0.1650355371169466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3139198649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9776863,0.00066305423,0.0002396493,0.00043362365,0.000014491291,0.000041130003,0.0069725504,0.00004483718,0.013904458],"genre_scores_gemma":[0.99075466,0.0004346598,0.00034946605,0.00008584247,0.0000041730705,0.000019657436,0.0027590364,0.000015151156,0.0055773915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996278,0.00001713946,0.000020799356,0.000077658726,0.00011513941,0.0001414058],"domain_scores_gemma":[0.9986388,0.00005895312,0.0001287861,0.000041007897,0.00086070586,0.00027173138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018157644,0.00034920083,0.0002936619,0.002457627,0.0028905594,0.0016548038,0.0008680563,0.00030373372,0.0041317306],"category_scores_gemma":[0.0010521103,0.00021895739,0.00020329648,0.004685001,0.0008736157,0.00032330578,0.0008002166,0.00040133466,0.00042333556],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000944073,0.000045702353,0.9510332,0.00011758795,0.000117539515,0.0006067908,0.002459796,0.0009828792,0.0031413166,0.00054698926,0.009149258,0.031704556],"study_design_scores_gemma":[0.0000025725196,0.0000045410156,0.99250925,0.000031497726,0.000015303554,0.000055450197,0.0033796339,0.0003432125,0.00014274775,0.000028692522,0.0034744586,0.000012542463],"about_ca_topic_score_codex":0.9974337,"about_ca_topic_score_gemma":0.999423,"teacher_disagreement_score":0.020842524,"about_ca_system_score_codex":0.020842524,"about_ca_system_score_gemma":0.019436343,"threshold_uncertainty_score":0.15122378},"labels":[],"label_agreement":null},{"id":"W3139255971","doi":"10.1146/annurev-earth-063016-015810","title":"Submarine Landslides and Their Tsunami Hazard","year":2021,"lang":"en","type":"article","venue":"Annual Review of Earth and Planetary Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"British Geological Survey; Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Submarine landslide; Landslide; Geology; Submarine pipeline; Seismology; Context (archaeology); Hazard; New guinea; Submarine; Oceanography; Paleontology; History","score_opus":0.01668253132885184,"score_gpt":0.22964773432979124,"score_spread":0.2129652030009394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3139255971","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.003598383,0.9923524,0.0003562919,0.0004042714,0.000176666,0.0000073542974,0.0000844837,0.000008601703,0.0030115333],"genre_scores_gemma":[0.015723744,0.98255473,0.00025518186,0.00017376784,0.0001755029,0.0000070821216,0.000084391395,0.0000023932278,0.001023327],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99984765,0.000022575388,0.000027651242,0.00003041979,0.00005169594,0.000019927556],"domain_scores_gemma":[0.9998337,0.00005700662,0.000046302317,0.0000044600865,0.000047109042,0.000011462529],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002502304,0.0006007087,0.0005954783,0.000815786,0.0002187018,0.0010468449,0.00039966774,0.000590595,0.0017662487],"category_scores_gemma":[0.00043758794,0.00017710784,0.00044937135,0.0010416717,0.00027793422,0.0009038411,0.00033729267,0.0006643998,0.00051749364],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015134436,0.00006516824,0.0062567187,0.03175799,0.00038349422,0.001247514,0.0013050439,0.002520367,0.008570306,0.010325462,0.018925156,0.91849136],"study_design_scores_gemma":[0.000010461235,0.00024506892,0.01950041,0.00506144,0.00043151286,0.0024322965,0.0010230277,0.00037111173,0.0026952121,0.0053958455,0.96278685,0.000046779583],"about_ca_topic_score_codex":0.0044264067,"about_ca_topic_score_gemma":0.0051186006,"teacher_disagreement_score":0.0044264067,"about_ca_system_score_codex":0.0004385568,"about_ca_system_score_gemma":0.001029289,"threshold_uncertainty_score":0.008801281},"labels":[],"label_agreement":null},{"id":"W3139395088","doi":"10.1029/2020jb021196","title":"The Role of Fluid Pressure‐Induced Aseismic Slip in Earthquake Cycle Modulation","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hudbay Minerals (Canada); Earthgen; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Ontario; University of Toronto; University of Michigan","keywords":"Induced seismicity; Seismology; Geology; Slip (aerodynamics); Perturbation (astronomy); Pore water pressure; Fluid pressure; Seismic hazard; Mechanics; Geotechnical engineering; Engineering; Physics","score_opus":0.029767459126492545,"score_gpt":0.30267881408545033,"score_spread":0.2729113549589578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3139395088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957521,0.00010992639,0.0030142434,0.00005262719,0.0000049740415,0.0000060879743,0.000051385734,0.000026676318,0.0009820476],"genre_scores_gemma":[0.9998344,0.000022623539,0.00009804657,0.0000015337041,8.1307724e-7,0.0000013103063,0.000006003395,0.0000010534351,0.000034109904],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999461,0.000014760051,0.0000043793502,0.000011201207,0.000010492257,0.000013049299],"domain_scores_gemma":[0.9997004,0.00012725402,0.00009017063,0.000022066097,0.000024808443,0.000035251636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001446512,0.00017828116,0.00019225609,0.00022543375,0.00015143029,0.0004922774,0.000240037,0.00028697908,0.00073830225],"category_scores_gemma":[0.0009853547,0.00012494755,0.0001574256,0.00014577845,0.0003949834,0.00038733392,0.0003373261,0.00018219855,0.00007348419],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059988187,0.000274017,0.08546816,0.00015747274,0.0000968829,0.00092477165,0.00022209215,0.57554656,0.31223926,0.005425157,0.00029675072,0.018749107],"study_design_scores_gemma":[0.000016744512,0.00016651444,0.055745985,0.000009163676,0.000022991233,0.000096007076,0.00008321352,0.9295898,0.012746618,0.0011441428,0.000360115,0.000018688283],"about_ca_topic_score_codex":0.0018678743,"about_ca_topic_score_gemma":0.00087790226,"teacher_disagreement_score":0.0018678743,"about_ca_system_score_codex":0.00030761078,"about_ca_system_score_gemma":0.00029293544,"threshold_uncertainty_score":0.003714025},"labels":[],"label_agreement":null},{"id":"W3140476314","doi":"10.1111/jpg.12783","title":"THE ROLE OF MULTIPLE WEAK LITHOLOGIES IN THE DEFORMATION OF COVER UNITS IN THE NORTHWESTERN SEGMENT OF THE ZAGROS FOLD‐AND‐THRUST BELT","year":2021,"lang":"en","type":"article","venue":"Journal of Petroleum Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Fold (higher-order function); Décollement; Fold and thrust belt; Lithology; Evaporite; Outcrop; Sedimentary rock; Marl; Imbrication; Stratigraphy; Paleontology; Thrust fault; Geomorphology; Petrology; Structural basin; Tectonics; Foreland basin","score_opus":0.012342188173146031,"score_gpt":0.2048014191881404,"score_spread":0.19245923101499438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3140476314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99957377,0.00004713544,0.000018267097,0.0000062554423,4.7131616e-7,0.0000010773194,0.000041923126,9.251714e-7,0.0003101951],"genre_scores_gemma":[0.99974185,0.00003619443,0.000038838218,0.000002319462,0.0000015145165,8.068652e-7,0.000077312565,5.6929997e-7,0.00010048105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998926,0.000009658382,0.000014150769,0.000026270987,0.000022007871,0.000035188106],"domain_scores_gemma":[0.9998203,0.000021927364,0.000098700206,0.000011812974,0.000020049716,0.00002726665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012300067,0.00019035324,0.00014576218,0.0014052077,0.0003479276,0.00069104315,0.00019673018,0.00017054885,0.00073695614],"category_scores_gemma":[0.00031020536,0.0001317738,0.0001332311,0.0010601691,0.00048817394,0.00028988434,0.00043424516,0.00010350117,0.00015759487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007018042,0.000016291526,0.9845158,0.000016482589,0.00001999644,0.00024504628,0.000636602,0.00033148754,0.005102215,0.000118400836,0.000037375983,0.0088901725],"study_design_scores_gemma":[7.658406e-7,0.0000064186734,0.9995622,0.0000022515187,0.0000026679093,0.00002882161,0.00019953478,0.000090046546,0.000044308283,0.0000076427,0.00005433239,8.444154e-7],"about_ca_topic_score_codex":0.024510125,"about_ca_topic_score_gemma":0.051923927,"teacher_disagreement_score":0.024510125,"about_ca_system_score_codex":0.00049886055,"about_ca_system_score_gemma":0.00031102772,"threshold_uncertainty_score":0.048734903},"labels":[],"label_agreement":null},{"id":"W3144132217","doi":"10.1016/j.jog.2021.101843","title":"Inversion for the static friction coefficient of seismogenic faults: Application to induced seismicity of the Basel Enhanced Geothermal System, Switzerland","year":2021,"lang":"en","type":"article","venue":"Journal of Geodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Geology; Geothermal gradient; Induced seismicity; Hydrostatic equilibrium; Fault (geology); Seismology; Microseism; Geomechanics; Petrology; Geophysics; Geotechnical engineering","score_opus":0.009130609514607245,"score_gpt":0.21306216570900338,"score_spread":0.20393155619439612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3144132217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96851724,0.00018636565,0.028797107,0.00010642416,0.000022714115,0.000021350254,0.0005333274,0.00050944794,0.0013060543],"genre_scores_gemma":[0.9937465,0.00005621498,0.005423343,0.000006236163,0.000009033631,0.000009427485,0.0002940231,0.00004236742,0.00041290186],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992836,0.000019658737,0.0000044551985,0.000016005702,0.00001369142,0.000017838816],"domain_scores_gemma":[0.9996344,0.00020755395,0.00003456983,0.000025796939,0.00007577704,0.000021928663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031292177,0.00061314134,0.00034027442,0.0007261944,0.00023028639,0.00049442553,0.0005647016,0.0006433848,0.001522937],"category_scores_gemma":[0.001502084,0.00034354784,0.00030571013,0.00068527315,0.00019593476,0.0004004477,0.0003275,0.00034378996,0.0002615484],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000636416,0.00024186676,0.03412166,0.00020379793,0.000139238,0.00045320924,0.00024511068,0.83341616,0.058536705,0.0010653817,0.0009896357,0.069950774],"study_design_scores_gemma":[0.00005424886,0.000040175622,0.013402735,0.000008134322,0.000016173592,0.000019229763,0.00004431186,0.98314303,0.0029106056,0.00014810666,0.00020080263,0.000012368302],"about_ca_topic_score_codex":0.041795466,"about_ca_topic_score_gemma":0.0505254,"teacher_disagreement_score":0.041795466,"about_ca_system_score_codex":0.00031933998,"about_ca_system_score_gemma":0.0010347343,"threshold_uncertainty_score":0.08310437},"labels":[],"label_agreement":null},{"id":"W3144140569","doi":"10.1038/s41467-021-26961-x","title":"Fluid-injection-induced earthquakes characterized by hybrid-frequency waveforms manifest the transition from aseismic to seismic slip","year":2021,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Victoria; Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Slip (aerodynamics); Geology; Waveform; San andreas fault; Slow earthquake; Coda; Episodic tremor and slip; Fault (geology); Foreshock; Interplate earthquake; Tectonics; Physics; Aftershock; Voltage; Subduction","score_opus":0.016848572020753412,"score_gpt":0.23790015711692483,"score_spread":0.22105158509617143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3144140569","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99382657,0.000104876024,0.004449497,0.000018913535,0.000007832137,0.00001739607,0.00021833915,0.000071083436,0.0012853927],"genre_scores_gemma":[0.99881625,0.000038861734,0.0007448989,0.000008610936,0.000005489178,0.000004973239,0.00014409036,0.000004972613,0.00023194792],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996364,0.0000033410242,0.000003890035,0.000008691873,0.000010915835,0.000009424021],"domain_scores_gemma":[0.9997607,0.0000369383,0.000114334005,0.000023923738,0.000023753322,0.00004048796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000052901807,0.00014593951,0.000129628,0.00038636144,0.00008797186,0.00019038828,0.00009410218,0.00014381294,0.0009848694],"category_scores_gemma":[0.00031229708,0.00007088307,0.00009688731,0.0003068074,0.00023254509,0.00016779716,0.00036494635,0.00018770163,0.00014120547],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000752034,0.00010506878,0.1261921,0.00017888268,0.000075655764,0.0017522908,0.00050824543,0.0009668444,0.812771,0.00096643594,0.000411509,0.055319857],"study_design_scores_gemma":[0.000023188952,0.0004784531,0.93131566,0.000012946068,0.00003405764,0.0030298734,0.00028912988,0.002899507,0.059228994,0.0009011301,0.0017656828,0.000021359241],"about_ca_topic_score_codex":0.00026020926,"about_ca_topic_score_gemma":0.00046333176,"teacher_disagreement_score":0.0009848694,"about_ca_system_score_codex":0.0000939839,"about_ca_system_score_gemma":0.00004777304,"threshold_uncertainty_score":0.003294766},"labels":[],"label_agreement":null},{"id":"W3146232375","doi":"10.48550/arxiv.2011.07237","title":"A Reanalysis of the October 2016 \"Meteotsunami\" in British Columbia with\\n Help of High-Frequency Radars and Autoregressive Modeling","year":2020,"lang":"","type":"article","venue":"arXiv (Cornell University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Radar; Meteorology; Amplitude; Environmental science; Geology; Seismology; Remote sensing; Geodesy; Computer science; Telecommunications; Physics","score_opus":0.03112985353723716,"score_gpt":0.14241483752749934,"score_spread":0.11128498399026218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3146232375","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9289966,0.0010687876,0.0019874284,0.001109434,0.00030418206,0.00007395594,0.050569274,0.0007909772,0.015099292],"genre_scores_gemma":[0.9592182,0.0010926188,0.0023165562,0.0001213692,0.000029464041,0.00003909058,0.027264923,0.00009718402,0.00982058],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998727,0.0000052292885,0.0000056270533,0.00002801981,0.00005982703,0.000028622739],"domain_scores_gemma":[0.9996823,0.0000113549695,0.000022581602,0.000017531544,0.00022763564,0.000038736547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013718434,0.0005385066,0.00032686803,0.0011972158,0.00094795134,0.001216793,0.0007489942,0.00069715385,0.0026637448],"category_scores_gemma":[0.0005980147,0.00028074338,0.000291971,0.0026835024,0.00036424803,0.00034045434,0.00037806822,0.0008179546,0.00054577395],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009682141,0.00041212642,0.4305089,0.0009161583,0.0009944113,0.0026469943,0.002103193,0.21947321,0.033608265,0.0030341225,0.14028817,0.1650463],"study_design_scores_gemma":[0.00008482707,0.000021928972,0.89511913,0.00011178663,0.00012410298,0.0001144761,0.000970222,0.056019742,0.002664448,0.00020789109,0.044443212,0.00011822355],"about_ca_topic_score_codex":0.98677546,"about_ca_topic_score_gemma":0.9922884,"teacher_disagreement_score":0.013224542,"about_ca_system_score_codex":0.009967154,"about_ca_system_score_gemma":0.0098137595,"threshold_uncertainty_score":0.072317064},"labels":[],"label_agreement":null},{"id":"W3146254152","doi":"10.1785/0120200273","title":"The 1900 Mw 7.6–8.0 Earthquake Offshore of Kodiak Island, Alaska","year":2021,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Submarine pipeline; Geology; Seismology; Geotechnical engineering","score_opus":0.012667795032932793,"score_gpt":0.20440170801396498,"score_spread":0.19173391298103218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3146254152","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99770504,0.000064268475,0.000091182206,0.000017709128,0.0000054225206,0.0000029236046,0.00025066108,0.0000053633553,0.0018574067],"genre_scores_gemma":[0.9981152,0.0001274594,0.00024020791,0.00000927856,0.0000033739752,0.0000024937565,0.000469036,0.000001803009,0.0010312704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997544,0.0000018312355,0.0000032016146,0.000007894858,0.000005476745,0.0000061209826],"domain_scores_gemma":[0.99989474,0.0000075565413,0.000028828588,0.000006165823,0.000038922586,0.00002372789],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000873546,0.00011553267,0.00009588684,0.00036838694,0.00041652308,0.00029504456,0.00009268211,0.00009832782,0.0010977404],"category_scores_gemma":[0.00016649332,0.00008771102,0.000101298654,0.00035967008,0.00019277594,0.00018709163,0.00032594256,0.00014241909,0.00018002851],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007905309,0.000023382852,0.9773866,0.000046899357,0.000042823638,0.00056085916,0.0010831204,0.0010648577,0.007989933,0.00014131794,0.00046757387,0.011113589],"study_design_scores_gemma":[0.0000017646852,0.000021563048,0.9960828,0.000015715274,0.000029363442,0.000101355035,0.0011989324,0.0005155059,0.0006245985,0.000033980137,0.0013691963,0.0000051599527],"about_ca_topic_score_codex":0.06843069,"about_ca_topic_score_gemma":0.112339646,"teacher_disagreement_score":0.06843069,"about_ca_system_score_codex":0.00039277834,"about_ca_system_score_gemma":0.00043942363,"threshold_uncertainty_score":0.13606477},"labels":[],"label_agreement":null},{"id":"W3146353910","doi":"10.1029/2021ea001800","title":"<i>P</i> ‐Wave Tomography for 3‐D Radial and Azimuthal Anisotropy Beneath Greenland and Surrounding Regions","year":2021,"lang":"en","type":"article","venue":"Earth and Space Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Geology; Upwelling; Mantle (geology); Outcrop; Bay; Breakup; Seismology; Geophysics; Groenlandia; Anisotropy; Oceanography; Geomorphology; Physics; Ice sheet","score_opus":0.02147777775652604,"score_gpt":0.22133192749234035,"score_spread":0.1998541497358143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3146353910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918584,0.00010947148,0.0041770963,0.00009251609,0.0000056334675,0.000012458849,0.0010441266,0.00032079316,0.0023794938],"genre_scores_gemma":[0.99456596,0.00005445355,0.004542578,0.000017672579,0.0000031101335,0.000005460292,0.00048525285,0.000023327539,0.00030225454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996793,0.0000025644129,0.0000011790445,0.000008123274,0.0000070327433,0.000013197793],"domain_scores_gemma":[0.99994624,0.000005492208,0.000013431173,0.000006638066,0.000017097911,0.0000111009895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000108357344,0.00021264007,0.000094080744,0.00094392226,0.00021189405,0.0004438956,0.0002050769,0.00015539375,0.0007757106],"category_scores_gemma":[0.0001381131,0.0001265408,0.00019275976,0.00059130666,0.0001922517,0.00018551845,0.00025272326,0.0001576171,0.00013008341],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029566424,0.00011114708,0.49358022,0.00010141756,0.00022674164,0.0012341504,0.0007783043,0.06424648,0.31813478,0.0014823574,0.003633065,0.11617558],"study_design_scores_gemma":[0.0000172084,0.00002042081,0.8912201,0.000022411152,0.000049479644,0.00014133613,0.00030511187,0.09715284,0.008711948,0.00027591636,0.0020566396,0.000026586758],"about_ca_topic_score_codex":0.098062135,"about_ca_topic_score_gemma":0.16969432,"teacher_disagreement_score":0.098062135,"about_ca_system_score_codex":0.00053434283,"about_ca_system_score_gemma":0.00073973084,"threshold_uncertainty_score":0.19498271},"labels":[],"label_agreement":null},{"id":"W3147313445","doi":"10.1038/s41598-021-86413-w","title":"Liquiñe-Ofqui’s fast slipping intra-volcanic arc crustal faulting above the subducted Chile Ridge","year":2021,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Norges Geologiske Undersøkelse; Agencia Nacional de Investigación y Desarrollo; Natural Environment Research Council; Sight Research UK; Newton Fund","keywords":"Geology; Subduction; Caldera; Stratovolcano; Seismology; Volcano; Forearc; Slipping; Fault (geology); Ridge; Volcanic arc; Tectonics; Volcanic rock; Paleontology","score_opus":0.014435618892914486,"score_gpt":0.2156387894870294,"score_spread":0.2012031705941149,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3147313445","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99262416,0.00022980102,0.00028742995,0.00012431832,0.0000039152364,0.000016498228,0.00058680744,0.0000343005,0.006092758],"genre_scores_gemma":[0.9985619,0.0000646778,0.0002570112,0.000014219945,0.0000019127374,0.000008926937,0.00028729616,0.0000034875936,0.0008005142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999923,0.0000073117094,0.0000033192646,0.000026741578,0.000012983604,0.000026678175],"domain_scores_gemma":[0.99984515,0.000022382865,0.000055225475,0.000021466556,0.000031766114,0.000023996643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013916871,0.00015228301,0.0001824294,0.00051571353,0.00045094313,0.0005690682,0.00024441216,0.0002530929,0.0016540105],"category_scores_gemma":[0.00051754003,0.00012844801,0.00012084595,0.0006259138,0.00042951666,0.0002611099,0.0005778127,0.00024062245,0.0001669994],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025125212,0.000030104988,0.917106,0.00015929867,0.00004502456,0.001091374,0.003269652,0.0010137336,0.039154015,0.0015990781,0.0009683608,0.03531217],"study_design_scores_gemma":[0.000009026229,0.000027579805,0.9924429,0.000026115122,0.00000817902,0.00030783037,0.0007834279,0.0004158047,0.0010930784,0.00024118739,0.0046385904,0.0000061543556],"about_ca_topic_score_codex":0.035268784,"about_ca_topic_score_gemma":0.041139044,"teacher_disagreement_score":0.035268784,"about_ca_system_score_codex":0.0009777956,"about_ca_system_score_gemma":0.0006794054,"threshold_uncertainty_score":0.07012701},"labels":[],"label_agreement":null},{"id":"W3149451288","doi":"10.5194/egusphere-egu21-2437","title":"Dominant strike-slip faulting and near-constant stress drop of induced earthquakes in the Kiskatinaw area, northeastern British Columbia, Canada","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Span (engineering); Life span; Seismology; Geology; Biology; Structural engineering; Engineering","score_opus":0.013458138882173534,"score_gpt":0.1913956277662497,"score_spread":0.17793748888407615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3149451288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883547,0.00028348537,0.00020886582,0.00018436722,0.000008691869,0.0000262165,0.0064746025,0.000051268602,0.00440763],"genre_scores_gemma":[0.99348843,0.00026575846,0.00021330516,0.000043873042,0.0000037822065,0.000014111531,0.0036781055,0.000014889516,0.0022777736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997991,0.00000836443,0.0000140509455,0.000047254547,0.000054334174,0.00007686352],"domain_scores_gemma":[0.99920446,0.00004735281,0.00009747647,0.000037030513,0.00043874912,0.0001749951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015358685,0.0003496882,0.00026768717,0.002203414,0.0016839388,0.0012688466,0.0007389703,0.00033509606,0.0030819012],"category_scores_gemma":[0.0010466,0.0002119185,0.00020996417,0.003876827,0.0005030394,0.00026747212,0.00071057153,0.0003449847,0.0004171879],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000101095655,0.00006013277,0.95405793,0.00010305254,0.0001246692,0.0007612322,0.0012629735,0.00493599,0.0027966776,0.00045348587,0.0073449267,0.027997803],"study_design_scores_gemma":[0.000007629349,0.00000351997,0.9942747,0.000023860379,0.000018890618,0.000068848196,0.0012489456,0.002438641,0.00011662333,0.00003106518,0.0017523413,0.000015008436],"about_ca_topic_score_codex":0.99281573,"about_ca_topic_score_gemma":0.99731606,"teacher_disagreement_score":0.010440208,"about_ca_system_score_codex":0.010440208,"about_ca_system_score_gemma":0.011868792,"threshold_uncertainty_score":0.0757494},"labels":[],"label_agreement":null},{"id":"W3150742605","doi":"10.1016/j.jsg.2021.104328","title":"Selective clast survival in an experimentally-produced pseudotachylyte","year":2021,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; H2020 European Research Council; Università degli Studi di Padova","keywords":"Plagioclase; Geology; Quartz; Slip (aerodynamics); Sillimanite; Mineralogy; Ilmenite; Mineral; Geochemistry; Petrology; Biotite; Materials science","score_opus":0.020170664320137466,"score_gpt":0.2628213091545839,"score_spread":0.24265064483444643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3150742605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994961,0.000018686018,0.00012985135,0.000011185664,0.0000037595637,0.000005390896,0.000044105862,0.000006174012,0.00028468482],"genre_scores_gemma":[0.9988111,0.0000155405,0.0001714509,0.0000124853805,0.0000018023796,0.000011956601,0.000090687616,0.0000119919905,0.00087283785],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997893,0.000035551886,0.000018708566,0.000063494364,0.000046198285,0.000046681293],"domain_scores_gemma":[0.99928904,0.0002829395,0.00010717737,0.00007500089,0.000080855985,0.0001649259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016342511,0.00027144872,0.0003040429,0.0003281191,0.0005465069,0.0003576862,0.0008773525,0.0007252445,0.0024421876],"category_scores_gemma":[0.0009242474,0.00033685903,0.00020055122,0.00014794071,0.0008098269,0.0001914459,0.00065002893,0.0007600033,0.00029123787],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006023428,0.00007860285,0.002156933,0.000018456582,0.000008744393,0.00019973544,0.00012512626,0.00023860445,0.9952674,0.00016497208,0.000023768138,0.0011152668],"study_design_scores_gemma":[0.0003975128,0.007447948,0.18063422,0.000041649153,0.00014160853,0.0029911073,0.001243465,0.016856058,0.78700763,0.00062502216,0.0025180723,0.000095789714],"about_ca_topic_score_codex":0.004974078,"about_ca_topic_score_gemma":0.008039156,"teacher_disagreement_score":0.004974078,"about_ca_system_score_codex":0.00061701774,"about_ca_system_score_gemma":0.00049747614,"threshold_uncertainty_score":0.009890258},"labels":[],"label_agreement":null},{"id":"W3151237919","doi":"","title":"Stacked uppermost mantle layers within the Slave craton of NW Canada as defined by anisotropic seismic discontinuities","year":2007,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Kimberlite; Classification of discontinuities; Mantle (geology); Seismology; Anisotropy; Craton; Geophysics; Seismic array; Seismogram; Discontinuity (linguistics); Seismic anisotropy; Petrology","score_opus":0.009531061210330852,"score_gpt":0.20267354881061914,"score_spread":0.1931424876002883,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3151237919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99718827,0.00007377957,0.00017696201,0.000014044612,0.0000010882576,0.00000949134,0.00044947152,0.000012370744,0.0020744384],"genre_scores_gemma":[0.9989635,0.00004023383,0.00027905076,0.0000045395077,5.7907766e-7,0.000002122673,0.00025209127,0.0000026285838,0.00045528333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999157,0.0000017756855,0.000002384411,0.000014039846,0.000025850752,0.00004023122],"domain_scores_gemma":[0.9998865,0.000005408268,0.000024956189,0.0000058350083,0.000047313697,0.00003002581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000045416706,0.00021530919,0.00012744575,0.0012232256,0.0008658349,0.0008222418,0.00030991776,0.00015100738,0.0012301415],"category_scores_gemma":[0.00029599748,0.00017174816,0.00009453145,0.0016809106,0.00045196374,0.00015237002,0.00051517726,0.00014692864,0.00009661356],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022877486,0.000023426788,0.92718583,0.00003487054,0.000054145014,0.00054070016,0.002062762,0.0016145295,0.043839503,0.00082849496,0.000578709,0.023008099],"study_design_scores_gemma":[0.0000019708677,0.000004663329,0.99788576,0.000003948777,0.000007718592,0.000055651613,0.00044803176,0.0005719518,0.000571174,0.000038847422,0.00040621404,0.000004111011],"about_ca_topic_score_codex":0.90667444,"about_ca_topic_score_gemma":0.96669286,"teacher_disagreement_score":0.093325555,"about_ca_system_score_codex":0.0030002554,"about_ca_system_score_gemma":0.0033297087,"threshold_uncertainty_score":0.18775028},"labels":[],"label_agreement":null},{"id":"W3151319682","doi":"10.1029/2020jb021221","title":"States of In Situ Stress in the Duvernay East Shale Basin and Willesden Green of Alberta, Canada: Variable In Situ Stress States Effect Fault Stability","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; Purdue University","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Borehole; Seismology; Pore water pressure; Fault (geology); Slip (aerodynamics); Microseism; Fault plane; Structural basin; Stress field; Differential stress; Petrology; Shear (geology); Geotechnical engineering; Deformation (meteorology); Geomorphology; Engineering","score_opus":0.019004179338103538,"score_gpt":0.26894933578912705,"score_spread":0.24994515645102353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3151319682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993892,0.000013768996,0.000037327667,0.00001275843,5.047698e-7,0.0000029922867,0.00018369922,0.000003881235,0.0003559595],"genre_scores_gemma":[0.99953854,0.000015169686,0.000054236265,0.0000046687765,3.0547199e-7,0.0000015393334,0.00016547556,0.0000011495326,0.00021883828],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998197,0.000019558709,0.000008807667,0.000034597877,0.00005303336,0.000064326065],"domain_scores_gemma":[0.99946743,0.00009724897,0.000065479806,0.000024427307,0.00024032332,0.00010506581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027443792,0.00025945442,0.00023768014,0.0008349431,0.0008532367,0.0010383595,0.0005696665,0.00027183097,0.000761815],"category_scores_gemma":[0.0011111939,0.00018558392,0.00014813805,0.0013099506,0.0008727646,0.00021802951,0.00044341135,0.00016273238,0.00006312232],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031378563,0.00009640345,0.97051406,0.000030573046,0.00009643453,0.00024609265,0.0011724973,0.010920443,0.0075168284,0.00035468076,0.0003850376,0.008353273],"study_design_scores_gemma":[0.000006524903,0.000013977885,0.9926247,0.0000050561916,0.000012025628,0.000013269305,0.0009467549,0.005580644,0.0005419109,0.000043086875,0.00020325866,0.000008801863],"about_ca_topic_score_codex":0.97317797,"about_ca_topic_score_gemma":0.98769057,"teacher_disagreement_score":0.02682203,"about_ca_system_score_codex":0.008973828,"about_ca_system_score_gemma":0.006007416,"threshold_uncertainty_score":0.06510997},"labels":[],"label_agreement":null},{"id":"W3153545921","doi":"10.1029/2021gl092889","title":"The Crustal Stress Field Inferred From Focal Mechanisms in Northern Chile","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Calgary; University of Victoria","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; University of Victoria","keywords":"Geology; Crust; Seismology; Stress field; Focal mechanism; Compression (physics); Margin (machine learning); Slip (aerodynamics); Stress (linguistics); Continental margin; Geophysics; Tectonics","score_opus":0.0280776844329247,"score_gpt":0.27390957960832957,"score_spread":0.24583189517540488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3153545921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983139,0.00016647553,0.000102602906,0.000019603634,8.732186e-7,0.0000049730897,0.0004081583,0.000012887594,0.00097052014],"genre_scores_gemma":[0.9994647,0.0000764583,0.00006986282,0.0000021642977,0.0000012120596,0.0000052688392,0.00023058701,0.0000018476151,0.00014783234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999151,0.000010913265,0.000008445754,0.000023968749,0.00001681862,0.000024754445],"domain_scores_gemma":[0.9994823,0.000090856025,0.00019731004,0.000049190152,0.00011080258,0.000069560825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026525432,0.00020367597,0.00023735654,0.0022303136,0.0003141584,0.0007000573,0.00032351358,0.00020418853,0.0016661533],"category_scores_gemma":[0.0011253522,0.00019337848,0.0002362554,0.0015845206,0.00029765067,0.00033661808,0.0006902622,0.000121991114,0.00019321428],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000099060606,0.000020998177,0.97988737,0.000065571985,0.000076590884,0.00033712146,0.00086280995,0.0019785028,0.0056620566,0.00020988777,0.00025678833,0.010543313],"study_design_scores_gemma":[0.0000073702095,0.000011091738,0.9971615,0.000017317196,0.000015282385,0.000068246,0.0005355268,0.0014649063,0.00023426041,0.000085418054,0.00039264586,0.0000065318363],"about_ca_topic_score_codex":0.036164932,"about_ca_topic_score_gemma":0.02903532,"teacher_disagreement_score":0.036164932,"about_ca_system_score_codex":0.0009280501,"about_ca_system_score_gemma":0.00049674045,"threshold_uncertainty_score":0.07190889},"labels":[],"label_agreement":null},{"id":"W3153813044","doi":"","title":"Assessing Variability of Intraplate Crustal Stress Orientation and Seismic Hazard in the Charlevoix Seismic Zone, Eastern Canada","year":2018,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Geology; Seismology; Seismic hazard; Hazard; Orientation (vector space); Tectonics; Geometry","score_opus":0.016864138440594447,"score_gpt":0.2363259990106283,"score_spread":0.21946186057003386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3153813044","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99766773,0.00013882783,0.00012038851,0.00006201645,0.0000023055115,0.000013512112,0.0006924429,0.000008458164,0.0012944817],"genre_scores_gemma":[0.9977083,0.000111622125,0.00018216192,0.000019760546,0.0000015101203,0.000007281655,0.0006648645,0.0000048880656,0.0012995409],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994742,0.00004952079,0.000028589731,0.00008646658,0.00016659274,0.00019462888],"domain_scores_gemma":[0.9980597,0.00024914666,0.00017554316,0.00005405468,0.0010665437,0.000395104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073125627,0.0003364099,0.00030647588,0.0019607681,0.0020840731,0.0017604749,0.0011565341,0.0003984115,0.0012565545],"category_scores_gemma":[0.0020847933,0.0003013145,0.0003384181,0.0029210043,0.0007446833,0.00038972552,0.000916061,0.00046509822,0.00017144285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012862349,0.000042154094,0.98473686,0.000020128082,0.00009372411,0.00009870458,0.0015084146,0.0016510135,0.0009743963,0.00021303544,0.00062216684,0.009910659],"study_design_scores_gemma":[0.0000044370063,0.000008818303,0.99668616,0.000008791441,0.000014268993,0.000014407413,0.0017254726,0.0009411475,0.00008682081,0.000016406913,0.00048663202,0.0000066582706],"about_ca_topic_score_codex":0.99758387,"about_ca_topic_score_gemma":0.9988715,"teacher_disagreement_score":0.021423066,"about_ca_system_score_codex":0.021423066,"about_ca_system_score_gemma":0.023601029,"threshold_uncertainty_score":0.15543592},"labels":[],"label_agreement":null},{"id":"W3153918573","doi":"10.1785/0120200344","title":"The Productivity of Cascadia Aftershock Sequences","year":2021,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Seismology; Subduction; Geology; Induced seismicity; Productivity; Fault (geology); Outlier; Statistics; Tectonics","score_opus":0.015249491571407139,"score_gpt":0.20701991426211233,"score_spread":0.19177042269070518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3153918573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99563134,0.00009635439,0.0007474202,0.000044684097,0.000005240294,0.000007892072,0.0017447944,0.000077037876,0.001645217],"genre_scores_gemma":[0.9982717,0.00005286275,0.00014255258,0.0000030417161,0.000003509943,0.000002732866,0.001323296,0.000008536189,0.00019179602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99934095,0.00009417655,0.00008417299,0.00023727678,0.00016951341,0.000073778596],"domain_scores_gemma":[0.99123096,0.0020297645,0.0035751106,0.0008790914,0.0016769579,0.00060804735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012121149,0.00052343257,0.00022792137,0.0033313865,0.00023379452,0.0012690049,0.0003453671,0.00020506182,0.0022957702],"category_scores_gemma":[0.01173848,0.00021764525,0.0003580202,0.0030703843,0.00044526492,0.00080394035,0.0009369053,0.00031485374,0.00044007905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026820868,0.00000509455,0.9923833,0.000019925645,0.00008921305,0.00005660698,0.00019011108,0.0026526114,0.00045032543,0.00012129261,0.00024341913,0.0037612594],"study_design_scores_gemma":[0.0000016497036,0.000011106413,0.9962475,0.000008894108,0.000015595926,0.00003450439,0.00017043692,0.0027625505,0.00019354667,0.000088366374,0.00046084353,0.000005059134],"about_ca_topic_score_codex":0.037357695,"about_ca_topic_score_gemma":0.03767008,"teacher_disagreement_score":0.037357695,"about_ca_system_score_codex":0.0009973063,"about_ca_system_score_gemma":0.00045025314,"threshold_uncertainty_score":0.0742805},"labels":[],"label_agreement":null},{"id":"W3154640686","doi":"10.1029/2021ea001825","title":"Reactivation Potential of Intraplate Faults in the Western Quebec Seismic Zone, Eastern Canada","year":2021,"lang":"en","type":"article","venue":"Earth and Space Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Intraplate earthquake; Geology; Seismology; Induced seismicity; Seismic hazard; Slip (aerodynamics); Fault (geology); Neotectonics; Seismic risk; Seismic gap; Tectonics","score_opus":0.007810698075457246,"score_gpt":0.19291241380928376,"score_spread":0.1851017157338265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3154640686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99552464,0.00017513386,0.0002762017,0.000068792375,0.000002028452,0.000009163179,0.000893023,0.000022679973,0.003028324],"genre_scores_gemma":[0.9989209,0.000060753082,0.00014192327,0.0000054001243,3.9754673e-7,0.0000018341957,0.00025032499,0.0000014694306,0.0006170922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999105,0.0000071963746,0.000004145442,0.000018472436,0.000024970903,0.000034722798],"domain_scores_gemma":[0.99966097,0.000043086897,0.000051088507,0.000013505707,0.00015796737,0.000073274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017180908,0.0001903467,0.00013228218,0.000985942,0.0008460053,0.0009893869,0.00047687304,0.00019539018,0.0017483666],"category_scores_gemma":[0.00062117225,0.00009427669,0.00015137269,0.0012647501,0.0004712372,0.00020668855,0.00027824895,0.00016013943,0.00009460866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001715752,0.00003301969,0.9259543,0.00005448836,0.00008132489,0.00024311517,0.00060565723,0.037862606,0.0026333942,0.0013846145,0.001344124,0.029631788],"study_design_scores_gemma":[0.000012330046,0.000019616775,0.9619394,0.000026782694,0.000025102681,0.000037633563,0.00089546334,0.03468895,0.0005048591,0.00012207446,0.0017107796,0.00001703628],"about_ca_topic_score_codex":0.99328125,"about_ca_topic_score_gemma":0.9961914,"teacher_disagreement_score":0.013413065,"about_ca_system_score_codex":0.013413065,"about_ca_system_score_gemma":0.008880802,"threshold_uncertainty_score":0.09731907},"labels":[],"label_agreement":null},{"id":"W3155878479","doi":"10.1126/sciadv.abf7282","title":"Synchronized and asynchronous modulation of seismicity by hydrological loading: A case study in Taiwan","year":2021,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Jarðvísindastofnun; Ministry of Science and Technology, Government of the People’s Republic of Bangladesh; Ministry of Science and Technology, Taiwan; Academia Sinica; National Aeronautics and Space Administration","keywords":"Induced seismicity; Asynchronous communication; Modulation (music); Seismology; Seismic hazard; Hazard; Environmental science; Water cycle; Geology; Climatology; Computer science; Biology; Telecommunications; Physics; Ecology","score_opus":0.015635299311759433,"score_gpt":0.2586114790363968,"score_spread":0.24297617972463736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3155878479","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992866,0.000035423906,0.00026008184,0.00007156058,0.0000013914965,0.0000078014245,0.000083400795,0.000008898094,0.00024488624],"genre_scores_gemma":[0.99942905,0.000048966158,0.00028787792,0.000010076301,0.0000051879188,0.000004565203,0.00010961702,0.0000032763007,0.00010140683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997656,0.000067126704,0.000027518627,0.000051521307,0.00002863163,0.00005963032],"domain_scores_gemma":[0.9989937,0.00041525075,0.00024179413,0.000102869184,0.00009998589,0.00014637542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005454282,0.0003324946,0.00031814782,0.0010131352,0.0005361683,0.00063245173,0.0006028791,0.00091610197,0.00061604875],"category_scores_gemma":[0.0017131952,0.00024595106,0.00041621883,0.0017963229,0.0005002906,0.0004921434,0.0007948682,0.00033343164,0.000093617346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033878232,0.00043824696,0.92094946,0.00007751429,0.00018003097,0.033322874,0.0029056054,0.020609852,0.0053281905,0.0007944146,0.0008205091,0.014234548],"study_design_scores_gemma":[0.000093103314,0.00045663156,0.86088365,0.000030125642,0.00019305683,0.004964566,0.010354116,0.11954837,0.0013248939,0.0009631587,0.0011031942,0.00008512564],"about_ca_topic_score_codex":0.044453718,"about_ca_topic_score_gemma":0.0541001,"teacher_disagreement_score":0.044453718,"about_ca_system_score_codex":0.0008201118,"about_ca_system_score_gemma":0.0005238765,"threshold_uncertainty_score":0.08838993},"labels":[],"label_agreement":null},{"id":"W3157194675","doi":"10.1785/0220200429","title":"Earthquake Depths, Focal Mechanisms, and Stress in the Lower St. Lawrence Seismic Zone","year":2021,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Dalhousie University","funders":"","keywords":"Seismology; Geology; Focal mechanism; Aftershock; Hypocenter; Induced seismicity; Tectonics; Cauchy stress tensor; Amplitude; Geodesy","score_opus":0.053834347252230325,"score_gpt":0.2901341297343499,"score_spread":0.23629978248211955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157194675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99863404,0.00004234325,0.0001510467,0.000032631357,6.727163e-7,0.0000026217117,0.00046688959,0.000020064064,0.00064957835],"genre_scores_gemma":[0.9991667,0.000023727149,0.00013280087,0.000004871553,5.1405857e-7,0.0000014178838,0.00037425233,0.0000028414215,0.0002929262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998623,0.000010187181,0.000008599017,0.000027636092,0.00004886998,0.00004235104],"domain_scores_gemma":[0.9994312,0.00006198788,0.00017736579,0.000028588582,0.00020461669,0.00009627451],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022196173,0.00021224648,0.00018797531,0.0013223855,0.0005595368,0.00081228727,0.00047588922,0.00021327315,0.0013255714],"category_scores_gemma":[0.001171308,0.00015586209,0.00013479005,0.0016004324,0.00057184626,0.00024104909,0.00055563136,0.00018766156,0.00015017454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008964864,0.000025865013,0.97057813,0.000031722862,0.00004260798,0.00012630636,0.00052795606,0.0137700625,0.002925389,0.00047695357,0.0005429808,0.01086231],"study_design_scores_gemma":[0.000008153811,0.000017977698,0.9797578,0.000014885612,0.000014553147,0.000027316495,0.0004989057,0.018184904,0.00068844913,0.00011495915,0.0006555715,0.000016391736],"about_ca_topic_score_codex":0.91185784,"about_ca_topic_score_gemma":0.95929116,"teacher_disagreement_score":0.08814216,"about_ca_system_score_codex":0.0041814,"about_ca_system_score_gemma":0.0025566565,"threshold_uncertainty_score":0.17732245},"labels":[],"label_agreement":null},{"id":"W3157370717","doi":"10.1029/2021gl093231","title":"On the Relevance of Geodetic Deformation Rates to Earthquake Potential","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geodetic datum; Geology; Viscoelasticity; Slip (aerodynamics); Strain rate; Geodesy; Deformation (meteorology); Fault (geology); Engineering","score_opus":0.03083872391617542,"score_gpt":0.28070972160211727,"score_spread":0.24987099768594184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157370717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.956867,0.0024724186,0.0035595305,0.0045197397,0.0001086966,0.000013771544,0.00042335238,0.000037783524,0.0319977],"genre_scores_gemma":[0.99931157,0.00016045767,0.000072260234,0.000053787302,0.000059005382,0.0000011714941,0.000033877768,0.000007859376,0.00030010822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992755,0.00042543808,0.00003131509,0.00013638195,0.000077415105,0.000053898122],"domain_scores_gemma":[0.95342016,0.038631976,0.0034247558,0.0014674952,0.0018737679,0.0011819362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027730009,0.00022032362,0.00022497853,0.0013530253,0.00031867056,0.0019865949,0.0006178578,0.00077477464,0.004160007],"category_scores_gemma":[0.04435317,0.0001599949,0.00023477874,0.0012882622,0.0019738579,0.0017124385,0.0010072485,0.0011542992,0.00052756065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00074223493,0.000059217084,0.90039986,0.00016264143,0.00013224533,0.00061608804,0.00090787024,0.011701475,0.002768626,0.041541617,0.0017173681,0.03925075],"study_design_scores_gemma":[0.000016489726,0.0001564348,0.9400409,0.00009022523,0.00008813079,0.0005394013,0.0013770418,0.014826056,0.0009976,0.039957397,0.0018753164,0.000034978595],"about_ca_topic_score_codex":0.0022800812,"about_ca_topic_score_gemma":0.0014504375,"teacher_disagreement_score":0.004160007,"about_ca_system_score_codex":0.0003364729,"about_ca_system_score_gemma":0.00022295566,"threshold_uncertainty_score":0.014665186},"labels":[],"label_agreement":null},{"id":"W3157595746","doi":"10.1002/essoar.10506952.1","title":"Complex 3D Migration and Delayed Triggering of Hydraulic Fracturing-Induced Seismicity","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Electronic mail; World Wide Web; Computer science","score_opus":0.0400754580857188,"score_gpt":0.2436846015755082,"score_spread":0.2036091434897894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157595746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96890074,0.00012573086,0.026505515,0.00024333755,0.00004352375,0.000029642402,0.001223466,0.0007217834,0.002206154],"genre_scores_gemma":[0.9937576,0.000066786975,0.0054999567,0.000019303634,0.000006593876,0.000007971989,0.00034140158,0.00005091105,0.00024941587],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999237,0.0000060856914,0.0000053970407,0.000019636012,0.000025167685,0.000020012207],"domain_scores_gemma":[0.9998024,0.000044820394,0.00006012241,0.000032746335,0.000026763277,0.000033169043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011767534,0.00031359284,0.00024658925,0.000474652,0.00018754869,0.0009484686,0.00022625482,0.0004780475,0.0018695742],"category_scores_gemma":[0.0005412223,0.0002800307,0.00025391637,0.00042460178,0.00046917348,0.0003927911,0.00045053562,0.000476577,0.0002453587],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061030214,0.00040586398,0.15630092,0.00050039927,0.00029001778,0.0038242359,0.001661055,0.37477553,0.3961319,0.007890082,0.005001042,0.052608576],"study_design_scores_gemma":[0.000066257075,0.00011354752,0.22870998,0.000040383424,0.00005297135,0.00097108586,0.00063542195,0.7401953,0.022475721,0.0034032501,0.0032251696,0.000110838],"about_ca_topic_score_codex":0.0022789824,"about_ca_topic_score_gemma":0.0037435777,"teacher_disagreement_score":0.0022789824,"about_ca_system_score_codex":0.0002373219,"about_ca_system_score_gemma":0.0004157315,"threshold_uncertainty_score":0.006254375},"labels":[],"label_agreement":null},{"id":"W3157641237","doi":"10.1785/0220200350","title":"Structure and Dynamics of the Southern Rocky Mountain Trench near Valemount, British Columbia, Inferred from Local Seismicity","year":2021,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Geology; Seismology; Trench; Seismometer; Tectonics; Fault (geology)","score_opus":0.02345908745386192,"score_gpt":0.2459800572087758,"score_spread":0.2225209697549139,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157641237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952253,0.0002720837,0.000074304626,0.00008656154,0.0000031870381,0.000014304034,0.0021375339,0.000017921238,0.0021687853],"genre_scores_gemma":[0.9970386,0.00022797182,0.00015754714,0.000021392994,0.0000018011003,0.000009307074,0.0014899437,0.0000056054455,0.0010477861],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997646,0.00001115028,0.000013765266,0.000067179026,0.00007279756,0.00007049163],"domain_scores_gemma":[0.9990446,0.00006822793,0.00012600521,0.000033524193,0.00052030635,0.00020729424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017478182,0.00030050144,0.00026635418,0.0022301483,0.0018199655,0.0014650222,0.00078385655,0.00036555566,0.0017223622],"category_scores_gemma":[0.0011951602,0.0002747026,0.00013944208,0.0037196106,0.0005978411,0.00023339406,0.00077812746,0.00026841502,0.00028451768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048915197,0.000024810943,0.97481877,0.00008941574,0.00006843717,0.00037012083,0.001603578,0.0013034678,0.0029467787,0.00015074517,0.0021172457,0.016457666],"study_design_scores_gemma":[0.0000023611235,0.0000037823165,0.9970655,0.000026780399,0.000009567267,0.000034422905,0.001168709,0.00058779883,0.00006733163,0.000012855198,0.0010139585,0.0000068648465],"about_ca_topic_score_codex":0.9907726,"about_ca_topic_score_gemma":0.99785244,"teacher_disagreement_score":0.009227395,"about_ca_system_score_codex":0.008169614,"about_ca_system_score_gemma":0.008859376,"threshold_uncertainty_score":0.059274912},"labels":[],"label_agreement":null},{"id":"W3157858215","doi":"10.1029/2020jb020308","title":"Investigation on Two M<sub>w</sub> 3.6 and M<sub>w</sub> 4.1 Earthquakes Triggered by Poroelastic Effects of Hydraulic Fracturing Operations Near Crooked Lake, Alberta","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Virtual Materials Group (Canada); University of Calgary","funders":"Canada First Research Excellence Fund","keywords":"Poromechanics; Geology; Hydraulic fracturing; Pore water pressure; Geomechanics; Fault (geology); Seismology; Induced seismicity; Slip (aerodynamics); Fluid pressure; Permeability (electromagnetism); Effective stress; Geotechnical engineering; Petrology; Mechanics; Engineering","score_opus":0.024705724865276724,"score_gpt":0.272006113906878,"score_spread":0.2473003890416013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157858215","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993457,0.000008231064,0.00014962617,0.00001051166,0.0000011932663,0.0000069458024,0.00005279486,0.0000100105535,0.00041497475],"genre_scores_gemma":[0.9994172,0.000014205589,0.00020226993,0.0000048405377,6.12368e-7,0.000002820215,0.00005673582,0.0000018429114,0.00029948945],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995375,0.0000023881723,0.0000013814843,0.000006052402,0.000020539592,0.00001587022],"domain_scores_gemma":[0.9999397,0.00000819073,0.000010712229,0.000004105252,0.000019226338,0.000018059993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006155209,0.00019104619,0.00017562295,0.00028844745,0.0005110998,0.00024247475,0.00029831319,0.00030652087,0.00064432825],"category_scores_gemma":[0.000090252244,0.00011528308,0.00018295548,0.00024251245,0.0002660514,0.000109302855,0.000172913,0.00021070919,0.00006343411],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011150348,0.0005982832,0.35057828,0.00018231022,0.00010184106,0.004023573,0.00089013536,0.061955072,0.5554266,0.0007475061,0.0007059469,0.023675393],"study_design_scores_gemma":[0.000037555088,0.00031776985,0.9047003,0.000005932984,0.000043627653,0.00012739738,0.0012451971,0.06404579,0.028541071,0.000086883425,0.00082406605,0.000024395462],"about_ca_topic_score_codex":0.21479154,"about_ca_topic_score_gemma":0.37551042,"teacher_disagreement_score":0.78520846,"about_ca_system_score_codex":0.0012801497,"about_ca_system_score_gemma":0.0007946505,"threshold_uncertainty_score":0.4270826},"labels":[],"label_agreement":null},{"id":"W3157951468","doi":"10.1785/0320210001","title":"Machine-Learning-Based High-Resolution Earthquake Catalog Reveals How Complex Fault Structures Were Activated during the 2016–2017 Central Italy Sequence","year":2021,"lang":"en","type":"article","venue":"The Seismic Record","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":156,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Basic Energy Sciences; British Geological Survey; Sight Research UK; Directorate for Geosciences; Natural Environment Research Council; U.S. Department of Energy; National Science Foundation","keywords":"Seismology; Aftershock; Geology; Fault (geology); Sequence (biology); Induced seismicity; Event (particle physics); Seismic hazard","score_opus":0.026453223537691736,"score_gpt":0.22689224226455734,"score_spread":0.2004390187268656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157951468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858732,0.00015433763,0.00064572896,0.000054772445,0.000012278255,0.00001405986,0.011049777,0.00013596694,0.0020599056],"genre_scores_gemma":[0.95507413,0.0001851016,0.0012171295,0.000011583014,0.000039552015,0.000026232718,0.042554792,0.000030242405,0.0008611559],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979013,0.000015755137,0.00002530337,0.00006429582,0.0000620602,0.00004252873],"domain_scores_gemma":[0.99908376,0.000064194544,0.00036631248,0.00014146072,0.000222066,0.0001221048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027736826,0.00022993864,0.00035750787,0.0029804986,0.00022416253,0.00048958283,0.00028755696,0.00017941109,0.0010909236],"category_scores_gemma":[0.0010138811,0.00010894189,0.00021741669,0.002884413,0.00026075117,0.00034304237,0.0005921899,0.00016804614,0.0010281565],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001561938,0.000052520474,0.9255475,0.00008383293,0.000075748656,0.00026531503,0.0002676439,0.005089098,0.0054124803,0.00030570553,0.0073357965,0.05540814],"study_design_scores_gemma":[0.0000055590062,0.000017562268,0.9910782,0.000014675014,0.000015534799,0.00009963537,0.00008175407,0.0057202606,0.00047113816,0.00007603671,0.0024117809,0.000007778893],"about_ca_topic_score_codex":0.015607234,"about_ca_topic_score_gemma":0.027775962,"teacher_disagreement_score":0.015607234,"about_ca_system_score_codex":0.00040257617,"about_ca_system_score_gemma":0.0005879026,"threshold_uncertainty_score":0.0310328},"labels":[],"label_agreement":null},{"id":"W3158081413","doi":"10.4095/328261","title":"The 1860 magnitude 6.1 Charlevoix, Quebec, earthquake: macroseismic information and interpretation","year":2021,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Magnitude (astronomy); Seismology; Interpretation (philosophy); Earthquake magnitude; Geology; Geodesy; Geography; Computer science; Physics; Mathematics; Geometry; Programming language","score_opus":0.013538296538324415,"score_gpt":0.23288897371583617,"score_spread":0.21935067717751175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158081413","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18523218,0.0007629924,0.0012489809,0.00069993484,0.00008547021,0.00066747086,0.6796673,0.0007006956,0.13093498],"genre_scores_gemma":[0.5816245,0.0018712545,0.004405712,0.00034027742,0.00007360573,0.00047591148,0.2850598,0.0002404976,0.12590842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996455,0.000016036982,0.0000252301,0.000037000427,0.00020438457,0.000071878116],"domain_scores_gemma":[0.99745995,0.00008415489,0.00019792713,0.00006258001,0.0019933572,0.00020204966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002900444,0.00044430073,0.00019898439,0.005579986,0.0013340991,0.001338242,0.00052537845,0.00023069997,0.03079238],"category_scores_gemma":[0.0020348267,0.0001366604,0.00015171024,0.009962356,0.00029612958,0.00034261437,0.0005132342,0.00022556318,0.0051141707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024149496,0.00007266909,0.52191556,0.00072579604,0.00004134743,0.0006989684,0.0033748404,0.0021785763,0.0030156083,0.001849468,0.3507132,0.11517252],"study_design_scores_gemma":[0.0000076070005,0.0000131615925,0.9052102,0.00008097769,0.0000070341043,0.000075584816,0.0014716317,0.0005085369,0.0002951019,0.00005279736,0.09225646,0.000020984082],"about_ca_topic_score_codex":0.98745817,"about_ca_topic_score_gemma":0.9918371,"teacher_disagreement_score":0.03079238,"about_ca_system_score_codex":0.013241688,"about_ca_system_score_gemma":0.00912625,"threshold_uncertainty_score":0.10301077},"labels":[],"label_agreement":null},{"id":"W3158155962","doi":"","title":"Constraints from Fault Roughness on the Scale-Dependent Strength of Rocks","year":2015,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Surface finish; Slip (aerodynamics); Surface roughness; Geology; Asperity (geotechnical engineering); Fault (geology); Geometry; Hydraulic roughness; Scale (ratio); Aspect ratio (aeronautics); Materials science; Geotechnical engineering; Seismology; Composite material; Engineering; Mathematics; Physics","score_opus":0.0314179368854049,"score_gpt":0.23351782350596692,"score_spread":0.20209988662056202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158155962","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919802,0.00028035464,0.003230648,0.00009030392,0.000004650068,0.0000061244546,0.00017845239,0.000027410075,0.0042019025],"genre_scores_gemma":[0.9996132,0.000041470026,0.0002231018,0.00001046277,0.000003752113,0.00000221228,0.000060910093,0.0000046230666,0.000040340517],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99960333,0.00006941503,0.000027157093,0.00011904477,0.0001110138,0.00007005399],"domain_scores_gemma":[0.99594706,0.002360245,0.00072319683,0.0005471156,0.000215984,0.00020651775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044072932,0.0002800331,0.00035445005,0.0005498698,0.00025488317,0.0008818108,0.0003779235,0.00034670118,0.0012216944],"category_scores_gemma":[0.0050675683,0.00028220296,0.00023345259,0.00029693783,0.0009715099,0.00078006746,0.0007259522,0.00031390958,0.00022689144],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008752059,0.00011678412,0.4232579,0.00030815855,0.0001836461,0.00096128153,0.00047406403,0.022791414,0.5047717,0.0117450785,0.0007101103,0.033804648],"study_design_scores_gemma":[0.00002371249,0.000112462476,0.957396,0.000019669333,0.00004819766,0.0002939597,0.00015366302,0.025401698,0.010053939,0.005988931,0.00045994413,0.000047838552],"about_ca_topic_score_codex":0.0017667288,"about_ca_topic_score_gemma":0.002719719,"teacher_disagreement_score":0.0017667288,"about_ca_system_score_codex":0.00024134897,"about_ca_system_score_gemma":0.00014704274,"threshold_uncertainty_score":0.0040869713},"labels":[],"label_agreement":null},{"id":"W3158159818","doi":"10.1785/0220200297","title":"Source Characterization for Two Small Earthquakes in Dartmouth, Nova Scotia, Canada: Pushing the Limit of Single Station","year":2021,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Seismology; Waveform; Geology; Aftershock; Geodesy; Nova scotia; Amplitude; Source model; Engineering; Telecommunications; Computer science; Physics","score_opus":0.10239880536953935,"score_gpt":0.2900893146392255,"score_spread":0.18769050926968614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158159818","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99340373,0.00010389911,0.0021357683,0.00007914622,0.0000075938096,0.00003387475,0.0018184301,0.00009103369,0.0023266096],"genre_scores_gemma":[0.9966994,0.00005761129,0.0011662788,0.000012554618,0.0000020837795,0.0000073286747,0.0013782516,0.000013644319,0.0006628051],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998709,0.000007380304,0.0000052408614,0.000029921579,0.000049260227,0.000037268914],"domain_scores_gemma":[0.9995283,0.000042471067,0.000049411334,0.000033131368,0.000256535,0.000090184505],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016119712,0.0004406573,0.00021498119,0.001065399,0.00070614205,0.00070344505,0.00067918433,0.00027323747,0.00087734376],"category_scores_gemma":[0.0009226205,0.00017585017,0.00020792533,0.0011133861,0.00025612215,0.00018860566,0.0003908823,0.00021119998,0.00022400804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003645808,0.0001706808,0.8011881,0.00014683732,0.00014553605,0.0021636647,0.0010912617,0.08454005,0.03430766,0.0012851359,0.004356297,0.07024016],"study_design_scores_gemma":[0.000049106413,0.000062776264,0.723253,0.000045015888,0.00006588854,0.00025378578,0.0017787736,0.26521003,0.0052340575,0.0001864199,0.0038023766,0.00005874612],"about_ca_topic_score_codex":0.96014595,"about_ca_topic_score_gemma":0.9709644,"teacher_disagreement_score":0.03985405,"about_ca_system_score_codex":0.0040337327,"about_ca_system_score_gemma":0.006980666,"threshold_uncertainty_score":0.080177486},"labels":[],"label_agreement":null},{"id":"W3158480126","doi":"10.1785/0220210014","title":"Earthquakes in the Eastern Canadian Arctic: Past Occurrences, Present Hazard, and Future Risk","year":2021,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"","keywords":"Mercalli intensity scale; Arctic; Permafrost; Zoning; Seismic hazard; Geology; Seismology; Physical geography; Magnitude (astronomy); Hazard; Active fault; Geography; Ground motion; Peak ground acceleration; Oceanography; Fault (geology); Law","score_opus":0.05275021173206764,"score_gpt":0.2866199637890418,"score_spread":0.23386975205697416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158480126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9838037,0.0027680243,0.0002036681,0.001208885,0.000037122176,0.00002190549,0.003727394,0.000011627862,0.008217556],"genre_scores_gemma":[0.9964083,0.0017232117,0.00014218583,0.000059561375,0.000020737627,0.000005545441,0.00074977573,0.000002072686,0.00088857685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995254,0.000036961705,0.000027631155,0.000036247042,0.00017808423,0.00019565555],"domain_scores_gemma":[0.99835545,0.00010668206,0.00032073568,0.000026269277,0.0008072265,0.0003835172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044452318,0.00029857637,0.0002100192,0.0023003248,0.002806908,0.0013177338,0.00063468324,0.00036532906,0.0022767878],"category_scores_gemma":[0.0018374597,0.00012935855,0.00026734642,0.0050480813,0.00071152323,0.0004572028,0.0009524554,0.00053941587,0.00017118148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000109357665,0.00005409737,0.9753449,0.00008903944,0.00006344649,0.0002705756,0.0011364509,0.00096132566,0.00016371033,0.00057168317,0.002074397,0.019161073],"study_design_scores_gemma":[0.000003136208,0.000024637506,0.98946136,0.00006774122,0.000034060642,0.00010834869,0.0057833553,0.00069519994,0.00006391336,0.00016569566,0.0035691995,0.000023340006],"about_ca_topic_score_codex":0.9872569,"about_ca_topic_score_gemma":0.99349916,"teacher_disagreement_score":0.015722455,"about_ca_system_score_codex":0.015722455,"about_ca_system_score_gemma":0.016458454,"threshold_uncertainty_score":0.114074945},"labels":[],"label_agreement":null},{"id":"W3158601690","doi":"10.1029/2021gl095108","title":"Surface Deformation and Seismicity Induced by Poroelastic Stress at the Raft River Geothermal Field, Idaho, USA","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Science Foundation","keywords":"Induced seismicity; Geology; Poromechanics; Geothermal gradient; Pore water pressure; Basement; Seismology; Stress field; Geotechnical engineering; Geomorphology; Geophysics; Porosity; Porous medium","score_opus":0.028176851456275333,"score_gpt":0.2677490307637777,"score_spread":0.23957217930750238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158601690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652725,0.000015613747,0.00023096241,0.00008014577,0.0000039125225,0.0000069389994,0.0013203985,0.000056603603,0.0017582101],"genre_scores_gemma":[0.9985672,0.000018824909,0.0002602471,0.000016677675,0.0000031726008,0.0000084269805,0.00080145686,0.000005659928,0.00031816424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999391,0.000010009497,0.0000040249793,0.000021457725,0.000012733387,0.000012666108],"domain_scores_gemma":[0.99982184,0.000038665068,0.0000341401,0.000024141702,0.00005427394,0.000027026752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018325071,0.00016072579,0.00012483512,0.0006384231,0.00025006823,0.00032750782,0.00033855927,0.00022753314,0.001177662],"category_scores_gemma":[0.00046030985,0.000122070254,0.00016516856,0.0005185953,0.00020765627,0.00016959937,0.0002480931,0.00018417121,0.00020181804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002633747,0.0001413905,0.94762933,0.00004491763,0.000096518204,0.00027621762,0.00025779824,0.023693,0.009614568,0.00021616607,0.0018903114,0.015876463],"study_design_scores_gemma":[0.000017523036,0.000026089707,0.96842366,0.0000088680135,0.000017370263,0.00004263329,0.00023666523,0.029506652,0.0012000002,0.00006254848,0.000448462,0.000009390556],"about_ca_topic_score_codex":0.08944924,"about_ca_topic_score_gemma":0.15679495,"teacher_disagreement_score":0.08944924,"about_ca_system_score_codex":0.0008302444,"about_ca_system_score_gemma":0.0005182795,"threshold_uncertainty_score":0.17785716},"labels":[],"label_agreement":null},{"id":"W3159054623","doi":"10.5194/egusphere-egu21-3354","title":"Historical evidence warns about disastrous tele-tsunami risk on the coast of East Africa.","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Swahili; Flooding (psychology); Indian ocean; Tanzania; Subduction; Tsunami wave; Oceanography; Seismology; Geology; Coastal flood; Geography; Hazard; Sea level rise; Tectonics; Climate change; Environmental planning","score_opus":0.044900604449136156,"score_gpt":0.21915089447813615,"score_spread":0.174250290029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159054623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9016367,0.034930896,0.0011401173,0.01573115,0.00067159685,0.000020271766,0.0017110765,0.00004709633,0.04411115],"genre_scores_gemma":[0.97699964,0.019090282,0.00046291816,0.0007748425,0.00024688648,0.0000052879946,0.00032903382,0.000007501991,0.0020835102],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998198,0.000039740884,0.000020316402,0.000034980483,0.000042230706,0.000043056898],"domain_scores_gemma":[0.9965629,0.00077146845,0.0016065411,0.00022583615,0.0006332342,0.00020011581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043451018,0.00028503573,0.00009597136,0.0015705416,0.000829394,0.0010011505,0.00031126357,0.00061173167,0.0046970593],"category_scores_gemma":[0.0036193358,0.00016580337,0.00010437176,0.0015467295,0.0012248096,0.0011182256,0.0007424555,0.0007893682,0.00049596763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003789217,0.00005075518,0.7203339,0.0014802259,0.00013250089,0.013269859,0.016065896,0.000707603,0.006426167,0.010923546,0.019211352,0.21101922],"study_design_scores_gemma":[0.000007255054,0.00013622084,0.8521786,0.0011441812,0.00010017739,0.007992889,0.013087881,0.00026675043,0.0019004664,0.0019067079,0.12124004,0.000038984996],"about_ca_topic_score_codex":0.013635405,"about_ca_topic_score_gemma":0.028070247,"teacher_disagreement_score":0.013635405,"about_ca_system_score_codex":0.0010205446,"about_ca_system_score_gemma":0.00046989674,"threshold_uncertainty_score":0.027112067},"labels":[],"label_agreement":null},{"id":"W3160103633","doi":"10.1785/0220210037","title":"Intensity of Induced Earthquakes in Northeast British Columbia, Canada","year":2021,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Geoscience BC","funders":"","keywords":"Mercalli intensity scale; Geology; Seismology; Magnitude (astronomy); Moment magnitude scale; Intensity (physics); Induced seismicity; Structural basin; Amplitude; Ground motion; Geomorphology; Peak ground acceleration; Scaling","score_opus":0.05501250699444127,"score_gpt":0.26457398184583575,"score_spread":0.20956147485139448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3160103633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82667017,0.0006779014,0.00024183631,0.00052355044,0.000027098396,0.00008183819,0.16116856,0.00010236361,0.010506653],"genre_scores_gemma":[0.8990513,0.0011039425,0.0004653568,0.00013425904,0.000012044047,0.00007328177,0.0909643,0.000035802732,0.008159637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99955434,0.000016469547,0.000035418805,0.00007804896,0.0001822433,0.00013352495],"domain_scores_gemma":[0.9974408,0.00008497482,0.00028497752,0.00007872726,0.0017822029,0.00032825588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021256223,0.00041698315,0.00030464117,0.0037429354,0.0011668969,0.0013786264,0.00081439264,0.00026646646,0.002922677],"category_scores_gemma":[0.0017255949,0.00019204633,0.00019356461,0.008934124,0.00039649446,0.00026821112,0.00076794747,0.0003964529,0.0006543579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011383161,0.000051858795,0.9436758,0.00018664244,0.00010933328,0.00036178096,0.0011161016,0.0016616376,0.0010470205,0.00029544544,0.029008064,0.022372505],"study_design_scores_gemma":[0.0000055389214,0.0000037271304,0.9904372,0.000050083312,0.000013052957,0.00003247191,0.0014199748,0.00072599703,0.00017059705,0.000023120938,0.0071024713,0.00001574289],"about_ca_topic_score_codex":0.99645776,"about_ca_topic_score_gemma":0.998365,"teacher_disagreement_score":0.016358579,"about_ca_system_score_codex":0.016358579,"about_ca_system_score_gemma":0.017643446,"threshold_uncertainty_score":0.11869031},"labels":[],"label_agreement":null},{"id":"W3161132630","doi":"","title":"An updated NAD83(CSRS) v7.1 velocity field and hybrid crustal velocity model for Canada","year":2019,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Field (mathematics); Seismology; Geodesy; Mathematics","score_opus":0.014879891169980017,"score_gpt":0.21709269983394874,"score_spread":0.20221280866396873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3161132630","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.062800094,0.00078045175,0.12226057,0.0016418177,0.0007916667,0.00040217055,0.65838706,0.030426577,0.12250959],"genre_scores_gemma":[0.28692612,0.0011958381,0.12659645,0.000528592,0.00010154348,0.00050552824,0.4968389,0.010048684,0.07725834],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999559,0.000025638006,0.00001785338,0.000059255173,0.0002222566,0.00011597507],"domain_scores_gemma":[0.9982798,0.00004442251,0.00003173792,0.00010325333,0.0014437608,0.000096950724],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005125033,0.0010586511,0.000826151,0.0015100014,0.0018178661,0.0017378728,0.00435896,0.0011855322,0.028402448],"category_scores_gemma":[0.0019727468,0.0008888312,0.0010196961,0.003548499,0.00037342147,0.0014498015,0.0008737751,0.001638491,0.015718212],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025215137,0.00014051468,0.014696594,0.00020140392,0.0001233429,0.00018104265,0.00021788651,0.41343972,0.0022294829,0.014647428,0.47250062,0.08136978],"study_design_scores_gemma":[0.00031887172,0.0000279793,0.012706736,0.00017710264,0.00008684103,0.00008275184,0.00024929157,0.613012,0.0029900202,0.0057461536,0.36434317,0.0002590291],"about_ca_topic_score_codex":0.9797258,"about_ca_topic_score_gemma":0.97131515,"teacher_disagreement_score":0.028402448,"about_ca_system_score_codex":0.013228254,"about_ca_system_score_gemma":0.028433332,"threshold_uncertainty_score":0.09597814},"labels":[],"label_agreement":null},{"id":"W3162847895","doi":"10.1029/2020jb019981","title":"New Megathrust Locking Model for the Southern Kurile Subduction Zone Incorporating Viscoelastic Relaxation and Non‐Uniform Compliance of Upper Plate","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Trench; Slip (aerodynamics); Seafloor spreading; Viscoelasticity; Episodic tremor and slip; Tsunami earthquake; Inversion (geology); Geodesy; Geophysics; Tectonics","score_opus":0.07066298588093715,"score_gpt":0.3186622890355948,"score_spread":0.24799930315465762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3162847895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5538296,0.00037795852,0.4379719,0.000229781,0.000047657017,0.000056038458,0.00027992908,0.0004197241,0.006787428],"genre_scores_gemma":[0.98873746,0.00011683284,0.008408051,0.000030576008,0.000011785044,0.00005144286,0.00011087672,0.000042691132,0.0024902883],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999925,0.000013072677,0.0000060638527,0.000022499713,0.000017378508,0.00001597911],"domain_scores_gemma":[0.9998838,0.000021183316,0.000037290796,0.000016514396,0.000021826168,0.000019432842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023082847,0.00049574405,0.0004593703,0.00042007616,0.00023996813,0.00064132566,0.0015521211,0.00073197996,0.0011974279],"category_scores_gemma":[0.00031792498,0.00036678603,0.00083308225,0.00021523469,0.00040374705,0.0007490663,0.00055239286,0.00043312937,0.00024192424],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025689746,0.000019682813,0.0027248631,0.000013820026,0.000030981482,0.000114192386,0.000038286373,0.9847794,0.00579903,0.0034516808,0.00012971768,0.0028726119],"study_design_scores_gemma":[0.00000442625,0.000007000036,0.00023204558,0.0000018895764,0.000004153281,0.000012110387,0.0000035937694,0.99898905,0.00021335045,0.0004151607,0.00011449292,0.0000026910186],"about_ca_topic_score_codex":0.007084357,"about_ca_topic_score_gemma":0.0045979014,"teacher_disagreement_score":0.007084357,"about_ca_system_score_codex":0.0005421646,"about_ca_system_score_gemma":0.000513209,"threshold_uncertainty_score":0.0140862465},"labels":[],"label_agreement":null},{"id":"W3163032978","doi":"10.2118/204157-ms","title":"2000-2020: Two Decades of Evolution of Hydraulic Fracturing-Induced Seismicity in the Western Canada Sedimentary Basin","year":2021,"lang":"en","type":"article","venue":"SPE Hydraulic Fracturing Technology Conference and Exhibition","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Magnitude (astronomy); Structural basin; Maximum magnitude; Seismology; Volume (thermodynamics); Longitude; Sedimentary rock; Permeability (electromagnetism); Latitude; Hydrology (agriculture); Geotechnical engineering; Geomorphology; Geodesy; Geochemistry","score_opus":0.012508809643486258,"score_gpt":0.21829268033755192,"score_spread":0.20578387069406567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3163032978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99366766,0.00016268434,0.00040761812,0.00021992244,0.000008522351,0.000009159695,0.004179565,0.00006716165,0.0012777208],"genre_scores_gemma":[0.99610716,0.000100749414,0.00022043251,0.000021058955,0.0000033005551,0.000003933361,0.0031131282,0.0000071004497,0.00042304577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981827,0.000010563563,0.000009069007,0.000046881716,0.00006465137,0.000050692044],"domain_scores_gemma":[0.99945694,0.00003904489,0.00009485561,0.000025098689,0.0002927035,0.00009134546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004431853,0.00043321733,0.00021138048,0.000990297,0.0005551049,0.0010388176,0.0007767258,0.00046093616,0.0009609469],"category_scores_gemma":[0.0012559323,0.00018895791,0.00037074814,0.0015291579,0.00038424283,0.0004068718,0.00049685437,0.00044683772,0.00021097175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015533,0.0000743979,0.9129892,0.000051978244,0.0001351149,0.00024063326,0.00038560168,0.067863874,0.0011804701,0.0006689014,0.0032549854,0.012999427],"study_design_scores_gemma":[0.0000147120145,0.000030857787,0.8597487,0.00004935172,0.000044655644,0.00004586812,0.0009733707,0.1347983,0.00072436314,0.00020233217,0.0033332338,0.00003417695],"about_ca_topic_score_codex":0.95642275,"about_ca_topic_score_gemma":0.9614197,"teacher_disagreement_score":0.043577254,"about_ca_system_score_codex":0.009948482,"about_ca_system_score_gemma":0.0064105447,"threshold_uncertainty_score":0.0876677},"labels":[],"label_agreement":null},{"id":"W3164368877","doi":"10.5194/egusphere-egu21-10233","title":"Distinguishing between hurricane and tsunami deposition using modern analogues from Anegada, British Virgin Islands (BVI)","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Storm; Storm surge; Deposition (geology); Erosion; Geology; Oceanography; Trench; Coastal erosion; Sediment; Geomorphology","score_opus":0.02320402041497953,"score_gpt":0.22332521799420094,"score_spread":0.20012119757922142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3164368877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9815491,0.00039691248,0.00031043927,0.00010319883,0.000020156052,0.000029625047,0.0057154824,0.000027860562,0.011847404],"genre_scores_gemma":[0.98727614,0.00030853716,0.0016420771,0.00010847966,0.000016380525,0.000038056383,0.008028111,0.000029924086,0.0025523058],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998822,0.000010213211,0.000014603041,0.00004200635,0.000028974115,0.00002187229],"domain_scores_gemma":[0.9993412,0.000043220756,0.000118263655,0.00006413275,0.0003417575,0.000091389855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017160148,0.00024116128,0.00016899918,0.0014420507,0.0007914606,0.00075050705,0.00038889196,0.0002961812,0.0024151546],"category_scores_gemma":[0.00061197806,0.00014911577,0.00016035947,0.002844612,0.0004939516,0.0002482701,0.00056273106,0.00031049387,0.00064249564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019820628,0.00007829658,0.9385839,0.00015152502,0.00014108582,0.0009895205,0.0035569645,0.000735883,0.009696311,0.0002814708,0.004761567,0.040825244],"study_design_scores_gemma":[0.0000041095327,0.000005994517,0.9924948,0.000023035742,0.0000117659665,0.00010155766,0.001022789,0.00014160323,0.00020415147,0.000018254674,0.0059667183,0.0000051548677],"about_ca_topic_score_codex":0.7061955,"about_ca_topic_score_gemma":0.91238517,"teacher_disagreement_score":0.7061955,"about_ca_system_score_codex":0.0014666371,"about_ca_system_score_gemma":0.00082333555,"threshold_uncertainty_score":0.5910696},"labels":[],"label_agreement":null},{"id":"W3164731713","doi":"10.1016/j.jvolgeores.2021.107295","title":"The Independent Volcanic Eruption Source Parameter Archive (IVESPA, version 1.0): A new observational database to support explosive eruptive column model validation and development","year":2021,"lang":"en","type":"article","venue":"Journal of Volcanology and Geothermal Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Climate Program Office; H2020 Marie Skłodowska-Curie Actions; Biological and Environmental Research; FP7 Coherent Development of Research Policies; Sidney Sussex College, University of Cambridge; Office of Science; U.S. Geological Survey; British Geological Survey; U.S. Department of Energy; European Commission; National Oceanic and Atmospheric Administration; Sight Research UK; Royal Society; Natural Environment Research Council","keywords":"Geology; Volcano; Explosive material; Explosive eruption; Seismology; Column (typography); Observational study; Database; Pyroclastic rock; Archaeology; Computer science; History","score_opus":0.12879842392550958,"score_gpt":0.3301680125223736,"score_spread":0.20136958859686402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3164731713","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.019164536,0.00051832106,0.03161527,0.00016131616,0.00008663551,0.0002054077,0.9228146,0.020533608,0.0049003228],"genre_scores_gemma":[0.030888597,0.00033833776,0.026992613,0.00006818884,0.000033207525,0.00033275955,0.93740994,0.002905923,0.0010304342],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977749,0.0002433025,0.00053698674,0.00050007034,0.00081453664,0.00013015048],"domain_scores_gemma":[0.9860715,0.0035057806,0.0020211993,0.004620116,0.003223636,0.00055766536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003886453,0.0014251189,0.0012860267,0.006067725,0.0004918442,0.002144991,0.0029743905,0.0016163598,0.007494117],"category_scores_gemma":[0.015894245,0.0010470344,0.0013826361,0.0058622058,0.0005443741,0.004088363,0.0024206154,0.0017538428,0.00784807],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010816659,0.0003731475,0.14263357,0.004969541,0.000733303,0.00073618046,0.0014737953,0.068582274,0.010798836,0.0091694845,0.56525296,0.19419524],"study_design_scores_gemma":[0.00039031313,0.00014390901,0.12358612,0.0009997414,0.00026644382,0.00043173032,0.00037072686,0.07875843,0.011796994,0.006554751,0.77629554,0.00040521342],"about_ca_topic_score_codex":0.021526022,"about_ca_topic_score_gemma":0.017287122,"teacher_disagreement_score":0.021526022,"about_ca_system_score_codex":0.00096365204,"about_ca_system_score_gemma":0.0027486167,"threshold_uncertainty_score":0.04280144},"labels":[],"label_agreement":null},{"id":"W3166770423","doi":"10.5194/egusphere-egu21-9819","title":"Vertical velocity fields along the Eastern Mediterranean coast as revealed by late Holocene sea-level markers","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Post-glacial rebound; Holocene; Geology; Lithosphere; Sea level; Tectonics; Subsidence; Oceanography; Vertical displacement; Geodesy; Geomorphology; Paleontology; Structural basin","score_opus":0.03310032446278959,"score_gpt":0.23613067198515353,"score_spread":0.20303034752236393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3166770423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98973364,0.00013975674,0.00057459547,0.000060083803,0.000024819554,0.000007585109,0.0030227844,0.00009516494,0.0063415505],"genre_scores_gemma":[0.99504846,0.00010697782,0.0010756113,0.00000888193,0.000009448761,0.000007274789,0.0022421824,0.000011326441,0.0014897644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996483,0.0000041761023,0.0000031798543,0.0000126982195,0.000007339696,0.000007700126],"domain_scores_gemma":[0.9998684,0.000014078828,0.000031092644,0.000010878902,0.000054880293,0.000020737585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009998341,0.00016188443,0.00007982587,0.0007975153,0.0000938407,0.00029475248,0.000111761095,0.00015403242,0.0020106253],"category_scores_gemma":[0.00037580437,0.00006487215,0.00010338586,0.00082816515,0.000089472196,0.00010848255,0.00011894973,0.00008925038,0.0005329997],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020893503,0.00003193232,0.8657917,0.000043536846,0.000057325167,0.0002686189,0.00073034165,0.0027024732,0.011175996,0.0007113719,0.004316934,0.113960885],"study_design_scores_gemma":[0.000004292734,0.00001823303,0.9951904,0.000008235736,0.000004948234,0.000024472454,0.00009956924,0.0015797968,0.00027259276,0.00004942841,0.0027440763,0.0000039547267],"about_ca_topic_score_codex":0.01883847,"about_ca_topic_score_gemma":0.02685235,"teacher_disagreement_score":0.01883847,"about_ca_system_score_codex":0.0002513684,"about_ca_system_score_gemma":0.0001104337,"threshold_uncertainty_score":0.037457645},"labels":[],"label_agreement":null},{"id":"W3167607589","doi":"10.1111/1755-6724.14724","title":"Tectonic Characteristics, Evolution, and Significance of the Zhouwang Fault, Lower Yangtze Area, Eastern China","year":2021,"lang":"en","type":"article","venue":"Acta Geologica Sinica - English Edition","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Sinistral and dextral; Geology; Tectonics; Nappe; Fault (geology); Strike-slip tectonics; Seismology; Thrust fault; Stress field; Compression (physics); Paleontology","score_opus":0.012147835541129892,"score_gpt":0.19683313411616335,"score_spread":0.18468529857503346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3167607589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99960595,0.00009370728,0.00003531715,0.000020991396,7.146524e-7,0.0000024053709,0.000066184744,0.0000025559636,0.00017223493],"genre_scores_gemma":[0.9995975,0.00006243258,0.00003822462,0.0000041969947,0.0000017176695,0.0000021853064,0.00014216221,6.295843e-7,0.00015095124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984896,0.000015941549,0.0000169946,0.00005170394,0.000033362525,0.00003296494],"domain_scores_gemma":[0.9997613,0.000027284652,0.00007842351,0.00001447149,0.00005264398,0.000065810746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029020788,0.00032962812,0.00020974225,0.0016666553,0.0005699701,0.00046349186,0.00022422535,0.00025307143,0.000524984],"category_scores_gemma":[0.00031932566,0.00018369277,0.00018259438,0.0022391428,0.0005813091,0.0003090659,0.00040926773,0.000116417825,0.000056555607],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047975518,0.0000149657235,0.98251915,0.00004902516,0.00006209092,0.00034845865,0.0008148422,0.000897111,0.007133891,0.00024751882,0.00008767143,0.0077771996],"study_design_scores_gemma":[0.0000031615903,0.000012992482,0.999044,0.0000030766755,0.000008735744,0.000048807964,0.0002484727,0.00028597203,0.00010484557,0.00003185395,0.00020499165,0.0000031659079],"about_ca_topic_score_codex":0.052303407,"about_ca_topic_score_gemma":0.10671753,"teacher_disagreement_score":0.052303407,"about_ca_system_score_codex":0.0010162189,"about_ca_system_score_gemma":0.001073788,"threshold_uncertainty_score":0.103997946},"labels":[],"label_agreement":null},{"id":"W3167725001","doi":"10.5194/egusphere-egu21-6324","title":"Modeling the Interaction between Slow Slip Events and Earthquake Ruptures in the Nicoya Peninsula, Costa Rica.&amp;#160;","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Subduction; Seismology; Geology; Slip (aerodynamics); Homogeneous; Peninsula; Episodic tremor and slip; Tectonics; Geography","score_opus":0.04511982343237628,"score_gpt":0.2658564023788692,"score_spread":0.22073657894649293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3167725001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98544353,0.0006831492,0.0029725593,0.00064178684,0.000041589235,0.000038075937,0.0011078089,0.00012424865,0.008947318],"genre_scores_gemma":[0.99565375,0.00020303372,0.0016629896,0.000050372357,0.000013900795,0.000030454808,0.00041361243,0.000025006379,0.0019468674],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999062,0.000028033577,0.000005964255,0.0000209977,0.000011070984,0.000027781907],"domain_scores_gemma":[0.9996984,0.00014471664,0.00005014507,0.000015717227,0.000051540304,0.0000395899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021973287,0.00069210987,0.00042903135,0.0005687691,0.00047894032,0.001196685,0.0009004875,0.0012679066,0.002017896],"category_scores_gemma":[0.0010387305,0.00039699694,0.00054777367,0.0004927088,0.0004138953,0.00043895704,0.0006594129,0.0005064399,0.00016545798],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039073195,0.000070683214,0.016191969,0.00003139784,0.00005676838,0.0001890014,0.000042280077,0.9801152,0.00055799354,0.0006700042,0.00047617694,0.0015594505],"study_design_scores_gemma":[0.000009405568,0.000008979461,0.0048516663,0.000005865782,0.000012147079,0.000012009099,0.000080010024,0.9944969,0.00006540555,0.00011176384,0.00033988775,0.0000059687836],"about_ca_topic_score_codex":0.28102702,"about_ca_topic_score_gemma":0.22622487,"teacher_disagreement_score":0.28102702,"about_ca_system_score_codex":0.0017249804,"about_ca_system_score_gemma":0.0013366562,"threshold_uncertainty_score":0.5587825},"labels":[],"label_agreement":null},{"id":"W3167803131","doi":"10.1016/j.tecto.2021.228953","title":"Inversion structures across the crest of the Larnaka Ridge associated with strike-slip faulting during the uppermost Messinian–Quaternary, eastern Mediterranean","year":2021,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Quaternary; Crest; Seismology; Ridge; Inversion (geology); Strike-slip tectonics; Paleontology; Mediterranean climate; Fault (geology); Tectonics","score_opus":0.018054063330844576,"score_gpt":0.22416691828181995,"score_spread":0.20611285495097537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3167803131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947983,0.000013451052,0.000022799893,0.000010192912,0.0000015267899,0.0000010877012,0.000036232737,0.0000018349175,0.00043313208],"genre_scores_gemma":[0.99975663,0.000006782083,0.00002265034,0.0000024480312,0.0000017955243,8.857815e-7,0.000060148846,8.967563e-7,0.00014775287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999436,0.0000063802067,0.000004396597,0.000017780916,0.000006673575,0.00002113716],"domain_scores_gemma":[0.99983084,0.000021501755,0.000061148035,0.000008541649,0.000044381053,0.00003358064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010876419,0.00010488948,0.0001493705,0.00046342297,0.000306267,0.00040501182,0.00016496221,0.0002449971,0.0013101746],"category_scores_gemma":[0.00037350177,0.00010215967,0.00011002796,0.000354023,0.00037471062,0.00014572925,0.00033130642,0.00013705452,0.0001555724],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049353676,0.00006455372,0.95735997,0.00002697765,0.00006220718,0.0006543808,0.0025803545,0.00077700894,0.026812397,0.00034675223,0.00036596454,0.010455878],"study_design_scores_gemma":[0.0000040715686,0.000010199994,0.9991617,0.0000023802327,0.0000042090387,0.000030374287,0.00026604166,0.000260565,0.00010507875,0.0000140401535,0.0001398017,0.0000013969627],"about_ca_topic_score_codex":0.019938886,"about_ca_topic_score_gemma":0.04952701,"teacher_disagreement_score":0.019938886,"about_ca_system_score_codex":0.0004538813,"about_ca_system_score_gemma":0.00031799165,"threshold_uncertainty_score":0.03964567},"labels":[],"label_agreement":null},{"id":"W3168166300","doi":"10.1093/gji/ggab234","title":"Lateral fluid propagation and strike slip fault reactivation related to hydraulic fracturing and induced seismicity in the Duvernay Formation, Fox Creek area, Alberta","year":2021,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Geology; Hydraulic fracturing; Seismology; Induced seismicity; Fault (geology); Shear (geology); Fluid pressure; Pore water pressure; Overpressure; Petrology; Slip (aerodynamics); Geotechnical engineering","score_opus":0.014474821899118546,"score_gpt":0.22695142986330147,"score_spread":0.2124766079641829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3168166300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993777,0.000016884402,0.000050869236,0.000012411475,4.054663e-7,0.0000029337532,0.00011117721,0.000005511279,0.0004220908],"genre_scores_gemma":[0.9993393,0.000024093122,0.00008565761,0.000002612057,3.1366943e-7,0.0000014788315,0.00013170623,0.0000011313102,0.00041361238],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999032,0.0000063489874,0.000005101307,0.000020510288,0.00003173199,0.00003315243],"domain_scores_gemma":[0.99987423,0.000023903054,0.000025202131,0.000007048648,0.000036392754,0.000033259326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012390464,0.0001717873,0.00012373533,0.00066264503,0.00050480297,0.0006721581,0.0004691934,0.00030234925,0.0010714357],"category_scores_gemma":[0.0003705918,0.00016262256,0.00022624919,0.00072078063,0.00053139945,0.00015165325,0.00034792908,0.00014473978,0.000083001076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018395126,0.00012377836,0.9195236,0.000044999346,0.000066143046,0.001120344,0.0008628396,0.058916803,0.0060123713,0.0007022738,0.0004571175,0.011985861],"study_design_scores_gemma":[0.000012471265,0.00005244864,0.95461494,0.000009597545,0.000019508088,0.00007945418,0.0011619373,0.042843133,0.0005859148,0.00008719704,0.000518307,0.000015136469],"about_ca_topic_score_codex":0.88891095,"about_ca_topic_score_gemma":0.94482183,"teacher_disagreement_score":0.11108905,"about_ca_system_score_codex":0.006119512,"about_ca_system_score_gemma":0.0032919121,"threshold_uncertainty_score":0.22348648},"labels":[],"label_agreement":null},{"id":"W3169195831","doi":"","title":"Crustal Seismic Attenuation of Western Canada from Lg Q Inversions","year":2019,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Attenuation; Geodesy; Physics","score_opus":0.014514735325648455,"score_gpt":0.1989153076705145,"score_spread":0.18440057234486604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3169195831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9825116,0.00019009823,0.00037767674,0.00018280836,0.000018440078,0.000011797666,0.0075295493,0.00016192804,0.009016263],"genre_scores_gemma":[0.9920473,0.000117469586,0.000357324,0.000037166337,0.0000048620973,0.000003992901,0.004595672,0.00006468389,0.0027716095],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997601,0.000009551131,0.000010344683,0.000046947796,0.00007951345,0.00009353965],"domain_scores_gemma":[0.99915576,0.00005134998,0.000047291294,0.000033032313,0.0006175614,0.00009500571],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028784497,0.00042921418,0.00024968325,0.0011700662,0.0010208222,0.001297652,0.0005448693,0.00035894447,0.004317249],"category_scores_gemma":[0.0015957123,0.00027095331,0.00024943435,0.0026108355,0.00038842714,0.00033365996,0.00055968534,0.00046254075,0.0007253388],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021920505,0.00017667506,0.7330368,0.00024470445,0.00046707183,0.0012977453,0.0026360396,0.051900797,0.056878187,0.0019594221,0.024682248,0.12452821],"study_design_scores_gemma":[0.00004390213,0.000016504106,0.9821293,0.000033047476,0.0000712778,0.000052961226,0.0006675968,0.010714223,0.0016997746,0.00011232322,0.004421419,0.000037734673],"about_ca_topic_score_codex":0.98496544,"about_ca_topic_score_gemma":0.98915195,"teacher_disagreement_score":0.015034556,"about_ca_system_score_codex":0.0059500085,"about_ca_system_score_gemma":0.0114694135,"threshold_uncertainty_score":0.04317051},"labels":[],"label_agreement":null},{"id":"W3169376344","doi":"10.5194/egusphere-egu21-6421","title":"Latent seismicity driven by aseismic creep and enhanced pore-fluid pressure in NE British Columbia","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Hydraulic fracturing; Seismology; Geology; Pore water pressure; Aftershock; Period (music); Geotechnical engineering; Physics","score_opus":0.007060313967984386,"score_gpt":0.18369683452457794,"score_spread":0.17663652055659357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3169376344","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948079,0.00009011524,0.00006157081,0.00014528842,0.000004493943,0.000011953886,0.0010956663,0.000022052836,0.0037609767],"genre_scores_gemma":[0.99771607,0.00009062232,0.00006194781,0.000029339199,0.0000021483927,0.000006929042,0.00060264545,0.0000050659537,0.0014852469],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998573,0.000007011341,0.000007688469,0.000027029102,0.000036469166,0.00006441228],"domain_scores_gemma":[0.9995034,0.000027940734,0.000060852424,0.00001848701,0.00024614253,0.00014309591],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009552853,0.00023601766,0.00019186916,0.0012386527,0.0014367473,0.001020598,0.0005665325,0.00036271347,0.0026900417],"category_scores_gemma":[0.0005919368,0.00019126218,0.000103741084,0.0018696951,0.0006037088,0.00022490731,0.00066440745,0.00043251851,0.00032925376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020830354,0.000087903325,0.95557696,0.00009740327,0.000066961016,0.0017670889,0.0022266963,0.0020245472,0.011282642,0.00036512016,0.0043845354,0.02191185],"study_design_scores_gemma":[0.0000057408274,0.000007535359,0.9958033,0.000017236278,0.000008783528,0.000061811836,0.0013723426,0.0008799413,0.00016696614,0.000020939779,0.0016438628,0.000011506564],"about_ca_topic_score_codex":0.97965276,"about_ca_topic_score_gemma":0.99451303,"teacher_disagreement_score":0.020347238,"about_ca_system_score_codex":0.008079444,"about_ca_system_score_gemma":0.0069236094,"threshold_uncertainty_score":0.05862069},"labels":[],"label_agreement":null},{"id":"W3170754246","doi":"10.1029/2021jb021963","title":"A Granular Jamming Model for Low‐Frequency Earthquakes","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada","keywords":"Slip (aerodynamics); Jamming; Seismology; Seismic moment; Geology; Granular material; Context (archaeology); Physics; Mechanics; Geotechnical engineering; Condensed matter physics; Fault (geology)","score_opus":0.06489501007304425,"score_gpt":0.33444373737440697,"score_spread":0.2695487273013627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3170754246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88440967,0.00039352453,0.10068691,0.0008281161,0.00007802825,0.00008955927,0.0009397299,0.0004334326,0.012140961],"genre_scores_gemma":[0.9956428,0.00011014885,0.0015570222,0.00002288587,0.000023628203,0.000022565291,0.00017646764,0.000023969644,0.0024205702],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998105,0.0000401832,0.000008967709,0.00003925861,0.000039591956,0.00006158519],"domain_scores_gemma":[0.99917287,0.0002847236,0.0002303239,0.000053634172,0.000105376166,0.00015298257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000630747,0.00043108012,0.0006093738,0.0014568515,0.0008105773,0.0019300671,0.0013133379,0.0010047881,0.0033559978],"category_scores_gemma":[0.0026556018,0.00031312768,0.00059537153,0.00082245807,0.000975482,0.0011308048,0.0007562739,0.0006952159,0.00045818862],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015404022,0.00011431478,0.020051168,0.00004364768,0.00005983714,0.00056246755,0.00019616494,0.91098,0.0017245122,0.058415134,0.0019205784,0.005778195],"study_design_scores_gemma":[0.00000873036,0.000007785898,0.0010422833,0.0000030635867,0.0000056964586,0.000020712438,0.00001841953,0.99471223,0.000023284445,0.00399889,0.00015485399,0.000004106611],"about_ca_topic_score_codex":0.0424557,"about_ca_topic_score_gemma":0.019746827,"teacher_disagreement_score":0.0424557,"about_ca_system_score_codex":0.0014589243,"about_ca_system_score_gemma":0.00079730793,"threshold_uncertainty_score":0.084417164},"labels":[],"label_agreement":null},{"id":"W3171002081","doi":"","title":"1,500-yr record of paleotsunamis impacting Ahuriri Lagoon (Hawke's Bay), New Zealand","year":2021,"lang":"en","type":"article","venue":"SFU Undergraduate Research Symposium Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Bay; Radiocarbon dating; Submarine pipeline; Seismology; Oceanography; Paleontology; Tectonics","score_opus":0.04794085789217964,"score_gpt":0.31358803981383887,"score_spread":0.26564718192165926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3171002081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939995,0.00023969743,0.00007701665,0.00003948513,0.000004429762,0.000017573731,0.0043956186,0.000009108545,0.0012176377],"genre_scores_gemma":[0.9923423,0.0007971351,0.0002977289,0.000029341578,0.000011299269,0.000025107667,0.0050564315,0.0000051283596,0.0014353859],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999118,0.0000036498238,0.000012958087,0.000029276678,0.000022450975,0.000019910256],"domain_scores_gemma":[0.99951315,0.000023134546,0.00018494308,0.000029081328,0.00014728095,0.00010248124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017679554,0.0002997069,0.0001890783,0.0022368704,0.00069443916,0.0005286547,0.00027259035,0.00018421635,0.0013589633],"category_scores_gemma":[0.0004662539,0.00021726915,0.00015809742,0.0019951968,0.0003898463,0.00039626946,0.0006156617,0.00028248725,0.00030691066],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006047833,0.00002790494,0.97878677,0.00007321815,0.00006427596,0.0005698493,0.0018905058,0.000116799485,0.0050388686,0.000031279244,0.00081226445,0.012527936],"study_design_scores_gemma":[0.0000010638907,0.00000596632,0.99908733,0.0000047493127,0.0000051672023,0.000040131777,0.00024925958,0.000021732298,0.00005963757,0.0000019690226,0.000521368,0.0000015022322],"about_ca_topic_score_codex":0.41452056,"about_ca_topic_score_gemma":0.68732285,"teacher_disagreement_score":0.41452056,"about_ca_system_score_codex":0.0012755614,"about_ca_system_score_gemma":0.00061004004,"threshold_uncertainty_score":0.82421553},"labels":[],"label_agreement":null},{"id":"W3172790783","doi":"10.1016/j.tecto.2021.228952","title":"Outer Cilicia Basin – A piggy back basin developed in an intramontane setting following the partitioning of a large ancestral Miocene basin across the northeastern Mediterranean","year":2021,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Istanbul Teknik Üniversitesi; Natural Sciences and Engineering Research Council of Canada; Memorial University of Newfoundland; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Geology; Structural basin; Mediterranean Basin; Paleontology; Sedimentary basin analysis; Mediterranean climate; Sedimentary basin; Archaeology; Geography","score_opus":0.03174624335387173,"score_gpt":0.27398622747081525,"score_spread":0.24223998411694353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3172790783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9773666,0.0003474401,0.00048386303,0.00010942185,0.000018750194,0.00003527395,0.00024513318,0.00008822195,0.02130524],"genre_scores_gemma":[0.99643075,0.000100096695,0.00036550112,0.000059653674,0.000010974275,0.00001255176,0.000286253,0.000013600452,0.0027206535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999267,0.0000033315753,0.0000032058672,0.000024598867,0.000014175063,0.00002799349],"domain_scores_gemma":[0.9999361,0.000005520156,0.000018283132,0.000010647018,0.000014642862,0.000014860467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009387552,0.00020495217,0.00021430133,0.0005054688,0.00064963906,0.00060654635,0.00025203096,0.0003464144,0.0017833106],"category_scores_gemma":[0.0002589515,0.00012142129,0.00030597078,0.00031566466,0.0007411516,0.00017611463,0.0010591309,0.00020230933,0.00029409816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007554223,0.00010218187,0.7495704,0.00030616345,0.00012224018,0.003730014,0.004334312,0.0017100358,0.09979018,0.0066645024,0.0026121761,0.13030241],"study_design_scores_gemma":[0.000014728751,0.000037265712,0.9890592,0.00001648905,0.000017076885,0.0004222189,0.00034214035,0.00033857717,0.0008749438,0.00017295271,0.008699878,0.00000442455],"about_ca_topic_score_codex":0.019557444,"about_ca_topic_score_gemma":0.03179111,"teacher_disagreement_score":0.019557444,"about_ca_system_score_codex":0.0012607006,"about_ca_system_score_gemma":0.00085514865,"threshold_uncertainty_score":0.038887203},"labels":[],"label_agreement":null},{"id":"W3172900029","doi":"10.1785/0120210026","title":"First Use of Fragile Geologic Features to Set the Design Motions for a Major Existing Engineered Structure","year":2021,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Fragility; Seismic hazard; Seismology; Fault (geology); Geology; Hazard; Physics","score_opus":0.04613911061600803,"score_gpt":0.2322831035515569,"score_spread":0.18614399293554887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3172900029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.73420924,0.00004594392,0.25342202,0.00018453474,0.000024651159,0.00014953944,0.00040337854,0.0021007718,0.009459935],"genre_scores_gemma":[0.9324788,0.000010679705,0.06635534,0.000029374442,0.000003913725,0.000033156593,0.00011777365,0.000073675066,0.0008973548],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9994037,0.000114075614,0.00004142272,0.00009775137,0.00026795312,0.00007504256],"domain_scores_gemma":[0.9975479,0.0008724351,0.00050572905,0.0006313194,0.0003494571,0.00009303808],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001305427,0.0003558736,0.00017296695,0.00057619915,0.00031278454,0.00053852715,0.00058766286,0.00030708482,0.001952716],"category_scores_gemma":[0.0050077746,0.0002072498,0.00026403763,0.0001651599,0.00080608705,0.0005316751,0.0008625313,0.00044203852,0.00030706462],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039047937,0.00025866297,0.10589934,0.00023672501,0.000092689144,0.001304599,0.0019384043,0.28750926,0.14229214,0.067072906,0.004277844,0.38872698],"study_design_scores_gemma":[0.00012358217,0.002427046,0.06975784,0.00018091426,0.00007175822,0.0011951575,0.0006692028,0.6659338,0.16926797,0.03173907,0.058452513,0.00018122508],"about_ca_topic_score_codex":0.002526697,"about_ca_topic_score_gemma":0.0064825425,"teacher_disagreement_score":0.002526697,"about_ca_system_score_codex":0.0008840823,"about_ca_system_score_gemma":0.00071147474,"threshold_uncertainty_score":0.006903887},"labels":[],"label_agreement":null},{"id":"W3172930586","doi":"10.1155/2021/9997597","title":"A Numerical Investigation of the Hazardous Injection Area of Induced Earthquake during Hydraulic Fracturing","year":2021,"lang":"en","type":"article","venue":"Shock and Vibration","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Suzhou University; University of Alberta","keywords":"Hydraulic fracturing; Geology; Hazardous waste; Geotechnical engineering; Petroleum engineering; Mining engineering; Seismology; Engineering; Waste management","score_opus":0.017610479726060883,"score_gpt":0.2037049395827515,"score_spread":0.1860944598566906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3172930586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98754627,0.000116772455,0.008705694,0.00012563102,0.00002108032,0.000027417096,0.0000930668,0.00007801649,0.0032860725],"genre_scores_gemma":[0.99824107,0.000031140957,0.0013989317,0.000008918614,0.0000030494214,0.000012700313,0.00003057556,0.0000057569446,0.00026769907],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998877,0.00002087448,0.00000923256,0.00002195703,0.000022134054,0.000038141945],"domain_scores_gemma":[0.9994106,0.00030051862,0.000115419774,0.000027857737,0.00007897607,0.00006651518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027266314,0.000406274,0.00045824214,0.00058826304,0.00062345096,0.00049108505,0.00045208377,0.0009607826,0.0011741179],"category_scores_gemma":[0.0010831867,0.00030589118,0.00055222964,0.00031793225,0.00078874227,0.00054919696,0.00051834126,0.0004770235,0.000056101497],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110569796,0.000118818585,0.015527452,0.00009141852,0.000037113252,0.00059244904,0.00012338611,0.97116125,0.007809927,0.0011206232,0.0002642577,0.0030428597],"study_design_scores_gemma":[0.000013982692,0.0000416155,0.001955443,0.0000037175032,0.000011929867,0.000020262385,0.000050519455,0.99708253,0.0006454178,0.00010018997,0.00006821484,0.0000061444475],"about_ca_topic_score_codex":0.012641996,"about_ca_topic_score_gemma":0.0063484856,"teacher_disagreement_score":0.012641996,"about_ca_system_score_codex":0.00043965617,"about_ca_system_score_gemma":0.0005566605,"threshold_uncertainty_score":0.025136828},"labels":[],"label_agreement":null},{"id":"W3174433284","doi":"10.1016/j.earscirev.2021.103719","title":"Miocene–Quaternary tectonic, kinematic and sedimentary evolution of the eastern Mediterranean Sea: A regional synthesis","year":2021,"lang":"en","type":"article","venue":"Earth-Science Reviews","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Istanbul Teknik Üniversitesi; Natural Sciences and Engineering Research Council of Canada; Dokuz Eylül Üniversitesi; Memorial University of Newfoundland; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Geology; Quaternary; Paleontology; Subduction; Forearc; Late Miocene; Neogene; Tectonics; Sedimentary rock; Isopach map; Anticline; Seismology; Structural basin; Facies","score_opus":0.03834499858093346,"score_gpt":0.246723936817173,"score_spread":0.20837893823623954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3174433284","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.41456065,0.5695535,0.00060032326,0.0033786253,0.00028172994,0.000017548506,0.0021605506,0.00003277158,0.009414371],"genre_scores_gemma":[0.8108999,0.18275818,0.00060211524,0.000641129,0.0005770152,0.000015224256,0.0016120662,0.000017988821,0.0028763853],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99984264,0.00003317604,0.00002708222,0.000051119434,0.000020738891,0.000025236282],"domain_scores_gemma":[0.999603,0.000088904984,0.00015547208,0.000035499794,0.00009877526,0.00001832343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007882516,0.00033177392,0.00032944907,0.001713403,0.00014771403,0.0005817303,0.00046056352,0.00027424752,0.002504672],"category_scores_gemma":[0.0014458403,0.0001260634,0.00037569102,0.003275348,0.00028102,0.00044513718,0.00041672285,0.00024172482,0.0002455862],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046445217,0.000061469174,0.2945707,0.010560262,0.002684801,0.00062627683,0.0047824103,0.00781446,0.005168662,0.0052336347,0.016965214,0.65106755],"study_design_scores_gemma":[0.0000096547665,0.000052851035,0.9589328,0.0007122551,0.0003826523,0.00009080264,0.00055706286,0.00023871212,0.00016552603,0.00036652808,0.038482115,0.000009095365],"about_ca_topic_score_codex":0.0368265,"about_ca_topic_score_gemma":0.07046714,"teacher_disagreement_score":0.0368265,"about_ca_system_score_codex":0.0009850506,"about_ca_system_score_gemma":0.0009407139,"threshold_uncertainty_score":0.07322425},"labels":[],"label_agreement":null},{"id":"W3175033296","doi":"10.5194/egusphere-egu21-10998","title":"Small wavelength features of the strain rate distribution for the St. Lawrence paleo-rift zone, eastern Canada","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Intraplate earthquake; Induced seismicity; Rift; Seismology; Post-glacial rebound; Geodetic datum; Tectonics; East African Rift; Seismic hazard; Rift zone; Deformation (meteorology); Strain rate; Glacial period; Geodesy; Paleontology; Oceanography","score_opus":0.019899034500477232,"score_gpt":0.19813266905530247,"score_spread":0.17823363455482524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175033296","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98679614,0.00023931064,0.00067602197,0.00006762792,0.0000045321194,0.000018731944,0.0069290665,0.00011225296,0.0051562157],"genre_scores_gemma":[0.9928964,0.00012257848,0.00086265843,0.000009939454,0.0000016261388,0.0000068749246,0.004140391,0.000015705406,0.0019438916],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989414,0.0000025910974,0.0000051429474,0.000024240162,0.000038103863,0.000035705874],"domain_scores_gemma":[0.99972445,0.000019205525,0.000028131259,0.0000124429735,0.00017735743,0.00003844405],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000113445996,0.00024650298,0.00014678483,0.001822293,0.00053661875,0.0006919483,0.00041303626,0.00020240618,0.0018049893],"category_scores_gemma":[0.00046425508,0.00011501165,0.00015617031,0.002480497,0.00022889786,0.00012283225,0.0001758552,0.00014095941,0.0002976805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010564956,0.000048425376,0.90000325,0.0000741955,0.00008733584,0.00030025837,0.0005078787,0.028568616,0.0063842363,0.0009982501,0.004465577,0.058456287],"study_design_scores_gemma":[0.0000058781657,0.0000039339347,0.98345953,0.00000879496,0.000007189542,0.000040909745,0.00019882877,0.014253728,0.0004290047,0.00004225947,0.0015402859,0.000009657716],"about_ca_topic_score_codex":0.9796147,"about_ca_topic_score_gemma":0.991165,"teacher_disagreement_score":0.020385325,"about_ca_system_score_codex":0.0050898436,"about_ca_system_score_gemma":0.003987706,"threshold_uncertainty_score":0.041010678},"labels":[],"label_agreement":null},{"id":"W3175365105","doi":"10.2118/206713-pa","title":"Comprehensive Characterization and Mitigation of Hydraulic Fracturing-Induced Seismicity in Fox Creek, Alberta","year":2021,"lang":"en","type":"article","venue":"SPE Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Hydraulic fracturing; Geomechanics; Geology; Poromechanics; Seismology; Pore water pressure; Fracture (geology); Geotechnical engineering","score_opus":0.017048853998031438,"score_gpt":0.2208537918473518,"score_spread":0.20380493784932036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175365105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947292,0.00018593326,0.00052407896,0.000043334985,0.0000021054295,0.000029552908,0.0027593507,0.000023793236,0.0017026566],"genre_scores_gemma":[0.9933828,0.00019429206,0.0008965392,0.00001957876,0.0000020397179,0.000012615985,0.003951286,0.000004286474,0.0015366169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99968576,0.000016849033,0.000015505324,0.000050159502,0.0001442301,0.00008755893],"domain_scores_gemma":[0.9991856,0.00006338599,0.00011026042,0.0000374761,0.00048820308,0.0001150131],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031041776,0.00026026808,0.0002382662,0.0024563593,0.00072431203,0.0006540346,0.00061913254,0.0002290743,0.00072802196],"category_scores_gemma":[0.00077496073,0.00013213645,0.00018316178,0.0036449754,0.0004370221,0.0001800177,0.00041236056,0.00014266428,0.00010637804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006604189,0.000040445397,0.97263056,0.000037738246,0.000046444256,0.00023284064,0.0004672055,0.0032057846,0.0034762258,0.0002892166,0.0008315323,0.018676009],"study_design_scores_gemma":[0.000002651993,0.000013776839,0.9953099,0.0000093001745,0.000013248197,0.000023814258,0.00075118605,0.0021849817,0.0003667591,0.000042231368,0.0012752843,0.0000068997115],"about_ca_topic_score_codex":0.96810025,"about_ca_topic_score_gemma":0.99126,"teacher_disagreement_score":0.03189975,"about_ca_system_score_codex":0.007928338,"about_ca_system_score_gemma":0.009555079,"threshold_uncertainty_score":0.06417519},"labels":[],"label_agreement":null},{"id":"W3175645228","doi":"10.1016/j.epsl.2021.117081","title":"Interplay of seismic and a-seismic deformation during the 2020 sequence of Atacama, Chile","year":2021,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Cardiological Society of India; Institut de Recherches Servier; Fondo Nacional de Desarrollo Científico y Tecnológico; Horizon 2020; Institut national des sciences de l'Univers; European Research Council; Agencia Nacional de Investigación y Desarrollo; Agence Nationale de la Recherche; H2020 European Research Council; Centre National de la Recherche Scientifique; Center for Sustainable Nanotechnology; Ministère de l'Écologie, du Développement Durable et de l'Énergie; European Commission","keywords":"Aftershock; Geology; Seismology; Subduction; Slip (aerodynamics); Sequence (biology); Geodesy; Tectonics","score_opus":0.007469996144898836,"score_gpt":0.1931163124208721,"score_spread":0.18564631627597325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175645228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915953,0.00025405153,0.00005269075,0.0004674586,0.000012167011,0.000010185948,0.002220604,0.0000084722205,0.0053790505],"genre_scores_gemma":[0.99603564,0.00020668311,0.00005974466,0.00006151073,0.000014770954,0.000013612885,0.0019194719,0.0000049345026,0.0016837145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987614,0.000012887773,0.000010711763,0.000026346099,0.000019504307,0.000054308937],"domain_scores_gemma":[0.99933416,0.00008707672,0.00017421,0.00003063842,0.00021841536,0.00015556536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034935234,0.00018040226,0.00015643248,0.0012452536,0.00058242574,0.0011328139,0.00042981282,0.0005436686,0.0040737498],"category_scores_gemma":[0.0016769856,0.00018023634,0.00015744497,0.001762077,0.00044619286,0.0006232665,0.001323536,0.00031910502,0.00054388033],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003735992,0.00009347296,0.9607084,0.00023990589,0.00013620264,0.0009522253,0.0055536665,0.0021798406,0.0040096426,0.0021999471,0.004784232,0.018768948],"study_design_scores_gemma":[0.000004106757,0.000009211916,0.9953152,0.000027157148,0.0000103968805,0.00003553497,0.002140926,0.00030706375,0.00006402001,0.00009740942,0.0019836447,0.0000052957025],"about_ca_topic_score_codex":0.20487435,"about_ca_topic_score_gemma":0.2561344,"teacher_disagreement_score":0.20487435,"about_ca_system_score_codex":0.0020008464,"about_ca_system_score_gemma":0.0024248715,"threshold_uncertainty_score":0.40736365},"labels":[],"label_agreement":null},{"id":"W3176638204","doi":"10.1029/2021gl092815","title":"Misconception of Waveform Similarity in the Identification of Repeating Earthquakes","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Waveform; Repeater (horology); Similarity (geometry); Robustness (evolution); Identification (biology); Azimuth; Computer science; Geology; Statistics; Geodesy; Mathematics; Artificial intelligence; Telecommunications","score_opus":0.05646824068064328,"score_gpt":0.31278783573998026,"score_spread":0.256319595059337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3176638204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9429952,0.0013607941,0.04759148,0.0024029282,0.00018909092,0.00004712761,0.00012800831,0.00020074163,0.0050846054],"genre_scores_gemma":[0.9951984,0.00012283269,0.0042555374,0.00019056386,0.000044115513,0.0000058069963,0.00003819515,0.000020418769,0.00012403633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.98639894,0.007321375,0.0010420568,0.0025058545,0.0024703126,0.00026145778],"domain_scores_gemma":[0.8286171,0.12615392,0.015816182,0.018534798,0.009410244,0.0014677078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.028177429,0.00032723034,0.00047789735,0.0015438845,0.0006477751,0.002519935,0.0016424106,0.0014096032,0.0010380123],"category_scores_gemma":[0.16242789,0.0003342515,0.0002691225,0.0007037427,0.003619408,0.0031403138,0.0014812055,0.0012071932,0.00041340516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020921943,0.00027364457,0.5771085,0.00097180204,0.0008160835,0.0017066615,0.017731372,0.014304213,0.051172875,0.03875245,0.0054310933,0.28963912],"study_design_scores_gemma":[0.00015607926,0.0016612499,0.5957875,0.0010971368,0.0004883437,0.0070714573,0.016680008,0.16004026,0.10191124,0.10161906,0.012961413,0.00052622426],"about_ca_topic_score_codex":0.0013422878,"about_ca_topic_score_gemma":0.0012602288,"teacher_disagreement_score":0.028177429,"about_ca_system_score_codex":0.00065119716,"about_ca_system_score_gemma":0.00041823197,"threshold_uncertainty_score":0.14901823},"labels":[],"label_agreement":null},{"id":"W3180754998","doi":"10.31223/x5zc99","title":"A reappraisal of active tectonics along the Fethiye-Burdur trend, southwestern Turkey","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; University of Victoria","keywords":"Geology; Seismology; Tectonics; Subduction; Induced seismicity; Plate tectonics; Fault (geology); Active fault; Plateau (mathematics)","score_opus":0.027239486274866918,"score_gpt":0.25218363538296074,"score_spread":0.22494414910809382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3180754998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99745697,0.0007720987,0.00012526348,0.000084086045,0.000016859232,0.0000042734273,0.00035944197,0.000007709259,0.0011733287],"genre_scores_gemma":[0.9975425,0.00074805546,0.00047182685,0.00003006971,0.00001443461,0.0000039531255,0.00075018755,0.0000035143,0.0004355966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990547,0.000008702945,0.0000119654205,0.000038415754,0.000014627215,0.000020773212],"domain_scores_gemma":[0.99981266,0.00001126628,0.00006497173,0.000017084656,0.00006975371,0.0000243697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017290065,0.0003749709,0.00019589366,0.0013135205,0.00024549983,0.00050808897,0.00019219506,0.00027758733,0.0006642808],"category_scores_gemma":[0.00025887968,0.00011266709,0.00014878825,0.0013569491,0.000217357,0.0004282456,0.00037642283,0.00019301393,0.00015214543],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015140709,0.00004912615,0.9166725,0.00017187918,0.00006961382,0.0017644282,0.0019303667,0.0015943693,0.0073391926,0.0003740913,0.0012088254,0.06867414],"study_design_scores_gemma":[0.0000034978889,0.000032548593,0.9948148,0.000036812635,0.0000250836,0.0002728808,0.0010502524,0.0006606043,0.00026797975,0.00003382414,0.002796012,0.000005658758],"about_ca_topic_score_codex":0.019399587,"about_ca_topic_score_gemma":0.042144313,"teacher_disagreement_score":0.019399587,"about_ca_system_score_codex":0.00047787116,"about_ca_system_score_gemma":0.00048248467,"threshold_uncertainty_score":0.038573325},"labels":[],"label_agreement":null},{"id":"W3182379475","doi":"10.1093/gji/ggab265","title":"Structure of the northwestern North Anatolian Fault Zone imaged via teleseismic scattering tomography","year":2021,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Environment Research Council; Boğaziçi Üniversitesi; British Geological Survey; Sakarya Üniversitesi; University of Leeds; Sight Research UK","keywords":"North Anatolian Fault; Seismology; Seismometer; Geology; Crust; Lithosphere; Mantle (geology); Passive seismic; Seismic tomography; Fault (geology); Tectonics; Geophysics","score_opus":0.006439625320621433,"score_gpt":0.20290626268479536,"score_spread":0.19646663736417394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3182379475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99883527,0.000048956295,0.00034174835,0.000018590381,9.786633e-7,0.0000026519842,0.00025195797,0.000018354374,0.0004815409],"genre_scores_gemma":[0.9990336,0.00004364046,0.00046083622,0.000003674448,0.0000021194744,0.0000029713624,0.0003185333,0.0000031422865,0.0001314667],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.000004617691,0.00000498554,0.000015337664,0.000013333881,0.000008991114],"domain_scores_gemma":[0.99986136,0.000016134187,0.00005277075,0.000015585856,0.00004158945,0.000012554368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000075987315,0.00016525663,0.00014648226,0.0007937,0.00014400657,0.0003392667,0.00019063313,0.00017325397,0.00052412954],"category_scores_gemma":[0.00022812486,0.00015201984,0.000096360454,0.00081983715,0.00015833684,0.00017137387,0.0002398725,0.0000800738,0.00014137698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023735235,0.00007795517,0.8065096,0.0000673174,0.00012541428,0.0008964601,0.0007463814,0.0146847,0.12580816,0.00046336625,0.0006472027,0.04973606],"study_design_scores_gemma":[0.000012334855,0.000025963323,0.97082806,0.000011078159,0.00003126704,0.000448863,0.00032132314,0.024941526,0.0025774264,0.00011514724,0.00067859533,0.00000841456],"about_ca_topic_score_codex":0.014915062,"about_ca_topic_score_gemma":0.023782663,"teacher_disagreement_score":0.014915062,"about_ca_system_score_codex":0.00030273173,"about_ca_system_score_gemma":0.00023471337,"threshold_uncertainty_score":0.02965647},"labels":[],"label_agreement":null},{"id":"W3183872154","doi":"10.1017/s0016756821000534","title":"Beyond ‘crumple zones’: recent advances, applications and future directions in deformable plate tectonic modelling","year":2021,"lang":"en","type":"article","venue":"Geological Magazine","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Kinematics; Deformation (meteorology); Plate tectonics; Geology; Intraplate earthquake; Work (physics); Computer science; Tectonics; Mechanical engineering; Seismology; Physics; Classical mechanics; Engineering","score_opus":0.015934686622725156,"score_gpt":0.22019541330367667,"score_spread":0.20426072668095152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183872154","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0018174526,0.9132716,0.04006003,0.0329325,0.0035617624,0.000012278697,0.00010210562,0.00012204873,0.008120102],"genre_scores_gemma":[0.032835916,0.94001716,0.014887222,0.0033067244,0.0058516827,0.000019100953,0.00013268039,0.000091774775,0.0028577903],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993186,0.00028105912,0.000063829386,0.0001183369,0.00018534137,0.00003281916],"domain_scores_gemma":[0.994555,0.004027784,0.00032956983,0.000233238,0.000720122,0.00013424436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0036647771,0.0008209942,0.0011637677,0.0019279014,0.00040819214,0.0035999715,0.0020998889,0.003170477,0.0049913647],"category_scores_gemma":[0.0066121067,0.00037964073,0.0012605783,0.002882562,0.0031138167,0.0053407475,0.001805627,0.0037726755,0.0015630719],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008269455,0.000034722772,0.0011005694,0.010464852,0.00017528009,0.0004063592,0.0012947043,0.028949821,0.0013514886,0.401755,0.040545166,0.51383936],"study_design_scores_gemma":[0.000008340856,0.00005341954,0.0010382566,0.0049459236,0.000077359146,0.00041844492,0.00058786524,0.021133997,0.0006539362,0.23653433,0.7344586,0.00008954548],"about_ca_topic_score_codex":0.0044713845,"about_ca_topic_score_gemma":0.00429535,"teacher_disagreement_score":0.0049913647,"about_ca_system_score_codex":0.0014997198,"about_ca_system_score_gemma":0.0016499244,"threshold_uncertainty_score":0.019381404},"labels":[],"label_agreement":null},{"id":"W3184102313","doi":"10.1029/2020gl092267","title":"Aftershock Triggering and Spatial Aftershock Zones in Fluid‐Driven Settings: Discriminating Induced Seismicity From Natural Swarms","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium","keywords":"Aftershock; Induced seismicity; Geology; Seismology; Magnitude (astronomy); Tectonics; Natural (archaeology); Spatial variability; Paleontology; Physics","score_opus":0.032852331797719014,"score_gpt":0.27755878431937026,"score_spread":0.24470645252165124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3184102313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993455,0.000023260427,0.00014979333,0.000005460688,6.3426666e-7,0.000003708665,0.00015303132,0.0000061444603,0.0003124898],"genre_scores_gemma":[0.9997117,0.000011462201,0.000097125536,0.0000010380662,8.3587344e-7,0.0000014189792,0.00013284756,7.510442e-7,0.00004275185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998634,0.000019921961,0.000018006644,0.000038496943,0.00002243619,0.00003779911],"domain_scores_gemma":[0.9988004,0.00019562274,0.0006345743,0.000072742536,0.00013473256,0.0001618352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020540801,0.00016123432,0.00016379674,0.0014204856,0.00022413219,0.00066187844,0.00015199302,0.00020159014,0.0012279885],"category_scores_gemma":[0.0013138321,0.00010086509,0.000105786574,0.0011541354,0.00033459233,0.0004443092,0.0005678808,0.00013142082,0.00015178576],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007187344,0.000027881766,0.99247897,0.000015156928,0.00003023508,0.00008134143,0.0002636214,0.0010245015,0.0026305772,0.00009432675,0.00007572555,0.0032057918],"study_design_scores_gemma":[0.00000166956,0.000018234055,0.99814355,0.0000031167701,0.0000043647074,0.000024630945,0.00032587335,0.0011576585,0.00020525993,0.000029821786,0.000083220664,0.0000025554782],"about_ca_topic_score_codex":0.011408229,"about_ca_topic_score_gemma":0.025007324,"teacher_disagreement_score":0.011408229,"about_ca_system_score_codex":0.00029234478,"about_ca_system_score_gemma":0.0002527129,"threshold_uncertainty_score":0.02268368},"labels":[],"label_agreement":null},{"id":"W3184890236","doi":"10.1130/g49063.1","title":"Hydrothermal alteration can result in pore pressurization and volcano instability","year":2021,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Volcano; Phreatic eruption; Hydrothermal circulation; Instability; Phreatic; Pore water pressure; Permeability (electromagnetism); Cabin pressurization; Porosity; Petrology; Magma; Geotechnical engineering; Mineralogy; Geochemistry; Groundwater; Seismology; Materials science; Aquifer; Composite material","score_opus":0.011296904001776055,"score_gpt":0.20368092761638396,"score_spread":0.1923840236146079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3184890236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973652,0.00005849495,0.0016259456,0.000034516164,0.000003640629,0.000004323185,0.000034699737,0.00003380559,0.00083939114],"genre_scores_gemma":[0.999703,0.000020185298,0.00021630598,0.0000019106799,5.340577e-7,0.0000010151543,0.000009011623,0.0000014070627,0.00004663348],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992585,0.000013472233,0.00000566658,0.000017335484,0.000022571494,0.000015036358],"domain_scores_gemma":[0.999828,0.0000636473,0.00006352456,0.000012678103,0.000013217622,0.000018898805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000119746124,0.00016987612,0.0001626641,0.00020533105,0.00023914975,0.0005694393,0.00029943217,0.00031218544,0.0005414637],"category_scores_gemma":[0.0005218812,0.00013969348,0.00022797156,0.00015316113,0.00045447962,0.00037795663,0.0003559396,0.00019405488,0.000039901493],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013803021,0.00015690712,0.22020549,0.00011178048,0.00010098785,0.0007383361,0.000126912,0.5526037,0.21470313,0.0024445322,0.00026820257,0.008401954],"study_design_scores_gemma":[0.00001645532,0.00009278041,0.11189045,0.000008890595,0.000031339125,0.00018533452,0.00016388347,0.8615521,0.024233611,0.00095131435,0.0008562817,0.000017639695],"about_ca_topic_score_codex":0.011424197,"about_ca_topic_score_gemma":0.009193203,"teacher_disagreement_score":0.011424197,"about_ca_system_score_codex":0.00070082996,"about_ca_system_score_gemma":0.00028000027,"threshold_uncertainty_score":0.02271539},"labels":[],"label_agreement":null},{"id":"W3188483001","doi":"10.7939/dvn/ym6fhk","title":"Event Data of the Recent Wastewater Disposal Induced Earthquakes near Musreau Lake, Alberta","year":2021,"lang":"en","type":"dataset","venue":"Borealis","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Seismology; Geology; Wastewater; Waveform; Event (particle physics); Hydrology (agriculture); Environmental science; Engineering; Geotechnical engineering; Environmental engineering; Telecommunications; Radar","score_opus":0.04103290878659194,"score_gpt":0.2572970966390783,"score_spread":0.21626418785248636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3188483001","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004304083,0.000028547096,0.000030156229,0.00002377056,0.000011427188,0.000007153912,0.99829596,0.0001279995,0.0010446447],"genre_scores_gemma":[0.00076066866,0.00003618595,0.00013265727,0.00000982667,0.0000029588196,0.000012375298,0.9981006,0.000028867924,0.0009159932],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995813,0.000017561064,0.000026166881,0.000071614806,0.00018520154,0.00011818009],"domain_scores_gemma":[0.9984864,0.00013715863,0.000111921385,0.00019271359,0.00085443386,0.00021744272],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041892103,0.0014934167,0.00076108176,0.0034852952,0.0011886469,0.0018310349,0.0020531886,0.0008640309,0.033625852],"category_scores_gemma":[0.0022154904,0.000485765,0.0004917343,0.008748832,0.0003537971,0.00050187437,0.001034686,0.00096464355,0.02359205],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086541775,0.000021477046,0.0033595788,0.00042323698,0.000023736406,0.00006690116,0.0000925761,0.00061974674,0.0003288979,0.0007088619,0.990042,0.004226469],"study_design_scores_gemma":[0.00020494201,0.000015692702,0.050141647,0.00030910637,0.000040400108,0.0000717023,0.0003611468,0.00095099123,0.0009159122,0.0007003745,0.9462396,0.000048446065],"about_ca_topic_score_codex":0.8114271,"about_ca_topic_score_gemma":0.906985,"teacher_disagreement_score":0.18857288,"about_ca_system_score_codex":0.0045248456,"about_ca_system_score_gemma":0.008495532,"threshold_uncertainty_score":0.37936682},"labels":[],"label_agreement":null},{"id":"W3189427479","doi":"10.3389/feart.2021.689457","title":"Paleoseismological Findings at a New Trench Indicate the 1714 M8.1 Earthquake Ruptured the Main Frontal Thrust Over all the Bhutan Himalaya","year":2021,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Japan Society for the Promotion of Science; Université de Lausanne; Mitacs; Natural Sciences and Engineering Research Council of Canada; Geological Society of America; Natural Environment Research Council; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Geographic Society; National Science Foundation","keywords":"Geology; Seismology; Slow earthquake; Décollement; Slip (aerodynamics); Trench; Thrust fault; Epicenter; Seismic gap; Radiocarbon dating; Intraplate earthquake; Interplate earthquake; Tectonics; Fault (geology); Paleontology","score_opus":0.01594245871161849,"score_gpt":0.21912674780150032,"score_spread":0.20318428908988184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3189427479","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924583,0.0001279346,0.0004908198,0.000037334277,0.0000044943095,0.000010011901,0.00053118885,0.000021242284,0.0063186837],"genre_scores_gemma":[0.99795973,0.00007916675,0.00037970097,0.000010701443,0.0000051685224,0.0000035341413,0.0002436778,0.000002692849,0.0013156732],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989986,0.0000110607525,0.0000032645576,0.00003444578,0.000023186132,0.00002817325],"domain_scores_gemma":[0.99977773,0.000034081826,0.00004589099,0.000020211426,0.000065069114,0.00005708133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000118918986,0.00021964888,0.00013918582,0.0010283726,0.00090542965,0.00043369248,0.00036804433,0.00023272875,0.0040394105],"category_scores_gemma":[0.00037334708,0.00013264318,0.00007033988,0.0010495051,0.0005730335,0.00024534797,0.00050422514,0.00023050717,0.00059290713],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012906331,0.00008503403,0.8988034,0.00011305236,0.00006132358,0.00215374,0.0072706547,0.001049552,0.037418026,0.0007188067,0.0005240651,0.051673204],"study_design_scores_gemma":[0.0000020135865,0.00003995666,0.99576795,0.0000054490743,0.000010270981,0.00033603894,0.0008811079,0.00026268887,0.0007341481,0.00011172008,0.0018403566,0.000008292364],"about_ca_topic_score_codex":0.028547492,"about_ca_topic_score_gemma":0.12495753,"teacher_disagreement_score":0.028547492,"about_ca_system_score_codex":0.00049372215,"about_ca_system_score_gemma":0.0002350186,"threshold_uncertainty_score":0.056762636},"labels":[],"label_agreement":null},{"id":"W3190282678","doi":"10.1785/0220210084","title":"Joint Inversion of Rupture across a Fault Stepover during the 8 August 2017 Mw 6.5 Jiuzhaigou, China, Earthquake","year":2021,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Seismology; Aftershock; Interferometric synthetic aperture radar; Geodesy; Fault (geology); Geodetic datum; Inversion (geology); Tectonics; Seafloor spreading; Strike-slip tectonics; Slip (aerodynamics); Synthetic aperture radar; Remote sensing; Geophysics","score_opus":0.06210759816604405,"score_gpt":0.3058994488797291,"score_spread":0.24379185071368503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3190282678","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909663,0.000034138542,0.0004335858,0.000023976027,0.0000063174894,0.0000029844095,0.00019890221,0.000036567824,0.00016694849],"genre_scores_gemma":[0.99876523,0.000020309804,0.00048366215,0.000007550165,0.000007197125,0.0000029274902,0.0005830069,0.000004726936,0.00012548435],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998964,0.0000092995,0.000006155093,0.000031060143,0.000021724358,0.000035277448],"domain_scores_gemma":[0.9998523,0.000014574209,0.000037125723,0.000018880493,0.00003686158,0.000040367868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028347928,0.0005597808,0.00042750998,0.00083667453,0.00024918572,0.0003940505,0.0004530989,0.0003311918,0.0005138272],"category_scores_gemma":[0.00049668935,0.00029997734,0.00038520058,0.0008088362,0.00021313758,0.00029236096,0.00040216287,0.0002267165,0.00011196996],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00096627756,0.00041580014,0.67318535,0.0001513233,0.00054452417,0.0022165193,0.00057979394,0.1631986,0.09047177,0.00073305547,0.002070771,0.06546619],"study_design_scores_gemma":[0.00006792162,0.00010903579,0.67336845,0.000014486275,0.00012634124,0.00014210673,0.00032589288,0.3194264,0.0053660753,0.0001680369,0.0008466604,0.0000385974],"about_ca_topic_score_codex":0.026627518,"about_ca_topic_score_gemma":0.037809167,"teacher_disagreement_score":0.026627518,"about_ca_system_score_codex":0.00042444334,"about_ca_system_score_gemma":0.00082320574,"threshold_uncertainty_score":0.052945018},"labels":[],"label_agreement":null},{"id":"W3190840288","doi":"10.1002/essoar.10506230.1","title":"Nearest-Neighbour Distance Analysis of Induced and Natural Seismicity within the Western Canada Sedimentary Basin","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Induced seismicity; Geology; Seismology; Structural basin; Tectonics; Magnitude (astronomy); Aftershock; Sedimentary rock; Natural hazard; Hydraulic fracturing; Seismic hazard; Paleontology","score_opus":0.010393761320723206,"score_gpt":0.20129147302539036,"score_spread":0.19089771170466716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3190840288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985098,0.000040237996,0.0003485789,0.000010353287,0.0000011215511,0.000008089228,0.0003235671,0.00000732889,0.0007508972],"genre_scores_gemma":[0.9989542,0.000027008757,0.00025954717,0.0000020407692,5.134897e-7,0.0000032085456,0.00042290566,0.0000018662008,0.0003287066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997985,0.000020018251,0.000014048485,0.00004223053,0.00006978226,0.00005549516],"domain_scores_gemma":[0.99944955,0.00009143647,0.00009110858,0.000032674485,0.00024393549,0.00009125666],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017908464,0.00011465512,0.0001685002,0.0015331067,0.0005732351,0.00044247863,0.00034176226,0.00013255302,0.0006510125],"category_scores_gemma":[0.0014500597,0.00006977642,0.00016874606,0.0018540829,0.00047177053,0.00011814024,0.00033559624,0.0001531382,0.00008051883],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023914584,0.000063464584,0.92510295,0.000064378546,0.00015411741,0.0005092748,0.0016978174,0.030810274,0.006370818,0.0020619512,0.0010436119,0.031882197],"study_design_scores_gemma":[0.0000034803359,0.000013210765,0.9788265,0.000006346525,0.000014796822,0.00005746803,0.0009484491,0.018960245,0.00029054345,0.0001154017,0.0007517149,0.000011803044],"about_ca_topic_score_codex":0.9151229,"about_ca_topic_score_gemma":0.931625,"teacher_disagreement_score":0.084877074,"about_ca_system_score_codex":0.0035804845,"about_ca_system_score_gemma":0.003139596,"threshold_uncertainty_score":0.17075384},"labels":[],"label_agreement":null},{"id":"W3192200537","doi":"","title":"The significance of tomographic edge zones for large earthquakes in Taiwan","year":2019,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Seismology","score_opus":0.01511803184473724,"score_gpt":0.22568539741468815,"score_spread":0.21056736556995093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3192200537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99886215,0.000057461268,0.00013295651,0.000039141407,0.0000029525613,0.0000041048115,0.00015412846,0.000008841171,0.00073827873],"genre_scores_gemma":[0.9997223,0.000019454885,0.000060845618,0.0000036275742,0.000003434826,0.000001540436,0.000114778726,0.0000026253952,0.00007128731],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989235,0.000020833013,0.000012011339,0.00002404974,0.000013444969,0.00003719635],"domain_scores_gemma":[0.99887544,0.00030932837,0.00033846244,0.00008581077,0.00023259566,0.0001584515],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027526994,0.00015966235,0.00015575495,0.0019083158,0.0004587828,0.0009823205,0.0003038134,0.00026703384,0.0011941144],"category_scores_gemma":[0.0021649224,0.00015537627,0.00015742921,0.0016880649,0.0002948899,0.0005786808,0.00059986423,0.00018259855,0.00012915199],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017642787,0.000031823547,0.98476195,0.000024122592,0.000027975626,0.00031560526,0.00040873993,0.0011097896,0.0022248297,0.00016884804,0.00020164457,0.010548169],"study_design_scores_gemma":[0.000005751525,0.000011744775,0.99697125,0.0000050249005,0.000018711944,0.000053208918,0.0005490322,0.0020186394,0.000116116375,0.00007840636,0.00016832737,0.0000037401087],"about_ca_topic_score_codex":0.025973363,"about_ca_topic_score_gemma":0.041369557,"teacher_disagreement_score":0.025973363,"about_ca_system_score_codex":0.00040319143,"about_ca_system_score_gemma":0.00055680674,"threshold_uncertainty_score":0.051644325},"labels":[],"label_agreement":null},{"id":"W3194009702","doi":"10.1126/sciadv.abi8368","title":"Basal nucleation and the prevalence of ascending swarms in Long Valley caldera","year":2021,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Science Foundation of Sri Lanka; National Science Foundation","keywords":"Caldera; Geology; Nucleation; Seismology; Basal (medicine); Volcano; Biology","score_opus":0.010973865074467648,"score_gpt":0.24462378243773988,"score_spread":0.23364991736327223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194009702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994562,0.000044967157,0.00006378493,0.000017359796,0.000001295267,0.0000012084022,0.00013098794,0.0000051317506,0.00027899462],"genre_scores_gemma":[0.9994778,0.000024614174,0.00006710085,0.000004906463,0.0000024486978,0.0000012123148,0.0003410148,0.000001968042,0.00007896315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992275,0.000006033917,0.0000049587707,0.00003489082,0.00001328506,0.000018054381],"domain_scores_gemma":[0.9992637,0.00011971485,0.00026358818,0.00005859182,0.00012970855,0.0001645902],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018313577,0.00010899477,0.00017059848,0.00089295115,0.00039682857,0.00071833335,0.00023012725,0.00027249785,0.0007788568],"category_scores_gemma":[0.0011297034,0.00010840892,0.00011638564,0.0005846329,0.00038357874,0.00025129266,0.00037477023,0.00025542566,0.000115357194],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007525923,0.000027598435,0.9874413,0.0000115110615,0.000030921343,0.00012736584,0.00044042617,0.0012667459,0.005812866,0.00016162611,0.00034476357,0.00425953],"study_design_scores_gemma":[0.0000019629229,0.0000064702836,0.99822515,0.0000027406363,0.0000050337208,0.000021754997,0.00017448413,0.0013051332,0.000114178656,0.000030086358,0.000111624795,0.0000014615318],"about_ca_topic_score_codex":0.036673542,"about_ca_topic_score_gemma":0.05889388,"teacher_disagreement_score":0.036673542,"about_ca_system_score_codex":0.0005093048,"about_ca_system_score_gemma":0.00019208936,"threshold_uncertainty_score":0.07292014},"labels":[],"label_agreement":null},{"id":"W3194153409","doi":"10.1111/j.1440-1738.2001.00347.x","title":"Changes in magnetic and fractal properties of fractured granites near the Nojima Fault, Japan","year":2001,"lang":"en","type":"article","venue":"Island Arc","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"","keywords":"Fault gouge; Geology; Fractal dimension; Rock magnetism; Fault (geology); Fractal; Anisotropy; Comminution; Cataclastic rock; Petrology; Geochemistry; Magnetic field; Mineralogy; Seismology; Magnetization; Remanence; Materials science","score_opus":0.014775958482679201,"score_gpt":0.19323421189763584,"score_spread":0.17845825341495664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194153409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99981064,0.000023113596,0.00003744826,0.000002440734,5.3061257e-7,6.6593344e-7,0.000032691558,0.0000035785436,0.00008906298],"genre_scores_gemma":[0.99981743,0.00001213506,0.000045341534,0.0000012247341,6.64207e-7,0.0000010200775,0.00006366617,0.0000013644653,0.000057037396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999411,0.000003998177,0.0000040446116,0.000020194091,0.000015118778,0.000015487589],"domain_scores_gemma":[0.999782,0.000019734638,0.00006411504,0.000014572224,0.000065040666,0.000054533524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007711558,0.00014645571,0.00016865114,0.0013686782,0.0003530491,0.00042256142,0.00015425288,0.00018520314,0.0003879703],"category_scores_gemma":[0.00028925462,0.00017922491,0.00013417861,0.00045417086,0.0003762157,0.000133012,0.00022807636,0.0001289305,0.00008199959],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059711095,0.000055489352,0.6997829,0.00006775286,0.00012629494,0.0005479675,0.0012511304,0.0017649463,0.28696463,0.00013322926,0.00013721766,0.008571257],"study_design_scores_gemma":[0.0000039166216,0.000021540458,0.9976284,0.0000013905158,0.000007286059,0.00009103081,0.00019184049,0.000646203,0.0012770066,0.000017804101,0.00010885624,0.000004857118],"about_ca_topic_score_codex":0.01255953,"about_ca_topic_score_gemma":0.014590309,"teacher_disagreement_score":0.01255953,"about_ca_system_score_codex":0.0003485574,"about_ca_system_score_gemma":0.00012622518,"threshold_uncertainty_score":0.024972856},"labels":[],"label_agreement":null},{"id":"W3194491437","doi":"10.1029/2021jb022839","title":"Raton Basin Induced Seismicity Is Hosted by Networks of Short Basement Faults and Mimics Tectonic Earthquake Statistics","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Induced seismicity; Seismology; Geology; Tectonics; Structural basin; Fault (geology); Slip (aerodynamics); Basement; Geomorphology","score_opus":0.03966873536569286,"score_gpt":0.3138336121222472,"score_spread":0.2741648767565543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194491437","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935382,0.00007666857,0.0002542601,0.000053629567,0.000009044148,0.000008140071,0.001981849,0.000076427736,0.0040018456],"genre_scores_gemma":[0.99647105,0.000038922233,0.00024919555,0.000011792754,0.0000067016454,0.0000056678487,0.0021555775,0.000015694717,0.0010454882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988127,0.000010915405,0.000008485859,0.000037983504,0.00002479739,0.000036582307],"domain_scores_gemma":[0.9996495,0.000033462158,0.00014203369,0.000031575943,0.00009940025,0.00004396245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013517786,0.0002279359,0.00013099806,0.0013946964,0.00021149238,0.0005087051,0.00021562044,0.00011846446,0.003913747],"category_scores_gemma":[0.00050527207,0.000086712564,0.00016298238,0.001096023,0.0002197626,0.00023333888,0.00040136007,0.00011261091,0.000384853],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012427398,0.000030614956,0.96701753,0.000067352295,0.00006148641,0.00027109965,0.0003445944,0.002508354,0.005070475,0.00042098138,0.003242315,0.02084108],"study_design_scores_gemma":[0.0000031369077,0.000014434909,0.99302226,0.00001441756,0.000012125655,0.00007719641,0.0002624559,0.004062981,0.0003767157,0.00006770769,0.0020803353,0.0000062777026],"about_ca_topic_score_codex":0.07408861,"about_ca_topic_score_gemma":0.20135532,"teacher_disagreement_score":0.07408861,"about_ca_system_score_codex":0.0005859321,"about_ca_system_score_gemma":0.00048823393,"threshold_uncertainty_score":0.14731473},"labels":[],"label_agreement":null},{"id":"W3195011086","doi":"","title":"Geological constraints on the mechanisms of slow earthquakes","year":2020,"lang":"en","type":"article","venue":"eScholarship@McGill (McGill)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Seismology; Slip (aerodynamics); Plate tectonics; Episodic tremor and slip; Geodetic datum; Shear (geology); Limiting; Tectonics; Remotely triggered earthquakes; Shear zone; Seismic gap; Elastic-rebound theory; Fault (geology); Subduction; Active fault; Geodesy; Petrology","score_opus":0.03529838121505816,"score_gpt":0.20800841514842125,"score_spread":0.1727100339333631,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195011086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8015855,0.12177039,0.01149655,0.0034227208,0.00016335989,0.000064999476,0.0011975133,0.00016305684,0.060135864],"genre_scores_gemma":[0.96026224,0.0357679,0.0013371053,0.00032048993,0.000090728616,0.000022271797,0.00042982431,0.0000136544995,0.0017557398],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9996946,0.00004673188,0.00003926293,0.00007610222,0.000086954904,0.000056435998],"domain_scores_gemma":[0.9990069,0.00037848295,0.00028567252,0.00008984739,0.00015292378,0.00008610843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008857277,0.00030629418,0.00034097306,0.0011656459,0.000357118,0.0010188678,0.00077958737,0.0005182057,0.002037216],"category_scores_gemma":[0.001946204,0.00025648234,0.00020245096,0.0007087489,0.0015786693,0.0009822793,0.00090581924,0.00054586167,0.00041234013],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005521113,0.00010178188,0.21728612,0.0065375217,0.00050506153,0.004989549,0.005180214,0.017685467,0.06720477,0.3925663,0.0047965334,0.2825946],"study_design_scores_gemma":[0.00007709108,0.00039209484,0.6028847,0.0011331183,0.00035132276,0.0034076204,0.0034377715,0.0042387256,0.009559552,0.15325707,0.22112466,0.0001362223],"about_ca_topic_score_codex":0.004562905,"about_ca_topic_score_gemma":0.005442258,"teacher_disagreement_score":0.004562905,"about_ca_system_score_codex":0.00079647376,"about_ca_system_score_gemma":0.0008946259,"threshold_uncertainty_score":0.009072721},"labels":[],"label_agreement":null},{"id":"W3195487486","doi":"10.1029/2020jb021573","title":"Toward Waveform‐Based Characterization of Slab &amp; Mantle Wedge (SAM) Earthquakes","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Subduction; Seismogram; Classification of discontinuities; Slab; Mantle (geology); Discontinuity (linguistics); Mantle wedge; Seismic array; Crust; Geophysics; Tectonics","score_opus":0.08176908914775273,"score_gpt":0.3249869136564549,"score_spread":0.24321782450870216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195487486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86642385,0.00022276177,0.12473141,0.000095716765,0.000023999904,0.000103018094,0.004569546,0.0016914441,0.0021382978],"genre_scores_gemma":[0.8991849,0.00013095881,0.09524686,0.000018243774,0.000025840862,0.00003940028,0.0046952097,0.00012786941,0.00053078233],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9998344,0.000033272372,0.000022722008,0.000053929554,0.000031327556,0.00002425666],"domain_scores_gemma":[0.99895334,0.00023805922,0.0001983373,0.00015573956,0.0003539886,0.00010043062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005894818,0.00047991026,0.00027052325,0.0045614084,0.00010921741,0.0006907587,0.0003854936,0.00044838866,0.0010068595],"category_scores_gemma":[0.0016397724,0.00016164534,0.00035046766,0.0016681921,0.0001242942,0.0003954947,0.0006030023,0.0002927601,0.00085266907],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044102868,0.00033682174,0.29777125,0.0002578609,0.00012174864,0.00036632543,0.00040266526,0.024079373,0.32793516,0.00085468416,0.001575951,0.3458571],"study_design_scores_gemma":[0.000057299367,0.00020777932,0.57025445,0.000043610893,0.00007285739,0.0003752937,0.00044040487,0.37516847,0.04873951,0.0009108828,0.0036794308,0.000050121784],"about_ca_topic_score_codex":0.0030154036,"about_ca_topic_score_gemma":0.0039807423,"teacher_disagreement_score":0.0045614084,"about_ca_system_score_codex":0.00016491002,"about_ca_system_score_gemma":0.0002979843,"threshold_uncertainty_score":0.005995691},"labels":[],"label_agreement":null},{"id":"W3195644098","doi":"10.1016/s0967-0653(97)85153-8","title":"10.1016/s0967-0653(97)85153-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Inversion (geology); Slip (aerodynamics); Seismic moment; Tsunami earthquake; Tectonics; Tsunami wave; Geodesy; Physics","score_opus":0.009972151233005813,"score_gpt":0.16626719750506697,"score_spread":0.15629504627206114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195644098","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010935307,0.00071236875,0.0012774876,0.0007125546,0.0005335853,0.0002320838,0.0018477545,0.0016111238,0.9919796],"genre_scores_gemma":[0.0009981577,0.00035776297,0.0006841398,0.00042674388,0.00010725869,0.00011687041,0.0007431513,0.0003176861,0.9962482],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989518,0.000074212556,0.000118667245,0.0004181627,0.00021872047,0.00021840488],"domain_scores_gemma":[0.99742955,0.00062085903,0.00020864501,0.00037371067,0.00057630223,0.00079089083],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0019587397,0.0041657756,0.0028917524,0.0040777214,0.0024433716,0.005327031,0.004991102,0.008730664,0.991479],"category_scores_gemma":[0.0016475901,0.0015389323,0.0021581908,0.003428025,0.003288122,0.0080953725,0.004812465,0.0036365534,0.9942983],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048259523,0.00050613424,0.0015071763,0.0009178621,0.00007740678,0.00060219504,0.0001706115,0.0008016042,0.003597821,0.00718291,0.307837,0.6763166],"study_design_scores_gemma":[0.000108873566,0.0002489535,0.0011066461,0.0007081678,0.00002505518,0.0006776292,0.00023056821,0.0004261154,0.00046840703,0.0010996098,0.9948521,0.000047877216],"about_ca_topic_score_codex":0.0032554343,"about_ca_topic_score_gemma":0.0027144833,"teacher_disagreement_score":0.008730664,"about_ca_system_score_codex":0.0014489265,"about_ca_system_score_gemma":0.0011434741,"threshold_uncertainty_score":0.012154222},"labels":[],"label_agreement":null},{"id":"W3196828395","doi":"","title":"Comparison of Seismic Qualification Challenges for Nuclear Power Plants in North America and Peninsular India","year":2015,"lang":"en","type":"article","venue":"NCSU Libraries Repository (North Carolina State University Libraries)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Bhabha Atomic Research Centre; Atomic Energy Regulatory Board; Bruce Power","keywords":"Nuclear power; Geology; Geography; Seismology; Nuclear physics; Physics","score_opus":0.0266589984984588,"score_gpt":0.20766455053081112,"score_spread":0.18100555203235233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3196828395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9703525,0.0002569752,0.00063731486,0.0015808964,0.000015237165,0.00001753814,0.00036119326,0.000033531916,0.026744746],"genre_scores_gemma":[0.997264,0.00014717985,0.00016682576,0.000087097615,0.000004503531,0.000004523659,0.00021001707,0.0000068004792,0.0021090028],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99931884,0.00012277583,0.000042924774,0.000052658885,0.00021299349,0.0002499115],"domain_scores_gemma":[0.9962923,0.0009713924,0.0006491333,0.00010548713,0.001528394,0.00045316288],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008030828,0.000186335,0.00020725452,0.00089347846,0.0011256128,0.0015963286,0.00063394173,0.0006084,0.0039948844],"category_scores_gemma":[0.00457149,0.00016695863,0.0002417437,0.0018215689,0.00046620212,0.00090716407,0.001194973,0.0005436922,0.0004589556],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006838837,0.0002003754,0.7966205,0.00030728168,0.00012065787,0.0038014073,0.012937911,0.042245746,0.005951624,0.012161047,0.010220671,0.114748925],"study_design_scores_gemma":[0.000013603585,0.00015768979,0.9359722,0.00006589934,0.00003319602,0.0005989047,0.044551656,0.0053144842,0.0007320418,0.0011312444,0.011396604,0.000032405547],"about_ca_topic_score_codex":0.12531497,"about_ca_topic_score_gemma":0.3082587,"teacher_disagreement_score":0.12531497,"about_ca_system_score_codex":0.003153017,"about_ca_system_score_gemma":0.003236603,"threshold_uncertainty_score":0.24917108},"labels":[],"label_agreement":null},{"id":"W3198398481","doi":"","title":"How Is Induced Seismicity Affected by Transitional Stress Regimes","year":2021,"lang":"en","type":"article","venue":"55th U.S. Rock Mechanics/Geomechanics Symposium","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Stress (linguistics); Geology; Seismology","score_opus":0.0132590634174427,"score_gpt":0.20086517232153103,"score_spread":0.18760610890408833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3198398481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99594265,0.00008130607,0.0004236675,0.00017238467,0.000011422973,0.000006700609,0.00014802862,0.000028772482,0.0031850971],"genre_scores_gemma":[0.9996681,0.00003926579,0.000040879244,0.000021127951,0.0000037757413,0.0000017637002,0.00005965272,0.0000075005487,0.00015774767],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996464,0.00006642075,0.000023268783,0.00010212386,0.00004238828,0.0001193309],"domain_scores_gemma":[0.9986161,0.00040331285,0.00039326138,0.00013906293,0.00020734807,0.00024096509],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046596446,0.00013433685,0.00036720044,0.0007191964,0.0003258941,0.0021406107,0.00040639928,0.00077258423,0.004352874],"category_scores_gemma":[0.00554291,0.0003483048,0.00027834313,0.00057134044,0.0009299443,0.001237345,0.0010217383,0.0006463564,0.0007197754],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020030353,0.0004970132,0.83301055,0.00022677261,0.00047501383,0.0009090216,0.002376797,0.017046042,0.087514825,0.00990733,0.0017087137,0.044324916],"study_design_scores_gemma":[0.00002113055,0.00012723923,0.98611164,0.00002287631,0.000044676115,0.00013746234,0.00122174,0.00641907,0.0015262782,0.0037356252,0.0006090886,0.000023280078],"about_ca_topic_score_codex":0.002970092,"about_ca_topic_score_gemma":0.002121312,"teacher_disagreement_score":0.004352874,"about_ca_system_score_codex":0.00044082306,"about_ca_system_score_gemma":0.0003935765,"threshold_uncertainty_score":0.014561772},"labels":[],"label_agreement":null},{"id":"W3198520477","doi":"10.1111/bre.12611","title":"Mass transport deposits in reflection seismic data offshore Oregon, USA","year":2021,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Submarine landslide; Submarine pipeline; Landslide; Continental margin; Seismology; Subduction; Margin (machine learning); Sediment; Thrust fault; Passive margin; Geomorphology; Submarine; Tectonics; Oceanography; Rift","score_opus":0.16779481410731142,"score_gpt":0.36553209228900935,"score_spread":0.19773727818169792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3198520477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946181,0.00003006769,0.00013800766,0.000015591682,0.0000017394019,0.000009845084,0.0032095977,0.000019871197,0.0019571374],"genre_scores_gemma":[0.9919933,0.00009961178,0.0006601104,0.000010069188,0.0000028291422,0.000016785989,0.0060225436,0.000006138346,0.0011885308],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999466,0.0000021027554,0.000008883649,0.000015550038,0.000019562685,0.000007294456],"domain_scores_gemma":[0.9997466,0.000020453834,0.000106823696,0.000016609672,0.0000828841,0.000026749052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007942367,0.00018993733,0.00007194906,0.001160098,0.0002398748,0.00034358894,0.00015576594,0.000105196494,0.0014568925],"category_scores_gemma":[0.00031314918,0.00009309097,0.00008390038,0.0014751765,0.00009385869,0.00020196126,0.00035149406,0.00010088981,0.00023551006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003910475,0.000019175195,0.98681706,0.000020424857,0.000013176417,0.00013893965,0.00020901595,0.0002741299,0.0032808585,0.00003317777,0.0004113,0.008743656],"study_design_scores_gemma":[0.000003896127,0.00001058862,0.9961449,0.000012330876,0.000009894145,0.000079360674,0.0006270577,0.000714147,0.00093754625,0.000014885654,0.0014430301,0.0000024434528],"about_ca_topic_score_codex":0.06367167,"about_ca_topic_score_gemma":0.16010103,"teacher_disagreement_score":0.06367167,"about_ca_system_score_codex":0.0003177068,"about_ca_system_score_gemma":0.00033335693,"threshold_uncertainty_score":0.12660211},"labels":[],"label_agreement":null},{"id":"W3198967983","doi":"","title":"A Further Source of Tokyo Earthquakes and Pacific Ocean Tsunamis","year":2020,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Subduction; Pacific Plate; Seismology; Plate tectonics; Trench; Submarine pipeline; Convergent boundary; Trough (economics); Peninsula; Triple junction; Pacific ocean; Continental shelf; Oceanography; Tectonics; Oceanic crust; Geography; Archaeology","score_opus":0.018542148410323606,"score_gpt":0.20415004352512534,"score_spread":0.18560789511480172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3198967983","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9816799,0.00087196036,0.0096306065,0.0005716151,0.00008041862,0.00002443249,0.00080778304,0.00014959837,0.006183599],"genre_scores_gemma":[0.99616504,0.0003964449,0.001636109,0.00003708803,0.000017775494,0.000008457353,0.00052958436,0.000016780585,0.0011927711],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992895,0.000012551697,0.0000071584427,0.000019565849,0.000018755416,0.000013065748],"domain_scores_gemma":[0.9996164,0.00008250944,0.00010722026,0.00003976813,0.00010116009,0.000052921387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028418395,0.00063415535,0.0002564271,0.00092234625,0.000526658,0.00063553214,0.00046820397,0.00043263007,0.0030692008],"category_scores_gemma":[0.0012525724,0.00031228547,0.00056504866,0.0013131122,0.00021407199,0.00073823717,0.00057091966,0.00048826233,0.00031589315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014845622,0.00012499897,0.8354958,0.000396436,0.0004649072,0.0030459599,0.001496365,0.084359564,0.007499327,0.005433357,0.002726275,0.05880838],"study_design_scores_gemma":[0.000060900846,0.00045530856,0.7480668,0.00015223361,0.0005540542,0.0020534142,0.0032844273,0.21359299,0.004358867,0.0063467193,0.02095852,0.000115742674],"about_ca_topic_score_codex":0.011921569,"about_ca_topic_score_gemma":0.01732116,"teacher_disagreement_score":0.011921569,"about_ca_system_score_codex":0.00053623883,"about_ca_system_score_gemma":0.0006547094,"threshold_uncertainty_score":0.02370435},"labels":[],"label_agreement":null},{"id":"W3201228016","doi":"10.1029/2021jb022177","title":"Seismic Velocity Structure Along and Across the Ultraslow‐Spreading Southwest Indian Ridge at 64°30′E Showcases Flipping Detachment Faults","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut national des sciences de l'Univers; Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche","keywords":"Geology; Seafloor spreading; Lithosphere; Detachment fault; Ridge; Mid-Atlantic Ridge; Seismology; Ridge push; Mid-ocean ridge; Seismometer; Volcano; Mantle (geology); Crust; Perpendicular; Geophysics; Tectonics; Hydrothermal circulation; Geometry; Paleontology; Extensional definition","score_opus":0.03497886114568297,"score_gpt":0.321850281704336,"score_spread":0.286871420558653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201228016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984068,0.000014401089,0.0005253848,0.000023963448,0.000002706375,0.0000035932133,0.00022006997,0.000058546997,0.0007445425],"genre_scores_gemma":[0.9990879,0.00001079482,0.0003379648,0.0000031316483,0.0000011605977,0.000002616877,0.00033960995,0.0000043286577,0.00021248743],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999529,0.000004157824,0.000002568462,0.000013847444,0.000010860674,0.000015585918],"domain_scores_gemma":[0.9999161,0.00000871957,0.000020945909,0.000013735404,0.000016807362,0.000023726312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000046566853,0.00025345996,0.00014009433,0.00042542,0.00023750616,0.0005283386,0.00037479884,0.0003017296,0.001187293],"category_scores_gemma":[0.00018401112,0.00020559788,0.00033362082,0.00037832343,0.00020832835,0.0001587058,0.00031236795,0.00022016447,0.00023104867],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036526358,0.00016415822,0.80540985,0.00004905991,0.00011532869,0.00065638934,0.0008931135,0.118609056,0.04109564,0.0007567239,0.00093845394,0.030946938],"study_design_scores_gemma":[0.000034544635,0.000072232135,0.84604645,0.000012536368,0.00003611257,0.00015469891,0.00054492516,0.14973886,0.0020657151,0.00031296804,0.0009484713,0.000032581676],"about_ca_topic_score_codex":0.052400235,"about_ca_topic_score_gemma":0.049978092,"teacher_disagreement_score":0.052400235,"about_ca_system_score_codex":0.00041497682,"about_ca_system_score_gemma":0.00045599285,"threshold_uncertainty_score":0.10419047},"labels":[],"label_agreement":null},{"id":"W3202362314","doi":"10.1029/2021gl095347","title":"Seismic Formation Fluid Pressure Observations Reveal High Anisotropy of Oceanic Crust","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Crust; Oceanic crust; Anisotropy; Geophysics; Igneous rock; Compressibility; Hydrothermal circulation; Lithosphere; Petrology; Seismology; Borehole; Seismic anisotropy; Mantle (geology); Geochemistry; Subduction; Tectonics; Geotechnical engineering; Mechanics","score_opus":0.05097705315586851,"score_gpt":0.27558613945293314,"score_spread":0.22460908629706464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202362314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993599,0.000026512513,0.0001434983,0.000006776289,6.2816093e-7,6.7598063e-7,0.000060555412,0.00001213189,0.00038927616],"genre_scores_gemma":[0.9998092,0.000009397188,0.00007064088,0.0000013030756,7.6762035e-7,3.742189e-7,0.000051968633,0.0000012932358,0.000055079116],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994457,0.0000033846525,0.0000034603402,0.000016219486,0.000017546381,0.000014808361],"domain_scores_gemma":[0.99986064,0.000018012743,0.00005813088,0.0000150554215,0.000021919488,0.00002614458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009416664,0.00016712237,0.00010174629,0.0005122452,0.00016421599,0.00022715032,0.000116197894,0.00015307484,0.00064646784],"category_scores_gemma":[0.00031413743,0.0001650889,0.00008996036,0.00027597393,0.0003722716,0.0001632429,0.0003270856,0.00018870873,0.00012163707],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001620337,0.00002068086,0.41758624,0.00002965565,0.000028490636,0.0003250689,0.00083018903,0.00075910037,0.5706664,0.00015535472,0.0000814971,0.009355267],"study_design_scores_gemma":[0.0000022380705,0.000017848399,0.98642576,0.0000015563411,0.0000039232036,0.00012584886,0.0000765888,0.0007091347,0.01241127,0.000025318845,0.00019658392,0.000003986924],"about_ca_topic_score_codex":0.0041915164,"about_ca_topic_score_gemma":0.0044742892,"teacher_disagreement_score":0.0041915164,"about_ca_system_score_codex":0.00024471065,"about_ca_system_score_gemma":0.00009152716,"threshold_uncertainty_score":0.008334219},"labels":[],"label_agreement":null},{"id":"W3202395399","doi":"10.1029/2021jb022539","title":"What Controls the Presence and Characteristics of Aftershocks in Rock Fracture in the Lab?","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"AXA Research Fund; Deutsche Forschungsgemeinschaft; Alexander von Humboldt-Stiftung","keywords":"Aftershock; Geology; Seismology; Induced seismicity; Differential stress; Acoustic emission; Slip (aerodynamics); Microseism; Fracture (geology); Deformation (meteorology); Geotechnical engineering; Physics","score_opus":0.030305041288087455,"score_gpt":0.3089532536213502,"score_spread":0.2786482123332627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202395399","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987527,0.00007213791,0.00065278943,0.00001523281,0.0000023692955,0.0000052587284,0.000074229334,0.000017627919,0.00040767156],"genre_scores_gemma":[0.9996903,0.000027840617,0.00011444344,0.000009241394,0.0000023510413,0.0000046880787,0.000050708135,0.0000042188544,0.00009611368],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997811,0.00003551012,0.00001257133,0.00006455698,0.000035162415,0.00007116515],"domain_scores_gemma":[0.9991905,0.00019954678,0.0003085305,0.000077398705,0.00008156499,0.00014241476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034142568,0.00015128206,0.0003266101,0.00028554542,0.00010604179,0.00055827317,0.00024416507,0.00026680887,0.0015911653],"category_scores_gemma":[0.0010422529,0.00014499312,0.00015580888,0.00019209247,0.00031310917,0.00031952118,0.00033476556,0.00020152864,0.00022762318],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000921591,0.00018254523,0.22024132,0.000104424995,0.00007859069,0.00026003108,0.00014954938,0.001764253,0.76259506,0.00030870576,0.00014027122,0.013253524],"study_design_scores_gemma":[0.000012027917,0.0005421337,0.945693,0.000010005681,0.000039594604,0.00014235903,0.00033592887,0.005557422,0.046975046,0.0002592663,0.00041398645,0.000019182286],"about_ca_topic_score_codex":0.0006625336,"about_ca_topic_score_gemma":0.0006737351,"teacher_disagreement_score":0.0015911653,"about_ca_system_score_codex":0.00022931684,"about_ca_system_score_gemma":0.00012370407,"threshold_uncertainty_score":0.005322993},"labels":[],"label_agreement":null},{"id":"W3203067527","doi":"10.1029/2021jb022523","title":"Cataloging Tectonic Tremor Energy Radiation in the Cascadia Subduction Zone","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Episodic tremor and slip; Tectonics; Epicenter; Terrane; Slip (aerodynamics)","score_opus":0.04064541655784556,"score_gpt":0.3099892620855354,"score_spread":0.26934384552768986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203067527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99420565,0.0001951009,0.0005613408,0.000031887823,0.000003814695,0.000017208786,0.0025698892,0.00013268637,0.0022824872],"genre_scores_gemma":[0.993509,0.00019241219,0.00082697824,0.000007127733,0.0000057037473,0.000017594148,0.0047380845,0.000016986494,0.0006861084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998056,0.000013953091,0.00002678798,0.000060195922,0.00006927947,0.000024166742],"domain_scores_gemma":[0.9992461,0.000068376154,0.00023819963,0.000078161705,0.00022074893,0.0001483639],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027200105,0.0004112982,0.00018666078,0.004703421,0.00036507123,0.00052476715,0.00026415547,0.00016106898,0.0011685877],"category_scores_gemma":[0.0008680116,0.0001687298,0.00025352376,0.0038743585,0.00021739182,0.00022617888,0.00072917115,0.00014578261,0.00027025875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042090527,0.000012161186,0.9795363,0.00005210599,0.00006138877,0.00016294872,0.00051023107,0.0013932341,0.0035686083,0.00006207658,0.00057762384,0.0140211275],"study_design_scores_gemma":[0.0000017355009,0.000007504857,0.9984097,0.000006328879,0.000009760372,0.000031226133,0.00010719913,0.0005214187,0.00019537863,0.000023069611,0.0006837977,0.0000029307882],"about_ca_topic_score_codex":0.054782927,"about_ca_topic_score_gemma":0.08316802,"teacher_disagreement_score":0.054782927,"about_ca_system_score_codex":0.00070871675,"about_ca_system_score_gemma":0.0005247836,"threshold_uncertainty_score":0.108928084},"labels":[],"label_agreement":null},{"id":"W3204480156","doi":"10.4095/328953","title":"An earthquake catalogue for seismic events in the Norman Wells region of the central Mackenzie Valley, Northwest Territories, using waveform data from local seismic stations","year":2021,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismometer; Induced seismicity; Seismology; Geology; Period (music); Hydraulic fracturing; Paleontology","score_opus":0.07807635051840367,"score_gpt":0.28883420404320587,"score_spread":0.2107578535248022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3204480156","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.21205546,0.00043641,0.0034476568,0.00014306488,0.000026967318,0.0009449291,0.7559841,0.0005754605,0.026385844],"genre_scores_gemma":[0.14676967,0.0009393856,0.009355828,0.00004637019,0.000023918003,0.0009424721,0.8241296,0.00014285177,0.017649895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999648,0.000018989991,0.000065451546,0.00004949257,0.00014395737,0.00007415218],"domain_scores_gemma":[0.9978065,0.00010774042,0.0005680958,0.00024005485,0.0010013501,0.00027628458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040716652,0.00067112176,0.000314788,0.008411013,0.0010485752,0.00056408916,0.0007707668,0.00023525892,0.0063717463],"category_scores_gemma":[0.0016040051,0.00026652895,0.0002479375,0.011141439,0.00027461434,0.00040216188,0.0009279484,0.00022604136,0.0031912648],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002918866,0.00013515847,0.6115418,0.0013308211,0.00016137259,0.001419447,0.0056139817,0.004382276,0.012698041,0.001687591,0.21832713,0.14241056],"study_design_scores_gemma":[0.000012587262,0.000022202934,0.92345655,0.000079903475,0.00002287311,0.00024020736,0.0014069456,0.00064476155,0.0008128385,0.000050321105,0.07322319,0.000027527738],"about_ca_topic_score_codex":0.84881663,"about_ca_topic_score_gemma":0.9347746,"teacher_disagreement_score":0.15118337,"about_ca_system_score_codex":0.0023162796,"about_ca_system_score_gemma":0.011962501,"threshold_uncertainty_score":0.30414736},"labels":[],"label_agreement":null},{"id":"W3204728355","doi":"10.31223/x58w4c","title":"Structural controls on earthquake rupture revealed by the 2020 Mw 6.0 Jiashi earthquake (Kepingtag belt, SW Tian Shan, China)","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; China Scholarship Council","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Anticline; Aftershock; Décollement; Thrust fault; Slip (aerodynamics); Fault (geology); Geodesy; Tectonics; Synthetic aperture radar","score_opus":0.014770459086705599,"score_gpt":0.22594350026539667,"score_spread":0.21117304117869107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3204728355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995103,0.000020420273,0.000014944422,0.000010890292,0.0000011804555,0.0000015354793,0.00011213321,0.0000027366953,0.00032570303],"genre_scores_gemma":[0.99960154,0.000026321235,0.000018205359,0.000005980456,0.0000025436675,0.0000023955486,0.00024408451,0.0000011972072,0.00009786709],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998908,0.0000069671228,0.000011957147,0.000032844437,0.000017954664,0.000039471062],"domain_scores_gemma":[0.999724,0.000015183689,0.0001079592,0.00002250433,0.000038072176,0.00009235799],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014096856,0.00025485185,0.00019235456,0.0007230899,0.00036594883,0.00048106172,0.00021827161,0.00025926426,0.0009397253],"category_scores_gemma":[0.00042026202,0.00017342356,0.00015539063,0.0007726663,0.00041303964,0.00024452267,0.0005236444,0.00018600357,0.00018612831],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002734741,0.000058194855,0.9552203,0.000044683205,0.000044807766,0.00061317254,0.0008680453,0.0014330051,0.0336715,0.00021943312,0.0003155494,0.007237907],"study_design_scores_gemma":[0.0000023421478,0.00001244129,0.9993299,0.0000015764044,0.000005991228,0.00002042132,0.00012361276,0.0002517601,0.00014892923,0.00001000403,0.000090536094,0.0000024925187],"about_ca_topic_score_codex":0.026118413,"about_ca_topic_score_gemma":0.053287517,"teacher_disagreement_score":0.026118413,"about_ca_system_score_codex":0.000630036,"about_ca_system_score_gemma":0.00041637302,"threshold_uncertainty_score":0.051932752},"labels":[],"label_agreement":null},{"id":"W3204992236","doi":"","title":"An improved earthquake catalogue in southern British Columbia supplies new constraints on the fault responsible for the 1946 M 7.3 Vancouver Island earthquake","year":2020,"lang":"en","type":"article","venue":"AGU Fall Meeting Abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Fault (geology); Earthquake casualty estimation; Intraplate earthquake; Aftershock; Urban seismic risk; Seismic hazard","score_opus":0.020650253955703527,"score_gpt":0.2166567231888792,"score_spread":0.1960064692331757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3204992236","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.23314796,0.00051505,0.0016912024,0.00049786054,0.00011142239,0.0002195721,0.7170437,0.00084748917,0.045925815],"genre_scores_gemma":[0.24808018,0.00073107006,0.0062218397,0.00015388321,0.00003721922,0.00020755176,0.69097453,0.0003096489,0.053283956],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9995198,0.00002238318,0.000059015827,0.00006551209,0.00020091316,0.00013237026],"domain_scores_gemma":[0.99432373,0.00023495662,0.00043953754,0.00051192206,0.0038907428,0.00059911935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037610185,0.0004950343,0.0004329246,0.011360301,0.0022436802,0.0012610676,0.0007491936,0.00043058195,0.024396518],"category_scores_gemma":[0.002194876,0.00045888318,0.00022620306,0.020154508,0.00029285223,0.00043118163,0.0009999732,0.00071470917,0.006408431],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043621138,0.00016010755,0.32651663,0.00063682767,0.00013610134,0.0006797092,0.0021574877,0.0026479925,0.008189872,0.0017625702,0.45255008,0.20412628],"study_design_scores_gemma":[0.00003129982,0.000011188898,0.8536801,0.000069610236,0.000033944314,0.000070336806,0.0006598813,0.0005360818,0.0007400903,0.00010542927,0.1440268,0.000035254314],"about_ca_topic_score_codex":0.9783092,"about_ca_topic_score_gemma":0.9957176,"teacher_disagreement_score":0.024396518,"about_ca_system_score_codex":0.0058613247,"about_ca_system_score_gemma":0.01818425,"threshold_uncertainty_score":0.081614435},"labels":[],"label_agreement":null},{"id":"W3205988845","doi":"10.1093/gji/ggab420","title":"Machine-learning-based earthquake locations reveal the seismogenesis of the 2020 <i>M</i>w 5.0 Qiaojia, Yunnan earthquake","year":2021,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Natural Science Foundation of China","keywords":"Aftershock; Seismology; Geology; Foreshock; Magnitude (astronomy); Fault (geology); Induced seismicity; Earthquake prediction","score_opus":0.0112291389348593,"score_gpt":0.21678113415096234,"score_spread":0.20555199521610304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3205988845","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99833846,0.000030052719,0.00074729667,0.000025388345,0.00000506779,0.0000044504823,0.00047642025,0.00004623938,0.00032658945],"genre_scores_gemma":[0.9972682,0.000017244158,0.001175474,0.000006655625,0.0000055624782,0.0000041566345,0.0013493975,0.000004052026,0.00016925026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989307,0.000010326955,0.000009094891,0.00003790897,0.000021841823,0.00002776888],"domain_scores_gemma":[0.99960786,0.00005841212,0.0001126603,0.000036303893,0.00009893309,0.000085948326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037456022,0.00031589164,0.00020557533,0.0012104518,0.00022833703,0.00032183545,0.00026546256,0.00024036608,0.00044261682],"category_scores_gemma":[0.00082012865,0.00015524786,0.00021095606,0.001001469,0.00016461717,0.00023758183,0.00031588922,0.00020719111,0.00022243778],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016324282,0.00007349276,0.9169713,0.00003511479,0.000053201664,0.00022728047,0.00018139952,0.028093336,0.013376569,0.0001662461,0.0011913483,0.039467495],"study_design_scores_gemma":[0.00000864876,0.00003346042,0.9047593,0.000006008879,0.000017218921,0.000045196877,0.000114896815,0.093481585,0.0010807631,0.00006529332,0.0003774256,0.000010255271],"about_ca_topic_score_codex":0.023227489,"about_ca_topic_score_gemma":0.03685572,"teacher_disagreement_score":0.023227489,"about_ca_system_score_codex":0.00040320912,"about_ca_system_score_gemma":0.00043945128,"threshold_uncertainty_score":0.04618454},"labels":[],"label_agreement":null},{"id":"W3206115997","doi":"10.1130/g49388.1","title":"Lateral variation in slab window viscosity inferred from global navigation satellite system (GNSS)–observed uplift due to recent mass loss at Patagonia ice fields","year":2021,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Universidad de Chile; Technische Universiteit Delft; Geological Society of America","keywords":"Geology; Post-glacial rebound; Slab; Slab window; Geophysics; Subduction; Ice field; Lithosphere; Mantle (geology); Ridge; Geodesy; Seismology; Glacial period; Geomorphology; Tectonics; Oceanic crust; Paleontology; Glacier","score_opus":0.01815197998862327,"score_gpt":0.2190520249260038,"score_spread":0.20090004493738053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3206115997","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993382,0.0000073048695,0.00013019935,0.0000067139968,5.543698e-7,0.0000012923973,0.00018653505,0.000010239946,0.0003188794],"genre_scores_gemma":[0.99978894,0.000004442215,0.000060977763,0.0000013632663,3.2347572e-7,0.0000012846273,0.00009942131,0.0000015288796,0.000041657207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995184,0.00000810649,0.0000025985198,0.000017758863,0.0000067644337,0.00001293067],"domain_scores_gemma":[0.9998573,0.0000363043,0.000044409793,0.000023021179,0.000019687,0.000019271398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001461438,0.00016430981,0.00012492706,0.000430268,0.00012977752,0.00041502787,0.00025966007,0.00021452457,0.0007586375],"category_scores_gemma":[0.00054681645,0.00019021046,0.00020191928,0.00036962237,0.00022660846,0.00016780356,0.00020630441,0.00017303918,0.00010506095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038707667,0.00004339369,0.8958969,0.000022232765,0.00010223834,0.00023577771,0.0002751192,0.06835964,0.02866116,0.00020357201,0.00026760824,0.0055452893],"study_design_scores_gemma":[0.000007174434,0.000021730651,0.9694378,0.000002721524,0.000008360434,0.00003182775,0.00007308255,0.029430142,0.00080666103,0.000032837255,0.0001417149,0.000006040672],"about_ca_topic_score_codex":0.028840609,"about_ca_topic_score_gemma":0.019315312,"teacher_disagreement_score":0.028840609,"about_ca_system_score_codex":0.0004780807,"about_ca_system_score_gemma":0.00015365511,"threshold_uncertainty_score":0.05734545},"labels":[],"label_agreement":null},{"id":"W3208379170","doi":"","title":"Fault accommodation of permanent strain in the northern Cascadia forearc","year":2021,"lang":"en","type":"article","venue":"eScholarship (California Digital Library)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Forearc; Geology; Seismology; Subduction; Terrane; Fault (geology); Slip (aerodynamics); Tectonics","score_opus":0.018482876501776668,"score_gpt":0.2104160572515115,"score_spread":0.19193318074973484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3208379170","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99801576,0.000062943924,0.00009770475,0.00001956424,9.143094e-7,0.0000013180074,0.00004772019,0.000012689675,0.0017414409],"genre_scores_gemma":[0.99955946,0.00003115385,0.00003899479,0.0000023211765,4.79478e-7,7.2680376e-7,0.000049248265,0.00000200631,0.00031548642],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999818,0.0000106391335,0.000013280198,0.00005485911,0.000047255035,0.000056111392],"domain_scores_gemma":[0.9996222,0.000041921638,0.00010104758,0.00005082455,0.000116073694,0.00006783238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017739634,0.00017927172,0.00020454904,0.0008608166,0.00073369837,0.00084524706,0.00034741568,0.00028522845,0.0014711833],"category_scores_gemma":[0.0008206247,0.00026528517,0.00018292756,0.0008695476,0.0006304183,0.00027951697,0.0005773547,0.00027251447,0.00015373278],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011158732,0.000017084112,0.96125436,0.000040748433,0.000044414784,0.00048021798,0.0015771635,0.0044854004,0.018702628,0.0004732244,0.00014231895,0.01267101],"study_design_scores_gemma":[0.0000015078881,0.000011385878,0.9985134,0.0000037565478,0.0000046628543,0.00005428594,0.0003570971,0.0005200453,0.00023627718,0.00004041586,0.00025401937,0.0000031607974],"about_ca_topic_score_codex":0.19110744,"about_ca_topic_score_gemma":0.43646008,"teacher_disagreement_score":0.19110744,"about_ca_system_score_codex":0.0025789249,"about_ca_system_score_gemma":0.0014160454,"threshold_uncertainty_score":0.37999016},"labels":[],"label_agreement":null},{"id":"W3208750809","doi":"10.1130/abs/2021am-367923","title":"PALEOSEISMIC SURF AND TURF: UPDATES FROM THE USGS POWELL CENTER CASCADIA EARTHQUAKE WORKING GROUP ON SYSTEMATIC INTEGRATION OF ONSHORE AND OFFSHORE RECORDS AND FUTURE DIRECTIONS","year":2021,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Subduction; Seismology; Induced seismicity; Submarine pipeline; Landslide; Context (archaeology); Paleoseismology; Oceanography; Tectonics; Paleontology","score_opus":0.017361581831722733,"score_gpt":0.21317938214666876,"score_spread":0.19581780031494603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3208750809","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03530613,0.0053122705,0.004828692,0.0048057283,0.0017931743,0.00035230583,0.92592096,0.0052432306,0.016437411],"genre_scores_gemma":[0.07011987,0.004996181,0.030374907,0.00091383146,0.000597275,0.000789352,0.882292,0.0020650947,0.007851529],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9986098,0.00016903083,0.000225044,0.00018863569,0.0007120992,0.00009540101],"domain_scores_gemma":[0.9856881,0.0014157695,0.0017927274,0.0017634766,0.008037593,0.0013023339],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0047484506,0.0012559389,0.0006999736,0.011970648,0.0005842388,0.0023670776,0.0017983947,0.0007071573,0.009262779],"category_scores_gemma":[0.01516718,0.0007906868,0.0005919314,0.012486983,0.0003973415,0.0020007151,0.0024810373,0.001222663,0.0052327323],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017459088,0.00009709276,0.08487153,0.0006139167,0.00014520076,0.0001179965,0.0006638301,0.0019421903,0.0008090411,0.0006909235,0.7704881,0.13938566],"study_design_scores_gemma":[0.00006841884,0.0000302268,0.23889329,0.00053935946,0.00006380647,0.00010188896,0.00053912005,0.0010729196,0.0008529821,0.0007210874,0.75704175,0.00007512491],"about_ca_topic_score_codex":0.15439653,"about_ca_topic_score_gemma":0.25072443,"teacher_disagreement_score":0.15439653,"about_ca_system_score_codex":0.0017958225,"about_ca_system_score_gemma":0.0029371642,"threshold_uncertainty_score":0.3069957},"labels":[],"label_agreement":null},{"id":"W3209048981","doi":"10.1130/abs/2021am-365394","title":"EVOLUTION OF MAGMATISM ALONG A FLAT-SLAB SUBDUCTION-TRANSFORM TRANSITION, WRANGELL ARC, ALASKA-YUKON","year":2021,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magmatism; Geology; Subduction; Slab; Seismology; Arc (geometry); Transition zone; Geochemistry; Paleontology; Tectonics; Geometry","score_opus":0.013336700894225412,"score_gpt":0.2122725667100785,"score_spread":0.19893586581585307,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3209048981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992206,0.000021041937,0.000020652866,0.000012744994,6.3332186e-7,0.0000015888552,0.00008387385,0.0000031291681,0.0006357704],"genre_scores_gemma":[0.9994394,0.000018951694,0.00003889655,0.000003634345,3.2088383e-7,0.0000011582138,0.00011687392,0.0000010732422,0.00037973054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999579,0.000005618122,0.000003281832,0.000015180944,0.00000590843,0.000011993274],"domain_scores_gemma":[0.99980503,0.000027654281,0.00004332263,0.000010184517,0.00006702163,0.0000468684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013409638,0.000111429086,0.00011104501,0.0007749633,0.0008878823,0.0006831826,0.00024117438,0.00027708756,0.0013262003],"category_scores_gemma":[0.0003728968,0.00010587023,0.00013638208,0.0006283745,0.00045786728,0.00027976572,0.0005177033,0.00018901739,0.00016706581],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028519428,0.000049741542,0.9760523,0.000026424035,0.00005076108,0.0004187945,0.0034325728,0.0015843131,0.010898087,0.00042002683,0.00015046941,0.006631422],"study_design_scores_gemma":[0.000002504224,0.000025350471,0.9972324,0.0000047557,0.00000791848,0.00004403552,0.0016488536,0.00034205106,0.0003543054,0.00003544754,0.00029996058,0.0000024371138],"about_ca_topic_score_codex":0.22878557,"about_ca_topic_score_gemma":0.36226925,"teacher_disagreement_score":0.7712144,"about_ca_system_score_codex":0.0011608413,"about_ca_system_score_gemma":0.00091977447,"threshold_uncertainty_score":0.45490777},"labels":[],"label_agreement":null},{"id":"W3209244424","doi":"10.1029/2021gl095074","title":"From Seismic Quiescence to Surged Activity After Decades of Wastewater Disposal: A Case Study in Central‐West Alberta, Canada","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Geological Survey of Canada","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Devonian; Reef; Seismology; Hydraulic fracturing; Aquifer; Structural basin; Sedimentary rock; Sedimentary basin; Geochemistry; Geomorphology; Geotechnical engineering; Oceanography; Groundwater","score_opus":0.025502378531678215,"score_gpt":0.2771036802901066,"score_spread":0.25160130175842843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3209244424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945398,0.0003926438,0.00016648066,0.00049755134,0.000010137214,0.000047769114,0.0006139174,0.000012469176,0.0037191382],"genre_scores_gemma":[0.99681085,0.0003759645,0.00021457173,0.00013475957,0.00000613342,0.00000863082,0.0002989022,0.0000053850135,0.0021446955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99954236,0.00003293667,0.000015420892,0.000044345998,0.00013607665,0.00022893542],"domain_scores_gemma":[0.9991185,0.000072049974,0.00009635111,0.00002028249,0.00038364567,0.00030912642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032716047,0.00044301507,0.0002927696,0.0019261405,0.004621735,0.0013693783,0.0012794378,0.0009560306,0.0017488712],"category_scores_gemma":[0.00076162117,0.00028819923,0.00025857898,0.0037300347,0.0011826832,0.00026162874,0.0009334352,0.0007156501,0.00015873472],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034105405,0.00034723425,0.90805674,0.00019394222,0.000119169905,0.018875923,0.022247754,0.0018678873,0.0035117408,0.00082794734,0.004492022,0.03911864],"study_design_scores_gemma":[0.000020481353,0.00009108135,0.91542023,0.00009648811,0.000060966686,0.0015533286,0.0750317,0.0014895516,0.00044488013,0.00014616211,0.005592031,0.00005297499],"about_ca_topic_score_codex":0.9949274,"about_ca_topic_score_gemma":0.9985667,"teacher_disagreement_score":0.033939384,"about_ca_system_score_codex":0.033939384,"about_ca_system_score_gemma":0.034343503,"threshold_uncertainty_score":0.2462486},"labels":[],"label_agreement":null},{"id":"W3209314633","doi":"10.1021/acs.energyfuels.1c02950","title":"Role of Fluid Diffusivity in the Spatiotemporal Migration of Induced Earthquakes during Hydraulic Fracturing in Unconventional Reservoirs","year":2021,"lang":"en","type":"article","venue":"Energy & Fuels","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Canada First Research Excellence Fund","keywords":"Geology; Hydraulic fracturing; Poromechanics; Induced seismicity; Thermal diffusivity; Petrophysics; Shear (geology); Pore water pressure; Seismology; Permeability (electromagnetism); Geotechnical engineering; Stress field; Petrology; Porous medium; Porosity","score_opus":0.014410922210142148,"score_gpt":0.2131725364240584,"score_spread":0.19876161421391625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3209314633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99915314,0.00004773709,0.00062235026,0.000010761705,6.9611826e-7,0.0000016695204,0.000016290327,0.000008729069,0.00013868451],"genre_scores_gemma":[0.9998828,0.000010792966,0.00008354364,5.006352e-7,2.5785195e-7,7.599737e-7,0.0000047001745,8.621261e-7,0.000015842179],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999529,0.000009646961,0.0000051038373,0.000013683494,0.000006527547,0.000012057447],"domain_scores_gemma":[0.99964404,0.00014539101,0.00011816971,0.000022110014,0.000034904628,0.00003530492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015700616,0.00018653995,0.00012696287,0.0004284526,0.00016038041,0.0002481823,0.00015619371,0.00019446609,0.00023532892],"category_scores_gemma":[0.0006237812,0.00014519414,0.00013739106,0.00018895448,0.0003028856,0.00041765405,0.0002536069,0.000108785236,0.00003321125],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010100628,0.00022134982,0.2949563,0.00014020091,0.00007407661,0.0018140344,0.00085694634,0.09378331,0.5817358,0.0013648228,0.00015007361,0.023893053],"study_design_scores_gemma":[0.000043146676,0.00029612257,0.41905865,0.000026497059,0.0000574918,0.0004110098,0.0006799014,0.47040975,0.10795197,0.00059704756,0.00039522338,0.000073318646],"about_ca_topic_score_codex":0.0022582146,"about_ca_topic_score_gemma":0.0016257439,"teacher_disagreement_score":0.0022582146,"about_ca_system_score_codex":0.00030390406,"about_ca_system_score_gemma":0.00016940608,"threshold_uncertainty_score":0.0044901967},"labels":[],"label_agreement":null},{"id":"W3210751055","doi":"10.1029/2021jb022569","title":"The Spatial Relationship Between Contemporaneous Tremor Detections in Relatively Low‐ and High‐Frequency Bands","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Offset (computer science); Low frequency; Geology; Subduction; Guard (computer science); Physics; Seismology; Energy (signal processing); Geodesy; Acoustics; Computer science; Telecommunications","score_opus":0.06610620334319858,"score_gpt":0.3241029477832629,"score_spread":0.25799674444006426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3210751055","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985538,0.00010986856,0.0004977908,0.000010928663,0.0000043020614,0.0000023494617,0.00015766727,0.000014777403,0.000648564],"genre_scores_gemma":[0.9993099,0.00002681525,0.00027731032,0.0000034762475,0.000003378526,0.0000017207196,0.00016776484,0.0000033603226,0.00020628463],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999778,0.000017554003,0.000017996144,0.00008625579,0.000057412624,0.000042760515],"domain_scores_gemma":[0.99800855,0.0006397266,0.00057277444,0.0001410341,0.00049169693,0.00014631839],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027549756,0.00010985499,0.00016089508,0.0011371126,0.00027776946,0.00054191967,0.00023811315,0.00025709614,0.0016447697],"category_scores_gemma":[0.0025232502,0.00014416581,0.000100246034,0.0008623592,0.000230183,0.00021399852,0.0003629724,0.0002383021,0.0002858159],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010618164,0.00001932992,0.96971107,0.000031173877,0.00006508419,0.00010309099,0.0003378949,0.0004297585,0.016212653,0.00007917577,0.00012699542,0.012777499],"study_design_scores_gemma":[0.0000013897226,0.000009266236,0.99878865,0.0000038765215,0.000008465374,0.00003944147,0.00009120137,0.00036328047,0.0005406466,0.00001138642,0.0001403931,0.0000019909153],"about_ca_topic_score_codex":0.022350866,"about_ca_topic_score_gemma":0.053056963,"teacher_disagreement_score":0.022350866,"about_ca_system_score_codex":0.00025174685,"about_ca_system_score_gemma":0.00018021453,"threshold_uncertainty_score":0.04444158},"labels":[],"label_agreement":null},{"id":"W3211376733","doi":"10.1007/s00024-021-02893-x","title":"The Impact of the Chiapas Tsunami of 8 September 2017 on the Coast of Mexico. Part 1: Observations, Statistics, and Energy Partitioning","year":2021,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Geology; Seismology; Submarine pipeline; Tide gauge; Intraplate earthquake; Trough (economics); Oceanography; Sea level; Tectonics","score_opus":0.01957602683237242,"score_gpt":0.2159761910709439,"score_spread":0.19640016423857148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3211376733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9606005,0.00038830738,0.00016222449,0.00023458488,0.000034350174,0.000015736141,0.036703233,0.000033853026,0.001827105],"genre_scores_gemma":[0.9410103,0.00089125807,0.00022038589,0.000039634007,0.00008306714,0.000045554036,0.056294918,0.000022582131,0.0013923411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998203,0.000022616015,0.00001966867,0.00004728616,0.000045415105,0.00004479919],"domain_scores_gemma":[0.9983728,0.00037617044,0.00068267295,0.00009772405,0.00035122343,0.00011939536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002920715,0.000353316,0.00026611306,0.0015601194,0.0003679096,0.0008119982,0.0003352258,0.0003766113,0.0013365066],"category_scores_gemma":[0.0023526642,0.00019460094,0.0002438268,0.0021515705,0.000296686,0.0005262049,0.00063086906,0.00041523363,0.00037498467],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017790073,0.00003252233,0.98453796,0.00006332776,0.00014663415,0.00008932103,0.00017966848,0.0029832118,0.0004491194,0.00022856373,0.005236024,0.00587567],"study_design_scores_gemma":[0.0000048446177,0.000012645904,0.9967534,0.000011858741,0.000023823563,0.00002716365,0.00023317267,0.00076720567,0.00016515821,0.00005348088,0.0019421525,0.0000052051055],"about_ca_topic_score_codex":0.18540931,"about_ca_topic_score_gemma":0.18097445,"teacher_disagreement_score":0.18540931,"about_ca_system_score_codex":0.0012451676,"about_ca_system_score_gemma":0.0008199317,"threshold_uncertainty_score":0.3686602},"labels":[],"label_agreement":null},{"id":"W3211643953","doi":"10.1785/0220210139","title":"Earthquakes Induced by Wastewater Disposal near Musreau Lake, Alberta, 2018–2020","year":2021,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Alberta","funders":"","keywords":"Seismology; Geology; Fault (geology); Seismic hazard; Earthquake swarm; Structural basin; Induced seismicity; Hydraulic fracturing; Focal mechanism; Natural hazard; Geomorphology; Paleontology; Oceanography","score_opus":0.05022501746908546,"score_gpt":0.2867950377161839,"score_spread":0.23657002024709844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3211643953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975809,0.00005888056,0.0001754608,0.00005407545,0.0000043540836,0.000008215972,0.0010222354,0.000020944395,0.0010748943],"genre_scores_gemma":[0.9985108,0.000049942835,0.00011175133,0.000008992116,0.000002667254,0.0000031805462,0.0008181986,0.0000015770242,0.00049291394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989486,0.0000066778593,0.0000047179838,0.00001733589,0.000045474146,0.000030814183],"domain_scores_gemma":[0.9996489,0.000022706443,0.00009608835,0.000013239475,0.00015062797,0.000068400914],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018269868,0.00025407667,0.00014547545,0.00069878757,0.00056101015,0.00047175298,0.00035466976,0.00016691312,0.0008598206],"category_scores_gemma":[0.00057107507,0.00008588116,0.0001446363,0.0011067684,0.00034203657,0.0001316953,0.00039462,0.00018524517,0.00010250521],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014230963,0.000035162782,0.9788544,0.000031440457,0.000053443266,0.00026842012,0.00053348066,0.0034795308,0.0024056847,0.00015331195,0.0012727788,0.012770003],"study_design_scores_gemma":[0.0000033870722,0.00001505049,0.9961273,0.0000051664374,0.000010667165,0.000024040479,0.0006197786,0.0022936545,0.00023396636,0.000027472872,0.0006346808,0.000004820198],"about_ca_topic_score_codex":0.88070107,"about_ca_topic_score_gemma":0.9437928,"teacher_disagreement_score":0.119298935,"about_ca_system_score_codex":0.00465378,"about_ca_system_score_gemma":0.0038516042,"threshold_uncertainty_score":0.24000299},"labels":[],"label_agreement":null},{"id":"W3212162016","doi":"10.26464/epp2021057","title":"Preface to the special collection of Induced Earthquakes","year":2021,"lang":"en","type":"article","venue":"Earth and Planetary Physics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"History; Seismology; Geology; Geography","score_opus":0.02120066384445988,"score_gpt":0.20433228022771555,"score_spread":0.18313161638325567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3212162016","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0015822038,0.007709387,0.010424755,0.0415077,0.898216,0.00040598057,0.005972174,0.0014045823,0.032777242],"genre_scores_gemma":[0.007417293,0.0059533864,0.0052936203,0.01759001,0.6878483,0.00041840615,0.014407945,0.002073052,0.25899804],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992976,0.00012567044,0.0001010087,0.00015353196,0.00026382698,0.000058223053],"domain_scores_gemma":[0.9860599,0.0024424621,0.0006373928,0.0013723646,0.0076158834,0.0018720238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00221065,0.0013204971,0.0012090966,0.0033536525,0.001921643,0.002328676,0.0014448039,0.0020251628,0.081473105],"category_scores_gemma":[0.010704852,0.0003931329,0.0011738659,0.0017716805,0.0004990282,0.0022158043,0.0015944418,0.003591133,0.050983258],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042975975,0.000022395501,0.00014541579,0.000090906244,0.000005646971,0.000066530374,0.000017692864,0.00006249665,0.0004574208,0.00053495256,0.9807344,0.017819216],"study_design_scores_gemma":[0.000013081227,0.00006061281,0.0019320546,0.00007014311,0.000007945403,0.00015038528,0.000040525087,0.00020695693,0.00031346065,0.0012171704,0.9959722,0.000015468246],"about_ca_topic_score_codex":0.00254404,"about_ca_topic_score_gemma":0.0036203554,"teacher_disagreement_score":0.081473105,"about_ca_system_score_codex":0.000832968,"about_ca_system_score_gemma":0.0011645949,"threshold_uncertainty_score":0.2725547},"labels":[],"label_agreement":null},{"id":"W3212499949","doi":"10.7185/gold2021.5203","title":"Cumulate origin for Isua dunites rules out formation as an Eoarchaean ophiolite","year":2021,"lang":"en","type":"article","venue":"Goldschmidt2021 abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Ophiolite; Geology; Computer science; Paleontology","score_opus":0.04851200935242549,"score_gpt":0.291183892423271,"score_spread":0.24267188307084547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3212499949","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8977641,0.00054256583,0.005158823,0.0008149905,0.00061734515,0.00010055188,0.00068316783,0.00035012147,0.09396838],"genre_scores_gemma":[0.9862365,0.00022570654,0.0016603329,0.00018036025,0.000086469656,0.00001653882,0.0004504751,0.00007850815,0.011065171],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999676,0.000020649752,0.000020116726,0.000081061895,0.0000685888,0.00013348798],"domain_scores_gemma":[0.9994655,0.00007286946,0.000075099895,0.00013502971,0.0001439359,0.00010755522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037297214,0.00054483867,0.00068077684,0.0010936497,0.0029558742,0.0020403701,0.0006860086,0.0010853718,0.010354144],"category_scores_gemma":[0.0013660424,0.00024223723,0.00040325391,0.0008785454,0.0021404864,0.0010271805,0.0015572698,0.0012331728,0.0017914984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017530996,0.00031667895,0.43872684,0.000723971,0.00021350343,0.005162907,0.0078924475,0.001603195,0.17372645,0.20669939,0.004690393,0.15849113],"study_design_scores_gemma":[0.00015122486,0.00041957098,0.7641001,0.00019092998,0.00024624128,0.0046087387,0.007618116,0.0027844047,0.030021613,0.022369934,0.16742855,0.000060554263],"about_ca_topic_score_codex":0.013483191,"about_ca_topic_score_gemma":0.020004299,"teacher_disagreement_score":0.013483191,"about_ca_system_score_codex":0.0014570589,"about_ca_system_score_gemma":0.001576218,"threshold_uncertainty_score":0.034638047},"labels":[],"label_agreement":null},{"id":"W3212664649","doi":"10.7185/gold2021.5319","title":"Rapid, paced garnet growth in blueschists from Lu-Hf dating of laser-cut domains combined with trace-element mapping","year":2021,"lang":"en","type":"article","venue":"Goldschmidt2021 abstracts","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Trace element; TRACE (psycholinguistics); Laser; Geochemistry; Optics; Physics","score_opus":0.01707158507840669,"score_gpt":0.205634796284626,"score_spread":0.1885632112062193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3212664649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998126,0.000103205035,0.00089442794,0.0000067838505,0.0000013484602,0.000005419896,0.00014607221,0.000013593883,0.00070316286],"genre_scores_gemma":[0.9969723,0.000081661005,0.0020985566,0.000008433427,0.0000023790797,0.00000574188,0.00014245845,0.000013153375,0.0006752477],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999057,0.0000055394794,0.0000029603343,0.000040168252,0.000027343978,0.000018344701],"domain_scores_gemma":[0.99992824,0.0000135343735,0.000020027455,0.00000845877,0.000019562998,0.000010218611],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010080336,0.00020553458,0.00018074368,0.0008934201,0.00030407042,0.00038247416,0.00025206245,0.00027324635,0.0006949294],"category_scores_gemma":[0.00013731718,0.00017332585,0.00010954452,0.0005371466,0.00045262338,0.00019586639,0.00042193272,0.00019084064,0.00019790472],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015337032,0.000013894379,0.13751344,0.00006436594,0.000027744049,0.0004763632,0.00088557834,0.0008335678,0.84680414,0.00013363195,0.000047593177,0.0130463205],"study_design_scores_gemma":[0.000006560829,0.00006710938,0.95176506,0.000009325833,0.000024631672,0.0006019184,0.00041555168,0.0015377459,0.044010215,0.000100614256,0.0014522934,0.000008956172],"about_ca_topic_score_codex":0.012287081,"about_ca_topic_score_gemma":0.060710628,"teacher_disagreement_score":0.012287081,"about_ca_system_score_codex":0.00040655333,"about_ca_system_score_gemma":0.00018774997,"threshold_uncertainty_score":0.02443111},"labels":[],"label_agreement":null},{"id":"W3213276065","doi":"10.1029/2021jb022201","title":"New Insights Into the Rift to Drift Transition Across the Northeastern Nova Scotian Margin From Wide‐Angle Seismic Waveform Inversion and Reflection Imaging","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Division of Ocean Sciences; Ocean Frontier Institute","keywords":"Geology; Continental margin; Oceanic crust; Seismology; Rift; Magmatism; Continental crust; Mantle (geology); Breakup; Crust; Basement; Inversion (geology); Paleontology; Subduction; Tectonics","score_opus":0.03017986193174319,"score_gpt":0.30963600026370663,"score_spread":0.2794561383319634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3213276065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996725,0.000079781945,0.00067827554,0.000041999694,0.00000419314,0.000008796313,0.00037675723,0.000029687812,0.002055602],"genre_scores_gemma":[0.99906343,0.00003478791,0.00033398956,0.000005566744,0.0000015258946,0.0000014627732,0.00020971891,0.0000062583817,0.0003431962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999604,0.0000035431824,0.0000020574496,0.000011840121,0.000009062254,0.000013055983],"domain_scores_gemma":[0.99988365,0.000018737474,0.000024804023,0.000009043515,0.000039827537,0.000023990291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010165978,0.00019415833,0.00008872495,0.00065176684,0.00021372385,0.0005282029,0.00014568855,0.00013781447,0.001398109],"category_scores_gemma":[0.00040549357,0.00015294572,0.00016806778,0.00049303105,0.00021116696,0.000142443,0.0002650253,0.00012167792,0.00017140737],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000187671,0.00005587589,0.8475033,0.00007278019,0.00008763969,0.0011191731,0.0010025905,0.020082576,0.0845278,0.0006534432,0.0008524925,0.043854654],"study_design_scores_gemma":[0.000007962968,0.000007677963,0.9817359,0.000010119642,0.000009386312,0.00006628391,0.00028295146,0.016730143,0.00061326835,0.00006614316,0.0004642761,0.0000059636745],"about_ca_topic_score_codex":0.36586136,"about_ca_topic_score_gemma":0.5243254,"teacher_disagreement_score":0.63413864,"about_ca_system_score_codex":0.00081667275,"about_ca_system_score_gemma":0.00092935166,"threshold_uncertainty_score":0.7274636},"labels":[],"label_agreement":null},{"id":"W3214402774","doi":"10.1002/essoar.10508717.1","title":"Tectonic evolution of the Nootka fault zone and deformation of the shallow subducted Explorer plate in northern Cascadia as revealed by earthquake distributions and seismic tomography","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Geology; Geological survey; Seismology; Plate tectonics; Tectonics; Geophysics","score_opus":0.00848805877109269,"score_gpt":0.19241982262989332,"score_spread":0.18393176385880064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3214402774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948466,0.000025103504,0.000028830373,0.000013838426,5.923879e-7,0.0000015648595,0.00010836881,0.0000057081115,0.000331175],"genre_scores_gemma":[0.9995388,0.000033031738,0.00006467763,0.0000035740852,7.846605e-7,0.0000033528324,0.00015938161,0.0000021767398,0.00019417441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998523,0.00001423224,0.00001205267,0.000057897745,0.00003487952,0.000028580942],"domain_scores_gemma":[0.9995803,0.00003189857,0.00013698597,0.000042246247,0.00005968401,0.0001488088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019498038,0.00027022863,0.00021603261,0.0010750465,0.00040426233,0.00047356373,0.00024515364,0.00023444254,0.0006946622],"category_scores_gemma":[0.0007318318,0.0002095038,0.00018841225,0.00094566634,0.00058894185,0.00019812355,0.00056124787,0.00017058806,0.00010136754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010451581,0.00002240517,0.97804123,0.000024906923,0.000048776554,0.00039242953,0.0013122042,0.002520102,0.013270404,0.00011489868,0.00013153176,0.0040166145],"study_design_scores_gemma":[0.0000016542795,0.0000060029706,0.999373,0.0000020414109,0.0000044004787,0.00002650376,0.00014609803,0.00028176658,0.0000655975,0.000007027306,0.00008365703,0.0000024312974],"about_ca_topic_score_codex":0.13055055,"about_ca_topic_score_gemma":0.24913865,"teacher_disagreement_score":0.86944944,"about_ca_system_score_codex":0.0011476934,"about_ca_system_score_gemma":0.0007721169,"threshold_uncertainty_score":0.25958133},"labels":[],"label_agreement":null},{"id":"W3215033000","doi":"10.1029/2021jb022161","title":"Continuous Tremor Activity With Stable Polarization Direction Following the 2014 Large Slow Slip Event in the Hikurangi Subduction Margin Offshore New Zealand","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"Japan Society for the Promotion of Science; University of Tokyo; Ministry of Education, Culture, Sports, Science and Technology; National Science Foundation","keywords":"Seismology; Geology; Episodic tremor and slip; Subduction; Slip (aerodynamics); Seismometer; Submarine pipeline; Seamount; Plate tectonics; Tectonics; Paleontology; Oceanography","score_opus":0.022386872690543576,"score_gpt":0.290037639695184,"score_spread":0.2676507670046404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3215033000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994646,0.000014135123,0.000039247127,0.000008915336,0.0000016265493,0.0000050313456,0.00013170879,0.000002812227,0.00033188885],"genre_scores_gemma":[0.9994497,0.000028586765,0.00006461848,0.000004597419,0.0000027696399,0.000005850854,0.00019113004,0.0000011994068,0.0002514761],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998957,0.000006948551,0.000007678314,0.000024601226,0.000040115174,0.000024965439],"domain_scores_gemma":[0.99960035,0.000032301214,0.00015549838,0.000020539932,0.00011243588,0.000078780715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017747909,0.00018956137,0.00022468294,0.00085903076,0.0003804733,0.0003845475,0.00020622005,0.00023178851,0.0007939341],"category_scores_gemma":[0.00065364985,0.00014681017,0.00013404217,0.00077622157,0.0005112523,0.00020509213,0.0005618125,0.0002345675,0.00015641653],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039849256,0.0001038338,0.9386743,0.00005261353,0.000057930105,0.0012012037,0.0024032816,0.00036433208,0.04512136,0.000046527068,0.00042122847,0.011154975],"study_design_scores_gemma":[0.0000022283853,0.000024619903,0.9993549,0.0000019587771,0.0000030733624,0.00002934846,0.00024021562,0.00010010344,0.00016701203,0.0000034336722,0.00007118457,0.0000019462457],"about_ca_topic_score_codex":0.078392856,"about_ca_topic_score_gemma":0.13550511,"teacher_disagreement_score":0.078392856,"about_ca_system_score_codex":0.0005353283,"about_ca_system_score_gemma":0.000409513,"threshold_uncertainty_score":0.15587312},"labels":[],"label_agreement":null},{"id":"W3215941549","doi":"10.1002/essoar.10502924.1","title":"Are narrow spatial aftershock zones specific to fluid-induced earthquakes?","year":2020,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Aftershock; Induced seismicity; Seismology; Geology; Tectonics","score_opus":0.04905235235039591,"score_gpt":0.221391089366668,"score_spread":0.1723387370162721,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3215941549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943615,0.00047258651,0.0015856153,0.00018615813,0.000013095406,0.0000162778,0.00049109367,0.00003682602,0.0028370016],"genre_scores_gemma":[0.9992768,0.0001099351,0.00025588408,0.000023331206,0.000009889452,0.0000047936737,0.00015137414,0.000004271795,0.0001637235],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997516,0.000028566374,0.00002534594,0.000092409,0.000026559506,0.00007544382],"domain_scores_gemma":[0.99824095,0.000278987,0.0009499299,0.00017717702,0.00019353561,0.00015947202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033632907,0.0001504404,0.00027796577,0.0012163346,0.00026096008,0.0009511957,0.0002857772,0.00049567793,0.0019426025],"category_scores_gemma":[0.0024860755,0.00017350343,0.0001585104,0.0011988848,0.0007402809,0.0008750745,0.0004575453,0.00020769487,0.00039900365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013347165,0.000034067045,0.96772766,0.00007959815,0.00006392776,0.00018583087,0.00069287117,0.0006643473,0.008129568,0.0006649765,0.0005089727,0.021114748],"study_design_scores_gemma":[0.000001998616,0.000018056551,0.99808586,0.0000095637415,0.000010149694,0.00008549813,0.0004929189,0.0002986399,0.0002592088,0.00022362167,0.0005099539,0.000004484056],"about_ca_topic_score_codex":0.006613754,"about_ca_topic_score_gemma":0.016337378,"teacher_disagreement_score":0.006613754,"about_ca_system_score_codex":0.00030367845,"about_ca_system_score_gemma":0.0002534457,"threshold_uncertainty_score":0.013150513},"labels":[],"label_agreement":null},{"id":"W3216058452","doi":"10.4138/atlgeol.2021.015","title":"Investigation of the Cape Fear arch and East Coast fault system in the Coastal Plain of North Carolina and northeastern South Carolina, USA, using LiDAR data","year":2021,"lang":"en","type":"article","venue":"Atlantic Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Coastal plain; Lineament; Fault scarp; Cape; Batholith; Fault (geology); Sinistral and dextral; Geomorphology; Structural basin; Seismology; Paleontology; Tectonics; Archaeology; Geography","score_opus":0.04129484985427751,"score_gpt":0.22233487366468208,"score_spread":0.18104002381040457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216058452","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924281,0.000073731004,0.00024584623,0.00010104434,0.0000040255863,0.00003548756,0.0011832205,0.000024539471,0.00590403],"genre_scores_gemma":[0.9944682,0.00013175615,0.0011203733,0.00005638412,0.0000041409457,0.000046116867,0.0014237959,0.0000061146534,0.002743006],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985576,0.000007917549,0.0000068383197,0.000034239696,0.00006549012,0.000029796545],"domain_scores_gemma":[0.9993693,0.00007240576,0.0001173633,0.000020965543,0.00033467956,0.00008530206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011032224,0.00015765033,0.00011046383,0.00212576,0.0011906457,0.0006212913,0.00046004116,0.00016600855,0.0014963355],"category_scores_gemma":[0.00058745785,0.00012036581,0.00011270675,0.0026677041,0.00040362217,0.00019930491,0.0005387494,0.00022437742,0.00016157169],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054279495,0.000050404065,0.93878037,0.00008288531,0.000032818607,0.0016919038,0.0037192577,0.0010768697,0.013096894,0.00063886866,0.0034011977,0.03737426],"study_design_scores_gemma":[0.0000020242287,0.0000073795563,0.9931138,0.000020715395,0.000006282564,0.00011428498,0.00276657,0.00068588357,0.00024837206,0.000030372252,0.0029982242,0.0000060629272],"about_ca_topic_score_codex":0.65292853,"about_ca_topic_score_gemma":0.9021951,"teacher_disagreement_score":0.65292853,"about_ca_system_score_codex":0.0016921802,"about_ca_system_score_gemma":0.003137947,"threshold_uncertainty_score":0.69823086},"labels":[],"label_agreement":null},{"id":"W3216153088","doi":"10.3390/rs13234872","title":"What Is the Impact of Tectonic Plate Movement on Country Size? A Long-Term Forecast","year":2021,"lang":"en","type":"article","venue":"Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Akademia Górniczo-Hutnicza im. Stanislawa Staszica; York University; Uniwersytet Pedagogiczny im. Komisji Edukacji Narodowej w Krakowie; Uniwersytet Rolniczy im. Hugona Kołłątaja w Krakowie","keywords":"Tectonics; Plate tectonics; Geology; Land area; Term (time); Lithosphere; Geography; Seismology; Environmental science","score_opus":0.019745255487956557,"score_gpt":0.2529787215762465,"score_spread":0.23323346608828996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216153088","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8351718,0.005143945,0.023326369,0.02812078,0.00078177033,0.00007661233,0.016922876,0.00037635575,0.09007953],"genre_scores_gemma":[0.99114764,0.0021013832,0.0012655462,0.00021792595,0.00012024986,0.000018841392,0.0018130549,0.000031951255,0.003283388],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997929,0.000043714714,0.000013055725,0.00004872721,0.000050612216,0.000050939798],"domain_scores_gemma":[0.9982254,0.00060480175,0.0004224007,0.000090118505,0.00047218337,0.00018503182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007825867,0.00032163828,0.0002547197,0.0010818441,0.00022830653,0.0014379738,0.00042994495,0.00066207343,0.0051196567],"category_scores_gemma":[0.004961892,0.00013859727,0.00047880062,0.0011761261,0.0004203057,0.001984844,0.0004370221,0.0009139503,0.000630863],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002322963,0.000088425,0.47584087,0.00045466985,0.00027030995,0.0008474394,0.000661731,0.33360687,0.0026660222,0.046340562,0.032433055,0.10655778],"study_design_scores_gemma":[0.00002150804,0.00027726425,0.64926994,0.00038861937,0.00020702167,0.00033135805,0.0026606345,0.26678026,0.0021651296,0.026973693,0.050813116,0.00011141949],"about_ca_topic_score_codex":0.035884663,"about_ca_topic_score_gemma":0.023776613,"teacher_disagreement_score":0.035884663,"about_ca_system_score_codex":0.001322812,"about_ca_system_score_gemma":0.00063563214,"threshold_uncertainty_score":0.07135159},"labels":[],"label_agreement":null},{"id":"W3216512515","doi":"10.1080/00288306.2021.1995007","title":"Paleoseismology of the Hyde Fault, Otago, New Zealand","year":2021,"lang":"en","type":"article","venue":"New Zealand Journal of Geology and Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"Earthquake Commission","keywords":"Fault scarp; Paleoseismology; Geology; Seismology; Fault (geology); Seismic hazard; Digital elevation model; Alluvial fan; Structural basin; Alluvium; Thermoluminescence dating; Active fault; Surface rupture; Basin and range topography; Geomorphology; Paleontology; Tectonics; Remote sensing","score_opus":0.009736795166581325,"score_gpt":0.20803565828713066,"score_spread":0.19829886312054934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216512515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971033,0.00017974354,0.00013972005,0.000027432367,0.0000019013527,0.000012244073,0.00013538981,0.000002655034,0.0023977144],"genre_scores_gemma":[0.99896514,0.00016600084,0.00019970279,0.000006248463,0.0000011664823,0.0000050107546,0.00007228239,0.0000014857488,0.00058294873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998945,0.0000059834297,0.000008336486,0.000036147176,0.000030581083,0.000024439632],"domain_scores_gemma":[0.99970454,0.000036128455,0.00012805572,0.000021108137,0.000068897316,0.000041144387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018234887,0.00019397515,0.00017153473,0.001057697,0.00061238883,0.0007117904,0.0001967628,0.00020313605,0.0020458272],"category_scores_gemma":[0.0006283419,0.00019661953,0.00012700415,0.0011725427,0.0010184399,0.00057683163,0.0006082933,0.0002775479,0.00014046002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003647853,0.000040889387,0.87616557,0.0002648075,0.00007955467,0.002582984,0.012329899,0.0007671862,0.049232222,0.00076319446,0.00020327461,0.057205625],"study_design_scores_gemma":[0.0000038057976,0.00002586151,0.9973189,0.000013534299,0.000006154363,0.00029565673,0.0009055089,0.00007625713,0.0001817603,0.000042782038,0.0011253619,0.0000044019503],"about_ca_topic_score_codex":0.16629997,"about_ca_topic_score_gemma":0.35451734,"teacher_disagreement_score":0.16629997,"about_ca_system_score_codex":0.0012348748,"about_ca_system_score_gemma":0.00062726013,"threshold_uncertainty_score":0.33066398},"labels":[],"label_agreement":null},{"id":"W3216674056","doi":"10.1785/0320210032","title":"Seismic Constraint on Heterogeneous Deformation and Stress State in the Forearc of the Hikurangi Subduction Zone, New Zealand","year":2021,"lang":"en","type":"article","venue":"The Seismic Record","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Forearc; Geology; Seismology; Subduction; Crust; Slip (aerodynamics); Oceanic crust; Convergent boundary; Tectonics; Geophysics","score_opus":0.014574669714048973,"score_gpt":0.2063104621373631,"score_spread":0.19173579242331412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216674056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995029,0.000019268022,0.000033619668,0.0000039158913,1.7327241e-7,0.0000017620806,0.00010996249,0.0000010178862,0.00032742845],"genre_scores_gemma":[0.9996773,0.000027246791,0.000053529835,0.0000016012848,3.3870876e-7,0.0000022845177,0.00014598608,7.4995626e-7,0.00009095656],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989164,0.00000805127,0.000011039785,0.00003105926,0.000025018224,0.0000330672],"domain_scores_gemma":[0.99956626,0.00006425771,0.00017072166,0.000033308716,0.00009052469,0.000074858755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018457061,0.00019422409,0.0002208227,0.00084515364,0.00036834218,0.0006084661,0.00023213639,0.00012672132,0.001135285],"category_scores_gemma":[0.00081801467,0.0002060801,0.00012422192,0.0010862594,0.00061520416,0.00027680796,0.0004940774,0.00016024911,0.00013679756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023424202,0.000030723168,0.9428147,0.000046736754,0.00004634042,0.0003027547,0.0022914023,0.0005718707,0.04467224,0.00010942494,0.000076958495,0.008802467],"study_design_scores_gemma":[0.0000012887343,0.000007520015,0.9994764,0.0000018255276,0.0000032578764,0.00002358333,0.00021411794,0.0000896057,0.00012085626,0.0000050647964,0.000055185898,0.0000013718899],"about_ca_topic_score_codex":0.20923762,"about_ca_topic_score_gemma":0.35780597,"teacher_disagreement_score":0.20923762,"about_ca_system_score_codex":0.0008179788,"about_ca_system_score_gemma":0.0006265563,"threshold_uncertainty_score":0.41603947},"labels":[],"label_agreement":null},{"id":"W3217208577","doi":"10.1029/2021jb023013","title":"3D Active Source Seismic Imaging of the Alpine Fault Zone and the Whataroa Glacial Valley in New Zealand","year":2021,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"Canada Research Chairs; Technische Universität Bergakademie Freiberg; Victoria University of Wellington; Victoria University; Deutsche Forschungsgemeinschaft; University of Alberta; Natural Sciences and Engineering Research Council of Canada; Government of Alberta; Earthquake Commission; University of Otago","keywords":"Geology; Borehole; Seismology; Fault (geology); Geophysical imaging; Tectonics; Drilling; Glacial period; Trough (economics); Reflector (photography); Geomorphology; Paleontology","score_opus":0.020964325325717216,"score_gpt":0.2870343089268938,"score_spread":0.26606998360117656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3217208577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99075085,0.0002057326,0.0011026686,0.000112012436,0.000013244659,0.00006649822,0.0020068414,0.00010214033,0.0056400555],"genre_scores_gemma":[0.99420726,0.0002170492,0.0029206425,0.000029879935,0.000012869597,0.000034320987,0.00093228207,0.00003032004,0.0016152972],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999219,0.0000025205122,0.0000031452216,0.000018616713,0.000035340105,0.000018612382],"domain_scores_gemma":[0.9998847,0.000010980341,0.000029537397,0.0000068016525,0.000040500672,0.000027448013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011653834,0.00039027762,0.0002469683,0.0021977099,0.00039443534,0.0009211172,0.00031413353,0.00037548834,0.0026310184],"category_scores_gemma":[0.00026874535,0.0003732672,0.00025050947,0.0015110774,0.00028382544,0.0002895551,0.00046882787,0.00028671246,0.00031966955],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006425725,0.00033177264,0.33148307,0.0005195138,0.00024611884,0.007073467,0.006617761,0.009907093,0.52475846,0.0006106849,0.0042606927,0.11354891],"study_design_scores_gemma":[0.000050716837,0.00005912341,0.98757625,0.000052180403,0.00004263725,0.00068257184,0.0014582892,0.0057571027,0.0018244059,0.000073793824,0.0023957784,0.000027087597],"about_ca_topic_score_codex":0.13575277,"about_ca_topic_score_gemma":0.29697597,"teacher_disagreement_score":0.13575277,"about_ca_system_score_codex":0.00055611215,"about_ca_system_score_gemma":0.0007090485,"threshold_uncertainty_score":0.26992518},"labels":[],"label_agreement":null},{"id":"W34584202","doi":"10.4401/ag-4625","title":"Inge Lehmann’s work materials and seismological epistolary archive","year":2009,"lang":"en","type":"article","venue":"Annals of Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Commission; History; Art history; Work (physics); Biography; Library science; Political science; Physics; Computer science; Law","score_opus":0.03948391675846632,"score_gpt":0.2494475941080468,"score_spread":0.20996367734958046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W34584202","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.003196915,0.028846761,0.0061333487,0.016595036,0.01824452,0.00021984463,0.030437864,0.0039507854,0.89237493],"genre_scores_gemma":[0.023340102,0.023845298,0.0065007797,0.0018300512,0.00556633,0.00019636363,0.018877886,0.0028134568,0.9170298],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987562,0.00013578132,0.00012336177,0.00011515668,0.0007064135,0.00016312867],"domain_scores_gemma":[0.99763,0.000480853,0.00021850751,0.00047556372,0.0008042764,0.00039072646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011834889,0.0009036173,0.0005433104,0.00726297,0.002524848,0.005368783,0.0007310988,0.0008647265,0.24305658],"category_scores_gemma":[0.0062557794,0.00033040871,0.0002724737,0.006329111,0.00091080513,0.0027255646,0.002699349,0.0010264394,0.13857603],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025981524,0.00001103218,0.00010338655,0.00015139022,0.000002679199,0.000088549605,0.00038196286,0.00007439307,0.0002598104,0.01201836,0.9080578,0.07882464],"study_design_scores_gemma":[8.417944e-7,0.000001365221,0.00018945345,0.00005021338,6.507918e-7,0.000036769772,0.00008328033,0.000012494594,0.00007979449,0.000836853,0.99870396,0.000004261942],"about_ca_topic_score_codex":0.008666083,"about_ca_topic_score_gemma":0.011832513,"teacher_disagreement_score":0.24305658,"about_ca_system_score_codex":0.001717168,"about_ca_system_score_gemma":0.002804396,"threshold_uncertainty_score":0.8131053},"labels":[],"label_agreement":null},{"id":"W379177299","doi":"","title":"Observation and data analysis","year":2009,"lang":"en","type":"book","venue":"Birkhäuser eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tsunami earthquake; Geology; Seismology; Tide gauge; Bay; Oceanography; Subduction; Intraplate earthquake; Shore; Trench; Sea level; Tectonics","score_opus":0.07076520799477123,"score_gpt":0.25252825388969397,"score_spread":0.18176304589492273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W379177299","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.018014574,0.0009941766,0.026325312,0.0022088748,0.0014054241,0.007858651,0.7788384,0.0031745902,0.16118011],"genre_scores_gemma":[0.07514184,0.0017618355,0.048525464,0.002391519,0.000883109,0.019424886,0.7147627,0.0012729547,0.13583575],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9922929,0.0011403038,0.0015575942,0.0021704773,0.002219402,0.0006193112],"domain_scores_gemma":[0.980821,0.0019777503,0.0014666336,0.0043339636,0.0107244635,0.000676198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004346668,0.0011551122,0.0011850541,0.0072816354,0.0014487857,0.0027367743,0.0022008722,0.0011278469,0.11482692],"category_scores_gemma":[0.017163126,0.0004575274,0.00093763083,0.01289518,0.0005617167,0.002240575,0.0034356068,0.0012941733,0.07507631],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004045609,0.00035315132,0.05400643,0.0014589821,0.00011990791,0.00033688132,0.0013658289,0.0010912073,0.00181852,0.00625102,0.57969815,0.3530953],"study_design_scores_gemma":[0.00006538024,0.00009354753,0.043789096,0.00042616256,0.000040937637,0.00011243532,0.0018045151,0.00094542035,0.0010777308,0.0020626613,0.9495295,0.000052727737],"about_ca_topic_score_codex":0.02620391,"about_ca_topic_score_gemma":0.016213173,"teacher_disagreement_score":0.11482692,"about_ca_system_score_codex":0.002667444,"about_ca_system_score_gemma":0.008464524,"threshold_uncertainty_score":0.3841343},"labels":[],"label_agreement":null},{"id":"W4200191173","doi":"10.1007/s00024-021-02918-5","title":"Introduction to “Sixty Years of Modern Tsunami Science, Volume 1: Lessons and Progress”","year":2021,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Hazard; Volume (thermodynamics); Probabilistic logic; History; Seismology; Geology; Geography; Statistics; Mathematics","score_opus":0.008693657342083019,"score_gpt":0.2109852750252137,"score_spread":0.20229161768313067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200191173","genre_codex":"review","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00096147263,0.45710608,0.014014124,0.2004476,0.26864702,0.000112084315,0.0019835755,0.0004730896,0.056254916],"genre_scores_gemma":[0.014031864,0.35834536,0.015685543,0.17706662,0.2714568,0.00031700634,0.0029569762,0.0007430736,0.15939684],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99907887,0.00027024845,0.000098123775,0.00016482518,0.00030287472,0.000085049134],"domain_scores_gemma":[0.99733835,0.0013923306,0.0001612539,0.00013013091,0.0007127651,0.00026521218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015378292,0.0013110926,0.0008555072,0.0018123507,0.0012978542,0.0036999246,0.0014564194,0.0023397205,0.027712068],"category_scores_gemma":[0.005413063,0.00033423238,0.00074494234,0.0024507327,0.0027303293,0.0046153693,0.0023810114,0.005142894,0.011889035],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027206892,0.000014975546,0.00015486246,0.00046142275,0.000007638665,0.000027733182,0.00021841482,0.00009436501,0.00021424996,0.015684042,0.9394354,0.043659694],"study_design_scores_gemma":[0.000003694576,0.000011869029,0.000350708,0.000328635,0.0000031359643,0.00006950873,0.00012906539,0.00003193179,0.000060079972,0.008550543,0.99045134,0.000009493601],"about_ca_topic_score_codex":0.003392576,"about_ca_topic_score_gemma":0.0074555255,"teacher_disagreement_score":0.027712068,"about_ca_system_score_codex":0.0013569393,"about_ca_system_score_gemma":0.0031951247,"threshold_uncertainty_score":0.092706144},"labels":[],"label_agreement":null},{"id":"W4200326451","doi":"10.1002/essoar.10507370.1","title":"Mass transfer into the leading edge of the mantle wedge: Initial results from Oman Drilling Project Hole BT1B","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Calgary","funders":"Alfred P. Sloan Foundation; National Science Foundation","keywords":"World Wide Web; Computer science","score_opus":0.0450580480383939,"score_gpt":0.2620288236232673,"score_spread":0.21697077558487338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200326451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99484456,0.0004543729,0.00034756443,0.000043044296,0.0000063531465,0.000023180808,0.001301814,0.000033510052,0.0029455654],"genre_scores_gemma":[0.9962883,0.00038571973,0.0009386877,0.00003561031,0.000007948909,0.000028388982,0.0010397121,0.000021010723,0.0012545944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979776,0.00002066653,0.000009919617,0.000038550483,0.00006542428,0.00006772107],"domain_scores_gemma":[0.9998772,0.000025757941,0.000030682448,0.000012646159,0.000041284988,0.0000124753315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040221176,0.00076288107,0.00041822498,0.0013057671,0.0008871188,0.00066370843,0.0003410537,0.00058868394,0.0012134729],"category_scores_gemma":[0.00041294767,0.00026180563,0.00031145618,0.0012209063,0.00046294788,0.00072690926,0.0006194433,0.00027506426,0.0004104393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025378717,0.0005703101,0.6732273,0.0009833891,0.0002529113,0.0028055387,0.005820237,0.007657543,0.17337741,0.0008647117,0.0018676008,0.13003512],"study_design_scores_gemma":[0.00005488976,0.00039140705,0.9492436,0.000079912505,0.00011094552,0.00033499452,0.0015205562,0.0030966378,0.034985356,0.00024701134,0.0099027455,0.000032055195],"about_ca_topic_score_codex":0.03471383,"about_ca_topic_score_gemma":0.051594414,"teacher_disagreement_score":0.03471383,"about_ca_system_score_codex":0.0009872726,"about_ca_system_score_gemma":0.0004919837,"threshold_uncertainty_score":0.06902355},"labels":[],"label_agreement":null},{"id":"W4200329631","doi":"10.1130/b35887.1","title":"Late Quaternary active faulting on the inherited Baoertu basement fault within the eastern Tian Shan orogenic belt: Implications for regional tectonic deformation and slip partitioning, NW China","year":2021,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Sinistral and dextral; Seismology; Quaternary; Fault (geology); Strike-slip tectonics; Thrust fault; Tectonics; Basement; Paleontology","score_opus":0.02886168348724688,"score_gpt":0.23595721309040604,"score_spread":0.20709552960315916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200329631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948645,0.00008239092,0.00007557084,0.000014339176,0.0000010209338,0.0000021712226,0.000062196916,0.0000027719377,0.00027308243],"genre_scores_gemma":[0.99973065,0.000049649698,0.000056305566,0.000004170162,0.0000013475441,0.0000016073882,0.00007351626,8.3447077e-7,0.0000820119],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989974,0.0000119956085,0.000011797171,0.000030506179,0.000021159225,0.000024711724],"domain_scores_gemma":[0.99979764,0.000015947575,0.00010155904,0.000012536819,0.000039082533,0.000033310964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022879422,0.0003068077,0.0002491679,0.0013269855,0.0003435845,0.0005465439,0.0002668806,0.00019394614,0.00068674714],"category_scores_gemma":[0.00025722117,0.000151691,0.00022851976,0.0017047566,0.00042927047,0.0002974311,0.00027809697,0.00011191872,0.00008661801],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004981812,0.000016425769,0.9796091,0.000037118232,0.000047146794,0.00015495741,0.0003928808,0.0009351581,0.010841546,0.00011938899,0.00004842636,0.0077480883],"study_design_scores_gemma":[0.0000017378941,0.000008648597,0.99853826,0.0000034939424,0.0000111006875,0.000020407848,0.00014030545,0.0010336954,0.00015146074,0.00001935234,0.0000694724,0.0000020646585],"about_ca_topic_score_codex":0.037350446,"about_ca_topic_score_gemma":0.070424184,"teacher_disagreement_score":0.037350446,"about_ca_system_score_codex":0.0007068598,"about_ca_system_score_gemma":0.0005467745,"threshold_uncertainty_score":0.074266076},"labels":[],"label_agreement":null},{"id":"W4200343524","doi":"10.3390/geohazards2040022","title":"Potential Fault Displacement Hazard Assessment Using Stochastic Source Models: A Retrospective Evaluation for the 1999 Hector Mine Earthquake","year":2021,"lang":"en","type":"article","venue":"GeoHazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Fault (geology); Displacement (psychology); Seismic hazard; Hazard; Seismology; Hazard analysis; Probabilistic logic; Geology; Engineering; Reliability engineering; Statistics; Mathematics","score_opus":0.03723132720387742,"score_gpt":0.2883193130649558,"score_spread":0.2510879858610784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200343524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99383295,0.000037756618,0.0055629206,0.000025282709,0.0000011711696,0.00001712101,0.00013609602,0.00002750158,0.00035916193],"genre_scores_gemma":[0.99800676,0.000034378692,0.0016811402,0.0000020487823,0.0000014545566,0.0000047457734,0.00014928369,0.000002559369,0.00011769982],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99974066,0.0001077786,0.000018998002,0.000034490553,0.00008298374,0.000015221667],"domain_scores_gemma":[0.99873513,0.00055244216,0.0002540188,0.00013082678,0.00029081493,0.000036621204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00112329,0.00030466035,0.00027162165,0.0007813069,0.00014525202,0.0002840366,0.00034337988,0.00039002136,0.00031629484],"category_scores_gemma":[0.00295753,0.00019771272,0.0002805344,0.00038481614,0.00018820129,0.0004533067,0.00035720944,0.00020595654,0.00008532559],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073018746,0.00040222422,0.4488202,0.00012312552,0.00016608738,0.0012927616,0.0007078988,0.4809844,0.013796658,0.001349114,0.0006021505,0.05102523],"study_design_scores_gemma":[0.000028334225,0.00087900116,0.14409119,0.000012934602,0.00006163602,0.00040883917,0.00042434633,0.8480573,0.005042786,0.00042493944,0.00052574347,0.00004299335],"about_ca_topic_score_codex":0.0098202815,"about_ca_topic_score_gemma":0.015809309,"teacher_disagreement_score":0.0098202815,"about_ca_system_score_codex":0.00048482066,"about_ca_system_score_gemma":0.00027758387,"threshold_uncertainty_score":0.019526243},"labels":[],"label_agreement":null},{"id":"W4200454914","doi":"10.1029/2021gl093979","title":"Complex 3D Migration and Delayed Triggering of Hydraulic Fracturing‐Induced Seismicity: A Case Study Near Fox Creek, Alberta","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Hydrogeology; Hydraulic fracturing; Seismology; Poromechanics; Pore water pressure; Fault (geology); Natural hazard; Geotechnical engineering","score_opus":0.06524063724748795,"score_gpt":0.30958456258838823,"score_spread":0.24434392534090027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200454914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952897,0.00006763287,0.0008276301,0.00015301889,0.0000074302097,0.000037768066,0.0005033728,0.00005474518,0.003058707],"genre_scores_gemma":[0.997431,0.000055250926,0.0013863852,0.000013522414,0.0000022325614,0.0000059404874,0.00018918382,0.000006527386,0.0009100129],"study_design_codex":"observational","study_design_gemma":"case_report","domain_scores_codex":[0.9998919,0.00000873989,0.000004454203,0.0000156963,0.00004501783,0.00003425906],"domain_scores_gemma":[0.99985254,0.000035257875,0.000015535532,0.000013914014,0.00003857054,0.00004416133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011145151,0.0003056903,0.00015372502,0.0008405533,0.0012568933,0.0009173803,0.00063025544,0.00063080864,0.0016862729],"category_scores_gemma":[0.00040161252,0.00017865775,0.00019401584,0.0012886573,0.00076478923,0.00019631401,0.0005147763,0.00034879107,0.00015014934],"study_design_candidate":"case_report","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006984505,0.0011003133,0.5846806,0.00033944388,0.0002023584,0.05186431,0.010447819,0.20411022,0.0444574,0.0039939797,0.0071395254,0.09096562],"study_design_scores_gemma":[0.00008055823,0.00016796791,0.7777948,0.00007159355,0.0000757683,0.0022566929,0.015290463,0.19107044,0.003948547,0.00094134075,0.008168007,0.00013380553],"about_ca_topic_score_codex":0.7497651,"about_ca_topic_score_gemma":0.92183673,"teacher_disagreement_score":0.2502349,"about_ca_system_score_codex":0.003143695,"about_ca_system_score_gemma":0.0030168104,"threshold_uncertainty_score":0.50341713},"labels":[],"label_agreement":null},{"id":"W4200508585","doi":"10.1007/978-3-030-85018-0_11","title":"Earthquake-Tsunami Risk Assessment and Critical Multi-hazard Loss Scenarios: A Case Study in Japan Under the Nankai-Tonankai Mega-Thrust","year":2021,"lang":"en","type":"book-chapter","venue":"Springer tracts in civil engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Seismic hazard; Geology; Subduction; Hazard; Fragility; Earthquake scenario; Hazard analysis; Risk assessment; Tectonics; Engineering; Reliability engineering; Computer science","score_opus":0.027280759087600092,"score_gpt":0.2645895608864007,"score_spread":0.2373088017988006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200508585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9675762,0.0012622249,0.009013782,0.0005648487,0.00004599715,0.00008522736,0.00049415225,0.00006730501,0.020890191],"genre_scores_gemma":[0.9922144,0.0005929165,0.0024447746,0.000023371756,0.000014900034,0.000018267154,0.00018128446,0.000018574365,0.0044915243],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996996,0.00011098035,0.000018300052,0.000036388792,0.00004758493,0.00008721612],"domain_scores_gemma":[0.9995203,0.00023974634,0.00006634331,0.00001598386,0.00008515839,0.00007240849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007293719,0.00092741055,0.00063440774,0.0009172894,0.0009291043,0.0018320759,0.0010339032,0.0011057046,0.002814261],"category_scores_gemma":[0.0012335777,0.00039094436,0.0008527092,0.0018163277,0.0007577268,0.0011511989,0.0009039397,0.0005111926,0.00019260708],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00068379496,0.0005561184,0.056811288,0.00033545058,0.00025546178,0.015320974,0.0018103374,0.8192999,0.0037488407,0.019428097,0.007903233,0.07384651],"study_design_scores_gemma":[0.00007953372,0.0006339654,0.078487836,0.00010503488,0.00036028682,0.0018745192,0.008470016,0.8790553,0.0013146746,0.020575756,0.008925824,0.00011727818],"about_ca_topic_score_codex":0.055973243,"about_ca_topic_score_gemma":0.089903444,"teacher_disagreement_score":0.055973243,"about_ca_system_score_codex":0.0028372905,"about_ca_system_score_gemma":0.0011683216,"threshold_uncertainty_score":0.111294866},"labels":[],"label_agreement":null},{"id":"W4205175616","doi":"10.1002/essoar.10510181.1","title":"Aseismic Fault Slip during a Shallow Normal-Faulting Seismic Swarm Constrained Using a Physically-Informed Geodetic Inversion Method","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Natural Environment Research Council; Canadian Space Agency; Banco Bilbao Vizcaya Argentaria; Fundación BBVA; Sight Research UK; Ministerio de Ciencia e Innovación; Cabildo de Tenerife","keywords":"Slip (aerodynamics); Seismology; Geology; Geodetic datum; Slipping; Swarm behaviour; Episodic tremor and slip; Geodesy; Inversion (geology); Computer science; Tectonics; Geometry; Subduction; Mathematics; Artificial intelligence; Engineering","score_opus":0.030218041105970667,"score_gpt":0.2764779109223658,"score_spread":0.2462598698163951,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205175616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8406145,0.000074358475,0.1573388,0.0002040593,0.00001825381,0.000029952313,0.00018155728,0.0002810226,0.0012575559],"genre_scores_gemma":[0.9711727,0.000030983425,0.02817955,0.000024150475,0.000014243075,0.000023331446,0.00017508416,0.00001886665,0.00036113162],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999541,0.000010391824,0.0000035156104,0.0000145963895,0.00000898283,0.000008552451],"domain_scores_gemma":[0.99987864,0.000040076786,0.000031384174,0.000015073968,0.00002300839,0.000011842474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019824145,0.0003086016,0.00021653746,0.0002454832,0.00013487748,0.00030068602,0.00048390764,0.00040979183,0.0004440427],"category_scores_gemma":[0.0005962407,0.0002453517,0.00029532574,0.00019975998,0.00029426953,0.00025379294,0.00026218308,0.00035867232,0.000059389895],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007094452,0.0000611706,0.008338273,0.00003311511,0.000040597053,0.00013127642,0.00008271135,0.95124054,0.019514639,0.0011968117,0.000286783,0.019003166],"study_design_scores_gemma":[0.0000047914264,0.000004385971,0.0010357182,0.0000010726054,0.0000022645659,0.0000048662396,0.0000045628894,0.99843496,0.00035870099,0.000099234145,0.00004672965,0.0000027558756],"about_ca_topic_score_codex":0.009284153,"about_ca_topic_score_gemma":0.009972463,"teacher_disagreement_score":0.009284153,"about_ca_system_score_codex":0.0002456644,"about_ca_system_score_gemma":0.0005954232,"threshold_uncertainty_score":0.018460214},"labels":[],"label_agreement":null},{"id":"W4205229079","doi":"10.26686/wgtn.13876499.v1","title":"Petrophysical, geochemical, and hydrological evidence for extensive fracture-mediated fluid and heat transport in the Alpine Fault's hanging-wall damage zone","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Alberta","funders":"Marsden Fund; Natural Environment Research Council; Victoria University; Ministry of Business, Innovation and Employment; Royal Society Te Apārangi; Victoria University of Wellington; Royal Society; University of Otago","keywords":"Geology; Borehole; Petrophysics; Seismology; Fault (geology); Active fault; Crust; Shear zone; Petrology; Permeability (electromagnetism); Geophysics; Geotechnical engineering; Porosity; Tectonics","score_opus":0.03399968277812067,"score_gpt":0.2589348601526312,"score_spread":0.22493517737451052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205229079","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995536,0.00004509398,0.00006318429,0.00001125972,4.1260725e-7,0.0000010431902,0.00005837771,0.000005412622,0.0002616966],"genre_scores_gemma":[0.9997639,0.00003121608,0.00006521924,0.0000036474398,0.0000024159592,7.5375135e-7,0.000096721495,7.229921e-7,0.000035446643],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988496,0.000013394484,0.000012248549,0.00003028274,0.000033509514,0.00002553474],"domain_scores_gemma":[0.99965644,0.000035623318,0.00019240857,0.00002584496,0.00003924964,0.000050392486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015864741,0.00021147686,0.00020517956,0.0013298601,0.00041555162,0.0005458684,0.00021046042,0.00031029232,0.00077187706],"category_scores_gemma":[0.00034796758,0.00014793887,0.0001331215,0.000858067,0.0007992606,0.0003766318,0.0005757734,0.00016755189,0.00008924664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007937424,0.00004078746,0.96543336,0.000024999805,0.00003514808,0.00040472887,0.00047826263,0.0007295114,0.026209202,0.000113894115,0.000060095994,0.0063906093],"study_design_scores_gemma":[0.000002723347,0.000014859283,0.9986842,0.0000023059117,0.000004437175,0.000091186346,0.00013860568,0.00053899427,0.00039981815,0.000037158923,0.00008381475,0.0000019403376],"about_ca_topic_score_codex":0.0081552,"about_ca_topic_score_gemma":0.013193444,"teacher_disagreement_score":0.0081552,"about_ca_system_score_codex":0.00042297534,"about_ca_system_score_gemma":0.00019732965,"threshold_uncertainty_score":0.016215444},"labels":[],"label_agreement":null},{"id":"W4205455636","doi":"10.1029/2021jb023060","title":"The Rise, Peak and Decline of the Seismic Hazard Related to Hydraulic Fracturing Activities in the Duvernay Play, Fox Creek Area, Alberta","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Alberta Energy","funders":"","keywords":"Induced seismicity; Seismic hazard; Hydraulic fracturing; Seismology; Geology; Maximum magnitude; Magnitude (astronomy); Hazard; Seismic risk; Geotechnical engineering","score_opus":0.02540457904909806,"score_gpt":0.2925095162745289,"score_spread":0.2671049372254309,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205455636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99684566,0.00012027531,0.00014608713,0.00008020741,0.0000025162685,0.000008448229,0.0009016959,0.000011699565,0.0018833991],"genre_scores_gemma":[0.9975198,0.00009675357,0.00012992304,0.000013496535,0.0000016763064,0.0000033356605,0.00055544823,0.00000204699,0.0016774972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981874,0.000010056551,0.0000060632083,0.00002777847,0.000073145566,0.00006413085],"domain_scores_gemma":[0.99951947,0.000048818154,0.0000908562,0.000014372605,0.000199238,0.00012716561],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018984573,0.00018817814,0.00012312284,0.0012880457,0.0005779463,0.0007776631,0.0005507943,0.0002590372,0.0016188602],"category_scores_gemma":[0.0007453574,0.00013000653,0.00017515836,0.0012671744,0.0006562849,0.00018200406,0.00046624415,0.00017543785,0.00012729404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008838127,0.000022464532,0.9855735,0.00002270962,0.000042043543,0.00025319715,0.00080030813,0.0024317743,0.0017797401,0.00031449168,0.0008074955,0.007863861],"study_design_scores_gemma":[0.0000020884258,0.000009748584,0.9973901,0.0000057241837,0.0000052375394,0.000023892244,0.0008386619,0.00090234453,0.00008320401,0.000022831386,0.00071213185,0.000004142919],"about_ca_topic_score_codex":0.9655159,"about_ca_topic_score_gemma":0.98849046,"teacher_disagreement_score":0.03448409,"about_ca_system_score_codex":0.008458895,"about_ca_system_score_gemma":0.0057156407,"threshold_uncertainty_score":0.06937426},"labels":[],"label_agreement":null},{"id":"W4205812252","doi":"10.1029/2021gl096974","title":"Upper Plate Structure and Megathrust Properties in the Shumagin Gap Near the July 2020 M7.8 Simeonof Event","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Subduction; Seismology; Episodic tremor and slip; Slip (aerodynamics); Crust; Plate tectonics; Tectonics; Interplate earthquake; Convergent boundary; Induced seismicity; Geophysics; Oceanic crust","score_opus":0.03878019524748188,"score_gpt":0.26878755371604446,"score_spread":0.23000735846856257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205812252","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997352,0.000006846467,0.00006699458,0.000008844824,5.040366e-7,7.5384463e-7,0.000030542695,0.000004939633,0.00014550789],"genre_scores_gemma":[0.999819,0.000005887547,0.0000397815,0.0000018115587,5.6480167e-7,7.6430274e-7,0.000078478246,0.0000014702159,0.000052324718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999504,0.000008520482,0.0000034887014,0.000015684604,0.0000071823524,0.000014749772],"domain_scores_gemma":[0.9998853,0.000018300014,0.00002573772,0.000012945566,0.000021870084,0.00003587588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019573292,0.0002966266,0.0002945412,0.0004470812,0.0003405907,0.0006477624,0.00040359714,0.0006614209,0.0009739232],"category_scores_gemma":[0.00044792413,0.0002651451,0.00037729766,0.0002462648,0.00032924153,0.00034857105,0.00036920473,0.00019609867,0.00020724346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020340054,0.0001293866,0.9109269,0.000023564822,0.000083998246,0.0002915488,0.00031275206,0.074798375,0.009292471,0.0004637002,0.00019604074,0.0032778839],"study_design_scores_gemma":[0.000017486944,0.000105689636,0.7364506,0.000010653273,0.000031860447,0.000071182156,0.000500979,0.261484,0.00093509245,0.0001934092,0.00018001333,0.00001911666],"about_ca_topic_score_codex":0.04411158,"about_ca_topic_score_gemma":0.041814525,"teacher_disagreement_score":0.04411158,"about_ca_system_score_codex":0.0007742274,"about_ca_system_score_gemma":0.00035252245,"threshold_uncertainty_score":0.087709665},"labels":[],"label_agreement":null},{"id":"W4205864738","doi":"10.26686/wgtn.13876499","title":"Petrophysical, geochemical, and hydrological evidence for extensive fracture-mediated fluid and heat transport in the Alpine Fault's hanging-wall damage zone","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Alberta","funders":"Marsden Fund; Natural Environment Research Council; Victoria University; Ministry of Business, Innovation and Employment; Royal Society Te Apārangi; Victoria University of Wellington; Royal Society; University of Otago","keywords":"Geology; Borehole; Petrophysics; Seismology; Fault (geology); Shear zone; Crust; Active fault; Petrology; Permeability (electromagnetism); Slip (aerodynamics); Monocline; Geophysics; Geotechnical engineering; Porosity; Tectonics","score_opus":0.03399968277812067,"score_gpt":0.2589348601526312,"score_spread":0.22493517737451052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205864738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995536,0.00004509398,0.00006318429,0.00001125972,4.1260725e-7,0.0000010431902,0.00005837771,0.000005412622,0.0002616966],"genre_scores_gemma":[0.9997639,0.00003121608,0.00006521924,0.0000036474398,0.0000024159592,7.5375135e-7,0.000096721495,7.229921e-7,0.000035446643],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988496,0.000013394484,0.000012248549,0.00003028274,0.000033509514,0.00002553474],"domain_scores_gemma":[0.99965644,0.000035623318,0.00019240857,0.00002584496,0.00003924964,0.000050392486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015864741,0.00021147686,0.00020517956,0.0013298601,0.00041555162,0.0005458684,0.00021046042,0.00031029232,0.00077187706],"category_scores_gemma":[0.00034796758,0.00014793887,0.0001331215,0.000858067,0.0007992606,0.0003766318,0.0005757734,0.00016755189,0.00008924664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007937424,0.00004078746,0.96543336,0.000024999805,0.00003514808,0.00040472887,0.00047826263,0.0007295114,0.026209202,0.000113894115,0.000060095994,0.0063906093],"study_design_scores_gemma":[0.000002723347,0.000014859283,0.9986842,0.0000023059117,0.000004437175,0.000091186346,0.00013860568,0.00053899427,0.00039981815,0.000037158923,0.00008381475,0.0000019403376],"about_ca_topic_score_codex":0.0081552,"about_ca_topic_score_gemma":0.013193444,"teacher_disagreement_score":0.0081552,"about_ca_system_score_codex":0.00042297534,"about_ca_system_score_gemma":0.00019732965,"threshold_uncertainty_score":0.016215444},"labels":[],"label_agreement":null},{"id":"W4206167616","doi":"10.1002/essoar.10508772.1","title":"The evolving deformation field in central Afar from two decades of InSAR observations: Implications for the decoupling between the upper and lower crusts","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Deutsches Zentrum für Luft- und Raumfahrt; National Aeronautics and Space Administration; European Space Agency; California Institute of Technology; Canadian Space Agency; Jet Propulsion Laboratory","keywords":"Geology; Crust; Rift; Seismology; Subsidence; Dike; East African Rift; Volcano; Ridge; Echelon formation; Tectonics; Paleontology","score_opus":0.04968854618888107,"score_gpt":0.27773549498884426,"score_spread":0.22804694879996318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206167616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957145,0.0008540379,0.00037149916,0.00025515092,0.000031733263,0.0000059836993,0.0009701603,0.000033962064,0.0017630465],"genre_scores_gemma":[0.9980854,0.0002498839,0.00034274138,0.000058491816,0.000031296175,0.0000044871,0.0010981105,0.000008513679,0.00012113582],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970144,0.000028262211,0.000023291312,0.00011062117,0.000045174693,0.00009125869],"domain_scores_gemma":[0.99945253,0.0000824768,0.00015336112,0.00006477674,0.00016862935,0.00007828036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090410083,0.00046640192,0.00044269697,0.00189143,0.0007907253,0.0015968713,0.00038553766,0.0005728525,0.0007441307],"category_scores_gemma":[0.0012482854,0.00031187487,0.00044367692,0.0026036731,0.0004339766,0.00060861284,0.00056696753,0.00041884303,0.00022970287],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035073253,0.0000830225,0.94522625,0.00008089636,0.00024506918,0.0007408443,0.00059736107,0.0034942897,0.01448099,0.00039681053,0.0011585715,0.03314517],"study_design_scores_gemma":[0.000009248782,0.000013718595,0.9958335,0.000022614127,0.00003743475,0.00011489605,0.00020181932,0.002330956,0.0003904501,0.00008745267,0.0009475233,0.000010360199],"about_ca_topic_score_codex":0.04598416,"about_ca_topic_score_gemma":0.045685932,"teacher_disagreement_score":0.04598416,"about_ca_system_score_codex":0.0008873626,"about_ca_system_score_gemma":0.00061566546,"threshold_uncertainty_score":0.09143299},"labels":[],"label_agreement":null},{"id":"W4206377843","doi":"10.1029/2021gl095759","title":"Are Low‐Frequency Earthquake Moments Area‐ or Slip‐Limited? A Rock Record Examination","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Slip (aerodynamics); Seismology; Geology; Subduction; Moment magnitude scale; Fault plane; Fault (geology); Geometry; Tectonics; Physics; Mathematics","score_opus":0.06605891953492406,"score_gpt":0.28806635047954854,"score_spread":0.2220074309446245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206377843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977708,0.000055679124,0.00026780882,0.000015317046,7.4229024e-7,0.0000044616527,0.00062069076,0.000012089172,0.001252472],"genre_scores_gemma":[0.9993443,0.000031046548,0.00011498552,0.0000029248804,0.000003597887,0.0000028871182,0.00033915718,0.0000027330382,0.00015839079],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970907,0.000047563328,0.000048507998,0.00008756215,0.000064932115,0.000042320167],"domain_scores_gemma":[0.9943346,0.0015486188,0.0024805812,0.0007473114,0.00062095455,0.00026791397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051289133,0.00012341906,0.00028332014,0.0023907607,0.0003075759,0.00067693193,0.00038433843,0.00018460547,0.002489686],"category_scores_gemma":[0.0047178944,0.00014711425,0.0001467448,0.0018527869,0.00060965726,0.00070840784,0.00046801544,0.00012352006,0.00040081047],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070335926,0.00001020653,0.9895874,0.00002115528,0.0000390896,0.00007618738,0.00018489051,0.00033964598,0.0026485343,0.00021610202,0.00008110831,0.006725289],"study_design_scores_gemma":[9.858722e-7,0.000019359639,0.998792,0.000002505482,0.000007924543,0.00006928611,0.000113792994,0.0005057035,0.00021839244,0.00006616599,0.00020127163,0.000002639335],"about_ca_topic_score_codex":0.005754749,"about_ca_topic_score_gemma":0.0128536755,"teacher_disagreement_score":0.005754749,"about_ca_system_score_codex":0.0003274547,"about_ca_system_score_gemma":0.00018461233,"threshold_uncertainty_score":0.0114424825},"labels":[],"label_agreement":null},{"id":"W4206904139","doi":"10.1002/essoar.10510226.1","title":"Relocation of the 1982 Miramichi, New Brunswick, Canada, aftershock sequence","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Epicenter; Geology; Seismology; Relocation; Focal mechanism; Magnitude (astronomy); Fault (geology)","score_opus":0.02695401087505633,"score_gpt":0.21897702021836615,"score_spread":0.19202300934330982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206904139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95620275,0.0019298167,0.00057314074,0.000855848,0.00009569067,0.00031616574,0.007917055,0.00008752911,0.03202198],"genre_scores_gemma":[0.9369368,0.0026830006,0.0020553053,0.00038647844,0.00002107228,0.00014787869,0.01506488,0.000054815555,0.042649657],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995722,0.000012427322,0.000017101149,0.0000823844,0.00014006256,0.00017575588],"domain_scores_gemma":[0.99893206,0.000027595297,0.00012669177,0.000048054404,0.0006717896,0.00019377454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030761107,0.00045295616,0.00030771314,0.002000324,0.0035624076,0.0011552739,0.00087194704,0.0002885682,0.0040779267],"category_scores_gemma":[0.0013096394,0.0002663943,0.00013973864,0.003086179,0.00069518806,0.00035887773,0.0010101041,0.00066690694,0.00064956635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007777096,0.0001824302,0.7496453,0.0003760851,0.00008400233,0.002944103,0.0107524255,0.0020780456,0.019363381,0.0023645707,0.031986613,0.17944528],"study_design_scores_gemma":[0.000018144334,0.0000354367,0.95917195,0.00006315371,0.000012663307,0.00015265551,0.0034091105,0.00027901688,0.0012516134,0.000052544292,0.03553021,0.000023407936],"about_ca_topic_score_codex":0.9923268,"about_ca_topic_score_gemma":0.9987105,"teacher_disagreement_score":0.029896054,"about_ca_system_score_codex":0.029896054,"about_ca_system_score_gemma":0.037906665,"threshold_uncertainty_score":0.21691203},"labels":[],"label_agreement":null},{"id":"W42071534","doi":"","title":"Relocation of earthquakes in the Northeast Indian region using joint hypocentre determination method","year":2005,"lang":"en","type":"article","venue":"Current Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Humanities; Seismology; Geophysics; History; Philosophy","score_opus":0.06949188793607265,"score_gpt":0.3065369484126736,"score_spread":0.23704506047660096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W42071534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84881055,0.0013577716,0.1284301,0.00027921997,0.00022568725,0.00021501494,0.0063949665,0.0019035946,0.0123832],"genre_scores_gemma":[0.91454804,0.00039491043,0.0769221,0.000024260438,0.00006172721,0.00007902744,0.005734576,0.000088131725,0.002147219],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997962,0.000031326686,0.000016887849,0.000061891296,0.00005619162,0.00003755924],"domain_scores_gemma":[0.99949193,0.000037629576,0.00009989562,0.00005607512,0.00023493063,0.000079569254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042361996,0.00040713002,0.00031942036,0.003864417,0.00042660316,0.00052197324,0.00045317705,0.00022479885,0.0013457092],"category_scores_gemma":[0.0009634096,0.0001563126,0.00040100823,0.002918066,0.0001508784,0.00030917287,0.00073528517,0.00030238414,0.00075331907],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050668005,0.00017928651,0.4086061,0.00033797033,0.0002583477,0.0011966651,0.001173582,0.029623853,0.04027913,0.0022742825,0.020032562,0.49553162],"study_design_scores_gemma":[0.00009696055,0.00017481601,0.68776196,0.00006315845,0.00024901057,0.00075120386,0.0011126824,0.28058186,0.008193204,0.0013313965,0.019523738,0.00016012214],"about_ca_topic_score_codex":0.01931321,"about_ca_topic_score_gemma":0.037643347,"teacher_disagreement_score":0.01931321,"about_ca_system_score_codex":0.00025996103,"about_ca_system_score_gemma":0.00082608324,"threshold_uncertainty_score":0.038401604},"labels":[],"label_agreement":null},{"id":"W4210274574","doi":"10.1029/2021jb022822","title":"Evolution of Short‐Term Seismic Hazard in Alberta, Canada, From Induced and Natural Earthquakes: 2011–2020","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Alberta Energy","funders":"","keywords":"Induced seismicity; Seismic hazard; Seismology; Hazard; Natural hazard; Geology; Earthquake scenario; Term (time); Natural (archaeology); Baseline (sea)","score_opus":0.022628172416721788,"score_gpt":0.27387174531162145,"score_spread":0.2512435728948997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210274574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97153723,0.00035481233,0.001377172,0.00039573628,0.000018022396,0.000024184852,0.021989943,0.00014019743,0.004162667],"genre_scores_gemma":[0.9813115,0.00021516754,0.00070130156,0.00003235978,0.000004776428,0.000008366049,0.015541616,0.000009652534,0.0021752862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999759,0.000014310336,0.000010105847,0.000027365113,0.00013243817,0.000056735855],"domain_scores_gemma":[0.9990682,0.00006109394,0.0001055043,0.00002606406,0.00062134844,0.00011775098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004734712,0.00035787447,0.00014719198,0.0014000168,0.00045816047,0.0009118041,0.0006053636,0.00034071296,0.0013962574],"category_scores_gemma":[0.001420897,0.00017560956,0.0002933446,0.001760882,0.00030802164,0.0002358858,0.00045549433,0.00029588997,0.00025221246],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042170816,0.000077521145,0.7790923,0.00012005474,0.00023029908,0.00041312588,0.00037730942,0.17551461,0.0019293947,0.0017056118,0.00939973,0.030718291],"study_design_scores_gemma":[0.000016532535,0.000038092214,0.91721,0.00003755114,0.0000410535,0.000086053355,0.00072009856,0.07405192,0.000617764,0.00031902493,0.0068197497,0.000042091557],"about_ca_topic_score_codex":0.9714916,"about_ca_topic_score_gemma":0.98025745,"teacher_disagreement_score":0.028508425,"about_ca_system_score_codex":0.013363112,"about_ca_system_score_gemma":0.011416805,"threshold_uncertainty_score":0.09695661},"labels":[],"label_agreement":null},{"id":"W4210441798","doi":"10.4095/327999","title":"Integrated analyses of density, P-wave velocity, lithogeochemistry, and mineralogy to investigate effects of hydrothermal alteration and metamorphism on seismic reflectivity: a summary of results from the Lalor volcanogenic massive-sulfide deposit, Snow Lake, Manitoba","year":2022,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Mafic; Hydrothermal circulation; Volcanogenic massive sulfide ore deposit; Felsic; Geochemistry; Metamorphism; Metamorphic facies; Greenschist; Volcano; Petrology; Facies; Mineralogy; Geomorphology; Seismology; Structural basin","score_opus":0.05226330792330382,"score_gpt":0.2638873294458316,"score_spread":0.2116240215225278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210441798","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99786925,0.0001689767,0.0008595392,0.000009586291,7.1345977e-7,0.00001285673,0.00051622244,0.000022961189,0.0005399908],"genre_scores_gemma":[0.9952246,0.0001593174,0.0026702497,0.00001825518,0.0000024890612,0.000017282502,0.0012930117,0.0000137877505,0.00060086744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998667,0.000016142862,0.000010488324,0.000034357436,0.00004021613,0.000032155513],"domain_scores_gemma":[0.9997801,0.000026179525,0.00004479829,0.000017726,0.000099240075,0.000031953787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026191972,0.0006577135,0.00031350256,0.0012384687,0.00036838467,0.00058665103,0.00028952278,0.00015757744,0.0007939035],"category_scores_gemma":[0.00033562232,0.00025456262,0.00043292996,0.0014086451,0.00026214882,0.00019564353,0.0005446385,0.00017189725,0.00018326381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012201238,0.000039054223,0.89956534,0.00006389405,0.0003038283,0.00013618503,0.0004278074,0.00056659407,0.08127106,0.000024494879,0.000076065524,0.017403768],"study_design_scores_gemma":[0.000004534088,0.000048843063,0.9948775,0.0000055233254,0.00008508354,0.00005977943,0.00034349726,0.00077986857,0.003539319,0.000010994128,0.0002401761,0.0000049894047],"about_ca_topic_score_codex":0.16797255,"about_ca_topic_score_gemma":0.41909063,"teacher_disagreement_score":0.83202744,"about_ca_system_score_codex":0.0007358192,"about_ca_system_score_gemma":0.000808352,"threshold_uncertainty_score":0.33398974},"labels":[],"label_agreement":null},{"id":"W4210625102","doi":"10.1103/physreve.105.024901","title":"Sheared granular matter and the empirical relations of seismicity","year":2022,"lang":"en","type":"article","venue":"Physical review. E","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Induced seismicity; Tectonics; Instability; Quasistatic process; Hurst exponent","score_opus":0.03941774419389909,"score_gpt":0.2913446818071672,"score_spread":0.2519269376132681,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210625102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98260903,0.00025863174,0.014797879,0.00017177139,0.000011371616,0.000012694414,0.000105814484,0.00008459695,0.0019481863],"genre_scores_gemma":[0.9990601,0.0000529525,0.00076227327,0.0000049224996,0.0000038989115,0.0000040655555,0.000026065714,0.0000040698847,0.00008175752],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99979025,0.000061785366,0.000015228811,0.00005512594,0.0000503377,0.000027308872],"domain_scores_gemma":[0.99674356,0.0016408197,0.00096485636,0.0004165088,0.000104770486,0.00012951178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069823704,0.0002367402,0.0002308267,0.00086245,0.00019047651,0.00081461266,0.00039483994,0.00034473732,0.00091850024],"category_scores_gemma":[0.007662872,0.0002196231,0.0001441889,0.0005837459,0.0015146883,0.0009165154,0.00062111334,0.0004804852,0.00008730446],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00084829563,0.00028716924,0.100023136,0.00049669767,0.00023533954,0.001653966,0.0013555739,0.4866517,0.117557034,0.2569421,0.00068265584,0.033266358],"study_design_scores_gemma":[0.00003914923,0.000097538614,0.06721624,0.000022660386,0.000020650174,0.0002118243,0.00013800059,0.8322149,0.010127556,0.089347176,0.00050616823,0.000058173573],"about_ca_topic_score_codex":0.000839076,"about_ca_topic_score_gemma":0.00047913185,"teacher_disagreement_score":0.00091850024,"about_ca_system_score_codex":0.00043968493,"about_ca_system_score_gemma":0.00014189626,"threshold_uncertainty_score":0.0036926866},"labels":[],"label_agreement":null},{"id":"W4210667031","doi":"10.1029/2021gc010205","title":"Complex Structure in the Nootka Fault Zone Revealed by Double‐Difference Tomography and a New Earthquake Catalog","year":2022,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; Geological Survey of Canada; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Lithosphere; Subduction; Aftershock; Seismic tomography; Plate tectonics; Tectonics; Paleontology; Mantle (geology)","score_opus":0.017021820501579892,"score_gpt":0.20565135833326487,"score_spread":0.18862953783168498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210667031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963128,0.000038765847,0.0011978463,0.00001618248,0.0000019709237,0.000015165064,0.0013700253,0.000034299923,0.0010128326],"genre_scores_gemma":[0.9936872,0.00003955857,0.0028643701,0.0000041667477,0.0000020458588,0.000010308069,0.00292116,0.000007350529,0.00046391314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984956,0.000009577681,0.000014353937,0.00004266312,0.00004900942,0.000034853718],"domain_scores_gemma":[0.9993086,0.00006389989,0.00017149835,0.00008954762,0.00027161842,0.000094787276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016181405,0.0001689328,0.00016478082,0.0022663956,0.00032304975,0.0010037811,0.00024520367,0.00013907677,0.000696515],"category_scores_gemma":[0.0008426115,0.00014727341,0.000104162864,0.0026313786,0.00024169945,0.0002311983,0.0005160949,0.000121880665,0.00016175327],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009606773,0.00003270707,0.9459053,0.000031876123,0.00002847605,0.00022415222,0.00044953916,0.0039008975,0.011173525,0.00030215143,0.0007283785,0.037126873],"study_design_scores_gemma":[0.000004096478,0.000007908081,0.98930025,0.000005055489,0.000008493937,0.000076550044,0.00019456347,0.008864305,0.0005512647,0.000034384768,0.00094778545,0.000005274337],"about_ca_topic_score_codex":0.3554658,"about_ca_topic_score_gemma":0.5959925,"teacher_disagreement_score":0.3554658,"about_ca_system_score_codex":0.0009497874,"about_ca_system_score_gemma":0.001254533,"threshold_uncertainty_score":0.70679355},"labels":[],"label_agreement":null},{"id":"W4210947010","doi":"10.1038/s41598-022-06129-3","title":"InSAR data reveal that the largest hydraulic fracturing-induced earthquake in Canada, to date, is a slow-slip event","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria; University of Calgary","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Canada First Research Excellence Fund; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geology; Magnitude (astronomy); Slip (aerodynamics); Interferometric synthetic aperture radar; Seismometer; Moment magnitude scale; Episodic tremor and slip; Subduction; Foreshock; Tectonics; Scaling; Aftershock; Synthetic aperture radar","score_opus":0.03987938421192678,"score_gpt":0.23745447867185762,"score_spread":0.19757509445993085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210947010","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9205691,0.00087642105,0.0029960468,0.00037203927,0.000051135306,0.000053125063,0.036684446,0.00045345534,0.037944116],"genre_scores_gemma":[0.9753994,0.0008601832,0.002082671,0.000089127934,0.00001410413,0.00001295179,0.017959733,0.00002354571,0.0035584627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998511,0.0000030035558,0.000005570581,0.000016143009,0.0000869007,0.000037177975],"domain_scores_gemma":[0.9989197,0.000052911342,0.00020084232,0.000041079013,0.00068110815,0.00010429762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016085243,0.00040129127,0.00018005737,0.0010584837,0.00067793234,0.00057717867,0.00026814902,0.000121390156,0.0024682684],"category_scores_gemma":[0.0007152907,0.00011195757,0.000116070216,0.0021307059,0.0003102305,0.00019642971,0.00037165958,0.00026637095,0.00051559217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023780712,0.00009948108,0.824515,0.00028322477,0.00016825042,0.00044222097,0.00086508464,0.004552016,0.012989599,0.0016426907,0.021230176,0.1329745],"study_design_scores_gemma":[0.000007669251,0.000018562929,0.97712976,0.000025400937,0.00003427817,0.00006147347,0.0004614718,0.0018118027,0.0018200288,0.00021017139,0.018402768,0.000016583335],"about_ca_topic_score_codex":0.8846938,"about_ca_topic_score_gemma":0.95051205,"teacher_disagreement_score":0.1153062,"about_ca_system_score_codex":0.0029769866,"about_ca_system_score_gemma":0.0047476054,"threshold_uncertainty_score":0.23197049},"labels":[],"label_agreement":null},{"id":"W4211097969","doi":"10.3390/app12041809","title":"The Analysis of the Aftershock Sequences of the Recent Mainshocks in Alaska","year":2022,"lang":"en","type":"article","venue":"Applied Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Schulich School of Medicine and Dentistry; Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Markov chain Monte Carlo; Bayesian probability; Seismology; Induced seismicity; Geology; Sequence (biology); Posterior probability; Markov chain; Statistics; Mathematics","score_opus":0.018675936681195708,"score_gpt":0.2165791984762064,"score_spread":0.1979032617950107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4211097969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996612,0.000108597866,0.0022643227,0.000026440748,0.0000066921507,0.000007938013,0.00025542744,0.000022873504,0.00069570605],"genre_scores_gemma":[0.9981927,0.00011586802,0.0009369928,0.000004029342,0.000004379182,0.000005999462,0.0004486055,0.0000042857737,0.0002870908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988246,0.000022447553,0.000017180815,0.00002872376,0.000031192074,0.000017965822],"domain_scores_gemma":[0.99954695,0.00016470674,0.000116669544,0.000026097572,0.00009601406,0.000049516413],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005824887,0.0001899578,0.00023700533,0.0013967135,0.0002616841,0.00038925896,0.0002816211,0.00030948457,0.0006953392],"category_scores_gemma":[0.0014065519,0.00017371416,0.000451723,0.0012695743,0.00020170455,0.00031403173,0.00037352633,0.00031132143,0.00013043318],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028119248,0.00013571972,0.593846,0.00022103013,0.00025881574,0.0023534968,0.0016557218,0.34015986,0.014460964,0.0035665655,0.00047285712,0.042587683],"study_design_scores_gemma":[0.000011769533,0.0001168414,0.6876146,0.000059672082,0.00012563904,0.00033292017,0.0011956301,0.30363816,0.0030799292,0.0020904576,0.0016792013,0.00005512706],"about_ca_topic_score_codex":0.024467478,"about_ca_topic_score_gemma":0.021877237,"teacher_disagreement_score":0.024467478,"about_ca_system_score_codex":0.00033075383,"about_ca_system_score_gemma":0.0005048913,"threshold_uncertainty_score":0.048650086},"labels":[],"label_agreement":null},{"id":"W4211147960","doi":"10.1007/s00024-019-02266-5","title":"Introduction to “Twenty Five Years of Modern Tsunami Science Following the 1992 Nicaragua and Flores Island Tsunamis, Volume I”","year":2019,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Volume (thermodynamics); Seismology; Geography; Geology; Physics","score_opus":0.004195112927789072,"score_gpt":0.18557915434204814,"score_spread":0.18138404141425907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4211147960","genre_codex":"review","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0052279974,0.5435641,0.008998399,0.08339412,0.19878224,0.00015255479,0.004781977,0.00060235395,0.15449633],"genre_scores_gemma":[0.048707787,0.3642834,0.015252302,0.05335395,0.14289033,0.0005308203,0.0078426665,0.00097410276,0.3661646],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99972063,0.00007795809,0.000035769946,0.00006616968,0.00006276564,0.000036645666],"domain_scores_gemma":[0.9991654,0.00031741505,0.00007730904,0.00005732516,0.00029657665,0.00008592741],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068960927,0.0010300134,0.0004053726,0.0023374578,0.0012595917,0.002209631,0.0007723604,0.00088373397,0.019256616],"category_scores_gemma":[0.0021531477,0.00018866501,0.00033487985,0.002967062,0.0014757055,0.0019347499,0.0014799689,0.0016527938,0.004584386],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004909892,0.000014504991,0.0009259141,0.00081585255,0.00001080205,0.00012917854,0.0010684433,0.00025109688,0.00064580474,0.021105222,0.89776844,0.07721565],"study_design_scores_gemma":[9.107799e-7,0.000004723899,0.0009248391,0.00018311158,0.0000013894306,0.00005391815,0.00018497751,0.00001571772,0.000052185256,0.0010244399,0.99754983,0.000003963381],"about_ca_topic_score_codex":0.018755957,"about_ca_topic_score_gemma":0.04516588,"teacher_disagreement_score":0.019256616,"about_ca_system_score_codex":0.0020681168,"about_ca_system_score_gemma":0.0022269366,"threshold_uncertainty_score":0.064419806},"labels":[],"label_agreement":null},{"id":"W4212829447","doi":"10.1029/2021gc009959","title":"Borehole Seismic Observations From the Chicxulub Impact Drilling: Implications for Seismic Reflectivity and Impact Damage","year":2022,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Universidad Nacional Autónoma de México; National Science Foundation","keywords":"Geology; Borehole; Seismology; Scientific drilling; Lithology; Vertical seismic profile; Impact structure; Reflection (computer programming); Drilling; Fault (geology); Seismic tomography; Impact crater; Breccia; Geophysical imaging; Petrology; Geophysics; Geotechnical engineering","score_opus":0.03343392549281333,"score_gpt":0.2630957875115536,"score_spread":0.22966186201874028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212829447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99829966,0.000028286875,0.00017408592,0.000015448984,0.0000018051353,0.0000060104817,0.00030665798,0.000013018919,0.0011550299],"genre_scores_gemma":[0.99892384,0.000022524051,0.00039547513,0.000010676738,0.000001931123,0.00001030483,0.00042138278,0.0000030994165,0.00021073026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991393,0.000011871545,0.000005885265,0.000015642385,0.000031384443,0.000021380054],"domain_scores_gemma":[0.99983656,0.0000221559,0.000041469444,0.000012771471,0.000046860223,0.00004021534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017805709,0.00017528703,0.00016266086,0.0010300443,0.00044240424,0.0003169405,0.00023820352,0.0002854303,0.0006816069],"category_scores_gemma":[0.00038831387,0.00019143842,0.000083298735,0.0008212403,0.00022501845,0.00015316157,0.00045773594,0.00017096911,0.00012752404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002517259,0.00008199659,0.8956506,0.000057335128,0.000024003102,0.00059365184,0.0010202792,0.0013441703,0.08271178,0.00015274764,0.0006475886,0.017464159],"study_design_scores_gemma":[0.000005641106,0.000036610625,0.9966181,0.000008761731,0.000004559506,0.000074512725,0.00027616115,0.0013344497,0.0012866942,0.000010140027,0.00033956254,0.0000049096757],"about_ca_topic_score_codex":0.03484042,"about_ca_topic_score_gemma":0.08886791,"teacher_disagreement_score":0.03484042,"about_ca_system_score_codex":0.00036057664,"about_ca_system_score_gemma":0.00032698957,"threshold_uncertainty_score":0.0692752},"labels":[],"label_agreement":null},{"id":"W4212923419","doi":"10.1002/essoar.10506454.1","title":"The 2019-2020 Khalili (Iran) earthquake sequence - anthropogenic seismicity in the Zagros Simply Folded Belt?","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; British Columbia Knowledge Development Fund; European Commission; Natural Sciences and Engineering Research Council of Canada; Iran National Science Foundation; Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Aftershock; Hypocenter; Sequence (biology); Foreshock; Seismic hazard; Interferometric synthetic aperture radar; Synthetic aperture radar","score_opus":0.03975150109137419,"score_gpt":0.2655750053458025,"score_spread":0.2258235042544283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212923419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993911,0.000051001847,0.000058345064,0.000039326176,0.0000026420994,0.000002077987,0.00007246259,0.0000034213326,0.00037968266],"genre_scores_gemma":[0.99941874,0.000050356775,0.00010917084,0.000015123885,0.000007211697,0.0000015195499,0.00024363038,0.0000012372434,0.00015301074],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994314,0.0000042465017,0.000003515488,0.00001567329,0.000010206715,0.000023262954],"domain_scores_gemma":[0.9998635,0.0000074902186,0.000085838896,0.0000078110825,0.000015504133,0.000019866373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011478737,0.00012704085,0.00010155262,0.00036822035,0.00019789963,0.00036292017,0.00016931821,0.00022071366,0.00076294545],"category_scores_gemma":[0.00023328573,0.00007284829,0.000112014706,0.00048502308,0.00020431649,0.00026220258,0.00021415182,0.00013992637,0.00019853447],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008075047,0.00003679492,0.98566043,0.000018490924,0.000020418378,0.00033724547,0.000299437,0.0007630242,0.0029333667,0.00028732876,0.00027997186,0.00928271],"study_design_scores_gemma":[0.000002697286,0.000020228297,0.99835986,0.0000030390472,0.000006025537,0.0000793385,0.00027691384,0.00078649604,0.00010997761,0.00003876774,0.00031491736,0.0000017862487],"about_ca_topic_score_codex":0.014331721,"about_ca_topic_score_gemma":0.027725304,"teacher_disagreement_score":0.014331721,"about_ca_system_score_codex":0.00045758477,"about_ca_system_score_gemma":0.00030993842,"threshold_uncertainty_score":0.028496623},"labels":[],"label_agreement":null},{"id":"W4213010337","doi":"10.4095/329612","title":"A revised moment magnitude catalog of eastern Canada's largest earthquakes","year":2022,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Magnitude (astronomy); Moment magnitude scale; Richter magnitude scale; Seismology; Geology; Moment (physics); Maximum magnitude; Seismic moment; Scale (ratio); Earthquake magnitude; Seismic hazard; Geodesy; Geography; Cartography; Physics; Mathematics; Scaling; Fault (geology); Geometry","score_opus":0.030367234408571125,"score_gpt":0.23401777946506833,"score_spread":0.2036505450564972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213010337","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12036639,0.0029358065,0.0058370843,0.001148019,0.00036459396,0.0010776734,0.7305446,0.0022070024,0.13551888],"genre_scores_gemma":[0.25502232,0.0052279443,0.022846214,0.00027054935,0.00025753502,0.0004778678,0.6370542,0.00041584802,0.078427635],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9991984,0.00002400297,0.00009760052,0.00006117834,0.00046044763,0.00015836615],"domain_scores_gemma":[0.9809533,0.00041770955,0.0008274432,0.0006171469,0.016417192,0.0007672874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007253364,0.0006846801,0.00043004725,0.024957879,0.002047482,0.0016350556,0.0011390423,0.0002540539,0.014213891],"category_scores_gemma":[0.0039782603,0.00026730157,0.0003146113,0.019074166,0.0003599922,0.00074008974,0.0007863558,0.0004003524,0.0032991595],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029729737,0.00012616035,0.19404939,0.0012707243,0.00006300403,0.00086278404,0.0021588886,0.0028201018,0.0044163507,0.00595277,0.43693763,0.35104495],"study_design_scores_gemma":[0.000017623635,0.000036681347,0.57094604,0.00021814721,0.00004059903,0.0003700031,0.0010918382,0.00082432234,0.001184604,0.0003038082,0.4249126,0.000053718537],"about_ca_topic_score_codex":0.9512056,"about_ca_topic_score_gemma":0.9779579,"teacher_disagreement_score":0.04879439,"about_ca_system_score_codex":0.0097672,"about_ca_system_score_gemma":0.033285692,"threshold_uncertainty_score":0.098163426},"labels":[],"label_agreement":null},{"id":"W4213095114","doi":"10.1111/sed.12986","title":"Unravelling a 2300 year long sedimentary record of megathrust and intraslab earthquakes in proglacial Skilak Lake, south‐central Alaska","year":2022,"lang":"en","type":"article","venue":"Sedimentology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Fonds Wetenschappelijk Onderzoek; Austrian Science Fund","keywords":"Geology; Seismology; Subduction; Varve; Sedimentary rock; Turbidite; Landslide; Submarine landslide; Paleoseismology; Sediment; Paleontology; Fault (geology); Tectonics","score_opus":0.011053681646793908,"score_gpt":0.207844528160746,"score_spread":0.1967908465139521,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213095114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995278,0.00007045323,0.000036431982,0.0000056560434,9.4874366e-7,0.0000010973088,0.00013229359,0.0000034053542,0.00022190636],"genre_scores_gemma":[0.99949765,0.00004928168,0.000085623884,0.0000033141528,0.0000025327022,0.0000019637614,0.00021687744,0.0000013538129,0.00014148436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.0000053897897,0.000009934144,0.000016142338,0.00001682663,0.0000105823965],"domain_scores_gemma":[0.9996563,0.00002934438,0.00012178681,0.000027092154,0.00009449438,0.000070967806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016890929,0.00014711257,0.00016424057,0.0015098585,0.0004507092,0.00044230596,0.0001674861,0.0002024498,0.00049346476],"category_scores_gemma":[0.00037979422,0.00014672003,0.000106924665,0.0011166332,0.00028619627,0.00033553658,0.00057037716,0.00011796644,0.00015114032],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036203124,0.000011790617,0.98911256,0.000020838996,0.000030152272,0.0001743048,0.00090772327,0.00008958805,0.0054176124,0.00002083774,0.00006021027,0.004118239],"study_design_scores_gemma":[4.3971696e-7,0.000008298686,0.99924505,0.0000031382165,0.0000074620293,0.00003833481,0.00033771698,0.000079264246,0.00011501347,0.0000044187204,0.00015955238,0.0000013495627],"about_ca_topic_score_codex":0.02710879,"about_ca_topic_score_gemma":0.07654868,"teacher_disagreement_score":0.02710879,"about_ca_system_score_codex":0.00030000764,"about_ca_system_score_gemma":0.00029724513,"threshold_uncertainty_score":0.05390197},"labels":[],"label_agreement":null},{"id":"W4213251495","doi":"10.1029/2021gl095199","title":"The Effect of Correlated Permeability on Fluid‐Induced Seismicity","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"","keywords":"Induced seismicity; Geology; Permeability (electromagnetism); Seismology; Footprint; Seismic hazard; Basement; Scaling; Spatial variability; Porosity; Petrology; Geotechnical engineering; Geometry; Paleontology","score_opus":0.029396918995999808,"score_gpt":0.2841619573934513,"score_spread":0.25476503839745146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213251495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947508,0.000042851636,0.0044016084,0.000043175623,0.000004464885,0.000005125508,0.000090719084,0.000054864297,0.0006064391],"genre_scores_gemma":[0.9998977,0.0000054234106,0.000066632565,0.0000014483621,8.4127646e-7,6.0168054e-7,0.000011208144,0.0000022384286,0.000013919181],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99952936,0.00018885495,0.000028367242,0.00011918557,0.00006105508,0.000073248986],"domain_scores_gemma":[0.9869811,0.008493379,0.002537148,0.0010183493,0.0005463275,0.00042370876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001173304,0.00031153878,0.00028561676,0.0006322803,0.00023256995,0.0006255893,0.00046087953,0.0003401424,0.0011330794],"category_scores_gemma":[0.016361702,0.00027653942,0.00023292833,0.0004378429,0.0012666936,0.0009982669,0.00074414205,0.00047906977,0.00009131027],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010208798,0.0003105831,0.38903034,0.00010864017,0.00029193392,0.0013693508,0.00021009913,0.5403765,0.04806771,0.0044528027,0.00041347247,0.0143477535],"study_design_scores_gemma":[0.00003296077,0.0002460385,0.41665012,0.000015998132,0.00007430871,0.0004085541,0.00014207115,0.5630662,0.015756056,0.0032946062,0.00025193836,0.000061277475],"about_ca_topic_score_codex":0.0033292247,"about_ca_topic_score_gemma":0.001434275,"teacher_disagreement_score":0.0033292247,"about_ca_system_score_codex":0.0006144213,"about_ca_system_score_gemma":0.0003736004,"threshold_uncertainty_score":0.006619692},"labels":[],"label_agreement":null},{"id":"W4213425164","doi":"10.1139/cjes-2022-0015","title":"Reply to the discussion by van Staal et al. on “The northern Appalachian terrane wreck model”","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Saint Mary's University; Martec (Canada)","funders":"","keywords":"Geology; Terrane; Geochemistry; Geomorphology; Archaeology; Seismology; Tectonics; History","score_opus":0.026340557499726226,"score_gpt":0.22217545225373245,"score_spread":0.19583489475400623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213425164","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00017156122,0.0008072857,0.0001329484,0.98216426,0.016263472,0.0000033945319,0.00009123373,0.000015039353,0.00035089423],"genre_scores_gemma":[0.0026266286,0.00082130893,0.00019260024,0.9759567,0.018980678,0.000022462737,0.00004925065,0.00003441497,0.0013159992],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99682873,0.0009853969,0.0004110442,0.0006147873,0.00075054826,0.0004094608],"domain_scores_gemma":[0.9727763,0.017749097,0.0013696544,0.0008291267,0.0056105102,0.0016653922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010546383,0.0009076565,0.0013680467,0.0008895476,0.004168888,0.0046109227,0.00487098,0.030689813,0.01088549],"category_scores_gemma":[0.059336428,0.0007698166,0.0011377307,0.0013310303,0.006115157,0.0075325654,0.0040176115,0.038567837,0.00607436],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020282958,0.0000053813624,0.00023471506,0.000044849116,0.000011470827,0.00006605175,0.00027192908,0.00003743755,0.000027927288,0.00211224,0.9950033,0.0021643399],"study_design_scores_gemma":[0.00012409672,0.000025785354,0.001686997,0.00053706043,0.00006216419,0.00044129402,0.0025072484,0.00033973154,0.00036945555,0.018491065,0.9752847,0.00013044066],"about_ca_topic_score_codex":0.02093208,"about_ca_topic_score_gemma":0.026700849,"teacher_disagreement_score":0.030689813,"about_ca_system_score_codex":0.0031756037,"about_ca_system_score_gemma":0.0060846754,"threshold_uncertainty_score":0.055775285},"labels":[],"label_agreement":null},{"id":"W4213437435","doi":"10.5194/nhess-2022-59","title":"Time-dependent Probabilistic Tsunami Hazard Analysis for Western Sumatra, Indonesia, Using Space-Time Earthquake Rupture Modelling and Stochastic Source Scenarios","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Horizon 2020; University of Bristol; European Commission; Leverhulme Trust","keywords":"Seismology; Subduction; Geology; Hazard; Space time; Seismic hazard; Probabilistic logic; Statistics; Mathematics; Engineering; Tectonics","score_opus":0.029884512487849044,"score_gpt":0.23765332313474516,"score_spread":0.20776881064689612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213437435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97499746,0.0001355466,0.02231508,0.0001674307,0.000009423713,0.000029636647,0.0004592524,0.00008670912,0.001799418],"genre_scores_gemma":[0.9972108,0.000044601504,0.0023627938,0.000006704133,0.000003300593,0.000014184842,0.00015043851,0.000007632427,0.00019956379],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983156,0.00007751937,0.00001247601,0.00003353285,0.000029053992,0.00001573564],"domain_scores_gemma":[0.99908006,0.00049783563,0.0002166277,0.00007325929,0.00008000975,0.0000521686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006405297,0.00055925443,0.00038915878,0.00072865223,0.00019483933,0.00068889523,0.0007527285,0.0004518063,0.0007725441],"category_scores_gemma":[0.0018550113,0.00026582065,0.00076263066,0.0005943658,0.00030699465,0.000683879,0.0005396221,0.00048332752,0.000079504214],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003147955,0.000040845087,0.0098178005,0.000015552403,0.000051647854,0.000116977666,0.000019568759,0.98576236,0.00056775485,0.000932803,0.00008390505,0.002559201],"study_design_scores_gemma":[0.0000025865875,0.000009557145,0.0023862794,0.0000013857104,0.0000069628377,0.000015501642,0.000010442066,0.99707115,0.000098978446,0.00035215332,0.000041188607,0.0000036813271],"about_ca_topic_score_codex":0.017115638,"about_ca_topic_score_gemma":0.008925608,"teacher_disagreement_score":0.017115638,"about_ca_system_score_codex":0.0008990099,"about_ca_system_score_gemma":0.00068173546,"threshold_uncertainty_score":0.034032047},"labels":[],"label_agreement":null},{"id":"W4214893986","doi":"10.1093/gji/ggac096","title":"A reappraisal of active tectonics along the Fethiye<i>–</i>Burdur trend, southwestern Turkey","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation; British Columbia Knowledge Development Fund; University of Victoria","keywords":"Geology; Seismology; Subduction; Tectonics; Induced seismicity; Focal mechanism; Plate tectonics; Fault (geology); Strike-slip tectonics","score_opus":0.015510681083265044,"score_gpt":0.24323412894642604,"score_spread":0.227723447863161,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4214893986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99512625,0.0008878669,0.0003476549,0.00007731652,0.000025750962,0.0000075362846,0.000876086,0.000025382938,0.0026261008],"genre_scores_gemma":[0.99645895,0.00076870096,0.00089182606,0.000024102943,0.000012393946,0.0000046170308,0.0012515663,0.000008500057,0.0005793454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999074,0.0000071598038,0.0000139609,0.00003634717,0.000015203139,0.000019915353],"domain_scores_gemma":[0.99981207,0.000009189531,0.000060094728,0.000019862244,0.00008343995,0.000015451511],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018283425,0.00034961922,0.00022359453,0.0013777168,0.0002088811,0.00045732988,0.00019468836,0.00017730976,0.0009210917],"category_scores_gemma":[0.00022836185,0.000117860516,0.00018678505,0.0014529064,0.00016079216,0.00033379105,0.00032545073,0.00016147281,0.00020204445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024613316,0.000037297526,0.8300261,0.00032901677,0.00016009637,0.0018544808,0.0017577322,0.005811186,0.014970384,0.0006464637,0.002246712,0.14191444],"study_design_scores_gemma":[0.000004733434,0.00004035708,0.9917931,0.000063883504,0.00004065228,0.00026336033,0.00079537224,0.0011008572,0.0006203307,0.000041814437,0.0052268226,0.000008685384],"about_ca_topic_score_codex":0.02649593,"about_ca_topic_score_gemma":0.04355045,"teacher_disagreement_score":0.02649593,"about_ca_system_score_codex":0.00050283637,"about_ca_system_score_gemma":0.00041915276,"threshold_uncertainty_score":0.052683413},"labels":[],"label_agreement":null},{"id":"W4220664323","doi":"10.5194/egusphere-egu22-13502","title":"An unconsidered source of earthquakes and tsunamis from the Kanto region of Japan","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Subduction; Seismology; Trench; Plate tectonics; Interplate earthquake; Slow earthquake; Induced seismicity; Tectonics","score_opus":0.02968909843295002,"score_gpt":0.23099065539880195,"score_spread":0.20130155696585195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220664323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99713755,0.00085216627,0.000100482954,0.00018227851,0.000016024598,0.0000054642815,0.00019458948,0.0000065700006,0.0015048982],"genre_scores_gemma":[0.9978738,0.0008023812,0.0002149864,0.00008259812,0.000033607663,0.0000042774154,0.00039267103,0.0000040084537,0.00059171015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998801,0.000009927618,0.000024578798,0.000024067154,0.00003045282,0.000030981508],"domain_scores_gemma":[0.99959713,0.000028739232,0.00014248781,0.00003232527,0.00009862954,0.000100642275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020162358,0.00039489547,0.00019890869,0.0014301729,0.0010080116,0.00083479827,0.0002632742,0.00043658883,0.0009531294],"category_scores_gemma":[0.0004108211,0.0002643868,0.0001665897,0.0018180523,0.000437715,0.0005480648,0.0010638093,0.00023316898,0.0001968302],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012455606,0.000028718876,0.9536121,0.00018578525,0.00008049585,0.0062180106,0.0053915214,0.0002722049,0.011274712,0.0002266333,0.0010290417,0.021556204],"study_design_scores_gemma":[0.000003934443,0.000015515,0.9944522,0.000023520164,0.000038965885,0.00084650225,0.0024004697,0.00012091248,0.00022317225,0.000056220786,0.0018051887,0.000013344365],"about_ca_topic_score_codex":0.028824277,"about_ca_topic_score_gemma":0.0600444,"teacher_disagreement_score":0.028824277,"about_ca_system_score_codex":0.0004435428,"about_ca_system_score_gemma":0.0005618334,"threshold_uncertainty_score":0.057312965},"labels":[],"label_agreement":null},{"id":"W4220681004","doi":"10.5194/egusphere-egu22-127","title":"Exhumation of Eocene high-pressure metamorphic rock by coaxial flattening below a Miocene Cycladic-style detachment","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Metamorphic core complex; Geology; CYCLADES; Blueschist; Detachment fault; Zircon; Metamorphic rock; Tectonics; Flattening; Petrology; Seismology; Geochemistry; Extensional definition; Subduction; Eclogite","score_opus":0.01605151498419811,"score_gpt":0.22459044268086384,"score_spread":0.20853892769666574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220681004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9804443,0.00047661448,0.001156843,0.0001046452,0.000026302294,0.000021257123,0.00025083096,0.00010833686,0.017410846],"genre_scores_gemma":[0.99556524,0.00017972286,0.00053534505,0.000014260586,0.00001303257,0.000005429137,0.00017473461,0.000011163881,0.003501132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991965,0.0000047963367,0.000005644765,0.000043141226,0.000015673011,0.000011136363],"domain_scores_gemma":[0.9998851,0.0000063758253,0.000049056052,0.000025560666,0.000020339676,0.00001341929],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008218519,0.00029937507,0.00011632616,0.00064052694,0.00050164264,0.000879742,0.00036161972,0.00033462548,0.006207517],"category_scores_gemma":[0.0002836077,0.00020449112,0.00014687346,0.00044870426,0.0008037669,0.00051714183,0.00051587407,0.0003155599,0.00075422955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004663288,0.00008177805,0.5066726,0.00051006314,0.00015382718,0.0065585123,0.0039421334,0.0021225326,0.33202678,0.0081208665,0.0012257806,0.13811877],"study_design_scores_gemma":[0.00000897998,0.0001389149,0.95928437,0.00004145321,0.000028984025,0.0039937957,0.0008690395,0.0014418764,0.015754044,0.00056834106,0.017852698,0.000017487831],"about_ca_topic_score_codex":0.004979627,"about_ca_topic_score_gemma":0.013927164,"teacher_disagreement_score":0.006207517,"about_ca_system_score_codex":0.00056523987,"about_ca_system_score_gemma":0.0002679236,"threshold_uncertainty_score":0.020766258},"labels":[],"label_agreement":null},{"id":"W4220695315","doi":"10.5194/egusphere-egu22-10601","title":"Quantifying the effects of injection parameters on fault response under spatially homogenous and heterogenous pore-fluid conditions","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Induced seismicity; Slip (aerodynamics); Geothermal gradient; Geology; Perturbation (astronomy); Fluid pressure; Fault (geology); Seismology; Pore water pressure; Volume (thermodynamics); Mechanics; Geotechnical engineering; Thermodynamics; Physics; Geophysics","score_opus":0.035873429459050026,"score_gpt":0.2637252960831051,"score_spread":0.22785186662405504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220695315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945669,0.00012700775,0.0044554137,0.000051953102,0.00000813381,0.000008816067,0.00017731015,0.000080849684,0.0005235853],"genre_scores_gemma":[0.99940026,0.000039280058,0.00044614341,0.0000055411165,9.5192314e-7,0.0000040899035,0.000048113343,0.0000047974404,0.000050770155],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982786,0.000020987167,0.000024875766,0.00004582231,0.000032168067,0.000048163227],"domain_scores_gemma":[0.9989171,0.0005479787,0.00029934818,0.00009461163,0.00007933064,0.00006169957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002573593,0.0002925444,0.00032928202,0.00040568403,0.00018772349,0.00068498915,0.00037759653,0.0006616769,0.00081099145],"category_scores_gemma":[0.00200472,0.00014878598,0.0002799199,0.0003308901,0.00059137825,0.00081058656,0.00040724475,0.00040227213,0.0000905272],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049462274,0.00046639427,0.06434503,0.00024384767,0.00007963698,0.00069066696,0.00018865168,0.5209122,0.39725178,0.001876646,0.00032143752,0.013129038],"study_design_scores_gemma":[0.000028495586,0.00035290373,0.030589685,0.000017503127,0.0000466379,0.00010884136,0.00019663248,0.83044386,0.13706845,0.00068685366,0.00040654858,0.000053627704],"about_ca_topic_score_codex":0.002901288,"about_ca_topic_score_gemma":0.0019344451,"teacher_disagreement_score":0.002901288,"about_ca_system_score_codex":0.00045496426,"about_ca_system_score_gemma":0.0003021009,"threshold_uncertainty_score":0.0057688355},"labels":[],"label_agreement":null},{"id":"W4220710213","doi":"10.1029/2021jb022750","title":"Source Properties of Hydraulic‐Fracturing‐Induced Earthquakes in the Kiskatinaw Area, British Columbia, Canada","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Deutsche Forschungsgemeinschaft","keywords":"Seismology; Geology; Waveform; Hydraulic fracturing; Focal mechanism; Seismic moment; Slip (aerodynamics); Graben; Scaling; Geodesy; Induced seismicity; Geometry; Fault (geology); Geotechnical engineering; Physics; Voltage","score_opus":0.04288432064589042,"score_gpt":0.25769298465045554,"score_spread":0.2148086640045651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220710213","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891643,0.00024813405,0.0003683071,0.00007581942,0.000005326157,0.000033076205,0.0059377532,0.000051368224,0.0041158767],"genre_scores_gemma":[0.9939387,0.00020507316,0.00030606642,0.000020612537,0.0000019598358,0.000016398555,0.0033884882,0.000015436208,0.0021072985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979085,0.000007690502,0.000014065484,0.00004242959,0.00007535625,0.000069614354],"domain_scores_gemma":[0.9989968,0.00006990541,0.00008719629,0.000039594423,0.00068218523,0.00012439901],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017359694,0.0003826846,0.0002708748,0.0023382818,0.0016661746,0.0011817134,0.00084224984,0.0002993819,0.0026663279],"category_scores_gemma":[0.0011349963,0.00023125364,0.00021568808,0.004606473,0.00041953608,0.00027152637,0.00062998163,0.00028278554,0.00041165084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119298114,0.00004990831,0.9516721,0.00012211426,0.00014108648,0.0005897673,0.0015177731,0.0045377444,0.006631796,0.00026872352,0.0029351658,0.031414464],"study_design_scores_gemma":[0.0000076192455,0.00000508753,0.9948054,0.000022737106,0.000022888222,0.00006244002,0.0011604127,0.002030266,0.00038842406,0.000025065212,0.0014515934,0.000018105591],"about_ca_topic_score_codex":0.9934934,"about_ca_topic_score_gemma":0.9969531,"teacher_disagreement_score":0.0118232835,"about_ca_system_score_codex":0.0118232835,"about_ca_system_score_gemma":0.010217679,"threshold_uncertainty_score":0.085784316},"labels":[],"label_agreement":null},{"id":"W4220714224","doi":"10.5194/nhess-2022-59-rc3","title":"Comment on nhess-2022-59","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"University of Bristol; European Commission; Leverhulme Trust","keywords":"Seismology; Geology; Subduction; Hazard; Seismic hazard; Thrust; Physics; Tectonics","score_opus":0.04760129844526517,"score_gpt":0.27340151200383606,"score_spread":0.22580021355857088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220714224","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0023421342,0.0038358998,0.0012035016,0.38365498,0.27564025,0.0006781916,0.016953647,0.0022380997,0.31345326],"genre_scores_gemma":[0.007748936,0.0017580179,0.0008119413,0.59511006,0.037119463,0.0007753333,0.003064633,0.00036021636,0.35325146],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99836344,0.00013408462,0.00020956318,0.00022236242,0.0007758613,0.0002946374],"domain_scores_gemma":[0.99692255,0.00090816227,0.0002019075,0.00032018434,0.001303576,0.00034358056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002173338,0.0007576737,0.0009108303,0.00074155745,0.0015428711,0.0031789201,0.0022966801,0.021709073,0.074454196],"category_scores_gemma":[0.010969107,0.00037709848,0.0012739216,0.0011404934,0.0014207946,0.0018326106,0.0017296779,0.011473042,0.08274892],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006640621,0.000025621808,0.00037413053,0.000112370464,0.0000059240347,0.00028637587,0.00003208412,0.0000688712,0.0002469828,0.0025051944,0.9897557,0.0065203593],"study_design_scores_gemma":[0.000016949163,0.000012670569,0.0011378491,0.0001347314,0.0000037305124,0.000040840103,0.000041011168,0.000060877053,0.00012178517,0.00100553,0.99741167,0.000012363714],"about_ca_topic_score_codex":0.021628471,"about_ca_topic_score_gemma":0.020487247,"teacher_disagreement_score":0.074454196,"about_ca_system_score_codex":0.0030088024,"about_ca_system_score_gemma":0.004181241,"threshold_uncertainty_score":0.2490741},"labels":[],"label_agreement":null},{"id":"W4220793280","doi":"10.1007/s12517-022-09879-6","title":"The Genesis and Morphometry of the main Transversal Gorges in the Pera Magrun and Sara Anticlines, Iraqi Kurdistan Region, NE of the Arabian Plate","year":2022,"lang":"en","type":"article","venue":"Arabian Journal of Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"","keywords":"Anticline; Geology; Three gorges; Paleontology; Tectonics; Geologic map; Geomorphology; Geotechnical engineering","score_opus":0.013691204640034316,"score_gpt":0.20044591177401697,"score_spread":0.18675470713398265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220793280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992747,0.000045140467,0.000021570038,0.000011852896,0.0000012136635,0.0000016963704,0.0001813301,0.0000023359955,0.00046028607],"genre_scores_gemma":[0.9992118,0.00005017279,0.000113914015,0.0000042306433,0.0000015039232,0.0000029288942,0.00025106262,0.000002428291,0.00036187217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999304,0.0000143355755,0.000005557936,0.000022459295,0.000009569125,0.000017622033],"domain_scores_gemma":[0.99983394,0.000025362971,0.00006011731,0.000014772012,0.000041412142,0.000024490439],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012926102,0.00014773644,0.000088230954,0.0010693892,0.0003117417,0.0003818792,0.00020631464,0.00017001355,0.0010275498],"category_scores_gemma":[0.00033047269,0.00014940868,0.0001478362,0.0009897188,0.00040719972,0.00024038946,0.00035052595,0.00013281745,0.00025591053],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000099191966,0.000015390331,0.9836076,0.000020117312,0.000033970362,0.00017438158,0.0022573897,0.00037569,0.003547397,0.00025181114,0.00031035955,0.009306686],"study_design_scores_gemma":[7.128349e-7,0.0000055252003,0.9992304,0.0000015603073,0.0000022798713,0.0000430044,0.00039405856,0.000084598636,0.000037708374,0.000008928901,0.0001901858,9.840867e-7],"about_ca_topic_score_codex":0.023742458,"about_ca_topic_score_gemma":0.063394435,"teacher_disagreement_score":0.023742458,"about_ca_system_score_codex":0.0003454771,"about_ca_system_score_gemma":0.0002886868,"threshold_uncertainty_score":0.047208548},"labels":[],"label_agreement":null},{"id":"W4220808863","doi":"10.5194/egusphere-egu22-13588","title":"The global reach of the 2022 Tonga volcanic eruption","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Geology; Volcano; Climatology; Oceanography; Seismology","score_opus":0.018350952807760435,"score_gpt":0.2377069423227023,"score_spread":0.21935598951494187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220808863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8552638,0.0020668474,0.0048532863,0.0027120812,0.00021858778,0.00005817515,0.051514663,0.0006220885,0.08269039],"genre_scores_gemma":[0.9795843,0.00074437633,0.0014669833,0.000099287936,0.00001978021,0.000024433986,0.009711317,0.000044211374,0.008305353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996376,0.000004878276,0.0000016592924,0.000010252777,0.000009640664,0.000009745928],"domain_scores_gemma":[0.9998809,0.000009655341,0.000028232718,0.000012103698,0.00004382877,0.000025258822],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011936308,0.00025004463,0.00010543842,0.0003286817,0.0002826082,0.00068772305,0.00014072882,0.0001995949,0.005678051],"category_scores_gemma":[0.00048796364,0.00010253854,0.00022826475,0.001227512,0.00020889842,0.00038108585,0.0005347683,0.00029121008,0.00049107475],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015259067,0.000044273682,0.6876923,0.0006834766,0.00031116977,0.0011167238,0.0023359244,0.089425944,0.008079367,0.02326213,0.04733081,0.13956532],"study_design_scores_gemma":[0.000018745186,0.000038615006,0.8243394,0.000064278756,0.00009858083,0.00014872744,0.0007651749,0.022642324,0.0011425068,0.0027011638,0.14801097,0.000029504665],"about_ca_topic_score_codex":0.18844539,"about_ca_topic_score_gemma":0.20597701,"teacher_disagreement_score":0.18844539,"about_ca_system_score_codex":0.0014151421,"about_ca_system_score_gemma":0.0016449859,"threshold_uncertainty_score":0.37469703},"labels":[],"label_agreement":null},{"id":"W4220813342","doi":"10.5194/egusphere-egu22-1341","title":"A comparative analysis of approaches to expanding Canada&amp;#8217;s Earthquake Scenario Catalogue","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of British Columbia; McMaster University; University of Toronto; Geological Survey of Canada","funders":"","keywords":"Seismic hazard; Computer science; Seismology; Geography; Geology","score_opus":0.17575539297534287,"score_gpt":0.27552989582152143,"score_spread":0.09977450284617856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220813342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.58403486,0.0035913528,0.09035004,0.0038843302,0.00019454109,0.0040057255,0.07423094,0.0057046376,0.23400359],"genre_scores_gemma":[0.584967,0.0037477121,0.2754814,0.000748744,0.000055016106,0.0019642825,0.115241274,0.0015883219,0.016206276],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9908476,0.0024095902,0.00066201953,0.0007754902,0.0045703663,0.0007348659],"domain_scores_gemma":[0.9434859,0.02388687,0.0018976467,0.004973409,0.02359746,0.002158702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.012534901,0.001044359,0.0007758322,0.016354084,0.002274852,0.006264186,0.00400707,0.0011157745,0.00833246],"category_scores_gemma":[0.056164917,0.00071830594,0.0019234106,0.021799736,0.0012231772,0.0027554466,0.0037138879,0.0012168613,0.0010946206],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015531662,0.0006442845,0.14513762,0.0028373022,0.00082715496,0.0010051888,0.014466322,0.23648772,0.0045190486,0.08703558,0.052530173,0.45295647],"study_design_scores_gemma":[0.00026791348,0.00039392,0.26702407,0.0016223538,0.0008377524,0.00046009442,0.025507085,0.37414357,0.005802452,0.010610639,0.31263712,0.0006930054],"about_ca_topic_score_codex":0.87767786,"about_ca_topic_score_gemma":0.89488596,"teacher_disagreement_score":0.12232214,"about_ca_system_score_codex":0.031815704,"about_ca_system_score_gemma":0.028297367,"threshold_uncertainty_score":0.24608499},"labels":[],"label_agreement":null},{"id":"W4220824282","doi":"10.5194/egusphere-egu22-3267","title":"Olivine and enstatite formation during seismic faulting in serpentinite: an experimental approach","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Fault gouge; Geology; Compaction; Thermocouple; Mineralogy; Slip (aerodynamics); Geotechnical engineering; Enstatite; Materials science; Composite material; Thermodynamics; Seismology","score_opus":0.026379460088114162,"score_gpt":0.24751674899647114,"score_spread":0.221137288908357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220824282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979225,0.00020620282,0.00090096146,0.000011456231,0.0000056605036,0.00007232976,0.00022262271,0.000015764686,0.00064250734],"genre_scores_gemma":[0.9940323,0.00052616926,0.0033779272,0.000017760933,0.000012075975,0.00013221147,0.00043347207,0.0000143581465,0.001453687],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99983597,0.000011749545,0.000014391093,0.00006387937,0.000039626324,0.000034351793],"domain_scores_gemma":[0.99983644,0.000022920716,0.00004282709,0.000033031778,0.000037511956,0.00002727973],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001837907,0.00050364656,0.00024923444,0.00034732494,0.00042963686,0.00028058497,0.00033487284,0.0003766679,0.0017488861],"category_scores_gemma":[0.00014896072,0.0002275904,0.00025152232,0.0002530244,0.0004154734,0.00023402221,0.00035626604,0.0006045149,0.00022191793],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075504664,0.00010510552,0.0005186949,0.00003361438,0.0000029905364,0.000058085152,0.00007154318,0.000104075065,0.9984274,0.00003259357,0.000006718236,0.00056376075],"study_design_scores_gemma":[0.000042366668,0.0018526906,0.019438487,0.000011853137,0.000032869786,0.00015940034,0.00020872905,0.0017577377,0.9744368,0.000062077925,0.0019729594,0.00002392028],"about_ca_topic_score_codex":0.0011556161,"about_ca_topic_score_gemma":0.0019461772,"teacher_disagreement_score":0.0017488861,"about_ca_system_score_codex":0.00024136691,"about_ca_system_score_gemma":0.00019038918,"threshold_uncertainty_score":0.005850613},"labels":[],"label_agreement":null},{"id":"W4220827124","doi":"10.5194/egusphere-egu22-6819","title":"What are cratons?","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Craton; Lithosphere; Geology; Archean; Terrane; Crust; Mantle (geology); Tectonics; Geophysics; Paleontology","score_opus":0.036688297774106766,"score_gpt":0.2467535612212682,"score_spread":0.21006526344716145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220827124","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12935679,0.15927339,0.0040843785,0.13036904,0.0037065297,0.000116277784,0.0031604853,0.0004643657,0.5694688],"genre_scores_gemma":[0.7291405,0.09112785,0.0039184787,0.015860096,0.0017823086,0.000085024796,0.002141119,0.00024803673,0.15569657],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99936706,0.00009860844,0.000030000596,0.0001424042,0.00014337047,0.00021858551],"domain_scores_gemma":[0.99910873,0.00012145769,0.00012238976,0.000078745055,0.00022052543,0.00034806677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006338436,0.0004908658,0.00040383652,0.0021625976,0.003301451,0.0067657894,0.0008095491,0.0014856162,0.029388344],"category_scores_gemma":[0.0029611308,0.00032328514,0.00030660914,0.0034526687,0.0056058215,0.005355642,0.0019637835,0.0018889828,0.0053685997],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002483195,0.00003726006,0.044443753,0.001299162,0.000070774026,0.001371142,0.027215935,0.0001992605,0.0007650625,0.24302858,0.20669517,0.47462544],"study_design_scores_gemma":[0.0000071112677,0.00001611805,0.027856177,0.00083997915,0.000019559746,0.0009798373,0.017779179,0.00007625803,0.00016560176,0.015650716,0.9365849,0.000024566592],"about_ca_topic_score_codex":0.09396002,"about_ca_topic_score_gemma":0.1314958,"teacher_disagreement_score":0.09396002,"about_ca_system_score_codex":0.0032781668,"about_ca_system_score_gemma":0.0028072523,"threshold_uncertainty_score":0.18682623},"labels":[],"label_agreement":null},{"id":"W4220876610","doi":"10.5194/egusphere-egu22-3735","title":"Using numerical modelling to investigate the driving forces of permanent forearc deformation in northern Cascadia","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Forearc; Subduction; Geology; Seismology; Slip (aerodynamics); Episodic tremor and slip; Fault (geology); Tectonics; Physics","score_opus":0.05947713504889976,"score_gpt":0.25791578793468545,"score_spread":0.1984386528857857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220876610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9662063,0.00020854037,0.016063457,0.0006393091,0.000043748467,0.00004786699,0.00045118926,0.00037956313,0.015960049],"genre_scores_gemma":[0.9942433,0.00010331829,0.0037253357,0.000034752058,0.000006167896,0.00003987616,0.00015731368,0.0000387999,0.0016510541],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998221,0.000048692957,0.000012115758,0.000041909952,0.000042623604,0.00003255656],"domain_scores_gemma":[0.9994326,0.00027149724,0.000100219455,0.00005176094,0.000077442484,0.00006639585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037505545,0.00065996486,0.00050503085,0.00068250025,0.0008051022,0.001219032,0.001006032,0.0018321387,0.0023655456],"category_scores_gemma":[0.0018905677,0.0005383311,0.0007905987,0.00059742905,0.00089309114,0.00056703674,0.0007373225,0.0006192334,0.0003181985],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016285208,0.00001889784,0.0043997206,0.000018076335,0.000014506192,0.00007938174,0.000058013542,0.99283993,0.0011165354,0.00054621947,0.00007242541,0.0008200323],"study_design_scores_gemma":[0.000009227546,0.00000976727,0.0017061426,0.0000037668892,0.0000040293485,0.00000765778,0.000033399265,0.9976393,0.00011895033,0.0002666902,0.00019462928,0.000006444833],"about_ca_topic_score_codex":0.120355956,"about_ca_topic_score_gemma":0.07900966,"teacher_disagreement_score":0.120355956,"about_ca_system_score_codex":0.0025315422,"about_ca_system_score_gemma":0.0020975322,"threshold_uncertainty_score":0.2393108},"labels":[],"label_agreement":null},{"id":"W4220898876","doi":"10.5194/egusphere-egu22-12893","title":"To what extent do slip rates contribute to the seismic activity of faults?","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic moment; Seismology; Seismic hazard; Slip (aerodynamics); Geodetic datum; Geology; Geodesy; Fault (geology); Physics; Thermodynamics","score_opus":0.025316301226823677,"score_gpt":0.26170259781900695,"score_spread":0.23638629659218327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220898876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9716645,0.002714622,0.01415588,0.0010525737,0.000105985986,0.000029436917,0.0013960797,0.00014335144,0.008737514],"genre_scores_gemma":[0.997051,0.00071593764,0.0009307412,0.000062592604,0.00007820219,0.0000071418226,0.00043263388,0.000027816837,0.0006939112],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99957114,0.000070984366,0.000037048976,0.00016746689,0.00005996439,0.0000933777],"domain_scores_gemma":[0.99697137,0.0011100231,0.001120666,0.00020415903,0.00035734216,0.00023640395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009325129,0.00054907135,0.0005736415,0.0015376784,0.0002449992,0.001428022,0.0004278522,0.0006356785,0.003404018],"category_scores_gemma":[0.0070279366,0.00035802255,0.0004790725,0.001513282,0.00050592126,0.001516542,0.00045804493,0.0004051833,0.0013371921],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012456937,0.000037250582,0.9092232,0.00016891824,0.0002023857,0.00021501583,0.0004065345,0.009401174,0.0049459864,0.0018509629,0.0016600437,0.07176382],"study_design_scores_gemma":[0.000012132198,0.000059732836,0.9398193,0.0000690834,0.00015992977,0.00039202362,0.0009798254,0.048193384,0.0013425638,0.0049510677,0.0039748913,0.00004601731],"about_ca_topic_score_codex":0.0048591327,"about_ca_topic_score_gemma":0.0062766084,"teacher_disagreement_score":0.0048591327,"about_ca_system_score_codex":0.00038127517,"about_ca_system_score_gemma":0.00037411254,"threshold_uncertainty_score":0.011387587},"labels":[],"label_agreement":null},{"id":"W4220899728","doi":"10.5194/egusphere-egu22-12981","title":"Fault reactivation and halokinesis: an example from the Penobscot 3D seismic volume, offshore Nova Scotia, Canada","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto; McMaster University","funders":"","keywords":"Geology; Seismology; Tectonics; Submarine pipeline; Fault (geology); Population; Offset (computer science); Geodesy; Geotechnical engineering; Computer science","score_opus":0.036024880893848324,"score_gpt":0.21730049183584665,"score_spread":0.18127561094199834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220899728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9147631,0.003193342,0.00086311676,0.0013319982,0.00009159309,0.00014276346,0.021284156,0.00018315953,0.05814684],"genre_scores_gemma":[0.9841315,0.0011831328,0.0013040375,0.00012019894,0.00001202545,0.000014904951,0.0039521377,0.00003756375,0.009244363],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979156,0.0000058225255,0.000007490573,0.000028921795,0.00009880954,0.00006738546],"domain_scores_gemma":[0.9995409,0.000026122265,0.000047117534,0.000018812201,0.00027986732,0.000087192464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011918883,0.0004676634,0.00019499098,0.0022609239,0.0013666546,0.001148647,0.00043323176,0.000376542,0.002741913],"category_scores_gemma":[0.0005071135,0.00021150587,0.00020499107,0.0043547754,0.00066314125,0.0001587335,0.00070116663,0.00036880036,0.00043072377],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005580242,0.000091722286,0.82357705,0.0005240763,0.0001359843,0.009396659,0.008756766,0.0071288603,0.023743825,0.0019672872,0.029752826,0.09436696],"study_design_scores_gemma":[0.000010464736,0.000011701743,0.98309314,0.00007633064,0.000019917356,0.00033000778,0.003173879,0.0010883741,0.0004958855,0.00006689129,0.01160929,0.000024032981],"about_ca_topic_score_codex":0.99094266,"about_ca_topic_score_gemma":0.9977927,"teacher_disagreement_score":0.009057343,"about_ca_system_score_codex":0.008715849,"about_ca_system_score_gemma":0.012230446,"threshold_uncertainty_score":0.06323826},"labels":[],"label_agreement":null},{"id":"W4220930749","doi":"10.5194/nhess-2022-59-rc1","title":"Comment on nhess-2022-59","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"University of Bristol; European Commission; Leverhulme Trust","keywords":"Seismology; Geology; Subduction; Hazard; Seismic hazard; Thrust; Physics; Tectonics","score_opus":0.04760129844526517,"score_gpt":0.27340151200383606,"score_spread":0.22580021355857088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220930749","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0023421342,0.0038358998,0.0012035016,0.38365498,0.27564025,0.0006781916,0.016953647,0.0022380997,0.31345326],"genre_scores_gemma":[0.007748936,0.0017580179,0.0008119413,0.59511006,0.037119463,0.0007753333,0.003064633,0.00036021636,0.35325146],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99836344,0.00013408462,0.00020956318,0.00022236242,0.0007758613,0.0002946374],"domain_scores_gemma":[0.99692255,0.00090816227,0.0002019075,0.00032018434,0.001303576,0.00034358056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002173338,0.0007576737,0.0009108303,0.00074155745,0.0015428711,0.0031789201,0.0022966801,0.021709073,0.074454196],"category_scores_gemma":[0.010969107,0.00037709848,0.0012739216,0.0011404934,0.0014207946,0.0018326106,0.0017296779,0.011473042,0.08274892],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006640621,0.000025621808,0.00037413053,0.000112370464,0.0000059240347,0.00028637587,0.00003208412,0.0000688712,0.0002469828,0.0025051944,0.9897557,0.0065203593],"study_design_scores_gemma":[0.000016949163,0.000012670569,0.0011378491,0.0001347314,0.0000037305124,0.000040840103,0.000041011168,0.000060877053,0.00012178517,0.00100553,0.99741167,0.000012363714],"about_ca_topic_score_codex":0.021628471,"about_ca_topic_score_gemma":0.020487247,"teacher_disagreement_score":0.074454196,"about_ca_system_score_codex":0.0030088024,"about_ca_system_score_gemma":0.004181241,"threshold_uncertainty_score":0.2490741},"labels":[],"label_agreement":null},{"id":"W4220933785","doi":"10.1029/2021jb022480","title":"Magnitude‐Frequency Distributions and Slip‐History Predictions for Earthquakes Using Cellular Automata and Absorbing Markov Chains","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Alberta","funders":"","keywords":"Statistical physics; Slip (aerodynamics); Markov chain; Cellular automaton; Scaling; Markov chain Monte Carlo; Discretization; Markov process; Dissipation; Probability distribution; Series (stratigraphy); Mathematics; Monte Carlo method; Computer science; Physics; Statistics; Algorithm; Geology; Mathematical analysis; Geometry","score_opus":0.06157333613192281,"score_gpt":0.3058741097551804,"score_spread":0.2443007736232576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220933785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7021911,0.000115342475,0.29380456,0.0002767624,0.000023634382,0.000028573097,0.00019357647,0.00021680426,0.0031497097],"genre_scores_gemma":[0.9965383,0.000028973018,0.0030344245,0.0000072499306,0.0000054974653,0.000013612586,0.000043151806,0.000008098062,0.00032075788],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998715,0.000036720925,0.000008649216,0.000029522445,0.000029584085,0.000024013758],"domain_scores_gemma":[0.9973807,0.0019344436,0.00027949933,0.00010728144,0.00022131125,0.00007673978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000663544,0.00024434042,0.00026344723,0.0006776145,0.00031543057,0.0005935755,0.0005119021,0.00048485555,0.0010562948],"category_scores_gemma":[0.0048251813,0.00026410687,0.0003496822,0.00036642657,0.0006588425,0.0006678728,0.0002843498,0.00042045454,0.00011068008],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001389463,0.000012737559,0.002827589,0.000006252906,0.000006661455,0.000027066333,0.000030527943,0.983417,0.0005879098,0.011214507,0.000108591885,0.0017472648],"study_design_scores_gemma":[6.5828846e-7,0.0000015487783,0.0001841756,8.168956e-7,6.5880596e-7,0.0000020639359,0.0000021366618,0.99814117,0.00006064837,0.0015891829,0.000015701082,0.0000011834907],"about_ca_topic_score_codex":0.012399785,"about_ca_topic_score_gemma":0.008120756,"teacher_disagreement_score":0.012399785,"about_ca_system_score_codex":0.0009196251,"about_ca_system_score_gemma":0.00057788624,"threshold_uncertainty_score":0.024655223},"labels":[],"label_agreement":null},{"id":"W4220948824","doi":"10.5194/egusphere-egu22-7507","title":"Slip model of the 2013 April 16 Mw 7.7 Saravan intra-slab earthquake (Makran subduction zone) derived from InSAR, GPS, and Teleseismic P-wave modeling","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Subduction; Interferometric synthetic aperture radar; Geodesy; Slab; Slip (aerodynamics); Geodetic datum; Synthetic aperture radar; Tectonics; Geophysics; Remote sensing","score_opus":0.04591578991711508,"score_gpt":0.212732217335681,"score_spread":0.16681642741856595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220948824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97373235,0.00017911605,0.015325313,0.00020554665,0.00002005336,0.00002716979,0.0020581968,0.0002780823,0.008174039],"genre_scores_gemma":[0.99731356,0.000045209315,0.0011323394,0.000008454757,0.0000040661034,0.0000130036915,0.0006732055,0.000014717865,0.0007953186],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994767,0.000010005822,0.000005404711,0.000015215877,0.000009201442,0.000012537624],"domain_scores_gemma":[0.9998878,0.000031867996,0.00002844119,0.000009451352,0.000030620275,0.000011749908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014173967,0.00042834462,0.00024846947,0.0005310876,0.0002570584,0.00037143377,0.00066811376,0.00069006917,0.0019410168],"category_scores_gemma":[0.0004565108,0.0002290055,0.0003935632,0.00044836197,0.00023605837,0.00027797662,0.00025133076,0.00026293882,0.0003051784],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003018108,0.000016182323,0.0060500624,0.000015735128,0.000010249869,0.000087401255,0.000025062787,0.9901869,0.000871782,0.00047496156,0.00025531932,0.0019761748],"study_design_scores_gemma":[0.000005322408,0.000007154778,0.0026430883,0.00000196552,0.0000044401136,0.000009460298,0.0000069589096,0.9970409,0.00012194767,0.000062328145,0.00009228887,0.000004102688],"about_ca_topic_score_codex":0.044631347,"about_ca_topic_score_gemma":0.024103655,"teacher_disagreement_score":0.044631347,"about_ca_system_score_codex":0.00062514615,"about_ca_system_score_gemma":0.000485621,"threshold_uncertainty_score":0.08874315},"labels":[],"label_agreement":null},{"id":"W4220972324","doi":"10.1029/2022gl097984","title":"Supershear Rupture During the 2021 <i>M</i><sub>W</sub> 7.4 Maduo, China, Earthquake","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Aftershock; Earthquake rupture; Seismometer; Geodetic datum; Fault (geology); Geodesy","score_opus":0.01784879896368408,"score_gpt":0.24070417003934333,"score_spread":0.22285537107565925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220972324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997278,0.000013597156,0.000097874596,0.000010576588,0.0000010108321,0.0000011193416,0.000030611405,0.0000037819923,0.000113713686],"genre_scores_gemma":[0.9997545,0.000013218365,0.00006928068,0.0000033887275,0.0000025379234,0.0000012899798,0.00009363829,6.5542787e-7,0.000061450504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999398,0.0000058171777,0.0000036385786,0.00001489328,0.000013588876,0.000022205235],"domain_scores_gemma":[0.9998652,0.000012106324,0.000051043076,0.000014208107,0.000018328095,0.000039095463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012754324,0.00023302273,0.0002165738,0.00046769012,0.00032121508,0.00025184674,0.000242371,0.00020514865,0.00037809846],"category_scores_gemma":[0.00024882366,0.00018422425,0.00019240353,0.00031301007,0.00020245618,0.00024688497,0.0003638647,0.00013665832,0.00006198946],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031140415,0.000100723766,0.8882708,0.000078437755,0.00018581247,0.0012662981,0.0006095018,0.012437127,0.07053588,0.0003320499,0.00045380084,0.02541814],"study_design_scores_gemma":[0.00000783741,0.00005854951,0.984938,0.0000036921413,0.000046308614,0.00006821444,0.00019406686,0.012187532,0.0022153708,0.000044483622,0.00022698562,0.00000893606],"about_ca_topic_score_codex":0.012006139,"about_ca_topic_score_gemma":0.02419282,"teacher_disagreement_score":0.012006139,"about_ca_system_score_codex":0.0004101328,"about_ca_system_score_gemma":0.00027291334,"threshold_uncertainty_score":0.023872495},"labels":[],"label_agreement":null},{"id":"W4221032206","doi":"10.5194/nhess-2022-59-rc2","title":"Comment on nhess-2022-59","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"University of Bristol; European Commission; Leverhulme Trust","keywords":"Seismology; Geology; Subduction; Hazard; Seismic hazard; Thrust; Physics; Tectonics","score_opus":0.04760129844526517,"score_gpt":0.27340151200383606,"score_spread":0.22580021355857088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221032206","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0023421342,0.0038358998,0.0012035016,0.38365498,0.27564025,0.0006781916,0.016953647,0.0022380997,0.31345326],"genre_scores_gemma":[0.007748936,0.0017580179,0.0008119413,0.59511006,0.037119463,0.0007753333,0.003064633,0.00036021636,0.35325146],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99836344,0.00013408462,0.00020956318,0.00022236242,0.0007758613,0.0002946374],"domain_scores_gemma":[0.99692255,0.00090816227,0.0002019075,0.00032018434,0.001303576,0.00034358056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002173338,0.0007576737,0.0009108303,0.00074155745,0.0015428711,0.0031789201,0.0022966801,0.021709073,0.074454196],"category_scores_gemma":[0.010969107,0.00037709848,0.0012739216,0.0011404934,0.0014207946,0.0018326106,0.0017296779,0.011473042,0.08274892],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006640621,0.000025621808,0.00037413053,0.000112370464,0.0000059240347,0.00028637587,0.00003208412,0.0000688712,0.0002469828,0.0025051944,0.9897557,0.0065203593],"study_design_scores_gemma":[0.000016949163,0.000012670569,0.0011378491,0.0001347314,0.0000037305124,0.000040840103,0.000041011168,0.000060877053,0.00012178517,0.00100553,0.99741167,0.000012363714],"about_ca_topic_score_codex":0.021628471,"about_ca_topic_score_gemma":0.020487247,"teacher_disagreement_score":0.074454196,"about_ca_system_score_codex":0.0030088024,"about_ca_system_score_gemma":0.004181241,"threshold_uncertainty_score":0.2490741},"labels":[],"label_agreement":null},{"id":"W4221040421","doi":"10.31223/x56623","title":"Rapid tremor migration during few minute-long slow earthquakes in Cascadia","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council","keywords":"Seismology; Episodic tremor and slip; Geology; Slip (aerodynamics); Coherence (philosophical gambling strategy); Subduction; Geodesy; Tectonics; Physics","score_opus":0.024929480596685927,"score_gpt":0.22229501613441416,"score_spread":0.19736553553772823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221040421","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992211,0.00004244717,0.00008968318,0.000026336196,0.0000015018618,0.000001757838,0.00010699719,0.000015674974,0.00049442315],"genre_scores_gemma":[0.9996568,0.00003145163,0.00005570675,0.000004201845,0.0000018637735,0.0000017155646,0.00011233986,0.0000041313992,0.00013181342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999064,0.000009676642,0.000006908333,0.000030196352,0.000023284849,0.000023538976],"domain_scores_gemma":[0.99941254,0.00007980048,0.00020402152,0.000045886347,0.00010140873,0.0001564769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017474033,0.00019867327,0.00022271153,0.0011990936,0.00048022266,0.00044705562,0.00020703628,0.0003115094,0.0012578053],"category_scores_gemma":[0.0011409732,0.00019364843,0.00012336316,0.0011523174,0.00040303523,0.00024119347,0.0005308932,0.00023533116,0.0002397664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020480224,0.000050745653,0.9530833,0.00006268792,0.00006680232,0.0006524057,0.0018909498,0.002182119,0.032534026,0.00017738853,0.0005178535,0.008577074],"study_design_scores_gemma":[0.0000029316266,0.000016131393,0.9989182,0.0000025855632,0.000004918239,0.000048066522,0.00023365747,0.0004380152,0.00017430927,0.00002921469,0.00012851339,0.0000035247456],"about_ca_topic_score_codex":0.03192753,"about_ca_topic_score_gemma":0.05071225,"teacher_disagreement_score":0.9680725,"about_ca_system_score_codex":0.0004892915,"about_ca_system_score_gemma":0.0002766689,"threshold_uncertainty_score":0.06348336},"labels":[],"label_agreement":null},{"id":"W4221082814","doi":"10.3389/fmars.2022.796376","title":"SANTORY: SANTORini’s Seafloor Volcanic ObservatorY","year":2022,"lang":"en","type":"article","venue":"Frontiers in Marine Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Horizon 2020 Framework Programme; Hellenic Foundation for Research and Innovation","keywords":"Geology; Volcano; Submarine volcano; Seafloor spreading; Geochemistry; Lava; Hydrothermal circulation; Upwelling; Earth science; Hydrothermal vent; Oceanography; Seismology","score_opus":0.014364438348178946,"score_gpt":0.20904494848246521,"score_spread":0.19468051013428628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221082814","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.056578446,0.005208746,0.002176777,0.008121976,0.0044370014,0.00071583455,0.18132542,0.0036397257,0.737796],"genre_scores_gemma":[0.31470644,0.004414652,0.013314147,0.0024100733,0.0019158799,0.00038120645,0.13623863,0.0015969061,0.52502203],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9996891,0.000018875502,0.00001575,0.00010838365,0.000101805075,0.00006616185],"domain_scores_gemma":[0.99939907,0.0000318895,0.00007413909,0.00006426762,0.0002565363,0.00017411169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000450707,0.00088993035,0.0004284512,0.0012037731,0.0006363707,0.0020485958,0.00060059276,0.0007588685,0.10677847],"category_scores_gemma":[0.0007299612,0.00021913639,0.00018268301,0.000854872,0.00031278812,0.0009009839,0.0016996501,0.0008528616,0.045410153],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034478222,0.00011955729,0.06024727,0.0004898638,0.000045238135,0.00065094075,0.0004299314,0.00042211145,0.0064031957,0.002793936,0.7020601,0.2259931],"study_design_scores_gemma":[0.000061301034,0.000046896494,0.084904216,0.00020439483,0.000009733655,0.00013019911,0.00046122167,0.0009889193,0.00085800316,0.0005620181,0.9117563,0.000016835163],"about_ca_topic_score_codex":0.023982786,"about_ca_topic_score_gemma":0.026574956,"teacher_disagreement_score":0.10677847,"about_ca_system_score_codex":0.00090993516,"about_ca_system_score_gemma":0.0026410085,"threshold_uncertainty_score":0.35720956},"labels":[],"label_agreement":null},{"id":"W4221109011","doi":"10.1002/essoar.10510897.1","title":"Limited earthquake interaction during a geothermal hydraulic stimulation in Helsinki, Finland","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"German; World Wide Web; Electronic mail; Computer science; Geography; Archaeology","score_opus":0.026172436750597876,"score_gpt":0.2447634335810176,"score_spread":0.21859099683041971,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221109011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996611,0.0000067183055,0.00008301275,0.000003836798,7.9261116e-7,0.000002570623,0.000044754306,0.000003271263,0.00019389302],"genre_scores_gemma":[0.9998098,0.0000066909774,0.000037974158,0.0000018830644,0.0000017814575,0.0000027871083,0.00006905851,6.1185125e-7,0.00006946387],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998927,0.000013629664,0.0000073499814,0.000026374288,0.000028076596,0.000031713535],"domain_scores_gemma":[0.99973387,0.00006705522,0.00008605061,0.000016838167,0.00003801135,0.00005819062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014191927,0.00015926262,0.00018432792,0.0003686585,0.00020095166,0.00022557416,0.00021742145,0.00030724177,0.0007004347],"category_scores_gemma":[0.00045453446,0.00011144196,0.000115960356,0.00036595823,0.00028033202,0.00017698326,0.00035127383,0.00013146883,0.000088181325],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012200909,0.00046497554,0.8269264,0.00014807073,0.00018255092,0.0033164336,0.0019826705,0.013672257,0.13496073,0.00021514267,0.00041305422,0.01649756],"study_design_scores_gemma":[0.00001136564,0.0002755334,0.99013513,0.000005452274,0.0000252804,0.0001460497,0.0005268453,0.0048696822,0.0037426525,0.00003206017,0.00021903592,0.000010809936],"about_ca_topic_score_codex":0.0032269903,"about_ca_topic_score_gemma":0.008091641,"teacher_disagreement_score":0.0032269903,"about_ca_system_score_codex":0.00032484686,"about_ca_system_score_gemma":0.00026010186,"threshold_uncertainty_score":0.00641644},"labels":[],"label_agreement":null},{"id":"W4221118131","doi":"10.21203/rs.3.rs-1452299/v1","title":"Fault-based Probabilistic Seismic Hazard Analysis in Regions with Low Strain Rates and a Thick Seismogenic Layer: A Case Study from Malawi","year":2022,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Probabilistic logic; Fault (geology); Geology; Seismic hazard; Hazard; Layer (electronics); Strain (injury); Computer science; Materials science; Composite material; Artificial intelligence","score_opus":0.065037071991766,"score_gpt":0.3419593075581492,"score_spread":0.2769222355663832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221118131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99612194,0.00017275821,0.0020604494,0.00029658605,0.0000033910198,0.00004223343,0.0008097733,0.000023269084,0.000469524],"genre_scores_gemma":[0.997241,0.00015416855,0.0016781867,0.000026681859,0.000007811181,0.000015209434,0.0006190955,0.000007904545,0.00024988182],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99948007,0.00022297338,0.000039015198,0.00006070853,0.000061729625,0.0001356529],"domain_scores_gemma":[0.9973604,0.001378077,0.00050390395,0.00018404295,0.00037422165,0.00019934737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010377424,0.00042469794,0.00033498235,0.0021131067,0.0007065682,0.0011228385,0.00085320295,0.0006438307,0.0011886532],"category_scores_gemma":[0.0045883264,0.00027331096,0.0006035293,0.0025746564,0.00060715456,0.0006016177,0.0012025296,0.0006090893,0.00014749181],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020415398,0.00020052631,0.9287639,0.0002104189,0.00024249389,0.010043625,0.004004129,0.031039987,0.0015374029,0.0016286335,0.0012541743,0.020870477],"study_design_scores_gemma":[0.00004624681,0.00018083562,0.82600003,0.00020610893,0.00021926229,0.003380738,0.01616258,0.14622393,0.0016529405,0.0016328343,0.004212824,0.000081723825],"about_ca_topic_score_codex":0.13780323,"about_ca_topic_score_gemma":0.15878549,"teacher_disagreement_score":0.13780323,"about_ca_system_score_codex":0.001792836,"about_ca_system_score_gemma":0.0010637505,"threshold_uncertainty_score":0.27400225},"labels":[],"label_agreement":null},{"id":"W4221123003","doi":"10.5194/egusphere-egu22-407","title":"Strain localization along a detachment system: Deformation of natural dolomitic and calcitic mylonites (Mt. Hymittos, Attica, Greece)","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Ottawa","funders":"","keywords":"Mylonite; Greenschist; Geology; Cataclastic rock; Geochemistry; Blueschist; Metamorphic facies; Shear zone; Protolith; Metamorphism; Petrology; Seismology; Facies; Eclogite; Geomorphology; Fault (geology)","score_opus":0.016241906139945517,"score_gpt":0.23053047407678368,"score_spread":0.21428856793683815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221123003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951637,0.000011420162,0.000014808528,0.0000025298552,2.6411115e-7,0.0000015499687,0.000091591995,0.0000035401233,0.0003578999],"genre_scores_gemma":[0.9996766,0.000008537449,0.000039579558,0.000001633751,4.9905634e-7,0.0000018501988,0.00014453115,0.0000015226898,0.0001252066],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999101,0.000006517452,0.00000808708,0.000042182313,0.000013719088,0.00001930378],"domain_scores_gemma":[0.9999039,0.000007014296,0.000041036354,0.000011737888,0.00001548837,0.000020858222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000067273744,0.00021187223,0.0001335175,0.001154512,0.00027470756,0.0003432686,0.00028428962,0.00025898387,0.0012947125],"category_scores_gemma":[0.00017501012,0.00014384299,0.00012072099,0.0008412573,0.0004657371,0.0001527063,0.0004414879,0.00009117115,0.0003050539],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015716824,0.0000453038,0.94632006,0.000037841623,0.000041404743,0.000555335,0.0011457292,0.000752384,0.043035295,0.000099665645,0.00011591943,0.0076937503],"study_design_scores_gemma":[0.000001956379,0.000016472393,0.9992143,0.0000015640633,0.0000025052939,0.00008521208,0.00016018047,0.0001363559,0.00028639883,0.000006220812,0.00008743664,0.0000013223846],"about_ca_topic_score_codex":0.019230062,"about_ca_topic_score_gemma":0.030967012,"teacher_disagreement_score":0.019230062,"about_ca_system_score_codex":0.0005182373,"about_ca_system_score_gemma":0.00025780624,"threshold_uncertainty_score":0.03823626},"labels":[],"label_agreement":null},{"id":"W4221129693","doi":"10.5194/nhess-2022-59-cc1","title":"Comment on nhess-2022-59","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"University of Bristol; European Commission; Leverhulme Trust","keywords":"Seismology; Geology; Subduction; Hazard; Seismic hazard; Thrust; Physics; Tectonics","score_opus":0.04760129844526517,"score_gpt":0.27340151200383606,"score_spread":0.22580021355857088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221129693","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0023421342,0.0038358998,0.0012035016,0.38365498,0.27564025,0.0006781916,0.016953647,0.0022380997,0.31345326],"genre_scores_gemma":[0.007748936,0.0017580179,0.0008119413,0.59511006,0.037119463,0.0007753333,0.003064633,0.00036021636,0.35325146],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99836344,0.00013408462,0.00020956318,0.00022236242,0.0007758613,0.0002946374],"domain_scores_gemma":[0.99692255,0.00090816227,0.0002019075,0.00032018434,0.001303576,0.00034358056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002173338,0.0007576737,0.0009108303,0.00074155745,0.0015428711,0.0031789201,0.0022966801,0.021709073,0.074454196],"category_scores_gemma":[0.010969107,0.00037709848,0.0012739216,0.0011404934,0.0014207946,0.0018326106,0.0017296779,0.011473042,0.08274892],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006640621,0.000025621808,0.00037413053,0.000112370464,0.0000059240347,0.00028637587,0.00003208412,0.0000688712,0.0002469828,0.0025051944,0.9897557,0.0065203593],"study_design_scores_gemma":[0.000016949163,0.000012670569,0.0011378491,0.0001347314,0.0000037305124,0.000040840103,0.000041011168,0.000060877053,0.00012178517,0.00100553,0.99741167,0.000012363714],"about_ca_topic_score_codex":0.021628471,"about_ca_topic_score_gemma":0.020487247,"teacher_disagreement_score":0.074454196,"about_ca_system_score_codex":0.0030088024,"about_ca_system_score_gemma":0.004181241,"threshold_uncertainty_score":0.2490741},"labels":[],"label_agreement":null},{"id":"W4225003216","doi":"10.1029/2022jb024091","title":"Multistage Nucleation of the 2021 Yangbi M<sub>S</sub> 6.4 Earthquake, Yunnan, China and Its Foreshocks","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Natural Science Foundation of China","keywords":"Foreshock; Seismology; Geology; Nucleation; Slip (aerodynamics); Fault (geology); Aftershock; Physics","score_opus":0.02676441118395927,"score_gpt":0.27962201763087796,"score_spread":0.2528576064469187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225003216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99944407,0.0000441034,0.00021052275,0.0000051800125,0.0000019154554,0.0000075453167,0.00013196825,0.0000066470693,0.00014796708],"genre_scores_gemma":[0.9990964,0.000029640674,0.00021136912,0.0000021976039,0.0000033760489,0.0000068841446,0.00048840715,0.0000013908815,0.00016039604],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999014,0.0000061580013,0.0000071842337,0.000028620641,0.000026044956,0.00003050431],"domain_scores_gemma":[0.9996965,0.000022375012,0.00011648021,0.000023898123,0.000050521114,0.00009027852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020375154,0.00024024007,0.0002680276,0.001175528,0.00044833974,0.00033225247,0.00033324352,0.00019514648,0.0004899169],"category_scores_gemma":[0.0004364754,0.0001931929,0.00022463342,0.0008797357,0.00016143048,0.0002160248,0.0003889778,0.00012628887,0.000103821054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017406617,0.000042783697,0.9549454,0.000054540807,0.000057836012,0.0011111517,0.00040990583,0.0041610333,0.025553966,0.00020571967,0.0003619972,0.012921566],"study_design_scores_gemma":[0.0000034119257,0.000026172282,0.9948106,0.0000025146735,0.000010531313,0.00006302376,0.00009275234,0.0035507747,0.0011476205,0.000032729145,0.000254618,0.000005257951],"about_ca_topic_score_codex":0.018186772,"about_ca_topic_score_gemma":0.027947035,"teacher_disagreement_score":0.018186772,"about_ca_system_score_codex":0.000464728,"about_ca_system_score_gemma":0.0004385913,"threshold_uncertainty_score":0.03616184},"labels":[],"label_agreement":null},{"id":"W4225115513","doi":"10.1016/j.ocemod.2022.102009","title":"Data assimilation for the two-dimensional shallow water equations: Optimal initial conditions for tsunami modelling","year":2022,"lang":"en","type":"article","venue":"Ocean Modelling","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Data assimilation; Shallow water equations; Bathymetry; Buoy; Nonlinear system; Convergence (economics); Grid; Isotropy; Boundary value problem; Waves and shallow water; Finite volume method; Computer science; Geology; Geometry; Applied mathematics; Mathematics; Mathematical analysis; Meteorology; Mechanics; Physics","score_opus":0.14272031998301393,"score_gpt":0.30135232341717705,"score_spread":0.15863200343416312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225115513","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06928476,0.00020641382,0.9280646,0.00044323428,0.00004385371,0.000051802363,0.00017793509,0.00010285382,0.0016245724],"genre_scores_gemma":[0.7107571,0.00019530901,0.28720972,0.00007935178,0.00003140899,0.00018332752,0.0003475894,0.00008606395,0.001110157],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984324,0.00006219539,0.000011788757,0.00002450805,0.000041624324,0.000016662969],"domain_scores_gemma":[0.9994615,0.0002950484,0.00006617303,0.000051558272,0.0000927327,0.00003311267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007972919,0.00041398293,0.0005053453,0.0002372606,0.00035319067,0.0005752216,0.0005508426,0.00085633906,0.0006836672],"category_scores_gemma":[0.0037868386,0.00040742164,0.00042311227,0.00024703966,0.000719269,0.0008884438,0.0009840436,0.0012263638,0.00011698805],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027753904,0.000018172768,0.0008871371,0.000026554937,0.000014057727,0.000022777242,0.00003368506,0.9798059,0.0031774994,0.011589136,0.00016966634,0.0042276653],"study_design_scores_gemma":[0.00000335016,0.0000027052681,0.000068855414,0.0000020058762,5.7871745e-7,0.0000011421076,0.0000024964488,0.9982765,0.0003165836,0.0012266642,0.0000968192,0.0000024305734],"about_ca_topic_score_codex":0.012485089,"about_ca_topic_score_gemma":0.009170628,"teacher_disagreement_score":0.012485089,"about_ca_system_score_codex":0.0006278145,"about_ca_system_score_gemma":0.0009623395,"threshold_uncertainty_score":0.024824858},"labels":[],"label_agreement":null},{"id":"W4225147078","doi":"10.3390/app12094504","title":"Editorial of the Special Issue “Statistics and Pattern Recognition Applied to the Spatio-Temporal Properties of Seismicity”","year":2022,"lang":"en","type":"article","venue":"Applied Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Induced seismicity; Geology; Seismology","score_opus":0.021491907486614066,"score_gpt":0.20248138238873947,"score_spread":0.1809894749021254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225147078","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000048202495,0.0025321734,0.00033058226,0.019191345,0.97720873,0.000014441124,0.000109579705,0.0000791471,0.00048579727],"genre_scores_gemma":[0.00020899388,0.0012818412,0.00010350447,0.006765218,0.9900496,0.0000118012695,0.000050746534,0.000031012572,0.0014972734],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9939452,0.0009180157,0.0009463414,0.0012205904,0.0025889147,0.0003808918],"domain_scores_gemma":[0.96149135,0.015129973,0.0025296633,0.0012274226,0.015563373,0.0040582702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.007055232,0.0044166795,0.0057200817,0.004887376,0.002634301,0.008347173,0.004319074,0.0102886995,0.014084165],"category_scores_gemma":[0.029654466,0.0015079898,0.004488706,0.0021693902,0.002461413,0.0044285,0.0015205344,0.014968823,0.0117494445],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007463361,0.000021368269,0.00006682958,0.00021624824,0.0000419102,0.00008307326,0.000007392427,0.00005675119,0.00011915355,0.00018111104,0.994678,0.004453515],"study_design_scores_gemma":[0.00011618789,0.000089425674,0.0013632778,0.00042587848,0.00014547801,0.00041616402,0.000031550677,0.0008825725,0.0003404277,0.0014444526,0.99469924,0.000045255758],"about_ca_topic_score_codex":0.0016087889,"about_ca_topic_score_gemma":0.0035675142,"teacher_disagreement_score":0.014084165,"about_ca_system_score_codex":0.0022122967,"about_ca_system_score_gemma":0.0024250722,"threshold_uncertainty_score":0.04711622},"labels":[],"label_agreement":null},{"id":"W4225424851","doi":"10.3389/feart.2022.894549","title":"Spatiotemporal Clustering of Seismicity in the Kiskatinaw Seismic Monitoring and Mitigation Area","year":2022,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium; Canadian Natural Resources Limited","keywords":"Induced seismicity; Aftershock; Geology; Seismology; Hydraulic fracturing; Cluster analysis; Fault (geology); Microseism; Geotechnical engineering","score_opus":0.01442265819806856,"score_gpt":0.2125562227061826,"score_spread":0.19813356450811404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225424851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99796236,0.00008190159,0.00019558595,0.000024939753,0.0000018561162,0.000015744912,0.00095596,0.000015876638,0.0007456471],"genre_scores_gemma":[0.9972682,0.0001106738,0.0002621127,0.000008554993,0.0000022345678,0.000017690236,0.0017915952,0.000005380881,0.0005335106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997423,0.000016332751,0.000022913073,0.00007603157,0.00005636581,0.00008610437],"domain_scores_gemma":[0.99909556,0.00007233893,0.00032199745,0.00006223683,0.00026210156,0.00018571009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001934615,0.00021275727,0.00033827228,0.0032511558,0.0005899604,0.0005986642,0.0003781776,0.00021678307,0.0007264668],"category_scores_gemma":[0.001016614,0.00016111492,0.0001570126,0.004333199,0.00046321496,0.00022842456,0.0008006293,0.00019912541,0.00016763405],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013155502,0.000038158065,0.9702463,0.00006810596,0.000067852605,0.0003108079,0.002470538,0.0012317058,0.007497789,0.0002421655,0.0008830641,0.016811892],"study_design_scores_gemma":[0.0000014877843,0.000007291979,0.9983038,0.000007061235,0.0000065058157,0.000039227118,0.00065585674,0.0004327689,0.0001140777,0.000012919075,0.00041412166,0.0000048514034],"about_ca_topic_score_codex":0.67525125,"about_ca_topic_score_gemma":0.8109116,"teacher_disagreement_score":0.32474875,"about_ca_system_score_codex":0.002382602,"about_ca_system_score_gemma":0.0026435468,"threshold_uncertainty_score":0.6533225},"labels":[],"label_agreement":null},{"id":"W4225625002","doi":"10.1029/2021jb022878","title":"Time‐Lapse Record of an Earthquake in the Dry Felsic Lower Continental Crust Preserved in a Pseudotachylyte‐Bearing Fault","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Continental crust; Felsic; Quartz; Granulite; Ilmenite; Mylonite; Shear zone; Feldspar; Crust; Slip (aerodynamics); Petrology; Geochemistry; Mineralogy; Seismology; Mafic; Tectonics; Geomorphology","score_opus":0.03980202957972251,"score_gpt":0.30695919499104257,"score_spread":0.26715716541132006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225625002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999132,0.000040515326,0.00008880692,0.0000047702515,9.686253e-7,0.0000027391054,0.00029841822,0.000007180869,0.00042472436],"genre_scores_gemma":[0.99901617,0.000027344493,0.00013571813,0.0000037392726,0.000003691767,0.0000029718717,0.00059568527,0.0000025860559,0.0002121401],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997234,0.0000019517004,0.0000020250352,0.000009131523,0.0000062209497,0.000008390976],"domain_scores_gemma":[0.99985766,0.000012325433,0.000049220598,0.000013484,0.000031428626,0.000035830988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008730721,0.00010969933,0.0001354518,0.0009529885,0.00029762796,0.00023354634,0.00016918975,0.00021365703,0.0008899639],"category_scores_gemma":[0.00018797729,0.000100899335,0.00009748273,0.0005681382,0.00020677963,0.000117659525,0.00029850466,0.00013807636,0.0002490888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035882587,0.000088399465,0.7335539,0.00006317613,0.00009557277,0.0009303118,0.0010146876,0.00051077077,0.24909,0.00015257737,0.00030337198,0.0138384085],"study_design_scores_gemma":[0.0000012966885,0.000028410215,0.99856645,0.0000015023298,0.0000059003714,0.00009742891,0.00004395064,0.00015711,0.00084409094,0.0000056827853,0.00024674338,0.0000014641747],"about_ca_topic_score_codex":0.00522688,"about_ca_topic_score_gemma":0.013176104,"teacher_disagreement_score":0.00522688,"about_ca_system_score_codex":0.00021932117,"about_ca_system_score_gemma":0.000063488886,"threshold_uncertainty_score":0.010392904},"labels":[],"label_agreement":null},{"id":"W4225686858","doi":"10.1029/2021jb023519","title":"Community‐Driven Code Comparisons for Three‐Dimensional Dynamic Modeling of Sequences of Earthquakes and Aseismic Slip","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"High Performance Research Computing, Texas A and M University; Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; European Commission; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Japan Society for the Promotion of Science; Southern California Earthquake Center; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Slip (aerodynamics); Observable; Finite element method; Geology; Earthquake rupture; Seismology; Computer science; Mechanics; Physics; Fault (geology); Structural engineering; Engineering","score_opus":0.09982133201517948,"score_gpt":0.3492980179679504,"score_spread":0.24947668595277092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225686858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9689322,0.00019542637,0.015157536,0.000266072,0.00013793856,0.0002109978,0.0022054578,0.0027956893,0.010098685],"genre_scores_gemma":[0.96527404,0.00009504537,0.026932273,0.0001096399,0.000017942262,0.00034942152,0.0053847535,0.0008053102,0.001031473],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986773,0.00041073453,0.00013810386,0.00018519437,0.0004225301,0.00016609931],"domain_scores_gemma":[0.99371225,0.002217,0.00028117592,0.0010311215,0.0023224663,0.00043588315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0037157536,0.0008071701,0.00051940215,0.0011822837,0.0007271535,0.0008730819,0.002319526,0.0013400913,0.0021854318],"category_scores_gemma":[0.008869159,0.00035062808,0.0008693695,0.0010116416,0.0006479112,0.0011627149,0.001696446,0.001144831,0.00055481424],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010756939,0.0022240367,0.038704667,0.00036588783,0.00024436085,0.00027496877,0.00046314218,0.8804521,0.013501048,0.008198282,0.008865791,0.045630027],"study_design_scores_gemma":[0.00019247516,0.0003794471,0.005020565,0.000028186243,0.000020390074,0.000031131025,0.00014561745,0.9849834,0.0058000176,0.0011291003,0.0022332268,0.00003640961],"about_ca_topic_score_codex":0.011472295,"about_ca_topic_score_gemma":0.012297137,"teacher_disagreement_score":0.011472295,"about_ca_system_score_codex":0.0009340401,"about_ca_system_score_gemma":0.0016303741,"threshold_uncertainty_score":0.022810996},"labels":[],"label_agreement":null},{"id":"W4225871861","doi":"10.1093/gji/ggac159","title":"Structural controls on coseismic rupture revealed by the 2020<i>M</i>w 6.0 Jiashi earthquake (Kepingtag belt, SW Tian Shan, China)","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; China Scholarship Council; Canada Research Chairs; Sight Research UK; Royal Society; Canada Foundation for Innovation; Natural Environment Research Council; University of Victoria; Cummings Foundation","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Décollement; Aftershock; Anticline; Thrust fault; Slip (aerodynamics); Subduction; Fault (geology); Geodesy; Synthetic aperture radar; Tectonics","score_opus":0.0085902306458558,"score_gpt":0.2190793441373378,"score_spread":0.210489113491482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225871861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993844,0.000020941758,0.000022087876,0.000018054801,0.0000019858624,0.0000015016432,0.00014371163,0.000004396284,0.00040274434],"genre_scores_gemma":[0.99963355,0.000017688904,0.000012673038,0.0000063329276,0.0000030338233,0.0000017698092,0.00023705713,0.0000014069998,0.00008653416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998547,0.000010731757,0.000011871634,0.00004750706,0.000026237942,0.00004887487],"domain_scores_gemma":[0.9996742,0.000016295993,0.00011873098,0.000030299434,0.00005965479,0.000100771824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001879755,0.00032700517,0.00024795902,0.00094010244,0.00038948518,0.00059538294,0.00029087628,0.0003437367,0.0011571904],"category_scores_gemma":[0.00044836925,0.00021449041,0.00020931193,0.0009275763,0.0004654832,0.0002472218,0.0005897695,0.0002198863,0.00028428205],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024286877,0.00005688457,0.96162665,0.000027755044,0.000050766932,0.00037378125,0.00054431346,0.00132279,0.029337995,0.00019184433,0.00038474303,0.0058396533],"study_design_scores_gemma":[0.0000019473612,0.000012208219,0.99927086,0.000001268986,0.0000041447893,0.000014490292,0.00009604358,0.00037980307,0.00012110644,0.000010876258,0.00008481509,0.0000024640203],"about_ca_topic_score_codex":0.030025866,"about_ca_topic_score_gemma":0.044622134,"teacher_disagreement_score":0.030025866,"about_ca_system_score_codex":0.00075772277,"about_ca_system_score_gemma":0.00041346153,"threshold_uncertainty_score":0.059702218},"labels":[],"label_agreement":null},{"id":"W4226028241","doi":"10.1093/gji/ggac165","title":"Aftershock distributions, moment tensors and stress evolution of the 2016 Iniskin and 2018 Anchorage <i>M</i>w 7.1 Alaskan intraslab earthquakes","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of British Columbia","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Geology; Seismology; Fault (geology); Interplate earthquake; Seismic moment; Slow earthquake; Pore water pressure; Focal mechanism; Slab; Seismic gap; Foreshock; Geophysics; Geotechnical engineering","score_opus":0.006057430347668259,"score_gpt":0.1947021791850102,"score_spread":0.18864474883734195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226028241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992538,0.0000274098,0.00006371688,0.000006544568,0.000002430087,0.0000013842125,0.00021406436,0.00001011248,0.00042053682],"genre_scores_gemma":[0.99876213,0.000060831426,0.000101131496,0.0000032538783,0.0000044445396,0.000002826005,0.0006261377,0.000003741928,0.00043568542],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999515,0.0000025024458,0.000006810376,0.00001376705,0.000013731503,0.000011768329],"domain_scores_gemma":[0.9998035,0.000010008807,0.000084774954,0.000014925031,0.0000523269,0.000034555374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000102802005,0.00015764702,0.00018678345,0.0007967899,0.00022931838,0.00033145145,0.00008941616,0.0001496562,0.00076942786],"category_scores_gemma":[0.00026348062,0.00007451095,0.00014392434,0.0005857295,0.00014296142,0.00017956701,0.00032916557,0.00013417914,0.00020269936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017511549,0.000047024387,0.94419914,0.000038328064,0.00006624619,0.0004998698,0.0008607998,0.00255241,0.029024744,0.00010908388,0.00036513756,0.022062067],"study_design_scores_gemma":[0.0000011105604,0.000025445348,0.99785185,0.000003369484,0.0000105237095,0.00004604048,0.00022632674,0.0004655421,0.0009546334,0.00002482111,0.00038520264,0.0000051397024],"about_ca_topic_score_codex":0.0068134824,"about_ca_topic_score_gemma":0.012382799,"teacher_disagreement_score":0.0068134824,"about_ca_system_score_codex":0.00023363164,"about_ca_system_score_gemma":0.00014570536,"threshold_uncertainty_score":0.013547659},"labels":[],"label_agreement":null},{"id":"W4226030992","doi":"10.1007/s11600-022-00770-2","title":"The aftershock sequence at a deep nickel mine: temporal and spatial distribution, magnitude distribution, and aftershock decay following major events","year":2022,"lang":"en","type":"article","venue":"Acta Geophysica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Vale (Canada)","funders":"National Institute for Occupational Safety and Health; National Key Scientific Instrument and Equipment Development Projects of China","keywords":"Aftershock; Magnitude (astronomy); Structural geology; Geology; Seismology; Sequence (biology); Distribution (mathematics); Mathematics; Physics","score_opus":0.00853673376484704,"score_gpt":0.20781992554232118,"score_spread":0.19928319177747414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226030992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993567,0.000040823503,0.00005367612,0.000015501417,0.0000017221448,0.0000036048696,0.00019946675,0.0000033417998,0.00032523554],"genre_scores_gemma":[0.9992471,0.00004230238,0.00003271694,0.000007666151,0.0000055812393,0.0000027901553,0.00039230706,0.0000015866411,0.0002680169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999207,0.000012137876,0.0000117404825,0.00001803693,0.000016336335,0.000021095153],"domain_scores_gemma":[0.99861574,0.00022584472,0.00052523945,0.00006334948,0.00029432846,0.0002755615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002084573,0.00011500376,0.00017464855,0.0010360606,0.0002423763,0.0003811129,0.00021950337,0.0002823728,0.0015891349],"category_scores_gemma":[0.001246267,0.000103134764,0.00013483736,0.0007325746,0.00022718975,0.00026560912,0.0004621003,0.00025317422,0.00032604637],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047953447,0.000042647363,0.99112445,0.00001540547,0.000031698328,0.00023184658,0.00042298593,0.000118677366,0.0029581378,0.00005892159,0.00015546172,0.004360105],"study_design_scores_gemma":[0.0000016354111,0.000035864046,0.99950206,0.0000016513499,0.000003604555,0.00007585231,0.0001840414,0.00006359471,0.000056938334,0.000008834442,0.00006438932,0.0000014826538],"about_ca_topic_score_codex":0.009278782,"about_ca_topic_score_gemma":0.01665664,"teacher_disagreement_score":0.009278782,"about_ca_system_score_codex":0.00020984586,"about_ca_system_score_gemma":0.0002074554,"threshold_uncertainty_score":0.018449545},"labels":[],"label_agreement":null},{"id":"W4226296977","doi":"10.1002/essoar.10508582.2","title":"Community-Driven Code Comparisons for Three-Dimensional Dynamic Modeling of Sequences of Earthquakes and Aseismic Slip (SEAS)","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada; Southern California Earthquake Center; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Slip (aerodynamics); Geology; Observable; Finite element method; Earthquake rupture; Seismology; Mechanics; Fault (geology); Physics; Structural engineering; Engineering","score_opus":0.06772072077341547,"score_gpt":0.2829962847760441,"score_spread":0.21527556400262865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226296977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87944704,0.00051586813,0.07591642,0.000593218,0.00037291556,0.0007047881,0.005759809,0.009969679,0.026720362],"genre_scores_gemma":[0.89163053,0.0002211243,0.09069164,0.00024426536,0.000033685978,0.001023954,0.011659441,0.002243621,0.0022518022],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99817324,0.00048708043,0.00019482241,0.00027773605,0.00064464565,0.00022246533],"domain_scores_gemma":[0.99296993,0.001966112,0.0003013433,0.0014710011,0.0028344637,0.00045704754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004024928,0.000918997,0.00059501134,0.0011642672,0.00097548106,0.0009384388,0.0031462691,0.001571169,0.0034593905],"category_scores_gemma":[0.010462464,0.00038794568,0.0010940466,0.0010861963,0.0007010227,0.0013864766,0.002061267,0.0015115164,0.00090902526],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013013496,0.002825536,0.038203523,0.0007645853,0.00038125497,0.0004609768,0.0008368098,0.79762626,0.020444667,0.019599233,0.020512396,0.09704342],"study_design_scores_gemma":[0.0002577501,0.0004974113,0.005092909,0.000066278946,0.000038815884,0.00007936426,0.00025563303,0.9716239,0.010525478,0.003256848,0.008242938,0.00006275692],"about_ca_topic_score_codex":0.010002714,"about_ca_topic_score_gemma":0.011180208,"teacher_disagreement_score":0.010002714,"about_ca_system_score_codex":0.0010496266,"about_ca_system_score_gemma":0.0020482205,"threshold_uncertainty_score":0.02128607},"labels":[],"label_agreement":null},{"id":"W4226305257","doi":"10.1785/0320220003","title":"Stress Drop Variations of Induced Earthquakes near the Dallas–Fort Worth Airport, Texas","year":2022,"lang":"en","type":"article","venue":"The Seismic Record","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Southern Methodist University","keywords":"Drop (telecommunication); Seismology; Moment magnitude scale; Geology; Slip (aerodynamics); Stress (linguistics); Stress field; Magnitude (astronomy); Geotechnical engineering; Engineering; Structural engineering; Mathematics; Physics; Finite element method; Geometry","score_opus":0.021256377169331344,"score_gpt":0.21739284173546816,"score_spread":0.19613646456613681,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226305257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999196,0.00000808731,0.0001398073,0.000008536606,0.0000017639602,0.0000037727598,0.00028266342,0.000009532316,0.00034980703],"genre_scores_gemma":[0.99938214,0.00000775122,0.00011054451,0.0000024829358,0.0000024315605,0.0000033563374,0.0003346931,0.0000014224062,0.00015518327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993825,0.0000046198584,0.0000053886847,0.000017880193,0.000018257768,0.00001563492],"domain_scores_gemma":[0.9996735,0.000034441397,0.00013139028,0.00002047521,0.00008599299,0.00005412995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000091450645,0.00019722225,0.00012491872,0.00076548004,0.00025545125,0.00031273594,0.00018711785,0.00017220713,0.00088065956],"category_scores_gemma":[0.0004018877,0.00008533495,0.000101112775,0.00046837272,0.00018623377,0.00024322521,0.00019185341,0.00019347754,0.000184988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016925937,0.0000947619,0.96364236,0.000018662891,0.00004289435,0.0003035624,0.00037886598,0.004108588,0.023121238,0.000080185666,0.00048750482,0.0075520007],"study_design_scores_gemma":[0.0000030943527,0.000040803818,0.9956136,0.000001757983,0.0000039283723,0.000026918335,0.0001702981,0.002867874,0.0011100679,0.000008326181,0.00014972962,0.0000036036777],"about_ca_topic_score_codex":0.01716451,"about_ca_topic_score_gemma":0.029870246,"teacher_disagreement_score":0.01716451,"about_ca_system_score_codex":0.0004617348,"about_ca_system_score_gemma":0.00017447777,"threshold_uncertainty_score":0.034129202},"labels":[],"label_agreement":null},{"id":"W4226322364","doi":"10.1785/0120210210","title":"The Influence of a Transitional Stress Regime on the Source Characteristics of Induced Seismicity and Fault Activation: Evidence from the 30 November 2018 Fort St. John ML 4.5 Induced Earthquake Sequence","year":2022,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Seismology; Induced seismicity; Clockwise; Slip (aerodynamics); Focal mechanism; Stress field; Fault (geology); Seismometer; Graben; Geodesy; Rotation (mathematics); Geometry; Tectonics","score_opus":0.035581766444648076,"score_gpt":0.2289931495730263,"score_spread":0.19341138312837822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226322364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993986,0.00001591499,0.00003519437,0.000008753357,5.848784e-7,0.0000027262934,0.00010572283,0.0000026743603,0.0004298113],"genre_scores_gemma":[0.99969363,0.000015728832,0.000026843385,0.0000050381655,9.677216e-7,0.000002594682,0.00015759861,0.0000015572598,0.00009608284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998441,0.00001809671,0.000013398587,0.000036089485,0.000035477726,0.000052875774],"domain_scores_gemma":[0.99915314,0.00012284167,0.00030371174,0.000052287178,0.00015710549,0.00021084698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015398864,0.00014342184,0.00023305029,0.0010902892,0.00043517732,0.00067216187,0.00031621734,0.00028934426,0.0010722914],"category_scores_gemma":[0.0011546859,0.00018957835,0.00011799625,0.00085913914,0.0007579084,0.00016504482,0.0005527655,0.00025280085,0.0001920238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030718403,0.00004342787,0.96476036,0.000019460284,0.000033679586,0.00035096979,0.0007790382,0.00020512281,0.029492108,0.000081683465,0.0001077009,0.0038192263],"study_design_scores_gemma":[9.35027e-7,0.000009065484,0.9996263,0.0000013649592,0.0000016872076,0.000017183262,0.00011158624,0.00007406053,0.00011409742,0.000005477167,0.000036723126,0.000001691869],"about_ca_topic_score_codex":0.08229661,"about_ca_topic_score_gemma":0.19461735,"teacher_disagreement_score":0.9177034,"about_ca_system_score_codex":0.0009329275,"about_ca_system_score_gemma":0.0005897864,"threshold_uncertainty_score":0.1636352},"labels":[],"label_agreement":null},{"id":"W4229038324","doi":"10.1785/0220220075","title":"Delineating the Controlling Factors of Hydraulic Fracturing-Induced Seismicity in the Northern Montney Play, Northeastern British Columbia, Canada, With Machine Learning","year":2022,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Induced seismicity; Structural basin; Tectonics; Seismology; Fault (geology); Geomorphology","score_opus":0.037627728053554764,"score_gpt":0.24146679521948666,"score_spread":0.2038390671659319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229038324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979724,0.000051445677,0.000969752,0.00009161079,0.0000015949025,0.000008914624,0.0002383968,0.000024543395,0.0006413069],"genre_scores_gemma":[0.9989791,0.000022395065,0.0005027943,0.000009872965,0.0000011119762,0.0000023728699,0.0002305095,0.000002664556,0.00024925589],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998307,0.00002717488,0.000006904905,0.0000347822,0.000035778052,0.00006463005],"domain_scores_gemma":[0.9993617,0.00017721886,0.00010403892,0.000025229,0.0002270175,0.00010482532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038220518,0.00041549714,0.00020282,0.0011614182,0.00077022926,0.0008871128,0.00065327866,0.00025045,0.0008710988],"category_scores_gemma":[0.0015145816,0.00014266103,0.00022789788,0.0014739296,0.0006139319,0.00024280792,0.000331296,0.00032009927,0.000102048674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006665205,0.00004417409,0.9045319,0.000026808582,0.000061005197,0.0001720994,0.000213289,0.07175002,0.0018602979,0.00048202666,0.0007861099,0.020005671],"study_design_scores_gemma":[0.0000067321957,0.00000989781,0.68747956,0.000014420222,0.000020546247,0.000022108823,0.00075275416,0.310422,0.0004774575,0.00027424982,0.0005064572,0.000013800888],"about_ca_topic_score_codex":0.958544,"about_ca_topic_score_gemma":0.97968334,"teacher_disagreement_score":0.041455984,"about_ca_system_score_codex":0.007095085,"about_ca_system_score_gemma":0.0062028053,"threshold_uncertainty_score":0.08340019},"labels":[],"label_agreement":null},{"id":"W4229848863","doi":"10.31223/x5b028","title":"Resolving Northern Alaska Earthquake Sequences Using the Transportable Array and Probabilistic Location Methods","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lawrence Livermore National Laboratory; National Science Foundation","keywords":"Seismology; Aftershock; Geology; Sequence (biology); Range (aeronautics); Tectonics; Event (particle physics); Probabilistic logic; Geodesy; Computer science","score_opus":0.048395522696999066,"score_gpt":0.2865369388059844,"score_spread":0.23814141610898534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229848863","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.28351307,0.00080355373,0.70771,0.0003562146,0.00016984332,0.00007359299,0.0013090419,0.0017599879,0.0043047187],"genre_scores_gemma":[0.734792,0.00023692376,0.2608583,0.00006744965,0.000111456655,0.00007276399,0.0018501888,0.00009776369,0.0019131529],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995765,0.00011232805,0.000036455895,0.00012744131,0.000109231405,0.000038043407],"domain_scores_gemma":[0.9992021,0.00025134886,0.00017483137,0.00010292047,0.00022033894,0.00004843737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068037084,0.0006083423,0.000343166,0.0013539303,0.00033573562,0.0008243505,0.00081378093,0.0004999728,0.0012012207],"category_scores_gemma":[0.003981493,0.0004356798,0.00042230435,0.0010891769,0.00022165656,0.00094624906,0.0011162248,0.00051297003,0.0005622979],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043462805,0.000111016016,0.055424567,0.00015783976,0.0002238662,0.00049162883,0.00043816038,0.45663917,0.009818523,0.007471546,0.0034259497,0.46536303],"study_design_scores_gemma":[0.000034262717,0.000059440812,0.008060095,0.000022383972,0.000036502643,0.00011777343,0.00014329958,0.9818602,0.0015952467,0.0056216954,0.002405967,0.00004313772],"about_ca_topic_score_codex":0.010702408,"about_ca_topic_score_gemma":0.018225549,"teacher_disagreement_score":0.010702408,"about_ca_system_score_codex":0.00033194633,"about_ca_system_score_gemma":0.0007880567,"threshold_uncertainty_score":0.02128023},"labels":[],"label_agreement":null},{"id":"W4229900834","doi":"10.4095/301267","title":"Tsunamis","year":2010,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Computer science","score_opus":0.036191632440439596,"score_gpt":0.2554757715518717,"score_spread":0.21928413911143207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229900834","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.035806045,0.0045496137,0.0017988795,0.0014900242,0.0011558881,0.0017993066,0.21065342,0.001078431,0.7416683],"genre_scores_gemma":[0.18382922,0.014073924,0.0029074529,0.0013155988,0.00040320004,0.00075738603,0.24909069,0.0002400674,0.5473824],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983682,0.00005296056,0.000096739954,0.000095816176,0.0010233031,0.00036299543],"domain_scores_gemma":[0.99757177,0.00006924476,0.0002389278,0.00012293647,0.0017145084,0.0002827128],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003420302,0.00092830433,0.000403774,0.003151054,0.0018223571,0.0015547342,0.0009596687,0.0004371079,0.05790404],"category_scores_gemma":[0.0026834588,0.00018375828,0.0003470835,0.00419794,0.0004580301,0.0005797507,0.0013112962,0.00078238494,0.018208753],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002082306,0.00013585821,0.061596397,0.000662246,0.000061146224,0.0012679034,0.001957996,0.0007186501,0.0013972111,0.010053096,0.745388,0.17655326],"study_design_scores_gemma":[0.00001693228,0.000055159242,0.13187343,0.0004088156,0.000019397703,0.0007848286,0.0013399717,0.0001091649,0.00042296437,0.0007484175,0.8641935,0.00002744794],"about_ca_topic_score_codex":0.41291195,"about_ca_topic_score_gemma":0.49892858,"teacher_disagreement_score":0.41291195,"about_ca_system_score_codex":0.0036225424,"about_ca_system_score_gemma":0.008224647,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4229946712","doi":"10.1002/cpe.1520","title":"Large‐scale numerical simulations of earthquake fault systems: illuminating the role of dilatational gravity in earthquake nucleation","year":2009,"lang":"en","type":"article","venue":"Concurrency and Computation Practice and Experience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; TD Bank Group","funders":"Basic Energy Sciences; Natural Sciences and Engineering Research Council of Canada; Institute for Catastrophic Loss Reduction; National Aeronautics and Space Administration","keywords":"Seismology; Geology; Foreshock; Shear (geology); Nucleation; Earthquake simulation; Slip (aerodynamics); Tectonics; Earthquake prediction; Physics; Aftershock; Petrology","score_opus":0.014360412734274002,"score_gpt":0.27918148626289824,"score_spread":0.2648210735286242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229946712","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945878,0.00004525854,0.0041661616,0.00007270516,0.000005476918,0.0000075536723,0.00007357616,0.000073502015,0.00096800906],"genre_scores_gemma":[0.99815375,0.000028270983,0.0016386289,0.000005355634,0.0000025601657,0.0000056271706,0.00005118213,0.000009461523,0.00010523437],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988973,0.000047632573,0.0000094793895,0.000019556834,0.000021682732,0.000011829499],"domain_scores_gemma":[0.99802315,0.0015905749,0.00013356144,0.00009737478,0.00007746473,0.000077880286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057791045,0.000195033,0.00025189476,0.0003229435,0.00025408395,0.00048526798,0.00040884153,0.00029947955,0.0007531931],"category_scores_gemma":[0.0031996185,0.0002481456,0.00016612683,0.0003637175,0.0006005224,0.0003407105,0.0003629544,0.0003619577,0.000047081874],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009671351,0.00006505447,0.01799608,0.00002694257,0.00002816892,0.000063507374,0.0001318021,0.9732141,0.0027995259,0.001996615,0.00019937426,0.0033822216],"study_design_scores_gemma":[0.000018104462,0.000019494773,0.0027428456,0.0000018954748,0.00000508602,0.00000585824,0.000017424298,0.99618644,0.00056827004,0.00034225915,0.00008924809,0.0000030172375],"about_ca_topic_score_codex":0.01770888,"about_ca_topic_score_gemma":0.013045405,"teacher_disagreement_score":0.01770888,"about_ca_system_score_codex":0.0005910855,"about_ca_system_score_gemma":0.0005675212,"threshold_uncertainty_score":0.035211563},"labels":[],"label_agreement":null},{"id":"W4229994300","doi":"10.1785/01/20200344","title":"The Productivity of Cascadia Aftershock Sequences","year":2021,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Seismology; Subduction; Geology; Induced seismicity; Productivity; Fault (geology); Outlier; Statistics; Tectonics","score_opus":0.015249491571407139,"score_gpt":0.20701991426211233,"score_spread":0.19177042269070518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229994300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99563134,0.00009635439,0.0007474202,0.000044684097,0.000005240294,0.000007892072,0.0017447944,0.000077037876,0.001645217],"genre_scores_gemma":[0.9982717,0.00005286275,0.00014255258,0.0000030417161,0.000003509943,0.000002732866,0.001323296,0.000008536189,0.00019179602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99934095,0.00009417655,0.00008417299,0.00023727678,0.00016951341,0.000073778596],"domain_scores_gemma":[0.99123096,0.0020297645,0.0035751106,0.0008790914,0.0016769579,0.00060804735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012121149,0.00052343257,0.00022792137,0.0033313865,0.00023379452,0.0012690049,0.0003453671,0.00020506182,0.0022957702],"category_scores_gemma":[0.01173848,0.00021764525,0.0003580202,0.0030703843,0.00044526492,0.00080394035,0.0009369053,0.00031485374,0.00044007905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026820868,0.00000509455,0.9923833,0.000019925645,0.00008921305,0.00005660698,0.00019011108,0.0026526114,0.00045032543,0.00012129261,0.00024341913,0.0037612594],"study_design_scores_gemma":[0.0000016497036,0.000011106413,0.9962475,0.000008894108,0.000015595926,0.00003450439,0.00017043692,0.0027625505,0.00019354667,0.000088366374,0.00046084353,0.000005059134],"about_ca_topic_score_codex":0.037357695,"about_ca_topic_score_gemma":0.03767008,"teacher_disagreement_score":0.037357695,"about_ca_system_score_codex":0.0009973063,"about_ca_system_score_gemma":0.00045025314,"threshold_uncertainty_score":0.0742805},"labels":[],"label_agreement":null},{"id":"W4230353787","doi":"10.4095/314591","title":"Regional centroid moment tensor solutions for eastern Canadian earthquakes: 2017","year":2019,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Centroid; Moment tensor; Moment (physics); Seismology; Geology; Tensor (intrinsic definition); Geodesy; Geography; Mathematics; Physics; Geometry; Meteorology; Classical mechanics","score_opus":0.10363100081395364,"score_gpt":0.2685114281130684,"score_spread":0.16488042729911473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230353787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90644324,0.00091666676,0.008442551,0.00041466183,0.000102502774,0.00020337885,0.063341826,0.00086233014,0.019272862],"genre_scores_gemma":[0.9252854,0.0008333291,0.016414426,0.000037569323,0.00002611256,0.000051425377,0.050133348,0.00019824803,0.007020106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99950457,0.00000972851,0.00002822675,0.000054293207,0.00026046252,0.00014268782],"domain_scores_gemma":[0.9980692,0.00003643114,0.00014160428,0.00006343386,0.0015577193,0.0001316193],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047789398,0.0008610598,0.0002920885,0.0033470448,0.0014385668,0.00097118097,0.00089243276,0.00042560496,0.0028620292],"category_scores_gemma":[0.0022196916,0.0002794578,0.00045887177,0.004452415,0.0004181056,0.00064148026,0.0008032198,0.0005664876,0.000957298],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006852181,0.00021628627,0.5705217,0.0008108782,0.00051181065,0.001457301,0.0023892135,0.042326584,0.050027877,0.003379101,0.047093093,0.280581],"study_design_scores_gemma":[0.000058345147,0.000061096915,0.9400634,0.00006763264,0.00015971444,0.0003143658,0.0017949209,0.023511132,0.012895711,0.0004399085,0.020463292,0.00017051835],"about_ca_topic_score_codex":0.9258331,"about_ca_topic_score_gemma":0.9750939,"teacher_disagreement_score":0.074166894,"about_ca_system_score_codex":0.00715664,"about_ca_system_score_gemma":0.012922169,"threshold_uncertainty_score":0.1492073},"labels":[],"label_agreement":null},{"id":"W4230568749","doi":"10.1016/j.ijrmms.2004.07.006","title":"A statistical approach for the integrated analysis of mine-induced seismicity and numerical stress estimates, a case study—Part I: developing the relations","year":2004,"lang":"en","type":"article","venue":"International Journal of Rock Mechanics and Mining Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Smoothing; Variable (mathematics); Set (abstract data type); Multivariate statistics; Data mining; Induced seismicity; Computer science; Univariate; Data set; Microseism; Statistics; Geology; Mathematics; Seismology","score_opus":0.05014974289764641,"score_gpt":0.2995494122367968,"score_spread":0.24939966933915042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230568749","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.015438754,0.00007454143,0.9833477,0.00015966786,0.000009065586,0.000040335995,0.00008012557,0.00006796375,0.0007817994],"genre_scores_gemma":[0.38757825,0.00030462802,0.60982674,0.00008030573,0.00010317234,0.00041428895,0.00031910665,0.00009590553,0.0012775502],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99600166,0.0025540702,0.00023339712,0.00034663838,0.0007613096,0.00010282629],"domain_scores_gemma":[0.9705969,0.025376411,0.0012461337,0.00096879754,0.00163904,0.000172673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008359402,0.00057208154,0.00054371683,0.0030451948,0.00064581697,0.0018821679,0.0012318582,0.0006818618,0.001936668],"category_scores_gemma":[0.03324268,0.0005178356,0.0009774743,0.0027762372,0.001639781,0.0020317081,0.0015413412,0.001051672,0.00023911576],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011432613,0.0003755315,0.037868995,0.00021589962,0.00044732902,0.0006868418,0.000919979,0.23803297,0.006671915,0.47160846,0.0020068623,0.24105097],"study_design_scores_gemma":[0.000011112768,0.00018040651,0.009533067,0.00002332265,0.0000693534,0.00024087935,0.00025727547,0.884842,0.0010908362,0.10167701,0.002041699,0.000033078944],"about_ca_topic_score_codex":0.0056911632,"about_ca_topic_score_gemma":0.008341141,"teacher_disagreement_score":0.008359402,"about_ca_system_score_codex":0.0011224818,"about_ca_system_score_gemma":0.0031080362,"threshold_uncertainty_score":0.0442093},"labels":[],"label_agreement":null},{"id":"W4230867634","doi":"10.5194/se-2020-139","title":"Seismicity during and after stimulation of a 6.1 km deep Enhanced Geothermal System in Helsinki, Finland","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Deutsche Forschungsgemeinschaft","keywords":"Induced seismicity; Geology; Seismology; Geothermal gradient; Borehole; Geophone; Framing (construction); Geophysics; Paleontology; Geography; Archaeology","score_opus":0.011619351252882236,"score_gpt":0.2030010080576438,"score_spread":0.19138165680476155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4230867634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99818534,0.00003518459,0.00013207091,0.000012732067,0.000003913505,0.000006755981,0.0011826619,0.000018484636,0.00042273317],"genre_scores_gemma":[0.9975661,0.000030287718,0.00020928442,0.0000051269135,0.000005600864,0.0000098891815,0.0019350322,0.0000034323407,0.00023523503],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987555,0.000012180591,0.000008861408,0.000034845783,0.000027967508,0.000040600306],"domain_scores_gemma":[0.99982893,0.000027419901,0.00003566788,0.000020569174,0.000029590756,0.00005784325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000198336,0.0002997069,0.00024282829,0.00085386826,0.0003069051,0.0003356044,0.0003533414,0.00050482486,0.0008455443],"category_scores_gemma":[0.00039636597,0.00015633585,0.00023055881,0.00092111545,0.0003133675,0.00034557708,0.0007087519,0.00018889594,0.00022770371],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011198474,0.00038060264,0.8803504,0.0002785118,0.00025008625,0.0040277457,0.0028563486,0.02028826,0.05441602,0.0003213809,0.002202106,0.03350879],"study_design_scores_gemma":[0.000023878629,0.00009131703,0.9913119,0.000013433076,0.00003021975,0.0001679989,0.0006192585,0.0045053028,0.002150759,0.00003909212,0.0010293201,0.000017599174],"about_ca_topic_score_codex":0.011950677,"about_ca_topic_score_gemma":0.023806304,"teacher_disagreement_score":0.011950677,"about_ca_system_score_codex":0.00046377495,"about_ca_system_score_gemma":0.0005166703,"threshold_uncertainty_score":0.023762226},"labels":[],"label_agreement":null},{"id":"W4231096207","doi":"10.31223/osf.io/a9gd6","title":"Structure of the North Anatolian Fault Zone imaged via teleseismic scattering tomography","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"British Geological Survey; Natural Environment Research Council; Sakarya Üniversitesi; University of Leeds; Sight Research UK","keywords":"North Anatolian Fault; Seismology; Geology; Fault (geology); Seismic hazard; Deformation (meteorology); Geophysical imaging; Seismic zone; Induced seismicity","score_opus":0.01172659960781375,"score_gpt":0.20115220459209965,"score_spread":0.1894256049842859,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4231096207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971802,0.000067449284,0.00089884363,0.0000541763,0.0000023668292,0.0000039131605,0.00038230722,0.000048820395,0.0013619362],"genre_scores_gemma":[0.997943,0.000091026,0.0011581811,0.0000074939344,0.0000034260129,0.000004327191,0.0004380891,0.0000065211893,0.00034795303],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999738,0.0000021777453,0.000002038454,0.000009462265,0.000007652237,0.0000049071705],"domain_scores_gemma":[0.9999379,0.00000796945,0.000021208578,0.0000075096523,0.000019630432,0.000005781615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000050431074,0.0001591474,0.00009779604,0.0005235646,0.0001380224,0.00029278078,0.00013631825,0.00018221748,0.0006693329],"category_scores_gemma":[0.00013141106,0.00013484675,0.000059922604,0.0006023891,0.00015477282,0.00017333015,0.00018109058,0.00008454377,0.00015488117],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045493015,0.00017987078,0.3805297,0.00014422499,0.000105219915,0.0014634142,0.0010179661,0.037172932,0.49033368,0.0027894531,0.0025724457,0.08323616],"study_design_scores_gemma":[0.000037399885,0.00005936629,0.8876702,0.00002160668,0.000052364692,0.0008883023,0.00050671695,0.09420584,0.014203351,0.0005249788,0.0018105609,0.000019195893],"about_ca_topic_score_codex":0.0105862,"about_ca_topic_score_gemma":0.014630063,"teacher_disagreement_score":0.0105862,"about_ca_system_score_codex":0.00023356457,"about_ca_system_score_gemma":0.00025716526,"threshold_uncertainty_score":0.021049142},"labels":[],"label_agreement":null},{"id":"W4231593048","doi":"10.1007/978-3-319-12712-5_1","title":"Meteorological tsunamis on the US East Coast and in other regions of the World Ocean","year":2014,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Oceanography; Geography; East coast; Climatology; Geology","score_opus":0.03201980863227034,"score_gpt":0.2030787910839639,"score_spread":0.17105898245169357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4231593048","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09135867,0.052202463,0.0017509433,0.00785351,0.0020005633,0.000025929414,0.003015979,0.00012553536,0.8416665],"genre_scores_gemma":[0.48753226,0.11462958,0.002564847,0.0011034537,0.0008130916,0.000029820636,0.0046755844,0.000120315126,0.38853103],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99996924,0.000004530223,0.000002295674,0.000003960189,0.000013056285,0.0000068481027],"domain_scores_gemma":[0.99996555,0.000010884463,0.000005142613,0.0000020886132,0.000011762974,0.000004563665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058558253,0.0002344204,0.00007655777,0.00052620843,0.00035506353,0.00058527576,0.00021137828,0.00022015374,0.0068174424],"category_scores_gemma":[0.00024051718,0.00010310507,0.00011189034,0.001778682,0.00022107697,0.00049007824,0.00030911894,0.00032474656,0.00059030886],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039829018,0.00004104617,0.030507375,0.00030620865,0.000038264963,0.00052867504,0.002582235,0.0037774993,0.0012972244,0.10348981,0.33155286,0.5258389],"study_design_scores_gemma":[0.000004395082,0.000019439396,0.14785647,0.0003957965,0.000022187638,0.00031400684,0.0029094499,0.0010038904,0.0004459266,0.019380553,0.8276314,0.00001647239],"about_ca_topic_score_codex":0.0968641,"about_ca_topic_score_gemma":0.27816352,"teacher_disagreement_score":0.0968641,"about_ca_system_score_codex":0.0009352752,"about_ca_system_score_gemma":0.0007240819,"threshold_uncertainty_score":0.19260061},"labels":[],"label_agreement":null},{"id":"W4231667303","doi":"10.1002/cpe.1640","title":"Proceedings of the 6th ACES Symposium, May 11–16, 2008, Cairns, Australia: Introduction to the Special Issue","year":2010,"lang":"en","type":"article","venue":"Concurrency and Computation Practice and Experience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"China; Government (linguistics); Natural disaster; History; Political science; Geography; Economic growth; Economic history; Meteorology; Law; Economics","score_opus":0.01648935469475344,"score_gpt":0.28082067041236053,"score_spread":0.2643313157176071,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4231667303","genre_codex":"other","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009851363,0.06773046,0.023310024,0.07723964,0.2328703,0.0011487468,0.0054650228,0.004585779,0.5777987],"genre_scores_gemma":[0.011009558,0.022326555,0.0055555697,0.004036913,0.02047615,0.00027018358,0.004693961,0.0015967946,0.9300344],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99899346,0.00012071196,0.00005917902,0.00014828338,0.00055499916,0.00012345063],"domain_scores_gemma":[0.996999,0.00018370329,0.00012333033,0.00015553657,0.0016528253,0.00088553096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022795962,0.0012086713,0.00097126333,0.0014836215,0.0017508643,0.004626289,0.0015719166,0.001705635,0.18816718],"category_scores_gemma":[0.0030649956,0.0007096636,0.00062458037,0.001183193,0.00076261,0.0029724257,0.0031280422,0.0027315333,0.084492646],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043104126,0.000044893328,0.00025440886,0.00016297793,0.000006353937,0.000058015277,0.00009385815,0.00017984648,0.00044530668,0.00073136267,0.95339763,0.044582386],"study_design_scores_gemma":[0.000008403691,0.0000237003,0.0012310672,0.00012081096,0.0000044385647,0.00004949375,0.000089929476,0.00023360147,0.00011357076,0.00042492725,0.99769163,0.000008411502],"about_ca_topic_score_codex":0.009412456,"about_ca_topic_score_gemma":0.024397297,"teacher_disagreement_score":0.18816718,"about_ca_system_score_codex":0.0017782263,"about_ca_system_score_gemma":0.0036150753,"threshold_uncertainty_score":0.6294819},"labels":[],"label_agreement":null},{"id":"W4232397877","doi":"10.1190/tle22050491.1","title":"Review","year":2003,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Capilano University","funders":"","keywords":"Library science; Art; Geology; Computer science","score_opus":0.040464614533537675,"score_gpt":0.2543485590659502,"score_spread":0.21388394453241255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232397877","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00031143133,0.8872147,0.00082454114,0.012875957,0.012340653,0.000100860605,0.0017428173,0.00029085207,0.08429816],"genre_scores_gemma":[0.0026106124,0.8788672,0.0012650128,0.00913959,0.006698469,0.000108961984,0.0028578509,0.00011171382,0.09834065],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99945205,0.000070455746,0.00007308284,0.00010096402,0.00024453076,0.000058955455],"domain_scores_gemma":[0.9987627,0.00030837307,0.00011639516,0.00007887627,0.0005519293,0.00018162669],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068201945,0.00087264273,0.0013340159,0.0034725151,0.0006183889,0.0028899726,0.0020101059,0.0018575939,0.14347781],"category_scores_gemma":[0.003978667,0.00031367058,0.0006137932,0.0037842747,0.00048041766,0.0026822686,0.0015215642,0.0017684544,0.11407138],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032760538,0.000020704263,0.00012182317,0.0030282731,0.000023125638,0.000112974994,0.000052781215,0.000048971127,0.00016023513,0.0017282667,0.64766425,0.34700587],"study_design_scores_gemma":[0.0000033123872,0.000006087156,0.00015681566,0.00095683854,0.000012125398,0.00023963719,0.000025275838,0.0000050623603,0.000021845979,0.00039901078,0.998171,0.0000031107502],"about_ca_topic_score_codex":0.00299194,"about_ca_topic_score_gemma":0.004887054,"teacher_disagreement_score":0.14347781,"about_ca_system_score_codex":0.0012642798,"about_ca_system_score_gemma":0.0040727053,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4232594896","doi":"10.1007/s00024-004-2516-3","title":"Methods for Evaluation of Geodetic Data and Seismicity Developed with Numerical Simulations: Review and Applications","year":2004,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"University of Colorado Boulder; Los Alamos National Laboratory; U.S. Geological Survey; Universidad Complutense de Madrid; Southern California Earthquake Center; National Aeronautics and Space Administration; U.S. Department of Energy; National Science Foundation","keywords":"Geodetic datum; Induced seismicity; Global Positioning System; Geology; Computer science; Field (mathematics); Data mining; Geodesy; Seismology; Mathematics","score_opus":0.05721963417533806,"score_gpt":0.33685315297295915,"score_spread":0.2796335187976211,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232594896","genre_codex":"methods","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0030141405,0.012292452,0.98124117,0.00009626548,0.0001239051,0.00009829456,0.00019784765,0.0009259872,0.0020100519],"genre_scores_gemma":[0.10361357,0.03800854,0.8529977,0.00013782123,0.00029196506,0.0006840129,0.0006973512,0.0007306628,0.0028383106],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9968491,0.0011165407,0.00031203785,0.00042188977,0.0012305175,0.00006988323],"domain_scores_gemma":[0.99275476,0.004254523,0.00067798415,0.0007026129,0.0015162065,0.000093870105],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0034883507,0.002017774,0.0025877948,0.004443046,0.00043720397,0.0021146236,0.0023802638,0.001730283,0.0026560945],"category_scores_gemma":[0.013868955,0.0009655346,0.001077223,0.004475897,0.0013672932,0.0017210625,0.00159494,0.0012788628,0.0016251821],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019667586,0.00017006193,0.005581668,0.0036576944,0.0004317,0.00018581301,0.00027429033,0.15931165,0.010035076,0.02981447,0.003940721,0.7864002],"study_design_scores_gemma":[0.00008637024,0.00016787724,0.003247789,0.0012941225,0.00027017907,0.00070913107,0.00019287645,0.8929502,0.015624143,0.039570916,0.045679696,0.00020676803],"about_ca_topic_score_codex":0.003683633,"about_ca_topic_score_gemma":0.002211943,"teacher_disagreement_score":0.004443046,"about_ca_system_score_codex":0.0007033857,"about_ca_system_score_gemma":0.001299646,"threshold_uncertainty_score":0.018448353},"labels":[],"label_agreement":null},{"id":"W4232693749","doi":"10.5194/se-2020-146","title":"Nano-scale earthquake records preserved in plagioclase microfractures from the lower continental crust","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"European Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Plagioclase; Geology; Slip (aerodynamics); Crust; Wall rock; Fault (geology); Petrology; Mineralogy; Seismology; Geochemistry; Quartz","score_opus":0.0249576089808979,"score_gpt":0.22737356763113775,"score_spread":0.20241595865023984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232693749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99910766,0.0000970117,0.00007894129,0.000007673667,0.0000012863144,0.0000032796293,0.00027347897,0.000007207513,0.0004234148],"genre_scores_gemma":[0.99907,0.00005740979,0.00015517963,0.0000057956786,0.0000017487076,0.0000034359452,0.00044364264,0.0000027078884,0.00026015274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999584,0.0000017046464,0.0000035284597,0.000015272974,0.0000104596775,0.000010514925],"domain_scores_gemma":[0.9998945,0.000006473123,0.0000358773,0.000009028912,0.000036412795,0.000017755574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006397594,0.000117506694,0.00011431299,0.00071576296,0.00026977813,0.0002759613,0.00014424144,0.00017948468,0.00062685553],"category_scores_gemma":[0.00015465052,0.000104124825,0.00010618032,0.0003819615,0.0001938999,0.00012133912,0.00021001861,0.000108462475,0.00016822056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013567784,0.000021099026,0.53218985,0.00008999963,0.00005201472,0.00067049154,0.0013429057,0.00031541157,0.45596534,0.00009474504,0.00020634185,0.008916242],"study_design_scores_gemma":[6.5671315e-7,0.000011320165,0.99831605,0.0000017661893,0.000004031124,0.00008096637,0.00012102546,0.00006056489,0.001150554,0.0000049407276,0.00024730148,8.278775e-7],"about_ca_topic_score_codex":0.018058557,"about_ca_topic_score_gemma":0.042714525,"teacher_disagreement_score":0.018058557,"about_ca_system_score_codex":0.00042927495,"about_ca_system_score_gemma":0.00013216026,"threshold_uncertainty_score":0.03590691},"labels":[],"label_agreement":null},{"id":"W4232728373","doi":"10.1007/s10704-006-0030-6","title":"Laboratory Earthquakes","year":2006,"lang":"en","type":"article","venue":"International Journal of Fracture","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Office of Naval Research; California Institute of Technology; National Science Foundation","keywords":"Seismology; Natural phenomenon; Geology; Mechanism (biology); Forensic engineering; Visualization; Engineering; Geophysics; Geotechnical engineering; Natural (archaeology); Physics; Mechanical engineering","score_opus":0.005554408591929648,"score_gpt":0.21646570017663716,"score_spread":0.2109112915847075,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4232728373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6712978,0.00058432727,0.012864584,0.0020555044,0.0013295505,0.0010674795,0.03349548,0.0055869333,0.2717184],"genre_scores_gemma":[0.9310569,0.0003323097,0.0036396226,0.00056796154,0.0004918343,0.0005285561,0.019180192,0.00022154527,0.04398112],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99942756,0.000092144466,0.000062215724,0.00013132113,0.0001697258,0.00011700234],"domain_scores_gemma":[0.9984017,0.00023842293,0.00028840924,0.00047497122,0.0003302377,0.0002663059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046389035,0.00047620642,0.00031963206,0.0014916266,0.0006016123,0.0006205713,0.0005801072,0.0005545219,0.03459184],"category_scores_gemma":[0.0020232843,0.00016781475,0.00031926812,0.0014924272,0.00043146222,0.00060780795,0.0009658382,0.0007658949,0.0072501637],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0050107813,0.0032623848,0.122790016,0.0011980785,0.00042958083,0.0023497585,0.0026166718,0.0073746885,0.11356452,0.057376955,0.35013574,0.33389091],"study_design_scores_gemma":[0.001310385,0.0059401765,0.35920358,0.00015644771,0.00033872694,0.0023867548,0.0020277791,0.011553979,0.06948488,0.011701342,0.5356389,0.00025702646],"about_ca_topic_score_codex":0.0011684246,"about_ca_topic_score_gemma":0.0023403317,"teacher_disagreement_score":0.03459184,"about_ca_system_score_codex":0.0005164684,"about_ca_system_score_gemma":0.00039017663,"threshold_uncertainty_score":0.115721166},"labels":[],"label_agreement":null},{"id":"W4233182053","doi":"10.1002/essoar.10504739.1","title":"Strain accumulation and release rate in Canada: Implications for long-term crustal deformation and earthquake hazards","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Geology; Geodetic datum; Post-glacial rebound; Seismology; Seismic hazard; Crust; Deformation (meteorology); Strain rate; Continental crust; Glacial period; Geodesy; Geophysics; Paleontology; Oceanography","score_opus":0.051135247498770124,"score_gpt":0.2710620054428177,"score_spread":0.2199267579440476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233182053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98620147,0.00096758583,0.00062301435,0.0015347053,0.000011675047,0.000020840074,0.0065410193,0.000048088874,0.0040516662],"genre_scores_gemma":[0.996617,0.00044639077,0.0003605052,0.00009051775,0.0000032454843,0.0000048213533,0.0016288442,0.000011064536,0.0008375784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995548,0.000023390417,0.000032848464,0.00008119999,0.00013450361,0.0001731563],"domain_scores_gemma":[0.99788755,0.00023256514,0.0004634338,0.00008755611,0.00095924485,0.00036954053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067509606,0.0003572796,0.00033682113,0.0017254339,0.0014264855,0.0017986106,0.0011010875,0.00038102322,0.0019327501],"category_scores_gemma":[0.0031609011,0.0002123649,0.00051628065,0.0047278106,0.00082824216,0.00071415835,0.00084446254,0.00057488424,0.00012268827],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000895517,0.000025609812,0.98056066,0.00004044916,0.00010515685,0.00016263637,0.00044815455,0.004259763,0.00084186794,0.0010937499,0.0009907093,0.011381684],"study_design_scores_gemma":[0.0000032713544,0.0000054669895,0.9930821,0.000021289414,0.000024740233,0.00003561785,0.00081374054,0.0047890837,0.00017016652,0.00020409859,0.0008364893,0.000013921281],"about_ca_topic_score_codex":0.99640226,"about_ca_topic_score_gemma":0.9966092,"teacher_disagreement_score":0.030428654,"about_ca_system_score_codex":0.030428654,"about_ca_system_score_gemma":0.026585229,"threshold_uncertainty_score":0.22077638},"labels":[],"label_agreement":null},{"id":"W4233296647","doi":"10.1130/geol.s.12275744","title":"Supplemental Material: Uplift and exhumation in Haida Gwaii driven by terrane translation and transpression along the southern Queen Charlotte fault, Canada","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Transpression; Geology; Terrane; Queen (butterfly); Seismology; Fault (geology); Archaeology; History; Tectonics; Sinistral and dextral","score_opus":0.01834781526257785,"score_gpt":0.21193338867579362,"score_spread":0.19358557341321578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233296647","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0059983567,0.00005857838,0.0006474313,0.00022135348,0.00024573202,0.00004217721,0.9823309,0.0013497655,0.009105614],"genre_scores_gemma":[0.06895475,0.0004118708,0.0049039195,0.00020440696,0.0001718145,0.00011856766,0.89648825,0.0016675439,0.0270788],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9997863,0.000005064111,0.00001353546,0.000033813856,0.00009689594,0.000064335814],"domain_scores_gemma":[0.9990029,0.00013769457,0.0000536163,0.000053018695,0.00062259973,0.00013027687],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021381355,0.0007063679,0.0007756371,0.0022717102,0.001784089,0.0013756296,0.0016185212,0.000745686,0.45266804],"category_scores_gemma":[0.0013784007,0.00047820495,0.0007067968,0.005206544,0.00020725651,0.0005404709,0.00051751063,0.0005487407,0.050222415],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014238193,0.000109882254,0.014274265,0.00042072556,0.000069032016,0.00024290395,0.00015849671,0.0049950387,0.0014870466,0.00082619087,0.9641445,0.013129518],"study_design_scores_gemma":[0.0005757314,0.00006224553,0.41673657,0.0008176183,0.00017194593,0.00049713935,0.001155738,0.021749709,0.002070531,0.003945924,0.5520427,0.00017410306],"about_ca_topic_score_codex":0.7538882,"about_ca_topic_score_gemma":0.8637338,"teacher_disagreement_score":0.45266804,"about_ca_system_score_codex":0.0029106725,"about_ca_system_score_gemma":0.0054422244,"threshold_uncertainty_score":0.7807026},"labels":[],"label_agreement":null},{"id":"W4233336326","doi":"10.31223/osf.io/c3s5g","title":"Pseudotachylyte as field evidence for lower crustal earthquakes during the intracontinental Petermann Orogeny (Musgrave Block, Central Australia)","year":2017,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Geology; Continental crust; Crust; Orogeny; Seismology; Shearing (physics); Induced seismicity; Mylonite; Petrology; Slip (aerodynamics); Shear zone; Tectonics; Geophysics; Geotechnical engineering","score_opus":0.06328580762373501,"score_gpt":0.311021992274597,"score_spread":0.24773618465086197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233336326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946946,0.000029564577,0.00001976681,0.0000052746614,5.02778e-7,0.000002690893,0.000048873753,0.0000013964192,0.00042246963],"genre_scores_gemma":[0.9995105,0.000047795667,0.000072806826,0.000004883576,0.0000014396846,0.000003798012,0.00012191907,0.000001363525,0.00023550233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988186,0.00001643593,0.0000096412905,0.00003875108,0.000028628272,0.000024674477],"domain_scores_gemma":[0.99966204,0.000031922722,0.00012563799,0.000025909023,0.00009179959,0.000062713734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016923236,0.00016325629,0.00014256786,0.0010751494,0.00035883632,0.00030750228,0.00021182012,0.000187125,0.00065786525],"category_scores_gemma":[0.0005864562,0.00013254379,0.00007669207,0.00077117747,0.00047890402,0.00019658449,0.000501823,0.000117510725,0.00010522258],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012278192,0.000028743263,0.964417,0.000042559834,0.000023751634,0.00039566096,0.00387806,0.00013309624,0.023107229,0.00014922998,0.00012401094,0.0075777974],"study_design_scores_gemma":[5.0680495e-7,0.000008793882,0.9996363,0.0000016429503,0.0000018842896,0.000033412416,0.00013529797,0.000032773038,0.000075477576,0.0000045590045,0.00006887823,5.830586e-7],"about_ca_topic_score_codex":0.065748915,"about_ca_topic_score_gemma":0.12846209,"teacher_disagreement_score":0.065748915,"about_ca_system_score_codex":0.00046729905,"about_ca_system_score_gemma":0.0003344794,"threshold_uncertainty_score":0.13073248},"labels":[],"label_agreement":null},{"id":"W4233353850","doi":"10.1002/essoar.10504189.1","title":"Statistics and Forecasting of Aftershocks during the 2019 Ridgecrest, California, Earthquake Sequence","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Foreshock; Sequence (biology); Seismology; Geology; Extreme value theory; Induced seismicity; Statistics; Mathematics","score_opus":0.044633720653360145,"score_gpt":0.2340658931898498,"score_spread":0.18943217253648964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4233353850","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933564,0.00009256131,0.0050271903,0.00009168627,0.000008018428,0.000010937766,0.00079078204,0.000073505034,0.00054886524],"genre_scores_gemma":[0.99648476,0.00007741307,0.0014861828,0.000004345228,0.0000100544385,0.000005321357,0.0016702274,0.000005652241,0.00025596147],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997919,0.000047216818,0.000016344266,0.00005569935,0.00006272913,0.00002610347],"domain_scores_gemma":[0.9967415,0.0017714979,0.0006637832,0.00014660275,0.0005273825,0.00014937196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012376768,0.00029003253,0.00029562094,0.0011486986,0.00018986326,0.00054102036,0.00032548018,0.0003677133,0.00040119732],"category_scores_gemma":[0.005044165,0.00016090505,0.00020597361,0.00079682795,0.0002968566,0.00034605098,0.00024711905,0.00032667175,0.000111761845],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024030071,0.00006799669,0.33365977,0.000053580254,0.0000709553,0.00025909746,0.00008647468,0.63714427,0.001770813,0.0020797385,0.0018723019,0.022694802],"study_design_scores_gemma":[0.000009988989,0.000066140376,0.21751645,0.000011422643,0.000021164204,0.00003299164,0.000108464046,0.78038555,0.0008029946,0.0006820564,0.00034409962,0.000018722516],"about_ca_topic_score_codex":0.033284962,"about_ca_topic_score_gemma":0.030439945,"teacher_disagreement_score":0.033284962,"about_ca_system_score_codex":0.0005391445,"about_ca_system_score_gemma":0.00073086267,"threshold_uncertainty_score":0.066182435},"labels":[],"label_agreement":null},{"id":"W4234231488","doi":"10.1139/cjes-2019-0225","title":"Understanding tectonic processes and their consequences: a tribute to A.M. Celâl Şengör: Part 2","year":2019,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Geology; Tribute; Tectonics; Paleontology; Geochemistry; Archaeology","score_opus":0.0765119907827635,"score_gpt":0.2256693713715996,"score_spread":0.1491573805888361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234231488","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0033970415,0.09591885,0.010152239,0.84007865,0.027613781,0.000035757956,0.00030999724,0.00014176195,0.022351908],"genre_scores_gemma":[0.18972343,0.29960036,0.029969905,0.19544947,0.098210216,0.00021718006,0.00072836556,0.00089178944,0.18520923],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99929416,0.0001940821,0.00003790657,0.00018469512,0.0002326916,0.00005651646],"domain_scores_gemma":[0.994679,0.0024500315,0.00023735958,0.00026314185,0.0018140569,0.0005564707],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003313783,0.00080897426,0.0008462242,0.0014595365,0.002693845,0.006204787,0.0011369523,0.0027036914,0.012897899],"category_scores_gemma":[0.009077035,0.00031863473,0.0005330162,0.0012613528,0.0048671467,0.008038802,0.0026814013,0.0063573746,0.0034592603],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006271532,0.00005793109,0.0026181198,0.00040925606,0.000055948512,0.00015761158,0.0010700072,0.0016573434,0.0007806458,0.05484784,0.81868947,0.119593106],"study_design_scores_gemma":[0.000011910821,0.000034386016,0.0042305505,0.0005996253,0.00003899044,0.00035839458,0.0015508899,0.0020598758,0.001020105,0.12793851,0.8620811,0.00007556519],"about_ca_topic_score_codex":0.01985378,"about_ca_topic_score_gemma":0.026617682,"teacher_disagreement_score":0.01985378,"about_ca_system_score_codex":0.002167829,"about_ca_system_score_gemma":0.0057491725,"threshold_uncertainty_score":0.043147802},"labels":[],"label_agreement":null},{"id":"W4234474728","doi":"10.5194/npg-2019-19","title":"Magnitude correlations in a self-similar aftershock rates model of seismicity","year":2019,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Society for the Study of Amphibians and Reptiles","keywords":"Aftershock; Magnitude (astronomy); Induced seismicity; Geology; Seismology; Distribution (mathematics); Mathematics; Physics","score_opus":0.029696212366493707,"score_gpt":0.23523973451956012,"score_spread":0.20554352215306643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234474728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81984395,0.0001297094,0.17572388,0.0008446742,0.000045088247,0.000038128823,0.00040723523,0.0002473448,0.0027200032],"genre_scores_gemma":[0.9955258,0.00005851645,0.0026949663,0.000052260624,0.00002087744,0.00001709415,0.00013352002,0.00002568873,0.001471262],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994079,0.00022442028,0.000028540378,0.0001583637,0.00007960469,0.0001011881],"domain_scores_gemma":[0.99317545,0.0035697669,0.0017060753,0.00060215173,0.00055042014,0.00039612906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028635564,0.0004014282,0.0009765141,0.0007983841,0.00030439644,0.0011269033,0.0019516876,0.001204871,0.0021238734],"category_scores_gemma":[0.009772102,0.00048608717,0.0009262705,0.00062843773,0.0016419025,0.0015895889,0.00078179874,0.0011527132,0.00019551654],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015734452,0.00009352212,0.012319687,0.000040959705,0.00011505281,0.00024511735,0.00013311024,0.85434645,0.0027188836,0.12570596,0.00069214427,0.003431747],"study_design_scores_gemma":[0.00001253022,0.00002111437,0.0013640786,0.0000024448302,0.000009627697,0.000016679141,0.000009628404,0.9880685,0.00014414378,0.010279671,0.00006320267,0.000008405446],"about_ca_topic_score_codex":0.0092146145,"about_ca_topic_score_gemma":0.004541108,"teacher_disagreement_score":0.0092146145,"about_ca_system_score_codex":0.0010449084,"about_ca_system_score_gemma":0.0007913184,"threshold_uncertainty_score":0.018321931},"labels":[],"label_agreement":null},{"id":"W4234474908","doi":"10.1007/978-3-319-73568-9_102","title":"Earthquake Magnitude","year":2018,"lang":"en","type":"book-chapter","venue":"Encyclopedia of earth sciences series/Encyclopedia of earth sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Magnitude (astronomy); Earthquake magnitude; Geology; Seismology; Physics; Mathematics; Geometry; Astronomy","score_opus":0.02207567289425352,"score_gpt":0.2327178814708059,"score_spread":0.2106422085765524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234474908","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007131059,0.002500368,0.005280503,0.0007329676,0.001059434,0.000096282056,0.024927957,0.0017737986,0.95649767],"genre_scores_gemma":[0.10321014,0.00863886,0.005450789,0.00046746348,0.0007832868,0.00016893158,0.04855243,0.0006198611,0.83210826],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998223,0.000013339952,0.000012074272,0.00004630117,0.00009160405,0.000014430503],"domain_scores_gemma":[0.999765,0.000031640906,0.000037150425,0.000031118765,0.0000983051,0.000036702695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016863491,0.00065977464,0.0002569861,0.0020254806,0.00027677682,0.0011768731,0.0003846069,0.000240703,0.18286373],"category_scores_gemma":[0.0011071791,0.00013474174,0.0002189841,0.0017608502,0.00017772803,0.0008479163,0.0006026527,0.0004395227,0.10919267],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009744868,0.00004895044,0.006244149,0.00052379776,0.000029001263,0.00006561884,0.00030326052,0.0012872473,0.001941955,0.045418095,0.5481824,0.3958579],"study_design_scores_gemma":[0.000008257481,0.000050218096,0.01488097,0.00009177937,0.000010772271,0.00015575746,0.00014213956,0.00023717289,0.00038499827,0.0067304717,0.977294,0.000013409146],"about_ca_topic_score_codex":0.0017770046,"about_ca_topic_score_gemma":0.0028660533,"teacher_disagreement_score":0.18286373,"about_ca_system_score_codex":0.00037727016,"about_ca_system_score_gemma":0.00034851703,"threshold_uncertainty_score":0.6117401},"labels":[],"label_agreement":null},{"id":"W4234885487","doi":"10.1007/978-3-319-12127-7_168-1","title":"Induced Seismicity","year":2018,"lang":"en","type":"book-chapter","venue":"Techniques in Dentistry and Oral & Maxillofacial Surgery","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Induced seismicity; Geology; Seismology","score_opus":0.042053999961043656,"score_gpt":0.26202554857431715,"score_spread":0.2199715486132735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4234885487","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05258374,0.009112747,0.12673289,0.0016701687,0.0018473361,0.000117981246,0.00045029167,0.0008896983,0.8065952],"genre_scores_gemma":[0.5590545,0.016345523,0.019473672,0.0008649672,0.0010090853,0.00016794848,0.00079562026,0.00028577528,0.40200293],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998363,0.00002254067,0.000005738945,0.000026277976,0.000086639666,0.00002243276],"domain_scores_gemma":[0.9998566,0.000044777622,0.000020573274,0.00003439695,0.000027383056,0.000016128477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014535329,0.00050035707,0.00022101584,0.00052418845,0.00028897042,0.0007325637,0.00051032554,0.0006477037,0.0228403],"category_scores_gemma":[0.00051072164,0.00020270246,0.00025768977,0.00048149456,0.00088302104,0.0005965135,0.0010537881,0.0010209252,0.0036551652],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012663774,0.00010670467,0.00097325933,0.0008679861,0.000044619163,0.0006838174,0.00054473226,0.012622442,0.0635737,0.6038897,0.028027408,0.28853896],"study_design_scores_gemma":[0.000063967505,0.00039537007,0.0061183223,0.00041698388,0.000059384794,0.0031060039,0.00041878544,0.0137343565,0.040889688,0.21909387,0.71563333,0.000069907685],"about_ca_topic_score_codex":0.0001433271,"about_ca_topic_score_gemma":0.0002609424,"teacher_disagreement_score":0.0228403,"about_ca_system_score_codex":0.00039741382,"about_ca_system_score_gemma":0.00035388736,"threshold_uncertainty_score":0.076408386},"labels":[],"label_agreement":null},{"id":"W4235101629","doi":"10.4095/213482","title":"Focal mechanisms for eastern Canadian earthquakes of 2000","year":2002,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Focal mechanism; Geography; Induced seismicity","score_opus":0.051761218904326854,"score_gpt":0.2413056554033246,"score_spread":0.18954443649899774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235101629","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84998757,0.0018539777,0.0011691313,0.00048847665,0.000028120829,0.00021635852,0.10756755,0.00020166698,0.03848711],"genre_scores_gemma":[0.9481442,0.0013935053,0.0014029876,0.000057783098,0.000010512964,0.000061606595,0.037338667,0.000031236043,0.011559481],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995223,0.000010485411,0.000028518942,0.000050738214,0.00020702364,0.00018099093],"domain_scores_gemma":[0.99789196,0.000066912275,0.00034917012,0.000097246455,0.0014164675,0.00017826265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004615621,0.0005183124,0.00023476084,0.005714533,0.0015828339,0.00082268496,0.0009995735,0.00029519878,0.0051947176],"category_scores_gemma":[0.0028633769,0.0002490394,0.00033719995,0.005210435,0.00027554407,0.00042177248,0.0008054099,0.00019817853,0.00043316526],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027803873,0.000049417067,0.86048335,0.00036511137,0.00013798903,0.000619259,0.0019118903,0.0024900867,0.0029037115,0.004057729,0.03258974,0.09411377],"study_design_scores_gemma":[0.000006036368,0.000008404165,0.98951334,0.00002169629,0.000033109438,0.000134044,0.0005743145,0.00050057354,0.0004673971,0.00013345764,0.008591253,0.000016474341],"about_ca_topic_score_codex":0.97586584,"about_ca_topic_score_gemma":0.9898594,"teacher_disagreement_score":0.02413416,"about_ca_system_score_codex":0.013921612,"about_ca_system_score_gemma":0.014432807,"threshold_uncertainty_score":0.10100883},"labels":[],"label_agreement":null},{"id":"W4235485944","doi":"10.5194/se-2020-203","title":"Unprecedented quiescence in resource development area allowsdetection of long-lived latent seismicity","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium; Canadian Natural Resources Limited","keywords":"Induced seismicity; Geology; Seismology; Hydraulic fracturing; Period (music); Geotechnical engineering","score_opus":0.05373079698608971,"score_gpt":0.23388419943484867,"score_spread":0.18015340244875896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235485944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945463,0.00006425138,0.0006591141,0.0000428557,0.0000040151785,0.000007950637,0.0009407346,0.00005458573,0.0036802387],"genre_scores_gemma":[0.9981293,0.000029785488,0.00025067801,0.0000053755875,0.0000025769436,0.0000036578456,0.00077221997,0.0000055272867,0.0008007884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998747,0.0000057945026,0.000003912681,0.00002758351,0.00004505524,0.00004292793],"domain_scores_gemma":[0.9997029,0.000023025703,0.00008528522,0.000024967074,0.00007977046,0.00008409931],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000103625,0.00017932644,0.00012672447,0.00080271787,0.0005258642,0.0006955085,0.00023762825,0.00015552106,0.0021945252],"category_scores_gemma":[0.00037758535,0.000083853745,0.000050569815,0.0012428942,0.000410496,0.00020586525,0.0005138159,0.00028864553,0.0002671864],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022165329,0.000059616563,0.9012615,0.0000692837,0.0000334792,0.0006071936,0.0012987294,0.0010675087,0.058367755,0.0005855128,0.001797193,0.034630522],"study_design_scores_gemma":[0.000002019668,0.000010947207,0.9963123,0.0000041558797,0.0000036879003,0.00005787345,0.0003892895,0.0007029339,0.0012163725,0.00004525395,0.001251523,0.0000037305217],"about_ca_topic_score_codex":0.23083295,"about_ca_topic_score_gemma":0.46045673,"teacher_disagreement_score":0.23083295,"about_ca_system_score_codex":0.001064058,"about_ca_system_score_gemma":0.0010482316,"threshold_uncertainty_score":0.45897865},"labels":[],"label_agreement":null},{"id":"W4235670847","doi":"10.1007/978-3-7643-8757-0_14","title":"The Stress Accumulation Method and the Pattern Informatics Index: Complementary Approaches to Earthquake Forecasting","year":2008,"lang":"en","type":"book-chapter","venue":"Birkhäuser Basel eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Index (typography); Informatics; Anomaly (physics); Resolution (logic); Computer science; Data mining; Joint (building); Artificial intelligence; Engineering; Physics","score_opus":0.19039534064080404,"score_gpt":0.25826635807842174,"score_spread":0.0678710174376177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235670847","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.014648996,0.0021274432,0.9669252,0.00053280476,0.00013869145,0.000058471996,0.00029462774,0.0006720667,0.014601685],"genre_scores_gemma":[0.19281426,0.0028088558,0.79816735,0.000111013185,0.0004801309,0.00013496801,0.0004814303,0.00025716817,0.00474473],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991709,0.00025292052,0.000051254174,0.000098518765,0.00040018352,0.00002627567],"domain_scores_gemma":[0.9967974,0.0022175177,0.00025760417,0.00027957465,0.00038114857,0.000066726025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001785417,0.0008716468,0.000671882,0.004071178,0.0002511389,0.002101676,0.0009989233,0.0004721579,0.00290987],"category_scores_gemma":[0.0063324072,0.00033861044,0.0005345637,0.0059738057,0.0007230833,0.0028521018,0.000987759,0.001061354,0.00075301836],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050592094,0.000045259294,0.0072527085,0.00018921508,0.000068477675,0.000078105804,0.00024515105,0.025800413,0.0019151852,0.063797906,0.0031955284,0.8973615],"study_design_scores_gemma":[0.000034831886,0.0002210915,0.02201613,0.00018551767,0.000092470145,0.00057117065,0.0004302072,0.7707751,0.005550813,0.14854395,0.051455844,0.00012292375],"about_ca_topic_score_codex":0.0015387514,"about_ca_topic_score_gemma":0.0025233594,"teacher_disagreement_score":0.004071178,"about_ca_system_score_codex":0.00040615452,"about_ca_system_score_gemma":0.0005465447,"threshold_uncertainty_score":0.009734452},"labels":[],"label_agreement":null},{"id":"W4235678604","doi":"10.1190/tle31121428.1","title":"Introduction to this special section: Passive seismic and microseismic—Part 2","year":2012,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Calgary Laboratory Services; University of Calgary","funders":"U.S. Department of Energy","keywords":"Microseism; Induced seismicity; Special section; Hydraulic fracturing; Geology; Seismology; Section (typography); Passive seismic; Geotechnical engineering; Engineering; Engineering physics; Computer science","score_opus":0.016570786862612884,"score_gpt":0.21933661514367414,"score_spread":0.20276582828106127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235678604","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0011975575,0.03779111,0.014909453,0.03591728,0.8239242,0.00032382793,0.00064786,0.00075099274,0.08453781],"genre_scores_gemma":[0.0062819095,0.041147713,0.0064948257,0.028488107,0.6123307,0.00030812694,0.0013019298,0.00097050297,0.30267623],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990422,0.00013613181,0.0001188904,0.00016873995,0.0004350437,0.00009895918],"domain_scores_gemma":[0.9951617,0.0011967304,0.00032253875,0.00030543297,0.0020783707,0.00093526597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001817636,0.0018124293,0.0014613945,0.0031864434,0.0013406159,0.0034557874,0.0016105422,0.0040804204,0.062138837],"category_scores_gemma":[0.0040931925,0.00066772953,0.0012850539,0.0012886174,0.0011120914,0.0034058013,0.0027627058,0.0055626635,0.040098615],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046430494,0.0000768845,0.00029730212,0.00031675366,0.000010679818,0.00018892916,0.00004581636,0.00022272042,0.001557896,0.0020476663,0.9171217,0.07806728],"study_design_scores_gemma":[0.000004012192,0.000060409533,0.00080931187,0.00014839324,0.0000045375295,0.00036610547,0.000046181613,0.00012240733,0.00016701079,0.0013157825,0.99694294,0.00001283304],"about_ca_topic_score_codex":0.0010312333,"about_ca_topic_score_gemma":0.0023731976,"teacher_disagreement_score":0.062138837,"about_ca_system_score_codex":0.00093833817,"about_ca_system_score_gemma":0.0011007498,"threshold_uncertainty_score":0.20787513},"labels":[],"label_agreement":null},{"id":"W4235721834","doi":"10.1007/978-3-319-73568-9_168","title":"Induced Seismicity","year":2018,"lang":"en","type":"book-chapter","venue":"Encyclopedia of earth sciences series/Encyclopedia of earth sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Induced seismicity; Geology; Seismology; Environmental science","score_opus":0.02824948513057521,"score_gpt":0.23703250110726737,"score_spread":0.20878301597669216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235721834","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.02593412,0.0067879697,0.040019304,0.0014441042,0.001407095,0.00010592567,0.0015457527,0.0015687522,0.921187],"genre_scores_gemma":[0.3615938,0.017884916,0.009206628,0.0008220139,0.0010720392,0.00016809032,0.0031029317,0.00037945758,0.6057702],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.999841,0.00001662097,0.000007381646,0.000029729457,0.000084050385,0.000021210708],"domain_scores_gemma":[0.9998161,0.00004248419,0.000030069545,0.000043502874,0.000041299005,0.000026519989],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015830439,0.0005256177,0.00020668165,0.0007305796,0.00020799751,0.00086616585,0.0005131141,0.00052644144,0.04920268],"category_scores_gemma":[0.00067713874,0.00017238638,0.00028406558,0.0005629644,0.00048004114,0.0007154578,0.0010029357,0.0008203158,0.011914864],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016158447,0.00016720315,0.0021498578,0.0012080272,0.000058206864,0.0006423336,0.00034316763,0.008520313,0.044779863,0.36442208,0.10641329,0.47113413],"study_design_scores_gemma":[0.00004088635,0.00026350637,0.0069161872,0.00029899544,0.000046148227,0.0018069976,0.00015982788,0.0054305526,0.02238328,0.07310814,0.8895034,0.000042145217],"about_ca_topic_score_codex":0.00022489102,"about_ca_topic_score_gemma":0.0004357209,"teacher_disagreement_score":0.04920268,"about_ca_system_score_codex":0.00046268516,"about_ca_system_score_gemma":0.00046825662,"threshold_uncertainty_score":0.16459936},"labels":[],"label_agreement":null},{"id":"W4235875550","doi":"10.1139/cgj-37-4-796","title":"Analysis of self-boring pressuremeter (SBPM) and Marchetti dilatometer (DMT) tests in granite saprolites","year":2000,"lang":"en","type":"article","venue":"Canadian Geotechnical Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Dilatometer; Geotechnical engineering; Geology; Materials science","score_opus":0.014136476739203072,"score_gpt":0.2158566729916774,"score_spread":0.20172019625247434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235875550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981914,0.000026417922,0.0004666446,0.0000069916596,0.000003305459,0.00000568651,0.00026524722,0.000044634122,0.0009895609],"genre_scores_gemma":[0.9990395,0.000012438457,0.0001882391,0.000004184419,0.000001431299,0.0000036576423,0.00020287241,0.000009977458,0.0005377363],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99959856,0.00003507555,0.000028358654,0.00008896379,0.00017635507,0.000072676914],"domain_scores_gemma":[0.9988918,0.00030176487,0.0001812646,0.000053896845,0.00044769264,0.00012366749],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027250798,0.0004689857,0.00028633408,0.0015136832,0.00040481013,0.0004340475,0.0005298099,0.00046685207,0.0012091773],"category_scores_gemma":[0.0011299939,0.0002417437,0.00028290527,0.0009353506,0.00050223834,0.00026085734,0.00034971003,0.0002730263,0.00047843566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002673803,0.00033970142,0.52962214,0.00015902464,0.0000800841,0.0011045984,0.0014469661,0.004465044,0.42353335,0.0002447598,0.0005658808,0.035764657],"study_design_scores_gemma":[0.000013211689,0.0007409757,0.9191851,0.0000064689234,0.00004561009,0.00034182688,0.00065829564,0.0055437805,0.07261382,0.00007345216,0.00075530814,0.000022159391],"about_ca_topic_score_codex":0.015114238,"about_ca_topic_score_gemma":0.017941628,"teacher_disagreement_score":0.015114238,"about_ca_system_score_codex":0.0005030504,"about_ca_system_score_gemma":0.00036978172,"threshold_uncertainty_score":0.030052543},"labels":[],"label_agreement":null},{"id":"W4235922287","doi":"10.4095/301263","title":"Major Tornadoes","year":2010,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tornado; Environmental science; Geography; Meteorology","score_opus":0.02946898737008857,"score_gpt":0.2489525526034942,"score_spread":0.21948356523340562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4235922287","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43367815,0.0069717495,0.0023207506,0.001768773,0.0012619105,0.0023010175,0.08966378,0.0024168666,0.45961696],"genre_scores_gemma":[0.7839306,0.01076648,0.0017704677,0.0008853085,0.00036717596,0.0003534424,0.046980478,0.00022304812,0.15472306],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9994973,0.000015280963,0.000027904027,0.000049169365,0.00016343244,0.0002469124],"domain_scores_gemma":[0.99906594,0.000022651751,0.00021212034,0.000056591503,0.0003508524,0.00029182405],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017048024,0.0011499894,0.00040017234,0.0015828273,0.0019435791,0.0011113468,0.0006430727,0.00036507924,0.020858238],"category_scores_gemma":[0.0010331764,0.00016780324,0.00032354626,0.00193538,0.00052786793,0.0005463108,0.0014673895,0.00058578304,0.0034368918],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058047526,0.00039293407,0.2671225,0.0020013642,0.0001918038,0.004288091,0.0070881546,0.0015832947,0.0045641246,0.009054992,0.39584094,0.3072914],"study_design_scores_gemma":[0.000030555766,0.00016586027,0.54202455,0.00050985854,0.000043453234,0.002501416,0.0060166013,0.00017658343,0.0011588115,0.00049482717,0.44682994,0.000047518763],"about_ca_topic_score_codex":0.15438676,"about_ca_topic_score_gemma":0.27733648,"teacher_disagreement_score":0.15438676,"about_ca_system_score_codex":0.0023927938,"about_ca_system_score_gemma":0.003799389,"threshold_uncertainty_score":0.30697626},"labels":[],"label_agreement":null},{"id":"W4236439260","doi":"10.1007/978-3-7643-9964-1_7","title":"Postseismic Deformation Following the 1994 Northridge Earthquake Identified Using the Localized Hartley Transform Filter","year":2008,"lang":"en","type":"book-chapter","venue":"Birkhäuser Basel eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Princess Margaret Cancer Centre; Western University","funders":"","keywords":"Superposition principle; Deformation (meteorology); Filter (signal processing); Global Positioning System; Relaxation (psychology); Geodesy; Spatial filter; Viscoelasticity; SIGNAL (programming language); Geology; Seismology; Computer science; Geography; Meteorology; Physics; Telecommunications; Artificial intelligence; Computer vision","score_opus":0.03733947007362907,"score_gpt":0.2204634204744105,"score_spread":0.18312395040078144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4236439260","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.67491406,0.0013512871,0.30487454,0.00022125081,0.00007085074,0.000027924947,0.00093241304,0.00085267867,0.016755031],"genre_scores_gemma":[0.8972991,0.0013237123,0.08389608,0.000053423573,0.000064004555,0.000018579694,0.0012565022,0.000071409806,0.016017104],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99995995,0.0000035970083,0.0000019662893,0.000013197121,0.000017449314,0.0000039655224],"domain_scores_gemma":[0.9999187,0.000031896892,0.000021298732,0.0000091395195,0.000015301319,0.000003628882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001142134,0.00017535823,0.000147151,0.0004299806,0.00009020303,0.00038651266,0.00020677154,0.00021739306,0.0015148218],"category_scores_gemma":[0.00030236252,0.00007673655,0.00011962481,0.00069998566,0.00016102707,0.0003669952,0.00011568888,0.00012651233,0.00044747046],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014459428,0.0000507791,0.025998406,0.00016328241,0.000056948425,0.0004114365,0.00039089072,0.05828036,0.06488752,0.006599191,0.0054632267,0.83755344],"study_design_scores_gemma":[0.000038776077,0.0003492647,0.4287654,0.0000588786,0.00012885263,0.00064296863,0.00046130872,0.47139958,0.055841297,0.008270368,0.033954915,0.00008849688],"about_ca_topic_score_codex":0.008954997,"about_ca_topic_score_gemma":0.01861569,"teacher_disagreement_score":0.008954997,"about_ca_system_score_codex":0.00032693005,"about_ca_system_score_gemma":0.00022497037,"threshold_uncertainty_score":0.017805755},"labels":[],"label_agreement":null},{"id":"W4237201843","doi":"10.1002/essoar.10503731.1","title":"Statistical Modeling and Characterization of Induced Seismicity within the Western Canada Sedimentary Basin","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Induced seismicity; Aftershock; Seismology; Geology; Tectonics; Structural basin; Magnitude (astronomy); Maximum magnitude; Sedimentary rock; Paleontology","score_opus":0.032630929964655685,"score_gpt":0.21983278836351974,"score_spread":0.18720185839886405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237201843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99508387,0.00004535225,0.003525668,0.0000564102,0.0000023321115,0.000020874186,0.0006351391,0.000038221027,0.0005920478],"genre_scores_gemma":[0.9971405,0.00005825222,0.0010430004,0.0000061353608,0.000002315601,0.000010289828,0.001094316,0.0000066489997,0.00063858955],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99971026,0.00003628951,0.000018438466,0.00007591248,0.00007558545,0.00008354109],"domain_scores_gemma":[0.99908495,0.00032377016,0.00014315663,0.00006637154,0.00029257004,0.00008912489],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004989887,0.00025488707,0.00024506927,0.001168714,0.0005442916,0.000740247,0.0007434258,0.00021222908,0.0007272842],"category_scores_gemma":[0.0026631812,0.00016967475,0.0003948012,0.0012922242,0.00064945366,0.00021100555,0.00037662388,0.0003216039,0.000074833384],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013508023,0.000067597684,0.5375197,0.000037266425,0.00019399218,0.00035434533,0.00046506978,0.4313826,0.002499442,0.0031911922,0.0010004311,0.023153232],"study_design_scores_gemma":[0.0000066923453,0.00002438617,0.36582068,0.000006445038,0.000032750024,0.000035369638,0.0004453534,0.63177687,0.00040562882,0.000590667,0.0008344485,0.000020764795],"about_ca_topic_score_codex":0.9385667,"about_ca_topic_score_gemma":0.9041769,"teacher_disagreement_score":0.061433315,"about_ca_system_score_codex":0.005209902,"about_ca_system_score_gemma":0.0057491125,"threshold_uncertainty_score":0.12359017},"labels":[],"label_agreement":null},{"id":"W4237246515","doi":"10.1002/essoar.10504243.1","title":"Seismicity and the State of Stress in the Dezful Embayment, Zagros Fold and Thrust Belt","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Seismology; Induced seismicity; Borehole; Thrust fault; Focal mechanism; Strike-slip tectonics; Fault (geology); Stress field; Petrology; Geotechnical engineering","score_opus":0.02413291785571523,"score_gpt":0.22450785640687973,"score_spread":0.2003749385511645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237246515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99980646,0.000020300542,0.000015934504,0.000007183702,3.0893875e-7,5.1743865e-7,0.00005484529,8.0527457e-7,0.00009355738],"genre_scores_gemma":[0.99968576,0.000026336962,0.000045362984,0.000002680934,0.0000014054787,9.685634e-7,0.00017461117,3.1185252e-7,0.000062603125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998777,0.000013595796,0.000015019812,0.000029996496,0.000023134642,0.000040559058],"domain_scores_gemma":[0.99975854,0.000027465365,0.00014202291,0.000014560048,0.000031313022,0.000026040887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024901755,0.00022029044,0.00018202784,0.0013462451,0.00022386029,0.00049969816,0.00017378376,0.00021045319,0.00039475432],"category_scores_gemma":[0.00055619306,0.00012849443,0.0001399883,0.0011368878,0.0003359224,0.00032149232,0.0002371276,0.00013929112,0.0001134896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089474306,0.0000215957,0.99242896,0.000007869997,0.00002955458,0.00011006462,0.00035690554,0.0003638824,0.0017667592,0.00006704589,0.00004370067,0.0047141733],"study_design_scores_gemma":[0.0000015296721,0.0000116267765,0.99954814,0.0000014491543,0.0000028995069,0.000021190166,0.00015226133,0.00014477645,0.000048840837,0.000008494116,0.000057660363,0.000001108826],"about_ca_topic_score_codex":0.029582541,"about_ca_topic_score_gemma":0.051889416,"teacher_disagreement_score":0.029582541,"about_ca_system_score_codex":0.0008148918,"about_ca_system_score_gemma":0.0002349964,"threshold_uncertainty_score":0.058820665},"labels":[],"label_agreement":null},{"id":"W4237351315","doi":"10.5194/se-2020-48","title":"On morphology and amplitude of 2D and 3D thermal anomalies induced by buoyancy-driven flow within and around fault zones","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"Bureau de Recherches Géologiques et Minières; Agence Nationale de la Recherche","keywords":"Buoyancy; Geology; Geothermal gradient; Petrology; Fault (geology); Thermal; Amplitude; Convection; Fluid dynamics; Permeability (electromagnetism); Hydrothermal circulation; Geophysics; Mechanics; Seismology; Meteorology","score_opus":0.027184382514123563,"score_gpt":0.23253044899549707,"score_spread":0.20534606648137352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237351315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910216,0.00012531053,0.0063670296,0.00008251867,0.000018945277,0.00001388049,0.00047376906,0.00023554282,0.0016615402],"genre_scores_gemma":[0.9987219,0.00004645887,0.0008095921,0.000006622905,0.0000036299384,0.000005862764,0.00019216216,0.000014494769,0.00019934156],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991786,0.000015797445,0.0000061219907,0.00002054953,0.000019812318,0.000019949588],"domain_scores_gemma":[0.9997615,0.00007789416,0.00005765837,0.000026265114,0.000034150347,0.000042377716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097019605,0.00038873532,0.0003254532,0.00056382094,0.0002098777,0.0007249069,0.00031009773,0.00050196337,0.0016272996],"category_scores_gemma":[0.0005954388,0.00021052986,0.0005261999,0.00035875593,0.0005066692,0.00034883365,0.00034324225,0.00031535243,0.000117659525],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012247273,0.00008527735,0.016201962,0.00008225104,0.00005846924,0.0003425846,0.000116412564,0.9544002,0.02199643,0.0011572759,0.00037261064,0.0050641126],"study_design_scores_gemma":[0.000014175994,0.000035010147,0.012431996,0.000006310321,0.000012600661,0.000051197396,0.000037849077,0.98534364,0.0015561936,0.00027154258,0.00022284908,0.000016592281],"about_ca_topic_score_codex":0.0049453056,"about_ca_topic_score_gemma":0.002404271,"teacher_disagreement_score":0.0049453056,"about_ca_system_score_codex":0.0004018716,"about_ca_system_score_gemma":0.0002815937,"threshold_uncertainty_score":0.009833038},"labels":[],"label_agreement":null},{"id":"W4237449230","doi":"10.5194/sed-5-2483-2013","title":"Lithosphere and upper-mantle structure of the southern Baltic Sea estimated from modelling relative sea-level data with glacial isostatic adjustment","year":2013,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ","keywords":"Geology; Post-glacial rebound; Lithosphere; Deglaciation; Mantle (geology); Ice sheet; Glacial period; Graben; Isostasy; Geophysics; Geomorphology; Seismology; Tectonics","score_opus":0.05258176048854654,"score_gpt":0.23813060015900286,"score_spread":0.18554883967045632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237449230","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926966,0.000026652637,0.00027662853,0.000008677941,0.0000015487043,0.0000015367459,0.00019917908,0.00002222335,0.00019394912],"genre_scores_gemma":[0.9991198,0.000023143311,0.0002256467,0.0000027474832,0.0000011708561,0.0000032417536,0.00050797797,0.000005384377,0.00011078173],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999459,0.000014310159,0.0000044818344,0.000016886319,0.000006755368,0.000011614544],"domain_scores_gemma":[0.99987495,0.00004291599,0.000024797257,0.000017651446,0.000022908225,0.00001673529],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021545007,0.00045077535,0.00020101566,0.00056390534,0.00023126068,0.0006390093,0.00039574943,0.00047729939,0.00078693783],"category_scores_gemma":[0.0006516998,0.000303324,0.0006183588,0.000570447,0.00023370626,0.00038279154,0.0002403205,0.00019550405,0.00016673177],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018491878,0.00008066432,0.3281753,0.000052891573,0.00030925055,0.0002540115,0.00019607274,0.656006,0.0051848455,0.00027822237,0.0002963883,0.008981558],"study_design_scores_gemma":[0.000055895558,0.000095401636,0.310316,0.000026195446,0.00010981247,0.00005874224,0.00019775804,0.68689746,0.0012094617,0.00023372321,0.00077047537,0.000029037505],"about_ca_topic_score_codex":0.047746614,"about_ca_topic_score_gemma":0.032935176,"teacher_disagreement_score":0.047746614,"about_ca_system_score_codex":0.00053558423,"about_ca_system_score_gemma":0.0003843888,"threshold_uncertainty_score":0.094937384},"labels":[],"label_agreement":null},{"id":"W4237855318","doi":"10.1007/978-3-662-44185-5_100667","title":"Magmatic Rock","year":2015,"lang":"en","type":"book-chapter","venue":"Encyclopedia of Astrobiology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Geochemistry","score_opus":0.019992189478229044,"score_gpt":0.2149684058726776,"score_spread":0.19497621639444856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237855318","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010327018,0.01002933,0.004324017,0.0007336551,0.0008243371,0.000023435143,0.0005725437,0.0004443171,0.9820155],"genre_scores_gemma":[0.011417286,0.006151644,0.002202085,0.00025040645,0.00034651358,0.000016542845,0.00063281093,0.00017907281,0.9788036],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99993837,0.000004390079,0.0000023812518,0.000018275887,0.000030881838,0.0000056740487],"domain_scores_gemma":[0.999972,0.0000035042287,0.00000230005,0.0000093607905,0.000007900887,0.00000507017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000090219284,0.0004990522,0.00024235573,0.0010521354,0.0005094711,0.0013341454,0.00050453405,0.0004589389,0.10756478],"category_scores_gemma":[0.00021987307,0.00013464567,0.00016004586,0.00062100386,0.0005555747,0.001204205,0.0009166748,0.0007086918,0.051589165],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002372425,0.000015222419,0.00016347594,0.00021633222,0.0000059500585,0.000060842533,0.0002743118,0.00031432463,0.0025565478,0.26039264,0.24792683,0.4880498],"study_design_scores_gemma":[8.093869e-7,0.0000027967624,0.000121118814,0.000021946462,9.441967e-7,0.000050617306,0.000013990388,0.000030794017,0.00019502886,0.0054643364,0.9940964,0.0000011111063],"about_ca_topic_score_codex":0.0016880279,"about_ca_topic_score_gemma":0.0048956885,"teacher_disagreement_score":0.10756478,"about_ca_system_score_codex":0.00044357183,"about_ca_system_score_gemma":0.00044354517,"threshold_uncertainty_score":0.35984004},"labels":[],"label_agreement":null},{"id":"W4237971251","doi":"10.1002/essoar.10506205.1","title":"The Crustal Stress Field of Northern Chile","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; University of Calgary; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"World Wide Web; Electronic mail; Computer science","score_opus":0.013951410422572258,"score_gpt":0.2233614257654523,"score_spread":0.20941001534288003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4237971251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99466854,0.0002814951,0.000101899255,0.00006716227,0.0000022367853,0.000007150153,0.0011192532,0.000029297711,0.003722835],"genre_scores_gemma":[0.9983853,0.00018786089,0.00009386772,0.000008226747,0.000002613825,0.000008252103,0.00068298297,0.000005484215,0.0006253967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999554,0.000004557234,0.0000035715946,0.000016163272,0.000008720487,0.000011553551],"domain_scores_gemma":[0.9998287,0.000021220727,0.000054078442,0.000014954702,0.000047177145,0.00003373029],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009400657,0.0001680253,0.00016256906,0.0009516439,0.000291725,0.0005755737,0.00020354553,0.00014408802,0.0025314076],"category_scores_gemma":[0.00056665315,0.00013667578,0.00014315403,0.00111724,0.00025220835,0.0002672478,0.00057211507,0.0001181781,0.00028150482],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020094376,0.000050232633,0.92156136,0.00031778764,0.00013457907,0.00087495096,0.0025754366,0.006146229,0.027516095,0.00074154575,0.0021040458,0.037776936],"study_design_scores_gemma":[0.000009567192,0.000008459524,0.99592006,0.000023660246,0.000012058327,0.000068211826,0.00078187865,0.001153292,0.0003060513,0.0001709222,0.0015371025,0.000008661986],"about_ca_topic_score_codex":0.07154907,"about_ca_topic_score_gemma":0.058149423,"teacher_disagreement_score":0.07154907,"about_ca_system_score_codex":0.00093226245,"about_ca_system_score_gemma":0.0006784348,"threshold_uncertainty_score":0.1422652},"labels":[],"label_agreement":null},{"id":"W4238377552","doi":"10.31223/osf.io/ks6rg","title":"Monoclinal flexure of an orogenic plateau margin during subduction, south Turkey","year":2018,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"European Social Fund; Natural Sciences and Engineering Research Council of Canada; Nederlandse Organisatie voor Wetenschappelijk Onderzoek","keywords":"Geology; Forearc; Outcrop; Plateau (mathematics); Subduction; Monocline; Paleontology; Seismology; Continental margin; Syncline; Geomorphology; Escarpment; Submarine pipeline; Sedimentary rock; Tectonics","score_opus":0.024189763005581535,"score_gpt":0.23354996443605724,"score_spread":0.2093602014304757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4238377552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994247,0.00004629503,0.000024934005,0.0000060963657,8.268162e-7,0.0000012643756,0.00004977505,0.0000026287491,0.0004435628],"genre_scores_gemma":[0.99972945,0.00002738929,0.00003182062,0.0000016079136,9.2321767e-7,0.0000011321223,0.00010320367,9.752591e-7,0.00010348633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.000005202837,0.0000067873125,0.000021930746,0.000009776378,0.000015359088],"domain_scores_gemma":[0.9999198,0.000006620012,0.000032331263,0.0000068191675,0.000022624869,0.00001182116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011308407,0.0001656632,0.00011442575,0.0006780796,0.0002736859,0.00038818098,0.0001736491,0.00016519203,0.0006433673],"category_scores_gemma":[0.0001909484,0.0001021548,0.000097331416,0.00062300346,0.000267002,0.00021280801,0.00028686365,0.000083723666,0.00011640417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016053427,0.000021718659,0.96984005,0.000044357006,0.000027274107,0.00082652154,0.0016423564,0.0008211672,0.011858484,0.00014818461,0.00018597595,0.014423277],"study_design_scores_gemma":[0.0000013863846,0.000014346249,0.99867094,0.000005772115,0.000004645647,0.00012014717,0.0004368415,0.00030220035,0.00020080361,0.00001492299,0.00022640907,0.0000016640726],"about_ca_topic_score_codex":0.013925886,"about_ca_topic_score_gemma":0.02908865,"teacher_disagreement_score":0.013925886,"about_ca_system_score_codex":0.00036931437,"about_ca_system_score_gemma":0.0002641915,"threshold_uncertainty_score":0.027689636},"labels":[],"label_agreement":null},{"id":"W4238663155","doi":"10.22215/etd/2006-08510","title":"Finite fault stochastic modeling of the 1999 Chi-Chi Taiwan earthquake","year":2006,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; Canadian Heritage; Library and Archives Canada","funders":"","keywords":"Fault (geology); Humanities; Computer science; Seismology; Geology; Philosophy","score_opus":0.015367188943931713,"score_gpt":0.2200636358030762,"score_spread":0.20469644685914448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4238663155","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9626522,0.00039274644,0.027986567,0.0017516991,0.000063101026,0.00001680584,0.0011619467,0.00014681798,0.0058280346],"genre_scores_gemma":[0.9967842,0.0001075457,0.0005627991,0.000026980177,0.000019597688,0.000008456301,0.00024811787,0.000017650684,0.0022246987],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998727,0.000046686742,0.0000072665266,0.000025116697,0.000013323765,0.00003486084],"domain_scores_gemma":[0.998781,0.0007134583,0.00023133667,0.00005758628,0.00011227335,0.00010428891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060258695,0.0003664865,0.0004709577,0.00045343762,0.0003268378,0.0008506597,0.0010549417,0.0011542053,0.002177615],"category_scores_gemma":[0.0032682803,0.00040553883,0.00043135305,0.0004339555,0.0006313746,0.0008206278,0.00049986655,0.00084690383,0.00016693142],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020242545,0.000009962118,0.0019638494,0.0000059828285,0.000011272315,0.000041012994,0.000014607534,0.99346876,0.00009945578,0.0035402158,0.0002505328,0.00057412236],"study_design_scores_gemma":[0.0000029134935,0.000005425641,0.000571093,0.0000015695848,0.0000026937419,0.0000030275376,0.0000082713395,0.99851245,0.0000222121,0.0008115328,0.000056150355,0.0000026288458],"about_ca_topic_score_codex":0.09264782,"about_ca_topic_score_gemma":0.053198934,"teacher_disagreement_score":0.09264782,"about_ca_system_score_codex":0.0016747342,"about_ca_system_score_gemma":0.00096059544,"threshold_uncertainty_score":0.1842171},"labels":[],"label_agreement":null},{"id":"W4239159752","doi":"10.1130/geol.s.12275744.v1","title":"Supplemental Material: Uplift and exhumation in Haida Gwaii driven by terrane translation and transpression along the southern Queen Charlotte fault, Canada","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Transpression; Terrane; Geology; Seismology; Fault (geology); Queen (butterfly); Archaeology; History; Tectonics; Sinistral and dextral","score_opus":0.01834781526257785,"score_gpt":0.21193338867579362,"score_spread":0.19358557341321578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239159752","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0059983567,0.00005857838,0.0006474313,0.00022135348,0.00024573202,0.00004217721,0.9823309,0.0013497655,0.009105614],"genre_scores_gemma":[0.06895475,0.0004118708,0.0049039195,0.00020440696,0.0001718145,0.00011856766,0.89648825,0.0016675439,0.0270788],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9997863,0.000005064111,0.00001353546,0.000033813856,0.00009689594,0.000064335814],"domain_scores_gemma":[0.9990029,0.00013769457,0.0000536163,0.000053018695,0.00062259973,0.00013027687],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00021381355,0.0007063679,0.0007756371,0.0022717102,0.001784089,0.0013756296,0.0016185212,0.000745686,0.45266804],"category_scores_gemma":[0.0013784007,0.00047820495,0.0007067968,0.005206544,0.00020725651,0.0005404709,0.00051751063,0.0005487407,0.050222415],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014238193,0.000109882254,0.014274265,0.00042072556,0.000069032016,0.00024290395,0.00015849671,0.0049950387,0.0014870466,0.00082619087,0.9641445,0.013129518],"study_design_scores_gemma":[0.0005757314,0.00006224553,0.41673657,0.0008176183,0.00017194593,0.00049713935,0.001155738,0.021749709,0.002070531,0.003945924,0.5520427,0.00017410306],"about_ca_topic_score_codex":0.7538882,"about_ca_topic_score_gemma":0.8637338,"teacher_disagreement_score":0.45266804,"about_ca_system_score_codex":0.0029106725,"about_ca_system_score_gemma":0.0054422244,"threshold_uncertainty_score":0.7807026},"labels":[],"label_agreement":null},{"id":"W4239211646","doi":"10.1002/essoar.10503605.2","title":"Detailed nucleation process and mechanism of the July 2019 Mw 6.4 Ridgecrest, California earthquake","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Preprint; Beijing; Space Science; Library science; World Wide Web; Computer science; Physics; History; China; Archaeology; Astronomy","score_opus":0.012846690105410074,"score_gpt":0.21389110096306688,"score_spread":0.2010444108576568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239211646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977558,0.00014430683,0.0005136165,0.000019477613,0.0000053368713,0.000015466478,0.00086444756,0.00004545838,0.0006361429],"genre_scores_gemma":[0.99668914,0.00013258406,0.00066449225,0.0000055988708,0.000011240684,0.000009491494,0.002129989,0.000006272705,0.00035112753],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991524,0.0000034262393,0.0000063765096,0.000024981813,0.00002635796,0.000023717223],"domain_scores_gemma":[0.999705,0.000022620978,0.00014271561,0.000025131772,0.00006358844,0.000040843068],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016451502,0.00022872705,0.00022197783,0.0011383682,0.0004355527,0.00033403328,0.00023259723,0.00019183384,0.0005556878],"category_scores_gemma":[0.00042388638,0.00019249199,0.000189127,0.000695258,0.0001638214,0.00032802369,0.0003199894,0.00017592666,0.00015635343],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019432539,0.00006590851,0.94349664,0.000086825676,0.000054832384,0.0008873965,0.00052405254,0.0053906124,0.02500836,0.00025529804,0.0015992709,0.02243648],"study_design_scores_gemma":[0.0000062437266,0.000022073787,0.9934453,0.0000074126506,0.000016195088,0.00006425747,0.00011036115,0.003938485,0.0016072989,0.00003422571,0.00073874986,0.000009500112],"about_ca_topic_score_codex":0.029504124,"about_ca_topic_score_gemma":0.061820168,"teacher_disagreement_score":0.029504124,"about_ca_system_score_codex":0.00036684895,"about_ca_system_score_gemma":0.00042119029,"threshold_uncertainty_score":0.0586648},"labels":[],"label_agreement":null},{"id":"W4239498192","doi":"10.1186/bf03352379","title":"Preface","year":2014,"lang":"en","type":"article","venue":"Earth Planets and Space","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Computer science","score_opus":0.009880675305384648,"score_gpt":0.1866830782514112,"score_spread":0.17680240294602656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239498192","genre_codex":"other","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00078007096,0.010957882,0.0025912395,0.03841059,0.31113884,0.0004712578,0.010060577,0.0022794504,0.62331015],"genre_scores_gemma":[0.002128152,0.005691635,0.00096695573,0.008364834,0.05253862,0.00019454228,0.008439373,0.0010494263,0.9206265],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99896026,0.00011373285,0.00008731767,0.00020927413,0.000519125,0.00011035019],"domain_scores_gemma":[0.99608266,0.0005712004,0.00016644406,0.00038054617,0.0019534337,0.0008456049],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013368414,0.0012915265,0.0011338476,0.0020507474,0.0016953051,0.0059214258,0.0017213419,0.0020475092,0.6626914],"category_scores_gemma":[0.007244688,0.00038857124,0.0007155976,0.0017321298,0.0005094623,0.004129879,0.00268051,0.0028151218,0.5413899],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011444357,0.000009213232,0.000034815137,0.000068962116,0.0000012231471,0.000017825061,0.000019521645,0.000013209472,0.00006105231,0.00074638077,0.97611415,0.022902116],"study_design_scores_gemma":[0.0000029669425,0.000007852911,0.00014481942,0.0000547184,0.0000011007251,0.000028137487,0.00003061011,0.000012284014,0.00002632209,0.00041509527,0.9992737,0.000002385777],"about_ca_topic_score_codex":0.0013553372,"about_ca_topic_score_gemma":0.0017514603,"teacher_disagreement_score":0.6626914,"about_ca_system_score_codex":0.0012631202,"about_ca_system_score_gemma":0.0018622678,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4239499996","doi":"10.1007/978-3-030-05451-9_172","title":"Sudbury, Canada","year":2019,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Proterozoic; Archean; Geology; Archaeology; Situated; Geochemistry; Geography; Paleontology; Tectonics","score_opus":0.014779054211331891,"score_gpt":0.17482612780746182,"score_spread":0.16004707359612994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239499996","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010650015,0.004955322,0.000517322,0.00083710917,0.00044783382,0.000041787294,0.0027454402,0.000154098,0.98923606],"genre_scores_gemma":[0.0012777636,0.0012077254,0.00025439478,0.000083122315,0.000009329552,0.000008314859,0.0003885292,0.000066365064,0.9967044],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99946684,0.000023743307,0.0000132452205,0.00013260519,0.00022263026,0.0001408693],"domain_scores_gemma":[0.9993217,0.00007630023,0.00002194408,0.00004598472,0.00043770747,0.0000964759],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00025517083,0.0013796372,0.0007250189,0.0018412197,0.0057405196,0.0055152103,0.0011884238,0.0011004254,0.51933366],"category_scores_gemma":[0.0010523013,0.00060234923,0.0004084724,0.0036561587,0.0008331529,0.0014393999,0.0016307473,0.0017398703,0.18842325],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000065311695,0.000033656022,0.0009310819,0.00027704355,0.000012916871,0.00041708478,0.00039139832,0.00053947046,0.0007630038,0.038123168,0.7048437,0.25360212],"study_design_scores_gemma":[0.0000036988724,0.0000035729329,0.00066001323,0.00008634212,0.0000033343313,0.000046688867,0.00017738604,0.00007438813,0.00017057618,0.00080109853,0.99796706,0.0000057581096],"about_ca_topic_score_codex":0.8147373,"about_ca_topic_score_gemma":0.9590944,"teacher_disagreement_score":0.51933366,"about_ca_system_score_codex":0.012089441,"about_ca_system_score_gemma":0.0153433755,"threshold_uncertainty_score":0.6856122},"labels":[],"label_agreement":null},{"id":"W4239514014","doi":"10.3133/ofr20141025a","title":"Earthquake catalog for estimation of maximum earthquake magnitude, Central and Eastern United States: Part A, Prehistoric earthquakes","year":2014,"lang":"en","type":"article","venue":"Antarctica A Keystone in a Changing World","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Magnitude (astronomy); Seismology; Geology; Maximum magnitude; Seismic hazard; Prehistory; Geography; Paleontology","score_opus":0.01665187587137833,"score_gpt":0.2287501539217343,"score_spread":0.21209827805035597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239514014","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.049569007,0.0004283054,0.011234311,0.00026362482,0.00011674897,0.0016571323,0.89404845,0.004052213,0.03863029],"genre_scores_gemma":[0.049642477,0.00060786103,0.03004402,0.0001141007,0.00008812933,0.0015401532,0.90548027,0.00032529645,0.012157724],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99966836,0.00003330221,0.000073057956,0.000046485427,0.00014664394,0.000032166306],"domain_scores_gemma":[0.9945167,0.0003533392,0.0006011124,0.000731001,0.0033736867,0.00042412794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000712826,0.00050412805,0.0003391155,0.008251104,0.00081843295,0.0008881082,0.0006907152,0.0003534588,0.020583533],"category_scores_gemma":[0.0034353717,0.00038788986,0.00018494869,0.008288728,0.00011574085,0.00088520074,0.000988378,0.00042483254,0.015069769],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014110834,0.00022727267,0.13892229,0.00026881974,0.00004131651,0.00018654476,0.0003311879,0.0015707844,0.0019774712,0.0020153704,0.70694983,0.14736807],"study_design_scores_gemma":[0.00008602434,0.00009155444,0.5175595,0.00016503909,0.0000375096,0.0002585175,0.00048453733,0.0026913811,0.0018753881,0.000648518,0.4760569,0.00004509199],"about_ca_topic_score_codex":0.059490178,"about_ca_topic_score_gemma":0.08391485,"teacher_disagreement_score":0.059490178,"about_ca_system_score_codex":0.0006064753,"about_ca_system_score_gemma":0.0027170507,"threshold_uncertainty_score":0.1182878},"labels":[],"label_agreement":null},{"id":"W4239603042","doi":"10.1007/978-1-4020-4399-4_132","title":"Fault","year":2013,"lang":"en","type":"book-chapter","venue":"Encyclopedia of earth sciences series/Encyclopedia of earth sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Computer science; Fault (geology); Geology; Seismology","score_opus":0.02062612324433195,"score_gpt":0.22577872984561242,"score_spread":0.20515260660128048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4239603042","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008835479,0.00030704914,0.009624407,0.0006683151,0.0012534613,0.0001113046,0.003981244,0.0014072886,0.9738114],"genre_scores_gemma":[0.11787378,0.0006913052,0.004125961,0.00029718422,0.0002798577,0.00006299258,0.005988071,0.00030644774,0.87037444],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99986386,0.0000067861424,0.000009099223,0.00004214554,0.0000508654,0.000027187392],"domain_scores_gemma":[0.9998109,0.000013564714,0.000022934277,0.000035623318,0.00008736511,0.000029741013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011366028,0.00051255705,0.00022090714,0.0011585734,0.00084481307,0.0013664991,0.00042782593,0.0005726058,0.31206512],"category_scores_gemma":[0.0005160841,0.00014305442,0.0002073241,0.0009194958,0.00036434422,0.0013241847,0.00086456246,0.0005504584,0.1026543],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001974108,0.00005477495,0.0031809392,0.00036998506,0.00001494341,0.00043696497,0.00056533987,0.0011885412,0.0059771365,0.14821048,0.43313992,0.40666357],"study_design_scores_gemma":[0.000025910831,0.000069350564,0.002829055,0.000047663536,0.000009963958,0.0002990853,0.00019594787,0.00048318395,0.0016351142,0.0082537355,0.9861406,0.000010445396],"about_ca_topic_score_codex":0.002387632,"about_ca_topic_score_gemma":0.0025617247,"teacher_disagreement_score":0.31206512,"about_ca_system_score_codex":0.0004755002,"about_ca_system_score_gemma":0.00068631826,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4240635919","doi":"10.1190/tle37030232.1","title":"Reviews","year":2018,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"College of Veterinarians of British Columbia","funders":"","keywords":"Art history; Political science; History; Media studies; Library science; Economic history; Sociology; Computer science","score_opus":0.05628866084405556,"score_gpt":0.2704669002249336,"score_spread":0.21417823938087802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240635919","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005091535,0.4673163,0.0024554776,0.041930288,0.07473507,0.00019686701,0.004217142,0.0011784197,0.4074613],"genre_scores_gemma":[0.0042309733,0.4138239,0.0027219953,0.031519048,0.033785146,0.00023222974,0.006301372,0.000755294,0.50663],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99851507,0.00019569203,0.00013176777,0.0002694777,0.0007339239,0.0001540877],"domain_scores_gemma":[0.9972639,0.00058107614,0.00020063105,0.00028003007,0.0012540029,0.00042027835],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010974283,0.0010812161,0.0011583136,0.003158288,0.00081368943,0.004383429,0.0023949519,0.0028508177,0.31560373],"category_scores_gemma":[0.0063773366,0.00038782627,0.00081097253,0.0028498527,0.0007975921,0.0033904633,0.0023973137,0.0025827202,0.26108792],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018279621,0.000015079661,0.000054555177,0.00101835,0.000008499816,0.000061447,0.000048190803,0.00004564137,0.00017654819,0.0046411604,0.8648608,0.1290516],"study_design_scores_gemma":[0.0000020325124,0.0000033646975,0.00005323329,0.0003352496,0.0000027997064,0.000075909404,0.000014761868,0.0000041212406,0.000021751433,0.00069751416,0.9987872,0.000002102865],"about_ca_topic_score_codex":0.0021234956,"about_ca_topic_score_gemma":0.0035363333,"teacher_disagreement_score":0.68439627,"about_ca_system_score_codex":0.0016802275,"about_ca_system_score_gemma":0.004346637,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4240874027","doi":"10.1130/0091-7613(2002)030<0480:r>2.0.co;2","title":"REPLY","year":2002,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Library science; Citation; Geological survey; National laboratory; Archaeology; Geology; State (computer science); History; Computer science; Geophysics; Physics; Engineering physics; Algorithm","score_opus":0.02306422001374908,"score_gpt":0.197806367900893,"score_spread":0.17474214788714393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4240874027","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00041342582,0.0013688138,0.00014406926,0.88854045,0.0895156,0.00003242169,0.0003704358,0.00014949875,0.019465392],"genre_scores_gemma":[0.0030932517,0.0008621616,0.00015798588,0.8813625,0.023412941,0.00007576371,0.00020193063,0.00007424865,0.09075921],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980399,0.0003794023,0.00019097787,0.00037649643,0.00065052876,0.00036269653],"domain_scores_gemma":[0.9946392,0.0015411096,0.00022017883,0.0003497138,0.0023388914,0.00091091986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026131026,0.0007698452,0.00070640224,0.00076939736,0.0033227121,0.0037904114,0.002012471,0.026517529,0.063534364],"category_scores_gemma":[0.020315245,0.00054945296,0.0012473601,0.0008039461,0.0018363931,0.00355564,0.0016339219,0.022659004,0.039853882],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012940139,0.0000059307986,0.00009182914,0.000012859155,0.0000018860273,0.00008327398,0.00002810139,0.000004395231,0.000025804431,0.0008537296,0.9965243,0.0023548503],"study_design_scores_gemma":[0.00001964206,0.000014077819,0.0003109281,0.00006767859,0.0000064608967,0.00020182892,0.00014955759,0.000022469341,0.00008874025,0.0010341038,0.9980725,0.000012049312],"about_ca_topic_score_codex":0.006848638,"about_ca_topic_score_gemma":0.008335727,"teacher_disagreement_score":0.063534364,"about_ca_system_score_codex":0.0029439393,"about_ca_system_score_gemma":0.0039657587,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4241157669","doi":"10.1130/geos.s.14779818","title":"Supplemental Material: Mantle control on magmatic flare-ups in the southern Coast Mountains batholith, British Columbia","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Batholith; Geology; Flare; Mantle (geology); Geochemistry; Earth science; Seismology; Tectonics; Engineering","score_opus":0.011500239123546334,"score_gpt":0.20871485219150898,"score_spread":0.19721461306796265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241157669","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004877042,0.000053111064,0.00025197625,0.00029525667,0.00013446771,0.000024832665,0.9828258,0.00037470917,0.011162654],"genre_scores_gemma":[0.04799883,0.00029308695,0.0018059855,0.00013990367,0.000118103184,0.00007687107,0.8919269,0.0005517292,0.057088673],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99974483,0.000014417089,0.000022394028,0.000049847247,0.00009161853,0.0000768444],"domain_scores_gemma":[0.99681455,0.00054458453,0.00015819035,0.0002493616,0.0018838522,0.0003495392],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037828035,0.00062313763,0.00048930483,0.002787367,0.0013354275,0.0013436006,0.0010955944,0.00045028594,0.39622417],"category_scores_gemma":[0.0034918264,0.00031775923,0.0004151232,0.004896822,0.00015633689,0.00060617825,0.0006555917,0.00037709362,0.042148635],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054911427,0.000041571642,0.014384222,0.00020483913,0.000026216458,0.000068118774,0.000137797,0.00047341306,0.00025853328,0.0005607135,0.9697581,0.01403165],"study_design_scores_gemma":[0.00014976118,0.000033104876,0.51486856,0.0005529417,0.00008543265,0.00019016917,0.0013355754,0.0022516246,0.001280907,0.0024721075,0.47671,0.000069766604],"about_ca_topic_score_codex":0.74839884,"about_ca_topic_score_gemma":0.88093513,"teacher_disagreement_score":0.39622417,"about_ca_system_score_codex":0.0029924747,"about_ca_system_score_gemma":0.004316503,"threshold_uncertainty_score":0.86121297},"labels":[],"label_agreement":null},{"id":"W4241854367","doi":"10.4095/299816","title":"Regional centroid moment tensor solutions for eastern Canadian earthquakes: 2015","year":2017,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Centroid; Moment tensor; Moment (physics); Geology; Seismology; Geography; Geodesy; Mathematics; Physics; Geometry; Oceanography; Classical mechanics","score_opus":0.10567682914858934,"score_gpt":0.28881738756478703,"score_spread":0.1831405584161977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4241854367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9203412,0.0008348058,0.0039787292,0.00026385303,0.000058020603,0.00009683357,0.061558045,0.000436924,0.01243165],"genre_scores_gemma":[0.9440269,0.0005809408,0.006933193,0.000028043383,0.00001422265,0.000028996807,0.04376939,0.000081015845,0.004537393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996018,0.000007217813,0.000025907633,0.000058230613,0.00018784672,0.000119094555],"domain_scores_gemma":[0.9987884,0.000022147135,0.000113947994,0.00004273229,0.0009278176,0.00010490315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003863156,0.0006102874,0.00028263568,0.0032039832,0.0014448122,0.0008907014,0.0008960851,0.0003837693,0.0019160942],"category_scores_gemma":[0.0016068339,0.00025475782,0.00043620297,0.004943959,0.000404803,0.00052022364,0.0007864876,0.0004605688,0.0005854465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005539941,0.00017368144,0.7119701,0.0005182239,0.00045706023,0.00084356155,0.0020694921,0.04034451,0.026929336,0.0028036889,0.03445981,0.17887655],"study_design_scores_gemma":[0.000022399414,0.000023506127,0.9772828,0.000027460304,0.000067638306,0.00011802936,0.00074307766,0.008806402,0.0041853846,0.00017276744,0.008478505,0.00007199539],"about_ca_topic_score_codex":0.9672444,"about_ca_topic_score_gemma":0.9882929,"teacher_disagreement_score":0.032755613,"about_ca_system_score_codex":0.009737295,"about_ca_system_score_gemma":0.013166106,"threshold_uncertainty_score":0.070649385},"labels":[],"label_agreement":null},{"id":"W4242388182","doi":"10.5194/se-2018-37","title":"Channel flow, tectonic overpressure, and exhumation of high-pressure rocks in the Greater Himalayas","year":2018,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Fundação para a Ciência e a Tecnologia; University Grants Commission; Department of Science and Technology, Ministry of Science and Technology, India","keywords":"Geology; Subduction; Overpressure; Tectonics; Continental collision; Seismology; Geodynamics; Petrology; Geomorphology; Geophysics","score_opus":0.019731738067853517,"score_gpt":0.2186850740992284,"score_spread":0.19895333603137488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242388182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987795,0.000039325387,0.00036596318,0.000048551432,0.0000021957947,0.0000026902128,0.00004745262,0.000016841353,0.0006975383],"genre_scores_gemma":[0.9997106,0.000028549024,0.00009434822,0.0000048125694,0.0000015620028,0.0000015691604,0.000015262694,0.0000024376498,0.00014072856],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.000018310015,0.000004318508,0.000014042752,0.000009774471,0.000016920047],"domain_scores_gemma":[0.99987006,0.00004878398,0.000021417236,0.000011789251,0.000015599451,0.00003230349],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018091491,0.00022783336,0.00020402235,0.0005375156,0.00047464814,0.000850712,0.00030150873,0.0005263958,0.0011851704],"category_scores_gemma":[0.00046910305,0.00021813638,0.00032391696,0.00061570096,0.0008813802,0.0004373271,0.000337701,0.00023545843,0.00008437045],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013084627,0.00010753527,0.10474739,0.000051576557,0.00006331954,0.00049119134,0.00038532933,0.87738127,0.008372396,0.0044065733,0.00019875425,0.0036637965],"study_design_scores_gemma":[0.00006616079,0.00009320962,0.104616486,0.000010199016,0.000027814422,0.00008057948,0.00024811705,0.8920026,0.001384917,0.0011449814,0.00030024786,0.000024818391],"about_ca_topic_score_codex":0.055537783,"about_ca_topic_score_gemma":0.023398638,"teacher_disagreement_score":0.055537783,"about_ca_system_score_codex":0.0017016594,"about_ca_system_score_gemma":0.00082368904,"threshold_uncertainty_score":0.11042905},"labels":[],"label_agreement":null},{"id":"W4242678499","doi":"10.1007/s00024-008-0440-7","title":"Tsunamis on the Pacific Coast of Canada Recorded in 1994–2007","year":2009,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; Canadian Hydrographic Service","funders":"","keywords":"Geology; Seismology; Tide gauge; Pacific ocean; Oceanography; Period (music); Arrival time; Sea level","score_opus":0.007482300549930623,"score_gpt":0.16841629236550085,"score_spread":0.16093399181557022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4242678499","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9416866,0.0010877005,0.00013003788,0.0002476321,0.00004808035,0.00004918751,0.049240258,0.000052075535,0.0074585443],"genre_scores_gemma":[0.9518846,0.0019827893,0.0004084981,0.00012111533,0.000025899033,0.000039077036,0.037789617,0.00001365903,0.0077347006],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99961495,0.000010178805,0.00003099197,0.000041776264,0.0001616832,0.00014042204],"domain_scores_gemma":[0.99798274,0.000053266307,0.00033476483,0.000031221327,0.001333648,0.00026435143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018609015,0.00057731726,0.00031733268,0.003703412,0.0019457762,0.0008402878,0.00074968324,0.00039258483,0.0018361335],"category_scores_gemma":[0.0011231289,0.00027104968,0.0003158546,0.007297871,0.0005201847,0.0003768532,0.0007657953,0.0005469314,0.0003396489],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027785942,0.000046597375,0.9600717,0.00024733137,0.00023798872,0.0005185061,0.0016624364,0.0012397115,0.0011086689,0.00030283415,0.017454116,0.016832218],"study_design_scores_gemma":[0.000004603162,0.000011617176,0.9925604,0.000040728137,0.00003139918,0.00008282994,0.0014179469,0.00022554195,0.00013113108,0.000014332032,0.0054682544,0.000011096155],"about_ca_topic_score_codex":0.9954657,"about_ca_topic_score_gemma":0.99846137,"teacher_disagreement_score":0.015034824,"about_ca_system_score_codex":0.015034824,"about_ca_system_score_gemma":0.023883943,"threshold_uncertainty_score":0.1090858},"labels":[],"label_agreement":null},{"id":"W4243398950","doi":"10.4095/212211","title":"Tsunamis","year":2001,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Geography; Environmental science","score_opus":0.049565671357642165,"score_gpt":0.26159247768173344,"score_spread":0.21202680632409127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243398950","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.022619179,0.004509735,0.0025085425,0.0014270451,0.0015097668,0.0014192553,0.18152057,0.0015005141,0.7829854],"genre_scores_gemma":[0.12302721,0.014658716,0.0047646617,0.0014047638,0.0009547134,0.0011498593,0.28117618,0.00032075684,0.572543],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9984137,0.00011194269,0.00015617225,0.00014006523,0.00092133286,0.0002567888],"domain_scores_gemma":[0.9971058,0.0002050788,0.0003751671,0.00028379765,0.0017011191,0.00032917183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047897385,0.0011996798,0.00052136614,0.003767955,0.0013280691,0.0018750097,0.00089943147,0.0006161771,0.10090799],"category_scores_gemma":[0.0039027857,0.00022873665,0.0004040601,0.004806563,0.00036481136,0.0010206647,0.0013857484,0.0010024518,0.048063695],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016347018,0.00018554945,0.035245772,0.0005784392,0.00004403262,0.00050739414,0.0009936636,0.00062089873,0.0008730877,0.010055923,0.74295604,0.20777576],"study_design_scores_gemma":[0.0000146629545,0.0000659332,0.054923553,0.00020782891,0.000012368306,0.00041921024,0.00054024707,0.00011355507,0.0002909345,0.0009777406,0.9424118,0.000022188913],"about_ca_topic_score_codex":0.030347835,"about_ca_topic_score_gemma":0.038009174,"teacher_disagreement_score":0.10090799,"about_ca_system_score_codex":0.0013335611,"about_ca_system_score_gemma":0.0028040626,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4243592932","doi":"10.1002/essoar.10502973.3","title":"Earthquake rupture through a step-over fault system: An exploratory numerical study of the Leech River Fault, southern Vancouver Island","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geology; Fault (geology); Offset (computer science); Shear stress; Shear (geology); Slip (aerodynamics); Jump; Stress (linguistics); Geodesy; Engineering; Mechanics; Petrology; Physics; Computer science","score_opus":0.029106665895469442,"score_gpt":0.23898057080511492,"score_spread":0.20987390490964547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4243592932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982672,0.000037760474,0.00019689229,0.00008158526,0.0000028799468,0.0000091875545,0.00014565619,0.000014336975,0.0012444955],"genre_scores_gemma":[0.998787,0.000033487726,0.00047674088,0.000022450242,0.0000021268124,0.000009686129,0.00018548196,0.000006791633,0.00047621242],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998853,0.000023227114,0.00000629192,0.000024479368,0.000020004569,0.00004064805],"domain_scores_gemma":[0.99950707,0.00020849518,0.00005395855,0.00002795123,0.00007145081,0.00013098412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022260752,0.00044605084,0.00048659922,0.00055241387,0.0008848036,0.0010657619,0.0010950331,0.0015690902,0.0015269687],"category_scores_gemma":[0.0012635371,0.00038256444,0.00046066914,0.0007143813,0.0009375535,0.00038368133,0.0007094932,0.0006869864,0.000113568305],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003425089,0.00049723074,0.09530571,0.0000846801,0.00017748651,0.0014163468,0.00031157906,0.89250356,0.0034881108,0.0012617918,0.0010199592,0.003591012],"study_design_scores_gemma":[0.00010178443,0.00010650359,0.02441239,0.000015719366,0.00003549177,0.000063363485,0.000632616,0.9736908,0.00035050052,0.0002557265,0.00031020644,0.00002491311],"about_ca_topic_score_codex":0.25517946,"about_ca_topic_score_gemma":0.2647001,"teacher_disagreement_score":0.74482054,"about_ca_system_score_codex":0.0018260872,"about_ca_system_score_gemma":0.0016890038,"threshold_uncertainty_score":0.50738835},"labels":[],"label_agreement":null},{"id":"W4244416196","doi":"10.1002/essoar.10507748.1","title":"Raton Basin induced seismicity is hosted by networks of short basement faults and mimics tectonic earthquake statistics","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Induced seismicity; Tectonics; Geology; Seismology; World Wide Web; Computer science","score_opus":0.020791230780888532,"score_gpt":0.23305695756999567,"score_spread":0.21226572678910713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244416196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98147136,0.00020565996,0.000853596,0.000063377185,0.000018612325,0.00003322252,0.0049820766,0.0002120376,0.01216012],"genre_scores_gemma":[0.9909372,0.00016008591,0.0010684762,0.00002667844,0.000011386763,0.000025153064,0.0047585964,0.00004176867,0.0029706797],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989045,0.0000071845798,0.000008280149,0.00002984362,0.000033636683,0.000030686835],"domain_scores_gemma":[0.999671,0.000030500567,0.00014436172,0.000030768293,0.000086793785,0.0000367074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000100824116,0.0002839984,0.00017334866,0.0015036315,0.00022821558,0.00040650333,0.0002374557,0.000120253266,0.003994861],"category_scores_gemma":[0.0004517163,0.000099566016,0.00012510826,0.0018619656,0.00024729205,0.00025852968,0.00044132382,0.00012932181,0.0004433235],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016393239,0.00005396582,0.91399413,0.00031505752,0.00007193944,0.0006946712,0.001281296,0.0019964483,0.013672684,0.00087453536,0.006576986,0.060304333],"study_design_scores_gemma":[0.000003887252,0.00002947671,0.9865073,0.00003001429,0.00001777374,0.0002515653,0.00047220816,0.0020878243,0.0007991413,0.00011048082,0.009680511,0.0000097311],"about_ca_topic_score_codex":0.04235146,"about_ca_topic_score_gemma":0.1651832,"teacher_disagreement_score":0.04235146,"about_ca_system_score_codex":0.00046195998,"about_ca_system_score_gemma":0.00063138455,"threshold_uncertainty_score":0.08420986},"labels":[],"label_agreement":null},{"id":"W4244453886","doi":"10.1002/essoar.10504307.2","title":"Subduction, underplating, and return flow recorded in the Cycladic Blueschist Unit exposed on Syros Island, Greece","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Blueschist; World Wide Web; Geology; Subduction; Computer science; Tectonics; Seismology","score_opus":0.0367044162438454,"score_gpt":0.23375733657364756,"score_spread":0.19705292032980215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244453886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997715,0.00010989861,0.00010656026,0.00000834724,0.0000023479536,0.0000059422355,0.0003758115,0.000016816088,0.001659126],"genre_scores_gemma":[0.9987036,0.00006862187,0.00029296166,0.0000047595518,0.000002412504,0.0000054046313,0.00033895668,0.000008719552,0.0005746166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992657,0.0000040422774,0.000007592264,0.000032631957,0.0000180774,0.000011059603],"domain_scores_gemma":[0.9999341,0.000005817267,0.000020677984,0.000011547841,0.000019529149,0.000008412786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009716366,0.00020871687,0.00020332052,0.0011040622,0.00025113768,0.00031227712,0.00023730178,0.00024250691,0.0011493055],"category_scores_gemma":[0.00017783904,0.00013248087,0.0001349759,0.00092747196,0.0005576475,0.00022387781,0.00048971473,0.00014533265,0.00027724056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043299605,0.000055150995,0.77963644,0.00030587168,0.0001277261,0.0022186167,0.0067064604,0.0030073642,0.14861481,0.0007657809,0.0007417157,0.057387035],"study_design_scores_gemma":[0.0000063150082,0.000026029878,0.9957314,0.000014101611,0.000014126687,0.00033109603,0.0005354461,0.00056442386,0.0013540491,0.000035768702,0.0013813901,0.0000058792666],"about_ca_topic_score_codex":0.027724847,"about_ca_topic_score_gemma":0.057300035,"teacher_disagreement_score":0.027724847,"about_ca_system_score_codex":0.00035222783,"about_ca_system_score_gemma":0.00026774025,"threshold_uncertainty_score":0.055126965},"labels":[],"label_agreement":null},{"id":"W4244516271","doi":"10.5194/nhess-6-1035-2006","title":"Meteotsunamis: atmospherically induced destructive ocean waves in the tsunami frequency band","year":2006,"lang":"en","type":"article","venue":"Natural hazards and earth system sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":492,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Division of Ocean Sciences; Russian Foundation for Basic Research; Strong","keywords":"Geology; Seismology; Seiche; Froude number; Tsunami wave; Wind wave; Landslide; Barotropic fluid; Seismic wave; Schumann resonances; Geophysics; Climatology; Meteorology; Oceanography; Physics; Mechanics","score_opus":0.010651550918077273,"score_gpt":0.2140280621468235,"score_spread":0.20337651122874623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244516271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.984101,0.0019746239,0.0055419905,0.000063955486,0.00007002893,0.00002667572,0.00040337184,0.00007587575,0.007742547],"genre_scores_gemma":[0.9978377,0.00039801028,0.00081574434,0.000011597078,0.00004002268,0.000009292388,0.00022392199,0.000009771299,0.0006539752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990547,0.000011992701,0.000010250782,0.000016993485,0.00003345305,0.000021843865],"domain_scores_gemma":[0.99974257,0.000043348646,0.00013894378,0.000015813363,0.000020667516,0.000038693102],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010306231,0.00033543215,0.0001303193,0.0009459006,0.0002826384,0.00052675063,0.00016331623,0.000224801,0.0011123049],"category_scores_gemma":[0.00035004292,0.00007451593,0.00012428698,0.00081414595,0.000345154,0.00030398607,0.0005326467,0.00025366037,0.00018147138],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012480697,0.00013411783,0.64879906,0.00064097147,0.00018616545,0.0064690034,0.0017843827,0.012385143,0.18092188,0.022929963,0.003665513,0.120835714],"study_design_scores_gemma":[0.000022546243,0.0002441063,0.9510257,0.00007263352,0.000067820074,0.0045657256,0.0008667093,0.011911009,0.013109005,0.004523497,0.013552172,0.00003906501],"about_ca_topic_score_codex":0.0010458073,"about_ca_topic_score_gemma":0.0014353817,"teacher_disagreement_score":0.0011123049,"about_ca_system_score_codex":0.00017169116,"about_ca_system_score_gemma":0.000111954694,"threshold_uncertainty_score":0.0037210584},"labels":[],"label_agreement":null},{"id":"W4244922976","doi":"10.1190/tle24030320.1","title":"Reviews","year":2005,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"College of Veterinarians of British Columbia","funders":"","keywords":"Officer; Humanities; Philosophy; Political science; Law","score_opus":0.04762121923236551,"score_gpt":0.25993918470552624,"score_spread":0.21231796547316073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244922976","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00047101016,0.3585435,0.0026034832,0.018167673,0.043615036,0.00019815115,0.0044950917,0.0013177035,0.57058835],"genre_scores_gemma":[0.002821997,0.2427825,0.002743935,0.009606202,0.012999564,0.00016651656,0.00511664,0.00061964453,0.72314304],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986203,0.00015783815,0.00011426634,0.0002861647,0.000700862,0.000120641205],"domain_scores_gemma":[0.9982937,0.00030306124,0.000116361356,0.00016954131,0.00082048227,0.00029687572],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008827729,0.0014783787,0.0013350181,0.0032521016,0.0009083607,0.0053106057,0.0023539606,0.0020747415,0.39486378],"category_scores_gemma":[0.0039839046,0.00047338367,0.0007790735,0.0032937168,0.0007464788,0.0035603924,0.0022862821,0.0024242857,0.37249896],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019219193,0.000020154877,0.00006799067,0.0010702792,0.000008135187,0.00006387608,0.000059428035,0.000061804334,0.00023164641,0.004231016,0.81480664,0.1793598],"study_design_scores_gemma":[0.00000135232,0.0000029339183,0.000054475615,0.00019695592,0.0000018383924,0.00006358079,0.000016929453,0.0000048667207,0.000019574729,0.00055620424,0.99907947,0.000001920314],"about_ca_topic_score_codex":0.0026769992,"about_ca_topic_score_gemma":0.0047105984,"teacher_disagreement_score":0.6051362,"about_ca_system_score_codex":0.0020672095,"about_ca_system_score_gemma":0.0039428985,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4245090803","doi":"10.1002/essoar.10504240.1","title":"Crustal velocity variations and constraints on material properties in the Charlevoix Seismic Zone, eastern Canada","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Geology; Bouguer anomaly; Seismology; Seismic velocity; Impact structure; Seismic tomography; Tectonics; Gravity anomaly; Rift; Plateau (mathematics); Petrology; Geophysics; Mantle (geology); Paleontology; Impact crater","score_opus":0.03203163647737697,"score_gpt":0.20164876216452413,"score_spread":0.16961712568714715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245090803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976724,0.000116663396,0.00009827913,0.000042780797,0.0000010454846,0.0000046605933,0.0004014722,0.000016865786,0.0016457824],"genre_scores_gemma":[0.9990269,0.000078749414,0.000121183264,0.000006768303,4.4539863e-7,0.0000018393514,0.0002896865,0.0000045241845,0.00046986155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977463,0.0000070664005,0.000007875685,0.000048824284,0.0000754565,0.00008620994],"domain_scores_gemma":[0.9995486,0.000041911997,0.00007114677,0.000017726274,0.00021222321,0.000108391774],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018819679,0.00036820228,0.00026085883,0.0017437745,0.0016350975,0.0015308231,0.00063518126,0.00028883133,0.0014400479],"category_scores_gemma":[0.00088820007,0.00026786485,0.00025043043,0.0018977327,0.000874799,0.00029094148,0.00077201973,0.00026098694,0.00011273437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112927766,0.000031822925,0.97022575,0.000032785938,0.00007028763,0.00029436263,0.00079135824,0.0079673715,0.006308967,0.00085083494,0.0005495848,0.012763826],"study_design_scores_gemma":[0.000005110815,0.000005382069,0.99378914,0.000009027499,0.0000115393,0.00002803049,0.0006423612,0.004509271,0.0002941252,0.00006388133,0.00063063164,0.0000116000965],"about_ca_topic_score_codex":0.9924043,"about_ca_topic_score_gemma":0.99533564,"teacher_disagreement_score":0.019428706,"about_ca_system_score_codex":0.019428706,"about_ca_system_score_gemma":0.012873107,"threshold_uncertainty_score":0.14096582},"labels":[],"label_agreement":null},{"id":"W4245319960","doi":"10.1002/essoar.10506832.1","title":"Spatiotemporal changes in seismic velocity associated with hydraulic fracturing-induced earthquakes near Fox Creek, Alberta, Canada","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Natural Resources Canada","funders":"","keywords":"Geology; Hydraulic fracturing; Preprint; Seismology; World Wide Web; Geotechnical engineering; Computer science","score_opus":0.018616553746978636,"score_gpt":0.20286398717691892,"score_spread":0.1842474334299403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245319960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984118,0.0000535454,0.00021379405,0.000026600135,0.0000034009483,0.000009697681,0.00044847914,0.000015000909,0.0008176339],"genre_scores_gemma":[0.9983676,0.000047867485,0.00026664956,0.000012594857,0.0000020400498,0.000006297516,0.0005580599,0.0000027022145,0.00073621847],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980205,0.000006721983,0.00000539659,0.00003876573,0.00009234168,0.000054702286],"domain_scores_gemma":[0.9995982,0.000026025738,0.00005559718,0.000010277483,0.00023053492,0.00007933205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014118163,0.00024594262,0.0001972625,0.0009542911,0.0006895097,0.000445267,0.0005132965,0.00028563367,0.0005910607],"category_scores_gemma":[0.00038237154,0.00013475845,0.00012150886,0.0012369544,0.00040921956,0.00012461461,0.00030482362,0.00020092906,0.000082053404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022017014,0.00009743388,0.9320076,0.000049470695,0.000064853106,0.0005119228,0.0015180239,0.0027213842,0.040885888,0.00014477815,0.0009447467,0.020833738],"study_design_scores_gemma":[0.0000029510443,0.00001598013,0.99760854,0.0000038101389,0.000006164369,0.000017999237,0.00045298287,0.0010950192,0.0004651526,0.00000777418,0.00031687724,0.000006722175],"about_ca_topic_score_codex":0.91120046,"about_ca_topic_score_gemma":0.97157276,"teacher_disagreement_score":0.088799536,"about_ca_system_score_codex":0.0044083763,"about_ca_system_score_gemma":0.0041839164,"threshold_uncertainty_score":0.17864496},"labels":[],"label_agreement":null},{"id":"W4245396006","doi":"10.1002/essoar.10504243.2","title":"Seismicity and the State of Stress in the Dezful Embayment, Zagros Fold and Thrust Belt","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Induced seismicity; Preprint; Geology; World Wide Web; Computer science; Seismology","score_opus":0.017405056833672983,"score_gpt":0.21924613787952738,"score_spread":0.20184108104585438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245396006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99980646,0.000020300542,0.000015934504,0.000007183702,3.0893875e-7,5.1743865e-7,0.00005484529,8.0527457e-7,0.00009355738],"genre_scores_gemma":[0.99968576,0.000026336962,0.000045362984,0.000002680934,0.0000014054787,9.685634e-7,0.00017461117,3.1185252e-7,0.000062603125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998777,0.000013595796,0.000015019812,0.000029996496,0.000023134642,0.000040559058],"domain_scores_gemma":[0.99975854,0.000027465365,0.00014202291,0.000014560048,0.000031313022,0.000026040887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024901755,0.00022029044,0.00018202784,0.0013462451,0.00022386029,0.00049969816,0.00017378376,0.00021045319,0.00039475432],"category_scores_gemma":[0.00055619306,0.00012849443,0.0001399883,0.0011368878,0.0003359224,0.00032149232,0.0002371276,0.00013929112,0.0001134896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089474306,0.0000215957,0.99242896,0.000007869997,0.00002955458,0.00011006462,0.00035690554,0.0003638824,0.0017667592,0.00006704589,0.00004370067,0.0047141733],"study_design_scores_gemma":[0.0000015296721,0.0000116267765,0.99954814,0.0000014491543,0.0000028995069,0.000021190166,0.00015226133,0.00014477645,0.000048840837,0.000008494116,0.000057660363,0.000001108826],"about_ca_topic_score_codex":0.029582541,"about_ca_topic_score_gemma":0.051889416,"teacher_disagreement_score":0.029582541,"about_ca_system_score_codex":0.0008148918,"about_ca_system_score_gemma":0.0002349964,"threshold_uncertainty_score":0.058820665},"labels":[],"label_agreement":null},{"id":"W4245404223","doi":"10.1193/1.2205874","title":"Lifeline Systems in the Andaman and Nicobar Islands (India) after the December 2004 Great Sumatra Earthquake and Indian Ocean Tsunami","year":2006,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Defence Research and Development Canada","funders":"","keywords":"Geology; Indian ocean; Seismology; Oceanography","score_opus":0.007041959727726124,"score_gpt":0.19466495202091835,"score_spread":0.18762299229319224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245404223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970554,0.000109646375,0.000029088578,0.000034161716,0.000002225294,0.0000072982816,0.0002003656,0.00000764663,0.0025541645],"genre_scores_gemma":[0.99800664,0.0001792421,0.00006525621,0.000016746257,0.0000014763158,0.00001770671,0.00047387494,0.000004619226,0.0012344813],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986184,0.00002513394,0.000014158109,0.000020020207,0.00002227725,0.000056562265],"domain_scores_gemma":[0.9996617,0.00002242048,0.00009840431,0.00003264034,0.00013946142,0.00004534913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000117247255,0.0001858304,0.00012905449,0.001214218,0.00078358926,0.00082518556,0.00053217704,0.00022158006,0.0012915012],"category_scores_gemma":[0.0008768331,0.00014074922,0.00010809861,0.0016861527,0.0004974614,0.00047527382,0.0010437529,0.00019718822,0.00031056133],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026597336,0.000047932375,0.94206995,0.00010985378,0.000096200085,0.0029651346,0.018644882,0.0016881797,0.0077363066,0.00087962684,0.0011391895,0.02435689],"study_design_scores_gemma":[0.000002984217,0.00003099896,0.98415726,0.000018592558,0.000022396041,0.00026575255,0.011569847,0.00033414224,0.00062707026,0.000051276784,0.002907202,0.000012503707],"about_ca_topic_score_codex":0.29178545,"about_ca_topic_score_gemma":0.37236375,"teacher_disagreement_score":0.29178545,"about_ca_system_score_codex":0.001962667,"about_ca_system_score_gemma":0.00059130613,"threshold_uncertainty_score":0.58017415},"labels":[],"label_agreement":null},{"id":"W4245524077","doi":"10.1007/s11069-018-3405-x","title":"Correction to: New constraints on coseismic slip during southern Cascadia subduction zone earthquakes over the past 4600 years implied by tsunami deposits and marine turbidites","year":2018,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Chart; Subduction; Geology; Seismology; Slip (aerodynamics); Geodesy; Statistics; Tectonics; Mathematics; Engineering","score_opus":0.005928387734716601,"score_gpt":0.20699379517978678,"score_spread":0.20106540744507018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245524077","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00096819253,0.00077939144,0.0010614285,0.016786609,0.95602405,0.000047439265,0.019777196,0.001093414,0.0034622645],"genre_scores_gemma":[0.08660585,0.0056795403,0.0151594365,0.028847577,0.34938085,0.000761407,0.06963231,0.008259897,0.43567303],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975036,0.00022058854,0.00049074704,0.00054072833,0.00072851585,0.0005158087],"domain_scores_gemma":[0.96832126,0.0038199953,0.0016360752,0.0033596668,0.020623196,0.0022397542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002500174,0.0036385371,0.0036150909,0.00837837,0.0028570802,0.004619099,0.0053776437,0.0041471533,0.20754178],"category_scores_gemma":[0.042250734,0.0022855666,0.0026067968,0.008382526,0.0015627728,0.0037044673,0.0033767119,0.0072440025,0.06530165],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056798803,0.0000073151605,0.00039070076,0.00020116923,0.000032556207,0.00007070735,0.000034990193,0.00015942809,0.000065660315,0.0004024749,0.9931912,0.005386996],"study_design_scores_gemma":[0.00035294678,0.00003426724,0.020205926,0.0004457887,0.00010678851,0.00037917375,0.00032163796,0.0012147917,0.00045930987,0.0017543697,0.97461003,0.00011508202],"about_ca_topic_score_codex":0.051021915,"about_ca_topic_score_gemma":0.077203535,"teacher_disagreement_score":0.20754178,"about_ca_system_score_codex":0.0029743763,"about_ca_system_score_gemma":0.0060827923,"threshold_uncertainty_score":0.6942964},"labels":[],"label_agreement":null},{"id":"W4245813949","doi":"10.1007/978-90-481-8702-7_61","title":"Seismic Properties of Rocks","year":2011,"lang":"en","type":"book-chapter","venue":"Encyclopedia of earth sciences series/Encyclopedia of earth sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Geochemistry","score_opus":0.030020397161197927,"score_gpt":0.21238334470653122,"score_spread":0.1823629475453333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4245813949","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46600458,0.009219508,0.11896287,0.00081809075,0.00022134843,0.000057245234,0.015882254,0.0013872491,0.38744682],"genre_scores_gemma":[0.91564554,0.0067920866,0.0074847597,0.00004692899,0.00015159935,0.000022406242,0.010082331,0.0002550569,0.059519347],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99993205,0.000005911969,0.0000044729168,0.00001569241,0.00003587759,0.0000059494],"domain_scores_gemma":[0.99988055,0.000027095055,0.000028793887,0.000020674233,0.000033654193,0.000009199175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000096146134,0.0002954446,0.00017700605,0.00077785616,0.00009486513,0.00043173027,0.00028306825,0.00016894875,0.010741287],"category_scores_gemma":[0.00052872876,0.00014132076,0.00012645878,0.00096071576,0.00014370575,0.0005653722,0.00027433303,0.00020713717,0.0032366002],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027332443,0.00007559273,0.039317235,0.000733491,0.00015191888,0.00054505566,0.00050052284,0.13819066,0.14776844,0.06867667,0.033224024,0.57054305],"study_design_scores_gemma":[0.000037047925,0.00032212748,0.21832798,0.00025868914,0.00016187764,0.0024422663,0.0007500303,0.25527793,0.07548573,0.063903876,0.38293138,0.00010116836],"about_ca_topic_score_codex":0.0010027841,"about_ca_topic_score_gemma":0.0010672362,"teacher_disagreement_score":0.010741287,"about_ca_system_score_codex":0.00015857512,"about_ca_system_score_gemma":0.00010635096,"threshold_uncertainty_score":0.035933197},"labels":[],"label_agreement":null},{"id":"W4246482358","doi":"10.1007/s00024-015-1175-x","title":"Introduction to “Tsunami Science: Ten Years after the 2004 Indian Ocean Tsunami. Volume II.”","year":2015,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Indian ocean; Tsunami wave; Geology; Oceanography; Seismology; Pacific ocean; Tsunami earthquake; Natural hazard; Volume (thermodynamics)","score_opus":0.006116750309044702,"score_gpt":0.187619083344389,"score_spread":0.1815023330353443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246482358","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0014534859,0.6937627,0.007051745,0.054371223,0.1781684,0.000109237575,0.005441807,0.00054524903,0.05909603],"genre_scores_gemma":[0.01871292,0.6066914,0.0074243858,0.033662528,0.15227887,0.00024521933,0.008677396,0.0007497846,0.17155741],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99941766,0.000112683025,0.00007884794,0.00010632211,0.00021699164,0.00006757162],"domain_scores_gemma":[0.9979534,0.00066758797,0.00017975205,0.00010779915,0.0007673419,0.00032404994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012780196,0.0014843598,0.00077176077,0.0044588065,0.0010203477,0.0029572195,0.0013914355,0.0013411919,0.030851709],"category_scores_gemma":[0.0035660216,0.00044518407,0.00080881396,0.004963835,0.0017661419,0.0030006762,0.002111814,0.0034593642,0.012613726],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005245809,0.000021786105,0.00067506236,0.0010029903,0.000015150061,0.00007068203,0.00025410333,0.00037194314,0.0005611393,0.0101412535,0.86552656,0.12130678],"study_design_scores_gemma":[0.000001794943,0.000010467728,0.0010471613,0.00030570454,0.0000037030134,0.00007642059,0.000079266014,0.00003206771,0.00007601138,0.002822489,0.9955375,0.000007363029],"about_ca_topic_score_codex":0.011483923,"about_ca_topic_score_gemma":0.017441954,"teacher_disagreement_score":0.030851709,"about_ca_system_score_codex":0.0019852084,"about_ca_system_score_gemma":0.0034748921,"threshold_uncertainty_score":0.10320932},"labels":[],"label_agreement":null},{"id":"W4246994965","doi":"10.1002/essoar.10502613.2","title":"The 2020 Mw 6.8 Elaziğ (Turkey) earthquake reveals rupture behavior of the East Anatolian Fault","year":2020,"lang":"ceb","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Aftershock; Seismology; Geology; Slip (aerodynamics); Subduction; Fault (geology); North Anatolian Fault; Earthquake rupture; Foreshock; Geodesy; Tectonics","score_opus":0.023805117059771487,"score_gpt":0.23877673738391617,"score_spread":0.21497162032414469,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4246994965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976763,0.000049829196,0.00006325452,0.000023575523,0.0000049089076,0.0000016966591,0.0010784334,0.0000235555,0.001078512],"genre_scores_gemma":[0.9964424,0.000054564924,0.00014158842,0.000007632497,0.0000055473656,0.0000028266024,0.0028362237,0.000007219263,0.0005019949],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999584,0.0000029555451,0.0000029954333,0.00001314105,0.000007338571,0.000015180647],"domain_scores_gemma":[0.99993265,0.0000037476357,0.00002113602,0.0000061143733,0.000017458773,0.000018974684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005496187,0.0002534503,0.00016830802,0.00078984903,0.00015676171,0.00030458107,0.0001236444,0.0002955153,0.0015679477],"category_scores_gemma":[0.00016637953,0.00011429183,0.00009110266,0.00060814404,0.00011429249,0.00022656158,0.0002580347,0.00014567826,0.0006735836],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005034374,0.0002245053,0.89351726,0.00007849143,0.00005945974,0.0011098593,0.00045952076,0.0035746105,0.06293937,0.00034506698,0.0046758293,0.03251264],"study_design_scores_gemma":[0.000003546566,0.000021205495,0.99681914,0.000003864169,0.0000044998997,0.0001189479,0.00011705454,0.001769753,0.0006259166,0.000023841727,0.0004890062,0.0000032352727],"about_ca_topic_score_codex":0.00628739,"about_ca_topic_score_gemma":0.007748088,"teacher_disagreement_score":0.00628739,"about_ca_system_score_codex":0.00020908893,"about_ca_system_score_gemma":0.00011856312,"threshold_uncertainty_score":0.012501597},"labels":[],"label_agreement":null},{"id":"W4247204617","doi":"10.4095/314592","title":"Regional centroid moment tensor solutions for eastern Canadian earthquakes: 2016","year":2019,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Moment tensor; Centroid; Geology; Moment (physics); Seismology; Geography; Geodesy; Mathematics; Geometry; Physics; Classical mechanics","score_opus":0.0759309805968713,"score_gpt":0.2545459276925524,"score_spread":0.1786149470956811,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247204617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8741117,0.000863162,0.006281901,0.0003707667,0.00008955269,0.0002011284,0.09236183,0.0007514616,0.024968484],"genre_scores_gemma":[0.9105881,0.00090024667,0.015962604,0.000033470107,0.000022516975,0.000051111805,0.061425194,0.00018399539,0.010832801],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99955994,0.000007658289,0.000028088138,0.00005117213,0.00023726471,0.00011584242],"domain_scores_gemma":[0.99838316,0.000027834249,0.00012805537,0.00005197187,0.0013035508,0.000105344516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040047706,0.0008484473,0.000294603,0.0034838181,0.0014115633,0.0008758657,0.0008289807,0.00038644602,0.0031377026],"category_scores_gemma":[0.0019770795,0.00028584286,0.00046755152,0.0048113596,0.0003401479,0.00054596335,0.00068505935,0.00046841,0.00095770403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006235901,0.00018299016,0.58213174,0.0007661216,0.00047102306,0.0013393566,0.001978368,0.05234784,0.044157553,0.002863776,0.047443405,0.26569414],"study_design_scores_gemma":[0.000043265132,0.000048257094,0.952353,0.00004841239,0.00011101264,0.00027108332,0.0011316467,0.017325433,0.010329089,0.00029109887,0.017914636,0.00013307169],"about_ca_topic_score_codex":0.9505093,"about_ca_topic_score_gemma":0.98478633,"teacher_disagreement_score":0.04949069,"about_ca_system_score_codex":0.008101531,"about_ca_system_score_gemma":0.012772198,"threshold_uncertainty_score":0.099564254},"labels":[],"label_agreement":null},{"id":"W4247415567","doi":"10.1007/978-3-7643-8757-0_1","title":"Earthquakes: Simulations, Sources and Tsunamis","year":2008,"lang":"en","type":"book-chapter","venue":"Birkhäuser Basel eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Death toll; Seismology; Toll; Natural hazard; Natural disaster; Geography; Geology; Socioeconomics; Meteorology; Medicine","score_opus":0.02585599490281296,"score_gpt":0.20186562634304508,"score_spread":0.17600963144023213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247415567","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.028741466,0.009681613,0.547518,0.0049304087,0.0014272402,0.00024135884,0.022937607,0.013821794,0.37070045],"genre_scores_gemma":[0.3814454,0.01872824,0.34168413,0.0009956667,0.0009375549,0.0011270929,0.021956349,0.0050124195,0.22811314],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990344,0.000031366668,0.0000075478342,0.000013833679,0.000035114368,0.000008682005],"domain_scores_gemma":[0.99968314,0.00018234744,0.000016212898,0.000032499986,0.00006156777,0.000024180565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002712839,0.0007962961,0.0005859726,0.0003510515,0.00040402,0.0014414912,0.0012582337,0.0013261013,0.029588992],"category_scores_gemma":[0.0013104791,0.00053025346,0.000453587,0.0010985339,0.0003091835,0.0016782457,0.0007760057,0.0008051314,0.008314171],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048529702,0.00006731477,0.0013035734,0.00029621244,0.000046432957,0.00010233373,0.00014228158,0.72597194,0.00040433227,0.07082636,0.11885182,0.081938885],"study_design_scores_gemma":[0.000047912625,0.000015141809,0.0005229313,0.00009753997,0.00001677987,0.000104618564,0.00007243621,0.78466827,0.00041717486,0.07454026,0.13947251,0.000024429848],"about_ca_topic_score_codex":0.009814551,"about_ca_topic_score_gemma":0.011533101,"teacher_disagreement_score":0.029588992,"about_ca_system_score_codex":0.0004052335,"about_ca_system_score_gemma":0.00046730423,"threshold_uncertainty_score":0.098985076},"labels":[],"label_agreement":null},{"id":"W4247800108","doi":"10.1142/s1793431108000311","title":"TSUNAMI EARLY WARNING SYSTEM — AN INDIAN OCEAN PERSPECTIVE","year":2008,"lang":"en","type":"article","venue":"Journal of Earthquake and Tsunami","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Indian ocean; Warning system; Seismology; Early warning system; Geology; Archipelago; Geography; Meteorology; Cartography; Oceanography; Computer science; Telecommunications","score_opus":0.016449652465529083,"score_gpt":0.2170988037597437,"score_spread":0.20064915129421462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247800108","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15482773,0.08183491,0.20559709,0.10665074,0.0071108304,0.00083173916,0.020251721,0.025802517,0.39709267],"genre_scores_gemma":[0.87165487,0.042090666,0.041588426,0.00341259,0.0013067758,0.00018710285,0.008881382,0.00035121822,0.03052688],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994467,0.000102438375,0.00007440265,0.00006014345,0.00020950685,0.00010693331],"domain_scores_gemma":[0.9986368,0.00014477046,0.00011647852,0.000092338174,0.00082926545,0.00018033941],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001278324,0.00056153064,0.00034075373,0.0030764986,0.0005835866,0.0045251744,0.0010150418,0.0007842922,0.0029616684],"category_scores_gemma":[0.0020979624,0.00024834232,0.0003406985,0.0038827925,0.00046634255,0.0022710143,0.0013908282,0.0015102711,0.0017173126],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046723773,0.00025610474,0.041969307,0.0011979648,0.00018630987,0.00091088086,0.0008231179,0.029723983,0.011465364,0.041815184,0.12301057,0.7481739],"study_design_scores_gemma":[0.00005030803,0.000561174,0.09940372,0.0013389082,0.0004862896,0.0013394377,0.0052664406,0.1770471,0.011662272,0.015991595,0.6864972,0.00035559293],"about_ca_topic_score_codex":0.044489875,"about_ca_topic_score_gemma":0.019682804,"teacher_disagreement_score":0.044489875,"about_ca_system_score_codex":0.0015760012,"about_ca_system_score_gemma":0.002856382,"threshold_uncertainty_score":0.08846182},"labels":[],"label_agreement":null},{"id":"W4247818489","doi":"10.1080/01490410601008895","title":"Analysis of the Tsunami of December 26, 2004, on the Kerala Coast of India—Part II: Arrival Times","year":2006,"lang":"en","type":"article","venue":"Marine Geodesy","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; York University","funders":"","keywords":"Geography; Tsunami wave; Arrival time; Morning; Indian ocean; Oceanography; Seismology; Geology; Engineering; Medicine","score_opus":0.008474281869954099,"score_gpt":0.19108390548283297,"score_spread":0.18260962361287886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4247818489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99684626,0.000058542904,0.00016383993,0.000025139401,0.0000043166233,0.000011715807,0.00082033244,0.000009717351,0.0020601493],"genre_scores_gemma":[0.99628216,0.00015949535,0.00026579073,0.000008376827,0.000009989634,0.000016755534,0.001766881,0.000006977874,0.0014836349],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998841,0.000011565978,0.00001567395,0.000016299417,0.000024253934,0.000048212998],"domain_scores_gemma":[0.9992254,0.00022585741,0.00014546157,0.00003275619,0.000260185,0.00011046079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012157851,0.00027772656,0.00020915274,0.0020841209,0.00057915034,0.0006492395,0.00027085748,0.00020658747,0.0017819979],"category_scores_gemma":[0.0010942145,0.00015317295,0.00034054148,0.002371815,0.00018851181,0.00018527238,0.00037060998,0.00033640748,0.0005347237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006246443,0.00011745463,0.9443365,0.00015831045,0.00017959002,0.002057521,0.005273428,0.007985083,0.010611608,0.0007756269,0.0017839741,0.026096327],"study_design_scores_gemma":[0.0000032543253,0.000052858417,0.9946843,0.0000055773176,0.000029706274,0.00016411381,0.0024388793,0.0008225788,0.00063941913,0.000019185796,0.0011293154,0.0000109820485],"about_ca_topic_score_codex":0.06702958,"about_ca_topic_score_gemma":0.08329628,"teacher_disagreement_score":0.06702958,"about_ca_system_score_codex":0.00057440606,"about_ca_system_score_gemma":0.00051303365,"threshold_uncertainty_score":0.1332789},"labels":[],"label_agreement":null},{"id":"W4248489858","doi":"10.1007/978-1-4020-4410-6_101","title":"Lake Outbursts","year":2012,"lang":"en","type":"book-chapter","venue":"Encyclopedia of earth sciences series/Encyclopedia of earth sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke; Université Laval","funders":"","keywords":"Geography; Environmental science; Geology","score_opus":0.023676669884801556,"score_gpt":0.23077152488882643,"score_spread":0.20709485500402489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248489858","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.067604914,0.002748484,0.0014201947,0.008239844,0.00087884784,0.000086378925,0.004360349,0.0007578238,0.9139031],"genre_scores_gemma":[0.41604963,0.00472385,0.0010672807,0.0014884467,0.00044111526,0.00008668291,0.0053100204,0.00047293986,0.57036],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998221,0.000012398179,0.000009656615,0.000026711354,0.00006774378,0.00006150004],"domain_scores_gemma":[0.99977607,0.000020143698,0.00005406147,0.000021493073,0.000053366806,0.000074845346],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021476483,0.00027933368,0.00020499887,0.0009532551,0.0014054887,0.0018136961,0.00041726168,0.00043370033,0.07890917],"category_scores_gemma":[0.0010590864,0.0001639186,0.00022426921,0.0013135312,0.00042794787,0.001581689,0.0023012825,0.0007916802,0.008143012],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031043592,0.00006730107,0.024215057,0.0005008285,0.00004838918,0.0011306215,0.0061667063,0.0007838566,0.0019416619,0.08559972,0.5629424,0.31629315],"study_design_scores_gemma":[0.000012477592,0.00002920779,0.025333684,0.00011312924,0.000015280199,0.00023309732,0.0025080708,0.0002756926,0.00044040137,0.005789632,0.9652357,0.000013550086],"about_ca_topic_score_codex":0.015285484,"about_ca_topic_score_gemma":0.051297758,"teacher_disagreement_score":0.07890917,"about_ca_system_score_codex":0.0012503999,"about_ca_system_score_gemma":0.0013064494,"threshold_uncertainty_score":0.26397747},"labels":[],"label_agreement":null},{"id":"W4248676580","doi":"10.1002/essoar.10503048.1","title":"Injection-induced earthquakes on complex fault zones of the Raton Basin illuminated by machine-learning phase picker and dense nodal array","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Seismology; Induced seismicity; Hypocenter; Geology; Basement; Tectonics; Structural basin; Focal mechanism; Fault (geology); Magnitude (astronomy); Geomorphology; Engineering","score_opus":0.033723545208832965,"score_gpt":0.2508736069233318,"score_spread":0.21715006171449885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248676580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991386,0.000022535318,0.00016664308,0.000010864318,0.000002576444,0.000003538819,0.0003036888,0.000028293562,0.00032310307],"genre_scores_gemma":[0.9989291,0.000016612905,0.00029568505,0.000002561236,0.0000027788221,0.0000021457845,0.00056171214,0.0000035747607,0.00018592279],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999243,0.0000106525395,0.0000051222846,0.000022881233,0.000015411624,0.000021685095],"domain_scores_gemma":[0.99984634,0.000018383382,0.00004276731,0.000016856739,0.000043760305,0.000031846565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000109497414,0.00027696052,0.00013369587,0.001050554,0.00017334023,0.00022766743,0.00020090779,0.0001696741,0.0009730765],"category_scores_gemma":[0.0002909373,0.00010887687,0.00012567657,0.00086505234,0.00022160394,0.00017316693,0.00027205265,0.00009715653,0.00013372544],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039452047,0.00012745197,0.9086442,0.00008147898,0.00007468416,0.0012261024,0.0006974131,0.014864877,0.027270341,0.0003797978,0.0014360988,0.044802897],"study_design_scores_gemma":[0.0000053613135,0.00003292039,0.9794447,0.0000074894524,0.00001632739,0.00009972034,0.00018686475,0.018651403,0.0010751187,0.00006088188,0.00041193544,0.0000072480484],"about_ca_topic_score_codex":0.026761316,"about_ca_topic_score_gemma":0.05928833,"teacher_disagreement_score":0.026761316,"about_ca_system_score_codex":0.0002794149,"about_ca_system_score_gemma":0.00029256282,"threshold_uncertainty_score":0.053211093},"labels":[],"label_agreement":null},{"id":"W4248750099","doi":"10.1002/essoar.10502973.2","title":"Earthquake rupture through a step-over fault system: An exploratory numerical study of the Leech River Fault, southern Vancouver Island","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geology; Fault (geology); Offset (computer science); Shear stress; Shear (geology); Slip (aerodynamics); Jump; Stress (linguistics); Engineering; Mechanics; Physics; Petrology; Computer science; Aerospace engineering","score_opus":0.029106665895469442,"score_gpt":0.23898057080511492,"score_spread":0.20987390490964547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248750099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982672,0.000037760474,0.00019689229,0.00008158526,0.0000028799468,0.0000091875545,0.00014565619,0.000014336975,0.0012444955],"genre_scores_gemma":[0.998787,0.000033487726,0.00047674088,0.000022450242,0.0000021268124,0.000009686129,0.00018548196,0.000006791633,0.00047621242],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998853,0.000023227114,0.00000629192,0.000024479368,0.000020004569,0.00004064805],"domain_scores_gemma":[0.99950707,0.00020849518,0.00005395855,0.00002795123,0.00007145081,0.00013098412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022260752,0.00044605084,0.00048659922,0.00055241387,0.0008848036,0.0010657619,0.0010950331,0.0015690902,0.0015269687],"category_scores_gemma":[0.0012635371,0.00038256444,0.00046066914,0.0007143813,0.0009375535,0.00038368133,0.0007094932,0.0006869864,0.000113568305],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003425089,0.00049723074,0.09530571,0.0000846801,0.00017748651,0.0014163468,0.00031157906,0.89250356,0.0034881108,0.0012617918,0.0010199592,0.003591012],"study_design_scores_gemma":[0.00010178443,0.00010650359,0.02441239,0.000015719366,0.00003549177,0.000063363485,0.000632616,0.9736908,0.00035050052,0.0002557265,0.00031020644,0.00002491311],"about_ca_topic_score_codex":0.25517946,"about_ca_topic_score_gemma":0.2647001,"teacher_disagreement_score":0.74482054,"about_ca_system_score_codex":0.0018260872,"about_ca_system_score_gemma":0.0016890038,"threshold_uncertainty_score":0.50738835},"labels":[],"label_agreement":null},{"id":"W4248764488","doi":"10.1002/essoar.10503731.2","title":"Statistical Modeling and Characterization of Induced Seismicity within the Western Canada Sedimentary Basin","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Induced seismicity; Aftershock; Seismology; Geology; Tectonics; Structural basin; Magnitude (astronomy); Sedimentary rock; Maximum magnitude; Paleontology","score_opus":0.032630929964655685,"score_gpt":0.21983278836351974,"score_spread":0.18720185839886405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248764488","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99541533,0.000043748067,0.0032332197,0.000059335987,0.0000022734553,0.000021689644,0.00065938936,0.00003676663,0.0005283407],"genre_scores_gemma":[0.9971782,0.000055551303,0.0009944803,0.0000071791883,0.0000023913049,0.00001086337,0.0011392172,0.0000067638366,0.00060543226],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996717,0.000042959186,0.00002178993,0.000089860805,0.00008126466,0.00009237967],"domain_scores_gemma":[0.998933,0.0003776284,0.0001746983,0.000082617546,0.0003299506,0.00010211493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005585212,0.0002587664,0.0002602001,0.0011900017,0.0005765914,0.0007923364,0.00077664404,0.00023233832,0.0007424088],"category_scores_gemma":[0.002930813,0.00017841942,0.0004233527,0.0013357786,0.000731171,0.00022483572,0.00041104676,0.00034305739,0.00007700102],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013522206,0.00007105304,0.60374445,0.000036650454,0.00022140628,0.00036920037,0.000516962,0.36566657,0.0025419204,0.0032786685,0.0010907643,0.022327129],"study_design_scores_gemma":[0.0000072147122,0.000026271748,0.40164316,0.0000073374677,0.000036392394,0.000037226753,0.00051129586,0.5957489,0.00040142695,0.00065533153,0.0009029303,0.000022495067],"about_ca_topic_score_codex":0.9364519,"about_ca_topic_score_gemma":0.9029726,"teacher_disagreement_score":0.06354809,"about_ca_system_score_codex":0.0053756144,"about_ca_system_score_gemma":0.0056455373,"threshold_uncertainty_score":0.12784463},"labels":[],"label_agreement":null},{"id":"W4248798752","doi":"10.1190/tle38100813.1","title":"Reviews","year":2019,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"College of Veterinarians of British Columbia","funders":"","keywords":"Publishing; Scientific publishing; Library science; Sociology; Political science; Computer science; Law","score_opus":0.03646001362129933,"score_gpt":0.2454301433010226,"score_spread":0.20897012967972328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4248798752","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004807368,0.67535585,0.0018533428,0.031035908,0.06464162,0.00014786168,0.0033263946,0.0007714272,0.22238684],"genre_scores_gemma":[0.0036879987,0.6337423,0.0027809832,0.025341319,0.03723066,0.0001834483,0.0056139273,0.00056853023,0.2908509],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986461,0.000186732,0.00014591812,0.00025280527,0.0006467237,0.00012172165],"domain_scores_gemma":[0.99710065,0.00076229207,0.00022448543,0.0002496904,0.001299294,0.00036345926],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010773317,0.001114036,0.0013667698,0.0034681763,0.00076314283,0.0045057978,0.0023327135,0.0025446415,0.25889617],"category_scores_gemma":[0.006095167,0.00043237032,0.0008619648,0.0033345942,0.00077839935,0.0034869185,0.0020661012,0.002511946,0.19811742],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028732655,0.000020451984,0.00006460434,0.0021424615,0.0000147604,0.00009700221,0.00007459879,0.000056884033,0.00022442655,0.0037398937,0.7987957,0.19474053],"study_design_scores_gemma":[0.000002317388,0.0000041869534,0.000058900998,0.0005319432,0.000004235443,0.00012976602,0.000020614587,0.0000040433074,0.000021952761,0.0005611121,0.9986583,0.0000026235289],"about_ca_topic_score_codex":0.002300641,"about_ca_topic_score_gemma":0.0032930607,"teacher_disagreement_score":0.7411038,"about_ca_system_score_codex":0.0015851075,"about_ca_system_score_gemma":0.0041128346,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4249098108","doi":"10.1002/essoar.10501237.2","title":"Correlating earthquake static stress drop values with fault complexity in the 2016 Amatrice-Norcia earthquake sequence, Central Italy","year":2019,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Seismic moment; Geology; Aftershock; Sequence (biology); Fault (geology); Earthquake simulation; Earthquake swarm; Moment magnitude scale; Induced seismicity; Scaling; Mathematics; Geometry","score_opus":0.05076797802312211,"score_gpt":0.25960635289723366,"score_spread":0.20883837487411155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4249098108","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99803275,0.00010323438,0.00013793736,0.000032985274,0.000008168103,0.000009329361,0.00082099834,0.000021987016,0.00083256],"genre_scores_gemma":[0.9965867,0.000095570984,0.00023114607,0.000010458045,0.000029700965,0.000013018797,0.0027870573,0.000011212656,0.0002352267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977297,0.000024761597,0.000025085681,0.00007443652,0.000050418796,0.000052361946],"domain_scores_gemma":[0.9990707,0.00011365261,0.0004346118,0.00011113468,0.00015404087,0.00011600898],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034853234,0.00037717,0.0003077026,0.00174507,0.00018788286,0.0006716788,0.00028593309,0.00031825888,0.0006438813],"category_scores_gemma":[0.002469991,0.00016380407,0.00023634845,0.0012924802,0.00045304923,0.0002532341,0.0006752096,0.00021150507,0.0003413818],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022468397,0.000045731587,0.980135,0.00005455636,0.00006497031,0.00034712875,0.0005257784,0.0028894546,0.0037902482,0.0001016558,0.0011932495,0.010627526],"study_design_scores_gemma":[0.0000050058657,0.000010196123,0.9989303,0.0000045377815,0.0000057585685,0.000042755117,0.000052108968,0.0006154948,0.00005798044,0.0000135635755,0.00025933734,0.000002921124],"about_ca_topic_score_codex":0.026859825,"about_ca_topic_score_gemma":0.03266464,"teacher_disagreement_score":0.026859825,"about_ca_system_score_codex":0.0005751909,"about_ca_system_score_gemma":0.00031809747,"threshold_uncertainty_score":0.053406954},"labels":[],"label_agreement":null},{"id":"W4250477124","doi":"10.1007/978-3-7643-8364-0_2","title":"The 26 December 2004 Sumatra Tsunami: Analysis of Tide Gauge Data from the World Ocean Part 1. Indian Ocean and South Africa","year":2007,"lang":"en","type":"book-chapter","venue":"Birkhäuser Basel eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Tide gauge; Indian ocean; Oceanography; Geology; Tsunami wave; Seismology; Climatology; Tsunami earthquake; Geography; Sea level","score_opus":0.06334815100108626,"score_gpt":0.24119429356500086,"score_spread":0.1778461425639146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250477124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90871274,0.021307217,0.0050551505,0.0015576365,0.00021778808,0.00009764406,0.016477628,0.00029155886,0.04628268],"genre_scores_gemma":[0.8467428,0.032795507,0.010710494,0.0003203867,0.00025614517,0.000135769,0.041373093,0.00021812793,0.067447655],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.999944,0.000009256682,0.000005607162,0.0000091935835,0.000025710306,0.000006186376],"domain_scores_gemma":[0.9997559,0.00009382713,0.000056615798,0.00001933529,0.000053151794,0.000021202959],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018797263,0.00033070587,0.00016924269,0.0014097489,0.00024367179,0.0007755439,0.00031212476,0.00015549838,0.0017273994],"category_scores_gemma":[0.0010581142,0.00020308897,0.00013290069,0.0032314847,0.00023936074,0.00040323526,0.0003851536,0.00020955235,0.0008327953],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010620927,0.00009774449,0.26760766,0.0005171687,0.00010715524,0.0025383634,0.0045960224,0.01071338,0.0070140287,0.002582195,0.07866096,0.62545925],"study_design_scores_gemma":[0.000006173358,0.00003789731,0.9010442,0.00009785835,0.000036773043,0.0008796532,0.0011247873,0.003222107,0.0014192774,0.001185122,0.090924345,0.000021833252],"about_ca_topic_score_codex":0.025630455,"about_ca_topic_score_gemma":0.078599915,"teacher_disagreement_score":0.025630455,"about_ca_system_score_codex":0.0008601201,"about_ca_system_score_gemma":0.0005539944,"threshold_uncertainty_score":0.050962508},"labels":[],"label_agreement":null},{"id":"W4250657049","doi":"10.4095/293321","title":"Ground deformation produced by 2013 M6.4 Bushehr earthquake in Iran mapped with RADARSAT-2 DInSAR","year":2013,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Geodesy; Seismology; Deformation (meteorology); Remote sensing; Oceanography","score_opus":0.029172925529539106,"score_gpt":0.22323664571893304,"score_spread":0.19406372018939394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250657049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930102,0.000096168485,0.00018262891,0.00009753974,0.00003136976,0.000022564212,0.004668543,0.000046025198,0.001844937],"genre_scores_gemma":[0.98846453,0.00024086218,0.0005336382,0.0000366892,0.000030300142,0.000017301587,0.009287822,0.000007903134,0.0013809692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998727,0.000008607902,0.000010470088,0.000022111275,0.00004462436,0.000041521675],"domain_scores_gemma":[0.999818,0.000008866663,0.00004932197,0.000015467067,0.000079452104,0.000028845654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002180875,0.00047581663,0.00028065158,0.0010639769,0.00029633092,0.0002469111,0.0003233369,0.00040196432,0.0008294283],"category_scores_gemma":[0.00027142826,0.00017734358,0.00026116642,0.0016644337,0.0001744826,0.00025886338,0.00028672366,0.0002754448,0.0003998537],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015342138,0.00049529155,0.8800588,0.0002949997,0.00026919137,0.0026953768,0.0010616521,0.013653689,0.02616881,0.0005151045,0.021849398,0.05140339],"study_design_scores_gemma":[0.000030702515,0.00004458996,0.9950787,0.000008775353,0.00003490463,0.00014406355,0.00037771548,0.0013894223,0.0010867433,0.000027880676,0.0017675933,0.000008985579],"about_ca_topic_score_codex":0.061111026,"about_ca_topic_score_gemma":0.0859303,"teacher_disagreement_score":0.061111026,"about_ca_system_score_codex":0.00070612156,"about_ca_system_score_gemma":0.0010667788,"threshold_uncertainty_score":0.121510625},"labels":[],"label_agreement":null},{"id":"W4250828927","doi":"10.5194/se-2017-123","title":"Pseudotachylyte as field evidence for lower crustal earthquakes during the intracontinental Petermann Orogeny (Musgrave Block, Central Australia)","year":2017,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Geology; Continental crust; Crust; Orogeny; Shearing (physics); Seismology; Mylonite; Slip (aerodynamics); Induced seismicity; Petrology; Shear zone; Tectonics; Geophysics; Geotechnical engineering","score_opus":0.06328580762373501,"score_gpt":0.311021992274597,"score_spread":0.24773618465086197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4250828927","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994548,0.000029483024,0.000027013688,0.0000058268233,5.68175e-7,0.0000025360061,0.000066449,0.0000014100322,0.0004120447],"genre_scores_gemma":[0.9994936,0.00003440431,0.00005976934,0.000004321051,0.0000013253477,0.0000032136231,0.00014140044,0.0000011811801,0.00026087437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998877,0.000019303934,0.000007982414,0.000033668235,0.000027184362,0.000024117518],"domain_scores_gemma":[0.99961495,0.0000398814,0.00014556604,0.00002662391,0.00010247076,0.000070393005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017074576,0.0001590905,0.00014133182,0.0010537204,0.00035340778,0.0002770696,0.00019434356,0.00018746841,0.00092678604],"category_scores_gemma":[0.00051698164,0.00012530835,0.00007843235,0.0008157382,0.0004333375,0.00018686414,0.0004669836,0.00012733047,0.00013255997],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011400349,0.000024756295,0.97503996,0.000033576438,0.000023564771,0.0003580496,0.0027144921,0.000106805055,0.015255469,0.00009610315,0.00012351427,0.0061095944],"study_design_scores_gemma":[4.2371383e-7,0.0000076794895,0.9996722,0.0000013466369,0.0000014573395,0.000027602893,0.0001335333,0.000030691866,0.000062916915,0.0000032108394,0.000058353686,4.5998482e-7],"about_ca_topic_score_codex":0.064178176,"about_ca_topic_score_gemma":0.14036314,"teacher_disagreement_score":0.064178176,"about_ca_system_score_codex":0.0004640051,"about_ca_system_score_gemma":0.00029733617,"threshold_uncertainty_score":0.1276092},"labels":[],"label_agreement":null},{"id":"W4251036703","doi":"10.1002/essoar.10504862.1","title":"Benchmarking Scenario Performance in the First Generation Canadian Seismic Risk Assessment","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; Geological Survey of Canada","funders":"","keywords":"Benchmarking; Seismic risk; Context (archaeology); Risk assessment; Earthquake scenario; Disaster risk reduction; Hazard; Seismic hazard; Urban seismic risk; Benchmark (surveying); Population; Environmental resource management; Environmental science; Geography; Computer science; Engineering; Business; Civil engineering; Cartography; Environmental health; Computer security","score_opus":0.03398216874890846,"score_gpt":0.2276743511897054,"score_spread":0.19369218244079692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251036703","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91660595,0.00085810554,0.023363318,0.001798181,0.00015714818,0.00041251606,0.02116496,0.0022779098,0.033361927],"genre_scores_gemma":[0.9667099,0.000309683,0.015361471,0.00014017563,0.000012004508,0.000063611435,0.015607865,0.00014085961,0.0016544148],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99840075,0.0003857083,0.00007262971,0.00036176245,0.0004924482,0.00028666822],"domain_scores_gemma":[0.996876,0.0006899216,0.00013951035,0.00039607572,0.0016465567,0.00025191598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0034829692,0.0015880028,0.0005475659,0.0016509214,0.0013110889,0.0019459903,0.002806345,0.000973343,0.0018578157],"category_scores_gemma":[0.007933789,0.00046066407,0.0011027172,0.0022360606,0.00090888835,0.0014220855,0.001316991,0.0011060891,0.0003006261],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020502802,0.00008473568,0.017609827,0.00007022363,0.00014060439,0.000077513214,0.000072619,0.9633512,0.0005356982,0.0021149607,0.004117579,0.011620021],"study_design_scores_gemma":[0.00008513456,0.000109304834,0.024364963,0.00003416372,0.0000633928,0.000038711383,0.00028300783,0.9657478,0.0018288877,0.0016554311,0.005692754,0.00009653469],"about_ca_topic_score_codex":0.9524038,"about_ca_topic_score_gemma":0.95360744,"teacher_disagreement_score":0.047596216,"about_ca_system_score_codex":0.0223618,"about_ca_system_score_gemma":0.016091486,"threshold_uncertainty_score":0.162247},"labels":[],"label_agreement":null},{"id":"W4251504044","doi":"10.1007/978-3-319-57822-4_19","title":"Real-Time Assessment of the 16 September 2015 Chile Tsunami and Implications for Near-Field Forecast","year":2017,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Epicenter; Seismology; Geology; Geography; Quarter (Canadian coin); Climatology; Archaeology","score_opus":0.026672785810993752,"score_gpt":0.27726481659032903,"score_spread":0.2505920307793353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251504044","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5391087,0.010083124,0.020800456,0.023565825,0.0017691607,0.00012270563,0.029207753,0.0012557952,0.37408653],"genre_scores_gemma":[0.92016196,0.0036238967,0.0060726074,0.00025332786,0.00018630548,0.000043492564,0.00794418,0.000111244066,0.061603095],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99992955,0.000013007905,0.000004738344,0.000011409487,0.000029841374,0.000011489283],"domain_scores_gemma":[0.9997491,0.00007281316,0.000035364545,0.000016430424,0.000098828714,0.000027387034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041696723,0.00018080557,0.00013118557,0.00063140347,0.00021456467,0.0014774962,0.00041407268,0.00046532083,0.009611639],"category_scores_gemma":[0.001895348,0.00011290595,0.00017756558,0.000846554,0.00021939709,0.0013092976,0.0005022455,0.0004149222,0.0014509679],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028422623,0.000118042924,0.12761065,0.0006707477,0.00010681594,0.0012338758,0.0020363433,0.2102036,0.0051538954,0.034849487,0.19426723,0.42346504],"study_design_scores_gemma":[0.00008141536,0.00014310537,0.40015182,0.0010608488,0.00007210105,0.00037631183,0.009762551,0.19832258,0.0034987638,0.033761196,0.35256654,0.00020280918],"about_ca_topic_score_codex":0.13238001,"about_ca_topic_score_gemma":0.18361591,"teacher_disagreement_score":0.13238001,"about_ca_system_score_codex":0.0027293141,"about_ca_system_score_gemma":0.0014632758,"threshold_uncertainty_score":0.26321894},"labels":[],"label_agreement":null},{"id":"W4251814165","doi":"10.31223/osf.io/x9wjz","title":"Brittle Deformation of Carbonated Peridotite – Insights from Listvenites of the Samail Ophiolite (Oman Drilling Project Hole BT1B)","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Japan Agency for Marine-Earth Science and Technology; Sultan Qaboos University; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; University of Southampton; Alfred P. Sloan Foundation; Deutsche Forschungsgemeinschaft; Japan Society for the Promotion of Science; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Peridotite; Cataclastic rock; Geochemistry; Ophiolite; Petrology; Shear zone; Metamorphic rock; Mantle (geology); Tectonics; Seismology","score_opus":0.028923010739334423,"score_gpt":0.21925680900602038,"score_spread":0.19033379826668595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4251814165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990484,0.000103213555,0.000054313423,0.000009029673,0.0000011045638,0.0000036917877,0.00021851288,0.0000051647153,0.0005565055],"genre_scores_gemma":[0.99935013,0.00006514403,0.00013493559,0.0000058437754,0.0000022711945,0.0000031070147,0.0002065183,0.0000051648462,0.00022696637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998754,0.0000070329847,0.000010689927,0.000032523913,0.000041426858,0.00003277044],"domain_scores_gemma":[0.9998857,0.000010636241,0.000045544162,0.000009902124,0.00003222126,0.000016018028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001413701,0.00024249581,0.00018263615,0.0020842855,0.00056472694,0.0007511256,0.0003170469,0.00036945086,0.0011638197],"category_scores_gemma":[0.00023630405,0.00021298561,0.000166958,0.0010630231,0.00039469844,0.00031869943,0.00046589095,0.00014409819,0.0001691001],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024904072,0.000049422702,0.72742844,0.00016348339,0.0000750412,0.001168538,0.0020929775,0.00084266835,0.25009087,0.0001903636,0.00020870396,0.017440515],"study_design_scores_gemma":[0.0000020166317,0.000012936012,0.99745184,0.0000048104316,0.000005483886,0.00013613654,0.00022303611,0.0003030024,0.0013976299,0.000014386958,0.00044616094,0.0000026134715],"about_ca_topic_score_codex":0.03278836,"about_ca_topic_score_gemma":0.072716065,"teacher_disagreement_score":0.03278836,"about_ca_system_score_codex":0.0006219539,"about_ca_system_score_gemma":0.00024613802,"threshold_uncertainty_score":0.065195024},"labels":[],"label_agreement":null},{"id":"W4252396020","doi":"10.31223/x5kw3s","title":"Cascadia megathrust earthquake rupture model constrained by geodetic fault locking","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Subduction; Seismology; Earthquake rupture; Episodic tremor and slip; Fault (geology); Tide gauge; Geodetic datum; Slip (aerodynamics); Interplate earthquake; Margin (machine learning); Subsidence; Tsunami earthquake; Geodesy; Tectonics; Sea level; Geomorphology; Oceanography","score_opus":0.028569007873629804,"score_gpt":0.23088969626870728,"score_spread":0.20232068839507747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252396020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9735135,0.0002479064,0.017042583,0.00039501322,0.00003595715,0.00003278,0.0008540544,0.00017392228,0.0077043823],"genre_scores_gemma":[0.9978606,0.000069827365,0.0005671549,0.000017491371,0.000005682501,0.00002578466,0.00020902143,0.000012843519,0.0012314988],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998783,0.000026728245,0.000009983606,0.000037844184,0.000014444475,0.000032639688],"domain_scores_gemma":[0.9996389,0.00008032277,0.00010460609,0.000033407727,0.00005957366,0.00008318319],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028163532,0.0006444016,0.0006582789,0.00048201074,0.0004567474,0.00089667743,0.001620751,0.0013197435,0.0025622477],"category_scores_gemma":[0.0010477823,0.00045733334,0.00077332667,0.00041294572,0.0006490796,0.0005668249,0.0006998229,0.0005536566,0.000248029],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032743104,0.000015176884,0.0038223462,0.000010747181,0.000015824715,0.00011070988,0.000021526495,0.99405575,0.00047348067,0.0010165178,0.00011352936,0.0003117073],"study_design_scores_gemma":[0.000014620734,0.000010315479,0.00076397957,0.00000232391,0.0000073004207,0.000010317743,0.000011947089,0.9987382,0.00004188241,0.00033142033,0.00006410334,0.0000036001452],"about_ca_topic_score_codex":0.045306675,"about_ca_topic_score_gemma":0.016983105,"teacher_disagreement_score":0.045306675,"about_ca_system_score_codex":0.0011288223,"about_ca_system_score_gemma":0.0009946664,"threshold_uncertainty_score":0.09008592},"labels":[],"label_agreement":null},{"id":"W4253889985","doi":"10.1002/essoar.10502973.4","title":"Earthquake rupture through a step-over fault system: An exploratory numerical study of the Leech River Fault, southern Vancouver Island","year":2020,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geology; Fault (geology); Offset (computer science); Shear stress; Shear (geology); Jump; Slip (aerodynamics); Stress (linguistics); Engineering; Mechanics; Petrology; Physics; Computer science","score_opus":0.029106665895469442,"score_gpt":0.23898057080511492,"score_spread":0.20987390490964547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4253889985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982672,0.000037760474,0.00019689229,0.00008158526,0.0000028799468,0.0000091875545,0.00014565619,0.000014336975,0.0012444955],"genre_scores_gemma":[0.998787,0.000033487726,0.00047674088,0.000022450242,0.0000021268124,0.000009686129,0.00018548196,0.000006791633,0.00047621242],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998853,0.000023227114,0.00000629192,0.000024479368,0.000020004569,0.00004064805],"domain_scores_gemma":[0.99950707,0.00020849518,0.00005395855,0.00002795123,0.00007145081,0.00013098412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022260752,0.00044605084,0.00048659922,0.00055241387,0.0008848036,0.0010657619,0.0010950331,0.0015690902,0.0015269687],"category_scores_gemma":[0.0012635371,0.00038256444,0.00046066914,0.0007143813,0.0009375535,0.00038368133,0.0007094932,0.0006869864,0.000113568305],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003425089,0.00049723074,0.09530571,0.0000846801,0.00017748651,0.0014163468,0.00031157906,0.89250356,0.0034881108,0.0012617918,0.0010199592,0.003591012],"study_design_scores_gemma":[0.00010178443,0.00010650359,0.02441239,0.000015719366,0.00003549177,0.000063363485,0.000632616,0.9736908,0.00035050052,0.0002557265,0.00031020644,0.00002491311],"about_ca_topic_score_codex":0.25517946,"about_ca_topic_score_gemma":0.2647001,"teacher_disagreement_score":0.74482054,"about_ca_system_score_codex":0.0018260872,"about_ca_system_score_gemma":0.0016890038,"threshold_uncertainty_score":0.50738835},"labels":[],"label_agreement":null},{"id":"W4254147212","doi":"10.1190/tle23070704.1","title":"Reviews","year":2004,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"BC Studies; Memorial University of Newfoundland","funders":"","keywords":"Seismogram; Interpretation (philosophy); Geology; Humanities; Philosophy; Seismology","score_opus":0.0476000100464794,"score_gpt":0.25552760932873975,"score_spread":0.20792759928226034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254147212","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00052675966,0.5496136,0.0021797619,0.034957707,0.054433826,0.00019582268,0.0050092256,0.0011503388,0.35193294],"genre_scores_gemma":[0.0039274585,0.45564893,0.0026051172,0.023937758,0.022824356,0.00020387201,0.0073076217,0.00066056265,0.4828844],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99865615,0.0001629606,0.00012387105,0.00027677102,0.000646547,0.00013356077],"domain_scores_gemma":[0.9974437,0.00053187145,0.0001746912,0.00024722115,0.001250524,0.0003520547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010299585,0.001189956,0.0013306076,0.003582831,0.0008671618,0.004297602,0.0024475965,0.0025500015,0.32938474],"category_scores_gemma":[0.005719382,0.00046100258,0.0008226548,0.0036732436,0.0007674609,0.003073261,0.0021099537,0.0023383643,0.28499368],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023515564,0.000018387896,0.00006919153,0.0011457375,0.00000968781,0.00007503353,0.000051340918,0.000049428687,0.00017210352,0.0028367445,0.83955723,0.15599164],"study_design_scores_gemma":[0.0000022929487,0.0000037588773,0.00007283047,0.00033269147,0.0000030607814,0.0000944866,0.000017995235,0.0000043461923,0.000019912812,0.00050050946,0.9989459,0.0000022294432],"about_ca_topic_score_codex":0.0032778287,"about_ca_topic_score_gemma":0.0047260225,"teacher_disagreement_score":0.32938474,"about_ca_system_score_codex":0.0018409974,"about_ca_system_score_gemma":0.00412306,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4254955980","doi":"10.4095/296822","title":"Regional centroid moment tensor solutions for eastern Canadian earthquakes: 2014","year":2015,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Centroid; Moment tensor; Moment (physics); Geology; Seismology; Tensor (intrinsic definition); Geodesy; Geography; Computer science; Mathematics; Physics; Geometry; Artificial intelligence; Classical mechanics","score_opus":0.10672379547159248,"score_gpt":0.2693418569616776,"score_spread":0.16261806149008512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4254955980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9345413,0.0005959952,0.003723521,0.00026175083,0.000043505894,0.00009921023,0.049512636,0.0003694522,0.010852576],"genre_scores_gemma":[0.9442831,0.00064297457,0.009530964,0.000025506182,0.000017263908,0.000037705475,0.040005792,0.00009581969,0.0053609023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99965966,0.0000071518484,0.00002149588,0.000045121436,0.00016165095,0.000105061365],"domain_scores_gemma":[0.99877805,0.00002428688,0.00011782415,0.00004397131,0.00093722576,0.000098491495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033764335,0.0006190856,0.00027117762,0.0033486742,0.0015209429,0.0008107592,0.0008890561,0.00039124594,0.002125044],"category_scores_gemma":[0.0016369716,0.0002915215,0.0004356204,0.0053796237,0.000371776,0.00048366576,0.0007883268,0.000484561,0.00059582456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005145032,0.00017560855,0.7169006,0.0004309364,0.00040553327,0.0008513757,0.0019253701,0.039753865,0.028666565,0.0022197997,0.028763816,0.179392],"study_design_scores_gemma":[0.000025048845,0.000022296546,0.9784162,0.000020906831,0.00006290982,0.0001252435,0.0007035183,0.009715517,0.0040626954,0.00015359152,0.0066176653,0.000074375486],"about_ca_topic_score_codex":0.9629698,"about_ca_topic_score_gemma":0.98727775,"teacher_disagreement_score":0.03703022,"about_ca_system_score_codex":0.008622499,"about_ca_system_score_gemma":0.011694658,"threshold_uncertainty_score":0.07449657},"labels":[],"label_agreement":null},{"id":"W4255041722","doi":"10.1130/geos.s.14779818.v1","title":"Supplemental Material: Mantle control on magmatic flare-ups in the southern Coast Mountains batholith, British Columbia","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Batholith; Zircon; Geology; Trace element; Geochemistry; Mantle (geology); Isotope; Seismology; Tectonics","score_opus":0.011500239123546334,"score_gpt":0.20871485219150898,"score_spread":0.19721461306796265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255041722","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004877056,0.000053111064,0.00025197648,0.00029525667,0.00013446734,0.000024832665,0.9828258,0.0003747088,0.011162659],"genre_scores_gemma":[0.04799894,0.00029308666,0.0018059859,0.0001399039,0.00011810305,0.000076871125,0.8919267,0.00055172935,0.057088748],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99974483,0.000014417062,0.000022393986,0.000049847247,0.000091618356,0.00007684433],"domain_scores_gemma":[0.99681455,0.00054458453,0.0001581902,0.00024936133,0.0018838495,0.0003495392],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00037828018,0.00062313647,0.00048930483,0.002787363,0.0013354275,0.0013436006,0.0010955939,0.00045028576,0.39622396],"category_scores_gemma":[0.0034918247,0.00031775894,0.000415123,0.0048968173,0.00015633703,0.0006061777,0.00065559195,0.00037709324,0.04214852],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005491147,0.000041571602,0.014384261,0.0002048393,0.000026216478,0.00006811876,0.00013779738,0.00047341274,0.00025853352,0.00056071323,0.969758,0.014031648],"study_design_scores_gemma":[0.00014976095,0.000033104858,0.5148697,0.0005529413,0.0000854326,0.00019016914,0.0013355771,0.002251623,0.0012809043,0.002472101,0.47670904,0.00006976649],"about_ca_topic_score_codex":0.7483994,"about_ca_topic_score_gemma":0.8809355,"teacher_disagreement_score":0.39622396,"about_ca_system_score_codex":0.0029924717,"about_ca_system_score_gemma":0.0043165013,"threshold_uncertainty_score":0.8612132},"labels":[],"label_agreement":null},{"id":"W4255441631","doi":"10.31223/x5190t","title":"Interplay of seismic and a-seismic deformation during the 2020 sequence of Atacama, Chile.","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Agencia Nacional de Investigación y Desarrollo; Agence Nationale de la Recherche; Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique; European Commission","keywords":"Aftershock; Seismology; Geology; Subduction; Slip (aerodynamics); Sequence (biology); Geodesy; Tectonics","score_opus":0.013162051584372147,"score_gpt":0.22473539181304303,"score_spread":0.2115733402286709,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4255441631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99505097,0.00016671959,0.00007210389,0.0001094368,0.000008416564,0.000009799617,0.001973096,0.000014729975,0.002594712],"genre_scores_gemma":[0.99671566,0.00009406567,0.00007770501,0.000026170914,0.0000076220763,0.000013486427,0.0021003287,0.000005088106,0.00095996493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999926,0.000010158771,0.000006241805,0.000021457116,0.000014362963,0.000021932068],"domain_scores_gemma":[0.9997414,0.000029860264,0.00006735208,0.00001252125,0.00006930211,0.00007968367],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001477749,0.00019701963,0.00014807675,0.0009689724,0.00028035074,0.00055164227,0.0003073581,0.00034936797,0.0021965934],"category_scores_gemma":[0.00069442723,0.00014475633,0.00012829108,0.0010921494,0.00021137847,0.0002887267,0.00049976126,0.00015318712,0.00031623634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003680069,0.00015333321,0.9459136,0.00022954163,0.00020870923,0.0013051992,0.0015478384,0.0059149424,0.014457943,0.0006222038,0.0046412707,0.02463737],"study_design_scores_gemma":[0.000005023478,0.000014189472,0.9975344,0.000009169199,0.000007880417,0.000028362885,0.0003977072,0.0010535488,0.00008450806,0.00004394899,0.0008168052,0.0000045523357],"about_ca_topic_score_codex":0.08452612,"about_ca_topic_score_gemma":0.113476604,"teacher_disagreement_score":0.08452612,"about_ca_system_score_codex":0.00090380927,"about_ca_system_score_gemma":0.00067547517,"threshold_uncertainty_score":0.16806823},"labels":[],"label_agreement":null},{"id":"W4256353345","doi":"10.1130/abs/2020am-353785","title":"A DOUBLE DIFFERENCE TOMOGRAPHY STUDY OF THE WASHINGTON FOREARC: DOES SILETZIA CONTROL CRUSTAL SEISMICITY?","year":2020,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Induced seismicity; Forearc; Geology; Seismology; Tomography; Tectonics; Subduction; Physics; Optics","score_opus":0.021029472929831903,"score_gpt":0.21884534895926405,"score_spread":0.19781587602943215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4256353345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887997,0.000034614743,0.000111534624,0.000040324187,0.0000015558618,0.0000030324616,0.00012255127,0.0000020189145,0.00080432504],"genre_scores_gemma":[0.9992931,0.000032858847,0.00009703128,0.000015567704,0.0000017414668,0.0000019162803,0.000113512164,0.0000020038333,0.00044229635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996054,0.0000056120275,0.0000018793347,0.000012526217,0.000004317079,0.000015138881],"domain_scores_gemma":[0.99985945,0.00003439738,0.00003407038,0.000014476183,0.00003577253,0.000021863427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001353227,0.0001606717,0.00015728967,0.0005253104,0.00039658108,0.00046498387,0.00031450123,0.00033547595,0.0015891638],"category_scores_gemma":[0.00046201595,0.00017281312,0.00014147258,0.0007012716,0.0003905979,0.00036724034,0.00025402024,0.000321691,0.00017132681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012928628,0.00028542653,0.9261965,0.000038052876,0.00020668373,0.001369218,0.0013044259,0.0024114938,0.04497353,0.0012078512,0.0005086643,0.020205293],"study_design_scores_gemma":[0.000022155828,0.00005952936,0.99394566,0.000007136254,0.000064078784,0.00017634989,0.0013483905,0.0021342998,0.0014141547,0.00016905759,0.00065267045,0.000006598244],"about_ca_topic_score_codex":0.16999823,"about_ca_topic_score_gemma":0.24923027,"teacher_disagreement_score":0.16999823,"about_ca_system_score_codex":0.0007733341,"about_ca_system_score_gemma":0.00066385267,"threshold_uncertainty_score":0.33801746},"labels":[],"label_agreement":null},{"id":"W4280604608","doi":"10.1002/essoar.10510181.2","title":"Aseismic Fault Slip during a Shallow Normal-Faulting Seismic Swarm Constrained Using a Physically-Informed Geodetic Inversion Method","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geodetic datum; Preprint; Seismology; Geology; Slip (aerodynamics); Inversion (geology); Geodesy; Solid earth; Swarm behaviour; Computer science; Geophysics; World Wide Web; Engineering; Artificial intelligence; Aerospace engineering","score_opus":0.030218041105970667,"score_gpt":0.2764779109223658,"score_spread":0.2462598698163951,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280604608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92333955,0.00006144885,0.074994,0.00012630787,0.000012740849,0.000024154537,0.00018941936,0.00022156815,0.0010308161],"genre_scores_gemma":[0.9838605,0.000023859428,0.015678905,0.0000134366155,0.000008772137,0.000014259538,0.00016357038,0.0000146088205,0.0002220871],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995184,0.000009901618,0.000003870546,0.00001609716,0.000009157394,0.000009223806],"domain_scores_gemma":[0.9998816,0.000036503036,0.00003119425,0.000016081636,0.000022380267,0.000012182547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017930541,0.00027229267,0.00021349962,0.00027709102,0.00011756071,0.00031703783,0.00049040257,0.0003913937,0.00045270904],"category_scores_gemma":[0.00063568965,0.00023508738,0.0002817919,0.00021780861,0.00026400594,0.00023773476,0.00024307406,0.00030162977,0.000059687176],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008738152,0.000068928704,0.01410448,0.00004078461,0.00004995577,0.00017597784,0.00010448419,0.9451839,0.019372597,0.0009721317,0.0002643875,0.019575112],"study_design_scores_gemma":[0.000006316485,0.000005992854,0.0023173837,0.0000015390569,0.0000033679373,0.000007607308,0.000007352506,0.9970362,0.00045551982,0.00009767078,0.00005766672,0.0000034463296],"about_ca_topic_score_codex":0.010431955,"about_ca_topic_score_gemma":0.01110304,"teacher_disagreement_score":0.010431955,"about_ca_system_score_codex":0.0002459799,"about_ca_system_score_gemma":0.0005253352,"threshold_uncertainty_score":0.020742476},"labels":[],"label_agreement":null},{"id":"W4280610389","doi":"10.5194/se-2022-9-ac1","title":"Reply on RC1","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Universitetet i Oslo; Universitetet i Tromsø; European Commission; Centre of Excellence for Environmental Decisions, Australian Research Council; San Diego State University; Norges Forskningsråd; Utah State University","keywords":"Geology; Echelon formation; Strike-slip tectonics; Seismology; Fault (geology); Strain partitioning; Transpression; Paleontology; Merge (version control); Structural basin; Tectonics; Sinistral and dextral","score_opus":0.043221275894052634,"score_gpt":0.26733609400960556,"score_spread":0.22411481811555292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280610389","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00021160263,0.0018113268,0.00027797537,0.6959719,0.24527407,0.00016021683,0.0007225737,0.0005895839,0.054980714],"genre_scores_gemma":[0.0021123628,0.0008867295,0.0002244346,0.711986,0.06173961,0.0001930471,0.00024507378,0.00026560135,0.22234714],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99726427,0.00048335345,0.00028285888,0.0005080939,0.0010215471,0.00043994302],"domain_scores_gemma":[0.9920677,0.00230129,0.00029454406,0.0005668996,0.0035209383,0.0012486209],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0029069479,0.0009639922,0.0011055372,0.0012652146,0.0035457064,0.00511444,0.0035360188,0.024734758,0.22403695],"category_scores_gemma":[0.028500274,0.0006842734,0.0013152594,0.0009833425,0.0022205778,0.0041920496,0.0031856874,0.021910664,0.18372726],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000073359056,0.0000031924594,0.00002426506,0.000013214607,0.0000010609908,0.00003757712,0.0000100577945,0.0000031648856,0.000016054308,0.00025864964,0.99767715,0.0019482255],"study_design_scores_gemma":[0.000008504856,0.0000053965737,0.0001389324,0.000042070445,0.0000017404917,0.000041312913,0.000057578876,0.000013912407,0.00003962384,0.00035461737,0.99928904,0.0000073285473],"about_ca_topic_score_codex":0.008382411,"about_ca_topic_score_gemma":0.01028701,"teacher_disagreement_score":0.22403695,"about_ca_system_score_codex":0.0034085503,"about_ca_system_score_gemma":0.0034980222,"threshold_uncertainty_score":0.7494782},"labels":[],"label_agreement":null},{"id":"W4280614805","doi":"10.5194/se-2022-9-ac2","title":"Reply on RC2","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Universitetet i Oslo; Universitetet i Tromsø; European Commission; Centre of Excellence for Environmental Decisions, Australian Research Council; San Diego State University; Norges Forskningsråd; Utah State University","keywords":"Geology; Echelon formation; Seismology; Strike-slip tectonics; Fault (geology); Strain partitioning; Paleontology; Tectonics","score_opus":0.043221275894052634,"score_gpt":0.26733609400960556,"score_spread":0.22411481811555292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280614805","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00025425697,0.0018002948,0.00031976594,0.6494656,0.28578952,0.00015529727,0.00074577035,0.0006356728,0.06083382],"genre_scores_gemma":[0.00249853,0.00087806454,0.00023582154,0.6607479,0.06898734,0.00018440654,0.00024890905,0.00030430127,0.2659148],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99761885,0.00041112097,0.00022950425,0.0004454452,0.0009156336,0.00037942492],"domain_scores_gemma":[0.99373806,0.0017627685,0.00022454748,0.00047589638,0.0027541365,0.001044587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002474587,0.0009198187,0.0009853401,0.0011384902,0.003260882,0.004827034,0.0031680835,0.021874875,0.21527193],"category_scores_gemma":[0.023691593,0.0005964607,0.0012233218,0.0008724183,0.0019839534,0.0039029168,0.0028835381,0.019632304,0.16975798],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008363776,0.0000034719078,0.00002618132,0.000012237116,0.000001165875,0.00004416832,0.00000983643,0.0000036279532,0.0000191922,0.00028417588,0.9975514,0.0020361624],"study_design_scores_gemma":[0.00000812458,0.0000049363866,0.00012630805,0.00003429225,0.0000016730208,0.000041531905,0.000052377727,0.0000151783215,0.00004399715,0.00034294146,0.99932206,0.0000064928304],"about_ca_topic_score_codex":0.00763394,"about_ca_topic_score_gemma":0.009725522,"teacher_disagreement_score":0.21527193,"about_ca_system_score_codex":0.002956722,"about_ca_system_score_gemma":0.003023823,"threshold_uncertainty_score":0.7201564},"labels":[],"label_agreement":null},{"id":"W4281642889","doi":"10.1029/2022gl098062","title":"A Small CO<sub>2</sub> Leakage May Induce Seismicity on a Sub‐Seismic Fault in a Good‐Porosity Clastic Saline Aquifer","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centennial College","funders":"","keywords":"Induced seismicity; Plume; Geology; Aquifer; Seismology; Fault (geology); Overpressure; Pore water pressure; Overburden; Petrology; Geotechnical engineering; Groundwater","score_opus":0.05224254457878158,"score_gpt":0.27903641660491996,"score_spread":0.22679387202613838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281642889","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992878,0.000009442365,0.00035206063,0.000015122522,0.0000012255431,0.0000019041196,0.00004119216,0.000027182406,0.00026421642],"genre_scores_gemma":[0.99980897,0.0000043712225,0.000099933306,0.0000021287715,4.077333e-7,7.584912e-7,0.000025427098,0.0000015463617,0.00005655334],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999504,0.0000035846665,0.0000034324396,0.0000095642345,0.0000120715,0.00002097201],"domain_scores_gemma":[0.9998667,0.000023995743,0.00005329489,0.000013599927,0.000019487648,0.00002293396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000860059,0.00013716512,0.00012408507,0.00019788907,0.00020175242,0.00027356253,0.00016994141,0.0002196273,0.0010421467],"category_scores_gemma":[0.00023995187,0.00008841861,0.00009177729,0.00018645248,0.00028473532,0.00023273852,0.00023795404,0.0001276424,0.00008343038],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008123244,0.00012684843,0.32514623,0.00009046172,0.00006016833,0.0020042697,0.00038271392,0.022019759,0.6293291,0.0005836903,0.0005628444,0.018881563],"study_design_scores_gemma":[0.000024226863,0.00043925134,0.76709193,0.000011153112,0.000050076247,0.0005645911,0.0006804215,0.073485896,0.15571372,0.00043414134,0.0014737807,0.000030753115],"about_ca_topic_score_codex":0.0037400739,"about_ca_topic_score_gemma":0.0054497784,"teacher_disagreement_score":0.0037400739,"about_ca_system_score_codex":0.0003329374,"about_ca_system_score_gemma":0.00021066499,"threshold_uncertainty_score":0.007436633},"labels":[],"label_agreement":null},{"id":"W4281694293","doi":"10.1007/s00024-022-03061-5","title":"Stochastic Source Modelling and Tsunami Hazard Analysis of the 2012 Mw7.8 Haida Gwaii Earthquake","year":2022,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Excellence Research Chairs, Government of Canada","keywords":"Bathymetry; Geology; Seismology; Tsunami earthquake; Submarine pipeline; Stochastic modelling; Hazard; Seismic hazard; Hazard analysis; Oceanography; Statistics","score_opus":0.011580062516630414,"score_gpt":0.18505223106243324,"score_spread":0.17347216854580283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281694293","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97669446,0.000121498706,0.018701741,0.00048055002,0.000029332337,0.000013949911,0.00041832853,0.000108867855,0.0034311658],"genre_scores_gemma":[0.9983546,0.00004314269,0.00069419853,0.0000067014166,0.00001011277,0.0000053428657,0.00013145668,0.000012325674,0.0007420573],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999242,0.000023141984,0.000004960452,0.000012732723,0.000015449426,0.000019490722],"domain_scores_gemma":[0.9996308,0.00020455297,0.000057917445,0.000016056672,0.00006624057,0.000024440204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036552086,0.00047704784,0.00035262716,0.00042703628,0.00025393695,0.00043153216,0.0006968669,0.00072753197,0.00089001225],"category_scores_gemma":[0.0013454868,0.00037893906,0.0004938015,0.00033942246,0.00025440345,0.00045584224,0.00035206837,0.00054518203,0.000104054656],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038489095,0.000019474268,0.0021838024,0.000010828235,0.000016606245,0.000042982352,0.00002818655,0.9934488,0.000559807,0.0019299964,0.00019018748,0.0015309183],"study_design_scores_gemma":[0.0000025674963,0.000003887993,0.0010644834,7.9633116e-7,0.000003392918,0.0000035244107,0.0000067832766,0.9985366,0.000070794675,0.00027320746,0.000030814703,0.000003290003],"about_ca_topic_score_codex":0.054240137,"about_ca_topic_score_gemma":0.037304167,"teacher_disagreement_score":0.9457599,"about_ca_system_score_codex":0.0007933888,"about_ca_system_score_gemma":0.0007825326,"threshold_uncertainty_score":0.10784882},"labels":[],"label_agreement":null},{"id":"W4281738773","doi":"10.1007/s00445-022-01571-7","title":"Phreatic and Hydrothermal Eruptions: From Overlooked to Looking Over","year":2022,"lang":"en","type":"article","venue":"Bulletin of Volcanology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Ludwig-Maximilians-Universität München; Deutsche Forschungsgemeinschaft","keywords":"Geology; Phreatic eruption; Hydrothermal circulation; Phreatic; Volcano; Caldera; Seismology; Induced seismicity; Petrology; Geochemistry; Earth science; Geophysics; Aquifer; Magma; Groundwater; Geotechnical engineering","score_opus":0.010030522925486608,"score_gpt":0.20764912965196256,"score_spread":0.19761860672647594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281738773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82048464,0.13218386,0.007802456,0.015199234,0.0011165907,0.000061374136,0.0010030043,0.00017509962,0.021973692],"genre_scores_gemma":[0.97125936,0.023162315,0.002118127,0.00074271887,0.0005888819,0.000007826971,0.0003170291,0.000022208747,0.001781605],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9995701,0.00010506457,0.000048533737,0.00011231073,0.00011227442,0.000051824372],"domain_scores_gemma":[0.9982235,0.0005112351,0.00051920785,0.00013884476,0.00036723915,0.00024004802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011049123,0.00023197378,0.00035722615,0.0017522374,0.0004372427,0.0022114464,0.00045241826,0.00049321534,0.0034138446],"category_scores_gemma":[0.0033615718,0.0001274291,0.00015762192,0.0016447385,0.001207624,0.0031174733,0.0013717788,0.0007634756,0.00033933527],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043942282,0.000088255125,0.4180507,0.0010520488,0.00010315256,0.004405342,0.008373425,0.00050495716,0.0030619123,0.010537221,0.006554822,0.5468287],"study_design_scores_gemma":[0.00001877328,0.00040597166,0.81961983,0.0025903496,0.00020610187,0.017948106,0.031123828,0.002987981,0.00180381,0.035980847,0.087216064,0.000098342076],"about_ca_topic_score_codex":0.0035587382,"about_ca_topic_score_gemma":0.0060050213,"teacher_disagreement_score":0.0035587382,"about_ca_system_score_codex":0.000639108,"about_ca_system_score_gemma":0.0006199979,"threshold_uncertainty_score":0.011420488},"labels":[],"label_agreement":null},{"id":"W4281747257","doi":"10.1002/essoar.10511475.1","title":"Seismic anisotropy along the Haida Gwaii margin from receiver function analysis","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Margin (machine learning); Preprint; Geology; Open science; Library science; Computer science; World Wide Web; Physics; Astronomy","score_opus":0.0199073263736155,"score_gpt":0.21702748058464835,"score_spread":0.19712015421103285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281747257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99123377,0.0001290671,0.0012410495,0.00004594172,0.0000046067435,0.000010088621,0.0018488858,0.00008470428,0.0054019843],"genre_scores_gemma":[0.9934509,0.00015698935,0.0011722305,0.000008142081,0.0000022462734,0.000005984564,0.0023723477,0.000014207248,0.0028169872],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999069,0.0000036125034,0.0000025909771,0.000014502724,0.000037626996,0.000034684548],"domain_scores_gemma":[0.9997439,0.000013570662,0.000021623324,0.000008846428,0.00017948971,0.00003264224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010890076,0.0003561776,0.00014696507,0.0012582672,0.0005494451,0.0007543568,0.00021345585,0.00014066698,0.0016241434],"category_scores_gemma":[0.00036557292,0.00013869617,0.00009263413,0.002006011,0.0002022966,0.00012851869,0.00026454538,0.00021140791,0.00048690406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024402415,0.000060206807,0.7866294,0.00007644192,0.00009398482,0.0007058851,0.0016537874,0.01136734,0.08229504,0.0007471588,0.004322743,0.11180402],"study_design_scores_gemma":[0.0000031610757,0.000006193946,0.9888969,0.000011148273,0.000015452257,0.00006604349,0.0004885786,0.0073332167,0.0017119354,0.00004207218,0.001411856,0.0000133369085],"about_ca_topic_score_codex":0.89133984,"about_ca_topic_score_gemma":0.9498594,"teacher_disagreement_score":0.10866016,"about_ca_system_score_codex":0.0018346389,"about_ca_system_score_gemma":0.0038748148,"threshold_uncertainty_score":0.2186001},"labels":[],"label_agreement":null},{"id":"W4281898677","doi":"10.1007/s10950-022-10096-7","title":"Effect of fault reactivation on deformation of off-fault fractures near a generic deep geological repository in crystalline rock in Canada","year":2022,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Nuclear Waste Management Organization","funders":"Nuclear Waste Management Organization","keywords":"Structural geology; Geology; Seismology; Fault (geology); Hydrogeology; Deformation (meteorology); Geotechnical engineering","score_opus":0.006654084424806645,"score_gpt":0.20747187172776207,"score_spread":0.20081778730295544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281898677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991635,0.000014452249,0.000018850813,0.00003073051,7.3387497e-7,0.000003632683,0.0001356111,0.0000034939237,0.0006289624],"genre_scores_gemma":[0.9994784,0.000016895576,0.000028076207,0.000005389916,3.414087e-7,0.0000011559955,0.00008834557,0.0000012511529,0.00038017076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99957365,0.000034961664,0.000021465905,0.000055990728,0.00010703443,0.0002068898],"domain_scores_gemma":[0.9985845,0.00017268327,0.00023929265,0.00006396067,0.000553929,0.00038564246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003015904,0.00013783327,0.00030272338,0.00085667823,0.0017298565,0.0012962784,0.0011316291,0.00046815778,0.0016223321],"category_scores_gemma":[0.0017178875,0.00023154332,0.00030475183,0.0012406666,0.0011801335,0.00036651024,0.0011120765,0.0003825254,0.00015096203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035604718,0.000082831895,0.9800586,0.000027049018,0.00006513422,0.00048672146,0.0021052964,0.0027489,0.0038620646,0.00035124732,0.00044243652,0.009413587],"study_design_scores_gemma":[0.000004767198,0.000028889423,0.99563605,0.000007237718,0.000012373263,0.000033381664,0.002835491,0.00088482484,0.00021021323,0.000026328464,0.00031402192,0.0000063740654],"about_ca_topic_score_codex":0.96039957,"about_ca_topic_score_gemma":0.9896421,"teacher_disagreement_score":0.039600432,"about_ca_system_score_codex":0.014790236,"about_ca_system_score_gemma":0.014720195,"threshold_uncertainty_score":0.10731119},"labels":[],"label_agreement":null},{"id":"W4283014003","doi":"10.1785/0220220116","title":"Machine Learning-Based Earthquake Catalog and Tomography Characterize the Middle-Northern Section of the Xiaojiang Fault Zone","year":2022,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Induced seismicity; Seismology; Tectonics; Fault (geology); Active fault; Block (permutation group theory); Geodesy; Slip (aerodynamics); Earthquake location; Geometry","score_opus":0.053089607780494326,"score_gpt":0.2486260280429014,"score_spread":0.19553642026240708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283014003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971252,0.00004051806,0.0016728054,0.000029480329,0.0000027863127,0.000008035428,0.0007453827,0.000079507736,0.0002963377],"genre_scores_gemma":[0.99590427,0.000026942738,0.0021535277,0.000004293716,0.0000061193846,0.000007115366,0.0017072579,0.0000060386287,0.00018432575],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999858,0.000011609547,0.000017207074,0.000052003692,0.000034240624,0.000026999314],"domain_scores_gemma":[0.9995734,0.000045628527,0.0001511536,0.00006369083,0.000098364086,0.00006778134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032791987,0.0002781105,0.00023798832,0.0017938467,0.000204418,0.00037294455,0.00033718065,0.00025057778,0.0006512549],"category_scores_gemma":[0.0007580189,0.00016359413,0.00021590186,0.0017521683,0.00023462142,0.00038269683,0.00044642107,0.00014369836,0.00022242336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086319684,0.00012326459,0.8847887,0.000036744023,0.000046729063,0.00027797132,0.00024509788,0.06208913,0.010230193,0.00037119703,0.00076564174,0.040938973],"study_design_scores_gemma":[0.000016263823,0.000034765806,0.8028715,0.000009297385,0.000019938901,0.00009352366,0.00010571626,0.19415273,0.00170237,0.00015129718,0.0008247655,0.000017829194],"about_ca_topic_score_codex":0.019843787,"about_ca_topic_score_gemma":0.02798583,"teacher_disagreement_score":0.019843787,"about_ca_system_score_codex":0.0004193276,"about_ca_system_score_gemma":0.00054812856,"threshold_uncertainty_score":0.039456546},"labels":[],"label_agreement":null},{"id":"W4283017608","doi":"10.1002/esp.5432","title":"Late Holocene rupture history of the Ash Hill fault, Eastern California Shear Zone, and the potential for seismogenic strain transfer between nearby faults","year":2022,"lang":"en","type":"article","venue":"Earth Surface Processes and Landforms","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Southern California Earthquake Center","keywords":"Geology; Holocene; Seismology; Fault scarp; Paleoseismology; Fault (geology); Alluvial fan; Shear zone; Shear (geology); Alluvium; Slip (aerodynamics); Paleontology; Sedimentary rock; Tectonics","score_opus":0.01099337615926509,"score_gpt":0.18979150430422217,"score_spread":0.17879812814495707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283017608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907863,0.000088022425,0.000043163644,0.000015318208,0.0000011687284,0.0000010747647,0.0001286817,0.000004025023,0.00063980545],"genre_scores_gemma":[0.9996113,0.000057251673,0.000042770556,0.0000035670098,0.0000016945532,0.000001120573,0.00011605228,6.191184e-7,0.00016561044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999479,0.000003978175,0.0000036642796,0.000020490364,0.000011864252,0.000011992171],"domain_scores_gemma":[0.9997582,0.000029665172,0.00009391212,0.000017692308,0.000050927007,0.000049625505],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015345906,0.00010958421,0.000084663734,0.0006141727,0.0003431786,0.0005242557,0.00020446615,0.00016192487,0.00074308546],"category_scores_gemma":[0.00040293593,0.00010756763,0.00006260366,0.00032303372,0.00025725993,0.00027151083,0.00027341468,0.00015811386,0.00007260369],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000455183,0.000021669732,0.9882124,0.000014153197,0.000026499212,0.00009390952,0.00038847132,0.0004274809,0.0024238185,0.000096019874,0.00021844386,0.008031681],"study_design_scores_gemma":[0.0000011042849,0.000006646214,0.99945074,0.000002347362,0.0000029996916,0.0000159786,0.000079077516,0.00015257309,0.00010282354,0.0000096310405,0.0001751795,8.9279104e-7],"about_ca_topic_score_codex":0.043096412,"about_ca_topic_score_gemma":0.1166225,"teacher_disagreement_score":0.043096412,"about_ca_system_score_codex":0.00063241227,"about_ca_system_score_gemma":0.00024054354,"threshold_uncertainty_score":0.085691154},"labels":[],"label_agreement":null},{"id":"W4283027882","doi":"10.1002/essoar.10511638.1","title":"Interdependent effects of fluid injection parameters on triggered aseismic fault slip and seismic clusters","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Preprint; Slip (aerodynamics); Interdependence; Seismology; Geology; Computer science; Engineering; World Wide Web; Aerospace engineering","score_opus":0.014622677909550005,"score_gpt":0.22641718607630015,"score_spread":0.21179450816675016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283027882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976851,0.00014136106,0.0011966968,0.000027133921,0.000007622581,0.000008949951,0.00012481878,0.00007220175,0.00073624466],"genre_scores_gemma":[0.9996474,0.000037093694,0.00018871143,0.0000041755447,0.0000013690243,0.0000026601917,0.000046786347,0.0000093891185,0.000062565814],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998493,0.000026307453,0.000018566001,0.000033221313,0.000030337273,0.000042129337],"domain_scores_gemma":[0.9988098,0.00065775844,0.0002601058,0.0000638987,0.00008566449,0.00012279712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000275517,0.00037695776,0.00036552537,0.0005794366,0.0001720117,0.00080159074,0.0002899941,0.0004709631,0.0010480168],"category_scores_gemma":[0.0023145447,0.00019023257,0.0002821906,0.00033059463,0.0005144532,0.00044487434,0.00041783784,0.00043545204,0.00012272992],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016241776,0.00067666743,0.17272455,0.00048864743,0.0002847973,0.0012634658,0.0003650998,0.40909585,0.39079106,0.0013002184,0.00055023714,0.020835288],"study_design_scores_gemma":[0.00009484556,0.0011025876,0.24051432,0.000055879795,0.0002397302,0.0003458044,0.00052608,0.61602414,0.13909501,0.0008449003,0.0010477053,0.00010893912],"about_ca_topic_score_codex":0.0015584402,"about_ca_topic_score_gemma":0.0011957131,"teacher_disagreement_score":0.0015584402,"about_ca_system_score_codex":0.00032645694,"about_ca_system_score_gemma":0.0002152934,"threshold_uncertainty_score":0.0035060048},"labels":[],"label_agreement":null},{"id":"W4283075153","doi":"10.1093/gji/ggac226","title":"The AlpArray Research Seismicity-Catalogue","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Commission for Environmental Cooperation","keywords":"Induced seismicity; Seismology; Seismic hazard; Geology; Python (programming language); Magnitude (astronomy); Earthquake location; Geodesy; Computer science; Physics","score_opus":0.04490344828711125,"score_gpt":0.29852798835692745,"score_spread":0.2536245400698162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283075153","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.038189538,0.0010381482,0.050460383,0.00030912235,0.00022121312,0.000493229,0.8143576,0.048458554,0.046472233],"genre_scores_gemma":[0.030432083,0.0003197075,0.03769749,0.00007192486,0.0001391858,0.00035645903,0.9206353,0.0039640004,0.0063839564],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9986615,0.00012494545,0.00018270532,0.00034647065,0.00055978383,0.0001245923],"domain_scores_gemma":[0.99792826,0.00013943776,0.0003300295,0.00062003994,0.0007810691,0.00020113152],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012038661,0.0012163764,0.0006488777,0.007608011,0.00046305027,0.0019416063,0.0012977418,0.0005599489,0.02757422],"category_scores_gemma":[0.0027108006,0.0003988287,0.0007634091,0.006522796,0.00020556359,0.0012905949,0.0018687235,0.00081524206,0.044117216],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091953797,0.00014797704,0.045199044,0.0013220917,0.00021481984,0.00046098864,0.00076343503,0.01387669,0.017260587,0.007213741,0.64987856,0.26274255],"study_design_scores_gemma":[0.00018753171,0.00010119443,0.06371103,0.00018013916,0.00006885938,0.00036089163,0.00024612714,0.013638442,0.0068952627,0.003157152,0.91135263,0.000100789046],"about_ca_topic_score_codex":0.00865739,"about_ca_topic_score_gemma":0.0063642636,"teacher_disagreement_score":0.02757422,"about_ca_system_score_codex":0.0006062918,"about_ca_system_score_gemma":0.0011795879,"threshold_uncertainty_score":0.09224492},"labels":[],"label_agreement":null},{"id":"W4283078545","doi":"10.5194/egusphere-2022-446","title":"Shear zone evolution and the path of earthquake rupture","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Mylonite; Geology; Shear zone; Seismology; Shear (geology); Lithology; Petrology; Tectonics","score_opus":0.013664265072694488,"score_gpt":0.21059359153035734,"score_spread":0.19692932645766284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283078545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998767,0.00005266566,0.00027412482,0.000020573778,0.0000010043075,0.0000013503123,0.00009839558,0.0000074608215,0.0007774214],"genre_scores_gemma":[0.9996666,0.000018999148,0.000098871365,0.0000015203891,5.889555e-7,7.409318e-7,0.000055227254,0.0000019496545,0.00015548895],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999541,0.000010398247,0.0000030438337,0.000013766193,0.00000797497,0.000010654015],"domain_scores_gemma":[0.99953306,0.00014288674,0.0001649901,0.000020322046,0.00007934928,0.000059416096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017103172,0.00007956019,0.00006628207,0.00072878523,0.00015891992,0.0005967757,0.00011585249,0.00019657529,0.0023785129],"category_scores_gemma":[0.0014241502,0.00013138274,0.00008553765,0.00045135492,0.0002279735,0.00019273018,0.00018613486,0.00017210095,0.0003306917],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030133757,0.00003374632,0.94539106,0.00004401015,0.000070777336,0.0002983084,0.00062921055,0.0089048855,0.025611667,0.002350864,0.00028390292,0.016080331],"study_design_scores_gemma":[0.0000065495215,0.000031192696,0.9914826,0.000010229959,0.000009655428,0.00014336138,0.00024707842,0.0061532906,0.0008308194,0.00060544064,0.00047373076,0.000006181384],"about_ca_topic_score_codex":0.0028878888,"about_ca_topic_score_gemma":0.0037186989,"teacher_disagreement_score":0.0028878888,"about_ca_system_score_codex":0.00028973128,"about_ca_system_score_gemma":0.00009917041,"threshold_uncertainty_score":0.007956982},"labels":[],"label_agreement":null},{"id":"W4283375616","doi":"10.1130/b36363.1","title":"The 180-km-long Meers-Willow fault system in the Southern Oklahoma Aulacogen: A potential U.S. mid-continent seismic hazard","year":2022,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Seismology; Lineament; Dike; Fault (geology); Permian; Basement; Seismic hazard; Paleontology; Tectonics","score_opus":0.00833245048144247,"score_gpt":0.18586512517653409,"score_spread":0.17753267469509162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283375616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963652,0.00012338362,0.00008118743,0.00024416568,0.0000052573464,0.00001060493,0.0006117438,0.000017359944,0.0025410468],"genre_scores_gemma":[0.9991184,0.000065341126,0.00016679728,0.000042204418,0.000003827032,0.000005664931,0.00021561718,0.0000012010876,0.00038088867],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999899,0.000010511363,0.0000052525174,0.000017086002,0.00002066204,0.000047475285],"domain_scores_gemma":[0.9997441,0.000025754021,0.000083814215,0.00001802348,0.000059160717,0.00006915309],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015291553,0.00012176287,0.00008918616,0.0007115904,0.0010956372,0.0006997232,0.00024983255,0.0002726187,0.001983251],"category_scores_gemma":[0.00029236375,0.00008472706,0.00007693702,0.0008909366,0.00029580787,0.0003216732,0.0005176949,0.00019967562,0.00011018462],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007283304,0.000060393784,0.9584038,0.00005663967,0.00004437236,0.0005819477,0.0011396373,0.0013353948,0.0040439847,0.00035126726,0.0018036866,0.03210596],"study_design_scores_gemma":[0.0000056852273,0.000023320681,0.98924667,0.00004502022,0.000022313252,0.00009302075,0.0034989333,0.0017920723,0.0003557119,0.00009488745,0.0048141754,0.000008165378],"about_ca_topic_score_codex":0.26448673,"about_ca_topic_score_gemma":0.52818733,"teacher_disagreement_score":0.26448673,"about_ca_system_score_codex":0.0021162268,"about_ca_system_score_gemma":0.002040738,"threshold_uncertainty_score":0.5258945},"labels":[],"label_agreement":null},{"id":"W4283576300","doi":"10.1002/essoar.10511713.2","title":"Do shallow injection wells contribute to the triggering of the 2020 M5.0 Mentone earthquake in the Delaware Basin, Texas?","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Preprint; Structural basin; Space (punctuation); Space Science; Geology; World Wide Web; Library science; Engineering; Seismology; Computer science; Operating system; Geomorphology; Aerospace engineering","score_opus":0.019271558266164578,"score_gpt":0.2373988692113884,"score_spread":0.2181273109452238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283576300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995654,0.00002717285,0.00006823825,0.000055655943,0.0000017052525,0.0000025895094,0.000052853982,0.0000038847347,0.00022253164],"genre_scores_gemma":[0.99983776,0.00002536452,0.00003593149,0.000008510127,0.0000019546374,8.710572e-7,0.000036615373,7.59696e-7,0.00005214935],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991643,0.000010249252,0.00000723859,0.000021330985,0.000010523411,0.000034179495],"domain_scores_gemma":[0.9996246,0.00007308911,0.00016655013,0.000020253961,0.000045534445,0.00006992787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018870783,0.00022773347,0.00019178865,0.00044503255,0.00029400454,0.00062412815,0.00040153158,0.00047102463,0.00095740147],"category_scores_gemma":[0.0007360697,0.00027193726,0.00023155856,0.00033640602,0.0003592337,0.0005372195,0.0005291793,0.00024295194,0.000100481855],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000111956135,0.00007091941,0.98256254,0.000025403599,0.000044267832,0.0006395707,0.00023414468,0.0050994577,0.0061475514,0.00024022473,0.00017745237,0.0046465728],"study_design_scores_gemma":[0.000009418063,0.000043746237,0.9789863,0.000010695253,0.00003293896,0.0000639647,0.00084025145,0.01906098,0.00065750227,0.0001244815,0.00015722663,0.0000124322705],"about_ca_topic_score_codex":0.036783896,"about_ca_topic_score_gemma":0.058022365,"teacher_disagreement_score":0.036783896,"about_ca_system_score_codex":0.0006691856,"about_ca_system_score_gemma":0.00052966597,"threshold_uncertainty_score":0.07313961},"labels":[],"label_agreement":null},{"id":"W4283582315","doi":"10.1029/2021jb022621","title":"Aseismic Fault Slip During a Shallow Normal‐Faulting Seismic Swarm Constrained Using a Physically Informed Geodetic Inversion Method","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"University of Liverpool; Natural Environment Research Council; Sight Research UK","keywords":"Slip (aerodynamics); Seismology; Geology; Interferometric synthetic aperture radar; Geodetic datum; Slipping; Geodesy; Episodic tremor and slip; Tectonics; Geometry; Synthetic aperture radar; Subduction; Mathematics; Remote sensing; Engineering","score_opus":0.050034415162463056,"score_gpt":0.3408482736245999,"score_spread":0.29081385846213686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283582315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8723887,0.00006265,0.1259017,0.00016578598,0.000015645452,0.000025358433,0.0001435159,0.00022307198,0.0010736218],"genre_scores_gemma":[0.9814285,0.000019677296,0.018053744,0.000017643055,0.000010619823,0.000015015979,0.00013278572,0.000013569211,0.00030845028],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999505,0.000012245917,0.0000035185328,0.00001510448,0.0000097943885,0.000008784374],"domain_scores_gemma":[0.9998696,0.0000441783,0.0000341585,0.000015559639,0.000023647322,0.0000129099535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002076137,0.00032588787,0.00022667284,0.0002681651,0.00014807054,0.0003284067,0.00048302097,0.00043632754,0.00047756082],"category_scores_gemma":[0.00055290933,0.00024428777,0.0003047693,0.00019829119,0.00030637742,0.00025782935,0.00023982105,0.00034737826,0.00005724019],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007926587,0.00006206738,0.008013043,0.000026627064,0.00004467051,0.00011788917,0.0000618877,0.9602704,0.013973755,0.00097042974,0.00022954983,0.016150516],"study_design_scores_gemma":[0.0000042760116,0.0000040142027,0.000948548,8.1846673e-7,0.000001946005,0.0000035902838,0.0000035019411,0.99862564,0.00029964722,0.00007217126,0.00003363196,0.0000022781678],"about_ca_topic_score_codex":0.010072242,"about_ca_topic_score_gemma":0.010978889,"teacher_disagreement_score":0.010072242,"about_ca_system_score_codex":0.00026115746,"about_ca_system_score_gemma":0.0005705612,"threshold_uncertainty_score":0.02002722},"labels":[],"label_agreement":null},{"id":"W4283711635","doi":"10.1002/essoar.10510181.3","title":"Aseismic Fault Slip during a Shallow Normal-Faulting Seismic Swarm Constrained Using a Physically-Informed Geodetic Inversion Method","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geodetic datum; Seismology; Geology; Slip (aerodynamics); Geodesy; Inversion (geology); Swarm behaviour; Solid earth; Computer science; Geophysics; Engineering; Artificial intelligence","score_opus":0.030218041105970667,"score_gpt":0.2764779109223658,"score_spread":0.2462598698163951,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283711635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92333955,0.00006144885,0.074994,0.00012630787,0.000012740849,0.000024154537,0.00018941936,0.00022156815,0.0010308161],"genre_scores_gemma":[0.9838605,0.000023859428,0.015678905,0.0000134366155,0.000008772137,0.000014259538,0.00016357038,0.0000146088205,0.0002220871],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995184,0.000009901618,0.000003870546,0.00001609716,0.000009157394,0.000009223806],"domain_scores_gemma":[0.9998816,0.000036503036,0.00003119425,0.000016081636,0.000022380267,0.000012182547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017930541,0.00027229267,0.00021349962,0.00027709102,0.00011756071,0.00031703783,0.00049040257,0.0003913937,0.00045270904],"category_scores_gemma":[0.00063568965,0.00023508738,0.0002817919,0.00021780861,0.00026400594,0.00023773476,0.00024307406,0.00030162977,0.000059687176],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008738152,0.000068928704,0.01410448,0.00004078461,0.00004995577,0.00017597784,0.00010448419,0.9451839,0.019372597,0.0009721317,0.0002643875,0.019575112],"study_design_scores_gemma":[0.000006316485,0.000005992854,0.0023173837,0.0000015390569,0.0000033679373,0.000007607308,0.000007352506,0.9970362,0.00045551982,0.00009767078,0.00005766672,0.0000034463296],"about_ca_topic_score_codex":0.010431955,"about_ca_topic_score_gemma":0.01110304,"teacher_disagreement_score":0.010431955,"about_ca_system_score_codex":0.0002459799,"about_ca_system_score_gemma":0.0005253352,"threshold_uncertainty_score":0.020742476},"labels":[],"label_agreement":null},{"id":"W4283766829","doi":"10.1002/essoar.10511785.1","title":"Depth-dependent crustal stress rotation and strength variation in the Charlevoix Seismic Zone (CSZ), Québec, Canada","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Preprint; Geology; Variation (astronomy); Space (punctuation); Seismology; Computer science; World Wide Web; Physics; Astronomy; Operating system","score_opus":0.013128893600699696,"score_gpt":0.2066260528251715,"score_spread":0.1934971592244718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283766829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97237056,0.00051511265,0.0003444935,0.00028137435,0.000011742382,0.000023645032,0.021249969,0.00009037413,0.0051127123],"genre_scores_gemma":[0.98557174,0.00018919932,0.00042402407,0.00005164875,0.000003907744,0.00001121964,0.010862788,0.00002022758,0.0028652365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997533,0.0000142971185,0.00001068543,0.00006963976,0.000058174934,0.00009383771],"domain_scores_gemma":[0.99888915,0.00007551487,0.0001275288,0.000054429565,0.0006570667,0.00019637136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030962212,0.00036031206,0.00025923338,0.0015549391,0.0009964894,0.0010842879,0.0007298681,0.00029431892,0.0034760828],"category_scores_gemma":[0.0011612732,0.00017523438,0.0002174509,0.0025658926,0.0005563325,0.00027029432,0.00049358665,0.0003130626,0.00038191234],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020491595,0.000047550267,0.95313424,0.00007415303,0.00016000993,0.00016813415,0.0008322846,0.0055373344,0.0031257009,0.00067284994,0.011417001,0.024625774],"study_design_scores_gemma":[0.000010077978,0.0000046681835,0.99415463,0.000019436393,0.000010728618,0.000015469406,0.00045634448,0.002474376,0.00016066298,0.000025950198,0.002656687,0.000010922165],"about_ca_topic_score_codex":0.99728835,"about_ca_topic_score_gemma":0.9987174,"teacher_disagreement_score":0.018419132,"about_ca_system_score_codex":0.018419132,"about_ca_system_score_gemma":0.011335723,"threshold_uncertainty_score":0.13364077},"labels":[],"label_agreement":null},{"id":"W4284690992","doi":"10.1038/s41598-022-15363-8","title":"Injection-induced fault slip assessment in Montney Formation in Western Canada","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"Mitacs","keywords":"Geology; Induced seismicity; Geomechanics; Slip (aerodynamics); Hydraulic fracturing; Seismology; Pore water pressure; Geotechnical engineering; Petrology; Engineering","score_opus":0.01788446942402107,"score_gpt":0.23323069233809735,"score_spread":0.2153462229140763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4284690992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989447,0.000025572695,0.00018308927,0.000014034106,6.494121e-7,0.000009000434,0.00026884957,0.000012617194,0.00054156303],"genre_scores_gemma":[0.9992073,0.000027655178,0.00023960271,0.0000037702164,3.9990988e-7,0.0000025663214,0.0002391092,0.0000015125178,0.00027809673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984694,0.000006785885,0.000008433637,0.000028045526,0.000066372704,0.00004340335],"domain_scores_gemma":[0.99971634,0.000027205062,0.00004682502,0.000014223236,0.00013718831,0.000058188878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014449554,0.0002446514,0.00017250872,0.0011290234,0.0009799588,0.0006552032,0.00043286,0.00030949875,0.0007324876],"category_scores_gemma":[0.0005823735,0.00013275312,0.0002274557,0.0012072289,0.0005936971,0.00017028334,0.00044353568,0.00016656905,0.00007734278],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001432206,0.000056228833,0.9458122,0.000035575,0.000053510335,0.00077966345,0.0007524713,0.026661318,0.0058919927,0.00041324273,0.00037770203,0.019022858],"study_design_scores_gemma":[0.000008324339,0.000033357144,0.96310997,0.000011005075,0.000018536588,0.000092528135,0.0010894003,0.033841863,0.0011005669,0.00008284682,0.0005962022,0.000015340283],"about_ca_topic_score_codex":0.9563315,"about_ca_topic_score_gemma":0.9853791,"teacher_disagreement_score":0.04366851,"about_ca_system_score_codex":0.0075361594,"about_ca_system_score_gemma":0.006732574,"threshold_uncertainty_score":0.087851286},"labels":[],"label_agreement":null},{"id":"W4285590116","doi":"10.1002/essoar.10511867.1","title":"Long-term Fluid Injection Can Expedite Fault Reactivation and Development: Riedel Shear Structures Illuminated by Induced Earthquakes in Alberta, Canada","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Shear (geology); Preprint; Solid earth; Geological survey; Term (time); Geology; Seismology; World Wide Web; Computer science; Physics; Geophysics; Astronomy; Petrology","score_opus":0.016514808887841816,"score_gpt":0.21867386008476306,"score_spread":0.20215905119692124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285590116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976532,0.00013603672,0.00011700978,0.000100541154,0.0000026313169,0.000009646883,0.00049385853,0.000012207114,0.001475022],"genre_scores_gemma":[0.9981433,0.00012433635,0.00019580824,0.00001777977,0.0000016410568,0.0000027467906,0.00038323557,0.0000035105763,0.0011276646],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998361,0.000008400498,0.0000072262146,0.00002628544,0.00005070726,0.00007123575],"domain_scores_gemma":[0.99975544,0.000020073096,0.00003995973,0.000008259592,0.000105248546,0.000071031856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013775128,0.00022744833,0.0002170509,0.0011647708,0.0012752053,0.0008823599,0.0006607808,0.0004153605,0.0014628258],"category_scores_gemma":[0.00039912178,0.00017685995,0.00020969566,0.0021361124,0.0006775722,0.00018537947,0.0005445072,0.00024877078,0.00012255696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002239772,0.00011423174,0.953496,0.000088032946,0.00010670257,0.0021815675,0.0040834565,0.00520742,0.007754636,0.00067372475,0.0015898253,0.024480497],"study_design_scores_gemma":[0.000006151592,0.000014803757,0.99347806,0.000011788164,0.000017720498,0.00005909543,0.002969311,0.0020595356,0.00020798497,0.0000476775,0.0011136701,0.000014184377],"about_ca_topic_score_codex":0.9876035,"about_ca_topic_score_gemma":0.9962184,"teacher_disagreement_score":0.012396514,"about_ca_system_score_codex":0.01173831,"about_ca_system_score_gemma":0.012466866,"threshold_uncertainty_score":0.085167825},"labels":[],"label_agreement":null},{"id":"W4286009134","doi":"10.1002/essoar.10511959.1","title":"The 2020 Mw 6.5 Monte Cristro Range (Nevada) earthquake: anatomy of a large rupture through a region of highly-distributed faulting","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Leverhulme Trust; Canada Foundation for Innovation; University of Victoria","keywords":"Preprint; Geology; World Wide Web; Library science; Seismology; Computer science","score_opus":0.020973005588357588,"score_gpt":0.2663452541771328,"score_spread":0.2453722485887752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286009134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99205387,0.00052229466,0.00044170374,0.00012326919,0.0000053601634,0.000014048874,0.00040839484,0.000036413672,0.0063948347],"genre_scores_gemma":[0.9980627,0.00023203832,0.0005696486,0.000017466838,0.0000034475918,0.0000046128685,0.000284302,0.000004903218,0.0008209442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999677,0.0000030585288,0.0000013867611,0.00001133606,0.000008803461,0.000007709634],"domain_scores_gemma":[0.99993074,0.000005753429,0.000025668809,0.0000038282114,0.000011765257,0.000022190427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007163203,0.00009471291,0.00006948373,0.0005220892,0.00031337913,0.0004603399,0.00019823221,0.0003636218,0.0009786218],"category_scores_gemma":[0.00020655556,0.00009193259,0.00005534228,0.00040364446,0.0002397769,0.00020205523,0.00044527528,0.00010946536,0.00014478782],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028546952,0.0001376154,0.8375791,0.00014218934,0.000064209606,0.006109099,0.0019420137,0.0071671447,0.06985355,0.0031660749,0.0026735398,0.07087997],"study_design_scores_gemma":[0.0000055726828,0.000039976225,0.99127626,0.000030073077,0.0000074213376,0.0012159141,0.0008385236,0.0020577803,0.00045822375,0.00034756784,0.0037136998,0.00000887775],"about_ca_topic_score_codex":0.03419277,"about_ca_topic_score_gemma":0.06181997,"teacher_disagreement_score":0.03419277,"about_ca_system_score_codex":0.00046156472,"about_ca_system_score_gemma":0.00032671943,"threshold_uncertainty_score":0.0679875},"labels":[],"label_agreement":null},{"id":"W4286697463","doi":"10.1038/s41598-022-16842-8","title":"A new chronology for tsunami deposits prior to the 1700 CE Cascadia earthquake from Vancouver Island, Canada","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Subduction; Seismology; Paleoseismology; Chronology; Submarine pipeline; Macrofossil; Subsidence; Turbidite; Oceanography; Paleontology; Holocene; Sediment; Tectonics; Structural basin","score_opus":0.009160703017865054,"score_gpt":0.1942688294229029,"score_spread":0.18510812640503785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286697463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9216182,0.003140316,0.0010830433,0.0002782714,0.00013093588,0.00025687518,0.037200134,0.000117590316,0.03617457],"genre_scores_gemma":[0.94984186,0.0030610196,0.003231481,0.00007686626,0.0000325157,0.0001365865,0.025419578,0.000035927296,0.018164204],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998115,0.000005740729,0.000019831987,0.000036361747,0.00007225799,0.000054456446],"domain_scores_gemma":[0.99746764,0.000058818765,0.00020389982,0.000063784486,0.0018825497,0.0003232833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023634057,0.0005152711,0.000210007,0.0080829,0.002392011,0.0013748176,0.0005321618,0.0002063471,0.004194618],"category_scores_gemma":[0.00090680417,0.00027704795,0.00014767179,0.0075383317,0.0004225677,0.00039581375,0.00071013556,0.0005387967,0.00061141106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016746916,0.00003721961,0.9103674,0.00025716133,0.00005683307,0.0010436362,0.0040861997,0.00068691256,0.006745259,0.00068157347,0.008796553,0.06707386],"study_design_scores_gemma":[0.000004869693,0.000011596341,0.970487,0.00006403671,0.000015404348,0.00020753495,0.001289197,0.00014298302,0.0004532433,0.000024702433,0.027290592,0.000008950076],"about_ca_topic_score_codex":0.97158897,"about_ca_topic_score_gemma":0.9954613,"teacher_disagreement_score":0.02841103,"about_ca_system_score_codex":0.009021832,"about_ca_system_score_gemma":0.012987057,"threshold_uncertainty_score":0.0654583},"labels":[],"label_agreement":null},{"id":"W4286717606","doi":"10.1038/s41598-022-15365-6","title":"Short-term forecasting of Mmax during hydraulic fracturing","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium; Canadian Natural Resources Limited; ConocoPhillips","keywords":"Induced seismicity; Hydraulic fracturing; Maximum magnitude; Geology; Seismology; Seismic hazard; Earthquake prediction; Robustness (evolution); Geotechnical engineering","score_opus":0.027462035445376082,"score_gpt":0.2185865666960981,"score_spread":0.191124531250722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286717606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99067545,0.000074110525,0.0077048647,0.000058658632,0.000011976139,0.000011195281,0.0006224277,0.00019136802,0.00065005274],"genre_scores_gemma":[0.9985972,0.000014431086,0.0010368424,0.000003088838,0.0000036988404,0.0000027278456,0.00025912878,0.0000026138614,0.00008028239],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998994,0.000018287343,0.000008199692,0.00003194931,0.000023312103,0.000018721388],"domain_scores_gemma":[0.9988752,0.0005130242,0.00022511175,0.0000729892,0.00021031687,0.000103330676],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00059955614,0.00049515796,0.0002755493,0.00059015554,0.00016877454,0.0004440215,0.0005282744,0.00044534283,0.00044789826],"category_scores_gemma":[0.002855798,0.00014245087,0.00013658081,0.00040556275,0.00016715105,0.0003776687,0.00027209258,0.00042459957,0.00017348473],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065793016,0.00013653205,0.2534857,0.00008556123,0.000095905045,0.00018536918,0.00010421329,0.68191314,0.0086487,0.0005093362,0.0010765889,0.05310091],"study_design_scores_gemma":[0.000007179385,0.00003824551,0.04737176,0.000008426363,0.000008332356,0.0000109873135,0.000030489477,0.95061684,0.0016499411,0.000108904576,0.00013788849,0.000011017522],"about_ca_topic_score_codex":0.04129355,"about_ca_topic_score_gemma":0.04984019,"teacher_disagreement_score":0.04129355,"about_ca_system_score_codex":0.000636563,"about_ca_system_score_gemma":0.0005396619,"threshold_uncertainty_score":0.08210641},"labels":[],"label_agreement":null},{"id":"W4289334784","doi":"10.5194/se-13-1169-2022","title":"Tectonic evolution of the Indio Hills segment of the San Andreas fault in southern California, southwestern USA","year":2022,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Universitetet i Oslo; Universitetet i Tromsø; European Commission; Centre of Excellence for Environmental Decisions, Australian Research Council; San Diego State University; H2020 European Research Council; Norges Forskningsråd; Utah State University","keywords":"Geology; Echelon formation; Seismology; Strike-slip tectonics; Tectonics; Fault (geology); Transform fault; Fold (higher-order function); Paleontology; Structural basin","score_opus":0.010221959506846826,"score_gpt":0.20018942254574942,"score_spread":0.1899674630389026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289334784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953477,0.00030263467,0.000052426873,0.000089911,0.0000045772927,0.0000057759357,0.000577623,0.000018095032,0.0036013157],"genre_scores_gemma":[0.9979863,0.00017607381,0.00019348275,0.00001659528,0.0000041535704,0.000004879078,0.00053974526,0.0000029112807,0.0010758548],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999392,0.000005361092,0.0000038597486,0.000025667383,0.00001582515,0.000010104431],"domain_scores_gemma":[0.9998079,0.000015744978,0.0000581623,0.000009695382,0.000079581274,0.000028882192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013927717,0.00012140115,0.00010682877,0.0008744494,0.0004386998,0.0004994817,0.00025552505,0.00018871647,0.0011452368],"category_scores_gemma":[0.00032331655,0.000108104796,0.00009004507,0.0006922612,0.00021897827,0.00013325155,0.00024399097,0.00015599083,0.00014373864],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006384725,0.000038185775,0.979954,0.000050388404,0.000060223574,0.00017657463,0.0009854988,0.0013286774,0.0035298867,0.00022096829,0.0012055644,0.012386166],"study_design_scores_gemma":[0.0000021036794,0.0000055669634,0.9982722,0.000009178344,0.000008505866,0.000016803095,0.00023932893,0.00037894465,0.00008118069,0.000008103584,0.00097653695,0.0000016164981],"about_ca_topic_score_codex":0.36699826,"about_ca_topic_score_gemma":0.64422107,"teacher_disagreement_score":0.36699826,"about_ca_system_score_codex":0.001434777,"about_ca_system_score_gemma":0.0009759138,"threshold_uncertainty_score":0.72972417},"labels":[],"label_agreement":null},{"id":"W4289799850","doi":"","title":"Stratigraphic modelling of relief and terrigenous fluxes in tectonic source area : results on the Meso-Hellenic piggy-back basin (Greece)","year":2007,"lang":"en","type":"preprint","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"","keywords":"Terrigenous sediment; Geology; Tectonics; Structural basin; Paleontology; Seismology","score_opus":0.03015244068676177,"score_gpt":0.20459735850653232,"score_spread":0.17444491781977056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289799850","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982639,0.000050677376,0.00045035366,0.000046175555,0.0000028403326,0.0000053970098,0.00034697604,0.00006352549,0.00077022734],"genre_scores_gemma":[0.9990459,0.000036452777,0.00035812758,0.0000041081403,0.0000017764349,0.00000440091,0.00024083306,0.000016685255,0.00029163016],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999068,0.000022713946,0.000008850671,0.000033124863,0.000008809484,0.000019727368],"domain_scores_gemma":[0.9997533,0.000102810336,0.000029963916,0.000038492704,0.000042180724,0.00003335183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027936805,0.00040153903,0.0005117479,0.0007373084,0.00032548516,0.00078062405,0.00080350536,0.0007140519,0.0019056186],"category_scores_gemma":[0.0007521076,0.00031532987,0.00071983994,0.0009885026,0.00040273336,0.00044039526,0.0004515107,0.00034492405,0.00026891785],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003147259,0.00016189598,0.1199871,0.00010224225,0.00019913507,0.0003453041,0.0003816037,0.8599413,0.004771093,0.000749045,0.00044817614,0.012598363],"study_design_scores_gemma":[0.00016298114,0.00009215955,0.2071495,0.000025620111,0.00010630357,0.00007788884,0.00043641715,0.7892161,0.0012687424,0.0006881314,0.00073783036,0.000038234517],"about_ca_topic_score_codex":0.11239566,"about_ca_topic_score_gemma":0.06273666,"teacher_disagreement_score":0.11239566,"about_ca_system_score_codex":0.0010786282,"about_ca_system_score_gemma":0.0007114476,"threshold_uncertainty_score":0.22348285},"labels":[],"label_agreement":null},{"id":"W4289835404","doi":"10.1002/essoar.10512083.1","title":"Heterogeneity versus Anisotropy and the State of Stress in Stable Cratons: Observations from a Deep Borehole of Opportunity in Northeastern Alberta, Canada","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Helmholtz-Alberta Initiative; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Purdue University","keywords":"Geology; Breakout; Anisotropy; Borehole; Seismology; Azimuth; Stress field; Monte Carlo method; Slip (aerodynamics); Geophysics; Petrology; Geometry; Geotechnical engineering; Physics","score_opus":0.042136628598047184,"score_gpt":0.23108768178336775,"score_spread":0.18895105318532057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289835404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99875236,0.000062865685,0.00006378264,0.000021220498,9.539951e-7,0.0000056432536,0.0003398417,0.0000075804273,0.00074575254],"genre_scores_gemma":[0.9990871,0.000066099434,0.0001299186,0.0000079845995,0.0000011564458,0.0000023229643,0.00021840322,0.0000022870304,0.00048457392],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998319,0.000003797089,0.0000057795137,0.000027255632,0.000069380534,0.0000619544],"domain_scores_gemma":[0.9996364,0.000025574129,0.00006465855,0.000011204937,0.00015625931,0.00010582961],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012931514,0.00031501046,0.00023496011,0.0017639542,0.0016104608,0.00090820057,0.00072973245,0.00032350555,0.0009143758],"category_scores_gemma":[0.00046904714,0.00029674795,0.00016280175,0.002020743,0.0010782188,0.0002152306,0.0005227609,0.00028039858,0.00016598323],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001643371,0.000047919966,0.97279197,0.000032906562,0.000038154772,0.00061374623,0.002353145,0.00094814337,0.013022074,0.00012485583,0.0003485657,0.00951421],"study_design_scores_gemma":[0.0000024709186,0.000006111909,0.9984426,0.0000047515236,0.000004676605,0.00003731412,0.0007629562,0.00032191531,0.00020201392,0.0000093613535,0.00020101671,0.000004827247],"about_ca_topic_score_codex":0.97074133,"about_ca_topic_score_gemma":0.99202794,"teacher_disagreement_score":0.029258668,"about_ca_system_score_codex":0.007700113,"about_ca_system_score_gemma":0.004404749,"threshold_uncertainty_score":0.05886191},"labels":[],"label_agreement":null},{"id":"W4290068935","doi":"10.31223/x5d93c","title":"Within the subducting Nazca Plate: The 2020 Mw 6.8 Calama earthquake and its similarity with the surrounding inslab seismicity","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Centre National de la Recherche Scientifique; Strong","keywords":"Geology; Seismology; Aftershock; Intraplate earthquake; Induced seismicity; Foreshock; Subduction; Oceanic crust; Interplate earthquake; Sequence (biology); Tectonics","score_opus":0.029703719310765736,"score_gpt":0.2301090421414905,"score_spread":0.20040532283072476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4290068935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990314,0.00006751614,0.00012808158,0.000028362898,0.0000036755653,0.000004207117,0.00010687542,0.000005913887,0.00062397454],"genre_scores_gemma":[0.9991553,0.00008999058,0.00019001793,0.0000091777165,0.000007067871,0.0000043965338,0.00036818787,0.0000024293793,0.00017345013],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999324,0.000005431477,0.000004655665,0.000022401136,0.000015036528,0.000020132155],"domain_scores_gemma":[0.9998704,0.00001003652,0.000059654325,0.000009464662,0.000023914272,0.000026497662],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000814664,0.00030104283,0.00024078562,0.0006549974,0.00036154976,0.00063419255,0.00037605973,0.00047672898,0.00051334494],"category_scores_gemma":[0.0005253184,0.00014156663,0.00021985317,0.00079673145,0.00032991424,0.00033035266,0.00051253045,0.00027001667,0.00009428533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025642657,0.00024355201,0.91032547,0.00008426418,0.0001398895,0.0018721392,0.00044181535,0.056488033,0.014544627,0.0011636805,0.0006895013,0.013750669],"study_design_scores_gemma":[0.00002483147,0.0000636232,0.93661094,0.000012971182,0.000036289908,0.00017837205,0.0003616989,0.060650345,0.00077417324,0.00016564775,0.0011036482,0.00001746201],"about_ca_topic_score_codex":0.09931931,"about_ca_topic_score_gemma":0.0867696,"teacher_disagreement_score":0.09931931,"about_ca_system_score_codex":0.0008102699,"about_ca_system_score_gemma":0.0006427143,"threshold_uncertainty_score":0.1974824},"labels":[],"label_agreement":null},{"id":"W4291754626","doi":"10.1190/image2022-3738967.1","title":"Examples of fault steps controlling event migration in seismic swarms","year":2022,"lang":"en","type":"article","venue":"Second International Meeting for Applied Geoscience &amp; Energy","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Fault (geology); Event (particle physics); Seismology; Computer science; Geology; Physics","score_opus":0.01964705503918492,"score_gpt":0.23485169148920174,"score_spread":0.2152046364500168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291754626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98089474,0.000113795955,0.014970228,0.00006562756,0.000009649115,0.00001537349,0.00029349665,0.00021087579,0.0034261635],"genre_scores_gemma":[0.9967253,0.000027975195,0.0029084482,0.0000027374685,0.0000023584032,0.0000050007507,0.00012565395,0.0000120811355,0.000190356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999899,0.000014399936,0.000008820605,0.00003520038,0.000019037923,0.000023475919],"domain_scores_gemma":[0.99951816,0.00012585592,0.00014495794,0.0000819378,0.00006163157,0.00006749423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116573785,0.00014002647,0.00016528217,0.0006909029,0.0003844121,0.00040052918,0.00023917938,0.00024417762,0.0014820569],"category_scores_gemma":[0.0014209861,0.00013438195,0.00012054534,0.000742315,0.00032672097,0.00030435435,0.00036532053,0.00019689662,0.00016253947],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00095087424,0.00015374266,0.48441547,0.00033269625,0.00015325284,0.0033582551,0.0043059676,0.07225518,0.27470598,0.030663997,0.0036208313,0.12508373],"study_design_scores_gemma":[0.0000843419,0.00026368798,0.77565265,0.000061125895,0.000087355285,0.0021787556,0.002352062,0.15071312,0.039177388,0.017502131,0.011793588,0.00013389031],"about_ca_topic_score_codex":0.002405313,"about_ca_topic_score_gemma":0.003438921,"teacher_disagreement_score":0.002405313,"about_ca_system_score_codex":0.0002574317,"about_ca_system_score_gemma":0.00014784466,"threshold_uncertainty_score":0.0049580336},"labels":[],"label_agreement":null},{"id":"W4291806117","doi":"10.4095/321857","title":"Seismicity in the Labrador-Baffin Seaway and surrounding onshore regions","year":2022,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Bay; Induced seismicity; Seismology; Seismometer; Focal mechanism; Post-glacial rebound; Oceanography; Sea level","score_opus":0.06326092196394313,"score_gpt":0.26953784315497253,"score_spread":0.20627692119102942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291806117","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98909926,0.0005962676,0.000059948197,0.0002561907,0.0000072413563,0.000016462625,0.0016481417,0.00001213209,0.008304564],"genre_scores_gemma":[0.99405044,0.00039084157,0.00016766929,0.000049505365,0.000011865253,0.000015644564,0.0022395852,0.000003994436,0.0030704068],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974865,0.00003666973,0.000014646192,0.000047572787,0.00007286655,0.000079614976],"domain_scores_gemma":[0.99960107,0.000053557156,0.000102564074,0.000020254816,0.00012546846,0.00009704702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023000661,0.00023453441,0.00017690768,0.0023017917,0.0007832294,0.00087548775,0.0003250879,0.00043150558,0.003616008],"category_scores_gemma":[0.0009806774,0.00013891229,0.00011075747,0.0026218523,0.00048874057,0.0003683866,0.00053248275,0.00023528407,0.0005210295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000102765145,0.000061425286,0.96289575,0.00008218264,0.00004283382,0.0005049188,0.0019118536,0.0005026427,0.0025269135,0.0002891003,0.0024421343,0.02863733],"study_design_scores_gemma":[0.0000030039403,0.0000133800795,0.99719834,0.000011903973,0.0000034778989,0.00007382931,0.000751682,0.00008868435,0.00005997016,0.000009890384,0.0017829051,0.0000029624948],"about_ca_topic_score_codex":0.6087221,"about_ca_topic_score_gemma":0.8358352,"teacher_disagreement_score":0.3912779,"about_ca_system_score_codex":0.0023565309,"about_ca_system_score_gemma":0.0012914735,"threshold_uncertainty_score":0.78716445},"labels":[],"label_agreement":null},{"id":"W4292242318","doi":"10.1016/j.jsg.2022.104704","title":"Influence of décollement-cover thickness variations in fold-and-thrust belts: Insights from centrifuge analog modeling","year":2022,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Ministerio de Economía y Competitividad","keywords":"Geology; Décollement; Anticline; Sedimentary rock; Fold (higher-order function); Wedge (geometry); Structural basin; Geomorphology; Geometry; Petrology; Paleontology","score_opus":0.011487201866094202,"score_gpt":0.21721539656626476,"score_spread":0.20572819470017056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292242318","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99283147,0.000042642132,0.0037569571,0.00009987457,0.000006167413,0.000011678307,0.00010299031,0.000053752243,0.0030944538],"genre_scores_gemma":[0.99935824,0.000021470103,0.00027624494,0.000007409107,0.0000021197263,0.0000031232128,0.000021323143,0.000007272776,0.00030269544],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998983,0.000035434507,0.0000068710488,0.000021566319,0.000011958925,0.000025833495],"domain_scores_gemma":[0.9996965,0.00012426989,0.00007188096,0.00003347107,0.000026717194,0.000047190886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021785434,0.00040469307,0.00029493743,0.0005210407,0.0002873383,0.0008694888,0.0006136219,0.0007813825,0.0015947677],"category_scores_gemma":[0.0014227146,0.00028286618,0.00049457257,0.00031736353,0.00068209326,0.00051309547,0.0005224529,0.00028367856,0.00010866476],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004779305,0.000045208442,0.011202181,0.000012471724,0.000015952884,0.00015171836,0.000044137487,0.98278266,0.002697237,0.0013507815,0.00006573989,0.0015841072],"study_design_scores_gemma":[0.000009496255,0.000014866681,0.003980289,0.0000020774778,0.0000059008817,0.000016171645,0.000018251763,0.9954465,0.00020026657,0.00023110323,0.00006862938,0.000006485723],"about_ca_topic_score_codex":0.028193336,"about_ca_topic_score_gemma":0.013004329,"teacher_disagreement_score":0.028193336,"about_ca_system_score_codex":0.0010189625,"about_ca_system_score_gemma":0.0004197891,"threshold_uncertainty_score":0.056058466},"labels":[],"label_agreement":null},{"id":"W4292607378","doi":"10.36487/acg_repo/2205_76","title":"Characterisation of seismic activity at a kimberlite block caving operation in a complex geological setting in Quebec, Canada","year":2022,"lang":"en","type":"article","venue":"Caving 2022: Fifth International Conference on Block and Sublevel Caving","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Kimberlite; Geology; Block (permutation group theory); Mining engineering; Geochemistry; Mantle (geology)","score_opus":0.03886436224351968,"score_gpt":0.2413475754002365,"score_spread":0.2024832131567168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292607378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98978525,0.00018327725,0.00065972994,0.00016866685,0.000007350405,0.000070302696,0.0038391587,0.00004471167,0.0052415184],"genre_scores_gemma":[0.99490464,0.00012660044,0.00061212125,0.000047794798,0.0000035227242,0.000020192132,0.0016525438,0.00001230956,0.0026202768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997353,0.000013033627,0.000008986322,0.00005312967,0.000104271145,0.00008527131],"domain_scores_gemma":[0.99935526,0.000038097714,0.000063417065,0.000017461512,0.0003961704,0.0001296727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001784293,0.00042285805,0.00024636695,0.0014268359,0.0015090852,0.0007747714,0.00091468036,0.0005148695,0.0022961174],"category_scores_gemma":[0.000631706,0.0002112598,0.00016826532,0.0021502718,0.000709237,0.00021541886,0.0005083157,0.0003624577,0.00036899553],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021426291,0.00014581183,0.9169888,0.00017376627,0.00010306972,0.0021058782,0.006225187,0.0063500865,0.020230992,0.0006633502,0.007253143,0.039545633],"study_design_scores_gemma":[0.000007258201,0.000028463277,0.98876196,0.00003399271,0.000011011573,0.000112780115,0.0029387996,0.0039230785,0.00035076519,0.00002316837,0.00378739,0.000021323276],"about_ca_topic_score_codex":0.99061954,"about_ca_topic_score_gemma":0.997493,"teacher_disagreement_score":0.010692501,"about_ca_system_score_codex":0.010692501,"about_ca_system_score_gemma":0.009619436,"threshold_uncertainty_score":0.077579916},"labels":[],"label_agreement":null},{"id":"W4292702761","doi":"10.1038/s43017-022-00327-3","title":"Giant tsunami monitoring, early warning and hazard assessment","year":2022,"lang":"en","type":"review","venue":"Nature Reviews Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Warning system; Hazard; Shore; Early warning system; Submarine pipeline; Emergency management; Scale (ratio); Hazard analysis; Seismology; Forensic engineering; Environmental resource management; Environmental science; Geology; Geography; Computer science; Cartography; Oceanography; Engineering","score_opus":0.040382422620101686,"score_gpt":0.2945850945041426,"score_spread":0.25420267188404094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292702761","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00008566044,0.998473,0.00014552125,0.00028916466,0.0001896068,0.000012831108,0.000082665385,0.000007162882,0.00071426295],"genre_scores_gemma":[0.0008648425,0.99803466,0.00023198446,0.00022065378,0.00022685749,0.00001091869,0.00010946451,0.0000019116999,0.00029862314],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99945945,0.000109110544,0.00008250041,0.000108000655,0.00020219227,0.0000387591],"domain_scores_gemma":[0.99851817,0.0008603713,0.0002346259,0.00003601194,0.00029300142,0.000057745492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016999237,0.0013295169,0.0020464319,0.003228276,0.00019659215,0.0013467015,0.0016929391,0.0015628024,0.0055554784],"category_scores_gemma":[0.003820438,0.0003825447,0.00085732783,0.003979183,0.00065976364,0.0013463707,0.0009319604,0.00116798,0.0017384819],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004726411,0.000046090143,0.0003514557,0.026743414,0.00023575108,0.000058207865,0.00003157646,0.000601378,0.00032813774,0.0015893203,0.026717938,0.9432496],"study_design_scores_gemma":[0.000074842676,0.00020624581,0.005074056,0.026080858,0.0010117155,0.0007051915,0.00015876278,0.00034726187,0.00027874924,0.004669848,0.96133566,0.0000568781],"about_ca_topic_score_codex":0.006883787,"about_ca_topic_score_gemma":0.013797474,"teacher_disagreement_score":0.006883787,"about_ca_system_score_codex":0.00073616713,"about_ca_system_score_gemma":0.0029651935,"threshold_uncertainty_score":0.018584907},"labels":[],"label_agreement":null},{"id":"W4292712481","doi":"10.1029/2022jb024744","title":"Spatiotemporal Variations in Earthquake Triggering Mechanisms During Multistage Hydraulic Fracturing in Western Canada","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Induced seismicity; Hydraulic fracturing; Magnitude (astronomy); Pore water pressure; Fault (geology); Fracture (geology); Geotechnical engineering","score_opus":0.02855768288526143,"score_gpt":0.28538316221635296,"score_spread":0.2568254793310915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292712481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996591,0.00011542456,0.00018930809,0.000042932217,0.0000023674456,0.000010866731,0.0019104722,0.00001779592,0.0011199642],"genre_scores_gemma":[0.99772924,0.00009578408,0.00024413296,0.000012373018,0.0000014873535,0.0000051288375,0.0011119773,0.0000037995828,0.00079600036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978274,0.000007562644,0.000008188008,0.00004629042,0.00006982663,0.000085377236],"domain_scores_gemma":[0.99917644,0.000047052672,0.00011976858,0.000023878676,0.00047311015,0.00015962118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000164969,0.00029074016,0.00022295969,0.0017414446,0.0010029351,0.00091219123,0.0006500587,0.00026220182,0.001081925],"category_scores_gemma":[0.0006539209,0.0001886535,0.00015121083,0.0030118034,0.0005815928,0.00018942477,0.00058006076,0.00022595085,0.00015843802],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014397906,0.00003200995,0.9662788,0.000048409653,0.0000686632,0.00037716003,0.0019637302,0.0016345858,0.00876813,0.00022166736,0.0010798379,0.019383157],"study_design_scores_gemma":[0.0000021758497,0.0000057802513,0.99732035,0.000008037967,0.000009212463,0.00002682943,0.0010223257,0.0007633517,0.00027100331,0.000014457471,0.00054804166,0.000008440484],"about_ca_topic_score_codex":0.98971295,"about_ca_topic_score_gemma":0.9958377,"teacher_disagreement_score":0.010287046,"about_ca_system_score_codex":0.00914831,"about_ca_system_score_gemma":0.009144365,"threshold_uncertainty_score":0.06637597},"labels":[],"label_agreement":null},{"id":"W4292787935","doi":"10.1093/gji/ggac333","title":"Effects of large aftershocks on spatial aftershock forecasts during the 2017–2019 western Iran sequence","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; International Institute of Earthquake Engineering and Seismology; Hirschmann-Stiftung; Deutsche Forschungsgemeinschaft","keywords":"Aftershock; Magnitude (astronomy); Geology; Seismology; Jackknife resampling; Metric (unit); Sequence (biology); Grid; Geodesy; Statistics; Mathematics; Physics; Engineering","score_opus":0.014296398009986402,"score_gpt":0.23926338238808612,"score_spread":0.2249669843780997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292787935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99570364,0.0002318237,0.0021122117,0.00020536952,0.0000777841,0.000011308409,0.0005438446,0.00020860024,0.00090542535],"genre_scores_gemma":[0.99829084,0.00004789156,0.00051013497,0.000017576385,0.000024754616,0.000003121609,0.0009950718,0.00000964256,0.000101052254],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995554,0.000115333285,0.000034777866,0.00011372206,0.00009484759,0.00008593127],"domain_scores_gemma":[0.9970282,0.0016360352,0.00032253496,0.00020079207,0.0005573362,0.00025518757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018013333,0.0005981603,0.0003784461,0.0006664577,0.00023248016,0.0006572013,0.00043560087,0.0005143385,0.00088476983],"category_scores_gemma":[0.007864832,0.00015549261,0.00039632217,0.00038237937,0.00027184395,0.0007949504,0.0006485846,0.0007780145,0.00037680633],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021869408,0.00027121176,0.29991636,0.00013001179,0.00023574672,0.00051996013,0.0003758177,0.5719541,0.00549235,0.0006388398,0.0063010654,0.11197759],"study_design_scores_gemma":[0.000054565844,0.00027465512,0.10446925,0.000047916667,0.00006967321,0.00006326364,0.0004360672,0.8894767,0.003434335,0.00049003185,0.0011440548,0.000039475926],"about_ca_topic_score_codex":0.024432002,"about_ca_topic_score_gemma":0.01955364,"teacher_disagreement_score":0.024432002,"about_ca_system_score_codex":0.0005015941,"about_ca_system_score_gemma":0.0007890347,"threshold_uncertainty_score":0.048579574},"labels":[],"label_agreement":null},{"id":"W4293067972","doi":"10.1029/2021jb023722","title":"Evaluating the Tsunamigenic Potential of Buried Versus Trench‐Breaching Megathrust Slip","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seafloor spreading; Trench; Subduction; Slip (aerodynamics); Seismology; Episodic tremor and slip; Tsunami earthquake; Thickening; Deformation (meteorology); Tectonics; Geophysics","score_opus":0.12211788151624407,"score_gpt":0.39711334012206206,"score_spread":0.274995458605818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293067972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99904853,0.0000431356,0.0004415581,0.000009147272,0.0000017926312,0.00000355323,0.00005327607,0.000010137803,0.00038890092],"genre_scores_gemma":[0.9996966,0.000016317043,0.00017030435,0.0000018176843,7.795383e-7,0.0000015878697,0.00003797819,0.0000014746977,0.000073091236],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999013,0.000020326237,0.000007833953,0.000018636367,0.000019996609,0.00003180952],"domain_scores_gemma":[0.999278,0.00038667102,0.00012683553,0.00003882268,0.00007312183,0.00009648023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039753775,0.00045044158,0.00031965156,0.00062125985,0.0001824734,0.000573148,0.00033196848,0.000501122,0.001052351],"category_scores_gemma":[0.0013174572,0.00021159263,0.00036219053,0.0004022664,0.00033515805,0.00047688483,0.0003985013,0.00024047773,0.00010792475],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000678325,0.00017560057,0.13456103,0.00007946075,0.00013205515,0.00039540793,0.00006400495,0.83849454,0.01667727,0.00061976403,0.00011585456,0.008006691],"study_design_scores_gemma":[0.000024068531,0.000669911,0.07460892,0.000013717865,0.000050183942,0.00007058682,0.00019920175,0.9179266,0.0059402664,0.0003556688,0.00011779587,0.000023174489],"about_ca_topic_score_codex":0.005021014,"about_ca_topic_score_gemma":0.0052011157,"teacher_disagreement_score":0.005021014,"about_ca_system_score_codex":0.0004944291,"about_ca_system_score_gemma":0.0002146242,"threshold_uncertainty_score":0.00998354},"labels":[],"label_agreement":null},{"id":"W4293105639","doi":"10.1038/s41598-022-18505-0","title":"Basin-scale multi-decadal analysis of hydraulic fracturing and seismicity in western Canada shows non-recurrence of induced runaway fault rupture","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium; University of Bristol; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Research Councils UK; Sight Research UK","keywords":"Induced seismicity; Hydraulic fracturing; Geology; Seismology; Structural basin; Scale (ratio); Fault (geology); Geomorphology; Geotechnical engineering; Geography; Cartography","score_opus":0.01573320947071825,"score_gpt":0.22600575556649208,"score_spread":0.21027254609577384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293105639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99734026,0.000100634104,0.00007460164,0.00008805584,0.0000047002295,0.000007595554,0.0015543343,0.000019798406,0.0008099986],"genre_scores_gemma":[0.99815685,0.00006899788,0.00009322138,0.000020843494,0.000002575995,0.0000043684136,0.0012531043,0.000004735134,0.00039512833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998387,0.000006865085,0.000007126016,0.00003802683,0.000047119254,0.00006208665],"domain_scores_gemma":[0.9992944,0.000039684714,0.00009253319,0.00003080711,0.00033346296,0.00020905204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021318208,0.00025664966,0.00023872986,0.0013212803,0.0008291861,0.0007208092,0.0004992009,0.0003841348,0.0011086515],"category_scores_gemma":[0.0006805284,0.00017862846,0.00024181769,0.0020245374,0.00046280932,0.00020472599,0.00061643025,0.00038151117,0.0001590855],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012798727,0.000049796938,0.97950256,0.000036410715,0.00013240134,0.0002761703,0.00091798016,0.0018741131,0.0053227204,0.00018766196,0.0017471572,0.0098249335],"study_design_scores_gemma":[0.0000019279466,0.000005200619,0.99814105,0.000004375031,0.000008831537,0.000015013126,0.00034417163,0.0009690116,0.00007381268,0.000009565685,0.0004217514,0.0000053870695],"about_ca_topic_score_codex":0.95972514,"about_ca_topic_score_gemma":0.980415,"teacher_disagreement_score":0.04027486,"about_ca_system_score_codex":0.006310249,"about_ca_system_score_gemma":0.005294901,"threshold_uncertainty_score":0.08102405},"labels":[],"label_agreement":null},{"id":"W4293213571","doi":"10.1029/2022gl100146","title":"Hidden Roughness of Subducting Seafloor and Implications for Megathrust Seismogenesis: Example From Northern Manila Trench","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Youth Innovation Promotion Association of the Chinese Academy of Sciences; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Seafloor spreading; Trench; Seismology; Subduction; Bathymetry; Seamount; Accretion (finance); Basement; Tectonics; Geophysics; Geochemistry; Oceanography","score_opus":0.07315823155903257,"score_gpt":0.29431640046450225,"score_spread":0.2211581689054697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293213571","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987864,0.00006403928,0.00008066247,0.000024172494,0.0000015092514,0.0000038009036,0.000052374067,0.0000063645202,0.0009807466],"genre_scores_gemma":[0.99964404,0.000034147768,0.000080610254,0.000003219721,0.0000019407971,0.0000012565911,0.000030494071,0.0000013684519,0.00020296266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992585,0.000010430092,0.0000037361053,0.000014739482,0.0000124510125,0.00003292936],"domain_scores_gemma":[0.99973255,0.00006345311,0.00006254078,0.00003287305,0.000053712032,0.00005474613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015158053,0.00023785878,0.00021896469,0.0010917572,0.00071212905,0.0005554595,0.0003293966,0.00034803478,0.0015012809],"category_scores_gemma":[0.0004547349,0.00012109477,0.00016008203,0.0010360996,0.0006681484,0.00019589628,0.00054424437,0.00015365276,0.00016079216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024085461,0.000066605644,0.9426069,0.00010613842,0.00006013234,0.020564117,0.004743971,0.003805214,0.010060721,0.00037667915,0.00029931962,0.01706925],"study_design_scores_gemma":[0.0000032396513,0.00004119918,0.9945005,0.000013029936,0.000013950035,0.0010836759,0.0022489151,0.0009994473,0.0004491846,0.00008946607,0.00054540945,0.000011847429],"about_ca_topic_score_codex":0.03922054,"about_ca_topic_score_gemma":0.09452725,"teacher_disagreement_score":0.03922054,"about_ca_system_score_codex":0.0005684071,"about_ca_system_score_gemma":0.00036639912,"threshold_uncertainty_score":0.07798451},"labels":[],"label_agreement":null},{"id":"W4293660864","doi":"10.5194/egusphere-alpshop2022-28","title":"Quartz and zircon in garnet elastic geobarometry of HP rocks from the Sesia Zone","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Greenschist; Blueschist; Eclogite; Metamorphic rock; Epidote; Geology; Gneiss; Geochemistry; Metamorphic facies; Zircon; Quartz; Orogeny; Mineralogy; Subduction; Facies; Geomorphology; Seismology; Chlorite","score_opus":0.016730562551270183,"score_gpt":0.21542692323030316,"score_spread":0.19869636067903299,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293660864","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985386,0.00009362588,0.000408344,0.000006733552,0.0000028905324,0.0000031016655,0.00022663095,0.000025727923,0.00069440523],"genre_scores_gemma":[0.9985891,0.000072636074,0.00046814236,0.000006525698,0.000002302598,0.0000029583798,0.0003974822,0.0000132556415,0.00044760542],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998741,0.0000046525397,0.000009054165,0.00005434945,0.000038767266,0.000019104798],"domain_scores_gemma":[0.9999534,0.0000063834586,0.000014109328,0.0000060933403,0.000013502265,0.0000065606523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014037339,0.000378269,0.00021729773,0.0010787464,0.0002457996,0.00046227803,0.00026514634,0.00023168817,0.0011042262],"category_scores_gemma":[0.00018737245,0.00022372739,0.00022188746,0.0006106212,0.00029947524,0.00023605455,0.00036451206,0.00016504688,0.00025421867],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028977278,0.00003967281,0.116253436,0.00009140463,0.00010075224,0.0005798643,0.00050529273,0.0020819437,0.8700932,0.00018837451,0.000073259114,0.009702897],"study_design_scores_gemma":[0.000014042671,0.000092425566,0.88036305,0.000013471657,0.00006442813,0.00032577763,0.00034127026,0.004743808,0.11227654,0.00007687615,0.0016758995,0.000012425096],"about_ca_topic_score_codex":0.0075308825,"about_ca_topic_score_gemma":0.0140483165,"teacher_disagreement_score":0.0075308825,"about_ca_system_score_codex":0.00028862653,"about_ca_system_score_gemma":0.00012482036,"threshold_uncertainty_score":0.014974058},"labels":[],"label_agreement":null},{"id":"W4294176442","doi":"10.5194/egusphere-2022-446-ac1","title":"Reply on RC1","year":2022,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Mylonite; Geology; Shear zone; Seismology; Shear (geology); Lithology; Crust; Tectonics; Petrology; Geophysics","score_opus":0.043221275894052634,"score_gpt":0.26733609400960556,"score_spread":0.22411481811555292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294176442","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0002457532,0.002012025,0.0001914587,0.7893118,0.16937277,0.00010973483,0.0005053129,0.0004006359,0.03785045],"genre_scores_gemma":[0.0025277045,0.000996889,0.00017299484,0.79979163,0.045722503,0.00014457887,0.00018433161,0.00018023356,0.15027918],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99797064,0.00036980255,0.0002211005,0.00040532797,0.0006891456,0.00034399965],"domain_scores_gemma":[0.9952924,0.0015615636,0.00018783323,0.00034702852,0.0018156569,0.00079555635],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.002165392,0.0009018707,0.0010348014,0.00096069,0.002953673,0.0039543817,0.0033033986,0.025596486,0.17515868],"category_scores_gemma":[0.020610847,0.00059589074,0.0012984853,0.00077632884,0.0019675386,0.00339617,0.002570642,0.02182106,0.12665236],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009296975,0.0000037255218,0.000032389155,0.000013434672,0.0000013832749,0.00006864407,0.000010711238,0.0000043436876,0.000019351406,0.0003100155,0.9975204,0.0020063089],"study_design_scores_gemma":[0.000010284156,0.000006837494,0.00018256714,0.00005069982,0.0000022949591,0.00007169847,0.00006533471,0.000019100555,0.00004750278,0.000445,0.99908984,0.000008874193],"about_ca_topic_score_codex":0.007855287,"about_ca_topic_score_gemma":0.009568676,"teacher_disagreement_score":0.8248413,"about_ca_system_score_codex":0.003367011,"about_ca_system_score_gemma":0.0028920784,"threshold_uncertainty_score":0.58596414},"labels":[],"label_agreement":null},{"id":"W4294688160","doi":"10.1029/2022gc010540","title":"Monitoring the 2021 M<sub>w</sub> 8.2 Alaska Earthquake by an Offshore Seismic and Fluid Pressure Observation Network and Implications for Ocean‐Crust Dynamic Coupling","year":2022,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Seismology; Seismometer; Seafloor spreading; Accretionary wedge; Borehole; Submarine pipeline; Microseism; Subduction; Tectonics; Geophysics; Oceanography; Geotechnical engineering","score_opus":0.011722580450031437,"score_gpt":0.20846281348738513,"score_spread":0.1967402330373537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294688160","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988446,0.000023194598,0.00018832553,0.000029836185,0.000004504186,0.0000053588815,0.00043070977,0.000012929749,0.00046043607],"genre_scores_gemma":[0.9985518,0.00002972277,0.00050983496,0.000010041375,0.0000061866895,0.000008267857,0.0006433287,0.0000015175225,0.00023936652],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998559,0.000021606369,0.000012616495,0.000038215658,0.000042255277,0.000029335602],"domain_scores_gemma":[0.99956983,0.00003864703,0.00013997381,0.000027080563,0.00013710163,0.000087272856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022861586,0.0002021678,0.00011088258,0.00058864465,0.0003015553,0.00032613808,0.00020995055,0.00026976783,0.0002979221],"category_scores_gemma":[0.00065403053,0.00011561665,0.000072163995,0.0006668596,0.00012994195,0.00024270723,0.0004753801,0.00015476602,0.000091213056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048465725,0.00002984486,0.98114437,0.000014866472,0.000019793164,0.00020773517,0.00024061509,0.0016117463,0.006533857,0.00003839161,0.00042165216,0.009688622],"study_design_scores_gemma":[0.000003701676,0.000033573913,0.9926765,0.0000066635503,0.000016346707,0.000049766983,0.00056447723,0.005349294,0.0006313214,0.000028432409,0.00063506747,0.0000048197435],"about_ca_topic_score_codex":0.051242854,"about_ca_topic_score_gemma":0.11556153,"teacher_disagreement_score":0.051242854,"about_ca_system_score_codex":0.00041701095,"about_ca_system_score_gemma":0.0004181602,"threshold_uncertainty_score":0.10188919},"labels":[],"label_agreement":null},{"id":"W4294904778","doi":"10.21203/rs.3.rs-1906712/v1","title":"Conversations between earthquakes: Dynamics and delays of the 2019 Ridgecrest rupture sequence","year":2022,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geodetic datum; Earthquake simulation; Earthquake rupture; Geology; Fault (geology); Seismic hazard; Stress field; Sequence (biology); Aftershock; Geodesy; Engineering; Structural engineering","score_opus":0.07281497015321686,"score_gpt":0.33658128047884817,"score_spread":0.2637663103256313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294904778","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938293,0.00019040226,0.00022345252,0.0016380012,0.000024467554,0.0000039974498,0.0006668999,0.000019227618,0.0034041668],"genre_scores_gemma":[0.9991013,0.000069541275,0.00008749698,0.000087362234,0.000018100487,0.0000038745748,0.00023407725,0.000006874351,0.00039132824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999642,0.00014502817,0.000019471383,0.00007928138,0.00006330871,0.000050980707],"domain_scores_gemma":[0.99766445,0.0012013407,0.0004940551,0.00008829497,0.00022106219,0.00033076675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008662195,0.00011356961,0.00013299957,0.00065435696,0.0008704661,0.001471589,0.00027275234,0.00070815167,0.002994252],"category_scores_gemma":[0.006850113,0.00013988289,0.00006582904,0.0006267097,0.0006614663,0.001389522,0.001636254,0.0006754559,0.00028002964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082546513,0.0001617178,0.70584035,0.00027254134,0.00010488733,0.0026994746,0.16554311,0.005988543,0.007982093,0.0167786,0.027693102,0.06611011],"study_design_scores_gemma":[0.000021993337,0.00016369385,0.8153536,0.00022716586,0.000035103047,0.00034483994,0.13085791,0.009588996,0.0013606003,0.004703507,0.037238702,0.00010393252],"about_ca_topic_score_codex":0.024575345,"about_ca_topic_score_gemma":0.037712384,"teacher_disagreement_score":0.024575345,"about_ca_system_score_codex":0.0014940312,"about_ca_system_score_gemma":0.00053103716,"threshold_uncertainty_score":0.048864603},"labels":[],"label_agreement":null},{"id":"W4295037292","doi":"10.1029/2022jb024354","title":"Limited Earthquake Interaction During a Geothermal Hydraulic Stimulation in Helsinki, Finland","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Helmholtz Association","keywords":"Induced seismicity; Geophone; Geothermal gradient; Seismology; Geology; Hydraulic fracturing; Magnitude (astronomy); Borehole; Rock mass classification; Geophysics; Geotechnical engineering; Physics","score_opus":0.045155125991264485,"score_gpt":0.31703675698758316,"score_spread":0.2718816309963187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295037292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996798,0.000006083319,0.00006484549,0.000003873444,6.988365e-7,0.0000024334704,0.000045719065,0.0000037327252,0.00019281],"genre_scores_gemma":[0.9998399,0.0000049057744,0.000024651355,0.0000016608852,0.0000012418867,0.0000023912482,0.00006289118,4.4282098e-7,0.00006197191],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988914,0.000016179072,0.0000074093673,0.000023348042,0.000032211727,0.000031755546],"domain_scores_gemma":[0.9996871,0.000086912136,0.000094808354,0.00002013787,0.000041492352,0.00006955073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015879754,0.00015053453,0.00018514275,0.00040175268,0.00018972174,0.00022657777,0.00019192658,0.00028660777,0.0008227097],"category_scores_gemma":[0.0004906434,0.00010202932,0.00011338521,0.00039611047,0.0002828376,0.00017377813,0.0003761739,0.00012309184,0.000091283015],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011372279,0.00036259956,0.87270457,0.000115791976,0.00016786881,0.0026916703,0.0015488437,0.013445518,0.09123567,0.00018053183,0.00041729544,0.015992489],"study_design_scores_gemma":[0.0000107419255,0.00024134059,0.9919384,0.0000043635373,0.000021317608,0.00010471531,0.00047909326,0.003908754,0.003039041,0.0000273771,0.00021457562,0.000010134446],"about_ca_topic_score_codex":0.0037671993,"about_ca_topic_score_gemma":0.0075064483,"teacher_disagreement_score":0.0037671993,"about_ca_system_score_codex":0.00038985204,"about_ca_system_score_gemma":0.00026811348,"threshold_uncertainty_score":0.0074905157},"labels":[],"label_agreement":null},{"id":"W4295279329","doi":"10.1785/0220220001","title":"Source Parameters of the Mw 5.7 Pica Crustal Earthquake in Northern Chile","year":2022,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Calgary; University of Victoria","funders":"","keywords":"Geology; Seismology; Aftershock; Crust; Fault (geology); Intraplate earthquake; Seismic hazard; Tectonics; Geophysics","score_opus":0.055611602747301356,"score_gpt":0.27398735254018064,"score_spread":0.21837574979287927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295279329","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936633,0.00016109251,0.00032854476,0.000103193146,0.0000054405086,0.000021444637,0.0018248439,0.00006670165,0.0038254529],"genre_scores_gemma":[0.9985671,0.00004116332,0.00008224224,0.00000479865,0.000002985002,0.000010649633,0.00081244216,0.000006851674,0.00047176497],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995923,0.0000070994015,0.0000044398666,0.0000097269685,0.000010399728,0.000009125563],"domain_scores_gemma":[0.9997658,0.00005662802,0.00005897734,0.000020674248,0.00006670375,0.000031160816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014324798,0.00020815166,0.00018700103,0.00085068116,0.00024172387,0.000361334,0.000277536,0.00019330512,0.0026985658],"category_scores_gemma":[0.0009930204,0.00012729781,0.00014194864,0.00082322134,0.00013843758,0.00021539174,0.000393941,0.00014241147,0.00043594214],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035048506,0.000090661335,0.9082422,0.00025024544,0.00011861422,0.0023534552,0.0009331649,0.035115287,0.011347917,0.0008497985,0.0054058814,0.034942247],"study_design_scores_gemma":[0.000038991824,0.00003186447,0.9733666,0.00003189852,0.000026193557,0.00017596887,0.0008347373,0.02244031,0.0007224872,0.00025735784,0.002054717,0.000018826247],"about_ca_topic_score_codex":0.038700566,"about_ca_topic_score_gemma":0.023381243,"teacher_disagreement_score":0.038700566,"about_ca_system_score_codex":0.0006565771,"about_ca_system_score_gemma":0.0003993492,"threshold_uncertainty_score":0.07695061},"labels":[],"label_agreement":null},{"id":"W4295911722","doi":"10.1080/00288306.2022.2117829","title":"Late Holocene earthquakes on the Papatea Fault and its role in past earthquake cycles, Marlborough, New Zealand","year":2022,"lang":"en","type":"article","venue":"New Zealand Journal of Geology and Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Hazards Research Platform","keywords":"Geology; Seismology; Sinistral and dextral; Holocene; Fault (geology); Trench; Seismic gap; Active fault; Slip (aerodynamics); Strike-slip tectonics; Paleontology; Engineering","score_opus":0.01113059074966935,"score_gpt":0.20483655793574926,"score_spread":0.1937059671860799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295911722","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99774325,0.00014051015,0.000048141806,0.00009257222,0.0000022454078,0.0000066538437,0.0002645732,0.0000039348984,0.0016981425],"genre_scores_gemma":[0.99922955,0.00011599435,0.000045739198,0.000005204523,0.0000018189778,0.0000039317624,0.000090428024,0.0000014770679,0.00050590135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991727,0.00000806908,0.0000075330386,0.000026737394,0.000018531919,0.000021910615],"domain_scores_gemma":[0.99957055,0.000039455746,0.00020406525,0.000020490095,0.0000923336,0.000073030955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019021625,0.00016655635,0.00011098562,0.0009636552,0.0006390549,0.0009070111,0.00031905816,0.00020740139,0.002836495],"category_scores_gemma":[0.0010135135,0.00018409747,0.00012805055,0.0012243441,0.0006105658,0.0005036149,0.0005222539,0.00023359935,0.00025405682],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009724194,0.000030134033,0.9673804,0.00008808383,0.00004446697,0.00085081207,0.0047142124,0.00035214517,0.0049604694,0.00033998763,0.00040137675,0.02074067],"study_design_scores_gemma":[0.0000011739655,0.0000086293885,0.99907315,0.000007248858,0.0000030028937,0.000036280395,0.00037762447,0.00009200942,0.00002821314,0.000016090746,0.00035482607,0.0000016960137],"about_ca_topic_score_codex":0.38284463,"about_ca_topic_score_gemma":0.63840824,"teacher_disagreement_score":0.38284463,"about_ca_system_score_codex":0.0017659839,"about_ca_system_score_gemma":0.0011055983,"threshold_uncertainty_score":0.76123244},"labels":[],"label_agreement":null},{"id":"W4296142652","doi":"10.21203/rs.3.rs-2007128/v1","title":"Spatial and temporal variations in b-value of earthquake magnitude–frequency distributions and crustal stress in north part of the Zagros region","year":2022,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; International Institute of Earthquake Engineering and Seismology","keywords":"Geology; Magnitude (astronomy); Induced seismicity; Seismology; Tectonics; Stress field; Spatial distribution; Geodesy","score_opus":0.0460671747673464,"score_gpt":0.3036594775656285,"score_spread":0.2575923027982821,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296142652","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991411,0.00011304379,0.000070921764,0.000012187208,0.000002217416,0.0000014523181,0.00029611163,0.0000050646963,0.00035778547],"genre_scores_gemma":[0.99911636,0.00006446492,0.0001357794,0.0000037941686,0.0000031191648,0.0000017938869,0.00046376712,0.0000016523097,0.00020924395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989176,0.00001307264,0.000014293331,0.00004213321,0.000013305581,0.000025354424],"domain_scores_gemma":[0.9997298,0.00002669371,0.00013410446,0.000029079918,0.000046310357,0.000033965334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019958235,0.00013944713,0.00016040428,0.00090646645,0.00017027864,0.0003315652,0.00012689654,0.00012321351,0.0007482059],"category_scores_gemma":[0.00032057505,0.000089478344,0.00015738764,0.0008912006,0.00014771982,0.00016896985,0.0002229276,0.00010720349,0.00017427908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013479334,0.000017325501,0.98362386,0.000038089012,0.00006538713,0.00017648935,0.0006685984,0.00044556655,0.0030042746,0.000078127494,0.0003003142,0.011447193],"study_design_scores_gemma":[9.839746e-7,0.000005260428,0.9995159,0.000003834587,0.0000043097434,0.000026930631,0.000108637,0.000109039116,0.000045234458,0.0000045206657,0.00017436434,9.927376e-7],"about_ca_topic_score_codex":0.033661377,"about_ca_topic_score_gemma":0.048137873,"teacher_disagreement_score":0.033661377,"about_ca_system_score_codex":0.0002789095,"about_ca_system_score_gemma":0.0001412988,"threshold_uncertainty_score":0.06693089},"labels":[],"label_agreement":null},{"id":"W4296337586","doi":"10.1007/978-3-031-11898-2_62","title":"Influence of Local Soil Conditions on the Damage Distribution in Izmir Bay During the October 30, 2020, Samos Earthquake","year":2022,"lang":"en","type":"book-chapter","venue":"Geotechnical, geological and earthquake engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"Epicenter; Alluvium; Bay; Moment magnitude scale; Seismology; Geology; Structural basin; Geomorphology; Oceanography","score_opus":0.008692167437880623,"score_gpt":0.18153489298997208,"score_spread":0.17284272555209146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296337586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963103,0.0002640917,0.00003409002,0.00007741547,0.000006102493,0.000001940603,0.000856169,0.0000074619356,0.0024424093],"genre_scores_gemma":[0.99827075,0.00011611946,0.000024562416,0.000008602228,0.0000041630205,0.0000013065364,0.00054993207,0.0000021036503,0.001022329],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999207,0.000012603147,0.000007231528,0.000017036338,0.000014750291,0.000027569498],"domain_scores_gemma":[0.9998447,0.000024286328,0.00005975955,0.0000065856575,0.00003815871,0.000026620812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016481303,0.00015850921,0.0001275582,0.000610247,0.0002665846,0.00056598056,0.00021871409,0.00022505254,0.0026232942],"category_scores_gemma":[0.00038986898,0.000091943024,0.00017846706,0.0007841827,0.00023053751,0.00026226082,0.00041219158,0.00015732882,0.0003650448],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023561186,0.00006224996,0.9728405,0.00004984092,0.00007706229,0.00061192206,0.000658419,0.0037887462,0.0016563609,0.0002879043,0.0019072543,0.017824112],"study_design_scores_gemma":[7.8044326e-7,0.00001518428,0.99872226,0.0000039164615,0.000010870505,0.000024266375,0.00046036497,0.00035046073,0.00005219858,0.000019757814,0.0003379205,0.0000020807472],"about_ca_topic_score_codex":0.06364285,"about_ca_topic_score_gemma":0.19272943,"teacher_disagreement_score":0.06364285,"about_ca_system_score_codex":0.0009471005,"about_ca_system_score_gemma":0.0004057035,"threshold_uncertainty_score":0.12654483},"labels":[],"label_agreement":null},{"id":"W4296345968","doi":"10.3390/geosciences12090350","title":"Hazard and Risk-Based Tsunami Early Warning Algorithms for Ocean Bottom Sensor S-Net System in Tohoku, Japan, Using Sequential Multiple Linear Regression","year":2022,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Warning system; Epicenter; Akaike information criterion; Early warning system; Seismology; Hazard; Computer science; Amplitude; Algorithm; Linear regression; Real-time computing; Geology; Data mining; Machine learning; Telecommunications","score_opus":0.03375404353456371,"score_gpt":0.2523060530694178,"score_spread":0.21855200953485407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296345968","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.45468992,0.0003214367,0.542497,0.00020474398,0.000035568213,0.000026629426,0.000110902736,0.00091605214,0.0011978055],"genre_scores_gemma":[0.9336478,0.00010323248,0.06487103,0.000021168813,0.000013074068,0.000024014325,0.0002011698,0.000030666524,0.0010878353],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987817,0.000024020883,0.00000861654,0.00003628301,0.000035807192,0.000017200742],"domain_scores_gemma":[0.9997731,0.00007438898,0.00004806515,0.00001478931,0.00007471033,0.000015033658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032541383,0.00068121887,0.00033484952,0.00029932428,0.00021195144,0.0003039939,0.00047417104,0.00024537533,0.0004590868],"category_scores_gemma":[0.0010466704,0.00024439074,0.00034807442,0.00030417857,0.0001387504,0.0004164526,0.00036475484,0.0003987504,0.00013320416],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017624725,0.00006623715,0.008617326,0.00004322636,0.00005624424,0.00007158066,0.000055656717,0.87642443,0.007667936,0.0004943101,0.00055827486,0.10576856],"study_design_scores_gemma":[0.000002006928,0.0000122299025,0.00064968417,4.89162e-7,0.0000035946348,0.000003573358,0.0000044161625,0.9986914,0.00051493966,0.00007429475,0.0000416191,0.0000017325503],"about_ca_topic_score_codex":0.01524517,"about_ca_topic_score_gemma":0.012320418,"teacher_disagreement_score":0.01524517,"about_ca_system_score_codex":0.00036914737,"about_ca_system_score_gemma":0.0006584514,"threshold_uncertainty_score":0.030312836},"labels":[],"label_agreement":null},{"id":"W4296457604","doi":"10.1785/0220220144","title":"Positive Correlation between DYFI Intensity Data and Microzonation Site Classes for Ottawa, Quebec City, and the Metropolitan Area of Montreal","year":2022,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; McGill University","funders":"","keywords":"Seismology; Seismic microzonation; Seismometer; Geology; Borehole; Seismic hazard; Peak ground acceleration; Magnitude (astronomy); Richter magnitude scale; Ground motion; Geotechnical engineering","score_opus":0.08448553180941969,"score_gpt":0.3132676615780593,"score_spread":0.2287821297686396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296457604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9680836,0.00023374784,0.0003340383,0.00028714098,0.000015626532,0.00007913173,0.023146823,0.00011462731,0.007705272],"genre_scores_gemma":[0.9887277,0.00012130397,0.00032773352,0.000036179725,0.0000057833527,0.000033651693,0.008092394,0.000014336395,0.0026409829],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999595,0.000024470532,0.000021943906,0.00008543043,0.00012290664,0.00015031477],"domain_scores_gemma":[0.99687284,0.00022455318,0.00058855297,0.00010204885,0.0016318732,0.0005801574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000289079,0.00039890857,0.00023536326,0.0024546818,0.0010587021,0.0015008007,0.00085944333,0.0002591407,0.0044882465],"category_scores_gemma":[0.002060594,0.00016071124,0.00032186188,0.0030318494,0.00048733866,0.00029113903,0.00057928753,0.00036229362,0.00040556045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004576068,0.000018065082,0.98925704,0.000022943763,0.00006595838,0.000046250887,0.00026463863,0.0005003564,0.0005383025,0.0001289153,0.0036401683,0.005471572],"study_design_scores_gemma":[0.000002588437,0.0000047386775,0.99801636,0.000008000001,0.000009497029,0.000008745504,0.0004969491,0.000430647,0.00011468564,0.0000080089785,0.00089075556,0.000008977024],"about_ca_topic_score_codex":0.99163216,"about_ca_topic_score_gemma":0.99690765,"teacher_disagreement_score":0.012164966,"about_ca_system_score_codex":0.012164966,"about_ca_system_score_gemma":0.007870702,"threshold_uncertainty_score":0.08826339},"labels":[],"label_agreement":null},{"id":"W4296740998","doi":"10.3390/en15196877","title":"Assessment of the Brittle–Ductile State of Major Injection and Confining Formations in the Alberta Basin","year":2022,"lang":"en","type":"article","venue":"Energies","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Waterloo; University of Alberta","funders":"","keywords":"Geology; Brittleness; Caprock; Structural basin; Induced seismicity; Seismology; Geotechnical engineering; Overburden pressure; Hazard analysis; Mining engineering; Petrology; Geomorphology; Engineering","score_opus":0.0107494947541109,"score_gpt":0.2194403865384298,"score_spread":0.20869089178431888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296740998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988649,0.000060265826,0.0003231692,0.0000073158517,3.6058884e-7,0.0000064106184,0.00012854917,0.000011037456,0.00059798715],"genre_scores_gemma":[0.99904317,0.00006463249,0.0005400484,0.0000034827317,4.134598e-7,0.0000026105809,0.000116122676,0.0000016598055,0.00022785597],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981874,0.000011582473,0.00001026906,0.000032471617,0.0000933352,0.000033673587],"domain_scores_gemma":[0.99967957,0.00003976859,0.000081432714,0.000018752295,0.00012126382,0.00005926995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030035566,0.00027979133,0.00016404211,0.0022047814,0.00056196545,0.00065307476,0.00045382185,0.00019022186,0.00042259027],"category_scores_gemma":[0.0006394589,0.00018892044,0.00015392332,0.0014716842,0.00062635355,0.00020773013,0.0004988156,0.00013886872,0.00005519239],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000067819296,0.000020659845,0.9640806,0.000020900108,0.000031111384,0.00021337594,0.00062051456,0.0056139794,0.013924406,0.00014450494,0.000050347146,0.0152118085],"study_design_scores_gemma":[0.000001661743,0.000014701721,0.9953725,0.00000402272,0.00000922493,0.000039302628,0.00029977114,0.0028531442,0.001189258,0.000036939473,0.0001747971,0.0000048065745],"about_ca_topic_score_codex":0.6407805,"about_ca_topic_score_gemma":0.8710333,"teacher_disagreement_score":0.3592195,"about_ca_system_score_codex":0.002939127,"about_ca_system_score_gemma":0.0018211302,"threshold_uncertainty_score":0.72266996},"labels":[],"label_agreement":null},{"id":"W4297312356","doi":"10.1111/bre.12716","title":"Architecture, structural and tectonic significance of the Seagap fault (offshore Tanzania) in the framework of the East African Rift","year":2022,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; Università degli Studi di Napoli Federico II; National Science Foundation","keywords":"Geology; Seismology; Rift; Fault (geology); Seafloor spreading; Tectonics; Paleontology; Strike-slip tectonics; Neogene; Detachment fault; Trough (economics); Fracture zone; Structural basin; Extensional definition","score_opus":0.040038904698186856,"score_gpt":0.28710718077102954,"score_spread":0.24706827607284268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297312356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991053,0.00013533086,0.00006381406,0.000015234612,8.953878e-7,0.0000018176402,0.000045616027,0.0000032027847,0.00062878],"genre_scores_gemma":[0.9997409,0.000049264156,0.00009061696,0.000001929097,6.812615e-7,8.438716e-7,0.000029457173,6.7629776e-7,0.00008556676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999676,0.000004572562,0.0000021457465,0.000008044151,0.0000050586427,0.000012609809],"domain_scores_gemma":[0.9999114,0.000007984202,0.000043298696,0.000005617042,0.00001755586,0.000014162375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008487859,0.000119005876,0.000059263904,0.0010123652,0.00028604787,0.00040200993,0.00011348126,0.000169869,0.00096956256],"category_scores_gemma":[0.00024825186,0.000113609676,0.00006186521,0.0007117694,0.0003845523,0.00016989055,0.00032907267,0.0001190808,0.000114344824],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013864976,0.000024333314,0.91303444,0.00009095579,0.000036020454,0.0020366749,0.0040128515,0.002957949,0.038426213,0.0018770989,0.00026714712,0.037097633],"study_design_scores_gemma":[0.0000020977384,0.000028489912,0.9976368,0.000023093296,0.000008495808,0.00020142226,0.0006020611,0.0005719043,0.00027776105,0.00008818994,0.00055642903,0.0000032518367],"about_ca_topic_score_codex":0.011600402,"about_ca_topic_score_gemma":0.025708623,"teacher_disagreement_score":0.011600402,"about_ca_system_score_codex":0.0003435845,"about_ca_system_score_gemma":0.00029118176,"threshold_uncertainty_score":0.023065746},"labels":[],"label_agreement":null},{"id":"W4297349457","doi":"10.56952/arma-2022-0713","title":"Waveform Similarity of Micro-Seismicity at the ToC2ME Hydraulic Fracturing Experiment Site","year":2022,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Microseism; Induced seismicity; Seismology; Hydraulic fracturing; Waveform; Geology; Magnitude (astronomy); PageRank; Similarity (geometry); Geotechnical engineering; Engineering; Computer science","score_opus":0.016785596090011835,"score_gpt":0.21380312826908668,"score_spread":0.19701753217907483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297349457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998387,0.000010147664,0.00036672334,0.000007354734,0.00000202848,0.000011042511,0.0006539568,0.000022098578,0.0005396724],"genre_scores_gemma":[0.99816895,0.00000873193,0.00037181447,0.0000043018963,0.0000020626674,0.00000803297,0.0009513209,0.0000035523199,0.00048124237],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997886,0.000014973711,0.000008477212,0.000035474033,0.00011303272,0.00003955603],"domain_scores_gemma":[0.9994628,0.00007493186,0.0001178385,0.000030445395,0.0002115007,0.000102523576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020636678,0.00015585092,0.00014236613,0.0008696645,0.00026321047,0.00032407077,0.00021891376,0.00023388391,0.0013105789],"category_scores_gemma":[0.0007305872,0.00006860659,0.000085662294,0.0007451007,0.00018841944,0.00013975357,0.0002794301,0.00014210153,0.00020255097],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005412458,0.0001431004,0.9120687,0.00006255625,0.000067449546,0.00043475686,0.00096594304,0.0013474236,0.055325493,0.000114095914,0.00084474235,0.028084502],"study_design_scores_gemma":[0.0000019580393,0.000041681706,0.99791855,0.0000012748156,0.0000034688726,0.0000404618,0.00020018347,0.0006277891,0.0009841017,0.000008634908,0.0001687245,0.000003223935],"about_ca_topic_score_codex":0.03681908,"about_ca_topic_score_gemma":0.11201605,"teacher_disagreement_score":0.03681908,"about_ca_system_score_codex":0.0005414111,"about_ca_system_score_gemma":0.00037049784,"threshold_uncertainty_score":0.073209524},"labels":[],"label_agreement":null},{"id":"W4297386154","doi":"10.1002/essoar.10512473.1","title":"A Long-Term Earthquake Catalog for the Endeavour Segment: Constraints on the Extensional Cycle and Evidence for Hydrothermal Venting Supported by Propagating Rifts","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Ocean Networks Canada Society; University of Victoria","funders":"National Defense Science and Engineering Graduate; National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Seismometer; Rift; Magmatism; Ridge; Observatory; Bathymetry; Mid-ocean ridge; Crust; Geophysics; Paleontology; Tectonics; Oceanography","score_opus":0.058044571494088454,"score_gpt":0.2823882320555445,"score_spread":0.22434366056145602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297386154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98531795,0.00009543536,0.00041106876,0.00003109652,0.0000029552416,0.000028125023,0.012191977,0.000057626363,0.0018638439],"genre_scores_gemma":[0.94230634,0.00015483315,0.0019436816,0.000016294693,0.00001611836,0.00004550259,0.05445597,0.000026351914,0.0010350151],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999798,0.000013712005,0.000025680458,0.000047442612,0.00006225642,0.000053040654],"domain_scores_gemma":[0.99836725,0.00010630887,0.0005505465,0.00019682808,0.0004018375,0.00037731664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002967655,0.00027137317,0.00024549608,0.003478806,0.00036312177,0.00054327183,0.00035589127,0.00022107255,0.001481068],"category_scores_gemma":[0.0012410785,0.0001347014,0.0002280981,0.0032381,0.00020967808,0.00035799338,0.0008143418,0.0001821829,0.0005550494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032614753,0.00002237005,0.9813291,0.000032402975,0.000023573959,0.00018052963,0.00033803677,0.0005335652,0.005103349,0.000072858886,0.00076595694,0.011565538],"study_design_scores_gemma":[0.0000035154803,0.00001144701,0.99797934,0.000005508529,0.000006188688,0.00006143466,0.000120128905,0.00042585476,0.0002094538,0.000015985157,0.001157527,0.0000035941348],"about_ca_topic_score_codex":0.09181899,"about_ca_topic_score_gemma":0.2354461,"teacher_disagreement_score":0.09181899,"about_ca_system_score_codex":0.000562422,"about_ca_system_score_gemma":0.0009827206,"threshold_uncertainty_score":0.18256909},"labels":[],"label_agreement":null},{"id":"W4297900407","doi":"10.3389/feart.2022.945297","title":"Long-term triggered seismicity on the Mosha fault by Damavand volcano, Iran: Implications on the seismic hazard of Tehran metropolis","year":2022,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; International Institute of Earthquake Engineering and Seismology; École Polytechnique Fédérale de Lausanne; Strong","keywords":"Seismology; Geology; Induced seismicity; Aftershock; Volcano; Fault (geology); Active fault; Seismic hazard; North Anatolian Fault","score_opus":0.021526503732638008,"score_gpt":0.23132073340289552,"score_spread":0.20979422967025751,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297900407","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992636,0.00013440326,0.000022896622,0.00008803176,0.0000039267475,0.0000021558146,0.0000792398,0.0000022931747,0.0004034112],"genre_scores_gemma":[0.9996178,0.00015045171,0.00002843812,0.000009188938,0.000014284483,0.000001313891,0.000099311146,6.2148337e-7,0.00007852017],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999162,0.000009024493,0.000006426436,0.000015954225,0.000021835705,0.000030536256],"domain_scores_gemma":[0.9997322,0.000029108318,0.00012663435,0.00000963481,0.000044418208,0.00005796631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018947462,0.00023963567,0.00017169806,0.0011048734,0.0004236434,0.0004830424,0.00024331102,0.00029850152,0.0007867586],"category_scores_gemma":[0.00042791668,0.000110496476,0.00019892729,0.00094451016,0.00041624406,0.00033377385,0.0004225216,0.00019419241,0.00010998286],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056962526,0.000039655588,0.98716104,0.000024915813,0.000031164676,0.0008924769,0.0006963289,0.0006125836,0.0019080166,0.00016149768,0.00027752304,0.008137921],"study_design_scores_gemma":[0.000002306625,0.000018033246,0.99846554,0.0000041138624,0.000007332592,0.000112831054,0.00075476407,0.00031108526,0.00006371088,0.00004022386,0.00021743694,0.0000027083931],"about_ca_topic_score_codex":0.015554464,"about_ca_topic_score_gemma":0.025035894,"teacher_disagreement_score":0.015554464,"about_ca_system_score_codex":0.0007062303,"about_ca_system_score_gemma":0.00065053033,"threshold_uncertainty_score":0.030927837},"labels":[],"label_agreement":null},{"id":"W4297973559","doi":"10.1029/2022jb024471","title":"Finding Simplicity in the Complexity of Postseismic Coastal Uplift and Subsidence Following Great Subduction Earthquakes","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; McGill University; University of Victoria","funders":"","keywords":"Geology; Subduction; Seismology; Slip (aerodynamics); Forearc; Subsidence; Lithosphere; Trench; Tectonics; Geomorphology","score_opus":0.1008226732484277,"score_gpt":0.3390219616011674,"score_spread":0.23819928835273968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297973559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99556136,0.000043189542,0.0033097507,0.00006738733,0.000004806427,0.0000061326873,0.000100965764,0.00002794154,0.00087844604],"genre_scores_gemma":[0.9995746,0.0000143338375,0.00024785282,0.0000043723408,0.0000015170558,0.0000022103259,0.000039545,0.0000035982016,0.00011184585],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.000016116417,0.000007696675,0.000027143764,0.000009493201,0.000016625341],"domain_scores_gemma":[0.9997931,0.00005698322,0.0000661235,0.000039549115,0.000020868367,0.000023381761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019954164,0.0002126934,0.00016978708,0.00026501063,0.00015593877,0.0005324508,0.0003231215,0.00047710835,0.0006986234],"category_scores_gemma":[0.00078183605,0.00018282606,0.00038105788,0.00020563023,0.0004356943,0.00049868063,0.00038902953,0.00033381776,0.00007564441],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001303846,0.00014723817,0.19991481,0.00004789898,0.00015029976,0.00035115422,0.00028395804,0.7647845,0.019058451,0.0048306785,0.00039633358,0.009904268],"study_design_scores_gemma":[0.000012269,0.00005259766,0.11976123,0.000006346628,0.000018638593,0.000036985064,0.00007570077,0.877361,0.0011884993,0.0011172107,0.00035685935,0.000012639099],"about_ca_topic_score_codex":0.008766362,"about_ca_topic_score_gemma":0.005610784,"teacher_disagreement_score":0.008766362,"about_ca_system_score_codex":0.000384215,"about_ca_system_score_gemma":0.0002542439,"threshold_uncertainty_score":0.017430663},"labels":[],"label_agreement":null},{"id":"W4297983960","doi":"10.1029/2022jb025126","title":"Long‐Term Fluid Injection Can Expedite Fault Reactivation and Development: Riedel Shear Structures Illuminated by Induced Earthquakes in Alberta, Canada","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Induced seismicity; Shear (geology); Slip (aerodynamics); Lineament; RSS; Shear stress; Strike-slip tectonics; Active fault; Outcrop; Fault (geology); Tectonics; Petrology; Geomorphology; Engineering","score_opus":0.027194059656748735,"score_gpt":0.2772226014817455,"score_spread":0.25002854182499673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297983960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99702877,0.00014632789,0.0001091021,0.00010628608,0.0000028810796,0.000010547641,0.00077874475,0.000013265649,0.0018040757],"genre_scores_gemma":[0.99796695,0.00012242231,0.00016770563,0.000016853011,0.0000016374746,0.0000029636362,0.0004805422,0.0000034980396,0.0012373459],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998301,0.000008821091,0.0000073282026,0.000026753607,0.00004964105,0.00007743466],"domain_scores_gemma":[0.99968886,0.000023377539,0.00004724636,0.000010064551,0.00014677062,0.00008376155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001429782,0.0002453522,0.00020712888,0.0013389201,0.0013467554,0.0009137513,0.0006368861,0.00040367086,0.0016115276],"category_scores_gemma":[0.00040859295,0.0001730613,0.00020871825,0.0022837992,0.00064957066,0.00018646261,0.00051152625,0.00025592686,0.00014327858],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020970732,0.00009352914,0.96077895,0.00008323011,0.00009857979,0.0014808483,0.0039744466,0.0037945004,0.005706776,0.0006801279,0.0019086432,0.021190679],"study_design_scores_gemma":[0.000005757292,0.0000126916575,0.9932766,0.000013673549,0.00001696475,0.000046974168,0.003398348,0.0017480932,0.00018688412,0.000041928615,0.0012389731,0.000013171875],"about_ca_topic_score_codex":0.9907755,"about_ca_topic_score_gemma":0.99708694,"teacher_disagreement_score":0.013513257,"about_ca_system_score_codex":0.013513257,"about_ca_system_score_gemma":0.01316511,"threshold_uncertainty_score":0.098046005},"labels":[],"label_agreement":null},{"id":"W4300481497","doi":"10.1130/focus052008.1.","title":"Suprasubduction zone ophiolites and Archean tectonics","year":2008,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Archean; Ophiolite; Geology; Tectonics; Plate tectonics; Geochemistry; Earth science; Paleontology","score_opus":0.022185638194666867,"score_gpt":0.20372043039294807,"score_spread":0.1815347921982812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300481497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97887427,0.00097618415,0.00009536676,0.00014129744,0.00001509808,0.0000036200265,0.0003381439,0.000008607969,0.019547483],"genre_scores_gemma":[0.99752,0.00032094165,0.000048292048,0.00001150311,0.000007010906,0.0000010010658,0.00016945468,0.000002888735,0.0019189457],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998909,0.000013121442,0.0000072302787,0.000016787333,0.000021751914,0.00005024109],"domain_scores_gemma":[0.99976724,0.00003361551,0.000056397916,0.0000141091095,0.00006695023,0.00006163752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014384778,0.00017211473,0.0001539471,0.001821542,0.000510884,0.0009345885,0.00017252548,0.0001159367,0.0076257694],"category_scores_gemma":[0.0006853944,0.000058207832,0.00009393839,0.002306897,0.0006242694,0.0005656012,0.00078999955,0.00019552214,0.00028360338],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003169676,0.000028649745,0.9271867,0.00010385938,0.00007083472,0.00041571038,0.0029150953,0.0009195667,0.0049809474,0.012313786,0.00075446506,0.049993336],"study_design_scores_gemma":[0.000003930683,0.000012043373,0.9942725,0.0000144286505,0.000009632494,0.00006031239,0.0015506094,0.0001564814,0.00016737712,0.0005902782,0.003161025,0.0000014700727],"about_ca_topic_score_codex":0.16909741,"about_ca_topic_score_gemma":0.32983947,"teacher_disagreement_score":0.16909741,"about_ca_system_score_codex":0.0013485227,"about_ca_system_score_gemma":0.0014926888,"threshold_uncertainty_score":0.33622634},"labels":[],"label_agreement":null},{"id":"W4300703544","doi":"10.1139/cjes-2021-0103","title":"Deep long-period earthquakes near Mount Meager, British Columbia","year":2022,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Volcano; Seismology; Induced seismicity; Seismometer; Mount; Period (music); Volcanism; Tectonics","score_opus":0.015034311945706449,"score_gpt":0.19512019181929716,"score_spread":0.1800858798735907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300703544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99329245,0.000112904476,0.00021440037,0.00010174043,0.0000045357874,0.000018770757,0.0018455599,0.000046749185,0.0043628924],"genre_scores_gemma":[0.99497294,0.00012250098,0.0005076278,0.000028643273,0.0000017419617,0.000007740771,0.0013810667,0.000007339992,0.0029703395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984765,0.0000083593895,0.0000059428985,0.000035630743,0.000050039806,0.000052264175],"domain_scores_gemma":[0.9995516,0.00004230777,0.0000623577,0.000025990246,0.00022275384,0.00009502994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010583602,0.00022720448,0.00013834046,0.0011997798,0.001563249,0.00078528456,0.00045158563,0.00023003577,0.002238399],"category_scores_gemma":[0.00097596727,0.00013833572,0.000074844516,0.0016334521,0.00032130786,0.00019476782,0.00045908464,0.00024940984,0.00027193595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015630088,0.00005680571,0.9183726,0.000075109856,0.000045768636,0.00092639076,0.002043719,0.0029609753,0.015472659,0.00040531237,0.0060513043,0.053433057],"study_design_scores_gemma":[0.0000037570846,0.0000061891897,0.9943644,0.000012446484,0.0000056929457,0.00004958158,0.00074873806,0.0014141232,0.00064216345,0.000026138197,0.0027194193,0.0000074748277],"about_ca_topic_score_codex":0.97774875,"about_ca_topic_score_gemma":0.9964018,"teacher_disagreement_score":0.022251248,"about_ca_system_score_codex":0.008220245,"about_ca_system_score_gemma":0.0052510994,"threshold_uncertainty_score":0.059642315},"labels":[],"label_agreement":null},{"id":"W4300817537","doi":"10.1029/2022jb024881","title":"Analysis of the Hydrogeological Conditions Affecting Fault Response to Nearby Hydraulic Fracturing","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"University Research Board, American University of Beirut","keywords":"Induced seismicity; Hydrogeology; Hydraulic fracturing; Geology; Fault (geology); Pore water pressure; Petrology; Seismology; Microseism; Geotechnical engineering","score_opus":0.04006466938936335,"score_gpt":0.3358536811700587,"score_spread":0.29578901178069533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300817537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997017,0.000008106046,0.000098955206,0.0000030806748,5.385491e-7,0.0000020326218,0.00004520379,0.0000040690825,0.00013626002],"genre_scores_gemma":[0.9998889,0.000004216551,0.000027799715,7.040471e-7,3.121724e-7,5.525138e-7,0.000032995853,5.153337e-7,0.000043942793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992156,0.000008618048,0.000004934517,0.000014744986,0.000022153643,0.000027995162],"domain_scores_gemma":[0.99964714,0.0000613453,0.00011805968,0.000017872604,0.00009302258,0.000062468964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000120876604,0.00014896896,0.00018077988,0.0007648658,0.00025545977,0.00043505518,0.00019171077,0.00022945442,0.0006782212],"category_scores_gemma":[0.00059559435,0.00007456462,0.00013120909,0.0005003509,0.00035174968,0.00015104741,0.0001774999,0.00011867736,0.000093494775],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030748866,0.00007499188,0.8872616,0.000042414846,0.000058881058,0.00071523373,0.0003881931,0.011376394,0.092177995,0.00010454485,0.00010286947,0.0073892777],"study_design_scores_gemma":[0.000001451112,0.00003692578,0.99277425,0.0000012959147,0.000006632372,0.000034628276,0.00030516114,0.0046360716,0.0021190098,0.000016916903,0.000063007436,0.0000047050025],"about_ca_topic_score_codex":0.036541328,"about_ca_topic_score_gemma":0.04396227,"teacher_disagreement_score":0.036541328,"about_ca_system_score_codex":0.0005667647,"about_ca_system_score_gemma":0.00032916118,"threshold_uncertainty_score":0.07265729},"labels":[],"label_agreement":null},{"id":"W4300964738","doi":"10.1007/s40808-022-01542-z","title":"Tectonic geomorphology-based modeling reveals dominance of transpression in Taxila and the contiguous region in Pakistan: implications for seismic hazards","year":2022,"lang":"en","type":"article","venue":"Modeling Earth Systems and Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of the Fraser Valley","funders":"","keywords":"Geology; Tectonics; Active fault; Seismology; Geodetic datum; Geologic map; Transpression; Seismic hazard; Lineament; Geomorphology; Geodesy; Shear zone","score_opus":0.02465022580623598,"score_gpt":0.2292609924859661,"score_spread":0.2046107666797301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4300964738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99892443,0.000014744028,0.0001763096,0.000038507478,0.0000019691258,0.0000037062186,0.00022678272,0.000012382052,0.0006011669],"genre_scores_gemma":[0.9997085,0.000022549182,0.000088625515,0.0000023472285,7.799484e-7,0.0000015787894,0.000097843316,0.0000014066745,0.00007623418],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992967,0.000009977342,0.0000047386975,0.000017901131,0.0000069897956,0.000030631752],"domain_scores_gemma":[0.9998363,0.000046882204,0.00003967118,0.000015084446,0.000032959462,0.000028926568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011272705,0.00022054979,0.00020209918,0.0006681338,0.0006712615,0.00091641105,0.00046462077,0.00032053137,0.0014716365],"category_scores_gemma":[0.00048480058,0.00025949057,0.00034302895,0.0011421181,0.0003856926,0.00056075485,0.0003782917,0.00030402548,0.00018710876],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016188703,0.00016638802,0.83452487,0.00005208723,0.000110730136,0.0006230471,0.0009198517,0.1450076,0.0031834794,0.0013537195,0.00075733697,0.013139024],"study_design_scores_gemma":[0.000032784905,0.00007312284,0.6986907,0.000021097108,0.00006617883,0.00019018551,0.0032812415,0.29582617,0.00059023494,0.00046743554,0.00073055405,0.00003029495],"about_ca_topic_score_codex":0.31503007,"about_ca_topic_score_gemma":0.29155356,"teacher_disagreement_score":0.31503007,"about_ca_system_score_codex":0.0013124051,"about_ca_system_score_gemma":0.0018335956,"threshold_uncertainty_score":0.6263928},"labels":[],"label_agreement":null},{"id":"W4303021237","doi":"10.3389/feart.2022.1023018","title":"Dynamic risk framework for cascading compounding climate-geological hazards: A perspective on coastal communities in subduction zones","year":2022,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada","keywords":"Risk analysis (engineering); Computer science; Risk management; Hazard; Vulnerability (computing); Environmental resource management; Resilience (materials science); Climate change; Risk assessment; Coastal hazards; Subduction; Environmental science; Geology; Business; Oceanography; Computer security; Ecology; Seismology","score_opus":0.0169774619282756,"score_gpt":0.2593958103403303,"score_spread":0.24241834841205473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4303021237","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.015266319,0.0018758491,0.96526015,0.0029080706,0.00020431592,0.000056540408,0.0001680346,0.000069612506,0.014191183],"genre_scores_gemma":[0.8109099,0.0055316575,0.16510719,0.00044921,0.0006174724,0.00045748096,0.00028008275,0.00013317417,0.016513817],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9989104,0.0005766038,0.00005654375,0.00015038712,0.00019457012,0.00011147741],"domain_scores_gemma":[0.99823403,0.00088628544,0.00026472355,0.0000898356,0.00027918362,0.00024585292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026675493,0.0014895571,0.0010031889,0.0021048847,0.00094913936,0.0029778641,0.0021787726,0.001833134,0.0035673873],"category_scores_gemma":[0.0034921232,0.00043714914,0.0015660728,0.0014217576,0.0023114493,0.003433893,0.0030668832,0.002144794,0.0003322414],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007772279,0.000025026806,0.00069177616,0.00006951877,0.000042532705,0.00020842896,0.00022787655,0.27308184,0.00033781808,0.7194196,0.0010690254,0.004818765],"study_design_scores_gemma":[0.000004960847,0.00003509191,0.0004490139,0.00006709507,0.000029743713,0.000115046685,0.00028372207,0.6335398,0.00008167943,0.3610212,0.00434167,0.000031014133],"about_ca_topic_score_codex":0.008169668,"about_ca_topic_score_gemma":0.0071786935,"teacher_disagreement_score":0.008169668,"about_ca_system_score_codex":0.0028576548,"about_ca_system_score_gemma":0.0019175091,"threshold_uncertainty_score":0.020733833},"labels":[],"label_agreement":null},{"id":"W4303987197","doi":"10.1029/2022tc007317","title":"Eocene Terrane Accretion in Northern Cascadia Recorded by Brittle Left‐Lateral Slip on the San Juan Fault","year":2022,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Division of Earth Sciences; Natural Sciences and Engineering Research Council of Canada; Geological Society of America","keywords":"Terrane; Geology; Accretion (finance); Slip (aerodynamics); Paleontology; Seismology; Fault (geology); Cenozoic; Geomorphology; Tectonics; Structural basin","score_opus":0.0166026915486218,"score_gpt":0.21102355202018447,"score_spread":0.19442086047156268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4303987197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977162,0.000057104884,0.000027930138,0.0000248426,0.0000027090898,0.0000023401144,0.0004198841,0.000011560189,0.0017374518],"genre_scores_gemma":[0.9991053,0.000046554556,0.000046606307,0.0000052153623,0.0000026045857,0.0000034588936,0.00041973652,0.0000032950993,0.00036734276],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988043,0.000011216291,0.000009776345,0.00003948707,0.000031383992,0.000027670589],"domain_scores_gemma":[0.9994943,0.0000337889,0.00014909655,0.000041814226,0.00016678717,0.00011419611],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002341432,0.00029869,0.00020314437,0.0010939045,0.0007659803,0.0004823966,0.00028618128,0.00027801798,0.0016093779],"category_scores_gemma":[0.00059560314,0.00020297302,0.00017280094,0.0012821717,0.00042861028,0.00017255264,0.0005082057,0.00020383917,0.0002826761],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000063861764,0.000010452184,0.9917572,0.00002440853,0.000036262314,0.00026353117,0.0010250501,0.00031850257,0.003669778,0.000052941898,0.00026421086,0.0025137535],"study_design_scores_gemma":[0.0000010789498,0.0000037572304,0.9993332,0.000003753692,0.0000030491642,0.000023832208,0.0001987354,0.00007225698,0.00005056743,0.000006428474,0.0003019178,0.0000014904025],"about_ca_topic_score_codex":0.27498886,"about_ca_topic_score_gemma":0.5563795,"teacher_disagreement_score":0.27498886,"about_ca_system_score_codex":0.0015524449,"about_ca_system_score_gemma":0.0007937662,"threshold_uncertainty_score":0.54677653},"labels":[],"label_agreement":null},{"id":"W4304693772","doi":"10.1785/0220220162","title":"Revised Earthquake Geology Inputs for the Central and Eastern United States and Southeast Canada for the 2023 National Seismic Hazard Model","year":2022,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic hazard; Geology; Seismology; Fault (geology); Polygon (computer graphics); Active fault; Seismic gap; Geospatial analysis; Earthquake scenario; Remote sensing; Engineering","score_opus":0.06978799654659407,"score_gpt":0.2855360256528437,"score_spread":0.21574802910624963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4304693772","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0732631,0.00042575147,0.01862838,0.0018629504,0.0002782724,0.0004948428,0.800221,0.0047470722,0.100078665],"genre_scores_gemma":[0.40024,0.0013759828,0.03692715,0.00071180396,0.00006681733,0.00059661653,0.5176349,0.001384632,0.041062184],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994838,0.000045711367,0.000035493398,0.000076447075,0.00025425432,0.00010417674],"domain_scores_gemma":[0.99635327,0.00016670281,0.000085644635,0.0001503893,0.003095323,0.0001487806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063360744,0.00091205514,0.00053751585,0.0025955576,0.0014138025,0.002126358,0.002599862,0.00078897265,0.02113654],"category_scores_gemma":[0.0035641682,0.000590954,0.0009936104,0.0054398477,0.00037736332,0.0009318956,0.0007200207,0.0009869669,0.0047328547],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019620179,0.00017442486,0.08026586,0.0002703552,0.000183226,0.0003126398,0.00039679877,0.49330238,0.0006030383,0.024281891,0.34756696,0.052446257],"study_design_scores_gemma":[0.00023080151,0.000030364525,0.04966637,0.00029060966,0.0001397068,0.0001389388,0.0009958571,0.5204183,0.0017976555,0.008818141,0.4172677,0.00020565809],"about_ca_topic_score_codex":0.9794166,"about_ca_topic_score_gemma":0.9733863,"teacher_disagreement_score":0.030116616,"about_ca_system_score_codex":0.030116616,"about_ca_system_score_gemma":0.03299855,"threshold_uncertainty_score":0.21851236},"labels":[],"label_agreement":null},{"id":"W4306923006","doi":"10.1130/g50258.1","title":"Fault surface morphology as an indicator for earthquake nucleation potential","year":2022,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Nucleation; Slip (aerodynamics); Asperity (geotechnical engineering); Surface finish; Fault (geology); Fault plane; Surface roughness; Isotropy; Fractal; Surface (topology); Microscale chemistry; Mineralogy; Geometry; Seismology; Geotechnical engineering; Materials science; Composite material; Optics","score_opus":0.012871898977635342,"score_gpt":0.22915287387535524,"score_spread":0.21628097489771989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306923006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907327,0.000062437866,0.00044705055,0.0000037098087,0.000001215288,0.000004866203,0.000057214304,0.000012102782,0.000338161],"genre_scores_gemma":[0.9997311,0.000012405484,0.00015498142,0.0000014061069,5.600077e-7,0.0000022645343,0.00004510672,8.931096e-7,0.00005121996],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999026,0.000015819123,0.0000082601055,0.000020492094,0.00003491955,0.00001795082],"domain_scores_gemma":[0.9994842,0.00014758729,0.00018183295,0.00003726253,0.00008309722,0.00006611713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013832319,0.00012637729,0.0001690435,0.0005134788,0.00012775918,0.00033872743,0.000095177194,0.000174028,0.00070071546],"category_scores_gemma":[0.0006725794,0.0000876585,0.00009800431,0.00023072661,0.0002059921,0.00015917487,0.00018635721,0.00014028254,0.000101882404],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023841644,0.00005887084,0.16818099,0.000048068454,0.00003035545,0.00014465446,0.00011163733,0.0009162973,0.8246332,0.0001233445,0.00008140951,0.0054328395],"study_design_scores_gemma":[0.0000063399184,0.00041725655,0.8642802,0.0000072637636,0.000019310717,0.00032931333,0.00019317691,0.006507418,0.12787648,0.000081773316,0.00027133978,0.000010011965],"about_ca_topic_score_codex":0.0007067254,"about_ca_topic_score_gemma":0.0008297944,"teacher_disagreement_score":0.0007067254,"about_ca_system_score_codex":0.0001765319,"about_ca_system_score_gemma":0.00005900929,"threshold_uncertainty_score":0.0023441315},"labels":[],"label_agreement":null},{"id":"W4307045772","doi":"10.1093/gji/ggac416","title":"Modelling of fluid pressure migration in a pressure sensitive fault zone subject to cyclic injection and implications for injection-induced seismicity","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Helmholtz-Gemeinschaft","keywords":"Induced seismicity; Geology; Microseism; Amplitude; Pore water pressure; Permeability (electromagnetism); Geothermal gradient; Attenuation; Fault (geology); Poromechanics; Seismic hazard; Fluid pressure; Seismology; Mechanics; Geotechnical engineering; Geophysics; Chemistry","score_opus":0.025225214868038335,"score_gpt":0.2527026062607669,"score_spread":0.22747739139272857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307045772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.955523,0.00023636046,0.03704208,0.0002503323,0.000037597696,0.000059661004,0.0002620859,0.00016764319,0.0064212773],"genre_scores_gemma":[0.9973584,0.000068149355,0.0017110369,0.000010415232,0.000004490798,0.000021651531,0.00004136579,0.000009843647,0.000774542],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990356,0.000021884149,0.000007824307,0.000020716672,0.000020241383,0.000025712308],"domain_scores_gemma":[0.9996909,0.00013574376,0.000083609295,0.000022769329,0.000042095267,0.000024886453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018600357,0.00044071948,0.00030593286,0.00046233734,0.00030190684,0.0007261626,0.0006590108,0.0014616548,0.0012859128],"category_scores_gemma":[0.0009035544,0.0002210778,0.00047848007,0.00031631143,0.00094877265,0.0004061069,0.00043178376,0.00045241741,0.0000966308],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003809388,0.00004216572,0.0021338246,0.000029239669,0.000007632746,0.00015709942,0.000034936682,0.98895043,0.0063042934,0.0009091511,0.00006753271,0.0013255569],"study_design_scores_gemma":[0.000003721337,0.000017821836,0.00043026672,0.000002290547,0.0000022167862,0.000012301764,0.000010495017,0.9987317,0.0005938287,0.00012608699,0.00006606565,0.0000031711268],"about_ca_topic_score_codex":0.012011582,"about_ca_topic_score_gemma":0.003366395,"teacher_disagreement_score":0.012011582,"about_ca_system_score_codex":0.0006225268,"about_ca_system_score_gemma":0.00065081747,"threshold_uncertainty_score":0.023883343},"labels":[],"label_agreement":null},{"id":"W4307237962","doi":"10.3390/geosciences12110392","title":"The Response of the Rivers of NW Greece to Late Quaternary Neotectonics, as Interpreted from Detrital Petrology","year":2022,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Saint Mary's University; Bedford Institute of Oceanography; Dalhousie University; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Quaternary; Graben; Fluvial; Neotectonics; River terraces; Clastic rock; Terrace (agriculture); Geomorphology; Geochemistry; Paleontology; Structural basin; Archaeology","score_opus":0.009376938597000643,"score_gpt":0.20893315474352278,"score_spread":0.19955621614652214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307237962","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982476,0.0000811557,0.000048280977,0.00001647615,0.00000122097,0.0000019239685,0.00008507673,0.0000040883824,0.0015142006],"genre_scores_gemma":[0.9993581,0.00006801335,0.000040244387,0.000006633485,0.0000014984136,0.000001819434,0.000096484844,0.0000025748093,0.00042462017],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999902,0.000018085026,0.000011530788,0.000035079676,0.000016412156,0.00001681763],"domain_scores_gemma":[0.99986374,0.000020411566,0.000049889226,0.00001794841,0.000028357765,0.000019593963],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012471531,0.00011070488,0.00010478441,0.0009523215,0.00021484759,0.0005822731,0.00016821799,0.00022270114,0.001226045],"category_scores_gemma":[0.00065058394,0.00013082207,0.00010379718,0.00078662334,0.0004651942,0.00025944848,0.00046043072,0.00011105602,0.00021232177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007509219,0.000021565978,0.9520604,0.00006998674,0.000090940004,0.00050401414,0.0024216291,0.0013132474,0.020386126,0.00080507935,0.0002100182,0.022041947],"study_design_scores_gemma":[0.000001539117,0.000011632515,0.9983463,0.000004418158,0.0000039887177,0.00011073514,0.0003948012,0.00021491516,0.00018760469,0.00007546973,0.00064654805,0.0000020191105],"about_ca_topic_score_codex":0.009283262,"about_ca_topic_score_gemma":0.021228159,"teacher_disagreement_score":0.009283262,"about_ca_system_score_codex":0.00051997154,"about_ca_system_score_gemma":0.00028782935,"threshold_uncertainty_score":0.018458486},"labels":[],"label_agreement":null},{"id":"W4307545826","doi":"10.5194/se-13-1607-2022","title":"Shear zone evolution and the path of earthquake rupture","year":2022,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Mylonite; Geology; Shear zone; Seismology; Shear (geology); Cataclastic rock; Crust; Earthquake rupture; Fault (geology); Petrology; Tectonics; Geophysics","score_opus":0.009380362333644655,"score_gpt":0.20064227472747834,"score_spread":0.1912619123938337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307545826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987626,0.00007447514,0.00025792303,0.000016767031,0.0000010827308,0.0000017208404,0.00017355946,0.000009102003,0.00070283946],"genre_scores_gemma":[0.9996462,0.000024075434,0.00008599319,0.0000013397691,5.053938e-7,8.7715677e-7,0.000092808674,0.0000020790367,0.00014623861],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999956,0.000009161433,0.0000035801424,0.000014481172,0.000007425341,0.000009369822],"domain_scores_gemma":[0.99960274,0.000106908396,0.0001488932,0.00002096412,0.000067757996,0.000052641954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016118192,0.00009103631,0.00007511636,0.00089653727,0.0001472282,0.0006025422,0.00011507209,0.00017340007,0.0024405038],"category_scores_gemma":[0.001355019,0.00013486283,0.0000964281,0.0005112267,0.0002072166,0.00016885599,0.00019300418,0.00015815593,0.00034743786],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032110326,0.000024352545,0.9462215,0.00004813089,0.00007428506,0.00027908364,0.00047721688,0.008581323,0.027578752,0.0016190037,0.00025471926,0.014520617],"study_design_scores_gemma":[0.0000062263766,0.000029653662,0.9921171,0.000010333354,0.000008930798,0.00014270116,0.0001672789,0.0056893323,0.0008987389,0.00043461277,0.0004895564,0.000005596073],"about_ca_topic_score_codex":0.0033296533,"about_ca_topic_score_gemma":0.004133189,"teacher_disagreement_score":0.0033296533,"about_ca_system_score_codex":0.00027496513,"about_ca_system_score_gemma":0.00009507823,"threshold_uncertainty_score":0.008164346},"labels":[],"label_agreement":null},{"id":"W4307564328","doi":"10.1029/2022gl099995","title":"Small Magnitude Events Highlight the Correlation Between Hydraulic Fracturing Injection Parameters, Geological Factors, and Earthquake Occurrence","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Hydraulic fracturing; Geology; Seismology; Induced seismicity; Magnitude (astronomy); Structural basin; Maximum magnitude; Fault (geology); Earthquake prediction; Petroleum engineering; Paleontology","score_opus":0.06648559747517907,"score_gpt":0.2746445716022773,"score_spread":0.20815897412709822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307564328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997212,0.000023419241,0.00037463443,0.000019066381,0.0000010929514,0.0000066979037,0.0010520016,0.000018997212,0.0012920359],"genre_scores_gemma":[0.9990233,0.000010868255,0.00017718996,0.0000025714564,6.3799814e-7,0.0000016191591,0.0004886587,0.000001734899,0.00029343384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998698,0.00001751912,0.000013068515,0.00003177147,0.000033941724,0.000033741497],"domain_scores_gemma":[0.9988072,0.0003755296,0.0003364032,0.00009433599,0.0002724046,0.00011414351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016943821,0.0001436348,0.00012316581,0.0009756064,0.0003368057,0.0005342489,0.00014516574,0.00012379127,0.0020222082],"category_scores_gemma":[0.0018232855,0.0000656912,0.00007934926,0.001212712,0.00022323069,0.00017940786,0.00026070766,0.00016504247,0.00017445233],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002323562,0.0000075376834,0.99315006,0.0000048575926,0.0000121244175,0.000036537545,0.000079645964,0.0005332819,0.000923683,0.000037967893,0.00017074552,0.005020316],"study_design_scores_gemma":[3.6552217e-7,0.000003052024,0.9988483,0.0000011359166,0.000002498958,0.000012080513,0.000114217466,0.00074932084,0.000107145024,0.000013888484,0.00014680703,0.0000011176662],"about_ca_topic_score_codex":0.5034946,"about_ca_topic_score_gemma":0.8142572,"teacher_disagreement_score":0.5034946,"about_ca_system_score_codex":0.000779029,"about_ca_system_score_gemma":0.001013996,"threshold_uncertainty_score":0.9988588},"labels":[],"label_agreement":null},{"id":"W4307812068","doi":"10.1038/s41598-022-22791-z","title":"A reservoir induced earthquake swarm in the Central Highlands of Sri Lanka","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Faculty of Science, University of Melbourne; University of Peradeniya","keywords":"Seismology; Geology; Induced seismicity; Earthquake swarm; Seismic hazard; Remotely triggered earthquakes; Swarm behaviour","score_opus":0.026321678653815364,"score_gpt":0.2294902132324672,"score_spread":0.20316853457865186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307812068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968581,0.000053986616,0.0013548388,0.000029796562,0.0000038591456,0.000020896792,0.0006711487,0.00014748574,0.00085986214],"genre_scores_gemma":[0.99691594,0.000053832115,0.001991613,0.0000059326653,0.0000025876477,0.000012616258,0.0008862137,0.000005022801,0.0001262186],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999081,0.000013467626,0.00001200033,0.000026209682,0.000013802011,0.00002631412],"domain_scores_gemma":[0.9998989,0.000014563925,0.00003499486,0.000011884768,0.000020741521,0.000018896164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012206758,0.0002633523,0.00016759633,0.0004970332,0.00024507023,0.0004909954,0.0002723584,0.00017442422,0.0010200775],"category_scores_gemma":[0.00028300023,0.00014551957,0.00024941936,0.0010639897,0.00018555259,0.00022076248,0.000478737,0.00014136107,0.00019410078],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002990677,0.000107565735,0.8025461,0.00047999853,0.0003054985,0.002989716,0.002099975,0.013316384,0.087066576,0.0005222754,0.0017171588,0.08854972],"study_design_scores_gemma":[0.00002357646,0.00016550702,0.97314394,0.00002674969,0.00009259415,0.00087172457,0.0016284274,0.016666265,0.005012146,0.00015978889,0.0021740864,0.00003519824],"about_ca_topic_score_codex":0.021872863,"about_ca_topic_score_gemma":0.034855813,"teacher_disagreement_score":0.021872863,"about_ca_system_score_codex":0.00030064158,"about_ca_system_score_gemma":0.00052447437,"threshold_uncertainty_score":0.043491125},"labels":[],"label_agreement":null},{"id":"W4308015747","doi":"10.1190/tle41110748.1","title":"Implications of slow fault slip for hydraulic-fracturing-induced seismicity","year":2022,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Alberta Science Network; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Government of Canada","keywords":"Slip (aerodynamics); Geology; Seismology; Induced seismicity; Episodic tremor and slip; Seismic hazard; Interferometric synthetic aperture radar; Synthetic aperture radar; Tectonics; Remote sensing; Engineering","score_opus":0.042685327737973816,"score_gpt":0.26253132874269486,"score_spread":0.21984600100472104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308015747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99610424,0.00031566643,0.00085666974,0.00031193942,0.00002132575,0.000008700092,0.00024276243,0.000025908217,0.0021127167],"genre_scores_gemma":[0.99978894,0.0000560813,0.000043577846,0.000012988314,0.000008056057,8.946267e-7,0.000034009674,0.0000011130719,0.000054341504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998442,0.000038544553,0.00001546274,0.000022729037,0.000041066633,0.0000379031],"domain_scores_gemma":[0.9975539,0.0009858054,0.00084796513,0.00008987891,0.00027619884,0.0002461972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051365554,0.0002415055,0.00019279137,0.0007041486,0.00025038052,0.00053438335,0.0001808559,0.0003104092,0.0025809593],"category_scores_gemma":[0.0030173669,0.00007663666,0.00012950925,0.00046390516,0.0005379672,0.0003931389,0.00044608483,0.0002691341,0.00021277634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006431284,0.00015048555,0.91958237,0.00021128728,0.00006691181,0.0015118414,0.00023323933,0.01874988,0.031231774,0.0023939873,0.0007007434,0.024524344],"study_design_scores_gemma":[0.000023297953,0.00024193496,0.96368086,0.00003470213,0.00002235791,0.00045566593,0.00057782413,0.02536966,0.003954747,0.0049912035,0.0006314896,0.000016124082],"about_ca_topic_score_codex":0.0027393352,"about_ca_topic_score_gemma":0.0022505866,"teacher_disagreement_score":0.0027393352,"about_ca_system_score_codex":0.0004527904,"about_ca_system_score_gemma":0.00027723738,"threshold_uncertainty_score":0.00863421},"labels":[],"label_agreement":null},{"id":"W4308252005","doi":"10.1038/s43247-022-00586-4","title":"Microgravity effect of inter-seismic crustal dilatation","year":2022,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; North Pacific Marine Science Organization; Natural Resources Canada; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Science and ICT, South Korea; National Research Foundation of Korea","keywords":"Geology; Seismology; Gravimeter; Subduction; Crust; Episodic tremor and slip; Slip (aerodynamics); Compression (physics); Geodesy; Gravity anomaly; Geophysics; Tectonics; Paleontology","score_opus":0.01513793150129387,"score_gpt":0.2208803633640597,"score_spread":0.20574243186276583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308252005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982235,0.000064783395,0.000060769926,0.000016256741,0.000003821876,0.0000016020119,0.00026374377,0.000012879288,0.0013526113],"genre_scores_gemma":[0.9996037,0.000024245905,0.000020371257,0.0000064149926,0.0000016107515,8.45045e-7,0.000115695126,0.0000031750735,0.00022384644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992657,0.000008901747,0.000003879517,0.00002180761,0.000016520773,0.000022267584],"domain_scores_gemma":[0.9997763,0.00003921532,0.000052532178,0.00002875272,0.0000608308,0.000042435204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007382188,0.0001984633,0.00017001647,0.00035033707,0.00029763137,0.00042593898,0.00012566961,0.00012922134,0.0021464752],"category_scores_gemma":[0.00034167382,0.000107051485,0.00013911245,0.00035509196,0.00027817892,0.0001199833,0.00032042412,0.00012495065,0.00020083635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046200637,0.000048083115,0.9008736,0.00005315214,0.00022552905,0.0002758274,0.00044180668,0.003652435,0.07843945,0.00009861875,0.00063241564,0.01479699],"study_design_scores_gemma":[0.0000011124409,0.000012491031,0.9992079,0.0000011182018,0.0000052390947,0.000010872659,0.000053614876,0.00016808865,0.00040457203,0.000003904795,0.00012930066,0.0000017274394],"about_ca_topic_score_codex":0.082198024,"about_ca_topic_score_gemma":0.13510773,"teacher_disagreement_score":0.082198024,"about_ca_system_score_codex":0.00058738736,"about_ca_system_score_gemma":0.0003293784,"threshold_uncertainty_score":0.16343915},"labels":[],"label_agreement":null},{"id":"W4308562635","doi":"10.26443/seismica.v1i1.217","title":"Source Model and Characteristics of the 27 July 2022 MW 7.0 Northwestern Luzon Earthquake, Philippines","year":2022,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; European Commission","keywords":"Geology; Seismology; Sinistral and dextral; Slip (aerodynamics); Subduction; Geodesy; Kinematics; Shear (geology); Interferometric synthetic aperture radar; Focal mechanism; Fault (geology); Tectonics; Synthetic aperture radar; Petrology; Remote sensing","score_opus":0.011936038801155877,"score_gpt":0.18668762355927596,"score_spread":0.17475158475812008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308562635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95968187,0.00018393398,0.0056823916,0.00033692736,0.000025947124,0.0001304811,0.023855032,0.00091337063,0.009189953],"genre_scores_gemma":[0.98877865,0.000098203855,0.0011820938,0.000020201716,0.000016244212,0.000090176414,0.008146683,0.000058600224,0.0016090248],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99994767,0.000010128268,0.000003567931,0.000015207043,0.000011067094,0.000012345236],"domain_scores_gemma":[0.99980944,0.000028033057,0.000039719747,0.000018525821,0.00008216979,0.0000221987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000115872375,0.00063572964,0.00027086263,0.0008535156,0.0003354003,0.0003955565,0.0010775734,0.00053836266,0.0033333583],"category_scores_gemma":[0.00045511566,0.00024270237,0.00019587162,0.0011581001,0.00019577454,0.00030964604,0.0002465392,0.00029169637,0.00078417745],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024333237,0.0001780553,0.11574298,0.00019880636,0.00006894337,0.0013253378,0.00032735924,0.85251206,0.005928688,0.0020380926,0.0068301284,0.0146062095],"study_design_scores_gemma":[0.00011522384,0.000092139344,0.07053349,0.000029029121,0.000039703238,0.00022573615,0.00021620425,0.91987914,0.0016914775,0.0005650892,0.0065577137,0.00005511476],"about_ca_topic_score_codex":0.09936965,"about_ca_topic_score_gemma":0.06604585,"teacher_disagreement_score":0.09936965,"about_ca_system_score_codex":0.0012956829,"about_ca_system_score_gemma":0.00078637974,"threshold_uncertainty_score":0.19758248},"labels":[],"label_agreement":null},{"id":"W4308593435","doi":"10.1029/2022gl100276","title":"Depth‐Dependent Crustal Stress Rotation and Strength Variation in the Charlevoix Seismic Zone (CSZ), Québec, Canada","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Intraplate earthquake; Crust; Seismology; Induced seismicity; Tectonics; Clockwise; Cauchy stress tensor; Focal mechanism; Inversion (geology); Stress (linguistics); Geophysics; Geodesy; Rotation (mathematics); Geometry","score_opus":0.020651083827161597,"score_gpt":0.24596223423463545,"score_spread":0.22531115040747385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308593435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912401,0.00022389121,0.00018843214,0.00012910031,0.0000053403533,0.000014741617,0.0049714735,0.000035684192,0.0031913186],"genre_scores_gemma":[0.99603266,0.00008554028,0.00018550997,0.000024935647,0.0000017322525,0.000006341352,0.0021843673,0.0000067817714,0.001472087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997894,0.000014662078,0.000008344009,0.000048305214,0.00006332227,0.00007596825],"domain_scores_gemma":[0.9989477,0.00007402918,0.00012032187,0.000037673268,0.00063566735,0.00018469941],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002798535,0.00028607706,0.00020365462,0.0012628813,0.0009572652,0.00086153625,0.0005929193,0.00022545827,0.0023373454],"category_scores_gemma":[0.00086459506,0.00015406222,0.00015897494,0.0018256154,0.00053635053,0.00020537237,0.0003664947,0.00027385767,0.00023350112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016781302,0.00003863714,0.9717065,0.000038338945,0.00009819516,0.00011830983,0.00067102717,0.0028178259,0.004566082,0.00028550587,0.003386107,0.016105628],"study_design_scores_gemma":[0.0000056317463,0.000004513357,0.99762684,0.000007699455,0.000005946563,0.000009116623,0.00030396876,0.0010077449,0.0001552525,0.000009753734,0.0008578074,0.0000056991535],"about_ca_topic_score_codex":0.99618834,"about_ca_topic_score_gemma":0.9982344,"teacher_disagreement_score":0.017189795,"about_ca_system_score_codex":0.017189795,"about_ca_system_score_gemma":0.008953372,"threshold_uncertainty_score":0.12472129},"labels":[],"label_agreement":null},{"id":"W4308668132","doi":"10.1785/0220220208","title":"Revisiting Paleoearthquakes with Numerical Modeling: A Case Study of the 1679 Sanhe–Pinggu Earthquake","year":2022,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Slip (aerodynamics); Geology; Seismic gap; Earthquake scenario; Induced seismicity; Disaster area; Seismic hazard; Engineering","score_opus":0.09884613574758086,"score_gpt":0.308968007711756,"score_spread":0.21012187196417512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308668132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928718,0.00013836457,0.0051506823,0.00023660003,0.000016040158,0.00003129923,0.00010125441,0.00003223536,0.0014215747],"genre_scores_gemma":[0.9953803,0.00015546779,0.0039516347,0.00001422823,0.000009860129,0.000016642452,0.000092212606,0.000007048901,0.00037259233],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997584,0.00010457112,0.00002550277,0.000034689252,0.00004104753,0.000035816225],"domain_scores_gemma":[0.9993262,0.00039030277,0.00007712816,0.00007943347,0.00007741393,0.000049531784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079691067,0.00061192585,0.000496434,0.0009723989,0.00096075697,0.0011124208,0.0008420576,0.0014203537,0.0008365597],"category_scores_gemma":[0.0015481985,0.00042831764,0.00071002694,0.0010931315,0.00085426786,0.00086714525,0.0010191319,0.00077487325,0.00009301953],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011370422,0.00039118886,0.06590649,0.000115800955,0.00009594205,0.007907186,0.00094516523,0.90663904,0.0033504653,0.0031449234,0.0006712613,0.010718866],"study_design_scores_gemma":[0.00001267702,0.000040098133,0.0067753457,0.000012567851,0.000021559197,0.000105338775,0.00054994854,0.9911975,0.00046609517,0.00039482117,0.00040797054,0.000016025162],"about_ca_topic_score_codex":0.032005012,"about_ca_topic_score_gemma":0.037269372,"teacher_disagreement_score":0.032005012,"about_ca_system_score_codex":0.00085875497,"about_ca_system_score_gemma":0.00065139023,"threshold_uncertainty_score":0.063637435},"labels":[],"label_agreement":null},{"id":"W4308728881","doi":"10.21203/rs.3.rs-2136108/v1","title":"The December 2020 Magnitude (Mw) 6.4 Petrinja earthquake, Croatia: Seismological aspects, emergency response and impacts","year":2022,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Hrvatska Zaklada za Znanost","keywords":"Magnitude (astronomy); Emergency response; Seismology; Earthquake magnitude; Geology; Environmental science; Physics; Mathematics; Medical emergency; Medicine","score_opus":0.05419195355897485,"score_gpt":0.3440043380430445,"score_spread":0.28981238448406965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308728881","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7105304,0.0059234495,0.0034379368,0.012802773,0.0068802168,0.00014022007,0.12128832,0.00074238196,0.13825427],"genre_scores_gemma":[0.8638583,0.0019478048,0.0018194987,0.0004624422,0.0007151163,0.00003895318,0.06228751,0.00019481439,0.06867562],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99986255,0.000013509023,0.00000395414,0.000012467024,0.00005955415,0.00004790374],"domain_scores_gemma":[0.99973196,0.0000139046415,0.000031761396,0.000014429503,0.00016893375,0.00003904826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043390004,0.0003568116,0.00021377052,0.00065895205,0.00028939283,0.0008629527,0.00021582571,0.0006180209,0.009227269],"category_scores_gemma":[0.0008878646,0.0001375826,0.00013953757,0.0007708068,0.00009946845,0.00039323355,0.00039816147,0.00046622855,0.0031787555],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016470442,0.00031553008,0.15085508,0.00075827935,0.00016630518,0.0011752414,0.00042547096,0.01782033,0.0054336656,0.00922491,0.6277913,0.18438692],"study_design_scores_gemma":[0.0000697039,0.00014183893,0.74738824,0.00019030135,0.00007201503,0.0002794982,0.00060520653,0.007474594,0.002112173,0.0020097664,0.23962972,0.000026985557],"about_ca_topic_score_codex":0.036348987,"about_ca_topic_score_gemma":0.052284762,"teacher_disagreement_score":0.036348987,"about_ca_system_score_codex":0.0006462002,"about_ca_system_score_gemma":0.0010587863,"threshold_uncertainty_score":0.07227486},"labels":[],"label_agreement":null},{"id":"W4308853790","doi":"10.5772/intechopen.108195","title":"Locations of the 1982 Miramichi (Canada) Aftershocks: Implication of Two Rupture Regions Activated","year":2022,"lang":"en","type":"book-chapter","venue":"IntechOpen eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Seismology; Geology; Epicenter; Intraplate earthquake; Foreshock; Induced seismicity; Event (particle physics); Sequence (biology); Tectonics","score_opus":0.018625583406600796,"score_gpt":0.2178419315144726,"score_spread":0.1992163481078718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308853790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8580972,0.007333113,0.0016266088,0.00062309013,0.000041476225,0.000055904784,0.0015749831,0.00014702005,0.1305007],"genre_scores_gemma":[0.95905846,0.0047105183,0.0016788336,0.0000762266,0.000010216041,0.000009245511,0.0008716737,0.00001999996,0.033564854],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999635,0.000001316463,0.0000010242322,0.000006128433,0.00001426731,0.000013653631],"domain_scores_gemma":[0.99991536,0.000008376875,0.000020305404,0.0000039449283,0.000028922923,0.000023097728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000044613123,0.0001946039,0.00009677208,0.0006783976,0.0005801586,0.00092635216,0.000507919,0.00031616096,0.0021671052],"category_scores_gemma":[0.00021939981,0.0001386471,0.00008376504,0.0013273585,0.00037616494,0.0002959441,0.0003272993,0.00026688902,0.00031426206],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001264634,0.00015506866,0.2800726,0.0011899907,0.00009752611,0.015889108,0.012823685,0.015222691,0.0833864,0.033044014,0.024057262,0.5327971],"study_design_scores_gemma":[0.00002483308,0.00006885971,0.9346426,0.00012848698,0.000047507787,0.0013163331,0.0040319352,0.0019303216,0.008272703,0.0014210317,0.048070867,0.00004459476],"about_ca_topic_score_codex":0.65570486,"about_ca_topic_score_gemma":0.8751033,"teacher_disagreement_score":0.34429514,"about_ca_system_score_codex":0.0042837677,"about_ca_system_score_gemma":0.002562284,"threshold_uncertainty_score":0.69264555},"labels":[],"label_agreement":null},{"id":"W4309121723","doi":"10.1061/9780784484449.036","title":"Applying Consequence-Driven Scenario Selection to Lifelines","year":2022,"lang":"en","type":"article","venue":"Lifelines 2022","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Vulnerability (computing); Stakeholder; Metric (unit); Critical infrastructure; Risk analysis (engineering); Computer science; Population; Seismic hazard; Hazard; Seismic risk; Vulnerability assessment; Event (particle physics); Engineering; Computer security; Business; Civil engineering; Psychological resilience; Operations management","score_opus":0.02518727468232497,"score_gpt":0.23936852522741373,"score_spread":0.21418125054508874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309121723","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.005008164,0.00015869699,0.9852313,0.00061103515,0.00005069098,0.00032782552,0.0004348445,0.00044707593,0.007730417],"genre_scores_gemma":[0.24747758,0.0003747814,0.74626553,0.0003457106,0.00011840723,0.0006594986,0.0013752842,0.0002789038,0.003104365],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99291116,0.0036527538,0.0003822958,0.0010402413,0.0016136006,0.0003998349],"domain_scores_gemma":[0.9844209,0.010564633,0.0011596158,0.0014977513,0.0017530487,0.0006039626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.007627502,0.0016702532,0.00088452426,0.0032903827,0.001162075,0.0039511523,0.0031737343,0.0016140592,0.009317629],"category_scores_gemma":[0.026753832,0.00084005564,0.0025601755,0.0023330452,0.0028055536,0.0045407005,0.0045534135,0.0031132794,0.00091201445],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012246796,0.00015381094,0.0045520137,0.0003068599,0.00018389388,0.000991155,0.00072799827,0.59687835,0.0010059918,0.3179403,0.004563872,0.07257333],"study_design_scores_gemma":[0.00003957142,0.000063693114,0.00046236577,0.000081360304,0.000047463793,0.00021505717,0.00022749943,0.7161457,0.0007601289,0.26695842,0.014956587,0.000042123396],"about_ca_topic_score_codex":0.009565085,"about_ca_topic_score_gemma":0.012540532,"teacher_disagreement_score":0.009565085,"about_ca_system_score_codex":0.0029728736,"about_ca_system_score_gemma":0.0032908202,"threshold_uncertainty_score":0.040338576},"labels":[],"label_agreement":null},{"id":"W4309288284","doi":"10.1785/0220220264","title":"Earthquake Delay and Rupture Velocity in Near-Field Dynamic Triggering Dictated by Stress-Controlled Nucleation","year":2022,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Seismology; Nucleation; Geology; Shear (geology); Rayleigh wave; Earthquake rupture; Stress field; Phase (matter); Wave velocity; Stress (linguistics); Seismic wave; Fault (geology); Wave propagation; Physics; Petrology; Structural engineering; Engineering; Optics","score_opus":0.02291889574492112,"score_gpt":0.2761905230251311,"score_spread":0.25327162728020997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309288284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991184,0.00005339959,0.0004859409,0.0000042629954,0.0000012953195,0.0000019034337,0.000020754842,0.00000802587,0.00030597893],"genre_scores_gemma":[0.9998975,0.000010825081,0.000037548038,5.8405703e-7,7.0723354e-7,7.818588e-7,0.000013122454,7.969299e-7,0.000038165927],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995375,0.000005366459,0.0000028941208,0.000017085635,0.000008056048,0.000012843521],"domain_scores_gemma":[0.99952555,0.00014438092,0.00015781166,0.00003737334,0.000041658783,0.000093228045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013295139,0.00009119219,0.00015258738,0.0003037989,0.000093098686,0.00031342515,0.00014989999,0.00014640014,0.001057559],"category_scores_gemma":[0.00077870314,0.00010352595,0.000044244644,0.000114634124,0.00018836484,0.00023961764,0.00021551253,0.0001558869,0.00012419315],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00084300333,0.00015176722,0.07445232,0.000068106434,0.000032393484,0.00034891753,0.00019049222,0.007541842,0.90259093,0.0016684631,0.00012346864,0.011988242],"study_design_scores_gemma":[0.00004720202,0.0014127423,0.724438,0.000021184082,0.000041008923,0.00083167583,0.00037789982,0.06019866,0.2102633,0.0015188418,0.000805268,0.000044138284],"about_ca_topic_score_codex":0.00042671623,"about_ca_topic_score_gemma":0.0003836669,"teacher_disagreement_score":0.001057559,"about_ca_system_score_codex":0.00022601419,"about_ca_system_score_gemma":0.00006829647,"threshold_uncertainty_score":0.0035378933},"labels":[],"label_agreement":null},{"id":"W4309624730","doi":"10.1029/2022jb024748","title":"Crustal Seismic Anisotropy Along the Continental Margin in Western Canada From Receiver Function Analysis","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Calgary; University of Ottawa","funders":"","keywords":"Geology; Terrane; Seismology; Receiver function; Subduction; North American Plate; Tectonics; Crust; Lithosphere; Plate tectonics; Continental margin; Oceanic crust; Seismic hazard; Convergent boundary; Geophysics","score_opus":0.024006005920878027,"score_gpt":0.26983054460417544,"score_spread":0.2458245386832974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309624730","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952813,0.00019141615,0.00029859104,0.00004308439,0.0000032886478,0.000006452876,0.0019566321,0.000037863025,0.0021813007],"genre_scores_gemma":[0.9968265,0.0001351826,0.00037021493,0.000009232383,0.0000016446363,0.0000025849763,0.0015657981,0.000008245617,0.0010806212],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998721,0.000004890969,0.0000047337853,0.000019920824,0.000050443126,0.00004785986],"domain_scores_gemma":[0.99957126,0.000021849479,0.000033520926,0.000012584081,0.0003064091,0.00005446559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013877024,0.00043236124,0.00019832862,0.0016069838,0.00089893874,0.0008343752,0.00036111622,0.00017154013,0.0015723918],"category_scores_gemma":[0.0004452282,0.00017613209,0.00016193476,0.0028428556,0.00024794295,0.00014279112,0.00033659048,0.00019322716,0.00030857595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016714212,0.000041319316,0.92643136,0.000050097224,0.00009098962,0.00046132933,0.0011668373,0.0060148444,0.017492557,0.00034634813,0.0022686669,0.045468617],"study_design_scores_gemma":[0.000004083777,0.0000051829984,0.9927946,0.000015297795,0.00002093339,0.00004369006,0.0006622821,0.004410181,0.00073506526,0.000029668025,0.0012687562,0.000010300666],"about_ca_topic_score_codex":0.98823535,"about_ca_topic_score_gemma":0.9935894,"teacher_disagreement_score":0.011764646,"about_ca_system_score_codex":0.0058599585,"about_ca_system_score_gemma":0.0073255757,"threshold_uncertainty_score":0.042517185},"labels":[],"label_agreement":null},{"id":"W4309761239","doi":"10.1029/2022jb023989","title":"Using Seafloor Geodesy to Detect Vertical Deformation at the Hikurangi Subduction Zone: Insights From Self‐Calibrating Pressure Sensors and Ocean General Circulation Models","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Directorate for Geosciences; Ministry for Business Innovation and Employment; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Seafloor spreading; Geology; Subduction; Submarine pipeline; Seismology; Slip (aerodynamics); Trench; Geodesy; Tectonics; Oceanography","score_opus":0.04956741121461599,"score_gpt":0.2916262080576809,"score_spread":0.24205879684306492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309761239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974873,0.00005574054,0.0019058656,0.00004433538,0.000005062074,0.0000040739387,0.0001060421,0.0000220044,0.00036939897],"genre_scores_gemma":[0.9985228,0.00004296403,0.0012122787,0.0000066953903,0.000002317341,0.0000018182392,0.00011067404,0.0000042384404,0.000096346484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991226,0.000017667464,0.0000062396357,0.000030679163,0.000016106873,0.00001710072],"domain_scores_gemma":[0.99982315,0.00004630183,0.00004564659,0.000021484066,0.000041946907,0.000021535041],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003281538,0.00037259722,0.00018011782,0.0005417562,0.00016936909,0.00058774464,0.00023634911,0.0002660004,0.0003888662],"category_scores_gemma":[0.0009330768,0.00019778495,0.0003207065,0.0005279158,0.0002588481,0.00052338344,0.00033699023,0.00021817423,0.000092636954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009918576,0.00007108016,0.914751,0.000036590187,0.00013439723,0.00028009666,0.00026149442,0.038851902,0.019665329,0.00030146772,0.00024109945,0.025306422],"study_design_scores_gemma":[0.000009137557,0.00004325076,0.7967189,0.000010900093,0.00003618754,0.000043284264,0.00019600466,0.20115736,0.001390422,0.0001235309,0.00025154848,0.000019385725],"about_ca_topic_score_codex":0.037550386,"about_ca_topic_score_gemma":0.048754662,"teacher_disagreement_score":0.037550386,"about_ca_system_score_codex":0.00031131046,"about_ca_system_score_gemma":0.00032317144,"threshold_uncertainty_score":0.07466364},"labels":[],"label_agreement":null},{"id":"W4309921706","doi":"10.1088/1755-1315/1103/1/012041","title":"Nowcasting Earthquake Occurrence in Sabah","year":2022,"lang":"en","type":"article","venue":"IOP Conference Series Earth and Environmental Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nowcasting; Geology; Seismology; Magnitude (astronomy); Hazard; Geography; Quarter (Canadian coin); Meteorology; Archaeology","score_opus":0.01953933048520749,"score_gpt":0.20019239364920544,"score_spread":0.18065306316399796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309921706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914636,0.0001569722,0.0029748485,0.00012420483,0.00006404416,0.000012780997,0.0026945644,0.00009878119,0.0024102193],"genre_scores_gemma":[0.9956524,0.000095396106,0.0013320396,0.000007108588,0.00002050604,0.000005740001,0.0024372877,0.000008599128,0.00044110144],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997701,0.000054988523,0.000026778804,0.00005998834,0.000056445264,0.00003166878],"domain_scores_gemma":[0.998965,0.00027827546,0.00023270905,0.00015308676,0.0003015298,0.000069422196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045855978,0.00013408142,0.0001571059,0.0015027255,0.00014237007,0.0004951042,0.00021359307,0.0001634739,0.0010667244],"category_scores_gemma":[0.0027874918,0.00007954828,0.00017984664,0.0012915756,0.00017732565,0.0004537438,0.0004274955,0.00031526556,0.00019866854],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038015583,0.000059911974,0.87774134,0.00013867005,0.00008785116,0.00032302088,0.0013578978,0.013401996,0.005457058,0.0010550995,0.0024861197,0.09751093],"study_design_scores_gemma":[0.000010043164,0.00009212017,0.9612423,0.00004331484,0.00003876694,0.00014809855,0.0016819376,0.028747736,0.0021526727,0.00047852183,0.005342771,0.000021598999],"about_ca_topic_score_codex":0.018849159,"about_ca_topic_score_gemma":0.023574106,"teacher_disagreement_score":0.018849159,"about_ca_system_score_codex":0.00032571022,"about_ca_system_score_gemma":0.00035608505,"threshold_uncertainty_score":0.037478924},"labels":[],"label_agreement":null},{"id":"W4310058910","doi":"10.1029/2022tc007490","title":"Direct Evidence for Dextral Shearing in the Shanxi Graben System: Geologic and Geomorphologic Constraints From the North Liulengshan Fault","year":2022,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Toronto","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Sinistral and dextral; Geology; Graben; Strike-slip tectonics; Seismology; Transtension; Tectonics; Fault scarp; Fault (geology); Rift; Active fault; Echelon formation; Shear zone; Paleontology","score_opus":0.06827058818335506,"score_gpt":0.2505275823401181,"score_spread":0.18225699415676305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310058910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941874,0.000039180588,0.0000636264,0.000010482694,9.891767e-7,0.0000021662177,0.000059726175,0.0000026204862,0.00040261666],"genre_scores_gemma":[0.99964046,0.00003072492,0.00010754173,0.0000058094715,0.0000018928419,0.0000024732863,0.00011005128,6.3913853e-7,0.00010031508],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998746,0.000014220021,0.000014087833,0.000037472375,0.000040701918,0.000019048355],"domain_scores_gemma":[0.9996407,0.00003788422,0.0001500678,0.00002626547,0.00008054798,0.00006460723],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023895326,0.00019824714,0.00019193813,0.0016129307,0.00039996504,0.00033156332,0.00021642371,0.00021610328,0.000934906],"category_scores_gemma":[0.00033697562,0.00016508371,0.00012342283,0.0013848909,0.00066865166,0.0001997575,0.00043613478,0.00014265082,0.000119623204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061734616,0.000023127135,0.9637632,0.000042469295,0.000017399023,0.0003122491,0.00082069205,0.00033599406,0.027192036,0.00016470635,0.00007397888,0.0071924073],"study_design_scores_gemma":[0.0000027908363,0.000016673072,0.998904,0.0000030185374,0.000004112271,0.00005300713,0.00017622898,0.00037297164,0.0003173759,0.000025787827,0.00012204418,0.00000202099],"about_ca_topic_score_codex":0.026535964,"about_ca_topic_score_gemma":0.06588794,"teacher_disagreement_score":0.026535964,"about_ca_system_score_codex":0.0004452541,"about_ca_system_score_gemma":0.000549841,"threshold_uncertainty_score":0.052762985},"labels":[],"label_agreement":null},{"id":"W4310061856","doi":"10.1029/2022jb024612","title":"Fault Slip Behaviors Modulated by Locally Increased Fluid Pressure: Earthquake Nucleation and Slow Slip Events","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Slip (aerodynamics); Episodic tremor and slip; Seismology; Geology; Seismic gap; Remotely triggered earthquakes; Nucleation; Fault (geology); Engineering; Subduction; Tectonics; Physics","score_opus":0.021566967466016603,"score_gpt":0.28434478516103606,"score_spread":0.26277781769501946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310061856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99248296,0.00015583212,0.004511339,0.00009030033,0.00002896808,0.000021890331,0.00020992775,0.00008366115,0.002415082],"genre_scores_gemma":[0.99915826,0.000052110026,0.00056730944,0.000010217288,0.0000038131038,0.000010086587,0.00006623963,0.000009402541,0.00012256287],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999156,0.000015568387,0.0000068759396,0.000015972775,0.000014945065,0.000031004452],"domain_scores_gemma":[0.9996208,0.00013128854,0.00011495187,0.000030467987,0.000042071213,0.0000603261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018942513,0.00035778322,0.0004583035,0.0004163891,0.0004171336,0.00055662496,0.0004764142,0.0005880037,0.0019117822],"category_scores_gemma":[0.0011384994,0.00027284518,0.0005127765,0.00031935517,0.00062891375,0.0005013384,0.00047094782,0.00047212618,0.00011131121],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019846999,0.00023725582,0.054149956,0.00022495023,0.00015410788,0.000616547,0.00016472659,0.9079838,0.02700303,0.005046668,0.0006925107,0.00352794],"study_design_scores_gemma":[0.000035062396,0.000062382445,0.008966871,0.00000856025,0.00002533601,0.00003417347,0.000051684572,0.9880751,0.0017229621,0.0007816043,0.00022032647,0.000016026503],"about_ca_topic_score_codex":0.0064389626,"about_ca_topic_score_gemma":0.0030704048,"teacher_disagreement_score":0.0064389626,"about_ca_system_score_codex":0.00037462325,"about_ca_system_score_gemma":0.00053020474,"threshold_uncertainty_score":0.0128029585},"labels":[],"label_agreement":null},{"id":"W4310839414","doi":"10.21203/rs.3.rs-2096959/v1","title":"Do fault systems impede fluvial incision in active orogens?","year":2022,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Natural Science Foundation of China; University of Melbourne; Australian Government","keywords":"Fluvial; Geology; Fault (geology); Geomorphology; Paleontology","score_opus":0.08384059412558391,"score_gpt":0.3738144843293068,"score_spread":0.2899738902037229,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310839414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983032,0.00009321025,0.00010817136,0.000118487216,0.0000029216299,0.0000018005081,0.00005545509,0.0000023341074,0.0013143392],"genre_scores_gemma":[0.99971014,0.00007416457,0.00003301775,0.000013129133,0.0000037669226,8.7827095e-7,0.000024322577,0.0000013858421,0.00013917134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99965227,0.000073884825,0.000022800827,0.000048222875,0.000030113542,0.00017266313],"domain_scores_gemma":[0.99428153,0.0029292346,0.0016739964,0.000326545,0.00034671475,0.00044205095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010037548,0.00019935051,0.00033048433,0.0005003673,0.0004076168,0.0017162153,0.0003974447,0.00078535307,0.007315299],"category_scores_gemma":[0.009001808,0.00026228433,0.00025147697,0.00082464237,0.0012846268,0.0021008253,0.0007139698,0.00036968567,0.0005718831],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004998443,0.0000753033,0.9841055,0.00008681685,0.00007019428,0.0001735419,0.00071576174,0.0010282032,0.0028472543,0.0021165283,0.00013330318,0.008147821],"study_design_scores_gemma":[0.0000117180425,0.000070566944,0.9949078,0.000017462145,0.00004245922,0.00007569348,0.0021517638,0.00073693553,0.00029833612,0.0012616231,0.00042053484,0.00000499996],"about_ca_topic_score_codex":0.008148364,"about_ca_topic_score_gemma":0.013087878,"teacher_disagreement_score":0.008148364,"about_ca_system_score_codex":0.00035142386,"about_ca_system_score_gemma":0.0005566271,"threshold_uncertainty_score":0.024472117},"labels":[],"label_agreement":null},{"id":"W4310965511","doi":"10.1038/s41598-022-25239-6","title":"Interdependent effects of fluid injection parameters on triggered aseismic slip and seismicity","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Standards Association; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Government of Ontario","keywords":"Induced seismicity; Slip (aerodynamics); Geology; Seismology; Physics; Thermodynamics","score_opus":0.010545751784372656,"score_gpt":0.20288158401605494,"score_spread":0.19233583223168227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310965511","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951567,0.00018422007,0.0030383458,0.00005122607,0.000014936895,0.00001726057,0.00016427116,0.00008473561,0.0012883442],"genre_scores_gemma":[0.9995165,0.000052289935,0.0002788205,0.000005934701,0.0000012425617,0.000004958127,0.0000441715,0.000008580006,0.0000875867],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998386,0.000032994572,0.000021027561,0.00003062946,0.00003058118,0.00004610215],"domain_scores_gemma":[0.9989347,0.0006381196,0.00019955715,0.000057239606,0.00008486284,0.000085491316],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034384322,0.0004300421,0.00038044032,0.0005843232,0.00018870746,0.0008853513,0.0003723586,0.0005487755,0.0011697509],"category_scores_gemma":[0.0024966185,0.00020911625,0.0003819828,0.00028754055,0.00060966046,0.000542551,0.00043774358,0.00054600264,0.00011774729],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00085892016,0.00047531456,0.08934055,0.00036657273,0.00019061021,0.0008465592,0.00021765794,0.7264305,0.16609919,0.0015972386,0.0003822348,0.0131946625],"study_design_scores_gemma":[0.000054272798,0.0006646533,0.06841234,0.0000480209,0.00014118974,0.00016538486,0.00031257974,0.86384153,0.064670384,0.00083385047,0.00077532337,0.00008044311],"about_ca_topic_score_codex":0.0027570114,"about_ca_topic_score_gemma":0.0018178532,"teacher_disagreement_score":0.0027570114,"about_ca_system_score_codex":0.00042300398,"about_ca_system_score_gemma":0.00035143943,"threshold_uncertainty_score":0.0054819584},"labels":[],"label_agreement":null},{"id":"W4310966806","doi":"10.1130/b36500.1","title":"Modern dextral strain controls active hydrothermal systems in the southeastern Canadian Cordillera","year":2022,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Victoria; University of Alberta","funders":"","keywords":"Geology; Sinistral and dextral; Seismology; Geothermal gradient; Induced seismicity; Fault (geology); Trench; Stress field; Active fault; Strike-slip tectonics; Geomorphology; Paleontology","score_opus":0.015568982692676819,"score_gpt":0.19708793819284603,"score_spread":0.18151895550016922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4310966806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977036,0.00020030761,0.00008098873,0.000054302942,0.0000018795188,0.0000050594012,0.00023588279,0.000013476847,0.0017044628],"genre_scores_gemma":[0.9991829,0.00011678688,0.000116279334,0.000009752024,0.0000011724017,0.0000029649104,0.00014301033,0.000002565456,0.00042453498],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998348,0.000008617004,0.000007295143,0.000051187082,0.000046646343,0.000051487787],"domain_scores_gemma":[0.99974126,0.000013816538,0.000059923485,0.0000090881695,0.00012082824,0.000055024342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012592944,0.00024131815,0.00016989622,0.001141987,0.0011745217,0.0007656731,0.00043252573,0.00017811178,0.0014345461],"category_scores_gemma":[0.0006471737,0.00012008792,0.000095555224,0.0010918223,0.0007792023,0.00019278072,0.0004289193,0.00014867465,0.00010867854],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001893023,0.000035642228,0.9121697,0.00006593599,0.00005127075,0.0002310999,0.0021917983,0.0025268064,0.033632584,0.0011052325,0.00071999314,0.047080733],"study_design_scores_gemma":[0.000002293006,0.0000059183076,0.99871945,0.0000039670067,0.0000034308669,0.000015368792,0.00023482229,0.0003405637,0.00022028231,0.000039526203,0.00041076244,0.0000037080422],"about_ca_topic_score_codex":0.9456044,"about_ca_topic_score_gemma":0.98334694,"teacher_disagreement_score":0.054395616,"about_ca_system_score_codex":0.010920519,"about_ca_system_score_gemma":0.0041653616,"threshold_uncertainty_score":0.10943186},"labels":[],"label_agreement":null},{"id":"W4311029801","doi":"10.1093/gji/ggac473","title":"The 2015–2017 Pamir earthquake sequence: foreshocks, main shocks and aftershocks, seismotectonics, fault interaction and fluid processes","year":2022,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Aftershock; Geology; Seismology; Foreshock; Induced seismicity; Seismotectonics; Tectonics; Slip (aerodynamics); Shock (circulatory); Seismic gap; Fault (geology)","score_opus":0.01929798033979771,"score_gpt":0.2595130283552167,"score_spread":0.240215048015419,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311029801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960317,0.00032727083,0.00048488032,0.00008212986,0.0000149964235,0.00001022635,0.0008367745,0.000045834557,0.002166264],"genre_scores_gemma":[0.99834645,0.00013835494,0.00029580417,0.0000116608735,0.000018179639,0.000005699121,0.0008816699,0.0000040283844,0.00029808725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999218,0.000006826339,0.0000076218994,0.00001929528,0.000023179522,0.000021325282],"domain_scores_gemma":[0.9998447,0.000014727987,0.00007061118,0.000012667062,0.000034336437,0.000023030154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001456177,0.00023793068,0.00014558203,0.0007896952,0.00021697723,0.000360202,0.00018059157,0.00013066559,0.0012723507],"category_scores_gemma":[0.0003490259,0.000080290876,0.00014287177,0.0007655975,0.0002006262,0.00029103356,0.00044270055,0.00019109302,0.00023121727],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026611314,0.000058727474,0.8848046,0.00038741025,0.0001466237,0.0016003407,0.0017489857,0.006019841,0.034728024,0.0017002767,0.0026447533,0.06589424],"study_design_scores_gemma":[0.0000036698864,0.000040139243,0.99149674,0.0000228782,0.000019356166,0.0002195328,0.0004249,0.003148047,0.0012922054,0.0003158991,0.0030045907,0.000012052227],"about_ca_topic_score_codex":0.005877518,"about_ca_topic_score_gemma":0.0074785636,"teacher_disagreement_score":0.005877518,"about_ca_system_score_codex":0.00020845195,"about_ca_system_score_gemma":0.00036147458,"threshold_uncertainty_score":0.011686623},"labels":[],"label_agreement":null},{"id":"W4311107789","doi":"10.22541/essoar.167079464.41555160/v1","title":"Seismic velocity structure of the easternmost segment of the Gofar transform fault, East Pacific Rise","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Transform fault; Crust; Seismometer; Induced seismicity; Seismic zone; Slipping; Fault (geology); Geophysics; Geometry","score_opus":0.014538950360028946,"score_gpt":0.2045594823410017,"score_spread":0.19002053198097277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311107789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99812156,0.000028872028,0.00011659698,0.000028554767,0.0000020093346,0.000005327816,0.00084609183,0.000030619343,0.0008202586],"genre_scores_gemma":[0.9974915,0.00004540531,0.0003248713,0.000006850667,0.0000033914878,0.000004615622,0.0017869603,0.000009189018,0.00032714495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999434,0.0000031501522,0.0000034156053,0.000022771517,0.000012659086,0.000014612167],"domain_scores_gemma":[0.9998783,0.000012256014,0.00003506239,0.000009828469,0.000029488796,0.00003513187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008706046,0.00037948255,0.0001958705,0.0012592768,0.0003630226,0.00047092585,0.0002604905,0.0003926578,0.0014235291],"category_scores_gemma":[0.00036675035,0.00020423585,0.00018355042,0.001246983,0.0003112259,0.0002767082,0.00032793896,0.00031123596,0.0002762061],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015870982,0.00017942174,0.93985677,0.00005950841,0.000066190514,0.0004137511,0.0010468282,0.012092496,0.019747766,0.00036544952,0.0013330536,0.02468011],"study_design_scores_gemma":[0.000004216336,0.000016439926,0.99384683,0.0000035794908,0.0000068475297,0.000031739564,0.0001061034,0.005446199,0.00025610247,0.000024671155,0.00025074912,0.000006460312],"about_ca_topic_score_codex":0.113124296,"about_ca_topic_score_gemma":0.1325099,"teacher_disagreement_score":0.113124296,"about_ca_system_score_codex":0.00051190867,"about_ca_system_score_gemma":0.00052587397,"threshold_uncertainty_score":0.22493172},"labels":[],"label_agreement":null},{"id":"W4311187301","doi":"10.23860/diss-he-bing-2022","title":"DETECTING SLOW SLIP EVENTS FROM SEAFLOOR PRESSURE DATA USING MACHINE LEARNING","year":2022,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seafloor spreading; Geology; Seismology; Submarine pipeline; Subduction; Slip (aerodynamics); Trench; Geodetic datum; Episodic tremor and slip; Geodesy; Tectonics; Geophysics; Geotechnical engineering; Engineering","score_opus":0.04421164607824465,"score_gpt":0.2735944091391352,"score_spread":0.22938276306089053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311187301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.873949,0.0003837429,0.12127572,0.00022734494,0.0001192393,0.00007189373,0.00050521916,0.0018528452,0.001614961],"genre_scores_gemma":[0.9712903,0.00006437369,0.027125908,0.00003356042,0.00002484195,0.00002622772,0.00081959914,0.000016919199,0.00059823215],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996301,0.00005076159,0.000040066294,0.000114648356,0.00010199594,0.00006246784],"domain_scores_gemma":[0.9986217,0.0006216992,0.0001974092,0.00009417341,0.00036757716,0.000097495555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006887154,0.00073800224,0.00046792557,0.0015074866,0.00024304114,0.0005423821,0.0005201252,0.0006124297,0.00043390272],"category_scores_gemma":[0.0025733195,0.00019090361,0.00038601665,0.00064906874,0.00023457108,0.00059115223,0.00037594215,0.0005697053,0.00031098325],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029964486,0.0007390694,0.09112058,0.00011004254,0.00017103594,0.0007651685,0.00013123275,0.42592704,0.032144077,0.0004959956,0.0028492033,0.44524693],"study_design_scores_gemma":[0.0000035770356,0.00004464058,0.009256371,0.000003839283,0.0000050843323,0.000030173313,0.000021891821,0.98586583,0.0043546287,0.0001570791,0.00024824304,0.000008648492],"about_ca_topic_score_codex":0.0050296783,"about_ca_topic_score_gemma":0.003845584,"teacher_disagreement_score":0.0050296783,"about_ca_system_score_codex":0.00039948188,"about_ca_system_score_gemma":0.0004322405,"threshold_uncertainty_score":0.010000825},"labels":[],"label_agreement":null},{"id":"W4311510520","doi":"10.31905/8ipr1pjd","title":"The Seismic Record Supplement to “Hosgri Fault Transpressional Slip Rates Reproduce Observed Central California Coast Uplift Rates”","year":2022,"lang":"en","type":"dataset","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"BGC Engineering (Canada)","funders":"","keywords":"Geology; Seismology; Fault (geology); Slip (aerodynamics); Engineering","score_opus":0.03243159417095206,"score_gpt":0.2538383546011513,"score_spread":0.22140676043019922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311510520","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0001579197,0.0000066913426,0.000018573526,0.000015781423,0.00001235938,0.0000052145933,0.9994154,0.000051624134,0.0003164259],"genre_scores_gemma":[0.00036337358,0.000015626947,0.00008558407,0.0000123864065,0.000006052771,0.00003826009,0.998288,0.000023106893,0.0011676827],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99921775,0.00005545351,0.000111318965,0.0001765293,0.00024050492,0.00019841478],"domain_scores_gemma":[0.9954886,0.00040736797,0.00074202544,0.00080691214,0.002134253,0.00042082366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090897584,0.0020772822,0.0011957632,0.0055825505,0.0008934163,0.0022300156,0.0019917465,0.0014996214,0.08396618],"category_scores_gemma":[0.004342539,0.00141222,0.0008897718,0.0090942625,0.000320609,0.0011595009,0.0014112688,0.0014498498,0.08671746],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056509223,0.00002734529,0.002394558,0.00024962373,0.00003227398,0.00001763569,0.000023124378,0.00032639707,0.000084700485,0.00019851413,0.99455357,0.0020357566],"study_design_scores_gemma":[0.00034937897,0.000030420979,0.042843595,0.00023403754,0.000058634505,0.000050332044,0.00013895215,0.0006141668,0.00046740545,0.00033234726,0.9548395,0.00004123887],"about_ca_topic_score_codex":0.1852717,"about_ca_topic_score_gemma":0.24103194,"teacher_disagreement_score":0.8147283,"about_ca_system_score_codex":0.0015032098,"about_ca_system_score_gemma":0.004950367,"threshold_uncertainty_score":0.36838657},"labels":[],"label_agreement":null},{"id":"W4311588723","doi":"10.1038/s41598-022-23998-w","title":"Shallow magmatic intrusion evolution below La Palma before and during the 2021 eruption","year":2022,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Agencia Estatal de Investigación","keywords":"Unrest; Volcano; Geology; Seismology; Interferometric synthetic aperture radar; Intrusion; Magma; Population; Synthetic aperture radar; Geochemistry; Remote sensing","score_opus":0.006455027086613933,"score_gpt":0.19487227371755106,"score_spread":0.18841724663093712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311588723","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99715805,0.00006447603,0.0003608535,0.00005240225,0.000002976157,0.0000040449804,0.0003287768,0.000086839056,0.0019415156],"genre_scores_gemma":[0.99912506,0.000031709893,0.00025992995,0.0000033645745,0.000001996831,0.0000021738788,0.00020656297,0.000008626924,0.00036054663],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999511,0.000003918208,0.0000018381285,0.000018579547,0.0000075520607,0.000017088962],"domain_scores_gemma":[0.9999094,0.000016881773,0.000029165054,0.000011844962,0.00001646043,0.00001623498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007252777,0.0002489537,0.00017243257,0.00039530377,0.0003317625,0.0007847441,0.0003022608,0.00041110185,0.0012757113],"category_scores_gemma":[0.00038236534,0.00013254948,0.00023286506,0.00044769765,0.00019650614,0.00034988244,0.00031917528,0.00021801038,0.00022692521],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063360855,0.00025719372,0.85398203,0.00012928566,0.00016815588,0.00146636,0.0009427181,0.046926275,0.0494763,0.0008549382,0.00082870875,0.044334576],"study_design_scores_gemma":[0.000020908792,0.000042830314,0.9351622,0.000011362192,0.00006180866,0.00023115284,0.00043904147,0.057795115,0.0043814136,0.00022896648,0.0016036604,0.000021645172],"about_ca_topic_score_codex":0.038100824,"about_ca_topic_score_gemma":0.035881568,"teacher_disagreement_score":0.038100824,"about_ca_system_score_codex":0.0006991439,"about_ca_system_score_gemma":0.00032485585,"threshold_uncertainty_score":0.07575816},"labels":[],"label_agreement":null},{"id":"W4311816500","doi":"10.1029/2022jb024113","title":"Geometric Control on Seismic Rupture and Earthquake Sequence Along the Yingxiu‐Beichuan Fault With Implications for the 2008 Wenchuan Earthquake","year":2022,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; McGill University","funders":"National Key Research and Development Program of China","keywords":"Seismology; Geology; Slip (aerodynamics); Earthquake rupture; Strike-slip tectonics; Fault (geology); Magnetic dip; Surface rupture; Tectonics; Geodesy; Engineering; Geophysics","score_opus":0.05285330245016274,"score_gpt":0.31852828033026065,"score_spread":0.2656749778800979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311816500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981481,0.00003681041,0.0011478739,0.000046089033,0.000004893365,0.0000038984517,0.000035819114,0.000015786245,0.0005608516],"genre_scores_gemma":[0.99977857,0.00001765685,0.00009758699,0.0000032243058,0.0000015657721,0.0000015314204,0.000020228103,0.0000026928114,0.000076847],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989045,0.000021294434,0.0000063115804,0.000040032795,0.000013813869,0.00002805983],"domain_scores_gemma":[0.999729,0.000055747496,0.00010421571,0.00003223674,0.000032861364,0.000046022946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020871747,0.00037324708,0.00040222594,0.0005082347,0.00033950014,0.0005981264,0.00039217767,0.00047676804,0.0011071512],"category_scores_gemma":[0.0009150068,0.00032429886,0.00038550587,0.00037587713,0.00059129595,0.00039579565,0.00050969236,0.00023176154,0.00008736493],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019307197,0.00014430749,0.10906552,0.00004737451,0.000097000135,0.0007515316,0.00012165614,0.8586397,0.020196427,0.0037865145,0.00030334754,0.006653482],"study_design_scores_gemma":[0.000018692113,0.000101387326,0.09635532,0.0000053158637,0.00003533156,0.0000870523,0.000090036985,0.9005469,0.0011730349,0.001372639,0.00018988819,0.000024473642],"about_ca_topic_score_codex":0.012458855,"about_ca_topic_score_gemma":0.007255022,"teacher_disagreement_score":0.012458855,"about_ca_system_score_codex":0.0009099442,"about_ca_system_score_gemma":0.00062476646,"threshold_uncertainty_score":0.024772704},"labels":[],"label_agreement":null},{"id":"W4312007164","doi":"10.22541/essoar.167065821.11251161/v2","title":"Statistical and clustering analysis of microseismicity from a Saskatchewan potash mine","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Nutrasource; Western University","funders":"","keywords":"Poisson distribution; Cluster analysis; Magnitude (astronomy); Pareto distribution; Potash; Scaling; Pareto principle; Geology; Statistics; Data mining; Computer science; Mining engineering; Mathematics; Physics","score_opus":0.018294852170566447,"score_gpt":0.23845435577313834,"score_spread":0.2201595036025719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312007164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966918,0.00001578855,0.0015251178,0.000033936412,0.0000023157095,0.000018551726,0.00094326626,0.00003251408,0.00073678454],"genre_scores_gemma":[0.99571615,0.000031426185,0.0012052312,0.000010049433,0.0000018895656,0.000014805473,0.0023475445,0.000008999572,0.00066390145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997793,0.000023975801,0.000016569491,0.0000615289,0.000074545824,0.000044159944],"domain_scores_gemma":[0.9988747,0.00022237086,0.0001366949,0.00011321635,0.0005528177,0.00010011672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028890322,0.00027121074,0.00025937305,0.0014933278,0.00058398466,0.00050371134,0.00054956536,0.0003681654,0.0007794229],"category_scores_gemma":[0.0011888258,0.00017368222,0.00028044803,0.0026991654,0.00044281746,0.00016985282,0.00046429227,0.0003012335,0.000167765],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029902847,0.00018517471,0.6705191,0.00014851193,0.00026783196,0.002258905,0.0013465678,0.24872185,0.032134317,0.002521784,0.0034318017,0.03816515],"study_design_scores_gemma":[0.000012702884,0.000029604353,0.8222233,0.000013726137,0.000028404489,0.0001132738,0.00092279655,0.17265148,0.0024704337,0.00044802384,0.0010350612,0.00005114207],"about_ca_topic_score_codex":0.54057807,"about_ca_topic_score_gemma":0.68241185,"teacher_disagreement_score":0.45942193,"about_ca_system_score_codex":0.0025243715,"about_ca_system_score_gemma":0.0022870742,"threshold_uncertainty_score":0.92425513},"labels":[],"label_agreement":null},{"id":"W4312068045","doi":"10.22541/essoar.167065821.11251161/v1","title":"Statistical and clustering analysis of microseismicity from a Saskatchewan potash mine","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Nutrasource; Western University","funders":"","keywords":"Poisson distribution; Cluster analysis; Magnitude (astronomy); Potash; Pareto distribution; Scaling; Pareto principle; Distribution (mathematics); Statistics; Generalized Pareto distribution; Data mining; Geology; Computer science; Mining engineering; Mathematics; Physics; Extreme value theory; Materials science","score_opus":0.018294852170566447,"score_gpt":0.23845435577313834,"score_spread":0.2201595036025719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312068045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966918,0.00001578855,0.0015251178,0.000033936412,0.0000023157095,0.000018551726,0.00094326626,0.00003251408,0.00073678454],"genre_scores_gemma":[0.99571615,0.000031426185,0.0012052312,0.000010049433,0.0000018895656,0.000014805473,0.0023475445,0.000008999572,0.00066390145],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997793,0.000023975801,0.000016569491,0.0000615289,0.000074545824,0.000044159944],"domain_scores_gemma":[0.9988747,0.00022237086,0.0001366949,0.00011321635,0.0005528177,0.00010011672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028890322,0.00027121074,0.00025937305,0.0014933278,0.00058398466,0.00050371134,0.00054956536,0.0003681654,0.0007794229],"category_scores_gemma":[0.0011888258,0.00017368222,0.00028044803,0.0026991654,0.00044281746,0.00016985282,0.00046429227,0.0003012335,0.000167765],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029902847,0.00018517471,0.6705191,0.00014851193,0.00026783196,0.002258905,0.0013465678,0.24872185,0.032134317,0.002521784,0.0034318017,0.03816515],"study_design_scores_gemma":[0.000012702884,0.000029604353,0.8222233,0.000013726137,0.000028404489,0.0001132738,0.00092279655,0.17265148,0.0024704337,0.00044802384,0.0010350612,0.00005114207],"about_ca_topic_score_codex":0.54057807,"about_ca_topic_score_gemma":0.68241185,"teacher_disagreement_score":0.45942193,"about_ca_system_score_codex":0.0025243715,"about_ca_system_score_gemma":0.0022870742,"threshold_uncertainty_score":0.92425513},"labels":[],"label_agreement":null},{"id":"W4312385590","doi":"10.4095/330927","title":"Scientific basis of Canada's first public national seismic risk model","year":2022,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismic risk; Fragility; Disaster risk reduction; Preparedness; Seismic hazard; Vulnerability (computing); Probabilistic logic; Urban seismic risk; Government (linguistics); Geography; Environmental science; Civil engineering; Engineering; Environmental resource management; Computer science; Political science","score_opus":0.048908132190824315,"score_gpt":0.2264732469628683,"score_spread":0.17756511477204398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312385590","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09182172,0.00083224755,0.35608667,0.017122557,0.00026637266,0.0007547157,0.061956026,0.0022851215,0.46887454],"genre_scores_gemma":[0.77936167,0.0015379124,0.1260441,0.00084143115,0.000120616314,0.0008092065,0.030132256,0.00056252937,0.060590357],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99842215,0.00021741856,0.000053596326,0.00017842217,0.00085714384,0.00027125844],"domain_scores_gemma":[0.9969285,0.00048691867,0.00012652186,0.0002662591,0.0020580806,0.00013363015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018440358,0.0006394245,0.0004871394,0.001432557,0.0019092743,0.0032341212,0.002875183,0.0008589653,0.006792209],"category_scores_gemma":[0.006667627,0.00049132295,0.00067391363,0.002310605,0.0011750393,0.0014706049,0.0014521609,0.0014442021,0.00090751814],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005192455,0.00006533402,0.0062722657,0.00005913976,0.00003718607,0.00013141317,0.0002895622,0.6232873,0.00028419858,0.30844095,0.03702344,0.024057334],"study_design_scores_gemma":[0.000040936746,0.000017033593,0.0040708454,0.000061550454,0.000028163087,0.000062457155,0.00025528067,0.859877,0.00036786858,0.06264112,0.07252469,0.00005306578],"about_ca_topic_score_codex":0.96041185,"about_ca_topic_score_gemma":0.92778,"teacher_disagreement_score":0.039588153,"about_ca_system_score_codex":0.032195378,"about_ca_system_score_gemma":0.04663697,"threshold_uncertainty_score":0.2335949},"labels":[],"label_agreement":null},{"id":"W4312678027","doi":"10.4095/331199","title":"Seismic hazard investigations at select DND facilities in Southwestern British Columbia: subduction, in-slab, and crustal scenarios","year":2022,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Subduction; Geology; Seismology; Slab; Aftershock; Seismic hazard; Fault (geology); Hazard; Tectonics; Paleontology","score_opus":0.026681630919405633,"score_gpt":0.21590601237078394,"score_spread":0.18922438145137832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312678027","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951851,0.000041016083,0.000110874986,0.00006750565,0.0000012735006,0.000068607565,0.0011582287,0.00001608469,0.003351259],"genre_scores_gemma":[0.99669987,0.00010807275,0.00038290297,0.00004032711,0.0000012890689,0.000033295084,0.0010869106,0.0000035190922,0.0016437549],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997205,0.000032020147,0.000012589741,0.000030294452,0.00008710573,0.000117370735],"domain_scores_gemma":[0.99927694,0.0000897771,0.000107006126,0.000030031611,0.00025493465,0.00024134127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020706569,0.00041868552,0.00020000468,0.0016437968,0.0015682321,0.000643877,0.00084249466,0.00037661326,0.0022844588],"category_scores_gemma":[0.0009899465,0.00026696944,0.00015941258,0.002469829,0.00042683483,0.0002552431,0.0006470374,0.00038050977,0.0001617397],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019969391,0.00025549866,0.95796573,0.00014357209,0.000073817166,0.0020933521,0.0021222883,0.010206178,0.0028785432,0.0003570186,0.0023770428,0.021327276],"study_design_scores_gemma":[0.00002572662,0.00010872295,0.9784792,0.00003495252,0.000027150296,0.00019927723,0.009349739,0.008769549,0.00062880106,0.00013187245,0.002218807,0.00002628773],"about_ca_topic_score_codex":0.9428286,"about_ca_topic_score_gemma":0.98562396,"teacher_disagreement_score":0.057171404,"about_ca_system_score_codex":0.011849474,"about_ca_system_score_gemma":0.0067614266,"threshold_uncertainty_score":0.11501616},"labels":[],"label_agreement":null},{"id":"W4312796380","doi":"10.4095/330943","title":"Mapping tectonic stress at subduction zones with earthquake focal mechanisms: application to Cascadia, Japan, Nankai, Mexico, and northern Chile","year":2022,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Seismology; Subduction; Focal mechanism; Classification of discontinuities; Tectonics; Forearc; Slip (aerodynamics); Trench; Discontinuity (linguistics); Induced seismicity; Seismic hazard; Plate tectonics","score_opus":0.015098026230548333,"score_gpt":0.21421415113542192,"score_spread":0.19911612490487357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312796380","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99645907,0.00015930415,0.0011703034,0.000048671045,0.000005076798,0.000028699847,0.0012475043,0.00018145074,0.00069989386],"genre_scores_gemma":[0.9904417,0.00018958522,0.0068636932,0.000009660738,0.0000084782205,0.000046880363,0.0019588182,0.000034678884,0.00044654895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998716,0.000012874275,0.000014278493,0.000050106573,0.000023737139,0.000027374981],"domain_scores_gemma":[0.9997228,0.000038264465,0.00007955667,0.000036057485,0.00006421208,0.000059058493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002799373,0.0006827124,0.00039239996,0.0026569685,0.00048660685,0.0008851017,0.00040618549,0.00026657776,0.0008908046],"category_scores_gemma":[0.00081606006,0.00035077636,0.0005392036,0.0032819612,0.0002184944,0.00035340543,0.00084340706,0.00019784851,0.00015756542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019086197,0.00019908436,0.86754173,0.00016300351,0.00027374545,0.00078638643,0.0015822991,0.022271108,0.013592205,0.00020718205,0.001639511,0.091552876],"study_design_scores_gemma":[0.000034543267,0.00003765766,0.9465782,0.000032525033,0.00008369526,0.00012921356,0.0016545252,0.04839354,0.0012927414,0.0001821854,0.0015501243,0.000031219475],"about_ca_topic_score_codex":0.08798477,"about_ca_topic_score_gemma":0.10530316,"teacher_disagreement_score":0.9120152,"about_ca_system_score_codex":0.0006172747,"about_ca_system_score_gemma":0.00096827484,"threshold_uncertainty_score":0.1749453},"labels":[],"label_agreement":null},{"id":"W4312920016","doi":"10.1109/oceans47191.2022.9977059","title":"Assessment of tsunami coastal hazard along the Northwest Vancouver Island from coseismic sources in Cascadia and Alaska subduction zones","year":2022,"lang":"en","type":"article","venue":"OCEANS 2022, Hampton Roads","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society","funders":"","keywords":"Subduction; Geology; Seismology; Oceanography; Hazard analysis; Tectonics","score_opus":0.0072535802900442386,"score_gpt":0.2058990110556897,"score_spread":0.19864543076564545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312920016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926292,0.00014921703,0.00031343353,0.00006555035,0.00000672174,0.000033001994,0.00095438765,0.000023235309,0.005825276],"genre_scores_gemma":[0.9954464,0.00024050305,0.0005776316,0.0000126150335,0.0000020260266,0.000016324833,0.0013124136,0.0000052138003,0.0023868561],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998192,0.000013697841,0.000010274736,0.000021822598,0.00009060314,0.000044416356],"domain_scores_gemma":[0.99966896,0.000020520429,0.000025879246,0.0000108613385,0.00018444327,0.000089390545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020332924,0.00045363302,0.00019155967,0.0015721688,0.0014171387,0.0015814224,0.00038164627,0.0002789898,0.00092743005],"category_scores_gemma":[0.0005394151,0.00021618757,0.00022247511,0.0017963159,0.00026185557,0.00017589428,0.0006991629,0.00032169928,0.00015660246],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011676866,0.000070688875,0.9401221,0.00005964585,0.000096846445,0.0011724301,0.0010284263,0.024181902,0.0020106877,0.00035574156,0.0015640677,0.029220715],"study_design_scores_gemma":[0.000011424275,0.000028468947,0.9645354,0.000058855294,0.00005421585,0.00011411094,0.0046105697,0.027570097,0.00050176145,0.0001235463,0.0023685773,0.000022897313],"about_ca_topic_score_codex":0.9224357,"about_ca_topic_score_gemma":0.96752733,"teacher_disagreement_score":0.0775643,"about_ca_system_score_codex":0.0040371455,"about_ca_system_score_gemma":0.0049065463,"threshold_uncertainty_score":0.15604216},"labels":[],"label_agreement":null},{"id":"W4313002566","doi":"10.4095/331095","title":"Temporal variations in coda Q before and after the 2017 Barrow Strait earthquake (Mw 5.9) in Nunavut and the 2012 Haida Gwaii earthquake (Mw 7.8) in British Columbia","year":2022,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Coda; Geology; Seismometer; Aftershock; Induced seismicity; Subduction; Plate tectonics; Tectonics","score_opus":0.015236698387290165,"score_gpt":0.2216860816377052,"score_spread":0.20644938325041504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313002566","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964222,0.0001748578,0.00007407456,0.00006219533,0.000009951452,0.000012356184,0.001148372,0.000009844307,0.0020861963],"genre_scores_gemma":[0.997008,0.00016935526,0.000095961994,0.000026747795,0.0000071890545,0.000009833059,0.0014617706,0.0000045782863,0.0012166904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974734,0.000009087617,0.000012386924,0.000048963724,0.00009069241,0.00009146467],"domain_scores_gemma":[0.9987722,0.00006372201,0.00021996393,0.000028105698,0.0006816216,0.00023441717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020296451,0.00024099303,0.00020336897,0.0016783496,0.0009800928,0.0008119847,0.0003722984,0.00031594856,0.0010521375],"category_scores_gemma":[0.0012272694,0.00013459112,0.00014421805,0.0022485713,0.00054822705,0.000295767,0.00066118524,0.000402013,0.00018112532],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011872715,0.000023357079,0.9843908,0.00003194684,0.0000415896,0.00031048467,0.0016448771,0.00017950531,0.0021514022,0.000076451804,0.00092323817,0.010107686],"study_design_scores_gemma":[5.98957e-7,0.0000038346507,0.9989262,0.0000034588775,0.0000032796747,0.000015004331,0.0005150759,0.000049342216,0.000045665958,0.0000030245953,0.00043160396,0.0000029796806],"about_ca_topic_score_codex":0.92130125,"about_ca_topic_score_gemma":0.97484946,"teacher_disagreement_score":0.078698754,"about_ca_system_score_codex":0.004815494,"about_ca_system_score_gemma":0.0037968878,"threshold_uncertainty_score":0.15832442},"labels":[],"label_agreement":null},{"id":"W4313471278","doi":"10.3390/w15010164","title":"The Michoacán Tsunami of 19 September 2022 on the Coast of Mexico: Observations, Spectral Properties and Modelling","year":2022,"lang":"en","type":"article","venue":"Water","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration; Instituto Politécnico Nacional; Shirshov Institute of Oceanology, Russian Academy of Sciences; Northwestern University","keywords":"Seiche; Tide gauge; Submarine pipeline; Geology; Seismology; Period (music); Oceanography; Tsunami wave; Tsunami earthquake; East coast; Sea level","score_opus":0.0589286285844586,"score_gpt":0.1955509143057104,"score_spread":0.1366222857212518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313471278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99571973,0.00013096491,0.00096507435,0.00008388734,0.000007420572,0.000015337017,0.0007757472,0.000081359525,0.0022203536],"genre_scores_gemma":[0.9971577,0.0001767643,0.0010300251,0.000009964687,0.000010193505,0.000022059607,0.00095586176,0.000013833714,0.00062361796],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999622,0.0000045663755,0.00000227954,0.00001248259,0.000007308427,0.000011254498],"domain_scores_gemma":[0.9999331,0.000011992004,0.000019479763,0.000005235612,0.00001886922,0.000011360994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000104115694,0.00044181902,0.00015797491,0.00058188586,0.00036474687,0.0006746604,0.00048861245,0.00056042545,0.0008751312],"category_scores_gemma":[0.00029908153,0.00023284771,0.00031153165,0.0007233288,0.0001721863,0.00032065608,0.00025196225,0.00019167001,0.00018759035],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033038692,0.00027179814,0.49555895,0.00014207717,0.0001667981,0.0017587821,0.0005991503,0.4555877,0.012833777,0.0011441176,0.0034664427,0.02814007],"study_design_scores_gemma":[0.000056748064,0.000051840623,0.4425198,0.000021191616,0.000041100964,0.0001926045,0.00036311575,0.5535427,0.0006496832,0.00019429959,0.0023233646,0.000043582095],"about_ca_topic_score_codex":0.13512479,"about_ca_topic_score_gemma":0.090982825,"teacher_disagreement_score":0.13512479,"about_ca_system_score_codex":0.000824644,"about_ca_system_score_gemma":0.00033201659,"threshold_uncertainty_score":0.26867658},"labels":[],"label_agreement":null},{"id":"W4313585762","doi":"10.3389/fbuil.2022.1022736","title":"Future perspectives of earthquake-tsunami catastrophe modelling: From single-hazards to cascading and compounding multi-hazards","year":2023,"lang":"en","type":"article","venue":"Frontiers in Built Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Natural hazard; Risk management; Disaster risk reduction; Hazard; Natural disaster; Risk assessment; Risk analysis (engineering); Forensic engineering; Probabilistic logic; Emergency management; Earthquake scenario; Environmental resource management; Environmental science; Engineering; Computer science; Civil engineering; Geography; Business; Seismic hazard; Computer security; Meteorology; Political science","score_opus":0.02265477443329355,"score_gpt":0.2179822598895657,"score_spread":0.19532748545627215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313585762","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021995027,0.54914206,0.26918784,0.113721505,0.0029425411,0.00009776825,0.00037422508,0.00044249365,0.04209659],"genre_scores_gemma":[0.24612974,0.618941,0.11907599,0.003190678,0.0042723357,0.0001542069,0.00037866863,0.00012402362,0.0077332724],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99906605,0.0005721348,0.00005354202,0.000058221554,0.00019271186,0.000057336954],"domain_scores_gemma":[0.99578285,0.0032813372,0.00018030812,0.00015136896,0.00042065472,0.00018350352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003703702,0.0007543636,0.00096896966,0.0012494969,0.0005656282,0.0032229193,0.0015447345,0.0021723546,0.0041595865],"category_scores_gemma":[0.004041287,0.00030998274,0.0008946685,0.002124291,0.0016820632,0.0054701357,0.0017770512,0.002694988,0.00068188977],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009548048,0.00025482607,0.0038473774,0.003263664,0.00014448822,0.00046301796,0.0010229786,0.16913424,0.001414475,0.49358928,0.025803376,0.3009668],"study_design_scores_gemma":[0.000012264314,0.0001931177,0.0014473203,0.0016636383,0.00005491475,0.0003877626,0.0017014418,0.14256243,0.000556841,0.7045737,0.14670326,0.00014329885],"about_ca_topic_score_codex":0.003541847,"about_ca_topic_score_gemma":0.0049725,"teacher_disagreement_score":0.0041595865,"about_ca_system_score_codex":0.001138392,"about_ca_system_score_gemma":0.0019013534,"threshold_uncertainty_score":0.019587278},"labels":[],"label_agreement":null},{"id":"W4313947397","doi":"10.1785/0120220066","title":"Incorporating Full Elastodynamic Effects and Dipping Fault Geometries in Community Code Verification Exercises for Simulations of Earthquake Sequences and Aseismic Slip (SEAS)","year":2023,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Agence Nationale de la Recherche","keywords":"Slip (aerodynamics); Seismic hazard; Earthquake simulation; Earthquake engineering; Geology; Seismology; Algorithm; Computer science; Structural engineering; Engineering","score_opus":0.02229245475521408,"score_gpt":0.24379068257414957,"score_spread":0.2214982278189355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313947397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98302865,0.00004244703,0.011642322,0.00009499622,0.000025930525,0.000047995683,0.00033449865,0.00070829334,0.004074963],"genre_scores_gemma":[0.98613495,0.000016386935,0.012883271,0.000023443825,0.000003803979,0.00003554723,0.00041127703,0.00010919118,0.0003821977],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993806,0.00018425664,0.00005040944,0.000086200955,0.00019784129,0.00010068979],"domain_scores_gemma":[0.9960167,0.0020700437,0.00024908455,0.0004981436,0.00095148524,0.00021443084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015965246,0.0005247971,0.00036507877,0.0005691946,0.0004686391,0.000493473,0.0012857988,0.0005519071,0.0017940659],"category_scores_gemma":[0.0062700305,0.00020000088,0.00038352056,0.00050223403,0.00049736514,0.0007469011,0.0009777779,0.00075015886,0.00019550536],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082513853,0.0009702825,0.03424378,0.00023676264,0.00008146248,0.00029538965,0.00041871675,0.8830502,0.015814042,0.004521382,0.0025254332,0.05701734],"study_design_scores_gemma":[0.00010477225,0.00019301096,0.0033951278,0.000015253993,0.000009599777,0.000021690801,0.00009961529,0.9869467,0.00784822,0.0005314946,0.0008201183,0.000014377285],"about_ca_topic_score_codex":0.016858913,"about_ca_topic_score_gemma":0.015856922,"teacher_disagreement_score":0.016858913,"about_ca_system_score_codex":0.00064642535,"about_ca_system_score_gemma":0.001056933,"threshold_uncertainty_score":0.033521533},"labels":[],"label_agreement":null},{"id":"W4315701619","doi":"10.2113/2022/9823275","title":"Resolving Quaternary Tectonic Activity with High-Resolution Data in Space and Time","year":2022,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Institute of Geology, China Earthquake Administration; National Natural Science Foundation of China","keywords":"Geology; Tectonics; Active fault; Seismology; Fault (geology); Paleoseismology; Quaternary; Geologic record; Paleontology","score_opus":0.015770073779200817,"score_gpt":0.21067429460194362,"score_spread":0.1949042208227428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315701619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5111033,0.09535609,0.18853109,0.0382271,0.041860726,0.00028052562,0.06320335,0.008241344,0.05319654],"genre_scores_gemma":[0.6933131,0.037420746,0.1460078,0.0041802237,0.03345458,0.00015109146,0.06541835,0.0023110213,0.0177431],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9994573,0.000074192074,0.000060739923,0.00013416562,0.00020597296,0.00006757565],"domain_scores_gemma":[0.9974783,0.0005035403,0.00039105842,0.00037519127,0.00092855335,0.00032330744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020183348,0.00041855322,0.0007321719,0.003148223,0.00066431466,0.0034506053,0.00085724326,0.0012757793,0.004390512],"category_scores_gemma":[0.004019967,0.0004424706,0.0004938415,0.0038069582,0.00048354844,0.0021352647,0.0019024343,0.0014237834,0.0018571969],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003481808,0.00025868902,0.15863676,0.0013262149,0.00062999135,0.0013309916,0.001250265,0.02196149,0.053566888,0.007264075,0.2607642,0.49266222],"study_design_scores_gemma":[0.00007725272,0.00016093542,0.27989125,0.0005735558,0.0003983771,0.00081252115,0.0011684237,0.1068041,0.0117877675,0.01477952,0.5833195,0.00022675801],"about_ca_topic_score_codex":0.0043255542,"about_ca_topic_score_gemma":0.010453315,"teacher_disagreement_score":0.004390512,"about_ca_system_score_codex":0.00048044603,"about_ca_system_score_gemma":0.00070138054,"threshold_uncertainty_score":0.014687717},"labels":[],"label_agreement":null},{"id":"W4315784240","doi":"10.1029/2022jb025048","title":"Quantitative Evaluation of the Competing Effects of Wastewater Disposal and Hydraulic Fracturing on Causing Induced Earthquakes: A Case Study of an M3.1 Earthquake Sequence in Western Canada","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Geology; Hydraulic fracturing; Seismology; Pore water pressure; Perturbation (astronomy); Structural basin; Poromechanics; Geotechnical engineering; Paleontology; Physics","score_opus":0.10674662721159774,"score_gpt":0.378138658603342,"score_spread":0.2713920313917443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315784240","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99850684,0.00004824863,0.00048763744,0.000018376919,0.0000012738216,0.000022927486,0.00039426563,0.00001797707,0.0005024572],"genre_scores_gemma":[0.99842536,0.000047622092,0.0009227233,0.0000044499993,0.0000016672498,0.0000050653753,0.00038218708,0.0000034340428,0.00020745165],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973077,0.000029232266,0.000019414181,0.000037016216,0.00010717761,0.0000764481],"domain_scores_gemma":[0.9988881,0.000420426,0.00017694797,0.000063614876,0.00031089116,0.00014002557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046047027,0.00044971093,0.0003564984,0.0020683755,0.00060940685,0.0006910138,0.0005701608,0.0004084683,0.00064762693],"category_scores_gemma":[0.0018062845,0.00018244504,0.00040966645,0.002586627,0.00059058005,0.00029412704,0.00041870246,0.0002280307,0.00005742137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021640141,0.00021619082,0.86308146,0.00019689092,0.00021655521,0.004803572,0.0009152092,0.09265631,0.0110792825,0.0010000477,0.0006501811,0.02496793],"study_design_scores_gemma":[0.000020802674,0.00008059668,0.8440333,0.0000199727,0.00011537621,0.0003415789,0.0019836265,0.14958268,0.0027158519,0.00020710954,0.00086650584,0.000032580243],"about_ca_topic_score_codex":0.68208814,"about_ca_topic_score_gemma":0.7935473,"teacher_disagreement_score":0.31791186,"about_ca_system_score_codex":0.0035214082,"about_ca_system_score_gemma":0.002349536,"threshold_uncertainty_score":0.6395682},"labels":[],"label_agreement":null},{"id":"W4315796720","doi":"10.3389/feart.2022.1017632","title":"The present-day stress field along the Northwest Pacific Wadati-Benioff zone constrained by focal mechanisms of moderate earthquakes","year":2023,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Earthquake Administration","keywords":"Trench; Slab; Geology; Seismology; Stress field; Compression (physics); Focal mechanism; Stress (linguistics); Pacific Plate; Petrology; Subduction; Induced seismicity; Geophysics; Tectonics; Materials science","score_opus":0.00936951919031584,"score_gpt":0.20596092289355294,"score_spread":0.1965914037032371,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4315796720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99908066,0.00003362717,0.00003221292,0.000010518407,0.0000010660796,0.000002472665,0.0005491066,0.000003871381,0.00028645695],"genre_scores_gemma":[0.9982041,0.000051807972,0.000082820174,0.000004479176,0.0000031254544,0.0000051639345,0.0014572515,0.0000015939254,0.00018965194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992263,0.000005758696,0.000006358449,0.000020380126,0.000015863707,0.000029036722],"domain_scores_gemma":[0.9997482,0.000015552558,0.000076037235,0.000012525742,0.0000695079,0.00007825357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013056633,0.00028157383,0.00020979987,0.0015902452,0.00031863808,0.00044421983,0.00025751465,0.00025630562,0.00095534587],"category_scores_gemma":[0.00035460503,0.0001566779,0.00015667909,0.0014899649,0.00024138764,0.00026708757,0.0004021876,0.00014370233,0.00013820083],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008633866,0.000019477502,0.99171853,0.000023439543,0.000043603846,0.00021578562,0.00028264386,0.0005688785,0.002538363,0.000059399314,0.0002718647,0.0041716523],"study_design_scores_gemma":[0.000001812807,0.0000059929157,0.9992073,0.000002612068,0.0000049633572,0.000020709711,0.00016707291,0.00039226434,0.00006454621,0.000008395824,0.00012219632,0.0000020465047],"about_ca_topic_score_codex":0.07091659,"about_ca_topic_score_gemma":0.11894405,"teacher_disagreement_score":0.07091659,"about_ca_system_score_codex":0.000567953,"about_ca_system_score_gemma":0.00040303313,"threshold_uncertainty_score":0.1410076},"labels":[],"label_agreement":null},{"id":"W4317473413","doi":"10.5670/oceanog.2023.s1.24","title":"Assessment of Tsunami Hazard Along British Columbia Coastlines from Coseismic Sources","year":2023,"lang":"en","type":"article","venue":"Oceanography","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society","funders":"","keywords":"Signage; Indigenous; Geography; Hazard analysis; Hazard; West coast; Natural hazard; Oceanography; Environmental resource management; Meteorology; Geology; Environmental science; Engineering; Ecology","score_opus":0.01294448710133639,"score_gpt":0.22346286897600254,"score_spread":0.21051838187466615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317473413","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9786885,0.00020128682,0.0002538299,0.000096586016,0.0000053762137,0.00007526009,0.0021989744,0.00002670023,0.01845344],"genre_scores_gemma":[0.9908313,0.0003817214,0.0005452134,0.000026442061,0.0000021537003,0.00003305526,0.0017304958,0.000007239869,0.0064423257],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99973994,0.000010870317,0.000011318811,0.000028874061,0.00015663046,0.00005242537],"domain_scores_gemma":[0.999303,0.000046891528,0.000047250833,0.00001387149,0.000505053,0.000083899075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001423246,0.0004140875,0.00015988601,0.0025824034,0.0025013897,0.0015021675,0.00042163138,0.0002831897,0.0034616943],"category_scores_gemma":[0.0008435349,0.00017949253,0.0001264489,0.0039751725,0.00037346012,0.00024385237,0.0007323135,0.00038745266,0.00046977046],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025397696,0.00014307353,0.8891352,0.00016994971,0.00008459866,0.0013153609,0.0034027146,0.0053902236,0.007378661,0.00044188742,0.005784405,0.08650002],"study_design_scores_gemma":[0.0000069536595,0.000027219618,0.9886827,0.00004593383,0.000022648686,0.000073188574,0.005307469,0.002339734,0.0006565085,0.000053105803,0.002768845,0.000015693555],"about_ca_topic_score_codex":0.97997415,"about_ca_topic_score_gemma":0.9948756,"teacher_disagreement_score":0.02002585,"about_ca_system_score_codex":0.008386625,"about_ca_system_score_gemma":0.0070750318,"threshold_uncertainty_score":0.060849547},"labels":[],"label_agreement":null},{"id":"W4318191475","doi":"10.1029/2022jb025034","title":"Rapid Tremor Migration During Few Minute‐Long Slow Earthquakes in Cascadia","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Seismology; Episodic tremor and slip; Geology; Slip (aerodynamics); Subduction; Coherence (philosophical gambling strategy); Geodesy; Tectonics; Physics","score_opus":0.05701483990482568,"score_gpt":0.3162004412671169,"score_spread":0.2591856013622912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318191475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994048,0.000029938508,0.000063278596,0.000018048713,0.0000010298977,0.0000017715856,0.000107819906,0.000009509353,0.00036388525],"genre_scores_gemma":[0.9997316,0.000021103555,0.000043356806,0.000003060316,0.0000013348483,0.0000018380474,0.00009329619,0.0000020447899,0.000102324506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999299,0.000008550931,0.000005482181,0.000020408515,0.000018448147,0.000017209706],"domain_scores_gemma":[0.999395,0.00009292723,0.00019946242,0.000040887528,0.0001223947,0.00014935769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001771026,0.00017782209,0.00018877855,0.0012277167,0.00044820856,0.0003799559,0.00019789021,0.00025509883,0.0012450491],"category_scores_gemma":[0.00094529707,0.0001693791,0.00011510151,0.0009915016,0.00033274954,0.00019536281,0.0005044761,0.00019095751,0.00023508962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019213714,0.000042445205,0.9609338,0.000051220082,0.00006295036,0.00045081906,0.0016589429,0.0011882639,0.027978517,0.000102749495,0.00035991584,0.006978322],"study_design_scores_gemma":[0.0000021996514,0.0000160391,0.999236,0.0000019192141,0.0000037666446,0.000035090394,0.00021034769,0.00024518886,0.00012757661,0.000014091087,0.0001054871,0.000002304362],"about_ca_topic_score_codex":0.036346883,"about_ca_topic_score_gemma":0.06284465,"teacher_disagreement_score":0.9636531,"about_ca_system_score_codex":0.0005186746,"about_ca_system_score_gemma":0.00026838252,"threshold_uncertainty_score":0.07227063},"labels":[],"label_agreement":null},{"id":"W4318257706","doi":"10.1007/s40789-022-00560-7","title":"Numerical modelling of spatially and temporally distributed on-fault induced seismicity: implication for seismic hazards","year":2023,"lang":"en","type":"article","venue":"International Journal of Coal Science & Technology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Japan Society for the Promotion of Science","keywords":"Induced seismicity; Seismology; Geology; Fault plane; Slip (aerodynamics); Stress field; Fault (geology); Seismic risk; Structural engineering; Engineering; Finite element method","score_opus":0.03110331924418568,"score_gpt":0.2842021773888885,"score_spread":0.2530988581447028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318257706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86456376,0.00023386265,0.12610945,0.0003140736,0.00007231785,0.00007511394,0.00024476644,0.00022473374,0.008161878],"genre_scores_gemma":[0.9939611,0.000076587254,0.004946083,0.00001304482,0.000007761936,0.000025917745,0.00004939929,0.000011764216,0.0009083576],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998996,0.000040871124,0.00000663532,0.000013771956,0.000021664944,0.000017354978],"domain_scores_gemma":[0.99964154,0.00017942669,0.00006541893,0.00002737568,0.000050339,0.000035998313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025073648,0.00036252648,0.00037901962,0.0004248755,0.000336642,0.0005911399,0.00059991964,0.0012325159,0.0012540844],"category_scores_gemma":[0.00094148907,0.00019550088,0.00045132719,0.0003390549,0.0006187577,0.00034650226,0.00050140126,0.00044002995,0.000095816],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000109062585,0.000020570053,0.00090831204,0.0000062693794,0.00000550178,0.000043687316,0.0000094171,0.9970884,0.00080836075,0.00045952242,0.000026641063,0.0006124234],"study_design_scores_gemma":[0.0000017105741,0.0000067195724,0.0001284284,8.22256e-7,0.0000010753766,0.0000030980666,0.000003966238,0.99966466,0.00007529639,0.00008867523,0.000024541183,0.0000010965488],"about_ca_topic_score_codex":0.013207961,"about_ca_topic_score_gemma":0.0050317403,"teacher_disagreement_score":0.013207961,"about_ca_system_score_codex":0.00047558156,"about_ca_system_score_gemma":0.00058374205,"threshold_uncertainty_score":0.026262164},"labels":[],"label_agreement":null},{"id":"W4319602865","doi":"10.1029/2022jb025662","title":"A Long‐Term Earthquake Catalog for the Endeavour Segment: Constraints on the Extensional Cycle and Evidence for Hydrothermal Venting Supported by Propagating Rifts","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Ocean Networks Canada Society; University of Victoria","funders":"National Defense Science and Engineering Graduate; National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Seismometer; Rift; Ridge; Magmatism; Bathymetry; Observatory; Mid-ocean ridge; Geophysics; Tectonics; Paleontology; Oceanography","score_opus":0.10001777294504052,"score_gpt":0.3574782625628935,"score_spread":0.25746048961785295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319602865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99345917,0.00006614999,0.0002670761,0.00002222498,0.0000021231479,0.000011685,0.005028549,0.000025122792,0.0011179814],"genre_scores_gemma":[0.9852769,0.00006402788,0.0006734936,0.000009185334,0.0000076751385,0.000014873822,0.013553435,0.00000960763,0.00039086302],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977595,0.000021077558,0.000030121346,0.00004780645,0.000070132,0.000054943397],"domain_scores_gemma":[0.998125,0.00014441146,0.00068025675,0.00022222071,0.00048493742,0.0003431601],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003746972,0.00019451746,0.00021608475,0.0026112502,0.00032555498,0.00057246175,0.00030424702,0.00019022169,0.0011942049],"category_scores_gemma":[0.0013517966,0.00011536072,0.00020596146,0.0024422004,0.00022118325,0.0003387817,0.0007046124,0.00014298651,0.00037729103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022810476,0.0000123965665,0.9908308,0.000014957492,0.000017258628,0.000092807175,0.00015090767,0.0002859543,0.0029943243,0.00003880141,0.00030688016,0.0052321474],"study_design_scores_gemma":[0.0000017268734,0.0000070461037,0.99897003,0.0000038807175,0.000003794912,0.000031768046,0.00008198648,0.00031160566,0.00014735304,0.000009228019,0.0004294752,0.0000022173028],"about_ca_topic_score_codex":0.06463119,"about_ca_topic_score_gemma":0.15774573,"teacher_disagreement_score":0.06463119,"about_ca_system_score_codex":0.00048842013,"about_ca_system_score_gemma":0.0006515821,"threshold_uncertainty_score":0.12851},"labels":[],"label_agreement":null},{"id":"W4319795474","doi":"10.22541/essoar.167525181.10212724/v1","title":"When Plates Collide","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Oxford; University of Alberta","keywords":"Plate tectonics; Geology; Subduction; Tectonics; Seismology; Geodynamics; Convergent boundary; Oceanic crust","score_opus":0.05422123597547404,"score_gpt":0.24275964500291544,"score_spread":0.1885384090274414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319795474","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.55424845,0.0027569688,0.011934815,0.0034570477,0.0023350008,0.00013918556,0.0035760042,0.0011883244,0.42036423],"genre_scores_gemma":[0.9378455,0.0008826355,0.0028253484,0.00069767935,0.00040137628,0.000081157326,0.0033662396,0.00039193858,0.053508088],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986608,0.00010760183,0.0000663752,0.0003326901,0.00039843807,0.0004340525],"domain_scores_gemma":[0.9979219,0.00041188835,0.00054758746,0.0003417512,0.00033105438,0.0004458024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061437325,0.00053770497,0.0006617599,0.0018531706,0.0019865865,0.005074155,0.0010157368,0.0015861086,0.055785153],"category_scores_gemma":[0.0050826934,0.00060039986,0.0005091951,0.0014614584,0.0016431191,0.0036759686,0.004066125,0.0014829809,0.019527363],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027237935,0.00020058505,0.30636442,0.001335557,0.00053998653,0.026813935,0.020223033,0.0113784,0.029431356,0.17228162,0.15047248,0.2782349],"study_design_scores_gemma":[0.00013204593,0.0006139889,0.34640473,0.00074091996,0.00034201244,0.015556204,0.05078505,0.007884232,0.017839422,0.109979585,0.4492787,0.00044297366],"about_ca_topic_score_codex":0.0033029828,"about_ca_topic_score_gemma":0.004110534,"teacher_disagreement_score":0.055785153,"about_ca_system_score_codex":0.0008740978,"about_ca_system_score_gemma":0.00074428244,"threshold_uncertainty_score":0.18661994},"labels":[],"label_agreement":null},{"id":"W4320726353","doi":"10.31223/x5137d","title":"Coseismic Coulomb Stress Changes on Intraplate Faults in the Western Quebec Seismic Zone, Canada: Implications for Seismic Hazards","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; Western University; McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; McMaster University","keywords":"Intraplate earthquake; Seismology; Seismic hazard; Geology; Fault (geology); Stress field; Stress (linguistics); Coulomb; Seismic microzonation; Seismic risk; Tectonics; Structural engineering; Engineering; Finite element method; Physics","score_opus":0.04054652293092931,"score_gpt":0.2653469339439828,"score_spread":0.22480041101305348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320726353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952624,0.00021871571,0.0003314767,0.00025377562,0.0000035775574,0.00001032958,0.0008868391,0.000025293564,0.0030075791],"genre_scores_gemma":[0.99868935,0.00014796678,0.00017110106,0.000013510968,0.0000011332517,0.0000022416802,0.00022992524,0.0000025234456,0.00074224203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998915,0.000008395389,0.0000042831143,0.00001813537,0.00003144048,0.000046157693],"domain_scores_gemma":[0.9996909,0.00003695245,0.00006284283,0.000010025181,0.00013612374,0.00006330842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016564204,0.00030678048,0.00014980455,0.0011409905,0.0007970135,0.0010608318,0.000689674,0.00039894812,0.001825863],"category_scores_gemma":[0.00069592317,0.00010697494,0.00021026567,0.0014853737,0.0006135663,0.00030535474,0.00031212892,0.00024881036,0.0001049362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001609664,0.00007276771,0.8858412,0.00010578374,0.0000725594,0.00053390604,0.0009302744,0.05513092,0.0062119486,0.0018321483,0.0017575528,0.047350075],"study_design_scores_gemma":[0.0000071770296,0.00001853016,0.9652545,0.000023916338,0.000019783069,0.00004035161,0.0010821501,0.031873096,0.00042709918,0.0001710901,0.0010635366,0.00001880146],"about_ca_topic_score_codex":0.99260944,"about_ca_topic_score_gemma":0.99395543,"teacher_disagreement_score":0.020745186,"about_ca_system_score_codex":0.020745186,"about_ca_system_score_gemma":0.010753683,"threshold_uncertainty_score":0.15051758},"labels":[],"label_agreement":null},{"id":"W4320895070","doi":"10.1139/cjes-2022-0137","title":"Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; McMaster University","keywords":"Geology; Intraplate earthquake; Graben; Seismology; Tectonics; Induced seismicity; Seismic hazard; Tectonic uplift; Bedrock; Geomorphology; Post-glacial rebound; Escarpment; Structural basin; Half-graben; Glacial period","score_opus":0.040478294260731566,"score_gpt":0.23109273323384882,"score_spread":0.19061443897311725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320895070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99789304,0.0002255455,0.00008181644,0.00003122504,0.0000011048036,0.00001571328,0.0007092436,0.0000063831862,0.0010360429],"genre_scores_gemma":[0.9981184,0.00019227786,0.00029217245,0.000016216662,6.6390595e-7,0.000007631116,0.0004968144,0.000003315063,0.0008725637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979466,0.000007912317,0.000008387294,0.000041759908,0.000056427383,0.000091003414],"domain_scores_gemma":[0.9996729,0.00003200892,0.00006235338,0.000011796508,0.00013468754,0.00008636674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017135411,0.00033905267,0.0002205485,0.0018605589,0.0016181429,0.0010825539,0.00053291104,0.00020083385,0.0010994064],"category_scores_gemma":[0.00049873313,0.00020383977,0.00021470056,0.0030608564,0.0011420138,0.00024179697,0.0005120636,0.00019237968,0.00011464943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009148599,0.00001590824,0.9716185,0.000060277736,0.000039083152,0.00023564829,0.001974694,0.0010771652,0.0057459855,0.00032944803,0.0003231832,0.01848862],"study_design_scores_gemma":[9.573649e-7,0.0000042759884,0.99816895,0.0000068632085,0.000007134335,0.000025452755,0.0009543332,0.000260114,0.0001539905,0.000018119763,0.00039476005,0.000005064379],"about_ca_topic_score_codex":0.9922735,"about_ca_topic_score_gemma":0.99782443,"teacher_disagreement_score":0.017301043,"about_ca_system_score_codex":0.017301043,"about_ca_system_score_gemma":0.012901974,"threshold_uncertainty_score":0.12552845},"labels":[],"label_agreement":null},{"id":"W4320917779","doi":"10.1093/gji/ggad060","title":"Fault-based probabilistic seismic hazard analysis in regions with low strain rates and a thick seismogenic layer: a case study from Malawi","year":2023,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Engineering and Physical Sciences Research Council; University of Bristol","keywords":"Seismology; Geology; Seismic hazard; Fault (geology); Induced seismicity; Context (archaeology)","score_opus":0.023706118748093828,"score_gpt":0.26681481260689194,"score_spread":0.2431086938587981,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320917779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971917,0.00013488333,0.0013988086,0.00028280972,0.0000024261801,0.000034563887,0.00042324254,0.000014534442,0.000516966],"genre_scores_gemma":[0.99809724,0.00015620273,0.0011320345,0.00002564988,0.0000060666034,0.000013188677,0.00030476856,0.000006721358,0.000258085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994863,0.00022915084,0.000036080117,0.000051525883,0.00005410593,0.00014276156],"domain_scores_gemma":[0.99722856,0.0015573709,0.00051433494,0.00016535171,0.00032704035,0.00020726008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096479716,0.00046152357,0.00033431654,0.0016734765,0.0008015404,0.0012242286,0.0009098983,0.00067029457,0.001243593],"category_scores_gemma":[0.004714461,0.00031535362,0.00061967765,0.00236003,0.00077547634,0.00064419745,0.001284513,0.0006922883,0.00012477906],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002424715,0.00023562319,0.90011597,0.00025291072,0.00027480966,0.017504996,0.006580407,0.047290724,0.0020655538,0.0031156188,0.0011480263,0.021172835],"study_design_scores_gemma":[0.000051131894,0.00021196007,0.7921881,0.00020173512,0.00023376077,0.0045368224,0.02136291,0.17292412,0.0018250635,0.002324106,0.0040548807,0.00008544968],"about_ca_topic_score_codex":0.15599123,"about_ca_topic_score_gemma":0.17476885,"teacher_disagreement_score":0.15599123,"about_ca_system_score_codex":0.0021807733,"about_ca_system_score_gemma":0.0010619987,"threshold_uncertainty_score":0.31016654},"labels":[],"label_agreement":null},{"id":"W4321329740","doi":"10.1029/2022jb025344","title":"Stress Features Inferred From Induced Earthquakes in the Weiyuan Shale Gas Block in Southwestern China","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Seismology; Focal mechanism; Hydraulic fracturing; Stress field; Tectonics; Slip (aerodynamics); Shale gas; Stress (linguistics); Oil shale; Geotechnical engineering; Paleontology","score_opus":0.056071101433650065,"score_gpt":0.3287549339407007,"score_spread":0.27268383250705064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321329740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997521,0.000010856753,0.000048814152,0.0000053933877,5.753737e-7,0.0000016429902,0.00007803783,0.000004966433,0.00009759409],"genre_scores_gemma":[0.9997218,0.000010961614,0.000046298992,0.0000017689108,0.0000012982136,0.0000019607694,0.0001560786,7.797773e-7,0.00005905061],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999304,0.000005630739,0.000008811985,0.000016907503,0.000017217759,0.000021030635],"domain_scores_gemma":[0.99977416,0.000022175316,0.00006488193,0.000017875487,0.000054858796,0.00006619216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001390028,0.0002727825,0.00018365985,0.0012226233,0.00032412022,0.0002692154,0.00022413731,0.00022677012,0.00043688025],"category_scores_gemma":[0.00033371022,0.00015680329,0.00016592737,0.0010945101,0.00021341881,0.0001706105,0.0002932498,0.000095219315,0.00008095815],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007249757,0.000038012444,0.97564906,0.000030532094,0.000038239257,0.00046479198,0.00044967886,0.0028015058,0.011907364,0.000075536234,0.00017900471,0.008293917],"study_design_scores_gemma":[0.0000027785027,0.000011802629,0.99708587,0.0000018499746,0.0000074475533,0.000024069212,0.000107603584,0.0024560771,0.00022130807,0.000011214957,0.00006727434,0.0000026795365],"about_ca_topic_score_codex":0.041921254,"about_ca_topic_score_gemma":0.06436471,"teacher_disagreement_score":0.041921254,"about_ca_system_score_codex":0.00046961932,"about_ca_system_score_gemma":0.00044749843,"threshold_uncertainty_score":0.08335447},"labels":[],"label_agreement":null},{"id":"W4321452951","doi":"10.2139/ssrn.4357076","title":"Can a Tidal Wave Provoke and Intensify an Earthquake? (¿Puede un maremoto provocar e intensificar un terremoto? Могут ли цунами вызывать и усиливать землетрясения? 潮汐能引发和加剧地震吗？ 津波は地震を引き起こし、激化させることができますか?)","year":2023,"lang":"ru","type":"article","venue":"SSRN Electronic Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Seismology; Geology; Environmental science","score_opus":0.019326374492198806,"score_gpt":0.21890857351793566,"score_spread":0.19958219902573685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321452951","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7276532,0.03421008,0.0019139401,0.10030593,0.0038141333,0.00008444482,0.00067277113,0.00005396454,0.1312916],"genre_scores_gemma":[0.96380335,0.01743664,0.0005564694,0.0072661126,0.0034768675,0.000029402465,0.00017696817,0.000015973133,0.007238213],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99984217,0.00005507767,0.000013824536,0.000025203799,0.000035161876,0.000028539795],"domain_scores_gemma":[0.9991054,0.00051477243,0.0002026093,0.00004825233,0.00006702687,0.00006190913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008419052,0.00015165383,0.00016734099,0.0004729002,0.0005034598,0.00136759,0.00023139635,0.0017283494,0.005641133],"category_scores_gemma":[0.004482997,0.00016191916,0.00019118086,0.0006904181,0.0018922682,0.0015642473,0.0006737024,0.0005606325,0.00069301506],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015758255,0.00056971743,0.41132873,0.0017576672,0.00042719132,0.013707563,0.04790179,0.0009170039,0.009745864,0.17329922,0.066793166,0.27197626],"study_design_scores_gemma":[0.00009534962,0.00042250293,0.7871235,0.0005122654,0.00017642727,0.006167323,0.036843125,0.0003030673,0.00069480255,0.06608526,0.1015235,0.000052904357],"about_ca_topic_score_codex":0.0015687541,"about_ca_topic_score_gemma":0.0041823233,"teacher_disagreement_score":0.005641133,"about_ca_system_score_codex":0.00036644106,"about_ca_system_score_gemma":0.00032868766,"threshold_uncertainty_score":0.018871486},"labels":[],"label_agreement":null},{"id":"W4321489942","doi":"10.5194/egusphere-egu23-4047","title":"Drilling and monitoring in Hyuga-Nada: Unveiling effects of ridge subduction on slow earthquakes","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Seamount; Subduction; Seismology; Drilling; Paleontology; Tectonics","score_opus":0.03318808710866707,"score_gpt":0.23958811099844246,"score_spread":0.20640002388977538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321489942","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99306643,0.00026464977,0.0028259316,0.00012920343,0.000029101855,0.00008202792,0.0013078618,0.000085190266,0.0022096306],"genre_scores_gemma":[0.9768152,0.000305614,0.01944135,0.00008121167,0.000022309432,0.000080294994,0.0019288443,0.000014616448,0.0013105256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984217,0.000024860092,0.000011364295,0.000037464655,0.000046284084,0.000037882062],"domain_scores_gemma":[0.9996675,0.000020780139,0.000045001634,0.00003084937,0.00014885982,0.00008694343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003371348,0.00034737264,0.00019267449,0.0008318864,0.00042910947,0.00040290272,0.00040420724,0.00035229351,0.00036336432],"category_scores_gemma":[0.00036353306,0.00019362499,0.00019124502,0.0008587308,0.00021230032,0.00028721968,0.0005467226,0.00027207003,0.00014887567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018485835,0.00019792217,0.8638224,0.00016332201,0.00006227779,0.0010430447,0.0018489064,0.0020745983,0.058287263,0.00022855953,0.0017987202,0.070288084],"study_design_scores_gemma":[0.000015536214,0.000120533805,0.9834683,0.000020400692,0.000049213162,0.00015297091,0.001777672,0.008048778,0.0030374746,0.000056607394,0.0032282295,0.000024211498],"about_ca_topic_score_codex":0.07932993,"about_ca_topic_score_gemma":0.23788491,"teacher_disagreement_score":0.07932993,"about_ca_system_score_codex":0.00030061693,"about_ca_system_score_gemma":0.0007938297,"threshold_uncertainty_score":0.15773636},"labels":[],"label_agreement":null},{"id":"W4321490754","doi":"10.5194/egusphere-egu23-3007","title":"Complex postseismic vertical motion following megathrust earthquakes explained by simple mechanisms","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Geology; Forearc; Seismology; Subduction; Trench; Viscoelasticity; Slip (aerodynamics); Volcanic arc; Deformation (meteorology); Geodesy; Tectonics","score_opus":0.047118913162289326,"score_gpt":0.2552812734547775,"score_spread":0.2081623602924882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321490754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9853778,0.00020693132,0.011581927,0.00008133719,0.000022044882,0.000019562001,0.00015165315,0.00008985545,0.0024687333],"genre_scores_gemma":[0.9988366,0.00009894626,0.00048781242,0.0000059084496,0.000006937961,0.0000059515824,0.00005192229,0.000009884784,0.00049605797],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994636,0.00000761509,0.0000051193747,0.000017553659,0.000006838065,0.000016533457],"domain_scores_gemma":[0.99989927,0.000011301759,0.00004799861,0.000014784872,0.000009407682,0.00001723125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000117571806,0.00052992126,0.00027577823,0.00031155124,0.00018275026,0.0005160435,0.00051029463,0.0005865697,0.0010529817],"category_scores_gemma":[0.0003049079,0.00025328313,0.0006100217,0.00029511465,0.0004936118,0.00053316966,0.00043907482,0.0001847458,0.00013808032],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015688245,0.000116464,0.09186231,0.00012249916,0.00020285376,0.0017131618,0.00035649576,0.84226906,0.038184904,0.013772051,0.00043194857,0.010811436],"study_design_scores_gemma":[0.000027110256,0.00008632531,0.08979675,0.000011415057,0.000037555965,0.00015116663,0.00007037481,0.9056364,0.000834698,0.0029422168,0.00038126783,0.000024659086],"about_ca_topic_score_codex":0.0059341826,"about_ca_topic_score_gemma":0.0026382743,"teacher_disagreement_score":0.0059341826,"about_ca_system_score_codex":0.00032967277,"about_ca_system_score_gemma":0.00026069375,"threshold_uncertainty_score":0.011799276},"labels":[],"label_agreement":null},{"id":"W4321490966","doi":"10.5194/egusphere-egu23-2618","title":"Propagation of a fluid-induced aseismic crack leads to earthquake swarm migration controlled by fluid volume","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Induced seismicity; Geology; Seismic moment; Slip (aerodynamics); Fluid pressure; Seismology; Fluid dynamics; Hydraulic fracturing; Geothermal gradient; Fault (geology); Mechanics; Geotechnical engineering; Geophysics; Physics; Thermodynamics","score_opus":0.028682129780141608,"score_gpt":0.24570893616999828,"score_spread":0.21702680638985666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321490966","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98739713,0.0000620308,0.010473853,0.000055082844,0.000007986973,0.00000588144,0.000036477566,0.0000858119,0.0018757599],"genre_scores_gemma":[0.9992766,0.000023213728,0.0003791028,0.000003426589,0.0000016291648,0.0000019008379,0.000010439255,0.000003964623,0.0002996647],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996734,0.0000040081773,0.0000021029114,0.000010210135,0.000007054039,0.000009264263],"domain_scores_gemma":[0.9998242,0.000041566847,0.000079822916,0.000008742566,0.000017706543,0.00002792173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006202701,0.00016608408,0.00014751684,0.00021503326,0.0001352444,0.00033787472,0.00023230864,0.0002610646,0.0012151164],"category_scores_gemma":[0.00035436708,0.00012755893,0.00018416383,0.000095896256,0.00035935274,0.00016363563,0.0002603626,0.00021208366,0.00011825024],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004692766,0.00027169968,0.037618324,0.0001565765,0.00007424305,0.0029389625,0.00048240964,0.30578122,0.60985357,0.016807176,0.0010780221,0.024468599],"study_design_scores_gemma":[0.000019193976,0.00014489196,0.019042412,0.000009239315,0.000018604469,0.00020317252,0.00008717557,0.9613589,0.017180013,0.0015292664,0.00039258142,0.000014642364],"about_ca_topic_score_codex":0.0022344177,"about_ca_topic_score_gemma":0.0011817574,"teacher_disagreement_score":0.0022344177,"about_ca_system_score_codex":0.00031713487,"about_ca_system_score_gemma":0.00016173306,"threshold_uncertainty_score":0.004442811},"labels":[],"label_agreement":null},{"id":"W4321495407","doi":"10.5194/egusphere-egu23-1726","title":"Stochastic Source Modelling of the 2002 Denali Earthquake for Fault Displacement Hazard Assessment","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Displacement (psychology); Fault (geology); Seismology; Slip (aerodynamics); Seismic hazard; Geology; Geodesy; Engineering","score_opus":0.07498483645973646,"score_gpt":0.27776218822865695,"score_spread":0.20277735176892048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321495407","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.40402272,0.00067050784,0.57827395,0.00050138036,0.00008092973,0.000081679515,0.0010004344,0.0004941601,0.014874221],"genre_scores_gemma":[0.98585284,0.00023666184,0.010557951,0.000019518922,0.000018473767,0.00004476337,0.00032709268,0.000034096192,0.0029085635],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999021,0.00002930975,0.0000082710585,0.000018867628,0.000027567121,0.000013938305],"domain_scores_gemma":[0.9997615,0.00012243936,0.00004049974,0.000011848881,0.000051307074,0.000012374996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022713929,0.000424303,0.00032689015,0.0003975099,0.0002275008,0.0006245227,0.00061490136,0.0006233782,0.0011413482],"category_scores_gemma":[0.0009892927,0.00024429825,0.00045563545,0.00036213463,0.00020040461,0.00039359622,0.000548272,0.00039369677,0.00018260238],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015717173,0.000010579337,0.0009732359,0.000012263177,0.000010543309,0.000043677883,0.000025287789,0.9918235,0.0007753976,0.0035973452,0.00018004393,0.002532468],"study_design_scores_gemma":[0.0000014013825,0.000002391825,0.00016422226,8.517318e-7,0.000001952821,0.000003680606,0.0000032952678,0.9993012,0.0000777898,0.0003266367,0.00011477701,0.0000017111722],"about_ca_topic_score_codex":0.02249468,"about_ca_topic_score_gemma":0.015286037,"teacher_disagreement_score":0.02249468,"about_ca_system_score_codex":0.0005199817,"about_ca_system_score_gemma":0.0005355028,"threshold_uncertainty_score":0.044727504},"labels":[],"label_agreement":null},{"id":"W4321502107","doi":"10.5194/egusphere-egu23-4598","title":"Long-term Fluid Injection Can Expedite Fault Development: Riedel Shear Structures Illuminated by Induced Earthquakes in Alberta, Canada","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Geological Survey of Canada","funders":"","keywords":"RSS; Geology; Seismology; Shear (geology); Slip (aerodynamics); Fault (geology); Computer science; Engineering; Petrology","score_opus":0.02291091578216846,"score_gpt":0.22810131434801115,"score_spread":0.2051903985658427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321502107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864476,0.0005650223,0.00022465928,0.00096898864,0.000017567214,0.000027053698,0.0010388704,0.00003446941,0.0106758345],"genre_scores_gemma":[0.9935167,0.00053497404,0.0004118836,0.00012460502,0.0000072886683,0.0000057191137,0.00052422215,0.000009487305,0.0048651244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997476,0.000013549207,0.00000824286,0.000025374813,0.000085935586,0.00011930576],"domain_scores_gemma":[0.9995758,0.000031176325,0.000056284713,0.0000115187395,0.00019077989,0.00013451003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001993317,0.00022116848,0.00019253952,0.0011579583,0.002670089,0.0013266406,0.0008496738,0.0005872303,0.0022980901],"category_scores_gemma":[0.00051012466,0.00019739721,0.00018984318,0.002265834,0.00119985,0.00024864936,0.0008552966,0.00046280227,0.00018653463],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003090946,0.00014672524,0.89526254,0.00022831213,0.00012322732,0.007459542,0.019109648,0.0032627024,0.007713096,0.002971359,0.010134726,0.053279083],"study_design_scores_gemma":[0.000010081095,0.00002227941,0.96867305,0.00005186851,0.000025730506,0.00022394069,0.019640775,0.0010959823,0.00027943775,0.00016166802,0.00978387,0.000031346935],"about_ca_topic_score_codex":0.99432665,"about_ca_topic_score_gemma":0.9988649,"teacher_disagreement_score":0.0262603,"about_ca_system_score_codex":0.0262603,"about_ca_system_score_gemma":0.031571154,"threshold_uncertainty_score":0.19053274},"labels":[],"label_agreement":null},{"id":"W4321649613","doi":"","title":"Fluid Evolution During Mineralization of Atashkuh Fluorite-Barite (±Sulfide) Deposit, South of Delijan","year":2016,"lang":"en","type":"article","venue":"DOAJ (DOAJ: Directory of Open Access Journals)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Fluorite; Mineralization (soil science); Geochemistry; Sulfide; Geology; Mineralogy; Metallurgy; Materials science; Soil science","score_opus":0.12069703169929356,"score_gpt":0.4267630401765371,"score_spread":0.3060660084772435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321649613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99889416,0.00019318819,0.000059168735,0.00000850581,0.000004969938,0.000005647716,0.00017781889,0.000007853792,0.00064879307],"genre_scores_gemma":[0.9988279,0.00014081672,0.00027941284,0.000009441693,0.00000477436,0.0000056373437,0.00020170929,0.0000046454206,0.0005256926],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99988604,0.0000048603765,0.000008563499,0.00004176707,0.000032126216,0.00002655525],"domain_scores_gemma":[0.9999449,0.0000052409546,0.000016304215,0.0000021830615,0.000022724911,0.000008578201],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013698619,0.00030183574,0.00029651573,0.001250219,0.0006150716,0.00064778584,0.00028902278,0.0002714715,0.00073345157],"category_scores_gemma":[0.00014632562,0.00023822873,0.00020186769,0.000517787,0.0003781466,0.00029666166,0.00035616587,0.00018826302,0.00014278296],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004761994,0.000083683866,0.39669743,0.00032694516,0.00008242623,0.0016235705,0.0022981854,0.000521712,0.5829532,0.00018752745,0.00027882017,0.0144703295],"study_design_scores_gemma":[0.000010071212,0.000097045886,0.97897947,0.000017884733,0.000028264787,0.00043321983,0.001036473,0.0005397949,0.017151564,0.000036826877,0.0016593327,0.00001002271],"about_ca_topic_score_codex":0.026052464,"about_ca_topic_score_gemma":0.049513508,"teacher_disagreement_score":0.026052464,"about_ca_system_score_codex":0.0006050792,"about_ca_system_score_gemma":0.00047576855,"threshold_uncertainty_score":0.05180168},"labels":[],"label_agreement":null},{"id":"W4321763698","doi":"10.1093/gji/ggad086","title":"Tackling the challenges of tectonic tremor localization using differential traveltimes and Bayesian inversion","year":2023,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Met Office","keywords":"Geology; Seismology; Tectonics; Geodesy; Bayesian probability; Inversion (geology); Epicenter; Statistics; Mathematics","score_opus":0.025652573085907994,"score_gpt":0.24638248713447916,"score_spread":0.22072991404857117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321763698","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1461703,0.000106892614,0.85224676,0.00025940954,0.000006796915,0.000017979924,0.00014799145,0.00034363722,0.00070013996],"genre_scores_gemma":[0.82717735,0.00009727929,0.17172658,0.000042130992,0.000028022983,0.000035670484,0.00035033937,0.00010811773,0.0004345745],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991466,0.0003547271,0.000060561426,0.0001598615,0.00021551656,0.00006285596],"domain_scores_gemma":[0.9915074,0.0061808196,0.00086854177,0.0005131111,0.0007782225,0.0001519639],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031021822,0.0005567229,0.00055138784,0.0011208882,0.00037146333,0.0012307445,0.0011066726,0.0006017723,0.000469961],"category_scores_gemma":[0.018118035,0.00064113986,0.00045572472,0.0009849914,0.0007795774,0.0010632048,0.0012369237,0.001128015,0.00014006681],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035563306,0.000014099598,0.008549715,0.00002715152,0.00005387359,0.000049920814,0.00007944018,0.9608259,0.0013989534,0.0046688607,0.0001999037,0.024096608],"study_design_scores_gemma":[0.0000051984557,0.0000048784977,0.0014951292,0.0000036566075,0.0000037727816,0.000009828406,0.000016609187,0.99415743,0.00033752143,0.0038347025,0.0001242238,0.0000070174433],"about_ca_topic_score_codex":0.08594274,"about_ca_topic_score_gemma":0.06825226,"teacher_disagreement_score":0.08594274,"about_ca_system_score_codex":0.0013731453,"about_ca_system_score_gemma":0.0021100873,"threshold_uncertainty_score":0.17088503},"labels":[],"label_agreement":null},{"id":"W4321995300","doi":"10.5194/egusphere-egu23-9724","title":"A new algorithm to separate meteor trail echoes from ionospheric radar scatter","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Saskatchewan","funders":"","keywords":"Radar; Ionosphere; Meteoroid; Meteor (satellite); Incoherent scatter; Remote sensing; Geology; Algorithm; Computer science; Geophysics; Meteorology; Physics; Telecommunications; Astronomy","score_opus":0.035535818412969815,"score_gpt":0.25002931274680573,"score_spread":0.2144934943338359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321995300","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008441606,0.0001764037,0.98739076,0.000110970635,0.00012930314,0.00014747813,0.00030174066,0.0025921531,0.0007095628],"genre_scores_gemma":[0.02424085,0.00009515526,0.9712129,0.00010949629,0.00006349603,0.00018698917,0.0012660137,0.00023154802,0.002593497],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9986382,0.0000882693,0.00014116641,0.00052899006,0.00047707165,0.00012635361],"domain_scores_gemma":[0.99831486,0.0003502984,0.00014903853,0.0002812431,0.0008147514,0.00008984854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010000322,0.0012786662,0.001364195,0.0026355505,0.0011533402,0.0023950862,0.0022179352,0.001608919,0.0031551083],"category_scores_gemma":[0.0031624895,0.00067415193,0.0011728599,0.0032866378,0.0006579778,0.0020542333,0.0016586937,0.0015717795,0.0031523367],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002985518,0.00019785303,0.0032090212,0.00013918163,0.00013066741,0.00007889799,0.00014646817,0.02632524,0.02318799,0.0034878203,0.011944362,0.930854],"study_design_scores_gemma":[0.0002013862,0.00017613794,0.0032687192,0.000039850765,0.00007111013,0.00047380285,0.00016406093,0.93517816,0.021266079,0.010264918,0.028828438,0.00006728874],"about_ca_topic_score_codex":0.008155014,"about_ca_topic_score_gemma":0.010642701,"teacher_disagreement_score":0.008155014,"about_ca_system_score_codex":0.0007488246,"about_ca_system_score_gemma":0.0023301335,"threshold_uncertainty_score":0.016215086},"labels":[],"label_agreement":null},{"id":"W4321995869","doi":"10.5194/egusphere-egu23-10392","title":"Subsurface evidence for potentially seismogenic structures in the offshore Grand Banks region of Newfoundland, eastern Canada: present-day reactivation of inherited passive margin structures","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; McMaster University","funders":"","keywords":"Submarine pipeline; Seismology; Geology; Fault (geology); Active fault; Tectonics; Passive margin; Margin (machine learning); Seismic hazard; Continental margin; Neotectonics; Seismic risk; Oceanography","score_opus":0.0738228157365445,"score_gpt":0.27035951994749663,"score_spread":0.19653670421095212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321995869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968284,0.0001310001,0.00011727575,0.000079020465,0.0000017456696,0.0000058657174,0.0004615762,0.000009805557,0.002365324],"genre_scores_gemma":[0.99879456,0.00013123648,0.00017770303,0.000018382863,0.0000010711545,0.00000243827,0.00024455055,0.0000020073442,0.0006281105],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999105,0.000003756505,0.0000048070997,0.000017859622,0.000021921564,0.000041165113],"domain_scores_gemma":[0.9997209,0.000025363392,0.00007918493,0.000015389971,0.00011055877,0.00004866881],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009033025,0.00018846597,0.00010250208,0.0010233993,0.00079127925,0.0008245823,0.00033956324,0.0002828465,0.0012458373],"category_scores_gemma":[0.0003932926,0.00016713257,0.000076186196,0.00124687,0.0007878904,0.000258779,0.0005352933,0.0002352668,0.00016915878],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074291704,0.000031331307,0.9572317,0.00007926946,0.000029046003,0.0010080015,0.0023340543,0.0010621528,0.016100615,0.0002599386,0.00089290057,0.020896707],"study_design_scores_gemma":[0.000002149015,0.0000048526117,0.9971269,0.000012270523,0.0000071054824,0.000071539376,0.0016675671,0.00032732805,0.00031018947,0.000015403519,0.00045087558,0.0000038877356],"about_ca_topic_score_codex":0.9299985,"about_ca_topic_score_gemma":0.9787683,"teacher_disagreement_score":0.07000148,"about_ca_system_score_codex":0.0032173418,"about_ca_system_score_gemma":0.0034196689,"threshold_uncertainty_score":0.14082742},"labels":[],"label_agreement":null},{"id":"W4321996076","doi":"10.5194/egusphere-egu23-10831","title":"Do the statistical properties of aftershocks change in fluid-induced settings?","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Geology; Aftershock; Tectonics; Seismology; Geothermal gradient; Context (archaeology); Hydraulic fracturing; Geomechanics; Viscoelasticity; Geotechnical engineering; Geophysics; Physics","score_opus":0.11642566551408987,"score_gpt":0.27439700353609525,"score_spread":0.1579713380220054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321996076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9743997,0.00023142218,0.02185508,0.00085772795,0.000025912952,0.000024530495,0.00045852805,0.00016495869,0.001982127],"genre_scores_gemma":[0.9990546,0.0001144322,0.00042377406,0.00003403166,0.000020462378,0.0000074526283,0.00013232329,0.000016273349,0.00019665994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996898,0.0000651666,0.000022066579,0.00012270316,0.000031838394,0.00006841891],"domain_scores_gemma":[0.99494547,0.001688336,0.0020663585,0.00060317165,0.00027942224,0.00041719104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010960439,0.0002582136,0.00054379355,0.001178718,0.00026153744,0.0013702465,0.00090386055,0.001231047,0.0016995295],"category_scores_gemma":[0.010108277,0.00036828968,0.00055239967,0.0007368652,0.0016390044,0.0028735974,0.0005787097,0.0006294825,0.00030309244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044001607,0.00039019602,0.5419359,0.00034218747,0.0006017221,0.0017613891,0.0015587952,0.3042109,0.024654334,0.077623025,0.003055207,0.043426286],"study_design_scores_gemma":[0.000035585846,0.00019072155,0.36971095,0.000035793917,0.00007694582,0.0003863454,0.0006246667,0.5543469,0.0023414346,0.07050839,0.0016242599,0.0001179166],"about_ca_topic_score_codex":0.0034337412,"about_ca_topic_score_gemma":0.0023745403,"teacher_disagreement_score":0.0034337412,"about_ca_system_score_codex":0.00060183933,"about_ca_system_score_gemma":0.00028069064,"threshold_uncertainty_score":0.0068274736},"labels":[],"label_agreement":null},{"id":"W4321996157","doi":"10.5194/egusphere-egu23-10817","title":"Microstructural investigations along a blueschist facies paleomegathrust: Implications for deformation mechanisms for deep slow slip behavior","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Blueschist; Geology; Subduction; Shear zone; Lithology; Mylonite; Shear (geology); Petrology; Geochemistry; Metamorphic rock; Cataclastic rock; Seismology; Deformation mechanism; Metamorphic facies; Facies; Tectonics; Geomorphology; Eclogite","score_opus":0.05599117616426746,"score_gpt":0.2700261193599696,"score_spread":0.21403494319570215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321996157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988275,0.0000614545,0.00011614334,0.000012795649,6.0924066e-7,0.000005437824,0.0001340546,0.000006672843,0.000835441],"genre_scores_gemma":[0.9992487,0.00005497468,0.00023031436,0.000004873416,0.0000014247996,0.0000032229382,0.000084267864,0.0000021203227,0.00037009784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994767,0.0000018378995,0.0000029969212,0.000016792817,0.00001684604,0.000013919797],"domain_scores_gemma":[0.9999088,0.000009329932,0.00003085099,0.0000062882164,0.000029929448,0.000014749947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006328482,0.00018479813,0.00009336042,0.0015295233,0.00038912895,0.0003454763,0.00024551293,0.00024701987,0.0014776826],"category_scores_gemma":[0.00015737818,0.00015346754,0.00008698669,0.0007205122,0.0004667909,0.00019067932,0.00026451083,0.00014070117,0.00014906842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013916283,0.000039718787,0.72797203,0.000095695206,0.00004521244,0.0011609904,0.0017377231,0.0014877651,0.24600811,0.00034598453,0.00017543546,0.020792201],"study_design_scores_gemma":[0.0000010263984,0.000013003379,0.99726295,0.0000031751056,0.0000045744982,0.00012472802,0.00031236815,0.00038893623,0.0016569911,0.000012277395,0.00021799449,0.0000018956855],"about_ca_topic_score_codex":0.06383702,"about_ca_topic_score_gemma":0.15495315,"teacher_disagreement_score":0.06383702,"about_ca_system_score_codex":0.00051265233,"about_ca_system_score_gemma":0.00027464182,"threshold_uncertainty_score":0.12693089},"labels":[],"label_agreement":null},{"id":"W4321996411","doi":"10.5194/egusphere-egu23-11035","title":"Interdependent effects of injection volume and rate on fault slip behavior: A large-scale numerical study","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Optech (Canada); University of Toronto","funders":"","keywords":"Induced seismicity; Injection well; Slip (aerodynamics); Context (archaeology); Mechanics; Geology; Injection site; Seismology; Environmental science; Petroleum engineering; Geotechnical engineering; Engineering; Thermodynamics; Physics","score_opus":0.019479769814263487,"score_gpt":0.25880143810253353,"score_spread":0.23932166828827003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321996411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99520665,0.00013818193,0.0029046761,0.0001369827,0.000015860587,0.000025138965,0.00015743518,0.00006912883,0.0013457966],"genre_scores_gemma":[0.99827874,0.000054204957,0.0014421995,0.000017625704,0.0000047867356,0.000011682611,0.000066752575,0.000010117036,0.000113930466],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99978346,0.000057516958,0.000022993741,0.000042019026,0.00003821172,0.000055765104],"domain_scores_gemma":[0.99749607,0.0016269928,0.0004226506,0.0001565174,0.00017756222,0.00012021166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000581257,0.0005378508,0.00067298237,0.0007986139,0.0005470591,0.0008928686,0.00082777033,0.0013971139,0.0009261038],"category_scores_gemma":[0.0028700419,0.00034153965,0.0007772956,0.00066634564,0.0009335624,0.0008383244,0.0005927427,0.00083402946,0.000076212214],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000103399005,0.0003346698,0.031975675,0.000073260126,0.00008503424,0.00034171465,0.00006662185,0.95684296,0.0064664115,0.0007826079,0.00023149911,0.0026961553],"study_design_scores_gemma":[0.000019101008,0.00007037716,0.003987322,0.0000066792177,0.00002273906,0.000025247473,0.000059627637,0.9940601,0.0014572735,0.00015262244,0.00012505613,0.000013852508],"about_ca_topic_score_codex":0.014282035,"about_ca_topic_score_gemma":0.007966407,"teacher_disagreement_score":0.014282035,"about_ca_system_score_codex":0.0007572612,"about_ca_system_score_gemma":0.0006589699,"threshold_uncertainty_score":0.028397858},"labels":[],"label_agreement":null},{"id":"W4322005249","doi":"10.5194/egusphere-egu23-7653","title":"Earthquake relocations and three-dimensional VP, VS and VP/VS along the fast-slipping Gofar oceanic transform fault, East Pacific Rise.","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Transform fault; Induced seismicity; Slipping; Fault (geology); Ridge; Oceanic crust; Crust; Geophysics; Subduction; Tectonics; Geometry","score_opus":0.02882678638270148,"score_gpt":0.22423231691974235,"score_spread":0.19540553053704088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322005249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99863017,0.000016366395,0.00052292395,0.000016162709,0.000002390766,0.0000038528287,0.00041799815,0.000056278892,0.00033398293],"genre_scores_gemma":[0.9986506,0.0000107268625,0.00045566584,0.0000026650364,0.000001027368,0.0000027254846,0.00072352414,0.00000792962,0.00014506781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999697,0.0000030443457,0.000001880295,0.00001232893,0.000004686376,0.000008402117],"domain_scores_gemma":[0.9998939,0.000018442855,0.00003816892,0.000009905217,0.000015111722,0.000024431347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000073661904,0.00028427038,0.00010184637,0.0005049555,0.0001479929,0.00035022633,0.00030406463,0.00033742998,0.00089597417],"category_scores_gemma":[0.00043080916,0.00020350961,0.00026738746,0.0005463799,0.00020915791,0.00022236547,0.00022452296,0.0003435562,0.00015855167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030158792,0.00027371585,0.73035157,0.00006110199,0.00016704842,0.0005734565,0.00077573943,0.21014197,0.023723725,0.0011460423,0.0015084667,0.03097553],"study_design_scores_gemma":[0.000024277695,0.000052217452,0.69961566,0.000011656845,0.000026811982,0.00012388965,0.00031066826,0.29763493,0.0013227947,0.0002635833,0.0005848264,0.000028703924],"about_ca_topic_score_codex":0.040040165,"about_ca_topic_score_gemma":0.048980527,"teacher_disagreement_score":0.040040165,"about_ca_system_score_codex":0.0002841062,"about_ca_system_score_gemma":0.00029987068,"threshold_uncertainty_score":0.07961422},"labels":[],"label_agreement":null},{"id":"W4322006125","doi":"10.5194/egusphere-egu23-7207","title":"Deciphering earthquake source observations to motivate questions for physics-based models of earthquake simulation","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Intraplate earthquake; Seismology; Geology; Interplate earthquake; Drop (telecommunication); Fault (geology); Subduction; Volcano; Tectonics; Engineering","score_opus":0.12793880762284943,"score_gpt":0.2919474345328277,"score_spread":0.16400862690997825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322006125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6572488,0.00069534883,0.32198352,0.0030875406,0.000095105606,0.00007896873,0.0028308176,0.0013354078,0.012644536],"genre_scores_gemma":[0.9732506,0.00037919686,0.024798948,0.00010629434,0.000055659497,0.00003787108,0.00069530035,0.00014897854,0.0005270954],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9998857,0.000033422,0.000009376403,0.00003982568,0.00001777263,0.00001384448],"domain_scores_gemma":[0.99884725,0.000582923,0.00018304103,0.0002508071,0.00007809742,0.0000578374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005681371,0.00036633227,0.00042271634,0.000710451,0.0002715419,0.0010090898,0.0007603231,0.00067201775,0.0018142038],"category_scores_gemma":[0.005666154,0.00033192703,0.00032224323,0.00070211117,0.00063060876,0.0022006144,0.0010273879,0.00077737856,0.0002800817],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000878152,0.00012255817,0.06831669,0.00015292299,0.00010075343,0.0002685449,0.00077067915,0.81669855,0.009519759,0.06698255,0.0024536096,0.034525674],"study_design_scores_gemma":[0.000011418534,0.000011532964,0.016507588,0.000023615794,0.000007773876,0.000031071253,0.00013263246,0.9569737,0.000564088,0.024300704,0.0014225931,0.000013343878],"about_ca_topic_score_codex":0.008013776,"about_ca_topic_score_gemma":0.0061191143,"teacher_disagreement_score":0.008013776,"about_ca_system_score_codex":0.000657985,"about_ca_system_score_gemma":0.0003669929,"threshold_uncertainty_score":0.015934289},"labels":[],"label_agreement":null},{"id":"W4322212432","doi":"10.5194/egusphere-egu23-15559","title":"Aseismic rupture on rate-weakening faults before slip instability","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Slip (aerodynamics); Instability; Nucleation; Mechanics; Fault (geology); Dislocation; Materials science; Shear (geology); Geology; Seismology; Physics; Composite material; Thermodynamics","score_opus":0.040694758594000666,"score_gpt":0.25279343737750126,"score_spread":0.21209867878350058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322212432","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99120915,0.000042017044,0.0027922096,0.00006032927,0.000010651674,0.000015462365,0.00007841624,0.000049312715,0.0057425317],"genre_scores_gemma":[0.99904126,0.00002693217,0.00033128954,0.000012097006,0.0000017341113,0.000010106328,0.000036164583,0.000006626154,0.00053384015],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9999225,0.000010055044,0.000003886189,0.000015214016,0.000017182518,0.00003109175],"domain_scores_gemma":[0.9998567,0.000042724667,0.000027516542,0.000022210144,0.000016703607,0.000034142562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000112648195,0.00027048457,0.00032297644,0.00024106588,0.00027148286,0.00068798,0.0005150722,0.0006272236,0.0030408693],"category_scores_gemma":[0.0007842287,0.00015306185,0.00038599755,0.00016977184,0.0006923249,0.0005532715,0.0006308901,0.00054448744,0.0001704882],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041663132,0.00019796536,0.01187123,0.00010611177,0.00005111971,0.0008633168,0.0003171448,0.9123163,0.050450165,0.015259906,0.00056765025,0.0075824475],"study_design_scores_gemma":[0.00009899374,0.00037646474,0.011186074,0.000018943188,0.000026915382,0.00014570077,0.00019827705,0.97440976,0.0089762155,0.0034270757,0.0011065531,0.00002897635],"about_ca_topic_score_codex":0.0037071593,"about_ca_topic_score_gemma":0.0021061772,"teacher_disagreement_score":0.0037071593,"about_ca_system_score_codex":0.00043476184,"about_ca_system_score_gemma":0.00039158834,"threshold_uncertainty_score":0.010172784},"labels":[],"label_agreement":null},{"id":"W4322735239","doi":"10.1029/2022jb024985","title":"Complex 3‐D Surface Deformation in the 1971 San Fernando, California Earthquake Reveals Static and Dynamic Controls on Off‐Fault Deformation","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Canada Foundation for Innovation; Natural Sciences and Engineering Research Council of Canada; Centre National d’Etudes Spatiales; Southern California Earthquake Center","keywords":"Fault trace; Geology; Slip (aerodynamics); Seismology; Thrust fault; Fault (geology); Strike-slip tectonics; Geodesy; Thrust; Rake angle; Rake; Deformation (meteorology); Geometry; Geomorphology; Materials science; Engineering","score_opus":0.05692740955110933,"score_gpt":0.3371822339417742,"score_spread":0.2802548243906649,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322735239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887675,0.000014722615,0.000048511178,0.000012613315,0.0000012971249,0.0000016716949,0.00028354788,0.000011828192,0.0007489377],"genre_scores_gemma":[0.9994772,0.000015512973,0.00005741101,0.00000293743,0.0000014521889,0.0000011960609,0.00029330185,0.0000035543956,0.00014736713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996424,0.0000021594235,0.0000012979019,0.000009592631,0.000009769037,0.000012909636],"domain_scores_gemma":[0.9999205,0.00001291135,0.000021045757,0.000007775308,0.000016768134,0.0000209452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000061257546,0.00015945711,0.000158961,0.0006448332,0.00031305692,0.0003844117,0.00012168139,0.00022197654,0.0010869561],"category_scores_gemma":[0.00027757883,0.0001519494,0.00015017139,0.000661045,0.00023096321,0.0001800213,0.00021901082,0.00017233641,0.00016479874],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006101747,0.00017620473,0.91015506,0.00004226615,0.00005980428,0.00087554706,0.0007289903,0.018877063,0.03755086,0.00028360393,0.0022025467,0.02843792],"study_design_scores_gemma":[0.000002375858,0.0000052038267,0.9981493,0.0000010568021,0.0000018787343,0.000013821558,0.000056846082,0.0015352301,0.00013067824,0.000011627403,0.00008965073,0.000002388159],"about_ca_topic_score_codex":0.08890343,"about_ca_topic_score_gemma":0.1393742,"teacher_disagreement_score":0.08890343,"about_ca_system_score_codex":0.0006974476,"about_ca_system_score_gemma":0.00026064552,"threshold_uncertainty_score":0.17677188},"labels":[],"label_agreement":null},{"id":"W4322743936","doi":"10.46717/igj.56.1b.15ms-2023-2-23","title":"Relocation and Magnitude for Earthquakes in the Outer Arabian Platform of Iraq","year":2023,"lang":"en","type":"article","venue":"Iraqi Geological Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; Saint Louis University","keywords":"Magnitude (astronomy); Seismology; Geology; Mesopotamia; Relocation; Earthquake magnitude; Induced seismicity; Geography; Archaeology; Geometry","score_opus":0.0560003846224981,"score_gpt":0.26312961782945304,"score_spread":0.20712923320695495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322743936","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98951167,0.00026640025,0.00086371566,0.00008915482,0.000016039703,0.000023712291,0.007735293,0.00004632142,0.001447673],"genre_scores_gemma":[0.98565453,0.00017581714,0.0012810166,0.000018539582,0.0000141333085,0.00002490428,0.012209024,0.000009871787,0.000612197],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997675,0.000032027183,0.000024401947,0.00007151081,0.000053562704,0.00005101804],"domain_scores_gemma":[0.9995427,0.000058437843,0.00019384493,0.00004261608,0.0001291527,0.000033246397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031845007,0.000243094,0.00016975663,0.0021052454,0.000265068,0.00036971227,0.0002943262,0.00017459593,0.0017320284],"category_scores_gemma":[0.0013682669,0.00008191721,0.00023140472,0.002119493,0.00012985984,0.0003540792,0.00044742503,0.0001963301,0.00046300353],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054085598,0.000027813494,0.9746874,0.00008142232,0.000069109075,0.00016382121,0.00050707575,0.0014930558,0.0009869259,0.00016300601,0.0024118563,0.019354444],"study_design_scores_gemma":[0.000004504303,0.000014076533,0.9919578,0.000016033571,0.000022941853,0.000091496775,0.0013584584,0.0017300006,0.00024087529,0.000040296974,0.0045176614,0.0000058815244],"about_ca_topic_score_codex":0.038305685,"about_ca_topic_score_gemma":0.053400557,"teacher_disagreement_score":0.038305685,"about_ca_system_score_codex":0.00038610116,"about_ca_system_score_gemma":0.00045492328,"threshold_uncertainty_score":0.0761655},"labels":[],"label_agreement":null},{"id":"W4323314691","doi":"10.1007/s11069-023-05854-w","title":"Numerical modeling of a potential landslide-generated tsunami in the southern Strait of Georgia","year":2023,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Fisheries and Oceans Canada; Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Subaerial; Geology; Landslide; Seismology; Seafloor spreading; South carolina; Hydrogeology; Geophysics; Geotechnical engineering","score_opus":0.016543575896619242,"score_gpt":0.23385587954806009,"score_spread":0.21731230365144083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323314691","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9890914,0.00006358911,0.0019411452,0.00022324486,0.000026412805,0.000022040665,0.0003814061,0.0000831622,0.008167551],"genre_scores_gemma":[0.99751234,0.00003175108,0.0010375637,0.00003088475,0.00000285947,0.000014780825,0.00022264711,0.000012333988,0.001134729],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999125,0.000018172439,0.0000040976147,0.000014608595,0.000017646724,0.000032970464],"domain_scores_gemma":[0.9997042,0.00009563344,0.000039117618,0.000022746712,0.000078784775,0.000059504528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020133427,0.0004982838,0.00045724292,0.00045797354,0.0006748304,0.00084986445,0.00086634164,0.0010816313,0.0015570577],"category_scores_gemma":[0.0008920191,0.0003161975,0.00054417725,0.00047429194,0.0008313353,0.00027086367,0.0005747092,0.00051247963,0.00024917407],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052529493,0.000036941918,0.0053015584,0.000011693851,0.000019032617,0.00014010363,0.000037108333,0.99205315,0.00082839973,0.00070457504,0.00027090727,0.00054403115],"study_design_scores_gemma":[0.000025422187,0.000029856123,0.0021862963,0.0000053256304,0.000009842754,0.000011893932,0.00006885141,0.9969388,0.00020937134,0.00019915332,0.0003076782,0.0000074800064],"about_ca_topic_score_codex":0.15998527,"about_ca_topic_score_gemma":0.10224952,"teacher_disagreement_score":0.8400147,"about_ca_system_score_codex":0.00157207,"about_ca_system_score_gemma":0.0014136119,"threshold_uncertainty_score":0.31810814},"labels":[],"label_agreement":null},{"id":"W4323354864","doi":"10.1061/jggefk.gteng-11522","title":"The 2022 Chihshang, Taiwan, Earthquake: Initial GEER Team Observations","year":2023,"lang":"en","type":"article","venue":"Journal of Geotechnical and Geoenvironmental Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Division of Civil, Mechanical and Manufacturing Innovation; National Science Foundation","keywords":"Geotechnical engineering; Engineering; Geology; Forensic engineering","score_opus":0.013796258971517924,"score_gpt":0.20147959082073194,"score_spread":0.187683331849214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323354864","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43588632,0.0025181682,0.0025917992,0.018192941,0.005160714,0.0011510623,0.16138548,0.0045112935,0.36860216],"genre_scores_gemma":[0.5369455,0.0022898838,0.0028667557,0.0022466013,0.0014144839,0.00044359002,0.1465654,0.0005643733,0.3066634],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9998332,0.000009561819,0.000007440399,0.000013035511,0.000098986166,0.000037853883],"domain_scores_gemma":[0.9995906,0.000023557339,0.000040455023,0.00004518381,0.00018494698,0.00011526542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003046949,0.0003962366,0.00019786134,0.0008316225,0.00068367174,0.00060581,0.00027810864,0.00083528407,0.028965846],"category_scores_gemma":[0.0011890886,0.00014792786,0.00014802677,0.00080805284,0.00012214,0.00034371068,0.001104737,0.0008877432,0.010503399],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034134104,0.00007895768,0.044234347,0.00018942173,0.000026580487,0.0015981797,0.0009942942,0.00054086116,0.0037166763,0.00040246203,0.8858745,0.062002443],"study_design_scores_gemma":[0.00008767212,0.00023507113,0.4714182,0.0002851984,0.000027154427,0.00040586834,0.0030107803,0.0011241,0.0019972986,0.00046646735,0.5208778,0.00006440218],"about_ca_topic_score_codex":0.022630967,"about_ca_topic_score_gemma":0.08291846,"teacher_disagreement_score":0.028965846,"about_ca_system_score_codex":0.0004496584,"about_ca_system_score_gemma":0.0007973368,"threshold_uncertainty_score":0.09690046},"labels":[],"label_agreement":null},{"id":"W4323544766","doi":"10.1029/2022jb025287","title":"Heterogeneity Versus Anisotropy and the State of Stress in Stable Cratons: Observations From a Deep Borehole in Northeastern Alberta, Canada","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Anisotropy; Borehole; Stress field; Breakout; Azimuth; Seismology; Craton; Monte Carlo method; Slip (aerodynamics); Geophysics; Geometry; Petrology; Geotechnical engineering; Physics; Tectonics","score_opus":0.052466438501888514,"score_gpt":0.2975603682532464,"score_spread":0.24509392975135788,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323544766","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99873596,0.00006757217,0.00007370139,0.000020759368,0.0000010223624,0.000006479925,0.0003501176,0.000008106059,0.0007362927],"genre_scores_gemma":[0.9990576,0.000072353774,0.00013894541,0.000008688222,0.000001170714,0.0000027834394,0.00022326417,0.0000025580134,0.00049271225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998338,0.000004377914,0.000005896181,0.000027537071,0.00007055388,0.000057822846],"domain_scores_gemma":[0.9995468,0.000029643039,0.00006943945,0.000013464994,0.00021829543,0.00012225463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014815216,0.0003325678,0.0002443912,0.001862563,0.001711393,0.0009240694,0.000735,0.00031335224,0.00085648074],"category_scores_gemma":[0.0004597025,0.00029332977,0.00015958701,0.0020131932,0.0010862874,0.00021766809,0.00051884894,0.000271538,0.00016391235],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014269243,0.00004422244,0.97459376,0.000030218174,0.000034494147,0.0005065831,0.0022362305,0.00080002606,0.012432184,0.00011122907,0.000322792,0.008745686],"study_design_scores_gemma":[0.0000026662494,0.000007059965,0.9981699,0.000005783476,0.000004946878,0.00003799795,0.000900529,0.0003606911,0.00024018879,0.000011057412,0.00025376977,0.000005315847],"about_ca_topic_score_codex":0.97406536,"about_ca_topic_score_gemma":0.9928048,"teacher_disagreement_score":0.025934637,"about_ca_system_score_codex":0.008197274,"about_ca_system_score_gemma":0.0047153407,"threshold_uncertainty_score":0.05947572},"labels":[],"label_agreement":null},{"id":"W4323544769","doi":"10.1785/0120220166","title":"The 2020 Mw 6.5 Monte Cristo Range, Nevada, Earthquake: Anatomy of a Crossing-Fault Rupture through a Region of Highly Distributed Deformation","year":2023,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Seismology; Aftershock; Slip (aerodynamics); Interferometric synthetic aperture radar; Fault (geology); Earthquake rupture; Hypocenter; Geodesy; Induced seismicity; Synthetic aperture radar; Remote sensing","score_opus":0.01576563421511296,"score_gpt":0.23602634299188588,"score_spread":0.22026070877677292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323544769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928623,0.00053725543,0.00036473857,0.0001007562,0.000006622341,0.000013627561,0.00025155407,0.000024644834,0.0058384556],"genre_scores_gemma":[0.99842775,0.00014708118,0.0003085267,0.000017989076,0.0000031033742,0.0000038272065,0.00018973478,0.0000042734155,0.0008977723],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999658,0.0000026583098,0.0000014219304,0.000010925221,0.000010411973,0.000008858642],"domain_scores_gemma":[0.99992275,0.000004850234,0.000029690775,0.0000043112223,0.000016714463,0.000021746984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007873029,0.00007860637,0.000077120654,0.00051065715,0.00039699906,0.0005023355,0.00019227974,0.0003203221,0.0008853391],"category_scores_gemma":[0.0002188305,0.00007529486,0.000044285505,0.00039371086,0.0002822046,0.0002054609,0.0004619369,0.0001297967,0.00015294967],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027485882,0.000114479466,0.83943707,0.00011979304,0.00005424745,0.0065937196,0.0024991278,0.002666593,0.09179869,0.002215153,0.0025435092,0.05168272],"study_design_scores_gemma":[0.0000040596797,0.00003689824,0.99253255,0.000021349262,0.0000045208476,0.0012755943,0.0011417606,0.00074501504,0.00053349877,0.000216366,0.003482658,0.000005687576],"about_ca_topic_score_codex":0.031356033,"about_ca_topic_score_gemma":0.056990378,"teacher_disagreement_score":0.031356033,"about_ca_system_score_codex":0.0005096571,"about_ca_system_score_gemma":0.00034834098,"threshold_uncertainty_score":0.062347054},"labels":[],"label_agreement":null},{"id":"W4323967933","doi":"10.1007/978-3-031-23313-5_4","title":"Deformation: Strain and Rotation","year":2023,"lang":"en","type":"book-chapter","venue":"Springer geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Finite strain theory; Infinitesimal strain theory; Infinitesimal; Eulerian path; Deformation (meteorology); Displacement (psychology); State (computer science); Strain (injury); Tensor (intrinsic definition); Physics; Geometry; Mathematics; Classical mechanics; Mathematical analysis; Lagrangian; Finite element method","score_opus":0.022586875546783403,"score_gpt":0.20192380620007103,"score_spread":0.17933693065328762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323967933","genre_codex":"other","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0011840939,0.15291975,0.026884247,0.0028690554,0.005612388,0.00005211347,0.0013931607,0.000995228,0.80808985],"genre_scores_gemma":[0.007589257,0.054040924,0.0041471594,0.00091212196,0.002076349,0.000073321855,0.00090169406,0.00040908868,0.92985004],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99983144,0.000021757902,0.000010547978,0.000043855704,0.00008047488,0.000012026116],"domain_scores_gemma":[0.99985707,0.000045693127,0.000014495697,0.000033170036,0.000036064874,0.000013353106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020637033,0.0025338263,0.0014841972,0.0020118456,0.00052883365,0.002792958,0.0008375918,0.0013071365,0.07300387],"category_scores_gemma":[0.0006749845,0.00067454815,0.00042628017,0.0035071613,0.0011558661,0.003929044,0.0013946227,0.0022049535,0.0581656],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003142578,0.00003857688,0.00022976127,0.00045797793,0.000017841505,0.000118370604,0.00037612664,0.0015937996,0.001430608,0.16741574,0.32428586,0.5040039],"study_design_scores_gemma":[0.0000039929423,0.000017895705,0.00043573166,0.0001741143,0.0000074001223,0.00016598425,0.00007967294,0.0005041145,0.00019828975,0.049310755,0.94909215,0.000009938562],"about_ca_topic_score_codex":0.0019216979,"about_ca_topic_score_gemma":0.0038955477,"teacher_disagreement_score":0.07300387,"about_ca_system_score_codex":0.00065675547,"about_ca_system_score_gemma":0.0005373325,"threshold_uncertainty_score":0.24422228},"labels":[],"label_agreement":null},{"id":"W4327941334","doi":"10.21203/rs.3.rs-2696155/v1","title":"Moho Depth Variations in North West Iran estimated from the Moho reflected phases","year":2023,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; University of Tehran","keywords":"Geology; Moho; Seismology; Geodesy; Inversion (geology); Crust; Travel time; Fault (geology); Tectonics; Geophysics","score_opus":0.23682060768780255,"score_gpt":0.403136356008747,"score_spread":0.16631574832094442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4327941334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998637,0.00006866981,0.0004105809,0.0000129837845,0.0000030161625,0.0000036720157,0.00028627185,0.000011589522,0.00056617917],"genre_scores_gemma":[0.9990349,0.000045586465,0.000482933,0.0000027236563,0.000004038191,0.0000035720857,0.00029329842,0.0000022405384,0.00013081015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990904,0.00001052761,0.000007591016,0.000019903691,0.00003169201,0.0000212111],"domain_scores_gemma":[0.99977714,0.000029139763,0.0000676923,0.000014236273,0.000095383184,0.000016504178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013997054,0.00022911119,0.00013650126,0.00091235683,0.00012947604,0.0002951239,0.0001784315,0.00014291385,0.00048151452],"category_scores_gemma":[0.00065065315,0.00010455475,0.00012797328,0.0009193337,0.00010639366,0.00024514872,0.00023718008,0.00014069138,0.00011315515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011797253,0.000033242944,0.955668,0.00004303069,0.00006666917,0.00022609366,0.0005741985,0.004164642,0.0074742767,0.00017091184,0.00043295432,0.031028092],"study_design_scores_gemma":[0.0000044204626,0.000016626142,0.994584,0.0000056490503,0.000016457925,0.000080995545,0.00037816138,0.0035658965,0.0007026814,0.000056886263,0.0005822974,0.0000059125873],"about_ca_topic_score_codex":0.015858022,"about_ca_topic_score_gemma":0.02306281,"teacher_disagreement_score":0.015858022,"about_ca_system_score_codex":0.0002508546,"about_ca_system_score_gemma":0.00023037444,"threshold_uncertainty_score":0.031531453},"labels":[],"label_agreement":null},{"id":"W4353008514","doi":"10.5281/zenodo.7760706","title":"Microseismicity in the Northern Canadian Cordillera","year":2023,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology","score_opus":0.03620068616801943,"score_gpt":0.21748022555993268,"score_spread":0.18127953939191327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4353008514","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.077590644,0.0011728278,0.0006301466,0.00021373229,0.000057377765,0.00015791344,0.8725652,0.0007722485,0.046839975],"genre_scores_gemma":[0.17944214,0.0020446633,0.0028012076,0.00008273475,0.000043070824,0.00021096355,0.766761,0.00021474296,0.048399445],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9993555,0.000017489832,0.00006834211,0.00009072165,0.0002708115,0.00019717743],"domain_scores_gemma":[0.99724543,0.000081124505,0.00023198989,0.00017502031,0.001947248,0.00031927493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003437765,0.000852468,0.00053201296,0.015767725,0.0022382268,0.0015953993,0.001383668,0.00035610457,0.025042087],"category_scores_gemma":[0.0020687347,0.0003490777,0.00046209892,0.026012741,0.00028154138,0.00044020996,0.001005062,0.00041221734,0.005744478],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000589568,0.00006376966,0.2065549,0.0015548684,0.00025228728,0.00045348654,0.0030622883,0.00560724,0.0030696318,0.009037551,0.60917324,0.16058122],"study_design_scores_gemma":[0.000026558359,0.000021891337,0.7113612,0.00016109113,0.00004644409,0.0001189867,0.0009324413,0.0008796972,0.0004828397,0.00024387632,0.28568006,0.00004480375],"about_ca_topic_score_codex":0.99380267,"about_ca_topic_score_gemma":0.99497175,"teacher_disagreement_score":0.025042087,"about_ca_system_score_codex":0.014989326,"about_ca_system_score_gemma":0.028992727,"threshold_uncertainty_score":0.10875565},"labels":[],"label_agreement":null},{"id":"W4360610011","doi":"10.1029/2023gl102940","title":"Disposal From In Situ Bitumen Recovery Induced the <i>M</i><sub><i>L</i></sub> 5.6 Peace River Earthquake","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of Alberta","funders":"","keywords":"Geology; Asphalt; Seismology; Fault (geology); Tectonics; Geochemistry; Archaeology","score_opus":0.038698912940083305,"score_gpt":0.2696933580531697,"score_spread":0.23099444511308637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4360610011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998209,0.00001633374,0.00025939563,0.00002274,0.0000032982714,0.000004617788,0.00014544185,0.000021474556,0.0013176545],"genre_scores_gemma":[0.99957913,0.000012051619,0.00008226124,0.0000074948975,0.0000011267457,0.0000010201777,0.00010547232,0.0000023686796,0.0002091938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988246,0.0000091912125,0.0000075167736,0.00001443999,0.000050251205,0.000036095138],"domain_scores_gemma":[0.99975735,0.000029813365,0.00010279036,0.000022014847,0.000051969902,0.000036095444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012090485,0.00016587453,0.00016418796,0.00033873104,0.00029963176,0.00035487927,0.00024849956,0.00022454328,0.001597392],"category_scores_gemma":[0.00034754802,0.0000705745,0.00013109866,0.00038192072,0.000293306,0.00017075926,0.0003047013,0.00022383747,0.00015669955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007905127,0.00023019254,0.7153894,0.00020137773,0.00008428814,0.0015000138,0.0005865089,0.0048485445,0.23729314,0.00043725775,0.0013103131,0.037328415],"study_design_scores_gemma":[0.000008985059,0.00017566248,0.94816434,0.000008540479,0.000021502727,0.00017678867,0.00047566628,0.001933789,0.04799023,0.00008334158,0.0009537043,0.0000075048133],"about_ca_topic_score_codex":0.008789243,"about_ca_topic_score_gemma":0.019377764,"teacher_disagreement_score":0.99121076,"about_ca_system_score_codex":0.0005732376,"about_ca_system_score_gemma":0.00029728425,"threshold_uncertainty_score":0.017476141},"labels":[],"label_agreement":null},{"id":"W4360802777","doi":"10.5281/zenodo.7767767","title":"Microseismicity in the Northern Canadian Cordillera","year":2023,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Physical geography; Geography","score_opus":0.03620068616801943,"score_gpt":0.21748022555993268,"score_spread":0.18127953939191327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4360802777","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.077590644,0.0011728278,0.0006301466,0.00021373229,0.000057377765,0.00015791344,0.8725652,0.0007722485,0.046839975],"genre_scores_gemma":[0.17944214,0.0020446633,0.0028012076,0.00008273475,0.000043070824,0.00021096355,0.766761,0.00021474296,0.048399445],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9993555,0.000017489832,0.00006834211,0.00009072165,0.0002708115,0.00019717743],"domain_scores_gemma":[0.99724543,0.000081124505,0.00023198989,0.00017502031,0.001947248,0.00031927493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003437765,0.000852468,0.00053201296,0.015767725,0.0022382268,0.0015953993,0.001383668,0.00035610457,0.025042087],"category_scores_gemma":[0.0020687347,0.0003490777,0.00046209892,0.026012741,0.00028154138,0.00044020996,0.001005062,0.00041221734,0.005744478],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000589568,0.00006376966,0.2065549,0.0015548684,0.00025228728,0.00045348654,0.0030622883,0.00560724,0.0030696318,0.009037551,0.60917324,0.16058122],"study_design_scores_gemma":[0.000026558359,0.000021891337,0.7113612,0.00016109113,0.00004644409,0.0001189867,0.0009324413,0.0008796972,0.0004828397,0.00024387632,0.28568006,0.00004480375],"about_ca_topic_score_codex":0.99380267,"about_ca_topic_score_gemma":0.99497175,"teacher_disagreement_score":0.025042087,"about_ca_system_score_codex":0.014989326,"about_ca_system_score_gemma":0.028992727,"threshold_uncertainty_score":0.10875565},"labels":[],"label_agreement":null},{"id":"W4360868627","doi":"10.3390/iecg2022-14266","title":"Forecasting Tsunami Hazards Using Ocean Bottom Sensor Data and Classification Predictive Modeling","year":2023,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Akaike information criterion; Amplitude; Seismology; Shore; Slip (aerodynamics); Geology; Computer science; Data mining; Machine learning; Engineering","score_opus":0.15552725776183102,"score_gpt":0.2852276029436766,"score_spread":0.1297003451818456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4360868627","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9456176,0.00017541905,0.052287765,0.000121775214,0.000036765556,0.00002341045,0.0003542263,0.00024581517,0.00113718],"genre_scores_gemma":[0.99582916,0.000056304914,0.0036660242,0.000008576019,0.0000074689806,0.000009204736,0.0002486752,0.0000040657046,0.00017064276],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984765,0.000038459057,0.000013289144,0.000038781996,0.000035366138,0.000026477812],"domain_scores_gemma":[0.9994287,0.00030294462,0.00009245257,0.000043510245,0.00010477207,0.000027653681],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055397965,0.0006488109,0.0003982273,0.00081875507,0.00017387392,0.00048393442,0.00030587747,0.0003325824,0.00031455432],"category_scores_gemma":[0.001720235,0.00017133726,0.00035407094,0.000749844,0.00016989524,0.0005912165,0.00030808037,0.00031778013,0.000095819196],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000116397925,0.00008464989,0.031755716,0.000018920106,0.000037823305,0.0000515883,0.000020471818,0.9309208,0.0017293008,0.00023618681,0.0002474862,0.034780707],"study_design_scores_gemma":[0.000001353745,0.000007665496,0.0033510085,9.4045765e-7,0.0000036325864,0.000001508873,0.0000053049353,0.99629956,0.00023242459,0.00007824481,0.000016716687,0.0000016340188],"about_ca_topic_score_codex":0.01906727,"about_ca_topic_score_gemma":0.012974972,"teacher_disagreement_score":0.01906727,"about_ca_system_score_codex":0.0004506121,"about_ca_system_score_gemma":0.00035494153,"threshold_uncertainty_score":0.037912548},"labels":[],"label_agreement":null},{"id":"W4361221418","doi":"10.3390/w15071327","title":"Changes in Tidal and Barometric Response of Groundwater during Earthquakes—A Review with Recommendations for Better Management of Groundwater Resources","year":2023,"lang":"en","type":"article","venue":"Water","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institute for Advanced Research","keywords":"Hydrogeology; Groundwater; Aquifer; Geology; Atmospheric pressure; Water level; Tidal force; Hydrology (agriculture); Environmental science; Oceanography; Geotechnical engineering; Geography","score_opus":0.025577709700623674,"score_gpt":0.23789113040613663,"score_spread":0.21231342070551296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361221418","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00014732088,0.99845195,0.00022269921,0.00055885833,0.00022733337,0.000008148546,0.000044988043,0.000008422633,0.00033032426],"genre_scores_gemma":[0.00067875336,0.99844545,0.0002581502,0.00021705819,0.00020358105,0.000009633235,0.000041085477,0.0000018043817,0.00014453416],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.999529,0.00008089029,0.00013401092,0.00011457797,0.000105398256,0.00003605397],"domain_scores_gemma":[0.998387,0.00083668716,0.0002674172,0.000041144904,0.00040283691,0.00006487203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014298122,0.0010190435,0.0021952917,0.0041757193,0.00035241526,0.0015849393,0.0016924266,0.0016074613,0.0030089328],"category_scores_gemma":[0.0024229588,0.00046287262,0.0012446014,0.0046690544,0.0007868984,0.0025155882,0.0007869187,0.001547214,0.0011910576],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013307964,0.00014199704,0.0011995404,0.051713582,0.00030889167,0.00030281927,0.00016529222,0.001271663,0.0016541753,0.004477588,0.041060377,0.897571],"study_design_scores_gemma":[0.000025088655,0.0003072738,0.006990229,0.023360725,0.0006867628,0.0015613901,0.0003331161,0.0004932079,0.00069655926,0.0048003704,0.96063566,0.00010958169],"about_ca_topic_score_codex":0.0058921915,"about_ca_topic_score_gemma":0.0052820076,"teacher_disagreement_score":0.0058921915,"about_ca_system_score_codex":0.0011965209,"about_ca_system_score_gemma":0.0023234223,"threshold_uncertainty_score":0.01171577},"labels":[],"label_agreement":null},{"id":"W4361222278","doi":"10.1016/j.ringps.2023.100054","title":"Tectonic development of northeastern part of the Arabian Plate: Examples from Pirmam and Bana Bawi anticlines in the Kurdistan region of north Iraq","year":2023,"lang":"en","type":"article","venue":"Results in Geophysical Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"","keywords":"Anticline; Geology; Sedimentary depositional environment; Alluvial fan; Alluvium; Subsidence; Tectonics; Alluvial plain; Fluvial; Geomorphology; Paleontology; Sedimentary rock","score_opus":0.0445163149234681,"score_gpt":0.24337249625893073,"score_spread":0.19885618133546262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361222278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99511397,0.00029246206,0.000113430404,0.000030788284,0.0000063202597,0.000009885149,0.00065395754,0.00001270058,0.003766564],"genre_scores_gemma":[0.9976907,0.00029062663,0.000598212,0.000007038496,0.000004525184,0.0000061117753,0.0006060005,0.000004036633,0.0007927719],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993527,0.0000106677435,0.000007526037,0.000014256678,0.000015607717,0.000016625898],"domain_scores_gemma":[0.99983203,0.000016491962,0.000059876136,0.000010759594,0.000060498336,0.000020268735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011288583,0.00022835028,0.00009038945,0.0019913227,0.00032169162,0.0004737064,0.00017676453,0.0001654395,0.0012718042],"category_scores_gemma":[0.00024725197,0.00010776782,0.00015477651,0.0021921322,0.0002650033,0.00013376599,0.00023944565,0.00012334752,0.00015850058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007317698,0.00003141638,0.960524,0.0000921563,0.00005695498,0.0018816154,0.0018670367,0.0038221723,0.004795242,0.0008591194,0.00094351807,0.025053496],"study_design_scores_gemma":[0.0000025307243,0.000010087028,0.99607664,0.0000114146005,0.000009168479,0.00023709766,0.00056207925,0.0009873696,0.00021359221,0.00002609123,0.0018597564,0.00000415334],"about_ca_topic_score_codex":0.063492924,"about_ca_topic_score_gemma":0.11379655,"teacher_disagreement_score":0.063492924,"about_ca_system_score_codex":0.00047739083,"about_ca_system_score_gemma":0.00040182486,"threshold_uncertainty_score":0.12624669},"labels":[],"label_agreement":null},{"id":"W4361271262","doi":"10.3389/fams.2023.1126952","title":"Statistical and clustering analysis of microseismicity from a Saskatchewan potash mine","year":2023,"lang":"en","type":"article","venue":"Frontiers in Applied Mathematics and Statistics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs","keywords":"Potash; Cluster analysis; Magnitude (astronomy); Pareto distribution; Scaling; Rock mass classification; Pareto principle; Geology; Mining engineering; Statistics; Mathematics; Geotechnical engineering; Physics","score_opus":0.011826601361866695,"score_gpt":0.21729582378812776,"score_spread":0.20546922242626106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361271262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962715,0.00001747891,0.0020188913,0.00003372115,0.0000018242299,0.000019708785,0.00083924225,0.000027549871,0.0007701312],"genre_scores_gemma":[0.9955031,0.000033184395,0.0016565162,0.000009607109,0.0000015630616,0.000014812671,0.0019781804,0.0000076962415,0.0007953287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997814,0.000026252688,0.000017227443,0.000061205574,0.000071144415,0.000042737585],"domain_scores_gemma":[0.9986896,0.00024635572,0.00014260886,0.00011377308,0.00071033963,0.00009728845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003472584,0.00026562787,0.00023912397,0.0017508576,0.0006502349,0.0005440826,0.00051117165,0.00034106802,0.0007753785],"category_scores_gemma":[0.0013078898,0.0001656978,0.00026160327,0.0028335308,0.00040571223,0.00017458212,0.00051764067,0.00026617368,0.00018999023],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026529623,0.00011506268,0.78317547,0.00009986232,0.00019425782,0.0013640797,0.0013426653,0.14647593,0.022377878,0.0019695493,0.0023458174,0.040274218],"study_design_scores_gemma":[0.000008549573,0.000029058085,0.8628015,0.000012619048,0.000027486492,0.00009856498,0.0012571261,0.132176,0.0019885995,0.0003858905,0.0011691583,0.000045470162],"about_ca_topic_score_codex":0.64063615,"about_ca_topic_score_gemma":0.77689445,"teacher_disagreement_score":0.64063615,"about_ca_system_score_codex":0.002769589,"about_ca_system_score_gemma":0.002580196,"threshold_uncertainty_score":0.7229604},"labels":[],"label_agreement":null},{"id":"W4362470507","doi":"10.1007/s12613-023-2607-8","title":"Interaction between in situ stress states and tectonic faults: A comment","year":2023,"lang":"en","type":"article","venue":"International Journal of Minerals Metallurgy and Materials","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Classification of discontinuities; Fault (geology); Stress (linguistics); Seismology; Geology; Tectonics; Slip (aerodynamics); Engineering; Mathematics","score_opus":0.024866787014127437,"score_gpt":0.2783853130495232,"score_spread":0.25351852603539576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362470507","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0049039526,0.0016737051,0.0017525833,0.970974,0.01286513,0.000020979565,0.0006031315,0.00010613878,0.007100268],"genre_scores_gemma":[0.06362453,0.0020476864,0.0015491671,0.8887517,0.034188993,0.00008789998,0.0001873183,0.00010110811,0.009461699],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9943204,0.0006280073,0.0005329646,0.0024420393,0.0016071607,0.0004694082],"domain_scores_gemma":[0.94313014,0.03847007,0.0029585203,0.0033084725,0.010671415,0.0014613856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008266811,0.0010493691,0.0016430668,0.00092985213,0.004621424,0.0036261,0.00796273,0.030054988,0.015946345],"category_scores_gemma":[0.048145674,0.0008797697,0.0021839226,0.0021372947,0.007679922,0.007497764,0.0044493023,0.031395804,0.00819054],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038554784,0.00013648922,0.014977241,0.0006193213,0.00031880298,0.0023120842,0.0037218903,0.00079072436,0.0024031508,0.040185828,0.91324836,0.020900622],"study_design_scores_gemma":[0.00056643324,0.0004443823,0.04113084,0.0015341421,0.0006514528,0.004334758,0.007977719,0.0026192167,0.006857268,0.13845317,0.7948888,0.0005418559],"about_ca_topic_score_codex":0.029686501,"about_ca_topic_score_gemma":0.02807715,"teacher_disagreement_score":0.030054988,"about_ca_system_score_codex":0.0032585426,"about_ca_system_score_gemma":0.0036231708,"threshold_uncertainty_score":0.059027433},"labels":[],"label_agreement":null},{"id":"W4362475873","doi":"10.24908/iqurcp16331","title":"Influence Of Lithospheric Scale Basement Faults On Seismicity In The Himalayan Orogenic System","year":2023,"lang":"en","type":"article","venue":"Inquiry Queen s Undergraduate Research Conference Proceedings","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Geology; Seismology; Induced seismicity; Basement; Crust; Lithosphere; Tectonics; Geophysics","score_opus":0.07338210896229952,"score_gpt":0.3225209957909992,"score_spread":0.24913888682869967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362475873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986494,0.000038392533,0.00007868363,0.000033294673,0.0000013279806,0.0000019113786,0.00007524768,0.000011537977,0.0011102268],"genre_scores_gemma":[0.99976176,0.000041308416,0.00003761282,0.0000047899116,0.0000010460208,7.323408e-7,0.00004923719,0.000003210515,0.00010022274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998803,0.00003462982,0.000009439084,0.000019552323,0.00002328926,0.00003287016],"domain_scores_gemma":[0.99981195,0.000058546306,0.000033872053,0.00002035608,0.0000253733,0.000049896586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013509604,0.00028336284,0.00025496777,0.00056479016,0.00063243636,0.0012770146,0.00029955409,0.00027573536,0.0019315226],"category_scores_gemma":[0.0007367851,0.00016952063,0.00022102805,0.0008526979,0.00061337743,0.00030962063,0.0006924533,0.00021964949,0.0001705191],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047975534,0.00013754486,0.4847015,0.00011063756,0.00023577313,0.0014880367,0.0016548033,0.48079756,0.016821055,0.0019682795,0.0005214946,0.0110835815],"study_design_scores_gemma":[0.00009872403,0.00018990993,0.6740233,0.000033582688,0.00012862933,0.00021451729,0.0028671238,0.31627753,0.0038144412,0.0010639919,0.0012245865,0.00006366466],"about_ca_topic_score_codex":0.074438125,"about_ca_topic_score_gemma":0.058391675,"teacher_disagreement_score":0.074438125,"about_ca_system_score_codex":0.0015333244,"about_ca_system_score_gemma":0.0006810303,"threshold_uncertainty_score":0.14800972},"labels":[],"label_agreement":null},{"id":"W4362577984","doi":"10.1785/0320220042","title":"Coseismic Slip Model of the 19 September 2022 Mw 7.6 Michoacán, Mexico, Earthquake: A Quasi-Repeat of the 1973 Mw 7.6 Rupture","year":2023,"lang":"en","type":"article","venue":"The Seismic Record","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; National Natural Science Foundation of China; European Space Agency; National Science Foundation","keywords":"Seismology; Geology; Aftershock; Hypocenter; Slip (aerodynamics); Subduction; Trench; Episodic tremor and slip; Seismic moment; Submarine pipeline; Geodesy; Tectonics; Fault (geology); Induced seismicity; Geotechnical engineering","score_opus":0.022673074736210976,"score_gpt":0.22305197266140342,"score_spread":0.20037889792519245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362577984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937781,0.000049750608,0.0028612574,0.000112228015,0.0000062850213,0.000014192369,0.0003222688,0.00006714984,0.0027887637],"genre_scores_gemma":[0.9990381,0.000018044775,0.00017579772,0.000006551441,0.0000034755935,0.0000071431764,0.0001166789,0.0000062894073,0.0006279641],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999577,0.0000064299825,0.0000018249268,0.000013213487,0.0000074958766,0.0000133920985],"domain_scores_gemma":[0.9999318,0.000011397105,0.000023081835,0.000006029249,0.000015192466,0.000012494312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011875977,0.000343672,0.00022892754,0.00033134493,0.00029388373,0.00038299413,0.00050554523,0.0004680784,0.0015298051],"category_scores_gemma":[0.00034182583,0.00017097041,0.00023142899,0.00025204994,0.00023346931,0.0002452799,0.00014007148,0.00017964235,0.00019171955],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034310605,0.000114821174,0.06961939,0.000032903376,0.000072393326,0.00060522783,0.000126581,0.91282254,0.005792889,0.002736859,0.0015941699,0.00613921],"study_design_scores_gemma":[0.00001558226,0.000031807216,0.023056481,0.0000020051061,0.0000081740745,0.00002214485,0.000025218369,0.97640705,0.00011186246,0.00012162326,0.00019346744,0.000004584314],"about_ca_topic_score_codex":0.079206824,"about_ca_topic_score_gemma":0.043734934,"teacher_disagreement_score":0.079206824,"about_ca_system_score_codex":0.0010181512,"about_ca_system_score_gemma":0.00038791166,"threshold_uncertainty_score":0.15749156},"labels":[],"label_agreement":null},{"id":"W4362608794","doi":"10.1007/s00024-023-03251-9","title":"Local and Trans-oceanic Tsunamis in the Bering and Chukchi Seas Based on Numerical Modeling","year":2023,"lang":"en","type":"article","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization","funders":"","keywords":"Geology; Tsunami earthquake; Oceanography; Seismology; Peninsula; Pacific ocean; Tsunami wave; Arctic; Geography","score_opus":0.013738113559259838,"score_gpt":0.19817632703150398,"score_spread":0.18443821347224415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362608794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99716824,0.00006666331,0.0010612583,0.000051939824,0.000012243936,0.000007944701,0.00019539957,0.000059229977,0.001376963],"genre_scores_gemma":[0.9989039,0.00005769386,0.00047175534,0.0000042820434,0.0000035406472,0.000008100929,0.00018422285,0.000007069719,0.00035933245],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991953,0.000019043362,0.000009090579,0.000023413148,0.000009005781,0.00001990348],"domain_scores_gemma":[0.99968755,0.00011100198,0.000052608375,0.000025922734,0.00007454836,0.000048380003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020552105,0.0004818357,0.00041991402,0.00077521586,0.00064310245,0.0009008857,0.0005768143,0.00052453135,0.0014309359],"category_scores_gemma":[0.0008801558,0.00036493,0.00060498697,0.0009147252,0.00040969258,0.00057187246,0.0004095114,0.00048758445,0.0002142623],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012101504,0.000073476716,0.0641726,0.000031169497,0.00009617698,0.0001871408,0.00010789775,0.9291998,0.00093793584,0.00075689965,0.0002836596,0.004032215],"study_design_scores_gemma":[0.000013133415,0.00001387611,0.019367002,0.00000823266,0.000038681515,0.000014182593,0.000112547576,0.9800646,0.00013486968,0.000125449,0.000092827446,0.000014495211],"about_ca_topic_score_codex":0.28147298,"about_ca_topic_score_gemma":0.22259787,"teacher_disagreement_score":0.28147298,"about_ca_system_score_codex":0.0015444219,"about_ca_system_score_gemma":0.001326489,"threshold_uncertainty_score":0.55966926},"labels":[],"label_agreement":null},{"id":"W4362666738","doi":"10.1785/0120220164","title":"Lateral Variations of Attenuation in the Crust of Alaska Using <i>Lg</i> <i>Q</i> Tomography","year":2023,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Terrane; Seismology; Crust; Attenuation; San andreas fault; Range (aeronautics); Fault (geology); Tectonics; Paleontology","score_opus":0.02572079300335083,"score_gpt":0.22952149013774226,"score_spread":0.20380069713439142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362666738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99747795,0.000044350567,0.000736883,0.000014525338,0.0000031496697,0.0000034223435,0.00042166302,0.000051025727,0.001247059],"genre_scores_gemma":[0.9989448,0.00003282447,0.00048092866,0.000003305932,0.0000017939551,0.0000020710181,0.00034258436,0.000006881164,0.00018481692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999211,0.000008776495,0.00000811368,0.000022165974,0.000025127449,0.000014754771],"domain_scores_gemma":[0.9997876,0.000028076347,0.000048610458,0.000015735486,0.000102028454,0.000017916553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002534493,0.00024408476,0.000116541996,0.0010335782,0.0001902578,0.00049024646,0.0001880757,0.00017899707,0.00090858235],"category_scores_gemma":[0.0007745735,0.00014468803,0.00015726208,0.0009707425,0.00023314096,0.00036847917,0.00030956222,0.00018077127,0.00018735226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017801717,0.00005858052,0.88904387,0.00006256051,0.00011690048,0.0005044486,0.0010401946,0.019409493,0.055892244,0.00019838505,0.0003963369,0.033098914],"study_design_scores_gemma":[0.0000050744175,0.000041485702,0.97833854,0.000022412623,0.000038284194,0.00013246766,0.00064282905,0.015967937,0.0038779094,0.00006921544,0.0008448354,0.000019004809],"about_ca_topic_score_codex":0.03590879,"about_ca_topic_score_gemma":0.04756443,"teacher_disagreement_score":0.03590879,"about_ca_system_score_codex":0.00026247546,"about_ca_system_score_gemma":0.00022721358,"threshold_uncertainty_score":0.07139957},"labels":[],"label_agreement":null},{"id":"W4362719698","doi":"10.1016/j.geoen.2023.211776","title":"Reliability of earthquake-size distribution and stress regime relationships for fluid-injection-induced seismicity","year":2023,"lang":"en","type":"article","venue":"Geoenergy Science and Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Geothermal gradient; Seismology; Seismic hazard; Hydraulic fracturing; Slip (aerodynamics); Geotechnical engineering; Engineering; Geophysics","score_opus":0.0187352041469179,"score_gpt":0.2080910756207135,"score_spread":0.1893558714737956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362719698","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847227,0.00047069066,0.01082854,0.00013523817,0.00004585608,0.00004350071,0.0018983295,0.0003275741,0.0015276063],"genre_scores_gemma":[0.9989411,0.000030308416,0.00032004208,0.000016588756,0.000012945779,0.000006246525,0.00055966317,0.000030058476,0.00008301295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.991947,0.003342348,0.00083086296,0.002564914,0.00096204004,0.00035289826],"domain_scores_gemma":[0.59436655,0.34122354,0.017998042,0.029063467,0.015152731,0.002195692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.018668575,0.0007974709,0.00083328306,0.002373516,0.0005242897,0.0015344534,0.0018777417,0.001677134,0.0026904023],"category_scores_gemma":[0.14340532,0.00056076475,0.0014592953,0.0015540688,0.0016453688,0.0025525424,0.0010933528,0.0012870516,0.0015431958],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015859965,0.00007562852,0.961836,0.00009316522,0.00082786,0.0001310048,0.00043404862,0.020101275,0.0026858477,0.00047385675,0.0005580916,0.011197277],"study_design_scores_gemma":[0.00010854781,0.00065924256,0.8378453,0.00004986644,0.00037941473,0.0006778813,0.0003615639,0.15272537,0.003462809,0.0029549203,0.0006783424,0.00009667332],"about_ca_topic_score_codex":0.004248527,"about_ca_topic_score_gemma":0.002733364,"teacher_disagreement_score":0.018668575,"about_ca_system_score_codex":0.00060218363,"about_ca_system_score_gemma":0.00057151745,"threshold_uncertainty_score":0.09873003},"labels":[],"label_agreement":null},{"id":"W4363673522","doi":"10.1038/s41561-023-01160-z","title":"Submarine terraced deposits linked to periodic collapse of caldera-forming eruption columns","year":2023,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Caldera; Pyroclastic rock; Explosive eruption; Submarine; Subaerial; Seismology; Seabed; Volcano; Petrology; Oceanography","score_opus":0.013977571199775213,"score_gpt":0.2470901397751428,"score_spread":0.23311256857536758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4363673522","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990546,0.000031995314,0.000015720098,0.000026219446,0.0000027965593,0.0000018326298,0.00032807287,0.0000035560654,0.0005351808],"genre_scores_gemma":[0.9993703,0.000023595268,0.00003296371,0.000009350377,0.0000053731264,0.0000014048275,0.00034769386,0.0000011715072,0.00020829812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999119,0.000008452777,0.000007631826,0.00002738384,0.0000125091565,0.00003213425],"domain_scores_gemma":[0.99916613,0.00008789089,0.00043375805,0.00006597311,0.00011201733,0.00013430663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014767067,0.0001352858,0.00012629562,0.0012592636,0.00040916432,0.000459586,0.0003012415,0.00039860065,0.0032678142],"category_scores_gemma":[0.0007416356,0.00010860188,0.0001386233,0.0012581155,0.0003569676,0.0001971794,0.0005398222,0.00022288362,0.000202944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012701827,0.00002458797,0.9935601,0.000011255196,0.000039293634,0.0005692021,0.00022588864,0.00014787575,0.0021768624,0.000084207575,0.00035986226,0.0026739426],"study_design_scores_gemma":[0.0000021290348,0.0000062464915,0.99944264,0.0000028201687,0.000007032717,0.000089135545,0.00013234098,0.00010873818,0.000063097315,0.000016180702,0.00012895392,7.580998e-7],"about_ca_topic_score_codex":0.033096027,"about_ca_topic_score_gemma":0.065237,"teacher_disagreement_score":0.033096027,"about_ca_system_score_codex":0.0003585612,"about_ca_system_score_gemma":0.00035403855,"threshold_uncertainty_score":0.06580675},"labels":[],"label_agreement":null},{"id":"W4366188716","doi":"10.1080/17499518.2023.2201246","title":"Regional seismic loss estimation and critical earthquake scenarios for the Western Quebec seismic zone","year":2023,"lang":"en","type":"article","venue":"Georisk Assessment and Management of Risk for Engineered Systems and Geohazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; McMaster University; Western University","funders":"","keywords":"Urban seismic risk; Earthquake scenario; Seismic hazard; Seismology; Earthquake casualty estimation; Seismic risk; Geology; Seismic zone; Environmental Seismic Intensity scale; Estimation; Seismic microzonation; Vulnerability (computing); Intraplate earthquake; Induced seismicity; Tectonics; Engineering","score_opus":0.01785189389241232,"score_gpt":0.26764859162215077,"score_spread":0.24979669772973845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366188716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98689306,0.0001336187,0.006118344,0.00018328697,0.0000046579544,0.0000711214,0.0031876878,0.00015293868,0.0032552576],"genre_scores_gemma":[0.9950235,0.00006718835,0.0025382568,0.000013432417,0.0000019475717,0.000022334783,0.0015743736,0.000010174268,0.0007487801],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997948,0.00004963513,0.000008413011,0.000042260996,0.000040375246,0.00006442189],"domain_scores_gemma":[0.9992163,0.00026022206,0.00013593149,0.000049218117,0.0002534809,0.0000848501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006239203,0.0009145518,0.0003230023,0.0013183382,0.00050071994,0.00075259793,0.00091591873,0.0005658986,0.0012752564],"category_scores_gemma":[0.0018843164,0.00023227009,0.00042065763,0.0010761746,0.0003554654,0.00043792935,0.00047260363,0.00040355313,0.00012242603],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007544139,0.000033467306,0.023631904,0.000018333412,0.000040420437,0.00015977265,0.000032802058,0.9701818,0.0005067737,0.0005448683,0.00089846586,0.00387602],"study_design_scores_gemma":[0.000011551279,0.00002144878,0.017511506,0.000006811064,0.000015360347,0.000022039938,0.00009173276,0.98158836,0.00026569664,0.00016585868,0.00028682695,0.000012789869],"about_ca_topic_score_codex":0.8729252,"about_ca_topic_score_gemma":0.8442912,"teacher_disagreement_score":0.12707478,"about_ca_system_score_codex":0.009420676,"about_ca_system_score_gemma":0.0026830505,"threshold_uncertainty_score":0.25564623},"labels":[],"label_agreement":null},{"id":"W4366495134","doi":"10.1016/j.epsl.2023.118168","title":"Complexity of initiation and evolution of the 2013 Yunlong earthquake swarm","year":2023,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; National Key Research and Development Program of China; Ocean Frontier Institute","keywords":"Swarm behaviour; Geology; Earthquake swarm; Fault (geology); Seismology; Induced seismicity; Computer science; Artificial intelligence","score_opus":0.02688307984314138,"score_gpt":0.20680956775117357,"score_spread":0.17992648790803217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366495134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99701995,0.0001487632,0.00047950234,0.00020946568,0.0000058315345,0.0000065451,0.00008951702,0.000021278893,0.0020190554],"genre_scores_gemma":[0.9995499,0.000063296655,0.000119136086,0.0000126786745,0.000006635486,0.0000031497086,0.00011027138,0.0000061687533,0.00012864544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998387,0.0000268872,0.000013566902,0.0000445086,0.000026171023,0.000050105307],"domain_scores_gemma":[0.9991722,0.0002521014,0.00022811936,0.000070818125,0.000115108225,0.0001617124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037366967,0.00013733735,0.00033821748,0.0012204906,0.00067795295,0.0015257405,0.00031522766,0.0006611985,0.001890125],"category_scores_gemma":[0.0027858473,0.0004913166,0.0003010322,0.00067033485,0.00072720484,0.00093828456,0.0010961556,0.0006922075,0.00028720163],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026319394,0.00008699303,0.8833097,0.00010232479,0.00016162249,0.0009141747,0.00274347,0.03364141,0.040031753,0.0094892755,0.0014951772,0.02776088],"study_design_scores_gemma":[0.000010889868,0.00003564315,0.96421546,0.00002946473,0.000026784126,0.00016996678,0.0011646523,0.02956302,0.0005123813,0.0031990302,0.0010374688,0.00003530491],"about_ca_topic_score_codex":0.014349805,"about_ca_topic_score_gemma":0.022214504,"teacher_disagreement_score":0.014349805,"about_ca_system_score_codex":0.0008462544,"about_ca_system_score_gemma":0.0009159986,"threshold_uncertainty_score":0.028532565},"labels":[],"label_agreement":null},{"id":"W4366779099","doi":"10.1016/j.jsg.2023.104864","title":"3-D hydromechanical simulation of intersecting faults: Influences on fluid circulation and formation of oriented-orebodies","year":2023,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"iNano Medical (Canada)","funders":"Agence Nationale de la Recherche; Université de Lorraine","keywords":"Geology; Structural basin; Fluid dynamics; Unconformity; Petrology; Fault (geology); Fault block; Permeability (electromagnetism); Geotechnical engineering; Differential stress; Petroleum reservoir; Oil field; Geomorphology; Petroleum engineering; Seismology; Mechanics","score_opus":0.02144830516605369,"score_gpt":0.2627763381222311,"score_spread":0.2413280329561774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366779099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942762,0.000032356715,0.0023800624,0.00014805941,0.000037864927,0.000016778393,0.00054353854,0.00016545519,0.002399703],"genre_scores_gemma":[0.99903226,0.000016711367,0.00054546515,0.000016729737,0.0000053554018,0.0000071986233,0.00012855821,0.00001445232,0.00023313655],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989676,0.000023555074,0.000009310897,0.000024066823,0.000014733657,0.00003156984],"domain_scores_gemma":[0.9993469,0.00032583522,0.00006618583,0.00004278057,0.00007568628,0.00014257159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021483365,0.00043632588,0.0004702496,0.00062820385,0.0005427786,0.000850485,0.00064727984,0.0017455469,0.0034800114],"category_scores_gemma":[0.0012880849,0.00049578375,0.00069463707,0.00060511153,0.00086206634,0.00047583051,0.00047026374,0.0006088591,0.00024048392],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001020675,0.00011416735,0.009529029,0.000015872492,0.000027651591,0.0001337333,0.000048462527,0.98696077,0.0015805049,0.0002556531,0.00017569005,0.0010564887],"study_design_scores_gemma":[0.000026401112,0.000020820029,0.004017895,0.0000022212287,0.000007427823,0.000007219755,0.00003477009,0.99549013,0.00025536993,0.00006190405,0.000068683985,0.000007122942],"about_ca_topic_score_codex":0.043989126,"about_ca_topic_score_gemma":0.02737693,"teacher_disagreement_score":0.043989126,"about_ca_system_score_codex":0.0007794752,"about_ca_system_score_gemma":0.0009791832,"threshold_uncertainty_score":0.08746618},"labels":[],"label_agreement":null},{"id":"W4366825515","doi":"10.3390/geohazards4020008","title":"Fault Slip Tendency Analysis for a Deep-Sea Basalt CO2 Injection in the Cascadia Basin","year":2023,"lang":"en","type":"article","venue":"GeoHazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Remotely Operated Platform for Ocean Sciences; Geological Survey of Canada; Natural Resources Canada; Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Geology; Basalt; Induced seismicity; Structural basin; Carbon sequestration; Submarine pipeline; Seismology; Slip (aerodynamics); Permeability (electromagnetism); Crust; Carbonate; Pore water pressure; Injection well; Aquifer; Petrology; Geochemistry; Oceanography; Geotechnical engineering; Petroleum engineering; Geomorphology; Carbon dioxide; Groundwater","score_opus":0.024549374618154943,"score_gpt":0.2546285812044891,"score_spread":0.23007920658633418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366825515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99942267,0.000010392929,0.00015425848,0.0000074501427,7.258247e-7,0.00000267303,0.00011855856,0.00001254405,0.00027077497],"genre_scores_gemma":[0.99962044,0.000008136855,0.000086293876,0.0000011549334,4.205691e-7,0.0000014195969,0.00015245135,0.0000015451915,0.00012792704],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989724,0.000012206765,0.000014587782,0.000026391945,0.000028261977,0.000021350766],"domain_scores_gemma":[0.9995111,0.00011955394,0.0001201027,0.000030643732,0.00014783611,0.00007073845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020789003,0.0002554425,0.00022060532,0.0016197484,0.0002462143,0.00045966025,0.00019221338,0.00025734236,0.0010626474],"category_scores_gemma":[0.0007702469,0.00015521796,0.0003064373,0.0010355193,0.00020811196,0.00016245656,0.0001924551,0.00016455974,0.00011680545],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027829254,0.000082048435,0.9326454,0.00004377202,0.00009042499,0.0009841095,0.00034383094,0.046110477,0.010327991,0.00016986554,0.00030495308,0.0086188],"study_design_scores_gemma":[0.0000070326564,0.00007689301,0.93198377,0.000005936753,0.00003143149,0.00013758503,0.00043791078,0.06600507,0.0011116747,0.000047862624,0.00014231354,0.000012442409],"about_ca_topic_score_codex":0.04750821,"about_ca_topic_score_gemma":0.056313418,"teacher_disagreement_score":0.04750821,"about_ca_system_score_codex":0.0006692596,"about_ca_system_score_gemma":0.0003394236,"threshold_uncertainty_score":0.09446335},"labels":[],"label_agreement":null},{"id":"W4367050839","doi":"10.1785/0120220264","title":"Geomechanical Modeling of Ground Surface Deformation Associated with Thrust and Reverse-Fault Earthquakes: A Distinct Element Approach","year":2023,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mira Geoscience (Canada)","funders":"","keywords":"Fault scarp; Geology; Fault (geology); Seismology; Thrust fault; Deformation (meteorology); Slip (aerodynamics); Geotechnical engineering","score_opus":0.02491062796300388,"score_gpt":0.20634546799850922,"score_spread":0.18143484003550533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367050839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6171185,0.00023321142,0.37293854,0.00054590113,0.000061321,0.00008296366,0.00077085523,0.00047525787,0.007773459],"genre_scores_gemma":[0.97187287,0.0001304651,0.025048422,0.000063545354,0.0000184015,0.00007895214,0.00024983083,0.0000700993,0.0024673862],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999126,0.000028790364,0.000006862921,0.00001959309,0.000018764877,0.000013363543],"domain_scores_gemma":[0.9996933,0.00015213843,0.000042274885,0.00004028231,0.00004550033,0.000026469555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028407885,0.0003399816,0.00044131267,0.00069121044,0.0002948025,0.0007038245,0.0010642406,0.0013611608,0.0014291955],"category_scores_gemma":[0.0008399968,0.0004703052,0.00063281745,0.00044973518,0.0006166353,0.00055358006,0.0005539453,0.0005936012,0.00024293619],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010427049,0.00002403461,0.0010105806,0.0000073822457,0.000009514631,0.000028852537,0.000015901564,0.9952101,0.0013755958,0.0010971893,0.000059547197,0.0011508581],"study_design_scores_gemma":[9.662434e-7,0.0000021327992,0.00012139836,5.678183e-7,6.553724e-7,0.0000015547031,0.0000019618703,0.9995974,0.0000574619,0.00017549483,0.00003919017,0.0000012424974],"about_ca_topic_score_codex":0.0077945595,"about_ca_topic_score_gemma":0.004668636,"teacher_disagreement_score":0.0077945595,"about_ca_system_score_codex":0.0005894579,"about_ca_system_score_gemma":0.00048567986,"threshold_uncertainty_score":0.0154984},"labels":[],"label_agreement":null},{"id":"W4367051827","doi":"10.1029/2023gl102763","title":"Episodic Magma Hammers for the 15 January 2022 Cataclysmic Eruption of Hunga Tonga‐Hunga Ha'apai","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Instituto Dom Luiz, Universidade de Lisboa; Natural Resources Canada; University of California, Santa Barbara; U.S. Naval Observatory; Lamont-Doherty Earth Observatory, Columbia University; U.S. Geological Survey; Eidgenössische Technische Hochschule Zürich; Universidad de Chile; Institut de Physique du Globe de Paris; Universidade de Lisboa; University of California, San Diego; University of Oregon; National Oceanic and Atmospheric Administration; University of Texas at Austin; Univerzita Karlova v Praze; Dublin Institute for Advanced Studies; California Institute of Technology; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Magma; Volcano; Seismology; Plume; Geophysics; Meteorology; Physics","score_opus":0.058588516394545584,"score_gpt":0.3162117509459883,"score_spread":0.2576232345514427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367051827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985012,0.000034882214,0.00016048817,0.00009545644,0.0000058925075,0.00000815565,0.00038801343,0.00003137222,0.0007745758],"genre_scores_gemma":[0.99949896,0.00001595172,0.00007137593,0.0000062026943,0.0000044053504,0.0000041733647,0.00025144414,0.000002569961,0.00014483466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994516,0.000005079684,0.0000043819573,0.000015159439,0.000012884091,0.000017284776],"domain_scores_gemma":[0.99982834,0.00003035562,0.000043266824,0.000017814747,0.000027792517,0.000052483334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021701014,0.00021105263,0.00020934128,0.00064122357,0.000469258,0.00048230487,0.00026227682,0.00061427435,0.0018291118],"category_scores_gemma":[0.0006193131,0.00016948167,0.0002563127,0.0006466786,0.0002786283,0.00035584497,0.00055901194,0.00030102933,0.00016640523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035787365,0.000102390535,0.9304602,0.00013741711,0.0001960223,0.00365235,0.0023191485,0.01892009,0.017538013,0.0011035549,0.0024755166,0.022737445],"study_design_scores_gemma":[0.000008482948,0.000029992172,0.98531324,0.0000052339633,0.000020332463,0.00012469763,0.00038941522,0.012682112,0.0003912069,0.00012828814,0.00089642656,0.000010624172],"about_ca_topic_score_codex":0.030361256,"about_ca_topic_score_gemma":0.051553916,"teacher_disagreement_score":0.030361256,"about_ca_system_score_codex":0.0011048918,"about_ca_system_score_gemma":0.0004515701,"threshold_uncertainty_score":0.060369074},"labels":[],"label_agreement":null},{"id":"W4367059780","doi":"10.1130/geol.s.22704853.v1","title":"Supplemental Material: A mechanism for transient creep in crustal shear zones","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Creep; Shear zone; Transient (computer programming); Geology; Shear (geology); Seismology; Geotechnical engineering; Materials science; Petrology; Composite material; Computer science; Operating system","score_opus":0.04259026418141727,"score_gpt":0.2586349693182867,"score_spread":0.21604470513686946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367059780","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021806423,0.0013551771,0.2537485,0.007995144,0.006471184,0.00034187522,0.5705107,0.03687718,0.10089379],"genre_scores_gemma":[0.2692052,0.0027285556,0.20462413,0.0034421491,0.0026195932,0.0010563108,0.39889082,0.016146358,0.1012869],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996966,0.000027165535,0.000021546344,0.00009369746,0.00011420844,0.000046850982],"domain_scores_gemma":[0.9984403,0.0005188823,0.00012778734,0.00036774564,0.00040423253,0.00014104843],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005673279,0.0011751372,0.0007201586,0.0013332062,0.001344893,0.0020753893,0.0025949355,0.002591746,0.3604269],"category_scores_gemma":[0.0037241632,0.0007900444,0.0011678721,0.0012420109,0.00034133473,0.0025658768,0.0010572956,0.0014394905,0.057784997],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016885648,0.000131396,0.0027864273,0.0010999428,0.00009846081,0.0006088473,0.00014347155,0.0039162114,0.021463662,0.056391265,0.8821428,0.031048682],"study_design_scores_gemma":[0.00043554083,0.00016989786,0.024075357,0.00076065946,0.0002454255,0.0028345059,0.0002720416,0.097910866,0.045916907,0.14902543,0.67814755,0.00020586328],"about_ca_topic_score_codex":0.0030043342,"about_ca_topic_score_gemma":0.002798295,"teacher_disagreement_score":0.3604269,"about_ca_system_score_codex":0.0007236083,"about_ca_system_score_gemma":0.0011017544,"threshold_uncertainty_score":0.9122734},"labels":[],"label_agreement":null},{"id":"W4367060155","doi":"10.1130/geol.s.22704853","title":"Supplemental Material: A mechanism for transient creep in crustal shear zones","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Creep; Shear zone; Transient (computer programming); Geology; Shear (geology); Mechanism (biology); Seismology; Petrology; Materials science; Composite material; Physics; Computer science; Programming language","score_opus":0.04259026418141727,"score_gpt":0.2586349693182867,"score_spread":0.21604470513686946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367060155","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021806423,0.0013551771,0.2537485,0.007995144,0.006471184,0.00034187522,0.5705107,0.03687718,0.10089379],"genre_scores_gemma":[0.2692052,0.0027285556,0.20462413,0.0034421491,0.0026195932,0.0010563108,0.39889082,0.016146358,0.1012869],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996966,0.000027165535,0.000021546344,0.00009369746,0.00011420844,0.000046850982],"domain_scores_gemma":[0.9984403,0.0005188823,0.00012778734,0.00036774564,0.00040423253,0.00014104843],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005673279,0.0011751372,0.0007201586,0.0013332062,0.001344893,0.0020753893,0.0025949355,0.002591746,0.3604269],"category_scores_gemma":[0.0037241632,0.0007900444,0.0011678721,0.0012420109,0.00034133473,0.0025658768,0.0010572956,0.0014394905,0.057784997],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016885648,0.000131396,0.0027864273,0.0010999428,0.00009846081,0.0006088473,0.00014347155,0.0039162114,0.021463662,0.056391265,0.8821428,0.031048682],"study_design_scores_gemma":[0.00043554083,0.00016989786,0.024075357,0.00076065946,0.0002454255,0.0028345059,0.0002720416,0.097910866,0.045916907,0.14902543,0.67814755,0.00020586328],"about_ca_topic_score_codex":0.0030043342,"about_ca_topic_score_gemma":0.002798295,"teacher_disagreement_score":0.3604269,"about_ca_system_score_codex":0.0007236083,"about_ca_system_score_gemma":0.0011017544,"threshold_uncertainty_score":0.9122734},"labels":[],"label_agreement":null},{"id":"W4367317438","doi":"10.1029/2022jb025912","title":"Viscoelastic Response of a Self‐Gravitational Spherical Earth to Shear Dislocation Obtained Using the Fixed‐Talbot Method","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Viscoelasticity; Laplace transform; Gravitation; Mechanics; Physics; Classical mechanics; Geometry; Geology; Mathematical analysis; Mathematics","score_opus":0.0669513335210434,"score_gpt":0.3846918266381111,"score_spread":0.31774049311706765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367317438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6513509,0.00014447322,0.3410769,0.0001906759,0.00005580817,0.000032919914,0.00007104506,0.00031236405,0.0067648464],"genre_scores_gemma":[0.97537506,0.00007130294,0.022713881,0.00003354831,0.0000051787515,0.000013157355,0.000040607047,0.00003983687,0.0017071923],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999521,0.000013434659,0.0000023046282,0.0000062539084,0.000016468857,0.000009457098],"domain_scores_gemma":[0.999846,0.000060640818,0.000022408729,0.000018365152,0.00004188454,0.000010753179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025329835,0.00038827502,0.00021335005,0.00041714916,0.0001622324,0.00042370922,0.00044690864,0.00055649446,0.0009998755],"category_scores_gemma":[0.00066906126,0.00010726812,0.0003618026,0.00032669512,0.00044148602,0.00040016565,0.0003565936,0.00034575124,0.00014362027],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011214992,0.0000979849,0.0037309134,0.000091415015,0.00005160773,0.00048338782,0.0003264617,0.8381063,0.08069302,0.039391056,0.00065513555,0.03626066],"study_design_scores_gemma":[0.0000037101413,0.000013076048,0.00034286754,0.0000031303543,0.0000028543602,0.000016471138,0.000015284155,0.9967854,0.001989857,0.00067668495,0.00014489495,0.000005825027],"about_ca_topic_score_codex":0.00337479,"about_ca_topic_score_gemma":0.0024271682,"teacher_disagreement_score":0.00337479,"about_ca_system_score_codex":0.00036930313,"about_ca_system_score_gemma":0.0003688844,"threshold_uncertainty_score":0.006710291},"labels":[],"label_agreement":null},{"id":"W4367320603","doi":"10.1038/s41467-023-38137-w","title":"Laboratory earthquakes decipher control and stability of rupture speeds","year":2023,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Oxford; National Natural Science Foundation of China; California Institute of Technology; Tianjin University; China Postdoctoral Science Foundation; University of California, Santa Cruz","keywords":"Nucleation; Jump; Geology; Seismology; Wave speed; Shear (geology); Earthquake rupture; Stability (learning theory); Computer science; Mechanics; Physics; Machine learning; Thermodynamics; Fault (geology)","score_opus":0.02213259121741914,"score_gpt":0.263021417163932,"score_spread":0.24088882594651287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367320603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958189,0.000035549634,0.002812237,0.00003078484,0.000008839354,0.000004059588,0.00008721476,0.0000813214,0.0011212752],"genre_scores_gemma":[0.99948287,0.000011271977,0.0003594334,0.0000037075479,0.0000016424444,0.0000028746733,0.000037373415,0.0000062808163,0.000094527284],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99991775,0.000014332128,0.0000047860876,0.000021651995,0.000020727894,0.000020784366],"domain_scores_gemma":[0.9995419,0.00015344271,0.00012936041,0.00009046725,0.00004187596,0.000042980977],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016218184,0.00015568873,0.00013366692,0.0002352872,0.0001097598,0.00035642437,0.0002710848,0.0002254806,0.0014599722],"category_scores_gemma":[0.0008818065,0.00010220313,0.00010764817,0.000120145065,0.00031291522,0.00027613895,0.0003668995,0.00031614833,0.00016027386],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063244416,0.00088771165,0.0680964,0.00012659057,0.000083845145,0.00072843116,0.00034544937,0.1625975,0.70836246,0.014976464,0.0022001017,0.040962525],"study_design_scores_gemma":[0.00008975003,0.0010941741,0.08043479,0.000017950057,0.000047483445,0.00032707976,0.00035134068,0.5712226,0.33776298,0.0063020545,0.002292264,0.000057510726],"about_ca_topic_score_codex":0.0005180099,"about_ca_topic_score_gemma":0.00038130916,"teacher_disagreement_score":0.0014599722,"about_ca_system_score_codex":0.0001999452,"about_ca_system_score_gemma":0.00009972622,"threshold_uncertainty_score":0.004884124},"labels":[],"label_agreement":null},{"id":"W4367676502","doi":"10.29169/1927-5129.2023.19.04","title":"Geodynamics of the Caucasus – Anatolian-Arabian region and Turkey-Syria Earthquakes 2023","year":2023,"lang":"en","type":"article","venue":"Journal of Basic & Applied Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geodynamics; Geology; Induced seismicity; Seismology; Lithosphere; Natural hazard; Volcanism; Natural (archaeology); Natural disaster; Eurasian Plate; Tectonics; Earth science; Subduction; Paleontology; Oceanography","score_opus":0.02305808610514971,"score_gpt":0.22527242614893614,"score_spread":0.20221434004378644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367676502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936719,0.00060563575,0.00010732918,0.0006726941,0.000034209883,0.000008840778,0.0007416004,0.000019330835,0.0041383607],"genre_scores_gemma":[0.99869627,0.00018312964,0.000053735217,0.000032268184,0.000012117614,0.0000034756042,0.00040230222,0.000004268613,0.0006123957],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999232,0.000012184379,0.0000075851895,0.0000125209235,0.000018832772,0.000025609394],"domain_scores_gemma":[0.9998634,0.000009806302,0.0000396575,0.000005752789,0.000044991266,0.000036447516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009909025,0.00017325183,0.0001696094,0.00058840995,0.0003586414,0.0008236039,0.00020662136,0.00038718237,0.0014562599],"category_scores_gemma":[0.0003574992,0.00008153176,0.00016311547,0.00059352117,0.00017131408,0.00029755535,0.0005739086,0.00020195394,0.00025646744],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002446123,0.00007455475,0.9489994,0.000090261674,0.00013463016,0.0020866876,0.0015568684,0.01038968,0.0031136672,0.0024074658,0.01016549,0.02073669],"study_design_scores_gemma":[0.0000110327055,0.000020208956,0.98441076,0.000020677347,0.000018488696,0.00034178706,0.001748766,0.008714967,0.00011967675,0.00038681008,0.0041944673,0.000012397261],"about_ca_topic_score_codex":0.04966435,"about_ca_topic_score_gemma":0.042451747,"teacher_disagreement_score":0.04966435,"about_ca_system_score_codex":0.00060949026,"about_ca_system_score_gemma":0.00056703616,"threshold_uncertainty_score":0.09875053},"labels":[],"label_agreement":null},{"id":"W4375853656","doi":"10.1130/g50867.1","title":"A mechanism for transient creep in crustal shear zones","year":2023,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Creep; Geology; Slip (aerodynamics); Brittleness; Shear (geology); Dislocation creep; Shear zone; Shearing (physics); Strain rate; Dislocation; Seismology; Geotechnical engineering; Mechanics; Petrology; Materials science; Tectonics; Composite material; Thermodynamics","score_opus":0.025002170613857202,"score_gpt":0.2329536645991152,"score_spread":0.207951493985258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4375853656","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87169874,0.0009297684,0.11879346,0.00035907142,0.00007816285,0.00005729149,0.00019705386,0.0013967289,0.006489777],"genre_scores_gemma":[0.9976852,0.0000958525,0.001539741,0.0000140312295,0.0000071798045,0.00001399117,0.000029562472,0.000013049714,0.0006014373],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9999229,0.0000055230953,0.000006957758,0.000029874689,0.000015332951,0.000019445595],"domain_scores_gemma":[0.9997968,0.00004391629,0.00005325459,0.000043249784,0.000032752985,0.00003002976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014632003,0.00027840337,0.00029110681,0.0005690934,0.0006171083,0.00055970874,0.0006935516,0.00053135544,0.0021828285],"category_scores_gemma":[0.0006020425,0.00021238334,0.0004939229,0.000277345,0.00046079585,0.0008667388,0.00046706374,0.00036826317,0.0002783617],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004205599,0.00025463404,0.069039606,0.00059373304,0.00015958239,0.0020759688,0.0009772718,0.16258024,0.6006302,0.07943985,0.0020328697,0.0817955],"study_design_scores_gemma":[0.00008089049,0.00055791717,0.060363043,0.00007912767,0.00009335084,0.0024915184,0.00036283906,0.8200841,0.08137833,0.029072935,0.0053532445,0.00008265427],"about_ca_topic_score_codex":0.0014099315,"about_ca_topic_score_gemma":0.0008939872,"teacher_disagreement_score":0.0021828285,"about_ca_system_score_codex":0.00053791073,"about_ca_system_score_gemma":0.0003464334,"threshold_uncertainty_score":0.007302344},"labels":[],"label_agreement":null},{"id":"W4376257165","doi":"10.2205/2023es000835","title":"Tectonic Activities Description in the Ongoing Collision Zone of the Eurasia-Arabia Plates Using 2D Surface Waves Tomography","year":2023,"lang":"en","type":"article","venue":"Rossijskij žurnal nauk o zemle/Russian journal of earth sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; International Institute of Earthquake Engineering and Seismology; Institute for Advanced Studies in Basic Sciences; University of Tehran","keywords":"Geology; Crust; Tectonics; Seismology; Seismic tomography; Underplating; Rayleigh wave; Tomography; Low-velocity zone; Volcano; Mantle (geology); Continental collision; Sedimentary rock; Surface wave; Inversion (geology); Paleontology; Geophysics; Subduction; Lithosphere","score_opus":0.03958895425926755,"score_gpt":0.2530235075204675,"score_spread":0.21343455326119992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376257165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97388726,0.00029402814,0.018727472,0.000078305085,0.000017704875,0.000052981395,0.0030327423,0.00028014972,0.0036293003],"genre_scores_gemma":[0.98524994,0.0002516185,0.011272366,0.000011318335,0.000008901392,0.00003197113,0.0021119055,0.00003958033,0.0010223533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998952,0.000009684121,0.000009681065,0.000029901195,0.000033742483,0.000021757733],"domain_scores_gemma":[0.99988115,0.00001869623,0.00003731457,0.0000097046395,0.00003829119,0.000014872537],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016305498,0.0004222562,0.00015051688,0.003235382,0.00015890812,0.00076549395,0.00023514478,0.00023258146,0.001091608],"category_scores_gemma":[0.00037161334,0.00024236359,0.00036146631,0.0024421993,0.0001945668,0.00041547813,0.00036764215,0.00021873537,0.00025907275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003203226,0.00017225662,0.6405146,0.00034647898,0.0002094244,0.0025422133,0.0028910297,0.09265304,0.10634241,0.0023285737,0.002986545,0.1486931],"study_design_scores_gemma":[0.000024586812,0.000036102723,0.81361866,0.000050744264,0.00006027059,0.0005814295,0.001172974,0.17395703,0.0067405174,0.00056299556,0.0031369987,0.000057628313],"about_ca_topic_score_codex":0.018932048,"about_ca_topic_score_gemma":0.02566999,"teacher_disagreement_score":0.018932048,"about_ca_system_score_codex":0.00024099025,"about_ca_system_score_gemma":0.0005108823,"threshold_uncertainty_score":0.03764367},"labels":[],"label_agreement":null},{"id":"W4376506252","doi":"10.1108/ijdrbe-06-2022-0058","title":"Tsunami-resilient building guidelines for Sri Lankan coastal belt: a critical review and consolidation based on significant institutional perceptions","year":2023,"lang":"en","type":"review","venue":"International Journal of Disaster Resilience in the Built Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"George Brown College","funders":"","keywords":"Guideline; Built environment; Environmental planning; Local government; Sri lanka; Best practice; Capacity building; Environmental resource management; Civil engineering; Engineering; Geography; Political science; Environmental science","score_opus":0.1254217555132059,"score_gpt":0.3901876832100445,"score_spread":0.2647659276968386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376506252","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20816441,0.45408946,0.052333355,0.16909297,0.012784505,0.027926099,0.0029826579,0.00051274896,0.07211385],"genre_scores_gemma":[0.52048564,0.32370183,0.123471,0.01183342,0.00093308755,0.009751522,0.002360933,0.00021613519,0.007246529],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.955296,0.02044897,0.01083498,0.0016898129,0.010369608,0.0013606176],"domain_scores_gemma":[0.8395967,0.05917105,0.008299183,0.0034768463,0.0867679,0.002688353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.07311103,0.0010287978,0.0012997474,0.019851249,0.0038648392,0.007078007,0.00377645,0.0023623393,0.0017374015],"category_scores_gemma":[0.11888991,0.0008294078,0.001254653,0.014323223,0.005391636,0.0062294225,0.0050694076,0.004080242,0.00038066486],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013414315,0.00031786435,0.015664464,0.082578145,0.0002568369,0.005818961,0.18939912,0.0015835561,0.0051426864,0.03931187,0.07517654,0.5846159],"study_design_scores_gemma":[0.00003395698,0.0003462286,0.015543901,0.15400851,0.0007146886,0.0015399124,0.261132,0.0011410974,0.0029969262,0.005921452,0.5563502,0.00027108766],"about_ca_topic_score_codex":0.023593975,"about_ca_topic_score_gemma":0.046562027,"teacher_disagreement_score":0.07311103,"about_ca_system_score_codex":0.013202965,"about_ca_system_score_gemma":0.08276669,"threshold_uncertainty_score":0.3866527},"labels":[],"label_agreement":null},{"id":"W4376608815","doi":"10.1038/s41598-023-33310-z","title":"Tectonic evolution of the Nootka fault zone and deformation of the shallow subducted Explorer plate in northern Cascadia as revealed by earthquake distributions and seismic tomography","year":2023,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Ocean Networks Canada Society; University of Victoria","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada; Natural Resources Canada; U.S. Geological Survey","keywords":"Geology; Seismology; Subduction; Lineation; Induced seismicity; Aftershock; Transform fault; Fault (geology); Seismometer; Focal mechanism; Plate tectonics; Pacific Plate; Seismic tomography; Tectonics; Geophysics; Mantle (geology)","score_opus":0.008394282772371794,"score_gpt":0.19493749049527345,"score_spread":0.18654320772290167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376608815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99954826,0.000019017109,0.0000296385,0.000009486722,4.80619e-7,0.0000013915397,0.000118272364,0.000005149982,0.00026832864],"genre_scores_gemma":[0.99960524,0.000022035187,0.00005340432,0.0000024436747,6.366583e-7,0.0000025043673,0.00015972424,0.0000016407198,0.00015243974],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989533,0.000010659323,0.000008122188,0.000039940212,0.000025102849,0.00002080524],"domain_scores_gemma":[0.99962425,0.000031320014,0.00012151897,0.000036808782,0.000057889567,0.00012808025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015965688,0.00025219706,0.00019047906,0.000970871,0.00035129543,0.00039275474,0.00021682048,0.00020105246,0.00067847554],"category_scores_gemma":[0.00052846933,0.00018688962,0.0001666221,0.00081290863,0.0004712936,0.00018055868,0.0004767894,0.00014190045,0.00010109504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009080825,0.0000187238,0.981806,0.000020546977,0.000045118915,0.00034940176,0.000888052,0.0018314876,0.011720057,0.000069379064,0.000120854034,0.0030394949],"study_design_scores_gemma":[0.0000014510762,0.0000055579826,0.9993401,0.000001698186,0.0000038056555,0.000024466111,0.00012892594,0.0003355811,0.00007704293,0.000005503309,0.000073983996,0.0000018680189],"about_ca_topic_score_codex":0.099217616,"about_ca_topic_score_gemma":0.21262713,"teacher_disagreement_score":0.099217616,"about_ca_system_score_codex":0.0008717983,"about_ca_system_score_gemma":0.00054793135,"threshold_uncertainty_score":0.19728023},"labels":[],"label_agreement":null},{"id":"W4376868394","doi":"10.21203/rs.3.rs-2687050/v1","title":"Environmental effects following a seismic sequence: the 2019 Cotabato - Davao del Sur (Philippines) earthquakes","year":2023,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Sequence (biology); Seismology; Geology; Geography; Biology","score_opus":0.06522495749256375,"score_gpt":0.3197774660935398,"score_spread":0.25455250860097606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4376868394","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959935,0.000045200355,0.0000500975,0.0005318394,0.000012579702,0.0000047367103,0.0011806661,0.000008241698,0.0021731968],"genre_scores_gemma":[0.9988142,0.00007579419,0.000028210214,0.000023128778,0.000010276084,0.0000022224651,0.0005040875,0.000004767207,0.0005371946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988794,0.000025295278,0.0000065143813,0.000019783365,0.000016712254,0.000043729462],"domain_scores_gemma":[0.99910694,0.00017120018,0.0002549061,0.00004227685,0.00023576198,0.00018895311],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028262194,0.0002303683,0.00015474478,0.0005463007,0.0006036064,0.0008755152,0.00024831956,0.00062119536,0.00593322],"category_scores_gemma":[0.0021232804,0.0001501124,0.00015332771,0.0012802015,0.0004064086,0.0005057814,0.0007750021,0.00050459726,0.00042732828],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007828637,0.00029521235,0.9439678,0.00010449207,0.00024007529,0.0026582622,0.0019385407,0.024048539,0.003149453,0.0015435971,0.00583343,0.015437657],"study_design_scores_gemma":[0.000007705977,0.00004432695,0.99343324,0.000009915036,0.000029423965,0.000043533644,0.0019632035,0.002967981,0.00021918325,0.00021246521,0.0010599226,0.0000092064665],"about_ca_topic_score_codex":0.13668396,"about_ca_topic_score_gemma":0.2419896,"teacher_disagreement_score":0.13668396,"about_ca_system_score_codex":0.0010341929,"about_ca_system_score_gemma":0.0006170904,"threshold_uncertainty_score":0.27177668},"labels":[],"label_agreement":null},{"id":"W4377088658","doi":"10.1002/9781119773856.ch1","title":"When Plates Collide","year":2023,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Oxford; University of Alberta","keywords":"Plate tectonics; Geology; Subduction; Tectonics; Geodynamics; Seismology; Convergent boundary; Geophysics; Oceanic crust","score_opus":0.013908226543045516,"score_gpt":0.20713888041350356,"score_spread":0.19323065387045804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377088658","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32993037,0.0030859963,0.005180405,0.0043805,0.002588296,0.00013081642,0.0035803046,0.0007467388,0.6503766],"genre_scores_gemma":[0.86958796,0.0017643732,0.0025830073,0.001348671,0.00058980775,0.000094833274,0.0043211672,0.0003865817,0.11932364],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99886215,0.00011889414,0.000056216373,0.00022996611,0.00038949845,0.0003433341],"domain_scores_gemma":[0.99851745,0.00030434548,0.00040392694,0.00020189869,0.00026404698,0.00030845677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005721677,0.00044764258,0.00044323772,0.0016385885,0.0017190522,0.00431401,0.00085464487,0.0012059865,0.059805524],"category_scores_gemma":[0.004223458,0.00040008538,0.000396877,0.0014309831,0.0014485829,0.0026185676,0.0033569853,0.0012536747,0.022580197],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016196057,0.00014009255,0.30837792,0.0010141575,0.00028396095,0.024800377,0.019282255,0.004235513,0.0133722685,0.09456526,0.21668431,0.31562418],"study_design_scores_gemma":[0.000069112924,0.0003181709,0.2892294,0.00074253813,0.0001545176,0.01231006,0.050814122,0.0019337633,0.006648212,0.042093918,0.5954909,0.00019531498],"about_ca_topic_score_codex":0.004811202,"about_ca_topic_score_gemma":0.008173251,"teacher_disagreement_score":0.059805524,"about_ca_system_score_codex":0.0009463022,"about_ca_system_score_gemma":0.00078408106,"threshold_uncertainty_score":0.20006943},"labels":[],"label_agreement":null},{"id":"W4377990013","doi":"10.1038/s41586-023-05985-x","title":"Dynamics, interactions and delays of the 2019 Ridgecrest rupture sequence","year":2023,"lang":"en","type":"article","venue":"Nature","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geodetic datum; Seismology; Earthquake rupture; Geology; Fault (geology); Earthquake simulation; Sequence (biology); Seismic hazard; Geodesy","score_opus":0.013124116952713712,"score_gpt":0.2474471380976121,"score_spread":0.2343230211448984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377990013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983901,0.000059437534,0.000056256078,0.00016597348,0.0000064307605,0.0000014554622,0.0002684114,0.0000036842496,0.0010482857],"genre_scores_gemma":[0.99950314,0.000023183433,0.0000166055,0.000007203342,0.0000047437547,0.0000011052215,0.00018877904,0.0000012171893,0.00025385467],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986374,0.000019865543,0.000011741044,0.00003749403,0.000026078771,0.000041029776],"domain_scores_gemma":[0.99856013,0.00033343473,0.0006397571,0.000049846043,0.00018732464,0.00022956662],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044181818,0.000095403906,0.00012574368,0.0006837265,0.000358627,0.00085111085,0.00026070394,0.00045776885,0.0034041828],"category_scores_gemma":[0.0034834987,0.00013689647,0.000104500024,0.0005774496,0.00033221763,0.00046166507,0.00056973385,0.00046285478,0.00044830106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069312216,0.000102704405,0.9729666,0.00003207729,0.0000857558,0.00026696338,0.0011864376,0.0038458728,0.0037300712,0.0028325403,0.0016407578,0.012617061],"study_design_scores_gemma":[0.0000057509055,0.000042708438,0.99520916,0.000008011869,0.000012527838,0.000055705226,0.0006206638,0.002773235,0.00014454818,0.00029256704,0.00082808186,0.000006980537],"about_ca_topic_score_codex":0.024788342,"about_ca_topic_score_gemma":0.055897117,"teacher_disagreement_score":0.024788342,"about_ca_system_score_codex":0.00076541404,"about_ca_system_score_gemma":0.0005165144,"threshold_uncertainty_score":0.049288154},"labels":[],"label_agreement":null},{"id":"W4378364463","doi":"10.1016/j.jobe.2023.106884","title":"Earthquake response of historical church within the perspective of structural dynamics: Oltu Russian Church","year":2023,"lang":"en","type":"article","venue":"Journal of Building Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Atatürk Üniversitesi; Mount Allison University","keywords":"Microtremor; Seismology; Modal; Response spectrum; Amplification factor; Structural engineering; Acceleration; Geology; Damping ratio; Displacement (psychology); Geotechnical engineering; Engineering; Vibration; Bandwidth (computing); Physics; Materials science; Acoustics","score_opus":0.013041823066347494,"score_gpt":0.2310842915410154,"score_spread":0.2180424684746679,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378364463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980228,0.000015292071,0.000047000853,0.000050993163,0.0000039811557,0.0000015616382,0.000037079142,0.0000013044803,0.0018200632],"genre_scores_gemma":[0.99945766,0.000017670738,0.000012236263,0.0000050147937,0.0000015399283,7.587513e-7,0.000036532234,8.56814e-7,0.00046780147],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999435,0.000011292065,0.000001930795,0.000008595664,0.000009634089,0.000025011386],"domain_scores_gemma":[0.99984705,0.00002468708,0.000019529089,0.000009036477,0.0000579334,0.000041677198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013943344,0.00008457683,0.0001436278,0.00019284009,0.00047142396,0.00045853053,0.00020673922,0.0003248094,0.0023765336],"category_scores_gemma":[0.000484519,0.000067182,0.000114172995,0.0003218318,0.00019670824,0.0001963666,0.0003941352,0.0002701691,0.00020147159],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009514745,0.00041991033,0.86835283,0.00014314613,0.00018302507,0.003378342,0.020195978,0.03034373,0.035462346,0.008235688,0.004392922,0.027940538],"study_design_scores_gemma":[0.0000052570635,0.00013076398,0.9731968,0.000015816822,0.000030612304,0.00009473139,0.015688026,0.007864128,0.0005365136,0.00026552702,0.0021629736,0.000008838348],"about_ca_topic_score_codex":0.016364595,"about_ca_topic_score_gemma":0.032386824,"teacher_disagreement_score":0.016364595,"about_ca_system_score_codex":0.00057222607,"about_ca_system_score_gemma":0.00026305567,"threshold_uncertainty_score":0.032538712},"labels":[],"label_agreement":null},{"id":"W4378376334","doi":"10.1785/0120220200","title":"Separating Primary and Secondary Mechanisms for Seismicity Induced by Hydraulic Fracturing","year":2023,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Aftershock; Geology; Seismology; Induced seismicity; Tectonics; Hydraulic fracturing; Fault (geology); Microseism; Borehole; Hydrogeology; Geotechnical engineering","score_opus":0.017887222497199495,"score_gpt":0.22089869091132627,"score_spread":0.2030114684141268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378376334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971433,0.00007112952,0.0017448395,0.000012484602,0.0000032923315,0.000019068453,0.00016412586,0.000023780733,0.0008179088],"genre_scores_gemma":[0.99929976,0.000025532308,0.00033184869,0.0000029688567,0.000003938283,0.0000043697632,0.00021371663,0.0000031672982,0.00011462097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997105,0.000028327824,0.000028224005,0.000055211036,0.00009297518,0.00008468539],"domain_scores_gemma":[0.9985316,0.00046584482,0.0004741884,0.00006584223,0.00027926255,0.00018325457],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033485336,0.00031666327,0.00021394671,0.0017449453,0.00022842934,0.00058815564,0.0002667814,0.00022430428,0.0016726594],"category_scores_gemma":[0.0015349063,0.000095744945,0.00025780528,0.0010808813,0.0004238197,0.00025384472,0.00047166264,0.00018720156,0.00016419939],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022544083,0.00007089279,0.9351499,0.00009750159,0.00012285326,0.00039900004,0.00059032644,0.0025135884,0.041945912,0.00057681266,0.0001685324,0.01813926],"study_design_scores_gemma":[0.0000016314777,0.00003753351,0.99530447,0.000005856716,0.000015606503,0.00005636844,0.00023316257,0.0029871278,0.0011367735,0.00009746171,0.00011998702,0.0000041036005],"about_ca_topic_score_codex":0.021262223,"about_ca_topic_score_gemma":0.04106891,"teacher_disagreement_score":0.021262223,"about_ca_system_score_codex":0.0005946454,"about_ca_system_score_gemma":0.00073356554,"threshold_uncertainty_score":0.04227692},"labels":[],"label_agreement":null},{"id":"W4378376398","doi":"10.1785/0220220341","title":"Fault Geometry, Slip Distribution, and Potential Triggering of the 2022 Mw 6.2 Deadly Afghanistan Earthquake Revealed from Geodetic and Weather Data","year":2023,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Interferometric synthetic aperture radar; Geology; Seismology; Slip (aerodynamics); Geodetic datum; Geodesy; Induced seismicity; Fault (geology); Seismic gap; Synthetic aperture radar; Remote sensing","score_opus":0.06658260038104216,"score_gpt":0.2969226893310697,"score_spread":0.23034008895002753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378376398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990984,0.00002266314,0.00007059631,0.000021409363,0.0000023182631,0.0000022512597,0.0005232582,0.000008623758,0.00025054096],"genre_scores_gemma":[0.9989372,0.000015615902,0.00009395409,0.0000041702037,0.000004391426,0.0000019817999,0.00087046274,0.0000018457191,0.00007034857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983037,0.000023226792,0.00001151135,0.000037635997,0.00003403737,0.00006304683],"domain_scores_gemma":[0.9996076,0.000054872784,0.00014847775,0.00003074605,0.00007654694,0.00008180794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022580245,0.00034568005,0.0002358813,0.0017833896,0.00031487082,0.0005031195,0.00023330127,0.00035141734,0.0008052806],"category_scores_gemma":[0.0007665367,0.00016465138,0.00017347035,0.001708287,0.00023202997,0.00036882656,0.00026176646,0.00017474467,0.00034473304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013423516,0.00005250998,0.983652,0.000011755509,0.000024431078,0.00064919225,0.00011891477,0.004221952,0.00493741,0.000074691256,0.00047095888,0.00565207],"study_design_scores_gemma":[0.0000050228605,0.000028886298,0.99264055,0.0000027926212,0.0000072433836,0.000147095,0.00016330714,0.0064763785,0.00031310285,0.00002711632,0.00018163513,0.0000067580822],"about_ca_topic_score_codex":0.015909899,"about_ca_topic_score_gemma":0.022103254,"teacher_disagreement_score":0.015909899,"about_ca_system_score_codex":0.00041749005,"about_ca_system_score_gemma":0.00024416926,"threshold_uncertainty_score":0.03163463},"labels":[],"label_agreement":null},{"id":"W4378965521","doi":"10.1029/2022tc007494","title":"Microplate Evolution in the Queen Charlotte Triple Junction &amp; Explorer Region: New Insights From Microseismicity","year":2023,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Geology; Seismology; Induced seismicity; Triple junction; Echelon formation; Seafloor spreading; Submarine pipeline; Plate tectonics; Pacific Plate; Lineation; Transform fault; Subduction; Hotspot (geology); Tectonics; Paleontology; Geophysics; Oceanography","score_opus":0.03813994028741286,"score_gpt":0.22614596298472314,"score_spread":0.1880060226973103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378965521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982315,0.00005872246,0.00018776585,0.000031272175,8.1875635e-7,0.0000041884778,0.0004103799,0.000009290542,0.0010661543],"genre_scores_gemma":[0.999111,0.000028900236,0.00021272713,0.000006594615,0.0000012117971,0.0000024558008,0.00039346417,0.0000044094395,0.00023917896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999887,0.000012027884,0.000004879437,0.000037730097,0.000032574546,0.000025817808],"domain_scores_gemma":[0.9997081,0.00004358517,0.00007677771,0.00002392321,0.00008971294,0.00005785369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001623957,0.00014799446,0.00014771122,0.001777047,0.00048363995,0.00088205613,0.00030308723,0.0002516823,0.0011237935],"category_scores_gemma":[0.0005847207,0.00011882206,0.00015556112,0.0018406291,0.0003257133,0.00021348638,0.00048452083,0.0001723351,0.00018336833],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044038014,0.000022918832,0.97683436,0.00002200059,0.00003460337,0.0003781355,0.0015135095,0.0021899818,0.007668799,0.00023410293,0.00038569415,0.010671933],"study_design_scores_gemma":[0.0000010954893,0.000003724086,0.9974298,0.0000039365336,0.0000032246246,0.000029904259,0.0004457496,0.0015990265,0.00011793664,0.000028163213,0.00033387681,0.000003616654],"about_ca_topic_score_codex":0.45802972,"about_ca_topic_score_gemma":0.66612756,"teacher_disagreement_score":0.45802972,"about_ca_system_score_codex":0.0012804199,"about_ca_system_score_gemma":0.0009831149,"threshold_uncertainty_score":0.9107274},"labels":[],"label_agreement":null},{"id":"W4379161800","doi":"10.1007/s00024-023-03301-2","title":"Introduction to “Sixty Years of Modern Tsunami Science, Volume 2: Challenges”","year":2023,"lang":"en","type":"editorial","venue":"Pure and Applied Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Geography; History; Oceanography; Geology","score_opus":0.009404984198671617,"score_gpt":0.20862433503347683,"score_spread":0.19921935083480521,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379161800","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000010481545,0.010283988,0.000092539325,0.03136505,0.9575416,0.000007573176,0.000033065942,0.000024257399,0.0006415195],"genre_scores_gemma":[0.000118227,0.005476914,0.00007279921,0.02451232,0.9667905,0.000014278583,0.000022768116,0.000027812057,0.002964422],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9928591,0.0013620737,0.0009590393,0.000901666,0.003441839,0.00047625948],"domain_scores_gemma":[0.9645929,0.017441025,0.0018932071,0.0007532385,0.011215369,0.0041043125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010602649,0.0042208377,0.004833746,0.005630583,0.004648138,0.0123958625,0.0039217803,0.015824249,0.014847439],"category_scores_gemma":[0.03423927,0.0012779065,0.003389624,0.002944418,0.004400464,0.008440585,0.003222924,0.027495334,0.01235524],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015660537,0.000006281392,0.000011207161,0.00013404399,0.000008904759,0.000028163518,0.000008313552,0.000012754869,0.000024868918,0.0002378629,0.9965848,0.0029271925],"study_design_scores_gemma":[0.000039938775,0.000019401594,0.0001859785,0.00056510826,0.000040979427,0.00013016108,0.00004739876,0.00008095314,0.000044924847,0.002181644,0.9966388,0.000024841771],"about_ca_topic_score_codex":0.0035327629,"about_ca_topic_score_gemma":0.011624389,"teacher_disagreement_score":0.015824249,"about_ca_system_score_codex":0.0036227303,"about_ca_system_score_gemma":0.007418352,"threshold_uncertainty_score":0.05607283},"labels":[],"label_agreement":null},{"id":"W4379471799","doi":"10.1038/s43247-023-00861-y","title":"Fault systems impede incision of the Yarlung river into the Tibetan plateau","year":2023,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Natural Science Foundation of China; Ministry of Science and Technology of the People's Republic of China; University of Melbourne; Australian Government","keywords":"Geology; Rift; Tectonics; Plateau (mathematics); Thermochronology; Fluvial; Geomorphology; Fault (geology); Erosion; Terrain; Paleontology; Earth science; Structural basin; Geography","score_opus":0.02645957386414561,"score_gpt":0.2287885985451427,"score_spread":0.2023290246809971,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379471799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998841,0.000099959165,0.00016063928,0.00002394606,0.0000018387532,0.0000016859626,0.00003460689,0.000011726786,0.00082467025],"genre_scores_gemma":[0.99977845,0.000030326848,0.000041500698,0.0000055923824,0.0000013800518,0.0000011131538,0.000026915493,0.0000014389915,0.000113268106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999362,0.000010728683,0.000005101845,0.00001684109,0.000009148784,0.00002189858],"domain_scores_gemma":[0.99978966,0.000043054653,0.00007683392,0.000015253003,0.000040370494,0.000034815886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025920247,0.00015155393,0.00016391109,0.0004651062,0.000388554,0.0006843637,0.00024675342,0.00024709478,0.002336813],"category_scores_gemma":[0.00053611054,0.0001222367,0.00013013007,0.00048873987,0.00048445916,0.00024216033,0.00032728649,0.00021705545,0.00013138361],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003483992,0.000065520544,0.8870953,0.00017295123,0.00008834277,0.00079393625,0.0013434659,0.0066656647,0.08232935,0.0014844951,0.00019657411,0.019416023],"study_design_scores_gemma":[0.000013405164,0.00006397498,0.99503434,0.000018245459,0.00001564794,0.00010407392,0.0004098027,0.0026526756,0.0009582072,0.00023984634,0.00048312172,0.000006614637],"about_ca_topic_score_codex":0.010631911,"about_ca_topic_score_gemma":0.016910497,"teacher_disagreement_score":0.010631911,"about_ca_system_score_codex":0.00057224924,"about_ca_system_score_gemma":0.00043177657,"threshold_uncertainty_score":0.021140039},"labels":[],"label_agreement":null},{"id":"W4379619395","doi":"10.5772/intechopen.110728","title":"New Insights into Major Seismic Events by Coulomb Stress Change Pattern and Aftershock Distributions – Implication for Active Tectonics","year":2023,"lang":"en","type":"book-chapter","venue":"IntechOpen eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Seismology; Aftershock; Geology; Fault (geology); Fault plane; Coulomb; Active fault; Seismic hazard; Focal mechanism; Slip (aerodynamics); Tectonics; Physics","score_opus":0.027468398469192787,"score_gpt":0.24746997745274468,"score_spread":0.22000157898355188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379619395","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19739851,0.22890395,0.107304245,0.0032105267,0.0018409771,0.000086816464,0.0029033099,0.0017865958,0.45656496],"genre_scores_gemma":[0.45135394,0.17564346,0.06330289,0.0009798293,0.0020423844,0.000062687344,0.005182907,0.00035178554,0.3010801],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999784,0.0000022212266,0.0000010569662,0.0000056983426,0.000010042065,0.0000025178797],"domain_scores_gemma":[0.9999572,0.000015187144,0.000005897139,0.0000045494435,0.000012034225,0.000005172204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000079419275,0.00035932532,0.00027050314,0.0010730318,0.00013049203,0.00094486575,0.00031317456,0.00029601777,0.008548573],"category_scores_gemma":[0.00013109516,0.00012177565,0.00019199084,0.0020216194,0.0002798308,0.0013400371,0.00026196317,0.00051265355,0.002719225],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006416546,0.000081154605,0.0072628674,0.0010997755,0.000040579875,0.0006835676,0.0010238325,0.0043469453,0.032258853,0.035560098,0.042635325,0.87494284],"study_design_scores_gemma":[0.000012664813,0.00020568405,0.12218916,0.00065025134,0.000089273744,0.0034584354,0.002735438,0.018496836,0.008057773,0.110196106,0.7338342,0.000074216994],"about_ca_topic_score_codex":0.0006532556,"about_ca_topic_score_gemma":0.002183162,"teacher_disagreement_score":0.008548573,"about_ca_system_score_codex":0.00024315774,"about_ca_system_score_gemma":0.00015421126,"threshold_uncertainty_score":0.028597891},"labels":[],"label_agreement":null},{"id":"W4379653876","doi":"10.22541/essoar.168614604.40356164/v1","title":"Dynamic rupture process of the Mw 7.8 Kahramanmaraş earthquake (SE Türkiye): Variable rupture speed and implications for seismic hazard","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Bilimsel Araştırma Projeleri Birimi, İstanbul Teknik Üniversitesi; Southern University of Science and Technology; Istanbul Teknik Üniversitesi; Chinese University of Hong Kong; National Natural Science Foundation of China; King Abdullah University of Science and Technology; Alexander von Humboldt-Stiftung","keywords":"Seismic hazard; Seismology; Geology; Hazard; Earthquake prediction; Chemistry","score_opus":0.02594001526197855,"score_gpt":0.2684771134245705,"score_spread":0.24253709816259192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379653876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978156,0.00010965559,0.00026797262,0.00010148412,0.000005997847,0.0000032496757,0.0004653856,0.000014222903,0.0012165338],"genre_scores_gemma":[0.99947804,0.000030300134,0.00004225111,0.0000039586816,0.0000034780132,0.000002029237,0.00024852873,0.000003507639,0.00018788688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999923,0.000009613518,0.000005197819,0.000025044386,0.000011237754,0.00002586618],"domain_scores_gemma":[0.999647,0.00008876496,0.00012131147,0.00003290737,0.000070103706,0.000039908024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002902411,0.00021124531,0.00020365481,0.0011328706,0.00029343466,0.00069998024,0.00037768815,0.000557567,0.003224056],"category_scores_gemma":[0.0017461709,0.00021393731,0.00018803054,0.0006935787,0.00029140202,0.00064901036,0.00056127086,0.00033674872,0.0005163003],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015405711,0.00024918665,0.806438,0.00013850041,0.00032774967,0.0032966458,0.0013848834,0.07936768,0.02824826,0.009508987,0.005668561,0.06383084],"study_design_scores_gemma":[0.000030433517,0.000147117,0.9386978,0.000025371837,0.000066291665,0.0005404256,0.0007138515,0.055129383,0.001519621,0.0016956034,0.001382762,0.00005137275],"about_ca_topic_score_codex":0.010813786,"about_ca_topic_score_gemma":0.008736951,"teacher_disagreement_score":0.010813786,"about_ca_system_score_codex":0.00045651474,"about_ca_system_score_gemma":0.00024976442,"threshold_uncertainty_score":0.02150166},"labels":[],"label_agreement":null},{"id":"W4379741058","doi":"10.1029/2023gc010910","title":"Long‐Term Offshore Borehole Fluid‐Pressure Monitoring at the Northern Cascadia Subduction Zone and Inferences Regarding the State of Megathrust Locking","year":2023,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada","funders":"National Science Board","keywords":"Geology; Subduction; Seismology; Borehole; Slip (aerodynamics); Moment magnitude scale; Seafloor spreading; Episodic tremor and slip; Submarine pipeline; Tectonics; Geophysics; Geotechnical engineering","score_opus":0.015429137276507934,"score_gpt":0.2137019633077597,"score_spread":0.19827282603125176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379741058","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99945694,0.000011568095,0.00008575688,0.0000094321185,0.000001146952,0.0000022488248,0.00014483492,0.000011596449,0.00027651156],"genre_scores_gemma":[0.99965227,0.000010094972,0.000094269155,0.000002070535,0.0000013840448,0.0000022669767,0.00015450979,0.0000013633048,0.00008163857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998154,0.00001982541,0.000013720236,0.000062480736,0.00005435025,0.000034285957],"domain_scores_gemma":[0.999508,0.00005355105,0.00012461374,0.000060860486,0.00013864701,0.000114292685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003554686,0.00030992366,0.00019519523,0.00062907144,0.00035505134,0.00031170127,0.00034669455,0.0002828775,0.00045190105],"category_scores_gemma":[0.00068823935,0.00017138923,0.00019700744,0.00046216854,0.00031531093,0.00032313014,0.00050866196,0.00018166252,0.00014993474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000098510376,0.00004621454,0.9704799,0.000016934257,0.00003106976,0.00028848439,0.000540835,0.0007031188,0.023762742,0.000028273776,0.00011449122,0.003889369],"study_design_scores_gemma":[0.0000014096127,0.000021807296,0.99905926,0.0000012683593,0.0000038001801,0.00001963519,0.00009624722,0.0004337311,0.00029518935,0.000004102451,0.00006139331,0.0000022739528],"about_ca_topic_score_codex":0.030755635,"about_ca_topic_score_gemma":0.055490904,"teacher_disagreement_score":0.030755635,"about_ca_system_score_codex":0.00045931817,"about_ca_system_score_gemma":0.00029176535,"threshold_uncertainty_score":0.061153233},"labels":[],"label_agreement":null},{"id":"W4379746034","doi":"10.1093/gji/ggad226","title":"<i>En echelon</i> faults reactivated by wastewater disposal near Musreau Lake, Alberta","year":2023,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Basic Energy Sciences; U.S. Department of Energy","keywords":"Overpressure; Geology; Seismology; Fault (geology); Earthquake magnitude; San andreas fault; Pore water pressure; Geotechnical engineering","score_opus":0.008695612311230592,"score_gpt":0.22524515653789676,"score_spread":0.21654954422666617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379746034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858754,0.00018276773,0.00088314357,0.00010671856,0.000008741399,0.000027326892,0.004453703,0.00017308856,0.008289184],"genre_scores_gemma":[0.99213976,0.00010301597,0.0012939669,0.000026495396,0.000004157431,0.000005867957,0.0032375066,0.000009811864,0.0031794382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990535,0.000003702058,0.0000040358977,0.000015033755,0.00004252406,0.00002933174],"domain_scores_gemma":[0.9997732,0.000016081549,0.0000406659,0.00001316901,0.00009953312,0.00005734264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009360967,0.0002462852,0.00014904441,0.0011677392,0.0005111624,0.00067359133,0.00035009847,0.00021936298,0.0020473853],"category_scores_gemma":[0.00032568755,0.00009528371,0.00014881804,0.0015157394,0.00027914465,0.00011175151,0.00027994957,0.00015385699,0.00034475277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003761581,0.00008895488,0.8125284,0.00017522312,0.00014105256,0.00067234196,0.00068451435,0.02552587,0.021555578,0.00052022014,0.0076677944,0.13006389],"study_design_scores_gemma":[0.000009312369,0.000017990644,0.9864659,0.00001436402,0.000014625801,0.00006104584,0.00047475807,0.008055235,0.001506793,0.000076342156,0.003291554,0.000012169527],"about_ca_topic_score_codex":0.86319363,"about_ca_topic_score_gemma":0.9536535,"teacher_disagreement_score":0.13680637,"about_ca_system_score_codex":0.002840876,"about_ca_system_score_gemma":0.00234575,"threshold_uncertainty_score":0.27522403},"labels":[],"label_agreement":null},{"id":"W4379879740","doi":"10.1016/j.geomorph.2023.108781","title":"Recent basement fault reactivation and fluvial drainage modification in an intraplate setting, eastern Bundelkhand Craton, Madhya Pradesh, India","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Monocline; Fluvial; Basement; Geomorphology; Fault (geology); Paleontology; Craton; Archean; Palaeochannel; Precambrian; Geochemistry; Structural basin; Tectonics","score_opus":0.030555739589969797,"score_gpt":0.26209779432215047,"score_spread":0.23154205473218067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379879740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992768,0.00007395892,0.000018765146,0.000036857837,0.0000019606593,0.0000026895611,0.00012946555,0.000001677748,0.00045792342],"genre_scores_gemma":[0.99948275,0.000071496455,0.000037499118,0.000011407228,0.0000021183635,0.0000020623195,0.00014249067,5.5990176e-7,0.00024946456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999094,0.000010775019,0.000010734864,0.000021242082,0.000015505391,0.00003237011],"domain_scores_gemma":[0.9997123,0.00004459653,0.000104212486,0.00001711371,0.00007034846,0.00005152598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000115846306,0.00013574104,0.000117365926,0.00089577184,0.00056219904,0.00057840894,0.00045152172,0.00022173623,0.00095872045],"category_scores_gemma":[0.00043177948,0.00016188873,0.00013790952,0.0020101068,0.000873505,0.0002503464,0.00049569795,0.000316669,0.00013521513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013608686,0.00005287856,0.97746474,0.00006921339,0.00004553442,0.0015370008,0.0066404925,0.0002096366,0.003986861,0.00019096842,0.0002397669,0.009426721],"study_design_scores_gemma":[0.0000016163034,0.000016088608,0.99772173,0.0000044808303,0.00000782717,0.00019548174,0.0016255019,0.00003462816,0.0000700424,0.000009244886,0.00031108956,0.0000022564705],"about_ca_topic_score_codex":0.11839688,"about_ca_topic_score_gemma":0.30150318,"teacher_disagreement_score":0.11839688,"about_ca_system_score_codex":0.00096226664,"about_ca_system_score_gemma":0.0010784047,"threshold_uncertainty_score":0.23541546},"labels":[],"label_agreement":null},{"id":"W4379985518","doi":"10.1029/2022jb025817","title":"A Mixed‐Flux‐Based Nodal Discontinuous Galerkin Method for 3D Dynamic Rupture Modeling","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Fault (geology); Discontinuous Galerkin method; Benchmark (surveying); Earthquake rupture; Boundary (topology); Computer science; Geometry; Mechanics; Geology; Mathematical analysis; Mathematics; Physics; Structural engineering; Engineering; Finite element method; Seismology","score_opus":0.07994624622892851,"score_gpt":0.3713197780327263,"score_spread":0.29137353180379777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379985518","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.029583607,0.00013924943,0.9679615,0.00008864622,0.00003377871,0.000042973305,0.00007034946,0.00028108808,0.0017987997],"genre_scores_gemma":[0.66199523,0.00021536944,0.33414665,0.00007670121,0.000035730896,0.00027757307,0.00017494122,0.00017087047,0.0029068221],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998622,0.00004967949,0.00000824217,0.000018888064,0.000048057424,0.000012975598],"domain_scores_gemma":[0.9997131,0.00014769529,0.0000318245,0.00001924827,0.00006544733,0.000022606842],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048949564,0.00059839356,0.00064619863,0.0005685637,0.0003747631,0.00067461823,0.0011572052,0.0010258538,0.0016936533],"category_scores_gemma":[0.00080770906,0.00043418803,0.00065212813,0.0003467539,0.0006041552,0.0005652487,0.0006666439,0.00072987675,0.00028207386],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003125546,0.000041933457,0.00058243447,0.000046045367,0.000022291772,0.000053909807,0.00004470277,0.9773842,0.0042325007,0.0045103943,0.00022242877,0.012827992],"study_design_scores_gemma":[0.0000015990017,0.000002763362,0.000014301593,9.673136e-7,7.5650365e-7,0.0000015655386,0.0000011684698,0.9996113,0.00012560587,0.00014299405,0.000096021715,0.0000011105969],"about_ca_topic_score_codex":0.0048210295,"about_ca_topic_score_gemma":0.0034669817,"teacher_disagreement_score":0.0048210295,"about_ca_system_score_codex":0.00053669745,"about_ca_system_score_gemma":0.0008211476,"threshold_uncertainty_score":0.009585917},"labels":[],"label_agreement":null},{"id":"W4380051223","doi":"10.3390/rs15122981","title":"Contemporaneous Thick- and Thin-Skinned Seismotectonics in the External Zagros: The Case of the 2021 Fin Doublet, Iran","year":2023,"lang":"en","type":"article","venue":"Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; International Institute of Earthquake Engineering and Seismology","keywords":"Geology; Seismology; Aftershock; Tectonics; Interferometric synthetic aperture radar; Synthetic aperture radar","score_opus":0.03039903390262591,"score_gpt":0.23754276076008385,"score_spread":0.20714372685745794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380051223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99931717,0.00005245005,0.00009465476,0.00005717214,0.0000039508263,0.0000034766042,0.00009962548,0.0000036775843,0.00036781383],"genre_scores_gemma":[0.9994368,0.00005320709,0.00014412627,0.00000786966,0.000006213658,0.000001466501,0.00022489554,0.0000014992977,0.00012389745],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998952,0.00000838609,0.0000074896066,0.000028085236,0.000019225885,0.00004161093],"domain_scores_gemma":[0.9998493,0.000011645996,0.00006253019,0.00001601381,0.000030453803,0.000029943256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022731043,0.00030125416,0.00022253198,0.0011144897,0.0004619164,0.0006049109,0.00057359884,0.00041822955,0.00077603373],"category_scores_gemma":[0.00049358053,0.00016053817,0.00023978311,0.0011851913,0.00046170663,0.00033147828,0.00043717498,0.00027506924,0.0001484739],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016432992,0.00008449554,0.9746279,0.00002516949,0.000049333776,0.0032974596,0.00063295854,0.0071375947,0.0014350569,0.0009112291,0.00045623526,0.01117817],"study_design_scores_gemma":[0.000018205825,0.00004483087,0.98633724,0.00001283674,0.000028179476,0.0005771518,0.0013552108,0.010152182,0.00015726367,0.00030651566,0.0010012521,0.000009178038],"about_ca_topic_score_codex":0.0655872,"about_ca_topic_score_gemma":0.1046625,"teacher_disagreement_score":0.0655872,"about_ca_system_score_codex":0.0010120696,"about_ca_system_score_gemma":0.00062282593,"threshold_uncertainty_score":0.13041085},"labels":[],"label_agreement":null},{"id":"W4380151857","doi":"10.1007/s11069-023-06040-8","title":"Submarine landslide tsunami hazard assessment for the western Makran based on a deterministic approach","year":2023,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Submarine landslide; Geology; Landslide; Submarine; Seismology; Hazard; Subduction; Natural hazard; Hazard analysis; Oceanography; Tectonics; Engineering","score_opus":0.025382875773576695,"score_gpt":0.279562675148158,"score_spread":0.25417979937458135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380151857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882451,0.00005887819,0.010363871,0.00005449088,0.000005673733,0.0000282692,0.00022153386,0.000029547793,0.0009926783],"genre_scores_gemma":[0.9968015,0.000035518326,0.0026836835,0.0000040860114,0.000003029634,0.00001657117,0.000105208725,0.000002930681,0.00034755058],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988353,0.000036815658,0.000010567214,0.00003097946,0.000014448904,0.000023592194],"domain_scores_gemma":[0.9996767,0.00014664474,0.00006254933,0.000021484504,0.000069434296,0.000023127828],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032133269,0.00037294102,0.0003577745,0.0007554798,0.00050603336,0.00052032183,0.0005809161,0.00031428214,0.0010130063],"category_scores_gemma":[0.00088995614,0.00037161476,0.0005619298,0.00036698752,0.00020998338,0.0002843124,0.00044935656,0.00021036554,0.00008167082],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001103338,0.000068197856,0.04546496,0.000049617644,0.000088250534,0.00020950999,0.000087777385,0.9402182,0.0015886644,0.0016737311,0.00013738834,0.010303384],"study_design_scores_gemma":[0.00000821419,0.000029111889,0.013844682,0.000003065209,0.00002507444,0.000012101052,0.00004815502,0.9855173,0.00012794691,0.00029394956,0.00008281113,0.000007518652],"about_ca_topic_score_codex":0.062189948,"about_ca_topic_score_gemma":0.11152153,"teacher_disagreement_score":0.062189948,"about_ca_system_score_codex":0.0013077571,"about_ca_system_score_gemma":0.0015500106,"threshold_uncertainty_score":0.123655915},"labels":[],"label_agreement":null},{"id":"W4380591020","doi":"10.22541/essoar.168677203.35280987/v1","title":"Injected fluid volume controls seismicity migration in earthquake swarms through aseismic crack propagation","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Agence Nationale de la Recherche","keywords":"Induced seismicity; Geology; Seismology; Seismic moment; Slip (aerodynamics); Fluid dynamics; Fluid pressure; Geothermal gradient; Front (military); Fault (geology); Mechanics; Geophysics; Physics; Thermodynamics","score_opus":0.03522271359675718,"score_gpt":0.247654811316245,"score_spread":0.21243209771948782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380591020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965153,0.00005152988,0.0030100862,0.000020915639,0.0000017867817,0.0000025580775,0.00002129544,0.000031280753,0.000345258],"genre_scores_gemma":[0.99972314,0.000020445726,0.00016637336,0.0000015322848,7.330895e-7,9.514065e-7,0.000007674662,0.000004046951,0.000075188625],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994206,0.000011829972,0.000004930253,0.000014912203,0.000009417942,0.000016931373],"domain_scores_gemma":[0.99951196,0.0001753594,0.0002003888,0.000019571682,0.000034064644,0.000058671918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012709163,0.00023753336,0.00019627732,0.0005500365,0.00014003142,0.00058207166,0.00024155917,0.00040168528,0.00058766815],"category_scores_gemma":[0.0011163014,0.00023392272,0.0002341519,0.00019130921,0.0005415079,0.00036216722,0.00034126558,0.00019677727,0.00008528223],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004998272,0.0002781175,0.10910163,0.00010896567,0.000098952434,0.0011859795,0.00045997548,0.31454304,0.55206805,0.003998328,0.0002477773,0.017409258],"study_design_scores_gemma":[0.00002901439,0.00015174817,0.077687025,0.00000816333,0.000030323998,0.0001607803,0.00013419753,0.89747125,0.022877868,0.0012571863,0.00016573284,0.000026704238],"about_ca_topic_score_codex":0.0038498149,"about_ca_topic_score_gemma":0.0021140873,"teacher_disagreement_score":0.0038498149,"about_ca_system_score_codex":0.00036410568,"about_ca_system_score_gemma":0.00019894872,"threshold_uncertainty_score":0.007654786},"labels":[],"label_agreement":null},{"id":"W4380684614","doi":"10.3389/fams.2023.1126511","title":"Testing the forecasting skills of aftershock models using a Bayesian framework","year":2023,"lang":"en","type":"article","venue":"Frontiers in Applied Mathematics and Statistics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Markov chain Monte Carlo; Bayesian probability; Statistics; Statistical hypothesis testing; Bayesian inference; Econometrics; Markov chain; Computer science; Mathematics; Geology; Seismology","score_opus":0.04529279953527786,"score_gpt":0.23668239434663738,"score_spread":0.19138959481135953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380684614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9334691,0.00017997272,0.06383485,0.00033556667,0.000018254232,0.00005209548,0.00022979687,0.00016817013,0.0017122299],"genre_scores_gemma":[0.9895369,0.000081662125,0.009798895,0.000025212219,0.00001702492,0.000021563344,0.0003424398,0.000011989431,0.00016443977],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9973405,0.0016148026,0.00013723908,0.00036582435,0.00036347698,0.00017822566],"domain_scores_gemma":[0.9556789,0.038540546,0.0022074764,0.0015729895,0.0013679032,0.0006322834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.014316285,0.0007392467,0.00076232944,0.0017056357,0.00040020343,0.0011621442,0.0011461541,0.0010669068,0.001182478],"category_scores_gemma":[0.045098174,0.00043714038,0.00084848405,0.00084316643,0.00057744194,0.002595402,0.0010991995,0.0011169821,0.00018543711],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048670545,0.00030180163,0.07314844,0.00008351639,0.00029423603,0.00009540127,0.0002677417,0.86154026,0.0011721521,0.008808262,0.00075293035,0.05304869],"study_design_scores_gemma":[0.000018970046,0.000079278005,0.0056463787,0.000008262855,0.000016890936,0.000008956526,0.00004938569,0.99133915,0.00028966818,0.002448354,0.00008343271,0.000011288277],"about_ca_topic_score_codex":0.0159387,"about_ca_topic_score_gemma":0.011138429,"teacher_disagreement_score":0.0159387,"about_ca_system_score_codex":0.0008450545,"about_ca_system_score_gemma":0.0017300245,"threshold_uncertainty_score":0.07571268},"labels":[],"label_agreement":null},{"id":"W4380887040","doi":"10.21203/rs.3.rs-2998116/v1","title":"Bayesian inference elucidates fault-system anatomy and resurgent earthquakes induced by continuing saltwater disposal","year":2023,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of Calgary","funders":"","keywords":"Inference; Fault (geology); Bayesian inference; Bayesian probability; Geology; Seismology; Geography; Computer science; Artificial intelligence","score_opus":0.05642167462302631,"score_gpt":0.34393201666068307,"score_spread":0.28751034203765674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380887040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9845449,0.00003780866,0.013477982,0.00010173079,0.0000018441965,0.000008661032,0.0002705966,0.000053807344,0.0015026544],"genre_scores_gemma":[0.998514,0.000013521252,0.0010986711,0.000005393792,0.0000014265246,8.317227e-7,0.00014883687,0.0000047371445,0.00021261178],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99975365,0.000048952123,0.000011771164,0.00008105095,0.000060121027,0.000044460998],"domain_scores_gemma":[0.99866843,0.0005893387,0.00024967507,0.00010821012,0.00028166114,0.00010268947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069696986,0.00014268456,0.00019918883,0.0006365199,0.0002946224,0.00064596004,0.00029494334,0.0002533319,0.001382885],"category_scores_gemma":[0.0044572703,0.00020740555,0.00022825757,0.00039076307,0.0005613664,0.00034260002,0.000400967,0.00031271004,0.00016547376],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027638685,0.000053089407,0.79298097,0.00004762531,0.00021297926,0.0003880855,0.0007935017,0.12552193,0.02670842,0.0066659213,0.0006404443,0.045710612],"study_design_scores_gemma":[0.000015243099,0.00003195476,0.7162141,0.000012061769,0.000054138098,0.0000780916,0.0003226075,0.27655822,0.0022241022,0.0037590545,0.00070417376,0.000026179347],"about_ca_topic_score_codex":0.17922093,"about_ca_topic_score_gemma":0.26562783,"teacher_disagreement_score":0.17922093,"about_ca_system_score_codex":0.0012517548,"about_ca_system_score_gemma":0.0010930086,"threshold_uncertainty_score":0.3563555},"labels":[],"label_agreement":null},{"id":"W4381279927","doi":"10.22541/essoar.167525181.10212724/v2","title":"When Plates Collide","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Oxford; University of Alberta","keywords":"Plate tectonics; Geology; Subduction; Tectonics; Geodynamics; Seismology; Convergent boundary; Oceanic crust","score_opus":0.05422123597547404,"score_gpt":0.24275964500291544,"score_spread":0.1885384090274414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381279927","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.55424845,0.0027569688,0.011934815,0.0034570477,0.0023350008,0.00013918556,0.0035760042,0.0011883244,0.42036423],"genre_scores_gemma":[0.9378455,0.0008826355,0.0028253484,0.00069767935,0.00040137628,0.000081157326,0.0033662396,0.00039193858,0.053508088],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986608,0.00010760183,0.0000663752,0.0003326901,0.00039843807,0.0004340525],"domain_scores_gemma":[0.9979219,0.00041188835,0.00054758746,0.0003417512,0.00033105438,0.0004458024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061437325,0.00053770497,0.0006617599,0.0018531706,0.0019865865,0.005074155,0.0010157368,0.0015861086,0.055785153],"category_scores_gemma":[0.0050826934,0.00060039986,0.0005091951,0.0014614584,0.0016431191,0.0036759686,0.004066125,0.0014829809,0.019527363],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027237935,0.00020058505,0.30636442,0.001335557,0.00053998653,0.026813935,0.020223033,0.0113784,0.029431356,0.17228162,0.15047248,0.2782349],"study_design_scores_gemma":[0.00013204593,0.0006139889,0.34640473,0.00074091996,0.00034201244,0.015556204,0.05078505,0.007884232,0.017839422,0.109979585,0.4492787,0.00044297366],"about_ca_topic_score_codex":0.0033029828,"about_ca_topic_score_gemma":0.004110534,"teacher_disagreement_score":0.055785153,"about_ca_system_score_codex":0.0008740978,"about_ca_system_score_gemma":0.00074428244,"threshold_uncertainty_score":0.18661994},"labels":[],"label_agreement":null},{"id":"W4381511296","doi":"10.3390/geohazards4030013","title":"Probabilistic Tsunami Hazard Analysis for Vancouver Island Coast Using Stochastic Rupture Models for the Cascadia Subduction Earthquakes","year":2023,"lang":"en","type":"article","venue":"GeoHazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Subduction; Seismology; Geology; Hazard; Tsunami earthquake; Return period; Seismic hazard; Probabilistic logic; Geography; Statistics; Tectonics","score_opus":0.04032128509806295,"score_gpt":0.2548573924305723,"score_spread":0.21453610733250936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381511296","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.808991,0.00066342525,0.18043397,0.00056223734,0.000035607805,0.00007459514,0.0008305277,0.00023084763,0.008177826],"genre_scores_gemma":[0.99311745,0.0002743921,0.0031588783,0.000019183875,0.000011952913,0.000032206823,0.0003279236,0.00001605988,0.0030420574],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998331,0.000035145396,0.000009486449,0.00003755622,0.000041941727,0.000042663723],"domain_scores_gemma":[0.9995148,0.00020074495,0.000095179,0.000021300875,0.0001307435,0.000037240938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045247196,0.0007730681,0.00039128217,0.0006007808,0.00042174372,0.0009801525,0.0010177487,0.00067497196,0.001128489],"category_scores_gemma":[0.0011279925,0.00039857425,0.0007743591,0.0005199924,0.00036515898,0.00039936614,0.0005657875,0.0006998719,0.00018968215],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010285556,0.000010049849,0.0021542544,0.000006569259,0.000014947307,0.000072609495,0.000015154023,0.9948025,0.0003378989,0.0011086095,0.00010619419,0.0013610439],"study_design_scores_gemma":[0.0000011569732,0.0000032346006,0.00067083293,0.0000010540049,0.000003587619,0.0000073382976,0.0000069280236,0.99894327,0.000026642254,0.00027090588,0.00006222047,0.000002743589],"about_ca_topic_score_codex":0.2574257,"about_ca_topic_score_gemma":0.15272471,"teacher_disagreement_score":0.74257433,"about_ca_system_score_codex":0.0018444001,"about_ca_system_score_gemma":0.0018452395,"threshold_uncertainty_score":0.51185465},"labels":[],"label_agreement":null},{"id":"W4381738710","doi":"10.22541/essoar.168748485.58030882/v1","title":"Contrasting Styles of Salt-Tectonic Processes in the Ionian Zone (NW Greece and S Albania)","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Woodside; Petrobras; University of Crete; University of Texas at Austin; Department of Mechanical Engineering, University of Texas at Austin; Condor Petroleum","keywords":"Diapir; Geology; Tectonics; Salt tectonics; Geochemistry; Paleontology; Earth science","score_opus":0.04142712396322883,"score_gpt":0.24690334242880213,"score_spread":0.2054762184655733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381738710","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99582314,0.00008328605,0.000052191946,0.00002167332,0.0000014613044,0.00000423735,0.00009649758,0.0000049491946,0.0039124573],"genre_scores_gemma":[0.999342,0.00005223665,0.000056499604,0.0000038103658,0.0000014887607,0.000001649883,0.000084712876,0.0000024082517,0.00045515038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987066,0.000015715166,0.000015203509,0.00004235507,0.000020219628,0.00003575779],"domain_scores_gemma":[0.9998634,0.000014556992,0.000052122687,0.000015287871,0.00002784844,0.000026802994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001648127,0.00023936987,0.00022594589,0.0016240082,0.00028980584,0.00082851795,0.0002509704,0.00017519412,0.001976758],"category_scores_gemma":[0.0004128839,0.0001074151,0.00018161991,0.001467546,0.00088946585,0.00042736655,0.000770812,0.00010380531,0.00029447637],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005708422,0.000026987354,0.91002375,0.000112417285,0.00015287,0.0012240293,0.0053979056,0.0020604157,0.03731125,0.0028056935,0.00029000806,0.04002382],"study_design_scores_gemma":[0.0000055396868,0.000017025011,0.9979482,0.000005687435,0.000009652295,0.000098094926,0.0007467774,0.00018584849,0.00026091377,0.00013152616,0.0005872688,0.0000035920286],"about_ca_topic_score_codex":0.014278107,"about_ca_topic_score_gemma":0.020299219,"teacher_disagreement_score":0.014278107,"about_ca_system_score_codex":0.0008241542,"about_ca_system_score_gemma":0.0004033783,"threshold_uncertainty_score":0.02838999},"labels":[],"label_agreement":null},{"id":"W4382055310","doi":"10.1515/jag-2023-0004","title":"Modeling 3D crustal velocities in the vicinities of Alaska and the Bering sea","year":2023,"lang":"en","type":"article","venue":"Journal of Applied Geodesy","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Geodetic Survey","keywords":"Plate tectonics; Geodetic datum; Geology; Geodesy; Boundary (topology); North American Plate; Geospatial analysis; Tectonics; North American Datum of 1927; Geoid; Geography; Oceanography; Seismology; Geophysics; Remote sensing","score_opus":0.020847703192123115,"score_gpt":0.2136377193840898,"score_spread":0.19279001619196667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382055310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9840587,0.00016281282,0.010986627,0.00007813855,0.000030165258,0.000018277426,0.0007268451,0.0002170441,0.003721534],"genre_scores_gemma":[0.9937896,0.00010192113,0.004612229,0.0000051269813,0.0000041869353,0.0000083222685,0.0005041871,0.000023205394,0.0009511934],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999268,0.000014350147,0.0000069760767,0.000026369227,0.000014042626,0.000011336721],"domain_scores_gemma":[0.9998392,0.000051519255,0.000030396186,0.000011351999,0.00004353027,0.000023966082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024988997,0.0005630675,0.00022605665,0.0007537898,0.0004222001,0.00092974544,0.00036151166,0.000606007,0.0010594396],"category_scores_gemma":[0.0010494957,0.00038428657,0.00042202906,0.0005765483,0.00031174198,0.0005480183,0.00048931135,0.00030747446,0.00021032462],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035224177,0.000021389986,0.038671456,0.000016661907,0.00003062601,0.00010337078,0.00011160473,0.9526198,0.0010307187,0.00046637648,0.0001788787,0.006713974],"study_design_scores_gemma":[0.000010644662,0.000027593358,0.024284722,0.000020750344,0.000022622775,0.000026382351,0.00017605964,0.97328,0.0006937476,0.00040765878,0.0010302236,0.000019550806],"about_ca_topic_score_codex":0.1692491,"about_ca_topic_score_gemma":0.15507057,"teacher_disagreement_score":0.1692491,"about_ca_system_score_codex":0.00093761476,"about_ca_system_score_gemma":0.0008304671,"threshold_uncertainty_score":0.33652794},"labels":[],"label_agreement":null},{"id":"W4382999047","doi":"10.2139/ssrn.4489920","title":"Inquisition and Earthquake Processes","year":2023,"lang":"en","type":"article","venue":"SSRN Electronic Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Seismology; Geology; Forensic engineering; Geography; Engineering","score_opus":0.012882795179981412,"score_gpt":0.22167512003346757,"score_spread":0.20879232485348614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382999047","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47717878,0.0045635663,0.0066393926,0.015791655,0.00022489003,0.00007157245,0.000964996,0.00009897091,0.4944662],"genre_scores_gemma":[0.9416967,0.0016508668,0.00045695255,0.00034615223,0.00013892945,0.000013429397,0.00025289247,0.000037246362,0.05540673],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9994584,0.0002370339,0.000033073495,0.000096047035,0.000093394054,0.00008202617],"domain_scores_gemma":[0.9941399,0.003592179,0.00079801655,0.00042319673,0.00066266535,0.00038403366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017075017,0.00017304429,0.00027557585,0.0017025345,0.0012486884,0.0041556754,0.00046488128,0.0011190317,0.041062612],"category_scores_gemma":[0.0130078485,0.0002680695,0.00019618153,0.002500996,0.0020956246,0.0031910737,0.0014403906,0.0012172769,0.002626931],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027058745,0.00018072138,0.03922084,0.0001604187,0.00003969763,0.00044984618,0.0116257975,0.0016166494,0.00064219575,0.87490404,0.014044977,0.056844197],"study_design_scores_gemma":[0.00013711494,0.00019808376,0.17026193,0.0002053506,0.00010770202,0.0007484312,0.022354119,0.0066385763,0.0007022565,0.6184631,0.18011132,0.00007205075],"about_ca_topic_score_codex":0.0050302222,"about_ca_topic_score_gemma":0.0034108267,"teacher_disagreement_score":0.041062612,"about_ca_system_score_codex":0.0011106842,"about_ca_system_score_gemma":0.000581436,"threshold_uncertainty_score":0.13736814},"labels":[],"label_agreement":null},{"id":"W4383198643","doi":"10.3389/fams.2023.1152476","title":"How many strong earthquakes will there be tomorrow?","year":2023,"lang":"en","type":"article","venue":"Frontiers in Applied Mathematics and Statistics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Istituto Nazionale di Geofisica e Vulcanologia","keywords":"Poisson distribution; Negative binomial distribution; Akaike information criterion; Binomial distribution; Count data; Beta-binomial distribution; Statistics; Poisson binomial distribution; Mathematics; Distribution (mathematics); Quasi-likelihood; Moment tensor; Compound Poisson distribution; Poisson regression; Magnitude (astronomy); Physics; Mathematical analysis","score_opus":0.018716482066086268,"score_gpt":0.21458687675865215,"score_spread":0.1958703946925659,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383198643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9647955,0.0041585714,0.015282103,0.0054020565,0.00020600973,0.000024335615,0.0030661847,0.00007316824,0.0069920206],"genre_scores_gemma":[0.99513704,0.0011842046,0.000995633,0.00014960243,0.00013846338,0.000008221616,0.0010578568,0.000014745501,0.0013142717],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99973804,0.000047451213,0.000017326378,0.000111135334,0.000038022998,0.000048066857],"domain_scores_gemma":[0.997024,0.0015218558,0.00086939737,0.00013653222,0.00023399213,0.00021415268],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012010313,0.00020943291,0.00037225673,0.0010371528,0.00037102608,0.0011669446,0.00044282444,0.0005487886,0.0033578167],"category_scores_gemma":[0.009523699,0.00013174882,0.00021507981,0.0012113601,0.00058877654,0.0015020102,0.0003257245,0.00051157916,0.0008220945],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028383633,0.000046956677,0.8603773,0.00015771302,0.00023129622,0.00043874083,0.0008092275,0.008139823,0.00076275767,0.013637703,0.010419479,0.10469519],"study_design_scores_gemma":[0.000023852046,0.00014076111,0.905046,0.00009079323,0.00015999471,0.0010934884,0.004605504,0.041232742,0.0011709031,0.030802775,0.01556372,0.00006944722],"about_ca_topic_score_codex":0.008914619,"about_ca_topic_score_gemma":0.011643557,"teacher_disagreement_score":0.008914619,"about_ca_system_score_codex":0.00058075227,"about_ca_system_score_gemma":0.00029362048,"threshold_uncertainty_score":0.017725468},"labels":[],"label_agreement":null},{"id":"W4383747295","doi":"10.1139/cjes-2023-0057","title":"Seismicity at the intersection of the Coast Shear Zone and Anahim Volcanic Belt near Bella Coola, British Columbia, Canada","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Induced seismicity; Seismology; Shear zone; Volcanic belt; Volcano; Lithosphere; Batholith; Shear (geology); Transtension; Tectonics; Volcanic rock; Rift; Paleontology","score_opus":0.012155357745607906,"score_gpt":0.17899145319622567,"score_spread":0.16683609545061776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383747295","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9714604,0.0007221858,0.00018635028,0.00043238455,0.000022740942,0.00005928294,0.00903044,0.00007958341,0.018006757],"genre_scores_gemma":[0.98560727,0.00052841293,0.0005676466,0.00009000435,0.000007704785,0.00003355592,0.0046032113,0.000021404061,0.008540703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971336,0.000010679024,0.000009729216,0.00006537074,0.00008887293,0.00011190117],"domain_scores_gemma":[0.99921155,0.00002825596,0.000054853394,0.000018557983,0.00050993584,0.0001767691],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015866193,0.00037580688,0.00030369175,0.0025836246,0.003708761,0.0013942376,0.00078702555,0.000302935,0.0034994788],"category_scores_gemma":[0.00074178475,0.0002469111,0.00016076518,0.003858282,0.00065555103,0.00023548737,0.0008338943,0.0004983216,0.00041800196],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021199942,0.00007700321,0.918706,0.00020784048,0.000117500786,0.0008123064,0.004653382,0.0015438701,0.008575433,0.00076254347,0.020095527,0.044236574],"study_design_scores_gemma":[0.000007760499,0.000005952792,0.991751,0.000034055658,0.000014391346,0.000041720334,0.0025472674,0.0004580372,0.0002046817,0.000019791689,0.004902818,0.000012371546],"about_ca_topic_score_codex":0.99801147,"about_ca_topic_score_gemma":0.999624,"teacher_disagreement_score":0.019632904,"about_ca_system_score_codex":0.019632904,"about_ca_system_score_gemma":0.027473088,"threshold_uncertainty_score":0.14244735},"labels":[],"label_agreement":null},{"id":"W4383747376","doi":"10.1139/cjes-2023-0025","title":"Coseismic Coulomb stress changes on intraplate faults in the western Quebec seismic zone following three major earthquakes in the past century","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"McGill University; Western University; McMaster University","funders":"","keywords":"Intraplate earthquake; Seismology; Geology; Seismic hazard; Fault (geology); Stress field; Seismic gap; Magnitude (astronomy); Tectonics; Stress (linguistics); Finite element method","score_opus":0.026214828880806805,"score_gpt":0.2338805404117114,"score_spread":0.2076657115309046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383747376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99779177,0.00008916067,0.00007524597,0.000054142307,0.0000028467784,0.0000061773603,0.0004477356,0.00000919822,0.0015236713],"genre_scores_gemma":[0.9988605,0.00004970541,0.00004962707,0.000012130337,0.0000015000588,0.000002360975,0.00024504508,0.0000014091789,0.00077762053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998604,0.000005911089,0.0000059292684,0.000024225272,0.000052069525,0.000051338044],"domain_scores_gemma":[0.9995327,0.000026992098,0.000102996855,0.000014222671,0.00022896902,0.000094152136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001625466,0.00023159278,0.00019339306,0.00101686,0.00084266596,0.00078169303,0.00046202823,0.00032837476,0.0016150544],"category_scores_gemma":[0.0007205242,0.000090248715,0.00012145244,0.0012028528,0.0005574482,0.00019067204,0.0003571829,0.00024901234,0.00010701126],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016957245,0.000059595055,0.956404,0.000041247626,0.000089106004,0.00055956776,0.0012006985,0.0038653119,0.007395656,0.0003120093,0.0014353447,0.028467976],"study_design_scores_gemma":[0.0000019511021,0.000008549065,0.99828064,0.000004454331,0.0000058499663,0.00002110746,0.0002982163,0.0008235123,0.0001441773,0.000007151142,0.00040002223,0.000004462362],"about_ca_topic_score_codex":0.9716067,"about_ca_topic_score_gemma":0.98660177,"teacher_disagreement_score":0.028393328,"about_ca_system_score_codex":0.008991477,"about_ca_system_score_gemma":0.004058717,"threshold_uncertainty_score":0.06523806},"labels":[],"label_agreement":null},{"id":"W4383875820","doi":"10.1785/0220220374","title":"Earthquake Catalog Processing and Swarm Identification for the Pacific Northwest","year":2023,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Aftershock; Tectonics; Geology; Induced seismicity; Cluster analysis; Merge (version control); Identification (biology); Population; Computer science; Information retrieval; Machine learning","score_opus":0.08911301290155602,"score_gpt":0.3236370629395164,"score_spread":0.23452405003796037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383875820","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09550895,0.00032300228,0.029077737,0.0005274983,0.00013830877,0.0010186182,0.81893224,0.032992195,0.021481408],"genre_scores_gemma":[0.039644357,0.00022111225,0.074407965,0.000047524638,0.00003055173,0.00041824015,0.87880117,0.001346898,0.0050822576],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989214,0.000054442324,0.00014567314,0.00028880715,0.0004644292,0.00012533282],"domain_scores_gemma":[0.9938922,0.00051204255,0.0005707161,0.001452799,0.003136922,0.0004353889],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015548044,0.0007357867,0.0005298702,0.010516466,0.0012105895,0.0021669958,0.0013704258,0.00061742397,0.013718893],"category_scores_gemma":[0.0080646,0.00053687557,0.00068431546,0.012544289,0.00031126267,0.0015666456,0.002314341,0.0008388834,0.0075604604],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029910664,0.00019665499,0.11435663,0.000766175,0.00013153991,0.00054662244,0.00141953,0.0067848046,0.0063472264,0.005180697,0.4592261,0.40474492],"study_design_scores_gemma":[0.00013741298,0.00007236061,0.33246693,0.0003012288,0.00008120545,0.0003183758,0.0019444064,0.032959115,0.012371095,0.0028885275,0.61634034,0.000118962314],"about_ca_topic_score_codex":0.31603137,"about_ca_topic_score_gemma":0.39299077,"teacher_disagreement_score":0.31603137,"about_ca_system_score_codex":0.0020570809,"about_ca_system_score_gemma":0.007818163,"threshold_uncertainty_score":0.62838376},"labels":[],"label_agreement":null},{"id":"W4383894507","doi":"10.1002/essoar.10511713.3","title":"Potential Poroelastic Triggering of the 2020 M5.0 Mentone Earthquake in the Delaware Basin, Texas, by Shallow Injection Wells","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Poromechanics; Geology; Induced seismicity; Seismology; Stress field; Structural basin; Pore water pressure; Injection well; Seismic hazard; Fault (geology); Geotechnical engineering; Geomorphology; Engineering; Petroleum engineering; Porosity","score_opus":0.015923386706937995,"score_gpt":0.2177841448082292,"score_spread":0.2018607581012912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383894507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99923444,0.000016299937,0.00013386364,0.00003190159,0.000002661186,0.0000026018959,0.0000968152,0.000017141261,0.000464367],"genre_scores_gemma":[0.9997156,0.000015861739,0.00008823618,0.0000067585606,0.0000018794157,0.00000168821,0.00008920531,0.0000020325417,0.00007870269],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995637,0.0000050174112,0.0000030042097,0.0000118062935,0.0000064522596,0.000017347393],"domain_scores_gemma":[0.9999057,0.00002087434,0.000028025062,0.000008073797,0.000014831854,0.000022506832],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010580433,0.00036741034,0.00018806495,0.00029226203,0.0002575596,0.00048366183,0.00043654136,0.0004681,0.0008144427],"category_scores_gemma":[0.00038815345,0.00021118872,0.00034009153,0.00025086128,0.00027136202,0.00031200127,0.00037472576,0.00023070833,0.00007141977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039783356,0.0002682942,0.62639934,0.00009507235,0.00015517937,0.0019440943,0.00033276808,0.333302,0.025192544,0.0011232069,0.0010134958,0.009776192],"study_design_scores_gemma":[0.00008237078,0.00014751805,0.5005279,0.000029452109,0.00007631803,0.00012183008,0.00059118157,0.4943707,0.0032582877,0.000263089,0.0004853737,0.000045933422],"about_ca_topic_score_codex":0.04595355,"about_ca_topic_score_gemma":0.04154291,"teacher_disagreement_score":0.04595355,"about_ca_system_score_codex":0.00060970866,"about_ca_system_score_gemma":0.00052572886,"threshold_uncertainty_score":0.09137213},"labels":[],"label_agreement":null},{"id":"W4384202061","doi":"10.3390/en16145322","title":"Testing Hypotheses for Geological Controls on Hydraulic-Fracturing-Induced Seismicity in the Montney Formation, Canada","year":2023,"lang":"en","type":"article","venue":"Energies","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium","keywords":"Induced seismicity; Hydraulic fracturing; Geology; Statistical hypothesis testing; Seismology; Null hypothesis; Geotechnical engineering; Statistics; Mathematics","score_opus":0.0572410284821836,"score_gpt":0.23237096631898926,"score_spread":0.17512993783680567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384202061","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99862206,0.000016550848,0.0006832101,0.000040099243,0.0000013091218,0.000013557012,0.00023883472,0.00001503799,0.00036938954],"genre_scores_gemma":[0.99926454,0.000008939261,0.00031272447,0.000005169529,9.2206784e-7,0.0000031307563,0.00033516026,0.0000023384082,0.00006708885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99849904,0.00031486966,0.00009922944,0.00039577414,0.00035610638,0.00033497284],"domain_scores_gemma":[0.99227273,0.0046814326,0.000998308,0.00038073678,0.001106874,0.0005599922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022918514,0.00040960673,0.00034037046,0.00071410526,0.00095234055,0.0011672515,0.0012376928,0.0003922313,0.00095543324],"category_scores_gemma":[0.012042825,0.00021988209,0.00064127764,0.000978248,0.002195769,0.00046585832,0.0007332968,0.00045312743,0.0000557045],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005094482,0.00010324554,0.88859737,0.000033484223,0.00028735935,0.0003802528,0.00059686246,0.0934135,0.003480565,0.0024830713,0.00047550004,0.009639227],"study_design_scores_gemma":[0.00005421146,0.000081555154,0.7636561,0.000013988134,0.000065516775,0.000042134732,0.00087267946,0.2326167,0.0014852305,0.0006925976,0.00038566513,0.00003371084],"about_ca_topic_score_codex":0.9293637,"about_ca_topic_score_gemma":0.92002714,"teacher_disagreement_score":0.07063627,"about_ca_system_score_codex":0.010686985,"about_ca_system_score_gemma":0.012974686,"threshold_uncertainty_score":0.14210445},"labels":[],"label_agreement":null},{"id":"W4384209682","doi":"10.1007/978-3-030-85040-1_435","title":"Euler Poles of Tectonic Plates","year":2023,"lang":"en","type":"book-chapter","venue":"Encyclopedia of earth sciences series/Encyclopedia of earth sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Euler's formula; Geology; Mathematics; Geometry; Mathematical analysis","score_opus":0.024930277867286733,"score_gpt":0.23224030312808566,"score_spread":0.20731002526079892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384209682","genre_codex":"other","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0048580877,0.0038752817,0.022119356,0.00078416435,0.0011836143,0.00002474182,0.0004506194,0.00013682357,0.96656746],"genre_scores_gemma":[0.18251163,0.01249325,0.02815751,0.00036893683,0.0011458334,0.00007354,0.0013596686,0.00034126447,0.77354836],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99991226,0.000018782344,0.0000045765446,0.00001881953,0.000033862976,0.000011746229],"domain_scores_gemma":[0.9999218,0.000018058809,0.000009168024,0.0000114939285,0.000030150948,0.000009345459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016513346,0.00051034207,0.0001670177,0.001442945,0.0004883931,0.001647136,0.00027310752,0.0003177268,0.03455605],"category_scores_gemma":[0.00048696646,0.00029092233,0.00014590097,0.0009669514,0.00092074904,0.0018666943,0.00055309036,0.0014465427,0.0088711325],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008430325,0.0000024359115,0.00009099516,0.000036133504,0.0000014191037,0.000021723512,0.00016316735,0.0003219979,0.0003231638,0.9616728,0.0107945055,0.026563302],"study_design_scores_gemma":[0.000007743753,0.000010344651,0.00075903477,0.000055978788,0.0000037827886,0.00016142914,0.0001825256,0.0005647831,0.00046866646,0.4754163,0.5223643,0.000005065021],"about_ca_topic_score_codex":0.001491261,"about_ca_topic_score_gemma":0.0015473363,"teacher_disagreement_score":0.03455605,"about_ca_system_score_codex":0.0005984999,"about_ca_system_score_gemma":0.00034942877,"threshold_uncertainty_score":0.11560154},"labels":[],"label_agreement":null},{"id":"W4384934000","doi":"10.22541/essoar.168988434.40307775/v1","title":"Early Postseismic Deformation of the 29 July 2021 Mw8.2 Chignik Earthquake Provides New Constraints on the Downdip Coseismic Slip","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey; Institut de Physique du Globe de Paris; Istituto Nazionale di Geofisica e Vulcanologia; Natural Resources Canada; Nuclear Safety and Security Commission; College of Engineering, Michigan State University; National Aeronautics and Space Administration; California Institute of Technology; Michigan State University; National Science Foundation","keywords":"Geology; Slip (aerodynamics); Seismology; Viscoelasticity; Trench; Lithosphere; Subduction; Geodesy; Submarine pipeline; Inversion (geology); Tectonics; Geotechnical engineering","score_opus":0.03244417501501701,"score_gpt":0.22284567288985047,"score_spread":0.19040149787483346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384934000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944582,0.00011413071,0.0009304068,0.000083654755,0.000013701674,0.000004010759,0.0006393046,0.000054821176,0.0037016473],"genre_scores_gemma":[0.9985864,0.000057934067,0.00026509597,0.000012879314,0.000009793974,0.0000023169935,0.00075023074,0.000010405259,0.0003049502],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998895,0.000012158351,0.0000068850577,0.000028354196,0.000021916234,0.00004114996],"domain_scores_gemma":[0.99977106,0.00004715544,0.000041533098,0.0000336174,0.00006295706,0.0000437432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022233005,0.0005090054,0.00032067014,0.0008025229,0.00033268833,0.00046517048,0.0002521093,0.00030261918,0.002418254],"category_scores_gemma":[0.0006730067,0.00022177557,0.00029019598,0.0007233587,0.00020679459,0.00041468735,0.0004053531,0.0004552404,0.00038552884],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004386806,0.00027519456,0.85429466,0.00015339526,0.00014292556,0.0010117544,0.00054689834,0.03824102,0.055118043,0.0012340982,0.00222604,0.046317287],"study_design_scores_gemma":[0.000012419373,0.000051642328,0.9517168,0.000025102947,0.000037027643,0.00007640711,0.00024873947,0.04291976,0.0030610624,0.00021463246,0.0016104543,0.000025953008],"about_ca_topic_score_codex":0.036422346,"about_ca_topic_score_gemma":0.1100458,"teacher_disagreement_score":0.036422346,"about_ca_system_score_codex":0.0005530116,"about_ca_system_score_gemma":0.0005463418,"threshold_uncertainty_score":0.07242066},"labels":[],"label_agreement":null},{"id":"W4385146490","doi":"10.1038/s43247-023-00919-x","title":"Seafloor earthquake ruptures and mass wasting from the 2004 Mw 6.3 Les Saintes submarine earthquake","year":2023,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Agence Nationale de la Recherche; Centre National de la Recherche Scientifique; Flotte Océanographique Française","keywords":"Mass wasting; Geology; Seafloor spreading; Fault scarp; Seismology; Submarine; Subaerial; Bedrock; Fault (geology); Submarine landslide; Intraplate earthquake; Landslide; Tectonics; Paleontology; Oceanography","score_opus":0.034628183495047996,"score_gpt":0.2241078602806619,"score_spread":0.1894796767856139,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385146490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993581,0.000021444112,0.00007126868,0.000014384545,0.0000013930555,0.0000037038094,0.000099056204,0.000007162678,0.0004233998],"genre_scores_gemma":[0.99969494,0.000018614403,0.00006458128,0.0000037742516,0.0000022642516,0.0000012633552,0.000095094976,7.721528e-7,0.00011874862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999553,0.0000059664135,0.0000027255444,0.000008996524,0.000016492597,0.000010521011],"domain_scores_gemma":[0.99978465,0.000024472678,0.0001154284,0.000016499629,0.000027960805,0.000031018637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010331845,0.00017431198,0.0001386163,0.00059974764,0.00022655228,0.00024967847,0.000107848326,0.00025377286,0.00058935146],"category_scores_gemma":[0.0003434,0.000071562994,0.00011704049,0.0003946898,0.00022116172,0.0001451875,0.00033700117,0.00018255919,0.00008752495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024049921,0.000056480738,0.93840986,0.000051727224,0.000060925857,0.0028735676,0.00085704203,0.0020718405,0.040993325,0.00009289693,0.00044538765,0.013846568],"study_design_scores_gemma":[0.0000011239719,0.000029742636,0.99860376,0.0000022391807,0.000002610657,0.00016795738,0.00010182487,0.00029427104,0.0006093939,0.0000145036165,0.00017105181,0.0000015940193],"about_ca_topic_score_codex":0.009350367,"about_ca_topic_score_gemma":0.017140586,"teacher_disagreement_score":0.009350367,"about_ca_system_score_codex":0.00023798582,"about_ca_system_score_gemma":0.00011158262,"threshold_uncertainty_score":0.01859188},"labels":[],"label_agreement":null},{"id":"W4385158980","doi":"10.22541/essoar.168614604.40356164/v2","title":"Dynamic rupture process of the 2023 Mw 7.8 Kahramanmaraş earthquake (SE Türkiye): Variable rupture speed and implications for seismic hazard","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Bilimsel Araştırma Projeleri Birimi, İstanbul Teknik Üniversitesi; Southern University of Science and Technology; Istanbul Teknik Üniversitesi; Chinese University of Hong Kong; National Natural Science Foundation of China; King Abdullah University of Science and Technology; Alexander von Humboldt-Stiftung","keywords":"Seismology; Seismic hazard; Geology; Hazard; Earthquake prediction; Chemistry","score_opus":0.026155168779672576,"score_gpt":0.26924204655974177,"score_spread":0.24308687778006918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385158980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988059,0.000022770748,0.0003794911,0.00003537811,0.000005291346,0.0000041796043,0.00018726088,0.000019851926,0.00053992914],"genre_scores_gemma":[0.9996809,0.000010107688,0.00010177268,0.000003676145,0.0000012745471,0.0000039921533,0.00011344559,0.0000029546713,0.000081839295],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999279,0.000013067928,0.0000041615403,0.000015730266,0.000008333903,0.00003082631],"domain_scores_gemma":[0.9998821,0.00003294978,0.000029353303,0.000012942956,0.000020946554,0.000021741955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021398548,0.00049319933,0.00031801168,0.00039611573,0.0003552613,0.00065078394,0.0006347812,0.0008773483,0.0013276177],"category_scores_gemma":[0.000581188,0.0002659492,0.0005102251,0.00041343807,0.00030425485,0.00041823176,0.00035565317,0.00036604182,0.00015438398],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023860497,0.00016374514,0.08956001,0.000034934506,0.00012375865,0.000901909,0.000085132095,0.8936432,0.009930168,0.0007958894,0.0004430039,0.0040796935],"study_design_scores_gemma":[0.00004331795,0.00012473649,0.04923374,0.000006636944,0.000041699725,0.00010363339,0.00013165805,0.94772077,0.0020643412,0.00023210043,0.0002712298,0.000026096539],"about_ca_topic_score_codex":0.031625476,"about_ca_topic_score_gemma":0.01574036,"teacher_disagreement_score":0.031625476,"about_ca_system_score_codex":0.0007616647,"about_ca_system_score_gemma":0.00047308597,"threshold_uncertainty_score":0.06288278},"labels":[],"label_agreement":null},{"id":"W4385239435","doi":"10.5802/crgeos.225","title":"Extensional forearc structures at the transition from Alaska to Aleutian Subduction Zone: slip partitioning, terranes and large earthquakes","year":2023,"lang":"en","type":"article","venue":"Comptes Rendus Géoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"U.S. Geological Survey","keywords":"Geology; Subduction; Seismology; Trench; Terrane; Forearc; Episodic tremor and slip; Slip (aerodynamics); Volcanic arc; Convergent boundary; Tectonics; Oceanic crust","score_opus":0.025521056748463715,"score_gpt":0.23775607366633347,"score_spread":0.21223501691786975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385239435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947494,0.00004570647,0.000028250473,0.0000050309945,4.4226607e-7,0.0000010177888,0.00004318937,0.0000028405148,0.00039853973],"genre_scores_gemma":[0.9997482,0.000034150577,0.000038620325,0.000001418709,6.030272e-7,9.699227e-7,0.00006261646,6.4369937e-7,0.00011289887],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999498,0.0000065747654,0.000005890553,0.000016324258,0.0000072177236,0.000014140651],"domain_scores_gemma":[0.9999002,0.000011640537,0.000038225153,0.000008403496,0.000017556684,0.000023900304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012998843,0.00013673118,0.00012697303,0.0009872378,0.0002820709,0.0004971592,0.00012201473,0.00015895632,0.00092171726],"category_scores_gemma":[0.00029075012,0.00010142062,0.00010977812,0.0007876412,0.00030323176,0.00023536751,0.00043358083,0.00009613687,0.000106522995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089070396,0.000019586818,0.9829285,0.000017952854,0.000023705385,0.00026357413,0.0010238261,0.0006909953,0.007294208,0.00011469272,0.000035825175,0.007497983],"study_design_scores_gemma":[6.6867375e-7,0.0000067146857,0.99928063,0.0000027239212,0.0000037101256,0.00003712715,0.0002864837,0.00020579618,0.0000853285,0.00002030634,0.0000692114,0.0000013065915],"about_ca_topic_score_codex":0.016895005,"about_ca_topic_score_gemma":0.037483297,"teacher_disagreement_score":0.016895005,"about_ca_system_score_codex":0.00034343713,"about_ca_system_score_gemma":0.0002464287,"threshold_uncertainty_score":0.033593297},"labels":[],"label_agreement":null},{"id":"W4385285882","doi":"10.14379/iodp.sp.405.2023","title":"Expedition 405 Scientific Prospectus: Tracking Tsunamigenic Slip Across the Japan Trench (JTRACK)","year":2023,"lang":"en","type":"book","venue":"Scientific prospectus","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Japan Agency for Marine-Earth Science and Technology; Ministry of Education, Culture, Sports, Science and Technology; National Science Foundation","keywords":"Prospectus; Trench; Slip (aerodynamics); Geology; Seismology; Engineering; Materials science; Nanotechnology; Aerospace engineering; Business","score_opus":0.03080286736698108,"score_gpt":0.25276663301144997,"score_spread":0.2219637656444689,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385285882","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8068676,0.00048090282,0.0062051485,0.0006477024,0.00044973267,0.0010418971,0.11016702,0.005711298,0.068428636],"genre_scores_gemma":[0.73164237,0.00036270544,0.0422219,0.00026881407,0.00013029728,0.0005570982,0.18575197,0.0010524741,0.03801235],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997855,0.000015550795,0.000006848183,0.000044118926,0.000097461,0.00005056981],"domain_scores_gemma":[0.9995254,0.000022131142,0.000051799725,0.0000705145,0.00016090303,0.00016929896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005267456,0.0005165696,0.00031102894,0.00113015,0.00083583506,0.00074191333,0.0005527602,0.00031917376,0.0071763545],"category_scores_gemma":[0.00066255406,0.00027824365,0.0002660136,0.0009118523,0.00024243687,0.00046915177,0.000909396,0.0004958615,0.0016525838],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024101078,0.0010109287,0.36758348,0.00046154935,0.00037128752,0.001834114,0.0028521314,0.010176857,0.06830132,0.0016557834,0.31731492,0.22602747],"study_design_scores_gemma":[0.0003586761,0.00053886964,0.8044806,0.00007682793,0.00010297983,0.00028306345,0.001181662,0.022125008,0.004349074,0.00048769082,0.16592811,0.00008743486],"about_ca_topic_score_codex":0.09308487,"about_ca_topic_score_gemma":0.30343318,"teacher_disagreement_score":0.09308487,"about_ca_system_score_codex":0.00061384274,"about_ca_system_score_gemma":0.0018662243,"threshold_uncertainty_score":0.18508613},"labels":[],"label_agreement":null},{"id":"W4385303009","doi":"10.1103/physreve.108.014131","title":"Large-scale heterogeneities can alter the characteristics of compressive failure and accelerated seismic release","year":2023,"lang":"en","type":"article","venue":"Physical review. E","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; University of Calgary","keywords":"Acoustic emission; Brittleness; Compression (physics); Geology; Compressive strength; Stress (linguistics); Scale (ratio); Critical point (mathematics); Power law; Exponent; Geotechnical engineering; Physics; Materials science; Composite material; Geometry; Mathematics; Statistics","score_opus":0.02328587337881682,"score_gpt":0.2738253980301153,"score_spread":0.2505395246512985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385303009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953603,0.0003412054,0.003200282,0.000019153991,0.0000071072823,0.000015312822,0.00011176342,0.000040689,0.0009041879],"genre_scores_gemma":[0.9993291,0.0000821741,0.00029766271,0.000007790262,0.000002294117,0.0000075243865,0.00007264014,0.000005509907,0.00019537252],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981004,0.000018472449,0.0000138712385,0.00006601159,0.000063462925,0.000028292576],"domain_scores_gemma":[0.99941266,0.00018258955,0.00020963044,0.00009675651,0.00005677968,0.000041535077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023654367,0.00018261492,0.0002486368,0.00042409817,0.00013334981,0.00026690454,0.00021097959,0.00029152038,0.0014698474],"category_scores_gemma":[0.00067606894,0.00018545866,0.00013992345,0.0002691659,0.0005425854,0.00028193244,0.0002699603,0.00031638955,0.0001760624],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017369585,0.000066968205,0.037327364,0.00013682872,0.00005141903,0.0003069312,0.0001458049,0.0036008179,0.9479712,0.0004763962,0.00010229269,0.009640204],"study_design_scores_gemma":[0.000010940919,0.00055876863,0.75737035,0.000017377717,0.00004109606,0.00081607816,0.00034312133,0.011732926,0.22637789,0.0012166998,0.0014796248,0.00003525452],"about_ca_topic_score_codex":0.0003346159,"about_ca_topic_score_gemma":0.0006677238,"teacher_disagreement_score":0.0014698474,"about_ca_system_score_codex":0.00014893444,"about_ca_system_score_gemma":0.00011167641,"threshold_uncertainty_score":0.004917145},"labels":[],"label_agreement":null},{"id":"W4385359269","doi":"10.23939/jgd2023.01.070","title":"Focal mechanism of the induced earthquake of 2015-06-13 (Alberta, Canada), based on waveform inversion","year":2023,"lang":"en","type":"article","venue":"GEODYNAMICS","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Tectonics; Focal mechanism; Geodynamics; Seismic moment; Inversion (geology); Moment tensor; Fault (geology)","score_opus":0.010925984096565327,"score_gpt":0.19050708301379846,"score_spread":0.17958109891723312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385359269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98370624,0.0001964372,0.007884304,0.00010985898,0.000020052517,0.000037202204,0.003401944,0.00043269654,0.004211301],"genre_scores_gemma":[0.9908179,0.00012866758,0.0045500244,0.000012659977,0.000006713917,0.000007041025,0.0036327266,0.0000423895,0.0008018337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.0000020254781,0.0000030710364,0.000011645411,0.000017594564,0.000012924749],"domain_scores_gemma":[0.99987626,0.000010895599,0.000023399209,0.000013677774,0.000054776043,0.000021016143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010380402,0.00046131908,0.00014983612,0.0012378684,0.00023811066,0.00051965617,0.00059933844,0.00034217714,0.0016489658],"category_scores_gemma":[0.00068210333,0.00017385186,0.00026097102,0.0011952803,0.0002189248,0.0003800912,0.000220431,0.00029416097,0.00024059998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007045856,0.00020172494,0.4045102,0.00052358955,0.00034734857,0.001521973,0.0005149444,0.37860245,0.06752176,0.0061280616,0.0068172975,0.13260612],"study_design_scores_gemma":[0.000090942674,0.000046659457,0.39156464,0.000027353246,0.000115734205,0.00020247101,0.0002678315,0.5988841,0.0057836296,0.0007303753,0.0022338158,0.00005240324],"about_ca_topic_score_codex":0.47966063,"about_ca_topic_score_gemma":0.5370724,"teacher_disagreement_score":0.52033937,"about_ca_system_score_codex":0.0014035405,"about_ca_system_score_gemma":0.00234405,"threshold_uncertainty_score":0.9537374},"labels":[],"label_agreement":null},{"id":"W4385381426","doi":"10.1177/87552930231187407","title":"Evaluation of reduced computational approaches to assessment of tsunami hazard and loss using stochastic source models: Case study for Tofino, British Columbia, Canada, subjected to Cascadia megathrust earthquakes","year":2023,"lang":"en","type":"article","venue":"Earthquake Spectra","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Probabilistic logic; Seismology; Submarine pipeline; Hazard; Geology; Hazard analysis; Stochastic modelling; Probabilistic analysis of algorithms; Computer science; Geotechnical engineering; Engineering; Statistics; Reliability engineering","score_opus":0.12509656748952908,"score_gpt":0.28585486514021,"score_spread":0.16075829765068095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385381426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98040694,0.00013271382,0.011870195,0.00024320463,0.000012652987,0.00012814334,0.0003127867,0.00015135334,0.006741965],"genre_scores_gemma":[0.9933119,0.00007755028,0.0054893875,0.000015703468,0.0000031206241,0.000044865585,0.00018650368,0.000012759331,0.0008584046],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995883,0.00013424887,0.000021069845,0.000043184882,0.000114837036,0.00009835223],"domain_scores_gemma":[0.9985196,0.00087886304,0.00008948263,0.00007651184,0.00034935027,0.000086152155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009921252,0.0012806089,0.0007137474,0.0009104516,0.0009044028,0.0014014728,0.0015726823,0.0009077325,0.0013560001],"category_scores_gemma":[0.002683843,0.0004088719,0.00052639854,0.00094811217,0.00072078547,0.00047212618,0.00075225666,0.0007445659,0.00008577943],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016299117,0.00011986852,0.0034458372,0.000051697636,0.000025502479,0.00017502317,0.0000642439,0.9880987,0.0010258268,0.000734539,0.00023890295,0.0058567747],"study_design_scores_gemma":[0.000021000793,0.000053614716,0.0019738711,0.0000044137587,0.00001333689,0.0000121070325,0.00012126556,0.9970042,0.0005304874,0.00014911895,0.00010929905,0.0000072398575],"about_ca_topic_score_codex":0.57741475,"about_ca_topic_score_gemma":0.4988226,"teacher_disagreement_score":0.42258525,"about_ca_system_score_codex":0.005473016,"about_ca_system_score_gemma":0.0041570864,"threshold_uncertainty_score":0.85014784},"labels":[],"label_agreement":null},{"id":"W4385492370","doi":"10.1007/s00603-023-03477-y","title":"In Situ Stress Evolution and Fault-Slip Tendency Assessment of an Underground Gas Storage Reservoir in the Turpan Basin (China): In Situ Stress Measurements and Coupled Simulations","year":2023,"lang":"en","type":"article","venue":"Rock Mechanics and Rock Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada); University of Calgary","funders":"","keywords":"Geology; Slip (aerodynamics); Geomechanics; Caprock; Stress field; Pore water pressure; Geotechnical engineering; Shear stress; Finite element method; Fault (geology); Natural gas field; Stress (linguistics); Structural basin; Seismology; Mechanics; Engineering; Natural gas; Geomorphology; Structural engineering","score_opus":0.021611293502628023,"score_gpt":0.24587553553882902,"score_spread":0.224264242036201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385492370","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995615,0.000008306541,0.00013830262,0.0000165577,0.0000015235211,0.0000020311936,0.00009100441,0.000015190967,0.00016561957],"genre_scores_gemma":[0.99972767,0.000009125983,0.00010923844,0.000002907654,0.0000011825816,0.0000028173436,0.00007644983,0.0000021092435,0.00006855376],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991953,0.000011077808,0.000008381512,0.00003042897,0.000009407246,0.000021214886],"domain_scores_gemma":[0.9998368,0.00004429869,0.00002992815,0.000018287523,0.00003360134,0.000037009027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026821933,0.0006051715,0.00050170626,0.00069684006,0.0005085076,0.00052261795,0.00089476694,0.0009681572,0.00074413634],"category_scores_gemma":[0.00037296768,0.00059120497,0.0007059957,0.00076370116,0.00061990303,0.00065852393,0.0004129046,0.00028561594,0.00008309436],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005579461,0.0005702554,0.3242729,0.00013419394,0.000302237,0.0015412711,0.00055832585,0.6356732,0.023960771,0.0005319036,0.0006375287,0.011259503],"study_design_scores_gemma":[0.00007389579,0.00011990502,0.14587891,0.000008688516,0.00008505109,0.00005851115,0.0003131661,0.8514241,0.0017246418,0.00014949997,0.00012822042,0.000035419016],"about_ca_topic_score_codex":0.08694626,"about_ca_topic_score_gemma":0.07175937,"teacher_disagreement_score":0.08694626,"about_ca_system_score_codex":0.0011147684,"about_ca_system_score_gemma":0.00089385145,"threshold_uncertainty_score":0.17288035},"labels":[],"label_agreement":null},{"id":"W4385582237","doi":"10.1029/2023gl104787","title":"Dynamic Rupture Process of the 2023 <i>Mw</i> 7.8 Kahramanmaraş Earthquake (SE Türkiye): Variable Rupture Speed and Implications for Seismic Hazard","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Seismic hazard; Waveform; Fault (geology); Earthquake rupture; Engineering; Aerospace engineering","score_opus":0.03046785237440454,"score_gpt":0.3058243447439334,"score_spread":0.27535649236952886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385582237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907434,0.000014352195,0.0002799144,0.000027448952,0.000003972418,0.0000030435087,0.000102383994,0.000013871332,0.00048071015],"genre_scores_gemma":[0.9997652,0.0000068261943,0.00008043595,0.0000032715911,9.752912e-7,0.000003064186,0.00007560735,0.000001986312,0.0000626698],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999403,0.000010241602,0.0000034146242,0.000012944363,0.0000065149266,0.00002650874],"domain_scores_gemma":[0.99989545,0.000027850103,0.000026689402,0.000010787422,0.000018636507,0.000020643136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017672728,0.00038957412,0.00028288935,0.0003250479,0.00032496924,0.0005955146,0.0005950122,0.0006722778,0.0011386306],"category_scores_gemma":[0.00046060217,0.00021658701,0.00048051728,0.0003192791,0.00030034364,0.00033867708,0.00030735103,0.0003243805,0.0001328946],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025129833,0.00014057022,0.09002687,0.000030949523,0.00012814527,0.0009001484,0.00009074191,0.89102733,0.012094832,0.00086419645,0.00043611604,0.0040087886],"study_design_scores_gemma":[0.000045751538,0.00015349632,0.05428505,0.0000067859637,0.000051099094,0.00011674589,0.00016497239,0.94240266,0.0022287953,0.00023023064,0.0002868066,0.000027574542],"about_ca_topic_score_codex":0.028816631,"about_ca_topic_score_gemma":0.013224066,"teacher_disagreement_score":0.028816631,"about_ca_system_score_codex":0.00071264536,"about_ca_system_score_gemma":0.00046350865,"threshold_uncertainty_score":0.057297826},"labels":[],"label_agreement":null},{"id":"W4385602188","doi":"10.1007/978-3-031-34159-5_43","title":"Aftershock Record Selection Criteria for Structural Vulnerability Assessments","year":2023,"lang":"en","type":"book-chapter","venue":"Lecture notes in civil engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Aftershock; Seismology; Geology; Vulnerability (computing); Computer science","score_opus":0.02960317912025143,"score_gpt":0.26966833810183327,"score_spread":0.24006515898158184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385602188","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32288808,0.0011151559,0.6251078,0.0005710621,0.00017560109,0.0015718584,0.00949386,0.0022377376,0.03683886],"genre_scores_gemma":[0.67876756,0.00036609196,0.2906518,0.00013194968,0.00022511274,0.0008330479,0.016125085,0.0005543138,0.012345016],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9976301,0.00066448783,0.00034849043,0.00016042602,0.00094355975,0.00025286453],"domain_scores_gemma":[0.98172045,0.010615023,0.0010055015,0.00086490763,0.005166499,0.00062760414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005495677,0.00078128633,0.0010215446,0.0075180423,0.0009852336,0.0021884493,0.0016935823,0.00079904776,0.014461547],"category_scores_gemma":[0.024332726,0.00035654023,0.0010103702,0.0030978068,0.00040021335,0.0011066726,0.0014626699,0.0007562224,0.0027729387],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021735867,0.00049986766,0.102775075,0.0007781586,0.0004083916,0.00075575546,0.0005153861,0.057949297,0.018567134,0.0131875435,0.03516314,0.7672267],"study_design_scores_gemma":[0.00042577588,0.0014202115,0.12011801,0.00083396665,0.0010635878,0.0013554986,0.0020171327,0.7905027,0.023264812,0.024340661,0.034458417,0.00019910205],"about_ca_topic_score_codex":0.0028889987,"about_ca_topic_score_gemma":0.0058456664,"teacher_disagreement_score":0.014461547,"about_ca_system_score_codex":0.00045793908,"about_ca_system_score_gemma":0.001279006,"threshold_uncertainty_score":0.048378706},"labels":[],"label_agreement":null},{"id":"W4385766912","doi":"10.1016/j.geomorph.2023.108862","title":"Morphometric analysis of the North Liuleng Shan Fault in the northern Shanxi Graben System, China: Insights into active deformation pattern and fault evolution","year":2023,"lang":"en","type":"article","venue":"Geomorphology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Toronto","funders":"National Key Research and Development Program of China; China Scholarship Council; University of Toronto; National Natural Science Foundation of China","keywords":"Geology; Sinuosity; Graben; Fault (geology); Structural basin; Active fault; Half-graben; Geomorphology; Echelon formation; Strike-slip tectonics; Fault scarp; Seismology; Tectonics; Plateau (mathematics); Quaternary; Paleontology","score_opus":0.01063620591043577,"score_gpt":0.20409182772009057,"score_spread":0.1934556218096548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385766912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985512,0.000032686145,0.00041329762,0.000012449688,0.0000010832999,0.0000053703207,0.00021141199,0.000016636135,0.0007559127],"genre_scores_gemma":[0.9988182,0.000032180174,0.0004879917,0.0000029806201,0.000001755836,0.0000051293014,0.00021595403,0.0000060136213,0.00042974012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992776,0.0000063107323,0.0000051748148,0.000025824107,0.000019551462,0.000015449614],"domain_scores_gemma":[0.9998807,0.000011274313,0.00004427774,0.000009802769,0.00003552341,0.000018477524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001472508,0.00018778184,0.00017287163,0.0024802207,0.0005096906,0.00043321066,0.00027092436,0.00015999658,0.0014732203],"category_scores_gemma":[0.00026156087,0.00017932199,0.00020372492,0.0025911422,0.00052281976,0.00022123469,0.00035074525,0.0001029362,0.00017425051],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020023933,0.00006944772,0.8215331,0.00012434233,0.000069424554,0.00042330733,0.0021552057,0.0065673697,0.065188825,0.0009904926,0.00068085425,0.101997405],"study_design_scores_gemma":[0.0000012217552,0.000011405537,0.9968874,0.0000019414492,0.0000050665567,0.00007397294,0.00026781939,0.0022215876,0.00024479578,0.000036897633,0.00024344336,0.000004284123],"about_ca_topic_score_codex":0.053887814,"about_ca_topic_score_gemma":0.12322171,"teacher_disagreement_score":0.053887814,"about_ca_system_score_codex":0.00065591227,"about_ca_system_score_gemma":0.0009756971,"threshold_uncertainty_score":0.10714829},"labels":[],"label_agreement":null},{"id":"W4385783302","doi":"10.1038/s41598-023-40403-2","title":"Physics-informed deep learning to forecast $${\\widehat{{\\varvec{M}}}}_{{\\varvec{m}}{\\varvec{a}}{\\varvec{x}}}$$ during hydraulic fracturing","year":2023,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Hydraulic fracturing; Physics; Lag; Seismology; Magnitude (astronomy); Earthquake prediction; Geology; Computer science; Econometrics; Mathematics; Geotechnical engineering; Astrophysics","score_opus":0.018795776622781663,"score_gpt":0.232660180829607,"score_spread":0.21386440420682531,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385783302","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13808016,0.001821384,0.8233847,0.002418088,0.0007317801,0.00011864259,0.0056699137,0.017983904,0.009791362],"genre_scores_gemma":[0.784392,0.001187488,0.18046099,0.0010582511,0.0003312838,0.0001760209,0.015785785,0.00059400196,0.016014151],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998216,0.000027280053,0.00000845174,0.00006816667,0.0000382169,0.000036308542],"domain_scores_gemma":[0.99968386,0.00011491265,0.000029582681,0.00005237061,0.00009822722,0.000021097276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004094029,0.0014834823,0.00052646926,0.00062841014,0.00026947918,0.0007876536,0.0015443526,0.0007945744,0.0052892053],"category_scores_gemma":[0.0014771931,0.00056434196,0.0008421218,0.0008001225,0.0004278239,0.0015374018,0.0007693296,0.0023750227,0.0027371517],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020823293,0.0002436737,0.0048893695,0.00015076772,0.0001612908,0.00013220106,0.0000552303,0.50608,0.007552166,0.0079581905,0.043812145,0.42875677],"study_design_scores_gemma":[0.0000072675452,0.000015106616,0.0003342674,0.000006562375,0.000009153063,0.000011386586,0.0000052895107,0.99444735,0.0014535888,0.0024185644,0.0012854579,0.0000060624307],"about_ca_topic_score_codex":0.018778153,"about_ca_topic_score_gemma":0.03573702,"teacher_disagreement_score":0.018778153,"about_ca_system_score_codex":0.0010656731,"about_ca_system_score_gemma":0.0012676459,"threshold_uncertainty_score":0.03733766},"labels":[],"label_agreement":null},{"id":"W4386160906","doi":"10.1016/j.apgeochem.2023.105767","title":"Geochemical characteristics of natural springs within the Lenglongling fault zone related to the Menyuan Ms 6.9 earthquake on January 8, 2022, NW China","year":2023,"lang":"en","type":"article","venue":"Applied Geochemistry","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Visiting Professorships for Senior International Scientists; National Key Research and Development Program of China; Youth Innovation Promotion Association of the Chinese Academy of Sciences","keywords":"Geology; Crust; Geochemistry; Plateau (mathematics); Fault (geology); Carbonate; Seismology; Meteoric water; δ18O; Mantle (geology); Spring (device); Stable isotope ratio","score_opus":0.0067374050872722096,"score_gpt":0.20128347965363858,"score_spread":0.19454607456636636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386160906","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99938846,0.000021158854,0.000015582675,0.000011089931,0.0000015645313,0.0000021620904,0.0002576118,0.0000017270926,0.00030064667],"genre_scores_gemma":[0.99925953,0.000022228718,0.00002480015,0.0000067620067,0.0000034531681,0.0000036282163,0.00038587535,6.32118e-7,0.00029298442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.0000062021436,0.000009367994,0.00002314825,0.000018565053,0.000022415457],"domain_scores_gemma":[0.99976,0.000019712137,0.000094151896,0.000009600627,0.000056654048,0.000059980295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009041083,0.00013460536,0.00018032333,0.0010158704,0.0005086966,0.00025745155,0.00023421532,0.0002719878,0.0006524915],"category_scores_gemma":[0.00018970258,0.00013259196,0.00016146971,0.0012102125,0.00029288963,0.00018587291,0.00030059027,0.00011791268,0.000079586745],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011556185,0.00004369466,0.986246,0.00003599823,0.000037455095,0.00047878598,0.00051714777,0.00060033804,0.008469276,0.000073505405,0.000220419,0.0031617344],"study_design_scores_gemma":[0.0000010600249,0.00000760212,0.9994568,9.5215773e-7,0.000003221194,0.000019591163,0.0001258776,0.00020150337,0.00008923207,0.0000073643423,0.0000852278,0.0000015524638],"about_ca_topic_score_codex":0.054403856,"about_ca_topic_score_gemma":0.13012923,"teacher_disagreement_score":0.054403856,"about_ca_system_score_codex":0.000684248,"about_ca_system_score_gemma":0.00068941934,"threshold_uncertainty_score":0.108174324},"labels":[],"label_agreement":null},{"id":"W4386189241","doi":"10.1007/978-981-99-3955-8_2","title":"Stress Dissipation in the North-West Himalaya: What We Learnt from Post-seismic Stress Changes","year":2023,"lang":"en","type":"book-chapter","venue":"Advances in natural and technological hazards research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Induced seismicity; Seismology; Geology; Seismic hazard; Stress (linguistics); Tectonics; Subduction","score_opus":0.04239138697607629,"score_gpt":0.30300207727705286,"score_spread":0.26061069030097656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386189241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.47779676,0.41002217,0.0037358121,0.029002259,0.0015149893,0.000013366922,0.0006873913,0.00009413001,0.077133134],"genre_scores_gemma":[0.723814,0.24696428,0.0011451083,0.0014159976,0.0013781814,0.000007655311,0.00027794344,0.00004083204,0.024956062],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999473,0.000007794598,0.0000029061885,0.000012443135,0.000015739502,0.000013795],"domain_scores_gemma":[0.9998568,0.00006947343,0.000024730349,0.000012334501,0.00002250305,0.000014116324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019402416,0.00025655597,0.00024578744,0.00036926896,0.0003804285,0.0026055595,0.00053375034,0.00046692797,0.0024105257],"category_scores_gemma":[0.0005206376,0.00016564757,0.00015630604,0.0014855533,0.0015771938,0.001788815,0.0004251958,0.00065794546,0.00036436092],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019389736,0.000086287466,0.053929694,0.0024957312,0.00019123127,0.0017821589,0.041497912,0.008197939,0.008749852,0.077485725,0.022699026,0.7826905],"study_design_scores_gemma":[0.000010188667,0.0001386282,0.5283547,0.001226087,0.00008392123,0.0010665583,0.02247139,0.002342167,0.0021399863,0.102705,0.33937535,0.000086037224],"about_ca_topic_score_codex":0.022609945,"about_ca_topic_score_gemma":0.03853686,"teacher_disagreement_score":0.022609945,"about_ca_system_score_codex":0.001106039,"about_ca_system_score_gemma":0.00073837437,"threshold_uncertainty_score":0.044956684},"labels":[],"label_agreement":null},{"id":"W4386223821","doi":"10.1007/s10518-023-01758-z","title":"The December 2020 magnitude (Mw) 6.4 Petrinja earthquake, Croatia: seismological aspects, emergency response and impacts","year":2023,"lang":"en","type":"article","venue":"Bulletin of Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Hrvatska Zaklada za Znanost","keywords":"Masonry; Unreinforced masonry building; Epicenter; Capital city; Landslide; Emergency response; Forensic engineering; Foreshock; Seismology; Aftershock; Geology; Civil engineering; Geography; Engineering","score_opus":0.012146128356916879,"score_gpt":0.21329879888832456,"score_spread":0.20115267053140767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386223821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98399156,0.002497186,0.00071179227,0.00038666217,0.00020126135,0.00007780443,0.002060433,0.000053984648,0.010019206],"genre_scores_gemma":[0.9936041,0.0011127163,0.00049383193,0.00006133185,0.000092077295,0.000010442389,0.0016678284,0.000012436459,0.0029452764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984074,0.000022318056,0.000015028928,0.000019149267,0.000054621672,0.00004814897],"domain_scores_gemma":[0.99984026,0.000012849953,0.000043594795,0.00000816134,0.000057125962,0.0000379625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038096492,0.00031174676,0.00024422092,0.0007960648,0.00038135934,0.00071513123,0.00021748718,0.0004250104,0.0026314326],"category_scores_gemma":[0.00031907522,0.00013289182,0.00015309805,0.00066082494,0.00027733468,0.00030531632,0.00048254192,0.0003535756,0.00056314265],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012122813,0.00081951683,0.74651283,0.001079756,0.00013169627,0.0065853857,0.0015384723,0.009392622,0.01913206,0.0011516452,0.016295182,0.1961485],"study_design_scores_gemma":[0.000015370537,0.00017819452,0.9887639,0.000095874304,0.000018018734,0.0005185769,0.0014008754,0.00047940126,0.0004516987,0.000071619485,0.007994797,0.000011734029],"about_ca_topic_score_codex":0.016845332,"about_ca_topic_score_gemma":0.023249293,"teacher_disagreement_score":0.016845332,"about_ca_system_score_codex":0.00044832457,"about_ca_system_score_gemma":0.00077043416,"threshold_uncertainty_score":0.03349459},"labels":[],"label_agreement":null},{"id":"W4386283987","doi":"10.1785/0220230124","title":"Identification of Repeating Earthquakes: Controversy and Rectification","year":2023,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Identification (biology); Event (particle physics); Computer science; Fault (geology); Magnitude (astronomy); Geology; Simple (philosophy); Seismology; Epistemology; Physics","score_opus":0.07896205649575269,"score_gpt":0.32713280829745234,"score_spread":0.24817075180169965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386283987","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.40705535,0.030217936,0.3439086,0.18906361,0.0027609589,0.00039996477,0.0005462983,0.0006414997,0.025405763],"genre_scores_gemma":[0.9327948,0.004192143,0.05581212,0.0031823511,0.0022805943,0.00007339905,0.0002767155,0.00006687752,0.0013210602],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9859459,0.006157124,0.0022210462,0.0026221534,0.0026606158,0.0003932229],"domain_scores_gemma":[0.93830615,0.03261234,0.008023246,0.008758418,0.011271006,0.0010287836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0282697,0.0006015667,0.0012058256,0.00508484,0.002574496,0.00523376,0.004159063,0.0043165297,0.002279054],"category_scores_gemma":[0.11225023,0.00040192946,0.00059748173,0.0031592697,0.0066370247,0.007551793,0.0035596292,0.0030840775,0.00069928786],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024387367,0.00015522368,0.22095704,0.0014163291,0.00015763547,0.0040007085,0.012070576,0.0050722486,0.003965698,0.19289006,0.03183366,0.5272369],"study_design_scores_gemma":[0.00016848146,0.00028146265,0.13109197,0.003005755,0.00024884252,0.013435658,0.04852662,0.09033111,0.006420409,0.6096388,0.09649612,0.00035473416],"about_ca_topic_score_codex":0.0024263621,"about_ca_topic_score_gemma":0.0023487022,"teacher_disagreement_score":0.0282697,"about_ca_system_score_codex":0.0014577036,"about_ca_system_score_gemma":0.0018765321,"threshold_uncertainty_score":0.14950621},"labels":[],"label_agreement":null},{"id":"W4386308278","doi":"10.1029/2023gl103909","title":"Using Deep Learning for Flexible and Scalable Earthquake Forecasting","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Benchmark (surveying); Scalability; Earthquake prediction; Aftershock; Computer science; Data set; Earthquake simulation; Set (abstract data type); Scale (ratio); Artificial neural network; Seismology; Data mining; Machine learning; Artificial intelligence; Geology; Geography; Cartography; Database","score_opus":0.14191344088159213,"score_gpt":0.33394648219165884,"score_spread":0.1920330413100667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386308278","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3158456,0.00069017854,0.6703923,0.0012401339,0.00014296884,0.0000565727,0.0008667369,0.0064971712,0.0042683487],"genre_scores_gemma":[0.9113617,0.00014871957,0.08591078,0.00011891316,0.000043740198,0.00004012563,0.00078159827,0.00008003974,0.0015143754],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998369,0.000034274923,0.000012154557,0.000045927944,0.00004067322,0.000030058989],"domain_scores_gemma":[0.99939275,0.0002691975,0.000060304224,0.00011150826,0.00013101385,0.00003521431],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006329586,0.0006163383,0.00045862468,0.000426881,0.0002260836,0.00063774927,0.0009864367,0.00061037444,0.0014244105],"category_scores_gemma":[0.0021430575,0.00042219582,0.00029083996,0.0005410384,0.00035171647,0.0011929452,0.00092700816,0.0010297205,0.00046778866],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007216987,0.000051902844,0.0017234378,0.000022532959,0.000032941938,0.00003949675,0.000018505294,0.9196242,0.0037340196,0.0014055991,0.0018716592,0.07140354],"study_design_scores_gemma":[0.0000016526903,0.0000029593505,0.00004330041,5.8285406e-7,7.312036e-7,9.805678e-7,0.0000011995576,0.99918836,0.00024899066,0.00045224442,0.000058212358,7.838657e-7],"about_ca_topic_score_codex":0.016387591,"about_ca_topic_score_gemma":0.018575111,"teacher_disagreement_score":0.016387591,"about_ca_system_score_codex":0.0007199113,"about_ca_system_score_gemma":0.0008366128,"threshold_uncertainty_score":0.03258437},"labels":[],"label_agreement":null},{"id":"W4386448361","doi":"10.1029/2023gc010982","title":"Active Deformation Constraints on the Nubia‐Somalia Plate Boundary Through Heterogenous Lithosphere of the Turkana Depression","year":2023,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Addis Ababa University; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Geology; Lithosphere; Magmatism; Seismology; Rift; Plate tectonics; Mantle (geology); Shear zone; East African Rift; Geophysics; Tectonics","score_opus":0.01628159815043548,"score_gpt":0.2110080898715726,"score_spread":0.19472649172113712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386448361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986254,0.000092330694,0.0000825747,0.000020223084,0.0000010593188,0.000001611265,0.000098539014,0.0000055374853,0.0010727651],"genre_scores_gemma":[0.99972457,0.000028265804,0.00008018973,0.0000033744363,6.474285e-7,0.0000017069854,0.000093915325,0.0000016248791,0.000065821645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.000010392588,0.0000057917755,0.000015229987,0.000010471081,0.000020078063],"domain_scores_gemma":[0.9998234,0.00004021201,0.00005812206,0.000016377844,0.00004081138,0.000021137199],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010882809,0.00027453448,0.00026014997,0.0009885337,0.00049279124,0.00088882825,0.00027548178,0.00025242657,0.0016443024],"category_scores_gemma":[0.00046327966,0.0002300985,0.00015942946,0.0008489977,0.00043093014,0.00029064814,0.00046032848,0.0001275086,0.00030703912],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004216316,0.00006089503,0.89515543,0.000090227935,0.000119954995,0.00082407467,0.0009970444,0.0075468943,0.07266271,0.0012842579,0.0003030139,0.020533912],"study_design_scores_gemma":[0.000015960844,0.000021745447,0.99453604,0.000023188033,0.000019081233,0.000071508475,0.0005524032,0.0033791072,0.00079469173,0.0001548282,0.00042236786,0.000008993897],"about_ca_topic_score_codex":0.03964898,"about_ca_topic_score_gemma":0.094937496,"teacher_disagreement_score":0.03964898,"about_ca_system_score_codex":0.0007023709,"about_ca_system_score_gemma":0.00050414656,"threshold_uncertainty_score":0.07883638},"labels":[],"label_agreement":null},{"id":"W4386524836","doi":"10.56952/arma-2023-0270","title":"Stress Variation Around the Balarud Lineament in the Zagros Fold and Thrust Belt and its Implication for Reservoir Geomechanics","year":2023,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Lineament; Seismology; Borehole; Thrust fault; Diapir; Strike-slip tectonics; Tectonics; Petrology; Geotechnical engineering","score_opus":0.03524301140536052,"score_gpt":0.2544056479496639,"score_spread":0.2191626365443034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386524836","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99973184,0.000018178878,0.000023148854,0.000005658941,6.391463e-7,7.567334e-7,0.00005537056,0.0000018610342,0.00016261081],"genre_scores_gemma":[0.99979275,0.000012845422,0.00003839516,0.0000021690485,0.0000010849882,9.625506e-7,0.00007714901,3.5592e-7,0.000074405834],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999212,0.0000074507893,0.000007563915,0.00002021367,0.000017416136,0.0000262182],"domain_scores_gemma":[0.9998684,0.000010502874,0.00006633382,0.000007824899,0.000030565385,0.000016323645],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000115892035,0.00014039576,0.00015384115,0.0009527844,0.0002680639,0.00049619534,0.0001860286,0.0001814489,0.0006782199],"category_scores_gemma":[0.0001946605,0.00008711784,0.000121765894,0.000972738,0.00028518302,0.0001871291,0.00025423564,0.00008277904,0.00011832762],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057087465,0.000019457646,0.98904234,0.000011629843,0.0000214345,0.00017671158,0.00039351606,0.00050336076,0.0034705207,0.000053116306,0.00006143697,0.006189448],"study_design_scores_gemma":[0.0000012576048,0.000011036869,0.9993168,0.0000017050301,0.0000022242493,0.000024265706,0.00022932445,0.00024585635,0.00008122519,0.000009767322,0.00007539009,0.0000011123404],"about_ca_topic_score_codex":0.021114377,"about_ca_topic_score_gemma":0.03662253,"teacher_disagreement_score":0.021114377,"about_ca_system_score_codex":0.0004687749,"about_ca_system_score_gemma":0.00023245155,"threshold_uncertainty_score":0.04198295},"labels":[],"label_agreement":null},{"id":"W4386560914","doi":"10.31223/x59t0g","title":"A Cascadia Slab Model from Receiver Functions","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Slab; Terrane; Slab window; Seismology; Subduction; Receiver function; Underplating; Forearc; North American Plate; Crust; Oceanic crust; Geophysics; Tectonics; Lithosphere","score_opus":0.0695509994460263,"score_gpt":0.2413328202231008,"score_spread":0.1717818207770745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386560914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7039125,0.0007588151,0.25740623,0.0010207336,0.000098561475,0.00010704411,0.0065392465,0.002643493,0.02751335],"genre_scores_gemma":[0.96841073,0.00035435217,0.016716423,0.000040098083,0.000030285353,0.000116164716,0.0021997497,0.00018444414,0.011947804],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998609,0.00002762272,0.0000061411542,0.0000502926,0.00002556619,0.000029448627],"domain_scores_gemma":[0.99980706,0.000044754317,0.000031175117,0.000022546288,0.000063952735,0.00003038869],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027585684,0.0010869183,0.00043996685,0.0008536169,0.0005730259,0.001007199,0.0020801637,0.0012244234,0.004180072],"category_scores_gemma":[0.00076917675,0.0008108631,0.0009231415,0.0012110267,0.0006016733,0.0005575606,0.0006274027,0.0006650631,0.00081697357],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026987982,0.000010145252,0.0021577051,0.000012436767,0.000019760071,0.0000593984,0.000043686756,0.9924924,0.00068734225,0.0023721654,0.00033146297,0.0017866751],"study_design_scores_gemma":[0.0000121817175,0.000006150886,0.0009197572,0.0000040523805,0.000009451045,0.0000137401,0.000014677625,0.99739265,0.000056615223,0.001007321,0.0005543181,0.000009159725],"about_ca_topic_score_codex":0.21293071,"about_ca_topic_score_gemma":0.085356176,"teacher_disagreement_score":0.21293071,"about_ca_system_score_codex":0.0017612383,"about_ca_system_score_gemma":0.0018757944,"threshold_uncertainty_score":0.42338264},"labels":[],"label_agreement":null},{"id":"W4386620654","doi":"10.22541/essoar.169444217.76589378/v1","title":"Fluid-induced aseismic slip may explain the non-self-similar source scaling of the induced earthquake sequence near the Dallas-Fort Worth Airport, Texas","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Government of Ontario","keywords":"Scaling; Induced seismicity; Slip (aerodynamics); Geology; Stress field; Seismology; Seismic moment; Fault (geology); Mechanics; Structural engineering; Engineering; Physics; Geometry; Mathematics; Aerospace engineering","score_opus":0.059039356927137104,"score_gpt":0.25527227241726697,"score_spread":0.19623291549012986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386620654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99437666,0.000048811347,0.0041898107,0.000079833895,0.000005455979,0.000007953969,0.000062359984,0.00004389962,0.0011851966],"genre_scores_gemma":[0.99945503,0.000022555982,0.00037913903,0.000005274877,0.000002097895,0.0000027954027,0.000029773953,0.0000035671255,0.000099684665],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999658,0.000004908629,0.0000029491614,0.000010146511,0.000004485002,0.000011602685],"domain_scores_gemma":[0.9998809,0.000018996661,0.000051266637,0.000012105522,0.000016145554,0.00002060079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009912389,0.00027994957,0.00019465736,0.00033177706,0.00022651642,0.00036194889,0.0003779552,0.00038978274,0.00080898503],"category_scores_gemma":[0.0004939679,0.00013477771,0.00028952307,0.00020054472,0.0003163449,0.00036645067,0.00024310163,0.00020616381,0.0000754897],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007608676,0.00016181378,0.112822406,0.000052236537,0.000057155394,0.0008366408,0.00017644468,0.8481668,0.02848046,0.0035813649,0.00042964268,0.0051589063],"study_design_scores_gemma":[0.000012676747,0.00003337471,0.032531414,0.0000053628273,0.000010869574,0.000067152025,0.00006411016,0.9652866,0.0010812851,0.0007235424,0.0001742517,0.000009407084],"about_ca_topic_score_codex":0.0067341654,"about_ca_topic_score_gemma":0.0046491,"teacher_disagreement_score":0.0067341654,"about_ca_system_score_codex":0.00048886915,"about_ca_system_score_gemma":0.00026339246,"threshold_uncertainty_score":0.013389945},"labels":[],"label_agreement":null},{"id":"W4386694478","doi":"10.1093/gji/ggad354","title":"A commercial finite element approach to modelling Glacial Isostatic Adjustment on spherical self-gravitating compressible earth models","year":2023,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Environment Research Council; Helmholtz Association; Tsinghua University; Swedish National Space Agency; Sight Research UK; Bundesministerium für Bildung und Forschung; Glaucoma Research Foundation","keywords":"Finite element method; Spherical harmonics; Compressibility; Conformal map; Body force; Mixed finite element method; Geology; Extended finite element method; Post-glacial rebound; Mathematical analysis; Mechanics; Classical mechanics; Geometry; Physics; Mathematics; Ice sheet","score_opus":0.04973349739136877,"score_gpt":0.2646274727983398,"score_spread":0.21489397540697103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386694478","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.017991459,0.00005621047,0.97005534,0.000088508,0.000048940146,0.000066291585,0.00038667483,0.002107359,0.009199218],"genre_scores_gemma":[0.26850355,0.00023105723,0.71900105,0.00008707083,0.000022072261,0.0004538147,0.0011208081,0.0010907686,0.00948984],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999803,0.000036197995,0.000016234584,0.000028110111,0.00010228928,0.000014263999],"domain_scores_gemma":[0.99970716,0.00010145276,0.00002204191,0.00004837163,0.00010923016,0.000011659787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005140988,0.00053074723,0.000342267,0.0005281908,0.00033962895,0.0006936831,0.0012745819,0.0008771549,0.006006271],"category_scores_gemma":[0.0009380365,0.00048550928,0.0006765833,0.00039637525,0.0003656177,0.0004705092,0.0004978656,0.0006774563,0.0014261445],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039764887,0.00005074074,0.0010687255,0.00011538481,0.000035331013,0.00010897403,0.00012500345,0.91715133,0.017454613,0.02351345,0.0021567147,0.038179882],"study_design_scores_gemma":[0.0000053259178,0.000008793272,0.00012288691,0.000007939962,0.000004005938,0.000025321086,0.000013901498,0.9912039,0.002346141,0.0011314306,0.0051241918,0.000006236399],"about_ca_topic_score_codex":0.005039517,"about_ca_topic_score_gemma":0.00607669,"teacher_disagreement_score":0.006006271,"about_ca_system_score_codex":0.0004576814,"about_ca_system_score_gemma":0.0007473415,"threshold_uncertainty_score":0.020092964},"labels":[],"label_agreement":null},{"id":"W4386708823","doi":"10.26443/seismica.v2i2.384","title":"Assessing earthquake rates and b-value given spatiotemporal variation in catalog completeness: Application to Atlantic Canada","year":2023,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Seismometer; Completeness (order theory); Estimator; Seismic hazard; Seismology; Geology; Variation (astronomy); Statistics; Computer science; Mathematics; Physics","score_opus":0.019187591148806547,"score_gpt":0.24300042565094032,"score_spread":0.22381283450213377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386708823","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9466302,0.0005858159,0.038656782,0.0005873106,0.000016461358,0.00007000344,0.008615946,0.0009778532,0.0038596212],"genre_scores_gemma":[0.97662747,0.00012759614,0.019716669,0.000025333171,0.0000090028325,0.000014798116,0.002794151,0.00008196418,0.0006029259],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994754,0.00012764089,0.00003781213,0.00014915701,0.00014280439,0.00006718246],"domain_scores_gemma":[0.9945919,0.0021376244,0.0008032652,0.00069613237,0.0015076082,0.0002634246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021590136,0.00031929277,0.00029313046,0.0023714516,0.00059272436,0.0011890868,0.0008181019,0.0003960176,0.0010004615],"category_scores_gemma":[0.018634873,0.00019192074,0.00027309763,0.0036894495,0.00045354204,0.00052537845,0.000749163,0.0004396298,0.00018366054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011032829,0.00002073648,0.8564089,0.000053731885,0.00016676245,0.00014211169,0.0003940923,0.07060296,0.0017797375,0.0014179255,0.002742155,0.06616058],"study_design_scores_gemma":[0.000019372175,0.000015702331,0.73857373,0.000030142968,0.000041488067,0.000088109016,0.0004598102,0.2549001,0.0012475434,0.0011947755,0.0033983716,0.000030871826],"about_ca_topic_score_codex":0.81167436,"about_ca_topic_score_gemma":0.811049,"teacher_disagreement_score":0.18832564,"about_ca_system_score_codex":0.0033485612,"about_ca_system_score_gemma":0.0040186383,"threshold_uncertainty_score":0.3788694},"labels":[],"label_agreement":null},{"id":"W4386907662","doi":"10.1038/s41598-023-42433-2","title":"Analyzing the horizontal orientation of the crustal stress adjacent to plate boundaries","year":2023,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University; University of Calgary","funders":"Deutsche Forschungsgemeinschaft","keywords":"Stress (linguistics); Stress field; Geometry; Orientation (vector space); Lithosphere; Geology; Reference frame; Geodesy; Computer science; Mathematics; Tectonics; Finite element method; Structural engineering; Frame (networking); Seismology; Telecommunications; Engineering","score_opus":0.016714630413756953,"score_gpt":0.23564774437460453,"score_spread":0.21893311396084758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386907662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86248386,0.00034031828,0.13068324,0.000064733336,0.000028606597,0.00002728791,0.001252253,0.0005011881,0.0046184803],"genre_scores_gemma":[0.98257464,0.0002130328,0.015762242,0.000008943247,0.00001161658,0.00001586707,0.0006162975,0.000058619178,0.00073869695],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.000015014116,0.0000062087634,0.000044928765,0.000026695576,0.000018735545],"domain_scores_gemma":[0.99975544,0.000067413435,0.00008706824,0.000034316712,0.000038536167,0.000017184204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002722574,0.00036837044,0.00023978538,0.0008229046,0.00016326719,0.00037747074,0.00027914892,0.00024655845,0.0020631214],"category_scores_gemma":[0.00096331094,0.00014360137,0.00031520452,0.0010040714,0.0003804445,0.0002527553,0.00029672077,0.00016081792,0.000414518],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016684526,0.00009578119,0.3239692,0.00035837851,0.00027032167,0.00037602795,0.00033732623,0.32840064,0.098736405,0.0070817014,0.001367782,0.23883964],"study_design_scores_gemma":[0.000012079021,0.00015018393,0.46348402,0.000055247834,0.00008130662,0.00029091677,0.0002729951,0.5056399,0.020854488,0.0067776786,0.002315933,0.00006526899],"about_ca_topic_score_codex":0.00551022,"about_ca_topic_score_gemma":0.0075767175,"teacher_disagreement_score":0.00551022,"about_ca_system_score_codex":0.00031935883,"about_ca_system_score_gemma":0.00049487816,"threshold_uncertainty_score":0.010956287},"labels":[],"label_agreement":null},{"id":"W4387091684","doi":"10.1126/sciadv.adh4973","title":"A multifault earthquake threat for the Seattle metropolitan region revealed by mass tree mortality","year":2023,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of the Fraser Valley","funders":"U.S. Geological Survey","keywords":"Seismology; Magnitude (astronomy); Geology; Seismic hazard; Fault (geology); Metropolitan area; Hazard; Geography; Archaeology","score_opus":0.03962927364404527,"score_gpt":0.30037875928321706,"score_spread":0.2607494856391718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387091684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992654,0.000015419177,0.00009178723,0.000032800424,0.0000011789355,0.0000016959907,0.00007825033,0.000004043297,0.00050953485],"genre_scores_gemma":[0.9996137,0.000020679207,0.00017576905,0.0000058192586,0.0000015998429,0.0000016609133,0.00008839343,7.749028e-7,0.00009158257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999949,0.000016530314,0.0000030184551,0.0000137573825,0.000008423765,0.000009335728],"domain_scores_gemma":[0.99963653,0.00008689647,0.0001463008,0.000035589463,0.0000327081,0.000061991814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016261899,0.00018048416,0.000051752693,0.00065031426,0.0002408437,0.00040574916,0.00016424668,0.00024242298,0.0006892669],"category_scores_gemma":[0.0008234045,0.0000738773,0.000063192245,0.00035059062,0.00015881284,0.00031735474,0.0003905551,0.0003288058,0.00007323716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009320783,0.000043003714,0.97876257,0.000013668592,0.00002705166,0.00059189857,0.0009465082,0.0008705173,0.0056781205,0.0003287374,0.0004112413,0.01223341],"study_design_scores_gemma":[0.0000020789391,0.000092748414,0.99457955,0.000012070104,0.000012250095,0.00023458511,0.0012651714,0.0025491759,0.0005210691,0.00019541415,0.0005297889,0.000006059907],"about_ca_topic_score_codex":0.008528438,"about_ca_topic_score_gemma":0.03327032,"teacher_disagreement_score":0.008528438,"about_ca_system_score_codex":0.00024429592,"about_ca_system_score_gemma":0.00017160509,"threshold_uncertainty_score":0.016957581},"labels":[],"label_agreement":null},{"id":"W4387159462","doi":"10.22541/essoar.169603576.62422229/v1","title":"A complex Queen Charlotte Plate Boundary offshore Haida Gwaii","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Geological Survey of Canada; Natural Resources Canada; University of Victoria; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Induced seismicity; Seismology; Submarine pipeline; North American Plate; Plate tectonics; Thrust fault; Subduction; Aftershock; Pacific Plate; Fault (geology); Tectonics; Oceanography","score_opus":0.06205272788934058,"score_gpt":0.2598521272972844,"score_spread":0.19779939940794383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387159462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920989,0.00011249512,0.00048534252,0.00009830104,0.000011713878,0.000037850856,0.0005422544,0.00004059913,0.006572448],"genre_scores_gemma":[0.9952618,0.000066019835,0.0013093702,0.000036898364,0.0000038681046,0.00001882696,0.0007170074,0.000008319953,0.002577854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998728,0.0000051429356,0.0000054291536,0.00004003667,0.000046030622,0.000030449693],"domain_scores_gemma":[0.9997024,0.000024052142,0.000079977464,0.000028423334,0.00008611571,0.000078955745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000095757634,0.0001692861,0.00021577551,0.0008301072,0.0010173013,0.0010171807,0.00033419128,0.00038727006,0.0015248017],"category_scores_gemma":[0.0005765117,0.00022988296,0.0000932107,0.0013127982,0.0007299842,0.00030459618,0.00073420233,0.00030984712,0.00023382393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033738927,0.000059858427,0.88106275,0.00020797004,0.000057335004,0.006257741,0.0061308355,0.0055544134,0.042910088,0.002645475,0.0046787392,0.050097365],"study_design_scores_gemma":[0.000016294709,0.000032575448,0.98552555,0.000056452835,0.000015712758,0.0004916591,0.0020105876,0.0033983153,0.001647675,0.00018004245,0.006602146,0.000022994587],"about_ca_topic_score_codex":0.43373907,"about_ca_topic_score_gemma":0.654242,"teacher_disagreement_score":0.56626093,"about_ca_system_score_codex":0.0017749734,"about_ca_system_score_gemma":0.003149048,"threshold_uncertainty_score":0.86242884},"labels":[],"label_agreement":null},{"id":"W4387224709","doi":"10.36487/acg_repo/2325_11","title":"Delineation of hazard-based design events for dynamic support system analysis","year":2023,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic hazard; Process (computing); Hazard; Seismic analysis; Hazard analysis; Seismic loading; Incremental Dynamic Analysis; Systems design; Reliability engineering; Computer science; Engineering; Structural engineering; Civil engineering; Systems engineering","score_opus":0.034684915338712985,"score_gpt":0.2598232245134167,"score_spread":0.22513830917470373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387224709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6606013,0.00018259276,0.31620824,0.00014450641,0.000019721334,0.00090197736,0.0023838852,0.000919491,0.018638352],"genre_scores_gemma":[0.90001345,0.00007386501,0.09653694,0.000021882048,0.0000066247885,0.00022395507,0.0014114376,0.00007729751,0.0016345496],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99962544,0.00006119089,0.00002899752,0.000063623236,0.00013939559,0.00008137117],"domain_scores_gemma":[0.9986493,0.00045751827,0.00031116325,0.000091689624,0.00036651967,0.00012382296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082567363,0.0006140244,0.00034910697,0.0031136998,0.0005913979,0.001098574,0.00048729524,0.00052908395,0.003005553],"category_scores_gemma":[0.0024876536,0.00028229822,0.0003436594,0.0014214903,0.00048334477,0.00064107386,0.0008020736,0.00050830597,0.0005485417],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011609474,0.00080647954,0.297327,0.0005866256,0.00006418478,0.0017596647,0.0033245068,0.2709952,0.11074432,0.020193378,0.0048223156,0.2882154],"study_design_scores_gemma":[0.00007613987,0.00064177404,0.389525,0.00019355728,0.00006417211,0.00069620344,0.00457642,0.5409785,0.03661208,0.010185862,0.016319804,0.00013049241],"about_ca_topic_score_codex":0.010046515,"about_ca_topic_score_gemma":0.013655044,"teacher_disagreement_score":0.010046515,"about_ca_system_score_codex":0.0012062892,"about_ca_system_score_gemma":0.0010752053,"threshold_uncertainty_score":0.01997608},"labels":[],"label_agreement":null},{"id":"W4387380806","doi":"10.1139/cjes-2023-0077","title":"Structural geology of the Mount Meager Volcanic Complex, BC, Canada: implications for geothermal energy and geohazards","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"University of Lethbridge; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs; Natural Resources Canada; Geological Society of America","keywords":"Geology; Volcano; Massif; Geochemistry; Volcanic arc; Structural geology; Geothermal gradient; Seismology; Lineament; Subduction; Geomorphology; Paleontology; Tectonics","score_opus":0.03394532962066612,"score_gpt":0.22607933282606785,"score_spread":0.19213400320540172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387380806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9700825,0.0036300842,0.00024343278,0.0037336359,0.000026678255,0.000043033928,0.0023597812,0.00002965222,0.019851182],"genre_scores_gemma":[0.99436754,0.0015266549,0.00046786416,0.00015249795,0.000009622314,0.000008962835,0.00047977897,0.000012941337,0.0029742336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966335,0.000017046725,0.000008866407,0.000049989474,0.00012425889,0.00013648355],"domain_scores_gemma":[0.99910116,0.000051017214,0.00011306105,0.000022061748,0.0004784228,0.00023434458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002392898,0.00034444264,0.0002535211,0.0021781952,0.0038793283,0.0018300366,0.0013057193,0.0005644043,0.003661036],"category_scores_gemma":[0.0013115985,0.00020142355,0.00019943739,0.0039090193,0.00159951,0.0005123956,0.00075802754,0.0005642454,0.00026175124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009761926,0.000064180196,0.88426477,0.0002915357,0.00010253228,0.0010168058,0.007631683,0.0022711148,0.007495619,0.004732852,0.0073972936,0.084633924],"study_design_scores_gemma":[0.000002383388,0.0000075205085,0.9838335,0.000083960615,0.000012821862,0.00011439821,0.005577483,0.00083458837,0.00022468467,0.00020405086,0.009088105,0.000016593956],"about_ca_topic_score_codex":0.996741,"about_ca_topic_score_gemma":0.9991492,"teacher_disagreement_score":0.047879208,"about_ca_system_score_codex":0.047879208,"about_ca_system_score_gemma":0.04190578,"threshold_uncertainty_score":0.34738958},"labels":[],"label_agreement":null},{"id":"W4387407918","doi":"10.3390/e25101419","title":"Viscoelastic Slider Blocks as a Model for a Seismogenic Fault","year":2023,"lang":"en","type":"article","venue":"Entropy","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Viscoelasticity; Standard linear solid model; Geology; Fault (geology); Seismology; Rheology; Nonlinear system; Foreshock; Physics","score_opus":0.02442601624411549,"score_gpt":0.250670664647649,"score_spread":0.22624464840353348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387407918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81918776,0.00035219063,0.16204111,0.0005289148,0.000076053475,0.00009901636,0.0005284404,0.00023704478,0.01694945],"genre_scores_gemma":[0.98872924,0.00028599348,0.004765156,0.00002885692,0.000024256064,0.00008458726,0.00013626956,0.000025051417,0.0059206043],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999337,0.000019439727,0.0000047463327,0.000014674897,0.000014480586,0.000012998945],"domain_scores_gemma":[0.99979645,0.00007024563,0.000061914514,0.000023254637,0.000021628586,0.000026638854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014838502,0.0003370733,0.00041723382,0.00042166575,0.00029719755,0.0006785797,0.0008615535,0.00095497054,0.0031440537],"category_scores_gemma":[0.00063035544,0.00025840328,0.00052914396,0.00031845522,0.0005300051,0.0009305616,0.00044807186,0.0004486762,0.00041491629],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030594114,0.000026373118,0.001050969,0.000021445898,0.000018140696,0.00013146506,0.0000561601,0.97760856,0.0038900746,0.015842061,0.00014614145,0.0011779654],"study_design_scores_gemma":[0.000011321448,0.000027548389,0.00029176494,0.0000031845232,0.0000069122457,0.000023528108,0.000009866102,0.99730057,0.00021757795,0.0017379548,0.0003658854,0.000003997763],"about_ca_topic_score_codex":0.0045717782,"about_ca_topic_score_gemma":0.0018396457,"teacher_disagreement_score":0.0045717782,"about_ca_system_score_codex":0.00039362212,"about_ca_system_score_gemma":0.00047694374,"threshold_uncertainty_score":0.010517895},"labels":[],"label_agreement":null},{"id":"W4387521659","doi":"10.22541/essoar.169705905.51848949/v1","title":"Controls on Bending-Related Faulting Offshore of the Alaska Peninsula","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Seismology; Trench; Bathymetry; Subduction; Fault (geology); Submarine pipeline; Curvature; Seamount; Slab; Tectonics; Geophysics; Geometry; Paleontology; Geotechnical engineering","score_opus":0.03416116391202991,"score_gpt":0.24548665562719896,"score_spread":0.21132549171516904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387521659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983333,0.000058857124,0.00009720979,0.000015754897,0.0000022297681,0.0000015749134,0.00012860335,0.0000059116373,0.0013565719],"genre_scores_gemma":[0.9994254,0.00005532794,0.00008296896,0.0000065132126,9.27251e-7,0.0000018790314,0.000109500026,0.0000022331803,0.00031521768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986255,0.00001807833,0.000017386737,0.000054434826,0.000023358869,0.000024097417],"domain_scores_gemma":[0.9995553,0.00006252199,0.00017742791,0.000043477427,0.00007553973,0.00008567138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021622055,0.0002744183,0.00015824418,0.0005122862,0.00035270312,0.0006324355,0.00019263686,0.00016019044,0.0016905891],"category_scores_gemma":[0.00060757424,0.00017562966,0.0001368641,0.00045449697,0.00045732554,0.000303191,0.00049654517,0.00016664118,0.00019996714],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019727724,0.000028318242,0.91090953,0.00005755557,0.00007828214,0.000414732,0.0014094044,0.0023810037,0.07533033,0.00053019106,0.00014874931,0.008514587],"study_design_scores_gemma":[0.0000017462348,0.000021780266,0.99709976,0.000010477368,0.000011650601,0.000048821108,0.0007674887,0.00037542073,0.0011543421,0.000110878,0.00039023138,0.000007477433],"about_ca_topic_score_codex":0.021540465,"about_ca_topic_score_gemma":0.046423472,"teacher_disagreement_score":0.021540465,"about_ca_system_score_codex":0.0004699469,"about_ca_system_score_gemma":0.00037299274,"threshold_uncertainty_score":0.04283017},"labels":[],"label_agreement":null},{"id":"W4387706826","doi":"10.22541/essoar.169755236.64324581/v1","title":"Controls on Bending-Related Faulting Offshore of the Alaska Peninsula","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Seismology; Trench; Subduction; Bathymetry; Fault (geology); Submarine pipeline; Curvature; Slab; Seamount; Tectonics; Geophysics; Geometry; Paleontology; Geotechnical engineering","score_opus":0.03416116391202991,"score_gpt":0.24548665562719896,"score_spread":0.21132549171516904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387706826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983333,0.000058857124,0.00009720979,0.000015754897,0.0000022297681,0.0000015749134,0.00012860335,0.0000059116373,0.0013565719],"genre_scores_gemma":[0.9994254,0.00005532794,0.00008296896,0.0000065132126,9.27251e-7,0.0000018790314,0.000109500026,0.0000022331803,0.00031521768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986255,0.00001807833,0.000017386737,0.000054434826,0.000023358869,0.000024097417],"domain_scores_gemma":[0.9995553,0.00006252199,0.00017742791,0.000043477427,0.00007553973,0.00008567138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021622055,0.0002744183,0.00015824418,0.0005122862,0.00035270312,0.0006324355,0.00019263686,0.00016019044,0.0016905891],"category_scores_gemma":[0.00060757424,0.00017562966,0.0001368641,0.00045449697,0.00045732554,0.000303191,0.00049654517,0.00016664118,0.00019996714],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019727724,0.000028318242,0.91090953,0.00005755557,0.00007828214,0.000414732,0.0014094044,0.0023810037,0.07533033,0.00053019106,0.00014874931,0.008514587],"study_design_scores_gemma":[0.0000017462348,0.000021780266,0.99709976,0.000010477368,0.000011650601,0.000048821108,0.0007674887,0.00037542073,0.0011543421,0.000110878,0.00039023138,0.000007477433],"about_ca_topic_score_codex":0.021540465,"about_ca_topic_score_gemma":0.046423472,"teacher_disagreement_score":0.021540465,"about_ca_system_score_codex":0.0004699469,"about_ca_system_score_gemma":0.00037299274,"threshold_uncertainty_score":0.04283017},"labels":[],"label_agreement":null},{"id":"W4387770979","doi":"10.1134/s0016852123050060","title":"Neotectonic Indications in Iraq (North of the Arabian Plate): Analytical Overview","year":2023,"lang":"en","type":"article","venue":"Geotectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"","keywords":"Geology; Tectonics; Terrane; Seismology; Structural geology; Collision zone; Plate tectonics; Eurasian Plate; Collision; Neotectonics; Continental collision; Paleontology; Deformation (meteorology); Lineament; Lithosphere; Subduction; Oceanography","score_opus":0.03704880418681311,"score_gpt":0.24780527676068353,"score_spread":0.21075647257387042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387770979","genre_codex":"empirical","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9606174,0.004645084,0.001356978,0.00027014193,0.00002523602,0.00005717407,0.002315197,0.000030907468,0.03068204],"genre_scores_gemma":[0.99298954,0.0025827799,0.0014035241,0.000026228421,0.000034787332,0.00001708276,0.0009809149,0.0000051475804,0.0019599793],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998621,0.000024407003,0.0000151450295,0.000021952534,0.000043996417,0.00003243322],"domain_scores_gemma":[0.9995782,0.00005849222,0.000113266266,0.000012634975,0.00021256655,0.00002478389],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034047075,0.00025570297,0.00010734425,0.006140562,0.0003245271,0.00061233045,0.00026818455,0.00013982314,0.0022877303],"category_scores_gemma":[0.00048766276,0.00009702404,0.00021173632,0.00475703,0.00035800174,0.00034032227,0.0005198603,0.00015813224,0.0003372049],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053127846,0.000046185218,0.917981,0.00039024698,0.00007608587,0.00081300485,0.0040612696,0.0020072213,0.0020509644,0.0035013403,0.0015242214,0.0674954],"study_design_scores_gemma":[0.0000012743698,0.000019620538,0.9851805,0.000072362476,0.000017282631,0.00022466255,0.0048906314,0.00079519465,0.00025251176,0.00021558224,0.008325289,0.000005104255],"about_ca_topic_score_codex":0.034002505,"about_ca_topic_score_gemma":0.05299564,"teacher_disagreement_score":0.034002505,"about_ca_system_score_codex":0.00096570473,"about_ca_system_score_gemma":0.00061505317,"threshold_uncertainty_score":0.06760919},"labels":[],"label_agreement":null},{"id":"W4387779734","doi":"10.31223/x5pm4b","title":"Detection of Hidden Low-Frequency Earthquakes in Southern Vancouver Island with Deep Learning","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lawrence Livermore National Laboratory; U.S. Geological Survey; U.S. Department of Energy; National Science Foundation","keywords":"Magnitude (astronomy); Computer science; Waveform; Seismology; Subduction; Deep learning; Artificial intelligence; Geology; Physics; Telecommunications; Tectonics","score_opus":0.014235668798072408,"score_gpt":0.20243010064351577,"score_spread":0.18819443184544335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387779734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98887455,0.00030631694,0.0075652064,0.00038301197,0.00002263203,0.000015415624,0.0010982684,0.00035377848,0.0013808821],"genre_scores_gemma":[0.99311996,0.00007976806,0.0035288436,0.00003294493,0.000008470056,0.0000053986723,0.0019993482,0.000015235925,0.001210036],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999063,0.000011780014,0.000004937054,0.00003341704,0.000019227327,0.000024358784],"domain_scores_gemma":[0.9996524,0.00009800797,0.000039860308,0.000038700608,0.00010992022,0.0000612813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023301052,0.0006639352,0.00031789255,0.0006454813,0.0004195481,0.00069195457,0.000799821,0.0005336283,0.00073687115],"category_scores_gemma":[0.0012355166,0.00037183127,0.00024399912,0.0007201882,0.0002803887,0.0003798923,0.00060101337,0.0007733698,0.00026225383],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002556554,0.00021118532,0.20969033,0.00009876069,0.0001809257,0.0006110002,0.00023737233,0.6673568,0.005775832,0.0005134401,0.005949265,0.10911936],"study_design_scores_gemma":[0.000013237603,0.000010325503,0.023221944,0.000008753852,0.000009858509,0.000014457955,0.00006224308,0.9753982,0.00060227496,0.0002922737,0.00035945344,0.0000068899276],"about_ca_topic_score_codex":0.52679867,"about_ca_topic_score_gemma":0.6653941,"teacher_disagreement_score":0.47320133,"about_ca_system_score_codex":0.0017915119,"about_ca_system_score_gemma":0.0020767981,"threshold_uncertainty_score":0.95197624},"labels":[],"label_agreement":null},{"id":"W4387823780","doi":"10.1139/cjes-2023-0078","title":"Seismicity and seismic monitoring of Canada’s volcanic zones","year":2023,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Canadiana.org; Geological Survey of Canada","funders":"Natural Resources Canada","keywords":"Geology; Induced seismicity; Seismology; Volcano","score_opus":0.02697585243542734,"score_gpt":0.21328443844342276,"score_spread":0.18630858600799544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387823780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96584266,0.0014487866,0.00047436767,0.00045588592,0.000016648419,0.000051804327,0.010847884,0.00006004927,0.020801833],"genre_scores_gemma":[0.98973244,0.0009767701,0.0006510242,0.00007841367,0.000008645569,0.000012332127,0.0052438565,0.000010760581,0.003285777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996107,0.000011105439,0.000016261365,0.00005197368,0.00020350887,0.00010647447],"domain_scores_gemma":[0.99827147,0.00005876935,0.00019199509,0.000029057886,0.0012006356,0.00024809994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002429568,0.00024865576,0.0001197885,0.0030203736,0.0015988894,0.0012188625,0.0006247944,0.0002472489,0.0012115834],"category_scores_gemma":[0.0012740982,0.00017632802,0.00013171905,0.0042999657,0.0004499918,0.00034595368,0.00062007527,0.00034277642,0.00018142899],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007591597,0.00003135,0.947428,0.000095293086,0.00005493718,0.0001905283,0.002155624,0.0009652278,0.0023001372,0.00045353227,0.0047020344,0.04154743],"study_design_scores_gemma":[0.000003219327,0.0000093918525,0.9899442,0.000039891107,0.00001401305,0.000052280684,0.0014338924,0.0005528072,0.0005319068,0.00003410119,0.0073691807,0.000015055744],"about_ca_topic_score_codex":0.9924096,"about_ca_topic_score_gemma":0.9974371,"teacher_disagreement_score":0.01617358,"about_ca_system_score_codex":0.01617358,"about_ca_system_score_gemma":0.018692361,"threshold_uncertainty_score":0.117348075},"labels":[],"label_agreement":null},{"id":"W4387827063","doi":"10.1029/2023gc011088","title":"A Cascadia Slab Model From Receiver Functions","year":2023,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; University of British Columbia","funders":"RES’EAU-WaterNET; Deutsche Forschungsgemeinschaft","keywords":"Geology; Slab; Terrane; Slab window; Seismology; Subduction; Underplating; Receiver function; Forearc; North American Plate; Crust; Oceanic crust; Geophysics; Tectonics; Lithosphere","score_opus":0.018326230645954778,"score_gpt":0.20289774535558336,"score_spread":0.18457151470962857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387827063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7989662,0.0005297163,0.17067586,0.00089161244,0.00007960364,0.00008406906,0.0041552125,0.0018389123,0.022778656],"genre_scores_gemma":[0.98218817,0.00020884455,0.007763247,0.000029630937,0.000019867866,0.00008011707,0.0010174889,0.00010696788,0.008585505],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998481,0.000033221495,0.000006023532,0.000052806143,0.00002605743,0.00003365387],"domain_scores_gemma":[0.9997732,0.000059095448,0.000039127633,0.000025345738,0.00006903425,0.000034277124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032061417,0.0011032394,0.00045942722,0.0009736272,0.0006220473,0.0010769151,0.0020450437,0.0013153777,0.0043414338],"category_scores_gemma":[0.00079263805,0.0008186404,0.00091142673,0.0011389777,0.0007327666,0.00059748,0.00063763745,0.0006812217,0.0007476381],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026010248,0.000010736127,0.0023054508,0.000010044173,0.000019125951,0.000058341455,0.000038194215,0.9934189,0.00056565384,0.0019499969,0.0002333558,0.0013643097],"study_design_scores_gemma":[0.0000102030035,0.000006242868,0.00084295846,0.000003752684,0.000008434888,0.000011279445,0.000014410044,0.9979936,0.000047342222,0.00072075595,0.00033276537,0.000008221998],"about_ca_topic_score_codex":0.1908848,"about_ca_topic_score_gemma":0.066718064,"teacher_disagreement_score":0.1908848,"about_ca_system_score_codex":0.0019788719,"about_ca_system_score_gemma":0.0018442895,"threshold_uncertainty_score":0.37954748},"labels":[],"label_agreement":null},{"id":"W4388007591","doi":"10.1016/j.apor.2023.103784","title":"Improvement to stochastic tsunami hazard analysis of megathrust earthquakes for western Makran subduction zone","year":2023,"lang":"en","type":"article","venue":"Applied Ocean Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Iranian National Institute for Oceanography and Atmospheric Science","keywords":"Seismology; Subduction; Geology; Slip (aerodynamics); Tsunami earthquake; Seismic hazard; Induced seismicity; Tectonics; Physics","score_opus":0.07128284991455906,"score_gpt":0.33357977099430147,"score_spread":0.2622969210797424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388007591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8791589,0.00012527544,0.118669465,0.0001121022,0.000018548946,0.000040011695,0.0005204903,0.00034986966,0.0010053809],"genre_scores_gemma":[0.98856735,0.00004633789,0.0103835575,0.0000072978373,0.000012054587,0.000013532917,0.00056149496,0.00001535872,0.00039305203],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998425,0.000049454826,0.000015575073,0.000038363218,0.000028341996,0.000025645426],"domain_scores_gemma":[0.99933136,0.00024998785,0.00006666535,0.00006440498,0.00025298962,0.00003450172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005713086,0.00031671912,0.0002944278,0.0005084431,0.00028147077,0.00036583495,0.00060156867,0.00020903032,0.0014065505],"category_scores_gemma":[0.0022081388,0.0001637655,0.0005348394,0.0003381936,0.00006666037,0.00034149166,0.00035904898,0.0002434781,0.00024953354],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035714102,0.00022766457,0.11821448,0.00010872114,0.00018976172,0.00024517925,0.00019832425,0.7087053,0.013733345,0.002053504,0.0011149801,0.1548516],"study_design_scores_gemma":[0.0000051687452,0.000033168155,0.014158793,0.0000016459772,0.000012635231,0.000014237584,0.000030899526,0.98483235,0.00048631878,0.00025986813,0.00016110195,0.000003862059],"about_ca_topic_score_codex":0.018240435,"about_ca_topic_score_gemma":0.01742343,"teacher_disagreement_score":0.018240435,"about_ca_system_score_codex":0.00026015195,"about_ca_system_score_gemma":0.00094723405,"threshold_uncertainty_score":0.036268473},"labels":[],"label_agreement":null},{"id":"W4388039276","doi":"10.1016/j.tecto.2023.230086","title":"Seismogenic structures and earthquake mechanisms in the Changning area, China: Insights from seismicity and tomography","year":2023,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Seismology; Anticline; Induced seismicity; Tectonics; Seismic tomography; Fault (geology); Geophysics; Mantle (geology)","score_opus":0.014675617207608717,"score_gpt":0.19939382509640066,"score_spread":0.18471820788879195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388039276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999348,0.00008012742,0.00007370437,0.000035616667,0.0000012552966,0.0000034836116,0.00011933089,0.0000035804096,0.00033492944],"genre_scores_gemma":[0.9995721,0.00006766165,0.000057969522,0.0000045020965,0.0000025106165,0.0000017348622,0.00013255922,7.3493163e-7,0.00016023629],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990165,0.000010665117,0.00001036159,0.000026500866,0.000018820409,0.00003201026],"domain_scores_gemma":[0.9997063,0.000038936596,0.000099376135,0.000016826722,0.00007265121,0.00006582998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022074691,0.0003341473,0.00018862706,0.0026825953,0.0005075841,0.0005149102,0.00040733092,0.00029144148,0.00061079575],"category_scores_gemma":[0.0005069245,0.0002595999,0.00018459737,0.003417146,0.00065616803,0.0005357256,0.00052068004,0.00013622429,0.00007223174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009286599,0.000057256577,0.97153777,0.000049045375,0.000056410034,0.0005148936,0.0011463341,0.0037228034,0.00697482,0.00075816264,0.00021741836,0.014872246],"study_design_scores_gemma":[0.00000462697,0.000012968531,0.9970777,0.0000040330374,0.000013954397,0.000041899315,0.00042006042,0.002102603,0.00007937237,0.000096574106,0.00014112418,0.000005159849],"about_ca_topic_score_codex":0.16014622,"about_ca_topic_score_gemma":0.24024746,"teacher_disagreement_score":0.16014622,"about_ca_system_score_codex":0.0012951894,"about_ca_system_score_gemma":0.0017205381,"threshold_uncertainty_score":0.31842816},"labels":[],"label_agreement":null},{"id":"W4388160105","doi":"10.3390/min13111381","title":"Effects of Paleoregolith and Fault Offset on the Formation of Unconformity-Type Uranium Deposits","year":2023,"lang":"en","type":"article","venue":"Minerals","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Unconformity; Geology; Regolith; Sedimentary rock; Uranium ore; Geochemistry; Uranium; Fault (geology); Structural basin; Sedimentary basin; Petrology; Mineralogy; Geomorphology; Seismology","score_opus":0.01651682568552083,"score_gpt":0.21639566376564373,"score_spread":0.1998788380801229,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388160105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99939525,0.000084626634,0.00008651164,0.000006014422,0.0000014180729,8.4450386e-7,0.00004232165,0.0000092906375,0.00037368675],"genre_scores_gemma":[0.99976593,0.000041279134,0.000045121367,0.0000022211655,3.9998233e-7,6.071749e-7,0.000034351484,0.0000036581034,0.00010637874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998646,0.000023161005,0.000011832372,0.000030046749,0.00001879944,0.000051521252],"domain_scores_gemma":[0.99975556,0.00009919696,0.00006184341,0.000021330583,0.000021531634,0.00004046957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023418537,0.0003345432,0.00035636558,0.0005347943,0.0003284333,0.0007884146,0.00031548954,0.00032291425,0.0019986446],"category_scores_gemma":[0.0007009492,0.00021198235,0.00033582444,0.0004530609,0.000668479,0.0003036101,0.00068601646,0.0001691454,0.00016389327],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019110116,0.00013681175,0.7317631,0.00031402247,0.0003254531,0.0017250037,0.0005303743,0.051322974,0.1893664,0.0009220542,0.00021330915,0.021469431],"study_design_scores_gemma":[0.000026217695,0.00021252857,0.951989,0.000017092978,0.00014894642,0.00020739855,0.00065407366,0.020706603,0.025005277,0.0001888596,0.00082178955,0.00002227963],"about_ca_topic_score_codex":0.009470627,"about_ca_topic_score_gemma":0.011735782,"teacher_disagreement_score":0.009470627,"about_ca_system_score_codex":0.0005363978,"about_ca_system_score_gemma":0.0003950391,"threshold_uncertainty_score":0.018831015},"labels":[],"label_agreement":null},{"id":"W4388195608","doi":"10.1016/j.pepi.2023.107116","title":"Recognition of the causative fault of the 2017 MW 4.9 Malard (Tehran, Iran) earthquake from directivity analysis of the recorded ground motions","year":2023,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Directivity; Geology; Fault (geology); Geodesy; Computer science","score_opus":0.037627179410426655,"score_gpt":0.2287223857575899,"score_spread":0.19109520634716326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388195608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99308455,0.00027355342,0.0037322228,0.0001369628,0.00008523335,0.00003668883,0.000546947,0.00004715965,0.0020566897],"genre_scores_gemma":[0.9967796,0.00015143541,0.0018216086,0.000011950059,0.0000503458,0.000007892159,0.0006141018,0.000004366931,0.00055874785],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990165,0.0000067579554,0.000012166188,0.000021528414,0.000031518735,0.000026460863],"domain_scores_gemma":[0.99967337,0.00003352857,0.0000853237,0.000021690366,0.00014261682,0.00004349795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018539131,0.00029022834,0.00018364163,0.001770974,0.00025781337,0.0004696518,0.00025995483,0.00032290685,0.00078227534],"category_scores_gemma":[0.00065763015,0.00012349404,0.00020772716,0.0006000186,0.00023265867,0.0003106964,0.00037188642,0.00028559795,0.0003321711],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035216048,0.00017480121,0.8075805,0.0001738181,0.00008167741,0.0038516647,0.0011503865,0.0030352268,0.06996874,0.0009824221,0.0031009368,0.10954776],"study_design_scores_gemma":[0.000021236405,0.00013518345,0.97764456,0.00003327638,0.00006683673,0.0014329714,0.001574486,0.011627827,0.0042995824,0.00031369945,0.0028309294,0.00001932763],"about_ca_topic_score_codex":0.005083588,"about_ca_topic_score_gemma":0.010096842,"teacher_disagreement_score":0.005083588,"about_ca_system_score_codex":0.00017026662,"about_ca_system_score_gemma":0.0005355485,"threshold_uncertainty_score":0.010107994},"labels":[],"label_agreement":null},{"id":"W4388288867","doi":"10.1038/s43247-023-01064-1","title":"Bayesian inference elucidates fault-system anatomy and resurgent earthquakes induced by continuing saltwater disposal","year":2023,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Induced seismicity; Fault (geology); Hypocenter; Graben; Tectonics","score_opus":0.021858292348869216,"score_gpt":0.24379682510928963,"score_spread":0.22193853276042042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388288867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9866594,0.000027598946,0.011983555,0.00007888412,0.0000016468481,0.0000065684158,0.00017309886,0.00004540431,0.0010238667],"genre_scores_gemma":[0.9989322,0.000007803762,0.00084040326,0.0000045367347,0.0000010205915,5.633463e-7,0.000103742306,0.0000029228463,0.00010669393],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99976784,0.00004751435,0.000012412129,0.00007852642,0.000047952904,0.000045778725],"domain_scores_gemma":[0.99870574,0.0005557984,0.00026535505,0.00012853422,0.0002477836,0.000096825184],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006749311,0.0001449374,0.00017714094,0.00048816812,0.0002778725,0.0005865993,0.00029705674,0.00022028624,0.001015183],"category_scores_gemma":[0.0043186783,0.0001977689,0.00022712714,0.0002999536,0.00052280404,0.0003171415,0.00039866715,0.00030542287,0.000114628],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022738682,0.00004516427,0.79483783,0.00003530352,0.00019288703,0.0003174167,0.0005879427,0.13901296,0.021908835,0.004814801,0.0004624783,0.037557017],"study_design_scores_gemma":[0.000018461446,0.000033352426,0.6697849,0.000011375134,0.00006358508,0.00007330529,0.00029226666,0.32360813,0.002462221,0.0030327952,0.0005973092,0.000022342781],"about_ca_topic_score_codex":0.13120677,"about_ca_topic_score_gemma":0.22538723,"teacher_disagreement_score":0.13120677,"about_ca_system_score_codex":0.0010307982,"about_ca_system_score_gemma":0.001214,"threshold_uncertainty_score":0.26088607},"labels":[],"label_agreement":null},{"id":"W4388328532","doi":"10.5772/intechopen.1003138","title":"The Source Rupture Models and Seismogenic Structures of the Iran 2017 MW 7.3 Earthquake","year":2023,"lang":"en","type":"book-chapter","venue":"IntechOpen eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Epicenter; Interplate earthquake; Fault (geology); Intraplate earthquake; Tectonics","score_opus":0.043759698888151455,"score_gpt":0.2255080791186931,"score_spread":0.18174838023054166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388328532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8400266,0.0034782917,0.11494248,0.000452087,0.00006946029,0.0000753048,0.0031905374,0.001087035,0.036678087],"genre_scores_gemma":[0.9798361,0.0011927952,0.013517603,0.000009935936,0.000014244195,0.000027589454,0.0017828107,0.00006425253,0.003554704],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999776,0.0000042333445,0.0000014257411,0.000004731374,0.000008764194,0.00000315489],"domain_scores_gemma":[0.9999449,0.00002053843,0.000009766548,0.000007479957,0.000013416689,0.0000038550693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012492122,0.00033418142,0.00020887693,0.0005871438,0.00011966987,0.00043393334,0.0006206494,0.00037349356,0.001119172],"category_scores_gemma":[0.0003147568,0.00017750464,0.00045259795,0.000507926,0.000093048286,0.00050817296,0.00012931872,0.00026642147,0.0004133301],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010236756,0.000044180375,0.008441612,0.00010283831,0.000046267352,0.0004025434,0.00015827638,0.9200522,0.005263233,0.0049740956,0.0024519083,0.05796049],"study_design_scores_gemma":[0.0000073010806,0.000031824427,0.0066621364,0.000019847435,0.00001884257,0.00016291317,0.00008172991,0.98679733,0.001022132,0.0029594374,0.0022260116,0.00001045994],"about_ca_topic_score_codex":0.0053672483,"about_ca_topic_score_gemma":0.005306086,"teacher_disagreement_score":0.0053672483,"about_ca_system_score_codex":0.0004283736,"about_ca_system_score_gemma":0.00027106673,"threshold_uncertainty_score":0.010672033},"labels":[],"label_agreement":null},{"id":"W4388464397","doi":"10.1029/2023jb026482","title":"Long‐Lived Aftershocks in the New Madrid seismic Zone and the Rest of Stable North America","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Induced seismicity; Seismology; Geology; Seismic hazard; Magnitude (astronomy)","score_opus":0.04202204991743295,"score_gpt":0.3038474530686018,"score_spread":0.2618254031511688,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388464397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989287,0.00012320565,0.000047172092,0.000024038205,0.0000035312462,0.0000025666902,0.00014539315,0.00000254515,0.0007227855],"genre_scores_gemma":[0.99938476,0.00006232673,0.00005278665,0.000008178177,0.000004643142,0.0000021180365,0.0003128462,0.0000013259519,0.00017099353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998267,0.000029385454,0.000012119004,0.000048211055,0.000038409795,0.000045222165],"domain_scores_gemma":[0.9990214,0.00015824345,0.0003475145,0.000046605954,0.00022588605,0.00020031758],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002955976,0.0001290086,0.00018371308,0.0011759872,0.00033490348,0.00046093113,0.00023414363,0.00016482009,0.0010057617],"category_scores_gemma":[0.0013140792,0.00006295514,0.00015721185,0.0010439577,0.0003143031,0.00031588468,0.00048078876,0.00018476238,0.00013241495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006934511,0.000017234419,0.99517584,0.000013544698,0.00004761858,0.00008339058,0.00039154125,0.00025010362,0.00049097766,0.000087286375,0.00028258568,0.0030905053],"study_design_scores_gemma":[0.0000015209599,0.0000049157343,0.9990381,0.000003689884,0.000005790825,0.000012977755,0.0004789977,0.00020982923,0.000030094465,0.00001607164,0.00019652507,0.0000015802334],"about_ca_topic_score_codex":0.1324364,"about_ca_topic_score_gemma":0.20578818,"teacher_disagreement_score":0.8675636,"about_ca_system_score_codex":0.0007441701,"about_ca_system_score_gemma":0.00038624232,"threshold_uncertainty_score":0.26333106},"labels":[],"label_agreement":null},{"id":"W4388627281","doi":"10.1186/s40562-023-00306-6","title":"Statistical characterization of full-margin rupture recurrence for Cascadia subduction zone using event time resampling and Gaussian mixture model","year":2023,"lang":"en","type":"article","venue":"Geoscience Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Subduction; Geology; Gaussian; Margin (machine learning); Cluster analysis; Resampling; Seismology; Mixture model; Statistical model; Statistics; Algorithm; Tectonics; Computer science; Machine learning; Mathematics","score_opus":0.02394518181744822,"score_gpt":0.24816983167147982,"score_spread":0.2242246498540316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388627281","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78086126,0.0002361354,0.21769135,0.00011663525,0.00001556533,0.000032032603,0.00031572036,0.00031167612,0.0004196737],"genre_scores_gemma":[0.9922488,0.0000531611,0.0069839517,0.000006393715,0.000009974777,0.00001636624,0.00047708896,0.00001746689,0.00018675554],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993482,0.00019687123,0.000054809596,0.0002190576,0.0001307933,0.000050195387],"domain_scores_gemma":[0.99426126,0.003516061,0.00082641747,0.000715293,0.00051837874,0.00016245383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028397513,0.00036912345,0.00045296826,0.0015829146,0.00020420761,0.0005374992,0.00082424213,0.00045700412,0.0006505951],"category_scores_gemma":[0.009174402,0.00023796949,0.0007925135,0.0011360613,0.00039520333,0.00078320777,0.000511954,0.00044485275,0.00014224184],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003187242,0.00010947299,0.21890028,0.000081218066,0.0003858973,0.0003311847,0.00032306206,0.6939707,0.005901909,0.0073221326,0.0006875329,0.071667865],"study_design_scores_gemma":[0.0000018299214,0.000017227227,0.026436932,0.0000029073494,0.000017025142,0.000035139485,0.000021703798,0.97244275,0.00028950983,0.0006409029,0.00008216542,0.000011911893],"about_ca_topic_score_codex":0.009106298,"about_ca_topic_score_gemma":0.0052512214,"teacher_disagreement_score":0.009106298,"about_ca_system_score_codex":0.0004465611,"about_ca_system_score_gemma":0.00041090866,"threshold_uncertainty_score":0.01810658},"labels":[],"label_agreement":null},{"id":"W4388637036","doi":"10.3390/app132212243","title":"Nucleation Mechanism and Rupture Dynamics of Laboratory Earthquakes at Different Loading Rates","year":2023,"lang":"en","type":"article","venue":"Applied Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"China Scholarship Council","keywords":"Nucleation; Slip (aerodynamics); Strain rate; Shear (geology); Geology; Seismology; Materials science; Shear stress; Composite material; Thermodynamics; Physics","score_opus":0.015432536121815698,"score_gpt":0.2190357452055291,"score_spread":0.2036032090837134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388637036","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988367,0.00010221536,0.0007687648,0.000010607457,0.000006813867,0.000009084917,0.00006353655,0.000014182005,0.00018818527],"genre_scores_gemma":[0.99924576,0.00008821675,0.00040014618,0.0000062903305,0.000003811947,0.000014971048,0.00007869369,0.0000031851039,0.00015888255],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99982774,0.00002284209,0.000020764151,0.000036787915,0.000046805453,0.000045028984],"domain_scores_gemma":[0.99966085,0.00010424111,0.0000826533,0.0000482728,0.000041505395,0.00006242819],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028605852,0.0002464757,0.00025650192,0.00026779182,0.00017813129,0.00021147564,0.00027485113,0.00029119707,0.0010544212],"category_scores_gemma":[0.00060637185,0.00017685202,0.00019645276,0.00015580532,0.0003220359,0.00026578846,0.00027390962,0.00037692327,0.00011972625],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025819035,0.00018882066,0.0047938847,0.00005603657,0.000015647507,0.000115072915,0.00010116813,0.0023729017,0.9890832,0.00014961636,0.000065763896,0.002799709],"study_design_scores_gemma":[0.00003960602,0.0029769517,0.0599245,0.000016583183,0.00004502208,0.00016839904,0.0001913547,0.037323024,0.8985087,0.00027104496,0.00050001167,0.000034835884],"about_ca_topic_score_codex":0.000590069,"about_ca_topic_score_gemma":0.00056499476,"teacher_disagreement_score":0.0010544212,"about_ca_system_score_codex":0.00016822907,"about_ca_system_score_gemma":0.00011067384,"threshold_uncertainty_score":0.0035274625},"labels":[],"label_agreement":null},{"id":"W4388657755","doi":"10.1061/9780784485163.070","title":"Development of Tsunami Frequency-Fatality Numbers ( <i>F-N</i> ) Curve for Coastal Communities Subjected to Cascadia Subduction Earthquakes","year":2023,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; Western University","funders":"","keywords":"Subduction; Seismology; Geology; Tide gauge; Case fatality rate; Medicine; Oceanography","score_opus":0.04368960695075517,"score_gpt":0.25960969275900103,"score_spread":0.21592008580824587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388657755","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9859926,0.00008045486,0.005478979,0.00006556109,0.000004302446,0.000024943967,0.0008768992,0.00018047134,0.007295781],"genre_scores_gemma":[0.9970625,0.00004995418,0.0016695843,0.0000053168765,0.0000011655026,0.000010438879,0.00063305855,0.00001877463,0.000549167],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99974984,0.00002905267,0.000016527385,0.000040692103,0.00010096772,0.00006295974],"domain_scores_gemma":[0.9984357,0.00047072367,0.00033668254,0.00012216253,0.000514451,0.00012025573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047467346,0.00045169712,0.00022357832,0.0025949208,0.0003369663,0.0006615042,0.00033661455,0.0004086058,0.0015859319],"category_scores_gemma":[0.0027762717,0.00012142941,0.00040912942,0.0011627926,0.00038154717,0.00037011973,0.00050331035,0.0003416538,0.00027721783],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005246892,0.00010295714,0.59949094,0.000253117,0.00008856454,0.0010408394,0.0013900157,0.31030408,0.012132492,0.0030541029,0.0022114504,0.06940668],"study_design_scores_gemma":[0.00000934818,0.0002281654,0.6375293,0.000067473804,0.000030470426,0.0006855471,0.0016219928,0.34882146,0.0056205555,0.00129536,0.0040207123,0.000069566675],"about_ca_topic_score_codex":0.13084625,"about_ca_topic_score_gemma":0.11683725,"teacher_disagreement_score":0.13084625,"about_ca_system_score_codex":0.0015801514,"about_ca_system_score_gemma":0.00072171853,"threshold_uncertainty_score":0.26016933},"labels":[],"label_agreement":null},{"id":"W4388671775","doi":"10.1061/9780784485163.034","title":"Rapid Multi-Hazard Loss Estimation of Earthquake-Tsunami Impacts for Improved Disaster Response and Recovery","year":2023,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Hazard; Estimation; Computer science; Submarine pipeline; Seismology; Resource allocation; Emergency management; Resource (disambiguation); Hazard analysis; Environmental science; Geology; Reliability engineering; Engineering; Oceanography","score_opus":0.028294518835388294,"score_gpt":0.25826311353586395,"score_spread":0.22996859470047565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388671775","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.42653242,0.00012497211,0.57100415,0.00012134159,0.000015816158,0.000060546092,0.00024747947,0.0008753049,0.0010179636],"genre_scores_gemma":[0.9607762,0.000061815976,0.03855034,0.000009435718,0.0000064547726,0.00002887393,0.00022019245,0.000026758882,0.00031998605],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998135,0.00005838665,0.0000100008165,0.000033173394,0.000056635417,0.000028311459],"domain_scores_gemma":[0.99923027,0.0004147231,0.0001323266,0.000068833106,0.00012401865,0.000029798131],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009916717,0.00059129595,0.00034267822,0.0010411895,0.00018144283,0.00044440496,0.0005051548,0.0003208068,0.0007773478],"category_scores_gemma":[0.0027366257,0.00023500808,0.00040972387,0.0005485961,0.00013511318,0.00087120704,0.0005667115,0.0004030333,0.00019718653],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000806141,0.00012323147,0.019101525,0.000033369495,0.00004364768,0.000079164885,0.000047007088,0.9070313,0.0031186526,0.0007803346,0.00041103963,0.06915008],"study_design_scores_gemma":[0.0000014900747,0.000011857223,0.002426055,0.0000014753323,0.0000029633334,0.000010629173,0.000009210414,0.9967751,0.0005080147,0.00019893573,0.000051244682,0.0000030253152],"about_ca_topic_score_codex":0.0055756723,"about_ca_topic_score_gemma":0.0046551013,"teacher_disagreement_score":0.0055756723,"about_ca_system_score_codex":0.0003471998,"about_ca_system_score_gemma":0.00052241527,"threshold_uncertainty_score":0.011086464},"labels":[],"label_agreement":null},{"id":"W4388671965","doi":"10.26443/seismica.v2i3.1083","title":"The sharp turn: Backward rupture branching during the 2023 Mw 7.8 Kahramanmaraş (Türkiye) earthquake","year":2023,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Key Research and Development Program of China; Horizon 2020; Natural Resources Canada; HORIZON EUROPE European Research Council; National Natural Science Foundation of China; National Oceanic and Atmospheric Administration; Agence Nationale de la Recherche","keywords":"Seismology; Geology; Earthquake rupture; Fault (geology); Feature (linguistics); Branching (polymer chemistry); Materials science","score_opus":0.011432235103974508,"score_gpt":0.2098447296846702,"score_spread":0.19841249458069568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388671965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988318,0.000033538065,0.00020253296,0.000045444296,0.0000051075613,0.0000034842005,0.00006550373,0.000011755646,0.0008008848],"genre_scores_gemma":[0.99975675,0.000014443187,0.00008925178,0.000007818513,0.0000017241869,0.0000029714383,0.000051287847,0.0000023460773,0.00007348733],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992406,0.000013137678,0.0000034976974,0.000017409877,0.00001008685,0.00003176674],"domain_scores_gemma":[0.9998779,0.0000319674,0.000033292865,0.000011028248,0.000011888497,0.000033913588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022870896,0.0003710171,0.00034366266,0.00035587244,0.0004946624,0.0006037468,0.0005103316,0.00094433205,0.0012538693],"category_scores_gemma":[0.0005970664,0.00022524512,0.00043847776,0.00028101465,0.0004735899,0.00052964984,0.00059843686,0.00042935478,0.0001269608],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010635703,0.00037858894,0.23658936,0.00011730353,0.00043286115,0.0045478293,0.0007624204,0.693835,0.042665333,0.004860541,0.0017981549,0.012949056],"study_design_scores_gemma":[0.00022882067,0.00062844757,0.22371951,0.000031585336,0.00018303226,0.0006956459,0.0011724207,0.764901,0.004658307,0.0022614482,0.0014115926,0.00010817406],"about_ca_topic_score_codex":0.014194969,"about_ca_topic_score_gemma":0.016874554,"teacher_disagreement_score":0.014194969,"about_ca_system_score_codex":0.00062706793,"about_ca_system_score_gemma":0.00036802574,"threshold_uncertainty_score":0.028224707},"labels":[],"label_agreement":null},{"id":"W4388760443","doi":"10.26443/seismica.v2i2.498","title":"Inferring rock strength and fault activation from high-resolution in situ Vp/Vs estimates surrounding induced earthquake clusters","year":2023,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Resources Canada; Deutsche Forschungsgemeinschaft; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Geology; Induced seismicity; Poromechanics; Pore water pressure; Slip (aerodynamics); Seismology; Hydraulic fracturing; Fault (geology); Fluid pressure; Sedimentary rock; Structural basin; Shear (geology); Effective stress; Porosity; Geotechnical engineering; Petrology; Porous medium; Geochemistry; Geomorphology; Mechanics","score_opus":0.024385892833894175,"score_gpt":0.23671306766245917,"score_spread":0.212327174828565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388760443","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974542,0.00003674254,0.001271464,0.0000100241605,0.0000012005447,0.0000047968374,0.00044538866,0.000052316736,0.00072377815],"genre_scores_gemma":[0.998961,0.000024141054,0.0006464937,0.0000018988227,6.0676365e-7,0.0000027828094,0.00025428185,0.000005722427,0.0001031811],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999205,0.000006693486,0.000004901119,0.000026850039,0.00001952853,0.000021487347],"domain_scores_gemma":[0.9997732,0.000056592697,0.00005152883,0.000023681467,0.00007009732,0.000024953906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010508028,0.00025728962,0.000205553,0.0011061581,0.0003543318,0.00051393005,0.00038933396,0.00023533522,0.0008570366],"category_scores_gemma":[0.00078272575,0.00022584424,0.00012408341,0.0008911803,0.00023776037,0.00027584162,0.00032754464,0.0002095288,0.00016670793],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011044471,0.00005658233,0.84487486,0.00010121976,0.00011787607,0.0002741203,0.0004913007,0.019454438,0.107664965,0.00014235475,0.00032729717,0.026384471],"study_design_scores_gemma":[0.0000038599665,0.000014098678,0.97198546,0.000007513602,0.000023759378,0.00006376283,0.00030798794,0.02195594,0.005277959,0.000049721853,0.00030017618,0.000009737151],"about_ca_topic_score_codex":0.2420297,"about_ca_topic_score_gemma":0.4271724,"teacher_disagreement_score":0.2420297,"about_ca_system_score_codex":0.0010290468,"about_ca_system_score_gemma":0.0006269756,"threshold_uncertainty_score":0.48124188},"labels":[],"label_agreement":null},{"id":"W4388903579","doi":"10.1144/sp546-2023-63","title":"The importance of nodal plane orientation diversity for earthquake focal mechanism stress inversions","year":2023,"lang":"en","type":"article","venue":"Geological Society London Special Publications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ConocoPhillips (Canada)","funders":"U.S. Geological Survey; Brinson Foundation","keywords":"Focal mechanism; Geology; Fault plane; Seismology; Stress field; Inversion (geology); Stress (linguistics); Shear stress; Shear (geology); Slip (aerodynamics); Plane stress; Critical resolved shear stress; Induced seismicity; Geodesy; Fault (geology); Geometry; Mathematics; Petrology; Tectonics; Mechanics; Structural engineering; Physics","score_opus":0.03413880719341794,"score_gpt":0.24350917448019344,"score_spread":0.2093703672867755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388903579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.77050716,0.00031906614,0.22492057,0.00062048546,0.00004208832,0.00003295394,0.0005333979,0.00040521612,0.0026190705],"genre_scores_gemma":[0.987706,0.000052839903,0.011863643,0.000025393781,0.000023570066,0.000006695097,0.00019719021,0.00004212166,0.00008249168],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99639785,0.0020537353,0.00020645247,0.0005032957,0.00066575897,0.00017287151],"domain_scores_gemma":[0.9407009,0.046883155,0.0034577711,0.005557261,0.0026486658,0.0007522886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010643244,0.00040580062,0.0004037605,0.0009909128,0.00045752653,0.0016121024,0.00063599815,0.0008056904,0.00075870764],"category_scores_gemma":[0.078354865,0.00029125673,0.0002862492,0.00084877445,0.0011719123,0.001470504,0.0014810136,0.0007890148,0.0002474404],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00095921266,0.00010457309,0.44527656,0.00021857805,0.00035216913,0.00053631415,0.0008095195,0.3451585,0.034382083,0.010794936,0.0013233052,0.16008429],"study_design_scores_gemma":[0.00005437385,0.00033753042,0.11269466,0.00010540415,0.0000969241,0.00055889174,0.00045183318,0.8430283,0.01992943,0.021170793,0.0014791746,0.00009263816],"about_ca_topic_score_codex":0.0015594177,"about_ca_topic_score_gemma":0.0022582642,"teacher_disagreement_score":0.010643244,"about_ca_system_score_codex":0.00034898464,"about_ca_system_score_gemma":0.0005111597,"threshold_uncertainty_score":0.056287527},"labels":[],"label_agreement":null},{"id":"W4389154340","doi":"10.1080/08120099.2023.2279062","title":"Paleogene carbonate ramp development in the Kohat Basin of northwestern Pakistan","year":2023,"lang":"en","type":"article","venue":"Australian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"","keywords":"Paleogene; Geology; Sedimentology; Paleontology; Sedimentary rock; Structural basin; Subsidence; Sedimentary basin analysis; Sedimentary basin","score_opus":0.057242913887663414,"score_gpt":0.2826502750704186,"score_spread":0.2254073611827552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389154340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990151,0.000047297846,0.000030699674,0.000011024176,0.000001013978,0.0000029767218,0.000040799045,0.0000016927708,0.00084935944],"genre_scores_gemma":[0.999689,0.00005773975,0.00005665759,0.0000039911656,8.0436405e-7,0.0000014272488,0.00003990361,5.0875906e-7,0.00015004458],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999517,0.000003447568,0.0000031523905,0.000012126253,0.000008884727,0.000020644102],"domain_scores_gemma":[0.99993443,0.0000074619807,0.000026645273,0.000004324754,0.000013229862,0.000013894095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000085316315,0.00011211205,0.00009686107,0.0007260432,0.0007590265,0.0003893974,0.00010814718,0.00012531325,0.0009889002],"category_scores_gemma":[0.0001671866,0.00014534665,0.00007318523,0.0006603694,0.00051740784,0.00023372275,0.00032601965,0.00011288572,0.00010711468],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023142737,0.000048081376,0.925394,0.00008740189,0.00003563284,0.0029634794,0.006071819,0.0007185833,0.028210998,0.0009174374,0.00024801787,0.03507316],"study_design_scores_gemma":[0.0000052614437,0.000034233624,0.9968946,0.0000092326945,0.0000050687004,0.00047800623,0.0011139354,0.00016248367,0.0005026367,0.000059391758,0.00073040434,0.0000049046544],"about_ca_topic_score_codex":0.038895305,"about_ca_topic_score_gemma":0.08645226,"teacher_disagreement_score":0.038895305,"about_ca_system_score_codex":0.00055045576,"about_ca_system_score_gemma":0.0005755114,"threshold_uncertainty_score":0.0773378},"labels":[],"label_agreement":null},{"id":"W4389206890","doi":"10.1029/2023jb027349","title":"On the Potential Role of Viscoelasticity in Fluid‐Induced Seismicity","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Alberta Innovates; Microseismic Industry Consortium","keywords":"Aftershock; Induced seismicity; Geology; Viscoelasticity; Geothermal gradient; Seismology; Geomechanics; Hydraulic fracturing; Rheology; Tectonics; Fluid dynamics; Geotechnical engineering; Geophysics; Mechanics; Physics","score_opus":0.04427291331815409,"score_gpt":0.3141495109711545,"score_spread":0.2698765976530004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389206890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9399028,0.00029238354,0.05638071,0.00034057593,0.000032042804,0.000026985037,0.000080491714,0.00015444927,0.0027896147],"genre_scores_gemma":[0.99889225,0.00007655988,0.00080782,0.000008595755,0.0000044912795,0.0000041340504,0.000010073156,0.000005327355,0.0001906176],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991775,0.00002342959,0.000004835264,0.000020507068,0.000012931178,0.000020598325],"domain_scores_gemma":[0.9991431,0.00048806408,0.00017968936,0.000060552436,0.000051596737,0.00007688726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025066597,0.0004480665,0.00030622643,0.00042609434,0.00025618906,0.00073212996,0.00053424074,0.0008180248,0.0011230807],"category_scores_gemma":[0.0016315224,0.00023247195,0.00034963037,0.00022270136,0.00090785493,0.000992502,0.0005701263,0.00040472197,0.00007855287],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010265851,0.00014600933,0.008337296,0.000076476535,0.00003711399,0.00035470002,0.00007581745,0.93026656,0.04817137,0.00779929,0.0001397741,0.0044929394],"study_design_scores_gemma":[0.0000044639223,0.000029561208,0.0013802408,0.0000037463553,0.0000074421237,0.00001891892,0.000010936001,0.99525166,0.0019131046,0.0013011765,0.000071234805,0.0000074684017],"about_ca_topic_score_codex":0.0027273253,"about_ca_topic_score_gemma":0.001135787,"teacher_disagreement_score":0.0027273253,"about_ca_system_score_codex":0.00031570796,"about_ca_system_score_gemma":0.00028039457,"threshold_uncertainty_score":0.00542289},"labels":[],"label_agreement":null},{"id":"W4389386130","doi":"10.1785/0220220305","title":"Improved Earthquake Clustering Using a Density-Adaptive DBSCAN Algorithm: An Example from Iran","year":2023,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"DBSCAN; Cluster analysis; Computer science; Hyperparameter; Algorithm; Data mining; Variable (mathematics); Determining the number of clusters in a data set; CURE data clustering algorithm; Pattern recognition (psychology); Correlation clustering; Mathematics; Artificial intelligence","score_opus":0.22158956926697773,"score_gpt":0.3319680955618972,"score_spread":0.11037852629491948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389386130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.731719,0.0012654084,0.24982508,0.0012760941,0.00021973968,0.00025065982,0.0011093074,0.0019283234,0.012406362],"genre_scores_gemma":[0.84879476,0.0003801038,0.147452,0.00006244685,0.000042748383,0.000047483736,0.0008554024,0.00008387178,0.0022811948],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993729,0.00015787924,0.000045514294,0.00010918062,0.00023956585,0.00007502736],"domain_scores_gemma":[0.99898,0.00022907692,0.000052548585,0.000106602,0.0005855941,0.000046187048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013372718,0.0008288919,0.00093680434,0.0028524473,0.0010248389,0.00081471517,0.0013137083,0.00086107827,0.0011248817],"category_scores_gemma":[0.0019135162,0.00019150304,0.00094619626,0.004699416,0.0005708628,0.00050245906,0.0006307912,0.0004503235,0.00029477663],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007005094,0.0003324208,0.03101082,0.00043198577,0.00024476915,0.0023866647,0.0008552523,0.64157337,0.0063339574,0.011617901,0.014974149,0.28953815],"study_design_scores_gemma":[0.00006438444,0.00006380174,0.011346892,0.000011789546,0.00005563417,0.00024279988,0.0003775666,0.9775507,0.0026002068,0.0036853198,0.0039456296,0.000055192482],"about_ca_topic_score_codex":0.07385487,"about_ca_topic_score_gemma":0.051864702,"teacher_disagreement_score":0.07385487,"about_ca_system_score_codex":0.0012050287,"about_ca_system_score_gemma":0.0011449624,"threshold_uncertainty_score":0.14684999},"labels":[],"label_agreement":null},{"id":"W4389440224","doi":"10.1029/2023tc008170","title":"Discovery of an Active Forearc Fault in an Urban Region: Holocene Rupture on the XEOLXELEK‐Elk Lake Fault, Victoria, British Columbia, Canada","year":2023,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Division of Earth Sciences; Natural Sciences and Engineering Research Council of Canada; Centre National d’Etudes Spatiales; Canada Research Chairs; University of Victoria","keywords":"Fault scarp; Geology; Seismology; Forearc; Fault (geology); Active fault; Slip (aerodynamics); Paleoseismology; Subduction; Trench; Escarpment; Holocene; Earthquake rupture; Seismic hazard; Seismic gap; Tectonics; Geomorphology; Paleontology","score_opus":0.01519845018824336,"score_gpt":0.20961673628968547,"score_spread":0.1944182861014421,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389440224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963258,0.0001923683,0.00013715205,0.000102369086,0.0000019627244,0.000019889243,0.00074242253,0.000013017376,0.0024648772],"genre_scores_gemma":[0.99792284,0.00012986685,0.00026571102,0.000028707464,0.0000012311292,0.000005110063,0.00047609612,0.0000028148759,0.0011675591],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997991,0.000009641476,0.00000937214,0.00004337454,0.00006653532,0.00007198404],"domain_scores_gemma":[0.99949086,0.000027460055,0.00006447451,0.000022958422,0.000266142,0.00012811701],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015964973,0.00021526117,0.00012966408,0.0012903811,0.0018353392,0.0010752047,0.00053923804,0.00033074783,0.0010873419],"category_scores_gemma":[0.00046551935,0.00019564111,0.0001197492,0.0019094552,0.0005173097,0.00017195594,0.00060165126,0.00032791926,0.00015886949],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053675736,0.000040385985,0.96148306,0.00004836982,0.000032803906,0.000893368,0.002285694,0.0004174705,0.0069288723,0.0001494375,0.0011673092,0.026499556],"study_design_scores_gemma":[0.000001632329,0.0000063041966,0.99674064,0.000013408189,0.000004973261,0.00008655992,0.0015374626,0.0003514214,0.00017975016,0.000012682337,0.0010616614,0.0000035692703],"about_ca_topic_score_codex":0.9697325,"about_ca_topic_score_gemma":0.99402446,"teacher_disagreement_score":0.030267477,"about_ca_system_score_codex":0.0073902537,"about_ca_system_score_gemma":0.0063410997,"threshold_uncertainty_score":0.06089139},"labels":[],"label_agreement":null},{"id":"W4389563232","doi":"10.7185/gold2023.16252","title":"Crash, bang, crustal nuclei?","year":2023,"lang":"it","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Crash; Astrobiology; Computer science; Physics; Operating system","score_opus":0.028362261484735078,"score_gpt":0.23307003401317655,"score_spread":0.20470777252844147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389563232","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021139994,0.035183284,0.0043166787,0.048463617,0.0052697877,0.000062166626,0.004087811,0.0013560096,0.8801206],"genre_scores_gemma":[0.20161222,0.018411336,0.0020341617,0.010620775,0.0013117219,0.000055985667,0.0020913254,0.00044687628,0.7634156],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9998229,0.000021761742,0.000009299924,0.000066507026,0.000050091185,0.000029544133],"domain_scores_gemma":[0.9997979,0.000023833127,0.000027448405,0.00003222799,0.000056608234,0.00006199188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034190275,0.0003516345,0.00015587665,0.00037273488,0.00088162004,0.0023999105,0.0005805411,0.0010767181,0.10875408],"category_scores_gemma":[0.000987345,0.00017632231,0.00015636178,0.00055460545,0.0013476182,0.002369077,0.001064423,0.001046008,0.025135964],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011077478,0.000020744645,0.0060920995,0.00047475257,0.00001853725,0.00071493175,0.0008692988,0.00032523667,0.0018168448,0.31733707,0.40728152,0.2649382],"study_design_scores_gemma":[0.0000058990495,0.000011460804,0.003475766,0.000106641746,0.0000043720315,0.00043347973,0.00055583887,0.00011600142,0.0002188616,0.021696623,0.9733662,0.000008788444],"about_ca_topic_score_codex":0.010469422,"about_ca_topic_score_gemma":0.0119344,"teacher_disagreement_score":0.10875408,"about_ca_system_score_codex":0.0016503847,"about_ca_system_score_gemma":0.0007071569,"threshold_uncertainty_score":0.36381865},"labels":[],"label_agreement":null},{"id":"W4389606669","doi":"10.1029/2023jb026793","title":"New Insights Into the Active Tectonics of the Northern Canadian Cordillera From an Enhanced Earthquake Catalog","year":2023,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Colorado State University; National Science Foundation","keywords":"Geology; Seismology; Induced seismicity; Foreland basin; Crust; Tectonics; Active fault; Thrust fault; Fault (geology); Structural basin; Paleontology","score_opus":0.030382970479641443,"score_gpt":0.29878563229250227,"score_spread":0.2684026618128608,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389606669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978573,0.00063088053,0.0007846966,0.00018899453,0.000006103948,0.0000323177,0.012361758,0.00008036373,0.0073418836],"genre_scores_gemma":[0.98256665,0.00043850468,0.0023685023,0.000028947576,0.000010652742,0.000015820975,0.011891057,0.000016206852,0.002663704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990416,0.000005037261,0.0000058935034,0.000026518655,0.000029981931,0.000028351584],"domain_scores_gemma":[0.9995906,0.000033274984,0.00006679161,0.000033819684,0.00020496106,0.00007047722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016379938,0.00031941364,0.00016504577,0.003891877,0.00071078446,0.0008642965,0.00027893024,0.00014466664,0.0026849054],"category_scores_gemma":[0.00080867746,0.00009979538,0.00014487357,0.0047571817,0.0002015294,0.00020481776,0.00051064277,0.00013838189,0.00024138049],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008677376,0.000035369336,0.8754064,0.00008153367,0.00007542372,0.000358625,0.0010406176,0.0039127073,0.008644248,0.00083291886,0.005363309,0.10416213],"study_design_scores_gemma":[0.0000027446645,0.000003952249,0.99269706,0.000011254088,0.000013102343,0.000035527384,0.0003264322,0.0016558105,0.00018760376,0.00005836938,0.0050027026,0.000005552311],"about_ca_topic_score_codex":0.9517142,"about_ca_topic_score_gemma":0.987456,"teacher_disagreement_score":0.048285782,"about_ca_system_score_codex":0.0034677777,"about_ca_system_score_gemma":0.003369348,"threshold_uncertainty_score":0.09714025},"labels":[],"label_agreement":null},{"id":"W4389625534","doi":"10.1785/0120230142","title":"Potential Poroelastic Triggering of the 2020 <b>M</b> 5.0 Mentone Earthquake in the Delaware Basin, Texas, by Shallow Injection Wells","year":2023,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Poromechanics; Geology; Induced seismicity; Seismology; Stress field; Structural basin; Pore water pressure; Seismic hazard; Fault (geology); Fault plane; Injection well; Geotechnical engineering; Geomorphology; Engineering; Petroleum engineering; Porosity","score_opus":0.009416363773081231,"score_gpt":0.19951952761541714,"score_spread":0.19010316384233591,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389625534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99928516,0.000009895337,0.00014606248,0.000026189955,0.0000021095489,0.0000020643358,0.00009364773,0.000018431032,0.0004164039],"genre_scores_gemma":[0.9997985,0.000006520554,0.00006256805,0.0000041645826,0.0000011310447,9.736463e-7,0.00006181617,0.0000011582719,0.000063149164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999652,0.000004046322,0.0000024992175,0.0000084907815,0.0000053759713,0.000014439766],"domain_scores_gemma":[0.9999014,0.000018659737,0.000031841602,0.00000833869,0.000016021368,0.00002375345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009437439,0.00027031184,0.00016784997,0.00024517116,0.00021845233,0.00046037146,0.00036309753,0.00036635096,0.0009493962],"category_scores_gemma":[0.0002706311,0.00017414852,0.0002476809,0.00019530879,0.00021297831,0.0002637146,0.0003001713,0.00019870738,0.00008123592],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003943019,0.00019692632,0.7252604,0.00006783482,0.00013871494,0.001250953,0.00021913582,0.22735609,0.033470094,0.00077801023,0.001149729,0.009717748],"study_design_scores_gemma":[0.000059291528,0.0001472633,0.5967206,0.000017060886,0.000057826146,0.00008555781,0.00047398155,0.39799014,0.0036603163,0.00021561571,0.0005363846,0.000036017733],"about_ca_topic_score_codex":0.04152107,"about_ca_topic_score_gemma":0.04195316,"teacher_disagreement_score":0.04152107,"about_ca_system_score_codex":0.00062409276,"about_ca_system_score_gemma":0.00042089107,"threshold_uncertainty_score":0.08255881},"labels":[],"label_agreement":null},{"id":"W4389685951","doi":"10.1785/0220230289","title":"Induced or Natural? Toward Rapid Expert Assessment, with Application to the Mw 5.2 Peace River Earthquake Sequence","year":2023,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"MacEwan University; University of Calgary; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Sequence (biology); Perspective (graphical); Interpretation (philosophy); Natural (archaeology); Event (particle physics); Natural disaster; Set (abstract data type); Seismology; Geography; Geology; Computer science; Artificial intelligence; Paleontology; Meteorology; Biology","score_opus":0.15289669698442215,"score_gpt":0.3742384252220313,"score_spread":0.22134172823760917,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389685951","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.67319274,0.0008820648,0.22766769,0.03266798,0.00043075575,0.009583229,0.0012865395,0.0008652801,0.053423733],"genre_scores_gemma":[0.72774047,0.000475589,0.26095444,0.0034432914,0.00013557446,0.0044443132,0.00038719134,0.00007397196,0.002345122],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.90725416,0.07768502,0.0034811336,0.002640126,0.007197711,0.001741892],"domain_scores_gemma":[0.7623398,0.17691687,0.011980037,0.00700991,0.039189246,0.002564077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.12839282,0.0006611194,0.0004207697,0.0042360625,0.0028425811,0.00621534,0.0018845281,0.0024829144,0.004250278],"category_scores_gemma":[0.1853145,0.0003917076,0.00053660874,0.0019813813,0.0030954974,0.0043010805,0.0068133147,0.0018764704,0.0009136003],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00085168635,0.0016361868,0.07271273,0.0035649745,0.00009144429,0.0024693813,0.40493867,0.0069050603,0.01191416,0.022402741,0.025532492,0.44698054],"study_design_scores_gemma":[0.00043114478,0.0017419002,0.087980166,0.0052156933,0.00015127461,0.0012094879,0.622905,0.053902555,0.014285119,0.063146524,0.14839254,0.0006385195],"about_ca_topic_score_codex":0.011778209,"about_ca_topic_score_gemma":0.018675245,"teacher_disagreement_score":0.98822176,"about_ca_system_score_codex":0.005117272,"about_ca_system_score_gemma":0.008521022,"threshold_uncertainty_score":0.6790142},"labels":[],"label_agreement":null},{"id":"W4389715335","doi":"10.1093/mnras/stad3844","title":"The true fraction of repeating fast radio bursts revealed through CHIME source count evolution","year":2023,"lang":"en","type":"article","venue":"Monthly Notices of the Royal Astronomical Society","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science and Technology Council","keywords":"Repeater (horology); Physics; Astrophysics; Population; Repetition (rhetorical device); Fraction (chemistry); Confidence interval; Statistics; Limit (mathematics); Demography; Mathematics; Computer science","score_opus":0.009771641931384684,"score_gpt":0.20127733365889805,"score_spread":0.19150569172751336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389715335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968335,0.00007388553,0.0012388849,0.00004680082,0.0000023358357,0.0000042750958,0.0008106771,0.000053341737,0.00093629],"genre_scores_gemma":[0.9988438,0.000022097034,0.00035814644,0.000008829659,0.0000016028653,0.0000015425148,0.0005879494,0.000009437809,0.00016656786],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997625,0.000030429617,0.000008147143,0.00008438705,0.000068035806,0.00004650985],"domain_scores_gemma":[0.99814534,0.0005944226,0.00047983462,0.00027049618,0.00033118253,0.00017866843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066521525,0.00014969317,0.00015957121,0.00080016215,0.00022605255,0.00061227236,0.000300764,0.00023184573,0.0014892983],"category_scores_gemma":[0.0043501533,0.00018508134,0.00011846739,0.00037440725,0.0003683892,0.0004403489,0.00031648515,0.00025083212,0.00040698258],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003940889,0.0000054315615,0.98697215,0.000007934154,0.00003840625,0.00005148513,0.00015514696,0.00100845,0.0064189876,0.000200728,0.00026105894,0.004840702],"study_design_scores_gemma":[7.2068235e-7,0.000008631087,0.99576426,0.0000024999888,0.000007034418,0.000086534434,0.00006483219,0.0029195978,0.00078729814,0.000108998225,0.00024353484,0.0000059318954],"about_ca_topic_score_codex":0.02005067,"about_ca_topic_score_gemma":0.021529004,"teacher_disagreement_score":0.02005067,"about_ca_system_score_codex":0.00045031772,"about_ca_system_score_gemma":0.00014496464,"threshold_uncertainty_score":0.039867938},"labels":[],"label_agreement":null},{"id":"W4390275340","doi":"10.1785/0120230182","title":"The 2022 Aotearoa New Zealand National Seismic Hazard Model: Process, Overview, and Results","year":2023,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Western University","funders":"","keywords":"Aotearoa; Hazard; Process (computing); Corporate governance; Seismology; Computer science; Geography; Geology; Engineering; Political science; Business; Finance; Law","score_opus":0.026104323509915563,"score_gpt":0.24663024091661534,"score_spread":0.22052591740669977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390275340","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12071404,0.0064120027,0.12931305,0.008515937,0.00086400425,0.0066527715,0.5974163,0.008192642,0.12191932],"genre_scores_gemma":[0.31973064,0.006386329,0.113198146,0.00074432266,0.00018992755,0.004276679,0.5291884,0.0034033859,0.022882225],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9983411,0.00033648775,0.00010136448,0.00018781853,0.00093602226,0.00009719554],"domain_scores_gemma":[0.9941865,0.0007466224,0.0003284639,0.00049142365,0.003943659,0.0003033776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0066603827,0.001211621,0.0007506311,0.0022336799,0.0004195651,0.002162965,0.002260829,0.00070409826,0.008092494],"category_scores_gemma":[0.015203635,0.0005702826,0.0010073032,0.002531074,0.00038514478,0.0012237518,0.0012926414,0.00094840577,0.0033265343],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010586021,0.00048148644,0.0582272,0.0025635331,0.00094870233,0.00031361502,0.00034066295,0.4074371,0.004603751,0.011313141,0.31359974,0.19911247],"study_design_scores_gemma":[0.001006136,0.00032766038,0.083980784,0.0013444239,0.00087956653,0.00016985735,0.00042136354,0.4581601,0.0077856747,0.008882921,0.43664503,0.00039644717],"about_ca_topic_score_codex":0.5026597,"about_ca_topic_score_gemma":0.287096,"teacher_disagreement_score":0.5026597,"about_ca_system_score_codex":0.0054788333,"about_ca_system_score_gemma":0.009902602,"threshold_uncertainty_score":0.99946773},"labels":[],"label_agreement":null},{"id":"W4390486996","doi":"10.1029/2023jb027276","title":"Control of Seismicity Migration in Earthquake Swarms by Injected Fluid Volume and Aseismic Crack Propagation","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Agence Nationale de la Recherche","keywords":"Induced seismicity; Geology; Seismic moment; Seismology; Slip (aerodynamics); Fluid dynamics; Fluid pressure; Geothermal gradient; Front (military); Fault (geology); Mechanics; Geophysics; Physics","score_opus":0.01935156711211921,"score_gpt":0.2878030788456735,"score_spread":0.2684515117335543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390486996","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99393773,0.00003368319,0.0055637057,0.000018092334,0.0000020064078,0.0000032337973,0.000022598324,0.000028309933,0.00039064372],"genre_scores_gemma":[0.99976045,0.000007467089,0.00017382385,8.0431033e-7,5.286963e-7,0.00000104384,0.0000052289406,0.000001735133,0.000048925296],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995923,0.000010359658,0.0000030643657,0.000010004145,0.0000069810685,0.0000102674085],"domain_scores_gemma":[0.99965274,0.00013127559,0.0001298883,0.000015525186,0.000028816692,0.000041682608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012278037,0.00018670171,0.00015135898,0.00037729408,0.000109110726,0.0003713502,0.00021357964,0.00024120428,0.00042425527],"category_scores_gemma":[0.0007602669,0.00014881734,0.00020095835,0.000114167015,0.00041109207,0.00019377441,0.00021446218,0.0001604875,0.000049180235],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031448656,0.00025977675,0.07404132,0.00006762604,0.000102272206,0.00058910693,0.00021183645,0.48080397,0.42644423,0.0041403403,0.00020796385,0.012817106],"study_design_scores_gemma":[0.000016425467,0.00008337405,0.028839247,0.0000035373548,0.000012771042,0.0000519531,0.000038526243,0.9596507,0.010730232,0.0004681718,0.000093184135,0.000011937959],"about_ca_topic_score_codex":0.0033591476,"about_ca_topic_score_gemma":0.0019351052,"teacher_disagreement_score":0.0033591476,"about_ca_system_score_codex":0.00036615122,"about_ca_system_score_gemma":0.00018421213,"threshold_uncertainty_score":0.0066791773},"labels":[],"label_agreement":null},{"id":"W4390584285","doi":"10.5194/egusphere-2023-2548-cc1","title":"Comment on egusphere-2023-2548","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Rift; Terminology; Natural resource; Earth science; Natural (archaeology); East African Rift; Geology; Magmatism; Hazard; Tectonics; Paleontology; Political science; Ecology","score_opus":0.04034720616934387,"score_gpt":0.2749551315722734,"score_spread":0.23460792540292955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390584285","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00062338065,0.0013729227,0.00055454054,0.5241968,0.24321386,0.00043086626,0.004752544,0.0017790659,0.223076],"genre_scores_gemma":[0.0025458538,0.00068045774,0.00026849768,0.6028695,0.031130493,0.00028244872,0.0011597776,0.00050854107,0.3605545],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981553,0.00016637005,0.00018023852,0.0002097218,0.00091818353,0.00037004828],"domain_scores_gemma":[0.99569124,0.0014484312,0.0002034226,0.00027973784,0.001792337,0.0005848988],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025289683,0.0009017509,0.0009628609,0.0012306196,0.003949918,0.0038286806,0.0027331393,0.029224861,0.29978916],"category_scores_gemma":[0.017006604,0.0005436212,0.0014680828,0.0014847458,0.0019338166,0.003256663,0.002756727,0.013606705,0.2179069],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024992289,0.000009112296,0.00006174094,0.00003492381,0.0000015348635,0.00009841759,0.000017417487,0.0000073070355,0.00004955756,0.00084186124,0.9963643,0.0024886974],"study_design_scores_gemma":[0.000018775454,0.000010060516,0.00033550346,0.00008271362,0.0000019650058,0.000029219153,0.00005588821,0.000022412354,0.00006213614,0.00070175546,0.9986707,0.000008938652],"about_ca_topic_score_codex":0.028882721,"about_ca_topic_score_gemma":0.032990176,"teacher_disagreement_score":0.29978916,"about_ca_system_score_codex":0.0036399572,"about_ca_system_score_gemma":0.003116454,"threshold_uncertainty_score":0.99876577},"labels":[],"label_agreement":null},{"id":"W4390647113","doi":"10.1093/gji/ggae003","title":"Bootstrapping for parameter uncertainty in the space–time epidemic-type aftershock sequence model","year":2024,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bootstrapping (finance); Resampling; Confidence interval; Sequence (biology); Statistics; Aftershock; Parametric statistics; Quantile; Econometrics; Inference; Computer science; Geology; Seismology; Mathematics; Artificial intelligence","score_opus":0.05412327669698028,"score_gpt":0.2974388723066609,"score_spread":0.2433155956096806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390647113","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10986148,0.0003139815,0.88634264,0.0004690433,0.000044821325,0.000030810184,0.00019176153,0.00040692312,0.0023384762],"genre_scores_gemma":[0.94268596,0.00016983092,0.055905953,0.00008249034,0.00004003584,0.00008257495,0.00030253842,0.000133772,0.0005968632],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99594635,0.0030968206,0.00012927043,0.00025200477,0.00041880264,0.00015683859],"domain_scores_gemma":[0.95286393,0.041329943,0.0015598703,0.002540397,0.0014163784,0.0002896114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.012600055,0.0005146857,0.0010007737,0.0012585897,0.00047809468,0.0010728611,0.0016474214,0.00092876534,0.0015326426],"category_scores_gemma":[0.069609776,0.00038780613,0.0009827637,0.0009476926,0.0014473068,0.0012279687,0.0014730007,0.0015881924,0.00023115774],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000088994355,0.000024440771,0.0042106146,0.0000583819,0.00010167779,0.00028253396,0.00014432706,0.9074219,0.00056682655,0.0722639,0.00088750094,0.013948961],"study_design_scores_gemma":[0.0000055937453,0.000010263403,0.00045846446,0.000014531947,0.0000063641232,0.000025098803,0.000016983493,0.9687094,0.00015704475,0.030306643,0.000281422,0.000008063832],"about_ca_topic_score_codex":0.00730563,"about_ca_topic_score_gemma":0.003490045,"teacher_disagreement_score":0.012600055,"about_ca_system_score_codex":0.00070562883,"about_ca_system_score_gemma":0.0006388388,"threshold_uncertainty_score":0.066636205},"labels":[],"label_agreement":null},{"id":"W4390831011","doi":"10.1007/s10706-023-02721-0","title":"Understanding Seismic Hazards Associated with Development Mining: The Role of Local Geology and Structures","year":2024,"lang":"en","type":"article","venue":"Geotechnical and Geological Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Université Laval","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Induced seismicity; Hydrogeology; Geology; Seismology; Lithology; Mining engineering; Structural geology; Seismic risk; Earthquake scenario; Seismic hazard; Rock blasting; Geotechnical engineering; Petrology","score_opus":0.020278122063861384,"score_gpt":0.18543089565147894,"score_spread":0.16515277358761754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390831011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97848344,0.00094818725,0.011802311,0.000998179,0.000010558713,0.00001760488,0.00026014916,0.000028551896,0.007451018],"genre_scores_gemma":[0.99728394,0.0006417714,0.0015193627,0.000025470137,0.00000967514,0.000003130603,0.00007099898,0.000005005424,0.0004407345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991333,0.00003308003,0.000004202286,0.000019718807,0.000016720554,0.000013028949],"domain_scores_gemma":[0.99941623,0.0002471185,0.0001839456,0.000032552347,0.00006817674,0.00005203895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031526372,0.00025151248,0.0002368138,0.0007184764,0.00024866595,0.0012636604,0.00041772574,0.00032243066,0.0016573621],"category_scores_gemma":[0.0018757934,0.0001646897,0.00012147898,0.0008065543,0.0006240541,0.0016067283,0.0007477443,0.0003887452,0.00017867173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009205737,0.00023986757,0.79731584,0.00025858564,0.0001026186,0.0003202339,0.0016583916,0.06597922,0.005679766,0.01337157,0.0011950015,0.11378679],"study_design_scores_gemma":[0.000010461911,0.00012573651,0.82228845,0.00009083865,0.00007243538,0.00028963588,0.007629881,0.134731,0.0010569411,0.028950054,0.004723412,0.000031144296],"about_ca_topic_score_codex":0.01397581,"about_ca_topic_score_gemma":0.0342016,"teacher_disagreement_score":0.01397581,"about_ca_system_score_codex":0.00051592273,"about_ca_system_score_gemma":0.0008694524,"threshold_uncertainty_score":0.027788877},"labels":[],"label_agreement":null},{"id":"W4391024512","doi":"10.1785/0120230310","title":"Introduction to the <i>BSSA</i> Special Issue and <i>SRL</i> Focus Section on Seismic Hazard Models","year":2024,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Section (typography); Focus (optics); Hazard; Geology; Seismology; Computer science; Physics; Biology; Ecology; Optics","score_opus":0.011115390609362364,"score_gpt":0.20122085145427382,"score_spread":0.19010546084491145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391024512","genre_codex":"other","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00084188784,0.051026326,0.03702126,0.07298883,0.1968729,0.001250254,0.026864937,0.00943019,0.60370344],"genre_scores_gemma":[0.004987092,0.05596051,0.013466009,0.0125827,0.12089542,0.0008813888,0.02576768,0.0061691795,0.7592901],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982638,0.00015509492,0.00015238099,0.00020275242,0.0011050762,0.00012107292],"domain_scores_gemma":[0.99155056,0.0016235082,0.00057727814,0.0007372306,0.0042699096,0.0012414247],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0029131738,0.0018552894,0.0015081435,0.0059367567,0.0013200791,0.0064330776,0.0026878868,0.004338032,0.38772854],"category_scores_gemma":[0.010437572,0.0011014421,0.0021233452,0.005261748,0.0010722541,0.005530996,0.0031480764,0.0043558404,0.30053782],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000077759705,0.000011620266,0.00006970664,0.00013603004,0.0000030262554,0.000016780517,0.000008388654,0.00014777682,0.00013933492,0.0013891818,0.97533333,0.022737043],"study_design_scores_gemma":[0.000002974926,0.000014355822,0.00022909918,0.00015312716,0.0000025315037,0.00004195728,0.000013331472,0.0001232168,0.0000496074,0.001467654,0.9978935,0.000008632715],"about_ca_topic_score_codex":0.006456494,"about_ca_topic_score_gemma":0.009081844,"teacher_disagreement_score":0.38772854,"about_ca_system_score_codex":0.0027578203,"about_ca_system_score_gemma":0.004069077,"threshold_uncertainty_score":0.87333095},"labels":[],"label_agreement":null},{"id":"W4391025424","doi":"10.1785/0220230422","title":"Introduction to the <i>BSSA</i> Special Issue and <i>SRL</i> Focus Section on Seismic Hazard Models","year":2024,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Library science; Section (typography); History; Engineering; Art history; Computer science","score_opus":0.04595658057384211,"score_gpt":0.28649287515340066,"score_spread":0.24053629457955855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391025424","genre_codex":"other","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00084188784,0.051026326,0.03702126,0.07298883,0.1968729,0.001250254,0.026864937,0.00943019,0.60370344],"genre_scores_gemma":[0.004987092,0.05596051,0.013466009,0.0125827,0.12089542,0.0008813888,0.02576768,0.0061691795,0.7592901],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9982638,0.00015509492,0.00015238099,0.00020275242,0.0011050762,0.00012107292],"domain_scores_gemma":[0.99155056,0.0016235082,0.00057727814,0.0007372306,0.0042699096,0.0012414247],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0029131738,0.0018552894,0.0015081435,0.0059367567,0.0013200791,0.0064330776,0.0026878868,0.004338032,0.38772854],"category_scores_gemma":[0.010437572,0.0011014421,0.0021233452,0.005261748,0.0010722541,0.005530996,0.0031480764,0.0043558404,0.30053782],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000077759705,0.000011620266,0.00006970664,0.00013603004,0.0000030262554,0.000016780517,0.000008388654,0.00014777682,0.00013933492,0.0013891818,0.97533333,0.022737043],"study_design_scores_gemma":[0.000002974926,0.000014355822,0.00022909918,0.00015312716,0.0000025315037,0.00004195728,0.000013331472,0.0001232168,0.0000496074,0.001467654,0.9978935,0.000008632715],"about_ca_topic_score_codex":0.006456494,"about_ca_topic_score_gemma":0.009081844,"teacher_disagreement_score":0.38772854,"about_ca_system_score_codex":0.0027578203,"about_ca_system_score_gemma":0.004069077,"threshold_uncertainty_score":0.87333095},"labels":[],"label_agreement":null},{"id":"W4391032602","doi":"10.1111/bre.12841","title":"Rift segmentation caused by reactivation of multiple basement structure systems: Evidence from the Hailar‐Tamtsag Rift, northeast Asia","year":2024,"lang":"en","type":"article","venue":"Basin Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Minnow Environmental (Canada)","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Rift; Geology; Basement; Seismology; Segmentation; Fault (geology); Half-graben; Paleontology; Tectonics; Geography; Artificial intelligence","score_opus":0.07026883296117574,"score_gpt":0.31666076146664957,"score_spread":0.2463919285054738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391032602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996124,0.000032284453,0.000069066344,0.0000043707464,4.3407152e-7,0.0000021464496,0.000049569502,0.000003128837,0.00022656957],"genre_scores_gemma":[0.9997521,0.000024190074,0.00008182094,0.0000034170273,0.0000012830839,0.0000018450892,0.00008861366,0.0000010364128,0.00004570232],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979633,0.000023123803,0.000022720882,0.00006591482,0.00004940154,0.000042533535],"domain_scores_gemma":[0.9992818,0.00011804344,0.00030947517,0.00006538055,0.00014092129,0.00008434752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031532446,0.00030980312,0.0003034128,0.0014546418,0.0004892724,0.0005048648,0.00037266203,0.0003444479,0.00049697637],"category_scores_gemma":[0.0007244342,0.00030936155,0.0003000826,0.0015011466,0.0010779888,0.0003523447,0.00063256145,0.0002217948,0.000116604024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012231864,0.00003032884,0.97571915,0.000045358793,0.00006738251,0.0010332231,0.0018979785,0.00046716788,0.01612121,0.000071332855,0.000040248713,0.0043841745],"study_design_scores_gemma":[0.0000033986125,0.00003133815,0.99845517,0.0000041240364,0.000018560919,0.0001740463,0.0005524103,0.0002769017,0.0004033844,0.000018873718,0.00005849279,0.0000032792539],"about_ca_topic_score_codex":0.018577527,"about_ca_topic_score_gemma":0.03373151,"teacher_disagreement_score":0.018577527,"about_ca_system_score_codex":0.00049917353,"about_ca_system_score_gemma":0.00036712675,"threshold_uncertainty_score":0.036938787},"labels":[],"label_agreement":null},{"id":"W4391126661","doi":"10.5194/egusphere-2023-2548-rc2","title":"Comment on egusphere-2023-2548","year":2024,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Environmental science","score_opus":0.04034720616934387,"score_gpt":0.2749551315722734,"score_spread":0.23460792540292955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391126661","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00062338065,0.0013729227,0.00055454054,0.5241968,0.24321386,0.00043086626,0.004752544,0.0017790659,0.223076],"genre_scores_gemma":[0.0025458538,0.00068045774,0.00026849768,0.6028695,0.031130493,0.00028244872,0.0011597776,0.00050854107,0.3605545],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9981553,0.00016637005,0.00018023852,0.0002097218,0.00091818353,0.00037004828],"domain_scores_gemma":[0.99569124,0.0014484312,0.0002034226,0.00027973784,0.001792337,0.0005848988],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0025289683,0.0009017509,0.0009628609,0.0012306196,0.003949918,0.0038286806,0.0027331393,0.029224861,0.29978916],"category_scores_gemma":[0.017006604,0.0005436212,0.0014680828,0.0014847458,0.0019338166,0.003256663,0.002756727,0.013606705,0.2179069],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024992289,0.000009112296,0.00006174094,0.00003492381,0.0000015348635,0.00009841759,0.000017417487,0.0000073070355,0.00004955756,0.00084186124,0.9963643,0.0024886974],"study_design_scores_gemma":[0.000018775454,0.000010060516,0.00033550346,0.00008271362,0.0000019650058,0.000029219153,0.00005588821,0.000022412354,0.00006213614,0.00070175546,0.9986707,0.000008938652],"about_ca_topic_score_codex":0.028882721,"about_ca_topic_score_gemma":0.032990176,"teacher_disagreement_score":0.29978916,"about_ca_system_score_codex":0.0036399572,"about_ca_system_score_gemma":0.003116454,"threshold_uncertainty_score":0.99876577},"labels":[],"label_agreement":null},{"id":"W4391311954","doi":"10.54097/1ygn2714","title":"Analysis of Shallow Water Equation Based on Tsunami Simulations: Evidence from the Pacific Ocean","year":2023,"lang":"en","type":"article","venue":"Highlights in Science Engineering and Technology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Kwantlen Polytechnic University","funders":"","keywords":"Oceanography; Geology; Waves and shallow water; Pacific ocean; Environmental science","score_opus":0.021294836903897954,"score_gpt":0.2248081627739321,"score_spread":0.20351332587003412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391311954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912224,0.00022904709,0.0034961635,0.00030212654,0.00001848936,0.000014029912,0.0004052893,0.00011266929,0.0041997894],"genre_scores_gemma":[0.99804604,0.00019715811,0.0010699818,0.000019774701,0.0000064237884,0.00000830647,0.00026657435,0.000015830114,0.00036990352],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991333,0.00002306044,0.0000071756026,0.0000124135795,0.000024073328,0.000019962248],"domain_scores_gemma":[0.9991242,0.0005055175,0.000078749654,0.00006834519,0.00015288178,0.00007024703],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003085351,0.0003898803,0.00036371525,0.0004000714,0.00033116117,0.0005194645,0.00055065413,0.00045904503,0.0010750244],"category_scores_gemma":[0.001991647,0.00019578032,0.0004289984,0.0004316815,0.00041826148,0.00063168607,0.00050258456,0.00071451574,0.000103743354],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001162207,0.00013878604,0.052274946,0.00010215996,0.000096366326,0.00026582868,0.00018165719,0.9289955,0.0015076372,0.0038434188,0.001183077,0.011294378],"study_design_scores_gemma":[0.000010909359,0.000025733372,0.0066536036,0.000008779452,0.000016593844,0.000008408612,0.000088641085,0.99191004,0.00030617142,0.00066742353,0.00029683192,0.000006790391],"about_ca_topic_score_codex":0.08290559,"about_ca_topic_score_gemma":0.032310173,"teacher_disagreement_score":0.08290559,"about_ca_system_score_codex":0.00048538178,"about_ca_system_score_gemma":0.0007633239,"threshold_uncertainty_score":0.16484606},"labels":[],"label_agreement":null},{"id":"W4391446805","doi":"10.1029/2023gc011152","title":"Sedimentary Records in the Lesser Antilles Fore‐Arc Basins Provide Evidence of Large Late Quaternary Megathrust Earthquakes","year":2024,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"Agence Nationale de la Recherche","keywords":"Geology; Seismology; Subduction; Radiocarbon dating; Quaternary; Magnitude (astronomy); Paleoseismology; Period (music); Sedimentary rock; Paleontology; Fault (geology); Tectonics","score_opus":0.019503368573700414,"score_gpt":0.24946524835803882,"score_spread":0.2299618797843384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391446805","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992118,0.000064706684,0.000028910403,0.000014053397,6.6496295e-7,0.0000012936148,0.00013966425,0.0000038108649,0.0005351241],"genre_scores_gemma":[0.99954695,0.0000574378,0.000061809405,0.0000056324134,0.0000037380958,0.0000017515961,0.0001818657,0.0000010477218,0.00013972602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994504,0.000009786287,0.000005331236,0.000011245292,0.000013787196,0.000014712577],"domain_scores_gemma":[0.9996112,0.000044444358,0.00021481611,0.000023659435,0.000062024825,0.000043836673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013028488,0.00018814584,0.0001237771,0.0010872377,0.00035334512,0.00035914042,0.00011240932,0.00015679355,0.0008895603],"category_scores_gemma":[0.0003615861,0.000120955134,0.00009389003,0.0007625881,0.0003496332,0.0001792608,0.00027802886,0.00011323017,0.00016998728],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007516859,0.00001018734,0.9818009,0.000024464089,0.00002028804,0.0001485757,0.0005953704,0.00014208865,0.012566726,0.00006396612,0.0000990636,0.004453239],"study_design_scores_gemma":[5.373108e-7,0.000006288774,0.9996809,0.000001205285,0.0000012477942,0.000024384573,0.000037695056,0.000026088675,0.00008087589,0.0000034084946,0.00013687137,4.2660764e-7],"about_ca_topic_score_codex":0.012383528,"about_ca_topic_score_gemma":0.037712067,"teacher_disagreement_score":0.012383528,"about_ca_system_score_codex":0.0002873654,"about_ca_system_score_gemma":0.00014218705,"threshold_uncertainty_score":0.024622858},"labels":[],"label_agreement":null},{"id":"W4391677433","doi":"10.21203/rs.3.rs-3909443/v1","title":"Tectonic tremor: the chatter of mafic underplating beneath southern Vancouver Island?","year":2024,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University; University of British Columbia","funders":"","keywords":"Underplating; Mafic; Geology; Tectonics; Seismology; Paleontology; Subduction","score_opus":0.05571516809506058,"score_gpt":0.3207830065932787,"score_spread":0.26506783849821813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391677433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9701314,0.00054186827,0.00014020901,0.0015743654,0.000053743584,0.000014649556,0.0007104881,0.000030358377,0.026802883],"genre_scores_gemma":[0.9902434,0.000263433,0.00013794657,0.00010743803,0.000018983425,0.0000045917504,0.00030147118,0.000012739704,0.008910009],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999212,0.0000047750627,0.0000033240356,0.000016979722,0.000016737407,0.00003703563],"domain_scores_gemma":[0.99974436,0.000022019305,0.000043574324,0.000014535229,0.000098467826,0.00007703],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010679404,0.00017654084,0.0001458096,0.00077424874,0.0020594413,0.0023617665,0.0004631191,0.0010103899,0.0072253104],"category_scores_gemma":[0.0008372882,0.0001549345,0.00006622022,0.0018000836,0.00074349914,0.0005713734,0.0008823705,0.0004937855,0.00063475437],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004946161,0.00006389333,0.79467046,0.00031454797,0.00007312173,0.005795167,0.04079381,0.0011588255,0.015810013,0.005049556,0.023997322,0.111778624],"study_design_scores_gemma":[0.0000066475764,0.000015142826,0.94536334,0.00007963892,0.000012722118,0.0002392338,0.023968037,0.000476071,0.00021609715,0.0002850035,0.029327225,0.00001074825],"about_ca_topic_score_codex":0.7883052,"about_ca_topic_score_gemma":0.93264526,"teacher_disagreement_score":0.21169478,"about_ca_system_score_codex":0.0023334525,"about_ca_system_score_gemma":0.002528665,"threshold_uncertainty_score":0.42588294},"labels":[],"label_agreement":null},{"id":"W4391818382","doi":"10.31219/osf.io/xhbj6","title":"On the viability of detrital Rb-Sr geochronology","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Geochronology; Geology; Geochemistry","score_opus":0.02270630838361279,"score_gpt":0.23018143431751126,"score_spread":0.20747512593389847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391818382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.77229506,0.008790239,0.16363987,0.002166871,0.00036377515,0.00012602589,0.0027056998,0.0011232169,0.04878938],"genre_scores_gemma":[0.96692824,0.0013800666,0.02539083,0.000119335025,0.00008062522,0.00003775215,0.0004994068,0.00034230202,0.0052215336],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9961415,0.0014394425,0.00029460614,0.00072272494,0.0012196199,0.00018203827],"domain_scores_gemma":[0.99029607,0.00425188,0.00074990693,0.0021180932,0.0024240997,0.00016002065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0074194195,0.00074428925,0.00066437287,0.0014449732,0.00076721126,0.0025485442,0.0015548341,0.00045599,0.0012152687],"category_scores_gemma":[0.0131274415,0.00023517305,0.00041411238,0.0012925294,0.0015492942,0.0011381286,0.0014185417,0.0008145176,0.0009177217],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001898643,0.00009656792,0.28918877,0.0012932947,0.00046692364,0.0023019025,0.0044297352,0.014226,0.23955044,0.0426436,0.0019268548,0.4019773],"study_design_scores_gemma":[0.0000667382,0.00078740413,0.635724,0.00067060103,0.00050962414,0.0024376959,0.0028358977,0.05383699,0.19709425,0.012284813,0.093537025,0.00021490638],"about_ca_topic_score_codex":0.017429546,"about_ca_topic_score_gemma":0.020290043,"teacher_disagreement_score":0.017429546,"about_ca_system_score_codex":0.0010928916,"about_ca_system_score_gemma":0.001016108,"threshold_uncertainty_score":0.039238095},"labels":[],"label_agreement":null},{"id":"W4391906383","doi":"10.1016/j.epsl.2024.118619","title":"Geodetic signature of a weak Lithosphere-Asthenosphere Boundary in postseismic deformation of large subduction earthquakes","year":2024,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Commission Géologique du Canada","keywords":"Geology; Lithosphere; Subduction; Asthenosphere; Seismology; Plate tectonics; Deformation (meteorology); Geophysics; Geodetic datum; Viscosity; Geodesy; Tectonics","score_opus":0.005217428836415388,"score_gpt":0.19402501987904308,"score_spread":0.1888075910426277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391906383","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990609,0.0000318906,0.00010241553,0.000013076971,0.000002884387,0.0000019963109,0.0001315113,0.000007341976,0.00064796733],"genre_scores_gemma":[0.9996251,0.000013958397,0.000067977046,0.0000055997107,0.0000036354081,0.0000011731632,0.00013712294,0.0000025440334,0.0001428251],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999684,0.0000037493423,0.0000034604261,0.000007169712,0.0000061280302,0.000011074377],"domain_scores_gemma":[0.99973124,0.000042339107,0.00008117407,0.0000148117115,0.000058411308,0.00007198533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010535691,0.000110037516,0.00016133583,0.00085880654,0.00020456425,0.00036353982,0.00011468694,0.00024216471,0.0012394341],"category_scores_gemma":[0.0004658705,0.0000990485,0.000060679115,0.0005824485,0.00023060279,0.00014526698,0.00028524775,0.00015814521,0.00021780969],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012092632,0.00010281049,0.80745405,0.000054238946,0.000037728998,0.00056545914,0.00049596175,0.0012301938,0.17092586,0.00038834818,0.00046296488,0.017073011],"study_design_scores_gemma":[0.0000038139965,0.00002677578,0.99910635,0.0000013950747,0.0000029539028,0.000051998606,0.000059202473,0.00021190406,0.00043721663,0.000015382873,0.0000815901,0.0000013831809],"about_ca_topic_score_codex":0.004246254,"about_ca_topic_score_gemma":0.00866657,"teacher_disagreement_score":0.004246254,"about_ca_system_score_codex":0.00014300151,"about_ca_system_score_gemma":0.00017431598,"threshold_uncertainty_score":0.008443117},"labels":[],"label_agreement":null},{"id":"W4392122731","doi":"10.1007/s11069-024-06467-7","title":"Environmental effects following a seismic sequence: the 2019 Cotabato—Davao del Sur (Philippines) earthquakes","year":2024,"lang":"en","type":"article","venue":"Natural Hazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Università degli Studi dell'Insubria","keywords":"Landslide; Natural hazard; Seismology; Magnitude (astronomy); Sequence (biology); Geology; Scale (ratio); Mercalli intensity scale; Richter magnitude scale; Geography; Peak ground acceleration; Cartography; Mathematics; Ground motion; Geometry","score_opus":0.008142532965907995,"score_gpt":0.21884867171705882,"score_spread":0.21070613875115082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392122731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984232,0.00003211824,0.00018697987,0.00004612742,0.0000038429935,0.000009305558,0.0004576431,0.000015667209,0.00082522],"genre_scores_gemma":[0.99933416,0.000026060434,0.00016546209,0.0000075177186,0.0000034839056,0.0000049832165,0.00032603127,0.0000023046675,0.00012997602],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998448,0.000039759238,0.000012062158,0.000030392908,0.000038655417,0.000034420827],"domain_scores_gemma":[0.99925894,0.00009647564,0.00027293983,0.000053834865,0.00019824496,0.00011957554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002788058,0.00032112474,0.00012611413,0.0008528807,0.0002898241,0.00041986298,0.00018389554,0.00020906102,0.0013472852],"category_scores_gemma":[0.0011092203,0.00009127632,0.000118725795,0.0010619664,0.00040454336,0.00027618793,0.000642353,0.000310617,0.00011414024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017658538,0.0001163999,0.96405935,0.0000659296,0.000091467955,0.0013393919,0.0009754767,0.011261604,0.004025824,0.00022561569,0.0007589134,0.016903516],"study_design_scores_gemma":[0.0000022871025,0.000047175654,0.995698,0.0000073669553,0.00001239281,0.000057431578,0.00058725587,0.0026424788,0.00033132907,0.000038611903,0.00056881673,0.00000684601],"about_ca_topic_score_codex":0.038260717,"about_ca_topic_score_gemma":0.064491674,"teacher_disagreement_score":0.038260717,"about_ca_system_score_codex":0.0007602025,"about_ca_system_score_gemma":0.00038902325,"threshold_uncertainty_score":0.07607603},"labels":[],"label_agreement":null},{"id":"W4392231242","doi":"10.1080/19475705.2024.2311890","title":"Reappraisal of the 2012 magnitude (M <sub>W</sub> ) 6.7 Negros Oriental (Philippines) earthquake intensity and ShakeMap generation by using ESI-2007 environmental effects","year":2024,"lang":"en","type":"article","venue":"Geomatics Natural Hazards and Risk","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Toronto","funders":"Ministry of the Interior and Safety","keywords":"Magnitude (astronomy); Intensity (physics); Environmental science; Geography; Seismology; Geology; Physics","score_opus":0.005725709316565065,"score_gpt":0.19794330698986268,"score_spread":0.1922175976732976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392231242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99393374,0.00010543442,0.0011989046,0.00007668944,0.000012929574,0.000042156495,0.0013270974,0.000051845065,0.0032512422],"genre_scores_gemma":[0.99416566,0.00014566409,0.002976558,0.000027179956,0.000016970187,0.00003234281,0.0019821287,0.000016189315,0.00063722226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997955,0.00005249042,0.000020054189,0.000038911705,0.00006744539,0.000025686173],"domain_scores_gemma":[0.9991357,0.000059691723,0.00021099437,0.00006532499,0.00046143238,0.000066945475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052524154,0.00044621795,0.00012763291,0.0011418262,0.00013228205,0.0004315807,0.00021425882,0.00015533893,0.0007059234],"category_scores_gemma":[0.0014051809,0.0001392226,0.00020084783,0.0011782163,0.00011419194,0.0002718504,0.00046717032,0.00024489083,0.00020232129],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000080103935,0.000084642124,0.9397434,0.00009407331,0.000081416,0.00033359963,0.0006474687,0.0030304387,0.0072481427,0.00012466636,0.0012401298,0.047291875],"study_design_scores_gemma":[0.0000030920928,0.0000410895,0.99471766,0.00000993528,0.000026184367,0.000046413545,0.0004500355,0.0020754265,0.0008982767,0.000012054467,0.0017143746,0.0000055166424],"about_ca_topic_score_codex":0.012544767,"about_ca_topic_score_gemma":0.039577484,"teacher_disagreement_score":0.012544767,"about_ca_system_score_codex":0.00035869319,"about_ca_system_score_gemma":0.00034578043,"threshold_uncertainty_score":0.02494353},"labels":[],"label_agreement":null},{"id":"W4392248874","doi":"10.2139/ssrn.4741401","title":"Shatter Cone Indicating a Strong Paleoearthquake at Bowmanville, Ontario Province, Canada","year":2024,"lang":"en","type":"preprint","venue":"SSRN Electronic Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cone (formal languages); Geography; Mathematics","score_opus":0.009567250045415844,"score_gpt":0.19658125000082227,"score_spread":0.18701399995540643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392248874","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90825856,0.0006811789,0.00047578968,0.0016592025,0.00010268347,0.00015202098,0.013272624,0.00018203988,0.07521592],"genre_scores_gemma":[0.96045566,0.00041467586,0.00079772423,0.00018227128,0.000019967114,0.00002855785,0.0025977062,0.0000308168,0.03547272],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997731,0.0000060506222,0.000007564129,0.000039082282,0.00008901106,0.00008530756],"domain_scores_gemma":[0.9992193,0.00003789246,0.00007027776,0.000021428665,0.0004160615,0.00023507362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012421435,0.00027183926,0.00025294215,0.0016669743,0.00424171,0.0012339125,0.00070186803,0.00077804667,0.014173012],"category_scores_gemma":[0.0007620931,0.00019773253,0.00016054751,0.0027846657,0.00091348274,0.00031236972,0.0007767618,0.000552401,0.0010047298],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006021425,0.00012487567,0.8084016,0.00043007208,0.00013412046,0.005095486,0.015573507,0.0033811228,0.017641349,0.004727544,0.08468408,0.059204124],"study_design_scores_gemma":[0.000014898094,0.000014838653,0.9762071,0.00005212388,0.000014338867,0.00012370388,0.005122381,0.00076538307,0.0003268694,0.000112824804,0.017227126,0.000018366994],"about_ca_topic_score_codex":0.99465203,"about_ca_topic_score_gemma":0.99912673,"teacher_disagreement_score":0.014173012,"about_ca_system_score_codex":0.014075454,"about_ca_system_score_gemma":0.0246676,"threshold_uncertainty_score":0.10212505},"labels":[],"label_agreement":null},{"id":"W4392387548","doi":"10.1190/tle43030145.1","title":"Fault locking and alternate fault activity revealed by simple tools and approaches — Examples from the Western Canadian Sedimentary Basin with implications for hydrocarbon exploration and production","year":2024,"lang":"en","type":"article","venue":"The Leading Edge","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Structural basin; Sedimentary rock; Hydrocarbon exploration; Sedimentary basin; Outcrop; Fault (geology); Software; Regional geology; Seismology; Earth science; Paleontology; Metamorphic petrology; Computer science; Tectonics","score_opus":0.08197935646356035,"score_gpt":0.24996466062903147,"score_spread":0.16798530416547114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392387548","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9652838,0.0015405569,0.0027148759,0.0003830977,0.000012732044,0.00006196921,0.0017252293,0.00009528738,0.028182315],"genre_scores_gemma":[0.9919036,0.0012038973,0.0033712366,0.000036321144,0.0000034622117,0.000009428596,0.00057636405,0.000027895914,0.002867846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996666,0.00003354395,0.000015995438,0.000053633757,0.0001361682,0.00009402377],"domain_scores_gemma":[0.99949837,0.00008790628,0.000060514263,0.00004050572,0.00024958578,0.00006309759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002990282,0.0004759453,0.00023948197,0.0049479976,0.002727748,0.001621824,0.0008040522,0.0003309027,0.001415405],"category_scores_gemma":[0.0011433342,0.00015682781,0.00025145637,0.008628163,0.001995699,0.0004297444,0.0007882336,0.0002780609,0.00013502006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034553296,0.00008446986,0.62407494,0.00091209135,0.0002159335,0.0077425875,0.03844931,0.01410992,0.019123139,0.0134585975,0.0071493713,0.27433416],"study_design_scores_gemma":[0.000007705535,0.000031543168,0.9436345,0.00016444363,0.00006340042,0.00062497274,0.021520114,0.00670448,0.0016669779,0.001575734,0.023926454,0.00007974256],"about_ca_topic_score_codex":0.9611624,"about_ca_topic_score_gemma":0.98903054,"teacher_disagreement_score":0.03883761,"about_ca_system_score_codex":0.009292594,"about_ca_system_score_gemma":0.0055253725,"threshold_uncertainty_score":0.07813263},"labels":[],"label_agreement":null},{"id":"W4392388673","doi":"10.1126/sciadv.adi8533","title":"On-fault earthquake energy density partitioning from shocked garnet in an exhumed seismic midcrustal fault","year":2024,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Seismology; Geology; Fault (geology); Seismic energy","score_opus":0.01487382695540445,"score_gpt":0.25064107819186476,"score_spread":0.2357672512364603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392388673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996643,0.00003609439,0.00007793207,0.0000050490607,4.6041436e-7,4.6851656e-7,0.000047550133,0.000004065183,0.00016415055],"genre_scores_gemma":[0.9997367,0.000025056584,0.00004719607,0.000002024278,5.51789e-7,5.430908e-7,0.00009612942,0.0000024184476,0.00008925493],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999579,0.0000029730058,0.0000029010303,0.00001229192,0.000010014526,0.000013913662],"domain_scores_gemma":[0.99993014,0.000014330431,0.000019122985,0.0000063962225,0.000018114983,0.000011913203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000051051593,0.0001610369,0.00022081513,0.00068808196,0.00022273384,0.0003309958,0.0002324212,0.00023698725,0.0012057676],"category_scores_gemma":[0.0002105379,0.0001442959,0.00012845143,0.0004286755,0.00035776052,0.00023285238,0.00031119116,0.00013149003,0.00011314836],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009221496,0.000089824665,0.23603275,0.00019725961,0.00011709468,0.002401137,0.00055892434,0.010260265,0.73458195,0.0004395607,0.00014907029,0.014249932],"study_design_scores_gemma":[0.000006300444,0.00008345598,0.961106,0.000008906794,0.00002287874,0.00042821452,0.00035197186,0.010965727,0.02663148,0.00014059519,0.00024269446,0.0000118580765],"about_ca_topic_score_codex":0.0031681904,"about_ca_topic_score_gemma":0.004758516,"teacher_disagreement_score":0.0031681904,"about_ca_system_score_codex":0.00039551163,"about_ca_system_score_gemma":0.000076595155,"threshold_uncertainty_score":0.0062994957},"labels":[],"label_agreement":null},{"id":"W4392585902","doi":"10.5194/egusphere-egu24-4090","title":"Deciphering the Role of Plate Motion Changes and Inherited Structures in Mega-Transform Fault Development Using Geodynamic Numerical Models","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital","funders":"","keywords":"Mega-; Motion (physics); Fault (geology); Geology; Transform fault; Seismology; Computer science; Physics; Artificial intelligence","score_opus":0.026796813394630144,"score_gpt":0.23448337066029787,"score_spread":0.20768655726566773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392585902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97145575,0.00017805662,0.021244032,0.00029990816,0.00003131108,0.000029520488,0.00041901693,0.00019318705,0.0061493283],"genre_scores_gemma":[0.9919213,0.00014697525,0.0070936545,0.000035909037,0.0000067095198,0.00002495439,0.00019283213,0.000047066733,0.00053060433],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998977,0.000022615091,0.000008358301,0.000025595531,0.000024772884,0.000020895843],"domain_scores_gemma":[0.99945384,0.00026039517,0.000109809545,0.000063825115,0.000055948043,0.00005605475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029381036,0.00037387578,0.00037017922,0.0004821879,0.0003594163,0.001245052,0.00076485047,0.0010921854,0.0016339172],"category_scores_gemma":[0.0018733249,0.0003384455,0.00060003775,0.0004599173,0.00062850927,0.0008342524,0.00061611074,0.000688695,0.00020557849],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015818478,0.000024644065,0.009518603,0.0000196735,0.000015472953,0.0000601074,0.00005022578,0.98426646,0.0026340317,0.0017249101,0.00007916559,0.0015908598],"study_design_scores_gemma":[0.0000036093923,0.0000055187666,0.0012310176,0.0000031321733,0.0000029687728,0.000009522306,0.000019353625,0.99790215,0.000286415,0.00039920892,0.00013323381,0.00000385747],"about_ca_topic_score_codex":0.015402763,"about_ca_topic_score_gemma":0.011983474,"teacher_disagreement_score":0.015402763,"about_ca_system_score_codex":0.0009119853,"about_ca_system_score_gemma":0.0009943018,"threshold_uncertainty_score":0.030626237},"labels":[],"label_agreement":null},{"id":"W4392593374","doi":"10.2172/2318777","title":"Central Asia Seismic Hazard Assessment (CASHA): A Probabilistic Seismic Hazard Assessment for Kazakhstan, Kyrgyzstan and Tajikistan","year":2024,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Central asia; Seismology; Hazard; Geology; Seismic hazard; Hazard analysis; Geography; Physical geography; Engineering; Reliability engineering","score_opus":0.032064148637701365,"score_gpt":0.3028175347745023,"score_spread":0.27075338613680094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392593374","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9439283,0.00084661966,0.01081189,0.0015213002,0.000119797805,0.00061703066,0.021645024,0.00057511387,0.019934822],"genre_scores_gemma":[0.9702195,0.0004981857,0.011529042,0.00014831229,0.000030756983,0.00019830298,0.0138965845,0.000045299606,0.0034340625],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99967563,0.00005921819,0.000031091367,0.00004354923,0.00011655489,0.000073912626],"domain_scores_gemma":[0.9989973,0.00007328194,0.00015139385,0.00006214543,0.000552032,0.00016400097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014703072,0.00066583656,0.00028922732,0.0024148468,0.00078259635,0.0011515196,0.0005499754,0.0004784717,0.0014810989],"category_scores_gemma":[0.0011904989,0.0002348103,0.00053501024,0.0024342695,0.00033677407,0.0008773078,0.0011035764,0.00055610744,0.00035764903],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007438723,0.0005550814,0.6414551,0.000677737,0.0004967349,0.0021192033,0.0034611921,0.068172395,0.0106659215,0.0075708115,0.05530674,0.20877524],"study_design_scores_gemma":[0.00017423237,0.0005958022,0.83995676,0.0002616406,0.00029099453,0.00047090274,0.008600885,0.085886635,0.0047735027,0.0033094345,0.055585094,0.00009396138],"about_ca_topic_score_codex":0.106023714,"about_ca_topic_score_gemma":0.09190521,"teacher_disagreement_score":0.106023714,"about_ca_system_score_codex":0.001910195,"about_ca_system_score_gemma":0.0055499827,"threshold_uncertainty_score":0.21081322},"labels":[],"label_agreement":null},{"id":"W4392595961","doi":"10.5194/egusphere-egu24-1114","title":"Spatial and Temporal Variability of Slip Rates on the Tuz G&amp;#246;l&amp;#252; Fault Zone: Insights from Zircon Double&amp;#160;Dating of Offset Lavas of Mount Hasan, Central Anatolia&amp;#160;","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Muscular Dystrophy Canada","funders":"","keywords":"Zircon; Geology; Offset (computer science); Mount; Fault (geology); Seismology; Geodesy; Geochemistry","score_opus":0.044411182839912314,"score_gpt":0.26555444492997576,"score_spread":0.22114326209006346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392595961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993606,0.00009742757,0.000091815586,0.00000926138,0.0000018469241,0.0000012092319,0.00018246115,0.0000047585104,0.00025053596],"genre_scores_gemma":[0.99935097,0.000056449535,0.00014593257,0.00000416075,0.0000032076596,0.0000032426303,0.0002804896,0.0000036448243,0.0001519483],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987686,0.00000888486,0.000010847551,0.00005741589,0.000018852672,0.000027124814],"domain_scores_gemma":[0.9997968,0.000020452053,0.00009483865,0.000018428476,0.000049978746,0.000019515057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002109997,0.00020305743,0.00023088945,0.000989115,0.00025951752,0.00047963494,0.00024566185,0.00029593566,0.0004201869],"category_scores_gemma":[0.00034035504,0.00012904858,0.00013366934,0.000969382,0.00032535332,0.00027254358,0.00042898965,0.00019690789,0.00014278841],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008625752,0.000028416132,0.9557368,0.000027789049,0.00006213714,0.00026815597,0.0009920481,0.0006726471,0.027360963,0.00014780535,0.00017136517,0.014445603],"study_design_scores_gemma":[0.000001783015,0.000011051893,0.9977118,0.0000034575398,0.000015050067,0.00011633701,0.00020265054,0.000590593,0.00076710415,0.000019498422,0.000557378,0.0000033333195],"about_ca_topic_score_codex":0.009409727,"about_ca_topic_score_gemma":0.02191525,"teacher_disagreement_score":0.009409727,"about_ca_system_score_codex":0.00037222868,"about_ca_system_score_gemma":0.00019361428,"threshold_uncertainty_score":0.018709898},"labels":[],"label_agreement":null},{"id":"W4392596432","doi":"10.5194/egusphere-egu24-1067","title":"Conceptual proof, current application, and lab procedures to quantify crustal thickness variations with muon paleotopometry","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Proof of concept; Current (fluid); Muon; Computer science; Geology; Nuclear engineering; Physics; Particle physics; Engineering; Operating system; Thermodynamics","score_opus":0.022605202646216006,"score_gpt":0.2671073969567321,"score_spread":0.24450219431051606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392596432","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004328555,0.0011353807,0.95141816,0.0021647834,0.00069323194,0.00097607705,0.0033114254,0.0065718465,0.029400587],"genre_scores_gemma":[0.039720356,0.0028239447,0.92441475,0.0010430705,0.000624098,0.0040021674,0.0042814445,0.0013997322,0.021690374],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99851805,0.00030962317,0.0000948629,0.00036882237,0.0006077183,0.00010096485],"domain_scores_gemma":[0.99754876,0.00037097727,0.00013472076,0.001294786,0.0005177279,0.00013300704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0042080483,0.0018580537,0.00076352514,0.0014413368,0.0011188224,0.0040302933,0.0037938827,0.0021924628,0.05307548],"category_scores_gemma":[0.005414593,0.0011835925,0.000960611,0.001247192,0.0021354011,0.0037899935,0.002774312,0.0026433873,0.02914515],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039995805,0.0005470142,0.0037746718,0.0016961014,0.00007815172,0.0007433372,0.00069481647,0.0047442303,0.08826834,0.4862623,0.05875161,0.3540395],"study_design_scores_gemma":[0.00015285356,0.0006210666,0.0038320357,0.00059253146,0.00006438472,0.0017070115,0.00030555789,0.030817475,0.08981801,0.108136125,0.76378596,0.00016697163],"about_ca_topic_score_codex":0.0016777719,"about_ca_topic_score_gemma":0.0011327805,"teacher_disagreement_score":0.05307548,"about_ca_system_score_codex":0.0009809196,"about_ca_system_score_gemma":0.0018899865,"threshold_uncertainty_score":0.17755514},"labels":[],"label_agreement":null},{"id":"W4392604773","doi":"10.5194/egusphere-egu24-12430","title":"Tectonic &amp;#8220;quakes&amp;#8221;, scaling and the turbulence of solids","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Turbulence; Scaling; Tectonics; Geology; Mechanics; Physics; Seismology; Mathematics; Geometry","score_opus":0.029503239749114188,"score_gpt":0.25075098295977494,"score_spread":0.22124774321066076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392604773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82976675,0.0069130473,0.04646103,0.023490332,0.0005966029,0.000025360761,0.0054702014,0.0011593682,0.08611738],"genre_scores_gemma":[0.9762265,0.0018890445,0.0088295685,0.0006250604,0.00015824937,0.000013652926,0.0015136442,0.00024930667,0.01049492],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9998752,0.000016524242,0.000008745146,0.000038390677,0.000043381937,0.000017772814],"domain_scores_gemma":[0.999589,0.00010105088,0.00013363952,0.00007010479,0.00007102383,0.00003510031],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028218198,0.00022762622,0.00025762687,0.0007799984,0.00049717986,0.0018522465,0.00030714602,0.0005111256,0.0049194144],"category_scores_gemma":[0.0016320926,0.00016713192,0.00020032188,0.0016350136,0.0021493358,0.0011975642,0.0007660595,0.00072932953,0.0009325494],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002507186,0.00008650583,0.15665159,0.00025348787,0.00011368158,0.0013915434,0.004387537,0.05177,0.022917993,0.39382893,0.09236441,0.27598366],"study_design_scores_gemma":[0.000012073539,0.000051398867,0.4648885,0.00011749296,0.000024928599,0.00070675835,0.0019179978,0.05502671,0.007015872,0.28548345,0.18459997,0.00015494936],"about_ca_topic_score_codex":0.009701996,"about_ca_topic_score_gemma":0.0077499687,"teacher_disagreement_score":0.009701996,"about_ca_system_score_codex":0.00061343156,"about_ca_system_score_gemma":0.0003070169,"threshold_uncertainty_score":0.019291043},"labels":[],"label_agreement":null},{"id":"W4392630659","doi":"10.5194/egusphere-egu24-15534","title":"Post-orogenic extension in Kos Island (Greece): geodynamic implications","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Extension (predicate logic); Geology; Geodynamics; Paleontology; Geography; Geodesy; Seismology; Tectonics; Computer science","score_opus":0.017004580176850782,"score_gpt":0.24238722663343462,"score_spread":0.22538264645658385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392630659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973907,0.00018202962,0.000030295016,0.000054805467,0.0000019682636,0.0000042055385,0.000088475885,0.0000036185204,0.0022438057],"genre_scores_gemma":[0.9993419,0.0001872151,0.000046793066,0.000013317809,0.0000026529221,0.00000197672,0.00009817245,0.0000020806408,0.00030596394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.000007816152,0.000005783431,0.000019936033,0.000008229584,0.000018187138],"domain_scores_gemma":[0.9999027,0.000010705135,0.000040682495,0.000008137345,0.000018031307,0.000019792207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010929504,0.00013817856,0.00011642914,0.0010337608,0.00024108494,0.000572327,0.00028518683,0.00027030386,0.0014437243],"category_scores_gemma":[0.00028357364,0.00009398175,0.00012602867,0.0011524666,0.0006356676,0.00037867308,0.0006976181,0.00014289764,0.00013792004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011496906,0.00005820584,0.9610297,0.00012207736,0.00009215226,0.0024956395,0.002678015,0.001404576,0.009978408,0.0011322513,0.00025007667,0.020643922],"study_design_scores_gemma":[0.0000026720138,0.000013087976,0.9968862,0.000015320185,0.000008181674,0.00019946096,0.0015205821,0.0002461859,0.00012031072,0.0001164539,0.0008680669,0.0000033855208],"about_ca_topic_score_codex":0.025252916,"about_ca_topic_score_gemma":0.049479116,"teacher_disagreement_score":0.025252916,"about_ca_system_score_codex":0.00075045123,"about_ca_system_score_gemma":0.00053893385,"threshold_uncertainty_score":0.050211847},"labels":[],"label_agreement":null},{"id":"W4392642938","doi":"10.22498/pages.32.1.34","title":"Earthquake-related tsunami archives based on sediments from coastal lagoons in the Lesser Antilles","year":2024,"lang":"en","type":"article","venue":"Past Global Change Magazine","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"Interreg; Labex UnivEarthS","keywords":"Geology; Oceanography; Seismology","score_opus":0.027274601044267245,"score_gpt":0.2456937067893211,"score_spread":0.21841910574505385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392642938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95794946,0.0003136337,0.00013437576,0.00025261065,0.000029594716,0.000037247217,0.033175882,0.000096958975,0.008010155],"genre_scores_gemma":[0.95918095,0.0010669803,0.0007594698,0.000086895154,0.000097038086,0.00003381625,0.031162607,0.000042059884,0.007570152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992704,0.000008596573,0.000016928276,0.0000103957145,0.000020091096,0.000016840184],"domain_scores_gemma":[0.9992409,0.00008770814,0.00024990132,0.00003504054,0.00026492792,0.00012150829],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020754145,0.00024359046,0.00013348796,0.0062708175,0.0005928221,0.00063521334,0.0001770435,0.00023048717,0.0048050643],"category_scores_gemma":[0.0006575111,0.0001374681,0.00010644075,0.0054574106,0.00020122316,0.00039411397,0.00071675406,0.00014044877,0.0013910069],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035742458,0.00006734684,0.9168549,0.0003898004,0.00005056211,0.001875677,0.0066398433,0.0005598672,0.012396766,0.00017478307,0.01517909,0.045454018],"study_design_scores_gemma":[0.00000410172,0.000012630549,0.9891249,0.000025181447,0.000010353661,0.0001876592,0.0023162633,0.00007795728,0.00028085895,0.000009779866,0.007945271,0.000004958653],"about_ca_topic_score_codex":0.0685316,"about_ca_topic_score_gemma":0.23331434,"teacher_disagreement_score":0.0685316,"about_ca_system_score_codex":0.00035659785,"about_ca_system_score_gemma":0.0006074251,"threshold_uncertainty_score":0.1362654},"labels":[],"label_agreement":null},{"id":"W4392651812","doi":"10.5194/egusphere-egu24-20139","title":"Evaluation of stochastic source models for the fault displacement hazard analyses using InSAR data: 2019 Ridgecrest earthquakes&amp;#160;","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Interferometric synthetic aperture radar; Seismology; Hazard; Fault (geology); Displacement (psychology); Seismic hazard; Geology; Geodesy; Stochastic modelling; Econometrics; Statistics; Mathematics; Remote sensing; Synthetic aperture radar","score_opus":0.3483084275772162,"score_gpt":0.4039154662116645,"score_spread":0.055607038634448325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392651812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9029338,0.00017941812,0.0938891,0.00024168202,0.00001785097,0.00007760411,0.00042416356,0.00037624207,0.0018600767],"genre_scores_gemma":[0.98883116,0.00006622351,0.010481236,0.000016773365,0.000009343996,0.000028332886,0.0003386449,0.000013720542,0.0002145071],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99954337,0.00022951693,0.000029142953,0.000072642,0.00008515775,0.000040110983],"domain_scores_gemma":[0.99599314,0.0032281328,0.0002878164,0.00012878269,0.00028654042,0.00007563275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022055025,0.0007060667,0.00032838038,0.00087657076,0.0002640719,0.0006380782,0.00081612734,0.0006921425,0.00043364888],"category_scores_gemma":[0.0052454183,0.00030147392,0.00061205885,0.00040002415,0.0002791798,0.0006413531,0.0004668074,0.0004586107,0.00010894272],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008433661,0.00007605739,0.006695886,0.000025679741,0.000049832728,0.00004564286,0.00003627978,0.98257726,0.00063120335,0.001150744,0.000116878255,0.008510173],"study_design_scores_gemma":[0.0000038718,0.000015591262,0.00077435526,0.000001325257,0.00000375634,0.0000045761694,0.000008054631,0.9988801,0.0001572148,0.00012685332,0.000021908249,0.0000023779603],"about_ca_topic_score_codex":0.01627766,"about_ca_topic_score_gemma":0.0108806295,"teacher_disagreement_score":0.01627766,"about_ca_system_score_codex":0.0008731376,"about_ca_system_score_gemma":0.0008027075,"threshold_uncertainty_score":0.03236586},"labels":[],"label_agreement":null},{"id":"W4392671861","doi":"10.22498/pages.32.1.8","title":"A major paleoearthquake in central Canada interpreted from early postglacial subaqueous mass transport deposits","year":2024,"lang":"en","type":"article","venue":"Past Global Change Magazine","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Mass transport; Geomorphology; Physics","score_opus":0.012449080667497421,"score_gpt":0.20375534774937784,"score_spread":0.19130626708188042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392671861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.979791,0.0012411961,0.0002439363,0.000758699,0.00010309124,0.000035671812,0.0020467904,0.00005898082,0.015720595],"genre_scores_gemma":[0.9928301,0.0006118862,0.00032568417,0.00014726009,0.00001695279,0.000006193516,0.0007528518,0.000023870403,0.0052852947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986506,0.0000034070815,0.000006555045,0.00001852286,0.000044471337,0.00006192915],"domain_scores_gemma":[0.99952674,0.000030239398,0.000052104595,0.000016115702,0.00025395918,0.00012095495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001242301,0.00038240617,0.00023711249,0.0032205058,0.004901367,0.0017283906,0.0007491733,0.00082538376,0.004588878],"category_scores_gemma":[0.0006843503,0.0002213499,0.0001987555,0.005695013,0.0016101588,0.0004210883,0.001059858,0.0007602409,0.00031831014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091502577,0.00014447935,0.7388474,0.00066911685,0.00025563687,0.016193204,0.05194344,0.0026015993,0.0412024,0.005679162,0.023061348,0.11848722],"study_design_scores_gemma":[0.000012070899,0.000011871603,0.9653872,0.00011674246,0.00003659031,0.0005220199,0.012619289,0.00036550537,0.0007033954,0.00016609879,0.020039145,0.000019959369],"about_ca_topic_score_codex":0.9902733,"about_ca_topic_score_gemma":0.9976497,"teacher_disagreement_score":0.010593793,"about_ca_system_score_codex":0.010593793,"about_ca_system_score_gemma":0.019503197,"threshold_uncertainty_score":0.07686365},"labels":[],"label_agreement":null},{"id":"W4392759473","doi":"10.5194/egusphere-egu24-13072","title":"Poseidon&amp;#8217;s seismic breadcrumbs: ultracataclasite vein evolution within a granodiorite along the Naxos Detachment System","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Vein; Geology; Internal medicine; Medicine","score_opus":0.018592186745684955,"score_gpt":0.22915305974907757,"score_spread":0.2105608730033926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392759473","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985702,0.000017099934,0.000053510597,0.0000068850154,0.0000010090225,0.0000015105014,0.00009575508,0.0000033808064,0.0012505878],"genre_scores_gemma":[0.99911183,0.000016262149,0.00012444537,0.0000028350482,0.0000010869638,0.0000014381075,0.00014631065,0.0000036667645,0.0005922406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999951,0.000004206703,0.0000028620107,0.00002472702,0.0000095553605,0.000007643523],"domain_scores_gemma":[0.99994516,0.000004184104,0.000017030794,0.00000866922,0.000012520255,0.000012426886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000059173322,0.00012634668,0.00010523833,0.0006013331,0.0002000537,0.00038397402,0.00013867473,0.000127662,0.001109196],"category_scores_gemma":[0.00016680491,0.00008676251,0.00009119557,0.0005029061,0.00039710672,0.00009465992,0.00037882113,0.00009594584,0.00016861303],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015999323,0.000028426633,0.89646983,0.000034679855,0.000042060707,0.00068139774,0.001972176,0.0017124703,0.07740614,0.00046978373,0.0002740663,0.020748962],"study_design_scores_gemma":[0.0000036605652,0.000017159662,0.99656785,0.0000041858107,0.0000044977915,0.00014138655,0.00036170057,0.0005758178,0.0012704784,0.000051673644,0.0009991232,0.0000024332192],"about_ca_topic_score_codex":0.014899622,"about_ca_topic_score_gemma":0.029517377,"teacher_disagreement_score":0.014899622,"about_ca_system_score_codex":0.00033977942,"about_ca_system_score_gemma":0.00018116225,"threshold_uncertainty_score":0.029625773},"labels":[],"label_agreement":null},{"id":"W4392761377","doi":"10.1080/21664250.2024.2324520","title":"Probabilistic tsunami hazard assessment for the makran subduction zone using logic tree and stochastic rupture sources","year":2024,"lang":"en","type":"article","venue":"Coastal Engineering Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canada Research Chairs","keywords":"Subduction; Geology; Seismology; Bathymetry; Moment magnitude scale; Slip (aerodynamics); Seismic hazard; Tsunami earthquake; Tectonics; Oceanography; Geometry","score_opus":0.020757766984126996,"score_gpt":0.23876162051317046,"score_spread":0.21800385352904347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392761377","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9263161,0.000118678225,0.071258865,0.00010627052,0.000005296638,0.000033067136,0.0003067629,0.00011471729,0.0017403575],"genre_scores_gemma":[0.99403965,0.000050753042,0.0055030156,0.0000069114994,0.0000026541966,0.000015519361,0.00016770329,0.000004317379,0.00020952598],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980146,0.00007216423,0.00001299642,0.000030867246,0.000053019397,0.000029534544],"domain_scores_gemma":[0.9989041,0.0007072955,0.00018048854,0.000032342534,0.00013098701,0.00004467681],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060593453,0.00045302784,0.00031581573,0.0011257683,0.00025408613,0.0005493056,0.000531537,0.00038897523,0.00079639326],"category_scores_gemma":[0.0016313795,0.00018986526,0.0005520428,0.0007393052,0.00019192787,0.0006671224,0.00043588065,0.0002177615,0.000067244044],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003910643,0.000017442238,0.0050131693,0.000010992419,0.000018394992,0.00006886524,0.000019008094,0.9886785,0.00040430523,0.0013839158,0.00005492715,0.0042914012],"study_design_scores_gemma":[0.0000015884738,0.00001226688,0.000627386,9.815333e-7,0.0000033393223,0.000009299163,0.000006830653,0.9987463,0.00006424101,0.0005031841,0.000022936592,0.0000018097894],"about_ca_topic_score_codex":0.008264235,"about_ca_topic_score_gemma":0.0059248735,"teacher_disagreement_score":0.008264235,"about_ca_system_score_codex":0.0008594565,"about_ca_system_score_gemma":0.0006561114,"threshold_uncertainty_score":0.016432285},"labels":[],"label_agreement":null},{"id":"W4392783621","doi":"10.21203/rs.3.rs-3953181/v1","title":"Subduction thrust valving action revealed from time-lapse imaging of deep Hikurangi slow slip events","year":2024,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Subduction; Geology; Thrust; Seismology; Slip (aerodynamics); Episodic tremor and slip; Tectonics; Engineering; Aerospace engineering","score_opus":0.050851328663723966,"score_gpt":0.3356864768357329,"score_spread":0.28483514817200895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392783621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976986,0.00010612851,0.000748338,0.000018369243,0.000005582079,0.0000035180963,0.00026815134,0.00001506667,0.0011361332],"genre_scores_gemma":[0.9984499,0.0001267014,0.0006668909,0.000008007049,0.000011955617,0.0000041681456,0.00031075865,0.0000069586686,0.0004146643],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999984,0.0000010673937,9.005808e-7,0.0000042904603,0.0000027396877,0.0000069303824],"domain_scores_gemma":[0.99992955,0.00001037991,0.000017210863,0.000008141584,0.000014003748,0.000020760404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008336922,0.0001868702,0.00013472684,0.0005320705,0.00014552707,0.0004166196,0.00013205092,0.0002536785,0.0008853539],"category_scores_gemma":[0.00018179542,0.00019541927,0.000069446105,0.00044315954,0.00016650395,0.00027813384,0.0002598659,0.0002493528,0.00016446231],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045313165,0.00007289667,0.08241586,0.00007890357,0.000048190395,0.0012693143,0.0006237883,0.0011825687,0.89548063,0.00054806744,0.0006364406,0.017190231],"study_design_scores_gemma":[0.0000103682305,0.00004901935,0.97789633,0.000009466482,0.000035399018,0.0005456957,0.00034540784,0.0040727686,0.015798511,0.00017736752,0.0010474434,0.000012149976],"about_ca_topic_score_codex":0.0010229932,"about_ca_topic_score_gemma":0.0025515032,"teacher_disagreement_score":0.0010229932,"about_ca_system_score_codex":0.00008215816,"about_ca_system_score_gemma":0.00008289864,"threshold_uncertainty_score":0.002961874},"labels":[],"label_agreement":null},{"id":"W4392890910","doi":"10.30897/ijegeo.1441082","title":"The Investigation of Tropospheric Changes with GNSS: A study on 6 February 2023 Kahramanmaraş Earthquake Sequence","year":2024,"lang":"en","type":"article","venue":"International Journal of Environment and Geoinformatics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada","keywords":"Troposphere; Zenith; GNSS applications; Geology; Geodetic datum; Seismology; Geodesy; Environmental science; Atmospheric sciences; Global Positioning System","score_opus":0.018659094731989807,"score_gpt":0.2228633857041642,"score_spread":0.20420429097217438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392890910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994618,0.00005150335,0.000022572964,0.000014215913,0.0000017257408,0.0000029949852,0.000246653,0.0000017979811,0.00019673276],"genre_scores_gemma":[0.99919146,0.00009306579,0.000075730386,0.000010764407,0.0000062959903,0.0000051619486,0.0004737259,0.000001136025,0.00014256463],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999348,0.000007733218,0.000005019705,0.000014572755,0.000020011208,0.000017834425],"domain_scores_gemma":[0.9998815,0.000008559607,0.000051383162,0.000007792191,0.000029659639,0.000021017338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010299619,0.0002483371,0.00014991444,0.0004654377,0.00026223558,0.00027213877,0.00016992846,0.00027382115,0.00029570496],"category_scores_gemma":[0.00021025444,0.00008259382,0.00018188193,0.00071172364,0.00012714096,0.000152453,0.00018013101,0.00018392553,0.00011671794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011608249,0.000074080046,0.9752371,0.000030824518,0.00008576046,0.0008873123,0.001137288,0.00043123995,0.013075625,0.000046765163,0.00026232266,0.008615588],"study_design_scores_gemma":[8.595393e-7,0.000028192899,0.9989287,0.0000013757684,0.000009125657,0.000067845845,0.0003429366,0.000121301775,0.00023513484,0.000003639006,0.00025892077,0.0000020161],"about_ca_topic_score_codex":0.039835703,"about_ca_topic_score_gemma":0.08032715,"teacher_disagreement_score":0.039835703,"about_ca_system_score_codex":0.0003164393,"about_ca_system_score_gemma":0.00023850828,"threshold_uncertainty_score":0.07920766},"labels":[],"label_agreement":null},{"id":"W4392963350","doi":"10.1029/2023jb027578","title":"Rupture Dynamics of Cascading Earthquakes in a Multiscale Fracture Network","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"King Abdullah University of Science and Technology; Southern California Earthquake Center; Directorate for Geosciences; National Aeronautics and Space Administration; National Science Foundation","keywords":"Slip (aerodynamics); Fracture (geology); Earthquake rupture; Geology; Seismology; Fault (geology); Stress field; Geotechnical engineering; Structural engineering; Engineering; Finite element method","score_opus":0.028456264270282087,"score_gpt":0.3229930380350393,"score_spread":0.29453677376475723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392963350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99371076,0.00004159638,0.005226793,0.000058034915,0.000004429396,0.000006328845,0.000062006744,0.00003983124,0.000850245],"genre_scores_gemma":[0.9992483,0.000016591675,0.0005983377,0.0000058570217,0.0000015526181,0.0000048682214,0.000021760708,0.0000038082685,0.000098829994],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991524,0.000013583788,0.0000053232734,0.000024897356,0.000015281186,0.000025595053],"domain_scores_gemma":[0.99958104,0.000151242,0.00011462032,0.00003219695,0.000038532165,0.00008238434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022962074,0.0002458969,0.00032667207,0.0004703747,0.0003998177,0.00059171766,0.0005232994,0.00059005036,0.0012291074],"category_scores_gemma":[0.0010465502,0.00024615586,0.00045728651,0.0002892924,0.0006176411,0.0006194973,0.0006676313,0.00035164304,0.00006556641],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000063390755,0.00007369885,0.02304286,0.000027486325,0.00007808052,0.00031578616,0.00008992209,0.9575272,0.011876618,0.0040157437,0.0002461971,0.0026429547],"study_design_scores_gemma":[0.000009735768,0.000042545096,0.008164893,0.0000038851613,0.000014320741,0.00004252587,0.000049321276,0.98937887,0.0005735944,0.0015815134,0.00012780979,0.000011051846],"about_ca_topic_score_codex":0.0067085777,"about_ca_topic_score_gemma":0.0035966516,"teacher_disagreement_score":0.0067085777,"about_ca_system_score_codex":0.0006837603,"about_ca_system_score_gemma":0.00030045447,"threshold_uncertainty_score":0.013339102},"labels":[],"label_agreement":null},{"id":"W4392964935","doi":"10.1029/2023jb027714","title":"Fluid‐Induced Aseismic Slip May Explain the Non‐Self‐Similar Source Scaling of the Induced Earthquake Sequence Near the Dallas‐Fort Worth Airport, Texas","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Slip (aerodynamics); Scaling; Seismic moment; Induced seismicity; Geology; Seismology; Moment magnitude scale; Drop (telecommunication); Pore water pressure; Mechanics; Fault (geology); Geotechnical engineering; Engineering; Geometry; Physics; Mathematics","score_opus":0.06280816725862677,"score_gpt":0.3229982099822097,"score_spread":0.2601900427235829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392964935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99683833,0.000025585152,0.0020975792,0.000065700246,0.000003991712,0.000005960677,0.0000478844,0.000029850578,0.00088489224],"genre_scores_gemma":[0.9997061,0.000009442039,0.0001699461,0.000003506857,0.0000014735265,0.000002005468,0.000020676107,0.0000019376882,0.000084849686],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999691,0.0000039542447,0.000002590192,0.000008764354,0.000003985668,0.000011580979],"domain_scores_gemma":[0.99986804,0.000017734223,0.000056228837,0.0000132346495,0.000018716055,0.000025973346],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008258839,0.00027188123,0.00017182447,0.00030764448,0.00026611888,0.00040132913,0.00041810758,0.00037319356,0.0011176676],"category_scores_gemma":[0.00043078823,0.0001496345,0.00025466894,0.00016751324,0.00033878995,0.00032850594,0.0002939835,0.00025323316,0.000090313886],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013607022,0.0002365643,0.2079939,0.00005528523,0.00008217811,0.0009836216,0.00021694847,0.7369028,0.043654088,0.0040685423,0.00057898485,0.0050909915],"study_design_scores_gemma":[0.000018971261,0.00005155684,0.06447778,0.0000059082395,0.000013064335,0.00007082639,0.00010999442,0.93275166,0.0016367106,0.00064122875,0.00021217272,0.000010233797],"about_ca_topic_score_codex":0.00868905,"about_ca_topic_score_gemma":0.0054888735,"teacher_disagreement_score":0.00868905,"about_ca_system_score_codex":0.0005755564,"about_ca_system_score_gemma":0.00026046616,"threshold_uncertainty_score":0.017276943},"labels":[],"label_agreement":null},{"id":"W4393000273","doi":"10.1029/2023gc011271","title":"Controls on Bending‐Related Faulting Offshore of the Alaska Peninsula","year":2024,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Peninsula; Submarine pipeline; Seismology; Oceanography; Paleontology; Archaeology; Geography","score_opus":0.008469382441906823,"score_gpt":0.20489085399357576,"score_spread":0.19642147155166895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393000273","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998896,0.000033241904,0.000054892793,0.000008336394,0.000001200605,0.0000011821874,0.00010988399,0.000003250022,0.0008920667],"genre_scores_gemma":[0.99955076,0.000037638358,0.000059742437,0.0000038224566,6.367007e-7,0.0000015015738,0.00009894886,0.000001345359,0.0002456029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999902,0.0000126165005,0.000013162283,0.00003869986,0.000017773038,0.000015783824],"domain_scores_gemma":[0.99956447,0.000063854466,0.00018116608,0.00004153806,0.000076234974,0.00007274863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002177642,0.00022192026,0.00014375935,0.0005489581,0.00029041074,0.0005494161,0.00017408394,0.00013260182,0.001608624],"category_scores_gemma":[0.00047549471,0.00014504911,0.000121553705,0.0004769051,0.00036277037,0.00026607118,0.00042601326,0.00013336138,0.0001795699],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015377138,0.000025651843,0.92428994,0.000049111975,0.00007507388,0.00031505324,0.0009397805,0.0024061922,0.064130984,0.00032817345,0.000111348665,0.0071748644],"study_design_scores_gemma":[0.0000013086718,0.000017763676,0.99756503,0.000007604718,0.000008170444,0.00003525042,0.0004959233,0.00032593336,0.0011824202,0.00006727144,0.00028866404,0.000004742022],"about_ca_topic_score_codex":0.019103149,"about_ca_topic_score_gemma":0.042122316,"teacher_disagreement_score":0.019103149,"about_ca_system_score_codex":0.00047771016,"about_ca_system_score_gemma":0.00032025002,"threshold_uncertainty_score":0.037983894},"labels":[],"label_agreement":null},{"id":"W4393471012","doi":"10.5281/zenodo.5717482","title":"Supplementary data files for JGR 2021JB022729R, Initial results from the Oman Drilling Project Multi-Borehole Observatory: Petrogenesis and ongoing alteration of mantle peridotite in the weathering horizon","year":2021,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Petrogenesis; Peridotite; Geology; Geochemistry; Borehole; Observatory; Drilling; Mantle (geology); Weathering; Horizon; Petrology; Paleontology; Engineering","score_opus":0.1182754969859849,"score_gpt":0.28676825525785815,"score_spread":0.16849275827187327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393471012","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000021630527,0.000009217976,0.000027799508,0.000026987282,0.000018556791,0.000004000154,0.99948007,0.00007989191,0.00033195384],"genre_scores_gemma":[0.00024041253,0.000025038302,0.00019681195,0.000040133193,0.00001599564,0.000044938082,0.99858814,0.00016664184,0.0006819072],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99884605,0.00013050335,0.00018043416,0.0003005884,0.0003188154,0.00022360211],"domain_scores_gemma":[0.9950702,0.0015031466,0.0006374886,0.00094302796,0.0013569454,0.000489205],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0014934494,0.0018377386,0.00171222,0.0044760844,0.0011669174,0.0035318148,0.0030069163,0.001954849,0.38956067],"category_scores_gemma":[0.009351534,0.0008675345,0.0011824358,0.010527119,0.00047751283,0.0025523845,0.002536502,0.0021561638,0.24277763],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028765437,0.000014212314,0.00046916702,0.00044750495,0.000018329574,0.00001559028,0.000021436535,0.00019664041,0.000069553666,0.0004671292,0.99728775,0.00096406013],"study_design_scores_gemma":[0.00021258072,0.000011742156,0.0055916617,0.0002744453,0.000029447374,0.00004135877,0.00010616265,0.0002144238,0.00024617428,0.0017423233,0.99149853,0.000031268042],"about_ca_topic_score_codex":0.028749622,"about_ca_topic_score_gemma":0.050364777,"teacher_disagreement_score":0.38956067,"about_ca_system_score_codex":0.0018877123,"about_ca_system_score_gemma":0.0034161021,"threshold_uncertainty_score":0.87071764},"labels":[],"label_agreement":null},{"id":"W4393476695","doi":"10.5281/zenodo.5056915","title":"Data for: A further source of Tokyo earthquakes and Pacific Ocean tsunamis","year":2021,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Seismology; Pacific ocean; Geology; Oceanography; Climatology; Geography","score_opus":0.04706032324780955,"score_gpt":0.24050129409702753,"score_spread":0.19344097084921796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393476695","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00017819357,0.000022103208,0.00007893353,0.000053240925,0.000029155957,0.00001363167,0.99818856,0.0002677815,0.0011684241],"genre_scores_gemma":[0.0011235584,0.00005494092,0.00051546184,0.00004836802,0.00001584893,0.000081982515,0.9957858,0.00025311706,0.0021209691],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.999305,0.000049130613,0.00015261807,0.00014824506,0.00024183904,0.00010320857],"domain_scores_gemma":[0.99556535,0.00061953237,0.0007104606,0.00070110214,0.0019939407,0.00040957532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090456265,0.0014122005,0.001221108,0.0043579005,0.0007564249,0.0021409316,0.0023494363,0.0013931002,0.2620315],"category_scores_gemma":[0.005879182,0.0008101055,0.00051623024,0.011163983,0.00034494247,0.001611589,0.0020985473,0.0017439515,0.15303072],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110385925,0.000036017867,0.002903677,0.0007508516,0.00003382849,0.00006295097,0.000111727284,0.00032996942,0.00037894878,0.00081589597,0.9861649,0.008300765],"study_design_scores_gemma":[0.00020035465,0.000021717336,0.011489864,0.00023543269,0.00003396925,0.000054108477,0.00018889642,0.00032234658,0.0006476928,0.0009249312,0.98584425,0.00003649248],"about_ca_topic_score_codex":0.02879524,"about_ca_topic_score_gemma":0.040246867,"teacher_disagreement_score":0.2620315,"about_ca_system_score_codex":0.0011097239,"about_ca_system_score_gemma":0.0029257247,"threshold_uncertainty_score":0.8765827},"labels":[],"label_agreement":null},{"id":"W4393483876","doi":"10.5281/zenodo.4698675","title":"Reactivation Potential of Intraplate Faults in the Western Quebec Seismic Zone (Supporting Info)","year":2021,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Seismology; Geology; Seismic zone; Induced seismicity; Tectonics","score_opus":0.0229504147406884,"score_gpt":0.2346696313151998,"score_spread":0.2117192165745114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393483876","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00022561075,0.0000327428,0.000011411429,0.000018913699,0.0000043479645,0.0000030999768,0.99932086,0.000034416087,0.0003485496],"genre_scores_gemma":[0.0019793622,0.00007878902,0.0001100146,0.000019480776,0.000004454164,0.000028869465,0.99666804,0.000027890395,0.0010830696],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99946195,0.00003535624,0.00004356023,0.00011590201,0.00018261335,0.00016055837],"domain_scores_gemma":[0.99684393,0.00046930363,0.0002862851,0.00031293623,0.0017849122,0.00030270108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006669635,0.0013859662,0.0010968131,0.004996023,0.0011180649,0.0018168982,0.0020318155,0.0011178566,0.07552529],"category_scores_gemma":[0.004472535,0.0004336069,0.0006638824,0.010214014,0.00033210017,0.0006558173,0.0010715578,0.0009982393,0.021379665],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000844185,0.000013979323,0.0063754832,0.0006078045,0.000057405257,0.000035059085,0.000041543863,0.0008158809,0.00010505742,0.0004667727,0.98787063,0.003525984],"study_design_scores_gemma":[0.00037478816,0.000018013317,0.12116046,0.001158351,0.00010016837,0.00006266081,0.00029624923,0.0018777935,0.0005082048,0.0007736305,0.87358093,0.00008870212],"about_ca_topic_score_codex":0.9154457,"about_ca_topic_score_gemma":0.9526184,"teacher_disagreement_score":0.084554315,"about_ca_system_score_codex":0.007385096,"about_ca_system_score_gemma":0.0103407595,"threshold_uncertainty_score":0.25265723},"labels":[],"label_agreement":null},{"id":"W4393716222","doi":"10.5281/zenodo.3467375","title":"Shear Wave Splitting and Mantle Flow beneath Alaska Data Set","year":2018,"lang":"en","type":"dataset","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Shear wave splitting; Shear (geology); Mantle (geology); Seismology; Geophysics; Petrology","score_opus":0.09916838610900831,"score_gpt":0.26529283934906156,"score_spread":0.16612445324005326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393716222","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011526724,0.00023809698,0.00011647404,0.00009888879,0.00008111742,0.000034923552,0.98437923,0.00022456526,0.0032999339],"genre_scores_gemma":[0.01076893,0.0001777182,0.0004525107,0.000034152752,0.000025500218,0.00012279776,0.98460984,0.000073361145,0.0037352147],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990256,0.00008694397,0.00014913654,0.00017065648,0.00047665267,0.00009112257],"domain_scores_gemma":[0.9940661,0.00061457587,0.00064306794,0.0009235062,0.003390995,0.00036164798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012561615,0.00061294617,0.0006398979,0.0050339946,0.0006804029,0.0011976988,0.0011432692,0.0005076356,0.033754677],"category_scores_gemma":[0.006229759,0.00034866625,0.00061201304,0.007897546,0.0001720094,0.00066987885,0.001089891,0.0006036691,0.019979069],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047166797,0.00013294189,0.087004624,0.0009568973,0.00032308255,0.00032721655,0.00046716578,0.0018698806,0.0014648573,0.0010515044,0.86981136,0.036118854],"study_design_scores_gemma":[0.00009136879,0.00006504804,0.45559406,0.00048860017,0.00014528076,0.00015493223,0.000846666,0.00071727997,0.0015546498,0.00045962795,0.5397952,0.000087281296],"about_ca_topic_score_codex":0.114919946,"about_ca_topic_score_gemma":0.12984999,"teacher_disagreement_score":0.114919946,"about_ca_system_score_codex":0.0008575668,"about_ca_system_score_gemma":0.0027365112,"threshold_uncertainty_score":0.2285021},"labels":[],"label_agreement":null},{"id":"W4393756606","doi":"10.5281/zenodo.5056914","title":"Data for: A further source of Tokyo earthquakes and Pacific Ocean tsunamis","year":2021,"lang":"en","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Pacific ocean; Seismology; Geology; Oceanography; Geography; Climatology","score_opus":0.04706032324780955,"score_gpt":0.24050129409702753,"score_spread":0.19344097084921796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393756606","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00017819357,0.000022103208,0.00007893353,0.000053240925,0.000029155957,0.00001363167,0.99818856,0.0002677815,0.0011684241],"genre_scores_gemma":[0.0011235584,0.00005494092,0.00051546184,0.00004836802,0.00001584893,0.000081982515,0.9957858,0.00025311706,0.0021209691],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.999305,0.000049130613,0.00015261807,0.00014824506,0.00024183904,0.00010320857],"domain_scores_gemma":[0.99556535,0.00061953237,0.0007104606,0.00070110214,0.0019939407,0.00040957532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090456265,0.0014122005,0.001221108,0.0043579005,0.0007564249,0.0021409316,0.0023494363,0.0013931002,0.2620315],"category_scores_gemma":[0.005879182,0.0008101055,0.00051623024,0.011163983,0.00034494247,0.001611589,0.0020985473,0.0017439515,0.15303072],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110385925,0.000036017867,0.002903677,0.0007508516,0.00003382849,0.00006295097,0.000111727284,0.00032996942,0.00037894878,0.00081589597,0.9861649,0.008300765],"study_design_scores_gemma":[0.00020035465,0.000021717336,0.011489864,0.00023543269,0.00003396925,0.000054108477,0.00018889642,0.00032234658,0.0006476928,0.0009249312,0.98584425,0.00003649248],"about_ca_topic_score_codex":0.02879524,"about_ca_topic_score_gemma":0.040246867,"teacher_disagreement_score":0.2620315,"about_ca_system_score_codex":0.0011097239,"about_ca_system_score_gemma":0.0029257247,"threshold_uncertainty_score":0.8765827},"labels":[],"label_agreement":null},{"id":"W4394109113","doi":"10.6084/m9.figshare.12659339","title":"Merrill_et_al_2020_JGR","year":2020,"lang":"en","type":"dataset","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geography","score_opus":0.050917849125939336,"score_gpt":0.2372348971188131,"score_spread":0.18631704799287377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394109113","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000043985936,0.000024582485,0.00004368107,0.00004358744,0.000020944459,0.0000040568584,0.9986272,0.0003462962,0.00084562367],"genre_scores_gemma":[0.00024573389,0.00004420846,0.00020973278,0.000046529807,0.000009480948,0.00003547652,0.99847037,0.00023632312,0.0007021143],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99939656,0.00007976154,0.00007045324,0.0001703099,0.0001711569,0.00011178477],"domain_scores_gemma":[0.99835974,0.00029664175,0.0002065761,0.00050542725,0.00040562366,0.00022601389],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011164636,0.0019730371,0.0012809461,0.002851402,0.00065897935,0.003013214,0.0035623466,0.0014450166,0.15942016],"category_scores_gemma":[0.0046556513,0.0009079349,0.001015243,0.005682789,0.0003430275,0.0018740793,0.0024501265,0.0013199602,0.16671126],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037707672,0.0000057336483,0.00032177,0.00034353338,0.00001923192,0.000009845221,0.000014863049,0.00015229329,0.00008014462,0.00051573245,0.9967895,0.0017095399],"study_design_scores_gemma":[0.0001301865,0.000008672112,0.0028605368,0.00017108709,0.00001791259,0.00002545125,0.000032332355,0.0002502594,0.00023530713,0.0007032327,0.99554414,0.00002095868],"about_ca_topic_score_codex":0.034984726,"about_ca_topic_score_gemma":0.035903472,"teacher_disagreement_score":0.15942016,"about_ca_system_score_codex":0.0015592952,"about_ca_system_score_gemma":0.0018900685,"threshold_uncertainty_score":0.5333136},"labels":[],"label_agreement":null},{"id":"W4394593589","doi":"10.1016/j.soildyn.2024.108634","title":"Türkiye Mw 7.7 Pazarcık and Mw 7.6 Elbistan earthquakes of February 6th, 2023: Contribution of valley effects on damage pattern","year":2024,"lang":"en","type":"article","venue":"Soil Dynamics and Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"Seismology; Geology; Environmental science","score_opus":0.003881157879069908,"score_gpt":0.18148221629893238,"score_spread":0.17760105841986248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394593589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9810331,0.004538009,0.00031433825,0.0016927102,0.00011916311,0.000019240757,0.0026497717,0.00001910184,0.009614673],"genre_scores_gemma":[0.99244326,0.002044019,0.00019870764,0.000090489215,0.000055091943,0.000008298821,0.0019661668,0.000009967621,0.0031838783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987245,0.000014823329,0.0000086503305,0.00002070145,0.00002233865,0.000061027713],"domain_scores_gemma":[0.9997651,0.000029668094,0.00006748078,0.000011572213,0.00009711312,0.000029076342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024470946,0.00041613256,0.00026641233,0.00077275245,0.00032334923,0.00055142597,0.00023579608,0.00042413274,0.0053992714],"category_scores_gemma":[0.00065114873,0.00020438508,0.00032150798,0.0010362768,0.00024146336,0.0005079614,0.00049371907,0.0004024365,0.0006133605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013847324,0.00014528121,0.83113045,0.0006749548,0.0007251128,0.004275953,0.0010082736,0.005126125,0.0065285396,0.0038309933,0.01456103,0.13060845],"study_design_scores_gemma":[0.000021791931,0.00004235921,0.9905218,0.00004988889,0.00008550336,0.0004032894,0.0006111611,0.0011365856,0.0005072218,0.00032497718,0.00628326,0.000012247223],"about_ca_topic_score_codex":0.04420577,"about_ca_topic_score_gemma":0.054164473,"teacher_disagreement_score":0.04420577,"about_ca_system_score_codex":0.0011129619,"about_ca_system_score_gemma":0.0013825459,"threshold_uncertainty_score":0.08789694},"labels":[],"label_agreement":null},{"id":"W4394765899","doi":"10.22541/essoar.171291920.01431352/v1","title":"Pressure dependence of permeability in cracked rocks: experimental evidence of non-linear pore-pressure gradients from local measurements","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique; China Scholarship Council","keywords":"Permeability (electromagnetism); Micromechanics; Geology; Pore water pressure; Pressure gradient; Exponential function; Fluid dynamics; Linearity; Relative permeability; Mechanics; Mineralogy; Materials science; Porosity; Geotechnical engineering; Composite material; Chemistry; Physics; Mathematics","score_opus":0.05815511520747866,"score_gpt":0.29488543080719,"score_spread":0.23673031559971133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394765899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903977,0.00020494034,0.008638615,0.000027331502,0.000003366322,0.000009665406,0.00015241279,0.000084915795,0.00048115628],"genre_scores_gemma":[0.9987208,0.000056231478,0.0011085235,0.000004047454,0.0000013497671,0.0000048262814,0.000037543927,0.00000945095,0.000057218123],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997044,0.000026267795,0.000021029371,0.00008076927,0.00012438033,0.00004306622],"domain_scores_gemma":[0.9989485,0.0004969675,0.00020828053,0.00015990148,0.00013239418,0.000053976502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002850425,0.00022888019,0.00023498184,0.00043990774,0.00021295658,0.00027229736,0.0004740653,0.00036746304,0.00090821105],"category_scores_gemma":[0.0015466949,0.00031351423,0.000097379976,0.0003142276,0.0008217996,0.00070550776,0.0005168555,0.00067320786,0.0001240865],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007620249,0.000025394638,0.003880725,0.00008250398,0.000007808686,0.00009525111,0.00013478937,0.0007960108,0.9919552,0.00010665797,0.000023715282,0.002815803],"study_design_scores_gemma":[0.000011407001,0.0001597973,0.051834375,0.000009403352,0.000014787907,0.0002790183,0.0000935007,0.014391219,0.9327317,0.00018851274,0.00026862527,0.000017706134],"about_ca_topic_score_codex":0.00059019827,"about_ca_topic_score_gemma":0.00080160605,"teacher_disagreement_score":0.00090821105,"about_ca_system_score_codex":0.00012655504,"about_ca_system_score_gemma":0.00009620602,"threshold_uncertainty_score":0.0030383468},"labels":[],"label_agreement":null},{"id":"W4394879855","doi":"10.62481/eec45dc3","title":"M3.6 earthquake below eastern shore of Lake Ontario shakes upstate New York, Canada","year":2023,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shore; Geography; Archaeology; Oceanography; Seismology; Geology","score_opus":0.052812242125057335,"score_gpt":0.21665190829567604,"score_spread":0.1638396661706187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394879855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9305017,0.00027532826,0.00015860307,0.00078090135,0.00003742845,0.000052290467,0.017454179,0.000051677718,0.0506879],"genre_scores_gemma":[0.9540431,0.00029680974,0.00023027576,0.000065365246,0.000009904136,0.000014971882,0.0064052544,0.000017201643,0.038917247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998394,0.000006762667,0.0000057000284,0.000019838064,0.000048413433,0.00007978867],"domain_scores_gemma":[0.99947494,0.000026571735,0.000029236353,0.000012800062,0.0003519433,0.000104595914],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008778809,0.00017095883,0.0001871994,0.00088760024,0.0025997558,0.0008699669,0.00038024868,0.00034387782,0.011749661],"category_scores_gemma":[0.0007013104,0.00014597764,0.00013853768,0.0017400831,0.00029470387,0.0002922896,0.0005330375,0.00033006902,0.0008083124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038764082,0.00008913706,0.8583666,0.00017775202,0.00008387559,0.0010281805,0.006395208,0.003966937,0.0032795432,0.0027943924,0.08558175,0.03784894],"study_design_scores_gemma":[0.000008685159,0.000007170605,0.9861348,0.000019127323,0.0000121252615,0.00002333248,0.003314205,0.0011023786,0.00023010856,0.000082270024,0.009056334,0.00000960117],"about_ca_topic_score_codex":0.9971644,"about_ca_topic_score_gemma":0.9993143,"teacher_disagreement_score":0.014108008,"about_ca_system_score_codex":0.014108008,"about_ca_system_score_gemma":0.015482621,"threshold_uncertainty_score":0.10236126},"labels":[],"label_agreement":null},{"id":"W4394891429","doi":"10.1785/0120240051","title":"<i>Erratum to</i> The Influence of a Transitional Stress Regime on the Source Characteristics of Induced Seismicity and Fault Activation: Evidence from the 30 November 2018 Fort St. John ML 4.5 Induced Earthquake Sequence","year":2024,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Citation; Induced seismicity; Geology; Library science; History; Seismology; Computer science","score_opus":0.035527117592799265,"score_gpt":0.23695950158745527,"score_spread":0.20143238399465602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394891429","genre_codex":"editorial","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010579504,0.0020259821,0.0011232258,0.092172734,0.8423841,0.00011962211,0.01901085,0.0013585058,0.040747017],"genre_scores_gemma":[0.03433367,0.011745944,0.0072078924,0.07951552,0.24865928,0.0005078389,0.039295137,0.006127728,0.572607],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99715483,0.00024810288,0.00041131472,0.00027623243,0.0017057272,0.00020369013],"domain_scores_gemma":[0.964766,0.005528262,0.0026451354,0.0022610482,0.023917282,0.00088221394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018644973,0.0010445461,0.0008356829,0.0035603698,0.0025823715,0.0030688285,0.0022064932,0.0025533973,0.1210641],"category_scores_gemma":[0.04649928,0.00059722946,0.00087900844,0.004740113,0.0011936476,0.0017352502,0.0016303834,0.0048679253,0.053658515],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010315255,0.0000016102647,0.00015110902,0.000047519505,0.0000021396331,0.000036795773,0.000020465677,0.000013271564,0.00003047252,0.00013853828,0.9967488,0.0027990027],"study_design_scores_gemma":[0.000022174052,0.0000118046955,0.0027580576,0.00042189824,0.000011344986,0.0001256954,0.0001531265,0.00006123235,0.00021747689,0.00033584522,0.99585766,0.000023755712],"about_ca_topic_score_codex":0.0550528,"about_ca_topic_score_gemma":0.0874445,"teacher_disagreement_score":0.9449472,"about_ca_system_score_codex":0.0033782064,"about_ca_system_score_gemma":0.0054897275,"threshold_uncertainty_score":0.40499973},"labels":[],"label_agreement":null},{"id":"W4395083238","doi":"10.22541/essoar.171288712.29849026/v1","title":"Pressure dependence of permeability in cracked rocks: experimental evidence of non-linear pore-pressure gradients from local measurements","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique; China Scholarship Council","keywords":"Permeability (electromagnetism); Micromechanics; Pore water pressure; Nonlinear system; Materials science; Pressure gradient; Mineralogy; Geology; Geotechnical engineering; Composite material; Chemistry; Physics","score_opus":0.05815511520747866,"score_gpt":0.29488543080719,"score_spread":0.23673031559971133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395083238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848178,0.00039137434,0.013694801,0.000051374365,0.0000058838536,0.000010545854,0.00015311538,0.0000932556,0.0007818277],"genre_scores_gemma":[0.9983748,0.00009965548,0.0013555019,0.0000048040815,0.0000025516376,0.0000058133655,0.000033851175,0.000011175993,0.00011182502],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997609,0.000022717953,0.000013174954,0.00006866099,0.000102799255,0.00003165053],"domain_scores_gemma":[0.999124,0.00045694975,0.00017431327,0.000108759195,0.000097985125,0.00003790337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017647923,0.00020851994,0.00025921015,0.00028229988,0.00018421213,0.00027339044,0.00040764947,0.00032096528,0.0009306734],"category_scores_gemma":[0.0013665024,0.00029794112,0.00006879213,0.00025209103,0.0009891994,0.0006596495,0.00047019584,0.0006527148,0.00014607566],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004222857,0.000010098571,0.0007594006,0.000067989706,0.0000031993432,0.000053118347,0.0000638968,0.00040229547,0.996951,0.00011536631,0.000014988492,0.0015163987],"study_design_scores_gemma":[0.000009360796,0.00009144603,0.018883608,0.0000059865283,0.0000069451035,0.00023307042,0.000044161876,0.0085412925,0.97171944,0.00024613907,0.00020672205,0.000011833865],"about_ca_topic_score_codex":0.00044093357,"about_ca_topic_score_gemma":0.00050716376,"teacher_disagreement_score":0.0009306734,"about_ca_system_score_codex":0.000120660225,"about_ca_system_score_gemma":0.00007493536,"threshold_uncertainty_score":0.003113389},"labels":[],"label_agreement":null},{"id":"W4395455662","doi":"10.1080/17499518.2024.2346656","title":"Probabilistic earthquake-tsunami financial risk evaluation for the District of Tofino, British Columbia, Canada","year":2024,"lang":"en","type":"article","venue":"Georisk Assessment and Management of Risk for Engineered Systems and Geohazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Probabilistic logic; Seismology; Geography; Finance; Geology; Business; Statistics; Mathematics","score_opus":0.00978993907265788,"score_gpt":0.22631272455758228,"score_spread":0.2165227854849244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395455662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9760448,0.0003968403,0.011202119,0.000524366,0.0000102504255,0.00015794102,0.0029951264,0.000103913175,0.008564715],"genre_scores_gemma":[0.9930184,0.00022101443,0.0017510321,0.00002010584,0.0000027424883,0.00003070453,0.0011245135,0.000012895511,0.0038187068],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99954516,0.00009431193,0.000019515337,0.00005190088,0.00016657518,0.00012250044],"domain_scores_gemma":[0.9988405,0.0003362045,0.00013223098,0.000047814996,0.00052675785,0.00011642654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007734214,0.00070651533,0.00038278513,0.0013254124,0.0007859984,0.0013607861,0.0010659838,0.00048181615,0.0022826695],"category_scores_gemma":[0.0032201966,0.00031779922,0.0003797129,0.0017221917,0.00043727687,0.00042402864,0.0006489414,0.00042451257,0.00015778223],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008510486,0.00004931597,0.050296545,0.000033040982,0.000061341474,0.00022985568,0.00006613028,0.93368125,0.0003400249,0.0027353966,0.0016741935,0.010747817],"study_design_scores_gemma":[0.000012451128,0.000024313904,0.027373781,0.000011510383,0.000025060413,0.000045866014,0.0002160999,0.9700804,0.00017132235,0.00090055884,0.0011176612,0.000021038843],"about_ca_topic_score_codex":0.9586655,"about_ca_topic_score_gemma":0.9531664,"teacher_disagreement_score":0.04133451,"about_ca_system_score_codex":0.019572746,"about_ca_system_score_gemma":0.013167519,"threshold_uncertainty_score":0.14201093},"labels":[],"label_agreement":null},{"id":"W4395675610","doi":"10.1029/2024jc020926","title":"The 2022 Tonga Tsunami on the Pacific and Atlantic Coasts of the Americas","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Oceans","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Geology; Volcano; Oceanography; Seismology; Pacific ocean; Tsunami wave; Tide gauge; Atmospheric wave; Wind wave; Climatology; Sea level; Wave propagation; Gravity wave","score_opus":0.037823960527622984,"score_gpt":0.3061081870297719,"score_spread":0.2682842265021489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395675610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938339,0.0003881702,0.00008935445,0.00018629264,0.000022033724,0.000013715355,0.0027553167,0.000009829819,0.0027013642],"genre_scores_gemma":[0.9957957,0.0004740492,0.0001573584,0.00006051555,0.000019993553,0.000014264811,0.0023120008,0.0000034481366,0.0011627461],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999201,0.0000071098016,0.00000781072,0.000014787916,0.000018771534,0.000031436044],"domain_scores_gemma":[0.99948007,0.000027436017,0.00018060001,0.000021473252,0.00017505955,0.000115368595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017129986,0.00021411608,0.00013564205,0.000825702,0.00040030683,0.0005667331,0.000116704025,0.00018478792,0.0016325986],"category_scores_gemma":[0.00050110003,0.00008337391,0.0002112455,0.001809806,0.00021955403,0.0002494555,0.00073055347,0.00022432716,0.00016433926],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003140386,0.000008260778,0.9901036,0.000042926895,0.000044716537,0.00032469258,0.0006292421,0.00023117922,0.001397362,0.000076835226,0.0010866736,0.006023101],"study_design_scores_gemma":[6.907327e-7,0.0000056545764,0.9979571,0.000006746061,0.000008101529,0.000027458502,0.0005236812,0.00011788348,0.000054063352,0.0000073546666,0.0012893295,0.0000018924046],"about_ca_topic_score_codex":0.20709802,"about_ca_topic_score_gemma":0.27961263,"teacher_disagreement_score":0.20709802,"about_ca_system_score_codex":0.0009768589,"about_ca_system_score_gemma":0.0008905886,"threshold_uncertainty_score":0.41178513},"labels":[],"label_agreement":null},{"id":"W4396660626","doi":"10.1038/s41561-024-01444-y","title":"Hydrothermal flow and serpentinization in oceanic core complexes controlled by mafic intrusions","year":2024,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Ocean Frontier Institute; National Science Foundation","keywords":"Geology; Mafic; Ultramafic rock; Hydrothermal circulation; Geochemistry; Lithology; Peridotite; Mantle (geology); Petrology; Lithosphere; Detachment fault; Geophysics; Tectonics; Seismology; Extensional definition","score_opus":0.007699528919952478,"score_gpt":0.22773404121325516,"score_spread":0.22003451229330268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396660626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996774,0.000010315269,0.00001258927,0.0000017048957,3.362993e-7,8.244069e-7,0.000012927861,0.0000012166006,0.00028271764],"genre_scores_gemma":[0.9997987,0.000009547512,0.000017969473,0.000001854527,6.592867e-7,0.0000011558391,0.000032976553,0.0000014831829,0.00013566132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999317,0.0000098711525,0.0000058761943,0.000021869599,0.000007675157,0.00002303262],"domain_scores_gemma":[0.9997377,0.000045493493,0.000083771,0.000016650758,0.000036801055,0.00007958586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010579505,0.0001194306,0.00020127151,0.00071472954,0.00044458057,0.0008179776,0.0002796788,0.0001558979,0.0013886212],"category_scores_gemma":[0.0005894279,0.00016117531,0.000100751655,0.00041353764,0.00066626054,0.0003504618,0.0006025063,0.0001567184,0.00013971199],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012408856,0.00007520316,0.87335616,0.000035650322,0.00008598314,0.00033157723,0.0030399784,0.0010429352,0.112355575,0.0009509152,0.00011933457,0.007365773],"study_design_scores_gemma":[0.000008786988,0.000036731253,0.99780613,0.000001865897,0.000007023545,0.0000426357,0.00040954657,0.0005160483,0.0009670901,0.00004554025,0.00015572246,0.0000029725443],"about_ca_topic_score_codex":0.021352278,"about_ca_topic_score_gemma":0.03127799,"teacher_disagreement_score":0.021352278,"about_ca_system_score_codex":0.0006267456,"about_ca_system_score_gemma":0.0003264476,"threshold_uncertainty_score":0.04245603},"labels":[],"label_agreement":null},{"id":"W4396696011","doi":"10.1038/s44304-024-00006-x","title":"Time-dependent probabilistic tsunami risk assessment: application to Tofino, British Columbia, Canada, subjected to Cascadia subduction earthquakes","year":2024,"lang":"en","type":"article","venue":"npj natural hazards.","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Subduction; Seismology; Geology; Probabilistic logic; Computer science; Tectonics","score_opus":0.003575002853140307,"score_gpt":0.20213485774727458,"score_spread":0.19855985489413427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396696011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94380844,0.00032334696,0.04349864,0.0006138482,0.000022638484,0.00014710933,0.001120597,0.00022468684,0.010240703],"genre_scores_gemma":[0.9902954,0.0002499968,0.0053061233,0.000020678839,0.000005393585,0.00003084672,0.00030971275,0.000018663504,0.0037632077],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984276,0.000033774322,0.0000071274585,0.000027151013,0.000043893397,0.000045238416],"domain_scores_gemma":[0.9995327,0.00014188484,0.00006482093,0.000017356138,0.00019191818,0.000051350245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044648562,0.00087020453,0.00033954822,0.00070015003,0.0008024803,0.0011138858,0.0013139873,0.0005805201,0.0013103585],"category_scores_gemma":[0.0015110321,0.00028591236,0.00042998962,0.00085365557,0.0004420358,0.0003534401,0.0006559707,0.00043244142,0.00011113812],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034633314,0.000028516148,0.013208289,0.00001731394,0.000028491957,0.00018644122,0.00008929455,0.9759991,0.00042721594,0.001654779,0.0005358583,0.0077901264],"study_design_scores_gemma":[0.00000631654,0.0000202206,0.005769924,0.0000051874763,0.000015246187,0.000040103278,0.00014851076,0.99264455,0.00014952234,0.000726408,0.0004576422,0.000016296157],"about_ca_topic_score_codex":0.92104447,"about_ca_topic_score_gemma":0.88695955,"teacher_disagreement_score":0.07895553,"about_ca_system_score_codex":0.009824038,"about_ca_system_score_gemma":0.00761971,"threshold_uncertainty_score":0.15884095},"labels":[],"label_agreement":null},{"id":"W4396704540","doi":"10.59429/ear.v2i1.1880","title":"Magnetogravimetric study on the Scotia Plate, in the South Atlantic Ocean for the characterization of tsunamis","year":2024,"lang":"en","type":"article","venue":"Earthquake","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Nova scotia; Geology; Geography","score_opus":0.02619976869716699,"score_gpt":0.2317605627982793,"score_spread":0.20556079410111233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396704540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99584347,0.00015034333,0.00053426175,0.000036136462,0.000008741173,0.000015240847,0.0008861506,0.000018623112,0.0025070452],"genre_scores_gemma":[0.99779594,0.000107568754,0.00066931266,0.000012089396,0.0000058622454,0.000003411867,0.00063207163,0.0000035650032,0.00077013654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000029119437,0.0000026599353,0.000009736026,0.000016667458,0.000010819473],"domain_scores_gemma":[0.9998913,0.0000061528312,0.00002377839,0.000007719477,0.00005356872,0.000017601626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000089917914,0.00023159101,0.000093497445,0.0010632626,0.00027372612,0.0002686488,0.00010522679,0.000115313094,0.00058674667],"category_scores_gemma":[0.0001587438,0.00009145222,0.00015113904,0.0011706856,0.00013871111,0.00009856909,0.00020372415,0.00009815629,0.00016390297],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016108595,0.000044440385,0.89889264,0.00006145443,0.00006038241,0.0010219194,0.00051946763,0.0040108175,0.0713535,0.00022583782,0.0010485791,0.02259977],"study_design_scores_gemma":[0.0000025892477,0.000013370119,0.9968771,0.0000037117036,0.0000073524125,0.00006875712,0.00021547309,0.0016308976,0.000638399,0.000009160974,0.0005307019,0.0000024330714],"about_ca_topic_score_codex":0.260341,"about_ca_topic_score_gemma":0.4628116,"teacher_disagreement_score":0.260341,"about_ca_system_score_codex":0.00039757622,"about_ca_system_score_gemma":0.0006690951,"threshold_uncertainty_score":0.51765126},"labels":[],"label_agreement":null},{"id":"W4398205129","doi":"10.1029/2024jb028752","title":"Incipient Subduction and Slip Partitioning at High Obliquity: The Haida Gwaii Plate Boundary","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Geological Survey of Canada; Natural Resources Canada; University of Victoria; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Subduction; Geology; Seismology; Slip (aerodynamics); Plate tectonics; Engineering; Aerospace engineering; Tectonics","score_opus":0.04314574524424953,"score_gpt":0.316515748697,"score_spread":0.2733700034527505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398205129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99889934,0.000024611802,0.000060122547,0.00002430962,0.0000021258531,0.000004162147,0.000118659314,0.0000064334763,0.00086024473],"genre_scores_gemma":[0.99941194,0.000015496731,0.000089179906,0.000005964389,0.0000018991202,0.0000030064714,0.000208498,0.0000022936267,0.00026163433],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993503,0.0000035762591,0.0000035480596,0.00001900095,0.000018642968,0.000020215186],"domain_scores_gemma":[0.99976736,0.000017596589,0.00007356952,0.00001988171,0.0000547234,0.00006697438],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097879354,0.00021463445,0.00020470805,0.0010802227,0.00059608044,0.0007158765,0.0002052782,0.00027546185,0.0010647253],"category_scores_gemma":[0.00040952762,0.00021611544,0.00012277487,0.0010794053,0.0006152584,0.0002949155,0.00065876084,0.00026327296,0.00016522275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011865353,0.00002812364,0.97616553,0.00003231848,0.000034538083,0.000999752,0.0013380642,0.002163062,0.009624369,0.00026771415,0.0006114078,0.008616367],"study_design_scores_gemma":[0.0000035353262,0.000007439539,0.9975967,0.0000054637585,0.0000055101154,0.000057878027,0.0003899897,0.0014036591,0.00021284432,0.000038699854,0.00027423297,0.000004121961],"about_ca_topic_score_codex":0.11173217,"about_ca_topic_score_gemma":0.21426784,"teacher_disagreement_score":0.8882678,"about_ca_system_score_codex":0.0010134942,"about_ca_system_score_gemma":0.0007556277,"threshold_uncertainty_score":0.22216368},"labels":[],"label_agreement":null},{"id":"W4398254121","doi":"10.1029/2023tc008140","title":"Earthquake Relocations Delineate a Discrete Fault Network and Deformation Corridor Throughout Southeast Alaska and Southwest Yukon","year":2024,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Yukon University; Geological Survey of Canada; Natural Resources Canada; University of Calgary","funders":"","keywords":"Geology; Seismology; Fault (geology); Deformation (meteorology); Geomorphology; Oceanography","score_opus":0.015153343234071354,"score_gpt":0.2377448734361907,"score_spread":0.22259153020211933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398254121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956304,0.000017584422,0.00003193013,0.0000051406364,2.7579617e-7,0.0000020319446,0.00015713816,0.000003079302,0.00021966876],"genre_scores_gemma":[0.9993606,0.000025864827,0.000099484736,0.0000033138595,2.3622621e-7,0.0000034848117,0.00032937137,7.2494396e-7,0.00017695877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999002,0.000009081626,0.000014995819,0.00004037196,0.000014769357,0.000020561089],"domain_scores_gemma":[0.9996338,0.000042665186,0.00014002736,0.000030345604,0.000097357966,0.000055865334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012770802,0.0001010824,0.00011889053,0.0010622016,0.00044779322,0.0004585618,0.00019326273,0.00017613058,0.00077497883],"category_scores_gemma":[0.00042413577,0.00010362847,0.00010692539,0.0013540605,0.00034083123,0.00024568973,0.0005362488,0.00008102093,0.00011718701],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003381125,0.000013238011,0.98812056,0.000017096023,0.000019884268,0.00014965418,0.0010558955,0.00079710886,0.0028641238,0.00013299935,0.00011563088,0.0066799694],"study_design_scores_gemma":[0.0000015173523,0.000011027614,0.99786866,0.0000071273817,0.000005811787,0.00005532121,0.0012529306,0.0004110071,0.000119511365,0.000027398313,0.00023691701,0.000002660853],"about_ca_topic_score_codex":0.13039961,"about_ca_topic_score_gemma":0.3385112,"teacher_disagreement_score":0.8696004,"about_ca_system_score_codex":0.00078334025,"about_ca_system_score_gemma":0.00074030703,"threshold_uncertainty_score":0.25928122},"labels":[],"label_agreement":null},{"id":"W4398767222","doi":"10.1029/2023jf007444","title":"Testing Megathrust Rupture Models Using Tsunami Deposits","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Earth Surface","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Seismology; Forensic engineering; Engineering","score_opus":0.12733425803226014,"score_gpt":0.34083279677951867,"score_spread":0.21349853874725852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398767222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99688333,0.00004640887,0.0016276053,0.000099893114,0.0000148595,0.000020854954,0.00029499712,0.00011784561,0.00089424563],"genre_scores_gemma":[0.9978028,0.000027303468,0.0015717037,0.000019152345,0.000006939815,0.000016919159,0.00030450203,0.00001631405,0.00023449313],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9992888,0.00025652145,0.000055570115,0.00020725002,0.000091692265,0.00010016892],"domain_scores_gemma":[0.99112684,0.0067602247,0.00068153447,0.00028806773,0.00057492685,0.0005684073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025418592,0.0012881261,0.0006827325,0.0011364049,0.0006762913,0.0015595091,0.002211981,0.0019080762,0.00223293],"category_scores_gemma":[0.008972487,0.000971571,0.001354401,0.00058528024,0.0006900438,0.0013062796,0.0008422301,0.00090917293,0.00038730993],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016746353,0.00019494258,0.030144623,0.000015027311,0.00009796618,0.00006687974,0.00003016953,0.96697235,0.0002520623,0.00035244203,0.00015925655,0.0015467696],"study_design_scores_gemma":[0.000032216805,0.000057521524,0.0013987558,0.000003100236,0.000012623866,0.000008144946,0.000026068876,0.9980956,0.00016810067,0.00014625942,0.00004691977,0.0000047429194],"about_ca_topic_score_codex":0.055099163,"about_ca_topic_score_gemma":0.022127822,"teacher_disagreement_score":0.055099163,"about_ca_system_score_codex":0.0022024948,"about_ca_system_score_gemma":0.001592694,"threshold_uncertainty_score":0.10955691},"labels":[],"label_agreement":null},{"id":"W4399073695","doi":"10.1130/ges02722.1","title":"Geological fingerprints of deep slow earthquakes: A review of field constraints and directions for future research","year":2024,"lang":"en","type":"review","venue":"Geosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University; Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK; Southern California Earthquake Center; National Science Foundation","keywords":"Geology; Seismology; Field (mathematics); Mining engineering","score_opus":0.07098498125472136,"score_gpt":0.3564663336069379,"score_spread":0.28548135235221656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399073695","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00044069227,0.99781764,0.00029446033,0.0008067001,0.00011181518,0.000009227101,0.00008289713,0.000009088467,0.0004274979],"genre_scores_gemma":[0.0028660216,0.995626,0.0006340338,0.00034519046,0.00027829647,0.00001790564,0.000114754286,0.000004689636,0.00011310584],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99874085,0.0002705773,0.00029090702,0.00038738566,0.00023822024,0.00007208843],"domain_scores_gemma":[0.986317,0.008875662,0.0014435027,0.00035202602,0.002570195,0.00044174446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006319971,0.0011231755,0.0028904204,0.009997916,0.0006361039,0.0029799629,0.0025290258,0.001763866,0.00337119],"category_scores_gemma":[0.0108166225,0.0009729202,0.0009287286,0.009169112,0.0029809987,0.0048676943,0.0016380419,0.0018117763,0.0009841073],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016386592,0.00007850474,0.009889408,0.027444348,0.0002409948,0.0003241445,0.00040535335,0.00042175775,0.0006656409,0.006013611,0.015715765,0.9386368],"study_design_scores_gemma":[0.00005648337,0.00055588695,0.06802655,0.08076196,0.0013007696,0.0059832544,0.0027362253,0.0010070705,0.00090076536,0.016590573,0.8217822,0.00029831612],"about_ca_topic_score_codex":0.0074558114,"about_ca_topic_score_gemma":0.0077596516,"teacher_disagreement_score":0.009997916,"about_ca_system_score_codex":0.001995894,"about_ca_system_score_gemma":0.0034588496,"threshold_uncertainty_score":0.033423603},"labels":[],"label_agreement":null},{"id":"W4399104346","doi":"10.22541/essoar.171691108.86550630/v1","title":"Variations in Reflection Signature and Slip Behavior of the Subduction Interface Offshore Alaska Peninsula From 152º to 161º W","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Seismology; Slip (aerodynamics); Subduction; Submarine pipeline; Reflection (computer programming); Slipping; Asperity (geotechnical engineering); Homogeneous; Geotechnical engineering; Geometry; Tectonics","score_opus":0.02053519386689041,"score_gpt":0.2611563846532187,"score_spread":0.24062119078632832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399104346","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900985,0.000027744722,0.00004520427,0.0000041789194,0.0000010163523,0.0000012828001,0.00020184035,0.000009724602,0.0006991499],"genre_scores_gemma":[0.9992021,0.000034937537,0.00009468557,0.000002143096,0.0000010682855,0.0000020127898,0.00026592985,0.0000020226921,0.00039517862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999967,0.000001967935,0.0000032057821,0.0000125708875,0.000007783594,0.0000075433345],"domain_scores_gemma":[0.9998839,0.000009731543,0.000043141867,0.000007460636,0.00003588794,0.000019844414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007582337,0.00018135582,0.00009307534,0.0007388076,0.00017468286,0.00028131998,0.00012893259,0.00016926286,0.0012067581],"category_scores_gemma":[0.00022343107,0.00013231157,0.00011043465,0.00046288365,0.00015982961,0.00016723046,0.00023431449,0.00011147596,0.00022686637],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018122698,0.000031734744,0.9457528,0.000032165433,0.000055381803,0.0003905963,0.0011344183,0.0013634289,0.037726767,0.00006414833,0.00026011062,0.013007238],"study_design_scores_gemma":[5.659303e-7,0.000009249552,0.999131,0.0000024043334,0.00000408778,0.000024424187,0.00021286878,0.00020925881,0.00029899966,0.0000034934171,0.00010210372,0.0000016423518],"about_ca_topic_score_codex":0.023366483,"about_ca_topic_score_gemma":0.03736349,"teacher_disagreement_score":0.023366483,"about_ca_system_score_codex":0.0001707521,"about_ca_system_score_gemma":0.0001234586,"threshold_uncertainty_score":0.046460927},"labels":[],"label_agreement":null},{"id":"W4399263908","doi":"10.1029/2024gc011493","title":"Influence of Farallon Slab Loading on Intraplate Stress and Seismicity in Eastern North America in the Presence of Pre‐Existing Weak Zones","year":2024,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Intraplate earthquake; Induced seismicity; Seismology; Geology; Slab; Stress (linguistics); Geophysics; Tectonics","score_opus":0.012094823862156401,"score_gpt":0.220715963681084,"score_spread":0.2086211398189276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399263908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998073,0.000010308328,0.00002049698,0.000009196202,3.5067552e-7,4.3316157e-7,0.000020398076,0.0000028549211,0.00012868029],"genre_scores_gemma":[0.99989545,0.0000072322146,0.000023768423,0.0000022725205,4.3789797e-7,4.8341724e-7,0.000029494027,8.8445756e-7,0.00003996182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999194,0.000016223892,0.000004947143,0.000023217963,0.000012017221,0.000024069343],"domain_scores_gemma":[0.9996916,0.000088960536,0.000085744214,0.000025251005,0.000035524452,0.000073022245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017601642,0.0003431215,0.00019190556,0.00043764428,0.00027921094,0.0006591927,0.0003379459,0.00034865012,0.0011113357],"category_scores_gemma":[0.0006756136,0.0002006346,0.00020765112,0.00026359118,0.0005999583,0.00035913166,0.00050536357,0.00017204811,0.00006658235],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041515846,0.0001028402,0.9348005,0.000038027403,0.00012925181,0.0005547183,0.0003378077,0.035919055,0.022694997,0.0003439171,0.00016062376,0.0045032077],"study_design_scores_gemma":[0.000022749566,0.000078256955,0.9526293,0.000008265712,0.00005883021,0.000060738963,0.0005449715,0.04451496,0.0017175557,0.00014824355,0.00020006133,0.00001592164],"about_ca_topic_score_codex":0.048013337,"about_ca_topic_score_gemma":0.07209826,"teacher_disagreement_score":0.048013337,"about_ca_system_score_codex":0.00078109774,"about_ca_system_score_gemma":0.00031663518,"threshold_uncertainty_score":0.095467746},"labels":[],"label_agreement":null},{"id":"W4399318847","doi":"10.1007/s10950-024-10225-4","title":"Investigation of the discrepancy in the earthquake magnitude values reported by different agencies in the Western Canada Sedimentary basin","year":2024,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Structural geology; Geology; Magnitude (astronomy); Seismology; Sedimentary rock; Structural basin; Hydrogeology; Earthquake magnitude; Sedimentary basin; Paleontology; Tectonics; Geometry; Geotechnical engineering; Physics","score_opus":0.02158513846207391,"score_gpt":0.222648582310009,"score_spread":0.2010634438479351,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399318847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99329925,0.00039463522,0.00015476976,0.00043599313,0.000008165688,0.000018621009,0.00087234477,0.000006205159,0.0048101083],"genre_scores_gemma":[0.99797624,0.00028351686,0.00030896184,0.00007854747,0.000005444704,0.0000075930443,0.00043293484,0.000004607132,0.0009021725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9983796,0.00027242905,0.00017361704,0.00014294333,0.00069253234,0.00033879583],"domain_scores_gemma":[0.9917686,0.0013251832,0.0011351957,0.00017227327,0.0051156916,0.00048294684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015064965,0.00017501797,0.00019154725,0.0053954753,0.0020160587,0.0016685614,0.00088250084,0.0002995455,0.000921946],"category_scores_gemma":[0.0075387703,0.00021717926,0.00015655438,0.0078088176,0.0014051615,0.0003712382,0.0010792526,0.0004056074,0.00012140695],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096877775,0.000020390285,0.9797808,0.00006429965,0.000059489073,0.00019062354,0.006139268,0.00021492167,0.0012379576,0.00054014946,0.0005360873,0.011119005],"study_design_scores_gemma":[0.000002109213,0.000005703964,0.9943989,0.000017410655,0.000010596948,0.00003353726,0.0043292223,0.00011286361,0.0001429294,0.000021265823,0.00092156575,0.0000038318312],"about_ca_topic_score_codex":0.98377925,"about_ca_topic_score_gemma":0.9957676,"teacher_disagreement_score":0.016247215,"about_ca_system_score_codex":0.016247215,"about_ca_system_score_gemma":0.019888142,"threshold_uncertainty_score":0.11788231},"labels":[],"label_agreement":null},{"id":"W4399425542","doi":"10.1126/sciadv.adl3198","title":"Subducting plate structure and megathrust morphology from deep seismic imaging linked to earthquake rupture segmentation at Cascadia","year":2024,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Subduction; Seismology; Plate tectonics; Intraplate earthquake; Pacific Plate; Episodic tremor and slip; Earthquake rupture; Slip (aerodynamics); Lithology; Fault (geology); Paleontology; Tectonics","score_opus":0.00921464567213999,"score_gpt":0.2443097845368322,"score_spread":0.2350951388646922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399425542","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983529,0.00006282346,0.00015226254,0.000025545558,0.0000012413377,0.0000028768889,0.00037154657,0.0000254172,0.0010055838],"genre_scores_gemma":[0.99897265,0.00005895466,0.00018664882,0.0000054440106,9.58676e-7,0.000002588196,0.00052558776,0.0000044872013,0.00024274002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999087,0.000006220399,0.0000060657085,0.000034434655,0.00002290666,0.000021651074],"domain_scores_gemma":[0.99972254,0.000018547722,0.000095619056,0.000027266584,0.00006628065,0.000069806374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013175335,0.0002534602,0.00014183173,0.0012898367,0.00030478672,0.00051871047,0.0001664687,0.00021253465,0.00092093163],"category_scores_gemma":[0.00043484705,0.00019320211,0.00014791799,0.00097068143,0.0003214828,0.00017245133,0.000533747,0.00024064699,0.00017080616],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011010343,0.000034679066,0.9354166,0.000056000063,0.00005568054,0.000403221,0.0012438389,0.0017928097,0.050230388,0.000115324365,0.00038825546,0.010153138],"study_design_scores_gemma":[8.5240146e-7,0.000005415592,0.9989812,0.0000037422349,0.0000045208035,0.000036438945,0.00016886888,0.0003301141,0.00032346524,0.000016019723,0.00012712972,0.0000022638005],"about_ca_topic_score_codex":0.05025212,"about_ca_topic_score_gemma":0.14641903,"teacher_disagreement_score":0.05025212,"about_ca_system_score_codex":0.0006725772,"about_ca_system_score_gemma":0.00042131337,"threshold_uncertainty_score":0.0999192},"labels":[],"label_agreement":null},{"id":"W4399712285","doi":"10.3208/jgssp.v10.os-33-06","title":"Site effects observed in Antakya after the M&lt;sub&gt;W&lt;/sub&gt; 7.7 Pazarcik and M&lt;sub&gt;W&lt;/sub&gt; 7.6 Elbistan Earthquakes on the 6&lt;sup&gt;th &lt;/sup&gt;February 2023 (Türkiye)","year":2024,"lang":"en","type":"article","venue":"Japanese Geotechnical Society Special Publication","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"Geotechnical engineering; Geology; Seismology; Chemistry","score_opus":0.01376996363083624,"score_gpt":0.2114649015468172,"score_spread":0.19769493791598097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399712285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99936134,0.000027577551,0.00001589051,0.000012304262,0.0000031811705,0.000004346076,0.0001069563,0.0000038085757,0.00046456774],"genre_scores_gemma":[0.9992242,0.000056359324,0.000043969565,0.000009907121,0.0000032862865,0.0000075552343,0.00032227428,0.0000024259837,0.00032999794],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998771,0.00001269817,0.000011884701,0.000028050677,0.000024639206,0.000045543686],"domain_scores_gemma":[0.9996917,0.0000312869,0.00013034606,0.000022541344,0.00006407398,0.000059969225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010345617,0.00018309873,0.00026819247,0.00057112164,0.00056005194,0.00051572046,0.00028794107,0.0003658182,0.0008428094],"category_scores_gemma":[0.0002918669,0.00014307203,0.00019387697,0.00085697585,0.000590577,0.00016181158,0.0005837982,0.0003580333,0.00016922623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017771232,0.00027207803,0.9067458,0.00021344493,0.0002164104,0.009740368,0.0050469055,0.0024254122,0.05141296,0.00018938795,0.001143772,0.020816412],"study_design_scores_gemma":[0.0000050901153,0.000057335117,0.9979942,0.000003804733,0.000012303376,0.00017027963,0.0007990819,0.00011447635,0.00044139635,0.0000075463436,0.00038943955,0.000005190475],"about_ca_topic_score_codex":0.026884971,"about_ca_topic_score_gemma":0.08709584,"teacher_disagreement_score":0.026884971,"about_ca_system_score_codex":0.00056997605,"about_ca_system_score_gemma":0.00048425555,"threshold_uncertainty_score":0.053456962},"labels":[],"label_agreement":null},{"id":"W4399839918","doi":"10.1016/j.epsl.2024.118849","title":"Systematic observation of a seismic back-front during fluid injection in both natural and anthropogenic earthquake swarms","year":2024,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Agence Nationale de la Recherche","keywords":"Geology; Seismology; Front (military); Natural (archaeology); Paleontology; Oceanography","score_opus":0.009706268368433099,"score_gpt":0.19623618303061735,"score_spread":0.18652991466218424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399839918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948484,0.000107513755,0.0014382076,0.000051088933,0.00003361677,0.000018218057,0.0004165141,0.000064700944,0.003021827],"genre_scores_gemma":[0.99833053,0.000044451128,0.0005363479,0.00001783329,0.00001637352,0.000007084912,0.00031622808,0.00001018663,0.00072097144],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999946,0.0000043694167,0.0000036090119,0.000014148852,0.000015208743,0.000016662902],"domain_scores_gemma":[0.99961215,0.000047321424,0.000126921,0.000034939883,0.00008944779,0.00008923878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012009513,0.00016660496,0.00016137352,0.0008611308,0.00035074208,0.00032691073,0.00019416056,0.00035685103,0.0013476792],"category_scores_gemma":[0.00063850614,0.00015894402,0.00013167785,0.00050903036,0.00025697338,0.00017719383,0.000543291,0.0003557254,0.00035084173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012696502,0.0002291977,0.6290832,0.00015689724,0.00008674006,0.0012816123,0.0019134842,0.0013015352,0.32301772,0.00045094168,0.0016308004,0.03957819],"study_design_scores_gemma":[0.000008789162,0.00012227676,0.9935545,0.00001603905,0.000016166052,0.00018147894,0.00024379497,0.0010957276,0.0036804976,0.000041275827,0.0010320562,0.0000074711684],"about_ca_topic_score_codex":0.0024785767,"about_ca_topic_score_gemma":0.0064310175,"teacher_disagreement_score":0.0024785767,"about_ca_system_score_codex":0.00014568701,"about_ca_system_score_gemma":0.00019393631,"threshold_uncertainty_score":0.0049283504},"labels":[],"label_agreement":null},{"id":"W4399981130","doi":"10.1098/rsta.2023.0418","title":"Sealing faults and fluid-induced seismicity","year":2024,"lang":"en","type":"article","venue":"Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Pore water pressure; Fault (geology); Permeability (electromagnetism); Hydraulic fracturing; Petrology; Fluid pressure; Slip (aerodynamics); Geotechnical engineering; Seismology; Mechanics; Engineering","score_opus":0.023055762219744508,"score_gpt":0.22972704114358256,"score_spread":0.20667127892383805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399981130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99829525,0.00006190337,0.0010782107,0.000018542767,0.0000017066203,0.0000021705885,0.000047474554,0.000018071658,0.00047672843],"genre_scores_gemma":[0.99982065,0.00002200184,0.000085429834,0.0000013572035,8.125855e-7,5.5316355e-7,0.000021222095,0.000001457759,0.000046489316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991584,0.000012739297,0.0000072436405,0.00001963816,0.000019947283,0.000024630737],"domain_scores_gemma":[0.9996263,0.00008571989,0.00017364032,0.00002890632,0.000045583576,0.00003978483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008789279,0.0001318373,0.00012372907,0.00042536302,0.0001614226,0.00035668525,0.0002208631,0.00025377478,0.00083308545],"category_scores_gemma":[0.0010216783,0.00012046433,0.00011968939,0.00039529434,0.0005543903,0.0002969755,0.0003528232,0.0001920097,0.00005049984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032517168,0.000100244346,0.752181,0.0001472148,0.00014056153,0.0008551358,0.00071814854,0.14071193,0.0827976,0.0034471226,0.0002537255,0.01832222],"study_design_scores_gemma":[0.000012531609,0.00010874269,0.8835663,0.000012173791,0.00003134927,0.00018632828,0.0003931577,0.10721203,0.0064283963,0.0014313395,0.0005957065,0.000021781667],"about_ca_topic_score_codex":0.02618053,"about_ca_topic_score_gemma":0.02427469,"teacher_disagreement_score":0.02618053,"about_ca_system_score_codex":0.0009814757,"about_ca_system_score_gemma":0.00045181383,"threshold_uncertainty_score":0.052056313},"labels":[],"label_agreement":null},{"id":"W4400001980","doi":"10.1190/int-2024-0624-spseintro.1","title":"Introduction to special section: Induced seismicity","year":2024,"lang":"en","type":"article","venue":"Interpretation","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Section (typography); Special section; Geology; Seismology; Computer science; Physics; Engineering physics; Operating system","score_opus":0.0121172137143915,"score_gpt":0.23479908182146575,"score_spread":0.22268186810707424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400001980","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013902565,0.016431743,0.0038042767,0.03806946,0.82051164,0.00044958625,0.0036234858,0.0008918982,0.11482768],"genre_scores_gemma":[0.007887658,0.0331827,0.0021434363,0.02787796,0.7029111,0.00034098653,0.005402883,0.00084545946,0.21940793],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987625,0.00015596287,0.00019781341,0.00028959988,0.00045332673,0.0001409776],"domain_scores_gemma":[0.99405813,0.0013755413,0.000573348,0.0002727658,0.002602865,0.0011173345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015394225,0.0016871812,0.0012445464,0.002716848,0.0013541173,0.0035605545,0.0017705499,0.0041434234,0.15330204],"category_scores_gemma":[0.0060796915,0.00044017704,0.0008292079,0.0016864922,0.0008493901,0.0026823196,0.002006836,0.0029198814,0.09080675],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022995475,0.000030389421,0.000308806,0.0003093218,0.0000032168705,0.00008417003,0.000030178533,0.00005744459,0.00032688194,0.001083012,0.96730596,0.03043762],"study_design_scores_gemma":[0.00000567533,0.000044345834,0.0010621925,0.00023651033,0.0000036012823,0.00018097009,0.000045449582,0.000054450677,0.00010419121,0.0007796595,0.99747616,0.000006867661],"about_ca_topic_score_codex":0.0017519081,"about_ca_topic_score_gemma":0.002555917,"teacher_disagreement_score":0.15330204,"about_ca_system_score_codex":0.000923588,"about_ca_system_score_gemma":0.0018653494,"threshold_uncertainty_score":0.51284647},"labels":[],"label_agreement":null},{"id":"W4400009355","doi":"10.20884/1.jtf.2023.6.2.8370","title":"","year":2023,"lang":"","type":"article","venue":"Jurnal Teras Fisika","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"WiLAN (Canada)","funders":"","keywords":"Computer science","score_opus":0.03414638837274409,"score_gpt":0.25124989477779963,"score_spread":0.21710350640505555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400009355","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9242045,0.000108981825,0.0012272915,0.00038060205,0.00018464855,0.0003306564,0.009583001,0.00033437446,0.06364595],"genre_scores_gemma":[0.89391667,0.00018984587,0.0017862208,0.00021156187,0.00006107252,0.00015203073,0.017053407,0.00004954362,0.086579695],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9999281,0.000004840445,0.0000058677397,0.000015099102,0.000019796676,0.000026313994],"domain_scores_gemma":[0.99990034,0.0000054918874,0.00001227067,0.000012839944,0.00003252848,0.000036530186],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00009490059,0.0003005046,0.00018846526,0.0005163968,0.00081832416,0.00026829145,0.00019636474,0.00026055358,0.017455842],"category_scores_gemma":[0.0002531344,0.00009251089,0.00012945135,0.0008902077,0.00013325587,0.00017056952,0.00064728665,0.00027842887,0.003912305],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013382372,0.0008485708,0.5202913,0.000661606,0.00013224263,0.019385295,0.009876783,0.0008634411,0.096443005,0.0055357153,0.06908519,0.27553868],"study_design_scores_gemma":[0.000037220976,0.00032322007,0.88507855,0.000039157676,0.00003152709,0.0025400482,0.0025449086,0.00077781605,0.0033351849,0.00040288735,0.10486402,0.00002544309],"about_ca_topic_score_codex":0.008017346,"about_ca_topic_score_gemma":0.042766556,"teacher_disagreement_score":0.9825442,"about_ca_system_score_codex":0.00037024572,"about_ca_system_score_gemma":0.000632683,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4400225667","doi":"10.26443/seismica.v2i4.1177","title":"Forearc faults in northern Cascadia do not accommodate elastic strain driven by the megathrust seismic cycle","year":2024,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Centre National d’Etudes Spatiales; National Science Foundation","keywords":"Forearc; Geology; Seismology; Strain (injury); Subduction; Tectonics; Medicine; Anatomy","score_opus":0.011813055607519381,"score_gpt":0.22284257562718446,"score_spread":0.21102952001966507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400225667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884438,0.00007798737,0.0043024346,0.0003143167,0.000010932973,0.000010899691,0.0002514179,0.00022556003,0.006362638],"genre_scores_gemma":[0.9982469,0.000057634526,0.0007180758,0.00001987824,0.0000035299436,0.000010586573,0.00010533656,0.000017987377,0.0008201172],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998852,0.000025111935,0.0000068930635,0.000035498208,0.000017378561,0.0000298932],"domain_scores_gemma":[0.9996697,0.00007768405,0.00008861304,0.000045973284,0.00004029519,0.00007777093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019631065,0.0005381608,0.0004632425,0.00043131894,0.0006743168,0.00095052796,0.00094011443,0.0011733857,0.0022817934],"category_scores_gemma":[0.0013776079,0.00047941852,0.00057548896,0.00047850932,0.0006207316,0.0005688499,0.00061194337,0.0004928213,0.00027553775],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002969695,0.00003085601,0.025017392,0.00002070652,0.00003682883,0.00013262116,0.0000683736,0.97119945,0.0012125765,0.0009895279,0.000117167314,0.0011448167],"study_design_scores_gemma":[0.00002391348,0.00003174348,0.017497856,0.00000839358,0.00002055154,0.000031365642,0.00007825211,0.9809569,0.00017650874,0.0006997503,0.000463601,0.000011110581],"about_ca_topic_score_codex":0.1491864,"about_ca_topic_score_gemma":0.14139159,"teacher_disagreement_score":0.1491864,"about_ca_system_score_codex":0.0022360214,"about_ca_system_score_gemma":0.0018996918,"threshold_uncertainty_score":0.2966361},"labels":[],"label_agreement":null},{"id":"W4400432819","doi":"10.1093/gji/ggae236","title":"Leveraging the ETAS model to forecast mining microseismicity","year":2024,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology","score_opus":0.03650233478653986,"score_gpt":0.26248297396789544,"score_spread":0.22598063918135558,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400432819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86004466,0.00016297415,0.13310552,0.00043347556,0.00004397791,0.000057309728,0.00080847304,0.00030092426,0.0050427294],"genre_scores_gemma":[0.9954873,0.00005015816,0.003055741,0.000013557428,0.0000058448013,0.000017375989,0.00019616786,0.000007497519,0.0011662723],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999876,0.00002948465,0.000009214218,0.000034291665,0.000023771792,0.000027277247],"domain_scores_gemma":[0.9991449,0.00049705367,0.00014610382,0.000029960795,0.00013687198,0.00004508302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061273127,0.00044438927,0.0004726181,0.0005197015,0.00025454853,0.0009365955,0.0008244244,0.00086862844,0.0013325828],"category_scores_gemma":[0.001880567,0.00031954216,0.0004747253,0.00045035017,0.00036764177,0.0004738105,0.00041894862,0.00089081476,0.00020691335],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012482162,0.0000040547766,0.0011499326,0.0000024292551,0.0000056748436,0.000017709997,0.000004403724,0.9975466,0.00014022921,0.00039453933,0.000036263948,0.00068559445],"study_design_scores_gemma":[7.692688e-7,0.000001925008,0.0001899336,7.263785e-7,0.0000011400674,0.0000017678634,0.0000020951236,0.9996189,0.00002923814,0.00013264712,0.00001958033,0.0000012445546],"about_ca_topic_score_codex":0.095629156,"about_ca_topic_score_gemma":0.045651518,"teacher_disagreement_score":0.095629156,"about_ca_system_score_codex":0.00091637875,"about_ca_system_score_gemma":0.0011194566,"threshold_uncertainty_score":0.19014508},"labels":[],"label_agreement":null},{"id":"W4400458220","doi":"10.1680/978-1-83549-560-520241012","title":"Seismic Design for Buildings","year":2024,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"","keywords":"Architectural engineering; Geology; Engineering","score_opus":0.040343791459492594,"score_gpt":0.22511928544958332,"score_spread":0.18477549399009072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400458220","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0021613704,0.022403924,0.09869283,0.0017821268,0.0013290723,0.00009050818,0.00035751064,0.000651989,0.87253064],"genre_scores_gemma":[0.052700114,0.024564007,0.08822593,0.00108282,0.0009106956,0.00023119045,0.00069504726,0.0006201231,0.83097],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.999728,0.00007353318,0.000010833737,0.00004059385,0.00012923183,0.000017827268],"domain_scores_gemma":[0.99990785,0.00002499514,0.000006019797,0.000014796538,0.000038300725,0.000008027143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023779416,0.0010539683,0.00033373886,0.00048985175,0.00081664236,0.0016426117,0.00054590043,0.0009363596,0.039102115],"category_scores_gemma":[0.00051233603,0.00025361465,0.000274973,0.0006576048,0.0010332774,0.0012416578,0.00092456833,0.0010181813,0.016902264],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011563121,0.000015522739,0.00007834366,0.0003517645,0.000005324149,0.000062374944,0.00045485084,0.00435826,0.0016680394,0.7416059,0.10325752,0.14813049],"study_design_scores_gemma":[0.0000022126617,0.000014792348,0.00007397318,0.000091887865,0.0000023896212,0.0001279747,0.00007568407,0.001012218,0.00024055217,0.07567912,0.92267495,0.000004189279],"about_ca_topic_score_codex":0.0010506025,"about_ca_topic_score_gemma":0.0018112824,"teacher_disagreement_score":0.039102115,"about_ca_system_score_codex":0.0011689367,"about_ca_system_score_gemma":0.0005669041,"threshold_uncertainty_score":0.1308096},"labels":[],"label_agreement":null},{"id":"W4400458407","doi":"10.1680/978-1-83549-560-520241007","title":"Movement and Tolerances","year":2024,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"","keywords":"Movement (music); Computer science; Art; Aesthetics","score_opus":0.017307568627993035,"score_gpt":0.19928350027761213,"score_spread":0.1819759316496191,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400458407","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01609427,0.01157063,0.065455414,0.0025369148,0.0012899959,0.00006522996,0.00023613135,0.00042999373,0.9023214],"genre_scores_gemma":[0.4041399,0.015082698,0.038099475,0.001105551,0.0010980214,0.00018850973,0.00044478584,0.00087167596,0.5389694],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99883336,0.00014322765,0.00006340649,0.0002799016,0.000579754,0.00010030141],"domain_scores_gemma":[0.9994336,0.00018421108,0.00007995726,0.00013393603,0.00012830568,0.00004004008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056954403,0.00060518883,0.0005114741,0.0008484514,0.001027111,0.0029627287,0.0011184281,0.0010007451,0.01679381],"category_scores_gemma":[0.0019702774,0.00039720195,0.00048250073,0.00093379855,0.0033777824,0.002769086,0.0018799915,0.0018000244,0.0053976583],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052463314,0.000031680927,0.0006505239,0.0003393593,0.000013603297,0.0002331873,0.0019925216,0.0071966858,0.009462987,0.7241423,0.018172547,0.23771216],"study_design_scores_gemma":[0.000009804805,0.000109400185,0.0023922615,0.00025426384,0.000016335023,0.0010580291,0.0008115817,0.00282348,0.0036279603,0.20073348,0.7881169,0.0000465275],"about_ca_topic_score_codex":0.0014321308,"about_ca_topic_score_gemma":0.0011313629,"teacher_disagreement_score":0.01679381,"about_ca_system_score_codex":0.001006253,"about_ca_system_score_gemma":0.0006823344,"threshold_uncertainty_score":0.056180894},"labels":[],"label_agreement":null},{"id":"W4400622066","doi":"10.1029/2024gc011476","title":"Water Geochemistry and Stable Isotope Changes Record Groundwater Mixing After a Regional Earthquake in Northeast India","year":2024,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institute for Advanced Research; United States - India Educational Foundation; Institute of International Education","keywords":"Geology; Groundwater; Hydrogeology; Aquifer; Tectonics; Period (music); Geochemistry; Hydrology (agriculture); Water well; Seismology; Geotechnical engineering","score_opus":0.010528092486298785,"score_gpt":0.19259080316774327,"score_spread":0.18206271068144447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400622066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99965525,0.000015099674,0.00003010737,0.000012240235,9.165313e-7,0.0000015412113,0.00011943533,0.000003996691,0.00016138653],"genre_scores_gemma":[0.9996866,0.00002160543,0.000038889924,0.000005620976,0.0000016051436,0.0000021113626,0.00015619147,0.0000010826559,0.00008637252],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999225,0.000008716292,0.000005590463,0.00001950761,0.000015953701,0.000027641814],"domain_scores_gemma":[0.99974304,0.000036476406,0.0000967537,0.00002130277,0.00006454886,0.000037856313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008553251,0.00015385349,0.0001888801,0.00074129924,0.0003632869,0.0004561887,0.00032838134,0.0002435949,0.00033956324],"category_scores_gemma":[0.00024617722,0.0001481574,0.00013391582,0.00104573,0.0003318786,0.00024128801,0.0003328698,0.0002315769,0.000114371964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016850447,0.00005761918,0.9592092,0.00002952058,0.00003792918,0.000571643,0.0013194685,0.00038428052,0.03202288,0.00004412279,0.0001628169,0.005992013],"study_design_scores_gemma":[0.0000011875042,0.000024006516,0.9982553,0.0000014153077,0.0000078524,0.000079581005,0.000558398,0.00015713535,0.00079981325,0.000010836592,0.00010083957,0.0000037229654],"about_ca_topic_score_codex":0.027682474,"about_ca_topic_score_gemma":0.046319306,"teacher_disagreement_score":0.027682474,"about_ca_system_score_codex":0.00042976794,"about_ca_system_score_gemma":0.00028781287,"threshold_uncertainty_score":0.055042684},"labels":[],"label_agreement":null},{"id":"W4400873359","doi":"10.26443/seismica.v3i2.1165","title":"An exploration of potentially reversible controls on millennial-scale variations in the slip rate of seismogenic faults: Linking structural observations with variable earthquake recurrence patterns","year":2024,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Slip (aerodynamics); Variable (mathematics); Mathematics; Engineering","score_opus":0.030454710709517822,"score_gpt":0.24136196041794525,"score_spread":0.21090724970842742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400873359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99636406,0.0004373528,0.0019128061,0.000057464076,0.0000027723688,0.000008911519,0.00017127243,0.000023734427,0.0010217117],"genre_scores_gemma":[0.99959594,0.00009076883,0.00021023271,0.0000060635743,0.000001742307,0.0000023518262,0.0000336372,0.0000025625816,0.00005662369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999206,0.000015292682,0.000007095567,0.000026980386,0.000010760321,0.000019183719],"domain_scores_gemma":[0.9994506,0.00018872666,0.00019771406,0.00008253337,0.000044610417,0.000035864934],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005619713,0.0002858614,0.0002835531,0.00066000136,0.00029833708,0.0004966233,0.00045679725,0.0003103799,0.0012394926],"category_scores_gemma":[0.0011647941,0.00024116793,0.0003115967,0.0004732526,0.0005707464,0.0006972871,0.00039302555,0.00034665142,0.00010130241],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018858883,0.00010128512,0.6191159,0.0003011133,0.00039923802,0.00041322887,0.00074294745,0.012453102,0.3186079,0.004542489,0.00016707982,0.042967103],"study_design_scores_gemma":[0.000006373079,0.00009873553,0.98172194,0.000012957954,0.00006456205,0.00013352573,0.00024407722,0.008599319,0.007135452,0.0013468926,0.00061878277,0.000017392955],"about_ca_topic_score_codex":0.0013246919,"about_ca_topic_score_gemma":0.0019519913,"teacher_disagreement_score":0.0013246919,"about_ca_system_score_codex":0.0003220408,"about_ca_system_score_gemma":0.0002230762,"threshold_uncertainty_score":0.0041464567},"labels":[],"label_agreement":null},{"id":"W4400902407","doi":"10.1146/annurev-earth-040722-111915","title":"Autobiography: A 50-Year Quest for Understanding in Geoscience","year":2024,"lang":"en","type":"article","venue":"Annual Review of Earth and Planetary Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Biography; Earth science; Astrobiology; Geology; Environmental ethics; History; Art history; Philosophy; Biology","score_opus":0.03768162823675269,"score_gpt":0.2716401447533702,"score_spread":0.23395851651661753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400902407","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0011458402,0.25194162,0.004465921,0.64338404,0.06356443,0.00002228974,0.00041099262,0.0002724676,0.03479237],"genre_scores_gemma":[0.05375193,0.3385284,0.015071943,0.31229073,0.15723467,0.00017385701,0.0008705809,0.00084387,0.12123398],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99673295,0.0013442206,0.00025359882,0.0006187506,0.00080612337,0.00024441027],"domain_scores_gemma":[0.97686744,0.010965966,0.0008226447,0.0034374627,0.00450205,0.0034044534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.007373915,0.0013994244,0.0018821117,0.0044267196,0.0035946867,0.012776883,0.001737261,0.006592641,0.036615238],"category_scores_gemma":[0.020256361,0.0004782293,0.0008806168,0.0041156653,0.019276781,0.026921296,0.007370987,0.013819058,0.015600305],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000328115,0.000024649293,0.0005325133,0.0004316766,0.000029859571,0.00013187785,0.002895178,0.00014810833,0.00022703847,0.144771,0.75557667,0.09519865],"study_design_scores_gemma":[0.000005043751,0.000009139466,0.0003613323,0.00059430825,0.000005636975,0.00013343611,0.0012090858,0.00009479359,0.000029533412,0.062341783,0.93520164,0.000014250024],"about_ca_topic_score_codex":0.003424718,"about_ca_topic_score_gemma":0.0040943143,"teacher_disagreement_score":0.036615238,"about_ca_system_score_codex":0.0038484803,"about_ca_system_score_gemma":0.0038711026,"threshold_uncertainty_score":0.12249011},"labels":[],"label_agreement":null},{"id":"W4400974552","doi":"10.1126/science.adj9587","title":"Fault size–dependent fracture energy explains multiscale seismicity and cascading earthquakes","year":2024,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Induced seismicity; Seismology; Geology; Fault (geology); Seismic energy","score_opus":0.010122493890202608,"score_gpt":0.22653017075332993,"score_spread":0.2164076768631273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400974552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933193,0.000120499426,0.004863246,0.00019857715,0.00000582268,0.000004632154,0.000070201415,0.00006035228,0.0013574772],"genre_scores_gemma":[0.99952924,0.00003754638,0.00034060085,0.0000067618585,0.0000061923324,0.0000018613581,0.000016130949,0.0000081737535,0.00005351777],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999244,0.000010683245,0.000005216548,0.000026684347,0.000015263704,0.000017680793],"domain_scores_gemma":[0.99927634,0.00027447264,0.00017777026,0.00013870504,0.00005527718,0.00007753383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003185178,0.00021625232,0.00028118456,0.0006149787,0.00029380052,0.000523585,0.00038651103,0.00033874248,0.0012874876],"category_scores_gemma":[0.0020618082,0.00022901881,0.00027129348,0.0003982725,0.00088744506,0.0010383569,0.00064405776,0.00037274355,0.00010603512],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002241747,0.00020158943,0.44654277,0.00017529432,0.00022554521,0.0011651384,0.0011989375,0.38347286,0.05568164,0.06372725,0.0017615262,0.045623258],"study_design_scores_gemma":[0.000017279268,0.00006136048,0.37557784,0.000019503548,0.000060399845,0.0002513506,0.00037780716,0.54810286,0.0024758184,0.07189152,0.0011222162,0.000042097658],"about_ca_topic_score_codex":0.003271219,"about_ca_topic_score_gemma":0.0028946646,"teacher_disagreement_score":0.003271219,"about_ca_system_score_codex":0.00046731846,"about_ca_system_score_gemma":0.00015659037,"threshold_uncertainty_score":0.006504357},"labels":[],"label_agreement":null},{"id":"W4401026553","doi":"10.1785/0120240005","title":"Impact of Geometric Spreading in the Fourier Domain on Source Spectra: Observations of Steep Amplitude Decay and Frequency Dependence from the 2019 Ridgecrest, California, Earthquake, Sequence","year":2024,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Amplitude; Scaling; Attenuation; Spectral line; Source model; Physics; Strong ground motion; Geology; Fourier transform; Geometry; Seismology; Spectral shape analysis; Event (particle physics); Geodesy; Computational physics; Ground motion; Mathematics; Optics; Astrophysics","score_opus":0.03183049278103131,"score_gpt":0.2486150631139055,"score_spread":0.21678457033287418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401026553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99780864,0.000046586323,0.00035420584,0.00003595685,0.0000034599602,0.0000035549617,0.00046108084,0.000056147874,0.0012304127],"genre_scores_gemma":[0.9991211,0.000020210715,0.00018577685,0.0000053417384,0.0000051014604,0.0000016780497,0.00053582474,0.000010526018,0.00011428245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998964,0.000007067443,0.0000055471673,0.000026680444,0.00004606122,0.000018227742],"domain_scores_gemma":[0.99949443,0.00009226064,0.00015615892,0.00005415614,0.00014036548,0.00006259019],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022021066,0.00025573175,0.00019442031,0.0007357982,0.00025989066,0.00033428686,0.0002746819,0.000255499,0.001254708],"category_scores_gemma":[0.0011273781,0.00020476994,0.00016589447,0.0005346508,0.00022186675,0.00029129506,0.00034837666,0.0002902563,0.00030888326],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046183553,0.00013272124,0.90417284,0.00007824499,0.000091313625,0.00039148083,0.00045239518,0.010467372,0.057012383,0.0002509778,0.0017332884,0.024755273],"study_design_scores_gemma":[0.000004861335,0.000019466102,0.9956344,0.0000037957366,0.0000051526845,0.00004133404,0.000043037573,0.0034495892,0.0005927698,0.00002574149,0.0001745427,0.0000051787993],"about_ca_topic_score_codex":0.021798424,"about_ca_topic_score_gemma":0.029469805,"teacher_disagreement_score":0.021798424,"about_ca_system_score_codex":0.00035996424,"about_ca_system_score_gemma":0.00019096187,"threshold_uncertainty_score":0.043343127},"labels":[],"label_agreement":null},{"id":"W4401224245","doi":"10.1029/2024gl109308","title":"Pressure Dependence of Permeability in Cracked Rocks: Experimental Evidence of Non‐Linear Pore‐Pressure Gradients From Local Measurements","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique; China Scholarship Council","keywords":"Geology; Permeability (electromagnetism); Pore water pressure; Fluid dynamics; Brittleness; Linearity; Mineralogy; Materials science; Geotechnical engineering; Mechanics; Composite material; Chemistry","score_opus":0.0765959401472368,"score_gpt":0.33700452324149693,"score_spread":0.2604085830942601,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401224245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99295276,0.0001204861,0.0063735475,0.000015258529,0.0000019521901,0.000007969179,0.00009101509,0.000049358354,0.0003877118],"genre_scores_gemma":[0.99903655,0.000031222506,0.0008385184,0.0000027631904,6.622089e-7,0.0000044190333,0.000027023301,0.0000053728645,0.000053323773],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99978393,0.000022622873,0.000014949812,0.00005233506,0.00009569773,0.0000305633],"domain_scores_gemma":[0.9991455,0.00040484552,0.00016057643,0.00012401782,0.000119774355,0.000045272493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025122342,0.00016066252,0.00019149028,0.0003102867,0.00017782005,0.00023471472,0.0003578951,0.00027575353,0.00084136904],"category_scores_gemma":[0.0010893258,0.00024992594,0.00007365551,0.00022063937,0.0006473137,0.00046030106,0.00036516905,0.00052102905,0.000094360876],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005640364,0.000016148173,0.0024467097,0.00003871098,0.000005110339,0.00004495737,0.000065902175,0.0005741776,0.99492353,0.000060151975,0.00001227308,0.0017559616],"study_design_scores_gemma":[0.000009848281,0.00015782965,0.048517015,0.0000057654825,0.000009397905,0.00016650591,0.00006737514,0.011846706,0.9389114,0.00011503561,0.00018101836,0.000012029024],"about_ca_topic_score_codex":0.0005748585,"about_ca_topic_score_gemma":0.00076591864,"teacher_disagreement_score":0.00084136904,"about_ca_system_score_codex":0.00012130696,"about_ca_system_score_gemma":0.000075461125,"threshold_uncertainty_score":0.0028147101},"labels":[],"label_agreement":null},{"id":"W4401263910","doi":"10.1016/j.tecto.2024.230441","title":"A scaling relationship for the width of secondary deformation around strike-slip faults","year":2024,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Canada First Research Excellence Fund","keywords":"Geology; Slip (aerodynamics); Geometry; Fault (geology); Strike-slip tectonics; Scaling; Deformation (meteorology); Seismology; Physics; Mathematics","score_opus":0.03018908071472377,"score_gpt":0.24671135860465002,"score_spread":0.21652227788992626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401263910","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94811386,0.0007089341,0.03929974,0.00023477321,0.000026585292,0.000036212732,0.0002934315,0.00047336612,0.010813068],"genre_scores_gemma":[0.99802196,0.000089286594,0.0015734056,0.0000097558195,0.000007959211,0.000007735254,0.00006569682,0.000016523416,0.00020775679],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99988544,0.000008049946,0.000006263238,0.000054483386,0.000026444894,0.000019200084],"domain_scores_gemma":[0.9994068,0.00016887301,0.00019910347,0.00008109373,0.00008411658,0.000060081602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015415937,0.00028892138,0.00013511795,0.00064462307,0.00017852611,0.0003691238,0.00039494914,0.0002777525,0.0013134956],"category_scores_gemma":[0.0010503953,0.00024715817,0.00024899407,0.00024044357,0.000584697,0.00047209466,0.00030408375,0.00042094765,0.0002334012],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002281137,0.00014200297,0.3516403,0.00034750986,0.00014003653,0.001175641,0.001126772,0.21551074,0.32049215,0.030566031,0.0017661647,0.076864555],"study_design_scores_gemma":[0.000038073915,0.0002268212,0.7276587,0.000059423925,0.000032951702,0.0012842565,0.00025305807,0.21929651,0.032851875,0.015648125,0.0025564982,0.00009379272],"about_ca_topic_score_codex":0.0010488684,"about_ca_topic_score_gemma":0.00078449736,"teacher_disagreement_score":0.0013134956,"about_ca_system_score_codex":0.0004264692,"about_ca_system_score_gemma":0.00013873068,"threshold_uncertainty_score":0.004394114},"labels":[],"label_agreement":null},{"id":"W4401527231","doi":"10.1093/gji/ggae248","title":"Constraints on the 2013 Saravan intraslab earthquake using permanent GNSS, InSAR and seismic data","year":2024,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Canadian Space Agency","keywords":"Geology; Seismology; Subduction; Geodesy; Interferometric synthetic aperture radar; Slab; Slip (aerodynamics); Kinematics; Epicenter; Hypocenter; Crust; Focal mechanism; GNSS applications; Tectonics; Synthetic aperture radar; Satellite; Geophysics; Induced seismicity; Remote sensing","score_opus":0.04959507129408495,"score_gpt":0.27403119342011195,"score_spread":0.224436122126027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401527231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98018825,0.00015323839,0.0016677751,0.00015202632,0.00001936281,0.000022716635,0.006553478,0.00015089604,0.011092193],"genre_scores_gemma":[0.9860306,0.000092753,0.0017886498,0.000035597543,0.000023096682,0.000019535331,0.011452954,0.000023419849,0.00053352717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997248,0.000045093017,0.000019325802,0.000065325316,0.00006936543,0.000076101256],"domain_scores_gemma":[0.99927586,0.00017439266,0.00018618841,0.0000905996,0.0001851363,0.00008789912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035075028,0.0005498648,0.00041195884,0.0009991594,0.00038211394,0.0008592354,0.00031066884,0.00026894733,0.002350993],"category_scores_gemma":[0.0013339721,0.00026219658,0.00027979052,0.0013117584,0.00026130863,0.00037248072,0.00072068966,0.00029166744,0.00084367994],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007037958,0.00015203629,0.87712705,0.000204284,0.00023948358,0.0013812856,0.00041023263,0.02660941,0.023745008,0.0014344453,0.00847774,0.05951525],"study_design_scores_gemma":[0.00002878716,0.00009693815,0.96632105,0.000053743144,0.000058811103,0.00023179328,0.0007328188,0.022410572,0.0031626194,0.00047484483,0.006391479,0.000036537756],"about_ca_topic_score_codex":0.026710417,"about_ca_topic_score_gemma":0.068730906,"teacher_disagreement_score":0.026710417,"about_ca_system_score_codex":0.00050524465,"about_ca_system_score_gemma":0.0008854466,"threshold_uncertainty_score":0.053109884},"labels":[],"label_agreement":null},{"id":"W4401639492","doi":"10.1029/2024jb029159","title":"Spatial Distribution of Tremor Episodes From Long‐Term Monitoring in the Northern Cascadia Subduction Zone","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"","keywords":"Subduction; Geology; Term (time); Seismology; Episodic tremor and slip; Spatial distribution; Remote sensing; Tectonics","score_opus":0.04535060136841667,"score_gpt":0.3246652609147982,"score_spread":0.2793146595463815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401639492","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99814296,0.000062576175,0.00012515885,0.000011510393,9.840682e-7,0.000003648416,0.0011502893,0.000025543475,0.00047734648],"genre_scores_gemma":[0.9979754,0.00004222345,0.00010227011,0.000002612144,0.0000023236014,0.000004876559,0.0017110108,0.0000035159123,0.00015568578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977547,0.000022535087,0.000026230959,0.00007516948,0.00006561634,0.00003496986],"domain_scores_gemma":[0.99891734,0.00016029482,0.0003879727,0.0001104421,0.00021639689,0.00020758674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037671113,0.00023722553,0.00021008511,0.0022746832,0.0003176853,0.000509998,0.00029569454,0.00024471368,0.0007245606],"category_scores_gemma":[0.0010594093,0.00013445463,0.00030427775,0.0021443826,0.00027232774,0.00019205107,0.00060025515,0.00016515708,0.00016696008],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005354793,0.000012586502,0.99014306,0.000028394918,0.00009318383,0.00013593408,0.00036126282,0.0015859896,0.0026938152,0.000022967684,0.0001834112,0.004685805],"study_design_scores_gemma":[9.242431e-7,0.000007096221,0.9991881,0.0000026570685,0.000008110587,0.000023901624,0.00006866283,0.0005004516,0.00008259428,0.000004601505,0.00011118198,0.0000017850592],"about_ca_topic_score_codex":0.056853965,"about_ca_topic_score_gemma":0.09306732,"teacher_disagreement_score":0.056853965,"about_ca_system_score_codex":0.0006181667,"about_ca_system_score_gemma":0.00031014712,"threshold_uncertainty_score":0.11304605},"labels":[],"label_agreement":null},{"id":"W4401790762","doi":"10.1029/2023tc008034","title":"Time Constraints on the Late Cenozoic Fault Evolution Along the Northern Margin of the Iranian Plateau in the Arabia‐Eurasia Collision Zone","year":2024,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Cenozoic; Geology; Plateau (mathematics); Margin (machine learning); Collision; Collision zone; Paleontology; Fault (geology); Seismology; Tectonics; Lithosphere; Structural basin","score_opus":0.01384774611454505,"score_gpt":0.20898815096667694,"score_spread":0.19514040485213188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401790762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990877,0.00010574338,0.00009598157,0.000010063095,0.000001199622,0.0000012533144,0.00010568631,0.000004219948,0.0005882966],"genre_scores_gemma":[0.9997012,0.000037440266,0.00006683634,0.0000020880134,0.000001562803,0.0000014073607,0.0001274984,0.0000014267913,0.00006051131],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991953,0.000010931637,0.000006793034,0.000024509032,0.000019395304,0.000018775281],"domain_scores_gemma":[0.99975437,0.000030178577,0.00009083189,0.000016842494,0.00008195662,0.000025822657],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023535496,0.00016193907,0.00013540724,0.0013187691,0.00039222086,0.0005529299,0.00020935765,0.00019688855,0.0011112802],"category_scores_gemma":[0.00051760784,0.0001007407,0.00013136608,0.0012521943,0.00034563473,0.00026954905,0.00033065263,0.00014112915,0.00012476348],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011720847,0.00001542706,0.9639745,0.000021447437,0.00003974271,0.00024092542,0.0007455025,0.0010768931,0.021207131,0.00037941843,0.00009818326,0.012083857],"study_design_scores_gemma":[0.0000017378949,0.0000080486225,0.998912,0.0000025636577,0.0000049113087,0.000036441044,0.00018065631,0.00036005984,0.00023120159,0.000036942398,0.00022416115,0.0000014529437],"about_ca_topic_score_codex":0.022205604,"about_ca_topic_score_gemma":0.026827738,"teacher_disagreement_score":0.022205604,"about_ca_system_score_codex":0.00044940304,"about_ca_system_score_gemma":0.00030539464,"threshold_uncertainty_score":0.044152677},"labels":[],"label_agreement":null},{"id":"W4401832787","doi":"10.1016/j.geomat.2024.100019","title":"Assessment of active tectonics of the Tripura-Mizoram fold belt (Surma Basin), North East India","year":2024,"lang":"en","type":"article","venue":"GEOMATICA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Fold (higher-order function); Tectonics; Geology; Structural basin; Seismology; Paleontology","score_opus":0.01259397735877207,"score_gpt":0.22989319849885406,"score_spread":0.217299221140082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401832787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989435,0.00012456284,0.000096988915,0.000020596792,0.0000011674452,0.000006037737,0.00014887548,0.0000074893815,0.0006506773],"genre_scores_gemma":[0.9994925,0.000083542815,0.00012002833,0.0000038829144,0.0000014681023,0.000002620522,0.00015426206,0.0000011230458,0.00014054336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991167,0.000014010469,0.0000089287705,0.00001732585,0.000021788843,0.000026224725],"domain_scores_gemma":[0.99977857,0.000034865137,0.00008474641,0.000014883071,0.00004864294,0.0000383544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012421115,0.00027124898,0.00012009375,0.0016440174,0.00027878134,0.0008202771,0.00018911202,0.00015428376,0.0005347306],"category_scores_gemma":[0.00036843456,0.000113743656,0.00014445891,0.0013039428,0.0002975783,0.00030698528,0.00034527737,0.00012732658,0.00010748211],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006382167,0.000030894356,0.97263926,0.00005759905,0.0000610442,0.0007395691,0.0015133388,0.0015525285,0.0045479247,0.00037267042,0.00023542953,0.018185953],"study_design_scores_gemma":[0.0000013653037,0.000016975355,0.99768865,0.000006256628,0.00001652138,0.00016671322,0.000861589,0.00064392,0.00018068147,0.000029683177,0.00038444332,0.0000032686185],"about_ca_topic_score_codex":0.026195832,"about_ca_topic_score_gemma":0.059572753,"teacher_disagreement_score":0.026195832,"about_ca_system_score_codex":0.0005550298,"about_ca_system_score_gemma":0.00040772953,"threshold_uncertainty_score":0.05208671},"labels":[],"label_agreement":null},{"id":"W4401840815","doi":"10.62481/a23a9f0a","title":"Swarm offshore Vancouver Island punctuated by M6.4 earthquake","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Submarine pipeline; Seismology; Swarm behaviour; Geology; Punctuated equilibrium; Oceanography; Computer science; Paleontology; Artificial intelligence","score_opus":0.013846757884436418,"score_gpt":0.21613371985039095,"score_spread":0.20228696196595453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401840815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9687008,0.00009514965,0.00019501279,0.0003127156,0.0000553891,0.000013250793,0.0026158798,0.0000467808,0.027965013],"genre_scores_gemma":[0.98130316,0.00006551254,0.00018282903,0.000019456304,0.00001036708,0.0000037164396,0.0024153432,0.000014146287,0.01598549],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999348,0.0000044430835,0.0000019167485,0.000011167514,0.00001990779,0.000027791448],"domain_scores_gemma":[0.9997787,0.000013757086,0.000018250013,0.000020597387,0.000098898956,0.00006980723],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007150426,0.00021567637,0.00019294585,0.000594862,0.0013901427,0.0010319906,0.00023746338,0.00051356986,0.006568639],"category_scores_gemma":[0.0005197904,0.00012260734,0.000116963725,0.0008495536,0.00022296778,0.00021012776,0.00066786766,0.00034345879,0.0008278697],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008914306,0.00020214854,0.7679723,0.00023573525,0.00030660143,0.006814058,0.0028240937,0.027871804,0.021008564,0.00691592,0.08546053,0.07949679],"study_design_scores_gemma":[0.00003508569,0.00003565235,0.9546336,0.00003429546,0.000043326243,0.0002395375,0.0028252813,0.017878309,0.0015261874,0.0010762122,0.021649493,0.00002297154],"about_ca_topic_score_codex":0.67701674,"about_ca_topic_score_gemma":0.8164522,"teacher_disagreement_score":0.32298326,"about_ca_system_score_codex":0.0017872356,"about_ca_system_score_gemma":0.0017855717,"threshold_uncertainty_score":0.64977074},"labels":[],"label_agreement":null},{"id":"W4402018214","doi":"10.1007/s10064-024-03869-6","title":"Development of a loading and diagnostic system to study laboratory earthquakes","year":2024,"lang":"en","type":"article","venue":"Bulletin of Engineering Geology and the Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Nature Conservation; Geology; Forensic engineering; Seismology; Engineering; Biology; Ecology","score_opus":0.004563737369461064,"score_gpt":0.16142823725072,"score_spread":0.15686449988125895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402018214","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.09779658,0.00007955207,0.87583196,0.00012866847,0.000071977476,0.00069683674,0.001523711,0.020801922,0.0030688024],"genre_scores_gemma":[0.43353146,0.00009216754,0.5568482,0.00014661846,0.00009032299,0.0010722106,0.0032641797,0.00072860543,0.0042263],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996351,0.00006465352,0.0000458095,0.00009363176,0.00012677682,0.00003399494],"domain_scores_gemma":[0.99810326,0.00044360114,0.00011554648,0.0002921343,0.0008805764,0.0001648006],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008102186,0.0007223547,0.00072921935,0.0019245389,0.00044294685,0.0007178577,0.00093849597,0.0006403759,0.0051301937],"category_scores_gemma":[0.0016665141,0.00033555433,0.0003111962,0.0007534264,0.0002524771,0.0009604251,0.00069505884,0.00042876703,0.0019541255],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008281062,0.0010323783,0.068714656,0.00023881276,0.0001444942,0.00035202067,0.00036200715,0.0220821,0.39864278,0.0033269753,0.008775507,0.49550006],"study_design_scores_gemma":[0.00036850985,0.0013896,0.087209225,0.00006864461,0.00030597363,0.0009909633,0.00026609146,0.61912423,0.2619591,0.0027407128,0.025359297,0.00021765273],"about_ca_topic_score_codex":0.0027913516,"about_ca_topic_score_gemma":0.0022494188,"teacher_disagreement_score":0.0051301937,"about_ca_system_score_codex":0.0003548348,"about_ca_system_score_gemma":0.0010859831,"threshold_uncertainty_score":0.017162263},"labels":[],"label_agreement":null},{"id":"W4402232958","doi":"10.1029/2024jb029104","title":"Strong Lg‐Wave Attenuation Reveals Quarter‐Toroidal Crustal Melting Around the Yakutat Terrane in South‐Central Alaska","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Terrane; Attenuation; Quarter (Canadian coin); Seismology; Geology; Toroid; Physics; Geography; Tectonics; Nuclear physics; Optics; Archaeology","score_opus":0.05875102686652766,"score_gpt":0.3251521146795741,"score_spread":0.26640108781304644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402232958","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99867046,0.000041252155,0.0003976778,0.000031557087,0.0000028264492,0.0000018903595,0.00015782546,0.000060673126,0.00063587405],"genre_scores_gemma":[0.9995017,0.000020097534,0.00020182072,0.0000042792203,0.0000018512445,0.0000015925567,0.0001296964,0.000005196293,0.00013364403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996233,0.000003501556,0.00000200169,0.000012622148,0.0000068337613,0.000012771664],"domain_scores_gemma":[0.9999355,0.000008939403,0.000013681585,0.0000076213933,0.000018176343,0.00001610227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009043212,0.00026308,0.00022240491,0.00044449474,0.0003725514,0.00045996965,0.00026175697,0.00034501564,0.0013600029],"category_scores_gemma":[0.00020440943,0.00022417684,0.00020903492,0.0004133045,0.00027128728,0.00024825186,0.000358804,0.00024456417,0.000247679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031749162,0.00013368133,0.8412095,0.00007892451,0.00013820673,0.00094109005,0.001036515,0.039972477,0.09683454,0.00026476555,0.0006985545,0.018374301],"study_design_scores_gemma":[0.000015259728,0.00004510188,0.9360519,0.000011152049,0.00004461364,0.00013252033,0.00067036494,0.0606458,0.0018578854,0.00010865009,0.0003998205,0.000016871512],"about_ca_topic_score_codex":0.035306007,"about_ca_topic_score_gemma":0.037028573,"teacher_disagreement_score":0.035306007,"about_ca_system_score_codex":0.00023694974,"about_ca_system_score_gemma":0.00027088847,"threshold_uncertainty_score":0.07020098},"labels":[],"label_agreement":null},{"id":"W4402274891","doi":"10.1029/2024jb029253","title":"A 3‐D Seismic Tomographic Study of Spreading Structures and Smooth Seafloor Generated by Detachment Faulting—The Ultra‐Slow Spreading Southwest Indian Ridge at 64°30′E","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut Polaire Français Paul Emile Victor; Agence Nationale de la Recherche","keywords":"Geology; Seafloor spreading; Detachment fault; Magmatism; Tectonics; Seismology; Bathymetry; Lithology; Mid-Atlantic Ridge; Ridge; Volcano; Mid-ocean ridge; Magma chamber; Mantle (geology); Ridge push; Transform fault; Petrology; Lithosphere; Geophysics; Magma; Paleontology; Hydrothermal circulation","score_opus":0.027809278758774796,"score_gpt":0.30517472304389026,"score_spread":0.27736544428511545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402274891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946934,0.000007701531,0.00009596615,0.000008483803,7.1386745e-7,0.0000028240524,0.00014734924,0.000014080794,0.00025351945],"genre_scores_gemma":[0.99923146,0.000010119624,0.0003428157,0.0000036780546,0.0000017374081,0.000002619438,0.00030898568,0.000004815853,0.00009379741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999567,0.0000042934585,0.0000024424717,0.000010915333,0.000011885171,0.00001369894],"domain_scores_gemma":[0.999866,0.00001951339,0.000035019417,0.000012851411,0.000025803582,0.00004079997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007602755,0.00024723666,0.00018025697,0.00089709315,0.00030417362,0.00035761407,0.00030741698,0.0002243691,0.0005763052],"category_scores_gemma":[0.0002103852,0.00024366229,0.00036580182,0.0006624761,0.00026512082,0.00013146282,0.00028082263,0.00019403287,0.00011160104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044518014,0.00026350655,0.83860224,0.00005905093,0.00017614377,0.00168273,0.0012752672,0.023733834,0.112273745,0.00026095894,0.00065831136,0.020568976],"study_design_scores_gemma":[0.0000135915525,0.000033085147,0.98368025,0.000004196228,0.000020327068,0.000119671786,0.0002649576,0.014566382,0.001001648,0.000023569131,0.0002619562,0.0000103177845],"about_ca_topic_score_codex":0.04854345,"about_ca_topic_score_gemma":0.08871679,"teacher_disagreement_score":0.04854345,"about_ca_system_score_codex":0.00045077922,"about_ca_system_score_gemma":0.0004114425,"threshold_uncertainty_score":0.096521795},"labels":[],"label_agreement":null},{"id":"W4402316880","doi":"10.1029/2024gc011639","title":"The Role of Upper Mantle Forces in Post‐Subduction Tectonics: Plumelet and Active Rifting in the East Anatolian Plateau","year":2024,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Rift; Tectonics; Mantle (geology); Seismology; Plateau (mathematics); Geophysics","score_opus":0.004377281437126051,"score_gpt":0.1896886846044878,"score_spread":0.18531140316736175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402316880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993075,0.000050865612,0.00028439882,0.000021946173,6.4986546e-7,0.0000013110752,0.00002910031,0.000008150343,0.00029598727],"genre_scores_gemma":[0.99984574,0.000018758255,0.0000617819,0.0000016089643,7.206309e-7,0.0000012215353,0.000023666138,0.0000015628591,0.00004489802],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999969,0.000005651934,0.000003485587,0.000008842582,0.0000055191063,0.000007551555],"domain_scores_gemma":[0.99992716,0.00001590835,0.000026066027,0.000006777129,0.0000123434875,0.000011679137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000108780565,0.00022080606,0.00017336007,0.00055927073,0.00032750782,0.00073957717,0.00036633312,0.00045029735,0.00081997545],"category_scores_gemma":[0.00025195506,0.00017945985,0.00027263272,0.00043470113,0.00029837491,0.00039774703,0.0004368563,0.00018590376,0.00008199849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023903573,0.00013188084,0.64634854,0.000087606946,0.00020081467,0.0008819723,0.00076716003,0.23748524,0.09325546,0.0030939246,0.00019567215,0.017312633],"study_design_scores_gemma":[0.000027603197,0.000046425906,0.53782535,0.000017186352,0.000043649474,0.00015078804,0.00035298883,0.45722887,0.0030099875,0.0008855391,0.00038922086,0.000022306473],"about_ca_topic_score_codex":0.016890952,"about_ca_topic_score_gemma":0.011446734,"teacher_disagreement_score":0.016890952,"about_ca_system_score_codex":0.00054531766,"about_ca_system_score_gemma":0.00033938285,"threshold_uncertainty_score":0.03358525},"labels":[],"label_agreement":null},{"id":"W4402362511","doi":"10.62481/c6952f3d","title":"Montreal jolted by M3.8 earthquake - small by historical standards","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; History; Political science","score_opus":0.016053955778379394,"score_gpt":0.2191218723142701,"score_spread":0.2030679165358907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402362511","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06468654,0.0023766474,0.006682288,0.010676667,0.0040605855,0.00027266308,0.23807599,0.0027607898,0.6704078],"genre_scores_gemma":[0.32736665,0.0018669793,0.0030306492,0.00037273637,0.00049021497,0.00007878257,0.056846794,0.00088950136,0.6090576],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99969006,0.000023252076,0.000011510261,0.00007501969,0.00013034994,0.00006970772],"domain_scores_gemma":[0.9989681,0.00008882615,0.00009341816,0.0001872788,0.00048495698,0.00017744194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002794213,0.00056838465,0.00043032813,0.0015251,0.0013318539,0.0020728312,0.00063061743,0.00052850257,0.12570207],"category_scores_gemma":[0.003199527,0.0002057275,0.00026188453,0.0039628386,0.00033145555,0.00064654025,0.00063141674,0.0009023323,0.01275619],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028439815,0.000031325402,0.017400283,0.00015732703,0.000059189188,0.0003958016,0.0003317296,0.0021159323,0.0010898208,0.03877637,0.83983016,0.09952765],"study_design_scores_gemma":[0.000050140985,0.000028879844,0.13581114,0.0000702353,0.0000276997,0.00015283294,0.0003652736,0.0019236822,0.0012128445,0.0052348906,0.8550927,0.000029735867],"about_ca_topic_score_codex":0.800424,"about_ca_topic_score_gemma":0.872869,"teacher_disagreement_score":0.19957602,"about_ca_system_score_codex":0.004747682,"about_ca_system_score_gemma":0.004830219,"threshold_uncertainty_score":0.4205153},"labels":[],"label_agreement":null},{"id":"W4402390647","doi":"10.1038/s41561-024-01531-0","title":"Urgent need for greater earthquake resilience in continental Asia","year":2024,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Resilience (materials science); Geology; Seismology","score_opus":0.010777519565427749,"score_gpt":0.240747195272526,"score_spread":0.22996967570709825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402390647","genre_codex":"empirical","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.79750013,0.007011357,0.001987929,0.14669348,0.00096383685,0.000033375116,0.0010332214,0.00025014134,0.044526625],"genre_scores_gemma":[0.9926232,0.0016263684,0.0005198979,0.003134547,0.0002446009,0.000010407636,0.00019972067,0.000010852625,0.0016304264],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998332,0.000025324234,0.000014441552,0.000022936692,0.000017389311,0.00008669725],"domain_scores_gemma":[0.9985287,0.00014805053,0.00026374517,0.00011329754,0.00030625073,0.0006398726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007913418,0.00019536914,0.00025192287,0.00041943233,0.0008882708,0.0018948655,0.0005466833,0.0008633318,0.012180017],"category_scores_gemma":[0.0019178658,0.00008356661,0.00023866068,0.00042580787,0.0009301277,0.0021901398,0.0020780356,0.0010314102,0.0005612356],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010770157,0.00032620234,0.45340684,0.0032484124,0.0006413701,0.0044771475,0.014231243,0.009652019,0.022584876,0.088466585,0.078551464,0.32333684],"study_design_scores_gemma":[0.00009252628,0.0004605993,0.72307307,0.0014987213,0.00027224308,0.0014449066,0.04901176,0.0035847728,0.0019570973,0.06305116,0.15544684,0.000106168125],"about_ca_topic_score_codex":0.010815285,"about_ca_topic_score_gemma":0.014491827,"teacher_disagreement_score":0.012180017,"about_ca_system_score_codex":0.0009431069,"about_ca_system_score_gemma":0.0035859905,"threshold_uncertainty_score":0.04074627},"labels":[],"label_agreement":null},{"id":"W4402520871","doi":"10.1016/b978-0-443-19098-8.00023-3","title":"Application in structural geology","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Regina","funders":"","keywords":"Geology","score_opus":0.011468309988021131,"score_gpt":0.2191703208159363,"score_spread":0.20770201082791517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402520871","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.001528422,0.019675631,0.1215319,0.0019650084,0.002205567,0.00006691291,0.0006054433,0.0015527828,0.85086834],"genre_scores_gemma":[0.017381333,0.015912049,0.055097178,0.00065485435,0.0011664547,0.0000837317,0.0006288022,0.0005939744,0.90848154],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997855,0.000036866855,0.000017521903,0.000054020955,0.000089994195,0.000016183303],"domain_scores_gemma":[0.9997316,0.000107022766,0.000007915162,0.00005360544,0.000078226905,0.000021760667],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003633314,0.0010512031,0.00074686523,0.0018060412,0.0006866761,0.0023335002,0.0009280771,0.0013354707,0.14186941],"category_scores_gemma":[0.0010391377,0.00042524686,0.0006961166,0.002627557,0.0010105878,0.0023351538,0.0014782167,0.0013371189,0.048353575],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011400882,0.00002535661,0.0002591374,0.00038585076,0.0000117729405,0.00013915871,0.0002874892,0.0026885702,0.0014167317,0.19950809,0.12667961,0.66858685],"study_design_scores_gemma":[0.0000038181925,0.000010522298,0.00042594897,0.00017482728,0.000007518728,0.00020831282,0.00010336671,0.002525169,0.00029717176,0.09294436,0.9032916,0.0000073515303],"about_ca_topic_score_codex":0.0044806995,"about_ca_topic_score_gemma":0.0063722143,"teacher_disagreement_score":0.14186941,"about_ca_system_score_codex":0.0009615458,"about_ca_system_score_gemma":0.00060081144,"threshold_uncertainty_score":0.47460043},"labels":[],"label_agreement":null},{"id":"W4402522004","doi":"10.1038/s41467-024-52126-7","title":"Multistage lithospheric drips control active basin formation within an uplifting orogenic plateau","year":2024,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Alliance de recherche numérique du Canada; Natural Sciences and Engineering Research Council of Canada; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu; Government of Canada","keywords":"Lithosphere; Geology; Structural basin; Crust; Magmatism; Plateau (mathematics); Tectonics; Mantle (geology); Gravity anomaly; Subsidence; Pull apart basin; Geomorphology; Paleontology; Seismology; Sedimentary basin","score_opus":0.021210550484330175,"score_gpt":0.26971685214027713,"score_spread":0.24850630165594695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402522004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996681,0.00001916604,0.000046005665,0.0000035676205,2.8978047e-7,0.0000015401674,0.000013109564,0.000002829599,0.0002454594],"genre_scores_gemma":[0.99985135,0.000016243112,0.000028836163,0.0000021017254,5.9190194e-7,0.0000015633508,0.000024494042,0.0000010194382,0.00007380565],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999571,0.0000065991176,0.0000033362296,0.000012535685,0.0000047224366,0.000015614369],"domain_scores_gemma":[0.99989855,0.000013355851,0.000041433348,0.00001040618,0.000011012374,0.000025200892],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000703802,0.00007701174,0.00017646156,0.00028342765,0.00020631858,0.00038052246,0.00015846628,0.0001326471,0.00074868085],"category_scores_gemma":[0.00024001364,0.00010744901,0.00008548408,0.00022456233,0.0002864253,0.0001501134,0.00038296945,0.00012377521,0.000100087294],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005171846,0.00008118652,0.49051812,0.00006263815,0.00005920442,0.0008727283,0.0009846877,0.0016252416,0.49455598,0.0006425402,0.000110473164,0.009970136],"study_design_scores_gemma":[0.000005092236,0.00005059332,0.9961273,0.0000025067793,0.0000074111176,0.000073354604,0.00024321207,0.00072583015,0.0024582027,0.000076035445,0.00022752311,0.000003052681],"about_ca_topic_score_codex":0.0029051336,"about_ca_topic_score_gemma":0.0046700956,"teacher_disagreement_score":0.0029051336,"about_ca_system_score_codex":0.0002521163,"about_ca_system_score_gemma":0.00017839833,"threshold_uncertainty_score":0.005776465},"labels":[],"label_agreement":null},{"id":"W4402570378","doi":"10.1029/2024jf007705","title":"Temporal Behavior of Glacially Induced Stresses and Strains at Potential Sites for Long‐Term Storage of Used Nuclear Fuel in Canada","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Earth Surface","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Nuclear Waste Management Organization","keywords":"Term (time); Nuclear engineering; Physics; Engineering; Astronomy","score_opus":0.054621863230466916,"score_gpt":0.3083214728491843,"score_spread":0.2536996096187174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402570378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985164,0.000026198624,0.0001041039,0.000039052065,0.0000016944803,0.0000045917855,0.00071137765,0.000014814241,0.00058184005],"genre_scores_gemma":[0.99888843,0.000019839203,0.00010073612,0.0000058826845,4.65981e-7,0.0000035409034,0.00069529307,0.0000034742577,0.00028236362],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998908,0.000008632688,0.0000049369255,0.000025227026,0.00002452846,0.000045919383],"domain_scores_gemma":[0.99947065,0.00009895329,0.00006502277,0.00003014016,0.00017673806,0.00015849723],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023343168,0.00027517704,0.00021279379,0.0006402929,0.0010268668,0.0009632407,0.0008624401,0.0005586327,0.0016037059],"category_scores_gemma":[0.0011387992,0.00029601523,0.0004395233,0.0008808135,0.00070842134,0.0002606475,0.00042319615,0.00036844015,0.000114767456],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020225665,0.00008109241,0.64539295,0.00003194536,0.00014073156,0.00022077834,0.0003754662,0.3440577,0.0030106208,0.0009346962,0.0013711838,0.0041805883],"study_design_scores_gemma":[0.000033933306,0.000049487837,0.713575,0.000017690198,0.00004134276,0.00004425079,0.000763522,0.28324506,0.0009632301,0.00022930195,0.000990291,0.000046854988],"about_ca_topic_score_codex":0.93620026,"about_ca_topic_score_gemma":0.9465408,"teacher_disagreement_score":0.06379974,"about_ca_system_score_codex":0.011144623,"about_ca_system_score_gemma":0.004717353,"threshold_uncertainty_score":0.12835091},"labels":[],"label_agreement":null},{"id":"W4402572682","doi":"10.1029/2024jb028691","title":"How Induced Earthquakes Respond to Pre‐Existing Fractures and Hydraulic Fracturing Operations? A Case Study in South China","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Fundamental Research Funds for the Central Universities; Higher Education Discipline Innovation Project; Dalhousie University; Canada Foundation for Innovation; National Natural Science Foundation of China; Ocean Frontier Institute; China Scholarship Council","keywords":"Hydraulic fracturing; China; Geology; Geotechnical engineering; Seismology; Petroleum engineering; Forensic engineering; Engineering; Geography","score_opus":0.0707356037291648,"score_gpt":0.3750260418518048,"score_spread":0.30429043812264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402572682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99884015,0.000054435353,0.00044286516,0.000119124175,0.0000029107164,0.000010663339,0.00011705999,0.000011124394,0.00040175204],"genre_scores_gemma":[0.9987897,0.00007755041,0.0006126221,0.000015663576,0.000004778305,0.000006727818,0.00012884117,0.0000034988711,0.00036070053],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997863,0.000042914602,0.00001741103,0.000042197124,0.000043312728,0.00006791135],"domain_scores_gemma":[0.9994659,0.0001709303,0.00009930184,0.00005276004,0.00010645387,0.00010482264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005300258,0.000363209,0.0002493093,0.0010708694,0.00072969036,0.0004544264,0.0005773566,0.0006810137,0.00089307793],"category_scores_gemma":[0.0009432035,0.00018277309,0.0004381408,0.0014738482,0.00065045967,0.00049648416,0.00052426994,0.00026537268,0.000095865624],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027881167,0.00036400137,0.87613946,0.00023972003,0.0001739927,0.022736777,0.0053387457,0.042541012,0.009431638,0.0016747601,0.0017677557,0.039313268],"study_design_scores_gemma":[0.000049900053,0.00022665366,0.87201804,0.000051619103,0.00016685796,0.0012761999,0.016401479,0.10168489,0.0032734228,0.00152648,0.0032467674,0.00007768679],"about_ca_topic_score_codex":0.080961615,"about_ca_topic_score_gemma":0.14003056,"teacher_disagreement_score":0.080961615,"about_ca_system_score_codex":0.001419128,"about_ca_system_score_gemma":0.0010125692,"threshold_uncertainty_score":0.16098076},"labels":[],"label_agreement":null},{"id":"W4402725530","doi":"10.21203/rs.3.rs-4957032/v1","title":"Stress in the Geneva Basin","year":2024,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"GDG Environnement","funders":"Canton de Genève; Université de Fribourg","keywords":"Structural basin; Stress (linguistics); Geography; Geology; Archaeology; Paleontology; Philosophy; Linguistics","score_opus":0.08750586555756712,"score_gpt":0.36130164775172474,"score_spread":0.2737957821941576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402725530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867504,0.00049693254,0.00013150241,0.00037992705,0.000015689942,0.000003837407,0.0009104385,0.00002062294,0.011290681],"genre_scores_gemma":[0.99837303,0.00012866149,0.000044530712,0.0000072250464,0.0000110389865,0.0000055883465,0.00030479435,0.000008383199,0.0011167673],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979836,0.00005781396,0.000010214185,0.000047264068,0.000036972287,0.00004934768],"domain_scores_gemma":[0.99975723,0.000056268145,0.00005923048,0.000028058123,0.000053055344,0.000046149074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000263219,0.0003124865,0.00028444716,0.0014201961,0.0004952125,0.0012881187,0.00021562536,0.00041295713,0.004282885],"category_scores_gemma":[0.001108256,0.00013684022,0.00015051228,0.0021048547,0.00089937873,0.0008124545,0.0008444332,0.00023690164,0.00030534368],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015256392,0.00014993495,0.76385784,0.0002708989,0.000312807,0.001563522,0.009270783,0.064243756,0.0070656743,0.055851355,0.016856302,0.0790315],"study_design_scores_gemma":[0.000028372482,0.000058927963,0.98496234,0.000027966646,0.000021149122,0.000067841516,0.0012903541,0.002737396,0.0002508472,0.0032823745,0.0072538685,0.000018555067],"about_ca_topic_score_codex":0.080705635,"about_ca_topic_score_gemma":0.0813576,"teacher_disagreement_score":0.080705635,"about_ca_system_score_codex":0.0020602793,"about_ca_system_score_gemma":0.00057640235,"threshold_uncertainty_score":0.1604718},"labels":[],"label_agreement":null},{"id":"W4402738970","doi":"10.1139/cjes-2024-0080","title":"An investigation of subaqueous failures triggered by the 1935 CE M<sub>w</sub> 6.1 Témiscaming earthquake, Quebec, Canada, as an analogue for a paleoseismic study","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Nuclear Waste Management Organization","keywords":"Geology; Seismology; Geochemistry","score_opus":0.017954374799337883,"score_gpt":0.2221435884662137,"score_spread":0.2041892136668758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402738970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841285,0.000043906173,0.000048937876,0.000036748817,9.1850274e-7,0.0000133821895,0.00030396032,0.0000020295195,0.0011372957],"genre_scores_gemma":[0.9986632,0.000053353735,0.00009136915,0.000026065225,0.0000014448063,0.0000053143017,0.00027243368,0.0000012688349,0.0008856414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998913,0.0000076301685,0.000003368751,0.000020282137,0.000037685415,0.0000397714],"domain_scores_gemma":[0.999524,0.000025171425,0.00007836215,0.000013038566,0.00024680668,0.000112591246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001618105,0.00017189774,0.00012288439,0.00067692704,0.0011458063,0.00043137235,0.00036089512,0.0002734345,0.001132857],"category_scores_gemma":[0.00052565197,0.00012568232,0.00009681203,0.0011064474,0.0005041122,0.00016685376,0.00029335968,0.00019852312,0.0001105321],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016139043,0.000059715825,0.96891963,0.00003756663,0.000038136568,0.00077690394,0.0027907167,0.00059191615,0.012317178,0.00019239608,0.00074358704,0.013370795],"study_design_scores_gemma":[0.000001395239,0.000012996174,0.998681,0.0000020963844,0.000002418238,0.00003490078,0.0004769695,0.00014731378,0.0001157538,0.0000037978177,0.0005193824,0.0000019953463],"about_ca_topic_score_codex":0.97780174,"about_ca_topic_score_gemma":0.99297535,"teacher_disagreement_score":0.02219826,"about_ca_system_score_codex":0.008920877,"about_ca_system_score_gemma":0.004374976,"threshold_uncertainty_score":0.064725816},"labels":[],"label_agreement":null},{"id":"W4402839764","doi":"10.3846/gac.2024.19634","title":"Investigation of the effects of Kahramanmaraş earthquake series on Cyprus Arc, Dead Sea fault, Hatay regions and stations close to two earthquakes epicenters","year":2024,"lang":"en","type":"article","venue":"Geodesy and Cartography","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Seismology; Geology; Series (stratigraphy); Fault (geology); Dead sea; Island arc; Subduction; Tectonics; Paleontology; Oceanography","score_opus":0.009594148921548454,"score_gpt":0.21268551904792765,"score_spread":0.2030913701263792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402839764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99884546,0.000080615406,0.00002532526,0.000028759308,0.00000430287,0.000003527448,0.0001808087,0.0000053928356,0.0008258746],"genre_scores_gemma":[0.99931705,0.00010243368,0.000035723846,0.0000069608413,0.000006750064,0.000003078591,0.00022190232,0.0000018308853,0.00030416338],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998579,0.000020044658,0.000010473198,0.00003518994,0.000038842132,0.00003748494],"domain_scores_gemma":[0.9996667,0.000057991263,0.00011511798,0.00001962069,0.00009114297,0.00004948189],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001692325,0.000253322,0.0002180744,0.00087285554,0.0003840498,0.00046626639,0.00022538756,0.000223106,0.0007241509],"category_scores_gemma":[0.0005896386,0.00009188737,0.00018904837,0.0009517623,0.00023183844,0.00019210932,0.00026836665,0.00023060782,0.00011969978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037786114,0.00015488366,0.95178604,0.00009804622,0.00020177534,0.002429966,0.0012611406,0.0051815948,0.01139627,0.00034668928,0.0016406606,0.02512507],"study_design_scores_gemma":[0.0000018214116,0.000027797047,0.99813336,0.000003571256,0.00001930216,0.000055723795,0.00046515834,0.000690313,0.000249817,0.000007837691,0.0003421447,0.0000033404444],"about_ca_topic_score_codex":0.0806057,"about_ca_topic_score_gemma":0.14444758,"teacher_disagreement_score":0.0806057,"about_ca_system_score_codex":0.0005313334,"about_ca_system_score_gemma":0.00038591807,"threshold_uncertainty_score":0.16027302},"labels":[],"label_agreement":null},{"id":"W4402976370","doi":"10.1016/j.jseaes.2024.106342","title":"Tectonic framework of Iraq. A critical review and discussion","year":2024,"lang":"en","type":"review","venue":"Journal of Asian Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"","keywords":"Geology; Tectonics; Seismology; Earth science; Paleontology","score_opus":0.05324759686224144,"score_gpt":0.34528033252977747,"score_spread":0.292032735667536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402976370","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00007044662,0.998329,0.000029334833,0.00086260587,0.0003667921,0.0000026237472,0.00003442435,0.0000019592612,0.00030278537],"genre_scores_gemma":[0.00094086875,0.9980824,0.000052391835,0.00042937175,0.0003487174,0.000004257657,0.00003308742,9.4877765e-7,0.00010788096],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995945,0.000106797466,0.00008613821,0.00005158855,0.00011890156,0.00004204644],"domain_scores_gemma":[0.9985071,0.00076657796,0.00023387803,0.000028838838,0.00041338796,0.000050203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002158649,0.0011325998,0.0017708002,0.0050815246,0.0005403458,0.0016580446,0.0015699144,0.0011560807,0.0046883062],"category_scores_gemma":[0.0037706152,0.00041511393,0.00082779315,0.0054195053,0.0010506875,0.0019288283,0.0011025659,0.0017395539,0.001087331],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001318654,0.000036041743,0.0010229109,0.08042928,0.0006336787,0.0004043718,0.00050438754,0.00073887367,0.00051436364,0.009046281,0.114096686,0.7924412],"study_design_scores_gemma":[0.000026401241,0.00006574042,0.00548512,0.035596214,0.0006993138,0.00082920643,0.0005190667,0.00011385269,0.00016100898,0.0028543868,0.95360124,0.000048507798],"about_ca_topic_score_codex":0.0085674515,"about_ca_topic_score_gemma":0.016650435,"teacher_disagreement_score":0.0085674515,"about_ca_system_score_codex":0.002305237,"about_ca_system_score_gemma":0.0066413735,"threshold_uncertainty_score":0.017035186},"labels":[],"label_agreement":null},{"id":"W4403014804","doi":"10.1016/j.marpetgeo.2024.107143","title":"Exploring the evolution of antithetic normal fault architecture and its constraints on fault transmissibility: Evidence from sand–box simulation experiments","year":2024,"lang":"en","type":"article","venue":"Marine and Petroleum Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"Natural Science Foundation of Hebei Province","keywords":"Transmissibility (structural dynamics); Normal fault; Geology; Fault (geology); Architecture; Paleontology; Archaeology; Acoustics","score_opus":0.04429665835889063,"score_gpt":0.2567664414823604,"score_spread":0.21246978312346976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403014804","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99911743,0.000007841633,0.00035757196,0.00003060153,0.0000014267362,0.0000016964982,0.000051274263,0.000006302847,0.00042576506],"genre_scores_gemma":[0.99965966,0.000009936187,0.0001969803,0.0000029475307,3.9380393e-7,0.0000019556503,0.000049507547,0.0000032193202,0.000075413074],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989927,0.000039657793,0.000007572966,0.000024474015,0.000010447276,0.000018471525],"domain_scores_gemma":[0.9978157,0.0015064619,0.00022957583,0.00021238245,0.00009306155,0.00014286397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006875084,0.00027566045,0.00038275248,0.000425858,0.00036061823,0.00077750155,0.0005884082,0.00071970513,0.0028429166],"category_scores_gemma":[0.004161027,0.00033857397,0.00034135996,0.00040693875,0.00079975615,0.001026703,0.0003731382,0.00074066373,0.00014169709],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001057047,0.0007248579,0.059855387,0.00007325174,0.00016474507,0.00023234573,0.00029967376,0.9053617,0.01692208,0.009563409,0.0005738138,0.005171693],"study_design_scores_gemma":[0.00015072235,0.0002327509,0.023831824,0.0000075324324,0.00005100946,0.000029792198,0.00015525785,0.9696389,0.0016761151,0.0039369646,0.0002684268,0.000020627283],"about_ca_topic_score_codex":0.009050533,"about_ca_topic_score_gemma":0.011521398,"teacher_disagreement_score":0.009050533,"about_ca_system_score_codex":0.0006593365,"about_ca_system_score_gemma":0.00042963788,"threshold_uncertainty_score":0.017995715},"labels":[],"label_agreement":null},{"id":"W4403102495","doi":"10.1785/0220240157","title":"A Stochastic Model for Induced Seismicity at the Geothermal Systems: A Case of the Geysers","year":2024,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Induced seismicity; Geothermal gradient; Geology; Seismology; Microseism; Geophysics","score_opus":0.12799280031066726,"score_gpt":0.33461693285201993,"score_spread":0.20662413254135267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403102495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7880975,0.00015311212,0.2019307,0.0018204456,0.00002924156,0.000046623718,0.0003368631,0.00024019743,0.007345326],"genre_scores_gemma":[0.9947072,0.000052147534,0.0027953535,0.000021713793,0.000013452219,0.000018103216,0.000039212773,0.000008875481,0.0023439317],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99978024,0.00008898539,0.0000079037645,0.000050076676,0.000034152225,0.000038584232],"domain_scores_gemma":[0.99913293,0.0005122502,0.0001937054,0.000036731017,0.000063305735,0.00006107797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007528132,0.00041881425,0.00045417738,0.00040344155,0.0005287651,0.00081522076,0.0011048181,0.0013551202,0.001716604],"category_scores_gemma":[0.0020192934,0.0003674438,0.00054158375,0.00038390266,0.0012944599,0.0007517862,0.0005627869,0.0009163967,0.000119631084],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022141161,0.000020415064,0.00163167,0.0000068746695,0.0000121473595,0.0002758003,0.00005539655,0.9768544,0.00063977484,0.01949355,0.00021536392,0.00077257183],"study_design_scores_gemma":[0.000005416013,0.000007350964,0.00039508127,8.6277794e-7,0.0000032166367,0.000017276307,0.000012286551,0.99723214,0.000042017535,0.002208297,0.00007187938,0.000004296125],"about_ca_topic_score_codex":0.06428094,"about_ca_topic_score_gemma":0.038748395,"teacher_disagreement_score":0.06428094,"about_ca_system_score_codex":0.0015371068,"about_ca_system_score_gemma":0.0009886228,"threshold_uncertainty_score":0.12781352},"labels":[],"label_agreement":null},{"id":"W4403134362","doi":"10.55575/tektonika2024.2.2.47","title":"Signatures of Fluid-Rock Interactions in Shallow Parts of the San Andreas and San Gabriel Faults, Southern California","year":2024,"lang":"en","type":"article","venue":"Tektonika","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"SLAC National Accelerator Laboratory; Biological and Environmental Research; Basic Energy Sciences; National Institute of General Medical Sciences; U.S. Geological Survey; Office of Science; Utah State University; Southern California Earthquake Center; McGill University; U.S. Department of Energy; University Research Coordination Office, De La Salle University; National Institutes of Health; National Science Foundation","keywords":"Geology; San andreas fault; Seismology; Petrology; Geochemistry; Fault (geology)","score_opus":0.015001876255146535,"score_gpt":0.23229071392658562,"score_spread":0.21728883767143908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403134362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993531,0.00006302587,0.000033153472,0.000014239521,5.7140454e-7,0.00000257258,0.00007359524,0.000009634446,0.00045004237],"genre_scores_gemma":[0.9992767,0.00004311365,0.00012890733,0.00000737359,0.0000013723446,0.0000037925129,0.00015213568,0.0000016178254,0.0003849741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.0000045995157,0.0000052107516,0.0000457608,0.000030664007,0.000025297075],"domain_scores_gemma":[0.99984396,0.000012808744,0.000051787774,0.0000074057266,0.000050384067,0.00003361729],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010758434,0.00022275189,0.00022343063,0.00079592137,0.0006373479,0.0005513311,0.00030719052,0.00023823054,0.0005907943],"category_scores_gemma":[0.000268863,0.00022376962,0.00008727383,0.00046737664,0.00038933987,0.0002139614,0.00041391284,0.00016033836,0.00006475305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014318914,0.000059865244,0.96209896,0.00005552192,0.000054686523,0.00024126249,0.0019188812,0.00085803814,0.02500124,0.00014470523,0.00026747683,0.009156126],"study_design_scores_gemma":[0.000004831461,0.0000112260395,0.9990588,0.0000031970999,0.000006238402,0.000017464576,0.0001902099,0.00025439914,0.00020643388,0.000007704868,0.00023756204,0.0000019522618],"about_ca_topic_score_codex":0.23648961,"about_ca_topic_score_gemma":0.46657854,"teacher_disagreement_score":0.23648961,"about_ca_system_score_codex":0.0011287933,"about_ca_system_score_gemma":0.00064845296,"threshold_uncertainty_score":0.47022617},"labels":[],"label_agreement":null},{"id":"W4403136751","doi":"10.1038/s43247-024-01725-9","title":"Fast and full characterization of large earthquakes from prompt elastogravity signals","year":2024,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Grand Équipement National De Calcul Intensif; European Commission","keywords":"Characterization (materials science); Seismology; Geology; Computer science; Materials science; Nanotechnology","score_opus":0.01777093551811974,"score_gpt":0.22298848598148513,"score_spread":0.2052175504633654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403136751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84144735,0.00022391991,0.15291765,0.00030805494,0.00006137693,0.000027503416,0.0016209756,0.0011708409,0.0022222819],"genre_scores_gemma":[0.9827108,0.00007724897,0.014497602,0.000030319872,0.000015817232,0.000008622213,0.0015694635,0.000024618586,0.0010654576],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999335,0.00000707084,0.0000034461114,0.000018754354,0.000018839146,0.0000183562],"domain_scores_gemma":[0.9997818,0.00005752838,0.000034009598,0.00003324062,0.000060060254,0.00003347233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018322554,0.00061500043,0.00022190629,0.00038540023,0.00014056225,0.000323925,0.000266873,0.00032899177,0.0006222519],"category_scores_gemma":[0.0010794259,0.0001670271,0.00016987289,0.00030567922,0.00018075075,0.0005010188,0.0006043291,0.000708733,0.00029162408],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006028641,0.00025162325,0.09202564,0.00017535871,0.0001248803,0.00074972643,0.00032708532,0.44203106,0.15138984,0.002809799,0.007902044,0.30161014],"study_design_scores_gemma":[0.000010412565,0.000049121423,0.039735638,0.000012480228,0.000015472271,0.00008150699,0.000094596646,0.942774,0.014369786,0.0015461392,0.0012885213,0.000022291206],"about_ca_topic_score_codex":0.009584525,"about_ca_topic_score_gemma":0.017466553,"teacher_disagreement_score":0.009584525,"about_ca_system_score_codex":0.00024038808,"about_ca_system_score_gemma":0.00055839797,"threshold_uncertainty_score":0.019057453},"labels":[],"label_agreement":null},{"id":"W4403193676","doi":"10.1007/s10950-024-10248-x","title":"Analysis of the influential factors controlling the occurrence of injection-induced earthquakes in Northeast British Columbia, Canada, using machine-learning-based algorithms","year":2024,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Structural geology; Hydrogeology; Algorithm; Seismology; Geology; Computer science","score_opus":0.015233161798408912,"score_gpt":0.22168207078832783,"score_spread":0.2064489089899189,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403193676","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99737537,0.00016997536,0.000548287,0.00018758139,0.000009206254,0.000012970386,0.00093478966,0.000018163586,0.0007436804],"genre_scores_gemma":[0.9984149,0.00011258553,0.0003201625,0.000013076856,0.000004464584,0.000003996905,0.00066778646,0.0000044379717,0.00045846903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995745,0.00008858288,0.000044666907,0.00008262047,0.00009008295,0.00011954602],"domain_scores_gemma":[0.99567974,0.0014738258,0.00049594266,0.00012204452,0.0017505579,0.00047797587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080872804,0.0004276763,0.00040660874,0.0016652975,0.0012378567,0.0012947595,0.0010240913,0.00045183406,0.0010406119],"category_scores_gemma":[0.0051590065,0.0002554554,0.0004341106,0.002309585,0.0006475673,0.00027563734,0.00042070553,0.00067455135,0.0001502774],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000847335,0.00005518217,0.98149097,0.00002474458,0.00016511015,0.0001302421,0.00020757719,0.008615196,0.00049086317,0.00023078512,0.0007566142,0.0077478923],"study_design_scores_gemma":[0.000011118478,0.000012115861,0.9564664,0.000024042494,0.00009351619,0.000033448017,0.0008805843,0.041493397,0.00022793532,0.00010691246,0.0006373168,0.000013210069],"about_ca_topic_score_codex":0.98100555,"about_ca_topic_score_gemma":0.9881245,"teacher_disagreement_score":0.01899445,"about_ca_system_score_codex":0.0073879906,"about_ca_system_score_gemma":0.013545517,"threshold_uncertainty_score":0.053603888},"labels":[],"label_agreement":null},{"id":"W4403251406","doi":"10.2113/2024/lithosphere_2023_299","title":"The Benkar Fault Zone: An Orogen-Scale Cross Fault in the Eastern Nepal Himalaya","year":2024,"lang":"en","type":"article","venue":"Lithosphere","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Teck (Canada)","funders":"","keywords":"Geology; Fault (geology); Seismology; Scale (ratio); Normal fault; Geography; Cartography","score_opus":0.014115605177614883,"score_gpt":0.2573157925065447,"score_spread":0.2432001873289298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403251406","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935055,0.00027445742,0.00020059216,0.00006943501,0.000002798116,0.000012884696,0.00013863522,0.000010042959,0.00578573],"genre_scores_gemma":[0.99931467,0.00007048935,0.00016391592,0.000012383641,0.0000016120451,0.0000039932493,0.00007812272,0.0000010834335,0.00035370502],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999068,0.000012552688,0.0000063678144,0.000025674337,0.000017785891,0.00003092725],"domain_scores_gemma":[0.9999167,0.000021032512,0.000023270703,0.0000070363208,0.000021291176,0.000010704773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008563747,0.0001327896,0.00011063165,0.0013425894,0.0006006583,0.0006625986,0.00016658255,0.00024187118,0.0014809502],"category_scores_gemma":[0.00028673786,0.000100562946,0.0000691246,0.0014363677,0.00043248612,0.0002869698,0.00048545699,0.0001264677,0.0001484088],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010120697,0.000046045414,0.90492463,0.0001858767,0.000063688814,0.0032602923,0.0084693665,0.0010362348,0.016584568,0.0017811545,0.00046464388,0.06308223],"study_design_scores_gemma":[0.00000468837,0.000022433636,0.99238104,0.000039805684,0.000015818889,0.001108772,0.0025842404,0.000600379,0.00067656586,0.00023820558,0.0023203231,0.0000076265414],"about_ca_topic_score_codex":0.019060062,"about_ca_topic_score_gemma":0.03254195,"teacher_disagreement_score":0.019060062,"about_ca_system_score_codex":0.00043836495,"about_ca_system_score_gemma":0.0003208221,"threshold_uncertainty_score":0.037898242},"labels":[],"label_agreement":null},{"id":"W4403301598","doi":"10.1785/0120240139","title":"Coda Envelope Moment Magnitudes and Source Scaling for Southeastern Canada","year":2024,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Coda; Envelope (radar); Seismology; Scaling; Geology; Moment (physics); Scaling law; Physics; Geometry; Mathematics; Engineering; Telecommunications; Classical mechanics","score_opus":0.01395198823464614,"score_gpt":0.20055167856352102,"score_spread":0.18659969032887488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403301598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9594424,0.0001878251,0.0045542656,0.00031755562,0.000014100943,0.000042618212,0.015769906,0.00047105842,0.019200275],"genre_scores_gemma":[0.9925045,0.000054610726,0.0021759272,0.000013619299,0.0000018880656,0.000008402378,0.0032953129,0.000044902026,0.0019008265],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998518,0.000007878787,0.0000059327244,0.000032523145,0.00006678053,0.000035066972],"domain_scores_gemma":[0.9986413,0.00008370914,0.00010174212,0.000065435546,0.001016276,0.00009142947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026345375,0.00021294704,0.00013535302,0.001523248,0.00073149573,0.00085262395,0.0003588274,0.000132027,0.0034031477],"category_scores_gemma":[0.001541104,0.0001171651,0.0001663673,0.001961739,0.00026539346,0.00021521356,0.00029685858,0.00023232614,0.0003417364],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000179786,0.000057608413,0.81797063,0.00008349988,0.000069357775,0.00028453371,0.0010526449,0.031288125,0.006335092,0.0043097953,0.012536062,0.1258329],"study_design_scores_gemma":[0.000012186999,0.000007666434,0.94819874,0.00002544838,0.000013368637,0.000050740826,0.00066055846,0.03929576,0.0018533234,0.00039319508,0.009466332,0.000022701273],"about_ca_topic_score_codex":0.98529017,"about_ca_topic_score_gemma":0.9898358,"teacher_disagreement_score":0.01470983,"about_ca_system_score_codex":0.012548678,"about_ca_system_score_gemma":0.0076942276,"threshold_uncertainty_score":0.091047406},"labels":[],"label_agreement":null},{"id":"W4403409326","doi":"10.1139/cjes-2024-0095","title":"Crustal stress near the Yakutat microplate collision from probabilistic earthquake focal mechanisms","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Yukon University; University of Calgary; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Collision; Focal mechanism; Probabilistic logic; Stress (linguistics); Tectonics; Statistics; Computer science","score_opus":0.019615462363263426,"score_gpt":0.21567446831904363,"score_spread":0.1960590059557802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403409326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974043,0.000046612633,0.0012815616,0.000048441925,0.0000020177322,0.0000048987827,0.00022448761,0.000026791186,0.00096077524],"genre_scores_gemma":[0.9992173,0.000024486493,0.00045933595,0.0000049811133,0.0000012655606,0.0000023993412,0.00019970995,0.00000387002,0.00008660642],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998826,0.000012421772,0.000009976835,0.00003666094,0.000027939686,0.000030385305],"domain_scores_gemma":[0.9996717,0.000052661904,0.00010425199,0.00004057345,0.00009845748,0.000032417032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026589568,0.00037863266,0.00022381934,0.0007864097,0.00041091413,0.0009094107,0.00044464733,0.0003376667,0.00075700897],"category_scores_gemma":[0.001308481,0.00028773688,0.00027290295,0.0012227753,0.00031769864,0.00064310274,0.00082752935,0.00027448632,0.000101354686],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014393634,0.000038885482,0.8392708,0.00007030126,0.00017106479,0.00053156284,0.00068856817,0.10937155,0.0148369055,0.0018470628,0.00050988974,0.03251958],"study_design_scores_gemma":[0.000021381626,0.00003841623,0.83438134,0.000024369474,0.000077153214,0.00011698508,0.0006920919,0.16091968,0.0017391923,0.001317311,0.00063160167,0.000040429157],"about_ca_topic_score_codex":0.10613044,"about_ca_topic_score_gemma":0.1770459,"teacher_disagreement_score":0.8938696,"about_ca_system_score_codex":0.0011568486,"about_ca_system_score_gemma":0.001357276,"threshold_uncertainty_score":0.21102542},"labels":[],"label_agreement":null},{"id":"W4403449435","doi":"10.1130/abs/2024cd-399493","title":"RADIOGENIC ISOTOPIC DATA FROM CENOZOIC VOLCANIC ROCKS IN THE EUREKA, ELY AND WELLS AREAS DOCUMENT SPATIALLY DISTINCT ARCHEAN AND PROTEROZOIC CRATONIC DOMAINS ACROSS NORTHERN NEVADA, USA","year":2024,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Archean; Proterozoic; Radiogenic nuclide; Cenozoic; Geology; Volcano; Provenance; Geochemistry; Earth science; Precambrian; Paleontology; Tectonics; Mantle (geology); Structural basin","score_opus":0.02685524724462747,"score_gpt":0.25537613799305786,"score_spread":0.2285208907484304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403449435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736625,0.000098820965,0.00004019598,0.000024080322,0.0000019035888,0.0000019420079,0.0011024933,0.0000034234322,0.0013608523],"genre_scores_gemma":[0.9956246,0.00020417024,0.00022383995,0.00001671255,0.0000022560264,0.0000056229846,0.0025137477,0.0000050909716,0.0014041044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999558,0.0000039773718,0.0000055130677,0.000012172556,0.000012461684,0.000010082804],"domain_scores_gemma":[0.99979264,0.0000239641,0.00005407706,0.000011780361,0.00009034371,0.000027141055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013936432,0.00008705764,0.00007940352,0.0011057488,0.00028876276,0.0003369003,0.00020428553,0.00012758982,0.0013325397],"category_scores_gemma":[0.0002978727,0.000092691735,0.00006671341,0.0008540037,0.00018788858,0.00023349111,0.00033917453,0.00010428938,0.00016331593],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015011693,0.00002461497,0.9718974,0.0000333413,0.000046358953,0.00011761774,0.00082740013,0.00024416816,0.011181813,0.00012742374,0.00043433096,0.01491537],"study_design_scores_gemma":[0.0000029431058,0.0000028398688,0.99837506,0.0000046138193,0.00000705379,0.000026563208,0.00036834832,0.0000387169,0.00033666004,0.000009012407,0.00082719064,0.0000010067896],"about_ca_topic_score_codex":0.13423242,"about_ca_topic_score_gemma":0.4337183,"teacher_disagreement_score":0.13423242,"about_ca_system_score_codex":0.00047440434,"about_ca_system_score_gemma":0.0005019736,"threshold_uncertainty_score":0.26690215},"labels":[],"label_agreement":null},{"id":"W4403449555","doi":"10.1130/abs/2024cd-399342","title":"SYNDEPOSITIONAL FAULTING IN THE BELT BASIN: JUST ONE DAMNED TSUNAMI AFTER ANOTHER","year":2024,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Seismology; Structural basin; Geomorphology","score_opus":0.02667413002818606,"score_gpt":0.24173508563362803,"score_spread":0.21506095560544197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403449555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9914209,0.00018779334,0.0001373006,0.00076693774,0.000042816755,0.0000037293669,0.00012977385,0.000014055156,0.0072966125],"genre_scores_gemma":[0.9989742,0.00008638963,0.000043530665,0.000051477826,0.000009365542,8.3837e-7,0.000064223015,0.0000022745012,0.0007676793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999306,0.0000074030636,0.0000061970995,0.00001745724,0.000007879815,0.000030475718],"domain_scores_gemma":[0.99977094,0.000024530033,0.000052316565,0.000024921887,0.000054432276,0.000072853305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014216319,0.00011673709,0.00016643744,0.00043928437,0.001001191,0.0007528935,0.00018764564,0.0004536761,0.004415799],"category_scores_gemma":[0.00086588605,0.00008509482,0.00013016879,0.0007277951,0.0008086359,0.0009086593,0.0006475007,0.0004983026,0.00021146213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002165704,0.00024761047,0.7902704,0.00027139878,0.00017331075,0.0058192266,0.008986362,0.0036293904,0.031211836,0.02608882,0.008157474,0.12297845],"study_design_scores_gemma":[0.00006473185,0.0001693149,0.9742736,0.00006167751,0.00009312217,0.00045618074,0.0061268536,0.001214641,0.0011734325,0.0041812523,0.012161619,0.000023454542],"about_ca_topic_score_codex":0.029678935,"about_ca_topic_score_gemma":0.06344735,"teacher_disagreement_score":0.029678935,"about_ca_system_score_codex":0.00079581444,"about_ca_system_score_gemma":0.0006575371,"threshold_uncertainty_score":0.059012353},"labels":[],"label_agreement":null},{"id":"W4403558078","doi":"10.1029/2024gl109865","title":"Magnitude Clustering During Stick‐Slip Dynamics on Laboratory Faults","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Alberta Innovates; National Science Foundation","keywords":"Magnitude (astronomy); Cluster analysis; Slip (aerodynamics); Geology; Seismology; Statistics; Mathematics; Physics; Engineering; Aerospace engineering","score_opus":0.02669168726084268,"score_gpt":0.2900839262587189,"score_spread":0.2633922389978762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403558078","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99960476,0.000013399276,0.00021112665,0.00000218203,6.8491426e-7,0.0000021294775,0.000047381993,0.000008634647,0.00010980299],"genre_scores_gemma":[0.9998323,0.00000475591,0.000067117166,8.110156e-7,9.785944e-7,0.0000020167386,0.000053687636,0.0000013098661,0.00003697622],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998704,0.000011498689,0.000009355555,0.000037500067,0.000045393135,0.000025900215],"domain_scores_gemma":[0.9995877,0.00007713716,0.0001623489,0.00004781085,0.000061807084,0.00006315916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012993465,0.00011366071,0.00025975195,0.0007159382,0.00018076316,0.0002496185,0.0001623333,0.00014079486,0.0008671609],"category_scores_gemma":[0.0005272545,0.0001152022,0.000118164695,0.0003414374,0.00032501353,0.0001641914,0.0003143031,0.00015063002,0.00010033296],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012149271,0.0001432287,0.25307235,0.00007448578,0.000110095556,0.0003199373,0.00051467516,0.004570723,0.7238681,0.00017479931,0.00019844642,0.015738295],"study_design_scores_gemma":[0.0000071497175,0.00025905704,0.95060134,0.0000027266144,0.000014983684,0.000102585596,0.00018370734,0.007332351,0.041216165,0.000060331357,0.00020642365,0.000013164647],"about_ca_topic_score_codex":0.0013898661,"about_ca_topic_score_gemma":0.0013331661,"teacher_disagreement_score":0.0013898661,"about_ca_system_score_codex":0.00021777063,"about_ca_system_score_gemma":0.00006766138,"threshold_uncertainty_score":0.002900958},"labels":[],"label_agreement":null},{"id":"W4403633022","doi":"10.2139/ssrn.4996091","title":"Cool Transient Lithospheric Thermal Conditions Driven by Subduction Recorded by Neoarchean Diamonds from Knee Lake, Northwestern Superior Craton","year":2024,"lang":"en","type":"preprint","venue":"SSRN Electronic Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Subduction; Lithosphere; Craton; Geology; Transient (computer programming); Thermal; Geochemistry; Petrology; Seismology; Earth science; Tectonics; Geography; Meteorology","score_opus":0.008004168788949571,"score_gpt":0.21109189974415854,"score_spread":0.20308773095520896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403633022","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991715,0.000014928277,0.00001233263,0.000011888712,0.0000012699736,0.0000015926151,0.00021117709,0.00000361266,0.00057174003],"genre_scores_gemma":[0.99943656,0.00001947384,0.000021344184,0.000007085568,0.0000024851627,0.0000019235138,0.00027533757,0.0000024463118,0.00023327138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999579,0.0000027445403,0.0000027044855,0.0000102509985,0.000011524221,0.000014726944],"domain_scores_gemma":[0.9998685,0.000016182736,0.000033338685,0.000009408201,0.00003285238,0.000039602488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011785838,0.000201713,0.00021522894,0.00058134674,0.0005782408,0.00053463323,0.0002299121,0.000343237,0.0018968281],"category_scores_gemma":[0.00034489087,0.00015465007,0.00009057366,0.00073693856,0.000528358,0.00026760143,0.00067517074,0.00025101824,0.00022087006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005671195,0.00005592605,0.9585965,0.000067116125,0.000041896106,0.00073388836,0.0044996236,0.0007083676,0.028190369,0.00020981804,0.0007732998,0.0055561187],"study_design_scores_gemma":[0.0000052999403,0.000010476303,0.9990361,0.0000041853827,0.000003876835,0.000022352302,0.00045702505,0.00010645295,0.00010776347,0.000009825221,0.0002350395,0.0000014906416],"about_ca_topic_score_codex":0.13808319,"about_ca_topic_score_gemma":0.28675565,"teacher_disagreement_score":0.8619168,"about_ca_system_score_codex":0.0006860158,"about_ca_system_score_gemma":0.00069408945,"threshold_uncertainty_score":0.2745589},"labels":[],"label_agreement":null},{"id":"W4403779453","doi":"10.31223/x5xq4j","title":"Multi-Phase Tectonic and Volcanic Evolution of a Nascent Backarc Rift: Impacts of Spreading Centre Reorientation, Subduction Reversals, Ridge Collisions, and Asymmetric Slab Rollback on the Northern New Hebrides Backarc","year":2024,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Materials and Energy Research Center","keywords":"Geology; Subduction; Rift; Volcano; Ridge; Seismology; Tectonics; Slab; New Hebrides; Rift valley; Mid-ocean ridge; Rollback; Paleontology; Geography; Archaeology","score_opus":0.020896555481401208,"score_gpt":0.2549656100011894,"score_spread":0.23406905451978818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403779453","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99881506,0.00003989866,0.000022457447,0.000015537507,9.780641e-7,0.000003966429,0.00009213034,0.0000029246696,0.0010072498],"genre_scores_gemma":[0.99914587,0.00006185068,0.00006632516,0.000009729582,0.000001350858,0.0000052833634,0.0001259072,0.0000024682652,0.00058120134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994445,0.000006846248,0.0000032756466,0.000018001785,0.000011440165,0.000016078813],"domain_scores_gemma":[0.99982005,0.000026564288,0.000044144064,0.000008908679,0.000036586243,0.00006376952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013482013,0.00020681314,0.00016538968,0.0006602848,0.00036183573,0.00097318063,0.00028127467,0.00027037936,0.002371314],"category_scores_gemma":[0.0005871072,0.00018340978,0.000090899,0.00048204194,0.000526949,0.0002436339,0.00047501724,0.00024054812,0.00020185404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002185138,0.00006948544,0.94812095,0.000083748804,0.0001030002,0.0023306326,0.00515939,0.0076079536,0.016983664,0.00084478414,0.0006586264,0.017819319],"study_design_scores_gemma":[0.000005338653,0.000015678128,0.99733526,0.000013778003,0.000009865862,0.00007960067,0.0008083604,0.0011035283,0.0002319338,0.000031382868,0.00036086357,0.0000044072226],"about_ca_topic_score_codex":0.28844383,"about_ca_topic_score_gemma":0.41524154,"teacher_disagreement_score":0.28844383,"about_ca_system_score_codex":0.0020498147,"about_ca_system_score_gemma":0.0010848871,"threshold_uncertainty_score":0.57352984},"labels":[],"label_agreement":null},{"id":"W4403823180","doi":"10.1007/s40098-024-01101-6","title":"Seismic Vulnerability Along the Kaur-South OKU Highway in Bengkulu, Indonesia: Planning for More Resilient and Safer Cities","year":2024,"lang":"en","type":"article","venue":"Indian geotechnical journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Cargill (Canada)","funders":"Universitas Bengkulu","keywords":"SAFER; Vulnerability (computing); Geology; Environmental planning; Environmental science; Computer security; Computer science","score_opus":0.021234450200889963,"score_gpt":0.2558524136186884,"score_spread":0.23461796341779842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403823180","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952217,0.00004020836,0.00011485142,0.00039320128,0.0000045779834,0.00001466765,0.00018981576,0.0000066627754,0.004014334],"genre_scores_gemma":[0.99901354,0.000049419057,0.000098944445,0.000018077644,0.0000017058283,0.00001016122,0.00006394124,0.0000014449273,0.00074280734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987245,0.000028537912,0.0000069180533,0.000015578034,0.000013147729,0.0000634563],"domain_scores_gemma":[0.9997663,0.000022055958,0.000054632143,0.000007778448,0.00004258271,0.00010671196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009726472,0.00023734952,0.00016135367,0.0005448893,0.0011706253,0.0011535715,0.0005567078,0.0005267783,0.0025369036],"category_scores_gemma":[0.00037716067,0.00019602035,0.00020589292,0.00080505235,0.00046899685,0.00073608157,0.0010913378,0.0004452284,0.00023566866],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025002277,0.00039022457,0.9323427,0.00021819107,0.00013910714,0.006549513,0.010776985,0.011070062,0.004368143,0.0054081744,0.0032278504,0.025259042],"study_design_scores_gemma":[0.000009917437,0.00010689086,0.94017076,0.000051273983,0.000061885345,0.0005896792,0.048960384,0.006134171,0.0003810083,0.0009952488,0.0025149428,0.00002385435],"about_ca_topic_score_codex":0.06778788,"about_ca_topic_score_gemma":0.19072221,"teacher_disagreement_score":0.06778788,"about_ca_system_score_codex":0.0017619872,"about_ca_system_score_gemma":0.0027217942,"threshold_uncertainty_score":0.1347866},"labels":[],"label_agreement":null},{"id":"W4403854702","doi":"10.1016/j.epsl.2024.119073","title":"Characterization of bedrock mass-wasting at fault-bound abyssal hills","year":2024,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Agence Nationale de la Recherche","keywords":"Geology; Bedrock; Mass wasting; Abyssal zone; Fault (geology); Geochemistry; Geomorphology; Seismology; Oceanography; Sediment","score_opus":0.010541514241895202,"score_gpt":0.1938767909954455,"score_spread":0.1833352767535503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403854702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99877495,0.000064295804,0.00036337684,0.0000063404996,8.636744e-7,0.000005076624,0.0004325635,0.000021809306,0.00033070854],"genre_scores_gemma":[0.99869835,0.00006332161,0.0004885768,0.000004427672,0.0000018634237,0.0000034445998,0.00062356493,0.0000050534168,0.000111438436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999936,0.0000047432395,0.0000073927604,0.000022077233,0.000014586121,0.000015312868],"domain_scores_gemma":[0.99971324,0.000042497326,0.00011660375,0.00002721624,0.000045979585,0.000054477117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012179121,0.00025042327,0.00019311371,0.001019633,0.00014616553,0.00050062494,0.00023587345,0.00017636517,0.000993975],"category_scores_gemma":[0.0004764323,0.0001166652,0.00022218956,0.0010336782,0.00024169392,0.00024785998,0.00031079742,0.000113859554,0.00018273354],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006304095,0.000022858063,0.9644287,0.00007659878,0.000057920453,0.0003938061,0.00029578005,0.0071214065,0.018989671,0.00014863753,0.00015711265,0.008244358],"study_design_scores_gemma":[0.0000027994015,0.00001663088,0.9931299,0.0000053639,0.000010025596,0.00013042112,0.00013350084,0.005815353,0.0005718453,0.000031302203,0.00014888821,0.000003915894],"about_ca_topic_score_codex":0.016766487,"about_ca_topic_score_gemma":0.035684876,"teacher_disagreement_score":0.016766487,"about_ca_system_score_codex":0.0002449527,"about_ca_system_score_gemma":0.00021188396,"threshold_uncertainty_score":0.033337772},"labels":[],"label_agreement":null},{"id":"W4403978959","doi":"10.1016/b978-0-443-18987-6.00009-9","title":"Tsunamis triggered by splay faulting","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Seismology","score_opus":0.013920168349221423,"score_gpt":0.21605274777234135,"score_spread":0.20213257942311993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403978959","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03802651,0.006187172,0.003989108,0.0003546724,0.0005085164,0.000014174541,0.00038354003,0.00025676144,0.9502795],"genre_scores_gemma":[0.2759636,0.013051821,0.0019559306,0.00017818897,0.00048846204,0.000013468758,0.0007395186,0.000106512874,0.7075024],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999839,0.0000013363139,0.0000011648613,0.0000030286471,0.000008052074,0.000002476537],"domain_scores_gemma":[0.99996305,0.000012976065,0.0000061995174,0.000004708834,0.000009167144,0.0000038774174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000040602743,0.00021116534,0.000073083196,0.00026579303,0.00011645136,0.00073500414,0.0001716838,0.00026647787,0.02625596],"category_scores_gemma":[0.00013555982,0.000078438636,0.00006660394,0.0003706545,0.00019332024,0.00045786359,0.00022187561,0.00022998995,0.0040569766],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015895143,0.000043255073,0.00401501,0.00029290005,0.000021263042,0.0019747857,0.0010315726,0.007993198,0.023864202,0.09934056,0.10915009,0.7521142],"study_design_scores_gemma":[0.000013182216,0.0000711982,0.030486442,0.0001688077,0.000012861253,0.0014520492,0.00051941193,0.0028252264,0.002754943,0.0331788,0.9285059,0.000011199569],"about_ca_topic_score_codex":0.0027006497,"about_ca_topic_score_gemma":0.0045179026,"teacher_disagreement_score":0.02625596,"about_ca_system_score_codex":0.00025337128,"about_ca_system_score_gemma":0.00012955298,"threshold_uncertainty_score":0.087834954},"labels":[],"label_agreement":null},{"id":"W4403978966","doi":"10.1016/b978-0-443-18987-6.00003-8","title":"Tsunami propagation and runup modeling","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Western University","funders":"","keywords":"Geology; Geography; Seismology","score_opus":0.019837687140778208,"score_gpt":0.21263729585125413,"score_spread":0.1927996087104759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403978966","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.017853918,0.004502745,0.5471809,0.0011917661,0.00069840706,0.00005461225,0.0036124114,0.008955187,0.41595012],"genre_scores_gemma":[0.20346734,0.008798782,0.14484851,0.00025535378,0.00035757263,0.00014458984,0.005164447,0.0025343453,0.634429],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999492,0.00000779816,0.0000027455792,0.000009519107,0.000026156524,0.000004663129],"domain_scores_gemma":[0.99992716,0.000025335019,0.0000049845003,0.000013455917,0.000022762613,0.0000062147333],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001057671,0.00080909027,0.00048554398,0.00033137243,0.00022878157,0.0012655817,0.0009825274,0.00066036533,0.028563369],"category_scores_gemma":[0.00033116178,0.00040586945,0.00040807776,0.0006163077,0.0002088789,0.0011986027,0.000525389,0.00057933474,0.008963855],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021065007,0.000027113345,0.0004258795,0.00007359523,0.000028937027,0.00007674019,0.000047039088,0.7904945,0.0016546214,0.033500843,0.037144974,0.13650468],"study_design_scores_gemma":[0.0000060403604,0.000007944199,0.00031899128,0.000028010607,0.000010997298,0.00003666315,0.000020611677,0.8912951,0.0005300746,0.021686258,0.086048946,0.000010370065],"about_ca_topic_score_codex":0.02792422,"about_ca_topic_score_gemma":0.022808418,"teacher_disagreement_score":0.028563369,"about_ca_system_score_codex":0.00049447996,"about_ca_system_score_gemma":0.00058917346,"threshold_uncertainty_score":0.095554054},"labels":[],"label_agreement":null},{"id":"W4403978968","doi":"10.1016/b978-0-443-18987-6.00008-7","title":"Informing megathrust tsunami source models with knowledge of tectonics and fault mechanics","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Tectonics; Seismology; Geology; Fault (geology)","score_opus":0.015103488032418448,"score_gpt":0.2054805797685795,"score_spread":0.19037709173616105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403978968","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.045516685,0.0006151404,0.9187213,0.0010714579,0.00012472738,0.00003399738,0.00197914,0.002968798,0.028968768],"genre_scores_gemma":[0.64606017,0.002164891,0.3225359,0.00021188827,0.00014863795,0.00009436711,0.0045172684,0.0010006302,0.023266254],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993443,0.000018769008,0.000004677602,0.000013632222,0.000023707591,0.000004746173],"domain_scores_gemma":[0.99952734,0.00034399208,0.000025109865,0.000047639114,0.000043170843,0.000012746644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002566421,0.0005830458,0.00038798232,0.0003345247,0.00019272907,0.0015127683,0.0006694353,0.0009915422,0.008411084],"category_scores_gemma":[0.0017473566,0.0005106528,0.0003984128,0.0004311849,0.00024712092,0.0022553082,0.00064521463,0.00070408185,0.0017715135],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019745714,0.00001382979,0.0007423692,0.000032742,0.000022162076,0.00005795292,0.000046021156,0.94416875,0.0014562585,0.013678561,0.0028759206,0.036885686],"study_design_scores_gemma":[0.0000031146064,0.0000035148212,0.00010718362,0.0000067125084,0.0000054081665,0.000014931046,0.000014954402,0.97917366,0.00040086443,0.017080331,0.0031860159,0.0000033648864],"about_ca_topic_score_codex":0.00864359,"about_ca_topic_score_gemma":0.012997134,"teacher_disagreement_score":0.00864359,"about_ca_system_score_codex":0.00046998073,"about_ca_system_score_gemma":0.0005641263,"threshold_uncertainty_score":0.028137863},"labels":[],"label_agreement":null},{"id":"W4403978977","doi":"10.1016/b978-0-443-18987-6.00023-3","title":"Long-term tsunami risk considering time-dependent earthquake hazard and nonstationary sea-level rise","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Term (time); Hazard; Seismology; Geology; Environmental science; Physics","score_opus":0.020711153742880684,"score_gpt":0.22352315254498215,"score_spread":0.20281199880210146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403978977","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14349797,0.020603966,0.40324822,0.0049847886,0.0015086703,0.000042928474,0.0011599418,0.000369663,0.42458382],"genre_scores_gemma":[0.7876395,0.014121536,0.018031072,0.00023444346,0.0011608428,0.000034654033,0.00055334833,0.00020985855,0.17801477],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999219,0.000019929093,0.0000047421145,0.000013706408,0.000026082898,0.000013525321],"domain_scores_gemma":[0.9996661,0.00023142423,0.000029223018,0.000013885056,0.00003950214,0.000019922247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002763138,0.0006693387,0.0004258513,0.00032558915,0.00018141516,0.0012622981,0.0008894467,0.00091954705,0.010016993],"category_scores_gemma":[0.0010840488,0.00033012597,0.0005066258,0.000607774,0.00037357438,0.0014206588,0.0005653153,0.0009200642,0.001015418],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043734013,0.0000703711,0.003950323,0.00015758717,0.00012408302,0.00081767427,0.00012208603,0.69288695,0.0018288523,0.20218176,0.014125902,0.08369061],"study_design_scores_gemma":[0.0000070414335,0.00012180699,0.007158448,0.00012390406,0.00010158717,0.00043746113,0.00022512108,0.6144007,0.00036585997,0.35123333,0.025790015,0.00003472893],"about_ca_topic_score_codex":0.004642262,"about_ca_topic_score_gemma":0.007956374,"teacher_disagreement_score":0.010016993,"about_ca_system_score_codex":0.0006983562,"about_ca_system_score_gemma":0.0006614616,"threshold_uncertainty_score":0.033510208},"labels":[],"label_agreement":null},{"id":"W4403979115","doi":"10.1016/b978-0-443-18987-6.00006-3","title":"Tsunami disaster risk reduction and management","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Western University","funders":"","keywords":"Reduction (mathematics); Disaster risk reduction; Emergency management; Risk management; Business; Environmental planning; Geography; Political science; Mathematics; Finance","score_opus":0.012093584642047827,"score_gpt":0.20576698212707434,"score_spread":0.19367339748502652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403979115","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0020273668,0.013323213,0.0064628664,0.004188411,0.0009205084,0.000027556714,0.00043147884,0.00031501878,0.9723036],"genre_scores_gemma":[0.009794682,0.0117531195,0.0030591239,0.00035609145,0.00027300758,0.000014605595,0.00025867615,0.00007860849,0.97441214],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99991095,0.000008930391,0.0000038305097,0.000011590934,0.00005520957,0.000009463611],"domain_scores_gemma":[0.99991214,0.000021583652,0.0000072970433,0.000006986341,0.000035910663,0.000016100943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021550286,0.0004818874,0.0001902587,0.0006777308,0.00030073215,0.0023260687,0.0004051549,0.0007562649,0.10738156],"category_scores_gemma":[0.00037318,0.00012672374,0.000101660946,0.00090815005,0.0002711342,0.0011205011,0.0005866331,0.0006258126,0.027008576],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012565634,0.000031494943,0.00028717375,0.00011083451,0.0000043150644,0.00006834714,0.00016287205,0.0017829774,0.0008200514,0.03554012,0.32301554,0.6381637],"study_design_scores_gemma":[0.0000018135652,0.000010743713,0.00048090413,0.00010619634,0.0000023315306,0.00006360193,0.00016129707,0.0005575594,0.00016068785,0.011384005,0.98706764,0.0000032439998],"about_ca_topic_score_codex":0.010320766,"about_ca_topic_score_gemma":0.017924596,"teacher_disagreement_score":0.10738156,"about_ca_system_score_codex":0.0008275191,"about_ca_system_score_gemma":0.0011523295,"threshold_uncertainty_score":0.35922706},"labels":[],"label_agreement":null},{"id":"W4403979215","doi":"10.1016/b978-0-443-18987-6.00005-1","title":"Probabilistic tsunami hazard and risk assessments","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Western University","funders":"","keywords":"Probabilistic logic; Hazard; Probabilistic risk assessment; Computer science; Environmental science; Artificial intelligence; Biology","score_opus":0.018125378800016717,"score_gpt":0.24015551978243438,"score_spread":0.22203014098241766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403979215","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008108543,0.012915703,0.47969666,0.0032440387,0.0006801347,0.000077001656,0.002283812,0.0015088987,0.49148524],"genre_scores_gemma":[0.2453447,0.03185145,0.13793369,0.0005587904,0.0014300612,0.00019052342,0.003420141,0.0006925455,0.5785782],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996685,0.000082964536,0.000014910441,0.00003376908,0.00018817806,0.000011771149],"domain_scores_gemma":[0.99929225,0.00043317492,0.000050298284,0.000060484017,0.00014102587,0.000022773147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008441013,0.000795573,0.00041709346,0.001188764,0.00020301483,0.0017870374,0.0007174781,0.00059282297,0.04744834],"category_scores_gemma":[0.0031741566,0.00039402398,0.00033915867,0.0013653934,0.00046659648,0.0016899551,0.00067865854,0.0007098828,0.0072673922],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039440132,0.000037083595,0.0016181554,0.00019687183,0.000053062075,0.00009908187,0.00006974532,0.14149041,0.00068114087,0.18146098,0.08107284,0.5931812],"study_design_scores_gemma":[0.000010062503,0.00004621505,0.0030480807,0.00024031507,0.00003686715,0.00032624518,0.00012032995,0.15531915,0.00048479467,0.5583805,0.28195372,0.000033770142],"about_ca_topic_score_codex":0.003850755,"about_ca_topic_score_gemma":0.0063518942,"teacher_disagreement_score":0.04744834,"about_ca_system_score_codex":0.0007337358,"about_ca_system_score_gemma":0.0006417992,"threshold_uncertainty_score":0.1587305},"labels":[],"label_agreement":null},{"id":"W4403979219","doi":"10.1016/b978-0-443-18987-6.00002-6","title":"Tsunami generation","year":2024,"lang":"en","type":"book-chapter","venue":"Elsevier eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Western University","funders":"","keywords":"Geography; Environmental science; Geology","score_opus":0.024898339840627882,"score_gpt":0.21946820858469224,"score_spread":0.19456986874406434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403979219","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0020922646,0.0033009166,0.0028459667,0.0005215126,0.00039353955,0.000023242748,0.0006833858,0.00038387004,0.98975533],"genre_scores_gemma":[0.01060296,0.003192371,0.0011818174,0.00009006913,0.000081297534,0.000012771327,0.0007213454,0.00009134175,0.984026],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99995136,0.0000031506702,0.000002421095,0.000010955488,0.000025203546,0.0000069737735],"domain_scores_gemma":[0.9999542,0.000005680381,0.0000029996659,0.000009999135,0.00001848334,0.00000863424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009440192,0.0005597536,0.00016391702,0.00076965225,0.00039995665,0.0016988437,0.00038610297,0.0004134028,0.1977024],"category_scores_gemma":[0.00023636084,0.00019255621,0.00016735264,0.00079189515,0.00020862155,0.00097603136,0.00060627214,0.0005585915,0.06422677],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029801653,0.000025422461,0.0004517853,0.000093358576,0.0000050509375,0.000090082416,0.00018567774,0.00095047423,0.0017208526,0.06196166,0.21831322,0.7161726],"study_design_scores_gemma":[0.000003871925,0.000011284919,0.00084942195,0.000051563373,0.0000028836391,0.00011328629,0.00007122718,0.0003353754,0.00039895508,0.0091481805,0.9890105,0.0000034203915],"about_ca_topic_score_codex":0.005267197,"about_ca_topic_score_gemma":0.01015186,"teacher_disagreement_score":0.1977024,"about_ca_system_score_codex":0.0007034959,"about_ca_system_score_gemma":0.0006904191,"threshold_uncertainty_score":0.6613804},"labels":[],"label_agreement":null},{"id":"W4404099202","doi":"10.59150/ibgm2002a07","title":"Relocation and Stress Analysis of the 2018 Mandali-Sumar Earthquake Sequence, Iraq-Iran Border","year":2024,"lang":"en","type":"article","venue":"Iraqi Bulletin of Geology and Mining","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research","keywords":"Relocation; Sequence (biology); Seismology; Geology; Computer science","score_opus":0.01882379956390973,"score_gpt":0.24648345144750577,"score_spread":0.22765965188359605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404099202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99877506,0.00003978744,0.00017937103,0.00003173814,0.000007895758,0.000010652907,0.00040978208,0.000015083877,0.00053070794],"genre_scores_gemma":[0.99720997,0.000058933765,0.00075544143,0.000012249004,0.000019816069,0.000018301298,0.0015038368,0.0000070636493,0.00041439923],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998616,0.000011486092,0.000015280206,0.000032393516,0.000042640168,0.000036588917],"domain_scores_gemma":[0.999729,0.000015527228,0.00008224015,0.000019050756,0.00012008031,0.00003408462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018262796,0.00024561828,0.00020322787,0.0018483214,0.00035824877,0.0002854967,0.00029537585,0.00020855015,0.0007727694],"category_scores_gemma":[0.00071737013,0.00011330427,0.00019333184,0.0015343473,0.00018843003,0.00021698489,0.00034430754,0.00018115932,0.00027392662],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003155818,0.00018699662,0.9240512,0.000076912955,0.00006974305,0.0019615544,0.0022895557,0.0030914014,0.015286394,0.00038240556,0.003115021,0.049173243],"study_design_scores_gemma":[0.0000075696594,0.000027927817,0.9955585,0.0000057463935,0.000012568501,0.0001223171,0.0007898768,0.0018254889,0.0005340253,0.00003629665,0.0010730324,0.000006691997],"about_ca_topic_score_codex":0.023605542,"about_ca_topic_score_gemma":0.028924566,"teacher_disagreement_score":0.023605542,"about_ca_system_score_codex":0.00041539577,"about_ca_system_score_gemma":0.00038756535,"threshold_uncertainty_score":0.046936333},"labels":[],"label_agreement":null},{"id":"W4404106534","doi":"10.3390/geosciences14110300","title":"Investigation of the Effect of Integrated Offset, GPS, and InSAR Data in the Stochastic Source Modeling of the 2002 Denali Earthquake","year":2024,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Interferometric synthetic aperture radar; Global Positioning System; Offset (computer science); Geodesy; Geology; Source model; Seismology; Remote sensing; Computer science; Synthetic aperture radar; Telecommunications","score_opus":0.030793828581830354,"score_gpt":0.22882964413146317,"score_spread":0.19803581554963282,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404106534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870604,0.0002571822,0.011683936,0.00010963879,0.000013580941,0.000020324393,0.0002752631,0.00009458389,0.00048514706],"genre_scores_gemma":[0.9941017,0.00014598403,0.0049455944,0.000017937438,0.000012201325,0.000010782696,0.000617184,0.000018098288,0.00013045203],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987134,0.0006161622,0.0001066433,0.0002479578,0.00023051193,0.00008534157],"domain_scores_gemma":[0.9855149,0.011126014,0.0012081835,0.00094767933,0.0010121544,0.00019109675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003329008,0.0007897019,0.0005443868,0.00067606574,0.000359479,0.0009576429,0.0005349717,0.00058007234,0.00026480076],"category_scores_gemma":[0.017003782,0.00042102992,0.0006346291,0.0008391772,0.000365605,0.0011629725,0.00084853347,0.0006047679,0.000109652785],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013825091,0.00040214535,0.29133716,0.00020656394,0.00082841533,0.0006808418,0.00038118276,0.6067239,0.024507875,0.0011557153,0.00043243048,0.07196138],"study_design_scores_gemma":[0.000043925727,0.00026885097,0.15432546,0.000026783306,0.0003663252,0.00013930736,0.00018222515,0.83090836,0.012782697,0.0002657598,0.0006389952,0.000051264342],"about_ca_topic_score_codex":0.015346732,"about_ca_topic_score_gemma":0.018288752,"teacher_disagreement_score":0.015346732,"about_ca_system_score_codex":0.0005734114,"about_ca_system_score_gemma":0.00063360354,"threshold_uncertainty_score":0.030514836},"labels":[],"label_agreement":null},{"id":"W4404298568","doi":"10.1038/s43247-024-01864-z","title":"Fluid upwelling across the Hikurangi subduction thrust during deep slow-slip earthquakes","year":2024,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; University of Ottawa","keywords":"Subduction; Geology; Upwelling; Seismology; Episodic tremor and slip; Thrust; Slip (aerodynamics); Oceanography; Tectonics","score_opus":0.02336188097114945,"score_gpt":0.23383221127621423,"score_spread":0.2104703303050648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404298568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996137,0.000013728737,0.000104823754,0.000020439767,0.0000018126485,0.0000019805186,0.00004120968,0.000010413857,0.00019201558],"genre_scores_gemma":[0.99985754,0.000011213018,0.000042311516,0.0000024402946,8.959885e-7,0.0000011446607,0.000026173862,0.0000018004538,0.000056330817],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999443,0.000006874616,0.0000048905295,0.000017998933,0.000007751174,0.000018131072],"domain_scores_gemma":[0.9999044,0.000015211679,0.000025283853,0.000006927742,0.00001759234,0.000030521365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000121794335,0.0003709656,0.00033617744,0.00043324352,0.0004642314,0.0006401681,0.0002863876,0.0005020117,0.0010214653],"category_scores_gemma":[0.00036902667,0.00040954852,0.0004842343,0.00027479243,0.00054355926,0.0004931164,0.00064123084,0.0002772197,0.00010812151],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073119346,0.0004156222,0.72430223,0.00012180574,0.0002301781,0.0016348307,0.0009963491,0.08694888,0.1713451,0.0006359793,0.00039324863,0.01224469],"study_design_scores_gemma":[0.0000651054,0.00024123977,0.8880628,0.000011061476,0.00004696805,0.00009663567,0.000546223,0.10768071,0.0027842887,0.00021710432,0.00021142284,0.00003640933],"about_ca_topic_score_codex":0.03838363,"about_ca_topic_score_gemma":0.023228332,"teacher_disagreement_score":0.03838363,"about_ca_system_score_codex":0.0007903151,"about_ca_system_score_gemma":0.00057336106,"threshold_uncertainty_score":0.07632041},"labels":[],"label_agreement":null},{"id":"W4404362014","doi":"10.21203/rs.3.rs-5017726/v1","title":"Characteristic Earthquake Recurrence and Time-Dependent Seismic Hazard Modeling for the North and East Anatolian Faults","year":2024,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Seismology; Seismic hazard; Geology; Hazard; Earthquake scenario; Seismic microzonation","score_opus":0.06407922730097566,"score_gpt":0.3187859251809261,"score_spread":0.25470669787995043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404362014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99112236,0.0001571542,0.007545966,0.000108561944,0.000007037951,0.000007039884,0.00022051965,0.00004228832,0.0007889916],"genre_scores_gemma":[0.9984902,0.000057270034,0.0007483978,0.00000236164,0.0000036058957,0.000007070674,0.00010160824,0.000010330204,0.0005792515],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999559,0.000011573584,0.0000040843406,0.00001636426,0.0000042186675,0.000007992122],"domain_scores_gemma":[0.9997011,0.00014889195,0.00007648981,0.00001599262,0.000042631495,0.000014840363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020859948,0.00032892247,0.000335443,0.00041848997,0.00025415447,0.00053054316,0.0006205116,0.00059668015,0.0008114371],"category_scores_gemma":[0.00094866956,0.000310742,0.00037506316,0.0003582735,0.0002090381,0.00045992344,0.00022361563,0.0002867663,0.0000977524],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008736064,0.000028872926,0.01889023,0.000023576657,0.0000435257,0.00013164195,0.00007835418,0.9722402,0.0011064336,0.0014203739,0.00026891864,0.00568058],"study_design_scores_gemma":[0.0000026261287,0.000004314001,0.0019320946,0.000001317763,0.000006011458,0.000010504395,0.000010443086,0.9977602,0.000077915254,0.00015311282,0.00003965705,0.000001794439],"about_ca_topic_score_codex":0.04240872,"about_ca_topic_score_gemma":0.026795276,"teacher_disagreement_score":0.04240872,"about_ca_system_score_codex":0.0006750813,"about_ca_system_score_gemma":0.0005778868,"threshold_uncertainty_score":0.084323704},"labels":[],"label_agreement":null},{"id":"W4404407156","doi":"10.1016/j.eqrea.2024.100350","title":"Reexamination confirming additional seismic evidence for the 12 May 2010 low-yield nuclear test","year":2024,"lang":"en","type":"article","venue":"Earthquake research advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Yield (engineering); Nuclear test; Geology; Seismology; Materials science; Test site; Metallurgy","score_opus":0.13288556151955536,"score_gpt":0.35815292622388656,"score_spread":0.2252673647043312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404407156","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99174225,0.00009795058,0.0026182828,0.00018338903,0.00003158199,0.000022568673,0.00041496067,0.000063680236,0.004825331],"genre_scores_gemma":[0.99717736,0.00005517512,0.0010929542,0.000048380403,0.000019712923,0.000006725315,0.0006308722,0.000010416709,0.0009584936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997576,0.000025518246,0.000025961957,0.00005448644,0.000093019014,0.000043441378],"domain_scores_gemma":[0.9982888,0.00024507,0.0005649086,0.00015737608,0.0005229072,0.00022091552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050120294,0.00026650328,0.00024900783,0.00130117,0.00044348236,0.0005130972,0.00040747583,0.00040705942,0.00097583473],"category_scores_gemma":[0.0022382361,0.000107434564,0.00012792864,0.0010337658,0.0004079309,0.00045084537,0.00051429047,0.0005391026,0.00028481078],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005338085,0.00014550834,0.90265614,0.0001222249,0.00005247235,0.0028959971,0.001876014,0.0019196051,0.033457763,0.0012406555,0.0025872863,0.05251254],"study_design_scores_gemma":[0.00000869785,0.00015324299,0.9856996,0.000023078845,0.0000267293,0.00059179595,0.0010179719,0.0029408261,0.005145782,0.00022610767,0.004152301,0.0000139184895],"about_ca_topic_score_codex":0.010724393,"about_ca_topic_score_gemma":0.038021058,"teacher_disagreement_score":0.010724393,"about_ca_system_score_codex":0.0006855038,"about_ca_system_score_gemma":0.0004960773,"threshold_uncertainty_score":0.02132392},"labels":[],"label_agreement":null},{"id":"W4404424955","doi":"10.1029/2024jb029506","title":"Brittle Regime Slip Partitioned Damage and Deformation Mechanisms Along the Eastern Denali Fault Zone in Southwestern Yukon","year":2024,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Geology; Brittleness; Slip (aerodynamics); Seismology; Deformation (meteorology); Geotechnical engineering; Materials science; Engineering; Composite material","score_opus":0.03945882148677169,"score_gpt":0.30474166530980784,"score_spread":0.26528284382303613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404424955","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996743,0.00003951814,0.000023347187,0.000004097292,2.5761042e-7,0.0000017774559,0.000102344704,0.0000026621365,0.00015166547],"genre_scores_gemma":[0.9994825,0.000037997004,0.00004997695,0.000003341153,2.2655273e-7,0.0000023701928,0.00026150738,6.712581e-7,0.00016142837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999105,0.000005398761,0.000009230842,0.000026237729,0.000017111523,0.000031484615],"domain_scores_gemma":[0.9998621,0.000010966217,0.000041821953,0.000012052605,0.000048121212,0.000024881245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000092327144,0.00019177311,0.00021869742,0.00093564333,0.0004844423,0.000377377,0.00029690727,0.00020958173,0.00055235653],"category_scores_gemma":[0.0001644871,0.0001586751,0.00012310523,0.0010381835,0.0003119162,0.00020250908,0.00036664846,0.00007813867,0.0000680382],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004905285,0.000014227991,0.98195165,0.000040832452,0.00005040462,0.0002907376,0.0007985143,0.0004927032,0.00969077,0.00009269025,0.00008122052,0.006447132],"study_design_scores_gemma":[0.0000011484226,0.000006869434,0.99904007,0.0000031103307,0.000005762877,0.000043128486,0.00040797127,0.00020323349,0.00013991419,0.000008532841,0.00013849938,0.0000016721515],"about_ca_topic_score_codex":0.2520039,"about_ca_topic_score_gemma":0.55058396,"teacher_disagreement_score":0.7479961,"about_ca_system_score_codex":0.0011435698,"about_ca_system_score_gemma":0.0009421046,"threshold_uncertainty_score":0.5010742},"labels":[],"label_agreement":null},{"id":"W4404484335","doi":"10.1080/07038992.2024.2424768","title":"RADARSAT-2 DInSAR and GNSS-Derived Finite Fault Model of the 2012 Mw 7.8 Haida Gwaii Earthquake","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"GNSS applications; Seismology; Geography; Georeference; Fault (geology); Geology; Remote sensing; Global Positioning System; Computer science; Physical geography; Telecommunications","score_opus":0.023670493292229387,"score_gpt":0.20724965860782707,"score_spread":0.18357916531559768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404484335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99043953,0.000085763044,0.004523343,0.000085484025,0.000022920158,0.000021936532,0.0015290987,0.00018276079,0.0031091415],"genre_scores_gemma":[0.9974981,0.000043180233,0.00092930044,0.000009320424,0.0000035535602,0.000009193636,0.0009898132,0.000011936067,0.00050556206],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994683,0.0000076387905,0.0000035644996,0.000017506072,0.000009858536,0.000014537424],"domain_scores_gemma":[0.99993205,0.000014128914,0.000011283185,0.000010124866,0.000020804991,0.000011460553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009945849,0.00044220983,0.00028319214,0.0004243323,0.00026890554,0.00045387074,0.00057048915,0.00047206067,0.000990222],"category_scores_gemma":[0.00029339353,0.00025011497,0.00036102827,0.0003607487,0.00022073787,0.00039618468,0.00020302761,0.0003147571,0.00026743588],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008661236,0.00008558093,0.014398712,0.00002698587,0.00004078703,0.00020109382,0.000041080308,0.97571295,0.0029478716,0.00045983007,0.00057067204,0.0054277885],"study_design_scores_gemma":[0.00001457882,0.00001796123,0.0109935,0.0000042420716,0.000012876209,0.000020314868,0.000021806065,0.9883646,0.00026200953,0.00009565461,0.00018138626,0.000011084616],"about_ca_topic_score_codex":0.16072142,"about_ca_topic_score_gemma":0.11573781,"teacher_disagreement_score":0.8392786,"about_ca_system_score_codex":0.0009267499,"about_ca_system_score_gemma":0.000943563,"threshold_uncertainty_score":0.31957185},"labels":[],"label_agreement":null},{"id":"W4404510774","doi":"10.1093/gji/ggae413","title":"The effect of earthquake fault rupture kinematics on tsunami generation: a numerical study of real events","year":2024,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Council for Science, Technology and Innovation; Swine Innovation Porc","keywords":"Geology; Seismology; Kinematics; Earthquake rupture; Fault (geology); Earthquake simulation; Types of earthquake; Remotely triggered earthquakes; Foreshock; Intraplate earthquake; Interplate earthquake; Tsunami earthquake; Geodesy; Seismic gap; Aftershock; Tectonics","score_opus":0.014376743696837464,"score_gpt":0.2712513797461808,"score_spread":0.25687463604934335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404510774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99886465,0.000029396653,0.00047872684,0.000030206691,0.0000030363358,0.000005680879,0.0000940318,0.000015945763,0.00047843409],"genre_scores_gemma":[0.9994288,0.000022095031,0.0003474646,0.000004672687,0.0000020642644,0.0000056954386,0.00008006828,0.000003435367,0.00010580621],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997681,0.000090300826,0.00002279777,0.000041336934,0.000031114116,0.000046417896],"domain_scores_gemma":[0.9977787,0.0015572303,0.0002703236,0.00015252906,0.00012815933,0.00011303983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056888646,0.0003295596,0.00044460665,0.0005620506,0.0003700998,0.0006656633,0.0005056182,0.000901436,0.0013309821],"category_scores_gemma":[0.0032948127,0.00036111395,0.000572953,0.00066364865,0.00071737217,0.00063035666,0.00044547208,0.0005824455,0.00011760489],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002724282,0.0002783514,0.06365816,0.00005967368,0.000095460986,0.0005014101,0.00012120685,0.92756784,0.00350437,0.0006502338,0.00020602414,0.0030849339],"study_design_scores_gemma":[0.00005160276,0.0002038437,0.03169232,0.000009223603,0.00002926702,0.00008348967,0.00013712709,0.96629053,0.0011224487,0.00020207095,0.00015790894,0.000020128113],"about_ca_topic_score_codex":0.008939096,"about_ca_topic_score_gemma":0.004536696,"teacher_disagreement_score":0.008939096,"about_ca_system_score_codex":0.00059396285,"about_ca_system_score_gemma":0.00023394483,"threshold_uncertainty_score":0.017774105},"labels":[],"label_agreement":null},{"id":"W4404511863","doi":"10.1016/j.rines.2024.100045","title":"On the use of displaced river terraces to characterize active tectonics of the Zagros orogenic belt, SW Iran","year":2024,"lang":"en","type":"article","venue":"Results in Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Terry Fox Research Institute","funders":"State Key Laboratory of Geological Processes and Mineral Resources; China University of Geosciences, Wuhan; National Natural Science Foundation of China","keywords":"Geology; Tectonics; River terraces; Geochemistry; Active fault; Geomorphology; Earth science; Seismology; Fluvial","score_opus":0.06741293631583145,"score_gpt":0.25484558015767345,"score_spread":0.187432643841842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404511863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985073,0.00009189209,0.00025717882,0.000023270637,0.000002742342,0.000012657626,0.00024139241,0.000008135503,0.0008553685],"genre_scores_gemma":[0.9977387,0.00008634114,0.0015312276,0.000009105237,0.0000032513874,0.000006934765,0.00033771878,0.0000027724686,0.0002839862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999031,0.000019162082,0.0000074356767,0.000033307104,0.000018740624,0.000018276496],"domain_scores_gemma":[0.9998617,0.000024236602,0.00004284345,0.000011826879,0.000041548825,0.000017852264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030987518,0.0002306063,0.000090461705,0.0017148808,0.00027890416,0.00048762167,0.00025614412,0.00014140044,0.00044589036],"category_scores_gemma":[0.00040759196,0.00009396651,0.00016269622,0.0010963525,0.00022917455,0.00021108784,0.00025471384,0.000120308556,0.00015012213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008862931,0.00004055908,0.9467992,0.000036589416,0.000028507173,0.0002767505,0.0011131145,0.00087563804,0.0072294488,0.00010312171,0.00021124301,0.04319719],"study_design_scores_gemma":[0.0000042637803,0.000032528344,0.99598384,0.0000100504185,0.000011635563,0.00009046973,0.0012380303,0.0016512823,0.00039757704,0.0000324772,0.00054399064,0.000003944037],"about_ca_topic_score_codex":0.042186953,"about_ca_topic_score_gemma":0.114014514,"teacher_disagreement_score":0.042186953,"about_ca_system_score_codex":0.00034511072,"about_ca_system_score_gemma":0.00036012282,"threshold_uncertainty_score":0.08388281},"labels":[],"label_agreement":null},{"id":"W4404527300","doi":"10.1785/0120240143","title":"Source-Scaling Comparison and Validation for Ridgecrest, California: Radiated Energy, Apparent Stress, and Mw Using the Coda Calibration Tool (2.6&amp;lt;Mw&amp;lt;7.1)","year":2024,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Coda; Calibration; Scaling; Energy (signal processing); Stress (linguistics); Seismology; Environmental science; Geology; Mathematics; Statistics; Geometry","score_opus":0.033671763206445146,"score_gpt":0.24667009333318507,"score_spread":0.2129983301267399,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404527300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94518375,0.0003121705,0.042663816,0.00018073781,0.000097088676,0.0001393018,0.0026714848,0.0021930942,0.006558497],"genre_scores_gemma":[0.95381767,0.000099438934,0.038999867,0.00007644765,0.000035212142,0.000097820375,0.005477475,0.00039899047,0.0009970377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992906,0.00007067033,0.000049816143,0.00023404123,0.00030189945,0.000053015658],"domain_scores_gemma":[0.9981053,0.000306906,0.00026081302,0.00039182216,0.00081932195,0.00011586859],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018958325,0.00065870874,0.00033655678,0.0017584221,0.00065326213,0.000973445,0.0010175054,0.00054176495,0.0014369553],"category_scores_gemma":[0.0046430887,0.00033838052,0.00047937033,0.0010729679,0.00046369713,0.00057462486,0.0010593337,0.0006760561,0.00072630966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006649272,0.00094995595,0.48048896,0.00036205322,0.00048627536,0.0006296707,0.001690604,0.11551033,0.092640415,0.001961493,0.011034588,0.29358077],"study_design_scores_gemma":[0.00027351218,0.00023605315,0.64733,0.0001548758,0.00013904853,0.0003246963,0.00069118186,0.30703774,0.03428029,0.00064364343,0.008760132,0.00012882939],"about_ca_topic_score_codex":0.03254719,"about_ca_topic_score_gemma":0.065144315,"teacher_disagreement_score":0.03254719,"about_ca_system_score_codex":0.00052715547,"about_ca_system_score_gemma":0.00090581673,"threshold_uncertainty_score":0.064715445},"labels":[],"label_agreement":null},{"id":"W4404552283","doi":"10.1038/s41598-024-80136-4","title":"Insights on earthquake nucleation revealed by numerical simulation and unsupervised machine learning of laboratory-scale earthquake","year":2024,"lang":"en","type":"article","venue":"Scientific Reports","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Research Canada; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Foreshock; Seismology; Earthquake simulation; Geology; Nucleation; Earthquake rupture; Scale (ratio); Shear (geology); Computer science; Fault (geology); Petrology; Aftershock; Physics; Geography; Cartography","score_opus":0.011376997028272525,"score_gpt":0.22630793683846773,"score_spread":0.2149309398101952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404552283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98740387,0.00004625388,0.011286306,0.00007837465,0.000010307907,0.000007944547,0.00014310518,0.000094035415,0.00092976616],"genre_scores_gemma":[0.99819344,0.000018234949,0.0016211495,0.0000059358276,0.0000031470663,0.0000063742777,0.00007177474,0.0000060701745,0.00007387966],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992156,0.000020681115,0.0000060230955,0.000021055615,0.000012373366,0.000018197246],"domain_scores_gemma":[0.99939144,0.00034080195,0.0000885268,0.00009418436,0.000042679218,0.00004240572],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031800894,0.00018992755,0.0002470234,0.00026382273,0.00020657328,0.00035450174,0.00037346868,0.0003208236,0.00072883005],"category_scores_gemma":[0.0016286621,0.00015430569,0.0002881517,0.00018841925,0.00052547385,0.0004465007,0.000249228,0.00040248464,0.00006363982],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008979689,0.00017401009,0.0269261,0.00006806903,0.00005255534,0.00014219961,0.00010639469,0.94608027,0.01573118,0.00492685,0.0003645012,0.0053380476],"study_design_scores_gemma":[0.0000026887806,0.000011958042,0.0027861889,0.0000012569498,0.0000026188663,0.00000622736,0.000008150998,0.9952306,0.0011115121,0.0007959941,0.000039588962,0.0000031915201],"about_ca_topic_score_codex":0.003202258,"about_ca_topic_score_gemma":0.002847902,"teacher_disagreement_score":0.003202258,"about_ca_system_score_codex":0.00033638245,"about_ca_system_score_gemma":0.00031234353,"threshold_uncertainty_score":0.006367266},"labels":[],"label_agreement":null},{"id":"W4404651090","doi":"10.1029/2024gl110058","title":"Localization and Delocalization During Seismic Slip","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Division of Earth Sciences","keywords":"Geology; Seismology; Slip (aerodynamics); Geophysics; Engineering; Aerospace engineering","score_opus":0.02703587810722408,"score_gpt":0.2782699477206469,"score_spread":0.2512340696134228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404651090","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99659723,0.00014405504,0.0025623317,0.000018135452,0.0000026620385,0.0000043073705,0.0000971882,0.000031554737,0.00054253463],"genre_scores_gemma":[0.9992366,0.000029560506,0.0004686577,0.0000055930304,0.0000019383044,0.000002587389,0.00008809177,0.000007618972,0.00015940654],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986744,0.000018609984,0.000009306708,0.000046929785,0.000029886713,0.000027775453],"domain_scores_gemma":[0.99859804,0.00028896434,0.000566439,0.00012749965,0.00029223895,0.00012681959],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003552938,0.00011074415,0.00015048444,0.00080357306,0.00015114681,0.00041920747,0.00021177366,0.00011481091,0.0009081084],"category_scores_gemma":[0.0018386968,0.00018440069,0.00006383145,0.00039389502,0.0003200144,0.00044124428,0.00055768073,0.00021821939,0.00014701665],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011569539,0.000051405586,0.35253203,0.00015672369,0.00008849334,0.00028750178,0.0019197024,0.004121334,0.57887053,0.0010717108,0.00035098096,0.05939263],"study_design_scores_gemma":[0.000013041113,0.00014278339,0.93824244,0.000021565313,0.000027534465,0.00032520553,0.0007112937,0.014853682,0.043459427,0.00083714863,0.0013361837,0.00002960656],"about_ca_topic_score_codex":0.0017903604,"about_ca_topic_score_gemma":0.002404718,"teacher_disagreement_score":0.0017903604,"about_ca_system_score_codex":0.0003087826,"about_ca_system_score_gemma":0.00011557994,"threshold_uncertainty_score":0.0035598278},"labels":[],"label_agreement":null},{"id":"W4404786474","doi":"10.1016/j.epsl.2024.119115","title":"Soft barrier to megathrust rupture enabled by serpentinized mantle wedge: The Chile subduction zone","year":2024,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico; Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Mantle wedge; Mantle (geology); Geochemistry; Seismology; Petrology; Tectonics","score_opus":0.006556919036581238,"score_gpt":0.18988675990954618,"score_spread":0.18332984087296494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404786474","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955526,0.00016559445,0.00013150756,0.0002248848,0.000008161081,0.000006786407,0.00014935124,0.000021942378,0.0037391172],"genre_scores_gemma":[0.99946517,0.000051659506,0.00003235116,0.000014240221,0.0000029951725,0.0000029533408,0.000055315315,0.0000034941522,0.0003718087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999325,0.0000082289325,0.000004993852,0.0000148789195,0.000008898014,0.000030362316],"domain_scores_gemma":[0.9997814,0.000029187504,0.000057548004,0.00003630854,0.000030474335,0.000064961896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015589091,0.00019485959,0.00026598925,0.0005912991,0.0005606119,0.0010119963,0.00058011437,0.0004997615,0.0039805854],"category_scores_gemma":[0.0010505789,0.00018388554,0.00018665775,0.00038146754,0.00067636353,0.00056516926,0.0016617253,0.00046938082,0.00036640663],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023966564,0.00039851127,0.8122374,0.00053724146,0.00046247078,0.011672404,0.0047413018,0.017831191,0.09964009,0.012166334,0.003729394,0.034187123],"study_design_scores_gemma":[0.0001271668,0.00012405952,0.98040295,0.00006456638,0.00008191447,0.00050148746,0.0033974256,0.0066653113,0.0030685675,0.0018545334,0.003677503,0.000034434182],"about_ca_topic_score_codex":0.016136944,"about_ca_topic_score_gemma":0.012544838,"teacher_disagreement_score":0.016136944,"about_ca_system_score_codex":0.0009858053,"about_ca_system_score_gemma":0.0007674167,"threshold_uncertainty_score":0.032086015},"labels":[],"label_agreement":null},{"id":"W4405108651","doi":"10.1785/0120240172","title":"Smoothing-Based Aftershock Probabilistic Seismic Hazard Assessment Using the Spatiotemporal ETAS Model","year":2024,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Seismology; Geology; Smoothing; Seismic hazard; Hazard; Probabilistic logic; Statistics; Mathematics","score_opus":0.03044536814756501,"score_gpt":0.2555211193678969,"score_spread":0.22507575122033188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405108651","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15225339,0.00015832472,0.84477806,0.00024138551,0.00002959844,0.000056105542,0.00020658539,0.0003544546,0.0019221226],"genre_scores_gemma":[0.97095144,0.00012515184,0.027383192,0.000027924514,0.000023883256,0.000042539126,0.0001831508,0.000024649291,0.0012380945],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99963593,0.00014500349,0.000025571948,0.00007394501,0.00007651897,0.000043021766],"domain_scores_gemma":[0.99692047,0.002095034,0.00038449527,0.00015295684,0.00034669886,0.00010043952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018730583,0.00054951926,0.0006249731,0.0011249632,0.00024937608,0.0007540804,0.0011699867,0.00060586317,0.0018162195],"category_scores_gemma":[0.00488186,0.00026572665,0.00090920884,0.0008092302,0.0004297282,0.00093691546,0.00074226275,0.00073018635,0.0002072067],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029996243,0.000013044351,0.0017295089,0.000014089962,0.000023303332,0.000032166296,0.000021180242,0.98492646,0.00042482177,0.0052688546,0.00012070055,0.0073958044],"study_design_scores_gemma":[7.919019e-7,0.0000035750218,0.00013182824,7.6628777e-7,0.000002332994,0.0000032910843,0.000002697765,0.9988267,0.00003934709,0.00095631636,0.000030754094,0.0000015571577],"about_ca_topic_score_codex":0.01658459,"about_ca_topic_score_gemma":0.007267263,"teacher_disagreement_score":0.01658459,"about_ca_system_score_codex":0.0006466619,"about_ca_system_score_gemma":0.0009300134,"threshold_uncertainty_score":0.03297609},"labels":[],"label_agreement":null},{"id":"W4405123364","doi":"10.1029/2024ef004985","title":"Earthquake Iso‐Nuisance and Iso‐Damage Mapping for Alberta: Applications for Choosing Magnitude Thresholds to Manage Induced Seismicity","year":2024,"lang":"en","type":"article","venue":"Earth s Future","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy","funders":"","keywords":"Induced seismicity; Magnitude (astronomy); Seismology; Geology; Population; Environmental science; Physics","score_opus":0.019998978416118817,"score_gpt":0.2473773464145417,"score_spread":0.2273783679984229,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405123364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.57147664,0.00045208898,0.3316114,0.0010966491,0.00008495678,0.0005636053,0.030282225,0.01675097,0.047681503],"genre_scores_gemma":[0.7606634,0.00023454044,0.22115359,0.00004363217,0.000010690219,0.00012642496,0.013070571,0.00053340924,0.0041637165],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980396,0.000025353142,0.000007988592,0.000027094295,0.00010431352,0.00003137004],"domain_scores_gemma":[0.99927837,0.00016180411,0.00007173615,0.000060318493,0.0003680101,0.000059899623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007485175,0.00062587974,0.00021990598,0.0022902852,0.00034718608,0.00089407875,0.0007829872,0.00031168672,0.003099343],"category_scores_gemma":[0.0030226791,0.00023563203,0.00027257972,0.0020226499,0.0002515156,0.00026500583,0.0005606167,0.00031191978,0.00037645156],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003249492,0.00015436609,0.11540561,0.00018833663,0.000067005974,0.00028909696,0.0005468503,0.636271,0.0058502713,0.0069775637,0.0158125,0.21811251],"study_design_scores_gemma":[0.000062050975,0.000038639668,0.08085642,0.000064041866,0.000024126508,0.000068821195,0.00033389992,0.8965045,0.004101804,0.0036876337,0.014198071,0.000059948423],"about_ca_topic_score_codex":0.52435505,"about_ca_topic_score_gemma":0.66651154,"teacher_disagreement_score":0.47564495,"about_ca_system_score_codex":0.0025866944,"about_ca_system_score_gemma":0.0031621603,"threshold_uncertainty_score":0.95689225},"labels":[],"label_agreement":null},{"id":"W4405312757","doi":"10.1139/cjes-2024-0112","title":"Thermal control on the updip and downdip extents of megathrust earthquake rupture: revisiting Dr. Roy Hyndman's seminal contributions 30 years later","year":2024,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Paleontology","score_opus":0.01611101924327021,"score_gpt":0.22626182022631394,"score_spread":0.21015080098304373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405312757","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0598243,0.81948906,0.016502898,0.07002981,0.010175675,0.00003222696,0.0003411852,0.00010807241,0.023496665],"genre_scores_gemma":[0.40147352,0.5416771,0.0054236706,0.017124001,0.021079399,0.000089627574,0.00023197859,0.00021672185,0.012684005],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9996612,0.00007512198,0.000023088378,0.00013022155,0.00006260153,0.000047810583],"domain_scores_gemma":[0.99897987,0.00053620175,0.00012141574,0.00007947845,0.0002122004,0.00007072958],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016891588,0.0004967052,0.0006275896,0.0007438843,0.00047924262,0.0021465304,0.0009410035,0.0010866553,0.0009594708],"category_scores_gemma":[0.0027000126,0.000301106,0.0004128778,0.00081623666,0.0034177192,0.003372946,0.0018575002,0.0034629495,0.00051129813],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011305978,0.0002021156,0.016686153,0.0029565657,0.00031411875,0.0010263503,0.0069109853,0.0086538,0.021222813,0.3402648,0.07895736,0.52167434],"study_design_scores_gemma":[0.000054852808,0.00033187546,0.026504787,0.0016240256,0.0001536662,0.00082006323,0.0021887766,0.005456491,0.009197257,0.198213,0.7551936,0.00026163293],"about_ca_topic_score_codex":0.0031973836,"about_ca_topic_score_gemma":0.002463941,"teacher_disagreement_score":0.9968026,"about_ca_system_score_codex":0.0015635816,"about_ca_system_score_gemma":0.0010599135,"threshold_uncertainty_score":0.011344612},"labels":[],"label_agreement":null},{"id":"W4405352420","doi":"10.1002/9781394195947.ch1","title":"<scp>EarthScope</scp> Networks in Alaska and Northwestern Canada","year":2024,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Aeronautics and Space Administration; U.S. Department of Energy; National Nuclear Security Administration; National Science Foundation","keywords":"Geology; Oceanography","score_opus":0.005995637251736173,"score_gpt":0.18139797811508632,"score_spread":0.17540234086335013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405352420","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008600907,0.0032259969,0.00044768438,0.00363685,0.0007497359,0.00006575562,0.01767484,0.0007448435,0.96485347],"genre_scores_gemma":[0.018415008,0.0028945503,0.0007854817,0.00035879246,0.00006730294,0.000034020148,0.0063457834,0.00019094581,0.9709082],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997837,0.000009916584,0.000006507536,0.000028898852,0.00011053262,0.000060484395],"domain_scores_gemma":[0.9990036,0.000046652618,0.00003270367,0.00003569919,0.00055626326,0.00032507532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036426922,0.00030689692,0.00014399846,0.0013624507,0.0032983285,0.0017990668,0.00048508207,0.00047077748,0.106888674],"category_scores_gemma":[0.0008178576,0.0001916225,0.00012673317,0.0034844787,0.0006387664,0.00090879784,0.0011992651,0.00045101647,0.020653326],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002448489,0.0000162653,0.0041498234,0.0000954002,0.0000025248407,0.00017256814,0.0006233257,0.00031418377,0.00034922844,0.005979742,0.9219457,0.06632674],"study_design_scores_gemma":[0.000003029951,0.000003021865,0.010402354,0.00006259799,0.0000017871716,0.000038885442,0.0006749255,0.0000962156,0.00016883158,0.00032154156,0.9882181,0.000008738037],"about_ca_topic_score_codex":0.91378355,"about_ca_topic_score_gemma":0.9629899,"teacher_disagreement_score":0.106888674,"about_ca_system_score_codex":0.007585202,"about_ca_system_score_gemma":0.017323824,"threshold_uncertainty_score":0.35757828},"labels":[],"label_agreement":null},{"id":"W4405352587","doi":"10.1002/9781394195947","title":"Tectonics and Seismicity of Alaska and Western Canada ‐ EarthScope and Beyond","year":2024,"lang":"en","type":"book","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Tectonics; Seismology","score_opus":0.006202050933899503,"score_gpt":0.1787941203719788,"score_spread":0.1725920694380793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405352587","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009468555,0.16560268,0.001041035,0.00476754,0.002804354,0.000026799886,0.0022747894,0.0001478767,0.8138663],"genre_scores_gemma":[0.03267227,0.08659981,0.00078452483,0.00042411458,0.00033559758,0.000013325333,0.001600014,0.00008546739,0.877485],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998957,0.000004068778,0.0000033412975,0.000014196094,0.000069243826,0.000013465225],"domain_scores_gemma":[0.9998729,0.000015560077,0.0000057954758,0.000006978143,0.00007837245,0.000020295754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000121557525,0.00044485633,0.00017979092,0.0018825235,0.0017998308,0.002128651,0.00032370948,0.0003873186,0.016603125],"category_scores_gemma":[0.00034204128,0.00015702787,0.00013562292,0.0043495107,0.0011748592,0.0008958767,0.0004700831,0.00055817363,0.002700245],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037904923,0.000012023866,0.003476067,0.0003823982,0.00001440363,0.00015935683,0.003971562,0.0014293933,0.0009690011,0.08140253,0.6023768,0.3057686],"study_design_scores_gemma":[0.0000011512958,0.0000033835947,0.0064787082,0.00015432408,0.0000056789354,0.0000737024,0.00066871865,0.00009966648,0.00012059956,0.0022996424,0.99008757,0.000006888999],"about_ca_topic_score_codex":0.8640901,"about_ca_topic_score_gemma":0.95213497,"teacher_disagreement_score":0.13590991,"about_ca_system_score_codex":0.010738779,"about_ca_system_score_gemma":0.012689956,"threshold_uncertainty_score":0.27342057},"labels":[],"label_agreement":null},{"id":"W4405357792","doi":"10.1002/9781394195947.ch9","title":"Synthesis of the Seismic Structure of the Greater Alaska Region: Geodynamics Implications","year":2024,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geodynamics; Geology; Seismology; Geophysics; Tectonics","score_opus":0.008747522882793062,"score_gpt":0.19230099153343908,"score_spread":0.183553468650646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405357792","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6535762,0.06776781,0.010535064,0.0040648934,0.0007338507,0.00007583668,0.032942522,0.0005025684,0.22980128],"genre_scores_gemma":[0.86638546,0.07740761,0.009450331,0.00020695447,0.00023028771,0.000029864192,0.018215576,0.00007589557,0.027997937],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999471,0.0000075887715,0.000007723215,0.000014703292,0.000018827368,0.00000403175],"domain_scores_gemma":[0.9998485,0.000029966883,0.000032283977,0.000015850945,0.000065919376,0.000007441456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022308918,0.00021905385,0.000100572346,0.0018913894,0.0001755769,0.0006197273,0.0001462528,0.00012998,0.0047684694],"category_scores_gemma":[0.00060017704,0.00007069224,0.00012183291,0.0031804722,0.00019980247,0.00058266975,0.00031869853,0.00016305126,0.00029637362],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012255485,0.00003977878,0.13373825,0.003148427,0.00014448783,0.00051385723,0.0046980637,0.04111121,0.009840302,0.037492923,0.018919695,0.7502304],"study_design_scores_gemma":[0.000009908886,0.00009213572,0.6127896,0.0016252736,0.0001771691,0.00021663762,0.006730362,0.0053231823,0.0027645675,0.008155521,0.36207289,0.00004278735],"about_ca_topic_score_codex":0.13285396,"about_ca_topic_score_gemma":0.20757884,"teacher_disagreement_score":0.13285396,"about_ca_system_score_codex":0.0011638424,"about_ca_system_score_gemma":0.0014749139,"threshold_uncertainty_score":0.2641613},"labels":[],"label_agreement":null},{"id":"W4405357801","doi":"10.1002/9781394195947.ch8","title":"Synthesis of the Seismic Structure of the Greater Alaska Region: Subducting Slab Geometry","year":2024,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Slab; Seismology; Geometry; Geophysics","score_opus":0.00987829859575138,"score_gpt":0.18935453162137397,"score_spread":0.1794762330256226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405357801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8160615,0.00030483401,0.14693606,0.00022909106,0.000071871706,0.00007214426,0.01596946,0.0018053947,0.018549675],"genre_scores_gemma":[0.9606864,0.00013038295,0.033357307,0.000008484314,0.000016759337,0.000025480498,0.0045069465,0.00012378834,0.0011444992],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999224,0.0000134039055,0.0000053675194,0.00003123041,0.0000188366,0.000008763108],"domain_scores_gemma":[0.99987555,0.000018722105,0.000022943175,0.000018549428,0.000053776614,0.00001057219],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013404332,0.00031268972,0.00015144501,0.0011923584,0.00015777575,0.00045115597,0.00024778885,0.0001820768,0.002842384],"category_scores_gemma":[0.00067364494,0.00020791758,0.00021506136,0.0013164494,0.00012045847,0.00021316887,0.00023285682,0.00017040045,0.00048588426],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023092362,0.000059641527,0.13914996,0.00023954848,0.00012924151,0.00061661494,0.000826775,0.49544734,0.0609789,0.017141057,0.0053592366,0.27982077],"study_design_scores_gemma":[0.00003208285,0.00009271218,0.23720993,0.000049258982,0.0000569742,0.00025956894,0.0005045443,0.7307615,0.007214929,0.006003975,0.017750941,0.000063592786],"about_ca_topic_score_codex":0.022363279,"about_ca_topic_score_gemma":0.032830626,"teacher_disagreement_score":0.022363279,"about_ca_system_score_codex":0.00038069932,"about_ca_system_score_gemma":0.0004849323,"threshold_uncertainty_score":0.044466197},"labels":[],"label_agreement":null},{"id":"W4405357806","doi":"10.1002/9781394195947.ch6","title":"Synthesis of the Seismic Structure of the Greater Alaska Region: Continental Lithosphere","year":2024,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Lithosphere; Geology; Seismology; Collision zone; Geophysics; Earth science; Tectonics","score_opus":0.007040948264933434,"score_gpt":0.1814965399251677,"score_spread":0.17445559166023428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405357806","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6909515,0.02680213,0.012133341,0.0011384527,0.00033362157,0.00011566427,0.11008445,0.0008040119,0.15763678],"genre_scores_gemma":[0.88475865,0.026620034,0.012027999,0.00007758235,0.0000979273,0.00007347858,0.05760579,0.00009406877,0.018644536],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99994576,0.000007183086,0.000007936096,0.000018857047,0.000015322163,0.000004878663],"domain_scores_gemma":[0.9998852,0.000017395956,0.000017543902,0.000011212891,0.00005930148,0.000009310345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021597907,0.0003187511,0.00013335134,0.0020235868,0.00021443726,0.0005132374,0.00015355698,0.00014469659,0.005981385],"category_scores_gemma":[0.00045552844,0.00010681115,0.0001850651,0.003548044,0.000085955806,0.0002306472,0.00031163832,0.00012911727,0.0007797899],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022154371,0.00005500341,0.25746086,0.0032115043,0.00032413704,0.00038897112,0.003345534,0.106775634,0.014165014,0.010630802,0.03325835,0.5701626],"study_design_scores_gemma":[0.000013863833,0.00008365372,0.77144486,0.0008355733,0.00023799182,0.000108778586,0.0027664714,0.010363128,0.0017632958,0.0020351717,0.21030621,0.00004097913],"about_ca_topic_score_codex":0.15644915,"about_ca_topic_score_gemma":0.20782042,"teacher_disagreement_score":0.15644915,"about_ca_system_score_codex":0.00075115176,"about_ca_system_score_gemma":0.0010986237,"threshold_uncertainty_score":0.311077},"labels":[],"label_agreement":null},{"id":"W4405357824","doi":"10.1002/9781394195947.ch5","title":"Geodetic Observations of Tectonic Deformation in Alaska and Western Canada: The EarthScope Revolution","year":2024,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geodetic datum; Geology; Tectonics; Seismology; Geodesy; Deformation (meteorology); Oceanography","score_opus":0.013325709574258472,"score_gpt":0.19553385195820638,"score_spread":0.18220814238394792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405357824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.73265123,0.01030701,0.000578932,0.0018780164,0.0001336588,0.00014363544,0.15030126,0.00026007765,0.10374622],"genre_scores_gemma":[0.8314095,0.010184727,0.0019908869,0.0004179594,0.000048860515,0.00007073604,0.07732503,0.00009826413,0.07845402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997272,0.000009556557,0.000015118427,0.000037360063,0.00015320005,0.00005764837],"domain_scores_gemma":[0.99897337,0.000032592583,0.00007863345,0.00003619249,0.0006799907,0.00019930622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028172502,0.00026160802,0.00018634372,0.0029374491,0.0015638979,0.0010195845,0.0005442786,0.00021002423,0.0043198657],"category_scores_gemma":[0.00085385935,0.00019449483,0.00012297956,0.007423403,0.00031564716,0.0003989795,0.00084556645,0.00033010458,0.0008722159],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017210086,0.0000792236,0.76848584,0.00029475367,0.000078022735,0.00038923128,0.0049808677,0.00095099333,0.00201749,0.0013885592,0.07733574,0.14382714],"study_design_scores_gemma":[0.000006413913,0.000006734177,0.943427,0.000085800755,0.000012870463,0.00003981959,0.0018954801,0.00022400841,0.00019020306,0.000059243954,0.054040477,0.000011836107],"about_ca_topic_score_codex":0.99571913,"about_ca_topic_score_gemma":0.99836105,"teacher_disagreement_score":0.01290834,"about_ca_system_score_codex":0.01290834,"about_ca_system_score_gemma":0.018429112,"threshold_uncertainty_score":0.09365702},"labels":[],"label_agreement":null},{"id":"W4405357860","doi":"10.1002/9781394195947.ch3","title":"A Decade of Alaska Seismicity: 2013–2022","year":2024,"lang":"en","type":"other","venue":"Geophysical monograph","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Induced seismicity; Geology; Seismology; Oceanography","score_opus":0.010459161627582427,"score_gpt":0.21603550653676273,"score_spread":0.2055763449091803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405357860","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.26902115,0.12080601,0.002521283,0.0062172203,0.006031392,0.0001875834,0.33776698,0.001653795,0.25579453],"genre_scores_gemma":[0.42993155,0.13858083,0.0027354024,0.0013356765,0.002543867,0.00028502272,0.28650865,0.00039245718,0.13768646],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.999767,0.000012730043,0.000032319975,0.00004138896,0.00011328863,0.000033262957],"domain_scores_gemma":[0.9994814,0.000028178061,0.00010180343,0.000017530025,0.0002869476,0.0000842698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005291238,0.00052554376,0.00024640546,0.0022798965,0.00058022636,0.0013132829,0.0002578783,0.00040550283,0.010433313],"category_scores_gemma":[0.0009771112,0.00017425549,0.00026636483,0.004912456,0.00015386389,0.0009487271,0.00075941184,0.000403927,0.0064035086],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002839499,0.00007807691,0.15615694,0.002894014,0.00013502952,0.00076926546,0.002335736,0.0016568726,0.0024874357,0.0022036105,0.42684534,0.4041537],"study_design_scores_gemma":[0.000006869181,0.000059946615,0.36911145,0.0010756332,0.000058627407,0.00038611336,0.0026731968,0.0003255999,0.0007343381,0.00040964398,0.6251293,0.000029226654],"about_ca_topic_score_codex":0.06983259,"about_ca_topic_score_gemma":0.12399704,"teacher_disagreement_score":0.06983259,"about_ca_system_score_codex":0.0013301115,"about_ca_system_score_gemma":0.0017452578,"threshold_uncertainty_score":0.13885224},"labels":[],"label_agreement":null},{"id":"W4405364835","doi":"10.1016/j.engeos.2024.100368","title":"Traffic light system regulation of induced seismicity under multi-well fluid injection","year":2024,"lang":"en","type":"article","venue":"Energy Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"State Key Laboratory of Geomechanics and Geotechnical Engineering; National Natural Science Foundation of China","keywords":"Induced seismicity; Geology; Environmental science; Seismology","score_opus":0.018089774900949773,"score_gpt":0.21210514517181017,"score_spread":0.1940153702708604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405364835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9813581,0.00005480937,0.01602891,0.000069573434,0.00002299515,0.00002363884,0.00009382687,0.00026569384,0.0020825027],"genre_scores_gemma":[0.99940693,0.000010937051,0.00038752978,0.0000052408877,5.530639e-7,0.0000052764444,0.000016339887,0.0000031212269,0.00016402206],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986637,0.000016601525,0.0000072779517,0.000025878508,0.000038565333,0.000045212917],"domain_scores_gemma":[0.9997241,0.00006088595,0.00006891812,0.000017604136,0.00008942548,0.000039185044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021000781,0.0003422538,0.00027394984,0.0002678115,0.00037350546,0.0005053708,0.00044418938,0.00036668027,0.001088315],"category_scores_gemma":[0.00054479484,0.00014534095,0.00031955252,0.000103704784,0.00046397327,0.0003569492,0.00045223825,0.00033991892,0.00009862184],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000529591,0.00023509089,0.017207371,0.0001418984,0.00004916587,0.0005298585,0.00022169766,0.75426114,0.21285976,0.0019204274,0.00058113626,0.011462755],"study_design_scores_gemma":[0.000024082003,0.00013550256,0.0043604113,0.0000043892364,0.000019344161,0.000015643745,0.00007378348,0.96918607,0.025581585,0.00027034234,0.00031214237,0.000016632985],"about_ca_topic_score_codex":0.016314404,"about_ca_topic_score_gemma":0.012621115,"teacher_disagreement_score":0.016314404,"about_ca_system_score_codex":0.0010509484,"about_ca_system_score_gemma":0.00074181263,"threshold_uncertainty_score":0.032438934},"labels":[],"label_agreement":null},{"id":"W4405527421","doi":"10.21203/rs.3.rs-5654218/v1","title":"Signatures of Explosive Submarine Volcanism at the Northern Reykjanes Ridge","year":2024,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Kootenay Association for Science & Technology","funders":"","keywords":"Volcanism; Geology; Submarine; Ridge; Explosive material; Seismology; Earth science; Geochemistry; Paleontology; Archaeology; Oceanography; Tectonics; History","score_opus":0.054575011720198886,"score_gpt":0.3205947747659559,"score_spread":0.266019763045757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405527421","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978928,0.000055569166,0.00005990168,0.000019236615,0.000005165939,0.0000022412705,0.00021497738,0.000016924962,0.001733255],"genre_scores_gemma":[0.9988771,0.000042640575,0.00010368387,0.000004524041,0.0000060622715,0.0000020230257,0.00026536616,0.000010286105,0.00068838155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999936,0.000005514536,0.0000035445019,0.000020871945,0.000013684854,0.000020398931],"domain_scores_gemma":[0.9998646,0.000020548632,0.000045843182,0.000015965836,0.000028036688,0.000024950357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013129057,0.00020337926,0.00022119885,0.0005475839,0.00023405212,0.00046683341,0.0002571236,0.00036884923,0.0013263014],"category_scores_gemma":[0.00040642524,0.0001708161,0.000095158044,0.00031190968,0.00023951645,0.00021302929,0.00038624858,0.00024827436,0.0003666411],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014722492,0.00019572448,0.72324497,0.00021154936,0.00012675922,0.001815348,0.0029570009,0.0054750196,0.21101995,0.0012018967,0.0022228814,0.050056722],"study_design_scores_gemma":[0.0000060768366,0.000016558695,0.9983317,0.0000072276903,0.0000050792128,0.000060936636,0.00012680981,0.00043492633,0.0004931906,0.00002296125,0.0004913997,0.0000029941505],"about_ca_topic_score_codex":0.009049464,"about_ca_topic_score_gemma":0.014822573,"teacher_disagreement_score":0.009049464,"about_ca_system_score_codex":0.000194768,"about_ca_system_score_gemma":0.00018323305,"threshold_uncertainty_score":0.017993629},"labels":[],"label_agreement":null},{"id":"W4405632364","doi":"10.1016/j.eng.2024.12.010","title":"The Overcoring Technique for Precise Measurement of In Situ Rock Stress at Great Depths: Challenges and Solutions","year":2024,"lang":"en","type":"article","venue":"Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; In situ; Stress (linguistics); Mining engineering; Seismology; Geotechnical engineering; Geography; Meteorology","score_opus":0.03882491851620511,"score_gpt":0.21411395989125387,"score_spread":0.17528904137504875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405632364","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18707012,0.011425361,0.7685956,0.0058900616,0.0021996365,0.0002972544,0.0020505271,0.0020047086,0.020466747],"genre_scores_gemma":[0.4838454,0.009703038,0.49029568,0.0034074292,0.00095162966,0.0003338875,0.00093077077,0.0005992433,0.009932956],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9986571,0.00020214194,0.000059258928,0.00030794993,0.000638259,0.00013532021],"domain_scores_gemma":[0.99541473,0.0013906194,0.00050232554,0.00088315125,0.0015493211,0.00025976886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017193558,0.00094536995,0.0010360472,0.0010113886,0.0006687629,0.0013395936,0.0016728283,0.0016037838,0.003299774],"category_scores_gemma":[0.0034463855,0.00047897364,0.00023962128,0.0018582075,0.001133252,0.0021088447,0.0016259111,0.0017128991,0.0011016447],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020910543,0.000094470684,0.027613772,0.0008986528,0.00006765875,0.00028486148,0.0006086098,0.0011023179,0.6896533,0.006257055,0.0057782293,0.267432],"study_design_scores_gemma":[0.00012313848,0.0012192589,0.10668454,0.0007170815,0.00030067726,0.0044976254,0.002816756,0.05551638,0.6088002,0.028779343,0.19010459,0.00044048115],"about_ca_topic_score_codex":0.0045867,"about_ca_topic_score_gemma":0.014060526,"teacher_disagreement_score":0.0045867,"about_ca_system_score_codex":0.00046795412,"about_ca_system_score_gemma":0.0013405356,"threshold_uncertainty_score":0.01103884},"labels":[],"label_agreement":null},{"id":"W4405921881","doi":"10.1785/0120240145","title":"Source Characteristics of Tectonic and Induced Events near St. Gallen, Switzerland: Utilizing the Empirical Green’s Function Method and Generalized Inversion Technique","year":2024,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Inversion (geology); Tectonics; Seismology; Geology; Applied mathematics; Mathematics","score_opus":0.04271072647240336,"score_gpt":0.26231388257661686,"score_spread":0.2196031561042135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405921881","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962608,0.000035529916,0.003019909,0.000024237732,0.000003523925,0.0000060725824,0.00021481459,0.000055877426,0.00037908374],"genre_scores_gemma":[0.9981198,0.000023486275,0.0012453315,0.0000029731268,0.000003892516,0.0000054543443,0.00046008898,0.000009456763,0.00012945336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998926,0.000021178897,0.0000065145045,0.00002574758,0.000029177056,0.00002476607],"domain_scores_gemma":[0.99969923,0.00010876683,0.00007253951,0.000029330196,0.00006084334,0.000029173221],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024751519,0.00045643747,0.00016863555,0.0014978375,0.00014830186,0.00039172595,0.00035292126,0.00033629796,0.00057046954],"category_scores_gemma":[0.00083399285,0.00013635737,0.0003103225,0.0009347439,0.00024630516,0.00027602998,0.00034316388,0.0001789749,0.00013310589],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005405998,0.0002469522,0.61353207,0.00020786659,0.00024274524,0.0016299858,0.00096505973,0.21022552,0.066916496,0.0010669155,0.0016120023,0.102813825],"study_design_scores_gemma":[0.00001796154,0.00006441028,0.69518715,0.000016246517,0.000031980904,0.00012269452,0.0002194232,0.30008635,0.0036923958,0.00016699427,0.00036217668,0.000032220727],"about_ca_topic_score_codex":0.021135554,"about_ca_topic_score_gemma":0.025992831,"teacher_disagreement_score":0.021135554,"about_ca_system_score_codex":0.00023829052,"about_ca_system_score_gemma":0.00026636585,"threshold_uncertainty_score":0.04202509},"labels":[],"label_agreement":null},{"id":"W4406110861","doi":"10.1073/pnas.2407345121","title":"Pore pressure inhibits clustering of induced earthquakes in Western Canada","year":2025,"lang":"en","type":"article","venue":"Proceedings of the National Academy of Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Cluster analysis; Seismology; Pore water pressure; Geology; Materials science; Geotechnical engineering; Computer science","score_opus":0.03059294890855906,"score_gpt":0.2609710473127846,"score_spread":0.23037809840422552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406110861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981712,0.00003442764,0.00028465848,0.000025311303,0.0000010931506,0.000010181237,0.00058421,0.00002590401,0.00086302037],"genre_scores_gemma":[0.9989405,0.000041893534,0.0002712769,0.0000054377547,5.3508387e-7,0.0000036592198,0.0003762191,0.000003635102,0.00035684393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998211,0.000007873377,0.000008113117,0.00004208839,0.00006031046,0.0000605766],"domain_scores_gemma":[0.9995352,0.000033450353,0.00011985009,0.000022887385,0.00019726387,0.00009124943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001072586,0.00014079419,0.0001917212,0.0009985694,0.00081981806,0.000510211,0.00032528568,0.00017205747,0.0007954217],"category_scores_gemma":[0.0007795481,0.00013458046,0.00015684096,0.0020283929,0.00047270794,0.00013110916,0.00041880645,0.00013770255,0.00010663254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003345353,0.00007472996,0.900467,0.00011357896,0.00013264878,0.00065862254,0.0019211158,0.016282825,0.040088095,0.0006173591,0.0020169115,0.037292548],"study_design_scores_gemma":[0.000004287286,0.000016288175,0.99298096,0.000004228646,0.000011881176,0.00004330059,0.0006650099,0.0044630156,0.0011672071,0.000056997185,0.00057548704,0.000011231635],"about_ca_topic_score_codex":0.9425469,"about_ca_topic_score_gemma":0.97300786,"teacher_disagreement_score":0.057453096,"about_ca_system_score_codex":0.0053561833,"about_ca_system_score_gemma":0.0063575674,"threshold_uncertainty_score":0.115582824},"labels":[],"label_agreement":null},{"id":"W4406232501","doi":"10.1007/978-981-16-7408-2_1-1","title":"Earthquake Characteristics and Seismology Basics","year":2024,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal; Golder Associates (Canada)","funders":"","keywords":"Seismology; Geology; Forensic engineering; Engineering","score_opus":0.018686731842234003,"score_gpt":0.20327136483262295,"score_spread":0.18458463299038896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406232501","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.003476099,0.0335341,0.042151842,0.0016813567,0.0013771945,0.000094934294,0.0016079338,0.00037373512,0.9157028],"genre_scores_gemma":[0.037263375,0.043622375,0.017524611,0.0006987595,0.0021493318,0.0001248145,0.0022192472,0.00035804452,0.8960395],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9999105,0.000013689661,0.000007424422,0.000017755061,0.000043594286,0.000007071568],"domain_scores_gemma":[0.9998227,0.00007790176,0.000010407673,0.00001854254,0.00006073015,0.000009745212],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018434039,0.00057998556,0.0004186013,0.0013405553,0.00029226005,0.0012707763,0.0006967042,0.0004231548,0.033336855],"category_scores_gemma":[0.00062283035,0.00026021645,0.00020115411,0.0019382115,0.0006317427,0.0014369648,0.00040350558,0.00082410866,0.01738921],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003573029,0.000059089285,0.00073279225,0.00055948587,0.0000065777467,0.00019962434,0.00048981013,0.0026666336,0.0025258935,0.32092476,0.15587598,0.5159235],"study_design_scores_gemma":[0.0000025128752,0.000024308249,0.001889651,0.00011176315,0.000005689311,0.00045110125,0.00011084349,0.0009048366,0.00040775974,0.08472333,0.91135836,0.000009883848],"about_ca_topic_score_codex":0.0014430522,"about_ca_topic_score_gemma":0.0018421008,"teacher_disagreement_score":0.033336855,"about_ca_system_score_codex":0.000382156,"about_ca_system_score_gemma":0.0003845728,"threshold_uncertainty_score":0.11152285},"labels":[],"label_agreement":null},{"id":"W4406383451","doi":"10.1016/s0967-0653(97)86209-6","title":"10.1016/s0967-0653(97)86209-6","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Cluster analysis; Tectonics","score_opus":0.009973679331612464,"score_gpt":0.16641174560169378,"score_spread":0.1564380662700813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406383451","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005657877,0.00044129405,0.0006041025,0.00041609298,0.0003395011,0.00015381647,0.0011178829,0.0010270221,0.99533457],"genre_scores_gemma":[0.00058035855,0.00022230609,0.00032660738,0.00026524797,0.000080949234,0.00008612573,0.00046501085,0.00017701706,0.9977964],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99915993,0.000054335185,0.00008092931,0.00032986316,0.00018393157,0.00019104693],"domain_scores_gemma":[0.9972675,0.000654635,0.00020581511,0.00035322524,0.0006443271,0.00087450194],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0015035177,0.004163598,0.002803007,0.003471746,0.003185233,0.004767917,0.0047290265,0.007966271,0.9915911],"category_scores_gemma":[0.0019185652,0.0015358214,0.002007371,0.0034076546,0.0028773355,0.007774708,0.004253143,0.0035720652,0.9950133],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053100684,0.00030599802,0.0011956071,0.000859994,0.000057896727,0.00033927037,0.00016389474,0.00056421896,0.0024819693,0.006616868,0.39856747,0.5883159],"study_design_scores_gemma":[0.00009783581,0.00019227157,0.0009289456,0.0005517345,0.000023102872,0.00046147706,0.00017234373,0.00021729828,0.0003521224,0.0006375919,0.99632543,0.00003981857],"about_ca_topic_score_codex":0.0054990943,"about_ca_topic_score_gemma":0.0046485728,"teacher_disagreement_score":0.008408904,"about_ca_system_score_codex":0.0014871521,"about_ca_system_score_gemma":0.0012983851,"threshold_uncertainty_score":0.011994183},"labels":[],"label_agreement":null},{"id":"W4406397225","doi":"10.1016/0967-0653(96)82350-7","title":"10.1016/0967-0653(96)82350-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Ocean tide; Geology; Oceanography; Statistical analysis; Seismology; Statistics; Mathematics","score_opus":0.008536374600997328,"score_gpt":0.1629608877242178,"score_spread":0.15442451312322047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406397225","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005399261,0.00039323655,0.00047521084,0.0003760468,0.00028828028,0.00012825633,0.00091741834,0.00087273377,0.9960089],"genre_scores_gemma":[0.0007006388,0.00025672172,0.00029482512,0.00031126762,0.00008398917,0.00007656606,0.00043861667,0.00016798885,0.9976694],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99926525,0.000051574407,0.00007779768,0.0002747008,0.00015400651,0.00017665658],"domain_scores_gemma":[0.9974285,0.00066465896,0.00016192807,0.00031289257,0.0005887805,0.00084318925],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013755569,0.0038674045,0.0025407812,0.003223371,0.0034237094,0.004494478,0.004091789,0.0072990935,0.9915838],"category_scores_gemma":[0.0018445608,0.0016031197,0.0017655828,0.0030209166,0.003064614,0.0072134915,0.004091317,0.003389901,0.99497366],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051973877,0.00031693332,0.0013808729,0.00082769804,0.000057345984,0.00039983375,0.0001671521,0.00063158385,0.0028367795,0.0056174905,0.42471015,0.5625345],"study_design_scores_gemma":[0.000104657775,0.00022111049,0.0013259951,0.0006380039,0.000023285635,0.0005064671,0.0002415913,0.00023717439,0.00040901388,0.0008348479,0.9954131,0.000044735396],"about_ca_topic_score_codex":0.0058726496,"about_ca_topic_score_gemma":0.0053522675,"teacher_disagreement_score":0.008416176,"about_ca_system_score_codex":0.001326794,"about_ca_system_score_gemma":0.0009817175,"threshold_uncertainty_score":0.012004554},"labels":[],"label_agreement":null},{"id":"W4406399392","doi":"10.1016/0967-0653(94)91400-1","title":"10.1016/0967-0653(94)91400-1","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Mesozoic; Celtic languages; Structural basin; Paleontology; Oceanography; Archaeology; Geography","score_opus":0.008613039910805245,"score_gpt":0.16388770915395015,"score_spread":0.1552746692431449,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406399392","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005588417,0.00033138925,0.00046373744,0.00042594303,0.0002928748,0.00014044128,0.00090143335,0.00082880113,0.99605656],"genre_scores_gemma":[0.0006968069,0.0002572917,0.00031292377,0.0003301121,0.00008678243,0.00008248639,0.00043596097,0.00017066544,0.99762696],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992811,0.000050849187,0.00006803776,0.0002663052,0.00015936545,0.00017438608],"domain_scores_gemma":[0.99750465,0.0006243941,0.00013609767,0.0002908394,0.0005756908,0.0008683205],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012689874,0.0035802159,0.0023926243,0.0032079814,0.0034261034,0.0040083416,0.00384573,0.0071419906,0.9914791],"category_scores_gemma":[0.0019883863,0.0014629811,0.0015374859,0.0028674682,0.002745022,0.0067884335,0.0039490047,0.0032638095,0.99440634],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046286933,0.00035375138,0.0014758378,0.00072804774,0.0000509072,0.00039562266,0.00016270338,0.00060022774,0.0024345103,0.005132708,0.4511284,0.5370744],"study_design_scores_gemma":[0.000095968004,0.00019670579,0.0013874181,0.00057210453,0.000021563386,0.00048023212,0.0002269972,0.0002208099,0.0003440396,0.0007107626,0.99570507,0.000038273167],"about_ca_topic_score_codex":0.0064703953,"about_ca_topic_score_gemma":0.005947967,"teacher_disagreement_score":0.008520901,"about_ca_system_score_codex":0.0013499195,"about_ca_system_score_gemma":0.0010046767,"threshold_uncertainty_score":0.012865424},"labels":[],"label_agreement":null},{"id":"W4406415610","doi":"10.1016/s0967-0653(97)89165-x","title":"10.1016/s0967-0653(97)89165-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Finite element method; Seismology; Geodesy; Structural engineering; Engineering","score_opus":0.009967734870019318,"score_gpt":0.16654002153328024,"score_spread":0.15657228666326092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406415610","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000569423,0.0004177227,0.00057508267,0.0004006837,0.00031957007,0.0001443534,0.0010079024,0.0009572073,0.9956079],"genre_scores_gemma":[0.0005733589,0.00020890383,0.00031086622,0.0002479853,0.000073269366,0.00007867668,0.00042457727,0.00017332814,0.99790907],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99922204,0.000050291197,0.00007215116,0.00030885582,0.00017319311,0.00017338018],"domain_scores_gemma":[0.9975134,0.0005763127,0.00018668766,0.000334036,0.000538223,0.0008513249],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013564146,0.0040409956,0.0025268195,0.0033937031,0.0030716702,0.0044565853,0.0044982773,0.0075470414,0.99109167],"category_scores_gemma":[0.0017849664,0.0014703093,0.0018496494,0.0032271761,0.0028199635,0.007460061,0.004013519,0.0034106243,0.9942384],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048276846,0.000310963,0.0011751378,0.0008387902,0.00005356145,0.00035423893,0.0001730311,0.00054294575,0.002503063,0.007366467,0.40258113,0.5836179],"study_design_scores_gemma":[0.00008314996,0.00016921406,0.0009318097,0.0004750213,0.000020462225,0.00043488116,0.00017102886,0.00019084835,0.00033210253,0.00064603233,0.9965102,0.00003521845],"about_ca_topic_score_codex":0.005775713,"about_ca_topic_score_gemma":0.004895716,"teacher_disagreement_score":0.008908331,"about_ca_system_score_codex":0.0014189355,"about_ca_system_score_gemma":0.0012673525,"threshold_uncertainty_score":0.012706637},"labels":[],"label_agreement":null},{"id":"W4406415790","doi":"10.1016/s0967-0653(97)80323-7","title":"10.1016/s0967-0653(97)80323-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Graben; Geology; Mediterranean climate; Seismology; Reflection (computer programming); Paleontology; Archaeology; Geography; Tectonics","score_opus":0.009974176597004867,"score_gpt":0.16678754303183901,"score_spread":0.15681336643483415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406415790","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00046377452,0.0003743686,0.0005223271,0.0003786383,0.0002862377,0.00012268701,0.0009415728,0.00090721366,0.9960032],"genre_scores_gemma":[0.0005313078,0.00018231191,0.0002724181,0.00022570712,0.00006776962,0.00007163062,0.00041071346,0.00016698957,0.998071],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99924016,0.000050036404,0.00007031684,0.00029007098,0.00018142954,0.00016802244],"domain_scores_gemma":[0.99737996,0.00060689135,0.00019901014,0.0003354177,0.0006439657,0.0008346929],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013330043,0.003700767,0.0025041692,0.0033115223,0.002838775,0.004659321,0.0041573197,0.0072461357,0.9913918],"category_scores_gemma":[0.0018976443,0.0013452433,0.0017501592,0.0031690612,0.0025806085,0.006803406,0.0039924923,0.0032398845,0.99499434],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042923883,0.00024877183,0.0009957827,0.0006694071,0.00004689803,0.00029124384,0.00013707645,0.00047750163,0.0021617608,0.006051197,0.41387787,0.57461333],"study_design_scores_gemma":[0.00007800904,0.0001520273,0.00083179737,0.00044142522,0.000017989385,0.00037360805,0.00014579152,0.0001830387,0.00029582775,0.00060893653,0.9968381,0.000033466527],"about_ca_topic_score_codex":0.005219665,"about_ca_topic_score_gemma":0.0043126172,"teacher_disagreement_score":0.008608222,"about_ca_system_score_codex":0.0014219066,"about_ca_system_score_gemma":0.0012499611,"threshold_uncertainty_score":0.012278497},"labels":[],"label_agreement":null},{"id":"W4406429604","doi":"10.1016/0967-0653(96)85861-3","title":"10.1016/0967-0653(96)85861-3","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology; Margin (machine learning); Distribution (mathematics)","score_opus":0.008538262095771793,"score_gpt":0.1629724975549968,"score_spread":0.154434235459225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406429604","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00054291356,0.00040003104,0.00048292294,0.00037909017,0.00030787598,0.00012602183,0.0009304021,0.00081299804,0.9960179],"genre_scores_gemma":[0.00073006435,0.00027949724,0.00030881606,0.00031632127,0.00009225547,0.00007248296,0.00044876113,0.00015989279,0.997592],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99931896,0.000045602774,0.00006978246,0.00025402848,0.00015185957,0.00015974796],"domain_scores_gemma":[0.9974759,0.0006337162,0.00015669361,0.00030637457,0.0006112249,0.0008160729],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012667188,0.0035769988,0.0023465736,0.0029762054,0.0031731022,0.0043709357,0.003827737,0.006457839,0.9909931],"category_scores_gemma":[0.001734383,0.0014557276,0.0016989745,0.0029452874,0.0027769357,0.006930911,0.003673144,0.0034435845,0.994615],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050807575,0.00032778303,0.0015046798,0.00084760657,0.000059374357,0.00037690575,0.00016385487,0.00062122964,0.002792922,0.005419281,0.4185784,0.56879985],"study_design_scores_gemma":[0.00009615559,0.0002074247,0.0013618353,0.0006096533,0.000024358402,0.0005222676,0.00023462059,0.0002278823,0.00042978453,0.0007702361,0.9954721,0.000043748805],"about_ca_topic_score_codex":0.0056573325,"about_ca_topic_score_gemma":0.0051850104,"teacher_disagreement_score":0.0090069175,"about_ca_system_score_codex":0.0012604527,"about_ca_system_score_gemma":0.0009613242,"threshold_uncertainty_score":0.012847304},"labels":[],"label_agreement":null},{"id":"W4406433574","doi":"10.1016/0967-0653(95)91562-1","title":"10.1016/0967-0653(95)91562-1","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology; Baltic sea; Oceanography","score_opus":0.008598713328945136,"score_gpt":0.16378970716963331,"score_spread":0.15519099384068819,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406433574","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00048200725,0.00034386126,0.00043341386,0.00037950734,0.00026254932,0.00011896056,0.0008182331,0.0007238526,0.99643767],"genre_scores_gemma":[0.0006532833,0.00024319802,0.00029095035,0.00029646623,0.000076743745,0.00007095342,0.00041134204,0.00015114383,0.997806],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993499,0.000044643628,0.000060948427,0.00024546596,0.00015167611,0.00014730649],"domain_scores_gemma":[0.9977695,0.000565001,0.00012671834,0.00026205493,0.0005311015,0.0007457181],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011084698,0.0030755028,0.002153654,0.0029047444,0.0030276363,0.0040235594,0.0035297507,0.006284903,0.9907195],"category_scores_gemma":[0.0017707606,0.0012366788,0.0014297217,0.0025089884,0.002345895,0.0059950086,0.0035535155,0.0030053856,0.99408793],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041127315,0.0002955642,0.0012711381,0.0006633293,0.000044675493,0.00033685178,0.00014454775,0.00050366647,0.0023426344,0.005077984,0.43568528,0.5532231],"study_design_scores_gemma":[0.00007743377,0.00015871417,0.0011884932,0.0004849993,0.000018298324,0.00040837258,0.00018518743,0.00017938763,0.0003122141,0.00067432394,0.9962799,0.000032703483],"about_ca_topic_score_codex":0.005777893,"about_ca_topic_score_gemma":0.0054333634,"teacher_disagreement_score":0.009280503,"about_ca_system_score_codex":0.0012319754,"about_ca_system_score_gemma":0.00094861456,"threshold_uncertainty_score":0.013237536},"labels":[],"label_agreement":null},{"id":"W4406436843","doi":"10.1016/0967-0653(93)92575-5","title":"10.1016/0967-0653(93)92575-5","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Volcano; Geology; Seismology; Line (geometry); Geometry","score_opus":0.00805816542409597,"score_gpt":0.16025091547587186,"score_spread":0.1521927500517759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406436843","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005725033,0.0003435179,0.000487765,0.00039256646,0.0002714966,0.00013028376,0.0009520916,0.0008591134,0.9959906],"genre_scores_gemma":[0.0007880114,0.00024569832,0.00032462445,0.00032595528,0.00008272828,0.00007557781,0.00047525798,0.00016980489,0.9975122],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99930394,0.00004663719,0.00006816128,0.00025611345,0.00015666895,0.0001684741],"domain_scores_gemma":[0.99760866,0.00061317877,0.00014639623,0.00028580558,0.00055908464,0.0007868485],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012952739,0.0034069358,0.0022922254,0.0030525734,0.0032796473,0.0043604583,0.0038170135,0.006861574,0.99158067],"category_scores_gemma":[0.0018129341,0.0015120166,0.0016131095,0.0028275952,0.0027905235,0.0065457085,0.003887908,0.0031497441,0.99466383],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047874846,0.00034094907,0.0015903164,0.0007217898,0.000057048608,0.00041342748,0.00016709778,0.00058186305,0.0027288387,0.0053293672,0.4143207,0.57326984],"study_design_scores_gemma":[0.000103704035,0.00021330232,0.0014737678,0.0006060225,0.00002494481,0.000529847,0.00023577338,0.00023954977,0.0004383643,0.00080213655,0.9952922,0.0000404658],"about_ca_topic_score_codex":0.0058316174,"about_ca_topic_score_gemma":0.005391636,"teacher_disagreement_score":0.008419335,"about_ca_system_score_codex":0.001259531,"about_ca_system_score_gemma":0.0009718529,"threshold_uncertainty_score":0.012009144},"labels":[],"label_agreement":null},{"id":"W4406437767","doi":"10.1016/0967-0653(96)81009-x","title":"10.1016/0967-0653(96)81009-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Trench; Geology; Seismology; Ocean bottom; Intraplate earthquake; Tectonics","score_opus":0.008484435641751872,"score_gpt":0.16325046102486576,"score_spread":0.1547660253831139,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406437767","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005449377,0.0003423021,0.0004445949,0.00035616622,0.00028328763,0.0001199067,0.0008274746,0.00074956415,0.9963319],"genre_scores_gemma":[0.0006787377,0.0002399012,0.0002863538,0.00026188916,0.00007550302,0.00006718593,0.0004093193,0.00015984447,0.99782133],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993549,0.00004597713,0.00006431284,0.0002408763,0.00014083191,0.00015304604],"domain_scores_gemma":[0.9976659,0.0005714845,0.00014257497,0.00030873145,0.00048413363,0.000827131],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011903107,0.0035477828,0.0021723711,0.002840471,0.003203823,0.0040772185,0.0038769876,0.0064338217,0.99076194],"category_scores_gemma":[0.0017100974,0.001466464,0.0016024665,0.002787872,0.0028573275,0.006860818,0.0036890847,0.003261831,0.99420494],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005168897,0.00034301716,0.0014352057,0.0008568407,0.00005636054,0.00039054386,0.00019115894,0.00060301827,0.0027954613,0.0065622022,0.43776128,0.54848796],"study_design_scores_gemma":[0.00008776079,0.00018387864,0.0012703633,0.00053837756,0.000021398133,0.000444728,0.00023280068,0.00020620474,0.0003892759,0.00075434323,0.9958335,0.000037307334],"about_ca_topic_score_codex":0.006088252,"about_ca_topic_score_gemma":0.0057257656,"teacher_disagreement_score":0.009238064,"about_ca_system_score_codex":0.001235389,"about_ca_system_score_gemma":0.0009739603,"threshold_uncertainty_score":0.013176978},"labels":[],"label_agreement":null},{"id":"W4406438041","doi":"10.1016/0967-0653(95)96545-g","title":"10.1016/0967-0653(95)96545-g","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Promontory; Geology; Seismology; Geography; Archaeology","score_opus":0.00859295121422462,"score_gpt":0.16364330431762528,"score_spread":0.15505035310340065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406438041","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00059166865,0.00034384095,0.0005191551,0.00043618234,0.00028167837,0.0001417211,0.0010960302,0.00089956995,0.99569017],"genre_scores_gemma":[0.0009056277,0.00024253842,0.00036918226,0.00033640963,0.000083914376,0.00008833438,0.00049703923,0.00017398527,0.9973029],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99937457,0.000043978995,0.000057154597,0.00023968807,0.00013604847,0.0001485591],"domain_scores_gemma":[0.99794966,0.0005110707,0.00013881343,0.00025699913,0.00044117172,0.00070228474],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011424402,0.003251204,0.0021723134,0.0031578601,0.003311434,0.0038822722,0.0039285985,0.0065525738,0.9906086],"category_scores_gemma":[0.0017907677,0.0013547253,0.0015594141,0.0027045207,0.0026633206,0.006229806,0.0037627406,0.0029405847,0.9942878],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048650533,0.00033907135,0.0014469465,0.00076654035,0.000051502873,0.00038902985,0.00016864964,0.0005754069,0.0027142349,0.005784144,0.425095,0.562183],"study_design_scores_gemma":[0.00008962793,0.00017551926,0.0013805674,0.00052760966,0.000020755962,0.000458828,0.00021229532,0.00018244122,0.00035404915,0.00075485837,0.99580574,0.000037743852],"about_ca_topic_score_codex":0.0072959983,"about_ca_topic_score_gemma":0.0059550675,"teacher_disagreement_score":0.009391427,"about_ca_system_score_codex":0.0012915493,"about_ca_system_score_gemma":0.00091653416,"threshold_uncertainty_score":0.014507055},"labels":[],"label_agreement":null},{"id":"W4406438789","doi":"10.1016/0967-0653(95)94344-p","title":"10.1016/0967-0653(95)94344-p","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Trench; Margin (machine learning); Tectonics; Seismology; Paleontology","score_opus":0.00860363425632617,"score_gpt":0.1636775209116763,"score_spread":0.15507388665535013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406438789","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005528618,0.00035168807,0.00047008696,0.0004118777,0.00028318822,0.00014717119,0.0010391294,0.0008718886,0.9958721],"genre_scores_gemma":[0.00076585315,0.00027531854,0.00036863127,0.0003562771,0.00008927311,0.0000992415,0.00045280866,0.00018931967,0.9974032],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992644,0.000053497013,0.000068143316,0.00028719302,0.0001595751,0.00016710589],"domain_scores_gemma":[0.9973525,0.0007293915,0.00015758892,0.00032772604,0.00054529094,0.0008875835],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012883039,0.0038975968,0.0024553346,0.0034001088,0.0036779672,0.0042800778,0.004359109,0.007703662,0.9913545],"category_scores_gemma":[0.0021062815,0.0015961789,0.0016789801,0.0031336646,0.0030422502,0.0075083566,0.004416621,0.00335759,0.9942959],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048550716,0.00035227087,0.0012608101,0.00084333867,0.00005096609,0.00039299854,0.0001846933,0.0006177984,0.0022235485,0.00586436,0.45523164,0.5324921],"study_design_scores_gemma":[0.000097748234,0.00019509725,0.001298926,0.00057642243,0.000022002427,0.00045202379,0.0002219574,0.0002106328,0.00033225224,0.0008272787,0.99572515,0.000040447667],"about_ca_topic_score_codex":0.007033229,"about_ca_topic_score_gemma":0.0054509705,"teacher_disagreement_score":0.008645475,"about_ca_system_score_codex":0.0013817436,"about_ca_system_score_gemma":0.0010097312,"threshold_uncertainty_score":0.013984561},"labels":[],"label_agreement":null},{"id":"W4406438988","doi":"10.1016/0967-0653(94)93537-8","title":"10.1016/0967-0653(94)93537-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Bay; BENGAL; Mixing (physics); Barium; Geology; Oceanography; Environmental science; Chemistry; Physics","score_opus":0.008619931621516287,"score_gpt":0.1635603398435326,"score_spread":0.15494040822201632,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406438988","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00055651314,0.000354132,0.0004267647,0.00039097533,0.00028623577,0.00012749647,0.0009682968,0.0008388954,0.99605066],"genre_scores_gemma":[0.0007451848,0.00025885282,0.00030452447,0.00033336945,0.00008457476,0.00007718802,0.00047204664,0.00017247986,0.99755186],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993092,0.000047544847,0.00007216062,0.00024792005,0.00015357358,0.00016965714],"domain_scores_gemma":[0.9974477,0.00064827513,0.00015144255,0.00031425813,0.00058836944,0.0008498955],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012677212,0.0035576934,0.0023582983,0.003151451,0.0033805205,0.0043358207,0.004008587,0.0071334317,0.99203026],"category_scores_gemma":[0.0019167308,0.0016078585,0.0016949703,0.0029850702,0.0029600651,0.006871847,0.0040004663,0.0032316977,0.9950216],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004991614,0.0003440888,0.0016253883,0.0007841057,0.000057665915,0.00041365912,0.0001702844,0.0005664577,0.0026783852,0.0052356664,0.4368364,0.5507887],"study_design_scores_gemma":[0.00010578754,0.00020581216,0.0015386904,0.0006195201,0.00002435637,0.00054400624,0.0002490712,0.00021960301,0.0004144976,0.0008110154,0.9952238,0.000043873923],"about_ca_topic_score_codex":0.006014436,"about_ca_topic_score_gemma":0.005504602,"teacher_disagreement_score":0.007969737,"about_ca_system_score_codex":0.0012551742,"about_ca_system_score_gemma":0.0009939361,"threshold_uncertainty_score":0.0119588375},"labels":[],"label_agreement":null},{"id":"W4406439710","doi":"10.1016/0967-0653(96)86383-6","title":"10.1016/0967-0653(96)86383-6","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Geodesy","score_opus":0.00853264423483824,"score_gpt":0.16312710802195549,"score_spread":0.15459446378711725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406439710","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005663013,0.0004083093,0.0005261664,0.00039850865,0.00030102793,0.00014430315,0.0010038557,0.0009153591,0.9957361],"genre_scores_gemma":[0.0007343851,0.00027934005,0.00034750806,0.00032733713,0.00009090976,0.00008705516,0.0004850211,0.00018380956,0.99746454],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992465,0.0000514572,0.00008076091,0.0002794561,0.00016225,0.00017968962],"domain_scores_gemma":[0.9973212,0.0006880563,0.00017328172,0.00034112166,0.0005970843,0.0008794044],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0014487064,0.003986952,0.0026071118,0.0032111988,0.003488377,0.0044655153,0.0042359577,0.0071301255,0.9914356],"category_scores_gemma":[0.0018512417,0.0016628443,0.0018417177,0.0031303982,0.0031351768,0.00758227,0.004301113,0.0035842427,0.9951403],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005587513,0.0003409734,0.0014802958,0.0008814228,0.000062948,0.00040457898,0.00017359562,0.00064585323,0.0028737609,0.005550903,0.41792667,0.56910026],"study_design_scores_gemma":[0.00011572304,0.00022866996,0.0014323364,0.0006711578,0.00002575829,0.00053962483,0.00024978377,0.00024763463,0.00043617436,0.0008529543,0.9951513,0.00004884155],"about_ca_topic_score_codex":0.0059281886,"about_ca_topic_score_gemma":0.0055115526,"teacher_disagreement_score":0.008564413,"about_ca_system_score_codex":0.0013510103,"about_ca_system_score_gemma":0.0009947929,"threshold_uncertainty_score":0.012216091},"labels":[],"label_agreement":null},{"id":"W4406440483","doi":"10.1016/0967-0653(96)89997-2","title":"10.1016/0967-0653(96)89997-2","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Event (particle physics); Field (mathematics); Oceanography","score_opus":0.008596575748739722,"score_gpt":0.16341916129601716,"score_spread":0.15482258554727743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406440483","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005446636,0.00038328118,0.0005119071,0.00038043267,0.00029034904,0.00013298067,0.0009729522,0.0008657286,0.9959176],"genre_scores_gemma":[0.00070880685,0.00024689164,0.0003250632,0.00029519343,0.00007834524,0.00007664403,0.00047108115,0.00017315487,0.9976248],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993311,0.00004565768,0.00006702277,0.0002562846,0.0001468424,0.00015303702],"domain_scores_gemma":[0.9977678,0.00055911194,0.00014028451,0.00028183789,0.00052641495,0.0007246108],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012517959,0.0035547973,0.0022755913,0.003049097,0.003159519,0.0041746823,0.0038563781,0.0062682354,0.9907334],"category_scores_gemma":[0.0017185499,0.00147829,0.001636942,0.0028816222,0.0027891265,0.006851785,0.0037322983,0.0032775826,0.9948584],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005033,0.00032062692,0.0014352553,0.0007872309,0.000057382567,0.00039457364,0.00016008642,0.0005898719,0.0027593297,0.005447147,0.4319392,0.5556059],"study_design_scores_gemma":[0.00009886858,0.00019467033,0.0012680615,0.00059804175,0.000023024371,0.0005157778,0.00022861095,0.00023014,0.00039594038,0.0007790816,0.99562633,0.000041495045],"about_ca_topic_score_codex":0.0055446066,"about_ca_topic_score_gemma":0.0051188143,"teacher_disagreement_score":0.009266615,"about_ca_system_score_codex":0.0012649646,"about_ca_system_score_gemma":0.000913656,"threshold_uncertainty_score":0.013217628},"labels":[],"label_agreement":null},{"id":"W4406444459","doi":"10.1016/s0967-0653(97)80992-1","title":"10.1016/s0967-0653(97)80992-1","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Trench; Geology; Seismology; Volcano; Deformation (meteorology); Tectonics; Plate tectonics; Oceanography","score_opus":0.009964033557429383,"score_gpt":0.16649690023773958,"score_spread":0.1565328666803102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406444459","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00042528566,0.00032864528,0.0004835689,0.00037009816,0.0002705493,0.000114258066,0.00085628603,0.0008082242,0.99634296],"genre_scores_gemma":[0.0005014145,0.00017043947,0.00025979767,0.0002097005,0.00006279812,0.00006665429,0.00037892145,0.00015155181,0.9981987],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99931073,0.00004504048,0.000059899277,0.00027105023,0.00016718458,0.00014606482],"domain_scores_gemma":[0.9977876,0.0004956391,0.00015556892,0.00028436302,0.0005552568,0.00072159845],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011578663,0.0032743285,0.0022025115,0.0031032278,0.0026105111,0.00430115,0.0037086005,0.006487381,0.9910096],"category_scores_gemma":[0.0017706782,0.0011861343,0.0015508662,0.0028213274,0.00226023,0.006305718,0.003516531,0.0030592575,0.99449795],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037723864,0.00023918819,0.0009182593,0.00059954537,0.00003942206,0.00027018873,0.00013047307,0.00043702355,0.001971024,0.00584192,0.4216879,0.5674878],"study_design_scores_gemma":[0.000062757324,0.00012389837,0.00074544724,0.00038384084,0.000014926671,0.00032798428,0.00012747546,0.00016347317,0.00024494823,0.00054292,0.99723536,0.000026939282],"about_ca_topic_score_codex":0.0050585223,"about_ca_topic_score_gemma":0.0042585405,"teacher_disagreement_score":0.008990407,"about_ca_system_score_codex":0.0013036435,"about_ca_system_score_gemma":0.0011529543,"threshold_uncertainty_score":0.012823641},"labels":[],"label_agreement":null},{"id":"W4406446819","doi":"10.1016/s0967-0653(98)82901-3","title":"10.1016/s0967-0653(98)82901-3","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Accretion (finance); Astrophysics; Physics","score_opus":0.008730564413274876,"score_gpt":0.16662583287538968,"score_spread":0.1578952684621148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406446819","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00046569176,0.00034435285,0.0005147357,0.00038091152,0.0002827005,0.00011875213,0.00089939503,0.00087952876,0.9961138],"genre_scores_gemma":[0.00055713917,0.00017751726,0.00027424464,0.00022559502,0.00006956762,0.00006504656,0.000360701,0.00015533275,0.99811494],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99931014,0.000044240915,0.00006297155,0.00026999234,0.00016558217,0.00014697577],"domain_scores_gemma":[0.99751484,0.0005646543,0.00018462102,0.0003158748,0.0006313577,0.0007886104],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012262202,0.0032744827,0.0022277515,0.0031296248,0.002756917,0.0045386706,0.0038052716,0.00669463,0.9910397],"category_scores_gemma":[0.0018352448,0.0012575369,0.0016515173,0.0029015266,0.0024103674,0.006494718,0.0036590344,0.0032196182,0.9946504],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040546912,0.00025517523,0.0010741096,0.0006596529,0.000045670276,0.00029645237,0.00014603356,0.000482082,0.0021342223,0.006129081,0.4207508,0.5676213],"study_design_scores_gemma":[0.00007072122,0.00014712772,0.0008301582,0.00043078186,0.000017418237,0.00038345088,0.0001442087,0.00018291596,0.00027745625,0.0005733169,0.9969118,0.00003081266],"about_ca_topic_score_codex":0.004961765,"about_ca_topic_score_gemma":0.0041751685,"teacher_disagreement_score":0.008960307,"about_ca_system_score_codex":0.0012554503,"about_ca_system_score_gemma":0.0011269829,"threshold_uncertainty_score":0.012780786},"labels":[],"label_agreement":null},{"id":"W4406447144","doi":"10.1016/s0967-0653(98)82941-4","title":"10.1016/s0967-0653(98)82941-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Tectonics; Fracture (geology); Paleontology","score_opus":0.008733245647509272,"score_gpt":0.16628842740046174,"score_spread":0.15755518175295247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406447144","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00046214488,0.00036794646,0.00048592166,0.00039691495,0.00029120507,0.000120868346,0.0009318025,0.0008715781,0.9960716],"genre_scores_gemma":[0.0005186295,0.00017960368,0.00026460196,0.00023514961,0.000068493806,0.00006778421,0.000374531,0.00015204279,0.99813914],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99928683,0.000046643683,0.00006547522,0.00028143424,0.00017006157,0.00014952192],"domain_scores_gemma":[0.9974663,0.00058073446,0.00018610914,0.00032685793,0.00063831406,0.0008017232],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012630528,0.0034567234,0.0023140968,0.0032307506,0.002868637,0.004605583,0.004061673,0.0071359714,0.99128175],"category_scores_gemma":[0.0018644602,0.0013304777,0.0017474988,0.0030364043,0.0025213582,0.0067812484,0.0038142167,0.0033640058,0.9948272],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040277964,0.0002537244,0.0010467983,0.00068599405,0.00004667224,0.00029322188,0.00014302165,0.000469255,0.002069176,0.0060310164,0.4216273,0.56693107],"study_design_scores_gemma":[0.00007396331,0.00014636219,0.00083964015,0.0004627065,0.000017896444,0.0003797257,0.00014655494,0.00017714169,0.00027486178,0.00057490834,0.9968746,0.000031751275],"about_ca_topic_score_codex":0.0052993833,"about_ca_topic_score_gemma":0.0043503945,"teacher_disagreement_score":0.008718252,"about_ca_system_score_codex":0.0013314501,"about_ca_system_score_gemma":0.0011978243,"threshold_uncertainty_score":0.012435436},"labels":[],"label_agreement":null},{"id":"W4406447816","doi":"10.1016/s0967-0653(98)85881-x","title":"10.1016/s0967-0653(98)85881-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Transect; Margin (machine learning); Geology; Geography; Seismology; Oceanography; Computer science","score_opus":0.00874576309785715,"score_gpt":0.16638055062713622,"score_spread":0.15763478752927906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406447816","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00047686888,0.00035315266,0.0005006843,0.0003887383,0.000271962,0.000120508514,0.0008506748,0.0008701365,0.99616724],"genre_scores_gemma":[0.0005400342,0.00017703528,0.0002791929,0.00022815984,0.00006545486,0.00006531973,0.0003594331,0.00015028629,0.9981351],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993672,0.000040125105,0.000057065125,0.00024670584,0.00015282173,0.00013615013],"domain_scores_gemma":[0.99767035,0.0005252659,0.00017982569,0.0003038429,0.00051530683,0.0008054184],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011573314,0.0033248842,0.002089297,0.0030970504,0.0027247674,0.004081302,0.0038152407,0.0065998337,0.9906797],"category_scores_gemma":[0.0017542688,0.0012347397,0.001550286,0.0027634783,0.0023711168,0.0066440958,0.003523395,0.0031156407,0.993982],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038738028,0.00027062517,0.0011091426,0.00068785984,0.00004361862,0.00029838446,0.00015515967,0.00046150896,0.0021065157,0.0065402607,0.41435164,0.57358795],"study_design_scores_gemma":[0.00006592418,0.00013635741,0.0009053258,0.00039261946,0.000017006805,0.00037621136,0.00015404473,0.00016505134,0.00028427568,0.000577001,0.9968972,0.000028984532],"about_ca_topic_score_codex":0.0053617777,"about_ca_topic_score_gemma":0.004465865,"teacher_disagreement_score":0.009320319,"about_ca_system_score_codex":0.0012247988,"about_ca_system_score_gemma":0.0011401213,"threshold_uncertainty_score":0.01329428},"labels":[],"label_agreement":null},{"id":"W4406447887","doi":"10.1016/s0967-0653(98)85868-7","title":"10.1016/s0967-0653(98)85868-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Volcano; Geology; Ridge; Seismology; Swarm behaviour; Earthquake swarm; Earth science; Paleontology; Induced seismicity; Computer science; Artificial intelligence","score_opus":0.008739638035778374,"score_gpt":0.1663317749631336,"score_spread":0.15759213692735521,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406447887","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004928096,0.0003893651,0.00051011355,0.0003902473,0.00029852465,0.00011885718,0.0009008038,0.0009002863,0.995999],"genre_scores_gemma":[0.0005614122,0.00018674099,0.00028063476,0.00023512087,0.00007165223,0.00006712483,0.00037846007,0.00015301432,0.99806577],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993006,0.000045095636,0.00006645333,0.00026860804,0.00016606244,0.0001531563],"domain_scores_gemma":[0.9975292,0.00056241546,0.00018884767,0.0003165953,0.0006125546,0.0007904884],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012430702,0.0034079964,0.0022692322,0.0031667978,0.0027556038,0.004312718,0.003876444,0.006850282,0.99092263],"category_scores_gemma":[0.0018000879,0.0012652586,0.0016765137,0.0029393993,0.0024165763,0.0065879365,0.00368844,0.0031828056,0.9946169],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041970293,0.00025656098,0.0011342749,0.00068565545,0.000047115016,0.00029682877,0.00014370453,0.0004667751,0.0022223531,0.0059679816,0.40837425,0.5799847],"study_design_scores_gemma":[0.00007210838,0.00015118666,0.0008892854,0.00044993937,0.000017892742,0.00039128354,0.0001504042,0.0001773334,0.00029174748,0.00058693765,0.99679023,0.00003148959],"about_ca_topic_score_codex":0.004906472,"about_ca_topic_score_gemma":0.0041237823,"teacher_disagreement_score":0.00907737,"about_ca_system_score_codex":0.0012587083,"about_ca_system_score_gemma":0.0011371055,"threshold_uncertainty_score":0.012947738},"labels":[],"label_agreement":null},{"id":"W4406453418","doi":"10.1016/s0967-0653(97)87827-1","title":"10.1016/s0967-0653(97)87827-1","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Rift; Seismology; Strike-slip tectonics; Slip (aerodynamics); Paleontology; Fault (geology); Tectonics; Engineering","score_opus":0.01032464839604981,"score_gpt":0.1673042647727185,"score_spread":0.15697961637666868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406453418","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00042238776,0.00033916807,0.00048364527,0.00036770693,0.00026867512,0.000116013885,0.0008684917,0.00083650363,0.9962974],"genre_scores_gemma":[0.0004934806,0.00017581477,0.00025823934,0.00021016822,0.000064561114,0.00006479514,0.000377842,0.00014866848,0.9982064],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993124,0.000045131193,0.00006026931,0.00026346353,0.00017075872,0.00014805161],"domain_scores_gemma":[0.9977023,0.00050764903,0.00016497746,0.00028886125,0.00058835995,0.00074781646],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011497156,0.0032653813,0.0022626724,0.0032007897,0.0026513797,0.0042685284,0.0038008704,0.0064799604,0.99081343],"category_scores_gemma":[0.0018008891,0.0011650348,0.0015488561,0.0029090634,0.002191377,0.0061317743,0.0035033687,0.002947963,0.9943627],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036104347,0.00023546618,0.0009581049,0.0005997414,0.000040320527,0.00026882903,0.00012733364,0.00043779606,0.0019413691,0.0056022345,0.41838467,0.5710431],"study_design_scores_gemma":[0.00006359019,0.00012529099,0.0007652701,0.00039232915,0.000015884167,0.00032741931,0.0001287449,0.0001610019,0.00025120896,0.0005170763,0.99722517,0.0000270055],"about_ca_topic_score_codex":0.0053554955,"about_ca_topic_score_gemma":0.0045974627,"teacher_disagreement_score":0.009186566,"about_ca_system_score_codex":0.0013173693,"about_ca_system_score_gemma":0.001208857,"threshold_uncertainty_score":0.013103545},"labels":[],"label_agreement":null},{"id":"W4406453827","doi":"10.1016/s0967-0653(97)84673-x","title":"10.1016/s0967-0653(97)84673-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Margin (machine learning); Geology; Seismology; Computer science","score_opus":0.009984238886258134,"score_gpt":0.16645287768914152,"score_spread":0.1564686388028834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406453827","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000466203,0.0003772249,0.0004970478,0.00036388624,0.00028110744,0.000117595555,0.00092920806,0.0008543922,0.9961133],"genre_scores_gemma":[0.0005234115,0.00018557099,0.0002736876,0.00021776289,0.00006550817,0.00006526417,0.0003982249,0.00016035313,0.9981102],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99933654,0.000042471507,0.00006106363,0.00025643635,0.0001595571,0.00014392186],"domain_scores_gemma":[0.9976284,0.0005367541,0.0001860006,0.00031052728,0.0005195064,0.0008189007],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011810389,0.0036077881,0.0022714583,0.0031813446,0.0027642301,0.0042866548,0.0040510506,0.006841328,0.9909422],"category_scores_gemma":[0.0017199387,0.0013297005,0.0016478262,0.003061089,0.0024900637,0.006768033,0.0036735034,0.0032317608,0.9943878],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004004855,0.00026701196,0.0010659536,0.0007113108,0.00004581526,0.00029864794,0.00014823648,0.0004700834,0.0021736862,0.0065351655,0.4068621,0.5810214],"study_design_scores_gemma":[0.000068285204,0.00013655903,0.0008893699,0.00039915682,0.000017344139,0.00037299513,0.00015189461,0.00016567444,0.0003036463,0.0005970543,0.9968669,0.00003110776],"about_ca_topic_score_codex":0.0055919797,"about_ca_topic_score_gemma":0.004692057,"teacher_disagreement_score":0.00905782,"about_ca_system_score_codex":0.0013116184,"about_ca_system_score_gemma":0.0011850919,"threshold_uncertainty_score":0.012919903},"labels":[],"label_agreement":null},{"id":"W4406453949","doi":"10.1016/s0967-0653(97)84670-4","title":"10.1016/s0967-0653(97)84670-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Seismology; Sequence (biology); Geology; Trough (economics); Biology; Genetics; Economics","score_opus":0.009984464247976142,"score_gpt":0.1666927768421212,"score_spread":0.15670831259414505,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406453949","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00044421369,0.00038021908,0.00049953785,0.00036966405,0.0002916506,0.00011752067,0.00095753756,0.00085858285,0.99608105],"genre_scores_gemma":[0.0004858427,0.00017956708,0.00025321735,0.00021729711,0.00006556284,0.00006437321,0.00038255143,0.00015597577,0.9981956],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99927634,0.000047098143,0.0000674521,0.00027968362,0.00017411986,0.00015527653],"domain_scores_gemma":[0.99739337,0.0005945563,0.00019315674,0.0003289664,0.0006549107,0.00083493185],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012708955,0.0036568448,0.0024178685,0.0033712413,0.0028376929,0.0046466845,0.0041781035,0.00730534,0.9914069],"category_scores_gemma":[0.0018199421,0.0013870517,0.0017997477,0.003316315,0.0025294735,0.006838536,0.0038721322,0.0033714976,0.99509025],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039794063,0.00025088602,0.0010226434,0.00068790733,0.000047255806,0.00028270297,0.00013416377,0.00047909544,0.002146871,0.0059634433,0.40986383,0.5787232],"study_design_scores_gemma":[0.00007165765,0.00014171418,0.00082153035,0.00044583567,0.000017637482,0.00035865232,0.00014409749,0.00017207932,0.0002936389,0.00056869665,0.9969319,0.00003256822],"about_ca_topic_score_codex":0.005489199,"about_ca_topic_score_gemma":0.0045821364,"teacher_disagreement_score":0.008593082,"about_ca_system_score_codex":0.0014198932,"about_ca_system_score_gemma":0.0012363644,"threshold_uncertainty_score":0.01225692},"labels":[],"label_agreement":null},{"id":"W4406462860","doi":"10.1016/0967-0653(96)84144-5","title":"10.1016/0967-0653(96)84144-5","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Induced seismicity; Geology; Seismology; Structural basin; Oceanography; Paleontology; Tectonics","score_opus":0.008534101151230771,"score_gpt":0.16298565202093798,"score_spread":0.15445155086970722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406462860","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00060072186,0.0004214979,0.0005004073,0.0004039301,0.00032295875,0.00014870099,0.0010016629,0.0009251719,0.9956749],"genre_scores_gemma":[0.00072996237,0.00028449623,0.00031591477,0.00033574027,0.000094352195,0.00008653184,0.00044238966,0.00017986092,0.99753076],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99918157,0.000058337784,0.00008314925,0.00031463208,0.0001635314,0.00019880458],"domain_scores_gemma":[0.9972064,0.0007359571,0.00017309858,0.00033785275,0.00060482026,0.0009418718],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0014971878,0.0042128805,0.002896442,0.0034524521,0.0037625835,0.0046348935,0.0045267963,0.007698761,0.991797],"category_scores_gemma":[0.0019588086,0.0017439787,0.0019150268,0.003330323,0.0033722424,0.007939463,0.0046218294,0.0037046752,0.99505746],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006101489,0.00037103627,0.0016049087,0.00095625693,0.00006782135,0.0004535647,0.00019905934,0.00072143454,0.0030114003,0.0058118603,0.4192471,0.56694543],"study_design_scores_gemma":[0.00012508701,0.0002650763,0.0014741159,0.000763047,0.000028427565,0.0005423722,0.0002862634,0.00027112904,0.0004328269,0.00086500554,0.9948955,0.000051076153],"about_ca_topic_score_codex":0.00625615,"about_ca_topic_score_gemma":0.0058794604,"teacher_disagreement_score":0.00820303,"about_ca_system_score_codex":0.001418227,"about_ca_system_score_gemma":0.0010106165,"threshold_uncertainty_score":0.012439489},"labels":[],"label_agreement":null},{"id":"W4406463449","doi":"10.1016/0967-0653(96)80316-s","title":"10.1016/0967-0653(96)80316-s","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Ridge; Geology; Mid-Atlantic Ridge; Partial melting; Seismology; Paleontology; Basalt","score_opus":0.008556616588843395,"score_gpt":0.16349542757423968,"score_spread":0.15493881098539627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406463449","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004420551,0.0002516879,0.00038335222,0.00031488092,0.0002436743,0.000107697066,0.00078934775,0.00070420996,0.9967631],"genre_scores_gemma":[0.00062459306,0.0001827992,0.00025377824,0.00020472363,0.000067628294,0.000054525768,0.0003633573,0.00013487088,0.99811375],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994253,0.000045018067,0.000054455555,0.00020654546,0.00014378852,0.00012487869],"domain_scores_gemma":[0.9978142,0.00047277613,0.00012665213,0.00026272782,0.00054478616,0.0007788236],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010101849,0.0028209744,0.0018047969,0.0028461234,0.0027401065,0.003590846,0.0030277427,0.005402586,0.9905048],"category_scores_gemma":[0.0016365304,0.0010852308,0.0013658402,0.0025869566,0.0020333156,0.005179305,0.0033018934,0.0023740241,0.9933513],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041288018,0.00025763124,0.0011463306,0.0006176693,0.000040064093,0.00028957776,0.0001379749,0.0005084229,0.0024613242,0.005666579,0.43708664,0.551375],"study_design_scores_gemma":[0.000056713765,0.00013607067,0.0009925797,0.00033968745,0.000013410737,0.0002980751,0.00014525135,0.00014739542,0.0002806696,0.0005218836,0.9970432,0.000025085494],"about_ca_topic_score_codex":0.0058497107,"about_ca_topic_score_gemma":0.0049511916,"teacher_disagreement_score":0.009495199,"about_ca_system_score_codex":0.0011231824,"about_ca_system_score_gemma":0.0009356536,"threshold_uncertainty_score":0.013543725},"labels":[],"label_agreement":null},{"id":"W4406466534","doi":"10.1016/0967-0653(95)94345-q","title":"10.1016/0967-0653(95)94345-q","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Forearc; Geology; Induced seismicity; Seismology; Tectonics; Subduction","score_opus":0.00860363425632617,"score_gpt":0.1636775209116763,"score_spread":0.15507388665535013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406466534","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005323485,0.00027933027,0.00043037286,0.0003816481,0.00024513897,0.00012334806,0.00095742446,0.00076921354,0.9962812],"genre_scores_gemma":[0.0008282318,0.00020165187,0.00032662292,0.0003017086,0.00007526102,0.00007881671,0.00044687573,0.00016520116,0.9975756],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993326,0.000050236413,0.000059649876,0.00024291991,0.0001588441,0.00015566693],"domain_scores_gemma":[0.9975375,0.00061740255,0.00014474051,0.0003210382,0.00054178166,0.0008375729],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011730733,0.0030706574,0.002059362,0.003016224,0.0033255178,0.0039238967,0.0038274839,0.0064427434,0.9916198],"category_scores_gemma":[0.001978936,0.001318472,0.001513635,0.0027388546,0.0026472355,0.0062201545,0.00373982,0.0028685045,0.993999],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004349948,0.00034063513,0.0013940651,0.00068757386,0.000046501813,0.00036220506,0.0001703485,0.00049917126,0.0023478656,0.005995164,0.41332093,0.57440054],"study_design_scores_gemma":[0.00008351799,0.00017004959,0.0013603617,0.0004796462,0.00001907616,0.00040852925,0.00020050883,0.00016912981,0.00031058793,0.00077209336,0.9959913,0.00003523437],"about_ca_topic_score_codex":0.0071705445,"about_ca_topic_score_gemma":0.005827452,"teacher_disagreement_score":0.008380175,"about_ca_system_score_codex":0.0012434237,"about_ca_system_score_gemma":0.0010187353,"threshold_uncertainty_score":0.014257669},"labels":[],"label_agreement":null},{"id":"W4406467059","doi":"10.1016/0967-0653(96)80998-7","title":"10.1016/0967-0653(96)80998-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Subduction; Geology; Seismology; Shear zone; Induced seismicity; Shear (geology); Petrology; Tectonics","score_opus":0.008543053769359432,"score_gpt":0.16337763045921633,"score_spread":0.1548345766898569,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406467059","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00056222145,0.0004055563,0.00048333773,0.0003809676,0.00029902562,0.000130207,0.0009281673,0.0008863072,0.9959241],"genre_scores_gemma":[0.000715104,0.00025761526,0.00030223353,0.00029473577,0.00008297657,0.00008015245,0.00046172173,0.00017187081,0.99763346],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99928564,0.0000486815,0.00007425839,0.00026814995,0.0001505277,0.00017279678],"domain_scores_gemma":[0.9975248,0.0006276989,0.00016359425,0.0003082371,0.0005789718,0.0007965936],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013399669,0.0038757902,0.002521724,0.0031606138,0.0032836602,0.0043978305,0.0040975874,0.0066962503,0.9911981],"category_scores_gemma":[0.0018027278,0.0015469873,0.0017280994,0.0029860185,0.0030782553,0.0072703245,0.0040247715,0.0034200344,0.9950458],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055061845,0.00031872911,0.0013838757,0.00082693563,0.000058360714,0.0003989749,0.00016820626,0.00061247573,0.0028297252,0.005546521,0.4195333,0.5677723],"study_design_scores_gemma":[0.000104260034,0.00021837602,0.0013150299,0.0006468762,0.000023932515,0.0005285312,0.00024600935,0.00023938964,0.00041995783,0.00086185284,0.99535084,0.000044881173],"about_ca_topic_score_codex":0.0054623587,"about_ca_topic_score_gemma":0.004876683,"teacher_disagreement_score":0.0088018775,"about_ca_system_score_codex":0.0012929179,"about_ca_system_score_gemma":0.0009374999,"threshold_uncertainty_score":0.012554824},"labels":[],"label_agreement":null},{"id":"W4406468882","doi":"10.1016/0967-0653(95)99407-i","title":"10.1016/0967-0653(95)99407-i","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Shear (geology); Deformation (meteorology); Strain (injury); Strain rate; Seismology; Geodesy; Materials science; Petrology; Composite material; Anatomy; Oceanography; Biology","score_opus":0.008583481860234258,"score_gpt":0.16376564741253616,"score_spread":0.1551821655523019,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406468882","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00045028646,0.00031397594,0.00037071164,0.0003393873,0.00024895027,0.00012242085,0.0008756366,0.0007292916,0.99654937],"genre_scores_gemma":[0.00063948747,0.0002113752,0.00026847995,0.00029159122,0.00007342479,0.00007816744,0.00045438614,0.00015890927,0.9978243],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99935645,0.000043291548,0.00005974256,0.00023759587,0.00015177348,0.00015119878],"domain_scores_gemma":[0.9977648,0.00055705954,0.00013376342,0.0002824667,0.00050983945,0.0007520889],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0010953248,0.0032659245,0.0022255299,0.0031431243,0.0033746925,0.004123888,0.004036193,0.0066661965,0.99116135],"category_scores_gemma":[0.001763683,0.0012887635,0.0015301076,0.0027376646,0.0026416138,0.0063527767,0.0036678447,0.0030047258,0.9943785],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004203484,0.0003423025,0.0013325384,0.00076303206,0.000046506968,0.00034488126,0.0001602095,0.00047928237,0.002376968,0.0053756973,0.46482453,0.52353364],"study_design_scores_gemma":[0.00007991019,0.00016456223,0.0011858447,0.00049220095,0.00001898984,0.00037561415,0.00019909393,0.00017771866,0.00033569924,0.00070048886,0.9962358,0.000034276967],"about_ca_topic_score_codex":0.0065848543,"about_ca_topic_score_gemma":0.0059565976,"teacher_disagreement_score":0.008838654,"about_ca_system_score_codex":0.0012610747,"about_ca_system_score_gemma":0.0010021839,"threshold_uncertainty_score":0.013093054},"labels":[],"label_agreement":null},{"id":"W4406469511","doi":"10.1016/0967-0653(94)91416-8","title":"10.1016/0967-0653(94)91416-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Seismotectonics; Geology; Oceanography; Pacific ocean; Pacific basin; Seismology; Tectonics","score_opus":0.008634158652888933,"score_gpt":0.16384853171538652,"score_spread":0.15521437306249758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406469511","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005253695,0.00036048162,0.00044428508,0.00040950385,0.00028883916,0.00014249748,0.0009637311,0.0008629784,0.99600226],"genre_scores_gemma":[0.0007015548,0.00027071498,0.0003038806,0.00033294546,0.00008860989,0.00008749849,0.0004680847,0.00018289844,0.99756384],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992316,0.0000532325,0.000077862824,0.0002815889,0.00016943735,0.00018629774],"domain_scores_gemma":[0.9972747,0.00068322883,0.00016195222,0.00033828538,0.00063399546,0.0009078504],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013610214,0.0038420055,0.002564958,0.0033852197,0.0035347608,0.0044674403,0.004120533,0.0071887695,0.99196494],"category_scores_gemma":[0.0019456177,0.0016198123,0.0017333109,0.003101831,0.0031061617,0.0070689376,0.004378845,0.003499813,0.9950789],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005246803,0.00034270552,0.0014456498,0.0008060945,0.000060368024,0.00039035073,0.00016201961,0.00062115275,0.0025760583,0.0052676396,0.4500507,0.5377525],"study_design_scores_gemma":[0.0001132807,0.00020789998,0.001456377,0.00061791803,0.000024599882,0.0005162222,0.00023089106,0.0002141005,0.00039274152,0.00076097477,0.99542075,0.000044111108],"about_ca_topic_score_codex":0.0062941713,"about_ca_topic_score_gemma":0.0055855107,"teacher_disagreement_score":0.008035064,"about_ca_system_score_codex":0.0013756715,"about_ca_system_score_gemma":0.0010020507,"threshold_uncertainty_score":0.012515068},"labels":[],"label_agreement":null},{"id":"W4406480511","doi":"10.1016/0967-0653(93)95865-4","title":"10.1016/0967-0653(93)95865-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Bathymetry; Geology; Subduction; Seismology; Sedimentary rock; Oceanography; Paleontology; Tectonics","score_opus":0.008046155224861809,"score_gpt":0.16004143599869464,"score_spread":0.15199528077383284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406480511","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00055947015,0.00037155498,0.00047734755,0.00039535062,0.0002912597,0.00012921735,0.0009781528,0.00085092627,0.9959468],"genre_scores_gemma":[0.0007818968,0.0002581453,0.00030722158,0.00033283228,0.00008671724,0.00007684444,0.0004713141,0.00017404315,0.997511],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993186,0.000045244942,0.00006631171,0.0002568405,0.00015065949,0.00016224747],"domain_scores_gemma":[0.9977791,0.00055983535,0.00014140876,0.00027123734,0.0005191905,0.0007292569],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012270426,0.003574073,0.0023062408,0.0031059713,0.0033048969,0.0042607505,0.0038166542,0.006704463,0.99144816],"category_scores_gemma":[0.0016942322,0.0015058811,0.0016399286,0.0030139778,0.0028345438,0.006639477,0.003784005,0.0032362337,0.9946437],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047793135,0.00032949442,0.0015746485,0.0007550658,0.00005912982,0.00040642568,0.00016394857,0.000610764,0.0027388525,0.005308888,0.4359131,0.5516618],"study_design_scores_gemma":[0.000101273006,0.00020432635,0.0014526666,0.0005910569,0.00002446174,0.00053876423,0.00023702272,0.00022599875,0.00042620333,0.000784118,0.9953725,0.000041500018],"about_ca_topic_score_codex":0.006111055,"about_ca_topic_score_gemma":0.0055416487,"teacher_disagreement_score":0.008551836,"about_ca_system_score_codex":0.0012880653,"about_ca_system_score_gemma":0.00097482,"threshold_uncertainty_score":0.012198091},"labels":[],"label_agreement":null},{"id":"W4406480540","doi":"10.1016/0967-0653(95)94372-w","title":"10.1016/0967-0653(95)94372-w","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Cenozoic; Geology; Tectonics; Stress field; Structural basin; Paleontology; Seismology; Field (mathematics); Engineering","score_opus":0.008619273021593835,"score_gpt":0.16412506208800154,"score_spread":0.15550578906640772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406480540","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005885314,0.00031337328,0.000514452,0.00044357518,0.00026613305,0.00016629278,0.001003325,0.00091549486,0.99578875],"genre_scores_gemma":[0.0006918037,0.00020207038,0.00033799684,0.00032931683,0.00007033976,0.00008781266,0.00042906718,0.0001694045,0.9976821],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99934393,0.00004592093,0.000060352486,0.0002503109,0.00014557266,0.0001538234],"domain_scores_gemma":[0.9977597,0.00053021114,0.00013695037,0.00026808135,0.00050617853,0.00079888996],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011868626,0.0034794838,0.0021877196,0.0031061857,0.0033879522,0.003791985,0.003774576,0.0068360874,0.99066263],"category_scores_gemma":[0.0019193746,0.0013834949,0.0014563327,0.002736199,0.0025617077,0.006575908,0.0039080405,0.0028312101,0.99390644],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042089765,0.00034823015,0.0013432909,0.0007106378,0.000046714384,0.0003669659,0.00016274629,0.0004910516,0.0025619364,0.0049386006,0.44721144,0.54139745],"study_design_scores_gemma":[0.000092534305,0.00018017007,0.0014047452,0.0004916938,0.000020754649,0.0004030685,0.00020793689,0.0001828566,0.00034801115,0.00069170725,0.9959413,0.000035341563],"about_ca_topic_score_codex":0.0068572606,"about_ca_topic_score_gemma":0.005960252,"teacher_disagreement_score":0.009337366,"about_ca_system_score_codex":0.0012083425,"about_ca_system_score_gemma":0.0009518611,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4406483539","doi":"10.1016/0967-0653(95)94341-m","title":"10.1016/0967-0653(95)94341-m","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Subduction; Seismology; Geology; Tectonics","score_opus":0.00860363425632617,"score_gpt":0.1636775209116763,"score_spread":0.15507388665535013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406483539","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00049431564,0.00026464334,0.00040518751,0.00037955388,0.00022415633,0.00011722878,0.000926234,0.0007670738,0.9964216],"genre_scores_gemma":[0.00069049175,0.00016944611,0.00027084874,0.0002720699,0.00006499564,0.000062358515,0.00039682814,0.00013829181,0.9979348],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99946994,0.000038811067,0.000044008906,0.00020055051,0.0001236019,0.0001232489],"domain_scores_gemma":[0.99820983,0.00040773296,0.00011192966,0.00021936718,0.00039902423,0.00065207784],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0008909472,0.0026978257,0.0017698008,0.0027217346,0.0030257828,0.0034288138,0.0033667006,0.0058241026,0.9906446],"category_scores_gemma":[0.0015892395,0.0010833452,0.0013197918,0.0022746592,0.0019973998,0.0052679987,0.003437439,0.0023855702,0.9933722],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003721832,0.0002958411,0.0012127565,0.0006293636,0.00003822148,0.00030372216,0.00014267766,0.0004449285,0.0024031422,0.004653846,0.46884328,0.5206601],"study_design_scores_gemma":[0.000065634915,0.00013710091,0.0012554761,0.00038183053,0.000016699632,0.0003096003,0.00015580184,0.000139773,0.0003022182,0.00057856337,0.99663,0.000027371403],"about_ca_topic_score_codex":0.0064794593,"about_ca_topic_score_gemma":0.0057131704,"teacher_disagreement_score":0.009355426,"about_ca_system_score_codex":0.0010873269,"about_ca_system_score_gemma":0.0008461701,"threshold_uncertainty_score":0.013344288},"labels":[],"label_agreement":null},{"id":"W4406484674","doi":"10.1016/0967-0653(93)92626-u","title":"10.1016/0967-0653(93)92626-u","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Margin (machine learning); Submarine pipeline; Geology; Oceanography; Computer science","score_opus":0.0080618790293458,"score_gpt":0.15986119219143902,"score_spread":0.15179931316209322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406484674","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00052046514,0.00028631496,0.00039610217,0.00035876886,0.00024132356,0.00012352962,0.00090344064,0.00078863127,0.9963813],"genre_scores_gemma":[0.0007132154,0.00018270341,0.00026756525,0.00026003298,0.00006708399,0.00006564457,0.0004118891,0.00015465505,0.9978771],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994081,0.000042026495,0.000053233576,0.00021710197,0.0001352182,0.00014428496],"domain_scores_gemma":[0.99809605,0.00045413876,0.000115752766,0.00023564455,0.0004204898,0.00067789975],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0009931419,0.0028796403,0.0019172298,0.002854883,0.0031614793,0.0037724948,0.003244967,0.0061341687,0.99083954],"category_scores_gemma":[0.0016400479,0.0012618029,0.0013589548,0.0024947252,0.0022533573,0.00570429,0.0034641458,0.0025745926,0.9937643],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004217873,0.000317278,0.0014245969,0.00061585504,0.000041533458,0.00035986764,0.00015286046,0.0004466441,0.0024024844,0.004911802,0.42522052,0.5636847],"study_design_scores_gemma":[0.00007247841,0.00015632407,0.0013272829,0.0004010154,0.000017252047,0.00039956378,0.00018559677,0.00015931381,0.00033007853,0.0005730221,0.99634945,0.000028431068],"about_ca_topic_score_codex":0.0065364777,"about_ca_topic_score_gemma":0.0055085113,"teacher_disagreement_score":0.009160459,"about_ca_system_score_codex":0.0010490997,"about_ca_system_score_gemma":0.00087200355,"threshold_uncertainty_score":0.013066292},"labels":[],"label_agreement":null},{"id":"W4406485526","doi":"10.1016/0967-0653(96)86119-9","title":"10.1016/0967-0653(96)86119-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Field survey; Geology; Seismology; Field (mathematics); Mathematics","score_opus":0.008535813829888998,"score_gpt":0.1629535887325498,"score_spread":0.15441777490266081,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406485526","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005883281,0.00042532207,0.00049148407,0.00040649532,0.0003302517,0.00014566517,0.0009622097,0.00091163325,0.9957386],"genre_scores_gemma":[0.00075020257,0.00030963024,0.00032781315,0.00034591247,0.0000981076,0.00008835931,0.0004859994,0.00018391214,0.99741024],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99919266,0.00005645055,0.000087989414,0.00030281706,0.00016377607,0.00019625784],"domain_scores_gemma":[0.9973015,0.0007015195,0.00016520209,0.00034154495,0.0005814694,0.00090868166],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0014557359,0.0041378704,0.002757022,0.0033722296,0.003668284,0.004517285,0.0043309387,0.0075250715,0.9915799],"category_scores_gemma":[0.0019463338,0.0017351287,0.0018903149,0.0032837929,0.0031843479,0.0077908724,0.004563293,0.0037246128,0.99504447],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005676786,0.00038117156,0.0015514416,0.00093847583,0.000066648354,0.00043202713,0.00018808525,0.0006750061,0.002873998,0.0053663603,0.4263378,0.5606214],"study_design_scores_gemma":[0.000121403675,0.00024386008,0.0014734217,0.0007426486,0.000028120248,0.00057387655,0.0002900747,0.00026042483,0.0004373697,0.0008171921,0.99496067,0.000050861585],"about_ca_topic_score_codex":0.005888673,"about_ca_topic_score_gemma":0.005416599,"teacher_disagreement_score":0.00842011,"about_ca_system_score_codex":0.001337359,"about_ca_system_score_gemma":0.0009831678,"threshold_uncertainty_score":0.012010157},"labels":[],"label_agreement":null},{"id":"W4406493859","doi":"10.1016/0967-0653(94)91346-3","title":"10.1016/0967-0653(94)91346-3","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Hydrothermal circulation; Ophiolite; Geology; Permeability (electromagnetism); Geochemistry; Magma; Fracture (geology); Transition zone; Petrology; Seismology; Geotechnical engineering; Tectonics; Chemistry; Volcano","score_opus":0.008644256308933765,"score_gpt":0.16389023224059387,"score_spread":0.15524597593166012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406493859","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005401656,0.0003592244,0.000473302,0.00041000932,0.00029307886,0.00014173718,0.0010285578,0.0008850654,0.9958688],"genre_scores_gemma":[0.0007437264,0.0002692829,0.00032491944,0.00033594045,0.00009284991,0.000085125,0.00049195933,0.00018716636,0.99746895],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992544,0.000051326064,0.00007416774,0.00027624125,0.00016847425,0.00017539147],"domain_scores_gemma":[0.9972964,0.0006902942,0.00016147041,0.00033362402,0.0006381502,0.0008801045],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013357754,0.0037661649,0.0024805842,0.0033672987,0.003390858,0.004391661,0.0040012226,0.0068361787,0.9920219],"category_scores_gemma":[0.0019621302,0.0015673328,0.0017169849,0.0030568314,0.0029911762,0.0068080155,0.004241458,0.0034459205,0.9950748],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051549607,0.00034282668,0.0014823276,0.0007716772,0.000060508177,0.00038925602,0.00015864221,0.00063045975,0.0025840222,0.005105188,0.44775954,0.54020005],"study_design_scores_gemma":[0.000113861825,0.00021275152,0.0014979306,0.00060351175,0.000025034651,0.0005326882,0.00022578918,0.00022646482,0.00040503067,0.0007779949,0.99533373,0.000045299574],"about_ca_topic_score_codex":0.0062409337,"about_ca_topic_score_gemma":0.0054597305,"teacher_disagreement_score":0.007978082,"about_ca_system_score_codex":0.0013345929,"about_ca_system_score_gemma":0.0009811088,"threshold_uncertainty_score":0.01240921},"labels":[],"label_agreement":null},{"id":"W4406494737","doi":"10.1016/0967-0653(95)94893-7","title":"10.1016/0967-0653(95)94893-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology","score_opus":0.008602332965349312,"score_gpt":0.16363134715176966,"score_spread":0.15502901418642034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406494737","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0006109355,0.00041503558,0.0004923262,0.00043954168,0.00030346995,0.0001389229,0.0010088651,0.00089096924,0.9957],"genre_scores_gemma":[0.0007907757,0.00026114704,0.0003295634,0.0003581398,0.000081988044,0.00008273857,0.00048974017,0.00017408957,0.9974317],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992865,0.000049782597,0.00007277266,0.000263781,0.00015527618,0.00017196278],"domain_scores_gemma":[0.99752563,0.0006335734,0.0001600164,0.00029812977,0.0005794434,0.0008031767],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013038731,0.0035033587,0.0023755152,0.0030364678,0.0033007842,0.004244702,0.0039039613,0.0069455714,0.99123645],"category_scores_gemma":[0.0018666364,0.0014743085,0.0015995068,0.0028059566,0.0028864571,0.006812389,0.0039636027,0.003170518,0.99453753],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004981694,0.00033463078,0.001468759,0.00075303804,0.000055935347,0.00038022324,0.00015926977,0.0005536184,0.0026530637,0.005151306,0.41898936,0.56900257],"study_design_scores_gemma":[0.000102997925,0.00020939921,0.0014620776,0.00059791515,0.000024285624,0.00051036786,0.000232484,0.00021975381,0.00039873208,0.0008583582,0.99534047,0.000043225074],"about_ca_topic_score_codex":0.0059427787,"about_ca_topic_score_gemma":0.0054163625,"teacher_disagreement_score":0.008763552,"about_ca_system_score_codex":0.0013018487,"about_ca_system_score_gemma":0.0010162116,"threshold_uncertainty_score":0.012500048},"labels":[],"label_agreement":null},{"id":"W4406495409","doi":"10.1016/0967-0653(96)80573-4","title":"10.1016/0967-0653(96)80573-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Flood basalt; Geology; Mantle plume; Basalt; Mantle (geology); Geochemistry; Earth science; Flood myth; Paleontology; Archaeology; Geography; Volcanism; Tectonics","score_opus":0.008543737171029499,"score_gpt":0.16327662786974845,"score_spread":0.15473289069871896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406495409","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005303856,0.00038521242,0.00048322175,0.00038889438,0.00029379656,0.00013321411,0.000984806,0.00088078174,0.9959197],"genre_scores_gemma":[0.00067177665,0.0002626018,0.000298274,0.00030109083,0.000086751286,0.00008122078,0.00045196823,0.00017312862,0.99767333],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99926895,0.00004848868,0.00007462539,0.0002797584,0.00015770197,0.00017046397],"domain_scores_gemma":[0.9973416,0.00068725063,0.0001719656,0.00032727397,0.00061207643,0.00085999124],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001383209,0.004051668,0.0026461214,0.003283323,0.003455799,0.004717816,0.0042657224,0.00704422,0.99164385],"category_scores_gemma":[0.0018840356,0.0016588523,0.0018436366,0.00325755,0.0032467858,0.007456944,0.0041952417,0.0036196213,0.99522084],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052809407,0.00031666053,0.0013617128,0.0008286104,0.000061227125,0.0003792322,0.0001694139,0.00063220074,0.0027047894,0.005563192,0.44126296,0.5461919],"study_design_scores_gemma":[0.00011199738,0.00021277765,0.0012886764,0.0006329518,0.000025077275,0.000496439,0.00024440113,0.00024267967,0.0004128065,0.0008432559,0.9954418,0.00004708667],"about_ca_topic_score_codex":0.006458299,"about_ca_topic_score_gemma":0.005578791,"teacher_disagreement_score":0.008356154,"about_ca_system_score_codex":0.0014282198,"about_ca_system_score_gemma":0.0010353861,"threshold_uncertainty_score":0.012841463},"labels":[],"label_agreement":null},{"id":"W4406495533","doi":"10.1016/0967-0653(94)93044-9","title":"10.1016/0967-0653(94)93044-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Microearthquake; Geology; Fault plane; Seismology; Induced seismicity; Arc (geometry); Fault (geology); Geodesy; Geometry","score_opus":0.00862824524502648,"score_gpt":0.16368436168910847,"score_spread":0.155056116444082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406495533","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005899657,0.00039832812,0.00047357476,0.0004423039,0.00031118392,0.00014259231,0.0010480746,0.0009367633,0.9956572],"genre_scores_gemma":[0.00075975555,0.00028561588,0.0003415908,0.0003690303,0.00009507497,0.00008716901,0.00051087094,0.00018772602,0.99736315],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992632,0.000050367238,0.000075772245,0.000267121,0.00015824342,0.00018530707],"domain_scores_gemma":[0.99730647,0.0006808848,0.00016107554,0.0003363781,0.0006234404,0.0008916861],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013783042,0.0037945078,0.0025542148,0.0031863207,0.0035506326,0.004447706,0.0042062486,0.007447579,0.9920556],"category_scores_gemma":[0.0019819236,0.0016694338,0.0017764347,0.0030722502,0.0031462093,0.0072332155,0.0040306915,0.0035310222,0.9950675],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005359466,0.00036086858,0.0015387584,0.0008145813,0.00006367905,0.00040127226,0.00016948333,0.0005974895,0.002619239,0.0050646076,0.43578514,0.552049],"study_design_scores_gemma":[0.00011924041,0.00021745228,0.0015663158,0.00063699984,0.000027175742,0.0005487099,0.00024339753,0.00023136308,0.00042734185,0.00081713067,0.9951174,0.0000473661],"about_ca_topic_score_codex":0.0066762827,"about_ca_topic_score_gemma":0.0057221293,"teacher_disagreement_score":0.007944405,"about_ca_system_score_codex":0.0013671325,"about_ca_system_score_gemma":0.0010427668,"threshold_uncertainty_score":0.013274848},"labels":[],"label_agreement":null},{"id":"W4406498023","doi":"10.1016/0967-0653(96)86302-2","title":"10.1016/0967-0653(96)86302-2","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Archaeology; Geography","score_opus":0.008634440688697774,"score_gpt":0.16322117471612213,"score_spread":0.15458673402742434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406498023","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005119962,0.00034676728,0.00049443095,0.00036023383,0.00026987313,0.00012449893,0.0009052594,0.0008054496,0.9961816],"genre_scores_gemma":[0.0006799728,0.00023977776,0.0003249361,0.00028465575,0.000080322156,0.00007196304,0.0004316321,0.00016118641,0.99772555],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993388,0.000046116296,0.00006686132,0.00024506915,0.00015235275,0.00015081276],"domain_scores_gemma":[0.9977113,0.0005720413,0.00013895934,0.0002848692,0.0005357495,0.00075700355],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001247085,0.0034388327,0.0021603855,0.0028886579,0.0030753054,0.0040743477,0.003601715,0.0063298726,0.99115634],"category_scores_gemma":[0.0016729175,0.0014232188,0.0016044658,0.002796481,0.0025544928,0.006415646,0.0036447938,0.0031786268,0.9946621],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004857674,0.00031698812,0.0013719456,0.00076220324,0.000053052678,0.00036552167,0.00014847706,0.0005667485,0.0027382644,0.005275926,0.4214872,0.56642795],"study_design_scores_gemma":[0.00009379761,0.00018820762,0.0013046226,0.0005290692,0.000020453652,0.00046308938,0.00020029095,0.0002190404,0.00039144105,0.0006869992,0.99586487,0.00003809293],"about_ca_topic_score_codex":0.005577164,"about_ca_topic_score_gemma":0.005289017,"teacher_disagreement_score":0.00884366,"about_ca_system_score_codex":0.001242254,"about_ca_system_score_gemma":0.0008974732,"threshold_uncertainty_score":0.01261431},"labels":[],"label_agreement":null},{"id":"W4406498024","doi":"10.1016/0967-0653(96)86376-9","title":"10.1016/0967-0653(96)86376-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Magnitude (astronomy); Scale (ratio); Richter magnitude scale; Geology; Geography; Cartography; Mathematics; Geometry; Physics","score_opus":0.008535813829888998,"score_gpt":0.1629535887325498,"score_spread":0.15441777490266081,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406498024","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00055559515,0.00039883237,0.0004876503,0.00037931302,0.00029942268,0.00014038157,0.00095971365,0.00089520524,0.99588376],"genre_scores_gemma":[0.0007377759,0.00029127247,0.00033928675,0.00032630368,0.0000927972,0.000084563835,0.00048321535,0.00018473012,0.99746007],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99924076,0.000053147975,0.00008212195,0.00028099061,0.00016306624,0.0001799937],"domain_scores_gemma":[0.9973252,0.0006788287,0.00016214742,0.00034713562,0.00060212216,0.00088444725],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0014017111,0.0038655882,0.0025426247,0.003213512,0.0033741584,0.004377153,0.004060886,0.006979305,0.9913947],"category_scores_gemma":[0.0018533742,0.0015983818,0.0018054774,0.003110086,0.003022998,0.007274059,0.004222738,0.0035209232,0.99495465],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005434903,0.00034137373,0.0014515816,0.0008562093,0.000061222185,0.00040264643,0.00016689628,0.00063508766,0.0028835416,0.0052922056,0.42107305,0.5662927],"study_design_scores_gemma":[0.000110789384,0.00022021106,0.0014389346,0.00064656785,0.00002545472,0.00052970013,0.00024357016,0.00023869674,0.00042868,0.00079099834,0.99528015,0.00004633083],"about_ca_topic_score_codex":0.0059160446,"about_ca_topic_score_gemma":0.0053121196,"teacher_disagreement_score":0.008605301,"about_ca_system_score_codex":0.0012826445,"about_ca_system_score_gemma":0.0009598712,"threshold_uncertainty_score":0.012274444},"labels":[],"label_agreement":null},{"id":"W4406504007","doi":"10.1016/s0967-0653(97)85136-8","title":"10.1016/s0967-0653(97)85136-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Geography","score_opus":0.009978933109603327,"score_gpt":0.16644830506846453,"score_spread":0.1564693719588612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406504007","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00051105354,0.00044706816,0.0005774577,0.00039356767,0.0003381656,0.00014439912,0.0010522583,0.0010039923,0.99553216],"genre_scores_gemma":[0.0005423788,0.00022167886,0.00030339955,0.0002598249,0.00008064759,0.00008315479,0.00043700828,0.00017531207,0.9978967],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991301,0.00005653138,0.000082635255,0.0003423505,0.00019324615,0.00019524737],"domain_scores_gemma":[0.99722433,0.00065742206,0.00019931942,0.0003652707,0.0006631785,0.0008904379],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0014442641,0.004227633,0.0028284017,0.0035438857,0.0031316588,0.0048272423,0.0047325604,0.008002854,0.991703],"category_scores_gemma":[0.0018807496,0.001504847,0.0020961543,0.0034039582,0.0027979545,0.0076115155,0.0043254993,0.003669645,0.99495244],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004992648,0.00028891617,0.0011123006,0.0008595209,0.000057607052,0.0003189002,0.00015468462,0.00056143216,0.0024914066,0.006600891,0.40156096,0.5854941],"study_design_scores_gemma":[0.00009162585,0.0001791133,0.0008800474,0.0005405425,0.000022765471,0.0004348705,0.00016134218,0.0002011986,0.0003375013,0.00062925194,0.99648345,0.00003839075],"about_ca_topic_score_codex":0.0054239947,"about_ca_topic_score_gemma":0.004482827,"teacher_disagreement_score":0.008297026,"about_ca_system_score_codex":0.0015077126,"about_ca_system_score_gemma":0.0012897686,"threshold_uncertainty_score":0.011834681},"labels":[],"label_agreement":null},{"id":"W4406504344","doi":"10.1016/s0967-0653(97)87115-3","title":"10.1016/s0967-0653(97)87115-3","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Traverse; Geology; Front (military); Seismology; Geodesy; Oceanography","score_opus":0.009983344110739045,"score_gpt":0.16653756650515544,"score_spread":0.1565542223944164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406504344","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005030016,0.00043392126,0.00059682556,0.00039744092,0.00033226618,0.00014328198,0.001009867,0.0009703885,0.995613],"genre_scores_gemma":[0.0005506703,0.00022710506,0.0003150177,0.00026264298,0.000083989464,0.00008353741,0.00042794913,0.00017835134,0.9978707],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99910516,0.000057969522,0.00008341197,0.00036007402,0.00020129728,0.000192062],"domain_scores_gemma":[0.99707365,0.00071662705,0.00021035499,0.00037834048,0.0007139091,0.0009070694],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0015002984,0.004167501,0.0029017944,0.0037054762,0.0031661987,0.005074184,0.004752813,0.00801102,0.99153477],"category_scores_gemma":[0.0019828575,0.0015356768,0.0021059918,0.0036234737,0.0029424757,0.0077298307,0.0043221326,0.003702175,0.99500245],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004952212,0.00029388448,0.0011398774,0.0008168742,0.00005882223,0.0003384261,0.00015717179,0.00058783207,0.0023990169,0.006649262,0.4019475,0.58511615],"study_design_scores_gemma":[0.000095347874,0.00018332186,0.0008868553,0.00055580854,0.000023513852,0.0004562835,0.0001646931,0.00022020475,0.000325702,0.00065015716,0.99639785,0.000040169052],"about_ca_topic_score_codex":0.005475773,"about_ca_topic_score_gemma":0.0046052528,"teacher_disagreement_score":0.00846523,"about_ca_system_score_codex":0.0015550841,"about_ca_system_score_gemma":0.0012893,"threshold_uncertainty_score":0.012074649},"labels":[],"label_agreement":null},{"id":"W4406504396","doi":"10.1016/s0967-0653(97)87110-4","title":"10.1016/s0967-0653(97)87110-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Plume; Mantle plume; Mantle (geology); Seismology; Geophysics; Geography; Tectonics; Meteorology; Lithosphere","score_opus":0.009972058432328184,"score_gpt":0.1667974028904909,"score_spread":0.1568253444581627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406504396","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004907486,0.0004159777,0.0005856206,0.00037700727,0.00030592375,0.0001331731,0.000994369,0.00097587844,0.99572134],"genre_scores_gemma":[0.0005365166,0.00020879955,0.00029767843,0.0002386577,0.00007480505,0.00007644088,0.00041809524,0.00016914007,0.99797994],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99919623,0.000053475662,0.00007462451,0.00031626844,0.00018499537,0.00017452432],"domain_scores_gemma":[0.9972861,0.00066055235,0.00019595733,0.0003548322,0.00066901284,0.0008336232],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013933444,0.00397803,0.0026446043,0.0035041394,0.0030399617,0.004806125,0.0045371437,0.007504474,0.99127555],"category_scores_gemma":[0.0018526097,0.0014809516,0.0019425628,0.0034501608,0.00279965,0.007239944,0.0041202353,0.0034674578,0.9949443],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044285474,0.00027075078,0.0010489767,0.00075876055,0.000052625794,0.00030329663,0.0001427217,0.0005387653,0.0023193883,0.006529426,0.40265805,0.5849345],"study_design_scores_gemma":[0.00008358567,0.00016343755,0.0008477189,0.00050314766,0.00002070337,0.0004078929,0.00015322381,0.00020544245,0.00033172622,0.0006203251,0.9966264,0.00003642058],"about_ca_topic_score_codex":0.0055023395,"about_ca_topic_score_gemma":0.0045524146,"teacher_disagreement_score":0.008724451,"about_ca_system_score_codex":0.0015288272,"about_ca_system_score_gemma":0.0012690036,"threshold_uncertainty_score":0.012444258},"labels":[],"label_agreement":null},{"id":"W4406504498","doi":"10.1016/s0967-0653(97)87114-1","title":"10.1016/s0967-0653(97)87114-1","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Structural basin; Seismology; Paleontology","score_opus":0.009965454162614648,"score_gpt":0.16643437795930133,"score_spread":0.15646892379668667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406504498","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00047681306,0.00039254504,0.00054286903,0.00039761735,0.00030577212,0.0001358833,0.00092169555,0.0009144152,0.9959124],"genre_scores_gemma":[0.00051545113,0.0002083622,0.00029463865,0.00024575007,0.00007532847,0.000078509605,0.00039451834,0.00016066687,0.9980269],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99918014,0.00005338736,0.000073725096,0.00032774505,0.00018645202,0.00017860992],"domain_scores_gemma":[0.99738854,0.000626993,0.00018277686,0.00032886377,0.00062120997,0.0008516486],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013480162,0.0038607533,0.0027021475,0.003526145,0.003084661,0.0046157483,0.0043747537,0.007660468,0.99130964],"category_scores_gemma":[0.0019716385,0.0013827743,0.0018585233,0.0032181647,0.002620227,0.007292936,0.004021506,0.0033886335,0.9945651],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004402625,0.00027889418,0.0010487703,0.0007182504,0.000048461265,0.0003063591,0.00014775319,0.00052539527,0.0021414815,0.0063057085,0.4070666,0.5809721],"study_design_scores_gemma":[0.00008292339,0.00016369145,0.00084693165,0.0004889348,0.000020532907,0.00040119578,0.00015477273,0.00019933895,0.00029138275,0.00060332305,0.99671257,0.000034323115],"about_ca_topic_score_codex":0.0056967763,"about_ca_topic_score_gemma":0.004859347,"teacher_disagreement_score":0.008690357,"about_ca_system_score_codex":0.0014879182,"about_ca_system_score_gemma":0.0012879556,"threshold_uncertainty_score":0.01239568},"labels":[],"label_agreement":null},{"id":"W4406504651","doi":"10.1016/s0967-0653(97)89350-7","title":"10.1016/s0967-0653(97)89350-7","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Trough (economics); Geology; Hydrothermal circulation; JADE (particle detector); Flow (mathematics); Heat flow; Petrology; Seismology; Meteorology; Mechanics; Geography; Thermal","score_opus":0.009977570270841025,"score_gpt":0.16657230089225517,"score_spread":0.15659473062141413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406504651","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00047916424,0.00038903614,0.0005448939,0.00037945993,0.00029168517,0.00012411407,0.00096522504,0.0009360686,0.99589044],"genre_scores_gemma":[0.00054087845,0.00018176451,0.00027671066,0.00022769545,0.00006630727,0.000068975954,0.0004124056,0.00016870198,0.9980566],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992447,0.000050015784,0.00007141019,0.0002904241,0.00017706922,0.00016654337],"domain_scores_gemma":[0.9974412,0.0005968328,0.00018987966,0.00033480054,0.0006329316,0.00080436264],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013137151,0.0035924774,0.0024429534,0.0033505699,0.0028142584,0.0045679566,0.004203679,0.007301727,0.99128234],"category_scores_gemma":[0.0018526124,0.0013371349,0.0017574012,0.003149314,0.0025171116,0.0066774692,0.003956093,0.0031351754,0.99495244],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041770513,0.00025157578,0.0010092836,0.0006715725,0.000046938614,0.00029307956,0.00013797315,0.00047811682,0.0022077346,0.006064269,0.40445158,0.5839701],"study_design_scores_gemma":[0.0000754296,0.00015023918,0.0008319513,0.0004472974,0.000017685481,0.00037374612,0.00014392867,0.00018032518,0.00029794459,0.0006080948,0.9968405,0.00003294477],"about_ca_topic_score_codex":0.005188689,"about_ca_topic_score_gemma":0.0043843803,"teacher_disagreement_score":0.008717656,"about_ca_system_score_codex":0.0014032953,"about_ca_system_score_gemma":0.0012137885,"threshold_uncertainty_score":0.012434602},"labels":[],"label_agreement":null},{"id":"W4406513727","doi":"10.1016/s0967-0653(97)88842-4","title":"10.1016/s0967-0653(97)88842-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Accretion (finance); Earth science; Geology; Ecosystem; Astrobiology; Ecology; Biology; Astrophysics; Physics","score_opus":0.009969348529751173,"score_gpt":0.16635527385083254,"score_spread":0.15638592532108136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406513727","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00045538627,0.0003915753,0.0005368333,0.0003816573,0.0002900698,0.00012499589,0.0009983719,0.00091020117,0.995911],"genre_scores_gemma":[0.00052309886,0.00018863696,0.00027939313,0.00022367059,0.00006790801,0.00007035021,0.0004130766,0.00016095047,0.99807286],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992685,0.000047324964,0.00006675201,0.00028562715,0.00017538373,0.00015653076],"domain_scores_gemma":[0.9975134,0.0005707948,0.00018836102,0.00032098236,0.0006192156,0.00078725064],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012860541,0.0035851572,0.0023769068,0.0033063828,0.0027219185,0.0046390067,0.0041975295,0.0069404687,0.9912412],"category_scores_gemma":[0.0018079,0.0013344161,0.0017206464,0.003282242,0.0024732524,0.006726512,0.0038398507,0.0032347776,0.99480456],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004048675,0.00024951214,0.0010188872,0.0006960128,0.00004881355,0.00029035358,0.00013802262,0.00048405028,0.0021231137,0.0059013725,0.415982,0.572663],"study_design_scores_gemma":[0.00007414953,0.00014001476,0.00080671883,0.00043702754,0.000018039143,0.00036148046,0.00014084615,0.00017144858,0.0002863635,0.00055682333,0.9969752,0.00003194989],"about_ca_topic_score_codex":0.0053537227,"about_ca_topic_score_gemma":0.004419163,"teacher_disagreement_score":0.008758783,"about_ca_system_score_codex":0.001398071,"about_ca_system_score_gemma":0.0012203808,"threshold_uncertainty_score":0.012493253},"labels":[],"label_agreement":null},{"id":"W4406514707","doi":"10.1016/s0967-0653(97)84654-6","title":"10.1016/s0967-0653(97)84654-6","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Lithosphere; Trough (economics); Geology; Seismology; Tectonics; Economics","score_opus":0.009973679331612464,"score_gpt":0.16641174560169378,"score_spread":0.1564380662700813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406514707","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00047642874,0.00039959882,0.0005267624,0.00038505535,0.00029861115,0.000123177,0.0009782043,0.0008932422,0.99591905],"genre_scores_gemma":[0.0005356163,0.00019144526,0.00027316328,0.00022714617,0.00007045457,0.00006841558,0.00041051346,0.00016433236,0.998059],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992454,0.000048387068,0.00007125582,0.00028751392,0.0001791694,0.00016838922],"domain_scores_gemma":[0.99731404,0.00061583106,0.00020689491,0.00034399994,0.00065466843,0.00086453126],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013298374,0.0037242323,0.0024963443,0.0033168509,0.0028403061,0.004662347,0.004264643,0.0073140874,0.991499],"category_scores_gemma":[0.001877781,0.0013729726,0.0017953448,0.0032127178,0.0025314859,0.0070589744,0.004010836,0.003365827,0.9950622],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043714445,0.0002644458,0.0010847376,0.00071008253,0.000049852548,0.00029670025,0.00014486277,0.0004895602,0.0022233673,0.006011817,0.39695868,0.5913288],"study_design_scores_gemma":[0.0000788964,0.0001559468,0.00088071555,0.00046940305,0.000019390363,0.00038764384,0.0001542489,0.00018025616,0.00030848387,0.0006072951,0.99672323,0.000034552028],"about_ca_topic_score_codex":0.005283283,"about_ca_topic_score_gemma":0.0044045853,"teacher_disagreement_score":0.008500993,"about_ca_system_score_codex":0.0013710649,"about_ca_system_score_gemma":0.0012248317,"threshold_uncertainty_score":0.012125611},"labels":[],"label_agreement":null},{"id":"W4406514878","doi":"10.1016/s0967-0653(98)82151-0","title":"10.1016/s0967-0653(98)82151-0","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Ridge; Geology; Seismology; Paleontology","score_opus":0.008737908028932309,"score_gpt":0.16638322887590953,"score_spread":0.15764532084697722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406514878","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004076253,0.00027167168,0.00045344664,0.00033114554,0.00024656122,0.00010862158,0.00073093333,0.00078569655,0.9966642],"genre_scores_gemma":[0.00048215763,0.00014905448,0.00025688048,0.00020509538,0.000060308746,0.000059797658,0.00032227038,0.00014001851,0.99832445],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993679,0.000043180957,0.000055168224,0.00024359452,0.00015705971,0.00013316816],"domain_scores_gemma":[0.99772173,0.00050112186,0.00014934428,0.0002958825,0.0005569051,0.0007749531],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011250114,0.003018764,0.0019382725,0.0030157305,0.002598993,0.0040810346,0.0035719192,0.006469166,0.99114394],"category_scores_gemma":[0.0017520706,0.0011530909,0.0015755084,0.0026238032,0.0021956759,0.0059460304,0.003532449,0.00286299,0.9941584],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003586773,0.00025222747,0.0010383077,0.00058118993,0.000040176597,0.0002648995,0.00013701721,0.0004227985,0.0020528147,0.006057901,0.4211259,0.5676681],"study_design_scores_gemma":[0.00005972528,0.00012307924,0.0008072131,0.00036106256,0.000014459598,0.00031658434,0.00013194857,0.00015255748,0.00023350277,0.0004911313,0.99728346,0.000025266734],"about_ca_topic_score_codex":0.005539566,"about_ca_topic_score_gemma":0.00464788,"teacher_disagreement_score":0.008856058,"about_ca_system_score_codex":0.0011937505,"about_ca_system_score_gemma":0.0011108059,"threshold_uncertainty_score":0.012632012},"labels":[],"label_agreement":null},{"id":"W4406515110","doi":"10.1016/s0967-0653(98)81145-9","title":"10.1016/s0967-0653(98)81145-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology","score_opus":0.008755865159269594,"score_gpt":0.1666529752318032,"score_spread":0.1578971100725336,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406515110","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005384213,0.00043725315,0.0005535332,0.00042108056,0.00032858463,0.00015070078,0.0009609842,0.0010030764,0.99560624],"genre_scores_gemma":[0.000571612,0.00023099179,0.00032521455,0.0002883985,0.000084345345,0.00009085659,0.00040395634,0.00017611936,0.99782854],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99911815,0.000058789923,0.00008601065,0.0003530483,0.00018846191,0.00019559261],"domain_scores_gemma":[0.9971187,0.0007011087,0.0002105102,0.00036610593,0.00066550146,0.0009380762],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0015075003,0.0041777263,0.002842715,0.003585464,0.003404361,0.0048936745,0.004685521,0.008285672,0.9915815],"category_scores_gemma":[0.0020923296,0.0015513742,0.002034152,0.0033347923,0.0030837713,0.008114862,0.00448167,0.003794863,0.994899],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005107568,0.00030939994,0.001175428,0.00085923483,0.000055497432,0.00035922884,0.00017738102,0.0005661618,0.0023245474,0.0066624046,0.42147028,0.5655297],"study_design_scores_gemma":[0.00009854855,0.00019581887,0.000953278,0.0005825718,0.000022904409,0.00047315666,0.00018625708,0.0002165133,0.00030504283,0.0006686283,0.9962573,0.00003997183],"about_ca_topic_score_codex":0.005698219,"about_ca_topic_score_gemma":0.004669464,"teacher_disagreement_score":0.0084185,"about_ca_system_score_codex":0.0014648939,"about_ca_system_score_gemma":0.001271261,"threshold_uncertainty_score":0.012007952},"labels":[],"label_agreement":null},{"id":"W4406516885","doi":"10.1016/s0967-0653(97)80991-x","title":"10.1016/s0967-0653(97)80991-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Trough (economics)","score_opus":0.009991860314094212,"score_gpt":0.16672325785984948,"score_spread":0.15673139754575527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406516885","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00046483436,0.000365942,0.00049833435,0.00037444252,0.0002790694,0.000117806274,0.00088533864,0.0008409324,0.9961733],"genre_scores_gemma":[0.00053356634,0.00018035501,0.00026610628,0.00021175576,0.00006194025,0.00006729208,0.00039790955,0.00015767569,0.99812335],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99934846,0.000041894655,0.00005809645,0.00025162817,0.00015759663,0.0001422197],"domain_scores_gemma":[0.9977513,0.0005103188,0.00017192423,0.00029955537,0.0005085302,0.0007584911],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001172923,0.0034774654,0.002203548,0.0031208908,0.002661648,0.004229444,0.003903034,0.006582228,0.9907889],"category_scores_gemma":[0.0017121172,0.0012676639,0.0015576304,0.0028662318,0.0024505963,0.0065844767,0.0035724114,0.0031571607,0.99427325],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039396575,0.00025770644,0.00097607466,0.0006836938,0.000042671403,0.00028656822,0.00014718286,0.00045757342,0.0020910525,0.0066630375,0.40507618,0.5829243],"study_design_scores_gemma":[0.00006489809,0.00013019644,0.0008388964,0.00038814728,0.000016248694,0.00036318135,0.00014451495,0.00016427605,0.00029332077,0.00060063356,0.99696654,0.000029023502],"about_ca_topic_score_codex":0.005358595,"about_ca_topic_score_gemma":0.00441591,"teacher_disagreement_score":0.009211123,"about_ca_system_score_codex":0.0013167973,"about_ca_system_score_gemma":0.0011608984,"threshold_uncertainty_score":0.013138533},"labels":[],"label_agreement":null},{"id":"W4406527578","doi":"10.1016/0967-0653(96)85045-9","title":"10.1016/0967-0653(96)85045-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Oceanography; Seismology","score_opus":0.008547877083897249,"score_gpt":0.16329129176925447,"score_spread":0.1547434146853572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406527578","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00062863674,0.0003982431,0.0005037144,0.0003987782,0.00032320357,0.00014270321,0.00094895205,0.000878643,0.995777],"genre_scores_gemma":[0.00079337234,0.0002837056,0.0003380092,0.00034753108,0.00009434382,0.00008453853,0.00046520322,0.00017305254,0.9974203],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992556,0.000050170063,0.0000776498,0.0002824736,0.0001486599,0.00018541118],"domain_scores_gemma":[0.9975285,0.00060522027,0.00014855008,0.00031038807,0.00053503714,0.0008724472],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001363215,0.0038400001,0.0025339457,0.0031112423,0.003475166,0.004285025,0.0040057343,0.0070246463,0.9913384],"category_scores_gemma":[0.0018395678,0.0016006868,0.0017592375,0.002999375,0.0030519671,0.0074423817,0.0041292966,0.0034550647,0.9947307],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005878741,0.00038337204,0.0016228311,0.0008677009,0.00006082765,0.00044790204,0.00019007128,0.0006478059,0.0030151946,0.005681344,0.4179649,0.56853014],"study_design_scores_gemma":[0.00011199449,0.00024199371,0.0015238334,0.000656646,0.000026230382,0.00057190476,0.0002812415,0.00024558432,0.0004226608,0.0008457397,0.99502414,0.000047902256],"about_ca_topic_score_codex":0.005493136,"about_ca_topic_score_gemma":0.005299308,"teacher_disagreement_score":0.008661628,"about_ca_system_score_codex":0.0012769434,"about_ca_system_score_gemma":0.0009372829,"threshold_uncertainty_score":0.012354672},"labels":[],"label_agreement":null},{"id":"W4406527668","doi":"10.1016/0967-0653(96)85048-4","title":"10.1016/0967-0653(96)85048-4","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology","score_opus":0.008532985117405177,"score_gpt":0.16308403040436065,"score_spread":0.15455104528695546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406527668","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000587353,0.00039239184,0.00050712813,0.00039798676,0.0003204075,0.00014213633,0.0009854444,0.00086904515,0.9957982],"genre_scores_gemma":[0.0007272342,0.00026479916,0.00032227053,0.00032347112,0.00009110714,0.00008270154,0.0004566418,0.00016535081,0.99756646],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99928576,0.000047863006,0.00007285456,0.00027480762,0.00014679752,0.00017194053],"domain_scores_gemma":[0.9975617,0.00058722775,0.00015070905,0.0003024641,0.0005575956,0.0008402854],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013230004,0.0038955829,0.0024855197,0.0031810892,0.0033901024,0.0043214434,0.0040462916,0.0068339547,0.9913988],"category_scores_gemma":[0.0017993374,0.0016044863,0.0017616324,0.0030572426,0.0029873361,0.0073206816,0.0040116706,0.0033900735,0.99489486],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005507477,0.0003467508,0.0015420624,0.00085617485,0.000058586513,0.00041743048,0.00017354288,0.000633015,0.0028531896,0.0056115487,0.42601064,0.5609463],"study_design_scores_gemma":[0.000102843434,0.00022235526,0.0013859338,0.0006155789,0.00002439519,0.00053060113,0.0002514138,0.00022930464,0.00038909752,0.00080660294,0.99539655,0.00004532352],"about_ca_topic_score_codex":0.005810821,"about_ca_topic_score_gemma":0.005485491,"teacher_disagreement_score":0.008601189,"about_ca_system_score_codex":0.0013217479,"about_ca_system_score_gemma":0.00096965634,"threshold_uncertainty_score":0.012268484},"labels":[],"label_agreement":null},{"id":"W4406528673","doi":"10.1016/0967-0653(96)80999-9","title":"10.1016/0967-0653(96)80999-9","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Seismology","score_opus":0.00853424901081193,"score_gpt":0.1633546454314747,"score_spread":0.15482039642066278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406528673","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00058719807,0.00039542845,0.0004670958,0.00039136276,0.00030997183,0.00014707362,0.000955425,0.00090803765,0.9958384],"genre_scores_gemma":[0.0007361725,0.0002813256,0.00032402834,0.00032448696,0.00008382191,0.00009374672,0.0004667163,0.00017948094,0.9975102],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991897,0.000057016754,0.000086932785,0.0003049776,0.00016319683,0.00019815429],"domain_scores_gemma":[0.99745923,0.0006814358,0.00015692742,0.00032427456,0.0005371262,0.000841008],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0015099259,0.004366387,0.0028017755,0.0034063577,0.003866859,0.0047242194,0.0044866037,0.007826961,0.99149525],"category_scores_gemma":[0.002017362,0.0017729054,0.0018589187,0.0033828297,0.003563987,0.008060333,0.0046189,0.0037503345,0.9951487],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006054239,0.00037265112,0.0015351765,0.000956383,0.000060927592,0.00046474184,0.00020260178,0.0007032161,0.002737235,0.0061268224,0.42673704,0.55949783],"study_design_scores_gemma":[0.00012657081,0.0002511931,0.0013915675,0.0007730374,0.000025598443,0.00056856923,0.00030231843,0.00027420188,0.00041486684,0.00094503706,0.9948748,0.000052320815],"about_ca_topic_score_codex":0.0061101513,"about_ca_topic_score_gemma":0.005637312,"teacher_disagreement_score":0.008504748,"about_ca_system_score_codex":0.0014192017,"about_ca_system_score_gemma":0.0010287449,"threshold_uncertainty_score":0.012149215},"labels":[],"label_agreement":null},{"id":"W4406529395","doi":"10.1016/0967-0653(96)82047-3","title":"10.1016/0967-0653(96)82047-3","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Geology; Tectonics; Seismology; Plate tectonics; Paleontology; Oceanography; Geography","score_opus":0.008549971722270202,"score_gpt":0.1632947683681996,"score_spread":0.15474479664592938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406529395","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00050653995,0.00037316338,0.00046472915,0.00035907055,0.00029849395,0.00012257227,0.0009432461,0.00084272015,0.99608946],"genre_scores_gemma":[0.00066826976,0.00025522584,0.0002936363,0.0002927122,0.000088066765,0.00007142626,0.00045632548,0.00016952892,0.9977048],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993,0.0000489057,0.00007187321,0.00026248768,0.00015374259,0.0001629217],"domain_scores_gemma":[0.9974063,0.00065257685,0.00015638515,0.0003225481,0.0006340794,0.00082814187],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012985324,0.0036715167,0.002434366,0.0030989628,0.003199971,0.0044989605,0.0040171617,0.006545333,0.99149734],"category_scores_gemma":[0.0017812754,0.0015025488,0.0017736421,0.003014101,0.0028871517,0.0068599824,0.003768243,0.0034578769,0.9951165],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050725345,0.0003104138,0.0014316831,0.00082327425,0.000060116,0.0003711381,0.00016100325,0.0006025335,0.0027899046,0.0054951496,0.43764594,0.5498015],"study_design_scores_gemma":[0.00009899252,0.00019872951,0.0012295259,0.0005856363,0.000023375149,0.00048534264,0.00021840222,0.0002217301,0.000398968,0.00075737044,0.99573994,0.000041961062],"about_ca_topic_score_codex":0.0057480414,"about_ca_topic_score_gemma":0.005032376,"teacher_disagreement_score":0.008502662,"about_ca_system_score_codex":0.0012805997,"about_ca_system_score_gemma":0.0009702894,"threshold_uncertainty_score":0.0121279955},"labels":[],"label_agreement":null},{"id":"W4406532637","doi":"10.1016/0967-0653(95)94900-3","title":"10.1016/0967-0653(95)94900-3","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Swamp; Peat; Flooding (psychology); Sulfur; Environmental science; Geology; Earth science; Environmental chemistry; Geography; Archaeology; Ecology; Chemistry; Biology","score_opus":0.008603875813182648,"score_gpt":0.16386873651614747,"score_spread":0.15526486070296483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406532637","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00061772316,0.0004121873,0.0005292739,0.00042184678,0.00030445834,0.00014872696,0.0009880097,0.00089051103,0.9956873],"genre_scores_gemma":[0.00081126863,0.00028086052,0.00038016672,0.0003544347,0.00008726323,0.00008851241,0.00046334122,0.00017593881,0.99735814],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992743,0.000050778963,0.00007214001,0.00027460902,0.00015905811,0.00016907911],"domain_scores_gemma":[0.9974577,0.0006765687,0.00015517673,0.00030956292,0.0005799889,0.0008210474],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0013466163,0.003563855,0.0023737813,0.0030945542,0.003315645,0.0041937483,0.004039539,0.007039136,0.991143],"category_scores_gemma":[0.0019237073,0.0014938832,0.0016337896,0.002903089,0.0028249663,0.0068698754,0.003937954,0.0032475097,0.9943064],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052121846,0.0003821196,0.0015480093,0.0008221773,0.000055380227,0.00040908507,0.00017164889,0.0005893792,0.002700071,0.00565564,0.39770436,0.5894409],"study_design_scores_gemma":[0.00010465662,0.00022404939,0.0014126422,0.00060062285,0.000024350513,0.0005329232,0.00022565831,0.00022096743,0.00038655856,0.00083844387,0.9953869,0.00004224237],"about_ca_topic_score_codex":0.0059834626,"about_ca_topic_score_gemma":0.0054439693,"teacher_disagreement_score":0.008857012,"about_ca_system_score_codex":0.001291505,"about_ca_system_score_gemma":0.0009762127,"threshold_uncertainty_score":0.012633383},"labels":[],"label_agreement":null},{"id":"W4406533675","doi":"10.1016/0967-0653(95)90793-x","title":"10.1016/0967-0653(95)90793-x","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Extensional definition; Geology; Deformation (meteorology); Seismology; Paleontology; Oceanography; Tectonics","score_opus":0.008608424283066745,"score_gpt":0.16368040413253881,"score_spread":0.15507197984947207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406533675","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00053746207,0.00035954666,0.0004346287,0.00037672388,0.00027276916,0.00012955553,0.0008683207,0.00076395064,0.99625707],"genre_scores_gemma":[0.0007440691,0.00026074372,0.00031551858,0.0003285502,0.00008541002,0.00008126094,0.0004456528,0.00017558776,0.99756324],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993106,0.000045075405,0.000066360575,0.00026163572,0.00015352972,0.0001628082],"domain_scores_gemma":[0.99754566,0.00061407866,0.0001596815,0.00029821563,0.00051465334,0.0008676],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012659102,0.0036805698,0.0023944962,0.0031911298,0.0034654615,0.004286028,0.004096181,0.0069023147,0.9909928],"category_scores_gemma":[0.0017917021,0.0014772036,0.0015835667,0.002877553,0.0030263728,0.0071534356,0.0038658916,0.0033380461,0.9942741],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004940557,0.00036645174,0.0014223477,0.00080785825,0.000055195294,0.0003946103,0.00018433417,0.0005689636,0.0025876893,0.0060560657,0.44635984,0.5407026],"study_design_scores_gemma":[0.000098358905,0.0001944897,0.0013902807,0.0005401322,0.000022293942,0.00047711754,0.00023551822,0.00019862603,0.00037682214,0.0008212018,0.99560505,0.00004002845],"about_ca_topic_score_codex":0.006903358,"about_ca_topic_score_gemma":0.0062483195,"teacher_disagreement_score":0.0090072155,"about_ca_system_score_codex":0.0013476214,"about_ca_system_score_gemma":0.0010425652,"threshold_uncertainty_score":0.013726354},"labels":[],"label_agreement":null},{"id":"W4406535234","doi":"10.1016/0967-0653(93)95402-r","title":"10.1016/0967-0653(93)95402-r","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Microearthquake; Seismometer; Hypocenter; Seismology; Geology; Oceanography; Induced seismicity","score_opus":0.0080618790293458,"score_gpt":0.15986119219143902,"score_spread":0.15179931316209322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406535234","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00052832166,0.0002936166,0.0004931819,0.0003840191,0.00025784405,0.00013568441,0.0009378878,0.00091818353,0.9960514],"genre_scores_gemma":[0.0007975492,0.00022433553,0.00036484422,0.0003445654,0.00008920728,0.00007712902,0.00046509583,0.0002070179,0.99743026],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99931014,0.000050468127,0.00006236964,0.0002675756,0.00015402489,0.00015538045],"domain_scores_gemma":[0.99763525,0.0006060824,0.00014601307,0.00031408825,0.0005177245,0.0007809031],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012328217,0.0032235642,0.002153582,0.0031310502,0.0031193825,0.0039567337,0.0036698945,0.0063967616,0.9908896],"category_scores_gemma":[0.0018670559,0.0013994217,0.0016059437,0.002679828,0.002440846,0.0061583947,0.0037457354,0.0028560804,0.99403447],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004453965,0.00033808593,0.001365346,0.0006925614,0.000051141596,0.00038336543,0.00015196385,0.0005417738,0.002556747,0.004926995,0.44405356,0.544493],"study_design_scores_gemma":[0.00009668547,0.00019648459,0.0014609189,0.00048341957,0.000022855023,0.00051401963,0.00020926369,0.00020921939,0.00038316086,0.00069217273,0.9956938,0.00003804344],"about_ca_topic_score_codex":0.00645638,"about_ca_topic_score_gemma":0.0053680674,"teacher_disagreement_score":0.009110391,"about_ca_system_score_codex":0.0011519206,"about_ca_system_score_gemma":0.00089858467,"threshold_uncertainty_score":0.012994885},"labels":[],"label_agreement":null},{"id":"W4406537842","doi":"10.1016/s0967-0653(98)81359-8","title":"10.1016/s0967-0653(98)81359-8","year":2000,"lang":"en","type":"article","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Moment tensor; Geology; Tectonics; Seismology; Tensor (intrinsic definition); Surface (topology); Moment (physics); Geophysics; Geodesy; Oceanography; Physics; Geometry; Mathematics; Classical mechanics","score_opus":0.00874205625279584,"score_gpt":0.1663747596907023,"score_spread":0.15763270343790647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406537842","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004653153,0.00036475886,0.0005134835,0.00039566643,0.00029386053,0.00012284606,0.0008898302,0.0009012294,0.996053],"genre_scores_gemma":[0.00053546374,0.00017867934,0.0002806641,0.00024176907,0.000070352835,0.00007056665,0.00036918733,0.00015552576,0.99809784],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99927825,0.00004811408,0.00006870853,0.00028172776,0.00016756142,0.00015555993],"domain_scores_gemma":[0.99750036,0.0005702941,0.0001820762,0.00032723183,0.0006179816,0.00080209697],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0012972208,0.003455009,0.0023265611,0.0032090351,0.0028604388,0.0044596912,0.0040465975,0.0071688304,0.9911876],"category_scores_gemma":[0.0018603215,0.0012878237,0.001728645,0.00294843,0.0025286842,0.006784863,0.0038484747,0.0032735579,0.9947001],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041773208,0.00025675484,0.0010688669,0.00067863934,0.00004718172,0.00029858618,0.00014650468,0.00046548768,0.0021783216,0.0062492425,0.42347547,0.5647172],"study_design_scores_gemma":[0.00007211273,0.00014571799,0.00082136644,0.0004440828,0.000017234814,0.0003726327,0.00014568852,0.00017354995,0.0002637882,0.00057852356,0.996935,0.000030376708],"about_ca_topic_score_codex":0.00512842,"about_ca_topic_score_gemma":0.004198997,"teacher_disagreement_score":0.0088124275,"about_ca_system_score_codex":0.0013036149,"about_ca_system_score_gemma":0.0011569379,"threshold_uncertainty_score":0.012569785},"labels":[],"label_agreement":null},{"id":"W4406558695","doi":"10.1093/gji/ggaf014","title":"Estimation of the landslide source for the 1929 Grand Banks event using a deep-sea landslide tsunami simulation","year":2025,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministry of Education, Culture, Sports, Science and Technology","keywords":"Landslide; Geology; Seismology; Event (particle physics)","score_opus":0.015349725710940215,"score_gpt":0.27753098606837623,"score_spread":0.262181260357436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406558695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915801,0.000025981772,0.0068870755,0.000038194703,0.000005731558,0.000013911843,0.00024675825,0.000084888605,0.0011173434],"genre_scores_gemma":[0.9972398,0.000015065575,0.0022410508,0.0000039713454,0.0000027475674,0.000009067678,0.000235501,0.000011265003,0.00024151515],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995935,0.000008965041,0.0000034147968,0.00001011686,0.000008355652,0.000009765878],"domain_scores_gemma":[0.9997298,0.00012537671,0.000028126098,0.000017360473,0.000055905562,0.00004336922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019493113,0.00039285174,0.0002775799,0.00060602283,0.00030487854,0.00034260572,0.00038084254,0.0004573887,0.0012615889],"category_scores_gemma":[0.00067035406,0.00025760307,0.00039550805,0.0003244668,0.00016189244,0.00019883436,0.00023556419,0.00036531634,0.000158084],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006056883,0.00003157171,0.021312397,0.000011993687,0.000023800192,0.00010847319,0.000027363694,0.9733849,0.0017076903,0.00029053554,0.0001391156,0.0029015427],"study_design_scores_gemma":[0.000009344714,0.000010643387,0.0040460345,0.0000018187064,0.000005192459,0.0000059651297,0.000012553181,0.9955177,0.00029185,0.000048834423,0.000046265362,0.0000038454755],"about_ca_topic_score_codex":0.081192695,"about_ca_topic_score_gemma":0.050987534,"teacher_disagreement_score":0.081192695,"about_ca_system_score_codex":0.00081663457,"about_ca_system_score_gemma":0.0006488755,"threshold_uncertainty_score":0.1614402},"labels":[],"label_agreement":null},{"id":"W4406597403","doi":"10.1002/arp.1977","title":"World Archaeo‐Geophysics: Integrated Minimally Invasive Approaches Using Country‐Based ExamplesBy CarmenCuenca‐Garcia, AndreiAsăndulesei, and Kelsey M.Lowe (eds.), Springer, 2024. 482 pp. Free (E‐book); $39.99 (paperback). ISBN: 978‐3‐031‐57900‐4. https://doi.org/10.1007/978‐3‐031‐57900‐4","year":2025,"lang":"en","type":"article","venue":"Archaeological Prospection","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Garcia; Archaeology; Geography; Humanities; Art; Cartography; History","score_opus":0.03763613248336834,"score_gpt":0.22739215841851745,"score_spread":0.18975602593514912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406597403","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.002934572,0.80281174,0.021942217,0.0108836135,0.0081797335,0.00015722934,0.0005465594,0.00044664706,0.1520977],"genre_scores_gemma":[0.0107295755,0.7354069,0.02903306,0.002619002,0.0014668702,0.00022858194,0.0009334653,0.000451211,0.21913148],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994898,0.00011635865,0.00003330296,0.00006855314,0.000258939,0.000032974855],"domain_scores_gemma":[0.9996762,0.00018682748,0.00003298236,0.00002570423,0.000042684864,0.000035539593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072069,0.0016115054,0.00077686616,0.0015711698,0.00080685096,0.0053563844,0.0009674256,0.0016862995,0.026963575],"category_scores_gemma":[0.00086901424,0.0008848466,0.00071617536,0.0036123816,0.0012089958,0.0042876233,0.002850644,0.0025673367,0.01287136],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002925932,0.00007390507,0.00028276237,0.0022782923,0.000025664358,0.000310774,0.0020148077,0.0005802165,0.0012011655,0.012917134,0.41017556,0.5701104],"study_design_scores_gemma":[0.0000018102072,0.000011330543,0.00046299802,0.0008643197,0.0000061890873,0.00052023714,0.0007382512,0.000095145006,0.00018028043,0.0032612195,0.9938484,0.00000985229],"about_ca_topic_score_codex":0.0018426813,"about_ca_topic_score_gemma":0.004781415,"teacher_disagreement_score":0.026963575,"about_ca_system_score_codex":0.00066612306,"about_ca_system_score_gemma":0.0014470408,"threshold_uncertainty_score":0.09020209},"labels":[],"label_agreement":null},{"id":"W4406601682","doi":"","title":"Front and back-front of the seismic migration driven by fluid-induced aseismic slip in natural and anthropogenic earthquake sequences","year":2024,"lang":"en","type":"article","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Front (military); Geology; Seismology; Natural (archaeology); Slip (aerodynamics); Engineering; Oceanography; Paleontology; Aerospace engineering","score_opus":0.009467492812818591,"score_gpt":0.20392994311204882,"score_spread":0.19446245029923023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406601682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971173,0.000038396087,0.00045950527,0.000037345846,0.000011221686,0.000005644368,0.00018633663,0.000020797159,0.0021235314],"genre_scores_gemma":[0.9989955,0.000024867006,0.00013292774,0.0000046501586,0.0000037639713,0.00000139253,0.0001271945,0.000006690605,0.00070300366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999651,0.0000050612457,0.0000024721105,0.000008149501,0.0000063189777,0.000012870986],"domain_scores_gemma":[0.9996716,0.00007785731,0.000049712147,0.000012028287,0.000086789856,0.0001021118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011536104,0.0001524203,0.00014290828,0.0005416212,0.00028792486,0.00045135364,0.00015532605,0.000283422,0.0049094995],"category_scores_gemma":[0.00078305247,0.0001649078,0.000192176,0.00022713994,0.00023048605,0.0001878712,0.00035079673,0.0003336679,0.00041120566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0056742528,0.0007601948,0.4966562,0.00036588276,0.00024370247,0.002143182,0.0020712477,0.1186921,0.28067687,0.010125912,0.004295885,0.07829452],"study_design_scores_gemma":[0.000039984647,0.00018789058,0.90825397,0.000033655135,0.00003539944,0.00014667358,0.00042116735,0.08572347,0.003885485,0.00055930414,0.0006891116,0.000023887698],"about_ca_topic_score_codex":0.0050353296,"about_ca_topic_score_gemma":0.009015294,"teacher_disagreement_score":0.0050353296,"about_ca_system_score_codex":0.0002861892,"about_ca_system_score_gemma":0.00026356807,"threshold_uncertainty_score":0.016423881},"labels":[],"label_agreement":null},{"id":"W4406601772","doi":"","title":"Seismic migration driven by fluid-induced aseismic slip in natural swarms and anthropogenic induced sequences","year":2024,"lang":"en","type":"article","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Seismology; Slip (aerodynamics); Natural (archaeology); Engineering; Aerospace engineering; Paleontology","score_opus":0.012845895144949574,"score_gpt":0.22118850846012758,"score_spread":0.208342613315178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406601772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993637,0.000006915569,0.00023389769,0.0000109833,0.0000026263237,0.0000012129245,0.00002279581,0.0000059824897,0.00035176927],"genre_scores_gemma":[0.9997987,0.0000058581522,0.000046465295,0.000001248976,0.0000014889837,7.627196e-7,0.000023288714,0.0000015282487,0.00012068985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999659,0.000006833466,0.0000023945051,0.000010270053,0.0000038618914,0.000010774723],"domain_scores_gemma":[0.9997297,0.000059928618,0.00006741594,0.000013968206,0.000049944516,0.00007899556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000108561195,0.00012861738,0.00017498243,0.0003195379,0.0002160489,0.00041579234,0.00015497454,0.00022329688,0.0018396588],"category_scores_gemma":[0.00072795333,0.00010422466,0.00016421254,0.00020916351,0.00034206608,0.00016427535,0.0002445602,0.00017341346,0.00015956999],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021305783,0.0004265143,0.66349673,0.00014150963,0.00021310273,0.0018985871,0.001252638,0.16037796,0.13814533,0.005805636,0.0016751776,0.02443634],"study_design_scores_gemma":[0.00004180208,0.00024215589,0.7305565,0.000009467324,0.000033321165,0.00021406448,0.00067313045,0.2645222,0.0020157548,0.0012395035,0.00042822596,0.000024035837],"about_ca_topic_score_codex":0.00317452,"about_ca_topic_score_gemma":0.0045628333,"teacher_disagreement_score":0.00317452,"about_ca_system_score_codex":0.00034763486,"about_ca_system_score_gemma":0.00021708816,"threshold_uncertainty_score":0.0063120723},"labels":[],"label_agreement":null},{"id":"W4406655990","doi":"10.1016/b978-044482403-5/50070-0","title":"10.1016/b978-044482403-5/50070-0","year":2000,"lang":"en","type":"book-chapter","venue":"Time to knit","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Tectonics; Structural basin; Geology; Paleontology","score_opus":0.011476253500024703,"score_gpt":0.16315654051005285,"score_spread":0.15168028701002814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406655990","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00019413554,0.00029773737,0.0007157459,0.00023561076,0.00012807931,0.00003731944,0.0007550402,0.00080960046,0.9968267],"genre_scores_gemma":[0.00035352696,0.00014130097,0.00019363902,0.00006934827,0.000023823039,0.000018779176,0.00033906396,0.00017461942,0.9986858],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996433,0.000021415954,0.00002288135,0.00011618733,0.00013087185,0.000065344415],"domain_scores_gemma":[0.9985428,0.00039212516,0.000101907346,0.0002191574,0.00029314225,0.00045086694],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0007008514,0.0019352556,0.0011052692,0.001757674,0.001211887,0.004535923,0.0023427357,0.0035315997,0.9779661],"category_scores_gemma":[0.0015290901,0.0008088733,0.0006786227,0.0020135352,0.0009203355,0.0043648286,0.0027727925,0.0017992791,0.9886014],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096266456,0.00009159697,0.00035258307,0.0002744087,0.0000103451,0.00010164498,0.00006852378,0.00029900973,0.0015433247,0.0050081913,0.43395606,0.55819803],"study_design_scores_gemma":[0.000013914468,0.000032470674,0.0005485207,0.00017367485,0.0000055658425,0.00013096431,0.00006652924,0.00012796043,0.00024687094,0.0008066394,0.9978371,0.000009827187],"about_ca_topic_score_codex":0.004197619,"about_ca_topic_score_gemma":0.0051527624,"teacher_disagreement_score":0.02203387,"about_ca_system_score_codex":0.0008531014,"about_ca_system_score_gemma":0.0008135375,"threshold_uncertainty_score":0.031428635},"labels":[],"label_agreement":null},{"id":"W4406691490","doi":"10.1017/9781108686631.001","title":"Introduction","year":2025,"lang":"en","type":"book-chapter","venue":"Cambridge University Press eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC","funders":"","keywords":"Computer science","score_opus":0.014610666312212365,"score_gpt":0.17248020838621103,"score_spread":0.15786954207399867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406691490","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00042043763,0.005181821,0.0017999429,0.0023624832,0.0027840943,0.00006882798,0.0009092025,0.0003386682,0.9861347],"genre_scores_gemma":[0.0017895258,0.0032011052,0.00092848233,0.0011189294,0.00063709373,0.000037336173,0.00081951247,0.00016538709,0.9913026],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995265,0.00004136366,0.000018409952,0.00011595946,0.0002449002,0.00005291522],"domain_scores_gemma":[0.9995994,0.00007908529,0.000019143587,0.00005143759,0.00017003561,0.00008081425],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00031648276,0.00086679374,0.0005658592,0.00129486,0.0017201762,0.0049200286,0.0013525847,0.0019994883,0.4345066],"category_scores_gemma":[0.0012846788,0.00032357126,0.00045270298,0.0014501247,0.0008941167,0.003798434,0.0022488742,0.0022254633,0.25963682],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002009969,0.000041497064,0.00011812207,0.00023077628,0.0000020953605,0.00011559569,0.0005246516,0.00017057075,0.00038927214,0.05881311,0.8127259,0.1268484],"study_design_scores_gemma":[7.2058384e-7,0.0000037738255,0.000053826756,0.00007693969,4.3651636e-7,0.000057994544,0.000051782114,0.000013539577,0.000025380776,0.0024324255,0.9972817,0.0000014724492],"about_ca_topic_score_codex":0.002411698,"about_ca_topic_score_gemma":0.003839659,"teacher_disagreement_score":0.4345066,"about_ca_system_score_codex":0.0014818693,"about_ca_system_score_gemma":0.0013038551,"threshold_uncertainty_score":0.8066077},"labels":[],"label_agreement":null},{"id":"W4406691525","doi":"10.1017/9781108686631.006","title":"Role of Lithospheric Composition and Compositional Variations in Evolving Structural Styles","year":2025,"lang":"en","type":"book-chapter","venue":"Cambridge University Press eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC","funders":"","keywords":"Lithosphere; Geology; Composition (language); Earth science; Geochemistry; Paleontology; Tectonics; Art","score_opus":0.008987153528531877,"score_gpt":0.17639547530739141,"score_spread":0.16740832177885953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406691525","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8391026,0.010058998,0.006385881,0.00041066963,0.000048711117,0.00002261017,0.00043417982,0.00007244672,0.14346388],"genre_scores_gemma":[0.9815481,0.0056781042,0.0015758086,0.00004354986,0.000034309724,0.0000051453953,0.00017400402,0.00006527391,0.010875812],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99988735,0.000028812268,0.000007521529,0.000027493043,0.000030258792,0.000018512234],"domain_scores_gemma":[0.9998667,0.000055590266,0.000030180498,0.000012229114,0.000019953439,0.000015377529],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029270485,0.00019509047,0.00015532397,0.0005561233,0.00020658552,0.0019765547,0.00033795252,0.00021463874,0.00388678],"category_scores_gemma":[0.00070471753,0.00014087866,0.00011798714,0.0010529176,0.000923211,0.0010545895,0.00049279263,0.0003021412,0.0005994104],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007711783,0.00005438542,0.1264167,0.00061942847,0.00012592808,0.0013058551,0.0068113618,0.008441606,0.11378185,0.11332914,0.0013819281,0.62696064],"study_design_scores_gemma":[0.000030064479,0.0002492905,0.84288675,0.00025555294,0.00013478233,0.0016209263,0.004863693,0.008981338,0.0225856,0.054192424,0.06412079,0.000078736535],"about_ca_topic_score_codex":0.0020123587,"about_ca_topic_score_gemma":0.0051352535,"teacher_disagreement_score":0.00388678,"about_ca_system_score_codex":0.00043876877,"about_ca_system_score_gemma":0.00024856237,"threshold_uncertainty_score":0.013002634},"labels":[],"label_agreement":null},{"id":"W4406787367","doi":"10.1093/gji/ggaf031","title":"The 2020 <i>M</i>w 6.4 Koryak Highlands earthquake illustrates hidden seismic hazards in the northern Pacific Cordillera","year":2025,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Geology; Seismology","score_opus":0.007815140461328257,"score_gpt":0.22418815846939932,"score_spread":0.21637301800807107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406787367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960247,0.0001416094,0.000052721585,0.00010812611,0.000006973211,0.0000038540775,0.00018038995,0.000019328087,0.003462151],"genre_scores_gemma":[0.999132,0.00008991092,0.0001165654,0.000016082122,0.0000062415247,0.0000023534285,0.00023650788,0.0000028775307,0.0003975735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.0000043664118,0.0000035971145,0.000011177459,0.000013677314,0.000017722952],"domain_scores_gemma":[0.999907,0.000006586464,0.000028922488,0.000008547824,0.000020617208,0.00002829807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008840234,0.00022751643,0.00012427548,0.00043685985,0.0005708677,0.00068056665,0.00018890062,0.00023182783,0.002246436],"category_scores_gemma":[0.00025101966,0.000076862,0.000088668196,0.0005990158,0.00030632777,0.00024290424,0.0006843709,0.00017876255,0.0002490071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000273049,0.000042725896,0.9315621,0.00011554258,0.000050959774,0.0034458346,0.0016446057,0.0019455908,0.014044022,0.0005808691,0.0017633849,0.044531442],"study_design_scores_gemma":[0.0000047011918,0.000017418839,0.99651474,0.00001708605,0.000011733477,0.00015522592,0.00072209036,0.0009531642,0.0003022994,0.000095250536,0.0012017032,0.000004600903],"about_ca_topic_score_codex":0.050338693,"about_ca_topic_score_gemma":0.0816199,"teacher_disagreement_score":0.050338693,"about_ca_system_score_codex":0.0006358599,"about_ca_system_score_gemma":0.00042439057,"threshold_uncertainty_score":0.10009134},"labels":[],"label_agreement":null},{"id":"W4406790707","doi":"10.1139/cjes-2024-0118","title":"Effect of Lithospheric Thickness and Radial Mantle Viscosity Profile on Glacial Isostatic Adjustment Crustal Motions in North America","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Post-glacial rebound; Lithosphere; Mantle (geology); Isostasy; Glacial period; Petrology; Geophysics; Seismology; Geomorphology; Tectonics","score_opus":0.008928441499157586,"score_gpt":0.2247523836782533,"score_spread":0.2158239421790957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406790707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995426,0.000026340222,0.00010138644,0.000010450124,7.4865045e-7,0.0000011633571,0.000057190817,0.0000110009705,0.00024911147],"genre_scores_gemma":[0.99962115,0.000028655875,0.000117044314,0.0000043437867,4.777138e-7,0.0000014810809,0.00012215778,0.000006662649,0.000098066994],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988854,0.000031175314,0.0000071497616,0.00002855356,0.000015360642,0.000029194194],"domain_scores_gemma":[0.999746,0.0001258301,0.000035765162,0.000026253561,0.000034365872,0.000031835836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032565152,0.00046591024,0.00021597001,0.00034946905,0.00022628372,0.00085057825,0.00022940869,0.0003726704,0.0008869459],"category_scores_gemma":[0.0010713526,0.0002556613,0.0005317346,0.0002850178,0.00024523173,0.00036023787,0.00036679982,0.0001818313,0.00013010066],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00088815734,0.00014985455,0.53681594,0.000099075485,0.00045259015,0.0005382782,0.00047736533,0.37995785,0.06249839,0.00031555642,0.0003802973,0.017426567],"study_design_scores_gemma":[0.0000500685,0.00033182293,0.7510369,0.00003258019,0.0001600144,0.00014175016,0.00074865436,0.23738672,0.009267603,0.00017910922,0.0006166555,0.000048108996],"about_ca_topic_score_codex":0.031720098,"about_ca_topic_score_gemma":0.033300422,"teacher_disagreement_score":0.9682799,"about_ca_system_score_codex":0.00050271803,"about_ca_system_score_gemma":0.000366223,"threshold_uncertainty_score":0.06307095},"labels":[],"label_agreement":null},{"id":"W4406802150","doi":"10.1007/s10950-025-10279-y","title":"Improved earthquake locations through a new 1-D P-wave velocity model for the Isthmus of Panama using particle swarm optimization method","year":2025,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Secretaría Nacional de Ciencia, Tecnología e Innovación","keywords":"Panama; Particle swarm optimization; Seismology; Geology; Structural geology; Hydrogeology; Geodesy; Earthquake swarm; Particle velocity; Geophysics; Physics; Computer science; Mechanics; Mathematics; Algorithm; Induced seismicity; Geotechnical engineering; Statistics","score_opus":0.06771637850610839,"score_gpt":0.30732467383923284,"score_spread":0.23960829533312444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406802150","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3209275,0.00046425298,0.66898364,0.0004469042,0.00018014213,0.0000795502,0.00046641397,0.00086601684,0.007585534],"genre_scores_gemma":[0.9613544,0.00017222649,0.036341578,0.00003813311,0.00003372946,0.000073244715,0.00024017485,0.00005912404,0.0016873506],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992764,0.000015965077,0.000006226179,0.000029434084,0.000012058097,0.000008668828],"domain_scores_gemma":[0.9998809,0.000033047458,0.000022631626,0.000012268652,0.00003883058,0.000012217815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017172867,0.0007069787,0.00069608865,0.00034974204,0.0005046548,0.0007834089,0.0008008723,0.0011617971,0.0011721032],"category_scores_gemma":[0.0005865912,0.00055097387,0.00054093526,0.00046672503,0.0002638562,0.00076812383,0.0004882777,0.0006681908,0.00022719885],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008367424,0.000010906477,0.00060747535,0.000009015138,0.000010809452,0.000029235998,0.000011872992,0.99472636,0.0005326224,0.00025601813,0.0000998587,0.003697497],"study_design_scores_gemma":[0.0000023650452,0.000003010351,0.00011551874,7.533454e-7,0.0000025670583,0.0000013869521,0.000001836742,0.9997211,0.00004023789,0.00005511314,0.00005457281,0.0000014843682],"about_ca_topic_score_codex":0.03729636,"about_ca_topic_score_gemma":0.02163037,"teacher_disagreement_score":0.03729636,"about_ca_system_score_codex":0.00044014765,"about_ca_system_score_gemma":0.0008976399,"threshold_uncertainty_score":0.07415855},"labels":[],"label_agreement":null},{"id":"W4406937066","doi":"10.1111/bor.12689","title":"Drivers of glacially induced fault reactivation in the Baltic Sea sector of the Tornquist Fan","year":2025,"lang":"en","type":"article","venue":"Boreas","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Deutsche Forschungsgemeinschaft","keywords":"Geology; Quaternary; Seismology; Oceanography; Paleontology","score_opus":0.015988169388869884,"score_gpt":0.22598043053437739,"score_spread":0.2099922611455075,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406937066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999522,0.000049133832,0.000053766777,0.000023551973,0.000002312865,0.0000011800731,0.00008144659,0.0000062513373,0.00026050184],"genre_scores_gemma":[0.99973863,0.000031555428,0.00003527646,0.000003749911,0.0000011293322,0.0000014321068,0.00010078312,0.0000019095803,0.0000856273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998715,0.00002766947,0.000011280372,0.000045701367,0.000014668065,0.000029185318],"domain_scores_gemma":[0.99974877,0.00006127904,0.00009326078,0.000022293603,0.000031112922,0.000043292563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025339084,0.00028866477,0.00022122942,0.0005442895,0.00030952293,0.001021855,0.0002830186,0.0005017302,0.0016789209],"category_scores_gemma":[0.0008870021,0.0002627732,0.0003006413,0.0005858009,0.0005320419,0.00036856858,0.00042033094,0.00021832864,0.0001696094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010177601,0.00003560324,0.9599785,0.00002821634,0.00008072796,0.0004760368,0.00042530423,0.028540889,0.0032822834,0.00033452705,0.00021049519,0.0065058265],"study_design_scores_gemma":[0.00001211374,0.000042521424,0.97411186,0.000020115662,0.000026736592,0.00009612986,0.0006182944,0.024077127,0.00022237306,0.00018013765,0.00057932414,0.000013267496],"about_ca_topic_score_codex":0.035228815,"about_ca_topic_score_gemma":0.052445356,"teacher_disagreement_score":0.035228815,"about_ca_system_score_codex":0.0008833509,"about_ca_system_score_gemma":0.00065922056,"threshold_uncertainty_score":0.07004756},"labels":[],"label_agreement":null},{"id":"W4406965725","doi":"10.4095/puaddrjbu2","title":"An overview of seismic attenuation in the western Quebec seismic zone","year":2025,"lang":"en","type":"report","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Seismic zone; Attenuation; Induced seismicity; Physics","score_opus":0.07061073906460047,"score_gpt":0.3108076815465961,"score_spread":0.24019694248199563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406965725","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.25824696,0.1152263,0.0058456776,0.0052217953,0.0003492531,0.00072517607,0.28986517,0.0012384732,0.32328114],"genre_scores_gemma":[0.697024,0.06748612,0.006844287,0.0005842742,0.0003071269,0.00025280923,0.100298196,0.00027738983,0.12692578],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9992631,0.0000670961,0.00004675556,0.00007106876,0.0003357409,0.0002162774],"domain_scores_gemma":[0.99761534,0.00017275193,0.00016547232,0.00004662396,0.001875556,0.00012426062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00087618956,0.00073803216,0.00035361957,0.009194159,0.00096647575,0.0014595211,0.00086598017,0.00032392374,0.018225485],"category_scores_gemma":[0.0017828115,0.00021639462,0.0004165074,0.016849605,0.00027900073,0.00056243135,0.00045996183,0.00033198902,0.001487829],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003291595,0.00011079502,0.36090577,0.0022205599,0.00024693002,0.0005118895,0.0014933583,0.012309188,0.0020822396,0.0056640017,0.18021262,0.43391356],"study_design_scores_gemma":[0.0000090478825,0.000033978733,0.8801202,0.00035653566,0.00006042916,0.000094835246,0.0007065013,0.0013687294,0.00027186447,0.00012408108,0.116831414,0.00002241569],"about_ca_topic_score_codex":0.99318343,"about_ca_topic_score_gemma":0.99537486,"teacher_disagreement_score":0.021372892,"about_ca_system_score_codex":0.021372892,"about_ca_system_score_gemma":0.01672987,"threshold_uncertainty_score":0.15507191},"labels":[],"label_agreement":null},{"id":"W4407006612","doi":"10.1785/0120250005","title":"<i>Erratum to</i> Introduction to the <i>BSSA</i> Special Issue and <i>SRL</i> Focus Section on Seismic Hazard Models","year":2025,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Section (typography); Focus (optics); Hazard; Geology; Seismology; Computer science; Physics; Biology; Ecology","score_opus":0.009486279469923373,"score_gpt":0.203483246655223,"score_spread":0.19399696718529963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407006612","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003255662,0.002150743,0.007000319,0.059731122,0.8875071,0.000114202936,0.011382553,0.0025950633,0.029193364],"genre_scores_gemma":[0.0085109845,0.008250985,0.012239207,0.068679176,0.3725716,0.00048034944,0.034308545,0.0073450934,0.48761413],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99854374,0.00018608109,0.00018954033,0.00014244234,0.0008371469,0.00010107862],"domain_scores_gemma":[0.9854989,0.0033639476,0.000836419,0.001228234,0.008423045,0.00064945046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018866099,0.0021612758,0.0015076037,0.004916096,0.0018418552,0.004226818,0.0024692887,0.0028828047,0.11926378],"category_scores_gemma":[0.018277107,0.00095705036,0.001812393,0.003868948,0.000979529,0.0027536256,0.001596701,0.0063465303,0.10724699],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000005341981,0.000004047638,0.00002186789,0.000017302276,0.0000019631184,0.00000655089,0.0000017757262,0.0000513147,0.000024984207,0.00021150656,0.99771726,0.0019361468],"study_design_scores_gemma":[0.000016163845,0.000016881844,0.0011615128,0.0001263498,0.0000136520775,0.000046150308,0.000028655923,0.0006299967,0.00022184831,0.0017497105,0.99596405,0.000025039495],"about_ca_topic_score_codex":0.025353985,"about_ca_topic_score_gemma":0.04339475,"teacher_disagreement_score":0.11926378,"about_ca_system_score_codex":0.0026189152,"about_ca_system_score_gemma":0.003523494,"threshold_uncertainty_score":0.3989771},"labels":[],"label_agreement":null},{"id":"W4407049933","doi":"10.1785/0220250015","title":"<i>Erratum to</i> Introduction to the <i>BSSA</i> Special Issue and <i>SRL</i> Focus Section on Seismic Hazard Models","year":2025,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Section (typography); Focus (optics); Special section; Hazard; Geology; Seismology; Computer science; Engineering; Physics; Biology; Engineering physics; Ecology; Optics","score_opus":0.0368928155120024,"score_gpt":0.28583163390568733,"score_spread":0.24893881839368492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407049933","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00028267692,0.0016663297,0.0060410956,0.061450537,0.89978814,0.00007806124,0.0057046516,0.0018790277,0.02310948],"genre_scores_gemma":[0.009367418,0.0066886437,0.011600065,0.088365264,0.43878007,0.00039957985,0.020309323,0.0070949653,0.41739464],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9983223,0.00020112345,0.00020741044,0.00017215275,0.00096525444,0.00013164173],"domain_scores_gemma":[0.9854767,0.0034048324,0.00086094707,0.0013331404,0.00818248,0.00074190676],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020387676,0.002219773,0.0015686809,0.0046632877,0.002301128,0.004775798,0.002884347,0.0035353622,0.09805756],"category_scores_gemma":[0.018152218,0.0009935522,0.0020506333,0.0032910989,0.001134518,0.0027719897,0.0016846459,0.0073224427,0.08996115],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00000628469,0.0000042612596,0.00001981045,0.000016789198,0.000002453555,0.000008358774,0.0000017805938,0.000057194517,0.00003377812,0.00025446768,0.9976701,0.0019247222],"study_design_scores_gemma":[0.000016167862,0.000018975767,0.0010401176,0.000117161064,0.000017758177,0.00005744077,0.000032031796,0.000929322,0.00031438904,0.0022706809,0.9951567,0.000029164752],"about_ca_topic_score_codex":0.02529098,"about_ca_topic_score_gemma":0.04061366,"teacher_disagreement_score":0.09805756,"about_ca_system_score_codex":0.0030458057,"about_ca_system_score_gemma":0.0036532,"threshold_uncertainty_score":0.32803524},"labels":[],"label_agreement":null},{"id":"W4407311314","doi":"10.22541/essoar.173924247.70922881/v1","title":"Fluid-induced Earthquake Nucleation on Aging Rate-and-State Faults: Influence of Hydraulic Diffusivity and Injection Rate under Different Nucleation Regimes","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Nucleation; Thermal diffusivity; Materials science; Diffusion; Mechanics; Thermodynamics; Physics","score_opus":0.019190862663071212,"score_gpt":0.2423403880556801,"score_spread":0.22314952539260888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407311314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99588436,0.00018537803,0.0024691531,0.000056749177,0.000013504819,0.000015009297,0.00009391975,0.000041283583,0.0012405661],"genre_scores_gemma":[0.99918646,0.0000851241,0.00052601146,0.00000860224,0.000002287005,0.000009582482,0.00005640392,0.000008005043,0.000117391406],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991393,0.000014265921,0.000008548511,0.000019184652,0.000011885592,0.000032069074],"domain_scores_gemma":[0.9995433,0.00023477385,0.00009039149,0.000027903821,0.00005082694,0.00005272987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002634108,0.00037288983,0.0004774805,0.00045204948,0.0003234507,0.0005436808,0.00039307185,0.00048803457,0.0007755137],"category_scores_gemma":[0.0011655338,0.00023461448,0.00055944745,0.00022985182,0.00058421126,0.00052406534,0.00033038823,0.0004352207,0.000063894426],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033313886,0.0002917032,0.025696574,0.00017345192,0.00009532812,0.00044840254,0.00019985052,0.88124776,0.08254192,0.0034275735,0.0002857901,0.0052585257],"study_design_scores_gemma":[0.000023339842,0.000064477485,0.0036524632,0.000009308842,0.000021760397,0.000016463453,0.000038289367,0.98376197,0.012056372,0.00021225396,0.00012908423,0.000014244654],"about_ca_topic_score_codex":0.0072687585,"about_ca_topic_score_gemma":0.0038413287,"teacher_disagreement_score":0.0072687585,"about_ca_system_score_codex":0.00069207326,"about_ca_system_score_gemma":0.00051392737,"threshold_uncertainty_score":0.014452875},"labels":[],"label_agreement":null},{"id":"W4407369032","doi":"10.1175/bams-d-24-0040.1","title":"A Triple Jeopardy Flood Event: Coincident Arrival of the 2022 Tonga Tsunami with a Storm Surge and Meteotsunami on the East Coast of the United States","year":2025,"lang":"en","type":"article","venue":"Bulletin of the American Meteorological Society","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Storm surge; Flood myth; Storm; Surge; Meteorology; East coast; Climatology; Winter storm; Environmental science; Oceanography; Geology; Geography","score_opus":0.01036655849284258,"score_gpt":0.2057727955012227,"score_spread":0.19540623700838014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407369032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99647444,0.000085793545,0.00012544358,0.0005096659,0.00009008561,0.000014663246,0.00037105338,0.00003076089,0.0022980836],"genre_scores_gemma":[0.99866855,0.000059446174,0.00011425225,0.0001398032,0.000037277245,0.0000079672245,0.00041207904,0.0000037685863,0.0005569397],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991167,0.000010916987,0.000007612117,0.000013832592,0.000024351226,0.000031664356],"domain_scores_gemma":[0.9996699,0.00002672293,0.00006703315,0.0000253893,0.00007094448,0.00013995939],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020489239,0.00023441302,0.00016990917,0.000463288,0.00120859,0.00061708747,0.00013876535,0.0004902983,0.0015070016],"category_scores_gemma":[0.0004115808,0.0001376969,0.00016738263,0.0003122024,0.00027305546,0.00027190667,0.0011663596,0.0007813903,0.00015294194],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004240167,0.00016203975,0.94506514,0.000056586105,0.0001677584,0.01181057,0.0025250232,0.00091868197,0.010336868,0.00042076217,0.01305401,0.015058548],"study_design_scores_gemma":[0.000011205527,0.0001081313,0.99020046,0.00001916726,0.000030564064,0.00084576936,0.002244001,0.0012182652,0.00075700344,0.00008056914,0.0044684783,0.000016398926],"about_ca_topic_score_codex":0.039493363,"about_ca_topic_score_gemma":0.09440894,"teacher_disagreement_score":0.039493363,"about_ca_system_score_codex":0.0008447189,"about_ca_system_score_gemma":0.00065448886,"threshold_uncertainty_score":0.07852697},"labels":[],"label_agreement":null},{"id":"W4407370912","doi":"10.1029/2024gc011949","title":"Anomalous Sediment Consolidation and Alteration From Buried Incoming Plate Seamounts Along the Cascadia Margin","year":2025,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Seamount; Margin (machine learning); Consolidation (business); Seismology; Subduction; Sediment; Geochemistry; Petrology; Geomorphology; Tectonics","score_opus":0.007198353045150779,"score_gpt":0.20226309654085806,"score_spread":0.19506474349570727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407370912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99968946,0.00000742218,0.000031643165,0.0000023905304,3.0034292e-7,6.508179e-7,0.000073726944,0.000008459162,0.00018589174],"genre_scores_gemma":[0.99964464,0.00000985519,0.00004359421,0.0000013171556,4.885072e-7,8.7383904e-7,0.00013692633,0.0000018950044,0.00016034638],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994326,0.0000027787373,0.000004731085,0.000019174076,0.00001691259,0.00001304895],"domain_scores_gemma":[0.99986124,0.000010149011,0.00004713582,0.000017730008,0.000030220743,0.00003354824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000763837,0.00030867808,0.0001249647,0.0009948887,0.00032621893,0.00035889912,0.00019307193,0.00022421681,0.000945351],"category_scores_gemma":[0.00020965969,0.00021169009,0.0001795725,0.0005737662,0.0002674535,0.00013232646,0.00041432324,0.00012570713,0.00014821308],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015614975,0.000019345915,0.93707424,0.000026182262,0.000063923624,0.0005903236,0.000875072,0.0013916646,0.053939294,0.000046916724,0.00009045678,0.005726384],"study_design_scores_gemma":[5.7787275e-7,0.000008316382,0.9991636,0.0000011948558,0.0000035558328,0.000029474942,0.00010171255,0.00022260624,0.0004242338,0.0000039392075,0.00003962272,0.0000011499828],"about_ca_topic_score_codex":0.028495459,"about_ca_topic_score_gemma":0.05405354,"teacher_disagreement_score":0.028495459,"about_ca_system_score_codex":0.00041862266,"about_ca_system_score_gemma":0.00017212883,"threshold_uncertainty_score":0.05665922},"labels":[],"label_agreement":null},{"id":"W4407383376","doi":"10.5194/egusphere-2025-390","title":"Characterizing some major Archean faults at depth in the Superior craton, North America","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"Canada First Research Excellence Fund","keywords":"Archean; Craton; Geology; Geochemistry; Earth science; Paleontology; Tectonics","score_opus":0.025374048084671415,"score_gpt":0.24175802001181548,"score_spread":0.21638397192714406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407383376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984457,0.00022777074,0.0000622918,0.000018882434,8.592121e-7,0.0000049208943,0.00027837785,0.000006222551,0.00095499255],"genre_scores_gemma":[0.9986877,0.00017691281,0.00023090774,0.000009869116,0.0000017503273,0.0000038990343,0.00036506754,0.0000013964197,0.00052256044],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994147,0.0000034732138,0.0000041856933,0.000017512157,0.000018333149,0.0000150439655],"domain_scores_gemma":[0.99976915,0.000017088965,0.00005884203,0.000010225271,0.000102029684,0.000042669948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000102456936,0.00020128359,0.00010806357,0.0014330168,0.0005028186,0.00041342192,0.00014424048,0.00016394313,0.0009453637],"category_scores_gemma":[0.00024498775,0.00012237945,0.00006901763,0.0017198945,0.00038003467,0.00019953365,0.0002931419,0.00010757686,0.00008982826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003978923,0.000010946254,0.97681534,0.000050048,0.00002159191,0.00019049695,0.00090926484,0.00036103633,0.006741507,0.00010487055,0.00028058764,0.014474455],"study_design_scores_gemma":[0.0000011574976,0.0000039446245,0.9991788,0.0000053710523,0.0000029789564,0.000033989927,0.00020052383,0.00015067993,0.000085258645,0.000011293259,0.00032515192,8.064977e-7],"about_ca_topic_score_codex":0.3661171,"about_ca_topic_score_gemma":0.7537834,"teacher_disagreement_score":0.6338829,"about_ca_system_score_codex":0.001078695,"about_ca_system_score_gemma":0.00093553733,"threshold_uncertainty_score":0.7279721},"labels":[],"label_agreement":null},{"id":"W4407387179","doi":"10.1029/2024av001468","title":"Subduction Zone Obliquity Dictates Global Trench‐Parallel Inner Forearc Deformation","year":2025,"lang":"en","type":"article","venue":"AGU Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation","keywords":"Forearc; Subduction; Geology; Trench; Deformation (meteorology); Seismology; Tectonics; Oceanography; Materials science","score_opus":0.009495418143153859,"score_gpt":0.24320762674592225,"score_spread":0.2337122086027684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407387179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99934334,0.000028314287,0.00011638276,0.000007507986,6.3927524e-7,0.0000010640438,0.00005963652,0.00000509847,0.00043800342],"genre_scores_gemma":[0.99986386,0.000015855378,0.000026243013,0.0000014762983,5.673541e-7,3.3846197e-7,0.000036817393,0.0000015227369,0.000053247393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992776,0.000011111905,0.0000054636403,0.000023328645,0.000011454385,0.000020881293],"domain_scores_gemma":[0.9995735,0.00010984491,0.00018421754,0.000035872185,0.000050168128,0.000046345307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017229123,0.00019490512,0.00013839192,0.000561165,0.00011563947,0.0005572474,0.00010089481,0.000112291054,0.0011855802],"category_scores_gemma":[0.0008344237,0.00013376038,0.00015330271,0.00044991483,0.00035705674,0.00023142545,0.00027733337,0.00013225948,0.0001932585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031962405,0.0000060017796,0.985843,0.000011774595,0.000036486555,0.000048678183,0.00009583799,0.0035835805,0.008063302,0.00014075362,0.000055230037,0.0020834624],"study_design_scores_gemma":[0.0000010803218,0.000007189261,0.9974694,0.000002613677,0.000007721326,0.000026375916,0.00007998786,0.0017475963,0.0005044718,0.00005604427,0.0000955087,0.0000019440583],"about_ca_topic_score_codex":0.005115738,"about_ca_topic_score_gemma":0.009815933,"teacher_disagreement_score":0.005115738,"about_ca_system_score_codex":0.0003268297,"about_ca_system_score_gemma":0.00019798816,"threshold_uncertainty_score":0.01017195},"labels":[],"label_agreement":null},{"id":"W4407472075","doi":"10.26443/seismica.v2i4.1406","title":"Performance of Slab Geometry Constraints on Rapid Geodetic Slip Models, Tsunami Amplitude, and Inundation Estimates in Cascadia","year":2025,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Nuclear Safety and Security Commission; University of Oregon; University of Washington; National Aeronautics and Space Administration","keywords":"Seismology; Geology; Subduction; Geodetic datum; Slip (aerodynamics); GNSS applications; Tsunami earthquake; Amplitude; Earthquake rupture; Geodesy; Aftershock; Fault (geology); Global Positioning System; Tectonics; Computer science; Engineering; Aerospace engineering","score_opus":0.01397998412920392,"score_gpt":0.22069801250013246,"score_spread":0.20671802837092854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407472075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945305,0.000049872866,0.0036654933,0.00012532178,0.000008138059,0.0000057129723,0.00015294328,0.0002322089,0.0012297053],"genre_scores_gemma":[0.9986816,0.000015746948,0.0009836601,0.000010549741,0.0000016089035,0.0000022409574,0.00015855877,0.000012510398,0.00013344476],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999723,0.00010432487,0.000025218513,0.00006732605,0.0000338123,0.000046243003],"domain_scores_gemma":[0.9989011,0.0005582453,0.00011513606,0.00014515319,0.00015921768,0.00012112226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009406978,0.0008380956,0.00048909127,0.0003415776,0.00035710065,0.00077520224,0.00081261597,0.000761533,0.0012084967],"category_scores_gemma":[0.0036898332,0.0004951188,0.00047466147,0.00029731233,0.0004675631,0.0005487454,0.0006540929,0.00062642875,0.00016847708],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000103383456,0.000029148412,0.007980365,0.000007920817,0.00002696898,0.000028807008,0.000027590238,0.987763,0.0009408033,0.00023213966,0.00008023718,0.0027795816],"study_design_scores_gemma":[0.000013259766,0.000034674536,0.002060696,0.0000040858636,0.0000061692926,0.0000056465847,0.00002206279,0.99721885,0.00047402273,0.000101084006,0.000053391064,0.000005981463],"about_ca_topic_score_codex":0.09695662,"about_ca_topic_score_gemma":0.052723017,"teacher_disagreement_score":0.09695662,"about_ca_system_score_codex":0.0012849646,"about_ca_system_score_gemma":0.0015464054,"threshold_uncertainty_score":0.19278455},"labels":[],"label_agreement":null},{"id":"W4407531641","doi":"10.1103/physreve.111.024307","title":"Leveraging spurious Omori-Utsu relation in the nearest-neighbor declustering method","year":2025,"lang":"en","type":"article","venue":"Physical review. E","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Agencia Estatal de Investigación; European Regional Development Fund; Natural Sciences and Engineering Research Council of Canada","keywords":"Spurious relationship; Relation (database); k-nearest neighbors algorithm; Computer science; Data mining; Artificial intelligence; Machine learning","score_opus":0.026134944884501247,"score_gpt":0.33132131950336524,"score_spread":0.305186374618864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407531641","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05367798,0.00053363637,0.94229996,0.00013397302,0.00009442807,0.00008563298,0.00012679532,0.00026142586,0.0027861435],"genre_scores_gemma":[0.6066035,0.0004996986,0.3888744,0.00010089738,0.000121439036,0.00015882244,0.00032291748,0.00021148665,0.0031068518],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99856,0.0005769334,0.00013292785,0.00022989303,0.00038876207,0.00011147157],"domain_scores_gemma":[0.9911253,0.0053874794,0.0008269969,0.0013748885,0.001034508,0.0002508562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031833265,0.000494632,0.0005719153,0.0014692079,0.0006166638,0.0011738099,0.001397253,0.00070623157,0.002362607],"category_scores_gemma":[0.02497207,0.0002614893,0.0004656221,0.0010000704,0.0008769091,0.0020359976,0.0017904285,0.0010111266,0.0005837673],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005041273,0.00020943425,0.051713146,0.0007203005,0.00025832196,0.0010795778,0.0012276919,0.22640193,0.017651066,0.29112947,0.004527732,0.4045772],"study_design_scores_gemma":[0.000021001475,0.00006625367,0.004953223,0.00005547259,0.000033540553,0.00027656872,0.00012711821,0.92705303,0.004310142,0.059221305,0.00384078,0.00004160192],"about_ca_topic_score_codex":0.002711868,"about_ca_topic_score_gemma":0.0043011564,"teacher_disagreement_score":0.0031833265,"about_ca_system_score_codex":0.00056534517,"about_ca_system_score_gemma":0.001112318,"threshold_uncertainty_score":0.016835213},"labels":[],"label_agreement":null},{"id":"W4407682421","doi":"10.1093/gji/ggaf061","title":"Recent earthquakes on unmapped faults highlight hidden seismic hazards within the Golden Triangle region of Laos, Thailand and Myanmar","year":2025,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Seismology; Geology","score_opus":0.014096918166024474,"score_gpt":0.23737323814868339,"score_spread":0.2232763199826589,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407682421","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986129,0.00005059473,0.00008149957,0.000055867124,0.0000021406092,0.0000028876668,0.00035286724,0.000011140663,0.0008301191],"genre_scores_gemma":[0.9991886,0.000057732486,0.00013260824,0.000008702738,0.00000391637,0.000004987739,0.0004212907,0.0000035701423,0.00017859899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999082,0.00001658342,0.000008101993,0.000021542131,0.00001272315,0.0000327792],"domain_scores_gemma":[0.9997559,0.000029560388,0.00010276777,0.000023381293,0.000037815957,0.000050643608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015885812,0.00014505687,0.000103509265,0.00051783014,0.00030252515,0.00068211305,0.00020842373,0.00011997037,0.0014293962],"category_scores_gemma":[0.00046201635,0.00007225737,0.000120085286,0.000848168,0.00034994198,0.00039790114,0.0008442014,0.00017033807,0.00017415284],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011292908,0.000025110447,0.9673379,0.00006977446,0.000046754383,0.0012719852,0.003223334,0.0031241938,0.005686894,0.00034985252,0.0007111926,0.018040143],"study_design_scores_gemma":[0.0000045655,0.000036154932,0.99088305,0.00002856923,0.000017216418,0.00032686524,0.0038713545,0.002216232,0.00042747782,0.00007946408,0.0020982001,0.000010921109],"about_ca_topic_score_codex":0.022475936,"about_ca_topic_score_gemma":0.03844931,"teacher_disagreement_score":0.022475936,"about_ca_system_score_codex":0.00032383265,"about_ca_system_score_gemma":0.0003302478,"threshold_uncertainty_score":0.04469019},"labels":[],"label_agreement":null},{"id":"W4407755625","doi":"10.1029/2024wr037767","title":"Using Water Level Responses to Atmospheric Pressure Variations to Measure and Monitor Vertical Leakage Through Confining Units, With Application to the Jurassic Shaximiao Crust, China","year":2025,"lang":"en","type":"article","venue":"Water Resources Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China; Canadian Institute for Advanced Research","keywords":"China; Leakage (economics); Environmental science; Measure (data warehouse); Geology; Crust; Atmospheric pressure; Hydrology (agriculture); Geotechnical engineering; Geophysics; Geography; Oceanography","score_opus":0.09314575296459754,"score_gpt":0.3186628773885992,"score_spread":0.22551712442400168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407755625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99824786,0.000030490422,0.0012886232,0.000015575079,0.0000020138616,0.0000056103495,0.00010712637,0.000051251925,0.0002514503],"genre_scores_gemma":[0.99887127,0.000020003272,0.0009394436,0.0000029719906,0.0000011383014,0.0000036677318,0.00007181724,0.0000023301805,0.00008733613],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992585,0.0000075786224,0.000004709692,0.0000334038,0.000016358776,0.000012115698],"domain_scores_gemma":[0.999838,0.00003425065,0.00004696529,0.000018190383,0.000037871177,0.000024697123],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023163008,0.00045191118,0.00023553745,0.0006491282,0.0004391655,0.00047491948,0.00035977762,0.00033697224,0.00030142165],"category_scores_gemma":[0.00035095648,0.00019866021,0.00027434298,0.0011110133,0.0002780079,0.00031741738,0.00028290445,0.00017015335,0.000040767834],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026094855,0.00025193277,0.64607483,0.00011099064,0.0001794077,0.00040502005,0.00047348978,0.19137548,0.0965044,0.00025083835,0.000312679,0.06379995],"study_design_scores_gemma":[0.000033072996,0.00015341486,0.48702127,0.0000051374627,0.00006332191,0.00004388005,0.00018654988,0.49983013,0.012185608,0.00015147692,0.00028496044,0.00004123226],"about_ca_topic_score_codex":0.057320416,"about_ca_topic_score_gemma":0.06487831,"teacher_disagreement_score":0.057320416,"about_ca_system_score_codex":0.00070124754,"about_ca_system_score_gemma":0.00059267157,"threshold_uncertainty_score":0.11397356},"labels":[],"label_agreement":null},{"id":"W4407815896","doi":"10.1139/cjes-2024-0132","title":"The MacKenzie Mountains, Northwest Territories, earthquake sequence of 1953 to 1957","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Sequence (biology); Seismology; Physical geography; Geography","score_opus":0.02181227394475137,"score_gpt":0.2415953852151057,"score_spread":0.21978311127035433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407815896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9795561,0.0009216119,0.00011225995,0.00022720925,0.000025186555,0.00005517058,0.009028723,0.00002756566,0.010046094],"genre_scores_gemma":[0.9877928,0.00068145467,0.0004022197,0.00008412238,0.000015976713,0.00003229845,0.0068521323,0.000009830501,0.0041291662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998184,0.000006157771,0.00001003392,0.000032355343,0.00007659755,0.00005645973],"domain_scores_gemma":[0.9996692,0.000009430649,0.00006684064,0.000010868098,0.00017047321,0.00007309217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012618596,0.00022401831,0.00019040825,0.0014205985,0.0021420533,0.0006313671,0.00048030043,0.00020192564,0.0018886521],"category_scores_gemma":[0.0006596671,0.00009846745,0.00010074551,0.0020497064,0.00044019762,0.00017449258,0.00065561663,0.00023759564,0.00023205805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002789847,0.00006051492,0.910805,0.00032148632,0.00013994238,0.0023211562,0.0070349635,0.000981872,0.007938581,0.00092424,0.019572694,0.049620412],"study_design_scores_gemma":[0.0000026377684,0.0000063148004,0.9922975,0.000016050017,0.0000070121273,0.00004196933,0.0004998893,0.0000672639,0.00011737926,0.0000106247535,0.0069291256,0.000004274777],"about_ca_topic_score_codex":0.97117436,"about_ca_topic_score_gemma":0.9935301,"teacher_disagreement_score":0.02882564,"about_ca_system_score_codex":0.009614472,"about_ca_system_score_gemma":0.006465765,"threshold_uncertainty_score":0.06975818},"labels":[],"label_agreement":null},{"id":"W4407857620","doi":"10.1038/s43247-025-02113-7","title":"Variable fault geometry controls the cascading 2023 Herat, Afghanistan multiplet sequence","year":2025,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Natural Science Foundation of China","keywords":"Multiplet; Variable (mathematics); Sequence (biology); Fault (geology); Geometry; Physics; Geology; Mathematics; Seismology; Spectral line; Mathematical analysis; Biology; Astronomy; Genetics","score_opus":0.030806157697287444,"score_gpt":0.24778646540878543,"score_spread":0.21698030771149798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407857620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987055,0.000028289498,0.0001078161,0.000045350844,0.0000041057806,0.0000022481606,0.00016470735,0.000018005958,0.00092393294],"genre_scores_gemma":[0.9994573,0.000016819291,0.000046778525,0.000011781778,0.0000023247937,0.0000019836148,0.00020760487,0.0000052451373,0.00025007987],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999056,0.000011271744,0.000004529701,0.000032497734,0.0000119630495,0.00003422874],"domain_scores_gemma":[0.99980634,0.000026405078,0.00006742638,0.000016409444,0.000036774498,0.00004661518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012207538,0.00027020054,0.00019787623,0.00040593176,0.00045060992,0.00073240214,0.00015810043,0.00025629974,0.0032832825],"category_scores_gemma":[0.00063389976,0.000118763055,0.00015181588,0.00044194437,0.00028105298,0.00020600662,0.0002684383,0.00022719234,0.00057307375],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005738878,0.00016245288,0.8386414,0.00004761979,0.00011022922,0.0011502481,0.00067378266,0.009083996,0.12453328,0.001966657,0.0026079612,0.02044845],"study_design_scores_gemma":[0.00001543676,0.000055309272,0.98950166,0.000007350079,0.000020349298,0.00021238618,0.00029708623,0.0072339503,0.0012213812,0.0002877276,0.0011363396,0.000011055073],"about_ca_topic_score_codex":0.01708547,"about_ca_topic_score_gemma":0.0276906,"teacher_disagreement_score":0.01708547,"about_ca_system_score_codex":0.00069142587,"about_ca_system_score_gemma":0.00036285236,"threshold_uncertainty_score":0.033972025},"labels":[],"label_agreement":null},{"id":"W4407865559","doi":"10.1029/2024jb029476","title":"The Role of the Three‐Dimensional Geometry of Fault Steps on Event Migration During Fluid‐Induced Seismic Sequences","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Horizon 2020 Framework Programme; European Regional Development Fund; Science Foundation Ireland; European Commission; Microseismic Industry Consortium","keywords":"Geology; Geometry; Event (particle physics); Fault (geology); Seismology; Normal fault; Mathematics; Physics","score_opus":0.024167909217441164,"score_gpt":0.30314791263125873,"score_spread":0.27898000341381757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407865559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987984,0.000023592587,0.0008021521,0.0000061596725,0.0000011584967,0.0000024116907,0.00006981571,0.000018589606,0.00027780613],"genre_scores_gemma":[0.99968946,0.000010578845,0.00020243796,8.7260406e-7,7.596195e-7,8.1537104e-7,0.00005959122,0.0000037182122,0.000031827873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998802,0.000025817608,0.000010687878,0.00003903506,0.00001983562,0.000024369649],"domain_scores_gemma":[0.9993637,0.00020887045,0.00023189165,0.000060172242,0.000058681122,0.00007670318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017259641,0.00020183998,0.0002117254,0.0009069554,0.00019227313,0.0008329263,0.000186667,0.000182356,0.00085508305],"category_scores_gemma":[0.0015368646,0.00015587902,0.0001537171,0.00053429726,0.0003947308,0.00047958357,0.00037982897,0.00012342424,0.00018118853],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054768065,0.000114949755,0.8053508,0.00010047719,0.00015042187,0.00042608893,0.00092469214,0.0374689,0.12225031,0.001074061,0.00025811754,0.03133342],"study_design_scores_gemma":[0.000004879206,0.000047132107,0.97002923,0.000008522887,0.000021757976,0.00008771074,0.00031631187,0.025613181,0.0033189072,0.0002736475,0.0002615741,0.000017178685],"about_ca_topic_score_codex":0.0029389495,"about_ca_topic_score_gemma":0.0036960628,"teacher_disagreement_score":0.0029389495,"about_ca_system_score_codex":0.00022580549,"about_ca_system_score_gemma":0.00018778005,"threshold_uncertainty_score":0.005843699},"labels":[],"label_agreement":null},{"id":"W4408008134","doi":"10.20944/preprints202502.2064.v1","title":"Comparison Of Backprojection Techniques For Rupture Propagation Modelling Of The Mw=7,8 Earthquake Near Kahramanmaras And Its Mw=7,5 Aftershock Near Elbistan Turkey, 2023","year":2025,"lang":"en","type":"preprint","venue":"Preprints.org","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Seismology; Geology","score_opus":0.12486284952519487,"score_gpt":0.33280704292515556,"score_spread":0.20794419339996068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408008134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.51558924,0.0005990749,0.47968167,0.0002257118,0.00007419613,0.000083552564,0.00044430036,0.0014191419,0.001883108],"genre_scores_gemma":[0.85440004,0.00055465335,0.14294495,0.00003699966,0.000026130338,0.00006385066,0.0005725236,0.00014137222,0.0012593756],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981636,0.000054119053,0.000015251592,0.00004739482,0.000034292592,0.000032556156],"domain_scores_gemma":[0.9995753,0.00022999273,0.000041381143,0.000023063814,0.000105491024,0.00002479829],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008793418,0.0011112886,0.0003975787,0.0008134689,0.00021699317,0.00091311906,0.000577729,0.0007882719,0.0010272969],"category_scores_gemma":[0.0013694402,0.00039413426,0.0008083697,0.0005454022,0.0002324511,0.0006203848,0.00043964825,0.00045893676,0.00046164566],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023993262,0.000095113035,0.005169954,0.000056229834,0.000071084425,0.00011829449,0.00011372624,0.92361593,0.0076297787,0.0004914302,0.00030571615,0.062092718],"study_design_scores_gemma":[0.0000036753895,0.000021980004,0.00074260915,0.000002825244,0.000005796079,0.0000123166565,0.000013186073,0.99819523,0.0008544393,0.00007449425,0.00006957329,0.0000039796114],"about_ca_topic_score_codex":0.015263106,"about_ca_topic_score_gemma":0.009023506,"teacher_disagreement_score":0.015263106,"about_ca_system_score_codex":0.00027583214,"about_ca_system_score_gemma":0.0005850833,"threshold_uncertainty_score":0.03034854},"labels":[],"label_agreement":null},{"id":"W4408017172","doi":"10.1109/taes.2025.3546178","title":"Investigating the Impacts of a G4-Level Geomagnetic Storm on Airborne GNSS Performance Using Mass ADS-B Data in Southern Canada","year":2025,"lang":"en","type":"article","venue":"IEEE Transactions on Aerospace and Electronic Systems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"GNSS applications; Geomagnetic storm; Earth's magnetic field; Storm; Remote sensing; Meteorology; Environmental science; Ionosphere; Geology; Global Positioning System; Geodesy; Geophysics; Computer science; Telecommunications; Physics; Magnetic field","score_opus":0.02616952637498193,"score_gpt":0.22555190529679686,"score_spread":0.19938237892181493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408017172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982352,0.00005761989,0.00020584751,0.00004849787,0.0000030453202,0.0000064315295,0.00069467875,0.000021141353,0.0007274663],"genre_scores_gemma":[0.9980558,0.00007863522,0.00025300452,0.000016053527,0.0000027252436,0.0000028825186,0.0011712804,0.0000055688997,0.00041399908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995572,0.000028604132,0.000015104675,0.0000744223,0.00018373186,0.00014092868],"domain_scores_gemma":[0.99908984,0.00011154008,0.00012999604,0.00005223278,0.00051296497,0.00010350053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038417816,0.00044582467,0.00031785225,0.0008665745,0.00095495465,0.0008085935,0.00048860034,0.0002444525,0.0004700448],"category_scores_gemma":[0.0013346634,0.00018490071,0.00033464207,0.0020448237,0.0006400845,0.000250042,0.00050663156,0.0003094731,0.0001063251],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013993277,0.00004981882,0.9607842,0.000056355402,0.0001421974,0.0006713561,0.0006572263,0.016088707,0.0042026397,0.00026544038,0.0012146623,0.015727468],"study_design_scores_gemma":[0.000006803054,0.000019643245,0.9842516,0.000009085903,0.00004715006,0.00004629846,0.00086479913,0.0131967915,0.0007018016,0.000031989275,0.00080779026,0.000016234675],"about_ca_topic_score_codex":0.9765672,"about_ca_topic_score_gemma":0.9803212,"teacher_disagreement_score":0.023432791,"about_ca_system_score_codex":0.0065324283,"about_ca_system_score_gemma":0.007690376,"threshold_uncertainty_score":0.047396302},"labels":[],"label_agreement":null},{"id":"W4408131290","doi":"10.1093/gji/ggaf080","title":"MTUQ: a framework for estimating moment tensors, point forces, and their uncertainties","year":2025,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Geological Survey of Canada","funders":"Air Force Research Laboratory; University of Alaska Fairbanks; National Nuclear Security Administration; National Science Foundation","keywords":"Moment (physics); Inverse theory; Moment tensor; Point (geometry); Geology; Geophysics; Geodesy; Statistical physics; Mathematics; Classical mechanics; Geometry; Physics; Deformation (meteorology)","score_opus":0.014339425937532915,"score_gpt":0.26021415280987037,"score_spread":0.24587472687233747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408131290","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005553312,0.00004584258,0.97515976,0.00008801913,0.000029841773,0.00004180595,0.0018889904,0.020909173,0.0012811369],"genre_scores_gemma":[0.03893351,0.00024503324,0.9321433,0.00026966023,0.00008330931,0.000683121,0.00630731,0.016999986,0.004334785],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989281,0.00019172237,0.00009875509,0.00015667366,0.00052278524,0.00010194813],"domain_scores_gemma":[0.9986708,0.0004554902,0.00012795991,0.00021509062,0.00044001997,0.00009058309],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001912328,0.0015588491,0.0010768874,0.0018171931,0.0009803062,0.0029787025,0.004103414,0.0010969851,0.027759746],"category_scores_gemma":[0.0075785182,0.0014969932,0.0021058454,0.0014700902,0.001199329,0.002405956,0.0041565793,0.0023256484,0.00981351],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001766557,0.00009075851,0.0035655578,0.0008741827,0.0002668373,0.0005246279,0.00044351682,0.43038675,0.0076003997,0.1602009,0.1380063,0.2578635],"study_design_scores_gemma":[0.00004283364,0.000015784266,0.00047148086,0.00008988052,0.000014857019,0.00013545396,0.000044914275,0.870164,0.0040666894,0.07269342,0.052193478,0.000067122775],"about_ca_topic_score_codex":0.011785582,"about_ca_topic_score_gemma":0.011578602,"teacher_disagreement_score":0.027759746,"about_ca_system_score_codex":0.00094723445,"about_ca_system_score_gemma":0.0035340388,"threshold_uncertainty_score":0.092865646},"labels":[],"label_agreement":null},{"id":"W4408427573","doi":"10.5194/egusphere-egu25-11648","title":"Numerical simulations of gravitational perturbations due to pre-seismic deep slab deformations before the 2011 Mw 9.1 Tohoku earthquake","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University; Geological Survey of Canada","funders":"","keywords":"Slab; Geology; Seismology; Geodesy; Geophysics","score_opus":0.015982847780410057,"score_gpt":0.24808095715994635,"score_spread":0.2320981093795363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408427573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9773286,0.00012580708,0.014303331,0.00022292278,0.00003662885,0.00003093508,0.00052552985,0.00019888087,0.0072273286],"genre_scores_gemma":[0.9935097,0.00007065546,0.0050863223,0.000027272701,0.0000071081067,0.00002751821,0.00030141973,0.00002613053,0.00094379124],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998977,0.000030624786,0.0000073871497,0.000015287755,0.000021136633,0.000027818154],"domain_scores_gemma":[0.9995208,0.00026887358,0.00007956555,0.00003135506,0.000053397005,0.00004598476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025557843,0.0004971699,0.00039886674,0.00037681367,0.0003505158,0.0005482508,0.00063408224,0.0012873361,0.0015054353],"category_scores_gemma":[0.001104867,0.00024346719,0.0004149614,0.00047286367,0.0006343346,0.0003390984,0.00059954985,0.0004374956,0.00013109454],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035788053,0.000037886333,0.0018742848,0.000017459295,0.0000103885395,0.000065067354,0.00002648234,0.9953413,0.0010277719,0.00051899033,0.00009181465,0.00095275394],"study_design_scores_gemma":[0.000009017706,0.000014173861,0.0006338859,0.0000025970996,0.0000030595122,0.000006406023,0.000019069925,0.9988403,0.00025076806,0.0001251423,0.000092405186,0.000003200946],"about_ca_topic_score_codex":0.016497102,"about_ca_topic_score_gemma":0.011047767,"teacher_disagreement_score":0.016497102,"about_ca_system_score_codex":0.00045604957,"about_ca_system_score_gemma":0.0006007665,"threshold_uncertainty_score":0.032802165},"labels":[],"label_agreement":null},{"id":"W4408428162","doi":"10.5194/egusphere-egu25-13084","title":"A Thin and Weak Lithosphere-Asthenosphere Boundary (LAB) Beneath the Oceanic Lithosphere and its Effects on Subduction Earthquake Cycle Deformation&amp;#160;","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Asthenosphere; Lithosphere; Subduction; Seismology; Slab; Geophysics; Convergent boundary; Mantle (geology); Intraplate earthquake; Lithospheric flexure; Plate tectonics; Oceanic crust; Tectonics","score_opus":0.011642633678624377,"score_gpt":0.22028641689655187,"score_spread":0.2086437832179275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408428162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99832505,0.00042645918,0.00024086385,0.00005418473,0.000003587694,0.0000017562701,0.000099949655,0.000012202086,0.0008359119],"genre_scores_gemma":[0.99958616,0.00011616186,0.00008649615,0.000007752241,0.0000023182142,8.980103e-7,0.000043605713,0.0000016942101,0.00015487059],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996555,0.0000036914853,0.0000040611917,0.000008933263,0.000008108757,0.0000097194825],"domain_scores_gemma":[0.9998661,0.000016580603,0.00006757622,0.000010217635,0.000011392694,0.00002801698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007432325,0.00023503136,0.00011286655,0.0003005347,0.0001557272,0.00037806458,0.00012171888,0.00018898657,0.0014824973],"category_scores_gemma":[0.00023815925,0.00011619125,0.00013322475,0.0002494843,0.0004646777,0.00018452434,0.00049526984,0.00017097268,0.00011836712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045527203,0.000060873546,0.5861544,0.00020008248,0.00011476255,0.0010335685,0.0002938818,0.0054639443,0.36469543,0.00097052613,0.00037277336,0.040184446],"study_design_scores_gemma":[0.0000072793423,0.000041385112,0.98986757,0.000010186146,0.000032354685,0.00010728894,0.0001430022,0.0018995723,0.007208952,0.00018385133,0.0004942738,0.000004257088],"about_ca_topic_score_codex":0.0036007054,"about_ca_topic_score_gemma":0.004391223,"teacher_disagreement_score":0.0036007054,"about_ca_system_score_codex":0.00019866702,"about_ca_system_score_gemma":0.00013628445,"threshold_uncertainty_score":0.007159531},"labels":[],"label_agreement":null},{"id":"W4408431046","doi":"10.5194/egusphere-egu25-14030","title":"A rapid tectonic plate reorganization event dynamically modelled by subduction cessation","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Subduction; Seismology; Geology; Plate tectonics; Tectonics; Event (particle physics); Physics","score_opus":0.011567554812991517,"score_gpt":0.2147121693871269,"score_spread":0.20314461457413538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408431046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9735318,0.00014550303,0.012364679,0.00049374846,0.000104957726,0.00009788922,0.0031221493,0.0005857931,0.009553581],"genre_scores_gemma":[0.99562114,0.000051223007,0.0020639852,0.000038244,0.000016830081,0.0000640337,0.0006860475,0.000049267775,0.001409324],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986136,0.000029150307,0.000011038461,0.000039017355,0.000016429121,0.000042909393],"domain_scores_gemma":[0.9995333,0.0001575849,0.000068485424,0.000059696118,0.000054845685,0.00012609642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035310857,0.0005788554,0.0005560849,0.0006364144,0.0004178631,0.0012022898,0.0016477831,0.001795832,0.006875766],"category_scores_gemma":[0.0014194457,0.00036150886,0.0011396518,0.0005862061,0.0007601134,0.0005804435,0.0008506617,0.0011955372,0.00054559717],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001897007,0.00010214435,0.0146151595,0.000055891596,0.000059611877,0.000471208,0.00014352406,0.975111,0.0023771562,0.0037816258,0.0009780516,0.002114858],"study_design_scores_gemma":[0.000042985757,0.000027965816,0.0049513336,0.000008250164,0.000015775724,0.00004270818,0.00005073812,0.9930861,0.0002865429,0.000970584,0.00050065987,0.000016424194],"about_ca_topic_score_codex":0.022088582,"about_ca_topic_score_gemma":0.0134287225,"teacher_disagreement_score":0.022088582,"about_ca_system_score_codex":0.00084674486,"about_ca_system_score_gemma":0.00062403805,"threshold_uncertainty_score":0.04392004},"labels":[],"label_agreement":null},{"id":"W4408435820","doi":"10.5194/egusphere-egu25-7389","title":"Cluster analysis can identify differences in earthquake swarm patterns along the Mid-Atlantic Ridge","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Ridge; Mid-Atlantic Ridge; Seismology; Cluster (spacecraft); Geology; Swarm behaviour; Geography; Computer science; Paleontology; Artificial intelligence","score_opus":0.028319762610294424,"score_gpt":0.2539777602180305,"score_spread":0.22565799760773605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408435820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91696596,0.0007501417,0.058233544,0.00042026376,0.00008840579,0.000395384,0.009877773,0.0022063225,0.011062301],"genre_scores_gemma":[0.9409098,0.00031801645,0.046159264,0.000056566052,0.000041104435,0.00022772413,0.009956168,0.00015930003,0.0021720368],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99917465,0.00008983857,0.000117870375,0.00030538195,0.00020946101,0.00010263233],"domain_scores_gemma":[0.9972549,0.0009002446,0.0005862477,0.00028388423,0.000789993,0.00018476453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010212361,0.0003647439,0.00047250278,0.0067273085,0.00070925563,0.001425879,0.000528696,0.00039136404,0.0023632126],"category_scores_gemma":[0.0037364427,0.0001502837,0.00079595554,0.0048899073,0.00028910767,0.000552648,0.0008521212,0.00029479884,0.0007063558],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082905113,0.00036271306,0.6105638,0.0005471056,0.0010233675,0.0008236158,0.003998687,0.015035309,0.030922309,0.003754614,0.018319925,0.31381944],"study_design_scores_gemma":[0.000042652166,0.00017324513,0.914981,0.000083730025,0.0002064182,0.00031790385,0.0033045106,0.06203854,0.0045352825,0.002615638,0.011610936,0.00009010437],"about_ca_topic_score_codex":0.016679134,"about_ca_topic_score_gemma":0.022441372,"teacher_disagreement_score":0.016679134,"about_ca_system_score_codex":0.00058689935,"about_ca_system_score_gemma":0.0007455183,"threshold_uncertainty_score":0.033164084},"labels":[],"label_agreement":null},{"id":"W4408456718","doi":"10.1029/2024jb030903","title":"On Dislocation Modeling of Megathrust Tsunami Sources","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico","keywords":"Dislocation; Seismology; Geology; Materials science; Composite material","score_opus":0.04435415420441634,"score_gpt":0.33545435924199496,"score_spread":0.2911002050375786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408456718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.69859725,0.0005742222,0.2918208,0.00038913317,0.000058915808,0.00005920125,0.0003538176,0.00055975374,0.0075869435],"genre_scores_gemma":[0.99086654,0.00016963166,0.007380451,0.000016727952,0.000005731925,0.000014437912,0.000088993314,0.000032648637,0.0014247542],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989545,0.000034972254,0.00000894133,0.000016586595,0.000027561207,0.000016450296],"domain_scores_gemma":[0.99972266,0.000106443455,0.000043878917,0.000032198008,0.000072934796,0.000021845848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025052548,0.0004734094,0.0004754034,0.00066258595,0.0002514338,0.0008691293,0.0007507138,0.00083549303,0.0010701774],"category_scores_gemma":[0.0010348058,0.00023645053,0.00048621395,0.00052846957,0.00040158667,0.00047591035,0.00036754433,0.00033595765,0.00024235295],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011389771,0.000019888206,0.0012670277,0.000009344699,0.000008188768,0.000038338556,0.00002381351,0.99407494,0.00088934164,0.0011426099,0.00005965151,0.0024555204],"study_design_scores_gemma":[8.2650035e-7,0.0000035887879,0.00011799653,0.0000013584257,8.965529e-7,0.000003746469,0.000005119815,0.999466,0.00013555308,0.00018602272,0.000077775105,0.0000011781402],"about_ca_topic_score_codex":0.016678322,"about_ca_topic_score_gemma":0.009949914,"teacher_disagreement_score":0.016678322,"about_ca_system_score_codex":0.00097343896,"about_ca_system_score_gemma":0.0007321998,"threshold_uncertainty_score":0.033162534},"labels":[],"label_agreement":null},{"id":"W4408472092","doi":"10.1007/s40789-025-00769-2","title":"Contemporary stress state in the Zhao–Ping metallogenic belt, eastern China, and its correlation to regional geological tectonics","year":2025,"lang":"en","type":"article","venue":"International Journal of Coal Science & Technology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Geology; Tectonics; Ping (video games); China; Seismology; Geochemistry; Mining engineering; Archaeology; Geography","score_opus":0.020822048888720256,"score_gpt":0.27172764703214386,"score_spread":0.2509055981434236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408472092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997472,0.000037056845,0.000022247417,0.000009757039,3.9642646e-7,9.2087043e-7,0.000031105814,0.0000011768052,0.00015017459],"genre_scores_gemma":[0.9998554,0.000027192453,0.000015743968,0.000001351892,0.000001214612,8.7195775e-7,0.000047798123,1.9959282e-7,0.000050337672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998758,0.000012462506,0.000017020066,0.00003315819,0.00003194691,0.000029630744],"domain_scores_gemma":[0.99961674,0.000044742297,0.0001651078,0.000025250318,0.00008134471,0.00006671022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026426656,0.00019514201,0.00016019228,0.0018918882,0.00035548097,0.00045607256,0.00023022755,0.00018838116,0.00055294094],"category_scores_gemma":[0.0005052769,0.00013195211,0.00010924533,0.002266276,0.00059767364,0.0003537347,0.00037382788,0.000095418196,0.00005641169],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030186231,0.000007447436,0.9924615,0.000013366296,0.000021617447,0.00020575183,0.0007244357,0.0002945171,0.0016929794,0.00010577761,0.000027844764,0.0044147247],"study_design_scores_gemma":[6.2274637e-7,0.000007653541,0.999468,0.0000013738791,0.0000023440402,0.000027138221,0.00018210421,0.00016601014,0.000046586072,0.000019810792,0.00007711807,0.0000013089594],"about_ca_topic_score_codex":0.021363549,"about_ca_topic_score_gemma":0.037166517,"teacher_disagreement_score":0.021363549,"about_ca_system_score_codex":0.00089890923,"about_ca_system_score_gemma":0.00036909175,"threshold_uncertainty_score":0.042478442},"labels":[],"label_agreement":null},{"id":"W4408486287","doi":"10.5194/egusphere-egu25-17785","title":"Extreme flood event and their depositonal signatures: the case of the Storm Alex in the Roya Valley","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Musée de la Civilisation","funders":"","keywords":"Flood myth; Storm; Event (particle physics); History; Geography; Hydrology (agriculture); Meteorology; Geology; Archaeology; Geotechnical engineering; Physics","score_opus":0.02273222242772658,"score_gpt":0.22440856521606908,"score_spread":0.2016763427883425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408486287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982496,0.000055092303,0.00004637817,0.000057049656,0.000002209913,0.0000038091857,0.00024093364,0.000005078548,0.0013398025],"genre_scores_gemma":[0.9993019,0.000060579794,0.00012962669,0.000012338075,0.0000064143037,0.0000026443968,0.00022696255,0.0000034123566,0.00025614665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985695,0.000019189396,0.000010640308,0.000029039109,0.000040274845,0.000043927812],"domain_scores_gemma":[0.9997615,0.00002821269,0.00008028544,0.000019186393,0.000047476,0.00006334611],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001730669,0.000114231916,0.00019392336,0.001038167,0.00061406917,0.00087468646,0.00029373777,0.00028565462,0.00081445504],"category_scores_gemma":[0.00048753587,0.00011436794,0.00018296801,0.0012201559,0.00064166554,0.0002899424,0.00094965805,0.0002571324,0.00012348521],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009025434,0.000026768994,0.98015594,0.000036607235,0.00004141803,0.0038034187,0.0040477416,0.0004624123,0.002885519,0.00029250383,0.00059548527,0.007562036],"study_design_scores_gemma":[0.0000017806593,0.00001035815,0.9964401,0.000006102974,0.0000047871918,0.00033157444,0.002024999,0.0003038815,0.00007106119,0.00004713227,0.000753033,0.000005061232],"about_ca_topic_score_codex":0.059190083,"about_ca_topic_score_gemma":0.1168491,"teacher_disagreement_score":0.059190083,"about_ca_system_score_codex":0.0005610743,"about_ca_system_score_gemma":0.00053704315,"threshold_uncertainty_score":0.11769116},"labels":[],"label_agreement":null},{"id":"W4408541178","doi":"10.1016/j.oceaneng.2025.120892","title":"The Noto Peninsula tsunami of 1 January 2024 as observed in the northern Sea of Japan","year":2025,"lang":"en","type":"article","venue":"Ocean Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Russian Academy of Sciences; Russian Science Foundation","keywords":"Peninsula; Geology; Oceanography; Climatology; Geography; Seismology; Archaeology","score_opus":0.009975876758623816,"score_gpt":0.19583375064989325,"score_spread":0.18585787389126943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408541178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99671626,0.00015647023,0.000047512473,0.00021409884,0.000082884326,0.000010861662,0.0007119158,0.0000058777005,0.0020539584],"genre_scores_gemma":[0.9972583,0.00021639215,0.00007064554,0.000060826318,0.00004528586,0.000012802903,0.0012592964,0.0000023738958,0.0010740273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990153,0.000009644736,0.00000998961,0.0000156057,0.00002020568,0.000042959964],"domain_scores_gemma":[0.99964106,0.000016734888,0.00013751081,0.000015686675,0.000093919036,0.00009505748],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019878583,0.00044106727,0.00019335213,0.0007765682,0.00082204904,0.0006521536,0.00023700285,0.00081887917,0.0013092085],"category_scores_gemma":[0.0005866297,0.00015932399,0.00019514983,0.0009392013,0.0003127446,0.0005389572,0.0006746019,0.00043810072,0.00028555578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002779152,0.00009296893,0.97809803,0.00008579234,0.00009040959,0.002571237,0.0017117484,0.0008794222,0.005304798,0.0002203217,0.0037916654,0.006875707],"study_design_scores_gemma":[0.0000031553384,0.000036418947,0.9968317,0.000012526371,0.000016606413,0.00013979687,0.0011596087,0.00027795645,0.000094493655,0.000027952976,0.0013933496,0.000006542117],"about_ca_topic_score_codex":0.057861224,"about_ca_topic_score_gemma":0.15142585,"teacher_disagreement_score":0.057861224,"about_ca_system_score_codex":0.0008831671,"about_ca_system_score_gemma":0.0010140386,"threshold_uncertainty_score":0.115048826},"labels":[],"label_agreement":null},{"id":"W4408549139","doi":"10.1038/s43247-025-02156-w","title":"Internal volcano-magmatic structure of Öræfajökull volcano, Iceland","year":2025,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Volcano; Geology; Seismology","score_opus":0.011637343030758081,"score_gpt":0.21775315082037988,"score_spread":0.2061158077896218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408549139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99473816,0.00019918746,0.000425362,0.00007153905,0.00000483724,0.000009262216,0.001014235,0.00002867729,0.003508703],"genre_scores_gemma":[0.9985922,0.000080134734,0.0003278919,0.000009651453,0.0000031435263,0.000004592314,0.00059775345,0.0000060690095,0.0003785436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994576,0.0000052550777,0.000003299007,0.000018296703,0.0000064019005,0.000020966074],"domain_scores_gemma":[0.9999341,0.000007922097,0.000020679481,0.0000042707134,0.000014442995,0.000018633993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111669055,0.00024783352,0.00018231357,0.00061482727,0.00033064507,0.0011242186,0.00031073284,0.00030626994,0.0016302235],"category_scores_gemma":[0.00019155363,0.00012165936,0.00018363657,0.00057481934,0.00049839454,0.00031918412,0.0005931513,0.00016379078,0.00025445316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013849881,0.00010165892,0.90938795,0.00015007087,0.00008507784,0.0007481179,0.001259091,0.060336478,0.005917009,0.0018131678,0.0014855156,0.01857741],"study_design_scores_gemma":[0.000008035989,0.000025594496,0.96304375,0.00006423958,0.000020333679,0.00010201475,0.001317282,0.033256475,0.0002589979,0.00017392194,0.0017164523,0.000012915385],"about_ca_topic_score_codex":0.08050646,"about_ca_topic_score_gemma":0.091176406,"teacher_disagreement_score":0.08050646,"about_ca_system_score_codex":0.0012649213,"about_ca_system_score_gemma":0.0010538674,"threshold_uncertainty_score":0.16007566},"labels":[],"label_agreement":null},{"id":"W4408651813","doi":"10.3390/rs17061096","title":"Geodetic Observations and Seismogenic Structures of the 2025 Mw 7.0 Dingri Earthquake: The Largest Normal Faulting Event in the Southern Tibet Rift","year":2025,"lang":"en","type":"article","venue":"Remote Sensing","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Natural Science Foundation of China","keywords":"Geology; Seismology; Geodetic datum; Rift; Normal fault; Foreshock; Geodesy; Fault (geology); Tectonics; Aftershock","score_opus":0.02264113901834077,"score_gpt":0.23739838671231442,"score_spread":0.21475724769397364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408651813","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988147,0.000038244005,0.00005573004,0.000012190654,0.000002661606,0.0000034962302,0.00063716486,0.0000044264316,0.00043145104],"genre_scores_gemma":[0.99820244,0.000030721807,0.00007640785,0.0000055803143,0.0000057333054,0.0000044347767,0.0015321729,8.0209253e-7,0.00014171236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999211,0.000009639921,0.0000075260878,0.000020103014,0.0000177967,0.000023896744],"domain_scores_gemma":[0.99985063,0.000009754411,0.00004457608,0.000008018267,0.00003730379,0.000049631228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016781877,0.00026640447,0.00013963328,0.001017391,0.00020670195,0.00028741884,0.00017764128,0.0002535951,0.000594355],"category_scores_gemma":[0.00028321779,0.000089254565,0.0001268167,0.00096022023,0.00017112959,0.00012624793,0.00023487501,0.00010371744,0.00016256844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012742337,0.00006737826,0.97351336,0.00005675317,0.000042440424,0.00054415024,0.00044985718,0.0028584737,0.012177564,0.00015275281,0.00055405084,0.009455873],"study_design_scores_gemma":[0.000005434451,0.000020896732,0.9974534,0.000005687402,0.000008702494,0.000044861386,0.00014080168,0.0018235729,0.00019933042,0.000015737094,0.00027759533,0.000004034357],"about_ca_topic_score_codex":0.0228353,"about_ca_topic_score_gemma":0.03604401,"teacher_disagreement_score":0.0228353,"about_ca_system_score_codex":0.00039765507,"about_ca_system_score_gemma":0.0003174867,"threshold_uncertainty_score":0.04540479},"labels":[],"label_agreement":null},{"id":"W4408652762","doi":"10.5194/egusphere-2025-390-rc1","title":"Report on &amp;amp;#8220;Characterizing some major Archean faults at depth in the Superior craton, North America&amp;amp;#8221; by David Snyder et al.","year":2025,"lang":"en","type":"peer-review","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"","keywords":"Archean; Geology; Geochemistry","score_opus":0.04987322713368319,"score_gpt":0.30825330268488177,"score_spread":0.2583800755511986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408652762","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.45342058,0.004414196,0.007170656,0.0053682225,0.0010985944,0.0014622076,0.16696835,0.001424744,0.35867247],"genre_scores_gemma":[0.4343975,0.0031398803,0.016432744,0.0013125293,0.00071504654,0.00048314364,0.12466398,0.00043051262,0.4184248],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997584,0.000016664717,0.000016582913,0.000046284484,0.00013392796,0.000028106255],"domain_scores_gemma":[0.9989248,0.000055142184,0.00013572915,0.00008800409,0.0005739912,0.00022227727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036648332,0.00023029189,0.000088029934,0.0016650662,0.00089373253,0.00042897306,0.00033700003,0.00033414032,0.021584552],"category_scores_gemma":[0.0004779803,0.0001382819,0.0000885651,0.0017103944,0.00028821433,0.00033090205,0.0008921968,0.00027087633,0.005050113],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017657196,0.00016818226,0.24005963,0.00047484896,0.000031881355,0.00092594244,0.0022854982,0.0004991204,0.04430946,0.0006358886,0.46641645,0.24401654],"study_design_scores_gemma":[0.00000961551,0.00006470936,0.63727784,0.00003883256,0.000009631222,0.00019330572,0.0007690615,0.00018330097,0.0038958997,0.00013626319,0.3574099,0.0000116196425],"about_ca_topic_score_codex":0.0451985,"about_ca_topic_score_gemma":0.25066632,"teacher_disagreement_score":0.0451985,"about_ca_system_score_codex":0.0004505101,"about_ca_system_score_gemma":0.00092187885,"threshold_uncertainty_score":0.08987081},"labels":[],"label_agreement":null},{"id":"W4408731359","doi":"10.1007/978-981-16-7408-2_1-2","title":"Earthquake Characteristics and Seismology Basics","year":2025,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal; Golder Associates (Canada)","funders":"","keywords":"Seismology; Geology","score_opus":0.015668184663371266,"score_gpt":0.20116963602655757,"score_spread":0.1855014513631863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408731359","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.003349789,0.033095546,0.040509086,0.0016007901,0.0013634298,0.000090575806,0.0015493743,0.00036272258,0.91807866],"genre_scores_gemma":[0.035995845,0.043147027,0.017118143,0.0006775714,0.0020976586,0.00011524762,0.002206076,0.00034617522,0.89829624],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99991155,0.000013353923,0.000007356698,0.000017571288,0.00004324328,0.0000068814747],"domain_scores_gemma":[0.9998235,0.00007700914,0.000010414136,0.000018478546,0.000060794984,0.000009902055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018010286,0.00057647354,0.00041111416,0.0013380706,0.00028755944,0.0012699014,0.0006916381,0.00041780336,0.034212224],"category_scores_gemma":[0.00061343506,0.00025421844,0.00019967086,0.0019275518,0.00061248307,0.001417306,0.000400765,0.00081377826,0.01764576],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034221688,0.000057044388,0.0007006506,0.00055831316,0.000006402144,0.00019814713,0.0004774319,0.00256392,0.0024799097,0.31390116,0.15645581,0.52256703],"study_design_scores_gemma":[0.0000023726282,0.000023356224,0.0018233744,0.00011251722,0.0000054297725,0.00044228125,0.00010579221,0.0008755874,0.00039636667,0.07953296,0.9166703,0.000009586006],"about_ca_topic_score_codex":0.0014230974,"about_ca_topic_score_gemma":0.001866147,"teacher_disagreement_score":0.034212224,"about_ca_system_score_codex":0.00037899974,"about_ca_system_score_gemma":0.00037471004,"threshold_uncertainty_score":0.11445129},"labels":[],"label_agreement":null},{"id":"W4409259777","doi":"10.1016/j.epsl.2025.119348","title":"Modeling earthquake-induced seiche processes and subsequent homogenite deposition in lacustrine settings","year":2025,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"Ministère de l'Enseignement supérieur, de la Recherche et de l'Innovation","keywords":"Seiche; Geology; Deposition (geology); Seismology; Geophysics; Geochemistry; Geomorphology; Sediment","score_opus":0.013327215029439388,"score_gpt":0.21099761497426517,"score_spread":0.19767039994482577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409259777","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9817052,0.00013471553,0.01527867,0.000087613764,0.000009482919,0.000040298197,0.00021718392,0.0003039619,0.0022229294],"genre_scores_gemma":[0.9953153,0.00006921614,0.0037547024,0.000008555636,0.000004369799,0.000026819269,0.000115937,0.000019302424,0.0006857428],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991965,0.000015144747,0.0000064576493,0.000022277116,0.000009385069,0.00002711095],"domain_scores_gemma":[0.9997781,0.000091229136,0.00005101727,0.00001618064,0.00003154888,0.00003186298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019015241,0.00067733723,0.00042989576,0.00062339066,0.00040414385,0.0008519832,0.00090524426,0.0013544172,0.0013078881],"category_scores_gemma":[0.00072619616,0.00043103017,0.0005246021,0.00047981492,0.00045595478,0.00040275697,0.00066385197,0.00036299127,0.00010413982],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020492875,0.00003949495,0.0046257577,0.000015646878,0.000021316922,0.0001180071,0.00003156635,0.99144405,0.0019843045,0.00031733437,0.000045411784,0.0013365799],"study_design_scores_gemma":[0.000007988367,0.000012318431,0.0011371423,0.0000014206574,0.0000050985273,0.0000068387517,0.000013007073,0.9984686,0.00019748702,0.00008985542,0.000056761648,0.0000035042199],"about_ca_topic_score_codex":0.05094669,"about_ca_topic_score_gemma":0.04453225,"teacher_disagreement_score":0.05094669,"about_ca_system_score_codex":0.0010434212,"about_ca_system_score_gemma":0.0008674452,"threshold_uncertainty_score":0.1013003},"labels":[],"label_agreement":null},{"id":"W4409332983","doi":"10.1785/0120250004","title":"Earthquake Declustering Using Supervised Machine Learning","year":2025,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Computer science; Seismology; Machine learning; Artificial intelligence","score_opus":0.020410197207660657,"score_gpt":0.22426632408527106,"score_spread":0.2038561268776104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409332983","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6390279,0.00032420937,0.35355774,0.00033215695,0.00007802191,0.00014363036,0.00061290845,0.0034232922,0.0025001776],"genre_scores_gemma":[0.9617744,0.000024746663,0.036820572,0.000035379268,0.000022940047,0.00003095033,0.0007186984,0.000024930292,0.0005473968],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994363,0.00019548704,0.000048198668,0.00016539475,0.000099482124,0.000055006403],"domain_scores_gemma":[0.99645597,0.0017302335,0.0005717405,0.00043655798,0.0006562267,0.00014934043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013602711,0.00047470085,0.0006135564,0.0015041914,0.00031685864,0.00048463742,0.00081946346,0.0004065603,0.00085497915],"category_scores_gemma":[0.0040968056,0.00017879819,0.00048377368,0.00071557984,0.00034509442,0.0005781612,0.0006271056,0.0005811814,0.00030858183],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002890685,0.0003967656,0.04035239,0.00008646917,0.00008899824,0.00012846521,0.00010226728,0.70547044,0.002373007,0.0014457969,0.002370574,0.24689569],"study_design_scores_gemma":[0.0000036113167,0.000015555732,0.0010365234,0.0000020444068,0.0000018654572,0.0000067479996,0.000005934622,0.9979697,0.000366828,0.0005050657,0.00008350777,0.0000026331334],"about_ca_topic_score_codex":0.0052452497,"about_ca_topic_score_gemma":0.004933147,"teacher_disagreement_score":0.0052452497,"about_ca_system_score_codex":0.00067881064,"about_ca_system_score_gemma":0.00088840997,"threshold_uncertainty_score":0.010429442},"labels":[],"label_agreement":null},{"id":"W4409433063","doi":"10.1785/0120230179","title":"An Integrated Earthquake Catalog for Aotearoa New Zealand (Version 1), Event-Type Classifications, and Regional Earthquake Depth Distributions","year":2025,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society","funders":"","keywords":"Seismology; Geology; Event (particle physics); Type (biology); Types of earthquake; Foreshock; Aftershock; Paleontology","score_opus":0.020168218636690313,"score_gpt":0.2469293552753325,"score_spread":0.22676113663864217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409433063","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10800073,0.0005429639,0.0060536107,0.00024320648,0.0001270695,0.001544066,0.84809047,0.0018858425,0.033512082],"genre_scores_gemma":[0.106602274,0.0009887317,0.019264653,0.00012690997,0.00006905637,0.0017089342,0.84633374,0.00077679195,0.0241288],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99907076,0.000034007615,0.00021047362,0.0001676233,0.000392578,0.00012461102],"domain_scores_gemma":[0.99301046,0.00021530506,0.0012477199,0.00092899386,0.00401094,0.000586564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012120018,0.0008921981,0.00054197776,0.011757343,0.00067198736,0.0012195709,0.0010211626,0.000288335,0.021499658],"category_scores_gemma":[0.006126813,0.0006697314,0.00048000406,0.012678742,0.00032168793,0.0012621586,0.0013886145,0.0005867601,0.010643539],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042364193,0.000117929914,0.32519493,0.0016228367,0.00016688449,0.0007061009,0.0033033425,0.0024659012,0.009921692,0.002396824,0.39952353,0.2541563],"study_design_scores_gemma":[0.00004586326,0.000038087885,0.73988336,0.00015197931,0.000055271656,0.0002972499,0.0005249824,0.0012039541,0.000742829,0.00025804472,0.25673878,0.000059605132],"about_ca_topic_score_codex":0.5870306,"about_ca_topic_score_gemma":0.61210656,"teacher_disagreement_score":0.5870306,"about_ca_system_score_codex":0.002646084,"about_ca_system_score_gemma":0.0058186245,"threshold_uncertainty_score":0.8308029},"labels":[],"label_agreement":null},{"id":"W4409436319","doi":"10.3390/mining5020027","title":"An Induced Seismicity Indicator Using Accumulated Microearthquakes’ Frictional Energy","year":2025,"lang":"en","type":"article","venue":"Mining","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Comisión Nacional de Investigación Científica y Tecnológica","keywords":"Induced seismicity; Seismology; Geology; Microseism; Energy (signal processing); Physics","score_opus":0.03288976013322765,"score_gpt":0.2719801237616261,"score_spread":0.23909036362839847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409436319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9802294,0.00012740793,0.016364716,0.000039380895,0.00002319145,0.00004332039,0.0009076187,0.00018664742,0.002078446],"genre_scores_gemma":[0.99604744,0.000061445855,0.0029259883,0.0000030271833,0.000006773366,0.000010227487,0.000549611,0.0000054514876,0.00039009732],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997787,0.00002441542,0.000026166632,0.000045211582,0.00009013246,0.00003542628],"domain_scores_gemma":[0.99917597,0.00024128788,0.0002676632,0.000060948398,0.00017141836,0.00008270757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042662086,0.00062227645,0.0002986356,0.0023800228,0.00013205394,0.00049988396,0.00028858526,0.00035563097,0.0012363213],"category_scores_gemma":[0.0020812252,0.00014545424,0.0003599505,0.0011769986,0.00016491693,0.0004949393,0.00046605995,0.00027626165,0.00038065814],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035735776,0.00015382624,0.77804595,0.00022333529,0.00015270154,0.00060739747,0.00027750005,0.09749374,0.015971534,0.00040877442,0.00081901444,0.10548887],"study_design_scores_gemma":[0.000013276507,0.00038383208,0.7483448,0.000047396516,0.00007575096,0.00028632017,0.00048034143,0.2413704,0.007016776,0.00043595204,0.0014955914,0.00004963011],"about_ca_topic_score_codex":0.0039533037,"about_ca_topic_score_gemma":0.007728898,"teacher_disagreement_score":0.0039533037,"about_ca_system_score_codex":0.00023012924,"about_ca_system_score_gemma":0.0003097529,"threshold_uncertainty_score":0.007860601},"labels":[],"label_agreement":null},{"id":"W4409442399","doi":"10.3390/geosciences15040146","title":"Comparison of Backprojection Techniques for Rupture Propagation Modelling of the Mw = 7.8 Mainshock Earthquake near Kahramanmaras and the Mw = 7.5 Second-Largest Mainshock near Elbistan, Turkey, 2023","year":2025,"lang":"en","type":"article","venue":"Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology","score_opus":0.02521574048188342,"score_gpt":0.26185038127993593,"score_spread":0.23663464079805252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409442399","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.39231908,0.0006831125,0.6037435,0.0002067284,0.00006882674,0.00008483363,0.0002072938,0.0011754044,0.0015112411],"genre_scores_gemma":[0.8170605,0.0007798753,0.17985342,0.000044906425,0.000028654336,0.000084960666,0.00045071024,0.0001358258,0.0015611495],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997323,0.00008455609,0.000025252803,0.000059876733,0.000053320266,0.0000447316],"domain_scores_gemma":[0.9993963,0.00031653818,0.000051103678,0.000028376884,0.00017862215,0.000029061404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013434554,0.0012928939,0.00048648327,0.0008156065,0.00023967291,0.0009874757,0.00063684094,0.000807167,0.0011300875],"category_scores_gemma":[0.0017365415,0.00046909656,0.00095991837,0.00054786244,0.00028858168,0.0008509832,0.0005453658,0.000561242,0.00051102816],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031411485,0.00011271683,0.005154314,0.00007881918,0.000093483504,0.00012909781,0.00014439695,0.87602913,0.008336462,0.0007091238,0.0003266399,0.10857168],"study_design_scores_gemma":[0.0000037168088,0.000026616506,0.00058915536,0.0000036544213,0.000006500827,0.000011693656,0.000013554365,0.9981939,0.0009940201,0.00008471415,0.000068354006,0.0000040702553],"about_ca_topic_score_codex":0.013370533,"about_ca_topic_score_gemma":0.0066100396,"teacher_disagreement_score":0.013370533,"about_ca_system_score_codex":0.00027742778,"about_ca_system_score_gemma":0.0007193883,"threshold_uncertainty_score":0.02658546},"labels":[],"label_agreement":null},{"id":"W4409605254","doi":"10.1016/j.tecto.2025.230752","title":"Tectonic tremor source depths in relation to subduction zone structure in northern Cascadia","year":2025,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Tectonics; Seismology; Episodic tremor and slip; Paleontology","score_opus":0.007229738048359096,"score_gpt":0.20850141279853354,"score_spread":0.20127167475017443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409605254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99885976,0.000046811943,0.000030110854,0.00003123431,0.0000016618304,0.0000013084436,0.00020259929,0.000008935698,0.0008177173],"genre_scores_gemma":[0.9993643,0.000029450794,0.000021004342,0.000003943119,0.000001664323,0.0000019840884,0.00015212709,0.0000030262684,0.00042262566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998654,0.000017892333,0.000013118504,0.000050171962,0.000020951178,0.00003245638],"domain_scores_gemma":[0.9990025,0.00020626208,0.00022928294,0.000063662716,0.00020441583,0.00029392005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025975367,0.00038183972,0.000319192,0.002086582,0.0007231609,0.00073228456,0.00035148332,0.0003649839,0.003247678],"category_scores_gemma":[0.0014720045,0.00037711087,0.0003663841,0.0020333321,0.00079442223,0.0003879788,0.000995996,0.00032292254,0.00046781788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028352722,0.000024114868,0.98816967,0.000034962373,0.000074417505,0.00026970272,0.0021439153,0.0013375607,0.0042472095,0.00012114466,0.00019541812,0.0030983337],"study_design_scores_gemma":[0.0000015634022,0.000004748669,0.9995505,0.0000017781343,0.0000046508835,0.000012270682,0.00024337081,0.00008654801,0.000027856058,0.000011383332,0.00005378303,0.0000015791724],"about_ca_topic_score_codex":0.2151035,"about_ca_topic_score_gemma":0.3473733,"teacher_disagreement_score":0.2151035,"about_ca_system_score_codex":0.001729738,"about_ca_system_score_gemma":0.0007900647,"threshold_uncertainty_score":0.4277029},"labels":[],"label_agreement":null},{"id":"W4409768177","doi":"10.1029/2024jb030654","title":"Subducted Slab Slipping Underneath the Northern Edge of the Pacific Large Low‐Shear‐Velocity Province in D″","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; U.S. Geological Survey; Institut de Physique du Globe de Paris; China Earthquake Administration; University of California, Santa Barbara; University of Nevada, Reno; University of Oregon; Natural Resources Canada; University of Washington; National Oceanic and Atmospheric Administration; Universiteit Utrecht; California Institute of Technology","keywords":"Slipping; Slab; Geology; Subduction; Seismology; Shear (geology); Enhanced Data Rates for GSM Evolution; Slab window; Geometry; Petrology; Geophysics; Oceanic crust; Engineering","score_opus":0.028332611472710628,"score_gpt":0.2994384194717878,"score_spread":0.27110580799907713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409768177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981445,0.000010090432,0.00057339907,0.000020713127,0.0000024092137,0.0000025601837,0.0002151036,0.00006879176,0.0009623708],"genre_scores_gemma":[0.9987565,0.000007920212,0.00055940106,0.000005048971,7.778737e-7,0.0000017232439,0.0004005083,0.000008114253,0.00025989258],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996936,0.0000017578798,0.0000012741577,0.000008700729,0.0000068183617,0.000012128434],"domain_scores_gemma":[0.9999461,0.0000064571673,0.000008955437,0.000005515912,0.000014954376,0.00001803111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000052079202,0.00020758915,0.0001370349,0.00045927352,0.00023833211,0.0003979732,0.00025625355,0.00016993721,0.0012199502],"category_scores_gemma":[0.00022850995,0.00019585482,0.00022793809,0.0003735623,0.00018096356,0.00014142712,0.0003304541,0.0002622028,0.00015284687],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007453907,0.00021770953,0.7250411,0.00007412543,0.00019663671,0.0011478906,0.000949989,0.058884766,0.15323885,0.00081300887,0.0014288337,0.057261746],"study_design_scores_gemma":[0.00005838426,0.00006038217,0.778271,0.000015696598,0.00006413522,0.00017749897,0.00067508547,0.20532197,0.013348427,0.00029277572,0.0016801747,0.000034442346],"about_ca_topic_score_codex":0.08003178,"about_ca_topic_score_gemma":0.07978105,"teacher_disagreement_score":0.08003178,"about_ca_system_score_codex":0.0003159564,"about_ca_system_score_gemma":0.0006100449,"threshold_uncertainty_score":0.15913188},"labels":[],"label_agreement":null},{"id":"W4409770967","doi":"10.1029/2025gl115446","title":"Downdip Variations in Megathrust Seismogenic Behavior in the Japan Trench Subduction Zone Affected by Mantle Wedge Serpentinite","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Subduction; Geology; Trench; Mantle wedge; Wedge (geometry); Seismology; Mantle (geology); Geochemistry; Tectonics; Materials science; Layer (electronics)","score_opus":0.026082513553771242,"score_gpt":0.2926193668716989,"score_spread":0.2665368533179277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409770967","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997403,0.000025899117,0.00002965039,0.000005104091,5.3989515e-7,8.713071e-7,0.000043070027,0.0000030444019,0.000151452],"genre_scores_gemma":[0.9998691,0.000012878738,0.000015976555,0.0000018602374,6.285014e-7,5.660449e-7,0.000046875026,7.837985e-7,0.000051335162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999211,0.0000063770703,0.00000812239,0.000025098136,0.000011269501,0.000027956943],"domain_scores_gemma":[0.99978155,0.000015334263,0.00008198073,0.000018332683,0.00004500458,0.00005773282],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010986965,0.00022342999,0.00020772974,0.0011236083,0.00027001795,0.0004244021,0.00020692933,0.00019194308,0.0008334138],"category_scores_gemma":[0.00033141224,0.00015807706,0.00014731666,0.00060621236,0.000355116,0.00025295274,0.00049828173,0.00013205457,0.00013467597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013473186,0.000013830134,0.980316,0.000017983633,0.000040099007,0.00043289296,0.0007732693,0.0006163844,0.01447483,0.000050412065,0.000050921397,0.003078651],"study_design_scores_gemma":[0.0000012915427,0.000007990428,0.9992872,0.0000014211687,0.0000045328793,0.00003636823,0.00021838697,0.00020947162,0.00017902437,0.000007926069,0.00004486006,0.00000149792],"about_ca_topic_score_codex":0.01586548,"about_ca_topic_score_gemma":0.022255182,"teacher_disagreement_score":0.01586548,"about_ca_system_score_codex":0.0003445052,"about_ca_system_score_gemma":0.00014823567,"threshold_uncertainty_score":0.031546235},"labels":[],"label_agreement":null},{"id":"W4409879589","doi":"10.1017/9781108682800.011","title":"Iapetus and Pangea","year":2025,"lang":"en","type":"book-chapter","venue":"Cambridge University Press eBooks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Geology; Astrobiology; Oceanography; Physics","score_opus":0.018070952616615163,"score_gpt":0.17385301091318847,"score_spread":0.15578205829657332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409879589","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0017019591,0.014666657,0.0011587507,0.002110712,0.0015665969,0.000021335523,0.00014449871,0.00023605858,0.9783934],"genre_scores_gemma":[0.02540266,0.012874369,0.003026259,0.0014914012,0.0007344095,0.00007790453,0.00037099136,0.00039346772,0.9556286],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99984217,0.00003923833,0.000006415997,0.000049747523,0.00003837264,0.000023995337],"domain_scores_gemma":[0.9999591,0.000008661251,0.0000038730263,0.00000857968,0.000007799092,0.00001208605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014906388,0.00069128646,0.0002826532,0.0012984544,0.0014051221,0.0031723764,0.00038430342,0.0009463261,0.07469447],"category_scores_gemma":[0.0003505318,0.00019481481,0.00020829559,0.001448254,0.0015464203,0.0028279584,0.0019645295,0.0018395196,0.025244795],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004427818,0.00002724156,0.0004172152,0.00035876324,0.0000072846556,0.0002978538,0.0041566393,0.00018299246,0.0009124736,0.46785468,0.27513853,0.25060213],"study_design_scores_gemma":[7.648146e-7,0.000003371323,0.0001842698,0.000040790972,7.403703e-7,0.00008837232,0.0001061589,0.000011113643,0.000027979959,0.0035449935,0.99599046,0.0000010373731],"about_ca_topic_score_codex":0.00220376,"about_ca_topic_score_gemma":0.00458849,"teacher_disagreement_score":0.07469447,"about_ca_system_score_codex":0.0013095496,"about_ca_system_score_gemma":0.0006444554,"threshold_uncertainty_score":0.24987787},"labels":[],"label_agreement":null},{"id":"W4409891673","doi":"10.1029/2024tc008464","title":"Circum‐Antarctic Glacially Induced Fault Reactivation Since the Last Glacial Maximum","year":2025,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Norsk Polarinstitutt; Universität Hamburg","keywords":"Geology; Glacial period; Fault (geology); Glacier; Seismology; Geodesy; Geomorphology","score_opus":0.01834183237156977,"score_gpt":0.2386515973665325,"score_spread":0.22030976499496271,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409891673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99797624,0.00034714842,0.00016798331,0.000027452848,0.0000042381735,0.0000025213046,0.0006000627,0.000016557757,0.0008578108],"genre_scores_gemma":[0.99941266,0.00012494609,0.000054016567,0.0000041915387,0.0000026385028,0.0000012070295,0.00031937126,0.0000019461595,0.000079102116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998877,0.00002702276,0.000014203862,0.000026653279,0.000019688294,0.000024781873],"domain_scores_gemma":[0.9995807,0.000104068065,0.00015661358,0.000051665575,0.00006806673,0.00003895852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031260806,0.00032607,0.00019682474,0.0009674961,0.00022495001,0.00076345267,0.00015034777,0.00025916196,0.0010967556],"category_scores_gemma":[0.0007951527,0.00009943887,0.0004781065,0.0013016138,0.00024747037,0.0002823744,0.0002637913,0.00014233384,0.00017957127],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011796782,0.0000156205,0.9466787,0.000088317254,0.00018813256,0.00030594703,0.00017467568,0.033279862,0.00391674,0.00026198773,0.00030149947,0.01467048],"study_design_scores_gemma":[0.0000045580173,0.00004471173,0.98561007,0.00001540335,0.000046354315,0.00019263012,0.00014359973,0.012591658,0.00064563175,0.00011080887,0.0005876543,0.000006973278],"about_ca_topic_score_codex":0.010246252,"about_ca_topic_score_gemma":0.009408678,"teacher_disagreement_score":0.010246252,"about_ca_system_score_codex":0.0005806114,"about_ca_system_score_gemma":0.00024855573,"threshold_uncertainty_score":0.020373225},"labels":[],"label_agreement":null},{"id":"W4410013647","doi":"10.1038/s43247-025-02192-6","title":"Pure dip-slip along the Tuz Gölü Fault Zone accommodates east-west extension of Central Anatolia","year":2025,"lang":"en","type":"article","venue":"Communications Earth & Environment","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Minnesota","keywords":"Geology; Slip (aerodynamics); Seismology; Extension (predicate logic); Engineering","score_opus":0.02219703169090403,"score_gpt":0.22909625062825498,"score_spread":0.20689921893735094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410013647","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978212,0.00007803328,0.00015851314,0.000022406342,0.0000020174616,0.0000022826432,0.00011275824,0.000014682854,0.0017880957],"genre_scores_gemma":[0.9996327,0.00002501907,0.00011416804,0.0000041999774,0.0000013096085,0.0000012859905,0.000105775034,0.0000025443512,0.0001129567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999928,0.000010815216,0.000007194003,0.000021192216,0.000010748964,0.0000221133],"domain_scores_gemma":[0.99987376,0.000018239587,0.00004354224,0.000019710395,0.000031563217,0.000013175851],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016293468,0.00020143719,0.000178007,0.0011094644,0.0003710984,0.00076056697,0.00018030389,0.00016695338,0.0013484746],"category_scores_gemma":[0.00026374805,0.00010226688,0.00011299966,0.0006470433,0.0002614123,0.00024429825,0.00038547628,0.00009919339,0.00022851952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014259497,0.000032168136,0.9237795,0.000042848103,0.00008609527,0.00028760315,0.00034284353,0.0032342153,0.024903128,0.00065249973,0.00033140465,0.04616512],"study_design_scores_gemma":[0.000008258491,0.000036607278,0.99456257,0.000015045547,0.000023293665,0.0001858027,0.00030267495,0.0027368758,0.0010345113,0.00012615083,0.0009643302,0.000003794689],"about_ca_topic_score_codex":0.011548108,"about_ca_topic_score_gemma":0.02900915,"teacher_disagreement_score":0.011548108,"about_ca_system_score_codex":0.0005332949,"about_ca_system_score_gemma":0.0005520878,"threshold_uncertainty_score":0.022961795},"labels":[],"label_agreement":null},{"id":"W4410033109","doi":"10.1785/0120240158","title":"Overview of the SCEC/USGS Community Stress Drop Validation Study Using the 2019 Ridgecrest Earthquake Sequence","year":2025,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Geology; Seismic moment; Moment magnitude scale; Strong ground motion; Magnitude (astronomy); Ground motion; Drop (telecommunication); Geodesy; Fault (geology); Mathematics; Physics; Engineering; Geometry; Scaling","score_opus":0.06871219872265923,"score_gpt":0.2915112098518722,"score_spread":0.22279901112921296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410033109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8807428,0.0007451605,0.02208239,0.0009796468,0.00014413375,0.00408541,0.07874316,0.001142453,0.011334911],"genre_scores_gemma":[0.7228748,0.00041152566,0.03610483,0.00049852434,0.00017173438,0.004695483,0.23126622,0.00047356373,0.0035032895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9902895,0.0035339266,0.0008201062,0.0011058296,0.0037885702,0.0004621435],"domain_scores_gemma":[0.962322,0.006552884,0.0031029442,0.0059391283,0.020228134,0.0018548231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.016642792,0.00077163946,0.0004843567,0.0047690235,0.0012167558,0.0013178443,0.0017137333,0.00077423186,0.0016460145],"category_scores_gemma":[0.02827246,0.0003134105,0.00066814525,0.0036096708,0.0006423909,0.00076488435,0.0020850662,0.00054388685,0.0011234066],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008068741,0.0015476218,0.8295054,0.0005714273,0.000448809,0.00047891264,0.0014007556,0.009265408,0.009332842,0.00088084757,0.042284712,0.10347644],"study_design_scores_gemma":[0.00018999338,0.00045182873,0.94204825,0.00027244925,0.00009472787,0.00025610792,0.0013436845,0.017875789,0.0065054,0.00030271025,0.030568555,0.00009055666],"about_ca_topic_score_codex":0.045408864,"about_ca_topic_score_gemma":0.059968226,"teacher_disagreement_score":0.045408864,"about_ca_system_score_codex":0.0011759973,"about_ca_system_score_gemma":0.0029161882,"threshold_uncertainty_score":0.090289116},"labels":[],"label_agreement":null},{"id":"W4410104116","doi":"10.1016/j.epsl.2025.119388","title":"Fluid pressure fluctuations and the seismic signature of a fault-controlled fluid migration pulse","year":2025,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Cascades (Canada)","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico; Agencia Nacional de Investigación y Desarrollo; Natural Environment Research Council; University of Leicester","keywords":"Geology; Fluid pressure; Seismology; Signature (topology); Fault (geology); Geophysics; Pulse (music); Mechanics; Geometry","score_opus":0.0046550263857070675,"score_gpt":0.18757714455237645,"score_spread":0.1829221181666694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410104116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99850285,0.00006652889,0.0006500282,0.000031934764,0.0000022180166,0.0000028548097,0.000110809335,0.000029998619,0.0006027556],"genre_scores_gemma":[0.999516,0.00003535434,0.00025007577,0.000008725787,0.0000040353193,0.0000022334214,0.00006741927,0.0000033096653,0.00011287212],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999585,0.0000052814667,0.0000032366283,0.0000129918435,0.000010238625,0.000009700264],"domain_scores_gemma":[0.9997948,0.000027009994,0.00010408252,0.00001641589,0.000031072723,0.000026648517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009519335,0.0001268121,0.000105267034,0.0006531355,0.00012203404,0.00022150042,0.00015106397,0.00022099244,0.00074227725],"category_scores_gemma":[0.000524106,0.00011303782,0.000056870696,0.00063289073,0.00033927706,0.00023721492,0.0002797153,0.00016443206,0.00012650076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040815226,0.00007009671,0.59151727,0.000106916625,0.0000625064,0.00071886304,0.0010708816,0.0022985449,0.36219966,0.00043148504,0.00037189454,0.040743716],"study_design_scores_gemma":[0.000005538494,0.000048283353,0.9937137,0.0000043912983,0.0000073709834,0.00014888043,0.0001672143,0.0016488129,0.003672325,0.00010235662,0.00047562883,0.000005387895],"about_ca_topic_score_codex":0.0032572418,"about_ca_topic_score_gemma":0.0044142227,"teacher_disagreement_score":0.0032572418,"about_ca_system_score_codex":0.00018810926,"about_ca_system_score_gemma":0.00009924297,"threshold_uncertainty_score":0.006476581},"labels":[],"label_agreement":null},{"id":"W4410206407","doi":"10.26443/seismica.v2i4.1477","title":"No evidence for an active margin-spanning megasplay fault at the Cascadia Subduction Zone","year":2025,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Margin (machine learning); Geology; Seismology; Fault (geology); Computer science; Machine learning","score_opus":0.04159095065372495,"score_gpt":0.28878358234316703,"score_spread":0.24719263168944208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410206407","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985129,0.000042293235,0.0001131051,0.000036960406,0.0000011738714,0.0000019827896,0.000052314655,0.000015802503,0.0012233999],"genre_scores_gemma":[0.9997695,0.000019679304,0.000049826805,0.000004198713,6.7144765e-7,7.0719835e-7,0.000052273248,0.0000010766963,0.000102023296],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997961,0.000021330532,0.000022368367,0.00007124371,0.00005280294,0.00003617914],"domain_scores_gemma":[0.99915016,0.00008193771,0.00032428015,0.00010002969,0.00014194175,0.00020153186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021062624,0.00018429612,0.0001847932,0.0005613937,0.0004883822,0.0006284374,0.00040405296,0.0003686146,0.00202476],"category_scores_gemma":[0.0013433235,0.00019296315,0.00022080248,0.00056651246,0.00066818856,0.00042811458,0.00061477424,0.00020241487,0.00021021396],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000092221955,0.000016867145,0.98347545,0.000048473044,0.000038512415,0.0002529154,0.00088917057,0.0013917778,0.0088821,0.00033475342,0.00010593435,0.004471848],"study_design_scores_gemma":[0.0000045869097,0.00003627567,0.9978709,0.000012108779,0.000012492174,0.00007518587,0.0004140505,0.00088052585,0.00030193003,0.000073107505,0.00031518517,0.0000035286946],"about_ca_topic_score_codex":0.02708907,"about_ca_topic_score_gemma":0.061740708,"teacher_disagreement_score":0.02708907,"about_ca_system_score_codex":0.000634282,"about_ca_system_score_gemma":0.0005984528,"threshold_uncertainty_score":0.05386275},"labels":[],"label_agreement":null},{"id":"W4410359139","doi":"10.1109/radar58436.2024.10993981","title":"Differentiating Tsunamis from Atmospheric-Induced Events Using Coastal High-Frequency Radars","year":2024,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Remote sensing; Radar; Meteorology; Geology; Computer science; Geography; Telecommunications","score_opus":0.022651716752419636,"score_gpt":0.229485472561632,"score_spread":0.20683375580921234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410359139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99345523,0.00020407345,0.004238416,0.000024885478,0.000014969433,0.00003087481,0.00021638979,0.00004417284,0.0017710319],"genre_scores_gemma":[0.9910842,0.00023541982,0.007938016,0.00002174956,0.000025289602,0.0000123086875,0.00035733712,0.000005681173,0.00032010893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975485,0.00005826914,0.000030870397,0.000051138784,0.00005256593,0.000052276173],"domain_scores_gemma":[0.99876106,0.00043962055,0.00031506736,0.000098922836,0.0002742916,0.000111090485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006105996,0.00028308603,0.00018305528,0.0011155258,0.00016184646,0.0006777882,0.00022313834,0.00041942653,0.0006444222],"category_scores_gemma":[0.0025119113,0.00012066436,0.0001429298,0.00064086984,0.00017106204,0.0004437006,0.00029895778,0.00022355701,0.0002300849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006966445,0.00020773709,0.76251936,0.00019538762,0.000089602676,0.00072727696,0.00061510503,0.0031676467,0.10305579,0.0003075113,0.00045779347,0.12796023],"study_design_scores_gemma":[0.0000335508,0.00025498355,0.97302353,0.000026305837,0.000062695624,0.0005633197,0.00067686965,0.014173699,0.01009026,0.00014803167,0.00092467235,0.00002205412],"about_ca_topic_score_codex":0.0034361552,"about_ca_topic_score_gemma":0.01345096,"teacher_disagreement_score":0.0034361552,"about_ca_system_score_codex":0.00013536026,"about_ca_system_score_gemma":0.00020262902,"threshold_uncertainty_score":0.0068323016},"labels":[],"label_agreement":null},{"id":"W4410455357","doi":"10.1007/s10950-025-10297-w","title":"Estimating dynamic source parameters from S-Wave spectra for earthquakes in the Dahshour Region, Northwestern Egypt","year":2025,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Structural geology; Seismology; Geology; Hydrogeology; Geophysics; Geotechnical engineering","score_opus":0.02437231720621314,"score_gpt":0.24820404702214424,"score_spread":0.2238317298159311,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410455357","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99927706,0.000048159105,0.00021479634,0.00002006852,0.0000013373751,0.000003573381,0.00022775201,0.0000070462124,0.00020021677],"genre_scores_gemma":[0.99845004,0.000083993036,0.0005006727,0.0000035463095,0.000002623022,0.0000033469355,0.0006772047,0.0000030043338,0.00027556624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999076,0.0000102743315,0.000009571801,0.000018591183,0.000017062017,0.000036946403],"domain_scores_gemma":[0.9997346,0.00006596312,0.000053421467,0.00001686545,0.00009680226,0.000032375778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002590362,0.0004348106,0.00027621427,0.0016612451,0.00031720896,0.0006099775,0.00048741323,0.0004474662,0.000653737],"category_scores_gemma":[0.00075457676,0.0002498926,0.0002627719,0.0013066947,0.00020525412,0.00047917204,0.00042440937,0.00024135037,0.00026963823],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000547599,0.00020138423,0.8866424,0.00011237705,0.000204063,0.0013436375,0.0010368829,0.028065825,0.02012036,0.0002919602,0.00072555005,0.060708057],"study_design_scores_gemma":[0.00004469862,0.000047738333,0.96066296,0.000016694867,0.00009006038,0.000121879115,0.0027297465,0.033930127,0.0016767236,0.000114828894,0.0005439868,0.000020623233],"about_ca_topic_score_codex":0.08583954,"about_ca_topic_score_gemma":0.104743764,"teacher_disagreement_score":0.08583954,"about_ca_system_score_codex":0.00068306347,"about_ca_system_score_gemma":0.0010513188,"threshold_uncertainty_score":0.17067981},"labels":[],"label_agreement":null},{"id":"W4410516548","doi":"10.1785/0320250013","title":"Generalized Nearest-Neighbor Distance and Hawkes Point Process Modeling Applied to Mining-Induced Seismicity","year":2025,"lang":"en","type":"article","venue":"The Seismic Record","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Mitacs","keywords":"Induced seismicity; k-nearest neighbors algorithm; Process (computing); Data mining; Point (geometry); Point process; Computer science; Geology; Statistical physics; Seismology; Artificial intelligence; Mathematics; Physics; Statistics; Geometry","score_opus":0.02042530291984317,"score_gpt":0.2436763726522852,"score_spread":0.22325106973244202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410516548","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.16032499,0.00012663307,0.8372379,0.00015531485,0.000046530287,0.00005964758,0.000088827524,0.00008562172,0.0018745305],"genre_scores_gemma":[0.9607929,0.000108245105,0.036750343,0.000024146482,0.000024152885,0.000069116504,0.000076374075,0.000020675849,0.002133974],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993631,0.0002816284,0.000032843545,0.00014434892,0.00012551373,0.00005251242],"domain_scores_gemma":[0.9979705,0.0013231271,0.00026688838,0.0001095078,0.00024006731,0.00008985712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018581492,0.0004479258,0.00068450463,0.00076172134,0.00041610975,0.0008087769,0.0012404415,0.00094214274,0.001107913],"category_scores_gemma":[0.005430517,0.00033959045,0.00081650267,0.00067715003,0.0010933408,0.0009162282,0.0008864614,0.00079878897,0.00012237806],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009934714,0.000010783825,0.0011511043,0.000012959796,0.00002016629,0.000046490768,0.00004473379,0.98114717,0.0002808995,0.0141476635,0.000069899485,0.0030582494],"study_design_scores_gemma":[7.416698e-7,0.0000035543937,0.00013214925,8.087626e-7,0.0000010239124,0.0000031748216,0.000005256035,0.99735343,0.000026737598,0.002434839,0.00003561148,0.0000026028172],"about_ca_topic_score_codex":0.013400248,"about_ca_topic_score_gemma":0.008291476,"teacher_disagreement_score":0.013400248,"about_ca_system_score_codex":0.0009394685,"about_ca_system_score_gemma":0.00071698707,"threshold_uncertainty_score":0.026644528},"labels":[],"label_agreement":null},{"id":"W4410560778","doi":"10.1007/s10659-025-10135-7","title":"On the Influence of a Dilatant Asperity Patch on the Seismic Moment","year":2025,"lang":"en","type":"article","venue":"Journal of Elasticity","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"European Research Council; Natural Sciences and Engineering Research Council of Canada; Horizon 2020 Framework Programme","keywords":"Dilatant; Geology; Shear (geology); Fault plane; Asperity (geotechnical engineering); Fault (geology); Geotechnical engineering; Seismology; Moment (physics); Shear stress; Mechanics; Petrology; Physics; Classical mechanics","score_opus":0.013140708491686196,"score_gpt":0.2200811864869997,"score_spread":0.2069404779953135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410560778","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.77111304,0.00013315608,0.2261112,0.00006567508,0.000018221108,0.000038300703,0.0001549434,0.00016532882,0.0022002417],"genre_scores_gemma":[0.9873104,0.00006904582,0.012290533,0.000008853412,0.00000785658,0.0000141571045,0.000041987223,0.000021380138,0.00023572077],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99983394,0.000033641518,0.000008793516,0.000055566714,0.000054849468,0.000013141532],"domain_scores_gemma":[0.99900216,0.00062517525,0.00018165688,0.00009558633,0.000064936285,0.000030583586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044680535,0.00029929573,0.00028677422,0.00048761093,0.00015690169,0.0004580244,0.0005211254,0.00020953256,0.0012482557],"category_scores_gemma":[0.0029532476,0.00017755321,0.00028121594,0.00024261723,0.00039862233,0.00038113634,0.00045005747,0.0002275483,0.00016926447],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006060548,0.00012741503,0.06544765,0.00023041206,0.00013573184,0.00090267713,0.00028632724,0.48495835,0.33264744,0.006502717,0.00023959499,0.1079156],"study_design_scores_gemma":[0.000010108771,0.00020070675,0.04382185,0.000015170953,0.000048252015,0.00017658826,0.00007681673,0.90140456,0.05250243,0.0011621263,0.0005540455,0.000027372875],"about_ca_topic_score_codex":0.0015055628,"about_ca_topic_score_gemma":0.0020704987,"teacher_disagreement_score":0.0015055628,"about_ca_system_score_codex":0.0002732432,"about_ca_system_score_gemma":0.00025130226,"threshold_uncertainty_score":0.0041759014},"labels":[],"label_agreement":null},{"id":"W4410629122","doi":"10.1515/geo-2025-0779","title":"Simulation of seismic hazard parameters and earthquakes source mechanisms along the Red Sea rift, western Saudi Arabia","year":2025,"lang":"en","type":"article","venue":"Open Geosciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Research Institute of Astronomy and Geophysics; King Saud University","keywords":"Seismology; Geology; Rift; Seismic hazard; Hazard; Tectonics","score_opus":0.023332862319410185,"score_gpt":0.2539738598796779,"score_spread":0.23064099756026774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410629122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736005,0.000019298484,0.0014333924,0.000044649336,0.0000044958106,0.00000946163,0.00027308654,0.000030281144,0.0008252699],"genre_scores_gemma":[0.9984302,0.000014217338,0.00092551886,0.0000066361613,0.0000012170125,0.000008473869,0.0002406222,0.0000033557317,0.00036966495],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999273,0.00002195011,0.0000051108186,0.000013873024,0.000010716919,0.00002104004],"domain_scores_gemma":[0.9994172,0.00027788494,0.000086920336,0.00003122904,0.00013301987,0.00005363521],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003034877,0.00043751142,0.00028322372,0.00035765703,0.00026623203,0.00043382525,0.0005762815,0.0006249421,0.001438158],"category_scores_gemma":[0.0011728855,0.00021009574,0.0003957564,0.0002854148,0.00025406457,0.00021428539,0.00033435956,0.0003021121,0.00011375189],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007370504,0.00004188799,0.015265094,0.000014134466,0.000020248368,0.00011088935,0.000038290145,0.981942,0.0008026928,0.00038809745,0.00014616581,0.0011567207],"study_design_scores_gemma":[0.000011707176,0.000020219082,0.0023598184,0.000001706544,0.000006207248,0.0000070057035,0.000035115587,0.9972154,0.00022929814,0.000047174344,0.00006371783,0.000002532359],"about_ca_topic_score_codex":0.07705109,"about_ca_topic_score_gemma":0.03937967,"teacher_disagreement_score":0.07705109,"about_ca_system_score_codex":0.00061403343,"about_ca_system_score_gemma":0.00062798295,"threshold_uncertainty_score":0.15320522},"labels":[],"label_agreement":null},{"id":"W4410941985","doi":"10.1007/s10950-025-10301-3","title":"Identifying and removing quarry and mine blasts from the iranian seismological center’s (IRSC) earthquake catalog (2006–2024)","year":2025,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Structural geology; Geology; Center (category theory); Hydrogeology; Biogeosciences; Earth science; Geotechnical engineering","score_opus":0.01965389103986113,"score_gpt":0.23996602334894213,"score_spread":0.220312132309081,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410941985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7517846,0.0011981736,0.0075944522,0.00070804585,0.0006968686,0.0006432951,0.21312432,0.001248563,0.023001699],"genre_scores_gemma":[0.49072918,0.0012658484,0.02421361,0.00023652555,0.00029207257,0.00039622176,0.46204358,0.00023014458,0.02059267],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994006,0.000024524667,0.000105535575,0.00008098557,0.0002598232,0.00012842509],"domain_scores_gemma":[0.9978035,0.00010233532,0.0004289774,0.00028520895,0.0012871856,0.00009283995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006057234,0.0005331933,0.00032520632,0.008178304,0.00077827735,0.0006945404,0.0007602065,0.0004493801,0.0051606856],"category_scores_gemma":[0.003159115,0.00022986914,0.00033773962,0.0063250903,0.00016185896,0.00048386128,0.0008101916,0.0004242967,0.004724847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021866609,0.00015833088,0.5283199,0.00039938185,0.000077435005,0.00089082663,0.0008055411,0.001446811,0.009863084,0.0008329134,0.19820206,0.25878513],"study_design_scores_gemma":[0.000019719842,0.00003402114,0.9162962,0.00006415667,0.000053988355,0.00028129772,0.00075294037,0.0012043881,0.0020607552,0.00014301132,0.079074055,0.000015521755],"about_ca_topic_score_codex":0.09121671,"about_ca_topic_score_gemma":0.16147928,"teacher_disagreement_score":0.09121671,"about_ca_system_score_codex":0.000522554,"about_ca_system_score_gemma":0.003284851,"threshold_uncertainty_score":0.18137157},"labels":[],"label_agreement":null},{"id":"W4411056290","doi":"10.1080/21664250.2025.2516324","title":"Effect of calibration data on performance of tsunami early warning model","year":2025,"lang":"en","type":"article","venue":"Coastal Engineering Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Calibration; Warning system; Environmental science; Geology; Computer science; Engineering; Statistics; Mathematics; Telecommunications","score_opus":0.010585777875567333,"score_gpt":0.21537272880287522,"score_spread":0.2047869509273079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411056290","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.964893,0.0008516842,0.030203758,0.00029684472,0.00009187809,0.00006702498,0.0009060729,0.00059256924,0.0020971862],"genre_scores_gemma":[0.9935133,0.00012815441,0.004863894,0.00005904564,0.0000053387844,0.00003687779,0.0011907635,0.00003462373,0.00016804505],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99525094,0.0025416329,0.0003864346,0.0008744999,0.000666031,0.00028047274],"domain_scores_gemma":[0.96491843,0.02488079,0.0020424281,0.0041741296,0.0037227408,0.00026155234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010337304,0.0012658035,0.0005985843,0.00074660295,0.00063217967,0.0010326555,0.0009197096,0.0018167961,0.00073654536],"category_scores_gemma":[0.050970923,0.00043930407,0.00066136173,0.0008631788,0.0010819352,0.001898573,0.0012018712,0.0012657841,0.000198874],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011157008,0.00033320257,0.054051287,0.00019497596,0.0002681398,0.00020515529,0.00016193792,0.88992816,0.0065443157,0.0011003905,0.00094586005,0.04515087],"study_design_scores_gemma":[0.00013137517,0.0006194752,0.055069454,0.00018978307,0.00020019336,0.00020160519,0.00032403637,0.9063769,0.03308388,0.0019671773,0.0017092201,0.00012684039],"about_ca_topic_score_codex":0.0077472515,"about_ca_topic_score_gemma":0.0033701183,"teacher_disagreement_score":0.010337304,"about_ca_system_score_codex":0.0008649374,"about_ca_system_score_gemma":0.0008032607,"threshold_uncertainty_score":0.05466956},"labels":[],"label_agreement":null},{"id":"W4411136494","doi":"10.1016/j.epsl.2025.119485","title":"Tectonically induced changes in vent fluid compositions and metal concentrations at Main Endeavour Field, northeast Pacific Ocean","year":2025,"lang":"en","type":"article","venue":"Earth and Planetary Science Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Defense Science and Engineering Graduate; National Science Foundation","keywords":"Geology; Oceanography; Pacific ocean; Field (mathematics)","score_opus":0.010339450770674025,"score_gpt":0.20331946321177588,"score_spread":0.19298001244110186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411136494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999328,0.000021178752,0.000029990957,0.000010471982,8.822898e-7,0.000002079273,0.00021898175,0.0000031603936,0.00038523992],"genre_scores_gemma":[0.9992131,0.00004743272,0.00008931553,0.000011977565,0.0000013508034,0.0000032056573,0.0003314034,0.0000018225561,0.00030046553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999347,0.0000044891585,0.000004189267,0.000024565636,0.000014207076,0.000017919],"domain_scores_gemma":[0.999803,0.000016932958,0.00006888807,0.000011386239,0.000050136212,0.000049622093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010308413,0.00018148385,0.000111363865,0.0006745643,0.0003819526,0.00034517734,0.00022873425,0.00017596272,0.0007576531],"category_scores_gemma":[0.00039748906,0.00013515324,0.000112684065,0.00050538866,0.00034414328,0.00024875085,0.00039043112,0.00016777572,0.0000645507],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000069509224,0.0000192856,0.97150874,0.000015985017,0.00002787148,0.00010671674,0.00045712164,0.00014656827,0.02378047,0.000027415359,0.000090819536,0.0037495717],"study_design_scores_gemma":[6.112709e-7,0.0000074292766,0.9992625,0.0000010260279,0.000002598502,0.000011653911,0.0001336462,0.00006388293,0.00044734913,0.000004133079,0.000064236585,9.565236e-7],"about_ca_topic_score_codex":0.23862049,"about_ca_topic_score_gemma":0.40283442,"teacher_disagreement_score":0.23862049,"about_ca_system_score_codex":0.0008697987,"about_ca_system_score_gemma":0.0006733916,"threshold_uncertainty_score":0.4744631},"labels":[],"label_agreement":null},{"id":"W4411141344","doi":"10.1130/b37994.1","title":"Dextral slip along the Western Nepal Fault System accommodates significant orogen-parallel shear","year":2025,"lang":"en","type":"article","venue":"Geological Society of America Bulletin","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Sinistral and dextral; Geology; Seismology; Shear (geology); Strike-slip tectonics; Shear zone; Normal fault; Fault (geology); Slip (aerodynamics); Geodesy; Petrology; Tectonics","score_opus":0.015038891994033595,"score_gpt":0.22026814918490806,"score_spread":0.20522925719087445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411141344","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987879,0.000114881645,0.00056275347,0.000054583586,0.0000024513577,0.000012496409,0.0005060846,0.00005149893,0.010816352],"genre_scores_gemma":[0.99890566,0.00004617881,0.00024712796,0.000017292297,0.0000015280592,0.0000064853607,0.00030499385,0.000005071975,0.00046560884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999126,0.00000794955,0.0000074217337,0.000027096929,0.000019883346,0.000025021518],"domain_scores_gemma":[0.9998455,0.00002529049,0.000047742888,0.00002207673,0.00004230657,0.000017026467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000098511686,0.00016360145,0.00017572111,0.000985448,0.00048563792,0.0008157891,0.00018931915,0.00012950975,0.0030094134],"category_scores_gemma":[0.00042999125,0.00013585926,0.00010754095,0.000737515,0.00032368387,0.0003214816,0.00050846516,0.00014000271,0.00048996473],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008638033,0.00004396545,0.89527506,0.00010288623,0.00006196363,0.0011498632,0.0014762995,0.0014005911,0.037636843,0.0007806828,0.00090281956,0.061082646],"study_design_scores_gemma":[0.000006771061,0.000032145028,0.99241513,0.0000328346,0.000020662439,0.0007232401,0.0006444991,0.0012999149,0.0016161402,0.00027220804,0.0029277846,0.000008548501],"about_ca_topic_score_codex":0.013788943,"about_ca_topic_score_gemma":0.033334095,"teacher_disagreement_score":0.013788943,"about_ca_system_score_codex":0.00031350166,"about_ca_system_score_gemma":0.0005138749,"threshold_uncertainty_score":0.027417362},"labels":[],"label_agreement":null},{"id":"W4411148602","doi":"10.1130/abs/2025rm-410192","title":"FAULT BLOCK, TECTONIC DETACHMENT, OR MEGA-LANDSLIDE? EAST TRAVERSE MOUNTAINS, UTAH","year":2025,"lang":"en","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Queen's University","funders":"","keywords":"Traverse; Mega-; Landslide; Geology; Block (permutation group theory); Tectonics; Seismology; Fault (geology); Geodesy","score_opus":0.02048834689427692,"score_gpt":0.24728766090291762,"score_spread":0.2267993140086407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411148602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9566291,0.0063736686,0.0001240047,0.007578235,0.00014765299,0.000011003167,0.0027845823,0.000029445468,0.026322281],"genre_scores_gemma":[0.9795828,0.0023557213,0.00023678887,0.0003930537,0.00011329596,0.000011013548,0.00092779915,0.000008470795,0.01637104],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994254,0.00000930156,0.000003860306,0.000014817839,0.000013681695,0.000015850108],"domain_scores_gemma":[0.9997565,0.00004324998,0.000053772725,0.0000110127,0.00007156918,0.00006385468],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015596331,0.00006753658,0.00013669037,0.00041380315,0.0010680595,0.00060518505,0.0004063873,0.00031717448,0.006523083],"category_scores_gemma":[0.00090315245,0.000054774133,0.00005561008,0.0008410737,0.0004712936,0.00073222246,0.00050266,0.00018189478,0.00035623836],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025133716,0.0000650076,0.8313062,0.00022037704,0.00004797526,0.00062462874,0.0063713286,0.00057309045,0.0007928328,0.010096469,0.083080284,0.066570416],"study_design_scores_gemma":[0.000011953991,0.000022990755,0.9525562,0.00009911894,0.000027128484,0.00014358839,0.0071999007,0.0002897096,0.00011778436,0.0012428727,0.03828186,0.000007027174],"about_ca_topic_score_codex":0.23315714,"about_ca_topic_score_gemma":0.6815535,"teacher_disagreement_score":0.23315714,"about_ca_system_score_codex":0.0009363337,"about_ca_system_score_gemma":0.0012839504,"threshold_uncertainty_score":0.46360004},"labels":[],"label_agreement":null},{"id":"W4411350389","doi":"10.1016/j.tecto.2025.230827","title":"Recurrence of large earthquakes along the southern Xainza-Dinggye rift and comparison with the 7 January 2025, Mw7.1 Tingri earthquake, southern Tibet","year":2025,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Continental (Canada)","funders":"Chinese Academy of Geological Sciences; China Geological Survey; National Natural Science Foundation of China","keywords":"Geology; Seismology; Rift; Tectonics","score_opus":0.014468465642103127,"score_gpt":0.23473536342696533,"score_spread":0.2202668977848622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411350389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999295,0.00003922868,0.0000130530325,0.000022562976,0.0000047632097,0.0000011866103,0.00034949704,0.0000017036568,0.00027307984],"genre_scores_gemma":[0.9987243,0.000027941887,0.000011112109,0.000009841366,0.000008068758,0.0000019052068,0.00091031956,9.364016e-7,0.0003055979],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989843,0.000011217541,0.00001451043,0.000026285423,0.000016098957,0.000033440432],"domain_scores_gemma":[0.9995431,0.000054909753,0.000175308,0.00001887451,0.00006574344,0.0001421031],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023587568,0.00018081469,0.00013928261,0.0014091086,0.00034542044,0.00046442306,0.00024025587,0.0003633392,0.001647525],"category_scores_gemma":[0.0007701563,0.00009929825,0.00017807457,0.0014324485,0.0003073572,0.00026188002,0.00033074437,0.00018948746,0.00024300128],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027927486,0.00004828606,0.992504,0.000020100731,0.00004971407,0.00037535658,0.0007642977,0.00021400537,0.001375671,0.00006880362,0.00029046886,0.004009977],"study_design_scores_gemma":[0.0000028096956,0.00002001908,0.9995234,0.0000022112606,0.0000046697037,0.000043124543,0.00019864854,0.00008569243,0.000018457204,0.0000056271483,0.00009399829,0.0000013327362],"about_ca_topic_score_codex":0.029810568,"about_ca_topic_score_gemma":0.05277495,"teacher_disagreement_score":0.029810568,"about_ca_system_score_codex":0.00047824963,"about_ca_system_score_gemma":0.00037948583,"threshold_uncertainty_score":0.059274137},"labels":[],"label_agreement":null},{"id":"W4411621611","doi":"10.1007/s10950-025-10307-x","title":"Variation in the level of seismic hazard in Northeast British Columbia, Canada, due to induced seismicity","year":2025,"lang":"en","type":"article","venue":"Journal of Seismology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria; BGC Engineering (Canada)","funders":"","keywords":"Induced seismicity; Seismology; Structural geology; Geology; Seismic hazard; Variation (astronomy); Hydrogeology; Hazard; Geotechnical engineering","score_opus":0.025714362976823266,"score_gpt":0.22706133618314653,"score_spread":0.20134697320632328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411621611","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99449664,0.00015294232,0.0000796417,0.00019686355,0.000007021552,0.00001370117,0.0026817727,0.000011002956,0.002360347],"genre_scores_gemma":[0.9969798,0.000108377884,0.00006847946,0.000044644443,0.0000017459513,0.0000065639765,0.0010749394,0.0000051435322,0.0017102569],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994742,0.000054460925,0.00004491979,0.00010117841,0.00014210457,0.0001831203],"domain_scores_gemma":[0.9972179,0.00027693648,0.00034498685,0.00008423884,0.0014044648,0.00067150977],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038177677,0.0001949984,0.000284304,0.0011889169,0.0018312085,0.001143027,0.0012924562,0.0005417629,0.002664049],"category_scores_gemma":[0.002493228,0.00032484625,0.00026790367,0.0031460568,0.00088434806,0.00027460567,0.0008229586,0.000698655,0.0003128454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013812314,0.000047980084,0.99135965,0.000026910844,0.00008168056,0.00014746723,0.0010506466,0.00065446267,0.00078796066,0.00016754634,0.0012996392,0.004238019],"study_design_scores_gemma":[0.0000026404764,0.0000044529725,0.99837804,0.0000078798785,0.000007931372,0.000019262883,0.0009679771,0.00022127831,0.000038478673,0.000011653383,0.00033536757,0.0000050187678],"about_ca_topic_score_codex":0.99688524,"about_ca_topic_score_gemma":0.99883896,"teacher_disagreement_score":0.02130715,"about_ca_system_score_codex":0.02130715,"about_ca_system_score_gemma":0.019951588,"threshold_uncertainty_score":0.1545949},"labels":[],"label_agreement":null},{"id":"W4411649892","doi":"10.1029/2024gl113849","title":"Large Size of Two 19th‐Century Chile‐Peru Earthquakes Inferred From Trans‐Pacific Tsunami Records","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Fondo de Financiamiento de Centros de Investigación en Áreas Prioritarias; Fondo Nacional de Desarrollo Científico y Tecnológico; Agencia Nacional de Investigación y Desarrollo","keywords":"Geology; Seismology","score_opus":0.022085294022705,"score_gpt":0.29096716591570587,"score_spread":0.2688818718930009,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411649892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99826765,0.000081558304,0.00012939339,0.00005438092,0.0000017872491,0.000002651706,0.0003611131,0.0000071981026,0.0010942352],"genre_scores_gemma":[0.9993754,0.00007197776,0.000091909016,0.0000042716456,0.0000050617837,0.0000039981983,0.00033420188,0.000001770088,0.000111493995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.000023925611,0.000007814048,0.000019345307,0.00001556795,0.000010375951],"domain_scores_gemma":[0.99904484,0.00023027681,0.00035521737,0.00010104693,0.00018055803,0.00008805446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032936898,0.00013405994,0.00009583629,0.0011357729,0.00022981239,0.00049557706,0.00019647804,0.0001668563,0.0013748647],"category_scores_gemma":[0.0020923791,0.00012630428,0.00012586833,0.0007947319,0.00026599053,0.0004101514,0.00081904815,0.0002482017,0.00024682423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006606481,0.000015164547,0.98443246,0.000033823664,0.000087593624,0.00031808484,0.0010981503,0.00073348597,0.0034579043,0.00020300315,0.000353902,0.009200279],"study_design_scores_gemma":[0.0000031126679,0.000008339668,0.9982311,0.000010079534,0.000009859799,0.000078916346,0.00027671945,0.0004885355,0.00023417534,0.000045355766,0.00060910627,0.0000046921687],"about_ca_topic_score_codex":0.005396673,"about_ca_topic_score_gemma":0.008461466,"teacher_disagreement_score":0.005396673,"about_ca_system_score_codex":0.00028634802,"about_ca_system_score_gemma":0.00015217792,"threshold_uncertainty_score":0.010730505},"labels":[],"label_agreement":null},{"id":"W4411711991","doi":"10.1785/0220240380","title":"TOQUES: An Ocean-Bottom Seismometer Dataset on the Central Queen Charlotte Fault, Southeast Alaska","year":2025,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Dalhousie University; University of British Columbia","funders":"","keywords":"Seismometer; Queen (butterfly); Geology; Seismology; Fault (geology); Ocean bottom; Oceanography","score_opus":0.06786340260999732,"score_gpt":0.31990226605754696,"score_spread":0.25203886344754967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411711991","genre_codex":"empirical","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8413953,0.00062725105,0.00056594907,0.0003083623,0.00008873608,0.000045390123,0.1528953,0.00055051234,0.0035231595],"genre_scores_gemma":[0.62250215,0.00031458767,0.0022067183,0.00012317386,0.00008090304,0.00008656864,0.37291658,0.000078281,0.001690973],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.99960893,0.000051460156,0.000053315413,0.00011961696,0.00010366488,0.00006310866],"domain_scores_gemma":[0.99892384,0.00010542911,0.0001163784,0.00017895347,0.00051946467,0.00015595833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074646383,0.00036671522,0.00031918322,0.0016111932,0.000482178,0.0006592592,0.00060940685,0.0006667484,0.0012452026],"category_scores_gemma":[0.0016857833,0.00016011302,0.0002462047,0.0014965615,0.00027218886,0.00043865672,0.00090873515,0.00041519784,0.0007407396],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045131834,0.00032892247,0.86432683,0.00040950227,0.0003820264,0.0011000518,0.0013721279,0.014463343,0.0060651475,0.00063091435,0.08107588,0.02939405],"study_design_scores_gemma":[0.00007803117,0.000064779015,0.94662434,0.00012708407,0.00006829829,0.00014961573,0.0014384213,0.010684492,0.00081370113,0.0002492289,0.03965964,0.00004236574],"about_ca_topic_score_codex":0.18536557,"about_ca_topic_score_gemma":0.3031908,"teacher_disagreement_score":0.18536557,"about_ca_system_score_codex":0.00070778705,"about_ca_system_score_gemma":0.0011165465,"threshold_uncertainty_score":0.36857325},"labels":[],"label_agreement":null},{"id":"W4411844869","doi":"10.1007/s40328-025-00472-3","title":"Evidence of shear and tensile fracturing in the western desert earthquakes, Egypt","year":2025,"lang":"en","type":"article","venue":"Acta Geodaetica et Geophysica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Shear (geology); Desert (philosophy); Hydraulic fracturing; Seismology; Geotechnical engineering; Petrology; Political science","score_opus":0.022994822659086218,"score_gpt":0.26038169695748364,"score_spread":0.23738687429839742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411844869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989766,0.00007301742,0.000010378952,0.000023977444,0.000001177933,0.0000012631809,0.000105116014,6.244272e-7,0.0008078528],"genre_scores_gemma":[0.9994924,0.000097684475,0.000017589133,0.000009279276,0.0000033369063,0.000001061077,0.00012373064,3.982866e-7,0.0002545394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999157,0.000009598762,0.0000135498185,0.000010350853,0.000018035325,0.000032697022],"domain_scores_gemma":[0.9996499,0.00005123334,0.00013952442,0.000016899296,0.000090284215,0.00005204868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014110291,0.00016369772,0.00013057118,0.0012333656,0.000403561,0.00035268752,0.00023275362,0.00026249597,0.0012439981],"category_scores_gemma":[0.0005155799,0.00016222762,0.0001004991,0.0013757247,0.00053127465,0.00020563316,0.00038319716,0.00013663917,0.00019785736],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020869574,0.000030148794,0.98743117,0.000048772697,0.000049279042,0.0009770134,0.0015936466,0.00009259139,0.004281309,0.00013489659,0.00012627796,0.0050261794],"study_design_scores_gemma":[0.000002483151,0.000011093193,0.9984743,0.000004206757,0.00000666492,0.00017778078,0.0010163904,0.000022658964,0.0001128556,0.000013903476,0.00015605429,0.0000015775938],"about_ca_topic_score_codex":0.028566618,"about_ca_topic_score_gemma":0.05425192,"teacher_disagreement_score":0.028566618,"about_ca_system_score_codex":0.00052500254,"about_ca_system_score_gemma":0.00053809816,"threshold_uncertainty_score":0.056800723},"labels":[],"label_agreement":null},{"id":"W4411903245","doi":"10.5194/egusphere-2025-500","title":"Active Piedmont Zone Deformation, a manifestation of activity on the ‘Master Ray Fault’; insight into the seismic hazard analysis of the Tehran metropolitan area","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Geological Survey and Mineral Exploration of Iran; University of Tehran; Deutsche Forschungsgemeinschaft; Canadian Institutes of Health Research; Alexander von Humboldt-Stiftung","keywords":"Seismology; Metropolitan area; Seismic hazard; Fault (geology); Geology; Active fault; Hazard; Deformation (meteorology); Seismic risk; Geography; Archaeology; Oceanography","score_opus":0.024744236104876294,"score_gpt":0.23792435222277264,"score_spread":0.21318011611789633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411903245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99868816,0.00005921998,0.0002527636,0.000014494126,0.0000013368905,0.0000033165886,0.00015583116,0.0000103207385,0.00081461424],"genre_scores_gemma":[0.99936455,0.000030305911,0.000306923,0.000002995485,0.000002409834,0.0000016597331,0.00017308274,0.0000014831569,0.000116664276],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999181,0.000006706255,0.0000056584895,0.000019119727,0.000024980955,0.000025416659],"domain_scores_gemma":[0.9998901,0.000013803567,0.00004934496,0.000011093677,0.000021931384,0.000013780129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017153523,0.00026519084,0.00014334758,0.0018090724,0.00023279666,0.0003862896,0.00025343095,0.00016675482,0.0009914006],"category_scores_gemma":[0.0002831481,0.0000797599,0.00016239616,0.0011812752,0.00023457734,0.00020300689,0.00034426965,0.00012272735,0.00012371752],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086608685,0.00003066452,0.9470649,0.000049325932,0.000045737124,0.00047187967,0.00062834093,0.003611946,0.016090376,0.00053693366,0.00030089158,0.031082448],"study_design_scores_gemma":[0.0000021880767,0.000014174891,0.99405473,0.0000037235668,0.000011688537,0.00013302211,0.000291769,0.003883685,0.001076258,0.00008791797,0.00043645565,0.0000044695075],"about_ca_topic_score_codex":0.009466905,"about_ca_topic_score_gemma":0.013564171,"teacher_disagreement_score":0.009466905,"about_ca_system_score_codex":0.00041874018,"about_ca_system_score_gemma":0.00028601816,"threshold_uncertainty_score":0.018823624},"labels":[],"label_agreement":null},{"id":"W4412121131","doi":"10.5194/epsc-dps2025-322","title":"Scalloped Cliff Formations and Association with Radar Reflectors, a Radar - Imagery Integrated Approach","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Cliff; Radar; Geology; Remote sensing; Association (psychology); Radar imaging; Geography; Computer science; Telecommunications; Psychology; Paleontology","score_opus":0.017497028473705534,"score_gpt":0.22955790033625165,"score_spread":0.2120608718625461,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412121131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9377624,0.0024071145,0.033541124,0.00026819066,0.0000891792,0.00038159336,0.017851673,0.0012400869,0.0064586145],"genre_scores_gemma":[0.8512654,0.0012453365,0.10561548,0.00014625039,0.00012071097,0.00013877895,0.0380347,0.00021453443,0.0032188224],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996766,0.000020023332,0.00001670678,0.00012738977,0.000067329536,0.0000919718],"domain_scores_gemma":[0.9997162,0.000018387267,0.0000662125,0.000052739844,0.00009297394,0.00005337944],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037786696,0.0006202709,0.0003580369,0.0053491485,0.00045738416,0.0017555509,0.0007671016,0.0005653748,0.0010825503],"category_scores_gemma":[0.00046166944,0.0003148117,0.0006327689,0.0027942874,0.00025696872,0.0007196365,0.0013156546,0.00047930202,0.00079485687],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003013744,0.00062218495,0.66124314,0.00047132614,0.0004919837,0.001777971,0.0018944441,0.01396927,0.04550518,0.0014634789,0.015578551,0.25668108],"study_design_scores_gemma":[0.000028795163,0.00014255138,0.86800027,0.00018990497,0.00031334185,0.0011238162,0.0043691574,0.09195717,0.0056054113,0.0011266256,0.027067188,0.00007571004],"about_ca_topic_score_codex":0.031698406,"about_ca_topic_score_gemma":0.08762198,"teacher_disagreement_score":0.031698406,"about_ca_system_score_codex":0.00044397032,"about_ca_system_score_gemma":0.00068050704,"threshold_uncertainty_score":0.0630278},"labels":[],"label_agreement":null},{"id":"W4412163718","doi":"10.21203/rs.3.rs-6966040/v1","title":"Revised Probabilistic Seismic Hazard Mapping for Greater Tehran Based on Updated Tectonic Interpretations","year":2025,"lang":"en","type":"preprint","venue":"Research Square","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institutes of Health Research; International Institute of Earthquake Engineering and Seismology","keywords":"Tectonics; Probabilistic logic; Seismology; Hazard; Geology; Seismic hazard; Computer science; Artificial intelligence","score_opus":0.07240856745239899,"score_gpt":0.3440094494112081,"score_spread":0.2716008819588091,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412163718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6303608,0.0008906936,0.309146,0.0010927478,0.00030209508,0.00028175075,0.02949874,0.004592322,0.02383493],"genre_scores_gemma":[0.88160324,0.00032849718,0.10348988,0.00003514629,0.00006632336,0.00008357149,0.01010937,0.00025199418,0.0040320028],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99959975,0.00008643325,0.00003536496,0.00010158156,0.00012534068,0.000051498817],"domain_scores_gemma":[0.99903333,0.00014435277,0.00013487121,0.00016480213,0.000493738,0.000028993003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011652363,0.00071670656,0.00043357446,0.0030436637,0.00032519797,0.0009952685,0.00096938334,0.00040783742,0.0060797697],"category_scores_gemma":[0.0037447037,0.0004574668,0.00054471014,0.0022780218,0.00024797156,0.0010294934,0.00078115467,0.0005316812,0.001282154],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045552623,0.00013083931,0.11970694,0.00037896604,0.00022225043,0.0009041932,0.00089657085,0.49138182,0.011041943,0.0097801285,0.019486565,0.3456143],"study_design_scores_gemma":[0.00016280943,0.00010084821,0.19189875,0.000095291594,0.00022761004,0.00035782074,0.0007234926,0.76693785,0.0034027626,0.011194799,0.024793092,0.00010492417],"about_ca_topic_score_codex":0.060585596,"about_ca_topic_score_gemma":0.07248664,"teacher_disagreement_score":0.060585596,"about_ca_system_score_codex":0.0010168087,"about_ca_system_score_gemma":0.002113507,"threshold_uncertainty_score":0.120465875},"labels":[],"label_agreement":null},{"id":"W4412182178","doi":"10.1080/00288306.2025.2519711","title":"Paleoseismology of the Long Valley Fault, Central Otago, New Zealand","year":2025,"lang":"en","type":"article","venue":"New Zealand Journal of Geology and Geophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Paleoseismology; Fault (geology); Seismology; Geochemistry; Geomorphology","score_opus":0.007442731788280453,"score_gpt":0.21172379427007354,"score_spread":0.2042810624817931,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412182178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99739647,0.00013865235,0.000083544546,0.000019762756,8.7883774e-7,0.0000074919662,0.00022266456,0.0000031869565,0.0021274155],"genre_scores_gemma":[0.9990113,0.000120505,0.00013183035,0.0000041217127,6.822611e-7,0.000004568773,0.00011381451,0.0000012857206,0.0006117648],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999192,0.000004853219,0.000006438626,0.000027983642,0.000023362863,0.000018225792],"domain_scores_gemma":[0.9997099,0.00002575034,0.00012809671,0.000016760396,0.00007657018,0.000042769025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012536882,0.00014770968,0.000119244876,0.0011494051,0.00045798972,0.00060180895,0.00018420581,0.00013832029,0.0019098715],"category_scores_gemma":[0.000405983,0.00014109348,0.00009945746,0.0014034483,0.00069618085,0.00030727516,0.0004851602,0.00015315996,0.00012695935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023986709,0.000027549971,0.8962086,0.00019190337,0.00006481277,0.0013229082,0.007798306,0.00094491435,0.044370167,0.0005324273,0.0003331387,0.047965553],"study_design_scores_gemma":[0.0000022028225,0.000012922765,0.9984841,0.0000074819113,0.0000032493047,0.00014127823,0.00041789433,0.000066404034,0.00009203861,0.000020180174,0.0007493569,0.0000028816526],"about_ca_topic_score_codex":0.2995131,"about_ca_topic_score_gemma":0.5626874,"teacher_disagreement_score":0.2995131,"about_ca_system_score_codex":0.0013407149,"about_ca_system_score_gemma":0.0008751524,"threshold_uncertainty_score":0.59553945},"labels":[],"label_agreement":null},{"id":"W4412318186","doi":"","title":"The Lithosphere beneath Northern Europe: Structure and Evolution over Three Billion Years - Contributions from Geophysical Studies","year":2013,"lang":"en","type":"article","venue":"Helmholtz Centre for Ocean Research Kiel (GEOMAR)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lithosphere; Geology; Geophysics; Seismology; Earth science; Tectonics","score_opus":0.025283973738514372,"score_gpt":0.2779482819512758,"score_spread":0.2526643082127614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412318186","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99555427,0.0025758562,0.00010226484,0.00003887515,0.0000035583848,0.0000016962373,0.00065782754,0.0000076316155,0.0010580738],"genre_scores_gemma":[0.9955043,0.0023471278,0.00024377239,0.000017369957,0.0000075944968,0.000004020066,0.0014012494,0.000004719584,0.0004697973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988604,0.00002002054,0.000013601564,0.000039019025,0.000023442122,0.000017875458],"domain_scores_gemma":[0.9997633,0.000044589106,0.00007831112,0.000033998036,0.00005450032,0.000025313238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034598252,0.00021226126,0.00020099228,0.0010474499,0.0002227436,0.0007234384,0.00017551582,0.00017921891,0.00079174805],"category_scores_gemma":[0.000514274,0.00011666587,0.00031857518,0.0026695519,0.00021244914,0.0003757492,0.0005620527,0.00008943126,0.00017744],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054317938,0.000008420082,0.967855,0.00008417052,0.00016790789,0.00022244519,0.0007536511,0.00042828394,0.0013938637,0.00012667368,0.00018610751,0.028719267],"study_design_scores_gemma":[3.9887962e-7,0.000003768614,0.998735,0.000010207526,0.000018544426,0.00007920053,0.00016059374,0.000063243126,0.00006698363,0.000021552283,0.0008391159,0.000001329183],"about_ca_topic_score_codex":0.014707772,"about_ca_topic_score_gemma":0.019551525,"teacher_disagreement_score":0.014707772,"about_ca_system_score_codex":0.0003360773,"about_ca_system_score_gemma":0.00029030972,"threshold_uncertainty_score":0.029244304},"labels":[],"label_agreement":null},{"id":"W4412365704","doi":"10.1007/s11600-025-01632-3","title":"Seismotectonic implications and strong ground motion modulation of recent significant earthquakes at the North Central Red Sea, Western Saudi Arabia","year":2025,"lang":"en","type":"article","venue":"Acta Geophysica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Structural geology; Seismology; Geology; Ground motion; Motion (physics); Geodesy; Physics","score_opus":0.01878269073943391,"score_gpt":0.2252161584169308,"score_spread":0.20643346767749687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412365704","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992974,0.000095831754,0.000017163558,0.00005654532,0.0000033407377,7.647823e-7,0.000050138442,6.507495e-7,0.0004781735],"genre_scores_gemma":[0.9996673,0.000087005865,0.00001565112,0.000011343576,0.000004788181,4.5739554e-7,0.000052842788,3.9726407e-7,0.00016032951],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991715,0.000013818455,0.00001201959,0.000015358019,0.00001519675,0.0000264329],"domain_scores_gemma":[0.9995752,0.00006876225,0.00013894397,0.000018452492,0.00014048678,0.000058110072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002395427,0.00017769514,0.000121605306,0.0008101418,0.00049816724,0.0006799482,0.00028003764,0.00029457128,0.0011711591],"category_scores_gemma":[0.00073222036,0.000120468125,0.00014445587,0.00095563906,0.00039571646,0.00030689075,0.0004749525,0.00022169543,0.00018848538],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033157112,0.000058996477,0.9637533,0.0000683357,0.000069055095,0.001062429,0.0036266714,0.00095966074,0.009888649,0.00033466314,0.00027491816,0.019571694],"study_design_scores_gemma":[0.0000034161028,0.000021100372,0.9972337,0.0000074632694,0.0000144072865,0.00008617638,0.0018431386,0.00023824078,0.00014798154,0.000024409119,0.00037687708,0.0000031024929],"about_ca_topic_score_codex":0.07363179,"about_ca_topic_score_gemma":0.12034748,"teacher_disagreement_score":0.07363179,"about_ca_system_score_codex":0.00074941356,"about_ca_system_score_gemma":0.0006209458,"threshold_uncertainty_score":0.14640641},"labels":[],"label_agreement":null},{"id":"W4412395844","doi":"10.1038/s41467-025-61598-0","title":"Magmatic underplating and crustal intrusions accommodate extension during Red Sea continental rifting","year":2025,"lang":"en","type":"article","venue":"Nature Communications","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Università degli Studi di Pavia; Ministero dell’Istruzione, dell’Università e della Ricerca","keywords":"Underplating; Rift; Geology; Extension (predicate logic); Continental crust; Earth science; Paleontology; Tectonics; Subduction; Computer science","score_opus":0.01574071862188643,"score_gpt":0.267571304343963,"score_spread":0.25183058572207656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412395844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99972874,0.000044056927,0.000016459639,0.0000038040941,3.82786e-7,4.5870183e-7,0.000019594081,0.0000013463521,0.00018502741],"genre_scores_gemma":[0.999795,0.000032304484,0.000029148012,0.0000029329074,8.997205e-7,4.7063077e-7,0.000041635976,7.681455e-7,0.00009681901],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999946,0.00000643479,0.0000039216798,0.000015160912,0.0000075273233,0.00002096404],"domain_scores_gemma":[0.9998772,0.0000146819075,0.000059094153,0.000008458919,0.000020282954,0.000020255042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011534378,0.00016254457,0.00016413913,0.0005434469,0.00022351948,0.00042344598,0.00015923545,0.00019421465,0.00050708983],"category_scores_gemma":[0.00027787065,0.00012308246,0.000121128025,0.0003820684,0.00027974093,0.00021436714,0.00024836976,0.00016512936,0.000108619395],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020856825,0.000018680548,0.9023918,0.000038253012,0.0000373412,0.00049088226,0.0013967473,0.00066445634,0.0846923,0.00014007685,0.000040663115,0.009880229],"study_design_scores_gemma":[8.7830625e-7,0.000015877453,0.9985764,0.0000024319922,0.000004926488,0.000041967018,0.00026185525,0.00015408333,0.00082544034,0.000011869049,0.00010290587,0.0000014198004],"about_ca_topic_score_codex":0.010543104,"about_ca_topic_score_gemma":0.027920065,"teacher_disagreement_score":0.010543104,"about_ca_system_score_codex":0.0003517151,"about_ca_system_score_gemma":0.00021296775,"threshold_uncertainty_score":0.02096349},"labels":[],"label_agreement":null},{"id":"W4412444300","doi":"10.26443/seismica.v4i2.1303","title":"Seismicity and Surface Deformation in Kamanjab Inlier, Northern Namibia","year":2025,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; McGill University","funders":"","keywords":"Geology; Induced seismicity; Seismology; Deformation (meteorology); Surface (topology); Geodesy; Geomorphology; Geometry; Oceanography","score_opus":0.006934427402713624,"score_gpt":0.20327300433916684,"score_spread":0.1963385769364532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412444300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970487,0.0002456748,0.000052704265,0.00015396737,0.000005399243,0.00001348737,0.0011945405,0.0000075239886,0.0012781161],"genre_scores_gemma":[0.9975637,0.00032217134,0.00020284455,0.00008323612,0.000010647905,0.000036276644,0.0012290496,0.0000062588756,0.00054576993],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988055,0.000020938733,0.000011848619,0.000016932623,0.000014055589,0.000055714434],"domain_scores_gemma":[0.9998435,0.00001758917,0.0000637332,0.000006052301,0.000027003814,0.000042010008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014138884,0.00041397245,0.00025344666,0.0013256182,0.0009249062,0.00075140054,0.00030422234,0.00036117854,0.0025892819],"category_scores_gemma":[0.00054665987,0.00023032833,0.00016173784,0.0026905893,0.0003714352,0.00038548364,0.0006051383,0.00019003043,0.00034602545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003037328,0.00019861238,0.9486439,0.00025107892,0.0001471414,0.002577957,0.0101832,0.00062610785,0.010157666,0.0002757202,0.0017803422,0.024854485],"study_design_scores_gemma":[0.000012359333,0.000020998425,0.99243915,0.000032074702,0.00001935809,0.00021681614,0.0052146437,0.00023280042,0.00015761996,0.000030867803,0.001615462,0.000007852249],"about_ca_topic_score_codex":0.18419781,"about_ca_topic_score_gemma":0.35254228,"teacher_disagreement_score":0.18419781,"about_ca_system_score_codex":0.001508578,"about_ca_system_score_gemma":0.0006356821,"threshold_uncertainty_score":0.36625135},"labels":[],"label_agreement":null},{"id":"W4412450397","doi":"10.1029/2025gl116050","title":"Large Surface‐Rupturing Earthquakes and a &gt;12 kyr, Open Interseismic Interval on the Tintina Fault, Yukon","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Alberta; University of Victoria","funders":"Canada Foundation for Innovation; Polar Knowledge Canada; University of Victoria; British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; Yukon Foundation","keywords":"Geology; Seismology; Fault (geology); Interval (graph theory)","score_opus":0.04721395939675155,"score_gpt":0.3122501077528456,"score_spread":0.26503614835609407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412450397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994361,0.000039740673,0.000026283797,0.000008965787,0.0000010318992,0.0000018881084,0.00007330168,0.0000022863114,0.00041027702],"genre_scores_gemma":[0.99962795,0.000024517332,0.00002840274,0.0000049976575,6.2101685e-7,0.0000012009416,0.00014115643,6.416809e-7,0.0001705735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999198,0.0000048509596,0.000006525912,0.000019822714,0.000017345896,0.000031560547],"domain_scores_gemma":[0.999701,0.00001929617,0.00006644244,0.000017399718,0.000102279424,0.00009355866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009579471,0.00015871853,0.00014993288,0.0006555939,0.0007726262,0.00046481457,0.0002470234,0.00021438676,0.00087214855],"category_scores_gemma":[0.0003545962,0.00011548189,0.00010509131,0.0007862464,0.0005239949,0.00015823996,0.0005261605,0.00015968064,0.00010155166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007127937,0.00001779634,0.9859584,0.00001999103,0.000036495316,0.00053808675,0.0010320374,0.00015952725,0.006259564,0.000078456906,0.0001227404,0.005705652],"study_design_scores_gemma":[0.0000013814172,0.00000928565,0.9991788,0.000002256871,0.0000045756965,0.000066831046,0.0004540318,0.000047755213,0.00005968895,0.000009989256,0.00016398214,0.00000134417],"about_ca_topic_score_codex":0.43041706,"about_ca_topic_score_gemma":0.7363477,"teacher_disagreement_score":0.56958294,"about_ca_system_score_codex":0.0018524561,"about_ca_system_score_gemma":0.0013391089,"threshold_uncertainty_score":0.8558235},"labels":[],"label_agreement":null},{"id":"W4412493980","doi":"10.1126/sciadv.adt3003","title":"Seismic imaging reveals a strain-partitioned sliver and nascent megathrust at an incipient subduction zone in the northeast Pacific","year":2025,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; University of British Columbia; Dalhousie University","funders":"","keywords":"Subduction; Geology; Seismology; Forearc; Episodic tremor and slip; Convergent boundary; Thrust fault; Pacific Plate; Plate tectonics; Décollement; Crust; Slip (aerodynamics); Oceanic crust; Fault (geology); Tectonics; Paleontology","score_opus":0.010256577517920822,"score_gpt":0.24376717086810223,"score_spread":0.2335105933501814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412493980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974942,0.000058973845,0.00020927412,0.000066902954,0.0000019279787,0.000006991942,0.00017777694,0.00002683206,0.0019571749],"genre_scores_gemma":[0.9988232,0.000070289716,0.00044587452,0.000027655966,0.0000030329888,0.0000038730345,0.00021046522,0.000004738964,0.00041087504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999684,0.0000012239149,0.0000011019315,0.000008622479,0.000009588234,0.000011165132],"domain_scores_gemma":[0.99992204,0.0000066167204,0.000019248124,0.0000057922744,0.00001348164,0.000032841923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000054893357,0.000179775,0.00012813458,0.000532016,0.00035242367,0.00034856587,0.00024997836,0.00026591672,0.0009289631],"category_scores_gemma":[0.00016744649,0.00017668819,0.00005926057,0.00043186243,0.00037792514,0.0001383547,0.00043045633,0.00030319908,0.000133754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042745666,0.0001466628,0.6192908,0.00015380306,0.00007113507,0.008673368,0.0036667872,0.0024228771,0.31570262,0.00070146256,0.0024622644,0.046280704],"study_design_scores_gemma":[0.00000991835,0.000037017675,0.9933976,0.000015774125,0.000012291898,0.0007284425,0.000680463,0.0020984234,0.0021114869,0.00006886938,0.00083395565,0.000005723764],"about_ca_topic_score_codex":0.05063049,"about_ca_topic_score_gemma":0.11495197,"teacher_disagreement_score":0.05063049,"about_ca_system_score_codex":0.0003124427,"about_ca_system_score_gemma":0.00050957163,"threshold_uncertainty_score":0.10067153},"labels":[],"label_agreement":null},{"id":"W4412494094","doi":"10.1126/sciadv.adv6484","title":"Long-term dynamics of earthquake swarms in the Yellowstone caldera","year":2025,"lang":"en","type":"article","venue":"Science Advances","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Geology; Seismology; Caldera; Induced seismicity; Volcano; Hypocenter; Earthquake swarm; Context (archaeology); Swarm behaviour; Paleontology","score_opus":0.01059965789559229,"score_gpt":0.2621452957530931,"score_spread":0.2515456378575008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412494094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99961936,0.00003275511,0.00010920817,0.000023161047,7.4858514e-7,0.0000011221722,0.00013868521,0.0000048719057,0.000070044836],"genre_scores_gemma":[0.99938023,0.000030493353,0.00015245558,0.000005297702,0.0000015809042,0.0000018634497,0.0003487743,0.000001658971,0.00007772491],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994063,0.000007044372,0.000005248079,0.000027156466,0.0000073707743,0.000012529539],"domain_scores_gemma":[0.99967206,0.000060582934,0.00010203311,0.000034721175,0.00006640922,0.000064222906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002316776,0.00012767198,0.00017792928,0.0007685686,0.00022751513,0.00041179586,0.00022696957,0.0002512395,0.00042750916],"category_scores_gemma":[0.0010993294,0.00015498238,0.00014758944,0.0006374157,0.0002859083,0.0003828052,0.00058362633,0.00022124861,0.00008442864],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038534396,0.00003358518,0.9780191,0.000013829465,0.000052489053,0.00013230008,0.00030101353,0.008516898,0.0044946135,0.00019123807,0.00031018362,0.007896218],"study_design_scores_gemma":[0.0000045876636,0.000011601516,0.977774,0.000005689741,0.000010852731,0.000020304713,0.00014362916,0.021490036,0.00017686684,0.00010907637,0.00024927026,0.000003980331],"about_ca_topic_score_codex":0.04567797,"about_ca_topic_score_gemma":0.081096165,"teacher_disagreement_score":0.04567797,"about_ca_system_score_codex":0.00072310027,"about_ca_system_score_gemma":0.00031295785,"threshold_uncertainty_score":0.09082419},"labels":[],"label_agreement":null},{"id":"W4412548579","doi":"10.1007/s10291-025-01932-7","title":"Correction To: “EPC: MATLAB software to estimate Euler pole parameters”","year":2025,"lang":"en","type":"erratum","venue":"GPS Solutions","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"MATLAB; Software; Euler's formula; Computer science; Mathematics; Applied mathematics; Control theory (sociology); Mathematical analysis; Artificial intelligence; Operating system","score_opus":0.024819262187603337,"score_gpt":0.2635330337248121,"score_spread":0.2387137715372088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412548579","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005565585,0.00079293246,0.008897979,0.024489596,0.85893214,0.00019150318,0.05188825,0.011452148,0.042798877],"genre_scores_gemma":[0.008540309,0.0015223128,0.018379513,0.019696558,0.05660773,0.00058438326,0.05610913,0.018913798,0.8196462],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9968362,0.00037664568,0.00048817278,0.00034505792,0.0016834704,0.00027046466],"domain_scores_gemma":[0.96870416,0.003949671,0.0010778853,0.0021732938,0.023355843,0.0007390643],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001446425,0.0029368012,0.001772536,0.006046235,0.0029498767,0.0043835286,0.0031434468,0.0035446838,0.33744556],"category_scores_gemma":[0.035700303,0.0013850426,0.0016797091,0.0041476437,0.0011751407,0.0031377338,0.0027095296,0.0057049766,0.28608826],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001267571,0.0000033535405,0.000022709928,0.00003779158,0.0000023304626,0.00001784004,0.000005036388,0.00005530027,0.000020385041,0.0002267434,0.9969298,0.0026660846],"study_design_scores_gemma":[0.000050091694,0.000010152211,0.0006725088,0.00017217832,0.000013103264,0.00008589107,0.00005024657,0.0005423171,0.00045493612,0.0014540527,0.99646145,0.000033135628],"about_ca_topic_score_codex":0.04743842,"about_ca_topic_score_gemma":0.06161106,"teacher_disagreement_score":0.33744556,"about_ca_system_score_codex":0.0031032336,"about_ca_system_score_gemma":0.005359052,"threshold_uncertainty_score":0.9450535},"labels":[],"label_agreement":null},{"id":"W4412596509","doi":"10.1785/0220240427","title":"A Single-Station Earthquake Catalog for the Endeavour Segment of the Juan de Fuca Ridge (2011–2016): Challenges and Implications for the Spreading Cycle","year":2025,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Ridge; Geology; Seismology; Oceanography; Paleontology","score_opus":0.11172629338367439,"score_gpt":0.3292075828157065,"score_spread":0.2174812894320321,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412596509","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9541187,0.0013054189,0.0022041355,0.00046772018,0.000047443296,0.00007134823,0.038376026,0.0001850872,0.003224085],"genre_scores_gemma":[0.9085462,0.0009738268,0.0074277297,0.000053679778,0.0001171667,0.000113497335,0.0812189,0.00006699933,0.0014820395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994734,0.00005825907,0.000080339036,0.00013335532,0.00016219818,0.00009258579],"domain_scores_gemma":[0.99479216,0.0005094697,0.0013587401,0.00079393154,0.0020146978,0.0005309272],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015830698,0.00038115363,0.00042780637,0.005344113,0.0006061306,0.0011348553,0.00060133735,0.00038915433,0.0012551347],"category_scores_gemma":[0.005222828,0.00015946443,0.0002678434,0.0057116454,0.00025729893,0.0009270916,0.0010248247,0.00023867207,0.0006062606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052672487,0.00003196332,0.9385143,0.00019895931,0.00006461038,0.00015288689,0.00048176566,0.0014004245,0.001855033,0.00027325464,0.00506457,0.0519096],"study_design_scores_gemma":[0.000004694735,0.000018748466,0.9864699,0.00009800735,0.000026990527,0.000099809884,0.00055269775,0.0025647215,0.00031018557,0.00014411549,0.009696397,0.000013627654],"about_ca_topic_score_codex":0.087326914,"about_ca_topic_score_gemma":0.11860571,"teacher_disagreement_score":0.087326914,"about_ca_system_score_codex":0.0009223155,"about_ca_system_score_gemma":0.0016482453,"threshold_uncertainty_score":0.17363721},"labels":[],"label_agreement":null},{"id":"W4412613706","doi":"10.1785/0220250018","title":"Refined Stochastic Source Modeling and Selection Method for Complex Fault Systems Considering Data Uncertainty: A Case Study of the 2019 Ridgecrest Earthquakes","year":2025,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Fault (geology); Selection (genetic algorithm); Seismology; Geology; Computer science; Data mining; Machine learning","score_opus":0.20755348483438418,"score_gpt":0.389616949704815,"score_spread":0.1820634648704308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412613706","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.051768027,0.00007829935,0.9472074,0.00007355585,0.000005689018,0.000035205656,0.00004890847,0.00017341773,0.000609514],"genre_scores_gemma":[0.87347806,0.00013404872,0.12486373,0.000020139692,0.000020812553,0.00009756103,0.00015377456,0.000054305136,0.0011775319],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995732,0.00020286332,0.00002235758,0.00005792902,0.00010803293,0.000035603844],"domain_scores_gemma":[0.9985671,0.0009928513,0.00012524285,0.00006088919,0.00021645123,0.000037460723],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013276556,0.0005888038,0.0006738472,0.00077994337,0.00029045448,0.00063190167,0.00062122557,0.00053170195,0.0010459262],"category_scores_gemma":[0.0022552395,0.00029132728,0.0007888746,0.00047488097,0.00027433355,0.00042415372,0.00059281447,0.00046229566,0.00015774582],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037618713,0.000023568346,0.0014713588,0.000026575999,0.00002560065,0.0001670189,0.000054651973,0.9734169,0.0016968686,0.002815156,0.00016600562,0.020098686],"study_design_scores_gemma":[0.000001151266,0.000004347092,0.0000932522,7.527088e-7,0.0000018683347,0.00000759472,0.0000032865496,0.9994862,0.0001166253,0.00023230391,0.000051010644,0.0000015605103],"about_ca_topic_score_codex":0.005776009,"about_ca_topic_score_gemma":0.0042012185,"teacher_disagreement_score":0.005776009,"about_ca_system_score_codex":0.00041636964,"about_ca_system_score_gemma":0.0006529397,"threshold_uncertainty_score":0.011484802},"labels":[],"label_agreement":null},{"id":"W4412666481","doi":"10.1111/ter.70005","title":"Forearc Depressions Develop in Warm Subduction Zones by Underplating‐Induced Crustal Flexure","year":2025,"lang":"en","type":"article","venue":"Terra Nova","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; Simon Fraser University","keywords":"Forearc; Geology; Underplating; Subduction; Seismology; Tectonics","score_opus":0.03512265617099848,"score_gpt":0.2767858386956592,"score_spread":0.24166318252466074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412666481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99384636,0.00012172166,0.0028329166,0.000083852574,0.000003991217,0.000021124557,0.00006196336,0.000047852314,0.0029802122],"genre_scores_gemma":[0.9990152,0.000035475034,0.00041457926,0.000008954272,0.0000014778317,0.0000032601579,0.0000362703,0.0000019909492,0.00048285123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994826,0.0000046926307,0.0000031543252,0.000018058321,0.0000063468224,0.00001960444],"domain_scores_gemma":[0.9998989,0.000007710891,0.000036116566,0.00001587901,0.00001026911,0.000031102347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012454193,0.00023328685,0.00016769655,0.0003390617,0.000249373,0.000711329,0.0005218499,0.00041016468,0.0017079455],"category_scores_gemma":[0.00019166144,0.000267859,0.00040511918,0.0002200142,0.0005496256,0.00036781724,0.0004342245,0.00021081169,0.00028436174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038840127,0.00017480006,0.66304386,0.00018882577,0.00018166349,0.0038626324,0.0010361437,0.0734412,0.22143708,0.01640584,0.0010645337,0.018775],"study_design_scores_gemma":[0.000084572486,0.00039691644,0.855877,0.000030275842,0.00009486495,0.002355468,0.0010602351,0.11202122,0.012714942,0.0108941905,0.0044310507,0.000039216895],"about_ca_topic_score_codex":0.0049622026,"about_ca_topic_score_gemma":0.0057866517,"teacher_disagreement_score":0.0049622026,"about_ca_system_score_codex":0.00062334107,"about_ca_system_score_gemma":0.00023568528,"threshold_uncertainty_score":0.009866655},"labels":[],"label_agreement":null},{"id":"W4412685903","doi":"10.3389/feart.2025.1568069","title":"Risk-based multi-hazard microzonation for earthquakes and tsunamis","year":2025,"lang":"en","type":"article","venue":"Frontiers in Earth Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Seismic microzonation; Geology; Hazard; Earthquake scenario; Seismic hazard; Urban seismic risk","score_opus":0.009719501559608422,"score_gpt":0.23228612484906688,"score_spread":0.22256662328945845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412685903","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.35346302,0.00020778053,0.63847744,0.00022477703,0.000032330452,0.00023010021,0.0014481953,0.0015440311,0.004372306],"genre_scores_gemma":[0.8592538,0.00011237624,0.13806893,0.000014777067,0.000009638609,0.000115693605,0.00060132745,0.000087981985,0.0017355307],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982244,0.000053098232,0.0000116893,0.00004348764,0.00005094806,0.00001840157],"domain_scores_gemma":[0.9993777,0.00031949108,0.00012415483,0.00006016574,0.00007979138,0.00003864576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005241577,0.0005707711,0.00029677962,0.0012886174,0.00020840087,0.00071540254,0.0006598608,0.0002843086,0.0024516876],"category_scores_gemma":[0.0020593845,0.00024547125,0.0005655691,0.00068503973,0.00020562396,0.0006911242,0.00081708684,0.00042454796,0.00018845484],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014524668,0.000103099395,0.034844846,0.000100069934,0.000101063335,0.00016382155,0.00036630948,0.8598938,0.0034042536,0.0052904035,0.0011793751,0.09440771],"study_design_scores_gemma":[0.0000058111873,0.000028952154,0.009288488,0.0000065042623,0.000009139064,0.000052154897,0.000103394705,0.9866803,0.00067901995,0.0024470994,0.00068394246,0.000015285432],"about_ca_topic_score_codex":0.015805703,"about_ca_topic_score_gemma":0.027454073,"teacher_disagreement_score":0.015805703,"about_ca_system_score_codex":0.00060232397,"about_ca_system_score_gemma":0.00056901074,"threshold_uncertainty_score":0.031427383},"labels":[],"label_agreement":null},{"id":"W4412737985","doi":"10.1016/j.tecto.2025.230863","title":"Rethinking the 1946 Chatkal earthquake: Contributions of Pléiades and UAV images to a surface-rupturing event along the Talas-Fergana Fault","year":2025,"lang":"en","type":"article","venue":"Tectonophysics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Institut national des sciences de l'Univers; Conseil National de la Recherche Scientifique; Centre National d’Etudes Spatiales; Centre National de la Recherche Scientifique; Aix-Marseille Université; Fondation Aix-Marseille Universite; Centre national d'études spatiales","keywords":"Geology; Seismology; Fault (geology); Surface rupture; Event (particle physics); Intraplate earthquake; Tectonics","score_opus":0.010687029971463322,"score_gpt":0.23755951965997057,"score_spread":0.22687248968850726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412737985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99842995,0.00017228596,0.00014488713,0.000040972347,0.000011750075,0.0000068829,0.00020835573,0.000017727978,0.000967012],"genre_scores_gemma":[0.9986203,0.00014671149,0.0006396617,0.000019705481,0.000013884585,0.0000032478733,0.00037147687,0.000007265742,0.00017769489],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990296,0.000011134501,0.0000042524266,0.000028308754,0.000021453061,0.000031880096],"domain_scores_gemma":[0.99983895,0.000022579648,0.00004214272,0.00002065217,0.00003859415,0.000037035228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018597858,0.00026051907,0.00019373209,0.0010482196,0.00025097685,0.0007109135,0.00019712184,0.00034383175,0.00047621256],"category_scores_gemma":[0.00049495883,0.00017195003,0.00019143148,0.00067711354,0.00024288315,0.0004217196,0.00044878037,0.00026023109,0.00015000167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046534318,0.0001871797,0.81004435,0.00019215948,0.00020379681,0.0022799394,0.003370835,0.0045846743,0.087017745,0.0002784794,0.0016878641,0.08968769],"study_design_scores_gemma":[0.0000056495255,0.000024320876,0.9936684,0.000023621727,0.000038267473,0.00013993496,0.00095457945,0.0032897268,0.00094090006,0.000028736882,0.000875879,0.000009930727],"about_ca_topic_score_codex":0.020784851,"about_ca_topic_score_gemma":0.06946423,"teacher_disagreement_score":0.020784851,"about_ca_system_score_codex":0.00030696683,"about_ca_system_score_gemma":0.00025450412,"threshold_uncertainty_score":0.041327775},"labels":[],"label_agreement":null},{"id":"W4412908833","doi":"10.1093/gji/ggaf284","title":"Oligocene North American kinematic change driven by Canary plume activity","year":2025,"lang":"en","type":"article","venue":"Geophysical Journal International","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Geocenter Danmark","keywords":"Geology; Kinematics; Plume; Physical geography; Seismology; Earth science; Meteorology; Geography","score_opus":0.014395026116686884,"score_gpt":0.24559976973707995,"score_spread":0.23120474362039306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412908833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99604684,0.00009198459,0.00020532456,0.00005725949,0.0000059238764,0.0000032855671,0.0010096367,0.000035863937,0.0025438885],"genre_scores_gemma":[0.9978206,0.0000998602,0.00037752636,0.00001471395,0.0000053177287,0.0000062378763,0.0013229018,0.000010806532,0.00034193837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998702,0.000013221269,0.0000076024717,0.000046634876,0.000037286733,0.000024978995],"domain_scores_gemma":[0.99956065,0.00004726969,0.00010299227,0.00006272149,0.0001897281,0.000036675112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023436251,0.00023541175,0.00016071016,0.0010940249,0.00043936103,0.00068944925,0.0003253161,0.00015684411,0.002144893],"category_scores_gemma":[0.0010381829,0.00015133299,0.00018354009,0.0018440053,0.00037066106,0.00030650012,0.00046423273,0.00024114312,0.00027605367],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017232739,0.00002965355,0.9603492,0.000061989886,0.00012547453,0.00016122917,0.00076111377,0.005587301,0.009832525,0.00041613023,0.0009796965,0.021523297],"study_design_scores_gemma":[0.0000031692327,0.000008087271,0.9949248,0.0000108490085,0.000019365678,0.00003489271,0.00020675387,0.0026968166,0.00063956185,0.000069324706,0.0013790599,0.00000737951],"about_ca_topic_score_codex":0.16094999,"about_ca_topic_score_gemma":0.27161264,"teacher_disagreement_score":0.16094999,"about_ca_system_score_codex":0.0010435301,"about_ca_system_score_gemma":0.0005184359,"threshold_uncertainty_score":0.32002634},"labels":[],"label_agreement":null},{"id":"W4412913040","doi":"10.1785/0220250149","title":"Reflections on a Trio of North American Earthquakes in 1925","year":2025,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; History","score_opus":0.10046501955409583,"score_gpt":0.3825089840106771,"score_spread":0.2820439644565813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412913040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6954327,0.016137516,0.0010038407,0.1337046,0.008395949,0.000044091717,0.0015460125,0.00009888539,0.14363636],"genre_scores_gemma":[0.94732153,0.006175647,0.0003576647,0.014017002,0.0045401617,0.000029341802,0.0007326223,0.000052302785,0.026773764],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9996377,0.00007037616,0.000018698918,0.00005084541,0.00009692728,0.0001255104],"domain_scores_gemma":[0.99907744,0.00023342986,0.0002066631,0.00006452373,0.00027276092,0.00014525028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010787289,0.0003251437,0.00015862094,0.00078829256,0.003621262,0.0018886836,0.00035475258,0.0012932792,0.003233477],"category_scores_gemma":[0.0017384065,0.00023372586,0.00014227412,0.00089668593,0.0018197456,0.0013632021,0.0019659596,0.002464242,0.00041197296],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009116643,0.00016054367,0.1329903,0.0006537766,0.0001650681,0.0072293184,0.1879862,0.00049297145,0.006641867,0.02782863,0.46602425,0.16891535],"study_design_scores_gemma":[0.00001512766,0.000084133295,0.2676985,0.00042832078,0.000036260208,0.0005466064,0.07289406,0.00011151519,0.0007253443,0.0018326777,0.65557534,0.000052236013],"about_ca_topic_score_codex":0.079871416,"about_ca_topic_score_gemma":0.30076936,"teacher_disagreement_score":0.079871416,"about_ca_system_score_codex":0.0028707327,"about_ca_system_score_gemma":0.0011174643,"threshold_uncertainty_score":0.158813},"labels":[],"label_agreement":null},{"id":"W4413098092","doi":"10.1130/g53588.1","title":"A viable Labrador Sea rifting origin of the Northern Appalachian and related seismic anomalies","year":2025,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Rift; Continental margin; Breakup; Anomaly (physics); Passive margin; Asthenosphere; Paleontology; Magnetic anomaly; Seafloor spreading; Geophysics; Tectonics; Seismology; Lithosphere","score_opus":0.006473404426985648,"score_gpt":0.1959756383374686,"score_spread":0.18950223391048293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413098092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957237,0.00023951357,0.00029541022,0.00016142162,0.0000100628295,0.000006893785,0.00012766871,0.000027127648,0.0034082462],"genre_scores_gemma":[0.9994874,0.00006788088,0.00010288921,0.000019320936,0.000006572239,0.0000030497918,0.00008673391,0.0000023128334,0.000223849],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990606,0.000011644435,0.0000062991835,0.000023942715,0.000013028656,0.00003902297],"domain_scores_gemma":[0.999843,0.000021568414,0.000051188872,0.000012758162,0.00003509082,0.000036483114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015561853,0.000379358,0.0002361403,0.0008484845,0.00081016193,0.0011995175,0.00052605197,0.00045218697,0.002704136],"category_scores_gemma":[0.0004105471,0.00012222539,0.0002396809,0.0006596187,0.0005478927,0.00049064314,0.00056178577,0.0003320093,0.00030083425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022384725,0.00008340091,0.93918836,0.00010700303,0.00015425814,0.0041275145,0.0009237307,0.0061807325,0.022011751,0.0028369643,0.00071197655,0.023450347],"study_design_scores_gemma":[0.000018826762,0.000061752835,0.9778806,0.000053502845,0.000086199754,0.00052479195,0.0019074691,0.015034438,0.0011129772,0.00077474286,0.0025022076,0.000042493088],"about_ca_topic_score_codex":0.06437958,"about_ca_topic_score_gemma":0.07876652,"teacher_disagreement_score":0.06437958,"about_ca_system_score_codex":0.0010032811,"about_ca_system_score_gemma":0.0007702242,"threshold_uncertainty_score":0.12800968},"labels":[],"label_agreement":null},{"id":"W4413128340","doi":"10.1130/g52507.1","title":"Slab break-off and subduction polarity reversal after collision can be very fast","year":2025,"lang":"en","type":"article","venue":"Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Dalhousie University","keywords":"Geology; Slab; Subduction; Collision; Polarity (international relations); Seismology; Geophysics; Geodesy; Tectonics","score_opus":0.0070442297554087485,"score_gpt":0.20464438935484613,"score_spread":0.19760015959943739,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413128340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959021,0.00010162419,0.0011624862,0.000047912526,0.0000052426435,0.0000051008096,0.00010224177,0.000046358153,0.0026269506],"genre_scores_gemma":[0.9997062,0.000031812688,0.00012389422,0.000004451597,0.0000015430666,0.0000013677605,0.000046214984,0.0000021357673,0.000082403305],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990726,0.000010344528,0.000007180289,0.000027459788,0.000020543965,0.000027228923],"domain_scores_gemma":[0.99946505,0.00015868663,0.00020460371,0.00006607659,0.000050003535,0.000055596134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024657373,0.00011225625,0.00018503686,0.0004425206,0.00032921767,0.00070213526,0.00027738808,0.00025569543,0.0022931765],"category_scores_gemma":[0.001711379,0.00013565939,0.00017642153,0.00034316487,0.00056724815,0.00044496806,0.00044966678,0.00022288447,0.0003073452],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005476023,0.0001079507,0.85825586,0.0001510986,0.00015197437,0.001101239,0.0005780169,0.021926383,0.0722276,0.0071860324,0.000895769,0.03687054],"study_design_scores_gemma":[0.000028622195,0.000121759644,0.9687329,0.000014441007,0.000041131774,0.0003487238,0.00054509594,0.014925754,0.008654794,0.0038291968,0.0027339011,0.000023651863],"about_ca_topic_score_codex":0.0031430407,"about_ca_topic_score_gemma":0.0031097059,"teacher_disagreement_score":0.0031430407,"about_ca_system_score_codex":0.00044819873,"about_ca_system_score_gemma":0.00021773846,"threshold_uncertainty_score":0.007671416},"labels":[],"label_agreement":null},{"id":"W4413149815","doi":"10.26443/seismica.v2i4.1163","title":"Evidence for an active transtensional Beaufort Range fault in the northern Cascadia forearc","year":2025,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Forearc; Geology; Beaufort scale; Range (aeronautics); Seismology; Beaufort sea; Fault (geology); Oceanography; Subduction; Tectonics; Aerospace engineering; Engineering; Arctic","score_opus":0.062010749296405696,"score_gpt":0.2909406216000437,"score_spread":0.22892987230363798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413149815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983209,0.00022730354,0.00005643213,0.000054077434,0.0000035279534,0.0000036516876,0.00016215691,0.000014970505,0.0011568691],"genre_scores_gemma":[0.9992424,0.0001317074,0.000107443455,0.000014879743,0.000003359602,0.0000035621147,0.0002663594,0.0000021021247,0.00022827338],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996215,0.000026635871,0.000029082094,0.00012666438,0.00011168312,0.00008438215],"domain_scores_gemma":[0.998705,0.0000882821,0.00048246083,0.00009907514,0.00033106623,0.00029414883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003186238,0.00029466313,0.00022873121,0.0017898398,0.0009287565,0.00066790177,0.00045757275,0.00051204994,0.0010935351],"category_scores_gemma":[0.001146016,0.00032476947,0.00024530818,0.0015527279,0.0008890713,0.00026134824,0.0006060081,0.0003147079,0.00019203406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044242184,0.00001564911,0.989764,0.000031253585,0.00003357439,0.00024668896,0.0006402373,0.0002636057,0.0043585137,0.000044311266,0.00013244692,0.0044254423],"study_design_scores_gemma":[0.0000011813414,0.000006676607,0.9995586,0.000004573238,0.000003828685,0.00004505801,0.00012561254,0.00006077268,0.000036793062,0.000005598404,0.00014937187,0.0000018065001],"about_ca_topic_score_codex":0.33711496,"about_ca_topic_score_gemma":0.54877245,"teacher_disagreement_score":0.66288507,"about_ca_system_score_codex":0.0018296578,"about_ca_system_score_gemma":0.0014734146,"threshold_uncertainty_score":0.6703055},"labels":[],"label_agreement":null},{"id":"W4413167024","doi":"10.1785/0220250130","title":"Seismogenic Potential of Hydraulic Fracturing in the South Montney Play, Northeast British Columbia: A Seismogenic Index Approach","year":2025,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Hydraulic fracturing; Seismology; Index (typography); Geotechnical engineering","score_opus":0.029967563880678595,"score_gpt":0.2611549827853264,"score_spread":0.2311874189046478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413167024","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99646676,0.00005717513,0.00036821232,0.000041073563,0.0000011821206,0.000010866031,0.000666033,0.000017675293,0.002370967],"genre_scores_gemma":[0.99884593,0.00005333989,0.00020861813,0.00000387378,0.000001123027,0.0000046727687,0.00037047383,0.0000030228068,0.0005090696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987304,0.000014245719,0.000008761605,0.000019862888,0.000051815565,0.000032112563],"domain_scores_gemma":[0.9994367,0.00009533997,0.00012506833,0.000030103745,0.00022512533,0.00008752351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021365457,0.00030283708,0.0002025819,0.0033815007,0.0006309583,0.0012708948,0.0005245478,0.00019105166,0.0017176078],"category_scores_gemma":[0.0012143834,0.00013827557,0.00013895443,0.004181251,0.00054275943,0.00026420207,0.00078255235,0.00026493613,0.00016385718],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009729864,0.000047762056,0.9528452,0.000057177327,0.00008583955,0.0005628626,0.001082997,0.016688539,0.0050519533,0.0009656568,0.0008318573,0.021683022],"study_design_scores_gemma":[0.0000021164037,0.000011024461,0.98094064,0.000015134036,0.000013413499,0.000039773295,0.0013379242,0.016520748,0.0002767499,0.00017018017,0.0006598721,0.000012489123],"about_ca_topic_score_codex":0.877295,"about_ca_topic_score_gemma":0.92702514,"teacher_disagreement_score":0.12270498,"about_ca_system_score_codex":0.0045165108,"about_ca_system_score_gemma":0.0027965219,"threshold_uncertainty_score":0.2468552},"labels":[],"label_agreement":null},{"id":"W4413238118","doi":"10.1029/2024jb030976","title":"State of In Situ Stress and Implications for Fault Slip Potential in the Montney Play, Western Canada","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Seismology; Induced seismicity; Borehole; Geomechanics; Fault (geology); Thrust fault; Geotechnical engineering","score_opus":0.028403094553427845,"score_gpt":0.3244767969079105,"score_spread":0.29607370235448266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413238118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99821055,0.000037333808,0.000058286652,0.000030417634,8.06358e-7,0.0000041221183,0.00048222588,0.000007688289,0.001168514],"genre_scores_gemma":[0.9992403,0.00003183995,0.000073492665,0.0000055739565,5.451936e-7,0.0000020000693,0.00023728589,0.0000022076952,0.00040682923],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996983,0.000012295504,0.0000111007985,0.000048547136,0.00012102728,0.00010868378],"domain_scores_gemma":[0.99937797,0.000057515237,0.000106717926,0.000025183737,0.00029081572,0.00014179309],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019307873,0.0002794842,0.00023136589,0.0013983427,0.0015887469,0.001238014,0.00084059016,0.0003253521,0.0018757525],"category_scores_gemma":[0.001087991,0.00018466584,0.00020272778,0.0018685439,0.001110853,0.00030586493,0.0005915679,0.00024154555,0.00016366932],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001240506,0.00003184665,0.9844342,0.000023576176,0.00005121164,0.00043960553,0.0011179834,0.003519824,0.0036712224,0.00026418664,0.00038784675,0.005934406],"study_design_scores_gemma":[0.0000037500704,0.000016641925,0.9939553,0.000011982396,0.0000111544405,0.000045974197,0.0018411633,0.0029836134,0.0005333266,0.000056568002,0.00052768376,0.000012887642],"about_ca_topic_score_codex":0.9802049,"about_ca_topic_score_gemma":0.99341995,"teacher_disagreement_score":0.01979512,"about_ca_system_score_codex":0.0120928865,"about_ca_system_score_gemma":0.006953759,"threshold_uncertainty_score":0.08774048},"labels":[],"label_agreement":null},{"id":"W4413413915","doi":"10.1016/j.jvolgeores.2025.108429","title":"What Triggered the 2021 eruption at Nyiragongo volcano (D.R. Congo)? Unraveling the Complex Interplay between tectonism and magmatism","year":2025,"lang":"en","type":"article","venue":"Journal of Volcanology and Geothermal Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Northeastern University; Innovative Solutions Canada","keywords":"Geology; Magmatism; Volcano; Geochemistry; Earth science; Seismology; Tectonics","score_opus":0.054694259188436546,"score_gpt":0.35703227424244477,"score_spread":0.3023380150540082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413413915","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9760558,0.0034088246,0.00033063334,0.007829327,0.00008428984,0.0000142529825,0.0010526121,0.00000915107,0.01121526],"genre_scores_gemma":[0.99753016,0.0010169707,0.00011736459,0.00034364063,0.000052277373,0.000004086379,0.00028516536,0.000004336599,0.0006459301],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998691,0.00003769691,0.000007102818,0.000025513646,0.000013562955,0.00004690136],"domain_scores_gemma":[0.9995433,0.00011201004,0.0001649866,0.00001270247,0.000093521245,0.00007347879],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006571217,0.00016491425,0.00019474702,0.0004963306,0.000660529,0.0016378212,0.00023816538,0.0008081033,0.0020618367],"category_scores_gemma":[0.0013263709,0.00013667239,0.0001070962,0.00047764802,0.0005339027,0.0010388345,0.00058008754,0.0008542455,0.00022156148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022371156,0.00008703071,0.9218534,0.00052875344,0.00018051126,0.0019868563,0.010245887,0.002095223,0.006617037,0.00620239,0.008200709,0.041778505],"study_design_scores_gemma":[0.00000842784,0.00003714996,0.9651392,0.00025730266,0.000059154052,0.0001833583,0.011485255,0.0020684584,0.000598003,0.0015529632,0.01858604,0.000024710065],"about_ca_topic_score_codex":0.11927689,"about_ca_topic_score_gemma":0.2486354,"teacher_disagreement_score":0.11927689,"about_ca_system_score_codex":0.0025921355,"about_ca_system_score_gemma":0.0011655982,"threshold_uncertainty_score":0.23716521},"labels":[],"label_agreement":null},{"id":"W4413495319","doi":"10.1038/s41561-025-01778-1","title":"Interseismic secondary zone of subsidence during earthquake cycles in subduction zones","year":2025,"lang":"en","type":"article","venue":"Nature Geoscience","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Subduction; Geology; Seismology; Subsidence; Episodic tremor and slip; Tectonics; Geomorphology","score_opus":0.00527926166168335,"score_gpt":0.22351653345931577,"score_spread":0.21823727179763242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413495319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985525,0.000043735196,0.0000670833,0.000003841699,9.2943935e-7,0.0000017088388,0.00008695816,0.0000026123537,0.0012406296],"genre_scores_gemma":[0.99977666,0.000010228087,0.000015096425,0.0000011860303,0.0000010158983,9.0751394e-7,0.00006710441,8.4445077e-7,0.00012690172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999701,0.0000031554082,0.0000030412593,0.0000068455092,0.0000050842064,0.000011720521],"domain_scores_gemma":[0.99973327,0.00006371743,0.00006816236,0.000012177767,0.000048139478,0.00007456202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008843084,0.00008251053,0.00014389402,0.000808625,0.0003242386,0.00040818006,0.00010823094,0.00011670325,0.002003318],"category_scores_gemma":[0.00045540597,0.00006105896,0.00011142548,0.0006497855,0.00020184343,0.00015567419,0.00035900244,0.000090793656,0.0001783701],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012412952,0.00007973052,0.94882476,0.00006151885,0.000053471085,0.00047081197,0.001490962,0.0013802624,0.026889794,0.002015194,0.00050400273,0.016988182],"study_design_scores_gemma":[0.0000028069594,0.000025178288,0.9990845,0.0000022103104,0.0000037912553,0.00004904343,0.00016246908,0.00028003636,0.00017740438,0.00007313982,0.0001383524,0.0000010540614],"about_ca_topic_score_codex":0.0070807254,"about_ca_topic_score_gemma":0.016201837,"teacher_disagreement_score":0.0070807254,"about_ca_system_score_codex":0.0003111597,"about_ca_system_score_gemma":0.00025302655,"threshold_uncertainty_score":0.014079034},"labels":[],"label_agreement":null},{"id":"W4413575299","doi":"10.64628/aam.673s4mmw7","title":"Contrary to popular belief, Eastern Canada is more at risk of earthquakes than perceived","year":2021,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Risk perception; History; Seismology; Psychology; Political science; Epistemology; Geology; Philosophy; Perception","score_opus":0.015447284217754279,"score_gpt":0.21167260250869632,"score_spread":0.19622531829094203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413575299","genre_codex":"empirical","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.64091617,0.0025190294,0.0024879684,0.10982043,0.0007860217,0.000034711276,0.0018437612,0.00007669766,0.2415152],"genre_scores_gemma":[0.96657294,0.0021639417,0.00050366897,0.010354762,0.00024424537,0.000007751812,0.00028763938,0.000025157104,0.019839766],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992569,0.00007014261,0.00001966098,0.00010096539,0.000376767,0.00017558604],"domain_scores_gemma":[0.9938117,0.0017213571,0.000844681,0.00029331062,0.0026425687,0.0006862717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009769896,0.00017645012,0.00028006142,0.00081751053,0.0032844376,0.0038229616,0.0005629653,0.0010516789,0.01531447],"category_scores_gemma":[0.007146219,0.00008110016,0.00017075423,0.0023516817,0.0036717956,0.0012226445,0.0006571086,0.00196982,0.0007484198],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065639487,0.00032542465,0.6031697,0.0005965744,0.0003322288,0.00091246504,0.04227118,0.0009385504,0.0036701467,0.16054718,0.07595315,0.11062701],"study_design_scores_gemma":[0.000066496104,0.00013548165,0.67821544,0.0010284666,0.00023190527,0.0004596693,0.12764892,0.0012258316,0.0026770257,0.02375475,0.16441713,0.00013882446],"about_ca_topic_score_codex":0.83670396,"about_ca_topic_score_gemma":0.8779722,"teacher_disagreement_score":0.16329604,"about_ca_system_score_codex":0.0051694377,"about_ca_system_score_gemma":0.010217331,"threshold_uncertainty_score":0.3285154},"labels":[],"label_agreement":null},{"id":"W4413585359","doi":"10.64628/aam.9q6qpw4tg","title":"A new earthquake warning system will prepare Canada for dangerous shaking","year":2022,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"","keywords":"Earthquake warning system; Warning system; Computer security; Seismology; Business; Geology; Forensic engineering; Computer science; Engineering; Telecommunications","score_opus":0.02129798471735786,"score_gpt":0.2211308038288875,"score_spread":0.19983281911152964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413585359","genre_codex":"other","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13061647,0.0011177765,0.06842222,0.10366982,0.010842739,0.00061871693,0.041828524,0.010607129,0.6322766],"genre_scores_gemma":[0.41968456,0.00095127785,0.0892316,0.004765929,0.00053824193,0.00009755242,0.011998959,0.0010437276,0.47168827],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99944955,0.00003879821,0.000012631277,0.00003239104,0.00029529483,0.00017137981],"domain_scores_gemma":[0.99814403,0.00006701655,0.000033700027,0.00009553611,0.0014090475,0.00025064536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007696009,0.000532698,0.00026782093,0.0007599812,0.0020296846,0.002500337,0.0005995076,0.0014721103,0.03359185],"category_scores_gemma":[0.0031389259,0.00023605228,0.0003804385,0.00073148735,0.00044957382,0.0010358766,0.0008473731,0.0011220141,0.0032628481],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002268842,0.00009826237,0.016594062,0.00010463686,0.000058316713,0.00021045886,0.0003803172,0.008566788,0.004239448,0.09930692,0.72599804,0.144216],"study_design_scores_gemma":[0.00012440293,0.00005168649,0.029414132,0.00008536913,0.00008578273,0.00012811,0.0012545955,0.043494567,0.005484085,0.023662696,0.8960887,0.00012583766],"about_ca_topic_score_codex":0.94462615,"about_ca_topic_score_gemma":0.9674626,"teacher_disagreement_score":0.055373847,"about_ca_system_score_codex":0.01319627,"about_ca_system_score_gemma":0.04092911,"threshold_uncertainty_score":0.112375915},"labels":[],"label_agreement":null},{"id":"W4413636482","doi":"10.1175/jcli-d-24-0554.1","title":"Seasonal ITCZ Control on ENSO Responses to Extratropical Volcanic Forcing","year":2025,"lang":"en","type":"article","venue":"Journal of Climate","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Université du Québec à Montréal","funders":"Institute for Basic Science; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; Deutsches Klimarechenzentrum","keywords":"Extratropical cyclone; Climatology; Forcing (mathematics); Intertropical Convergence Zone; El Niño Southern Oscillation; Environmental science; Volcano; Geology; Meteorology; Geography; Precipitation","score_opus":0.01437224669471201,"score_gpt":0.2632819635900919,"score_spread":0.2489097168953799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413636482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99911386,0.00003471155,0.00014470292,0.000020750254,0.000004155346,0.0000023779996,0.00024118478,0.000012690572,0.00042556564],"genre_scores_gemma":[0.9996911,0.000018264747,0.00003898758,0.0000052906394,0.0000021173469,0.0000014337032,0.00018676168,0.0000032362193,0.000052819203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999018,0.00002694316,0.0000086249975,0.000028055947,0.000011889903,0.00002266532],"domain_scores_gemma":[0.9997043,0.000076926786,0.000064787004,0.00004896395,0.00004490447,0.000060009563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002491477,0.00021051764,0.00023964254,0.00017631962,0.00017067998,0.00039081468,0.00014653325,0.00013414318,0.0012050483],"category_scores_gemma":[0.00069734524,0.00009877223,0.00030490212,0.00016951578,0.00020460736,0.00020233018,0.0003456985,0.00019646942,0.00008547715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007104899,0.00012078241,0.7999602,0.00011015953,0.0006268667,0.0002731797,0.0002662079,0.08864277,0.096775286,0.0009486172,0.0009688928,0.010596502],"study_design_scores_gemma":[0.000019354286,0.000039208822,0.9676924,0.000004883618,0.00003677642,0.00002182766,0.000109503926,0.0298432,0.0015415734,0.00013436549,0.00054765906,0.000009352778],"about_ca_topic_score_codex":0.008453441,"about_ca_topic_score_gemma":0.012174103,"teacher_disagreement_score":0.008453441,"about_ca_system_score_codex":0.0002671884,"about_ca_system_score_gemma":0.0001874005,"threshold_uncertainty_score":0.01680845},"labels":[],"label_agreement":null},{"id":"W4413929669","doi":"10.1785/0120250089","title":"Exploring Seismic Hazard Scenarios of Potentially Active Faults in the Southern Coast Mountains of British Columbia, Canada","year":2025,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada; University of British Columbia","funders":"","keywords":"Active fault; Seismic hazard; Geology; Seismology; Hazard; Fault (geology); Ecology","score_opus":0.018677330465549702,"score_gpt":0.19318592730294729,"score_spread":0.17450859683739758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413929669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99717736,0.000067248766,0.00043029131,0.00011614979,0.0000015381183,0.000016063632,0.00064916495,0.000014103421,0.0015280262],"genre_scores_gemma":[0.998831,0.00004839879,0.00032697877,0.000009006922,7.0261234e-7,0.0000039230304,0.00039693154,0.0000018656343,0.0003810943],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997433,0.000049083486,0.000008904827,0.000040426494,0.000053253665,0.00010496879],"domain_scores_gemma":[0.9992029,0.00026015803,0.00009995611,0.000037582977,0.0002772489,0.00012210771],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004526372,0.00037114564,0.00019777287,0.0012616863,0.0008775026,0.001095382,0.0009157804,0.00043224607,0.0012728136],"category_scores_gemma":[0.0020657042,0.00019049103,0.00028944525,0.0015722653,0.0005356202,0.0003145645,0.0004315299,0.00029958834,0.000062950465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023352006,0.00008537916,0.5264751,0.000060687697,0.00012325156,0.0008820342,0.00038571804,0.45235732,0.0013846351,0.0024219407,0.0018318662,0.013758613],"study_design_scores_gemma":[0.0000438509,0.000068193054,0.38087758,0.00003257998,0.00007980685,0.00015859972,0.0027953621,0.6120674,0.00050744484,0.0013864933,0.0019388823,0.000043645054],"about_ca_topic_score_codex":0.9690897,"about_ca_topic_score_gemma":0.98052603,"teacher_disagreement_score":0.030910313,"about_ca_system_score_codex":0.013753454,"about_ca_system_score_gemma":0.0076060244,"threshold_uncertainty_score":0.099788725},"labels":[],"label_agreement":null},{"id":"W4414021799","doi":"10.1029/2025tc009014","title":"All Aligned on the Western Front of North America? Analyzing the Stress Field in the Northern Cordillera","year":2025,"lang":"en","type":"article","venue":"Tectonics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Lakehead University; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Geology; Front (military); Stress field; Field (mathematics); Seismology; Paleontology; Geophysics; Oceanography","score_opus":0.01676111990319735,"score_gpt":0.2335712795401747,"score_spread":0.21681015963697736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414021799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986743,0.00010406238,0.0002569563,0.00003441386,0.000002189585,0.000002446937,0.00022136276,0.000020436786,0.00068396516],"genre_scores_gemma":[0.9992217,0.000043085918,0.00022490439,0.0000059781373,0.0000031010472,0.00000211879,0.0002888389,0.0000036293072,0.00020664246],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998946,0.000010071212,0.0000051978996,0.000038004557,0.000022932807,0.000029215733],"domain_scores_gemma":[0.99976677,0.000032475284,0.00006384315,0.00001860637,0.00008629201,0.000031955253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018985423,0.00026486613,0.00019809918,0.0011326801,0.0006702183,0.00074155215,0.00021815239,0.00016230899,0.0011760757],"category_scores_gemma":[0.00062891585,0.00008475671,0.00022645359,0.0012157712,0.0003300536,0.00023897171,0.00033766736,0.00011078028,0.0001313548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007039292,0.000013424837,0.9748721,0.000019003326,0.000059847764,0.00013654251,0.0002521632,0.004112461,0.003297364,0.0006106443,0.00030936813,0.016246587],"study_design_scores_gemma":[0.0000025438414,0.000012032008,0.98572516,0.000008150647,0.000014414964,0.000033642194,0.000485244,0.012334002,0.00041325038,0.00025887063,0.00070621306,0.000006518634],"about_ca_topic_score_codex":0.3708886,"about_ca_topic_score_gemma":0.46016917,"teacher_disagreement_score":0.3708886,"about_ca_system_score_codex":0.0012846518,"about_ca_system_score_gemma":0.0010155332,"threshold_uncertainty_score":0.73745954},"labels":[],"label_agreement":null},{"id":"W4414027550","doi":"10.5194/se-16-785-2025","title":"Characterizing some major Archean faults at depth in the Superior craton, North America","year":2025,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Laurentian University","funders":"Canada First Research Excellence Fund","keywords":"Archean; Craton; Geology; Seismology; Paleontology; Earth science; Tectonics","score_opus":0.015416443268402975,"score_gpt":0.23838582591739485,"score_spread":0.22296938264899188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414027550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982198,0.00022474918,0.000078165314,0.000022291671,0.0000010319682,0.0000055038117,0.0003006487,0.000007540042,0.0011402575],"genre_scores_gemma":[0.9984738,0.00016693577,0.00032706486,0.000012397507,0.0000020523014,0.000004288477,0.00042362628,0.0000019802214,0.0005878348],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.0000028598472,0.0000041723065,0.000018030203,0.000022825374,0.000015407892],"domain_scores_gemma":[0.99978405,0.0000138434825,0.000057436522,0.000009262264,0.00010090475,0.00003441559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010742668,0.00019215714,0.00010464712,0.0014095543,0.00053412694,0.00041487,0.00013616885,0.00017783228,0.00083926],"category_scores_gemma":[0.0002306705,0.0001347181,0.00008473489,0.0015880966,0.00031910258,0.00017776988,0.00028457356,0.00011710456,0.00009344432],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034656277,0.000008724604,0.9743901,0.00004201043,0.000019574913,0.00019294153,0.0010203278,0.00042626177,0.009582457,0.000102382946,0.00029031653,0.013890353],"study_design_scores_gemma":[0.0000010040553,0.0000033294405,0.9991411,0.0000051113607,0.0000025583201,0.000034467106,0.00018225935,0.00016052165,0.000105328414,0.000009561299,0.00035398017,8.1414544e-7],"about_ca_topic_score_codex":0.38989308,"about_ca_topic_score_gemma":0.77013224,"teacher_disagreement_score":0.61010695,"about_ca_system_score_codex":0.0012308048,"about_ca_system_score_gemma":0.0009587996,"threshold_uncertainty_score":0.77524734},"labels":[],"label_agreement":null},{"id":"W4414099112","doi":"10.1144/jgs2025-032","title":"Middle–Late Pleistocene transverse faulting in wedge-top units of the Northern Apennines (Italy): implications for orogen-parallel extension during coeval foreland-ward migration of the compression and extension fronts","year":2025,"lang":"en","type":"article","venue":"Journal of the Geological Society","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Future Earth","funders":"Università di Bologna; Ministry of Education; National Science and Technology Council","keywords":"Extensional definition; Lineament; Compression (physics); Metamorphic core complex; Extension (predicate logic); Pleistocene; Deformation (meteorology); Front (military); Transverse plane","score_opus":0.03368985350439418,"score_gpt":0.240683796557779,"score_spread":0.2069939430533848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414099112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990914,0.00009916084,0.00007991899,0.000010293984,9.764377e-7,0.000001925073,0.000043339296,0.000004863276,0.0006682132],"genre_scores_gemma":[0.999663,0.00006933065,0.00007208752,0.0000034504926,0.000002279121,0.0000018575141,0.000075773925,0.000001383846,0.00011083159],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999424,0.000008897119,0.000004916666,0.000025049554,0.0000056374047,0.000013137632],"domain_scores_gemma":[0.9998913,0.000013890449,0.000054508182,0.000011686996,0.000012361551,0.00001631605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015591603,0.00025911478,0.00012590001,0.00078006194,0.00028145412,0.00055521156,0.00021282503,0.00022745179,0.0017537995],"category_scores_gemma":[0.00033039422,0.00011204984,0.00019638553,0.0006320878,0.00042915958,0.00028455566,0.00032615705,0.0001073293,0.00022167832],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015855856,0.00003871533,0.95324916,0.000078802994,0.00006204778,0.00048110657,0.0015128284,0.00127794,0.024567647,0.0002461099,0.00007407234,0.018253006],"study_design_scores_gemma":[0.0000013645667,0.000011491598,0.9992636,0.0000036534075,0.0000047234616,0.000069157366,0.00010350422,0.0002779594,0.00012535676,0.00002038261,0.00011767779,0.000001212692],"about_ca_topic_score_codex":0.005493589,"about_ca_topic_score_gemma":0.007451271,"teacher_disagreement_score":0.005493589,"about_ca_system_score_codex":0.0002915665,"about_ca_system_score_gemma":0.00015094489,"threshold_uncertainty_score":0.010923207},"labels":[],"label_agreement":null},{"id":"W4414112282","doi":"10.1007/s10518-025-02251-5","title":"Characteristic earthquake recurrence and time-dependent seismic hazard modeling for the North and East Anatolian Faults","year":2025,"lang":"en","type":"article","venue":"Bulletin of Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"North Anatolian Fault; Seismic hazard; Fault (geology); Hydrogeology; Hazard; Seismic gap; Probabilistic logic; Exponential function","score_opus":0.010541316732501908,"score_gpt":0.19484240571500822,"score_spread":0.1843010889825063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414112282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931532,0.00014446129,0.005566097,0.00007970116,0.000006998885,0.000007948152,0.0001462693,0.00003585851,0.00085948507],"genre_scores_gemma":[0.99876547,0.00005269416,0.0005903991,0.0000021318006,0.0000027649974,0.0000069111193,0.0000693933,0.0000069952403,0.00050321635],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999558,0.00001098813,0.000004704899,0.0000151855875,0.0000045614624,0.000008849349],"domain_scores_gemma":[0.9997402,0.000119302495,0.00006526373,0.000013354537,0.000047613325,0.000014163164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018768752,0.00033881288,0.00034900298,0.00046639572,0.00029889736,0.00052562513,0.0006331348,0.0005838347,0.0008146523],"category_scores_gemma":[0.00071500684,0.00030741346,0.0004654169,0.0003627382,0.00020321761,0.00040912942,0.00023400459,0.00028326776,0.00009297058],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007936478,0.000038521375,0.017787883,0.000022784016,0.000045678567,0.00016187974,0.00008231502,0.9747059,0.0011685508,0.0010743759,0.00019280647,0.004639921],"study_design_scores_gemma":[0.00000263511,0.0000058416213,0.0019989437,0.0000013557478,0.0000077619,0.000011700765,0.000013718841,0.99775827,0.00007034077,0.00008800616,0.000039394843,0.000002039244],"about_ca_topic_score_codex":0.04736031,"about_ca_topic_score_gemma":0.030328417,"teacher_disagreement_score":0.04736031,"about_ca_system_score_codex":0.0006948198,"about_ca_system_score_gemma":0.000682864,"threshold_uncertainty_score":0.09416926},"labels":[],"label_agreement":null},{"id":"W4414246770","doi":"10.3390/geohazards6030057","title":"Relative Uplift Rates Along the Central Mindoro Fault, Philippines","year":2025,"lang":"en","type":"article","venue":"GeoHazards","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Canadian Nuclear Safety Commission","funders":"","keywords":"Sinistral and dextral; Context (archaeology); Spatial distribution; Fault (geology); Archipelago; Oblique case; Mountain range (options)","score_opus":0.011825637950340799,"score_gpt":0.23804882412395573,"score_spread":0.22622318617361492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414246770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994024,0.000047287132,0.000060902126,0.000011822562,6.9486043e-7,0.0000017633928,0.00009363728,0.000009754568,0.00037166043],"genre_scores_gemma":[0.9996848,0.000038488968,0.000069196554,0.0000022018148,0.000001774118,0.0000019021222,0.000101799,0.0000012740211,0.000098560515],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999008,0.0000143622465,0.000009091076,0.000028777096,0.000022143571,0.00002483908],"domain_scores_gemma":[0.9994342,0.00006722128,0.00023346914,0.000027810693,0.00016969033,0.00006758188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020181591,0.00022650066,0.00013020603,0.0017082421,0.00029682886,0.00040386635,0.00019037993,0.00015399011,0.0006825754],"category_scores_gemma":[0.00081483705,0.00009863877,0.00008326157,0.0010491522,0.0003503544,0.00034072384,0.0003886283,0.00015235099,0.000107276705],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000075163014,0.0000187422,0.9666821,0.00004387792,0.000028926786,0.00048632093,0.0023447631,0.0010943328,0.0073894556,0.00014639774,0.0002432297,0.02144674],"study_design_scores_gemma":[8.377976e-7,0.000017412953,0.99853206,0.000004027642,0.000003508683,0.00010813561,0.00043755956,0.00041663088,0.00021117661,0.000015867243,0.00024911299,0.0000035745772],"about_ca_topic_score_codex":0.020634629,"about_ca_topic_score_gemma":0.025828697,"teacher_disagreement_score":0.020634629,"about_ca_system_score_codex":0.00035186435,"about_ca_system_score_gemma":0.0002051461,"threshold_uncertainty_score":0.041029036},"labels":[],"label_agreement":null},{"id":"W4414321812","doi":"10.1126/science.adu9116","title":"Crustal stresses and damage evolve throughout the seismic cycle of the Ridgecrest fault zone","year":2025,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Crust; Deformation (meteorology); Fault (geology); Seismic energy; Anisotropy; Elastic-rebound theory; Subduction","score_opus":0.009346919586073534,"score_gpt":0.2510625137913212,"score_spread":0.24171559420524769,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414321812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99928135,0.000024937017,0.000089813555,0.000016041418,6.8086257e-7,0.0000020511347,0.00025396442,0.0000073109627,0.00032378838],"genre_scores_gemma":[0.9995115,0.000024337558,0.00007384068,0.0000053158037,8.978301e-7,0.0000014378719,0.0002025052,0.0000016023971,0.00017860747],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999187,0.000009866489,0.000006773789,0.000023276056,0.000021361366,0.00002006305],"domain_scores_gemma":[0.9997334,0.000021944434,0.00013548866,0.000024081255,0.00005244948,0.000032649186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015997476,0.00012595502,0.00011812684,0.0005713764,0.00013496794,0.00034294723,0.00014092663,0.00018408676,0.00080178556],"category_scores_gemma":[0.0007698808,0.000119683566,0.00008662181,0.0005902622,0.00019924904,0.00023301852,0.00037174462,0.0001485685,0.00012863087],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057328696,0.000030059078,0.9700304,0.000018861128,0.000052831245,0.000094289455,0.00047454215,0.0025811165,0.012097537,0.00018177091,0.000265991,0.014115257],"study_design_scores_gemma":[8.4983174e-7,0.0000134838265,0.9983936,0.0000022324582,0.0000030412784,0.000019092215,0.000051831248,0.0011167355,0.00022591466,0.000022631997,0.00014874402,0.0000018414735],"about_ca_topic_score_codex":0.016625429,"about_ca_topic_score_gemma":0.029536603,"teacher_disagreement_score":0.016625429,"about_ca_system_score_codex":0.0003802309,"about_ca_system_score_gemma":0.00023836232,"threshold_uncertainty_score":0.033057332},"labels":[],"label_agreement":null},{"id":"W4414573427","doi":"10.1029/2025gc012290","title":"Influence of Glacial Isostatic Adjustment on Intraplate Stress and Seismicity in Eastern North America in the Presence of Pre‐Existing Weak Zones","year":2025,"lang":"en","type":"article","venue":"Geochemistry Geophysics Geosystems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Intraplate earthquake; Induced seismicity; Fault (geology); Tectonics; Post-glacial rebound; Lithosphere; Thrust fault","score_opus":0.009349785477997497,"score_gpt":0.22194233677699052,"score_spread":0.21259255129899302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414573427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99944836,0.000018689883,0.000060654696,0.000019015844,0.000001392383,0.0000014415733,0.00008976587,0.000010589394,0.0003500714],"genre_scores_gemma":[0.9997559,0.000012596577,0.00004588395,0.000005279294,7.915773e-7,0.0000017398575,0.00008294402,0.0000035422418,0.0000912333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999931,0.000009996614,0.0000042735724,0.000023225097,0.000008513389,0.000023039545],"domain_scores_gemma":[0.9998246,0.00005121879,0.00003402779,0.000014553097,0.000025378968,0.000050337556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016693349,0.0003443041,0.00021948076,0.00044344837,0.0003832403,0.0008887161,0.0004705877,0.00045513018,0.0011832054],"category_scores_gemma":[0.00067237235,0.00023455276,0.00032475832,0.00033834617,0.0006623044,0.00026514864,0.00046580745,0.00026498386,0.00008025773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026866733,0.00013788271,0.7357759,0.000036236517,0.0001765115,0.00030922474,0.0002425994,0.24743536,0.009672997,0.00044326432,0.0004248174,0.005076531],"study_design_scores_gemma":[0.000046710804,0.000076712044,0.7577121,0.000011565054,0.0000661303,0.000033531363,0.0002905323,0.24012686,0.0009420709,0.00016455396,0.00050041097,0.000028811222],"about_ca_topic_score_codex":0.25802034,"about_ca_topic_score_gemma":0.2692705,"teacher_disagreement_score":0.25802034,"about_ca_system_score_codex":0.0018466638,"about_ca_system_score_gemma":0.0007888219,"threshold_uncertainty_score":0.51303697},"labels":[],"label_agreement":null},{"id":"W4415009194","doi":"10.1029/2025jb031122","title":"Probing the Nature of Low‐Frequency Earthquakes Through the Deconvolution of Tectonic Tremor","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Seismogram; Deconvolution; Residual; Consistency (knowledge bases); Waveform; Moment (physics); Arrival time","score_opus":0.028340976247773427,"score_gpt":0.32346281611221644,"score_spread":0.295121839864443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415009194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854584,0.000044864246,0.013436221,0.00004366185,0.0000027652727,0.000004124966,0.00010985249,0.00009687248,0.00080331025],"genre_scores_gemma":[0.99737984,0.000015201037,0.002265555,0.000004811759,0.0000018190336,0.0000010215527,0.00011287014,0.000009895014,0.00020899824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992335,0.0000089187715,0.0000032429132,0.0000171691,0.000026897324,0.000020403284],"domain_scores_gemma":[0.9996032,0.00013429133,0.00008073822,0.000045552322,0.00008444033,0.000051632407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028866835,0.00023308228,0.00015721544,0.00069115934,0.00023004696,0.0004986559,0.00025853954,0.00029575685,0.0007344147],"category_scores_gemma":[0.0013271809,0.00017497459,0.00013979315,0.00045638834,0.00022280561,0.00027031804,0.0002579823,0.0002529969,0.00022897165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046113934,0.00016561602,0.47545686,0.00009887412,0.00017372008,0.0004903499,0.0006892492,0.08018991,0.3267111,0.0027167127,0.00092712627,0.11191934],"study_design_scores_gemma":[0.000015705245,0.000063400155,0.54178584,0.000011877053,0.000028390885,0.00018319147,0.00020628558,0.42984018,0.025294665,0.0014974228,0.0010408517,0.000032124088],"about_ca_topic_score_codex":0.01447135,"about_ca_topic_score_gemma":0.025598947,"teacher_disagreement_score":0.01447135,"about_ca_system_score_codex":0.00038835252,"about_ca_system_score_gemma":0.000378079,"threshold_uncertainty_score":0.028774261},"labels":[],"label_agreement":null},{"id":"W4415129128","doi":"10.26443/seismica.v4i2.1914","title":"Fast Reports of the 2025 Mw 7.8 Mandalay, Myanmar Earthquake: unraveling the rupture characteristics","year":2025,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Government (linguistics); Vulnerability (computing); Natural disaster; Southeast asia; Feature (linguistics)","score_opus":0.010695412123072873,"score_gpt":0.2187806450829718,"score_spread":0.20808523295989892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415129128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897949,0.0010053285,0.0004798192,0.0010600926,0.000038910246,0.00001336985,0.002040493,0.000012041056,0.0055550286],"genre_scores_gemma":[0.99573505,0.000777965,0.00039318128,0.0000904361,0.000055919085,0.000015303545,0.0015026877,0.000007251801,0.0014221626],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997758,0.000039742696,0.000027943392,0.00003427283,0.00006950505,0.00005283144],"domain_scores_gemma":[0.998871,0.00013996496,0.0005622423,0.000118614545,0.0002617023,0.000046331956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006978742,0.0001757392,0.00015098117,0.0009617305,0.00051348103,0.0006374749,0.00022676188,0.00032864694,0.0013102693],"category_scores_gemma":[0.0021087865,0.00011491112,0.00012284795,0.0012030957,0.00022946164,0.000765989,0.0006494583,0.0003634459,0.00023084103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016733406,0.00002870567,0.91346246,0.0002721275,0.000092804185,0.0014046035,0.005329774,0.0012268019,0.012394774,0.0038760772,0.0042346586,0.05750986],"study_design_scores_gemma":[0.000001957903,0.000030660918,0.99111825,0.000028475411,0.00001537203,0.0002860463,0.0012108792,0.00024398913,0.00064879743,0.00020391868,0.0061991806,0.000012285631],"about_ca_topic_score_codex":0.014940937,"about_ca_topic_score_gemma":0.044016637,"teacher_disagreement_score":0.014940937,"about_ca_system_score_codex":0.00078163645,"about_ca_system_score_gemma":0.0006724708,"threshold_uncertainty_score":0.029707968},"labels":[],"label_agreement":null},{"id":"W4415139719","doi":"10.1029/2024jb031083","title":"Contrasting Crustal Signatures Across the 2021 M <sub>S</sub> 6.0 Luxian (China) Induced Earthquake Revealed by Dense Seismic and Magnetotelluric Data","year":2025,"lang":"en","type":"article","venue":"Journal of Geophysical Research Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Magnetotellurics; Seismic velocity; Fault (geology); Structural basin; Seismotectonics; Anomaly (physics)","score_opus":0.03240947778401692,"score_gpt":0.31985399250716134,"score_spread":0.2874445147231444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415139719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900717,0.000028756887,0.0002230397,0.000024876546,0.0000017082479,0.0000028233012,0.0003178182,0.000018613237,0.00037521616],"genre_scores_gemma":[0.9988133,0.000018893692,0.0002419726,0.000010620183,0.000008176035,0.000004736428,0.00072248076,0.0000036427311,0.00017622104],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998965,0.000009837951,0.00000805048,0.000025424912,0.000027625416,0.000032417734],"domain_scores_gemma":[0.99976045,0.000019520825,0.0000890366,0.000023160184,0.00005286848,0.00005488897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017735339,0.00026197292,0.00021048912,0.0014309877,0.00020569905,0.0003537946,0.00020678474,0.00020854021,0.0006751514],"category_scores_gemma":[0.00030801576,0.00014915019,0.00016475286,0.0013303788,0.00025405368,0.0002387738,0.00054082857,0.00011461183,0.000116161675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012889983,0.000058529982,0.8799567,0.00007321539,0.00008256192,0.00062341994,0.00081180746,0.0019248258,0.081819504,0.00031141003,0.00084370916,0.03336537],"study_design_scores_gemma":[0.0000034342718,0.000013446166,0.9980806,0.000001923529,0.000008261852,0.000044051296,0.00009136393,0.0010188607,0.0004451039,0.000020530855,0.00026769075,0.000004751455],"about_ca_topic_score_codex":0.008218076,"about_ca_topic_score_gemma":0.019907964,"teacher_disagreement_score":0.008218076,"about_ca_system_score_codex":0.00021812868,"about_ca_system_score_gemma":0.00021860507,"threshold_uncertainty_score":0.016340494},"labels":[],"label_agreement":null},{"id":"W4415284101","doi":"10.22541/essoar.176071976.63804735/v1","title":"Cross-fault rupture within a depth-segmented flower structure revealed by the 2024 Hualien earthquakes, eastern Taiwan","year":2025,"lang":"","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"China Scholarship Council; Central South University; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Induced seismicity; Seismotectonics; Epicenter; Sequence (biology)","score_opus":0.011093448425320717,"score_gpt":0.252648146939846,"score_spread":0.24155469851452527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415284101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993722,0.000020127534,0.00014789056,0.000021150721,0.0000015490107,0.000001543456,0.00013872233,0.000012341685,0.00028449265],"genre_scores_gemma":[0.9992072,0.000013140172,0.00015355306,0.000005924338,0.0000029613711,0.0000022659046,0.00046577604,0.0000031211807,0.00014619768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999416,0.0000047636977,0.0000035225303,0.000020211346,0.000007505649,0.000022379645],"domain_scores_gemma":[0.99982554,0.00002202437,0.00005775265,0.000023751467,0.000028866289,0.000042006774],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009578869,0.00014925262,0.00013787033,0.00074464927,0.00030429894,0.00037023675,0.0002215581,0.00026352535,0.0005919201],"category_scores_gemma":[0.0004542146,0.000106555904,0.00012983408,0.0007463283,0.00031050036,0.00026965287,0.00049816753,0.00015512032,0.00012254422],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021026978,0.00006514281,0.93862414,0.000047589107,0.00010100896,0.0019229094,0.0012891189,0.008712548,0.02511354,0.0005449617,0.0015940142,0.02177477],"study_design_scores_gemma":[0.000006231047,0.000033883836,0.9895056,0.0000060997622,0.000020060275,0.0002142648,0.00066895905,0.007889807,0.0007023094,0.0001521974,0.0007904719,0.0000101581345],"about_ca_topic_score_codex":0.015047702,"about_ca_topic_score_gemma":0.027877796,"teacher_disagreement_score":0.015047702,"about_ca_system_score_codex":0.00033016186,"about_ca_system_score_gemma":0.0002551504,"threshold_uncertainty_score":0.02992022},"labels":[],"label_agreement":null},{"id":"W4415791316","doi":"10.1186/s40562-025-00430-5","title":"The 2021 South Sandwich Islands tsunami: from the Antarctic to the far Northeast corner of the Pacific Ocean","year":2025,"lang":"en","type":"article","venue":"Geoscience Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Pacific ocean; Tsunami wave; Front (military); Arrival time; Period (music); Tsunami earthquake; Submarine pipeline; Pacific Plate; Magnitude (astronomy)","score_opus":0.007322671576798089,"score_gpt":0.18713146256768923,"score_spread":0.17980879099089114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415791316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99388415,0.00010291453,0.00054812396,0.00021678711,0.0000382447,0.000023958382,0.0023745485,0.00004740305,0.002763842],"genre_scores_gemma":[0.9963726,0.00009394008,0.00050896325,0.000039069513,0.000014870355,0.000011419691,0.0022042987,0.00001036217,0.00074461376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.000010414793,0.000004628841,0.00001382796,0.000014794813,0.000016252394],"domain_scores_gemma":[0.9998222,0.000025784246,0.000039720213,0.000014246965,0.000051186194,0.000047017747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015801031,0.00035266348,0.00017623742,0.0003107361,0.00043481658,0.00065171404,0.0003012527,0.00047095725,0.0021811177],"category_scores_gemma":[0.000727078,0.00013010897,0.00034491502,0.00064078526,0.00014102207,0.0003367574,0.0005503954,0.00037154852,0.00046332378],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004606247,0.00012696497,0.79722416,0.00018078537,0.00019218202,0.0022256551,0.00045921982,0.15627672,0.007003676,0.0006550307,0.0069658738,0.028229095],"study_design_scores_gemma":[0.000044904024,0.00016166845,0.8148109,0.00008850778,0.00009451356,0.0003044644,0.001551755,0.17510907,0.002835795,0.00043433264,0.0045058024,0.000058370006],"about_ca_topic_score_codex":0.093106814,"about_ca_topic_score_gemma":0.101809815,"teacher_disagreement_score":0.093106814,"about_ca_system_score_codex":0.0007304115,"about_ca_system_score_gemma":0.0006835157,"threshold_uncertainty_score":0.1851297},"labels":[],"label_agreement":null},{"id":"W4416008004","doi":"10.1016/j.pepi.2025.107467","title":"Source characteristics of the June 21, 2022 (Mw 6.1) Khost earthquake, Afghanistan","year":2025,"lang":"en","type":"article","venue":"Physics of The Earth and Planetary Interiors","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Alberta Energy","funders":"","keywords":"Interferometric synthetic aperture radar; Joint (building); Slip (aerodynamics); Tectonics; Intraplate earthquake; Seismic microzonation; Seismic energy","score_opus":0.007010986870356464,"score_gpt":0.1895879766267876,"score_spread":0.18257698975643116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416008004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8924392,0.0005460063,0.00029520382,0.0005564541,0.00012795345,0.00004379318,0.09476416,0.00012473231,0.011102421],"genre_scores_gemma":[0.9517922,0.0003223029,0.00019987352,0.000076090444,0.000121136494,0.000042965195,0.04394983,0.000026147909,0.0034694837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998865,0.000007853255,0.00001689801,0.0000152092025,0.000032944336,0.0000405711],"domain_scores_gemma":[0.9994678,0.00007288867,0.0001657415,0.000028478684,0.00022195146,0.000043177613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000103129365,0.0003014159,0.00022631134,0.0018690919,0.00055576826,0.00043310664,0.00024695465,0.00034228317,0.004312857],"category_scores_gemma":[0.0007792072,0.000096328666,0.0001257383,0.0034059938,0.000085375075,0.0002164266,0.00035385462,0.00023267952,0.001434812],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014696672,0.00020461148,0.8486677,0.00044786106,0.00014875855,0.0031704407,0.0015546572,0.0054466156,0.010789252,0.00071161543,0.05895031,0.068438515],"study_design_scores_gemma":[0.0000293461,0.000032301406,0.99000716,0.000024936302,0.000023848566,0.00034781624,0.0004462792,0.000663115,0.0005298357,0.00005812856,0.007825735,0.0000115603825],"about_ca_topic_score_codex":0.08196798,"about_ca_topic_score_gemma":0.09190589,"teacher_disagreement_score":0.08196798,"about_ca_system_score_codex":0.0005583301,"about_ca_system_score_gemma":0.0005673224,"threshold_uncertainty_score":0.16298175},"labels":[],"label_agreement":null},{"id":"W4416016386","doi":"10.26443/seismica.v4i2.1700","title":"Potential for Continental Scientific Drilling to Inform Fault Mechanics and Earthquake Science","year":2025,"lang":"en","type":"article","venue":"Seismica","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC","funders":"U.S. Geological Survey","keywords":"Drilling; Fault (geology); Earthquake prediction; Scientific drilling; Hazard; Seismic hazard; Seismic gap; Bridging (networking)","score_opus":0.010576026380716981,"score_gpt":0.23483181192682503,"score_spread":0.22425578554610806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416016386","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1239609,0.08996643,0.22284739,0.11557407,0.0035281891,0.00034946649,0.011462503,0.0019106653,0.43040046],"genre_scores_gemma":[0.7652259,0.053376578,0.15707387,0.0065103853,0.00096331065,0.0002646703,0.0045766896,0.00025918032,0.011749491],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9988605,0.0005934079,0.000052139232,0.00013645305,0.00025080374,0.00010676016],"domain_scores_gemma":[0.99190193,0.0024188415,0.0007617852,0.0019718593,0.002129486,0.00081611495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004706565,0.0006862257,0.00043414708,0.0023201804,0.00076608104,0.003027573,0.0007504784,0.0012553583,0.008793129],"category_scores_gemma":[0.010648612,0.00028401223,0.0004711827,0.0034105158,0.0024228191,0.0043591917,0.005111738,0.0015800686,0.0016514333],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002979221,0.000055909102,0.03726405,0.0010225575,0.00016753812,0.0003208805,0.0012568306,0.013469597,0.009438415,0.19365129,0.028192936,0.7148621],"study_design_scores_gemma":[0.000043372693,0.00014698997,0.035930224,0.0010240412,0.00008134319,0.00026392922,0.0027837164,0.011571733,0.0038505718,0.2555119,0.68867534,0.00011677437],"about_ca_topic_score_codex":0.01006099,"about_ca_topic_score_gemma":0.0097098695,"teacher_disagreement_score":0.01006099,"about_ca_system_score_codex":0.001570825,"about_ca_system_score_gemma":0.003699102,"threshold_uncertainty_score":0.029415905},"labels":[],"label_agreement":null},{"id":"W4416375894","doi":"10.1007/s11430-024-1688-3","title":"A new-generation source mechanism catalogue for historical moderate-to-strong earthquakes in the Sichuan-Yunnan region constrained by a topographic high-resolution 3D velocity model and seismic waveform matching","year":2025,"lang":"en","type":"article","venue":"Science China Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Focal mechanism; Moment tensor; Inversion (geology); Source model; Waveform; Seismotectonics; Seismic moment; Broadband; Fault (geology)","score_opus":0.022875722369170362,"score_gpt":0.2303454405908442,"score_spread":0.20746971822167382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416375894","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.65921795,0.00082459813,0.07065245,0.00014688399,0.00012091568,0.00033751287,0.25930506,0.0051073204,0.0042872424],"genre_scores_gemma":[0.4436769,0.0004022761,0.034024287,0.000031348136,0.00004168603,0.00024197191,0.5188812,0.00023903634,0.002461191],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984455,0.0000074110726,0.000024070983,0.00005157051,0.000044192362,0.000028200586],"domain_scores_gemma":[0.99945766,0.000029076495,0.00009568182,0.00016720069,0.00018176677,0.000068606394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034335218,0.00065600104,0.00059321773,0.005565392,0.00048854493,0.0005021998,0.00117489,0.00076484284,0.003048383],"category_scores_gemma":[0.00075721246,0.00039738187,0.00071631465,0.0043229638,0.00012877815,0.0007588855,0.00085573475,0.00034481112,0.0018166335],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007642928,0.00061469723,0.4546863,0.0008360065,0.0005445744,0.0036858118,0.00079596945,0.087347366,0.06569963,0.0047516297,0.07213069,0.30814302],"study_design_scores_gemma":[0.00029635517,0.00013577758,0.7093673,0.00010369783,0.0004814741,0.0011089207,0.00035645024,0.21961123,0.00848973,0.002110592,0.057780143,0.00015835647],"about_ca_topic_score_codex":0.044522967,"about_ca_topic_score_gemma":0.051291823,"teacher_disagreement_score":0.044522967,"about_ca_system_score_codex":0.00037786155,"about_ca_system_score_gemma":0.002575542,"threshold_uncertainty_score":0.08852762},"labels":[],"label_agreement":null},{"id":"W4416424323","doi":"10.1080/10503307.2025.2584983","title":"Italian versions of the rupture resolution rating system and the working alliance inventory observer short form: preliminary reliability and convergent validity","year":2025,"lang":"en","type":"article","venue":"Psychotherapy Research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Generalizability theory; Alliance; Reliability (semiconductor); Convergent validity; Resolution (logic); Observer (physics); Test validity; Inter-rater reliability","score_opus":0.09527880021916188,"score_gpt":0.3269012551628818,"score_spread":0.23162245494371994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416424323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.953308,0.001228407,0.016522082,0.00071790174,0.0002110106,0.00250426,0.0023572329,0.00015616804,0.022994952],"genre_scores_gemma":[0.94009185,0.0008361692,0.04590054,0.0002030563,0.00012440907,0.0048838546,0.0030332368,0.000077975,0.004848932],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9938,0.0034976732,0.000819419,0.00037349845,0.0013150462,0.00019442703],"domain_scores_gemma":[0.98989254,0.003865066,0.0022312386,0.0010700886,0.0026920731,0.00024901202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0128696775,0.0005492836,0.00046468966,0.0014218247,0.0004562613,0.00071267213,0.0006131802,0.00039461246,0.003810222],"category_scores_gemma":[0.025134413,0.00026751572,0.00079256215,0.0011680773,0.00061837264,0.00065319956,0.0012218609,0.00048247637,0.0012385831],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017748396,0.0005775599,0.6929495,0.0008413793,0.00040353075,0.00037342566,0.012272547,0.0010221456,0.0067373053,0.0026805464,0.007099582,0.27326766],"study_design_scores_gemma":[0.00021446911,0.0009696782,0.9814901,0.00021695645,0.00013857035,0.0005141737,0.0015354607,0.0016823723,0.0013960092,0.00091964065,0.0108775655,0.000045105728],"about_ca_topic_score_codex":0.0013694245,"about_ca_topic_score_gemma":0.0037625458,"teacher_disagreement_score":0.0128696775,"about_ca_system_score_codex":0.00051542313,"about_ca_system_score_gemma":0.0011745885,"threshold_uncertainty_score":0.06806213},"labels":[],"label_agreement":null},{"id":"W4416549217","doi":"10.1016/j.jsg.2025.105591","title":"Dehydroxylation and amorphization of wet serpentinite gouges during experimental seismic slip and implications for coseismic fluid drainage","year":2025,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Academia Sinica; National Science and Technology Council","keywords":"Fault gouge; Slip (aerodynamics); Compaction; Shear (geology); Anisotropy; Drainage; Olivine; Shear stress","score_opus":0.008871857995980961,"score_gpt":0.2441344049249405,"score_spread":0.23526254692895954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416549217","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996075,0.000024326762,0.000033017317,0.000002951272,9.4874144e-7,0.000002274704,0.000063295294,0.0000028863642,0.000262911],"genre_scores_gemma":[0.9996245,0.000019639048,0.000036325626,0.0000026589794,8.029135e-7,0.000001940374,0.00009337555,0.000003829909,0.00021691283],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993706,0.000008434823,0.000004277227,0.0000148339595,0.000012615932,0.000022767877],"domain_scores_gemma":[0.99987197,0.00002582934,0.000038368627,0.000017453569,0.000024306177,0.000022058646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011291404,0.00018076782,0.00012847409,0.00031642726,0.00036247013,0.0003469409,0.00017219894,0.0001755051,0.0017991833],"category_scores_gemma":[0.00029674624,0.00012440613,0.00010228015,0.00022914723,0.00058191025,0.00031037428,0.00018101808,0.00023454626,0.000118676675],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014084182,0.00007800205,0.01377013,0.000047163598,0.00001991798,0.0003215154,0.0004971196,0.00037055634,0.981128,0.00018798519,0.000050597704,0.002120638],"study_design_scores_gemma":[0.000046738005,0.00068417017,0.24062233,0.000009741134,0.000032336884,0.00033717055,0.0013679025,0.0018296358,0.75330937,0.00014660701,0.0015981455,0.000015947822],"about_ca_topic_score_codex":0.0029869513,"about_ca_topic_score_gemma":0.004064735,"teacher_disagreement_score":0.0029869513,"about_ca_system_score_codex":0.00023225526,"about_ca_system_score_gemma":0.00019981846,"threshold_uncertainty_score":0.0060189366},"labels":[],"label_agreement":null},{"id":"W4416694339","doi":"10.1785/0120250061","title":"Subduction or Crustal Faulting? Evaluating Ground-Motion Models to Characterize Haida Gwaii in the Canadian Seismic Hazard Model","year":2025,"lang":"en","type":"article","venue":"Bulletin of the Seismological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada; University of British Columbia","funders":"","keywords":"Subduction; Seismic hazard; Induced seismicity; Hazard; Fault (geology); Hazard analysis; Tectonics; Ground motion","score_opus":0.0540953678859481,"score_gpt":0.26399314863115086,"score_spread":0.20989778074520277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416694339","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9834942,0.00015873266,0.010252006,0.0004230514,0.000013241497,0.000059349764,0.0018132705,0.00022745905,0.0035586858],"genre_scores_gemma":[0.99383825,0.00006156426,0.0039090365,0.000030632444,0.000004545323,0.000016282891,0.0014535127,0.000021916941,0.00066431094],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997702,0.00004856045,0.000011968631,0.000058774567,0.000049252445,0.00006126978],"domain_scores_gemma":[0.9991511,0.0003207526,0.00009686966,0.000047387413,0.0002784452,0.00010539991],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008275538,0.00097175146,0.00034883118,0.000704867,0.00055242964,0.0010718794,0.001433563,0.00052342087,0.0013143965],"category_scores_gemma":[0.0029985243,0.00034232053,0.0004854428,0.00054647855,0.0004370075,0.00045036967,0.0006379268,0.0006151578,0.00012236883],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000051825544,0.000038261096,0.048489556,0.000015955806,0.00004921835,0.000030012863,0.00003024526,0.94332445,0.00038016078,0.00078684126,0.0005325765,0.006270928],"study_design_scores_gemma":[0.000007008888,0.0000066785647,0.006364863,0.0000030589356,0.000006668541,0.000002738022,0.000017820923,0.9932286,0.00012381194,0.000108362525,0.00012477946,0.0000055815813],"about_ca_topic_score_codex":0.9365197,"about_ca_topic_score_gemma":0.903565,"teacher_disagreement_score":0.06348032,"about_ca_system_score_codex":0.008920397,"about_ca_system_score_gemma":0.008974964,"threshold_uncertainty_score":0.12770826},"labels":[],"label_agreement":null},{"id":"W4416770046","doi":"10.22541/essoar.176430162.28549214/v1","title":"Detailed Seismological Observations from the M L 5.6 Reno Earthquake Sequence, the Largest Induced Seismic Event in Canada","year":2025,"lang":"en","type":"preprint","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Discovery Air (Canada)","funders":"","keywords":"Event (particle physics); Aftershock; Sequence (biology); Foreshock; Epicenter; Intraplate earthquake","score_opus":0.0684413879214704,"score_gpt":0.24638498709326745,"score_spread":0.17794359917179703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416770046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9540669,0.00028225474,0.0009802063,0.00013446236,0.000010771458,0.00007332006,0.033605393,0.00017116024,0.010675543],"genre_scores_gemma":[0.9691288,0.00035537698,0.0017762039,0.000043507185,0.0000063117423,0.000025324713,0.021767834,0.000024336614,0.0068722297],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978226,0.0000049166756,0.00000854178,0.00003827065,0.00010068588,0.00006528042],"domain_scores_gemma":[0.999648,0.00001370481,0.00003986477,0.000013684397,0.00021551618,0.00006916807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001252337,0.00030617797,0.00020260082,0.0011474098,0.0008339865,0.0005656249,0.00036537784,0.00023429883,0.0017913594],"category_scores_gemma":[0.00041537537,0.00013423352,0.0001504721,0.0027341074,0.00025965387,0.00012227331,0.0003327949,0.00025250888,0.00032445905],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026679545,0.00015586369,0.8769199,0.00020422583,0.00016146782,0.0005355881,0.0017396484,0.013564868,0.02604368,0.00097534776,0.014397025,0.065035686],"study_design_scores_gemma":[0.000014103977,0.000021515372,0.9855311,0.000017658696,0.000031781165,0.000038193342,0.00081902597,0.0032487772,0.0013674061,0.000048744434,0.008839893,0.000021788888],"about_ca_topic_score_codex":0.9843269,"about_ca_topic_score_gemma":0.9957417,"teacher_disagreement_score":0.015673101,"about_ca_system_score_codex":0.0054124673,"about_ca_system_score_gemma":0.010374543,"threshold_uncertainty_score":0.03927046},"labels":[],"label_agreement":null},{"id":"W4416812791","doi":"10.1016/j.jsames.2025.105895","title":"Unusual number of large tectonic earthquakes before and during the birth of the Paricutin monogenetic volcano. Did they trigger, maintain, and boost the volcanic long-lasting activity from 1943 to 1952?","year":2025,"lang":"en","type":"article","venue":"Journal of South American Earth Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Tectonics; Volcano; Intraplate earthquake; Stress field; Period (music); Vulcanian eruption; Magma; Slow earthquake","score_opus":0.006989091011456883,"score_gpt":0.2339035607902422,"score_spread":0.2269144697787853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416812791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986596,0.00040163903,0.00014117605,0.00005427743,0.0000096835265,0.0000055894493,0.00023129002,0.0000064992773,0.0004902942],"genre_scores_gemma":[0.99875164,0.00028677093,0.00018068141,0.00001594069,0.000025128309,0.000003506788,0.0005046184,0.0000017195238,0.00023003848],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999404,0.0000034804914,0.000004634461,0.000020620295,0.000012021932,0.000018817009],"domain_scores_gemma":[0.9997489,0.000016263552,0.00014856856,0.000012602376,0.000027439628,0.000046216865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010879623,0.0001384925,0.00015352097,0.0007510304,0.00043890852,0.0003335003,0.00014644595,0.00028246758,0.00060344645],"category_scores_gemma":[0.00033788147,0.00010680392,0.000109490626,0.0005992779,0.00031309662,0.00032339577,0.0002912326,0.00023789439,0.00007857669],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014559239,0.000021214997,0.9721058,0.000038293005,0.000036510464,0.0023914035,0.00073802134,0.00015118078,0.011051756,0.00017222531,0.00029227973,0.01285571],"study_design_scores_gemma":[0.0000013238292,0.000015886839,0.9984731,0.0000031877325,0.0000061598985,0.00036450522,0.00017584061,0.000035844998,0.00021574851,0.000017988914,0.0006880474,0.0000024132978],"about_ca_topic_score_codex":0.011417419,"about_ca_topic_score_gemma":0.022681728,"teacher_disagreement_score":0.011417419,"about_ca_system_score_codex":0.00047070725,"about_ca_system_score_gemma":0.00018177307,"threshold_uncertainty_score":0.02270192},"labels":[],"label_agreement":null},{"id":"W4416897235","doi":"10.5194/se-16-1473-2025","title":"New paleoseismological and morphotectonic investigations along the 2018 surface ruptures of the Fiandaca Fault, eastern flank of Etna volcano (Italy)","year":2025,"lang":"en","type":"article","venue":"Solid Earth","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Registered Nurses' Association of Ontario","funders":"","keywords":"Trench; Volcano; Paleoseismology; Flank; Fault (geology); Lava; Fault scarp; Tephra; Neotectonics","score_opus":0.015930654231798184,"score_gpt":0.22730802497038807,"score_spread":0.2113773707385899,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416897235","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982626,0.000100266756,0.00022320655,0.000010960624,0.0000031204668,0.0000054537672,0.00023261395,0.0000064652645,0.0011553969],"genre_scores_gemma":[0.99887735,0.000081953,0.00037848455,0.000004271521,0.00000945979,0.000005892018,0.00032741582,0.0000056369668,0.00030960346],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991095,0.000011151326,0.000006559372,0.000030004388,0.000020753012,0.000020537693],"domain_scores_gemma":[0.99982375,0.000017653758,0.00007912137,0.000023148224,0.000031551917,0.000024762949],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001563503,0.00030190652,0.0001634767,0.0019347897,0.00031884958,0.00050791464,0.00020971865,0.00030807627,0.0014329097],"category_scores_gemma":[0.00048653586,0.00019245526,0.00024064767,0.0012324937,0.00048112337,0.00030914397,0.00040876103,0.0001899685,0.00026074544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012870156,0.000044156695,0.9480127,0.00006123865,0.000046817284,0.001171473,0.0013854845,0.0009927207,0.02688226,0.00021886903,0.00019712129,0.02085843],"study_design_scores_gemma":[0.0000012653319,0.000014466352,0.9985765,0.000004283115,0.00000440777,0.00023674437,0.00011520374,0.0002254812,0.0002176302,0.000024139586,0.0005776735,0.0000021715584],"about_ca_topic_score_codex":0.0034000585,"about_ca_topic_score_gemma":0.007859022,"teacher_disagreement_score":0.0034000585,"about_ca_system_score_codex":0.0002816745,"about_ca_system_score_gemma":0.0001363527,"threshold_uncertainty_score":0.0067605376},"labels":[],"label_agreement":null},{"id":"W4417218978","doi":"10.1130/abs/2025am-7929","title":"Lithologic heterogeneity and strain rate controls on stress amplification and seismic failure in a regional-scale, lower crustal shear zone; Western Churchill Province, Canada","year":2025,"lang":"","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shear (geology); Lithology; Strain rate; Shear zone; Shear stress; Strain partitioning","score_opus":0.01378059546753469,"score_gpt":0.2246791544260548,"score_spread":0.2108985589585201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417218978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99869424,0.00005530471,0.000039375846,0.000025716086,5.1777965e-7,0.000004614674,0.00031589772,0.000003864053,0.0008605476],"genre_scores_gemma":[0.99932003,0.000040417584,0.000052137155,0.0000058920778,5.4890796e-7,0.0000022677063,0.00015720443,0.0000036613571,0.00041776407],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999683,0.00003424312,0.000018031558,0.000059269703,0.000062514955,0.00014292823],"domain_scores_gemma":[0.9986084,0.0002083737,0.00021365349,0.000054208842,0.0005041233,0.00041123293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005201758,0.0002229361,0.0004345056,0.0018257196,0.0019138859,0.0017909928,0.0009643827,0.00021709932,0.0020562205],"category_scores_gemma":[0.0018774834,0.00031743405,0.00026116043,0.0023978346,0.0021401278,0.0003218637,0.000777815,0.0002824016,0.00020221407],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042439034,0.000053565018,0.9761361,0.000039847615,0.00011705166,0.00019500247,0.0026632133,0.0034809965,0.007341218,0.0011238831,0.0006154457,0.0078092664],"study_design_scores_gemma":[0.000005960398,0.000006783568,0.9983491,0.000005396724,0.000010505793,0.000010992771,0.00084327284,0.0004322863,0.00012041949,0.000056529116,0.00015237831,0.000006451984],"about_ca_topic_score_codex":0.98670584,"about_ca_topic_score_gemma":0.99444216,"teacher_disagreement_score":0.01329416,"about_ca_system_score_codex":0.011869916,"about_ca_system_score_gemma":0.010805439,"threshold_uncertainty_score":0.08612269},"labels":[],"label_agreement":null},{"id":"W4417219264","doi":"10.1130/abs/2025am-7201","title":"CRESCENT CFM: A 3-D Community Fault Model for the Cascadia Subduction Zone, Canada and USA","year":2025,"lang":"","type":"article","venue":"Abstracts with programs - Geological Society of America","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Fault (geology); Fault model; Oceanic crust; Government (linguistics)","score_opus":0.030570164863060578,"score_gpt":0.24396834880754137,"score_spread":0.2133981839444808,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417219264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49518743,0.001194228,0.13634597,0.0030029304,0.0005929604,0.00055272965,0.2140427,0.021284236,0.12779674],"genre_scores_gemma":[0.8886105,0.0007912039,0.044771135,0.00018167973,0.000048790742,0.00030802106,0.0335496,0.0017091592,0.030029882],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999008,0.000012171331,0.0000051303086,0.000020988378,0.000033989356,0.000026942442],"domain_scores_gemma":[0.9995449,0.00004626273,0.000022723858,0.000024544728,0.0002900294,0.00007150826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002023925,0.0010281164,0.00066856184,0.00088744215,0.0014361728,0.0013438469,0.0034463839,0.0014497434,0.016467905],"category_scores_gemma":[0.0013424731,0.00067845517,0.00093431113,0.0018805286,0.00051322,0.00071128696,0.0006895169,0.00096171943,0.0018936394],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007887085,0.00004030796,0.005444474,0.00006083634,0.00004287365,0.000094580944,0.00008955223,0.9637194,0.00036916262,0.0034984346,0.017662307,0.008899259],"study_design_scores_gemma":[0.00008011537,0.000009676472,0.0022675113,0.000023257033,0.000025356458,0.000018894496,0.00007283786,0.9856167,0.0002247397,0.00115131,0.010479004,0.000030723888],"about_ca_topic_score_codex":0.96177197,"about_ca_topic_score_gemma":0.9542812,"teacher_disagreement_score":0.038228035,"about_ca_system_score_codex":0.007583723,"about_ca_system_score_gemma":0.014998262,"threshold_uncertainty_score":0.076906264},"labels":[],"label_agreement":null},{"id":"W4417430361","doi":"10.5194/gi-14-513-2025","title":"High-speed infrared thermography for measuring flash temperatures in sheared fault gouge analogues","year":2025,"lang":"en","type":"article","venue":"Geoscientific instrumentation, methods and data systems","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Nederlandse Organisatie voor Wetenschappelijk Onderzoek","keywords":"Grain size; Thermography; Flash (photography); Slip (aerodynamics); Shearing (physics); Softening; Fault gouge; Infrared","score_opus":0.049031815779615066,"score_gpt":0.3260615461016002,"score_spread":0.27702973032198513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417430361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9880471,0.00033326173,0.010431188,0.000020946167,0.000011425993,0.000027033399,0.00028565232,0.00010931615,0.00073401013],"genre_scores_gemma":[0.9905392,0.00018432943,0.008423006,0.000013707314,0.0000037012203,0.00002605439,0.00015643268,0.000017722028,0.0006358201],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999918,0.0000070187034,0.0000047170715,0.000026926387,0.000028900307,0.000014392246],"domain_scores_gemma":[0.99986506,0.000031515476,0.000033891236,0.000014902965,0.000038325827,0.000016225747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011333808,0.00020723279,0.0001624135,0.0004240056,0.00016296483,0.00022728009,0.00024909046,0.0002284374,0.0010400603],"category_scores_gemma":[0.00031124102,0.00014348011,0.00011043939,0.00027228385,0.0002351533,0.00023831347,0.00014363273,0.000313148,0.00015186582],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006555129,0.000009399361,0.0031675627,0.000050087227,0.000005537897,0.000044152574,0.00008638498,0.00032992632,0.9935393,0.000040810235,0.000058013666,0.0026033618],"study_design_scores_gemma":[0.000010279156,0.0002234759,0.10465255,0.000023896928,0.000038792834,0.00024785812,0.00031274,0.0130268475,0.8796428,0.000062473395,0.0017318648,0.000026384798],"about_ca_topic_score_codex":0.0031779471,"about_ca_topic_score_gemma":0.0070007783,"teacher_disagreement_score":0.0031779471,"about_ca_system_score_codex":0.00033467083,"about_ca_system_score_gemma":0.00017847744,"threshold_uncertainty_score":0.006318867},"labels":[],"label_agreement":null},{"id":"W4417474441","doi":"10.1126/science.ady0234","title":"Extreme plate boundary localization promotes shallow earthquake slip at the Japan Trench","year":2025,"lang":"en","type":"article","venue":"Science","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"","keywords":"Trench; Subduction; Accretionary wedge; Plate tectonics; Slip (aerodynamics); Tsunami earthquake; Interplate earthquake; Pelagic sediment; San andreas fault; Convergent boundary","score_opus":0.022277106330705215,"score_gpt":0.23339767795146132,"score_spread":0.21112057162075612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417474441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99954623,0.000029890474,0.00003104065,0.000005893265,7.874302e-7,9.944469e-7,0.000013648792,0.000003072881,0.00036838057],"genre_scores_gemma":[0.999498,0.000034610435,0.000033250522,0.0000063493153,8.082624e-7,0.0000013462146,0.000035654648,0.0000017795014,0.00038822135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999268,0.000005494239,0.0000030462943,0.000016353784,0.00001140208,0.00003678675],"domain_scores_gemma":[0.9998635,0.000005822345,0.000053202,0.0000061922824,0.000015663285,0.000055631826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000069160276,0.00015352434,0.00017067525,0.00046261656,0.00032131246,0.00039197938,0.000102096375,0.00018434234,0.0013393672],"category_scores_gemma":[0.000191685,0.00017933841,0.00008864596,0.00018407516,0.00025344038,0.0001896185,0.00067313504,0.000174878,0.0002617767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044830653,0.0001706891,0.64154977,0.000086743654,0.000052967258,0.0016495767,0.0016463023,0.0008127627,0.33945465,0.0003817136,0.0004886786,0.013257816],"study_design_scores_gemma":[0.000003036843,0.000048454185,0.9968587,0.0000041562594,0.000005722323,0.00010929164,0.0004169838,0.00020995294,0.0021007424,0.000034138437,0.0002054067,0.0000033215942],"about_ca_topic_score_codex":0.008588262,"about_ca_topic_score_gemma":0.02675526,"teacher_disagreement_score":0.008588262,"about_ca_system_score_codex":0.00031051814,"about_ca_system_score_gemma":0.000290967,"threshold_uncertainty_score":0.017076552},"labels":[],"label_agreement":null},{"id":"W4417506957","doi":"10.1016/j.geomat.2025.100089","title":"Improving resolution model of probable asperity distribution along southern Sumatra Subduction Zone using denser GPS stations","year":2025,"lang":"en","type":"article","venue":"GEOMATICA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"Kementerian Riset, Teknologi dan Pendidikan Tinggi; Universitas Bengkulu","keywords":"Global Positioning System; Subduction; Submarine pipeline; Seafloor spreading; Geodetic datum; Slip (aerodynamics); Inversion (geology)","score_opus":0.023318263916015047,"score_gpt":0.22657632623704424,"score_spread":0.2032580623210292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417506957","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96668965,0.000117174415,0.030639315,0.00017078784,0.000008425204,0.00001520354,0.00033424288,0.00019006085,0.0018351218],"genre_scores_gemma":[0.9962269,0.000035831374,0.003299295,0.0000068870413,0.000002819794,0.0000057942075,0.00014147897,0.000008455281,0.0002724508],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988186,0.000030926483,0.00000864111,0.000041424522,0.000018704162,0.00001850442],"domain_scores_gemma":[0.99973077,0.00009173221,0.000056641806,0.000048209375,0.00004843971,0.000024247993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003004556,0.00039365946,0.0003313696,0.000430331,0.00025893966,0.00085305504,0.0007130169,0.00066923344,0.0008748061],"category_scores_gemma":[0.0012312698,0.00026132283,0.00050232356,0.0003850148,0.00031156343,0.00059442385,0.0004599096,0.0003891614,0.00011367893],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025715079,0.000021439595,0.014006129,0.000012660416,0.000020749887,0.00011070908,0.000045281486,0.9796794,0.0013232098,0.00064837007,0.00006977415,0.004036547],"study_design_scores_gemma":[0.0000043384694,0.0000044097374,0.002746994,0.0000021797182,0.000004386948,0.000008659079,0.000012801453,0.996878,0.00012436006,0.00014563881,0.00006494997,0.0000031943043],"about_ca_topic_score_codex":0.04750793,"about_ca_topic_score_gemma":0.019103475,"teacher_disagreement_score":0.04750793,"about_ca_system_score_codex":0.00075754017,"about_ca_system_score_gemma":0.0005917732,"threshold_uncertainty_score":0.09446281},"labels":[],"label_agreement":null},{"id":"W648083478","doi":"10.1016/j.jsg.2015.06.006","title":"Do faults preserve a record of seismic slip: A second opinion","year":2015,"lang":"en","type":"article","venue":"Journal of Structural Geology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":301,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Slip (aerodynamics); Seismology; Geologic record; Episodic tremor and slip; Earthquake rupture; Fault (geology); Subduction; Tectonics; Paleontology","score_opus":0.034001315074369674,"score_gpt":0.25989897449649163,"score_spread":0.22589765942212195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W648083478","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.027364092,0.030384991,0.00753283,0.9069749,0.010355133,0.000026629226,0.00087368727,0.000044294917,0.016443385],"genre_scores_gemma":[0.4884599,0.054852378,0.0053912103,0.37268505,0.06989389,0.000062517334,0.0012325818,0.00009135705,0.0073311045],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99713683,0.00042807675,0.00021556008,0.0014057691,0.00054380554,0.00026996172],"domain_scores_gemma":[0.9484032,0.023906449,0.0061953324,0.003043451,0.015766144,0.0026854854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009852372,0.0007255289,0.0016777671,0.0014647738,0.0016304975,0.0035412381,0.0039401613,0.010572035,0.009704094],"category_scores_gemma":[0.033265077,0.0003655651,0.00083891896,0.0013435328,0.010613609,0.0088296775,0.0021221864,0.0065755155,0.003937984],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013321429,0.00031351583,0.06260736,0.0043066205,0.0016008997,0.0014466842,0.009288635,0.0012001076,0.0083009405,0.11324021,0.33458096,0.46178195],"study_design_scores_gemma":[0.0003567852,0.0005342574,0.093859226,0.0041172802,0.00089465815,0.0013316371,0.027765423,0.002634293,0.0030079347,0.3937478,0.4714282,0.00032252076],"about_ca_topic_score_codex":0.0062990854,"about_ca_topic_score_gemma":0.007117256,"teacher_disagreement_score":0.010572035,"about_ca_system_score_codex":0.0015023063,"about_ca_system_score_gemma":0.0026283409,"threshold_uncertainty_score":0.05210489},"labels":[],"label_agreement":null},{"id":"W6885063367","doi":"10.13140/rg.2.2.20890.62405","title":"Envisioning E3 Futures at the Seismic Science-Society Interface: Preliminary Analysis of the Pan Canadian Bilingual E3 Survey.","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Futures contract; Government (linguistics); Feature (linguistics); Perspective (graphical)","score_opus":0.053930694965968924,"score_gpt":0.3401178948797816,"score_spread":0.2861871999138127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6885063367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9533779,0.00070440915,0.00075140013,0.009066318,0.000083520834,0.000943538,0.004860145,0.00002995676,0.030182749],"genre_scores_gemma":[0.9806943,0.0012658965,0.0012651542,0.002787905,0.000018706489,0.00071754627,0.0022317057,0.000045859037,0.010972946],"study_design_codex":"qualitative","study_design_gemma":"observational","domain_scores_codex":[0.9911759,0.0016959847,0.00035207887,0.00047517483,0.0032623596,0.0030384606],"domain_scores_gemma":[0.9743027,0.0035758426,0.0014181637,0.0004487409,0.015633348,0.0046211695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.011241444,0.00041651333,0.00040880468,0.0032840786,0.012424873,0.0050219935,0.0014397564,0.0010296808,0.005729953],"category_scores_gemma":[0.025529945,0.00051769346,0.00037685662,0.0068256585,0.0030282682,0.0026100855,0.005545916,0.002087998,0.0006748128],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015875271,0.0001469922,0.22512855,0.000440593,0.000019122323,0.00053780846,0.71773076,0.00007993672,0.00059189636,0.0038894957,0.017239714,0.034036357],"study_design_scores_gemma":[0.000006962233,0.00003473711,0.12817375,0.00014600383,0.0000091210895,0.00005780528,0.83954746,0.00012460984,0.00011130682,0.00016644182,0.031588793,0.000032939537],"about_ca_topic_score_codex":0.9838171,"about_ca_topic_score_gemma":0.99208087,"teacher_disagreement_score":0.055385858,"about_ca_system_score_codex":0.055385858,"about_ca_system_score_gemma":0.11924712,"threshold_uncertainty_score":0.4018544},"labels":[],"label_agreement":null},{"id":"W6887867902","doi":"10.1785/01201000013","title":"The 2007 Nazko, British Columbia, Earthquake Sequence: Injection of Magma Deep in the Crust beneath the Anahim Volcanic Belt","year":2015,"lang":"en","type":"article","venue":"ANU Open Research (Australian National University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Crust; Magma; Volcano; Oceanic crust; Phreatic eruption; Earth crust","score_opus":0.1518301068769734,"score_gpt":0.3267808449325154,"score_spread":0.174950738055542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6887867902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9906536,0.00021015437,0.000040281582,0.00036210788,0.000023960281,0.000016434713,0.0028725467,0.0000082764245,0.005812595],"genre_scores_gemma":[0.9913585,0.00032910137,0.00016584752,0.000107650034,0.000009457365,0.000010538105,0.0028087427,0.0000059814215,0.0052042655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994373,0.000002581606,0.0000042287143,0.0000075579496,0.000018454948,0.000023489956],"domain_scores_gemma":[0.9996966,0.0000140928105,0.00005888087,0.00000849647,0.00015322358,0.000068655005],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009522167,0.00015556261,0.00014407675,0.0009631439,0.0013617668,0.0007144824,0.000281507,0.00049296295,0.0017958379],"category_scores_gemma":[0.00045899054,0.00013339304,0.00007120935,0.0012046202,0.000355603,0.00023333487,0.00050437346,0.00048139217,0.0002846536],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043373686,0.000086671585,0.9515238,0.00013716269,0.00007665075,0.0013852016,0.0029422622,0.0006572686,0.0115024345,0.0006359388,0.011441348,0.019177426],"study_design_scores_gemma":[0.0000028427487,0.0000033474114,0.9974946,0.000009378964,0.0000073239667,0.000031708816,0.00066213997,0.00010232325,0.0001318482,0.000014491348,0.0015378854,0.0000022060187],"about_ca_topic_score_codex":0.92359704,"about_ca_topic_score_gemma":0.98688066,"teacher_disagreement_score":0.07640296,"about_ca_system_score_codex":0.0047645764,"about_ca_system_score_gemma":0.008442649,"threshold_uncertainty_score":0.15370578},"labels":[],"label_agreement":null},{"id":"W6891757291","doi":"10.48350/159394","title":"Sedimentological signatures of lacustrine tsunamis","year":2021,"lang":"en","type":"article","venue":"Bern Open Repository and Information System (University of Bern)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subaerial; Fault (geology); Geologic record; Submarine pipeline; Mass wasting; Radiocarbon dating; Volcano; Prehistory; Stratigraphy","score_opus":0.011584416967259002,"score_gpt":0.17971842073092478,"score_spread":0.16813400376366577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6891757291","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99596643,0.00037300627,0.00017979648,0.000032024916,0.0000071903155,0.000008661389,0.0010824652,0.000038637052,0.0023116465],"genre_scores_gemma":[0.9984395,0.00016307352,0.00016395177,0.000006925699,0.000007676703,0.0000035613505,0.0006604094,0.000006379596,0.000548631],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999231,0.0000056022773,0.000010661694,0.000019133759,0.00002284353,0.000018663808],"domain_scores_gemma":[0.9997247,0.000018289309,0.00011053537,0.000012430759,0.00007900805,0.00005512858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012235939,0.00040931397,0.00019373727,0.00251994,0.00027099747,0.00083102396,0.00016268413,0.00029295165,0.0017808938],"category_scores_gemma":[0.00040111705,0.00014499782,0.00015244297,0.0020680507,0.0002498516,0.00022705353,0.0004083058,0.00015987443,0.00040203347],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004520818,0.000037894708,0.9419029,0.00010975201,0.000100767706,0.001905623,0.00094525376,0.0010184761,0.034720276,0.00023504301,0.0007052285,0.017866785],"study_design_scores_gemma":[0.0000041481785,0.000029435887,0.99827945,0.000005130589,0.000009954798,0.00014417768,0.00020058251,0.0002753366,0.00038896894,0.000033107845,0.00062525197,0.000004393677],"about_ca_topic_score_codex":0.010084901,"about_ca_topic_score_gemma":0.0146852685,"teacher_disagreement_score":0.010084901,"about_ca_system_score_codex":0.00026551215,"about_ca_system_score_gemma":0.00016788389,"threshold_uncertainty_score":0.020052373},"labels":[],"label_agreement":null},{"id":"W6892448642","doi":"10.5281/zenodo.10030331","title":"New Insights into the Active Tectonics of the Northern Canadian Cordillera from an Enhanced Earthquake Catalog","year":2023,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tectonics; Seismotectonics; Intraplate earthquake; Plate tectonics; Feature (linguistics)","score_opus":0.021564495627570176,"score_gpt":0.21572865609315695,"score_spread":0.19416416046558677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6892448642","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15045805,0.0047757663,0.0045038196,0.0020815881,0.00035455704,0.0004702512,0.5925329,0.0013544247,0.24346872],"genre_scores_gemma":[0.2579024,0.009866253,0.025945084,0.0003313778,0.00021216867,0.00023440248,0.5443469,0.0004102,0.1607512],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997453,0.0000072966886,0.000025694118,0.000034846627,0.00013193603,0.000054912958],"domain_scores_gemma":[0.99799323,0.00007883714,0.00007812641,0.00017832035,0.0015077943,0.00016368466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003432308,0.00052863255,0.00028599988,0.013224887,0.0014663559,0.0017232242,0.0008278957,0.0002805291,0.0388237],"category_scores_gemma":[0.0020728153,0.00024896723,0.00022082058,0.018978294,0.00033137118,0.0009156988,0.000896074,0.00038738266,0.0041627064],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020685476,0.0000629829,0.1012024,0.000801608,0.00005114217,0.0005286177,0.004001406,0.002551674,0.004564838,0.015879165,0.43204996,0.43809938],"study_design_scores_gemma":[0.000018017588,0.000010757643,0.34652627,0.0001748385,0.00004875538,0.00014817012,0.0011664857,0.0008326689,0.0004496768,0.000881075,0.64971393,0.000029287688],"about_ca_topic_score_codex":0.9806208,"about_ca_topic_score_gemma":0.9930214,"teacher_disagreement_score":0.0388237,"about_ca_system_score_codex":0.007936421,"about_ca_system_score_gemma":0.018020466,"threshold_uncertainty_score":0.12987822},"labels":[],"label_agreement":null},{"id":"W6893630395","doi":"10.5281/zenodo.3727037","title":"PBO Strainmeter Tsunami Signals 2005-2012","year":2012,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tide gauge; Borehole; Observatory; Tsunami wave; Tiltmeter; Plate tectonics; Tsunami earthquake","score_opus":0.043991354174124545,"score_gpt":0.23303105797122042,"score_spread":0.1890397037970959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6893630395","genre_codex":"empirical","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8673353,0.00031427675,0.0045912624,0.00013816662,0.000119958175,0.00019671045,0.0947411,0.0007968741,0.031766273],"genre_scores_gemma":[0.8503424,0.00040990638,0.007004109,0.00011997444,0.00009292761,0.00012143416,0.13466512,0.00009053952,0.0071536177],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996966,0.000016881593,0.000029591129,0.000059050188,0.00014543832,0.00005258994],"domain_scores_gemma":[0.99927014,0.000036603455,0.00021122712,0.00006736298,0.0003242857,0.000090416965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031373158,0.0005222572,0.00023472995,0.0017360557,0.00025492813,0.0005645157,0.0002918719,0.00017246431,0.0026861888],"category_scores_gemma":[0.00091948354,0.00017386016,0.00009008088,0.002014533,0.00013393766,0.00040652062,0.0006863729,0.00031387608,0.00090567255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008111575,0.000105301406,0.8195676,0.00041596903,0.00010075959,0.00024758073,0.00058649684,0.0031015945,0.01727673,0.0008191807,0.022270152,0.1346975],"study_design_scores_gemma":[0.000029958783,0.0000873482,0.9712686,0.000038862127,0.000026268614,0.000115572424,0.00020267523,0.0019251346,0.0050847456,0.000111335874,0.02109062,0.000018983634],"about_ca_topic_score_codex":0.017955553,"about_ca_topic_score_gemma":0.041302443,"teacher_disagreement_score":0.017955553,"about_ca_system_score_codex":0.000469652,"about_ca_system_score_gemma":0.000539357,"threshold_uncertainty_score":0.03570205},"labels":[],"label_agreement":null},{"id":"W6898667626","doi":"10.57757/iugg23-0237","title":"Multi-hazard insurance premium rate-making using earthquake-tsunami risk model for the district of Tofino, British Columbia, Canada","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Subduction; Seismic risk; Population; Urban seismic risk; Earthquake casualty estimation; Risk assessment; Probabilistic logic","score_opus":0.06540188987851556,"score_gpt":0.3166046639864493,"score_spread":0.2512027741079338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6898667626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87217367,0.001722493,0.08119514,0.0028448496,0.00014259998,0.00027636532,0.0053413706,0.0005142007,0.03578929],"genre_scores_gemma":[0.97906005,0.00038052927,0.0027499045,0.00006932808,0.000020010024,0.00005798636,0.00089275476,0.000041783616,0.016727734],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994843,0.00008528926,0.000016570511,0.00008701549,0.000074705844,0.00025208417],"domain_scores_gemma":[0.9983115,0.0006270432,0.00022681072,0.000052761858,0.00053791236,0.00024399302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010429134,0.0012768247,0.0012498094,0.0010568569,0.0013080125,0.00231608,0.0034695447,0.0018152592,0.0052378303],"category_scores_gemma":[0.0027692623,0.00080157624,0.001068575,0.0010437891,0.0012024152,0.0006361057,0.0011021502,0.0018896556,0.0004821695],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004819779,0.000034737557,0.0036631683,0.000017777964,0.000021736965,0.00018191026,0.000038049933,0.9901202,0.00017163661,0.003312349,0.0010406466,0.0013496184],"study_design_scores_gemma":[0.000007922111,0.0000061603037,0.0012205135,0.0000046725527,0.000010904472,0.000013586736,0.00003911049,0.9979619,0.00002635061,0.0004675582,0.00023127814,0.000010054028],"about_ca_topic_score_codex":0.892149,"about_ca_topic_score_gemma":0.7757972,"teacher_disagreement_score":0.10785103,"about_ca_system_score_codex":0.012189538,"about_ca_system_score_gemma":0.008639582,"threshold_uncertainty_score":0.21697235},"labels":[],"label_agreement":null},{"id":"W6901639317","doi":"10.60692/0frty-5tf50","title":"Paleoseismological Findings at a New Trench Indicate the 1714 M8.1 Earthquake Ruptured the Main Frontal Thrust Over all the Bhutan Himalaya","year":2021,"lang":"en","type":"article","venue":"Greater South Information System","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Trench; Foreland basin; Slip (aerodynamics); Thrust fault; Slow earthquake; Seismic gap; Aftershock; Epicenter","score_opus":0.03254817741639325,"score_gpt":0.19830408185738396,"score_spread":0.1657559044409907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6901639317","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927965,0.000067709734,0.00029742433,0.000032468004,0.0000023067291,0.000008269417,0.0004946324,0.000012902581,0.0062879226],"genre_scores_gemma":[0.99782026,0.000058509417,0.0002780093,0.000009059606,0.000003075792,0.000003135063,0.00024733902,0.000001986377,0.0015785481],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991596,0.000011775635,0.0000031849372,0.000023633991,0.000020731928,0.000024694598],"domain_scores_gemma":[0.9997868,0.000035881894,0.00004442335,0.000017428067,0.00006317396,0.000052281182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011366743,0.00016920848,0.000095481264,0.0010474455,0.0008346106,0.00039537443,0.00026485528,0.00015057459,0.0046876096],"category_scores_gemma":[0.0004298124,0.000101127436,0.000049256694,0.0011637877,0.00043853422,0.00023185901,0.00045428582,0.00016995001,0.0004980345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083823405,0.000056087454,0.92944014,0.00006933991,0.000034459237,0.001742017,0.0090391645,0.0008159077,0.017130474,0.0007604132,0.0005279673,0.040300224],"study_design_scores_gemma":[0.0000013581727,0.000027823238,0.99591655,0.000004372055,0.0000066288794,0.00021049756,0.0012513822,0.0001964266,0.0005086522,0.00009027884,0.0017797129,0.000006229216],"about_ca_topic_score_codex":0.047571998,"about_ca_topic_score_gemma":0.2048096,"teacher_disagreement_score":0.047571998,"about_ca_system_score_codex":0.0005294896,"about_ca_system_score_gemma":0.0002771745,"threshold_uncertainty_score":0.09459019},"labels":[],"label_agreement":null},{"id":"W6901664232","doi":"10.60692/57qeg-w6k98","title":"Association between Chronic Pain and Diabetes/Prediabetes: A Population-Based Cross-Sectional Survey in Saudi Arabia","year":2020,"lang":"en","type":"article","venue":"Greater South Information System","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"","keywords":"Prediabetes; Diabetes mellitus; Waist; Chronic pain; Logistic regression; Body mass index; Anthropometry","score_opus":0.03873526306232514,"score_gpt":0.20925147836038013,"score_spread":0.170516215298055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6901664232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926776,0.00020239539,0.000031873515,0.000053272925,0.000002573398,0.000009284988,0.00029814616,0.0000010476219,0.00013363532],"genre_scores_gemma":[0.9992379,0.0002363555,0.000078975005,0.000074344265,0.000005242291,0.0000079166575,0.00025660452,4.223294e-7,0.00010229798],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996449,0.00010179114,0.00006221507,0.000051913135,0.00007985184,0.000059375496],"domain_scores_gemma":[0.9993142,0.00007103383,0.0003008337,0.00003307238,0.0001530855,0.00012781261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007010217,0.00023452593,0.00024817022,0.0005760805,0.00031814966,0.00046812766,0.00032749906,0.00039178078,0.0010053536],"category_scores_gemma":[0.00092655607,0.00023260631,0.00023303318,0.0007376633,0.00019030822,0.00032961936,0.0003460757,0.00029466764,0.00018037835],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025082923,0.000037136862,0.9983949,0.000019946461,0.000030286412,0.000057077395,0.00022868547,0.000012388785,0.00011081585,0.000008282608,0.00008762368,0.0009879123],"study_design_scores_gemma":[0.0000040772775,0.00007662615,0.9986743,0.00001592212,0.00001529769,0.0002102944,0.00068211,0.00009764212,0.000021802409,0.00000629446,0.00019254812,0.0000031252541],"about_ca_topic_score_codex":0.027279686,"about_ca_topic_score_gemma":0.029156897,"teacher_disagreement_score":0.027279686,"about_ca_system_score_codex":0.00042290197,"about_ca_system_score_gemma":0.00042140478,"threshold_uncertainty_score":0.054241776},"labels":[],"label_agreement":null},{"id":"W6902041339","doi":"10.6084/m9.figshare.17870556","title":"Additional file 3 of Long-duration seismicity and their relation to Copahue volcano unrest","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Unrest; Relation (database); Induced seismicity; Volcano; Seismotectonics; Tracking (education)","score_opus":0.022796957745342766,"score_gpt":0.19480304354590017,"score_spread":0.1720060858005574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6902041339","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00011437274,0.000006028615,0.00005919173,0.000041794,0.0000085898755,0.000034897952,0.9990565,0.000062821164,0.00061575824],"genre_scores_gemma":[0.006676948,0.0000905186,0.0012059575,0.00022631,0.00006647844,0.0009401057,0.9819474,0.00034198735,0.00850428],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993735,0.0000898999,0.00014324347,0.00013555631,0.00015338937,0.00010442942],"domain_scores_gemma":[0.9832255,0.011783327,0.0011602214,0.0008705101,0.0025917895,0.00036858645],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011234338,0.00080638094,0.0010017997,0.0027532657,0.0008497386,0.0014851021,0.0015894088,0.0010578376,0.8780161],"category_scores_gemma":[0.02484174,0.00044035813,0.0007446344,0.0059976056,0.00021483385,0.0018025194,0.0010635381,0.0007735954,0.15230446],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002172025,0.00006425768,0.0030612939,0.0014838292,0.000033188746,0.000058239068,0.00006687568,0.00038760467,0.000060684968,0.0006173442,0.9887961,0.0051534674],"study_design_scores_gemma":[0.003509506,0.00020455454,0.05749069,0.0034264561,0.00019436797,0.00044569917,0.0010100838,0.0017217378,0.00069009356,0.00837494,0.9227818,0.00015004518],"about_ca_topic_score_codex":0.025478184,"about_ca_topic_score_gemma":0.03165781,"teacher_disagreement_score":0.8780161,"about_ca_system_score_codex":0.0011810749,"about_ca_system_score_gemma":0.0017968323,"threshold_uncertainty_score":0.17399514},"labels":[],"label_agreement":null},{"id":"W6902313407","doi":"10.6084/m9.figshare.8131361.v1","title":"Airline Service Evaluation Report for the 3rd Quarter 2017.pdf","year":2019,"lang":"en","type":"other","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Quarter (Canadian coin); Service (business); Postal service; Customer service; Aviation","score_opus":0.06784035615101074,"score_gpt":0.2823152845983514,"score_spread":0.21447492844734067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6902313407","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0029175833,0.0012501152,0.0020069666,0.01900682,0.0077641453,0.0023132241,0.47389537,0.0029074159,0.48793837],"genre_scores_gemma":[0.018891355,0.0027582345,0.0030140295,0.006565383,0.0014346058,0.005048878,0.28209075,0.0030863232,0.6771105],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.987958,0.0016927889,0.00074608583,0.00030549674,0.00820831,0.0010892921],"domain_scores_gemma":[0.9593448,0.0032839978,0.0010286903,0.0013851309,0.032777864,0.002179468],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.010867643,0.0011100856,0.0008712062,0.0034702173,0.0017023813,0.0068352334,0.0018105126,0.002366098,0.30892882],"category_scores_gemma":[0.033143215,0.00066118466,0.0013626666,0.0045101354,0.0007808216,0.0033505461,0.0024863593,0.0028292155,0.2958292],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006827547,0.000041104107,0.00032063012,0.000059565973,0.000005144022,0.000005698286,0.000013232244,0.000059460468,0.000027081083,0.00046967735,0.99208075,0.0068493816],"study_design_scores_gemma":[0.00012732774,0.00007933838,0.0059614065,0.00040631494,0.000016880344,0.0000152106695,0.00019778448,0.00022361042,0.00037028207,0.0006095065,0.99196833,0.000023883462],"about_ca_topic_score_codex":0.08266163,"about_ca_topic_score_gemma":0.0753235,"teacher_disagreement_score":0.69107115,"about_ca_system_score_codex":0.005105536,"about_ca_system_score_gemma":0.016948424,"threshold_uncertainty_score":0.98572916},"labels":[],"label_agreement":null},{"id":"W6902386713","doi":"10.6084/m9.figshare.40741.v1","title":"Harbor seal pups were live-captured from three sites (Queen Charlotte Strait, Hornby Island, and Vancouver) in British Columbia, Canada, and two sites (Smith Island in Juan de Fuca Strait and Gertrude Island in Puget Sound) in Washington State, USA","year":2011,"lang":"en","type":"other","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Population; Notice; Seal (emblem); Proxy (statistics); Redistribution (election)","score_opus":0.012891875724526568,"score_gpt":0.1863310432765562,"score_spread":0.17343916755202962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6902386713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9470862,0.00021210877,0.00029676183,0.00007548279,0.00004205551,0.00028581062,0.030694867,0.000053586606,0.021253146],"genre_scores_gemma":[0.9147332,0.0006327472,0.0018261976,0.00014574004,0.000027570026,0.00031333385,0.022103405,0.000032455886,0.060185336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998555,0.000012746817,0.000008870887,0.00004643865,0.000036707737,0.000039740138],"domain_scores_gemma":[0.9997242,0.000026855703,0.00006860925,0.000024779476,0.000084363935,0.000071107715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016780915,0.00031931134,0.00020720117,0.0008526752,0.0012521221,0.00031880214,0.00030596263,0.0002750682,0.016050603],"category_scores_gemma":[0.0002765584,0.0002631259,0.00011564255,0.00066414184,0.00055300235,0.00017928985,0.00044963506,0.00021672873,0.0028575612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006055563,0.00023923165,0.938526,0.00008035847,0.000057605692,0.001174727,0.0020177732,0.000094474715,0.004350977,0.0003469995,0.017486453,0.03501985],"study_design_scores_gemma":[0.000023892211,0.0001494919,0.98649293,0.000023883553,0.000019680394,0.0002064283,0.001478765,0.000058108177,0.0011078486,0.000055558154,0.01037399,0.000009385959],"about_ca_topic_score_codex":0.24830894,"about_ca_topic_score_gemma":0.615928,"teacher_disagreement_score":0.75169104,"about_ca_system_score_codex":0.00079233036,"about_ca_system_score_gemma":0.0006615688,"threshold_uncertainty_score":0.49372727},"labels":[],"label_agreement":null},{"id":"W6902609158","doi":"10.6084/m9.figshare.c.5993862.v1","title":"A practical guide for translating in-person simulation curriculum to telesimulation","year":2022,"lang":"en","type":"other","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Curriculum; Curriculum development","score_opus":0.07997941334906994,"score_gpt":0.32658278551757586,"score_spread":0.24660337216850592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6902609158","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004688984,0.00046620608,0.73660386,0.0062676254,0.0015917856,0.0042393245,0.0027504836,0.030682093,0.21270968],"genre_scores_gemma":[0.014417525,0.00087354024,0.85236263,0.0013890855,0.000090973954,0.0024311356,0.0016832167,0.0040294174,0.12272243],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99760395,0.0009990623,0.0002393814,0.00018455407,0.0008126732,0.00016033479],"domain_scores_gemma":[0.9948478,0.0016826362,0.00019993761,0.0005422561,0.00205866,0.0006686915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003434983,0.0016448599,0.0005409912,0.002934109,0.0016129476,0.003964516,0.0022595332,0.002201711,0.13392986],"category_scores_gemma":[0.01235637,0.0008013067,0.0005682592,0.0016555381,0.00089491403,0.0031295726,0.0036658328,0.0029021557,0.09027494],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005693474,0.00062002795,0.0006243789,0.000504828,0.000007927756,0.0005838767,0.0027038744,0.0035619477,0.0041408013,0.029762758,0.32404956,0.6333832],"study_design_scores_gemma":[0.000040563882,0.00015743615,0.00070590706,0.00054332963,0.00000511969,0.0003077064,0.0019726348,0.003959999,0.0023021882,0.013277573,0.97668254,0.000044888133],"about_ca_topic_score_codex":0.00488224,"about_ca_topic_score_gemma":0.009340364,"teacher_disagreement_score":0.13392986,"about_ca_system_score_codex":0.0017781731,"about_ca_system_score_gemma":0.0043436787,"threshold_uncertainty_score":0.44804},"labels":[],"label_agreement":null},{"id":"W6902967928","doi":"10.7939/r3z60ch6s","title":"2017 Annual Report, Centre for Teaching and Learning, University of Alberta","year":2017,"lang":"en","type":"article","venue":"Open MIND","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Work (physics); Government (linguistics); Agency (philosophy); Curriculum","score_opus":0.02636697864688308,"score_gpt":0.26022584277571126,"score_spread":0.23385886412882817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6902967928","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.018160429,0.0156013705,0.0018875657,0.0424951,0.033044018,0.0014397366,0.31256858,0.0025193754,0.57228374],"genre_scores_gemma":[0.007756264,0.0055887,0.00078079215,0.00049820944,0.0006406887,0.00020957238,0.045282897,0.0002754719,0.9389674],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997951,0.00006433884,0.00008509169,0.00011815208,0.0013353579,0.00044607482],"domain_scores_gemma":[0.9888058,0.00039128354,0.00023331138,0.00028481713,0.0075857206,0.0026991123],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025723614,0.0013899198,0.00075606426,0.003982287,0.00204968,0.004926889,0.0013735312,0.0021739244,0.16972682],"category_scores_gemma":[0.0038786172,0.0004322405,0.0004560954,0.00536322,0.0006804376,0.0017498969,0.0017797786,0.0019373712,0.09979269],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007831495,0.000049739483,0.0013358851,0.00008602125,0.000003446068,0.00003593232,0.000042764303,0.00013163165,0.00014787582,0.00047936497,0.97741747,0.020191602],"study_design_scores_gemma":[0.00002660701,0.000027723065,0.014620535,0.0001387444,0.000007010371,0.000027445823,0.00036858168,0.00016170282,0.00041436366,0.0002503922,0.983943,0.000014020561],"about_ca_topic_score_codex":0.49441588,"about_ca_topic_score_gemma":0.550755,"teacher_disagreement_score":0.49441588,"about_ca_system_score_codex":0.009233514,"about_ca_system_score_gemma":0.0570113,"threshold_uncertainty_score":0.9830761},"labels":[],"label_agreement":null},{"id":"W6903316754","doi":"10.1130/2017046","title":"Supplemental material: Quaternary rupture of a crustal fault beneath Victoria, British Columbia, Canada","year":2017,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Quaternary; Fault (geology); Surface rupture; Deformation (meteorology); Period (music)","score_opus":0.01666245838213644,"score_gpt":0.211827643231415,"score_spread":0.19516518484927858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6903316754","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.006568992,0.00007805112,0.00029395512,0.00044414145,0.00031452443,0.000096226526,0.95885223,0.0006523714,0.032699402],"genre_scores_gemma":[0.07993921,0.00062674936,0.0035458468,0.00030468678,0.00017862476,0.00014682178,0.80391276,0.0008543103,0.11049098],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9997532,0.0000092866285,0.000018879107,0.00003214597,0.0001125492,0.000074108226],"domain_scores_gemma":[0.9960232,0.00035614092,0.000134673,0.00017908607,0.0029948931,0.00031207295],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00020803837,0.0005121671,0.00041033776,0.004002703,0.002347986,0.001608294,0.0011367059,0.00066386815,0.44018236],"category_scores_gemma":[0.0037733046,0.00028265614,0.00034415102,0.008198562,0.00022513088,0.00066003564,0.00058994663,0.00036770612,0.04517377],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007158053,0.00005042832,0.009514223,0.0002974447,0.00001904135,0.00020677956,0.00021074273,0.00078064064,0.00027657262,0.00036249505,0.9712559,0.016954258],"study_design_scores_gemma":[0.00022846027,0.000032197713,0.2504015,0.0008376893,0.00006893369,0.00030651907,0.0024114375,0.002975864,0.0010772127,0.0016601157,0.7399189,0.00008110507],"about_ca_topic_score_codex":0.8860393,"about_ca_topic_score_gemma":0.9597794,"teacher_disagreement_score":0.44018236,"about_ca_system_score_codex":0.0045588696,"about_ca_system_score_gemma":0.009166876,"threshold_uncertainty_score":0.7985119},"labels":[],"label_agreement":null},{"id":"W6903649268","doi":"10.13140/rg.2.2.13800.72960","title":"Local Magnitude Scale for Earthquakes in the Western Canada Sedimentary Basin, Northeastern British Columbia and Northwestern Alberta","year":2019,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Scale (ratio); Magnitude (astronomy); Richter magnitude scale; Sedimentary rock","score_opus":0.005832306055404339,"score_gpt":0.17591756111372855,"score_spread":0.17008525505832423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6903649268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.989502,0.00043016035,0.0000839339,0.00016815659,0.0000087125045,0.000016887938,0.0039886814,0.00002139395,0.005780025],"genre_scores_gemma":[0.99394566,0.00024095163,0.00009926836,0.000024372179,0.000003520413,0.0000087891,0.001820105,0.000006236853,0.0038511013],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977237,0.000015737589,0.000017004224,0.00004030517,0.00006172354,0.00009286422],"domain_scores_gemma":[0.99833506,0.00012207021,0.00018617637,0.000035175235,0.0009290851,0.00039249775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002419127,0.00018528527,0.00021531126,0.002898795,0.0016194353,0.0012139474,0.00068172964,0.00025464976,0.0035089317],"category_scores_gemma":[0.0015649489,0.00019916602,0.00023026136,0.0038392034,0.00067585736,0.00032894753,0.0009567309,0.00036534542,0.00029742176],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013613401,0.000025009605,0.9855298,0.000045819932,0.00005083552,0.00013536734,0.0015557976,0.00075781514,0.0006621813,0.0004041492,0.003005806,0.007691227],"study_design_scores_gemma":[0.000001948424,0.0000019047013,0.9981718,0.000008111885,0.0000058932546,0.0000117044765,0.0011912868,0.00010850861,0.00002293827,0.000014382906,0.0004585382,0.000002817437],"about_ca_topic_score_codex":0.9933943,"about_ca_topic_score_gemma":0.998514,"teacher_disagreement_score":0.011331914,"about_ca_system_score_codex":0.011331914,"about_ca_system_score_gemma":0.010358986,"threshold_uncertainty_score":0.08221918},"labels":[],"label_agreement":null},{"id":"W6903740676","doi":"10.13127/misc/23","title":"MED-SUV 1th YEAR MEETING - NICOLOSI (CATANIA) 7 | 9 JULY 2014","year":2014,"lang":"en","type":"article","venue":"Istituto Nazionale di Geofisica e Vulcanologia (INGV)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Volcano; Declaration; Work (physics); Natural disaster; Natural (archaeology)","score_opus":0.012555030813135309,"score_gpt":0.20684172345451238,"score_spread":0.19428669264137707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6903740676","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010914359,0.025298156,0.0057468168,0.052194495,0.09990532,0.0010188307,0.01901243,0.0032627655,0.7826468],"genre_scores_gemma":[0.023689825,0.0039212448,0.0033333013,0.0047806795,0.01078584,0.0005058108,0.009819154,0.0011507662,0.94201344],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988741,0.00029955516,0.000035548146,0.00022798956,0.00029583325,0.00026697165],"domain_scores_gemma":[0.9991548,0.000055226676,0.000044507942,0.000059708465,0.0002497123,0.00043597183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017517754,0.0011205625,0.0005938064,0.001129839,0.0013724086,0.003465526,0.0013278807,0.0029210465,0.23199432],"category_scores_gemma":[0.0014774596,0.000365738,0.0006217041,0.00038805927,0.0005970815,0.0010386276,0.0043697883,0.0021223298,0.13185313],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002753624,0.000052996686,0.0005778896,0.00026281778,0.000015035157,0.00029047392,0.00010973411,0.00021201767,0.001567685,0.003672675,0.9619736,0.030989729],"study_design_scores_gemma":[0.000010724342,0.000025765668,0.0009752531,0.00010170694,0.0000024234598,0.000078660145,0.000051737985,0.00006791704,0.00022242058,0.0003408418,0.99811804,0.000004552402],"about_ca_topic_score_codex":0.003498011,"about_ca_topic_score_gemma":0.007835552,"teacher_disagreement_score":0.23199432,"about_ca_system_score_codex":0.0018247283,"about_ca_system_score_gemma":0.0027359142,"threshold_uncertainty_score":0.7760983},"labels":[],"label_agreement":null},{"id":"W6910709606","doi":"10.5066/p13ojqyw","title":"Compiled onshore and offshore paleoseismic data along the Cascadia Subduction zone","year":2024,"lang":"en","type":"dataset","venue":"Durham Research Online (Durham University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Submarine pipeline; Event (particle physics); Landslide; Ranking (information retrieval)","score_opus":0.10040598014510284,"score_gpt":0.31448692912973253,"score_spread":0.2140809489846297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6910709606","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14010401,0.00046198152,0.0011658036,0.00026080332,0.000083803476,0.00023530266,0.83123183,0.0005048926,0.025951602],"genre_scores_gemma":[0.14640868,0.00081957784,0.004873635,0.00006400959,0.000041500607,0.00036623428,0.82969457,0.00017240841,0.01755936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994029,0.00004019824,0.00009653316,0.00008222917,0.0003173358,0.000060808543],"domain_scores_gemma":[0.9948244,0.00036712442,0.00082251575,0.0004922739,0.0031228156,0.0003708734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069218373,0.00057396444,0.0003266014,0.01144701,0.000556664,0.00086871366,0.0004393158,0.00020368629,0.006824834],"category_scores_gemma":[0.0027623076,0.00033032117,0.00020416146,0.01804248,0.00020660974,0.0003181375,0.00095460523,0.0003615161,0.0022403318],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029920728,0.00014611753,0.58207804,0.0015653303,0.00031848354,0.0008764736,0.0029887434,0.0047265724,0.006726052,0.0016119387,0.24708238,0.15158068],"study_design_scores_gemma":[0.000027162361,0.000027669628,0.79707277,0.00011608071,0.00005049281,0.000064410175,0.00082721666,0.00031292843,0.0013668928,0.00015150655,0.19995478,0.00002804961],"about_ca_topic_score_codex":0.26567134,"about_ca_topic_score_gemma":0.4620521,"teacher_disagreement_score":0.7343286,"about_ca_system_score_codex":0.0015658999,"about_ca_system_score_gemma":0.004452971,"threshold_uncertainty_score":0.5282499},"labels":[],"label_agreement":null},{"id":"W6920522474","doi":"10.60692/e8t4x-eqt65","title":"Genotypes and phenotypes of resistance in Ecuadorian Plasmodium falciparum","year":2019,"lang":"en","type":"article","venue":"Greater South Information System","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Plasmodium falciparum; Genotype; Malaria; Dihydroartemisinin; Drug resistance; Chloroquine; Apicomplexa; Phenotype; Artemether","score_opus":0.01662771328095514,"score_gpt":0.1803565310463049,"score_spread":0.16372881776534975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6920522474","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993375,0.00018037632,0.00005680807,0.00001713265,0.0000011941194,0.0000037498833,0.00011084222,0.00000289831,0.00028949758],"genre_scores_gemma":[0.9991534,0.00012624724,0.00019741167,0.000013159253,0.0000024456162,0.000008139291,0.00019932255,0.000002098088,0.0002977895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998735,0.000024297336,0.000017200417,0.00003153862,0.000017596376,0.000035810375],"domain_scores_gemma":[0.99985087,0.000018254952,0.000083998646,0.000010066067,0.00002313016,0.000013598104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001978917,0.00019292267,0.0001605002,0.0005035635,0.00017291862,0.00032101822,0.00015239442,0.00015913845,0.0017193748],"category_scores_gemma":[0.00065045035,0.00009805068,0.00008116841,0.000366209,0.00012051648,0.00017760113,0.00016361939,0.000110051675,0.00011842842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013594027,0.0002301473,0.8254326,0.00016345918,0.00010974568,0.003775978,0.0025482299,0.00037363262,0.10861102,0.00019947719,0.00049853843,0.056697767],"study_design_scores_gemma":[0.000007921835,0.00016103243,0.99340737,0.000014464103,0.000022331878,0.0014657084,0.00087535416,0.00020322733,0.002215172,0.000028678664,0.0015927131,0.0000060855014],"about_ca_topic_score_codex":0.0028408733,"about_ca_topic_score_gemma":0.0027766502,"teacher_disagreement_score":0.0028408733,"about_ca_system_score_codex":0.00018578327,"about_ca_system_score_gemma":0.00004914104,"threshold_uncertainty_score":0.005751908},"labels":[],"label_agreement":null},{"id":"W6920676522","doi":"10.6084/m9.figshare.17870562","title":"Additional file 5 of Long-duration seismicity and their relation to Copahue volcano unrest","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Relation (database); Unrest; Induced seismicity; Volcano; Seismotectonics","score_opus":0.022802605555465552,"score_gpt":0.19495495294601684,"score_spread":0.1721523473905513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6920676522","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00012358023,0.000009404173,0.000079490295,0.00006651177,0.000016828826,0.00004111211,0.9987068,0.00009367229,0.0008624638],"genre_scores_gemma":[0.008123526,0.00013291115,0.0017821329,0.0003571367,0.00010618726,0.00094532,0.97666025,0.0005375264,0.011355064],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993894,0.000104869614,0.00012100824,0.00013732053,0.0001437905,0.00010358895],"domain_scores_gemma":[0.97999763,0.014600012,0.0010608392,0.0009788631,0.0029115241,0.00045116653],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011690046,0.00082048704,0.0011195206,0.0028856571,0.0009281196,0.0015542309,0.0016869322,0.0009921532,0.8998079],"category_scores_gemma":[0.026999116,0.0004419924,0.0008021302,0.0058995867,0.00021374812,0.0021739989,0.0011106323,0.0007945059,0.16740125],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017791982,0.000058184945,0.0024503611,0.0013747582,0.000029975563,0.000044111384,0.000061206505,0.00031379703,0.000046983376,0.00058561773,0.9898086,0.0050484664],"study_design_scores_gemma":[0.0026475727,0.00019962278,0.04930239,0.004034555,0.00019072753,0.0003993486,0.0010980222,0.0015827491,0.0005616648,0.00948087,0.9303549,0.00014765827],"about_ca_topic_score_codex":0.022007532,"about_ca_topic_score_gemma":0.027292108,"teacher_disagreement_score":0.8998079,"about_ca_system_score_codex":0.0011177039,"about_ca_system_score_gemma":0.0016495043,"threshold_uncertainty_score":0.14291191},"labels":[],"label_agreement":null},{"id":"W6920721700","doi":"10.6084/m9.figshare.17870565","title":"Additional file 6 of Long-duration seismicity and their relation to Copahue volcano unrest","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Unrest; Relation (database); Induced seismicity; Volcano; Seismotectonics","score_opus":0.022797548001855187,"score_gpt":0.19490691153002979,"score_spread":0.1721093635281746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6920721700","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00011200472,0.000008247711,0.00008381073,0.00007394868,0.000017114722,0.000038464557,0.998744,0.00010185909,0.0008205338],"genre_scores_gemma":[0.008223715,0.00013927597,0.002055574,0.00036543116,0.000118520744,0.0010896492,0.975688,0.00065163476,0.0116682425],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99937797,0.00010246484,0.00012230418,0.00013923501,0.00014554542,0.00011237721],"domain_scores_gemma":[0.98037934,0.014313558,0.0010296513,0.0010142687,0.0028032404,0.00045992565],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001275472,0.0009023865,0.0011531964,0.0028470233,0.0009603881,0.0016258042,0.001825718,0.001136464,0.9074799],"category_scores_gemma":[0.027177615,0.0004881821,0.0008906972,0.00558821,0.00022838124,0.002240434,0.0011544708,0.0008732237,0.18352374],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017494505,0.00005468399,0.0021361038,0.0012758946,0.000026952068,0.00004574717,0.000060822338,0.00032074345,0.000047534064,0.00051831634,0.9906697,0.004668526],"study_design_scores_gemma":[0.0033707307,0.00019601117,0.04550793,0.0039517353,0.00019091064,0.00041707107,0.001115248,0.0017874351,0.0005890177,0.009681369,0.9330287,0.00016394004],"about_ca_topic_score_codex":0.022975095,"about_ca_topic_score_gemma":0.028252074,"teacher_disagreement_score":0.9074799,"about_ca_system_score_codex":0.0011248259,"about_ca_system_score_gemma":0.0018010717,"threshold_uncertainty_score":0.13196862},"labels":[],"label_agreement":null},{"id":"W6920828898","doi":"10.6084/m9.figshare.17870565.v1","title":"Additional file 6 of Long-duration seismicity and their relation to Copahue volcano unrest","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Unrest; Relation (database); Induced seismicity; Volcano; Seismotectonics","score_opus":0.022797548001855187,"score_gpt":0.19490691153002979,"score_spread":0.1721093635281746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6920828898","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00011200472,0.000008247711,0.00008381073,0.00007394868,0.000017114722,0.000038464557,0.998744,0.00010185909,0.0008205338],"genre_scores_gemma":[0.008223715,0.00013927597,0.002055574,0.00036543116,0.000118520744,0.0010896492,0.975688,0.00065163476,0.0116682425],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99937797,0.00010246484,0.00012230418,0.00013923501,0.00014554542,0.00011237721],"domain_scores_gemma":[0.98037934,0.014313558,0.0010296513,0.0010142687,0.0028032404,0.00045992565],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.001275472,0.0009023865,0.0011531964,0.0028470233,0.0009603881,0.0016258042,0.001825718,0.001136464,0.9074799],"category_scores_gemma":[0.027177615,0.0004881821,0.0008906972,0.00558821,0.00022838124,0.002240434,0.0011544708,0.0008732237,0.18352374],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017494505,0.00005468399,0.0021361038,0.0012758946,0.000026952068,0.00004574717,0.000060822338,0.00032074345,0.000047534064,0.00051831634,0.9906697,0.004668526],"study_design_scores_gemma":[0.0033707307,0.00019601117,0.04550793,0.0039517353,0.00019091064,0.00041707107,0.001115248,0.0017874351,0.0005890177,0.009681369,0.9330287,0.00016394004],"about_ca_topic_score_codex":0.022975095,"about_ca_topic_score_gemma":0.028252074,"teacher_disagreement_score":0.9074799,"about_ca_system_score_codex":0.0011248259,"about_ca_system_score_gemma":0.0018010717,"threshold_uncertainty_score":0.13196862},"labels":[],"label_agreement":null},{"id":"W6924741323","doi":"10.15468/dl.zyvy2t","title":"Occurrence Download","year":2021,"lang":"en","type":"dataset","venue":"Global Biodiversity Information Facility","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Download; Matching (statistics); Range (aeronautics); Data set; Set (abstract data type)","score_opus":0.017202455148829395,"score_gpt":0.20113408392003562,"score_spread":0.18393162877120622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6924741323","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0000375527,0.00001791405,0.00003040954,0.000028463453,0.000008293431,0.0000046767836,0.99907327,0.0002930371,0.0005063597],"genre_scores_gemma":[0.00014949002,0.000025803276,0.00014423666,0.000034404977,0.0000029812231,0.000032339663,0.9991079,0.00010682317,0.000396007],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.998955,0.00013325375,0.00013640142,0.00034288777,0.00025082985,0.00018171554],"domain_scores_gemma":[0.9975096,0.00062903407,0.00024447433,0.00064146536,0.00067899533,0.00029635243],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00090966944,0.00197376,0.0015627898,0.0052809482,0.0008677205,0.00235694,0.0026797084,0.0019822754,0.14605735],"category_scores_gemma":[0.0053905034,0.00087547395,0.0010775862,0.010214018,0.00041872464,0.0021327466,0.0023620494,0.0019468294,0.19672559],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031097316,0.000011872607,0.00037095172,0.00045153155,0.000014939521,0.000014126121,0.000018850453,0.00014477236,0.00011574302,0.0003514265,0.9970778,0.0013968074],"study_design_scores_gemma":[0.00008439671,0.000008403172,0.0022302938,0.0001635399,0.000013695678,0.000032048534,0.00006589322,0.00018599628,0.00021688669,0.0007022711,0.99627894,0.00001756505],"about_ca_topic_score_codex":0.026704146,"about_ca_topic_score_gemma":0.041186836,"teacher_disagreement_score":0.85394263,"about_ca_system_score_codex":0.0017961817,"about_ca_system_score_gemma":0.0024238753,"threshold_uncertainty_score":0.4886105},"labels":[],"label_agreement":null},{"id":"W6924833610","doi":"10.15468/dl.sd3cb2","title":"Occurrence Download","year":2023,"lang":"en","type":"dataset","venue":"Global Biodiversity Information Facility","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Download; Matching (statistics); Range (aeronautics); Data collection; Identification (biology)","score_opus":0.021040350935759167,"score_gpt":0.20905661517266888,"score_spread":0.1880162642369097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6924833610","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000043827873,0.000023235998,0.00004529875,0.00003490433,0.000010549139,0.000005313508,0.99885976,0.0003907843,0.0005863696],"genre_scores_gemma":[0.0001717404,0.000030361689,0.00020633271,0.000043152784,0.0000032136436,0.00004203613,0.99892825,0.00015354386,0.0004212396],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99908364,0.0001185492,0.000120123485,0.00031211044,0.00020920618,0.00015622072],"domain_scores_gemma":[0.997922,0.0005791051,0.00020675233,0.0005200663,0.00052803906,0.00024400227],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00089576025,0.0019387004,0.0015371902,0.004433298,0.0009396009,0.0023289963,0.0027530394,0.002074535,0.14443699],"category_scores_gemma":[0.005361137,0.0008791253,0.0010969463,0.008705947,0.00042309312,0.0020967287,0.0024220103,0.0020183963,0.19478819],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030662006,0.000011948869,0.0003778607,0.0004994363,0.000014102874,0.000016131844,0.000024084655,0.00014037374,0.00011396935,0.00038648307,0.9970331,0.0013517716],"study_design_scores_gemma":[0.00008995719,0.000008230171,0.001998641,0.00018364555,0.000013860185,0.000037950933,0.000075927455,0.00020353879,0.00019864016,0.00079487177,0.9963768,0.000017937386],"about_ca_topic_score_codex":0.023365026,"about_ca_topic_score_gemma":0.036862887,"teacher_disagreement_score":0.85556304,"about_ca_system_score_codex":0.0016511753,"about_ca_system_score_gemma":0.0021985185,"threshold_uncertainty_score":0.48318988},"labels":[],"label_agreement":null},{"id":"W6924917298","doi":"10.15468/dl.txgq6v","title":"Occurrence Download","year":2022,"lang":"en","type":"dataset","venue":"Global Biodiversity Information Facility","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Download; Matching (statistics); Range (aeronautics); State (computer science); Confidentiality","score_opus":0.0169754497309375,"score_gpt":0.19990136947859158,"score_spread":0.18292591974765407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6924917298","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00004777537,0.000023719958,0.000044759676,0.000038657956,0.000011848126,0.0000054196225,0.99884593,0.00035778468,0.0006241191],"genre_scores_gemma":[0.00017442225,0.000030707422,0.00019922972,0.000045303364,0.0000037194288,0.000040803232,0.998909,0.00013714853,0.0004596591],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990258,0.00013598245,0.00012372443,0.00034005067,0.00021128629,0.00016313678],"domain_scores_gemma":[0.9976507,0.0006835415,0.0002206825,0.00059485657,0.00057256327,0.0002776275],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0008976202,0.0019500618,0.0014854288,0.004830565,0.0009992331,0.0024685937,0.0028010535,0.0021776054,0.14906782],"category_scores_gemma":[0.005507033,0.00088335556,0.0010985484,0.009032491,0.0004605493,0.0023002767,0.002433656,0.0021206795,0.19627628],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029007042,0.000012662174,0.0003685641,0.0004734118,0.000013205309,0.000016074746,0.00002347568,0.00013123998,0.00010367424,0.00039639554,0.99720436,0.0012280603],"study_design_scores_gemma":[0.00008491759,0.000008171505,0.0018230008,0.000164425,0.000012409965,0.00003787727,0.00007716432,0.00018349689,0.00017632627,0.0008197502,0.9965952,0.000017192828],"about_ca_topic_score_codex":0.021369107,"about_ca_topic_score_gemma":0.036965813,"teacher_disagreement_score":0.8509322,"about_ca_system_score_codex":0.0016091863,"about_ca_system_score_gemma":0.0022584093,"threshold_uncertainty_score":0.49868155},"labels":[],"label_agreement":null},{"id":"W6925137837","doi":"10.1594/pangaea.967672","title":"Track of GPS-Drifter M184_8-1 (Drifter_201)","year":2024,"lang":"en","type":"dataset","venue":"Publishing Network for Geoscientific and Environmental Data (PANGAEA) (Alfred Wegener Institute for Polar and Marine Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Track (disk drive); Meteor (satellite); Hydrography; Underwater; Flow (mathematics); Mooring; Drifter; Heading (navigation)","score_opus":0.06175113648413682,"score_gpt":0.2770843370158672,"score_spread":0.21533320053173038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6925137837","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0008433202,0.000025326777,0.00010154728,0.000022625483,0.000016067404,0.0000151304785,0.997855,0.00021091773,0.0009099992],"genre_scores_gemma":[0.00073883845,0.000012163638,0.00026836674,0.000011177949,0.000003939363,0.000032140233,0.9983286,0.000024951118,0.00057983195],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99953735,0.00006438988,0.00004376335,0.00017376948,0.00010231399,0.00007841553],"domain_scores_gemma":[0.99937797,0.000054497086,0.000108272034,0.00017087173,0.00021679707,0.00007152809],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056581607,0.0013737535,0.0008753172,0.0019790037,0.00043222544,0.0009831298,0.0016196303,0.00085959205,0.032469787],"category_scores_gemma":[0.0012890643,0.0003556552,0.00043010482,0.003880766,0.00022906817,0.0005801047,0.000802807,0.0009418853,0.06455831],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014205622,0.000048794864,0.004876072,0.00028820272,0.00004058773,0.000056600224,0.00004173383,0.00052973523,0.0005683593,0.00051331165,0.98795915,0.0049353945],"study_design_scores_gemma":[0.00026639065,0.000044569453,0.01991235,0.00010759143,0.000027050482,0.00007543907,0.00011033455,0.0009297407,0.00091217534,0.0006357122,0.9769519,0.000026749463],"about_ca_topic_score_codex":0.019301996,"about_ca_topic_score_gemma":0.033808038,"teacher_disagreement_score":0.032469787,"about_ca_system_score_codex":0.0006505195,"about_ca_system_score_gemma":0.0011782796,"threshold_uncertainty_score":0.10862225},"labels":[],"label_agreement":null},{"id":"W6925431821","doi":"10.18712/nsd-nsd1854-v2","title":"Labour Force Survey, 2. quarter 1997 - 1. quarter 1999, panel","year":2014,"lang":"en","type":"dataset","venue":"NSD – Norsk senter for forskningsdata","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Quarter (Canadian coin); Data collection; Data file; Census; Schedule; Table (database); Revenue","score_opus":0.033389634098308654,"score_gpt":0.24593786165195922,"score_spread":0.21254822755365055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6925431821","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005572363,0.00007176305,0.00014026425,0.00019148973,0.000088387664,0.0001722861,0.99486744,0.00007257471,0.0038385664],"genre_scores_gemma":[0.0020893738,0.0002753327,0.000489073,0.00031687698,0.00007028738,0.0014331928,0.9841881,0.000057180197,0.011080544],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9986181,0.00021387576,0.00013065562,0.0002599309,0.0005222722,0.00025505904],"domain_scores_gemma":[0.99688846,0.00038133885,0.0003273047,0.00033399774,0.0018807712,0.00018820389],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019165182,0.000982789,0.0012193919,0.00226421,0.001014213,0.0014548025,0.0017197309,0.0009805406,0.08673736],"category_scores_gemma":[0.006322376,0.00062832574,0.00051509164,0.0066366512,0.00016544803,0.0009558822,0.0010948397,0.0015005856,0.08519192],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054457494,0.000023771756,0.0017883874,0.00013382414,0.000010302929,0.000012423994,0.00003844198,0.000051469025,0.000043893244,0.00039168715,0.99324656,0.0042047016],"study_design_scores_gemma":[0.00034697645,0.000059870366,0.088193096,0.0003681762,0.00003419447,0.00005184922,0.000340513,0.00021302723,0.00016701066,0.000678098,0.90952075,0.000026453265],"about_ca_topic_score_codex":0.07348407,"about_ca_topic_score_gemma":0.06414431,"teacher_disagreement_score":0.08673736,"about_ca_system_score_codex":0.0022022978,"about_ca_system_score_gemma":0.003995558,"threshold_uncertainty_score":0.29016536},"labels":[],"label_agreement":null},{"id":"W6925761750","doi":"10.18429/jacow-linac2022-tupoge01","title":"Commissioning of the VECC Cryomodule","year":2022,"lang":"en","type":"article","venue":"JACOW","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"TRIUMF","funders":"","keywords":"Upgrade; Superconducting radio frequency; Solenoid; Project commissioning; Cryostat; Cryogenics; Corrosion","score_opus":0.01396237402565053,"score_gpt":0.19511911168398824,"score_spread":0.1811567376583377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6925761750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93922263,0.0002548347,0.040637203,0.00021782996,0.0001146543,0.0005387448,0.0025306242,0.0021337986,0.014349692],"genre_scores_gemma":[0.94371116,0.00012160275,0.04171005,0.00010219706,0.00005438671,0.00040227865,0.0030838142,0.00060188374,0.010212672],"study_design_codex":"bench_or_experimental","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994061,0.00007853304,0.000014385428,0.000096439515,0.00027927588,0.00012527686],"domain_scores_gemma":[0.9991203,0.00009025799,0.00005805444,0.00021948772,0.00041758877,0.000094375646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012614682,0.00039362494,0.0005216124,0.000511331,0.00080874684,0.0004419753,0.00044325733,0.0003900636,0.0030535457],"category_scores_gemma":[0.00094501115,0.00025589124,0.00029679405,0.00032021126,0.0004497414,0.0002766702,0.00074140343,0.0007374135,0.0010371469],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007960885,0.00013018606,0.01920898,0.0003535046,0.000065903325,0.0011111874,0.001000771,0.015820466,0.86961895,0.002944525,0.009136048,0.079813436],"study_design_scores_gemma":[0.0001411446,0.0024020397,0.09839335,0.00005553032,0.00006367913,0.0010294624,0.0002533847,0.01812903,0.80281705,0.00027776923,0.07633535,0.00010219933],"about_ca_topic_score_codex":0.0035426887,"about_ca_topic_score_gemma":0.0046107997,"teacher_disagreement_score":0.0035426887,"about_ca_system_score_codex":0.0012126883,"about_ca_system_score_gemma":0.0014416106,"threshold_uncertainty_score":0.010215104},"labels":[],"label_agreement":null},{"id":"W6926120577","doi":"10.21949/he5v-qn72","title":"Transportation Commodity Brief U.S. Freight Flows with Canada and Mexico in Transportation Commodities: 2017-2024","year":2025,"lang":"en","type":"report","venue":"ROSA P","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Commodity; Commodity swap; Commodity market; Rail transportation; Commodity chain","score_opus":0.018342525883126435,"score_gpt":0.21871877126101028,"score_spread":0.20037624537788384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6926120577","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004856064,0.0036298996,0.00038888227,0.0076353857,0.0028261626,0.0006022667,0.86719346,0.0008711153,0.11199673],"genre_scores_gemma":[0.012639449,0.009984011,0.0014645539,0.0013343738,0.00063304463,0.00084338884,0.728686,0.00025308758,0.24416214],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.997983,0.000041617426,0.0000779467,0.00008612984,0.0013529873,0.00045830873],"domain_scores_gemma":[0.9935814,0.00017274657,0.0002652429,0.000082241495,0.0053956336,0.0005028111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011171093,0.0014628452,0.00054527196,0.007736321,0.0033457663,0.003110738,0.0014620028,0.0017540792,0.059315044],"category_scores_gemma":[0.0035876194,0.000909247,0.00073179445,0.011396109,0.0003738596,0.0020811795,0.0014999213,0.0024049939,0.021999735],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027156337,0.000021208416,0.0017898877,0.00013971707,0.000006841131,0.000031469623,0.00003898009,0.00017543444,0.000047786194,0.0009048768,0.9889585,0.007858153],"study_design_scores_gemma":[0.00001853893,0.000018944176,0.025030801,0.00030583068,0.000021304386,0.000027011518,0.0004252687,0.000310396,0.00034446994,0.00027003855,0.97319555,0.000031698364],"about_ca_topic_score_codex":0.90353024,"about_ca_topic_score_gemma":0.9032295,"teacher_disagreement_score":0.09646976,"about_ca_system_score_codex":0.019978773,"about_ca_system_score_gemma":0.07141107,"threshold_uncertainty_score":0.19842857},"labels":[],"label_agreement":null},{"id":"W6926571270","doi":"10.25318/3410016801-fra","title":"Distribution des stocks d’actifs routiers de propriété municipale sous forme de ponts et de tunnels, selon l’évaluation de l’état physique, la zone (urbaine ou rurale) et la taille de population, Infrastructure Canada, inactif","year":2019,"lang":"fr","type":"dataset","venue":"Statistics Canada Dissemination","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Distribution (mathematics); Limiting; Economic shortage; Stock (firearms)","score_opus":0.0097510800509544,"score_gpt":0.2600348050232481,"score_spread":0.25028372497229373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6926571270","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00071524637,0.00003342259,0.000027118915,0.000034590288,0.000007031385,0.00000364386,0.99868554,0.000040191306,0.00045323995],"genre_scores_gemma":[0.0031129671,0.00006651977,0.0001538443,0.000023967295,0.00000448001,0.000030855197,0.9951332,0.000017763281,0.0014563256],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99941576,0.000037942147,0.0000723969,0.00014036191,0.00020447075,0.00012906858],"domain_scores_gemma":[0.9967398,0.00044508372,0.0004147936,0.00025895407,0.001887086,0.0002542047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005779072,0.0009497296,0.0007868378,0.0038072637,0.00055605127,0.0013372507,0.0014226137,0.00080906093,0.01849127],"category_scores_gemma":[0.005341054,0.000482423,0.0006268139,0.010434062,0.00026805597,0.00077325857,0.0007941656,0.0010125122,0.011272205],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000086338005,0.00001902968,0.021490334,0.0004761585,0.000077801975,0.000032382308,0.00006897409,0.000819845,0.00011042852,0.0008054186,0.97225314,0.0037601271],"study_design_scores_gemma":[0.0002943784,0.000023116176,0.29329503,0.0005577588,0.0000934291,0.00011637058,0.0005559185,0.001872515,0.00062697317,0.00072775333,0.7017721,0.000064651],"about_ca_topic_score_codex":0.7272583,"about_ca_topic_score_gemma":0.7576563,"teacher_disagreement_score":0.27274168,"about_ca_system_score_codex":0.0040655457,"about_ca_system_score_gemma":0.0068738614,"threshold_uncertainty_score":0.5486958},"labels":[],"label_agreement":null},{"id":"W6931229357","doi":"10.5281/zenodo.4173719","title":"123.MOZI~ \"The Kid Detective (2020)\" FILMEK VIDEA-ONLINE MAGYAR jdb","year":2020,"lang":"hu","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Detective fiction; Video recording; Key (lock)","score_opus":0.04412370608916144,"score_gpt":0.22701930277009955,"score_spread":0.1828955966809381,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6931229357","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00094472576,0.00041381046,0.0006097863,0.0019993382,0.0029147125,0.0001431202,0.008803822,0.00471624,0.97945446],"genre_scores_gemma":[0.0033819953,0.00025996758,0.00039972717,0.000598281,0.00026626504,0.00006194536,0.0036528285,0.0013437889,0.99003524],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998287,0.000015325468,0.000005691114,0.000028692592,0.00006994394,0.000051546038],"domain_scores_gemma":[0.99945253,0.000042043834,0.00001581864,0.000030983505,0.00022525842,0.00023329047],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0003019857,0.00071641227,0.0002757367,0.0006774763,0.0017930594,0.0030024657,0.000579851,0.0012381886,0.79063994],"category_scores_gemma":[0.0012750967,0.00040361698,0.0002921258,0.0005270678,0.0002557993,0.0027843125,0.0019431915,0.0013169008,0.66440725],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013577046,0.000005458179,0.00007849744,0.000028338613,6.246245e-7,0.000026648993,0.00006671102,0.000006106193,0.00014581771,0.0004672185,0.990036,0.009124971],"study_design_scores_gemma":[0.000004025999,0.0000071287814,0.00075187377,0.000029334167,0.0000013652815,0.000039004484,0.00014799695,0.000023473536,0.000111498324,0.000082737635,0.9987968,0.000004671478],"about_ca_topic_score_codex":0.013198319,"about_ca_topic_score_gemma":0.040267356,"teacher_disagreement_score":0.20936006,"about_ca_system_score_codex":0.00079308904,"about_ca_system_score_gemma":0.00047831598,"threshold_uncertainty_score":0.29862672},"labels":[],"label_agreement":null},{"id":"W6936072547","doi":"10.57757/iugg23-4941","title":"Rethinking historical models of induced seismicity in Rocky Mountain House, Alberta, Canada: Is brine disposal to blame?","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Poromechanics; Phanerozoic; Brine; Devonian; Proterozoic; Aquifer","score_opus":0.0704836362500767,"score_gpt":0.307716434806798,"score_spread":0.2372327985567213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6936072547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.63850325,0.02537184,0.038843792,0.08448885,0.0011005276,0.00013553952,0.014753359,0.0008848458,0.19591802],"genre_scores_gemma":[0.97709227,0.00509509,0.0031334977,0.00080909627,0.00011575237,0.000024711118,0.0022765948,0.00013817631,0.011314746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966836,0.00005161165,0.000018867353,0.00006594409,0.00010093205,0.000094339746],"domain_scores_gemma":[0.9981844,0.00024199187,0.00024138614,0.00008188396,0.00097270356,0.0002775869],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014229788,0.00062218396,0.00030034935,0.0027774838,0.0020147217,0.003861894,0.0034398085,0.0010832688,0.0068986425],"category_scores_gemma":[0.0047735004,0.00032491778,0.0003569771,0.0033557345,0.002939665,0.0015249432,0.0010032146,0.0014796018,0.000615334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019288476,0.00009657099,0.35939202,0.00050457724,0.00024235682,0.0006843036,0.01438332,0.11003069,0.0012642691,0.3302613,0.0912989,0.09164882],"study_design_scores_gemma":[0.00007361949,0.00008260418,0.3973649,0.0013442687,0.00023130015,0.00033751118,0.02037862,0.2677941,0.0008144716,0.08027614,0.2309661,0.00033634272],"about_ca_topic_score_codex":0.99000484,"about_ca_topic_score_gemma":0.99124837,"teacher_disagreement_score":0.049010523,"about_ca_system_score_codex":0.049010523,"about_ca_system_score_gemma":0.025384696,"threshold_uncertainty_score":0.3555979},"labels":[],"label_agreement":null},{"id":"W6936263877","doi":"10.57757/iugg23-2442","title":"Identifying probable fault planes in the stable continental regions of Canada","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Active fault; Fault (geology); Aftershock; Seismic hazard; Hazard; Seismotectonics; Magnitude (astronomy); Seismic risk","score_opus":0.07415782242724299,"score_gpt":0.3237897381456896,"score_spread":0.24963191571844662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6936263877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.952359,0.002164968,0.0012460396,0.0007495985,0.000018710967,0.00010755945,0.015263761,0.000096257645,0.027994175],"genre_scores_gemma":[0.9871811,0.0011045157,0.0021924751,0.00005645757,0.000004061361,0.000016788823,0.0051736054,0.000012759198,0.004258223],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973756,0.000010404802,0.000014778731,0.000050847433,0.00009813773,0.00008832736],"domain_scores_gemma":[0.99895203,0.000055655695,0.00010504618,0.000024119412,0.000728122,0.000135052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020799195,0.00039753568,0.00015401875,0.0031208715,0.0018212775,0.0013640365,0.00062412873,0.00024400912,0.0028945394],"category_scores_gemma":[0.0011232017,0.00014152615,0.00023663684,0.005577182,0.0005394763,0.00026579964,0.0005085354,0.00021458082,0.0002841027],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013203583,0.000024307661,0.8797581,0.00017209916,0.000099784076,0.000636995,0.0014859989,0.00911437,0.0024296085,0.0037076464,0.011906985,0.09053199],"study_design_scores_gemma":[0.000010679941,0.000012365163,0.9762691,0.00009884648,0.000039412003,0.00012318761,0.0034696823,0.006657198,0.00067201274,0.00043263848,0.012186464,0.000028494347],"about_ca_topic_score_codex":0.99682957,"about_ca_topic_score_gemma":0.9989956,"teacher_disagreement_score":0.021696938,"about_ca_system_score_codex":0.021696938,"about_ca_system_score_gemma":0.02717783,"threshold_uncertainty_score":0.15742308},"labels":[],"label_agreement":null},{"id":"W6939354732","doi":"10.6084/m9.figshare.17870550","title":"Additional file 2 of Long-duration seismicity and their relation to Copahue volcano unrest","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Relation (database); Induced seismicity; Unrest; Volcano; Seismotectonics","score_opus":0.022376018732662078,"score_gpt":0.19464484682045574,"score_spread":0.17226882808779367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939354732","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00018154169,0.00000685286,0.00011856709,0.00005129847,0.000011126802,0.000035190376,0.9987238,0.00010839481,0.00076328544],"genre_scores_gemma":[0.012071992,0.00008687338,0.0018858829,0.00022291565,0.00008427367,0.00079037173,0.9755132,0.00057272764,0.008771785],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99959105,0.00006388431,0.00008485165,0.00009915661,0.00009239239,0.00006866937],"domain_scores_gemma":[0.9868765,0.00976763,0.00072934054,0.0006905106,0.0016733106,0.00026274117],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009305988,0.000685939,0.0008429824,0.0022179065,0.00068218843,0.0014363191,0.0014457613,0.00091070315,0.8660763],"category_scores_gemma":[0.021081056,0.00039345946,0.0006943157,0.004165202,0.00018435778,0.001633271,0.0008742673,0.0007030499,0.1390188],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020355046,0.00005827476,0.0035731765,0.0011704892,0.0000312856,0.00007811452,0.00005994974,0.0006639272,0.000066856126,0.0007826186,0.98675424,0.0065575116],"study_design_scores_gemma":[0.0032223866,0.00020829243,0.056020457,0.0025017594,0.0001853887,0.00066489656,0.00090820185,0.0035839416,0.00083470397,0.010722249,0.9210006,0.0001471367],"about_ca_topic_score_codex":0.016777575,"about_ca_topic_score_gemma":0.022605136,"teacher_disagreement_score":0.8660763,"about_ca_system_score_codex":0.00089908356,"about_ca_system_score_gemma":0.0013862969,"threshold_uncertainty_score":0.19102591},"labels":[],"label_agreement":null},{"id":"W6939513244","doi":"10.6084/m9.figshare.17870556.v1","title":"Additional file 3 of Long-duration seismicity and their relation to Copahue volcano unrest","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Unrest; Relation (database); Induced seismicity; Volcano; Seismotectonics; Tracking (education)","score_opus":0.022796957745342766,"score_gpt":0.19480304354590017,"score_spread":0.1720060858005574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6939513244","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00011437274,0.000006028615,0.00005919173,0.000041794,0.0000085898755,0.000034897952,0.9990565,0.000062821164,0.00061575824],"genre_scores_gemma":[0.006676948,0.0000905186,0.0012059575,0.00022631,0.00006647844,0.0009401057,0.9819474,0.00034198735,0.00850428],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9993735,0.0000898999,0.00014324347,0.00013555631,0.00015338937,0.00010442942],"domain_scores_gemma":[0.9832255,0.011783327,0.0011602214,0.0008705101,0.0025917895,0.00036858645],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011234338,0.00080638094,0.0010017997,0.0027532657,0.0008497386,0.0014851021,0.0015894088,0.0010578376,0.8780161],"category_scores_gemma":[0.02484174,0.00044035813,0.0007446344,0.0059976056,0.00021483385,0.0018025194,0.0010635381,0.0007735954,0.15230446],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002172025,0.00006425768,0.0030612939,0.0014838292,0.000033188746,0.000058239068,0.00006687568,0.00038760467,0.000060684968,0.0006173442,0.9887961,0.0051534674],"study_design_scores_gemma":[0.003509506,0.00020455454,0.05749069,0.0034264561,0.00019436797,0.00044569917,0.0010100838,0.0017217378,0.00069009356,0.00837494,0.9227818,0.00015004518],"about_ca_topic_score_codex":0.025478184,"about_ca_topic_score_gemma":0.03165781,"teacher_disagreement_score":0.8780161,"about_ca_system_score_codex":0.0011810749,"about_ca_system_score_gemma":0.0017968323,"threshold_uncertainty_score":0.17399514},"labels":[],"label_agreement":null},{"id":"W6949394760","doi":"10.5281/zenodo.15985965","title":"Data and code for \"Crustal stresses and damage evolve throughout the seismic cycle of the Ridgecrest fault zone\"","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Code (set theory); Fault (geology); Data file; Seismic analysis; Epicenter","score_opus":0.03837718347149556,"score_gpt":0.26822017348662935,"score_spread":0.2298429900151338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6949394760","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0004327133,0.000009609874,0.0009814413,0.00009801006,0.00007194763,0.00004267702,0.9876672,0.0058202464,0.0048761684],"genre_scores_gemma":[0.0022615849,0.000049799677,0.0034864855,0.00014688901,0.000047959522,0.00020302644,0.97980773,0.0052713486,0.00872523],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99946946,0.000043302636,0.000074119074,0.00012604243,0.00021077218,0.00007634718],"domain_scores_gemma":[0.99558026,0.0013131415,0.00037687458,0.00073463155,0.0017407468,0.00025440683],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0005380969,0.0010806945,0.000751044,0.0027798978,0.00060681987,0.0011902777,0.0014350804,0.00088609324,0.4266302],"category_scores_gemma":[0.005383927,0.0007207587,0.0008303124,0.0046107713,0.0002488716,0.0014154386,0.0010754137,0.0014850752,0.23881535],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008794044,0.000031739783,0.0014161067,0.00023930897,0.0000116935535,0.000030064326,0.000033805645,0.00044409087,0.0003902,0.00091111317,0.9892089,0.007194979],"study_design_scores_gemma":[0.00040055384,0.00003421849,0.012199973,0.00020069804,0.000019765537,0.00011596109,0.00010325199,0.0015568996,0.002285623,0.0033571033,0.9796703,0.00005564622],"about_ca_topic_score_codex":0.015414207,"about_ca_topic_score_gemma":0.012125537,"teacher_disagreement_score":0.4266302,"about_ca_system_score_codex":0.0011669542,"about_ca_system_score_gemma":0.0012821509,"threshold_uncertainty_score":0.8178424},"labels":[],"label_agreement":null},{"id":"W6950392637","doi":"10.5683/sp3/9pw48h","title":"Best Practices for Data Extractors","year":2000,"lang":"en","type":"dataset","venue":"Borealis","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Best practice; Key (lock); Presentation (obstetrics); Work (physics); Data collection","score_opus":0.12939727939502293,"score_gpt":0.33223016528514204,"score_spread":0.2028328858901191,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950392637","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":"methods","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":"methods","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0056918673,0.00270229,0.5356125,0.007263916,0.001163877,0.008518794,0.28077066,0.14274111,0.015534981],"genre_scores_gemma":[0.0127380835,0.002218724,0.6422529,0.0013195056,0.00030591319,0.009236955,0.31148115,0.014924753,0.005522048],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.93763274,0.017744431,0.022086574,0.008285776,0.012575943,0.001674583],"domain_scores_gemma":[0.7345115,0.07211905,0.009231218,0.116515905,0.06495111,0.0026712087],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.08348181,0.0036447502,0.0023553371,0.025820134,0.0024981818,0.011104757,0.0060397163,0.0023434155,0.01899516],"category_scores_gemma":[0.27592766,0.0031395631,0.0034513562,0.029955052,0.0018486963,0.013928735,0.0075526685,0.0052549117,0.034921248],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078755704,0.0003382166,0.0072160135,0.0034690865,0.00041881204,0.00034227094,0.0014901285,0.0019464795,0.0061346674,0.009606027,0.56686866,0.40138203],"study_design_scores_gemma":[0.00070390856,0.00014884524,0.00903765,0.0026463394,0.00042984425,0.00062326697,0.0015190223,0.010009583,0.035667628,0.0259942,0.91284966,0.00037015916],"about_ca_topic_score_codex":0.009058813,"about_ca_topic_score_gemma":0.006497688,"teacher_disagreement_score":0.9165182,"about_ca_system_score_codex":0.002383509,"about_ca_system_score_gemma":0.006981304,"threshold_uncertainty_score":0.4414993},"labels":[],"label_agreement":null},{"id":"W6950432277","doi":"10.5281/zenodo.7888779","title":"Rosa granulata Greene","year":2014,"lang":"fr","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Université de Sherbrooke","funders":"","keywords":"Natural (archaeology); Sequence (biology); Feature (linguistics)","score_opus":0.04190149423315951,"score_gpt":0.22017774550168717,"score_spread":0.17827625126852767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950432277","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19392575,0.015278624,0.019590538,0.00602079,0.0025505107,0.000686811,0.046501495,0.0053006606,0.7101448],"genre_scores_gemma":[0.5436574,0.0052012475,0.016298456,0.0026739761,0.0004470287,0.00022941647,0.04708469,0.001126011,0.3832817],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999747,0.000016854614,0.00001128299,0.0001145493,0.0000756973,0.000034578174],"domain_scores_gemma":[0.9997906,0.000011720093,0.00005767248,0.000040611765,0.00006024642,0.000039158178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020653036,0.00043820238,0.00045477325,0.0013183496,0.0010815905,0.000632597,0.00069589267,0.000490969,0.03277929],"category_scores_gemma":[0.00025353246,0.00012596691,0.0002235472,0.00087938627,0.0004428924,0.00045434106,0.001033114,0.00080398476,0.01869441],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007405825,0.00019889393,0.017481156,0.00070660707,0.00013346181,0.0023364436,0.0009997863,0.00043718185,0.38538533,0.041296456,0.22023077,0.3300533],"study_design_scores_gemma":[0.00004058624,0.00004348251,0.06035209,0.00009246926,0.000024835792,0.00089652365,0.00028190843,0.000114499104,0.004546766,0.0017883239,0.93179953,0.000018988765],"about_ca_topic_score_codex":0.012950134,"about_ca_topic_score_gemma":0.023408273,"teacher_disagreement_score":0.03277929,"about_ca_system_score_codex":0.0008761946,"about_ca_system_score_gemma":0.00024888132,"threshold_uncertainty_score":0.109657705},"labels":[],"label_agreement":null},{"id":"W6950470332","doi":"10.5683/sp3/niuc86","title":"Données de réplication pour : Postoperative complication rate and owner satisfaction comparison of enucleation versus evisceration","year":2024,"lang":"en","type":"dataset","venue":"Borealis","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal","funders":"","keywords":"Enucleation; Evisceration (ophthalmology); Complication; Patient satisfaction; Medical record; Eye Enucleation","score_opus":0.043260126850104434,"score_gpt":0.2917669852115856,"score_spread":0.24850685836148118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950470332","genre_codex":"empirical","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.38994023,0.110009365,0.056116305,0.08147521,0.049774654,0.038362283,0.1716274,0.0013593879,0.10133518],"genre_scores_gemma":[0.7961417,0.028398547,0.046858486,0.041875724,0.004135442,0.046196558,0.022375343,0.00080558466,0.013212657],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.8603586,0.049708135,0.052482493,0.0048083393,0.030459972,0.0021824304],"domain_scores_gemma":[0.4774044,0.32891628,0.04199889,0.03037945,0.119570345,0.0017307241],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.08904702,0.00096050935,0.0016812362,0.0042245868,0.0016842723,0.0035581377,0.0019648615,0.0027180251,0.015481597],"category_scores_gemma":[0.47282535,0.0007090194,0.004323914,0.0048290985,0.0019259911,0.0028043576,0.0016299883,0.0020586848,0.0030793343],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0056229103,0.0018070792,0.20635967,0.10725338,0.006804466,0.0053264704,0.03893879,0.0008782598,0.007301774,0.004205193,0.25213328,0.36336872],"study_design_scores_gemma":[0.0010586743,0.0026650399,0.23209457,0.06992069,0.0044724885,0.0058036437,0.022868317,0.0012092193,0.010485525,0.003712965,0.64510006,0.0006087229],"about_ca_topic_score_codex":0.013180438,"about_ca_topic_score_gemma":0.014513868,"teacher_disagreement_score":0.08904702,"about_ca_system_score_codex":0.0028339685,"about_ca_system_score_gemma":0.0073625557,"threshold_uncertainty_score":0.4709313},"labels":[],"label_agreement":null},{"id":"W6950650117","doi":"10.5281/zenodo.7760705","title":"New Insights into the Active Tectonics of the Northern Canadian Cordillera from an Enhanced Earthquake Catalog","year":2023,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tectonics; Seismotectonics; Intraplate earthquake; Plate tectonics; Feature (linguistics)","score_opus":0.021564495627570176,"score_gpt":0.21572865609315695,"score_spread":0.19416416046558677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6950650117","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15045805,0.0047757663,0.0045038196,0.0020815881,0.00035455704,0.0004702512,0.5925329,0.0013544247,0.24346872],"genre_scores_gemma":[0.2579024,0.009866253,0.025945084,0.0003313778,0.00021216867,0.00023440248,0.5443469,0.0004102,0.1607512],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997453,0.0000072966886,0.000025694118,0.000034846627,0.00013193603,0.000054912958],"domain_scores_gemma":[0.99799323,0.00007883714,0.00007812641,0.00017832035,0.0015077943,0.00016368466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003432308,0.00052863255,0.00028599988,0.013224887,0.0014663559,0.0017232242,0.0008278957,0.0002805291,0.0388237],"category_scores_gemma":[0.0020728153,0.00024896723,0.00022082058,0.018978294,0.00033137118,0.0009156988,0.000896074,0.00038738266,0.0041627064],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020685476,0.0000629829,0.1012024,0.000801608,0.00005114217,0.0005286177,0.004001406,0.002551674,0.004564838,0.015879165,0.43204996,0.43809938],"study_design_scores_gemma":[0.000018017588,0.000010757643,0.34652627,0.0001748385,0.00004875538,0.00014817012,0.0011664857,0.0008326689,0.0004496768,0.000881075,0.64971393,0.000029287688],"about_ca_topic_score_codex":0.9806208,"about_ca_topic_score_gemma":0.9930214,"teacher_disagreement_score":0.0388237,"about_ca_system_score_codex":0.007936421,"about_ca_system_score_gemma":0.018020466,"threshold_uncertainty_score":0.12987822},"labels":[],"label_agreement":null},{"id":"W6954917026","doi":"10.57745/q3li1k","title":"FRM DEPLOYMENT - Guidelines for forest managers and tree breeders","year":2023,"lang":"en","type":"dataset","venue":"Recherche Data Gouv France","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Tree (set theory); Software deployment; Forest industry; Variety (cybernetics); Forest management","score_opus":0.42377554309135773,"score_gpt":0.4003970031547701,"score_spread":0.023378539936587617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6954917026","genre_codex":"dataset","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00014346236,0.00003029925,0.0004340225,0.00013147721,0.000031579755,0.00004148373,0.9961498,0.0015288028,0.0015090556],"genre_scores_gemma":[0.00039391176,0.000038627793,0.0022385847,0.000081262406,0.000010181674,0.0002889819,0.9948915,0.0005939289,0.0014630693],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9972281,0.0006245541,0.00043471303,0.0006341345,0.00071147655,0.00036700364],"domain_scores_gemma":[0.990612,0.002440668,0.00073344575,0.0029896346,0.002566663,0.00065757066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0043097413,0.0023353302,0.0013756054,0.005612013,0.0008461322,0.0028271542,0.0030741303,0.0025929874,0.12135739],"category_scores_gemma":[0.020741865,0.0013180414,0.0017693377,0.0070513613,0.00044255753,0.0028636463,0.002803204,0.002189273,0.16900407],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045899375,0.000016568858,0.0006890296,0.00017187654,0.00001077751,0.000010896423,0.000024855395,0.00025327248,0.00008236454,0.00040397016,0.995158,0.0031323724],"study_design_scores_gemma":[0.00021948502,0.000014174378,0.0045376937,0.00037941968,0.00001805952,0.000034610366,0.00012885434,0.00085994415,0.00044434128,0.0024380155,0.99088585,0.000039446746],"about_ca_topic_score_codex":0.04620972,"about_ca_topic_score_gemma":0.06385864,"teacher_disagreement_score":0.12135739,"about_ca_system_score_codex":0.0019677419,"about_ca_system_score_gemma":0.0034375044,"threshold_uncertainty_score":0.40598089},"labels":[],"label_agreement":null},{"id":"W6955016373","doi":"10.57757/iugg23-0347","title":"Using relative event locations of swarms of small earthquakes to look for seismically active structures in Northeastern North America","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Earthquake swarm; Induced seismicity; Event (particle physics); Seismic hazard; Seismotectonics; Swarm behaviour; Foreshock; Remotely triggered earthquakes","score_opus":0.07807780299174381,"score_gpt":0.3457818024537986,"score_spread":0.26770399946205475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6955016373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.815292,0.0013041547,0.0018058859,0.00027647385,0.00004020237,0.000114904644,0.15984218,0.0002488503,0.021075312],"genre_scores_gemma":[0.7508512,0.0022754723,0.008197707,0.00006432139,0.000043401837,0.00016932086,0.22774556,0.00007122501,0.010581792],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972683,0.00003869264,0.000054330194,0.000070696384,0.00008520019,0.000024267052],"domain_scores_gemma":[0.99875927,0.00020716904,0.00031047896,0.00010327947,0.00053455005,0.000085229585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047371676,0.00014554455,0.00016897178,0.0044195196,0.00023033799,0.0005071546,0.0004285333,0.00018961236,0.005026868],"category_scores_gemma":[0.0014361604,0.00010795563,0.0000933549,0.006555741,0.00012945,0.00049310416,0.00038003974,0.00008506488,0.0012068828],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003075464,0.00008239231,0.80775297,0.0006025798,0.00009840833,0.00039220788,0.0014002806,0.0017058415,0.008041205,0.0007382638,0.0364232,0.14245518],"study_design_scores_gemma":[0.000009952338,0.000020083886,0.9872334,0.00003594757,0.000025458236,0.000055920304,0.00057201606,0.0006783168,0.0005686686,0.00005210382,0.010739325,0.00000882684],"about_ca_topic_score_codex":0.2537363,"about_ca_topic_score_gemma":0.43755826,"teacher_disagreement_score":0.2537363,"about_ca_system_score_codex":0.0007283419,"about_ca_system_score_gemma":0.00079901534,"threshold_uncertainty_score":0.50451875},"labels":[],"label_agreement":null},{"id":"W6955052635","doi":"10.57757/iugg23-1736","title":"Can glacial isostatic adjustment modelling confirm potential signs of glacially triggered faulting in Canada?","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Fault (geology); Post-glacial rebound; Stress field; Sea level; Glacial period","score_opus":0.06116297003673363,"score_gpt":0.30986034870080464,"score_spread":0.24869737866407102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6955052635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97051615,0.0007239268,0.0054766866,0.0007568488,0.000053706015,0.00004035093,0.008421224,0.00048367,0.013527481],"genre_scores_gemma":[0.991355,0.0004068642,0.0028746242,0.000041783213,0.000004230391,0.000008082931,0.002812059,0.000058539656,0.0024388002],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999145,0.0000066901594,0.0000046480977,0.000018231007,0.000026175729,0.000029665824],"domain_scores_gemma":[0.9997112,0.00004987981,0.000026186708,0.000019378951,0.00015435086,0.00003889485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013229037,0.00034864814,0.00023860518,0.0006620251,0.0005532027,0.0012482462,0.0007751453,0.00047451493,0.0033700939],"category_scores_gemma":[0.0010132104,0.00014989414,0.00037559523,0.0011338794,0.00045282964,0.00030869662,0.00026674324,0.0002934962,0.00036140674],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032407342,0.000087706314,0.3078731,0.00039321656,0.0001623903,0.00047836994,0.0004131613,0.61343324,0.005800606,0.0040784013,0.006565611,0.06039015],"study_design_scores_gemma":[0.00005410641,0.000051630177,0.20103948,0.00013061073,0.00010789765,0.00007001737,0.0008085551,0.78104746,0.0028923017,0.0014784687,0.01224196,0.00007746736],"about_ca_topic_score_codex":0.9648181,"about_ca_topic_score_gemma":0.9711546,"teacher_disagreement_score":0.03518188,"about_ca_system_score_codex":0.0067999563,"about_ca_system_score_gemma":0.010695937,"threshold_uncertainty_score":0.07077807},"labels":[],"label_agreement":null},{"id":"W6958299771","doi":"10.6084/m9.figshare.21430202","title":"Stochastic source modeling and tsunami simulations of cascadia subduction earthquakes for Canadian Pacific coast","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Tsunami earthquake; Moment magnitude scale; Seismic hazard; Shore; Hazard analysis; Fault (geology); Submarine pipeline","score_opus":0.03786096158399294,"score_gpt":0.22098643064528303,"score_spread":0.1831254690612901,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6958299771","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9667437,0.00016627985,0.023355214,0.00030977122,0.00001856319,0.000050729755,0.0012473422,0.00024582818,0.007862629],"genre_scores_gemma":[0.9949232,0.00011816017,0.0031086958,0.000015333373,0.000004285961,0.00002470784,0.00051347393,0.0000225538,0.001269642],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988925,0.000017419965,0.0000063641455,0.000017202394,0.00003578301,0.000034025677],"domain_scores_gemma":[0.9996699,0.000120403696,0.000052838943,0.00001755967,0.00010752593,0.000031850053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002251412,0.0007086827,0.00035911353,0.00070204923,0.00073613,0.00056271744,0.0011368678,0.0005990115,0.0012102535],"category_scores_gemma":[0.0010876459,0.00043072068,0.0005020928,0.0007104297,0.00043520678,0.0004265682,0.00043414623,0.00047940068,0.00009912739],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012214583,0.000010376242,0.002077739,0.0000061239157,0.000009727167,0.000025355539,0.000022243485,0.995741,0.00020493369,0.00090210175,0.00012508317,0.0008631191],"study_design_scores_gemma":[0.0000048089883,0.0000037399896,0.00085608085,9.679517e-7,0.0000032580945,0.0000036936128,0.000011376,0.9987533,0.00007449361,0.00017849208,0.00010648871,0.0000031485283],"about_ca_topic_score_codex":0.7816714,"about_ca_topic_score_gemma":0.7104438,"teacher_disagreement_score":0.2183286,"about_ca_system_score_codex":0.0045977836,"about_ca_system_score_gemma":0.0036307664,"threshold_uncertainty_score":0.4392287},"labels":[],"label_agreement":null},{"id":"W6966861319","doi":"10.48549/2681","title":"Sedimentological signatures of lacustrine tsunamis","year":2021,"lang":"en","type":"dissertation","venue":"BORIS Theses (Bern Open Research Information System) (Bern University Library, Hochschulstrasse 6, 3012 Bern, Switzerland)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Subaerial; Fault (geology); Geologic record; Submarine pipeline; Mass wasting; Radiocarbon dating; Volcano; Prehistory; Stratigraphy; Natural hazard; Geologic hazards","score_opus":0.045074312312127836,"score_gpt":0.27763081521684235,"score_spread":0.23255650290471452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6966861319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99596643,0.00037300627,0.00017979648,0.000032024916,0.0000071903155,0.000008661389,0.0010824652,0.000038637052,0.0023116465],"genre_scores_gemma":[0.9984395,0.00016307352,0.00016395177,0.000006925699,0.000007676703,0.0000035613505,0.0006604094,0.000006379596,0.000548631],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999231,0.0000056022773,0.000010661694,0.000019133759,0.00002284353,0.000018663808],"domain_scores_gemma":[0.9997247,0.000018289309,0.00011053537,0.000012430759,0.00007900805,0.00005512858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012235939,0.00040931397,0.00019373727,0.00251994,0.00027099747,0.00083102396,0.00016268413,0.00029295165,0.0017808938],"category_scores_gemma":[0.00040111705,0.00014499782,0.00015244297,0.0020680507,0.0002498516,0.00022705353,0.0004083058,0.00015987443,0.00040203347],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004520818,0.000037894708,0.9419029,0.00010975201,0.000100767706,0.001905623,0.00094525376,0.0010184761,0.034720276,0.00023504301,0.0007052285,0.017866785],"study_design_scores_gemma":[0.0000041481785,0.000029435887,0.99827945,0.000005130589,0.000009954798,0.00014417768,0.00020058251,0.0002753366,0.00038896894,0.000033107845,0.00062525197,0.000004393677],"about_ca_topic_score_codex":0.010084901,"about_ca_topic_score_gemma":0.0146852685,"teacher_disagreement_score":0.010084901,"about_ca_system_score_codex":0.00026551215,"about_ca_system_score_gemma":0.00016788389,"threshold_uncertainty_score":0.020052373},"labels":[],"label_agreement":null},{"id":"W6967466573","doi":"10.5281/zenodo.10146527","title":"SeisSol input files for \"Fault-size dependent fracture energy explains multi-scale seismicity and cascading earthquakes\"","year":2023,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Induced seismicity; Fracture (geology); Energy (signal processing); Seismic energy; Data file","score_opus":0.03390832087814432,"score_gpt":0.23566249298347952,"score_spread":0.2017541721053352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6967466573","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0024697534,0.000082084705,0.015316063,0.0002213672,0.00023310703,0.00012091935,0.87258154,0.08938457,0.019590532],"genre_scores_gemma":[0.012183153,0.00016460336,0.011827849,0.00029872463,0.00009077578,0.0004874628,0.89295524,0.06304823,0.018944064],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99972564,0.000032261483,0.000027265107,0.00005757136,0.00010602716,0.00005118677],"domain_scores_gemma":[0.99802136,0.00071667164,0.00011300328,0.00030991217,0.00073096494,0.00010807763],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00052212004,0.0016141697,0.000911745,0.0014321622,0.00059039914,0.0015802935,0.002628083,0.0010877185,0.45722473],"category_scores_gemma":[0.004123236,0.0010784797,0.0012722409,0.0018302718,0.00023107423,0.0016184718,0.0013909221,0.0013850023,0.22349896],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023287389,0.00005023343,0.0017705007,0.00061760395,0.00005024699,0.000114666036,0.00007167103,0.0029354868,0.000997358,0.002638657,0.9794448,0.011075861],"study_design_scores_gemma":[0.00089186034,0.0000757907,0.004729539,0.00032426737,0.000067345456,0.00026425743,0.00018506961,0.01657622,0.010315014,0.007880393,0.9585862,0.00010398806],"about_ca_topic_score_codex":0.0063335295,"about_ca_topic_score_gemma":0.008036392,"teacher_disagreement_score":0.45722473,"about_ca_system_score_codex":0.0011480084,"about_ca_system_score_gemma":0.0008149112,"threshold_uncertainty_score":0.77420306},"labels":[],"label_agreement":null},{"id":"W6967480521","doi":"10.5281/zenodo.13589207","title":"SeisSol input files and geodetic results for \"Non-typical supershear rupture: fault heterogeneity and segmentation govern unilateral supershear and cascading multi-fault rupture in the 2021 Mw 7.4 Maduo Earthquake\"","year":2024,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Continental (Canada)","funders":"Agence Nationale de la Recherche; European Commission; National Aeronautics and Space Administration","keywords":"Geodetic datum; Fault (geology); Segmentation","score_opus":0.029983306595423833,"score_gpt":0.24817710751923427,"score_spread":0.21819380092381044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6967480521","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0022687695,0.000033042274,0.0033858484,0.00013632013,0.00010339996,0.0000709999,0.9536587,0.025323687,0.015019297],"genre_scores_gemma":[0.012791738,0.000086846914,0.0050934795,0.00014982793,0.00004929919,0.00028275323,0.95507586,0.014428593,0.012041581],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99978465,0.00002131323,0.00001917246,0.00004185159,0.00008832083,0.000044699394],"domain_scores_gemma":[0.99870396,0.0004000547,0.00009865556,0.00018124314,0.00054005487,0.00007598752],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00035805927,0.0012170004,0.00080247,0.0015096506,0.0005091538,0.0013334068,0.0020237004,0.0009867849,0.4114542],"category_scores_gemma":[0.0028081308,0.0008648937,0.000826095,0.0022011015,0.00018878684,0.0010474409,0.0008541071,0.0009286033,0.18571247],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020656215,0.00005519332,0.0029658217,0.0004027607,0.00003766565,0.00010772044,0.00005509556,0.0042889426,0.0006231929,0.0015528912,0.9829784,0.0067257737],"study_design_scores_gemma":[0.0015052778,0.000119202436,0.012041086,0.0003039311,0.000080486425,0.0002487085,0.00034256157,0.02567891,0.010068262,0.0055212737,0.94396955,0.000120779405],"about_ca_topic_score_codex":0.0138500035,"about_ca_topic_score_gemma":0.01854649,"teacher_disagreement_score":0.4114542,"about_ca_system_score_codex":0.0011824218,"about_ca_system_score_gemma":0.00080918474,"threshold_uncertainty_score":0.83948916},"labels":[],"label_agreement":null},{"id":"W6967557288","doi":"10.5281/zenodo.10123384","title":"Fig. 49 in A revision of Scipopus Enderlein including the subgenera Scipopus s. str., Phaeopterina Frey and Parascipopus subgen. nov. (Diptera, Micropezidae, Taeniapterinae)","year":2023,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Subgenus; Holotype; Genus; Paratype","score_opus":0.04878140005579797,"score_gpt":0.2524224338556221,"score_spread":0.2036410337998241,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6967557288","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.043447163,0.0035262776,0.009522058,0.00091068447,0.0029905564,0.0009771634,0.049756147,0.0013756617,0.8874943],"genre_scores_gemma":[0.35674,0.009256584,0.030959534,0.0010355489,0.0017431603,0.0015006079,0.14396417,0.0014224186,0.45337787],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998472,0.000026584978,0.000014703408,0.000039343293,0.00005083487,0.000021423468],"domain_scores_gemma":[0.99984336,0.000029334591,0.000026716329,0.000022661941,0.00005996894,0.0000179948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017142895,0.00067374925,0.00022178846,0.0028060835,0.0009557838,0.0006207582,0.00054532394,0.0003807249,0.09943067],"category_scores_gemma":[0.0006958167,0.0001889999,0.00020120166,0.0028704992,0.00080652075,0.0008468522,0.0006560373,0.0008527999,0.023985464],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036717244,0.000060535076,0.012839218,0.0015690499,0.00005073567,0.0007831189,0.0019028618,0.0007033375,0.006223724,0.015252074,0.47760144,0.4826467],"study_design_scores_gemma":[0.00001797951,0.00003513757,0.04091338,0.00019705552,0.000021319596,0.0008428671,0.0004675146,0.00015696169,0.00056908076,0.000864789,0.9559002,0.000013714937],"about_ca_topic_score_codex":0.010661536,"about_ca_topic_score_gemma":0.021734865,"teacher_disagreement_score":0.09943067,"about_ca_system_score_codex":0.00054091,"about_ca_system_score_gemma":0.00054802536,"threshold_uncertainty_score":0.3326288},"labels":[],"label_agreement":null},{"id":"W6967769975","doi":"10.5281/zenodo.11910779","title":"schiller die räuber pdf","year":2024,"lang":"de","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"German; Poetry; Download; First world war; Middle Ages","score_opus":0.029883917540749833,"score_gpt":0.2247329053336797,"score_spread":0.19484898779292986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6967769975","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00056852016,0.0006981536,0.0001555273,0.0025344659,0.0018843183,0.00010368872,0.0022238498,0.0013806282,0.9904509],"genre_scores_gemma":[0.002124271,0.0004321529,0.000115894836,0.001019095,0.0004721198,0.000038365997,0.0011906447,0.00037781292,0.9942297],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99942493,0.000050810646,0.000020990235,0.00006885362,0.00032890256,0.00010546228],"domain_scores_gemma":[0.99886596,0.0001212302,0.00005762827,0.00009598434,0.0004508275,0.0004083758],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00043600137,0.0008831885,0.00056427845,0.0018080384,0.0023641505,0.0056368015,0.0007047481,0.0019142767,0.8789071],"category_scores_gemma":[0.0026460197,0.00038413788,0.00038739596,0.001277231,0.0004309595,0.003669708,0.0027106137,0.0013688724,0.77250224],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015564188,0.000012470493,0.00004803076,0.000043494307,7.8557946e-7,0.000033100558,0.000022164439,0.000010454453,0.00010816357,0.000873088,0.97510624,0.023726435],"study_design_scores_gemma":[0.000004850643,0.0000084899075,0.00032962344,0.000033145127,7.008062e-7,0.000035828143,0.00003852823,0.000014267904,0.000063935106,0.0001651282,0.9993017,0.0000039192723],"about_ca_topic_score_codex":0.0034582992,"about_ca_topic_score_gemma":0.012617129,"teacher_disagreement_score":0.121092916,"about_ca_system_score_codex":0.0012188113,"about_ca_system_score_gemma":0.00092097244,"threshold_uncertainty_score":0.17272425},"labels":[],"label_agreement":null},{"id":"W6973275606","doi":"10.57757/iugg23-2989","title":"Evidence of the ambiguous critical state transition from aseismic to seismic slip","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Induced seismicity; Aftershock; Slip (aerodynamics); Remotely triggered earthquakes; Shear (geology); Passive seismic; Foreshock; Fault (geology)","score_opus":0.0828378630555488,"score_gpt":0.35151360747078897,"score_spread":0.26867574441524017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6973275606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954202,0.00010486363,0.0010643122,0.00007298724,0.000005000007,0.000011347057,0.00046092636,0.000039323415,0.0028210816],"genre_scores_gemma":[0.9990907,0.000047286543,0.00031839873,0.000017234071,0.0000021345884,0.0000024744827,0.00027031274,0.0000032824337,0.00024823725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989617,0.0000044826756,0.000006647058,0.000025087314,0.000038746428,0.000028828383],"domain_scores_gemma":[0.9992865,0.00009728952,0.0001444315,0.000034232344,0.00035442374,0.00008327036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014079807,0.00011190101,0.00013176414,0.0005250128,0.0004400453,0.0005124427,0.00028908756,0.00025476,0.0016610933],"category_scores_gemma":[0.000830737,0.000111016525,0.00009026361,0.00058961497,0.000671834,0.00017823934,0.00025681048,0.00024843373,0.00017832451],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042766464,0.000092925504,0.6362664,0.00018896353,0.00007094585,0.0011345524,0.0022216814,0.002002687,0.32422486,0.0015960335,0.0013554321,0.030417806],"study_design_scores_gemma":[0.000006247191,0.00007442266,0.9816939,0.000016923763,0.000016790347,0.00025594106,0.0010051805,0.0024374009,0.012427276,0.00031817012,0.0017331254,0.00001460221],"about_ca_topic_score_codex":0.15145573,"about_ca_topic_score_gemma":0.27875367,"teacher_disagreement_score":0.15145573,"about_ca_system_score_codex":0.001119204,"about_ca_system_score_gemma":0.00082475797,"threshold_uncertainty_score":0.3011483},"labels":[],"label_agreement":null},{"id":"W6974098827","doi":"10.57757/iugg23-2522","title":"The next cascadia slab model","year":2023,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of British Columbia","funders":"","keywords":"Subduction; Oceanic crust; Crust; Slab; Receiver function; Shear zone; Convergent boundary","score_opus":0.0992378699110365,"score_gpt":0.3438069607067189,"score_spread":0.2445690907956824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6974098827","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.38271692,0.0018177074,0.38880005,0.0032207593,0.0004889593,0.00021498847,0.023756664,0.004172126,0.19481176],"genre_scores_gemma":[0.9175262,0.0009207057,0.029957559,0.00019009369,0.00008144443,0.00024678785,0.005657681,0.00037988203,0.045039598],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999182,0.000018905917,0.0000044644335,0.000026505299,0.000016301854,0.000015659438],"domain_scores_gemma":[0.9998301,0.000028961167,0.00001558583,0.00002490692,0.000071114846,0.000029148145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016700545,0.0008422069,0.00051864225,0.000582947,0.00066234946,0.0011096611,0.0020052905,0.0009111133,0.011037462],"category_scores_gemma":[0.0005703657,0.00045922623,0.0008260324,0.0008603476,0.0005343678,0.0007243534,0.0009264166,0.0007111656,0.0014009392],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031931275,0.000009023273,0.001091009,0.00002439255,0.000026189186,0.00007412719,0.000038279104,0.98364645,0.00048330956,0.010004942,0.0013942372,0.0031761136],"study_design_scores_gemma":[0.000019563242,0.0000078645035,0.00052744447,0.00000795211,0.000017116838,0.000021950927,0.000027126778,0.99025905,0.000090426394,0.005339833,0.003672228,0.000009499474],"about_ca_topic_score_codex":0.11915069,"about_ca_topic_score_gemma":0.059048817,"teacher_disagreement_score":0.11915069,"about_ca_system_score_codex":0.0017693402,"about_ca_system_score_gemma":0.0017740019,"threshold_uncertainty_score":0.23691434},"labels":[],"label_agreement":null},{"id":"W6977042200","doi":"10.6084/m9.figshare.21430202.v1","title":"Stochastic source modeling and tsunami simulations of cascadia subduction earthquakes for Canadian Pacific coast","year":2022,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Tsunami earthquake; Moment magnitude scale; Seismic hazard; Shore; Hazard analysis; Fault (geology); Submarine pipeline","score_opus":0.03786096158399294,"score_gpt":0.22098643064528303,"score_spread":0.1831254690612901,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6977042200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9667437,0.00016627985,0.023355214,0.00030977122,0.00001856319,0.000050729755,0.0012473422,0.00024582818,0.007862629],"genre_scores_gemma":[0.9949232,0.00011816017,0.0031086958,0.000015333373,0.000004285961,0.00002470784,0.00051347393,0.0000225538,0.001269642],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988925,0.000017419965,0.0000063641455,0.000017202394,0.00003578301,0.000034025677],"domain_scores_gemma":[0.9996699,0.000120403696,0.000052838943,0.00001755967,0.00010752593,0.000031850053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002251412,0.0007086827,0.00035911353,0.00070204923,0.00073613,0.00056271744,0.0011368678,0.0005990115,0.0012102535],"category_scores_gemma":[0.0010876459,0.00043072068,0.0005020928,0.0007104297,0.00043520678,0.0004265682,0.00043414623,0.00047940068,0.00009912739],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012214583,0.000010376242,0.002077739,0.0000061239157,0.000009727167,0.000025355539,0.000022243485,0.995741,0.00020493369,0.00090210175,0.00012508317,0.0008631191],"study_design_scores_gemma":[0.0000048089883,0.0000037399896,0.00085608085,9.679517e-7,0.0000032580945,0.0000036936128,0.000011376,0.9987533,0.00007449361,0.00017849208,0.00010648871,0.0000031485283],"about_ca_topic_score_codex":0.7816714,"about_ca_topic_score_gemma":0.7104438,"teacher_disagreement_score":0.2183286,"about_ca_system_score_codex":0.0045977836,"about_ca_system_score_gemma":0.0036307664,"threshold_uncertainty_score":0.4392287},"labels":[],"label_agreement":null},{"id":"W6980773370","doi":"","title":"Contribution des boues d'alun d'usines de traitement d'eau potable à la déphosphatation chimique des eaux résiduaires au Québec","year":2005,"lang":"fr","type":"other","venue":"PolyPublie (École Polytechnique de Montréal)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Water pollution; Potable water; Sewage sludge; Water quality","score_opus":0.011612595579603218,"score_gpt":0.22063314280241786,"score_spread":0.20902054722281463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6980773370","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8962122,0.005738334,0.0052617653,0.0024115953,0.00038475855,0.00040053207,0.0029654233,0.00015064639,0.08647484],"genre_scores_gemma":[0.75868446,0.003648507,0.005649603,0.0005531735,0.00006260474,0.00006999626,0.0013008531,0.00007155177,0.22995922],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9993105,0.0000743862,0.00002250412,0.00010309149,0.00034238116,0.00014719578],"domain_scores_gemma":[0.99809545,0.00014464729,0.000114216855,0.0000591749,0.0012471903,0.00033929458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081247924,0.0004805434,0.00029859517,0.0011983179,0.0026538016,0.0012365327,0.0006454542,0.00039502725,0.006974518],"category_scores_gemma":[0.0009988962,0.00020793959,0.0003061561,0.000738202,0.0006224532,0.00038526708,0.0005350816,0.0005949096,0.0006373871],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019560421,0.0011968979,0.3058707,0.0007867412,0.00027163676,0.003205687,0.007278759,0.0047139646,0.07447503,0.0046150247,0.030197484,0.5654321],"study_design_scores_gemma":[0.00006155961,0.0008676475,0.55430007,0.00015192172,0.00014106222,0.00066398835,0.004009896,0.0030845571,0.035627477,0.00035238,0.40066966,0.00006975339],"about_ca_topic_score_codex":0.90343964,"about_ca_topic_score_gemma":0.9529821,"teacher_disagreement_score":0.09656036,"about_ca_system_score_codex":0.011517081,"about_ca_system_score_gemma":0.015846431,"threshold_uncertainty_score":0.19425797},"labels":[],"label_agreement":null},{"id":"W6987778717","doi":"","title":"TWO DECADES OF GLOBAL TSUNAMIS - 1982-2002","year":2003,"lang":"en","type":"article","venue":"DOAJ (DOAJ: Directory of Open Access Journals)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pacific ocean; Death toll; Nautical mile; Indian ocean; Mediterranean sea; Mediterranean climate; Caribbean island","score_opus":0.1827295017805838,"score_gpt":0.49623505588768246,"score_spread":0.3135055541070987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6987778717","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.08468326,0.007636244,0.001031009,0.0008583928,0.00096120447,0.00021252599,0.790846,0.0010752842,0.1126961],"genre_scores_gemma":[0.12244724,0.0060464256,0.0013946589,0.00048222032,0.00041322436,0.0002678303,0.8099721,0.0002770932,0.058699224],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9997515,0.000011397386,0.000041241314,0.00005764768,0.00009295124,0.00004521208],"domain_scores_gemma":[0.99902797,0.00003826578,0.00023143756,0.00007197319,0.0005406637,0.00008976397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002589678,0.0009459426,0.00044676062,0.00556857,0.00043496813,0.0014273797,0.00054749387,0.0003644314,0.015776549],"category_scores_gemma":[0.0009274707,0.00020116905,0.00031153104,0.009996823,0.00010993148,0.00092611957,0.0008871433,0.00039608573,0.011109004],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043602774,0.00008034585,0.15727335,0.0022192425,0.00014040015,0.0005995733,0.0013629331,0.0011814465,0.0014879879,0.00180899,0.6294301,0.20397954],"study_design_scores_gemma":[0.000021398057,0.000044814606,0.48954967,0.00032874782,0.000039331724,0.00038289235,0.00060182356,0.00025335434,0.00036301234,0.00022395937,0.50817364,0.000017331633],"about_ca_topic_score_codex":0.026172653,"about_ca_topic_score_gemma":0.046221357,"teacher_disagreement_score":0.026172653,"about_ca_system_score_codex":0.00076540024,"about_ca_system_score_gemma":0.0009450169,"threshold_uncertainty_score":0.052777827},"labels":[],"label_agreement":null},{"id":"W6987886849","doi":"","title":"11210760 from United States/Minnesota/Fort Snelling/Fort Snelling Short Barracks/10 S :: 20 E southeast quarter","year":2016,"lang":"en","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Quarter (Canadian coin); Southeast asia; Population; Period (music)","score_opus":0.01707475706742338,"score_gpt":0.21964889168994506,"score_spread":0.2025741346225217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6987886849","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0009864803,0.00015231484,0.0002856688,0.000717185,0.0006018552,0.00016868032,0.029584266,0.001429593,0.966074],"genre_scores_gemma":[0.0014762366,0.000121679295,0.00017014744,0.00014442364,0.000055620985,0.000048620106,0.010333133,0.00029685453,0.9873533],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997812,0.000015884123,0.000010625124,0.00004705242,0.00009855451,0.00004677066],"domain_scores_gemma":[0.9990382,0.00005260851,0.000043735738,0.000099885896,0.0003884015,0.00037719557],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00030553326,0.0013183741,0.0004704805,0.001645455,0.0017386914,0.0017645302,0.0010681048,0.0011853278,0.8735732],"category_scores_gemma":[0.0014962472,0.0004852647,0.00035034606,0.0011761099,0.0003387754,0.0006951563,0.0019825583,0.0010242957,0.81502634],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039787243,0.00006238364,0.0004912533,0.000056540935,0.0000025570093,0.000025162637,0.000021770029,0.000047338817,0.00020395164,0.0005482177,0.9645321,0.03396907],"study_design_scores_gemma":[0.000039174323,0.00003380895,0.0034823832,0.000103684535,0.0000043926807,0.000027765089,0.00007779244,0.00012173062,0.00024249092,0.00027406533,0.9955872,0.0000055860337],"about_ca_topic_score_codex":0.04759063,"about_ca_topic_score_gemma":0.123397276,"teacher_disagreement_score":0.8735732,"about_ca_system_score_codex":0.0011426726,"about_ca_system_score_gemma":0.0030668657,"threshold_uncertainty_score":0.18033242},"labels":[],"label_agreement":null},{"id":"W6989265294","doi":"","title":"The Antarctic Seismographic Argentinean Italian Network (ASAIN): Recording Earthquakes in the Scotia Sea Region","year":2021,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nova scotia; Submarine pipeline; Feature (linguistics); North sea; Field (mathematics)","score_opus":0.05237218267920251,"score_gpt":0.306060545779696,"score_spread":0.2536883631004935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6989265294","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3651387,0.0014964374,0.00032980286,0.00028085036,0.00009442813,0.00024372282,0.6088791,0.00014158223,0.023395445],"genre_scores_gemma":[0.45251393,0.003090631,0.0022074413,0.00012110121,0.00012312634,0.00035926542,0.5212803,0.00014432317,0.020159911],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99965024,0.000042191543,0.00006184503,0.000054690903,0.000101002624,0.00008996151],"domain_scores_gemma":[0.99684405,0.00025945503,0.0006586448,0.00028456456,0.001522314,0.00043088198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062254875,0.00055866095,0.00029777442,0.007553694,0.000581234,0.00090344547,0.00042649682,0.00018965808,0.007220113],"category_scores_gemma":[0.0027400036,0.00020829738,0.00017511194,0.015541613,0.00020189946,0.0002780021,0.0007907735,0.00015306813,0.0024292772],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006122291,0.000064968124,0.83218515,0.00091699685,0.00011056036,0.0005815971,0.0013556755,0.00068061537,0.0027510154,0.00041118663,0.10595573,0.054374207],"study_design_scores_gemma":[0.000015578722,0.000018728228,0.9651603,0.00007224746,0.000031067197,0.000067802146,0.0003431227,0.0000981215,0.00021492146,0.00001702873,0.033956368,0.000004731906],"about_ca_topic_score_codex":0.60179335,"about_ca_topic_score_gemma":0.6823086,"teacher_disagreement_score":0.60179335,"about_ca_system_score_codex":0.0013913461,"about_ca_system_score_gemma":0.0050713755,"threshold_uncertainty_score":0.80110353},"labels":[],"label_agreement":null},{"id":"W6989799795","doi":"","title":"A case study of dynamic triggering in the Kiskatinaw area of the Montney Formation, British Columbia","year":2021,"lang":"en","type":"dissertation","venue":"eScholarship@McGill (McGill)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Waveform; Magnitude (astronomy); Ground motion; Surface wave; Filter (signal processing)","score_opus":0.017125925863766614,"score_gpt":0.21697484883555332,"score_spread":0.1998489229717867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6989799795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98482794,0.00019145444,0.00017949668,0.00035564296,0.000006440694,0.00004710601,0.00010730683,0.000007877957,0.014276761],"genre_scores_gemma":[0.9941999,0.00023559506,0.00020477072,0.000055148466,0.000002566894,0.000010399997,0.00006936159,0.0000048188704,0.005217353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995389,0.000081985614,0.000017029346,0.000039533898,0.000088160785,0.00023439048],"domain_scores_gemma":[0.9992908,0.00016892413,0.0001046377,0.000039109018,0.00017800696,0.00021849693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028821983,0.00027663197,0.00027580635,0.0011095585,0.008456135,0.0018454944,0.001297434,0.0012194279,0.004021443],"category_scores_gemma":[0.0016399933,0.00027532084,0.00014084119,0.0037705258,0.002194076,0.00045905134,0.0017690834,0.00086287863,0.00024989113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003855921,0.0004582722,0.492466,0.0005426569,0.00015145658,0.14175113,0.21132919,0.006645602,0.008650468,0.011275357,0.013182365,0.113161825],"study_design_scores_gemma":[0.000037508067,0.0001429761,0.51331306,0.00025575244,0.00009385002,0.006334759,0.43241295,0.003346916,0.0010036641,0.0011032196,0.04189348,0.00006184271],"about_ca_topic_score_codex":0.93949974,"about_ca_topic_score_gemma":0.98721284,"teacher_disagreement_score":0.060500264,"about_ca_system_score_codex":0.01321756,"about_ca_system_score_gemma":0.009939107,"threshold_uncertainty_score":0.1217131},"labels":[],"label_agreement":null},{"id":"W6992852728","doi":"","title":"Modeling Tsunamis for Improved Hazard Assessment and Detection","year":2016,"lang":"en","type":"article","venue":"Journal of Media Literacy Education","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Hazard; Context (archaeology); Hazard analysis; Warning system; Estuary; Submarine; Submarine pipeline; Numerical modeling; Tsunami wave","score_opus":0.015908878506442927,"score_gpt":0.2872361597387729,"score_spread":0.27132728123233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6992852728","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.040924095,0.00076409435,0.9467427,0.00047075565,0.00014422325,0.0000912927,0.00034034997,0.0012588898,0.009263538],"genre_scores_gemma":[0.6966236,0.0022103828,0.28879553,0.00016570665,0.00012534943,0.0001945557,0.000608473,0.00020040966,0.011075977],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984646,0.000045083798,0.000011448517,0.000026373193,0.00005488715,0.000015790412],"domain_scores_gemma":[0.9996469,0.00015930463,0.000039890285,0.00005821858,0.00007864933,0.000017057017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038028383,0.00073680474,0.0004475703,0.0004204784,0.00030073646,0.0010495941,0.00081690314,0.0006810014,0.0027859665],"category_scores_gemma":[0.0015504858,0.00030261718,0.0006429526,0.00042199044,0.00027005066,0.0010291846,0.0006509043,0.00066057115,0.0006041958],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020122945,0.00004581243,0.0019760258,0.000055331635,0.00003583275,0.00003088225,0.000053936954,0.9460538,0.002751096,0.008062085,0.00091038115,0.04000463],"study_design_scores_gemma":[0.0000029438177,0.000009628035,0.00018134814,0.0000062600348,0.000005571083,0.000007853079,0.000010250974,0.99560225,0.00055562303,0.0023320997,0.0012812545,0.000004871741],"about_ca_topic_score_codex":0.010142383,"about_ca_topic_score_gemma":0.010691825,"teacher_disagreement_score":0.010142383,"about_ca_system_score_codex":0.0005565963,"about_ca_system_score_gemma":0.0008487777,"threshold_uncertainty_score":0.020166695},"labels":[],"label_agreement":null},{"id":"W6994722044","doi":"","title":"Righetti, Alberta","year":2017,"lang":"sv","type":"other","venue":"Research Portal (King's College London)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"","score_opus":0.0479503235007479,"score_gpt":0.31757136548355885,"score_spread":0.26962104198281095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6994722044","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0028957522,0.0037095102,0.00067879516,0.00090145395,0.00049640506,0.000038878963,0.0068733557,0.00059387373,0.98381203],"genre_scores_gemma":[0.0049921502,0.0013045461,0.0007854158,0.00013748165,0.000026215293,0.000011120831,0.0021066018,0.00022977624,0.9904067],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996716,0.00001812146,0.000008851223,0.000087088345,0.00012980284,0.00008458298],"domain_scores_gemma":[0.99938965,0.000106348845,0.000024441484,0.000074380165,0.0002520223,0.00015325205],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00028861332,0.0011673722,0.0005694336,0.0018602022,0.0036576842,0.0040994696,0.001271218,0.00096810784,0.6390112],"category_scores_gemma":[0.0008453131,0.0004015568,0.00033532424,0.0027797073,0.0009331146,0.0008345629,0.0013920128,0.0014216616,0.26180768],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022527324,0.00008474641,0.0020004052,0.00051156315,0.000024318697,0.0006860934,0.00036289514,0.0011277344,0.0013202921,0.02706826,0.59373707,0.37285143],"study_design_scores_gemma":[0.000019251152,0.000010802617,0.0025325576,0.0001459032,0.000008922095,0.00012698009,0.00035501987,0.0002880875,0.00032638703,0.0027870983,0.9933884,0.000010517832],"about_ca_topic_score_codex":0.5429007,"about_ca_topic_score_gemma":0.81835383,"teacher_disagreement_score":0.5429007,"about_ca_system_score_codex":0.0051920344,"about_ca_system_score_gemma":0.011430472,"threshold_uncertainty_score":0.91958255},"labels":[],"label_agreement":null},{"id":"W6997423564","doi":"","title":"Wave Characteristics of Tsunamis Generated by Landslides of Varying Size and Mobility","year":2018,"lang":"en","type":"dissertation","venue":"QSpace (Queen's University Library)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Impulse (physics); Amplitude; Limiting; Long-term prediction","score_opus":0.007208999340420695,"score_gpt":0.1735332775210404,"score_spread":0.1663242781806197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6997423564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99828327,0.000019821588,0.001003961,0.000006177563,0.0000021315032,0.0000065594463,0.000098612785,0.00001743666,0.00056207326],"genre_scores_gemma":[0.99917287,0.000020168092,0.0004008262,0.0000035794544,0.0000011657118,0.000005414912,0.00010307384,0.0000025230909,0.00029032098],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999651,0.0000030165754,0.0000025087597,0.000008255329,0.000013093263,0.000008039638],"domain_scores_gemma":[0.9998186,0.000054589324,0.00003930917,0.000012191589,0.000043898657,0.00003138289],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009914951,0.0001126311,0.0001209977,0.00045868504,0.00011556253,0.00015497631,0.00012019331,0.00014445464,0.000792396],"category_scores_gemma":[0.00023176838,0.00007220606,0.00009759165,0.00022515879,0.00017688879,0.00016783748,0.000118193544,0.00019133314,0.000097305994],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012124298,0.000361127,0.10220273,0.00009794132,0.000073337316,0.0006060759,0.00051223463,0.029825518,0.82490224,0.0009329869,0.0006624496,0.038611002],"study_design_scores_gemma":[0.000051151867,0.0013643691,0.73106533,0.000018825725,0.000052350013,0.00052229664,0.0008842234,0.13149725,0.13314824,0.0005884089,0.00072952977,0.00007800814],"about_ca_topic_score_codex":0.0010621632,"about_ca_topic_score_gemma":0.0014505404,"teacher_disagreement_score":0.0010621632,"about_ca_system_score_codex":0.0001310233,"about_ca_system_score_gemma":0.00006349766,"threshold_uncertainty_score":0.0026507974},"labels":[],"label_agreement":null},{"id":"W6999967115","doi":"","title":"The distance analysis of a mine scale event","year":2022,"lang":"en","type":"dissertation","venue":"Lu Zone Ul (Laurentian University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Event (particle physics); Scale (ratio); Dispersion (optics); Magnitude (astronomy); Fault (geology); Spatial ecology","score_opus":0.0064073307102991955,"score_gpt":0.19370296790358912,"score_spread":0.18729563719328993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W6999967115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9357582,0.00023911624,0.041481275,0.00015236712,0.000061033836,0.00009730631,0.002084898,0.00027277143,0.01985311],"genre_scores_gemma":[0.9775802,0.00015082888,0.017305113,0.000014095225,0.000019419771,0.00002540826,0.0014052826,0.000024358873,0.0034752912],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99974006,0.000030436277,0.000025938538,0.00006006628,0.00011258626,0.000030795283],"domain_scores_gemma":[0.9993942,0.00016356884,0.00012806858,0.00004468062,0.0002223919,0.000047016492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019628875,0.00015760072,0.00018942368,0.0015828513,0.0002618703,0.00067696103,0.00024005849,0.00022000939,0.002240395],"category_scores_gemma":[0.0013631106,0.00006171819,0.0002304575,0.0012818621,0.0001447112,0.00028534676,0.00048249224,0.00024744135,0.0005491624],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008767448,0.00028493474,0.25767285,0.00040003663,0.00019304191,0.0015341926,0.0020567146,0.05872721,0.07878473,0.022097748,0.006194193,0.5711776],"study_design_scores_gemma":[0.000029734818,0.0004294815,0.64942616,0.00005018074,0.000076832446,0.0010305989,0.0022007935,0.30084708,0.021777658,0.004744076,0.019304687,0.00008257112],"about_ca_topic_score_codex":0.0047353106,"about_ca_topic_score_gemma":0.0059047313,"teacher_disagreement_score":0.0047353106,"about_ca_system_score_codex":0.00040005313,"about_ca_system_score_gemma":0.00032918816,"threshold_uncertainty_score":0.009415507},"labels":[],"label_agreement":null},{"id":"W7006093986","doi":"","title":"Stochastic Source Modelling and Tsunami Analysis of the 2012 Mw 7.8 Haida Gwaii Earthquake","year":2021,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tsunami earthquake; Hazard analysis; Hazard; Probabilistic logic; Stochastic modelling; Tsunami wave; Source model; Range (aeronautics)","score_opus":0.0661837335945827,"score_gpt":0.255109468034268,"score_spread":0.1889257344396853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7006093986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9730601,0.000061813356,0.020447077,0.00020015574,0.000013133539,0.000032090622,0.0005419754,0.00013766569,0.0055059637],"genre_scores_gemma":[0.9976246,0.000037525504,0.0015771011,0.0000067663673,0.0000047706058,0.00001309591,0.00023682383,0.0000134487145,0.00048582716],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998765,0.000037431084,0.000008392413,0.000018070634,0.000033074175,0.000026659438],"domain_scores_gemma":[0.9995969,0.00020121974,0.00008148603,0.000026174,0.00007029957,0.000023906045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034009537,0.00056109164,0.0003234115,0.00062448817,0.00036003086,0.00048727499,0.0007247456,0.0006015816,0.00074435765],"category_scores_gemma":[0.0011851185,0.00032633246,0.00058539736,0.00048280924,0.00038875223,0.00044693865,0.00041008196,0.00039771438,0.00010026937],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023533967,0.00001727929,0.0028476622,0.000008606779,0.000015632379,0.000053996984,0.000029754743,0.9930583,0.0005984471,0.0017380703,0.00016296508,0.0014457091],"study_design_scores_gemma":[0.0000047800445,0.000006935669,0.0016257555,0.0000012930383,0.000004319123,0.000007131149,0.000010592721,0.99766797,0.00018966815,0.0004235022,0.00005297022,0.0000051581737],"about_ca_topic_score_codex":0.09229576,"about_ca_topic_score_gemma":0.06417594,"teacher_disagreement_score":0.90770423,"about_ca_system_score_codex":0.0014642851,"about_ca_system_score_gemma":0.0010709408,"threshold_uncertainty_score":0.1835171},"labels":[],"label_agreement":null},{"id":"W7008883735","doi":"","title":"Detection and relocation of earthquakes in the sparsely instrumented Mackenzie Mountains region, Yukon and Northwest Territories, Canada","year":2020,"lang":"en","type":"article","venue":"Digital Collections of Colorado (Colorado State University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Relocation; Field (mathematics); Epicenter; Period (music)","score_opus":0.017976798223726897,"score_gpt":0.15780351593218525,"score_spread":0.13982671770845836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7008883735","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99512094,0.00022898965,0.00005180289,0.00007078779,0.0000038216167,0.000026059757,0.0027948176,0.000008873941,0.0016938321],"genre_scores_gemma":[0.9955244,0.00029337814,0.00020759767,0.000030245306,0.000002587456,0.000019868072,0.002192015,0.0000049988757,0.0017249758],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997298,0.000017903629,0.00002700162,0.00005744754,0.000075019234,0.00009280051],"domain_scores_gemma":[0.99860686,0.00009185411,0.0002599493,0.00005397384,0.00073883013,0.00024858603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002643616,0.0001996248,0.0002789523,0.0024234843,0.0019249117,0.0009950617,0.0009390871,0.0002912309,0.0012026632],"category_scores_gemma":[0.0016474418,0.00020941375,0.00020305839,0.0030564824,0.0005951838,0.00034882282,0.001201743,0.00028063232,0.00021692098],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058077054,0.000015461956,0.99022853,0.000039868864,0.000039621806,0.00013677993,0.0014353341,0.00018330532,0.0010308113,0.000102763006,0.0010105371,0.005718901],"study_design_scores_gemma":[0.000002154519,0.0000036017768,0.9977187,0.000011809321,0.000006932774,0.00003136435,0.0014598122,0.00009481182,0.000057021167,0.000005189428,0.0006047479,0.0000038142168],"about_ca_topic_score_codex":0.98675495,"about_ca_topic_score_gemma":0.99599874,"teacher_disagreement_score":0.013245046,"about_ca_system_score_codex":0.0065132827,"about_ca_system_score_gemma":0.011744778,"threshold_uncertainty_score":0.047257423},"labels":[],"label_agreement":null},{"id":"W7011484960","doi":"","title":"Miocene to recent stratigraphy, structural arcitecture and tectonic evolution of the florence rise, Eastern Mediterranean sea","year":2015,"lang":"tr","type":"dissertation","venue":"DSpace Repository","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mediterranean climate; Tectonics; Mediterranean sea; North sea","score_opus":0.015084547225358472,"score_gpt":0.23882949286555744,"score_spread":0.22374494564019898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7011484960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99418724,0.0010098177,0.00003236826,0.0003295724,0.000012767605,0.0000026420007,0.00032795392,0.000005198968,0.0040924773],"genre_scores_gemma":[0.9978436,0.00034765882,0.000047240992,0.000028938157,0.000012229815,0.0000021741216,0.00028003578,0.0000034869995,0.0014346148],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.0000075851435,0.0000044639773,0.000017241273,0.000008143167,0.000022584753],"domain_scores_gemma":[0.9998698,0.0000112401585,0.000048648584,0.000008395103,0.000025392901,0.000036544752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017996485,0.00010516068,0.00008412831,0.000692126,0.00041679534,0.00074456196,0.0002461,0.00020795148,0.0037373726],"category_scores_gemma":[0.00052690454,0.00009657618,0.00013362091,0.0006187258,0.00052755256,0.00030197736,0.00043494132,0.0001807461,0.0003767287],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014757438,0.000026290058,0.9623432,0.00004783241,0.00005675068,0.0004550187,0.0026114504,0.00037468478,0.0015015524,0.0008267329,0.0013787405,0.030230181],"study_design_scores_gemma":[8.558216e-7,0.00000485507,0.9984963,0.000005616993,0.0000022601741,0.00001818261,0.00026853266,0.000028211995,0.00001127167,0.000018398627,0.0011447263,7.570144e-7],"about_ca_topic_score_codex":0.25966427,"about_ca_topic_score_gemma":0.5457346,"teacher_disagreement_score":0.25966427,"about_ca_system_score_codex":0.0021059718,"about_ca_system_score_gemma":0.00076014595,"threshold_uncertainty_score":0.5163057},"labels":[],"label_agreement":null},{"id":"W7011488596","doi":"","title":"Mikroobikoosluse analüüsi võimalikkus Eesti jämesoolevähi sõeluuringus kasutatavatest peitvere testi proovidest","year":2024,"lang":"et","type":"dissertation","venue":"DSpace repository (University of Tartu)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Quarter (Canadian coin); Power (physics); Subject (documents); Character (mathematics)","score_opus":0.011560137497490592,"score_gpt":0.1946985911899671,"score_spread":0.1831384536924765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7011488596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.72550607,0.018696534,0.0930488,0.003401273,0.002496835,0.0016303161,0.011460621,0.003660291,0.14009936],"genre_scores_gemma":[0.56826353,0.010127938,0.15612763,0.0023670904,0.00030823387,0.0017783993,0.014796665,0.0020492808,0.2441812],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99308914,0.0008203618,0.0005749381,0.0014955379,0.003471668,0.00054846064],"domain_scores_gemma":[0.99529415,0.0014622879,0.00053861813,0.0004334856,0.0019426484,0.0003287543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033962217,0.0014873482,0.0014518595,0.0026435356,0.0018026077,0.0039765546,0.0010201008,0.001751738,0.028739326],"category_scores_gemma":[0.0048106587,0.0011346564,0.0016251743,0.0017060952,0.0013276202,0.0020096686,0.0023370197,0.0026921674,0.014058001],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011726526,0.0006220212,0.050686773,0.0020870708,0.0002504756,0.00074356544,0.0036011313,0.00050939695,0.8054127,0.0030916177,0.00652978,0.12529272],"study_design_scores_gemma":[0.000026601003,0.0016118307,0.08076308,0.0005664491,0.00034313617,0.0015211576,0.004206783,0.0013879756,0.7403933,0.0021449265,0.1668244,0.00021030496],"about_ca_topic_score_codex":0.003089301,"about_ca_topic_score_gemma":0.008324796,"teacher_disagreement_score":0.028739326,"about_ca_system_score_codex":0.0011052423,"about_ca_system_score_gemma":0.0014945925,"threshold_uncertainty_score":0.09614265},"labels":[],"label_agreement":null},{"id":"W7014753385","doi":"","title":"The postseismic response to the 2002 M 7.9 Denali Fault earthquake: constraints from InSAR 2003-2005","year":2009,"lang":"en","type":"article","venue":"Oxford University Research Archive (ORA) (University of Oxford)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Crust; Interferometric synthetic aperture radar; Viscoelasticity; Mantle (geology); Amplitude; Fault (geology); Satellite; Displacement (psychology); Vertical displacement","score_opus":0.022889589257223376,"score_gpt":0.23630338260478245,"score_spread":0.21341379334755908,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7014753385","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9708053,0.00039654446,0.0013272794,0.00034021636,0.000029607205,0.000022321956,0.01581831,0.00017371474,0.011086763],"genre_scores_gemma":[0.96582496,0.00026292598,0.0023626033,0.00012761683,0.000034089026,0.000017236704,0.02994298,0.00007435253,0.0013532194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99956125,0.00003354707,0.0000345862,0.00011807612,0.0001203323,0.00013222081],"domain_scores_gemma":[0.9989882,0.00007691356,0.00027690214,0.00014395473,0.00037617446,0.00013778094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005234677,0.0008414649,0.0005520765,0.0011583793,0.00079135085,0.0016104808,0.0008062411,0.0005420718,0.0020736232],"category_scores_gemma":[0.0014061836,0.0005234221,0.00037391574,0.0016726707,0.0002939039,0.00041217427,0.00049679424,0.00043851914,0.0010795185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007867716,0.00034533255,0.87028784,0.00026772055,0.00053872017,0.00088123395,0.00075889996,0.029596262,0.032410424,0.001679413,0.01539473,0.04705258],"study_design_scores_gemma":[0.000024818468,0.000026684289,0.97624594,0.00003104043,0.000078921075,0.00010152725,0.00025062036,0.011642249,0.0025363083,0.00014553749,0.008872401,0.000043897133],"about_ca_topic_score_codex":0.38179886,"about_ca_topic_score_gemma":0.6293713,"teacher_disagreement_score":0.38179886,"about_ca_system_score_codex":0.0019357456,"about_ca_system_score_gemma":0.0016806,"threshold_uncertainty_score":0.7591531},"labels":[],"label_agreement":null},{"id":"W7014996638","doi":"","title":"On the relationship between levels of seismicity and pump parameters in a hydraulic fracturing job","year":2013,"lang":"en","type":"article","venue":"University of Groningen research database (University of Groningen / Centre for Information Technology)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Shell (Canada)","funders":"","keywords":"Induced seismicity; Moment (physics); Hydraulic fracturing; Fractal dimension; Second moment of area; Seismic moment; Dimension (graph theory)","score_opus":0.06205269973562183,"score_gpt":0.24259408436349814,"score_spread":0.1805413846278763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7014996638","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923226,0.00030887575,0.003537666,0.00016472713,0.0000046792234,0.000010572625,0.0018626739,0.00007787402,0.0017102575],"genre_scores_gemma":[0.9976286,0.00006199072,0.0009370114,0.0000108100285,0.000008044946,0.000005484816,0.0011372773,0.000014699647,0.00019595904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993937,0.00013138284,0.00008089847,0.00022058959,0.00009788287,0.00007554689],"domain_scores_gemma":[0.9594284,0.03197646,0.006036462,0.0013029539,0.0007937761,0.0004619038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017105134,0.00028552857,0.00024663087,0.0024815402,0.00025865887,0.0010147353,0.00044127437,0.0008633701,0.0028973965],"category_scores_gemma":[0.014775005,0.00025074268,0.00034660235,0.0020807092,0.0008284892,0.0012440219,0.00053549075,0.0005901848,0.00068686594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019036233,0.000023581324,0.9627978,0.00005331255,0.0001417832,0.00022274106,0.00025715082,0.018421533,0.0034776155,0.0010714282,0.0005128617,0.012830013],"study_design_scores_gemma":[0.0000071602285,0.000053433363,0.9797768,0.000014644888,0.000036341702,0.00019049483,0.00018496966,0.01772484,0.0006804556,0.00089146313,0.00041410144,0.000025317277],"about_ca_topic_score_codex":0.0063297525,"about_ca_topic_score_gemma":0.007394172,"teacher_disagreement_score":0.0063297525,"about_ca_system_score_codex":0.00048741972,"about_ca_system_score_gemma":0.00023168024,"threshold_uncertainty_score":0.012585819},"labels":[],"label_agreement":null},{"id":"W7015661551","doi":"","title":"Uncovering Hidden Seismic Risks: Paleoseismic Insights in Québec's Intraplate Seismic Zones","year":2024,"lang":"en","type":"dissertation","venue":"Open MIND","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Seismic zone; Deformation (meteorology); Fault (geology); Seismotectonics","score_opus":0.03081290775211363,"score_gpt":0.27720716399494993,"score_spread":0.2463942562428363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7015661551","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.75756466,0.01012911,0.004951218,0.04009744,0.00022804085,0.000075844204,0.0060042706,0.00009069022,0.18085879],"genre_scores_gemma":[0.9693681,0.003349201,0.0017489414,0.00059276784,0.000042369717,0.000014478424,0.0007524223,0.000042075048,0.024089618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983037,0.000030552943,0.0000037747698,0.000025034567,0.000043648444,0.00006654102],"domain_scores_gemma":[0.99887997,0.00040647105,0.00009175419,0.00004357553,0.00044893235,0.00012926858],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005715643,0.00019657961,0.00017952557,0.0012163938,0.0025144517,0.0033099,0.00049237214,0.00063027284,0.009349939],"category_scores_gemma":[0.0035916227,0.00010976535,0.00016024314,0.0025304337,0.0012876512,0.0009680262,0.0006823871,0.0011413705,0.0003303624],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025210986,0.000094830975,0.35935342,0.0002964131,0.000110783345,0.00095200364,0.04841507,0.014772628,0.0021306137,0.11162369,0.105462,0.3565365],"study_design_scores_gemma":[0.000019858826,0.000025184672,0.7185046,0.0006948159,0.000052453135,0.00012586934,0.05004037,0.011243181,0.0005555459,0.02166635,0.19699621,0.000075587704],"about_ca_topic_score_codex":0.9870881,"about_ca_topic_score_gemma":0.9954756,"teacher_disagreement_score":0.020455703,"about_ca_system_score_codex":0.020455703,"about_ca_system_score_gemma":0.020192258,"threshold_uncertainty_score":0.14841723},"labels":[],"label_agreement":null},{"id":"W7026511989","doi":"","title":"Amherstburg, Ontario – Essex County, Ontario, Canada","year":2024,"lang":"en","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Work (physics); Agency (philosophy); Table (database)","score_opus":0.011523581679011172,"score_gpt":0.18309421859997232,"score_spread":0.17157063692096114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7026511989","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.018388499,0.006826162,0.0018022864,0.005650165,0.0010686965,0.00036719997,0.045505796,0.0005989966,0.91979223],"genre_scores_gemma":[0.012806405,0.0016335403,0.0010169386,0.00035008727,0.000027847353,0.0000509399,0.0034364962,0.00020012041,0.98047763],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994469,0.00002898388,0.000024117397,0.000101302125,0.000221852,0.00017683099],"domain_scores_gemma":[0.9983297,0.00011864844,0.0000663756,0.000054730033,0.0010749976,0.00035553923],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003399986,0.00081766705,0.00054585066,0.0012623486,0.0054333815,0.00282241,0.00094950834,0.0010170038,0.38498223],"category_scores_gemma":[0.0016540351,0.00048722044,0.0004105285,0.0027142833,0.0009105778,0.0007892253,0.0008768176,0.0010773692,0.07605157],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017294075,0.00005802908,0.008413995,0.00049784395,0.000031556032,0.00045658034,0.00063500745,0.00064047455,0.0010086771,0.010152104,0.8535005,0.12443232],"study_design_scores_gemma":[0.000034209155,0.00002012929,0.028362773,0.00026329,0.000014837963,0.0001005323,0.0008495978,0.00047925088,0.0003014938,0.00067710294,0.9688774,0.000019352205],"about_ca_topic_score_codex":0.96844256,"about_ca_topic_score_gemma":0.99489933,"teacher_disagreement_score":0.38498223,"about_ca_system_score_codex":0.020940155,"about_ca_system_score_gemma":0.039361827,"threshold_uncertainty_score":0.8772482},"labels":[],"label_agreement":null},{"id":"W7026539866","doi":"","title":"The Antibacterial Activity of Silicone-Polyether Surfactants","year":2017,"lang":"en","type":"dissertation","venue":"MacSphere (McMaster University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Concordia University","keywords":"Adhesion; Antibacterial activity; Silicone; Biofilm; Escherichia coli; Methacrylate; Contact angle; Bacteria","score_opus":0.016417640758832466,"score_gpt":0.2112574154330751,"score_spread":0.19483977467424263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7026539866","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9792443,0.010828525,0.002652967,0.000112345646,0.000059492282,0.000052695836,0.00016253084,0.00006743359,0.0068196575],"genre_scores_gemma":[0.97371835,0.008884383,0.00412656,0.000056160854,0.000018621648,0.000061550825,0.00025359093,0.000014162793,0.012866687],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999151,0.000008848112,0.000008585491,0.000014974633,0.000037815706,0.000014634877],"domain_scores_gemma":[0.9999212,0.000024267187,0.000021512908,0.000004020511,0.000019934649,0.00000908613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000101697304,0.0002704299,0.00011119854,0.00014278066,0.00008595146,0.00021645262,0.00008384886,0.00019804499,0.001546915],"category_scores_gemma":[0.00014493935,0.00010418174,0.00023904236,0.00010454757,0.00006973817,0.00012569058,0.00011482613,0.00024408942,0.0003206903],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022427965,0.000021748046,0.00012060819,0.00008432794,0.0000024936626,0.000021346284,0.000010032358,0.00010149498,0.9954976,0.000060993792,0.00002945925,0.004027482],"study_design_scores_gemma":[0.0000017173207,0.0003419821,0.0008781558,0.000012921823,0.0000063426055,0.00003245103,0.000006320204,0.00018256395,0.9970222,0.000011795271,0.0015018524,0.0000016960513],"about_ca_topic_score_codex":0.00022878354,"about_ca_topic_score_gemma":0.0005527544,"teacher_disagreement_score":0.001546915,"about_ca_system_score_codex":0.00013479519,"about_ca_system_score_gemma":0.00019063259,"threshold_uncertainty_score":0.005174935},"labels":[],"label_agreement":null},{"id":"W7033523512","doi":"","title":"The role of inositol polyphosphate 4-phosphatase type II alpha (Inpp4bα) in mature osteoclasts «in vivo»","year":2012,"lang":"en","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Inositol; Osteoclast; Bone resorption; Osteopetrosis; Alpha (finance); Gene expression; Cytoskeleton; Transgene","score_opus":0.002180391571854639,"score_gpt":0.13387795070728126,"score_spread":0.1316975591354266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7033523512","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9792179,0.012700355,0.0052891853,0.00031151244,0.0000900037,0.00004070076,0.00045890524,0.00011451097,0.0017769209],"genre_scores_gemma":[0.983282,0.0064273444,0.004401463,0.00013858775,0.00004478668,0.00006624253,0.00090428063,0.000020055304,0.004715139],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998336,0.000018664949,0.000014327463,0.0000389495,0.00005597384,0.000038474547],"domain_scores_gemma":[0.9998653,0.00001240179,0.000038620798,0.000009447552,0.00001750663,0.000056721918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027626535,0.00032469764,0.00022432822,0.00025766226,0.00025923064,0.0006050893,0.00030817348,0.00046592046,0.0005737446],"category_scores_gemma":[0.00014890874,0.00021282362,0.00021136114,0.00012270652,0.0003870676,0.00023192313,0.00030597168,0.00066953903,0.00023927564],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013390234,0.000020946947,0.0005436115,0.000027390824,0.000002165449,0.000075153825,0.000010766227,0.000017152382,0.9977748,0.0001527844,0.000039675106,0.0012017027],"study_design_scores_gemma":[0.000102617734,0.0006604331,0.030057358,0.000028428924,0.00006173872,0.0015564973,0.00011142141,0.0008117294,0.9551736,0.00031545036,0.0111075025,0.000013307962],"about_ca_topic_score_codex":0.0008263088,"about_ca_topic_score_gemma":0.00095008704,"teacher_disagreement_score":0.0008263088,"about_ca_system_score_codex":0.00041990803,"about_ca_system_score_gemma":0.0003679384,"threshold_uncertainty_score":0.0030466914},"labels":[],"label_agreement":null},{"id":"W7033896635","doi":"","title":"Review and synthesis of sustainable community indicators used in monitoring forest community sustainability / by Abdul Wahid Khan.","year":2017,"lang":"en","type":"other","venue":"Knowledge Commons (Lakehead University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sustainability; Sustainable forest management; Sustainable community; Community forestry; Poverty; Sustainable development; Social sustainability; Sustainable management","score_opus":0.02483571551350839,"score_gpt":0.2467641875912354,"score_spread":0.221928472077727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7033896635","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000314091,0.99064904,0.0004928577,0.003140918,0.001282086,0.000110951,0.00045289187,0.000011059895,0.003546138],"genre_scores_gemma":[0.0055920645,0.9876457,0.0012932204,0.0016384328,0.00034498394,0.00022790153,0.00060967077,0.000012468963,0.0026355153],"study_design_codex":"design_other","study_design_gemma":"systematic_review","domain_scores_codex":[0.9965777,0.0015066316,0.00064249296,0.00026575374,0.00089159387,0.00011583621],"domain_scores_gemma":[0.99480456,0.0024937359,0.0007481397,0.00017589518,0.001674897,0.000102762766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006284346,0.00070805283,0.000998148,0.006847574,0.00051316054,0.0019900524,0.000831905,0.00068800786,0.009071967],"category_scores_gemma":[0.010813367,0.00041149568,0.00077048806,0.010060131,0.0007082455,0.0027554177,0.001728588,0.0011487406,0.0021410119],"study_design_candidate":"systematic_review","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015968892,0.000048511152,0.00069999474,0.19588175,0.0004767835,0.00024465384,0.0019836493,0.00039417893,0.0010982472,0.011664014,0.1916131,0.59573543],"study_design_scores_gemma":[0.000024354424,0.000069220216,0.006017695,0.0839155,0.0004001186,0.00022695417,0.0012513219,0.000102776,0.00054949167,0.0016164071,0.9057989,0.0000273318],"about_ca_topic_score_codex":0.011980227,"about_ca_topic_score_gemma":0.02064711,"teacher_disagreement_score":0.011980227,"about_ca_system_score_codex":0.0028843773,"about_ca_system_score_gemma":0.010120045,"threshold_uncertainty_score":0.033235192},"labels":[],"label_agreement":null},{"id":"W7034066175","doi":"","title":"Some amazing photographers and amazing women","year":2021,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Photography; Subject (documents); Work (physics)","score_opus":0.006599774398088469,"score_gpt":0.1712352617388619,"score_spread":0.1646354873407734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7034066175","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0021631038,0.010339342,0.0008569167,0.03547275,0.011469121,0.000118350355,0.0014973582,0.0013597829,0.9367233],"genre_scores_gemma":[0.002535794,0.0018945638,0.0004431633,0.0026221173,0.0006306387,0.00002203159,0.0002344297,0.00022532138,0.991392],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991708,0.000097962155,0.000015459134,0.000077319564,0.0004463203,0.00019222817],"domain_scores_gemma":[0.99829644,0.000119862285,0.000045847606,0.00013346532,0.0008195847,0.0005848654],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009035824,0.00083571795,0.00032561054,0.0016300466,0.0064001875,0.0038475755,0.00070216006,0.0012136283,0.25506613],"category_scores_gemma":[0.002552138,0.000530831,0.00025218696,0.0018828103,0.0009850026,0.0034269418,0.0022589455,0.0018829976,0.123152785],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000051765487,0.000005318932,0.000117624484,0.000019188545,3.54008e-7,0.000047638718,0.00033483328,0.0000040631585,0.00009273255,0.00055992184,0.9760021,0.022811027],"study_design_scores_gemma":[8.4482485e-7,0.0000016102798,0.00030710772,0.000021043359,5.587196e-7,0.00005622855,0.0008504723,0.0000032312732,0.000030801682,0.000088464134,0.9986364,0.0000030950928],"about_ca_topic_score_codex":0.0859426,"about_ca_topic_score_gemma":0.3236137,"teacher_disagreement_score":0.74493384,"about_ca_system_score_codex":0.0022458772,"about_ca_system_score_gemma":0.001871612,"threshold_uncertainty_score":0.8532812},"labels":[],"label_agreement":null},{"id":"W7034141551","doi":"","title":"TES Ships 13.6MVA Hydro Generators for Tretheway Creek Project in Canada","year":2015,"lang":"en","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Hydropower; Hydroelectricity; Hydro power; Hydrology (agriculture); Work (physics)","score_opus":0.035584615100331195,"score_gpt":0.22406137789823985,"score_spread":0.18847676279790865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7034141551","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.048734013,0.00086422294,0.004784925,0.004238633,0.000430975,0.00046935488,0.081193425,0.0030210007,0.8562634],"genre_scores_gemma":[0.093339086,0.0006278713,0.0022538071,0.00031597225,0.00003383365,0.000054750508,0.022532474,0.0005816981,0.8802605],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99954623,0.000014696473,0.000009392995,0.000042901305,0.00022690138,0.00015988153],"domain_scores_gemma":[0.99896896,0.000023492608,0.000025356017,0.00003593524,0.0007454737,0.00020078059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031024765,0.0005292113,0.00026733495,0.0011693655,0.0029842374,0.0015778443,0.00086864666,0.0005651938,0.11433994],"category_scores_gemma":[0.0010733247,0.00032819575,0.00023830643,0.0016772242,0.00042346492,0.0005910911,0.0009939352,0.0006605894,0.0210342],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022081479,0.00009508318,0.020427037,0.00019085249,0.000025868172,0.00036129297,0.00049170805,0.0018002772,0.0016534912,0.008343304,0.84443027,0.12196008],"study_design_scores_gemma":[0.000090644586,0.00006506477,0.05653845,0.00012556739,0.000025003834,0.00014514916,0.0015697825,0.0036242453,0.001812324,0.0012627646,0.9347053,0.000035718305],"about_ca_topic_score_codex":0.9762706,"about_ca_topic_score_gemma":0.9921543,"teacher_disagreement_score":0.11433994,"about_ca_system_score_codex":0.011710976,"about_ca_system_score_gemma":0.04776001,"threshold_uncertainty_score":0.38250524},"labels":[],"label_agreement":null},{"id":"W7036584258","doi":"","title":"Climate Change as a Human Rights Issue-Inuit Environmental Activist Sheila Watt- Cloutier","year":2010,"lang":"en","type":"article","venue":"DigitalCommons (California Polytechnic State University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climate change; Human rights; Environmentalism; Government (linguistics); Political economy of climate change; Social movement","score_opus":0.012912779178521013,"score_gpt":0.20380868620336762,"score_spread":0.1908959070248466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7036584258","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.017378721,0.008837352,0.00022185656,0.8234122,0.0023529092,0.000032434804,0.00005512943,0.000033068714,0.14767629],"genre_scores_gemma":[0.34994093,0.012988693,0.0006909979,0.17833163,0.0013249231,0.00007086079,0.00006351969,0.00010183888,0.4564867],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991425,0.00021601983,0.000013927676,0.000077959536,0.00019001045,0.00035956502],"domain_scores_gemma":[0.99771994,0.0010709739,0.00008110476,0.000039033872,0.00032832116,0.00076066324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016581203,0.00028611225,0.00025850898,0.00037264675,0.019697618,0.005693117,0.00082039234,0.004919344,0.012098824],"category_scores_gemma":[0.0032422214,0.00021899017,0.00014883677,0.0005490876,0.0031496675,0.0028983846,0.0022707062,0.0065334346,0.00094604574],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032094427,0.0000754057,0.0019971912,0.00007391197,0.000007179206,0.00063623866,0.02171235,0.00011874867,0.0006612457,0.055857245,0.89127326,0.027555194],"study_design_scores_gemma":[0.000008284126,0.000020022355,0.0032933317,0.00018474182,0.0000073946635,0.00017638243,0.060274605,0.0002073842,0.00064424245,0.0049536508,0.9302063,0.000023675857],"about_ca_topic_score_codex":0.27012807,"about_ca_topic_score_gemma":0.6057539,"teacher_disagreement_score":0.7298719,"about_ca_system_score_codex":0.005159114,"about_ca_system_score_gemma":0.010672344,"threshold_uncertainty_score":0.5371115},"labels":[],"label_agreement":null},{"id":"W7037337193","doi":"","title":"Drilling in the Great Lakes: Background and Issues","year":2006,"lang":"en","type":"report","venue":"University of North Texas Digital Library (University of North Texas)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Drilling; Drilling rig; Production (economics); Fossil fuel; Natural (archaeology); Petroleum; Natural gas","score_opus":0.025065315204496716,"score_gpt":0.19164852147250117,"score_spread":0.16658320626800444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7037337193","genre_codex":"review","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.042768903,0.51001686,0.0023488372,0.37153468,0.004415288,0.00010811253,0.0045881444,0.000227175,0.06399203],"genre_scores_gemma":[0.19171812,0.72848916,0.005668311,0.03252263,0.016860303,0.00015845051,0.0037169422,0.00010586441,0.020760175],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99840456,0.0004226077,0.00023402311,0.00031490054,0.00043865741,0.0001852812],"domain_scores_gemma":[0.9938459,0.0024477227,0.0009639442,0.00016345852,0.001799012,0.0007798936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0029803426,0.00055536855,0.00037255386,0.002885833,0.0016898152,0.004431815,0.001568849,0.0029652172,0.0052602435],"category_scores_gemma":[0.00641464,0.00065374176,0.00021511057,0.00841821,0.002850728,0.003357869,0.0023232477,0.0024242406,0.00082401134],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017590102,0.00031179696,0.054297373,0.01336524,0.00007258839,0.0019563916,0.008158445,0.0042342087,0.0013432094,0.06705563,0.31997296,0.5290562],"study_design_scores_gemma":[0.000014541235,0.000102118,0.08587358,0.0059931516,0.000031731823,0.0007861945,0.008701074,0.0006192019,0.00045885684,0.009922738,0.88744354,0.000053246524],"about_ca_topic_score_codex":0.123941846,"about_ca_topic_score_gemma":0.15111399,"teacher_disagreement_score":0.87605816,"about_ca_system_score_codex":0.0041225315,"about_ca_system_score_gemma":0.010310304,"threshold_uncertainty_score":0.24644083},"labels":[],"label_agreement":null},{"id":"W7038593287","doi":"","title":"The impact of person-organization fit and perceptions of justice on employee organizational commitment, job satisfaction, and trust towards management after an acquisition","year":2001,"lang":"en","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Organizational justice; Perception; Economic Justice; Procedural justice; Interactional justice; Human resource management","score_opus":0.004952105145421347,"score_gpt":0.17137540084407193,"score_spread":0.16642329569865058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7038593287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99883693,0.00003392526,0.000011583034,0.00018605746,0.0000052724895,0.0000066729126,0.00006390823,0.0000012322606,0.0008545076],"genre_scores_gemma":[0.99881375,0.000053881333,0.000040013034,0.00007435879,0.000004236248,0.00001109688,0.00010660693,0.0000018795583,0.00089424656],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990742,0.0002423409,0.00005579957,0.00005333138,0.00024964384,0.00032459613],"domain_scores_gemma":[0.98709285,0.0031450407,0.0028738803,0.0003787106,0.0016112356,0.0048982813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015291462,0.00024604978,0.00028994848,0.00052784407,0.002360945,0.0015350824,0.0006734735,0.00082199264,0.003920246],"category_scores_gemma":[0.009033135,0.00025873608,0.00044233573,0.0007134448,0.00085479795,0.0005844805,0.001084073,0.0020194943,0.00047015972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003169077,0.0015679192,0.9879116,0.000011036803,0.00006286953,0.00010406677,0.0024211947,0.0001256927,0.00016921597,0.000103925144,0.00071177527,0.006493727],"study_design_scores_gemma":[0.0000074464597,0.00008596309,0.9972,0.0000070542687,0.000014594984,0.000013488722,0.0023751487,0.00010468978,0.000035652993,0.000026974601,0.00012469529,0.0000043098444],"about_ca_topic_score_codex":0.22388782,"about_ca_topic_score_gemma":0.4904318,"teacher_disagreement_score":0.22388782,"about_ca_system_score_codex":0.0026217303,"about_ca_system_score_gemma":0.0063555255,"threshold_uncertainty_score":0.44516927},"labels":[],"label_agreement":null},{"id":"W7039237536","doi":"","title":"Let the sun shine in: Record solar power installation at Edmonton Convention Centre expected to reduce greenhouse gas emissions, electricity bill","year":2019,"lang":"en","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Electricity; Greenhouse gas; Convention; Solar energy; Power (physics); Solar power; Greenhouse","score_opus":0.014656531837945934,"score_gpt":0.2193792895982891,"score_spread":0.20472275776034315,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7039237536","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0014196354,0.0016314872,0.00031831593,0.022614772,0.008381877,0.00008074972,0.0099804215,0.00075779005,0.954815],"genre_scores_gemma":[0.001527542,0.00034498755,0.00010540255,0.0016366072,0.0002642741,0.000011100251,0.0010957618,0.00012544982,0.99488884],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997702,0.000011425155,0.000004254969,0.000019352981,0.00013272125,0.000062003346],"domain_scores_gemma":[0.99952054,0.00002881777,0.000019419245,0.000018894181,0.00020418156,0.00020812708],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0003351133,0.00052942295,0.0002229733,0.0007267382,0.0020546918,0.0027807648,0.00064783526,0.0020260767,0.33869922],"category_scores_gemma":[0.0014190503,0.00030647762,0.00034407538,0.00053527724,0.00043600093,0.0014777369,0.0011378435,0.0032831982,0.11132107],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000009537472,0.000009467303,0.00009244286,0.000017686105,7.074199e-7,0.0000114353215,0.000011075527,0.000019729863,0.00004282894,0.0010292939,0.99063396,0.008121895],"study_design_scores_gemma":[0.000005271986,0.0000049713212,0.0011287457,0.0000366689,0.0000010225106,0.000008672917,0.000044273085,0.000030826082,0.00006217824,0.0002638429,0.9984101,0.000003346754],"about_ca_topic_score_codex":0.15683384,"about_ca_topic_score_gemma":0.47501752,"teacher_disagreement_score":0.33869922,"about_ca_system_score_codex":0.0025532965,"about_ca_system_score_gemma":0.004662639,"threshold_uncertainty_score":0.9432653},"labels":[],"label_agreement":null},{"id":"W7039786134","doi":"","title":"Norton Phone Number 1.800.769.2805 Norton Technical support Norton Antivirus support phone number","year":2016,"lang":"en","type":"other","venue":"OSF Preprints (OSF Preprints)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Phone; Mobile phone; Service (business); Phone call","score_opus":0.014153906635892706,"score_gpt":0.25116290412135983,"score_spread":0.23700899748546714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7039786134","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005174055,0.0007807027,0.0017126079,0.0010576171,0.0008899789,0.00011657262,0.0026935192,0.004613811,0.9876178],"genre_scores_gemma":[0.00077635224,0.00048539578,0.00042192574,0.00017367803,0.000087471904,0.000025939287,0.0011835062,0.0006429091,0.99620277],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993024,0.000038849885,0.000030439582,0.00014786275,0.00042122495,0.00005921014],"domain_scores_gemma":[0.9977591,0.00018891804,0.00008527125,0.0001672644,0.0012493016,0.0005501697],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00048628062,0.0011907014,0.0010053609,0.0015020058,0.0013976309,0.005654759,0.0012670417,0.0013122795,0.8828356],"category_scores_gemma":[0.0021644146,0.000778751,0.00042120993,0.0016049196,0.00039729147,0.0030148076,0.001364412,0.0012085923,0.878918],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004516298,0.00004190075,0.00020933975,0.00012607496,0.0000030291494,0.00009352553,0.00006150834,0.00006877789,0.0013269057,0.002386052,0.94213605,0.05350155],"study_design_scores_gemma":[0.0000096152135,0.00001929497,0.00028749605,0.00007182275,0.000005577057,0.000106753316,0.00007266646,0.00015715054,0.00037983782,0.00024899316,0.99863166,0.000009170492],"about_ca_topic_score_codex":0.007596197,"about_ca_topic_score_gemma":0.015348397,"teacher_disagreement_score":0.11716437,"about_ca_system_score_codex":0.0012324366,"about_ca_system_score_gemma":0.0015307151,"threshold_uncertainty_score":0.1671207},"labels":[],"label_agreement":null},{"id":"W7040970842","doi":"","title":"Cleveland, Ohio","year":2009,"lang":"en","type":"other","venue":"OhioLink ETD Center (Ohio Library and Information Network)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Table (database); Period (music); Quarter (Canadian coin)","score_opus":0.009124836146795604,"score_gpt":0.18569693999436263,"score_spread":0.17657210384756702,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7040970842","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00070323294,0.0024655438,0.00055973773,0.0026816532,0.0028379846,0.000112005844,0.009019553,0.00069382286,0.9809264],"genre_scores_gemma":[0.0041007004,0.0026285597,0.0009539402,0.0007040038,0.00053147477,0.00014299063,0.0038091217,0.00049889076,0.9866303],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99885714,0.00013143884,0.0000674978,0.00046774783,0.00034210493,0.00013406062],"domain_scores_gemma":[0.9986731,0.00020898464,0.00009740893,0.00020078679,0.00040453856,0.00041520636],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0009914945,0.001758105,0.00096510974,0.001807203,0.0031033782,0.0052818875,0.0013913282,0.0025209072,0.86418307],"category_scores_gemma":[0.0024093322,0.0007187647,0.00074117596,0.0025245864,0.0007112578,0.0030295267,0.0020567372,0.001980567,0.57781726],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007952404,0.00009158094,0.00064849114,0.00012397628,0.000012766193,0.00021077954,0.00007708844,0.00005560071,0.0002370441,0.0049403957,0.9013173,0.09220549],"study_design_scores_gemma":[0.000026369591,0.000013736658,0.0007605887,0.00006935315,0.000004640539,0.000060240458,0.000058678947,0.000029492547,0.000050642095,0.00037000127,0.9985483,0.000007896058],"about_ca_topic_score_codex":0.010941981,"about_ca_topic_score_gemma":0.027973479,"teacher_disagreement_score":0.86418307,"about_ca_system_score_codex":0.0015772119,"about_ca_system_score_gemma":0.0024506662,"threshold_uncertainty_score":0.1937263},"labels":[],"label_agreement":null},{"id":"W7042680673","doi":"","title":"Probabilistic Multi-hazard Shaking-Tsunami Risk Assessment for the District of Tofino, British Columbia, Canada, Subjected to Megathrust Cascadia Subduction Events","year":2023,"lang":"en","type":"article","venue":"Trinity's Access to Research Output (TARA) (Trinity College Dublin)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Earthquake casualty estimation; Episodic tremor and slip; Probabilistic logic; Moment magnitude scale; Population; Urban seismic risk; Earthquake scenario; Seismic risk","score_opus":0.11085535374012404,"score_gpt":0.35755274402852466,"score_spread":0.24669739028840063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7042680673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850425,0.00020887998,0.009316766,0.00038360638,0.000011490678,0.00012817733,0.001531033,0.0001069446,0.003270586],"genre_scores_gemma":[0.9964935,0.00012621796,0.0011581379,0.000016614258,0.0000033206054,0.000024160534,0.00051971007,0.0000071050463,0.0016511454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996884,0.000050684685,0.000014141268,0.00005085216,0.000090865404,0.0001050743],"domain_scores_gemma":[0.9992773,0.00026783312,0.00010598376,0.000026978436,0.00022023599,0.000101599355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005611639,0.0008542813,0.0004837029,0.0010989294,0.00096861896,0.0015843402,0.0014428584,0.0008587742,0.0015834203],"category_scores_gemma":[0.0019806696,0.0005513587,0.0005557638,0.001129167,0.0006336301,0.00034976206,0.00082304294,0.0004931714,0.0001497844],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006745526,0.000046780984,0.034652967,0.000029431636,0.000055454224,0.00031747966,0.000053654563,0.9591818,0.00041773284,0.00068767427,0.0005397893,0.003949759],"study_design_scores_gemma":[0.000007526079,0.000020890307,0.014441681,0.000006626752,0.000023588618,0.00003202171,0.0001506399,0.9846964,0.00008879443,0.00029850093,0.00021828384,0.000015000246],"about_ca_topic_score_codex":0.8969005,"about_ca_topic_score_gemma":0.85153073,"teacher_disagreement_score":0.103099525,"about_ca_system_score_codex":0.008041114,"about_ca_system_score_gemma":0.008286687,"threshold_uncertainty_score":0.20741338},"labels":[],"label_agreement":null},{"id":"W7067176598","doi":"","title":"Leveraging food-based recommendations for women and children in Nairobi slums with animal source foods","year":2014,"lang":"en","type":"other","venue":"CGSPace A Repository of Agricultural Research Outputs (Consultative Group for International Agricultural Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; Economic and Social Research Council; Medical Research Council; Leverhulme Centre for Integrative Research on Agriculture and Health; London School of Hygiene and Tropical Medicine; Government of Canada; Consortium of International Agricultural Research Centers","keywords":"Population; Poverty; Work (physics); Public health","score_opus":0.04222006460997667,"score_gpt":0.30017981177599407,"score_spread":0.2579597471660174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7067176598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95876926,0.0034248945,0.00033073194,0.013043867,0.00012224613,0.00056509575,0.0016775641,0.0000608772,0.022005366],"genre_scores_gemma":[0.985444,0.0035157092,0.0034963083,0.0016533443,0.000026416057,0.0005073525,0.00056149403,0.000012840107,0.004782481],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993611,0.00022340252,0.000042258176,0.000045549277,0.00008957683,0.00023807693],"domain_scores_gemma":[0.9992224,0.00016785896,0.00017837234,0.000030089974,0.00008745911,0.0003138798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017007841,0.00024573706,0.0002510975,0.00058694405,0.0013570298,0.0008834612,0.0010554624,0.00066206144,0.0079863435],"category_scores_gemma":[0.0045902887,0.0002645928,0.000296338,0.0009611877,0.0004509986,0.00061933964,0.0020431613,0.0007293629,0.0006388768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000414429,0.0011246182,0.5421907,0.003021316,0.0001536578,0.0026476579,0.050970364,0.00034042393,0.0033993435,0.0013512805,0.031366024,0.36302024],"study_design_scores_gemma":[0.00017368814,0.0005569205,0.8306759,0.0036928623,0.00017679961,0.000527881,0.07961299,0.00051934813,0.000769968,0.0008422147,0.082385525,0.000065887056],"about_ca_topic_score_codex":0.12578623,"about_ca_topic_score_gemma":0.2865483,"teacher_disagreement_score":0.12578623,"about_ca_system_score_codex":0.0022155126,"about_ca_system_score_gemma":0.0073331883,"threshold_uncertainty_score":0.25010818},"labels":[],"label_agreement":null},{"id":"W7067556822","doi":"","title":"Miscarried Justice The Murder of Sandy Seale &amp; Conviction of Donald Marshall Jr. (NS)","year":2019,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Conviction; Economic Justice; Indigenous; Prison; Criminal justice; Commission","score_opus":0.009891340177581165,"score_gpt":0.1889829428133543,"score_spread":0.17909160263577312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7067556822","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.062137514,0.021821335,0.0003776738,0.21088292,0.008283329,0.00011336532,0.0012712687,0.00028709884,0.6948255],"genre_scores_gemma":[0.19980647,0.007202749,0.00022602528,0.051812563,0.00064242387,0.000050820996,0.00028093337,0.000112710346,0.73986524],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99902105,0.00013302473,0.000031097214,0.00011079729,0.00033376555,0.00037017412],"domain_scores_gemma":[0.9990095,0.00014214948,0.000075197466,0.000059043716,0.0003526302,0.00036153864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000761467,0.00042446604,0.00027513193,0.00055120967,0.018429704,0.0025993588,0.0009985617,0.0032536048,0.017368045],"category_scores_gemma":[0.0038815308,0.00039440693,0.00024289056,0.00044708693,0.0024788103,0.0012245884,0.0024730996,0.0051081427,0.0051949346],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018146935,0.000015624908,0.0020739327,0.000046252313,0.0000076110373,0.0028540804,0.016155295,0.000031107433,0.00019244764,0.0060830177,0.95809716,0.014425496],"study_design_scores_gemma":[0.000004034923,0.000017405991,0.0037834896,0.00018491928,0.000010530592,0.0011730964,0.020951584,0.000025847716,0.00028538366,0.00036374136,0.97317284,0.000027045015],"about_ca_topic_score_codex":0.68583965,"about_ca_topic_score_gemma":0.8809343,"teacher_disagreement_score":0.68583965,"about_ca_system_score_codex":0.008321813,"about_ca_system_score_gemma":0.008585627,"threshold_uncertainty_score":0.63202095},"labels":[],"label_agreement":null},{"id":"W7067570001","doi":"","title":"Mental Health Promotion: A Framework for Action and Education","year":2010,"lang":"en","type":"article","venue":"LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mental health; Action (physics); Health promotion; Equity (law); Face (sociological concept); Order (exchange)","score_opus":0.029685670556205877,"score_gpt":0.2746712613108873,"score_spread":0.24498559075468143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7067570001","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0028874862,0.019774513,0.059010793,0.74486905,0.0031998279,0.0012879046,0.000090411,0.0002262493,0.16865371],"genre_scores_gemma":[0.46829674,0.04205698,0.29102096,0.13826911,0.0044984226,0.013198662,0.00024872494,0.0002874102,0.042123012],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9345671,0.05105516,0.0017916514,0.0025321937,0.005776361,0.00427756],"domain_scores_gemma":[0.96329325,0.021474112,0.0018099828,0.0012409589,0.003603948,0.008577779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.07171241,0.002741011,0.002855468,0.006264972,0.017693607,0.032507643,0.0065304483,0.026129737,0.006474648],"category_scores_gemma":[0.023342125,0.0012133995,0.001793308,0.0027002438,0.08462865,0.019516917,0.019441424,0.02201481,0.0016311978],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001803564,0.00017488455,0.00045514785,0.00052673224,0.000020764044,0.00019078533,0.025914978,0.00046542485,0.000067600675,0.9389258,0.015013501,0.01822638],"study_design_scores_gemma":[0.000086436885,0.00015508094,0.00058921095,0.0035087573,0.000024237721,0.00021944378,0.03211151,0.00081012567,0.00010888543,0.7252975,0.23702356,0.00006524741],"about_ca_topic_score_codex":0.021638898,"about_ca_topic_score_gemma":0.014198238,"teacher_disagreement_score":0.07171241,"about_ca_system_score_codex":0.025426978,"about_ca_system_score_gemma":0.07672021,"threshold_uncertainty_score":0.379256},"labels":[],"label_agreement":null},{"id":"W7067575799","doi":"","title":"Literature and loss Bertrand William Sinclair's British Columbia","year":2000,"lang":"en","type":"other","venue":"OpenGrey (Institut de l'Information Scientifique et Technique)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"George (robot); Government (linguistics); Exposition (narrative); Gloom","score_opus":0.009006042230338204,"score_gpt":0.21757134918094634,"score_spread":0.20856530695060813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7067575799","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.002949094,0.13541435,0.00020367306,0.15373747,0.043053236,0.00004461598,0.0015870936,0.000101778816,0.6629087],"genre_scores_gemma":[0.016926708,0.052379385,0.00013650057,0.014835797,0.004061918,0.00002821177,0.00040481254,0.00009720673,0.9111295],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990012,0.00009897795,0.000056329874,0.00011252258,0.00052081497,0.00021020403],"domain_scores_gemma":[0.99719787,0.0004153786,0.00010188857,0.00019407598,0.0016643206,0.00042637903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010017386,0.000523724,0.00051197404,0.0058674826,0.007741198,0.0055379895,0.001184584,0.0018729897,0.059138272],"category_scores_gemma":[0.00612625,0.00033472056,0.0002169942,0.007854518,0.00262353,0.0022436343,0.002561537,0.0030821473,0.012738739],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008218212,0.000003897009,0.00012824747,0.00004863702,0.0000014442385,0.00006376872,0.00026917778,0.000012723033,0.000020517797,0.006243188,0.97449785,0.018702332],"study_design_scores_gemma":[8.5174594e-7,5.5847994e-7,0.0003140017,0.00011706617,0.0000011086826,0.000035289733,0.000176646,0.0000037818586,0.000011582446,0.00036105563,0.99897575,0.000002338178],"about_ca_topic_score_codex":0.63061124,"about_ca_topic_score_gemma":0.7885849,"teacher_disagreement_score":0.36938876,"about_ca_system_score_codex":0.016043149,"about_ca_system_score_gemma":0.015623409,"threshold_uncertainty_score":0.7431283},"labels":[],"label_agreement":null},{"id":"W7067663491","doi":"","title":"Meeting the challenge of climate change: A status report on initiatives in Ontario to reduce greenhouse gas emissions","year":2019,"lang":"en","type":"report","venue":"The Atrium (University of Guelph)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Greenhouse gas; Climate change; Work (physics); Control (management); Private sector; Global warming","score_opus":0.0656065718200002,"score_gpt":0.2609156157754135,"score_spread":0.19530904395541332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7067663491","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13799351,0.012274927,0.0014390015,0.06674105,0.001971773,0.0026114532,0.1622478,0.0006360857,0.6140844],"genre_scores_gemma":[0.2485364,0.030642722,0.0050371196,0.0033289343,0.0005196224,0.0011727669,0.10145073,0.0003136804,0.608998],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975937,0.000054111533,0.00006788136,0.00005165792,0.001770023,0.00046259977],"domain_scores_gemma":[0.99617046,0.000092719216,0.00017832377,0.000058856782,0.0026590228,0.0008405592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014649461,0.000525224,0.00023464423,0.0019183316,0.0043650214,0.0030250424,0.00070256833,0.0008694403,0.00812328],"category_scores_gemma":[0.0021112806,0.0003808667,0.00033239156,0.0039587882,0.00059009873,0.0007447774,0.0013272351,0.00079234724,0.0021730433],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013618085,0.00012303995,0.04609161,0.0011399533,0.000037051752,0.00061680796,0.006018761,0.00088053365,0.0017671853,0.0036812567,0.88071686,0.058790773],"study_design_scores_gemma":[0.000026583204,0.000044517386,0.17850977,0.00026008065,0.000027147871,0.00006546122,0.005750461,0.0002808157,0.0005469587,0.00020135152,0.8142557,0.000031143656],"about_ca_topic_score_codex":0.9916802,"about_ca_topic_score_gemma":0.996031,"teacher_disagreement_score":0.036179155,"about_ca_system_score_codex":0.036179155,"about_ca_system_score_gemma":0.18451144,"threshold_uncertainty_score":0.2624994},"labels":[],"label_agreement":null},{"id":"W7068390801","doi":"","title":"DCP_0998","year":2010,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cove; Byte; Shot (pellet); Table (database); Quarter (Canadian coin)","score_opus":0.006084084776938386,"score_gpt":0.17092571693444397,"score_spread":0.16484163215750558,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7068390801","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00019116155,0.000116845025,0.00036618285,0.00045825163,0.0010995364,0.00013248244,0.0687059,0.0028737541,0.9260559],"genre_scores_gemma":[0.00073054724,0.00017561548,0.0003355699,0.00019990896,0.00015017936,0.00007507325,0.0320524,0.0013246535,0.9649559],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997223,0.000015886037,0.00001584438,0.000046434325,0.00014855497,0.00005090755],"domain_scores_gemma":[0.9986994,0.000109903965,0.00003114477,0.00020568808,0.0007192672,0.00023444726],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00032180233,0.0009108945,0.00074298104,0.0026173075,0.001520129,0.0040343395,0.0015088064,0.0012131123,0.9505608],"category_scores_gemma":[0.0019753173,0.00064117316,0.00047740247,0.00434225,0.00044934495,0.001979273,0.0015482,0.0014617306,0.9162491],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000121964495,0.0000113213855,0.00003982468,0.00005860373,9.2687924e-7,0.000012438994,0.0000068235454,0.000020683108,0.00008411851,0.00040603607,0.9829811,0.016365906],"study_design_scores_gemma":[0.000012705317,0.000006064111,0.00059980084,0.000044169235,0.000001201933,0.000021328475,0.000019369969,0.000026459782,0.00013116687,0.00017171557,0.99896014,0.000005804937],"about_ca_topic_score_codex":0.021487249,"about_ca_topic_score_gemma":0.026197767,"teacher_disagreement_score":0.04943919,"about_ca_system_score_codex":0.0015996539,"about_ca_system_score_gemma":0.0019504386,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W7068488635","doi":"","title":"Contributors","year":2017,"lang":"en","type":"book-chapter","venue":"OpenEdition (OpenEdition)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Economic Justice; Racism; Sexual assault; Common law; Legal history","score_opus":0.023753302161044577,"score_gpt":0.2247522570012564,"score_spread":0.20099895484021182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7068488635","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0009126638,0.00788373,0.0007984596,0.016682198,0.025631992,0.00015298657,0.004118499,0.0006092554,0.9432101],"genre_scores_gemma":[0.0016666029,0.002127521,0.00025919426,0.0011858147,0.0012601942,0.000032186126,0.00103093,0.00016839542,0.9922691],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99869126,0.00011143329,0.00004341947,0.0001909575,0.00079650583,0.00016643478],"domain_scores_gemma":[0.9945102,0.00053696294,0.00011735503,0.00039988518,0.003424541,0.0010110209],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00088410586,0.0004942137,0.0005965803,0.0029867582,0.0032955331,0.0050326264,0.0014378341,0.0011922732,0.47196],"category_scores_gemma":[0.006443451,0.00028933847,0.00029522498,0.002990593,0.0007911047,0.003145387,0.002009687,0.001520945,0.24771322],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000045698002,0.000004386778,0.000056496403,0.000034526343,4.4447543e-7,0.000018819703,0.00013829595,0.000010981247,0.000029434546,0.004823241,0.9745242,0.020354563],"study_design_scores_gemma":[4.550767e-7,7.378794e-7,0.00007346369,0.000029722918,2.5686612e-7,0.000016153737,0.00009458572,0.0000037741272,0.000009599604,0.0003435825,0.9994266,9.850902e-7],"about_ca_topic_score_codex":0.016099777,"about_ca_topic_score_gemma":0.036070187,"teacher_disagreement_score":0.52804,"about_ca_system_score_codex":0.0046266844,"about_ca_system_score_gemma":0.0043997825,"threshold_uncertainty_score":0.753185},"labels":[],"label_agreement":null},{"id":"W7068645197","doi":"","title":"İstanbul: Metis","year":2014,"lang":"tr","type":"article","venue":"DergiPark (Istanbul University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"","score_opus":0.011828344182069689,"score_gpt":0.17255761022274047,"score_spread":0.16072926604067078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7068645197","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011204626,0.04793932,0.002846233,0.0046975524,0.0063028247,0.00012458705,0.1302967,0.009680593,0.7869075],"genre_scores_gemma":[0.058074843,0.018338673,0.006576512,0.00075689924,0.0011446683,0.00027805043,0.06828787,0.0050585927,0.8414839],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.999648,0.00004928918,0.000040106228,0.00009260885,0.00011155206,0.000058392074],"domain_scores_gemma":[0.999652,0.00003359539,0.00006105582,0.000054679007,0.0001339234,0.00006476348],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00042929422,0.0027526086,0.0012552638,0.0026296098,0.0012976576,0.0041319993,0.0009730263,0.0010312859,0.40156657],"category_scores_gemma":[0.000691495,0.0006186875,0.00027894432,0.0053777867,0.00050484913,0.0026642645,0.0016217876,0.0016780907,0.2574013],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039124218,0.00006832413,0.0015062145,0.000873073,0.00002827912,0.00037252496,0.0002188143,0.00063599576,0.0010168073,0.01060931,0.7194588,0.26482064],"study_design_scores_gemma":[0.00003696554,0.00002658547,0.003315846,0.00015855579,0.00001077613,0.0002264498,0.0002729733,0.00022594933,0.0005696296,0.0018732118,0.99326706,0.000015995283],"about_ca_topic_score_codex":0.008415762,"about_ca_topic_score_gemma":0.008079005,"teacher_disagreement_score":0.40156657,"about_ca_system_score_codex":0.0013566305,"about_ca_system_score_gemma":0.00182479,"threshold_uncertainty_score":0.85359263},"labels":[],"label_agreement":null},{"id":"W7068911221","doi":"","title":"Dynamic response","year":2015,"lang":"en","type":"book-chapter","venue":"CINECA IRIS Institutial Research Information System (University of Genoa)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Underwater; Hull; Serviceability (structure); Vibration; Slosh dynamics; Noise (video); Transient (computer programming); Underwater explosion; Response analysis; Submarine pipeline","score_opus":0.08407260376546664,"score_gpt":0.2708676756767199,"score_spread":0.18679507191125322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7068911221","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008322631,0.0034614026,0.08056993,0.0039407373,0.004710132,0.00044692174,0.008279159,0.010578627,0.87969047],"genre_scores_gemma":[0.10364689,0.0032370046,0.01793825,0.0030311705,0.0010344653,0.000598761,0.012692865,0.002364481,0.8554561],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99864525,0.00011030215,0.000058651014,0.00035441338,0.0006569658,0.00017431019],"domain_scores_gemma":[0.99891794,0.00011530667,0.000047431964,0.00020603623,0.00061356975,0.00009972481],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006545104,0.0015174854,0.000876046,0.0012658342,0.0012297994,0.003860247,0.001938647,0.0023303917,0.34973907],"category_scores_gemma":[0.0021698126,0.00050786743,0.00081291253,0.0011348985,0.00052281626,0.0025570698,0.0031902622,0.0012805229,0.20268176],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049940153,0.00015773524,0.0016552281,0.0007711751,0.000041034637,0.00042423492,0.00028292523,0.0066351444,0.022949051,0.026994465,0.4991895,0.4404002],"study_design_scores_gemma":[0.00003322238,0.00014501864,0.002271945,0.00019373056,0.000021280011,0.00043493294,0.00026952906,0.009086782,0.0076064486,0.007214551,0.97264785,0.00007474309],"about_ca_topic_score_codex":0.0024738112,"about_ca_topic_score_gemma":0.0021114654,"teacher_disagreement_score":0.34973907,"about_ca_system_score_codex":0.0015121383,"about_ca_system_score_gemma":0.0013820898,"threshold_uncertainty_score":0.9275183},"labels":[],"label_agreement":null},{"id":"W7069050974","doi":"","title":"","year":2021,"lang":"en","type":"other","venue":"Directory of Open access Books (OAPEN Foundation)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Reading (process); Key (lock); Constructed language; English language; Plain language","score_opus":0.09675828294860353,"score_gpt":0.36769414410816076,"score_spread":0.27093586115955726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7069050974","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.001114335,0.005111153,0.0021621622,0.0057608956,0.0006356972,0.000024834695,0.000112660084,0.000078718,0.9849996],"genre_scores_gemma":[0.040745817,0.0069213468,0.0026870333,0.0035374574,0.0005748747,0.000052937947,0.00018048946,0.00015036989,0.94514966],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99936074,0.00017320391,0.000033752858,0.00011588828,0.0002335709,0.000082797924],"domain_scores_gemma":[0.99963295,0.000125925,0.000028689876,0.00005118251,0.00009546443,0.00006579414],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00054178404,0.0004354803,0.00030057822,0.00062386645,0.0026289357,0.0065245265,0.0006681246,0.0012945017,0.056408115],"category_scores_gemma":[0.0012900494,0.00020077584,0.00022171468,0.0007943996,0.005125236,0.0041608866,0.002481395,0.0017111787,0.026925027],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010246516,0.000016004884,0.00030831355,0.00013551347,0.0000034377215,0.00014281333,0.006229124,0.00009650394,0.00042085495,0.67903036,0.21240449,0.10120243],"study_design_scores_gemma":[9.652815e-7,0.0000052743835,0.0002576223,0.00013591713,9.842486e-7,0.00007295088,0.0010166485,0.0000326736,0.0000965114,0.02604164,0.9723359,0.0000029494713],"about_ca_topic_score_codex":0.004840572,"about_ca_topic_score_gemma":0.008753234,"teacher_disagreement_score":0.9435919,"about_ca_system_score_codex":0.002060294,"about_ca_system_score_gemma":0.0023961083,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W7069102209","doi":"","title":"9781552387351.pdf","year":2013,"lang":"en","type":"other","venue":"OAPEN (The OAPEN Foundation)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Service (business); Work (physics); Settlement (finance); Community service","score_opus":0.015069908701165946,"score_gpt":0.21696690628234572,"score_spread":0.20189699758117977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7069102209","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00013462594,0.0004901557,0.00038207383,0.0001889005,0.0003427263,0.000025688225,0.0016034102,0.0008818361,0.9959506],"genre_scores_gemma":[0.0006080257,0.000734649,0.00031279624,0.00014385904,0.000101784026,0.000025318997,0.0016485674,0.00059879903,0.9958262],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99971384,0.000022321436,0.000015081576,0.00004854595,0.00016437957,0.000035829657],"domain_scores_gemma":[0.99927455,0.00016290201,0.000035422298,0.00010692569,0.00022970764,0.00019062348],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00031626047,0.00086703914,0.00057350454,0.0015804432,0.0010416217,0.007480634,0.0010825533,0.00122448,0.89488333],"category_scores_gemma":[0.0015286512,0.0005011387,0.0004889728,0.0031779623,0.0005182385,0.003081938,0.0025800266,0.0014394069,0.91194665],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018385133,0.00003160635,0.00012044675,0.00013861088,0.0000022503293,0.00003902882,0.000076366785,0.000053573098,0.00029128577,0.0030521015,0.8374863,0.15869008],"study_design_scores_gemma":[0.0000028907043,0.000005266084,0.00024994355,0.0000791203,8.744757e-7,0.000040665036,0.000049423623,0.000016441194,0.000054923483,0.00027245123,0.9992249,0.0000030436163],"about_ca_topic_score_codex":0.0029107623,"about_ca_topic_score_gemma":0.004425108,"teacher_disagreement_score":0.105116665,"about_ca_system_score_codex":0.0005922449,"about_ca_system_score_gemma":0.0008563424,"threshold_uncertainty_score":0.1499362},"labels":[],"label_agreement":null},{"id":"W7069204088","doi":"","title":"22716.pdf","year":2022,"lang":"en","type":"other","venue":"OAPEN (The OAPEN Foundation)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Statute; Politics; State (computer science); Work (physics); Distribution (mathematics)","score_opus":0.015485774545870088,"score_gpt":0.22092158680094834,"score_spread":0.20543581225507826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7069204088","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00024253369,0.00043130424,0.0009180169,0.0009454662,0.0010482593,0.00013731554,0.024503062,0.0047616824,0.96701235],"genre_scores_gemma":[0.001852759,0.0005886419,0.0007203867,0.0008781963,0.00034157836,0.00011529924,0.014518673,0.002153704,0.9788309],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99901557,0.00011530881,0.00007312425,0.00015771823,0.0004854113,0.00015282462],"domain_scores_gemma":[0.9976291,0.00034152696,0.00011312867,0.00048590905,0.0010182395,0.0004121376],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0010415397,0.0008798297,0.0009616797,0.0026712155,0.00122857,0.008839773,0.0019434559,0.0022682801,0.94598806],"category_scores_gemma":[0.0049644774,0.0006528274,0.00074966863,0.0027685617,0.0006269881,0.0037565841,0.003544864,0.0015555485,0.95541865],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003719097,0.000041281015,0.00019388596,0.00019049994,0.0000040362847,0.000046293564,0.00004281626,0.000060495713,0.00017427492,0.0041208803,0.8815912,0.113497205],"study_design_scores_gemma":[0.000011115883,0.00000914099,0.00034489465,0.00010821669,0.0000015030088,0.00004699923,0.00003599407,0.00003850545,0.00009864853,0.0008213788,0.99847573,0.000007865423],"about_ca_topic_score_codex":0.0034624985,"about_ca_topic_score_gemma":0.0031368465,"teacher_disagreement_score":0.05401194,"about_ca_system_score_codex":0.0013534088,"about_ca_system_score_gemma":0.0013925763,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W7070316281","doi":"","title":"Ontario Teachers Pension Plan Board Buys Shares of 50,217 Southern Co (SO)","year":2018,"lang":"en","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pension plan; Plan (archaeology); Pension; Government (linguistics); Financial plan","score_opus":0.025797474664506697,"score_gpt":0.2211214239285941,"score_spread":0.19532394926408742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7070316281","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.042261526,0.00071622216,0.00023879115,0.0037787512,0.0003294994,0.0002297628,0.02806942,0.00046966472,0.92390627],"genre_scores_gemma":[0.022928508,0.0002157797,0.00008442443,0.00022162942,0.000042029544,0.000024263089,0.0040470604,0.00005212346,0.9723841],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9992704,0.000016376373,0.000015075648,0.000053006803,0.00040606761,0.00023905246],"domain_scores_gemma":[0.99870133,0.0000567344,0.00006640696,0.00007127029,0.000616153,0.00048810887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036247,0.0004648981,0.00030415624,0.0014718868,0.0042176,0.0018131108,0.0004846649,0.0009910327,0.19298254],"category_scores_gemma":[0.0013941508,0.00041073284,0.00031425036,0.0015252169,0.0004538372,0.0005224389,0.0007480216,0.00076106103,0.050968587],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021136647,0.000081887665,0.013638558,0.000060093185,0.000013796948,0.0001856031,0.00038620786,0.00016858951,0.0007082146,0.0039232452,0.9460877,0.034534696],"study_design_scores_gemma":[0.000042020878,0.000027956405,0.028661445,0.000022569724,0.000008426206,0.000035404537,0.0004884084,0.00028660084,0.0004431975,0.00017450273,0.9698001,0.000009275555],"about_ca_topic_score_codex":0.8441041,"about_ca_topic_score_gemma":0.96392274,"teacher_disagreement_score":0.8441041,"about_ca_system_score_codex":0.009808589,"about_ca_system_score_gemma":0.023217916,"threshold_uncertainty_score":0.6455909},"labels":[],"label_agreement":null},{"id":"W7070549212","doi":"","title":"Overview of ductile seismic brace fuse systems in Canada","year":2011,"lang":"en","type":"other","venue":"PolyPublie (École Polytechnique de Montréal)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Brace; Fuse (electrical); Deformation (meteorology); Welding; Compression (physics)","score_opus":0.018258036543991347,"score_gpt":0.20448862930186656,"score_spread":0.1862305927578752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7070549212","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.124487855,0.06661304,0.009152744,0.0048690867,0.0005021811,0.0010921516,0.061833963,0.0023217453,0.72912717],"genre_scores_gemma":[0.36162093,0.12225127,0.020567829,0.00089639565,0.00013661319,0.0002068047,0.044174787,0.0004934967,0.44965187],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99912757,0.000026001331,0.0000397621,0.00006744315,0.0004829085,0.00025632893],"domain_scores_gemma":[0.9979736,0.00005029202,0.000072556286,0.000029214802,0.001618025,0.00025617165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051175884,0.0009506407,0.00035122776,0.008154822,0.002696362,0.002831439,0.000996922,0.00046398657,0.01901986],"category_scores_gemma":[0.0009145038,0.00042970566,0.0003739817,0.0128447,0.0004827867,0.0007790846,0.0008525329,0.00054628926,0.00270891],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024943252,0.00017088765,0.061942816,0.0019403048,0.000090010595,0.00072242075,0.0014334061,0.016566793,0.0048307986,0.028974082,0.16402146,0.7190576],"study_design_scores_gemma":[0.000015004064,0.00007192383,0.11391597,0.0004715218,0.000048259477,0.00025231089,0.0018873962,0.0021911068,0.001223867,0.0006640708,0.8791979,0.00006060245],"about_ca_topic_score_codex":0.9893797,"about_ca_topic_score_gemma":0.99490154,"teacher_disagreement_score":0.03896184,"about_ca_system_score_codex":0.03896184,"about_ca_system_score_gemma":0.07588045,"threshold_uncertainty_score":0.28268927},"labels":[],"label_agreement":null},{"id":"W7070604990","doi":"","title":"Petrology, geochemistry, and isotopic composition of magmatic&#13;\\nsulphide occurrences in the Montagnais Sill Complex, northern&#13;\\nQuébec, Canada","year":2021,"lang":"en","type":"dissertation","venue":"ORCA Online Research @Cardiff (Cardiff University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sill; Igneous rock; Gabbro; Pluton; Mafic; Magma; Metallogeny; Ultramafic rock","score_opus":0.031366309246699,"score_gpt":0.264178553762494,"score_spread":0.232812244515795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7070604990","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99237,0.00040957495,0.00009511398,0.00006105412,0.000001518881,0.000022571116,0.0020681194,0.000022313472,0.0049496414],"genre_scores_gemma":[0.99383897,0.00025542898,0.00025206842,0.000022509057,0.000001714352,0.00000911147,0.0010300233,0.0000081750595,0.0045820596],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998437,0.0000054945417,0.0000051015772,0.00003540751,0.00006260728,0.000047640242],"domain_scores_gemma":[0.99970335,0.000012319547,0.000052681407,0.000005943514,0.00016263423,0.00006306588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010896089,0.0002700393,0.00016503365,0.002530348,0.0016754653,0.00078920426,0.00066179485,0.00022545569,0.002650618],"category_scores_gemma":[0.00023037949,0.00016798238,0.00013732517,0.002231907,0.0005904535,0.00018190622,0.00033603614,0.00015075027,0.00033775088],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013033049,0.00004224115,0.9583995,0.000054562548,0.000050166247,0.00055957097,0.0024486003,0.00052343495,0.013678834,0.0002842724,0.0016891821,0.022139315],"study_design_scores_gemma":[0.000002187944,0.0000079938445,0.9960508,0.000008872834,0.000005723064,0.000067404,0.0008334546,0.0003639896,0.00055991823,0.0000085920265,0.0020852317,0.000005871592],"about_ca_topic_score_codex":0.99169546,"about_ca_topic_score_gemma":0.9978255,"teacher_disagreement_score":0.01506618,"about_ca_system_score_codex":0.01506618,"about_ca_system_score_gemma":0.0054174033,"threshold_uncertainty_score":0.10931325},"labels":[],"label_agreement":null},{"id":"W7070819701","doi":"","title":"Positioning in Olympic Winter sports: analysing national prioritisation of funding and success in eight nations","year":2018,"lang":"en","type":"article","venue":"ARBOR - Bern University of Applied Sciences Repository","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Distribution (mathematics); Proxy (statistics); Position (finance); Portfolio; Investment (military); Index (typography)","score_opus":0.01177030893304815,"score_gpt":0.2093125108610457,"score_spread":0.19754220192799754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7070819701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964288,0.00011874585,0.00018240744,0.00010638707,0.000005940498,0.000012034081,0.00031650372,0.000002474248,0.00282685],"genre_scores_gemma":[0.9988361,0.00008719631,0.00023231871,0.000013259022,0.000005653014,0.000028674387,0.00042689216,0.0000027786907,0.00036718024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99873954,0.00038919557,0.0001785303,0.0001594782,0.00026304644,0.0002702551],"domain_scores_gemma":[0.993012,0.0014414897,0.0037544505,0.00024000483,0.0005648046,0.0009872617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020232736,0.00024935778,0.00038403753,0.0034587623,0.0006142278,0.0017269761,0.00054894784,0.00030942087,0.0035771825],"category_scores_gemma":[0.009571317,0.00012583281,0.00036614144,0.0050298525,0.0011069683,0.0013667652,0.0018794297,0.00041546326,0.00030250003],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057229714,0.000025547548,0.9897203,0.000039545317,0.00006718217,0.000075045464,0.0027331125,0.00042745308,0.000091097405,0.0009973698,0.00032402624,0.005442059],"study_design_scores_gemma":[0.0000023153304,0.00003441714,0.9918611,0.000037587957,0.00001206373,0.000026505137,0.0068457494,0.00027862057,0.00003884624,0.00018545781,0.0006718138,0.000005432397],"about_ca_topic_score_codex":0.03238809,"about_ca_topic_score_gemma":0.036616787,"teacher_disagreement_score":0.03238809,"about_ca_system_score_codex":0.0012765543,"about_ca_system_score_gemma":0.0011699075,"threshold_uncertainty_score":0.06439912},"labels":[],"label_agreement":null},{"id":"W7070833654","doi":"","title":"recensione al volume di P. Losacco, Wop o mangiacake. Consumi e identita etnica","year":2004,"lang":"it","type":"article","venue":"Archivio istituzionale della ricerca (Alma Mater Studiorum Università di Bologna)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Volume (thermodynamics); Population; Context (archaeology)","score_opus":0.018038258569261008,"score_gpt":0.2162074931882169,"score_spread":0.1981692346189559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7070833654","genre_codex":"other","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.024791628,0.30562946,0.0033699123,0.0760858,0.06415074,0.00014761357,0.0036174404,0.00052476896,0.52168256],"genre_scores_gemma":[0.06109809,0.08044794,0.0015110918,0.0067619053,0.02307877,0.000056268545,0.0015047665,0.0004031402,0.82513803],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9996582,0.00002572108,0.000012722613,0.0000858514,0.00016287585,0.00005460441],"domain_scores_gemma":[0.99948186,0.000096013486,0.000042327494,0.000047181114,0.00021993264,0.00011268059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004230413,0.00085049844,0.00033893294,0.0031997703,0.0016597828,0.0037168376,0.00084059173,0.00081020046,0.05123197],"category_scores_gemma":[0.0009742322,0.00035620423,0.0002686393,0.0046806163,0.0017469232,0.0015624944,0.0013055177,0.0013160958,0.010203722],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013640779,0.00007913855,0.0048510125,0.0008261689,0.000023310331,0.000270459,0.0017841096,0.00022796476,0.003100167,0.017627692,0.68670666,0.28436682],"study_design_scores_gemma":[0.0000026715857,0.000010244409,0.004490779,0.00009520612,0.000005761717,0.000092690934,0.00028394876,0.000041519077,0.00023327736,0.0011441498,0.99359554,0.0000042989172],"about_ca_topic_score_codex":0.13617769,"about_ca_topic_score_gemma":0.3307919,"teacher_disagreement_score":0.13617769,"about_ca_system_score_codex":0.004878553,"about_ca_system_score_gemma":0.0042015617,"threshold_uncertainty_score":0.27077007},"labels":[],"label_agreement":null},{"id":"W7070929302","doi":"","title":"Questionnaire sur les innovations en milieu de travail dans le secteur manufacturier au Québec","year":2008,"lang":"fr","type":"other","venue":"Érudit documents and data repository (Érudit Consortium, University of Montreal)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nucleofection; Gestational period; TSG101; Hyporeflexia; Fusible alloy; Diafiltration; Demotion","score_opus":0.011168384206527625,"score_gpt":0.1876161691465298,"score_spread":0.17644778494000216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7070929302","genre_codex":"empirical","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98022103,0.00016141516,0.00091786485,0.0009875513,0.000027274473,0.00045668439,0.003624316,0.00005615868,0.01354775],"genre_scores_gemma":[0.9543082,0.0005712464,0.0028158333,0.00042374653,0.00001828806,0.0009924974,0.0027245414,0.000022114482,0.038123444],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988556,0.00032533452,0.00009141883,0.000110988745,0.00039051461,0.00022610393],"domain_scores_gemma":[0.9905296,0.0029168485,0.0010603737,0.00024782645,0.0040783663,0.0011670348],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026092576,0.00025651904,0.00024739205,0.0011057609,0.0014304699,0.0011627349,0.00052531186,0.0005375727,0.009542984],"category_scores_gemma":[0.007194905,0.00014929248,0.00015382237,0.0015894489,0.0008160803,0.0006148234,0.0007442367,0.0006632089,0.0009882197],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027488687,0.0007062733,0.70396453,0.0005905759,0.000057727,0.00060677686,0.13010126,0.0010939005,0.0049663656,0.0021607096,0.034811396,0.12066568],"study_design_scores_gemma":[0.00001684047,0.00013490794,0.9255815,0.000116167896,0.000013588339,0.000039244613,0.040007487,0.00052272086,0.00055753376,0.00008620853,0.032880172,0.000043563166],"about_ca_topic_score_codex":0.742071,"about_ca_topic_score_gemma":0.82082134,"teacher_disagreement_score":0.25792903,"about_ca_system_score_codex":0.009343024,"about_ca_system_score_gemma":0.010065227,"threshold_uncertainty_score":0.518896},"labels":[],"label_agreement":null},{"id":"W7070988674","doi":"","title":"Psychosocial factors impacting rural oldest-old adults’ quality of life while aging in place","year":2022,"lang":"en","type":"other","venue":"Summit (Simon Fraser University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Psychosocial; Aging in place; Quality of life (healthcare); Rural area; Social support; Social isolation; Successful aging; Older people","score_opus":0.0211467549612149,"score_gpt":0.22585392499031307,"score_spread":0.20470717002909816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7070988674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856755,0.008218118,0.00007148408,0.0013732361,0.000028169059,0.000054719538,0.00034690578,0.000003746784,0.0042280117],"genre_scores_gemma":[0.99262637,0.00614724,0.00015462583,0.00033623597,0.000009131162,0.000022656859,0.00011007266,0.0000011959308,0.0005924854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994228,0.00014736824,0.000054888802,0.000050963205,0.0001753404,0.00014863629],"domain_scores_gemma":[0.99841917,0.00026578028,0.00039079803,0.000025605355,0.00052710745,0.00037155033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011420029,0.00014651816,0.0004353962,0.0009679842,0.0023911837,0.0021896814,0.0005117045,0.00032116054,0.0013830765],"category_scores_gemma":[0.0033660464,0.0001407554,0.00024823743,0.0016193805,0.0010072178,0.00061760726,0.001316324,0.0005332827,0.00009358245],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010271506,0.00016827164,0.80277354,0.002129671,0.00018972247,0.0010146976,0.10304837,0.00016024866,0.00058006565,0.00055392424,0.0038091952,0.085469685],"study_design_scores_gemma":[0.000006991759,0.00010439447,0.8899341,0.0009437378,0.00007685909,0.00022444486,0.10281727,0.00004619788,0.000044198427,0.00010472373,0.005673978,0.00002310686],"about_ca_topic_score_codex":0.71819556,"about_ca_topic_score_gemma":0.9179142,"teacher_disagreement_score":0.71819556,"about_ca_system_score_codex":0.0048689186,"about_ca_system_score_gemma":0.009577597,"threshold_uncertainty_score":0.566928},"labels":[],"label_agreement":null},{"id":"W7071058682","doi":"","title":"SolarEdge Technologies (NASDAQ:SEDG) Given “Sector Perform” Rating at Royal Bank of Canada","year":2024,"lang":"en","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Payment; Work (physics)","score_opus":0.01117312987281127,"score_gpt":0.1861515747580097,"score_spread":0.17497844488519843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071058682","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013820487,0.00021986147,0.0010661561,0.0035184412,0.0007911523,0.00019368171,0.013512167,0.0018914648,0.9774251],"genre_scores_gemma":[0.0034067216,0.000109795365,0.00038406666,0.000382789,0.00004351298,0.000018898048,0.0029040072,0.00033386573,0.9924164],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99838626,0.00003802718,0.00002649656,0.000081433536,0.0010850001,0.00038275242],"domain_scores_gemma":[0.99202913,0.00019517458,0.00008317202,0.00022852846,0.00604034,0.0014237085],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011848062,0.0007774634,0.00058583217,0.0015033653,0.0038117515,0.0048556915,0.0012970138,0.0019758644,0.4310931],"category_scores_gemma":[0.0035757022,0.00053826644,0.0005184302,0.0012899215,0.00078122946,0.0010730012,0.0011251973,0.0019383638,0.18740281],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029124483,0.000026095395,0.000367502,0.000030232039,0.0000018442206,0.000022969421,0.000020653179,0.0001463581,0.000224798,0.0028139802,0.97751004,0.018806424],"study_design_scores_gemma":[0.00001877865,0.000019238407,0.0017816212,0.000034131725,0.0000028359066,0.00001665193,0.00008576827,0.00047745314,0.0003698168,0.00056186813,0.9966209,0.000010929292],"about_ca_topic_score_codex":0.8216034,"about_ca_topic_score_gemma":0.92370015,"teacher_disagreement_score":0.8216034,"about_ca_system_score_codex":0.009968857,"about_ca_system_score_gemma":0.034965314,"threshold_uncertainty_score":0.81147665},"labels":[],"label_agreement":null},{"id":"W7071115995","doi":"","title":"The role of the male partner in infant feeding and reproduction choices and practices of women engaged in a PMTCT programme, Abidjan, Côte d'Ivoire","year":2006,"lang":"en","type":"other","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Reproduction; Infant feeding; Government (linguistics); Breastfeeding; Infant mortality; Transmission (telecommunications)","score_opus":0.012672873134554381,"score_gpt":0.22005755193251175,"score_spread":0.20738467879795738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071115995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963815,0.0017104887,0.000017396325,0.0004945976,0.00001234588,0.000005235897,0.00009559569,9.703002e-7,0.0012819101],"genre_scores_gemma":[0.99771273,0.0009987613,0.00004032461,0.000085848646,0.0000035730582,0.000007770352,0.00003429074,9.333741e-7,0.0011158107],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9991627,0.000486392,0.000025888623,0.000038682498,0.00007919644,0.00020720469],"domain_scores_gemma":[0.99933064,0.0002717602,0.00014070631,0.000019056191,0.0000684214,0.00016945736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008360676,0.00018534057,0.00028926428,0.00037771947,0.0017317375,0.0010222436,0.00045611648,0.00039736574,0.00259576],"category_scores_gemma":[0.0032311373,0.00025156714,0.0001044544,0.0010592141,0.0005762785,0.0003044719,0.00093624665,0.0004707551,0.00018589455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037766332,0.0003039167,0.81322026,0.00023221118,0.00006146814,0.0020018257,0.1283849,0.00010238532,0.0005979928,0.00047826814,0.0021692435,0.0520699],"study_design_scores_gemma":[0.000017712373,0.0001978763,0.87097025,0.00016656023,0.00002832916,0.00064944103,0.12492091,0.00007568136,0.00012629227,0.00007969499,0.0027540093,0.000013258516],"about_ca_topic_score_codex":0.20127392,"about_ca_topic_score_gemma":0.2894606,"teacher_disagreement_score":0.20127392,"about_ca_system_score_codex":0.0012678083,"about_ca_system_score_gemma":0.0018133586,"threshold_uncertainty_score":0.40020472},"labels":[],"label_agreement":null},{"id":"W7071120401","doi":"","title":"The Relationship between Calcium-phosphorus Metabolism Disorder and Cognitive Impairment in Maintenance Hemodialysis Patients","year":2022,"lang":"en","type":"article","venue":"DOAJ (DOAJ: Directory of Open Access Journals)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Logistic regression; Incidence (geometry); Diabetes mellitus; Correlation; Hemodialysis; Receiver operating characteristic; Montreal Cognitive Assessment; Cognitive impairment","score_opus":0.14461241242390685,"score_gpt":0.44181303106150766,"score_spread":0.29720061863760083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071120401","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900085,0.00044626268,0.00004857475,0.000036839574,0.000005161293,0.000005133984,0.00010074804,0.0000020342193,0.00035440287],"genre_scores_gemma":[0.99963355,0.00009953469,0.00004224761,0.00001267357,0.000012237938,0.0000042883357,0.00009060351,3.6914759e-7,0.000104430306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997855,0.000037810947,0.000035560974,0.000037528367,0.000060841627,0.000042858737],"domain_scores_gemma":[0.99936193,0.00011309876,0.00030552509,0.000021395943,0.0000757111,0.00012224553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035342175,0.00019916927,0.00025107042,0.00066318456,0.00034161407,0.0003915469,0.00015667835,0.00029205115,0.0012206441],"category_scores_gemma":[0.0013051559,0.00014289941,0.00026952542,0.00054587517,0.00014967077,0.00029732139,0.00024839677,0.00040024784,0.00010840665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007351091,0.000024457959,0.9989937,0.0000051784286,0.000016823164,0.000050705963,0.000018181714,0.000014700499,0.000056976005,0.0000046662185,0.00002749523,0.0007135139],"study_design_scores_gemma":[0.000005024588,0.000098849196,0.9992632,0.0000031488291,0.0000142948675,0.00026605904,0.00005609817,0.00016757568,0.000034777317,0.000016047385,0.000072915675,0.0000020524224],"about_ca_topic_score_codex":0.0025752357,"about_ca_topic_score_gemma":0.0033848449,"teacher_disagreement_score":0.0025752357,"about_ca_system_score_codex":0.00019882811,"about_ca_system_score_gemma":0.0002261295,"threshold_uncertainty_score":0.005120456},"labels":[],"label_agreement":null},{"id":"W7071132368","doi":"","title":"Rescue!: The Companies' Creditors Arrangement Act, 2nd ed.","year":2013,"lang":"en","type":"article","venue":"eYLS (Yale Law School)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Insolvency; Creditor; Restructuring; Bankruptcy; Going concern; Resource (disambiguation); Capital (architecture)","score_opus":0.015093829006561907,"score_gpt":0.21797457503298456,"score_spread":0.20288074602642264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071132368","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.001282514,0.2262751,0.0012881386,0.053564116,0.011480949,0.00018720038,0.0044053933,0.0006589626,0.7008577],"genre_scores_gemma":[0.009710621,0.08651386,0.0015219039,0.015889697,0.0014395664,0.00019816506,0.0029703774,0.0002457505,0.88151014],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99812585,0.00012069721,0.00008179035,0.00009090464,0.0013523515,0.00022843228],"domain_scores_gemma":[0.99890935,0.00018421245,0.000088517016,0.000047863323,0.00066165905,0.000108541884],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090401166,0.0010349355,0.00050626276,0.0018844276,0.0035591712,0.006255996,0.0014052364,0.004972986,0.040413674],"category_scores_gemma":[0.0033696508,0.0007002252,0.00045338512,0.0029790946,0.0015189521,0.0034878186,0.001239051,0.003466336,0.023252657],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000024256308,0.000004722683,0.00008256572,0.000043836022,4.3913175e-7,0.000023518283,0.0001513573,0.00003855187,0.000035238216,0.0069319187,0.9768943,0.015791094],"study_design_scores_gemma":[0.0000013297139,0.00000242287,0.000547399,0.000164911,8.212907e-7,0.000027480504,0.00014799343,0.000029951381,0.000019954643,0.0007056316,0.9983473,0.0000046938385],"about_ca_topic_score_codex":0.46134466,"about_ca_topic_score_gemma":0.65009797,"teacher_disagreement_score":0.46134466,"about_ca_system_score_codex":0.011452931,"about_ca_system_score_gemma":0.02604269,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W7071286794","doi":"","title":"Siemens Confirms 270 MW Order For K2 Wind Project In Ontario","year":2014,"lang":"en","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Siemens; Order (exchange); Work (physics); Wind power","score_opus":0.02846286572337788,"score_gpt":0.23491760947729018,"score_spread":0.2064547437539123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071286794","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03704288,0.0004068006,0.0010497766,0.007092053,0.00051689823,0.00032434362,0.040937155,0.00084428774,0.9117857],"genre_scores_gemma":[0.045728877,0.00024624183,0.00059228746,0.00038491216,0.00004444927,0.000042467178,0.0074564703,0.00026239318,0.9452419],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990994,0.00003111508,0.00002525232,0.00008064452,0.00047618194,0.0002874549],"domain_scores_gemma":[0.997265,0.00009736542,0.00006781597,0.00013150845,0.002004023,0.0004343392],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005280421,0.00041189778,0.00028498625,0.0009077853,0.004130193,0.0020641084,0.00057925907,0.0011244515,0.16032867],"category_scores_gemma":[0.0021367893,0.00035032202,0.00023392384,0.0011327503,0.00053011376,0.0006735088,0.0009681572,0.0008106615,0.02714852],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030545442,0.00005824698,0.0209759,0.00015792831,0.000016653525,0.0006193131,0.0010094941,0.0005398632,0.0019108059,0.01352745,0.9236836,0.03719522],"study_design_scores_gemma":[0.000047537116,0.000027743894,0.0536257,0.00005878336,0.0000100561965,0.00008394037,0.0010235289,0.00052208663,0.0010333674,0.00082052185,0.9427282,0.00001839087],"about_ca_topic_score_codex":0.9531086,"about_ca_topic_score_gemma":0.9846164,"teacher_disagreement_score":0.16032867,"about_ca_system_score_codex":0.015202322,"about_ca_system_score_gemma":0.040427998,"threshold_uncertainty_score":0.5363529},"labels":[],"label_agreement":null},{"id":"W7071391669","doi":"","title":"Royals' Ventura killed in car crash in Dominican Republic","year":2017,"lang":"en","type":"other","venue":"Internet Archive (Internet Archive)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Crash; Job loss; Quarter (Canadian coin); Work (physics)","score_opus":0.01641032122061582,"score_gpt":0.23970504138953813,"score_spread":0.22329472016892232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071391669","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8801029,0.0062573,0.00011776491,0.009341113,0.0004914843,0.000058800048,0.009689541,0.00010887778,0.09383227],"genre_scores_gemma":[0.92666435,0.0055023124,0.00009801423,0.0012774849,0.00017560896,0.000026855976,0.0040503973,0.000056025638,0.06214897],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9998826,0.000015889536,0.0000058462756,0.000012516894,0.000025520168,0.000057595116],"domain_scores_gemma":[0.99983406,0.000013123999,0.00004001466,0.000007370903,0.000052350664,0.00005301566],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00014120438,0.00022928865,0.00014304732,0.0006799874,0.0019845418,0.0008524611,0.00031419194,0.00044057643,0.012501132],"category_scores_gemma":[0.0005561578,0.0001037214,0.00010105176,0.0008220267,0.0002517634,0.00031031598,0.0009024789,0.00055546773,0.0012814678],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000385443,0.00018805363,0.29688588,0.00081331923,0.00012252473,0.023612319,0.032419894,0.00037603284,0.0014972718,0.002259024,0.53024364,0.111196674],"study_design_scores_gemma":[0.000023286102,0.00006337871,0.7102373,0.0005368665,0.00003765539,0.0038825187,0.0828089,0.00019321093,0.0003033961,0.00019852225,0.20168696,0.00002806235],"about_ca_topic_score_codex":0.35851964,"about_ca_topic_score_gemma":0.62138146,"teacher_disagreement_score":0.9874989,"about_ca_system_score_codex":0.0014618239,"about_ca_system_score_gemma":0.0012277091,"threshold_uncertainty_score":0.71286565},"labels":[],"label_agreement":null},{"id":"W7071453377","doi":"","title":"Stereoscope Slide, Underwood &amp; Underwood, Ice Grove","year":2020,"lang":"en","type":"article","venue":"UND Scholarly Commons (University of North Dakota)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Front (military); White (mutation); Snow; Photography; Window (computing)","score_opus":0.04732271707928125,"score_gpt":0.21332754981925525,"score_spread":0.16600483273997402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071453377","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011661914,0.0007371368,0.027364746,0.0008501463,0.0010615535,0.0007294708,0.05152786,0.007644811,0.89842224],"genre_scores_gemma":[0.023132721,0.0011756702,0.052126836,0.0003163017,0.00018059259,0.00032646576,0.036573667,0.005267828,0.8808998],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997534,0.000010878522,0.000011897111,0.00006200124,0.00012309906,0.00003867515],"domain_scores_gemma":[0.99948657,0.000040734496,0.000016457157,0.000063478044,0.00027816117,0.00011453715],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0002801338,0.00087322743,0.00045555335,0.0025302568,0.0011163476,0.0011329255,0.00083995925,0.0004826951,0.4795848],"category_scores_gemma":[0.00055965944,0.0007452598,0.00039349135,0.0019684883,0.00038828645,0.0011965989,0.00094642804,0.0011654961,0.19019677],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010016999,0.00005192718,0.00093089306,0.00019742869,0.000005375991,0.00012864363,0.00014149451,0.00034290593,0.015642766,0.0018494746,0.87129205,0.10931699],"study_design_scores_gemma":[0.00003879011,0.000047753114,0.014897874,0.00015170367,0.00001280253,0.0005590436,0.00046949013,0.0010804655,0.007074853,0.0007900856,0.97484493,0.00003215454],"about_ca_topic_score_codex":0.03035109,"about_ca_topic_score_gemma":0.12432793,"teacher_disagreement_score":0.4795848,"about_ca_system_score_codex":0.00069931685,"about_ca_system_score_gemma":0.0023167492,"threshold_uncertainty_score":0.7423091},"labels":[],"label_agreement":null},{"id":"W7071475566","doi":"","title":"Strutture castrensi, ricerca sul campo, rilievi cartografici. La stagione del Neomedievalismo nell’Appennino faentino","year":2022,"lang":"en","type":"article","venue":"Archivio istituzionale della ricerca (Alma Mater Studiorum Università di Bologna)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Middle Ages; Excavation; Period (music); Quarter (Canadian coin); Prospection; Plan (archaeology)","score_opus":0.01426785240850442,"score_gpt":0.2055642236892881,"score_spread":0.19129637128078367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071475566","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.102615386,0.29092538,0.0015167651,0.05698112,0.0021991846,0.000045705645,0.0015115192,0.00027715255,0.5439278],"genre_scores_gemma":[0.86403203,0.04852516,0.0022115114,0.0011510651,0.0014309889,0.000040812265,0.00067106466,0.00011301991,0.08182429],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9998116,0.00006413578,0.0000054976204,0.000038724127,0.00004691226,0.000033107026],"domain_scores_gemma":[0.9998479,0.000058128473,0.000029901008,0.00002310974,0.000025483536,0.00001546756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036756907,0.00031274487,0.00010759696,0.0028062686,0.0011695421,0.0022396073,0.00023932583,0.0004479914,0.007865305],"category_scores_gemma":[0.00064310984,0.00015922617,0.00008195441,0.0026187957,0.0019354518,0.000793356,0.0006690402,0.0005638857,0.00068447884],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005856206,0.000036503625,0.01875249,0.0005643215,0.000015911599,0.000514701,0.027840478,0.00059057254,0.00053341326,0.45700967,0.1793338,0.31474957],"study_design_scores_gemma":[0.000002420365,0.0000055659243,0.033985514,0.00033733548,0.000002933822,0.00019833862,0.0023544806,0.000099718556,0.000060811806,0.0046746423,0.95827293,0.000005372017],"about_ca_topic_score_codex":0.09241079,"about_ca_topic_score_gemma":0.18222359,"teacher_disagreement_score":0.09241079,"about_ca_system_score_codex":0.0024144056,"about_ca_system_score_gemma":0.0011297512,"threshold_uncertainty_score":0.1837458},"labels":[],"label_agreement":null},{"id":"W7071502999","doi":"","title":"The Suicide Disease: Trigeminal Neuralgia","year":2022,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Trigeminal neuralgia; Trigeminal nerve; Biting; Sensation; Face (sociological concept); Phantom pain; Conversation","score_opus":0.007439180429860543,"score_gpt":0.18143248629727513,"score_spread":0.17399330586741457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071502999","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.006375817,0.058848582,0.0006055273,0.12974155,0.022330742,0.00006776092,0.0009281585,0.00038724887,0.7807146],"genre_scores_gemma":[0.12429475,0.08629737,0.0007213669,0.086315036,0.026986368,0.00007596918,0.0014220858,0.0002560234,0.67363095],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99974316,0.000046546134,0.000017850845,0.000027725875,0.00010045828,0.0000642031],"domain_scores_gemma":[0.9997129,0.000056591547,0.000034125933,0.000019201128,0.000073461684,0.00010374866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017264133,0.00040373165,0.00026375684,0.0006851289,0.001578292,0.0015110257,0.00032163487,0.00243064,0.08681659],"category_scores_gemma":[0.0017684291,0.00010358816,0.0002517651,0.00091150834,0.0006236028,0.0013591057,0.0013176509,0.0020181993,0.027252438],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026499318,0.000025393943,0.0014554679,0.00020452465,0.000004578145,0.005403348,0.00044399107,0.000024812649,0.00014168333,0.0034707172,0.9056966,0.08310236],"study_design_scores_gemma":[0.000013630761,0.000018368642,0.0035609955,0.00076283776,0.000006260366,0.020884486,0.0008579487,0.000030229832,0.00007483432,0.0026338142,0.97114646,0.000010155472],"about_ca_topic_score_codex":0.00760935,"about_ca_topic_score_gemma":0.011504211,"teacher_disagreement_score":0.08681659,"about_ca_system_score_codex":0.00078318827,"about_ca_system_score_gemma":0.0007708321,"threshold_uncertainty_score":0.29043037},"labels":[],"label_agreement":null},{"id":"W7071572254","doi":"","title":"From shiftless fruit tramps to a respected seasonal reservoir of people","year":2009,"lang":"en","type":"other","venue":"Bulletin of Miscellaneous Information (Royal Gardens Kew)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Event (particle physics); Work (physics); Selection (genetic algorithm); Life history","score_opus":0.008032421271075561,"score_gpt":0.18770471883463438,"score_spread":0.17967229756355882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071572254","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.11267803,0.011199547,0.0012159342,0.16882218,0.0062084445,0.00005356328,0.0011715883,0.00033337064,0.6983173],"genre_scores_gemma":[0.6318664,0.0062846243,0.0010288064,0.01523382,0.0007890356,0.000030434423,0.0005255842,0.0002187393,0.34402254],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993092,0.00011863715,0.000015815858,0.00007323933,0.00021193821,0.00027112634],"domain_scores_gemma":[0.9990188,0.000045805322,0.000057562924,0.000047432,0.00013846316,0.000691995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008116474,0.00016761056,0.00018619823,0.00046435688,0.008831171,0.0045302333,0.00076564896,0.0009594036,0.035263166],"category_scores_gemma":[0.0014150646,0.00015383998,0.00010277486,0.00092844944,0.0034464167,0.003698464,0.0054166634,0.0029309331,0.0026092923],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012392757,0.000053833504,0.005597209,0.00016754707,0.00001049742,0.0016298901,0.05471439,0.000076795455,0.0008572869,0.056613836,0.7596059,0.12054891],"study_design_scores_gemma":[0.0000035231008,0.000015352725,0.00813276,0.00010374011,0.000002202443,0.00031210444,0.05084236,0.000013000929,0.000092533075,0.0020589053,0.9384125,0.000011071037],"about_ca_topic_score_codex":0.24089518,"about_ca_topic_score_gemma":0.58765775,"teacher_disagreement_score":0.24089518,"about_ca_system_score_codex":0.006350405,"about_ca_system_score_gemma":0.00909419,"threshold_uncertainty_score":0.47898602},"labels":[],"label_agreement":null},{"id":"W7071622743","doi":"","title":"Social Interaction in a Multicultural Group: How People from Different Cultural and Linguistic Background Negotiate Communication and Establish Relations","year":2010,"lang":"en","type":"other","venue":"Research Output (Edinburgh Napier University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Negotiation; Politeness; Ethnography; Solidarity; Meaning (existential); Multiculturalism; Intercultural communication; Ethnic group; Cultural diversity; Focus (optics); Immigration","score_opus":0.06903877070770129,"score_gpt":0.29446382957298955,"score_spread":0.22542505886528827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071622743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9305475,0.004428152,0.0034815564,0.00616667,0.00022707264,0.00010395846,0.000022528138,0.000057673624,0.054965034],"genre_scores_gemma":[0.9940147,0.0011312674,0.0013324637,0.00085035624,0.000038535123,0.000046653433,0.000014964613,0.000027769336,0.0025434238],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.98590267,0.010863852,0.00024246225,0.0007400664,0.0011623242,0.0010886408],"domain_scores_gemma":[0.9942625,0.00289497,0.0006965177,0.00032624273,0.00067926187,0.001140428],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0085892,0.0007587398,0.00073580456,0.0042558922,0.025111105,0.016850546,0.0020472587,0.0030666587,0.0020440698],"category_scores_gemma":[0.009341722,0.0005901901,0.0006547877,0.0019551525,0.030194601,0.00880065,0.014163435,0.0026818272,0.00045853248],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000057595776,0.000008954651,0.0023281288,0.000027491116,0.000009474364,0.00028318088,0.9913727,0.000015807338,0.0002110457,0.0015190053,0.00021499363,0.004003479],"study_design_scores_gemma":[0.000004324574,0.000026695234,0.0030999887,0.00006966728,0.000014458135,0.00026425283,0.9838652,0.000060878683,0.00008105705,0.0023455808,0.010149715,0.000018222407],"about_ca_topic_score_codex":0.028013134,"about_ca_topic_score_gemma":0.03461018,"teacher_disagreement_score":0.028013134,"about_ca_system_score_codex":0.004086232,"about_ca_system_score_gemma":0.004488517,"threshold_uncertainty_score":0.055700183},"labels":[],"label_agreement":null},{"id":"W7071992688","doi":"","title":"Validité de construit dâun test dâévaluation de la stabilité lombo-pelvienne, le soulèvement actif de la jambe tendue (SAJT) version objective","year":2010,"lang":"fr","type":"other","venue":"Library and Archives Canada (Government of Canada)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Nucleofection; TSG101; Gestational period; Hyporeflexia; Liquation; Dysgeusia","score_opus":0.004368978635226044,"score_gpt":0.15789561479784495,"score_spread":0.1535266361626189,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7071992688","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7571172,0.01402823,0.07738441,0.004591576,0.0065281917,0.023115842,0.02717652,0.0017357784,0.08832225],"genre_scores_gemma":[0.8503687,0.002190999,0.06982995,0.0016051605,0.00051163713,0.041291587,0.007229749,0.0004170877,0.026555125],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.97339046,0.01103637,0.0041329814,0.0028013957,0.007924259,0.0007144986],"domain_scores_gemma":[0.9114675,0.052550245,0.011442588,0.005134642,0.01837746,0.0010275696],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.027873222,0.0010228626,0.0013196327,0.0013986003,0.0009227849,0.0020949736,0.0011258894,0.0012945813,0.023771988],"category_scores_gemma":[0.09531887,0.00052451313,0.003161242,0.0010852029,0.0011899389,0.0012955564,0.0015761536,0.001619948,0.0034187427],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.014144944,0.0021978193,0.43818855,0.012635057,0.004840017,0.00043082068,0.0061707417,0.002217536,0.011292974,0.008059036,0.05489285,0.4449297],"study_design_scores_gemma":[0.002136193,0.009389269,0.8304597,0.0055433656,0.0021339238,0.0009650258,0.0023486686,0.007178808,0.015058146,0.005628336,0.11883938,0.0003191485],"about_ca_topic_score_codex":0.0023067684,"about_ca_topic_score_gemma":0.0049241297,"teacher_disagreement_score":0.027873222,"about_ca_system_score_codex":0.0016219645,"about_ca_system_score_gemma":0.003009704,"threshold_uncertainty_score":0.14740944},"labels":[],"label_agreement":null},{"id":"W7072235497","doi":"","title":"Ventajas e inconvenientes de los BIA","year":2012,"lang":"es","type":"other","venue":"RUA, Repositorio Institucional de la Universidad de Alicante (Universidad de Alicante)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Work (physics); Public health; MEDLINE; Politics","score_opus":0.008691821664035579,"score_gpt":0.23635028124682292,"score_spread":0.22765845958278735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072235497","genre_codex":"empirical","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6396703,0.017420854,0.004570168,0.023690065,0.0016594607,0.00015058214,0.0056210915,0.0005709001,0.30664656],"genre_scores_gemma":[0.8870887,0.0112305675,0.002242631,0.000697205,0.000275111,0.000039852952,0.0010238091,0.00014847949,0.09725356],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99939895,0.00009742936,0.00003335215,0.000058076006,0.0002419446,0.00017022084],"domain_scores_gemma":[0.99853456,0.00016383982,0.00039142623,0.000083164305,0.0005005132,0.000326558],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005149389,0.0005923598,0.00025323048,0.0011057663,0.004029876,0.0028096358,0.0005533801,0.000912392,0.01494453],"category_scores_gemma":[0.0034671647,0.00019681855,0.00018616932,0.001803308,0.0020425792,0.0009388081,0.0014267953,0.0017197661,0.0019553541],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075356575,0.00014721949,0.26772845,0.0016572574,0.0001158515,0.022215812,0.13263205,0.0013351113,0.01060848,0.026225783,0.20372991,0.33285052],"study_design_scores_gemma":[0.000024029974,0.00010762319,0.4011007,0.0009702795,0.000114243325,0.009734101,0.16683972,0.0006154645,0.0023288385,0.0033502334,0.41466224,0.00015250532],"about_ca_topic_score_codex":0.3743558,"about_ca_topic_score_gemma":0.67982805,"teacher_disagreement_score":0.3743558,"about_ca_system_score_codex":0.004434767,"about_ca_system_score_gemma":0.0038457192,"threshold_uncertainty_score":0.7443536},"labels":[],"label_agreement":null},{"id":"W7072284030","doi":"","title":"We need quality growth","year":2013,"lang":"en","type":"other","venue":"Universiti Utara Malaysia Institutional Repository (Universiti Utara Malaysia)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Surprise; Quality (philosophy); Product (mathematics); Quarter (Canadian coin); Beat (acoustics)","score_opus":0.015541519459176239,"score_gpt":0.19991679732285883,"score_spread":0.1843752778636826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072284030","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010303813,0.0053741336,0.0014312275,0.923063,0.012403329,0.0000482468,0.0014493129,0.000759996,0.054440364],"genre_scores_gemma":[0.078205295,0.028082319,0.01081481,0.66586775,0.021439174,0.00027653194,0.0051577087,0.0020698805,0.18808657],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.98867744,0.0022841957,0.00054408686,0.0010026634,0.0043439553,0.0031476498],"domain_scores_gemma":[0.9281272,0.007050046,0.0035896578,0.005065877,0.024563966,0.031603288],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.012151891,0.0011576137,0.0011823328,0.0024577815,0.0051524956,0.022417383,0.0024509227,0.009310522,0.143145],"category_scores_gemma":[0.05089402,0.00054363755,0.0013921546,0.0043065404,0.00556988,0.027227065,0.012137601,0.014944896,0.06229557],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034761106,0.00005874561,0.0010973864,0.00018079311,0.000015397338,0.000043399155,0.00023174103,0.00007869424,0.00008838479,0.028870894,0.9181753,0.051124483],"study_design_scores_gemma":[0.000043955148,0.000045686164,0.0026853094,0.00068106374,0.000012546968,0.00006861511,0.0013760122,0.000121640405,0.00013336737,0.025069749,0.9697272,0.000034955414],"about_ca_topic_score_codex":0.026819784,"about_ca_topic_score_gemma":0.025158158,"teacher_disagreement_score":0.143145,"about_ca_system_score_codex":0.008975824,"about_ca_system_score_gemma":0.02676763,"threshold_uncertainty_score":0.4788677},"labels":[],"label_agreement":null},{"id":"W7072286155","doi":"","title":"Vieillir à domicile : disparités territoriales, enjeux et perspectives","year":2023,"lang":"fr","type":"report","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Medical Association; World Health Organization","keywords":"Context (archaeology); Nursing homes; Social assistance; Disabled people","score_opus":0.055571101215405046,"score_gpt":0.2680154869117195,"score_spread":0.21244438569631446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072286155","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6436882,0.014268294,0.0031903184,0.043001648,0.0002657074,0.00002163139,0.00012674383,0.000027308832,0.29541016],"genre_scores_gemma":[0.98636705,0.002564021,0.00031006068,0.00082874554,0.000038579263,0.000018018423,0.000021625656,0.000014527782,0.009837318],"study_design_codex":"qualitative","study_design_gemma":"observational","domain_scores_codex":[0.9967024,0.0021810343,0.00005953965,0.0003084995,0.00027479941,0.000473704],"domain_scores_gemma":[0.9975616,0.0012510605,0.00026578305,0.00016338605,0.00032535646,0.00043284448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0032987124,0.00020980707,0.0003610997,0.0011991583,0.00892352,0.008540764,0.0006246679,0.0013490211,0.0049337978],"category_scores_gemma":[0.0036496955,0.00020165686,0.00019196431,0.0017607177,0.01627356,0.004583755,0.005414218,0.0021850658,0.00045654105],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026555335,0.000017504897,0.011363757,0.00009824984,0.000012045462,0.00042212743,0.64344174,0.00010303027,0.00027379708,0.31671113,0.0034476507,0.024082394],"study_design_scores_gemma":[0.000004479591,0.000030913983,0.01893171,0.0004991813,0.000009551186,0.00033242704,0.7855233,0.000117023184,0.00016399883,0.019520989,0.17483874,0.00002768523],"about_ca_topic_score_codex":0.061379645,"about_ca_topic_score_gemma":0.099561825,"teacher_disagreement_score":0.061379645,"about_ca_system_score_codex":0.0058343965,"about_ca_system_score_gemma":0.005094902,"threshold_uncertainty_score":0.12204474},"labels":[],"label_agreement":null},{"id":"W7072718164","doi":"","title":"فرسان الدواوين ولاية نينوى","year":2022,"lang":"ar","type":"other","venue":"Internet Archive (Internet Archive)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Brother; Islam; State (computer science); Supporter; Spanish Civil War; Hinduism","score_opus":0.016396784564606148,"score_gpt":0.22084639379582927,"score_spread":0.20444960923122313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7072718164","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.004077848,0.0023478179,0.005105276,0.008195334,0.008669126,0.00030079723,0.0014821157,0.0015017001,0.96831995],"genre_scores_gemma":[0.013098531,0.0030403007,0.004583545,0.0018108945,0.0012836169,0.0002870264,0.0013428612,0.0017084585,0.9728449],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985024,0.00018251827,0.00009455485,0.00016876204,0.0008356395,0.00021621768],"domain_scores_gemma":[0.9972645,0.000344132,0.00014349133,0.0002713318,0.0015767085,0.00039984687],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.001509632,0.00078583433,0.0004898478,0.0017816467,0.0032482601,0.008272247,0.00077388104,0.0012987698,0.58181065],"category_scores_gemma":[0.005806517,0.00058148033,0.000557958,0.0020681156,0.0020968665,0.0028479144,0.0026280857,0.003890053,0.54777646],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017067598,0.00006749429,0.00070593477,0.00061721174,0.000013848751,0.00057807594,0.0030099594,0.0001240785,0.00353747,0.045116782,0.7271496,0.21890883],"study_design_scores_gemma":[0.0000064122846,0.0000104139735,0.0005778701,0.00014602896,0.000003044367,0.00015493702,0.0011171646,0.00002497351,0.0005683825,0.0011172702,0.9962625,0.000010945135],"about_ca_topic_score_codex":0.004917874,"about_ca_topic_score_gemma":0.006909421,"teacher_disagreement_score":0.41818935,"about_ca_system_score_codex":0.0022758306,"about_ca_system_score_gemma":0.0034317737,"threshold_uncertainty_score":0.59649634},"labels":[],"label_agreement":null},{"id":"W7073553931","doi":"","title":"Antimicrobial Peptides Protect Coho Salmon from Vibrio anguillarum Infections","year":2000,"lang":"en","type":"article","venue":"PubMed Central","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Medical Research Council; Medical Research Council Canada","keywords":"Vibrio anguillarum; Antimicrobial; Antimicrobial peptides; Pathogen; Aquaculture; Fish <Actinopterygii>; Vibrio; Fish farming","score_opus":0.010648599213781012,"score_gpt":0.18220620904218437,"score_spread":0.17155760982840337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073553931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708503,0.001623866,0.00042389624,0.00006228254,0.000019852321,0.000020250112,0.0001309866,0.000019949,0.0006138648],"genre_scores_gemma":[0.9943679,0.0014439839,0.0019432778,0.0001282698,0.00002162205,0.000027758126,0.000369086,0.0000066260363,0.0016915579],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999542,0.0000071574764,0.00000511158,0.000007749372,0.000012518494,0.000013212635],"domain_scores_gemma":[0.99992156,0.00001068726,0.000022421345,0.0000040348937,0.000021335854,0.000019926958],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009944693,0.00023108016,0.00016732518,0.0000884111,0.000083612766,0.00016289661,0.0001004285,0.00022581259,0.0010317478],"category_scores_gemma":[0.000100511184,0.00005404128,0.0001481478,0.000045914323,0.00011030446,0.00010730023,0.000104032624,0.0001672365,0.00018397006],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012370301,0.000017780909,0.00040773614,0.0000406048,0.0000029273338,0.000018028806,0.0000030058095,0.000026460726,0.99813485,0.0000063516036,0.00001996311,0.0011984934],"study_design_scores_gemma":[0.000074617565,0.0044894232,0.035521764,0.00003037468,0.000040324045,0.00037610796,0.00008373005,0.0007674801,0.9560596,0.00003530184,0.0025099358,0.00001136557],"about_ca_topic_score_codex":0.00048714894,"about_ca_topic_score_gemma":0.00069048454,"teacher_disagreement_score":0.0010317478,"about_ca_system_score_codex":0.000121734316,"about_ca_system_score_gemma":0.00014602428,"threshold_uncertainty_score":0.0034515858},"labels":[],"label_agreement":null},{"id":"W7073616287","doi":"","title":"Search for a heavy charged Higgs boson decaying into a $W$ boson and a Higgs boson in final states with leptons and $b$-jets in $\\\\sqrt{s} = 13$ TeV $pp$ collisions with the ATLAS detector","year":2024,"lang":"en","type":"other","venue":"CERN Document Server (European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"H2020 Marie Skłodowska-Curie Actions; Institut National de Physique Nucléaire et de Physique des Particules; Agencia Estatal de Investigación; Agencia Nacional de Promoción Científica y Tecnológica; Ministero dell'Università e della Ricerca; Agencia Nacional de Investigación y Desarrollo; Narodowa Agencja Wymiany Akademickiej; Universidade do Minho; Universidad de Tarapacá; Université Paris-Saclay; Univerzita Palackého v Olomouci; Forskningsrådet om Hälsa, Arbetsliv och Välfärd; Universidad de Granada; Japan Society for the Promotion of Science; Universidade de Coimbra; H2020 European Research Council; Norges Forskningsråd; Universitetet i Oslo; Ministerio de Ciencia e Innovación; Knut och Alice Wallenbergs Stiftelse; Akademie Věd České Republiky; Bundesministerium für Wissenschaft, Forschung und Wirtschaft; Generalitat Valenciana; Generalitat de Catalunya; Austrian Science Fund; University of Pennsylvania; Grantová Agentura České Republiky; Natural Sciences and Engineering Research Council of Canada; University of Oregon; Ministry of Education, Culture, Sports, Science and Technology; Bundesministerium für Bildung und Forschung; National Science and Technology Council; Ministerstvo Školství, Mládeže a Tělovýchovy; Leverhulme Trust; European Commission; Fundação de Amparo à Pesquisa do Estado de São Paulo; Danmarks Grundforskningsfond; Instituto Superior Técnico; Deutsche Forschungsgemeinschaft; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Universidade de Lisboa; Ministry of Science and Technology of the People's Republic of China; Agence Nationale de la Recherche; Horizon 2020 Framework Programme; Vetenskapsrådet; Oklahoma State University; National Science Foundation; Sorbonne Université; Istituto Nazionale di Fisica Nucleare; UK Research and Innovation; Centres de Recerca de Catalunya; Univerzita Karlova v Praze; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Ministerstwo Edukacji i Nauki; CERN; Science and Technology Facilities Council; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Universidad Técnica Federico Santa María; Canarie; European Regional Development Fund; British Columbia Knowledge Development Fund; Centre National de la Recherche Scientifique; Max-Planck-Gesellschaft; European Social Fund; Centre National pour la Recherche Scientifique et Technique; Royal Society; University of Oxford; Alexander von Humboldt-Stiftung; University of Oklahoma; TRIUMF; Pontificia Universidad Católica de Chile; Baden-Württemberg Stiftung; Fundação para a Ciência e a Tecnologia; University of Washington; University of Pittsburgh; Türkiye Enerji, Nükleer ve Maden Araştırma Kurumu; Fundação Carlos Chagas Filho de Amparo à Pesquisa do Estado do Rio de Janeiro; U.S. Department of Energy; Carl Tryggers Stiftelse för Vetenskaplig Forskning; České Vysoké Učení Technické v Praze; Ohio State University; National Natural Science Foundation of China","keywords":"Higgs boson; Large Hadron Collider; Boson; Lepton; Branching fraction; Invariant mass; Top quark; ATLAS experiment","score_opus":0.02589081266251371,"score_gpt":0.2567159390115672,"score_spread":0.2308251263490535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073616287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99252456,0.00019506452,0.002106221,0.000029560106,0.0000056738677,0.000013954007,0.0015205555,0.00015245049,0.0034519592],"genre_scores_gemma":[0.98914975,0.00013181838,0.0034173632,0.00003716708,0.0000072940493,0.000010302584,0.004667346,0.00004529149,0.0025336684],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99978584,0.00003271692,0.00000834495,0.00005094143,0.00007221295,0.000049967188],"domain_scores_gemma":[0.9998704,0.00003336464,0.00003295732,0.000013443969,0.000018038896,0.000031710708],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004925346,0.00029600313,0.0003424421,0.0011319051,0.0004933505,0.0007405899,0.00039537385,0.0003497092,0.0022857743],"category_scores_gemma":[0.00024361208,0.00023471742,0.00026029834,0.0013884803,0.00015481295,0.00023722713,0.00049523066,0.00013136909,0.0007992564],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003466451,0.00036359119,0.6096465,0.00018465923,0.00040143027,0.0036332272,0.00042784715,0.0046341605,0.32729965,0.0031162053,0.0044605066,0.04236568],"study_design_scores_gemma":[0.00022244704,0.0010748003,0.73092484,0.00002085809,0.000310247,0.00317844,0.00077686826,0.016691765,0.23365764,0.0020009812,0.011043145,0.00009800723],"about_ca_topic_score_codex":0.0032392931,"about_ca_topic_score_gemma":0.009563595,"teacher_disagreement_score":0.0032392931,"about_ca_system_score_codex":0.0003247391,"about_ca_system_score_gemma":0.0003623843,"threshold_uncertainty_score":0.00764668},"labels":[],"label_agreement":null},{"id":"W7073624652","doi":"","title":"Expert recommendations on treatment sequencing and challenging clinical scenarios in human epidermal growth factor receptor 2-positive (HER2-positive) metastatic breast cancer.","year":2024,"lang":"en","type":"report","venue":"Digital Access to Libraries (Université catholique de Louvain (UCL), l'Université de Namur (UNamur) and the Université Saint-Louis (USL-B))","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Metastatic breast cancer; Breast cancer; Discontinuation; Disease; Systemic therapy; CLARITY; Targeted therapy; Cancer; Incidence (geometry)","score_opus":0.03164699067330246,"score_gpt":0.264393263438195,"score_spread":0.23274627276489257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073624652","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0021333925,0.084004425,0.030483114,0.8148543,0.025253396,0.0015698617,0.0010030532,0.0007242882,0.039974228],"genre_scores_gemma":[0.04573574,0.12839784,0.20500723,0.562349,0.023057502,0.0049153883,0.0042344234,0.00059148297,0.025711343],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.96780795,0.018394345,0.006187127,0.0010822299,0.0048692357,0.001659051],"domain_scores_gemma":[0.91898435,0.035652857,0.006046725,0.0017374589,0.03051446,0.007064148],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.037049823,0.001330045,0.0016972407,0.002506288,0.0024355703,0.0033075493,0.0055504697,0.019389434,0.008373153],"category_scores_gemma":[0.09617498,0.0007982879,0.0041476637,0.0017116129,0.0022616875,0.0054902663,0.0043565,0.01564265,0.006176053],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008548658,0.00010638489,0.0007953304,0.0034949412,0.00009054948,0.0011315356,0.0013346125,0.0012672421,0.0006240048,0.007246467,0.804805,0.17901844],"study_design_scores_gemma":[0.000112679714,0.00006793107,0.00080289115,0.012000242,0.00015418493,0.0012366262,0.0012901587,0.0005844802,0.00033537217,0.013204819,0.9701047,0.000105839674],"about_ca_topic_score_codex":0.005902843,"about_ca_topic_score_gemma":0.013409178,"teacher_disagreement_score":0.037049823,"about_ca_system_score_codex":0.0042255884,"about_ca_system_score_gemma":0.016899481,"threshold_uncertainty_score":0.1959405},"labels":[],"label_agreement":null},{"id":"W7073650370","doi":"","title":"Global patterns and environmental drivers of forest functional composition","year":2024,"lang":"","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsches Zentrum für integrative Biodiversitätsforschung Halle-Jena-Leipzig","keywords":"Biome; Composition (language); Trait; Ecosystem; Forest ecology; Taiga; Environmental change","score_opus":0.0361748316666866,"score_gpt":0.29498755665337045,"score_spread":0.25881272498668384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073650370","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9876837,0.0010333447,0.00048705234,0.00022504079,0.0000065351937,0.0000060534285,0.0087192785,0.000021259963,0.0018176677],"genre_scores_gemma":[0.9941063,0.00037357793,0.00031898703,0.000031756117,0.000008703052,0.0000066767825,0.004880227,0.00000901226,0.00026475385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991405,0.000022439253,0.000006753954,0.000026515756,0.000011233539,0.000019009361],"domain_scores_gemma":[0.99940646,0.00013206461,0.000241672,0.00006534058,0.00007486363,0.0000797421],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003256264,0.00013258046,0.00017985232,0.0012027032,0.00013162299,0.0003462409,0.00012622266,0.00015814295,0.0034712795],"category_scores_gemma":[0.000798413,0.00007123414,0.00017565727,0.002402684,0.00014449818,0.0004956921,0.0003027782,0.00019197546,0.00039729927],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000719913,0.000019673784,0.97848916,0.000068995156,0.00020004547,0.000040352243,0.00010179102,0.0005463275,0.0026215257,0.00064208,0.0009017844,0.016296186],"study_design_scores_gemma":[0.0000017882028,0.000005537452,0.9990289,0.0000043308305,0.000014764821,0.000014719326,0.00006258628,0.00018115003,0.00005220007,0.00018135017,0.00045134357,0.0000012670586],"about_ca_topic_score_codex":0.007564827,"about_ca_topic_score_gemma":0.01432927,"teacher_disagreement_score":0.007564827,"about_ca_system_score_codex":0.00012982938,"about_ca_system_score_gemma":0.00016184783,"threshold_uncertainty_score":0.01504159},"labels":[],"label_agreement":null},{"id":"W7073783740","doi":"","title":"Frailty factors and outcomes in vascular surgery patients: a systematic review and meta-analysis","year":2019,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Frailty Index; Confidence interval; Hazard ratio; Vascular surgery; PsycINFO; MEDLINE; Meta-analysis; Quality of life (healthcare)","score_opus":0.07171398090001313,"score_gpt":0.24814062023665573,"score_spread":0.1764266393366426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073783740","genre_codex":"review","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":"review","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0028074142,0.9959871,0.00024234065,0.00017917596,0.0000838566,0.00021444961,0.0003257308,0.000011010863,0.00014883107],"genre_scores_gemma":[0.09309264,0.9028925,0.0012623577,0.00068437855,0.00022953202,0.0009545511,0.00063089264,0.000014230733,0.0002388912],"study_design_codex":"systematic_review","study_design_gemma":"meta_analysis","domain_scores_codex":[0.99222165,0.003439821,0.0023367282,0.0007239257,0.00094209536,0.00033571542],"domain_scores_gemma":[0.9824806,0.012234526,0.00321701,0.0005230841,0.0013214385,0.00022333667],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.014253546,0.0024205016,0.01544021,0.0065705986,0.00070316385,0.0032938828,0.0020286853,0.0018650602,0.0041765245],"category_scores_gemma":[0.03255978,0.0012073048,0.03038548,0.0074376105,0.00068291544,0.0018817845,0.0017194689,0.0016413735,0.00026222208],"study_design_candidate":"meta_analysis","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010820198,0.000032872696,0.0049218046,0.6354025,0.34212777,0.00013345822,0.0001173522,0.00044803432,0.00014406856,0.00015016146,0.00088111236,0.014558789],"study_design_scores_gemma":[0.00047185892,0.00024018763,0.0066501754,0.0983557,0.8906969,0.00015740431,0.00008239161,0.00021970217,0.00010455631,0.00024995054,0.0027360455,0.000035044963],"about_ca_topic_score_codex":0.0075667882,"about_ca_topic_score_gemma":0.020657683,"teacher_disagreement_score":0.01544021,"about_ca_system_score_codex":0.0026493552,"about_ca_system_score_gemma":0.0055804094,"threshold_uncertainty_score":0.07538086},"labels":[],"label_agreement":null},{"id":"W7073835986","doi":"","title":"Partnerships across the line: Arthritis research in a First Nations community","year":2009,"lang":"en","type":"article","venue":"cIRcle (University of British Columbia)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"General partnership; Public health; Arthritis; Joint (building)","score_opus":0.0668331199727052,"score_gpt":0.25570939124589576,"score_spread":0.18887627127319057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073835986","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06126795,0.03408187,0.00028811532,0.8602525,0.0019548766,0.00016930934,0.00019878885,0.000020145299,0.041766413],"genre_scores_gemma":[0.8526152,0.034902886,0.001395841,0.08624225,0.0009557171,0.00054796896,0.00021928508,0.000035453788,0.023085391],"study_design_codex":"not_applicable","study_design_gemma":"qualitative","domain_scores_codex":[0.9750923,0.01447116,0.00045374135,0.0005852118,0.0020516475,0.007345988],"domain_scores_gemma":[0.87275386,0.018725974,0.0039111925,0.0014737513,0.0082388,0.094896525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.019376274,0.00047145673,0.0007827567,0.002466672,0.023827508,0.015038793,0.0018958921,0.010476978,0.022449477],"category_scores_gemma":[0.036121577,0.00077302277,0.00039240596,0.005214446,0.0074490285,0.011693362,0.01924273,0.011286387,0.0011484415],"study_design_candidate":"qualitative","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054098933,0.0020096474,0.09971723,0.001306552,0.00015513712,0.0034484174,0.11481416,0.0003101741,0.0005952109,0.08913361,0.38761067,0.30035818],"study_design_scores_gemma":[0.00039849075,0.0005368819,0.07829516,0.0052866545,0.000121082914,0.0010771304,0.515146,0.0003792884,0.00021798843,0.032812305,0.36558202,0.00014708235],"about_ca_topic_score_codex":0.24780641,"about_ca_topic_score_gemma":0.48194176,"teacher_disagreement_score":0.75219357,"about_ca_system_score_codex":0.020979377,"about_ca_system_score_gemma":0.15827087,"threshold_uncertainty_score":0.49272805},"labels":[],"label_agreement":null},{"id":"W7073903944","doi":"","title":"An unusual hotspot in a young woman with Hodgkin's lymphoma","year":2008,"lang":"en","type":"article","venue":"Digital Academic REpository of VU University Amsterdam (Vrije Universiteit Amsterdam)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pediatric Oncology Group","funders":"","keywords":"Lymphoma; Hotspot (geology); Pseudolymphoma; Mantle cell lymphoma; Aggressive lymphoma","score_opus":0.010847965310948662,"score_gpt":0.18577211059290402,"score_spread":0.17492414528195535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073903944","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97103935,0.0024348646,0.0013115475,0.0050949366,0.00058077835,0.0001395182,0.00075722905,0.00022243467,0.018419337],"genre_scores_gemma":[0.99560356,0.00063830975,0.0003141941,0.00079629204,0.00096582214,0.0000150772175,0.00017572312,0.000030291303,0.0014606208],"study_design_codex":"case_report","study_design_gemma":"case_report","domain_scores_codex":[0.9996517,0.000034761386,0.000031998716,0.000070769725,0.000040888124,0.00016984255],"domain_scores_gemma":[0.99830496,0.00044449844,0.00025276904,0.00010160663,0.00009524501,0.00080096256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001684933,0.0011356004,0.00112813,0.0036555924,0.0018886253,0.0010004372,0.001389262,0.0045020906,0.006648875],"category_scores_gemma":[0.0031012977,0.0008752876,0.0007778543,0.001898133,0.00094684964,0.0017738517,0.001520082,0.0019883723,0.0017915188],"study_design_candidate":"case_report","study_design_consensus":"case_report","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005710811,0.000023662044,0.011141597,0.0000126345185,0.0000038775966,0.9874977,0.000106219406,0.000025958441,0.0002756499,0.000048217837,0.00030219238,0.00050510594],"study_design_scores_gemma":[0.00001717989,0.000120061595,0.021645457,0.000017040913,0.000020161862,0.97689396,0.00041301432,0.00014956648,0.00014104924,0.00013037596,0.00043895183,0.0000131242905],"about_ca_topic_score_codex":0.0032136724,"about_ca_topic_score_gemma":0.0033463878,"teacher_disagreement_score":0.006648875,"about_ca_system_score_codex":0.0007146778,"about_ca_system_score_gemma":0.000637446,"threshold_uncertainty_score":0.022242665},"labels":[],"label_agreement":null},{"id":"W7073954676","doi":"","title":"International procedures for environmental protection initiated by individuals","year":2015,"lang":"en","type":"article","venue":"SCIndeks","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Context (archaeology); Limiting; Work (physics); Derogation","score_opus":0.050260791491416476,"score_gpt":0.2477634511391986,"score_spread":0.19750265964778213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073954676","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0022972424,0.002630519,0.06286536,0.008435433,0.0055529843,0.0030025847,0.0012279927,0.0011122609,0.9128755],"genre_scores_gemma":[0.06665278,0.0050392654,0.13343874,0.023769163,0.0035409844,0.01231022,0.0036568763,0.001466952,0.75012493],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9507257,0.018451497,0.006044346,0.0053121457,0.015918005,0.0035482661],"domain_scores_gemma":[0.97817504,0.0077176043,0.0014085792,0.0071975267,0.005115974,0.00038535486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.024708854,0.001497963,0.0011187546,0.003099753,0.007333601,0.009248331,0.0039330474,0.01302662,0.029447474],"category_scores_gemma":[0.033810038,0.0013564683,0.0024373285,0.0028716812,0.0091943145,0.006259711,0.007805963,0.016674286,0.032982837],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043104734,0.000054257285,0.00014607002,0.00022121238,0.000009908153,0.00013293892,0.0032930637,0.00022233842,0.000695634,0.8682587,0.09959638,0.027326357],"study_design_scores_gemma":[0.000013161137,0.00004189056,0.00024088699,0.00030594185,0.000008378239,0.00010263652,0.0003206922,0.00011997296,0.0006800141,0.033648703,0.96448,0.00003774685],"about_ca_topic_score_codex":0.005504302,"about_ca_topic_score_gemma":0.0059707146,"teacher_disagreement_score":0.029447474,"about_ca_system_score_codex":0.0044899955,"about_ca_system_score_gemma":0.015612311,"threshold_uncertainty_score":0.13067448},"labels":[],"label_agreement":null},{"id":"W7073994105","doi":"","title":"Identification of Staphylococcus aureus brain abscesses: rat and human studies with 1H MR spectroscopy","year":2005,"lang":"en","type":"article","venue":"NPARC","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Staphylococcus aureus; In vivo; Abscess; Ex vivo; Brain abscess; Staphylococcal infections; Metabolite; Biopsy; Glioblastoma","score_opus":0.01660880356892251,"score_gpt":0.26276208927076783,"score_spread":0.2461532857018453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7073994105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951983,0.0014769295,0.0029258323,0.00004450139,0.0000082999595,0.00004883454,0.00007286512,0.000021771408,0.00020270118],"genre_scores_gemma":[0.9940202,0.0012706,0.004080596,0.000051198273,0.000016922022,0.000034620487,0.00023921374,0.000008729629,0.00027791178],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9995067,0.00021792413,0.000029194347,0.000115155555,0.000087109605,0.00004388785],"domain_scores_gemma":[0.9993229,0.00019210055,0.00020245096,0.000084931205,0.00013765004,0.00006012814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001352834,0.0005431662,0.00047623232,0.0005438239,0.00019187096,0.00029686905,0.00015186235,0.00036407379,0.0008775071],"category_scores_gemma":[0.0013000006,0.00017809002,0.00023503497,0.00023817856,0.00074057095,0.00030332457,0.00030153402,0.00033418456,0.00025089813],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.012687456,0.0019203556,0.09047274,0.00070958794,0.00025906178,0.0012685653,0.00067604054,0.0010740412,0.8317342,0.00026080967,0.00040448824,0.05853268],"study_design_scores_gemma":[0.00049060077,0.06762129,0.48751447,0.00012920094,0.0005686905,0.024250569,0.00124247,0.012457183,0.40044168,0.00074148545,0.0044391486,0.00010322648],"about_ca_topic_score_codex":0.00090344675,"about_ca_topic_score_gemma":0.0014344,"teacher_disagreement_score":0.001352834,"about_ca_system_score_codex":0.00019621968,"about_ca_system_score_gemma":0.00028562386,"threshold_uncertainty_score":0.0071545243},"labels":[],"label_agreement":null},{"id":"W7074009528","doi":"","title":"Contribuição do espaço da escuta terapêutica, com orientação fenomenológica hermenêutica, para a compreensão do discurso dos doentes após alívio abrupto e agudo da nocicepção","year":2018,"lang":"pt","type":"article","venue":"Americanae (AECID Library)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Context (archaeology); Peripheral neuropathy; Lumbar spine; Neuropathic pain","score_opus":0.02529601305649717,"score_gpt":0.25533895964453934,"score_spread":0.23004294658804217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074009528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6037683,0.17747322,0.12049058,0.026736632,0.0031478622,0.0008150614,0.00041588448,0.0004942011,0.0666582],"genre_scores_gemma":[0.9080263,0.043043982,0.032753058,0.0022522663,0.0006267466,0.0003515039,0.00009081612,0.000099065415,0.012756375],"study_design_codex":"design_other","study_design_gemma":"qualitative","domain_scores_codex":[0.99810624,0.0008851956,0.000102398204,0.0002462837,0.00048264634,0.0001771739],"domain_scores_gemma":[0.9974503,0.0012817075,0.00035933207,0.00024396116,0.00056863436,0.000096054195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033242144,0.00040863166,0.00059789355,0.0010531603,0.0011672387,0.003944311,0.0008048126,0.0013986656,0.0050808806],"category_scores_gemma":[0.0049755843,0.0002583865,0.0005426759,0.00065731903,0.002164982,0.001482011,0.0012922296,0.0008261033,0.0009806363],"study_design_candidate":"qualitative","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013192238,0.00038153134,0.04400307,0.005210272,0.00013992678,0.003619917,0.014219831,0.0015128978,0.2507423,0.019796059,0.0057942728,0.6532607],"study_design_scores_gemma":[0.00015138282,0.0066519473,0.124950945,0.0068225185,0.00075094635,0.026566613,0.04406106,0.0077233,0.22768971,0.039485816,0.5147527,0.00039310448],"about_ca_topic_score_codex":0.0015823164,"about_ca_topic_score_gemma":0.002913853,"teacher_disagreement_score":0.0050808806,"about_ca_system_score_codex":0.0010049954,"about_ca_system_score_gemma":0.0019453631,"threshold_uncertainty_score":0.01758033},"labels":[],"label_agreement":null},{"id":"W7074093847","doi":"","title":"Ethical Issues in Health Research in Children","year":2008,"lang":"en","type":"article","venue":"PubMed Central","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ethical issues; Foundation (evidence); Research ethics; Duty; Informed consent; Vulnerability (computing); Health care; Ethical code","score_opus":0.08927169741722903,"score_gpt":0.30996831338847963,"score_spread":0.22069661597125062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074093847","genre_codex":"commentary","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.013637647,0.02984454,0.05352813,0.8125434,0.011657141,0.002837165,0.00029858644,0.00017327147,0.075480096],"genre_scores_gemma":[0.31854042,0.022661876,0.156088,0.44814616,0.014781181,0.012094235,0.00030742804,0.000369533,0.027011227],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.4657117,0.45189983,0.026853569,0.009205969,0.03774861,0.0085803475],"domain_scores_gemma":[0.36593777,0.53226393,0.01905051,0.035848476,0.029650165,0.017249165],"candidate_categories":["metaresearch","research_integrity"],"consensus_categories":[],"category_scores_codex":[0.39647636,0.0010088043,0.002975051,0.0021130745,0.013866048,0.014005958,0.0060566664,0.027347272,0.0042764135],"category_scores_gemma":[0.39110407,0.0017261,0.0017682044,0.0034511692,0.07178477,0.010632809,0.011351097,0.036929496,0.0020546282],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029802497,0.00015598745,0.0031923829,0.0017589111,0.00016637858,0.0029874053,0.14537771,0.00056522613,0.001102323,0.62440735,0.1525466,0.06744169],"study_design_scores_gemma":[0.00022652383,0.0002161355,0.0025426424,0.009189001,0.000102790684,0.004668917,0.045364432,0.0008490153,0.0013941702,0.26442602,0.6708158,0.00020457972],"about_ca_topic_score_codex":0.009069986,"about_ca_topic_score_gemma":0.015386212,"teacher_disagreement_score":0.97265273,"about_ca_system_score_codex":0.009189542,"about_ca_system_score_gemma":0.059472725,"threshold_uncertainty_score":0.7442521},"labels":[],"label_agreement":null},{"id":"W7074100624","doi":"","title":"The Continuing Education of Faculty as Teachers at a Mid-sized Ontario University","year":2011,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Excellence; Continuing education; Higher education; Professional development; University faculty","score_opus":0.08830148738180778,"score_gpt":0.27151048629552804,"score_spread":0.18320899891372028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074100624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":"methods","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":"methods","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95186377,0.0010627969,0.0002994145,0.011532449,0.00014757,0.000100254765,0.00007479847,0.000035671983,0.034883168],"genre_scores_gemma":[0.9738201,0.00061760953,0.0003874761,0.0012635795,0.000038371512,0.00005268275,0.000056144123,0.000014353902,0.023749702],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.99580115,0.0011020352,0.000116816846,0.00030672358,0.001059535,0.0016136469],"domain_scores_gemma":[0.98130035,0.0021535826,0.0015497118,0.0004902233,0.0034017062,0.011104428],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.003373908,0.00015888644,0.0002186651,0.0010446253,0.018172387,0.0059998436,0.0015203138,0.0012578717,0.008696186],"category_scores_gemma":[0.01262713,0.00023384043,0.00017819772,0.0017000416,0.0049831322,0.002062878,0.0038778125,0.0011780671,0.00069409085],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000068724985,0.00019691627,0.077853434,0.00014727474,0.0000068180507,0.0013994697,0.8289059,0.000040515082,0.0019252795,0.003472416,0.014687564,0.07129562],"study_design_scores_gemma":[0.000009216467,0.00010953884,0.06990806,0.00010759591,0.000005105812,0.00021557705,0.7859337,0.00004804265,0.00036311612,0.0003985493,0.14288124,0.00002023575],"about_ca_topic_score_codex":0.45418432,"about_ca_topic_score_gemma":0.7531836,"teacher_disagreement_score":0.9966261,"about_ca_system_score_codex":0.031079954,"about_ca_system_score_gemma":0.06623967,"threshold_uncertainty_score":0.90308136},"labels":[],"label_agreement":null},{"id":"W7074137668","doi":"","title":"Agent-mediated electronic commerce and trading agent design and analysis AAMAS 2007 workshop, AMEC 2007, Honolulu, Hawaii, May 14, 2007 and AAAI 2007 workshop, TADA 2007, Vancouver, Canada, July 23, 2007 ; selected and revised papers","year":2008,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"E-commerce; Multi-agent system; Intelligent agent","score_opus":0.01781500445419053,"score_gpt":0.20724456168351363,"score_spread":0.1894295572293231,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074137668","genre_codex":"methods","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.025090547,0.0024714586,0.9520298,0.0014345672,0.00027116764,0.00016420553,0.000061831815,0.00034213843,0.018134253],"genre_scores_gemma":[0.4538787,0.0027647968,0.49389687,0.00031186568,0.0002575736,0.0003739664,0.0002977003,0.00023553128,0.047983058],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.997726,0.001324099,0.000110400695,0.00025722446,0.0004880756,0.000094166506],"domain_scores_gemma":[0.9964055,0.0022532048,0.000092864204,0.00040731122,0.0006929093,0.0001481614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004146671,0.0006209997,0.0007710176,0.0006167135,0.0009841275,0.005376784,0.0016759457,0.001586944,0.008933841],"category_scores_gemma":[0.007815926,0.0007960146,0.00071211514,0.0006939777,0.0016004567,0.004538953,0.0015957307,0.0015077292,0.0011028444],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038973466,0.00063135306,0.0035464924,0.0003331097,0.00026699193,0.00049222464,0.0013855144,0.15363814,0.005502064,0.5386175,0.01500121,0.28019565],"study_design_scores_gemma":[0.000054554825,0.00014237374,0.0007419636,0.00006289776,0.00009292584,0.00021085769,0.0003378722,0.70279914,0.0046716738,0.24838422,0.042466544,0.000034950834],"about_ca_topic_score_codex":0.002432818,"about_ca_topic_score_gemma":0.002901011,"teacher_disagreement_score":0.008933841,"about_ca_system_score_codex":0.0011276153,"about_ca_system_score_gemma":0.0014361598,"threshold_uncertainty_score":0.029886663},"labels":[],"label_agreement":null},{"id":"W7074157392","doi":"","title":"Diagnosis of the Nutrient Compositional Space of Fruit Crops","year":2011,"lang":"en","type":"article","venue":"LA Referencia (Red Federada de Repositorios Institucionales de Publicaciones Científicas)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nutrient; Nutrient deficiency; Orchard; Composition (language); Compositional data; Ternary plot; Nutrient cycle; Phosphorus","score_opus":0.028404962414389417,"score_gpt":0.22067971209685805,"score_spread":0.19227474968246863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074157392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9319553,0.00011464577,0.06448029,0.000037954418,0.0000032928815,0.000042357897,0.00061672035,0.00029556098,0.0024537817],"genre_scores_gemma":[0.9857041,0.000023271123,0.013458593,0.000004306864,9.659668e-7,0.000009087422,0.00030089362,0.000014781364,0.0004840468],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998325,0.000023306098,0.000008055179,0.0000588282,0.000049766022,0.000027381117],"domain_scores_gemma":[0.9997631,0.00008249732,0.000034911576,0.000013358639,0.00008553815,0.000020632455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022833027,0.00030351925,0.00024436068,0.0011142285,0.00032606503,0.00064942084,0.00052159076,0.00020784087,0.0011684368],"category_scores_gemma":[0.00072046206,0.00016625455,0.00030559764,0.0004632315,0.00030120963,0.00034863685,0.00034954838,0.00018133716,0.00013732255],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006143374,0.00013171589,0.19327392,0.00026724514,0.00011234199,0.00081063656,0.0004439436,0.55235827,0.12671927,0.010042817,0.0008309036,0.11439456],"study_design_scores_gemma":[0.000005282043,0.000027119484,0.04230921,0.000005292561,0.000009775434,0.0000638715,0.00013239014,0.94871414,0.0069347564,0.0013314923,0.00045132593,0.0000152558605],"about_ca_topic_score_codex":0.10164702,"about_ca_topic_score_gemma":0.08314331,"teacher_disagreement_score":0.10164702,"about_ca_system_score_codex":0.0020921205,"about_ca_system_score_gemma":0.001149305,"threshold_uncertainty_score":0.20211071},"labels":[],"label_agreement":null},{"id":"W7074159070","doi":"","title":"The Pseudomonas aeruginosa whole genome sequence:A 20th anniversary celebration","year":2021,"lang":"en","type":"article","venue":"Technical University of Denmark, DTU Orbit (Technical University of Denmark, DTU)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; University of British Columbia; Simon Fraser University","funders":"","keywords":"Genome; Pseudomonas aeruginosa; Whole genome sequencing; Bacteria; Pseudomonadales; Pseudomonadaceae","score_opus":0.017482309909702703,"score_gpt":0.20059039984496096,"score_spread":0.18310808993525826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074159070","genre_codex":"editorial","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.027707145,0.10892011,0.013854467,0.24016367,0.54601854,0.00017798727,0.031179547,0.0038658974,0.028112615],"genre_scores_gemma":[0.13774385,0.124310754,0.056559287,0.12634219,0.17466313,0.0007472128,0.14931037,0.005073405,0.22524983],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99845016,0.00014526516,0.000071502465,0.00024941156,0.00073222077,0.000351354],"domain_scores_gemma":[0.99131763,0.00058996986,0.00032916438,0.00037220557,0.0027707124,0.004620378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0060856706,0.0012072128,0.0014721735,0.0020775916,0.0012523005,0.00400551,0.00086814765,0.003896986,0.011801086],"category_scores_gemma":[0.008609872,0.00055734516,0.0009411371,0.0014861801,0.0010390646,0.003225601,0.0062880004,0.0062255273,0.010464991],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005736646,0.000086506145,0.00082504173,0.0004907602,0.000062590334,0.00020451813,0.00016890289,0.0001872334,0.0146903945,0.0016855082,0.85033697,0.13068801],"study_design_scores_gemma":[0.000032381085,0.00009179336,0.006233373,0.0001768088,0.000028543278,0.00018516791,0.0001370012,0.00013370243,0.0016886257,0.001584131,0.9896667,0.000041744926],"about_ca_topic_score_codex":0.002011679,"about_ca_topic_score_gemma":0.004460282,"teacher_disagreement_score":0.011801086,"about_ca_system_score_codex":0.0016319645,"about_ca_system_score_gemma":0.002931698,"threshold_uncertainty_score":0.0394786},"labels":[],"label_agreement":null},{"id":"W7074216663","doi":"","title":"Knowledge for the People: The Struggle for Adult Learning in English-Speaking Canada 1828–1973","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Adult education; Adult Learning; Experiential learning; Training (meteorology); Agency (philosophy)","score_opus":0.021293593503130474,"score_gpt":0.21473826371843538,"score_spread":0.1934446702153049,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074216663","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95391613,0.0009045726,0.00007419971,0.004413832,0.00004860222,0.000022805858,0.00056578394,0.0000060613165,0.040048037],"genre_scores_gemma":[0.9781059,0.0005357178,0.000090991416,0.00029899366,0.000008718899,0.000008384516,0.00015250841,0.000005948337,0.020792756],"study_design_codex":"qualitative","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991357,0.00006293697,0.000015101876,0.00006319391,0.000178859,0.0005442133],"domain_scores_gemma":[0.998104,0.0001382256,0.0001073706,0.00003159907,0.0008267791,0.00079198775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000646255,0.00014774883,0.0002912423,0.00084574166,0.01390791,0.0027730141,0.001236849,0.00068917824,0.00547052],"category_scores_gemma":[0.0021429881,0.00015831571,0.00015239327,0.0020352527,0.004233396,0.0011225968,0.0023024753,0.0018416318,0.0002899114],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001374271,0.00011841624,0.195417,0.00010645155,0.000025701549,0.0016029183,0.679879,0.00022485988,0.00070254743,0.020413823,0.017780118,0.083591715],"study_design_scores_gemma":[0.0000067680567,0.000029738554,0.39966628,0.00013059146,0.000016136191,0.00027856932,0.4998505,0.00013845634,0.00021946026,0.00071422575,0.09891861,0.000030745476],"about_ca_topic_score_codex":0.99598724,"about_ca_topic_score_gemma":0.99886835,"teacher_disagreement_score":0.94421226,"about_ca_system_score_codex":0.055787727,"about_ca_system_score_gemma":0.059552953,"threshold_uncertainty_score":0.4047702},"labels":[],"label_agreement":null},{"id":"W7074225734","doi":"","title":"DNA Methylation and mRNA Expression of SYN III, a Candidate Gene for Schizophrenia","year":2008,"lang":"en","type":"article","venue":"Scholarship@Western (Western University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"CpG site; DNA methylation; Methylation; Gene; Cytosine; Differentially methylated regions; Illumina Methylation Assay; Population; Schizophrenia (object-oriented programming)","score_opus":0.07061345731988942,"score_gpt":0.27012217336901145,"score_spread":0.19950871604912201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074225734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990445,0.0003070308,0.0002022921,0.000013894789,0.0000025377951,0.0000032411135,0.00018393541,0.0000040458244,0.00023855119],"genre_scores_gemma":[0.99842393,0.00021130382,0.0003529575,0.000012995134,0.0000036367235,0.00000779747,0.0003403443,0.0000031676595,0.0006437974],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999596,0.000006810899,0.0000027997705,0.000015861964,0.0000085271695,0.000006451161],"domain_scores_gemma":[0.99992037,0.000015048827,0.000029211667,0.0000034461812,0.000016945962,0.000014973427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008508663,0.00012230818,0.00007733193,0.00027731538,0.000105730694,0.00011964398,0.00004914104,0.00011818001,0.0015230726],"category_scores_gemma":[0.00021859256,0.00008863768,0.000054271666,0.00013193827,0.000104639636,0.000045427056,0.000084553365,0.00009937697,0.0001652037],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012037561,0.000032770044,0.18995385,0.00009028688,0.00009255331,0.0002815879,0.00037043588,0.00010539551,0.79762447,0.000083618135,0.00018640148,0.009974847],"study_design_scores_gemma":[0.000024547136,0.0002520708,0.9623242,0.000008860471,0.000050333838,0.0009742268,0.0001437029,0.00033052976,0.03520877,0.00008649348,0.0005912591,0.0000049163705],"about_ca_topic_score_codex":0.0014321799,"about_ca_topic_score_gemma":0.0020369047,"teacher_disagreement_score":0.0015230726,"about_ca_system_score_codex":0.00013719809,"about_ca_system_score_gemma":0.00008993977,"threshold_uncertainty_score":0.005095184},"labels":[],"label_agreement":null},{"id":"W7074246921","doi":"","title":"Is God a Racist?: The Right Wing in Canada","year":2023,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Right wing; Government (linguistics); Wing","score_opus":0.019538550756327107,"score_gpt":0.19814712069906956,"score_spread":0.17860856994274246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074246921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.46181667,0.008518707,0.00037817835,0.36418208,0.002116057,0.00008898089,0.0006622075,0.000038320788,0.16219874],"genre_scores_gemma":[0.88739485,0.0037357025,0.00031952804,0.03091716,0.0001134811,0.00003402301,0.00013637799,0.000101628975,0.07724726],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9956185,0.00037392593,0.000058554953,0.00032553353,0.00073412154,0.0028894],"domain_scores_gemma":[0.9915228,0.00059316074,0.00024436633,0.000095200325,0.0018349224,0.0057095666],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021189868,0.0003259084,0.00072557526,0.0009305896,0.06519282,0.010692416,0.002950379,0.006140804,0.015954023],"category_scores_gemma":[0.0054310136,0.00063435244,0.000419328,0.0027111422,0.011874138,0.0037502062,0.0058011347,0.013020877,0.00087870605],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025165337,0.00025182945,0.05981408,0.0002037892,0.00007740625,0.0034255048,0.3383403,0.00030989884,0.00065047905,0.13296531,0.39654878,0.067160964],"study_design_scores_gemma":[0.000029394385,0.000025903222,0.031220436,0.0004647358,0.0000478694,0.0003888347,0.6234328,0.00020680911,0.00020530561,0.004373165,0.3394852,0.00011958948],"about_ca_topic_score_codex":0.9974602,"about_ca_topic_score_gemma":0.9993893,"teacher_disagreement_score":0.122120805,"about_ca_system_score_codex":0.122120805,"about_ca_system_score_gemma":0.27452984,"threshold_uncertainty_score":0.8860526},"labels":[],"label_agreement":null},{"id":"W7074619388","doi":"","title":"Strategies to increase the sugar concentration and overall sugar recovery from steam pretreated wheat straw and corn stover","year":2012,"lang":"en","type":"other","venue":"cIRcle (University of British Columbia)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sugar; Enzymatic hydrolysis; Yield (engineering); Xylose; Cellulose; Raw material","score_opus":0.00811039061191672,"score_gpt":0.16307250347665883,"score_spread":0.1549621128647421,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074619388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98807377,0.0016472385,0.0076159984,0.00010273448,0.000020058815,0.000073983174,0.00014385917,0.00007801664,0.0022444795],"genre_scores_gemma":[0.9820786,0.002222678,0.012129103,0.00006454819,0.000009570911,0.00005117932,0.00035374064,0.00003651689,0.0030540072],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998499,0.000013650101,0.000014793225,0.000026299043,0.00006246632,0.00003290812],"domain_scores_gemma":[0.9999263,0.00000910493,0.00003089089,0.000006289478,0.000018706118,0.000008695304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019831632,0.000537688,0.00037638503,0.0003487347,0.00016430339,0.00053755456,0.00028573468,0.00029099945,0.00100713],"category_scores_gemma":[0.00014582559,0.00027571435,0.0005126081,0.00041023738,0.0001391841,0.00039524253,0.00024398633,0.00072298176,0.00031304886],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023745797,0.000030259162,0.00011489526,0.000062442035,0.0000059856743,0.000027693428,0.000010319678,0.00023893235,0.9968167,0.000042611216,0.0000168034,0.0026096727],"study_design_scores_gemma":[0.0000032793848,0.00019647405,0.001408319,0.000009172473,0.000013552753,0.000031687418,0.000030786076,0.000814207,0.9964992,0.000022424167,0.00096613984,0.000004697045],"about_ca_topic_score_codex":0.0012407642,"about_ca_topic_score_gemma":0.0046795076,"teacher_disagreement_score":0.0012407642,"about_ca_system_score_codex":0.00036194065,"about_ca_system_score_gemma":0.00031049474,"threshold_uncertainty_score":0.0033692122},"labels":[],"label_agreement":null},{"id":"W7074677329","doi":"","title":"Home-Work : Postcolonialism, Pedagogy, and Canadian Literature","year":2004,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Nationalism; Colonialism; Canadian literature; Duty; Canadian studies; Postcolonial literature","score_opus":0.012420865453189947,"score_gpt":0.20634567637046425,"score_spread":0.19392481091727432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074677329","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3105983,0.039155934,0.0013884497,0.052506723,0.000501743,0.0000734499,0.00022268521,0.00013775272,0.5954149],"genre_scores_gemma":[0.9648028,0.0070025306,0.0005227423,0.0010959913,0.00004430816,0.000018953824,0.000039919672,0.000032785305,0.02644003],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99737287,0.0006416929,0.000052130737,0.00019660617,0.00068477954,0.0010520375],"domain_scores_gemma":[0.99521565,0.0016242767,0.00026119332,0.0001687805,0.001431581,0.0012984935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003547383,0.00036933145,0.00042833952,0.004918546,0.030723281,0.009898227,0.002355092,0.0014083124,0.009651949],"category_scores_gemma":[0.006231191,0.0001991742,0.00018231844,0.007800428,0.025304895,0.0025586819,0.0033195128,0.0020783371,0.00030349524],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":true,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056802568,0.00008829366,0.0073970924,0.00031009733,0.000012407537,0.00065186544,0.43904224,0.000272966,0.00028808595,0.44027916,0.022231488,0.08936949],"study_design_scores_gemma":[0.000019047086,0.00003507524,0.035454683,0.0009398167,0.000021542912,0.00021626237,0.4344409,0.0002784845,0.0004392355,0.022204703,0.50589585,0.000054321034],"about_ca_topic_score_codex":0.99007773,"about_ca_topic_score_gemma":0.9959913,"teacher_disagreement_score":0.1795747,"about_ca_system_score_codex":0.1795747,"about_ca_system_score_gemma":0.19201079,"threshold_uncertainty_score":0.95157707},"labels":[],"label_agreement":null},{"id":"W7074686113","doi":"","title":"Changing Toronto : Governing Urban Neoliberalism","year":2009,"lang":"en","type":"other","venue":"EspaceINRS (National Institute for Scientific Research (Canada))","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Metropolitan area; Neoliberalism (international relations); Formative assessment; Period (music); Urban planning; Megacity; Urbanization; Government (linguistics)","score_opus":0.03778056731313565,"score_gpt":0.2856666475793261,"score_spread":0.24788608026619044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7074686113","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.08060968,0.0065767015,0.0013293489,0.049823582,0.00053767615,0.000048949227,0.000387679,0.00009654346,0.86058974],"genre_scores_gemma":[0.84593594,0.0026072613,0.0005620588,0.002781071,0.00013494624,0.000041692278,0.00018667337,0.00007398972,0.14767632],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.9985648,0.00030300015,0.000022365206,0.00014293904,0.00027498748,0.00069189956],"domain_scores_gemma":[0.9989361,0.00013974294,0.000093276554,0.000099411474,0.00014977365,0.0005816834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094029366,0.00031159935,0.0001644805,0.00072033674,0.012652011,0.0083047245,0.0010661026,0.0015069318,0.012983995],"category_scores_gemma":[0.0015082347,0.00018125177,0.00020979607,0.0016616058,0.01272822,0.002524806,0.00412306,0.0018683102,0.00052781083],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033845867,0.000012151625,0.003984585,0.00008755138,0.000010290216,0.0004622122,0.06846607,0.0007479053,0.00022151737,0.8201532,0.0828552,0.022965437],"study_design_scores_gemma":[0.000008802834,0.000007615741,0.009243187,0.00010368708,0.000007655661,0.00005319872,0.031843692,0.0003035284,0.00022352944,0.017528964,0.9406595,0.000016629296],"about_ca_topic_score_codex":0.91088265,"about_ca_topic_score_gemma":0.9738351,"teacher_disagreement_score":0.109533384,"about_ca_system_score_codex":0.109533384,"about_ca_system_score_gemma":0.051491056,"threshold_uncertainty_score":0.79472405},"labels":[],"label_agreement":null},{"id":"W7075291085","doi":"","title":"Tickets … and More Tickets: A Case Study of the Enforcement of the Ontario Safe Streets Act","year":2014,"lang":"en","type":"article","venue":"Project Muse (Johns Hopkins University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Law enforcement; Deterrence (psychology); Context (archaeology); Subject (documents)","score_opus":0.019005967547085483,"score_gpt":0.20467019051072158,"score_spread":0.1856642229636361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7075291085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98396724,0.0003785831,0.00021581077,0.0025483675,0.000033046766,0.0000784356,0.000091836075,0.0000041099115,0.012682543],"genre_scores_gemma":[0.9862708,0.00083698396,0.0003761917,0.0006387794,0.000022266695,0.000045040702,0.00008237865,0.000010547243,0.011717013],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.9956067,0.0013617123,0.00012660741,0.00024518569,0.001207755,0.0014519689],"domain_scores_gemma":[0.9955252,0.0012785732,0.0011447025,0.0002501337,0.00084098056,0.00096039794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020334048,0.00040784635,0.00040807386,0.0013880837,0.015365889,0.0027106688,0.0016833056,0.0024140186,0.0033425032],"category_scores_gemma":[0.00717572,0.000629111,0.00038257954,0.0030248123,0.0051191733,0.0013566428,0.0024594795,0.0024115178,0.00027086082],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002168498,0.0005331527,0.30943063,0.00025331962,0.00009579124,0.026906062,0.59835434,0.0008526039,0.0015815627,0.016430719,0.013694591,0.031650346],"study_design_scores_gemma":[0.000030189072,0.00015123122,0.2295994,0.00023052862,0.000050749,0.0024442028,0.70866674,0.0009353347,0.00046410714,0.0006161734,0.056742266,0.000069099646],"about_ca_topic_score_codex":0.94189477,"about_ca_topic_score_gemma":0.9840397,"teacher_disagreement_score":0.05810523,"about_ca_system_score_codex":0.03751738,"about_ca_system_score_gemma":0.02844586,"threshold_uncertainty_score":0.27220893},"labels":[],"label_agreement":null},{"id":"W7083176628","doi":"10.5281/zenodo.17189856","title":"Effectiveness of Proprioceptive Training Versus Muscle Energy Technique on Pain, Range of Motion and Functional Disability in Individuals with Knee Osteoarthritis","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Proprioception; Osteoarthritis; Range of motion; Rehabilitation; Knee Joint; Psychological intervention","score_opus":0.024192228777532843,"score_gpt":0.21612258041177548,"score_spread":0.19193035163424263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083176628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99751186,0.001975643,0.00006355705,0.00003567816,0.000015020728,0.0000330698,0.000016371785,0.0000026403652,0.00034620863],"genre_scores_gemma":[0.9982121,0.0010051788,0.00035881126,0.00005057534,0.000035712263,0.0000597793,0.00003878693,7.2415355e-7,0.00023838175],"study_design_codex":"design_other","study_design_gemma":"randomized_trial","domain_scores_codex":[0.99958056,0.00019241581,0.000048784186,0.000036058922,0.00008840838,0.00005379742],"domain_scores_gemma":[0.9995086,0.00018725813,0.0001072226,0.000020291222,0.00003310678,0.00014348053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000706312,0.00024017412,0.0005712133,0.0002782402,0.00020443926,0.00017824631,0.00018034276,0.00038349282,0.0012094261],"category_scores_gemma":[0.0013255936,0.00009822408,0.00039669673,0.00016837237,0.00018262953,0.00017343597,0.00024933426,0.00023705779,0.00012170181],"study_design_candidate":"randomized_trial","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.1615462,0.059874933,0.11366129,0.004464493,0.002325024,0.00038008622,0.00095113757,0.00102634,0.05107432,0.00014828595,0.00046074987,0.6040872],"study_design_scores_gemma":[0.0123398965,0.38970688,0.5910552,0.00026806444,0.0010503132,0.0005301039,0.00063115783,0.0005811643,0.0027730688,0.00011513305,0.0009079086,0.000040966617],"about_ca_topic_score_codex":0.0004269429,"about_ca_topic_score_gemma":0.0014110061,"teacher_disagreement_score":0.0012094261,"about_ca_system_score_codex":0.000093066476,"about_ca_system_score_gemma":0.0001848309,"threshold_uncertainty_score":0.0040459633},"labels":[],"label_agreement":null},{"id":"W7083180273","doi":"10.4018/979-8-3373-0250-8.ch009","title":"A Critical Comparative Analysis of Google Chrome and Microsoft Edge","year":2025,"lang":"en","type":"book-chapter","venue":"Advances in computational intelligence and robotics book series","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Artificial Intelligence in Medicine (Canada)","funders":"","keywords":"Rendering (computer graphics); Empirical research; Web browser; Enhanced Data Rates for GSM Evolution; Competitive advantage; Web application","score_opus":0.026807768483353766,"score_gpt":0.29948850576209723,"score_spread":0.2726807372787435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083180273","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5192891,0.013304213,0.0031646956,0.0024787942,0.00030693764,0.00016339257,0.0028576602,0.001550675,0.45688462],"genre_scores_gemma":[0.8899476,0.007876321,0.0055439435,0.000760609,0.00013660072,0.00005660185,0.0058601354,0.0017726556,0.08804546],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9980463,0.0002367568,0.00005319238,0.0001770776,0.0012730544,0.00021365423],"domain_scores_gemma":[0.9906142,0.0033110827,0.0003498628,0.00028602322,0.0049004564,0.000538408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021407888,0.00037993412,0.00029719557,0.007353745,0.0012224067,0.0048205974,0.00067434704,0.0005190557,0.008805647],"category_scores_gemma":[0.009949942,0.0002934134,0.00032233907,0.0080578625,0.0010374795,0.0049731466,0.0008080747,0.00078947726,0.0025173775],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001384335,0.00034799837,0.059061885,0.002170454,0.00011485644,0.0021128084,0.023767157,0.001307345,0.008742953,0.08966317,0.19158165,0.6197454],"study_design_scores_gemma":[0.000040838724,0.00052177545,0.33952796,0.0009744846,0.00018271377,0.0018060447,0.030268976,0.003300982,0.0076333103,0.0060907784,0.6094606,0.00019150155],"about_ca_topic_score_codex":0.046342418,"about_ca_topic_score_gemma":0.07506745,"teacher_disagreement_score":0.046342418,"about_ca_system_score_codex":0.002752318,"about_ca_system_score_gemma":0.0015544661,"threshold_uncertainty_score":0.09214538},"labels":[],"label_agreement":null},{"id":"W7083296536","doi":"10.4153/s0008414x25101636","title":"On uniformly continuous surjections between function spaces","year":2025,"lang":"en","type":"article","venue":"Canadian Journal of Mathematics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Nipissing University","funders":"Natural Sciences and Engineering Research Council of Canada; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Bijection, injection and surjection; Surjective function; Function (biology); Continuous function (set theory); Uniform continuity; Linear growth","score_opus":0.016856785300055785,"score_gpt":0.21108422437385038,"score_spread":0.19422743907379458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083296536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7220251,0.0021053185,0.21460378,0.0011112186,0.0002719115,0.00009142932,0.00034079223,0.00025911655,0.059191324],"genre_scores_gemma":[0.98374015,0.00053913984,0.01031768,0.00013427947,0.00012178398,0.000052106407,0.0001332641,0.00003487433,0.0049267868],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9979213,0.00066353416,0.000102256374,0.00051803025,0.00046121274,0.00033368505],"domain_scores_gemma":[0.9934911,0.0030771985,0.0004932098,0.00052736007,0.0012423109,0.001168804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022484097,0.0008414207,0.00058220845,0.0017256432,0.0016775075,0.002782695,0.0008540395,0.00086840783,0.0043430254],"category_scores_gemma":[0.0071865544,0.00049301086,0.00088210864,0.00093587564,0.00427685,0.004503785,0.004308796,0.0024674442,0.00043501664],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084835985,0.00006230425,0.0014915444,0.00009342359,0.000035036755,0.0005304632,0.0010587593,0.0030658795,0.0038177161,0.9779279,0.00073081703,0.0111013325],"study_design_scores_gemma":[0.0000354432,0.000385198,0.0051133186,0.00009559594,0.000040604336,0.0010006782,0.0017652283,0.039013345,0.006532212,0.9352604,0.010688467,0.000069476664],"about_ca_topic_score_codex":0.0010879542,"about_ca_topic_score_gemma":0.00048072572,"teacher_disagreement_score":0.0043430254,"about_ca_system_score_codex":0.0012284062,"about_ca_system_score_gemma":0.00039289048,"threshold_uncertainty_score":0.014528871},"labels":[],"label_agreement":null},{"id":"W7083598727","doi":"10.1016/j.jedc.2025.105185","title":"Pandemic consumption","year":2025,"lang":"en","type":"article","venue":"Journal of Economic Dynamics and Control","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Burns Memorial Fund; Universität zu Köln; Deutsche Forschungsgemeinschaft","keywords":"Consumption (sociology); Pandemic; Coronavirus disease 2019 (COVID-19); German; Risk of infection; Durable good; Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2)","score_opus":0.008430988907101599,"score_gpt":0.21801333292410405,"score_spread":0.20958234401700246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083598727","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05085071,0.00061243086,0.0038702155,0.013309888,0.0010970939,0.00012066089,0.0054642847,0.00022782272,0.92444694],"genre_scores_gemma":[0.6059654,0.0009657815,0.0011386098,0.0023671016,0.0003702106,0.00008431219,0.00400796,0.00006146719,0.3850392],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9997347,0.00004562022,0.000009281968,0.000042694614,0.00008812148,0.00007962624],"domain_scores_gemma":[0.99949014,0.000106490064,0.000041621573,0.00011886069,0.00016291293,0.00008006396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003885379,0.00026590633,0.00023692354,0.0005104603,0.00053872244,0.0014397716,0.000465815,0.00094789814,0.11153628],"category_scores_gemma":[0.0023664604,0.00016168882,0.000265825,0.0005232567,0.00037154357,0.0013451421,0.0006430388,0.0014242782,0.008197205],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027296622,0.00016507991,0.013348681,0.00017017659,0.00006828126,0.00038087062,0.00037727036,0.0051666135,0.0012696056,0.5238503,0.32193607,0.1329941],"study_design_scores_gemma":[0.000091967566,0.0001627361,0.026117312,0.00014900189,0.00003685028,0.00079404295,0.0016893265,0.019614551,0.0014075667,0.15386575,0.7960194,0.00005160507],"about_ca_topic_score_codex":0.006330937,"about_ca_topic_score_gemma":0.0051885606,"teacher_disagreement_score":0.11153628,"about_ca_system_score_codex":0.0011552161,"about_ca_system_score_gemma":0.0010132312,"threshold_uncertainty_score":0.37312603},"labels":[],"label_agreement":null},{"id":"W7083625499","doi":"10.5281/zenodo.17220587","title":"CANADA 🇨🇦, AUSTRALIA 🇦🇺,UK 🇬🇧 WORK VISAS AVAILABLE CALL OR WHATSAPP MR PETER OBENDE ON ☎(08143870581).","year":2025,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Work (physics)","score_opus":0.04164889910352479,"score_gpt":0.22939260243727727,"score_spread":0.18774370333375248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083625499","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000290257,0.00027037464,0.00037831962,0.0013613871,0.0006201983,0.000049889328,0.0060667186,0.00118791,0.98977506],"genre_scores_gemma":[0.0004346148,0.000082005165,0.00008675268,0.00012795882,0.00001359272,0.0000064449177,0.00081962516,0.0003113291,0.9981177],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993581,0.000020266509,0.000013478228,0.000102805876,0.00036265576,0.00014270078],"domain_scores_gemma":[0.9976718,0.00010251637,0.000057698417,0.00011443183,0.0011475494,0.0009060366],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000475538,0.0009831337,0.0006590202,0.00089225714,0.0029380373,0.0035494638,0.001089717,0.00232342,0.86134225],"category_scores_gemma":[0.0016994374,0.00056427467,0.0004239985,0.0015821453,0.00067287206,0.0014464154,0.0014111693,0.0015374135,0.7947037],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002978831,0.000007642782,0.0000823118,0.000046128767,0.0000012210166,0.000016566812,0.000029749617,0.000039223607,0.000154747,0.0011651847,0.9763647,0.022062762],"study_design_scores_gemma":[0.0000051035254,0.000005172511,0.0002930859,0.000023567807,0.0000010834617,0.000010807904,0.000042578828,0.00004849715,0.00008577658,0.00014001553,0.9993406,0.0000037916197],"about_ca_topic_score_codex":0.37675104,"about_ca_topic_score_gemma":0.6127828,"teacher_disagreement_score":0.37675104,"about_ca_system_score_codex":0.0055954726,"about_ca_system_score_gemma":0.009541263,"threshold_uncertainty_score":0.7491162},"labels":[],"label_agreement":null},{"id":"W7083693746","doi":"10.5281/zenodo.17228948","title":"CANADA 🇨🇦, AUSTRALIA 🇦🇺,UK 🇬🇧 WORK VISAS AVAILABLE CALL OR WHATSAPP MR PETER OBENDE ON ☎(08143870581).","year":2025,"lang":"en","type":"other","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Work (physics)","score_opus":0.04164889910352479,"score_gpt":0.22939260243727727,"score_spread":0.18774370333375248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083693746","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.000290257,0.00027037464,0.00037831962,0.0013613871,0.0006201983,0.000049889328,0.0060667186,0.00118791,0.98977506],"genre_scores_gemma":[0.0004346148,0.000082005165,0.00008675268,0.00012795882,0.00001359272,0.0000064449177,0.00081962516,0.0003113291,0.9981177],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9993581,0.000020266509,0.000013478228,0.000102805876,0.00036265576,0.00014270078],"domain_scores_gemma":[0.9976718,0.00010251637,0.000057698417,0.00011443183,0.0011475494,0.0009060366],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.000475538,0.0009831337,0.0006590202,0.00089225714,0.0029380373,0.0035494638,0.001089717,0.00232342,0.86134225],"category_scores_gemma":[0.0016994374,0.00056427467,0.0004239985,0.0015821453,0.00067287206,0.0014464154,0.0014111693,0.0015374135,0.7947037],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002978831,0.000007642782,0.0000823118,0.000046128767,0.0000012210166,0.000016566812,0.000029749617,0.000039223607,0.000154747,0.0011651847,0.9763647,0.022062762],"study_design_scores_gemma":[0.0000051035254,0.000005172511,0.0002930859,0.000023567807,0.0000010834617,0.000010807904,0.000042578828,0.00004849715,0.00008577658,0.00014001553,0.9993406,0.0000037916197],"about_ca_topic_score_codex":0.37675104,"about_ca_topic_score_gemma":0.6127828,"teacher_disagreement_score":0.37675104,"about_ca_system_score_codex":0.0055954726,"about_ca_system_score_gemma":0.009541263,"threshold_uncertainty_score":0.7491162},"labels":[],"label_agreement":null},{"id":"W7083865314","doi":"","title":"4/2: Freshmen All-Americans, Jays trade another veteran, Watson returns","year":2019,"lang":"en","type":"other","venue":"Internet Archive (Internet Archive)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Watson; League; Pillar; Ankle injury; Minor (academic)","score_opus":0.02150952015097898,"score_gpt":0.232739241406278,"score_spread":0.211229721255299,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7083865314","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00388888,0.0004921941,0.0004316097,0.009547294,0.008445879,0.00020999601,0.0009273467,0.0011427486,0.9749141],"genre_scores_gemma":[0.0021356854,0.00012668768,0.000073444025,0.00093013124,0.0002162392,0.000016880595,0.00015520323,0.00013149322,0.9962142],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99954045,0.000023938182,0.000010263609,0.00006560542,0.00016890236,0.00019081972],"domain_scores_gemma":[0.9987626,0.000018116505,0.0000227869,0.00003926825,0.0002807038,0.0008765475],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.00045901877,0.00088955904,0.00038037213,0.0007640087,0.0045726136,0.0044327844,0.0006411441,0.0016524736,0.81723464],"category_scores_gemma":[0.0009681917,0.00045466554,0.00046289386,0.00046880957,0.0005142042,0.002404327,0.002742444,0.0023881793,0.6413799],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025783587,0.00006179661,0.00037669524,0.00001571288,0.0000013548159,0.00006328343,0.00004429695,0.0000103398625,0.00025502636,0.00074949267,0.9803064,0.018089904],"study_design_scores_gemma":[0.000008545552,0.000028316976,0.0013731682,0.000032582167,0.0000012883277,0.00006357318,0.000373656,0.000028363329,0.00010998936,0.00011449961,0.99786013,0.000005920461],"about_ca_topic_score_codex":0.011943563,"about_ca_topic_score_gemma":0.045113444,"teacher_disagreement_score":0.18276536,"about_ca_system_score_codex":0.0010913985,"about_ca_system_score_gemma":0.0018807127,"threshold_uncertainty_score":0.26069254},"labels":[],"label_agreement":null},{"id":"W7084043285","doi":"10.64628/aam.uypqygusa","title":"Impaired on the job or behind the wheel? It’s not just a cannabis problem","year":2019,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Toronto Metropolitan University","funders":"","keywords":"Cannabis; Action (physics); Government (linguistics); Perspective (graphical)","score_opus":0.03902713363416391,"score_gpt":0.2328330947971293,"score_spread":0.1938059611629654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084043285","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.060129568,0.012212243,0.0007097624,0.81912345,0.0073757633,0.000036988517,0.00046365353,0.000075124844,0.09987353],"genre_scores_gemma":[0.613196,0.02257922,0.0011350288,0.2519077,0.0040004295,0.00006111624,0.00039533686,0.00015249562,0.10657264],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99877936,0.00022603126,0.000047103502,0.00008668098,0.00032555952,0.0005352633],"domain_scores_gemma":[0.99657565,0.000435427,0.00028224307,0.00017776081,0.00085290207,0.0016759462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010974078,0.00029151427,0.0005718087,0.00096838415,0.0069155395,0.002977087,0.0009661405,0.0031355273,0.02187235],"category_scores_gemma":[0.007809443,0.0002077543,0.00045133708,0.000883686,0.0082295295,0.0048731393,0.0030837771,0.0067608273,0.0032609534],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042566186,0.0008951792,0.05928706,0.00049884606,0.00017221108,0.007332469,0.015488879,0.00018161433,0.0012008194,0.09755297,0.534177,0.28278726],"study_design_scores_gemma":[0.00013376832,0.0002845917,0.044038218,0.0026679176,0.00011662174,0.0086953025,0.09262471,0.00022754344,0.00076449034,0.08790606,0.7623119,0.00022889633],"about_ca_topic_score_codex":0.08172983,"about_ca_topic_score_gemma":0.1004449,"teacher_disagreement_score":0.08172983,"about_ca_system_score_codex":0.0028752158,"about_ca_system_score_gemma":0.006981169,"threshold_uncertainty_score":0.16250819},"labels":[],"label_agreement":null},{"id":"W7084054764","doi":"10.59350/cam25-azh61","title":"Analysing research funding flows in the Global South","year":2025,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Latin Americans; Global South; South–South cooperation; Research council; Public funding; International relations","score_opus":0.09585328720081955,"score_gpt":0.3499446568386763,"score_spread":0.2540913696378568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084054764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":"incentives","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":"incentives","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7789799,0.008887629,0.002353658,0.032588985,0.00018841327,0.00013895983,0.0067163785,0.00008035738,0.1700657],"genre_scores_gemma":[0.97786796,0.0047944575,0.0020064532,0.00082433195,0.00007167708,0.00019332759,0.0016295994,0.00007178242,0.012540346],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9974112,0.00095739495,0.00018179479,0.00023486317,0.0007418518,0.0004729062],"domain_scores_gemma":[0.99255836,0.0038644637,0.0013414265,0.0004024084,0.0012791818,0.0005541995],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.004201857,0.00020476193,0.00036860068,0.00710378,0.0010270126,0.004905194,0.000367026,0.00074003125,0.008832536],"category_scores_gemma":[0.018326111,0.00022367641,0.00029389324,0.022629859,0.001494182,0.0036328007,0.0044186385,0.0006981219,0.00054736657],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038255035,0.000083420324,0.24342968,0.0015933062,0.00029171447,0.0008179876,0.043072227,0.0048054764,0.0010494927,0.4792712,0.046904832,0.17829822],"study_design_scores_gemma":[0.00011210544,0.00006695902,0.48757195,0.0020038574,0.00020223482,0.00032550158,0.06042608,0.003359025,0.000894173,0.104517885,0.34045637,0.000063943895],"about_ca_topic_score_codex":0.04539053,"about_ca_topic_score_gemma":0.03828953,"teacher_disagreement_score":0.9957982,"about_ca_system_score_codex":0.0075220247,"about_ca_system_score_gemma":0.0075082136,"threshold_uncertainty_score":0.0902527},"labels":[],"label_agreement":null},{"id":"W7084058589","doi":"10.64628/aam.s4u67h4up","title":"How one research project is ‘re-neighbouring’ two Indigenous communities","year":2025,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Indigenous; Traditional knowledge; Work (physics); Government (linguistics)","score_opus":0.13027342914029388,"score_gpt":0.3362506890710277,"score_spread":0.2059772599307338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084058589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.41716528,0.0031874874,0.019895054,0.20944607,0.0047602844,0.0014342462,0.00033162013,0.00044077207,0.34333917],"genre_scores_gemma":[0.8727851,0.0012542545,0.015979655,0.016484024,0.00028359686,0.0010931126,0.00023766942,0.00023784129,0.091644794],"study_design_codex":"qualitative","study_design_gemma":"qualitative","domain_scores_codex":[0.9776379,0.013962954,0.0005520422,0.0020166654,0.0023420874,0.003488392],"domain_scores_gemma":[0.9668163,0.008289413,0.0017603991,0.0065417862,0.0067623053,0.009829849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.021784239,0.0004251435,0.0006113324,0.0014755706,0.021473892,0.0125483,0.0033906745,0.0048159324,0.015003524],"category_scores_gemma":[0.03586407,0.00045041757,0.00052334054,0.0021535216,0.012380414,0.013443419,0.01513891,0.007863229,0.0020583458],"study_design_candidate":"qualitative","study_design_consensus":"qualitative","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003357505,0.0005923337,0.011425977,0.0007370566,0.000108601766,0.0017700522,0.5696927,0.0003286885,0.0051459046,0.22123344,0.038021926,0.15060773],"study_design_scores_gemma":[0.000077999444,0.000323217,0.008881778,0.00070541364,0.000100524645,0.00056668825,0.5271616,0.00027822767,0.0024931538,0.04362217,0.41570133,0.00008788559],"about_ca_topic_score_codex":0.03657093,"about_ca_topic_score_gemma":0.05984738,"teacher_disagreement_score":0.03657093,"about_ca_system_score_codex":0.0077301925,"about_ca_system_score_gemma":0.04567723,"threshold_uncertainty_score":0.115207374},"labels":[],"label_agreement":null},{"id":"W7084068813","doi":"10.6084/m9.figshare.30134872.v2","title":"Identifying Hidden Dangers with Indoor Environmental Testing Services by Built Environments","year":2025,"lang":"en","type":"dataset","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Hazard; Built environment; Quality (philosophy); Hazard analysis; Environmental hazard; Test (biology); Asbestos; Indoor air quality","score_opus":0.02592290705403939,"score_gpt":0.22062551496990646,"score_spread":0.19470260791586708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084068813","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00025840753,0.00008795664,0.000039121078,0.000058196696,0.000018689956,0.0000055109062,0.99909484,0.00009219623,0.00034511855],"genre_scores_gemma":[0.0009252571,0.000070619804,0.00018295909,0.00004832995,0.0000053211206,0.000036641683,0.998381,0.000018826013,0.00033109932],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990189,0.00013440958,0.00014422684,0.00036086314,0.00017190675,0.00016969506],"domain_scores_gemma":[0.9975816,0.00070029055,0.00034083446,0.00044940875,0.0007058718,0.00022190453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000735942,0.0019692492,0.001307835,0.0025833626,0.0008113643,0.0019639782,0.0027739888,0.0027196554,0.03408002],"category_scores_gemma":[0.006194387,0.0005800002,0.001759328,0.0056849825,0.00033940678,0.0013957137,0.0019453012,0.0015890865,0.032352526],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001603733,0.000036240024,0.007589136,0.0014919437,0.00010617034,0.00005944438,0.00003876898,0.0007660283,0.00011854056,0.00045946226,0.98482066,0.0043532415],"study_design_scores_gemma":[0.0005751451,0.00005606644,0.04310184,0.0016226341,0.0002152085,0.00018195764,0.0003282549,0.0021833845,0.0005744237,0.0024770088,0.9485775,0.00010656966],"about_ca_topic_score_codex":0.07910697,"about_ca_topic_score_gemma":0.14764863,"teacher_disagreement_score":0.07910697,"about_ca_system_score_codex":0.0017599737,"about_ca_system_score_gemma":0.0023533101,"threshold_uncertainty_score":0.15729308},"labels":[],"label_agreement":null},{"id":"W7084090425","doi":"10.5040/9798216357025.ch-003","title":"English Provincial Accents: The Midlands, Yorkshire","year":2013,"lang":"en","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Period (music); Stress (linguistics); Population; Quarter (Canadian coin); Feature (linguistics)","score_opus":0.01162346273767019,"score_gpt":0.19590757446819138,"score_spread":0.18428411173052117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084090425","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.015495354,0.0066861077,0.0004569127,0.0029894693,0.0019418587,0.00008514979,0.024508836,0.00024697438,0.9475894],"genre_scores_gemma":[0.05414348,0.0029953478,0.00039675253,0.00037632996,0.00016722089,0.000062468425,0.006796607,0.0003074584,0.93475425],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99981505,0.000017144712,0.000015355514,0.00004118266,0.000057305188,0.000053916523],"domain_scores_gemma":[0.9995359,0.000042139432,0.000029197372,0.000023649578,0.0002683361,0.000100766534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002095288,0.000383674,0.00024609437,0.0008566705,0.0018483422,0.0022084296,0.00030229308,0.00030023683,0.23398423],"category_scores_gemma":[0.0006617794,0.00023016633,0.000086633045,0.0023184007,0.0006607396,0.0012474844,0.0009821109,0.00073436217,0.046891052],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066390625,0.000012238134,0.002718669,0.00026300308,0.0000022933693,0.00017361686,0.0042762854,0.00007752115,0.00080304133,0.013972078,0.93727833,0.04035646],"study_design_scores_gemma":[0.0000050188296,0.0000046835853,0.012926462,0.0000838777,0.0000011135465,0.000049212475,0.0018556812,0.000013999242,0.000089451925,0.00025696235,0.9847074,0.0000062298054],"about_ca_topic_score_codex":0.4969849,"about_ca_topic_score_gemma":0.71394646,"teacher_disagreement_score":0.4969849,"about_ca_system_score_codex":0.002692083,"about_ca_system_score_gemma":0.0027272177,"threshold_uncertainty_score":0.9881843},"labels":[],"label_agreement":null},{"id":"W7084100105","doi":"10.64628/aam.y5uuhqurk","title":"Underwater Arctic forests are expanding with rapid warming","year":2019,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"","keywords":"Arctic; Underwater; The arctic; Climate change","score_opus":0.017818641167511938,"score_gpt":0.21015032529681169,"score_spread":0.19233168412929974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084100105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8363727,0.008388929,0.003617977,0.0076744296,0.0012908787,0.000023937577,0.0038237134,0.00029865312,0.13850887],"genre_scores_gemma":[0.981282,0.0064647854,0.0013083708,0.0006755416,0.00047421854,0.000013781731,0.0011364683,0.000061227816,0.008583651],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998306,0.000018882982,0.000008639004,0.000034169814,0.000052522806,0.000055112712],"domain_scores_gemma":[0.999387,0.00006325973,0.00013955864,0.00004680718,0.00026695034,0.00009638987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004515271,0.00034197234,0.00021109408,0.00097603415,0.0014576821,0.0020686905,0.00024808955,0.00046018237,0.008820618],"category_scores_gemma":[0.0010581445,0.000112268775,0.00023851328,0.0016379529,0.00067640055,0.0014105062,0.00091815856,0.00066084915,0.0011137478],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044992912,0.000113037706,0.56889105,0.0008371694,0.00024822223,0.001536717,0.0040004877,0.008111263,0.015244749,0.023035044,0.03467491,0.34285745],"study_design_scores_gemma":[0.000008790861,0.00006523702,0.77311766,0.00019147327,0.000079628924,0.00036010833,0.009647808,0.001296228,0.0015507553,0.0039981348,0.20965743,0.000026655209],"about_ca_topic_score_codex":0.06496372,"about_ca_topic_score_gemma":0.12696238,"teacher_disagreement_score":0.06496372,"about_ca_system_score_codex":0.001266179,"about_ca_system_score_gemma":0.0015188515,"threshold_uncertainty_score":0.1291712},"labels":[],"label_agreement":null},{"id":"W7084114558","doi":"10.6084/m9.figshare.29955787.v1","title":"Additional file 2 of The ocular surface microbiome of rhesus macaques","year":2025,"lang":"en","type":"article","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Microbiome; Rhesus macaque; Immune system; Isolation (microbiology)","score_opus":0.01287256962132349,"score_gpt":0.19477336353124974,"score_spread":0.18190079390992625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084114558","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00056520395,0.00002515502,0.00018353372,0.00007816513,0.000028005239,0.000048475824,0.99780244,0.00018079343,0.001088282],"genre_scores_gemma":[0.017516555,0.00022930927,0.00531848,0.00081796315,0.00013922031,0.0017795583,0.95676255,0.0007796641,0.016656594],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9997291,0.000039324434,0.000039169176,0.000077492135,0.000056280303,0.00005866083],"domain_scores_gemma":[0.992419,0.0052947705,0.00052415684,0.00057003,0.0008682525,0.00032378692],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0006008888,0.00073344214,0.0008014457,0.0020440037,0.00090940547,0.0012350461,0.0011604042,0.0010841629,0.85305774],"category_scores_gemma":[0.01335584,0.00034544794,0.00057346275,0.00232845,0.00021756164,0.00095538923,0.000944269,0.00051794515,0.12425859],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035940064,0.00014235674,0.0067367004,0.002476322,0.00006990381,0.00012960701,0.00015137735,0.0003223097,0.00040159133,0.00083939993,0.97195417,0.016416958],"study_design_scores_gemma":[0.0027769322,0.0003987183,0.10825378,0.0033846525,0.00025538393,0.0012554456,0.001048661,0.001512952,0.001314594,0.013909744,0.8656878,0.00020128895],"about_ca_topic_score_codex":0.010631294,"about_ca_topic_score_gemma":0.01676997,"teacher_disagreement_score":0.85305774,"about_ca_system_score_codex":0.0004733938,"about_ca_system_score_gemma":0.0009810985,"threshold_uncertainty_score":0.2095952},"labels":[],"label_agreement":null},{"id":"W7084117547","doi":"10.6084/m9.figshare.29993008.v1","title":"Additional file 3 of Structural brain differences in school-aged children who are HIV-exposed uninfected","year":2025,"lang":"en","type":"dataset","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Women's College Hospital; Toronto General Hospital; SickKids Foundation; University of Toronto; Children's Hospital of Eastern Ontario; University of Ottawa; Hospital for Sick Children","funders":"","keywords":"Table (database); Brain size; Population; Volume (thermodynamics); Statistical analysis","score_opus":0.016267146513063147,"score_gpt":0.20607444597277289,"score_spread":0.18980729945970973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084117547","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00011908367,0.000010600529,0.00004046135,0.000027617252,0.0000051938114,0.000015505679,0.99954283,0.000033186185,0.0002055567],"genre_scores_gemma":[0.0042769257,0.000070346694,0.0006345898,0.00016996688,0.000033379787,0.00079986826,0.9911946,0.0001350996,0.0026850523],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9993795,0.00010030993,0.000117745556,0.00018627875,0.000102936,0.00011324495],"domain_scores_gemma":[0.9921894,0.004585168,0.0008859063,0.0007374502,0.0012859796,0.0003161807],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0011975813,0.0012897551,0.0012218487,0.0019945418,0.00087923626,0.0015962085,0.0022985372,0.0016866351,0.6097233],"category_scores_gemma":[0.019795954,0.0006823539,0.0012320646,0.004185017,0.0002714125,0.0015823194,0.001450224,0.0011534876,0.07999053],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024825233,0.000047110756,0.006742717,0.0015738511,0.000097043056,0.000054348347,0.000054828644,0.00036701845,0.000047300193,0.0005608759,0.98655826,0.0036483963],"study_design_scores_gemma":[0.006543502,0.00026001286,0.13966367,0.0053571276,0.00058467983,0.000764404,0.0007545397,0.0019159755,0.00058772886,0.010515062,0.83286655,0.00018682],"about_ca_topic_score_codex":0.030397842,"about_ca_topic_score_gemma":0.04530775,"teacher_disagreement_score":0.6097233,"about_ca_system_score_codex":0.0012183674,"about_ca_system_score_gemma":0.0016336371,"threshold_uncertainty_score":0.5566823},"labels":[],"label_agreement":null},{"id":"W7084130305","doi":"10.36926/editorainovar-978-65-5388-337-6_007","title":"CONFERE, CONFIRMA E CUIDA: UMA NOVA ROTINA NA SALA DE MEDICAÇÃO","year":2024,"lang":"pt","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subject (documents); Interval (graph theory); Nobility; Predestination","score_opus":0.04858310558060265,"score_gpt":0.255869087595731,"score_spread":0.20728598201512838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084130305","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.011679629,0.13251734,0.005435938,0.59581125,0.01703108,0.000093680086,0.00015482915,0.0002409927,0.23703527],"genre_scores_gemma":[0.26313037,0.112274446,0.009060373,0.1265584,0.0117121395,0.0001628499,0.00019801855,0.0005193395,0.476384],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.98928994,0.006943093,0.00044617007,0.00070555357,0.0021119798,0.000503312],"domain_scores_gemma":[0.98655546,0.006530578,0.00086067885,0.0012748535,0.002110644,0.0026677619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0056214225,0.0006101618,0.00077111245,0.0015339346,0.0065026274,0.0134526165,0.001716738,0.0052078264,0.020240432],"category_scores_gemma":[0.018726792,0.000507341,0.0006479106,0.0015116127,0.017041028,0.008384393,0.007901911,0.007880881,0.0049077664],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009482861,0.0001297509,0.0027798773,0.0011603923,0.000041582003,0.0010704991,0.047115237,0.00019034442,0.0009415785,0.25689113,0.45952004,0.23006473],"study_design_scores_gemma":[0.000009357438,0.0000567458,0.0009070185,0.00076657336,0.000010161259,0.000664019,0.0066665676,0.00006918954,0.00015177349,0.01740833,0.97326905,0.000021268761],"about_ca_topic_score_codex":0.0078891255,"about_ca_topic_score_gemma":0.0136033455,"teacher_disagreement_score":0.020240432,"about_ca_system_score_codex":0.007011434,"about_ca_system_score_gemma":0.013334298,"threshold_uncertainty_score":0.067710996},"labels":[],"label_agreement":null},{"id":"W7084137781","doi":"10.64628/aam.yh9hedc9w","title":"Canada must change the law that bans sexual assault survivors from revealing their own identities","year":2021,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Toronto Metropolitan University","funders":"","keywords":"Sexual assault; Legislation; Sexual abuse; Poison control; Sexual violence; Homicide; Law enforcement; Government (linguistics)","score_opus":0.05059446241649413,"score_gpt":0.20576615929077843,"score_spread":0.1551716968742843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084137781","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.03681403,0.001498702,0.0035171371,0.6916031,0.009923781,0.0007902117,0.0013939776,0.0005468904,0.25391215],"genre_scores_gemma":[0.107272476,0.0015840626,0.004964724,0.6092061,0.0006886477,0.0002952744,0.00053739554,0.00020006036,0.27525124],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.98326725,0.0011360372,0.0006541237,0.0008349309,0.008760042,0.0053475876],"domain_scores_gemma":[0.9336801,0.011913749,0.0014605963,0.002723908,0.034369837,0.015851773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.008463699,0.00044869655,0.0009278764,0.0021021403,0.01775392,0.0077972673,0.005144983,0.024536425,0.016255349],"category_scores_gemma":[0.03999695,0.0012679924,0.0011589244,0.0019129853,0.007174239,0.0033293257,0.003180799,0.019429535,0.002508991],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093620445,0.00029187876,0.01372528,0.00017092409,0.000081240556,0.00066417747,0.003636216,0.00050731015,0.0014629138,0.12578905,0.8229249,0.030652449],"study_design_scores_gemma":[0.00014418077,0.00007400785,0.020299336,0.0004269862,0.00011713042,0.00021986348,0.005397477,0.00056762533,0.0012180037,0.00873505,0.9625942,0.00020610935],"about_ca_topic_score_codex":0.98406684,"about_ca_topic_score_gemma":0.99407345,"teacher_disagreement_score":0.049807705,"about_ca_system_score_codex":0.049807705,"about_ca_system_score_gemma":0.378778,"threshold_uncertainty_score":0.3613819},"labels":[],"label_agreement":null},{"id":"W7084139615","doi":"10.6084/m9.figshare.29999126","title":"Additional file 2 of Pre-diagnostic serum metabolome and breast cancer risk: a nested case-control study","year":2025,"lang":"en","type":"dataset","venue":"Figshare","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Alberta Health Services; University of British Columbia","funders":"","keywords":"Breast cancer; Metabolome; Cancer; BRCA2 Protein; MEDLINE","score_opus":0.010794088964983507,"score_gpt":0.2260168689112642,"score_spread":0.2152227799462807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084139615","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00020618974,0.00001915458,0.00006978712,0.000029603914,0.000009506271,0.000034206314,0.99942017,0.00004918827,0.00016221058],"genre_scores_gemma":[0.0053166226,0.0000864921,0.0012389298,0.00034432102,0.000044099655,0.0014445924,0.98787373,0.00023745814,0.0034137897],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.9987446,0.00022429721,0.00021491542,0.00043044204,0.0001631078,0.00022255468],"domain_scores_gemma":[0.9854585,0.009115116,0.0014569166,0.0017916824,0.0013744264,0.0008033383],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.0021161998,0.0019961607,0.002339389,0.0032485283,0.0011700406,0.002903804,0.0028423935,0.0027821271,0.6209351],"category_scores_gemma":[0.022895489,0.0012429369,0.0028921403,0.0051255887,0.0006172951,0.0014460345,0.0018634684,0.0012511946,0.09421183],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014378434,0.0002340844,0.014877871,0.004727014,0.00069146365,0.00017379259,0.00011833768,0.0012542767,0.00022064768,0.0008741646,0.9699602,0.0054303845],"study_design_scores_gemma":[0.026176121,0.0007275062,0.12851922,0.0049174926,0.002385666,0.0011021527,0.0007159619,0.003829603,0.0010360588,0.013985528,0.8162204,0.00038433447],"about_ca_topic_score_codex":0.020019034,"about_ca_topic_score_gemma":0.02980237,"teacher_disagreement_score":0.6209351,"about_ca_system_score_codex":0.0014627255,"about_ca_system_score_gemma":0.002914264,"threshold_uncertainty_score":0.54069006},"labels":[],"label_agreement":null},{"id":"W7084151694","doi":"10.64628/ade.h74wt4hrk","title":"Como os nossos cães se conectam emocionalmente conosco e como melhorar essa sintonia com eles","year":2025,"lang":"pt","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Sequence (biology); Disease; Perspective (graphical); Identification (biology)","score_opus":0.02175629916914491,"score_gpt":0.26239346476065756,"score_spread":0.24063716559151266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084151694","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20583569,0.0010730518,0.02096939,0.016745435,0.0027372243,0.00014059908,0.00040288558,0.0005098889,0.7515859],"genre_scores_gemma":[0.6705844,0.001047178,0.0105683105,0.0028192038,0.00052188913,0.000063738065,0.00023784616,0.00026193488,0.31389552],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99899846,0.00031107,0.000052291252,0.00015520449,0.00029446933,0.00018845641],"domain_scores_gemma":[0.9962788,0.000811471,0.0005133583,0.0006614042,0.0010953355,0.000639568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091929483,0.00028088046,0.00017649135,0.0005369938,0.0021475898,0.0029919567,0.0006233467,0.0008535994,0.026404783],"category_scores_gemma":[0.0067398776,0.00018722082,0.00026453857,0.00052158185,0.0021447265,0.001415481,0.0018727455,0.0012474592,0.005678563],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035912477,0.00032988098,0.07221384,0.00055580627,0.00006130231,0.005183647,0.063454255,0.0007590902,0.02967321,0.4186919,0.09128285,0.3174351],"study_design_scores_gemma":[0.000020998863,0.00021583226,0.03238596,0.0003876212,0.0000674833,0.002544482,0.05851551,0.0008147243,0.007768977,0.01987373,0.8773476,0.00005708943],"about_ca_topic_score_codex":0.0043321764,"about_ca_topic_score_gemma":0.012550332,"teacher_disagreement_score":0.026404783,"about_ca_system_score_codex":0.0009326044,"about_ca_system_score_gemma":0.002226943,"threshold_uncertainty_score":0.08833277},"labels":[],"label_agreement":null},{"id":"W7084395169","doi":"10.82231/tk1z-6e49","title":"Understanding the Manitoba Election 2016: Campaigns, Participation, Issues, Place","year":2025,"lang":"en","type":"book","venue":"UMANMANIFOLD","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Field (mathematics); Work (physics); Agency (philosophy)","score_opus":0.06114712810408748,"score_gpt":0.2513447627122864,"score_spread":0.1901976346081989,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084395169","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.12744014,0.017664207,0.0028282816,0.19423315,0.0020807101,0.00007403737,0.002540567,0.00011320974,0.6530257],"genre_scores_gemma":[0.66382396,0.015669202,0.0016695978,0.006478678,0.0005939949,0.000115713425,0.0017678157,0.00015506141,0.309726],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9995833,0.00014205152,0.000008982316,0.00004003134,0.0000694378,0.00015620884],"domain_scores_gemma":[0.9990778,0.0002813679,0.00010519486,0.00003514103,0.00020329661,0.0002972387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013025147,0.0004660013,0.00023959157,0.0012159873,0.0049962928,0.00817789,0.0009676439,0.0015822372,0.01654973],"category_scores_gemma":[0.003057564,0.0003776201,0.00024946814,0.0032034484,0.003415352,0.0057386365,0.0023502235,0.0027417252,0.0014803762],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039482584,0.00006873268,0.026795989,0.000259264,0.000021973776,0.00032615347,0.12806876,0.0011508677,0.00023084368,0.46838474,0.28385285,0.090800345],"study_design_scores_gemma":[0.000006424262,0.000010286462,0.041794855,0.00082680705,0.000013705222,0.00010158892,0.17935097,0.0009099875,0.00014031083,0.06363708,0.71318376,0.00002426781],"about_ca_topic_score_codex":0.6911948,"about_ca_topic_score_gemma":0.86552054,"teacher_disagreement_score":0.30880523,"about_ca_system_score_codex":0.014757989,"about_ca_system_score_gemma":0.033476803,"threshold_uncertainty_score":0.62124765},"labels":[],"label_agreement":null},{"id":"W7084621102","doi":"10.1362/147539225x17573317988832","title":"<i>Logarithm</i>: A Cinematic Exploration of Time","year":2025,"lang":"he","type":"article","venue":"Journal of Customer Behaviour","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"","score_opus":0.02268427913869221,"score_gpt":0.26394890589786635,"score_spread":0.24126462675917415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7084621102","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.024702497,0.008398946,0.020260427,0.072948776,0.009702207,0.000060396105,0.001847672,0.0009533028,0.8611257],"genre_scores_gemma":[0.6949357,0.007066831,0.019556923,0.009317131,0.017744472,0.00010184057,0.0009572462,0.0013734573,0.24894638],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99990034,0.000045690438,0.000003084418,0.000011138868,0.000024822848,0.000014969244],"domain_scores_gemma":[0.99920636,0.0004887238,0.000042899646,0.000046735433,0.00010536042,0.00010985871],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037707546,0.00050999946,0.00011208042,0.0012994807,0.0011602184,0.0038765895,0.00059085846,0.00059595803,0.029203465],"category_scores_gemma":[0.002204987,0.00010910521,0.00016915395,0.0011515861,0.0019107024,0.003994345,0.0007295113,0.0016214293,0.0018697316],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001131458,0.00002686298,0.0009032474,0.00022892446,0.00001063566,0.00031332337,0.021930374,0.00031757777,0.0026808928,0.35118547,0.57492614,0.047363475],"study_design_scores_gemma":[0.0000074649897,0.000018173681,0.0022780977,0.00013709484,0.000006869408,0.0002562278,0.0071083666,0.0009917977,0.0005328284,0.023178568,0.96546835,0.000016115522],"about_ca_topic_score_codex":0.0049642962,"about_ca_topic_score_gemma":0.0088591585,"teacher_disagreement_score":0.029203465,"about_ca_system_score_codex":0.00081104704,"about_ca_system_score_gemma":0.00038834513,"threshold_uncertainty_score":0.09769535},"labels":[],"label_agreement":null},{"id":"W7088306182","doi":"10.5281/zenodo.17327479","title":"Pentagonica picticornis Bates 1883","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"BATES; Plenum space; Confusion","score_opus":0.02587367055831288,"score_gpt":0.22979476214979516,"score_spread":0.20392109159148228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7088306182","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.066067085,0.014541139,0.0020581803,0.000811086,0.00065230357,0.00032543732,0.008858769,0.00066883175,0.9060171],"genre_scores_gemma":[0.83575207,0.010228486,0.0044950885,0.0009864516,0.0003642093,0.00030352717,0.011628058,0.00017822011,0.1360639],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.999814,0.00001484419,0.00000913654,0.00005664117,0.00008084756,0.000024530902],"domain_scores_gemma":[0.9997942,0.000021190106,0.000067621324,0.000018261857,0.00007961359,0.000019165844],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010639579,0.00045981712,0.00029778152,0.001282389,0.001697408,0.00048786617,0.00042901887,0.0004204802,0.026306607],"category_scores_gemma":[0.00027919843,0.00027235266,0.00014872073,0.0017759773,0.00079363456,0.00054943364,0.00045670648,0.0008248024,0.010075066],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048081836,0.00009372835,0.046491142,0.0010750149,0.00006775774,0.0024955105,0.0041954084,0.0011720967,0.01021457,0.009210559,0.18011774,0.7443856],"study_design_scores_gemma":[0.000019527777,0.000046013927,0.17193204,0.0002354407,0.00003194181,0.0021468014,0.00089079014,0.00014508041,0.0005059074,0.0005670024,0.82346547,0.000014118024],"about_ca_topic_score_codex":0.07828652,"about_ca_topic_score_gemma":0.1662031,"teacher_disagreement_score":0.07828652,"about_ca_system_score_codex":0.001170238,"about_ca_system_score_gemma":0.0006088345,"threshold_uncertainty_score":0.1556617},"labels":[],"label_agreement":null},{"id":"W7088563405","doi":"10.5281/zenodo.17327441","title":"Stenolophus (Stenolophus) limbalis LeConte 1857","year":2025,"lang":"en","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Government (linguistics); Context (archaeology); Subject (documents); Period (music)","score_opus":0.028424164053831868,"score_gpt":0.22542896436367327,"score_spread":0.1970048003098414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7088563405","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5473884,0.005003978,0.004951433,0.00049308635,0.00029678352,0.0002585948,0.007895588,0.00047581233,0.43323636],"genre_scores_gemma":[0.9434277,0.001344388,0.0020634837,0.00024445687,0.00008537483,0.00006529449,0.003942303,0.000029729239,0.048797403],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99991286,0.0000068594945,0.0000061747965,0.000023829709,0.000031521493,0.000018722947],"domain_scores_gemma":[0.9999329,0.000010479259,0.00002322543,0.0000044422018,0.00001907981,0.000009893502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000797599,0.000349326,0.00020345685,0.0011173615,0.0011796756,0.00031239743,0.0002403159,0.0002541278,0.010429484],"category_scores_gemma":[0.00017863253,0.00010849827,0.0001052586,0.00066908833,0.0005276519,0.0005359016,0.0005512578,0.00024696218,0.0043626637],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007780368,0.00014262852,0.11114175,0.00083160726,0.00008140256,0.0033567238,0.0023977428,0.0012976639,0.06386384,0.005556723,0.044980735,0.7655711],"study_design_scores_gemma":[0.00004444979,0.00021800412,0.7471023,0.00023782131,0.000055401175,0.004067112,0.0011745067,0.00060424366,0.0045739617,0.0009121858,0.2409766,0.000033403267],"about_ca_topic_score_codex":0.037687216,"about_ca_topic_score_gemma":0.095752515,"teacher_disagreement_score":0.037687216,"about_ca_system_score_codex":0.00084768166,"about_ca_system_score_gemma":0.0003306794,"threshold_uncertainty_score":0.074935675},"labels":[],"label_agreement":null},{"id":"W7090618821","doi":"","title":"Real-Time Semantic Segmentation of Aerial Images Using an Embedded U-Net: A Comparison of CPU, GPU, and FPGA Workflows","year":2024,"lang":"en","type":"article","venue":"HAL (Le Centre pour la Communication Scientifique Directe)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"Agence Nationale de la Recherche","keywords":"Segmentation; Workflow; Field-programmable gate array; Image segmentation; Image (mathematics); Key (lock)","score_opus":0.020461749045691376,"score_gpt":0.25667865127996103,"score_spread":0.23621690223426967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7090618821","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.42293015,0.001337643,0.5285552,0.0003600195,0.00029205944,0.00028129944,0.0018565669,0.031562667,0.01282441],"genre_scores_gemma":[0.58733255,0.00058244454,0.4026159,0.00014081663,0.000030347415,0.000069294554,0.0020162319,0.0014347195,0.0057776533],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99980074,0.000024267874,0.000014936838,0.000061200335,0.00005735461,0.000041543437],"domain_scores_gemma":[0.999689,0.00011309942,0.000020605874,0.000047596677,0.00009283787,0.000036871385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003563569,0.00059371407,0.0005201701,0.0009657071,0.00034878575,0.001434271,0.00082002976,0.0005890861,0.0057034595],"category_scores_gemma":[0.00073255325,0.0003202891,0.00037416213,0.0009312672,0.0001979991,0.0004899248,0.00034732893,0.0002549804,0.001194214],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0031411396,0.00026516235,0.0032887026,0.0006368419,0.00018266545,0.00046245023,0.00026714368,0.08197594,0.13082261,0.0024567856,0.01072645,0.76577425],"study_design_scores_gemma":[0.0001275826,0.00024682135,0.005983379,0.000051634677,0.00007774574,0.00038153824,0.0002367874,0.9044867,0.07713597,0.0015925417,0.009638921,0.000040348154],"about_ca_topic_score_codex":0.010402491,"about_ca_topic_score_gemma":0.017134426,"teacher_disagreement_score":0.010402491,"about_ca_system_score_codex":0.0005760311,"about_ca_system_score_gemma":0.00096906663,"threshold_uncertainty_score":0.020683885},"labels":[],"label_agreement":null},{"id":"W7092499443","doi":"10.5281/zenodo.17392133","title":"Métadonnées — Art de scénariser malgré la censure, ou l'usage de lettres et de l'art dans les séries historiques chinoises Harem : biographie de Zhen Huan (2011) et Rêve de la prospérité (2022)","year":2025,"lang":"fr","type":"dataset","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal","funders":"","keywords":"Harem; The arts; Cultural exchange","score_opus":0.02299438604081748,"score_gpt":0.2500848504210644,"score_spread":0.22709046438024688,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7092499443","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0045015397,0.00056828,0.00015312045,0.0002044711,0.000097068245,0.000023796287,0.9880094,0.00016230144,0.006279956],"genre_scores_gemma":[0.0105052,0.0004992652,0.00048637594,0.00006880709,0.000053375094,0.00013977228,0.9781812,0.00006178271,0.010004223],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9995173,0.00006555781,0.000050918232,0.00010569043,0.0001383097,0.00012226954],"domain_scores_gemma":[0.9986613,0.00032481772,0.00025628292,0.00024067078,0.00038168617,0.00013518457],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000479587,0.0007364384,0.0003802909,0.005069302,0.00081418,0.0015007829,0.00090398325,0.0006051496,0.022456598],"category_scores_gemma":[0.0027148242,0.00024801906,0.00042379,0.008323057,0.0004553708,0.0010142167,0.0012021506,0.0008036122,0.0099810865],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009024858,0.000014480799,0.011528283,0.0009997756,0.000029181661,0.00007467913,0.00093766826,0.00016164708,0.00038266004,0.003210363,0.96604574,0.01652527],"study_design_scores_gemma":[0.000018401242,0.0000058739247,0.07141165,0.00022400593,0.000012135044,0.00005055603,0.00087980705,0.000113582195,0.00025501288,0.0004101689,0.9266032,0.000015614847],"about_ca_topic_score_codex":0.15941136,"about_ca_topic_score_gemma":0.3188093,"teacher_disagreement_score":0.15941136,"about_ca_system_score_codex":0.0022156294,"about_ca_system_score_gemma":0.0028962754,"threshold_uncertainty_score":0.316967},"labels":[],"label_agreement":null},{"id":"W7095729033","doi":"","title":"Commentary Commentaire Table of Contents","year":2000,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Relation (database); Table of contents; Table (database); Dissection (medical); Association (psychology)","score_opus":0.019445637963646397,"score_gpt":0.21725026083970714,"score_spread":0.19780462287606074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7095729033","genre_codex":"commentary","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00012302147,0.0015709939,0.00005512602,0.8422221,0.14972442,0.000045070014,0.0003287748,0.000033154385,0.0058973297],"genre_scores_gemma":[0.0007562853,0.0006889531,0.000046838933,0.94372326,0.043489672,0.000075598924,0.00007256846,0.000023452958,0.01112343],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9896807,0.0014213116,0.0011335792,0.0014043149,0.0041252994,0.0022349115],"domain_scores_gemma":[0.95275426,0.024456933,0.0022500257,0.0012697901,0.015746094,0.0035228312],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.008633283,0.0016375678,0.002512828,0.0031557726,0.009356288,0.0063094385,0.006819784,0.10055147,0.047610797],"category_scores_gemma":[0.079462856,0.001786704,0.004283676,0.0023404453,0.004112901,0.0038118607,0.0033180425,0.056362867,0.022242347],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015518632,0.000003909355,0.0000699658,0.000049325776,0.0000073323486,0.00010074335,0.000042773845,0.000010320565,0.000014789281,0.00044722995,0.99844766,0.00079043035],"study_design_scores_gemma":[0.00009093739,0.000012824172,0.000761122,0.0007690942,0.00006853378,0.00016053891,0.0003079099,0.000058004993,0.00010382039,0.0013911444,0.9962274,0.000048689206],"about_ca_topic_score_codex":0.11822099,"about_ca_topic_score_gemma":0.14905176,"teacher_disagreement_score":0.9523892,"about_ca_system_score_codex":0.017154554,"about_ca_system_score_gemma":0.02364198,"threshold_uncertainty_score":0.2350657},"labels":[],"label_agreement":null},{"id":"W7095799566","doi":"","title":"TELESEISMIC AND NEAR-FIELD ANALYSIS OF THE NAHANNI EARTHQUAKES IN THE NORTHWEST TERRITORIES, CANADA","year":2008,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Aftershock; Epicenter; Fault (geology); Foreshock; Focal mechanism; Fault plane; Seismic zone","score_opus":0.010297493406487552,"score_gpt":0.18390163682602526,"score_spread":0.1736041434195377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7095799566","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99554294,0.00022364536,0.00015778017,0.00008173335,0.000003943069,0.000010704592,0.0018559577,0.000007296662,0.002116071],"genre_scores_gemma":[0.99496377,0.0003274029,0.00035431466,0.000018406485,0.0000037394186,0.0000054399916,0.0022704732,0.0000051343654,0.002051185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998129,0.000012620346,0.000011558682,0.000030457804,0.000066675406,0.00006586953],"domain_scores_gemma":[0.9993007,0.000034861736,0.000070928625,0.000018408076,0.00045499922,0.000120218814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020545756,0.00017194364,0.00018530949,0.0017871215,0.0009826284,0.00055771525,0.00039436785,0.00015500824,0.0012621647],"category_scores_gemma":[0.00093248714,0.00017120205,0.00014041208,0.0028629696,0.00031966926,0.0002268192,0.00036008627,0.00015002083,0.00016441732],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013447092,0.00007902447,0.94544935,0.00007016085,0.000121261764,0.00045809476,0.0011737015,0.004486853,0.003691126,0.0010425244,0.0025313322,0.04076205],"study_design_scores_gemma":[0.000003064707,0.0000056961294,0.99629337,0.000007278377,0.000012101931,0.00003096724,0.00088116346,0.0013786008,0.0001620668,0.000030312462,0.0011883585,0.0000070575943],"about_ca_topic_score_codex":0.9919566,"about_ca_topic_score_gemma":0.99717474,"teacher_disagreement_score":0.011000812,"about_ca_system_score_codex":0.011000812,"about_ca_system_score_gemma":0.009020122,"threshold_uncertainty_score":0.07981688},"labels":[],"label_agreement":null},{"id":"W7096013135","doi":"","title":"Canadian Journal of Counselling / Revue canadienne de counseling/2006, Vol. 40:4 209 Alliance Skill Development within Canadian First Nations and Aboriginal Counsellor Education","year":2016,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Alliance; Plan (archaeology); Foundation (evidence); Process (computing)","score_opus":0.007717673349219938,"score_gpt":0.19977057210618898,"score_spread":0.19205289875696904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7096013135","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.022806471,0.28038967,0.0016142844,0.16887873,0.0061205155,0.0001433836,0.000316188,0.00020084222,0.51952994],"genre_scores_gemma":[0.4784063,0.22478023,0.0038534438,0.021835815,0.0013490078,0.00017984088,0.00038257646,0.0001578228,0.26905498],"study_design_codex":"not_applicable","study_design_gemma":"qualitative","domain_scores_codex":[0.99659413,0.0008506011,0.0000961878,0.00022885586,0.0015235728,0.00070662994],"domain_scores_gemma":[0.995333,0.0007025688,0.00016540659,0.000186702,0.0015410379,0.0020712088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033506418,0.0005382731,0.0005077426,0.002299305,0.0118728345,0.006090316,0.0019729768,0.0037862218,0.05674462],"category_scores_gemma":[0.0073950677,0.00038370746,0.00032978153,0.003485714,0.007532907,0.0015503576,0.0038646536,0.0036619476,0.0041178823],"study_design_candidate":"qualitative","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046468427,0.0002025477,0.01114048,0.0015809787,0.0000372482,0.0012204064,0.023025578,0.0003782406,0.00039368795,0.08700058,0.5761561,0.2988177],"study_design_scores_gemma":[0.0000063991138,0.00001643263,0.0136831105,0.0014963272,0.000012094473,0.0009120999,0.013926484,0.00010341504,0.000084746716,0.0035933147,0.96613395,0.00003165419],"about_ca_topic_score_codex":0.8496363,"about_ca_topic_score_gemma":0.92110556,"teacher_disagreement_score":0.15036368,"about_ca_system_score_codex":0.041216996,"about_ca_system_score_gemma":0.10230466,"threshold_uncertainty_score":0.3024984},"labels":[],"label_agreement":null},{"id":"W7097201321","doi":"","title":"Abstract Basement-controlled faulting of Paleozoic strata in southern Ontario, Canada: new evidence from geophysical","year":2000,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Paleozoic; Fault (geology); Paleomagnetism; Seismic tomography","score_opus":0.02032255174304644,"score_gpt":0.20574921243627578,"score_spread":0.18542666069322933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7097201321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909492,0.00040518513,0.00014798097,0.00012516917,0.0000034047944,0.000017540533,0.0012341632,0.0000063129482,0.007111061],"genre_scores_gemma":[0.99751955,0.00033783028,0.00016116665,0.000026178435,0.0000016030639,0.000004890115,0.00033630902,0.0000033336055,0.0016091948],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997491,0.000013522958,0.000014083312,0.000040503095,0.00009108991,0.00009175349],"domain_scores_gemma":[0.9983223,0.000081061364,0.00030177349,0.00007408181,0.0010603429,0.0001603369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022455955,0.0001624908,0.00018334526,0.0018451053,0.002383603,0.0015932734,0.0006411032,0.0002780678,0.0023477382],"category_scores_gemma":[0.0018151263,0.0002287096,0.00011190101,0.003823025,0.0013132959,0.0003604694,0.00066953007,0.0002712472,0.00019219084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008943053,0.000015301684,0.9728205,0.00009005925,0.000032713306,0.00014981595,0.005673483,0.0004838475,0.0057159252,0.000885388,0.00057604205,0.01346745],"study_design_scores_gemma":[0.000002479776,0.0000047734743,0.996905,0.000019784653,0.000007687143,0.000025242096,0.001523323,0.00006801445,0.00018130684,0.00006653318,0.0011927453,0.0000030906667],"about_ca_topic_score_codex":0.9928281,"about_ca_topic_score_gemma":0.99848336,"teacher_disagreement_score":0.011933017,"about_ca_system_score_codex":0.011933017,"about_ca_system_score_gemma":0.0140130725,"threshold_uncertainty_score":0.086580455},"labels":[],"label_agreement":null},{"id":"W7097635856","doi":"","title":"Published by Canadian","year":2016,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Induced seismicity; Earthquake prediction; Foreshock; Series (stratigraphy); Seismic microzonation; Earthquake swarm; Types of earthquake","score_opus":0.008808714816132941,"score_gpt":0.1741825306679467,"score_spread":0.16537381585181377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7097635856","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005441217,0.00097445777,0.00041906914,0.0019782346,0.0013530813,0.000053263317,0.0036402603,0.00050539314,0.99053204],"genre_scores_gemma":[0.0012403767,0.00051166036,0.0002680899,0.0002999557,0.0000564794,0.000010693367,0.000834971,0.0001805699,0.99659723],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9989812,0.000058842546,0.00006163883,0.0003358341,0.00041199895,0.00015037482],"domain_scores_gemma":[0.9973105,0.00017485922,0.00008038045,0.0006300226,0.001366841,0.00043736346],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0008128359,0.0010894269,0.00088808115,0.0025758152,0.00419044,0.009353053,0.001321281,0.002733702,0.86123216],"category_scores_gemma":[0.0031316408,0.0006984683,0.00059753895,0.003673898,0.00181713,0.0027987729,0.003056782,0.0018715924,0.77950436],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057656613,0.00004623116,0.0010309075,0.00024032252,0.000009584513,0.0002634917,0.00022963663,0.00014140975,0.0009239656,0.020136703,0.82654464,0.15037544],"study_design_scores_gemma":[0.0000019128045,0.0000026532684,0.0004605998,0.000046858797,8.654851e-7,0.00004664029,0.000067798996,0.00002079894,0.00006705993,0.00028339762,0.99899787,0.0000035676774],"about_ca_topic_score_codex":0.10417385,"about_ca_topic_score_gemma":0.17315567,"teacher_disagreement_score":0.13876784,"about_ca_system_score_codex":0.005122881,"about_ca_system_score_gemma":0.010574844,"threshold_uncertainty_score":0.20713496},"labels":[],"label_agreement":null},{"id":"W7097752087","doi":"","title":"GEOSCIENCE CANADA SERIES International Year of Planet Earth 7. Oceans: Submarine Land- slides and Consequent","year":2016,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Landslide; Submarine landslide; Continental margin; Submarine; Margin (machine learning); Continental shelf; Series (stratigraphy); Planet","score_opus":0.009331708271841434,"score_gpt":0.17881144225633774,"score_spread":0.1694797339844963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7097752087","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0009913681,0.0074927043,0.0016657999,0.003474405,0.015631625,0.00021108521,0.39764547,0.0022911367,0.5705964],"genre_scores_gemma":[0.013182154,0.020812213,0.0034682453,0.001027008,0.0018481405,0.00018436293,0.34385905,0.0022965113,0.6133222],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99935216,0.00002979992,0.00004198136,0.00006421686,0.00040475413,0.00010703215],"domain_scores_gemma":[0.995823,0.00011314992,0.00016941036,0.0003934456,0.002882413,0.0006186098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006901277,0.0014505314,0.0008814759,0.007279402,0.0018782269,0.006394168,0.0012341418,0.00079697673,0.22202095],"category_scores_gemma":[0.0027600718,0.00044605462,0.00041604866,0.018710343,0.00077916146,0.002845666,0.0022648748,0.0016243722,0.1267645],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012245598,0.000005053449,0.00038514467,0.00015057095,0.000003869968,0.000016051252,0.000020836484,0.00006137467,0.00007406214,0.0019567609,0.9785962,0.018717786],"study_design_scores_gemma":[0.0000015055728,0.0000014773833,0.0009578691,0.00003800282,0.0000014098043,0.000010771625,0.000026700736,0.000025635323,0.000029028106,0.00021817659,0.9986864,0.0000031189497],"about_ca_topic_score_codex":0.5296021,"about_ca_topic_score_gemma":0.5706747,"teacher_disagreement_score":0.5296021,"about_ca_system_score_codex":0.0047368794,"about_ca_system_score_gemma":0.022006629,"threshold_uncertainty_score":0.9463363},"labels":[],"label_agreement":null},{"id":"W7098087389","doi":"","title":"Session Topic:","year":2014,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Landslide; Submarine; Submarine landslide; Session (web analytics); Reflection (computer programming)","score_opus":0.01511841323825228,"score_gpt":0.212195479322807,"score_spread":0.19707706608455472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7098087389","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0015465663,0.0025901743,0.00189579,0.028335694,0.11939899,0.0013925942,0.009085112,0.0031256787,0.8326294],"genre_scores_gemma":[0.002860552,0.0011620352,0.0006262812,0.0071942257,0.015105933,0.00038276133,0.0036899757,0.00050044263,0.9684778],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9994204,0.00006619726,0.000026296244,0.00016845776,0.0001991926,0.000119406825],"domain_scores_gemma":[0.99803025,0.0001291138,0.0000474362,0.0000945665,0.0007456712,0.0009529388],"candidate_categories":["insufficient_payload"],"consensus_categories":["insufficient_payload"],"category_scores_codex":[0.0011103405,0.0013460252,0.0009940014,0.00080250297,0.0019458336,0.0045207855,0.0012880389,0.0041649328,0.76402295],"category_scores_gemma":[0.0019135005,0.00030868457,0.00097535364,0.00072698586,0.00034059084,0.0027770293,0.003012895,0.0026790434,0.60421264],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006557787,0.000046471265,0.000094375515,0.00010032903,0.000002550047,0.00003148532,0.000014667526,0.00001393092,0.0001882704,0.00033029835,0.98202527,0.017086852],"study_design_scores_gemma":[0.0000275281,0.000035741035,0.00064039184,0.0000623751,0.0000035173582,0.00004334815,0.000060405648,0.00003510909,0.00008472866,0.00035079604,0.9986506,0.00000555329],"about_ca_topic_score_codex":0.0013164814,"about_ca_topic_score_gemma":0.003968408,"teacher_disagreement_score":0.23597705,"about_ca_system_score_codex":0.0011529131,"about_ca_system_score_gemma":0.001757407,"threshold_uncertainty_score":0.3365926},"labels":[],"label_agreement":null},{"id":"W7099202804","doi":"","title":"ⒺShort Note Casualties Directly Caused by an Earthquake in Canada: First Contemporaneous Written Accounts from the M 6.5 Charlevoix,","year":2016,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Submarine; Period (music); Earthquake casualty estimation; Epicenter; Point (geometry)","score_opus":0.018316248405035762,"score_gpt":0.20699151121374879,"score_spread":0.18867526280871302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7099202804","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6086601,0.0066001597,0.0003207379,0.0038940422,0.00048007356,0.00030167412,0.25778243,0.00019013596,0.12177066],"genre_scores_gemma":[0.78879476,0.008879608,0.00047181125,0.0010586,0.00022214615,0.00010692663,0.059892505,0.000078014935,0.14049569],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994665,0.000015395963,0.000031858395,0.00004160884,0.00028293926,0.00016170822],"domain_scores_gemma":[0.99717736,0.00024567932,0.00043164063,0.00007417773,0.0017398071,0.0003313009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027508603,0.00028709404,0.00014406577,0.0053218766,0.002995525,0.0014416937,0.00045607326,0.00030394897,0.015422728],"category_scores_gemma":[0.0024361266,0.00019848488,0.00016498064,0.007991037,0.00047365692,0.00035794475,0.0007563503,0.00036927106,0.0018353148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021968667,0.000085029475,0.6288826,0.0010983475,0.00007002041,0.0030047419,0.03932575,0.00028003225,0.0014532441,0.0013373385,0.24222037,0.08202282],"study_design_scores_gemma":[0.0000028737613,0.000015031005,0.872391,0.00017586598,0.000014865213,0.0003127541,0.013488621,0.000079408004,0.00043286162,0.000033473218,0.11302859,0.000024647168],"about_ca_topic_score_codex":0.9887632,"about_ca_topic_score_gemma":0.9933073,"teacher_disagreement_score":0.015422728,"about_ca_system_score_codex":0.012640794,"about_ca_system_score_gemma":0.016330544,"threshold_uncertainty_score":0.09171575},"labels":[],"label_agreement":null},{"id":"W7099497280","doi":"","title":"Community Epidemiology Work Group Highlights and Executive Summary","year":2004,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Executive summary; Context (archaeology); Government (linguistics); Work (physics); Publication; Citation; Epidemiology; Law enforcement","score_opus":0.042058292857744324,"score_gpt":0.2461308184740665,"score_spread":0.2040725256163222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7099497280","genre_codex":"editorial","genre_gemma":"review","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"review","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0010523213,0.027609386,0.0024620309,0.22328357,0.3958084,0.00794425,0.02711063,0.0012159706,0.31351343],"genre_scores_gemma":[0.006028755,0.048360165,0.0027518137,0.038204607,0.1378734,0.00936667,0.032700695,0.00093580125,0.7237782],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9938187,0.0009368057,0.0007773283,0.00058255804,0.0028861016,0.0009985463],"domain_scores_gemma":[0.96459234,0.002758421,0.0014967155,0.0011940597,0.022765297,0.007193229],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.013248288,0.0024582515,0.0014101712,0.0057093524,0.002643626,0.008306,0.004162659,0.006856351,0.22604693],"category_scores_gemma":[0.0287969,0.0008966082,0.0009263081,0.006241203,0.0006432805,0.0036711642,0.0037351504,0.0038800968,0.20386073],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015143666,0.000016149832,0.000065249136,0.0001487915,0.0000011919483,0.000017510458,0.000015438858,0.000010370666,0.000024031438,0.0002351949,0.9827544,0.016696388],"study_design_scores_gemma":[0.000018326342,0.000025966872,0.0008825255,0.00043530687,0.000003275186,0.00002295313,0.00012203209,0.000017390657,0.00003864351,0.00037083623,0.99805474,0.00000801942],"about_ca_topic_score_codex":0.006338438,"about_ca_topic_score_gemma":0.0048452513,"teacher_disagreement_score":0.22604693,"about_ca_system_score_codex":0.0031881053,"about_ca_system_score_gemma":0.0135899205,"threshold_uncertainty_score":0.75620234},"labels":[],"label_agreement":null},{"id":"W7099972209","doi":"","title":"Income and the Outcomes of Children","year":2006,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Confidentiality; General partnership; Subject (documents); Official statistics; Human resources; Newspaper; Human rights; Statistician","score_opus":0.00582329043714246,"score_gpt":0.18588364270768912,"score_spread":0.18006035227054665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7099972209","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9453517,0.004604122,0.00015868996,0.011825136,0.00015978853,0.000022286555,0.006117495,0.000020619242,0.031740144],"genre_scores_gemma":[0.9925563,0.0016016157,0.00005610472,0.00016203287,0.000056185785,0.000013577886,0.0014852957,0.000011672064,0.0040572654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9984718,0.00047313148,0.00008725584,0.000115297065,0.00033241877,0.0005200291],"domain_scores_gemma":[0.9906425,0.0014420751,0.0037441237,0.0003266949,0.0011887986,0.0026557813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001460591,0.00023553656,0.00035301398,0.0017927412,0.0010775329,0.0018310908,0.00065561535,0.00048362243,0.014849782],"category_scores_gemma":[0.013495127,0.00016565721,0.000494116,0.0024436016,0.0007586288,0.0012241312,0.0014101785,0.0014115524,0.0014688631],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013223683,0.00010524676,0.9754608,0.000046566125,0.00011020619,0.00028553678,0.0010650713,0.0002683232,0.000025343772,0.0048828926,0.007967554,0.009650225],"study_design_scores_gemma":[0.000008590705,0.000052354644,0.99175596,0.000098042576,0.00003343773,0.00013626905,0.0014224811,0.00015832501,0.000054417324,0.0014764467,0.0047890535,0.000014659317],"about_ca_topic_score_codex":0.07062266,"about_ca_topic_score_gemma":0.07962509,"teacher_disagreement_score":0.07062266,"about_ca_system_score_codex":0.0020651734,"about_ca_system_score_gemma":0.0015138455,"threshold_uncertainty_score":0.14042318},"labels":[],"label_agreement":null},{"id":"W7100428799","doi":"","title":"and Aftershock Sequence: Constraints on Earthquake Source Parameters and Fault Geometry","year":2011,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aftershock; Seismometer; Moment tensor; Fault (geology); Epicenter; Foreshock; Magnitude (astronomy); Intraplate earthquake; Seismic hazard","score_opus":0.04556356757544864,"score_gpt":0.22328663099501062,"score_spread":0.17772306341956198,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7100428799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98739934,0.00019465278,0.0034675319,0.0001598253,0.000007485716,0.000029445684,0.0026891727,0.000075997756,0.0059765517],"genre_scores_gemma":[0.99701786,0.00005105913,0.0010419147,0.000008262064,0.000005860882,0.000006432845,0.0016395402,0.000018363991,0.0002107641],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996326,0.00014425379,0.000038950064,0.00008562794,0.00005149736,0.000047112415],"domain_scores_gemma":[0.9973743,0.0010184826,0.0007539154,0.00035784813,0.00030705702,0.00018829184],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007377217,0.0004291426,0.0004250041,0.0013469683,0.00036893855,0.0009753742,0.00039367634,0.00044585482,0.0037478285],"category_scores_gemma":[0.0069176415,0.00023333622,0.00022087133,0.0011892442,0.00026474043,0.0009955704,0.0005186368,0.00025296383,0.00070418144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005861013,0.00013737833,0.9208539,0.00007724812,0.000107741085,0.00048849074,0.00026358844,0.03369326,0.003655796,0.0043140417,0.002097147,0.033725336],"study_design_scores_gemma":[0.00009883296,0.000121954,0.89267385,0.00005218557,0.00006822418,0.0005130226,0.0005108074,0.09766991,0.0011408621,0.0039849845,0.0031332702,0.000032016673],"about_ca_topic_score_codex":0.008667796,"about_ca_topic_score_gemma":0.019732567,"teacher_disagreement_score":0.008667796,"about_ca_system_score_codex":0.0003925504,"about_ca_system_score_gemma":0.00050858536,"threshold_uncertainty_score":0.017234683},"labels":[],"label_agreement":null},{"id":"W7100533519","doi":"","title":"Theses and Dissertations. Paper 193. STORIES OF CANADA: NATIONAL IDENTITY IN LATE-NINETEENTH- CENTURY ENGLISH-CANADIAN FICTION","year":2003,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dominion; National identity; Identity (music); Reading (process); Narrative; Non-fiction; National heritage","score_opus":0.01001481737284603,"score_gpt":0.20474635683403145,"score_spread":0.1947315394611854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7100533519","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0048481217,0.028721565,0.00027962396,0.047791313,0.011543348,0.00019852111,0.008149948,0.00012100429,0.89834654],"genre_scores_gemma":[0.06094481,0.036594056,0.00056941377,0.0037066152,0.0030738476,0.0002272906,0.0030156504,0.0001292727,0.89173895],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99919254,0.00006246695,0.000024155976,0.00006414456,0.00051343034,0.00014330402],"domain_scores_gemma":[0.9970715,0.00033698784,0.000120441466,0.00013627464,0.001433839,0.00090096146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009140138,0.00056131504,0.00045702962,0.0028003477,0.009784199,0.006997037,0.0008026567,0.0011612462,0.110635355],"category_scores_gemma":[0.0044996655,0.00021174118,0.00029814657,0.005364202,0.0023090248,0.0011787186,0.0012785296,0.0018472255,0.016250873],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019697398,0.000040254952,0.00042890408,0.0002800421,0.00000325793,0.0001575396,0.0111831585,0.00005555528,0.00014912164,0.04600714,0.8910621,0.050613202],"study_design_scores_gemma":[0.0000022647605,0.000003303312,0.0012962237,0.00019457191,0.0000014460942,0.00003648375,0.0031543027,0.000010582905,0.000029609131,0.0011255896,0.99414223,0.000003368689],"about_ca_topic_score_codex":0.4406836,"about_ca_topic_score_gemma":0.64168257,"teacher_disagreement_score":0.5593164,"about_ca_system_score_codex":0.023628071,"about_ca_system_score_gemma":0.026997112,"threshold_uncertainty_score":0.8762371},"labels":[],"label_agreement":null},{"id":"W7100796119","doi":"","title":"Raven Chacon: Solos","year":2023,"lang":"","type":"other","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Navajo; The arts; Musical; Conversation; Applied arts; Singing; Native american; The Renaissance","score_opus":0.028385852232006813,"score_gpt":0.2256239182973137,"score_spread":0.1972380660653069,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7100796119","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012481537,0.004381555,0.0011918352,0.0030687058,0.003490373,0.000053942276,0.00068999577,0.0019603546,0.9839152],"genre_scores_gemma":[0.007268645,0.001136119,0.0007825429,0.0007240273,0.00044147775,0.000045095363,0.00043591516,0.0012838372,0.98788226],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9991574,0.00014267198,0.00003337597,0.00019031705,0.0003642194,0.000111951966],"domain_scores_gemma":[0.9994123,0.00007329889,0.000032246946,0.0000969742,0.0001802402,0.00020487819],"candidate_categories":["insufficient_payload"],"consensus_categories":[],"category_scores_codex":[0.00087875046,0.0012670942,0.000419861,0.0015379273,0.0043964987,0.005251869,0.0010277967,0.0016589684,0.3912801],"category_scores_gemma":[0.0018379075,0.00047621937,0.0003354555,0.0009396515,0.0012039337,0.0032781495,0.003457331,0.0018918909,0.18096407],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007293146,0.000026838252,0.0001367671,0.00007366789,0.0000020302664,0.00018116676,0.00050864863,0.000052281022,0.0005770171,0.016336871,0.9083405,0.073691316],"study_design_scores_gemma":[0.0000021283836,0.0000052096966,0.00008475973,0.000032045133,3.2147398e-7,0.000064343156,0.0001348029,0.000018484481,0.00010776079,0.00039645965,0.9991503,0.0000033364574],"about_ca_topic_score_codex":0.008745785,"about_ca_topic_score_gemma":0.02152222,"teacher_disagreement_score":0.3912801,"about_ca_system_score_codex":0.0015809956,"about_ca_system_score_gemma":0.0011389338,"threshold_uncertainty_score":0.86826503},"labels":[],"label_agreement":null},{"id":"W7101057766","doi":"","title":"Ó Birkhäuser Verlag, Basel, 2002 GEM Plate Boundary Simulations for the Plate Boundary Observatory: A Program for Understanding the Physics of Earthquakes on Complex Fault Networks via Observations, Theory and Numerical Simulation","year":2008,"lang":"en","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geodetic datum; Plate tectonics; Boundary (topology); Deformation (meteorology); Observatory; Bay; Fault (geology)","score_opus":0.1193698700277217,"score_gpt":0.2866217168165326,"score_spread":0.1672518467888109,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7101057766","genre_codex":"other","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":"other","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0050447206,0.07517268,0.22099818,0.004563314,0.006430948,0.00037200574,0.024165163,0.0340061,0.62924695],"genre_scores_gemma":[0.036032103,0.07863049,0.13757548,0.0012061637,0.0011865334,0.0008187904,0.03903405,0.0125513375,0.6929651],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99939895,0.00006645797,0.000055203727,0.00019948564,0.0002157164,0.00006422385],"domain_scores_gemma":[0.9988586,0.00033930189,0.000069926406,0.00035217617,0.00029856313,0.00008151029],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00092925964,0.0024359713,0.0022807699,0.0018377588,0.00059190183,0.0037326175,0.0016859183,0.0017690918,0.21494882],"category_scores_gemma":[0.0015113996,0.0013902758,0.0007617797,0.0025245408,0.0008959164,0.0046085683,0.0017736481,0.0032371262,0.26626137],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020555667,0.00016882512,0.0007579354,0.00095031905,0.00007762428,0.00044684217,0.00014073175,0.007541817,0.0070754183,0.030990014,0.32583502,0.6258099],"study_design_scores_gemma":[0.000086282475,0.000060923165,0.001108486,0.00046847502,0.000059178252,0.00061474874,0.00006930578,0.01474475,0.0027932217,0.017883733,0.96204686,0.00006417933],"about_ca_topic_score_codex":0.0047526998,"about_ca_topic_score_gemma":0.0027915651,"teacher_disagreement_score":0.21494882,"about_ca_system_score_codex":0.00064422074,"about_ca_system_score_gemma":0.000939635,"threshold_uncertainty_score":0.71907544},"labels":[],"label_agreement":null},{"id":"W7107952567","doi":"10.1016/j.ijrmms.2025.106358","title":"Influence of stress heterogeneity on shear behavior of rock discontinuities in laboratory experiments: New insights from numerical simulations","year":2025,"lang":"en","type":"article","venue":"International Journal of Rock Mechanics and Mining Sciences","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Hong Kong Polytechnic University; Research Grants Council, University Grants Committee","keywords":"Shear stress; Shear (geology); Classification of discontinuities; Critical resolved shear stress; Stress (linguistics); Slip (aerodynamics); Direct shear test; Stress concentration","score_opus":0.020239082248094155,"score_gpt":0.28740174827853365,"score_spread":0.2671626660304395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7107952567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973935,0.000060337952,0.001997787,0.00003652189,0.0000058925752,0.000007785428,0.00005284179,0.000026778278,0.0004185365],"genre_scores_gemma":[0.9996666,0.000027901942,0.0002378712,0.000003872558,0.000002611089,0.0000038944386,0.0000135989685,0.0000034550824,0.00004026065],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981886,0.000050739472,0.000021115424,0.00004169371,0.000033508193,0.000034088625],"domain_scores_gemma":[0.99858165,0.0009844044,0.00013102341,0.00018301993,0.000060434668,0.00005936837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038001421,0.00024678188,0.00038450683,0.00023813926,0.00019074877,0.0005177334,0.00035687588,0.00037290173,0.0010149988],"category_scores_gemma":[0.0018873285,0.00023545619,0.00022246112,0.00016466896,0.00069613516,0.00049974606,0.00032474188,0.0004129164,0.000092060756],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015540888,0.0012371314,0.011021443,0.00021009771,0.000065388725,0.0004124727,0.00029072436,0.16669229,0.8037247,0.0015086517,0.00034764223,0.012935473],"study_design_scores_gemma":[0.00020741823,0.0017510974,0.035733253,0.000020971245,0.00009815822,0.00014781528,0.00024524383,0.7709497,0.18891254,0.0013989587,0.0004692765,0.00006552255],"about_ca_topic_score_codex":0.0010294165,"about_ca_topic_score_gemma":0.00073736353,"teacher_disagreement_score":0.0010294165,"about_ca_system_score_codex":0.00024092456,"about_ca_system_score_gemma":0.00017756304,"threshold_uncertainty_score":0.0033955574},"labels":[],"label_agreement":null},{"id":"W7110778122","doi":"10.1785/0120060411\">https://dx.doi.org/10.1785/0120060411</a","title":"Late Holocene Rupture of the Northern San Andreas Fault and Possible Stress Linkage to the Cascadia Subduction Zone","year":2008,"lang":"","type":"article","venue":"University of New Hampshire Scholars Repository (University of New Hampshire at Manchester)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Canyon; Holocene; Fault (geology); Continental margin; San andreas fault; Aftershock; Quaternary; Cenozoic","score_opus":0.0166422591951333,"score_gpt":0.17870787677863004,"score_spread":0.16206561758349675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7110778122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983956,0.00006394309,0.00004957044,0.000044935205,0.0000020847217,0.0000014126557,0.00016788299,0.000008081493,0.0012663146],"genre_scores_gemma":[0.9992687,0.00007468881,0.000046595622,0.0000047312988,0.0000042016522,0.0000017496427,0.00027544418,0.0000015719064,0.00032230155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990845,0.000010524011,0.000007903948,0.000037185215,0.000015469159,0.000020472406],"domain_scores_gemma":[0.9995415,0.000031377695,0.00021512136,0.00004208316,0.000070818496,0.00009914318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017024309,0.00018466462,0.00012289787,0.0006446341,0.00032392034,0.00037024007,0.00017321963,0.00014047047,0.001638924],"category_scores_gemma":[0.00082738977,0.0001322596,0.00014099987,0.00059706444,0.00027668366,0.00020940576,0.00040325237,0.00018029891,0.00020794178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025075127,0.00001001908,0.994975,0.000010805824,0.000026252806,0.00009556997,0.00031322948,0.00041462385,0.0014690406,0.0001081314,0.00016056998,0.0023916771],"study_design_scores_gemma":[8.9727365e-7,0.000005017704,0.999275,0.0000023476925,0.0000033699866,0.000022458215,0.000077835924,0.00023371774,0.000056131965,0.000019319154,0.00030289113,0.0000010376958],"about_ca_topic_score_codex":0.050762285,"about_ca_topic_score_gemma":0.11615817,"teacher_disagreement_score":0.050762285,"about_ca_system_score_codex":0.0006813133,"about_ca_system_score_gemma":0.00048193423,"threshold_uncertainty_score":0.10093367},"labels":[],"label_agreement":null},{"id":"W7111073058","doi":"10.4401/ag-3452\">https://dx.doi.org/10.4401/ag-3452</a","title":"Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems","year":2003,"lang":"","type":"article","venue":"University of New Hampshire Scholars Repository (University of New Hampshire at Manchester)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Holocene; Subduction; San andreas fault; Subsidence; Turbidite; Submarine pipeline; Deglaciation; Radiocarbon dating","score_opus":0.014565262506045099,"score_gpt":0.17795706078752177,"score_spread":0.16339179828147668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7111073058","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99683243,0.00026349883,0.00011220573,0.00009471883,0.0000042982338,0.0000027424587,0.00057469413,0.000017955792,0.0020975117],"genre_scores_gemma":[0.9987551,0.00014073422,0.00012703103,0.000009889021,0.000006992679,0.0000030261256,0.000640607,0.0000054819784,0.0003110645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982196,0.00003340454,0.000020576977,0.000053534364,0.000035587647,0.000034864788],"domain_scores_gemma":[0.9987895,0.00019465512,0.00042616227,0.00008844345,0.00014258288,0.00035863245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004948218,0.00037975147,0.00024090019,0.0019747221,0.00037163583,0.0011648601,0.00026423432,0.00026481744,0.0018013658],"category_scores_gemma":[0.0017781919,0.00018922007,0.00020633018,0.0022074664,0.00048845203,0.00055276835,0.0008007792,0.0003171899,0.00026819785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024029383,0.000009435464,0.99572265,0.000017153498,0.0000453818,0.000049641683,0.000564874,0.00027233237,0.00080792705,0.00008789097,0.00016060394,0.0022380447],"study_design_scores_gemma":[0.0000010553316,0.0000050091066,0.9990834,0.000004294195,0.0000063846596,0.000011163114,0.00028200907,0.00026752896,0.00003573713,0.000036828846,0.0002644308,0.000002141961],"about_ca_topic_score_codex":0.06355577,"about_ca_topic_score_gemma":0.1919493,"teacher_disagreement_score":0.06355577,"about_ca_system_score_codex":0.0008002208,"about_ca_system_score_gemma":0.0004949357,"threshold_uncertainty_score":0.12637168},"labels":[],"label_agreement":null},{"id":"W7113149024","doi":"","title":"Structure of the Southern Canadian Rocky Mountain Foreland and Western San Joaquin Basin Fold-and-Thrust Belts","year":2025,"lang":"en","type":"article","venue":"Digital Access to Scholarship at Harvard (DASH) (Harvard University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Foreland basin; San Joaquin; Tectonics; Structural basin; Fold and thrust belt; Mountain formation; Front (military); Kinematics; Canyon","score_opus":0.011613835162170594,"score_gpt":0.20100907521308992,"score_spread":0.18939524005091932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7113149024","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.989465,0.0005890485,0.00023806687,0.00014356921,0.0000035303997,0.00001986779,0.0008419149,0.000024133635,0.008674904],"genre_scores_gemma":[0.9972511,0.00031295748,0.00046995518,0.000018897144,0.0000015563287,0.0000068612017,0.00068968575,0.000005348965,0.0012436208],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998292,0.0000054710786,0.000004683537,0.000045259552,0.00006449197,0.000050979703],"domain_scores_gemma":[0.99977165,0.000011649757,0.00004035276,0.000008705914,0.00012955019,0.00003800528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015302915,0.00017292636,0.00016890316,0.0017068653,0.0011630977,0.0010725188,0.0005341972,0.00020398266,0.0015395171],"category_scores_gemma":[0.00046623815,0.00013461588,0.00016006951,0.0019966757,0.00066203176,0.00021401444,0.00044747983,0.00013765175,0.00012182105],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059522423,0.000019990519,0.9329643,0.000090922855,0.000066687644,0.00021520835,0.004337966,0.003268033,0.0048587574,0.0023520538,0.0021483575,0.04961805],"study_design_scores_gemma":[0.0000017757725,0.000004042794,0.995955,0.000014326445,0.0000067238393,0.000039229362,0.00088211213,0.0008905118,0.00008697515,0.000062058534,0.0020517986,0.0000054752077],"about_ca_topic_score_codex":0.96161234,"about_ca_topic_score_gemma":0.988122,"teacher_disagreement_score":0.038387656,"about_ca_system_score_codex":0.0066660326,"about_ca_system_score_gemma":0.008166265,"threshold_uncertainty_score":0.07722741},"labels":[],"label_agreement":null},{"id":"W7114895124","doi":"10.18280/ijdne.201020","title":"Mapping the Research Landscape of Ecological Impacts of Earthquakes: A Scientometric Analysis","year":2025,"lang":"","type":"article","venue":"International Journal of Design & Nature and Ecodynamics","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":true,"route_about_ca":false,"ca_institutions":"","funders":"","keywords":"Field (mathematics); Ecological footprint; Quantitative analysis (chemistry)","score_opus":0.044473160254827435,"score_gpt":0.3206735933719731,"score_spread":0.27620043311714565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7114895124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9819811,0.00046072452,0.0045693736,0.00022284623,0.000006277977,0.000055392466,0.0048458674,0.00007462001,0.007783767],"genre_scores_gemma":[0.992845,0.00039373484,0.003807223,0.000011234447,0.000010200264,0.00003139231,0.0023435364,0.00002064003,0.0005370898],"study_design_codex":"observational","study_design_gemma":"not_applicable","domain_scores_codex":[0.9988226,0.00041059102,0.00015499658,0.00017220389,0.00032359533,0.00011588532],"domain_scores_gemma":[0.99491984,0.0026674725,0.00077140867,0.00034914407,0.0010742816,0.00021788213],"candidate_categories":["bibliometrics"],"consensus_categories":[],"category_scores_codex":[0.0016129883,0.00031522888,0.00040331733,0.032239936,0.00068667385,0.002705357,0.0003571204,0.00035860398,0.005124964],"category_scores_gemma":[0.011546574,0.00022689793,0.0008097697,0.041412137,0.00049130793,0.0018013067,0.0016558527,0.00020488338,0.0005668054],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019477906,0.0001346809,0.8120669,0.0005226659,0.00056221883,0.0004290727,0.0030238237,0.015577625,0.004692045,0.008194727,0.0036295662,0.15097198],"study_design_scores_gemma":[0.000011458987,0.00006604488,0.9606653,0.00006136588,0.00017953047,0.00031880903,0.0044099092,0.022313789,0.0004996769,0.003025529,0.008417234,0.00003137498],"about_ca_topic_score_codex":0.022342252,"about_ca_topic_score_gemma":0.022544242,"teacher_disagreement_score":0.9677601,"about_ca_system_score_codex":0.00072849734,"about_ca_system_score_gemma":0.0008580511,"threshold_uncertainty_score":0.044424415},"labels":[],"label_agreement":null},{"id":"W7114925044","doi":"10.5281/zenodo.17904201","title":"EURATOM METIS D4.1 Seismic source characterizations methodologies and applications","year":2025,"lang":"","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic hazard; Hazard; Statistic; Range (aeronautics); Probabilistic logic; Test statistic; Statistical hypothesis testing","score_opus":0.050799079144970644,"score_gpt":0.26753678465343217,"score_spread":0.21673770550846153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7114925044","genre_codex":"methods","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01138236,0.0007222298,0.89080423,0.00025576627,0.00016340341,0.00054352847,0.0120630255,0.045464057,0.03860146],"genre_scores_gemma":[0.07490738,0.0011974714,0.8431917,0.00016459588,0.00013219938,0.0011863727,0.046252515,0.007967179,0.025000542],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99875176,0.00021257115,0.00015548478,0.00021474792,0.0005652487,0.000100101905],"domain_scores_gemma":[0.9988971,0.00013024716,0.00013628701,0.00033675367,0.00043744678,0.00006208588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019657519,0.0012927318,0.00075366156,0.0023637412,0.0003177871,0.0018247259,0.0019840298,0.00073790585,0.017616937],"category_scores_gemma":[0.0041383067,0.000719122,0.00095895166,0.0022656615,0.00026742928,0.0012935257,0.002074388,0.0006825631,0.009824868],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005548194,0.00017703827,0.008757798,0.0010820028,0.00028339593,0.00031043697,0.00036542048,0.05672941,0.029308591,0.030178044,0.086300455,0.7859527],"study_design_scores_gemma":[0.00034192269,0.00031552144,0.013964558,0.00026889276,0.000074653624,0.0007134455,0.00019611444,0.32947424,0.03910576,0.027559523,0.58786786,0.000117560936],"about_ca_topic_score_codex":0.0049874256,"about_ca_topic_score_gemma":0.004035208,"teacher_disagreement_score":0.017616937,"about_ca_system_score_codex":0.0008413855,"about_ca_system_score_gemma":0.0011896646,"threshold_uncertainty_score":0.05893451},"labels":[],"label_agreement":null},{"id":"W7114931539","doi":"10.5281/zenodo.17904202","title":"EURATOM METIS D4.1 Seismic source characterizations methodologies and applications","year":2025,"lang":"","type":"article","venue":"Zenodo (CERN European Organization for Nuclear Research)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic hazard; Hazard; Statistic; Range (aeronautics); Probabilistic logic; Test statistic; Statistical hypothesis testing","score_opus":0.050799079144970644,"score_gpt":0.26753678465343217,"score_spread":0.21673770550846153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7114931539","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.01138236,0.0007222298,0.89080423,0.00025576627,0.00016340341,0.00054352847,0.0120630255,0.045464057,0.03860146],"genre_scores_gemma":[0.07490738,0.0011974714,0.8431917,0.00016459588,0.00013219938,0.0011863727,0.046252515,0.007967179,0.025000542],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.99875176,0.00021257115,0.00015548478,0.00021474792,0.0005652487,0.000100101905],"domain_scores_gemma":[0.9988971,0.00013024716,0.00013628701,0.00033675367,0.00043744678,0.00006208588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019657519,0.0012927318,0.00075366156,0.0023637412,0.0003177871,0.0018247259,0.0019840298,0.00073790585,0.017616937],"category_scores_gemma":[0.0041383067,0.000719122,0.00095895166,0.0022656615,0.00026742928,0.0012935257,0.002074388,0.0006825631,0.009824868],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005548194,0.00017703827,0.008757798,0.0010820028,0.00028339593,0.00031043697,0.00036542048,0.05672941,0.029308591,0.030178044,0.086300455,0.7859527],"study_design_scores_gemma":[0.00034192269,0.00031552144,0.013964558,0.00026889276,0.000074653624,0.0007134455,0.00019611444,0.32947424,0.03910576,0.027559523,0.58786786,0.000117560936],"about_ca_topic_score_codex":0.0049874256,"about_ca_topic_score_gemma":0.004035208,"teacher_disagreement_score":0.017616937,"about_ca_system_score_codex":0.0008413855,"about_ca_system_score_gemma":0.0011896646,"threshold_uncertainty_score":0.05893451},"labels":[],"label_agreement":null},{"id":"W7115713025","doi":"10.71846/18-wcee-0850","title":"EARTHQUAKE-TSUNAMI INSURANCE RISK EXPOSURE ESTIMATION FOR THE DISTRICT OF TOFINO, BRITISH COLUMBIA","year":2025,"lang":"en","type":"article","venue":"World Conference of Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Urban seismic risk; Seismic risk; Earthquake casualty estimation; Estimation; Episodic tremor and slip; Population; Risk assessment","score_opus":0.013961819893158632,"score_gpt":0.19614897308235937,"score_spread":0.18218715318920073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7115713025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917378,0.00014483908,0.0034799722,0.00017567932,0.0000041429685,0.000041742383,0.002002557,0.0000736059,0.002339627],"genre_scores_gemma":[0.9961422,0.00009293507,0.0009206476,0.000015749985,0.0000018563957,0.000015247702,0.0011575959,0.000007520246,0.0016462582],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982387,0.000023522312,0.000008694106,0.00003659996,0.0000417828,0.000065502594],"domain_scores_gemma":[0.9994548,0.00014293143,0.000063004154,0.0000331565,0.00022371535,0.00008235304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027976758,0.0005012335,0.00035307423,0.0008726236,0.0005986143,0.0009355735,0.0010008086,0.00048460608,0.0022669693],"category_scores_gemma":[0.001379835,0.00025164126,0.0003044864,0.001195835,0.0002544255,0.00021641236,0.00042794054,0.00038382015,0.00020747438],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016768523,0.00013948898,0.25003436,0.00007837939,0.00014715364,0.0006350187,0.00015334104,0.7171998,0.0017677223,0.0013164356,0.0032192587,0.025141338],"study_design_scores_gemma":[0.00001367567,0.000019788282,0.10850885,0.000016215638,0.000027722524,0.00005326693,0.0003743555,0.88941836,0.00026065152,0.00030514924,0.0009801484,0.000021887698],"about_ca_topic_score_codex":0.9644436,"about_ca_topic_score_gemma":0.9582349,"teacher_disagreement_score":0.035556376,"about_ca_system_score_codex":0.00792147,"about_ca_system_score_gemma":0.005787019,"threshold_uncertainty_score":0.071531475},"labels":[],"label_agreement":null},{"id":"W7115722651","doi":"10.71846/18-wcee-1668","title":"METIS PROJECT: GEM'S CONTRIBUTIONS TO THE HAZARD WORK PACKAGE","year":2025,"lang":"en","type":"article","venue":"World Conference of Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Context (archaeology); Hazard; Process (computing); Latin hypercube sampling; Uncertainty quantification; Monte Carlo method; Convolution (computer science); Metis","score_opus":0.02257091214324365,"score_gpt":0.23657359353853485,"score_spread":0.21400268139529122,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7115722651","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008156139,0.001242456,0.6901011,0.0029323988,0.0015470905,0.00039534474,0.03899503,0.20214118,0.054489315],"genre_scores_gemma":[0.07720707,0.0013962045,0.6695465,0.0014823521,0.0009670378,0.0009745132,0.09716345,0.12141841,0.029844442],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99775463,0.0006072653,0.000103048835,0.00026271038,0.0010891395,0.00018330663],"domain_scores_gemma":[0.99673414,0.00091176527,0.00017781756,0.0011493149,0.0007562484,0.0002706323],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0059616505,0.0020299552,0.0010831171,0.0017658898,0.0006201758,0.002900309,0.0039879084,0.0018649155,0.04250872],"category_scores_gemma":[0.011697066,0.0009287286,0.0020855225,0.0016286738,0.0006552472,0.0029570663,0.0059666233,0.0029234316,0.02452923],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006361218,0.00017564456,0.0051451083,0.0008662294,0.00033443177,0.00033121902,0.0007704062,0.0500842,0.0038040797,0.11491281,0.5523172,0.27062258],"study_design_scores_gemma":[0.00018641514,0.0000894683,0.0013402065,0.00015022824,0.000066666944,0.00022704632,0.00007709451,0.07975281,0.004240728,0.061732974,0.85203797,0.00009837404],"about_ca_topic_score_codex":0.0035232427,"about_ca_topic_score_gemma":0.0022835776,"teacher_disagreement_score":0.04250872,"about_ca_system_score_codex":0.0013231869,"about_ca_system_score_gemma":0.0020745283,"threshold_uncertainty_score":0.14220583},"labels":[],"label_agreement":null},{"id":"W7115810793","doi":"","title":"Tectono-Geomorphic Mapping of Neotectonic Bedrock Structures","year":2025,"lang":"en","type":"dissertation","venue":"MacSphere (McMaster University)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lineament; Intraplate earthquake; Fault scarp; Fault (geology); Bedrock; Shear zone; Transform fault; Precambrian; Mylonite; Basement","score_opus":0.01453788461900359,"score_gpt":0.1895019557436899,"score_spread":0.1749640711246863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7115810793","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99713826,0.000056983212,0.00030503314,0.000012540588,4.0965844e-7,0.000009374712,0.00096312497,0.00001981421,0.0014945429],"genre_scores_gemma":[0.9977234,0.000057597546,0.00058067427,0.0000022357904,3.35681e-7,0.0000045508536,0.0008219921,0.0000022228642,0.0008070002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999647,0.0000019060582,0.0000016597451,0.000010161549,0.000014163535,0.00000735483],"domain_scores_gemma":[0.99994206,0.0000035609626,0.000014377735,0.0000058233354,0.000022077262,0.000012100502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000034947152,0.00012542598,0.00006431322,0.0005636079,0.00023875834,0.00032697213,0.0001449439,0.000096484306,0.001121663],"category_scores_gemma":[0.00015193044,0.00009713513,0.00008092596,0.00067969935,0.00014540236,0.000098539116,0.00024232846,0.000057012097,0.00015053352],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007251247,0.000023130537,0.94246197,0.0000646937,0.000023577637,0.00020908749,0.0010459586,0.005470293,0.018139113,0.00029768722,0.00045790014,0.031734042],"study_design_scores_gemma":[0.0000031530014,0.000015192539,0.99281293,0.000006548353,0.000006114369,0.000057344198,0.00036404977,0.005042912,0.00055504043,0.000026827387,0.001107241,0.0000026956757],"about_ca_topic_score_codex":0.66307914,"about_ca_topic_score_gemma":0.8697044,"teacher_disagreement_score":0.66307914,"about_ca_system_score_codex":0.0020072095,"about_ca_system_score_gemma":0.0013428886,"threshold_uncertainty_score":0.6778101},"labels":[],"label_agreement":null},{"id":"W7116046256","doi":"10.71846/17-wcee-2095","title":"SEISMIC HAZARD IN SOUTHEASTERN CANADA: UNCERTAINTY AND CONTROLS IN A REGION OF LOW-TO-MODERATE SEISMICITY","year":2025,"lang":"en","type":"article","venue":"World Conference of Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Seismotectonics; Seismic risk; Hazard; Seismic hazard; Epicenter","score_opus":0.01582089464090054,"score_gpt":0.19288430948010488,"score_spread":0.17706341483920435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7116046256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972025,0.000110445515,0.00017303503,0.0005000607,0.0000028558104,0.000008456767,0.0005699506,0.000010044039,0.0014226512],"genre_scores_gemma":[0.9990971,0.000051778417,0.000091412854,0.000028547018,0.0000013944074,0.0000018685766,0.00016153042,0.000003148738,0.00056316244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99931455,0.00012322221,0.000041458505,0.00010619077,0.0001627646,0.00025187244],"domain_scores_gemma":[0.99564266,0.0016208157,0.0005319835,0.00012477915,0.001454068,0.0006257209],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010041824,0.00024217163,0.00040408704,0.0008165778,0.0020734258,0.002156692,0.0016397334,0.00053007255,0.0015271795],"category_scores_gemma":[0.0048003555,0.00025360932,0.00038058104,0.0016514844,0.0015668402,0.00045910434,0.0008871627,0.0007650608,0.000120133845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042469666,0.000116268704,0.9577632,0.00003220442,0.00015788553,0.00037597213,0.0019024943,0.024796713,0.00079989794,0.0024984218,0.0017383666,0.009393852],"study_design_scores_gemma":[0.000030691997,0.000037088827,0.93140006,0.00003445049,0.00007289025,0.00008160075,0.009116332,0.056058716,0.00040483696,0.00086536125,0.00184211,0.00005587917],"about_ca_topic_score_codex":0.9971903,"about_ca_topic_score_gemma":0.9977932,"teacher_disagreement_score":0.033749837,"about_ca_system_score_codex":0.033749837,"about_ca_system_score_gemma":0.025174165,"threshold_uncertainty_score":0.24487334},"labels":[],"label_agreement":null},{"id":"W7116104670","doi":"10.71846/16-wcee-0613","title":"EARTHQUAKE SITE CLASS CHARACTERIZATION OF SEISMOGRAPH AND STRONG-MOTION STATIONS IN CANADA AND CHILE","year":2025,"lang":"en","type":"article","venue":"World Conference of Earthquake Engineering","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismometer; Class (philosophy); Epicenter; Seismic risk; Seismotectonics","score_opus":0.011105033349565035,"score_gpt":0.17843932703977833,"score_spread":0.1673342936902133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7116104670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896355,0.000117800606,0.00011524693,0.00005094264,0.00000201632,0.00004236993,0.0055070003,0.000016350918,0.00451279],"genre_scores_gemma":[0.99245596,0.00015238457,0.0002388077,0.000020203383,0.0000016169126,0.000030202275,0.00392943,0.000010520494,0.0031608606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972683,0.000019368796,0.000020364909,0.00005423407,0.000057732304,0.000121492274],"domain_scores_gemma":[0.99840134,0.00013739816,0.00024124482,0.000091253074,0.00081796816,0.00031072102],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002877254,0.00020250562,0.00024714545,0.0039134216,0.0010541134,0.0010916205,0.00067792105,0.00025396553,0.0031524997],"category_scores_gemma":[0.0014957073,0.00023540904,0.00023814698,0.0046226196,0.00040024042,0.00032598485,0.0007364384,0.0002540142,0.00041885776],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008898342,0.000030712723,0.9836821,0.00004549056,0.000040373383,0.0001795171,0.0012556987,0.00058962154,0.002351979,0.00031174588,0.0009947757,0.010429103],"study_design_scores_gemma":[0.0000022113782,0.0000036500198,0.9973341,0.0000095394835,0.000010514529,0.00002700039,0.0014475911,0.00020897134,0.00011918449,0.00001545708,0.0008172056,0.000004455912],"about_ca_topic_score_codex":0.9226938,"about_ca_topic_score_gemma":0.96103406,"teacher_disagreement_score":0.07730621,"about_ca_system_score_codex":0.0060097678,"about_ca_system_score_gemma":0.0083551975,"threshold_uncertainty_score":0.15552294},"labels":[],"label_agreement":null},{"id":"W7116848290","doi":"10.1201/9781003761259-30","title":"Tsunami deposit mapping at Seaside, Oregon, USA","year":2025,"lang":"en","type":"book-chapter","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Margin (machine learning); Wetland; Prehistory; Radiocarbon dating; Historical record","score_opus":0.021702747117944485,"score_gpt":0.20061988508720652,"score_spread":0.17891713796926204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7116848290","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.34177655,0.001141433,0.0064864764,0.0011580228,0.00013069127,0.00023573422,0.061712675,0.0028411823,0.5845172],"genre_scores_gemma":[0.2943217,0.0037007052,0.033115402,0.0002709386,0.000096840646,0.0002212951,0.061364047,0.00069680234,0.60621226],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9999635,0.0000016883162,0.0000025835534,0.000009512291,0.00002027049,0.0000023699881],"domain_scores_gemma":[0.99992335,0.0000059966956,0.0000058407236,0.000006157772,0.000047975096,0.00001068839],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000085590924,0.00023932218,0.000053840045,0.0014769905,0.00050828705,0.0004780894,0.00032516077,0.00011105655,0.026266836],"category_scores_gemma":[0.00014280624,0.00012416721,0.000080514525,0.0016967852,0.00006212462,0.0003984711,0.00032707377,0.00015458815,0.0054171025],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000109336885,0.00021536024,0.1562825,0.00019673002,0.00003654665,0.0008805483,0.0014346571,0.0011419305,0.022123238,0.0026605388,0.29502296,0.5198956],"study_design_scores_gemma":[0.000019787336,0.000041779836,0.32460418,0.00016392011,0.000029314517,0.00057319255,0.0018911079,0.004243055,0.010527328,0.0006648711,0.6572184,0.000023067405],"about_ca_topic_score_codex":0.054762952,"about_ca_topic_score_gemma":0.31834778,"teacher_disagreement_score":0.054762952,"about_ca_system_score_codex":0.0004167946,"about_ca_system_score_gemma":0.00035856105,"threshold_uncertainty_score":0.10888839},"labels":[],"label_agreement":null},{"id":"W7130579760","doi":"10.1785/0220250237","title":"The Earthquake Swarms of Eastern Maine and Nearby New Brunswick Since 2006","year":2025,"lang":"en","type":"article","venue":"Seismological Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Earthquake swarm; Devonian; Stress field; Rock mass classification; Swarm behaviour; Magnitude (astronomy); Inclusion (mineral)","score_opus":0.04381871067429969,"score_gpt":0.299141593159893,"score_spread":0.2553228824855933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7130579760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939628,0.00040116638,0.00007131578,0.00013748927,0.000014900434,0.000029390896,0.0029427863,0.0000106205325,0.0024293528],"genre_scores_gemma":[0.99382,0.00038094315,0.00017572143,0.000060112197,0.000008672479,0.000020930485,0.0037116348,0.000005462345,0.0018165153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981374,0.000011445173,0.00001935268,0.000036457976,0.00004830634,0.00007080679],"domain_scores_gemma":[0.99904877,0.00006367622,0.00032243162,0.000046880716,0.00037870943,0.00013959777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024041103,0.00025454245,0.0002600379,0.002051247,0.0006769971,0.000832317,0.00054042734,0.00021678246,0.0014986157],"category_scores_gemma":[0.0008811052,0.00017319896,0.00019871723,0.0024926446,0.00042597024,0.0003902337,0.0007706827,0.00022740345,0.00020742691],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005340382,0.00001575149,0.9863282,0.000052127976,0.000065259475,0.0003379367,0.0009711541,0.00042162565,0.0016817051,0.00005796908,0.001167927,0.008846903],"study_design_scores_gemma":[0.0000016071162,0.0000060006687,0.9977482,0.000011020092,0.000005949442,0.00003561005,0.0007571225,0.00011337299,0.00006472452,0.0000047157273,0.0012480804,0.0000035640844],"about_ca_topic_score_codex":0.771686,"about_ca_topic_score_gemma":0.9299842,"teacher_disagreement_score":0.22831398,"about_ca_system_score_codex":0.003755683,"about_ca_system_score_gemma":0.0025709146,"threshold_uncertainty_score":0.4593171},"labels":[],"label_agreement":null},{"id":"W7132143698","doi":"","title":"Source Rupture Models and Tsunami Simulations of Destructive October 28 2012 Queen Charlotte Islands British Columbia Mw 7 8 and September 16 2015 Illapel Chile Mw 8 3 Earthquakes","year":2016,"lang":"en","type":"article","venue":"Kocaeli Üniversitesi - AVESİS","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Queen (butterfly); Period (music); Epicenter","score_opus":0.00842712010358807,"score_gpt":0.18798659911259302,"score_spread":0.17955947900900496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7132143698","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9865025,0.00016579883,0.00077040074,0.00042233808,0.000054059063,0.00002241296,0.004296969,0.0002954252,0.00746994],"genre_scores_gemma":[0.994628,0.000111492714,0.0004744778,0.000041064173,0.00001221589,0.000027362363,0.0024381739,0.000075043376,0.0021922744],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985766,0.00003099494,0.000012169041,0.00003390456,0.000021029566,0.000044334567],"domain_scores_gemma":[0.99888307,0.00051483733,0.00010909276,0.00007017899,0.00026885787,0.00015391914],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040378745,0.00074625615,0.00069070107,0.0012328388,0.00081200746,0.0014385607,0.0020201614,0.002242501,0.006112671],"category_scores_gemma":[0.002578351,0.0010194387,0.0006506615,0.0015061528,0.0006767339,0.0008097597,0.00048608557,0.0013082444,0.0007097513],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022950972,0.00011990562,0.008398573,0.000032923297,0.00006970116,0.00013917309,0.00008056541,0.98604983,0.00034616207,0.00075311854,0.0020542594,0.001726305],"study_design_scores_gemma":[0.00009550642,0.000024499299,0.007021674,0.00001142788,0.000023135577,0.000014410445,0.000116483025,0.99175733,0.0001798375,0.0002828985,0.00045270464,0.000020030786],"about_ca_topic_score_codex":0.595661,"about_ca_topic_score_gemma":0.49989286,"teacher_disagreement_score":0.40433902,"about_ca_system_score_codex":0.0049892147,"about_ca_system_score_gemma":0.0027055782,"threshold_uncertainty_score":0.8134405},"labels":[],"label_agreement":null},{"id":"W7132471726","doi":"","title":"Observations and Numerical Simulation of 28 October 2012 Earthquake Mw 7 8 and the Tsunami in Queen Charlotte Islands British Columbia","year":2016,"lang":"en","type":"article","venue":"Kocaeli Üniversitesi - AVESİS","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Queen (butterfly); Computer simulation; Numerical models; Numerical modeling","score_opus":0.012790713280885766,"score_gpt":0.19034211492617198,"score_spread":0.1775514016452862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7132471726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99626476,0.00003693548,0.00010575931,0.00013016113,0.000010914826,0.000008817694,0.0014693355,0.00004332273,0.0019300673],"genre_scores_gemma":[0.99730635,0.000045315563,0.00018810133,0.000020884745,0.0000032981343,0.000013696864,0.0015708782,0.000010309202,0.00084109965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999782,0.000030973628,0.000020771717,0.000049580045,0.000039758295,0.00007685452],"domain_scores_gemma":[0.9993777,0.00013234613,0.000067564535,0.000055270717,0.0002456138,0.00012145402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002594621,0.00031076482,0.0003477885,0.00062070973,0.0010325118,0.0009854255,0.0011630838,0.0012254524,0.002284099],"category_scores_gemma":[0.0016241133,0.00055221806,0.00036731144,0.0011410671,0.00057462597,0.00042446863,0.00061977486,0.0008260282,0.0004684377],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010535523,0.00069620775,0.5437864,0.00014305726,0.00031158378,0.0011183781,0.0014826632,0.4175344,0.005789558,0.0009027728,0.012599015,0.014582433],"study_design_scores_gemma":[0.00016129148,0.000077530625,0.6120149,0.000043918873,0.00008571061,0.000054247776,0.0018264052,0.38116306,0.00097298855,0.00012777006,0.003384681,0.00008745763],"about_ca_topic_score_codex":0.932126,"about_ca_topic_score_gemma":0.94142133,"teacher_disagreement_score":0.067874014,"about_ca_system_score_codex":0.004759905,"about_ca_system_score_gemma":0.003634073,"threshold_uncertainty_score":0.13654745},"labels":[],"label_agreement":null},{"id":"W7132567291","doi":"","title":"Multistage lithospheric drips control active basin formation within an uplifting orogenic plateau","year":2024,"lang":"en","type":"article","venue":"Publication Database GFZ (GFZ German Research Centre for Geosciences)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Alliance de recherche numérique du Canada; Türkiye Bilimsel ve Teknolojik Araştırma Kurumu","keywords":"Lithosphere; Structural basin; Plateau (mathematics); Crust; Subsidence; Mantle (geology); Tectonics; Massif","score_opus":0.046798759730714797,"score_gpt":0.32433684154604203,"score_spread":0.27753808181532724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7132567291","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995332,0.0000263682,0.00004549716,0.0000041948438,3.2436532e-7,0.0000017608353,0.00002940957,0.0000036517313,0.00035551982],"genre_scores_gemma":[0.9997812,0.00002281993,0.000032322627,0.00000184899,7.489763e-7,0.0000015539129,0.00005471148,0.0000014518024,0.000103455175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994767,0.000007962486,0.0000042900347,0.000016133687,0.0000066100397,0.000017343982],"domain_scores_gemma":[0.9998741,0.000018918576,0.000053372954,0.00001294157,0.000014382614,0.000026199446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008064077,0.00007053144,0.00017090977,0.00038330036,0.00018934188,0.00044402637,0.0001530086,0.000116076306,0.001070997],"category_scores_gemma":[0.00030562707,0.000097836324,0.000086540735,0.00034575156,0.00026283856,0.00016801074,0.0003960406,0.00010136958,0.0001355399],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045515393,0.00007630769,0.76046175,0.00006694532,0.000061885374,0.000795359,0.000972725,0.0014799964,0.221558,0.00067747245,0.00016321271,0.013231285],"study_design_scores_gemma":[0.0000032416717,0.000026184733,0.9979518,0.0000020994796,0.000005815981,0.000049314633,0.00016838594,0.00045104357,0.0010770767,0.000056405508,0.00020681726,0.0000019006276],"about_ca_topic_score_codex":0.0035876895,"about_ca_topic_score_gemma":0.0057598506,"teacher_disagreement_score":0.0035876895,"about_ca_system_score_codex":0.00024102011,"about_ca_system_score_gemma":0.00018959536,"threshold_uncertainty_score":0.007133603},"labels":[],"label_agreement":null},{"id":"W7135701194","doi":"","title":"Which operational factors lead to seismogenic fluid-injections? observations from ten large-scale studies in North America","year":2025,"lang":"en","type":"article","venue":"Bristol Research (University of Bristol)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Induced seismicity; Tectonics; Lead (geology); Block (permutation group theory); Sedimentary rock; Hydraulic fracturing; Seismic energy","score_opus":0.09713952560845847,"score_gpt":0.31020120628466225,"score_spread":0.2130616806762038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7135701194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99756086,0.00031501512,0.00031759634,0.00011703913,0.0000035954006,0.000008766282,0.0008773374,0.000008899789,0.00079092523],"genre_scores_gemma":[0.9981041,0.0002490442,0.00036809855,0.000048624588,0.000008682124,0.000011844081,0.0010109432,0.000005399904,0.0001932682],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970764,0.00006424504,0.000037048525,0.00009724591,0.000041639207,0.000052234038],"domain_scores_gemma":[0.9984546,0.00031901305,0.00075412844,0.00013717597,0.00020972546,0.00012531415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047107603,0.00017861722,0.0001822114,0.0009218332,0.00040483504,0.00070219114,0.0003028189,0.00029094506,0.0008543704],"category_scores_gemma":[0.0015584609,0.00020186613,0.000217357,0.0020298662,0.0004538266,0.00046315158,0.00072816625,0.000225377,0.00010469084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020382422,0.000009823385,0.9935719,0.000037548227,0.00005057767,0.000085669366,0.0011043902,0.00011295132,0.0012515861,0.000058751863,0.0003180127,0.003378485],"study_design_scores_gemma":[0.0000013826166,0.000004679063,0.9976725,0.000012121736,0.000018830728,0.000020588011,0.0012293208,0.00012350993,0.00011666551,0.00002919443,0.00076890056,0.0000022912557],"about_ca_topic_score_codex":0.10529929,"about_ca_topic_score_gemma":0.25511295,"teacher_disagreement_score":0.10529929,"about_ca_system_score_codex":0.00055329944,"about_ca_system_score_gemma":0.00065577537,"threshold_uncertainty_score":0.20937276},"labels":[],"label_agreement":null},{"id":"W7139160523","doi":"","title":"Integrated Theoretical Modeling and Empirical Analysis of Injection-Induced Fault Slip and Seismic Hazard: From Parameter Sensitivity to Real-World Case Studies","year":2025,"lang":"","type":"dissertation","venue":"TSpace (University of Toronto)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Government of Ontario","keywords":"Poromechanics; Induced seismicity; Slip (aerodynamics); Seismic moment; Hydrogeology; Seismic hazard; Foreshock; Sensitivity (control systems); Geomechanics","score_opus":0.03556738849787369,"score_gpt":0.2958317627480813,"score_spread":0.26026437425020765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7139160523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9724339,0.00048690918,0.022444122,0.00053585303,0.000011774794,0.000031614014,0.00032427692,0.00008253607,0.0036490827],"genre_scores_gemma":[0.99716574,0.00017349576,0.0023139378,0.000021442294,0.000007474342,0.000016881562,0.00009769772,0.000011006917,0.00019216031],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996131,0.0001680885,0.000029031362,0.00007644414,0.0000628159,0.000050475148],"domain_scores_gemma":[0.99440104,0.004510468,0.00045999707,0.0003640423,0.00018951281,0.00007500535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018536302,0.0006035445,0.00054472836,0.0010598858,0.00029529392,0.001098807,0.0011184643,0.0015212976,0.0012340536],"category_scores_gemma":[0.007337959,0.00041725053,0.0008423895,0.00074361044,0.0012710715,0.0012265543,0.0009248679,0.0011959318,0.00008983332],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002200991,0.00004895823,0.0066389134,0.00003050288,0.000026852647,0.00009131629,0.000038283342,0.9878318,0.0004616085,0.0028778976,0.0001297032,0.0018022317],"study_design_scores_gemma":[0.0000026955584,0.000019225829,0.0016083817,0.000006332627,0.000008231537,0.000020009362,0.000032916763,0.99653745,0.00024251343,0.001426402,0.00008908164,0.0000068161253],"about_ca_topic_score_codex":0.007298102,"about_ca_topic_score_gemma":0.0039128195,"teacher_disagreement_score":0.007298102,"about_ca_system_score_codex":0.0014927791,"about_ca_system_score_gemma":0.00043908908,"threshold_uncertainty_score":0.014511287},"labels":[],"label_agreement":null},{"id":"W7146720058","doi":"","title":"プレート沈込み型地震に対する半特異面数学モデルの構築","year":2024,"lang":"en","type":"article","venue":"Institutional Repositories DataBase (IRDB)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"123 Certification (Canada)","funders":"","keywords":"Plate tectonics; Subduction; Point (geometry); Geodynamics; Plate theory; Euler's formula; Pacific Plate; Fault (geology)","score_opus":0.01913422890686745,"score_gpt":0.24076521674772733,"score_spread":0.22163098784085988,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7146720058","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.054158743,0.078246735,0.4142082,0.017644519,0.0057952474,0.00021768277,0.0023081433,0.0011715225,0.42624924],"genre_scores_gemma":[0.6423594,0.060694378,0.09712559,0.0027634483,0.0040939976,0.00021860165,0.001903726,0.0003036283,0.19053721],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996729,0.000049018196,0.000021583015,0.000086304986,0.00014254957,0.000027705557],"domain_scores_gemma":[0.9996798,0.00006413711,0.00004831286,0.00004220607,0.00013389929,0.000031706713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005463679,0.00041203815,0.00037199046,0.0008180177,0.0011255356,0.00122901,0.00045900172,0.00082122267,0.010371216],"category_scores_gemma":[0.00094388094,0.00023198791,0.00027141636,0.0010106171,0.0018310673,0.0025824315,0.0009463807,0.001157618,0.005916808],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010147661,0.000052734813,0.00420334,0.0004121055,0.000022425142,0.00043553466,0.00086804037,0.003986206,0.005471426,0.6925122,0.04248628,0.2494482],"study_design_scores_gemma":[0.000017610319,0.00015787588,0.005093541,0.00019958979,0.000035026176,0.0016218476,0.00077727094,0.011666516,0.0052405302,0.35001302,0.6251004,0.00007673979],"about_ca_topic_score_codex":0.0026110515,"about_ca_topic_score_gemma":0.0018812984,"teacher_disagreement_score":0.010371216,"about_ca_system_score_codex":0.0010724396,"about_ca_system_score_gemma":0.0008023879,"threshold_uncertainty_score":0.03469515},"labels":[],"label_agreement":null},{"id":"W7146945780","doi":"10.70675/61417179z0d00z4580zb92dz7c11e7c98612","title":"Tectonique active de la zone de collision Yakutat - Nord Amérique : apport du GPS et de la géomorphologie à l'étude de la partition de la déformation","year":2015,"lang":"","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Pacific ocean; Poison control; North American Plate","score_opus":0.016411752939146037,"score_gpt":0.3018659926201711,"score_spread":0.28545423968102507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7146945780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929066,0.00040850486,0.0008213424,0.00017110427,0.000017864433,0.000011709359,0.00070038566,0.0000415056,0.0049210805],"genre_scores_gemma":[0.996157,0.00035179235,0.0009806091,0.000021019257,0.0000059430527,0.000008190994,0.00049424305,0.000010748054,0.0019704683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999237,0.000005648773,0.0000034636523,0.00001990476,0.000030594638,0.000016604155],"domain_scores_gemma":[0.9998425,0.000027405895,0.00003387273,0.000007867639,0.0000717724,0.0000166248],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016259728,0.00021965116,0.0001561666,0.00057147635,0.00042053816,0.00091162947,0.00025856073,0.0002820752,0.0013610272],"category_scores_gemma":[0.00038673158,0.00018209017,0.00019085921,0.0014242342,0.00035489263,0.00032568382,0.0003436823,0.00033270734,0.00018182628],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002145174,0.00003944967,0.90442044,0.00013664729,0.000070116694,0.00052569754,0.0044349683,0.015083997,0.017822074,0.00085808634,0.0010840981,0.055309955],"study_design_scores_gemma":[0.000008272381,0.000019665114,0.98667425,0.000035432604,0.000026174745,0.000086168715,0.0020243076,0.00724261,0.0007254112,0.00010159616,0.0030404585,0.0000156999],"about_ca_topic_score_codex":0.47198096,"about_ca_topic_score_gemma":0.63292104,"teacher_disagreement_score":0.5280191,"about_ca_system_score_codex":0.0013375711,"about_ca_system_score_gemma":0.001681663,"threshold_uncertainty_score":0.93846744},"labels":[],"label_agreement":null},{"id":"W7148632382","doi":"10.70675/6a48ec8fz1423z4e3bza460z2d0feda122c4","title":"Localisation de la déformation et de la sismicité en domaine intraplaque : réactivation des paléo-structures crustales et lithosphériques","year":2018,"lang":"","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"North sea; Prospection; Global Positioning System; Structural failure","score_opus":0.00807309693827874,"score_gpt":0.28535951713855334,"score_spread":0.2772864202002746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7148632382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98707855,0.0006649093,0.0040884437,0.00014590952,0.00000876015,0.000010212957,0.00041637963,0.000051059436,0.0075358907],"genre_scores_gemma":[0.9967002,0.00027360037,0.0010592993,0.000011749222,0.0000038563235,0.0000038848007,0.00014012505,0.000009902058,0.0017973592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999863,0.000009930506,0.000005569043,0.00003871526,0.00005372519,0.000028984115],"domain_scores_gemma":[0.9997651,0.0000379405,0.00005501752,0.000023692704,0.0000958013,0.000022413584],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020868143,0.00022732712,0.00020127726,0.0009870685,0.0004898347,0.001068438,0.00027683855,0.0003291684,0.002670381],"category_scores_gemma":[0.0005135268,0.00019312662,0.00019273514,0.0012493208,0.00090360694,0.00064594374,0.00056838326,0.0003294852,0.00036344383],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002577962,0.00005688357,0.741348,0.0005303467,0.00017126906,0.0009330165,0.0041787666,0.024805786,0.11884832,0.009187621,0.0006034906,0.0990786],"study_design_scores_gemma":[0.0000033926167,0.000037219426,0.9805173,0.000056739103,0.000030322297,0.0002129768,0.0013210189,0.005006602,0.008038878,0.00062789343,0.004123992,0.000023671353],"about_ca_topic_score_codex":0.10709366,"about_ca_topic_score_gemma":0.21319194,"teacher_disagreement_score":0.10709366,"about_ca_system_score_codex":0.0013041737,"about_ca_system_score_gemma":0.0014046584,"threshold_uncertainty_score":0.21294063},"labels":[],"label_agreement":null},{"id":"W7155576704","doi":"","title":"Using Episodic Tremor and Slip to Characterize Subduction Under Vancouver Island","year":2025,"lang":"en","type":"dissertation","venue":"KU ScholarWorks (The University of Kansas)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subduction; Episodic tremor and slip; Slip (aerodynamics); Plate tectonics; Tectonics; Seismotectonics; Amplitude; Fault (geology)","score_opus":0.022610426356501512,"score_gpt":0.21244183556085391,"score_spread":0.1898314092043524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7155576704","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99533135,0.00013930733,0.0006319302,0.000028269602,0.0000041618055,0.000018375955,0.0008640489,0.000027610526,0.002954899],"genre_scores_gemma":[0.9971148,0.00016474357,0.00078533095,0.000010707209,0.000004242259,0.00001455307,0.0012274578,0.000008212665,0.0006698845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973553,0.000020805444,0.000023852537,0.000065647015,0.00009233554,0.000061806204],"domain_scores_gemma":[0.9992924,0.00011394939,0.0001522414,0.00004628484,0.00026846598,0.00012665047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033993073,0.0004810172,0.00022898431,0.0019380684,0.0007169193,0.0011625299,0.0004085201,0.00030605655,0.00077333814],"category_scores_gemma":[0.001615399,0.0001719743,0.0001838,0.0021123667,0.0004162631,0.00031118997,0.00074617506,0.0003291229,0.00020125923],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006981252,0.00001975011,0.97395724,0.000053774605,0.00006045142,0.00029280203,0.00082866795,0.0033474797,0.0037215985,0.00010026242,0.00032002994,0.017228227],"study_design_scores_gemma":[0.0000026291932,0.000012422989,0.99371755,0.000023245038,0.000014723261,0.00004585147,0.00059547176,0.004614389,0.0003347573,0.000038986185,0.0005922117,0.000007833482],"about_ca_topic_score_codex":0.57430243,"about_ca_topic_score_gemma":0.81268317,"teacher_disagreement_score":0.42569757,"about_ca_system_score_codex":0.0017151544,"about_ca_system_score_gemma":0.0015480865,"threshold_uncertainty_score":0.8564092},"labels":[],"label_agreement":null},{"id":"W7161824543","doi":"10.82308/32809","title":"A case study of dynamic triggering in the Kiskatinaw area of the Montney Formation, British Columbia","year":2021,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Water level","score_opus":0.014868213679377962,"score_gpt":0.22152485445041267,"score_spread":0.2066566407710347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161824543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99215955,0.00015220807,0.0003285635,0.00013303556,0.0000054695734,0.000061649356,0.00020793708,0.0000107174055,0.0069408068],"genre_scores_gemma":[0.99490213,0.00020055851,0.00056540273,0.00003709524,0.000003084807,0.000022958004,0.00013939461,0.00000793545,0.004121432],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99928254,0.00009184704,0.00002754242,0.000091076676,0.00022093051,0.0002860286],"domain_scores_gemma":[0.9992347,0.00016541059,0.00011066848,0.000057146925,0.00027136065,0.00016078813],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037956706,0.0003549493,0.0003230528,0.0013725902,0.0047445083,0.0017804175,0.0010168789,0.000854381,0.0023255998],"category_scores_gemma":[0.0017833614,0.0003127416,0.00022588558,0.0033898365,0.0018691195,0.0003457997,0.0013871263,0.0005889373,0.0001920172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024285394,0.0001926933,0.86058956,0.00035351474,0.00012506751,0.02711308,0.040406916,0.0080618765,0.0102000935,0.0024420905,0.002296339,0.047975797],"study_design_scores_gemma":[0.000019678579,0.00010403595,0.90531576,0.000113313385,0.00007147355,0.001511268,0.07233393,0.0034254082,0.0014198497,0.00035201054,0.015275533,0.00005781236],"about_ca_topic_score_codex":0.948762,"about_ca_topic_score_gemma":0.9861078,"teacher_disagreement_score":0.051238,"about_ca_system_score_codex":0.011237458,"about_ca_system_score_gemma":0.0101962695,"threshold_uncertainty_score":0.10307944},"labels":[],"label_agreement":null},{"id":"W7161834671","doi":"10.82308/33906","title":"Earthquake source inversion and crustal structure imaging of the Charlevoix seismic zone, eastern Canada","year":2022,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismotectonics; Quaternary; Urban environment; Fold and thrust belt","score_opus":0.00479569575162855,"score_gpt":0.17970112929786988,"score_spread":0.17490543354624133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161834671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9835751,0.00026678186,0.004137328,0.00020962849,0.000018857121,0.000047561167,0.0028932455,0.0005546262,0.008296809],"genre_scores_gemma":[0.9874792,0.00023806722,0.0042786924,0.000029232948,0.0000058225737,0.0000110419305,0.0021773998,0.00005017786,0.005730492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998708,0.0000034256395,0.0000034485977,0.000020182892,0.000059501617,0.000042644464],"domain_scores_gemma":[0.9998406,0.000010829214,0.000008517557,0.00000685037,0.000105996485,0.000027289732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014196217,0.00041871602,0.00024921162,0.001368067,0.0005988525,0.0008513915,0.0006302287,0.00030352533,0.0021099509],"category_scores_gemma":[0.00052976975,0.0002282441,0.00023023873,0.0015335697,0.00025763622,0.00022188557,0.00040883975,0.00034765308,0.00033472312],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012328641,0.00043307018,0.33100614,0.00040101557,0.00027012103,0.0020889097,0.0025246285,0.13003258,0.20532148,0.004261794,0.011335069,0.31109238],"study_design_scores_gemma":[0.0001048875,0.000043304524,0.79741955,0.00005532567,0.00007395349,0.00016446228,0.0013885804,0.1806503,0.012611684,0.00037311934,0.007046974,0.00006794007],"about_ca_topic_score_codex":0.9595271,"about_ca_topic_score_gemma":0.9762274,"teacher_disagreement_score":0.040472925,"about_ca_system_score_codex":0.0045309993,"about_ca_system_score_gemma":0.011304625,"threshold_uncertainty_score":0.08142251},"labels":[],"label_agreement":null},{"id":"W7161840911","doi":"10.82308/49808","title":"Fault zone geometrical complexity and material contrast on earthquake rupture propagation: Observation and modeling","year":2021,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Induced seismicity; Fault (geology); Extensional definition; Seismic hazard; Seismotectonics; Seismic gap; Transform fault","score_opus":0.05096205257066404,"score_gpt":0.2517973323047199,"score_spread":0.20083527973405585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161840911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934969,0.00010007064,0.004211083,0.00009557044,0.00000336965,0.000010233571,0.00017165102,0.000039892228,0.0018712997],"genre_scores_gemma":[0.99866223,0.00012402004,0.0008651177,0.000005109354,0.0000030142373,0.000004566915,0.00005882875,0.0000044602334,0.00027269492],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999193,0.000015130261,0.0000058181845,0.000024764277,0.000014535277,0.00002044395],"domain_scores_gemma":[0.9997372,0.00012902798,0.000064784625,0.0000233958,0.000023819593,0.000021735817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017028658,0.00033190835,0.00025170893,0.0005012309,0.00023163407,0.00077616464,0.00054882804,0.0008253775,0.0008159478],"category_scores_gemma":[0.00092883734,0.00035493865,0.00039073348,0.00056663965,0.00048622504,0.00059772463,0.00043666083,0.00032413195,0.00010640675],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025787815,0.000063924505,0.042380065,0.000029645102,0.000022430497,0.00012895212,0.00008904134,0.9473885,0.0033709372,0.0011880085,0.0001228126,0.0051898765],"study_design_scores_gemma":[0.000003660537,0.0000089339965,0.017612346,0.0000054128077,0.000007115022,0.00001652586,0.00003246858,0.981811,0.0002167924,0.00016561715,0.00011363632,0.0000064611854],"about_ca_topic_score_codex":0.05748934,"about_ca_topic_score_gemma":0.03690531,"teacher_disagreement_score":0.05748934,"about_ca_system_score_codex":0.00091169897,"about_ca_system_score_gemma":0.00061017403,"threshold_uncertainty_score":0.11430943},"labels":[],"label_agreement":null},{"id":"W7161965355","doi":"10.82308/6914","title":"Earthquake dynamic triggering in western Quebec seismic zone","year":2019,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic zone; Western europe; Statistical analysis; Aftershock","score_opus":0.009677467327346728,"score_gpt":0.22851201502214338,"score_spread":0.21883454769479666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161965355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856231,0.00028866724,0.00041720073,0.0002483631,0.000014817605,0.00004044425,0.006665231,0.000047706264,0.006654526],"genre_scores_gemma":[0.9930373,0.00011345025,0.00028086707,0.000040818686,0.0000035822145,0.000017608265,0.002526824,0.000007260833,0.0039723055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998417,0.0000119633,0.000008733253,0.00003651077,0.000047151087,0.00005390007],"domain_scores_gemma":[0.99918455,0.00006912137,0.00012463258,0.00003267922,0.00046528314,0.0001237927],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002259782,0.00021775487,0.00022861651,0.0011402278,0.0009839175,0.00090203225,0.0005186561,0.0003169943,0.0042597535],"category_scores_gemma":[0.0011982848,0.00013472812,0.00017680245,0.0017589487,0.000351419,0.00018743677,0.00040613263,0.00026892067,0.000308903],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024371051,0.00003706887,0.9483942,0.0000991118,0.000101680016,0.00039862865,0.0011214522,0.009302735,0.0038559502,0.0006479898,0.0072098905,0.028587637],"study_design_scores_gemma":[0.000005656608,0.000010144105,0.993437,0.000019726076,0.0000142117915,0.00001920678,0.00052312185,0.0036212879,0.00016698499,0.000021941569,0.0021513405,0.000009336531],"about_ca_topic_score_codex":0.9936685,"about_ca_topic_score_gemma":0.9973236,"teacher_disagreement_score":0.014083186,"about_ca_system_score_codex":0.014083186,"about_ca_system_score_gemma":0.009729202,"threshold_uncertainty_score":0.10218114},"labels":[],"label_agreement":null},{"id":"W7161995908","doi":"10.82308/50536","title":"Uncovering Hidden Seismic Risks: Paleoseismic Insights in Québec's Intraplate Seismic Zones","year":2024,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismic exploration; Population; Seismic survey; Numerical modeling; Geophysical imaging","score_opus":0.016397988347353707,"score_gpt":0.2396087070648619,"score_spread":0.2232107187175082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161995908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.957669,0.0015362529,0.0037438422,0.0021247654,0.000015168195,0.000044124514,0.004189167,0.000051264866,0.030626412],"genre_scores_gemma":[0.99432147,0.00038271508,0.0010082565,0.00006808104,0.0000058993187,0.000008760226,0.00081257796,0.000010637788,0.0033814437],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998287,0.000020597277,0.000006807819,0.00002981555,0.000057887108,0.00005615278],"domain_scores_gemma":[0.99909484,0.00017585029,0.00013619589,0.000051845003,0.00042721865,0.00011403187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037714824,0.00025322736,0.00020525766,0.0032240988,0.0012530294,0.0019250526,0.00057867,0.00048243892,0.004499294],"category_scores_gemma":[0.0020713531,0.00014990842,0.00014918645,0.0038570154,0.00097574457,0.0005942658,0.00090492127,0.00054476055,0.00024354148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013506401,0.000039858383,0.8591278,0.00013772122,0.00013319252,0.0007556053,0.009127701,0.013543774,0.0029612174,0.0126015255,0.004414009,0.09702245],"study_design_scores_gemma":[0.000004261567,0.000008381786,0.967818,0.00011740476,0.00003426665,0.0000853462,0.005332764,0.014447907,0.00020842259,0.0017663117,0.010153779,0.000023198936],"about_ca_topic_score_codex":0.97573483,"about_ca_topic_score_gemma":0.99048513,"teacher_disagreement_score":0.02426517,"about_ca_system_score_codex":0.010771461,"about_ca_system_score_gemma":0.008410846,"threshold_uncertainty_score":0.078152835},"labels":[],"label_agreement":null},{"id":"W7161999893","doi":"10.82308/21459","title":"Human Induced Earthquakes, Naturally Triggered Seismicity, and Their Interactions","year":2021,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Fault (geology); Remotely triggered earthquakes; Microseism; Hydraulic fracturing; Sedimentary rock; San andreas fault; Basement","score_opus":0.023837419901062643,"score_gpt":0.2585891021432537,"score_spread":0.23475168224219106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7161999893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98623616,0.0009482517,0.0017551963,0.00046317876,0.000027730786,0.000024993518,0.00035057022,0.00002265653,0.010171302],"genre_scores_gemma":[0.9983664,0.00050840905,0.00029199684,0.000041130326,0.000022452263,0.000009058307,0.00009325607,0.0000023067919,0.00066491455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975604,0.000075102886,0.0000142331355,0.000051161187,0.00005233914,0.00005123775],"domain_scores_gemma":[0.99928695,0.00023671406,0.00032022188,0.000039524195,0.000060896484,0.000055775698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025561205,0.0001402015,0.00009412686,0.00052147947,0.00035316392,0.00065224007,0.00016374847,0.000337221,0.0017984529],"category_scores_gemma":[0.0013102419,0.000119733675,0.000106593514,0.0004969223,0.00063224806,0.00041750062,0.00059670204,0.00024727202,0.00012474754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001998481,0.0002146201,0.8840308,0.0002797914,0.00018202241,0.0014997766,0.0044966727,0.006042045,0.0060578254,0.016730826,0.004103177,0.07616262],"study_design_scores_gemma":[0.00000775125,0.00010587799,0.97930497,0.00004513017,0.000022687658,0.00042710238,0.004081248,0.002540632,0.000496622,0.004351217,0.008590923,0.000025793628],"about_ca_topic_score_codex":0.005822107,"about_ca_topic_score_gemma":0.011527112,"teacher_disagreement_score":0.005822107,"about_ca_system_score_codex":0.00074092386,"about_ca_system_score_gemma":0.00036136518,"threshold_uncertainty_score":0.011576474},"labels":[],"label_agreement":null},{"id":"W7162026926","doi":"10.82308/2874","title":"Double-difference earthquake relocation of Charlevoix seismicity, Eastern Canada and implication for regional geological structures","year":2014,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Intraplate earthquake; Hypocenter; Interplate earthquake; Seismometer; Earthquake location; Fault (geology); Seismic gap; Earthquake scenario; Seismic hazard; Foreshock","score_opus":0.02423993022491902,"score_gpt":0.2377967809291013,"score_spread":0.2135568507041823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7162026926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99166846,0.00022360552,0.0010032128,0.00020335024,0.000009352425,0.00001887682,0.0009473536,0.000047668873,0.0058780243],"genre_scores_gemma":[0.99571794,0.00014043144,0.001304126,0.000013972094,0.0000014363831,0.000003596625,0.0005111416,0.0000083943005,0.0022990087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975556,0.000010624061,0.000008539377,0.000059647526,0.000102778904,0.00006287603],"domain_scores_gemma":[0.9989243,0.000081050246,0.00012738086,0.000041173334,0.0007047118,0.00012129453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026353967,0.00019477728,0.000121790166,0.00087618496,0.0010083661,0.0012156513,0.0004332006,0.00017924643,0.0011264548],"category_scores_gemma":[0.0016709898,0.000104551254,0.000114123686,0.0017346612,0.00039590625,0.00021932741,0.00037774973,0.0002957103,0.00012117123],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001847671,0.00004162693,0.9070715,0.00007951222,0.000049606802,0.0006228036,0.0025248334,0.0070262193,0.0069075087,0.0029354992,0.0033063476,0.069249794],"study_design_scores_gemma":[0.0000044779767,0.000012202204,0.9806558,0.00002059111,0.000016667827,0.00008851749,0.0030871003,0.010785865,0.0013225462,0.00017770068,0.003812042,0.000016499209],"about_ca_topic_score_codex":0.95499986,"about_ca_topic_score_gemma":0.97672504,"teacher_disagreement_score":0.045000136,"about_ca_system_score_codex":0.006075089,"about_ca_system_score_gemma":0.008888524,"threshold_uncertainty_score":0.09053028},"labels":[],"label_agreement":null},{"id":"W7162129424","doi":"10.82308/41110","title":"Shallow, old and hydrologically inactive fault zones in the Appalachian orogen","year":2013,"lang":"en","type":"dissertation","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Groundwater; Groundwater flow; Hydrology (agriculture); MODFLOW; Aquifer; Groundwater model; Surface water; Subsurface flow; Fault (geology)","score_opus":0.012512136974095877,"score_gpt":0.219151613777498,"score_spread":0.20663947680340214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7162129424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993605,0.000058881342,0.000056362496,0.000009335717,3.4476975e-7,0.0000072609764,0.00007445052,0.000002282405,0.00043053663],"genre_scores_gemma":[0.99945825,0.0000944562,0.00016493717,0.000006993887,8.496993e-7,0.000009226931,0.00009689186,8.7342784e-7,0.00016754173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997881,0.000025306166,0.000012943862,0.0000684953,0.00003176191,0.00007343521],"domain_scores_gemma":[0.9997662,0.000054274802,0.00007745969,0.000014055589,0.00006258542,0.000025483347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016985685,0.00021595086,0.00026005972,0.0012439566,0.0010257493,0.00095817854,0.00035252413,0.00022597023,0.00042249818],"category_scores_gemma":[0.0005320741,0.00016929448,0.00014187326,0.0019247358,0.0010502487,0.00031712643,0.0006001524,0.00013180172,0.00005534328],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000117387695,0.00003257343,0.9756512,0.00006004131,0.00004286979,0.00088481966,0.0037124108,0.0014068373,0.0054683858,0.00025415685,0.00007574184,0.012293617],"study_design_scores_gemma":[0.000003875982,0.000015535883,0.99645776,0.000011920094,0.000015740918,0.00007645791,0.0018528347,0.0010460851,0.00017931499,0.000051491934,0.00028144478,0.0000074960803],"about_ca_topic_score_codex":0.65045065,"about_ca_topic_score_gemma":0.8290918,"teacher_disagreement_score":0.65045065,"about_ca_system_score_codex":0.0027694139,"about_ca_system_score_gemma":0.0017009953,"threshold_uncertainty_score":0.70321584},"labels":[],"label_agreement":null},{"id":"W7164326838","doi":"10.67165/gsvrjvrx","title":"Episodic tremor and slip: The Case of the Mystery Earthquakes | Lessons on Plate Tectonics","year":2022,"lang":"","type":"article","venue":"","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Plate tectonics; Episodic tremor and slip; Oceanic crust; Tectonics; North American Plate; Crust; Slip (aerodynamics); Global Positioning System","score_opus":0.028470796652093452,"score_gpt":0.2326519434242929,"score_spread":0.20418114677219945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7164326838","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.10228216,0.026280934,0.0026377277,0.7532462,0.0051475028,0.000029170846,0.00017807522,0.000118554904,0.11007977],"genre_scores_gemma":[0.81060934,0.03922024,0.0036929632,0.05490253,0.0076468657,0.0000531085,0.00017368709,0.00023020952,0.08347101],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99925417,0.00035529063,0.00002924515,0.00007531235,0.0001380473,0.0001478298],"domain_scores_gemma":[0.9964954,0.002020758,0.0002841137,0.00021707993,0.00031324595,0.00066938705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015058574,0.00047534247,0.00038479175,0.00078754546,0.0036526013,0.0037507121,0.001239489,0.0053283074,0.006045201],"category_scores_gemma":[0.008415253,0.00045164264,0.00043103984,0.0006470072,0.006159988,0.0077659613,0.002331942,0.0073171756,0.00089063693],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009367084,0.00014285768,0.01963158,0.00030629552,0.000073614436,0.020421663,0.09815022,0.0011610743,0.00039409375,0.14748912,0.6212227,0.090913065],"study_design_scores_gemma":[0.000045930956,0.000067290435,0.01473234,0.0010190058,0.000030979365,0.013535694,0.14057021,0.0012831996,0.00021691583,0.18546852,0.64294904,0.00008085162],"about_ca_topic_score_codex":0.019842144,"about_ca_topic_score_gemma":0.04946044,"teacher_disagreement_score":0.019842144,"about_ca_system_score_codex":0.0029119262,"about_ca_system_score_gemma":0.0013491156,"threshold_uncertainty_score":0.039453328},"labels":[],"label_agreement":null},{"id":"W760034925","doi":"10.1007/s00445-015-0951-x","title":"Facies distribution of ejecta in analog tephra rings from experiments with single and multiple subsurface explosions","year":2015,"lang":"en","type":"article","venue":"Bulletin of Volcanology","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"University at Buffalo; Ministry of Business, Innovation and Employment; National Science Foundation","keywords":"Ejecta; Impact crater; Geology; Tephra; Facies; Volcano; Petrology; Clastic rock; Geochemistry; Geomorphology; Sedimentary rock; Astrobiology; Astronomy; Supernova","score_opus":0.03557422034105363,"score_gpt":0.2134165930496978,"score_spread":0.17784237270864417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W760034925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989542,0.000043340286,0.0002158854,0.000002577679,0.0000018035508,0.0000042693446,0.00026792684,0.000012239643,0.0004977573],"genre_scores_gemma":[0.9985121,0.00004489012,0.00026259533,0.0000054803836,0.0000019733575,0.0000068081,0.00040392712,0.000016759883,0.00074534526],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993825,0.000008101758,0.000005752254,0.000022395114,0.000011639005,0.000013889698],"domain_scores_gemma":[0.99932384,0.0002495203,0.00009448367,0.00008731414,0.00011218908,0.00013264743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014597486,0.0001874527,0.00016613571,0.00076986314,0.0002578945,0.00027808317,0.0002551577,0.0002846053,0.0024636397],"category_scores_gemma":[0.0005259158,0.00021703953,0.00017753984,0.00027981214,0.00025120642,0.00026018496,0.000328866,0.00030149493,0.0002980164],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.006962748,0.0003509438,0.11461034,0.00009803757,0.0001781338,0.00029162012,0.00046187147,0.002126278,0.8556081,0.00023088178,0.00019589113,0.01888514],"study_design_scores_gemma":[0.000027337184,0.00033916568,0.96052337,0.000004729416,0.00006711815,0.00023310672,0.00014915316,0.0011507755,0.03719241,0.00004769813,0.00025457318,0.000010533234],"about_ca_topic_score_codex":0.0022262512,"about_ca_topic_score_gemma":0.002517169,"teacher_disagreement_score":0.0024636397,"about_ca_system_score_codex":0.00014660382,"about_ca_system_score_gemma":0.0000659605,"threshold_uncertainty_score":0.008241713},"labels":[],"label_agreement":null},{"id":"W83648095","doi":"","title":"Episodic Seismicity from Near Surface to Base of the Crust","year":2010,"lang":"en","type":"article","venue":"EGUGA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of New Brunswick","funders":"","keywords":"Geology; Crust; Seismology; Induced seismicity; Geophysics","score_opus":0.012295754633871801,"score_gpt":0.20102738569198011,"score_spread":0.1887316310581083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W83648095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99553126,0.00009182823,0.00017377229,0.00003470213,0.000006620415,0.0000032596756,0.0007513707,0.000013671924,0.0033935502],"genre_scores_gemma":[0.9990576,0.0000743785,0.00008608151,0.000005420001,0.000009206798,0.0000014151517,0.00034610403,0.0000024119604,0.00041739971],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993384,0.0000088146135,0.000006193693,0.00001770546,0.000015668062,0.000017788918],"domain_scores_gemma":[0.99968195,0.00004587723,0.000081606195,0.000027658101,0.000087976776,0.00007496873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010388017,0.00012022747,0.00016455847,0.001104925,0.00048003264,0.0005329806,0.00019105148,0.00020118919,0.0014634765],"category_scores_gemma":[0.0009085923,0.00011561224,0.00009230997,0.0010162571,0.00024869226,0.0004354807,0.0007058958,0.00023477447,0.00018495995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018643885,0.00004294289,0.95573115,0.00007820985,0.000070923445,0.00037924194,0.0035723688,0.001306218,0.008534543,0.0006328664,0.0011736827,0.028291352],"study_design_scores_gemma":[0.0000015589247,0.000030204857,0.9980375,0.0000071242107,0.000012865497,0.00007859652,0.0005438464,0.00024776545,0.00018147561,0.000048817838,0.00080752146,0.0000027732087],"about_ca_topic_score_codex":0.033051725,"about_ca_topic_score_gemma":0.10883738,"teacher_disagreement_score":0.033051725,"about_ca_system_score_codex":0.0003811478,"about_ca_system_score_gemma":0.00031814116,"threshold_uncertainty_score":0.06571871},"labels":[],"label_agreement":null},{"id":"W84630796","doi":"10.3133/ofr02328","title":"The Cascadia Subduction Zone and related subduction systems: Seismic structure, intraslab earthquakes and processes, and earthquake hazards","year":2002,"lang":"en","type":"article","venue":"Antarctica A Keystone in a Changing World","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Geological Survey of Canada","funders":"U.S. Geological Survey; Oregon State University; National Science Foundation","keywords":"Subduction; Geology; Seismology; Slab; Geological survey; Lithosphere; Geophysics; Tectonics","score_opus":0.010138546774065216,"score_gpt":0.19756978577935247,"score_spread":0.18743123900528724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W84630796","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.69973207,0.09479097,0.0013572545,0.026202977,0.0005421877,0.000101043726,0.0084735835,0.00009021054,0.16870974],"genre_scores_gemma":[0.91831636,0.042052153,0.0005133747,0.0003692709,0.0003237338,0.000028745178,0.0032926837,0.000021275438,0.03508244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991536,0.000023528368,0.000004537355,0.000012158537,0.000023395327,0.000021006324],"domain_scores_gemma":[0.9996101,0.00006096104,0.00007184748,0.0000103807615,0.00010512531,0.00014158696],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015673587,0.00025945518,0.00012152253,0.0014580216,0.00073801563,0.001164768,0.00025442455,0.00031189065,0.0064025833],"category_scores_gemma":[0.00072206877,0.00013260625,0.0000648152,0.0049256557,0.0008374183,0.00052728516,0.00078018825,0.00035266177,0.00047600808],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014969324,0.000058074125,0.7006441,0.00039503697,0.00010356811,0.0004724174,0.00601641,0.0020782272,0.0012484333,0.013175037,0.10816433,0.16749474],"study_design_scores_gemma":[0.00000669315,0.000024815005,0.8818887,0.000086228974,0.00002049718,0.0001395259,0.004344131,0.00021567185,0.00004317458,0.0023270382,0.11089626,0.0000072311846],"about_ca_topic_score_codex":0.26281503,"about_ca_topic_score_gemma":0.57971084,"teacher_disagreement_score":0.26281503,"about_ca_system_score_codex":0.0020260534,"about_ca_system_score_gemma":0.0022520819,"threshold_uncertainty_score":0.52257055},"labels":[],"label_agreement":null},{"id":"W8468346","doi":"10.1007/978-3-642-55463-6_14","title":"The Osmussaar Breccia in Northwestern Estonia — Evidence of a ~475 Ma Earthquake or an Impact?","year":2003,"lang":"en","type":"book-chapter","venue":"Impact studies","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Breccia; Geology; Geochemistry; Tectonics; Impact structure; Clastic rock; Paleontology; Geomorphology; Seismology; Sedimentary rock; Impact crater","score_opus":0.0962635143845526,"score_gpt":0.3405884622903048,"score_spread":0.2443249479057522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W8468346","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8944226,0.014468786,0.0003415174,0.0011480915,0.00021378545,0.00001942632,0.0013151027,0.000043947886,0.08802673],"genre_scores_gemma":[0.96726793,0.00612312,0.00044057798,0.0002505853,0.000034889716,0.0000146573875,0.0015339672,0.00002760622,0.02430667],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991083,0.000007928837,0.00001100027,0.00001580407,0.000016718534,0.00003772405],"domain_scores_gemma":[0.99992454,0.00001165952,0.000033250944,0.0000069739526,0.000014716358,0.000008940652],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016590222,0.00026815105,0.0002599209,0.00096541544,0.00092828803,0.0012852908,0.0004393937,0.00048224028,0.0025994675],"category_scores_gemma":[0.0004024288,0.00022529237,0.00015825397,0.0020267593,0.0007923968,0.00059510523,0.0009248653,0.00032371443,0.0004430058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094278046,0.00012867368,0.52350086,0.0018408897,0.00035519173,0.02460962,0.035249997,0.007541478,0.022472294,0.02195094,0.03242806,0.32897922],"study_design_scores_gemma":[0.000011816412,0.000030223799,0.9504046,0.00025574164,0.00002900212,0.0008434418,0.0043423,0.000281693,0.00041023555,0.00027731256,0.04310036,0.000013307346],"about_ca_topic_score_codex":0.24133904,"about_ca_topic_score_gemma":0.5438439,"teacher_disagreement_score":0.24133904,"about_ca_system_score_codex":0.0018069786,"about_ca_system_score_gemma":0.0015213456,"threshold_uncertainty_score":0.47986853},"labels":[],"label_agreement":null},{"id":"W88590308","doi":"10.3133/ofr01408","title":"Report for borehole explosion data acquired in the 1999 Los Angeles Region Seismic Experiment (LARSE II), Southern California: Part I, description of the survey","year":2001,"lang":"en","type":"article","venue":"Antarctica A Keystone in a Changing World","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"U.S. Forest Service; California Department of Parks and Recreation; California State University, Northridge; Southern California Gas Company; Australian Government","keywords":"Geology; Seismology; Sedimentary basin; Structural basin; Tectonics; Seismic hazard; Geological survey; Borehole; Thrust fault; Sedimentary rock; Paleoseismology; Fault (geology); Geomorphology; Paleontology","score_opus":0.09863168064259346,"score_gpt":0.27668972687917776,"score_spread":0.17805804623658428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W88590308","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.038815517,0.00022999794,0.0010651124,0.00030232282,0.00026065687,0.00039376068,0.9444546,0.0006850693,0.013793002],"genre_scores_gemma":[0.048776977,0.00031466753,0.0036355415,0.0001880963,0.00009855668,0.00065163674,0.9335727,0.00017865807,0.012583252],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99902,0.000051045863,0.00010391214,0.00015738865,0.0005763762,0.00009122171],"domain_scores_gemma":[0.9959045,0.00037582524,0.00070667855,0.00044073138,0.0023433971,0.00022890413],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012591891,0.000768551,0.00038940652,0.0032142513,0.0006584423,0.0011146442,0.0007242734,0.00053438643,0.01343125],"category_scores_gemma":[0.0026346142,0.0003245234,0.00022128639,0.0026364506,0.00016623475,0.0008939685,0.000798529,0.00062445475,0.009721785],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005107439,0.00050827884,0.18448845,0.0003917307,0.00012991224,0.000384077,0.0003508052,0.0006444894,0.0030006089,0.00051044486,0.7634141,0.045666356],"study_design_scores_gemma":[0.00012831042,0.00017015287,0.6940371,0.00010190898,0.000072705036,0.00022956172,0.00064617826,0.0006060005,0.0017773879,0.00017645712,0.30200288,0.00005140889],"about_ca_topic_score_codex":0.05298619,"about_ca_topic_score_gemma":0.088325486,"teacher_disagreement_score":0.05298619,"about_ca_system_score_codex":0.00085033715,"about_ca_system_score_gemma":0.0011896738,"threshold_uncertainty_score":0.10535556},"labels":[],"label_agreement":null},{"id":"W9119232","doi":"10.1007/s10040-009-0440-4","title":"Compartmented flow at the Bátaapáti site in Hungary","year":2009,"lang":"en","type":"article","venue":"Hydrogeology Journal","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Golder Associates (Canada)","funders":"Nationale Genossenschaft für die Lagerung radioaktiver Abfälle","keywords":"Hydrogeology; Geology; Hydraulic conductivity; Rock mass classification; Hydraulic head; Matrix (chemical analysis); Petrology; Geotechnical engineering; Soil science; Soil water; Materials science","score_opus":0.013783933647874655,"score_gpt":0.21993079612791258,"score_spread":0.20614686248003794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W9119232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992429,0.000013163922,0.000046272486,0.000011409135,0.0000029891307,0.0000029998628,0.0002558144,0.000010217851,0.00041429233],"genre_scores_gemma":[0.9996414,0.000010004036,0.000032975488,0.000002479689,0.00000180896,0.0000016867843,0.0001531384,0.0000014856745,0.0001550015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998913,0.000009769312,0.000006276136,0.000026725509,0.000016805552,0.00004908809],"domain_scores_gemma":[0.99989057,0.000016346861,0.000017749375,0.0000073467277,0.000021083373,0.000046892394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006747909,0.00009853254,0.00038805816,0.00049319415,0.00035466603,0.0007270288,0.0003782526,0.00038319168,0.0017189917],"category_scores_gemma":[0.00025459466,0.00012924561,0.00014836606,0.0006339188,0.0005263867,0.00032020514,0.00042037078,0.0001694127,0.00019377624],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023778693,0.0003939581,0.91156626,0.0001494001,0.0001892211,0.009781491,0.0035782277,0.00930835,0.03391594,0.0025568125,0.0017425464,0.024439944],"study_design_scores_gemma":[0.000041615287,0.000053162996,0.99532926,0.0000086494365,0.000015599007,0.00020877052,0.0009957525,0.00199729,0.0007306152,0.00010425052,0.0005045884,0.00001036673],"about_ca_topic_score_codex":0.04253677,"about_ca_topic_score_gemma":0.03238192,"teacher_disagreement_score":0.04253677,"about_ca_system_score_codex":0.0010329561,"about_ca_system_score_gemma":0.001010696,"threshold_uncertainty_score":0.084578335},"labels":[],"label_agreement":null},{"id":"W916226211","doi":"","title":"Near Field Dynamic, Co-seismic and Post-seismic Deformations Associated with the 2013, M7.8, and 2003, M7.6, South Scotia Ridge Earthquakes Observed with GPS","year":2014,"lang":"en","type":"article","venue":"Open Repository and Bibliography (University of Luxembourg)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Global Positioning System; Ridge; Nova scotia; Field (mathematics); Geodesy; Paleontology; Engineering; Oceanography; Telecommunications","score_opus":0.009822999098703262,"score_gpt":0.17911990831292585,"score_spread":0.16929690921422258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W916226211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965431,0.00002830278,0.00003823414,0.000024742594,0.000006047489,0.000010024464,0.002207774,0.000010574997,0.0011311782],"genre_scores_gemma":[0.99634945,0.000049226623,0.00011983222,0.000017379249,0.0000085840275,0.000010570231,0.002461363,0.0000035258317,0.0009801239],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999194,0.0000039046477,0.0000036177305,0.000015020725,0.000030880663,0.000027160839],"domain_scores_gemma":[0.9997502,0.000011562422,0.000050826988,0.000012778786,0.000096015545,0.00007861074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000093968934,0.00018705774,0.00017697617,0.0007119827,0.00043648313,0.00027965292,0.0002587309,0.00028950404,0.0009239084],"category_scores_gemma":[0.00035372496,0.0001227435,0.0001374854,0.0010338445,0.00025538818,0.00009376511,0.0003205836,0.00022381036,0.00027665676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060739473,0.00013969785,0.9560443,0.000071719274,0.00007104418,0.0015183805,0.0013309503,0.002513455,0.020096416,0.00015766201,0.0053609656,0.012087986],"study_design_scores_gemma":[0.0000032118571,0.000013063144,0.9991959,0.0000028635175,0.000002485607,0.000039959534,0.00015229624,0.00025789472,0.0000703313,0.000005040163,0.0002551258,0.0000018365422],"about_ca_topic_score_codex":0.33343711,"about_ca_topic_score_gemma":0.63069934,"teacher_disagreement_score":0.33343711,"about_ca_system_score_codex":0.0010169452,"about_ca_system_score_gemma":0.0007832812,"threshold_uncertainty_score":0.6629926},"labels":[],"label_agreement":null},{"id":"W95154854","doi":"10.1007/1-4020-3331-1_11","title":"Distribution of Cumulative Tsunami Energy from Alaska-Aleutians to Western Canada","year":2005,"lang":"en","type":"book-chapter","venue":"Advances in natural and technological hazards research","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Peninsula; Seismology; Geology; Trench; Geography; Physical geography; Archaeology","score_opus":0.023661768644293805,"score_gpt":0.2885898620951616,"score_spread":0.26492809345086776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W95154854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95960855,0.0008335171,0.0003439969,0.00015172534,0.000011900719,0.00001652984,0.017703667,0.00008257491,0.021247583],"genre_scores_gemma":[0.9726704,0.0010967375,0.0003213921,0.00003413589,0.0000050990766,0.0000104706705,0.00813291,0.000021493848,0.017707316],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998808,0.000005398369,0.0000096240465,0.000024854555,0.0000446745,0.00003459824],"domain_scores_gemma":[0.9990152,0.000109792236,0.00011356742,0.00002206717,0.00059862406,0.00014063965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000167244,0.00017388469,0.00014358878,0.002328241,0.0007552811,0.0008121518,0.00046006902,0.00017753511,0.004479128],"category_scores_gemma":[0.0010852029,0.00013264646,0.00020399509,0.0036371907,0.00030681616,0.0002657535,0.0003612567,0.0002229397,0.00041790973],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001422448,0.000016366506,0.9433963,0.00007564815,0.00011346445,0.0003788303,0.0020175593,0.006780928,0.0012220748,0.002878878,0.010416622,0.032561176],"study_design_scores_gemma":[0.0000038570392,0.000009034705,0.98803663,0.000035215282,0.000022587377,0.00014277226,0.002949573,0.0019888459,0.00027499377,0.00018815143,0.006327855,0.000020497175],"about_ca_topic_score_codex":0.9794587,"about_ca_topic_score_gemma":0.98747474,"teacher_disagreement_score":0.02054131,"about_ca_system_score_codex":0.006378283,"about_ca_system_score_gemma":0.005853081,"threshold_uncertainty_score":0.04627788},"labels":[],"label_agreement":null},{"id":"W95268571","doi":"","title":"Induced seismicity risk in Irani oil and gas fields","year":2008,"lang":"en","type":"article","venue":"The 42nd U.S. Rock Mechanics Symposium (USRMS)","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Induced seismicity; Geomechanics; Geology; Context (archaeology); Structural basin; Seismology; Natural gas field; Oil field; Sedimentary rock; Natural gas; Geomorphology; Geochemistry; Paleontology; Geotechnical engineering","score_opus":0.01727021241978658,"score_gpt":0.1987488187735031,"score_spread":0.18147860635371652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W95268571","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996916,0.000015305024,0.00003635122,0.000010866112,6.230087e-7,0.0000020881607,0.00004753756,0.0000019759073,0.00019366],"genre_scores_gemma":[0.999721,0.00003031111,0.000034408855,0.0000022523855,0.0000018261852,0.0000017346988,0.00013208365,4.049821e-7,0.00007599087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987936,0.000018727944,0.000009955758,0.000018964702,0.000034499975,0.000038422153],"domain_scores_gemma":[0.99954635,0.00007400858,0.0002133789,0.00002278802,0.000082235005,0.00006125576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017833489,0.00013587091,0.00012720135,0.0010602231,0.00017874397,0.00024102587,0.0001201736,0.00015838048,0.00050315855],"category_scores_gemma":[0.001016171,0.00008588436,0.00009698232,0.0006973101,0.00016449855,0.00022648166,0.0002475841,0.00010979906,0.00006798378],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013453921,0.000075688404,0.98373944,0.000011238335,0.000016661123,0.00032002263,0.00028193457,0.0027522075,0.002284471,0.00015341022,0.00016260019,0.0100677125],"study_design_scores_gemma":[0.0000034853476,0.00005403396,0.9976714,0.000002176462,0.0000044048584,0.00008530605,0.00021517703,0.0015580016,0.0002143271,0.000050418774,0.00013895164,0.000002448647],"about_ca_topic_score_codex":0.011258873,"about_ca_topic_score_gemma":0.018611146,"teacher_disagreement_score":0.011258873,"about_ca_system_score_codex":0.000646895,"about_ca_system_score_gemma":0.0003363119,"threshold_uncertainty_score":0.02238667},"labels":[],"label_agreement":null},{"id":"W98506830","doi":"","title":"Fault geometries and deformation mechanisms in the evolution of low-angle normal faults (Kea, Greece)","year":2009,"lang":"en","type":"article","venue":"EGUGA","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Boulevard; Structural geology; Sedimentology; Geology; Fault (geology); Archaeology; Seismology; Geography; Geomorphology","score_opus":0.008246711353092382,"score_gpt":0.19688381040444558,"score_spread":0.1886370990513532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W98506830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985104,0.00007420496,0.0000887532,0.000018414737,7.1489103e-7,0.0000018381534,0.00008683335,0.000004151925,0.001214717],"genre_scores_gemma":[0.9996344,0.000035714507,0.000063713305,0.0000011957233,4.6998377e-7,5.6728186e-7,0.000057593454,0.000001960396,0.00020431781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989617,0.000017544495,0.000016038555,0.000031745956,0.00001802024,0.000020472155],"domain_scores_gemma":[0.99943286,0.00012493992,0.00021126233,0.0000431645,0.00012547607,0.000062278334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024720602,0.00011052852,0.00013556279,0.0014191915,0.0002167589,0.00068490265,0.00020132544,0.00027705135,0.0015823413],"category_scores_gemma":[0.0013454951,0.00014635408,0.00011838643,0.0012451629,0.0005129588,0.0004856754,0.000482905,0.0001451147,0.00044774843],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000242872,0.000032839387,0.9521153,0.000054950593,0.000040345785,0.00038119196,0.00081899884,0.008333268,0.011453418,0.0023843877,0.00021231,0.023929976],"study_design_scores_gemma":[0.000006284559,0.000037435653,0.9957104,0.000009946504,0.000007867403,0.00029890356,0.00039639566,0.002106598,0.00036683946,0.00069033704,0.00036267255,0.000006342808],"about_ca_topic_score_codex":0.0049160775,"about_ca_topic_score_gemma":0.0091498885,"teacher_disagreement_score":0.0049160775,"about_ca_system_score_codex":0.00047724365,"about_ca_system_score_gemma":0.00023292255,"threshold_uncertainty_score":0.009774923},"labels":[],"label_agreement":null}]}